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
27689|Aarons Pass Granite|22529|6|Mentioned|1, 8|Visean|Visean|||||||
27689|Aarons Pass Granite|22857|6|Mentioned|p231|Late Carboniferous|Early Carboniferous|||||||
27689|Aarons Pass Granite|22863|6|Mentioned|p231|||||||||
27689|Aarons Pass Granite|23043|5|Briefly described|Map Legend|Namurian|Visean|||||||
27689|Aarons Pass Granite|23170|2|Defined|p276|Carboniferous|Carboniferous|Age: Middle Carboniferous.||||||
27689|Aarons Pass Granite|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
27689|Aarons Pass Granite|32045|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
27689|Aarons Pass Granite|32046|6|Mentioned|p269|||See also p270,271||||||11-MAY-17
27689|Aarons Pass Granite|32047|4|Described|p24|||Mineralisation discussed||||||
27689|Aarons Pass Granite|32485|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
27689|Aarons Pass Granite|33004|6|Mentioned|p177|||||||||
27689|Aarons Pass Granite|33007|5|Briefly described|p12|||Genesis & history. See gold & copper P16.||||||
27689|Aarons Pass Granite|35257|6|Mentioned|Fig.24|||p128||||||11-MAY-17
27689|Aarons Pass Granite|36285|4|Described|p58|||See also Fig.2.& 3.||||||
27689|Aarons Pass Granite|39214|5|Briefly described|p25|||||||||
27689|Aarons Pass Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
27689|Aarons Pass Granite|43043|5|Briefly described|p103|||age of 320-322 Ma.||||||
27689|Aarons Pass Granite|43188|5|Briefly described|p221,Table 7 p220||Carboniferous|Rb/Sr age of 328 Ma, middle Carboniferous.||||||
27689|Aarons Pass Granite|43476|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
27689|Aarons Pass Granite|73299|6|Mentioned|p1095, p1096 Fig.3, p1098, p1101, p1108|Carboniferous|Carboniferous|Western margin of granite faulted along the Mudgee Fault against the Hill End Trough succession.||||||
69898|Abercrombie Formation|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Adaminaby Group. Includes Willigam Sandstone, Peach Tree Chert, Nattery Chert and Mummel Chert Members. Brown and buff to grey thinly to thickly bedded fine- to coarse-grained mica-quartz (+/-feldspar) sandstone, interbedded with laminated siltst.||||||09-SEP-08
69898|Abercrombie Formation|66713|4|Described|p1, p4 Fig.3, p5, p6, p10|Middle Ordovician|Early Ordovician|Predominantly fine-grained quartzofeldspathic sediments: shale, coarse quartz greywacke, hornfels, metachert, minor siliceous slate, quartzite. Hosts the Main vein system in the Phoenix W deposit. In Adaminaby Group.||||||
69898|Abercrombie Formation|67322|4|Described|p13, p14, p16-17, fig.5.|Middle Ordovician|Early Ordovician|Albury-Bega Terrane. Age based on conodonts in thin sections of chert that occur in horizons interbedded with sandstone-dominated units. Redefined by Thomas et al. (in press), incorporating several units previously recognised on the Taralga 1:100 0000 sheet by Scheibner (1973). Occurs in the Goulburn-Taralga region.||Of the Adaminaby Group.|Mummel Chert Member, Nattery Chert Member, Peach Tree Chert Member, Willigam Sandstone Member.||Turbiditic sandstones; framework grains in sandstone beds are dominated by plutonic quartz. Feldspar and lithic fragments are more common low in the Abercrombie Formation beneath the oldest chert beds.|21-FEB-18
69898|Abercrombie Formation|68466|5|Briefly described|p65-68, 70|Middle Ordovician|Early Ordovician|Albury-Bega Terrane. Photomicrographs. Apparently free of bioturbation, implying anoxic/oxygen-poor Early Ordovician deep ocean waters.|||Willigam Sandstone, Mummel Chert, Peach Tree Chert, Nattery Chert, Members.|Is overlain by Bendoc Group. Contemporaneous with Numeralla Chert.||
69898|Abercrombie Formation|68592|2|Defined|p272, p274-5, p277-8, p280, p282-319|Late Ordovician|Early Ordovician|See also p11-12, p116-8, p128-9, p202-3, p322, p324, p326, p341, p343, p350, p355, p357, p361, p363, p391, p393, p398, p425, p750, p757, p802, p1316, p1676, p1858-62. Synonymy described. Here defined to include the entire quartzose turbidite and chert sequence of the Adaminaby Group; mappable chert horizons included as Members. A composite representative section is described. Thickness probably c.2500m. Hosts Pb-Ag-Zn mineralisation at Dalton (Wallah Wallah deposit) and W at the Phoenix deposit near Frogmore (both detailed). Appears as Abercrombie Group on page xxiv. Metamorphism described; palaeontology detailed. Is intruded by Bishopthorpe Suite dykes, Gunning and Burrawinda Suites and Banshea Granite. Faulted against Rockley Volcanics.||Unit in Adaminaby Group.|Includes Nattery Chert, Peach Tree Chert, Mummel Chert, Willigam Sandstone, Members.|Unconformably/disconformably overlies Shivering Conglomerate. Is overlain conformably by Bumballa Formation or Warbisco Shale, and unconformably by Woodlawn Volcanics.|A thick sequence of fine- to very coarse-grained, thinly- to thickly-bedded quartzose sandstone with interbedded laminated siltstone and mudstone; chert bands up to several tens of metres thick.|
69898|Abercrombie Formation|69159|5|Briefly described|Map legend|Darriwilian|Lancefieldian|Also includes two un-named but separately mapped units: Oaas = black, laminated to medium-bedded, pyritic, carbonaceous shale, commonly strongly foliated and folded, minor quartzose sandstone; and Oaac = Grey, brown to khaki, medium-bedded to laminated chert interbedded with grey, massive to laminated siltstone, mudstone and fine-grained sandstone.||Unit in Adaminaby Group.|Includes Willigam Sandstone Member and Peach Tree, Nattery, Mummel, Chert Members.||Undivided: buff to brown, grey, fawn to cream, thinly- to very thickly-bedded, fine- to coarse-grained mica-quartz+/-feldspar sandstone, interbedded with laminated siltstone and mudstone. Discrete chert-rich packages occur within the Formation.|07-SEP-15
69898|Abercrombie Formation|69270|4|Described|p2 Tb.1.1, p4-15, p23|Late Ordovician|Late Ordovician|Sample dated is a massive, fine- to medium-grained, poorly-sorted feldspathic wacke, and was taken from outcrop in an abandoned quarry north of Captains Flat Road, at Mount Balcombe. Dating method: zircon U-Pb by SHRIMP, n=12. Measured age spectrum is consistent with interpretation of Stauffer (1964) and Stauffer & Rickard (1966) that this package represents a klippe of Ordovician Abercrombie Formation that has been structurally emplaced above Late Silurian Captains Flat Formation (although absence of Silurian detrital zircon in sample does not definitively rule out a Late Silurian depositional age for the host sandstone). Eastern Lachlan Orogen.|486.5+/-3.2 Ma, maximum depositional age|Adaminaby Group||a klippe of Ordovician Abercrombie Formation has been structurally emplaced above Late Silurian Captains Flat Formation; is intruded by Anembo Granodiorite; is intruded by Tinderry Granite|feldspathic and matrix-supported sandstone|
69898|Abercrombie Formation|69668|5|Briefly described|p929 Fig.2, p930 Fig.3, p931|Middle Ordovician|Early Ordovician|Goulburn-Braidwood area, Albury-Bega terrane.||Unit in Adaminaby Group.|Includes Willigam Sandstone Member; Mummel, Peach Tree, Nattery, Chert Members.|Is overlain by Bumballa Formation.|Turbiditic sandstones and cherts.|
69898|Abercrombie Formation|70192|5|Briefly described|Map Legend|Gisbornian|Lancefieldian|[Theta]aa. Includes one unnamed member of thin-medium bedded, chert and cherty mudstone interbedded with siltstone, mudstone and fine-medium grained quartzose sandstone. On Boorowa, Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.||Adaminaby Group|Includes Mummel Chert Member, Nattery Chert Member, Peach Tree Chert Member, Willigam Sandstone Member and two unnamed units.||Thinly-very thickly bedded, fine-very coarse grained, mica quartz sandstone interbedded with laminated siltstone and mudstone. Sandstone beds show normal grading and ripple cross laminations with discrete chert rich packages.|
69898|Abercrombie Formation|70540|5|Briefly described|Map Legend|Ordovician|Ordovician|||Adaminaby Group|Includes Nattery Chert Member.||Thinly-thickly bedded, fine-coarse grained mica-quartz sandstone, interbedded with laminated siltstone and mudstone, sandstone beds show normal grading and ripple cross lamination; discrete chert-rich packages.|
69898|Abercrombie Formation|70541|4|Described|Map Legend|Ordovician|Ordovician|Includes one unnamed mapped member composed of thin-medium bedded chert and cherty mudstone, interbedded with siltstone, mudstone and fine-medium grained quartz sandstone.||Adaminaby Group|Includes Mummel Chert Member, Nattery Chert Member, Peach Tree Chert Member, and one unnamed member.||Thinly-thickly bedded fine-coarse grained mica-quartz sandstone, interbedded laminated siltstone and mudstone, sandstone beds normal grading and ripple cross lamination; discrete chert-rich packages.|
69898|Abercrombie Formation|70542|5|Briefly described|Map Legend|Ordovician|Ordovician|Contains two unnamed members; one of chert and cherty mudstone that is interbedded with siltstone and one of laminated to thinly bedded siltstone and cherty mudstone.||Adaminaby Group|Includes Nattery Chert Member, Peach Tree Chert Member, Willigam Sandstone Member amd two unnamed members.||Thinly-very thickly bedded, fine-very coarse grained, mica quartz sandstone interbedded with laminated siltstone and mudstone. Sandstone beds show normal and ripple cross laminations with discrete chert rich packages.|
69898|Abercrombie Formation|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes one unnamed member of thin-medium bedded, chert and cherty mudstone interbedded with siltstone, mudstone and fine-medium grained quartzose sandstone.||Adaminaby Group|Includes Mummel Chert Member, Nattery Chert Member, Peach Tree Chert Member, Willigam Sandstone Member and one unnamed member||Thinly-very thickly bedded, fine-very coarse grained, mica quartz sandstone interbedded with laminated siltstone and mudstone. Sandstone beds show normal grading and ripple cross laminations with discrete chert rich packages.|
69898|Abercrombie Formation|70544|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes one unnamed member of brown-grey, thin-medium bedded chert and cherty mudstone interbedded with siltstone, mudstone and fine-medium grained quartzose sandstone.||Adaminaby Group|Includes Mummel Chert Member, Nattery Chert Member and one unnamed member||Thinly-very thickly bedded, fine-very coarse grained mica quartz sandstone, interbedded with laminated siltstone and mudstone; sandstone beds show normal grading and ripple cross lamination; discrete chert-rich packages.|
69898|Abercrombie Formation|70545|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes two unnamed Members; a strongly cleaved, laminated carbonaceous shale and a laminated to thinly bedded siltstone and cherty mudstone.||Adaminaby Group|Includes Nattery Chert Member.||Thinly to very thickly bedded, fine to very coarse grained mica quartz sandstone interbedded with laminated siltstone and mudstone. Sandstone beds show normal grading and ripple cross lamination; discrete chert rich packages.|20-SEP-17
69898|Abercrombie Formation|70546|5|Briefly described|Map Legend|Ordovician|Ordovician|||Adaminaby Group|||Thinly to very thickly bedded, fine to very coarse grained, mica quartz sandstone interbedded with laminated siltstone and mudstone; sandstone beds show normal grading and ripple cross lamination with discrete chert rich packages.|
69898|Abercrombie Formation|70661|6|Mentioned|p7|||||Adaminaby Group|Nattery Chert Member|||
69898|Abercrombie Formation|71069|3|Fully described|p19, p21-p23, p33, p39 fig 16|Gisbornian|Lancefieldian|Name derived from the Abercrombie River. Previously referred to as the Abercrombie Beds. Incorporates rocks that were previously assigned to the Jerrawa Beds, Bendoc, Margules and Douro Groups. Outcrop of this unit is low, blocky or rubbly and often very weathered. Lithology discussed in great detail. Estimated thickness of 2-2.5km in NSW and 2-3km in Victoria. A composite representative section is given. Rare graptolites occur in addition to conodonts that are found commonly in the chert horizons. Probably equivalent to the Girilambone and Wagga Groups.Equivalent to the Pittman Formation, Mallacoota Beds and the Pinnak Sandstone.  On the basis of Bouma sequences this formation is interpreted to have been deposited as turbidity currents in a basin plain setting. Hosts orogenic gold mineralisation in addition to polymettalic Cu-Pb-Zn-Ag-Au vein systems. Also hosts some structurally controlled mineral deposits including silver-lead, gold, base metal and gold, and orogenic base metal and copper mineralisation. Intruded by the Lockhart Igneous Complex, Harrisons Peak Granite and the Gibraltar Granite.Tectonic structure, geophysical characteristics and metamorphism are discussed. See also p40 fig 17, p51, p52, p54 and 55 fig 20, p55, p57-69, p73 fig 26, p75, p76 fig 27, p78-82, p84, p88, p95, p106, p169, p180, p181, p184, p196, p200, p201. ||Adaminaby Group|Includes Willigam Sandstone Member, Mummel Chert Member, Peach Tree Chert Member, Nattery Chert Member|Potentially overlies the Nattery Chert Member. Unconformably overlain by the Captains Flat Formation or is faulted over it. Conformably overlain by the Warbisco Shale and the Bumballa Formation.|Micaceous, mostly quartz rich, turbiditic sandstone (wacke and sublitharenite), siltstone and mudstone with fine grained quartz sandstone laminae. Minor chert-rich intervals also occur.|
69898|Abercrombie Formation|71656|4|Described|p11-14, p12, 13 Fig.2|Sandbian|Tremadocian|Graptolites are relatively common in two horizons within the uppermost Abercrombie Formation. Constraints from fossils in underlying and overlying stratigraphic units imply likely age for the top of the Abercrombie Formation is early Gisbornian [Sandbian]. Cherts near base of unit suggest late Tremadoc to early Floian (early Bendigonian) for max. age. Literature describes latest Abercrombie Formation details.||Adaminaby Group|Includes Mummel Chert Member, Peach Tree Chert Member, Nattery Chert Member, and other unnamed cherts.|Underlies Warbisco Shale.|Includes siliceous black siltstones, fossiliferous chert.|
69898|Abercrombie Formation|71691|5|Briefly described|Map legend.|Ordovician|Ordovician|||Adaminaby Group.|Nattery Chert Member.|Is overlain by Nattery Chert.|Brown, grey to cream, thin- to very thick-bedded, fine- to coarse-grained mica-quartz +/- feldsdpar sandstone, interbedded with laminated siltstone and mudstone; sandstone beds typically have normal grading and prominent ripple cross-lamination.|
69898|Abercrombie Formation|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|The six Members (including two un-named) are mapped separately.||Adaminaby Group.|Willigam Sandstone, Mummel Chert, Peach Tree Chert, Nattery Chert, Members.|Is overlain by Bumballa Formation and Warbisco Shale.|Buff to brown, grey, fawn to cream, fine- to coarse-grained mica-quartz+/-feldspar sandstone, interbedded with laminated siltstone and mudstone; sandstone typically normal graded and ripple cross-laminated; discrete chert-rich packages.|
69898|Abercrombie Formation|71700|3|Fully described|vi, p5, p7-p10, p12, p25, p39-p41|Gisbornian|Lancefieldian|Albury-Bega Terrane. Named for the Abercrombie River. A composite representative section was constructed by M.M Scott in Thomas and Pogson (2012). Previously the "Abercrombie Beds" of Packham (1968) and includes parts of the Bubalahla Formation of Scheibner (1973b). This unit was subsequently defined by Thomas and Pogson (2012). Distribution, geomorphic expression, outcrop characteristics, structure, metamorphism, geophysical characteristics, fossils, distinguihsing features, stratigraphic correlation and economic geology are discussed. Lithology is discussed in detail on the CD. Intruded by the Butmaroo Granite. Interpreted to have been deposited either by a huge fan system or a passive margin depositional system comprised of smaller fans. Up to 2.5km thick in the Mummel-Baw Baw area, northwest of Goulburn (Goulburn250). Seperated from the Comerong Volcanics and Merrimbula Group by the Mongarlowe Fault. Equivalent to the Pinnak Sandstone. Faulted against the Tangerang Formation, Mundoonen Sandstone, Bendoc Group and Bungonia Group. See also  p43-p50, p52, p54-p58, p61-p62, p64, p71, p74, p82-p83-p84, p114, CD.||Adaminaby Group|Includes the Willigam Sandstone Member, Mummel Chert Member, Peach Tree Chert Member, Nattery Chert Member.|Overlain by the Bumballa Formation. Conformably overlain by the Warbisco Shale.|Fine- to coarse-grained, thin- to thick-bedded quartzose sandstone with interbedded laminated siltstone and mudstone.|
69898|Abercrombie Formation|73140|5|Briefly described|p495|Gisbornian|Lancefieldian|Proposed to incorporate and supersede the Clements Formation and Pinnak Sandstone. Age based on conodonts and graptolites. Uncertainty indicated for maximum age.||Adaminaby Group||Underlies Sunlight Creek Formation, Warbisco Shale, Currawalla Shale, Bumballa Formation||
69898|Abercrombie Formation|73582|5|Briefly described|p109|Ordovician|Ordovician|Extensively distributed in the N half of the Taralga 1:100,000 sheet, SW of Jenolan area.|||||Homogeneous, quartz-rich sandstones and cherts.|
80144|Aberglen Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Werrie Basin. Shown only as Aberglen. Ending assumed from references to other Coal Members in text.||Rowan Formation.||||28-SEP-17
77434|Abernethy Lens|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Lochinvar area.||Unit in Kurri Kurri Conglomerate.||||
82282|Accommodation Creek Monzogranite|71628|4|Described|p12: 1, 3-4; p15: 40, 116|Early Triassic|Late Permian|New name. Previously included in Stanthorpe Monzogranite by Brown et al. (2007). Excluded from this author's definition of Stanthorpe Complex. Named after a local watercourse. Forms a thick (up to 350m wide), ~4 km long, NNW-trending dyke just N of Wallangarra. Limited geochemistry is briefly described.||Sailor Jack Suite.||Intrudes Wallangarra Volcanics.|Pale grey to pale brownish-grey, medium- to coarse-grained, highly porphyritic biotite-hornblende monzogranite. Has undergone deformation and alteration. I-type.|
23323|Adderley Formation|22857|5|Briefly described|p478 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Crudine Group. Volcanic arenite, rhyolitic agglomerate, minor slate. Max. thickness: 700m. Geological Province: Caperteee Rise.||||||
23323|Adderley Formation|23214|3|Fully described|p196|Lochkovian|Lochkovian|Of Crudine Group. Intruded by the Tarana Granite. Upward fining sequence of felsic volcaniclastic conglomerate and sandstone. Max. thickness 900m.||||||
23323|Adderley Formation|42712|4|Described|8; Table 1 p14.|Early Devonian|Late Silurian|Within Crudine Group. Unconformable on Lambie Group, conformable under Buckburraga Slate and Dunchurch Formation.||||||
23323|Adderley Formation|43639|5|Briefly described|Map Legend|Devonian|Devonian|||||||
23323|Adderley Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
23323|Adderley Formation|68592|6|Mentioned|p1038|||Native Dog Syncline, southern Hill End Trough.||Unit in Crudine Group.||||
23323|Adderley Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
41273|Adelargo Basalt Member|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Warrumba Volcanics (Rocky Ponds Group).||||||05-JUL-04
28319|Agnes Banks Sand|31056|4|Described|p6|||||||||
28319|Agnes Banks Sand|33671|6|Mentioned|Fig.2|||||||||
28319|Agnes Banks Sand|35098|4|Described|p5|||||||||
28319|Agnes Banks Sand|35312|6|Mentioned|Fig.2|||||||||
28319|Agnes Banks Sand|42925|2|Defined|p37||early Pleistocene|||||||
28319|Agnes Banks Sand|42926|4|Described|map legend||Pleistocene|||||||
28319|Agnes Banks Sand|65195|6|Mentioned|p4 Fig.2|Quarternary|Quarternary|Overlies Londonderry Clay.||||||
26339|Agnes Greywacke|23720|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Part of the "Coffs Harbour Association".  Lithofeldspathic wacke, slate, minor chert, rare mafic and felsic volcanics.||||||08-DEC-04
26339|Agnes Greywacke|31694|6|Mentioned|p345|||||||||
26339|Agnes Greywacke|41347|4|Described|Table 4|||||||||
26339|Agnes Greywacke|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|Part of the "Coffs Harbour Association".||||||16-DEC-04
26339|Agnes Greywacke|44450|3|Fully described|p12 Table 1|Late Carboniferous|Late Carboniferous|Geological Province: New England Fold Belt.||||||
26339|Agnes Greywacke|71628|5|Briefly described|p2: 7, 37; p3: 19, 22, 44, 68, 97|Late Carboniferous|Late Carboniferous|||Coffs Harbour Association.||Is intruded by Moona Plains Complex, Blue Nobby, Garibaldi, Kimberley Park Monzogranites and Argyll Granodiorite.||
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||
29276|Alberta Conglomerate|22772|4|Described|p67,Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
29276|Alberta Conglomerate|22857|4|Described|Tb 13.1 (insert p70), p400 App 1 Tb A1.3|Marinoan|Marinoan|Of the Teamsters Creek Subgroup (TorrowangeeGroup). Diamictite, siltstone, sandstone, some conglomerate. Age: ~593+/-32Ma. Max. thickness: 300m. Geological Province: Adelaide Fold Belt. See also p67 (photo 3).||||||
29276|Alberta Conglomerate|30261|4|Described|Table 1|||Marinoan age||||||
29276|Alberta Conglomerate|34812|3|Fully described|p87|||||||||
29276|Alberta Conglomerate|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
29276|Alberta Conglomerate|36411|6|Mentioned|p267|||Refs Cooper et al for definition.||||||
29276|Alberta Conglomerate|36733|6|Mentioned|Table 5|||||||||
29276|Alberta Conglomerate|37931|4|Described|p532|||||||||
29276|Alberta Conglomerate|38157|6|Mentioned|p265|||||||||
29276|Alberta Conglomerate|39214|5|Briefly described|p7|||||||||
29276|Alberta Conglomerate|41405|5|Briefly described|p204|||||||||
29276|Alberta Conglomerate|68241|5|Briefly described|p21, p24 Fig.3, p32, p33 Fig.3|||||||Correlative of the Elatina Formation.|Comprises diamictite, pebbly siltstone and some conglomerate, with a mixture of intra- and extrabasinal clasts.|
29276|Alberta Conglomerate|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Teamsters Creek Subgroup.||||
29276|Alberta Conglomerate|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Teamsters Creek Subgroup.||Overlies Yowahro and Floods Creek Formations. Is overlain by Dering Siltstone and Gairdners Creek Quartzite.|Laminated siltstone and sandstone with variably developed rounded cobbles of polymict material derived from Willyama Supergroup and Neoproterozoic rocks.|07-SEP-15
34207|Alkaline Volcanics|22671|5|Briefly described|Fig2p837|Neoproterozoic|Neoproterozoic|Correlated with the Mt Arrowsmith Volcanics. Possibly not intended as a formal name.||||||17-JAN-06
73519|Allambie Woolshed Granite|66623|2|Defined|p161, pp176-178. |Silurian|Silurian|Defined in this study. Does not outcrop; studied from drill chips. Of similar age to Tibooburra Suite; interpreted to have formed in the same thermal event. At least 98 m deep. Soil around drill site contains coarse quartz sand grains.|423.1 +/- 2.4 Ma.|||Intrudes Teltawongee Group. Is possibly overlain to the south by Wana Karnu Group.|Grey, quartz-orthoclase-biotite granitoid, grainsize typically 3-4 mm; with zircon, apatite, monazite and garnet.|
27315|Allans Creek Formation|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Of the Sydney Subgroup.||||||08-JAN-08
27315|Allans Creek Formation|23881|5|Briefly described|p69 Fig. 7.2|||Of the Illawarra Coal Measures.  Geological Province: Sydney Basin.||||||
27315|Allans Creek Formation|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Underlies: Kembla Sandstone.||||||29-NOV-04
27315|Allans Creek Formation|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||
27315|Allans Creek Formation|29900|6|Mentioned|Table 1|||||||||
27315|Allans Creek Formation|29901|4|Described|Table 1|||||||||
27315|Allans Creek Formation|29944|6|Mentioned|Fig.18|||||||||
27315|Allans Creek Formation|30006|4|Described|p24|||||||||
27315|Allans Creek Formation|31128|6|Mentioned|Table 1|||||||||
27315|Allans Creek Formation|32618|6|Mentioned|Table 1|||Strat. table. Perm.||||||
27315|Allans Creek Formation|32849|6|Mentioned|Table 1|||Permian||||||
27315|Allans Creek Formation|34060|6|Mentioned|p24|||Perm. Table||||||
27315|Allans Creek Formation|34569|6|Mentioned|p8|||See Fig.2. Sydney Sub Group||||||
27315|Allans Creek Formation|36220|4|Described|p52|||See also Table 1, p49 and p50.||||||08-JAN-08
27315|Allans Creek Formation|37089|6|Mentioned|p208|||||||||
27315|Allans Creek Formation|37090|6|Mentioned|Fig.2|||||||||
27315|Allans Creek Formation|39309|5|Briefly described|p127|||||||||
27315|Allans Creek Formation|39661|6|Mentioned|Fig.1|||||||||
27315|Allans Creek Formation|42787|5|Briefly described|p133|||||||||
27315|Allans Creek Formation|42896|4|Described|p21|||Of Sydney Subgroup.||||||08-JAN-08
27315|Allans Creek Formation|42925|5|Briefly described|Table 18||Late Permian|||||||
27315|Allans Creek Formation|45090|6|Mentioned|p189|||Refers Anom.(1969)||||||
27315|Allans Creek Formation|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
27315|Allans Creek Formation|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
27315|Allans Creek Formation|63832|5|Briefly described|p131 Fig.2|Lopingian|Lopingian|Sydney Basin. Final (P4) Paleozoic glaciation.||Unit in Illawarra Coal Measures.||||13-DEC-17
27315|Allans Creek Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Darkes Forest Sandstone. Is overlain by Kembla Sandstone.||
27315|Allans Creek Formation|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
27315|Allans Creek Formation|73421|5|Briefly described|p3, p19|Wuchiapingian|Wuchiapingian|Sydney Basin, southern.||Sydney Subgroup||Overlies Darkes Forest Sandstone|Siltstone, sandstone and claystone/shale.|
23327|Allara Shale Member|37094|5|Briefly described|p243|||||||||
23327|Allara Shale Member|43194|5|Briefly described|p109|Late Permian|Late Permian|In this article, described as part of undifferentiated Arkarula Sandstone Member (Black Jack Formation). In a separate paper (Tadros, in press, summarised in Appendix 1) this unit is redefined to extend its lateral coverage.||||||
70446|Allawa Ignimbrite Member|62095|2|Defined|p276 Appdx.|Late Carboniferous|Late Carboniferous|Of Currabubula Fm. Beige unwelded ignimbrite; groundmass micropoikilitic. Overlies Rockford and Kankool Ignimbrite members. Age: ~310ma. Thickness: 10m. Geological Province: Werrie block/Tamworth Belt.||||||22-MAY-06
23328|Allendale Metasediments|6823|6|Mentioned|p205|||||Broken Hill Group||||
23328|Allendale Metasediments|22553|5|Briefly described|fig2p77,p80|Proterozoic|Proterozoic|||||||
23328|Allendale Metasediments|22575|6|Mentioned|p179 Fig.2|||Of the Broken Hill Group.||||||11-JUN-08
23328|Allendale Metasediments|22771|6|Mentioned|Table12.2p45,45|||||||||
23328|Allendale Metasediments|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Thickness at Mount Robe: 1000m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
23328|Allendale Metasediments|22884|6|Mentioned|p45|||Geological province: Broken Hill Domain.||||||26-MAR-09
23328|Allendale Metasediments|22964|6|Mentioned|p56||Proterozoic|||||||
23328|Allendale Metasediments|22965|6|Mentioned|Fig 1||Statherian|||||||
23328|Allendale Metasediments|22966|6|Mentioned|Fig 1||Proterozoic|Rift stage of geological development.||||||
23328|Allendale Metasediments|22967|6|Mentioned|p39||Statherian|||||||
23328|Allendale Metasediments|23025|6|Mentioned|Fig1p75|||||||||
23328|Allendale Metasediments|23160|6|Mentioned|fig1|||||||||
23328|Allendale Metasediments|23223|6|Mentioned|Table.2|||||||||
23328|Allendale Metasediments|23248|5|Briefly described|Fig2p169|||||||||
23328|Allendale Metasediments|23461|5|Briefly described|p204 Fig. 3|||Of the Broken Hill Group.||||||29-MAY-07
23328|Allendale Metasediments|24307|5|Briefly described|p975|Proterozoic|Proterozoic|Of the Broken Hill Group.  Previously included in the Purnamoota Subgroup, which has been abandoned by this study.||||||29-MAY-07
23328|Allendale Metasediments|38969|4|Described|p208|||||||||
23328|Allendale Metasediments|39662|2|Defined|p423|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23328|Allendale Metasediments|39849|6|Mentioned|Table 2|||||||||
23328|Allendale Metasediments|40822|6|Mentioned|Fig.2|||||||||
23328|Allendale Metasediments|41093|6|Mentioned|p252|||||||||
23328|Allendale Metasediments|41145|6|Mentioned|Fig.4|||||||||
23328|Allendale Metasediments|41630|6|Mentioned|p27|||See also Fig.1.3||||||
23328|Allendale Metasediments|41633|6|Mentioned|Fig.2.2|||||||||
23328|Allendale Metasediments|42261|6|Mentioned|Fig 1 P530|||||||||
23328|Allendale Metasediments|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23328|Allendale Metasediments|42537|4|Described|p13|||||||||
23328|Allendale Metasediments|42595|6|Mentioned|Fig. 2 P5|||||||||
23328|Allendale Metasediments|42813|6|Mentioned|p9|||||||||
23328|Allendale Metasediments|42897|5|Briefly described|Fig.3, P321|||||||||
23328|Allendale Metasediments|43052|6|Mentioned|Fig.4.22|||||||||
23328|Allendale Metasediments|43086|6|Mentioned|Fig.3|||||||||
23328|Allendale Metasediments|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23328|Allendale Metasediments|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the  Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|43572|6|Mentioned|Fig.3.2 p6|||||||||
23328|Allendale Metasediments|43583|5|Briefly described|Table 1, p2139|||||||||
23328|Allendale Metasediments|46598|4|Described|p303|||||||||
23328|Allendale Metasediments|50045|4|Described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Broken Hill Group (Willyama Supergroup). Overlain by Purnamoota Subgroup; underlain by Thackaringa Group. Includes: Ettlewood Calc-Silicate Member.||||||31-MAY-07
23328|Allendale Metasediments|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Contains the Ettlewood Cal-Silicate Member. Geological Province: Broken Hill Block.||||||24-FEB-10
23328|Allendale Metasediments|60485|5|Briefly described|p30|||Of the Broken Hill Group.  Contains the Ettlewood Calc-Silicate Member.||||||
23328|Allendale Metasediments|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
23328|Allendale Metasediments|61735|5|Briefly described|p636 Fig. 2, p638, 639|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Presented as Allendale only in Fig. 2. Max depositional age ~1750 Ma.||||||04-JUN-15
23328|Allendale Metasediments|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Ettlewood Calc-Silicate Member. Geological province: Olary Domain.||||||24-FEB-10
23328|Allendale Metasediments|62473|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Age: 1691+/-3Ma. Tuffaceous metasediments.||||||17-JUN-09
23328|Allendale Metasediments|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|62536|5|Briefly described|p633, 636, 638-639, 641, 646|||Broken Hill area.|c.1690 Ma. MDA of ~1750 Ma.|Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|62592|5|Briefly described|p16 Fig.2.2. |Statherian|Statherian|Broken Hill Domain, Curnamona Province.|1693 +/- 4 Ma.|Unit in Broken Hill Group.||||
23328|Allendale Metasediments|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Broken Hill Group|Includes Ettlewood Calc-Silicate Member|||19-DEC-21
23328|Allendale Metasediments|63102|5|Briefly described|p13-14,26,32|||Geological province: Broken Hill Domain, Curnamona Province.||Unit of Broken Hill Group.|Includes Ettlewood Calcasilicate Member.|||
23328|Allendale Metasediments|63519|5|Briefly described|p5, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Include the Ettlewood Calc-Silicate Member. See also p10 Fig. 3,  p29 Fig. 11..||||||07-NOV-08
23328|Allendale Metasediments|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province. ||Broken Hill Group|Includes the Ettlewood Calc-Silicate Member.|Overlain by the Parnell Formation.|Thin bedded pelite to psammopelite with minor mafic gneiss and calc-silicate nodules.|
23328|Allendale Metasediments|64097|5|Briefly described|p302 Tb.1, p303 Fig. 2|||Of Broken Hill Group. Contains Ettlewood Calc-Silicate Member.||||||07-FEB-11
23328|Allendale Metasediments|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group (Willyama Supergroup). Geological Province: Broken Hill Block.||||||07-FEB-11
23328|Allendale Metasediments|64741|5|Briefly described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Gp. Contains Ettlewood Calc-Silicate Mbr. Overlain by Parnell Gneiss. Geol.prov: Broken Hill Domain. Lower pelitic unit (very minor psammite) and upper, dominantly siliciclastic facies, with finely bedded pelites + minor thin psammites.||||||07-FEB-11
23328|Allendale Metasediments|64742|6|Mentioned|p321 Fig.3, P323. |||||Unit in Broken Hill Group.|||Albitic psammite, pelite.|
23328|Allendale Metasediments|64944|5|Briefly described|p29 Tb.1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Equivalent to Plumbago Formation in the Olary Domain. Geological province: Broken Hill Domain.||||||07-FEB-11
23328|Allendale Metasediments|66302|4|Described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Broken Hill Group|Includes the Ettlewood Calc-silicate Member.|Overlies the Himalaya Formation. Overlain by the Purnamoota Subgroup, Parnell Gneiss.|Thin-bedded mudstone to siltstone with minor mafic gneiss and calc-silicate nodules.|
23328|Allendale Metasediments|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1693 +/- 3 Ma.|Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|70000|5|Briefly described|p34, p36|Statherian|Statherian|||Unit in Broken Hill Group.|Includes Ettlewood Calc-Silicate Member.|Is overlain by Purnamoota Subgroup.|Siliciclastic, pelite-dominated rocks.|
23328|Allendale Metasediments|70014|5|Briefly described|Map legend|||||Basal unit in Broken Hill Group.|Includes Ettlewood Calc-Silicate Member.|Overlies Rasp Ridge Gneiss and Himalaya Formation (Broken Hill Group). Is overlain by Purnamoota Subgroup.|Mainly metasediment and metasedimentary composite gneiss. Variable ratio of pelite:psammopelite:psammite. Commonly garnet-rich. Sproradic bodies of basic gneiss and quartz-gahnite, quartz-iron sulfide. Sporadic zoned calc-silicate nodules.|07-SEP-15
23328|Allendale Metasediments|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Broken Hill Group.||Overlies Himalaya Formation.|Pelitic to psammitic metasedimentary composite gneiss, including garnet-bearing feldspathic composite gneiss, sporadic basic gneiss and quartz-gahnite rock. Calc-silicate bodies at base.|07-SEP-15
23328|Allendale Metasediments|70405|6|Mentioned|p40, p43 table 3|Paleoproterozoic|Paleoproterozoic|||Broken Hill Group||||
23328|Allendale Metasediments|70657|4|Described|p13 Fig.6, p14-17, p34, p37, p39|Statherian|Statherian|Curnamona Province: Broken Hill Domain. (Stevens et al, in prep). With Ettlewood Calc-Silicate Member, is equivalent to Larry Macs Subgroup (Saltbush Group) of Olary Domain.|~1700-1685 Ma|Broken Hill Group|Includes Ettlewood Calc-Silicate Member.|Underlies Purnamoota Subgroup. Overlies Himalaya Formation (Thackaringa Group). Intruded by Stephens Creek Granite Gneiss and Wondervale Well Granite Gneiss, of the Silver City Suite.||
23328|Allendale Metasediments|70658|5|Briefly described|p7, 15, 47|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Broken Hill Group.||Locally overlies Plumbago Formation.||
23328|Allendale Metasediments|72461|5|Briefly described|p16 fig 9, p17|||||Broken Hill Group|Includes the Ettlewood Calc-silicate Member.|Overlies the Himalaya Formation. Ovderlain by the Parnell Gneiss.||
23328|Allendale Metasediments|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian|Broken Hill block-Euriowie block.||Broken Hill Group|Ettlewood CS|||
23328|Allendale Metasediments|73308|6|Mentioned|p607 Fig.1|||||Broken Hill Group.|Ettlewood Calc-Silicate Member.|||
23328|Allendale Metasediments|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Broken Hill Group|Ettlewood Calc-Silicate Member|Underlies Purnamoota Subgroup||
23328|Allendale Metasediments|73482|6|Mentioned|p422 Fig.3|||||Broken Hill Group|Ettlewood CS|||
23328|Allendale Metasediments|73512|6|Mentioned|p2|||||||||
23328|Allendale Metasediments|73524|6|Mentioned|p5 Fig.3|||||Broken Hill Group||||
23328|Allendale Metasediments|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p831 Fig.5|Statherian|Statherian|||Broken Hill Group|Ettlewood Calc-Silicate Member|Overlies Himalaya Formation, underlies Purnamoota Subgroup, Parnell Formation||
26341|Alley Sandstone Member|22857|4|Described|p436 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Biddabirra Formation (Amphitheatre Group, Cobar Supergroup). Max. thickness: 300m. Geological Province: Cobar Basin.||||||
26341|Alley Sandstone Member|23173|4|Described|Map Legend|Pragian|Pragian|||||||
26341|Alley Sandstone Member|38292|6|Mentioned|p5|||||||||
26341|Alley Sandstone Member|41138|6|Mentioned|Map legend|Pragian|Pragian|||||||
26341|Alley Sandstone Member|41452|6|Mentioned|Fig.1|||||||||
26341|Alley Sandstone Member|42144|6|Mentioned|Fig.6 P609|||||||||
26341|Alley Sandstone Member|42521|5|Briefly described|Fig.7 P21|||||||||
26341|Alley Sandstone Member|43032|2|Defined|p110|Early Devonian||of Biddabirra Formation||||||
26341|Alley Sandstone Member|43153|5|Briefly described|Map Legend|Pragian|Pragian|of Biddabirra Formation||||||
26341|Alley Sandstone Member|43774|1|Redefined|p67|||||||||
26341|Alley Sandstone Member|61905|5|Briefly described|p135 Fig. 1|||Geological Province: Cobar Basin.||||||
26341|Alley Sandstone Member|65469|5|Briefly described|p14|Lochkovian|Lochkovian|Lachlan Orogen.||Biddabirra Formation||||
26341|Alley Sandstone Member|68823|6|Mentioned|p378 Fig.4, p404|Pragian|Lochkovian|||Of Biddabirra Formation.||||
26341|Alley Sandstone Member|69002|5|Briefly described|p11|Lochkovian|Lochkovian|A sample from the Cobar 1:100k sheet GR 384858 6518889, constrained in age by the brachiopod Howellela jaqueti, was inferred to be Pragian in age during the mapping program but is now regarded as Lochkovian (Early Devonian) in age (Pogson & Glen 2008, based on Sherwin 1995).||Of the Biddabirra Formation.||||
26341|Alley Sandstone Member|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Early Devonian|Lachlan Orogen.||||||
26341|Alley Sandstone Member|73174|5|Briefly described|p1037, p1039-1043, p1045-1046|Pragian|Pragian|Cobar Basin. Variable thickness from <200 to 350 m thick. Contains age-diagnostic brachiopod. Geochron are maximum depositional ages from this study and Glen et al. (2010).|424 +/- 10 Ma and 500 +/- 7 Ma LA-ICP-MS|Biddabirra Formation, Amphitheatre Group, Cobar Supergroup|||Thick-bedded sandstone marker unit.|24-NOV-22
26341|Alley Sandstone Member|73264|5|Briefly described|p1394 Fig.16|Early Devonian|Silurian|Cobar Basin.||Biddabirra Formation|||Quartz-rich sandstone.|
23329|Allyn River Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Of the Flagstaff Formation. Max. thickness: 1000m. Geological Province: Tamworth Forearc Basin.||||||10-MAR-06
23329|Allyn River Member|40883|6|Mentioned|p7|||||||||
23329|Allyn River Member|43576|6|Mentioned|p350|||||||||
23329|Allyn River Member|44244|4|Described|p65-68|Visean|Visean|Of the Flagstaff Formation.  Conformably overlies Bonnington Siltstone. Type section in text.   Max. thickness: >1000m.  Geological Procince: Gresford Block.||||||27-JUL-04
23329|Allyn River Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Flagstaff Formation.  Green to brown, medium to thickly bedded lithic sandstone with turbiditic sedimentary structure and interbeds of brown thinly bedded mudstone. Geological Province: Gresford Block||||||
23329|Allyn River Member|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Gresford Block.  Of the Flagstaff Formation.||||||
23329|Allyn River Member|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Gresford Block, Tamworth Belt. Appears as Allyn River.||Unit in Flagstaff Formation.||||
83652|Alstonville basalt|73581|5|Briefly described|p14|Oligocene|Eocene|Basalt sequence is well exposed at Lennox Heads, where it exhibits columnar jointing and dips westwards. Up to 150 m thick, probably forms extensive aquifers in the region.|41.4-27.6 Ma K-Ar||||Largely consists of high Mg sodic trachybasaltic magmas that fractionated in closed magma chambers.|
23331|Alton Limestone Member|22857|5|Briefly described|p472 App.1 Tb.A1.6||Silurian|Of the Bells Creek Volcanics (Mumbil Group). Fossiliferous marble, minor talc schist.||||||10-MAR-06
23331|Alton Limestone Member|23214|4|Described|p140|Lochkovian|Ludlow|Of Bells Creek Volcanics. Formerly known as Jericho Limestone and Cow Quarries limestone. Thickly bedded iohite, coarse grained fossilerous marble containing rare talc schist bands.||||||
23331|Alton Limestone Member|42712|4|Described|Table1p14; Fig3p10.|Early Devonian|Late Silurian|Replaces invalid "Jericho Limestone" of Binns 1958. Member of Vale Creek Volcanics.||||||
23331|Alton Limestone Member|43639|5|Briefly described|Map Legend||Silurian|||||||
23331|Alton Limestone Member|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Bells Creek Volcanics (Mumbil Group east). Thickly bedded, white, coarse-grained fossiliferous marble; minor talc schist.||||||17-JUL-08
23331|Alton Limestone Member|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Bells Creek Volcanics, Mumbil Group.||||||17-JUL-08
23331|Alton Limestone Member|67847|6|Mentioned|p29|Pridoli|Ludlow|Age constrained on the basis of coral fossil assemblage (De Deckker, 1976). Alternative age of Wenlock-Ludlow derived from conodont fossil assemblage (Simpson, 1995)||||Equivalent to the Kildrummie Limestone.||
23332|Ambone Volcanics|22768|5|Briefly described|p171|||||||||
23332|Ambone Volcanics|22857|4|Described|p171, p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Mount Hope Group (Cobar Supergroup). Max. thickness: 280m. Geological Province: Mount Hope Trough (Darling Basin).||||||
23332|Ambone Volcanics|37772|4|Described|p8|||||||||
23332|Ambone Volcanics|40269|4|Described|p149|||Mention P147||||||
23332|Ambone Volcanics|40913|6|Mentioned|Map legend|Pragian|Pragian|||||||
23332|Ambone Volcanics|41126|2|Defined|p60|early Pragian|early Pragian|Mention P42||||||
23332|Ambone Volcanics|41821|6|Mentioned|p15|||Occurs in the Mount Allen sheet area||||||
23332|Ambone Volcanics|42144|6|Mentioned|Fig.3 P604|||||||||
23332|Ambone Volcanics|42521|5|Briefly described|Fig.3b P16|||||||||
23332|Ambone Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
23332|Ambone Volcanics|43089|5|Briefly described|Map Legend|||of Mount Hope Group||||||
23332|Ambone Volcanics|43202|5|Briefly described|Table 2,p20.|||||||||
23332|Ambone Volcanics|70751|6|Mentioned|p17, p19, p30|||||Mount Hope Group||||
23332|Ambone Volcanics|72908|6|Mentioned|p3|||Simpson (2014) (see also Downes, Blevin et al., 2016) proposed that the stratigraphy of the Mount Hope Group be simplified, with the Ambone, Regina, Goona and part of the Coando Volcanics being grouped into the Mount Halfway Volcanics.||Mount Hope Group||||
24656|American Creek Coal Member|29900|6|Mentioned|Table 1|||||||||
24656|American Creek Coal Member|29901|4|Described|Table 1|||||||||
24656|American Creek Coal Member|31128|6|Mentioned|Table 1|||||||||
24656|American Creek Coal Member|32849|6|Mentioned|Table 1|||||||||
24656|American Creek Coal Member|33869|6|Mentioned|Fig.2|||||||||
24656|American Creek Coal Member|36220|4|Described|p52|||See also Table 1 & P50.||||||
24656|American Creek Coal Member|37089|6|Mentioned|p208|||||||||
24656|American Creek Coal Member|37090|6|Mentioned|p222|||||||||
24656|American Creek Coal Member|39661|6|Mentioned|p447|||Replaces Bimlow seam||||||
24656|American Creek Coal Member|42787|6|Mentioned|Table 1 P126|||||||||
24656|American Creek Coal Member|42896|5|Briefly described|p21|||of Allans Creek Formation||||||
24656|American Creek Coal Member|42925|6|Mentioned|Fig.23|||||||||
82283|Amiens Leucomonzogranite|71628|4|Described|p12: 10; p15: 34-35, 43-46, 75-76,82,97|Middle Triassic|Early Triassic|See also p3: 102, 115. New name, after the locality of the same name. Extends 37 km from Sorrento almost to the Severn River NW of Ballandean; outcrop area c.197 km2. Crops out as large boulders, tors, whalebacks and extensive pavements in hilly country. Geochemistry detailed. Is spatially associated with several minor Sn deposits (named).||Amiens Suite.||Intrudes Passchendaele Monzogranite and Texas beds (and is faulted against the latter). Abuts Severn River, Benalla Monzogranites, Mount Norman Leucomonzogranite and Ruby Creek Leucogranite.|Pale pink to pale pinkish-grey, medium-grained, moderately porphyritic, leucocratic biotite (rarely amphibole-bearing) monzogranite to syenogranite; locally fine-grained and highly porphyritic. I-type.|
82284|Amiens Suite|71628|5|Briefly described|p15: 35, 43-44, 50, 75-76, 88|Middle Triassic|Early Triassic|||Stanthorpe Supersuite.|Amiens, Mount Norman Leucomonzogranites.|||
39242|Amphitheatre Group, upper|22857|5|Briefly described|p436 App.1, Tb.A1.6|Early Devonian|Early Devonian|Informal - see Amphitheatre Group. Of the Cobar Supergroup. Max. thickness: ~4km. Geological Province: Cobar Basin. See also p440 App.1, Tb.A1.6.||||||
39242|Amphitheatre Group, upper|23171|5|Briefly described|p15,Fig15p45|||||||||21-JAN-05
39242|Amphitheatre Group, upper|23173|4|Described|Map Legend|Pragian|Lochkovian|||||||21-JAN-05
39242|Amphitheatre Group, upper|24019|5|Briefly described|p353|||Informal name. Of Cobar Supergroup.||||||16-MAR-05
39242|Amphitheatre Group, upper|43032|3|Fully described|p117|||Intended as informal use||||||21-JAN-05
39242|Amphitheatre Group, upper|43153|5|Briefly described|Map Legend||Pragian|Informal name for unit of Amphitheatre Group. Formerly Elouera Beds.||||||21-JAN-05
39242|Amphitheatre Group, upper|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Informal subdivision of the Amphitheatre Group.  Geological Province: Cobar Basin.||||||
39242|Amphitheatre Group, upper|70950|6|Mentioned|p1029,1033,1038|||Geological province: Central Lachlan Orogen. See also Amphitheatre Group. Includes a sequence of quartz-rich to quartz-lithic sandstones and siltstones.||||Separated from lower Amphitheatre Group by Shume Formation||12-MAY-20
39242|Amphitheatre Group, upper|71693|5|Briefly described|Map legend.|Devonian|Devonian|Two informal units (Amphitheatre Group, lower and Amphitheatre Group, upper) are also mapped, but share the same lithological description in the Legend. In the Time-Space Plot, they unfortunately appear as Lower Amphitheatre Formation and Upper Amphitheatre Formation.|||||Thin- to medium-bedded, massive or graded, parallel-laminated and ripple cross-laminated, poorly sorted, fine- to medium-grained, quartzose to quartz-lithic sandstone interbedded with siltstone and mudstone.|
39242|Amphitheatre Group, upper|72908|5|Briefly described|p3, p7, p18|||Cobar Basin. Hosts the Mallee Bull deposit.||Amphitheatre Group|||Sequence of quartz-rich to quartz-lithic sandstones and siltstones.|
39242|Amphitheatre Group, upper|72958|5|Briefly described|p5, p7-8, p12-19, p21-27, p29, p60|||Cobar Basin, sag phase. Volcanics have complex boundary relationships. Edgecombe and Soininen (2019) define 4 separate units including the upper and lower volcaniclastics. [Also written as Amphitheatre Group (upper); Fig.1.1]. Dated rhyolites are mapped as this unit; however, may correlate directly with the underlying Shume Formation. Rhyolite MBDD007 yielded a SHRIMP U-Pb age of 420.0 +/- 1.9 and rhyolite MBDD003 an age of 419.2 +/- 1.8. These unnamed rhyolites from Mallee Bull are interpreted as blocks from an olistolithic slump, slide or breccia horizon.||Amphitheatre Group||Underlain by Shume Formation.|Includes hyaloclastic, porphyritic rhyolite, porphyritic felsic volcanic breccia, volcanic-rich sandstone horizon, mass flow slump breccias/olistostromes and slump blocks/olistoliths, quartzose sandstone.|
39242|Amphitheatre Group, upper|73174|5|Briefly described|p1037|||Cobar Basin. Represents sag phase of sedimentation. Variable thickness of 6-8 km.|||||Thin- to medium bedded turbidite sequence of sandstone, siltstone and mudstone. Sandstones are typically quartz-rich with well-developed Bouma divisions.|24-NOV-22
25684|Anembo Granodiorite|22815|4|Described|p77|||||||||
25684|Anembo Granodiorite|36413|2|Defined|p116|Devonian|Devonian|||||||
25684|Anembo Granodiorite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25684|Anembo Granodiorite|39626|6|Mentioned|p275|||||||||
25684|Anembo Granodiorite|40276|2|Defined|p16|Early Devonian|Early Devonian|||||||
25684|Anembo Granodiorite|40328|4|Described|p202|||||||||
25684|Anembo Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Glenbog Suite.||||||
25684|Anembo Granodiorite|62070|5|Briefly described|p40,|Emsian|Pragian|Of Bega Batholith. 406 +/- 6 Ma SHRIMP U-Pb date|406+/-6 Ma SHRIMP U/Pb zircon|||||
25684|Anembo Granodiorite|68592|6|Mentioned|p1675|Early Devonian|Early Devonian|||Unit in Glenbog Suite.||||
25684|Anembo Granodiorite|69270|4|Described|p1, p2 Tb.1.1, p15-23, p31|Early Devonian|Early Devonian|Sample comprises fresh grey-cream, enclave-rich, coarse-grained hornblende-biotite granodiorite sourced from roadside blast-site material on western side of Jerangle-Captains Flat Road. Dating method: zircon U-Pb by SHRIMP. Sample size is n=24 (Tb.3.2 all results), though n=23 was reported in Tb.1.1 summary table (possible typing error). Previous dating: SHRIMP U-Pb age 406+/-6 Ma from zircons within a mafic inclusion of Anembo Granodiorite (Chen et al. 1990). Eastern Lachlan Orogen. Considered contemporaneous with Towneys Creek Monzogranite based on field relationships (Richardson, 1976).|412.7+/-1.9 Ma, magmatic crystallisation|Glenbog Suite||intrudes Abercrombie Formation; adjacent to Towneys Creek Monzogranite|granodiorite|
25684|Anembo Granodiorite|71069|6|Mentioned|p28|Lochkovian|Lochkovian|Age is a SHRIMP U-Pb age from Chisholm et al. 2014.|412.4 +/- 1.7 Ma |Glenbog Suite||||
27693|Angullong Formation|13139|5|Briefly described|p8, p9 Fig. 4|Late Ordovician|Late Ordovician|Predominantly volcaniclastic. Overlies the Malongulli Formation. Geological Province: Western Molong Volcanic Belt.||||||17-JUL-08
27693|Angullong Formation|22503|6|Mentioned|Fig.4 p646|||||||||
27693|Angullong Formation|22679|6|Mentioned|p 21|||||||||
27693|Angullong Formation|22857|4|Described|p424 App.1 Tb.A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Basaltic sandstone, thin to medium-bedded calcareous siltstone. Max. thickness: 1050m in the Cowra area.||||||
27693|Angullong Formation|23181|6|Mentioned|Fig.2||Late Ordovician|||||||
27693|Angullong Formation|23214|2|Defined|p60|Llandovery|Bolindian|Of Cabonne Group. Formerly Angullong Tuff. Max thickness 1050m||||||
27693|Angullong Formation|23334|5|Briefly described|9 Fig.4|Late Ordovician|Late Ordovician|||||||
27693|Angullong Formation|24398|5|Briefly described|p265, p259 Fig. 2|Bolindian|Bolindian|Geological Province: Lachlan Fold Belt.||||||
27693|Angullong Formation|29905|6|Mentioned|p6|||||||||
27693|Angullong Formation|38444|6|Mentioned|p303|||||||||
27693|Angullong Formation|40026|5|Briefly described|p245|||||||||
27693|Angullong Formation|43640|5|Briefly described|Map Legend||Ordovician|||||||
27693|Angullong Formation|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Consists of basaltic sandstone, thin to medium-bedded calcareous siltstone.||||||17-JUL-08
27693|Angullong Formation|43782|5|Briefly described|Map Legend|Bolindian|Bolindian|of Cabonne Group.||||||
27693|Angullong Formation|44093|5|Briefly described|p194 App. 1|Early Silurian|Late Ordovician|||||||
27693|Angullong Formation|60417|5|Briefly described|p154 Fig.1|Ordovician|Ordovician|||||||
27693|Angullong Formation|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p154, p155|Late Ordovician|Late Ordovician|Conformably underlain by Malongulli Formation. Geol Prov: Molong Volcanic Belt, LFB. Probably age equivalent to  Millambri Formation and Malachis Hill Formation. Consists of andesite and volcaniclastic rocks (sandstone, conglomerate, and siltstone).||||||07-FEB-11
27693|Angullong Formation|63283|5|Briefly described|p189 Tb. 1, p195 Fig. 2, p210|Late Ordovician|Late Ordovician|Underlain by Malongulli Formation. Age: 440Ma (basal mafic unit and basaltic andesite). Geological Province: Molong Volcanic Belt.||||||07-FEB-11
27693|Angullong Formation|63286|5|Briefly described|p294 Fig. 1, p308 Fig. 9|Early Silurian|Bolindian|Consists of basaltic sandstone and calcareous siltstone. Geological Province: Molong Volcanic Belt.||||||17-MAY-16
27693|Angullong Formation|63287|4|Described|p318 Fig. 3, p317 Fig. 2, p335|Late Ordovician|Late Ordovician|Of Cabonne Group. Conformably underlain by Malongulli Formation. Geological Province: Molong Volcanic Belt. Consists mainly of  interbedded siltstones and shales deposited in deep water but volcaniclastics in the unit suggest close to volcanic centre.|440Ma Rb/Sr.|||||07-FEB-11
27693|Angullong Formation|63290|4|Described|p385, p392 Tb. 1, p396 Fig. 3|Bolindian|Bolindian|Overlain by Ashburnia Group and Cobblers Creek Limestone unconformably, underlain by Malongulli Formation. Contains Bolindian (ca 447-448.4Ma) graptolites. Geological Province: Molong Volcanic Belt.||||||
27693|Angullong Formation|63293|6|Mentioned|p469 Fig. 2|Bolindian|Bolindian|Underlain by Malongulli Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
27693|Angullong Formation|64826|5|Briefly described|p1040 Tb. 1|Bolindian|Bolindian|Of the Cabonne Group.||||||04-MAR-09
27693|Angullong Formation|67322|5|Briefly described|p20 Fig.5, p24|Katian|Katian|Macquarie Arc. Krynen and Pogson, in Pogson and Watkins (1998), after Stevens (1952). Mid-Bolindian graptolites are present in several siltstone horizons of this unit. Occurs in the Cliefden Caves region. ||Of the Cabonne Group.||Overlies the Malongulli Formation.|Volcaniclastic-dominated.|
27693|Angullong Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
27693|Angullong Formation|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3). Molong Volcanic Belt.|c. 449-443 Ma|Cabonne Group||||
27693|Angullong Formation|70684|5|Briefly described|p3, p33-35, p44, p50-52, p75|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Bolindian. Diverse graptolite species listed.||||Conformably overlies Malongulli Formation. Is overlain unconformably (inferred) by Ashburnia Group.|Primary andesite and volcaniclastic conglomerate, sandstone and siltstone; breccia. Rare allochthonous limestone blocks in the lower part.|
27693|Angullong Formation|70754|6|Mentioned|p449-450|Late Ordovician|Late Ordovician|||||Overlies Malongulli Formation.||
27693|Angullong Formation|71091|5|Briefly described|p141-165|Late Ordovician|Late Ordovician|Krynen and Pogson, in Pogson and Watkins (1998) after Stevens (1952). Cliefden Caves district. Contains late Katian conodont fauna. International correlations given. Graptolite and coral species listed. Paleoecology and depositional setting discussed. Systematic descriptions.||||Conformably overlies Malongulli Formation. Correlated with Malachis Hill Formation.|Andesite and volcaniclastic rocks (conglomerate, sandstone and siltstone) with rare allochthonous limestone blocks.|
27693|Angullong Formation|73492|6|Mentioned|p706|Katian|Katian|||||||
24602|Angus Place Sandstone|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Charbon Subgroup (Illawarra Coal Measures). Quartz lithic-sandstone. Max. thickness: 15m. Geological Province: Sydney Basin.||||||
24602|Angus Place Sandstone|38614|6|Mentioned|Fig.6|||||||||
24602|Angus Place Sandstone|39232|4|Described|p110|||||||||
24602|Angus Place Sandstone|40166|6|Mentioned|p348|||See also Table 1||||||
24602|Angus Place Sandstone|40256|6|Mentioned|Fig.3|||||||||
24602|Angus Place Sandstone|40321|6|Mentioned|Fig.3|||||||||
24602|Angus Place Sandstone|40332|6|Mentioned|Fig.4|||||||||
24602|Angus Place Sandstone|40806|2|Defined|p156|Permian|Permian|Prob. Permian||||||
24602|Angus Place Sandstone|42182|6|Mentioned|p299|||||||||
24602|Angus Place Sandstone|42657|6|Mentioned|p82|||Synonym of Watts Sandstone, which has priority||||||
24602|Angus Place Sandstone|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
24602|Angus Place Sandstone|73625|5|Briefly described|p2|Permian|Permian|Western coalfield, Sydney Basin.||Illawarra Coal Measures.||Overlies Baal Bone Formation.||
24660|Annalee Pyroclastics|22857|4|Described|p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Group. Rhyodacitic to dacitic fragmental volcanics; basal coarse ashflow and airfall tuffs. Max. thickness: 45m. Geological Province: New England Fold Belt.||||||
24660|Annalee Pyroclastics|23720|5|Briefly described|Map Legend|||Of Wandsworth Volcanics.  Felsic pyroclastics, rhyolite, trachyte, minor rhyolitic tuffaceous sandstone.||||||15-DEC-04
24660|Annalee Pyroclastics|23859|6|Mentioned|p930 Fig. 2|||Geological Province New England Fold Belt.||||||
24660|Annalee Pyroclastics|30911|6|Mentioned|Map legend|Permian|Permian|||||||
24660|Annalee Pyroclastics|31806|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
24660|Annalee Pyroclastics|32671|6|Mentioned|Map legend|Permian|Permian|||||||
24660|Annalee Pyroclastics|32944|6|Mentioned|p699|||See also P709. Permian||||||
24660|Annalee Pyroclastics|34350|2|Defined|p13|Permian|Permian|See also p14 and Fig.1.||||||10-DEC-07
24660|Annalee Pyroclastics|35803|6|Mentioned|p321|||||||||
24660|Annalee Pyroclastics|36961|6|Mentioned|p220|||||||||
24660|Annalee Pyroclastics|38288|5|Briefly described|Table 1|||||||||
24660|Annalee Pyroclastics|39214|4|Described|p37|||||||||
24660|Annalee Pyroclastics|42284|6|Mentioned|p108|||||||||
24660|Annalee Pyroclastics|42378|4|Described|Table 1 P10|||||||||
24660|Annalee Pyroclastics|44450|4|Described|p26 Table 6|Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
24660|Annalee Pyroclastics|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
24660|Annalee Pyroclastics|69639|6|Mentioned|p133, p219|||||Wandsworth Volcanic Group||Intruded by the Llangothlin Monzogranite.||
24660|Annalee Pyroclastics|71628|5|Briefly described|p8: 13, 34|||||Wandsworth Volcanic Group.||Is intruded by Llangothlin and Mount Duval Monzogranites.||
82392|Annandale Metadolerite|73512|6|Mentioned|p2|||||||||
29659|Anson Formation|22679|5|Briefly described|p 26|Silurian|Silurian|||||||
29659|Anson Formation|22857|4|Described|p470 App.1 Tb.A1.6|Silurian|Silurian|Of the Mumbil Group. Max. thickness: ~1km. Geological Province: Hill End Trough.||||||24-FEB-06
29659|Anson Formation|23048|5|Briefly described|p11 table2||Late Silurian|||||||
29659|Anson Formation|23214|3|Fully described|p135|Ludlow|Ludlow|Of Mumbil Group. Originally informally referred to as Licking Hole Limestone Member. Previously has been included in Barnby Hills Shale and Mullions Range Volcanics. Also formerly referred to as Clifton Grove Formation.  Max. thickness 400m.||||||
29659|Anson Formation|43653|5|Briefly described|Map Legend||Silurian|||||||
29659|Anson Formation|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group (northwest). Carbonaceous pyritic siltstone, felsic volcanics, volcanic sandstone, limestone.||||||17-JUL-08
29659|Anson Formation|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|of Mumbil Group.||||||
29659|Anson Formation|50124|5|Briefly described|p126|Late Silurian|Late Silurian|Of the Mumbil Group. Overlain by the Mullions Range Volcanics. Geological Province: eastern Lachlan Fold Belt.||||||
29659|Anson Formation|60424|5|Briefly described|p350 Fig. 1, p351 Fig. 2|Silurian|Silurian|Of the Mumbil Group. Geological Province: Hill End Trough. Siltstone, shale, minor sandstone and limestone.||||||
29659|Anson Formation|63290|5|Briefly described|p393 Tb. 1, p395|Ludlow|Ludlow|Unconformably underlain by Byng Volcanics and Oakdale Formation. Age: 423-421Ma. Geological Province: Molong Volcanic Belt. ||||||
29659|Anson Formation|66197|5|Briefly described|p632, p633 Fig.4b|Ludlow|Ludlow|Molong High-Hill End Trough. Shallow marine clastics, limestone and silicic volcanics. Underlies the Mullions Range Volcanics.||||||14-MAR-12
29659|Anson Formation|67847|5|Briefly described|p30|Ludlow|Ludlow|Forms part of the Hill End Trough sequences (Scott and Meakin 1998). ||||Overlain by the Mullions Range Volcanics.|Pyritic siltstones and shales that contain poorly-sorted conglomerate and debris-flow horizons with clasts of chert, microlitic basalt, latite and basaltic andesite.|
29659|Anson Formation|68592|6|Mentioned|p650|Late Silurian|Late Silurian|||||Correlated with Cuddyong Formation (Campbells Group).||
29659|Anson Formation|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Hosts volcanic-associated massive sulfide base metal deposits, on western side of Hill End Trough; classified as siliciclastic-felsic hosted (i.e. Iberian-type).||Mumbil Group|||Dominantly pyritic and calcareous siltstone and rhyolitic volcaniclastic rock.|
80764|Apple Tree Gully Granodiorite|71628|5|Briefly described|p10: 2-4|Late Permian|Late Permian|The name Apple Tree Granodiorite was reserved in ASUD by Blevin (May, 2011). Named probably after a local waterhole. Crops out ~26 km NNW of Emmaville. Very limited geochemistry described.||Apple Tree Gully Suite (tentative).||Intrudes Emmaville Volcanics and Bondonga beds.|Quartz-poor granodiorite. I-type.|
82285|Apple Tree Gully Suite|71628|5|Briefly described|p10: 3|Late Permian|Late Permian|||Boxwell Supersuite.|Apple Tree Gully Granodiorite.|||
37907|Appleogue Dacite Member|24605|3|Fully described|p931, p939|Namurian|Namurian|Of the Clifden Formation. Geological Province: New England Orogen. Defined as Appleogue Dacite in Appendix 1 (p950 ).||||||17-JAN-06
82287|Applethorpe Monzogranite Phase|71628|5|Briefly described|p15: 35, 99, 101-104, 115|Middle Triassic|Early Triassic|This subunit does not ""technically"" qualify as a Phase according to stratigraphic naming conventions. Geochemistry described.",,||Severn River Monzogranite.|||Grey to pinkish grey, fine-grained, relatively biotite-rich, porphyritic biotite granite.|
67896|Apsley River Complex|71628|4|Described|p2:4-7; p3: 44-45|||Originally the Apsley River Diorite (Binns et al., 1967) for ""dioritic and gabbroic intrusions"". Subsequently the Apsley River Gabbro and Apsley River Complex (Hensel, 1982); the latter term was adopted later by Landenberger (1996). Crops out ~38 km ESE of Walcha. Geochemistry detailed.|295 Ma.||Garibaldi Monzogranite.|Intrudes the Coffs Harbour Association.|Mafic igneous complex comprising gabbro, diorite, granodiorite.|
24663|Ararat Formation|22736|6|Mentioned|p629|Visean|Tournaisian|||||||
24663|Ararat Formation|22857|4|Described|p498 App.1 Tb.A1.7|Visean|Visean|Includes Trevallyn, Gresford and Glenroy Conglomerate Members. Pebbly sandstone, oolitic and crinoidal limestone; coarse volcanolithic sandstone, mudstone; lenses of conglomerate. Max. thickness: 800m. Geological Province: Tamworth Forearc Basin.||||||
24663|Ararat Formation|24121|5|Briefly described|p4, p76, p86|Carboniferous|Carboniferous|||||||25-AUG-22
24663|Ararat Formation|31228|4|Described|p77|||||||||
24663|Ararat Formation|31706|6|Mentioned|p651|||L.Carb. Correlation Chart||||||
24663|Ararat Formation|32324|6|Mentioned|Table 8.1|||||||||
24663|Ararat Formation|32527|6|Mentioned|p403|||Refers Roberts & Oversby (1973)||||||
24663|Ararat Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
24663|Ararat Formation|32866|6|Mentioned|p7|||Fossil content||||||
24663|Ararat Formation|32867|6|Mentioned|p26|||||||||
24663|Ararat Formation|32869|4|Described|p167|||See also Fig.2, Fig.3B||||||
24663|Ararat Formation|33728|6|Mentioned|p50|||||||||
24663|Ararat Formation|34072|6|Mentioned|Fig.4.5|Carboniferous|Carboniferous|Contains Orthotetes australis||||||31-JUL-08
24663|Ararat Formation|34077|5|Briefly described|p252|||||||||
24663|Ararat Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
24663|Ararat Formation|34086|6|Mentioned|p262|||Assemblages||||||
24663|Ararat Formation|34238|6|Mentioned|Table 1|||||||||
24663|Ararat Formation|36528|6|Mentioned|p175|||||||||
24663|Ararat Formation|36599|6|Mentioned|Fig.1|||||||||
24663|Ararat Formation|37068|6|Mentioned|p59|||||||||
24663|Ararat Formation|39302|5|Briefly described|p342|||||||||
24663|Ararat Formation|39979|6|Mentioned|p62|||||||||
24663|Ararat Formation|40883|6|Mentioned|p5|||See also p13||||||31-JUL-08
24663|Ararat Formation|41826|6|Mentioned|p344|||||||||
24663|Ararat Formation|42547|4|Described|p28|||||||||
24663|Ararat Formation|43383|14|Not recorded|p18|||||||||
24663|Ararat Formation|43432|14|Not recorded|p206,207||Early Carboniferous|||||||
24663|Ararat Formation|43447|14|Not recorded|Table 1&2,p7,10,11,||Visean|||||||
24663|Ararat Formation|43451|14|Not recorded|Map Legend||Carboniferous|||||||
24663|Ararat Formation|43576|6|Mentioned|Fig.1,p348|||||||||
24663|Ararat Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
24663|Ararat Formation|44093|5|Briefly described|p229 App. 1|Visean|Tournaisian|In the Gresford Block.||||||
24663|Ararat Formation|44244|2|Defined|p48-59|Tournaisian|Tournaisian|Includes: Glenroy, Gresford and Treavallyn Conglomerate Members.  Conformably overlies Bingleburra Formation.  Max. thickness: 740m.  Type section in text.Geological Procince: Gresford Block.||||||27-JUL-04
24663|Ararat Formation|44797|14|Not recorded|p174|||||||||
24663|Ararat Formation|44833|14|Not recorded|p107-121|||||||||
24663|Ararat Formation|45088|5|Briefly described|p63|||Stratigraphy||||||31-JUL-08
24663|Ararat Formation|45097|6|Mentioned|Fig.|||Carboniferous correlation chart||||||
24663|Ararat Formation|46803|6|Mentioned|Fig. 3|||||||||
24663|Ararat Formation|47056|6|Mentioned|Fig.2 P523|||||||||
24663|Ararat Formation|50132|6|Mentioned|p246 Fig. 4|Early Carboniferous|Early Carboniferous|New England Fold Belt, Raymond Terrace area||||||
24663|Ararat Formation|50147|5|Briefly described|Map legend|Visean|Visean|Green to brown, thick to medium-bedded lithic sandstone, lensoidal units of grey, crossbedded oolitic and crinoidal limestone, cobble, conglomerate, minor mudstone and occasional ignimbrite. Geol. Province: Gresford Block||||||
24663|Ararat Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Tournaisian|Gresford Block, Tamworth Belt.||||||
26350|Archerfield Sandstone|22857|4|Described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Jerrys Plains Subgroup (Wittingham Coal Measures, Singleton Supergroup). Max. thickness: 25m. Geological Province: Sydney Basin.||||||03-MAR-06
26350|Archerfield Sandstone|29942|3|Fully described|p11|||||||||
26350|Archerfield Sandstone|29943|6|Mentioned|p37|||See also p39.||||||04-AUG-08
26350|Archerfield Sandstone|29944|6|Mentioned|Fig.18|||||||||
26350|Archerfield Sandstone|31375|6|Mentioned|p4|||Stratigraphy||||||
26350|Archerfield Sandstone|37087|5|Briefly described|p197|||||||||
26350|Archerfield Sandstone|38614|6|Mentioned|p1|||||||||
26350|Archerfield Sandstone|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26350|Archerfield Sandstone|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26350|Archerfield Sandstone|40166|6|Mentioned|p347|||See also Table 1||||||
26350|Archerfield Sandstone|40256|6|Mentioned|p304|||||||||
26350|Archerfield Sandstone|40330|6|Mentioned|p66|||See also Fig.4||||||
26350|Archerfield Sandstone|40805|6|Mentioned|p133|||||||||
26350|Archerfield Sandstone|41010|6|Mentioned|Fig.1|||||||||
26350|Archerfield Sandstone|41054|6|Mentioned|Fig.3|||||||||
26350|Archerfield Sandstone|41604|6|Mentioned|Table 1|||||||||
26350|Archerfield Sandstone|41902|5|Briefly described|p5 Table 1|||||||||
26350|Archerfield Sandstone|42182|5|Briefly described|p299|||||||||
26350|Archerfield Sandstone|42648|6|Mentioned|p37|||||||||
26350|Archerfield Sandstone|42916|5|Briefly described|Table 1||Late Permian|||||||
26350|Archerfield Sandstone|42922|6|Mentioned|Fig.14|||||||||
26350|Archerfield Sandstone|43017|5|Briefly described|Fig.1,p372|||||||||
26350|Archerfield Sandstone|43257|5|Briefly described|Map Legend||Late Permian|Of Wittingham Coal Measures.||||||
26350|Archerfield Sandstone|44244|4|Described|p237|Late Permian|Late Permian|Overlies Bulga Formation (Vane Subgroup); underlies Jerrys Plains Subgroup.  Max. thickess: >30m.||||||
26350|Archerfield Sandstone|50268|5|Briefly described|Map Legend|Tatarian|Tatarian|Geological Province: Sydney Basin. Of the Wittingham Coal Measures. Overlies Vane Subgroup. Underlies Jerrys Plains Subgroup.||||||25-SEP-08
26350|Archerfield Sandstone|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wittingham Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
26350|Archerfield Sandstone|61529|5|Briefly described|p857 Fig. 3a|||At base of Jerrys Plain Subgroup. Overlain by Jerrys Plains Group; overlies Bulga Formation. Geological Province: Sydney Basin.||||||
26350|Archerfield Sandstone|61770|6|Mentioned|p111|||Unconformably underlain by Foybrook Formation.||||||04-AUG-08
26350|Archerfield Sandstone|68003|5|Briefly described|p38 Fig.3-j, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Unit in Wittingham Coal Measures.||Overlies Bulga Formation. Is overlain by Jerrys Plains Subgroup.|Well-sorted quartz lithic sandstone.|
26350|Archerfield Sandstone|68004|5|Briefly described|p23 Table 1, p51 Table 5.|Late Permian|Late Permian|Hunter Coalfield.||Unit in Wittingham Coal Measures.||Overlies Bulga Formation and Vane Subgroup. Is overlain by Jerrys Plains Subgroup.|Massive well-sorted sandstone.|
26350|Archerfield Sandstone|69683|6|Mentioned|p411 Fig.2, p416 Fig.3|Late Permian|Late Permian|||Unit in Wittingham Coal Measures.||Overlies Vane Subgroup. Is overlain by Jerrys Plains Subgroup.||
26350|Archerfield Sandstone|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield.||Wittingham Coal Measures.||||
26350|Archerfield Sandstone|73304|6|Mentioned|p75|||||Whittingham Coal Measures, Singleton Supergroup||||
26350|Archerfield Sandstone|73625|5|Briefly described|p2|Permian|Permian|Hunter coalfield, Sydney Basin.||Wittingham Coal Measures.||Overlies Bulga Sandstone.||
31543|Ardlethan Suite|42726|5|Briefly described|map legend||Silurian|||||||
31543|Ardlethan Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone.||||||
31543|Ardlethan Suite|69043|6|Mentioned|p24||||||Ardlethan Granite.|||19-JAN-17
26253|Argalong Granite|42313|2|Defined|p162|Early Devonian|Early Devonian|Reserved May 1982.||||||
26253|Argalong Granite|42314|5|Briefly described|Map legend|Early Devonian||||||||
26253|Argalong Granite|42726|5|Briefly described|map legend|Silurian||||||||
28148|Argyle Formation|22768|6|Mentioned|p177|||||||||
28148|Argyle Formation|22857|5|Briefly described|p177, p480 App.1 Tb.A1.6|Early Devonian|Late Silurian|Of the Taralga Group. Max. thickness: 800m. Sandstone, arenite, greywacke, shale in turbiditic sequence. Geological Province: Murruin Basin.||||||
28148|Argyle Formation|32999|3|Fully described|p25|||Stratigraphy p20.||||||11-JUN-08
28148|Argyle Formation|34481|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
28148|Argyle Formation|37727|6|Mentioned|p36|||See also p87.||||||04-AUG-08
28148|Argyle Formation|40328|4|Described|p186|||||||||
28148|Argyle Formation|50234|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Taralga Group.  Underlies Whipbird Creek Formation.||||||11-JUN-08
28148|Argyle Formation|61892|5|Briefly described|p206|||Scheibner (1973).||||Conformably overlies Cobra Formation. Correlated with the Whipbird Creek Formation.|Thinly-bedded (<1m thick), deep-water, turbiditic arenites, lutites and siltstones.|
28148|Argyle Formation|63633|5|Briefly described|Map Legend|Pridolian|Ludlovian|Of Taralga Group. Flysch - like sequence, sandstones, arenite, greywacke, shale.||||||
28148|Argyle Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Grey, green, massive to graded and ripple x-laminated med.- to thick-bedded, poorly sorted, fine- to med.-gr. quartzose to lithic-quartzose sandstone, interbedded with green, purplish or reddish, graded, laminated fine-gr. sst.+silst||||||11-JUN-08
28148|Argyle Formation|68592|1|Redefined|p810, p813, p821-2, p829-835, p840-1|Pridoli|Ludlow|See also p118, p232, p326, p350, p360, p725-6, p728, p730-2 Fig.132, p736, p741, p744, p751, p757-9, p768, p771, p852 Fig.143, p856, p861-3, p873-4, p889. Retained in a form close to original definition (Scheibner 1973). Mapped previously as Lambie Group (Brunker and Offenberg 1970; Scheibner 1973), unnamed Ordovician and Upper Silurian (Brunker and Offenberg 1970), and as Argyle Formation and Whipbird Creek Formation within Taralga Group (Scheibner 1973). Type section is redefined from Scheibner (1973); representative section and other exposures are detailed. Thickness: 235 m (at type section), thins to north, and max thickness is ~650 m. Covan Creek, Boxers Creek, Carwoola and (former) Palerang Formations are probable correlatives. Indicated age: late Ludlow-Pridoli. Depositional environment: turbidity currents in a moderately deep marine environment and high-density debris flows in a shelf or slope depositional system. Metamorphism: regional, sub-greenschist to lower greenschist facies; and contact metamorphism adjacent to Forest Lodge Quartz Monzodiorite. Quarried for slate at Chatsbury; limited production continues. Classification and provenance plots. Is overlain by Rhyanna Formation conformably and by Lambie Group, Gundary Volcanics and Crookwell Basalt unconformably.||Unit in Mount Fairy Group.||Overlies Bendoc Group and Poidevins Sandstone unconformably and Kerrawary Siltstone and De Drack Formation conformably. Intruded by Forest Lodge Quartz Monzodiorite. See Comments for overlying units.|Packets of grey to white, medium-thick bedded, fine-medium grained, quartz and lithic-quartz sandstone, interbedded with packets of greenish grey and red, laminated to thinly bedded, rhythmically interbedded, fine-grained sandstone and siltstone.|
28148|Argyle Formation|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Sfa. Includes one unnamed unit of allochthonous algal limestone. On Taralga, and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group|Includes one unnamed unit.|Overlies De Drack Formation and Kerrawary Siltstone. Is overlain by Rhyanna Formation. Interleaves with Covan Creek Formation.|Medium-thick bedded, fine-medium grained, quartz and lithic quartz sandstone interbedded with laminated-thinly bedded, rhythmically interbedded, fine grained sandstone and siltstone; sandstone sporadically ripple cross laminated or slumped.|
28148|Argyle Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Mount Fairy Group|||Turbiditic sequence of sandstone, greywacke and shale.|
28148|Argyle Formation|70542|5|Briefly described|Map Legend|Devonian|Silurian|Includes one unnamed member of algal limestone.||Mount Fairy Group|||Medium-thick bedded, fine-medium grained quartz and lithic quartz sandstone, interbedded with packets of laminated-thinly bedded, interbedded fine-grained, normally graded with sporadic ripple cross-laminated, slumped sandstone and siltstone.|
28148|Argyle Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|||Medium-thick bedded, fine-medium grained, quartz and lithic quartz sandstone interbedded with laminated-thinly bedded, rhythmically interbedded, fine grained sandstone and siltstone; sandstone sporadically ripple cross laminated or slumped.|
28148|Argyle Formation|71069|5|Briefly described|p27, p76 fig 27, p90, p134|||Up to 233m thick. Deposited in a deep marine setting. See also  p137-138 fig 44, p142, p144, p151, p169.||Mount Fairy Group||Overlies the De Drack Formation. Overlain by the Rhyanna Formation. Equivalent to the Covan Creek Formation.|Lithic-quartz to quartzose, planar and ripple cross laminated sandstone, siltstone, slate and mudstone turbidite package.|
28148|Argyle Formation|71700|5|Briefly described|CD|||||||Equivalent to the Covan Creek Formation.||
73911|Argyll Suite|71628|5|Briefly described|p3: 19, 68|||||Hillgrove Supersuite.|Kimberley Park Monzogranite (tentative).|||
30027|Arkarula Formation|22857|5|Briefly described|p264, p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Brothers Subgroup (Black Jack Group). Fining-up sequence of fine to medium-grained lithic sandstone and siltstone with worm burrows. Age: 265Ma. Max. thickness: 51m. Geological Province: Sydney and Gunnedah Basins. ||||||
30027|Arkarula Formation|22864|6|Mentioned|p264||Late Permian|Max Age: 256 Ma.||||||
30027|Arkarula Formation|24159|5|Briefly described|p149|Permian|Permian|Geological Province: Gunnedah Basin.||||||17-SEP-08
30027|Arkarula Formation|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Of Brothers Subgroup. Replaces/supersedes Arkarula Sandstone Member of Black Jack Formation (now Black Jack Group). Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||13-NOV-13
30027|Arkarula Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Brothers Subgroup.||||||
30027|Arkarula Formation|61612|6|Mentioned|p272, p277, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Gunnedah Basin.||||||17-MAR-09
30027|Arkarula Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Brothers Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Lithic sandstone, laminite and siltstone.||||||
30027|Arkarula Formation|65116|4|Described|p444, 446, Fig 6 p441|Late Permian|Late Permian|Of Black Jack Group. Upward fining lithic sandstone with bioturbation and burrows.||||||
30027|Arkarula Formation|68003|5|Briefly described|p38 Fig.3-j, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Coeval with Brigalow Formation.||Unit in Brothers Subgroup.||Overlies Pamboola Formation. Is overlain by Hoskissons Coal.|Fining-up sequence of fine-medium lithic sandstone and siltstone with worm burrows.|
30027|Arkarula Formation|68004|5|Briefly described|p23 Table 1, p44 Table 3.|||Gunnedah Basin.||Upper unit in Brothers Subgroup.||Overlies Pamboola Formation. Is overlain by Hoskissons Coal.|Fining-up sequence from medium-grained sandstone with sub-vertical worm burrows to alternating sequences of poorly sorted sandstone and siltstone.|
30027|Arkarula Formation|70791|5|Briefly described|p277|Permian|Permian|Gunnedah Basin.||Brothers Subgroup.||||
30027|Arkarula Formation|70878|5|Briefly described|p717 Fig.12|Permian|Permian|In Santos Brawboy 1 well, shown in the well completion report as overlying Pamboola Formation, but subsequent reinterpretation has it absent.||Black Jack Group.||||
37004|Armidale beds|44093|5|Briefly described|p76 (photo)|Tertiary|Tertiary|Fluvial. Lateritic profile capping the exposure. Unconformably overlain by Sandon beds.||||||
37004|Armidale beds|44450|4|Described|p28|Early Oligocene|Late Eocene|Geological Province: New England Fold Belt||||||
37004|Armidale beds|71628|6|Mentioned|p3: 49|||||||Locally overlies Gostwyck Monzogranite.||
29572|Arramagong West Granite|22638|3|Fully described|p59|||Possibly related to Young Granodiorite. Probably Late Silurian.||||||
29572|Arramagong West Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
36829|Arranmor Ignimbrite Member|23859|2|Defined|p242 Appendix 1|Late Permian|Permian|See also page 933. Type locality 392000E, 6745000N. Of Emmaville Volcanics. Geological Province: New England Fold Belt. Max. thickness: 150 m.||||||
36829|Arranmor Ignimbrite Member|70876|5|Briefly described|p82|Late Permian|Late Permian||256.4 +/- 1.6 Ma (Black, 2006)|Emmaville Volcanics||||
36829|Arranmor Ignimbrite Member|72528|5|Briefly described|p2, p71, p109.|Lopingian|Lopingian|Occuring 40km north of Glen Innes.|256.4+/-1.6 Ma|Emmaville Volcanics||Intruded by Deepwater Syenogranite.||
77272|Arrowfield Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Mount Thorley Formation.||||
31547|Arthursleigh Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31547|Arthursleigh Suite|44093|5|Briefly described|P214 App. 1|Early Devonian|Early Devonian|Granite.||||||24-FEB-05
31547|Arthursleigh Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes named 8 granitic units and one unnamed unit - Torwood Granodiorite, Springponds Tonalite and Columba, Marula, Lumley, Mount Hannibal, Corridgery and Banshea Granites.||||||19-JUN-08
31547|Arthursleigh Suite|66300|5|Briefly described|pp76-80.|||Eastern Lachlan Orogen. Overall, units have a metaluminous, oxidised affinity. Plutons are broadly contemporaneous with the Bindook Group volcanics which they intrude.|||Includes Pleasant Hill and Marulan Granites.|Intrudes Bindook Group.||
31547|Arthursleigh Suite|68592|1|Redefined|p138, p1610-49|Early Devonian|Early Devonian|Defined by Chappell et al. (1991) with 4 other Suites as subdivision of Marulan Batholith. Named after Arthursleigh homestead. Comprises 12 plutons in a discontinuous, 95 by 25 km N-S belt. Fourteen plutons of the Arthursleigh Suite were incorrectly referred to as Marulan Suite in White et al. (2001). The Inverary Tonalite (Carr et al., 1979) was originally placed in the Arthursleigh Suite by Chappell et al. (1991) but is now assigned to the Carne Dacite Member of the Tangerang Formation. The Arthursleigh Tonalite is the type pluton. Geochemistry and metamorphism described. High magnetic susceptibility. Comagmatic with Bindook Group volcanics. A SHRIMP U-Pb zircon age of 416.7 +/- 3.1 Ma (Black, 2005) does not accord with established palaeontologic constraints. Potential for dimension stone and aggregate.|406 +/- 7 Ma (K-Ar biotite; Carr et al., 1980).|Unit in Marulan Supersuite.|Includes Banshea, Bullio, Uringalla, Columba, Mount Hannibal, Corridgery, Marulan and Lumley Granites; Springponds and Arthursleigh Tonalites; Torwood and Glenrock Granodiorites.|Intrudes and contact metamorphoses the Bindook Group. Comparable age and chemistry with Mandari, Bangadilly and Koo-rilla Suites.|Predominantly granite to granodiorite or tonalite, typically with biotite-hornblende mineralogy, divided into two groups: internally uniform composition, and more varied composition. All are massive and undeformed. I-type.|
31547|Arthursleigh Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Includes one unnamed member of microgranite dykes with high magnetic susceptibilities. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Banshea Granite, Corridgery Granite, Mount Hannibal Granite, Lumley Granite, Marulan Granite, Columba Granite, Springponds Tonalite, Torwood Granodiorite, and one unnamed unit.|||
31547|Arthursleigh Suite|70541|5|Briefly described|Map Legend|Devonian|Devonian||||||Microgranite dykes; high magnetic susceptibility.|
31547|Arthursleigh Suite|70542|5|Briefly described|Map Legend|Early Devonian|Early Devonian||||Includes Corridgery Granite, Mount Hannibal Granite, Lumley Granite, Marulan Granite, Springponds Tonalite, Torwood Granodiorite.|||
31547|Arthursleigh Suite|70543|5|Briefly described|Map Legend |Devonian|Devonian|Includes one unnamed member of microgranite dykes with high magnetic susceptibilities.|||Includes Banshea Granite, Corridgery Granite|||
31547|Arthursleigh Suite|70661|3|Fully described|vii, viii, p4, p9, p13, p31|Early Devonian|Early Devonian|Name derived from Arthursleigh property. Originally mapped as part of the undifferentiated Marulan Batholith. Comagmatic with Bindook Group. Generally poorly exposed as tors and low pavement outcrop forming a flat to gently undulating landscape. Arthursleigh Tonalite is regarded as the type pluton for this suite. Structure, metamorphism and geochemistry discussed. Minor base metal concentrations occur in the Banshea granite. See also p77 - p80, p243.|406 +/- 7 Ma, 416.7 +/- 3.1 Ma|Marulan Supersuite|Arthursleigh Tonalite, Marulan Granite, Pleasant Hill Granite, Glenrock Granodiorite, Bangadilly Granite, Johnniefelds granodiorite||Zoned to very homogenous granites to granodiorites or tonalites. Elsewhere they exhibit biotite-hornblende mineralogy.|
31547|Arthursleigh Suite|71303|5|Briefly described|map legend|Pragian|Pragian||||Includes Glenrock Granodiorite, Marulan Granite, Johnniefelds granodiorite, Pleasant Hill Granite, Arthursleigh Tonalite, Bangadilly Granite.|||
31547|Arthursleigh Suite|72528|5|Briefly described|p25, p108.|Lochkovian|Lochkovian|Ages from Banshea Granite, Pleasant Hills Granite.|413.3+/-1.8 Ma, 412.6+/-2.2 Ma|Marulan Supersuite|Includes Banshea Granite and Pleasant Hills Granite||Includes porphyritic granite.|
83667|Arumpo bentonites|73581|5|Briefly described|p28|||Murray Basin. Occurs 90 km northeast of Mildura. Originated from two separate volcanic events (Gardam et al., 2008). The lower bed was deposited in a marine environment, within a graben associated with the Neckarboo Fault. The overlying sediments are comprised of fluvial sequences and some additional bentonite formations.|||||Comprises 2 significant horizontal beds of bentonite that are 5-8 m thick, and are Na-Mg enriched.|
29663|Ashburnia Group|13139|5|Briefly described|p8, p9 Fig. 4|Llandovery|Llandovery|Limestone-shale succession.  Unconformably overlies the Angullong Formation.  Geological Province: Western Molong Volcanic Belt.||||||12-APR-05
29663|Ashburnia Group|22679|5|Briefly described|p 27|Silurian|Silurian|||||||
29663|Ashburnia Group|22857|5|Briefly described|p127, p426 App. 1 Tb. A1.5|||Includes Cadia Coach Shale and Bagdad Formation.||||||
29663|Ashburnia Group|23214|2|Defined|p103|Early Silurian|Early Silurian|Originally included in the Panuara Group. Then named Cadia Group when separated from Panuara Group. Since changed due to similarity with consitituent unit. Max thickness 205m.||||||17-MAY-16
29663|Ashburnia Group|23245|6|Mentioned|p127|||||||||
29663|Ashburnia Group|23309|6|Mentioned|p390|||||||||
29663|Ashburnia Group|23334|5|Briefly described|9 Fig.4|Early Silurian|Early Silurian|||||||
29663|Ashburnia Group|24398|5|Briefly described|p259 Fig. 2|Llandovery|Llandovery|Geological Province: Lachlan Fold Belt.||||||
29663|Ashburnia Group|43640|5|Briefly described|Map Legend||Silurian|||||||
29663|Ashburnia Group|43642|5|Briefly described|Map Legend|Silurian|Silurian|Includes Bagdad Formation and Cadia Coach Shale.||||||17-JUL-08
29663|Ashburnia Group|43654|5|Briefly described|Map Legend|Silurian|Silurian|Includes Cadia Coach Shale.||||||
29663|Ashburnia Group|43782|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||
29663|Ashburnia Group|44093|5|Briefly described|p202 App. 1|Early Silurian|Early Silurian|||||||
29663|Ashburnia Group|60989|6|Mentioned|p113|||||||Is overlain by the Waugoola Group.||
29663|Ashburnia Group|63278|6|Mentioned|p147 Fig. 2b, p154|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
29663|Ashburnia Group|63283|6|Mentioned|p195 Fig. 2|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29663|Ashburnia Group|63287|6|Mentioned|p317 Fig. 2|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29663|Ashburnia Group|63290|5|Briefly described|p385, p392 Tb. 1, p401 Fig. 5(d)|Llandovery|Llandovery|Includes; Wire Gully Lst Mbr, Bridge Creek Lst Mbr, Bagdad Fm + Cadia Coach Shale. Underlain unconformably Angullong Formation. Consists of shallow-water conglomerate, sandstone, and limestone overlian by graptolitic deeper water shale and siltstone.||||||
29663|Ashburnia Group|64826|5|Briefly described|p1040 Tb. 1|Landovery|Llandovery|||||||
29663|Ashburnia Group|70297|4|Described|map legend, on side 2 of map sheet|Llandovery|Llandovery|Age: early to middle Llandovery. Interpreted as a marginal shallow to deep water facies to the upper portion of a volcaniclastic fan formed during Phase 4 volcanism. Erosional base.|||Bagdad Formation, Cadia Coach Shale|Is disconformably overlain by Waugoola Group.|Grey-green feldspathic siltstone, graptolitic mudstone; thin-bedded graded fine-grained sandstone to siltstone upsequence; sporadic thin limestone conglomerate lenses; fossiliferous siltstone, algal limestone, massive-bedded fossiliferous limestone.|
29663|Ashburnia Group|70684|5|Briefly described|p34, p50-52, p75|Early Silurian|Early Silurian|Molong Volcanic Belt. Llandovery.|||Cadia Coach Shale, Bagdad Formation.|Unconformably overlies (inferred) Angullong Formation.||
29663|Ashburnia Group|71091|6|Mentioned|p143|Early Silurian|Early Silurian||||Wire Gully Limestone Member.|||
25701|Ashfield Shale|22731|6|Mentioned|p536|||||||||
25701|Ashfield Shale|22745|6|Mentioned|Fig14,p138|||Wianamatta Group, Sydney Basin.||||||
25701|Ashfield Shale|22857|4|Described|p530 App.1 Tb.A1.9|Middle Triassic|Middle Triassic|Of the Wianamatta Group. Black to light grey shale and laminite. Max. thickness: 61.6m. Geological Province: Sydney Basin. See also p265 (photo 3).||||||24-FEB-06
25701|Ashfield Shale|22864|6|Mentioned|p265|||||||||
25701|Ashfield Shale|22865|6|Mentioned|p309|||||||||
25701|Ashfield Shale|22969|5|Briefly described|p 26|||||||||
25701|Ashfield Shale|23218|6|Mentioned|p30|||||||||
25701|Ashfield Shale|24117|5|Briefly described|p3|||Of Wianamatta Group. Geological Basin: Sydney Basin.||||||
25701|Ashfield Shale|24123|5|Briefly described|p3|||Of Wianamatta Group. Geological Province: Sydney Basin.||||||
25701|Ashfield Shale|29361|6|Mentioned|p4|||||||||
25701|Ashfield Shale|29901|4|Described|Table 1|||||||||
25701|Ashfield Shale|30132|4|Described|p4|||||||||
25701|Ashfield Shale|30285|4|Described|p546|||||||||
25701|Ashfield Shale|30286|5|Briefly described|p1094|||Upper Triassic age. See also P1096-1100||||||
25701|Ashfield Shale|31056|5|Briefly described|p3|||||||||
25701|Ashfield Shale|31128|6|Mentioned|p7|||||||||
25701|Ashfield Shale|31296|6|Mentioned|p29|||||||||
25701|Ashfield Shale|31381|6|Mentioned|p55|||||||||
25701|Ashfield Shale|31725|6|Mentioned|p4|||||||||
25701|Ashfield Shale|31887|5|Briefly described|p9|||||||||
25701|Ashfield Shale|32187|6|Mentioned|p6|||||||||
25701|Ashfield Shale|32801|6|Mentioned|Fig.10|||||||||
25701|Ashfield Shale|33671|6|Mentioned|p3|||||||||
25701|Ashfield Shale|33872|6|Mentioned|Fig.1|||||||||
25701|Ashfield Shale|34010|6|Mentioned|Cor. chart|||Mid Triassic.  Wianamatta Gp.||||||
25701|Ashfield Shale|34034|6|Mentioned|p554|||||||||
25701|Ashfield Shale|34205|4|Described|p34|||||||||
25701|Ashfield Shale|34209|6|Mentioned|p148|||Triassic. Table 1.||||||
25701|Ashfield Shale|34228|6|Mentioned|p171|||||||||
25701|Ashfield Shale|34242|6|Mentioned|p417|||||||||
25701|Ashfield Shale|34243|6|Mentioned|p423|||Plant microfossils||||||
25701|Ashfield Shale|34274|6|Mentioned|p121|||U.Triassic||||||
25701|Ashfield Shale|34305|3|Fully described|p418|||Triassic||||||
25701|Ashfield Shale|34306|5|Briefly described|p443|||||||||
25701|Ashfield Shale|34490|6|Mentioned|p69|||||||||
25701|Ashfield Shale|34506|6|Mentioned|p408|||||||||
25701|Ashfield Shale|35062|6|Mentioned|p279|||||||||
25701|Ashfield Shale|35095|6|Mentioned|p116|||||||||
25701|Ashfield Shale|35098|6|Mentioned|p4|||P5.||||||
25701|Ashfield Shale|35312|6|Mentioned|p3|||||||||
25701|Ashfield Shale|35502|5|Briefly described|p174|||Described from point of view of occurrence of guiliemites.||||||
25701|Ashfield Shale|35690|1|Redefined|p176|Middle Triassic|Middle Triassic|||||||
25701|Ashfield Shale|36042|6|Mentioned|Fig.22|||||||||
25701|Ashfield Shale|36121|6|Mentioned|p25|||||||||
25701|Ashfield Shale|36220|6|Mentioned|p91|||||||||
25701|Ashfield Shale|36222|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
25701|Ashfield Shale|37322|6|Mentioned|p723|||||||||
25701|Ashfield Shale|37757|6|Mentioned|p29|||||||||
25701|Ashfield Shale|38206|6|Mentioned|p53|||Clay resources||||||
25701|Ashfield Shale|38784|6|Mentioned|p78|||||||||
25701|Ashfield Shale|39287|6|Mentioned|p50|||See also Fig.2.18||||||
25701|Ashfield Shale|39293|5|Briefly described|p160|||||||||
25701|Ashfield Shale|39298|3|Fully described|p262|||||||||
25701|Ashfield Shale|39306|6|Mentioned|p389|||See also P425,P426||||||
25701|Ashfield Shale|39308|6|Mentioned|p504|||||||||
25701|Ashfield Shale|39626|6|Mentioned|p275|||||||||
25701|Ashfield Shale|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
25701|Ashfield Shale|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
25701|Ashfield Shale|40592|5|Briefly described|p229|||||||||
25701|Ashfield Shale|40602|3|Fully described|p22|||||||||
25701|Ashfield Shale|40603|6|Mentioned|p1|||||||||
25701|Ashfield Shale|40625|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
25701|Ashfield Shale|40629|6|Mentioned|p184|||||||||
25701|Ashfield Shale|40630|6|Mentioned|p173|||||||||
25701|Ashfield Shale|40631|6|Mentioned|p156|||||||||
25701|Ashfield Shale|40651|6|Mentioned|Table 6|||||||||
25701|Ashfield Shale|40653|6|Mentioned|p121|||||||||
25701|Ashfield Shale|40654|6|Mentioned|p116|||||||||
25701|Ashfield Shale|40767|6|Mentioned|p14|||||||||
25701|Ashfield Shale|40870|6|Mentioned|p7|||||||||
25701|Ashfield Shale|41391|6|Mentioned|p49|||||||||
25701|Ashfield Shale|41639|6|Mentioned|p9|||||||||
25701|Ashfield Shale|41939|5|Briefly described|p27|||||||||
25701|Ashfield Shale|42737|5|Briefly described|map legend|Triassic||||||||
25701|Ashfield Shale|42896|3|Fully described|p40, Table 2|||of Wianamatta Group, see also Fig.7||||||
25701|Ashfield Shale|42925|4|Described|p17|||of Wianamatta Group||||||
25701|Ashfield Shale|42926|4|Described|map legend||Middle Triassic|||||||
25701|Ashfield Shale|43194|5|Briefly described|p122, p131|Middle Triassic|Middle Triassic|Sydney Basin. Shallow-marine or estuarine laminated silt. Time equivalent to the middle part of the Napperby Formation, Gunnedah Basin.||||||
25701|Ashfield Shale|43317|5|Briefly described|Table 1 p13|||||||||
25701|Ashfield Shale|43318|14|Not recorded|opp p6||Late Triassic|||||||
25701|Ashfield Shale|43319|14|Not recorded|Map Legend|||||||||
25701|Ashfield Shale|43320|14|Not recorded|Table1 p13,14|||Part of Liverpool Sub-group||||||
25701|Ashfield Shale|43344|14|Not recorded|p22,24,29,30,36,47||Triassic|Unit of Wianamatta Group. p39-44,50-52,57,58,61-66,69,71,170,173,182,186||||||
25701|Ashfield Shale|43365|14|Not recorded|p169-210||Triassic|||||||
25701|Ashfield Shale|43373|14|Not recorded|p163|||||||||
25701|Ashfield Shale|43383|14|Not recorded|p23|||Part of Liverpool Sub-Group||||||
25701|Ashfield Shale|43385|14|Not recorded|p182 Table||Late Triassic|Ref to Crook 1957 (Keiper)||||||
25701|Ashfield Shale|43395|14|Not recorded|map|||||||||
25701|Ashfield Shale|43880|14|Not recorded|p58|||||||||
25701|Ashfield Shale|43980|14|Not recorded|Pl.1|||||||||
25701|Ashfield Shale|45018|14|Not recorded|p167-9,171-9,184-5|||||||||
25701|Ashfield Shale|45090|6|Mentioned|p72|||Palynological zones||||||
25701|Ashfield Shale|60281|6|Mentioned|p64 |Triassic|Triassic|Shallow marine or estuarine laminated silt sequence.||||||
25701|Ashfield Shale|60726|5|Briefly described|p3-4.|Anisian|Anisian|See also references to Ashfield Formation. Formerly known as the Wianamatta Shales. 40-60m thick. Contains a diverse fauna (listed). Extensively quarried for house bricks.||Wianamatta Group.||Overlies the Mittagong Formation.|Siltstone and clay.|
25701|Ashfield Shale|61315|5|Briefly described|p176|||Of the lower Wianamatta Group. Shallow marine deposits; promary inferred reservoir seal in the offshore part of basin. Geological Province: Sydney Basin||||||
25701|Ashfield Shale|65195|5|Briefly described|p3, p4 Fig.2, p13 Fig.4, p28 Fig.9|Triassic|Triassic|Most extensive Formation in Wianamatta Group. Dark grey to black sideritic siltstone-claystone, grading up into a fine sandstone-siltstone. Overlies Mittagong Formation||||||
25701|Ashfield Shale|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Wianamatta Group.||||
25701|Ashfield Shale|67560|6|Mentioned|p263-p269, p271 Fig.12|||||||Underlain by the Hawkesbury Sandstone.||
25701|Ashfield Shale|67663|6|Mentioned|p521|Triassic|Triassic|||Of the Wianamatta Group||||
25701|Ashfield Shale|70661|3|Fully described|p199, p203, p209-p214|Middle Triassic|Middle Triassic|Named after the suburb of Ashfield.Distribution, distinguishing characteristics, structure, geomorphology, geochemistry and fossil assemblage discussed. 35-61.5m thick. Deposited in lacustrine to brackish or shallow marine environment.||Wianamatta Group|Mulgoa Laminite Member, Regentville Siltstone Member, Kellyville Laminite Member, Rouse Hill Siltstone Member.|Disconformably? overlies Hawkesbury Sandstone, Mittagong Formation, Overlain conformably by Minchinbury Sandstone|Shale, dark grey to black sideritic claystone -siltstone and laminated fine grained sandstone and siltstone. Sandstone contains cross laminations and is bioturbated.|
25701|Ashfield Shale|71303|5|Briefly described|map legend|Middle Triassic|Middle Triassic|Of Sydney Basin.||Of Wianamatta Group.|||Light grey to chocolate brown sideritic claystone to siltstone; dark-grey to black when fresh. Intercalated sandstone/siltstone laminite. Sandstone is quartzose with minor mlabile content. Rare plant fossils.|
25701|Ashfield Shale|73248|6|Mentioned|p301, p307, App. p3|Middle Triassic|Middle Triassic|||Wianamatta Group||Unconformably overlain by Rickabys Creek Gravel.||
25701|Ashfield Shale|73304|6|Mentioned|p76|||||||||
25701|Ashfield Shale|75059|6|Mentioned|p4, 9-10|Middle Triassic|Middle Triassic|Sydney Basin.||Wianamatta Group.||Is overlain by Minchinbury Sandstone.||
77318|Ashford Member|68005|5|Briefly described|pp37-39.|Early Permian|Early Permian|Contains the economically important Ashford seam; bituminous, medium volatile, high rank coking coal. 2.5 to 17 m thick; extreme local variability due to small-scale step faulting.||Basal unit in Ashford Coal Measures.||Overlies Texas beds unconformably. Is overlain by Bonshaw Member.|Coal, conglomerate.|
27696|Ashton Member|5250|6|Mentioned|p45||Late Ordovician|Member of Regans Creek Limestone.||||||
27696|Ashton Member|23214|3|Fully described|p49|Eastonian|Eastonian|Of Regans Creek Limestone. 41 m thick at type section.||||||
27696|Ashton Member|24398|5|Briefly described|p264, p259 Fig. 2|Eastonian|Eastonian|Of Regans Creek Limestone.  Geological Province: Lachlan Fold Belt.||||||
27696|Ashton Member|32151|3|Fully described|p200|||||||||
27696|Ashton Member|32590|6|Mentioned|p10|||||||||
27696|Ashton Member|38219|5|Briefly described|p300|||||||||
27696|Ashton Member|40136|6|Mentioned|p38|||||||||
27696|Ashton Member|42479|5|Briefly described|p109|||||||||
27696|Ashton Member|63287|6|Mentioned|p333|||Of the Regans Creek Limestone. Located at the base of Regans Creek Limestone.||||||07-FEB-11
31545|Ashvale Suite|42726|5|Briefly described|map legend||Silurian|||||||
33796|Asylum Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Foliated to massive, porphyritic biotite granite.||||||
33796|Asylum Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Crooked Corner Suite. Foliated to massive biotite granite; intruded by massive to foliated, porphyritic and myarolitic, allanite-bearing biotite microgranite and subspherulitic rhyolite.||||||09-SEP-08
33796|Asylum Granite|68592|3|Fully described|p1466-74|Early Devonian|Early Devonian|New name, after Asylum Creek. Placed in Crooked Corner Suite by Blevin (2011). Initially part of Wyangala Batholith (Stevens, 1955); later grouped with the Yarra Granite by Chappell et al. (1991). Deeply weathered and poorly exposed. Type area described. Geochemistry detailed (similar to Binda Granite); geophysical properties described. Hosts a lead prospect in quartz veins.||Unit in Crooked Corner Suite.||Intrudes Cuddyong Formation.|Grey to pink, generally medium-grained, massive to foliated, commonly porphyritic, hornblende-biotite granite and granodiorite; marginal phase of cream, aphanitic rhyolite and quartz-feldspar porphyry to S and E. I-type.|
33796|Asylum Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dra. Includes one unnamed sub unit of aphantic rhyolite and quartz-feldspar porphyry. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Crooked Corner Suite|Includes one unnamed subunit.||Medium-grained, massive-foliated, commonly porphyritic, hornblende-biotite granite and granodiorite; low K, Th and U response.|
33796|Asylum Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed sub unit of aphantic rhyolite and quartz-feldspar porphyry.||Crooked Corner Suite|Includes one unnamed subunit||Medium-grained, massive-foliated, commonly porphyritic, hornblende-biotite granite and granodiorite; low K, Th and U response.|
41049|Attunga Creek Monzogranite|24366|5|Briefly described|p6, 16 Fig. 3|Early Triassic|Late Permian|Of the Moonbi Plutonic Suite.||||||
41049|Attunga Creek Monzogranite|65398|5|Briefly described|p5 Tb.1, p8-9, Fig 3|Early Triassic|Late Permian|Intrudes the Wandsworth Volcanic Group. Unit in Moonbi Supersuite. Incorporates dismembered portions of Woodsreef Melange. Massive, weakly to strongly porphyritic, biotite-hornblende monzogranite. Results in large contact aureoles of albite-epidote to upper hornblende facies. Age: 248 +/- 5 Ma (biotite) K-Ar from Cooper et al. (1963) recalculated by Kent (1993).||||||
41049|Attunga Creek Monzogranite|66720|5|Briefly described|Map legend|Early Triassic|Late Permian|||Unit in Moonbi Supersuite.|||Massive, weakly to strongly porphyritic, biotite-hornblende monzogranite.|
41049|Attunga Creek Monzogranite|68005|5|Briefly described|p67, p133.|Permian|Permian|Listed on p.133 as a unit in Moonbi Supersuite. K-Ar age from Cooper et al. (1963). Radiometric and magnetic imagery has revealed previously unrecognised zoning in this unit. Moderate to high K, Th and U.|248 +/- 5 Ma (biotite).|Unit in Southern Moonbi Supersuite.|||Massive, medium- to coarse-grained biotite and hornblende monzogranite with prominent pink K-feldspar crystals, and minor titanite and magnetite grains.|
41049|Attunga Creek Monzogranite|68006|6|Mentioned|p143, p146.|||Mo mineralisation is accompanied by tungsten and chalcopyrite in quartz veins or disseminated in pegmatite. The skarn-like Kensington Scheelite deposit is 2 km NW of this unit.||||||
41049|Attunga Creek Monzogranite|68111|5|Briefly described|p968 Tb.1|Olenekian|Olenekian||ca. 249 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
41049|Attunga Creek Monzogranite|69323|4|Described|p20-21,70|Lopingian|Lopingian|Geological province: New England Orogen. Shaw et al., 1994 reported Rb-Sr age of c. 249 Ma, which aligns with Rb-Sr ages of other granites in Moonbi Supersuite. The SHRIMP U-Pb age of 255.8+\-1.3 Ma for the 'Attunga Creek volcanics' is consistent with the Moonbi Supersuite granites, and can be inferred that the 'Attunga Creek volcanics' and Attunga Creek Monzogranite are co-magmatic.|c. 249 Ma (Rb-Sr; Shaw et al., 1994)|Unit of Moonbi Supersuite.||Intrudes into, and metamorphoses 'Attunga Creek volcanics'.||
41049|Attunga Creek Monzogranite|69639|4|Described|p2, p6, p8-p9, p211-p218, p241|Changhsingian|Changhsingian|New England Orogen. Sampling locality, petrography and geochronology are discussed.|253.5 +/- 1.4 Ma (SHRIMP U-Pb)|Moonbi Supersuite||Intrudes the Wandsworth Volcanic Group, Whitlow Formation and the Silver Gully Formation.|Medium-grained, mildly porphyritic grey to pale-pink monzogranite.|
41049|Attunga Creek Monzogranite|71628|4|Described|p7: 2, 4-9, 19, 22-23, 31|||First published by Brown (2003), after Chappell and Bryant (1994). Originally Attunga Creek Adamellite (Chappell, 1961). Named after a local stream. Occurs ~8 km W of Bendemeer and 20 km NNE of Tamworth; outcrop area c. 67 km2. Contains a pendant of Wandsworth Volcanic Group rocks. Is concentrically zoned. Mineralogy detailed; geochemistry described. Associated with several small W-Mo-bearing vein and skarn deposits, and the Kensington Cu-Au skarn deposit.|253.5 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Attunga Creek Suite.||Intrudes Cara and ?Wiseman Arm Formations. Is overlain by comagmatic Wandsworth Volcanic Group.|Medium- to coarse-grained, weakly to strongly porphyritic, biotite-hornblende monzogranite, with rare granodiorite. I-type.|
40176|Attunga Eclogite|24599|5|Briefly described|p499|Neoproterozoic|Neoproterozoic|Geological Province: New England Orogen||||||20-JUN-13
23347|Avenall Basic Intrusive Complex|22768|6|Mentioned|p156|||||||||
23347|Avenall Basic Intrusive Complex|22857|6|Mentioned|p156|||||||||
23347|Avenall Basic Intrusive Complex|37529|5|Briefly described|p6|||||||||
23347|Avenall Basic Intrusive Complex|40678|5|Briefly described|p13|||||||||
23347|Avenall Basic Intrusive Complex|42313|4|Described|p50|Late Silurian|Early Silurian|||||||
23347|Avenall Basic Intrusive Complex|42314|5|Briefly described|Map|Middle Silurian|Early Silurian|||||||
23347|Avenall Basic Intrusive Complex|42828|5|Briefly described|Fig.2 P128|||||||||
24675|Avoca Valley Shale|22857|4|Described|p458 App.1, Tb.A1.6|Wenlockian|Wenlcokian|Of the Cudal Group. Green and red-brown shale, coarse garnetiferous arenite, conglomerate. Max. thickness: 370m. Geological Province: Cowra Trough.||||||
24675|Avoca Valley Shale|23214|3|Fully described|p118|Ludlow|Wenlock|Of Cudal Group. Originally named Upper Avoca Valley Shale. Intruded by Cowra Granodiorite. 370m thick at type section.||||||
24675|Avoca Valley Shale|31852|6|Mentioned|p718|||||||||
24675|Avoca Valley Shale|32590|6|Mentioned|Fig.2|||||||||
24675|Avoca Valley Shale|33006|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24675|Avoca Valley Shale|33282|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24675|Avoca Valley Shale|33285|5|Briefly described|p20|||||||||
24675|Avoca Valley Shale|34405|6|Mentioned|p122|||Fig.3.9||||||
24675|Avoca Valley Shale|34406|6|Mentioned|p219|||Lower part ?Upper Llandoverian||||||
24675|Avoca Valley Shale|37727|5|Briefly described|p36|||||||||
24675|Avoca Valley Shale|39655|6|Mentioned|Plate 1|||||||||
24675|Avoca Valley Shale|40328|2|Defined|p73|Silurian|Silurian|Also mentioned on p10||||||05-AUG-08
24675|Avoca Valley Shale|43515|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition) (M.Sil)||||||
24675|Avoca Valley Shale|43516|14|Not recorded|Map Legend||Early Silurian|(M.Sil.)||||||
24675|Avoca Valley Shale|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of green and red-brown shale, coarse garnetiferous sandstone, conglomerate.||||||15-JUL-08
24675|Avoca Valley Shale|43782|5|Briefly described|Map Legend|Ludlow|Wenlock|of Cudal Group.||||||
24675|Avoca Valley Shale|63287|5|Briefly described|p317 Fig. 2|Ludlow|Wenlock|Of the Cudal Group. Overlain by Ghost Hill Formation, underlain by Canowindra Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
24675|Avoca Valley Shale|63288|6|Mentioned|p359|||Underlain by Gospel Oak Shale.||||||
24675|Avoca Valley Shale|64994|5|Briefly described|p7|Ludlow|Wenlock|Of Pickett (1982). Contains graptolites.||||||07-FEB-11
24675|Avoca Valley Shale|67847|5|Briefly described|p33|||Graptolite fauna briefly discussed. ||||Disconformably overlies the Canowindra Volcanics. Overlain by the Ghost Hill Formation.||
24675|Avoca Valley Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group||||
29277|Avondale Granite|42726|5|Briefly described|map legend|Carboniferous||27. Variation on the informal Avondale complex?||||||
29277|Avondale Granite|71206|6|Mentioned|p373|||Named by Wormald (1991). The pluton was named Wattle Park Granite, also in 1991, by Chappell et al. Lachlan Fold Belt.||||||
24603|Baal Bone Formation|22578|6|Mentioned|p391|||||||||
24603|Baal Bone Formation|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Charbon Subgroup (Illawarra Coal Measures). Mudstone, siltstone, claystone, bioturbation. Max. thickness: 24m. Geological Province: Sydney Basin.||||||
24603|Baal Bone Formation|38614|6|Mentioned|p14|||||||||
24603|Baal Bone Formation|39232|4|Described|p110|||||||||
24603|Baal Bone Formation|40166|6|Mentioned|p348|||See also Table 1||||||
24603|Baal Bone Formation|40256|6|Mentioned|p305|||Mention Fig.3||||||
24603|Baal Bone Formation|40321|6|Mentioned|p19|||||||||
24603|Baal Bone Formation|40332|6|Mentioned|Fig.4|||||||||
24603|Baal Bone Formation|40806|2|Defined|p156|Permian|Permian|Prob. Permian||||||
24603|Baal Bone Formation|42182|6|Mentioned|p299|||||||||
24603|Baal Bone Formation|42657|4|Described|p81|||Western Coalfield. Synonymous with Denman Formation, Hunter Coalfield.||||||
24603|Baal Bone Formation|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
24603|Baal Bone Formation|43194|5|Briefly described|p112, p129 Tb. 8.3, p130|Late Permian|Late Permian|Of Illawarra Coal Measures, Western Coalfield, Sydney Basin. Correlates with an organic-rich mudstone unit (now part of Clare Sandstone) within the upper part of the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
24603|Baal Bone Formation|61315|5|Briefly described|p182|Late Permian|Late Permian|Marine incursion into Late Permian coal measures - offers good hydrocarbon source potential. ||||||
24603|Baal Bone Formation|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Late Permian.||Of the Illawarra Coal Measures.||||
24603|Baal Bone Formation|68003|5|Briefly described|p38 Fig.3-j.|Late Permian|Late Permian|Western Coalfield, Brigalow Belt South Bioregion.||Unit in Charbon Subgroup.||||
24603|Baal Bone Formation|73625|6|Mentioned|p2|Permian|Permian|Western coalfield, Sydney Basin.||Illawarra Coal Measures.||Is overlain by Angus Place Sandstone.||
24168|Baan Baa Formation|40952|4|Described|p5|||||||||
24168|Baan Baa Formation|70791|6|Mentioned|p281|||After Thomson (1986). Subsequently the Leard Formation.||||||
23349|Babepercy Volcanics|22857|5|Briefly described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|Part of the Coombadhja Volcanic Complex within the Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
23349|Babepercy Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Coombadjha Volcanic Complex.  Bedded volcaniclastic rocks and fine-grained silicic porphyry.||||||20-DEC-04
23349|Babepercy Volcanics|23812|5|Briefly described|p29 Tb.3|Late Permian|Early Permian|Of Coombadjha Volcanic Complex. Maximum thickness: ~100m.||||||
23349|Babepercy Volcanics|41041|3|Fully described|p265|||||||||
23349|Babepercy Volcanics|42378|5|Briefly described|Table 1 P6, Fig.1 P5|||Coombadjha Volcanic Complex.||||||
23349|Babepercy Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Coombadjha Volcanic Complex.||||||
25702|Babinda Volcanics|22768|6|Mentioned|p170|||||||||
25702|Babinda Volcanics|22857|4|Described|p170, p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Kopyje Group (Cobar Supergroup). Lavas and pyroclastics - interfinger with Baledmund Formation. Max. thickness: >1.5m. Geological Province: Kopyje Shelf (Darling Basin).||||||
25702|Babinda Volcanics|23171|5|Briefly described|p15,31|||||||||
25702|Babinda Volcanics|23173|4|Described|Map Legend|Lochkovian|Lochkovian|||||||
25702|Babinda Volcanics|29987|4|Described|p17|||||||||
25702|Babinda Volcanics|31016|6|Mentioned|p23|||||||||
25702|Babinda Volcanics|31018|6|Mentioned|Fig. 2|||||||||
25702|Babinda Volcanics|31161|5|Briefly described|PA3|||||||||
25702|Babinda Volcanics|31993|6|Mentioned|p677|||||||||
25702|Babinda Volcanics|32087|4|Described|p10|||||||||
25702|Babinda Volcanics|32088|6|Mentioned|p2|||U.Silurian||||||
25702|Babinda Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
25702|Babinda Volcanics|32672|6|Mentioned|p672|||||||||
25702|Babinda Volcanics|32674|6|Mentioned|p31|||||||||
25702|Babinda Volcanics|33004|6|Mentioned|p171|||||||||
25702|Babinda Volcanics|33340|6|Mentioned|p33|||||||||
25702|Babinda Volcanics|34057|6|Mentioned|Map legend|Silurian|Silurian|||||||
25702|Babinda Volcanics|34404|6|Mentioned|Fig.3.8|||Silurian?||||||
25702|Babinda Volcanics|34406|6|Mentioned|p220|||Probably Middle Silurian||||||
25702|Babinda Volcanics|34449|4|Described|Table 2-1|||U.Silurian - L.Devonian||||||
25702|Babinda Volcanics|34469|6|Mentioned|p108|||Table. Silurian? See also P115||||||
25702|Babinda Volcanics|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
25702|Babinda Volcanics|35219|6|Mentioned|p16|||||||||
25702|Babinda Volcanics|35287|6|Mentioned|p7|||||||||
25702|Babinda Volcanics|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
25702|Babinda Volcanics|37727|4|Described|p36|||||||||
25702|Babinda Volcanics|39214|6|Mentioned|p15|||See also Table 11||||||
25702|Babinda Volcanics|39618|1|Redefined|p55|Early Devonian|Early Devonian|||||||
25702|Babinda Volcanics|40328|6|Mentioned|p35|||||||||
25702|Babinda Volcanics|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25702|Babinda Volcanics|41528|2|Defined|p44|Early Devonian||||||||
25702|Babinda Volcanics|41529|6|Mentioned|Map legend|Lochkovian||||||||
25702|Babinda Volcanics|42467|5|Briefly described|Map Legend|||||||||
25702|Babinda Volcanics|42566|3|Fully described|p48|||||||||
25702|Babinda Volcanics|42568|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
25702|Babinda Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
25702|Babinda Volcanics|43032|5|Briefly described|Table 1.|||||||||
25702|Babinda Volcanics|43089|5|Briefly described|Map Legend|||of Kopyje Group||||||
25702|Babinda Volcanics|43389|14|Not recorded|Map Legend||Silurian|||||||
25702|Babinda Volcanics|43398|14|Not recorded|Map Legend||Silurian|||||||
25702|Babinda Volcanics|48958|6|Mentioned|p3|||See also P8||||||
25702|Babinda Volcanics|65469|5|Briefly described|p15-p17|Early Devonian|Late Silurian|Lachlan Orogen.||Kopyje Group||||
25702|Babinda Volcanics|67416|6|Mentioned|p84-85|||Canbelego-Mineral Hill Volcanic Belt.||Kopyje Group.|||I-type.|
25702|Babinda Volcanics|70751|5|Briefly described|p5, p7, p12, p17, p21, 22|||Also misspelt as the Badinda Volcanics on p22.||Kopyje Group||Interfingers with the Baledmund Formation.|Thick felsic volcanic rocks.|24-SEP-19
25702|Babinda Volcanics|70876|4|Described|p1, p3, p9-p15, p76, p94|Devonian|Silurian|Lachlan Orogen. I-type geochemistry. SHRIMP age is interpreted as the age of magmatic crystallisation. Deposited in a shallow marine age. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|418.9 +/- 2.5 Ma (SHRIMP U-Pb)|Kopyje Group||Interfingers with (and overlies) the Baledmund Formation.|Dark grey, moderately crystal-rich and locally vesicular porphyritic rhyolite.|
25702|Babinda Volcanics|70950|6|Mentioned|p1030|||Geological province: Central Lachlan Orogen. Forms part of the Canbelego-Mineral Hill Volcanic Belt.||Unit of Kopyje Group.||Interfingers with Baledmund Formation.|Thick felsic volcanics.|
25702|Babinda Volcanics|71039|5|Briefly described|p11-12, p25|Devonian|Silurian|Consistently preserve zeolite to epizone greenschist facies rift basin metamorphic mineral assemblages. Many samples are partly recrystallised and hydrated.||Kopyje Group||||08-MAR-23
25702|Babinda Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Kopyje Group.|||Aphyric to sparsely plagioclase +/- quartz-phyric coherent, often amygdular to vesicular dacitic lava, pumice-rich volcanic sandstone, and less abundant vitric-rich volcanic siltstone, crystal-lithic volcanic sandstone and volcanic lithic breccia.|
25702|Babinda Volcanics|72080|5|Briefly described|p5-p7, p9, p12, p13|Early Devonian|Late Silurian|Harts Tank area.||Kopyje Group||Interfingers with the Baledmund Formation.|Felsic volcaniclastics.|07-JAN-22
25702|Babinda Volcanics|72958|6|Mentioned|p11|Lochkovian|Pridoli|Cobar Basin. Nymagee area.||||Equivalent to Baledmund Formation and Mount Knobby Formation.||
25702|Babinda Volcanics|73174|6|Mentioned|p1038|||Kopyje Shelf.|||||Rhyolite and rhyodacite ashflow and airfall tuffs.|
25702|Babinda Volcanics|73578|6|Mentioned|p7, p14, p21, p32, p35|Lochkovian|Pridoli|Shallow-level I-type rocks. Age of 418.9 +/- 2.5 Ma reported by Waltenberg et al. (2016).|418.9 +/- 2.5 Ma|||||
70448|Back Creek Ignimbrite Member|62095|5|Briefly described|p274 Appdx.|Late Carboniferous|Late Carboniferous|Underlies Rockford Ignimbrite Member. Age: 308.9+/-2.8Ma. Unclear from text how this unit relates to Back Creek Tuff Member (which has been superseded by Kankool Ignimbrite Member)?||||||22-MAY-06
37355|Back Forest Tuff Bed|71542|4|Described|p23,25,29-30,34, 35|Late Permian|Late Permian|Of southern Sydney Basin. Identified in a disused roadside quarry near Back Forest bridge (56/288250E, 61601250N), Thickness: average 3cm. Could not be traced laterally due to soil and vegetation cover. Evidence of explosive volcanic eruption during deposition of the Westley Park Sandstone Member, previously undetected in the southern Sydney Basin. Likely resulted from a Surtseyan eruption depositing a thick ash-flow in proximal channels, and distally as an ash-fall or pyroclastic flow. See also Facies 5 description p27.||Unit of Gerringong Volcanics.||Within Westley Park Sandstone Member, Broughton Formation.|Thin tuffaceous ash deposit containing latitic clasts, pumiceous material and glass shards.|20-OCT-21
69887|Back Station Ignimbrite Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Blue-grey crystal-rich welded dacitic ignimbrite composed of crystals/fragments of plagioclase, qtz-hornblende, clinopyroxene+orthopyroxene, +accessory opaques, K-feldspar, apatite + zircon, set in micro- to crypto-crystalline matrix||||||
69887|Back Station Ignimbrite Member|68592|2|Defined|p851-6, p858-62, p865, p868-74, p876|Lochkovian|Lochkovian|See also p107-8, p726, p730 Fig.132, p827, p878, p1662. New name. Equivalent to dacitic ignimbrite unit of Gundary Formation of Jones et al. (1995). Outcrops in Strathaird area were formerly placed in Turrallo Quartz Diorite by Scheibner (1973). A xenolitihc dacitic porphyry described by Scheibner (1973) is probably this unit. Type section provided where thickness is ~1150 m. Metamorphism: mildly affected by an alteration assemblage consistent with sub-greenschist facies. Age: early Lochkovian. Is lithologically similar to, but distinguishable from, Barrallier Ignimbrite. Inferred displacement of c.35 km by Mulwaree Fault. Is overlain by Lambie Group unconformably and Bullamalita Conglomerate disconformably (or entirely cut through by it).|414 +/- 4 Ma, SHRIMP zircon U-Pb, Wilde (2002).|Unit in Gundary Volcanics.||Overlies Tirranna Andesite Member, Bradfordville Volcaniclastic Member, Rhyanna Formation and Boxers Creek Formation (locally conformably). Is locally intruded by Forest Lodge Quartz Monzodiorite.|A thick sequence of blue-grey, crystal-rich, two pyroxene and hornblende-bearing, dacitic, welded ignimbrite.|
69887|Back Station Ignimbrite Member|69159|5|Briefly described|Map legend|Lochkovian|Late Silurian|||Unit in Gundary Volcanics.|||Blue-grey crystal-rich welded dacitic ignimbrite that contains crystals and fragments of plagioclase, quartz, hornblende, clinopyroxene and orthopyroxene, set in a microcrystalline to cryptocrystalline matrix.|07-SEP-15
69887|Back Station Ignimbrite Member|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfgb. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Gundary Volcanics||Overlies Boxers Creek Formation, and Bradfordville Volcaniclastic Member and Tirranna Andesite Member (of Gundary Volcanics). Over- and underlies|Crystal rich, welded dacitic ignimbrite with crystals and fragments of plagioclase, quartz, hornblende and pyroxenes; K-feldspar, apatite and zircon in a microcrystalline-cryptocrystalline matrix; spherulites, perlitic and eutaxitic textures common.|
69887|Back Station Ignimbrite Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Gundary Volcanics|||Crystal rich, welded dacitic ignimbrite with crystals and fragments of plagioclase, quartz, hornblende and pyroxenes.  K-feldspar, apatite and zircon in a microcrystalline-cryptocrystalline matrix. Perlitic and eutaxitic textures are common.|
69887|Back Station Ignimbrite Member|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Gundary Volcanics|||Crystal rich, welded dacitic ignimbrite with crystals and fragments of plagioclase, quartz, hornblende and pyroxenes; K-feldspar, apatite and zircon in a microcrystalline-cryptocrystalline matrix; spherulites, perlitic and eutaxitic textures common.|
69887|Back Station Ignimbrite Member|71069|6|Mentioned|p135, p137 fig 44, p143|Early Devonian|Early Devonian|Up to 150m thick. |414 +/- 4 Ma (SHRIMP U-PB, Wilde 2002)|Gundary Volcanics||||
69887|Back Station Ignimbrite Member|71699|5|Briefly described|Map legend.|Devonian|Silurian|||Gundary Volcanics.|||Blue to grey crystal-rich welded dacitic ignimbrite that contains crystals and fragments of plagioclase, quartz, hornblende, clinopyroxene and orthopyroxene, set in a microcrystalline to cryptocrystalline matrix.|
69887|Back Station Ignimbrite Member|71700|2|Defined|vi, p15, p24, CD|Lochkovian|Lochkovian|Named for the Back Station Creek near GR 754780 6142260. The type section is in McKellars Creek between GR 754890 6141950 and GR 753680 6142380. This unit has not previously been recognised in Braidwood and outcrop was previously assigned to the Long Flat Volcanics. Distribution, geomorphic expression, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics and distinguishing features are discussed.  This unit has a maximum thickness of approximately 1150m. This unit may be a shallow water equivalent to the Rhyanna Formation. An implied strike length of 110km is interpreted.|414 +/- 4 Ma (SHRIMP, Wilde, 2002)|Gundary Volcanics||Faulted against the Abercrombie Formation and the Kain Porphyry Member.|Uniform, greenish-grey, crystal-rich, welded dacitic ignimbrite.|
25770|Back Swamp Granodiorite|22815|4|Described|p45|Silurian|Silurian|||||||
25770|Back Swamp Granodiorite|35263|6|Mentioned|Table 3|||||||||
25770|Back Swamp Granodiorite|41898|6|Mentioned|p1184|||||||||
25770|Back Swamp Granodiorite|41905|2|Defined|p79|Silurian||||||||
25770|Back Swamp Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
76031|Baconian Swamp granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Baconian Swamp Granite Suite.|||Interpreted S-type granites.|
76031|Baconian Swamp granite|70718|4|Described|p75, p124|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics. Interpreted as S-type granite.||Baconian Swamp granite suite|||S-type granitic rocks.|31-MAY-19
80443|Baconian Swamp granite suite|70718|5|Briefly described|p3, p75-p76, p94, p124-127|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics with no known outcrop or drillcore intersecting this suite. Suite distinguished by larger metamorphic aureoles. Age derived from relationship of the Oolambeyan granite cross cutting the Early Devonian Eurolie granite.|||Includes the Baconian Swamp, Darcoola, Glenhope, Maude, Toopuntul, Warwaegae, Nyangay and Oolambeyan granites.|Intrudes the Eurolie granite.|S-type granitic rocks.|31-MAY-19
25771|Badgerys Breccia|22857|5|Briefly described|p504 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Of the Talaterang Group - but now interpreted as part of the Shoalhaven Group by Tye, Fielding and Jones (1996). Poorly sorted angular clasts, upper part is a megabreccia (a lateral moraine?). Max. thickness: 26m. Geol. Prov: Kanimblan Highlands.||||||
25771|Badgerys Breccia|31081|6|Mentioned|p51|||||||||
25771|Badgerys Breccia|31298|2|Defined|p11|Carboniferous|Carboniferous|Prob. Carboniferous||||||
25771|Badgerys Breccia|37924|5|Briefly described|p488|||||||||
25771|Badgerys Breccia|39290|6|Mentioned|p83|||||||||
25771|Badgerys Breccia|39299|5|Briefly described|p283|||||||||
25771|Badgerys Breccia|39308|4|Described|p519|||||||||
25771|Badgerys Breccia|68592|6|Mentioned|p1779, p1786|Permian|Permian|||Unit in Shoalhaven Group.||||
76755|Badgerys Breccia Member|70661|3|Fully described|x, p137, p139, p141, p147-p149|Early Permian|Early Permian|Name derived from Badgerys Lookout. Previously described as Badgerys Breccia (formation rank) but now demoted to member status because it is not well defined as a stratigraphic unit but rather appears to be a distinctive facies of the Tallong Conglomerate. Forms high cliffs. No type section given. 25-30m thick. Depostion and structure described. ||Tallong Conglomerate||Unconformably overlies Adaminaby Group, correlated with Yadboro Conglomerate|Sedimentary pebble breccia, conglomerate, small local megabreccia and some sandstone lenses. The unit is massive to poorly stratified. Clasts consist primarily of quartzite, phyllite and black chert. Somewhat upward fining.|
76755|Badgerys Breccia Member|71303|5|Briefly described|map legend|Cisuralian|Cisuralian|Of Sydney Basin.||Of Tallong Conglomerate.|||Sedimentary pebble breccia with a local mega-breccia and some sandstone lenses. Massive to poorly stratified.|
82289|Bakers Creek Complex|71628|4|Described|p2: 7-14; p3-40|||Originally the Bakers Creek Diorite (Binns et al., 1967) which later became the Bakers Creek Diorite Complex (Ashley and Craw, 2004). Named after the Bakers Creek which deeply incises the intrusion. Forms an irregularly-shaped intrusion 2 km S of Hillgrove. Crops out as isolated rubbly outcrops, boulders in creeks and gorges, and as whalebacks. Different detailed descriptions are given due to contradictions in the literature. Geochemistry detailed. Associated with Sb-Au(W) deposits in the Hillgrove-Metz area. Has local graphite deposits.|299.7 +/- 2.0 Ma (SHRIMP: McKibbin et al, 2017).|Bakers Creek Supersuite.||Intrudes the Girrakool beds. Cut by aplitic dykes of ?Hillgrove Suite.|Gabbro, diorite, quartz diorite, tonalite, granodiorite, adamellite and granophyre.|
37374|Bakers Creek Suite|24040|5|Briefly described|p468 Fig. 1, p470 Fig. 2, p471, p475|Late Carboniferous|Late Carboniferous|In the Tablelands Complex. Contains a variety of rock types ranging from gabbros and diorites through to tonalites and granophyres. Age of gabbros: ca.300Ma. Gabbros are given the informal name Bakers Creek gabbros (p486).||||||21-AUG-08
37374|Bakers Creek Suite|66183|5|Briefly described|p359|Early Permian|Gzhelian|New England Fold Belt. Gabbro/diorite bodies, intra oceanic back arc setting. Coeval with Hillgrove Plutonic Suite (c.300 Ma).||||||
37374|Bakers Creek Suite|71280|6|Mentioned|p402 Fig.1|||||||||
37374|Bakers Creek Suite|71628|5|Briefly described|p2: 1, 6, 10, 15, 17, 23, 34, 37; p3:3|||Landenberger and Collins (2000), after unpublished work by Landenberger (1996); for calc-alkaline and tholeiitic complexes in the southern New England Orogen. Subsequently (Landenberger et al., 2010) altered to Bakers Creek Supersuite.|||Bakers Creek Complex.|||
37374|Bakers Creek Suite|71703|5|Briefly described|p203, p193 Fig. 1|Latest Carboniferous|Latest Carboniferous|~304 Ma; McKibbin et al., 2017.|Ages from 293.3+/-3.2 Ma to 305.1+/-2.9 Ma.||Includes Cheyenne Complex and kilburnie Monzogranite.|Spatially associated with Hillgrove Supersuite granites.|small mafic bodies.|
37374|Bakers Creek Suite|73197|6|Mentioned|p471, 472 Tb.2|Kungurian|Moscovian|New England Orogen, southern. Formed in a back-arc setting. U-Pb zircon ages from McKibbin et al., (2017) and Rosenbaum et al., (2012).|305.1 +/- 2.9 Ma, 280.0 +/- 2.8 Ma U-Pb zircon||||Small mafic plutonic rocks.|
37374|Bakers Creek Suite|73202|5|Briefly described|p626-628, p637, p638, p639 Fig.10, p640|Early Permian|Late Carboniferous|New England Orogen, southern. I-type gabbros. Mingling occurs with the Hillgrove Plutonic Supersuite. Mostly has a MORB-like geochemical signature. Zircon age from McKibbin et al., (2017).|299.3 +/- 3.1 Ma U-Pb zircon||||Tholeiitic gabbros.|
75958|Bakers Creek Supersuite|71628|4|Described|p1:1, 6, 11, 15, 18; 2:1-71; p3: 3-5, 7|||See also p3: 9-11, 28, 30, 44, 56, 86; p8: 54, 92; p19: 105-107, 150, 152, 154, 165. Comprises a series of small (1-20 km2) mafic-intermediate intrusive complexes. Spatially associated with the Hillgrove Supersuite. Herein defined as having a mantle-derived component. Has a broad range of compositional, mineralogical, geochemical and isotopic attributes.|305-280 Ma (Rosenbaum et al., 2012).||Woodburn, Cheyenne, Moona Plains, Sheep Station Creek, Apsley River, Bakers Creek Complexes; Days Creek, Barney House Gabbros.|Is intruded by Wards Mistake Monzogranite.|Small mafic-intermediate complexes: olivine gabbros, two-pyroxene gabbros through hornblende-biotite(-pyroxene) diorite and quartz diorite to hornblende or pyroxene granodiorites or tonalites, and locally granophyre.|
73063|Bald Hill Formation|61392|4|Described|p163-165, p167|Early Devonian|Early Devonian|Of the Silverwood Group (Keinjan Terrane). Divided into Units A, B and C. Age: 389-386 Ma [probably from 1995 timesscale]. Max. thickness: 2450m.||||||03-SEP-18
73063|Bald Hill Formation|63731|5|Briefly described|Map legend|Devonian|Silurian|Of Silverwood Gp. Volcaniclastic arenite+siltstone, basaltic to andesitic lavas; arenite+mudstone with chert; basaltic debris flow deposits, metabasite sills+hybassyl intrusions; metagabbro, lenses of limestone+marble; pepperites; polymictic paraconglom.||||||19-AUG-08
73063|Bald Hill Formation|63748|4|Described|p7 Fig. 3, p8|Emsian|Pragian|Of Silverwood Group. Unconformable on Connolly Volcanics; conformably overlain by Ormoral Volcanics. Max. thickness: ~2450m. Geol. Prov: Silverwood province. Subdivided into four lithological packages; includes a subunit, Kelvin Falls Sill.||||||07-FEB-11
73063|Bald Hill Formation|68679|5|Briefly described|p445-447|Emsian|Emsian|Van Noord (1999). Silverwood Province. ~2450m thick. Considerable material was derived from older Silverwood Group.||Silverwood Group.||Unconformably overlies Connolly Volcanics. Is overlain by Ormoral Volcanics conformably and Bromley Hills Formation unconformably.|Basal polymictic conglomerate and breccia; middle unit mainly syn-depositional sills and cryptodomes (low-K tholeiitic basalt), some peperite, volcaniclastics, minor lava and limestone; upper turbidites and some chert with abundant slumping.|
73063|Bald Hill Formation|71628|5|Briefly described|p16: 4|||||Silverwood Group.||Is intruded by Cullendore Syenogranite.||
76050|Baldon granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given. Similar to Lake Boga and Pyramid Hill Granites.||Unit in Cunninyuek Granite Suite.|||Muscovite-biotite granite; interpreted S-type granite.|
76050|Baldon granite|70718|4|Described|p48, 49, p78-p79, p128|Late Devonian|Late Devonian|Bendigo Zone, Murray Basin. Informal name [Only known from geophysical interpretation]. Size and rough shape of magnetic anomalies is provided. Interpreted as S-type granite similar to the Lake Boga and Pyramid Hill granites as their geophysical signature is similar.||Cunninyeuk granite suite|||S-type granitic rocks similar to Lake Boga (medium- to coarse-grained, porphyritic, two-mica granite) and Pyramid Hill granites (a coarse-grained leucocratic monzogranite).|31-MAY-19
27324|Balgownie Coal Member|29900|6|Mentioned|Table 2|||||||||
27324|Balgownie Coal Member|29901|4|Described|Table 1|||||||||
27324|Balgownie Coal Member|29944|6|Mentioned|Fig.18|||||||||
27324|Balgownie Coal Member|30006|5|Briefly described|p37|||||||||
27324|Balgownie Coal Member|31128|6|Mentioned|p7|||||||||
27324|Balgownie Coal Member|31887|6|Mentioned|p7|||||||||
27324|Balgownie Coal Member|32849|6|Mentioned|Table 1|||Permian||||||
27324|Balgownie Coal Member|33869|6|Mentioned|Fig.2|||||||||
27324|Balgownie Coal Member|36220|4|Described|p53|||See also Table 1, Fig.4 & P50.||||||
27324|Balgownie Coal Member|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27324|Balgownie Coal Member|36593|6|Mentioned|Table 2|||||||||
27324|Balgownie Coal Member|37089|6|Mentioned|p208|||||||||
27324|Balgownie Coal Member|37090|6|Mentioned|p221|||||||||
27324|Balgownie Coal Member|37730|6|Mentioned|p18|||||||||
27324|Balgownie Coal Member|39309|6|Mentioned|p128|||||||||
27324|Balgownie Coal Member|39661|6|Mentioned|p447|||Replaces Gillan Creek seam. See also Fig.1||||||
27324|Balgownie Coal Member|40631|6|Mentioned|p163|||||||||
27324|Balgownie Coal Member|42787|6|Mentioned|Table 1 P126|||||||||
27324|Balgownie Coal Member|42896|5|Briefly described|p24|||of Eckersley Formation||||||
27324|Balgownie Coal Member|42925|6|Mentioned|Fig.23|||of Eckersley Formation||||||
82290|Ballandean Monzogranite|71628|3|Fully described|p12: 1-2, 6-7, 13-14; p15: 33, 40, 82,97|Early Permian|Early Permian|See also 1-5,p15: 101-102; p19: 5-9. New name (this study); previously Ballandean Granite. Historically included within Stanthorpe Adamellite. Named after Ballandean Station. Forms a roughly 8 x 8 km intrusion at the W of Ballandean township. Crops out as sparse scattered boulders and pavements, and rare whalebacks. Two type locations have been proposed: GR 38238117 on Stanthorpe 1:100,000 sheet (Butler, 1974) and MGA 382406 6812031 (Donchak et al., 2007). Lithology, mineralogy and geochemistry detailed. Excluded from the new Sailor Jack Supersuite.|295 Ma (unpub. data in Rosenbaum et al., 2012)|Ballandean Suite.||Intrudes Texas beds. Is intruded by Sailor Jack, Severn River Monzogranites, Ruby Creek Leucogranite and Stanthorpe Complex. Is overlain unconformably by Wallangarra Volcanics.|White to grey, fine- to medium-grained, variably porphyritic hornblende-biotite monzogranite and biotite-hornblende-(clinopyroxene) granodiorite to monzogranite, and minor quartz monzonite. I-type.|
33967|Ballast Formation|22555|4|Described|p371, Fig.1p372|Caradoc|Llanvirn|Supersedes 'Ballast beds'.||||||20-OCT-08
33967|Ballast Formation|22557|6|Mentioned|p569||Early Ordovician|||||||
33967|Ballast Formation|22857|4|Described|p133, p414 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|For this study, not included in the Girilambone Group. Quartzose arenite (turbidite), siltstone, black siliceous mudstone, less common chert. Interfingers with Mount Dijou Volcanics. ||||||
33967|Ballast Formation|23213|5|Briefly described|Fig.10|Late Ordovician|Darriwilian|Age: Late Darriwilian to Late Ordovician. Of Girilambone Group, Cobar Trough.||||||20-OCT-08
33967|Ballast Formation|23245|5|Briefly described|p133||Late Ordovician|||||||
33967|Ballast Formation|24215|5|Briefly described|p805|||Of the Girrilambone Group.  Geological Province:  Lachlan Fold Belt.||||||20-OCT-08
33967|Ballast Formation|24417|6|Mentioned|p13|||Formerly "Ballast Beds".||||||
33967|Ballast Formation|44093|5|Briefly described|p50, p114|Gisbornian|Darriwilian|||||||
33967|Ballast Formation|50098|6|Mentioned|p10|||Geological Province: Lachlan Fold Belt.||||||
33967|Ballast Formation|63119|5|Briefly described|p214|Late Ordovician|Late Ordovician|East of Cobar.||||||
33967|Ballast Formation|67322|3|Fully described|p19, p20 Fig.5|Middle Ordovician|Middle Ordovician|Hermidale Terrane. First termed the Ballast Series by Andrews (1913); has been variously called the Ballast Chert, Beds, Group and Formation (this last of Iwata et al. 1995). Initially excluded from the Girilambone Series, the Ballast Beds (now Ballast Formation) is a constituent of the Girilambone Group. Used to include the Merrere Conglomerate Member, which is now regarded as a basal conglomerate of the Cobar Supergroup (Glen et al. 2010). Maximum age is determined from p20 Fig.5 (Strat. column). Occurs in the Sussex-Byrock region.||Of the Girilambone Group|Whinfell Chert Member|Facies variant of the Lang Formation. Chert units correlate with Alandoon Chert.|Interbedded turbiditic sandstone-dominated beds grading to siltstone and chert, as well as thick persistent packages of ribbon chert tens of metres thick. Very small outcrops of basaltic and other mafic rocks are also present.|21-FEB-18
33967|Ballast Formation|68466|5|Briefly described|p65-66, 69|Middle Ordovician|Middle Ordovician|Hermidale Terrane. Late Darriwilian radiolaria have been extracted from black mudstone from the Ballast Quarry, E of Cobar.|||Whinfell Chert Member.||Comprises interbedded turbidites and chert, as well as thick persistent packages of ribbon cherts tens of metres thick in the upper part.|
33967|Ballast Formation|69094|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|||Unit in Girilambone Group.|||Variably metamorphosed quartzose and micaceous fine- to medium-grained sandstone (includes quartzite), siltstone, claystone/shale and radiolarian and conodont-bearing chert (Darriwilian); basalt layers locally.|
33967|Ballast Formation|69095|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Includes an un-named but separately mapped sub-unit: 'subsurface, highly altered vesicular basalt, gabbro and ultramafic rocks'.||Unit in Girilambone Group.|||Variably metamorphosed quartzose and micaceous fine- to medium-grained sandstone (includes quartzite), siltstone, claystone/shale and radiolarian and conodont-bearing chert (Darriwilian); local highly altered basalt layers.|
33967|Ballast Formation|69541|5|Briefly described|p652|Early Ordovician|Early Ordovician|Chert units contain conodonts of late Darriwilian age.||Unit in Girilambone Group.||||
33967|Ballast Formation|69635|4|Described|p84-87, p69|Darriwilian|Darriwilian|North-western Lachlan Orogen. Age constrained by conodont biozonation to be middle to late Darriwilian, but neither top nor base tightly constrained. U-Pb SHRIMP zircon maximum depositional age does not constrain deposition any better than already determined.|507+/-13 Ma|Of Girilambone Group.|||Interbedded metasedimentary and concordant mafic vesicular basaltic rocks.|
33967|Ballast Formation|69668|5|Briefly described|p929 Fig.2, p931|Middle Ordovician|Middle Ordovician|Hermidale terrane, central NSW. The cherts contain conodonts including Pygodus serra and Periodon aculeatus.||Unit in Girilambone Group.|Includes Whinfell Chert Member.|Overlies Narrama Formation.|Interbedded turbidites and chert, as well as thick persistent packages of ribbon chert tens of metres thick (Whinfell Chert Member).|
33967|Ballast Formation|70602|6|Mentioned|p66,Fig 2, p67,72|Middle Ordovician|Middle Ordovician|Aeromagnetic map data given.||Girilambone Group||||
33967|Ballast Formation|70821|5|Briefly described|p28|Late Ordovician|Middle Ordovician|Previously the Ballast Beds. Has deep in situ weathering profiles from 10m to over 50m below ground surface, producing noise in EM-37 ground electromagnetic surveys.||Girilambone Group.||||
33967|Ballast Formation|70941|3|Fully described|pviii, px, p6, p7 fig 3, p8 fig 4,|Darriwilian|Darriwilian|Named for the Ballast quarry. Previously termed Ballast Series, Ballast Chert, Ballast Group, Ballast Beds. May partly correlate with the Whinfell Chert. Age derived from conodont fossil assemblage. Distribution, geomorphology, geochemistry, geophysical characteristics, structure and distinguishing characteristics discussed.  Metamorphosed to subgreenschist or lower greenschist facies. Previously quarried for construction materials. Type section mentioned and type areas described. Estimated to be several kilometers thick.  Deposited as bouma sequences in an intraplate oceanic setting. Laterally equivalent to the Lang Formation.  See also  p13 fig 7, p12, p21, p26,  p27, p38, p42-50, p86,  p90, p117, p127, p133, p135, p136, p140 fig 58, p141, p146, p147, p149||Girilambone Group||Unconformably overlain by Meryula Formation. Conformably overlies (or is faulted against) Narrama Formation. Unconformably overlain (or faulted against) the Cobar Supergroup|Interbedded medium to fine grained quartz sandstone, very fine grained trough cross laminated quartz sandstone, siltstone, claystone, shale, chert and local basalt layers. Lamprophyre and very minor serpentinised ultramafic rock is also present.|
33967|Ballast Formation|71360|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Mapped (and lithology described) with the Lang Formation as one unit. Geophysical signature: broad areas of low magnetic intensity with linear trends of moderate magnetic intensity occurring parallel to regional foliation directions. Previously included the Merrere Conglomerate Member, which is now within the Kopyje Group and apparently part of the Meryula Formation.||Girilambone Group.|||Sandstone, siltstone, claystone and chert. Local thin flows and sills of vesicular basalt.|
33967|Ballast Formation|71693|5|Briefly described|Map legend.|Ordovician|Ordovician|This unit and the Lang Formation are mapped as one unit.||Girilambone Group.||Overlies Narrama Formation [??].|Interbedded quartz-rich sandstone, siltstone, slate and phyllite with minor thin chert horizons.|13-SEP-19
33967|Ballast Formation|71700|5|Briefly described|p8|||Chert units in this formation may be equivalent to the Nattery Chert Member.||Girilambone Group||||
33967|Ballast Formation|72080|4|Described|p2, p4-p5, p9, p12-p14, p19|Darriwilian|Darriwilian|Age is derived from conodont fossils in the chert units up to 20 m thick. See also old name Ballast Chert. A 'Sussex basalt' sample from this unit discussed p19-22.||Girilambone Group.||Equivalent to the Lang Formation, Alandoon Chert and Whinfell Chert.||07-JAN-22
33967|Ballast Formation|72083|6|Mentioned|p45|||||||Is overlain by the Hazeldene Sandstone.||
33967|Ballast Formation|72296|5|Briefly described|p6, p24, p81-82|Middle Ordovician|Middle Ordovician|See p6 for the complicated evolution of this unit's name and relationships with the Girilambone Group. Contains late Darriwilian microfossils (Iwata et al., 1995); listed.||||Correlated with Lang Formation.||
33967|Ballast Formation|72958|6|Mentioned|p45|Ordovician|Ordovician|Presumably intruded by unnamed tonalite dated herein as 424.9 +/-2 Ma.||Girilambone Group|||Turbidites|
33967|Ballast Formation|73264|6|Mentioned|p1390 Fig.12|Middle Ordovician|Middle Ordovician|Hermidale Terrane. Shown as Ballast Fm.||Girilambone Group||||
28166|Ballingoole Limestone|13139|5|Briefly described|p4|Late Ordovician|Late Ordovician|Of the Bowan Park Limestone Subgroup.  Contains the Downderry Limestone Member.  Overlain by Oakdale Formation.||||||
28166|Ballingoole Limestone|23213|6|Mentioned|p21|||||||||
28166|Ballingoole Limestone|23214|3|Fully described|p39|Late Ordovician|Late Ordovician|Of Bowan Park Limestone Subgroup. No single type section due to outcrop problems. Max. thickness 280m. Geological Province: Lachlan Fold Belt.||||||
28166|Ballingoole Limestone|23334|6|Mentioned|4|||||||||
28166|Ballingoole Limestone|23736|5|Briefly described|p19|||Parent: Bowen Park Group||||||
28166|Ballingoole Limestone|32590|6|Mentioned|p13|||||||||
28166|Ballingoole Limestone|33063|1|Redefined|p83|Ordovician|Ordovician|Part of Bowan Park Group. See also p84||||||04-DEC-12
28166|Ballingoole Limestone|33065|5|Briefly described|p130|||||||||
28166|Ballingoole Limestone|33737|6|Mentioned|p180|||||||||
28166|Ballingoole Limestone|33740|6|Mentioned|p125|||||||||
28166|Ballingoole Limestone|35118|6|Mentioned|Fig.5|||||||||
28166|Ballingoole Limestone|35646|6|Mentioned|Fig.3|||||||||
28166|Ballingoole Limestone|38219|6|Mentioned|p315|||See also Table 2.||||||
28166|Ballingoole Limestone|40127|6|Mentioned|p9|||||||||
28166|Ballingoole Limestone|40136|5|Briefly described|p16|||||||||
28166|Ballingoole Limestone|41046|6|Mentioned|Fig.2|||||||||
28166|Ballingoole Limestone|42479|5|Briefly described|p111|||||||||
28166|Ballingoole Limestone|63278|5|Briefly described|p153|||Of the Bowan Park Limestone Subgroup. Includes; Downderry Limestone Member. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
28166|Ballingoole Limestone|64015|5|Briefly described|p79|Ordovician|Ordovician|Of the Bowan Park Group.||||||28-AUG-08
28166|Ballingoole Limestone|67322|5|Briefly described|p20 Fig.5, p23|Katian|Katian|Semeniuk 1970, 1973. T.tumidis present in this formation is indicative of a late Eastonian age. Occurs in the Bowan Park region.||Of the Bowan Park Limestone Subgroup.|Downderry Limestone Member|Overlain by the Malachis Hill Formation.||
28166|Ballingoole Limestone|70684|5|Briefly described|p39 Fig.17, p40-42|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Bowan Park Subgroup.|Corner, Clearview, Downderry, Limestone Members.|||
28166|Ballingoole Limestone|70754|5|Briefly described|p447, p450-451, p455, p457-464, p466-468|||See also p472-473, p477-480. Systematic palaeontological descriptions.||Topmost Bowan Park Subgroup.|Downderry Limestone Member.|Is overlain conformably by Malachis Hill Formation.||
28166|Ballingoole Limestone|71091|5|Briefly described|p143, p146|||||Bowan Park Limestone Group.|Downderry Limestone Member.|Is overlain conformably by Malachis Hill Formation.||
28166|Ballingoole Limestone|73210|6|Mentioned|p893 Fig.2|||||||||
69875|Balmeringa Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tumboramboro Suite. Brownish-grey, medium-grained, equigranular biotite-quartz-feldspar xenolithic granodiorite. Xenoliths of composite gneiss, metasedimentary rock and quartz-feldspathic segregations.||||||
69875|Balmeringa Granite|68592|3|Fully described|p105, p294-5, p1543-6, p1577-81|Early Devonian|Early Devonian|New name. Type area described. Sporadic low bouldery exposures. Encloses and partly assimilates Fullerton Gneiss. Inferred to be heavily contaminated by Adaminaby Group material. Well-developed schistosity at western margin: Turkey Hill Shear Zone. Geochemistry and geophysical properties described.||Unit in Tumboramboro Suite.||Is overlain by Crookwell Basalt. Is faulted against Tumboramboro Granite. Encloses Fullerton Gneiss.|Grey-brown to cream, fine-grained, equigranular, biotite granite; heavily xenolithic with gneissic and high-grade metasedimentary inclusions. S-type.|
69875|Balmeringa Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dtb. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Tumboramboro Suite|||Fine grained, equigranular, cordierite?-biotite granite; xenoliths of composite gneiss, metasedimentary rock and quartzo-feldspathic segregations; high K and Th, low-high U response; low magnetic susceptibility.|
69875|Balmeringa Granite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Tumboramboro Suite|||Fine grained, equigranular, cordierite?-biotite granite; xenoliths of composite gneiss, metasedimentary rock and quartzo-feldspathic segregations; high K and Th, low-high U response; low magnetic susceptibility.|
41050|Banalasta Monzogranite|24366|5|Briefly described|p12 Fig. 10|Early Permian|Early Permian|Of the Bundarra Plutonic Suite.||||||26-MAY-04
41050|Banalasta Monzogranite|68005|5|Briefly described|p62, p136.|Early Permian|Late Carboniferous|Boundaries have been refined using radiometric imagery.||Unit in Banalasta Suite.|||Porphyritic biotite-muscovite-cordierite granite.|
41050|Banalasta Monzogranite|69323|5|Briefly described|p34,69|Cisularian|Cisularian|Geological province: New England Orogen. Date derived from Black, 2007 is a SHRIMP age.|286.2+\-2.2 Ma (Black, 2007)|Unit of Bundarra Supersuite.||||03-DEC-19
41050|Banalasta Monzogranite|71628|4|Described|p4: 1, 3-5, 7-16, 20, 29-31, 34, 37-39|||See also p4: 44-52, 55-57; p7: 10-11, 28, 40; p19-1. Brown (2003). Southern New England Orogen. Named after a local homestead. Crops out ~15 km W of Uralla; irregular distribution described. Crops out as fresh tors or whalebacks; commonly moderately to strongly weathered. Extensively metamorphosed by younger intrusions. Several age determinations given. Geochemistry described in some detail. No mineralisation known; has been used for building stone. RELATED UNITS (continued): Is intruded by Moonbi Supersuite, Mountain Home Granite, Pringles and Walcha Road Monzogranites and Fox Tor Quartz Diorite.|289.2 +/- 1.7 Ma (SHRIMP: Jeon et al., 2012).|Banalasta Suite.|Flaggy Range Monzogranite Phase.|Intrudes Cara and Whitlow Formations and Sandon beds. Abuts the Pringles and MacDonald River Monzogranites, Glencair Syenogranite and Balala Granodiorite. See COMMENTS for more.|Bluish grey (fresh) to buff (weathered) coloured, coarse- to very coarse-grained, strongly porphyritic biotite (+/- muscovite, +/- cordierite, +/- garnet) monzogranite. Contains abundant K-feldspar megacrysts to 90mm.|
41050|Banalasta Monzogranite|73264|6|Mentioned|p1398 Fig.20|Permian|Permian|New England Orogen.||Bundarra Supersuite||||
67897|Banalasta Suite|24222|5|Briefly described|p4|||Geological Province: New England Fold Belt.||||||
67897|Banalasta Suite|68005|5|Briefly described|p136.|Permian|Permian|||Unit in Bundarra Supersuite.|Includes Banalasta and Pringles Monzogranites.|||
67897|Banalasta Suite|71628|5|Briefly described|p4: 2-3, 10, 15, 24, 29, 48, 51, 55|||Chappell (1978). Bryant et al. (2001?) restricted this unit to include Banalasta and Pringles Monzogranites. In this study it consists solely of the one single solitary unit [???].||Bundarra Supersuite.|Banalasta Monzogranite.|||
79643|Bancannia andesite""|69043|5|Briefly described|p4-6, p100-105, p120|Cambrian|Cambrian|Delamerian Orogen. The sample dated resembles (in hand specimen) the Mount Wright Volcanics, but because it is younger than the Cymbric Vale Formation, it cannot be part of the Mount Wright Volcanics.|506.1 +/- 2.7 Ma.||||Feldspar-phyric andesite.|17-JAN-17
26367|Banda Banda Monzodiorite|38916|6|Mentioned|p348|||||||||
26367|Banda Banda Monzodiorite|40590|6|Mentioned|Fig.1|||||||||
26367|Banda Banda Monzodiorite|41348|5|Briefly described|Map legend|Early Paleozoic||Granitoid of the Gundle Belt.||||||07-NOV-08
26367|Banda Banda Monzodiorite|44450|5|Briefly described|p105 Fig 30|||Geological Province: New England Fold Belt.||||||
26367|Banda Banda Monzodiorite|71628|5|Briefly described|p17: 1-2, 88-89|||Leitch et al. (1982), after the unpublished Mount Banda Porphyrites of Matthias (1967). Unaffiliated. Named after Mount Banda Banda, 50 km N of Port Macquarie.|222.9 Ma (Rb-Sr biotite; Shaw, 1994).|||Intrudes Boonanghi beds.|Coarse-grained monzodiorite.|
82291|Banda Banda Suite|71628|5|Briefly described|p17: 89|||||Coastal Granite Association.|Banda Banda Monzodiorite.|||
23357|Bandon Grove Limestone Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Of the Flagstaff Formation. Biogenic limestone, grading into sandstone with pebbles. Max. thickness: 15m. Geological Province: Tamworth Forearc Basin.||||||
23357|Bandon Grove Limestone Member|40883|6|Mentioned|p7|||||||||
23357|Bandon Grove Limestone Member|43576|5|Briefly described|p350|||||||||
23357|Bandon Grove Limestone Member|44244|4|Described|p71|Visean|Visean|Biogenic limestone of crinoid columnals, brachiopods and solitary corals.  Max. thickness: 15m.  Geological Procince: Gresford Block.||||||
23357|Bandon Grove Limestone Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Flagstaff Formation.  Brown to yellow biogenic limestone with interbeds cross-stratified calcareous lithic sandstone and pebbles of volcanic origin.||||||
82346|Bannaweera Gabbro|71628|4|Described|p19: 1-3, 9-11|||Brown et al. (1990) after unpublished works by Ransley (1970) and Brown (1986). Named after a local homestead. Forms a curvilinear, ~4 x 0.350 km intrusion, with a prominent ridge, about 13 km WNW of Uralla. Lithologies and mineralogy detailed.||Bannaweera Suite.||Intrudes the Sandon beds. Bounds (?intrudes) Balala Granodiorite.|Medium-grained hornblende gabbro, hornblende melagabbro, gabbro-diorite, with a pegmatite-appinite facies.|
26369|Barcaldane Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
27325|Barfield Formation|13516|5|Briefly described|p145 fig 3|Late Permian|Late Permian|From Taroom Shelf, Bowen Basin. Age: APP5004||||||
27325|Barfield Formation|22973|5|Briefly described|p10|Late Permian|Late Permian|||||||
27325|Barfield Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
27325|Barfield Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
27325|Barfield Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
27325|Barfield Formation|23037|5|Briefly described|p64,5,66||Permian|Equivalent to Back Creek Group, contains Four Mile Mudstone, Cottenham Sandstone and Station Mudstone Members. Max. thickness 700 m.||||||22-MAR-12
27325|Barfield Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
27325|Barfield Formation|24491|5|Briefly described|p20|||Geological Province: Bowen Basin.||||||
27325|Barfield Formation|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pbr].  Mudstone, siltstone, lithic and feldspathic sandstone, minor conglomerate.||||||
27325|Barfield Formation|29436|6|Mentioned|p317||Permian|||||||
27325|Barfield Formation|29964|6|Mentioned|p5|||||||||
27325|Barfield Formation|30141|5|Briefly described|p134|||||||||
27325|Barfield Formation|30449|6|Mentioned|p4|||Brachiopods. See also P6,8,14,21||||||
27325|Barfield Formation|30450|6|Mentioned|Table 1|||Permian age.Southeast Bowen Basin||||||
27325|Barfield Formation|30451|3|Fully described|p54|||See also p55,56.||||||16-NOV-15
27325|Barfield Formation|30546|6|Mentioned|p107|||Upper Permian age. Correlation.See also P114,fauna||||||
27325|Barfield Formation|30743|6|Mentioned|p24|||Geological map||||||
27325|Barfield Formation|30916|6|Mentioned|p98|||||||||
27325|Barfield Formation|31079|6|Mentioned|Fig. 6|||||||||
27325|Barfield Formation|32577|6|Mentioned|p23|||Unit of Blenheim Sub Gp.||||||
27325|Barfield Formation|33711|6|Mentioned|Table 3|||||||||
27325|Barfield Formation|33745|6|Mentioned|p204|||||||||
27325|Barfield Formation|33774|3|Fully described|p35|||Map||||||
27325|Barfield Formation|34132|6|Mentioned|p2|||Upper Permian||||||
27325|Barfield Formation|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
27325|Barfield Formation|35284|6|Mentioned|Fig.1|||||||||
27325|Barfield Formation|35426|3|Fully described|p656|||||||||
27325|Barfield Formation|35845|6|Mentioned|Fig.36|||||||||
27325|Barfield Formation|35873|6|Mentioned|Fig.38|||||||||
27325|Barfield Formation|36241|6|Mentioned|p130|||||||||
27325|Barfield Formation|36243|6|Mentioned|Table 4A|||||||||
27325|Barfield Formation|36333|6|Mentioned|Map legend|Late Permian|Late Permian|Of the Back Creek Group.||||||15-JUL-04
27325|Barfield Formation|36739|6|Mentioned|Fig.2|||||||||
27325|Barfield Formation|36925|6|Mentioned|p179|||||||||
27325|Barfield Formation|37075|5|Briefly described|Table 1|||||||||
27325|Barfield Formation|37756|6|Mentioned|p73|||||||||
27325|Barfield Formation|37858|6|Mentioned|p82|||||||||
27325|Barfield Formation|38204|4|Described|p75|||||||||
27325|Barfield Formation|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27325|Barfield Formation|39212|5|Briefly described|p12|||||||||
27325|Barfield Formation|39252|6|Mentioned|Fig.13|||||||||
27325|Barfield Formation|39261|6|Mentioned|Fig.6|||||||||
27325|Barfield Formation|39262|6|Mentioned|p126|||||||||
27325|Barfield Formation|39267|6|Mentioned|p238|||See also P240||||||
27325|Barfield Formation|39445|5|Briefly described|Table 8|||||||||
27325|Barfield Formation|39943|6|Mentioned|Table 6A|||||||||
27325|Barfield Formation|40091|6|Mentioned|p72|||||||||
27325|Barfield Formation|40093|4|Described|p32|||||||||
27325|Barfield Formation|40539|6|Mentioned|Fig.2|||||||||
27325|Barfield Formation|41246|6|Mentioned|Map legend|Permian||||||||
27325|Barfield Formation|41546|6|Mentioned|Fig.2|||||||||
27325|Barfield Formation|41666|5|Briefly described|p3|||||||||
27325|Barfield Formation|41809|6|Mentioned|p64|||||||||
27325|Barfield Formation|42249|6|Mentioned|p22|||||||||
27325|Barfield Formation|42250|6|Mentioned|Fig.4 P31|||||||||
27325|Barfield Formation|42641|6|Mentioned|Fig.3 P110|||||||||
27325|Barfield Formation|42994|6|Mentioned|p149|||||||||
27325|Barfield Formation|43000|5|Briefly described|p111|||see also Fig.5,p112||||||
27325|Barfield Formation|43017|5|Briefly described|Fig.3,p375|||||||||
27325|Barfield Formation|43050|5|Briefly described|p4|||||||||
27325|Barfield Formation|43185|6|Mentioned|6||Late Permian|||||||
27325|Barfield Formation|43460|14|Not recorded|p100|||||||||
27325|Barfield Formation|43471|14|Not recorded|p247,248|||Megadesmus, Astartila||||||
27325|Barfield Formation|43474|14|Not recorded|p66,74,52,104|||Permian fossils||||||
27325|Barfield Formation|43475|14|Not recorded|p553,555|||||||||
27325|Barfield Formation|43585|6|Mentioned|p15||Late Permian|||||||
27325|Barfield Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
27325|Barfield Formation|43894|14|Not recorded|p791|||||||||
27325|Barfield Formation|43987|14|Not recorded|p267,270|||||||||
27325|Barfield Formation|43994|14|Not recorded|Map Legend|||||||||
27325|Barfield Formation|44118|14|Not recorded|Map Legend||Late Permian|||||||
27325|Barfield Formation|44169|2|Defined|Tb.1,p8,map||Late Permian|||||||
27325|Barfield Formation|44170|4|Described|Tb.1,8,9,11||Late Permian|||||||
27325|Barfield Formation|44218|14|Not recorded|p17,19||Kazanian|||||||
27325|Barfield Formation|44243|14|Not recorded|p649,map||Late Permian|||||||
27325|Barfield Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
27325|Barfield Formation|44381|14|Not recorded|p6|||Equivalent to Orange Creek, Acacia and Passion Hill Formations and to Four Mile Mudstone, Cottenham Sandstone and Station Mudstone.||||||
27325|Barfield Formation|44390|14|Not recorded|p15|||||||||
27325|Barfield Formation|44424|14|Not recorded|p293-301|||Passes laterally into Boomer Formation.||||||
27325|Barfield Formation|44426|14|Not recorded|p11|||||||||
27325|Barfield Formation|44427|14|Not recorded|p159,160,162-165|||Theodore-Banana area.||||||
27325|Barfield Formation|44490|14|Not recorded|p46,48|||Fossils.||||||
27325|Barfield Formation|44514|2|Defined|p27,30||Permian|Conformably overlies Oxtrack Formation. Conformably overlain by Orange Creek Formation. Basal formation of Back Creek Group. (Middle Permian).||||||20-MAY-08
27325|Barfield Formation|44571|2|Defined|p205-206,Fig.28|||||||||
27325|Barfield Formation|44640|14|Not recorded|p30|||||||||
27325|Barfield Formation|44857|14|Not recorded|p96-98||Permian|||||||
27325|Barfield Formation|44859|14|Not recorded|p67,72||Permian|Gastropods. Strotostoma, sp.nov.||||||
27325|Barfield Formation|45006|14|Not recorded|Tb.1,p5,6,97,103,140|||p144||||||
27325|Barfield Formation|45031|14|Not recorded|p9,Fig.3||Permian|||||||
27325|Barfield Formation|45071|3|Fully described|Table 10|||See also p54.||||||16-NOV-15
27325|Barfield Formation|46949|6|Mentioned|Fig.3|||||||||
27325|Barfield Formation|48898|6|Mentioned|p25|||Back Creek Group||||||
27325|Barfield Formation|48900|6|Mentioned|p84|||Table opposite.||||||
27325|Barfield Formation|48919|4|Described|p22|||See also P23-26||||||
27325|Barfield Formation|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Back Creek Group.  Includes Four Mile Mudstone, Cottenham Sandstone, and Station Mudstone Members.||||||17-MAY-04
27325|Barfield Formation|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Back Creek Group. Mudstone, siltstone, lithic and feldspathic sandstone and minor conglomerate.||||||
27325|Barfield Formation|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Back Creek Group.||||||27-MAY-04
27325|Barfield Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province:  eastern margin Bowen Basin.||||||04-FEB-08
27325|Barfield Formation|60282|5|Briefly described|p7|||Mudstone and some lithic sandstone. Passes laterally into undivided rocks of Back Creek Group.||||||20-MAY-08
27325|Barfield Formation|60330|5|Briefly described|p259|Late Permian|Late Permian|Geological Province: Bowen Basin||||||
27325|Barfield Formation|61076|5|Briefly described|p188 Fig. 2|Late Permian|Late Permian|Age: >260Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
27325|Barfield Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
27325|Barfield Formation|61778|5|Briefly described|p239||Late Permian|Geological Province: Bowen Basin.||||||07-FEB-11
27325|Barfield Formation|61782|5|Briefly described|p280|||Of Blenheim Subgroup. Contains tuffs and andesite.||||||
27325|Barfield Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Bowen Basin.||||||
27325|Barfield Formation|63773|6|Mentioned|p1059|||||||||
27325|Barfield Formation|64856|3|Fully described|p42, p49, p52-53, p55 Fig.7, p66, p102|Late Permian|Late Permian|Derrington et al. (1959). Bowen Basin. Mudstones and siltstones with lesser sandstones, tuffs, conglomerates. Unconformably overlies Camboon Volcanics or Buffel Formation. Is overlain by Flat Top Formation. Age from palynoflora (formerly considered APP33, now APP5). Max thickness 714m.| | ||||28-NOV-17
27325|Barfield Formation|64857|5|Briefly described|p118-119, p113 Fig.3|Late Permian|Late Permian|Taroom Trough, Bowen Basin. Marine mudstones overlying the Oxtrack Formation.||||||
27325|Barfield Formation|64858|5|Briefly described|p181, p180 Fig.2, p182 Fig.3, p191|Late Permian|Late Permian|Bowen Basin. Includes coals.||||||30-NOV-09
27325|Barfield Formation|64859|6|Mentioned|p196, 225|Permian|Permian|Gas source rocks.||||||
27325|Barfield Formation|65112|5|Briefly described|p313; p316; p317; 321; Fig 4 p314.|Triassic|Late Permian|Post-extension sequences of the Taroom Trough. Interpreted as turbidite facies.||||Overlies the Oxtrack Formation; underlies Flat Top Formation.|Contains intervals that include breccia, diamictite and conglomerate that interrupted thin marine strata.|22-MAR-12
27325|Barfield Formation|65113|5|Briefly described|p349, Fig 4 p340|Late Permian|Late Permian|Taroom Trough. Deposited in a passive thermal subsidence phase. Fine grained deep water turbidites.Overlies Oxtrack Formation, underlies Flat Top Formation.||||||
27325|Barfield Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
27325|Barfield Formation|65115|5|Briefly described|p413, 415, Fig 2 p403|Kazanian|Ufimian|Underlies the  Flat Top Formation, Overlies the Oxtrack Formation in the Taroom Trough, Bowen Basin. Part of Supersequence D. Includes mud and thin interbeds of feldspathic sandstone, in places calcareous.||||||
27325|Barfield Formation|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|?Underlies the Flat Top Formation, Overlies the Oxtrack Formation in the Taroom Trough, Bowen Basin.||||||
27325|Barfield Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|?Underlies the Flat Top Formation, overlies the Oxtrack Formation in the Taroom Trough, Bowen Basin.||||||
27325|Barfield Formation|65119|6|Mentioned|Fig 4-6, Fig 9-10|||Present in the Cockatoo Creek 1 and Burunga 1 Wells.||||||
27325|Barfield Formation|65388|4|Described|p168-170, p161, 163, 166, 437, 439, 447|Roadian|Kungurian|Of Derrington & others (1959). Back Creek Group, Bowen Basin. Massive mudstone and subordinate siltstone, sandstone, tuff and conglomeratic mudstone and limestone sequence, dominantly marine,  conformably overlying the Oxtrack Formation in the Banana and Cracow areas, or disconformably overlying Buffel Formation, Camboon Volcanics. Conformably overlain by the Flat Top Formation. Correlated with Moah Creek beds. Age from marine fossils and palynoflora - Ufimian - Kazanian. Fossils correlated with Ingelara and lower Peawaddy Formations. Generally poor exposure. Minor tuff in upper part of Fmn.||||||16-NOV-15
27325|Barfield Formation|66615|6|Mentioned|p2 Fig.1, p9|||Southern Taroom Trough, Bowen Basin.||||||
27325|Barfield Formation|67402|6|Mentioned|p21, p45|Capitanian|Capitanian|Bowen Basin. ||||Overlain by the Burunga Formation. Overlies the Oxtrack Formation.||
27325|Barfield Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Flat Top Formation. Underlain by Oxtrack Formation.||
27325|Barfield Formation|68679|4|Described|p350, p353, p378, p380-382, p419|Permian|Permian|Derrington et al. (1959). SE Bowen Basin. 900m thick. Offshore marine with local turbidite fan deposits. Mentioned as having the same fossil species as, and thus establishing the age of, the Warminster Formation (Yarrol Province).||Back Creek Group.|Cottenham Sandstone Member.|Overlies Oxtrack Formation. Is overlain by Flat Top Formation. Correlates with Muggleton Formation. Is intruded by The Pride Gabbro.|Mudstone, siltstone and tuff; conglomerate and sandstone occur locally; marine fossils.|
27325|Barfield Formation|73450|6|Mentioned|p55|||Bowen Basin.||||||
27325|Barfield Formation|73570|6|Mentioned|p916|Late Permian|Late Permian|||||||
27325|Barfield Formation|73625|6|Mentioned|p5 Fig.3|Permian|Permian|Taroom Trough, Eastern Bowen Basin.||||Overlies Moah Creek Beds. Is overlain by Flat Top Formation.||
23361|Barmedman Granite|22638|4|Described|p76|Late Devonian|Late Devonian|Age 364 +/-2 Ma.||||||
23361|Barmedman Granite|24007|6|Mentioned|p329|Devonian|Devonian|||||||
23361|Barmedman Granite|24101|6|Mentioned|p110 Fig.3|||Geological Province: Lachlan Fold Belt||||||26-NOV-04
23361|Barmedman Granite|24106|6|Mentioned|p188|||||||||
23361|Barmedman Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
23361|Barmedman Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
23361|Barmedman Granite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
23361|Barmedman Granite|50191|6|Mentioned|p27|Late Devonian|Late Devonian|||||||
23361|Barmedman Granite|60423|6|Mentioned|p372|||Geological Province: Lachlan Fold Belt.||||||
23361|Barmedman Granite|72084|5|Briefly described|p39-40|||||||||
31550|Barmedman Suite|42726|5|Briefly described|map legend||Late Devonian|||||||
31550|Barmedman Suite|44093|5|Briefly described|p179 App. 1|Early Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
31550|Barmedman Suite|44192|5|Briefly described|Map Legend|||||||||
31550|Barmedman Suite|60423|5|Briefly described|p372, Fig. 3|Late Devonian|Late Devonian|Potassic I-Type granites. Of the Temora Complex/Narraburra Complex. Age: ~364Ma. Geological Province: Lachlan Fold Belt.||||||
24694|Barnby Hills Shale|6969|5|Briefly described|p12|Pridoli|Ludlow|Of the Mumbil Group.  Early graptolites found near Eurimbla.  Geological Province: Lachlan Fold Belt.||||||
24694|Barnby Hills Shale|13996|6|Mentioned|p130-131|Silurian|Silurian|Allochthonous blocks contain Ludlow-aged conodonts (species listed). Graptolites mentioned.||||||
24694|Barnby Hills Shale|22857|4|Described|p466 App.1 Tb.A1.6|Pridolian|Ludlovian|Of the Mumbil Group. Thinly interbedded shale, siltstone and minor quartzose arenite; minor limestone. Max. thickness: 450m.||||||
24694|Barnby Hills Shale|23043|5|Briefly described|Map Legend|Lochkovian|Ludlow|of Mumbil Group.||||||
24694|Barnby Hills Shale|23048|5|Briefly described|p11 table2||Ludlow|||||||
24694|Barnby Hills Shale|23170|2|Defined|p89|Devonian|Ludlow|of Mumbil Group. Supersedes 'Barnby Hills Shale Member'.||||||13-MAR-12
24694|Barnby Hills Shale|23214|3|Fully described|p133|Lochkovian|Ludlow|Of Mumbil Group. Originally included in Molong Beds.  Max. thickness 600m.||||||
24694|Barnby Hills Shale|23225|6|Mentioned|p12|Pridoli|Ludlow|Lateral facies equivalent of the Narragal Limestone. derived from Narragal Limestone? of Mumbil Group. Underlying unit Narragal Limestone.||||||
24694|Barnby Hills Shale|23335|6|Mentioned|p17|||||||||27-OCT-04
24694|Barnby Hills Shale|24029|6|Mentioned|p118|Ludlow|Ludlow|||||||
24694|Barnby Hills Shale|24247|5|Briefly described|p37|Late Silurian|Late Silurian|See also p39 Fig.2. Shale, chert, metadolerite, rhyolite||||||
24694|Barnby Hills Shale|30099|6|Mentioned|Fig.2|||||||||
24694|Barnby Hills Shale|31543|6|Mentioned|p111|||||||||
24694|Barnby Hills Shale|32154|6|Mentioned|p181|||Stratigraphy. Refers Vandyke (1970 unpubl.)||||||
24694|Barnby Hills Shale|33611|6|Mentioned|p127|||Mumbil Group||||||10-SEP-18
24694|Barnby Hills Shale|40328|4|Described|p146|||||||||
24694|Barnby Hills Shale|43127|5|Briefly described|p4,Fig.2,Fig.3||Late Silurian|||||||
24694|Barnby Hills Shale|43517|14|Not recorded|p153-4,160||Ludlovian|Upper member of Mumbil Formation||||||
24694|Barnby Hills Shale|43640|5|Briefly described|Map Legend||Silurian|||||||
24694|Barnby Hills Shale|43653|5|Briefly described|Map Legend||Silurian|||||||
24694|Barnby Hills Shale|43782|5|Briefly described|Map Legend|Lochkovian|Ludlow|of Mumbil Group.||||||
24694|Barnby Hills Shale|50095|4|Described|p108 Fig.1, p109 Fig.2|Silurian|Silurian|Overlain by Camelford Limestone, probably conformably. Shale, chert, meta-dolerite, rhyolite and limestone blocks.||||||
24694|Barnby Hills Shale|50124|5|Briefly described|p126|||Of the Mumbil Group. Geological Province: eastern Lachlan Fold Belt.||||||
24694|Barnby Hills Shale|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Mumbil Group.  Thinly interbedded shale, siltstone and minor quartzose sandstone.||||||
24694|Barnby Hills Shale|60332|5|Briefly described|p938|Ludlow||Conformably overlain by Camelford Limestone.||||||
24694|Barnby Hills Shale|60424|5|Briefly described|p350 Fig. 1, p351 Fig. 2|Silurian|Silurian|Of the Mumbil Group. Geological Province: Hill End Trough. Siltstone, shale; minor sandstone.||||||
24694|Barnby Hills Shale|60987|3|Fully described|p153-155, p157-161, p164-165      |Late Ludlow|Late Wenlock|Originally the Barnby Hills Shale Member of Strusz (1960), of his Mumbil Formation. Raised to Formation status by Vandyke and Byrnes (1976). Lachlan Fold Belt. The original type section was a road cutting just E of the Mitchell Highway at Neurea; this is so degraded a new type section along a railway cutting at Dripstone was proposed by Morgan (in Meakin and Morgan, 1999). 209m thick. Contains a diverse graptolite fauna (described in detail).||Mumbil Group.||Conformably overlies Narragal Limestone. Is overlain conformably by Camelford Limestone. Is faulted against Catombal Group and Cuga Burga Volcanics.|Shale and siltstone; subordinate chert, meta-dolerite, rhyolite, Ordovician limestone blocks, and isolated blocks of Camelford Limestone.|
24694|Barnby Hills Shale|66197|5|Briefly described|p633 Fig.4b, p633 Fig.4c|Lochkovian|Ludlow|Molong High-Hill End Trough. Deep marine shale.||||Underlies the Bay Formation and Cuga Burga Volcanics; overlies the Mullions Range Volcanics and Narragal Limestone.||14-MAR-12
24694|Barnby Hills Shale|67322|5|Briefly described|p25|Late Silurian|Late Silurian|Allochthonous Late Ordovician limestone clasts occur in this unit.|||||Shale containing allochthonous limestone clasts.|21-FEB-18
24694|Barnby Hills Shale|67493|6|Mentioned|p79|Ludlow|Ludlow|Upper part of this unit contains Linograptus posthumus introversus, specimens of which were also found in the Lone Star Siltstone (northeastern Tas).||||||
24694|Barnby Hills Shale|68003|5|Briefly described|p24 Fig.3-e, p146. |Pridoli|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Mumbil Group.|||Poorly bedded to laminated, buff to brown to grey, quartzose shale and siltstone; minor rhyolitic tuff and tuffaceous sandstone; calcareous sandstone and siltstone.|
24694|Barnby Hills Shale|68592|6|Mentioned|p912, p1877|Ludlow|Ludlow|Central west NSW. Includes Ludlovian allochthonous limestone blocks containing Ozarkodina sp.nov. conodonts, resembling those in Lookdown Limestone Member in Goulburn and Wollongong areas. Also contains one of only two occurrences of the dendroid graptoloid Dictyonema delicatulum barnbyensis.||||||
24694|Barnby Hills Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
24694|Barnby Hills Shale|70754|5|Briefly described|p447, p451, p461-462, p467-480|Late Silurian|Late Silurian|Numerous Late Ordovician fossil species listed. Systematic palaeontological descriptions.|||||Graptolitic shales, with early Eastonian allochthonous limestone blocks (of Bowan Park Subgroup).|
24694|Barnby Hills Shale|71069|6|Mentioned|p146|||||||Part equivalent to the De Drack Formation.||
24694|Barnby Hills Shale|71600|6|Mentioned|p23 Fig 1|Silurian|Silurian|Geological province: Lachlan Fold Belt.||Unit of Mumbil Group.||||
24694|Barnby Hills Shale|71656|6|Mentioned|p31|Ludlow|Ludlow|Not shown in correlation chart (Fig.2). Ozarkodina conodonts compared with those in Lookdown Limestone Member.|||||Contains allochthonous limestone blocks.|
24694|Barnby Hills Shale|73299|6|Mentioned|p1102 Fig.8, p1105|Early Devonian|Late Silurian|Molong High. Hill End Trough, western. [Map symbol suggests Silurian age]||||Overlies the Mullions Range Volcanics, Narragal Limestone, underlies the Bay Formation, Cuga Burga Volcanics.||
24694|Barnby Hills Shale|73492|5|Briefly described|p696-697, p703|Late Silurian|Late Silurian|Contains allochthonous limestones with T. blandus Biozone fauna of early Katian age.|||Underlies Cuga Burga Volcanics|||
36970|Barney House Gabbro|23720|5|Briefly described|Map Legend|Early Permian|Early Permian|Olivine gabbro.||||||15-DEC-04
36970|Barney House Gabbro|71628|5|Briefly described|p2: 14-17, 32-33, 51, 61; p3-36|||Binns et al. (1967). Forms a small (100 x 300m) intrusion located 25 km SSE of Armidale. Primitive, uncontaminated and undifferentiated magma. Mineralogy and geochemistry described in some detail. Has strong compositional similarities with Big Bull Gabbro.|303.9 +/- 3.2 Ma (SHRIMP: McKibbin et al.,2017).|Bakers Creek Supersuite.||Intrudes Girrakool beds. Abuts and intrudes the Enmore Monzogranite.|Fine- to medium-grained, locally porphyritic, olivine orthopyroxene gabbro.|
23362|Barneys Spring Andesite Member|721|5|Briefly described|Map legend|Namurian|Namurian|Porphyritic andesite.||||||
23362|Barneys Spring Andesite Member|22857|5|Briefly described|p496 App.1 Tb.A1.7|Visean|Visean|Of the Caroda Formation. Porphyritic Andesite. Geological Province: Tamworth Forearc Basin.||||||
23362|Barneys Spring Andesite Member|41009|3|Fully described|p4|||||||||
23362|Barneys Spring Andesite Member|43091|5|Briefly described|Map legend|||||||||
23362|Barneys Spring Andesite Member|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geol. Prov.: New England Fold Belt.||||||
23362|Barneys Spring Andesite Member|50629|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Caroda Formation.  Geological Province: New England Orogen.||||||
70451|Barongarook Ignimbrite Member|62095|2|Defined|p279 Appdx.|Permian|Permian|Of the Woodton Formation. See also the misspelt Barangarook Tuff Formation (should be Barogarook Tuff Formation) and abbreviated version, Barongarook Member. Beige unwelded ignimbrite. Thickness: 12m. See also Plate 1, p260 Tb. 1.||||||22-MAY-06
76020|Baroorangee Creek Formation|66623|1|Redefined|pp74-75, pp81-83. |Middle Cambrian|Middle Cambrian|Redefined in this publication; formerly part of Wonominta beds (Warris 1967), then Baroorangee Creek Subgroup (Buckley 2000). Multiply-deformed schistose facies, upthrust on a series of faults. Schists are siliceous and potassic rather than peraluminous. No fossils identified.||Basal unit in Ponto Group.||Is overlain by Weinteriga Creek Formation. Intruded by Macs Tank and Cliffs Tank Ultramafic Complexes, and Bittles Tank Volcanics dolerite dykes. Is overlain unconformably by Ravendale Formation.|Medium- to coarse-grained quartz-mica schist and micaceous, schistose metasandstones, lesser units of metabasalts; very minor calcite-quartz schist, magnetite-chlorite schist; rare quartz-hematite schist, feldspathic metatuff, quartz-magnetite rock.|
76020|Baroorangee Creek Formation|66918|5|Briefly described|Map legend|Cambrian|Cambrian|The red-brown to black quartz-magnetite rock and pyritic quartz veins are mapped separately from the schists and dolerite.||Unit in Ponto Group.||Is overlain by Bittles Tank Volcanics.|Mica schists including magnetite-chlorite schist, hematite-quartz gneiss, minor dolerite; very minor calcite-quartz schist. Also red-brown to black, very fine-grained quartz and magnetite rock; white quartz veins with pyrite.|
76020|Baroorangee Creek Formation|67322|5|Briefly described|p11, p39, p20 Fig.5|Cambrian|Cambrian|Previously the Baroorangee Subgroup. More metamorphosed (lower amphibolite grade) than rest of Ponto Group. Age determined from p20 Fig.5 (Strat. column) - not well constrained. Occurs in the Kayrunnera-Koonenberry region.||Of the Ponto Group.||||21-FEB-18
76020|Baroorangee Creek Formation|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|Un-named unit: red-brown to black, very fine-grained, well-banded or laminated to locally massive quartz and magnetite rock; milky white quartz veining contains pyrite, discontinuous boudins.||Ponto Group|Includes un-named unit.||Mica schists including magnetite-chlorite schist, hematite-quartz gneiss and very minor calcite-quartz schist, with minor dolerite intrusions.|
76020|Baroorangee Creek Formation|70651|5|Briefly described|Map Legend|Cambrian|Cambrian|||Ponto Group|||Mica schists including magnetite-chlorite schist, hematite-quartz gneiss, and very minor calcite-quartz schist, with minor dolerite intrusions.|
34265|Barrallier Ignimbrite|22678|4|Described|Fig3p714,723-25||Early Devonian|Of the Bindook Volcanic Complex. Max Age: 399 (+/-) 7 Ma.||||||17-JAN-06
34265|Barrallier Ignimbrite|50234|5|Briefly described|Map Legend|Emsian|Pragian|Of the Bindook Volcanic Complex.  Bluish grey, welded, dacitic ignimbrite containing fractured phenocrysts of plagioclase, quartz, hornblende, enstatite, with minor biotite set in a recrystallised quartzo-feldspathic groundmass.||||||12-MAY-04
34265|Barrallier Ignimbrite|63151|5|Briefly described|p4|||Max. thickness: 700m; min. thickness: 500m.  A dacitic pyroclastic flow deposit in the northern part of the Bindook Volcanic Complex.||||||05-APR-07
34265|Barrallier Ignimbrite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Bindook Gp. Bluish-grey, welded, crystal-rich, compositionally uniform dacitic ignimbrite containing whole + fractured phenocrysts of plagioclase, quartz, hornblende, ferroan enstatite, with minor augite and biotite set in ...||||||09-SEP-08
34265|Barrallier Ignimbrite|66300|5|Briefly described|p76, 85.|||Age indistinguishable from Marulan Granite (416.7 +/- 3.1Ma) and from Kerillon Tuff (412.7 +/- 2.2 Ma).|414.4 +/- 2.9 Ma.|Unit in Bindook Group.||||29-OCT-13
34265|Barrallier Ignimbrite|68592|2|Defined|p1061-70, p1074-8, p1141-7, p1628, p1632|Pragian|Pragian|See also p138, p226-8, p241, p269, p843, p847, p859-60, p872, p884. Formerly included in undifferentiated Bindook Porphyry by McElroy and Relph (1961). A large area of hypersthene porphyry (now this unit) was distinguished by Scheibner (1973), and part of this unit was mapped as informal Brayton volcanics by O'Reilly (1972). Simpson (1990) distinguished the Barrallier Ignimbrite as a mappable unit; formally defined by Simpson, Carr and Jones (1997). Type and representative sections described. Generally over 500m thick, thinning to S. Has minor deposits of industrial silica and construction materials, eg the proposed Gunlake quarry, NW of Marulan. Is lithologically similar to, but distinguishable from, Back Station Ignimbrite Member. Has petrographic similarities with Banshea Granite. The 'Boulder Conglomerate Member' and overlying 'Lenticle Tuff' unit of Cas et al. (1981) are now included in Murruin Formation (Bindook Group) with the upper part considered as a possible reworked equivalent of Barrallier Ignimbrite. Geochemistry detailed; geophysical properties described. Is comagmatic with Arthursleigh Suite. Correlated with upper part of Murruin Formation and possibly Merrions Formation.. A slightly different SHRIMP U-Pb zircon (Black, 2006) age is also given: 414.5 +/- 3.2 Ma. Carr et al. (1980) obtained a biotite K-Ar isotopic age of 406 +/- 7 Ma.|414.4 +/- 2.9 Ma (SHRIMP U-Pb zircon: Black,2006)|Unit in Bindook Group.||Overlies Joaramin Ignimbrite, and Tangerang Formation disconformably. Is inferred to be faulted against Longreach Volcanics. Is intruded by Lumley, Marulan and Lockyersleigh Granites.|Dark bluish-grey, crystal-rich welded dacitic ignimbrite which is remarkably uniform in composition across its large extent; often forms columnar-jointed cliffs from 30m thick flows. I-type.|
34265|Barrallier Ignimbrite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dkb. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.||Bindook Group|||Massive, welded, crystal rich, compositionally uniform dacitic ignimbrite; whole and fractured phenocrysts are set in a cryptocrystalline to recrystallised matrix.|
34265|Barrallier Ignimbrite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Bindook Group|||Dark bluish grey, massive, welded, crystal rich, compositionally uniform dacitic ignimbrite. Whole and fractured phenocrysts are set in a cryptocrystalline to recrystallised matrix.|
34265|Barrallier Ignimbrite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Bindook Group|||Massive, welded, crystal rich, compositionally uniform dacitic ignimbrite; whole and fractured phenocrysts are set in a cryptocrystalline to recrystallised matrix.|
34265|Barrallier Ignimbrite|70661|3|Fully described|p52 fig 5, p53, p71-p73|Pragian|Lochkovian|Faulted against Adaminaby Group, intruded by Marulan Granite, Arthursleigh Suite.|414.4 +/-2.9 Ma (SHRIMP U-Pb)|Bindook Group||Disconformably overlies Tangerang Formation, overlies Joaramin Ignimbrite probably disconformably, Unconformably overlain by Tallong Conglomerate.|Dark blue-grey, crystal rich, welded dacitic ignimbrite that is uniform in composition over a large area. Mostly massive but in some places flattened pumice clasts define a prominent fiamme foliation. Very rare lithic fragments occur.|
34265|Barrallier Ignimbrite|70876|5|Briefly described|p1, p77|Lochkovian|Lochkovian|Lachlan Orogen.|414.4 +/- 2.9 Ma (Black, 2006)|Bindook Group||||
34265|Barrallier Ignimbrite|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Bindook Group.|||Blue-grey, crystal-rich welded dacitic ignimbrite. Fragmented phenocrysts of plagioclase, quartz and green-brown hornblende. Typically massive but with a fiamme foliation defined by flattened pumice clasts locally.|
34265|Barrallier Ignimbrite|71656|6|Mentioned|p13 Fig.2|Emsian|Emsian|Shown only in correlation chart (Fig.2), as Emsian, but correlated with Murruin Formation which is interpreted to be Lochkovian to Emsian.||Bindook Group||Overlies Joaramin ignimbrite. Shown as lateral equivalent with Murruin Formation.||
34265|Barrallier Ignimbrite|73248|6|Mentioned|p307|||Occurs within the modern Wollondilly catchment.||||||
26371|Barrandella Shale Member|6969|5|Briefly described|p14, p15-16|Early Ludlow|Early Ludlow|Geological Province: Lachlan Fold Belt.||||||
26371|Barrandella Shale Member|13996|5|Briefly described|p142-143, p146|Silurian|Silurian|Yass area. Bivalve taxa distribution Table. A  Ludlow-aged nautiloid discussed. Echinoderm taxa Table.||Silverdale Formation.||||
26371|Barrandella Shale Member|22857|4|Described|p460 App.1 Tb.A1.6|Ludlovian|Ludlovian|Of the Silverdale Formation. Shaly mudstone, limestone, turbiditic siltstone. Max. thickess: 122.8m. Geological Province: Canberra-Yass Shelf.||||||
26371|Barrandella Shale Member|24248|5|Briefly described|p54, p67|Gorstian|Gorstian|Parent: Silverdale Formation. Geological Province: Yass Syncline.||||||
26371|Barrandella Shale Member|30069|5|Briefly described|p5|||See also Table 10||||||
26371|Barrandella Shale Member|32155|6|Mentioned|Fig.1|||Refers fossil occurrences||||||
26371|Barrandella Shale Member|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
26371|Barrandella Shale Member|35386|3|Fully described|p30|||Part of Silverdale Formation||||||
26371|Barrandella Shale Member|39331|6|Mentioned|Fig.5-5|||||||||
26371|Barrandella Shale Member|40328|4|Described|p111|||||||||
26371|Barrandella Shale Member|45075|6|Mentioned|Fig.1|||See also Fig.5||||||
26371|Barrandella Shale Member|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Silverdale Formation (Hattons Corner Group).  Overlies the Bowspring Limestone Member (Silverdale Formation); underlies Hume Limestone Member (Silverdale Formation).||||||
26371|Barrandella Shale Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Silverdale Formation (Hattons Corner Group). Grey mudstone with thin siltstone and very fine-grained sandstone interbeds, fossiliferous shale, and thinly bedded limestone.||||||
26371|Barrandella Shale Member|68592|2|Defined|p560, p562, p575-8, p1869, p1878-9|Gorstian|Gorstian|See also p430 Fig.89. Formerly Barrandella Shale, named after its prolific brachiopods, of Etheridge (1904); wrongly cited by Shearsby (1912) as Barrandella Shales. Transferred by Link (1970, 1971) as Barrandella Shale [sic] Member to his Silverdale Formation. Type section described. Thickens northwards, from 27m to 123m. Richly fossiliferous: fauna listed.||Unit in Silverdale Formation.||Conformably overlies Bowspring Limestone Member. Is overlain conformably by Hume Limestone Member.|Fossiliferous green or grey shaly mudstone containing thin beds of turbiditic siltstone, calcareous siltstone and shale; minor thin interbedded crinoidal limestone.|12-JAN-17
26371|Barrandella Shale Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Shsr. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Silverdale Formation||Is overlain by Hume Limestone Member. Overlies Bowspring Limestone Member.|Fossiliferous, shaly mudstone with thin beds of siltstone, calcareous siltstone and shale; minor, thin, interbedded crinoidal limestone.|
26371|Barrandella Shale Member|70540|5|Briefly described|Map Legend|Devonian|Silurian|||Silverdale Formation|||Fossiliferous, shaly mudstone with thin beds of siltstone, calcareous siltstone and shale; minor, thin, interbedded crinoidal limestone.|
26371|Barrandella Shale Member|70546|5|Briefly described|Map Legend|Devonian|Silurian|||Silverdale Formation|||Fossiliferous, shaly mudstone with thin beds of siltstone, calcareous siltstone and shale; minor thin interbedded crinoidal limestone.|
26371|Barrandella Shale Member|71656|4|Described|p12 Fig.2, p19, p23-24|Ludlow|Ludlow|Contains the greatest diversity of rugose corals in the Yass Basin. A specimen of polyplacophoran (chiton) was found to be the only Silurian example in NSW. Includes tabullate corals, nautiloids, bryozoa and crinoids.||Of Silverdale Formation, Hattons Corner Group||Hattons Corner Group. Overlies Bloomfield Limestone Member and underlies Hume Limestone Member.|Fossiliferous shales.|
35611|Barrat Formation|61964|3|Fully described|p14 Fig. 4, p115-116, p117 Fig. 35|Frasnian|Frasnian|Supersedes "Barrat Conglomerate". Basal unit of Cocoparra Gp. Mainly pebbly polymictic paraconglom., pebbly sandstone, med.grained lithic sandstone, quartz-lithic sandstone + minor siltstone. Conformable below Naradhan Sandstone and Hazeldene Sandstone||||||
35611|Barrat Formation|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Conglomerate, pebbly sandstone, lithic sandstone, sandstone and siltstone.||||||
35611|Barrat Formation|69160|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.||Is overlain by Hazeldene Sandstone.|Conglomerate, pebbly sandstone, lithic sandstone, sandstone and siltstone.|
35611|Barrat Formation|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.||Unconformably overlies Bootheragandra Group. Is overlain by Naradhan Sandstone.|Conglomerate, pebbly sandstone, lithic sandstone, sandstone and siltstone.|
35611|Barrat Formation|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|||Conglomerate, pebbly sandstone, lithic sandstone, sandstone and siltstone.|
35611|Barrat Formation|69164|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|||Conglomerate, pebbly sandstone, lithic sandstone, sandstone and siltstone.|
35611|Barrat Formation|71889|4|Described|p46, p48-p50, p52-p54, p56|||Wynn (1962b) first named and descirbed the unit. The unit was further described by Connolly (1966 and 1969) and Colquhoun et al (2005a). In the present study the unit is described as ranging from the highest level of widespread pebble occurrence in the sequence to any sandstone or (rare) finer grained lithologies below this level. An unnamed informal unit is recognised in places between this formation and the Naradhan Sandstone.||Cocoparra Group||Overlain by the Bogolong Formation. Equivalent to and conformably overlain (in part) by the Naradhan Sandstone.|Medium to coarse grained conglomerate, sandstone and rare finer grained sedimentary rocks.|
35611|Barrat Formation|72083|4|Described|p7, p9, p39-43, p45, p48|||Mapped by Pogson (1974). Stratigraphy is doubtful: this unit may include the Bogolong Formation and Narrandera Sandstone; discussed. 40-170m thick. Braided river deposits.||Basal Cocoparra Group.||Is overlain by Bogolong Formation and Naradhan Sandstone.|Basal crowded matrix-supported cobble conglomerate with minor rounded quartz clasts, passing upwards into typical quartz clast dominated conglomerate. Local lenses and beds of red-purple, fine-grained sandstone.|
74589|Barrier Suite|64097|5|Briefly described|p3234|||Of the Potosi Supersuite.||||||07-FEB-11
82347|Barrington River Granodiorite|71628|4|Described|p6: 2, 4-8, 10-16, 18-19; p9-1|||New name (this study) after the Barrington River pluton of Mason and Kavalieris (1984). One of three units that replaced Barrington Tops Granodiorite, in Bryant et al. (2003), after unpublished work by Chappell and Bryant (1994). Named after a local watercourse. An irregularly-shaped (~22 km x ~7 km) intrusion ~40 km W of Gloucester. Poor outcrops of rounded boulders and low-level whalebacks. Limited geochemistry described.|277.1 +/- 1.9 Ma (Waltenberg et al., 2015).|Omadale Brook Suite.|Glowang Granodiorite Phase.|Intrudes Isismurra Formation.|Equigranular, medium-grained orthopyroxene-clinopyroxene-(amphibole-biotite) granodiorite; minor dark grey, biotite-clinopyroxene-orthopyroxene granodiorite and amphibole-(pyroxene-opaque oxide) granodiorite. Micrographic textures common. I-type.|
82349|Barrington Tops Supersuite|71628|5|Briefly described|p6: 1-25; p9: 2-3|||New unit and name (this study) to delineate a group of rocks that occurs within the Barrington Tops Complex (formerly Barrington Tops Granodiorite). Has the same constituents as Barrington Tops Complex [??!] but the author claims that this ""facilitates alteration to the Barrington River Supersuite"" [a unit name which does not appears again in the 1,153 pages of this study]. Contrasted with Clarence River Supersuite. Intrudes the Tamworth Belt (forearc basin sediments). Geochemistry briefly summarised.|280-265 Ma.||Barrington Tops Complex, i.e. Omadale Brook, Gummi Plain, Barrington River, Gloucester Tops Granodiorites; Omadale Brook, Gummi Plain Suites.||A magmatic complex incorporating early quartz diorite dykes and stocks, clinopyroxene-orthopyroxene granodiorite and hornblende-biotite-granodiorite plutons (dominant), and later aplitic, granodioritic and hornblende-phyric dykes. I-type.|
31549|Barry Suite|42726|5|Briefly described|map legend||Silurian|||||||
31549|Barry Suite|44093|5|Briefly described|p201 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31549|Barry Suite|68592|6|Mentioned|p1318|||Brief comparison with Gunning Suite geochemistry.||||||
29526|Bartletts Creek Granite|22679|4|Described|p 44- 45|||||||||
29526|Bartletts Creek Granite|23214|3|Fully described|p166|Silurian|Silurian|Intrudes Adaminaby Group. Probably S-type granite. Geological Province: Wyangala Batholith.||||||
29526|Bartletts Creek Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Biotite granite.||||||17-JUL-08
29526|Bartletts Creek Granite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Wyangala Batholith.||||||17-JUL-08
29526|Bartletts Creek Granite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian S-type granitoids.||||||
68979|Basin Tuff|60299|5|Briefly described|p211|Early Permian|Early Permian|Located at Kankool, NSW||||||
24700|Bass Point Sandstone|29901|4|Described|Table 1|||||||||
24700|Bass Point Sandstone|36220|6|Mentioned|Table 33|||||||||
24700|Bass Point Sandstone|36223|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
24700|Bass Point Sandstone|61155|5|Briefly described|p19|Pleistocene|Pleistocene|In the Bathurst-Goulburn region. ||||||
35879|Basso Suite|23347|3|Fully described|p51 Tb. 1, p53 Fig. 3, p55|Paleoproterozoic|Paleoproterozoic|Characterises lower part of Willyama Supergroup, the Curnamona Group. Comprises Abminga and Ameroo Subsuites, and Ameroo Gneiss. Age: 1.69Ga and less. Albitic granofels and granite gneiss; A-type.||||||24-MAR-09
35879|Basso Suite|24307|6|Mentioned|p975 Tb. 1|||||||||
35879|Basso Suite|60485|5|Briefly described|p26|||Includes the Abminga Subsuite volcanics.||||||
35879|Basso Suite|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.71 Ga (U-Pb)|||Intrudes the Curnamona Group. Is intruded by Lady Louise Suite.|Albitic granofels and granite gneiss.|
35879|Basso Suite|61736|5|Briefly described|p666 Fig. 3, p673|Paleoproterozoic|Paleoproterozoic|Ages: 1713+/2, 1710+/-3, 1713+/-3Ma. Geological province: Olary Domain.||||||
35879|Basso Suite|62373|6|Mentioned|p503, p504 Fig.3|||Synsedimentary a-type.||||||
35879|Basso Suite|62514|5|Briefly described|p746, p748 Fig. 3|Paleoproterozoic|Paleoproterozoic|Intrudes the Willyama Supergroup.  A-type granitoids. Age: ca.1.71-1.70Ga. Geological Province: Olary Domain/Curnamona Province.||||||01-DEC-09
35879|Basso Suite|62535|5|Briefly described|p666, p672-673|Paleoproterozoic|Paleoproterozoic|Several age determinations given.|1713 +/- 3 Ma.|Wiperaminga Subgroup.|||Felsic metavolcanic rocks.|
35879|Basso Suite|62536|5|Briefly described|p643|||Olary Domain. Coeval with Alma Gneiss (Broken Hill area).|1720-1705 Ma.|||||
35879|Basso Suite|62592|5|Briefly described|p14, p16 Fig.2.2.|Statherian|Statherian|Olary Domain. A-type magmatism. Hosts Au-Cu deposits.|1718-1712 Ma.|||Intrudes Curnamona Group. Is cut by Lady Louise Suite.|Includes mafic volcanics.|
35879|Basso Suite|62728|5|Briefly described|p24, p28|||A set of felsic granitic gneisses and albitic granofels. A-type. The granitoid component is Ameroo Subsuite, outcropping in Olary Domain. Geol.P: Olary Domain/Curnamona Province.||||||07-FEB-11
35879|Basso Suite|62993|5|Briefly described|p2, p8, p12, p39, p40|Paleoproterozoic|Paleoproterozoic|In the form of a sill at the Mount Mulga Mine traverse.Intruded by mafic dykes (Lady Louise Sute) at Mulga Bore Creek.|1718 - 1711 Ma||Includes Ameroo Subsuite, Abminga Subsuite|Intrudes Willyama Supergroup, Curnamona Group, George Mine Formation. Intruded by Lady Louise Suite|Includes foliated A-type metagranite.|19-DEC-21
35879|Basso Suite|63020|5|Briefly described|p983, p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Consists of lavas, volcaniclastics and shallow subvolcanic granite sills of felsic A-type composition. Age: 1715-1710Ma. Geological Province: Curnamona Province.||||||07-NOV-08
35879|Basso Suite|63102|4|Described|p6,10-11,13-14,16,20,28,30-32|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Extensive in central part of Olary Domain. A-type igneous magmatism coeval with Curnamona Group sedimentation i.e. Montstephen Basalt. Has U-Pb zircon ages including 1712+\-3 and 1713+\-3 Ma (Mulga Bore Creek), 1707+\-3 Ma (Cathedral Rock) and 1715+\-3 Ma (Mount Howden). See p39 for additional zircon U-Pb results. See also p35,38-40,52/|~1715-1710 Ma|Unit of Ethiudna Subgroup.|Includes the Abminga Subsuite and the Ameroo Subsuite.||Felsic subvolcanic intrusives, volcanics and epiclastics with possible coeval mafic volcanics.|22-OCT-19
35879|Basso Suite|63186|5|Briefly described|p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1705 Ma. Geological Province: Curnamona Province.||||||07-NOV-08
35879|Basso Suite|63224|6|Mentioned|p12|||Geological Province: Curnamona Province.||||||07-FEB-08
35879|Basso Suite|63866|4|Described|p37, p40-p41, p49|Statherian|Statherian|Olary Domain, Curnamona Province. |1710 +/- 9 Ma (Conor et al., 2006)||Includes the Amaroo Subsuite and the Abminga Subsuite.|Intrudes the Curnamona Group.||
35879|Basso Suite|64741|5|Briefly described|p301 Fig. 4, p302|Paleoproterozoic|Paleoproterozoic|Includes Abminga Subsuite. Intrudes the Curnamona Group. Age: 1719-1713Ma. Geological province: Olary Domain. A-type felsic quartz-eye volcanic units and subvolcanic granite sills intercalated with the Wiperaminga and Ethiudna Subgroups.||||||07-FEB-11
35879|Basso Suite|64742|6|Mentioned|p320, p321 Fig.3.||||c.1715-1710 Ma.|Unit in Curnamona Group.||||29-MAR-12
35879|Basso Suite|64944|5|Briefly described|p27, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Associated with the Curnamona Group. Age: 1719-1713Ma (mainly 1718-1715Ma). Geological province: Olary Domain. A-type igneous rocks.||||||07-FEB-11
35879|Basso Suite|65220|5|Briefly described|p21 Fig.3|Statherian|Statherian|1715-1700 Ma, A-types||||||10-DEC-09
35879|Basso Suite|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||c.1710 Ma.|||||
35879|Basso Suite|66302|5|Briefly described|p36 Fig.9, p37|Statherian|Statherian|Olary Domain, Curnamona Province. Largely A-type igneous and volcanic rocks. |ca. 1715-1719 Ma||Includes the Abminga and Ameroo Subsuites.|Intrudes the Curnamona Group.||
35879|Basso Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Olary Domain, Curnamona Province.|1713 +/- 3 Ma to 1710 +/- 3 Ma.|||Intrudes Wiperaminga Subgroup.||
35879|Basso Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|ca. 1712 +/- 2 Ma - 1699 +/- 10 Ma||||A-type metagranitoids and felsic metavolcanics.|02-APR-14
35879|Basso Suite|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
35879|Basso Suite|67653|6|Mentioned|p4|||Geological province: Curnamona Province. |||||medium- to coarse-grained and massive, rangingM from tonalite to monzogranite, and accompanied by abundant alaskitic pegmatites.|
35879|Basso Suite|68126|6|Mentioned|p6, p26, p30|||Olary Domain, Curnamona Province.|c.1715 Ma.|||||
35879|Basso Suite|68315|6|Mentioned|p764|||Curnamona Province.|1.71 Ga.|||||
35879|Basso Suite|69562|6|Mentioned|p674 Fig.6|||||Unit in Ninnerie Supersuite.||||
35879|Basso Suite|70405|5|Briefly described|p1,p15, p33|Paleoproterozoic|Paleoproterozoic||1710 Ma - 1720 Ma|Kalabity Supersuite|Includes Abminga Subsuite, Ameroo Subsuite|Intrudes into Curnamona Group|Felsic igneous rocks.|
35879|Basso Suite|70657|4|Described|p6 Fig.1, p12, p13 Fig.6, p15-16, p18|Statherian|Statherian|See also p21, p23, p26, p30, p32, p45-47, p59. Conor (2000). Curnamona Province. Characterises Curnamona Group of Olary Domain. Regionally extensive and distinctive. In Broken Hill Domain, known only from detrital material. Various ages given between ~1718-1702 Ma. Comprises the co-magmatic (meta)granites, and (meta)rhyolitic volcanics and volcaniclastics of the Curnamona Group. Sodic alteration described.|1719-1713 Ma||Abminga, Ameroo Subsuites.|Extrusive flows in Curnamona Group (Wiperamina and Ethiudna Subgroups). Intruded by Lady Louise Suite.|Volcanics and epiclastics; granite sills. A-type.|
35879|Basso Suite|70658|5|Briefly described|p1-2, 5, 8, 11-12, 15, 29, 32, 42|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|1720-1710 Ma.||Abminga, Ameroo Subsuites.|Associated with the Curnamona Group.|Metagranite; felsic metavolcanics. A-type.|
35879|Basso Suite|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain. Shown only on p2 Fig.2.||||Shown as younger than Willyama Supergroup and older than Lady Louise Suite.||
35879|Basso Suite|73021|6|Mentioned|p224||||1.71 Ga.|Willyama Supergroup.||||
35879|Basso Suite|73030|6|Mentioned|p2150|Statherian|Statherian||ca. 1720-1710 Ma|||||
31450|Bathurst Suite|24278|5|Briefly described|p1765|Late Carboniferous|Late Carboniferous|I-type granitoids. Contains Bruinbun Granite.||||||24-JUL-06
31450|Bathurst Suite|42726|5|Briefly described|Map legend|Carboniferous|Carboniferous|Of the Bathurst Supersuite.  Includes the Icely, Bathurst, Duronal, Eusdah and Tarana Granites.||||||07-FEB-05
31450|Bathurst Suite|44093|5|Briefly described|p207 App. 1|Late Carboniferous|Early Carboniferous|Geological Province: Lachlan Fold Belt.||||||
31449|Bathurst Supersuite|23549|5|Briefly described|Fig 2 p517|||Geological Province: Lachlan Fold Belt.||||||05-APR-05
31449|Bathurst Supersuite|42726|5|Briefly described|Map legend||Carboniferous|Contains the Bathurst, Gulgong, Hartley, Sloggetts and Wuuluuman Suites.||||||07-FEB-05
31449|Bathurst Supersuite|68592|5|Briefly described|p1756|Carboniferous|Carboniferous|Contrasted with the similarly-aged Oberon Supersuite which is less oxidised and has a higher ASI (weakly peraluminous). Plutons in this unit are more elongate E-W compared with the circular intrusions of the Oberon Supersuite.|||||I-type granites.|
31449|Bathurst Supersuite|70297|4|Described|map legend, on side 2 of map sheet|Carboniferous|Carboniferous|Age: Middle to Late Carboniferous.|||Bathurst, Bruinbun, Dunkeld, Durandal, Eusdale, Evans Crown, Falnash, Gresham, Icely, Lewis Ponds, Millah Murrah, Mount Stromlo, Tarana, Wiagdon, Granites.||Potassium-rich, oxidised, I-type biotite(+/- hornblende) granite, leucogranite, granodiorite, aplite, porphyry and rare hornblende gabbro and diorite. Commonly medium- to coarse-grained and equigranular to slightly porphyritic.|17-MAY-16
31449|Bathurst Supersuite|71069|6|Mentioned|p10|Carboniferous|Carboniferous||||Includes the Millah Murrah Granite|||
31449|Bathurst Supersuite|73570|6|Mentioned|p918|Carboniferous|Carboniferous|Lachlan Orogen.|340-312 Ma|||||
68154|Bawley Gabbro|60281|6|Mentioned|p61|||See also Bawley Microgranite - one may supersede the other?||||||17-MAR-05
81159|Beabula igneous intrusions|70718|5|Briefly described|p118, p3, p55, 56|Phanerozoic|Phanerozoic|No outcrop. Intrude Hay-Booligal basement. Aeromag. character: Circulate 2-5 km diameter anomalies with peak amplitudes of approximately 20-40 nT. Interpreted as ultramafic intrusion with modelled depths approximately between 1300-2300m and magnetic susceptibility of approximately 40-90x10-3 SI.|||||Ultramafic intrusions.|07-JAN-22
25779|Beauchamp Falls Shale Member|31373|6|Mentioned|Table 1|||||||||
25779|Beauchamp Falls Shale Member|33683|6|Mentioned|Table 1|||Narrabeen Gp.||||||
25779|Beauchamp Falls Shale Member|33685|6|Mentioned|Table 2|||||||||
25779|Beauchamp Falls Shale Member|34205|2|Defined|p20|Triassic|Triassic|||||||
25779|Beauchamp Falls Shale Member|34209|6|Mentioned|p140|||Triassic. See also Table 1.||||||
25779|Beauchamp Falls Shale Member|37804|6|Mentioned|Table 1|||||||||
25779|Beauchamp Falls Shale Member|39287|6|Mentioned|p42|||||||||
25779|Beauchamp Falls Shale Member|39293|6|Mentioned|p146|||||||||
25779|Beauchamp Falls Shale Member|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
25779|Beauchamp Falls Shale Member|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
25779|Beauchamp Falls Shale Member|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
79400|Beckom South Granite|70777|4|Described|p2-p4, p16-p22, p80-p81, p96|Lochkovian|Lochkovian|Lachlan Orogen. Age provided is interpreted as the age of magmatic crystallisation. Sample location and map sheet are provided. The exposure from which the dated sample was taken had previously been mapped as Ardlethan Granite, however Trigg (2016) defined the Beckom South Granite on the basis of its seperation from dated Ardlethan Granite by ordovician and late devonian rocks. Petrography, zircon description and U-Pb isotopic results are discussed in detail.|413.4 +/- 2.2 ma (this record)||||Leucocratic muscovite-biotite granite.|
79400|Beckom South Granite|72083|6|Mentioned|p37|Devonian|Devonian||c.413 Ma (Bodorkos et al.,in prep.).|||||
24705|Bedlam Formation|37727|4|Described|p37|||See also P17.||||||
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.|
69599|Begargo Leucitite|61155|5|Briefly described|p19|Late Miocene|Middle Miocene|Geological Province: Lachlan Valley.||||||
81963|Belar Member|72700|5|Briefly described|Mapsheet 1|Cenozoic|Cenozoic|||Of Siding Spring Formation.|||Poorly sorted, matrix to clast-supported volcaniclastic mudstone, sandstone, conglomerate and breccia. Inferred lahar deposits.|02-NOV-20
34752|Belgrave Formation|22892|6|Mentioned|p41|Quaternary|Quaternary|||||||
30910|Bell River Member|6969|5|Briefly described|p12|Middle Silurian|Middle Silurian|Of the Dripstone Formation.  Age stated to be Homerian.i.e. Late Wenlock.  Geological Province: Lachlan Fold Belt.||||||
30910|Bell River Member|22857|5|Briefly described|p466 App.1 Tb.A1.6|Wenlockian|Wenlockian|Of the Dripstone Formation (Mumbil Group). Felsic volcanics and limestone. Max. thickness: 120m.||||||
30910|Bell River Member|23043|5|Briefly described|Map Legend|Wenlock|Wenlock|of Dripstone Formation, Mumbil Group.||||||
30910|Bell River Member|23170|2|Defined|p84|Wenlock|Wenlock|of Dripstone Formation, Mumbil Group. Supersedes 'Catombal Park Formation'.||||||
30910|Bell River Member|23225|6|Mentioned|p12||Homerian|of Dripstone Formation. Lachlan Fold Belt.||||||
30037|Bellata Group|22857|5|Briefly described|p520 App.1 Tb.A1.9|Early Permian|Early Permian|Includes the Maules Creek, Leard and Goonbri Formations.||||||
30037|Bellata Group|23566|5|Briefly described|p116 Fig. 2|Early Permian|Early Permian|Includes the Maules Creek, Goonbri and Leard Formations. Geological Province: Gunnedah Basin.||||||01-SEP-15
30037|Bellata Group|43194|5|Briefly described|Appendix 8.1 p133|Early Permian|Early Permian|Encompasses Goonbri, Leard and Maules Creek Formations. Age Stage 2 to Upper Stage 4. Formal definition published in an article released immediately prior, however a summary of new nomenclature is provided in Appendix 1.||||||13-NOV-13
30037|Bellata Group|50629|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Gunnedah Basin.  Includes: Maules Creek Formation, Goonbri Formation, Leard Formation.||||||
30037|Bellata Group|68003|5|Briefly described|p38 Fig.3-j, p129.|Early Permian|Early Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Correlative of Greta Coal Measures in the Hunter Coalfield, and of Koogah and Willow Tree Formations in the Werrie Basin.|||Includes Leard, Goonbri and Maules Creek Formations.|Overlies Boggabri Volcanics and Werrie Basalt. Is overlain by Millie Group.||
30037|Bellata Group|68004|5|Briefly described|p23 Table 1, p139.|||Gunnedah Basin. Coeval with Greta Coal Measures and lower Shoalhaven Group in the Sydney Basin. Kaolin prospectivity is discussed.|||Includes Leard, Goonbri and Maules Creek Formations.|Is overlain by Millie Group.||
30037|Bellata Group|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Early Permian coal measures: conglomerate, lithic sandstone, siltstone, claystone, carbonaceous claystone and coal.||||||
30037|Bellata Group|70791|5|Briefly described|p275-277, p279, p283, p292-293|Cisuralian|Cisuralian|Gunnedah Basin. Hosts large coal seam gas and deep underground coal resources in the Mullaley Sub-basin, and significant open-cut and underground coal mines in the Maules Creek Sub-basin.|||Leard, Goonbri, Maules Creek Formations.|||
30037|Bellata Group|70878|5|Briefly described|p716, p718 Fig.13|Permian|Permian|Gunnedah Basin. 177.27m thick in Santos Slacksmith 1 well.|||Leard, Goonbri, Maules Creek Formations.|Overlies Boggabri Volcanics. Is overlain by Millie Group.||
36330|Bellbird Lens|23540|5|Briefly described|Fig 2 p 419|||Of Paxton Formation.||||||20-FEB-07
36330|Bellbird Lens|69683|6|Mentioned|p411 Fig.2|Middle Permian|Middle Permian|Hunter Coalfield; Lochinvar area.||Unit in Paxton Formation.||||
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.|
37003|Bellingen Slate|22857|5|Briefly described|p516 App.1 Tb.A1.8|Permian||Dark micaceous slate, lithofeldspathic sandstone; minor conglomerate. Max. thickness: >1300m. ||||||
37003|Bellingen Slate|23720|5|Briefly described|Map Legend|||Of Nambucca beds.  Dark micaceous slate, lithofeldspathic sandstone, minor conglomerate.||||||15-DEC-04
37003|Bellingen Slate|24120|5|Briefly described|p6|Permian|Permian|||||||
37003|Bellingen Slate|24129|5|Briefly described|p70|||||||||
37003|Bellingen Slate|44450|5|Briefly described|p20|||Of Nambucca beds. Geological Province: Nambucca Block||||||
37003|Bellingen Slate|71628|5|Briefly described|p3:46|||Nambucca Block.||Nambucca Beds.||Is faulted against (and ?intruded by) Gleniffer Monzogranite.||
24709|Bells Creek Volcanics|22472|5|Briefly described|p36|Silurian|Silurian|of the Mumbil Group||||||
24709|Bells Creek Volcanics|22486|5|Briefly described|p 5, 7|||||||||
24709|Bells Creek Volcanics|22529|6|Mentioned|4 fig 2|Ludlow|Ludlow|Overlying unit Chesleigh Group, underlying unit Tanwarra Shale||||||
24709|Bells Creek Volcanics|22590|6|Mentioned|P750|||||||||
24709|Bells Creek Volcanics|22679|4|Described|p 28, 29||Late Silurian|||||||
24709|Bells Creek Volcanics|22768|6|Mentioned|p180|||||||||
24709|Bells Creek Volcanics|22857|4|Described|p180, p472 App.1 Tb.A1.6|Middle Silurian|Middle Silurian|Of the Mumbil Group. Conformably overlies Tanwarra Shale. Rhyolitic tuffs and lavas; graptolites. Max. thickness: 2400m. Geological Province: Hill End Trough and Capertee Rise.||||||
24709|Bells Creek Volcanics|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Mumbil Group.||||||17-JUL-08
24709|Bells Creek Volcanics|23170|2|Defined|p99|Ludlow|Wenlock|Of Mumbil Group.||||||17-JUL-08
24709|Bells Creek Volcanics|23214|3|Fully described|p141|Lochkovian|Ludlow|Of Mumbil Group. Originally named Bells Creek Rhyolite.  Intruded by both Bathurst and Tarana Granites. Max. thickness 2400m.||||||
24709|Bells Creek Volcanics|23738|5|Briefly described|p251|Silurian|Silurian|Geological Province: Hill End Trough.||||||
24709|Bells Creek Volcanics|24394|5|Briefly described|p170|Ludlow|Ludlow|||||||
24709|Bells Creek Volcanics|29669|6|Mentioned|p604|||||||||
24709|Bells Creek Volcanics|29993|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
24709|Bells Creek Volcanics|30099|6|Mentioned|Fig.2|||||||||
24709|Bells Creek Volcanics|31161|5|Briefly described|PA3|||||||||
24709|Bells Creek Volcanics|31411|6|Mentioned|p16|||||||||
24709|Bells Creek Volcanics|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
24709|Bells Creek Volcanics|32088|6|Mentioned|p10|||||||||
24709|Bells Creek Volcanics|32485|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24709|Bells Creek Volcanics|32621|6|Mentioned|p1|||||||||
24709|Bells Creek Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
24709|Bells Creek Volcanics|32672|6|Mentioned|p672|||||||||
24709|Bells Creek Volcanics|33006|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24709|Bells Creek Volcanics|33282|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24709|Bells Creek Volcanics|33285|6|Mentioned|p20|||Middle Sil.||||||
24709|Bells Creek Volcanics|33742|6|Mentioned|p116|||Equiv. "Vale Cr. Volc."||||||
24709|Bells Creek Volcanics|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
24709|Bells Creek Volcanics|34404|6|Mentioned|Fig.3.5b|||Middle Silurian||||||
24709|Bells Creek Volcanics|34405|4|Described|p105|||||||||
24709|Bells Creek Volcanics|34406|6|Mentioned|p220|||Probably Middle Silurian||||||
24709|Bells Creek Volcanics|34572|6|Mentioned|p84|||Silurian. See also PP87,89 etc.||||||
24709|Bells Creek Volcanics|35185|6|Mentioned|p245|||||||||
24709|Bells Creek Volcanics|35257|6|Mentioned|Fig.32|||||||||
24709|Bells Creek Volcanics|36285|6|Mentioned|Fig.6|||||||||
24709|Bells Creek Volcanics|37727|4|Described|p37|||See also P17 and P30.||||||
24709|Bells Creek Volcanics|39214|6|Mentioned|p25|||||||||
24709|Bells Creek Volcanics|39331|6|Mentioned|Fig.0-3|||See also Fig.7-1||||||
24709|Bells Creek Volcanics|40328|3|Fully described|p163|||||||||
24709|Bells Creek Volcanics|42413|5|Briefly described|p54|||||||||
24709|Bells Creek Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
24709|Bells Creek Volcanics|43188|6|Mentioned|p205|||Sofala district.||||||
24709|Bells Creek Volcanics|43263|6|Mentioned|Map Legend||Silurian|Age Middle Silurian.||||||
24709|Bells Creek Volcanics|43344|14|Not recorded|p139,150,152,153,155||Silurian|||||||
24709|Bells Creek Volcanics|43476|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition)Middle Silurian||||||
24709|Bells Creek Volcanics|43494|5|Briefly described|p24||Silurian|Of the Mumbil Group. Includes rhyolitic rocks forming weathered, massive, blocky outcrops.||||||16-MAR-06
24709|Bells Creek Volcanics|43515|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition) (M.Sil)||||||
24709|Bells Creek Volcanics|43516|14|Not recorded|Map Legend|Early Silurian|Early Silurian|(L-M Sil)||||||
24709|Bells Creek Volcanics|43639|5|Briefly described|Map Legend||Silurian|||||||
24709|Bells Creek Volcanics|43641|5|Briefly described|Map Legend||Silurian|||||||
24709|Bells Creek Volcanics|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group (east). Includes Alton Limestone Member. Rhyolitic tuff and lava, quartz feldspar porphyry, tuffaceous sandstone, breccia.||||||17-JUL-08
24709|Bells Creek Volcanics|43782|5|Briefly described|Map Legend|Lochkovian|Ludlow|Of Mumbil Group.||||||17-JUL-08
24709|Bells Creek Volcanics|43834|6|Mentioned|p32|||Capertee High||||||
24709|Bells Creek Volcanics|44093|5|Briefly described|p207 App. 1|Early Devonian|Early Silurian|Of Mumbil Group. Geological Province: Lachlan Fold Belt.||||||
24709|Bells Creek Volcanics|50124|6|Mentioned|p126|||Geological Province: eastern Lachlan Fold Belt.||||||
24709|Bells Creek Volcanics|68592|5|Briefly described|p624, p650|Late Silurian|Late Silurian|||Unit in Mumbil Group.||Correlated with Cuddyong Formation (Campbells Group).||
24709|Bells Creek Volcanics|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Parent age: late early Silurian to earliest Devonian. ||Mumbil Group|||Submarine to subaerial felsic volcanic units of rhyolitic to dacitic lavas and volcaniclastics.|18-MAY-16
24709|Bells Creek Volcanics|71069|6|Mentioned|p125, p154|||||Mumbil Group||Partly equivalent to the Kohinoor Volcanics.||
24709|Bells Creek Volcanics|73299|6|Mentioned|p1102 Fig.8|||Hill End Trough, eastern. [Map symbol suggests Silurian age]||||Faulted against Sofala Volcanics.||
81954|Belougery Split Rock Member|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Macha Formation|||Orange to white weathering, flow foliated, porphyritic trachyte; contains late, interstitial quartz.|02-NOV-20
30472|Belowra Granodiorite|22815|4|Described|p73|||||||||
30472|Belowra Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Belowra Suite.||||||
30471|Belowra Suite|22815|6|Mentioned|p73|||||||||
30471|Belowra Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Candelo Supersuite. Includes the Belowra Granite (informally named).||||||09-FEB-05
30471|Belowra Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Bega Batholith.||||||
24178|Belowrie Formation|22857|5|Briefly described|p456 App.1 Tb.1A1.6|Devonian|Silurian|Of the Toongi Group. Shale, tuff. Max. thickness: 400m. Geological Province: Cowra Trough.||||||
24178|Belowrie Formation|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Toongi Group.||||||
24178|Belowrie Formation|23170|2|Defined|p118|Late Silurian|Late Silurian|of Toongi Group.||||||
24178|Belowrie Formation|40328|2|Defined|p125|Silurian|Silurian|||||||
24178|Belowrie Formation|68003|5|Briefly described|p24 Fig.3-e, p144. |Ludlow|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Wambangalong Formation. Is overlain by Whylandra Formation.|Shale, minor basic tuff and lava, phyllite.|
30473|Bemboka Suite|22778|5|Briefly described|p 161|||||||||
30473|Bemboka Suite|22815|5|Briefly described|p73|||||||||
30473|Bemboka Suite|23549|5|Briefly described|p518 Fig 4, p516|||Geological Province: Lachlan Fold Belt.||||||05-APR-05
30473|Bemboka Suite|42726|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite.  Includes the Wadbilliga and Bemboka Granites.||||||07-FEB-05
30473|Bemboka Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Bega Batholith.||||||
30473|Bemboka Suite|44093|5|Briefly described|p222 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
70035|Bemm River beds|22857|6|Mentioned|p213|Late Devonian|Late Devonian|||||||
30745|Ben Bullen Igneous Complex|43363|14|Not recorded|Map Legend|||(Provisional first edition)||||||
30745|Ben Bullen Igneous Complex|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|Included in general description for Unassigned mafic intrusions (Ben Bullen Igneous Complex and Greengrove mafic intrusion).|||||Small plutons of hornblende diorite, gabbro and dolerite. Irregular areas of olivine norite, and gabbroic anorthosite. Rare limestone blocks xenoliths at Ben Bullen.|18-MAY-16
33192|Bena Monzodiorite|24417|4|Described|p57|Early Silurian|Early Silurian|Intrudes the Clements Formation.||||||
33192|Bena Monzodiorite|50554|5|Briefly described|Map legend|Silurian|Silurian|Grey-pink, glomero/porphyritic biotite, quartz monzodiorite.||||||
33192|Bena Monzodiorite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||13-JUL-04
41051|Bendemeer Monzogranite|24366|5|Briefly described|p11 Fig. 9|Early Triassic|Late Permian|Of the Moonbi Plutonic Suite.||||||
41051|Bendemeer Monzogranite|68005|5|Briefly described|pp67-68, p133.|Permian|Permian|Listed on p.133 [and in the database] as a unit in Moonbi Suite. Radiometric and magnetic imagery has revealed previously unrecognised concentric zoning in this unit.||Unit in Southern Moonbi Supersuite.|||Medium- to coarse-grained hornblende-biotite monzogranite with prominent pink K-feldspar crystals, and minor titanite and magnetite grains; minor monzonite.|
41051|Bendemeer Monzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca. 247 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
41051|Bendemeer Monzogranite|68679|5|Briefly described|p458, p461 Fig.5.132|||Tamworth district. Geochemical plots.||Moonbi Supersuite.||||
41051|Bendemeer Monzogranite|69323|5|Briefly described|p21,70|Lopingian|Lopingian|Geological province: New England Orogen. Previous SHRIMP U-Pb dating includes 247.5+\-1.6 Ma (Jeon, 2012).|247.5+\-1.6 Ma (Jeon, 2012)|Unit of Moonbi Supersuite.||||
41051|Bendemeer Monzogranite|69639|5|Briefly described|p10, p218|Triassic|Triassic|New England Orogen.|247.5 +/- 1.6 Ma (Jeon, 2012)|Moonbi Supersuite||||
41051|Bendemeer Monzogranite|71628|4|Described|p1:14; p4:15; p7: 1-2, 4, 8, 10-14, 22|||See also p7: 27, 30-31, 35. Brown (2003), after Chappell and Bryant (1994). Previously the Bendemeer Adamellite of Binns et al. (1967) after Chappell (1966). Partly equivalent to the Moonbi granite of Benson (1913, 1915). Named after the village of Bendemeer. Forms a thin (2 to 4 km with no root) ovoid intrusion approx. 11 km x 7 km. Crops out prominently. Has a distinct metamorphic aureole (described). Lithology and mineralogy detailed. Geochemistry described; has similarities with Moonbi Monzogranite.|247.5 +/- 1.6 Ma (SHRIMP: Jeon et al., 2014).|Moonbi Suite.||Intrudes Flaggy Range Monzogranite Phase (Banalasta Monzogranite). Is intruded by Moonbi Monzogranite.|Grey to pale grey, coarse-grained, equigranular to porphyritic biotite-hornblende(-pyroxene) monzogranite, with minor leucomonzogranite and rare granodiorite. I-type.|
41051|Bendemeer Monzogranite|73264|6|Mentioned|p1398 Fig.20, p1399|Triassic|Permian|New England Orogen.|248 Ma|Moonbi Supersuite||||
38325|Bendemeer Supersuite|23812|5|Briefly described|p63|Early Triassic|Late Permian|||||||
38325|Bendemeer Supersuite|61773|5|Briefly described|p139|||Includes the Bendemeer Suite.||||||
38325|Bendemeer Supersuite|61795|6|Mentioned|p368|Early Triassic|Late Permian|Geological Province: New England Fold Belt. I-type granites.||||||17-NOV-08
25781|Bendora Granodiorite|36441|5|Briefly described|map legend|Pridolian|Pridolian|Of Gingera Batholith. Intrusive. S-type. Granodiorite. Intrudes Nungar Beds. BMR map code: Sgo.||||||
25781|Bendora Granodiorite|45147|2|Defined|M214|Late Silurian|Late Silurian|Probably Late Silurian||||||
41275|Benelabri Formation|22857|4|Described|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Coogal Subgroup (Black Jack Group). Interbedded claystone, siltstone and fine-grained quartzose sandstone and coal. Includes Caroona and Howes Hill seams. Max. thickness: 35m. Geological Province: Gunnedah Basin.||||||
41275|Benelabri Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Coogal Subgroup.||||||
41275|Benelabri Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Coogal Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Claystone, siltstone, sandstone, tuff and coal.||||||
41275|Benelabri Formation|65116|5|Briefly described|p447-448, 449, Fig 6, p441|Late Permian|Late Permian|?Of Black Jack Group. Lacustrine unit, Organic rich laminated siltstone, claystone and coal, bioturbation and burrows. Overlies the Hoskisson Coal. Sequence D2||||||
41275|Benelabri Formation|68003|5|Briefly described|p38 Fig.3-j, p41, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Mis-spelt as Benelebri Formation in Fig.3-j.||Unit in Coogal Subgroup.||Overlies Hoskissons Coal and, locally, Clare Sandstone. Is overlain by Clare Sandstone.|Organic-rich, mudstone-dominated freshwater lacustrine deposits.|
41275|Benelabri Formation|68004|5|Briefly described|p23 Table 1. |||Gunnedah Basin.||Unit in Coogal Subgroup.||Is overlain by Clare Sandstone.||
41275|Benelabri Formation|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Gunnedah Basin. CA-TIMS age of 258.08 Ma (Laurie etal., in prep). Corresponding to APP4.2 zone (Guadalupian-Lopingian).||||||
41275|Benelabri Formation|70878|5|Briefly described|p718 Fig.13|Permian|Permian|Gunnedah Basin.|258.05 +/- 0.08 Ma.|Black Jack Group.||Overlies Hoskissons Coal. Is overlain by Wallala Formation.||
26385|Bengalla Coal Member|29942|4|Described|Fig.1|||Permian||||||
26385|Bengalla Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26385|Bengalla Coal Member|68004|6|Mentioned|p51 Table 5.|||||||||
70127|Bengoro Ridge Formation|66623|2|Defined|pp192-193, pp203-204. |Middle Devonian|Early Devonian|Defined in this study. Formerly upper part of Snake Cave Sandstone. Correlated with Muckabunnya Formation and Menamurtee Sandstone. Forms prominent NNW trending strike ridges. Contains 11 taxa of fish fossils, many new forms. Cross-beds common. Further deposition of Wana Karnu Group was terminated by Tabberabberan Orogeny.||Uppermost unit in Wana Karnu Group.||Overlies Shell Hill Formation. Is unconformably overlain by Ravendale Formation.|White to buff quartz sandstone, pebbly sandstone, conglomerate; rare siltstone; sandstones dominate and are fine- to coarse-grained and medium- to thickly-bedded. Conglomerate clasts comprise grey quartzites and vein quartz; rare black volcanics.|
70127|Bengoro Ridge Formation|66918|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Wana Karnu Group.||Overlies Old Coach Road Formation.|White to buff quartz sandstone, pebbly sandstone, conglomerate, and rare siltstone.|
70127|Bengoro Ridge Formation|70650|5|Briefly described|Map Legend|Devonian|Devonian|||Wana Karnu Group|||White to buff quartz sandstone, pebbly sandstone, conglomerate and rare siltstone.|
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.|
35363|Bennys Top Limestone|23185|6|Mentioned|Fig1p156|||||||||
35363|Bennys Top Limestone|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
23378|Benwerrin Diorite|22768|6|Mentioned|p178|||||||||
23378|Benwerrin Diorite|22857|6|Mentioned|p178|Early Devonian|Early Devonian|||||||
23378|Benwerrin Diorite|42313|2|Defined|p140|Late Silurian|Late Silurian|Reserved April 1985. Unrelated to Benwerrin Seam, Vic mentioned in 90/27106.||||||
23378|Benwerrin Diorite|42314|5|Briefly described|Map legend|Late Silurian||||||||
23378|Benwerrin Diorite|42828|5|Briefly described|Fig.2 P128|||||||||
33412|Berendebba Granite|24417|3|Fully described|p106|Early Devonian|Early Devonian|||||||
33412|Berendebba Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|||||||13-JUL-04
33412|Berendebba Granite|60548|6|Mentioned|map legend|||||||||29-NOV-04
29661|Berkley Formation|22768|6|Mentioned|p179-80|||||||||
29661|Berkley Formation|22857|4|Described|p179, p454 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Gregra Group. Overlain by ?Garra Formation; overlies the Maradana Shale. Rich invertebrate fauna. Equivalent to Cuga Burga Volcanics. Max. thickness: 1200m. Geological Province: Cowra Trough/Molong Rise.||||||
29661|Berkley Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Gregra Group.||||||
29661|Berkley Formation|23170|2|Defined|p193|Lochkovian|Lochkovian|of Gregra Group.||||||
29661|Berkley Formation|23214|3|Fully described|p181|Lochkovian|Lochkovian|Of Gregra Group. Previously named Mandagery Park Formation, also parts use to be included in Manildra Beds. Well bedded, lithic, volcaniclastic sandstone with minor siltstone, shale and fossilerous limestone. Max thickness >500m.||||||
29661|Berkley Formation|24248|6|Mentioned|p59|||Supersedes Mandagery Park Formation.||||||
29661|Berkley Formation|43640|5|Briefly described|Map Legend||Devonian|||||||
29661|Berkley Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Gregra Group.||||||
29661|Berkley Formation|60987|5|Briefly described|p155, p157-158, |Early Devonian|Early Devonian|||||Overlies the Hanover Formation. Laterally equivalent to the Cuga Burga Volcanics||
29661|Berkley Formation|66197|5|Briefly described|p633 Fig.4c|Lochkovian|Lochkovian|Cowra Trough-Molong High. Mafic/intermediate volcaniclastics and minor volcanics. Underlies the Garra Formation, overlies the Hanover Formation.||||||13-MAR-12
29661|Berkley Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Grega Group||||
29661|Berkley Formation|71600|6|Mentioned|p23 Fig 1|Devonian|Devonian|Geological province: Lachlan Fold Belt.||Unit of Gregra Group.||||
29661|Berkley Formation|73299|6|Mentioned|p1105|||Cowra Trough. [Map symbol suggests Devonian age]||||Underlies the Garra Formation.||
27336|Berry Siltstone|22500|6|Mentioned|p 7|||||||||
27336|Berry Siltstone|22578|5|Briefly described|p394, Fig.6 p396|||Of Shoalhaven Group.||||||12-MAR-09
27336|Berry Siltstone|22591|5|Briefly described|Fig 2||Late Permian|||||||
27336|Berry Siltstone|22601|6|Mentioned|417|||Geol province Sydney Basin||||||
27336|Berry Siltstone|22663|5|Briefly described|NSW97 - 1 Fig.2|Late Permian|Late Permian|||||||
27336|Berry Siltstone|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Shoalhaven Group. Siltstone. Lithic sandstone, bioturbation. Disconformably overlies Snapper Point Formation. Max. thickness: 230m. Geological Province: Sydney Basin. See also p532 App.1 Tb.A1.9.||||||
27336|Berry Siltstone|22969|4|Described|p 22, Fig 2.2||Late Permian|Max. thickness: 550 m.||||||
27336|Berry Siltstone|22970|5|Briefly described|Plate 6|Late Permian||||||||
27336|Berry Siltstone|23214|4|Described|p265|Late Permian|Early Permian|Of Shoalhaven Group. Sandy grey mudstone. Geological Province: Sydney Basin.||||||
27336|Berry Siltstone|23544|5|Briefly described|Fig 2 p358|||correlate of the Mulbring Formation. Of the Shoalhaven Group in the Sydney Basin. Underlies the Broughton Formation.||||||
27336|Berry Siltstone|29752|3|Fully described|p30|||||||||
27336|Berry Siltstone|29901|5|Briefly described|p163|||||||||
27336|Berry Siltstone|31128|5|Briefly described|p5|||||||||
27336|Berry Siltstone|32769|6|Mentioned|Fig.1|||||||||
27336|Berry Siltstone|32938|6|Mentioned|p67|||Geology||||||
27336|Berry Siltstone|36042|6|Mentioned|Fig.7|||||||||
27336|Berry Siltstone|36220|3|Fully described|p22|||See also Table 1 & 16.||||||
27336|Berry Siltstone|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27336|Berry Siltstone|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27336|Berry Siltstone|38603|6|Mentioned|p79|||||||||
27336|Berry Siltstone|38614|6|Mentioned|Fig.6|||||||||
27336|Berry Siltstone|38615|6|Mentioned|p17|||||||||
27336|Berry Siltstone|38690|6|Mentioned|p288|||||||||
27336|Berry Siltstone|39232|6|Mentioned|p107|||||||||
27336|Berry Siltstone|39287|6|Mentioned|p20|||See also Fig.2.2||||||
27336|Berry Siltstone|39289|5|Briefly described|p78|||||||||
27336|Berry Siltstone|39290|6|Mentioned|Fig. 5.8|||Isopach map||||||
27336|Berry Siltstone|39293|4|Described|p137|||||||||
27336|Berry Siltstone|39299|6|Mentioned|Photo 14.7|||||||||
27336|Berry Siltstone|39305|5|Briefly described|p379|||Fossils occurrences||||||
27336|Berry Siltstone|39307|6|Mentioned|Table 22.1|||||||||
27336|Berry Siltstone|39308|6|Mentioned|p501|||||||||
27336|Berry Siltstone|39309|4|Described|p117|||See also Table 7.1||||||
27336|Berry Siltstone|40166|6|Mentioned|p348|||||||||
27336|Berry Siltstone|40256|6|Mentioned|p301|||||||||
27336|Berry Siltstone|40519|6|Mentioned|Fig.3|||||||||
27336|Berry Siltstone|40591|6|Mentioned|p323|||||||||
27336|Berry Siltstone|40806|6|Mentioned|p148|||||||||
27336|Berry Siltstone|40872|6|Mentioned|p37|||||||||
27336|Berry Siltstone|41580|5|Briefly described|p7|||||||||
27336|Berry Siltstone|41832|5|Briefly described|p569|||||||||
27336|Berry Siltstone|42310|5|Briefly described|p209|||||||||
27336|Berry Siltstone|42379|5|Briefly described|p209|||||||||
27336|Berry Siltstone|42758|6|Mentioned|p11|||||||||
27336|Berry Siltstone|42896|5|Briefly described|Table 2|||Of Shoalhaven Group.||||||12-MAR-09
27336|Berry Siltstone|42925|5|Briefly described|Table 18||Late Permian|||||||
27336|Berry Siltstone|42974|5|Briefly described|p193|||Of Shoalhaven Group.||||||12-MAR-09
27336|Berry Siltstone|43188|6|Mentioned|p221|||||||||
27336|Berry Siltstone|43194|5|Briefly described|p105, p128, p129 Tb. 8.3|Middle Permian|Middle Permian|Of Shoalhaven Group, Western and Southern Coalfields, Sydney Basin. Lower part correlates with Watermark Formation, Gunnedah Basin.||||||
27336|Berry Siltstone|43641|5|Briefly described|Map Legend||Permian|||||||
27336|Berry Siltstone|43782|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Shoalhaven Group.||||||12-MAR-09
27336|Berry Siltstone|44093|5|Briefly described|p64 Photo 1|Permian|Permian|Overlies Snapper Point Formation. Shelfal sandy siltstone. Geological Province: Sydney Basin.||||||
27336|Berry Siltstone|45006|14|Not recorded|p45|||||||||
27336|Berry Siltstone|60281|4|Described|p60|Late Permian|Late Permian|Of the Maitland Group. Equivalent to the southern onshore Sydney Basin Mulbring Formation. Overlain by the Broughton Sandstone and Pheasants Nest Formation.   Age: 265-264Ma.   Max. thickness: 550m.  Geological Province: Sydney Basin.  See also p58.||||||
27336|Berry Siltstone|60285|4|Described|p182 Fig.2|Kungurian|Artinskian|Of the Shoalhaven Group. Overlies Nowra Sandstone. Overlain by Broughton Formation. Offshore marine. Geological Province: Sydney Basin.||||||
27336|Berry Siltstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Shoalhaven Group. Geological Province: Sydney Basin||||||
27336|Berry Siltstone|61609|5|Briefly described|p239, p240 Tb. 1, p241, p244, p247|Late Permian|Late Permian|Of Shoalhaven Group. Underlain by Nowra Sandstone. Geological Province: Sydney Basin.||||||07-FEB-11
27336|Berry Siltstone|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||12-MAR-09
27336|Berry Siltstone|62043|6|Mentioned|p438 Fig.2. |Late Permian|Late Permian|Southern Sydney Basin.||Unit in Shoalhaven Group.||Overlies Nowra Sandstone. Is overlain by Broughton Formation.||
27336|Berry Siltstone|63773|5|Briefly described|p1058 Fig. 2, p1059, p1069|Middle Permian|Middle Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||07-APR-09
27336|Berry Siltstone|63832|5|Briefly described|p131 fig 2, p136|Guadalupian|Guadalupian|Of Sydney Basin. Seventh (P3) glaciation. Volcanic-dominated sediment provenance at the base. Also a major flooding surface.||Unit in Shoalhaven Group.||||13-DEC-17
27336|Berry Siltstone|64631|5|Briefly described|p44 Fig.2, p48 Fig.4.|Roadian|Roadian|NW, SW & SE Sydney Basin. Biostratigraphic age control at base and top.||Unit in upper Shoalhaven Group.||Overlies Nowra Sandstone. Is overlain by Broughton Formation.||
27336|Berry Siltstone|64877|5|Briefly described|p296|Permian|Permian|Southern Sydney Basin.||Shoalhaven Group.||||
27336|Berry Siltstone|66300|6|Mentioned|p64.|Permian|Permian|||Unit in Shoalhaven Group.||Unconformably overlies Tullyangela Granite.||
27336|Berry Siltstone|66577|6|Mentioned|p995, p997 Fig.2.|Permian|Permian|Indicative of a flooding event caused by sudden deepening of the Sydney Basin in response to an initial pulse of foreland loading (Fielding et al., 2001).||Unit in Shoalhaven Group.||Overlies Nowra Sandstone. Is overlain by Gerringong Volcanics.||
27336|Berry Siltstone|67663|6|Mentioned|p518|Permian|Permian|||Of the Shoalhaven Group.||||
27336|Berry Siltstone|68003|5|Briefly described|p38 Fig.3-j.|Late Permian|Late Permian|Western Coalfield, Brigalow Belt South Bioregion.||Unit in Shoalhaven Group.||Overlies Nowra Sandstone. Is overlain by Budgong Sandstone and Nile Subgroup.|Fine-grained offshore sediments.|
27336|Berry Siltstone|68592|6|Mentioned|p1779|Permian|Permian|||Unit in Shoalhaven Group.||Overlies Nowra Sandstone. Is overlain by Broughton Formation.||
27336|Berry Siltstone|69297|6|Mentioned|p501, p502 fig 5.43|Capitanian|Capitanian|Sydney Basin. Mistakenly referred to as the Berry Formation on p502 fig 5.43. ||Shoalhaven Group||Overlies the Nowra Sandstone. Overlain by the Broughton Formation and the Budgong Sandstone.||
27336|Berry Siltstone|70661|3|Fully described|ix, p6, p132, p137|Middle Permian|Middle Permian|Named for the town of Berry. Previously named Nowra-Berry Shales, Berry Shale and Berry Formation before being named the Berry Siltstone. Potentially a hydrocarbon source and seal. Incorrectly referred to as the Berry Formation (p176). Distribution, distinguishing characteristics, geomorphology, geophysical characteristics, fossil assemblage, structure and depositional environment discussed. Lithology discussed in great detail.  Estimated to be from 143m to 224m thick. Deposited in marine nearshore environment on the basis of fossil evidence. Age derived from unit relationships, fossil evidence and dating of correlative unit. Conformably overlain by Illawarra Coal Measures, Broughton Formation, disconformably overlain by Hawkesbury Sandstone, Equivalent to Mulbring Siltstone. See also  p139, p154, p167, p177-p182.|ca 264 Ma|Shoalhaven Group||Disconformably overlies Snapper Point Formation, Conformably (transitionally) overlies Nowra Sandstone,  Unconformably overlies Adaminaby Group, Bangadilly Granite.|Interbedded sandy siltstone and lithic quartzose, commonly silty, very fine and fine grained sandstone and medium grained sandstone (sublitharenites or litharenites).  The unit is commonly micaceous, bioturbated with rare conglomerate.|
27336|Berry Siltstone|71303|5|Briefly described|map legend|Guadalupian|Guadalupian|Of Sydney Basin.||Of Shoalhaven Group.|||Light to dark grey lithic-quartz sandy siltstone, very fine and fine-grained (commonly silty) and medium-grained sandstone, rare siltstone and conglomerate. Micaceous. Bioturbation and scattered clasts common.|
27336|Berry Siltstone|73304|6|Mentioned|p78|||||||||
27336|Berry Siltstone|73421|4|Described|p1, p2 Fig.1, p3, p5, p16-20|Wordian|Wordian|Sydney Basin, southern. Early Wordian. Fine-grained offshore facies deposited following transgression. May be laterally equivalent to and coeval with uppermost parts of Wandrawandian Siltstone. Previously correlated with Mulbring Siltstone of earliest Capitanian age based on sedimentary facies and marine faunas.||Shoalhaven Group||Overlies Nowra Sandstone, Wandrawandian Siltstone, conformably underlies Broughton Formation|Fine-grained offshore facies of siltstone and sandstone, variably fossiliferous.|
27336|Berry Siltstone|73625|6|Mentioned|p2|Permian|Permian|Western and Southern coalfields, Sydney Basin.||||Is overlain by Nile Sub-group (Illawarra Coal Measures) in the west, or Broughton Formation in the south.||
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)|||||
28365|Bethungra Formation|22638|1|Redefined|p65||Early Devonian|Thought equivalent to the Stockinbingal Formation. 7500 m wide; thickness given as ?500 - 1000 m. Possibly faulted against the Frampton Volcanics, but recorded as a disconformity.||||||13-NOV-13
28365|Bethungra Formation|22685|5|Briefly described|p728,Fig1p729||Early Devonian|Dacite, rhyolite, siltstone and sandstone.||||||17-JAN-06
28365|Bethungra Formation|22857|4|Described|p450 App.1, Tb.A1.6|Early Devonian|Early Devonian|Dacitic to rhyolitic tuffs. Max. thickness: 1000m. Geological Province: Bogan Gate Terrace.||||||
28365|Bethungra Formation|35608|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
28365|Bethungra Formation|35609|2|Defined|p77|Early Devonian|Early Devonian|||||||
28365|Bethungra Formation|39626|6|Mentioned|p275|||||||||
28365|Bethungra Formation|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
28365|Bethungra Formation|44192|5|Briefly described|Map Legend||Lochkovian|||||||
37908|Bexley Rhyolite Member|24605|3|Fully described|p931, pp940, 941, p944 Fig.9|Namurian|Visean|Of the Clifden Formation. Age: 327.2 +/- 2.9 Ma (U-Pb). Geological Province: New England Orogen. Defined as Bexley Rhyolite.||||||23-SEP-18
37908|Bexley Rhyolite Member|61214|5|Briefly described|p171 Fig. 1|Namurian|Namurian|Of the Clifden Formation. Geological Province: Kathrose Block. See also p172 Fig. 2. Presented only as Bexley in text of figure. ||||||
37908|Bexley Rhyolite Member|65382|5|Briefly described|p714|Namurian|Visean|Age of 323.2 +/- 3.2 Ma SHRIMP,  [which corresponds to Serpukhovian on current international timescale], however stated age is 'at the Visean/Namurian boundary'. Eastern Australia.||||||23-SEP-18
79325|Bibblewindi Coal Member|70791|5|Briefly described|p275-276, p281, p283, p285-288, p292-294|Cisuralian|Cisuralian|New name. Mullaley Sub-basin. 0-10m thick. Is developed in three localised occurrences in the Bohena and Bando Troughs. Has similarities with Glenara Coal Member (Werris Creek) and Lewis/Loder Coal Members (Muswellbrook). Borehole cross-sections and long-sections; correlations. Isopachs. Coal properties described. In situ coal estimates.|||||Dull coal with a conchoidal fracture, becoming brighter towards the top.|
28129|Biddabirra Formation|730|5|Briefly described|p24.|Devonian|Devonian|Middle, thick-bedded turbidite unit in Amphitheatre Group, between two thin-bedded units. Contains brachiopods (Howellella jaqueti). Probably thrust over Kopyje Group.||||||11-NOV-14
28129|Biddabirra Formation|22857|4|Described|p436 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Amphitheatre Group (Cobar Supergroup). Sandstone-rich unit, massive to medium-bedded, interbedded mudstone. Max. thickness: 4km. Geological Province: Cobar Basin.||||||
28129|Biddabirra Formation|23096|6|Mentioned|p601 (Fig 1)|||Misspelt Biddabirra Foration.||||||
28129|Biddabirra Formation|23101|5|Briefly described|p568|||||||||
28129|Biddabirra Formation|23171|5|Briefly described|p15,44,Fig15p45|||||||||
28129|Biddabirra Formation|23173|4|Described|Map Legend|Pragian|Lochkovian|||||||
28129|Biddabirra Formation|23734|5|Briefly described|p12 Fig. 1|||Parent: Amphitheatre Group.  Sandstone.||||||
28129|Biddabirra Formation|24019|4|Described|p353|Pragian|Lochkovian|Contains triolobite fauna (12 species).||||||
28129|Biddabirra Formation|38292|4|Described|p5|||||||||
28129|Biddabirra Formation|41138|6|Mentioned|Map legend|Pragian|Pragian|||||||
28129|Biddabirra Formation|41452|6|Mentioned|Fig.1|||||||||
28129|Biddabirra Formation|41528|6|Mentioned|p19|||See also P76||||||
28129|Biddabirra Formation|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
28129|Biddabirra Formation|41821|2|Defined|p38|Early Devonian||||||||
28129|Biddabirra Formation|41872|6|Mentioned|p8|||||||||
28129|Biddabirra Formation|42144|5|Briefly described|p605|||See also Fig.1 and2||||||
28129|Biddabirra Formation|42172|5|Briefly described|Fig.5 P167|||||||||
28129|Biddabirra Formation|42521|5|Briefly described|p15, Figs|||||||||
28129|Biddabirra Formation|42566|5|Briefly described|Fig.5 P11|||||||||
28129|Biddabirra Formation|42907|6|Mentioned|Fig.8, P8|||||||||
28129|Biddabirra Formation|42983|5|Briefly described|p343|||||||||
28129|Biddabirra Formation|43032|2|Defined|p83|Early Devonian||Of Amphitheatre Group.||||||08-APR-09
28129|Biddabirra Formation|43089|5|Briefly described|Map Legend|||Of Amphitheatre Group.||||||08-APR-09
28129|Biddabirra Formation|43153|5|Briefly described|Map Legend|Pragian|Pragian|Of Amphitheatre Group.||||||08-APR-09
28129|Biddabirra Formation|61905|5|Briefly described|p135 Fig. 1|||Geological Province: Cobar Basin.||||||
28129|Biddabirra Formation|64962|5|Briefly described|p202|||Deep-water turbidites.||||||11-NOV-14
28129|Biddabirra Formation|65469|5|Briefly described|p14, p15, p43, p52|Pragian|Lochkovian|Lachlan Orogen. See also p55 fig 3-19, p62, p67, p133, p136, p139, p330, p340, App A-VI 3.||Amphitheatre Group|Includes the Alley Sandstone Member.|Overlies the CSA Siltstone.||
28129|Biddabirra Formation|68823|6|Mentioned|p378 Fig.4|Pragian|Lochkovian|Cobar Basin; Lachlan Orogen.|||Includes Alley Sandstone Member.|Overlies CSA Siltstone.||
28129|Biddabirra Formation|69002|5|Briefly described|p11|Early Devonian|Early Devonian|||Of the Amphitheatre Group.|Includes the Alley Sandstone Member.|||
28129|Biddabirra Formation|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Early Devonian|Lachlan Orogen.||||||
28129|Biddabirra Formation|71039|6|Mentioned|p14|||Northwestern Amphitheatre Group.||Amphitheatre Group|Includes the Lerida Limestone Member.|||
28129|Biddabirra Formation|71285|5|Briefly described|p538, p552 Fig.9|Early Devonian|Late Silurian|Cobar region.||Amphitheatre Group.||||
28129|Biddabirra Formation|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|Geophysical signature: low magnetic intensity and only very slight contrast with adjacent sedimentary rocks in aeromagnetic data. Boundaries are based on existing geological mapping.||Amphitheatre Group.|||Medium to thickly bedded sandstone, siltstone and mudstone.|
28129|Biddabirra Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Amphitheatre Group.||Overlies CSA Siltstone.|Medium- to thick-bedded, massive to graded to parallel-laminated, moderately to poorly sorted, fine- to medium-grained, quartzose to lithic-quartz sandstone packets, interbedded with thin-bedded siltstone, mudstone and fine-grained sandstone.|
28129|Biddabirra Formation|72958|6|Mentioned|p5, p8, p61|Pragian||Cobar Basin, northwest. Contains olistolithic horizons that contain Pragian conodonts and are correlated with the Shume Formation.|||Includes Lerida Limestone Member.|||
28129|Biddabirra Formation|73143|6|Mentioned|p2|||||Amphitheatre Group||||
28129|Biddabirra Formation|73174|6|Mentioned|p1037, p1039|Pragian|Lochkovian|Cobar Basin. Contains age-diagnostic brachiopod and trilobite. [Written as Biddabirra Group on p1036; probably unintentional].||Amphitheatre Group, Cobar Supergroup|Alley Sandstone Member|Underlain by CSA Siltstone.||
28129|Biddabirra Formation|73264|5|Briefly described|p1394 Fig.16|Early Devonian|Silurian|Cobar Basin.|||Alley Sandstone Member||Includes quartz-rich sandstone.|
28129|Biddabirra Formation|73578|6|Mentioned|p2|||Cobar Basin. [Written as Biddabirra/Shume formation on p2].||||||
25783|Biddi Granodiorite|22815|4|Described|p48|Silurian|Silurian|||||||
25783|Biddi Granodiorite|33782|6|Mentioned|Fig.2|||||||||
25783|Biddi Granodiorite|40328|4|Described|p202|||||||||
25783|Biddi Granodiorite|41905|2|Defined|p83|Silurian||||||||
25783|Biddi Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
25783|Biddi Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Ingebyrah Suite.||||||
25783|Biddi Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb14.||||||
25783|Biddi Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
40754|Bideroie Ignimbrite Member|50613|2|Defined|p209, p227 App.1|Late Carboniferous|Late Carboniferous|Of the Willuri Formation.  Volcanic member of the Kaputar package (informal grouping of stratigraphically recognisable distinctive, mappable units).  Max.thickess of rhyodacitic ignimbrite: 35m; of dacitic ignimbrite:20m. Geol.Prov: New England Orogen.||||||22-FEB-05
29517|Big Box Hill Syenite|23214|3|Fully described|p93|Late Ordovician|Late Ordovician|Intrudes the Weemalla Formation.||||||
29517|Big Box Hill Syenite|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Syenite.||||||17-JUL-08
29517|Big Box Hill Syenite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29517|Big Box Hill Syenite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
82358|Big Hill Creek Granite|71628|5|Briefly described|p17: 2, 89-90|||New name (this study) for an unnamed granite, N of Mount Seaview, ~70 km NNW of Port Macquarie. Identified as Rgz in Gilligan et al. (1987); currently shown as Gundle Granite within the current GSNSW map. Unaffiliated. Named after a local watercourse. Is approximately 9 x 5 km.||Big Hill Creek Suite.||Intrudes Myra beds, Sandon beds, and Werrikimbe Volcanics.|Porphyry and leucomonzogranite.|
24181|Big Hole Formation|22815|6|Mentioned|p102|||||||||
24181|Big Hole Formation|22857|5|Briefly described|p216, p494 App. 1 Tb.A1.7|Frasnian|Frasnian|Of the Minuma Range Group. Together with the Curmulee Conglomerate separates the Long Swamp Creek and Deua Formations. Max. thickness: 114m. Locally overlies Gundillion Conglomerate. Geological Province: Lambie Shelf.||||||
24181|Big Hole Formation|22859|6|Mentioned|p216|||||||||
24181|Big Hole Formation|39028|6|Mentioned|Map legend|Famennian|Famennian|||||||
24181|Big Hole Formation|40276|2|Defined|p26|Late Devonian|Late Devonian|||||||
24181|Big Hole Formation|41796|6|Mentioned|p305|||||||||
24181|Big Hole Formation|42497|5|Briefly described|Map legend|Famennian|Frasnian|||||||
24181|Big Hole Formation|71700|5|Briefly described|CD|Late Devonian|Late Devonian|Ages derived from fossil assemblage.||Minuma Range Group||Conformably overlies the Gundillion Conglomerate.||
24181|Big Hole Formation|73181|6|Mentioned|p61, p65|Frasnian|Frasnian|Contains invertebrate and plant fossils. Possibly contains impressions of Leptoploeum [palaeoflora].||Minuma Range Group||Underlain by Gundillion Conglomerate. Overlain by Curmulee Conglomerate. Equivalent to Long Swamp Creek Formation.|Marine sandstones[?]|
29201|Big Jack Granite|22815|4|Described|p86|||||||||
29201|Big Jack Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
29201|Big Jack Granite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
34932|Big Sink beds|22952|5|Briefly described|p178,Table1p179||Early Pliocene|Consists of: Big Sink unit and conglomerate unit.||||||
28168|Bijerkerno Metasediments|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
28168|Bijerkerno Metasediments|22575|6|Mentioned|p179 Fig.2|||Of the Paragon Group, Broken Hill Block.||||||11-JUN-08
28168|Bijerkerno Metasediments|22771|5|Briefly described|Table12.2p45,47|||||||||
28168|Bijerkerno Metasediments|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb. A1.1|Paleoproterozoic|Paleoproterozoic|Supersedes the Bijerkerno Beds. Of the Paragon Group. Max. thickness: 700m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
28168|Bijerkerno Metasediments|22884|6|Mentioned|p47|||Geological province: Broken Hill Domain.||||||26-MAR-09
28168|Bijerkerno Metasediments|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Mt Isa Soldiers Cap Group and Georgetown (Qld) Etheridge Group upper sequence.||||||07-NOV-08
28168|Bijerkerno Metasediments|22965|6|Mentioned|p14,Fig1||Statherian|||||||
28168|Bijerkerno Metasediments|22967|6|Mentioned|p39||Statherian|||||||
28168|Bijerkerno Metasediments|23248|5|Briefly described|Fig2p169|||||||||
28168|Bijerkerno Metasediments|24307|5|Briefly described|p974|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|38969|4|Described|p211|||||||||
28168|Bijerkerno Metasediments|39662|2|Defined|p437|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28168|Bijerkerno Metasediments|40822|6|Mentioned|Fig.2|||||||||
28168|Bijerkerno Metasediments|41093|6|Mentioned|p252|||||||||
28168|Bijerkerno Metasediments|41630|6|Mentioned|Fig.1.3|||||||||
28168|Bijerkerno Metasediments|42261|6|Mentioned|Fig 1 P530|||||||||
28168|Bijerkerno Metasediments|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28168|Bijerkerno Metasediments|42537|4|Described|p16|||||||||
28168|Bijerkerno Metasediments|43052|6|Mentioned|Fig.4.22|||||||||
28168|Bijerkerno Metasediments|43086|6|Mentioned|Fig.3|||||||||
28168|Bijerkerno Metasediments|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|43572|6|Mentioned|Fig.3.2 p6|||||||||
28168|Bijerkerno Metasediments|46598|5|Briefly described|p305|||||||||
28168|Bijerkerno Metasediments|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Paragon Group (Willyama Supergroup). Overlain by Dalnit Bore Metasediments; underlain by Cartwrights Creek Metasediments.||||||31-MAY-07
28168|Bijerkerno Metasediments|50619|5|Briefly described|p178 Fig. 3||Paleoproterozoic|Of the Paragon Group (Willyama Supergroup).  Geological Province: Broken Hill Block.||||||07-NOV-08
28168|Bijerkerno Metasediments|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Marker unit.  Of the Paragon Group.  Age: <1655+/-4Ma.   Geological Province: Broken Hill Domain.||||||28-APR-05
28168|Bijerkerno Metasediments|61606|5|Briefly described|p4 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
28168|Bijerkerno Metasediments|61735|5|Briefly described|p635 Fig. 1, 639|||Lower part of unit sampled twice and tuffaceous sediment gives depositional ages: 1657+/-4 Ma, 1655+/-4 Ma U/Pb SHRIMP.||||||04-JUN-15
28168|Bijerkerno Metasediments|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Ages: 1655+/-4Ma and 1657+/-4Ma. Geological province: Broken Hill Domain. Includes cream coloured, albitic, fine-grained psammites.||||||
28168|Bijerkerno Metasediments|62473|5|Briefly described|p74|||Of the Paragon Group. Age: 1656+/-5Ma. Geological province: Broken Hill Domain. Contains tuffaceous siltstones.||||||17-JUN-09
28168|Bijerkerno Metasediments|62535|5|Briefly described|p666 Fig.3, p668, p671-672, p674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1657 +/- 4 Ma; 1655 +/- 4 Ma.|Paragon Group.||Correlated with Mooleulooloo Formation.|Includes cream-coloured, albitic, fine-grained psammites.|
28168|Bijerkerno Metasediments|62536|5|Briefly described|p633, 636, 639, 641, 651-653, 655, 657|||See also p659. Broken Hill area. Depositional ages for this unit in the northern Broken Hill Block and Euriowie Block respectively.|1655 +/- 4 Ma and 1657 +/- 4 Ma (MDA).|Paragon Group.|||Tuffaceous metasiltstones, derived partly from air-fall volcaniclastic material.|
28168|Bijerkerno Metasediments|62592|5|Briefly described|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.|<1655 +/- 4 Ma.|Unit in Paragon Group.||||
28168|Bijerkerno Metasediments|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1655 +/- 4 Ma|Paragon Group||Overlain by Dalnit Bore Metaseidments, Overlies Cartwrights Creek Metasediments, correlated with Mooleulooloo Formation||15-DEC-21
28168|Bijerkerno Metasediments|63102|5|Briefly described|p13-14,36, p38||Neoproterozoic|Geological province: Broken Hill Domain, Curnamona Province.  Has U-Pb zircon age of 1656+\-5 Ma (Page et al. 2000).|<1655+\-4 Ma|Unit of Paragon Group.||Equivalent to Mooleulooloo Formation.||22-OCT-19
28168|Bijerkerno Metasediments|63186|5|Briefly described|p67|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group (Willyama Supergroup). Geological Province: Broken Hill Domain, Curnamona Province.||||||07-NOV-08
28168|Bijerkerno Metasediments|63519|5|Briefly described|p6 Fig. 2, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Overlain by Dalnit Bore Metasediments gradationally; overlies Cartwrights Creek Metasediments. Age: <1656+/-5Ma, 1660-1650Ma. Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
28168|Bijerkerno Metasediments|63866|4|Described|p36, p38|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Age is interpreted as the maximum depostional age for this unit.|1657 +/- 4 Ma (Page et al., 2005a)|Paragon Group||Overlies the King Gunnia Calc-Silicate Member (Cartwrights Creek Metasediments). Overlain by the Dalnit Bore Metasediments.|Thin-bedded to laminated, cross-bedded, fine feldspathic and graphitic psammite.|
28168|Bijerkerno Metasediments|64097|5|Briefly described|p302 Tb. 1, p303|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Depositional age: 1657+/-4 , 1655+/-4Ma (Page et al 2005a).||||||07-FEB-11
28168|Bijerkerno Metasediments|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Age in lower section: <1655+/-4Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
28168|Bijerkerno Metasediments|64742|6|Mentioned|p321 Fig.3.||||<1655 Ma.|Unit in Paragon Group.|||Psammite, psammopelite, pelite.|
28168|Bijerkerno Metasediments|64944|5|Briefly described|p26, p28 Fig. 1, , p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Paragon Group. Interpreted to be equivalent to the Mooeulooloo Formation in the Olary Domain. Age: <1655+/-4Ma. Geological province: Broken Hill Domain. Dating also indicates a temporal similarity with Mount Isa Group (Qld.)||||||07-FEB-11
28168|Bijerkerno Metasediments|66302|4|Described|p36 Fig.9, p38, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. |1655 +/- 4 Ma (Page et al, 2000 and Conor, 2006)|Paragon Group||Overlies the Cartwrights Creek Metasediments. Overlain by the Dalnit Bore Metasediments.|Thin-bedded to laminated, cross-bedded, fine-grained feldspathic graphitic sandstone.|
28168|Bijerkerno Metasediments|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1655 +/- 4 Ma (maximum depositional age).|Paragon Group.||||
28168|Bijerkerno Metasediments|70000|5|Briefly described|p34, p37|Statherian|Statherian|||Unit in Paragon Group.||Conformably (gradationally) overlies Cartwrights Creek Metasediments.|Albitic, rippled and cross-laminated psammitic and interbedded phyllitic rocks.|
28168|Bijerkerno Metasediments|70014|5|Briefly described|Map legend|||Psammites are white to pale yellow, very fine-grained and finely laminated, with sporadic small-scale high to low angle crossbeds, flame structures, load casts, and rare graded beds. Rarely dark grey to black and lenticular.||Unit in Paragon Group.||Overlies Cartwrights Creek Metasediments. Is overlain by Dalnit Bore Metasediments.|Variably graphitic metasediments with regular, alternating psammite-rich and phyllitic intervals, 5-300m thick. Intervening phyllites are graphitic, finely laminated, spotted or non-spotted.|
28168|Bijerkerno Metasediments|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Paragon Group.||Overlies Cartwrights Creek Metasediments.|Graphitic metapsammite and metaphyllite; the former finely laminated, with sporadic, small-scale to low-angle crossbeds, flame structures and load casts.|
28168|Bijerkerno Metasediments|70405|6|Mentioned|p9 table 1, p32, p43 Table 3|||||||Correlates with Mooleulooloo Formation||
28168|Bijerkerno Metasediments|70657|5|Briefly described|p13 Fig.6, p14-15, p43, p45|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|1656 +/- 5 Ma (Page et al., 2000).|Paragon Group||Overlies Cartwrights Creek Metasediments. Underlies Dalnit Bore Metasediments. Equivalent to Mooleuloloo Formation (Olary Domain).||
28168|Bijerkerno Metasediments|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|<1655 +/- 4 Ma.|Paragon Group.||||
28168|Bijerkerno Metasediments|71968|4|Described|p18,28,45|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Page et al., (2005a) reported maximum depositional ages of 1655+\-4 Ma and 1657+\-4 Ma at Broken Hill.||Unit of Paragon Group.||Overlain by Dalnit Bore Metasediments. Underlain by Cartwrights Creek Metasediments.|Thin-bedded to laminated, cross-bedded, fine feldspathic graphitic psammite.|
28168|Bijerkerno Metasediments|72461|5|Briefly described|p6, p13, p16|||Additional ages include 1655 +/- 4 Ma and 1657 +/- 4 Ma.|1656 +/- 5 Ma|Paragon Group||Overlies the Cartwrights Creek Metasediments. Overlain by the Dalnit Bore Metasediments.||
28168|Bijerkerno Metasediments|73482|5|Briefly described|p422 Fig.3, p429 Fig.8|Statherian|Statherian||1655+/-4 Ma, 1657+/-4 Ma|Paragon Group||||
28168|Bijerkerno Metasediments|73575|5|Briefly described|p828 Fig.2|Statherian|Statherian||<1655+/-4 Ma, 1657+/-4 Ma|Paragon Group||Overlies Cartwrights Creek Metasediments, underlies Dalnit Bore Metasediments||
38194|Billabong Creek Formation|23736|3|Fully described|p12|Eastonian|Darriwilian|Formerly Billabong Creek Limestone.  Of the Northparkes Group.  Maximum thickness: 320m.||||||30-JUN-08
80456|Billabong Creek granodiorite|70718|5|Briefly described|p61-p63|||Informal name, interpreted from geophysics. Also intrudes the Bendigo Zone of the Murray Basin. Likely to be I-type based on magnetic signature.||Jawbone Creek granodiorite suite||||03-APR-18
24721|Billy Brook Formation|22610|5|Briefly described|p127, 129||Early Permian|Age 287.9 +/- 3Ma, Stevenson pers. comm., 1997.||||||19-SEP-18
24721|Billy Brook Formation|22857|5|Briefly described|p536 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Sandstone, siltstone, claystone, conglomerate. Max. thickness: 100m. Should not be confused with Billy Creek Formation (Lake Frome Group).||||||
24721|Billy Brook Formation|23350|5|Briefly described|262|||||||||
24721|Billy Brook Formation|23540|4|Described|p 419|||r||||||20-FEB-07
24721|Billy Brook Formation|39288|6|Mentioned|p57|||See also Fig.3.3||||||
24721|Billy Brook Formation|46849|6|Mentioned|p195|||||||||
24721|Billy Brook Formation|60289|5|Briefly described|p2 Fig. 2|Early Permian|Early Permian|Of Dalwood Group. Overlies Cranky Corner Sandstone. Underlies Greta Coal Measures. Geological Province: Cranky Corner Basin.||||||
24721|Billy Brook Formation|60290|3|Fully described|p15, 26, 37, 43|Early Permian|Early Permian|Of Dalwood Gp. Thickness: 45 m. Overlies Cranky Corner Sst. Unconformably overlain by Greta Coal Measures. Age: c.285 Ma. Bioturbated prodelta + shelf sandstone + siltstone. Basal conglomerate. Geol Prov: Cranky Corner Basin.||||||07-FEB-11
24721|Billy Brook Formation|60291|4|Described|p51, 53 Tb.1|Early Permain|Early Permain|Of Dalwood Group. Overlain by Greta Coal Measures. Sandstone and siltstone, shelly paraconglomerate at base. Prodelta and shelf environments. Geological Province: Cranky Corner Basin. Petrology descirbed.||||||
24721|Billy Brook Formation|60292|4|Described|p65|Early Permian|Early Permian|Uppermost unit of Dalwood Group. Overlies Cranky Corner Sandstone. Overlain by Greta Coal Measures. Geological Province: Cranky Corner Basin. Petrography and geochemistry described.||||||
24721|Billy Brook Formation|60293|5|Briefly described|p108 Fig.1|||Overlies Cranky Corner Sandstone. Overlain by Greta Coal Measures. Vitrinite reflectance of organic matter described.||||||
24721|Billy Brook Formation|60294|5|Briefly described|p115, 116 Fig.1|Early Permian|Early Permian|Uppermost unit of Dalwood Group. Overlies Cranky Corner Sandstone. Overlain by Greta Coal Measures. Contains hydrocarbon source rock potential. Lower delta plain deposition. Geological Province: Cranky Corner Basin.||||||
24721|Billy Brook Formation|60295|4|Described|p127, p133 Fig.9|Artinskian|Artinskian|Of Dalwood Group. Overlies Cranky Corner Sandstone. Overlain by Greta Coal Measures. Plant microfossils indicate a shallow, oxygenated brackish water environment. Age: 285 Ma. Geological Province: Cranky Corner Basin.||||||
24721|Billy Brook Formation|60296|5|Briefly described|p155, p156 Fig.1|Sakmarian|Sakmarian|Of the Dalwood Group. Correlated with Rutherford Formation, upper Pebbley Beach Formation, Faulkner Group and Liffey Group. Geological Province: Cranky Corner Basin.||||||18-MAY-05
24721|Billy Brook Formation|60297|5|Briefly described|p167|Permian|Permian|Of the Dalwood Group. Overlain by the Greta Coal Measures. Geological Province: Cranky Corner Basin.||||||
24721|Billy Brook Formation|60298|5|Briefly described|p179, 181, 188, 190|Artinskian|Sakmarian|Bioturbated conglomerate, sandstone and siltstone. Age: ca. 285 Ma (SHRIMP zircon U-Pb). Geological Province: Cranky Corner Basin. Tuffaceous sample ?low in Formation and volcaniclastic sample high in formation dated (285.8+/-3 Ma max. depositional age).|285.4+/-2.2 Ma U/Pb SHRIMP crystallisation|||||19-SEP-18
24721|Billy Brook Formation|60299|5|Briefly described|p218|||Palaeomagnetism measured||||||
24721|Billy Brook Formation|60300|5|Briefly described|p246 Fig.2|Early Permian|Early Permian|Of the Dalwood Group. Overlies Cranky Corner Sandstone. Overlain by Greta Coal Measures.||||||
24721|Billy Brook Formation|63832|5|Briefly described|p131 fig 2|Artinskian|Artinskian|Cranky Corner/Gresford block, Southern New England Fold Belt. Sixth (P2) glaciation.||Unit in Dalwood Group.||||13-DEC-17
24721|Billy Brook Formation|64631|5|Briefly described|p44 Fig.2.|Artinskian|Artinskian|Southern New England Fold Belt, Cranky Corner/Gresford Block. Biostratigraphic age control near base.||Unit in Dalwood Group.||Overlies Cranky Corner Sandstone. Is overlain by Greta Coal Measures.||
24721|Billy Brook Formation|68493|6|Mentioned|p10 Fig.4|Artinskian|Artinskian|||||Correlative of Rutherford Formation of Sydney Basin.||
24721|Billy Brook Formation|69793|6|Mentioned|p1121 Fig.12|Artinskian|Sakmarian|Gresford Block, Tamworth Belt.||||||
24721|Billy Brook Formation|70096|6|Mentioned|Supp2|||Includes angular volcanic orthoconglomerate clasts interpreted to be locally derived, rather than glacial transport.||||||
82359|Billygoat Hill Complex|71628|4|Described|p13: 1, 7, 23-28|||New name (this study) to reflect the internal complexity of the unit. Originally Billygoat Hill Monzonite (Binns et al., 1967) after work by Ransley (1964). Located ~25 km ENE of Armidale. Comprises two main bodies, the larger composed of several even smaller stocks. Geochemistry described; petrology detailed.|250 +/- 5 Ma and 257 +/- 6 Ma (Kent, 1994).|Highlands Suite.||Intrudes the Girrakool beds and Rockvale Monzogranite.|Comprises early stocks of porphyritic, fine biotite-hornblende-cpx-(opx) quartz monzonite to monzogranite, with later more felsic, weakly porphyritic to inequigranular biotite-hornblende-(cpx) quartz monzonite to monzogranite. I-type.|
79193|Billyrambija Dolerite Member|68592|4|Described|p847, p1804-6, p1811-3|Paleogene|Paleogene|O'Reilly (1972), after Billyrambija Trigonometrical Station. Type locality specified. At least 100m thick. Has a strong magnetic response. See also references to the shortened name Billyrambija Dolerite, which appears to be the authors' preferred form (p847, p1762, p1766). Not dated; age inferred from field relations and composition.||Unit in Crookwell Basalt.||Intrudes Longreach Volcanics. Disconformably overlies Lockyersleigh Granite.|Black, massive, porphyritic coarse-grained dolerite sill.|
79193|Billyrambija Dolerite Member|71069|6|Mentioned|p135|Cenozoic|Cenozoic|||||||
38268|Billyrimba Leucomonzogranite|23811|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Medium- to coarse-grained, equigranular, buff biotite leucomonzogranite.   An I-type granitoid.||||||20-DEC-04
38268|Billyrimba Leucomonzogranite|23812|5|Briefly described|p19 Tb.2|Triassic|Triassic|Age: 235-233Ma (whole rock Rb-Sr).||||||
38268|Billyrimba Leucomonzogranite|68111|5|Briefly described|p969 Tb.1|Carnian|Carnian||235 - 233 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38268|Billyrimba Leucomonzogranite|69639|4|Described|p2, p5, p8, p26-p30|Ladinian|Ladinian|New England Orogen. Sampling locality, petrography and geochronology are discussed. Contacts the Dundee Rhyodacite, Wallangara Volcanics (of the Wandsworth Volcanic Group), Cottesbrook Monzogranite and Bungulla Monzogranite; however, the nature of these contacts is not clear due to poor outcrop. See also p62-p68, p219, p221, p240.|241.4 +/- 1.2 Ma (SHRIMP U-Pb)|Bolivia Range Suite||Intrudes the Coffs Harbour Association. Intruded by (inferred) the Cottesbrook Monzogranite.|Medium- to coarse-grained, massive and inequigranular leucocratic biotite granite.|
38268|Billyrimba Leucomonzogranite|70217|5|Briefly described|p74 tbl 14.1|Anisian|Anisian|New England Orogen.|241.4 +/- 1.2 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
38268|Billyrimba Leucomonzogranite|71628|3|Fully described|p8:80; p11: 10-11; p15: 1-2, 4-8; p17:5|||Henley et al. (2001) after unpublished work by Barnes (1987). Named after Billyrimba Falls. An irregular, c.12 x 8 km E-W intrusion 10 km E of Sandy Flat locality. Type locality (Shaw, 1964) is just under half a kilometre E of Scrub Road, 19 km SE of Tenterfield. Associated with a 500m-high plateau with deeply incised NW-striking joint planes. Geochemistry described. Is associated with only minor Mo, Bi, W (Ag, Au) mineralisation.|241.4 +/- 1.2 Ma (SHRIMP: Chisholm et al., 2014).|Bolivia Range Suite.||Intrudes Coffs Harbour Association, various units (some named) of Wandsworth Volcanic Group, Cottesbrook and ?Bungulla Monzogranites. Is intruded by Dandahra Creek Leucosyenogranite.|Buff, medium-grained, inequigranular, biotite K-feldspar-rich leucomonzogranite. Contains miarolitic cavities. I-type.|
82361|Billys Creek Granodiorite|71628|4|Described|p2: 45, 48; p17: 1-2, 47-52, 94|||See also p19: 164-165. Formerly (Jones, 1976) part of the Sheep Station Creek Complex; later Billys Creek Tonalite. Renamed in this study to reflect the average composition of the unit. Named after a local watercourse. A small (7 km2), elongate intrusion 25 km NW of Dorrigo. Crops out as boulders with a thin weathered skin. Distinctive geochemistry described. Included in the Coastal Granite Association. Associated with disseminated and vein Mo-Cu mineralisation (prospects named and briefly described).|231.8 Ma (U-Pb; LA-ICP-MS: Blevin pers. comm).|Billys Creek Suite.||Intrudes Brooklana beds.|Fine- to medium-grained, commonly porphyritic, hornblende-biotite tonalite, granodiorite and monzogranite. I-type. Lithology and mineralogy described thoroughly.|
82360|Billys Creek Suite|71628|5|Briefly described|p17: 2, 47-53|||Dundurrabin area. A distinct grouping of moderately reduced to moderately oxidised, moderately to strongly evolved, medium- to high-K, calc-alkaline, I-type granites.|||Billys Creek, Tyringham East, Granodiorites.|||
27107|Billys Lookout Granite|24417|4|Described|p57|Silurian|Silurian|Intrudes the Girilambone Group.  Age: 427+/-2.2Ma (SHRIMP U-Pb).||||||
27107|Billys Lookout Granite|29907|2|Defined|Appendix 1|Early Devonian|Early Devonian|Prob.Early Devonian||||||
27107|Billys Lookout Granite|29910|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27107|Billys Lookout Granite|36411|6|Mentioned|p267|||Refers Bowman 1977 for definition.||||||
27107|Billys Lookout Granite|40328|4|Described|p202|||||||||
41598|Bilpa Conglomerate|50618|5|Briefly described|p249 Fig. 2|Late Cambrian|Late Cambrian|Of the Mootwingee Group.||||||
41598|Bilpa Conglomerate|66623|2|Defined|p122, pp135-140. |Late Cambrian|Late Cambrian|Formerly part of Torrowangee Series (Mawson 1912), Mootwingee Series (Andrews 1922), Scopes Range beds (Rose and Brunker 1968). Informally named Bilpa conglomerate by Pahl and Sikorska (2004). Defined in this study. Contains a wide range of clasts derived from the Delamerian mountains; prominent imbrication textures suggest transport towards the north. Correlates with Williams Creek Conglomerate to the east.||Unit in Mutawintji Group.||Unconformably overlies Ponto Group. Is overlain by Nuchea Conglomerate.|Basal clast-supported oligomict conglomerate, angular clasts in ferruginous cement; polymict conglomerate with increasing variety of clasts, particularly basic volcanics; matrix-supported polymict facies with greatest variety of rock types.|
41598|Bilpa Conglomerate|67105|6|Mentioned|p659|||SW and S Koonenberry Belt. 600m thick. Derived from locally-sourced pre-Delamerian Orogeny units such as Teltawongee and Ponto Groups.||Basal Mutawintji Group.|||Fluvial deposits.|
41598|Bilpa Conglomerate|67322|4|Described|p12, p20 Fig.5|Late Cambrian|Late Cambrian|First noted by Packham (1968) and Webby (1983); informally named by Pahl and Sikorska (2004) and formally described by Greenfield and Percival (in Greenfield et al. (2010). Rare mudstone pebbles contain early Cambrian trilobite, possibly eroded from Cymbric Vale Formation. Maximum age is determined from p20 Fig.5 (Strat. column). Occurs in the Bilpa-Comarto, Scropes Range region.||Basal unit of the Mutawintji Group.||Locally overlies Teltawongee and Ponto Groups. Conformably overlain by the Nuchea Conglomerate.|Very poorly sorted, pebble to boulder polymictic conglomerate with rounded to angular clasts and carbonate-rich cement.|21-FEB-18
41598|Bilpa Conglomerate|70838|4|Described|p269 Fig.3, p270-272, p275, p277-278|Late Cambrian|Late Cambrian|Koonenberry Belt. Contains clasts of the Teltawongee and Ponto Groups, implying local derivation. Deposition had ceased by the Datsonian (488-485 Ma): fossils of that age occur in the overlying unit. Detrital zircon analyses. Provenance discussed.|>488 Ma.|Basal Mutawintji Group.||Is overlain by Nootumbulla Sandstone.|Polymict conglomerate: dominantly metamorphic and mafic lithic fragments as well as coarse, angular clasts of quartz and alkali feldspar.|
41598|Bilpa Conglomerate|73059|5|Briefly described|p1060-1062|||Koonenberry Belt, northwest NSW. Part of a coarse-grained delta deposit formed in continental and shallow-marine environments. Detrital zircon age plots and discussion.||Mutawintji Group.|||Poorly sorted; clasts up to 1m across. Dominantly metasandstone, metapelite and mafic volcanic rocks.|
41598|Bilpa Conglomerate|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
26254|Bimberi Leucogranite|36443|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Gingera Batholith. Intrusive. Leucogranite, leucoadamellite, aplite. S-type. BMR map code: Sgb.||||||
26254|Bimberi Leucogranite|39660|6|Mentioned|p449|||||||||
26254|Bimberi Leucogranite|44092|5|Briefly described|map legend|Silurian|Silurian|glw3||||||
26254|Bimberi Leucogranite|45147|2|Defined|M222|Late Silurian|Late Silurian|Probably Late Silurian.||||||20-MAY-08
26254|Bimberi Leucogranite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
38303|Bindaboo seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
70455|Bindawalla Ignimbrite Member|62095|2|Defined|p274 Appdx.|Late Carboniferous|Late Carboniferous|Of Currabubula Fm. Red to green unwelded ignimbrite. Overlies White Rocks Ignimbrite Member in Castle Mt. Dome area. Thickness: 3m. Age: 315.3Ma. Geological Province: Werrie block/Tamworth Belt..||||||31-JAN-08
39363|Bindo Creek Formation|24123|5|Briefly described|p3|Devonian|Silurian|Geological Province: Sydney Basin [??this unit is much too old to be Sydney Basin].||||||26-NOV-10
28368|Bindogandri Granite|24125|5|Briefly described|p93|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
28368|Bindogandri Granite|24417|3|Fully described|p108|Middle Devonian|Early Devonian|Previously referred to as "Bumberry Granite".  Named after Bindogandri Creek, in 1979 the spelling of  the geographical location was changed to Bindogundra, however the stratigraphic name retains the old spelling.||||||
28368|Bindogandri Granite|29907|2|Defined|Appendix 1|Early Devonian|Early Devonian|||||||
28368|Bindogandri Granite|29910|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
28368|Bindogandri Granite|36411|6|Mentioned|p267|||Refers Bowman 1977 for definition.||||||
28368|Bindogandri Granite|40328|4|Described|p202|||||||||
28368|Bindogandri Granite|40882|6|Mentioned|Fig.1|||||||||
28368|Bindogandri Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
28368|Bindogandri Granite|60009|5|Briefly described|Map Legend|Eifelian|Eifelian|||||||13-JUL-04
31552|Bindogandri Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31552|Bindogandri Suite|67847|5|Briefly described|p60 fig 3.3.4|Middle Devonian|Middle Devonian|A-type intrusive rocks. ||||||
69879|Bindook Group|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes Bullamalita Conglomerate, Windellama Limestone, Tangerang Formation, Quialigo Volcanics, Murruin Formation , and Joaramin and Barrallier Ignimbrites.||||||16-JUN-08
69879|Bindook Group|66087|6|Mentioned|p5, p3 Fig 2|Early Devonian|Early Devonian|Of the Bishopthorpe Suite?||||Overlies the Mount Fairy Group.||10-MAY-12
69879|Bindook Group|66300|5|Briefly described|p41, p76, p81.|Early Devonian|Early Devonian|Felsic volcanic rocks.|||Includes Long Flat Volcanics, Barrallier Ignimbrite, Quialigo Volcanics and Tangerang Formation.|Intruded by Arthursleigh Suite plutons.||24-OCT-13
69879|Bindook Group|68592|1|Redefined|xxiii, p74 Tb.5, p226, p271, p1060-1192|Lochkovian|Lochkovian|See also p726, p740-5, p840, p851, p852 Fig.143, p858, p873-4, p878, p882-3, p889-90, p893, p900. Redefined. Originally Bindook Porphyry (McElroy and Relph, 1961), after Bindook Highlands. Now also includes Quialigo Volcanics (ages 411+/-3 Ma, 409+/-4 Ma SHRIMP, Wilde, 2002) and other units. Massive subaerial pyroclastic volcanism. Long Flat Volcanics and 'Bombay Volcanics' were included by Felton and Huleatt (1977) and Wyborn and Owen (1986) in Mount Fairy Group in Braidwood and Araluen 1:100 000 map sheet areas. However, recent mapping (Fitzherbert et al. 2011) and age dating (Bodorkos and Simpson 2008) has combined Long Flat Volcanics and 'Bombay Volcanics' and placed them in Bindook Group. Western belt over 2.7 km thick; eastern belt over 3.5 km. Several representative stratigraphic columns presented and discussed. Geochemistry detailed: comagmatic with Arthursleigh Suite. Sparse fauna constrain max age to Lochkovian, only found in the eastern belt. Discussion of overlapping upper age contraints from volcanics (Barralier Ignimbrite) and intrusive units (Springponds Tonalite, Marulan Granite). Age-equivalent with Crudine Group. Significant quarrying for aggregate, and small quantities of refractory silica, construction materials, limestone and dolomite, have occurred. Goulburn and Bungonia structural zones: deformation described. Is faulted against Mares Forest Volcanics and Adaminaby Group.|414.4+/-2.9 Ma SHRIMP min age.||Barrallier and Joaramin Ignimbrites, Bullamalita Conglomerate, Quialigo Volcanics, Murruin and Tangerang Formations.|Unconformably overlies Mount Fairy Group. Is overlain unconformably by Lambie and Shoalhaven Groups. Is intruded by Arthursleigh Suite and Lockyersleigh Granite etc. Equivalent to Black Range Group.|Dominated by several regionally extensive felsic ignimbrite sheets; intermediate to felsic lavas, and volcanic and quartzose sedimentary rocks, are also significant. Basal boulder conglomerate is time transgressive, younging considerably northwards.|10-SEP-18
69879|Bindook Group|69159|5|Briefly described|Map legend|Devonian|Devonian||||Includes Tangerang Formation, Quialigo Volcanics, Long Flat Volcanics, Jinglemoney Conglomerate and Larbert Conglomerate.|||
69879|Bindook Group|70192|5|Briefly described|Map Legend|Pragian|Lochkovian|On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Barrallier Ignimbrite, Joaramin Ignimbrite, Murruin Formation, Quialigo Volcanics, Tangerang Formation, Bullamalita Conglomerate.|||
69879|Bindook Group|70542|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Barrallier Ignimbrite, Joaramin Ignimbrite, Quialigo Volcanics, Tangerang Formation, Bullamalita Conglomerate.|||
69879|Bindook Group|70543|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Barrallier Ignimbrite, Murruin Formation|||
69879|Bindook Group|70601|5|Briefly described|p55|Devonian|Devonian|Post-Benambran Orogeny.|||||Quartzose and lithic sandstones, felsic volcanics and limestones.|
69879|Bindook Group|70661|3|Fully described|vii, viii, p4, p9, p33|Pragian|Lochkovian|Comagmatic with Arthursleigh Suite. Name derived from Bindook Highlands. Synonymous with Bindook Porphyry, Brayton volcanics, Bindook Porphyry Complex, Bindook Complex or the Bindook Volcanic Complex. Forms deeply incised mountainous terrain to subdued and cleared terrain. Estimated thickness ranging from 2.7km to 3.5km. Deposited in shallow to moderately deeper marine and tidally reworked  shallow marine.  Fluvio-lacustrine to subaerial material also present. Structure, metamorphism, geochemistry and fossil assemblage discussed. Equivalent in age to Black Range Group, Crudine Group. Age based on biostratigraphic evidence. See also  p51-p55, p64, p83, p145.|||Barrallier Ignimbrite, Joaramin Ignimbrite, Tangerang Formation|Unconformably overlies Adaminaby group, disconformably? overlies Bungonia Group, unconformably overlain by Tallong Conglomerate, locally intruded by Arthursleigh Suite.|Felsic ignimbrite sheets, intermediate to felsic lavas, volcanic quartzose sedimentary rocks.|
69879|Bindook Group|70876|5|Briefly described|p1, p30, p77|Lochkovian|Lochkovian|Lachlan Orogen.|||Includes the Barrallier Ignimbrite.|||
69879|Bindook Group|71069|6|Mentioned|p23, p40 fig 17, p43, p135, p143|Lochkovian|Pragian|A SHRIMP age of 411 +/- 3 Ma was also obtained. Age further supported by SHRIMP ages obtained for the Long Flat Volcanics. See also p154, p163. |409 +/- 4 Ma (SHRIMP U-Pb)||Includes the Bullamalita Conglomerate, Murruin Formation and Quialigo and Long Flat Volcanics.|Intruded by the Candelo and Arthursleigh Supersuites. Unconformably overlies the Mount Fairy Group.||
69879|Bindook Group|71303|5|Briefly described|map legend|Pragian|Lochkovian||||Includes Tangarang Formation, Joaramin Ignimbrite, Barrallier Ignimbrite.|||
69879|Bindook Group|71656|5|Briefly described|p10 Fig.1, p13 Fig.2, p38-40|Emsian|Pridoli|Only early Devonian stratigrpahy around Windellama discussed here. Shown in Fig.2 as Pragian to Emsian, but discussion of Tangerang and Murruin Formations suggest at least older base age for this Group.|||Includes Tangerang Formation, Bullamalita Conglomerate, Quialigo Volcanics, Barrallier Ignimbrite, Joaramin Ignimbrite, Murruin Formation.||Volcanics including ignimbrite. Contains limestone pods.|
69879|Bindook Group|71699|5|Briefly described|Map legend.|Devonian|Devonian||||Tangerang Formation; Quialigo, Long Flat Volcanics; Jinglemoney, Larbert Conglomerates.|||
69879|Bindook Group|71700|2|Defined|vi, p7, p10, p15, p23-p25, CD|Pragian|Lochkovian|Named for the Bindook Highlands. Type sections are defined for constituent units. The name Bindook Porphyry was first used by McElroy and Relph (1961), other terms used include Bindook Porphyry Complex, Bindook Complex and Bindook Complex. The Bindook Group was formally defined by Thomas and Pogson (2012) and extended to include the Quialigo Volcanics, Bullamalita Conglomerate, Murruin Formation, Long Flat Volcanics and rocks previously assigned to the Gundary Beds, Towrang Beds, Gundary Formation.  Also includes the Jinglemoney Conglomerate, Tangerang Formation, Joaramin Ignimbrite and the Barrallier Ignimbrite. Thickness of constituent units is provided. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils, distinguishing features and economic geology are discussed. Age is derived from biostratigraphy and SHRIMP U-Pb dates obtained for constituents and their sub-units. This group is temporally equivalent to the Black Range Group and may be equivalent in part to the Crudine Group. See also p36-p38, p41-p43, p58, p62, p74, p79, p82, p110.|||Includes the Bullamalita Conglomerate, Larbert Conglomerate and the Murruin Formation.|Unconformably overlies the Mount Fairy Group, Bungonia Group, Adaminaby Group, Bendoc Group and Margules Group.|Large volume ignimbrites, coherent dacite, minor intermediate to mafic lavas, volcaniclastic conglomerate, snadstone, siltstone, limestone and rare quartz sandstone.|
69879|Bindook Group|73215|6|Mentioned|p1003|||Eastern Lachlan Orogen. Caldera collapse structures have been recognised in this rock assemblage; the authors suggest a similar tectonic setting for the Talmo Formation.||||||
69879|Bindook Group|73582|5|Briefly described|p114|Early Devonian|Early Devonian|Wombeyan Caves area. Previously the Bindook Volcanic Complex.|||||A variable association of volcanic, volcaniclastic, clastic and carbonate rocks, united by their silicic volcanic affinities, esp. dacite.|
69825|Bingara Volcanics|63347|2|Defined|p5 Fig. 2, p29|Early Miocene|Late Oligocene|Of Delungra Volcanic Suite. Unconformable on Parry Group; interfingers with Derra Derra Volcanics. Age: 24Ma (K-Ar). Max.thickness: 60m. Alkaline olivine basalt + basanite lavas with minor volcaniclastic rocks + diamond-bearing gravels. See also p7, p13.||||||03-JUL-14
69825|Bingara Volcanics|73581|5|Briefly described|p14-15|Oligocene|Oligocene|Up to 20 m thick lavas.|23.9+/-0.3 Ma K-Ar|||Interbedded with Derra Derra Volcanics|Basanites and volcaniclastic units.|
70031|Binghams Back Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Grey to buff, fine- to coarse-grained quartzose to quartzo-feldspathic sandstone interbedded with green-grey siltstone and mudstone. Rare vitric tuff. Two subunits.||||||15-NOV-16
70031|Binghams Back Formation|68592|3|Fully described|p608-9, p611-3, p667-72, p1041|Lochkovian|Ludlow|New name, after Binghams Back Creek (a tributary of the Abercrombie River). These rocks appeared as Sks (Kildrummie Group flysch-like sequence) on Taralga 1:100 000 sheet (1st edition). Type section described. 820-1200m thick. Geophysical properties described. Age range from surrounding units.|Between c.424 Ma and c.411 Ma.|Unit in Campbells Group.||Conformably overlies Kangaloolah Volcanics. Is overlain gradationally by Dunchurch Formation.|Basal siltstone, mudstone and fine-grained sandstone commonly showing horizontal lamination and climbing ripples; massive, normal graded, quartzose to quartzofeldspathic turbiditic sandstones with ripple cross-lamination.|
70031|Binghams Back Formation|70192|5|Briefly described|Map Legend|Lochkovian|Pridoli|Scb[3 asterisks]. Includes two unnamed subunits; thin-thickly bedded, fine-medium grained quartzose-quartzofeldspathic sandstone and a massive, medium-thick bedded sericite-biotite-quartz siltstone and mudstone. On Crookwell and Taralga 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Campbells Group|Includes two unnamed members.|Is overlain by Dunchurch Formation (of Crudine Group). Overlies, and interfingers with, Kangaloolah Volcanics.|Fine-medium grained quartzose-quartzofeldspathic sandstone, siltstone and mudstone; rare vitric tuff.|
70031|Binghams Back Formation|70297|5|Briefly described|map legend|Silurian|Silurian|Presented as Binghams Back Fm.||||||
70031|Binghams Back Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed subunits; thin-thickly bedded, fine-medium grained quartzose-quartzofeldspathic sandstone and a massive, medium-thick bedded sericite-biotite-quartz siltstone and mudstone.||Campbells Group|Includes two unnamed members||Fine-medium grained quartzose-quartzofeldspathic sandstone, siltstone and mudstone; rare vitric tuff.|
70031|Binghams Back Formation|70544|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed members; thin-thickly bedded, fine-medium grained quartzose-quartzofeldspathic sandstone and a massive, medium-thickly bedded, sericite biotite quartz siltstone and mudstone||Campbells Group|Includes two unnamed members||Fine-medium grained quartzose-quartzofeldspathic sandstone, siltstone and mudstone; rare vitric tuff (only subunits appear on map).|
70031|Binghams Back Formation|71656|6|Mentioned|p13 Fig.2|Lochkovian|Ludlow|||Campbells Group||Overlies Kangaloolah Volcanics. Overlain by Dunchurch Formation.||
30469|Bingie Bingie Suite|22815|5|Briefly described|p89,90|||||||||
30469|Bingie Bingie Suite|43233|5|Briefly described|Map Legend||Devonian|of Moruya Batholith.||||||
81956|Bingie Grumble Formation|72700|5|Briefly described|Mapsheet 1|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|||Orange to white-weathering, flow-foliated, porphyritic trachyte, Contains bright green aegerine, olive green wilkinsonite and feldspathoids. Minor autobreccia.|02-NOV-20
30648|Biraganbil Formation|22529|5|Briefly described|p1|||Parent Chesleigh Group||||||
30648|Biraganbil Formation|22590|6|Mentioned|Fig3 P754||Ludlow|||||||
30648|Biraganbil Formation|22857|4|Described|p470 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Chesleigh Group. Quartz-lithic arenite, slate, mudstone. Max. thickness: 800m. Geological Province: Hill End Trough.||||||
30648|Biraganbil Formation|23043|5|Briefly described|Map Legend|Pridoli|Ludlow|of Chesleigh Group.||||||
30648|Biraganbil Formation|23170|2|Defined|p74|Ludlow|Wenlock|of Chesleigh Group.||||||
30648|Biraganbil Formation|24394|5|Briefly described|p170|Pridoli|Ludlow|Of Chesleigh Formation.||||||
30648|Biraganbil Formation|68003|5|Briefly described|p24 Fig.3-e, p146. |Ludlow|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Lower unit in Chesleigh Group.||Is overlain by Piambong Formation.|Quartz-lithic, feldspar-lithic and quartz sandstone, siltstone, slate, shale.|
30648|Biraganbil Formation|68592|5|Briefly described|p650|Late Silurian|Late Silurian|||Unit in Chesleigh Group.||Correlated with Cuddyong Formation (Campbells Group).||
30648|Biraganbil Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Chesleigh Group||||
30648|Biraganbil Formation|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4|Early Devonian|Late Silurian|Hill End Trough. [Map symbol suggests Silurian age]||||Underlies the Piambong Formation.||
35167|Bird Cage Bed|23055|6|Mentioned|Fig13p25|||||||||
38921|Bird Flat Volcanic Member|24417|2|Defined|p90|Early Devonian|Early Devonian|Of Kadungle Group.  Previously mapped as undifferentiated Trundle Group (Brunker, 1976) and also "acid volcanics" of Connolly (1956) and Foldvary (1969).  Overlain by Hervey Group; underlain by Beugamel Sandstone.  Max. thickness: ~300m.||||||
38921|Bird Flat Volcanic Member|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Kadungle Volcanics (Trundle Group).||||||09-JUN-04
38921|Bird Flat Volcanic Member|60009|5|Briefly described|Map Legend|Pragian|Pragian|Of the Trundle Group.||||||13-JUL-04
28370|Birdwood Formation|22616|6|Mentioned|Fig.1 p670|Devonian|Devonian|||||||
28370|Birdwood Formation|22736|2|Defined|p614|Frasnian|Frasnian|revised upgrading of Birdwood beds||||||
28370|Birdwood Formation|22857|4|Described|p500 App.1 Tb.A1.7|Frasnian|Frasnian|Laminated arenite-mudstone, shale and volcaniclastic arenite, ashfall tuff and rare basalt. Ellenborough Volcanics pass laterally into these rocks. Max. thickness: 1550m.||||||
28370|Birdwood Formation|42547|5|Briefly described|p39|||||||||
28370|Birdwood Formation|44093|5|Briefly described|p67 Fig. 6.6|Devonian|Devonian|In the Southern Hastings Block. Geological Province: New England Fold Belt.||||||
28370|Birdwood Formation|47056|6|Mentioned|Fig.2 P523|||Variation of Birdwood beds?||||||
28370|Birdwood Formation|65940|6|Mentioned|p197|Frasnian|Frasnian|Yarras district, NSW. Dominantly mafic clastic provenance.||||Underlain by Mile Road Formation.||
28370|Birdwood Formation|70939|6|Mentioned|p826, p828|Devonian|Devonian|Southern Hastings Block.||||||
28370|Birdwood Formation|71628|6|Mentioned|p17:97|||||||Is intruded by Forbes River Porphyrite.||
77319|Birken Head Rhyolite|68005|5|Briefly described|p57, pp138-139.|Late Carboniferous|Late Carboniferous|Associated with at least 11 ignimbrite members of the Willuri Formation.|324.0 +/- 3.0 Ma.||||Red-green, glassy to partly pumiceous, unwelded ignimbrite. Also purple, grey to beige rhyolitic ignimbrites, welded and unwelded, pumiceous to fine-grained to glassy to spherulitic; rhyolite lava; crystal-rich resedimented pyroclastics.|
39258|Birken Head Volcanic Member|50613|2|Defined|p211, p229 App. 1|Westphalian|Westphalian|Of the Willuri Formation.  Volcanic member of theTulcumba package (informal grouping of stratigraphically recognisable distinctive, mappable units). Overlies Penrhyn Rhyolite Member.  Age: 315+/-2.8Ma (SHRIMP). Max.thick:650m.||||||22-FEB-05
39258|Birken Head Volcanic Member|62095|6|Mentioned|p266|||Of the Willuri Formation in the Carroll-Nandewar region of the Tamworth Belt.||||||
81175|Birrimba Member|72296|2|Defined|x, p5, p8-10, p13, p16-19, p57-58|Early Ordovician|Early Ordovician|New name, after Birrimba property and homestead: defined in this study (Gilmore, in Gilmore et al., 2018). Type locality designated on the Narringa property at Lat. -31.4027 degrees, Long. 146.9081 degrees. Part of this unit was previously mapped as the Pink Quartzite [Member]. Crops out as reddish boulders. Thickness unknown. An interpreted exhalative unit. Unfossiliferous; age from conformity with Narrama Formation. Geophysical properties detailed. Several photographs.||Narrama Formation.|||Red-grey, massive to finely laminated, quartz-hematite +/- magnetite units; white quartz veining common. Contains euhedral pyrite cubes <3mm, commonly weathered or removed entirely, leaving vughs. Also a white to beige, massive silica-pyrite rock.|
36147|Bishopthorpe Dolerite|50234|5|Briefly described|Map Legend|Emsian|Pragian|||||||
36147|Bishopthorpe Dolerite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Bishopthorpe Suite. Greenish-grey, massive, medium-grained quartz dolerite with a subophitic texture.||||||
36147|Bishopthorpe Dolerite|68592|3|Fully described|p771, p778, p786, p794-5, p1664-73|Early Devonian|Early Devonian|See also p730 Fig.132. New name, after Bishopthorpe Manor. Type locality and representative exposure are described. Thickness unknown. Geochemistry briefly discussed. Age unknown, but younger than Late Silurian.||||Intrudes Kingsdale Limestone Member, Sooley Volcanic Member and Joppa Siltstone Member (De Drack Formation, Mount Fairy Group).|Green-grey massive equigranular subophitic dolerite with up to 2% interstitial quartz, and medium-grained gabbro without the quartz.|
36147|Bishopthorpe Dolerite|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dsd. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.||Bishopthorpe Suite|||Massive, equigranular, sub-ophitic dolerite and gabbro with up to 2% interstitial quartz.|
36147|Bishopthorpe Dolerite|70210|6|Mentioned|p38|||Yass-Goulburn district. Yielded no zircons for dating.||||||
36147|Bishopthorpe Dolerite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Bishopthorpe Suite|||Green-grey, massive, equigranular, sub-ophitic dolerite and gabbro with up to 2% interstitial quartz.|
36147|Bishopthorpe Dolerite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Bishopthorpe Suite|||Massive, equigranular, sub-ophitic dolerite and gabbro with up to 2% interstitial quartz.|
36147|Bishopthorpe Dolerite|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Bishopthorpe Suite|||Massive, equigranular, sub-ophitic dolerite and gabbro with 2% interstitial quartz.|
36147|Bishopthorpe Dolerite|71069|6|Mentioned|p147, p149|||||||Intrudes the De Drack Formation.||
74311|Bishopthorpe Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Contains Bishopthorpe Dolerite and 2 unnamed units; includes quartz dolerite and gabbro rocks.||||||18-JUN-08
74311|Bishopthorpe Suite|66087|6|Mentioned|p3 Fig. 2|Devonian|Devonian|||||||
74311|Bishopthorpe Suite|68592|4|Described|p74 Tb.5, p298, p650, p1657, p1664-73|Early Devonian|Late Silurian|See also p803, p845 Fig.141. New name, after Bishopthorpe Dolerite, the type (and only defined) plutonic constituent. Previously unnamed dolerite and gabbro intrusions on the first edition map. Geochemistry discussed. No known volcanic equivalent. Records widespread tholeiitic magmatism. Wyangala, Peelwood, Goulburn and Bungonia structural zones: deformation described.||||Intrudes Cuddyong Formation, Abercrombie Formation, Wyangala and Wologorong Supersuites, and Woodlawn Volcanics.|Gabbro, and dolerite with up to 2% interstitial quartz; mainly dyke swarms, some sills.|
74311|Bishopthorpe Suite|70192|5|Briefly described|Map Legend|Emsian|Emsian|Includes two unnamed units: massive, eqigranular, sub-ophitic dolerite and gabbro; gabbro. On Boorowa, Crookwell, Taralga, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Bishopthorpe Dolerite and two unnamed units.|||
74311|Bishopthorpe Suite|70541|5|Briefly described|Map Legend|Devonian|Devonian||||||Green-grey, massive, equigranular, sub-ophitic dolerite and gabbro.|
74311|Bishopthorpe Suite|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes two unnamed members, one of gabbro and the other of massive, equigranular, sub-ophitic dolerite and gabbro.|||Includes Bishopthorpe Dolerite.|||
74311|Bishopthorpe Suite|70543|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed gabbro|||Includes Bishopthorpe Dolerite and one unnamed member|||
74311|Bishopthorpe Suite|70544|5|Briefly described|Map Legend|Devonian|Devonian|Includes an unnamed member of massive, equigranular, sub-ophitic dolerite and gabbro.|||Includes Bishopthorpe Dolerite and one unnamed member.|||
74311|Bishopthorpe Suite|70545|5|Briefly described|Map Legend|Devonian|Devonian|Lithology is of an unnamed member.|||||Massive, equigranular, sub-ophitic dolerite and gabbro.|
74311|Bishopthorpe Suite|71069|6|Mentioned|p135, p156|Early Devonian|Silurian|||||Intrudes the Woodlawn Volcanics, Mount Fairy Group.||
82363|Bitter Vine Leucomonzogranite Phase|71628|5|Briefly described|p17: 13, 15, 17-19|||New name. Originally Petroi Leucoadamellite of Flinter (1981 unpublished); invalid as the Petroi Metabasalt has precedence. Named after a local mountain. Crops out as four small bodies ~22 km SSW of Ebor in remote, rugged and forested areas. Is geochemically assigned to the Bitter Vine Suite.||Botumburra Range Granodiorite.||Intrudes Nambucca beds.|Fine-grained biotite leucomonzogranite.|
73421|Bittles Tank Volcanics|66623|2|Defined|p74, 80, pp95-97, p229.|Middle Cambrian|Middle Cambrian|Defined as an igneous suite in this study. Formerly part of Wonominta beds (Warris 1967), unit in Ponto beds (Mills 1992), in Ponto Group (Stevens et al. 2000). Tholeiitic magmatism which continued late into the Delamerian Orogeny, with numerous small, scattered gabbro plutons. Deeper water environment. Type locality at Benny Hill, Kayrunnera Station. Has age and geochemical correlations with Glenelg Complex.|c.510 Ma (Black 2006) to 496.3 +/- 3.1 Ma.|Unit in Ponto Group.|No formal members; includes previously (Buckley 2000) reserved Ponto Group members including Blue Rock Well, Gum Creek and Tekum Creek Basalts; informal Kayrunnera Gabbro and Nuntherungie Dolerite.|Intrudes Teltawongee, Grey Range and Ponto Groups. Is unconformably overlain by Kayrunnera Group.|Dark grey-green mafic outcrops of gabbro, dolerite; football-sized E-MORB pillow lavas with sparse and small vesicles; basaltic flows, basic tuffs, basaltic to doleritic sills.|
73421|Bittles Tank Volcanics|66918|5|Briefly described|Map legend|Cambrian||Three un-named units are mapped separately.||Unit in Ponto Group.||Map key shows: Overlies Baroorangee Creek Formation. Is overlain by Grasmere Formation.|Variably deformed mafic intrusives, and extrusive lavas with a tholeiitic geochemical affinity: small dykes and plutons of dolerite; gabbro; porphyritic metabasalt with pillow textures.|25-SEP-13
73421|Bittles Tank Volcanics|67105|5|Briefly described|p650, 653-654, 658-659, 661, 665-666|Cambrian|Cambrian|Wonnaminta Zone, Koonenberry Belt. Geochemistry discussed.||Ponto Group.|||Basalt dykes and lavas, both tholeiitic (mainly) and alkaline.|
73421|Bittles Tank Volcanics|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Ponto Group.|||Undifferentiated: variably deformed mafic intrusives, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|67322|4|Described|p11, p13|Stage 9|Paibian|Age determined using SHRIMP zircon analysis of one intrusive rock.|496.3 +/- 3.1 Ma (SHRIMP  zircon: Black, 2005).|Unit in Ponto Group||Intrudes the Teltawongee and Grey Range Groups.|Consists of enriched mid-ocean ridge basalts, tholeiitic pillow lavas, basaltic flows and basic tuffs. Also included in this unit are intrusive basaltic to doleritic sills.|21-FEB-18
73421|Bittles Tank Volcanics|69961|5|Briefly described|Map legend|Cambrian|Cambrian|No outcrop in map area. Three facies are mapped separately.||Unit in Ponto Group.|||Undifferentiated: variably deformed mafic intrusions, and extrusive mafic, tholeiitic lavas; coarse- and fine-grained gabbros and dolerites, and strongly magnetic phyllite.|
73421|Bittles Tank Volcanics|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|3 un-named units: Coarse-grained, plagioclase with amphibole dominated gabbro to dolerite; relic pyroxene, amphibole and plagioclase; altered by epidote-carbonate-sericite or epidote-albite-chlorite-quartz; hornsfel contacts. Fine- to medium-grained, plagioclase with amphibole or pyroxene-dominated gabbro and dolerite; epidote-carbonate-sericite alteration, hornfels contacts. Pale to dark green-grey, variably cleaved, fine-grained porphyritic metabasalt, with plagioclase phenocrysts to >1cm; mm scale vesicles and pillow textures; weakly magnetic; widely distributed.||Ponto Group|Includes 3 un-named units.||Variably deformed mafic intrusions, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|3 unnamed subunits: Small dykes and plutons of diorite with clear intrusive relationship with country rocks (Ponto and Grey Range Group phyllite); restricted to south of Cymbric Vale homestead. Fine- to medium-grained, plagioclase with amphibole or pyroxene dominated gabbro and dolerite; epidote-carbonate-sericite alteration; hornfelsed contacts. Pale to dark green-grey, variably cleaved, fine-grained porphyritic metabasalt, with plagioclase phenocrysts to >1cm; mm scale vesicles and pillow textures; weakly magnetic; widely distributed throughout Ponto Group.||Ponto Group|Includes 3 un-named units.||Variably deformed mafic intrusives, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|70651|5|Briefly described|Map Legend|Cambrian|Cambrian|5 unnamed sub-units: Fine- to medium-grained, plagioclase with amphibole or pyroxene-dominated intrusions with epidote-carbonate-sericite alteration, hornfels contacts. Green-grey cleaved metadolerite intrusions. Phyllite; epidote-pyrite-quartz alteration, epidote veins, calcite amygdules. Variably cleaved mafic rock in Willandra region. Porphyric metabasalt with plagioclase phenocrysts >1cm. ||Ponto Group|Includes 5 unnamed sub-units.||Variably deformed mafic intrusions, and extrusive mafic lavas with a tholeiitic geochemical affinity.|
73421|Bittles Tank Volcanics|70838|4|Described|p269-270|Cambrian|Cambrian|Koonenberry Belt.|c.510 Ma.|Ponto Group.||Is overlain unconformably by Kayrunnera Group.|Discontinuous lenses of tholeiitic to alkaline basalt.|
73421|Bittles Tank Volcanics|71262|6|Mentioned|p9 Fig 7|Cambrian|Cambrian|Map symbol suggests part of Ponto Group.||||||
73421|Bittles Tank Volcanics|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Dykes and plutons of foliated diorite; coarse-grained gabbro to dolerite; green-grey cleaved magnetic metadolerite; Green-grey, variably cleaved, fine-grained porphyritic metabasalt.|09-DEC-21
73421|Bittles Tank Volcanics|73177|6|Mentioned|1115 Fig.17|Cambrian|Cambrian|||Ponto Group.||||30-AUG-22
34791|Black Hill Gabbroic Complex|22945|6|Mentioned|p8|||Mentioned under - Area C geology.||||||
34791|Black Hill Gabbroic Complex|24509|5|Briefly described|p39 Fig. 1, p40, p42 Tab.1|Early Ordovician|Early Ordovician|Diorite. Age: 489+/-10Ma (isochron age). Geological Province: Murray Basin.||||||04-MAY-05
34791|Black Hill Gabbroic Complex|60567|5|Briefly described|p38|||||||||
82366|Black Knob Monzogranite|71628|4|Described|p3-72; p13-1; p14: 17, 20; p19:12-17,108|||New name (this study). Previous names, after a local homestead, included the (unpublished) Woodlands Adamellite (Stolz, 1976) and Woodlands Quartz Monzonite (Hensel, 1982); Woodlands Monzonite is reserved in ASUD; but all are void due to the Woodlands Granite (Chappell et al., 1991) having priority. Named after a prominent geographic feature. Forms a small, N-trending narrow intrusion ~40 km NE of Guyra. Lithologies, mineralogy and geochemistry described in great detail. Age determination by Landenberger (1996).|249 +/- 2 Ma (biotite whole-rock).|Black Knob Suite.||Intrudes Kookabookra Monzogranite, Oban River Leucomonzogranite and Sara beds (and faulted against this last). A small outlier occurs within Wards Mistake Monzogranite.|Slightly porphyritic, hornblende-biotite-(clinopyroxene-orthopyroxene) quartz monzonite to quartz-poor monzogranite, possibly minor monzonite. Characterised by abundant mafic enclaves (similar to Moggs Swamp Complex). A-type.|
24186|Black Mountain Sandstone|12185|5|Briefly described|map legend|Lower Ordovician|Lower Ordovician|Quartz sandstone, quartzite, thin shales. BMR map symbol: Ol.||||||
24186|Black Mountain Sandstone|22815|6|Mentioned|p18|Silurian|Silurian|Reassigned Silurian in age from Ordovician.||||||
24186|Black Mountain Sandstone|22857|4|Described|p134, p424 App.1 Tb.A1.5|Early Silurian|Early Silurian|Grey, thickly bedded, massive, medium-grained arenite with siltstone and shale interbeds. Max. thickness: >450m. ||||||
24186|Black Mountain Sandstone|22941|5|Briefly described|p291||Early Silurian|||||||
24186|Black Mountain Sandstone|23245|5|Briefly described|p134||Early Silurian|||||||
24186|Black Mountain Sandstone|23309|6|Mentioned|p390|||||||||
24186|Black Mountain Sandstone|23454|6|Mentioned|p33|||||||||
24186|Black Mountain Sandstone|29992|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
24186|Black Mountain Sandstone|29994|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
24186|Black Mountain Sandstone|30332|3|Fully described|p124|||||||||
24186|Black Mountain Sandstone|31019|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
24186|Black Mountain Sandstone|31111|6|Mentioned|p66|||Also mention P68, 72, 26||||||
24186|Black Mountain Sandstone|31161|5|Briefly described|PA6|||||||||
24186|Black Mountain Sandstone|31284|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
24186|Black Mountain Sandstone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
24186|Black Mountain Sandstone|32672|6|Mentioned|p672|||||||||
24186|Black Mountain Sandstone|32820|6|Mentioned|Table 1|||Refers Crook et al (1973)||||||
24186|Black Mountain Sandstone|33125|6|Mentioned|p15|||Correlation chart||||||
24186|Black Mountain Sandstone|33325|4|Described|p21|||Ord? or Camb. See also Table 1||||||
24186|Black Mountain Sandstone|33328|4|Described|Table 1|||P10.||||||
24186|Black Mountain Sandstone|34404|4|Described|p89|||||||||
24186|Black Mountain Sandstone|34405|6|Mentioned|p119|||||||||
24186|Black Mountain Sandstone|35110|6|Mentioned|p3|||||||||
24186|Black Mountain Sandstone|35614|5|Briefly described|p14|||||||||
24186|Black Mountain Sandstone|36413|6|Mentioned|Table 3|||||||||
24186|Black Mountain Sandstone|36633|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
24186|Black Mountain Sandstone|37348|6|Mentioned|p97|||||||||
24186|Black Mountain Sandstone|37727|4|Described|p38|||See also P17 and P29.||||||
24186|Black Mountain Sandstone|37728|4|Described|Table 2|||||||||
24186|Black Mountain Sandstone|37752|6|Mentioned|p106|||||||||
24186|Black Mountain Sandstone|38664|5|Briefly described|p5|||||||||
24186|Black Mountain Sandstone|39331|4|Described|p49|||||||||
24186|Black Mountain Sandstone|39800|6|Mentioned|Map legend|Cambrian|Cambrian|Pre Middle OrdovicianProb. Cambrian||||||
24186|Black Mountain Sandstone|39947|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
24186|Black Mountain Sandstone|40328|3|Fully described|p50|||||||||
24186|Black Mountain Sandstone|41356|3|Fully described|p10|||Described P32||||||
24186|Black Mountain Sandstone|42497|5|Briefly described|Map legend|Llandoverian|Llandoverian|||||||
24186|Black Mountain Sandstone|42727|5|Briefly described|map legend|Early Silurian|Early Silurian|Sandstone, siltstone and minor shale (proximal quartz turbidites). Unconformably underlies Canberra Formation, including Camp Hill Sandstone Member. Overlies State Circle Shale. BMR map symbol: Slb. Geol. Prov: Canberra Block.||||||
24186|Black Mountain Sandstone|42820|2|Defined|p12|Early Silurian||||||||
24186|Black Mountain Sandstone|43159|5|Briefly described|Fig.2p4,p9.||Early Silurian|||||||
24186|Black Mountain Sandstone|43344|14|Not recorded|p3,4,109,110,112,113||Early Ordovician|p115,116||||||
24186|Black Mountain Sandstone|43383|14|Not recorded|p7,8||Cambrian|||||||
24186|Black Mountain Sandstone|43384|14|Not recorded|Map Legend||Ordovician|||||||
24186|Black Mountain Sandstone|43385|14|Not recorded|p169-171|||Older than Middle Ordovician||||||
24186|Black Mountain Sandstone|43479|14|Not recorded|p62,77,95f||Early Ordovician|pre M.Ord||||||
24186|Black Mountain Sandstone|43481|6|Mentioned|3-8||Devonian|||||||
24186|Black Mountain Sandstone|43682|5|Briefly described|p291||Early Silurian|||||||
24186|Black Mountain Sandstone|44093|5|Briefly described|p197 App. 1|Early Silurian|Early Silurian|In the Bruce Block. Geological Province: Lachlan Fold Belt.||||||
24186|Black Mountain Sandstone|44970|2|Defined|p5-12,18,20-2,63-5,||Early Ordovician|p69-71,74-5,78-80,84,87-8,91,map. See also Lexicon||||||
24186|Black Mountain Sandstone|45147|6|Mentioned|M118|||||||||
24186|Black Mountain Sandstone|47033|5|Briefly described|p78|||||||||
24186|Black Mountain Sandstone|49043|5|Briefly described|p6|||||||||
24186|Black Mountain Sandstone|63290|6|Mentioned|p385|Llandovery|Llandovery|Underlain unconformably by Acton Shale.||||||
24186|Black Mountain Sandstone|66197|6|Mentioned|p629|||Deep marine quartz and lithic turbidites.||||||14-MAR-12
24186|Black Mountain Sandstone|67322|5|Briefly described|p16|Silurian|Silurian|Lower Silurian age. Occurs in the Canberra region.||||Equivalent to the Tidbinbilla Quartzite.||21-FEB-18
24186|Black Mountain Sandstone|68592|6|Mentioned|p13, p357|Early Silurian|Early Silurian|Has many features in common with Mundoonen Sandstone, but age differences rule out correlation.||||||
24186|Black Mountain Sandstone|71069|6|Mentioned|p87, p93|||||||||
24186|Black Mountain Sandstone|73215|6|Mentioned|p994|||Canberra area.||||||
24186|Black Mountain Sandstone|73264|6|Mentioned|p1392 Fig.14, p1407|||||||||
28374|Black Rock Subgroup|22857|5|Briefly described|p217, p492 App.1 Tb.A1.7|Devonian|Devonian|Basal section of the Catombal Group. Geological Province: Lambie Basin.||||||
28374|Black Rock Subgroup|22859|6|Mentioned|p217|||||||||
28374|Black Rock Subgroup|23043|5|Briefly described|Map Legend|Famennian|Frasnian|Of the Catombal Group.||||||09-SEP-08
28374|Black Rock Subgroup|23170|6|Mentioned|p250|||Of the Catombal Group.||||||09-SEP-08
28374|Black Rock Subgroup|23214|3|Fully described|p234|Late Devonian|Late Devonian|Of Catombal Group. Geological Province: Lambie Basin. Overlain by Canangle Subgroup.||||||09-SEP-08
28374|Black Rock Subgroup|24126|6|Mentioned|p172|||Of the Catombal Group.||||||
28374|Black Rock Subgroup|24247|5|Briefly described|p37|Late Devonian|Late Devonian|Of the Catombal Group.||||||09-SEP-08
28374|Black Rock Subgroup|39655|6|Mentioned|Plate 1|||||||||
28374|Black Rock Subgroup|39657|6|Mentioned|M30|||||||||
28374|Black Rock Subgroup|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
28374|Black Rock Subgroup|43507|14|Not recorded|p125|||||||||
28374|Black Rock Subgroup|43513|14|Not recorded|p72|||||||||
28374|Black Rock Subgroup|43782|5|Briefly described|Map Legend|Famennian|Frasnian|Of the Catombal Group.||||||09-SEP-08
28374|Black Rock Subgroup|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Catombal Group.  Massive to bedded quartz and lithic sandstone, haematitic shale, conglomerate.||||||
28374|Black Rock Subgroup|68003|5|Briefly described|p24 Fig.3-e. p142. |Frasnian|Givetian|Lachlan Fold Belt, Brigalow Belt South Bioregion. Northern Sydney Basin. ||Unit in Catombal Group.||Is overlain by Kurrool Formation.|Massive to bedded quartz and lithic sandstone, hematitic shale, conglomerate.|
28374|Black Rock Subgroup|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Catombal Group||||
28374|Black Rock Subgroup|73299|6|Mentioned|p1105|Late Devonian|Late Devonian|||Catombal Group||Overlies the Brymedura Sandstone, underlies the Kurrool Formation.||
82121|Black Snake Creek Suite|71628|6|Mentioned|p19:18||||||Black Snake Creek Granite.|||
82121|Black Snake Creek Suite|72528|5|Briefly described|p78.|Lopingian|Lopingian|Date from Black Snake Creek Granite.|252.0+/-1.2 Ma U238/Pb206 (Pb207-corrected)||Includes Black Snake Creek Granite|||
67907|Blackfellows Gully Leucomonzogranite|71628|4|Described|p8: 4, 7-12, 72, 115; p11: 25; p19:79|||DMR NAND04 Nandewar Geology Integration and Upgrade Project, after unpublished work by Chappell and Bryant (1994). Previously the Blackfellows Gully Leucoadamellite of Leitch et al. (1971) after unpublished work by Flood (1971). Named after a local geographical feature. Forms an irregularly-shaped intrusion 20km W of Armidale and 10km E of Yarrowyck. Crops out as angular blocks to large sheets. No radiometric age; but is cut by a dyke swarm dated at 252.5 Ma (SHRIMP: Cross and Blevin, 2010). Limited geochemistry described.||Llangothlin Suite.||Intrudes Sandon beds. Is intruded by Yarrowyck Granodiorite and ?Uralla Granodiorite.|Texturally heterogeneous biotite(-hornblende) leucomonzogranite, with porphyritic, flow-banded, and coarse-grained equigranular variants (quartz porphyry, flow-banded quartz porphyry, leucomonzogranite). Contains sedimentary xenoliths. I-type.|
31551|Blackmans Creek Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
31551|Blackmans Creek Suite|71206|6|Mentioned|p373|||Lachlan Fold Belt.|||Blackmans Creek Granite.||Aluminous A-type granite.|
82414|Blacksmiths Creek Monzogranite|71628|5|Briefly described|p12: 1-2, 4-6; p15: 33, 57, 65|||See also p19: 159-160. Name ascribed by Bultitude (unpublished), after a local watercourse. Occurs several kilometres W and NW of Tenterfield. Not adequately mapped. Has an irregular distribution comprising three components (described). Limited geochemistry briefly described.||Sailor Jack Suite.||Intrudes Wallangarra Volcanics and Dundee Rhyodacite (Wandsworth Volcanic Group). Abuts Stanthorpe Complex.|Pale grey, fine-grained, moderately porphyritic hornblende-biotite granodiorite. I-type.|
26399|Blakefield Coal Member|29942|4|Described|Fig.1|||Permian||||||
26399|Blakefield Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26399|Blakefield Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26399|Blakefield Coal Member|40805|6|Mentioned|Table 1|||||||||
26399|Blakefield Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Malabar Formation.||||
25792|Bland Diorite|22434|5|Briefly described|11 fig 15|Early Silurian|Early Silurian|Geol Province Lachlan Fold Belt||||||
25792|Bland Diorite|24417|3|Fully described|p55|Early Silurian|Early Silurian|Age: 433.7+/-2.3Ma.||||||
25792|Bland Diorite|29907|2|Defined|Appendix 1|Early Silurian|Late Ordovician|Late Ordovician to Early Silurian||||||
25792|Bland Diorite|29910|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
25792|Bland Diorite|36411|6|Mentioned|p267|||Refers Bowman 1977 for definition.||||||
25792|Bland Diorite|39627|5|Briefly described|p267|||||||||
25792|Bland Diorite|40678|6|Mentioned|p6|||||||||
25792|Bland Diorite|50191|6|Mentioned|p13|||||||||
25792|Bland Diorite|50385|5|Briefly described|Map Legend|Silurian|Silurian|Medium to coarse diorite and hornblende porphyrite.||||||23-JUN-04
25792|Bland Diorite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||13-JUL-04
25792|Bland Diorite|60423|6|Mentioned|p376 Table 3|Ordovician|Ordovician|Temora region.||||||
25792|Bland Diorite|67322|5|Briefly described|p20|Early Silurian|Early Silurian||433.7 +/- 2.3|||Intrudes Narragudgil Volcanics.||21-FEB-18
25792|Bland Diorite|68822|5|Briefly described|p335|Homerian|Telychian||433.7 +/- 2.3 Ma|||||
25792|Bland Diorite|70777|6|Mentioned|p39|||||||||
70462|Blandford Rhyodacite Member|62095|2|Defined|p279 Appdx.|Early Permian|Early Permian|Of Woodton Formation. Beige to white rhyodacite lava with scattered medium to coarse phenocrysts of plagioclase and fine opaque minerals. Age: 291.1+/-3.6Ma (Asselian). Max. thickness: 10m. See also Plate 1, p260 Tb. 1.||||||31-JAN-08
31256|Blathery Creek Conglomerate Member|24247|5|Briefly described|p37|Late Devonian|Late Devonian|Parent: Canangle Subgroup (Catombal Group)||||||
31256|Blathery Creek Conglomerate Member|43512|2|Defined|p89||Late Devonian|Member of the Curra Creek Conglomerate, maximum recorded thickness 500 ft, massive red conglomerate||||||
29501|Blayney Volcanics|13139|6|Mentioned|p10|||||||||
29501|Blayney Volcanics|22679|3|Fully described|p 21|Ordovician|Ordovician|||||||
29501|Blayney Volcanics|22798|5|Briefly described|p850|Late Ordovician|Ordovician|Max Age: Middle Ordovician.||||||
29501|Blayney Volcanics|22857|5|Briefly described|p428 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Clinopyroxene basalt, agglomerate in places, volcanic arenite.||||||
29501|Blayney Volcanics|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
29501|Blayney Volcanics|23170|6|Mentioned|p34|||||||||
29501|Blayney Volcanics|23202|6|Mentioned|p1059, Fig.1|||||||||
29501|Blayney Volcanics|23213|6|Mentioned|p13|||Correlates with Fairbridge Volcanics in the Cabonne Group. of Cabonne Group.||||||
29501|Blayney Volcanics|23214|2|Defined|p61|Late Ordovician|Late Ordovician|Of Cabonne Group. Representative of shallow to moderately deep marine volcanism.||||||
29501|Blayney Volcanics|23334|6|Mentioned|10|||||||||
29501|Blayney Volcanics|24015|5|Briefly described|p10|Ordovician|Ordovician|Include ultramafic lavas and volcaniclastics.||||||21-DEC-04
29501|Blayney Volcanics|43653|5|Briefly described|Map Legend||Ordovician|||||||
29501|Blayney Volcanics|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Includes Cowringa Limestone Member. Clinopyroxene basalt, agglomeratic in places; volcanic sandstone.||||||17-JUL-08
29501|Blayney Volcanics|43782|5|Briefly described|Map Legend|Gisbornian|Gisbornian|Of Cabonne Group.||||||22-APR-09
29501|Blayney Volcanics|61815|5|Briefly described|p77, p78|||||||||
29501|Blayney Volcanics|63278|4|Described|p156|Late Ordovician|Middle Ordovician|Includes; Cowriga Limestone Member. Underlain by Coombing Formation. Geological Prov: Molong Volcanic Belt, LFB. Consists of basalt and basaltic andesite. Lower part consists of clinopyroxene-phyric and olivine-phyric, upper part is plagioclase-phyric.||||||07-FEB-11
29501|Blayney Volcanics|63283|5|Briefly described|p202, p208, p209|Late Ordovician|Darriwilian|Infomally sub-dividied into two units; lower Blayney Volcanics and upper Blayney Volcanics. Overlian by Millthorpe Volcanics, underlain by Coombing Formation. Geological Province: Molong Volcanic Belt. See p202-203.||||||07-FEB-11
29501|Blayney Volcanics|63284|6|Mentioned|p249||Darriwilian|Geological Province: Molong Volcanic Belt.||||||
29501|Blayney Volcanics|63285|5|Briefly described|p275 Fig. 2, p288|||Geological Province: Molong Volcanic Belt. Consists of basaltic lavas, limestone and volcaniclastic facies.||||||
29501|Blayney Volcanics|63286|5|Briefly described|p294 Fig. 1, p306|Ordovician|Ordovician|Includes Cowringa Limestone Member and Eagle Hawk Basalt. Consists of basalt breccias and calcareous sandstone, also has mudium-K and high-K calc-alkaline affinities (Crawford et al. 2007). Informally divided into upper and lower parts.||||||07-FEB-11
29501|Blayney Volcanics|63287|6|Mentioned|p337|||Geological Province: Molong Volcanic Belt. Comprise high-K to shoshonitic lavas.||||||07-FEB-11
29501|Blayney Volcanics|63290|5|Briefly described|p393 Tb. 1, p405, p396 Fig. 3|Bolindian|Darriwilian|Geological Province: Molong Volcanic Belt. Contains Eastonian (ca 455-450Ma) allochthonous limestone lenses.||||||
29501|Blayney Volcanics|63293|5|Briefly described|p473, p475, p469 Fig. 2|Bolindian|Darriwilian|Overlain by Millthorpe Volcanics, underlain by Coombing Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29501|Blayney Volcanics|64963|5|Briefly described|p182 Fig. 2|||Probably represent a volcanic centre in shallow marine conditions.||||||22-APR-09
29501|Blayney Volcanics|67322|5|Briefly described|Fig.5, p25|Sandbian||Macquarie Arc. Described by Wyborn, in Pogson and Watkins (1998). Age is determined from p20 Fig.5 (Strat. column) where the unit appears as Lower Blayney Volcanics and Upper Blayney Volcanics. The text on p25 suggests these are not formal names. Occurs in the Blayney region. |||Cowriga Limestone Member.|Comagmatic in its upper part with the Byng Volcanics. Overlies Coombing Formation.|Has a clinopyroxene-phyric and olivine-phyric lower part, and a plagioclase-phyric upper part; includes limestone.|21-FEB-18
29501|Blayney Volcanics|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
29501|Blayney Volcanics|70684|6|Mentioned|p3, p18, p33, p75|||||||||
29501|Blayney Volcanics|72495|6|Mentioned|p235|||Occurs to the south of Orange.||||||
29501|Blayney Volcanics|73431|5|Briefly described|p364-365|Ordovician|Ordovician|Lachlan Orogen.|||Cowriga Limestone Member|Intruded by Browns Creek Intrusive Complex||
23393|Bletchley Park Volcanic Member|42313|2|Defined|p112|Late Silurian|Middle Silurian|Reserved 1977, name varied 1986.||||||
23393|Bletchley Park Volcanic Member|42314|5|Briefly described|Map legend|Middle Silurian||||||||
26402|Bloomfield Limestone Member|22857|5|Briefly described|p462 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Taemas Limestone. Fossiliferous thinly bedded limestone, shaly limestone. Max. thickness: 98m. Geological Province: Canberra-Yass Shelf.||||||
26402|Bloomfield Limestone Member|23898|4|Described|p269, p272 Fig.3|Emsian|Emsian|Of Taemas Limestone. Overlies Currajong Limestone Member.||||||
26402|Bloomfield Limestone Member|24250|5|Briefly described|p105, p109 Fig.5|Early Devonian|Early Devonian|Of the Taemas Limestone (Murrumbidgee Group). Maximum Thickness: 120m. Overlain by Receptaculites Limestone Member (conformable). Underlain by Currajong Limestone Member (conformable)||||||18-JUN-08
26402|Bloomfield Limestone Member|32483|6|Mentioned|p33|||Refers Browne (1959)||||||
26402|Bloomfield Limestone Member|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26402|Bloomfield Limestone Member|35386|4|Described|p54|||||||||
26402|Bloomfield Limestone Member|36411|6|Mentioned|p267|||Refers Cramsie et al 1978 for definition.||||||
26402|Bloomfield Limestone Member|50230|4|Described|Map legend|Emsian|Emsian|Of the Taemas Limestone (Murrumbidgee Group).  Overlies the Currajong Limestone Member; underlies the Cockatoo Point  and Receptaculites Limestone Members.  Thinly-bedded fossiliferous limestone, impure silty limestone.||||||26-JUL-04
26402|Bloomfield Limestone Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Taemas Limestone (Murrumbidgee Group). Thinly bedded fossiliferous limestone, impure silty limestone.||||||
26402|Bloomfield Limestone Member|64992|5|Briefly described|p60 Fig. 1, p61, p76|Devonian|Devonian|Part of Taemas-Wee Jasper succession. Of Taemas Fm.Overlies Currajong Limestone Member. Contains Dipnorhynchus suessmilchi (lungfish) at its very base; and Speonesydrion iani. Bloomfield-Receptaculites Limestone Mbr contact is richest area for dipnoans.||||||30-MAR-09
26402|Bloomfield Limestone Member|65214|6|Mentioned|p272|Devonian|Devonian|NSW, Taemas. Appears in text as Bloomfield Limestone Mb. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26402|Bloomfield Limestone Member|68592|3|Fully described|p982, p984 Fig.162, p985-6, p1017-20|Emsian|Emsian|See also p1824, p1898-9. Named after Bloomfield property. Originally Bloomfield Limestone (Browne, 1959) in the Taemas Stage; when this latter became a Formation (Offenberg, 1974), its constituents became Members. Type section described. 98-122m thick. Diverse fauna described. It is also the source of boulders to cobbles in the representative deposit for colluvium.||Unit in Taemas Limestone.||Conformably overlies Currajong Limestone Member. Is overlain conformably by Cockatoo Point, or Receptaculites, Limestone Members.|Blue-grey, thinly interbedded, massive or laminated limestone and shale.|
26402|Bloomfield Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmtb. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Taemas Limestone||Overlies Currajong Limestone Member. Is overlain by Cockatoo Point Limestone Member and Receptaculites Limestone Member.|Blue-grey, thinly interbedded, massive or laminated fossiliferous limestone and shale.|
26402|Bloomfield Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, thinly interbedded, massive or laminated fossiliferous limestone and shale.|
26402|Bloomfield Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, thinly interbedded, massive or laminated fossiliferous limestone and shale.|
26402|Bloomfield Limestone Member|71656|4|Described|p12 Fig.2, p35|Emsian|Emsian|Includes numerous bivalve examples, condononts and fish. Some corals documented.||Of Taemas Limestone, Murrumbidgee Group.||Overlies Currajong Limestone Member and underlies Cockatoo Point Member.|Fossiliferous limestone.|
25794|Blow Clear Member|22857|5|Briefly described|p446 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Of Burcher Greywacke. Sandstone, conglomerate.||||||
25794|Blow Clear Member|24417|3|Fully described|p49|Silurian|Silurian|Of Burcher Greywacke.  A conglomerate lens enclosed within the Burcher Greywacke.||||||
25794|Blow Clear Member|35503|2|Defined|p206|Early Devonian|Early Devonian|New name refs Kemezys (1976). Part of Burcher Greywacke.Prob.Early Devonian||||||
25794|Blow Clear Member|40328|6|Mentioned|p38|||||||||
25794|Blow Clear Member|50385|5|Briefly described|Map Legend|Silurian|Silurian|Of Burcher Greywacke. Matrix (coarse-grained greywacke) supported lithic conglomerate.||||||23-JUN-04
25794|Blow Clear Member|60009|5|Briefly described|Map Legend|Wenlock|Llandovery|Of the Burcher Greywacke.||||||13-JUL-04
27671|Blowering Formation|22638|1|Redefined|p46|Late Silurian|Early Silurian|Previously "Blowering porphyry", "Blowering beds", "Blowering Porphyry" and "Blowering Group". Overlies Jindalee Group||||||
27671|Blowering Formation|22687|5|Briefly described|109,111,117,118|||Geol province Lachlan Fold Belt||||||
27671|Blowering Formation|22691|6|Mentioned|P315, Fig2||Silurian|||||||
27671|Blowering Formation|22768|6|Mentioned|p174-75|||||||||
27671|Blowering Formation|22857|4|Described|p173, p452 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Dacitic volcanics. Contains graptolites, corals, conodonts, trilobites, crinoids. Geological Province: Tumut Trough.||||||
27671|Blowering Formation|23309|6|Mentioned|p390|||||||||
27671|Blowering Formation|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
27671|Blowering Formation|42045|4|Described|p153|||||||||
27671|Blowering Formation|42145|6|Mentioned|Table 1 P624|||||||||
27671|Blowering Formation|42313|1|Redefined|p115|Ludlovian||Age: mid Late Silurian (early middle Ludlovian)||||||
27671|Blowering Formation|42314|5|Briefly described|Map|Late Silurian|Middle Silurian|||||||
27671|Blowering Formation|42828|5|Briefly described|Table 1 P129|Late Silurian|Middle Silurian|||||||
27671|Blowering Formation|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv6||||||
27671|Blowering Formation|44093|5|Briefly described|p182 App. 1|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
27671|Blowering Formation|44192|5|Briefly described|Map Legend|Ludlovian|Llandoverian|||||||
27671|Blowering Formation|44936|5|Briefly described|Map Legend||Silurian|||||||
27671|Blowering Formation|50191|6|Mentioned|p6, 19|||Interfingers with or underlies: Honeysuckle beds.||||||
27671|Blowering Formation|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
27671|Blowering Formation|60280|5|Briefly described|p1|||Formerly included the rocks of the newly named unit, Brawlin Formation.||||||
27671|Blowering Formation|66197|5|Briefly described|p629, p631 Fig.3a|Ludlow|Ludlow|Shallow marine environment deposition. Tumut Trough.||||?underlies the Minjary Volcanics, overlies the Bumbolee Creek and Wyangle Formations.|Silicic volcanics and volcaniclastics.|14-MAR-12
27671|Blowering Formation|67060|5|Briefly described|p505 Table 1|Silurian|Silurian|Shown as S-type and of Wagga Batholith.|432.4 +/-4.3 U/Pb zircon  SHRIMP|||||
27671|Blowering Formation|68592|6|Mentioned|p451|||Gradational into Goobarragandra Volcanics to the east.||||||
27671|Blowering Formation|71708|5|Briefly described|p335|||||||In fault contact with central body of Coolac Serpentinite.|Dacites, associated sedimentary rocks.|
27671|Blowering Formation|73215|5|Briefly described|p994|||Tumut Trough.|430 +/- 2 Ma (Black, 2007).|||Is intruded by North Mooney Complex.|Includes leucogabbro and plagiogranite.|
27671|Blowering Formation|73483|5|Briefly described|p407-409|||Tumut Trough.|||Fences Creek beds, Fences Creek Conglomerate|Faulted against Jindalee Group|Metasedimentary and metavolcanic rocks.|
75836|Blue Knob Serpentinite|65317|6|Mentioned|p622 Fig. 1c|||||||||
82367|Blue Nobby Monzogranite|71628|4|Described|p3: 1, 10, 22-25|||Originally the Blue Knobby Adamellite of Binns et al. (1967). Subsequently Blue Knobby Monzogranite (Brown, 2003). The spelling is changed here to Blue Nobby Monzogranite because the local homestead, mountain and road appear thus in the Australian Gazetteer. Occurs as an E-W intrusion of c.10 km by c.3.5 km, ~28 km SE of Armidale and a similar distance ESE of Uralla. Crops out as low shelves and small boulders. Geochemistry described. Low magnetic response; moderate radiometric character.|296 +/- 3.3 Ma (SHRIMP: Rosenbaum et al., 2012).|Blue Nobby Suite.||Intrudes the Girrakool beds and Agnes Greywacke.|Grey, coarse-grained K-feldspar-rich biotite monzogranite, with small pods and dykes of leucocratic syenogranite; rare garnet; massive to foliated. S-type.|
81949|Bluff Mountain Trachyte Member|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Mount Naman Formation|||Flow-foliated, porphyritic, medium-grained, aegerine-arfvedsonite trachyte forming blocky outcrop.|02-NOV-20
24189|Boat Harbour Breccia|22773|6|Mentioned|p348|||||||||
24189|Boat Harbour Breccia|22857|5|Briefly described|p348|Miocene|Miocene|Volcanic breccias. Age: ~6.9Ma. On Lord Howe Island.||||||
24189|Boat Harbour Breccia|36958|3|Fully described|p160|||Massive, well-indurated breccia. Basaltic fragments in a fine grained matrix.||||||14-MAR-06
24189|Boat Harbour Breccia|61943|5|Briefly described|Map Legend|||Angular basaltic fragments in a massive fined grained matrix. Lord Howe Island.||||||
24189|Boat Harbour Breccia|73136|6|Mentioned|p190-191, p195|||Lord Howe Island. Composes Intermediate Hill. Deposited after the caldera of the original volcano collapsed. Shows the broadest range of lithologies and encompasses a wide range of coastal landforms.||||||
24189|Boat Harbour Breccia|73554|4|Described|Map legend, back of map|Neogene|Neogene|Lord Howe Island. Part of the Lord Howe Volcanic Complex. Likely a solidified slope or talus deposit. Intruded by many dykes of various compositions and textures, most of which strike toward Mount Lidgbird. Found in the Intermediate Hill area.||Lord Howe Volcanic Complex|||Breccia composed mostly of basaltic and other rock fragments (usually less than 10 cm, but locally up to 1 m) in a fine-grained matrix.|
24189|Boat Harbour Breccia|73581|6|Mentioned|p28 Fig.8|||||||||
77134|Bobelah Granite|69635|4|Described|p127-133, 134, 136, p69|Early Devonian|Early Devonian|North-western Lachlan Orogen.  U-Pb SHRIMP zircon magmatic crystallisation age.|417.1+/-2.0 Ma|Of Tarcoon Suite. ||Age indistinguishable from Sainsbury Park Granite,  Compton Downs Granite. Similar magnetic signature, I-type geochemistry + proximal to Compton Downs Granite.|Sample: weakly foliated quartz-biotite granite. I-type.|15-JUL-15
77134|Bobelah Granite|70602|5|Briefly described|p65-67,72|Early Devonian|Late Silurian|Aeromagnetic map data given.|417.1+/-2.0Ma|Tarcoon Plutonic Complex||Intrudes Girilambone Group.|I-type granite.|
77134|Bobelah Granite|70821|5|Briefly described|p9-10, p13 Tb.2.1|Early Devonian|Early Devonian||417.1 +/- 2.0 Ma (Fraser et al., 2014).||||Includes granodiorite.|01-DEC-16
77134|Bobelah Granite|71345|5|Briefly described|p6-7|Early Devonian|Early Devonian|Geochemically, petrologically and in age similar to the Compton Downs Granite (~10km to the SE; Blevin 2011), suggesting they are separate plutons from the same magmatic reservoir.||Unit of Tarcoon Suite.||||
77134|Bobelah Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: hammer-shaped area of moderate magnetic intensity with a band of very high amplitude across the northern margin. Associated dykes have been interpreted.||Tarcoon Plutonic Complex.|||Biotite granite, altered and deformed locally.|
77134|Bobelah Granite|72296|6|Mentioned|p6|Devonian|Devonian|||||Intrudes the Girilambone Group (presumably: no contacts observed).||
77134|Bobelah Granite|72522|4|Described|p1, p10, p13, p16, p29, p133.|Lochkovian|Lochkovian|Magmatic age by Fraser et al., 2014.|417.1 +/- 2.0 Ma|Tarcoon Suite||||
79359|Boblegigbie Granite|70777|4|Described|p1-p4, p9-p11, p13-p15, p80, p96|Lochkovian|Lochkovian|Lachlan Orogen. Age provided is interpreted as the age of magmatic crystallisation. Petrography and zircon description are provided in detail. Time equivalent and may be a high level intrusion associated with the Walleroobie and Gurragong Volcanics. Sample location and map sheet are provided.|418.8 +/- 2.2 Ma  (SHRIMP, this volume)||||Porphyritic granite with abundant euhedral phenocrysts of alkali feldspar in a fine-grained quartzofeldspathic groundmass.|
79359|Boblegigbie Granite|72083|5|Briefly described|p20, p38|Devonian|Devonian|Trigg (2016). A few outcrops discovered W of the Newell Highway in 2016 indicates it forms NE-trending elongate bodies (?dykes) in the Rosemorder Granite in that area.||||Possibly intrudes Rosemorder Granite.|Porphyritic granite.|
25796|Bobs Creek Formation|721|5|Briefly described|Map legend|Late Devonian|Silurian|Of the Woolomin Group.  Low-grade, regionally metamorphosed, multiply deformed cherts and green siliceous mudrocks.||||||21-DEC-04
25796|Bobs Creek Formation|22857|5|Briefly described|p484 App.1 Tb.A1.6|Late Devonian|Middle Silurian|Of the Woolomin Group. Cherts and green siliceous mudrocks. Geological Province: Woolomin Basin.||||||09-MAR-06
25796|Bobs Creek Formation|23050|4|Described|p15 Table 1|Late Devonian|Silurian|Age: Middle Silurian to Late Devonian based on Radiolaria.||||||
25796|Bobs Creek Formation|23051|5|Briefly described|Map Legend|Late Devonian|Late Silurian|of Woolomin Group.||||||
25796|Bobs Creek Formation|41328|2|Defined|p13|Early Carboniferous|Middle Devonian|Reserved as Bobs Creek.||||||26-JUL-04
25796|Bobs Creek Formation|41329|5|Briefly described|p5|||||||||
25796|Bobs Creek Formation|42554|5|Briefly described|p38|||||||||
25796|Bobs Creek Formation|42629|6|Mentioned|p363|||||||||
25796|Bobs Creek Formation|42748|6|Mentioned|Fig.3 P9|Devonian||||||||
25796|Bobs Creek Formation|43091|5|Briefly described|Map legend|||of Woolomin Group||||||
25796|Bobs Creek Formation|65398|1|Redefined|p4 Fig.2, p5 Tb.1, p8,14, Fig 2-3|Late Devonian|Late Silurian|Of the Woolomin Group. Low-grade regionally metamorphosed, multiply deformed argillite, siliceous argillite, local thinly bedded chert, and minor wacke, jasper and mafic volcanic rocks.||||||
25796|Bobs Creek Formation|66720|5|Briefly described|Map legend|Late Devonian|Late Silurian|||Unit in Woolomin Group.|||Massive to well-bedded siliceous argillite; minor chert, jasper; rare basalt.|
25796|Bobs Creek Formation|68003|5|Briefly described|p140.|Devonian|Silurian|||Unit in Woolomin Group.|||Low grade regionally metamorphosed, multiply deformed thinly-bedded chert, mudstone, wacke, basic volcanics and rare limestone.|
25796|Bobs Creek Formation|68005|4|Described|pp26-28, p29 Photo.3-C, p156, p170.|Early Carboniferous|Middle Devonian|Central Block, New England Fold Belt. Low radiometric response; magnetic response is lower than Nangahrah Formation. Text says age is from radiolarian data; Appendix 4 gives age as Silurian with no further explanation..||Unit in Woolomin Group.||Overlies Nangahrah Formation, gradationally to thrust fault contact. Is overlain by Cara Formation.|Moderately deformed; metabasalts overlain by ribbon bedded and radiolarian chert, in turn overlain by a distinctive sequence of argillites and cherts.|
25796|Bobs Creek Formation|71628|5|Briefly described|p4:17|||||Woolomin Group.||Is intruded by Copeton Monzogranite.||
23398|Bocobidgle Conglomerate|22831|3|Fully described|p 34|Wenlockian|Wenlockian|Forbes Group||||||
23398|Bocobidgle Conglomerate|22857|4|Described|p450 App.1, Tb.A1.6|Wenlockian|Wenlockian|Of the Forbes Group. Cobble conglomerate to medium sandstone, limy beds; contains corals. Max. thickness: <200m. Geological Province: Bogan Gate Terrace.||||||
23398|Bocobidgle Conglomerate|24125|5|Briefly described|p3|Silurian|Silurian|Of the Forbes Group.  Geological Province: Lachlan Fold Belt.||||||
23398|Bocobidgle Conglomerate|24417|3|Fully described|p42|Wenlock|Wenlock|Of Forbes Group.  Overlain by Mumbidgle Formation; overlies Cotton Formation.  Max. thickness:  300m; 160m at type-section.||||||
23398|Bocobidgle Conglomerate|40891|2|Defined|p14|Middle Silurian|Middle Silurian|||||||
23398|Bocobidgle Conglomerate|42489|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
23398|Bocobidgle Conglomerate|43441|5|Briefly described|24|||Now includes Burrandong Creek Member. Formerly regarded as part of Goonumbla Volcanics.||||||08-JAN-10
23398|Bocobidgle Conglomerate|44160|5|Briefly described|Map Legend||Ludlovian|||||||08-JAN-10
23398|Bocobidgle Conglomerate|46522|2|Defined|p58|Middle Silurian||||||||
23398|Bocobidgle Conglomerate|46525|6|Mentioned|Fig.1 P143|||||||||
23398|Bocobidgle Conglomerate|46528|5|Briefly described|Map legend|Silurian||||||||
23398|Bocobidgle Conglomerate|50299|5|Briefly described|Map Legend|Silurian|Silurian|Of the Forbes Group.||||||
23398|Bocobidgle Conglomerate|60009|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Forbes Group. Underlies: Mumbidgle Formation.||||||13-JUL-04
23398|Bocobidgle Conglomerate|63290|5|Briefly described|p395|Late Silurian|Late Silurian|Of Forbes Group. Contains clasts of chert and quartzite. Geological Province: Junee - Narromine Volcanic Belt.||||||
36110|Bodalla Monzogranite|23439|6|Mentioned|p125|||||||||
36110|Bodalla Monzogranite|23549|5|Briefly described|p521|||Of the Moruya Suite.  Felsic granites mostly. - virtually free of encalves and is a very homgeneous pluton with a finer grain size than other rocks of the Moruya Suite.||||||05-APR-05
42412|Bodonga beds|23811|5|Briefly described|Map legend|Early Permian|Early Permian|Here described as undifferentiated Bodonga beds - ortho- and paraconglomerate, lithic sandstone and minor siltstone, locally fossiliferous; commonly weakly metamorphosed.||||||
42412|Bodonga beds|44093|5|Briefly described|p238 App. 1|Early Permian|Early Permian|Age: Late Early Permian. Shelfal sediments. Geological Province: New England Fold Belt.||||||
42412|Bodonga beds|63733|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic, locally pebbly arenite, clast to matrix supported sandy to muddy conglomerate, locally pebbly mudstone; minor siltstone; rare limestone and basalt.||||||11-DEC-07
31620|Bogalong Suite|24417|3|Fully described|p99|Early Devonian|Early Devonian|Intrudes the Kirribilli Formation.  Formerly referred to as "Bogalong Granite".||||||
31620|Bogalong Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31620|Bogalong Suite|60009|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Mortray Hill Granite Complex, Milroy Granite.||||||13-JUL-04
27715|Boggy Plain Granitic Complex|40882|5|Briefly described|p25, Fig.2 p26|||||||||
27715|Boggy Plain Granitic Complex|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|gah12 - adamellite phase, ggh25 - granodiorite phase.||||||
27715|Boggy Plain Granitic Complex|60078|6|Mentioned|Map Legend|Devonian|Late Silurian|Granodiorite phase.||||||
27715|Boggy Plain Granitic Complex|68592|5|Briefly described|p1397|||Wyborn et al. (1987) after Wyborn (1983). The type pluton for their Boggy Plain Supersuite. Named after Boggy Plain and Boggy Plain Creek.||||||
23400|Boginderra Granite|22638|4|Described|p74||Late Devonian|New name.||||||
23400|Boginderra Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
23400|Boginderra Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
23400|Boginderra Granite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
23400|Boginderra Granite|71206|6|Mentioned|p373, 384|||Lachlan Fold Belt.||Narraburra Suite.||||
23400|Boginderra Granite|72084|6|Mentioned|p55 Fig.57|||A-type geochemical discrimination diagrams.||||||
79858|Bogolong Formation|71889|5|Briefly described|p8, p48-p49|||Originally defined by Trigg (2017). Obsolete name as it is recognised in this study as a southerly continuation of the Confreys Formation.||Cocoparra Group||Overlies the Barrat Formation. Overlain by the Narrandera Sandstone. Equivalent to the Confreys Formation.||
79858|Bogolong Formation|72083|3|Fully described|p7, p39-41, p43-46|||New name, after Bogolong Hills; a subdivision of previously undifferentiated Cocoparra Group. Stratigraphy doubtful: this unit, as well as the Narrandera Sandstone, may be parts of the Barrat Formation; discussed. A thin, laterally extensive, recessive unit; forms distinctive valleys; distribution described. The type area is on private property around GR 473140 6160000 (Narrandera 1:100K sheet). Floodplain deposits flanking a braided stream channel. Differentiated from over and underlying units by lack of pebbles and conglomerate and is generally finer grained and thinly bedded.||Cocoparra Group.||Overlies Barrat Formation. Is overlain conformably by Narrandera Sandstone. Probable correlative of Hazeldene Sandstone (brief comment).|Mostly red-purple, fine- to medium-grained quartzose sandstone, locally micaceous; typically thin- to medium-bedded; local well-developed ripple marks characteristic.|31-AUG-19
31481|Bogong Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains the Killimicat and Bogong Granites.||||||08-FEB-05
31481|Bogong Suite|44093|5|Briefly described|p184 App. 1|Early Devonian|Early Devonian|See also Bogong Suites p183 Appendix 1. Of Boggy Plain Supersuite. Geological Province: Lachlan Fold Belt.||||||08-APR-05
74588|Bogungra Dacite Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tangerang Fm (Bindook Gp). Greenish-grey, massive, medium-grained porphyritic intrusive dacite composed of plagioclase, ferroan enstatite, augite and minor quartz phenocrysts set in a finely granophyric groundmass.||||||16-JUN-08
74588|Bogungra Dacite Member|68592|1|Redefined|p1061, p1109-12, p1610-1, p1632|Early Devonian|Early Devonian|New name. Originally distinguished as a pluton of undifferentiated Marulan Batholith by Hall (1981). Defined by Jones, Hall et al. (1986) as Bogungra Microtonalite. Here (Thomas and Pogson, 2012) redefined as the Bogungra Dacite Member of the Tangerang Formation on the basis of textural and compositional similarities with the Carne Dacite Member. Type locality described. c.800-1000m thick. Also similar to Jemidee Microgranodiorite. Geophysical properties described.||Unit in Tangerang Formation.||Truncated by Torwood Granodiorite. Correlative of Carne Dacite Member.|Grey-green to pinkish-green, uniformly fine- to medium-grained, dacite sill.|
74588|Bogungra Dacite Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dkto. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Tangerang Formation||Is overlain by Joaramin Ignimbrite (of Bindook Group). Overlies unnamed member near middle of Tangerang Formation.|Massive, medium-grained, porphyritic intrusive dacite composed of plagioclase, augite and minor quartz phenocrysts set in a finely granophyric groundmass.|
74588|Bogungra Dacite Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Tangerang Formation|||Massive, medium-grained, porphyritic intrusive dacite composed of plagioclase, augite and minor quartz phenocrysts set in a finely granophyric groundmass.|
74588|Bogungra Dacite Member|70661|6|Mentioned|p55|||||||||
79331|Bohena Coal Member|70791|5|Briefly described|p275-276, p283, p285-289, p291-294|Cisuralian|Cisuralian|New name. Mullaley Sub-basin. 3-18m thick. Isopachs. Borehole cross-sections and long-sections; correlations. Marks the boundary between palynological zones APP31 and APP32. Coal properties described. In situ coal estimates.||||Is correlated with Faithful Coal Member.||
23401|Bold Slate Granite|22815|4|Described|p87|||||||||
23401|Bold Slate Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
23401|Bold Slate Granite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
38267|Bolivia Range Leucomonzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Inhomogeneous, pink granite varying from medium-grained leucomonzogranite to porphyritic and coarse-grained granite with rapikivi texture; microgranite also present; miarolitic cavities abundant in places.  An I-type granitoid.||||||20-DEC-04
38267|Bolivia Range Leucomonzogranite|23812|5|Briefly described|p19 Fig.2|Triassic|Triassic|Age: 254Ma.||||||
38267|Bolivia Range Leucomonzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca. 241 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38267|Bolivia Range Leucomonzogranite|69639|4|Described|p2, p5, p8, p26-p31|Anisian|Anisian|New England Orogen. Sampling locality, petrography and geochronology are discussed. See also p51, p80, p221, p235-p236.|247.7 +/- 1.5 Ma (SHRIMP)|Bolivia Range Suite||Intrudes the Wandsworth Volcanic Group.|Coarse-grained, massive and underformed, alkali feldspar-rich, leucocratic granite.|
38267|Bolivia Range Leucomonzogranite|70217|5|Briefly described|v, p49, p74 tbl 14.1, p75|Olenekian|Olenekian|New England Orogen. SHRIMP ages are derived from Chisholm et al, 2014b.|247.7 +/- 1.5 Ma (SHRIMP U-Pb)|Stanthorpe Supersuite||Intrudes the Pyes Creek Leucomonzogranite.||
38267|Bolivia Range Leucomonzogranite|71628|4|Described|p15: 1-2, 8-12, 22, 24-25|||Henley et al. (2001) after unpublished work by Barnes (1987). Named after Bolivia Hill. Occurs just S of Bolivia locality, ~37 km S of Tenterfield. Resistant to weathering (forms a hill ~350m in elevation) and has excellent exposures as pavements and tors. Geochemistry described. Source of 11 occurrences of Mo-dominant mineralisation (listed), and associated with Sn and base-metal mineralisation (probably sourced from Mole Leucogranite). RELATED UNITS (continued): Is faulted against Pyes Creek Leucomonzogranite.|247.7 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Bolivia Range Suite.||Intrudes Dundee Rhyodacite and undifferentiated Wandsworth Volcanic Group, Yarramundi Andesite Member and Welcome Volcanic Member. Is intruded by Pyes Creek Leucomonzogranite. See COMMENTS for more.|Texturally heterogeneous, pink to flesh coloured, medium- to coarse-grained, K-feldspar-rich leucomonzogranite, and rarely leucosyenogranite; porphyritic, rapakivi and microgranite variants. I-type.|
73987|Bolivia Range Suite|69639|5|Briefly described|p20-21, p26, p50, p62, p80, p87, p221|||New England Orogen.||Stanthorpe Supersuite|Includes the Bolivia Range Leucomonzogranite, Dandahra Creek Leucogranite, Billyrimba Leucomonzogranite, Sandy Flat Monzogranite, and the Mount Jonblee Leucomonzogranite.|||
73987|Bolivia Range Suite|70217|6|Mentioned|p66|||New England Orogen.||Stanthorpe Supersuite|Includes the Dandahra Creek Leucogranite|||
73987|Bolivia Range Suite|71628|5|Briefly described|p11-11; p14-1; p15: 1-2, 4-25, 29, 111|Middle Triassic|Early Triassic|See also p15: p19: 142, 144. Chisholm et al. (2014) assigned Bungulla Monzogranite to this Suite and Supersuite; reassigned in this study to the Bungulla Suite and Supersuite. Geochemistry briefly summarised.|256-241 Ma.|Stanthorpe Supersuite.|Billyrimba, Bolivia Range, Nonnington, Pyes Creek, Leucomonzogranites; Deepwater Syenogranite; Mount Mackenzie Monzogranite.|||
31536|Bombala Suite|22878|6|Mentioned|p74|||Tonghi Supersuite||||||
31536|Bombala Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31536|Bombala Suite|44093|5|Briefly described|p204 App. 1|Devonian|Silurian|Orogenic granite. See also p218 Appendix 1. Geological Province: Lachlan Fold Belt.||||||
77132|Bombala Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
32182|Bombala Tonalite|22815|4|Described|p84|||||||||
32182|Bombala Tonalite|23329|5|Briefly described|1042|Pridoli|Ludlow|419-413Ma||||||
32182|Bombala Tonalite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Kelvin Suite.||||||
24744|Bombay Volcanics|12185|5|Briefly described|map legend|Silurian|Silurian|Rhyolite, sandstone, conglomerate, siltstone. BMR map symbol: Svb.||||||
24744|Bombay Volcanics|22768|6|Mentioned|p176|||||||||
24744|Bombay Volcanics|22857|6|Mentioned|p176|||Submarine felsic volcanics.||||||
24744|Bombay Volcanics|24116|5|Briefly described|p81|||||||||
24744|Bombay Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
24744|Bombay Volcanics|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
24744|Bombay Volcanics|30735|2|Defined|p34|Silurian|Silurian|See alsp P35||||||
24744|Bombay Volcanics|30736|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
24744|Bombay Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
24744|Bombay Volcanics|31161|5|Briefly described|PA7|||||||||
24744|Bombay Volcanics|31411|5|Briefly described|p16|||||||||
24744|Bombay Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
24744|Bombay Volcanics|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
24744|Bombay Volcanics|33325|6|Mentioned|p14|||||||||
24744|Bombay Volcanics|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
24744|Bombay Volcanics|35503|6|Mentioned|p201|||Defined in Felton and Huleatt (1977)||||||
24744|Bombay Volcanics|36413|6|Mentioned|Table 3|||||||||
24744|Bombay Volcanics|37727|4|Described|p39|||See also P18 and P21||||||
24744|Bombay Volcanics|40276|6|Mentioned|p6|||||||||
24744|Bombay Volcanics|40328|4|Described|p184|||Mention P17||||||
24744|Bombay Volcanics|68592|6|Mentioned|p725-6|||Superseded. Long Flat Volcanics and 'Bombay Volcanics' were included by Felton and Huleatt (1977) and Wyborn and Owen (1986) in Mount Fairy Group in Braidwood and Araluen 1:100 000 map sheet areas. However, recent mapping (Fitzherbert et al. 2011) and age dating (Bodorkos and Simpson 2008) has combined Long Flat Volcanics and 'Bombay Volcanics' and placed them in Bindook Group.||||||
24744|Bombay Volcanics|71069|6|Mentioned|p134|||Discontinued and constituent rocks placed within the Bindook Group.||||||
70102|Bomera Conglomerate Member|22857|5|Briefly described|p518 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Digby Formation. Max. thickness: 113m. Geological Province: Gunnedah Basin.||||||
70102|Bomera Conglomerate Member|43194|5|Briefly described|p133 App. 1|Early Triassic|Early Triassic|Newly defined member within the Digby Formation. Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||
70102|Bomera Conglomerate Member|68003|5|Briefly described|p42.|Early Triassic|Early Triassic|Southeastern Gunnedah Basin. Thick conglomerate sequences formed by large alluvial fans, generated by erosion in the uplifted New England Fold Belt.||Unit in Digby Formation.||||
70033|Bondo Ankaramite|61819|5|Briefly described|p92|||A lava rock of doleritic appearance with large pyroxene, plagioclase and olivine crystals.||||||
34930|Bone Cave breccia unit|22952|6|Mentioned|p178,Table1p179|||||||||
27113|Bongalaby Formation|22857|4|Described|p472 App.1 Tb.A1.6|Middle Devonian|Early Devonian|Of the Mulwaree Group. Thinly bedded calcareous arenite and siltstone, limestone; minor rhyolite. Max. thickness: 200m. Geological Province: Captains Flat-Goulburn Trough.||||||
27113|Bongalaby Formation|23048|5|Briefly described|p7||Early Devonian|||||||
27113|Bongalaby Formation|30730|6|Mentioned|p10|||Geological map||||||
27113|Bongalaby Formation|30735|2|Defined|p47|Devonian|Devonian|||||||
27113|Bongalaby Formation|30736|6|Mentioned|Map legend|Devonian|Devonian|||||||
27113|Bongalaby Formation|35503|6|Mentioned|p201|||Defined in Felton and Huleatt (1977)||||||
27113|Bongalaby Formation|39331|6|Mentioned|p57|||||||||
27113|Bongalaby Formation|66498|6|Mentioned|p43, 45|Emsian|Emsian|Braidwood area.||||||
27113|Bongalaby Formation|69159|5|Briefly described|Map legend|Emsian|Pragian|||Unit in Mulwaree Group.|Includes Lake Bathurst Limestone Member.|Overlies Tarago Conglomerate.|Maroon to red, immature, moderately to porly sorted, feldspar-quartz-lithic volcaniclastic sandstone, pebbly granulestone and minor clast-supported conglomerate; interbedded with siltstone, thin beds of fossiliferous limestone and limestone breccia.|07-SEP-15
27113|Bongalaby Formation|71656|4|Described|p12 Fig.2, p40, p41|Emsian|Pragian|Some conodont elements are fragmented and that hinders identification, but conodonts support correlation with Taemas Formation. Turbulent shallow marine environment. Clastic facies in Braidwood area includes fragments of primative terrestrial plants.||Mulwaree Group|Includes Lake Bathurst Limestone Member.|Overlies Tarago Conglomerate.|Fossiliferous limestone. Also includes reddish purple siltstone to pale greenish grey silty mudstone in Braidwood area.|
27113|Bongalaby Formation|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Mulwaree Group.|Lake Bathurst Limestone Member.||Maroon to red, moderately to poorly sorted feldspar-quartz-lithic volcaniclastic sandstone, pebbly granulestone and minor clast-supported conglomerate interbedded with siltstone; thin beds of fossiliferous limestone and limestone breccia.|
27113|Bongalaby Formation|71700|3|Fully described|vi, p7, p27, p48-p49, p52, p63, CD|Emsian|Pragian|Named for the property of Bongalaby near GR 741450 6122529 not to be confused with Bongaralaby Creek. Two representative sections exist, one ranging from 740800 6121250 to GR 740850 6121850; another ranging from 740900 6120675 to 740565 6120895. Rocks mapped as Tarago Conglomerate by Felton and Huleatt (1975) are now interpreted to be part of this unit instead. Distribution, geomorphic expression, outcrop,  depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils, distinguishing features, economic geology and geological hazards are discussed.  This unit has a minimum original thickness of 800m as not stratigraphic top has been found. Lithology is discussed in detail. Age is derived from fossil assemblage. This unit may be equivalent to the Cavan Bluff Limestone of the Murrumbidgee Group. ||Mulwaree Group|Includes the Lake Bathurst Limestone Member.|Conformably overlies the Tarago Conglomerate. Unconformably overlies the Covan Creek Formation and Adaminaby Group. Conformably overlain by the Lake Bathurst Limestone Member.|Maroon to red, immature, moderately to poorly sorted, feldspar-quartz-lithic volcaniclastic sandstone, pebbly granulestone and minor clast-supported conglomerate interbedded with siltstone.|
27717|Bonnington Siltstone|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Thinly to medium-bedded siltstone. and cherty mudstone; minor interbeds of fine sandstone and friable mudstone. Conformably overlies Ararat Formation; conformably overlain by Flagstaff Formation. Max. thickness: 260m. Geol. Prov.: Tamworth Forearc Basin.||||||
27717|Bonnington Siltstone|24121|5|Briefly described|p4, p86||Carboniferous|||||||25-AUG-22
27717|Bonnington Siltstone|31228|4|Described|p77|||See also P76||||||
27717|Bonnington Siltstone|31519|6|Mentioned|Fig. 1|||||||||
27717|Bonnington Siltstone|32527|6|Mentioned|p403|||Refers Roberts & Oversby (1973)||||||
27717|Bonnington Siltstone|32866|6|Mentioned|p8|||Fossil content||||||
27717|Bonnington Siltstone|32867|6|Mentioned|p66|||||||||
27717|Bonnington Siltstone|32869|5|Briefly described|p169|||Depositional environment. See also Fig.2 & Fig.3B||||||
27717|Bonnington Siltstone|36599|6|Mentioned|Fig.1|||||||||
27717|Bonnington Siltstone|37068|6|Mentioned|p59|||||||||
27717|Bonnington Siltstone|40883|6|Mentioned|p7|||||||||
27717|Bonnington Siltstone|42547|4|Described|p29|||||||||
27717|Bonnington Siltstone|44093|5|Briefly described|p229 App. 1|Visean|Tournaisian|Geological Province: New England Fold Belt.||||||
27717|Bonnington Siltstone|44244|2|Defined|p59|Visean|Visean|Conformably overlies Ararat Formation; conformably underlies Flagstaff Formation.  Max. thickness: >460m.  Type section in text.  Geological Province: Gresford Block.||||||13-JUL-04
27717|Bonnington Siltstone|45088|5|Briefly described|p63|||Correlation. Fauna P7||||||
27717|Bonnington Siltstone|45097|6|Mentioned|p25|||Brachiopods. Carboniferous correlation chart||||||
27717|Bonnington Siltstone|45169|6|Mentioned|p1|||||||||
27717|Bonnington Siltstone|46803|6|Mentioned|p145|||Refers Jones et al. (1973). See also Fig. 3||||||
27717|Bonnington Siltstone|47056|6|Mentioned|Fig.2 P523|||||||||
27717|Bonnington Siltstone|50147|5|Briefly described|Map legend|Visean|Visean|Grey, thinly bedded siliceous siltstone, cherty mudstone, and minor lithic sandstone. Geological Province: Gresford Block||||||
27717|Bonnington Siltstone|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Gresford Block, Tamworth Belt.||||||
77320|Bonshaw Member|68005|5|Briefly described|pp37-39.|Early Permian|Early Permian|Contains the Bonshaw seam and its splits; carbonaceous claystone and thin coal layers, with little or no economic significance. 50 m thick.||Middle unit in Ashford Coal Measures.||Overlies the Ashford Member. Is overlain by the Bukkulla Member.|Mainly coarse sandstone, conglomerate and interbedded layers of fine sediments including carbonaceous shale with rare, thin coal plies.|
78892|Booda Formation|69635|5|Briefly described|p139-155, p69|Ordovician||Southern Thomson Orogen. U-Pb SHRIMP zircon maximum depositional age. Informally called Mount Oxley turbidite. Detrital zircon spectra similar to Ordovician turbidites of Lachlan Orogen.|495+/-9 Ma; 501+/-7 Ma|||Unconformably overlain by Moira Formation, Mulga Downs Group.|Sample 1: cleaved feldspathic sandstone, comes from a ~20 cm thick coherent sandy bed within strongly cleaved and folded phyllites (turbidite sequence). Sample2: quartz-rich, coarse-grained, moderately east-dipping metasandstone bed.|
78892|Booda Formation|70602|5|Briefly described|p66|Middle Ordovician|Late Cambrian|North of the Louth-Eumarra Shear Zone. Previously mapped as Girilambone Group. Geochronology by Fraser et al. (2014).|495+/-9Ma Max deposition age.|||Unconformably underlies Moira and Mount Oxley Formations, Mulga Downs Group. Potential correlative of Girilambome Group.|Interbeds of metasiltstone and fine- to medium-grained metasandstone with a potential turbiditic origin.|27-JUN-16
78892|Booda Formation|71360|5|Briefly described|Map legend|Paleozoic|Paleozoic|Mapped and described as part of a unit labelled "Mount Oxley area metasedimentary rocks". Geophysical signature: broad zone of non-magnetic metasedimentary rocks with minor linear NNE trends of elevated magnetic intensity parallel to the regional structural fabric. Age also given as "possible Late Ordovician".|||||Siltstone, sandstone, possible crystal tuffs.|
78892|Booda Formation|71965|6|Mentioned|p903|||Geological province: Thomson Orogen. Mapped by Dunstan et al. (2016) on the flanks of Mount Oxley. Fraser et al. (2014) provided two MDAs of c. 501 and c. 495 Ma.|||||Steeply dipping, cleaved, siliciclastic siltstone and sandstone, possibly of turbiditic origin.|
78892|Booda Formation|72522|4|Described|p1, p5 Tb.1.1, p18-23.|Middle Devonian|Cambrian|Thomson Orogen. Age poorly constrained by unconformably overlying units. May be equivalent to younger parts of the Ordovician Girilambone Group. Maximum depositional age derived from SHRIMP U-Pb methods. Previous max. dep. ages determined for this unit: 495+/-9 Ma, 501+/-7 Ma.|494 +/- 7 Ma 206Pb/238U (204Pb-corrected)|||Unconformably underlies Moira Formation and the Mulga Downs Group.|Dated sample is moderately weathered grey to beige, very fine to fine-grained, quartz-rich sandstone interbedded with siltstone. Steeply dipping cleaved and folded phyllites at Mount Oxley.|
73824|Bookookoorara Monzogranite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Grey , medium- to fine-grained (marginal zone), moderately to highly porphyritic (titanite-) hornblende-biotite monzogranite; locally granophyric; with mafic inclusions to ~10cm; moderate magnetic response.||||||11-DEC-07
73824|Bookookoorara Monzogranite|63748|6|Mentioned|p36|||Supersedes Bookookoorara Adamellite.||||||07-FEB-11
73824|Bookookoorara Monzogranite|68111|5|Briefly described|p969-972 Figs.2,4, Table 1; p974|Ladinian|Anisian|Large pluton. Dating detailed.|240.1 +/- 2.4 Ma, U-Pb SHRIMP (Li et al. 2012).|||||
73824|Bookookoorara Monzogranite|69639|4|Described|p2, p6, p8-p9, p157-p163, p222, p239|Triassic|Triassic|New England Orogen. Sampling locality, petrography and geochronology are discussed. Geochemically similar to the Bungulla Monzogranite and Undercliffe Falls Monzogranite.|249.8 +/- 1.3 Ma (SHRIMP U-Pb)|Bungulla Suite||Intruded by the Stanthorpe Granite.|Grey-pink, strongly porphyritic biotite monzogranite with a medium-fine grained groundmass.|
73824|Bookookoorara Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Olenekian|Induan|New England Orogen.|249.8 +/-1.3 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
73824|Bookookoorara Monzogranite|71592|5|Briefly described|Appendix A.|||New England Orogen.|250+/-1.3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
73824|Bookookoorara Monzogranite|71628|4|Described|p11: 1, 4-7, 14, 36, 45; p15: 33, 52, 57|||See also p15: 62-63, 68; p19: 20-22. Donchak et al. (2007) after Brown et al. (2001). Previously the Bookookoorara Creek body of the Bookookoorara Adamellite (Thomson, 1973, 1976). Named after a local creek. The c.3 x 5 km intrusion occurs ~20 km SE of Stanthorpe. Other age determinations given. Petrology and geochemistry described.|249.8 +/- 1.3 Ma (SHRIMP: Chisholm et al., 2014).|Bookookoorara Suite.||Is bounded by Jenners and Mount Lindesay Monzogranites (Stanthorpe Complex).|Grey, medium-grained, moderately to highly porphyritic hornblende-biotite monzogranite with fine-grained margins; locally granophyric. I-type.|
24748|Boolahbone Granite|22768|6|Mentioned|p170|||||||||
24748|Boolahbone Granite|22857|6|Mentioned|p170|||||||||05-NOV-07
24748|Boolahbone Granite|22887|5|Briefly described|p29|||Strong magnetic signature.||||||
24748|Boolahbone Granite|23252|5|Briefly described|Map Legend|||Actually refers to Boolahbone Granite equivalent.||||||
24748|Boolahbone Granite|29987|5|Briefly described|p14|||||||||
24748|Boolahbone Granite|34449|6|Mentioned|Table 2-1|||||||||
24748|Boolahbone Granite|37772|5|Briefly described|p8|||||||||
24748|Boolahbone Granite|39627|6|Mentioned|Table 3|||||||||
24748|Boolahbone Granite|40269|4|Described|p141|||||||||
24748|Boolahbone Granite|40328|4|Described|p203|||||||||
24748|Boolahbone Granite|40913|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
24748|Boolahbone Granite|41126|2|Defined|p82|Early Devonian|Early Devonian|||||||
24748|Boolahbone Granite|41528|6|Mentioned|p98|||||||||
24748|Boolahbone Granite|41821|6|Mentioned|p24|||In Mount Allen sheet area.||||||03-JUN-08
24748|Boolahbone Granite|42313|6|Mentioned|p219|||||||||
24748|Boolahbone Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
24748|Boolahbone Granite|43089|5|Briefly described|Map Legend|||||||||
24748|Boolahbone Granite|43757|6|Mentioned|p510|||||||||
24748|Boolahbone Granite|63891|5|Briefly described|p240, p243 Fig. 3.|||Exposed. Intrudes a local rhyolite and nonvolcanic conglomerate, and exhibits common graphic (granophyric) textures, suggesting shallow crystallisation. Composed entriely of graphic textures of myrmekite and minor granophyre. ||||||
24748|Boolahbone Granite|70751|5|Briefly described|p4, 6, 8, p11, p28, p31, p38|Silurian|Silurian|An additional date of 415.8 +/- 3.1 Ma is derived from this study. SHRIMP dates are derived from zircon. Spatially associated with magmatic-related mineralisation.|420 +/- 2.5 Ma (SHRIMP, Black, 2007)|||Intrudes the Mount Kennan Volcanics.|Felsic A-type granitic rocks.|24-SEP-19
24748|Boolahbone Granite|71039|5|Briefly described|p15, p21, p26|Devonian|Silurian|Contact metamorphosed the Northwestern Amphitheatre Group. 415.8 Ma age is derived from Downes et al, 2016.|420 +/- 2.5 Ma, Black, 2007; 415.8 +/- 3.1 Ma|||Intrudes the Amphitheatre Group.|A-type granite.|09-MAR-23
24748|Boolahbone Granite|71693|5|Briefly described|Map legend.|Devonian|Devonian||||||A-type. Biotite-graphic granite, biotite-graphic monzogranite with secondary muscovite, and minor porphyritic biotite microgranodiorite. Primary feldspars and ferromagnesians typically moderately to strongly altered.|
24748|Boolahbone Granite|72908|6|Mentioned|p14|Lochkovian|Lochkovian||415+/-3.1 Ma U-Pb SHRIMP zircon|||||
24748|Boolahbone Granite|72951|5|Briefly described|p1013, 1015-1016|Lochkovian|Pridoli|Lachlan Orogen. Albury-Bega Terrane. A-type granite. SHRIMP U-Pb zircon isotope analyses from Black (2007). eHf = -7.2 +/- 1.2, and d18O = 9.72 +/- 0.26.|420.0 +/- 2.4 Ma, 420.0 +/- 2.5 Ma||||Granodiorite.|
24748|Boolahbone Granite|72958|6|Mentioned|p11|Lochkovian|Lochkovian|Cobar Basin. Nymagee area.||||||
23408|Boolambayte Formation|22736|6|Mentioned|p628 Fig7||Visean|||||||
23408|Boolambayte Formation|22857|4|Described|p500 App.1 Tb.A1.7|Visean|Visean|Sandstones and siltstone. Max. thickness: 1370m. Geological Province: Tamworth Forearc Basin.||||||
23408|Boolambayte Formation|36057|2|Defined|p346|Visean|Visean|Prob. Visean||||||
23408|Boolambayte Formation|36528|6|Mentioned|p178|||||||||
23408|Boolambayte Formation|39660|6|Mentioned|p449|||||||||
23408|Boolambayte Formation|40883|6|Mentioned|p7|||Mention Fig.2||||||
23408|Boolambayte Formation|42547|4|Described|p34|||||||||
23408|Boolambayte Formation|44093|5|Briefly described|p231 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
23408|Boolambayte Formation|44244|2|Defined|p200|Visean|Visean|Overlies Kataway Mudstone; underlies Nerong Volcanics.  Max. thickness: 1370m.  Type section in text.  Geological Province: Myall Block.||||||27-JUL-04
23408|Boolambayte Formation|47056|6|Mentioned|Fig.2 P523|||||||||
23408|Boolambayte Formation|50132|5|Briefly described|p248  Fig.6|Namurian|Namurian|Early Namurian age||||Overlies the Kataway Mudstone. Underlies the Nerong Volcanics.||27-MAR-12
23408|Boolambayte Formation|50263|5|Briefly described|Map Legend|Visean|Visean|Underlies: Nerong Volcanics. Geological Province: Eastern Myall Block.||||||
23408|Boolambayte Formation|63832|6|Mentioned|P131 Fig.2|Visean|Visean|Eastern Myall block, Southern New England Fold Belt.||||||
23408|Boolambayte Formation|64631|5|Briefly described|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt: eastern Myall Block. Biostratigraphic age control for base.||||Overlies Kataway Mudstone.||
23408|Boolambayte Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Myall Block, Tamworth Belt.||||||
24749|Boomerang Creek Gneiss|34544|6|Mentioned|p187|||Cordierite-bearing||||||
24749|Boomerang Creek Gneiss|40328|4|Described|p203|||||||||
24749|Boomerang Creek Gneiss|48894|6|Mentioned|p20|||||||||
27345|Boomerang Tank Limestone Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||
27345|Boomerang Tank Limestone Member|23171|6|Mentioned|p31|||||||||
27345|Boomerang Tank Limestone Member|23173|6|Mentioned|Map Legend|||||||||
27345|Boomerang Tank Limestone Member|23522|5|Briefly described|p253|Devonian|Devonian|Of Baledmund Formation.||||||
27345|Boomerang Tank Limestone Member|35287|6|Mentioned|p7|||||||||
27345|Boomerang Tank Limestone Member|36118|6|Mentioned|p67|||||||||
27345|Boomerang Tank Limestone Member|39618|3|Fully described|p54|||||||||
27345|Boomerang Tank Limestone Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27345|Boomerang Tank Limestone Member|42566|5|Briefly described|p62|||Of Baledmund Formation.||||||17-SEP-08
27345|Boomerang Tank Limestone Member|46900|6|Mentioned|Fig.2|||Stratigraphic table||||||
27345|Boomerang Tank Limestone Member|65469|6|Mentioned|p15, p17|||Lachlan Orogen.||Baledmund Formation||||
27345|Boomerang Tank Limestone Member|73174|6|Mentioned|p1039|Lochkovian|Lochkovian|Contains late Lochkovian age-diagnostic conodont.||Baledmund Formation, Kopyje Group, Cobar Supergroup||||24-NOV-22
37903|Boomi Rhyolite Member|24605|2|Defined|p931, p948 App.1|Visean|Visean|Of the Caroda Formation. Maximum Thickness: 25m. Geological Province: New England Orogen.||||||
37903|Boomi Rhyolite Member|61214|5|Briefly described|p171 Fig. 1|Carboniferous|Carboniferous|||||||
32497|Boonabah Volcanics|22638|4|Described|p27|Early Silurian|Late Ordovician|New name. Does not outcrop. Age questionable||||||
32497|Boonabah Volcanics|22857|5|Briefly described|p416 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|||||||
32497|Boonabah Volcanics|44192|5|Briefly described|Map Legend|Bolindian|Bolindian|Misspelling of Boonbah?||||||
32497|Boonabah Volcanics|44936|5|Briefly described|Map Legend||Ordovician|||||||
32497|Boonabah Volcanics|50191|6|Mentioned|p5 Fig. 4|Silurian|Ordovician|||||||
32497|Boonabah Volcanics|63278|6|Mentioned|p145 Fig. 1|||Geological Province: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
32497|Boonabah Volcanics|67322|6|Mentioned|p23|Ordovician|Ordovician|Defined and Ordovician age assigned by Warren et al. (1995). Age is speculative.||||||
32497|Boonabah Volcanics|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
32497|Boonabah Volcanics|72495|5|Briefly described|p218, p225|||North-northwest-trending. Lithology description is derived from Warren et al. 1995.||Of Cowal Igneous Complex?  Figure 2 suggests not.|||Basalt, andesitic breccia and volcaniclastic rocks intruded by quartz diorite dykes.|26-MAR-20
73902|Boonoo Granite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Grey to pinkish grey, medium- to fine-grained, slightly to moderately porphyritic muscovite-titanite-biotite monzogranite; with scarce mafic inclusions to ~3cm.||||||11-DEC-07
73902|Boonoo Granite|63748|4|Described|p35-36|||Of the Boonoo Suite. Referred to as the "Spring Creek body" of the Bookookoorara Adamellite by Thomson (1976). Grey to pinkish grey, fine- to medium-grained, porphyritic (hornblende-titanite-) biotite monzogranite, with scattered feldspar.||||||07-FEB-11
73902|Boonoo Granite|68111|5|Briefly described|p969, p970 Fig.2, p971, p972 Fig.4, p974|Anisian|Olenekian|Dating detailed.|245.6 +/- 2.5 Ma, U-Pb SHRIMP (Li et al. 2012).|Of the Herries Supersuite.||||
73902|Boonoo Granite|69639|5|Briefly described|p44, p74, p217, p220|Anisian|Anisian|New England Orogen.|245.6 +/- 2.5 Ma  (SHRIMP U-Pb, Li et al, 2012)|Herries Supersuite||||
73902|Boonoo Granite|70876|5|Briefly described|p80-p81|Early Triassic|Early Triassic|Provided age is a SHRIMP U-Pb zircon date.|245.6 +/- 2.5 Ma (Li et al, 2012)|Herries Supersuite||||
73902|Boonoo Granite|71628|6|Mentioned|p11:4|||Donchak et al. (2007).||||||
82369|Boonoo Monzogranite|71628|3|Fully described|p19: 20-22; p15: 33, 52, 57, 62, 77|||See also p11: 4-6, 36. New name (this study), after the Boonoo State Forest. Originally the Spring Creek body of Bookookoorara Adamellite of Thomson (1973, 1976); later the Boonoo Granite of Donchak et al. (2007). Forms ~3 x 1 km intrusion about 10 km NNW of Tenterfield. Crops out as scattered, sometimes large, rounded boulders. The type locality is roadside outcrops along the Mount Lindesay Highway (Donchak et al., 2007). Geochemistry described.|245.69 +/- 2.5 Ma (SHRIMP: Li et al., 2012).|Boonoo Suite.||Abuts The Ram Swamp Monzogranite and is enclosed by Mount Lindesay Monzogranite (Stanthorpe Complex); probably intruded by them.|Grey to pinkish grey, medium- to fine-grained, weakly to moderately porphyritic biotite-(amphibole) monzogranite. I-type.|
73903|Boonoo Suite|63748|5|Briefly described|p35-36|||Of Herries Supersuite. Includes Boonoo Granite.||||||07-FEB-11
73903|Boonoo Suite|71628|6|Mentioned|p19: 21||||||Boonoo Monzogranite.|||
39259|Boorabil Ignimbrite Member|50613|2|Defined|p211, p229 App. 1|Westphalian|Westphalian|Of  Willuri Formation.  Volcanic member of the Tulcumbar package (informal grouping of stratigraphically recongnisable distinctive, mappable units). Max.thickness: 60m; 50m in type section.  Geological province: New England Orogen. Type section included.||||||22-FEB-05
29733|Booralee Volcanics|22519|5|Briefly described|p8|||||||||
29733|Booralee Volcanics|23053|5|Briefly described|Fig8p15,22,65||Silurian|||||||
29733|Booralee Volcanics|43277|5|Briefly described|Map Legend|Late Silurian||of Lachlan Fold Belt.Middle-Late Silurian.||||||
26416|Boorolong Granodiorite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26416|Boorolong Granodiorite|38288|6|Mentioned|Fig.4|||||||||
26416|Boorolong Granodiorite|71628|4|Described|p8: 3, 18-20, 23, 33-34|||Leitch et al. (1971) after unpublished work by Neilson (1970). Binns et al. (1967) first referred to this pluton as Booralong [sic] Granodiorite, and credited its mapping and petrographic description to Neilson. The history of inconsistent spelling is outlined; most likely named after Boorolong homestead. Forms a ~6km x 2km ovoid intrusion. Limited geochemistry described.|249.8 Ma (Rb-Sr biotite: Shaw, 1994).|Mount Duval Suite.||Is entirely surrounded by, and was intruded by, Mount Duval Monzogranite.|Medium-grained, porphyritic biotite-hornblende granodiorite-monzogranite. I-type.|
80447|Booroorban granite|70718|4|Described|p68-p71, p77, p86, p122|Early Devonian|Early Devonian|Informal name, interpreted from geophysics and an intersections in Hay No.1 and waterbore GWO36235. Appears to be intruded by the Wanganella granodiorite; however radiometric ages suggest that the Wanganella granodiorite is older than the Booroorban granite, this could be resolved if it is found the units do not physically cut one another; alternatively emplacement of the Booroorban granite may have stoped surrounding sediments leaving the older Wanganella granodiorite in place. Mistakenly referred to as the Booroorban granodiorite on p77.|398+/- 4 Ma (SHRIMP)|Booroorban granite suite||Intrudes the Eurolie granite.|I-type course-grained metaluminous porphyritic granite assemblage with phenocrysts.|31-MAY-19
80438|Booroorban granite suite|70718|5|Briefly described|p3, p64, p68, p94, p122|Devonian|Silurian|Informal name, derived from geophysics and intersections of Booroorban granite in Hay No.1 and waterbore GWO36235.|||Includes the Eurolie and Booroorban granites.|Intruded by Willurah igneous intrusions, part of Leeton Igneous Complex.|Granite, granodiorite known and inferred.|31-MAY-19
23410|Booth Limestone Member|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|Of Gundaroo Sandstone||||||
23410|Booth Limestone Member|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
23410|Booth Limestone Member|41821|2|Defined|p49|early Pragian||Age: mid Early Devonian (early Pragian)||||||
23410|Booth Limestone Member|65469|5|Briefly described|p16|Pragian|Lochkovian|Lachlan Orogen.||Gundaroo Sandstone||||
23410|Booth Limestone Member|70751|6|Mentioned|p7, p12|||Exposed in the Manuka silver mine.||Gundaroo Sandstone|||Limestones.|
23410|Booth Limestone Member|70950|6|Mentioned|p1030,1033,1037|||Geological province: Central Lachlan Orogen. Exposed in the Manuka Ag mine. Where exposed, shows development of a tower karst-like weathering surface, which interfingers with and is draped by pyritic black shales. Contains a upper fossiliferous unit that hosts sulfide-rich mineralisation.||Unit of Gundaroo Sandstone.||Underlain unconformably by Thule Granite.||
23410|Booth Limestone Member|71039|5|Briefly described|p14|||Outcrops in the Manuka mine where CAI is measured.||Winduck Group.|||Limestone.|
23410|Booth Limestone Member|72908|6|Mentioned|p5, p16|||Exposed in the wall of the Manuka silver-lead mine where it is associated with sulfide-rich mineralisation.||Gundaroo Sandstone|||Dolomitic.|
23410|Booth Limestone Member|72958|6|Mentioned|p11|Emsian|Pragian|Cobar Basin. Nymagee area. Overlain, underlain and equivalent to the Gundaroo Sandstone and Buckambool Sandstone. Unclear which, if either, is the parent unit.||Of Gundaroo Sandstone?, Winduck Group||||
25803|Boothenba Sandstone Member|29870|6|Mentioned|p13|||||||||
25803|Boothenba Sandstone Member|30610|2|Defined|p324|Late Triassic|Late Triassic|Part of Talbragar Formation||||||
25803|Boothenba Sandstone Member|35095|6|Mentioned|p111|||Also Table.1,reference Dulhunty 1973.||||||
25803|Boothenba Sandstone Member|61377|5|Briefly described|p152|Triassic|Triassic|Upper part of the Wallingarah Formation. Medium- to coarse-grained, massive to crossbedded, quartz sandstone. Max. thickness: 20m. Geological Province: Surat Basin, Coonamble Embayment.||||||07-FEB-11
42361|Bootheragandra Group|61964|3|Fully described|p14 Fig. 4, p97|Lochkovian|Pridoli|Includes Square Head Fm+Yegi Conglom. Includes thick seq.of pebble-boulder conglom.composed of clasts of mostly qrtz sst + lesser granite; less common lithologies include quartz sst, pebbly qtz sandstone slate + phyllite.  Geophysics of group - p226-227||||||
42361|Bootheragandra Group|62405|5|Briefly described|Map legend|Early Devonian|Silurian|Includes the Yegi Conglomerate and Square Head Formation, and at least nine unnamed sedimentary units. Boothumble Formation occurs at the base of the group.||||||10-APR-08
42361|Bootheragandra Group|65469|5|Briefly described|p18, p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, App A-VI 3.|||Includes the Square Head Formation.|Overlain by the Crossleys Tank Formation. Intruded by the Nyora Granite.||
42361|Bootheragandra Group|69161|5|Briefly described|Map legend|Silurian|Silurian||||Includes Yegi Conglomerate.|Is faulted over Wagga Group. Is overlain by Crossleys Tank Formation and unconformably by Barrat Formation.|Undifferentiated sandstone, pebbly sandstone, conglomerate and minor slate.|
42361|Bootheragandra Group|69162|5|Briefly described|Map legend|Silurian|Silurian||||Includes Square Head Formation.|Unconformably overlies Clements Formation (Wagga Group). Underlies (?faulted contact) Mailman Gap Member (Rankin Formation).||
42361|Bootheragandra Group|69163|5|Briefly described|Map legend|Silurian|Silurian||||Includes Square Head Formation.|Unconformably overlies Clements Formation (Wagga Group). Underlies (?faulted contact) Mailman Gap Member (Rankin Formation).||
42361|Bootheragandra Group|69164|5|Briefly described|Map legend|Silurian|Silurian||||Includes Square Head Formation.|||
42361|Bootheragandra Group|69798|6|Mentioned|p6|||Part of the basement to Oaklands Basin.||||||
42361|Bootheragandra Group|70751|6|Mentioned|p4, p6, p15|Devonian|Late Silurian|Cobar Superbasin, Mount Hope Trough.||||||
42361|Bootheragandra Group|71039|5|Briefly described|p6, p23|Devonian|Silurian|||||||
42361|Bootheragandra Group|71693|5|Briefly described|Map legend.|Devonian|Devonian||||||Thick sequence of pebble-boulder conglomerate composed of clasts of mostly quartz sandstone and lesser granite; less common quartz sandstone beds, pebbly quartz sandstone, slate and phyllite.|
42361|Bootheragandra Group|72908|6|Mentioned|p4|Early Devonian|Silurian|Mount Hope Trough.||||||
24752|Booti Booti Sandstone|22500|5|Briefly described|p 7||Early Carboniferous|Myall Trough||||||
24752|Booti Booti Sandstone|22736|6|Mentioned|p629|Namurian|Visean|||||||
24752|Booti Booti Sandstone|22857|4|Described|p512 App.1 Tb.A1.8|Visean|Visean|Cream to grey, cross-bedded quartz, feldspathic or lithic arenite with sorted shells, concretions. Disconformably overlies Nerong Volcanics, Boolambayte Formation, and also conformable on Nerong Volcanics. Max. thickness: 150m. ||||||
24752|Booti Booti Sandstone|23157|5|Briefly described|p110 fig2,7,8|Carboniferous|Carboniferous|||||||
24752|Booti Booti Sandstone|32868|6|Mentioned|p212|||||||||
24752|Booti Booti Sandstone|36057|2|Defined|p347|early Namurian|Visean|Visean - Early Namurian||||||
24752|Booti Booti Sandstone|36528|6|Mentioned|p179|||||||||
24752|Booti Booti Sandstone|38801|6|Mentioned|Fig.3|||||||||
24752|Booti Booti Sandstone|39660|6|Mentioned|p449|||||||||
24752|Booti Booti Sandstone|40883|6|Mentioned|p8|||||||||
24752|Booti Booti Sandstone|42547|5|Briefly described|p32, 37|||||||||
24752|Booti Booti Sandstone|44244|4|Described|p206-209|Namurian|Visean|Overlies Nerong Volcanics and Boolambayte Formation; underlies Yagon Siltstone. Type section in text. Geological Province: Myall Block.||||||24-FEB-06
24752|Booti Booti Sandstone|47056|6|Mentioned|Fig.2 P523|||||||||
24752|Booti Booti Sandstone|50132|5|Briefly described|p248  Fig.6|Namurian|Namurian|Early Namurian age||||Overlies the Nerong Volcanics. Underlies the Yagon Siltstone.||27-MAR-12
24752|Booti Booti Sandstone|50263|5|Briefly described|Map Legend|Visean|Visean|Underlies: Yagon Siltstone. Geological Province: Eastern Myall Block.||||||
24752|Booti Booti Sandstone|63832|6|Mentioned|p131 Fig.2|Visean|Visean|Eastern Myall block, Southern New England Fold Belt.||||||
24752|Booti Booti Sandstone|64631|5|Briefly described|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt: eastern Myall Block. Biostratigraphic age control for base and top and radiometric age control at base.||||Is overlain by Yagon Siltstone.||
24752|Booti Booti Sandstone|69323|5|Briefly described|p62|||Geological province: New England Orogen.||||Underlain disconformably by Nerong Volcanics.||
24752|Booti Booti Sandstone|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Myall Block, Tamworth Belt.||||||
39667|Bootoowa Fossil Member|61964|3|Fully described|p14 Fig. 4, p81-82|Emsian|Pragian|Of Ural Volcanics (Rast Group). Fossiliferous rhyolitic breccia with clasts of porphyritic rhyolite, limestone, silicified shelly fossils and crystals of quartz and feldspar; forms narrow lenses. Max. thickness: 30m. See also p76.||||||20-JUN-13
39667|Bootoowa Fossil Member|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Ural Volcanics (Rast Group). Fossiliferous rhyolitic breccia with clasts of porphyritic rhyolite, limestone, silicified shelly fossils and crystals of quartz and feldspar.||||||14-OCT-08
39667|Bootoowa Fossil Member|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Ural Volcanics.|||Breccia containing clasts of rhyolite, rare limestone and shelly fossils (some siliceous pseudomorphs).|
28143|Borah Limestone Member|22857|5|Briefly described|p498 App.1 Tb.A1.7|Famennian|Famennian|Three interbedded limestone horizons; contains ammonoids, conodonts. Geological Province: Tamworth Forearc Basin.||||||
28143|Borah Limestone Member|34262|6|Mentioned|p243|||||||||
28143|Borah Limestone Member|37987|2|Defined|p216|Late Devonian|Late Devonian|||||||
28143|Borah Limestone Member|38222|6|Mentioned|Fig.2|||||||||
28143|Borah Limestone Member|41238|6|Mentioned|p83|||Equals Kiah Limestone Member||||||
28143|Borah Limestone Member|43429|14|Not recorded|Map Legend|||||||||
28143|Borah Limestone Member|43435|14|Not recorded|Map Legend|||||||||
28143|Borah Limestone Member|44244|5|Briefly described|p19|Visean|Famennian|Of the Goonoo Goonoo Mudstone.  Contains ammonoids and conodonts.  Max. thickness: 1m.  Geological Province: Rouchel Block.||||||16-SEP-04
28143|Borah Limestone Member|66720|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Mandowa Mudstone.|||Fine-grained, grey, thinly bedded and laminated micritic lithographic limestone; minor bioclastic layers of shell fragments.|
24753|Boraig Group|22768|6|Mentioned|p178|||||||||
24753|Boraig Group|22857|5|Briefly described|p178, p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Partly a volcanic shield complex. Geological Province: Bogan Gate Terrace.||||||
24753|Boraig Group|23309|6|Mentioned|p390|||||||||
24753|Boraig Group|29648|6|Mentioned|p19|||||||||
24753|Boraig Group|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
24753|Boraig Group|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
24753|Boraig Group|31161|5|Briefly described|PA7|||||||||
24753|Boraig Group|31448|6|Mentioned|p33|||||||||
24753|Boraig Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
24753|Boraig Group|32672|6|Mentioned|p673|||||||||
24753|Boraig Group|33325|5|Briefly described|Table 4|||||||||
24753|Boraig Group|33326|6|Mentioned|p441|||Fauna||||||
24753|Boraig Group|33732|5|Briefly described|p111|||Equiv. Snowy River Volc.||||||
24753|Boraig Group|34403|4|Described|p143|||||||||
24753|Boraig Group|34405|5|Briefly described|p117|||||||||
24753|Boraig Group|34406|6|Mentioned|p222|||||||||
24753|Boraig Group|34692|6|Mentioned|p187|||||||||
24753|Boraig Group|35070|6|Mentioned|p115|||||||||
24753|Boraig Group|37491|6|Mentioned|p292|||||||||
24753|Boraig Group|37727|6|Mentioned|p33|||See also P82 and Fig.1.||||||
24753|Boraig Group|40328|6|Mentioned|p44|||||||||
24753|Boraig Group|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
24753|Boraig Group|40498|6|Mentioned|p364|||||||||
24753|Boraig Group|40882|6|Mentioned|p25|||||||||
24753|Boraig Group|42313|6|Mentioned|p151|Middle Devonian||||||||
24753|Boraig Group|42726|5|Briefly described|map legend|Early Devonian||V43.  Of the Boggy Plain Suite (Boggy Plain Supersuite).||||||08-FEB-05
24753|Boraig Group|44092|5|Briefly described|map legend|Early Devonian|Early Devonian|Dlv2||||||
24753|Boraig Group|60078|6|Mentioned|Map Legend|Devonian|Devonian|||||||
24753|Boraig Group|60086|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Includes the Cumberland Rhyolite, Talbingo Basalt, Buddong Volcanics, Saddle Tuff, Landers Creek Formation.||||||
24753|Boraig Group|63290|6|Mentioned|p403 Fig. 6(c)|Early Devonian|Early Devonian|Geological Province: Tumut Block.||||||
24753|Boraig Group|68592|6|Mentioned|p936|||Moye et al. (1969) after Adamson (1956). Wagga 1:250 000 sheet.||||Equivalent to Black Range Group (Goulburn 250).||
35122|Borehole coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within Lambton Formation (Newcastle Coal Measures).||||||
35122|Borehole coal seam|23055|6|Mentioned|p35|||||||||
35122|Borehole coal seam|68711|5|Briefly described|p119, p116 Tbl 3|||Informal unit. ||Within Lambton Formation||||
23411|Boshy Formation|22857|5|Briefly described|p91 Fig. 14.7B, p122|Late Cambrian|Late Cambrian|Of the Kayrunnera Group? Interbedded fine-grained quartz sandstone, feldspathic sandstone, siltstone, clacarenite and impure limestone beds and lenses. Overlies the Morden Formation. Max. thickness: 100m. See also p410 App. 1 Tb. A1.4.||||||
23411|Boshy Formation|22858|6|Mentioned|Fig14.7bp90-1|Late Cambrian|Late Cambrian|||||||
23411|Boshy Formation|23245|6|Mentioned|p122|||||||||
23411|Boshy Formation|41587|4|Described|p908|||||||||
23411|Boshy Formation|41810|6|Mentioned|p107|||||||||
23411|Boshy Formation|62793|5|Briefly described|p270|Late Cambrian|Late Cambrian|Unit of Kayrunnera Group, Northern Koonenberry belt. Contains trilobites of Mindyallan age.||||Overlies Morden Formation and underlies Watties Bore Formation.||21-MAR-12
23411|Boshy Formation|63790|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of Kayrunnera Group. Shallow wter trace fossils, trilobites and shelly fauna.||||||27-NOV-08
23411|Boshy Formation|64671|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of Kayrunnera Gp. Well-laminated quartzose sandstones and quartzites, mostly white, some red and maroon. Festoon cross-bedding in some units. Minor siltstone and conglomerate interbeds. Lacking detrital mica. Mindyallen trilobite remains near base.||||||26-NOV-08
23411|Boshy Formation|64684|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of Kayrunnera Group. Well-laminated quartzose sandstones and quartzites, mostly white, some red and maroon. Festoon cross-bedding in some units. Minor siltstone and conglomerate interbeds. Lacking detrital mica. Mindyallan trilobite at base.||||||08-DEC-08
23411|Boshy Formation|66623|3|Fully described|p110, pp114-118. |Late Cambrian|Late Cambrian|Kayrunnera Basin. Defined by Webby et al. (1988) from rocks in the Kayrunnera beds of Brunker et al. (1971). Shallow marine: contains late Mindyallan trilobites. Correlative of Hummock Formation. Its basal conglomerate is likely correlative with Williams Creek Conglomerate. Thickness varies from 100 m to 500 m.||Unit in Kayrunnera Group.||Overlies Morden Formation. Is locally unconformably or disconformably overlain by Ravendale Formation.|White to maroon, well-laminated quartzite interbedded with minor limestone, siltstone and conglomerate horizons. Local basal polymictic rounded cobble conglomerate.|
23411|Boshy Formation|66929|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Mindyallan trilobite remains near base.|||||Well-laminated quartzose sandstones and quartzites; mostly white, some red and maroon; local festoon cross-bedding; minor siltstone and conglomerate interbeds.|
23411|Boshy Formation|66933|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Mindyallan trilobite remains near base.||Unit in Kayrunnera Group.|||Well-laminated quartzose sandstones and siltstones; mostly white, some red and maroon; local festoon cross-bedding; minor siltstone and conglomerate interbeds; lacking detrital mica.|
23411|Boshy Formation|67322|4|Described|p11-12, p20 Fig.5|Mindyallan|Mindyallan|Defined by Webby et al. (1988). Age determined from trilobite fossils from two stratigraphic levels, the lower about one third from the base of the formation, and the other in the upper third (Wang et al. 1989). About 94m thick in the type section, c. 18 km SE of Koonenberry Mountain.||Of the Kayrunnera Group.||Conformably overlies Morden Formation. Is overlain conformably by Watties Bore Formation.|Interbedded fine-grained sandstones and siltstones, with minor calcarenites and limestone lenses.|21-FEB-18
23411|Boshy Formation|69573|6|Mentioned|p657, 661, 667|||Subtidal, mid-shelf setting.||Kayrunnera Group.||||
23411|Boshy Formation|70648|5|Briefly described|Map Legend|Ordovician|Cambrian|||Kayrunnera Group|||White to maroon, well-laminated quartzite containing festoon cross-bedding, interbedded with minor limestone, siltstone and conglomerate horizons.|
23411|Boshy Formation|70838|4|Described|p269 Fig.3, p270-272, p275, p278|Late Cambrian|Late Cambrian|Kayrunnera Basin, SE Koonenberry Belt. Contains Mindyallan trilobites. Detrital zircon analyses.|501-499 Ma.|Kayrunnera Group.||Conformably overlies Morden Formation.|Dominantly quartzose.|
23411|Boshy Formation|73177|5|Briefly described|p1113-1115 Figs.15-17, 1116 Tb.2|Ordovician|Cambrian||505 +/- 11 Ma.|Kayrunnera Group.||||30-AUG-22
23411|Boshy Formation|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
32390|Boulderwood Formation|22857|5|Briefly described|p518 App.1 Tb.A1.9|Middle Triassic|Early Triassic|Thin-bedded quartz lithic conglomerate, coarse pebbly quartz-lithic sandstone, siltstone. Max. thickness: 20m. Geological Province: Gunnedah Basin.||||||
32390|Boulderwood Formation|23043|5|Briefly described|Map Legend|Early Triassic|Early Triassic|of Gunnedah Basin.||||||
32390|Boulderwood Formation|23170|2|Defined|p307|Middle Triassic|Early Triassic|of Sydney Basin||||||
32390|Boulderwood Formation|50590|5|Briefly described|Map Legend|Triassic|Triassic|Geological Province: Gunnedah Basin. Thick-bedded conglomerate, sandstone and siltstone.||||||29-JUN-04
32390|Boulderwood Formation|71600|6|Mentioned|p23 Fig 1|Mesozoic|Mesozoic|||||||
33410|Boulton Formation|23217|2|Defined|p1, p3-6|Frasnian|Givetian|Basal formation of Hervey Group. Replaces 'Kadina Formation' (of the "Beargamil Sub-group") as used by Connolly (1965a). Also, supersedes "Bolten Formation" and "Bolton Formation". Max. thickness: 707m in type section.||||||08-MAR-06
33410|Boulton Formation|24417|3|Fully described|p129|Late Devonian|Middle Devonian|Formerly "Bolten Formation" - spelling changed to avoid confusion with "Bolton beds" elsewhere in NSW.||||||
33410|Boulton Formation|60009|5|Briefly described|Map Legend|Frasnian|Frasnian|Of the Hervey Group. Underlies: Mandagery Formation.||||||13-JUL-04
33410|Boulton Formation|68592|6|Mentioned|p1707|||In the Forbes 1:250 000 map area.||Basal unit in Hervey Group.||Is correlated with Bendick Formation.||
27115|Bourimbla Limestone Member|5250|5|Briefly described|p42, p45, p47||Early Caradoc|Member of  Daylesford Limestone. Includes brachiopod fauna. Overlain by Manooka Limestone Member.||||||16-JAN-12
27115|Bourimbla Limestone Member|23214|3|Fully described|p37|Late Ordovician|Late Ordovician|Of Daylesford Limestone. Max. thickness 24m. For lithology description see Semeniuk (1973a,b).||||||
27115|Bourimbla Limestone Member|33063|2|Defined|p80|Ordovician|Ordovician|Mb. Daylesford Gp.||||||
27115|Bourimbla Limestone Member|33064|4|Described|p450|||See also PP451-452. Strat. column.||||||
27115|Bourimbla Limestone Member|33065|5|Briefly described|Table 1|||Lithology||||||
27115|Bourimbla Limestone Member|33740|6|Mentioned|Fig.1|||||||||
27115|Bourimbla Limestone Member|38219|6|Mentioned|Table 2|||||||||
27115|Bourimbla Limestone Member|40136|6|Mentioned|p23|||||||||
27115|Bourimbla Limestone Member|41046|6|Mentioned|Fig.2|||||||||
27115|Bourimbla Limestone Member|42479|5|Briefly described|p111|||||||||
27115|Bourimbla Limestone Member|70684|5|Briefly described|p39, p41|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Daylesford Limestone.||Overlies Ranch Member.|Contains shell banks (described in some detail).|
27115|Bourimbla Limestone Member|73210|5|Briefly described|p893, 900 Fig.7, 902 Fig.9|||Semeniuk (1973, 2011). Exhibits subaerial disconformities and diagenesis/pedogenesis. Summary profile of a subaerial disconformity.||Daylesford Limestone.||Overlies Ranch Member. Is overlain by Manooka Limestone Member.||14-DEC-22
31724|Bowan Park Limestone Subgroup|13139|5|Briefly described|p7, p9 Fig. 4|Late Ordovician|Late Ordovician|Includes the Ballingoole Limestone.  Geological Province: Western Molong Volcanic Belt.||||||
31724|Bowan Park Limestone Subgroup|22857|5|Briefly described|p426 App. 1 Tb. A1.5|Eastonian|Eastonian|Of the Barrajin Group. Thin-bedded to massive, partly fossiliferous limestone, marl. Max. thickness: 564m.||||||
31724|Bowan Park Limestone Subgroup|23213|6|Mentioned|p22|||Sourges Shale macrofauna match Gerybong Limestone Member of the Daylesford Limestone within the Bowan Park Limestone Subgroup.||||||
31724|Bowan Park Limestone Subgroup|23214|3|Fully described|p34|Late Ordovician|Late Ordovician|Of Barrajin Group. Formerly known as Bowan Park Group. Thinly to thickly bedded to massive limestone and marl with minor lithic sandstone and mudstone at the base. Max. thickness 564m.||||||
31724|Bowan Park Limestone Subgroup|23334|5|Briefly described|9 Fig.4|Late Ordovician|Late Ordovician|||||||
31724|Bowan Park Limestone Subgroup|24398|5|Briefly described|p264|Eastonian|Eastonian|Geological Province: Lachlan Fold Belt.||||||
31724|Bowan Park Limestone Subgroup|43640|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Barrajin Group.||||||01-SEP-08
31724|Bowan Park Limestone Subgroup|43782|5|Briefly described|Map Legend|Eastonian|Eastonian|Of Barrajin Group.||||||01-SEP-08
31724|Bowan Park Limestone Subgroup|60989|6|Mentioned|p112|||Formerly known as the Barton Limestone.||||||
31724|Bowan Park Limestone Subgroup|63278|4|Described|p147 Fig. 2b, p153|Late Ordovician|Late Ordovician|Includes; Daylesford Limestone, Ranch Member, Downderry Limestone Member, Quondong Limestone, Ballingoole Limestone. Underlain unconformably by Cargo Volcanics. Thickness: 564m. Geological Province: Molong Volcanic Belt, LFB. Consists of limestone.||||||07-FEB-11
31724|Bowan Park Limestone Subgroup|63283|5|Briefly described|p195 Fig. 2, p208|Late Ordovician|Late Ordovician|Overlain by Malachis Hill Formation, underlain by Cargo Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
31724|Bowan Park Limestone Subgroup|63290|5|Briefly described|p410, p396 Fig. 3|Eastonian|Eastonian|Overlain by Malachis Hill Formation. Geological Province: Molong Volcanic Belt.||||||
31724|Bowan Park Limestone Subgroup|64295|6|Mentioned|p201|||Overlies Cargo Volcanics. Central NSW.||||||01-SEP-08
31724|Bowan Park Limestone Subgroup|64826|5|Briefly described|p1040 Tb. 1|Eastonian|Eastonian|Of the Barrajin Group.||||||04-MAR-09
31724|Bowan Park Limestone Subgroup|67106|6|Mentioned|p673, 677|||Molong Volcanic Belt.|||Daylesford Limestone.|||
31724|Bowan Park Limestone Subgroup|67322|4|Described|p20 Fig.5, p23, p24|Katian|Katian|Macquarie Arc. Modified after Stevens (1957). Age constrained by over- and underlying stratigraphy. Occurs in the Bowan Park region.||Of the Cabonne Group.|Daylesford, Quondong and Ballingoole Limestones.|Unconformably overlies Cargo Volcanics. Correlative of Cliefden Caves Limestone Subgroup. Overlain by the Malachis Hill Formation.|Highly fossiliferous limestone.|21-FEB-18
31724|Bowan Park Limestone Subgroup|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
31724|Bowan Park Limestone Subgroup|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Post-phase 2 volcanic hiatus. Age: deposited from early to late Eastonian.|c. 455-450 Ma|Cabonne Group||||
31724|Bowan Park Limestone Subgroup|70684|5|Briefly described|p34, p39-42, p75|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian. The superseded version, Bowan Park Subgroup (see references p34-35, p39-42) is used, as often as not, as an equivalent name for this unit. About 565m thick.|||Daylesford Limestone.|Unconformably overlies Cargo Volcanics. Is overlain by Malachis Hill Formation.||
31724|Bowan Park Limestone Subgroup|73154|5|Briefly described|p77 Fig.3|Eastonian|Eastonian|Macquarie Arc, Molong Volcanic Belt.||||Underlies Malachis Hill Formation.|Limestone.|
31724|Bowan Park Limestone Subgroup|73208|6|Mentioned|p870 Fig.1|Late Ordovician|Late Ordovician|||||||
31724|Bowan Park Limestone Subgroup|73209|6|Mentioned|p880|Late Ordovician|Late Ordovician|Molong-Cudal area, central-west NSW.|||Daylesford Limestone|||
31724|Bowan Park Limestone Subgroup|73210|6|Mentioned|p892|||Percival et al. (2011). Formerly the Bowan Park Group of Semeniuk (1973).|||Daylesford Limestone.|||
31724|Bowan Park Limestone Subgroup|73492|5|Briefly described|p696-697, p702-703, p705, p707|Katian|Katian|T. blandus Biozone of early Katian age in lower part (Zhen et al., 1999).|||Daylesford Limestone, Quondong Limestone|Overlies Cargo Volcanics, underlies Malachis Hill Formation||
77273|Bowfield Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Mount Thorley Formation.||||
26419|Bowman beds|22612|6|Mentioned|424 fig 2, 429|Devonian|Devonian|||||||
26419|Bowman beds|41347|4|Described|Table 3|||Mention P198||||||
26419|Bowman beds|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Laminated siltstone, sandstone, minor limestone.||||||16-DEC-04
26419|Bowman beds|44244|6|Mentioned|p124|Devonian|Devonian|||||||
72934|Bowral Trachyte|61186|6|Mentioned|p18|||Traditional building stone used in Sydney for buildings and paving and curbing - probably an informal name. ||||||
72934|Bowral Trachyte|64769|6|Mentioned|p23|||Dimension stone name.||||||06-MAY-09
72934|Bowral Trachyte|68204|6|Mentioned|p47|||Mittagong-Bowral area, Sydney Basin. Obsolete quarrying term for what is now called the Mount Gibraltar Microsyenite.||||||
29583|Box Ridge Volcanics|22679|2|Defined|p 30|Early Devonian|Late Silurian|replaces Grove Formation, Box Ridge Member and Pine Ridge Volcanics||||||
29583|Box Ridge Volcanics|22857|4|Described|p472 App.1 Tb.A1.6|Devonian|Silurian|Of the Mumbil Group. Max. thickness: 1350m. Geological Province: Hill End Trough.||||||24-FEB-06
29583|Box Ridge Volcanics|23048|5|Briefly described|p9 fig14||Early Devonian|||||||
29583|Box Ridge Volcanics|23214|3|Fully described|p146|Early Devonian|Late Silurian|Of Mumbil Group. Previously named Box Ridge Formation, Box Ridge Member and Pine Ridge Volcanics. Can be subdivided into three informal units: "Pine Ridge Volcanics", "Crawford Formation" and "Barrier Volcanics". Max. thickness 914m.||||||
29583|Box Ridge Volcanics|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group (east). Does not appera on map face.||||||17-JUL-08
29583|Box Ridge Volcanics|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Mumbil Group. Does not appear on map face.||||||17-JUL-08
29583|Box Ridge Volcanics|44093|5|Briefly described|p207 App. 1|Early Devonian|Early Silurian|Of Mumbil Group. Geological Province: Lachlan Fold Belt.||||||
29583|Box Ridge Volcanics|50233|5|Briefly described|Map Lagend|Lochkovian|Pridoli|Of the Campbells Group. Mafic and minor siliceous volcanics, lithic siltstone.||||||
29583|Box Ridge Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Mafic and minor siliceous volcanics, lithic siltstone.||||||11-JUN-08
29583|Box Ridge Volcanics|68592|2|Defined|p608, p610, p613, p615, p619-20, p673-82|Early Devonian|Early Devonian|See also p259-61, p808, p845 Fig.141, p863. Originally named Box Ridge Member by Roy (1961) but first published as Box Ridge Formation by Brunker and Offenberg (1970). Differentiated into three sub-units (Barrier and Pine Ridge Volcanics, Crawford Formation) by Green (1980), but this was not adopted by Pogson and Watkins (1998). A type section defined by Collins (1966), a more representative section, and "best and most extensive outcrops", are all described. c.1600m thick. Trace elements, geochemistry and geophysical properties detailed. Similar characteristics between the alkali basalts and Goonoonglah Monzodiorite dykes, and between the peralkaline rhyolite lavas and Wrens Nest Trachyte. Forms prominent hills. Minor hydrothermal metamorphism/alteration.||Unit in Campbells Group.||Conformably overlies Cuddyong Formation. Is faulted against Crudine Group and Copperhannia Member (Cunningham Formation). Correlated with Gundary Volcanics.|Broadly divided into two interbedded units: alkali basalt and peralkaline rhyolite lavas; and siltstone, medium- to very coarse-grained lithic sandstone and minor basalt.|
29583|Box Ridge Volcanics|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Scx[3 asterisks]. Includes two unnamed members; pillow-massive, aphanitic-plagioclase phyric basalt and a massive, fine-coarse grained, poorly sorted, lithic sandstone. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||At top of Campbells Group|Includes two unnamed members.|Is within uppermost part of Cuddyong Formation. Is overlain by undifferentiated Crudine Group.|Basalt with fine to coarse grained, locally pebbly to conglomeratic, lithic sandstone, siltstone and mudstone; minor diorite.|
29583|Box Ridge Volcanics|70297|5|Briefly described|map legend|Silurian|Silurian|||||||
29583|Box Ridge Volcanics|70544|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed members; pillow-massive, aphanitic-plagioclase phyric basalt and a massive, fine-coarse grained, poorly sorted, lithic sandstone.||Campbells Group|Includes two unnamed members||Basalt with fine to coarse grained, locally pebbly to conglomeratic, lithic sandstone, siltstone and mudstone; minor diorite.|
29583|Box Ridge Volcanics|71069|6|Mentioned|p163|||Contains interstitial quartz and rounded quartz xenocrysts. ||Campbells Group||||
29583|Box Ridge Volcanics|71656|6|Mentioned|p13 Fig.2|Lochkovian|Lochkovian|||Campbells Group||Overlies Cuddyong Formation? Overlain by Crudine Group.||
31756|Boxers Creek Formation|22857|5|Briefly described|p480 App.1 Tb.A1.6|||See also ERRATA sheet for comments.||||||
31756|Boxers Creek Formation|43834|4|Described|p28|||Thickness: 600m. Underlies Towrang Formation.||||||11-JUN-08
31756|Boxers Creek Formation|50234|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Mount Fairy Group.  Overlies Covan Creek Formation.  Underlies Gundary Formation.||||||11-JUN-08
31756|Boxers Creek Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Fawn, cream and brown, very thinly to very thickly-bedded fine- to v. coarse-gr.feldspar-lithic-quartz sandstone, siltstone, shale; crystal-rich in places; metsedimentary, tuffaceous chert, and meta-vein quartz lithic fragments...||||||09-SEP-08
31756|Boxers Creek Formation|66087|5|Briefly described|p3 Fig. 2|Early Devonian|Silurian|||Of the Mount Fairy Group.||||10-MAY-12
31756|Boxers Creek Formation|67820|5|Briefly described|p133, p136 Fig.3|Late Silurian|Late Silurian|||Mount Fairy Group.|||Quartz-lithic sandstone and siltstone.|
31756|Boxers Creek Formation|68592|1|Redefined|p821, p823-8, p834, p851, p852 Fig.143|Lochkovian|Pridoli|See also p235, p640-1, p726, p728, p729 Fig.132, p732, p856, p868, p871-3, p876, p878, p880, p883, p916. Jones et al. (1995) redefined. Previously mapped as an unnamed subunit of the Towrang Beds by Brunker and Offenberg (1970) and as undifferentiated Towrang Beds by Felton (1974). The Towrang Beds included rocks now defined as the Gundary Volcanics, Quialigo Volcanics, Bullamalita Conglomerate, and part of the Boxers Creek Formation. Type section: contact relationships with adjacent units is contentious. Representative section: passes through typical thin- to medium-bedded Boxers Creek Formation and siltstone-rich subunit. Potential source of structural clay/shale and kaolin. Thickness to 1.5 km, with some apparently thicker sections probably affected by folding and faulting. Age: Pridoli to earliest Lochkovian sparse brachiopod fauna. Metamorphism: sub-greenschist to possible lower greenschist facies. Fossils include trilobite and brachiopods. Classification and provenance plots. Is intruded by Turrallo Suite and (?) Komungla Rhyolite Member.||Unit in Mount Fairy Group.||Gradationally overlies, and is laterally equivalent to, Covan Creek Formation. Is locally conformably overlain by Gundary Volcanics; overlain by Back Station Ignimbrite and Tirranna Andesite Members.|Interbedded brown to cream, lithic-quartz, very fine- to very coarse-grained sandstone, which is feldspathic in places, and laminated, cream to grey siltstone and shale; sandstone is predominantly litharenite with rare lithic feldsarenite.|
31756|Boxers Creek Formation|69159|5|Briefly described|Map legend|Lochkovian|Pridoli|||Unit in Mount Fairy Group.|||Fawn, cream and brown, very thinly- to very thickly-bedded, fine- to very coarse-grained feldspar-lithic-quartz sandstone, siltstone and shale; rare distal crystal-vitric-ashy rhyolitic siltstone.|07-SEP-15
31756|Boxers Creek Formation|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfb. Contains one unnamed member of laminated siltstone and mudstone with thinly bedded, fine grained feldspar-lithic-quartz sandstone. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group|Includes one unnamed unit.|Is overlain by Back Station Ignimbrite Member and Tirranna Andesite Member. Overlies Covan Creek Formation.|Brown to cream, very fine to very coarse-grained, lithic quartz sandstone, feldspathic in places, interbedded with laminated cream to grey siltstone and shale, rare lenses of rhyolitic volcanic sandstone and crystal vitric rhyolitic tuff.|
31756|Boxers Creek Formation|70542|5|Briefly described|Map Legend|Devonian|Silurian|Contains one unnamed member of laminated siltstone and mudstone with thinly bedded, fine grained feldspar-lithic-quartz sandstone. ||Mount Fairy Group|||Brown to cream, very fine to very coarse-grained, lithic quartz sandstone, feldspathic in places, interbedded with laminated cream to grey siltstone and shale, rare lenses of rhyolitic volcanic sandstone and crystal vitric rhyolitic tuff.|
31756|Boxers Creek Formation|71069|5|Briefly described|p27, p40 fig 17, p133, p135|||Outcrops poorly in the map sheet area. Up to 1400m thick. Contains fossils of brachiopods assigned to Notanoplia sp. See also p136 fig 44, p142, p143-p145, p159, p170.||Mount Fairy Group||Conformably overlies the Covan Creek Formation, Woodlawn Volcanics. Overlain by the Tirranna Andesite Member, Gundary Volcanics.|Lithic-quartz to quartzose, planar and ripple cross laminated sandstone, litharenite and lithic arkose, siltstone and mudstone turbidite package.|
31756|Boxers Creek Formation|71656|5|Briefly described|p13 Fig.2, p30|Lochkovian|Pridoli|The brachiopod Notanoplia sp. and a trilobite referred to Phacops sp. have been identified from strata now attributed to the Boxers Creek Formation, near the top of that formation.||Mount Fairy Group||Overlies Covan Creek Formation. Underlies Gundary Volcanics.|Fossiliferous strata.|
31756|Boxers Creek Formation|71699|5|Briefly described|Map legend.|Devonian|Silurian|Lithology continued:  Sandstone beds up to 3m thick. Rare distal crystal-vitric-ashy rhyolitic siltstone.||Mount Fairy Group.||Overlies Covan Creek Formation.|Fawn cream and brown, very thinly- to very thickly-bedded fine- to very coarse-grained feldspar-lithic-quartz sandstone, siltstone and shale; metasedimentary tuffaceous chert and meta-vein quartz lithic fragments commonly comprise 20-40% of the rock.|
31756|Boxers Creek Formation|71700|2|Defined|vi, p7, p15-p16, p49, p59, CD|Lochkovian|Ludlow|Named for Boxers Creek, a tributary of the Wollondilly River. A type section was nominated by Jones et al (1995) from GR 757000 6153000 to 757750 6153100. A representative section occurs near a creek between GR 739100 6126000 to 740100 6125800. This unit was first defined by Jones et al (1995). The definition was expanded by Thomas and Pogson to include more sandstones above the Covan Creek Formation. Some rocks belonging to this formation were previously mapped as De Drack Formation. Hosts one unnamed constituent unit. Distribution, geomorphic expression, outcrop, depositional environment,  structure, metamorphism, geophysical characteristics, fossil assemblage and distinguishing features are discussed. Age is derived from fossil assemblages both of the formation and the underlying units. Together with the Covan Creek Formation forms a 3km thick turbidite package; the unit itself is inferred to be up to 1.5km thick.||Mount Fairy Group||Conformably overlies the Covan Creek Formation. Conformably overlain by the Gundary Volcanics. Overlain by the Quialigo Volcanics. Unconformably overlain by the Tarago Conglomerate.|Interbedded brown to cream, very fine- to very coarse-grained, lithic quartz sandstone which is feldspathic in places, and laminated cream to grey siltstone and shale.|
27116|Boxwell Granodiorite|42748|2|Defined|p6|Late Triassic|Late Permian|||||||
27116|Boxwell Granodiorite|63733|5|Briefly described|Map legend|Late Permian|Late Permian|Pale to dark grey or pinkish grey, medium- to fine-grained biotite-hornblende and hornblende-biotite granodiorite; minor monzodiorite-quartz monzodiorite, monzogranite, syenogranite; high magnetic response.||||||11-DEC-07
27116|Boxwell Granodiorite|63748|4|Described|p32|Late Permian|Early Permian|Of Boxwell Suite. Mascotte granodiorite (Shaw 1981). Intrudes Texas beds. Age: 255-252Ma (Rb-Sr biotite). Compositionally zoned with monzodiorite-qtz monzodiorite margin grading inwards to granodiorite and core of monzogranite + leucocratic syenogranite||||||07-FEB-11
27116|Boxwell Granodiorite|65668|6|Mentioned|p1|Permian|Permian|Texas area. Age: ~ 257 Ma.||||||
27116|Boxwell Granodiorite|68003|5|Briefly described|p31, p32 Fig.3-h, p131.|Late Permian|Late Permian|Central Block, New England Fold Belt. I-type. Also called Boxwell Creek Granodiorite on p31.||Unit in Clarence River Suite.|||Dark grey, medium- to coarse-grained, equigranular, hornblende-bearing monzodiorite and quartz monzodiorite.|
27116|Boxwell Granodiorite|68005|5|Briefly described|p63, p135.|Early Permian|Early Permian|||Unit in Clarence River Supersuite.|||Dark grey, medium- to coarse-grained, equigranular, hornblende-bearing monzodiorite and quartz monzodiorite.|
27116|Boxwell Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, as well as Ballandean, Clare Hills, Fairleigh, Herries, Jibbinbar, Mount Bullaganang, Mount You You and Palgrave Granites, and Greymare Granodiorite, are all mapped under the symbol, Pgn.||||||
27116|Boxwell Granodiorite|68679|4|Described|p455-457, p464-465|Permian|Permian|Northern New England Batholith. Crops out mainly in NSW. ~22 km2. A zoned pluton with a margin of monzodiorite to quartz monzodiorite grading into granodiorite, and a core of monzogranite and leucocratic syenogranite. Generally strongly oxidised, moderately-highly evolved, low-medium-K, I-type. Geochemistry briefly described: geochemical plots; similar to Dumbudgery Creek Granodiorite.|256.6 +/- 1.7 Ma (SHRIMP: Cross and Blevin, 2010).|Boxwell Suite.||Intrudes Texas beds.|Grey or pinkish-grey, fine- to medium-grained porphyritic (pyroxene-)hornblende-biotite and biotite-hornblende granodiorite to quartz monzodiorite; accessory titanite, allanite; rarely miarolitic.|
27116|Boxwell Granodiorite|68901|6|Mentioned|p8 Fig. iii|Early Triassic|Late Permian|||||||26-SEP-18
27116|Boxwell Granodiorite|70036|5|Briefly described|Map legend|Permian|Permian|New England Fold Belt.|||||Includes granodiorite.|
27116|Boxwell Granodiorite|70217|5|Briefly described|v, p73 tbl 14.1 , p74|Wuchiapingian|Wuchiapingian|New England Orogen. SHRIMP ages are derived from Cross and Blevin (2010). |256.6 +/- 1.7 Ma (SHRIMP U-Pb)|Boxwell Suite||||
27116|Boxwell Granodiorite|70876|5|Briefly described|p78|Permian|Permian|SHRIMP date is derived from Cross and Blevin, 2010. [Either part of the Clarence River Supersuite or a correlative-not made clear in the text].|256.6 +/- 1.7 Ma (SHRIMP U-Pb zircon)|Boxwell Suite||||
27116|Boxwell Granodiorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|257+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
27116|Boxwell Granodiorite|71628|4|Described|p9: 1-2; p10: 1-10; p19: 103, 158|||Stroud (1992). Included in Clarence River Supersuite by Bryant et al. (2003) after unpublished work by Chappell and Bryant (1994). Removed to Boxwell Suite within Boxwell Supersuite by Donchak et al. (2007) on locational and geochemical grounds. Named after a local island in the Dumaresq River. Crops out ~10 km W of Texas, as boulders in undulating country. Mostly covered by alluvium. A zoned pluton; petrology and geochemistry detailed. I-type.|256.6 +/- 1.7 Ma (Cross and Blevin, 2010).|Boxwell Suite.||Intrudes Texas beds.|Dark grey, medium- to coarse-grained, equigranular quartz monzodiorite (margin), medium-grained, slightly porphyritic hornblende-biotite granodiorite (dominant), and light pink, locally porphyritic, monzogranite to leucocratic syenogranite (core).|
69438|Boxwell Suite|63748|5|Briefly described|p32|Late Permian|Early Permian|Of the Boxwell Supersuite. Includes Boxwell Granodiorite.||||||07-FEB-11
69438|Boxwell Suite|68679|5|Briefly described|p457, p465|Permian|Permian|Northern New England Batholith; mostly in NSW.|~256 Ma.|Clarence River Supersuite.|Boxwell Granodiorite.|||
69438|Boxwell Suite|70217|5|Briefly described|p32|||New England Orogen. ||Boxwell Supersuite|Includes the Rocky Creek Granodiorite and the Boxwell Granodiorite.|||
69438|Boxwell Suite|70876|5|Briefly described|p80|Permian|Permian|Age derived from SHRIMP dates for the constituent Boxwell Granodiorite and Rocky Creek Granodiorite.||Clarence River Supersuite|Includes the Boxwell Granodiorite and Rocky Creek Granodiorite.|||
69438|Boxwell Suite|71628|5|Briefly described|p5: 1; p9:2; p10: 1, 3, 5, 9, 11|||Donchak et al. (2007) after unpublished work by Blevin (ca. 2004). Redefined in this study as a Supersuite.||Boxwell Supersuite.|Boxwell Granodiorite.|||
69437|Boxwell Supersuite|63748|5|Briefly described|p32|Late Permian|Early Permian|Includes the Boxwell Suite.||||||07-FEB-11
69437|Boxwell Supersuite|70217|5|Briefly described|v, p73 tbl 14.1, p74|Permian|Permian|Includes 4 I type granodiorites in the Northwest New England Orogen. Is geochemically similar to the Clarence River Supersuite. |||Includes the Boxwell Granodiorite and the Rocky Creek Granodiorite.|||
69437|Boxwell Supersuite|71628|5|Briefly described|p9:2; p10: 1-11; p19: 157-158|Late Permian|Late Permian|Donchak et al. (2007); redefined in this study. Comprises a handful of more sodic intrusives in the NW portion of the Southern New England Orogen. Geochemistry summarised and contrasted with other Supersuites.|||Apple Tree Gully, Boxwell, Dry Creek, Kings Plains Suites.||Quartz monzodiorite, granodiorite (dominant) and monzogranite.|
27117|Boyd Volcanic Complex|22580|6|Mentioned|p94|Late Devonian|Middle Devonian|||||||
27117|Boyd Volcanic Complex|22815|2|Defined|p92,93 fig28|Devonian|Devonian|||||||
27117|Boyd Volcanic Complex|22857|4|Described|p202, p215, p496 App.1 Tb.A1.7|Frasnian|Frasnian|Incorporates former "Eden Rhyolite". Includes Paradise Porphyry and Bunga beds. Frasnian age of sediments is indicated by fossil fish, with exception of basal Bunga beds which are probably Givetian, predating the onset of volcanism. Max. thickness: 1500m.||||||
27117|Boyd Volcanic Complex|22859|5|Briefly described|p202,215|||||||||
27117|Boyd Volcanic Complex|23278|6|Mentioned|Table3p93||Devonian|(Cas and Bull, 1993).||||||13-FEB-07
27117|Boyd Volcanic Complex|23309|5|Briefly described|p348||Late Devonian|Coeval with Gabo Suite of Vic.||||||
27117|Boyd Volcanic Complex|23327|4|Described|1009|Late Devonian|Late Devonian|||||||
27117|Boyd Volcanic Complex|23329|5|Briefly described|1046|Frasnian|Givetian|||||||
27117|Boyd Volcanic Complex|23456|4|Described|p49|Late Devonian|Late Devonian|||||||
27117|Boyd Volcanic Complex|23464|5|Briefly described|p249|Late Devonian|Late Devonian|||||||
27117|Boyd Volcanic Complex|23541|5|Briefly described|p398|||In the Lachlan Fold Belt.||||||13-FEB-07
27117|Boyd Volcanic Complex|24164|6|Mentioned|p17|Late Devonian|Late Devonian|This unit, about 30 km north of Victorian border, is considered coeval with earliest phases of Sydney-Bowen Basin system (Fergusson et al. 1979).||||||
27117|Boyd Volcanic Complex|24417|5|Briefly described|p114|||||||||
27117|Boyd Volcanic Complex|24551|6|Mentioned|p189||Frasnian|||||||
27117|Boyd Volcanic Complex|24580|5|Briefly described|p829|Late Devonian|Middle Devonian|Overlain by the Merrimbula Group. Geological Province: Eastern Lachlan Fold Belt.||||||
27117|Boyd Volcanic Complex|35526|2|Defined|p87|Late Devonian|Late Devonian|Discussion throughout paper||||||
27117|Boyd Volcanic Complex|37501|6|Mentioned|p414|||||||||
27117|Boyd Volcanic Complex|38320|6|Mentioned|p189|||||||||
27117|Boyd Volcanic Complex|38782|6|Mentioned|p53|||||||||
27117|Boyd Volcanic Complex|38899|6|Mentioned|p71|||||||||
27117|Boyd Volcanic Complex|39313|6|Mentioned|p280|||||||||
27117|Boyd Volcanic Complex|39626|6|Mentioned|p275|||||||||
27117|Boyd Volcanic Complex|40387|6|Mentioned|p137|||||||||
27117|Boyd Volcanic Complex|40646|4|Described|p23|||Mention p9.||||||13-FEB-07
27117|Boyd Volcanic Complex|41385|6|Mentioned|p373|||||||||
27117|Boyd Volcanic Complex|41430|6|Mentioned|p16|||||||||
27117|Boyd Volcanic Complex|41641|6|Mentioned|p189|||||||||
27117|Boyd Volcanic Complex|41919|5|Briefly described|p159|||||||||
27117|Boyd Volcanic Complex|42050|6|Mentioned|p227|||||||||
27117|Boyd Volcanic Complex|42726|5|Briefly described|map legend|Middle Devonian||||||||
27117|Boyd Volcanic Complex|42786|5|Briefly described|p359|||||||||
27117|Boyd Volcanic Complex|43129|6|Mentioned|p520|||||||||
27117|Boyd Volcanic Complex|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
27117|Boyd Volcanic Complex|44093|5|Briefly described|p222 App. 1|Givetian|Givetian|Geological Province: Lachlan Fold Belt.||||||
27117|Boyd Volcanic Complex|61181|5|Briefly described|p169|Late Devonian|Late Devonian|Comprises var.of volcanic rocks incl: agglomerates, basalts, and intrusive/extrusive rhyolites, tog.with intercalations of seds. Contains the Pambula deposit (NSW) of pyrophyllite - host rocks mainly flow-banded rhyolites, volcanic breccias, pyroclastics.||||||20-DEC-07
27117|Boyd Volcanic Complex|61964|6|Mentioned|p81|||A-type. Geological Province: Lachlan Orogen.||||||
27117|Boyd Volcanic Complex|62070|5|Briefly described|p34 Fig.1,|Late Devonian|Middle Devonian|||||||
27117|Boyd Volcanic Complex|62569|5|Briefly described|p606 Fig. 1A, p610 Fig. 4|Late Devonian|Middle Devonian|||||||
27117|Boyd Volcanic Complex|63605|5|Briefly described|p991, p993|Givetian|Eifelian|Of Fergusson et al (1979). Formerly the rocks were divided into "Eden Rhyolite" and "Lochiel Formation". The Complex includes the Bunga beds. Unconformably or disconformably  overlain by Merrimbula Group. An Emsian or Eifelian maximum age is possible.||||||07-FEB-11
27117|Boyd Volcanic Complex|66499|5|Briefly described|p61, p62 Fig.6|Middle Devonian|Early Devonian|Stratigraphically below the marine Bellbird Creek Formation; a published isotopic age of 395 +/- 4 Ma for igneous intrusives assumed to be contemporaneous is given by Williams (1992). Includes fish and plant fossils at several levels. |||Includes Bunga beds|?Unconformably underlies Twofold Bay Formation, Merrimbula Group.||
27117|Boyd Volcanic Complex|66768|6|Mentioned|p210 Fig.1, p210|||||||||
27117|Boyd Volcanic Complex|67847|5|Briefly described|p60 fig 3.3.4|||Eden-Comerong-Yalwal Rift. ||||||
27117|Boyd Volcanic Complex|68298|5|Briefly described|p214, p232, p233|||Interbedded with sediments containing fish faunas||||Is overlain by Merrimbula Group with local angular unconformities. Nonconformably overlies Bega Batholith units.|Rhyolites and basalts|
27117|Boyd Volcanic Complex|68592|5|Briefly described|p33|Middle Devonian|Middle Devonian|Eden-Comerong-Yalwal Volcanic Zone.|||||A-type felsic volcanics and associated plutons.|
27117|Boyd Volcanic Complex|70351|5|Briefly described|p55-56|||Described by Fergusson et al. 1979 to have eight facies associations, including the 'flyschoid facies', represented by the Bunga beds. Previous age interpretations include Late Devonian (Fergusson et al., 1979; Lewis et al., 1994), but have been superseded by an age of 395+\-4 Ma for granitic intrusives, however this numerical age may be unreliable (p56).|||Includes Bunga beds, Eden Rhyolite and Lochiel Formation.|||
27117|Boyd Volcanic Complex|70601|5|Briefly described|p25, p27-28, p31, p55, p58|Givetian|Eifelian|Onshore geology. Associated with A-type granites. Overlies Ordovician rocks and Bega Batholith. Age from fish fauna.||||Southern equivalent of Comerong Volcanics. Underlies Merrimbula Group. Is intruded by Gabo Suite.|Bimodal silicic and basaltic volcanics.|
27117|Boyd Volcanic Complex|70661|6|Mentioned|viii|||Major part of the Eden-Comerong-Yalwal Volcanic Zone.||||Correlated with Yawal Volcanics.||
27117|Boyd Volcanic Complex|71700|5|Briefly described|p29|Middle Devonian|Middle Devonian|||||||
27117|Boyd Volcanic Complex|73181|6|Mentioned|p62, p64-65, p67|Givetian|Eifelian|Of Fergusson et al. (1979). Includes the volcanics and associated sediments lying unconformably beneath the Upper Devonian strata in the Eden-Pambula district. Contains plant and fish fossils.|||Eden Rhyolite, Bunga beds|Underlain by Bunga beds. Overlain by Twofold Bay Formation.||
70026|Bradfordville Volcaniclastic Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Cream to grey-green massive to weakly stratified vitriclast-bearing coarse- to v.coarse-gr.crystal-rich volcanic sst. Comprises fragments of qtz, plagioclase, K-feldspar and mostly rhyolitic to dacitic lithics...||||||09-SEP-08
70026|Bradfordville Volcaniclastic Member|68592|2|Defined|p851-4, p857-8, p862, p864-8,p870,p873-4|Early Silurian|Early Silurian|See also p107-8, p726, p730 Fig.132, p732, p840, p883. New name. Crops out poorly. Type section in Kenmore Creek. Thickness: max ~850 m largely unconstrained by bedding measurements; and 170 m at type section. Sub-greenschist to possible lowest greenschist facies regional metamorphism. Age: early Lochkovian likely. A moderately deep marine to lacustrine depositional environment is suggested. Inferred displacement of c.35 km by Mulwaree Fault.||Unit in Gundary Volcanics.||Is overlain by 'upper' portion of Back Station Ignimbrite Member; conformably and erosionally overlies different parts of Rhyanna Formation; intruded by Forest Lodge Quartz Monzodiorite.|Pyroclastic; a basal, crystal-rich, rhyolitic, volcanic sandstone; cream, grey-green and bluish grey, generally unstratified, crystal-rich vitriclast-bearing volcanic sandstone, minor, very fine-grained vitric tuff or mudstone, and conglomerate.|
70026|Bradfordville Volcaniclastic Member|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfgr. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Gundary Volcanics||Overlies Rhyanna Formation. Is overlain by Back Station Ignimbrite Member.|Unstratified, crystal rich, vitriclast bearing rhyolitic volcanic sandstone, conglomerate and minor very fine-grained vitric tuff or mudstone; coarse grained volcaniclastic rocks have obvious K-feldspar.|
70026|Bradfordville Volcaniclastic Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Gundary Volcanics|||Unstratified, crystal rich, vitriclast bearing rhyolitic volcanic sandstone, conglomerate and minor very fine-grained tuff or mudstone; coarse-grained volcaniclastic rocks have obvious K-feldspar.|
70026|Bradfordville Volcaniclastic Member|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Gundary Volcanics|||Unstratified, crystal rich, vitriclast bearing rhyolitic volcanic sandstone, conglomerate and minor very fine-grained vitric tuff or mudstone; coarse grained volcaniclastic rocks have obvious K-feldspar.|
70026|Bradfordville Volcaniclastic Member|71069|6|Mentioned|p137 fig 44, p144|||Up to 770m thick.||Gundary Volcanics||Unconformably overlies the Rhyanna Formation.Also overlies the Forest Lodge Quartz Monzodiorite and Wombeyan Limestone.||
70026|Bradfordville Volcaniclastic Member|71700|5|Briefly described|CD|||Recognised in the Braidwood100 sheet area.||Gundary Volcanics||||
34467|Bradleys Creek Metamorphic Complex|22721|2|Defined|p507, Fig.1 p502|Middle Devonian|Silurian|||||||
31487|Braidwood Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Candelo Supersuite.  Includes the Braidwood Granite (informally named).||||||09-FEB-05
31487|Braidwood Suite|44093|5|Briefly described|p220 App. 1|Early Devonian|Early Devonian|Massive granites. Geological Province: Lachlan Fold Belt.||||||01-MAR-05
31487|Braidwood Suite|66300|6|Mentioned|p35. |||Eastern Lachlan Orogen plutons.||||||
31487|Braidwood Suite|68592|6|Mentioned|p1677, p1680 Fig.346||||||Includes Braidwood Granodiorite.|||
31487|Braidwood Suite|69159|5|Briefly described|Map legend|Devonian|Devonian||||Includes Euradux Granite and Braidwood Granodiorite.|||
31487|Braidwood Suite|69564|5|Briefly described|p5|Early Devonian|Early Devonian|Fitzherbert and Deyssing (in press).||Candelo Supersuite.|Braidwood Granodiorite.|||
31487|Braidwood Suite|71069|6|Mentioned|p175, p176, p189|Early Devonian|Early Devonian|||||||
31487|Braidwood Suite|71699|5|Briefly described|Map legend.|Devonian|Devonian||||Braidwood Granodiorite, Euradux Granite.|||
31487|Braidwood Suite|71700|2|Defined|vi, viii, ix, p7, p26, p28|Early Devonian|Early Devonian|Named for the town of Braidwood at GR 754107 6074135 which is also the source for the name of the type pluton, the Braidwood Granodiorite. The Warri and part of the Glenrossal granites of the Warri Suite are now recognised as extensions of the Braidwood Granodiorite. Thus the Braidwood Granodiorite now incorporates and replaces the Warri Suite. Rocks previously mapped as Boro Granite have been recognised as belonging to the Braidwood Suite. See also p36-p38, p42, p57, p65, p76, p80-p81, p98, CD. This suite also includes three unnamed subunits. Distribution, geomorphic expression, outcrop, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. Age is derived from SHRIMP U-Pb dates obtained for the Braidwood Granodiorite. Equivalent to other suites in the Candelo Supersuite. Unconformably overlain by the Minuma Range Group.||Candelo Supersuite|Includes the Braidwood Granodiorite and Euradux Granite.|Faulted against the Glenbog Suite. Intrudes the Abercrombie Formation, Bendoc Group, Mundoonen Sandstone, Cardinal View Formation, Bindook Group and De Drack Formation.|Granite to granodiorites, leucogranites, aplites and pegmatitic dykes also belong to this suite.|
82370|Branch Swamp Monzogranite|71628|5|Briefly described|p15: 35, 47-48, 58, 116|||New name, after a local feature. Forms a broad ovoid intrusion immediately S of Boonoo Boonoo Falls. A single geochemical analysis is described.||Surface Hill Suite (tentative).||Intrudes Mount Lindesay Monzogranite. Is entirely surrounded by Stanthorpe Complex granites.|Pink, medium-grained, equigranular granite. I-type.|
26422|Brandy Springs beds|41347|4|Described|Table 4|||||||||
26422|Brandy Springs beds|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Part of the "Sandon Association".||||||16-DEC-04
26422|Brandy Springs beds|71628|5|Briefly described|p3:76|||||Sandon Association.||Is intruded by Murder Dog Monzogranite.||
31717|Brangan Volcanics|13139|5|Briefly described|p9 Fig. 4, p11|||Geological Province: Cowra Trough.||||||
31717|Brangan Volcanics|22434|6|Mentioned|11 fig 15|||Grenfell area. Geol province Lachlan Fold Belt||||||
31717|Brangan Volcanics|23334|5|Briefly described|9 Fig.4|Silurian|Ordovician|||||||
31717|Brangan Volcanics|24215|5|Briefly described|p801|||Parent: Jindalee Group.  Geological Province:  Lachlan Fold Belt||||||
31717|Brangan Volcanics|24417|3|Fully described|p7|Late Ordovician|Middle Ordovician|Originally included as part of the now discarded "Hoskins Formation". Now included as part of the Jindalee Group. Contacts with Kirribilli Formation (probably faulted) and Hoskins Chert (probably equivalent) are not exposed. Slab enclosed by Grenfell Granite is considered to be a roof pendant.||||||25-MAR-20
31717|Brangan Volcanics|50628|5|Briefly described|Map Legend|Ordovician|Ordovician|Fine to medium grained metadolerite and basalt.||||||05-JUL-04
31717|Brangan Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Basalt and chert.||||||
31717|Brangan Volcanics|60009|5|Briefly described|Map Legend|Eastonian|Darriwilian|Of the Jindalee Group.||||||13-JUL-04
31717|Brangan Volcanics|63278|6|Mentioned|p145 Fig. 1|Ordovician|Ordovician|||||||07-FEB-11
31717|Brangan Volcanics|63289|5|Briefly described|p372|||Of Jindalee Group. Geological Province: Junee - Narromine Volcanic Belt. Consists of basalts and dolerites.||||||07-FEB-11
31717|Brangan Volcanics|67322|5|Briefly described|p20|Pridoli|Ludlow|Lyons, Duggan and Wallace, in Lyons et al. (2000). Age constrained by that of the parent Jindalee Group: an Ordovician fragmented ophiolite sequence within a Silurian sedimentary matrix. On Tumut 1:100 000 sheet: (Basden 1990).||Of the Jindalee Group||||21-FEB-18
31717|Brangan Volcanics|68466|6|Mentioned|p66|||Crops out N and S of Grenfell.||Jindalee Group.||||
31717|Brangan Volcanics|69668|6|Mentioned|p932|Silurian|Silurian|Exposed north and south of Grenfell.||Unit in Jindalee Group.||||
31717|Brangan Volcanics|70684|6|Mentioned|p3|||||||||
31717|Brangan Volcanics|72495|6|Mentioned|p233|||||Jindalee Group.|Includes the Hoskins Chert Member.|||
32509|Brassington mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
40188|Brawlin Formation|50191|5|Briefly described|p6, 21 Fig. 1|Silurian|Silurian|Interfingers with or underlies: Honeysuckle beds.||||||08-DEC-04
40188|Brawlin Formation|60280|2|Defined|p1-2|Early Silurian|Early Silurian|Formerly the Blowering Formation.  Contains the Fencers Creek Conglomerate Member.||||||12-AUG-04
74536|Brayton Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Longreach Volcanics (Mount Fairy Group). White to cream bedded fossiliferous marble.||||||03-JUN-08
74536|Brayton Limestone Member|68592|2|Defined|p726, p847-50, p916, p1891|Lochkovian|Lochkovian|New name. Modified after Naylor (1950) first used 'Brayton limestone'. Use of term Brayton in 'Brayton volcanics' by O'Reilly (1972) is considered invalid (Carr et al. 1979). This limestone lens occurs near top of Longreach Volcanics. Contains sparse conodonts, giving an Early Devonian, probably early Lochkovian, age. Type section located. Thickness: estimated ~30 m, though poor outcrop. This unit is distinguished as a recrystallised limestone lens enclosed by mafic volcanic rocks. Brayton Limestone Member may overlap in age with the top of the Frome Hill Formation (Bungonia Group).||Enclosed by Longreach Volcanics.||Intruded by Lockyersleigh Granite; correlated with Gundary Volcanics.|Marine limestone is coarsely recrystallised to white marble with a grainsize of up to about 1 mm; outcrop is white to cream with fossil material (crinoid ossicles and, rarely, crinoid stems) obvious on weathered surfaces.|20-SEP-16
74536|Brayton Limestone Member|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sflb. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Longreach Volcanics||Is within undifferentiated Longreach Volcanics.|White to cream, bedded, fossiliferous marble.|
74536|Brayton Limestone Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Longreach Volcanics|||White to cream, bedded, fossiliferous marble.|
74536|Brayton Limestone Member|71656|5|Briefly described|p13 Fig.2, p30|Pragian|Lochkovian|Described in text (p30) as younger Lochkovian to Pragian age.||Longreach Volcanics||Mount Fairy Group. Within Longreach Volcanics.|Fossiliferous limestone.|
81965|Breadknife Trachyte Member|72700|5|Briefly described|Mapsheet 2|Cenozoic|Cenozoic|||Mount Naman Formation|||Pale orange-white lava deposits and intrusions that contain small, variable-sized crystals and are faintly banded.|
23416|Break O'Day Amphibolite|730|6|Mentioned|p19.|||West of Bobadah. Contains metamorphosed limestone.||||||11-NOV-14
23416|Break O'Day Amphibolite|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
23416|Break O'Day Amphibolite|42566|3|Fully described|p26|||||||||
23416|Break O'Day Amphibolite|42568|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
23416|Break O'Day Amphibolite|43089|5|Briefly described|Map Legend|||of Girilambone Group||||||
23416|Break O'Day Amphibolite|65469|6|Mentioned|p16|||Lachlan Orogen.||||||
23416|Break O'Day Amphibolite|67322|5|Briefly described|p20|Darriwilian|Tremadocian|On the Bobadah 1:100 000 map sheet (Pogson, 1991). Age from the parent Girilambone Group. Occurs in the Condobolin - West Wyalong region.||Of the Girilambone Group||||21-FEB-18
23416|Break O'Day Amphibolite|70751|5|Briefly described|p5, p12, p26|Ordovician|Ordovician|Age is interpreted on the basis of unit relationships.||Girilambone Group.||Intruded by the Erimeran Granite.|Mafic amphibolitic rocks.|
23416|Break O'Day Amphibolite|70828|5|Briefly described|p2,4-8,10,13-17|Ordovician|Ordovician|Situated 13km southwest of Bobadah. Originally defined by Pogson (1991a). Occurs as a series of NNW-trending elogate basaltic rock bodies within metasediments of Girilambone Group; variably altered to calc-silicate skarn assemblages. Also occurs adjacent Erimeran Granite. Deformed by Late Ordovician-Early Silurian Benambran Orogeny (Burton et al., 2012). Geochemical analysis indicate an alkaline within-plate basaltic affinity, likely originating from a seamount within oceanic arc environment. Exhibits similar remnant magnetisation to Mount Dijou Volcanic Member and Kaiwilta Member of the Narrama Formation, Girilambone Group.||Girilambone Group.||Hosted within Girilambone Group.|Amphibolite, meta-basalt, calc-silicate rock.|11-DEC-19
23416|Break O'Day Amphibolite|72908|6|Mentioned|p25||||||||Mafic unit.|
25809|Breckin Ignimbrite Member|22857|5|Briefly described|p508 App.1 Tb.A1.8|Visean|Visean|Of the Mowbray Formation (Gilmore Volcanic Group). Basal grey andesitic ignimbrite overlain by red ignimbrite. Max. thickness: 20m. Geological Province: Tamworth Forearc Basin.||||||
25809|Breckin Ignimbrite Member|24121|5|Briefly described|p4|||Of Mowbray Formation.||||||25-AUG-22
25809|Breckin Ignimbrite Member|31228|2|Defined|p82|Carboniferous|Carboniferous|||||||
25809|Breckin Ignimbrite Member|44244|5|Briefly described|p93|||Of the Mowbray Formation.  Grey andesitic ignimbrite overlain by red ignimbrite with crystals of oligoclase, hornblende and biotite in a welded matrix of glass shards. Max. thickness: >20m.  Type section in text.  Geological Province: Gresford Block.||||||
25809|Breckin Ignimbrite Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Mowbray Formation (Gilmore Volcanic Group).||||||
25809|Breckin Ignimbrite Member|50268|5|Briefly described|Map Legend|Visean|Visean|Of the Mowbray Formation.  Geological Province: Gresford Block.  Overlies: Newtown Formation.||||||
25809|Breckin Ignimbrite Member|73487|6|Mentioned|p566|||||||||
76052|Breeza Coal Member|65116|6|Mentioned|p448|Late Permian|Late Permian|Low energy fluvial deposits including coal. Top of Sequence D2.||||||05-AUG-11
79467|Brevelon Tank Quartzite|70602|4|Described|p67-72,74,75,78|Middle Ordovician|Early Ordovician|Southern extremity of the Louth-Eumarra Shear Zone. Age inferred by inclusion in Girilambone Group p68. Metamorphosed thick sand package within surrounding metasedimentary rocks of Girilambone Group. Lithology compared to Budgery Sandstone Member. Petrographic and structural descriptions and map given. Silicification obscures primary sedimentary features, such as bedding and grainsize, in the field. Aeromagnetic map data given. This is a different unit to the informal ?igneous Siluro-Devonian Brevelon Unit shown in Fig 3 and Fig 8.|inferred structural data already formed c435 Ma|Girilambone Group||Rare subcrop exposures of interlaminated metasiltstone and metasandstone from the Girilambone Group were found adjacent to the Brevelon Tank Quartzite.|Quartzite, poorly sorted subrounded to angular quartz clasts with undulose extinction, in a matrix of finer aligned quartz grains and minor muscovite grains that define a foliation.|27-JUN-16
78458|Brewarrina Granite|68823|5|Briefly described|p378 Fig.4, p394, p399|Pridoli|Pridoli|Thomson Orogen.|421 Ma, SHRIMP-IIe U-Pb (Bodorkos et al. 2013)||||S-type granite.|13-JUL-16
78458|Brewarrina Granite|69042|5|Briefly described|map, map legends|Devonian|Silurian|Thomson Orogen? ?Low-magnetic intensity.||||||
78458|Brewarrina Granite|69541|5|Briefly described|p645 Fig.1(b)|Late Silurian|Late Silurian|Thomson Orogen.|421 Ma.|||||
78458|Brewarrina Granite|69635|5|Briefly described|p159|Early Devonian|Late Silurian||~420 Ma|||||
78458|Brewarrina Granite|70602|5|Briefly described|p65-67,72|Early Devonian|Late Silurian|Found north of the Louth-Eumarra Shear Zone. Aeromagnetic map data given.|420.9+/-2.3Ma||||S-type granite.|
78458|Brewarrina Granite|70821|6|Mentioned|p9-10, p13 Tb.2.1|Early Devonian|Late Silurian||420.9 +/- 2.3 Ma (Bodorkos et al., 2013).||||Granite.|01-DEC-16
78458|Brewarrina Granite|71360|5|Briefly described|Map legend|Late Silurian|Late Silurian|Geophysical signature: non-magnetic unit with contacts defined by increased magnetic intensity (interpreted as a weak aureole effect in metasedimentary rocks). Zones of very high radioelement values suggest unmapped exposures exist.|420 +/- 2.4 Ma.||||White feldspar S-type granite with biotite and cordierite, aplite.|
78458|Brewarrina Granite|71860|5|Briefly described|p7|||Age is a SHRIMP U-Pb date.|420.9 +/- 2.3 (Bodorkos et al. 2013)||||Granite.|
78458|Brewarrina Granite|71965|5|Briefly described|p903-904,910,913|||Geological province: Thomson Orogen. S-type granite occuring in the Gumbercoo zone immediately north of the Mount Oxley Fault, with a magmatic crystallisation age of 420.9+\-2.3 Ma, which was represents the minimum depositional age of the host metasediments. Includes 1729 Ma to 1108 Ma and 872 Ma to 466 Ma inherited zircon populations.|420.9+\-2.3 Ma (Magmatic)|||||
78458|Brewarrina Granite|72522|6|Mentioned|p10.|Lochkovian|Silurian|Magmatic age Bodorkos et al., 2013.  Age indistinguishable from nearby dated granodiorite at Glen Idol prospect (421.9+/-3.5 Ma) and Glenariff Granite (422.7+/-2.4 Ma).|420.9 +/- 2.3 Ma||||Includes granite.|
78458|Brewarrina Granite|72915|6|Mentioned|p17|||[Formal or informal use is not explicit].||||||
78458|Brewarrina Granite|72951|5|Briefly described|p1013-1014, p1020, p1025-1026, p1028|Lochkovian|Ludlow|Thomson Orogen, southeast. S-type. SHRIMP U-Pb zircon isotope analyses from Bodorkos et al. (2013). eHf = -6.5 +/- 0.5, and d18O = 9.16 +/- 0.23.|420.9 +/- 2.3 Ma||||Medium-grained biotite-cordierite granite.|
78371|Brewarrina granite|69002|5|Briefly described|p9, Map 1b|Pridoli|Pridoli|Occurs in the eastern Thompson Orogen. Contains significant inherited and xenocrystic zircons - the youngest two of which yielded a U-Pb age of ~467 Ma.|c.421 Ma, SHRIMP II-e (Geoscience Australia)||||S-type granite.|
78371|Brewarrina granite|69043|4|Described|p3, p5-6, p11, p86-92, p96, p118|Late Silurian|Late Silurian|Thomson Orogen. Aeromagnetic patterns indicate several NE-trending plutons. This age is indistinguishable from the Glenariff granite (422.7 +/- 2.4 Ma).|420.9 +/- 2.3 Ma.||||White, coarse-grained, equigranular, biotite- and cordierite-bearing alkali-feldspar granite. Crosscut by aplite dykes. S-type.|
78371|Brewarrina granite|69541|6|Mentioned|p644 Fig.1(a)|||Thomson Orogen.||||||
35709|Briarlee Granite|50231|5|Briefly described|Map Legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
35709|Briarlee Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Pinkish-cream to leucocratic, medium- to coarse-grained, massive to locally foliated,  equigranular to porphyritic biotite granite and granodiorite.||||||16-JUN-08
35709|Briarlee Granite|68592|3|Fully described|p1379-84|Late Silurian|Late Silurian|New name, after Briarlee property. Previously included in the Whistle Waa Granite of Chappell et al. (1991). Part of the Wyangala Batholith. Type locality described. Geochemistry detailed; geophysical properties described and discussed. Not isotopically dated: age from Wyangala Batholith. May be a composite body or contaminated during intrusion.||||Intrudes Wyangala Granite and Cocomingla Complex.|Pinkish cream to leucocratic, medium- to coarse-grained, massive to locally foliated, equigranular to porphyritic biotite granite (in the S) and granodiorite (in the N) with muscovite-bearing pegmatite dykes. I-type granite; A-type granodiorite.|
35709|Briarlee Granite|70192|5|Briefly described|Map Legend|Lochkovian|Pridoli|Sxb. Includes one unnamed subunit of pegmatite dykes. Ungrouped Silurian intrusion. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||Includes one unnamed sub unit.||Leucocratic, medium-coarse grained, massive-locally foliated, equigranular-porphyritic biotite granite and granodiorite.|
35709|Briarlee Granite|70545|5|Briefly described|Map Legend |Silurian|Silurian|Includes one unnamed subunit of pegmatite dykes.|||||Leucocratic, medium-coarse grained, massive-locally foliated, equigranular-porphyritic biotite granite and granodiorite.|20-SEP-17
78993|Briars Sharrow Gabbro|71069|4|Described|p21 fig 7, p29, p29 fig 11, p36|Ludlow|Wenlock|Named for Briars Sharrow Road. Previously mapped as unnamed gabbro/dolerite (Abell 1991) unnamed intermediate basic rocks (best et al 1964) and unnamed basic rocks (1953). Type area given at GR 717081 6093100. Tholeiitic geochemical affinity. Geochemically similar to the gabbro-dolerite phase of the Lockhart Igneous Complex and basalt of the Currawang Basalt and Captains Flat Formation. Distribution, geomorphology, primary textures, geochemistry, tectonic structure and metamorphism discussed. See also  p104 fig 32, p111, p174, p175, p179, p185, p197-p199.||Thurralilly Suite||Intrudes the Captains Flat Formation and the Hoskinstown Group. Equivalent to the Butmaroo Granite, Ellenden Granite, Gourock Granodiorite and the Tallaganda Granodiorite.|Grey to green, massive, medium to very coarse-grained, gabbro with some fine to medium-grained dolerite.|
78993|Briars Sharrow Gabbro|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Thurralilly Suite.|||Grey to green, massive, medium- to very coarse-grained gabbro, with some fine- to medium-grained dolerite.|
36405|Bridle Creek Dolerite|50126|2|Defined|p76, p77, p83 App.2|Middle Eocene|Middle Eocene|Of the Monaro Volcanics.  Age: 44.5 +/- 0.6 Ma (K/Ar).  Thickness at Type Section: ~5m.  Relatively coarse-grained basaltic rock.||||||27-MAY-04
30030|Brigalow Formation|22857|4|Described|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Brothers Subgroup (Black Jack Group). Fining-up sequence of medium to coarse-grained quartzose sandstone and siltstone. Max. thickness: 28m. Geological Province: Gunnedah Basin.||||||
30030|Brigalow Formation|24159|5|Briefly described|p149|Permian|Permian|Geological Province: Gunnedah Basin.||||||
30030|Brigalow Formation|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Of Brothers Subgroup. New, formal name for the 'lower quartz sandstone unit' in Black Jack Formation (now Black Jack Group). Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||13-NOV-13
30030|Brigalow Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Brothers Subgroup.||||||
30030|Brigalow Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Brothers Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Quartz sandstone and siltstone.||||||17-SEP-08
30030|Brigalow Formation|65116|5|Briefly described|p447, 448, Fig 6 p441|Late Permian|Late Permian|?Of Black Jack Group. Coarse grained pebbly quartzose sandstone. Channel deposits. Sequence boundary at base.||||||
30030|Brigalow Formation|68003|5|Briefly described|p38 Fig.3-j, p41, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Coeval with Arkarula Formation. Alluvial deposits sourced from Lachlan Fold Belt. Bed-load fluvial sediments.||Unit in Brothers Subgroup.||Overlies Pamboola Formation. Is overlain by Hoskissons Coal.|Fining-up sequence of medium-grained quartzose sandstone and siltstone.|
30030|Brigalow Formation|68004|5|Briefly described|p23 Table 1, p176.|Late Permian|Late Permian|Gunnedah Basin. Considered prospective for hydrocarbons; typical porosities of 15 - 20% and good permeabilities.||Upper unit in Brothers Subgroup.||Overlies Pamboola Formation. Is overlain by Hoskissons Coal.|Includes sandstone beds up to 20 m thick.|
30030|Brigalow Formation|70791|5|Briefly described|p277|Permian|Permian|Gunnedah Basin.||Brothers Subgroup.||||
30030|Brigalow Formation|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Overlies Arkaroola Formation. Is overlain by Hoskisson Coal.||
29525|Brittlejack Granite|23214|5|Briefly described|p255|Carboniferous|Carboniferous|Of Lewis Ponds Granite. An elongate shape of approximately 450m x 150m.||||||
29525|Brittlejack Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
29525|Brittlejack Granite|43782|6|Mentioned|Map Legend|Early Carboniferous|Early Carboniferous|of Lewis Ponds Granite.||||||
80143|Britton Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Werrie Basin. Shown only as Britton. Ending assumed from references to other Coal Members in text.||Rowan Formation.||||28-SEP-17
77058|Brogans Creek Limestone Member|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Carwell Creek Formation||||
70467|Brogans Rhyodacite Member|62095|2|Defined|p279 Appdx.|Permian|Permian|Of the Woodton Formation. Red to pink lava flow with small folds is interbedded with multicoloured siltstone, volcanolithic sandstone and pebble to cobble conglomerate. Age: 290.5+/-2.8Ma. Thickness: ~8m.  See also Plate 1, p259.||||||
70467|Brogans Rhyodacite Member|65114|5|Briefly described|p395|Sakmarian||Of Woodton Formation. SHRIMP age of 290.5 +/- 2.8 Ma; stratigraphically below the Temi Formation and Werrie Basalt||||||
30475|Brogo Granodiorite|22815|4|Described|p69|||||||||
30475|Brogo Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Brogo Suite.||||||
30474|Brogo Suite|22815|6|Mentioned|p69|Early Devonian|Late Silurian|||||||
30474|Brogo Suite|22878|6|Mentioned|p83|||||||||
30474|Brogo Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Cobargo Supersuite.  Includes the Brogo Granite (informal name).||||||09-FEB-05
30474|Brogo Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Bega Batholith.||||||
23424|Broken Cart Granodiorite|36441|5|Briefly described|map legend|Pridolian|Late Silurian|Of Young Batholith. Intrusive. S-type. Granodiorite, porphyritic granodiorite, minor adamellite. BMR map code: Syb.||||||
23424|Broken Cart Granodiorite|36443|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Young Batholith. Intrusive. Granodiorite, adamellite. S-type. BMR map code: Syb.||||||
23424|Broken Cart Granodiorite|37529|6|Mentioned|p5|||||||||
23424|Broken Cart Granodiorite|39660|6|Mentioned|p449|||||||||
23424|Broken Cart Granodiorite|42313|6|Mentioned|p135|||Subdivision of Young Granodiorite||||||
23424|Broken Cart Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb7.||||||
23424|Broken Cart Granodiorite|45147|2|Defined|M234|Late Silurian|Late Silurian|Prob.Late Silurian||||||
23424|Broken Cart Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
26255|Broken Range Group|22768|5|Briefly described|p170-71|||||||||
26255|Broken Range Group|22857|6|Mentioned|p170|||Of the Cobar Supergroup. Turbiditic sediments. Max. thickness: 2.3km. Geological Province: Cobar Basin.||||||
26255|Broken Range Group|22887|3|Fully described|p23, Fig.4 p11|Middle Devonian|Early Devonian|||||||
26255|Broken Range Group|23252|5|Briefly described|Map Legend||Early Devonian|part of the initial Cobar Basin development.||||||
26255|Broken Range Group|37772|6|Mentioned|p2|||||||||
26255|Broken Range Group|40269|4|Described|p144|||||||||
26255|Broken Range Group|40913|6|Mentioned|Map legend|Zlichovian|Pragian|Zlichovian-Pragian||||||
26255|Broken Range Group|41126|2|Defined|p70|Early Devonian|Early Devonian|||||||
26255|Broken Range Group|41394|6|Mentioned|p10|||See also P95||||||
26255|Broken Range Group|41528|6|Mentioned|p19|||||||||
26255|Broken Range Group|41821|6|Mentioned|p24|||In Mount Allen sheet area||||||
26255|Broken Range Group|42144|5|Briefly described|p605|||||||||
26255|Broken Range Group|42521|5|Briefly described|p15, Fig 3 p16|||||||||
26255|Broken Range Group|43089|5|Briefly described|Map Legend|||Of Cobar Supergroup.||||||03-JUN-08
26255|Broken Range Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
26255|Broken Range Group|61964|6|Mentioned|p140|||Mentioned only in terms of equivalents of the Olney Formation (Renmark Group).||||||27-OCT-08
26255|Broken Range Group|63891|5|Briefly described|p237|Early Devonian|Early Devonian|Interpreted as overlying Mount Hope Group. Age: late Early Devonian.||||||
26255|Broken Range Group|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, App A-VI 3.||||||
26255|Broken Range Group|69163|5|Briefly described|Map legend|Early Devonian|Early Devonian||||||Undifferentiated lithic and muddy sandstone, minor pebble conglomerate beds, siltstone, mudstone and shale.|
26255|Broken Range Group|70751|5|Briefly described|p4-p6, p12-p13, p15|Devonian|Late Silurian|Cobar Superbasin, Mount Hope Trough. David (2005) suggested these form the sag phase of the Mount Hope Trough.|||||Fine- to coarse-grained clastic sedimentary rocks.|
26255|Broken Range Group|70950|5|Briefly described|p1028-1029,1032,1034, 1035|Early Devonian|Late Silurian|Geological province: Mount Hope Trough, Central Lachlan Orogen. Hosts gold mineralisation in the Mount Solar Au mine.|||||Medium- and fine-grained micaceous sandstones and siltstones; undeformed thinly bedded to laminated shale, wacke, some intraclastic breccia horizons. The sequence becomes shale-rich and sandstone-poor, well-defined slaty cleavage.|
26255|Broken Range Group|71039|6|Mentioned|p6, p21|Devonian|Silurian|||||||
26255|Broken Range Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|||Massive to graded to parallel-laminated and ripple cross-laminated, poorly sorted, fine- to medium-grained, quartzose to lithic sandstone and interbedded siltstone. Minor pebbly sandstone, conglomerate, coherent rhyolite volcanics.|
26255|Broken Range Group|72908|6|Mentioned|p3-4, p7, p14|Lochkovian|Pridoli|Mount Hope Trough. Hosts the Mount Hope and the Mount Solar deposits.|||||Includes fine- to coarse-grained clastic rocks.|
26255|Broken Range Group|72958|6|Mentioned|p8, p11|Lochkovian|Pridoli|Cobar Basin. Nymagee area.||||Equivalent to Mount Hope Group, Amphitheatre Group.||
26255|Broken Range Group|73578|6|Mentioned|p2|||Cobar Basin.||||||
35393|Bromley Hills Formation|61392|4|Described|p163-165, p170|Early Carboniferous|Middle Devonian|Of the Silverwood Group (Keinjan Terrane). Sand-rich point-source submarine fan. Max. thickness: 1720m.||||||07-FEB-11
35393|Bromley Hills Formation|63731|5|Briefly described|Map legend||Silurian|Of Silverwood Group. Includes the Long Mountain Breccia Member. Very thick-bedded, amalgamated, coarse, volcaniclastic arenite; and thin-bedded volcaniclastic arenite/mudstone turbidites punctuated by gravel-rich bands and debris-flow deposits.||||||12-DEC-07
35393|Bromley Hills Formation|63748|4|Described|p7 Fig. 3, p8|Late Devonian|Middle Devonian|Of Silverwood Gp. Includes Long Mountain Breccia Member at base. Unconformable on Bald Hill Fm and Ormoral Volcanics; unconformable below Eight Mile Creek beds. Max.thickness: ~1720m. Geol.Prov: Silverwood province. Sand-rich volcaniclastic turbidites.||||||07-FEB-11
35393|Bromley Hills Formation|68679|4|Described|p445-447|Mississippian|Middle Devonian|Van Noord (1999). Silverwood Province. ~1720m thick. Sandy volcaniclastic turbidites. Similar to parts of the Texas beds.||Topmost Silverwood Group.|Long Mountain Breccia Member.|Unconformably overlies Bald Hill Formation and Ormoral Volcanics. Is faulted locally against Bald Hill Formation and Connolly Volcanics. Is overlain by Eight Mile Creek beds.|Basal polymict megabreccia overlain by two units: one typified by thin-bedded turbidites with interbedded gravel-rich bands and debris-flow deposits, and a second unit dominated by very thick-bedded amalgamated coarse-grained turbidites.|
35393|Bromley Hills Formation|73600|6|Mentioned|p204|Devonian|Devonian|New England Orogen.||||||
29574|Bronxhome Formation|22638|4|Described|p21|Late Ordovician||New name.||||||
29574|Bronxhome Formation|22857|5|Briefly described|p418 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Interbedded arentie, siltstone and shale, occasional chert.||||||
29574|Bronxhome Formation|44192|5|Briefly described|Map Legend|Llandoverian|Eastonian|||||||
29574|Bronxhome Formation|44936|5|Briefly described|Map Legend||Ordovician|||||||
29574|Bronxhome Formation|65890|6|Mentioned|p159|Early Silurian|Late Ordovician|Sedimentary rocks. Intruded by Middledale Gabbroic Diorite.||||||13-APR-11
29574|Bronxhome Formation|67322|5|Briefly described|p20|||Warren et al. (1995). Occurs in the Parkes-Forbes-Junee area.||||Possible equivalent of the Kirribilli Formation.||21-FEB-18
29574|Bronxhome Formation|67847|5|Briefly described|p21-p22|||||||Equivalent to the Kirribilli, Cotton and Jingerangle Formations.|Inter-bedded sandstones, siltstones and slate.|
29574|Bronxhome Formation|72082|5|Briefly described|p22|Late Ordovician|Late Ordovician|Warren et al. (1995). Has similar age, lithology, metamorphic facies, bedding strike/dip, folding and interpreted turbiditic depositional environment, as the Trigalong, Bribbaree and Illabo Formations. No confirmed age; has an Early Silurian intrusion.||||Is intruded by the Wallundry Suite.||
28402|Brooklana beds|22857|5|Briefly described|p514 App.1 Tb.A1.8|Carboniferous|Carboniferous|Included in the informal "Coffs Harbour Association". Thinly bedded siliceous mudstone and siltstone with rare lithofeldspathic wacke. Several kilometres thick. Geological Province: Texas-Coffs Harbour Slope and Basin.||||||
28402|Brooklana beds|23720|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Part of the "Coffs Harbour Association".  Thinly bedded siliceous mudstone and siltstone with rare lithofeldspathic wacke, locally chert, jasper, magnetite-bearing chert and metabasalt.||||||08-DEC-04
28402|Brooklana beds|23811|5|Briefly described|Map Legend|Westphalian|Tournaisian|Part of the "Coffs Harbour Association".  Thinly bedded siliceous mudstone and siltstone with rare lithofeldspathic wacke, locally chert, jasper, magnetite-bearing chert and metabasalt.||||||08-DEC-04
28402|Brooklana beds|23812|5|Briefly described|p10, p12 Tb.1|Late Carboniferous|Early Carboniferous|Part of the 'Coffs Harbour Sequence' (Fergusson, 1982) or 'Coffs Harbour Association'.||||||
28402|Brooklana beds|37489|5|Briefly described|p262|||||||||
28402|Brooklana beds|40177|6|Mentioned|p47|||||||||
28402|Brooklana beds|44450|3|Fully described|p14 Table 2|Late Carboniferous|Late Carboniferous|Geological Province: Coffs Harbour Block. Max. thickness: >1000 m.||||||
28402|Brooklana beds|60079|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of the Coffs Harbour beds.||||||
28402|Brooklana beds|71628|5|Briefly described|p2: 20, 45, 49; p3: 27-28; p11-20|Carboniferous|Carboniferous|See also p17: 28, 48, 51, 91; p19: 137, 165. Coffs Harbour Block. Westphalian to Tournaisian. Associated with As-Au mineralisation (prospect named). RELATED UNITS (continued): Is also intruded by Big Bull Gabbro; and Bruisers Creek Granodiorite Phase (of Mount Mitchell Monzogranite); also faulted against this last.||Coffs Harbour Association.||Is intruded by Charon Creek Quartz Diorite; Dundurrabin, Billys Creek, Newto Boyd and Guy Fawkes Granodiorites; Tuting Monzogranite; see COMMENTS for more.||
34254|Brooklyn Conglomerate Member|22678|4|Described|p715-16,724||Early Devonian|Quartzose sandstone, siltstone and local fan-delta conglomerate deposits.||||||17-JAN-06
34254|Brooklyn Conglomerate Member|50234|5|Briefly described|Map Legend|Pragian|Lochkovian|Of the Tangerang Formation (Bindook Volcanic Complex).||||||
34254|Brooklyn Conglomerate Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Tangerang Formation (Bindook Group). Massive to diffusely bedded cobble to boulder conglomerate, containing clasts to 60cm of quartz arenite, siltstone and mudstone, increasing interbeds of graded quartz arenite towards the top.||||||09-SEP-08
34254|Brooklyn Conglomerate Member|68592|3|Fully described|p1061, p1064, p1083, p1098-1101|Early Devonian|Early Devonian|First described by Jones, Carr et al. (1984), but formally defined by Jones, Hall et al. (1986), after Brooklyn property. Type section described. Up to 60m thick. Clasts sourced solely from underlying Adaminaby Group. Geochemistry unknown; geophysical properties briefly described. Fossils are rare and not age-diagnostic. Probably time-correlative of Sharpeningstone Conglomerate.||Basal unit in Tangerang Formation.||Unconformably overlies Abercrombie Formation. Correlated with Bullamalita Conglomerate.|Diffusely bedded, massive to rarely normally graded, cobble to boulder conglomerate interbedded with normally graded and cross-bedded, pebbly and coarse-grained sandstone; graded sandstone beds to 1m thick more abundant near the top of the unit.|
34254|Brooklyn Conglomerate Member|70661|6|Mentioned|p55|||||||||
34254|Brooklyn Conglomerate Member|71700|5|Briefly described|p23-p24, p27|||Occurs in the Goulburn 250k map sheet.||Tangerang Formation||Equivalent to the Jinglemoney and Larbert Conglomerates.||
26426|Broonie Coal Member|29942|4|Described|Fig.1|||Permian||||||
26426|Broonie Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26426|Broonie Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26426|Broonie Coal Member|40805|6|Mentioned|Table 1|||||||||
26426|Broonie Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Burnamwood Formation.||||
29587|Brothers Creek Granite|23214|5|Briefly described|p255|Carboniferous|Carboniferous|Of Lewis Ponds Granite. An elongate shape of approximately 450m x 250m.||||||
29587|Brothers Creek Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
29587|Brothers Creek Granite|43782|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|of Lewis Ponds Granite.||||||
30028|Brothers Subgroup|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Black Jack Group. Includes the Brigalow, Arkarula and Pamboola Formations. Geological Province: Gunnedah Basin.||||||
30028|Brothers Subgroup|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Of Black Jack Group. Encompasses newly defined Pamboola, Brigalow and Arkarula Formations. Age Lower Stage 5a-5c. Formal definition published in an article released immediately prior to this article, however a summary of new nomenclature is provided in Appendix 1.||||||13-NOV-13
30028|Brothers Subgroup|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin.  Of the Black Jack Group. Underlies: Coogal & Nea Subgroups.  Overlies: Watermark Formation.||||||05-JUL-04
30028|Brothers Subgroup|68003|5|Briefly described|p38 Fig.3-j, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion.||Basal unit in Black Jack Group.|Includes Pamboola, Brigalow and Arkarula Formations.|Overlies Watermark Formation. Is overlain by Coogal Subgroup.||
30028|Brothers Subgroup|68004|5|Briefly described|p23 Table 1. |||Gunnedah Basin.||Lower unit in Black Jack Group.|Includes Pamboola, Brigalow and Arkarula Formations.|Overlies Millie Group. Is overlain by Coogal Subgroup.||
30028|Brothers Subgroup|70791|5|Briefly described|p277|Permian|Permian|Gunnedah Basin.||Black Jack Group.|Pamboola, Brigalow, Arkarula Formations.|||
29521|Broula Granite|23214|3|Fully described|p210|Early Devonian|Early Devonian|Originially included in the Young Granite and the Bumbaldry Granite. May intrude the Young Granodiorite. I-type granite. Of the Young Batholith.||||||17-JUL-08
29521|Broula Granite|24417|3|Fully described|p101|Early Devonian|Early Devonian|Has previously been included in Young Granodiorite and "Bumbaldry Granite".||||||
29521|Broula Granite|43642|5|Briefly described|Map Legend|Devonian|Devonian|Hornblende biotite orthopyroxene granite.||||||17-JUL-08
29521|Broula Granite|43782|5|Briefly described|Map Legend|Emsian|Emsian|||||||
29521|Broula Granite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Hornblende biotite orthopyroxene granite.||||||05-JUL-04
29521|Broula Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|||||||13-JUL-04
29521|Broula Granite|68592|5|Briefly described|p963|Early Devonian|Early Devonian|Possibly comagmatic with Warrangong Volcanics and Crowther Monzodiorite.||Unit in Boggy Plain Supersuite.||Intrudes Warrangong Volcanics.||
29521|Broula Granite|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Boggy Plain Supersuite||||
28233|Browning Vale Andesite Member|38802|2|Defined|p116|Famennian|Famennian|||||||
28233|Browning Vale Andesite Member|42728|5|Briefly described|p5|||||||||
28233|Browning Vale Andesite Member|66720|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Baldwin Formation.|||Massive, porphyritic andesite olistoliths and sills.|
23426|Brownmore Sandstone Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Of the Flagstaff Formation. Fine to medium-grained massive, laminated and crossbedded lithic sandstone with mudstone; lenses of shelly and coralline limestone. Max. thickness: 950m. Geological Province: Tamworth Forearc Basin.||||||
23426|Brownmore Sandstone Member|40883|6|Mentioned|p7|||||||||
23426|Brownmore Sandstone Member|43576|6|Mentioned|p350|||||||||
23426|Brownmore Sandstone Member|44244|4|Described|p69-70|Visean|Visean|Of the Flagstaff Formation.  Conformably overlies Underbank Mudstone Member; conformably underlies Bandon Grove Limestone Member.  Max. thickness: 950m.  Geological Province: Gresford Block.||||||
23426|Brownmore Sandstone Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Flagstaff Formation.  Brown, massive, crossbedded or laminated lithic sandstone with interbeds of conglomerate, mudstone and lenses of shelly and coralline limestone. Geological Province: Gresford Block||||||
77664|Browns Creek Intrusive Complex|67806|6|Mentioned|p109|Silurian||[New name; may just be informal usage here]. Hosts the Browns Creek Au-Cu deposit near Blayney.|||Includes Carcoar Granodiorite.|||24-MAY-17
77664|Browns Creek Intrusive Complex|73431|4|Described|p362-364, p366-367, p369 Fig.5, p370-375|Devonian|Silurian|Originally named as 'Carcoar Granodiorite' (Pogson and Watkins, 1998), 'Browns Creek intrusive Complex' is used in this paper, after Kovacs (2000). Intrudes Macquarie Arc. Compositionally plots on I-, S-type transitional line of Chappell et al., (1998). SHRIMP zircon U-Pb age of 426.1+/-2.2 Ma, eNd values of -5.9 to +2.44. Multiple previous U-Pb SHRIMP and Ar/Ar dating with errors are listed. Parts of granodiorite and dykes at 430-437 Ma are coeval with Sunset Hills Granite and Canowindra Volcanics, and at 420-426 Ma are coeval with Wyangala Granite and Barry Granodiorite. Zircon margin analyses of 396.3+/-5.7 Ma represents a recrystallisation event, coeval with aplite dykes of Davies Creek Granite. Contains very few inherited zircon xenocrysts.|437.1+/-5.9 Ma U/Pb SHRIMP, 407+/-4 Ma Rb/Sr||Carcoar Granodiorite, Long Hill Diorite, Browns Creek dykes|Intrudes Stokefield Metagabbro, Blayney Volcanics, Cowriga Limestone Member, Coombing Formation, faulted against Tallwood Monzonite and Weemalla Formation|Includes granodiorite, a more mafic part of diorite, dykes, and leucogranite.|
23428|Brungle Creek Metabasalt|22638|1|Redefined|p41|Early Silurian||Previously "Brungle Creek Volcanics", previously "Bauld Hill Basic Formation"||||||
23428|Brungle Creek Metabasalt|22768|6|Mentioned|p174|||||||||
23428|Brungle Creek Metabasalt|22857|4|Described|p174, p452 App.1, Tb.A1.6|Silurian|Silurian|Basalts, basaltic hyaloclastics, cherts, polymictic conglomerate. Contain radiolaria. Basement of the Tumut Trough.||||||24-FEB-06
23428|Brungle Creek Metabasalt|37529|5|Briefly described|p7|||||||||
23428|Brungle Creek Metabasalt|42045|4|Described|p153|||||||||
23428|Brungle Creek Metabasalt|42145|4|Described|Table 1 P624|||||||||
23428|Brungle Creek Metabasalt|42313|3|Fully described|p63||Early Silurian|Probable correlative of Wermatong Metabasalt. Age late Early Silurian||||||
23428|Brungle Creek Metabasalt|42314|5|Briefly described|Map|Early Silurian||||||||
23428|Brungle Creek Metabasalt|42828|5|Briefly described|Table 1 P129|Middle Silurian|Early Silurian|||||||
23428|Brungle Creek Metabasalt|44192|5|Briefly described|Map Legend||Llandoverian|||||||
23428|Brungle Creek Metabasalt|60280|5|Briefly described|p2, p3 Fig. 1|||||||||
23428|Brungle Creek Metabasalt|66197|6|Mentioned|p631 Fig.3a|||Mafic volcanics. Is overlain by Wyangle Formation.||||||14-MAR-12
23428|Brungle Creek Metabasalt|67322|5|Briefly described|p20|Pridoli|Ludlow|Age constrained by that of the parent Jindalee Group: an Ordovician fragmented ophiolite sequence within a Silurian sedimentary matrix. On Tumut 1:100 000 sheet: (Basden, 1990).||Of the Jindalee Group||||21-FEB-18
35364|Brusches Formation|23185|6|Mentioned|Fig4p160|||||||||
82371|Bruxner Granodiorite|71628|4|Described|p2:54; p9: 1-2, 4-10, 33; p10:7; p19: 26|||See also p19: 52, 94. Originally Bruxner Adamellite (Thomson, 1973). Renamed Bruxner Monzogranite (Cranfield et al., 2001) after unpublished work by Barnes and Willis (1989). Renamed again in this study to reflect general composition. Named after Bruxner Highway. Forms an 18km long intrusion ~8km W of Tabulam. Crops out as small tors; alteration is widespread. Geochemistry detailed. Has evidence of crustal contamination. The text states it intrudes (p19-52) and is intruded by (p9-5) the Girard Creek Diorite. Is associated with several quartz-cinnabar deposits, Sb-Au lodes, and two ironstone deposits.|256.0 +/- 1.4 Ma (SHRIMP: Waltenberg et al. 2016).|Bruxner Suite.||Intrudes Emu Creek Formation, Drake Volcanics, Razorback Creek Mudstone. Is overlain by Laytons Range Conglomerate and Gatton Sandstone.|Grey, fine- to medium-grained, equigranular, hornblende-biotite-(pyroxene) quartz diorite to granodiorite and pink, hydrothermally altered leucocratic hornblende-biotite monzogranite. Detailed descriptions. I-type.|
30504|Buccleuch Formation|10010|5|Briefly described|p12 Fig. 3|Late Eocene|Middle Eocene|Geological Province: Murray Basin.||||||13-AUG-07
30504|Buccleuch Formation|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
30504|Buccleuch Formation|22773|5|Briefly described|p351,Fig24.8p352|Eocene|Late Eocene|||||||
30504|Buccleuch Formation|22857|5|Briefly described|p351, p352 Fig.24.8|Late Eocene|Late Eocene|Marine deposits. Geological Province: Murray Basin. Equivalents mentioned on p352 Fig.24.8. See also p353 Fig. 24.9.||||||
30504|Buccleuch Formation|43195|5|Briefly described|Map Legend|Early Oligocene|Late Eocene|||||||
30504|Buccleuch Formation|44133|5|Briefly described|p158, 152 Fig. 10.2|Late Oligocene|Late Eocene|Formerly Buccleuch Beds, Buccleuch Group. Geological Province: Murray Basin.  ||||||
30504|Buccleuch Formation|60785|5|Briefly described|p184 Fig.1, p195.  |Rupelian|Rupelian|South Australia. Has yielded a fossil cetacean heterodont tooth.|||||Green and slightly glauconitic fine-grained limestone.|
30504|Buccleuch Formation|63887|5|Briefly described|p20, p21 Fig. 1|Late Eocene|Late Eocene|Of Renmark Group[?]. Marnie incursion indicated by deposition of fossilerous clay and marl.||||||03-DEC-13
30504|Buccleuch Formation|67462|5|Briefly described|Map legend.|Oligocene|Oligocene|Murray Basin.||||||
30504|Buccleuch Formation|68715|6|Mentioned|p31 Fig.5|Oligocene|Eocene|Murray Basin. Late Eocene to Late Oligocene age.||||||
30504|Buccleuch Formation|73188|6|Mentioned|p320|Oligocene|Oligocene|Murray Basin.|||||Limestone, marl, clay.|
30504|Buccleuch Formation|73228|4|Described|p50, p54-57, p60|Late Eocene|Late Eocene|Murray Basin, northern SA. Resulted from a minor marine incursion. Grades laterally into the marginal marine upper Olney Formation.||Renmark Group|||Bryozoal and glauconitic limestones, bryozoal clayey sand, and black pyritic/ferruginous clay.|
30504|Buccleuch Formation|73229|6|Mentioned|p67|Early Oligocene|Late Paleocene|Murray Basin.||Renmark Group||||
31581|Buccleugh Suite|42726|5|Briefly described|map legend||Silurian|||||||
27639|Buckambool Sandstone|22857|5|Briefly described|p442|Pragian|Pragian|Of the Winduck Group. Max. thickness: >950m. Geological Province: Winduck Shelf (Darling Basin).||||||10-MAR-06
27639|Buckambool Sandstone|23171|6|Mentioned|p15|||||||||
27639|Buckambool Sandstone|23173|6|Mentioned|Map Legend|||||||||
27639|Buckambool Sandstone|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|Of Winduck Group.||||||
27639|Buckambool Sandstone|35925|5|Briefly described|p2|||To be defined by Glen et al.||||||
27639|Buckambool Sandstone|37798|4|Described|p128|||See also Table 1.||||||
27639|Buckambool Sandstone|38292|6|Mentioned|p3|||||||||
27639|Buckambool Sandstone|39660|6|Mentioned|p449|||||||||
27639|Buckambool Sandstone|39978|6|Mentioned|p75|||||||||
27639|Buckambool Sandstone|41018|6|Mentioned|p239|||||||||
27639|Buckambool Sandstone|41138|6|Mentioned|Map legend|Pragian|Pragian|||||||
27639|Buckambool Sandstone|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27639|Buckambool Sandstone|41821|3|Fully described|p43|||||||||
27639|Buckambool Sandstone|42983|6|Mentioned|Fig.3,p345|||||||||
27639|Buckambool Sandstone|43032|2|Defined|p133|Early Devonian||of Winduck Group||||||
27639|Buckambool Sandstone|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Winduck Group (Cobar Supergroup).  Interbedded 'flaggy' quartz sandstone and recessive siltstone; rich in shelly fossils locally.   Age is Pragian. Geological Province: Winduck Shelf.||||||
27639|Buckambool Sandstone|64967|5|Briefly described|p114 Fig. 2|Lochkovian|Late Silurian|Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). See also p115 Fig. 3.||||||
27639|Buckambool Sandstone|65469|5|Briefly described|p15-p17|Lochkovian|Lochkovian|Lachlan Orogen.||Winduck Group||||
27639|Buckambool Sandstone|70037|4|Described|p309 Fig.2, p311|Early Devonian|Early Devonian|Glen (1979) initially placed this unit towards the top of the Amphitheatre Group, but reassigned it to the Winduck Group (Glen, 1982). Darling Basin. Average thickness is c.1000m. Lochkovian to Pragian.||Lower part of Winduck Group.||Is overlain by Sawmill Tank Siltstone.|Predominantly sandstone interbedded with siltstone and shale.|
27639|Buckambool Sandstone|70751|6|Mentioned|p12|Emsian|Lochkovian|||Winduck Group||||
27639|Buckambool Sandstone|72908|5|Briefly described|p5, p7, p14|Emsian|Lochkovian|Winduck Shelf. Lochkovian to early Emsian in age. Hosts the Gundaroo deposit.||Winduck Group||Unconformably overlies Thule Granite|Sandstones.|
27639|Buckambool Sandstone|72958|6|Mentioned|p11|Emsian|Pridoli|Cobar Basin. Nymagee area.||Winduck Group||Partly underlain by Amphitheatre Group, Mount Hope Group. Partly overlain by Meadows Tank Formation. Partly overlain and equivalent to Sawmill Tank Siltstone. Equivalent to Walters Range Group.||
27639|Buckambool Sandstone|73174|4|Described|p1038-1042, p1044-1045|Emsian|Pragian|Winduck Shelf. Time-transgressive basal and upper boundaries. Traction current indicators and the presence of shelly fauna suggest a shallow marine environment, with hummocky cross stratification in some horizons. Contains age-diagnostic brachiopod. Geochron is maximum depositional age. [Misspelt as Buckanbool Sandstone on p1037].|421 +/- 10 Ma LA-ICP-MS|Winduck Group, Cobar Supergroup||Unconformably[?] underlain by Wittagoona Sandstone. Overlain and equivalent to Sawmill Tank Siltstone.|Massive, medium-grained and clean, white to light grey sandstone with large-scale cross-bedding, fossil casts and fossil fragments with interbedded mudstone.|
78492|Buckenbowra Andesite Member|66768|4|Described|p212-218|Late Devonian|Middle Devonian|Informal member of Comerong Volcanics. Max thickness 180m. Mafic tuff, breccia, lapilli tuff and fine-grained chloritic tuff in addition to andesitic lava flows.||||||07-NOV-13
26429|Buckenbowra Granodiorite|35248|6|Mentioned|Fig.1|||||||||
26429|Buckenbowra Granodiorite|42497|5|Briefly described|Map legend|Zlichovian|Pragian|||||||
26429|Buckenbowra Granodiorite|68255|5|Briefly described|p1049, p1051-p1063|Frasnian|Emsian|Intrudes the Adaminaby Group around 395.8 +/- 8.1 Ma.|384.6 +/- 7.9 Ma - 395.8 +/- 8.1 Ma, K-Ar.|Of the Moruya Suite.||Intrudes the Adaminaby Group.||20-JUL-15
26430|Buckets Gap Formation|22857|4|Described|p510 App.1 Tb.A1.8|Namurian|Namurian|Mudstone interbedded with fine lithic arenites; randomly pebbly. Max. thickness: 610m.||||||
26430|Buckets Gap Formation|30074|3|Fully described|p15|||See also P16,P17.||||||
26430|Buckets Gap Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26430|Buckets Gap Formation|32866|6|Mentioned|p22|||Fossil content||||||
26430|Buckets Gap Formation|32868|6|Mentioned|p199|||||||||
26430|Buckets Gap Formation|32869|6|Mentioned|Fig.2|||||||||
26430|Buckets Gap Formation|34072|6|Mentioned|Fig.4.5|||Carb. Fossils||||||
26430|Buckets Gap Formation|34168|5|Briefly described|p254|||Carboniferous||||||
26430|Buckets Gap Formation|36528|6|Mentioned|p179|||||||||
26430|Buckets Gap Formation|38801|6|Mentioned|Fig.3|||||||||
26430|Buckets Gap Formation|39302|5|Briefly described|p349|||||||||
26430|Buckets Gap Formation|39308|4|Described|p487|||||||||
26430|Buckets Gap Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|||||||16-DEC-04
26430|Buckets Gap Formation|42547|5|Briefly described|Fig.8 P30|||Misspelling of Bucketts Gap Formation?||||||
26430|Buckets Gap Formation|44093|5|Briefly described|p230 App. 1|Late Devonian|Late Devonian|Geological Province: New England Fold Belt.||||||
26430|Buckets Gap Formation|44244|2|Defined|p154|Namurian|Namurian|Conformably overlies the Copeland Road Formation; underlies the McInnes Formation.  Type section in text.  Max. thickness: 610m. Geological Province: Myall Block.||||||
26430|Buckets Gap Formation|45063|6|Mentioned|p228|||Visean - Namurian||||||
26430|Buckets Gap Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
26430|Buckets Gap Formation|47056|6|Mentioned|Fig.2 P523|||||||||
26430|Buckets Gap Formation|48924|6|Mentioned|p12||Early Carboniferous|L.Carb.||||||
26430|Buckets Gap Formation|50147|5|Briefly described|Map legend|Namurian|Visean|Dark grey to black mudstone, siltstone, and fine lithic sandstone, with minor coarse (pebbly) lithic sandstone.  Geological Province: Western Myall Block.||||||
38308|Bucketts Way seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
80755|Buckingbong Granite|71889|3|Fully described|p7-p8, p12, p40-p43, p68|Silurian|Silurian|Small outcrops of 'biotite granite' in and near the Buckingbong State Forest were shown in earlier geological maps (Pogson 1974; Chappell et al, 1991) and granite has been mentioned in early studies (Dun, 1930; Keble and Macpherson, 1941; Clare et al, 1997). This unit outcrops poorly and has not previously been described; however outcrops in earlier mapping were confirmed and it is proposed in the present study to name the granite as the Buckingbong Granite. A type area is proposed as ERIVSJT1548 where the most extensive outcrop of this unit is found. This unit is interpreted in magnetic imagery as a roughly oval shaped pluton with a long axis c. 19km long trending approximately 340". The pluton is c. 9.5km wide at its widest point.|~430 Ma inferred||||Medium- to coarse-grained, bioitite-muscovite granite.|28-FEB-19
31501|Buckleys Lake Suite|22815|5|Briefly described|p53,58|Silurian|Silurian|||||||
31501|Buckleys Lake Suite|42726|5|Briefly described|map legend||Silurian|||||||
31501|Buckleys Lake Suite|43233|5|Briefly described|Map Legend|Late Silurian||Berridale Batholith||||||
31501|Buckleys Lake Suite|44093|5|Briefly described|p190 App. 1|Early Devonian|Silurian|||||||
23432|Buddigower Granite|22638|3|Fully described|p55|||Probably Late Silurian. Previously "Buddigower Granite" (informal)||||||
23432|Buddigower Granite|42726|5|Briefly described|map legend|||Reserved Nov 1993.||||||
23432|Buddigower Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
23432|Buddigower Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
23432|Buddigower Granite|70777|4|Described|p1, p3-p4, p46-p50, p79, p95-p96|Wenlock|Wenlock|Lachlan Orogen. Age provided is interpreted as the magmatic crystallisation age. Low magnetic susceptibility (10 x 10^-5 SI). Flanked by the Ungarie and Yalgogrin Granites. Petrography, zircon description, U-Pb isotopic results and geochronological interpretation are discussed. This granite is interpreted to be an S-type.|431.7 +/- 2.2 Ma (SHRIMP zircon, This volume)|Koetong Supersuite||Coeval with the Ungarie and Yalgogrin Granites. Intrudes the Wagga Group.|Equigranular, fine-grained and unfoliated granite which hosts small microgranular enclaves.|
23432|Buddigower Granite|73082|6|Mentioned|p24|||"West Wyalong district. Is presented as ""the Kikoira Granite (aka the Buddigower Granite)"" [both of which occur in the Stratigraphic Units Database but there has not been any article so far indexed (as at 1/6/2022) stating that one of these units has been superseded]."||||||
30046|Budgee Formation|43188|6|Mentioned|p217|||||||||
35306|Budgery Sandstone Member|23173|6|Mentioned|Map Legend|||||||||
35306|Budgery Sandstone Member|67322|5|Briefly described|p39|Darriwilian|Tremadocian|Obsolete: a heavily altered quartzite mentioned in the legend of the Cobar 1:250 000 metallogenic map (Gilligan et al. 1994), but never defined. Age is from the parent Girilambone Group. Occurs in the Sussex-Byrock region.||Formerly of the Girilambone Group.|||Heavily altered quartzite.|21-FEB-18
35306|Budgery Sandstone Member|69635|5|Briefly described|p88-95, p69|Early Ordovician|Early Ordovician|North-western Lachlan Orogen. U-Pb SHRIMP zircon maximum depositional age.|497+/-25 Ma|Of Narrama Formation.||||
35306|Budgery Sandstone Member|70602|5|Briefly described|p66,Fig 2, p68|Middle Ordovician|Early Ordovician|Lithology compared with Brevelon Tank Quartzite.||Narrama Formation|||Rare, thick packages of medium-grained metasandstone-quartzite.|27-JUN-16
35306|Budgery Sandstone Member|71360|5|Briefly described|Map legend|Paleozoic|Paleozoic|Identifiable as a unit of the Narrama Formation only on the basis of its map symbol (Oginb) which is similar to other Members of that Formation. Geophysical signature: non-magnetic areas which are not discernible from adjacent metasedimentary units in aeromagnetic data. The unit distribution is based on geological mapping and small linear trends with very low counts in radiometric data.||Narrama Formation.|||Quartzite.|
35306|Budgery Sandstone Member|72296|1|Redefined|ix, p1, p5, p8-13, p20-23, p27, p58-59|Early Ordovician|Early Ordovician|See also p62, p66, p68, p72 Fig.17, p77. Redefined in this study (Trigg, in Gilmore et al., 2018). Originally the Budgery Sandstone (Rayner, 1961, 1969). See pp6,9,20 for the complicated evolution of the unit's name and relationships. No type section; type area is at Trig Hill Lat. -31.263263 degrees, Long. 146.895719 degrees, and nearby rises, just W of Girilambone town. Here defined as the packets of quartz-rich sandstone that crop out, forming a series of distinctive steep rises that run through COOLABAH [100K sheet area] and beyond, and their subsurface equivalents. A useful marker horizon over 150km along strike despite discontinuous exposures. Is written also as Budgery Quartzite Member once on p20 in a sentence describing quartzites in the Girilambone Group. Unfossiliferous: age from parent. Geophysical properties briefly described. Associated with VAMS Cu mineralisation (described in detail).|497 +/- 7 Ma (MDA: Fraser et al., 2014).|Narrama Formation.|||Massive to well-foliated, fine- to medium-grained quartz-rich metasandstone to quartzite; total lack of fine-grained intercalations. Metamorphic mica rare to minor; locally gives the rock a schistose aspect. Greenschist facies regional metamorphism.|
80312|Budginigi Ignimbrite|73457|5|Briefly described|p10-15|Early Devonian|Early Devonian|Interpreted to unconformably underlie the Yambla Formation, exact relationship is uncertain. Boundary with the Granya Granite is either a fault or a nonconformity. Over 100m of vertical thickness is exposed.|ca. 414 Ma|||Unconformably underlies Yambla Formation||
73654|Budhang Chert Member|63279|5|Briefly described|p167, p177|Lancefieldian|Lancefieldian|Of the Triangle Formation. Age from conodonts present in the unit. Geological Province: Rockley-Gulgong Volcanic Belt.||||||19-OCT-22
73654|Budhang Chert Member|63286|6|Mentioned|p308 Fig. 9|Early Odrovician|Early Ordovician|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
73654|Budhang Chert Member|70297|5|Briefly described|map legend|Ordovician|Ordovician|||Adaminaby Group||||
24777|Budthingeroo Granite|42726|5|Briefly described|map legend|Carboniferous||43.||||||
78863|Buff Point Coal Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Catherine Hill Bay Formation.||||
36963|Buffers Creek Formation|22857|5|Briefly described|p516 App.1 Tb.A1.8|Early Permian|Carboniferous|Siltstone, lithic wacke, diamictite, felsic tuff, minor metabasalt and dolerite. Max. thickness: >1400m. Geological Province: Barnard Basin (Nambucca Basin).||||||
36963|Buffers Creek Formation|23720|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Siltstone, lithic wacke, diamictite, felsic tuff, minor metabasalt and dolerite.||||||15-DEC-04
36963|Buffers Creek Formation|24127|5|Briefly described|p5|||||||||
36963|Buffers Creek Formation|44450|3|Fully described|p22 Table 4|Early Permian|Late Carboniferous|Geological Province: Nambucca Block. Max. thickness: >1500 m||||||
36963|Buffers Creek Formation|71628|5|Briefly described|p2:34; p3: 27, 46|||Nambucca Block. Underwent regional metamorphism and deformation, and contact metamorphism by the Dundurrrabin Granodiorite intrusion. Age given as ?Early Permian.||||Is intruded by Dorrigo Mountain Complex and Dundurrabin Granodiorite. Is faulted against Gleniffer Monzogranite.||
31651|Buggary Suite|22815|5|Briefly described|p52|Early Devonian|Late Silurian|||||||
31651|Buggary Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
23434|Bugtown Tonalite|36443|5|Briefly described|map legend|Lochkovian|Pridolian|Intrusive. Tonalite, granodiorite. BMR map code: Sbt.||||||
23434|Bugtown Tonalite|39660|6|Mentioned|p449|||||||||
23434|Bugtown Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh3||||||
23434|Bugtown Tonalite|45147|2|Defined|M250|Late Silurian|Late Silurian|Prob.Late Silurian||||||
23434|Bugtown Tonalite|49705|6|Mentioned|p19|||||||||
23434|Bugtown Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
29529|Bugwah Formation|22773|6|Mentioned|Fig24.10p355|Holocene|Late Pleistocene|||||||
29529|Bugwah Formation|23053|4|Described|p7,12,Fig11p34,45-9|Holocene|Late Pleistocene|||||||
29529|Bugwah Formation|24042|5|Briefly described|p513|||||||||
29529|Bugwah Formation|43276|5|Briefly described|Map Legend|Holocene|Late Pleistocene|||||||
29529|Bugwah Formation|43277|5|Briefly described|Map Legend|Holocene|Late Pleistocene|of Great Australian Basin.||||||
29529|Bugwah Formation|68003|5|Briefly described|p92 Fig.3-v and Table 3-b, p96.|Holocene|Late Pleistocene|Coonamble Embayment. Age from Watkins and Meakin (1996).|13.4 - 6 ka.|||Overlies Carrabear Formation. Is overlain by Marra Creek Formation.||
29529|Bugwah Formation|68069|5|Briefly described|Map legend.|Quaternary|Quaternary|Has several facies mapped separately: channel, meandering plain, crevasse splay and backplain.|||Includes Nullawa Member.||Unconsolidated yellow-grey to dark grey sand, sandy silt, silt, clayey silt, silty clay and clay; sparse carbonate nodules.|
29529|Bugwah Formation|68593|4|Described|p12-17, p1-3, p20, p45, p48|Holocene|Pleistocene|Watkins and Meakin (1996). Typically consists of a relatively wide meander plain facies flanking the channel and a bordering backplain facies. Estimated age range based on thermoluminescence dating (Watkins, 1992). Various facies are described in some detail: channel, meander plain, crevasse splay and backplain. Sand and loam are extracted from the Mission (Ginghi) pit.|13.4-6.4 ka (Watkins and Meakin, 1996).||Nullawa Member.|Is overlain by Marra Creek Formation.|Unconsolidated Quaternary alluvium surrounding silcrete-capped ridges: sand, silt, clay, carbonate nodules.|11-DEC-15
28410|Bukalong Granite|22815|4|Described|p83,84||Silurian|Of the Bukalong Suite. Referred to as the "Bukalong Adamellite" by Beams (1980 unpub.).  Fine leucogranite to coarse-grained leucocratic biotite granite. Intruded by Paradise Porphyry. Rb/Sr Age: 420Ma.||||||16-FEB-05
28410|Bukalong Granite|23329|5|Briefly described|1042|Silurian|Silurian|||||||
28410|Bukalong Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Bukalong Granodiorite.||||||
28410|Bukalong Granite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Bukalong Suite.||||||
30476|Bukalong Suite|22815|6|Mentioned|p83|||||||||
30476|Bukalong Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
30476|Bukalong Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
77321|Bukkulla Member|68005|5|Briefly described|pp37-39.|Early Permian|Early Permian|Contains the Bukkulla seam.||Topmost unit in Ashford Coal Measures.||Overlies the Bonshaw Member.||
27727|Bulahdelah Formation|22612|6|Mentioned|424|||Max thickness 1500 m||||||
27727|Bulahdelah Formation|22857|4|Described|p536 App.1 Tb.A1.9|Late Permian|Late Permian|Grey to brown, massive to thickly bedded lithic sandstone with occasional stringers of pebbles. Max. thickness: 1000m. Geological Province: Sydney Basin.||||||
27727|Bulahdelah Formation|24118|5|Briefly described|p3|Permian|Permian|||||||
27727|Bulahdelah Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
27727|Bulahdelah Formation|34059|6|Mentioned|Map legend|Permian|Permian|||||||
27727|Bulahdelah Formation|34345|6|Mentioned|p329|||||||||
27727|Bulahdelah Formation|34556|4|Described|p267|||Permian||||||
27727|Bulahdelah Formation|36057|6|Mentioned|Fig.1|||||||||
27727|Bulahdelah Formation|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27727|Bulahdelah Formation|40883|6|Mentioned|p9|||||||||
27727|Bulahdelah Formation|42833|4|Described|p227|||see also Fig.2 P225||||||
27727|Bulahdelah Formation|43447|14|Not recorded|Table 1, p28||Permian|||||||
27727|Bulahdelah Formation|43451|14|Not recorded|Map Legend||Permian|||||||
27727|Bulahdelah Formation|44093|5|Briefly described|p231 App. 1|Kungurian|Kungurian|Geological Province: New England Fold Belt.||||||
27727|Bulahdelah Formation|44244|4|Described|p229|Late Permian|Late Permian|Max. thickness: ~1000m.  Geological Province: Myall Block.||||||
27727|Bulahdelah Formation|47056|6|Mentioned|Fig.2 P523|||||||||
27727|Bulahdelah Formation|50263|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Eastern Myall Block.||||||
27351|Bulga Formation|22578|6|Mentioned|p391|||||||||
27351|Bulga Formation|22601|6|Mentioned|413|Permian|Permian|Geol province Sydney Basin||||||
27351|Bulga Formation|29942|4|Described|p11|||Permian||||||
27351|Bulga Formation|29943|6|Mentioned|p39|||||||||
27351|Bulga Formation|29944|6|Mentioned|Fig.18|||||||||
27351|Bulga Formation|31375|6|Mentioned|p4|||Stratigraphy||||||
27351|Bulga Formation|37087|6|Mentioned|p197|||||||||
27351|Bulga Formation|38603|6|Mentioned|p79|||||||||
27351|Bulga Formation|38614|6|Mentioned|Fig.6|||||||||
27351|Bulga Formation|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27351|Bulga Formation|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27351|Bulga Formation|40166|6|Mentioned|p347|||See also Table 1||||||
27351|Bulga Formation|40256|6|Mentioned|p304|||||||||
27351|Bulga Formation|40321|6|Mentioned|p19|||||||||
27351|Bulga Formation|40330|6|Mentioned|Fig.4|||||||||
27351|Bulga Formation|41054|6|Mentioned|Fig.3|||||||||
27351|Bulga Formation|41604|6|Mentioned|Table 1|||||||||
27351|Bulga Formation|42916|5|Briefly described|Table 1||Late Permian|||||||
27351|Bulga Formation|42922|6|Mentioned|Fig.14|||||||||
27351|Bulga Formation|43017|5|Briefly described|Fig.1,p372|||||||||
27351|Bulga Formation|43194|5|Briefly described|p129 Tb. 8.3, 130|Late Permian|Late Permian|Of Wittingham Coal Measures, Singleton Subgroup, Hunter region, Sydney Basin.||||||
27351|Bulga Formation|44244|4|Described|p237|Late Permian|Late Permian|Of the Vane Subgroup (Wittingham Coal Measures).  Overlies the Foybrook Formation; underlies Archerfield Sandstone.||||||
27351|Bulga Formation|45090|6|Mentioned|p217|||L. Tatarian||||||
27351|Bulga Formation|60281|6|Mentioned|p61|Late Permian|Late Permian|Different from the coastal Bulgo Sandstone.  Coarse-grained equivalent of the Kulnura Marine Tongue.||||||23-MAR-05
27351|Bulga Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Vane Subgroup (Wittingham Coal measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
27351|Bulga Formation|61529|5|Briefly described|p854 Fig. 1b|Late Permian|Late Permian|Overlain by Archerfield Sandstone; overlies Vane Subgroup. Geological Province: Sydney Basin.||||||
27351|Bulga Formation|61612|6|Mentioned|p272, p277, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||17-MAR-09
27351|Bulga Formation|61770|6|Mentioned|p110, p111|||Of the Vane Supergroup.||||||25-SEP-08
27351|Bulga Formation|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Late Permian.||Of the Singleton Supergroup.||||
27351|Bulga Formation|68003|5|Briefly described|p38 Fig.3-j.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Unit in Vane Subgroup.||Is overlain by Archerfield Sandstone.||
27351|Bulga Formation|68004|5|Briefly described|p23 Table 1, p51 Table 5.|Late Permian|Late Permian|Hunter Coalfield.||Upper unit in Vane Subgroup.||Overlies Foybrook Formation. Is overlain by Archerfield Sandstone.|Laminated siltstone and fine-grained sandstone with abundant burrows.|
27351|Bulga Formation|69683|6|Mentioned|p411 Fig.2, p415 Fig.3|Late Permian|Late Permian|||Unit in Vane Subgroup.||||
27351|Bulga Formation|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield.||Vane Subgroup.||||
27351|Bulga Formation|73304|6|Mentioned|p75|||||Whittingham Coal Measures, Singleton Supergroup||||
74015|Bullaganang Suite|63748|5|Briefly described|p25-26|Early Permian|Early Permian|Of the Bullaganang Supersuite.||||||07-FEB-11
74015|Bullaganang Suite|68679|5|Briefly described|p457, p459|Permian|Permian|Northern New England Batholith.|~292 Ma.|Stanthorpe Supersuite.|Bullaganang Granite.|||
74015|Bullaganang Suite|71628|5|Briefly described|p5:5; p10:1|||Now Mount Bullaganang Suite.||Bullaganang Supersuite.|Bullaganang Granite.|||
74065|Bullaganang Supersuite|63748|5|Briefly described|p25-26|Early Permian|Early Permian|Includes the Bullaganang and Mingimarny Suites.||||||07-FEB-11
74065|Bullaganang Supersuite|70876|5|Briefly described|p80|||Donchak et al (2013) incorporated this Supersuite into the Stanthorpe Supersuite; the authors of this volume however, note significant age ranges of the incorporated Supersuites and thus suggest this issue be revisited.||||||
74065|Bullaganang Supersuite|71628|5|Briefly described|p5: 1-2, 7; p19:103|||Donchak et al. (2007). Now the Mount Bullaganang Supersuite.|||Bullaganang Granite.|||
36336|Bullamalita Conglomerate|50234|5|Briefly described|Map Legend|Pragian|Lochkovian|Of the Bindook Volcanic Complex.  Underlies: Quialigo Formation.||||||
36336|Bullamalita Conglomerate|64238|5|Briefly described|Map legend|Devonian|Devonian|Basal unit of Bindook Group. Cream to grey, matrix- to clast-supported boulder conglom. Clasts of qtz'ose sst., lithic-quartz sst., siltst., shale + qtz-feldspar-phyric rhyolite up to 60cm but predom. <30cm in a coarse-grained to granule-sized...||||||09-SEP-08
36336|Bullamalita Conglomerate|68592|2|Defined|p873, p876, p878, p1060-3, p1156-61|Lochkovian|Lochkovian|See also p851, p852 Fig.143. New name, after Bullamalita property. Formerly included un-named in the Gundary Beds (Brunker, Offenberg et al., 1970), Towrang Beds (Brunker and Offenberg, 1970) and Gundary Formation (Jones, Carr et al., 1995). Type locality described. From 100m to c.750m thick. Clasts sourced from Adaminaby Group, Covan Creek and Boxers Creek Formations, and underlying Gundary Volcanics. Important marker horizon in the Goulburn region. Geophysical properties described. Age range from surrounding units. Probably equivalent to Tarago Conglomerate, and possibly to Sinclair Conglomerate Member.|413-412 Ma.|Unit in Bindook Group.||Overlies Back Station Ignimbrite Member disconformably and Tirranna Andesite Member unconformably. Is overlain conformably by Quialigo Volcanics. Correlated with Brooklyn Conglomerate Member.|Cream, matrix- to clast-supported, cobble to boulder conglomerate; largely poorly sorted; diffuse horizontal lamination.|
36336|Bullamalita Conglomerate|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dku. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Bindook Group||Erosional at base. Is overlain by Quialigo Volcanics.|Matrix-clast supported, cobble-boulder conglomerate; clasts of quartzose sandstone, lithic quartz sandstone, siltstone, shale and quartz-feldspar phyric rhyolite in a coarse-grained - granule-sized quartz lithic volcaniclastic matrix.|
36336|Bullamalita Conglomerate|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Bindook Group|||Matrix-clast supported, cobble-boulder conglomerate; clasts of quartzose sandstone, lithic quartz sandstone, siltstone, shale and quartz-feldspar phyric rhyolite in a coarse-grained - granule-sized quartz lithic volcaniclastic matrix.|
36336|Bullamalita Conglomerate|71040|6|Mentioned|p19|Early Devonian|Early Devonian|`||||||
36336|Bullamalita Conglomerate|71069|6|Mentioned|p135|||||Bindook Group ||Unconformably overlies the Mount Fairy Group.||
36336|Bullamalita Conglomerate|71656|6|Mentioned|p13 Fig.2|Pragian|Pragian|Shown only in correlation chart (Fig.2).||Base of Bindook Group.||Overlain by Quialigo Volcanics.||
36336|Bullamalita Conglomerate|71700|5|Briefly described|p23, p27,  CD|||||Bindook Group||||
27120|Bullenbalong Granodiorite|22815|4|Described|p45|Silurian|Silurian|Rb/Sr age: 411.9+/-9.4 Ma. May correspond with Berridale Batholith.||||||
27120|Bullenbalong Granodiorite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27120|Bullenbalong Granodiorite|35109|2|Defined|p57|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
27120|Bullenbalong Granodiorite|35263|6|Mentioned|Table.3|||||||||
27120|Bullenbalong Granodiorite|36411|6|Mentioned|p268|||Refers White et al 1977 for definition.||||||
27120|Bullenbalong Granodiorite|40328|4|Described|p203|||||||||
27120|Bullenbalong Granodiorite|41898|5|Briefly described|p1184|||||||||
27120|Bullenbalong Granodiorite|41905|4|Described|p78|||||||||
27120|Bullenbalong Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
27120|Bullenbalong Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
27120|Bullenbalong Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb17.||||||
27120|Bullenbalong Granodiorite|49705|5|Briefly described|p38|||||||||
27120|Bullenbalong Granodiorite|60078|6|Mentioned|Map Legend||Silurian|||||||
27120|Bullenbalong Granodiorite|68592|6|Mentioned|p1225|||Named after Bullenbalong North Hill, NE of Jindabyne.||Unit in Bullenbalong Suite.||||
70000|Bulliac Formation|61766|4|Described|p67|Late Devonian|Late Devonian|Supersedes Bulliac beds. Characterised by thick structureless beds of blue-grey coarse-grained feldspathic lithic sst and breccia. Conformable on Ghanghat Basalt. Geological Province: Tamworth Belt.||||||
33275|Bumballa Formation|24037|2|Defined|p435 Appendix 1|Gisbornian|Gisbornian|See also page 426. Previously included as an unnamed unit in the Bendoc Group. Overlain by Warbisco Shale. Underlain by Numeralla Chert. Geological Province: Lachlan Fold Belt. Maximum thickness: ~300m||||||28-MAY-08
33275|Bumballa Formation|50234|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Of the Bendoc Group.  Overlies the Adaminaby Group; underlies the Warbisco Shale.||||||13-MAY-04
33275|Bumballa Formation|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Bendoc Group. Olive to grey, buff and cream ripple cross-laminated to graded fine-grained sandstone interbedded with grey to black laminated siltstone + mudstone with v. minor chert. Lesser intervals ......quartzose sst; 2 subunits - siltst.+shale||||||11-JUN-08
33275|Bumballa Formation|67322|5|Briefly described|p17|Sandbian|Sandbian|Defined by Fergusson and Fanning (2002). 300 m thick. Shales within this Formation contain graptolites of late Gisbornian age. Occurs east of Goulburn.||||Overlain conformably by the Warbisco Shale.|Distinctive thin-bedded turbidite sequence, consisting of cross-laminated sandstones interbedded with graptolitic shales.|21-FEB-18
33275|Bumballa Formation|68466|6|Mentioned|p65|Late Ordovician|Late Ordovician|Albury-Bega Terrane.||||||
33275|Bumballa Formation|68592|4|Described|p320, p322-6, p328-37, p339, p342, p367|Late Ordovician|Late Ordovician|See also p116-8, p230, p275 Fig.57, p285 Fig.59, p287, p288 Fig.60, p298, p310, p519, p1862-4. Fergusson and Fanning (2002). Type section in Shoalhaven Gorge area. Is quarried at Carrick Hill for road materials. Geochemical similarities with Laidlaw Volcanics. Fossils, mainly graptolites, detailed.||Unit in Bendoc Group.||Overlies Abercrombie Group. Locally overlies Nattery Chert Member. Equivalent to Sunlight Creek Formation.|Interbedded turbiditic sandstones and dark grey to black shale: thinly-bedded fine-grained sandstone, thickly-bedded quartzose sandstone.|
33275|Bumballa Formation|69159|5|Briefly described|Map legend|Gisbornian|Gisbornian|||Unit in Bendoc Group.||Is overlain by Warbisco Shale.|Grey to cream, ripple cross-laminated to graded, fine-grained sandstone interbedded with grey to black, laminated siltstone and mudstone with very minor chert. Lesser intervals of medium- to thickly-bedded fine- to coarse-grained quartzose sandstone.|07-SEP-15
33275|Bumballa Formation|69668|6|Mentioned|p929 Fig.2|Late Ordovician|Late Ordovician|Goulburn-Braidwood area, Albury-Bega terrane.||||Overlies Abercrombie Formation. Is overlain by Warbisco Shale.||
33275|Bumballa Formation|70125|5|Briefly described|p394, p396 Fig.9|Late Ordovician|Late Ordovician|Lachlan Orogen. Probability density plot of U-Pb ages of detrital zircons is compared with that of other units.|460 Ma (Fergusson and Fanning, 2001).||||Turbidites.|
33275|Bumballa Formation|70192|5|Briefly described|Map Legend|Gisbornian|Gisbornian|[Theta]bb. On Taralga, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Bendoc Group|Includes two unnamed units.|Overlies Nattery Chert Member and Abercrombie Formation. Is overlain by (and interfingers with?) Warbisco Shale.|Laminated shale and siltstone, interbedded with fine grained, thinly bedded, graded-ripple cross laminated quartz sandstone. Some interbedded massive-planar laminated/ripple cross laminated, medium-coarse grained sandstone, siltstone and mudstone.|06-SEP-16
33275|Bumballa Formation|70297|5|Briefly described|map legend|Ordovician|Ordovician|||Bendoc Group||||
33275|Bumballa Formation|70493|6|Mentioned|p63|Late Ordovician|Late Ordovician|Shoalhaven River area, Lachlan Orogen. Zircons may have been derived from an area between the Bunger Hills and Transantarctic Mountains, East Antarctica.||||||
33275|Bumballa Formation|70541|4|Described|Map Legend|Ordovician|Ordovician|Includes two unnamed mapped members: a black, strongly cleaved, laminated siliceous carbonaceous shale; and a laminated to thinly bedded siltstone and mudstone.||Bendoc Group|Includes two unnamed members.||Laminated shale and siltstone, interbedded with fine grained, graded-ripple cross-laminated medium-coarse quartzose sandstone, some bedded massive/planar or ripple cross-laminated quartzose sandstone, silstone and mudstone, cherty siltstone/mudstone.|
33275|Bumballa Formation|70542|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|||Bendoc Group|||Laminated shale and siltstone, interbedded with fine grained, graded ripple cross laminated medium-coarse quartz sandstone, some bedded massive/planar or ripple cross-laminated quartzose sandstone, siltstone and mudstone, cherty siltstone/mudstone.|
33275|Bumballa Formation|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|||Bendoc Group|||Laminated shale and siltstone, interbedded with fine grained, thinly bedded, graded-ripple cross laminated quartz sandstone. Some interbedded massive-planar laminated/ripple cross laminated, medium-coarse grained sandstone, siltstone and mudstone.|
33275|Bumballa Formation|70661|3|Fully described|p4, p17, p19, p20 fig 3, p21, p22, p23|Eastonian|Gisbornian|Correlates with subunit 2 of Fergusson and Vandenberg. Name derived from parish of Bumballa. 300-800m thick. Deposited in a deep marine environment with some pelagic sedimentation. Fossil assemblage discussed.|480-630 Ma (U-Pb SHRIMP)|Bendoc Group||Equivalent to the Sunlight Creek Formation, conformably overlies the Adaminaby Group,  Nattery Chert Member, conformably overlain by Warbisco Shale|Mudstone, quartz sandstone and siltstone forming a turbiditic succession of mainly thin-bedded turbidites. Rare intervals of black siliceous shales with graptolites and concretions.|
33275|Bumballa Formation|70744|6|Mentioned|p944-945|Late Ordovician|Late Ordovician|SE Lachlan Orogen. Detrital zircon age distribution graph.||||||
33275|Bumballa Formation|71069|3|Fully described|p21 fig 7, p22, p39 fig 16, p40 fig 17|Eastonian|Gisbornian|Named for the Parish of Bumballa. Included previously as an unnamed unit of the Bendoc Group or the Abercrombie Beds/Adaminaby Group. Subdued outcrop character. Occurs in an imbricate thrust system with the Douro Group and Warbisco Shale.A composite type section  and two representative sections have been proposed. Estimated thickness ranging from 200-800m (it should be noted that thrusting and folding probably caused apparently greater thickness). Generally has subdued exposure or occurs as low outcrop, subcrop or shale float. Lithology discussed in greater detail on p79.  Age based on fossil assemblage. Interpreted to have been deposited in a deep marine setting on the basis of turbidite deposits and hemipelagic sedimentation. Faulted against the Hoskinstown Group. Is equivalent to the Sunlight Creek Formation. Potentially equivalent to the Glen Fergus Member. Distribution, primary structures/textures, tectonic structure, metamorphism, fossil assemblage and geophysical characteristics are discussed. See also p53 fig 19, p59, p65 fig 21, p67 fig 22, p68, p71, p73 fig 26, p74-p84, p86, p106.||Bendoc Group||Conformably overlies the Abercrombie Formation and the Nattery Chert Member. Conformably overlain by, and interfingers with the Warbisco Shale.|Thinly bedded turbidites, fining upwards sequence of shale, cross-laminated fine-grained quartzose sandstone, mudstone, grey siltstone and cherty siltstone.|
33275|Bumballa Formation|71303|5|Briefly described|map legend|Katian|Katian|||Of Bendoc Group.|||Turbiditic sequence of mostly thinly bedded quartz sandstone and mudstone. Rare intervals of black, laminated to medium bedded, pyritic carbonaceous shale, commonly strongly foliated and folded.|
33275|Bumballa Formation|71656|4|Described|p13 Fig.2, p14, p15|Gisbornian|Darriwilian|Most fossils obtained from the Bumballa Formation are graptolites, but at many localities these are poorly preserved, so identifications and age connotations are not necessarily precise. Conodonts also found in chert beds.||Bendoc Group||Overlies Nattery Chert Member, underlies Warbisco Shale.|Cherts are associated with this formation.|
33275|Bumballa Formation|71691|5|Briefly described|Map legend.|Ordovician|Ordovician|||Bendoc Group.||Overlies Adaminaby Group. Is overlain by Warbisco Shale.|Grey-cream, cross-laminated to graded, fine-grained sandstone interbedded with grey to black, laminated, siltstone/mudstone with minor chert; lesser intervals of medium- to thick-bedded, massive, planar-laminated or cross-laminated quartz sandstone.|
33275|Bumballa Formation|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|||Bendoc Group.||Overlies Abercrombie Formation. Is overlain by Warbisco Shale.|Grey to cream, ripple cross-laminated to graded, fine-grained sandstone interbedded with grey to black, laminated siltstone and mudstone with very minor chert; lesser intervals of medium- to thick-bedded, laminated quartzose sandstone.|
33275|Bumballa Formation|71700|2|Defined|vi, p7, p9-p10, p64, CD|Early Gisbornian|Early Gisbornian|Lachlan Orogen. This unit is named for the parish of Bumballa. This unit was first included as part of the "Undifferentiated Ordovician" on the 1st edition Goulburn 1:250k and along with the Warbisco Shale occupied part of the "Bubalahla Formation" on the 1st edition Taralga 1:100k map. The formation was thereafter included as an unnamed unit within the Bendoc Group by Fergusson (1998b) before being named by Murray and Stewart (2001) and subsequently defined by Fergusson and Fanning (2002).The Shoalhaven Gorge in Mossvale hosts a composite type section between GR 231984 6148610 and GR 231604 6148720. A continuous section occurs in the Abercrombie River national park from GR 747860 6216700 to GR 751570 6216700 (Thomas and Pogson, 2012).  Distribution, geomorphic expression, outcrop, structure, metamorphism, geophysical characteristics, fossils and depositional environment are discussed. This unit ranges in thickness from 5 to 200m thick in different areas. ||Bendoc Group||Conformably overlain by the Warbisco Shale. Overlies the Abercrombie Formation. Intruded by the Ellenden Granite.|Thin- to very thin-bedded, fissile, grey to black shale and siltstone, and medium to very thin-bedded, buff to grey, very fine- to medium-grained quartzose sandstone.|
33275|Bumballa Formation|73059|5|Briefly described|p1060-1061|Ordovician|Ordovician|Shoalhaven River, Lachlan Fold Belt. Detrital zircon age plots show a prominent Delamerian signature at 500 Ma and in the interval 570-520 Ma.|||||Turbidites.|
33275|Bumballa Formation|73140|5|Briefly described|p495 Fig.1|Eastonian|Gisbornian|Age based on conodonts and graptolites. Misspelt as Bumbulla Formation Fig.6.||Bendoc Group||Overlies Nattery Chert Member, Abercrombie Formation, underlies Warbisco Shale||
68915|Bunaleer Dacite Member|50613|2|Defined|p211, p228 App.1|Westphalian|Westphalian|Of the Willuri Formation.  Lens-shaped volcanic body that dominates the centre of the Piney Range package (informal grouping of stratigraphically recognisable distinctive, mappable units). Overlies the Piney Range Member.Age: 315+/-3.5Ma (SHRIMP).||||||11-MAY-05
27121|Bundaburrah Granodiorite|24417|3|Fully described|p106|Early Devonian|Early Devonian|Intrudes the Carawandool Volcanics.  Formerly "Bundaburrah Granite" and earlier included in Grenfell Granite.||||||
27121|Bundaburrah Granodiorite|24580|5|Briefly described|p828|||Unconformably overlain by the Hervey Group. Geological Province: Eastern Lachlan Fold Belt.||||||
27121|Bundaburrah Granodiorite|29907|2|Defined|Appendix 1 P86|Early Devonian|Early Devonian|Prob.Early Devonian||||||
27121|Bundaburrah Granodiorite|36411|6|Mentioned|p268|||Refers Bowman 1977.||||||
27121|Bundaburrah Granodiorite|40328|4|Described|p203|||||||||
27121|Bundaburrah Granodiorite|60009|5|Briefly described|Map Legend|Emsian|Emsian|||||||13-JUL-04
27121|Bundaburrah Granodiorite|60548|5|Briefly described|map legend|Devonian|Devonian|Hypersthene-augite granodiorite.||||||19-NOV-04
24789|Bundanoon Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
24789|Bundanoon Granite|70661|4|Described|vii, p6, p126 fig 10, p131-p132, p145|Carboniferous|Carboniferous|Named after either Bundanoon Creek or Bundanoon township.Distribution discussed. No type section or locality. Outcrops in the Bundanoon and Tallowa creeks. Age is tentative. Previously included in the Marulan Batholith.  May correlate with the Bundundah Granite or Tallowa Gully Granite.||||Overlain by Snapper Point Formation or Berry Siltstone|Medium to coarse grained adamellite with biotite and hornblende altering to chlorite.|16-FEB-18
24789|Bundanoon Granite|71303|5|Briefly described|map legend|Carboniferous|Late Devonian||||||Poorly known medium- to coarse-grained hornblende-biotite granite.|
67901|Bundarra Supersuite|24513|5|Briefly described|p9|Early Permian|Early Permian|Coarse-grained, porphyritic S-type granite. Age: ~280Ma. Within southern New England Orogen.||||||
67901|Bundarra Supersuite|62534|4|Described|p6, p11 (legend), p13-14|Early Permian|Early Permian|Intruded by dykes of the "Willowrie diorite". S-type. Large body of distinctly coarse-grained, porphyritioc monzogranite with abundant K-feldspar megacrysts.||||||07-FEB-11
67901|Bundarra Supersuite|62757|5|Briefly described|p1-2|Early Permian|Early Permian|Plutonic suite of the New England Batholith. Peraluminous S-type granitoids. Age: 286Ma.||||||07-FEB-11
67901|Bundarra Supersuite|63347|5|Briefly described|p2|Early Permian|Early Permian|S-type granites of the New England Batholith. Geological Province: New England Orogen.||||||
67901|Bundarra Supersuite|65398|5|Briefly described|p4 Fig.2, p5, 8, Fig 2-3|Early Permian|Early Permian|S-type plutons. Includes Pringles Monzogranite. Age: 277 Ma (K-Ar: Hartono, 1984) and 270-273 Ma (Shaw and Flood, 1981).||||||19-DEC-16
67901|Bundarra Supersuite|66720|5|Briefly described|Map legend|Early Permian|Early Permian||||Includes Pringles Monzogranite and an un-named but separately mapped unit of dykes and bosses of fine- to medium-grained, equigranular quartz-feldspar-biotite granite.|||
67901|Bundarra Supersuite|68005|4|Described|p18, p20, p25, p32, pp60-64, pp135-136.|Early Permian|Late Carboniferous|New England Fold Belt. Part of New England Batholith. Formerly a suite of Shaw and Flood (1982); redefined as a Supersuite by Bryant (2001). S-type. Large, continuous, N-S elongate belt; an aggregate of individual plutons. Reduced and unfractionated, hence an apparent scarcity of associated mineralisation.|286-279 Ma (Shaw and Flood 1981, 1982).||Includes Banalasta and Glenclair Suites.|Intrudes Cara and Whitlow Formations and Ashford Limestone.|Coarse-grained, equigranular to porphyritic granitic rocks; contains muscovite, cordierite and rare garnet; K-feldspar megacrysts abundant in places.|
67901|Bundarra Supersuite|68006|5|Briefly described|p20 Fig.3-A, pp26-27, p117. pp140-141.|Early Permian|Late Carboniferous|New England Batholith, New England Fold Belt. Of Bryant (2001). S-type. Several small quarries have extracted dimension stone from this unit in the Nandewar area. Associated with several small tin deposits.|||Includes Pringles Monzonite.|||
67901|Bundarra Supersuite|69188|5|Briefly described|p2||||||Pringles Monzogranite.||S-type.|
67901|Bundarra Supersuite|69323|5|Briefly described|p1,34,69|Permian|Permian|Geological province: New England Orogen.|||Includes Banalasta Monzogranite, Pringles Monzogranite.|||
67901|Bundarra Supersuite|70217|5|Briefly described|v, p72|Artinskian|Sakmarian|New England Orogen. S-type supersuite. Age derived from age of constituents. |286-288 Ma (SHRIMP U-Pb)||Includes the Pringles Monzogranite and the Banalasta Adamellite.|||04-OCT-17
67901|Bundarra Supersuite|70939|6|Mentioned|p823||||c.292 Ma.|||||
67901|Bundarra Supersuite|71628|4|Described|p1: 1, 6, 8; p3: 6-9, 11-12, 59; p4:1-58|Permian|Permian|See also p5-1; p7: 4, 28, 40; p8: 3, 44, 48; p10-4; p19: 2, 4, 28, 39, 41-44, 136, 166-167, 171. Bryant et al. (2002, 2003, 2004). A 200 km long meridional belt towards the W margin of the southern New England Orogen; parallel to and just to the E of the Peel Fault. Constituents are identified by textural, geochemical and radiometric variations: problems discussed. Commonly deeply weathered. Comprises Banalasta, Copeton, Glenclair, Graman, MacDonald River, Pringles, Rocky Glen Suites. Geochemistry described.|292-285 Ma.||Linton, Graman, Copeton, Namoi Tops, Pringles, Banalasta, MacDonald River, Rocky Glen Monzogranites; Glenclair Syenogranite; Giants Den Leucosyenogranite.|Intrudes Tablelands Complex. Is intruded by Willowrie Diorite.|Mainly S-type granites: (leuco) monzogranite to (leuco) syenogranite. Characteristically coarse-grained, commonly porphyritic, whitish, with megacrysts/phenocrysts of white K-feldspar (up to 80mm) and large apatite crystals.|
67901|Bundarra Supersuite|71703|4|Described|p192-193, 198|Early Permian|Late Carboniferous|Of New England Batholith.|Ages from 285.3+/-2.3 Ma to 298.5+/-2.9 Ma||||Cordierite bearing monzogranites.|
67901|Bundarra Supersuite|72078|5|Briefly described|p5|||Geological province: New England Orogen. |||Includes Pringles Monzogranite.|||
67901|Bundarra Supersuite|73197|6|Mentioned|p471, 472 Tb.2|Kungurian|Asselian|New England Orogen, southern. Geosynchronous with rifting, intrudes accretionary wedge, S-type. [Written only as Bundarra on p472 Tb.2, could be Bundarra Suite?]. U-Pb zircon ages from Black (1994), Cawood et al., (2011a), Cross and Blevin (2013), Jeon et al., (2012), Jeon et al., (2014), Kemp et al., (2009), Phillips et al., (2011) and Rosenbaum et al., (2012).|292.3 +/- 1.5 Ma, 282.0 +/- 4.0 Ma U-Pb zircon||||Granitoids.|
67901|Bundarra Supersuite|73202|6|Mentioned|p634|||||||||
67901|Bundarra Supersuite|73264|6|Mentioned|p1398-1399|Permian|Permian|New England Orogen. S-type granitoids. Contains large amount of Carboniferous zircon cores. Zircon eHf values of +5 to +8 and +13 to +18.|||Banalasta Monzogranite|||
67901|Bundarra Supersuite|73570|6|Mentioned|p918|Early Permian|Early Permian|New England Orogen.||||||
39274|Bundeena Group|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
29518|Bundella Syenite|23214|3|Fully described|p94|Late Ordovician|Late Ordovician|Intrudes the Weemalla Formation. Mildly altered pyroxene monzodiorite.||||||
29518|Bundella Syenite|43640|5|Briefly described|Map Legend||Ordovician|||||||
29518|Bundella Syenite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29518|Bundella Syenite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
69877|Bundong Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Bundong Suite. Pink porphyritic hornblende-biotite granite with phenocrysts of K-feldspar, plagioclase and quartz. High radiometric response.||||||
69877|Bundong Granite|68592|3|Fully described|p1674-81|Early Devonian|Early Devonian|Named after Bundong homestead, Braidwood area. Labelled as Boro Granite on several geological maps (listed). Distinguished by Fitzherbert et al. (2011): reasons elaborated. Representative outcrop mentioned. Contact metamorphic aureole 300-600m wide, with cordierite. Has petrographic and geochemical affinities with other members of the Glenbog Suite.||Unit in Glenbog Suite.||Intrudes Abercrombie Formation and Mundoonen Sandstone.|Pink, massive, medium- to coarse-grained, inequigranular biotite granite; large prominent quartz crystals; some microgranite dykes and veinlets occur within the granite.|
69877|Bundong Granite|69159|5|Briefly described|Map legend|Pragian|Pragian|||Unit in Glenbog Suite.|||Pink, massive, medium- to coarse-grained, inequigranular, biotite granite.|07-SEP-15
69877|Bundong Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dob. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Glenbog Suite|||Pink, massive, medium-coarse grained, inequigranular biotite granite; minor microgranite dykes. Generally has a high radioelement response and high magnetic susceptibility.|
69877|Bundong Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Glenbog Suite|||Pink, massive, medium-coarse grained, inequigranular biotite granite; minor microgranite dykes. Generally has a high radioelement response and high magnetic susceptibility.|
69877|Bundong Granite|71069|6|Mentioned|p40 fig 17, p151|||||Glenbog Suite||||
69877|Bundong Granite|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Glenbog Suite.|||Pink, massive, medium- to coarse-grained, inequigranular biotite granite.|
69877|Bundong Granite|71700|3|Fully described|vi, ix, p7, p26, p37, p44|Early Devonian|Early Devonian|Named for the property of Bundong. Representative outcrops of the Bundong Granite occur in paddocks north and south of Glenoval Road, near GR 743366 6121667. The Bundong Granite was mapped as Boro Granite by Felton and Huleatt (1975). It was separated during recent mapping because of its different textural character and geographic separation from the Boro Granite. Chappell et al. (1991) used the invalid name Lake Bathurst Granite, and included the granite in a Lake Bathurst Suite, Bundong Granite is now the preferred name. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. See also p49, p62-p63, p71, p83, CD. Lithology is discussed in detail. May also intrude the Warbisco Shale. Age is derived from the geochemically similar Boro Granite dated at 411.5 +/- 3.1 Ma.||Glenbog Suite||Intrudes the Mundoonen Sandstone and the Abercrombie Formation.|Pink, massive, medium- to coarse-grained, inequigranular biotite granite.|
34392|Bundook beds|22736|6|Mentioned|p628,9|Famennian|Frasnian|||||||
34392|Bundook beds|22857|4|Described|p500 App.1 Tb.A1.7|Tournaisian|Famennian|Includes the "Bowman beds". Lithic arenite, mudstone, siltstone often with ribbon banding, minor conglomerate and shale. Max. thickness: >2740m. ||||||
34392|Bundook beds|44093|5|Briefly described|p67 Fig. 6.6, p231 App. 1|Tournaisian|Devonian|Geological Province: Myall Block; New England Fold Belt.||||||
34392|Bundook beds|44244|4|Described|p191-192|Late Devonian|Late Devonian|Max. thickess: 2740m.  Geological Province: Myall Block.  See also "Bundook Beds".||||||
34392|Bundook beds|50263|5|Briefly described|Map Legend|Late Devonian|Devonian|Underlies: Wallanbah Formation.  Geological Province: Eastern Myall Block.||||||
23439|Bundycoola Formation|22518|4|Described|Table 1, p 6, 7, 10||Late Devonian|Mulga Downs Group||||||
23439|Bundycoola Formation|22768|6|Mentioned|p186|||||||||
23439|Bundycoola Formation|22857|4|Described|p212, p486 App.1 Tb.A1.7|Famennian|Frasnian|Of Mulga Downs Group. Includes Keginni Conglomerate Member. Polymictic litharenite and polymictic conglomerate; gritty layers, interbedded with siltstone and friable silty arenite. Max. thickness: 600m in Mount Grenfell area. Geol. Prov: Barka Basin.||||||
23439|Bundycoola Formation|22859|5|Briefly described|p212|||||||||
23439|Bundycoola Formation|23171|6|Mentioned|p16|||||||||
23439|Bundycoola Formation|23173|6|Mentioned|Map Legend|||||||||
23439|Bundycoola Formation|37798|4|Described|Table I|||||||||
23439|Bundycoola Formation|38292|6|Mentioned|Fig.1|||||||||
23439|Bundycoola Formation|40913|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
23439|Bundycoola Formation|41126|3|Fully described|p129|||Mention P108||||||
23439|Bundycoola Formation|41138|6|Mentioned|Map legend|Devonian|Devonian|||||||
23439|Bundycoola Formation|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
23439|Bundycoola Formation|41821|2|Defined|p62|Middle Devonian||||||||
23439|Bundycoola Formation|42983|6|Mentioned|Fig.3,p345|||||||||
23439|Bundycoola Formation|43032|2|Defined|p190|Middle Devonian||Of Mulga Downs Group.||||||08-APR-09
23439|Bundycoola Formation|61213|5|Briefly described|p322|||Contains the Keginni Conglomerate Member. Overlain by the Crowl Formation. Geological Province: Darling Basin.||||||
23439|Bundycoola Formation|64964|5|Briefly described|p160, p163|||Of Mulga Downs Group. Includes the Keginni Conglomerate Member.||||||08-APR-09
23439|Bundycoola Formation|64967|5|Briefly described|p114 Fig. 2|Frasnian|Givetian|Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). See also p115 Fig. 3.||||||
23439|Bundycoola Formation|65759|5|Briefly described|p114 Fig.2||Frasnian|Underlies the Crowl Creek Formation, unconformably overlies the Bulgoo Formation. 300m thick, part of the Mulga Downs Group.||||||
23439|Bundycoola Formation|70751|6|Mentioned|p12|Emsian|Emsian|||Mulga Downs Group||||
23439|Bundycoola Formation|71040|5|Briefly described|p28 Fig.15|Devonian|Devonian|Diagram of major faults and contractional deformation related to Tabberabberan Orogeny.||Mulga Downs Group.|Keginni Conglomerate Member.|||
23439|Bundycoola Formation|72958|6|Mentioned|p11|Emsian|Emsian|Cobar Basin. Nymagee area.||Mulga Downs Group||Underlain by Bulgoo Formation. Overlain by and equivalent to Crowl Creek Formation.||
23440|Bungaba Coal Member|42657|3|Fully described|p81|||Of Glen Davis Formation.||||||04-AUG-04
23440|Bungaba Coal Member|68004|5|Briefly described|p60 Table 6, p61.|Late Permian|Late Permian|Western Coalfield. Uneconomic, but coalesces with Moolarben Coal Member (State Mine Creek Formation) to form a 13.6 m thick layered seam NW of Ulan.||Unit in Glen Davis Formation.||Is overlain by, and locally coalesces with, Moolarben Coal Member.|Dull/minor bright coal; numerous carbonaceous and tuffaceous claystone layers.|
79357|Bungambil Granite|71889|6|Mentioned|p7|||||||||
79357|Bungambil Granite|72083|5|Briefly described|p37|Devonian|Devonian|Trigg (2016). Crops out SE of Ardlethan.|c.413 Ma (Bodorkos et al.,in prep.).||||Biotite granite. I-type.|
82373|Bungawalbin Member|70820|6|Mentioned|p37|Cretaceous|Cretaceous|Richmond River catchment area (Casino-Kyogle area) basement aquitard.||||Overlies the Kangaroo Creek Sandstone Member.||
24203|Bungendore Formation|24128|5|Briefly described|p89|||Geological Province: Lachlan Fold Belt.||||||
24203|Bungendore Formation|42727|5|Briefly described|map schematic section|Quaternary|Tertiary|Clay, silt; lacustrine facies. Overlies Ondyong Point Formation. See Lake George Subsurface stratigraphy schematic section and chart.||||||
24203|Bungendore Formation|42820|2|Defined|p58|Pliocene||||||||
24203|Bungendore Formation|47060|5|Briefly described|p163|||Reserved R.Abell 1984.||||||
24203|Bungendore Formation|67125|5|Briefly described|Slide 36.|Cenozoic|Cenozoic|Tertiary-Quaternary.||||Overlies Ondyong Point Formation.|Lacustrine clay and silt.|
24203|Bungendore Formation|70377|5|Briefly described|p855, p856, p858 Fig 4|Quaternary|Quaternary|Lake George Basin. Maximum thickness at type section Core C354:54m. ||||Uppermost and youngest unit infilling Lake George. Underlain by Ondyong Point Formation.|Lacustrine clay|
24203|Bungendore Formation|71069|5|Briefly described|p21 fig 7, p33, p208-210|Quaternary|Quaternary|Name derived from the town of Bungendore. Type section defined in BMR drillhole at GR 71810 6113990. Fluvial to lacustrine depositional environment. Estimated maximum thickness of 54m. See also  p211 ph 100, p214.  ||Weereewa Group||Conformably overlies the Ondyong Point Formation or overlies the Gearys Gap Formation.|Clay and silt.|
24203|Bungendore Formation|71691|5|Briefly described|Map legend.|Quaternary|Neogene|||Weereewa Group.||Overlies Ondyong Point Formation.|Lake deposits: mottled clay, gravelly clay with quartz and lithic clasts, and clay with carbonaceous or silty laminations; red-brown ferruginous profiles occur sporadically throughout.|
34589|Bungonia Group|22842|4|Described|p25,26|Devonian|Late Silurian|Records Bungonia Limestone upgraded to group status.||||||03-JUN-08
34589|Bungonia Group|24317|5|Briefly described|p14, p15 Fig.1|Silurian|Silurian|Shallow marine limestone.||||||
34589|Bungonia Group|50234|5|Briefly described|Map Legend|Lochkovian|Ludlow|Includes: Frome Hill Formation, Cardinal View Formation.||||||
34589|Bungonia Group|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Wombeyan Limestone, and Frome Hill and Cardinal View Formations.||||||
34589|Bungonia Group|67820|5|Briefly described|p133, p136 Fig.3|Ludlow|Ludlow||||Cardinal View, Frome Hill Formations.||Includes shale.|
34589|Bungonia Group|68592|1|Redefined|p238, p240, p742, p771, p860, p898-925|Lochkovian|Wenlock|See also p74 Tb.5, p91. Of Bungonia Shelf. Originally Bungonia Limestone (Carne and Jones, 1919); later raised to Group status (James, Francis and Jennings, 1978) with 5 un-named subdivisions. Formally defined as Bungonia Group with 2 Formations by Bauer (1994). Redefined in this study and extended to include Wombeyan Limestone. Up to 1235m thick. Extensively quarried at South Marulan for cementmaking and steelworks. Diverse fauna described. The only direct contact between Mount Fairy Group and limestone and shale-rich Bungonia Group to the east occurs where Mares Forest Volcanics unconformably overlies Wombeyan Limestone near Wombeyan Caves (Osborne, 1993). Available evidence suggests that the Bungonia Group is age-equivalent to the lower part of the Mount Fairy Group. Bungonia structural zone: deformation described.|||Includes Karalinga, Frome Hill and Cardinal View Formations; Tugalong Limestone Member and Wombeyan Limestone.|Overlies Adaminaby Group (unconformably or faulted). Is intruded by Marulan Supersuite. Is overlain by (or faulted against) Tangerang Formation. Equivalent to lower Mount Fairy Group.|Limestone, siltstone, shale and sandstone.|
34589|Bungonia Group|69159|5|Briefly described|Map legend|Silurian|Silurian||||Includes Cardinal View Formation.|||
34589|Bungonia Group|70192|5|Briefly described|Map Legend|Pridoli|Wenlock|On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Cardinal View Formation, Frome Hill Formation, Wombeyan Limestone.|||
34589|Bungonia Group|70542|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Cardinal View Formation, Frome Hill Formation|||
34589|Bungonia Group|70543|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Wombeyan Limestone|||
34589|Bungonia Group|70661|3|Fully described|vii, viii, p4, p12,|Lochkovian|Wenlock|Formerly the Bungonia Limestone, raised to group status by Bauer (1994).  Hornfelsed where it contacts the Arthursleigh Suite. Estimated maximum thickness of 1235m.  Deposited in shallow marine environment with variations in lithology and facies reflecting minor changes in the depth of deposition.Structure, metamorphism and deformation discussed in detail. Fossil assemblage includes stromatolites, bivalves, corals, brachiopods, graptolites and conodonts. Fossil assemblage constrains age.  See also p31, p31 tbl 1, p19, p31-p36.|||Karalinga Formation, Tugalong Limestone Member, Wombeyan Limestone,  Cardinal View Formation, Lookdown Limestone|Unconformably overlies (and is faulted against) Adaminaby Group, Bendoc Group,  Tallong beds, intruded by Glenrock Granodiorite, Arthursleigh Tonalite, Unconformably overlain by Tangerang Formation|Shallow marine limestone, siltstone, shale, sandstone, skarn, marble and calc-silicate.|
34589|Bungonia Group|71040|6|Mentioned|p11|Silurian|Silurian|Deformed and considerably shortened by the Early Devonian Bindian (=Bowning) Orogeny.||||||
34589|Bungonia Group|71069|6|Mentioned|p23, p43, p73 fig 26, p100|||See also p134, p135, p146.||||Intruded by the Candelo and Arthursleigh Supersuites. Part equivalent to the De Drack Formation.||
34589|Bungonia Group|71303|5|Briefly described|map legend|Devonian|Silurian||||Includes Lookdown Limestone, Cardinal View Formation, Frome Hill Formation.||Limestone, siltstone, shale and sandstone; calc-silicate wollastonite-diopside hornfels, locally. Isolated bryzoan and brachiopod fragmants locally.|
34589|Bungonia Group|71656|4|Described|p10 Fig.1, p13 Fig.2, p31|Lochkovian|Ludlow||||Cardinal View Formation, Frome Hill Formation, Wombeyan Limestone.|Partially equivalent to Mount Fairy Group.||
34589|Bungonia Group|71699|5|Briefly described|Map legend.|Silurian|Silurian||||Cardinal View Formation.|||
34589|Bungonia Group|71700|4|Described|vi, p7, p10, p15-p16, p23-p24, CD|Lochkovian|Wenlock|Bungonia Shelf. Named for the village of Bungonia. This unit was previously the Bungonia Limestone of Carne and Jones (1919) before being divided by James et al (1978) who raised its status to the Bungonia Limestone Group. Subdivisions were described in greater detail by Carr, Jones et al (1980) before being formally defined as the Bungonia Group by Bauer (1994). Distribution, geomorphic expression, outcrop, structure, metamorphism, geophysical characteristics, geochemistry, fossils, economic geology and depositional environment are discussed. Equivalent to most of the Mount Fairy Group.Thickness is estimated at 1235m. Structural geology and metamorphism are discussed. See also p36-p39, p41, p43, p57-p58, p62, p74, p82, p96, p107, p110.|||Includes the Cardinal View Formation, Lookdown Limestone Member, Wombeyan Limestone Member, Karalinga Formation, Tugalong Limestone Member and the Frome Hill Formation|Unconformably overlies the Adaminaby Group.Unconformably overlain by the Bindook Group. Faulted against (or unconformably overlain by) the Tangerang Formation.|Limestone, siltstone, shale and sandstone.|
38279|Bungulla Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Of Moonbi Plutonic Suite.  Very coarse-grained porphyritic monzogranite; large euhedral, pink K-feldspar in medium-grained matrix of plagioclase, quartz, K-feldspar, biotite, hornbledne and sphene; rounded, mafic enclaves abundant in places.||||||20-DEC-04
38279|Bungulla Monzogranite|23812|4|Described|p21 Tb.2, p30|Early Triassic|Late Permian|Of Moonbi Plutonic Suite.  Intruded by the Stanthorpe Monzogranite.||||||
38279|Bungulla Monzogranite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Pale pinkish grey to grey, fine- to medium-grained (groundmass) , coarsely porphyritic titanite-hornblende-biotite monzogranite to granodiorite?; +pale pink to white K-feldspar megacrysts; locally granophyric; minor aplitic leucogranite; high magnetic res||||||12-DEC-07
38279|Bungulla Monzogranite|63748|3|Fully described|p81-82 Appdx.1 |||Of Bungulla Suite. Incl.in Undercliffe Falls Adamellite by Thomson (1976). Intruded by Stanthorpe + Ruby Ck Granites. Characterised by presence large euhedral K-feldspar phenocrysts + grains of titanite. I-type. See also p36, p41, p27 Fig. 27, p29 Fig. 33||||||07-FEB-11
38279|Bungulla Monzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Olenekian||248 - 243 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38279|Bungulla Monzogranite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Dormans Flat, Ruby Creek, Sailor Jack and Stanthorpe Granites, are all mapped under the symbol, Rgn.||||||
38279|Bungulla Monzogranite|68679|5|Briefly described|p453, p455-456, p458, p460-461, p464|Middle Triassic|Permian|Northern New England Batholith. Previously the Bungulla Porphyritic Adamellite of Shaw (1969). ~18 km2. Extends from Wallangarra into NSW. A relatively mafic unit. Geochemical plots.||Bungulla Suite.||Possibly intrudes the Wallangarra Volcanics. Is intruded by Stanthorpe and Ruby Creek Granites.|Pinkish-grey, coarsely porphyritic titanite-hornblende-biotite granodiorite? to monzogranite; K-feldspar phenocrysts; locally rapakivi textured, mafic enclaves, granophyric; relatively mafic. Oxidised, highly evolved, high-K; I-type.|
38279|Bungulla Monzogranite|68901|6|Mentioned|p8 Fig. iii|Early Triassic|Late Permian|||||||26-SEP-18
38279|Bungulla Monzogranite|69639|4|Described|p1-p2, p5, p8-p9, p50, p62|Lopingian|Lopingian|New England Orogen. Contact with the Billyrimba Leucomonzogranite is obscured by poor outcrop. Said to be of the Bolivia Range Suite on p80. Sampling locality, petrography and geochronology are discussed. Geochemically similar to the Bookookoorara Monzogranite. Mistakenly referred to as the Bungulla Granite on p9, p81, p240. See also p80-p86, p157, p163, p221, p240.|252.5 +/- 1.2 Ma (SHRIMP)|Bungulla Suite||Intruded by the Mount Jonblee Leucomonzogranite. Intrudes the Sandy Flat Monzogranite.|Coarse-grained, porphyritic biotite-amphibole bearing monzogranite.|
38279|Bungulla Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Changhsingian|Changhsingian|New England Orogen.|252.5 +/- 1.2 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
38279|Bungulla Monzogranite|71628|3|Fully described|p1:7; p7: 1, 37; p8:80; p11: 2, 7-15, 19|||See also p11: 24, 26, 35, 40, 45; p12: 4-5; p14: 12, 28; p15: 5, 16, 25, 33, 57, 65, 82, 92-93, 105; p16-20; p19: 18, 21-22, 94, 97, 160. Willis (1987). Previously the Bungulla Porphyritic Adamellite (Wilkinson,1969) after Bungulla Porphyritic-Adamellite (Shaw, 1964?); later Bungulla Adamellite (Robertson, 1970) and 'Bungulla Porphyritic Adamellite' (Thomson, 1976, with other, often informal, variations). The history of its varied and current definitions is detailed. Included in the Moonbi Plutonic Suite by Shaw and Flood (1981). Apparently previously included rocks here grouped as the Sailor Jack Supersuite. Named after the locality of Bungulla. Type locality is 8 km S of Tenterfield along the New England Highway. Comprises three bodies (described), bounded by numerous units (all named). Forms gently undulating country with outcrops of isolated tors and whalebacks. Described in great detail. Geochemistry described. RELATED UNITS (continued): Is 'bound' (?intruded) by Cottesbrook Monzogranite and Billyrimba Leucomonzogranite. Is faulted against Stanthorpe and Rocky River Monzogranites. Is intruded by Mount Jonblee Leucomonzogranite, Ruby Creek Leucogranite, Black Snake Creek Granite and Mount Lindesay Monzogranite. Abuts Tenterfield Creek Leucosyenogranite.|252.5 +/- 1.2 Ma (SHRIMP: Chisholm et al., 2014).|Bungulla Suite.||Intrudes Dundee Rhyodacite, Wallangarra Volcanics, Sandy Flat Leucomonzogranite and undifferentiated Wandsworth Volcanic Group. See COMMENTS for more.|Coarsely porphyritic, biotite-hornblende-(clinopyroxene) monzogranite characterised by large pink K-feldspar megacrysts set in a medium-grained matrix; locally contains abundant enclaves. I-type.|
38279|Bungulla Monzogranite|72528|5|Briefly described|p78, p109.|Lopingian|Lopingian|Age determined on the Kangaroo Swamp mass, Chisholm et al (2014). It is the Bungulla mass of this unit that is intruded by the Black Snake Creek Granite.|252.5+/-1.2 Ma U-Pb SHRIMP.|||Intruded by Black Snake Creek Granite||
67899|Bungulla Suite|61783|5|Briefly described|p296|||In the Tenterfield area.  Granites.||||||
67899|Bungulla Suite|63748|5|Briefly described|p35, p36|||Includes the Bungulla and Undercliffe Falls Monzogranites and part of Bookookoorara Monzogranite. I-type granites occur mainly scattered around eastern margins of the Stanthorpe Granite.||||||07-FEB-11
67899|Bungulla Suite|68679|5|Briefly described|p456, p458-461, p462 Fig.5.133, p464|||See also p465 Fig.5.143. Northern New England Batholith. Forms scattered remnant intrusions around the southern margins of the spatially-associated Stanthorpe Granite. Geochemistry plots, discussion.||Stanthorpe Supersuite.|Bungulla Monzogranite.|||
67899|Bungulla Suite|69639|5|Briefly described|p9, p157|||New England Orogen.||Stanthorpe Supersuite|Includes the Bungulla Monzogranite and the Bookookoorara Monzogranite.|||
67899|Bungulla Suite|71628|5|Briefly described|p8: 97; p11:1-2, 5, 11-12,26,40; p19-21|||Donchak et al. (2007). Northern New England Batholith. In this study it broadly corresponds to Bungulla Supersuite.||Bungulla Supersuite.|Bungulla, Undercliffe Falls Monzogranites.|||
82122|Bungulla Supersuite|71628|5|Briefly described|p5:7; p7: 1-2; p8: 3; p9:1; p11: 1-46|||See also p12: 2, 9-10, 14, 16-17; p15: 1, 33, 52-53, 93, 95; p18-10; p19: 37, 91, 94, 99, 138. Broadly corresponds to Bungulla Suite of Donchak et al. (2007). Comprises a small number of intermediate, high-K granites in the northern portion of the southern New England Orogen. Petrology and geochemistry described; contrasted with Moonbi Supersuite.|254-250 Ma (SHRIMP: Chisholm et al., 2014).||Undercliffe Falls Monzogranite; Bookookoorara, Bungulla, Rocky River and Mount Mitchell Suites.||Grey to pink, medium- to very coarse-grained, moderate to highly porphyritic to equigranular, titanite-bearing, biotite-hornblende-(clinopyroxene) monzogranite with lesser (locally) granodiorite, and rarer quartz monzonite. I-type.|
82122|Bungulla Supersuite|72528|6|Mentioned|p84.|||Geographically close to Malara Quartz Monzodiorite, but geochemically very distinct.||||||
73423|Bunker Creek Formation|66623|2|Defined|pp47-49, p38, p409.|Cambrian|Middle Cambrian|Defined in this study. Formerly part of Packsaddle Series (Andrews 1922), Wonominta Beds (Warris 1967) and Complex (Scheibner 1972), part of Teltawongee beds (Mills 1992). About 10 km thick. Equivalent to Nundora, Wonnaminta, Copper Mine Range Formations. Recent drilling has intersected gold mineralisation.|Minimum age of 515.5 +/- 2.7 Ma.|Unit in Teltawongee Group.||Intruded by Williams Peak Granite and Bittles Tank Volcanics. Faulted against Ponto Group. Is overlain by Copper Mine Range Formation and, unconformably, by Kayrunnera Group.|Coarse- to fine-grained, turbiditic, muscovite-bearing quartzo-feldspathic sandstone; graded bedded; sharp bases, fining up to siltstone and sporadic mudstone in upper parts of many bedding units. Trace fossils only (worm tubes and burrows).|
73423|Bunker Creek Formation|67105|5|Briefly described|p655, 661|Cambrian|Cambrian|Occurs E of the Koonenberry Fault.||Teltawongee Group.||Is intruded by Williams Peak Granite.||
73423|Bunker Creek Formation|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Turbiditic silty and muddy massive sandstone, erosional basal contact with some rip-up clasts, sand to 1 mm, detrital muscovite to 3 mm; up-section are climbing ripples, laminations, and rare muddy tops.|
73423|Bunker Creek Formation|67210|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Turbiditic silty and muddy massive sandstone, erosional basal contact with some rip-up clasts, sand grains to 1 mm, detrital muscovite to 3 mm; up-section are climbing ripples, laminations and rare muddy tops.|
73423|Bunker Creek Formation|67211|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Teltawongee Group.||Overlies Tibooburra Suite. Is overlain by Rolling Downs Group.|Turbiditic silty and muddy sandstone, erosional basal contact with some rip-up clasts, sand grains to 1 mm, detrital muscovite to 3 mm; up-section are climbing ripples, laminations and rare muddy tops.|
73423|Bunker Creek Formation|67322|5|Briefly described|p10, p20 Fig.5|Cambrian|Cambrian|Defined by Mills in Greenfield et al.,(2010). Maximum age is constrained from p20 Fig.5 (Strat. column). Occurs in the Kayrunnera-Koonenberry region.|<515.1 +/- 2.7 Ma.|Of the Teltawongee Group||Is intruded by Williams Peak Granite.||
73423|Bunker Creek Formation|69961|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Turbiditic silty and muddy sandstone, erosional basal contact with some rip-up clasts, sand grains to 1 mm, detrital muscovite to 3 mm; up-section are climbing ripples, laminations and rare muddy tops.|
73423|Bunker Creek Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|||Teltawongee Group|||Turbiditic silty and muddy massive sandstone; erosional basal contact with some rip-up clasts, sand grains to 1mm, detrital muscovite to 3mm; climbing ripples, laminations and rare muddy tops.|
73423|Bunker Creek Formation|70838|4|Described|p268-272, p274, p276|Cambrian|Cambrian|SE Koonenberry Belt. High-energy deep-water deposits. Maximum depositional age from detrital zircons (this study). Minimum age from intrusion (Black, 2007). Detrital zircon analyses.|517 +/- 10 Ma (MDA) to 515 +/- 2.7 Ma.|Teltawongee Group.||Is intruded by Williams Peak Granite.|Characterised by repetitive sequences of immature sandstone (up to 3m thick locally) overlain by an upward-fining sequence (locally absent) of fine sandstone, siltstone and mudstone. Ubiquitous large (<5mm) detrital white mica grains.|
73423|Bunker Creek Formation|71262|6|Mentioned|p9 Fig 6|Cambrian|Cambrian|Age inferred from parent Group.||Unit of Teltawongee Group||||
73423|Bunker Creek Formation|73177|5|Briefly described|p1109 Fig.13(a), 1113, 1114, 1115|Early Cambrian|Early Cambrian||517 +/- 10 Ma.|Teltawongee Group.||||
73423|Bunker Creek Formation|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
81946|Burbie Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|||Green, white weathering, porphyritic to equigranular fine-grained basaltic trachyandesite; minor trachyandesite.|02-NOV-20
23444|Burdekins Gap Basalt Member|22857|5|Briefly described|p504 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Alum Mountain Volcanics. Massive crystalline and amygdaloidal alkaline olivine basalt with thin interbeds of conglomerate, lithic sandstone; minor coal seams. Max. thickness: 350m.||||||
23444|Burdekins Gap Basalt Member|36057|2|Defined|p350|Early Permian|Late Carboniferous|Late Carboniferous - Early Permian.||||||
23444|Burdekins Gap Basalt Member|39660|6|Mentioned|p449|||||||||
23444|Burdekins Gap Basalt Member|42833|5|Briefly described|p225|||of Alum Mountain Volcanics||||||
23444|Burdekins Gap Basalt Member|44244|4|Described|p224|Early Permian|Early Permian|Of the Alum Mountain Volcanics.  Geological Province: Myall Block. Maximum Thickness: 350m.||||||16-SEP-04
23444|Burdekins Gap Basalt Member|50263|5|Briefly described|Map Legend|Sakmarian|Sakmarian|Underlies: Lakes Road Rhyolite Member.  Geological Province: Eastern Myall Block.||||||
25821|Burnamwood Formation|29942|3|Fully described|p11|||||||||
25821|Burnamwood Formation|29943|6|Mentioned|p37|||||||||
25821|Burnamwood Formation|35767|6|Mentioned|p9|||||||||
25821|Burnamwood Formation|37087|6|Mentioned|p197|||||||||
25821|Burnamwood Formation|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
25821|Burnamwood Formation|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
25821|Burnamwood Formation|40166|6|Mentioned|Table 1|||See also Fig.27||||||
25821|Burnamwood Formation|40256|6|Mentioned|Fig.3|||Mention Fig.4||||||
25821|Burnamwood Formation|40805|2|Defined|p137|Permian|Permian|||||||
25821|Burnamwood Formation|41010|6|Mentioned|Fig.3|||||||||
25821|Burnamwood Formation|41054|6|Mentioned|Fig.3|||||||||
25821|Burnamwood Formation|42078|6|Mentioned|Table 1 P5|||||||||
25821|Burnamwood Formation|42922|6|Mentioned|Fig.14|||||||||
25821|Burnamwood Formation|44244|4|Described|p236 Tb.4|Late Permian|Late Permian|Of the Jerrys Plains Subgroup.  Includes: Mount Arthur seam, Piercefield seam, Vaux seam, Broonie seam, Bayswater seam.  Underlies the Fairfield Formation.  Type section intext.  max. thickness: >214m.||||||
25821|Burnamwood Formation|45090|5|Briefly described|p56|||Relationship, correlation & age||||||
25821|Burnamwood Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Jerrys Plain Subgroup (Wittingham Coal Measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
25821|Burnamwood Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. 97.1 m thick. Includes Bayswater, Broonie, Vaux, Piercefield and Mount Arthur coal seams.||Basal unit in Jerrys Plains Subgroup.||Overlies Archerfield Sandstone. Is overlain by Fairford Formation.|Sandstone, siltstone and five named coal seams.|
25821|Burnamwood Formation|69683|6|Mentioned|p411 Fig.2, p415-419 Figs.3-4|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.||||
70469|Burnewang Ignimbrite Member|62095|5|Briefly described|p251, p272 Appdx.|Early Carboniferous|Early Carboniferous|Of the Merlewood Formation. Varies from single dense, red unwelded ignimbrite to thin interbeds of ignimbrite, siltstone and volcanolithic sandstone; some reworking shown. Age: ~343Ma. Max.thickness: 10m. Geological Province: Werrie block/Tamworth Belt.||||||
31556|Burnt Hill Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
31556|Burnt Hill Suite|68592|6|Mentioned|p1508|||Chappell et al. (1991); consisted of Burnt Hill Granite which was later assigned to the Whick Whack Suite (Blevin, 2011).||||||
31556|Burnt Hill Suite|71206|6|Mentioned|p373|||Lachlan Fold Belt.|||Burnt Hill Granite.||Aluminous A-type granite.|
77076|Burnt Yards Basalt Member|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3). Shown as Burnt Yards Basalt Mbr.||Forest Reefs Volcanics||||
28305|Burra-Moko Head Sandstone|22745|6|Mentioned|p129|||Sydney Basin.||||||
28305|Burra-Moko Head Sandstone|22857|5|Briefly described|p526 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Grose Subgroup (Narrabeen Group). Quartzose to quartz-lithic sandstone. Max. thickness: 112m. Geological Province: Sydney Basin.||||||
28305|Burra-Moko Head Sandstone|23214|5|Briefly described|p269|Triassic|Triassic|Quartz rich sandstone of the Narrabeen Group.||||||
28305|Burra-Moko Head Sandstone|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
28305|Burra-Moko Head Sandstone|29749|4|Described|p12|||||||||
28305|Burra-Moko Head Sandstone|31061|6|Mentioned|Table 1|||||||||
28305|Burra-Moko Head Sandstone|37804|6|Mentioned|Table 1|||||||||
28305|Burra-Moko Head Sandstone|39287|6|Mentioned|p44|||||||||
28305|Burra-Moko Head Sandstone|39293|4|Described|p146|||Isopach map Fig. 8.7||||||
28305|Burra-Moko Head Sandstone|39308|6|Mentioned|p501|||||||||
28305|Burra-Moko Head Sandstone|42925|4|Described|p11|||of Grose Subgroup||||||
28305|Burra-Moko Head Sandstone|42926|4|Described|map legend||Early Triassic|||||||
28305|Burra-Moko Head Sandstone|43194|5|Briefly described|p130|Triassic|Triassic|Sandy alluvial outwash material deposited along the western margins of the Sydney Basin.||||||
28305|Burra-Moko Head Sandstone|45090|6|Mentioned|p71|||Relationships in Narrabeen Gp.||||||
31555|Burraga Suite|42726|5|Briefly described|map legend||Carboniferous|||||||
31555|Burraga Suite|44093|5|Briefly described|p208 App. 1|Late Carboniferous|Late Carboniferous|Geological Province: Lachlan Fold Belt.||||||
26295|Burragundy Formation|40328|2|Defined|p75|Silurian|Silurian|||||||
26295|Burragundy Formation|43494|6|Mentioned|p18||Silurian|Mapped by Pickett (1982) - but is probably a continuation of the Cary Formation in the Loombah Creek area and further north||||||07-SEP-05
25822|Burralow Formation|22745|6|Mentioned|p133|||Sydney Basin.||||||
25822|Burralow Formation|22857|5|Briefly described|p526 App.1 Tb.A1.9|Middle Triassic|Early Triassic|Of the Narrabeen Group. Shale/sandstone laminite. Max. thickness: 6m. Geological Province: Sydney Basin.||||||
25822|Burralow Formation|22969|5|Briefly described|Fig 2.2||Middle Triassic|Narrabeen Group.||||||
25822|Burralow Formation|23218|6|Mentioned|p28|||||||||
25822|Burralow Formation|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
25822|Burralow Formation|24079|5|Briefly described|p433 Fig. 6|Triassic|Triassic|Of Narrabeen Group. Geological Province: Sydney Basin.||||||
25822|Burralow Formation|24123|5|Briefly described|p3|Triassic|Triassic|Of Narrabeen Group. Geological Province: Sydney Basin.||||||
25822|Burralow Formation|30007|6|Mentioned|Fig.1|||||||||
25822|Burralow Formation|31061|5|Briefly described|p1318|||Includes Tabarag Sandstone Member, and a red bed unit, Wentwoth Falls Claystone Member.||||||25-SEP-08
25822|Burralow Formation|31297|6|Mentioned|p4|||See also P6, Fig. 3||||||
25822|Burralow Formation|31373|6|Mentioned|Table 1|||||||||
25822|Burralow Formation|31426|5|Briefly described|Fig.1|||||||||
25822|Burralow Formation|31725|6|Mentioned|p10|||On table||||||
25822|Burralow Formation|31880|6|Mentioned|p18|||||||||
25822|Burralow Formation|31884|6|Mentioned|Table 1|||Triassic||||||
25822|Burralow Formation|33683|6|Mentioned|Table 1|||Narrabeen Gp.||||||
25822|Burralow Formation|33685|6|Mentioned|Table 2|||||||||
25822|Burralow Formation|34107|6|Mentioned|p217|||||||||
25822|Burralow Formation|34121|4|Described|p397|||Type section described||||||
25822|Burralow Formation|34205|2|Defined|p31|Triassic|Triassic|||||||
25822|Burralow Formation|34209|5|Briefly described|Table 1|||Triassic. See also Figs.4,5,pp137,141 etc.||||||13-MAR-07
25822|Burralow Formation|34236|6|Mentioned|p17|||||||||
25822|Burralow Formation|34240|4|Described|p395|||Triassic||||||
25822|Burralow Formation|34301|6|Mentioned|p403|||||||||
25822|Burralow Formation|34336|6|Mentioned|Table 5.15|||Triassic.||||||
25822|Burralow Formation|36042|6|Mentioned|Table 1|||See also Fig.25.||||||
25822|Burralow Formation|36058|6|Mentioned|p4|||||||||
25822|Burralow Formation|37093|5|Briefly described|p231|||||||||
25822|Burralow Formation|39287|6|Mentioned|Fig.2.5|||See also Fig.2.21||||||
25822|Burralow Formation|39293|4|Described|p154|||||||||
25822|Burralow Formation|39306|6|Mentioned|p414|||See also P422||||||
25822|Burralow Formation|39308|6|Mentioned|p496|||||||||
25822|Burralow Formation|40653|6|Mentioned|Fig.20|||||||||
25822|Burralow Formation|42663|5|Briefly described|Table 2 P11|||||||||
25822|Burralow Formation|42925|3|Fully described|p13|||Of Grose Subgroup.||||||13-MAR-07
25822|Burralow Formation|42926|4|Described|map legend||Middle Triassic|||||||
25822|Burralow Formation|43146|6|Mentioned|Fig.2 p41|||of Narrabeen Group.||||||
25822|Burralow Formation|43317|4|Described|Table 1 p11|||||||||
25822|Burralow Formation|43318|14|Not recorded|opp p6||Late Triassic|||||||
25822|Burralow Formation|43320|14|Not recorded|Table 1||Triassic|Part of Narrabeen Group||||||
25822|Burralow Formation|43344|14|Not recorded|p21||Triassic|||||||
25822|Burralow Formation|43352|14|Not recorded|p 209-223||Triassic|||||||
25822|Burralow Formation|43359|14|Not recorded|Map Legend||Triassic|Provisional first edition||||||
25822|Burralow Formation|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Narrabeen Group||||||
25822|Burralow Formation|43361|14|Not recorded|Map Legend||Triassic|(Provisional first edition) Part of Narrabeen Group||||||
25822|Burralow Formation|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
25822|Burralow Formation|43383|14|Not recorded|p22|||||||||
25822|Burralow Formation|43385|14|Not recorded|p182, Table|||Inc Tabarag Ss Mb, L.Bunter. Ref. to Crook 1957||||||
25822|Burralow Formation|43395|2|Defined|p61,62,64,65,67,74||Early Triassic|p76-79||||||
25822|Burralow Formation|43880|14|Not recorded|p57|||||||||
25822|Burralow Formation|45090|6|Mentioned|p71|||Relationships in Narrabeen Gp.||||||
25822|Burralow Formation|60281|5|Briefly described|Fig. 7 Appendix 1|Middle Triassic|Middle Triassic|Of the Narrabeen Group.  Age: ~240Ma.  Geological Province: Sydney Basin.||||||
25822|Burralow Formation|65195|5|Briefly described|p3-4, p7-12, p14-15, p22-27, p29, p33|Early Triassic|Early Triassic|Of Narrabeen Group. Overlies Wentworth Falls Claystone Member. Variable lithology containing mainly quartz sandstones, shales and red-brown claystones. Outcrops along the lower gorge walls of the Grose River, Wheeny Creek and Glenbrook Creek||||||
25822|Burralow Formation|69297|6|Mentioned|p501|Anisian|Anisian|Sydney Basin. ||Narrabeen Group||Overlies the Grose Subgroup. Overlain by the Hawkesbury Sandstone.||
24797|Burranah Formation|13139|5|Briefly described|p9 Fig. 4, p10|Late Ordovician|Late Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||12-APR-05
24797|Burranah Formation|22466|6|Mentioned|P8||Ordovician|||||||
24797|Burranah Formation|22529|4|Described|1|Late Ordovician|Late Ordovician|||||||
24797|Burranah Formation|22857|5|Briefly described|p430 App. 1 Tb. A1.5|||Of the Cabonne Group. Max. thickness: 2.5km. See also p129 (photo).||||||
24797|Burranah Formation|23043|5|Briefly described|Map Legend|Eastonian|Gisbornian|Of Cabonne Group.||||||22-APR-09
24797|Burranah Formation|23170|2|Defined|p41|Bolindian|Eastonian|SHRIMP zircon age 435.4 +/-4.6Ma (Black, 1998). Cabonne Group.||||||
24797|Burranah Formation|23181|5|Briefly described|p1,3,6,7, Fig.1||Eastonian|Maximum age from fossils in allochthonous blocks.||||||
24797|Burranah Formation|23213|5|Briefly described|Fig.10 p24|Eastonian|Eastonian|Of Rockley-Gulgong Volcanic Belt.||||||22-APR-09
24797|Burranah Formation|23245|5|Briefly described|p129|||||||||
24797|Burranah Formation|23309|6|Mentioned|p390|||||||||
24797|Burranah Formation|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
24797|Burranah Formation|24126|6|Mentioned|p65|||||||||
24797|Burranah Formation|24463|4|Described|p321|Late Ordovician|Late Ordovician| Geological Province: Lachlan Fold Belt.||||||
24797|Burranah Formation|29993|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
24797|Burranah Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
24797|Burranah Formation|32046|6|Mentioned|p146|||||||||
24797|Burranah Formation|32047|6|Mentioned|Fig.1|||||||||
24797|Burranah Formation|32088|6|Mentioned|p6|||L.Devonian andesite and tuff||||||
24797|Burranah Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
24797|Burranah Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
24797|Burranah Formation|39663|6|Mentioned|Table 1|||||||||
24797|Burranah Formation|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
24797|Burranah Formation|44093|5|Briefly described|p213 App. 1|Late Ordovician|Late Ordovician|Of Carbonne Group. Geological Province: Lachlan Fold Belt.||||||
24797|Burranah Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p157|Late Ordovician|Late Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt, LFB. Age determined from conodonts found in discrete limestone lenses, Eastonian.||||||07-FEB-11
24797|Burranah Formation|63283|5|Briefly described|p205, p10|Late Ordovician|Middle Ordovician|Age: 450Ma. Thickness : 2.5 km. Geological Province: Rockley-Gulgong Volcanic Belt. Consists of a sequence of mafic to intermediate volcaniclastics sandstone and breccia. Intrudes by small monzodiorite. See also p205-206.||||||07-FEB-11
24797|Burranah Formation|63290|6|Mentioned|p392 Tb. 1, p397 Fig. 3(b)|Llandovery|Late Ordovician|Age: 435.4+/-4.6Ma (U-Pb zircons, Perkins et al 1995b; Watkins 1998b). Geological Province: Rockley-Gulgong Volcanic Belt.||||||
24797|Burranah Formation|63293|6|Mentioned|p471, p468 Fig. 2|Bolindian|Gisbornian|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
24797|Burranah Formation|64963|5|Briefly described|p182 Fig. 2, p184|||Age: 435+/-5Ma (Ar/Ar for an intrusion within this unit).||||||22-APR-09
24797|Burranah Formation|67322|5|Briefly described|p26|Ordovician|Ordovician|Described by Watkins, in Meakin and Morgan (1999). E margin of Hill End Trough. Age assigned due to the high potassium response (typical of Ordovician rocks in the Macquarie Arc) on ternary U-K-Th radioelement imagery.||Of the Cabonne Group|||Mass-flow deposits, conglomerates; minor allochthonous limestones.|21-FEB-18
24797|Burranah Formation|68004|6|Mentioned|p189.|Late Ordovician|Late Ordovician|South of Rockley-Gulgong Volcanic Belt. Shoshonitic.  Mentioned in the context of why rocks of this age/location do not appear to be prospective for porphyry Au-Cu mineralisation.||||||
24797|Burranah Formation|68592|6|Mentioned|p371|||Rockley-Gulgong Volcanic Belt.||Unit in Cabonne Group.||||
24797|Burranah Formation|70684|6|Mentioned|p3, p74|Late Ordovician|Late Ordovician|Rockley-Gulgong Volcanic Belt.||||||
25710|Burrandong Creek Member|22831|6|Mentioned|p 34|||||||||
25710|Burrandong Creek Member|24125|5|Briefly described|p108|||Geological Province: Lachlan Fold Belt.||||||
25710|Burrandong Creek Member|42489|5|Briefly described|Map legend|Llandovery|Bolindian|||||||
25710|Burrandong Creek Member|42718|5|Briefly described|p4|||||||||
25710|Burrandong Creek Member|43441|6|Mentioned|24|||now part of Bocobidgle Conglomerate. Formerly part of Goonumbla Volcanics||||||08-JAN-10
25710|Burrandong Creek Member|46522|1|Redefined|p45|Early Silurian||Supersedes Burrandong Creek Conglomerate Member.||||||
25710|Burrandong Creek Member|46525|6|Mentioned|Fig.1 P143|||||||||
25710|Burrandong Creek Member|46528|5|Briefly described|Map legend|Silurian||||||||
75833|Burrawan serpentinite|65317|6|Mentioned|p633, p622 Fig. 1c, p635 Fig. 14|Early Permian|Late Carboniferous|Appears to be an informal name for serpentinites lying on the Sapling Creek Fault between the Port Macquarie Block and the Hastings Block, New England Orogen.  Structures suggest Early Permian emplacement. Shown as Burrawan Serpentinite in figs.||||||
69893|Burrawinda Suite|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Wallah, Sentry Box, Narrawa Granites, Mulgowrie Granodiorite, Julong Granite and Winduella Tonalite.||||||12-JUN-08
69893|Burrawinda Suite|66300|5|Briefly described|p92.|||S-type. Time-equivalent to Hovells and Gunning Suites in west-central GOULBURN area.|427 Ma.||Includes Mulgowrie Granodiorite and Winduella Tonalite.|||
69893|Burrawinda Suite|68592|3|Fully described|p270, p1228, p1256-8, p1262-3, p1354-78|Late Silurian|Early Silurian|See also p74 Tb.5, p231. New name, after Burrawinda Creek. Includes some plutons of the former, now superseded, Wheeo Suite. The Mulgowrie Granodiorite is the type pluton. Geochemistry detailed. Latest Early Silurian. Has undergone moderate to high greenschist facies metamorphism. Wyangala structural zone: deformation described.|||Includes Mulgowrie Granodiorite; Winduella Tonalite; Wallah, Narrawa and Sentry Box Granites.|Intrudes Abercrombie Formation. Is intruded by Wyangala Supersuite.|S-type. Massive to foliated biotite +/- cordierite tonalite, granodiorite and granite; typically grey to cream to white, and medium- to coarse-grained; often contains mafic enclaves and metasedimentary xenoliths.|
69893|Burrawinda Suite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|On Crookwell and Gunning 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Winduella Tonalite, Mulgowrie Granodiorite, Narrawa Granite, Sentry Box Granite, Wallah Granite.|||
69893|Burrawinda Suite|70541|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Winduella Tonalite, Mulgowrie Granodiorite.|||
69893|Burrawinda Suite|70544|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Mulgowrie Granodiorite, Narrawa Granite, Sentry Box Granite, Wallah Granite|||
69893|Burrawinda Suite|70545|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Wallah Granite|||
42497|Burridgee Diorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Dark grey to green-grey, massive equigranular to sparsely porphyritic quartz diorite; minor fine-grained quartz dolerite and coarse-grained equigranular gabbro.||||||
42497|Burridgee Diorite|68592|3|Fully described|p609, p611, p845 Fig.141, p1657, p1682-9|Early Devonian|Early Devonian|New name, after Parish of Burridgee. Ungrouped. Included as a dioritic phase of Wologorong Granite by Brunker and Offenberg (1970). Type locality described. Geochemistry detailed; geophysical properties described. Apparent magma mixing and contemporaneous emplacement with Tumboramboro Granite are discussed. Appears as Burridgee Suite in Fig.344.||||Intrudes Abercrombie and Cuddyong Formations and [?] Tumboramboro Granite.|Hard, massive, dark grey to green-grey, mainly equigranular quartz diorite; quartz dolerite dykes and pods, and weakly to strongly deformed tonalite; small intrusions of gabbro, dolerite and diorite.|
42497|Burridgee Diorite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dxb. Ungrouped Devonian intrusion. Includes an unnamed subunit of equigranular, K-feldspar-biotite-hornblende tonalite that is weakly-strongly foliated. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.|||Includes one unnamed sub unit.||Medium grained, massive, generaly weakly foliated, equigranular to sparsely porphyritic quartz diorite, minor fine-grained quartz dolerite and coarse grained, equigranular gabbro.|
42497|Burridgee Diorite|70543|5|Briefly described|Map Legend|Devonian|Devonian|Includes an unnamed subunit of equigranular, K-feldspar-biotite-hornblende tonalite that is weakly-strongly foliated.|||Includes one unnamed sub unit||Medium grained, massive, generaly weakly foliated, equigranular to sparsely porphyritic quartz diorite, minor fine-grained quartz dolerite and coarse grained, equigranular gabbro.|
70239|Burrowa Hills Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Pinkish-grey, medium-grained, massive, equigranular biotite-augite?-ferroan enstatite? granite and biotite-hornblende-quartz -augite-ferroqn enstatite monzonite.||||||
70239|Burrowa Hills Granite|68592|3|Fully described|p1398, p1425-8|Early Devonian|Early Devonian|New unit and name, after Burrowa Hills property. A small elongate body, 1.2 km2, forming low rounded outcrops and tors. Type locality described. No geochemical analysis; attributed to Gooramma Suite on the basis of mineralogy and petrophysics. Geophysical properties described. Age from parent unit. May intrude Hawkins Volcanics.||Unit in Gooramma Suite.||Probably intrudes and is comagmatic with Mountain Creek Volcanics.|Pinkish-grey, medium-grained, masssive, equigranular granitoid varying from granite to quartz monzonite in composition.|
70239|Burrowa Hills Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgb. On Yass and Boorowa 1:100 000 mapsheet portions of Time-Space Plot.||Gooramma Suite|||Medium grained, massive, equigranular granite to quartz monzonite; high magnetic susceptibility.|
70239|Burrowa Hills Granite|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Medium grained, massive, equigranular granite to quartz monzonite; high magnetic susceptibility.|
70239|Burrowa Hills Granite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Medium grained, massive, equigranular granite to quartz monzonite; high magnetic susceptibility.|
39004|Bushmans Volcanics|24417|6|Mentioned|p27|||Now included in the Nash Hill Volcanics.||||||
39004|Bushmans Volcanics|60008|5|Briefly described|Map Legend|Silurian|Silurian|Mafic volcanics.||||||
39004|Bushmans Volcanics|72495|5|Briefly described|p225|Early Silurian|Early Silurian|Occurs east of the Parkes Thrust. Age interpreted from geochemical data and the interpreted interfingering relationship with the Cotton Formation. Spelt both Bushmans and Bushman in same para???||||Interfingers with the Cotton Formation.||30-MAR-20
29507|Bushranger Volcanics|22679|2|Defined|p 33|Early Devonian|Early Devonian|Top most part of the Crudine Group||||||
29507|Bushranger Volcanics|22857|4|Described|p472 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Crudine Group. Dacite, dacitic volcaniclastics, minor andesite. Max. thickness: ~500m. Geological Province: Hill End Trough.||||||07-SEP-09
29507|Bushranger Volcanics|23214|3|Fully described|p197|Lochkovian|Lochkovian|Upper unit of Crudine Group. Previously known as Bushranger Ignimbrite.||||||
29507|Bushranger Volcanics|43653|5|Briefly described|Map Legend||Devonian|||||||
29507|Bushranger Volcanics|43654|5|Briefly described|Map Legend|Devonian|Devonian|Of Crudine Group. Dacite, dacitic volcaniclastics.||||||17-JUL-08
29507|Bushranger Volcanics|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Crudine Group.||||||17-JUN-08
29507|Bushranger Volcanics|50233|4|Described|Map Legend|Pragian|Lochkovian|Of the Crudine Group. Andesite, dacitic volcaniclastics. Overlain by the Cunningham Formation.||||||17-JUN-08
29507|Bushranger Volcanics|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Crudine Group. Porphyritic andesite with phenocrysts of plagioclase, diopsidic augite and orthopyroxene.||||||
29507|Bushranger Volcanics|68592|3|Fully described|p177, p1038, p1041-4, p1054-9|Early Devonian|Early Devonian|Wyborn and Henderson (in Pogson and Watkins, 1998) after Green (1980). Brunker and Offenberg (1970) grouped the southern outcrops of these rocks with Kangaloolah Volcanics. Named after Bushranger Hill, 14km N of Tuena; this is the inferred type section; Wyborn and Henderson (in Pogson and Watkins 1998) first published a description of the Formation and designated a more accessible type section (described). Trunkey Creek Syncline, southern Hill End Trough. Estimated thickness is 860m. Forms a prominent ridge. Geochemistry detailed: remarkable similarity with Forest Lodge Quartz Monzodiorite, 50km away, and Saltpetre Andesite Member (Quialigo Volcanics). Geophysical properties described. Poor age constraint from surrounding units. Hosts auriferous quartz veins.||Unit in Crudine Group.||Is overlain conformably by Cunningham Formation. May correlate with Merrions Formation.|Coarse-grained volcanic rocks including porphyritic andesite, less common basalt; minor rhyodacitic rocks at the S end of the belt; thin interbeds of siltstone and shale.|
29507|Bushranger Volcanics|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dcr. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot. Age max boundary on Time-Space plot is marked with ?-?-?. Related units inferred from Time-Space Plot.||At top of Crudine Group||Is overlain by Cunningham Formation. Overlies, and interfingers with, undifferentiated Crudine Group.|Porphyritic andesite with phenocrysts of plagioclase, diopsidic augite and orthopyroxene; minor olivine-augite basalt.|
29507|Bushranger Volcanics|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
29507|Bushranger Volcanics|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Crudine Group|||Porphyritic andesite with phenocrysts of plagioclase, diopsidic augite and orthopyroxene; minor olivine-augite basalt.|
29507|Bushranger Volcanics|71656|6|Mentioned|p13 Fig.2|Pragian|Pragian|Only shown in correlation chart (Fig.2).||Top of Crudine Group||Overlies Box Ridge Volcanics, overlain by Cunningham Formation.||
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.|
28421|Butmaroo Granite|42726|5|Briefly described|map legend|Early Devonian||Of Butmaroo Suite.||||||29-OCT-13
28421|Butmaroo Granite|69159|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Thurralilly Suite.|||Buff to orange-pink, medium-grained, foliated, equigranular, biotite granite.|
28421|Butmaroo Granite|71069|5|Briefly described|p28, p175, p178, p179, p189|||Intrudes the Ordovician basement of the Goulburn Basin. Some rocks previously assigned to this unit are now incorporated into the Lockhart Igneous Complex. ||||Equivalent to the Lockhart Igneous Complex, Ellenden Granite.|Buff to orange-pink, medium grained, foliated, equigranular, biotite granite.|
28421|Butmaroo Granite|71206|6|Mentioned|p384|||Lachlan Fold Belt.||||||
28421|Butmaroo Granite|71699|5|Briefly described|Map legend.|Silurian|Silurian|||Thurralilly Suite.|||Orange-pink, medium-grained, foliated, equigranular biotite granite.|
28421|Butmaroo Granite|71700|3|Fully described|vi, viii, p7, p17, p45, CD|Late Silurian|Middle Silurian|This unit  has a type locality on the North Black Range Fire Trail at GR 733537 6084027. Joplin et al (1953) mapped this unit as "unnamed granitic rocks" Mapping by Best et al. 1964 group this unit as the Early Devonian Boro Granite which was continued by Felton and Huleatt (1975). Finally the name Butmaroo Granite was introduced by Chappell et al (1991). Geomorphic expression, outcrop, structure, metamorphism, geochemistry, geophysical characteristics and distinguihsing features are discussed. Age is derived from unit relationships and ages for similar members of the Thurralilly Suite. Intrudes Ordovician basement below the southernmost part of the Goulburn basin. See also p52-p53, p77-p78, p81, p83.||Thurralilly Suite||Intrudes the Abercrombie Formation. Equivalent to the Lockhart Igneous Complex, Ellenden Granite and Tallaganda Granodiorite.|Buff to orange-pink, foliated, biotite granite.|
31655|Butmaroo Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
31655|Butmaroo Suite|44093|5|Briefly described|p209 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31655|Butmaroo Suite|71069|6|Mentioned|p174|||Obsolete, replaced by the Thurralilly Suite.||||||
35692|Byawatha Conglomerate Member|61964|5|Briefly described|p14 Fig. 4|Famennian|Famennian|Of Rankin Fm. Rocks were formerly undiff'd, along with Essex Mbr. Thick to v. thick bedded polymictic granule-pebble conglom.to pebbly sst; clast-supported, poorly sorted. Faulted against Square Head Fm. Max. thickness:170m. Also called Byawatha Member||||||
35692|Byawatha Conglomerate Member|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Rankin Formation. Polymictic, medium to thick bedded pebble-granule conglomerate to pebbly sandstone, medium to large scale trough cross beds (clasts: dominantly quartzite, minor black chert).||||||03-NOV-15
35692|Byawatha Conglomerate Member|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Rankin Formation.|||Polymictic, medium- to thick-bedded pebble-granule conglomerate to pebbly sandstone, medium- to large-scale trough cross beds; clasts dominantly quartzite, minor black chert.|
81250|Bygoo Hills sandstone|72083|5|Briefly described|p48, p54|||Trigg (2015, 2016). Informal name. Crops out E of Ardlethan. Has similar lithology to Narrandera Sandstone but lacks a basal conglomerate.||||Probable correlative of Narrandera Sandstone.|Mostly quartz-rich sandstone with mud-galls abundant locally.|
29500|Byng Volcanics|13139|6|Mentioned|p10|||||||||
29500|Byng Volcanics|22679|5|Briefly described|p 23|||||||||18-MAY-16
29500|Byng Volcanics|22857|5|Briefly described|p428 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Basalt, volcaniclastic arenite. Max. thickness: 2000m. Geological Province: Molong Volcanic Arc.||||||
29500|Byng Volcanics|23048|5|Briefly described|p11 table2|Early Silurian|Ordovician|||||||
29500|Byng Volcanics|23213|5|Briefly described|p20|||Conformably overlain by Oakdale Formation at Lucknow.||||||
29500|Byng Volcanics|23214|2|Defined|p63|Late Ordovician|Late Ordovician|Of Cabonne Group. Formerly named Links Andesite Formation. Suggested type section on Icely Road. For lithology description see page 63.||||||
29500|Byng Volcanics|23334|6|Mentioned|10|||||||||
29500|Byng Volcanics|43653|5|Briefly described|Map Legend||Ordovician|||||||
29500|Byng Volcanics|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Basalt, volcaniclastic sandstone.||||||17-JUL-08
29500|Byng Volcanics|43782|5|Briefly described|Map Legend|Eastonian|Eastonian|Of Cabonne Group.||||||17-JUL-08
29500|Byng Volcanics|60424|5|Briefly described|p350 Fig. 1|Ordovician|Ordovician|Geological Province: Hill End Trough.||||||
29500|Byng Volcanics|63278|6|Mentioned|p145 Fig. 1, p147 Fig. 2b, p156|Gisbornian|Gisbornian|Comprises mostly of lavas and pillows. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
29500|Byng Volcanics|63283|5|Briefly described|p188 Tb. 1, p203, p191 Tb. 2|Middle Ordovician|Late Ordovician|Of the Blayney Vocanic, upper. Age: 455Ma (4 samples of basalt). Geological Province: Molong Volcanic Belt. Consists of mafic lavas , cumulates and volcaniclastics (Pogson and Watkins, 1998).||||||07-FEB-11
29500|Byng Volcanics|63284|6|Mentioned|p268|||||||||
29500|Byng Volcanics|63286|5|Briefly described|p294 Fig. 1, p308 Fig. 9|Gisbornian|Darriwilian|Geological Province: Molong Volcanic Belt. Consists of basalt and volcanic sandstone.||||||07-FEB-11
29500|Byng Volcanics|63287|6|Mentioned|p337|||Geological Province: Molong Volcanic Belt. Comprise high-K to shoshonitic lavas.||||||07-FEB-11
29500|Byng Volcanics|63290|5|Briefly described|p389, p393 Tb. 1, p396 Fig. 3|Gisbornian|Gisbornian|Unconformably overlain by Anson Formation and Blayney Volcanics. Geological Province: Molong Volcanic Belt. Shoshonitic.||||||
29500|Byng Volcanics|63293|6|Mentioned|p473, p475|||||||||07-FEB-11
29500|Byng Volcanics|67322|4|Described|p20 Fig.5, p25|Sandbian|Sandbian|Macquarie Arc. The original definition and distribution of the Byng Volcanics (Scott, in Pogson and Watkins 1998), was modified by Crawford, Meffre et al. (2007) who transferred more evolved rocks into the Millthorpe Volcanics. Age is determined from p20 Fig.5 (Strat. column). Occurs in the Blayney region. ||Of the Cabonne Group.||Comagmatic with the upper Blayney Volcanics.|Limited to primitive basalts associated with ultramafic cumulates; has shoshonitic affinities.|21-FEB-18
29500|Byng Volcanics|67847|5|Briefly described|p20, p34|||Macquarie Arc, Lachlan Orogen. |||||Mafic-intermediate volcanics and silciic sediments, including spiculites.|
29500|Byng Volcanics|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
29500|Byng Volcanics|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3).|c. 449-443 Ma|Cabonne Group||||
29500|Byng Volcanics|70684|6|Mentioned|p3, p33||||||||Mostly lavas and pillows.|
29500|Byng Volcanics|72495|6|Mentioned|p235|||Occurs to the south of Orange.||||||
29500|Byng Volcanics|73154|6|Mentioned|p77 Fig.3|Gisbornian|Gisbornian|Macquarie Arc, Phase 4. Molong Volcanic Belt.||upper Blayney Volcanics||||
23449|Byrnes Creek Formation|37986|2|Defined|p309|Ordovician|Ordovician|||||||
23449|Byrnes Creek Formation|40774|6|Mentioned|Fig.2|||||||||
24803|Byrock Leucitite|34449|6|Mentioned|Table 2-1|||Invalid||||||
83664|Byrock Leucitite Suite|73581|5|Briefly described|p26|Miocene|Miocene|Only minor compositional variation. Characterised by large phlogopite crystals of up to 3 mm in length and perovskite-bearing assemblages. Byrock Volcanic Province. The product of an age-progressive hotspot track (Sutherland 1981) named as the CH-C or 'Cosgrove hotspot' (Davies et al.2015).|||||Olivine leucitite lava and scoria cones. Includes xenolith bearing intrusions.|
83285|Cadia Far East monzonite|73154|6|Mentioned|p79|Llandovery|Llandovery|437+/-4 Ma Pb/U zircon SHRIMP age from a Cadia Far East monzonite, considered to be igneous crystallisation Squire and Crawford (2007).|437+/-4 Ma Pb/U zircon|||||
29660|Cadia Hill Monzonite|13139|5|Briefly described|p8|Late Ordovician|Late Ordovician|Age: 439+/-6Ma (SHRIMP U-Pb zircon, Perkins, 1994).||||||
29660|Cadia Hill Monzonite|23090|5|Briefly described|p642, 644|||||||||
29660|Cadia Hill Monzonite|23214|3|Fully described|p92|Late Ordovician|Late Ordovician|Quartz monzonite, intermediate to coarse grained, reddish pink and black in colour, and displays a brecciated texture.||||||
29660|Cadia Hill Monzonite|23334|5|Briefly described|8|Silurian|Ordovician|439+/-6Ma||||||
29660|Cadia Hill Monzonite|43640|5|Briefly described|Map Legend||Ordovician|||||||
29660|Cadia Hill Monzonite|43653|5|Briefly described|Map Legend||Ordovician|||||||
29660|Cadia Hill Monzonite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29660|Cadia Hill Monzonite|63278|5|Briefly described|p156|Early Silurian|Late Ordovician|Of the Cadia Intrusive Complex. Age: 439+/-6Ma (U/Pb SHRIMP). Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
29660|Cadia Hill Monzonite|63292|6|Mentioned|p451|||Lagely porphyritic monzonite stock hosts Cadia Hill deposit.||||||
29660|Cadia Hill Monzonite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
29660|Cadia Hill Monzonite|70684|5|Briefly described|p46|||Hosts the large-tonnage, low-grade Cadia Hill Au-Cu deposit.|||||A large porphyritic monzonite stock.|
29519|Cadiangullong Porphyry|23214|2|Defined|p82|Late Ordovician|Late Ordovician|Intrudes Weemalla Formation. Dark, course grained feldspar-clinopyroxene porphyry with large phenocrysts of strongly sericitised and carbonatised feldspars and carbonatised clinopyroxene.||||||
29519|Cadiangullong Porphyry|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Feldspar porphyry.||||||17-JUL-08
29519|Cadiangullong Porphyry|43782|6|Mentioned|Map Legend|Eastonian|Eastonian|||||||
29519|Cadiangullong Porphyry|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
76945|Cairncross Monzogranite|71628|5|Briefly described|p17: 1-2, 54, 89|||Previously Cairncross Adamellite (Leitch et al., 1982); name altered to align with IUGS nomenclature. Probably named after Mount Cairncross, where the unit forms a ~3 km diameter circular intrusion. Is associated with minor Mo mineralisation (Stony Creek prospect).||Cairncross Suite.||Intrudes Hyndmans Creek and Pappinbarra Formations.|Micromonzogranite (outer rim); quartz-K-feldspar porphyry, monzogranite porphyry, and leucogranite porphyry (core).|
24205|Calamia Member|22857|5|Briefly described|p318 Fig. 22.10A, p548 App.1 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Gatton Sandstone (Marburg Subgroup, Bundamba Group). Siltstone, claystone, lithic-quartz arenite. Max. thickness: 100m. Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|22865|6|Mentioned|Fig.22.10ap318|||||||||
24205|Calamia Member|23799|5|Briefly described|p48|||Of Koukandowie Formation [??].  Geological Province: Clarence-Moreton Basin.||||||28-SEP-05
24205|Calamia Member|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Of Gatton Sandstone.  Geological Province: Clarence-Moreton Basin.  Maximum thickness: 100m.||||||
24205|Calamia Member|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|39907|4|Described|p15|||||||||
24205|Calamia Member|41631|4|Described|p17|||See also Fig.2||||||
24205|Calamia Member|42248|2|Defined|App.1 p414|Early Jurassic||||||||
24205|Calamia Member|42463|6|Mentioned|Fig.3 P170|||||||||
24205|Calamia Member|43736|6|Mentioned|p29|||||||||
24205|Calamia Member|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
24205|Calamia Member|60281|5|Briefly described|p30, Fig.18 App.1|Early Jurassic|Early Jurassic|Of the Gatton Sandstone. Siltstone, claystone, sandstone.  Max. thickness: 100m.  Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60993|5|Briefly described|p6 Fig. 2, p18|||Of the Gatton Sandstone (Marburg Subgroup, Bundamba Group). . Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60995|4|Described|p64, p51 Fig. 3|Early Jurassic|Early Jurassic|Of the Gatton Sandstone. An overbank/floodplain facies of siltstone, claystone, sandstone - identified as a "shale break" in logs and drill cores. Max. thickness: 100m. Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60997|5|Briefly described|p140 Fig. 2|||Of the Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60999|5|Briefly described|p169 Fig. 3|Early Jurassic|Early Jurassic|Basal member of the Gatton Sandstone. Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6, p178 Fig. 10.||||||
24205|Calamia Member|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Gatton Sandstone (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|61006|5|Briefly described|p286|||Of the Gatton Sandstone.  Potential hydrocarbon seal - although it is predominantly siltstone and fine sandstone in some places and therefore will not act as a seal. ||||||
24205|Calamia Member|61310|5|Briefly described|Table C1 (p22-23)||Late Triassic|Of the Gatton Formation. Siltstone, claystone, lithic quartz sandstone. Max. thickness: 100m. Geological Province: Clarence-Moreton Basin||||||
24205|Calamia Member|67402|5|Briefly described|p187, p188, p190 fig CLM6, p190, p193|||Clarence-Moreton Basin. Deposited in a floodplain or braided stream environment. Between 10-20m thick. ||Gatton Sandstone. ||Overlies the Ripley Road Sandstone. Overlain by the Gatton Sandstone.|Shale interbedded with fine-grained sandstone.|
24205|Calamia Member|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 5-500m thick. Potential hydrocarbon seal. ||Gatton Sandstone||Overlies the Ripley Road Sandstone. Overlain by the Koreelah Conglomerate.|Siltstone, claystone and sandstone.|
24205|Calamia Member|69594|5|Briefly described|p544|||Clarence-Moreton Basin (NSW only). Numerous coastal outcrops.||Basal Gatton Sandstone.|||Shale and fine sandstone.|
23454|Calderwood Latite Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
23454|Calderwood Latite Member|22488|5|Briefly described|p840-2|||||||||
23454|Calderwood Latite Member|22857|5|Briefly described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Pheasants Nest Formation (Cumberland Subgroup, Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
23454|Calderwood Latite Member|23544|5|Briefly described|Fig 2 p358|||In the Gerringong Volcanics||||||
23454|Calderwood Latite Member|38690|4|Described|p294|||||||||
23454|Calderwood Latite Member|40270|6|Mentioned|Table 1|||||||||
23454|Calderwood Latite Member|67500|5|Briefly described|p12 Tb.1|||Up to 38m thick.||Of the Pheasants Nest Formation and Gerringong volcanic facies.|||Coarsely porphyritic flow.|01-MAY-12
23454|Calderwood Latite Member|71115|5|Briefly described|p180, 182, 188|Permian|Permian|Southern Sydney Basin.||Gerringong Volcanics (Pheasants Nest Formation).||Overlies Five Islands Latite Member. Is overlain by Minnamurra Latite Member.|Basaltic andesite.|
23454|Calderwood Latite Member|73494|5|Briefly described|p542-543|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanics.|||Shoshonitic basaltic andesite; porphyritic, holocrystalline, dark grey to black.|
28198|Caley Formation|22745|6|Mentioned|p127|||Sydney Basin.||||||
28198|Caley Formation|22857|5|Briefly described|p526 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Narrabeen Group. Claystone, shale, quartz-lithic sandstone. Max. thickness: 46.6m. Geological Province: Sydney Basin.||||||
28198|Caley Formation|23214|5|Briefly described|p269|Triassic|Triassic|Lithic sandstone of the Narrabeen Group.||||||
28198|Caley Formation|23219|5|Briefly described|Map Legend||Permian|||||||
28198|Caley Formation|24079|5|Briefly described|p433 Fig. 6|Triassic|Triassic|Of Narrabeen Group. Geological Province: Sydney Basin.||||||
28198|Caley Formation|24123|5|Briefly described|p3|Triassic|Triassic|Of Narrabeen Group. Geological Province: Sydney Basin.||||||
28198|Caley Formation|29749|6|Mentioned|p12|||||||||
28198|Caley Formation|31061|6|Mentioned|Table 1|||||||||
28198|Caley Formation|31276|6|Mentioned|p147|||Palynology||||||
28198|Caley Formation|31297|6|Mentioned|p6|||||||||
28198|Caley Formation|31373|4|Described|Table 1|||||||||
28198|Caley Formation|31426|6|Mentioned|Fig.1|||||||||
28198|Caley Formation|31725|6|Mentioned|p7|||||||||
28198|Caley Formation|31884|6|Mentioned|Table 1|||Triassic||||||
28198|Caley Formation|31886|6|Mentioned|p394|||Re stratigraphy.||||||
28198|Caley Formation|33683|4|Described|Table 1|||||||||
28198|Caley Formation|33685|5|Briefly described|p396|||||||||
28198|Caley Formation|34009|6|Mentioned|p108|||Permian||||||
28198|Caley Formation|34042|6|Mentioned|p399|||||||||
28198|Caley Formation|34121|4|Described|p397|||||||||
28198|Caley Formation|34205|1|Redefined|p16|Triassic|Triassic|5 members.||||||
28198|Caley Formation|34209|6|Mentioned|p137|||See also P140,141 & Table 1.||||||
28198|Caley Formation|34236|6|Mentioned|p17|||||||||
28198|Caley Formation|34240|4|Described|p395|||Triassic||||||
28198|Caley Formation|34241|6|Mentioned|p404|||||||||
28198|Caley Formation|34336|6|Mentioned|Table 5.15|||||||||
28198|Caley Formation|36042|6|Mentioned|Fig.23|||||||||
28198|Caley Formation|36058|6|Mentioned|p4|||||||||
28198|Caley Formation|37093|5|Briefly described|p231|||||||||
28198|Caley Formation|37804|6|Mentioned|Table 1|||||||||
28198|Caley Formation|39232|6|Mentioned|p110|||||||||
28198|Caley Formation|39287|6|Mentioned|p42|||||||||
28198|Caley Formation|39293|3|Fully described|p141|||Isopach map Fig.8.6||||||
28198|Caley Formation|39306|6|Mentioned|p413|||Flora||||||
28198|Caley Formation|39308|6|Mentioned|p503|||See also Fig.23.12||||||
28198|Caley Formation|40806|6|Mentioned|p150|||||||||
28198|Caley Formation|42925|5|Briefly described|Table 18||Late Permian|||||||
28198|Caley Formation|42926|4|Described|map legend|Early Triassic|Late Permian|||||||
28198|Caley Formation|43146|6|Mentioned|Fig.2 p41|||of Narrabeen Group.||||||
28198|Caley Formation|43194|5|Briefly described|p130|Triassic|Triassic|Fine grained outwash and overbank sediments, western Sydney Basin.||||||
28198|Caley Formation|43317|4|Described|Table 1 p11|||||||||
28198|Caley Formation|43318|14|Not recorded|opp p6||Late Triassic|See also Lexicon||||||
28198|Caley Formation|43320|14|Not recorded|Table 1||Triassic|||||||
28198|Caley Formation|43344|14|Not recorded|p21,53||Triassic|Grose River||||||
28198|Caley Formation|43359|14|Not recorded|Map Legend||Triassic|Provisional first edition||||||
28198|Caley Formation|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Grose Sandstone part of Narrabeen Group||||||
28198|Caley Formation|43361|14|Not recorded|Map Legend||Triassic|(Provisional first edition) Part of Narrabeen Group||||||
28198|Caley Formation|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Narrabeen Group||||||
28198|Caley Formation|43383|14|Not recorded|p22|||||||||
28198|Caley Formation|43385|14|Not recorded|p182 Table||Early Triassic|Ref. to Crook 1957||||||
28198|Caley Formation|43395|2|Defined|p61,62,64,65,69-74||Early Triassic|p76,77||||||
28198|Caley Formation|45090|6|Mentioned|p201|||Refers Crook (1956) Goldbery (1966)||||||
28198|Caley Formation|46849|6|Mentioned|p195|||||||||
28198|Caley Formation|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Narrabeen Group. Geological Province: Sydney Basin||||||
28198|Caley Formation|68003|5|Briefly described|p42.|Triassic|Triassic|Western Sydney Basin. |||||Red, green and grey claystone and siltstone, often intercalated with or overlain by conglomeratic sediments.|
82375|Callaghans Creek Quartz Monzodiorite|71628|4|Described|p7: 1, 15-18, 23, 37-40; p8:105|||Originally Back Creek Complex of Binns et al. (1967) after Flood (1964). Later referred to as Back Creek Tonalite (Flood, 1971). Both names invalid as Back Creek Group had priority. Consequently renamed as Callaghan Creek Tonalite (DMR NAND04 Nandewar Geology Integration and Upgrade project), and again renamed in this study as Callaghans Creek Quartz Monzodiorite to more accurately reflect the geographic feature's name and the composition of the intrusion. Forms a small (3 x 2 km) lobate stock 22 km SE of Bendemeer. Excellent outcrop. This c.245 Ma age is almost certainly too young. Geochemistry described.|244.8 Ma (Rb-Sr biotite: Shaw and Flood, 1993).|Callaghans Creek Suite.||Abuts Walcha Road Monzogranite. Intrudes Sandon Association.|Fine-grained, microporphyritic biotite-hornblende-pyroxene quartz monzodiorite. I-type.|
41168|Calleen Granodiorite|50385|5|Briefly described|Map Legend|Silurian|Silurian|Gneissic, coarse-grained biotite granite||||||23-JUN-04
23458|Calytria Quartzite Member|22857|5|Briefly described|p212, p486 App.1 Tb.A1.7|Devonian|Devonian|Of the Crowl Creek Formation (Mulga Downs Group). Coarse- to medium-grained quartz arenite and quartzite, scarce scattered quartz pebbles. Max. thickness: 52m.||||||10-MAR-06
23458|Calytria Quartzite Member|22859|5|Briefly described|p212|||||||||
23458|Calytria Quartzite Member|40913|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Early Carboniferous-Late Devonian||||||
23458|Calytria Quartzite Member|41126|2|Defined|p137|Early Carboniferous|Givetian|Givetian to Early Carboniferous||||||
23458|Calytria Quartzite Member|73264|6|Mentioned|p1395 Fig.17, p1402 Fig.23|Late Devonian|Middle Devonian|Lachlan Orogen.||Mulga Downs Group||||
33680|Cambalong Metamorphic Complex|22721|6|Mentioned|Fig.1 p502|||||||||
33680|Cambalong Metamorphic Complex|22768|6|Mentioned|p155|||||||||
33680|Cambalong Metamorphic Complex|22815|4|Described|p27, fig13||Early Silurian|||||||
33680|Cambalong Metamorphic Complex|22857|5|Briefly described|p135, p422 App. 1, Tb. A1.5||Ordovician|Metamorphosed Adaminaby Group. Range from lower grade schists to a core of high-grade schists and gneisses. Geological Province: Monaro Forearc Basin.||||||21-APR-10
33680|Cambalong Metamorphic Complex|23245|6|Mentioned|p135|||||||||
33680|Cambalong Metamorphic Complex|24310|5|Briefly described|p1044|||Geological Province: Lachlan Fold Belt||||||
33680|Cambalong Metamorphic Complex|43233|5|Briefly described|Map Legend|Ordovician||||||||
33680|Cambalong Metamorphic Complex|44093|5|Briefly described|p192 App. 1|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
33680|Cambalong Metamorphic Complex|60541|6|Mentioned|p85|||Occurs near Bombala. Considered to be continuous with the Kuark Metamorphic Complex.||||||
33680|Cambalong Metamorphic Complex|60904|5|Briefly described|p794 Fig. 10|||Of the Lachlan Orogen.||||||31-JAN-06
33680|Cambalong Metamorphic Complex|60988|5|Briefly described|p144 Fig.1, p146|Early Ordovician|Early Ordovician|See reference to Cambalong Complex (p147).||||||
33680|Cambalong Metamorphic Complex|61413|6|Mentioned|p2 Fig.1.|||||||||
23460|Cambrai Granite|22638|4|Described|p77||Late Devonian|New name.||||||
23460|Cambrai Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
23460|Cambrai Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
23460|Cambrai Granite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
28197|Camden Haven Group|22616|5|Briefly described|p669, Fig.1 p670|Triassic|Triassic|||||||
28197|Camden Haven Group|22857|5|Briefly described|p269, p538 App.1 Tb.A1.9|Early Triassic|Early Triassic|Correlative of the Narrabeen Group. Max. thickness: 260m. Geological Province: Lorne Basin (New England Fold Belt).||||||
28197|Camden Haven Group|22864|6|Mentioned|p269||Early Triassic|||||||
28197|Camden Haven Group|24083|5|Briefly described|p457|Triassic|Triassic|Geological Province: Lorne Basin.||||||02-JUL-10
28197|Camden Haven Group|31276|6|Mentioned|p141|||Refers Hilby (1970b). Early Triassic||||||
28197|Camden Haven Group|32719|5|Briefly described|p212|||Early Triassic. Re Packham (1969).||||||19-OCT-15
28197|Camden Haven Group|33480|6|Mentioned|p244|||Age dating||||||
28197|Camden Haven Group|34398|6|Mentioned|p270|||Triassic||||||
28197|Camden Haven Group|35647|4|Described|p49|||||||||
28197|Camden Haven Group|36826|4|Described|p89|||||||||
28197|Camden Haven Group|36954|6|Mentioned|p114|||||||||
28197|Camden Haven Group|40134|5|Briefly described|p283|||||||||
28197|Camden Haven Group|40876|6|Mentioned|Fig.3|||||||||
28197|Camden Haven Group|41348|5|Briefly described|Map legend|Triassic|Triassic|Includes: Camden Head Claystone, Grants Head Formation, Jolly Nose Conglomerate and Laurieton Conglomerate.  Red and grey mudstone, lithic sandstone and conglomerate, tuffaceous sandstone, felsic volcanics and minor coal.||||||16-DEC-04
28197|Camden Haven Group|42182|5|Briefly described|p302|||||||||
28197|Camden Haven Group|43384|14|Not recorded|Map Legend||Triassic|||||||
28197|Camden Haven Group|43755|6|Mentioned|Fig.1,p548||Triassic|||||||
28197|Camden Haven Group|44093|5|Briefly described|p236 App. 1|Early Triassic|Early Triassic|Geological Province: New England Fold Belt.||||||
28197|Camden Haven Group|60281|5|Briefly described|p17, Fig. 15 App. 1|Triassic|Triassic|Supersedes the Camden Haven Series.  Includes the Grants Head Formation and Laurieton Conglomerate.  Geological Province: Lorne Basin.||||||17-MAR-05
28197|Camden Haven Group|62058|6|Mentioned|p5, map sheet|Early Triassic|Early Triassic||||Includes Jolly Nose Conglomerate, Laurieton Conglomerate and Grants Head Formation.|||
28197|Camden Haven Group|63119|5|Briefly described|p209|Early Triassic|Early Triassic|Unconformably overlies the Watonga Formation.||||||
28197|Camden Haven Group|63763|5|Briefly described|p4-5 Fig. 1|Early Triassic|Eary Triassic|||||||
28197|Camden Haven Group|65940|6|Mentioned|p194|||Wauchope-Port Macquarie area, NSW.||||||
28197|Camden Haven Group|66090|4|Described|pp1-2, p4, pp11-28, p32.|Early Triassic|Early Triassic|Formerly Camden Haven Series (Voisey 1939); stratigraphy formalised in Camden Haven Group by Packham (1969); reappraised by Pratt and Herbert (1973); further amended by Leitch and Bocking (1980). Folding and faulting of this group indicated that significant deformation, mainly from movement on basement faults, occurred in the eastern New England Orogen following the Late Permian orogenic climax.|||Includes Grants Head Formation, Coorabakh and Laurieton Conglomerates and Camden Head Claystone.|||19-OCT-15
28197|Camden Haven Group|71628|5|Briefly described|p17: 73-75, 78, 80, 84, 86|Early Triassic|Early Triassic|Lorne Basin.|||Camden Haven Claystone.|Is intruded by Hannam Vale, Middle Brother, North Brother and Juhle Mountain Granodiorites, and South Brother Microgranite.|Includes carbonaceous shales.|
24208|Camp Hill Sandstone Member|22857|4|Described|p462 App.1 Tb.A1.6|Silurian|Silurian|Of the Canberra Formation. Well-bedded arenite and siltstone; thin shale partings; thin beds of coarse-grained quartz arenite at the base. Max. thickness: 100m.||||||
24208|Camp Hill Sandstone Member|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24208|Camp Hill Sandstone Member|37728|4|Described|Table 2|||||||||
24208|Camp Hill Sandstone Member|39947|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24208|Camp Hill Sandstone Member|41356|6|Mentioned|p32|||||||||
24208|Camp Hill Sandstone Member|42727|5|Briefly described|map legend|Wenlock|Wenlock|Of Canberra Formation. Sandstone and siltstone. Unconformably overlies Murrumbateman Creek and Black Mountain Sandstone BMR map symbol: Smc1. Geol. Prov: Canberra Block.||||||
24208|Camp Hill Sandstone Member|42820|2|Defined|p19|Early Silurian||of Canberra Formation. Age not younger than late Wenlock.||||||
24208|Camp Hill Sandstone Member|49043|5|Briefly described|p7|||||||||
24208|Camp Hill Sandstone Member|68592|6|Mentioned|p16|Wenlock|Llandovery|||Basal unit in Canberra Formation.||Unconformably overlies State Circle Shale.||
24208|Camp Hill Sandstone Member|73211|6|Mentioned|p909|lower Silurian|lower Silurian|Maximum thickness: ~100 m.||Canberra Formation||Unconformably underlain by State Circle Shale.|Thinly bedded sandstone.|
82376|Campbells Hill Monzogranite Phase|71628|5|Briefly described|p7: 38-39, 41-42, 44, 49-51|||Originally Campbells Hill Adamellite of Chesnut et al. (1973) after unpublished work by Flood (1971). Subsequently renamed Campbells Hill Monzogranite by Brown (2003) after unpublished work by Chappell and Bryant (1994). In this study it becomes Campbells Hill Monzogranite Phase (of Walcha Road Monzogranite). Named after a local geographical feature. Located ~20km NNE of Bendemeer and ~20km SW of Uralla. Forms a plateau c.60m higher than the surrounding parent body. Geochemistry briefly described.||Walcha Road Monzogranite.||Is entirely surrounded by the parent unit.|Light grey, medium-grained, texturally heterogeneous, weakly porphyritic, felsic biotite plagioclase-rich monzogranite to granodiorite, characterised by sparse K-feldspar megacrysts and rare hornblende.|
67904|Campfire Monzogranite|71628|4|Described|p3: 1, 4, 25-27, 62-64|||Chappell and Bryant (1994). Previously the Campfire Adamellite (Pogson and Hitchins, 1973), but the rocks had been included in the Kilburnie Monzogranite (eg Binns et al., 1967). Named after a local homestead. Crops out ~45 km ESE of Tamworth and ~25 km SW of Walcha. No geochemistry available. Au mineralisation in quartz veins occurs to the W of the intrusion; unlikely to be genetically related.||Campfire Suite.||Intrudes Sandon Association. Abuts (?intrudes) Kilburnie Monzogranite.|Medium- to coarse-grained, biotite syenogranite-monzogranite; locally amphibole-bearing. Considerably altered. S-type.|
23463|Cana Creek Tuff Member|24603|5|Briefly described|p868|||Of the Currabubula Formation.  Relatively coarse-grained, crystal-rich, lithic, variably welded ignimbrite.   Geological Province: Tamworth Belt.||||||
23463|Cana Creek Tuff Member|39572|6|Mentioned|Fig.2|||||||||
23463|Cana Creek Tuff Member|41800|4|Described|p493|||||||||
23463|Cana Creek Tuff Member|43718|6|Mentioned|Table 8.2,p129|||||||||
23463|Cana Creek Tuff Member|50613|6|Mentioned|p219|||||||||
23463|Cana Creek Tuff Member|62095|1|Redefined|p272 Appdx., p251, p256|Late Carboniferous|Late Carboniferous|Of the Currabubula Formation. Synonymous with Cana Creek Tuff Member of McPhie (1983) and Opdyke et al (2000). Underlies White Rocks Ignimbrite Member. Age: >319Ma. Thickness: 85m in type section. Geol.Prov: Werrie block/Tamworth Belt. See also Plate 1.||||||25-MAY-06
23463|Cana Creek Tuff Member|65902|5|Briefly described|p195 Fig.2, p200 Fig.5, p201-2, p204|Bashkirian|Bashkirian|Of Currabubula Formation. Rhyolitic ignimbrite. Shown as Cana Creek Tuff p201, 202, Fig. 6, Fig. 7, p204.||||||
30477|Candelo Suite|22815|5|Briefly described|p71,72|||Consists of 2 members.||||||
30477|Candelo Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Candelo Supersuite.  Includes the Candelo and Yurammie Granites (informal names).||||||09-FEB-05
30477|Candelo Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
30477|Candelo Suite|71069|5|Briefly described|p9, p26 fig 9, p42, p43, p179|Early Devonian|Early Devonian||||||Granites.|
73521|Cannela Formation|66623|1|Redefined|pp74-75. |Middle Cambrian|Middle Cambrian|Redefined; formerly portion of Wonominta beds (Warris 1967); referred to as Cannela beds by Mills (2003). Comprises the Gorge Inlier, c. 14 km2 where thickness is c. 2km. Possible radiolarian fossils. Tuffs from Mount Wright Volcanic Arc activity; similar age to Noonthorangee Formation tuffs.|508.3 +/- 2.2 (Black 2006).|Unit in Ponto Group.||Overlies Grasmere Formation. Is overlain by Noonthorangee Formation.|Phyllite, felsic and vitric tuffs and tuffaceous mudstones; minor metasandstone.|
73521|Cannela Formation|66922|5|Briefly described|Map legend|Cambrian|Cambrian|The two components are mapped separately.||Unit in Ponto Group.|||Foliated phyllite, muddy sandstone and quartzose sandstone intercalated with felsic and vitric tuff units (30% of the section); cream, massive to finely-laminated tuffaceous mudstone up to 1 m thick, regionally metamorphosed to greenschist facies.|
73521|Cannela Formation|67207|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Ponto Group.|||Quartzose turbiditic metasediments consisting of foliated metamorphosed mudstone (phyllite), muddy sandstone and quartzose sandstone intercalated with felsic and vitric tuff units that make up about 30% of the section.|
73521|Cannela Formation|67322|5|Briefly described|p11; Fig.5|Cambrian|Cambrian|Confined to the Gorge Inlier at the northern extremity of the Koonenberry Belt. Age determined from p20 Fig.5 (Strat. column) - not well constrained. Occurs in the Kayrunnera-Koonenberry region.||Of the Ponto Group.||Correlative of Noonthorangee Formation.||21-FEB-18
73521|Cannela Formation|69001|6|Mentioned|p2 Fig.1B|Cambrian|Cambrian|||Of the Ponto Group.||||
79862|Canobolas Volcanics|67821|6|Mentioned|p150|||Age given as Tertiary.||||||
73680|Canonbar Igneous Complex|63278|6|Mentioned|p148|||||||||07-FEB-11
73680|Canonbar Igneous Complex|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
73680|Canonbar Igneous Complex|72495|5|Briefly described|p217-219, p226, p234-235, 236, 239|Ordovician|Ordovician|Coincides with a linear north-northwest-trending gravity high in the Junee-Narromine volcanic belt and is the northernmost complex in the belt. Underlies Carboniferous Tullamore Syncline. Only defined in the geophysics from potential field data. It is interpreted that geological bodies further north in Queensland that were once mapped as belonging to this unit are instead Early Devonian igneous units rather than Canonbar Igneous Complex. Described as Canonbar Complex p239.||||Intruded by Silurian Nyngan Intrusive Complex.||30-MAR-20
29527|Canowindra Volcanics|13139|5|Briefly described|p9 Fig. 4, p11|Silurian|Silurian|S-type volcanics. Geological Province: Cowra Trough.||||||17-JUL-08
29527|Canowindra Volcanics|22503|5|Briefly described|p648, Fig.6 p649||Late Silurian|||||||
29527|Canowindra Volcanics|22857|5|Briefly described|p456 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Cudal Group. Garnetiferous quartz-feldspar-cordierite porphyritic lava, tuff, ashtone, ignimbrite. Interfingers with one horizon of Hanover Formation. Max. thickness: 700m. Geological Province: Cowra Trough.||||||10-MAR-06
29527|Canowindra Volcanics|23043|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Cudal Group.||||||17-JUL-08
29527|Canowindra Volcanics|23170|2|Defined|p101|Wenlock||Of Cudal Group. Supersedes 'Canowindra Porphyry'.||||||01-OCT-09
29527|Canowindra Volcanics|23214|2|Defined|p116|Wenlock|Wenlock|Of Cudal Group. Originally named Canowindra Porphyry. Max. thickness 1000m||||||
29527|Canowindra Volcanics|23309|5|Briefly described|p383, 384, 390, 392.||Silurian|||||||
29527|Canowindra Volcanics|23334|5|Briefly described|9 Fig.4|Silurian|Silurian|||||||
29527|Canowindra Volcanics|23454|5|Briefly described|p32|Silurian|Ordovician|432+/-7Ma||||||
29527|Canowindra Volcanics|23549|6|Mentioned|p522|||Contain abundant garnets.  Geological Province: Lachlan Fold Belt.||||||05-APR-05
29527|Canowindra Volcanics|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
29527|Canowindra Volcanics|24417|6|Mentioned|p45|||Of Cudal Group.||||||
29527|Canowindra Volcanics|43158|4|Described|5|||||||||
29527|Canowindra Volcanics|43494|4|Described|p16, p18|Silurian|Silurian|Supersedes Canowindra Porphyry. Coarse porphyritic dacite. Overlie Kabadah Fm; conformable beneath Cary Fm. in E. and Hanover Fm. in W. Also unconformably overlain by Dulladerry Volcanics and intruded by Yeoval Batholith.  Age is Late Wenlockian.||||||17-JUL-08
29527|Canowindra Volcanics|43640|5|Briefly described|Map Legend||Silurian|||||||
29527|Canowindra Volcanics|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of garnetiferous quartz feldspar cordierite porphyry, ashstone, mass flow deposits.||||||17-JUL-08
29527|Canowindra Volcanics|43782|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Cudal Group.||||||17-JUL-08
29527|Canowindra Volcanics|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Cudal Group. Garnetiferous quartz feldspar cordierite porphyry, ashstone.||||||19-JUL-04
29527|Canowindra Volcanics|60987|6|Mentioned|p155, |Wenlock|Wenlock|||||||
29527|Canowindra Volcanics|63277|5|Briefly described|p139|Early Silurian|Early Silurian|S-type volcanics, garnet-bearing felsic ignimbrites. Geological Province: Lachlan Fold Belt.||||||
29527|Canowindra Volcanics|63286|6|Mentioned|p300|Early Silurian|Early Silurian|Age: ca 428-425Ma (microfossils), and 437+/-7Ma (U-Pb SHRIMP: Pogson and Watkins 1998). Contains Wenlockian are microfossils (Lawrie et al. 1998) and rhyolitic lavas.||||||07-FEB-11
29527|Canowindra Volcanics|63287|5|Briefly described|p317 Fig. 2, p335|Wenlock|Wenlock|Of the Cudal Group. Overlain by Avoca Valley Shale, underlain by Gospal Oak Shale. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29527|Canowindra Volcanics|63288|5|Briefly described|p354 Fig. 1, p359, p361|Early Wenlockian|Llandovery|Age: ca 428Ma, 432+/-7Ma (Pogson and Watkins, 1998. SHRIMP). Subaerial to shallow-water depositional environment.||||||
29527|Canowindra Volcanics|63290|5|Briefly described|p405, p409, p406 Fig. 7|Wenlock|Llandovery|Intruded by Cowra Granodiorite. Age: 432+/-7Ma (U/Pb SHRIMP) or ca 430Ma (based on graptolite control of underlying and overlying units. Geological Province: Molong Volcanic Belt.||||||
29527|Canowindra Volcanics|64994|5|Briefly described|p1, p7, Fig. 1 (between p8-9)|Wenlock|Wenlock|Conformably underlain by Gospel Oak Shale. Age: ~432Ma (SHRIMP U-Pb zircon); also, 431.7+/-3.1Ma (SHRIMP U-Pb zircon: Black 2006). Geological province: Lachlan Orogen.||||||07-FEB-11
29527|Canowindra Volcanics|66197|5|Briefly described|p632, p633 Fig.4c|Llandovery|Llandovery|Cowra Trough-Molong High. Age: 431.7 +/- 3.1 Ma.||||Underlies the Hanover and Cary Formations; overlies the Kabadah Formation.|S-type subaerial to shallow marine volcanics.|14-MAR-12
29527|Canowindra Volcanics|67847|5|Briefly described|p19, p32-p33|Llandovery|Llandovery|S-type geochemistry. (U-Pb zircon ages from Pogson and Percival, 2003). |432 +/- 7 Ma, 431.7 +/- 3.1 Ma|||Conformably overlies the Gospel Oak Shale. Disconformably overlain by the Avoca Valley Shale.||
29527|Canowindra Volcanics|68003|5|Briefly described|p24 Fig.3-e, p145. |Wenlock|Llandovery|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Basal unit in Cudal Group.|||Garnetiferous quartz-feldspar-cordierite porphyry, tuff.|
29527|Canowindra Volcanics|68310|6|Mentioned|p236-238|||Likely the extrusive equivalent of Cowra Granodiorite.|||||Cordierite- and garnet-bearing volcanic rocks.|
29527|Canowindra Volcanics|68592|5|Briefly described|p23, p428, p442, p457, p466, p1229|Early Silurian|Early Silurian|Rocks in the Bathurst 1:250 000 map, equivalent to the Douro Group, have been mapped as this unit by Pogson and Watkins (1998) after Stevens (1950, 1954). Thought to be comagmatic with Cowra Suite.|431.7 +/- 3.1 Ma SHRIMP U-Pb zircon; Black (2006)|Unit in Cudal Group.||Is intruded by Cowra Granodiorite. Stratigraphic equivalent to Hawkins and Glen Isla Volcanics.||
29527|Canowindra Volcanics|70210|5|Briefly described|p2, p32, p36, p39-41|Llandovery|Llandovery|Yass-Goulburn district. A similar, weighted mean age of 432.2 +/- 3.4 Ma is also given. Field relationships show this unit is older than the Laidlaw Volcanics, despite their age determinations in this Report.|431.7 +/- 3.1 Ma.|||Correlated with Hawkins Volcanics.||
29527|Canowindra Volcanics|70296|6|Mentioned|p19|||||||||
29527|Canowindra Volcanics|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group|||Two major felsic to intermediate volcaniclastic and pyroclastic units (Canowindra Volcanics and Nargong Volcanics).|
29527|Canowindra Volcanics|70684|6|Mentioned|p39 Fig.17|Early Silurian|Early Silurian|Molong Volcanic Belt.||||||
29527|Canowindra Volcanics|71600|6|Mentioned|p23 Fig 1|Silurian|Silurian|Geological province: Lachlan Fold Belt.||Unit of Cudal Group.||||
29527|Canowindra Volcanics|73215|6|Mentioned|p993|||||||||
29527|Canowindra Volcanics|73299|6|Mentioned|p1105|||Cowra Trough. [Map symbol suggests Silurian age]||||||
29527|Canowindra Volcanics|73431|6|Mentioned|p363 Fig.1, p365, p367 Tb.1, p372, p374|Silurian|Silurian|Lachlan Orogen. Coeval with Davies Creek Granite, parts of Browns Creek Igneous Complex. Previous U/Pb (SHRIMP) zircon age of 432.0+/-5.0 Ma with inherited cores of 495-1011 Ma detected (Atton, 2013). Contains abundant zircon xenocrysts. Location in text includes p368.|432.0+/-5.0 Ma zircon U/Pb SHRIMP||||Volcanic unit.|
83660|Caoura Basalt|73581|6|Mentioned|p23|Oligocene|Oligocene|List of K-Ar ages provided from Nott et al. (1996) and Wellman and McDougall (1974b). See also Caoura basalt p22.|31.2 Ma, 30.8 Ma, 28.7 Ma, 31.2 Ma K-Ar|||||
30309|Captain Rocks Formation|24008|5|Briefly described|p355|Middle Devonian|Early Devonian|||||||
30309|Captain Rocks Formation|61730|5|Briefly described|p1004|Middle Devonian|Middle Devonian|Geological Province: New England Orogen.||||||
30309|Captain Rocks Formation|68008|6|Mentioned|p16|Middle Devonian|Middle Devonian|Southern New England Orogen. Almost identical geochemistry to a sample of Craigilee beds.||||||
30309|Captain Rocks Formation|73440|6|Mentioned|p129-130, p132|Middle Devonian|Middle Devonian|[Also written as Captains Rocks Formation, p129]. Gamilaroi terrain.||||Overlain by Curricabark Formation.|Coarse-grained volcaniclastic rocks.|
28435|Cara Formation|721|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Low-grade, regionally metamorphosed, multiply deformed, siliceous siltstone, chert, and mudstone, minor metabasalt, volcaniclastic sandstone and pebble conglomerate.||||||29-JUL-14
28435|Cara Formation|22857|5|Briefly described|p220, p502 App.1 Tb.A1.7|Carboniferous||||||||
28435|Cara Formation|22859|5|Briefly described|p220|||||||||
28435|Cara Formation|23050|4|Described|p15 Table 1|Early Carboniferous|Late Devonian|Age: Famennian to Early Carboniferous based on radiolaria||||||29-JUL-14
28435|Cara Formation|23051|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
28435|Cara Formation|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Central Block||||||
28435|Cara Formation|24366|5|Briefly described|p7, 17 Fig. 3|Early Carboniferous|Late Devonian|||||||
28435|Cara Formation|41328|2|Defined|p10|Tournaisian|Famennian|||||||
28435|Cara Formation|41329|6|Mentioned|p6|||||||||
28435|Cara Formation|42554|5|Briefly described|p45|||||||||
28435|Cara Formation|42629|5|Briefly described|p359|||||||||
28435|Cara Formation|42748|6|Mentioned|Fig.3 P9|Carboniferous||||||||
28435|Cara Formation|43091|5|Briefly described|Map legend|||||||||
28435|Cara Formation|43582|6|Mentioned|p4|||||||||
28435|Cara Formation|62757|5|Briefly described|p3 Fig. 1|Early Carboniferous|Early Carboniferous|||||||07-FEB-11
28435|Cara Formation|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Cambrian|In Central Block and Woodsreef Melange.||||||31-MAY-07
28435|Cara Formation|65398|5|Briefly described|p4 Fig.2, p6-8 Fig.3|Early Carboniferous|Late Silurian|Low-grade regionally metamorphosed, multiply deformed massive and rhythmically-bedded siliceous argillite, chert, wacke, diamictite and rare basalt. Age from radiolaria and conodonts. Low-energy, deep water environment with periodic mass-flow deposits to the depocentre. Overlies Wandsworth Volcanic Group.||||||
28435|Cara Formation|66720|5|Briefly described|Map legend|Early Carboniferous|Late Silurian||||Includes two un-named members: ribbon-bedded argillite facies with rare basalt and chert; and massive argillite and diamictite facies, with pebbly argillite and chert.||Undifferentiated argillite, chert, wacke, diamictite and basalt.|
28435|Cara Formation|68003|5|Briefly described|p31, p32 Fig.3-h, p140.|?Early Carboniferous|Late Devonian|Central Block, New England Fold Belt.||||Is overlain by Whitlow Formation.|Low grade regionally metamorphosed, multiply deformed siliceous and tuffaceous thinly-bedded argillite, chert, volcaniclastic wacke, pebble conglomerate and rare basalt.|
28435|Cara Formation|68005|5|Briefly described|p18, p22, pp30-31, pp155-156, p170.|Early Carboniferous|Late Devonian|Anaiwan terrane, Central Block, New England Fold Belt. Deep marine deposition; locally highly deformed/intensely faulted; part of subduction complex. Has a distinctive heterogeneous, low to moderate radiometric response reflecting its lithologies. A distinct magnetic halo to 4 km surrounds the Bundarra Supersuite intrusion.||||Unconformably overlies, and is faulted against, Woolomin Group and Wisemans Arm Formation. Is intruded by Bundarra Supersuite. Is unconformably overlain by Whitlow Formation.|Mainly fine-grained, siliceous, commonly tuffaceous argillites, thinly bedded to massive, commonly containing radiolaria; subordinate metabasalt, chert, volcaniclastic sandstone and pebble conglomerate.|
28435|Cara Formation|68006|5|Briefly described|p20 Fig.3-A, p25, p115.|Early Carboniferous|Late Devonian|Central Block, New England Fold Belt. Deposited in a deep marine setting; forms part of a subduction complex. Hosts small, discontinuous limestone lenses of dubious economic importance.||||Unconformably overlies, and is faulted against, Woolomin Group and Wisemans Arm Formation. Is overlain unconformably by Whitlow Formation.||
28435|Cara Formation|70036|5|Briefly described|Map legend|||Central Block, New England Fold Belt. Included in a mapped unit of Silurian to Carboniferous strongly deformed, andesitic to rhyolitic metasedimentary rocks, lithic sandstone, argillite, chert and jasper.||||||
28435|Cara Formation|71628|5|Briefly described|p4: 9, 15, 17, 24, 29, 40, 45; p7: 5|||See also p7: 31-32; p19-27.||||Is intruded by Dumboy-Gragin Leucosyenogranite; Attunga Creek, Banalasta, Namoi Tops, Moonbi and Copeton Monzogranites.|Tuffaceous chert, siltstone, mudstone, sandstone and conglomerate.|
31544|Caragabal Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31544|Caragabal Suite|44093|5|Briefly described|p181 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31459|Carawandool Volcanics|22466|4|Described|P9, Fig8 P8||Early Devonian|Age of unit is 403.8+/-2.1 Ma||||||
31459|Carawandool Volcanics|24007|6|Mentioned|p325 Fig.2|||||||||
31459|Carawandool Volcanics|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
31459|Carawandool Volcanics|24417|3|Fully described|p82|Early Devonian|Early Devonian|Of Trundle Gp.  Previously mapped as unnamed Devonian volcanic rocks (Brunker, 1972) and as the southern continuation of "Milpose Volcanics" (Bowman, 1976).  Includes four mapped but unnamed units.  Overlain by Cloghan Shale; underlain by Pullabooka Fm.||||||
31459|Carawandool Volcanics|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Trundle Group.  Overlies: Pullabooka Formation.  Underlies: undifferentiated rocks of Hervey Group.  Interfingers/interbedded with: Kadungle Volcanics.||||||09-JUN-04
31459|Carawandool Volcanics|60008|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Sediments and/or volcanics.||||||08-JUL-04
31459|Carawandool Volcanics|60009|5|Briefly described|Map Legend|Pragian|Pragian|Of the Trundle Group. Overlies: Pullabooka Formation.||||||13-JUL-04
31459|Carawandool Volcanics|60548|5|Briefly described|map legend|Devonian|Devonian|Of Trundle Group.||||||
31459|Carawandool Volcanics|63290|6|Mentioned|p406 Fig. 7|||||||||
31459|Carawandool Volcanics|66197|5|Briefly described|p635 Fig.5b|Emsian|Emsian|Silicic volcanics and volcaniclastics. Jemalong Trough. Overlies the Pullabooka Formation. Age: 403.8 +/- 2.1 Ma.||||||13-MAR-12
31459|Carawandool Volcanics|71040|4|Described|p8 Fig.5, p13, p15-17, p31|Early Devonian|Early Devonian|The youngest unit in the Currowong Syncline to be folded by the Tabberabberan Orogeny; previously a N-trending rift. Folding is tightly dated at c.400 Ma.|404 +/- 2 Ma; Lyons et al. (2000).|Trundle Group.||Is overlain unconformably by the Hervey Group.|Andesite, sandstone.|
40934|Cardinal View Formation|50234|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Includes: Lookdown Limestone Member. Of the Bungonia Group.  Underlies: Frome Hill Formation.||||||
40934|Cardinal View Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Bungonia Group. Shale, siltstone and sandstone. Numerous mass flow deposits up to 4cm thick, consist of shale, sandstone and limestone clasts (up to 1m).||||||09-SEP-08
40934|Cardinal View Formation|67820|6|Mentioned|p136 Fig.3|Late Silurian|Late Silurian|||Bungonia Group.||||
40934|Cardinal View Formation|68592|2|Defined|p898-900, p904-13, p1891-2|Ludlow|Ludlow|Originally named Cardinal View Shale by James et al. (1978); more formally described by Bauer (1994). Mapped by Carr et al. (1979) as 'lower shale' within Bungonia Limestone. Here renamed cardinal View Formation to reflect its variety of lithologies. Type locality described. 170-400m thick. Early to late Ludlow.||Unit in Bungonia Group.|Includes Lookdown Limestone Member.|Overlies Adaminaby Group unconformably or with faulted contact. Is overlain by Frome Hill Formation or Tangerang Formation. Equivalent to Kerrawary Siltstone and Black Bog Shale.|Basal fossiliferous, biostromal limestone; overlain by a coarsening-upward, graded, siliciclastic sequence of siltstone, shale and sandstone.|
40934|Cardinal View Formation|69159|5|Briefly described|Map legend|Late Silurian|Early Silurian|||Unit in Bungonia Group.|||Quartz-mica siltstone, mudstone, rhyolitic crystal-vitric tuff; fine-to medium-grained sandstone, locally coarse-grained, conglomeratic and/or calcareous; minor allochthonous pods of fossiliferous limestone, variably recrystallised.|07-SEP-15
40934|Cardinal View Formation|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sbc. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Bungonia Group|Includes Lookdown Limestone Member.|Is overlain by Frome Hill Formation.|Medium grained, well-poorly sorted, massive quartz rich sandstone interbedded with commonly graded siltstone and siliceous mudstone, minor conglomerate and breccia with cobbles of shale and limestone; fossil fragments present.|
40934|Cardinal View Formation|70542|5|Briefly described|Map Legend|Silurian|Silurian|||Bungonia Group|Includes Lookdown Limestone Member||Medium grained, well-poorly sorted, massive quartz rich sandstone interbedded with commonly graded siltstone and siliceous mudstone, minor conglomerate and breccia with cobbles of shale and limestone; fossil fragments present.|
40934|Cardinal View Formation|70661|3|Fully described|p31 tbl 1, p33, p37, p39-p42|Ludlow|Ludlow|Name derived from Cardinal View lookout. Originally called Cardinal View Shale, also referred to as lower shale (Carr 1981), Maximum 400m thickness. Age constrained from underlying and overlying units. Deposited in high energy near shore environment changing to outer shelf deposition over time. Structure, metamorphism, fossil assemblage and geophysical characteristics described.||Bungonia Group|Main Gully limestone|Conformably overlies Lookdown Limestone Member, faulted over Adaminaby Group, overlain by Folly Point Limestone Member, Frome Hill Formation, Tangerang Formation|Shale, siltstone, fine grained sandstone with graded bedding and ripple marks, conglomerate and minor limestone. Mass flow deposits containing clasts of sandstone, shale and limestone also present.|
40934|Cardinal View Formation|71303|5|Briefly described|map legend|Ludlow|Ludlow|||Of Bungonia Group.|||Shale, siltstone and fine-grained sandstone with graded bedding and cross-laminations. 'Mass-flow' units to 4 m thick, with sandstone, shale and limestone clasts. Limestone locally.|
40934|Cardinal View Formation|71656|4|Described|p13 Fig.2, p31|Ludlow|Ludlow|Includes Lookdown Limestone Member.||Bungonia Group|Includes Lookdown Limestone Member.|Partially equivalent to Wombeyan Limestone. Overlain by Frome Hill Formation.|Includes fossiliferous limestone, shale.|
40934|Cardinal View Formation|71699|5|Briefly described|Map legend.|Silurian|Silurian|Lithology continued: The sandstone is locally coarse-grained, conglomeratic or calcareous; minor allochthonous pods of fossiliferous limestone (separately mapped).||Bungonia Group.|||Buff to cream, thinly-bedded to laminated, quartz-mica siltstone, mudstone, rhyolitic crystal-vitric tuff, and fine- to medium-grained sandstone, with sporadic thin beds of matrix-rich, medium-grained, quartzose to quartzofeldspathic sandstone.|
40934|Cardinal View Formation|71700|2|Defined|vi, ix, p7, p10, p15-p16, p25|Late Silurian|Middle Silurian|Named for the Cardinal View lookout at GR 227100 6145300. The type locality for this unit is Frome Hill (GR 227030 6146100; MGA Zone 56). A representatitve section is proposed at GR 758961 6122098 and GR 758846 6122107. Rocks now assigned to this unit were previously mapped as De Drack Formation. Distribution, geomorphic expression, outcrop, structure, metamorphism, geophysical characteristics, fossils, distinguishing features and economic geology are discussed.Thickness is estimated by varying authors to be between 170 to 500m thick. Lithology is described in detail at two localities. The southern and southwestern parts of this unit outcrops in Braidwood 1:100k map sheet. Hosts skarn mineralisation at Mayfield, Limekilns, Ennisclare and Glenrossal. Interpreted as a marine shelf and slope sequence.  See also p43, p57, p82, p107-p108, p110, p112, p124, CD.||Bungonia Group|Includes the Sawtooth Ridge Limestone Member, Efflux Siltstone Member and Folly Point Limestone Member.|Unconformably overlain by the Larbert Conglomerate. Intruded by the Braidwood Granodiorite. Overlies or interfingers with the Lookdown Limestone. Overlain by the Frome Hill Formation.|Siltstone, mudstone, polymictic conglomerate, lithic quartz sandstone; locally calcareous.|
33857|Cargelligo Formation|22508|6|Mentioned|p3||Early Devonian|Supersedes Cargelligo Group. Part of Rast Group.||||||
33857|Cargelligo Formation|22857|4|Described|p438 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Rast Group (Cobar Supergroup). Sandstone, siltstone and cleaved slate. Geological Province: Rast Trough (Darling Basin).||||||
33398|Carlachy Sandstone Member|24417|3|Fully described|p147|Late Devonian|Late Devonian|Of Weddin Sandstone.  Formerly included in "Bogan Gate Sandstone" and "Troffs Formation".  Essentially a large wedge or lens within the Cloghnan Shale.  Max. thickness: 350m.||||||
33398|Carlachy Sandstone Member|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Weddin Sandstone (Hervey Group).||||||
33398|Carlachy Sandstone Member|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Weddin Sandstone (Hervey Group). Underlies: Cudgelbar Sandstone Member.  Overlies: Cloghnan Shale.||||||13-JUL-04
25834|Carlton Formation|22857|5|Briefly described|p490 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Canangle Subgroup (Catombal Group). Massive oligomictic conglomerate. Max. thickness: 60m. Geological Province: Hervey Basin.||||||
25834|Carlton Formation|23214|3|Fully described|p238|Late Devonian|Late Devonian|Of Canangle Subgroup. Formerly named Carlton Conlgomerate. Geological Province: Lambie Basin. Underlying unit: Edinboro Formation, Overlying unit: Waree Creek Formation. Max. thickness: 120m.||||||15-JUL-08
25834|Carlton Formation|32151|2|Defined|p213|Early Carboniferous|Early Carboniferous|Not variation on Carlton Fm WA.See also Carlton Conglomerate, NSW. [CEBMar95]||||||
25834|Carlton Formation|43640|5|Briefly described|Map Legend||Devonian|||||||
25834|Carlton Formation|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Catombal Group. Consists of massive red-brown conglomerate, green and brown pebbly sandstone and siltstone.||||||15-JUL-08
25834|Carlton Formation|43782|6|Mentioned|map diagram|Famennian|Famennian|Of Canangle Subgroup, Catombal Group.||||||15-JUL-08
23470|Carlwood granite|36600|6|Mentioned|Table 1|||||||||
23473|Carne Dacite Member|22678|4|Described|p711,714,721-22|||Of the Tangerang Formation.||||||17-JAN-06
23473|Carne Dacite Member|22857|5|Briefly described|ERRATA sheet for p482|||Of the Tangerang Formation. ||||||
23473|Carne Dacite Member|39568|2|Defined|p82|Early Devonian|Early Devonian|||||||
23473|Carne Dacite Member|42210|6|Mentioned|Fig.1 P273|||||||||
23473|Carne Dacite Member|50234|5|Briefly described|Map Legend|Pragian|Pragian|Of the Tangerang Formation (Bindook Volcanic Complex).  Underlies Joaramin Ignimbrite||||||16-JUN-08
23473|Carne Dacite Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tangerang Fm (Bindook Gp). Small, greenish-grey, massive to rarely flow banded and autobrecciated, medium-grained, porphyritic intrusive dacite bodies at various stratigraphic levels within the formation. Abundant phenocrysts of plagioclase...||||||09-SEP-08
23473|Carne Dacite Member|68592|1|Redefined|p1061, p1063-4, p1079, p1083, p1113-20|Early Devonian|Early Devonian|See also p1610. Originally an undifferentiated part of Tangerang volcanics (Wass and Gould, 1969). Defined as a Member of Tangerang Formation by Jones, Carr et al. (1984). Redefined by Simpson, Carr and Jones (1997), and again here to include the former Inverary Tonalite of Carr et al. (1979), with which it is compositionally and texturally identical, which had been included in the Arthursleigh Suite by Chappell et al. (1991). Comprises 13 mapped bodies at different stratigraphic levels in the Formation. Type locality described. Geochemistry and geophysical properties described. Similar to Bogungra Dacite Member and Jemidee Microgranodiorite; interpreted as small, high-level intrusive bodies emplaced at various times during eruption of the Bindook Group. Abundant clasts of this unit occur in the Kerillon Tuff Member.||Unit in Tangerang Formation.||Overlies Kerillon Tuff Member. Is overlain by Kerrawarra Dacite Member. Is intruded by Corridgery Granite. Correlated with Bogungra Dacite Member.|Massive, crystal-rich, coarse-grained dacite sills and cross-cutting bodies; local flow-banding and auto-brecciation.|
23473|Carne Dacite Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dktc. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Tangerang Formation||Overlies unnamed member near middle of Tangerang Formation.|Massive-rarely flow banded and autobrecciated, medium-grained, porphyritic dacite intrusions. Abundant phenocrysts of plagioclase and altered pyroxene with minor hornblende and quartz set in an originally glassy groundmass.|
23473|Carne Dacite Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Tangerang Formation|||Massive-rarely flow banded and autobrecciated, medium-grained, porphyritic dacite intrusions. Abundant phenocrysts of plagioclase and altered pyroxene with minor hornblende and quartz set in an originally glassy groundmass.|
23473|Carne Dacite Member|70661|3|Fully described|p51, p52 fig 5, p64, p66 - p69|Early Devonian|Early Devonian|Named after Carne property. Originally an undifferentiated part of the Tangerang Volcanics, the former Inverary Tonalite has been incorporated into this member. Type section mentioned. Occurs as boulders to small Tor outcrops. Up to 300m thick. Structure, metamorphism, geochemistry and geophysical characteristics discussed. Complex intrusive relationship with the rest of the Tangerang Formation.||Tangerang Formation||Intrudes Tangerang Formation, correlated with parts of the Bogungra Dacite Member|Crystal rich dacite (40% phenocrysts) that is coarse grained consisting of 20-27% plagioclase, 12% ferromagnesian minerals, <5% quartz. The remaining groundmass is composed of quartz and feldspar with some spherulites.|
23473|Carne Dacite Member|71303|5|Briefly described|map legend|Pragian|Lochkovian|||Of Tangerang Formation.|||Discrete bodies of typically massive dacite containing abundant euhedral phenocrysts of plagioclase and less abundant quartz and altered ferromagnesian minerals. Rare hornblende locally.|16-FEB-18
23474|Carolees Granite|22638|3|Fully described|p76||Late Devonian|New name.||||||
23474|Carolees Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
23474|Carolees Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
30985|Carolina Forest Formation|22519|6|Mentioned|p6|||||||||
30985|Carolina Forest Formation|22831|2|Defined|p17, p6, p12 Table 2|Chewtonian|Bendigonian|Tottenham Subgroup||||||01-NOV-13
30985|Carolina Forest Formation|22857|5|Briefly described|p414 App. 1 Tb. A1.5|Ordovician||Of the Tottenham Subgroup (Girilambone Group). Basic schist with banded magnetite quartzite.||||||
30985|Carolina Forest Formation|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Tottenham Subgroup,Girilambone Group.||||||
30985|Carolina Forest Formation|43441|3|Fully described|10|||Age: ?Early Ordovician||||||08-JAN-10
30985|Carolina Forest Formation|44160|5|Briefly described|Map Legend|Chewtonian|Bendigonian|||||||
30985|Carolina Forest Formation|67322|5|Briefly described|p20|Darriwilian|Tremadocian|Defined by Sherwin (1996). Age assumed to Tottenham Subgroup. Moderately strongly metamorphosed and unfossiliferous. Occurs in the Condobolin - West Wyalong region. ||Of the Tottenham Subgroup||||21-FEB-18
29530|Carrabear Formation|22773|6|Mentioned|Fig24.10p355||Late Pleistocene|||||||
29530|Carrabear Formation|23053|4|Described|p7,12,Fig11p34,41-5||Late Pleistocene|||||||
29530|Carrabear Formation|24042|5|Briefly described|p513, 523|Pleistocene|Pleistocene||27-12 ka|||||11-SEP-12
29530|Carrabear Formation|43276|5|Briefly described|Map Legend||Late Pleistocene|||||||
29530|Carrabear Formation|43277|5|Briefly described|Map Legend||Late Pleistocene|of Great Australian Basin.||||||
29530|Carrabear Formation|68003|5|Briefly described|p92 Fig.3-v and Table 3-b, p103.|Late Pleistocene|Late Pleistocene|Coonamble Embayment. Ages from Watkins and Meakin (1996).|25.6+/-3.9 to 13.4+/-2.9 ka.|||Overlies Trangie Formation. Is overlain by Bugwah Formation.||
82123|Carrai Supersuite|71628|5|Briefly described|p1:5; p17: 1-2, 4-5, 13-46, 48, 50, 52|Triassic|Triassic|See also p17: 54, 56, 58, 62, 66, 69, 72, 88, 91, 93, 95, 97, 100; p19: 138, 140. Shaw et al. (2011); redefined in this study. Occurs S and SE of the main New England Batholith. Closely spatially associated with Hillgrove Supersuite. Geochemistry briefly summarised.||Coastal Granite Association.|Botumburra Range, Bitter Vine, Carrai, Daisy Plains, Guy Fawkes, Kindee Creek, Round Mountain, Valla, Yarrahapinni Suites.||Typically fine- to medium-grained, porphyritic to equigranular, intermediate to felsic granites. I-type.|
82123|Carrai Supersuite|72528|5|Briefly described|p2, p102, p110.|Carnian|Carnian|Age from Botumburra Range Granodiorite.|232.7+/-1.0 Ma||Includes Botumburra Range Monzogranite, Botumburra Suite||Includes granodiorite, monzogranite.|
40759|Carramundra Member|50613|2|Defined|p228 App.1|Westphalian|Westphalian|Of the Willuri Formation.  Volcanic member of the Piney Range package (informal grouping of stratigraphically recognisable distinctive, mappable units). Age: 309+/-4.3Ma (SHRIMP). Contains 3 beige ignimbrites (beds a, b and c). Max.thickness: 320m.||||||22-FEB-05
26257|Cartwrights Creek Metasediments|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
26257|Cartwrights Creek Metasediments|22575|6|Mentioned|p179 Fig.2|||Of the Paragon Group, Broken Hill Block.||||||11-JUN-08
26257|Cartwrights Creek Metasediments|22771|6|Mentioned|Table12.2p45,47|||||||||
26257|Cartwrights Creek Metasediments|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Max. thickness: 700m; in type area: 300m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
26257|Cartwrights Creek Metasediments|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Mt Isa Soldiers Cap Group and Georgetown (Qld) Etheridge Group upper sequence.||||||07-NOV-08
26257|Cartwrights Creek Metasediments|22965|6|Mentioned|Fig 1||Statherian|||||||
26257|Cartwrights Creek Metasediments|22967|6|Mentioned|p39||Statherian|||||||
26257|Cartwrights Creek Metasediments|23223|6|Mentioned|p43|||Correlate to interval in Paragon Group.||||||
26257|Cartwrights Creek Metasediments|23248|5|Briefly described|Fig2p169|||||||||
26257|Cartwrights Creek Metasediments|38969|4|Described|p210|||||||||
26257|Cartwrights Creek Metasediments|39662|2|Defined|p434|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26257|Cartwrights Creek Metasediments|40822|6|Mentioned|Fig.2|||||||||
26257|Cartwrights Creek Metasediments|41093|6|Mentioned|p252|||||||||
26257|Cartwrights Creek Metasediments|41145|6|Mentioned|Fig.4|||||||||
26257|Cartwrights Creek Metasediments|41630|6|Mentioned|Fig.1.3|||||||||
26257|Cartwrights Creek Metasediments|42261|6|Mentioned|Fig 1 P530|||||||||
26257|Cartwrights Creek Metasediments|42537|4|Described|p15|||||||||
26257|Cartwrights Creek Metasediments|43052|6|Mentioned|Fig.4.22|||||||||
26257|Cartwrights Creek Metasediments|43086|6|Mentioned|Fig.3|||Paragon Group||||||
26257|Cartwrights Creek Metasediments|43265|5|Briefly described|Map Legend||Paleoproterozoic|of Paragon Group||||||07-NOV-08
26257|Cartwrights Creek Metasediments|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
26257|Cartwrights Creek Metasediments|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
26257|Cartwrights Creek Metasediments|43572|6|Mentioned|Fig.3.2 p6|||||||||
26257|Cartwrights Creek Metasediments|50045|5|Briefly described|p116 Fig. 3.|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Paragon Group (Willyama Supergroup). Overlain by Bijerkerno Metasediments; underlain by Sundown Group. Contains King Gunnia Calc-Silicate Member.||||||31-MAY-07
26257|Cartwrights Creek Metasediments|50619|5|Briefly described|p178 Fig. 3||Paleoproterozoic|Of the Paragon Group (Willyama Supergroup).  Contains the King Gunnia Cac-Silicate Member.  Geological Province: Broken Hill Block.||||||07-NOV-08
26257|Cartwrights Creek Metasediments|60485|5|Briefly described|p28 Fig. 2|||Of the Paragon Group.  Geological Province: Broken Hill Domain.||||||03-MAR-05
26257|Cartwrights Creek Metasediments|61606|5|Briefly described|p4 Fig. 2|||Of Paragon Group.||||||18-MAY-06
26257|Cartwrights Creek Metasediments|61735|5|Briefly described|p635 Fig. 1|||Of Paragon Group.  Contains the King Gunnia Calc-silicate Member. Presented as Cartwirghts Creek only in Fig. 2||||||30-JUN-09
26257|Cartwrights Creek Metasediments|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Geological province: Broken Hill Domain.||||||
26257|Cartwrights Creek Metasediments|62535|5|Briefly described|p666 Fig.3, p671-672, p674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Paragon Group.|King Gunnia Calc-Silicate Member.||Graphitic, aluminosilicate-rich metasedimentary rocks.|
26257|Cartwrights Creek Metasediments|62536|5|Briefly described|p636, 641|||Broken Hill area. Appears only as Cartwrights Creek on p636, 641.||Sundown Group.||||
26257|Cartwrights Creek Metasediments|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Paragon Group.||||
26257|Cartwrights Creek Metasediments|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Paragon Group|Includes King Gunnia Calc-Silicate Member|Overlain by Bijerkerno Metasediments||19-DEC-21
26257|Cartwrights Creek Metasediments|63102|5|Briefly described|p13-14,35-36|||Geological province: Broken Hill Domain, Curnamona Province. Change in Nd isotope signature (Barovich 2003) indicate a switch in sediment provenance away from possible central Australian source.||Unit of Paragon Group.||Equivalent to Alconie Formation and parts of the Mount Howden Subgroup.||22-OCT-19
26257|Cartwrights Creek Metasediments|63519|5|Briefly described|Abstract, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Includes the King Gunnia Calc-Silicate Member. Overlain by Bijerkerno Metasediments. Dark grey, graphitic phyllite, after chiastolite schist. See also p10 Fig. 3.||||||07-NOV-08
26257|Cartwrights Creek Metasediments|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province. ||Paragon Group|Includes the King Gunnia Calc-Silicate Member|Overlain by the Bijerkerno Metasediments.|Thin-bedded to laminated graphitic pelite and psammopelite.|
26257|Cartwrights Creek Metasediments|64097|5|Briefly described|p302|Paleoproterozoic|Paleoproterozoic|In lower section of Paragon Group. Includes fine-grained graphitic metasandstone in upper section.||||||07-FEB-11
26257|Cartwrights Creek Metasediments|64741|4|Described|p301 Fig. 4, p311|Paleoproterozoic|Paleoproterozoic|Of Paragon Gr. Contains King Gunnia Calc-Silicate Mbr. Thickness:1000m.Geol.prov: Broken Hill Domain.Thickly interlayered graphitic metasiltstone and aluminous pelite grading upwards into Bijerkerno Metasediments. Equiv.to Alconie Fm. in Olary Domain||||||07-FEB-11
26257|Cartwrights Creek Metasediments|64742|6|Mentioned|p321 Fig.3.|||See also entries for the mis-named Cartwrights Creek Formation pp329-330.||Unit in Paragon Group.|||Psammite, pelitic schist.|29-MAR-12
26257|Cartwrights Creek Metasediments|64944|5|Briefly described|p28 Fig. 1, p31|Paleoproterozoic|Paleoproterozoic|Of Paragon Group. Geological province: Broken Hill Domain. Equivalent of Alconie Formation in Olary Domain.||||||07-FEB-11
26257|Cartwrights Creek Metasediments|66302|4|Described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Paragon Group||Overlain by the Bijerkerno Metasediments.|Thin-bedded to laminated graphitic mudstone and siltstone.|
26257|Cartwrights Creek Metasediments|68126|5|Briefly described|p5|||Broken Hill Domain, Curnamona Province.|1600 +/- 4 Ma (Page, 2006).||||Includes felsic intrusives.|
26257|Cartwrights Creek Metasediments|70000|5|Briefly described|p34, p37|Statherian|Statherian|||Unit in Paragon Group.|Includes King Gunnia Calc-Silicate Member.|Is overlain conformably (gradationally) by Bijerkerno Metasediments.|Graphitic siltstones and aluminous metapelitic rocks with minor thinly-bedded calc-silicate in the upper section.|
26257|Cartwrights Creek Metasediments|70014|5|Briefly described|Map legend|||At higher metamorphic grades, consists of graphitic micaceous psammopelitic schist with sporadic thick and thin chiastolite (or sillimanite pseudomorphs after chiastolite)-rich, pelitic to psammopelitic schist beds.||Basal unit in Paragon Group.|Includes King Gunnia Calc-Silicate Member.|Overlies Sundown Group. Is overlain by Bijerkerno Metasediments.|Grey phyllites, graphitic, pelitic to psammopelitic, finely laminated, spotted and minor non-spotted. Basal to middle sections contain extensive chiastolite-rich beds, lenticular, dark grey to black.|
26257|Cartwrights Creek Metasediments|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Paragon Group.|||Graphitic phyllite and chiastolite schist; includes graphitic metasandstone in upper section. Distinctive horizon of layered graphitic, amphibole-rich calcsilicate at top.|
26257|Cartwrights Creek Metasediments|70405|6|Mentioned|p9 table 1, p30, p43 Table 3|Paleoproterozoic|Paleoproterozoic||1640 Ma - 1655 Ma|||Correlates with Alconie Formation||
26257|Cartwrights Creek Metasediments|70657|5|Briefly described|p13 Fig.6, p14-15, p33, p40, p42-43|Statherian|Statherian|Curnamona Province; Broken Hill Domain.||Paragon Group|King Gunnia Calc-Silicate Member.|Overlies Sundown Group. Underlies Bijerkerno Metasediments. Equivalent to Alconie Formation (Olary Domain).||
26257|Cartwrights Creek Metasediments|70658|5|Briefly described|p7, 15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Paragon Group.|King Gunnia Calc-Silicate Member.|Equivalent to Alconie Formation.||
26257|Cartwrights Creek Metasediments|71968|4|Described|p1-3,5,18-24,26,28-33,35-36,38-32|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Sample GA 2464042 (monazite in carbonaceous metapelite) yielded a weighted mean age of 1582+\-4 Ma, interpreted as the main pervasive metamorphic event affecting the rock, with possible rare preservation of an earlier metamorphic event at 1619+\-16 Ma. Further in situ geochronology may firm up the timing of this earlier event. Sample GA 2533772 (monazite in cordierite andalusite granofels) yielded three main episodes of metamorphism and/or recrystallisation; weighted mean 207Pb/206Pb age of 1584+\-16 Ma, interpreted  to record first formed foliation in Paragon Group in the Mount Robe Sub-block; preservation of an earlier metamorphic event at 1618+\-13 Ma (weighted mean 207Pb/206Pb, similar to that in GA2462042); and hydrous muscovite-rich retrogression post-peak metamorphism at 1537+\-15 Ma (weighted mean 207Pb/206Pb). Sample GA 2676606 (zircon in cordierite andalusite granofels) yielded a weighted mean 207Pb/206Pb age of 1754+\-6 Ma, interpreted as a maximum depositional age for this sample of cordierite andalusite granofels. See also p47.||Unit of Paragon Group.|Includes King Gunnia-Calc-silicate.|Overlain by Bijerkerno Metasediments and the Dalnit Bore Metasediments.|Thickly interlayered graphitic metasiltstone and aluminous pelite (generally chiastolite-bearing).|06-DEC-19
26257|Cartwrights Creek Metasediments|72454|6|Mentioned|p21 Tb.3|Calymmian|Statherian|Part of the Broken Hill Domain. Age determined by Page (2006) on a felsic intrusive - no methodology given.|1600 +/- 4 Ma.||||Includes metasediments.|
26257|Cartwrights Creek Metasediments|72461|5|Briefly described|p16 fig 9, p19|||||Paragon Group|Includes the King Gunnia Calc-Silicate Member|Conformably overlies the Sundown Group. Overlain bvy the Bijerkerno Metasediments.|Dark-grey, graphitic phyllite, after chiastolite schist.|
26257|Cartwrights Creek Metasediments|73482|5|Briefly described|p422 Fig.3, p427, p429 Fig.8|||||Paragon Group, basal part|King Gunnia Calc-Silicate Member||Metasediments.|
26257|Cartwrights Creek Metasediments|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|||||Paragon Group|King Gunnia Calc-Silicate Member|Overlies Sundown Group, underlies Bijerkerno Metasediments||
28440|Cary Formation|22857|4|Described|p456 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Cudal Group. Fossiliferous cherts and shale; contains corals, bryozoans, crinoids, molluscs, brachiopods, algae. Max. thickness: 120m. Geological Province: Cowra Trough.||||||
28440|Cary Formation|23043|5|Briefly described|Map Legend|Ludlow|Wenlock|of Cudal Group.||||||
28440|Cary Formation|23170|2|Defined|p103|Ludlow|Wenlock|of Cudal Group.||||||
28440|Cary Formation|40328|2|Defined|p78|Silurian|Silurian|Also mentioned on P71 & Plate 3||||||
28440|Cary Formation|43494|3|Fully described|p18|Ludlovian|Late Wenlockian|Of the Cudal Group. Formerly the Cary Beds of Maggs(1963). Mainly shale and chert; minor quartzo-feldspathic sst. Conformably overlies Canowindra Volcanics; overlain by Burrawong Limestone. Mapped as Burragundy Formation in northern area (Pickett 1982).||||||01-OCT-09
28440|Cary Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Cudal Group.  Shale, tuffaceous sediment, chert, minor sandstone, rhyolitic tuff, minor limestone.||||||19-JUL-04
28440|Cary Formation|66197|5|Briefly described|p633 Fig.4c|Ludlow|Wenlock|Cowra Trough-Molong High. Deep marine shale. Underlies the Burrawong Limestone, overlies the Canowindra Volcanics.||||||14-MAR-12
28440|Cary Formation|73299|6|Mentioned|p1105|||Cowra Trough. [Map symbol suggests Silurian age]||||||
26465|Cascade Creek beds|41348|5|Briefly described|Map legend|Early Paleozoic|Early Paleozoic|Part of the "Woolomin Association".||||||07-NOV-08
26465|Cascade Creek beds|71628|6|Mentioned|p18:3|||||Woolomin Association.||||
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.|
82384|Cataract Creek Granodiorite|71628|5|Briefly described|p17: 2, 73-74|||New name, for a small (2 km across) intrusion identified by Pratt (2010), ~4.5 km NNW of Lorne. Named after a local watercourse. Very limited (one analysis) geochemistry described.||The Brothers Suite.||Intrudes Camden Haven Claystone.|Granodiorite.|
31521|Cathcart Suite|22815|5|Briefly described|p85|||||||||
31521|Cathcart Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31521|Cathcart Suite|43233|5|Briefly described|Map Legend|||of Bega Batholith.||||||
31521|Cathcart Suite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|||Unit in Glenbog Supersuite.||||
32271|Cemetery Creek Tonalite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb32.||||||
32271|Cemetery Creek Tonalite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
81964|Central Valley Breccia Member|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Of Siding Spring Formation.|||Volcaniclastic polymictic breccia, variably pyritic; rare metasedimentary clasts. Inferred near-vent deposits.|02-NOV-20
24835|Cessnock Sandstone Member|22610|5|Briefly described|Fig 1, 5|||Maximum thickness 16m||||||
24835|Cessnock Sandstone Member|22969|6|Mentioned|Fig 5.3|||||||||
24835|Cessnock Sandstone Member|23540|5|Briefly described|Fig 2 p 419|||||||||
24835|Cessnock Sandstone Member|33867|5|Briefly described|p6|||||||||
24835|Cessnock Sandstone Member|34015|6|Mentioned|Fig.5.4|||||||||
24835|Cessnock Sandstone Member|34345|2|Defined|p331|Permian|Permian|||||||
24835|Cessnock Sandstone Member|39287|6|Mentioned|p20|||||||||
24835|Cessnock Sandstone Member|39288|6|Mentioned|p63|||||||||
24835|Cessnock Sandstone Member|43447|14|Not recorded|p19|||||||||
24835|Cessnock Sandstone Member|45090|5|Briefly described|p156|||||||||
82124|Chaelundi Mountain Monzogranite|71628|4|Described|p13: 1; p17: 1-2, 4, 6-10, 28-29, 35, 67|||See also p17: 90-92, 103; p19: 13, 16, 73, 96. New name (this study) for the A-type granites in the NE portion of the Chaelundi Complex, after Landenberger and Collins (1996). Forms a blockish-shaped unit ~5 km across, 40 km NW of Dorrigo. Named after a local mountain. Geochemistry described in considerable detail. Dandahra Creek Suite.|237.7 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Chaelundi Complex.||Intrudes Moombil Siltstone and Guy Fawkes Granodiorite.|Medium- to coarse-grained biotite leucomonzogranite, and biotite-(hornblende) monzogranite to quartz monzodiorite. A-type.|
82124|Chaelundi Mountain Monzogranite|72528|6|Mentioned|p110.|Middle Triassic|Middle Triassic||c.238 Ma|Dandahra Creek Suite||||
24605|Chalk Mountain Formation|38689|3|Fully described|p300|||||||||
24605|Chalk Mountain Formation|43046|5|Briefly described|p267|||||||||
24605|Chalk Mountain Formation|49781|5|Briefly described|p5|||||||||
24605|Chalk Mountain Formation|61155|5|Briefly described|p19|Middle Miocene|Middle Miocene|Overlain by rocks associated with the Warrumbungle Volcano. In the Liverpool Range area.||||||
24605|Chalk Mountain Formation|71890|4|Described|p19, p52|Langhian|Burdigalian|Deposited in a lacustrine setting.|18-15.2 Ma|Warrumbungle Volcanics|||Sediments of white to pale grey siltstone, mudstone and clay with interbedded diatomite, tuff. One lignite band near the top. Fossiliferous.|
81960|Chalkers Ridge Member|72700|5|Briefly described|Mapsheet 1|Cenozoic|Cenozoic|||Shawns Creek Formation|||Massive to weakly bedded volcaniclastic breccia comprising quartz crystals and felsic coherent clasts in a glassy matrix.|02-NOV-20
34499|Champion-type granite|22771|6|Mentioned|p50|||||||||
32689|Charcoal Tank Granite|22434|6|Mentioned|11 fig 14|Silurian|Silurian|Geol province Lachlan Fold Belt||||||
32689|Charcoal Tank Granite|24417|3|Fully described|p53|Silurian|Silurian|Intrudes and is wholly contained with in the Humbug Sandstone (Wagga Group).||||||
32689|Charcoal Tank Granite|50385|5|Briefly described|Map Legend|Silurian|Silurian|Medium-grained cordierite-bearing two-mica granite||||||
32689|Charcoal Tank Granite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|Of the Ungarie Suite.||||||13-JUL-04
82385|Charon Creek Quartz Diorite|71628|4|Described|p2: 2, 19-22, 53; p3: 5, 28, 30-31|||Originally the Charon Creek Diorite of Burlinson (1977). Named after the watercourse of that name. Here renamed the Charon Creek Quartz Diorite to reflect the likely dominant composition. Occurs near the village of Dundurrabin, 80 km E of Guyra and ~60 km NW of Coffs Harbour. Crops out as numerous small bodies. May be merely a continuation of Sheep Station Creek Complex. Assigned to Bakers Creek Suite by Landenberger (1996) and later to Bakers Creek Supersuite (Landenberger et al., 2010). Geochemistry described.|290.4 +/- 3.2 Ma (McKibbin et al., 2017).|Bakers Creek Supersuite.||Within and around Dundurrabin Granodiorite. Intrudes Moombil Sandstone and Brooklana beds.|Dark grey, medium-grained quartz diorite; minor tonalite.|
28221|Chateau Douglas Sandstone Member|35245|2|Defined|p20|Early Carboniferous|Early Carboniferous|||||||
28221|Chateau Douglas Sandstone Member|44244|6|Mentioned|p22|||Of the Kingsfield Formation.  Lithic sandstone with scattered volcanic pebbles and magnetic sandstone.||||||
24837|Cheesemans Creek Formation|13139|5|Briefly described|p7, p9 Fig. 4, p10|Late Ordovician|Late Ordovician|Unconformably overlain by the "Limestone A" subunit of the Boree Creek Formation.||||||
24837|Cheesemans Creek Formation|22857|4|Described|p426 App. 1 Tb. A1.5|Ordovician|Ordovician|Of the Cabonne Group. Basaltic andesite, mafic and quartz latite, siltstone, sandstone, breccia, conglomerate. Max. thickness: 900m. ||||||
24837|Cheesemans Creek Formation|23170|6|Mentioned|p34|||||||||
24837|Cheesemans Creek Formation|23181|6|Mentioned|Fig.2|||Malongulli Formation equivalent.||||||
24837|Cheesemans Creek Formation|23213|5|Briefly described|p13,19 Fig.1,7,10|Bolindian|Eastonian|Age: Middle Eastonian to Early Bolindian. Part of Oakdale Formation. of Northern Molong Volcanic Belt.||||||
24837|Cheesemans Creek Formation|23214|3|Fully described|p68|Bolindian|Eastonian|||||||
24837|Cheesemans Creek Formation|23334|5|Briefly described|7|Late Ordovician|Late Ordovician|||||||
24837|Cheesemans Creek Formation|23739|5|Briefly described|p216 Fig. 2|Ordovician|Ordovician|||||||
24837|Cheesemans Creek Formation|30044|6|Mentioned|Fig.7|||||||||
24837|Cheesemans Creek Formation|30139|5|Briefly described|Table 1|||||||||
24837|Cheesemans Creek Formation|31161|5|Briefly described|PA2|||||||||
24837|Cheesemans Creek Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
24837|Cheesemans Creek Formation|33116|4|Described|p204|||Ordovician.||||||06-SEP-18
24837|Cheesemans Creek Formation|33121|6|Mentioned|p85|||Late Ord. Correlation table||||||
24837|Cheesemans Creek Formation|33735|6|Mentioned|Fig.2|||||||||
24837|Cheesemans Creek Formation|34895|6|Mentioned|Fig. 1|||||||||
24837|Cheesemans Creek Formation|35118|6|Mentioned|Fig.5|||||||||
24837|Cheesemans Creek Formation|35291|6|Mentioned|Fig.7|||||||||
24837|Cheesemans Creek Formation|35412|6|Mentioned|Fig.9|||||||||
24837|Cheesemans Creek Formation|35415|6|Mentioned|Fig.2|||Stratigraphic correlations.||||||
24837|Cheesemans Creek Formation|37727|6|Mentioned|Fig.1|||||||||
24837|Cheesemans Creek Formation|38219|6|Mentioned|Table 2|||||||||
24837|Cheesemans Creek Formation|39331|4|Described|p66|||See also Fig.6-3 & p57.||||||06-SEP-18
24837|Cheesemans Creek Formation|40136|5|Briefly described|p21|||||||||
24837|Cheesemans Creek Formation|40328|6|Mentioned|p147|||||||||
24837|Cheesemans Creek Formation|43640|5|Briefly described|Map Legend||Ordovician|||||||
24837|Cheesemans Creek Formation|43782|5|Briefly described|Map Legend|Bolindian|Eastonian|Of Cabonne Group.||||||01-SEP-08
24837|Cheesemans Creek Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p152|Late Ordovician|Late Ordovician|Geological Province: Molong Volcanic Belt, LFB. Consists of volcaniclastic sandstone and extensive basalt-andesite sills in the lower part, upper part has andesite flows, some are pillowed. Age idenified via grsptolite faunas.||||||07-FEB-11
24837|Cheesemans Creek Formation|63283|5|Briefly described|p202, p189 Tb. 1, p194 Fig. 2, p201|Late Ordovician|Bolindian|Underlain by Reedy Creek Limestone. Age: 445Ma (big plag basalt lava). Geological province: Molong Volcanic Belt. Graptolites indicate Bolindian age. See p202.||||||07-FEB-11
24837|Cheesemans Creek Formation|63286|5|Briefly described|p294 Fig. 1, p308 Fig. 9|Early Silurian|Late Ordovician|Consists of basaltic and andesitic lavas, breccia sandstone and mudstone. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
24837|Cheesemans Creek Formation|63287|5|Briefly described|p316 Fig. 1, p317 Fig. 2, p335, p337|Bolindian|Eastonian|Of Cabonne Group. Underlain by Fairbridge Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
24837|Cheesemans Creek Formation|63290|6|Mentioned|p393 Tb. 1|Bolindian|Eastonian|Geological Province: Molong Volcanic Belt. ||||||
24837|Cheesemans Creek Formation|63293|5|Briefly described|p470, p468 Fig. 2|Bolindian|Eastonian|Underlain by Reedy Creek Formation. Age: ca 452Ma (implied deposition age). Clasts of plagioclase+hornblende+quartz-phyric felsic intrusive rocks occur at the base. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
24837|Cheesemans Creek Formation|64295|5|Briefly described|p200 Fig. 2|||||||||
24837|Cheesemans Creek Formation|64963|5|Briefly described|p183|||||||||
24837|Cheesemans Creek Formation|67106|6|Mentioned|p673|||Molong Volcanic Belt.||||||
24837|Cheesemans Creek Formation|67322|5|Briefly described|p20 Fig.5, p23|Katian|Katian|Macquarie Arc. Sherwin (1971). Graptolite fauna revised by Vandenberg (2003), who assigned a late Eastonian to early Bolindian age. Occurs in the North Molong Volcanic Belt.||Of the Cabonne Group.||Overlies Reedy Creek Limestone.||21-FEB-18
24837|Cheesemans Creek Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
24837|Cheesemans Creek Formation|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3). Molong Volcanic Belt. Shown as Cheesemans Ck Fm.|c. 449-443 Ma|Cabonne Group||||18-MAY-16
24837|Cheesemans Creek Formation|70684|5|Briefly described|p3, p18-19, p27-29, p33, p74|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Late Eastonian to early Bolindian age.||||Overlies Reedy Creek Limestone.|Siltstone, sandstone intruded by rare sills, and an upper part of plagioclase-phyric andesite flows, some pillowed.|
24837|Cheesemans Creek Formation|70754|6|Mentioned|p450 Fig.2|Late Ordovician|Late Ordovician|||||Overlies Reedy Creek Limestone.||
24837|Cheesemans Creek Formation|72263|5|Briefly described|p516-517|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen.||||Underlain conformably by Fairbridge Volcanics.||
24837|Cheesemans Creek Formation|73154|5|Briefly described|p77 Fig.3|Bolindian|Eastonian|Macquarie Arc, Phase 4. Molong Volcanic Belt.|||||Intermediate-mafic lava, conglomerate.|
28449|Cheitmore Limestone Member|22857|5|Briefly described|p480 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the De Drack Formation.||||||
28449|Cheitmore Limestone Member|39028|6|Mentioned|Map legend|Ludlovian|Ludlovian|||||||
28449|Cheitmore Limestone Member|40276|2|Defined|p5|Late Silurian|Late Silurian|||||||
28449|Cheitmore Limestone Member|68592|5|Briefly described|p760|||Defined on Araluen 1:100 000; Wyborn and Owen (1989).||Unit in De Drack Formation.|||Limestone.|
28449|Cheitmore Limestone Member|71069|6|Mentioned|p146|||||De Drack Formation||||
30854|Chesleigh Group|22529|6|Mentioned|1|||||||||
30854|Chesleigh Group|22590|5|Briefly described|P750, Fig1|Pridoli|Ludlow|||||||
30854|Chesleigh Group|22768|6|Mentioned|p180||Wenlock|||||||
30854|Chesleigh Group|22857|5|Briefly described|p180, p470 App.1 Tb.A1.6|Late Silurian|Middle Silurian|Possibly interfingers with the Barnby Hill Shale in Hill End area. Max. thickness: 1.5km. Geological Province: Hill End Trough and Capertee Rise.||||||
30854|Chesleigh Group|23043|5|Briefly described|Map Legend|Lochkovian|Ludlow|||||||
30854|Chesleigh Group|23170|2|Defined|p72|Early Devonian|Silurian|Age Middle Silurian (LLandovery??) to E. Devonian. Lachlan Fold Belt.||||||
30854|Chesleigh Group|50124|5|Briefly described|p125 Fig.2, p130|Silurian|Silurian|Formerly Chesleigh Formation. Geological Province: eastern Lachlan Fold Belt.||||||
30854|Chesleigh Group|66197|5|Briefly described|p633 Fig.4a, b|Pridoli|Ludlow|Capertee High-Hill End Trough. Mudstone-dominated deep marine turbidites. Underlies Crudine Group. Age: 420 +/- 5 Ma, 417 +/- 5 Ma.||||||13-MAR-12
30854|Chesleigh Group|68003|5|Briefly described|p24 Fig.3-e, p146. |Pridoli|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Biraganbil and Piambong Formations.|||
30854|Chesleigh Group|68592|5|Briefly described|p624, p650|Late Silurian|Late Silurian||||Includes Biraganbil Formation.|Correlated with Campbells Group.||
30854|Chesleigh Group|70036|5|Briefly described|Map legend|||Lachlan Fold Belt. Included in a mapped unit of Silurian and Devonian sedimentary and volcanic rocks including strongly to moderately deformed felsic to andesitic metasedimentary rocks, conglomerate, sandstone, siltstone, mudstone, shale, tuff, basalt, andesite and rhyolite.||||||
30854|Chesleigh Group|70297|4|Described|map legend, on side 2 of map sheet|Lochkovian|Ludlow|Formerly Chesleigh Formation. Age: late Silurian to earliest Devonian. Include siltstone and sandstone that were deposited in a deep water environment; upper part includes felsic volcaniclastic rocks. The upper unit hosts base metal deposits, on eastern side of Hill End Trough; classified as siliciclastic-felsic hosted (i.e. Iberian-type).|||Piambong Formation, Biraganbil Formation|Overlies Campbells Group and Mumbil Group. ?Is overlain by Crudine Group.|Felsic volcaniclastic, quartz-lithic, feldspar-lithic and quartzose sandstone, siltstone, slate, shale; crystal and vitric tuff; breccia and conglomerate; chert, felsic porphyry.|
30854|Chesleigh Group|73299|6|Mentioned|p1101, p1102 Fig.8|Late Silurian|Late Silurian|Hill End Trough, exposed in the Hill End Anticline.||||Overlies the Bells Creek Volcanics, underlies the Cookman Formation.||
82387|Cheviot Hills Granite|71628|5|Briefly described|p19: 22-23|||New name, after work by Brown and Stroud (1997). The name is derived from Cheviot Hills homestead. Previous uses of ""Cheviot Hills"" applied to volcanigenic sediments near Drake are superseded. Forms a narrow (~4 x 0.5 km), N-S body 8-10 km SSW of Ashford.||Cheviot Hills Suite.||Intrudes Texas beds.|Felsic intrusive.|
24219|Chichester Formation|22857|4|Described|p508 App.1 Tb.A1.8|Visean|Visean|Dark usually fossiliferous siltstone and mudstone, with interbeds or lenses of lithic arenite, gravel and conglomerate. Disconformably overlain by Mount Johnstone Formation. Max. thickness: 1000m. Geological Province: Tamworth Forearc Basin.||||||
24219|Chichester Formation|35953|6|Mentioned|p589|||||||||
24219|Chichester Formation|36528|6|Mentioned|p178|||||||||
24219|Chichester Formation|39660|2|Defined|p452|late Visean|late Visean|||||||
24219|Chichester Formation|40883|6|Mentioned|p7|||||||||
24219|Chichester Formation|42547|4|Described|p31|||||||||
24219|Chichester Formation|43576|6|Mentioned|Fig.1,p348|||||||||
24219|Chichester Formation|43792|5|Briefly described|p363||Carboniferous|||||||
24219|Chichester Formation|44093|5|Briefly described|p228 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
24219|Chichester Formation|44244|2|Defined|p111|Visean|Visean|Includes Williams River Member.  Overlies the Verulam Oolite Member (Flagstaff Formation);  disconformably underlies Mount Johnstone Formation.Max. thickness: >630m.  Type section in text.  Geological Province: Gresford Block.||||||
24219|Chichester Formation|47056|6|Mentioned|Fig.2 P523|||||||||
24219|Chichester Formation|50147|5|Briefly described|Map legend|Visean|Visean|Dark grey, thinly bedded mudstone and siltstone.  Geological Province: Gresford Block||||||
24219|Chichester Formation|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Rouchel Block.  Overlies: Isismurra Formation.||||||
24219|Chichester Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Rouchel Block, Tamworth Belt.||||||
24219|Chichester Formation|71628|6|Mentioned|p6:22|||||Dewrang Group.||||
24219|Chichester Formation|73197|6|Mentioned|p467|Carboniferous|Carboniferous|New England Orogen, southern. Forearc basin, volcanic rocks sourced from the Currabubula-Connors Arc.|||||Volcanic rocks, predominantly ignimbrite.|
70476|Chilcotts Creek Ignimbrite Member|62095|2|Defined|p276 Appdx.|Late Carboniferous|Late Carboniferous|of Currabubula Formation. Beige, slightly welded to to unwelded ignimbrite. Age: ~310Ma. Thickness: ~15m. geological Province: Werrie block/Tamworth Belt. See also Plate 1, p254 Figs. 4,5.||||||
40949|Childowla Quartz Monzonite|50230|5|Briefly described|Map legend|Emsian|Pragian|Massive medium-grained equigranular biotite-hornblende quartz monzonite to granite.||||||
40949|Childowla Quartz Monzonite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Childowla Suite. Pink, medium- to fine-grained, foliated, equigranular biotite-hornblende quartz monzonite to granodiorite.||||||25-JUN-08
40949|Childowla Quartz Monzonite|68592|3|Fully described|p1398-9, p1401-3, p1413-20|Early Devonian|Early Devonian|New name, after Childowla property. A small (2 km2) body named Chowdilla Quartz Monzonite was named and mapped by MacDonald (1979), who mis-spelled the name of the property. The unit was previously shown as silicic volcanics of Mountain Creek Volcanics (Brunker and Offenberg, 1970; Cramsie et al., 1978). Type area described. Geochemistry detailed; geophysical properties described. Not isotopically dated: age from intrusive relationships and compositional similarity with Boggy Plain Supersuite plutons.||Unit in Childowla Suite.||Intrudes Mountain Creek Volcanics.|Pink, medium- to fine-grained, foliated, equigranular, biotite-hornblende-quartz monzonite to granodiorite; occasional hornblende-rich enclaves to 4 cm. I-type.|
40949|Childowla Quartz Monzonite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dic. On Yass 1:100 000 mapsheet portion of Time-Space Plot.||Childowla Suite|||Medium-fine grained, foliated, equigranular, biotite-hornblende-quartz monzonite to granodiorite; high magnetic susceptibility.|
40949|Childowla Quartz Monzonite|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Childowla Suite|||Medium-fine grained, foliated, equigranular, biotite-hornblende-quartz monzonite to granodiorite; high magnetic susceptibility.|
73233|Childowla Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Contains the Childowla Quartz Monzonite.||||||11-JUL-13
73233|Childowla Suite|68592|2|Defined|p1398, p1413-20|Early Devonian|Early Devonian|New name, after Childowla property. Consists of a single [!] small (2 km2) pluton (Childowla Quartz Monzonite) which is therefore the type pluton. Is distinguished on geochemical grounds; geochemistry detailed. Not isotopically dated: age from intrusive relationships and compositional similarity with Boggy Plain Supersuite plutons.||Unit in Boggy Plain Supersuite.|Includes Childowla Quartz Monzonite.|Intrudes and contact metamorphoses Mountain Creek Volcanics.|Pink, medium- to fine-grained, foliated, equigranular, biotite-hornblende-quartz monzonite to granodiorite; occasional hornblende-rich enclaves to 4 cm. I-type.|
73233|Childowla Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|On Yass 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Childowla Quartz Monzonite.|||
73233|Childowla Suite|70540|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Childowla Quartz Monzonite.|||
26477|Christine Judith Conglomerate|22631|6|Mentioned|p177|||||||||
26477|Christine Judith Conglomerate|22772|4|Described|p64,Table13.1|Cryogenian|Cryogenian|||||||
26477|Christine Judith Conglomerate|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Pintapah Subgroup (Poolamacca Group). Rounded, well-sorted quartzite pebbles and cobbles in quartzite matrix. Age: >802+/-10Ma based on correlation with SA. Max. thickness: 150m. Geological Province: Adelaide Fold Belt. See also p400 App. 1 Tb.A1.3.||||||29-AUG-18
26477|Christine Judith Conglomerate|30261|4|Described|Table 1|||Willouran age||||||
26477|Christine Judith Conglomerate|33004|6|Mentioned|p134|||||||||
26477|Christine Judith Conglomerate|34812|3|Fully described|p55|||||||||
26477|Christine Judith Conglomerate|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26477|Christine Judith Conglomerate|35692|6|Mentioned|p23|||||||||
26477|Christine Judith Conglomerate|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
26477|Christine Judith Conglomerate|36733|6|Mentioned|Table 5|||||||||
26477|Christine Judith Conglomerate|37854|6|Mentioned|Table 1|||||||||
26477|Christine Judith Conglomerate|37931|4|Described|p533|||||||||
26477|Christine Judith Conglomerate|38157|6|Mentioned|Table II|||||||||
26477|Christine Judith Conglomerate|39214|6|Mentioned|p5|||||||||
26477|Christine Judith Conglomerate|40294|6|Mentioned|Table 2|||||||||
26477|Christine Judith Conglomerate|40595|6|Mentioned|Table 3|||||||||
26477|Christine Judith Conglomerate|41403|4|Described|p48|||||||||
26477|Christine Judith Conglomerate|42222|6|Mentioned|p11|||||||||
26477|Christine Judith Conglomerate|42223|6|Mentioned|Fig.2 P36|||||||||
26477|Christine Judith Conglomerate|42531|5|Briefly described|Map legend|Adelaidean||||||||
26477|Christine Judith Conglomerate|42813|6|Mentioned|p14|||||||||
26477|Christine Judith Conglomerate|43265|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
26477|Christine Judith Conglomerate|43268|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
26477|Christine Judith Conglomerate|43269|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
26477|Christine Judith Conglomerate|62724|5|Briefly described|p17 Fig. 4|Willouran|Willouran|Of the Poolamacca Group. Geological Province: Broken Hill Domain.||||||07-FEB-11
26477|Christine Judith Conglomerate|69023|6|Mentioned|p63|||||||||
26477|Christine Judith Conglomerate|70000|5|Briefly described|p34|Neoproterozoic|Neoproterozoic|||Unit in Pintapah Subgroup.|||Fluviatile to shallow marine conglomerate.|
26477|Christine Judith Conglomerate|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Pintapah Subgroup.||Overlies Lady Don Quartzite. Is overlain by Boco Formation.|Monomictic conglomerate with rounded, well-sorted quartzite pebbles and cobbles in a quartzite matrix.|07-SEP-15
26477|Christine Judith Conglomerate|72461|6|Mentioned|p16 fig 9|||||Pintapah Subgroup||||
80145|Cintra Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Werrie Basin. Shown only as Cintra. Ending assumed from references to other Coal Members in text.||Rowan Formation.||||28-SEP-17
30040|Clandulla Limestone|22529|5|Briefly described|7|Early Devonian|Early Devonian|||||||
30040|Clandulla Limestone|22590|6|Mentioned|Fig3 P754||Lochkovian|Actually spelt Clandulla Lst.||||||
30040|Clandulla Limestone|22857|4|Described|p476 App.1 Tb.A1.6|Lochkovian|Lochkovian|Of the Kandos Group. Limestone and dolomite, carbonaceous shale. Max. thickness: 170m. Geological Province: Capertee Rise. ||||||
30040|Clandulla Limestone|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Kandos Group.||||||
30040|Clandulla Limestone|23170|2|Defined|p128|Middle Devonian|Early Devonian|of Kandos Group.||||||
30040|Clandulla Limestone|23522|5|Briefly described|p248 Fig 4|Lochkovian|Lochkovian|||||||
30040|Clandulla Limestone|43188|3|Fully described|p205,Table 3 p209|Lochkovian|Lochkovian|Type section location given. Age early to middle Lochkovian. Of Kandos Group.||||||
30040|Clandulla Limestone|44093|5|Briefly described|p212 App. 1|Early Devonian|Early Devonian|Of the Kandos Group. Geological Province: Lachlan Fold Belt.||||||
30040|Clandulla Limestone|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cudgegong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
30040|Clandulla Limestone|73143|6|Mentioned|p9|Lochkovian|Lochkovian|Lachlan Orogen, eastern. Contains conodonts, Caudicriodus woschmidti and postwoschmidti identified by Colquhoun (1995) subsequently identified as Cypricriodus hesperius (Drygant, 2010). Contains Lochkovian corals.||||||
26479|Clanricard Coal Member|29942|4|Described|Fig.1|||Permian||||||
26479|Clanricard Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26479|Clanricard Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Foybrook Formation.||||
30032|Clare Sandstone|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Coogal Subgroup (Black Jack Group). Medium to coarse-grained quartzose sandstone; quartzose conglomerate; Breeza coal seam at top. Max. thickness: >95mm. Geological Province: Gunnedah Basin.||||||
30032|Clare Sandstone|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Coogal Subgroup. Replaces Clare Sandstone Member of Black Jack Formation (now Black Jack Group). Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||13-NOV-13
30032|Clare Sandstone|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Coogal Subgroup.||||||
30032|Clare Sandstone|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Coogal Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Quartz sandstone, siltstone and coal.||||||
30032|Clare Sandstone|65116|5|Briefly described|p447, fig 6, p441|Late Permian|Late Permian|?Of Black Jack Group. Medium to coarse quartzose sandstone, with interbedded silt, clay and coal. Channel deposits. ||||||
30032|Clare Sandstone|68003|5|Briefly described|p38 Fig.3-j, p41, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Alluvial deposits sourced from Lachlan Fold Belt.||Unit in Coogal Subgroup.||Overlies Hoskisson Coal and Benelabri Formation. Is locally overlain by Benelabri Formation.||
30032|Clare Sandstone|68004|5|Briefly described|p23 Table 1, p176.|||Gunnedah Basin. Considered prospective for hydrocarbons. Is sealed by Trinkey Formation.||Unit in Coogal Subgroup.||Overlies Hoskissons Coal. Is adjacent to and overlies Benelabri Formation.||
30032|Clare Sandstone|70791|5|Briefly described|p277|Lopingian|Lopingian|Gunnedah Basin.||Coogal Subgroup.||||
30032|Clare Sandstone|70878|5|Briefly described|p715, p717, p724|Permian|Permian|Calibration of palynological ages (D. parvithola Zone). Other ages given.|257.33 +/- 0.57 Ma.|Black Jack Group.||Overlies Hoskissons Coal. Is overlain by Wallala Formation.||
30032|Clare Sandstone|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Overlies Hoskisson Coal. Is overlain by Wallala Formation.||
36112|Clarence River Supersuite|23439|6|Mentioned|p133|||||||||
36112|Clarence River Supersuite|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Geological Province: New England Fold Belt.||||||
36112|Clarence River Supersuite|23799|5|Briefly described|p115 Fig. 10|||Includes the Towgon, Bruxner and Duncan Suites.||||||
36112|Clarence River Supersuite|23812|6|Mentioned|p63|||||||||
36112|Clarence River Supersuite|24512|6|Mentioned|p6|||||||||
36112|Clarence River Supersuite|24513|5|Briefly described|p10-11|Early Triassic|Late Permian|Calcic and sodic, predominantly dioritc, tonalitic and granodiorite intrusive rocks; I-type granite.||||||
36112|Clarence River Supersuite|24521|5|Briefly described|p108 Fig. 2|Triassic|Permian|Trondjemitic and tonalitic rocks.||||||
36112|Clarence River Supersuite|60557|5|Briefly described|p27|||Includes the Ridgelands and Wattlebank Granodiorites and the Bouldercombe Igneous Complex.||||||09-JUN-05
36112|Clarence River Supersuite|61795|5|Briefly described|p368|Early Triassic|Late Permian|Appears to be derived from isotopically primitive lower crustal or mantle material (Bryant et al., 1997). I-type granites. Drake Volcanics amy be co-magmatic with this unit.||||||
36112|Clarence River Supersuite|62757|5|Briefly described|p1-2|Early Triassic|Late Permian|Plutonic suite of the New England Batholith.||||||07-FEB-11
36112|Clarence River Supersuite|63748|5|Briefly described|p27 Fig.27|||Includes Duncans River Trondhjemite.||||||07-FEB-11
36112|Clarence River Supersuite|63763|6|Mentioned|p14|||Part of the New England Batholith.||||||03-FEB-09
36112|Clarence River Supersuite|68005|5|Briefly described|p20, pp63-64, p135, p169 Plan 1, p170.|Early Triassic|Late Permian|Part of New England Batholith. Formerly a suite of Shaw and Flood (1982); redefined as a Supersuite by Bryant (2001). I-type. Chemically the most diverse in the New England Batholith.|||Includes Nundle Suite and Boxwell Granodiorite.||Dominantly tonalite and granodiorite, with gabbro through to monzogranite; typically fine- to medium-grained, unfractionated and moderately oxidised.|
36112|Clarence River Supersuite|68006|5|Briefly described|p20 Fig.3-A, p135, p144, p146, p155.|Early Triassic|Late Permian|New England Batholith, New England Fold Belt. Of Bryant (2001). I-type. May be favourable for porphyry copper-gold or porphyry-related gold only deposits. A constituent unit host Cu-Au vein occurrence at the Sugarloaf Prospect.|||Includes Duncans Creek Trondhjemite.|||
36112|Clarence River Supersuite|68008|5|Briefly described|p3, p332-333, p336, p492|Triassic|Permian|Shaw and Flood (1981), Bryant et al. (1997). New England Batholith. Comprises a number of different groups (described). Relatively oxidised and unfractionated; limited mineralisation potential.||||||
36112|Clarence River Supersuite|68111|5|Briefly described|p968 Tb.1, p973|Late Permian|Late Permian|Characterised by cordilleran-type mineralogy, geochemistry and isotopic signature (Bryant et al. 1997).|||Includes Barrington Tops Granodiorite, Dumbudgery Creek Granodiorite, Towgon Grange Granodiorite, Duncans Creek Trondhjemite, and Jenny Lind Granite.||Tonalitic I-type intrusions.|16-OCT-14
36112|Clarence River Supersuite|68679|5|Briefly described|p454, p457, p464-466, p470|Permian|Permian|Bryant et al. (1997); previously the Clarence River Plutonic Suite of Shaw and Flood (1981). Compositionally disparate with multiple sources: mostly arc magmatism or partial melting of juvenile, arc-derived rocks. Geochemical plots. Has some potential for arc-related mineralisation such as porphyry Cu and Cu-Au.|||Boxwell, Greymare Suites.|||
36112|Clarence River Supersuite|68822|6|Mentioned|p339|||||||||
36112|Clarence River Supersuite|69639|5|Briefly described|p1, p170, p217, p223|Cisuralian|Cisuralian|New England Orogen.|291.9 +/- 2 Ma (Cawood et al., 2011)||Includes the Kaloe Tonalite, Barrington Tops Granodiorite and the Bruxner Suite.|||
36112|Clarence River Supersuite|70217|5|Briefly described|v, p11, p17, p22, p27, p72, p73|Permian|Permian|New England Orogen. Primitive I-type geochemistry. Contains 12 I-type, isotopically primitive intrusions ranging in composition from gabbro to monzogranite. Its constituent units span an isotopic age range that exceeds 40 million years and as such the authors believe the current chemostratigraphic classification of primitive I type granites in the New England Orogen requires revision. Also includes the Kaloe Granodiorite, Gogs Top Trondhjemite, Dumbudgery Creek Granodiorite, Towgon Grange Granodiorite, Jenny Lind Granodiorite, Koreelan Creek Granodiorite, Duncans Creek Trondhjemite.    |||Includes the Nundle Suite, Mount Ephraim Suite.|||
36112|Clarence River Supersuite|70876|5|Briefly described|p2, p36, p42, p47, p53, p77-p80|Permian|Permian|New England Orogen. Also includes the Duncans Creek Trondhjemite, Gogs Top Trondhjemite, Mount Ephraim Granodiorite, Rocky Creek Granodiorite and the Kaloe Tonalite.|c. 257.5 to 246 Ma||Includes the Bruxner Suite, Jenny Lind Suite, Dumbudgery Creek Suite, Boxwell Suite, Towgon Grange Tonalite, Barrington Tops Granodiorite.|||
36112|Clarence River Supersuite|71628|4|Described|p1:11; p2:54; p6: 1-3, 6; p7:4; p8: 2-3|Early Triassic|Permian|See also p9: 1-42; p10: 1-2, 5, 7; p14: 1, 8; p17: 3, 14; p18: 1-2, 4, 8, 12, 14-15, 18, 21; p19: 24, 26, 62, 91, 94, 147-148, 176. Bryant et al. (2003) after unpublished work by Chappell and Bryant (1994). Included the Nundle Suite of Hensel et al. (1985) but with several renamings, additions and removals. Previously the Clarence River Plutonic Suite (Shaw and Flood, 1981). Redefined in this study. Contrasted with Barrington Tops Complex/Supersuite. Granites of this unit are associated with 38 Cu, Fe and base metal occurrences.|258-255 Ma (Waltenberg et al., 2016).||Dumbudgery Creek Complex; Bruxner, Mount Carnham, Jenny Lind, Towgon Grange Suites.|Intrudes Tablelands Complex (accretionary wedge).|Compositionally diverse (from gabbro to monzogranite) but typically intermediate: tonalite, diorite, granodiorite. Typically medium-grained, broadly equigranular, and speckled black-and-white. Ferromagnesian glomerophyric aggregates common. I-type.|
36112|Clarence River Supersuite|72528|5|Briefly described|p90.|Middle Triassic|Middle Triassic|Quoted age from Cullens Creek Granite.|246.7+/-1.5 Ma||Includes Cullens Creek Suite|||
36112|Clarence River Supersuite|72571|6|Mentioned|p89|||Of the Tasmanides of eastern Australia.||||||
36112|Clarence River Supersuite|73570|6|Mentioned|p918|Late Permian|Late Permian|New England Orogen.||||||
40924|Clarevale Barite Member|50234|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the De Drack Formation (Mount Fairy Group).  Off-white, grey and red-brown laminated to very thinly bedded barite with ferruginous laminae.||||||16-OCT-15
35169|Clay Bed|23055|6|Mentioned|Fig13p25|||||||||
33400|Clear Hills Monzodiorite|24417|3|Fully described|p98|Early Devonian|Early Devonian|Of Eugowra Suite.  Previously included in Eugowra Granite.||||||
33400|Clear Hills Monzodiorite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Two-pyroxene quartz monzodiorite.||||||05-JUL-04
33400|Clear Hills Monzodiorite|60009|5|Briefly described|Map Legend|Emsian|Emsian|Of the Eugowra Suite.||||||13-JUL-04
31567|Clear Range Suite|22815|6|Mentioned|p60|||||||||
31567|Clear Range Suite|42726|5|Briefly described|map legend||Silurian|||||||
31567|Clear Range Suite|43233|5|Briefly described|Map Legend||Silurian|Murrumbidgee Batholith.||||||
31567|Clear Range Suite|44093|5|Briefly described|p190 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
31567|Clear Range Suite|68592|6|Mentioned|p1225|||||Unit in Bullenbalong Supersuite.||||
25846|Clearview Limestone Member|23213|6|Mentioned|p21|||Contains Halysites praecedens in informal upper part of member. of Ballingoole Limestone.||||||
25846|Clearview Limestone Member|23214|4|Described|p39|Eastonian|Eastonian|Of Ballingoole Limestone. Age determined by fossil assembleges. Max. thickness 152m.||||||
25846|Clearview Limestone Member|32156|6|Mentioned|p233|||Refers fossil content||||||
25846|Clearview Limestone Member|33063|2|Defined|p83|Ordovician|Ordovician|||||||
25846|Clearview Limestone Member|33737|6|Mentioned|p179|||||||||
25846|Clearview Limestone Member|33740|6|Mentioned|p125|||||||||
25846|Clearview Limestone Member|35646|6|Mentioned|Fig.3|||||||||
25846|Clearview Limestone Member|38219|6|Mentioned|Table 2|||||||||
25846|Clearview Limestone Member|40127|6|Mentioned|p9|||||||||
25846|Clearview Limestone Member|40136|5|Briefly described|p17|||See also P22||||||
25846|Clearview Limestone Member|41046|6|Mentioned|Fig.2|||||||||
25846|Clearview Limestone Member|70684|6|Mentioned|p39 Fig.17|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Ballingoole Limestone.||||
76946|Clevedale Migmatite Member|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Thorndale Composite Gneiss||||15-DEC-21
76946|Clevedale Migmatite Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain. The rank [Member] is omitted.||Thorndale Composite Gneiss.||||
31725|Cliefden Caves Limestone Subgroup|13139|5|Briefly described|p9 Fig. 4|Late Ordovician|Late Ordovician|Conformably underlies the Malongulli Formation. Geological Province: Western Molong Volcanic Belt.||||||17-JUL-08
31725|Cliefden Caves Limestone Subgroup|23181|6|Mentioned|p6, Fig.2|Eastonian|Eastonian|early Eastonian.||||||
31725|Cliefden Caves Limestone Subgroup|23213|6|Mentioned|p18,19,20,22|||Periodon grandis and Taoqupognathus blandis are characterisitic conodonts of upper assemblage of subgroup.||||||
31725|Cliefden Caves Limestone Subgroup|23214|2|Defined|p39|Eastonian|Eastonian|Of Barrajin Group. Age determined by fossil assembleges. Max. thickness 460m||||||
31725|Cliefden Caves Limestone Subgroup|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
31725|Cliefden Caves Limestone Subgroup|24398|5|Briefly described|p264, p266|Eastonian|Eastonian|Geological Province: Lachlan Fold Belt.||||||
31725|Cliefden Caves Limestone Subgroup|24417|6|Mentioned|p24|||||||||
31725|Cliefden Caves Limestone Subgroup|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Barrajin Group. Consists of skeletal wackestone, packstone and grainstone; lime mudstone and siltstone, calcarenite.||||||17-JUL-08
31725|Cliefden Caves Limestone Subgroup|43782|5|Briefly described|Map Legend|Eastonian|Gisbornian|Of Barrajin Group.||||||30-JUN-08
31725|Cliefden Caves Limestone Subgroup|63278|5|Briefly described|p147 Fig. 2b, p153, p154|Eastonian|Eastonian|Geological Province: Molong Volcanic Belt, LFB. Consists of limestone. Age based on conodont faunas (Zhen amd Webby 1995). See also p154.||||||07-FEB-11
31725|Cliefden Caves Limestone Subgroup|63283|6|Mentioned|p195 Fig. 2, p199|Late Ordovician|Late Ordovician|Overlain by Malongulli Formation. Geological Province: Molong Volcanic Belt. Consists of limestone.||||||07-FEB-11
31725|Cliefden Caves Limestone Subgroup|63289|6|Mentioned|p366|Late Ordovician|Late Ordovician|Underlain by Walli Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
31725|Cliefden Caves Limestone Subgroup|63290|5|Briefly described|p410, p396 Fig. 3|Eastonian|Eastonian|Overlain by Malongulli Formation. Geological Province: Molong Volcanic Belt.||||||
31725|Cliefden Caves Limestone Subgroup|63293|6|Mentioned|p469 Fig. 2|Eastonian|Gisbornian|Overlain by Malongulli Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
31725|Cliefden Caves Limestone Subgroup|64295|5|Briefly described|p200 Fig. 2, p201|||Contains Fossil Hill Limestone. Overlain by Malongulli Formation. Lithology includes allochthonous limestones.||||||01-SEP-08
31725|Cliefden Caves Limestone Subgroup|64826|5|Briefly described|p1040 Tb. 1, p1045|Eastonian|Eastonian|Of the Barrajin Group.||||||04-MAR-09
31725|Cliefden Caves Limestone Subgroup|67322|5|Briefly described|Fig.5, p23, p24|Katian|Katian|Macquarie Arc. Modified by Krynen and Pogson, in Pogson and Watkins (1998), after Stevens (1952). Occurs in the Cliefden Caves area. Diverse fossil assemblage.||Of the Cabonne Group.|Fossil Hill Limestone, Belubula Limestone, Vandon Limestone|Correlative of the Reedy Creek Limestone, Regans Creek Limestone and Bowan Park Limestone Subgroup. Disconformably overlies the Walli Volcanics. Overlain by the Malongulli Formation.||21-FEB-18
31725|Cliefden Caves Limestone Subgroup|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
31725|Cliefden Caves Limestone Subgroup|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Post-phase 2 volcanic hiatus. Age: deposited from early to late Eastonian.|c. 455-450 Ma|Cabonne Group||||
31725|Cliefden Caves Limestone Subgroup|70684|5|Briefly described|p34, p75|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||||||
31725|Cliefden Caves Limestone Subgroup|70754|5|Briefly described|p448-451|Late Ordovician|Late Ordovician|||||Overlies ?unconformably Walli Volcanics. Is overlain by Malongulli Formation. Coeval with Reedy Creek Limestone.||
31725|Cliefden Caves Limestone Subgroup|71091|6|Mentioned|p142, p145|||||||Is overlain by Malongulli Formation.||
31725|Cliefden Caves Limestone Subgroup|73208|5|Briefly described|p869-870, 875|Late Ordovician|Late Ordovician|Globally significant: contains world's oldest known brachiopods shell beds and rugose corals.|||Vandon, Belubula, Fossil Hill Limestones.|Is overlain by Malongulli Formation.||
31725|Cliefden Caves Limestone Subgroup|73209|5|Briefly described|p879-881, 888|Late Ordovician|Late Ordovician|A richly fossiliferous shallow-water limestone succession.|||Fossil Hill, Vandon, Belubula Limestones.|Disconformably overlies Walli Volcanics. Is overlain by Malongulli Formation.||
31725|Cliefden Caves Limestone Subgroup|73210|6|Mentioned|p892-893|||Percival et al. (2011). Originally the Cliefden Caves Limestone Group of Webby and Packham (1982).|||Fossil Hill Limestone.|||14-DEC-22
31725|Cliefden Caves Limestone Subgroup|73492|5|Briefly described|p696, p702-703, p706-707|Katian|Katian|T. blandus Biozone of early Katian age in upper part (Zhen and Webby, 1995).|||Fossil Hill Limestone, Vandon Limestone|Overlies Walli Volcanics||
73522|Cliffs Tank Complex|66623|2|Defined|p194, pp224-228.|||Defined in this study. Name supersedes Barrongie Creek Ultramafic (Buckley 2002). Three outcrops in Baroorangee Creek area, Mount Wright Fault zone, Koonenberry Belt. Strong foliation (schistosity) implies pre-Delamerian Orogeny age; intruding basalt post-Delamerian. Geochemically similar to Macs Tank Ultramafic.||||Intruded by undeformed, massive porphyritic basalt with chilled margins.|Serpentinised pyroxene-olivine melange with knockers and clasts of dolerite, Kara Formation and Ponto Group rocks.|
73522|Cliffs Tank Complex|66918|5|Briefly described|Map legend|Paleozoic|Paleozoic||||||Serpentinised pyroxene-olivine melange with knockers and clasts of dolerite, Kara Formation and Ponto Group.|
73522|Cliffs Tank Complex|70650|5|Briefly described|Map Legend|Paleozoic|Paleozoic||||||Serpentinised pyroxene-olivine melange with knockers and clasts of dolerite, Kara Formation and Ponto Group.|
82388|Clive Leucomonzogranite|71628|3|Fully described|p15: 2, 25-28|Late Permian|Late Permian|New name, this study. Previously Clive Adamellite (Shaw, 1964), Clive Leucoadamellite of Flinter (1982), and later Clive Monzogranite of Henley et al. (2001) after unpublished work by Barnes (1987). The type locality is along the Woodside loop road, N of Clive (Shaw, 1964). Named after the locality of Clive. Occurs ~15 km W of Sandy Flat and ~23 km SW of Tenterfield. Resists weathering and crops out well. Geochemistry described. Hosts a silica deposit, and is associated with (but not genetically) several vein As-base metal deposits (listed).|254.6 +/- 1.4 Ma (SHRIMP: Waltenberg et al., 2015)|Clive Suite.||Intrudes Wandsworth Volcanic Group. Is faulted against Bondonga beds.|Pale buff to white, coarse-grained, equigranular biotite-(hornblende) leucomonzogranite. Banded sedimentary xenoliths and igneous xenoliths common locally. I-type.|
32327|Clonolly Ignimbrite Member|22831|3|Fully described|p 60|Pragian|Lochkovian|||||||
32327|Clonolly Ignimbrite Member|22857|5|Briefly described|p448 App.1, Tb.A1.6|Pragian|Pragian|Basal member of the Kadungle Volcanics. Fine-grained laminated ignimbrite; contains brachiopods. Max. thickness: 150m. Geological Province: Bogan Gate Terrace.||||||
32327|Clonolly Ignimbrite Member|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|Of Kadungie Volcanics. Max. thickness: 2000 m.||||||
32327|Clonolly Ignimbrite Member|44160|5|Briefly described|map legend|Lochkovian|Lochkovian|of Trundle Group.||||||
28458|Cloughers Creek Formation|24237|5|Briefly described|p6 Fig.2|Middle Triassic|Middle Triassic|Geological Province: Clarence-Moreton Basin.||||||
28458|Cloughers Creek Formation|32801|6|Mentioned|Fig.5|||||||||
28458|Cloughers Creek Formation|32803|6|Mentioned|Fig. 1|||||||||
28458|Cloughers Creek Formation|34340|3|Fully described|p459|||||||||
28458|Cloughers Creek Formation|37112|5|Briefly described|Table 1|||||||||
28458|Cloughers Creek Formation|37757|6|Mentioned|p19|||||||||
28458|Cloughers Creek Formation|60991|6|Mentioned|p40 |Middle Triassic|Middle Triassic|Contains Lepidopteris leaves: naming discussed.||Nymboida Coal Measures.||||
28458|Cloughers Creek Formation|73306|5|Briefly described|p565-566|Middle Triassic|Middle Triassic|Is mis-spelt as Coughers Creek Formation on p565.||Nymboida Coal Measures.||Is overlain by Bardool Conglomerate.||
78671|Cloyne Limestone Member|49690|5|Briefly described|Tb.4, p10-12, p16|Late Silurian|Late Silurian|Up to 150 m thick.||Of the Rothlyn Formation|||Pale, buff-grey, banded limestone and coarsely crystalline marble. Up to 150m thick|14-FEB-14
29203|Cloyne Member|40664|3|Fully described|p236|Miocene|Miocene|||||||13-JUN-13
29203|Cloyne Member|42035|5|Briefly described|Table 1 p130|||||||||14-FEB-14
27127|Clwydd Sandstone Member|33683|6|Mentioned|Table 1|||Narrabeen Gp.||||||
27127|Clwydd Sandstone Member|33685|6|Mentioned|Table 2|||||||||
27127|Clwydd Sandstone Member|34205|2|Defined|p21|Triassic|Triassic|||||||
27127|Clwydd Sandstone Member|34209|6|Mentioned|p140|||See also P141 & Table 1. Triassic.||||||
27127|Clwydd Sandstone Member|39232|6|Mentioned|p110|||||||||
27127|Clwydd Sandstone Member|39293|5|Briefly described|p145|||||||||
27127|Clwydd Sandstone Member|43360|14|Not recorded|Map Legend|||(Provisional first edition)||||||
27127|Clwydd Sandstone Member|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
27127|Clwydd Sandstone Member|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
27370|Coal Cliff Sandstone|22549|6|Mentioned|p526||Late Permian|||||||
27370|Coal Cliff Sandstone|22745|6|Mentioned|p127|||Sydney Basin.||||||
27370|Coal Cliff Sandstone|22857|5|Briefly described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Clifton Subgroup (Narrabeen Group). Medium-grained quartz-lithic sandstone. Disconformably overlies Illawarra Coal Measures. Max. thickness: ~9mm. Geological Province: Sydney Basin.||||||
27370|Coal Cliff Sandstone|23881|5|Briefly described|p69 Fig. 7.2|||Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
27370|Coal Cliff Sandstone|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Of the Narrabeen Group. Underlies: Bulli Coal Measure.||||||29-NOV-04
27370|Coal Cliff Sandstone|24342|5|Briefly described|p51|||Of Narrabeen Group. Geological Province: Sydney Basin.||||||
27370|Coal Cliff Sandstone|29901|4|Described|Table 1|||||||||
27370|Coal Cliff Sandstone|30007|6|Mentioned|p61|||||||||
27370|Coal Cliff Sandstone|31061|6|Mentioned|Table 1|||||||||
27370|Coal Cliff Sandstone|31128|6|Mentioned|Table 1|||||||||
27370|Coal Cliff Sandstone|31297|6|Mentioned|p4|||||||||
27370|Coal Cliff Sandstone|31725|6|Mentioned|p10|||On table||||||
27370|Coal Cliff Sandstone|31878|6|Mentioned|Table 1|||||||||
27370|Coal Cliff Sandstone|31884|6|Mentioned|Table 1|||Triassic||||||
27370|Coal Cliff Sandstone|31886|6|Mentioned|Table 1|||||||||
27370|Coal Cliff Sandstone|31887|5|Briefly described|p7|||||||||
27370|Coal Cliff Sandstone|32187|6|Mentioned|p4|||||||||
27370|Coal Cliff Sandstone|32801|6|Mentioned|Fig.10|||||||||
27370|Coal Cliff Sandstone|33683|4|Described|Table 1|||||||||
27370|Coal Cliff Sandstone|33685|6|Mentioned|Table 2|||||||||
27370|Coal Cliff Sandstone|33867|6|Mentioned|Table 1|||||||||
27370|Coal Cliff Sandstone|34009|6|Mentioned|p108|||Permian||||||
27370|Coal Cliff Sandstone|34058|5|Briefly described|p395|||Triassic||||||
27370|Coal Cliff Sandstone|34205|6|Mentioned|Table 6|||Correlated with part Caley Formation.||||||
27370|Coal Cliff Sandstone|34241|6|Mentioned|p404|||||||||
27370|Coal Cliff Sandstone|34336|6|Mentioned|Table 5.15|||||||||
27370|Coal Cliff Sandstone|34337|4|Described|p394|||||||||
27370|Coal Cliff Sandstone|34562|6|Mentioned|p60|||||||||
27370|Coal Cliff Sandstone|34605|5|Briefly described|p375|||||||||
27370|Coal Cliff Sandstone|36042|6|Mentioned|Fig.22|||||||||
27370|Coal Cliff Sandstone|36220|3|Fully described|p65|||See also Table 20 & p53.||||||
27370|Coal Cliff Sandstone|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Prob.Late Permian||||||
27370|Coal Cliff Sandstone|36222|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27370|Coal Cliff Sandstone|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
27370|Coal Cliff Sandstone|37089|5|Briefly described|p208|||||||||
27370|Coal Cliff Sandstone|38615|6|Mentioned|p18|||||||||
27370|Coal Cliff Sandstone|39287|6|Mentioned|Fig. 2.18|||||||||
27370|Coal Cliff Sandstone|39293|6|Mentioned|p145|||||||||
27370|Coal Cliff Sandstone|39296|6|Mentioned|Fig. 11.1|||||||||
27370|Coal Cliff Sandstone|39308|5|Briefly described|p511|||||||||
27370|Coal Cliff Sandstone|39450|6|Mentioned|Table 1|||||||||
27370|Coal Cliff Sandstone|40516|6|Mentioned|Fig.3|||||||||
27370|Coal Cliff Sandstone|42737|5|Briefly described|map legend|Permian||||||||
27370|Coal Cliff Sandstone|42896|3|Fully described|p25, Table 2|||of Clifton Subgroup||||||
27370|Coal Cliff Sandstone|42925|5|Briefly described|Table 18||Late Permian|||||||
27370|Coal Cliff Sandstone|42926|4|Described|map legend||Late Permian|||||||
27370|Coal Cliff Sandstone|45090|6|Mentioned|p71|||Narrabeen Gp.||||||
27370|Coal Cliff Sandstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
27370|Coal Cliff Sandstone|67560|6|Mentioned|p265|||See also references to Coalcliff Sandstone (p258, p260-270).||||||23-MAY-17
27370|Coal Cliff Sandstone|68202|6|Mentioned|p176|Early Triassic|Early Triassic|Bowen Basin.||Narrabeen Group.||||
27370|Coal Cliff Sandstone|73304|6|Mentioned|p61, p72, p74|||Sydney Basin, southern. End-Permian mass extinction is recognised at the base of this unit. No basal unconformity was observed.||Narrabeen Group||||
25849|Coan Granite|34449|6|Mentioned|Table 2-1|||||||||
25849|Coan Granite|37772|5|Briefly described|p8|||||||||
25849|Coan Granite|40269|4|Described|p141|||||||||
25849|Coan Granite|40913|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
25849|Coan Granite|41126|2|Defined|p85|Early Devonian|Early Devonian|||||||
25849|Coan Granite|41528|6|Mentioned|p98|||||||||
25849|Coan Granite|41821|6|Mentioned|p24|||In Mount Allen sheet area||||||
25849|Coan Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
25849|Coan Granite|43089|5|Briefly described|Map Legend|||||||||
25849|Coan Granite|43202|5|Briefly described|Table 2,p20.|||||||||
25849|Coan Granite|63891|5|Briefly described|p240|||Exposed.||||||
26259|Coando Volcanics|22857|4|Described|p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Mount Hope Group (Cobar Supergroup). Max. thickness: 300m. Geological Province: Mount Hope Trough (Darling Basin).||||||
26259|Coando Volcanics|37772|4|Described|p6|||||||||
26259|Coando Volcanics|40269|6|Mentioned|p156|||||||||
26259|Coando Volcanics|40913|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
26259|Coando Volcanics|41126|2|Defined|p25|early Lochkovian|early Lochkovian|||||||
26259|Coando Volcanics|41821|6|Mentioned|p15|||Occurs in the Mount Allen sheet area||||||
26259|Coando Volcanics|42144|6|Mentioned|Fig.3 P604|||||||||
26259|Coando Volcanics|42521|5|Briefly described|Fig.3b P16|||||||||
26259|Coando Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
26259|Coando Volcanics|43089|5|Briefly described|Map Legend|||of Mount Hope Group||||||
26259|Coando Volcanics|43202|5|Briefly described|Table 2,p20.|||||||||
26259|Coando Volcanics|69511|6|Mentioned|p6|||||||Is overlain conformably by Mount Halfway Volcanics.||
26259|Coando Volcanics|70751|6|Mentioned|p17, p19, p30|||||Mount Hope Group||||
26259|Coando Volcanics|72908|6|Mentioned|p3|||Simpson (2014) (see also Downes, Blevin et al., 2016) proposed that the stratigraphy of the Mount Hope Group be simplified, with the Ambone, Regina, Goona and part of the Coando Volcanics being grouped into the Mount Halfway Volcanics.||Mount Hope Group||||
82390|Coastal Granite Association|71628|5|Briefly described|p17: 1-103; p19: 147, 165|||New name (this study): informal, to capture a specific spatial-temporal magmatic event within the southern New England Orogen. Comprises granites <240 Ma along and E of the Demon Fault. Broadly corresponds to the Carrai Supersuite of Shaw et al. (2011). Is shortened to Coastal Association towards the end of the Chapter.|239-212 Ma.||Carrai, Glen Esk Supersuites; Dandahra Creek, Billys Creek, The Brothers, Suites; seven unaffiliated (undetermined) granites.|Intrudes Coffs Harbour and Nambucca Associations.||
77050|Coates Creek Ignimbrite Member|70297|5|Briefly described|map legend|Middle Devonian|Middle Devonian|||Dulladerry Volcanics||||
27673|Cobar Supergroup|730|5|Briefly described|p6, p7, p9, p16, p17, p18, p23, p60.||Early Devonian|Darling Basin. Turbidites, carbonates and clastics, silicic volcanics. Deformed by Tabberabberan and Kanimblan Orogenies.||||||11-NOV-14
27673|Cobar Supergroup|5252|5|Briefly described|p61, p65, p66. |Early Pragian|Pridoli|Includes Amphitheatre Group and Winduck Group. Fossils common, but isolated outcrops make stratgraphic correlation imprecise.||||||
27673|Cobar Supergroup|9548|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
27673|Cobar Supergroup|22580|5|Briefly described|p94|||||||||
27673|Cobar Supergroup|22768|5|Briefly described|p155-56,169-70||Early Devonian|||||||
27673|Cobar Supergroup|22799|5|Briefly described|p15|||Cobar Basin||||||
27673|Cobar Supergroup|22831|6|Mentioned|p 38|||||||||
27673|Cobar Supergroup|22857|4|Described|p436 App.1, Tb.A1.6, p153, p156|Early Devonian|Late Silurian|Possible correlative of Timbury Hills Formation. Max. thickness: ~7km. Geological Province: Cobar Basin (a sub-basin of the Darling Basin). See also p200.||||||
27673|Cobar Supergroup|22859|5|Briefly described|p200-01,207|Early Devonian|Late Silurian|||||||
27673|Cobar Supergroup|22887|5|Briefly described|p21, Fig.4 p11|Devonian|Devonian|Represented by correlatives of the Mount Hope Group and the Broken Range Group||||||
27673|Cobar Supergroup|22893|5|Briefly described|p11 table3|||Vague description on limited evidence as this unit completely concealed in the mapping area.||||||12-JUN-14
27673|Cobar Supergroup|23096|5|Briefly described|p602|||||||||
27673|Cobar Supergroup|23101|5|Briefly described|p567 (Fig 1)||Devonian|||||||
27673|Cobar Supergroup|23171|4|Described|p11,18-9,22,31,40|Early Devonian|Late Silurian|||||||
27673|Cobar Supergroup|23173|4|Described|Map Legend|||||||||
27673|Cobar Supergroup|23252|5|Briefly described|Map Legend|||||||||
27673|Cobar Supergroup|23309|6|Mentioned|p390|||||||||
27673|Cobar Supergroup|24019|5|Briefly described|p353|Lochkovian|Lochkovian|||||||
27673|Cobar Supergroup|24265|5|Briefly described|p1453|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
27673|Cobar Supergroup|24417|6|Mentioned|p16|||||||||
27673|Cobar Supergroup|36118|6|Mentioned|p67|||||||||
27673|Cobar Supergroup|37772|6|Mentioned|p1|||||||||
27673|Cobar Supergroup|37798|6|Mentioned|p128|||||||||
27673|Cobar Supergroup|38292|6|Mentioned|p3|||||||||
27673|Cobar Supergroup|38367|6|Mentioned|p26|||See also Fig.1||||||
27673|Cobar Supergroup|39064|6|Mentioned|p2|||||||||
27673|Cobar Supergroup|39083|6|Mentioned|p25|||||||||
27673|Cobar Supergroup|39084|6|Mentioned|Fig.1|||||||||
27673|Cobar Supergroup|39618|1|Redefined|p38|Early Devonian|Early Devonian|||||||
27673|Cobar Supergroup|39627|6|Mentioned|p263|||||||||
27673|Cobar Supergroup|40269|4|Described|p141|||||||||
27673|Cobar Supergroup|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27673|Cobar Supergroup|40676|6|Mentioned|p28|||||||||
27673|Cobar Supergroup|40913|6|Mentioned|Map legend|Pragian|Pragian|Pragian-Lochkovian||||||
27673|Cobar Supergroup|41090|6|Mentioned|p78|||||||||
27673|Cobar Supergroup|41126|6|Mentioned|p17|||||||||
27673|Cobar Supergroup|41138|6|Mentioned|Map legend|Devonian|Devonian|||||||
27673|Cobar Supergroup|41276|6|Mentioned|p73|||||||||
27673|Cobar Supergroup|41394|2|Defined|p38|Early Devonian||Mention p10.||||||20-OCT-08
27673|Cobar Supergroup|41395|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27673|Cobar Supergroup|41410|5|Briefly described|p295|||||||||18-JAN-10
27673|Cobar Supergroup|41452|6|Mentioned|Fig.1|||||||||
27673|Cobar Supergroup|41528|2|Defined|p34|Early Devonian||||||||
27673|Cobar Supergroup|41529|6|Mentioned|Map legend|Devonian||||||||
27673|Cobar Supergroup|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27673|Cobar Supergroup|41821|4|Described|p21|Early Devonian||||||||
27673|Cobar Supergroup|42144|5|Briefly described|p616|||See also Fig.1||||||
27673|Cobar Supergroup|42171|5|Briefly described|p145|||See also Table 2||||||
27673|Cobar Supergroup|42208|5|Briefly described|p304|||See also Fig.1||||||
27673|Cobar Supergroup|42408|5|Briefly described|p414|||||||||
27673|Cobar Supergroup|42456|6|Mentioned|p4|||||||||
27673|Cobar Supergroup|42521|4|Described|p13, Fig.1 p14|||||||||
27673|Cobar Supergroup|42566|3|Fully described|p40|||||||||
27673|Cobar Supergroup|42568|5|Briefly described|Map legend|Pragian|Late Silurian|||||||
27673|Cobar Supergroup|42581|6|Mentioned|p48|||||||||
27673|Cobar Supergroup|42954|6|Mentioned|p68|||||||||
27673|Cobar Supergroup|42966|6|Mentioned|p48|||||||||
27673|Cobar Supergroup|43032|3|Fully described|p27|||||||||
27673|Cobar Supergroup|43089|5|Briefly described|Map Legend|||||||||
27673|Cobar Supergroup|43090|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
27673|Cobar Supergroup|43441|6|Mentioned|24|||||||||08-JAN-10
27673|Cobar Supergroup|43757|5|Briefly described|p510||Early Devonian|||||||
27673|Cobar Supergroup|43774|4|Described|p11||Devonian|||||||
27673|Cobar Supergroup|44093|5|Briefly described|p54|Early Devonian|Silurian|Geological Province: Darling Basin.||||||
27673|Cobar Supergroup|44188|6|Mentioned|Map Legend|Late Devonian|Early Devonian|Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Fine-grained sandstone, bimodal silty and coarse pyritic quartz sandstone, dolomitic veins and calcite; pyritic siltstone, pyritic micaceous shale with slatey cleavage.||||||15-MAY-08
27673|Cobar Supergroup|44191|6|Mentioned|Map Legend|Early Devonian|Early Silurian|||||||
27673|Cobar Supergroup|46900|4|Described|p15|||Consists of Nurri and Kenmure Groups, folding discussed P16.||||||
27673|Cobar Supergroup|46974|6|Mentioned|p73|||||||||
27673|Cobar Supergroup|49012|5|Briefly described|p8|||||||||
27673|Cobar Supergroup|50095|6|Mentioned|p130|||Contains Amydrotaxis druceana. (conodont). NSW.||||||11-FEB-08
27673|Cobar Supergroup|50554|5|Briefly described|Map legend|Devonian|Silurian|Includes the Euglo Formation.||||||21-JUN-04
27673|Cobar Supergroup|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geological Province: Cobar Basin.||||||
27673|Cobar Supergroup|61311|6|Mentioned|p42|||Outside the eastern margin of the Darling Basin.||||||
27673|Cobar Supergroup|61314|5|Briefly described|p120|Early Devonian|Early Devonian|Fine-grained marine facies. Geological Province: Murray Basin.||||||
27673|Cobar Supergroup|61964|5|Briefly described|p61|Early Devonian|Late Silurian|Supersedes the "Cobar Series", "Cobar Group", and Cobar Super-Group. Overlies the Wagga Group.||||||
27673|Cobar Supergroup|62035|6|Mentioned|p31|||||||||
27673|Cobar Supergroup|62367|5|Briefly described|p10|Pragian|Lochkovian|Includes Mount Hope Group. Geological Province: Cobar Basin.||||||31-MAY-06
27673|Cobar Supergroup|63185|5|Briefly described|p3|Early Devonian|Late Silurian|Includes Kopyje Group.||||||12-APR-07
27673|Cobar Supergroup|64681|5|Briefly described|p3 Fig. 1, p5|Devonian|Silurian|||||||
27673|Cobar Supergroup|64962|5|Briefly described|p202|Early Devonian|Early Devonian|Partly overlain by Mulga Downs Group.||||||08-APR-09
27673|Cobar Supergroup|65384|6|Mentioned|S105, S113|||||||||
27673|Cobar Supergroup|65469|6|Mentioned|p21, p22|||Cobar Basin, Lachlan Orogen. |||Includes the Winduck Group.|||
27673|Cobar Supergroup|67322|6|Mentioned|p19, p39|||Now includes the Merrere Conglomerate Member (previously of the Ballast Formation) (Glen et al. 2010).|||Merrere Conglomerate|||
27673|Cobar Supergroup|67416|5|Briefly described|p83, p85|Early Devonian|Late Silurian||||Cobar, Kopyje Groups.||Sediments and volcanics.|
27673|Cobar Supergroup|68069|5|Briefly described|Map legend.|Devonian|Devonian|Shown on cross-sections and time-space plot and basement interpretation only. Lachlan Orogen. Correlatives mapped.|||||Quartzose shallow marine sedimentary rocks.|
27673|Cobar Supergroup|68297|6|Mentioned|p190||||||Said to include Amphitheatre Formation|||
27673|Cobar Supergroup|68298|5|Briefly described|p223|||Marine. Containing conodont faunas, but apparently lacking Polygnathus. Probably older (pre-Emsian) than any Polygonathus zone (see Pickett, 1980; Pickett and McClatchie, 1991; Sherwin, 1991).|||Includes Winduck Group|Is overlain by Mulga Downs Group.||12-JUN-14
27673|Cobar Supergroup|68823|5|Briefly described|p376 Fig.3, p377, p383, p385, p399-404|Devonian|Early Devonian|Cobar Basin. Thompson Orogen. Deposited in rift-related basins.|||Includes the Kopyje and Winduck Groups.|Underlies Mulga Downs Group.|Turbidites.|
27673|Cobar Supergroup|69002|6|Mentioned|p3, p11, p14, p15, p16, p17|Early Devonian|Early Devonian||||Includes the Mount Merrere Conglomerate.|||
27673|Cobar Supergroup|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian||||Includes Kopyje Group.|||
27673|Cobar Supergroup|69095|5|Briefly described|Map legend|Early Devonian|Late Silurian||||Includes Kopyje Group.|||
27673|Cobar Supergroup|69511|6|Mentioned|p6||||||Mount Hope Group.|||
27673|Cobar Supergroup|69541|6|Mentioned|p644 Fig.1(a), p654|||Central northern Lachlan Orogen.|||Includes Winduck Group.|||
27673|Cobar Supergroup|69635|5|Briefly described|p75, 120, 69|Early Devonian|Late Silurian||||Includes Kopyje Group.|||
27673|Cobar Supergroup|69801|6|Mentioned|p1, p11|||Cobar Basin.|||Includes the Kopyje Group.|||
27673|Cobar Supergroup|70602|6|Mentioned|p66 Fig 2, p67,75 Fig 11|Early Devonian|Silurian|Misspelt as Cobar Super Group p66 Fig2.|||Includes Winduck Group, Amphitheatre Group, Kopyje Group.|||
27673|Cobar Supergroup|70718|5|Briefly described|p20, p43, p102|Early Devonian|Early Devonian|Darling Basin. A deep to shallow marine depositional environment is interpreted for this supergroup. Intersected by Booligal-2.|||Includes the Amphitheatre Group, Winduck Group and Mulga Downs Group.|||
27673|Cobar Supergroup|70751|5|Briefly described|p11-p12, p25, p28|Early Devonian|Late Silurian|A distinct hiatus occurs between the lower and upper parts of this supergroup to the east of the Cobar Basin.|||Includes the Amphitheatre Group, Mount Hope Group, Mouramba Group, Rast Group, Kopyje Group.|Overlies the Girilambone Group.||
27673|Cobar Supergroup|70821|5|Briefly described|p9, p11, p13, p28|Devonian|Late Silurian|Electrical conductivity depends on the amount of pyrite and carbon contained in the rocks.|||Amphitheatre, Winduck, Kopyje and Nurri Groups; CSA Siltstone.||Metasedimentary rock sequences of deep-water turbidites (Amphitheatre Group) and shelf facies (Winduck, Kopyje Groups), and sandstone-dominated Nurri group. Typically non-magnetic.|
27673|Cobar Supergroup|70828|5|Briefly described|p4,17|Early Devonian|Late Silurian||||Includes Baledmund Formation.|||
27673|Cobar Supergroup|70876|5|Briefly described|p1, p9, p16, p76|||Lachlan Orogen.|||Includes the Kopyje Group and the Amphitheatre Group.|||
27673|Cobar Supergroup|70941|6|Mentioned|pviii, pix, p7 fig 3||Late Silurian|Name derived from the town of Cobar. In part equivalent to the old Cobar Group. Cobar Basin. Deformed by Cobar deformation event (producing S4 fabrics in the map area). The Meryula Formation (of the Kopyje Group) is estimated to be 1100m thick in the map area. Coronga Peak Quartzite is estimated at 450m thick. Deposited in nearshore shallow marine environment (in the map area). Age derived from fossil assemblage.  Structure, fossil assemblage and geophysical characteristics also discussed.Minor gold and base metal mineralisation is associated with the supergroup, contact with Girilambone group may be prospective for mineralisation. See also p8 fig 4, p9, p47, p76-p79, p85, p88, p94, p111, p117, p135, p137-p140, p143-p145, p147.|||Kopyje Group|Unconformably overlies (or is faulted against) Ballast Formation. Unconformably overlies the Girilambone Group.|Upwards fining sequence of cobble conglomerates, pebbly sandstone to siltstone and fine grained sandstone. Quartzite interfingers with conglomerate at its base.|
27673|Cobar Supergroup|71039|6|Mentioned|p6, p8, p24, p35|||||||||09-MAR-23
27673|Cobar Supergroup|71040|6|Mentioned|p6|Lochkovian|Pridoli|Cobar Basin.||||||
27673|Cobar Supergroup|71285|5|Briefly described|p539, p551-552|Early Devonian|Late Silurian|Cobar Basin.|||Nurri, Amphitheatre Groups.|||
27673|Cobar Supergroup|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian||||Kopyje, Amphitheatre and Winduck Groups.|||
27673|Cobar Supergroup|71693|5|Briefly described|Map legend.|Devonian|Devonian||||Kopyje, Mouramba, Rast, Broken Range, Mount Hope, Nurri, Amphitheatre, Winduck, Walters Range Groups; Tarran Volcanics.|||
27673|Cobar Supergroup|71965|5|Briefly described|p894,896,898,900-904,914|Early Devonian|Silurian|Geological province: Lachlan Orogen. ||||Underlain by Girilambone Group.||
27673|Cobar Supergroup|72080|5|Briefly described|p4, p6, p9, p12-p13|Early Devonian|Late Silurian|Deformed in Middle or Late Devonian.|||Includes the Kopyje Group.|Overlies the Girilambone Group.||07-JAN-22
27673|Cobar Supergroup|72083|5|Briefly described|p35-36|Devonian|Silurian|Deformed in Early Devonian: ?Bindian Orogeny; discussed.|||Square Head Formation, Yarra Yarra Group, Mineral Hill Volcanics, Talingaboolba Formation.|||
27673|Cobar Supergroup|72296|5|Briefly described|ix, p6, p21, p59|Devonian|Late Silurian|Does not occur in the Coolabah 100K sheet area.|||Kopyje Group, Doradilla Formation.|||
27673|Cobar Supergroup|72914|6|Mentioned|p5|||Map symbol suggests Devonian age.||||||
27673|Cobar Supergroup|72951|6|Mentioned|p1010|Devonian|Silurian|||||||
27673|Cobar Supergroup|72958|6|Mentioned|p10, p11, p37, p52, p60|||Cobar Basin. Nymagee area.|||Includes Mouramba Group, Kopyje Group, Rast Group, Amphitheatre Group, Mount Hope Group, Yarra Yarra Creek Group|||
27673|Cobar Supergroup|73174|4|Described|p1035-1039, p1046|Lochkovian|Lochkovian|Cobar Basin. Occurs mostly west of the Rookery Fault. Includes a syn-rift phase characterised by coarse-grained outwash fans grading into fine-grained turbidites, and a sag phase characterised by siltstones, with shallow marine sedimentary rocks that extended onto shelfs around the basin margins. Age is supported by fossil data including conodont and brachoiopod assemblages, although age-diagnostic fossils are rare in the basin. [Article includes conflicting information about the age range of this unit]. Similarity of combined detrital zircon spectra suggests constituents are of a single depositional system.|419-411 Ma||Kopyje Group, Nurri Group, Amphitheatre Group, Winduck Group and units within.||Overwhelmingly consists of sedimentary facies over volcanic facies.|22-NOV-22
27673|Cobar Supergroup|73578|6|Mentioned|p4, p11, p18, p25||||||Amphitheatre Group, Nurri Group|||
31492|Cobargo Suite|22606|6|Mentioned|P829|||||||||
31492|Cobargo Suite|22815|5|Briefly described|p65|Early Devonian|Late Silurian|||||||
31492|Cobargo Suite|22878|6|Mentioned|p83|||||||||
31492|Cobargo Suite|24514|6|Mentioned|p31|||Geological Province: Lachlan Fold Belt.||||||04-MAY-05
31492|Cobargo Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Cobargo Supersuite.  Includes the Coolagolite, Cobargo, Quaama and Murrabrine granites (informal names).||||||09-FEB-05
31492|Cobargo Suite|43233|5|Briefly described|Map Legend|||of Bega Batholith.||||||
31492|Cobargo Suite|44093|5|Briefly described|p222 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
31492|Cobargo Suite|72571|6|Mentioned|p101|||||||||
31492|Cobargo Suite|73264|6|Mentioned|p1405|||Lachlan Orogen. I-type suite.||||||
31492|Cobargo Suite|73514|6|Mentioned|p8|||Lachlan Fold Belt.|||||I-type.|
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.|
77257|Cobbora Formation|68004|5|Briefly described|p44 Table 3.|Early Permian|Early Permian|Gilgandra Sub-basin, Gunnedah Basin.||||Is overlain by Goondi Formation.|Conglomerate, breccias, arkose sandstone, coaly siltstone, mudstone.|
83330|Cobbys Corner Member|73136|5|Briefly described|p193|Upper Pleistocene|Upper Pleistocene|Lord Howe Island, west coast. Part of alloformation N2. May have been deposited during an interstadial, perhaps marine oxygen isotope stage 5a. [Written as Cobbys Corner member on p192, and Cobby's Corner Member on p198].|0.1-0.08 Ma thermoluminescence|Neds Beach Formation||Equivalent[?] to Middle Beach Member.|Volcanic-rich eolianite unit [dune?].|22-NOV-22
83330|Cobbys Corner Member|73554|4|Described|Map legend, back of map|Quaternary|Quaternary|Lord Howe Island. Well exposed in road cuts near the golf course.||Neds Beach Formation|||Yellow-brown, volcanic-rich calcarenite, displaying well developed medium- to large-scale cross-bedding.|
27372|Cobra Formation|22768|6|Mentioned|p177|||||||||
27372|Cobra Formation|22857|4|Described|p177, p480 App.1 Tb.A1.6|Early Devonian|Late Silurian|Of the Taralga Group. Shale, limestone, mudstone, basal breccia-conglomerate, rare keratophyre. Max. thickness: 500m. Geological Province: Murruin Basin.||||||03-MAR-06
27372|Cobra Formation|32999|3|Fully described|p20|||||||||
27372|Cobra Formation|34481|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27372|Cobra Formation|37727|4|Described|p87|||||||||
27372|Cobra Formation|40328|3|Fully described|p187|||||||||
27372|Cobra Formation|40821|6|Mentioned|p45|||||||||
27372|Cobra Formation|61892|5|Briefly described|p199-200, p202 Fig.2, p203-206, p209|Late Silurian|Late Silurian|See also p214, p218, p221. Murruin Creek area. Brachiopod and conodont faunas listed and described in detail. Includes the first Late Silurian linguliformean brachiopods documented from eastern Australia. ~670m thick. ?Mid-Wenlock to mid-Ludlow.||Basal Taralga Group.||Overlies the Burra Burra Creek Formation. Is overlain conformably by the Argyle Formation or Whipbird Creek Formation.|Interbedded fine-grained micrites, siltstones and limestones.|
27372|Cobra Formation|63633|5|Briefly described|Map Legend|Ludlovian|Ludlovian|Of Taralga Group. Shale, black shale limestone, silty shale, mudstone, keratophyre (rare), basal breccia conglomerate.||||||
27372|Cobra Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Marl interbedded with limestone and limestone breccia, calcareous siltstone with shelly detritus on bedding planes, siliceous siltstone+mudstone; minor porhyritic rhyolite with peperite (intrusive hyaloclastite); 2 subunits...||||||09-SEP-08
27372|Cobra Formation|68592|1|Redefined|p326, p725-7, p731, p746, p749, p752-9|Ludlow|Wenlock|See also p810, p813, p834, p887-90, p924, p1887. Retained in a form close to original definition (Scheibner 1973) after Jongsma (1968). Age range: fossils suggest mid Wenlock - early Ludlow. Upper part of Cobra Formation (as mapped by Scheibner, 1973), now considered to be part of overlying Kerrawary Siltstone. Conglomeratic base of Cobra Formation (Scheibner 1973), now defined as separate unit, Shivering Conglomerate. Note: Cobra Formation as defined herein includes both Cobra Formation and Whipbird Creek Formation sections measured by Scheibner (1973; fig. 12); detailed palaeontological sampling (Valentine et al. 2006), emphasis on conodonts, at type area. Fossil fauna listed. Thickness: ~550 m at composite type section. Mostly occupies lower, deeply incised, terrain. A massive limestone (~middle of type section) implies marked change in palaeoenvironment. Subsiding seafloor depositional environment, with a change to black graptolitic silts in the overlying Kerrawary Siltstone. Is overlain (diachronous or laterally interbedded) by Kerrawary Siltstone.||Unit in Mount Fairy Group.||Unconformably overlies and is faulted against Bendoc Group; conformably overlies Shivering Conglomerate. Is overlain conformably by Kowmung, Covan Creek and Argyle Formations.|Includes basal limestones, well-laminated siltstones; unnamed units: autochthonous and allochthonous limestone (plus limestone breccia); and, porphyritic, flow-banded rhyolite and peperite (angular rhyolite clasts in massive black mudstone matrix)|09-SEP-16
27372|Cobra Formation|70192|5|Briefly described|Map Legend|Lochkovian|Wenlock|Sfr. Includes two unnamed sub units; autochthonous-allochthonous limestone blocks and limestone breccia, Massive-flow banded quartz-feldspar-phyric rhyolite intrusion with peperite at margins. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group|Includes two unnamed members|Interleaves with and underlies Covan Creek Formation and Kerrawary Siltstone. Underlies Kowmung Formation. Overlies Shivering Conglomerate.|Massive pyritic mudstone, medium bedded marl and thinly bedded-laminated siltstone and shale. Flaggy, fine grained siliceous sandstone; 1-5cm calcareous, fossiliferous bands in fine grained rock; minor limestone, limestone breccia, rhyolite.|
27372|Cobra Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed sub units; autochthonous-allochthonous limestone blocks and limestone breccia, Massive-flow banded quartz-feldspar-phyric rhyolite intrusion with peperite at margins.||Mount Fairy Group|Includes two unnamed members||Massive pyritic mudstone, medium bedded marl and thinly bedded-laminated siltstone and shale. Flaggy, fine grained siliceous sandstone; 1-5cm calcareous, fossiliferous bands in fine grained rock; minor limestone, limestone breccia, rhyolite.|
27372|Cobra Formation|71069|5|Briefly described|p133, p135, p138 fig 44, p146, p170|||Up to 200m thick. ||Mount Fairy Group||Conformably overlain by the Covan Creek Formation. Overlain by the Kerrawary Siltstone or Kowmung Formation. Overlies the Shivering Conglomerate. Part equivalent to the De Drack Formation.|Marl, limestone and fossiliferous siltstone.|
27372|Cobra Formation|71656|4|Described|p13 Fig.2, p28, p30|Ludlow|Wenlock|Diverse fauna of linguliformean brachiopods and conodonts from the type section of the Cobra Formation in Murruin Creek near Taralga.||Mount Fairy Group||Mount Fairy Group. Partially overlies Shivering Conglomerate and partially equivalent to Kerrawary Siltstone. Partially underlies Longreach Volcanics.|Largely undisturbed bedding plane assemblages.|
23494|Cockabutta Creek Sandstone Member|22578|6|Mentioned|p398|||of Glen Davis Formation||||||
23494|Cockabutta Creek Sandstone Member|22857|5|Briefly described|p526 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Glen Davis Formation (Illawarra Coal Measures). Quartz-lithic coarse-grained sandstone, fines upwards. Max. thickness: 10m. Geological Province: Sydney Basin.||||||
23494|Cockabutta Creek Sandstone Member|42657|3|Fully described|p80|||of Glen Davis Formation.||||||
23494|Cockabutta Creek Sandstone Member|68004|5|Briefly described|p60 Table 6, p61.|Late Permian|Late Permian|Western Coalfield.||Unit in Glen Davis Formation.||||
40947|Cockatoo Point Limestone Member|50230|4|Described|Map legend|Emsian|Emsian|Of the Taemas Limestone (Murrumbidgee Group).  Overlies the Bloomfield Limestone Member; underlies Receptaculities Limestone Member.  Crinoidal limestone.||||||
40947|Cockatoo Point Limestone Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Taemas Limestone (Murrumbidgee Group). Crinoidal limestone.||||||
40947|Cockatoo Point Limestone Member|68592|2|Defined|p982, p984 Fig.162, p985, p1021, p1899|Emsian|Emsian|New name, after a promontory in Lake Burrinjuck. Refers to a thin, laterally discontinuous marker horizon of crinoidal limestone which had been included in either the Receptaculites Limestone Member or Bloomfield Limestone Member. Type locality described. Thickness to 4 m. May represent a major storm event. Contains abundant crinoid stems and ossicles, and lesser numbers of corals, stromatoporoids and brachiopods; no conodonts. Early Emsian age from confining Members.||Unit in Taemas Limestone.||Conformably overlies Bloomfield Limestone Member. Is overlain conformably by Receptaculites Limestone Member.|Blue-grey, massive, medium-bedded crinoidal limestone.|
40947|Cockatoo Point Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmtk. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Taemas Limestone||Overlies Bloomfield Limestone Member. Is overlain by Receptaculites Limestone Member.|Blue-grey, massive, medium bedded, crinoidal limestone.|
40947|Cockatoo Point Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, massive, medium bedded, crinoidal limestone.|
40947|Cockatoo Point Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, massive, medium bedded, crinoidal limestone.|
40947|Cockatoo Point Limestone Member|71656|5|Briefly described|p12 Fig.2, p35|Emsian|Emsian|Member only recently described (1985) includes lungfish fossils. Age inferred from overlying and underlying units.||Of Taemas Limestone, Murrumbidgee Group||Overlies Bloomfield Limestone Member and underlies Receptaculites Limestone Member.|Fossiliferous limestone.|
80115|Cocketgedong Member|69798|5|Briefly described|p4 Fig.2, p11-12, p15-19|Early Permian|Early Permian|New name; used here to replace the informal "Jerilderie sandstone" of the Urana Formation, thereby avoiding confusion with the Jerilderie Formation. Oaklands Basin. Seismic profiles. Good reservoir rocks.||Urana Formation.||||06-FEB-18
40952|Cocomingla Complex|50231|5|Briefly described|Map Legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
40952|Cocomingla Complex|64238|5|Briefly described|Map legend|Silurian|Silurian|Grey-green, medium- coarse-gr., porphyritic hornblende-pyroxene gabbro + quartz monzograbbro; grey, fine- to medium-gr., equigranular, quartz monzodiorite; greenish-grey, fine- to med.-gr., porphyritic, quartz monzonite. Low K and Th radioelement response||||||16-JUN-08
40952|Cocomingla Complex|68592|3|Fully described|p263, p1379-80, p1382-3, p1385-9|Late Silurian|Late Silurian|New name, after Cocomingla Parish. Mapped by Stevens (1955) as an un-named basic body in the Wyangala Batholith. Named Cocomingla Gabbro by Chappell et al. (1991). Here renamed to reflect its diversity of lithologies. Type area described. Geochemistry and geophysical properties detailed. Not isotopically dated; age from Wyangala Batholith.||||Intrudes Wyangala Granite. Is intruded by Briarlee Granite.|Grey-green, medium- to coarse-grained, porphyritic, hornblende-pyroxene gabbro and quartz monzogabbro; grey, fine- to medium-grained, equigranular quartz monzodiorites; greenish grey, fine- to medium-grained, porphyritic quartz monzonite. I-type.|
40952|Cocomingla Complex|70192|5|Briefly described|Map Legend|Lochkovian|Ludlow|Sxc. Ungrouped Silurian intrusion. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||||Medium-coarse grained, porphyritic, hornblende-pyroxene gabbro and quartz monzogabbro; fine to medium grained, equigranular, quartz monzodiorite; fine-medium grained, porphyritic quartz monzonite.|
40952|Cocomingla Complex|70545|5|Briefly described|Map Legend|Silurian|Silurian||||||Medium-coarse grained, porphyritic, hornblende-pyroxene gabbro and quartz monzogabbro; fine to medium grained, equigranular, quartz monzodiorite; fine-medium grained, porphyritic quartz monzonite.|
70478|Coeypolly Conglomerate Member|62095|5|Briefly described|p255|||Boulder conglomerate in basal region of Currabubula Formation originally informally named by Carey (1937) as Porphyry Boulder Horizon but later replaced by Voisey and Williams (1964).Current mapping does not recognise this as a discrete, mappable member.||||||25-MAY-06
70478|Coeypolly Conglomerate Member|65902|5|Briefly described|p202, 204|||Formerly Coeypolly Conglomerate (Voisey and Williams 1964); reduced to Member rank (of Currabubula Formation) in this paper. See also misspelt Coepolly Conglomerate Member. Represents a hiatus between Merlewood and Currabubula Formations.||||||09-MAR-12
38341|Coffs Harbour Association|23763|5|Briefly described|p543 Fig. 1|Permian|Carboniferous|Geological Province: New England Fold Belt.||||||
38341|Coffs Harbour Association|60937|6|Mentioned|p423 Fig. 1a|||Geological Province: New England Fold Belt.||||||
38341|Coffs Harbour Association|61003|5|Briefly described|p224|Carboniferous|Devonian|Informal name. Part of the Tablelands Complex of Korsch (1977).||||||
38341|Coffs Harbour Association|61805|6|Mentioned|p436|||Geological Province: New England Orogen.||||||17-NOV-08
38341|Coffs Harbour Association|69639|6|Mentioned|p100, p106, p139, p224|Westphalian|Tournaisian||||Includes the Moombil Siltstone and Coramba Formation.|||
38341|Coffs Harbour Association|71280|6|Mentioned|p402, p413|||New England Orogen.|||Girrakool Beds.|||
38341|Coffs Harbour Association|71628|5|Briefly described|p2:7; p3: 5, 44; p11: 16, 20; p13:24|Carboniferous|Carboniferous|See also p14: 3, 22; p15: 5, 12, 15; p17: 1, 4, 13, 28, 68, 93. RELATED UNITS (continued): Is also intruded by Guy Fawkes Granodiorite, Deepwater Syenogranite, Glen Garry Microleucosyenogranite, Dandahra Creek Suite and Hillgrove Supersuite.|||Brackendale Metamorphics, Agnes Greywacke, Coramba beds, Cunglebung Creek beds, Gundahl Complex.|Is intruded by the Apsley River and Billygoat Hill Complexes, Mount Mitchell Monzogranite, Billyrimba Leucomonzogranite, Red Range Microleucogranite. See COMMENTS for more.|Volcanic greywacke, siliceous siltstone, and pelites.|
38341|Coffs Harbour Association|73487|6|Mentioned|p563, p574 Fig.8|||||||||
24857|Coggan Coal|42657|6|Mentioned|p75|||Bylong area. Informal name?||||||
70480|Cohens Gully Ignimbrite Member|62095|2|Defined|p277 Appdx.|Late Carboniferous|Late Carboniferous|Of Currabubula Fm. Unwelded pink, green or red ignimbrite; distinguishable by its abundant biotite. Overlies Murrurundi Ignimbrite Member; underlies Rockford Ignimbrite Member. Age: probably Westphalian. Thickness: 70m in type section.||||||25-MAY-06
25851|Coila Basalt|22477|5|Briefly described|p175||Oligocene|||||||
25851|Coila Basalt|22815|5|Briefly described|p116|Oligocene|Oligocene|K/Ar Age: 29.1Ma.||||||
25851|Coila Basalt|23349|6|Mentioned|252|Oligocene|Oligocene|||||||
25851|Coila Basalt|29746|2|Defined|p2|middle Oligocene|middle Oligocene|||||||
25851|Coila Basalt|32129|6|Mentioned|p7|||Refers Bembrick (1972)||||||
25851|Coila Basalt|32673|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25851|Coila Basalt|35289|3|Fully described|p43|||Definition refers Bembrick 1972.||||||
25851|Coila Basalt|36411|6|Mentioned|p268|||Refers Chalker & Bembrick 1977 for definition.||||||
25851|Coila Basalt|73581|6|Mentioned|p22|Oligocene|Eocene|South Coast Volcanic Province. Outcrops 16 km south of Batemans Bay. Maximum thickness of 33 m. K-Ar ages from Wellman and McDougall (1974b).|35.0-28.7 Ma K-Ar|||||
23496|Collingullie Granite|22508|6|Mentioned|p13, map||| Lachlan Fold Belt||||||
23496|Collingullie Granite|22638|3|Fully described|p52|||Probably Late Silurian.||||||
23496|Collingullie Granite|23721|5|Briefly described|Map Legend|Silurian|Silurian|||||||
23496|Collingullie Granite|24119|5|Briefly described|p3|Silurian|Silurian|||||||
23496|Collingullie Granite|42726|5|Briefly described|map legend|Silurian||||||||
23496|Collingullie Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
23496|Collingullie Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
23496|Collingullie Granite|69371|6|Mentioned|p9, p14|Silurian|Silurian|||||||
23496|Collingullie Granite|69801|5|Briefly described|p2, p4-p5, p59-63, p137|Devonian|Early Devonian|Central Lachlan Orogen. Occurs west of Wagga Wagga.  Sample locality, petrography, SHRIMP analyses and interpretation are detailed. This unit is the sole member of the Collingullie Suite. SHRIMP age provided is interpreted as the magmatic crystallisation age.|415.4 +/- 2 Ma (SHRIMP)|Collingullie Suite||Intrudes the Wagga Group.|S-type, coarse-grained feldspar-porphyritic, biotite granitic rocks.|
23496|Collingullie Granite|70777|5|Briefly described|p81|Lochkovian|Lochkovian|Lachlan Orogen.|415.4 +/- 2.0 (Bodorkos et al., 2015)|||||
23496|Collingullie Granite|71889|4|Described|p7, p13-p15, p34-p38, p67|||Extensive exposure occurs in Guttlers Pit south of the Murrumbidgee River strongly resemble Collingullie Granite described by Trigg (2017) and Warren et al. (1995). Rocks previously assigned to the Bullenbung and French Park granites appear to be a part of the Collingulle Granite (present study).|||||Granite cut by steeply dipping aplitic and pegmatitic veins with some clusters of tourmaline.|
23496|Collingullie Granite|72083|5|Briefly described|p7-8, p13-16, p41, p58 Fig.9|||Formally defined by Warren et al. (1995). Here considered to include the Galore Granite, and possibly the Bullenbung granite, of Chappell et al. (1991). See also Collingullie granite (p7, p17, p39).|415.4 +/- 2.0 Ma (Bodorkos et al. in prep.)||||Medium- to coarse-grained feldspar-porphyritic granite.|
23496|Collingullie Granite|72084|5|Briefly described|p2, p6 Fig.5a, p8, p28 Fig.30, p44-48|Early Devonian|Early Devonian|Geochemical plots. Metamorphic petrography [in Wagga Group] detailed; several photomicrographs.|415.4 +/- 2 Ma (Bodorkos et al., 2015).|||Intrudes Wagga Group.|Inequigranular, medium- to coarse-grained granite with quartz grains to 7mm and stubby feldspar crystals to 25mm.|
31562|Collingullie Suite|42726|5|Briefly described|map legend||Silurian|||||||
31562|Collingullie Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
31562|Collingullie Suite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
31562|Collingullie Suite|69801|6|Mentioned|p59|||Central Lachlan Orogen.|||Includes the Collingullie Granite.|||
26486|Collinswood Granite|42726|5|Briefly described|map legend|Early Devonian||Reserved as Collinswood 1975. NLR 1988, but now publ.||||||
79332|Collygra Coal Member|70791|5|Briefly described|p275, p283-284, p286-287, p293|Cisuralian|Cisuralian|New name. Mullaley Sub-basin. 0.5-3m thick; two splits. Borehole cross-sections and long-sections; correlations. Coal properties not described. In situ coal estimates. Appears also as Colygra on p293.||||||
31561|Columba Suite|42726|5|Briefly described|map legend||Carboniferous|||||||
73422|Comarto Basalt|66623|2|Defined|p194, pp224-225, pp228-229.|||Defined in this study. Koonenberry Belt. Several outcrops, broken into small joint blocks. Pyroclastic tuff-breccia implies proximal explosive event. Lack of deformation implies post-Delamerian age; time-correlative with Macs Tank Ultramafic.|||||Nested basaltic vents with rare gabbroic intrusions; metabasalts, pyroclastic rocks and intrusive metadolerites; porphyritic, ophitic and pyroclastic igneous textures are preserved.|
69665|Come By Chance Formation|61155|5|Briefly described|p19|Late Pliocene|Early Pliocene|Overlain by Warrend Formation. Age: 3.5-2.0Ma. Thickness: 19m. In the Walgett area.||||||
25853|Comerong Volcanics|12185|5|Briefly described|map legend|Upper Devonian|Upper Devonian|Rhyolite, rhyolite breccia, basalt, shale, sandstone, conglomerate. Underlies Merrimbula Formation. BMR map symbol: Duc.||||||
25853|Comerong Volcanics|22761|6|Mentioned|p355|||Geological Province - Lachlan Fold Belt.||||||
25853|Comerong Volcanics|22815|2|Defined|p90,91,92 fig28|Devonian|Devonian|||||||
25853|Comerong Volcanics|22857|4|Described|p213-214, p496 App.1 Tb.A1.7|Late Devonian|Middle Devonian|Equivalent of Yalwal volcanics in the north. Max. thickness: ~300m. Geological Province: Lambie Basin. See also p202.||||||
25853|Comerong Volcanics|22859|6|Mentioned|p202,213-14|||||||||
25853|Comerong Volcanics|23549|6|Mentioned|p528|||Mentioned only as stratigraphical nomenclature example.||||||05-APR-05
25853|Comerong Volcanics|24040|5|Briefly described|p477|Middle Devonian|Middle Devonian|Associated with a dyke swarm along the NSW south coast.||||||21-AUG-08
25853|Comerong Volcanics|24116|6|Mentioned|p4|||||||||
25853|Comerong Volcanics|24334|5|Briefly described|p48 Tb.1|Frasnian|Givetian|Age: 370 - 379 Ma.||||||
25853|Comerong Volcanics|24346|5|Briefly described|p98|Late Devonian|Late Devonian|||||||
25853|Comerong Volcanics|24424|5|Briefly described|p539 Tb.4|Middle Devonian|Middle Devonian|Age: 372-376 Ma. Palaeomagnetic poles given.||||||
25853|Comerong Volcanics|24456|6|Mentioned|p327|||Informal name.||||||26-NOV-04
25853|Comerong Volcanics|24580|5|Briefly described|p829|Late Devonian|Middle Devonian|Overlain by the Merrimbula Group. Geological Province: Eastern Lachlan Fold Belt.||||||
25853|Comerong Volcanics|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
25853|Comerong Volcanics|29994|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25853|Comerong Volcanics|30735|4|Described|p48|||||||||
25853|Comerong Volcanics|30736|6|Mentioned|Map legend|Devonian|Devonian|||||||
25853|Comerong Volcanics|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
25853|Comerong Volcanics|31161|5|Briefly described|PA8|||||||||
25853|Comerong Volcanics|31993|6|Mentioned|p681|||||||||
25853|Comerong Volcanics|32126|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Prob.Middle Devonian||||||
25853|Comerong Volcanics|32127|4|Described|p249|||Refers Best et al. (1964)||||||
25853|Comerong Volcanics|32129|3|Fully described|p3|||||||||
25853|Comerong Volcanics|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25853|Comerong Volcanics|32672|6|Mentioned|p673|||||||||
25853|Comerong Volcanics|33325|5|Briefly described|Table 5|||? U.Dev.||||||
25853|Comerong Volcanics|34059|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25853|Comerong Volcanics|35248|6|Mentioned|p236|||||||||
25853|Comerong Volcanics|39028|6|Mentioned|Map legend|Frasnian|Givetian|Frasnian to Givetian||||||
25853|Comerong Volcanics|40276|2|Defined|p17|Late Devonian|Middle Devonian|Middle to Late Devonian. p17 or 22?||||||27-OCT-08
25853|Comerong Volcanics|40387|3|Fully described|p137|||||||||
25853|Comerong Volcanics|40834|5|Briefly described|p138|||[Originally entered for WA. CEBMar95]||||||
25853|Comerong Volcanics|42140|6|Mentioned|p559|||||||||
25853|Comerong Volcanics|42141|6|Mentioned|p569|||||||||
25853|Comerong Volcanics|42158|6|Mentioned|p1|||||||||
25853|Comerong Volcanics|42497|5|Briefly described|Map legend|Frasnian|Givetian|||||||
25853|Comerong Volcanics|42726|5|Briefly described|map legend|Middle Devonian||||||||
25853|Comerong Volcanics|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
25853|Comerong Volcanics|43465|14|Not recorded|Map Legend||Late Devonian|||||||
25853|Comerong Volcanics|44093|5|Briefly described|p224 App. 1|Givetian|Givetian|Dominantly felsic volcanics. Geological Province: Lachlan Fold Belt.||||||01-MAR-05
25853|Comerong Volcanics|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Budawang Rift. Geological Province: Lambian Transitional Province.  Rhyolite, rhyolite breccia, basalt, shale, sandstone, conglomerate and mudstone.||||||
25853|Comerong Volcanics|60007|5|Briefly described|Map legend|Late Devonian|Late Devonian|Rhyolite, felsite, rhyolite breccia, red shale, conglomerate.||||||
25853|Comerong Volcanics|60308|5|Briefly described|p38, p39|Frasnian|Givetian|Eastern Lachlan Fold Belt. "Important stratigraphic unit with contentious age" Preferred age quoted. Chemically similar mafic dyke swarm in central Bega Batholith has U-Pb zircon age of 387+/-5 Ma.|380 Ma|||Correlated with Donovan Complex.|Includes basalts.|07-SEP-15
25853|Comerong Volcanics|61964|6|Mentioned|p81|||A-type. ||||||
25853|Comerong Volcanics|62070|5|Briefly described|p34 Fig.1,|Late Devonian|Middle Devonian|||||||
25853|Comerong Volcanics|62569|5|Briefly described|p606 Fig. 1A, p610 Fig. 4|Frasnian|Givetian|||||||
25853|Comerong Volcanics|64827|6|Mentioned|p1051|Late Devonian|Middle Devonian|||||||
25853|Comerong Volcanics|66768|3|Fully described|p209-p221|Late Devonian|Middle Devonian|Middle-Late Devonian. Bimodal basalt-rhyolite volcanic sequence with minor intercalated fluviatile and lacustrine sedimentary rocks. South-eastern Lachlan Orogen, Eden Volcanic Zone, continental back arc setting. Outcrops on limbs of the Budawang Synclinorium. See text for more details.||||||
25853|Comerong 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).|380-390 Ma magnetic age range|||||10-AUG-15
25853|Comerong Volcanics|67847|5|Briefly described|p60 fig 3.3.4|||Eden-Comerong-Yalwal Rift. ||||||
25853|Comerong Volcanics|67849|6|Mentioned|p22 Fig.1.|Late Devonian|Middle Devonian|||||||
25853|Comerong Volcanics|68255|5|Briefly described|p1050 Fig.1, p1051, p1053, p1054, p1063|Late Devonian|Middle Devonian|Budawang Synclinorium.||Of the Moruya Suite.||Unconformably underlain by the Adaminaby Group.|Basalt flows and sedimentary rocks; rhyolite agglomerate and ignimbrite.|20-JUL-15
25853|Comerong Volcanics|68295|6|Mentioned|p29, p28-29 Fig. 2.2|Devonian|Devonian|Of SE Australia (Schmidt et al. 1986).||||||
25853|Comerong Volcanics|68298|5|Briefly described|p215, p234|||Some 700m of sediment north of Braidwood, overlying Nettletons Creek fish horizon. Relationship with Donovan Basic Igneous Complex unclear.||||Unconformably overlies Ordovician rocks. Conformably overlain by Merrimbula Group sediments.||
25853|Comerong Volcanics|68309|6|Mentioned|p225|Late Devonian|Middle Devonian||||||Turbidites.|
25853|Comerong Volcanics|68592|5|Briefly described|p33|Middle Devonian|Middle Devonian|Eden-Comerong-Yalwal Volcanic Zone.|||||A-type felsic volcanics and associated plutons.|
25853|Comerong Volcanics|69019|6|Mentioned|p78, p80 Fig.17.|Devonian|Devonian|Lachlan Fold Belt. Mentioned in comparison with Ooloo Hill Formation basalts; significant similarities are observed.||||||
25853|Comerong Volcanics|69159|5|Briefly described|Map legend|Givetian|Givetian|Four un-named sub-units are mapped separately.||||Is overlain by Worange Point Formation.|Vesicular to amygdaloidal fine-grained to porphyritic basalt; porphyritic rhyolite; rhyolitic volcanic sandstone with minor interbedded grey siltstone; lesser matrix-supported quartz-lithic pebbly sandstone and cobble conglomerate; minor siltstone.|07-SEP-15
25853|Comerong Volcanics|70601|5|Briefly described|p25,27 |Late Devonian|Middle Devonian|Onshore geology. Overlies Ordovician rocks and Bega Batholith. Appears also as Comerong Volcanic Complex on p25.||||Northern equivalent of Boyd Volcanic Complex. Underlies Merrimbula Group.|Bimodal silicic and basaltic volcanics, associated small subvolcanic A-type granites.|
25853|Comerong Volcanics|70661|6|Mentioned|viii|||Major part of the Eden-Comerong-Yalwal Volcanic Zone.||||Correlated with Yawal Volcanics||
25853|Comerong Volcanics|71699|5|Briefly described|Map legend.|Devonian|Devonian|Ungrouped. Four facies are mapped separately.||||Is overlain by Worrange Point Formation (Merrimbula Group).|Vesicular to amygdaloidal fine-grained to porphyritic basalt; porphyritic rhyolite; rhyolitic volcanic sandstone with minor interbedded grey siltstone; lesser matrix-supported quartz-lithic pebbly sandstone and cobble conglomerate; minor siltstone.|
25853|Comerong Volcanics|71700|3|Fully described|vi, p7, p27, p29-p30, p36-p38, CD|Late Devonian|Middle Devonian|Named for Comerong Mountain, west of Bodalla. Three representative sections are proposed: from GR 769113 6001144 to GR 768013 6001144; from GR 771414 6079272 to GR 772096 6079117 and one at GR 228692 6084200.The name was first used by Best et al (1964) to refer to a belf of mafic and felsic volcanic rocks mapped by McElroy and Rose (1962) and correlated with similar rocks in the Eden area. This unit forms a volcanic package at the base of the stratigraphic sequence of the Eden-Comerong-Yalwal rift zone. Contains a number of unnamed volcanic sub-units. Lithology is discussed in some detail for each informal subdivision of this unit. Seperated from the Abercrombie Formation and Willigam Sandstone Member by the Mongarlowe Fault. Wyborn and Owen (1986) described the mineral assemblage of the basalt of this unit. This unit as a whole has a thickness of about 870m in BRAIDWOOD100. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils and distinguishing features are discussed. May be equivalent to the Yalwal Volcanics, Boyd Volcanic Complex and the Dulladerry Volcanics. See also p40, p42, p44-p45, p54, p61-p62, p66, p78, p81.||||Conformably overlain by the Worange Point Formation (Merrimbula Group). Overlain by the Minuma Range Group. Faulted against the Willigam Sandstone Member.|A-type, felsic to bimodal volcanics including basalt, dolerite dykes.|
25853|Comerong Volcanics|73181|6|Mentioned|p65|||[Written as Comerong Volcanics and 'Comerong Volcanics'].||||Equivalent to the Boyd Volcanic Complex.||
27131|Comiala Shale Member|30610|2|Defined|p323|Middle Jurassic|Middle Jurassic|Belongs to Purlawaugh Formation||||||
27131|Comiala Shale Member|35095|6|Mentioned|Table 1|||Reference Dulhunty 1973.||||||
34399|Commong Formation|22736|6|Mentioned|p611 Fig2||Permian|||||||
34399|Commong Formation|22857|6|Mentioned|p514 App.1 Tb.A1.8|Permian|Permian|||||||
34399|Commong Formation|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|Geological Province: New England Fold Belt.||||||
34399|Commong Formation|70939|6|Mentioned|p828|Permian|Permian|Northern Hastings Block.||||||
31566|Condor Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
74202|Confreys Formation|61964|3|Fully described|p14 Fig. 4, p122, p117 Fig.35|Frasnian|Frasnian|Supersedes "Confreys Shale Member" (of "Womboyne Conglomerate") now upgraded to formation status within Cocoparra Group. Interbedded fine-gr.light red + white sandstone and siltstone. Conformably overlies Naradhan Sandstone. For palaeontology - see p261||||||
74202|Confreys Formation|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Interbedded fine-grained red and white  sandstone and siltstone.||||||
74202|Confreys Formation|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.||Overlies Naradhan Sandstone. Is overlain by Melbergen Sandstone.|Interbedded fine-grained red and white sandstone and siltstone.|
74202|Confreys Formation|71889|4|Described|p8, p48, p54. p64|||Outcrops on the Cargelligo 1:250k sheet area. The former Bogolong Formation is now recognised as the southern continuation of this unit. Fine-grained sandstone from this formation is only differentiated from other sandstones of the Cocoparra Group by its relatively higher abundance of muscovite and iron-oxide matrix.||Cocoparra Group||Equivalent to the Bogolong Formation.|Very poorly exposed, intercalated, very fine-grained sandstone and siltstone with some ripple marks.|
74202|Confreys Formation|72083|5|Briefly described|p45|||Cameron and Meakin (in Colquhoun et al., 2005). North of Rankin Springs in the Cargelligo 1:250k sheet area. A fine-grained recessive unit; one of few (listed) in the Group.||Cocoparra Group.||Overlies Naradhan Sandstone. Possible correlative of Bogolong Formation.||31-AUG-19
82377|Congi Creek Monzogranite Phase|71628|4|Described|p1:15; p7: 38-39, 41, 44-49, 51|||Originally the Congi Creek Adamellite of Flinter et al. (1972) after work by Flood (1971) and others. Subsequently the Congi Creek Monzogranite (Brown, 2003 after unpublished work by Chappell and Bryant, 1994). In this study it becomes Congi Creek Monzogranite Phase (of Walcha Road Monzogranite). Named after a local watercourse. Located ~15km ESE of Bendemeer and ~25km WNW of Walcha; crops out along Oxley Highway. Forms rugged topography. Geochemistry briefly described.|250.6 +/- 1.7 Ma (SHRIMP: Chisholm et al., 2014).|Walcha Road Monzogranite.||Is entirely surrounded by the parent unit.|Light grey, fine- to medium-grained, equigranular to very sparsely porphyritic, felsic biotite monzogranite (plagioclase-rich) to granodiorite, with sparse K-feldspar megacrysts and hornblende.|
79102|Conlea porphyry|69635|5|Briefly described|p177-181, p69|Early Devonian|Early Devonian|Informal name. Southern Thomson Orogen.  U-Pb SHRIMP zircon magmatic crystallisation age. Sample from 403.65-405.0 m in drillhole TFB002A (Meridian Minerals Limited). Shown as Conlea Porphyry p2.|398.0+/-2.8 Ma||||Grey, intermediate porphyry with disseminated pyrite.Gradational contact zones approximately two metres thick both above and below, passing into a pink granite phase.|
79102|Conlea porphyry|71860|5|Briefly described|p7|||Informal name. Age is a SHRIMP U-Pb date.|398.0 +/- 2.8 Ma (Fraser et al, 2014)||||Intermediate porphyry.|
79102|Conlea porphyry|71965|5|Briefly described|p902,913|||Geological province: Thomson Orogen. Intersected in drillhole TFB002A. Intrudes into the Nangunyah Zone, dated at 398+\-2.8 Ma (Fraser et al., 2014).||||||
79102|Conlea porphyry|72522|6|Mentioned|p29.|Early Devonian|Early Devonian|Ref. Fraser et al., 2014. With Tinchelooka diorite, age determined to be indistinguishable from the date of samples from the 52172127 volcaniclastic sandstone (Nimrod TDH6; 398.3 +/- 2.3 Ma).||||||
79189|Connell Member|68592|2|Defined|p428,p433, p436, p440-1, p473-6, p485-92|Wenlock|Wenlock|See also p1875. Name first published by Moignard (1970). Described by Cramsie et al. (1978). Feary (1984, 1986) introduced "considerable confusion", applying the names Snow Formation and Copplestone Formation to these rocks, disregarding prior usage of the name Copplestone Member to the rocks underlying the Connell Member: these he called the Glen Bower Formation. This study returns the nomenclature to that of Cramsie et al. (1978). Type and representative section/locality are described. Thickness to 350m. Low energy, deeper water, further offshore carbonate deposition. Reasonably fossiliferous: tabulate and rugose corals, brachiopods, gastropods, bryozoans, conodonts and stromatoporoids in carbonate mounds. Mid-Wenlock.||Unit in Glen Bower Formation.||Conformably overlies Copplestone Member. Is overlain unconformably by Boambolo Formation and Laidlaw Volcanics. Correlated with Cliftonwood Limestone Member (Yass Formation).|Medium- to coarse-grained quartzose sandstones, mudstones and thinly-bedded, very fine-grained sandstones with interbedded carbonates including lensoidal boundstone mounds.|16-OCT-15
79189|Connell Member|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdgc. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Glen Bower Formation||Appears to overlie Copplestone Member. Appears to be overlain by Boambolo Formation.|Medium-coarse grained quartzose sandstone; finely bedded, silty sandstone and carbonate rocks including algal lime mud and stromatolitic limestone.|
79189|Connell Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Glen Bower Formation|||Medium-coarse grained quartzose sandstone; finely bedded, silty sandstone and carbonate rocks including algal lime mud and stromatolitic limestone.|
79189|Connell Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Glen Bower Formation|||Medium-coarse grained, quartzose sandstone (generally cross bedded). Finely bedded, silty sandstone and carbonate rocks including algal, lime-mud and stromatolitic limestone.|
79189|Connell Member|71656|6|Mentioned|p12 Fig.2, p22|Wenlock|Wenlock|Includes rugose and tabulate corals along with brachiapods, nautiloids and conodonts.||Glen Bower Formation, Douro Group||Partially equivalent to Goobarragandra Volcanics, Hawkins Volcanics.||
23503|Coodravale Granodiorite|36441|5|Briefly described|map legend|Pridolian|Ludlovian|Of Young Batholith. Intrusive. Coodravale I-type Suite. Granodiorite, adamellite. BMR map code: Syo.||||||
23503|Coodravale Granodiorite|39660|6|Mentioned|p449|||||||||
23503|Coodravale Granodiorite|45147|2|Defined|M245|Late Silurian|Late Silurian|Prob.Late Silurian||||||
30031|Coogal Subgroup|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Black Jack Group. Includes the Clare Sandstone, Benelabri Formation and Hoskissons Coal. Geological Province: Gunnedah Basin.||||||
30031|Coogal Subgroup|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Of Black Jack Group. Encompasses Clare Sandstone and Hoskissons Coal. Age Upper Stage 5. Formal definition published in an article released immediately prior to this article, however a summary of new nomenclature is provided in Appendix 1.||||||13-NOV-13
30031|Coogal Subgroup|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Black Jack Group. Underlies: Digby Formation.  Overlies: Brothers Subgroup.||||||05-JUL-04
30031|Coogal Subgroup|68003|5|Briefly described|p38 Fig.3-j, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Mis-spelt as Coolgal Subgroup on p129.||Unit in Black Jack Group.|Includes Hoskissons Coal, Clare Sandstone and Benelabri Formation.|Overlies Brothers Subgroup. Is overlain by Nea Subgroup.||
30031|Coogal Subgroup|68004|5|Briefly described|p23 Table 1. |||Gunnedah Basin.||Middle unit in Black Jack Group.|Includes Hoskissons Coal, Clare Sandstone and Benelabri Formation.|Overlies Brothers Subgroup. Is overlain by Nea Subgroup.||
30031|Coogal Subgroup|70791|5|Briefly described|p277|Permian|Permian|Gunnedah Basin.||Black Jack Group.|Hoskissons Coal, Clare Sandstone, Benelebri Formation.|||
33193|Cookaburragong Granodiorite|24417|3|Fully described|p54|Silurian|Silurian|Intrudes Humbug Sandstone (Wagga Group).  Age: 432+/-3.1Ma (SHRIMP U-Pb).||||||
33193|Cookaburragong Granodiorite|50554|5|Briefly described|Map legend|Devonian|Devonian|Grey, porphyritic biotite granodiorite, with sedimentary zenoliths.||||||
33193|Cookaburragong Granodiorite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|Of the Ungarie Suite.||||||13-JUL-04
33193|Cookaburragong Granodiorite|61964|3|Fully described|p14 Fig. 4, p55-56|Llandovery|Llandovery|Of the Koetong Suite (Koetong Supersuite). S-type: grey, medium-grained, flow-banded,  porphyritic biotite granodiorite, with metasedimentary xenoliths. Age: 432.8+/-3Ma (SHRIMP U-Pb). See also p38, p41 Tb. 2.||||||
33193|Cookaburragong Granodiorite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Grey, medium-grained porphyritic biotite granodiorite, with metasedimentary xenoliths.||||||10-APR-08
33193|Cookaburragong Granodiorite|64568|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Grey porhyritic biotite granodiorite and sedimentary xenoliths.||||||23-SEP-08
33193|Cookaburragong Granodiorite|65469|5|Briefly described|p18|Early Silurian|Early Silurian|Lachlan Orogen.||Koetong Suite||||
40938|Cookbundoon Formation|50234|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Lambie Group.  Interfingers with and partly overlies Wiarborough Formation.  Underlies Tarlo Formation. Overlies Strathaird Formation.||||||25-JUN-08
40938|Cookbundoon Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Lambie Group. White to grey, thick bedded, medium-grained to pebbly quartzite and quartzose sandstone. Lenses of polymict conglomerate at base; rare lithic-quartz sandstone and mudstone.||||||
40938|Cookbundoon Formation|68592|2|Defined|p235, p1722-3, p1727, p1743-8|Late Devonian|Late Devonian|New name. First named as Cookbundoon Sandstone by Brunker et al. (1970), after Cookbundoon River (now called the Tarlo River) and Range. Here renamed Cookbundoon Formation because of the variety of other lithologies present. Forms very prominent outcrops. "Good exposures" mentioned by Scheibner (1973) and Offenberg (1974) are specified as the type locality, where the unit is 300m thick. Geochemistry unknown; geophysical properties described. Possible correlate of part of Nangar Subgroup and of Turon [River] Grits. Has been quarried for road construction, houses and drystone walls. Potential source of structural clay/shale and kaolin.||Unit in Lambie Group.||Overlies Strathaird Formation gradationally; overlies and interfingers with Cowpers Creek Conglomerate. Is overlain gradationally by Tarlo Formation.|Mostly medium- to coarse-grained, moderately to poorly sorted, generally massive quartzose to lithic-quartz sandstone, dominantly off-white; includes many pebble to cobble conglomerate lenses; very minor red mudstone.|
40938|Cookbundoon Formation|70192|5|Briefly described|Map Legend|Famennian|Famennian|Dlc. Includes two unnamed sub units: a mudstone; and, a massive, pebble-clast supported quartz lithic conglomerate. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Lambie Group|Includes two unnamed sub units.|Is overlain by Tarlo Formation. Overlies Cookbundoon Formation.|Medium-coarse grained, moderate-poorly sorted, massive or sporadically cross bedded quartzose and lithic quartz sandstone with sporadic pebble to cobble conglomerate horizons. Very minor mudstone present also.|
40938|Cookbundoon Formation|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed member of red mudstone.||Lambie Group|||Medium to coarse-grained, moderately-poorly sorted, massive to cross-bedded quartzose and lithic quartz sandstone with sporadic pebble to cobble conglomerate horizons and very minor red mudstone.|
40938|Cookbundoon Formation|70543|5|Briefly described|Map Legend|Devonian|Devonian|Includes two unnamed sub units; a mudstone and a massive, pebble-clast supported quartz lithic conglomerate.||Lambie Group|Includes two unnamed sub units||Medium-coarse grained, moderate-poorly sorted, massive or sporadically cross bedded quartzose and lithic quartz sandstone with sporadic pebble to cobble conglomerate horizons. Very minor mudstone present also.|
40938|Cookbundoon Formation|71656|6|Mentioned|p13 Fig.2|||Shown only in correlation chart (Fig.2).||Lambie Group||Qverlies Cowpers Creek Conglomerate, Strathaird Formation. Overlain by Tarlo Formation.||
24223|Cookeys Plains Formation|5178|6|Mentioned|p106 Fig.1, p107, p114|||||||||
24223|Cookeys Plains Formation|22519|6|Mentioned|p7|Devonian|Ordovician|part of the Derriwong Group||||||
24223|Cookeys Plains Formation|22831|3|Fully described|p 44|Lochkovian|Pridolian|||||||
24223|Cookeys Plains Formation|22857|4|Described|p448 App.1, Tb.A1.6|Pridolian|Pridolian|Of the Derriwong Group. Shale, siltstone and fine-grained arenite; limestone, coarse to medium-grained arenite; contains conodonts, corals, trilobites, brachiopods. Max. thickness: 1600m. Geological Province: Bogan Gate Terrace.||||||
24223|Cookeys Plains Formation|23522|5|Briefly described|p253|Devonian|Devonian|||||||
24223|Cookeys Plains Formation|24417|3|Fully described|p71|Early Devonian|Late Silurian|Of Derriwong Group.  Overlain by Yarrabandai Formation; underlain by Calarie Sandstone.  Max. thickness: 1200m.||||||
24223|Cookeys Plains Formation|36066|5|Briefly described|p9|||||||||
24223|Cookeys Plains Formation|39660|2|Defined|p452|Early Devonian|Early Devonian|Earliest Devonian||||||
24223|Cookeys Plains Formation|43441|5|Briefly described|27|Early Devonian|Late Silurian|Fossiliferous||||||08-JAN-10
24223|Cookeys Plains Formation|44160|5|Briefly described|Map Legend|Lochkovian|Pridolian|||||||08-JAN-10
24223|Cookeys Plains Formation|50299|5|Briefly described|Map Legend|Devonian|Silurian|Of the Derriwong Group.  Overlies: Calarie Sandstone.  Underlies: Pullabooka Formation.||||||
24223|Cookeys Plains Formation|60009|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Derriwong Group. Overlies: Edols Conglomerate.  Underlies: Yarrabandai Formation.||||||13-JUL-04
24223|Cookeys Plains Formation|60548|5|Briefly described|map legend|Devonian|Silurian|Of Derriwong Group.  Siltstone, shale, minor sandstone.||||||
24223|Cookeys Plains Formation|61894|6|Mentioned|p179 Fig.3, p180-181 |||||Derriwong Group.||||
24223|Cookeys Plains Formation|62070|5|Briefly described|p37,|Lochkovian|Pridoli|||||||
24223|Cookeys Plains Formation|63120|5|Briefly described|p217|Early Devonian|Late Silurian|Of the Derriwong Group.||||||
24223|Cookeys Plains Formation|68297|5|Briefly described|p181|Ludlow|Ludlow|Replaces Bogan Gate Sandstone Group. Includes acanthodian scales in limestone.||||||
24223|Cookeys Plains Formation|73143|6|Mentioned|p9, p11|Pragian|Late Silurian|Latest Silurian minimum age. Contains several rugose coral species and tabulate coral.||Derriwong Group||||
24223|Cookeys Plains Formation|73492|6|Mentioned|p691|||||||||
24224|Cookopie Monzonite|40365|2|Defined|p325|Devonian|Silurian|Siluro-Devonian||||||
33801|Cooks Vale Granite|50233|5|Briefly described|Map Legend|Emsian|Emsian|Of the Wologorong Batholith. Foliated, porphyritic to megacrystic biotite granite.||||||
33801|Cooks Vale Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tumboramboro Suite. Leucocratic coarse-grained muscovite-biotite granite which is extensively recrystallised.||||||24-JUN-08
33801|Cooks Vale Granite|68592|3|Fully described|p1542-3, p1545-6, p1582-4|Early Devonian|Early Devonian|New name, after Cooks Vale Creek. Type area described. Poorly exposed. Geochemistry and geophysical properties described. Tentative age based on intrusive relationship.||Unit in Tumboramboro Suite.||Intrudes Cuddyong Formation.|Coarse-graind, leucocratic granite; extensively recrystallised. Strongly foliated along W and NW margins.|
33801|Cooks Vale Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dtc. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Tumboramboro Suite|||Leucocratic, coarse grained, muscovite-biotite granite, extensively recrystallised; medium-high K, low Th, low-high U response; low magnetic susceptibility.|
33801|Cooks Vale Granite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Tumboramboro Suite|||Leucocratic, coarse grained, muscovite-biotite granite, extensively recrystallised; medium-high K, low Th, low-high U response; low magnetic susceptibility.|
33801|Cooks Vale Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Tumboramboro Suite|||Leucocratic, coarse grained, muscovite-biotite granite, extensively recrystallised; medium to high K, low Th and low to high U response; low magnetic susceptibility.|
81172|Coolabah Monzodiorite|72296|2|Defined|ix, p39, p41-43, p60||Early Devonian|New name, after the village of Coolabah. Dykes associated with prominent NNW-trending linear magnetic anomalies (Coolabah dyke swarm in Hegarty, 2016). A type locality is designated at Lat -31.2425 degrees Long 146.9159 degrees, ~150m N of the Okeh and Murrawombie road junction. Between 5 and 160m wide. Forms low (<50 cm), pod-shaped outcrops; float common. Maximum age based on overprinting of Devonian (Cobar) deformation. Geophysical properties described. Photomicrographs.||||Intrudes Narrama Formation.|Massive, coarse-grained porphyritic monzodiorite, with large labradorite crystals within a groundmass of augite, plagioclase, alkali feldspar and quartz.|
24606|Coolagolite Granodiorite|22815|4|Described|p65,68|Early Devonian|Late Silurian|||||||
24606|Coolagolite Granodiorite|40776|6|Mentioned|p504|||Misspelling of Coolagalite?||||||
24606|Coolagolite Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Cobargo Suite.||||||
25856|Coolamine Igneous Complex|23548|5|Briefly described|p533.|||||||||
25856|Coolamine Igneous Complex|29456|5|Briefly described|p423|||||||||
25856|Coolamine Igneous Complex|35185|6|Mentioned|p240|||||||||
25856|Coolamine Igneous Complex|36050|6|Mentioned|p399|||||||||
25856|Coolamine Igneous Complex|36443|5|Briefly described|map legend|Lochkovian|Lochkovian|Of Boggy Plain I-type Suite. Intrusives. BMR map code Dlx: granodiorite, quartz monzodiorite, quartz monzogabbro, quartz gabbro, minor adamellite and tonalite; Dlp: pyroxenite, meta-monzogabbro.||||||
25856|Coolamine Igneous Complex|40328|6|Mentioned|p62|||Also on p66.||||||09-OCT-08
25856|Coolamine Igneous Complex|40882|6|Mentioned|p22|||Mention Fig.1.||||||09-OCT-08
25856|Coolamine Igneous Complex|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh24||||||
25856|Coolamine Igneous Complex|45147|2|Defined|M267|Early Devonian|Early Devonian|See also M265||||||
25856|Coolamine Igneous Complex|60078|6|Mentioned|Map Legend|Devonian|Late Silurian|||||||
31468|Coolamine Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains the Coolamine and Gurrangorambla Granites (informally named).||||||08-FEB-05
37353|Coolangatta Latite Member|71542|4|Described|p23,25,30-32,34, 35|Late Permian|Late Permian|Of southern Sydney Basin. Type section: 56/291300E, 6141500N, between 204 to 226 m  elevation. Thickness: 30-40m. Deposited in a shallow marine environment directly above the breccia in the top Westley Park Sandstone Member. Deposited during ensuing, less violent eruptions after the intitial Koo-Lee Tuff Member eruption, associated with extrusion of fluidal lava (latite) down volcani flanks and into the sea. Deposited onto unconsolidated wet sand and formed a breccia at the sediment-lava interface. Pre-dates the Blow Hole flow.||Unit of Gerringong Volcanics.||Underlain by  and wavy contact with the Westley Park Sandstone Member.|Dark grey, trachytic porphyritic (feldspar-phyric) latite extrusion in a fine-grained groundmass.|20-OCT-21
37353|Coolangatta Latite Member|73494|5|Briefly described|p542-543|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanics.||||
31461|Coolangubra Suite|22815|5|Briefly described|p75|||Consists of three plutons.||||||
31461|Coolangubra Suite|22878|6|Mentioned|p77|||||||||
31461|Coolangubra Suite|24551|6|Mentioned|p235|||||||||
31461|Coolangubra Suite|42726|5|Briefly described|map legend|Early Devonian|Early Devonian|Of the Bemboka Supersuite.  Includes the Coolangubra, Loomat and Beehive Creek Granites.||||||07-FEB-05
31461|Coolangubra Suite|43233|5|Briefly described|Map Legend|||of Bega Batholith.||||||
25857|Cooleman Limestone|13996|6|Mentioned|p129|Silurian|Silurian|Contains an unillustrated conodont form of supposed European Wenlock affinity.||||||
25857|Cooleman Limestone|22857|4|Described|p466 App.1 Tb.A1.6|Pridolian|Wenlockian|Of the Cooleman Plains Group. Massive to well-bedded; commonly recrystallised. Max. thickness: 650m. ||||||
25857|Cooleman Limestone|23309|6|Mentioned|p383||Wenlock|||||||
25857|Cooleman Limestone|24266|5|Briefly described|p1486|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
25857|Cooleman Limestone|29456|5|Briefly described|p423|||||||||
25857|Cooleman Limestone|31019|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25857|Cooleman Limestone|32820|6|Mentioned|Table 1|||Refers Owen et al. (in press)||||||
25857|Cooleman Limestone|33325|5|Briefly described|Table 3|||||||||
25857|Cooleman Limestone|34405|4|Described|p117|||||||||
25857|Cooleman Limestone|34692|5|Briefly described|p186|||||||||
25857|Cooleman Limestone|36050|6|Mentioned|p399|||||||||
25857|Cooleman Limestone|36413|6|Mentioned|Table 3|||||||||
25857|Cooleman Limestone|36443|5|Briefly described|map legend|Pridolian|Wenlockian|Of Cooleman Plains Group. Massive to well-bedded limestone, commonly strongly recrystallised. Interfingers with Blue Waterhole Formation, Peppercorn Formation and Pocket Formation. BMR map code: Scl.||||||
25857|Cooleman Limestone|37727|5|Briefly described|p48|||||||||
25857|Cooleman Limestone|38555|6|Mentioned|p31|||||||||
25857|Cooleman Limestone|39409|6|Mentioned|Table XVII|||||||||
25857|Cooleman Limestone|39800|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
25857|Cooleman Limestone|40328|3|Fully described|p65|||||||||
25857|Cooleman Limestone|40415|6|Mentioned|p23|||||||||
25857|Cooleman Limestone|40419|6|Mentioned|p4|||||||||
25857|Cooleman Limestone|40424|6|Mentioned|p83|||||||||
25857|Cooleman Limestone|45147|2|Defined|M91|early Pridolian|Ludlovian|Late Wenlockian to Early Pridolian||||||
25857|Cooleman Limestone|68592|6|Mentioned|p92|Silurian|Silurian|In Tantangara and Brindabella 1:100 000 map areas. Part of a mid to late Silurian quartzose clastic and carbonate succession, which the Long Plain Fault has juxtaposed against the partly coeval Goobarragandra Volcanics.||||||
25857|Cooleman Limestone|73143|6|Mentioned|p10|Late Silurian|Late Silurian|Contains rugose corals, Neomphyma? Sp. (Hill, 1954a).||||||
24868|Coolringdon beds|22603|6|Mentioned|p100||Late Ordovician|Now incorporated in Adaminaby beds||||||
24868|Coolringdon beds|35191|6|Mentioned|p116|||||||||
31565|Coolumbooka Suite|22815|6|Mentioned|p83|||||||||
31565|Coolumbooka Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31565|Coolumbooka Suite|43233|5|Briefly described|Map Legend|||of Bega Batholith.||||||
31565|Coolumbooka Suite|44093|5|Briefly described|p204 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
24869|Cooma Creek Member|40664|3|Fully described|p234|Miocene|Miocene|||||||13-JUN-13
24869|Cooma Creek Member|42035|5|Briefly described|Table 1 P130|||||||||
31495|Cooma Supersuite|22778|6|Mentioned|p 162|||||||||
31495|Cooma Supersuite|23309|6|Mentioned|p338|||||||||
31495|Cooma Supersuite|23439|6|Mentioned|p135|||||||||
31495|Cooma Supersuite|23551|5|Briefly described|p491|||||||||
31495|Cooma Supersuite|24222|5|Briefly described|p9|||Strongly peraluminous S-type rocks.  Geological Province: Lachlan Fold Belt.||||||
31495|Cooma Supersuite|24551|6|Mentioned|p232|||||||||
31495|Cooma Supersuite|42726|5|Briefly described|map legend||Silurian|Includes the Bethanga and Cooma Suites.||||||09-FEB-05
31495|Cooma Supersuite|68310|6|Mentioned|p241|||Partial melting caused the source rock to disaggregate, producing restite enclaves.||||||
31842|Coomaloo Ignimbrite Member|24417|4|Described|p122|Middle Devonian|Middle Devonian|Of Warrumba Volcanics.||||||
31842|Coomaloo Ignimbrite Member|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Warrumba Volcanics (Rocky Ponds Group).||||||05-JUL-04
31842|Coomaloo Ignimbrite Member|60009|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Warrumba Volcanics (Rocky Ponds Group).||||||13-JUL-04
29939|Coomber Formation|22529|4|Described|1|Late Ordovician|Late Ordovician|||||||
29939|Coomber Formation|22545|4|Described|p498-507, Fig.5|Early Silurian|Late Ordovician|||||||
29939|Coomber Formation|22857|4|Described|p127, p430 App. 1 Tb. A1.5.|Late Ordovician|Late Ordovician|Of the Cabonne Group. Conformably overlies the Adaminaby Group. Max. thickness: 1750m. ||||||
29939|Coomber Formation|23043|5|Briefly described|Map Legend|Bolindian|Gisbornian|of Cabonne Group.||||||
29939|Coomber Formation|23170|2|Defined|p44|Late Ordovician|Late Ordovician|Of the Cabonne Group.||||||21-MAY-08
29939|Coomber Formation|23181|6|Mentioned|p6,7||Ordovician|Unfossiliferous. Correlated with Sofala Volcanics on radiometric signatures.||||||
29939|Coomber Formation|23245|6|Mentioned|p127,129|||||||||
29939|Coomber Formation|24463|4|Described|p321|Ordovician|Ordovician|Conformably overlies the Adaminaby Group; conformably overlain by Dungeree Volcanics. Geological Province: Lachlan Fold Belt.||||||04-DEC-07
29939|Coomber Formation|43188|4|Described|p199,Table 1 p200||Late Ordovician|Capertee High. Representative section location given in Table 1. Age Darriwilian to Gisbornian.||||||
29939|Coomber Formation|44093|5|Briefly described|p213 App. 1|Late Ordovician|Late Ordovician|Of the Cabonne Group. Geological Province: Lachlan Fold Belt.||||||
29939|Coomber Formation|61900|5|Briefly described|p129, p130 Fig. 3|Early Silurian|Late Ordovician|Phyllites.  Unconformably overlain by Rylstone Volcanics.||||||
29939|Coomber Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p157|Late Ordovician|Late Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt, LFB.  Consists of a deep-water volcaniclastic domainated apron (Pemberton et al. (1994).||||||07-FEB-11
29939|Coomber Formation|63283|6|Mentioned|p205|||Geological Province: Rockley-Gulgong Volcanic Belt. Consists of perdominantly fine-grained volcaniclastic snadstone and siltstone. See also p205.||||||07-FEB-11
29939|Coomber Formation|63289|6|Mentioned|p374|||Volcaniclatsics contain mostly feldspar and volcanic fragments (65-91%) woth almost no quartz.||||||07-FEB-11
29939|Coomber Formation|63290|6|Mentioned|p397 Fig. 3(b)|Late Ordovician|Late Ordovician|Geological Province: Rockley - Gulgong Volcanic Belt.||||||
29939|Coomber Formation|67322|4|Described|p25-26; Fig.5|Late Ordovician|Late Ordovician|(Pemberton et al. 1994; Colquhoun and Meakin, in Meakin and Morgan 1999). Lacks fossils, but assigned an age based on the underlying conformable contact with the Adaminaby Group. ||Of the Cabonne Group||Conformably overlies the Adaminaby Group. Overlies the Chakola Formation, Wagga Group, Bumballa Formation. Overlain by the Margules Group.|Diverse facies: massive lithic sandstone, thin-bedded sandstone and mudstone, siliceous or cherty mudstone, scattered allochthonous limestone blocks, and sporadic basalt flows and shallow intrusions.|21-FEB-18
29939|Coomber Formation|68592|6|Mentioned|p371|||Rockley-Gulgong Volcanic Belt.||Unit in Cabonne Group.||||
29939|Coomber Formation|70684|6|Mentioned|p3, p74|||||||||
29939|Coomber Formation|73299|6|Mentioned|p1096 Fig.3, p1098 Fig.4, p1100 Fig.5|Ordovician|Ordovician|Capertree High.||||||
31716|Coonambro Volcanics|24417|3|Fully described|p92|Early Devonian|Early Devonian|Overlies Moura Formation.||||||
31716|Coonambro Volcanics|60009|5|Briefly described|Map Legend|Emsian|Emsian|||||||13-JUL-04
77004|Coondella Creek Monzogranite|71206|6|Mentioned|p373|||The name Coondella Ck [sic] appears in a list of Suites; almost certainly placed in the wrong column.|||||Aluminous A-type granite.|
36363|Coonemia Complex|67663|6|Mentioned|p519|||Southern Sydney Basin.||||||
36363|Coonemia Complex|73197|6|Mentioned|p475 Fig.6, p478|Lopingian|Guadalupian|Attributed to the Currarong Arc.|||||Subsurface mafic intrusives.|
76918|Coopernook Conglomerate Member|66090|2|Defined|p1, p4, pp8-9, pp20-22, p30, pp32-33.|Early Triassic|Early Triassic|Defined in this study. Formerly part of the then-undifferentiated Camden Head Claystone. Forms most of the Lansdowne Escarpment. Widely distributed throughout Lorne Basin. Identified by >25% quartz clasts, <3 cobbles in 0.25 m2 area, and common occurrence of reddish purple mudstone beds. Clasts derived from outside the Basin perimeter; typical of the New England Orogen. Surrounds all of the circular Holey Flat Uplift, with beds dipping almost vertically. New name. Previously the lower part of the (then undifferentiated) Camden Head Claystone. Wide spread unit in Triassic sequence of Lorne Basin. Type section described. Reddish purple mudstone is diagnostic.||Basal unit in Camden Head Claystone.||Overlies conformably the Jolly Nose Conglomerate. Grades upwards into the rest of the Camden Head Claystone.|Upward-fining, chert, quartz and jasper pebble and granule conglomerate and sandstone, interbedded with grey and reddish purple mudstone.|12-OCT-15
76918|Coopernook Conglomerate Member|71628|5|Briefly described|p17:73|Early Triassic|Early Triassic|||Camden Haven Claystone.||||
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).||||||
75739|Coorabakh Conglomerate|66090|2|Defined|p1, p4, pp8-9, pp24-26. |Early Triassic|Early Triassic|Defined in this study. Laterally equivalent to Laurieton Conglomerate. A resistant, cliff-forming unit. Identified by >25% quartz clasts and absence of reddish purple mudstone beds. The significant chert and jasper clasts are typical of New England Orogen provenance. Unfossiliferous.||Unit in Camden Haven Group.||Overlies conformably the Camden Head Claystone. No overlying strata.|Predominantly pebble and granule conglomerate with interbedded sandstone.|
26493|Coorikiana Sandstone|13497|5|Briefly described|p115 fig 6.33, p170, p171|Early Cretaceous|Early Cretaceous|Eromanga Basin. Sandstone were deposited in a shoreface environment. ||Marree Subgroup||Overlies the Bulldog Shale. Overlain by the Oodnadatta Formation.|Sandstone.|
26493|Coorikiana Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Albian|Albian|In Eromanga Basin.||Of Marree Subgroup||||
26493|Coorikiana Sandstone|22874|6|Mentioned|P18|||||||||
26493|Coorikiana Sandstone|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Oodnadatta Formation, underlying unit is Bulldog Shale||||||
26493|Coorikiana Sandstone|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
26493|Coorikiana Sandstone|23054|5|Briefly described|p21,26,36||Albian|||||||
26493|Coorikiana Sandstone|23056|6|Mentioned|12 table 2|||||||||
26493|Coorikiana Sandstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group).||||||21-MAY-08
26493|Coorikiana Sandstone|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age - Aptian ?(text)     or     Albian ? (diagram)||||||
26493|Coorikiana Sandstone|23375|4|Described|Fig2 p265||Albian|In the Eromanga Basin.||||||21-MAY-08
26493|Coorikiana Sandstone|23982|5|Briefly described|p58 Fig.18|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24092|5|Briefly described|p8 Fig.3|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24175|3|Fully described|p26, p17 Fig. 3|Albian|Albian|Of Marree Group. Conformably overlain by Oodnadatta Sandstone;  transitionally overlies Bulldog Shale.  Max. thickness: 15m.  Geological Province: Eromanga Basin.||||||31-MAR-09
26493|Coorikiana Sandstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24321|5|Briefly described|Map legend|Albian|Albian|Of the Marree Subgroup.||||||21-MAY-08
26493|Coorikiana Sandstone|30804|6|Mentioned|p10|||||||||
26493|Coorikiana Sandstone|33819|6|Mentioned|p1|||Cretaceous||||||
26493|Coorikiana Sandstone|33822|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
26493|Coorikiana Sandstone|33827|6|Mentioned|p13|||||||||
26493|Coorikiana Sandstone|35002|6|Mentioned|p27|||||||||
26493|Coorikiana Sandstone|38730|6|Mentioned|p29|||||||||
26493|Coorikiana Sandstone|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
26493|Coorikiana Sandstone|39914|6|Mentioned|p3|||||||||
26493|Coorikiana Sandstone|40003|5|Briefly described|Table 15|||||||||
26493|Coorikiana Sandstone|40058|6|Mentioned|p5|||||||||
26493|Coorikiana Sandstone|40199|6|Mentioned|p16|||See also Fig.1||||||
26493|Coorikiana Sandstone|40220|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|40670|6|Mentioned|Fig.9|||||||||
26493|Coorikiana Sandstone|40681|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|40910|6|Mentioned|p15|||||||||
26493|Coorikiana Sandstone|40911|6|Mentioned|Map legend|Cenomanian|Cenomanian|Prob. Cenomanian||||||
26493|Coorikiana Sandstone|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|40926|6|Mentioned|p17|||||||||
26493|Coorikiana Sandstone|41060|6|Mentioned|p2|||Generalized stratigraphy. See also Fig.3||||||
26493|Coorikiana Sandstone|41061|6|Mentioned|p9|||||||||
26493|Coorikiana Sandstone|41062|6|Mentioned|Fig.5|||||||||
26493|Coorikiana Sandstone|41064|6|Mentioned|p62|||||||||
26493|Coorikiana Sandstone|41084|5|Briefly described|Fig.2|||||||||
26493|Coorikiana Sandstone|41086|3|Fully described|p98|||||||||
26493|Coorikiana Sandstone|41087|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41088|6|Mentioned|p143|||||||||
26493|Coorikiana Sandstone|41117|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41165|5|Briefly described|p362|||See also Fig.15||||||
26493|Coorikiana Sandstone|41175|6|Mentioned|Fig.1|||||||||
26493|Coorikiana Sandstone|41177|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41182|6|Mentioned|p287|||||||||
26493|Coorikiana Sandstone|41183|6|Mentioned|p307|||||||||
26493|Coorikiana Sandstone|41184|6|Mentioned|p328|||||||||
26493|Coorikiana Sandstone|41187|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41216|6|Mentioned|Fig.18|||||||||
26493|Coorikiana Sandstone|41266|6|Mentioned|Fig.3|||||||||
26493|Coorikiana Sandstone|41523|3|Fully described|p276|||||||||
26493|Coorikiana Sandstone|41535|6|Mentioned|p368|||||||||
26493|Coorikiana Sandstone|41724|6|Mentioned|p383|||||||||
26493|Coorikiana Sandstone|41950|5|Briefly described|Fig.2 P3|||||||||
26493|Coorikiana Sandstone|42071|6|Mentioned|Table 2 P120|||||||||
26493|Coorikiana Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
26493|Coorikiana Sandstone|42293|6|Mentioned|Fig.2 P.18|||||||||
26493|Coorikiana Sandstone|42375|5|Briefly described|Fig.27 P122|Late Cretaceous|Jurassic|Eromanga Basin||||||
26493|Coorikiana Sandstone|42395|5|Briefly described|Fig.13 P83|||||||||
26493|Coorikiana Sandstone|42429|5|Briefly described|p155|||||||||
26493|Coorikiana Sandstone|42520|6|Mentioned|p6|||||||||
26493|Coorikiana Sandstone|42673|6|Mentioned|Fig.5 P189|||||||||
26493|Coorikiana Sandstone|42746|4|Described|p12|||See also Fig.6.||||||21-MAY-08
26493|Coorikiana Sandstone|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||25-MAY-05
26493|Coorikiana Sandstone|43258|5|Briefly described|Map Legend||Cretaceous|||||||
26493|Coorikiana Sandstone|43298|5|Briefly described|Map Legend||Cretaceous|||||||
26493|Coorikiana Sandstone|43591|6|Mentioned|p176|||||||||
26493|Coorikiana Sandstone|43628|6|Mentioned|Fig.3||Early Cretaceous|||||||
26493|Coorikiana Sandstone|43681|5|Briefly described|p296|||||||||
26493|Coorikiana Sandstone|43711|6|Mentioned|p20|||||||||
26493|Coorikiana Sandstone|44133|4|Described|p120-121, 104 Fig 9.11, 117|Late Albian|Middle Albian|Geological Province: Eromanga Basin. Conformably overlies: Bulldog Shale. Formerly a member of the Oodnadatta Formation. Formerly named Attraction Hill Sandstone Member of the Marree Formation. ||||||
26493|Coorikiana Sandstone|44289|5|Briefly described|Map Legend||Albian|||||||
26493|Coorikiana Sandstone|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Bulldog Shale. Overlain by Oodnadatta Formation. Lateral to Toolebuc Formation and Allaru Mudstone; interfingers laterally with Mackunda Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
26493|Coorikiana Sandstone|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||
26493|Coorikiana Sandstone|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||
26493|Coorikiana Sandstone|61312|5|Briefly described|p78, p79 Table E2|Cretaceous|Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group). Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
26493|Coorikiana Sandstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
26493|Coorikiana Sandstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|63979|6|Mentioned|p48, Fig. 44|Albian|Albian|SA unit that equates to part of the Coreena Member of Wallumbilla Formation in Qld.||||||07-FEB-11
26493|Coorikiana Sandstone|64048|6|Mentioned|p72|||South Australia equivalent to upper part of Wallumbilla Formation in Qld. Geological Province: Cooper Basin. Contains porous sandstones.||||||07-FEB-11
26493|Coorikiana Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Cretaceous|Cretaceous|Eromanga Basin. Mis-spelt as Cooriakana in Fig.1c.||Unit in Marree Subgroup.||Underlies Oodnadatta Formation; overlies Bulldog Shale.||10-DEC-15
26493|Coorikiana Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Bulldog Shale. Overlain by Oodnadatta Formation.||||||08-MAR-12
26493|Coorikiana Sandstone|65489|6|Mentioned|p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 20m thick. Hosts gas discovery.  ||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|65925|5|Briefly described|Appendix 2.||||||||Fine-grained, calcareous, clayey sandstone; sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Occurs locally between underlying Bulldog Shale and overlying Oodnadatta Formation.||
26493|Coorikiana Sandstone|66529|6|Mentioned|p12 Fig.5|||||Unit in Neales River Group.||||
26493|Coorikiana Sandstone|66623|6|Mentioned|p262.|||Equivalent to Coreena Member in NSW.||Unit in Rolling Downs Group in South Australia.||||
26493|Coorikiana Sandstone|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Sandstone, fine-grained, calcareous, clayey; sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|67784|5|Briefly described|p26|Albian|Albian|Southern Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Subsurface only. Shoreface to open marine.||Unit in Marree Subgroup.||Conformably and gradationally overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation.|Silty fine- to medium-grained sand, broadly cross-bedded, buff to yellow.|
26493|Coorikiana Sandstone|68713|6|Mentioned|p22|Cretaceous|Cretaceous|||Of the Marree Subgroup.||||
26493|Coorikiana Sandstone|68715|6|Mentioned|p31 Fig.7|Albian|Albian|||||||
26493|Coorikiana Sandstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (SW). Shallow marine.||Of the Rolling Downs Group.||||
26493|Coorikiana Sandstone|69019|3|Fully described|p85 Fig.21, p97-98.|Albian|Albian|SW Eromanga Basin. Originally defined as a Member of Oodnadatta Formation (Freytag, 1966); elevated to Formation status by Thomson (1980). Type area along Coorikiana Creek, ~40 km SW of Oodnadatta. Thickness varies from <1 to 36 m. Locally an important aquifer.||Unit in Marree Subgroup.||Overlies Bulldog Shale conformably. Is overlain conformably by Oodnadatta Formation.|Coarsening-upwards succession of greenish-white to grey, fine- to very fine-grained sandstone; glauconitic, bioturbated and broadly cross-bedded; sandy siltstone and minor siltstone interbeds; weathers buff to yellow.|
26493|Coorikiana Sandstone|69023|5|Briefly described|p89 Fig.20, p93, p99-100, p102-104, p151|Albian|Albian|See also p191-192. Originally part of Oodnadatta Formation (Freytag, 1966); elevated to Formation status by Thomson (1980). Thickness from <1 to c.35m. Stratigraphic wells intersection data.||Unit in Marree Subgroup.||Conformably overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation.|A coarsening-upwards succession of greenish-white to grey, glauconitic, bioturbated, cross-bedded fine- to very fine-grained sandstone and silty sandstone; minor siltstone interbeds.|
26493|Coorikiana Sandstone|69457|5|Briefly described|p41:3, 6-8|Early Cretaceous|Early Cretaceous|Thomson (1980); Moore and Pitt (1982). Eromanga Basin. Has not been recognised in the NT; the Wilgunya Subgroup nomenclature is thus preferred to the Marree Subgroup.||Marree Subgroup.||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||12-JUL-16
26493|Coorikiana Sandstone|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||||Overlies Bulldog Shale, overlain by Oodnadatta Formation||
26493|Coorikiana Sandstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
26493|Coorikiana Sandstone|69946|3|Fully described|p21-23, p57, p94, p113-119|Albian|Albian|Moore and Pitt (1982). Previously defined as a Member of Oodnadatta Formation by Freytag (1966), whose type section in Coorikiana Creek, 40km SW of Oodnadatta, still applies. Moore, Pitt et al. (1986) designated a subsurface reference section from 1123 to 1131m in Dullingari 1. Typically <20m thick. Wireline log correlations.||Unit in Marree Subgroup.||Conformably overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation. Passes laterally into Wallumbilla Formation and Marree Subgroup.|Fine-grained, silty, glauconitic, feldspathic and lithic sandstone; minor conglomerate with dark grey siltstone and mudstone interbeds at the base.|
26493|Coorikiana Sandstone|69947|5|Briefly described|p9, p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin. Shoreline deposits.||Marree Subgroup.||Overlies Bulldog Shale.||
26493|Coorikiana Sandstone|69948|6|Mentioned|Fig.4.1|||Eromanga Basin.||||||
26493|Coorikiana Sandstone|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Of Marree Subgroup.|||Fine-grained, calcareous, clayey sandstone; sandy siltstone; minor siltstone.|12-JAN-16
26493|Coorikiana Sandstone|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin.||Marree Subgroup.||Gradationally overlies Bulldog Shale.|Mostly subsurface: silty fine- to medium-grained sand, broadly cross-bedded, buff to yellow.|
26493|Coorikiana Sandstone|70821|5|Briefly described|p21 Fig.2.6, p23|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 20m thick. Deposited in a regressive marine, shoreface environment.||||Overlies the Bulldog Shale. Overlain by the Oodnadatta Formation.||
26493|Coorikiana Sandstone|70860|6|Mentioned|p281|||Great Artesian Basin. Mis-spelled as Coorikianna Sandstone.||||||
26493|Coorikiana Sandstone|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.||||
26493|Coorikiana Sandstone|71321|6|Mentioned|p15, p65|||Of Eromanga Basin.||||||24-OCT-19
26493|Coorikiana Sandstone|71342|3|Fully described|Ch1 p19, Ch4 p8, Ch5 p21-p23|Albian|Albian|Originally defined as a member of the Oodnadatta Formation by Freytag (1966) before being elevated to formation status by Moore and Pitt (1982). A type section in Coorikiana Creek was given by Freytag (1966) and a reference section in Dullingari 11 by Moore, Pitt et al (1986). Outcrop, distribution and wireline log characteristics are discussed. Typically less than 20m thick. Sedimentology is discussed briefly. This unit is interpreted to have been deposited in a regressive marine, shoreface environment; however, it should be noted that Alley and White (1996) argue for a middle Albian marine transgressive setting instead. Spore-pollen zone is given in Ch5 p57 and elaborated on in Ch6 p9. Hosts commerically producible oil in Ulandi 12. See also Ch5 p33, Ch5 p57, Ch5 p114-p120, Ch6 p9-p10, Ch7 p10, Ch7 p13, Ch9 p4, Ch9 p9, Ch9 p11, Ch11 p2, Ch11 p5, Ch13 p2.||Marree Subgroup||Conformably overlies the Bulldog Shale. Conformably overlain by the Oodnadatta Formation. Laterally equivalent to the Wallumbilla Formation.|Fine-grained, silty, glauconitic, feldspathic and lithic sandstone with minor conglomerate and dark grey siltstone and mudstone interbeds at the base.|
26493|Coorikiana Sandstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Neales River Group.||Overlies Bulldog Shale. Is overlain by Oodnadatta FZ.||
26493|Coorikiana Sandstone|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet. |||||Sandstone, fine-grained, calcareous, clayey sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains gas.||||||
26493|Coorikiana Sandstone|73249|4|Described|p316-319, p320 Fig.2, p321-324, p326-338|Albian|Albian|Eromanga Basin. Early Albian age. Deposited during a partial marine regression to the southwest of the basin, subtidal to beach and fluvial environment. Typically 20m thick. Dominant clay mineral is montmorillonite, deposited in a more arid, warmer envionment than the Cadna-owie Formation. Unit described as sandstone dominated by other authors (Cotton et al., 2006; van der Weilen et al., 2011) but is mostly clay-rich in the samples studied. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks. [Specific locations in text include p324 Fig.4, p334 Tb.7 and p337 Fig.9.]. See also misspelling Coorkiana Sandstone p322.||||Conformably overlies the Bulldog Shale, conformably underlies the Oodnadatta Formation, lateral equivalent of the Toolebuc Formation.|Sandstone with interbedded siltstone and mudstone, typically 20m thick.|
26493|Coorikiana Sandstone|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Contains[?] gas.||||Underlain by Bulldog Shale. Overlain by Oodnadatta Formation. Equivalent to Wallumbilla Formation.||
26493|Coorikiana Sandstone|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin. Hosts gas.||||Underlain by Bulldog Shale. Overlain by Oodnadatta Formation. Equivalent to Wallumbilla Formation.||
26493|Coorikiana Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p175|Cretaceous|Cretaceous|Eromanga Basin. Shoreface depositional environment.|ca 105 Ma|||Overlies Bulldog Shale, underlies Oodnadatta Formation||
25861|Coorongooba Creek Sandstone|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Nile Subgroup (Illawarra Coal Measures). Medium-grained, quartz-lithic to lithic sandstone; thinly interbedded shale and sandstone. Max. thickness: 19m. Geological Province: Sydney Basin. ||||||
25861|Coorongooba Creek Sandstone|29751|5|Briefly described|P.5|||||||||
25861|Coorongooba Creek Sandstone|34204|6|Mentioned|Table|||||||||
25861|Coorongooba Creek Sandstone|34205|2|Defined|p10|Permian|Permian|||||||
25861|Coorongooba Creek Sandstone|34569|6|Mentioned|p10|||Permian||||||
25861|Coorongooba Creek Sandstone|39232|6|Mentioned|Table 1|||||||||
25861|Coorongooba Creek Sandstone|39293|6|Mentioned|Fig. 8.2|||||||||
25861|Coorongooba Creek Sandstone|40806|2|Defined|p151|Permian|Permian|Prob. Permian||||||
25861|Coorongooba Creek Sandstone|42657|6|Mentioned|Table 1 P74|||||||||
25861|Coorongooba Creek Sandstone|43360|14|Not recorded|Map Legend||Permian|(Provisional first edition) Part Nile Sub-Group of Illawarra Coal Measures.||||||21-MAY-08
25861|Coorongooba Creek Sandstone|43363|14|Not recorded|Map Legend|||(Provisional first edition)||||||
25861|Coorongooba Creek Sandstone|45090|6|Mentioned|p218|||Tatarian.||||||
25861|Coorongooba Creek Sandstone|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Unit in Nile Subgroup.||Overlies Mount Marsden Claystone. Is overlain by Gundangaroo Formation.||
27134|Cootralantra Granodiorite|22815|4|Described|p55|Silurian|Silurian|Rb/Sr Ages: 421Ma and 418+/-2.7 Ma.||||||
27134|Cootralantra Granodiorite|23439|5|Briefly described|p136|||Of the Bullenbalong Supersuite.||||||21-MAY-08
27134|Cootralantra Granodiorite|23551|5|Briefly described|p490|||S-type granite. Lachlan Fold Belt.||||||
27134|Cootralantra Granodiorite|33779|6|Mentioned|p168|||Map||||||
27134|Cootralantra Granodiorite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
27134|Cootralantra Granodiorite|33852|6|Mentioned|p500|||Date given.||||||
27134|Cootralantra Granodiorite|35109|2|Defined|p37|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
27134|Cootralantra Granodiorite|35192|6|Mentioned|p281|||||||||
27134|Cootralantra Granodiorite|36411|6|Mentioned|p268|||Refers White et al 1977 for definition.||||||
27134|Cootralantra Granodiorite|38327|6|Mentioned|Table 4|||||||||
27134|Cootralantra Granodiorite|38500|6|Mentioned|p81|||||||||
27134|Cootralantra Granodiorite|39240|5|Briefly described|p80|||||||||
27134|Cootralantra Granodiorite|39564|6|Mentioned|p16|||||||||
27134|Cootralantra Granodiorite|39721|6|Mentioned|p48|||||||||
27134|Cootralantra Granodiorite|40328|4|Described|p204|||||||||
27134|Cootralantra Granodiorite|40738|6|Mentioned|Fig.1|||||||||
27134|Cootralantra Granodiorite|41905|6|Mentioned|p42|||||||||
27134|Cootralantra Granodiorite|43158|6|Mentioned|9,10|||||||||
27134|Cootralantra Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Of the Bullenbalong Suite.||||||21-MAY-08
27134|Cootralantra Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb22.||||||
27134|Cootralantra Granodiorite|49705|5|Briefly described|p17|||||||||
27134|Cootralantra Granodiorite|60078|6|Mentioned|Map Legend||Silurian|||||||
27134|Cootralantra Granodiorite|67060|5|Briefly described|p503.|||S-type. Composed of at least a dozen individual intrusions with identical chemical composition and lithology.|428.7 +/- 4.3 Ma.|||||15-MAR-12
27134|Cootralantra Granodiorite|68310|6|Mentioned|p240|||Berridale Batholith. An S-type granite completely surrounding the younger (intruding) I-type Tara Granodiorite. Chemical analysis of schistose enclaves tabulated.|||||S-type granite.|
27134|Cootralantra Granodiorite|70125|5|Briefly described|p394|||Berridale Batholith.|430 Ma.||||S-type.|
27134|Cootralantra Granodiorite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. S-type. Hf and O18 isotope data included.|430 Ma|||||
27134|Cootralantra Granodiorite|72571|5|Briefly described|p90, p92, p94, p96-98, p100-101|||Of the Tasmanides of eastern Australia. Petrography of sample and zircon description and analyses are discussed in detail. S-type.|||||Mafic cordierite granite with ilmenite.|
34439|Copes Creek Andesite|22750|4|Described|p 228|||||||||
34439|Copes Creek Andesite|22768|6|Mentioned|p181|||||||||
34439|Copes Creek Andesite|22857|5|Briefly described|p181, p484 App.1 Tb.A1.6|Middle Devonian|Early Devonian|Of the Tamworth Group. Max. thickness: 300m. Geological Province: Tamworth Forearc Basin.||||||09-MAR-06
34439|Copes Creek Andesite|68005|5|Briefly described|p49 Fig.3-M, p50, p151, p170.|Lochkovian|Pridoli|Tamworth Belt. Fig.3-M shows this as a separate unit; the text states it is part of Drik-Drik Formation. Intrudes lower part of Drik-Drik Formation.||Basal unit in Tamworth Group.||Is overlain by and intrudes Drik-Drik Formation; is overlain by Bog Hole Formation.|Massive, green to grey keratophyre and quartz-keratophyre, minor brecciated or vesicular keratophyre.|
79315|Copeton Monzogranite|71628|4|Described|p4: 1, 3-4, 13-14, 16-22, 34, 37, 40,42|||See also p8-44; p19-43. Bryant and Chappell (2010). Southern New England Orogen. Named after Copeton Dam. Crops out over ~55 km long (N-S) and up to 20 km wide (E-W). Forms extensive sheets and massive tors. Several other age determinations given and zircon cores briefly discussed. Lithology, geochemistry detailed. Has been used as a source of dimension stone and rock aggregate.|288.7 +/- 2.9 Ma (SHRIMP: Rosenbaum et al., 2012).|Copeton Suite.|Sepoy Monzogranite Phase.|Intrudes Bobs Creek Formation (Woolomin Group), Whitlow and Cara Formations and Sandon beds. ?Abuts the Namoi Tops Monzogranite. Is intruded by Gilgai Leucogranite and Tingha Monzogranite.|Coarse-grained, porphyritic biotite (+/- muscovite, +/- cordierite) monzogranite and syenogranite; minor fine- and medium-grained variants. Numerous tourmaline-rich pods, veins and pegmatitic segregates; abundant rounded sedimentary? xenoliths.|
82398|Copeton Suite|71628|5|Briefly described|p4: 18, 21, 36, 41|||Said to be part of Bundarra Supersuite on p8-44.||Copeton Supersuite.|Copeton, Linton, Namoi Tops Monzogranites.|||
34357|Copi Dam Arenite Member|22730|4|Described|p559,61,62,69|Eifelian|Emsian|Variation on reserved name Copi Dam Sandstone Member.||||||
34357|Copi Dam Arenite Member|22857|5|Briefly described|p486 App.1 Tb.A1.7|Middle Devonian|Early Devonian|Of the Coco Range Sandstone. Pebbly coarse-grained arenite, fine arenite. Geological Province: Ravendale Basin.||||||
34357|Copi Dam Arenite Member|60648|6|Mentioned|p47, p50|Eifelian|Emsian|See also Copi Dam Member, Copi Dam Arenite and Copi Dam Pebbly Arenite Member.||||||26-APR-05
34357|Copi Dam Arenite Member|65759|5|Briefly described|p131|||Darling Basin. In Coco Range Sandstone. Braided fluvial lithofacies, predominantly medium to coarse pebbly sandstone, often with a basal lag of quartz pebbles and granules and shale or siltstone intraclasts.||||||
34357|Copi Dam Arenite Member|67562|6|Mentioned|p103|||~ 30m thick. See also Copi Dam Member p101.||Of the Coco Range Sandstone.||||23-JAN-17
68844|Copper Hill Suite|24518|5|Briefly described|p66|Late Ordovician|Late Ordovician|Porphyries. Mainly of dacitic composition. See also Copper Hill suite. Age: ~450-445Ma.||||||04-MAY-05
68844|Copper Hill Suite|63277|6|Mentioned|p138|Ordovician|Ordovician|Correlated with Cowal and Narromine Igneous Complexes. Age of emplacement of porphyries: 452-445Ma. Dominantly of dacitic porphyries, with distinctive medium-K calc-alkaline compositions. Geological Province: Lachlan Fold Belt.||||||21-FEB-23
68844|Copper Hill Suite|63278|5|Briefly described|p148, p161|Ordovician|Ordovician|Age: 456-447Ma Zircon rims (Crawford et al. 2007a) Geological Province: Molong Volcanic Belt, Lachlan Fold Belt.||||||07-FEB-11
68844|Copper Hill Suite|63283|5|Briefly described|p182, p191 Tb. 2, p206, p208, p209|Middle Ordovician|Middle Ordovician|Age: 448Ma (diorite intrusive + dacite intrusive). Consists; medium-K calc-alkaline largely felsic rocks that occurs in all three volcanic belts. See also p206. Name refers to a wide spread magmatic suite.||||||07-FEB-11
68844|Copper Hill Suite|63284|4|Described|p249, p253-255, p259, p268|Ordovician|Ordovician|Age: ca 455-445Ma. Intrusive dacites and granodiorites. Rocks described by Blevin (2002). See also p249, p253-255.||||||
68844|Copper Hill Suite|63285|6|Mentioned|p274, p288|||Consists of medium-K calc-alkaline dacitic intrusions.||||||
68844|Copper Hill Suite|63286|6|Mentioned|p304|Ordovician|Ordovician|Consists of dacites that are medium-K calc-alkaline suites.||||||07-FEB-11
68844|Copper Hill Suite|63293|5|Briefly described|p467, p470, p473|Late Ordovician|Middle Ordovician|Age: ca 453-450Ma. Small volume mainly felsic plutons with distinctive medium-K calc-alkaline composition.||||||07-FEB-11
68844|Copper Hill Suite|67106|6|Mentioned|p672, 679, 681||||450 Ma.|Narromine Igneous Complex.|||A small number of typically dacitic/granodioritic/tonalite intrusions.|
68844|Copper Hill Suite|67107|6|Mentioned|p700|||Mentioned in the context of source of anomalous Pb.||||||
68844|Copper Hill Suite|70684|5|Briefly described|p8 Fig.3(d), p12|Late Ordovician|Late Ordovician|Macquarie Arc. Age is c.450 Ma in the type area.|455-433 Ma.||||Porphyritic dacites and associated holocrystalline diorites and granodiorites with medium-K calc-alkaline compositions.|
68844|Copper Hill Suite|72263|5|Briefly described|p515,517|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen. Also referred to as Copper Hill Intrusion or Copper Hill porphyry in text. Associated with phase 3 volcanism c. 456-445 Ma within the Macquarie Arc, emplaced in the southern Molong Volcanic Belt. Intrudes into Fairbridge Volcanics.|446+\-6 Ma (K-Ar, hornblende)|||||
68844|Copper Hill Suite|73154|6|Mentioned|p92|Late Ordovician|Late Ordovician|Macquarie Arc, Phase 3. Quartz-bearing and medium-K. See also Copper Hill suite p75, p84, p92.|ca. 458 Ma|||||
37349|Copper Mine Range Formation|66623|1|Redefined|pp43-45, p31, p36 . |Early Cambrian|Early Cambrian|Redefined: formerly Copper Mine Range Beds (Pogson and Scheibner 1971) and beds (Scheibner and Basden 1998). Now included in Teltawongee Group. Contains sponge spicules, brachiopods; also glauconite-bearing dolomite beds in the northwest. About 1.5 km thick.||Unit in Teltawongee Group.||Overlies Bunker Creek and Kara Formations of Grey Range Group. Is unconformably overlain by Kandie Tank Limestone and Cupala Creek Formation, and by Muckabunnya Formation to the west.|Wide variety of lithologies. Grey, dark green-grey and maroon mudstone and siltstone, sporadically laminated but generally massive bedding; quartzite and ? conglomerate. Local black carbonaceous shale and siltstone, individual beds to 5 m thick.|24-SEP-13
37349|Copper Mine Range Formation|67105|6|Mentioned|p655|Cambrian|Cambrian|Occurs E of the Koonenberry Fault. Contains detrital zircons derived from a distal southern source, e.g. Ross Orogen in E Antarctica.||Teltawongee Group.||||
37349|Copper Mine Range Formation|67322|5|Briefly described|p10-11; Fig.5|Middle Cambrian|Early Cambrian|Redefined by Mills (in Greenfield et al., 2010). Age based on a trace fossil assemblage including Chondrites sp.and Planolites sp. (Webby 1984). Occurs in the Coturaundee Range, Kayrunnera-Koonenberry region.||Unit in Teltawongee Group.||?Unconformably overlain by the Williams Creek Conglomerate (Kayrunnera Group).||21-FEB-18
37349|Copper Mine Range Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|||Teltawongee Group|||Red, maroon, dark green-grey metamudstone and metasiltstone, lesser yellow dolomite and quartzite; traction current structures; turbidite and sedimentary slumping; rare Early-Middle Cambrian trace fossils, brachiopods and sponge spicules.|
37349|Copper Mine Range Formation|73059|6|Mentioned|p1061|||Appears mis-spelt as Cooper Mine Range Formation. Detrital zircon ages mentioned.||Teltawongee Group.||||
31721|Copperhannia Member|22679|3|Fully described|p 34|Devonian|Devonian|Formerly part of the Copperhannia Formation.||||||22-MAY-08
31721|Copperhannia Member|22857|4|Described|p472 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Cunningham Formation. Calcarenite, slate, limestone, marble, conglomerate. Max. thickness: ~300m. Geological Province: Hill End Trough.||||||
31721|Copperhannia Member|23214|4|Described|p202|Early Devonian|Early Devonian|A limestone bearing unit at the base of Cunningham Formation. Max. thickness 800m.||||||
31721|Copperhannia Member|43654|5|Briefly described|Map Legend|Devonian|Devonian|Of Cunnungham Formation. Calcarenite, slate, limestone, marble, conglomerate.||||||17-JUL-08
31721|Copperhannia Member|43782|5|Briefly described|Map Legend|Pragian|Pragian|Of Cunningham Formation.||||||22-MAY-08
31721|Copperhannia Member|50233|5|Briefly described|Map Legend|Pragian|Pragian|Of the Cunningham Formation. Calcarenite, slate, limestone, marble, conglomerate.||||||
31721|Copperhannia Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Cunningham Formation. Calcarenite, slate, limestone, marble, conglomerate.||||||
31721|Copperhannia Member|68592|2|Defined|p681, p1204-5, p1209-13, p1907|Early Devonian|Early Devonian|Formerly Copperhannia Formation (Langley, 1976) after unpublished work by Hobbs (1964). Type section described. 100m thick, thinning southwards. N of the map area, up to 300m thick. Near-vertical dip with a subparallel cleavage. Age from conodont elements.||Unit in Cunningham Formation.||Is faulted against Box Ridge Volcanics.|Limestone; cleaved and finely recrystallised, appearing as a cleaved white marble on freshly broken surfaces.|
31721|Copperhannia Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dxnc. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||In lower part of Cunningham Formation.|||Recrystallised limestone.|
31721|Copperhannia Member|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|Shown as Copperhannia Mbr.||Cunningham Formation||||
31721|Copperhannia Member|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Cunningham Formation|||Recrystallised limestone.|
31721|Copperhannia Member|71656|5|Briefly described|p13 Fig.2, p41|Pragian|Pridoli|Shown in Fig.2 as Pragian. Conodonts indicate Pridoli to early Devonian age. Includes a thin-bedded calcarenite with identifiable conodonts.||Shown near base of Cunningham Formation.|||Includes thin-bedded calcarenite containing conodonts.|
40929|Copplestone Member|50230|4|Described|Map legend|Wenlock|Wenlock|Of the Yass Formation (Douro Group).  Interbedded with the Snow Member within the Yass Formation. Partly overlain by and interbedded with the Boambolo Member.  Variably interbedded siliclastic and carbonate strata.||||||10-MAY-04
40929|Copplestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Ravenswood Fm (Douro Gp). Variably interbedded siliciclastic + carbonate strata. Limestone of pebble- to cobble-sized biohermal clasts in micritic matrix. Sporadic bimodal (v.coarse + v.fine-gr.) quartz litharenite; small cobble clasts of muddy limest.||||||09-SEP-08
40929|Copplestone Member|68592|2|Defined|p428, p433, p436, p440, p473-6, p482-7|Wenlock|Wenlock|See also p1875. Name first published by Cramsie et al. (1978); its usage by Feary (1984, 1986) introduced "considerable confusion", being applied as a Formation to the overlying part of the former Glen Bower Formation. This study restores the Copplestone Member to its former status, but retains Feary's modification to the base to include the first appearance of carbonates. Type and reference sections described. 40-70m thick. Restricted to Boambolo region. Nearshore shallow-water environments. Very fossiliferous: stromatoporoid colonies, several types of corals, and conodonts. Mid-Wenlock.||Unit in Glen Bower Formation.||Overlies Wyelba Member conformably. Is overlain conformably by Connell Member. Correlates with Yass Formation.|Laminated algal limestones interbedded with mudstones containing sporadic carbonate nodules and lenses; subordinate coarse-grained quartz-lithic sandstones with biohermal fossiliferous limestone at the top.|
40929|Copplestone Member|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdgp. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Glen Bower Formation||Appears to be overlain by Connell Member. Overlies Wyelba Member.|Laminated, algal limestone interbedded with mudstone and muddy limestone with sporadic carbonate nodules and lenses; coarse grained, quartz lithic sandstone; biohermal fossiliferous limestone and limestone breccia.|
40929|Copplestone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Glen Bower Formation|||Laminated, algal limestone interbedded with mudstone and muddy limestone with sporadic carbonate nodules and lenses; coarse grained, quartz lithic sandstone; biohermal fossiliferous limestone and limestone breccia.|
40929|Copplestone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Glen Bower Formation|||Laminated, algal limestone interbedded with mudstone and muddy limestone with sporadic carbonate nodules and lenses; coarse grained, quartz lithic sandstone; biohermal fossiliferous limestone and limestone breccia.|
24228|Coradgery Monzonite|40365|2|Defined|p325|Middle Devonian|Middle Devonian|||||||
34755|Corangula Formation|22892|6|Mentioned|p41|||||||||
26498|Corona Dolomite|22772|5|Briefly described|Table13.1|Neoproterozoic III|Cryogenian|||||||
26498|Corona Dolomite|22857|5|Briefly described|Tb 13.1 (insert p70), p400 App.1 Tb A1.3|Sturtian|Sturtian|Of the Eurowie Subgroup (Torrowangee Group). Massive, recrystallised, homogeneous, buff-coloured dolomite. Age: ~700Ma. Geological Province: Adelaide Fold Belt. ||||||
26498|Corona Dolomite|23368|6|Mentioned|p61|||||||||
26498|Corona Dolomite|30261|4|Described|Table 1|||Sturtian - Marinoan age.||||||26-MAY-08
26498|Corona Dolomite|31012|6|Mentioned|p10|||Adelaidean||||||
26498|Corona Dolomite|33875|6|Mentioned|p22|||Uranium deposit.||||||
26498|Corona Dolomite|34812|4|Described|p82|||||||||
26498|Corona Dolomite|34814|6|Mentioned|p282|||||||||
26498|Corona Dolomite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26498|Corona Dolomite|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
26498|Corona Dolomite|36733|6|Mentioned|Table 5|||||||||
26498|Corona Dolomite|37931|4|Described|p532|||||||||
26498|Corona Dolomite|39214|6|Mentioned|p7|||||||||
26498|Corona Dolomite|41405|5|Briefly described|p204|||||||||
26498|Corona Dolomite|46889|6|Mentioned|p272|||||||||
26498|Corona Dolomite|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Euriowie Subgroup.||||
26498|Corona Dolomite|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Euriowie Subgroup.||Overlies McDougalls Well Conglomerate. Is overlain by Floods Creek Formation.|Massive, poorly bedded, locally strongly recrystallised, yellow to buff-coloured dolomite.|08-SEP-15
73368|Coronga Peak Quartzite|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Kopyje Group.|||White to pale grey, fine- to medium-grained (rarely coarser), quartzose variably recrystallised sandstone; rare pebbly beds.|
73368|Coronga Peak Quartzite|69095|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Kopyje Group.||Is overlain ?conformably by Meryula Formation.|White to pale grey, fine- to medium-grained (rarely coarser), quartzose, variably recrystallised sandstone with rare pebbly beds; contains sporadic fossilised worm burrows.|
73368|Coronga Peak Quartzite|69635|4|Described|p75-83, p105-112, p69|Early Devonian|Late Silurian|North-western Lachlan Orogen. U-Pb SHRIMP zircon maximum depositional age.|471+/-12 Ma; 500+/-7 Ma|Of Kopyje Group.||Interfingers with Drouin Conglomerate Member in places. Detrital age spectrum compared with Girilambone Group.|Bioturbated quartzite containing worm burrow casts up to ~3 cm in diameter. Shallow marine facies?; Massive quartzite with occasional laminations, and represents partially recrystallised quartz-rich sandstone.|
73368|Coronga Peak Quartzite|70941|2|Defined|pviii, px, p4, p7 fig 3|Early Devonian|Late Ludlow|Time equivalent of the Meryula Formation. Name derived from Coronga Peak hill. Distribution, geomorphology, structure, metamorphism,  fossil assemblage, geophysical  and distinguishing characteristics  discussed. Deposited in a shallow marine/beach environment on the basis of fossilised worm burrows and cross bedding. Age inferred from stratigraphic relationships. Estimated thickness of over 450m in the map area. Type area mentioned and briefly described. Interfingers and may be equivalent to Drouin Conglomerate Member.  See also  p8 fig 4, p21, p27, p76,  p77 fig 31, p80 fig 33, p81-p85, p87,  p88, p94, p115, p122, p126-p130, p137, p140 fig 58||Kopyje Group||Interfingers with and is conformably overlain by Meryula Formation. Unconformably overlies or is locally faulted against the Girilambone Group.|White to pale grey, fine to medium grained, moderately to well sorted quartz rich sandstone. Quartzite with minor siltstone and chert grains with detrital muscovite/sericite.  Accessory tourmaline, zircon and pyrite occurs in the quartzite.|
73368|Coronga Peak Quartzite|71039|6|Mentioned|p13|||Northern and western exposures of the Kopyje Group.||Kopyje Group||||
73368|Coronga Peak Quartzite|71360|5|Briefly described|Map legend|Late Silurian|Late Silurian|Geophysical signature: non-magnetic unit not distinguishable in aeromagnetic data but shows low counts in a ternary radioelement image; boundaries are based on geological mapping. Age interpreted from mapping in Byrock and Sussex 1:100 000 map sheet areas.||Kopyje Group.||In Byrock and Sussex 1:100 000 map sheet areas, interfingers with Drouin Conglomerate Member (Meryula Formation).|Metamorphosed fine- to medium-grained quartzose sandstone, rare pebbly beds.|
78901|Corradigbee Formation|67823|5|Briefly described|p355-p368|Middle Devonian|Early Devonian|New name; of Hunt and Young (2010). Change from a well-drained system in the lower part, to swampy conditions. Represents a more distal part of a humid fan deposit. Contains abundant plant remains in both sandstone and mudstone lithologies. Contains a unique fossil fish assemblage.||Of the Hatchery Creek Group.||Overlies Wee Jasper Formation.|Sequence of grey-black siltstones and mudstones.|
78901|Corradigbee Formation|68592|4|Described|p1193-1202, p1907-8|Middle Devonian|Middle Devonian|260m thick. The Eifelian fossils, which occur in calcareous nodules in mudstone, are listed.||Unit in Hatchery Creek Group.||Overlies Wee Jasper Formation.|Consists of 15 or more fining-up cycles, consisting of basal, fine-grained, grey sandstone; grey, orange and dark red mudstones that are largely unfossiliferous; and grey mudstones rich in fish and plant remains.|
78901|Corradigbee Formation|71656|4|Described|p12 Fig.2, p38|Eifelian|Emsian|Includes early to mid Eifelian fish fossil fauna. Outcrop of the Hatchery Creek Group is bounded by the Goodradigbee Valley to the east, the Burrinjuck Granite to the west, and Burrinjuck Reservoir to the north.  Finer-grained than underlying Wee Jasper Formation.||Hatchery Creek Group.||Overlies Wee Jasper Formation.|Includes calcareous nodular mudstone.|
36774|Corridgery Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Part of the Marulan Batholith.||||||
36774|Corridgery Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Pink and green, medium- to coarse-grained, massive, equigranular and porphyritic, biotite-hornblende granite. High to very high magnetic susceptibility.||||||
36774|Corridgery Granite|68592|2|Defined|p1611, p1626-9|Early Devonian|Early Devonian|New name, after Corridgery property. Mapped and described informally as 'Rosedale Granodiorite' by Erickson (1986). Forms two small intrusions in the Big Hill area, 20km N of Marulan; possibly a sill-like body. Type locality described. Geochemistry and geophysical properties described. Probable magmatic association with the volcanics of the Bindook Group; this, and intrusive relationships, suggest a mid to late early Devonian age.||Unit in Arthursleigh Suite.||Intrudes Tangerang Formation (and possibly other units) in Bindook Group.|Uniform internal composition. Pink and green, medium- to coarse-grained, weakly porphyritic to equigranular, massive, biotite-hornblende granite. Contains rare meta-volcanic and sedimentary xenoliths near the margin.|
36774|Corridgery Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dac. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. [Note: shown erroneously as 'Dao' Corridgery Granite on Taralga 1:100 000 sheet].||Arthursleigh Suite|||Medium-coarse grained, massive, equigranular-weakly porphyritic, biotite-hornblende granite; high-very high magnetic susceptibility.|
36774|Corridgery Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Arthursleigh Suite|||Pink to green, medium to coarse-grained, massive equigranular to weakly porphyritic biotite-hornblende granite. Has a high to very high magnetic susceptibility.|
36774|Corridgery Granite|70543|5|Briefly described|Map Legend|Devonian|Devonian|[shown as Columba Granite on Goulburn 1:250 000 sheet]||Arthursleigh Suite|||Medium-coarse grained, massive, equigranular-weakly porphyritic, biotite-hornblende granite; high-very high magnetic susceptibility.|
38278|Cottesbrook Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Medium- to coarse-grained, grey, biotite-hornblende monzogranite, weakly porphyritic in places; abundant encalves in places; variable texture.  An I-type granitoid.||||||20-DEC-04
38278|Cottesbrook Monzogranite|23812|5|Briefly described|p20 Tb.2|Early Triassic|Late Permian|||||||
38278|Cottesbrook Monzogranite|69639|4|Described|p1, p5, p8, p32, p62, p68-72|Lopingian|Lopingian|New England Orogen. Contact with the Billyrimba Leucomonzogranite is obscured by poor outcrop. Sampling locality, petrography and geochronology are discussed. See also p95, p133, p219-p221, p240.|253.4 +/- 1.1 Ma (SHRIMP)|Wards Mistake Suite||Intrudes (inferred) Dundee Rhyodacite, Billyrimba Leucomonzogranite and the Mount Jonblee Leucomonzogranite.|Grey-white, medium-grained granodiorite with sparse porphyritic amphibole.|
38278|Cottesbrook Monzogranite|70217|5|Briefly described|p73 tbl 14.1|Changhsingian|Wuchiapingian|New England Orogen. Age derived from Chisholm et al, 2014b.|253.4 +/- 1.1 (SHRIMP U-Pb)|Uralla Supersuite||||
38278|Cottesbrook Monzogranite|71628|4|Described|p8: 4, 79-82; p11: 10-11; p14:12; p15:5|||Henley et al. (2001). Originally the Cottesbrook Adamellite (Pogson and Hitchins, 1973). Named after Cottesbrook Creek. Occurs ~7km E of Sandy Flat, c.20km S of Tenterfield. Comprises two irregularly-shaped bodies. Crops out poorly; is deeply weathered. Geochemistry described; similar to Wards Mistake Monzogranite. RELATED UNITS (continued): Is partly bound by Mount Jonblee Leucomonzogranite.|253.4 +/- 1.1 Ma (SHRIMP: Chisholm et al., 2014).|Wards Mistake Suite.||Intrudes Wandsworth Volcanic Group (Dundee Rhyodacite), and ""bounds"" (?intrudes) Mount Jonblee and Bungulla Monzogranites. Is intruded by Billyrimba Leucomonzogranite. See COMMENTS for more.|Texturally heterogeneous, grey, medium- to coarse-grained, equigranular to porphyritic monzogranite with minor quartz monzonite; xenoliths locally abundant. I-type.|
27752|Cotton Formation|13139|5|Briefly described|p9 Fig. 4|Llandovery|Llandovery|Geological Province: Junee-Narromine Volcanic Belt.||||||
27752|Cotton Formation|22519|6|Mentioned|p7|Devonian|Ordovician|||||||
27752|Cotton Formation|22638|6|Mentioned|p8||Bolindian|||||||
27752|Cotton Formation|22831|3|Fully described|p 31|Llandovery|Ordovician|||||||
27752|Cotton Formation|22857|5|Briefly described|p127, p416 App. 1 Tb. A1.5|Silurian|Late Ordovician|Well-bedded fine quartzose arenite and laminated siltstone, minor chert.||||||
27752|Cotton Formation|23245|6|Mentioned|p127|||||||||
27752|Cotton Formation|23309|6|Mentioned|p390|||||||||
27752|Cotton Formation|23334|5|Briefly described|9 Fig.4|Early Silurian|Late Ordovician|||||||
27752|Cotton Formation|23538|6|Mentioned|p 458|||||||||
27752|Cotton Formation|23737|4|Described|p87|Llandovery|Bolindian|Maximum thickness: 1500m.||||||
27752|Cotton Formation|24125|5|Briefly described|p3|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
27752|Cotton Formation|24265|5|Briefly described|p1450||Early Silurian|Geological Province: Lachlan Fold Belt||||||
27752|Cotton Formation|24417|3|Fully described|p35|Llandovery|Bolindian|Previously named "Cotton Series" (Andrews, 1910) and "Cotton Beds" (Sherwin, 1973b) before being upgraded to formation status by Sherwin et al (1987).  Max. thickness: 1500m.||||||
27752|Cotton Formation|40891|3|Fully described|p10|||Formerly Cotton Series.||||||27-NOV-06
27752|Cotton Formation|42262|6|Mentioned|Fig. 2 P1810|||||||||
27752|Cotton Formation|42489|5|Briefly described|Map legend|Llandovery||||||||
27752|Cotton Formation|42718|5|Briefly described|p1|||||||||
27752|Cotton Formation|42920|6|Mentioned|Fig.2|||||||||
27752|Cotton Formation|43263|6|Mentioned|Map Legend|Early Silurian|Late Ordovician|||||||
27752|Cotton Formation|43441|5|Briefly described|17, 21|||Age: ?Late Ordovician -  Early Silurian. Includes part of Mugincoble Chert||||||08-JAN-10
27752|Cotton Formation|44093|5|Briefly described|p178 App. 1||Ordovician|In the Parkes Zone. Min Age: maybe Silurian? Geological Province: Lachlan Fold Belt.||||||
27752|Cotton Formation|44160|5|Briefly described|Map Legend||Llandoverian|||||||
27752|Cotton Formation|46522|2|Defined|p40|Late Ordovician||No internal evidence for age.||||||26-MAY-08
27752|Cotton Formation|46525|6|Mentioned|p152|||See also Fig.8||||||
27752|Cotton Formation|46528|5|Briefly described|Map legend|Silurian||||||||
27752|Cotton Formation|50299|5|Briefly described|Map Legend|Ordovician|Ordovician|Underlies undifferentiated rocks of the Forbes Group.||||||26-MAY-08
27752|Cotton Formation|60008|5|Briefly described|Map Legend|Silurian|Ordovician|Sediments and/or volcanics?||||||
27752|Cotton Formation|60009|5|Briefly described|Map Legend|Llandovery|Bolindian|Overlies Northparkes Volcanic Group.||||||26-MAY-08
27752|Cotton Formation|61893|6|Mentioned|p244, p249-250|Late Ordovician|Late Ordovician|Sherwin (1973). W of Forbes. Bolindian age. Fauna listed. A close analogue to the Jingerangle Formation in terms of lithology, depositional environment and age.||||||
27752|Cotton Formation|63083|6|Mentioned|p218|Telychian|Telychian|In central NSW. Contains Llandovery trilobite fauna.||||||07-FEB-11
27752|Cotton Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p150, p151|Early Silurian|Late Ordovician|Geological Province: Junee-Narromine Volcanic Belt, LFB. Consists of fine-grained siltstone, with isolated calcareous horizons containing a shallow-water coralline assemblage. Lower part of unit has little or no sign of volcanic input.||||||07-FEB-11
27752|Cotton Formation|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
27752|Cotton Formation|63283|5|Briefly described|p192, p196 Fig. 4, p210|Early Silurian|Early Silurian|Structurally and conformably interfinger with Bushman and Nash Hill Volcanics. Consists of a detrital quartz-rich part.||||||07-FEB-11
27752|Cotton Formation|63289|6|Mentioned|p373 Fig. 7|Silurian|Late Ordovician|Underlain by Northparkes Group. Consists of quartz-rich distal turbidites.||||||07-FEB-11
27752|Cotton Formation|63290|5|Briefly described|p395, p393 Tb. 1, p397 Fig. 3(b)|Llandovery|Bolindian|Underlain by Wombin Volcanics. Age: ca 443Ma. Geological Province: Junee - Narromine Volcanic Belt. Consists volcaniclastic bands with quartz detritus in the bands also ashfall deposits.||||||
27752|Cotton Formation|63291|6|Mentioned|p419 Fig. 2|||||||||
27752|Cotton Formation|63293|5|Briefly described|p475, p468 Fig. 2|Llandovery|Bolindian|Overlies Wombin Volcanics. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
27752|Cotton Formation|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
27752|Cotton Formation|67107|6|Mentioned|p693, 696|||Goonumbla district, 20km NW of Parkes. Junee-Narromine Volcanic Belt.||||Overlies Goonumbla Volcanics.||
27752|Cotton Formation|67322|5|Briefly described|p20|Early Silurian|Early Silurian|(Krynen et al. 1990; Warren et al. 1995). Proposed but unsupported ages. Occurs in the Parkes-Forbes-Junee area. |||||Siltstones with minor chert beds.|21-FEB-18
27752|Cotton Formation|67805|6|Mentioned|p73|Silurian|Ordovician|||||||
27752|Cotton Formation|67821|6|Mentioned|p170, p173, p177, p181-182|Ordovician|Ordovician|Peak Hill district. Late Llandovery age.||||||
27752|Cotton Formation|67847|5|Briefly described|p21-p22|Early Silurian|Late Ordovician|||||Equivalent to the Bribbaree, Bronxhome and Trigalong Formations.||
27752|Cotton Formation|68003|5|Briefly described|p23, p24 Fig.3-e, pp147-148. |Ordovician|Ordovician|Lachlan Fold Belt. Post-tectonic granites.|||||Quartzose turbiditic sandstones and siltstones; phyllite and shale; meta sandstone; chert.|
27752|Cotton Formation|68004|6|Mentioned|p115.|Late Ordovician|Late Ordovician|Mineral potential and level of certainty are discussed.||||||
27752|Cotton Formation|70036|5|Briefly described|Map legend|Ordovician|Ordovician|Lachlan Fold Belt. Included in a mapped unit of strongly deformed basaltic metasedimentary rocks, basalt, conglomerate, sandstone and mudstone.||||||
27752|Cotton Formation|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
27752|Cotton Formation|70684|6|Mentioned|p3, p9 Fig.4(g), p54-55, p74-75|Early Silurian|Late Ordovician|Junee-Narromine Volcanic Belt.||||||
27752|Cotton Formation|70754|6|Mentioned|p451|||Forbes area.||||||
27752|Cotton Formation|71040|6|Mentioned|p15, p17-18|Silurian|Ordovician|Central NSW.||||||
27752|Cotton Formation|72082|6|Mentioned|p22|Early Silurian|Late Ordovician|Forbes 1:250K sheet area. Age based on Bolindian to late Llandovery graptolites.||||||
27752|Cotton Formation|72495|5|Briefly described|p218, 222, 225, 227, 230, 231, 233, p235|Llandovery|Late Ordovician|||||Interfingers with the Nash Hill Volcanics and the Bushmans Volcanics. Faulted against the Goonumbla Volcanics and the Forbes Group.|Fine-grained, plagioclase-rich turbidites.|02-MAR-20
27752|Cotton Formation|73154|5|Briefly described|p77 Fig.3|Llandovery|Bolindian|Macquarie Arc, Phase 4. Junee-Narromine Belt.||||Overlies Wombin Volcanics.|Siltstone.|
27752|Cotton Formation|73492|5|Briefly described|p691, p693|Early Silurian|Late Ordovician||||||Includes graptolitic siltstone.|
76148|Coturaundee Range Ultramafic|66623|2|Defined|pp193-194, pp212-214.|Permian|Middle Devonian|Formerly Cupala Creek kimberlitic sill (Bottrill and Neef 1998), Cupala Creek ultramafic sill (Stevens et al. 2000); defined in this study. Coturaundee Range. A phlogopite-rich sill, 1500 m long and up to 100 m thick, cut by dykes of darker grey basalt. Not brecciated, unlike diatremes, except for irregular and brecciated contacts with host sandstone.||||Intrudes Muckabunnya Formation.|Grey, phlogopite-rich rock, up to 20% pseudomorphs of serpentine after euhedral olivine; minor fine-grained secondary andradite; rare diopside; common accessory perovskite, sphene and apatite.|
27265|Couragago Granodiorite|36441|5|Briefly described|map legend|Pridolian|Pridolian|Of Young Batholith. Intrusive. S-type. Granodiorite, adamellite. Intruded by Burrinjuck Adamellite. BMR map code: Syc.||||||
27265|Couragago Granodiorite|39660|6|Mentioned|p449|||||||||
27265|Couragago Granodiorite|42313|6|Mentioned|p135|||Subdivision of Young Granodiorite||||||
27265|Couragago Granodiorite|45147|2|Defined|M238|Late Silurian|Late Silurian|Prob.Late Silurian||||||
28479|Cow Flat Granite Porphyry|36441|5|Briefly described|map legend|Pridolian|Pridolian|Of Murrumbidgee Batholith. Intrusive. S-type. Leucocratic quartz feldspar porphyry. Intrudes Tidbinbilla Quartzite and Adaminaby Beds. BMR map code: Scf.||||||
28479|Cow Flat Granite Porphyry|44092|5|Briefly described|map legend|Silurian|Silurian|glw2||||||
28479|Cow Flat Granite Porphyry|45147|3|Fully described|M206|||||||||
28479|Cow Flat Granite Porphyry|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
27135|Cowcumbala Rhyolite|22638|1|Redefined|p63||Early Devonian|Of the Cootamundra Group. 1750 m thick. Conformably overlain by Muttama Creek Siltstone||||||26-MAY-08
27135|Cowcumbala Rhyolite|22857|5|Briefly described|p450 App.1, Tb.A1.6|Pragian|Pragian|Of the Cootamundra Group. Massive and flow-banded rhyolite. Max. thickness: 1750m. Geological Province: Bogan Gate Terrace.||||||
27135|Cowcumbala Rhyolite|35070|2|Defined|p110|Early Devonian|Early Devonian|||||||
27135|Cowcumbala Rhyolite|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27135|Cowcumbala Rhyolite|35608|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27135|Cowcumbala Rhyolite|35609|6|Mentioned|p11|||||||||
27135|Cowcumbala Rhyolite|36411|6|Mentioned|p268|||Refers Basden et al 1978 for definition.||||||
27135|Cowcumbala Rhyolite|42313|6|Mentioned|p144|||||||||
27135|Cowcumbala Rhyolite|44192|5|Briefly described|Map Legend||Lochkovian|||||||
27135|Cowcumbala Rhyolite|44936|5|Briefly described|Map Legend||Early Devonian|||||||
27135|Cowcumbala Rhyolite|50191|5|Briefly described|p14|Early Devonian|Early Devonian|Of the Cootamundra Group.||||||
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.|
74598|Cowpers Creek Conglomerate|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Lambie Group. Reddish-purple, massive, clast-supported, poorly sorted quartz-lithic pebble to boulder conglomerate and coarse-grained sandstone.||||||25-JUN-08
74598|Cowpers Creek Conglomerate|68592|2|Defined|p1722-4, p1727, p1739-42|Late Devonian|Late Devonian|New name, after Cowpers Creek. These rocks were originally included as part of the Wiarborough Formation and part of the Cookbundoon Sandstone by Scheibner (1973); both names now obsolete. Type area described. Up to 250m thick. Geophysical properties described. Unfossiliferous. Possibly correlates with Slowmans Creek Conglomerate.||Unit in Lambie Group.||Conformably overlies Strathaird Conglomerate locally. Interfingers with or is overlain by Cookbundoon Formation. Is overlain locally by Tarlo Formation.|Buff to reddish-purple, poorly sorted, mostly thick-bedded, pebble to boulder conglomerate and coarse-grained, quartz-lithic and lithic-quartz sandstone; very  minor interbedded siltstone. Large-scale planar and trough cross-bedding is common.|
74598|Cowpers Creek Conglomerate|70192|5|Briefly described|Map Legend|Famennian|Famennian|Dlw. Includes and unnamed sub unit of poorly sorted, thickly bedded, matrix and clast supported, pebble-boulder, polymictic conglomerate; common large scale planar and trough cross bedding. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Lambie Group|Includes one unnamed subunit.|Is overlain by Cookbundoon Formation. Overlies Strathaird Formation or, where Strathaird Formation is absent, is erosional at base.|Poorly sorted, mostly thick bedded, matrix and clast supported, pebble-boulder, polymictic conglomerate and coarse grained, commonly pebbly, quartz lithic and lithic quartz sandstone; common large scale planar and trough cross bedding.|
74598|Cowpers Creek Conglomerate|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed member of poorly sorted, thickly bedded, matrix and clast supported, pebble to boulder sized polymictic granite.||Lambie Group|||Poorly sorted, mostly thickly bedded, matrix and clast supported, pebble to boulder, polymictic conglomerate and coarse grained, commonly pebbly, quartz lithic and lithic quartz sandstone, very minor interbedded siltstone. Crossbeds common.|
74598|Cowpers Creek Conglomerate|70543|5|Briefly described|Map Legend|Devonian|Devonian|Includes and unnamed sub unit of poorly sorted, thickly bedded, matrix and clast supported, pebble-boulder, polymictic conglomerate; common large scale planar and trough cross bedding.||Lambie Group|Includes one unnamed subunit||Poorly sorted, mostly thick bedded, matrix and clast supported, pebble-boulder, polymictic conglomerate and coarse grained, commonly pebbly, quartz lithic and lithic quartz sandstone; common large scale planar and trough cross bedding.|
74598|Cowpers Creek Conglomerate|71040|5|Briefly described|p19|Middle Devonian|Middle Devonian|W side of the Cookbundoon Syncline.|||||Contains disoriented cleaved clasts.|
74598|Cowpers Creek Conglomerate|71656|6|Mentioned|p13 Fig.2|||Shown only in correlation chart (Fig.2).||Lambie Group||Overlies Strathaird Formation. Shown as underlying and partly laterally equivalent to Cookbundoon Formation.||
31569|Cowra Suite|23549|5|Briefly described|p522|||Of Bullenbalong Supersuite.  Characterised by scattered large garnets rimmed by cordierite.  Geological Province: Lachlan Fold Belt.||||||12-JUN-08
31569|Cowra Suite|42726|5|Briefly described|map legend||Silurian|||||||
31569|Cowra Suite|44093|5|Briefly described|p195 App. 1|Devonian|Silurian|Granite. Geological Province: Lachlan Fold Belt.||||||
31569|Cowra Suite|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes the Whistle Waa Granite.||||||
31569|Cowra Suite|68592|4|Described|p1225-9, p1231-8, p1260, p1262-3|Late Silurian|Late Silurian|Chappell et al. (1991). Named after the town of Cowra. Cowra Granodiorite is the type pluton. Much of the Cucum Granite, and the southern portion of Whistle Waa Granite, have been reassigned to the Wyangala Granite on geochemical grounds. Geochemistry detailed. Thought to be comagmatic with Canowindra Volcanics. Age not well constrained.||Unit in Bullenbalong Supersuite.|Includes Whistle Waa and Cucum Granites and Cowra Granodiorite.||Granodiorite and granite. S-type.|
31569|Cowra Suite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Whistle Waa Granite.|||
31569|Cowra Suite|70545|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Whistle Waa Granite|||
31722|Cowriga Limestone Member|22679|4|Described|p 23|||||||||
31722|Cowriga Limestone Member|22857|5|Briefly described|p428 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of Blayney Volcanics. Foliated recrystallised grey limestone; corals.||||||09-MAR-06
31722|Cowriga Limestone Member|23100|5|Briefly described|p575 (Fig 1)||Ordovician|Of Cabonne Group.||||||17-JUL-08
31722|Cowriga Limestone Member|23202|6|Mentioned|p1059, Fig.1|||Of Blayney Volcanics||||||17-JUL-08
31722|Cowriga Limestone Member|23214|3|Fully described|p62|Late Ordovician|Late Ordovician|Of Blayney Volcanics. Formerly part of Panuara Formation.||||||17-JUL-08
31722|Cowriga Limestone Member|43653|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Blayney Volcanics.||||||17-JUL-08
31722|Cowriga Limestone Member|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Blayney Volcanics, Cabonne Group. Foliated, recrystallised, grey limestone.||||||17-JUL-08
31722|Cowriga Limestone Member|43782|5|Briefly described|Map Legend|Gisbornian|Gisbornian|Of Blayney Volcanics, Cabonne Group.||||||17-JUL-08
31722|Cowriga Limestone Member|63278|5|Briefly described|p156|Late Ordovician|Late Ordovician|Of the Blaney Volcanics. Upper member and contains conodonts. Limestone. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
31722|Cowriga Limestone Member|63283|6|Mentioned|p202, p205|Late Ordovician|Late Ordovician|Poorly dated.||||||07-FEB-11
31722|Cowriga Limestone Member|63286|6|Mentioned|p294 Fig. 1, p307|||Of the Blayney Volcanics. Intruded by Copper Hill Suite dacites.||||||07-FEB-11
31722|Cowriga Limestone Member|67322|5|Briefly described|p25|Late Ordovician|Late Ordovician|Conodonts indicate a Late Ordovician age. Occurs in the Blayney region. ||Of the upper Blayney Volcanics|||Recrystallised limestone.|
31722|Cowriga Limestone Member|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3). Shown as Cowriga Limestone Mbr.||Blayney Volcanics||||
31722|Cowriga Limestone Member|73431|5|Briefly described|p364-365|Ordovician|Ordovician|Lachlan Orogen.||Blayney Volcanics||Intruded by Browns Creek Intrusive Complex, Browns Creek dykes||
79333|Coxs Coal Member|70791|5|Briefly described|p275, p283, p286-287, p292-294|Cisuralian|Cisuralian|New name. Mullaley Sub-basin. 1.5-4m thick. Borehole cross-sections and long-sections; correlations. Coal properties described. In situ coal estimates.||||||
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.|
32254|Crack Hardy Point Monzodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh28.||||||
32254|Crack Hardy Point Monzodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
31294|Cranbrook Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Rhyolite.||||||
24888|Craven Subgroup|22857|5|Briefly described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Gloucester Coal Measures. Geological Province: Sydney Basin.||||||
24888|Craven Subgroup|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Gloucester Coal Measures.    Geological Province: New England Fold Belt||||||
24888|Craven Subgroup|40872|6|Mentioned|Fig.2|||||||||
24888|Craven Subgroup|41054|6|Mentioned|p153|||||||||
24888|Craven Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
24888|Craven Subgroup|44244|5|Briefly described|p181, p168 Tb. 2|Late Permian|Late Permian|Of the Gloucester Coal Measures.  Supersedes Craven Coal Measures, Stratford Coal Measures,  Lower and Upper Craven Measures.  Includes the Wenham Formation, Wards River Conglomerate, Jilleon and Leloma Formations, Crowthers Road Conglomerate.||||||27-JUL-04
24888|Craven Subgroup|50147|5|Briefly described|Map legend|||Of the Gloucester Coal Measures.  Geological Province: Western Myall Block.||||||
70521|Creswells Tank Granodiorite|66623|2|Defined|pp160-168.|Silurian|Silurian|Defined in this study. Previously included in the Tibooburra Granodiorite. A single, 1.1 km by 450 m outcrop of prominent stacked tors and whalebacks. Weak I-type affinity; geochemistry suggests a within-plate or volcanic arc tectonic setting. Contact relationships with country rocks are not exposed.|427.7 +/- 2.3 Ma.|Unit in Tibooburra Suite.|||Medium-grained, leucocratic equigranular, massive quartz-feldspar-biotite granodiorite.|06-MAY-13
70521|Creswells Tank Granodiorite|66920|5|Briefly described|Map legend|Silurian|Silurian||||||Massive, weakly porphyritic, leucocratic, medium-grained seriate granodiorite.|
70521|Creswells Tank Granodiorite|66927|5|Briefly described|Map legend|Silurian|Silurian|Low to moderate magnetic zones. Intrusive boundaries contrast strongly with magnetised aureole zones.|||Unit in Tibooburra Suite.||Hornblende granodiorite.|06-MAY-13
70521|Creswells Tank Granodiorite|67209|5|Briefly described|Map legend.|Silurian|Silurian|||Unit in Tibooburra Suite.|||Massive, weakly porphyritic, leucocratic, medium-grained seriate granodiorite.|
70521|Creswells Tank Granodiorite|71965|5|Briefly described|p897,909|Pridoli|Ludlow|Geological province: Thomson Orogen. |c. 427 Ma to 420 Ma|Unit of Tibooburra Suite.||Inrudes into the Easter Monday Formation.||
70521|Creswells Tank Granodiorite|72522|5|Briefly described|p119.|Pridoli|Ludlow||c. 420-427 Ma|Tibooburra Suite||||
80451|Cringadale granite|70718|5|Briefly described|p65, 66|||Informal name, interpreted from geophysics. Referred to as the Cringadale granodiorite on p65 fig 35, p66.||Glen Emu granite suite|||Interpreted as granite or granodiorite.|31-MAY-19
29283|Crinoidal Limestone Member|22857|4|Described|p460 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Taemas Limestone. Massive crinoidal limestone with interbedded tuff. Max. thickness: 152m. Geological Province: Canberra-Yass Shelf.||||||
29283|Crinoidal Limestone Member|24005|5|Briefly described|p293|Early Devonian|Early Devonian|Of Taemas Limestone. Geological Province: Lachlan Fold Belt||||||
29283|Crinoidal Limestone Member|24250|5|Briefly described|p105, p109 Fig.5|Early Devonian|Early Devonian|Parent: Taemas Limestone (Murrumbidgee Group). Maximum Thickness: 180m. Underlying Unit: Warroo Limestone Member (disconformable)||||||
29283|Crinoidal Limestone Member|32483|6|Mentioned|p33|||Refers Browne (1959)||||||
29283|Crinoidal Limestone Member|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
29283|Crinoidal Limestone Member|35386|4|Described|p54|||||||||
29283|Crinoidal Limestone Member|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
29283|Crinoidal Limestone Member|50230|4|Described|Map legend|Emsian|Emsian|Of the Taemas Limestone.  Overlies the Warroo Limestone Member.  Massive crinoidal limestone with interbedded tuffaceous sandstone.||||||
29283|Crinoidal Limestone Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Taemas Limestone (Murrumbidgee Group). Massive crinoidal limestone with interbedded tuffaceous sandstone.||||||
29283|Crinoidal Limestone Member|64992|5|Briefly described|p60 Fig. 1|Devonian|Devonian|Part of the Taemas-Wee Jasper succession. Of the Taemas Formation. Contains Dipnorhynchus (Placorhynchus) cathlesae (lungfish). Coarse-grained and composed of crinoidal stems, with occasional finer beds containing  articulated crinopid stems.||||||26-MAR-09
29283|Crinoidal Limestone Member|68592|2|Defined|p982, p984 Fig.162, p985-6, p1034-7|Early Devonian|Early Devonian|See also p1197, p1202, p1904. Originally Crinoidal Limestone of Browne (1959), an uppermost unit in her Taemas Stage. When the latter was raised to Formation status (Offenberg, 1974), it became Crinoidal Limestone Member. Type locality described. Preserved thickness 152m. Very restricted exposure. Characterised by tightly packed crinoidal debris (stems and ossicles), with lesser brachiopods, corals and bivalves.||Unit in Taemas Limestone.||Disconformably overlies Warroo Limestone Member.|Thin- to medium-bedded, blue-grey to white, cross-bedded, crinoidal limestone with minor tuffaceous sandstone mainly near the top.|
29283|Crinoidal Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmtn. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Taemas Limestone||May overlie Warroo Limestone Member, nature of contact unclear.|Blue-grey to white, thin-medium bedded, bioclastic limestone interbedded with tuffaceous sandstone particularly towards the top of the sequence.|
29283|Crinoidal Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey to white, thin-medium bedded, bioclastic limestone interbedded with tuffaceous sandstone particularly towards the top of the sequence.|
29283|Crinoidal Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey to white, thin-medium bedded, bioclastic limestone interbedded with tuffaceous sandstone particularly towards the top of the sequence.|
29283|Crinoidal Limestone Member|71656|5|Briefly described|p12 Fig.2, p33, p37-p38|Emsian|Emsian|Fossils include fish, crinoid fauna. A disconformity with the Warroo Limestone Member is evident.||Of Taemas Limestone, Murrumbidgee Group||Disconformably overlies Warroo Limestone Member.|White, thin-bedded limestone 69 m thick and commonly cross-bedded, interpreted as having been deposited in the intertidal zone.|
69868|Crooked Corner Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes Binda Granite and Asylum Granite.||||||09-SEP-08
69868|Crooked Corner Suite|68592|2|Defined|p74 Tb.5, p650, p1466-81|Early Devonian|Early Devonian|New name, after the locality of Crooked Corner N of Binda. Corresponds with Binda Granite and the southern pluton of Yarra Granite as interpreted by Chappell et al. (1991) who included them in the Wyangala Batholith. Forms an irregular belt 43 km long and 7 km wide. Mostly poor to moderate outcrop. Type pluton is Binda Granite. Miarolitic cavities and spherulitic textures indicate high-level emplacement. Geochemistry detailed, suggesting widespread alteration. SHRIMP U-Pb zircon age for Binda Granite. Hosts lead, and disseminated pyrite-arsenopyrite-gold, mineralisation in quartz veins and aplite dykes. Peelwood structural zone: deformation described.|405 +/- 12 Ma (Wilde, 2001).||Includes Binda Granite and Asylum Granite (part of former Yarra Granite).|Intrudes Cuddyong and Abercrombie Formations.|Generally medium to coarse-grained, equigranular to porphyritic, massive to foliated, hornblende-biotite granite and borderline tonalite/granodiorite; minor biotite-muscovite leucogranite; sills and dykes of aplite, microgranite and rhyolite; I-type.|
69868|Crooked Corner Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|On Crookwell and Gunning 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Asylum Granite, Binda Granite.|||
69868|Crooked Corner Suite|70541|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Binda Granite.|||
69868|Crooked Corner Suite|70544|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Asylum Granite, Binda Granite|||
35344|Crookwell Basalt|50232|5|Briefly described|Map legend|Eocene|Eocene|Alkali basalt.||||||
35344|Crookwell Basalt|50234|5|Briefly described|Map Legend|Eocene|Eocene|Alkali Basalt.||||||
35344|Crookwell Basalt|64238|5|Briefly described|Map legend|Cenozoic|Cenozoic|Silica-undersaturated olivine basalt with minor trachyte phases.||||||19-NOV-08
35344|Crookwell Basalt|68592|2|Defined|p257,p362, p833, p847, p1787-9, p1804-10|Eocene|Eocene|See also p37, p232, p236. New name, after the town of Crookwell. Also includes an un-named subunit of trachyte lava and pyroclastic rock (breccia). Type and representative areas described. Flows buried an eroded landscape with at least 140m relief. Geochemistry and geophysical properties described. Locally overlies ferricrete or deeply weathered strata. Geophysical properties described. Quarried for dimension stone in Crookwell and Taralga districts, and for emery near Crookwell. |51-36 Ma (Jones, 1986).||Includes Billyrambija Dolerite Member.|Locally overlies Poidevins Sandstone and Turrallo Suite; unconformably overlies Argyle Formation and Longreach Volcanics; nonconformably overlies Gunning Granite. Correlated with Reevesdale Basalt.|Dark-grey to black, mostly fine-grained, olivine-phyric, undersaturated alkali basalt bordering on basanite. Several separate basalt flows, very jointed and locally deeply weathered: has associated laterite.|
35344|Crookwell Basalt|70192|5|Briefly described|Map Legend|Eocene|Eocene|Czc. On Crookwell, Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||||Fine grained, alkali olivine basalt and dolerite with minor trachyte and lithic welded ignimbrite.|
35344|Crookwell Basalt|70541|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Dark grey to black, mostly fine grained, alkali olivine basalt and dolerite with minor trachyte and lithic welded ignimbrite.|
35344|Crookwell Basalt|70542|5|Briefly described|Map Legend|Neogene|Palaeogene||||Includes Billyrambija Dolerite.||Dark grey-black, mostly fine grained, alkali olivine basalt and dolerite with minor trachyte and lithic welded ignimbrite.|
35344|Crookwell Basalt|70543|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Fine grained, alkali olivine basalt and dolerite with minor trachyte and lithic welded ignimbrite.|
35344|Crookwell Basalt|71069|6|Mentioned|p135|Cenozoic|Cenozoic|||||Unconformably overlies the Mount Fairy Group.||
35344|Crookwell Basalt|71700|5|Briefly described|p33|||||||Equivalent to the Reevesdale Basalt.||
78645|Croppies Gunyah Ignimbrite Member|69159|5|Briefly described|Map legend|Pragian|Lochkovian|||Unit in Long Flat Volcanics.||Overlies Kadoona Dacite Member. Is overlain by Manar Ignimbrite Member.|Grey to white, medium-grained, moderately crystal-rich, densely-welded rhyolitic ignimbrite.|07-SEP-15
78645|Croppies Gunyah Ignimbrite Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Long Flat Volcanics.|||Grey to white, medium-grained, moderately crystal-rich, densely welded rhyolitic ignimbrite.|
78645|Croppies Gunyah Ignimbrite Member|71700|2|Defined|vi, p25-p26, p42, CD|Early Devonian|Early Devonian|Name derived from the Croppies Gunyah Creek which is a tributary of the Boro Creek. The type section occurs between GR 744952 6105925 and GR 746182 6104396. SHRIMP age is derived from Bodorkos et al (2010) and is in agreement with ages for other members of the Long Flat Volcanics. These rocks were included in the Long Flat Porphyries (Anderson 1893) and the Manar Porphyry (Joplin et al. 1953). They were defined as part of the Long Flat Volcanics by Best et al. (1964) and described as such by Felton and Huleatt (1975, 1977). Distibution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. Lithology is discussed in great detail. Faulted against the Abercrombie Formation and the Back Station Ignimbrite Member. Intruded by the Braidwood Granodiorite. Equivalent to the Newacres Ignimbrite Member. Intruded by the Kain Porphyry Member. Misspelt as the Croppies Gunya Ignimbrite Member on p82. See also p58, p62, p74, p79-p80, p82.|414 +/- 2.5 Ma (SHRIMP U-Pb)|Long Flat Volcanics||Conformably overlies the Tally Ho Ignimbrite Member and the Kadoona Dacite Member. Conformably overlain by the Manar Ignimbrite Member.|Moderately crystal-rich, densely-welded rhyolitic ignimbrite.|
23521|Crossleys Tank Formation|22508|6|Mentioned|p3||Early Devonian|Lachlan Fold Belt||||||
23521|Crossleys Tank Formation|22857|5|Briefly described|p438 App.1, Tb.A1.6|Emsian|Lochkovian|Of the Rast Group (Cobar Supergroup). Arenite and siltstone. Max. thickness: 2.5km. Geological Province: Rast trough (Darling Basin).||||||
23521|Crossleys Tank Formation|23365|5|Briefly described|8|Devonian|Devonian|||||||
23521|Crossleys Tank Formation|41394|2|Defined|p81|Early Devonian||||||||
23521|Crossleys Tank Formation|41395|6|Mentioned|Map legend|Early Devonian||||||||
23521|Crossleys Tank Formation|42144|6|Mentioned|Fig.3 P604|||||||||
23521|Crossleys Tank Formation|42521|5|Briefly described|Fig.3d P16|||||||||
23521|Crossleys Tank Formation|43089|5|Briefly described|Map Legend|||Of Rast Group.||||||26-MAR-08
23521|Crossleys Tank Formation|61964|3|Fully described|p14 Fig. 4, p64|Lochkovian|Pridoli|Of Rast Group (Cobar Supergp). Rift-fill sequence:qtz-rich sandstones - unbioturbated.Overlain by Preston Fm; conformable on Norholm Sst Mbr (Boothumble Fm).Thickness: 2.5km (est.) ?700m on CARGELLIGO. Geophysics aspects (p224); palaeontology (p259-260)||||||
23521|Crossleys Tank Formation|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Basal unit of the Rast Group. Interbedded, graded quartz sandstone, slate and rare conglomerate.||||||10-APR-08
23521|Crossleys Tank Formation|63019|5|Briefly described|p920, p921 Fig.2|Lochkovian|Lochkovian|Of Rast Group. Quartz-rich turbidites. Geological Province: Lachlan Orogen.||||||23-JAN-07
23521|Crossleys Tank Formation|63891|5|Briefly described|p237|||Underlies Ural Volcanics. Lithology (together with Preston Formation): basin-fill sequences of quartz-rich turbidites consisting of volcaniclastic and fossiliferous sandstones.||||||03-JUN-08
23521|Crossleys Tank Formation|65469|5|Briefly described|p18|Late Silurian|Late Silurian|Lachlan Orogen.||||||
23521|Crossleys Tank Formation|69161|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Rast Group.||Overlies Bootheragandra Group. Is overlain by Ural Volcanics.|Interbedded, graded, quartz sandstone, slate and rare conglomerate.|
23521|Crossleys Tank Formation|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Rast Group.||Is faulted against Clements Formation. Is overlain by Preston Formation.|Interbedded, graded, quartz sandstone, slate and rare conglomerate.|
23521|Crossleys Tank Formation|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
23521|Crossleys Tank Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Rast Group.||Is overlain by Preston Formation or Ural Volcanics.|Monotonous sequence of quartz sandstone to sublithic or subarkosic sandstone interbedded with minor mudstone, slate or siltstone.|
23521|Crossleys Tank Formation|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Underlain by Boothumble Formation. Overlain by and partly equivalent to[?] Ural Volcanics. Equivalent to Mount Knobby Formation.||
23523|Crowl Creek Formation|22518|5|Briefly described|Table 1, p 6, 7||Late Devonian|Of the Mulga Downs Group. geological province: Darling Basin.||||||13-OCT-08
23523|Crowl Creek Formation|22857|4|Described|p212, p486 App.1 Tb.A1.7|Early Carboniferous|Devonian|Of the Mulga Downs Group; contains the Calytria Quartzite Member. Max. thickness: >2km. Geological Province: Barka Basin.||||||24-FEB-06
23523|Crowl Creek Formation|22859|5|Briefly described|p212|||||||||
23523|Crowl Creek Formation|22893|4|Described|p12 table4|||Similar to Manfred Sandstone and Milton Grove Formation in mapping area.||||||
23523|Crowl Creek Formation|23171|6|Mentioned|p16|||||||||
23523|Crowl Creek Formation|23173|6|Mentioned|Map Legend|||||||||
23523|Crowl Creek Formation|37798|4|Described|Table I|||||||||
23523|Crowl Creek Formation|38292|6|Mentioned|Fig.1|||||||||
23523|Crowl Creek Formation|40913|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Early Carboniferous-Late Devonian||||||
23523|Crowl Creek Formation|41126|3|Fully described|p137|||Mention p108.||||||13-OCT-08
23523|Crowl Creek Formation|41138|6|Mentioned|Map legend|Carboniferous|Devonian|Carboniferous-Devonian||||||
23523|Crowl Creek Formation|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
23523|Crowl Creek Formation|41821|2|Defined|p64|Early Carboniferous|Middle Devonian|||||||
23523|Crowl Creek Formation|42521|5|Briefly described|Fig.6 P20|||||||||
23523|Crowl Creek Formation|42983|6|Mentioned|Fig.3,p345|||||||||
23523|Crowl Creek Formation|43032|2|Defined|p197|Early Carboniferous|Givetian|Of the Mulga Downs Group.||||||13-OCT-08
23523|Crowl Creek Formation|64967|5|Briefly described|p114 Fig. 2|Famennian||Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113).See also p115 Fig. 3.||||||
23523|Crowl Creek Formation|65759|5|Briefly described|p114 Fig.2||Famennian|Overlies the Bundycoola Formation. 2000m thick, fluvial, part of the Mulga Downs Group.||||||
23523|Crowl Creek Formation|70751|6|Mentioned|p12|Emsian|Emsian|||Mulga Downs Group||||
23523|Crowl Creek Formation|70821|5|Briefly described|p32|Devonian|Devonian|362m thick in Brewarrina 1 well (ca. 80km NNW of Brewarrina).||||Is overlain by Cadna-owie Formation.|Red-brown to grey-green sandstones.|
23523|Crowl Creek Formation|72958|6|Mentioned|p11|Eifelian|Emsian|Cobar Basin. Nymagee area.||Mulga Downs Group||Partly underlain by Winduck and Walters Range groups. Partly underlain and equivalent to[?] Bundycoola Formation. ?Partly equivalent to Bulgoo, Merrimerriwa and Meadows Tank formations.||
23523|Crowl Creek Formation|73181|6|Mentioned|p60|||Contains a fossil plant resembling Lepidosigillaria yalwalensis.||||||
29918|Crowther Monzodiorite|23214|3|Fully described|p210|Early Devonian|Early Devonian|Originally included in both the Young Granite and Bumbaldry Granite. Intrudes Canowindra Volcanics.||||||
29918|Crowther Monzodiorite|24417|3|Fully described|p104|Early Devonian|Early Devonian|Intrudes the Warrangong Volcanics.  Previously included in Young Granodiorite by Brunker (1972) and Bowan (1976). Also included in "Bumbaldry Granite" of Chappell et al (1991).||||||25-JUN-08
29918|Crowther Monzodiorite|43642|5|Briefly described|Map Legend|Devonian|Devonian|Consists of coarse, porphyritic, quartz monzodiorite.||||||17-JUL-08
29918|Crowther Monzodiorite|43782|5|Briefly described|Map Legend|Emsian|Emsian|||||||
29918|Crowther Monzodiorite|50231|5|Briefly described|Map Legend|Emsian|Emsian|||||||
29918|Crowther Monzodiorite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Medium grained hornblende diorite.||||||05-JUL-04
29918|Crowther Monzodiorite|60009|5|Briefly described|Map Legend|Emsian|Pragian|||||||13-JUL-04
29918|Crowther Monzodiorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Dark grey to pinkish-grey, fine- to medium-grained, massive, generally equigranular (but partly porphyritic), augite monzodiorite to biotite?-pyroxene-hornblende quartz monzonite to augite monzonite.||||||
29918|Crowther Monzodiorite|68592|2|Defined|p928,p959,p963, p1398, p1401-3, p1429-32|Devonian|Devonian|Moffitt, in Pogson and Watkins (1998); named after Crowther Range. Previously shown as part of the Young Granodiorite by Packham (1968) and later workers. Included in the Bumbaldry Granite of Chappell et al. (1991). Much of the area shown as this unit in the SW of Bathurst 1:250 000 sheet area (Raymond et al., 1998) is actually Warrangong Volcanics (Lyons et al., 2000), which is possibly comagmatic. A small intrusive; type area described. Mineralogy described in some detail. Geochemistry detailed; geophysical properties briefly described. Age from lithological and geochemical relationships.||Unit in Gooramma Suite.||Is overlain by and/or intrudes Warrangong Volcanics. Is faulted against Hervey Group.|Composite body with a wide range in composition. Dark grey to pinkish-grey, fine- to medium-grained, massive, generally equigranular, augite quartz monzodiorite to porphyritic augite monzonite to biotite?-pyroxene-hornblende quartz monzonite; I-type.|
29918|Crowther Monzodiorite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgc. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Gooramma Suite|||Fine-medium grained, massive, equigranular-partly porphyritic augite quartz monzodiorite to biotite?-pyroxene-hornblende quartz monzonite to augite monzonite; high K and Th; high-very high magnetic susceptibility.|
29918|Crowther Monzodiorite|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Boggy Plain Supersuite||||
29918|Crowther Monzodiorite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Fine-medium grained, massive, equigranular-partly porphyritic augite quartz monzodiorite to biotite?-pyroxene-hornblende quartz monzonite to augite monzonite; high K and Th; high-very high magnetic susceptibility.|
81959|Cruaich Member|72700|5|Briefly described|Mapsheet 1|||||Shawns Creek Formation|||Scoria crystal trachyte-lithic lapilli tuff, palagonite-altered ash matrix.|
70030|Cuddyong Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Siltstone, phyllite, black siltstone, quartzose and minor volcaniclastic sandstone, quartzite, quartz-muscovite schist, felsic tuff. Commonly pyritic and often containing clear rounded volcanic quartz grains in the sandstone.||||||
70030|Cuddyong Formation|68592|3|Fully described|p457, p607-18, p637-51, p743, p1886-7|Ludlow|Ludlow|See also p130-1, p151-5, p163-5, p170-2, p217, p424-5. New name. Previously (Scheibner, 1973) these rocks were assigned to Kildrummie Group, Rockley Volcanics, undifferentiated Ordovician-Silurian rocks, a combination of Burra Burra Creek Formation and overlying Bummaroo Formation in the original Campbells Formation, and Covan Creek Formation. Named after Cuddyong Creek. A representative section and a possible type section are described. From 50m to 3.5km thick. W-dipping thrust-faulting causes repetition. Dips and youngs to W. Trace elements, geochemistry, lithology detailed. Sandstone-rich packages form bold strike ridges. Turbiditic sandstones commonly show graded bedding, horizontal lamination and ripple cross-lamination. Classification and provenance plots. Regionally metamorphosed to greenschist facies: described in some detail. Geophysical properties and metamorphism described. Sparse, poorly-preserved fossils. Hosts massive sulfide mineralisation at Peelwood, Black Springs and Elsinora (all detailed) and Breadalbane mines; also auriferous quartz veins at Junction Point. Iron was extracted at Crookwell Iron Mine, Breadalbane (the B1 deposit: detailed) and Cullerin (Cu). Fossils are extremely rare. Is faulted against Crudine Group and Cunningham Formation. Is intruded by Wrens Nest Trachyte, Crooked Corner, Bishopthorpe and Whick Whack Suites, Wologorong and Oberon Supersuites, and Ghost Rocks and Oolong Granites. Correlated with Bells Creek Volcanics, Anson and Karawina Formations (Mumbil Group), and Biraganbil Formation (Chesleigh Group). Other equivalent units mentioned.|420 +/- 9 Ma (SHRIMP U-Pb; Wilde 2001).|Unit in Campbells Group.||Overlies Fosters Creek Conglomerate, Wet Lagoon Volcanics and Kildrummie Formation conformably, and Jeremy Formation unconformably. Is overlain conformably by Kangaloolah Volcanics.|Interbedded quartzose sandstone and siltstone, rhyolitic to dacitic coherent and volcaniclastic rocks, grey to black siltstone, shale and mudstone, and rare limestone.  Includes (probably allochthonous) limestone blocks.|28-SEP-16
70030|Cuddyong Formation|70192|5|Briefly described|Map Legend|Lochkovian|Wenlock|Scc. Includes four unnamed subunits: quartzose sandstone with interbedded siltstone; massive-laminated, thickly bedded allocthonous limestone blocks; rhyolite-dacite, volcaniclastic sandstone and siltstone; siliceous, carbonaceous, pyritic siltstone, mudstone and shale. On Gunning, Crookwell and Taralga 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot. Related Units continued: Overlies, and interfingers with, Kildrummie Formation and Fosters Creek Conglomerate.||Campbells Group|Includes four unnamed units.|Envelopes Wrens Nest Trachyte. Interfingers with, and over- and underlies, Kangaloolah Volcanics. Is overlain by undifferentiated Crudine Group. See comments.|Interbedded quartzose sandstone and siltstone, rhyolitic to dacitic coherent and volcaniclastic rocks. Shale, siltstone and mudstone, rare limestone.|
70030|Cuddyong Formation|70297|5|Briefly described|map legend|Silurian|Silurian|Presented as Cuddyong Fm.||||||
70030|Cuddyong Formation|70541|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed members: rhyolite to dacite, volcaniclastic sandstone and siltstone; siliceous, carbonaceous, pyritic siltstone, mudstone shale and phyllite with minor interbedded, quartzose or volcaniclastic sandstone.||Campbells Group|Includes two unnamed members.||Interbedded quartzose sandstone and siltstone, rhyolitic to dacitic coherent and volcaniclastic rocks, grey to black siltstone, shale and mudstone; rare limestone is also present.|
70030|Cuddyong Formation|70542|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed members, one of rhyolite-dacite volcanic sandstones and one of siliceous, carbonaceous pyritic siltstone.||Campbells Group|||Interbedded quartzose sandstone and siltstone, rhyolitic to dacitic coherent and volcaniclastic rocks, grey to black siltstone, shale and mudstone, rare limestone.|
70030|Cuddyong Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|Includes three unnamed subunits: massive-laminated, thickly bedded allochthonous limestone blocks; rhyolite-dacite, volcaniclastic sandstone and siltstone; siliceous, carbonaceous, pyritic siltstone, mudstone and shale.||Campbells Group|||Interbedded quartzose sandstone and siltstone, rhyolitic to dacitic coherent and volcaniclastic rocks. Shale, siltstone and mudstone, rare limestone.|15-NOV-16
70030|Cuddyong Formation|70544|5|Briefly described|Map Legend|Devonian|Silurian|Includes four unnamed members; a fine-coarse grained quartzose sandstone, massive or laminated allochthonous blocks, rhyolite-dacite lavas, siliceous carbonaceous pyritic siltstone.||Campbells Group|Includes four unnamed members||Interbedded quartzose sandstone and siltstone, rhyolitic-dacitic coherent and volcaniclastic rocks; siltstone, shale and mudstone with rare limestone also present.|
70030|Cuddyong Formation|71069|5|Briefly described|p50 tbl 3, p134, p146|||Hosts the Hannans Flat Pb, Zn, Cu, Au, Ag prospect.||Campbells Group||Part equivalent to the De Drack Formation.|Lithic-poor sandstone with a small but variable feldspathic component.|
70030|Cuddyong Formation|71656|5|Briefly described|p13 Fig.2, p28|Lochkovian|Wenlock|Fossils are sparse and consist of poorly preserved conodonts and occasional corals in limestones that are non-diagnostic of age but most likely Wenlockian or Ludlovian.||Campbells Group||Campbells Group. Partially overlying Kangalooh Volcanics. Underlying Crudine Group. Partially underlying Box Ridge Volcanics. Overlying and partially equivalent to Kildrummie Formation.||
33397|Cudgelbar Sandstone Member|24417|3|Fully described|p146|Late Devonian|Late Devonian|Of Weddin Sandstone.  Previously mapped as undifferentiated Weddin Sandstone.  Underlain by Carlachy Sandstone Member.||||||
33397|Cudgelbar Sandstone Member|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Weddin Sandstone (Hervey Group).||||||
33397|Cudgelbar Sandstone Member|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Weddin Sandstone (Hervey Group). Overlies: Carlachy Sandstone Member.  Underlies: Cookamidgera Subgroup.||||||13-JUL-04
33397|Cudgelbar Sandstone Member|64826|5|Briefly described|p1040 Tb. 1|Famennian|Famennian|Within the Hervey Group.||||||04-MAR-09
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.|
26261|Cues Formation|6823|5|Briefly described|p205, 208, 210-211, 216|Palaeoproterozoic|Palaeoproterozoic|A metamorphic age of 1571 +/- 11 Ma is provided; both ages are derived from this study. Lithology and petrography of the amphibolite are discussed in detail.|1683 +/- 5 Ma (Magmatic cryst. U-Pb zircon)|Thackaringa Group|||Hornblende plagioclase garnet orthopyroxene clinopyroxene amphibolite.|26-MAR-22
26261|Cues Formation|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
26261|Cues Formation|22575|6|Mentioned|p179 Fig.2|||Of the Thackaringa Group.||||||11-JUN-08
26261|Cues Formation|22752|6|Mentioned|p 277|||||||||
26261|Cues Formation|22771|6|Mentioned|Table12.2p45,46|||||||||
26261|Cues Formation|22857|4|Described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Thackeringa Group. Max. thickness: 1000m. Geological Province: Willyama Fold Belt. Also mentioned on p390 App.1 Tb.A1.1.||||||07-NOV-08
26261|Cues Formation|22884|5|Briefly described|p41, p43 Fig3|||Of the Thackeringa Group. Correlates generally with Tommie Wattie Formation in Olary Domain. Geological province: Broken Hill Domain.||||||26-MAR-09
26261|Cues Formation|22965|5|Briefly described|p13, Fig1||Statherian|Part of the Thackaringa Group.||||||
26261|Cues Formation|22966|6|Mentioned|Fig1||Proterozoic|Rift stage of development.||||||
26261|Cues Formation|22967|6|Mentioned|p39||Statherian|||||||
26261|Cues Formation|23025|5|Briefly described|p75-6|||||||||
26261|Cues Formation|23160|6|Mentioned|fig1|||||||||
26261|Cues Formation|23248|5|Briefly described|Fig2p169|||||||||
26261|Cues Formation|23912|6|Mentioned|p779|||||||||
26261|Cues Formation|24307|5|Briefly described|p973|Proterozoic|Proterozoic|Of the Thackaringa Group.||||||18-JUN-08
26261|Cues Formation|38969|4|Described|p206|||||||||
26261|Cues Formation|39662|2|Defined|p419|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26261|Cues Formation|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26261|Cues Formation|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26261|Cues Formation|39849|6|Mentioned|p86|||||||||
26261|Cues Formation|40290|6|Mentioned|p1|||||||||
26261|Cues Formation|40822|6|Mentioned|Fig.2|||||||||
26261|Cues Formation|41093|6|Mentioned|p251|||||||||
26261|Cues Formation|41145|6|Mentioned|Fig.4|||||||||
26261|Cues Formation|41630|6|Mentioned|Fig.1.3|||||||||
26261|Cues Formation|41633|6|Mentioned|p147|||||||||
26261|Cues Formation|42261|6|Mentioned|Fig 1 P530|||||||||
26261|Cues Formation|42286|6|Mentioned|p7|||||||||
26261|Cues Formation|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26261|Cues Formation|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26261|Cues Formation|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26261|Cues Formation|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26261|Cues Formation|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26261|Cues Formation|42537|4|Described|p10|||||||||
26261|Cues Formation|42595|4|Described|p3, p5|||||||||
26261|Cues Formation|42897|5|Briefly described|Fig.3, P321|||||||||
26261|Cues Formation|43052|6|Mentioned|Fig.4.22|||||||||
26261|Cues Formation|43086|6|Mentioned|Fig.3|||||||||
26261|Cues Formation|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43267|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43268|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
26261|Cues Formation|43572|5|Briefly described|p5|||||||||
26261|Cues Formation|46598|5|Briefly described|p303|||||||||
26261|Cues Formation|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Thackaringa Group (Willyama Supergroup). Overlain by Rasp Ridge Gneiss and Himalaya Formation; underlain by Alders Tank Formation and Alma Gneiss.||||||31-MAY-07
26261|Cues Formation|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Himalaya Suite/Potosi Supersuite. Geological Province: Broken Hill Block.||||||07-NOV-08
26261|Cues Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of theThackaringa Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
26261|Cues Formation|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa  Group.  Geological Province: Broken Hill Domain.||||||03-MAR-05
26261|Cues Formation|61606|5|Briefly described|p4 Fig.2|||Of the Thackaringa Group.||||||18-MAY-06
26261|Cues Formation|61735|5|Briefly described|p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Presented as Cues only in Fig. 2.||||||30-JUN-09
26261|Cues Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological province: Olary Domain.||||||
26261|Cues Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Thackaringa Group.||||
26261|Cues Formation|62536|5|Briefly described|p636|||Broken Hill area.||Thackaringa Group.||Hosts Alma Gneiss.||
26261|Cues Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
26261|Cues Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1700 +/- 3 Ma|Thackaringa Group||||15-DEC-21
26261|Cues Formation|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
26261|Cues Formation|63186|5|Briefly described|p70|Paleoproterozoic|Paleoproterozoic|Of the lower Thackringa Group. Geological Province: Broken Hill Domain, Curnamona Province. Pelitic paragneiss, contains cordierite.||||||07-NOV-08
26261|Cues Formation|63519|5|Briefly described|p6 Fig. 2,, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
26261|Cues Formation|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province.||Thackaringa Group||Intruded by the Alma Gneiss.||
26261|Cues Formation|64097|5|Briefly described|p302, p306-307, p319-320|Paleoproterozoic|Paleoproterozoic|Of Thackeringa Group. Overlies Alma Granite Gneiss and Lady Brassey Fm. Age: ca 1700 Ma. Interpreted as a deformed sill-like granite, including Potosi-type gneiss. Lithol.detail incl.||||||07-FEB-11
26261|Cues Formation|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group (Willyama Supergroup). Geological Province: Broken Hill Block. Contains quartz-feldspathic garnet-rich Potosi-type gneisses.||||||07-FEB-11
26261|Cues Formation|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Of Thackeringa Group. Age: 1700+/-4Ma. Geological province: Broken Hill Domain. Contains various styles of iron formation and a Broken Hill-type Pb-Zn-Ag deposit at Pinnacles Mine occurs in this unit.||||||07-FEB-11
26261|Cues Formation|64742|6|Mentioned|p321 Fig.3. |||||Unit in Thackaringa Group.||||
26261|Cues Formation|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackeringa Group. Age: 1700+/-3Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
26261|Cues Formation|66302|5|Briefly described|p36 Fig.9, p39, p40, p41|Statherian|Statherian|Broken Hill Domain, Curnamona Province. |1700 +/- 4 Ma (Stevens et al, 2008)|Thackaringa Group||Overlies the Alders Tank Formation. Overlain by the Himalaya Formation.  Intruded by the Alma Gneiss.||
26261|Cues Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1700 +/- 4 Ma.|Thackaringa Group.||||
26261|Cues Formation|68126|6|Mentioned|p30||||1700+/-4 Ma; 1701+/-3 Ma (Stevens et al., 2008).|||||
26261|Cues Formation|70000|5|Briefly described|p34-37|Statherian|Statherian|Hosts the Pinnacles Ag-Pb-Zn massive sulfide deposit along with widespread Fe-rich stratiform horizons. Protolith probably sandy marine shelf sediments. Intrusion under shallow cover was syn-depositional. Leucogneisses and Potosi-type gneisses are believed to represent a felsic volcanic or volcaniclastic protolith.||Unit in Thackaringa Group.||Is overlain by Himalaya Formation. Is intruded by Alma Granite Gneiss.|Leucocratic and garnet quartzofeldspathic gneiss ('Potosi-type' gneiss), with locally abundant dykes and sills of basic gneiss.|
26261|Cues Formation|70014|5|Briefly described|Map legend|||The basic gneisses occur in a substantial continuous interval in the middle sections of the Formation, underlain by thinner, less continuous bodies. They are moderately Fe-rich (abundant orthopyroxene or garnet) and finely layered, in places with pale feldspar-rich layers, and are associated with medium-grained quartz-feldspar-biotite-garnet gneiss or rock which occurs in thin bodies or pods. A distinctive leucocratic quartz-microcline-albite(-garnet) gneiss (interpreted as metarhyolite) occurs as thin, continuous and extensive horizons, in several areas. The sulfide-bearing rocks may be lateral equivalents of, or associates of, Broken Hill type stratiform mineralisation. Minor layered garnet-epidote-quartz calc-silicate rocks occur locally within the middle to basal section.||Unit in Thackaringa Group.||Overlies Alders Tank Formation. Is overlain by Himalaya Formation.|Mainly psammopelitic to psammitic composite gneisses or metasediments; intercalated bodies of basic gneiss. Characterised by stratiform horizons of granular garnet-quartz +/-magnetite rocks, quartz-iron oxide/sulfide rocks and quartz-magnetite rocks.|
26261|Cues Formation|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Thackaringa Group.||Overlies Lady Brassey Formation.|Psammopelitic to psammitic composite gneiss. Intercalated basic gneiss associated with quartz-feldspar-biotite-garnet gneiss. Thin magnetite, Fe-sulfide and Fe-garnet-rich horizons.|07-SEP-15
26261|Cues Formation|70405|6|Mentioned|p9 table 1, p40|Paleoproterozoic|Paleoproterozoic||1705 Ma|Thackaringa Group|||Felsic gneiss.|
26261|Cues Formation|70657|5|Briefly described|p13 Fig.6, p14-15, p33, p38|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|1700 +/- 3 Ma|Thackaringa Group||Underlies Himalaya Formation. Overlies Alders Tank Formation. ?Equivalent to Portia Formation in Mulyungarie Domain.||
26261|Cues Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|1700 +/- 3 Ma.|Thackaringa Group.||||
26261|Cues Formation|72461|6|Mentioned|p16 fig 9|||||Thackaringa Group||Overlies the Lady Brassey Formation. Overlain by the Himalaya Formation.||
26261|Cues Formation|73021|5|Briefly described|p224, 235|||Broken Hill. Hosts the Pinnacles deposit: three stratiform Zn-rich lodes and one Pb-rich lode..||Thackaringa Group.||||
26261|Cues Formation|73243|6|Mentioned|p62 Fig.11, p65|Statherian|Statherian|Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.||Thackaringa Group|||Contains amphibolite sills.|
26261|Cues Formation|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Broken Hill Domain. Correlated with Portia Formation.|1700+/-3 Ma maximum depositional age|Thackaringa Group||Overlies Alders Tank Formation, underlies Himalaya Formation||
26261|Cues Formation|73482|5|Briefly described|p422 Fig.3|Statherian|Statherian||1700+/-4 Ma|Thackaringa Group||||
26261|Cues Formation|73512|5|Briefly described|p2-4, p7|Statherian|Statherian|Curnamona Province, Broken Hill Block. Monozite U-Pb SHRIMP age of 1636.8 +/- 4.4 Ma reflects an amphibolite-facies pre-Olarian metamorphic event.||Thackaringa Group, Willyama Supergroup||||
26261|Cues Formation|73524|6|Mentioned|p5 Fig.3|Statherian|Statherian||1700+/-4 Ma|Thackaringa Group||||
26261|Cues Formation|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p838|Statherian|Statherian|Probable host for Pinnacles Mine.|1700+/-4 Ma|Thackaringa Group||Overlies Lady Brassey Formation, underlies Himalaya Formation||
24607|Cullen Bullen Subgroup|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
24607|Cullen Bullen Subgroup|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|||||||
24607|Cullen Bullen Subgroup|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
24607|Cullen Bullen Subgroup|39232|3|Fully described|p107|||See also P111||||||
24607|Cullen Bullen Subgroup|40256|6|Mentioned|Fig.3|||||||||
24607|Cullen Bullen Subgroup|40806|2|Defined|p149|Permian|Permian|Prob. Permian||||||
24607|Cullen Bullen Subgroup|42657|6|Mentioned|Table 1 P74|||||||||
24607|Cullen Bullen Subgroup|42925|5|Briefly described|Table 18||Late Permian|||||||
24607|Cullen Bullen Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
24607|Cullen Bullen Subgroup|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Of Illawarra Coal Measures, western Sydney Basin.||||||
24607|Cullen Bullen Subgroup|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin||||||
24607|Cullen Bullen Subgroup|63832|5|Briefly described|p131 fig 2|||Of Sydney Basin. Final (P4) Paleozoic glaciation.||Unit in Illawarra Coal Measures.||||13-DEC-17
24607|Cullen Bullen Subgroup|64631|6|Mentioned|p44 Fig.2.|Wuchiapingian|Capitanian|Sydney Basin.||Unit in Illawarra Coal Measures.||||
24607|Cullen Bullen Subgroup|68003|5|Briefly described|p38 Fig.3-j.|Late Permian|Late Permian|Western Coalfield, Brigalow Belt South Bioregion.||Unit in Illawarra Coal Measures.|Includes Marrangaroo Conglomerate.|Overlies Nile Subgroup. Is overlain by Charbon Subgroup.||
24607|Cullen Bullen Subgroup|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Unit in Illawarra Coal Measures.||Overlies Nile Subgroup. Is overlain by Charbon Subgroup.||
24607|Cullen Bullen Subgroup|70661|6|Mentioned|p187|||Not present in map area (Moss Vale)||Illawarra Coal Measures||||
82402|Cullendore Supersuite|71628|4|Described|p7: 2; p15: 1-3, 32; p16: 1-32|Middle Triassic|Early Triassic|New name (this study). In this study, includes that portion of the Stanthorpe Type grouping of Blevin and Chappell (1996) that occurs to the N and NE of Undercliffe Falls Monzogranite. Geochemistry summarised.|249-247 Ma.||Five Mile Creek Suite, Wylie Creek Suite, Rivertree Suite; Cullendore Syenogranite.|Intrudes Drake Volcanics and Gilgurry Mudstone.|Pale pink, greyish pink, or pale to dark grey, fine- to coarse-grained, mildly to moderately porphyritic, monzogranite-syenogranite, biotite monzogranite, and biotite-alkali feldspar granite. Locally abundant dykes (described).|
82401|Cullendore Syenogranite|71628|4|Described|p16: 1-26, 28, 30-31; p11: 38-39;|Middle Triassic|Middle Triassic|See also p15: 7, 33, 38-40, 56, 58-59, 69, 82, 115-116;  p19: 59, 67-68, 91, 97-98, 101, 163-164. Chisholm et al. (2014); redefined in this study. Chisholm et al. (2014) applied the name to what is here called the Wylie Creek Monzogranite Phase. Previously the Stanthorpe Monzogranite, then the Maryland River complex (Donchak et al., 2007). Excluded from this author's definition of Stanthorpe Complex. Forms a roughly circular body ~34 x 22 km straddling the Qld/NSW border. Contains five geochemical variants (""Phases""), which the author assigns to two [sic] Suites: Five Mile Creek and Wylie Creek Suites. The unit is not assigned to any Suite, just the Cullendore Supersuite (!?). Lithology described in detail. Hosts only small Sn, Mo, Mo-W deposits. RELATED UNITS (continued): Abuts Thulimbah Monzogranite Phase (Mount Lindesay Monzogranite). Encloses (pods of) Ruby Creek Leucogranite. is faulted against Rivertree Syenogranite and Koreelah Creek Granodiorite. Is locally overlain by Koreelah Conglomerate Member (Marburg Subgroup).|246.9 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Cullendore Supersuite.|Five Mile Creek Syenogranite Phase; Thomkins Gully Monzogranite Phase; Mossvale Alkali Feldspar Granite Phase; Kia-Ora Syenogranite Phase.|Intrudes Silverwood Group; Condamine, Rhyolite Range beds; Gilgurry, Razorback Creek Mudstones; Drake Volcanics; Maryland Granodiorite; Undercliffe Falls Monzogranite. See COMMENTS for more.|Granite complex comprising pale pink, greyish pink, or grey, fine- to coarse-grained, mildly to moderately porphyritic, monzogranite-syenogranite, biotite monzogranite, and biotite-alkali feldspar granite. Locally abundant dykes (described).|
82403|Cullens Creek Granodiorite|71628|4|Described|p9: 1-3; p16:29; p19: 23-27|||New name (this study); originally Cullens Creek Granite (Thomson, 1973) but much modified subsequently. Included in Clarence River Supersuite by Bryant et al. (2003); excluded in this study; unassigned. Named after a local watercourse. Is located E of Cullens Creek, ~25 km SW of Urbenville. Comprises one large and several small bodies. Lithology and mineralogy described; geochemistry detailed. Is located in close proximity to precious metal-bearing fissure veins (eg Bath Hole deposit).|c.246 Ma (Waltenberg and Blevin, unpublished).|Cullens Creek Suite.||Intrudes Emu Creek Formation. Is overlain unconformably by Bundamba Group.|Pale to dark grey, fine- to medium-grained, slightly porphyritic hornblende-biotite granodiorite, quartz diorite and quartz monzodiorite; pale pinkish-grey, leucocratic biotite granodiorite; minor tonalite and aplite. I-type.|
26507|Cumberland Subgroup|22857|5|Briefly described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Illawarra Coal Measures. Includes the Erins Vale and Pheasants Nest Formations. Geological Province: Sydney Basin.||||||
26507|Cumberland Subgroup|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Illawarra Coal Measures.||||||12-MAR-09
26507|Cumberland Subgroup|23544|5|Briefly described|Fig 2 p358|||IN the Illawarra Coal Measures||||||
26507|Cumberland Subgroup|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
26507|Cumberland Subgroup|24471|5|Briefly described|p32 Fig.4|Late Permian|Late Permian|Applies to eastern part of the Southern Coalfield of the Illawarra Coal Measures. Overlain by Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
26507|Cumberland Subgroup|30450|6|Mentioned|Table 1|||Sydney Basin. Permian||||||
26507|Cumberland Subgroup|31649|6|Mentioned|p59|||||||||
26507|Cumberland Subgroup|36593|6|Mentioned|Table 1|||||||||
26507|Cumberland Subgroup|37065|6|Mentioned|p32|||||||||
26507|Cumberland Subgroup|39661|6|Mentioned|p443|||||||||
26507|Cumberland Subgroup|40631|6|Mentioned|p161|||||||||
26507|Cumberland Subgroup|42737|5|Briefly described|map legend|Permian||||||||
26507|Cumberland Subgroup|42896|3|Fully described|p16, Table 2|||Of Illawarra Coal Measures.||||||12-MAR-09
26507|Cumberland Subgroup|42925|5|Briefly described|Table 18||Late Permian|||||||
26507|Cumberland Subgroup|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Abbreviated to Cumberland Subgp in text. Of Illawarra Coal Measures, western Sydney Basin. ||||||
26507|Cumberland Subgroup|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Illawarra Coal Measures. Includes the Pheasants Nest and Erins Vale Formations. Geological Province: Sydney Basin||||||
26507|Cumberland Subgroup|61609|5|Briefly described|p240 Tb. 1, p246 Fig. 5|Permian|Permian|Of Illawarra Coal Measures. Includes Erins Vale and Pheasants Nest Formations. Geological Province: Sydney Basin.||||||07-FEB-11
26507|Cumberland Subgroup|61610|6|Mentioned|p252 Fig. 2|Permian|Permian|Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
26507|Cumberland Subgroup|70661|6|Mentioned|p187|||Not present in map area (Moss Vale)||Illawarra Coal Measures||||
26507|Cumberland Subgroup|71115|5|Briefly described|p180|Permian|Permian|Southern Sydney Basin.||Illawarra Coal Measures.|Pheasants Nest Formation; upper part of Gerringong Volcanics.|Overlies Shoalhaven Group.||
26507|Cumberland Subgroup|73421|6|Mentioned|p19|Capitanian|Capitanian|Sydney Basin, southern. Only appears as Cumberland on p19 below the Sydney Subgroup.||Illawarra Coal Measures|Pheasant Nest Formation, Erins Vale Formation|||
26507|Cumberland Subgroup|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.||Illawarra Coal Measures.|Pheasants Nest Formation.|||
74587|Cumberoona Tonalite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Gunning Suite. Dark grey , coarse-grained, strongly  foliated, porphyritic hornblende-biotite granodiorite and tonalite. Low K, Th and U radioelement response.||||||12-JUN-08
74587|Cumberoona Tonalite|66300|5|Briefly described|p92.|||I-type.|429.2 +/- 2.3 Ma.|Unit in Gunning Suite.||||
74587|Cumberoona Tonalite|68592|2|Defined|p1312-4, p1320, p1323, p1331-3|Early Silurian|Early Silurian|New name, after Cumberoona property. Originally included in Wheeo Granite (now Mulgowrie Granodiorite) of Chappell et al. (1991): distinguished by geochemistry. Comprises four closely associated intrusions c.10km W of Binda. Type locality described. Geochemistry detailed; geophysical properties described. SHRIMP U-Pb zircon age.|429.2 +/- 2.3 Ma (Bodorkos and Simpson, 2008).|Unit in Gunning Suite.||Enclosed by Mulgowrie Granodiorite.|Dark grey to cream, medium- to coarse-grained, mildly to strongly foliated, generally equigranular but sporadically porphyritic, hornblende-biotite tonalite and biotite tonalite; mafic enclaves occur.|
74587|Cumberoona Tonalite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sgc. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Gunning Suite|||Medium-coarse grained, mildly-strongly foliated, generally equigranular but sporadically porphyritic, hornblende-biotite tonalite and biotite tonalite. Low K, Th and U responses; low magnetic susceptibility.|
74587|Cumberoona Tonalite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Gunning Suite|||Medium-coarse grained, mildly-strongly foliated, generally equigranular but sporadically porphyritic, hornblende-biotite tonalite and biotite tonalite. Low K, Th and U responses; low magnetic susceptibility.|
31563|Cumbijowa Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31563|Cumbijowa Suite|44093|5|Briefly described|p181 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31302|Cumboogle Formation|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hyandra Creek Group.  Porphyritic rhyolite, green rhyolite.||||||
80460|Cunninyeuk granite|70718|5|Briefly described|p48, 49, p78-p79|Late Devonian|Late Devonian|Bendigo Zone, Murray Basin. Informal name [Only known from geophysical interpretation]. Size and rough shape of magnetic anomalies is provided. Interpreted lithology and age  based on similar geophysical signature to outcropping Lake Boga and Pyramid Hill granites.||Cunninyeuk granite suite|||Interpreted to be S-type granite , with metamorphic aureole..|02-JUN-19
80441|Cunninyeuk granite suite|70718|5|Briefly described|p3,p49,  p71, p78-80, p60, p94, p128|Late Devonian|Late Devonian|Informal name, derived from geophysics. Magnetic response suggests S-type granites. Interpreted lithology and age  based on similar geophysical signature to outcropping Lake Boga and Pyramid Hill granites.|||Includes the Cunninyeuk, Baldon, Moolpa and Wyam Creek granites.||Interpreted to be S-type granites , with metamorphic aureoles.|02-JUN-19
24235|Cupala Creek Formation|22671|5|Briefly described|p832|Ordovician|Late Cambrian|Coarse terrestrial and shallow marine sediments.||||||17-JAN-06
24235|Cupala Creek Formation|22857|5|Briefly described|p91 Fig. 14.7B, p120|Late Cambrian|Late Cambrian|Olive-grey siltstone, red and grey arenite, basal conglomerate. Unconformably overlies the Copper Mine Range beds. Max. thickness: 1000m. Geological Province: Gnalta Shelf. See also p200 and p410 App. 1 Tb. A1.4.||||||
24235|Cupala Creek Formation|22858|6|Mentioned|Fig14.7bp90-1|Late Cambrian|Late Cambrian|||||||
24235|Cupala Creek Formation|22859|5|Briefly described|p200||Early Paleozoic|||||||07-NOV-08
24235|Cupala Creek Formation|23245|5|Briefly described|p120,122||Idamean|||||||
24235|Cupala Creek Formation|23336|6|Mentioned|3|||||||||
24235|Cupala Creek Formation|23380|5|Briefly described|p107,119||Late Cambrian|In the of Wonaminta Block.||||||11-SEP-07
24235|Cupala Creek Formation|23469|5|Briefly described|Fig 13 p 327|||||||||
24235|Cupala Creek Formation|38692|3|Fully described|p129|||||||||
24235|Cupala Creek Formation|39885|6|Mentioned|Fig.2|||||||||
24235|Cupala Creek Formation|41587|6|Mentioned|p905|||||||||
24235|Cupala Creek Formation|41810|6|Mentioned|p108|||||||||
24235|Cupala Creek Formation|42121|5|Briefly described|Fig.1 P97|||See also Fig.2b||||||
24235|Cupala Creek Formation|42140|6|Mentioned|p557|||||||||
24235|Cupala Creek Formation|42364|5|Briefly described|p211|||See also Fig. 1||||||
24235|Cupala Creek Formation|42460|5|Briefly described|Fig.1 P206|||||||||
24235|Cupala Creek Formation|43192|6|Mentioned|p64.|||Koonenberry Mountain. Includes conglomerates that relate to Mootwingee Group conglomerates.||||||
24235|Cupala Creek Formation|44093|5|Briefly described|p109|Late Cambrian|Late Cambrian|Unconformably overlies Copper Mine Range beds. See also p148 Appendix 1. Geological Province: Tasman Fold Belt.||||||01-APR-05
24235|Cupala Creek Formation|47036|6|Mentioned|p100|||||||||
24235|Cupala Creek Formation|50618|5|Briefly described|p249|||Quartzose sandstone, siltstone and shale.||||||
24235|Cupala Creek Formation|63489|5|Briefly described|Map legend|Ordovician|Late Cambrian|Fluvial and terrigenous coarse clastic sediments, including conglomerate.||||||10-SEP-07
24235|Cupala Creek Formation|63793|6|Mentioned|p19 Table 1, p38, p24.|Cambrian|Cambrian|||||||19-JAN-15
24235|Cupala Creek Formation|64671|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Unconformably overlies Copper Mine Range beds and Teltawongee beds east of Koonenberry Fault. Contains shale, sandstone and conglomerate equivalents to Watties Bore, Boshy and Morden Formations of the Kayrunnera Group.||||||26-NOV-08
24235|Cupala Creek Formation|64683|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Kayrnnera Group. Massive to well-laminated shales and siltstones, well-laminated quartzose sandstones and quartzites, and basal conglomerate with a wide range of local and foreign clasts.||||||
24235|Cupala Creek Formation|64684|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Unconformably overlies Copper Mine Range beds and Teltawongee beds east of Koonenberry Fault.||||||20-MAY-13
24235|Cupala Creek Formation|65381|6|Mentioned|p689|Cambrian|Cambrian|||||||
24235|Cupala Creek Formation|66623|1|Redefined|p43, pp120-121, pp126-127.|Late Cambrian|Late Cambrian|Defined in this study as comprising the upper (siltstone) sequence of the Cupala Creek Formation of Powell et al. (1982) which was included in Kayrunnera Group by Mills and Hicks (2000). Nuntherungie and Cupala Creek Basins. Represents continuation of post-Delamerian Orogeny erosion and deepening environment of deposition.||Unit in Kayrunnera Group.|Includes Williams Creek Conglomerate.|Conformably overlies Hummock Formation. Locally unconformably overlies Copper Mine Range Formation. Is unconformably overlain by Rocky Tank Conglomerate Member, or top of unit has faulted contacts.|Pale olive-grey or khaki, variably-cleaved shale and siltstone, interbedded with minor pale grey to red, fine-grained sandstone (brachiopod fossils) and impure limestone (trilobite fossils) lenses; yellow-brown weathering. From 390 to 4000 m thick.|20-MAY-13
24235|Cupala Creek Formation|66929|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Equivalent to Kayrunnera Group.||||Unconformably overlies Copper Mine Range beds and Teltawongee beds.|Shale, sandstone, conglomerate.|31-JAN-12
24235|Cupala Creek Formation|67322|4|Described|p11, p20 Fig.5|Late Cambrian|Late Cambrian|Of Powell et al. (1982); redefined and subdivided by Greenfield (in Greenfield et al. 2010) into the Hummock and Cupala Creek Formations; eg an unnamed basal conglomerate facies is now the Williams Creek Conglomerate. Idamean age is determined from trilobite fossils. Thickness varies between about 390m (Cupula Creek) to around 4000m (Nuntherungie structural outlier). Occurs in the Kayrunnera-Koonenberry region.||Of the Kayrunnera Group.||Conformably overlies the Hummock Formation.|Siltstone dominated.|21-FEB-18
24235|Cupala Creek Formation|67562|5|Briefly described|p95, p105 Fig.11, p112|Late Cambrian|Late Cambrian|~ 1km thick. Sediment was derived from uplift SW of the Koonenberry Fault.||||||23-JAN-17
24235|Cupala Creek Formation|70838|5|Briefly described|p269 Fig.3, p270|Late Cambrian|Late Cambrian|Nuntherungie Basin, SE Koonenberry Belt. Contains Idamean brachiopods and trilobites.|499-496 Ma.|Kayrunnera Group.||Overlies Williams Creek Conglomerate.||
24236|Curdimurka Subgroup|22589|6|Mentioned|p129||Neoproterozoic|||||||
24236|Curdimurka Subgroup|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
24236|Curdimurka Subgroup|22772|4|Described|p65,Table13.1|Cryogenian|Cryogenian|||||||
24236|Curdimurka Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Callana Group.||||||
24236|Curdimurka Subgroup|22926|6|Mentioned|37|||Geol province Spalding Inlier. Parent Callana Group||||||
24236|Curdimurka Subgroup|23054|6|Mentioned|p11,34|||||||||
24236|Curdimurka Subgroup|24175|3|Fully described|p9|Neoproterozoic|Neoproterozoic|Of Callana Group.  Overlain by Burra Group.  Max. thickness: 4700m.||||||
24236|Curdimurka Subgroup|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Callanna Group||||||
24236|Curdimurka Subgroup|24506|6|Mentioned|p17|Neoproterozoic|Neoproterozoic|||||||19-SEP-05
24236|Curdimurka Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Arkaroola Subgroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
24236|Curdimurka Subgroup|24584|6|Mentioned|p14 Fig. 2|Neoproterozoic|Neoproterozoic|Marble.||||||
24236|Curdimurka Subgroup|24586|5|Briefly described|p51 Fig. 1|Adelaidean|Adelaidean|Upper part of Callanna Group (Warrina Supergroup).  Allochthonous breccia comprising sandstone, limestone and shale contained within a matrix of yellow-weathering dolomite and associated volcanics of the Callana Volcanics. Geol.Prov: Adelaide Geosyncline.||||||05-JUL-06
24236|Curdimurka Subgroup|37854|2|Defined|p9|Adelaidean|Adelaidean|See also p9.Willouran||||||12-MAR-14
24236|Curdimurka Subgroup|38004|6|Mentioned|p82|||||||||
24236|Curdimurka Subgroup|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran to SturtianWillouran||||||
24236|Curdimurka Subgroup|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24236|Curdimurka Subgroup|39490|6|Mentioned|p10|||||||||
24236|Curdimurka Subgroup|40225|6|Mentioned|Map sheet|||||||||
24236|Curdimurka Subgroup|40294|6|Mentioned|p8|||See also P12||||||
24236|Curdimurka Subgroup|41401|6|Mentioned|Table 4|||||||||
24236|Curdimurka Subgroup|41402|6|Mentioned|p42|||||||||
24236|Curdimurka Subgroup|41403|4|Described|p59|||||||||
24236|Curdimurka Subgroup|41404|6|Mentioned|p73|||||||||
24236|Curdimurka Subgroup|41405|6|Mentioned|p125|||||||||
24236|Curdimurka Subgroup|41526|6|Mentioned|p31|||||||||
24236|Curdimurka Subgroup|42098|6|Mentioned|Table 2 P54|||||||||
24236|Curdimurka Subgroup|42101|6|Mentioned|p84|||||||||
24236|Curdimurka Subgroup|42222|4|Described|p12|||||||||
24236|Curdimurka Subgroup|42223|5|Briefly described|p37|||||||||
24236|Curdimurka Subgroup|42238|5|Briefly described|p71|||||||||
24236|Curdimurka Subgroup|42720|5|Briefly described|map legend|Willouran||||||||
24236|Curdimurka Subgroup|42813|4|Described|p14|||of Callanna Group||||||
24236|Curdimurka Subgroup|43052|4|Described|p175|||of Callanna Group||||||
24236|Curdimurka Subgroup|43742|6|Mentioned|p37|||||||||
24236|Curdimurka Subgroup|43845|5|Briefly described|Fig2 p42, 44||Neoproterozoic|In Callanna Group||||||12-JUL-16
24236|Curdimurka Subgroup|44133|6|Mentioned|p52|||||||||
24236|Curdimurka Subgroup|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24236|Curdimurka Subgroup|60718|5|Briefly described|p49 Fig. 2, p50|Adelaidean|Adelaidean|Geol Prov: Adelaide Geosyncline. See also p51 Fig. 3.||Of Callanna Group.|Includes: Boorloo Siltstone, Coranna Fm, Hogan Dolomite; Recovery Fm, Dunns Mine Limestone, and Rook Tuff; and Dome Sandstone, from top to bottom.|||15-APR-11
24236|Curdimurka Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Callanna Group.||||||
24236|Curdimurka Subgroup|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, p57.|Willouran|Willouran|Deposited in deeply subsiding graben structures during rifting. Colour scheme shown for interpretation of Curnamona seismic sections. Written as SubGroup.||Unit in Callanna Group.|||Clastics, carbonates, evaporites.|
24236|Curdimurka Subgroup|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in upper Callanna Group.|Includes Rook Tuff.|Unconformably overlies Arkaroola Subgroup. Is unconformably overlain by Burra Group.|Sandstone, siltstone, shale, carbonates, tuff.|
24236|Curdimurka Subgroup|62724|6|Mentioned|p16, p21|||Evaporitic clastic and carbonate sediments. Mostly absent from Curnamona Province - particularly over Olary Domain where it is eroded away.||||||07-FEB-11
24236|Curdimurka Subgroup|64793|6|Mentioned|p284 fig 3, p285|||||Unit in Callanna Group.|Includes Rook Tuff.|||
24236|Curdimurka Subgroup|64796|6|Mentioned|p183 fig 2, p184, p187-188, p200-202|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex. Type area in Willouran Ranges.||Unit in Callanna Group.|Includes Rook Tuff.|||
24236|Curdimurka Subgroup|64797|5|Briefly described|p151, p158, p163, p164 Fig.11 |||See also p169 Fig.12 . S-isotope data. International correlations.|800 Ma.|Unit in Callanna Group.|Includes River Broughton beds.|||
24236|Curdimurka Subgroup|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Rook Tuff dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986).||||||19-MAR-12
24236|Curdimurka Subgroup|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Rook Tuff dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986).||||||19-MAR-12
24236|Curdimurka Subgroup|65379|5|Briefly described|p643, p644, p646|Neoproterozoic|Neoproterozoic|Of Callanna Group (Warrina Supergroup). Siltstone, dark-grey; sandstone; dolomite; limestone, stromatolitic. N.B.  Asbestos deposit host, contains Adams, Arkaba, Peate and Mt Lyndhurst asbestos prospects, and Oraparinna asbestos mine.||||||07-MAR-12
24236|Curdimurka Subgroup|66522|5|Briefly described|p19.|Neoproterozoic|Neoproterozoic||||Includes Rook Tuff.|||
24236|Curdimurka Subgroup|66884|6|Mentioned|p36, p41 Fig.3|||Age: Willouran||Callanna Group|||Megabreccia.|
24236|Curdimurka Subgroup|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Callanna Group.|Rook Formation.|||
24236|Curdimurka Subgroup|67979|5|Briefly described|p528|Cryogenian|Cryogenian|||of the upper Callanna Group|includes Rook Tuff|||
24236|Curdimurka Subgroup|69019|4|Described|p36-38, p66.|Neoproterozoic|Neoproterozoic|Cyclic sequences of clastics and carbonates deposited under partly evaporitic conditions, partly in fault controlled basins. Age from Rook Tuff in adjacent map area.|802 +/- 10 Ma (U-Pb zircon: Fanning et al. 1986).|Unit in Callanna Group.|Includes Recovery Formation, Cooranna Formation, Boorloo Siltstone.||Siltstone: laminated, carbonaceous, lithic, pyritic and micaceous; sandstone: feldspathic to lithic, cross-bedded and ripple-marked; stromatolitic dolomite and limestone.|
24236|Curdimurka Subgroup|69666|6|Mentioned|p33||||||Rook Tuff.|||
24236|Curdimurka Subgroup|69873|6|Mentioned|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.|||Includes Rook Tuff.|||
24236|Curdimurka Subgroup|70334|5|Briefly described|p38|||Geological province: Gawler Craton. Of Adelaide Geosyncline.||Unit of Callana Group.||||
24236|Curdimurka Subgroup|70405|6|Mentioned|p97|Neoproterozoic|Neoproterozoic||||||Clastic-carbonate-evaporite sediments.|
24236|Curdimurka Subgroup|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Willouran||Of Callanna Group.||||
24236|Curdimurka Subgroup|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.||Callanna Group.|Rook Tuff.|||
24236|Curdimurka Subgroup|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet. |||||Siltstone, dark grey, carbonaceous, lithic, pyritic, laminated, micaecous; sandstone, feldspathic, lithic, cross-bedded, halite clasts; dolomite, stromatolitic, cryptalgal laminated, brown to yellow weathering; limestone, stromatolitic.|
24236|Curdimurka Subgroup|72492|3|Fully described|p1, p2-3, p5 Fig.4, p5 Fig.5|Neoproterozoic|Neoproterozoic|Type locality said to be in Willouran Ranges. Interpreted as a coastal sabkha or playa lake environment that became progressively more restricted from south to north. Alternative interpretation is alkaline lake environment, like East African rift valley, but this paper dismisses this option. See also p17-18. Samples collected from the type locality in the Willouran Ranges. Misspelt as Curdimurka Subroup twice on p2.|802 +/- 10 Ma|Callanna Group|Dome Sandstone, Rook Tuff, Dunns Mine, Waraco Limestones, Recovery, Cooranna Formations, Hogan, Worumba Dolomites, Boorloo Siltstone, Wirrawilka, Niggly Gap, Arkaba Hill beds, Kirwan Siltstone.|Overlies Arkaroola Subgroup.|Includes cyclically alternating siliciclastic sediments, carbonates, evaporites and minor volcanic flows. Major outcrop areas occur in the Peake and Denison Ranges, the Willourian Ranges, the Worumba Anticline and the Spalding Inlier.|16-SEP-20
24236|Curdimurka Subgroup|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Carbonaceous-pyritic siltstone and feldspathic-lithic sandstone, stromatolitic limestone and dolomite, minor felsic volcanics and volcaniclastics.|09-DEC-21
24236|Curdimurka Subgroup|73222|5|Briefly described|p6-7, p21|Tonian|Tonian|Adelaide Rift Complex. Upper part of the Callanna Group. Outcrops in the Willouran Ranges.||Callanna Group, Warrina Supergroup|Dunns Mine and Waraco limestones, Dome Sandstone; Boorloo and Kirwan siltstones; Hogan and Worumba dolomites; Cooranna and Recovery formations; Rook Tuff; Arkaba Hill, Niggly Gap, and Wirrawilka Beds|Underlain by Arkaroola Subgroup.||
24236|Curdimurka Subgroup|74367|5|Briefly described|p7 Fig.6, p8, p18, p20|Tonian|Tonian|Suggested to include the Oodla Wirra Volcanics based on evaporite mineralogy and SHRIMP ages. Age of 802+/-10 Ma from Rook Tuff (Fanning et al., 1986). Not deposited in the Arkaroola area.|802+/-10 Ma|Callanna Group|Dome Sandstone, Rook Tuff, Niggly Gap Beds, Recovery Formation, Cooranna Formation, Boorloo Siltstone|||
24238|Curmulee Conglomerate|22815|5|Briefly described|p102|||||||||
24238|Curmulee Conglomerate|22857|5|Briefly described|p216, p494 App. 1 Tb.A1.7|Frasnian|Frasnian|Of Minuma Range Group. Reddish-brown massive medium-grained polymictic conglomerate, minor pebbly arenite and siltstone. Together with Big Hole Formation, separates the Long Swamp Creek and Deua Formations. Max. thickness: 20m. Geol. Prov: Lambie Shelf.||||||
24238|Curmulee Conglomerate|22859|5|Briefly described|p216|||||||||
24238|Curmulee Conglomerate|39028|6|Mentioned|Map legend|Famennian|Famennian|||||||
24238|Curmulee Conglomerate|40276|2|Defined|p24|Late Devonian|Late Devonian|||||||
24238|Curmulee Conglomerate|42497|5|Briefly described|Map legend|Famennian|Frasnian|||||||
24238|Curmulee Conglomerate|71700|5|Briefly described|CD|Late Devonian|Late Devonian|Ages derived from fossil assemblage.||Minuma Range Group||Unconformably overlies the Long Swamp Creek Formation.||
24238|Curmulee Conglomerate|73181|6|Mentioned|p65-66|Frasnian|Frasnian|||Minuma Range Group||Underlain by Long Swamp Creek Formation and Big Hole Formation. Overlain by Deua Formation.||
33194|Currah Granite|24417|4|Described|p54|Early Silurian|Early Silurian|||||||
33194|Currah Granite|50554|5|Briefly described|Map legend|Silurian|Silurian|Biotite muscovite granite.||||||
33194|Currah Granite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|Of the Ungarie Suite.||||||13-JUL-04
33194|Currah Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Biotite-muscovite granite (as subcrop only).|
38099|Currangandi Group|50613|2|Defined|p205, p226 App.1|Westphalian|Namurian|Comprises Spion Kop Conglom., Ermelo Pyroclastics, Clifden Fm., Rocky Creek Conglom., Lark Hill Fm. in the Rocky Creek region; Willuri Fm. (Carroll-Nandewar region) and Currabubula Formation in the Werrie Syncline.  Age: 297-287Ma (SHRIMP).||||||22-FEB-05
38099|Currangandi Group|66720|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous||||Includes Currabubula Formation.|||
28491|Currango beds|45147|6|Mentioned|M78|||||||||
74607|Currawalla Shale|61964|2|Defined|p14 Fig. 4, p31|Bolindian|Gisbornian|Of Bendoc Gp. Formerly Trigg's Tallebung Group (1987). Finely laminated or massive shale (grading to slate) with minor interbedded qtz sst with graptolites. Conformable under Willandra Sst (inferred). Max.thickness: 200m. Palaeontology details (p258-259)||||||03-NOV-15
74607|Currawalla Shale|64568|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Bendoc Group. Massive or laminated black slate to siliceous mudstone, minor thin interbeds of fine sandstone.||||||23-SEP-08
74607|Currawalla Shale|65469|5|Briefly described|p18|Late Ordovician|Late Ordovician|Lachlan Orogen.||||Overlain by the Willandra Sandstone. Overlies the Clements Formation.||
74607|Currawalla Shale|67322|4|Described|p19; Fig.5|Late Ordovician|Late Ordovician|Formally defined by Colquhoun and Hendrickx, in Colquhoun et al. (2005). Contains graptolites which are Gisbornian to early Bolindian in age. Attains a thickness of about 100-200m (not allowing for internal thrust imbrication). Occurs in the Cargelligo region.||Of the Bendoc Group||Equivalent to the Warbisco Shale. Interfingers with and is overlain by the Willandra Sandstone. Overlies ?conformably Doongala Chert Member (Ballast Formation).|Black shales.|21-FEB-18
74607|Currawalla Shale|68466|6|Mentioned|p65|Late Ordovician|Late Ordovician|Albury-Bega Terrane.||||||
74607|Currawalla Shale|68592|5|Briefly described|p320, p343, p351, p364|||Central NSW.||Unit in Bendoc Group.||Is overlain conformably by Willandra Sandstone. Equivalent to Warbisco Shale.||
74607|Currawalla Shale|69160|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Bendoc Group.||Is overlain by Willandra Sandstone.|Massive or laminated black slate to siliceous mudstone, minor thin interbeds of fine sandstone.|
74607|Currawalla Shale|69540|5|Briefly described|p640|Bolindian|Gisbornian|Cargelligo 1:250 000 sheet area.||Unit in Bendoc Group.|||Mainly black shale; interbeds of quartz-rich sandstone.|
74607|Currawalla Shale|69668|6|Mentioned|p929 Fig.2|Late Ordovician|Late Ordovician|Cargelligo area, Albury-Bega terrane.||||Overlies Clements Formation. Is overlain by Willandra Sandstone.||
74607|Currawalla Shale|70751|6|Mentioned|p12|Eastonian|Gisbornian|||Bendoc Group||||
74607|Currawalla Shale|71069|5|Briefly described|p72, p74, p77, p87|Early Silurian|Gisbornian|Estimated 100-200m thick. Generally recessive outcrop characteristics except where it is contact metamorphosed.Contains Gisbornian graptolite fossils.||Bendoc Group||Conformably overlain by the Willandra Sandstone. Is equivalent to the Warbisco Shale and members of the Margules Group.|Laminated or massive, pyritic, carbonaceous black shale to siliceous mudstone with minor thin interbeds of fine grained, white sandstone.|
74607|Currawalla Shale|71889|5|Briefly described|p12, p17|Bolindian|Eastonian|||Bendoc Group||Overlain by the Willandra Sandstone.|Dark coloured shales with very minor fine-grained sandstone.|
74607|Currawalla Shale|72083|6|Mentioned|p10|||||Bendoc Group.||||
74607|Currawalla Shale|72084|5|Briefly described|p7|Late Ordovician|Late Ordovician|Forms low tabular outcrops. Thickness c.250m. Dips steeply (80 degrees) to the SW.||Bendoc Group.||Is overlain by, and intercalated with, the Willandra Sandstone. Is faulted against the Wagga Group.|Dark grey to black shale with well-developed slaty cleavage.|
74607|Currawalla Shale|73140|5|Briefly described|p495 Fig.1, Fig.6|Bolindian|Gisbornian|Age based on graptolites.||Bendoc Group||Overlies Abercrombie Formation, Doongala Chert Member, underlies Willandra Sandstone||
27138|Currawang Basalt|22857|4|Described|p176, p472 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Mount Fairy Group. Overlies and interfingers with Woodlawn Volcanics. Max. thickness: 1000m. Geological Province: Captains Flat-Goulburn Trough. ||||||
27138|Currawang Basalt|23048|5|Briefly described|p7 fig9|Late Silurian|Silurian|||||||
27138|Currawang Basalt|24318|5|Briefly described|p20|Late Silurian|Late Silurian|Basic volcanic and intrusive rocks commonly containing pillows and/or abundant vesicles.||||||
27138|Currawang Basalt|30730|4|Described|p8|||||||||
27138|Currawang Basalt|30734|6|Mentioned|p37|||||||||
27138|Currawang Basalt|30735|2|Defined|p23|Silurian|Silurian|||||||
27138|Currawang Basalt|30736|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
27138|Currawang Basalt|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
27138|Currawang Basalt|33959|6|Mentioned|p235|||||||||
27138|Currawang Basalt|35503|6|Mentioned|p201|||Defined in Felton and Huleatt (1977)||||||
27138|Currawang Basalt|35660|6|Mentioned|p155|||||||||
27138|Currawang Basalt|35662|6|Mentioned|p139|||Geology of the Woodlawn district.||||||
27138|Currawang Basalt|39174|6|Mentioned|p1959|||||||||
27138|Currawang Basalt|39331|6|Mentioned|p57|||||||||
27138|Currawang Basalt|40328|5|Briefly described|p184|||||||||
27138|Currawang Basalt|41140|6|Mentioned|p143|||||||||
27138|Currawang Basalt|42177|6|Mentioned|p214|||||||||
27138|Currawang Basalt|42727|5|Briefly described|map legend|Ludlow|Ludlow|Of Mount Fairy Group. Basalt with interbedded shale and minor quartz sandstone, chert and felsic tuff. Overlies Woodlawn Volcanics; underlies Covan Creek Formation; unconformably overlies Birkenburn beds. BMR map symbol: Suc. Geol. Prov: Rocky Pic Block.||||||
27138|Currawang Basalt|42820|3|Fully described|p54|||Of Mount Fairy Group.||||||22-MAY-08
27138|Currawang Basalt|50232|4|Described|Map legend|Ludlow|Ludlow|Of the Mount Fairy Group. Overlies Woodlawn Volcanics; overlain by Covan Creek Formation.  Dark green amygdaloidal meta-pillow-basalt, cherty mudstone, tuffaceous siltstone and mudstone.||||||22-MAY-08
27138|Currawang Basalt|50234|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Mount Fairy Group. Underlies: Covan Creek Formation.||||||22-MAY-08
27138|Currawang Basalt|60308|6|Mentioned|p40|||Directly overlies host silicic volcanics of Woodlawn deposit.||||||
27138|Currawang Basalt|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Dark green amygdaloidal meta-pillow basalt, cherty mudstone, tuffaceous siltstone and mudstone.||||||11-JUN-08
27138|Currawang Basalt|66087|5|Briefly described|p5, p3 Fig. 2|Silurian|Silurian|Probably interfingers with underlying Woodlawn Volcanics.||Of the Mount Fairy Group.||||10-MAY-12
27138|Currawang Basalt|67820|6|Mentioned|p136|Late Silurian|Late Silurian|||Mount Fairy Group.||||
27138|Currawang Basalt|68592|2|Defined|p729 Fig.132, p799, p802, p821, p805-809|Early Silurian|Early Silurian|See also p151, p174-176, p266, p726, p728, p879. Felton and Huleatt (1977) after Felton (1974). Type section is defined (Felton and Huleatt, 1977). Regular, rubbly outcrop in low hills. Thickness: estimated max: ~1000 m. unit is in a fold hinge; its distribution suggests it originally formed a lensoid pile. Eruptions in marine setting, in water below wave-base; crustal thinning and high-temperature, low-pressure melting of mantle material produced basalt with tholeiitic to transitional affinities. Lower greenschist facies metamorphism. Medium- to low-K calc-alkaline transitional to tholeiitic, in an intraoceanic arc/back arc setting. Max age: from underlying Woodlawn Volcanics. Min age: Ludlow is implied by mid-late Ludlow age of uppermost De Drack Formation which occupies same stratigraphic position beneath Covan Creek Formation. Thus age most likely mid-late Ludlow. Hosts historic Currawang copper mine and Currawang East Cu-Pb-Zn-Ag-Au deposit (detailed: mineralisation in sheared basalt units is interpreted as deformed replacement-type VHMS system). Geophysical properties described.||Unit in Mount Fairy Group.||Conformably overlies Woodlawn Volcanics; gradationally overlain by (and in part interfingers with) Covan Creek Formation.|Grey-green to grey, pillowed and flow-banded amygdaloidal basalt ; occasional interpillow hyaloclastite, rare mafic volcaniclastic sandstone, siltstone and mudstone; minor quartzose sandstone at top.|
27138|Currawang Basalt|69159|5|Briefly described|Map legend|Ludlow|Ludlow|||Unit in Mount Fairy Group.|||Grey-green to bluish-grey, fine- to medium-grained, aphanitic to porphyritic, pillow basalt and dolerite, commonly vesicular; minor quartz-sericite siltstone, siliceous mudstone and very fine-grained quartzose to quartzofeldspathic sandstone.|07-SEP-15
27138|Currawang Basalt|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sfc. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group||Overlies, and interfingers with, Woodlawn Volcanics. Is overlain by, and interfingers with, Covan Creek Formation.|Grey-green grey, amygdaloidal flow banded pillow basalt, fine grained basaltic hyaloclastite, rare mafic volcaniclastic sandstone, siltstone and mudstone.|
27138|Currawang Basalt|70541|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|||Grey-green to grey, amygdaloidal flow banded pillow basalt; fine grained basaltic hyaloclastite; rare volcaniclastic sandstone, siltstone and mudstone.|
27138|Currawang Basalt|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|||Grey-green grey, amygdaloidal flow banded pillow basalt, fine grained basaltic hyaloclastite, rare mafic volcaniclastic sandstone, siltstone and mudstone.|
27138|Currawang Basalt|71069|3|Fully described|p9, p21 fig 7, p26, p27, p28, p29|Ludlow|Ludlow|Named for the Currawang locality. Contains an unnamed dolerite and gabbro member. Type section given at GR 730113 6125484 to GR 730470 6125525. Hosts Pb-Zn-Cu-Ag-Au VAMS mineralisation and small scale vein base metal deposits. Tholeiitic to transitional geochemical affinities. Deposited in a deep marine environment in a back arc tectonic setting. 820m to an estimated 1000m thick. Equivalent to an unnamed basalt in the Captains Flat Formation and rocks of the Thurralilly Suite.Distribution, geomorphology, geochemistry, primary structures/textures, tectonic structure, metamorphism and geophysical characteristics discussed.  See also p29 fig 11 and 12, p35, p38 fig 15, p40 fig 17, p45, p133, p135, p136 fig 44, p139 fig 45, p140 tbl 4, p141, p144, p147, p156, p159, p162-168, p175, p178, p179, p184, p185. ||Mount Fairy Group||Overlies the Woodlawn Volcanics. Conformably overlain by (and partially interfingers with) the Covan Creek Formation. Conformably overlies the De Drack Formation.|Fine to medium grained, aphanitic to porphyritic, massive to pillowed basalt, dolerite and minor siltstone and fine grained sandstone. Basalt is in places interbedded with laminated to thinly bedded hyaloclastite, chert and mudstone.|
27138|Currawang Basalt|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Mount Fairy Group.||Overlies Woodlawn Volcanics. Is overlain by Covan Creek Formation.|Grey-green to blue-grey, fine- to medium-grained, aphanitic to porphyritic, massive- to pillow-basalt and dolerite; commonly vesicular; minor khaki-green, brown and buff laminated to thin-bedded quartz-sericite siltstone and siliceous mudstone.|
27138|Currawang Basalt|71699|5|Briefly described|Map legend.|Devonian|Silurian|Lithology continued: minor khaki to green, brown and buff, diffusely laminated to thinly bedded quartz-sericite siltstone, siliceous mudstone and very fine-grained quartzose to quartzofeldspathic sandstone. The igneous and sedimentary facies are mapped separately.||Mount Fairy Group.||Overlies Woodlawn Volcanics. Is overlain by Covan Creek Formation.|Grey-green to bluish-grey, fine- to medium-grained, aphanitic to porphyritic, pillow basalt and dolerite, commonly vesicular. See Comments for more.|
27138|Currawang Basalt|71700|2|Defined|vi, viii, p7, p17-p22|Ludlow|Ludlow|Contains two unnamed subunits. A type section was defined by Felton and Huleatt (1977) between GR 730113 6125484 to GR 730613 6125484. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. Age is derived from dating of related units and stratigraphic position of correlaative units, Composition is consistent with generation under an extensional back-arc tectonic regime. Up to 1km thick centered in the Currawang area from which this units name is derived. See also p48-p50, p76, p80, p84, p90, p95, p123, CD.||Mount Fairy Group||Conformably overlies the Woodlawn Volcanics. Conformably overlain by the Covan Creek Formation.|Massive to pillow basalt and fine-grained dolerite of extrusive or high level intrusive origin.|
30310|Curricabark Formation|24008|5|Briefly described|p355|||||||||
30310|Curricabark Formation|73440|6|Mentioned|p129-130, p132|||[Also written as Curricabank Formation, p129]. Gamilaroi terrain.||||Underlain by Captain Rocks Formation.|Fine-grained laminated volcaniclastic rocks.|
78494|Currowan Creek Basalt Member|66768|4|Described|p212, p212 Fig.3, p213-218|Late Devonian|Middle Devonian|Informal member of Comerong Volcanics. Also written as Currowan Creek Basaltic Member on p213. Max thickness 1700m. Many 1-2m thick flows, commonly amygdaloidal; amygdales filled with quartz, chlorite, calcite and epidote. Fluviatile, red sandstone and siltstone interbedded in the top 80m of unit.||||||07-NOV-13
31705|Curumbenya Ignimbrite Member|22857|5|Briefly described|p490 App.1 Tb.A1.7|Middle Devonian|Middle Devonian|Of the Dulladerry Volcanics. Geological Province: Dulladerry Rift.||||||
31705|Curumbenya Ignimbrite Member|23043|5|Briefly described|Map Legend|Givetian|Givetian|of Dulladerry Volcanics.||||||
31705|Curumbenya Ignimbrite Member|23170|4|Described|p232|Middle Devonian|Middle Devonian|of Dulladerry Volcanics.||||||
31705|Curumbenya Ignimbrite Member|23214|3|Fully described|p223|Givetian|Givetian|Of Dulladerry Volcanics. Quartz and K-feldspar - phyric ignimbrite. Age: 376+/-4Ma (SHRIMP U/Pb). Underlying unit: Warraberry Member. Maximum thickness: >200m.||||||
31705|Curumbenya Ignimbrite Member|24417|3|Fully described|p117|Middle Devonian|Middle Devonian|Of Dulladerry Volcanics.||||||
31705|Curumbenya Ignimbrite Member|43640|5|Briefly described|Map Legend|Devonian|Devonian|of Dulladerry Volcanics.||||||
31705|Curumbenya Ignimbrite Member|43782|5|Briefly described|Map Legend|Givetian|Givetian|of Dulladerry Volcanics.||||||
31705|Curumbenya Ignimbrite Member|60009|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Dulladerry Volcanics (Rocky Ponds Group).||||||13-JUL-04
31705|Curumbenya Ignimbrite Member|62569|5|Briefly described|p609|Middle Devonian|Middle Devonian|Of Dulladerry Volcanics. Age: 376+/-4Ma (Raymond, 1998)||||||
31705|Curumbenya Ignimbrite Member|70297|5|Briefly described|map legend|Middle Devonian|Middle Devonian|||Dulladerry Volcanics||||
33122|Cusin Creek Granite|22553|5|Briefly described|p77|Statherian|Statherian|Intruded Paragon Group sediments.||||||11-JUN-08
33122|Cusin Creek Granite|63519|5|Briefly described|p6 Fig. 2, p12|Mesoproterozoic|Mesoproterozoic|Age: 1596+/-3Ma. Geological Province: Broken Hill Block-Euriowie Block. Intrudes Bijerkerno Metasediments. Exhibits a biotite schistosity.||||||11-JUN-08
33122|Cusin Creek Granite|63866|5|Briefly described|p38||||1596 +/- 3 Ma (Page et al., 2005a)|||||
33122|Cusin Creek Granite|64316|6|Mentioned|p533 Fig. 1|||Mundi Mundi-type granites. Ages: ca1600Ma and 1600Ma (SHRIMP zircon for both). Older ages reported may have been based on results of probing xenocrysts rather than magmatic zircons.||||||07-FEB-11
33122|Cusin Creek Granite|64741|5|Briefly described|p313|||Age: 1596+/-3Ma U/Pb SHRIMP (Page et al. 2005). Geological province: Broken Hill Domain.||||||04-JUN-15
33122|Cusin Creek Granite|70657|5|Briefly described|p13 Fig.6|||Curnamona Province, Broken Hill Domain. Cusin Creek Granite and Purnamoota Road leucogneiss shown grouped together in Fig.6. Associated with Willyama Supergroup.||||May be equivalent to Purnamoota Road leucogneiss.|Granite.|
79634|Cuttaburra Granite|69511|6|Mentioned|p5|Late Silurian|Late Silurian|See references to "Cuttaburra granite" (p2, p34-39, p44, p48).||||||
79634|Cuttaburra Granite|70821|5|Briefly described|p9-10, p13 Tb.2.1|Ludlow|Wenlock||428.3 +/- 2.8 Ma (Chisholm et al., 2014).||||Includes granodiorite.|01-DEC-16
79634|Cuttaburra Granite|72915|6|Mentioned|p17|||[Formal or informal use is not explicit].||||||
27385|Cymbric Vale Formation|14019|5|Briefly described|p20|Early Cambrian|Early Cambrian|Geological Province: Gnalta Shelf.  Correlative of the Antrim Plateau Volcanics.||||||
27385|Cymbric Vale Formation|22671|3|Fully described|p835,838,846-48||Early Cambrian|Of the Gnalta Group. Felsic tuffs (pale green and grey, often colour-banded, rhyolitic vitric and vitric-crystal tuffs) and associated mainly pelitic sedimentary rocks. Overlain by Mootwingee Group rocks. Max Age: 525 (+/-) 8 Ma||||||18-JAN-06
27385|Cymbric Vale Formation|22857|5|Briefly described|p90 Fig. 14.7B, p94|Early Cambrian|Early Cambrian|Of the Gnalta Group. Age: ~526+/-4Ma and 525+/-8Ma (U/Pb SHRIMP, Zhou and Whitford, 1994). Max. thickness: 1900m. Geological Province: Mount Wright Block. See also p404 App. 1 Tb. A1.4.||||||
27385|Cymbric Vale Formation|22858|5|Briefly described|p94,97,Fig14.7bp90-1||Early Cambrian|Max Age: 525 (+/-) 8 Ma.||||||
27385|Cymbric Vale Formation|23469|5|Briefly described|Fig 8 p 322|||||||||
27385|Cymbric Vale Formation|23981|5|Briefly described|p61|Early Cambrian|Early Cambrian|Felsic tuffs have given an age of 525+/-8 Ma (U-Pb SHRIMP: Zhou and Whitford, 1994).  In NSW.||||||03-MAY-13
27385|Cymbric Vale Formation|29991|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
27385|Cymbric Vale Formation|30908|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Part of Gnalta Group.||||||
27385|Cymbric Vale Formation|31705|6|Mentioned|p27|||||||||
27385|Cymbric Vale Formation|32948|6|Mentioned|p110|||Re trilobites||||||22-JAN-21
27385|Cymbric Vale Formation|34469|6|Mentioned|p109|||Lower & Middle Cambrian. Table||||||
27385|Cymbric Vale Formation|35835|6|Mentioned|p209|||||||||
27385|Cymbric Vale Formation|38692|6|Mentioned|p139|||||||||
27385|Cymbric Vale Formation|39214|4|Described|p10|||||||||
27385|Cymbric Vale Formation|39885|6|Mentioned|p431|||||||||
27385|Cymbric Vale Formation|40455|6|Mentioned|Fig.2|||||||||
27385|Cymbric Vale Formation|40994|6|Mentioned|p236|||||||||
27385|Cymbric Vale Formation|41457|6|Mentioned|p10|||||||||
27385|Cymbric Vale Formation|41810|6|Mentioned|Fig.3|||||||||
27385|Cymbric Vale Formation|42206|5|Briefly described|p257|||See also Fig.1||||||
27385|Cymbric Vale Formation|42266|6|Mentioned|p292|||||||||
27385|Cymbric Vale Formation|42267|6|Mentioned|Fig.3 P312|||||||||
27385|Cymbric Vale Formation|42272|6|Mentioned|p413|||||||||
27385|Cymbric Vale Formation|42982|5|Briefly described|p333|||||||||
27385|Cymbric Vale Formation|42994|6|Mentioned|p4|||||||||
27385|Cymbric Vale Formation|43192|4|Described|p63|Early Cambrian|Early Cambrian|Of Gnalta Group.||||||12-FEB-07
27385|Cymbric Vale Formation|43501|14|Not recorded|Map Legend||Early Cambrian|(Provisional Edition) Part of Gnalta Group||||||03-MAY-13
27385|Cymbric Vale Formation|43502|14|Not recorded|Map Legend||Early Cambrian|(Provisional Edition) Part of Gnalta Group||||||
27385|Cymbric Vale Formation|43704|6|Mentioned|p67|||||||||
27385|Cymbric Vale Formation|43781|6|Mentioned|p3|||SHRIMP Zircon age: 525+/-8 Ma||||||
27385|Cymbric Vale Formation|44093|5|Briefly described|p108|Early Cambrian|Early Cambrian|Overlying Mount Wright Volcanics.  Age: 525+/-8Ma (U/Pb SHRIMP zircon, Zhou and Whitford, 1994). Geological Province: Tasman Fold Belt.||||||
27385|Cymbric Vale Formation|44133|5|Briefly described|p14, 31|||Maximum Thickness: 1900m.||||||
27385|Cymbric Vale Formation|45102|5|Briefly described|p5|||||||||
27385|Cymbric Vale Formation|60990|4|Described|p81-91        |Early Cambrian|Early Cambrian|Trilobite species described in detail, representing the first species-level correlation between the Early Cambrian of Australia and Antarctica (Shackleton Limestone). Biogeographic correlation with Koolywurtie Member, upper Ajax Limestone, and upper Wilkawillina Limestone, in SA. Up to 1900m thick. Age determinations by Zhou and Whitford (1994) and recalculated by Jenkins et al. (2002) respectively. Tuff age using the QGNG standard is 531.8 +/- 8 Ma (Jago and Haines 1998) which accords better with biostratigraphy.|525 +/- 8 Ma; 517.8 +/- 2.1 Ma.|Gnalta Group. ||Disconformably underlies the Coonigan Formation. Conformably overlies the Mount Wright Volcanics.|Interbedded blue, green and grey-white chert and green to brown tuff. Archaeocyath-bearing limestone lenses occur throughout. Lithic and feldspathic siltstone and sandstone, interbedded with impure iron-rich fossiliferous carbonate rocks, at top.|
27385|Cymbric Vale Formation|62785|6|Mentioned|p45|Early Cambrian|Early Cambrian|Contains trilobite species Estaingia, shown by Paterson (2005) to be conspecific with Pagetides (Discomesites) from Shackleton Limestone in Central Transantarctic Mountains, suggesting a continuous East Gondwanan margin carbonate-detrital shelf.||||||
27385|Cymbric Vale Formation|62787|5|Briefly described|p81|||Of Gnalta Group. Conformably underlain by Mount Wright Volcanics, unconformably overlain by Coonigan Formation.||||||03-MAY-13
27385|Cymbric Vale Formation|63489|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Rhyolite ash flow deposits, shale, porphyry.||||||
27385|Cymbric Vale Formation|63569|6|Mentioned|p122|Early Cambrian|Early Cambrian|Contains trilobite fauna of Pararaia janeae Zone.||||||
27385|Cymbric Vale Formation|63789|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group. Rhyolitic ashflow deposits, shale, feldspathic conglomeratic sandstones, minor limestones with Archaeocyathid fauna.||||||
27385|Cymbric Vale Formation|63793|5|Briefly described|pp22-23. |||At least 1372 m thick.|525 +/- 8 Ma (Zhou and Whitford 1994).|Middle unit in Gnalta Group.||Overlies Mount Wright Volcanics. Is overlain by Coonigan Formation.|Lithic and feldspathic sandstones, welded tuffs, cherts, siltstones and limestones.|
27385|Cymbric Vale Formation|64671|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Gnalta Group. Age is late Early Cambrian. Lithology includes rhyolitic ash flow deposits; shale, porphyry (may be a shallow intrusion); and a dacitic/rhyolitic dyke - latter intrudes Mount Arrowsmith Volcanics.||||||03-MAY-13
27385|Cymbric Vale Formation|64679|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Of the Gnalta Group. Rhyolite to dacite; shale; breccia; sandstone; minor limestone with archaeocyathid and trilobite fossils.||||||03-MAY-13
27385|Cymbric Vale Formation|64680|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group. Includes rhyolitic ashflow deposits and shale.||||||01-DEC-08
27385|Cymbric Vale Formation|65337|5|Briefly described|p95.|Early Cambrian|Early Cambrian|Gnalta Shelf. Correlative with Kalkarindji Volcanic Group.||Unit in Gnalta Group.||||
27385|Cymbric Vale Formation|65489|6|Mentioned|p119|||||||Correlated with Mooracoochie Volcanics (Warburton Basin).||
27385|Cymbric Vale Formation|65686|5|Briefly described|p420|Cambrian|Cambrian||U-Pb age from tuff: 525 +/- 8 Ma.|||||07-MAY-12
27385|Cymbric Vale Formation|65892|6|Mentioned|p23, p43. |Early Cambrian|Early Cambrian|Correlated with Shackleton Limestone in Central Transantarctic Mountains on basis of trilobite faunas. Contains 13 species of archaeocyatha common to Gnalta Group of western NSW and Ajax Limestone of SA.||||||
27385|Cymbric Vale Formation|66623|3|Fully described|pp56-63, pp430-431.|Early Cambrian|Early Cambrian|Defined by Warris (1967). Has same calc-alkaline chemistry and age as a felsic tuff in the Ponto Group. Contains barite with elevated Pb and Zn. Abundant archaeocyathids, trilobites and hyoliths in limestone lenses. About 1900 m thick.|510.4 +/- 3.1 Ma (Black 2007; Jagodzinski 2007).|Unit in Gnalta Group.||Faulted against underlying Mount Wright Volcanics. Is overlain disconformably by Coonigan Formation.|Pink to brown, medium to coarse-grained, poorly sorted feldspathic and lithic sandstone; interbeds of fossiliferous calcareous and cherty siltstone, blue-green chert, silicified sandstone; rhyolitic vitric tuffs; dacitic quartz-plagioclase porphyry.|
27385|Cymbric Vale Formation|66918|5|Briefly described|Map legend|Cambrian|Cambrian|Archaeocyathids occur in limestones.||Unit in Gnalta Group.||Overlies Mount Wright Volcanics. Is overlain by Coonigan Formation.|Rhyolitic ashflow deposits, feldspathic conglomeratic sandstones, minor limestones; quartz-plagioclase porphyry with quartz-rich groundmass. All regionally metamorphosed to prehnite-pumpellyite facies.|
27385|Cymbric Vale Formation|66929|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|||||Dyke intrudes Mount Arrowsmith Volcanics.|Shale; rhyolitic ashflow deposits; porphyry, may be a shallow intrusion; dacitic/rhyolitic dyke.|
27385|Cymbric Vale Formation|67105|5|Briefly described|p654- 655|Cambrian|Cambrian|Wonnaminta Zone (arc and forearc), Koonenberry Belt. Delamerian Orogeny Cycle deposits.|510.5 +/- 2.9 Ma (SHRIMP II zircon: Black, 2007)|Gnalta Group.||Overlies Mount Wright Volcanics.|Pyroclastic to tuffaceous rocks.|
27385|Cymbric Vale Formation|67322|3|Fully described|p5, p8, p10, p12; Fig.5|Stage 4|Stage 4|Of Warris (1967). Age from a tuffaceous bed; consistent with another of 510.3 +/- 3.2 Ma (Black, 2005) from slightly higher in this unit. Formation is between 1500-1900m thick. Trilobite-bearing mudstone pebbles, possibly eroded from this Formation, occur in the Bilpa Conglomerate. Occurs in the Mount Wright-Mutawintji region. |510.5+/-2.9Ma(SHRIMP II U-Pb zircon: Black, 2007)|Of the Gnalta Group.||Overlies Mount Wright Volcanics: faulted contact. Disconformably overlain by the Coonigan Formation.|Predominantly tuffs and cherts with limestone lenses occurring in the upper part of the formation. The uppermost beds comprise lithic and feldspathic sandstone with associated iron-rich carbonate.|21-FEB-18
27385|Cymbric Vale Formation|69043|5|Briefly described|p4, p100, p104|||Product of the subduction-related Mount Wright volcanic arc. Coeval eruptions occurred with the fore-arc Ponto Group to the E.|510.3 +/- 3.2 Ma (Black, 2005).|||Overlies Mount Wright Volcanics.||
27385|Cymbric Vale Formation|69445|5|Briefly described|p30:17|Early Cambrian|Early Cambrian|Gnalta Shelf, western NSW.||Gnalta Group.||Correlated with Kalkarindji Suite.||12-JUL-16
27385|Cymbric Vale Formation|69982|6|Mentioned|p15|Early Cambrian|Early Cambrian|A very thick volcanic unit. Same age as Mooracoochie Volcanics in SA.||||||
27385|Cymbric Vale Formation|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Koonenberry Belt.||Unit in Gnalta Group.||||
27385|Cymbric Vale Formation|70125|5|Briefly described|p400 Tb.5|||Kanmantoo Orogen.|525 Ma (Crawford et al., 1997).|||||
27385|Cymbric Vale Formation|70210|5|Briefly described|p1, p38|Middle Cambrian|Middle Cambrian|Koonenberry-Tibooburra district. Four felsic tuffs from this unit and Ponto Group have indistinguishable SHRIMP ages of c.511 Ma.||Gnalta Group.||||
27385|Cymbric Vale Formation|70296|5|Briefly described|p1-2, p21, p23-24|||Koonenberry District. Dated tuffs from Ponto Group correlated with dated tuff in Cymbric Vale Formation, suggesting both units saw the same volcanic event at ~511.1+/-1.7 Ma.|510.7+/-3.3 Ma (SHRIMP U-Pb)|Gnalta Group||||22-JAN-21
27385|Cymbric Vale Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|Appears to be shown as either a member of or partially equivalent to Mount Wright Volcanics.||Gnalta Group|||Non-outcropping rock fragments excavated from an old well consisting of fresh pink to brown feldspar-phyric rock with a eutaxitic texture; flow and fiamme textures suggest ignimbritic volcanic rock.
|
27385|Cymbric Vale Formation|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|||Gnalta Group|Includes un-named subunit.||Rhyolitic ashflow deposits, shale, feldspathic conglomeratic sandstone, minor limestone with archaeocyathid fauna. Un-named subunit: quartz-plagioclase porphyry with quartz-rich groundmass; dacitic composition with calc-alkaline geochemical affinity.|
27385|Cymbric Vale Formation|70749|5|Briefly described|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.|~510 Ma.|||||
27385|Cymbric Vale Formation|70838|5|Briefly described|p269|Cambrian|Cambrian|Koonenberry Belt. SHRIMP U-Pb zircon age from interbedded tuffaceous and pyroclastic rocks.|510.0 +/- 2.3 Ma (Black, 2005).|Gnalta Group.||Overlies Mount Wright Volcanics. Is overlain by Coonigan Formation.||
27385|Cymbric Vale Formation|71415|5|Briefly described|p15|Cambrian|Cambrian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Unit of the Mount Wright Arc.|c. 510 Ma|||||
27385|Cymbric Vale Formation|71966|6|Mentioned|p990|Series 2|Series 2|Geological province: southern Thomson Orogen.|c. 510 Ma|||||
27385|Cymbric Vale Formation|73177|5|Briefly described|p1114, 1115 Fig.17|Cambrian|Cambrian||525 +/- 8 Ma|Gnalta Group.||||31-AUG-22
82407|Daisy Plains Leucosyenogranite|71628|4|Described|p17: 1-2, 13-19, 21-27|||New name (this study). First published as Daisy Plains Leucoadamellite (Leitch et al., 1971). Subsequently Daisy Plains Leucogranite (Kinny et al., 1985) and Daisy Plains Leucomonzogranite (Chappell and Bryant, 1994 unpublished). First appears in this study as Daisy Plain Leucosyenogranite on p17-1. Named after the locality of that name. Occurs ~60 km NW of Kempsey. Crops out well as large boulders or smaller tors. Mineralogy, geochemistry described. Is spatially associated with alluvial Sn(Au) deposits.||Daisy Plains Suite.||Is enclosed by (?intrudes) Carrai Granodiorite.|Fine- to medium-grained, broadly equigranular, biotite leucosyenogranite with lesser leucomonzogranite. I-type.|
23530|Dalnit Bore Metasediments|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
23530|Dalnit Bore Metasediments|22575|6|Mentioned|p179 Fig.2|||Of the Paragon Group, Broken Hill Block.||||||11-JUN-08
23530|Dalnit Bore Metasediments|22771|5|Briefly described|Table12.2p45,47|||||||||
23530|Dalnit Bore Metasediments|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Max. thickness: 700m. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
23530|Dalnit Bore Metasediments|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Mt Isa Soldiers Cap Group and Georgetown (Qld) Langdon River Mudstone.||||||07-NOV-08
23530|Dalnit Bore Metasediments|22965|6|Mentioned|p14,Fig1||Statherian|||||||
23530|Dalnit Bore Metasediments|22967|6|Mentioned|p39||Statherian|||||||
23530|Dalnit Bore Metasediments|23248|5|Briefly described|Fig2p169|||||||||
23530|Dalnit Bore Metasediments|38969|4|Described|p211|||||||||
23530|Dalnit Bore Metasediments|39662|2|Defined|p438|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23530|Dalnit Bore Metasediments|40822|6|Mentioned|Fig.2|||||||||
23530|Dalnit Bore Metasediments|41093|6|Mentioned|p252|||||||||
23530|Dalnit Bore Metasediments|41145|6|Mentioned|Fig.4|||||||||
23530|Dalnit Bore Metasediments|41630|6|Mentioned|Fig.1.3|||||||||
23530|Dalnit Bore Metasediments|42261|6|Mentioned|Fig 1 P530|||||||||
23530|Dalnit Bore Metasediments|42537|6|Mentioned|p8|||||||||
23530|Dalnit Bore Metasediments|43052|6|Mentioned|Fig.4.22|||||||||
23530|Dalnit Bore Metasediments|43086|6|Mentioned|Fig.3|||||||||
23530|Dalnit Bore Metasediments|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
23530|Dalnit Bore Metasediments|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
23530|Dalnit Bore Metasediments|43572|6|Mentioned|Fig.3.2 p6|||||||||
23530|Dalnit Bore Metasediments|46598|5|Briefly described|p305|||||||||
23530|Dalnit Bore Metasediments|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Paragon Group (Willyama Supergroup). Underlain by Bijerkerno Metasediments.||||||31-MAY-07
23530|Dalnit Bore Metasediments|50606|6|Mentioned|p5.2|||Of the Paragon Group. Geological Province: Broken Hill Block.||||||
23530|Dalnit Bore Metasediments|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group (Willyama Supergroup). Geological Province: Broken Hill Block.||||||07-NOV-08
23530|Dalnit Bore Metasediments|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Of the Paragon Group. Age: <1642+/-5Ma. Geological Province: Broken Hill Domain.||||||28-APR-05
23530|Dalnit Bore Metasediments|61606|5|Briefly described|p4 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Paragon Group.||||||07-NOV-08
23530|Dalnit Bore Metasediments|61735|5|Briefly described|p635 Fig. 1, p639 Tb. 1|||Of Paragon Group. Depositional age: 1642+/-5 Ma U/Pb SHRIMP on tuffaceous sediment. Feldspathic tuffaceous sedimentary rocks. Presented as Dalnit Bore only in Fig. 2||||||04-JUN-15
23530|Dalnit Bore Metasediments|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Age: 1642+/-5Ma. Geological province: Broken Hill Domain.||||||
23530|Dalnit Bore Metasediments|62473|5|Briefly described|p74|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Age: 1642+/-5Ma. Geological province: Broken Hill Domain. Fine-grained, feldspathic beds interpreted as tuffaceous siltstones.||||||07-SEP-15
23530|Dalnit Bore Metasediments|62535|5|Briefly described|p666 Fig.3, p672, p674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1642 +/- 5 Ma.|Paragon Group.||||
23530|Dalnit Bore Metasediments|62536|5|Briefly described|p633, 636, 639, 641, 652-653, 659|||Broken Hill area. This MDA may also date deposition of the (partly air-fall) sediments.|1642 +/- 5 Ma (MDA).|Paragon Group.|||Tuffaceous metasiltstones, highly feldspathic psammopelitic bed. Greenschist facies metamorphism.|
23530|Dalnit Bore Metasediments|62592|5|Briefly described|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.|<1642 +/- 5 Ma.|Unit in Paragon Group.||||
23530|Dalnit Bore Metasediments|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1642 +/-5 Ma|Paragon Group||Overlies Bijerkerno Metasediments||15-DEC-21
23530|Dalnit Bore Metasediments|63102|5|Briefly described|p13-14,36||Neoproterozoic|Geological province: Broken Hill Domain, Curnamona Province.|<1642+\-5 Ma|Unit of Paragon Group.||Equivalent to Dayanna Formation.||
23530|Dalnit Bore Metasediments|63519|5|Briefly described|Abstract, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Topmost unit of the Paragon Group. Overlie Bijerkerno Metasediments gradationally. Age: <1642+/-5Ma (zircon). See also p10 Fig. 3.||||||07-NOV-08
23530|Dalnit Bore Metasediments|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province. Interpreted to have been deposited as deep water turbidites.||Paragon Group||Overlies the Bijerkerno Metasediments.|Laminated graphitic phyllite and rare graphitic psammite.|
23530|Dalnit Bore Metasediments|64097|5|Briefly described|p302 Tb. 1|Paleoproterozoic|Paleoproterozoic|Youngest unit in Paragon Group. Depositional age: 1642+/-5Ma (Page et al 2005a).||||||05-MAR-13
23530|Dalnit Bore Metasediments|64741|5|Briefly described|p301 Fig. 4, p311|Paleoproterozoic|Paleoproterozoic|Of the Paragon Group. Overlies Bijerkerno Metasediments. Age towards top: <1642+/-5Ma. Thickness: >700m. Geological province: Broken Hill Domain. Possible equivalent in Olary Domain is Dayana Formation.||||||07-FEB-11
23530|Dalnit Bore Metasediments|64742|6|Mentioned|p321 Fig.3. ||||<1642 Ma.|Unit in Paragon Group.|||Pelite.|
23530|Dalnit Bore Metasediments|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Paragon Group. Age in upper level: <1642+/-5Ma. Geological province: Broken Hill Domain. Equivalent of Dayana Formation in Olary Domain.||||||07-FEB-11
23530|Dalnit Bore Metasediments|66302|4|Described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. |1642 +/- 5 Ma |Paragon Group||Overlies the Bijerkerno Metasediments.|Laminated graphtitic phyllite and rare graphitic psammite.|
23530|Dalnit Bore Metasediments|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1642 +/- 5 Ma (maximum depositional age).|Paragon Group.||||
23530|Dalnit Bore Metasediments|70000|5|Briefly described|p34, p37|Statherian|Statherian|||Unit in Paragon Group.|||Thinly-bedded, graphitic, feldspathic psammite.|
23530|Dalnit Bore Metasediments|70014|5|Briefly described|Map legend|||Diagenetic, siliceous, gossanous pods locally abundant. Distinct and indistinct fine planar laminae, small-scale graded bedding, fading ripples, and crossbedding occur in phyllites.||Unit in Paragon Group.||Overlies Bijerkerno Metasediments.|Graphitic phyllite with rare lenticular psammite. Phyllite is pelitic to psammopelitic, spotted and minor non-spotted, grey to black, well-cleaved. Psammite is pale, feldspathic, graphitic, fine-grained.|
23530|Dalnit Bore Metasediments|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Paragon Group.||Overlies Bijerkerno Metasediments.|Graphitic, commonly spotted, pelitic to psammopelitic phyllite; rare lenticular, fine-grained graphitic feldspathic psammite; sporadic gossanous siliceous pods.|
23530|Dalnit Bore Metasediments|70405|6|Mentioned|p9 table 1,p32, p43 Table 3|||||||Correlates with Dayana Formation||
23530|Dalnit Bore Metasediments|70657|5|Briefly described|p13 Fig.6, p14-15, p43|||Curnamona Province; Broken Hill Domain.|<1642 +/- 5 Ma.|Paragon Group||Overlies Bijerkerno Metasediments. Equivalent to Dayana Formation (Olary Domain).||
23530|Dalnit Bore Metasediments|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|<1642 +/- 5 Ma.|Paragon Group.||||
23530|Dalnit Bore Metasediments|71968|4|Described|p18,28|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Page et al., (2005a) reported unimodal zircon population at 1642+\-5 Ma.||Unit of Paragon Group.||Underlain by Bijerkerno Metasediments and the Cartwrights Creek Metasediments.|Laminated graphitic phyllite and rare graphitic psammite.|06-DEC-19
23530|Dalnit Bore Metasediments|72461|5|Briefly described|p13, p16||||1642 +/- 5 Ma|Paragon Group||Overlies the Bijerkerno Metasediments.||
23530|Dalnit Bore Metasediments|73482|5|Briefly described|p422 Fig.3||Statherian||1642+/-5 Ma|Paragon Group||||
23530|Dalnit Bore Metasediments|73575|5|Briefly described|p828 Fig.2||Statherian||<1642+/-5 Ma|Paragon Group||Overlies Bijerkerno Metasediments||
31423|Dalrida Granite|24417|3|Fully described|p103|Emsian|Emsian|Intrudes Pullabooka Formation. Age: 395.4+/-1.7Ma. (SHRIMP U/Pb).||||||
31423|Dalrida Granite|24580|5|Briefly described|p828|Early Devonian|Early Devonian|Age: 395 +/- 1.7 Ma. Geological Province: Eastern Lachlan Fold Belt.||||||
31423|Dalrida Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|||||||13-JUL-04
31423|Dalrida Granite|60548|5|Briefly described|map legend|Devonian|Devonian|Muscovite-biotite granite.||||||
31423|Dalrida Granite|66197|5|Briefly described|p634, p635 Fig.5b|Eifelian|Eifelian|Jemalong Trough. Age: 395.4 +/- 1.7 Ma.||||||13-MAR-12
31423|Dalrida Granite|71040|6|Mentioned|p16|Devonian|Devonian|Currowong Syncline.||||||
28493|Dalwood Group|22601|6|Mentioned|409|Early Permian|Early Permian|||||||
28493|Dalwood Group|22610|5|Briefly described|p 123, Fig 1|||||||||
28493|Dalwood Group|22663|5|Briefly described|NSW97 - 1 p2||Early Permian|||||||
28493|Dalwood Group|22857|5|Briefly described|p522 App.1 Tb.A1.9|Early Permian|Early Permian|Max. thickness: 360m. Geological Province: Sydney Basin. Equivalent to Lochinvar and Allandale Formations. See also p536 App.1 Tb.A1.9.||||||
28493|Dalwood Group|22969|5|Briefly described|p 8||Permian|||||||
28493|Dalwood Group|23350|4|Described|263|Early Permian|Early Permian|See also p261 Fig. 2.||||||15-JUL-04
28493|Dalwood Group|23540|5|Briefly described|Fig 2 p 419|||Includes Rutherford and Farley Formations.||||||20-FEB-07
28493|Dalwood Group|24040|5|Briefly described|p469|Permian|Permian|Geological province: Cranky Corner Basin.  Lower section of group referred to as Lower Dalwood Group in Fig. 1, p468. Some former basalts of this group are now included in the Alum Mountains Volcanics.||||||21-AUG-08
28493|Dalwood Group|24079|5|Briefly described|p433 Fig.6|Permian|Permian|Geological Province: Sydney Basin.||||||
28493|Dalwood Group|24121|5|Briefly described|p4, p57, 136|Permian|Permian|||||||25-AUG-22
28493|Dalwood Group|24423|5|Briefly described|p230 Fig.3|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
28493|Dalwood Group|24547|6|Mentioned|p24|||Fossils indicate a broad correlation with some part of the Golden Valley Group.||||||10-MAY-04
28493|Dalwood Group|29437|6|Mentioned|p136|||Permian||||||
28493|Dalwood Group|29728|6|Mentioned|p394|||||||||
28493|Dalwood Group|29744|6|Mentioned|p5|||||||||
28493|Dalwood Group|29915|3|Fully described|p68|||||||||
28493|Dalwood Group|29922|6|Mentioned|Appendix 1|||||||||
28493|Dalwood Group|29944|6|Mentioned|Fig.18|||||||||
28493|Dalwood Group|30442|6|Mentioned|p24|||||||||
28493|Dalwood Group|30555|6|Mentioned|p296|||||||||
28493|Dalwood Group|30825|6|Mentioned|p40|||||||||
28493|Dalwood Group|31081|6|Mentioned|p51|||||||||
28493|Dalwood Group|31706|6|Mentioned|p671|||Correlation chart of the Gondwana System||||||
28493|Dalwood Group|31855|6|Mentioned|p14|||Stratigraphic table||||||
28493|Dalwood Group|31882|6|Mentioned|p243|||Refers Rattigan (1969)||||||
28493|Dalwood Group|31883|6|Mentioned|p593|||See also Table 1||||||
28493|Dalwood Group|31885|5|Briefly described|p1438|||Table 1||||||
28493|Dalwood Group|32094|6|Mentioned|p382|||||||||
28493|Dalwood Group|32266|6|Mentioned|p24|||||||||
28493|Dalwood Group|32324|6|Mentioned|Table 8.1|||||||||
28493|Dalwood Group|32379|6|Mentioned|p10|||||||||
28493|Dalwood Group|32671|6|Mentioned|Map legend|Permian|Permian|||||||
28493|Dalwood Group|32833|6|Mentioned|p108|||||||||
28493|Dalwood Group|32836|6|Mentioned|Table 1|||||||||
28493|Dalwood Group|32868|6|Mentioned|p208,Fig.7|||||||||
28493|Dalwood Group|32945|6|Mentioned|p74|||See also Fig.1 Permian||||||
28493|Dalwood Group|33129|6|Mentioned|Table 1|||Adapted from Packham (1969)||||||
28493|Dalwood Group|33132|6|Mentioned|Table 1|||||||||
28493|Dalwood Group|33584|6|Mentioned|p27|||O'lies Seaham Fm.||||||
28493|Dalwood Group|33685|6|Mentioned|Table 1|||Perm.||||||
28493|Dalwood Group|33711|6|Mentioned|Table 2|||||||||
28493|Dalwood Group|33867|4|Described|p3|||See also Fig.1||||||
28493|Dalwood Group|34015|6|Mentioned|p323|||Permian||||||
28493|Dalwood Group|34036|6|Mentioned|p434|||||||||
28493|Dalwood Group|34037|6|Mentioned|Table 5.27|||||||||
28493|Dalwood Group|34043|6|Mentioned|Table 5.32|||Perm. Correlation||||||
28493|Dalwood Group|34059|6|Mentioned|Map legend|Permian|Permian|||||||
28493|Dalwood Group|34084|6|Mentioned|p368|||Permian||||||
28493|Dalwood Group|34099|6|Mentioned|p17|||Perm.||||||
28493|Dalwood Group|34138|6|Mentioned|Cor.Chart|||Sakmarian - Artinskian||||||
28493|Dalwood Group|34170|6|Mentioned|p45|||Lower Permian||||||
28493|Dalwood Group|34171|6|Mentioned|p16|||||||||
28493|Dalwood Group|34237|6|Mentioned|p69|||||||||
28493|Dalwood Group|34238|6|Mentioned|p8|||||||||
28493|Dalwood Group|34239|6|Mentioned|p264|||||||||
28493|Dalwood Group|34292|6|Mentioned|p24|||See also P25. Carb.- Permian||||||
28493|Dalwood Group|34335|6|Mentioned|p369|||Permian||||||
28493|Dalwood Group|34345|6|Mentioned|p331|||||||||
28493|Dalwood Group|34399|6|Mentioned|p312|||||||||
28493|Dalwood Group|34400|5|Briefly described|p9|||Permian||||||
28493|Dalwood Group|34444|6|Mentioned|Map legend|Permian|Permian|||||||
28493|Dalwood Group|34445|3|Fully described|p319|||See also pp320-322.||||||21-AUG-08
28493|Dalwood Group|34446|6|Mentioned|p21|||||||||
28493|Dalwood Group|34447|6|Mentioned|Table 5.2|||||||||
28493|Dalwood Group|34448|6|Mentioned|p434|||||||||
28493|Dalwood Group|34466|6|Mentioned|Fig.5.22|||||||||
28493|Dalwood Group|34533|6|Mentioned|p1289|||||||||
28493|Dalwood Group|34570|6|Mentioned|p113|||||||||
28493|Dalwood Group|34692|5|Briefly described|p188|||||||||
28493|Dalwood Group|35284|6|Mentioned|Fig.12|||||||||
28493|Dalwood Group|35380|5|Briefly described|p191|||||||||
28493|Dalwood Group|35862|6|Mentioned|Fig.7|||||||||
28493|Dalwood Group|36042|6|Mentioned|Table 1|||||||||
28493|Dalwood Group|36045|6|Mentioned|p330|||||||||
28493|Dalwood Group|36069|6|Mentioned|p23|||||||||
28493|Dalwood Group|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
28493|Dalwood Group|36940|6|Mentioned|Table 2|||||||||
28493|Dalwood Group|37082|6|Mentioned|p160|||||||||
28493|Dalwood Group|37084|6|Mentioned|p176|||||||||
28493|Dalwood Group|37086|6|Mentioned|p182|||||||||
28493|Dalwood Group|37087|6|Mentioned|p192|||||||||
28493|Dalwood Group|37092|6|Mentioned|p229|||||||||
28493|Dalwood Group|37773|6|Mentioned|p18|||||||||
28493|Dalwood Group|37922|5|Briefly described|p481|||||||||
28493|Dalwood Group|37924|6|Mentioned|p488|||||||||
28493|Dalwood Group|38064|5|Briefly described|p41|||||||||
28493|Dalwood Group|38656|5|Briefly described|Table1.5.5|||P220||||||
28493|Dalwood Group|38837|6|Mentioned|p233|||||||||
28493|Dalwood Group|38917|6|Mentioned|p169|||||||||
28493|Dalwood Group|39287|6|Mentioned|p13|||See also Fig.2.5||||||
28493|Dalwood Group|39288|6|Mentioned|p57|||||||||
28493|Dalwood Group|39292|6|Mentioned|Fig. 6.1|||||||||
28493|Dalwood Group|39304|6|Mentioned|p361|||||||||
28493|Dalwood Group|39306|6|Mentioned|Fig. 21.2|||||||||
28493|Dalwood Group|39307|6|Mentioned|p437|||Permian foraminifera||||||
28493|Dalwood Group|39346|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
28493|Dalwood Group|40166|4|Described|p343|||||||||
28493|Dalwood Group|40222|6|Mentioned|Figure|||||||||
28493|Dalwood Group|40224|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
28493|Dalwood Group|40246|6|Mentioned|p173|||||||||
28493|Dalwood Group|40331|6|Mentioned|p3|||||||||
28493|Dalwood Group|40636|6|Mentioned|p43|||||||||
28493|Dalwood Group|40883|6|Mentioned|p8|||||||||
28493|Dalwood Group|41514|6|Mentioned|p81|||||||||
28493|Dalwood Group|41689|6|Mentioned|Table 1|||||||||
28493|Dalwood Group|41834|6|Mentioned|p590|||||||||
28493|Dalwood Group|41902|5|Briefly described|p5 Table 1|||||||||
28493|Dalwood Group|41903|6|Mentioned|Map legend|Early Permian||||||||
28493|Dalwood Group|41904|6|Mentioned|Map legend|||Age not stated on map||||||
28493|Dalwood Group|42000|6|Mentioned|p55|||||||||
28493|Dalwood Group|42182|6|Mentioned|Table 1|||||||||
28493|Dalwood Group|42214|6|Mentioned|p460|||||||||
28493|Dalwood Group|42648|6|Mentioned|p35|||||||||
28493|Dalwood Group|42780|5|Briefly described|p411, Fig.2 p412|||||||||
28493|Dalwood Group|42916|5|Briefly described|Table 1||Early Permian|||||||
28493|Dalwood Group|42925|5|Briefly described|Table 1||Early Permian|||||||
28493|Dalwood Group|43017|5|Briefly described|Fig.1,p372|||||||||
28493|Dalwood Group|43050|6|Mentioned|p12|||One of the locations for the fossil Earlandia condoni Crespin 1958. Geological province: Sydney Basin.||||||21-MAY-07
28493|Dalwood Group|43194|5|Briefly described|p128, p129 Tb. 8.3|Early Permian|Early Permian|Sydney Basin (Newcastle region). Contains Farley, Rutherford, Allandale and Lochinvar Formations. Upper part approximately time equivalent with Goonbri Formation.||||||
28493|Dalwood Group|43257|5|Briefly described|Map Legend||Early Permian|||||||
28493|Dalwood Group|43344|14|Not recorded|p11,18,19,78,79,88||Permian|||||||
28493|Dalwood Group|43383|14|Not recorded|p19-21,Fig.5||Permian|||||||
28493|Dalwood Group|43384|14|Not recorded|Map Legend|Early Permian||||||||
28493|Dalwood Group|43385|14|Not recorded|p178-180,167||Sakmarian|Newcastle SI65-2, Singleton SI56-1||||||
28493|Dalwood Group|43437|14|Not recorded|p169-175||Permian|||||||
28493|Dalwood Group|43440|14|Not recorded|p32,36,44,62-64,68,|||p82,91||||||
28493|Dalwood Group|43447|14|Not recorded|Tbl 1,p3,15,17,18,|||p48,49||||||
28493|Dalwood Group|43448|4|Described|p222-224,227,229,||Permian|Inc. Lochinvar, Allandale, Rutherford and Farley Formations. p233,235,236.||||||
28493|Dalwood Group|43450|14|Not recorded|p9,16,17|||||||||
28493|Dalwood Group|43451|14|Not recorded|Map Legend|||||||||
28493|Dalwood Group|43471|14|Not recorded|p235|||Megadesmus, Astartila||||||
28493|Dalwood Group|43477|14|Not recorded|p12,14-18,26,28-30,|||32-4,37-8,40-1,45,59,Pl.1,5||||||
28493|Dalwood Group|43479|14|Not recorded|p186,188-9,205,218-9||Permian|||||||
28493|Dalwood Group|43984|14|Not recorded|p135,138|||||||||
28493|Dalwood Group|44040|14|Not recorded|p23,26,27|||||||||
28493|Dalwood Group|44219|14|Not recorded|p35|||||||||
28493|Dalwood Group|44244|5|Briefly described|p231|Permian|Early Permian|||||||
28493|Dalwood Group|44253|14|Not recorded|p6|||(Balickera)||||||
28493|Dalwood Group|44254|14|Not recorded|p77||Permian|in Tb||||||
28493|Dalwood Group|44255|14|Not recorded|p119|||||||||
28493|Dalwood Group|44348|14|Not recorded|p56|||||||||
28493|Dalwood Group|44450|5|Briefly described|p147 Fig 43|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
28493|Dalwood Group|44489|14|Not recorded|p70|||||||||
28493|Dalwood Group|44859|14|Not recorded|p68,69|||Ref. to Fletcher 1958||||||
28493|Dalwood Group|44998|14|Not recorded|p104||Artinskian|basal Artinskian.||||||
28493|Dalwood Group|45016|14|Not recorded|p.72|||||||||
28493|Dalwood Group|45088|6|Mentioned|p59|||Equivalent||||||
28493|Dalwood Group|45090|6|Mentioned|p7|||Time correlation chart||||||
28493|Dalwood Group|46849|6|Mentioned|p195|||||||||
28493|Dalwood Group|48831|14|Not recorded|p.7,8,12,18,36,40-87|||||||||
28493|Dalwood Group|48841|14|Not recorded|p27|||Fauna related to lowest fauna of Middle Bowen Beds.||||||
28493|Dalwood Group|48926|6|Mentioned|p11|||P11 et seq.||||||
28493|Dalwood Group|48971|6|Mentioned|p9|||See also P11, P12, P18, P20.||||||
28493|Dalwood Group|50268|5|Briefly described|Map Legend|Artinskian|Asselian|Geological Province: Sydney Basin.  Underlies: Greta Coal Measures.||||||
28493|Dalwood Group|60281|5|Briefly described|p54|Early Permian|Early Permian|Subdivided into Lochinvar, Allandale, Rutherford and Farley Formations. Geological Province: Sydney Basin.||||||27-MAY-08
28493|Dalwood Group|60289|5|Briefly described|p1|Early Permian|Early Permian|Geological Province: Cranky Corner Basin.||||||22-FEB-05
28493|Dalwood Group|60290|4|Described|p15-16|Early Permian|Late Carboniferous|Overlies Paterson Volcanics. Overlain by Greta Coal Measures. Thickness: 308 m. Geological Province: Cranky Corner Basin. Proposed by Slee (1968) that this group be subdivided into Billy Brook Fm, Cranky Corner Sst, Branch Creek and Tamby Creek Fms.||||||07-FEB-11
28493|Dalwood Group|60291|4|Described|p51|Early Permain|Early Permain|Overlain by Greta Coal Measures. Marine shoreface to alluvial fan facies sediments. Geological Province: Cranky Corner Basin. Petrology described.||||||29-MAR-10
28493|Dalwood Group|60292|5|Briefly described|p65|Early Permian|Early Permian|Geological Province: Cranky Corner Basin.||||||
28493|Dalwood Group|60295|5|Briefly described|p127|Artinskian|Westphalian|Marine. Geological Province: Cranky Corner Basin.||||||
28493|Dalwood Group|60296|5|Briefly described|p155|||Marine. Geological Province: Cranky Corner Basin||||||
28493|Dalwood Group|60297|5|Briefly described|p167|Permian|Permian|Marine. Overlain by Greta Coal Measures. Geological Province: Cranky Corner Basin.||||||
28493|Dalwood Group|60298|6|Mentioned|p190|||||||||
28493|Dalwood Group|60300|5|Briefly described|p239|Early Permian|Late Carboniferous|Overlain by Greta Coal Measures. Marine. Geological Province: Cranky Corner Basin.||||||
28493|Dalwood Group|61315|5|Briefly described|p172, Table SY1|Early Permian|Early Permian|Includes Lochinvar, Allandale, Rutherford and Farley Formations in the Newcastle area and Gyarran Volcanics in the Hunter Valley area. Geological Province: Sydney Basin.||||||
28493|Dalwood Group|61529|5|Briefly described|p853, p854 Fig. 1b|Early Permian|Early Permian|Includes the Gyarran Volcanics. Overlain by Greta Coal Measures. Geological Province: Sydney Basin.||||||
28493|Dalwood Group|61768|6|Mentioned|p82|||Geological Province: Sydney Basin. Sedimentary and volcanic rocks.||||||13-MAY-08
28493|Dalwood Group|61772|6|Mentioned|p128 Fig. 1||Carboniferous|In New England Orogen.||||||24-SEP-08
28493|Dalwood Group|61791|6|Mentioned|p326 Fig. 2|Permian|Carboniferous|||||||
28493|Dalwood Group|63172|5|Briefly described|p301|||Contains Allandale and Rutherford Formations. In NSW.||||||07-FEB-11
28493|Dalwood Group|63832|5|Briefly described|p131 fig 2|Artinskian|Sakmarian|Cranky Corner/Gresford block, Southern New England Fold Belt; also NE Sydney Basin. Fifth (P1) and sixth (P2) glaciations.|||Includes Beckers Formation, Cranky Corner Sandstone and Billy Brook Formation (in NEFB); Lochinvar, Allandale, Rutherford, Farley Formations (SB).|||13-DEC-17
28493|Dalwood Group|64631|5|Briefly described|p44 Fig.2.|Artinskian|Asselian|Southern New England Fold Belt, Cranky Corner/Gresford Block; and Sydney Basin.  Biostratigraphic age control for base and top.|||In Cranky Corner/Gresford Block, includes Cranky Corner Sandstone, Beckers and Billy Brook Formations. In Sydney Basin, includes Lochinvar, Allandale and Rutherford Formations.|||
28493|Dalwood Group|65114|5|Briefly described|p383 Tb.1, p395|Cisuralian|Pennsylvanian|287-284 Ma (and 307-300 Ma?); of Cranky Corner Basin; below the Greta Coal Measures; abundant volcanic to volcaniclastic horizons; SHRIMP ages between 287 and 284 Ma; break of ~13 Ma between these rocks and underlying Late Carboniferous rocks (un-named)||||||
28493|Dalwood Group|67663|5|Briefly described|p518, p520 Tb.1, p529, p534|Permian|Permian|Early Permian.|||Includes Allendale and Lochinvar Formations.|Overlain by Greta Coal Measures. Overlies Seaham Formation and Kuttung Volcanics.|Basaltic and rhyolitic sequences.|
28493|Dalwood Group|67786|6|Mentioned|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||||Is overlain by Greta Coal Measures.||
28493|Dalwood Group|68003|5|Briefly described|p38 Fig.3-j, p40.|Early Permian|Early Permian|Hunter Coalfield, Brigalow Belt South Bioregion.|||Includes Gyarran Volcanics; Lochinvar, Allandale, Rutherford and Farley Formations.|Overlies Seaham Formation. Is overlain by Greta Coal Measures.||
28493|Dalwood Group|68004|5|Briefly described|p23 Table 1.|||Newcastle and Hunter Coalfields.|||Includes Lochinvar, Allandale, Rutherford and Farley Formations.|Overlies Seaham Formation. Is overlain by Greta Coal Measures.||
28493|Dalwood Group|68493|5|Briefly described|p1, p3 Fig.1, p5, p5 Fig.2, p6, p12, p13|Cisuralian|Cisuralian|Oldest Permian strata in the Hunter Valley. Includes locally derived volcanic debris.|298.7 Ma at base.||Includes Lochinvar Formation, Allandale Formation, Rutherford Formation, and Farley Formation.|Is overlain by Greta Coal Measures.|Marine sequence including locally derived volcanic debris.|
28493|Dalwood Group|68822|6|Mentioned|p321|Lower Permian|Lower Permian|||||||
28493|Dalwood Group|69297|6|Mentioned|p499, p501, p503|Kungurian|Sakmarian|Sydney Basin.|||Includes the Lochinvar Formation, Allandale Formation, Rutherford Formation and the Farley Formation.||Sandstones and marine siltstones.|
28493|Dalwood Group|69683|5|Briefly described|p410 Fig.1, p411 Fig.2, p420 Fig.5|Early Permian.|Early Permian.||||Includes Gyarran Volcanics.||Rhyolite, acid to basic volcanics, pyroclastics, sandstone, siltstone, basalt, marl.|
28493|Dalwood Group|70096|5|Briefly described|p220;Supp1,3|||Of northern Sydney Basin. Contains a thick vesicular basalt in the lower part of the section. See also supplementary files in appendix for additional stratigraphic and locality information.|||Includes Millifield Farm member, and Allandale, Rutherford and Farley formations.|||
28493|Dalwood Group|70791|5|Briefly described|p277, p292-293|Cisuralian|Cisuralian|Hunter Coalfield. The Boggabri Volcanics, Werrie Basalt and Goonbri Formation are assigned in this article to the Dalwood Group, "consistent with Hunter and Newcastle coalfield stratigraphy based on palynological ages and conformity relationships".|||Gyarran Volcanics.|||
28493|Dalwood Group|71233|6|Mentioned|p105|||||||Overlies the Kuttung Series.||
81945|Damnation Gully Gabbro|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|||Fine- to medium-grained, equigranular gabbro, outcrops are block and dark green-grey.|02-NOV-20
82125|Dandahra Creek Leucosyenogranite|71628|4|Described|p15: 5, 7; p17: 1-2, 4-7, 10, 12, 35|||See also p19-72. New name (this study). Originally Dandahra Creek Granite (Flinter et al., 1972); later Dandahra Creek Leucogranite (Barnes et al., 1991 after unpublished work by Willis, 1987). Named after a local watercourse. Comprises two masses, cut and displaced ~25-30 km by the Demon Fault (locations given). Characterised by strong NE-SW joint-controlled lineament pattern. Geochemistry described. Is associated with hard rock and alluvial Sn deposits (listed), various Ag, Pb, Zn, Cu, As deposits, and economically significant Mo-Bi-W-industrial silica deposits, and gems. RELATED UNITS (continued):  Is faulted against Dundee Rhyodacite and Grasstree Quartz Monzodiorite.|237.6 +/- 1.8 Ma (SHRIMP: Chisholm et al., 2014).|Dandahra Creek Suite.||Intrudes Cooramba, Cunglebung Creek beds; Gundahl Complex, Coombadjha Complex, Dundee Rhyodacite, Pheasant Creek Volcanics, Sandon Association, Billyrimba Leucomonzogranite. See COMMENTS for more.|Very coarse- to coarse-grained, equigranular, biotite leucosyenogranite. A-type.|
82125|Dandahra Creek Leucosyenogranite|72528|5|Briefly described|p110.|Ladinian|Ladinian||c. 238 Ma|Dandahra Creek Suite||||
80727|Dandahra Creek Suite|71628|4|Described|p17: 2, 4-13, 27, 72, 77, 86, 95, 100|||See also p19: 16, 73, 96. The author admits this is not a Suite 'in the strictest sense'. Appears as often as not as Dandahra Suite.|240-237 Ma (Chisholm et al., 2014, and others).|Coastal Granite Association.|Dandahra Creek Leucosyenogranite, Chaelundi Mountain Monzogranite, Mann River Leucogranite.|Intrudes Coffs Harbour Association sediments.|A-type.|
80727|Dandahra Creek Suite|72528|5|Briefly described|p2, p96, p110.|Ladinian|Ladinian|Age from Mann River Leoucogranite. Suite generally considered to be c. 238 Ma. Shown as part of the Coastal Granite Association. Shown as Dandahra Suite on p2.|239.1+/-1.2 Ma, c. 238 Ma.||Includes Mann River Leucogranite, Dandahra Creek Leucogranite and Chaelundi Mountain Monzogranite.|||
25714|Dangarfield Formation|22857|4|Described|p498 App.1 Tb.A1.7|Visean|Tournaisian|Includes the Brushy Hill, Wroxley Lithic Limestone and Macqueen Members. Disconformably overlain by Isismurra Formation. Max. thickness: 1020m. Thin-bedded brown to green lithic arenite, minor dark to light-grey oolitic or biogenic limestone. ||||||
25714|Dangarfield Formation|32529|3|Fully described|p198|||||||||
25714|Dangarfield Formation|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25714|Dangarfield Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25714|Dangarfield Formation|32866|6|Mentioned|p13|||Fossil content||||||
25714|Dangarfield Formation|32867|6|Mentioned|p30|||||||||
25714|Dangarfield Formation|32869|5|Briefly described|Fig.2|||Depositional environment. Equiv. Goonoo Goonoo Mudst. See Fig.3B||||||
25714|Dangarfield Formation|35245|1|Redefined|p21|Early Carboniferous|Early Carboniferous|||||||
25714|Dangarfield Formation|35879|6|Mentioned|p123|||||||||
25714|Dangarfield Formation|36057|6|Mentioned|p350|||||||||
25714|Dangarfield Formation|36390|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25714|Dangarfield Formation|36528|6|Mentioned|p175|||||||||
25714|Dangarfield Formation|39214|4|Described|p32|||Early Tournaisian||||||
25714|Dangarfield Formation|39979|6|Mentioned|p37|||||||||
25714|Dangarfield Formation|40883|6|Mentioned|p5|||||||||
25714|Dangarfield Formation|41279|6|Mentioned|p129|||||||||
25714|Dangarfield Formation|41542|3|Fully described|p234|||||||||
25714|Dangarfield Formation|42547|4|Described|p24|||||||||
25714|Dangarfield Formation|43576|6|Mentioned|Fig.1,p348|||||||||
25714|Dangarfield Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
25714|Dangarfield Formation|44093|5|Briefly described|p228 App. 1|Tournaisian|Late Devonian|Geological Province: New England Fold Belt.||||||
25714|Dangarfield Formation|44244|2|Defined|p22-23|Visean|Tournaisian|Includes the Macqueen, Wroxley Lithic Sandstone and the Brushy Hill Limestone Members. Conformably overlies the Kingsfield Formation; disconformably underlies Ayr Conglomerate Member.   Max. thickness: 1020m.  Geological Province: Rouchel Block.||||||
25714|Dangarfield Formation|45088|2|Defined|p20|Early Carboniferous|Early Carboniferous|See also Plate 2||||||
25714|Dangarfield Formation|45097|6|Mentioned|p15|||Previously Isismurra Fm. See also Correlation chart.||||||
25714|Dangarfield Formation|46803|6|Mentioned|p146|||Refers Roberts & Oversby (1974)||||||
25714|Dangarfield Formation|50268|5|Briefly described|Map Legend|Visean|Tournaisian|Overlies: Kingsfield Formation.  Underlies: Waverley Formation.  Geological Province: Rouchel Block.  Includes: Brushy Hill Limestone Member.||||||
25714|Dangarfield Formation|62095|5|Briefly described|p250|Early Carboniferous|Early Carboniferous|Includes Brushy Hill Limestone Member. Geological Province: Rouchel block/Tamworth Belt. See also Plate 1.||||||31-JAN-08
25714|Dangarfield Formation|63832|5|Briefly described|p131 fig 2|Tournaisian|Tournaisian|Rouchel block, Southern New England Fold Belt.|||||Coastal to nearshore marine sandstone dominated, contains little outsized gravel debris.|13-DEC-17
25714|Dangarfield Formation|64631|5|Briefly described|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Belt, Rouchel Block. Some biostratigraphic age control within unit. ||||Shown as laterally equivalent to Waverley Formation.|Includes oolitic limestone interval.|
25714|Dangarfield Formation|66498|6|Mentioned|p49|||Vertebrate fossils listed.||||||
25714|Dangarfield Formation|68003|5|Briefly described|p32 Fig.3-h. |Visean|Tournaisian|Tamworth Belt (South); New England Fold Belt.||||Overlies Kingsfield beds. Is overlain by Waverly and Isismurra Formations.||
25714|Dangarfield Formation|68297|5|Briefly described|p197|Tournasian|Tournasian|Includes shark faunas||||||
25714|Dangarfield Formation|70050|5|Briefly described|p361-362|Tournaisian|Tournaisian|Glenbawn Dam. Contains Pickettodendron (new genus) coral fossils (illustrations and systematic palaeontology), including the holotype of P. nudum.|||Brushy Hill Member.||Contains fossiliferous limestone beds.|
25714|Dangarfield Formation|70777|5|Briefly described|p8, p73, p83|Early Carboniferous|Early Carboniferous|Rouchel Block, New England Orogen. Age is derived from the presence of Late Tournaisian to Early Visean brachiopods, ammonoids and conodont fossils.||||Interfingers with the Waverley Formation.||
24240|Danswell Creek Granodiorite|23550|5|Briefly described|p504|||Subdivisions of the former Sapling Flat Igneous Complex.||||||
24240|Danswell Creek Granodiorite|36413|2|Defined|p100|Devonian|Devonian|||||||
24240|Danswell Creek Granodiorite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Sapling Flat Igneous Complex. Hornblende granodiorite. GSNSW map code: gsd.||||||
24240|Danswell Creek Granodiorite|39626|6|Mentioned|p275|||||||||
24240|Danswell Creek Granodiorite|39627|6|Mentioned|Table 1|||||||||
24240|Danswell Creek Granodiorite|40328|4|Described|p205|||Also mentioned on P210||||||
81955|Danu Rhyolite Member|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Macha Formation|||Porphyritic, flow-foliated rhyolite containing phenocrysts of anorthoclase, arfvedsonite, aegerine and quartz.|02-NOV-20
33453|Darbys Ridge Conglomerate|24417|3|Fully described|p78|Early Devonian|Early Devonian|Of the Yarra Yarra Creek Group. Previously referred to as "Darby Conglomerate Member" of the "Weelah Formation" by Kernezys (1976).  Overlies Ootha Group.  Max. thickness: 110m.||||||
33453|Darbys Ridge Conglomerate|60009|5|Briefly described|Map Legend|Pragian|Pragian|Of the Yarra Yarra Creek Group.||||||13-JUL-04
76032|Darcoola granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Baconian Swamp Granite Suite.|||Interpreted S-type granites.|
76032|Darcoola granite|70718|4|Described|p75, p126|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics.||Baconian Swamp granite suite|||S-type granitic rocks.|31-MAY-19
23533|Daroobalgie Volcanics|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
23533|Daroobalgie Volcanics|40891|2|Defined|p8|Late Ordovician|Late Ordovician|||||||
23533|Daroobalgie Volcanics|42489|5|Briefly described|Map legend|Bolindian||||||||
23533|Daroobalgie Volcanics|46522|2|Defined|p34|Late Ordovician||||||||
23533|Daroobalgie Volcanics|46524|4|Described|p103|||See also Appendix 1 P129||||||
23533|Daroobalgie Volcanics|46525|6|Mentioned|p165|||See also Fig.8||||||
23533|Daroobalgie Volcanics|46528|5|Briefly described|Map legend|Silurian||||||||
23533|Daroobalgie Volcanics|63278|6|Mentioned|p151|||||||||07-FEB-11
23533|Daroobalgie Volcanics|63283|5|Briefly described|p190|||Geological Province: Junee-Narromine Volcanic Belt. Clarke (1990) suggest that the volcanics are shoshonitic, and correlate with Goonumbla and Wombin Volcanics.||||||07-FEB-11
23533|Daroobalgie Volcanics|63289|6|Mentioned|p372|Late Ordovician|Late Ordovician|||||||07-FEB-11
23533|Daroobalgie Volcanics|67322|5|Briefly described|p20 Fig.5, p22|Ordovician|Ordovician|Macquarie Arc. Age is determined from p20 Fig.5 (Strat. column) - not well constrained. Has a shoshonitic signature comparable to Goonumbla Volcanics; implication is that this unit should not be merged with Parkes Volcanics. Occurs in the Junee-Narromine region.||Of the Northparkes Group.||||21-FEB-18
37914|Darthula Rhyodacite Member|24605|2|Defined|p931, p953 App.1|Namurian|Namurian|Of the Rocky Creek Conglomerate. Thickness in type locality: 50m. Geological Province: New England Orogen.||||||
37914|Darthula Rhyodacite Member|61214|5|Briefly described|p170, p171 Fig. 1|Namurian|Namurian|Of Rocky Creek Conglomerate. Geological Province: Darthula Block. See also p172 Fig. 2 (presented as only Darthula in text of figure).||||||
23537|Darts Creek Mudstone|22736|6|Mentioned|p629|Visean|Tournaisian|||||||
23537|Darts Creek Mudstone|22857|5|Briefly described|p500 App.1 Tb.A1.7|||Monotonous dark grey mudstone and interbedded siltstone. Max. thickness: 1100m. ||||||
23537|Darts Creek Mudstone|36057|2|Defined|p342|Devonian|Devonian|Prob. Devonian||||||
23537|Darts Creek Mudstone|36528|6|Mentioned|p175|||||||||
23537|Darts Creek Mudstone|39660|6|Mentioned|p449|||||||||
23537|Darts Creek Mudstone|40883|6|Mentioned|Fig.2|||||||||
23537|Darts Creek Mudstone|42547|4|Described|p33|Tournaisian|Late Devonian|||||||
23537|Darts Creek Mudstone|44093|5|Briefly described|p231 App. 1|Tournaisian|Late Devonian|Geological Province: New England Fold Belt.||||||
23537|Darts Creek Mudstone|44244|2|Defined|p196|Tournaisian|Late Devonian|Conformably overlies Wang Wauk beds.  Max. thickness: 1100m.  Geological Province: Myall Block.  Type section in text.||||||16-AUG-04
23537|Darts Creek Mudstone|47056|6|Mentioned|Fig.2 P523|||||||||
23537|Darts Creek Mudstone|50263|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Overlies: Wang Wauk beds.  Underlies: Wallanbah Formation.  Geological Province: Eastern Myall Block.||||||
23537|Darts Creek Mudstone|61766|4|Described|p68|Early Carboniferous|Late Devonian|Supersedes Darts Creek mudstone. Consists of monotonous succession of interbedded grey mudstone and siltstone. Conformably overlain by Wallanbah Formation. Conformably overlies Wang Wauk Formation. Geological Province: Tamworth Belt.||||||30-MAY-06
23537|Darts Creek Mudstone|63832|6|Mentioned|p131 Fig.2|||Eastern Myall block, Southern New England Fold Belt.||||||
23537|Darts Creek Mudstone|64631|6|Mentioned|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Belt, eastern Myall Block. Biostratigraphic age control for top.||||||
23537|Darts Creek Mudstone|69793|6|Mentioned|p1121 Fig.12|Tournaisian|Tournaisian|Myall Block, Tamworth Belt.||||||
35345|Dawsons Granite|50232|5|Briefly described|Map legend|Pragian|Lochkovian|Part of the Wologorong Batholith.  Grey muscovite, biotite soda granite.||||||
35345|Dawsons Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Parkesbourne Suite. White and cream to grey, leucocratic porphyritic biotite-muscovitegranite with quartz and feldspar phenocrysts, micaceous clots to up to 10mm and metsedimentary xenoliths up to 30mm, set in groundmass of 1mm crystals...||||||09-SEP-08
35345|Dawsons Granite|68592|3|Fully described|p1543, p1545-p6|Early Devonian|Early Devonian|New unit and name, after Dawsons Creek. Previously mapped as a satellite body of Wologorong Granite by Brunker and Offenberg (1970). Crops out as bold granite tors. Type area described. Geochemistry and geophysical properties described. Similar lithology, petrology and geochemistry to adjacent Wologorong Granite.||Unit in Parkesbourne Suite.||Intrudes Cuddyong Formation.|White and cream to grey, leucocratic, biotite-muscovite-bearing granite with quartz and feldspar phenocrysts, micaceous clots to 10mm and sedimentary xenoliths to 30mm. Unfractionated S-type.|
35345|Dawsons Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dpd. On Gunning 1:100 000 mapsheet portion of Time-Space Plot.||Parkesbourne Suite|||Leucocratic, porphyritic biotite-muscovite granite with quartz and feldspar phenocrysts. Micaceous clots  and metasedimentary xenoliths in a groundmass of crystals with local graphic textures. Low radioelement response and magnetic susceptibility.|
35345|Dawsons Granite|70541|4|Described|Map Legend|Devonian|Devonian|||Parkesbourne Suite|||Leucocratic, porphyritic biotite muscovite granite with quartz and feldspar phenocrysts, micaceous clots to 10mm and metasedimentary xenoliths to 30mm in a groundmass with local graphic textures; low radioelement response and magnetic susceptibility.|
35345|Dawsons Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Parkesbourne Suite|||Leucocratic, porphyritic biotite-muscovite granite with quartz and feldspar phenocrysts. Micaceous clots  and metasedimentary xenoliths in a groundmass of crystals with local graphic textures. Low radioelement response and magnetic susceptibility.|
27079|Daylesford Limestone|5250|5|Briefly described|p42, p45, p48, p53||Early Caradoc|Includes Bourimbla, Manooka and Gerybong Limestone Members (in ascending order). ||||||16-JAN-12
27079|Daylesford Limestone|13995|5|Briefly described|p68|Late Ordovician|Late Ordovician|Bowan Park, NSW. One unit in this formation has especially abundant receptaculitids.||||||
27079|Daylesford Limestone|23213|5|Briefly described|p22|||of Bowan Park Limestone Subgroup.||||||
27079|Daylesford Limestone|23214|2|Defined|p37|Eastonian|Eastonian|Of Bowan Park Limestone Subgroup.  Max. thickness 250m.||||||
27079|Daylesford Limestone|33063|1|Redefined|p79|Ordovician|Ordovician|Redefinition of Daylesford Fm. (Semeniuk, 1970)||||||
27079|Daylesford Limestone|33064|4|Described|p456|||P456-463 Sediment types & environmental interpretation||||||
27079|Daylesford Limestone|33065|5|Briefly described|p130|||See also P131. Biogenic structures||||||
27079|Daylesford Limestone|33737|6|Mentioned|p167|||||||||
27079|Daylesford Limestone|33740|6|Mentioned|Fig.1|||||||||
27079|Daylesford Limestone|35118|6|Mentioned|Fig.5|||||||||
27079|Daylesford Limestone|35646|6|Mentioned|Fig.5|||||||||
27079|Daylesford Limestone|38210|6|Mentioned|p185|||||||||
27079|Daylesford Limestone|38219|6|Mentioned|p315|||||||||
27079|Daylesford Limestone|40136|6|Mentioned|p23|||||||||
27079|Daylesford Limestone|42479|4|Described|p111|||||||||
27079|Daylesford Limestone|42603|6|Mentioned|p60|||Bowan Park succession.||||||
27079|Daylesford Limestone|60989|6|Mentioned|p114|Late Ordovician|Late Ordovician|Bowan Park. Shell beds contain trimerellide brachiopods.||||||
27079|Daylesford Limestone|61893|5|Briefly described|p249|Eastonian|Eastonian|W flank of Molong Volcanic Belt. Contains the coral Tetradium tenue, known elsewhere only from Jingerangle Formation.||Bowan Park Group.||||
27079|Daylesford Limestone|63278|4|Described|p153|||Overlain by Quondong Limestone. Includes; Ranch Member. Of the Bowan Park Limestone Subgroup. Geol Prov: Molong Volcanic Belt, LFB. Comprises coarse clastic to conglomerate facies containing volcaniclastic detritus.||||||07-FEB-11
27079|Daylesford Limestone|63287|5|Briefly described|p349, p333|Eastonian|Gisbornian|Of the Bowan Park Limestone Subgroup. Includes; Ranch Member. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
27079|Daylesford Limestone|63293|5|Briefly described|p470|||Of Bowan Park Subgroup. Includes; Ranch Member.||||||07-FEB-11
27079|Daylesford Limestone|67106|5|Briefly described|p677|||Molong Volcanic Belt.||Bowan Park Limestone Subgroup.|Ranch Member.|Overlies Cargo Volcanics.||
27079|Daylesford Limestone|67322|5|Briefly described|Fig.5; p23, p24|Katian|Katian|Described and subdivided into multiple members by Semeniuk (1970, 1973). Conodonts of early Eastonian age occur in this unit. Occurs in the Bowan Park region.||Of the Bowan Park Limestone Subgroup.||||21-FEB-18
27079|Daylesford Limestone|70684|5|Briefly described|p39-41|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian. Shelly faunas indicate water depth of c.30-50m.||Bowan Park Limestone Subgroup.|Ranch Member; Bourimbla, Manooka, Oakley, Gerybong, Glenrae, Davys Plains, Limestone Members.|Is overlain by Quondong Limestone.||
27079|Daylesford Limestone|70754|5|Briefly described|p450, p455|Late Ordovician|Late Ordovician|||Bowan Park Subgroup.|Ranch Member.|Correlated with Fossil Hill Limestone.||
27079|Daylesford Limestone|73209|6|Mentioned|p880 Fig.1, 885, 887|Late Ordovician|Late Ordovician|Bowan Park, Molong-Cudal area, central-west NSW.|||Bowan Park Limestone Subgroup|||
27079|Daylesford Limestone|73210|5|Briefly described|p891-893, 896-900, 902, 905|Late Ordovician|Late Ordovician|Bowan Park, NSW. Exhibits subaerial disconformities and diagenesis/pedogenesis. Microphotographs, stratigraphic columns.||Bowan Park Limestone Subgroup.|Ranch (?), Bourimbla, Manooka, Gerybong, Glenrae, Davys Plains Limestone Members.||Predominantly skeletal wackestone with lime mudstone as the pevasive matrix. The upper part is massively calcreted and pisolite- and lithoclast-dominated.|14-DEC-22
27079|Daylesford Limestone|73492|6|Mentioned|p696|||||Bowan Park Limestone Subgroup||||
79736|De Nardi granite|69511|5|Briefly described|28-33|Ludlow|Wenlock|Dated sample of unnamed granite at De Nardi Prospect from diamond drill core from hole CCR-144, 366.68 - 370 m.|427.2+/-3.1 Ma U/Pb SHRIMP mag cryst||||Partially carbonate- and sericite-altered, coarse-grained, leucocratic granite.|20-JAN-17
25874|Deakin Volcanics|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Of Red Hill Group. Rhyolite and tuff, tuffaceous and calcareous sandstone, tuffaceous shale, fossiliferous limestone. BMR map symbol: Sud.||||||
25874|Deakin Volcanics|13996|6|Mentioned|p148|||Tharwa area. Underlies a shale hosting acanthodian spines and associated scales.||||||
25874|Deakin Volcanics|22768|6|Mentioned|p176|||||||||
25874|Deakin Volcanics|22842|6|Mentioned|p30||Late Silurian|Syncronous with Lookdown Limestone.||||||26-FEB-10
25874|Deakin Volcanics|22857|4|Described|p176, p462 App.1 Tb.A1.6|Late Silurian|Late Silurian|Overlies the Yass Formation and the shelfal Yarralumla Formation in the Canberra area. Max. thickness: 1.5km. ||||||
25874|Deakin Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
25874|Deakin Volcanics|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25874|Deakin Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
25874|Deakin Volcanics|31111|6|Mentioned|p172|||Also mention on P174, 176, 178, 182, 186, 188.||||||
25874|Deakin Volcanics|31284|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25874|Deakin Volcanics|31852|6|Mentioned|p719|||See also Fig.5. Ludlovian||||||
25874|Deakin Volcanics|33325|5|Briefly described|Table 2|||See also Table 3.||||||
25874|Deakin Volcanics|33328|4|Described|Table 1|||See also PP5 & 14.||||||05-SEP-07
25874|Deakin Volcanics|34405|6|Mentioned|p119|||Table 3.5. Upper Silurian.||||||
25874|Deakin Volcanics|35110|6|Mentioned|Fig.3|||||||||
25874|Deakin Volcanics|35325|6|Mentioned|p483|||||||||
25874|Deakin Volcanics|35326|6|Mentioned|p485|||||||||
25874|Deakin Volcanics|35614|6|Mentioned|Fig.4|||||||||
25874|Deakin Volcanics|36633|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25874|Deakin Volcanics|37141|5|Briefly described|Plan 6|||||||||
25874|Deakin Volcanics|37348|6|Mentioned|p97|||See also P98.||||||
25874|Deakin Volcanics|37727|6|Mentioned|p27|||||||||
25874|Deakin Volcanics|37728|4|Described|Table 2|||||||||
25874|Deakin Volcanics|37752|6|Mentioned|Fig.2|||||||||
25874|Deakin Volcanics|38035|6|Mentioned|p91|||||||||
25874|Deakin Volcanics|38664|5|Briefly described|p14|||||||||
25874|Deakin Volcanics|39331|4|Described|p50|||||||||
25874|Deakin Volcanics|39975|4|Described|p123|||||||||
25874|Deakin Volcanics|40328|3|Fully described|p117|||||||||
25874|Deakin Volcanics|41356|5|Briefly described|p74|||||||||
25874|Deakin Volcanics|42497|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
25874|Deakin Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
25874|Deakin Volcanics|42727|5|Briefly described|map legend|Ludlow|Ludlow|Of Laidlaw Volcanic Suite. Includes Mugga Mugga Porphyry Member. Rhyodacitic ignimbrite and minor volcaniclastic and argillaceous sediments. Under Laidlaw Volcanics; faulted against Shannons Flat Adamellite. BMR map symbol: Sud. Geol. Prov: Canberra Block||||||
25874|Deakin Volcanics|42820|2|Defined|p31|early Ludlow||of Laidlaw Volcanic Suite. Age early Late Silurian (early Ludlow)||||||
25874|Deakin Volcanics|43159|4|Described|Fig.2p4,p6,p10||Late Silurian|of Laidlaw Suite.||||||
25874|Deakin Volcanics|43344|14|Not recorded|p110,113,115,116||Late Silurian|||||||
25874|Deakin Volcanics|43385|14|Not recorded|p172||Late Silurian|||||||
25874|Deakin Volcanics|43481|6|Mentioned|3,11|||||||||
25874|Deakin Volcanics|44852|14|Not recorded|p60||Silurian|||||||
25874|Deakin Volcanics|44970|2|Defined|p1,11,33-5,42-6,48-9||Late Silurian|p69,71,73,76,89,95,map. Unit of Red Hill Group. See also Lexicon||||||
25874|Deakin Volcanics|45147|6|Mentioned|M149|||||||||
25874|Deakin Volcanics|49690|5|Briefly described|p1-2, p12-14, p16-19, p22, p27, Tb.11|Late Silurian|Late Silurian|Of Opik (1958).||||Faulted against Colinton Volcanics. Conformably overlain by the Laidlaw Volcanics.|Rhyolitic to dacitic composition. Minor sedimentary interbeds in volcanics units. Lower part is both rhyolitic and dacitic, upper is only rhyolitic.|14-FEB-14
25874|Deakin Volcanics|68592|6|Mentioned|p428, p443, p522|Silurian|Silurian|Opik (1958). Equivalent to, but not yet formally included in, the Douro Group.||||||
38304|Deards seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
73365|Dederang Siltstone Member|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Meryula Formation.||Overlies ?conformably Drouin Conglomerate Member.|Buff to red, quartzose, micaceous, fine-grained sandstone and siltstone (locally ferruginised); strongly cleaved.|
73365|Dederang Siltstone Member|69095|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Meryula Formation.||Overlies ?conformably Drouin Conglomerate Member.|Buff to red, quartzose, micaceous, fine-grained sandstone and siltstone (locally ferruginised); strongly cleaved, contains macrofossils locally.|
73365|Dederang Siltstone Member|70941|3|Fully described|pviii, px, p7 fig 3, p8 fig 4, p76|Early Devonian|Pridoli|Named for Dederang parish. Rocks of this member were previously assigned to the Kopyje Beds and the undifferentiated Meryula Formation. Shallow marine depositional environment. Contains late Silurian brachiopods. Recessive and outcrops poorly. No type section available but a type area is proposed. Total thickness unknown but estimated as no greater than 1000m. Deposited in a shallow marine, low energy environment. Structure, metamorphism, fossil assemblage, geophysical and distinguishing characteristics discussed.  Age derived from fossil assemblage. Minor gold and base metal mineralisation is associated with this unit. The most prominent mineralisations are the Four Ms and North pole prospects.  See also p77,  p78 fig 32, p79, p80, p85-p88, p90, p93, p110, p111, p140 fig 58, p147.||Meryula Formation||Conformably overlies Drouin Conglomerate Member. Faulted against or unconformably overlies the Girilambone Group.|Pale yellow to red and purple massive cleaved to slaty cleaved sandy siltstone and angular, very fine-grained sandstone. Bedding is poorly defined.|
73365|Dederang Siltstone Member|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Meryula Formation.||||
80703|Deepwater Syenogranite|71628|4|Described|p14: 7, 10-11; p15: 2, 12-15|||New name; for the northern-most body of Kingsgate Leucogranite of Henley et al. (2001). Occurs ~3 km E of Deepwater. Named after the Parish of Deepwater. Crops out as large tors, minor whalebacks and rock platforms. Geochemistry described. Associated with historically significant Mo-W-Bi mineralisation (5 types of deposits are named with prospects/deposits listed for each).|~256 Ma (Waltenberg and Blevin (pers. comm. 2017).|Bolivia Range Suite.||Intrudes Coffs Harbour Association and Emmaville Volcanics.|Coarse-grained, biotite leucosyenogranite to K-feldspar-rich leucomonzogranite. I-type.|
80703|Deepwater Syenogranite|72528|5|Briefly described|p2, p4 Tb.1.2, p71-76, p109, p127.|Lopingian|Lopingian|Magmatic crystallisation age determined. Rocks previously included in Kingsgate Syenogranite. Coeval with Arranmor Ignimbrite Member (Emmaville Volcanics), occuring 40km north of Glen Innes. Includes Mo-Sn-W-Bi mineralisation. The unit is very well exposed in this area, mainly as extensive pavements, domes, and numerous boulders. Shown as part of the New England Orogen.|256.1+/-1.3 Ma U238/Pb206 (Pb207-corrected)|Stanthorpe Supersuite||Time equivalent to and intrudes Arranmor Ignimbrite Member. Emmaville Volcanics forms roof pendant. Shares boundaries with Wards Mistake Monzogranite.|Dated sample is pink, medium to coarse-grained, slightly porphyritic, leucocratic biotite syenogranite.|01-FEB-21
77005|Delegate Monzogranite|72571|5|Briefly described|p90-91, p96-99, p101|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail. I-type.|||||Felsic biotite granite with magnetite and a porphyritic texture dominated by plagioclase and quartz.|
31500|Delegate Suite|22815|5|Briefly described|p53,59|Silurian|Silurian|||||||
31500|Delegate Suite|42726|5|Briefly described|map legend||Silurian|||||||
31500|Delegate Suite|43233|5|Briefly described|Map Legend|Late Silurian||Berridale Batholith||||||
31500|Delegate Suite|44093|5|Briefly described|p191 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
31500|Delegate Suite|72571|6|Mentioned|p90|||Of the Tasmanides of eastern Australia.||||||
31499|Delegate Supersuite|42726|5|Briefly described|map legend|||||||||
36826|Dellwood Ignimbrite Member|23859|2|Defined|p942 Appendix 1|Late Permian|Permian|See also page 932. Type locality 399000E, 6746000N. Of Emmaville Volcanics. Geological Province: New England Fold Belt. Max. thickness: ~1200 m.||||||
36826|Dellwood Ignimbrite Member|70876|6|Mentioned|p82|Late Permian|Late Permian|Provided age is a SHRIMP U-Pb zircon date.|254.8 +/- 1.5 Ma (Black, 2006)|Emmaville Volcanics||||
69824|Delungra Volcanic Suite|63347|2|Defined|p5 Fig. 2, p28|Early Miocene|Late Oligocene|Includes Inverell, Mount Russell, Bingara and Derra Derra Volcanics. Age: 24-19Ma (K-Ar). Lithologies include mafic flows, intrusions and volcaniclastic rocks of theoleiitic and alkaline composition. See also p6, p12, p19, p22.||||||
69824|Delungra Volcanic Suite|73581|5|Briefly described|p10, p14-15, p30|Miocene|Miocene|Described by Vickery et al., (2007). Defined based on petrographic, geochemical and geochronological data. Plume-like geochemical signature.|21.3 Ma+/-0.4 Ma Ar-Ar, 23-19 Ma||Mount Russell Volcanics||Basalt lavas.|
25877|Denman Formation|22578|6|Mentioned|p391|||||||||
25877|Denman Formation|22607|6|Mentioned|p 57|||||||||
25877|Denman Formation|22857|4|Described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Included in both the Wittingham Coal Measures (Singleton Supergroup) and Charbon Subgroup (Illawarra Coal Measures). Contains the Bungaba coal seam. Max. thickness: 30m. In the Illawarra region. Geol. Province: Sydney Basin. See also p528 App.1 Tb.A1.9.||||||
25877|Denman Formation|22969|4|Described|Fig 4.1a||Late Permian|Of the Jerrys Plain Subgroup.||||||14-MAR-07
25877|Denman Formation|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Geological Province: Sydney Basin.||||||25-SEP-08
25877|Denman Formation|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Of the Wittingham Coal Measures. Geological Province: Sydney Basin||||||14-MAR-07
25877|Denman Formation|29942|3|Fully described|p11|||||||||
25877|Denman Formation|29944|6|Mentioned|Fig.18|||||||||
25877|Denman Formation|31375|6|Mentioned|p3|||Stratigraphy||||||
25877|Denman Formation|33334|6|Mentioned|p8|||Perm.||||||
25877|Denman Formation|36042|6|Mentioned|Fig.19|||||||||
25877|Denman Formation|36604|6|Mentioned|Fig.9|||||||||
25877|Denman Formation|37087|5|Briefly described|p198|||||||||
25877|Denman Formation|38603|5|Briefly described|p80|||||||||
25877|Denman Formation|38614|6|Mentioned|p14|||||||||
25877|Denman Formation|38656|6|Mentioned|Fig.1.5.14|||P281||||||
25877|Denman Formation|39232|6|Mentioned|p105|||See also P110||||||
25877|Denman Formation|39287|6|Mentioned|Fig. 2.15|||||||||
25877|Denman Formation|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
25877|Denman Formation|39666|6|Mentioned|p66|||||||||
25877|Denman Formation|39693|6|Mentioned|p17|||||||||
25877|Denman Formation|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
25877|Denman Formation|40166|6|Mentioned|p347|||See also Table 1||||||
25877|Denman Formation|40256|6|Mentioned|p304|||||||||
25877|Denman Formation|40321|6|Mentioned|p19|||||||||
25877|Denman Formation|40805|2|Defined|p142|Permian|Permian|||||||
25877|Denman Formation|41010|4|Described|p13|||||||||
25877|Denman Formation|41054|6|Mentioned|p156|||||||||
25877|Denman Formation|41604|6|Mentioned|Table 1|||||||||
25877|Denman Formation|41902|6|Mentioned|p3|||||||||
25877|Denman Formation|42078|6|Mentioned|Table 1 P5|||||||||
25877|Denman Formation|42657|5|Briefly described|p81|||||||||
25877|Denman Formation|42916|5|Briefly described|Table 1||Late Permian|||||||
25877|Denman Formation|43017|5|Briefly described|Fig.1,p372|||||||||
25877|Denman Formation|43194|5|Briefly described|p112, p129 Tb. 8.3, p130|Late Permian|Late Permian|Uppermost unit of Tomago Coal Measures, Newcastle Coalfield, Sydney Basin. Correlates with an organic-rich mudstone unit (now part of Clare Sandstone) in the upper part of the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
25877|Denman Formation|43257|5|Briefly described|Map Legend||Late Permian|Of Wittingham Coal Measures.||||||
25877|Denman Formation|45090|4|Described|p63|||Age, correlation, lithology, relationships.||||||
25877|Denman Formation|60281|6|Mentioned|p61|Late Permian|Late Permian|||||||
25877|Denman Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wittingham Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
25877|Denman Formation|61529|5|Briefly described|p854 Fig. 1b|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||
25877|Denman Formation|61612|6|Mentioned|p274, p277, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||17-MAR-09
25877|Denman Formation|61770|6|Mentioned|p110|||||||||
25877|Denman Formation|62033|5|Briefly described|p25 (Table)|||Of the Wittingham Coal Measures. Overlain by Lambton Formation.  Geological Province: Sydney Basin.||||||14-MAR-07
25877|Denman Formation|66891|6|Mentioned|p179. |Middle Permian|Middle Permian|Marine.||||||
25877|Denman Formation|67663|6|Mentioned|p520|Permian|Permian|Late Permian. Age defined by that of the parent Singleton Supergroup.||Of the Singleton Supergroup.||||
25877|Denman Formation|68003|5|Briefly described|p38 Fig.3-j, p41, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion. Mis-spelt as Denham Formation on p130.||Unit in Wittingham Coal Measures.||Overlies Jerrys Plains Subgroup. Is overlain by Watts Sandstone.|Includes sandstone siltstone laminite.|
25877|Denman Formation|68004|5|Briefly described|p23 Table 1, p51 Table 5.|Late Permian|Late Permian|Hunter and Western Coalfields. Equivalent to Dempsey Formation in the Newcastle Coalfield.||Upper unit in Wittingham Coal Measures.||Overlies Jerrys Plains Subgroup. Is overlain by Watts Sandstone.|Dark grey striped sandstone-siltstone laminite with abundant burrows.|
25877|Denman Formation|69297|6|Mentioned|p503|Upper Permian|Upper Permian|Sydney Basin. Has good oil and gas source rock potential.||||||
25877|Denman Formation|69683|6|Mentioned|p411 Fig.2, p415-417 Figs.3-4|Late Permian|Late Permian|||Unit in Wittingham Coal Measures.||||
25877|Denman Formation|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield.||Wittingham Coal Measures.||||
25877|Denman Formation|73304|6|Mentioned|p75|||||Whittingham Coal Measures, Singleton Supergroup||||
25877|Denman Formation|73625|6|Mentioned|p2|Permian|Permian|Hunter coalfield, Sydney Basin.||||Overlies Wittingham Coal Measures. Is overlain by Watts Sandstone.||
76024|Depot Glen Formation|66623|2|Defined|p31, p37, pp45-47. |Cambrian|Cambrian|See Depot Glen beds for naming history. Possible northern equivalent of Bunker Creek Formation, exposed over 50 km2. Likely thickness of 10 km. Unfossiliferous. Placer gold in (vein-)quartz scree.|504.5 +/- 2.6 Ma (Black 2006).|Unit in Teltawongee Group.||Intruded by Evelyn Creek volcanics. Is adjacent to Jeffreys Flat Formation. Is unconformably overlain by Namur Sandstone.|Strongly cleaved phyllite; interbedded siltstone and subarkose sandstone (containing detrital muscovite); regionally metamorphosed to greenschist facies; felsic tuffaceous mudstone.|04-NOV-13
76024|Depot Glen Formation|66921|5|Briefly described|Map legend|||Does not outcrop in map area. Position in cross-section is based on geological interpretation and geophysical modelling.||Unit in Teltawongee Group.|||Strongly-cleaved metamudstone (phyllite); interbedded metasiltstone and subarkose sandstone (containing detrital muscovite); regionally metamorphosed to greenschist facies.|
76024|Depot Glen Formation|66922|5|Briefly described|Map legend|Cambrian|Cambrian|Five un-named sub-units are mapped separately.||Unit in Teltawongee Group.|||Strongly-cleaved meta-mudstone (phyllite); interbedded meta-siltstone and subarkose sandstone (containing detrital muscovite); regionally metamorphosed to greenschist facies.|
76024|Depot Glen Formation|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Broad zone of low magnetic intensity containing numerous sub-parallel trends of moderate magnetic intensity; numerous fractures are indicated by narrow magnetic-destructive linear trends.||||Is overlain by Wonnaminta Formation.|Phyllite.|
76024|Depot Glen Formation|67105|5|Briefly described|p655, 659|Cambrian|Cambrian|Occurs E of the Koonenberry Fault.|504.5 +/- 2.6 Ma.|Teltawongee Group.|||Includes a laminated felsic tuffaceous bed (whence the age determination).|
76024|Depot Glen Formation|67207|5|Briefly described|Map legend.|Cambrian|Cambrian|Has five un-named sub-units of varying lithologies mapped separately.||Unit in Teltawongee Group.|||Strongly cleaved metamudstone (phyllite); interbedded metasiltstone and quartzo-feldspathic metasandstone (containing detrital muscovite); local slate, quartz arenite, tuffaceous metamudstone; regionally metamorphosed to greenschist facies.|
76024|Depot Glen Formation|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Strongly cleaved metamudstone (phyllite), interbedded metasiltstone and quartzo-feldspathic metasandstone (containing detrital muscovite).|
76024|Depot Glen Formation|67209|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Strongly cleaved metamudstone (phyllite), interbedded siltstone and quartzo-feldspathic metasandstone (containing detrital muscovite); regionally metamorphosed to greenschist facies.|
76024|Depot Glen Formation|67322|5|Briefly described|p10, p13; Fig.5|Cambrian Series 3|Cambrian Series 3|Defined by Mills in Greenfield et al., (2010). Age from a felsic tuff member. Occurs in the Kayrunnera-Koonenberry region.|504.5 +/- 2.6 Ma (U-Pb SHRIMP: Black, 2006).|Of the Teltawongee Group.|||Includes felsic tuff.|23-DEC-21
76024|Depot Glen Formation|69001|5|Briefly described|p2 Fig.1B, p12, p59|Drumian|Stage 5|Age derived from a felsic tuff in the formation. Occurs along the eastern margin of the Mount Poole Inlier.|504.5 +/- 2.6 Ma (Black 2006)|Of the Teltawongee Group.|||Comprises a turbidite sequence metamorphosed from low greenschist up to mid-greenschist facies.|
76024|Depot Glen Formation|69043|5|Briefly described|p4, p101, p104|||NE of the Koonenberry Fault. Age from a laminated tuff.|504.6 +/- 2.6 Ma (Greenfield et al., 2011).|Teltawongee Group.||||
76024|Depot Glen Formation|69961|5|Briefly described|Map legend|Cambrian|Cambrian|No outcrop in map area.||Unit in Teltawongee Group.|||Strongly cleaved metamudstone (phyllite); interbedded metasiltstone and quartzo-feldspathic metasandstone (containing detrital muscovite).|
76024|Depot Glen Formation|70749|5|Briefly described|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.|504.5 +/- 2.6 Ma.|||||
76024|Depot Glen Formation|70838|5|Briefly described|p268-269|Cambrian|Cambrian|SE Koonenberry Belt. Also appears as Deport Glen Formation on p268. Age from interlayered tuffs.|504.5 +/- 3.2 Ma (Black, 2007).|Teltawongee Group.|||Characterised by repetitive sequences of immature sandstone (up to 3m thick locally) overlain by an upward-fining sequence (locally absent) of fine sandstone, siltstone and mudstone. Ubiquitous large (<5mm) detrital white mica grains.|
76024|Depot Glen Formation|71262|6|Mentioned|p9 Fig 6|Cambrian|Cambrian|Age inferred from parent Group.||Unit of Teltawongee Group||||
76024|Depot Glen Formation|71966|6|Mentioned|p990|Late Cambrian|Late Cambrian|Geological province: southern Thomson Orogen.|504.5+\-2.6 Ma|||||
76024|Depot Glen Formation|72522|4|Described|p3, p120-121, p125-130.|Cambrian|Ediacaran|Koonenberry Belt. U-Pb SHRIMP maximum depositional age determined. Laminated tuffaceous bed near top of unit previously dated as 504.5 +/- 2.6 Ma (Black, 2006). Located in the Mount Poole inlier.|566 +/- 7 Ma  206Pb/238U (204Pb-corrected)|Teltawongee Group|||Predominantly metasiltstone and metasandstone with laminated felsic tuffaceous bed near the top of the formation.|
26517|Dering Siltstone|22772|4|Described|p67,Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
26517|Dering Siltstone|22857|5|Briefly described|Tb 13.1 (insert p70), p400 App. Tb A1.3|Marinoan|Marinoan|Of the Teamsters Creek Subgroup (Torrowangee Group). Finely laminated and well-bedded siltstone. Age: ~593+/-32Ma. Max. thickness: 200m. Geological Province: Adelaide Fold Belt. See also p67.||||||
26517|Dering Siltstone|30261|4|Described|Table 1|||Marinoan age||||||
26517|Dering Siltstone|34812|3|Fully described|p90|||||||||
26517|Dering Siltstone|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26517|Dering Siltstone|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
26517|Dering Siltstone|36733|6|Mentioned|Table 5|||||||||
26517|Dering Siltstone|38157|6|Mentioned|p265|||||||||
26517|Dering Siltstone|39214|6|Mentioned|p7|||Deltaic||||||
26517|Dering Siltstone|46889|6|Mentioned|p272|||||||||
26517|Dering Siltstone|68241|6|Mentioned|p21, p24 Fig.3, p32, p33 Fig.3|||Lithology described by Tuckwell (1981). Contains some dropstones.||||Underlain by the Elatina Formation. Overlain by the Nunduro Conglomerate.|Comprises dark grey laminated diamictite with interbedded thin (1m) gravel and boulder beds, and pebbly siltstone, siltstone and slump breccias with a high clast to matrix ratio.|26-MAY-17
26517|Dering Siltstone|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Teamsters Creek Subgroup.||||
26517|Dering Siltstone|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Teamsters Creek Subgroup.||Overlies Alberta Conglomerate and Gairdners Creek Quartzite. Is overlain by Nunduro Conglomerate.|Finely-laminated and well-bedded rippled siltstone to sandstone.|
69826|Derra Derra Volcanics|63347|2|Defined|p5 Fig. 2, p29|Early Miocene|Late Oligocene|Of the Delungra Volcanic Suite. Unconformable over Parry Group; interfingers with Bingara Volcanics. Age: 23Ma(K-Ar). , and 28Ma (unpub.). Max. thick: 150m in west. Quartz- and olivine-bearing tholeiitic basalt + diamond-bearing gravels. See also p7, p12.||||||10-DEC-07
69826|Derra Derra Volcanics|73581|5|Briefly described|p14-15|Miocene|Oligocene|Up to 20 m thick lavas. Interbedded with diamond-bearing non-volcanogenic sediments.|27.3+/-0.6 Ma, 22.6+/-0.5 Ma K-Ar|||Interbedded with Bingara Volcanics|Quartz- and olivine-bearing tholeiite.|
74616|Derrida Phase|61964|4|Described|p37, p40,47, p49-50, p238 Fig. 78|||Informal name. Describes a part of the Ungarie Granite formerly mapped separately as "Derrida Granite" (Chappell et al, 1991) - with different chemical properties and enhanced prospectivity compared with the rest of Ungarie Granite. On NYMAGEE sheet.||||||20-OCT-08
74616|Derrida Phase|70751|6|Mentioned|p4, p5, p15|||Previously Derrida Granite, now considered part of Ungarie Granite.|426.3 +/- 3.3 Ma (SHRIMP).|||||24-SEP-19
34256|Devils Pulpit Member|22678|3|Fully described|p717-18,724|Early Devonian|Early Devonian|Of Tangerang Formation.  Thick, extensive shallow-marine volcaniclastic deposits.||||||17-JAN-06
34256|Devils Pulpit Member|50234|5|Briefly described|Map Legend|Pragian|Lochkovian|Of the Tangerang Formation (Bindook Volcanic Complex).||||||
34256|Devils Pulpit Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tangerang Fm (Bindook Gp). Massive, thick-bedded, occasionally graded, rhyolitic polymictic volcanic breccia + rare fossil fragments, intercalated with thick-bedded, often graded, coarse- and fine-grained volcanic sst, minor laminated vitric mudstone.||||||16-JUN-08
34256|Devils Pulpit Member|68592|2|Defined|p1061, p1064, p1066, p1083, p1102-8|Early Devonian|Early Devonian|Originally part of undifferentiated Tangerang Formation described by Wass and Gould (1969) and others. The southern part was included in Aloes Tuff Member (Jones, Carr et al., 1984) but redefined by Simpson, Carr and Jones (1997) as Devils Pulpit Member, after a prominent bluff called Devils Pulpit. Type section and another good exposure are described. Up to 180m thick. A marker horizon. Thin but regionally extensive horizon of immature volcaniclastic rocks of explosive rhyolitic and dacitic provenance. Lithologies described in some detail. Geochemistry briefly described; geophysical properties described. Probable Pragian age; no age-diagnostic fossils.||Unit in Tangerang Formation.||The base is intruded by Carne Dacite Member.|Thick beds of polymictic volcanic breccia, some grading into fine-grained vitric sandstone; massive to graded beds of crystal-rich volcanic sandstone; massive bimodal tuffaceous sandstone.|
34256|Devils Pulpit Member|69159|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Tangerang Formation.|||Pale to mid grey, massive, thick-bedded, occasionally graded, rhyolitic polymictic volcanic breccia, intercalated with thick-bedded, often graded, coarse- and fine-grained volcanic sandstone; minor laminated vitric mudstone.|
34256|Devils Pulpit Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dktp. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Tangerang Formation||Unnamed members near middle of Tangerang Formation over- and underlie this unit.|Massive, thick-bedded,sporadically graded, rhyolitic, polymictic volcanic breccia intercalated with thickly bedded, commonly graded, coarse and fine-grained volcanic sandstone, massive tuffaceous sandstone and fine vitric mudstone.|
34256|Devils Pulpit Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Tangerang Formation|||Massive, thick-bedded,sporadically graded, rhyolitic, polymictic volcanic breccia intercalated with thickly bedded, commonly graded, coarse and fine-grained volcanic sandstone, massive tuffaceous sandstone and fine vitric mudstone.|
34256|Devils Pulpit Member|70661|3|Fully described|p51, p52 fig 5, p59 - p61|Pragian|Pragian|Named after Devils Pulpit bluff. Originally a part of undifferentiated Tangerang Formation,  partly included within Aloes Tuff Member . Outcrops variably in a rugged hill area in Moss Vale. Type section mentioned. Approximately 200m thick. Deposited in a shallow marine environment below storm wave conditions. Structure, metamorphism, geochemistry, fossil assemblage and geophysical characteristics discussed.  Age derived from fossils.||Tangerang Formation||Overlies Carne Dacite Member.|Shallow marine rhyolitic volcaniclastic rocks, mostly massive volcanic breccia and coarse and fine grained volcanogenic bimodal sandstone.|
34256|Devils Pulpit Member|71303|5|Briefly described|map legend|Lochkovian|Lochkovian|||Of Tangerang Formation.|||Thick-bedded polymictic volcanic breccia, vitric sandstone; massive to graded beds of crystal-rich volcanic sandstone; bimodal tuffaceous sandstone. All with angular crystal fragments of quartz, plagioclase, lesser orthoclase; rare fossil fragments.|16-FEB-18
34256|Devils Pulpit Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Tangerang Formation.|||Pale to mid grey, massive to thick-bedded, in places graded, rhyolitic polymictic volcanic breccia, intercalated with thick-bedded, commonly graded, coarse- and fine-grained volcanic sandstone; minor laminated vitric mudstone.|
34256|Devils Pulpit Member|71700|2|Defined|vi, p43, CD|Pragian|Pragian|Named for the Devils Pulpit in Bungonia Creek. The type section was nominated by Simpson, Carr and Jones (1997) in Bungonia Creek from GR 773348 6142809 to GR 773216 6142900. A representative section occurs from GR 760579 6122690 to GR 760393 6122841. Originally this member was a part of the undifferentiated Tangerang Formation. The southern part of this unit was included in the Aloes Tuff Member. That member was discarded by Simpson, Carr and Jones (1997) and rocks belonging to it in addition to older parts of the sequence were redefined as the Devils Pulpit Member. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils and distinguishing features are discussed. A maximum thickness of 180m is estimated. Underlain and overlain by unnamed members of the Tangerang Formation.||Tangerang Formation|||Crudely bedded, coarse- and medium-grained tuffaceous sandstone and minor volcanic breccia.|
24917|Dewrang Group|22601|6|Mentioned|409 fig 6|Late Permian|Early Permian|Early witten as 'Lower' Late written as 'Upper'||||||
24917|Dewrang Group|22857|5|Briefly described|p263, p534 App.1 Tb.A1.9|Early Triassic|Late Permian|Comprises Mammy Johnsons, Weismantels and Durallie Road Formations. In the Stroud-Gloucester Syncline.||||||
24917|Dewrang Group|22864|6|Mentioned|p263|||||||||
24917|Dewrang Group|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Includes the Mammy Johnsons, Weismantels and Durrallie  Formations.   Geological Province: New England Fold Belt||||||
24917|Dewrang Group|40872|6|Mentioned|p37|||||||||
24917|Dewrang Group|41054|5|Briefly described|p152|||||||||
24917|Dewrang Group|42182|5|Briefly described|p301|||Overlain by Gloucester Coal Measures.  Geological Province: Gloucester Basin.||||||
24917|Dewrang Group|42833|5|Briefly described|p227|||||||||
24917|Dewrang Group|44244|2|Defined|p169, p168 Tb.2|Late Permian|Late Permian|Includes Mammy Johnsons, Weismantels, Durallie Road Formations.  Disconformably overlies the Alum Mountain Volcanics.  Max. thickness: 580m.  Geological Province: Myall Block.||||||16-SEP-04
24917|Dewrang Group|50099|6|Mentioned|p13|Late Permian|Late Permian|Overlies the "Bucketts rhyolites" disconformably.||||||
24917|Dewrang Group|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Geological Province: Western Myall Block.||||||
24917|Dewrang Group|63832|6|Mentioned|p131 fig 2|Guadalupian|Cisuralian|Myall block, Southern New England Fold Belt. Seventh (P3) glaciation.||||||
24917|Dewrang Group|64631|5|Briefly described|p44 Fig.2.|Roadian|Kungurian|Southern New England Fold Belt, Myall Block. Biostratigraphic age control for base and top.||||Is overlain by Gloucester Coal Measures.||
24917|Dewrang Group|71628|6|Mentioned|p6:22||||||Chichester, Booral Formations; Salisbury Sandstone.|||
27141|Dicksons Road Dacite Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Florida Volcanics (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||
27141|Dicksons Road Dacite Member|23173|6|Mentioned|Map Legend|||||||||
27141|Dicksons Road Dacite Member|35287|6|Mentioned|p7|||||||||
27141|Dicksons Road Dacite Member|39618|2|Defined|p67|Early Devonian|Early Devonian|||||||
27141|Dicksons Road Dacite Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
28505|Dights Hill Tonalite|31278|6|Mentioned|Fig. 2|||||||||
37357|Dignams Siltstone|50234|5|Briefly described|Map Legend|Early Silurian|Late Ordovician|Of the Bendoc Group.  Thinly-bedded massive to laminated siltstone.  Overlies Warbisco Shale; underlies Poidevins Sandstone.||||||28-MAY-08
37357|Dignams Siltstone|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Bendoc Group. Grey to cream ripple laminated to medium-bedded siltstone with minor mudstone and quartzose fine-grained sandstone.||||||28-MAY-08
37357|Dignams Siltstone|67322|4|Described|p17; Fig.5|Late Ordovician|Katian|Thomas, in Thomas et al.(in press). Approximately 100-500m thick. Apparent conformable relations between the Warbisco Shale and the Dignams Siltstone suggest that the latter is laterally equivalent to the Akuna Mudstone. Age determined from p20 Fig.5 (Strat. column). Occurs in the Goulburn region.||Of the Margules Group.||Interfingers with and conformably overlies the Warbisco Shale. Laterally equivalent to the Akuna Mudstone. Is overlain conformably by Poidevins Sandstone.|Silty and sandy unit distinguished by its olive-grey to brown colour.|21-FEB-18
37357|Dignams Siltstone|68466|6|Mentioned|p65|Late Ordovician|Late Ordovician|Albury-Bega Terrane.||||||
37357|Dignams Siltstone|68592|4|Described|p12, p323, p327, p343-68|Late Ordovician|Late Ordovician|Named after Dignams Gully. A 'well-exposed section' is located. Poorly exposed except in creeks and road cuttings. Thickness to c.500m.||Unit in Margules Group.||Conformably overlies Bendoc Group. Conformably underlies Poidevins Sandstone. Is faulted against Jerrara Formation. Correlates with Mundoonen Sandstone.|Olive to grey, buff and cream laminated to medium-bedded, hard to fissile, micaceous siltstone, with minor mudstone and interlaminated quartzose fine-grained sandstone; bioturbation is typical in the laminated facies.|
37357|Dignams Siltstone|69668|6|Mentioned|p929 Fig.2|Late Ordovician|Late Ordovician|Goulburn-Braidwood area, Albury-Bega terrane.||||||
37357|Dignams Siltstone|70192|5|Briefly described|Map Legend|Bolindian|Bolindian|[Theta]md. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Margules Group |||Olive to grey, buff and cream, laminated to medium bedded siltstone, minor mudstone and fine grained quartzose sandstone.|
37357|Dignams Siltstone|70542|5|Briefly described|Map Legend|Ordovician|Ordovician|||Margules Group |||Olive to grey, buff and cream, laminated to medium bedded siltstone, minor mudstone and fine grained quartzose sandstone.|
37357|Dignams Siltstone|71069|5|Briefly described|p77, p84, p87-91|||||Margules Group||Conformably overlain by the Poidevins Sandstone.|Olive, grey and buff, laminated to medium-bedded siltstone, minor mudstone and quartzose sandstone.|
37357|Dignams Siltstone|71700|5|Briefly described|CD|||||Margules Group||Equivalent to the Mundoonen Sandstone.||
37357|Dignams Siltstone|73140|5|Briefly described|p495 Fig.1, Fig.7|Bolindian|Bolindian|||Margules Group||Overlies Warbisco Shale, underlies Poidevins Sandstone||
27390|Dilga Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
27390|Dilga Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
27390|Dilga Formation|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
78493|Dingo Road Basalt Member|66768|4|Described|p212-218|Late Devonian|Middle Devonian|Informal member of Comerong Volcanics. Max thickness 100m. Intercalated lacustrine sedimentary rocks, minor mafic tuff and lapilli tuff, sparsely amygdaloidal with amygdales filled with chlorite and quartz.||||||07-NOV-13
29267|Dinoga Formation|22857|4|Described|p484 App.1 Tb.A1.6|Early Devonian|Early Devonian|Siltstone, quartz and lithic wacke; minor mudstone and conglomerate. Max. thickness: >100m. Geological Province: Woolomin Basin.||||||24-FEB-06
29267|Dinoga Formation|23050|4|Described|p15 Table 1|Early Devonian|Early Devonian|Age: Early Devonian as indicated by Fossils.||||||
29267|Dinoga Formation|23051|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
29267|Dinoga Formation|41328|2|Defined|p14|Middle Devonian|Early Devonian|Reserved as Dinoga.||||||31-MAY-07
29267|Dinoga Formation|41329|5|Briefly described|p5|||||||||
29267|Dinoga Formation|61764|3|Fully described|p45-46||Late Ordovician|Comprises lenses of volcaniclastic sandstone, siltstone, ash fall tuff, and conglomerate, surrounded by serpentinites and their altered equivalents. Max. thickness: >900m. Shares many similarities with Wisemans Arm Fm||||||27-JAN-06
29267|Dinoga Formation|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Cambrian|In Central Block and Woodsreef Melange.||||||31-MAY-07
29267|Dinoga Formation|65398|6|Mentioned|p21, p22|Devonian|Late Ordovician |Bingara area; possible equivalent of the Glen Bell Formation. Contains Devonian faunas in limestone olistoliths.||||||19-DEC-16
29267|Dinoga Formation|67322|6|Mentioned|p27-28|||(Aitchison et al. 1998; Barclay et al. 1999).||||Possibly equivalent to Glen Bell Formation.||
29267|Dinoga Formation|68005|5|Briefly described|p22, p24, pp28-29, p156, p169 Plan 1.|Early Devonian|Early Devonian|Weraerai terrane, Central Block, New England Fold Belt. Volcaniclastic sediments. Biostratigraphic age from limestone blocks.||||Overlies Woodsreef Melange.|Well-bedded siltstone, quartz and lithic wacke, minor mudstone and conglomerates; blocks of coralline limestone of uncertain affinity.|
29267|Dinoga Formation|68006|6|Mentioned|p20 Fig.3-A.|||Central Block, New England Fold Belt.||||||
35865|Discovery Limestone|23336|5|Briefly described|p3|Middle Cambrian|Middle Cambrian|Parent shown as Cooningan Formation, probably misspelling of Coonigan Formation.||||||21-MAR-06
26521|Dochra Siltstone Member|33867|5|Briefly described|p6|||||||||
26521|Dochra Siltstone Member|34345|4|Described|p334|||||||||
26521|Dochra Siltstone Member|39830|6|Mentioned|Map legend|Late Permian|Middle Permian|Middle to Late Permian||||||
26521|Dochra Siltstone Member|43447|14|Not recorded|p20|||Maitland Group. Part of Mulbring Siltstone||||||
26521|Dochra Siltstone Member|45090|6|Mentioned|p165|||Refers McKellar(1969)||||||
23549|Doctor George Granite|22815|4|Described|p95,96|||||||||
23549|Doctor George Granite|38320|6|Mentioned|p191|||||||||
23549|Doctor George Granite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Mumbulla Suite.||||||
23550|Dog Trap Creek Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Avon Subgroup (Gloucester Coal Measures). Cyclic succession of shale, siltstone and sandstone. Max. thickness: 126m. Geological Province: Sydney Basin.||||||
23550|Dog Trap Creek Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Avon Subgroup.    Geological Province: New England Fold Belt||||||
23550|Dog Trap Creek Formation|40872|6|Mentioned|Fig.2|||||||||
23550|Dog Trap Creek Formation|41054|6|Mentioned|p152|||See also Fig.2||||||
23550|Dog Trap Creek Formation|44244|2|Defined|p178, p168 Tb. 2|Late Permian|Late Permian|Of the Avon Subgroup.  Overlies Waukivory Creek Formation.  Type section in text.  Max. thickness: 150m.  Geological Province: Myall Block.||||||
23550|Dog Trap Creek Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Avon Subgroup (Gloucester Coal Measures).  Geological Province: Western Myall Block.||||||
36335|Donganelly Formation|50234|5|Briefly described|Map Legend|Ludlow|Wenlock|Dark grey laminated siltstone.  Of the Mount Fairy Group.||||||
36335|Donganelly Formation|67820|6|Mentioned|p136 Fig.3|Late Silurian|Late Silurian|||Mount Fairy Group.||||
82408|Donnellys Castle Leucomonzogranite|71628|4|Described|p15: 34-35, 44, 48-51, 58, 70, 76, 82|||See also p15: 88, 97, 102, 115. New name, after a rock formation near Pozieres. Comprises two large and numerous small bodies within a ~20 km N-S belt from Mount Banca to Sorrento. Has various outcrop forms in rough hilly country. Geochemistry described. Spatially associated with minor Sn mineralisation.||Ruby Creek Suite (tentative).||Is entirely enclosed by (?intrudes) Severn River and Mount Lindesay Monzogranites and Ruby Creek Leucogranite.|Pale pink, medium-grained, slightly porphyritic, leucocratic biotite monzogranite. I-type.|
24250|Donovan Basic Complex|22857|6|Mentioned|p215|||Gabbroic intrusions. Geological Province: Lambie Basin.||||||
24250|Donovan Basic Complex|22859|6|Mentioned|p215|||||||||
24250|Donovan Basic Complex|39028|6|Mentioned|Map legend|Frasnian|Givetian|Frasnian to Givetian||||||
24250|Donovan Basic Complex|40276|2|Defined|p19|Late Devonian|Middle Devonian|Middle to Late Devonian. Age 355+/-13 Ma Rb/Sr.||||||03-SEP-18
24250|Donovan Basic Complex|42820|5|Briefly described|p76|||||||||
24250|Donovan Basic Complex|60308|6|Mentioned|p38|Frasnian|Givetian|"Important stratigraphic unit with contentious age" Preferred age quoted. See also Donovan Mafic Complex p39.|386 Ma|||||
24250|Donovan Basic Complex|68298|5|Briefly described|p233|||Provides a younger age constraint for the Nettletons Creek fauna [?because..]|355+/-13 Ma (Wyborn and Owen, 1986)|||||
23553|Doone Member|22857|4|Described|p440 App.1, Tb.A1.6|Devonian|Devonian|Of the Rast Group (Cobar Supergroup). Arenite and granule-cobble conglomerate. Max. thickness: 350m. ||||||
23553|Doone Member|41394|2|Defined|p68|Early Devonian||||||||
23553|Doone Member|41395|6|Mentioned|Map legend|Lochkovian||||||||
39535|Doongala Chert Member|61964|4|Described|p14 Fig. 4, p29|Chewtonian|Chewtonian|Of Clements Formation (Wagga Gp). Includes thin chert beds (up to 10m thick) which pass laterally into qtz sst turbidites+ shale of undiff.Clements Fm. Forms rare outcrops + abundant scree of v. fractured chert; numerous conodonts. Palaeontology (p258)||||||
39535|Doongala Chert Member|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Clements Formation (Wagga Group).  Dark grey to black radiolarian- and conodont-bearing chert (Darriwilian).||||||
39535|Doongala Chert Member|65469|5|Briefly described|p18|Middle Ordovician|Middle Orodovician|Lachlan Orogen.||Clements Formation||||
39535|Doongala Chert Member|67322|4|Described|p18; Fig.5|Darriwilian|Darriwilian|Named by Colquhoun, Hendrickx and Meakin (in Colquhoun et al. 2005). Estimated to be less than 10m thick in the Ungarie area. Vertical stratigraphic relationships are obscure. Age from graptolites. Occurs in the Cargelligo region.||Of the Clements Formation.||Is overlain ?conformably by Currawalla Shale (Bendoc Group).|A relatively poorly exposed and laterally impersistent chert which forms lenticular bodies that pass into sandstone, mudstone and shale of the turbiditic sequence.|21-FEB-18
39535|Doongala Chert Member|68466|5|Briefly described|p65-66|Middle Ordovician|Middle Ordovician|Albury-Bega Terrane. Conodonts indicate Darriwilian age. Quite thin (<10m).||Clements Formation.||Correlates with Numeralla Chert and Nattery Chert Member.||
39535|Doongala Chert Member|68592|6|Mentioned|p318|||On the Cargelligo 1:250 000 sheet.||||Equivalent to Nattery Chert Member (Abercrombie Formation).||
39535|Doongala Chert Member|69160|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Clements Formation.|||Dark grey to black radiolarian- and conodont-bearing chert (Darriwilian).
|
39535|Doongala Chert Member|69668|5|Briefly described|p929 Fig.2, p931|Middle Ordovician|Middle Ordovician|Cargelligo area, Albury-Bega terrane. Contains latest Darriwilian conodont assemblage of Pygodus serra-Periodon aculeatus. Less than 10m thick.||Unit in Clements Formation.||Correlated with Numeralla Chert and Nattery Chert Member.||
39535|Doongala Chert Member|71069|6|Mentioned|p68|||||||Equivalent to the Nattery Chert Member.||
39535|Doongala Chert Member|71700|5|Briefly described|p8|Middle Ordovician|Early Ordovician|||Wagga Group||Equivalent to the Nattery Chert Member.||
39535|Doongala Chert Member|73140|5|Briefly described|p495 Fig.1, Fig.3|Darriwilian|Darriwilian|Age based on conodonts.||Abercrombie Formation||Underlies Currawalla Shale||
24252|Dooralong Shale|22745|5|Briefly described|p127||Scythian|Narrabeen Group, Sydney Basin. Overlain by Munmorah Conglomerate||||||
24252|Dooralong Shale|22749|6|Mentioned|p 196|||||||||
24252|Dooralong Shale|22857|4|Described|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Narrabeen Group. Interbedded siltstone and claystone, and fine to coarse-grained sandstone. Max. thickness: 201m. Geological Province: Sydney Basin.||||||
24252|Dooralong Shale|22969|4|Described|Fig 4.1a||Early Triassic|||||||
24252|Dooralong Shale|24158|5|Briefly described|p173 Fig.4|Early Triassic|Early Triassic|Geological Province: Sydney Basin||||||
24252|Dooralong Shale|36042|6|Mentioned|Fig.22|||See also Fig.23.||||||
24252|Dooralong Shale|36901|6|Mentioned|p16|||||||||
24252|Dooralong Shale|39287|6|Mentioned|p42|||See also Fig.2.18||||||
24252|Dooralong Shale|39294|4|Described|p163|||See also p165||||||30-NOV-21
24252|Dooralong Shale|39307|6|Mentioned|Table 22.1|||||||||
24252|Dooralong Shale|39660|2|Defined|p453|Late Permian|Late Permian|Prob.Late Permian||||||
24252|Dooralong Shale|40625|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
24252|Dooralong Shale|41463|6|Mentioned|Fig.1|||||||||
24252|Dooralong Shale|43194|5|Briefly described|p130|Triassic|Triassic|Fine grained outwash and overbank sediments, eastern Sydney Basin.||||||
24252|Dooralong Shale|61315|5|Briefly described|Table SY1|Eary Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
24252|Dooralong Shale|68003|5|Briefly described|p42.|Triassic|Triassic|Eastern Sydney Basin.|||||Red, green and grey claystone and siltstone, often intercalated with or overlain by conglomeratic sediments.|
24252|Dooralong Shale|73304|6|Mentioned|p77|||Sydney Basin.||||||
81170|Doradilla Formation|72296|5|Briefly described|p6|Early Devonian|Early Devonian|||Cobar Supergroup.||Is faulted against the Girilambone Group.||
79104|Doradilla metasiltstone|69635|4|Described|p119-126, p69|Early Devonian|Late Silurian|Informal name. North-western Lachlan Orogen. U-Pb SHRIMP zircon maximum depositional age. Sampled from drill core DDH DR20 (Aberfoyle), at the depth interval 268.05 to 269.6 m.|415.9+/-3.4 Ma|||May be equivalent to Cobar Supergroup and younger than Girilambone Group.|sample: foliated and laminated metasiltstone.|
41585|Dormans Flat Granite|63732|5|Briefly described|Map legend|Early Triassic|Early Triassic|Pale pinkish grey to pale reddish brown, fine-grained, highly porphyritic (allanite-titanite-hornblende-) biotite monzogranite.||||||
41585|Dormans Flat Granite|63748|4|Described|p44|||Previously mapped as Dundee Rhyodacite and Wallangarra Volcanics. Intrudes Wallangarra Volcs. Pale pinkish grey to reddish brown (iron-stained) fine-gr.(groundmass), highly porph. (allanite-titanite-hornblende-) biotite monzogranite. See also p27 Fig.27.||||||07-FEB-11
41585|Dormans Flat Granite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Bungulla Monzogranite, and Ruby Creek, Sailor Jack and Stanthorpe Granites, are all mapped under the symbol, Rgn.||||||
41585|Dormans Flat Granite|68679|5|Briefly described|p453, p455, p457-459|Early Triassic|Permian|Northern New England Batholith. ~11 km2. Is similar chemically, but not mineralogically or texturally, to the Sailor Jack Granite. Photographs, geochemical plot.||Sailor Jack Suite.||Intrudes the Wallangarra Volcanics.|Pink, pinkish grey to reddish brown, fine-grained, moderately to highly porphyritic biotite quartz monzonite to monzogranite; accessory hornblende, titanite, allanite; local well-developed quench texture. Oxidised, moderately evolved, high-K, I-type.|
41585|Dormans Flat Granite|68901|6|Mentioned|p68 Fig. iii|Early Triassic|Late Permian|||||||26-SEP-18
41585|Dormans Flat Granite|69639|6|Mentioned|p220|||||||||
41585|Dormans Flat Granite|71628|6|Mentioned|p12: 6|||Donchak et al. (2007) after unpublished work by Purdy (2003). See Dormans Flat Monzogranite.||||||
82410|Dormans Flat Monzogranite|71628|5|Briefly described|p12: 1-2, 6-8|||Donchak et al. (2007). First mapped by Purdy (2003; unpublished). Named after a local geographic feature. An irregular shaped intrusion of ~11 km2, ~7 km W of Wallangarra. Geochemistry described.||Dormans Flat Suite.||Intrudes Wallangarra Volcanics.|Pale pinkish grey to pale reddish brown, fine-grained, highly porphyritic biotite-(hornblende) monzogranite. I-type.|
23556|Double Peak Volcanics|22857|4|Described|p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Mount Hope Group (Cobar Supergroup). Max. thickness: >2km. Geological Province: Mount Hope Trough (Darling Basin).||||||
23556|Double Peak Volcanics|37772|4|Described|p6|||||||||
23556|Double Peak Volcanics|40269|5|Briefly described|p147|||||||||
23556|Double Peak Volcanics|40913|6|Mentioned|Map legend|Pragian|Lochkovian|Pragian-Lochkovian||||||
23556|Double Peak Volcanics|41126|2|Defined|p43|early Lochkovian|early Lochkovian|||||||
23556|Double Peak Volcanics|41821|6|Mentioned|p15|||Occurs in the Mount Allen sheet area||||||
23556|Double Peak Volcanics|42144|6|Mentioned|Fig.3 P604|||||||||
23556|Double Peak Volcanics|42521|5|Briefly described|Fig.3b P16|||||||||
23556|Double Peak Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
23556|Double Peak Volcanics|43089|5|Briefly described|Map Legend|||of Mount Hope Group||||||
23556|Double Peak Volcanics|70751|6|Mentioned|p5, p10, p17, p19, p30|||||Mount Hope Group||Intruded by and gradational contact with Mount Allen Granite.|Include lavas of both feldspathic and quartzo-feldspathic composition|23-SEP-19
23556|Double Peak Volcanics|70950|5|Briefly described|p1029,1034-1035-1036|||Geological province: Central Lachlan Orogen.||Unit of Mount Hope Group.|||Siltstone, shale, fine-grained sandstone, felsic volcaniclastic rocks.|23-SEP-19
23556|Double Peak Volcanics|72908|6|Mentioned|p3, p7|||Lavas of the Double Peak Volcanics are very similar to the Mount Kennan and/or Nombiginni volcanics. Hosts the Mount Allen deposit.||Mount Hope Group||||
82481|Doughboy Volcanics|73581|6|Mentioned|p10, p14, p16|||Doughboy Volcanic Province. See also Doughboy basalts p16.||||||
24929|Dowd Formation|22857|5|Briefly described|p456 App.1 Tb.1A1.6|Devonian|Silurian|Of the Toongi Group. Fine-graimed sandstone, shale, lithic sandstone, rhyolite, calcarenite. Max. thickness: 600m. Geological Province: Cowra Trough.||||||09-MAR-06
24929|Dowd Formation|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|of Toongi Group.||||||
24929|Dowd Formation|23170|2|Defined|p121|Late Silurian|Late Silurian|of Toongi Group.||||||
24929|Dowd Formation|24126|6|Mentioned|p221|||||||||
24929|Dowd Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
24929|Dowd Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
24929|Dowd Formation|40328|2|Defined|p125|Silurian|Silurian|||||||
24929|Dowd Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
24929|Dowd Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Shale, coarse lithic arenite, rhyolite, limestone.||||||
24929|Dowd Formation|68003|5|Briefly described|p24 Fig.3-e, p144. |Pridoli|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Whychetella Formation. Is overlain by Trealmont Quartzite.|Shale, siltstone, fine-grained sandstone, lithic sandstone, rhyolite, calcarenite.|
37910|Downs Rhyodacite Member|24605|2|Defined|p931, p951 App.1|Namurian|Namurian|Of the Clifden Formation. Thickness at Type locality: 5m. Geological Province: New England Orogen.||||||
37910|Downs Rhyodacite Member|61214|5|Briefly described|p171 Fig. 1|Carboniferous|Carboniferous|Of the Clifden Formation. ||||||
80147|Doyles Hill Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Werrie Basin. Shown only as Doyles Hill. Ending assumed from references to other Coal Members in text.||Rowan Formation.||||28-SEP-17
75835|Doyles River Road Serpentinite|65317|6|Mentioned|p622 Fig. 1c|||||||||
28513|Drake Volcanics|22580|5|Briefly described|p97,p99||Late Permian|||||||
28513|Drake Volcanics|22857|4|Described|p258, p536 App.1 Tb.A1.9|Early Triassic|Late Permian|Of the Wandsworth Volcanic Group. Rhyodacitic to andesitic flows, crystal-lithic tuffs, breccias and agglomerates. Max. thickness: 1500m. Geological Province: New England Fold Belt. See also p319 Fig. 22.10B. ||||||
28513|Drake Volcanics|22864|6|Mentioned|p258|||||||||
28513|Drake Volcanics|22865|6|Mentioned|Fig22.10bp319|Early Triassic|Late Permian|||||||
28513|Drake Volcanics|23103|5|Briefly described|p551, Fig.1|Permian|Permian|||||||
28513|Drake Volcanics|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Parent: Wandsworth Volcanic Group.  Geological Province: New England Fold Belt.||||||
28513|Drake Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Wandsworth Volcanic Group.  Complexly interbedded rhyodacitic to andesitic flows, tuffs, breccias and volcanilithic sedimentary rocks.||||||12-DEC-07
28513|Drake Volcanics|23812|5|Briefly described|p28 Tb.3, p30|Late Permian|Early Permian|Of Wandsworth Volcanic Group. Intruded by Dumbudgery Creek Granodiorite and Bungulla Monzogranite. Maximum thickness:1500m.||||||
28513|Drake Volcanics|23859|5|Briefly described|p929|Late Permian|Late Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
28513|Drake Volcanics|29988|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
28513|Drake Volcanics|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28513|Drake Volcanics|31694|6|Mentioned|p350|||||||||
28513|Drake Volcanics|31993|6|Mentioned|p683|||||||||
28513|Drake Volcanics|32086|6|Mentioned|p325|||Subhorizontal andesitic volcanics||||||
28513|Drake Volcanics|32484|4|Described|p721|||||||||
28513|Drake Volcanics|32491|5|Briefly described|p14|||Permian||||||
28513|Drake Volcanics|32492|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
28513|Drake Volcanics|32672|6|Mentioned|p675|||||||||
28513|Drake Volcanics|32880|6|Mentioned|p3|||L.-U.Perm.||||||
28513|Drake Volcanics|33005|6|Mentioned|p11|||See also P13||||||
28513|Drake Volcanics|33436|6|Mentioned|Table 1|||Perm. Refers Voisey (1958). Cheviot Hills Gp.||||||
28513|Drake Volcanics|33476|6|Mentioned|Table 1|||||||||
28513|Drake Volcanics|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
28513|Drake Volcanics|34340|6|Mentioned|Table 6.1|||Permian||||||
28513|Drake Volcanics|34556|5|Briefly described|p268|||Permian. Cheviot Hills Group||||||
28513|Drake Volcanics|35911|6|Mentioned|p60|||Discussion re mineral deposits.||||||
28513|Drake Volcanics|36936|6|Mentioned|p208|||||||||
28513|Drake Volcanics|36961|6|Mentioned|p212|||||||||
28513|Drake Volcanics|38806|6|Mentioned|p76|||Geological Province: New England Fold Belt||||||
28513|Drake Volcanics|38837|6|Mentioned|p234|||||||||
28513|Drake Volcanics|39279|3|Fully described|p367|||See also p370.||||||12-DEC-07
28513|Drake Volcanics|39282|6|Mentioned|p401|||Au/Ag mineralisation||||||
28513|Drake Volcanics|40245|6|Mentioned|p182|||Mention Table 1||||||
28513|Drake Volcanics|40504|6|Mentioned|p97|||||||||
28513|Drake Volcanics|40505|5|Briefly described|p81|||||||||
28513|Drake Volcanics|40506|6|Mentioned|p76|||||||||
28513|Drake Volcanics|40514|6|Mentioned|p7|||||||||
28513|Drake Volcanics|40773|3|Fully described|p458|||Mention p458.||||||12-DEC-07
28513|Drake Volcanics|41413|4|Described|p327|||||||||
28513|Drake Volcanics|41474|6|Mentioned|p62|||||||||
28513|Drake Volcanics|42378|5|Briefly described|Table 1 P10|||Andrews 1908||||||
28513|Drake Volcanics|42559|5|Briefly described|p10|||Correlated with Wallangarra Volcanics.||||||
28513|Drake Volcanics|42963|5|Briefly described|p5|||||||||
28513|Drake Volcanics|43017|5|Briefly described|Fig.2,p374|||||||||
28513|Drake Volcanics|43385|14|Not recorded|p179,180||Sakmarian|||||||
28513|Drake Volcanics|43881|14|Not recorded|p6-7,9|||Formation of Cheviot Hills Group||||||
28513|Drake Volcanics|44093|5|Briefly described|p233 App. 1|Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
28513|Drake Volcanics|44852|14|Not recorded|p60|Permian|Late Carboniferous|||||||
28513|Drake Volcanics|46525|6|Mentioned|p148|||||||||
28513|Drake Volcanics|48940|3|Fully described|p49|||||||||
28513|Drake Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group.||||||
28513|Drake Volcanics|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|Of the Wandsworth Volcanic Group.||||||
28513|Drake Volcanics|60995|5|Briefly described|p51 Fig. 3|Early Triassic|Late Permian|Includes granite. Geological Province: Clarence-Moreton Basin. See also p56 Fig. 7.||||||
28513|Drake Volcanics|60996|6|Mentioned|p79|||Geological Province: Clarence-Moreton Basin.||||||
28513|Drake Volcanics|61772|6|Mentioned|p128, p133||Late Permian|In southern New England Orogen.||||||24-SEP-08
28513|Drake Volcanics|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
28513|Drake Volcanics|61795|5|Briefly described|p368|Permian|Permian|Geological Province: New England Fold Belt. May be co-magmatic with Clarence River Supersuite.||||||17-NOV-08
28513|Drake Volcanics|63732|5|Briefly described|Map legend|Late Permian|Late Permian|Andesite, dacite; minor rhyolite and associated pyroclastic rocks.||||||
28513|Drake Volcanics|63748|6|Mentioned|p20, p69|Late Permian|Late Permian|Correlated with Wallangarra Volcanics (Olgers et al 1974).||||||07-FEB-11
28513|Drake Volcanics|68111|5|Briefly described|p968 Tb.1, p970 Fig.2, p976|Capitanian|Wordian||264.4 +/- 2.5 Ma; U-Pb SHRIMP(Cross et al. 2010) |Of the Wandsworth Volcanic Group.||||
28513|Drake Volcanics|68679|6|Mentioned|p453|||Mentioned only as being older than the Emmaville Volcanics.||||||
28513|Drake Volcanics|69323|5|Briefly described|p1,70|Guadalupian|Guadalupian|Geological province: New England Orogen. Previosuly regarded as part of the basal succession of the Wandworth Volcanic Group, however has been dated at 264.4+\-2.5 Ma and its chemical composition is distinct from that of the Wandsworth Volcanic Group.|264.4+\-2.5 Ma (Cross and Blevin 2010)|||||
28513|Drake Volcanics|69639|5|Briefly described|p2, p182, p222|Guadalupian|Guadalupian|New England Orogen.|264.4 +/- 2.5 Ma; Cross and Blevin, 2010.|||Intruded by the Morgans Creek Monzogranite.||
28513|Drake Volcanics|69793|6|Mentioned|p1110, p1113 Fig.3|Permian|Permian|Southern New England Orogen.||||||
28513|Drake Volcanics|70876|5|Briefly described|p2-p3, p64-p75, p79, p81, p96|Permian|Permian|New England Orogen. Additional SHRIMP ages of 265.3 +/- 1.5 Ma (this study) and 264.4 +/- 2.5 Ma (Cross and Blevin, 2010) are provided. This unit was previously included in the Wandsworth Volcanic Group but in this study has been seperated out as a distinct unit on the basis of geochronology. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|265.3 +/- 1.4 Ma (SHRIMP U-Pb)|||||
28513|Drake Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|264+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite, dacite, rhyolite.|
28513|Drake Volcanics|71628|5|Briefly described|p9: 5, 11, 19, 32; p11: 26, 29, 31, 38|||See also p15: 33, 57; p16: 2, 4, 26; p19: 52, 72, 90, 95, 128, 131, 133, 174. RELATED UNITS (continued): Is also intruded by Girard Creek Diorite; Grasstree and Malara Quartz Monzodiorites; Rocky River, Undercliffe Falls Monzogranites (and faulted against the latter); Jenny Lind Tonalite; Cullendore Supersuite; and Mount Carnham Granodiorite (Dumbudgery Creek Complex). Abuts Moonta Gully Monzogranite.|||Navies Creek Member.|Is intruded by Mount Lindesay Monzogranite (Stanthorpe Complex); Morgans Creek Leucomonzogranite; Yellow Gully Leucosyenogranite;  Bruxner and Koreelah Creek Granodiorites; see COMMENTS for more.||
28513|Drake Volcanics|72528|5|Briefly described|p2, p84-85, p110.|Guadalupian|Guadalupian|Situated c. 42 km southeast of Tenterfield.|265.3+/-1.4 to 264.4+/-2.5 Ma|||Intruded by Malara Quartz Monzodiorite.||
28513|Drake Volcanics|73197|5|Briefly described|p475 Fig.6, p477-478, p484|Guadalupian|Guadalupian|New England Orogen, southern. Formed in a shallow shelf environment and is mineralised (Perkins, 1988). U-Pb zircon ages from Carr et al., (2003), Cross and Blevin (2010) and Waltenberg et al., (2016).|265.3 +/- 1.5 Ma, 264.4 +/- 4.0 Ma U-Pb zircon||||Rhyolitic to dacitic volcanics.|
27392|Drik-Drik Formation|22768|6|Mentioned|p181|||||||||
27392|Drik-Drik Formation|22857|5|Briefly described|p181, p484 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Tamworth Group. Breccia, siltstone, sandstone. Max. thickness: 550m. Geological Province: Tamworth Forearc Basin. ||||||
27392|Drik-Drik Formation|30650|4|Described|p317|||||||||
27392|Drik-Drik Formation|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
27392|Drik-Drik Formation|31216|6|Mentioned|p77|||Refers Crook (1961)||||||
27392|Drik-Drik Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
27392|Drik-Drik Formation|36961|6|Mentioned|p208|||||||||
27392|Drik-Drik Formation|38686|5|Briefly described|p54|Middle Devonian|Early Devonian|Geological Province: New England Fold Belt. Basal unit of the Tamworth Group. Underlying Unit: Pipeclay Creek Formation||||||
27392|Drik-Drik Formation|40328|6|Mentioned|p197|||||||||
27392|Drik-Drik Formation|41348|5|Briefly described|Map legend|Devonian|Devonian|Of the Tamworth Group.||||||16-DEC-04
27392|Drik-Drik Formation|41796|6|Mentioned|p305|||||||||
27392|Drik-Drik Formation|43400|2|Defined|p179,182,183,184,map||Early Devonian|(Coblenzian)||||||
27392|Drik-Drik Formation|43406|14|Not recorded|p42,44,45,48,49|||Formation of L.Dev. Tamworth Group||||||
27392|Drik-Drik Formation|50168|6|Mentioned|p157 Fig.2|||Gamilaroi Terrane.||||||
27392|Drik-Drik Formation|68005|4|Described|p49 Fig.3-M, p50, p52 Photo.3-L, p151.|Pragian|Lochkovian|Tamworth Belt. Basal unit on west side of Sandy Creek Fault. Fig.3-M shows Copes Creek Andesite as being a separate unit; the text states it is part of Drik-Drik Formation. Equivalent to lower part of Bog Hole Formation. Unhyphenated on p49 and 151.||Unit in Tamworth Group.|Includes Copes Creek Andesite.|Overlies and is intruded by Copes Creek Andesite. Is overlain by Northcotte Formation.|Arenites, argillites, haematitic breccias, minor siltstones and calcareous siltstone, keratophyre, conglomerate and crystalline limestone lenses and limestone breccia impregnated with haematite of Nemingha Limestone.|
32375|Drildool beds|12597|5|Briefly described|p492 Tb.1, p497, p501|Early Cretaceous|Early Cretaceous|S Surat Basin. 100m thick.|||||Sequence of lithic sandstone and interbedded siltstone and mudstone, with minor thin coal seams associated with carbonaceous siltstone and mudstone; has worm burrows, bioturbation and carbonised plant roots.|
32375|Drildool beds|23053|4|Described|p11,Fig10p17,27-8|Aptian|Neocomian|Lateral equivalent of Bungil Formation.||||||
32375|Drildool beds|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
32375|Drildool beds|24092|5|Briefly described|p8 Fig.3|||||||||
32375|Drildool beds|43277|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||||||
32375|Drildool beds|68003|5|Briefly described|p52, p54, p55 Fig.3-m, pp69-70, p127.|Early Cretaceous|Early Cretaceous|Surat Basin. Deposited in a coastal plain to inter-tidal environment. Lateral equivalent of the marginal marine Bungil Formation. 106 m thick at reference section locality.||||Overlies Keelindi beds. Is overlain by Rolling Downs Group.|Grey, fine-grained lithic sandstone, siltstone, mudstone and minor thin seams of coal; rare beds of mudstone breccia.|
32375|Drildool beds|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
32375|Drildool beds|70821|5|Briefly described|p80|||Coonamble Embayment. Tight aquitard and partial aquifer.||||Overlies Keelindi beds. Is overlain by Wallumbilla Formation (Rolling Downs Group).||04-JAN-17
32375|Drildool beds|71890|4|Described|p5-p7, p18, p26, p52|Barremian|Hauterivian|Surat Basin. Informal unit. Inferred to have been deposited in a coastal plain to intertidal environment.|133.9-126.3 Ma|||Conformably overlies the Keelindi beds.|Fine-grained lithic sandstone, laminated interbedded and intermixed with siltstone, mudstone and minor thin coal seams. Rare mudstone breccia.|
32375|Drildool beds|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Coonamble Embayment (NSW).||||Overlies Keelindi beds. Is overlain by Wallumbilla FZ.||
32375|Drildool beds|72700|5|Briefly described|Mapsheet 1|Mesozoic|Palaeozoic||||||Grey, fine-grained lithic sandstone interbedded with mudstone and minor thin coal seams, rare mudstone breccia.|
30526|Dripstone Formation|6969|5|Briefly described|p12|Early Ludlow|Wenloch|Of the Mumbil Group.  Includes the Bell River Member.  Geological Province: Lachlan Fold Belt.||||||
30526|Dripstone Formation|22857|5|Briefly described|p466 App.1 Tb.A1.6|Wenlockian|Wenlockian|Of the Mumbil Group. ||||||
30526|Dripstone Formation|23043|5|Briefly described|Map Legend|Wenlock|Wenlock|of Mumbil Group.||||||
30526|Dripstone Formation|23170|2|Defined|p80|Wenlock|Wenlock|of Mumbil Group.||||||
30526|Dripstone Formation|23225|6|Mentioned|p17|Ludlow|Wenlock|Age: Early Wenlock to Middle Ludlow. Age based on conodont sampling. Temporal equivalent of Nandillyan Limestone. of Mumbil Group.||||||
30526|Dripstone Formation|60989|6|Mentioned|p111, p114|Early Silurian|Early Silurian|Oakdale Anticline. Includes an uncommon Silurian trimerellide brachiopod (briefly described).||||||
30526|Dripstone Formation|66197|5|Briefly described|p633 Fig.4c|Wenlock|Llandovery|Cowra Trough-Molong High. Silicic volcanics and volcaniclastics. Underlies the Narragal Limestone. Age: 436 +/- 4 Ma.||||||13-MAR-12
30526|Dripstone Formation|68003|5|Briefly described|p24 Fig.3-e, p146. |Wenlock|Llandovery|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Mumbil Group.||Is overlain by Narragal Limestone.|Rhyolitic to felsitic tuff and tuffaceous sandstone; siltstone; mafic to felsic lava; limestone.|
30526|Dripstone Formation|73299|6|Mentioned|p1105|Early Devonian|Silurian|Molong High. [Map symbol suggests Silurian age]||||Overlies Oakdale Formation, underlies the Narragal Limestone.||
29673|Drogheda Volcanics|22857|5|Briefly described|p478 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Crudine Group. Felsic ignimbritic volcanics. Max. thickness: 400m. Geological Province: Capertee Rise.||||||10-MAR-06
29673|Drogheda Volcanics|23214|3|Fully described|p200|Early Devonian|Early Devonian|Consists of a succession of rhyolitic ignimbrite and pyroclastic surge and fall deposits.  Overlying unit: Gibbons Creek Sandstone, underlying unit: Hollanders Formation. Maximum thickness: 500m. May be genetically related to the Bindook Complex.||||||17-JAN-06
29673|Drogheda Volcanics|43639|5|Briefly described|Map Legend||Devonian|||||||
29673|Drogheda Volcanics|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|||||||
29673|Drogheda Volcanics|70297|5|Briefly described|map legend|Pragian|Lochkovian|Erosional base.||||||
73366|Drouin Conglomerate Member|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Meryula Formation.||Is overlain ?conformably by Dederang Siltstone Member.|Matrix- to clast-supported pebble to cobble conglomerate and pebbly sandstone with clasts of metamorphosed quartzose sandstone (dominant) and minor chert and vein quartz; strongly cleaved with clasts flattened and stretched.|
73366|Drouin Conglomerate Member|69095|5|Briefly described|Map legend|Early Devonian|Late Silurian|Conglomerate is matrix- to clast-supported.||Unit in Meryula Formation.||Is overlain ?conformably by Dederang Siltstone Member.|Pebble to cobble conglomerate, pebbly sandstone with clasts of metamorphosed quartzose sandstone (dominant) and minor chert and vein quartz, strongly cleaved with clasts flattened and stretched; massive coarse-grained lithic-quartz sandstone.|
73366|Drouin Conglomerate Member|69635|5|Briefly described|p105|Early Devonian|Late Silurian|||Of Meryula Formation.||Interfingers with Coronga Peak Quartzite in places.||
73366|Drouin Conglomerate Member|70941|3|Fully described|pviii, px, p7 fig 3, p8 fig 4, p9, p76,|Early Devonian|Ludlow|Named for the Drouin Trigonometric Station. Outwash fan deposit. Typically forms topographic highs and strike ridges. No type section defined but a fairly complete section is mentioned.Lithology discussed in great detail.  Distribution, structure, metamorphism, fossils and distinguishing characteristics discussed. Estimated thickness ranging from 100-400m. Unconformably overlies the Ballast Formation, Narrama Formation and the Girilambone Group. Probably equivalent to the Drysdale Conglomerate Member. See also  p77 fig 31, p79, p80, p80 fig 33, p82, p85, p86, p89-p95, p126, p137, p140 fig 58|422.9 Ma |Meryula Formation||Conformably overlain by Dederang Siltstone Member. Interfingers with and locally overlies the Coronga Peak Quartzite.|Upwards fining sequence of massive basal cobble conglomerate, massive pebble and cobble sandstone and massive lithic quartz sandstone. Clasts primarily consist of quartz rich sandstones with minor amounts of quartz and chert clasts also present.|
73366|Drouin Conglomerate Member|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Meryula Formation.||Interfingers with Coronga Peak Quartzite.||
82416|Dry Creek Granodiorite|71628|5|Briefly described|p10: 1, 8-10|||Originally the Rocky Creek Granite and included in the Boxwell Suite by Blevin (unpublished). Renamed the Dry Creek Granodiorite in this study, after a local watercourse. Occurs ~25 km NW of Emmaville; distribution is poorly defined. Geochemistry briefly described.|257.3 +/- 1.5 Ma (SHRIMP: Waltenberg et al., 2015)|||Intrudes Texas beds. Is bounded by Emmaville Volcanics.|Medium- to coarse-grained, equigranular, quartz-poor biotite-hornblende granodiorite to quartz monzodiorite - quartz diorite. I-type.|
23562|Dryden Sandstone Member|22857|5|Briefly described|p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Burthong Formation (Mouramba Group, Cobar Supergroup). Max. thickness: 200m. Geological Province: Mouramba Shelf. ||||||
23562|Dryden Sandstone Member|41528|2|Defined|p65|Early Devonian||||||||
23562|Dryden Sandstone Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
24931|Drysdale Conglomerate Member|730|6|Mentioned|p17.|Devonian|Devonian|Unit in Chesney Formation.||||||11-NOV-14
24931|Drysdale Conglomerate Member|22857|5|Briefly described|p436 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Chesney Formation (Nurri Group, Cobar Supergroup).||||||
24931|Drysdale Conglomerate Member|23171|6|Mentioned|p51|||||||||
24931|Drysdale Conglomerate Member|29621|4|Described|p6|||||||||
24931|Drysdale Conglomerate Member|33123|6|Mentioned|Fig.2|||||||||
24931|Drysdale Conglomerate Member|35185|6|Mentioned|p225|||||||||
24931|Drysdale Conglomerate Member|35219|6|Mentioned|Fig.2|||||||||
24931|Drysdale Conglomerate Member|35287|6|Mentioned|p6|||||||||
24931|Drysdale Conglomerate Member|35383|6|Mentioned|Map legend|Early Devonian|Late Silurian|||||||
24931|Drysdale Conglomerate Member|35385|3|Fully described|p23|||||||||
24931|Drysdale Conglomerate Member|38292|6|Mentioned|p7|||||||||
24931|Drysdale Conglomerate Member|39214|5|Briefly described|p11|||||||||
24931|Drysdale Conglomerate Member|39618|6|Mentioned|p86|||See also Table 1||||||
24931|Drysdale Conglomerate Member|41452|6|Mentioned|p22|||||||||
24931|Drysdale Conglomerate Member|42144|5|Briefly described|p612|||See also Fig.6||||||
24931|Drysdale Conglomerate Member|42521|5|Briefly described|Fig.7 P21|||||||||
24931|Drysdale Conglomerate Member|43032|6|Mentioned|p44|||of Chesney Formation ?||||||
24931|Drysdale Conglomerate Member|43153|5|Briefly described|Map Legend||Lochkovian|of Chesney Formation||||||
24931|Drysdale Conglomerate Member|43774|1|Redefined|p40-42|Early Devonian|Late Silurian|||||||
24931|Drysdale Conglomerate Member|46900|6|Mentioned|p16|||Refers Baker & others(1975), part of Chesney Formation||||||
24931|Drysdale Conglomerate Member|70941|6|Mentioned|p78 fig 32, p86, p137, p145|Late Silurian|Late Silurian|Rocks of this unit may be included in the Meryula Formation. Contains the Drysdale mine.||Chesney Formation||Overlain by the Chesney Formation. Probably equivalent to the Drouin Conglomerate Member.||
24931|Drysdale Conglomerate Member|71360|5|Briefly described|Map legend|||Mapped in the same unit as the Meryula Formation, "Little Mountain Formation", and conglomerates of Brookong Formation extending from the Cobar 1:100 000 map sheet area.||Kopyje Group.||||
24931|Drysdale Conglomerate Member|73174|6|Mentioned|p1037|Lochkovian|Lochkovian|||Chesney Formation, Nurri Group, Cobar Supergroup||||
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.||||||
29509|Dulladerry Volcanics|22466|6|Mentioned|P8||Middle Devonian|||||||
29509|Dulladerry Volcanics|22519|6|Mentioned|p10 Fig 4|||||||||
29509|Dulladerry Volcanics|22580|4|Described|p95|Late Devonian|Middle Devonian|||||||
29509|Dulladerry Volcanics|22768|6|Mentioned|p178,186||Givetian|||||||
29509|Dulladerry Volcanics|22831|3|Fully described|p 67|Late Devonian|Early Devonian|||||||
29509|Dulladerry Volcanics|22857|4|Described|p178, p186, p490 App.1 Tb.A1.7|Givetian|Givetian|Rhyolitic ignimbrites, lavas and breccia; minor basalt, sediments and rare andesites. Age: 376+/-4Ma (U/Pb SHRIMP zircon). Max. thickness: 2300m. Geological Province: Dulladerry Rift. See also p15 Fig. 11.9 and p198.||||||07-SEP-09
29509|Dulladerry Volcanics|22859|6|Mentioned|p198,202,213|||||||||
29509|Dulladerry Volcanics|22933|6|Mentioned|Fig11.9p15|||||||||
29509|Dulladerry Volcanics|23043|5|Briefly described|Map Legend|Givetian|Givetian|||||||14-NOV-05
29509|Dulladerry Volcanics|23170|3|Fully described|p229|Middle Devonian|Middle Devonian|In the Lachlan Fold Belt.||||||12-FEB-07
29509|Dulladerry Volcanics|23214|2|Defined|p214|Givetian|Middle Devonian|Formerly Dulladerry Rhyolite. Age: 376+/-4Ma (SHRIMP U-Pb zircon). Max. thickness 800m.||||||
29509|Dulladerry Volcanics|23217|5|Briefly described|p3, p6|||Includes the Merriganowry Beds. Overlain by Hervey Group units.||||||17-JUL-08
29509|Dulladerry Volcanics|23309|6|Mentioned|p390|||||||||
29509|Dulladerry Volcanics|23392|6|Mentioned|p7|||||||||
29509|Dulladerry Volcanics|23522|5|Briefly described|p249 Fig 5|Middle Devonian||||||||
29509|Dulladerry Volcanics|24126|5|Briefly described|p2|||||||||
29509|Dulladerry Volcanics|24233|5|Briefly described|p256|||Geological Province: Lachlan Orogen.||||||14-NOV-05
29509|Dulladerry Volcanics|24417|3|Fully described|p114|Middle Devonian|Middle Devonian|Of Rocky Ponds Group. Previously included as part of Glenisla Volcanics.  Supersedes "Dulladerry Rhyolite". Unconformably overlain by Hervey Group.||||||
29509|Dulladerry Volcanics|24580|5|Briefly described|p828|Late Devonian|Givetian|Unconformably overlain by the Hervey Group. Geological Province: Eastern Lachlan Fold Belt.||||||14-NOV-05
29509|Dulladerry Volcanics|43494|6|Mentioned|p18|||Unconformably overlie Canowindra Volcanics.||||||16-MAR-06
29509|Dulladerry Volcanics|43640|5|Briefly described|Map Legend||Devonian|||||||
29509|Dulladerry Volcanics|43642|5|Briefly described|Map Legend|Devonian|Devonian|Includes Merriganowry Shale Member.||||||17-JUL-08
29509|Dulladerry Volcanics|43782|5|Briefly described|Map Legend|Givetian|Givetian|||||||
29509|Dulladerry Volcanics|44093|5|Briefly described|p185 App. 1|Middle Devonian|Middle Devonian|Rift-related volcanics. Geological Province: Lachlan Fold Belt.||||||
29509|Dulladerry Volcanics|44160|5|Briefly described|Map Legend|Givetian|Eifelian|||||||
29509|Dulladerry Volcanics|60009|5|Briefly described|Map Legend|Givetian|Givetian|Of the Rocky Ponds Group.  Includes: Warraberry Member, Curumbenya Ignimbrite Member.||||||14-NOV-05
29509|Dulladerry Volcanics|60308|6|Mentioned|P39|||Eastern Lachlan Fold Belt.||||||
29509|Dulladerry Volcanics|61964|6|Mentioned|p81|Givetian|Givetian|A-type. On the BATHURST and DUBBO  1:250k map sheets.||||||
29509|Dulladerry Volcanics|62569|5|Briefly described|p606 Figs. 1A and C|Middle Devonian|Middle Devonian|Supersedes Dulladerry Rhyolite. Underlies Hervey Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
29509|Dulladerry Volcanics|63891|5|Briefly described|p236, p260|||Volcanic analogue of A type intrusion. Geol Prov: Dulladerry rift zone; Eastern Lachlan Orogen.||||||
29509|Dulladerry Volcanics|64826|5|Briefly described|p1040 Tb. 1|Givetian|Givetian|Of Rocky Ponds Group.||||||04-MAR-09
29509|Dulladerry Volcanics|65214|6|Mentioned|p278|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
29509|Dulladerry Volcanics|66768|5|Briefly described|p209, p211, p212||Frasnian|In Rocky Ponds Group. Post-orogenic magmatism. Dominantly felsic with minor mafic and andesitic units. 376 +/- 4 Ma U/Pb zircon age (Pogson and Watkins 1998).||||||
29509|Dulladerry Volcanics|67823|6|Mentioned|p366||||||Includes the Merriganowry Shale Member.|||
29509|Dulladerry Volcanics|68592|5|Briefly described|p33|Middle Devonian|Middle Devonian|Dulladerry Rift.||Unit in Rocky Ponds Group.|||A-type bimodal volcanics and associated plutons.|
29509|Dulladerry Volcanics|69043|5|Briefly described|p3, p6, p74-78, p118|Late Devonian|Late Devonian|Tumut Trough. An intrusive "Caloma dyke" is dated at 381.8 +/- 2.1 Ma.|376 +/- 4 Ma (Pogson and Watkins, 1998).|Rocky Ponds Group.||||
29509|Dulladerry Volcanics|70297|4|Described|map legend, on side 2 of map sheet|Middle Devonian|Middle Devonian|Age: late Middle to early Late Devonian. Deposited in Dulladerry Rift.||Rocky Ponds Group|Coates Creek Ignimbrite Member, Curumbenya Ignimbrite Member, Merriganowry Shale Member, Warraberry Member|Is overlain by Late Devonian Lambie, Catombal and Hervey Groups.|Bimodal and A-type affinities. Quartz-K feldspar phyric, welded rhyolitic ignimbrite, rhyolite lava, volcanic breccia, basalt, andesite; minor andesite, volcaniclastic sandstone, siltstone, conglomerate; intrusive rhyolite domes.|
29509|Dulladerry Volcanics|71040|6|Mentioned|p12 Fig.7|Middle Devonian|Middle Devonian|||||||
29509|Dulladerry Volcanics|71700|5|Briefly described|p29|Middle Devonian|Middle Devonian|||Rocky Ponds Group||||
37359|Duluth Gabbro|24037|6|Mentioned|p428|||||||||
37359|Duluth Gabbro|64647|6|Mentioned|p41|||Reference zircons.||||||
82418|Dumboy-Gragin Leucosyenogranite|71628|4|Described|p19: 27-32, 36, 48, 119, 169|||Stroud (1992) after Carne (1911). Has also been known as Delungra Granite (Tyne, 1989). The name is derived from the parishes of Dumboy and Gragin; leucosyenogranite emphasises its felsic nature. Crops out as several inliers N, W and SW of Delungra; these are regarded as being joined at depth to form a 40 x 15 km intrusion. Is extensively weathered with generally poor outcrop. Lithology, mineralogy and geochemistry are described in detail. Has an extremely high radiometric response. Is associated with Sn deposits, disseminated Cu deposits, Bi veins, and As veins and disseminations (all named and elaborated).|252.0 +/- 1.3 Ma (SHRIMP: Waltenberg et al., 2015)|Dumboy-Gragin Suite.||Intrudes Whitlow and Cara Formations and Texas beds. Is overlain unconformably by Gunnee Formation and Gragin Conglomerate.|White to grey, coarse- to fine-grained, seriate to porphyritic, leucocratic syenogranite and alkali feldspar granite with abundant miarolitic cavities, and granophyric intergrowths. I-type.|
82419|Dumbudgery Creek Complex|71628|4|Described|p1:11; p2:54; p9: 2, 9-23, 26-27, 30-31|||See also p9: 33, 35-36; p10-7; p18-13; p19-176. New name. Formerly? included Yugilbar Gabbro, which is here excluded from the Clarence River Supersuite. Crops out over ~200 km2, several km W of Baryulgil. Contacts and metamorphism are detailed. Geochemistry summarised; has evidence of crustal contamination and hybridism. A number of age determinations are given. Is spatially associated with numerous mineral deposits (listed): Au, Sb, Cu, base metals, Hg and Fe.|255 - 249 Ma.|Clarence River Supersuite.|Mount Carnham Granodiorite, Wave Hill Tonalite, Yugilbar Gabbro.|Intrudes Silverwood Group, Drake Volcanics, Gordonbrook Serpentinite (and is faulted against this last).|An intrusive complex comprising a diverse range of intermediate to felsic, heterogeneous, hybrid, low-K granites; several sinuous zones and dykes of mafic rocks; numerous country rock inclusions and roof pendants. I-type. Lithologies very detailed.|
25886|Dummy Creek Conglomerate|22857|4|Described|p263, p270, p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of Wandsworth Volcanic Group. Continental deposits of the New England Orogen. Conglomerate with abundant basal sediment fragments; minor sst. and mudstone; carbonaceous and shelly sediments; tuffs. Geol. Prov: New England Fold Belt.||||||24-FEB-06
25886|Dummy Creek Conglomerate|22864|6|Mentioned|p263,270|||||||||
25886|Dummy Creek Conglomerate|23720|5|Briefly described|Map Legend|||Of Wandsworth Volcanic Group.  Lithic conglomerate, coarse sandstone, massive mudstone.||||||15-DEC-04
25886|Dummy Creek Conglomerate|23859|5|Briefly described|p930 Fig. 2|Early Permian|Early Permian|Of Wandsworth Volcanic Group. Overlying Unit Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
25886|Dummy Creek Conglomerate|30911|6|Mentioned|Map legend|Permian|Permian|||||||
25886|Dummy Creek Conglomerate|31694|6|Mentioned|p346|||||||||
25886|Dummy Creek Conglomerate|31806|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25886|Dummy Creek Conglomerate|32671|6|Mentioned|Map legend|Permian|Permian|||||||
25886|Dummy Creek Conglomerate|32672|6|Mentioned|p675|||||||||
25886|Dummy Creek Conglomerate|32944|6|Mentioned|p709|||Permian||||||
25886|Dummy Creek Conglomerate|34026|6|Mentioned|p284|||Permian||||||
25886|Dummy Creek Conglomerate|34350|2|Defined|p13|Permian|Permian|See also PP14,18.||||||
25886|Dummy Creek Conglomerate|35257|6|Mentioned|Fig.15|||||||||
25886|Dummy Creek Conglomerate|36961|6|Mentioned|Fig.5|||||||||
25886|Dummy Creek Conglomerate|38288|5|Briefly described|Table 1|||||||||
25886|Dummy Creek Conglomerate|39214|4|Described|p37|||Fig.15||||||
25886|Dummy Creek Conglomerate|42378|4|Described|Table 1 P10|||||||||
25886|Dummy Creek Conglomerate|44093|5|Briefly described|p239 App. 1|Early Permian|Early Permian|Clastic sediments; Continental, fluvial molassic deposition in ?erosional intramotane depressions; folded and faulted; low-grade greenschist to unmetamorphosed. Geological Province: New England Fold Belt.||||||07-APR-05
25886|Dummy Creek Conglomerate|44450|5|Briefly described|p26 Table 6|Permian|Permian|Of Wandsworth Volcanic Group. Underlying unit Sandon beds. Geological Province: New England Fold Belt.||||||
25886|Dummy Creek Conglomerate|50016|6|Mentioned|p354 Fig.1|Permian|Permian|Geological Province: New England Fold Belt||||||
25886|Dummy Creek Conglomerate|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
25886|Dummy Creek Conglomerate|69188|5|Briefly described|p60|Permian|Permian|Armidale region. Described as Fauna IV-bearing.||Basal Wandsworth Volcanic Group.||Is intruded by the Highlands Complex.||
25886|Dummy Creek Conglomerate|71628|5|Briefly described|p8: 34, 107; p13:4|||||Wandsworth Volcanic Group.||Is intruded by Mount Duval Monzogranite, Tilbuster Granodiorite and Highlands Complex.||
39092|Duncans Creek Suite|23799|5|Briefly described|p117|||Of Shaw and Flood (1991), and Bryant and others (1997).  Of the Clarence River Supersuite.  Includes Duncan's Creek Trondhjemite, Mount Ephraim intrusion and the high-Si group within Kaloe Granodiorite.||||||
39092|Duncans Creek Suite|71628|6|Mentioned|p18: 4, 8, 21||||||Duncans Creek, Gogs Top Trondhjemites; Mount Ephraim Granodiorite.|||
24937|Dundurrabin Granodiorite|22636|6|Mentioned|p473||Permian|||||||
24937|Dundurrabin Granodiorite|23720|5|Briefly described|Map Legend|||Of Hillgrove Plutonic Suite.  Biotite granodiorite, leucogranite.||||||15-DEC-04
24937|Dundurrabin Granodiorite|24127|5|Briefly described|p4|Permian|Permian|||||||
24937|Dundurrabin Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
24937|Dundurrabin Granodiorite|31695|6|Mentioned|Fig. 1|||||||||
24937|Dundurrabin Granodiorite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
24937|Dundurrabin Granodiorite|35264|2|Defined|p17|Late Paleozoic|Late Paleozoic|Probably Late Palaeozoic.||||||07-NOV-08
24937|Dundurrabin Granodiorite|36411|6|Mentioned|p268|||Refs Korsch 1978 for definition.||||||
24937|Dundurrabin Granodiorite|40177|6|Mentioned|p52|||||||||
24937|Dundurrabin Granodiorite|44450|5|Briefly described|p17|||Of Hillgrove Plutonic Suite. Geological Province: Coffs Harbour Block.||||||
24937|Dundurrabin Granodiorite|70876|6|Mentioned|p81|||||Herries Supersuite||||
24937|Dundurrabin Granodiorite|71628|3|Fully described|p2: 2, 20, 22, 34, 45-46, 48-49, 53,55|||See also p2: 58-59; p3: 1, 4-5, 8, 10, 27-32; p17: 13, 48-49. Binns et al. (1967), Korsch (1978); after the village of that name. Type locality is road cuttings on the Grafton to Ebor road E of Dundurrabin and outcrops in Blicks River at the road crossing. Occurs between Dundurrabin and Dorrigo, 31 km long (much under basalt cover). Geochemistry detailed. Contains low-K, often amphibole-bearing variants which are spatially associated with Charon Creek Quartz Diorite and likely reflect hybridised components. Has similarities with contaminated granites of the Sheep Station Creek Complex. Hosts numerous small, vein-related Au occurrences; and some As, Sb and Cu deposits. Also called Dundurrabin Monzogranite on p2-45, and mis-spelled as Dundurabbin Granodiorite (Kemp et al., 2009).|290.9 +/- 2.9 Ma (Rosenbaum et al., 2012).|Dundurrabin Suite.||Intrudes Moombil Sandstone, Brooklana beds, Dorrigo Mountain Complex and Buffers Creek Formation. Surrounds and abuts Charon Creek Quartz Diorite.|Medium- to coarse-grained porphyritic granodiorite with minor monzogranite, and leucocratic, finer-grained garnet- and independently, amphibole-bearing variants; massive to moderately deformed. S-type.|
24937|Dundurrabin Granodiorite|73197|6|Mentioned|p473|Artinskian|Gzhelian|Reprocessing of U-Pb zircon ages from 290.3 +/- 5.5 Ma to 295.2 +/- 6.9 Ma to include all dated zircons including those older than 300Ma.|295.2 +/- 6.9 Ma U-Pb zircon|||||
34758|Dungarubba Clay|22892|6|Mentioned|table9 p69|Quaternary|Quaternary|Age: 250000yrs Bp.||||||
24256|Dungay Group|36961|6|Mentioned|p215|||Informal name, see also P221.||||||
24258|Dunhill Bluff Limestone Member|23214|3|Fully described|p41|Eastonian|Eastonian|Of Fossil Hill Limestone. 24.5 m thick at type section.  Underlying Unit: Taplow Limestone Member.||||||
24258|Dunhill Bluff Limestone Member|38219|2|Defined|p307|Late Ordovician|Late Ordovician|Part of Cliefden Caves Group. See also Fig.2.||||||
24258|Dunhill Bluff Limestone Member|41046|6|Mentioned|p144|||||||||
24258|Dunhill Bluff Limestone Member|42479|5|Briefly described|p108|||||||||
24258|Dunhill Bluff Limestone Member|42603|5|Briefly described|Fig.4 P57|||||||||
24258|Dunhill Bluff Limestone Member|70754|5|Briefly described|p449, p455, p459, p465|Late Ordovician|Late Ordovician|Outer shelf, deeper-water deposits. Some fossil species named. Systematic palaeontological descriptions.||Fossil Hill Limestone.||||
24258|Dunhill Bluff Limestone Member|73208|5|Briefly described|p874|Late Ordovician|Late Ordovician|Characterised by abundant plectambonitoid brachiopods and trilobites.||||Is overlain by Belubula Limestone.||
26531|Dunmoogin Formation|22529|6|Mentioned|1|||Junior synonym of Waterbeach Formation||||||
26531|Dunmoogin Formation|24126|6|Mentioned|p234|||Geological Province: Hill End Trough.||||||
26531|Dunmoogin Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
26531|Dunmoogin Formation|32046|6|Mentioned|p133|||||||||
26531|Dunmoogin Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
26531|Dunmoogin Formation|40328|6|Mentioned|p173|||See also P174||||||
26531|Dunmoogin Formation|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
26531|Dunmoogin Formation|43494|5|Briefly described|p27|Devonian|Devonian|Of the Crudine Group. Consists of laminated siltstone, minor sandstone beds in places.  Max. thickness: ~500m.||||||16-MAR-06
24938|Dunoon Dacite|22857|5|Briefly described|p492 App.1 Tb.A1.7|Devonian|Devonian|Of the Hyandra Creek Group. Dacite, rhyolite. Max. thickness: 400m.||||||
24938|Dunoon Dacite|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Hyandra Creek Complex.||||||
24938|Dunoon Dacite|23170|2|Defined|p209|Early Devonian|Early Devonian|Age: SHRIMP U/Pb Zircon Age 406+/-2.7 Ma. of Hyandra Creek Group.||||||
24938|Dunoon Dacite|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
24938|Dunoon Dacite|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
24938|Dunoon Dacite|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
24938|Dunoon Dacite|68003|5|Briefly described|p24 Fig.3-e, p142. |Lochkovian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Hyandra Group.|||Dacite, rhyolite.|
36473|Dunskeig Granite|23550|4|Described|p504|||Fig 1 p502 and p509. of Wangrah Suite. Lachlan Fold Belt Province.||||||
36473|Dunskeig Granite|71206|6|Mentioned|p373, 377|||Lachlan Fold Belt.||Wangrah Suite.|||Aluminous A-type granite.|
23566|Durallie Road Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Early Permian|Of Dewrang Gp. Basal pebbly conglomerate dominated by porphyritic felsic volcanic clasts; massive, thickly bedded lithic sst., mudstone. Correlative of part of Branxton and Bulahdelah Fms (Myall Syncline). Max. thickness: 250m. Geol. Prov: Sydney Basin.||||||24-FEB-06
23566|Durallie Road Formation|40872|6|Mentioned|Fig.1|||See also Fig.2||||||
23566|Durallie Road Formation|41054|6|Mentioned|p152|||See also Fig.2||||||
23566|Durallie Road Formation|42833|5|Briefly described|p227|||see also Fig.2 P225, of Dewrang Group||||||
23566|Durallie Road Formation|43017|5|Briefly described|Fig.1,p372|||||||||
23566|Durallie Road Formation|44244|2|Defined|p169, p168 Tb. 2|Late Permian|Late Permian|Of the Dewrang Group.  Underlies the Weismantels Formation.  Max. thickness: 250m. Geological Province: Myall Block.||||||
23566|Durallie Road Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Dewrang Group.  Geological Province: Western Myall Block.||||||
23566|Durallie Road Formation|73487|6|Mentioned|p564, p567, p570, p574, p576-577|Kungurian|Artinskian|Western Myall Block. Shown as Durallie Road p566. See also p568 Fig.3.|||||Includes tuffs.|
30352|Durandal Granite|23214|3|Fully described|p250|Carboniferous|Carboniferous|Of Bathurst Batholith. Formerly referred to as Durandal Stock, Durondal Stock, Yetholme Granite (with the Eusdale Granite) and Durandal Adamellite.  Mafic I-type Granite.  Age: 305 +/- 10Ma - 318 +/- 17Ma.||||||
30352|Durandal Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
30352|Durandal Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|of Bathurst Batholith. Does not appear on map face.||||||
30352|Durandal Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
38300|Durrallie Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Dewrang Group.   Geological Province: New England Fold Belt||||||
70522|Dynamite Tank Granodiorite|66623|2|Defined|pp160-165.|Silurian|Silurian|Defined in this study. Age of diorite unit 420.2 +/- 3.3 Ma, almost identical with that of Tibooburra Granodiorite, with which it was previously included. Granodiorite crops out as prominent tors and pavement; the diorite as low rubble.|Granodiorite 425.7 +/- 2.2 Ma.|Unit in Tibooburra Suite.||Intrudes Easter Monday Formation.|Massive, medium-grained quartz-feldspar-biotite-hornblende granodiorite with minor mafic enclaves and abundant narrow aplitic dykes; and a single outcrop of fine- to medium-grained, pale to dark green feldspar-hornblende-pyroxene diorite.|
70522|Dynamite Tank Granodiorite|66920|5|Briefly described|Map legend|Silurian|Silurian|Higher magnetic susceptibility than other plutons in the Suite.|||||Massive, medium-grained, quartz-feldspar-biotite-hornblende granodiorite with minor mafic enclaves; massive, equigranular diorite.|
70522|Dynamite Tank Granodiorite|67209|5|Briefly described|Map legend.|Silurian|Silurian|Higher magnetic susceptibility than other plutons in this Suite.||Unit in Tibooburra Suite.|||Massive, medium-grained, quartz-feldspar-biotite-hornblende granodiorite with minor mafic enclaves; lesser massive, equigranular plagioclase-amphibole diorite with subordinate biotite, K-feldspar and quartz.|
70522|Dynamite Tank Granodiorite|71965|5|Briefly described|p897,909|Pridoli|Ludlow|Geological province: Thomson Orogen. |c. 427 Ma to 420 Ma|Unit of Tibooburra Suite.||Inrudes into the Easter Monday Formation.||
70522|Dynamite Tank Granodiorite|72522|5|Briefly described|p119.|Pridoli|Ludlow||c. 420-427 Ma|Tibooburra Suite||||
70522|Dynamite Tank Granodiorite|72951|5|Briefly described|p1013, 1019, 1024|Lochkovian|Ludlow|Thomson Orogen, southwest. I-type. SHRIMP U-Pb zircon isotope analyses from Black (2007). eHf = -0.5 +/- 0.2, d18O = 6.42 +/- 0.22.|420.2 +/- 3.3 Ma|Tibooburra Suite|||Includes Hornblende diorite marginal phase.|
73552|Easter Monday Formation|66623|2|Defined|p51, pp98-104, p239.|Early Ordovician|Late Cambrian|Defined in this study. Originally part of Torrowangee Series (Mawson 19121); named after Easter Monday beds of Scheibner and Basden (1996). Correlates with Jeffreys Flat Formation, and possibly Dullingari Group of Warburton Basin. Turbiditic continental margin slope deposits. Excellent outcrops. No fossils identified.|497.2 +/- 2.6 Ma (Black 2006).|Unit in Warratta Group.||Intruded by Evelyn Creek volcanics and Tibooburra Suite. Is unconformably overlain by Namur Sandstone and Eyre Formation. Is in faulted contact with Cadna-owie Formation.|Metasandstone, metamudstone and phyllite, felsic tuffaceous units; minor pebble- to boulder-diamictite and calcareous sandstone.|30-MAY-13
73552|Easter Monday Formation|66920|5|Briefly described|Map legend|Cambrian|Cambrian|Includes 10 un-named but separately mapped units.||Unit in Warratta Group.|||Phyllitic pelite, metasiltstone and siliciclastic metasandstone, minor conglomerate and calcareous sandstone. Locally, felsic volcaniclastic beds to 1 m thick; tectonic breccia; reworked felsic volcaniclastics, metabasalt and diamictite.|
73552|Easter Monday Formation|66921|5|Briefly described|Map legend|Cambrian|Cambrian|Does not outcrop in map area. Position in cross-section is based on geological interpretation and geophysical modelling.||Unit in Warratta Group.||Overlies Jeffreys Flat Formation.|Phyllitic pelite, metasiltstone and siliciclastic metasandstone; minor conglomerate and calcareous sandstone.|
73552|Easter Monday Formation|66927|5|Briefly described|Map legend|Cambrian||Numerous narrow trends of low to moderate magnetic intensity occur where basement is shallow, and broad areas of low magnetic intensity where it is deeper.||||Overlies Yancannia Formation [?].|Phyllite, slate and metasediments; minor conglomerate, diamictite and felsic volcaniclastics. Locally hornfelsed and altered.|24-SEP-13
73552|Easter Monday Formation|67105|6|Mentioned|p659|||||Warratta Group.|||Deep-marine environment; turbidites.|
73552|Easter Monday Formation|67207|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Warratta Group.|||Phyllitic sandstone, metasiltstone, and siliciclastic metasandstone, minor conglomerate and calcareous sandstone; regionally metamorphosed to lower greenschist facies.|
73552|Easter Monday Formation|67209|5|Briefly described|Map legend.|Cambrian|Cambrian|Six un-named sub-units with differing lithologies are mapped separately.||Unit in Warratta Group.||Is intruded by granodiorites of the Tibooburra Suite. Is overlain by Namur Sandstone.|Phyllitic sandstone, metasiltstone and siliciclastic metasandstone, minor conglomerate and calcareous sandstone; regionally metamorphosed to lower greenschist facies.|
73552|Easter Monday Formation|67211|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Warratta Group.||Is intruded by Tibooburra Suite. Is overlain by Wallumbilla Formation.|Phyllitic sandstone, metasiltstone and siliciclastic metasandstone, minor conglomerate and calcareous sandstone; regionally metamorphosed to lower greenschist facies.|
73552|Easter Monday Formation|67322|4|Described|p13; Fig.5|Late Cambrian|Late Cambrian|(Vickery, in Greenfield et al., 2010). Age from a laminated felsic tuff (Black 2006, 2007). Occurs only in the Tibooburra Inlier.|497.2 +/- 2.6 Ma (SHRIMP II U-Pb zircon analysis)|Of the Warratta Group.|||Predominantly metasandstone, metamudstone and phyllite of probable turbiditic origin (displaying graded bedding and Bouma sequences) with rare diamictite.|21-FEB-18
73552|Easter Monday Formation|68823|5|Briefly described|p383|Late Cambrian|Late Cambrian|Jiangshanian minimum age. Geochronology by Black (2006); Greenfield (2010b).|497 +/- 2.6 Ma, SHRIMP II|Of the Warratta Group||||
73552|Easter Monday Formation|69001|5|Briefly described|p2 Fig.1B, p13, p28 Fig.15, p59|Paibian|Guzhangian|Occurs within the Tibooburra Inlier. Age derived from tuffaceous mudstones by sensitive high-resolution ion microprobe.|497.2 +/- 2.6 Ma, U-Pb SHRIMP (Black 2006)|Of the Warratta Group.||Overlain by the Algebuckina Sandstone.|Metasediments.|
73552|Easter Monday Formation|69002|5|Briefly described|p7|Paibian|Guzhangian|Felsic tuff dated by SHRIMP II from a locality on the Olive Downs 1:100k sheet at zone 54. Deep water depositional environment.|497 +/- 2.6 Ma, SHRIMP II (Greenfield 2010b)|Of the Warratta Group.||Correlative of the Jeffreys Flat Formation.||
73552|Easter Monday Formation|69043|6|Mentioned|p11|||Thomson Orogen.||||||
73552|Easter Monday Formation|69541|5|Briefly described|p654|Late Cambrian|Late Cambrian|Cleaved; low-grade greenschist metamorphosed.||Unit in Warratta Group.|||Sandstone, mudstone, phyllite; less common conglomeratic and volcaniclastic subunits of turbiditic aspect.|
73552|Easter Monday Formation|70649|5|Briefly described|Map Legend|Cambrian|Cambrian|6 un-named units: Magnetic unit differentiated only during geophysical modelling. Laminated to finely bedded, strongly cleaved and moderately siliceous phyllite and slate. Thinly bedded phyllite and sandy phyllite; variably metamorphosed and foliated. Moderately well-bedded, variably cleaved sandy phyllite with subordinate metasandstone and phyllite. Well-bedded, variably foliated, weakly siliceous, immature lithic wacke; regionally metamorphosed to greenschist facies; also hornsfelsed variant. Moderately well-bedded, variably cleaved metasandstone and sandy phyllite.||Warratta Group|Includes 6 un-named units.||Phyllitic sandstone, metasiltstone and siliciclastic metasandstone, minor conglomerate and calcareous sandstone; regionally metamorphosed to lower greenschist facies.|
73552|Easter Monday Formation|70652|5|Briefly described|Map Legend|Cambrian|Cambrian|||Warratta Group|||Phyllitic sandstone, metasiltstone and siliciclastic metasandstone, minor conglomerate and calcareous sandstone; regionally metamorphosed to lower greenschist facies.|
73552|Easter Monday Formation|70749|5|Briefly described|p42-43|Ordovician|Cambrian|Tibooburra Inlier. Shelf to deep-marine deposits.|||||Variably deformed and metamorphosed siltstone, sandstone and mudstone.|
73552|Easter Monday Formation|71415|5|Briefly described|p11,17|||Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Associated with marine deposition and volcanism post-delamarian Orogeny. Includes felsic volcanism at c. 497 Ma. Underwent deformation and metamorphism between c. 441-424 Ma, intruded by post-D1 monzodioritic sills and dykes between c. 423 and 416 Ma, and by Tibooburra Granodiorite.||Unit of Warratta Group.||||
73552|Easter Monday Formation|71965|4|Described|p897-899,909|||Geological province: Thomson Orogen. Occurs in the Tibooburra Inlier. Interpreted as a deep marine turbiditic package. A tuffaceous unit has been dated at 497.2+\-2.6 Ma.|497.2+\-2.6 Ma (tuff dep age)|Unit of Warratta Group.||Correlable with Jeffreys Flat Formation and Yancannia Formation. Intruded by Tibooburra Granodiorite.|Interbedded, variably cleaved and metamorphosed metamudstone and metasandstone, minor felsic tuffaceous beds, diamictite and calcareous sandstone.|
73552|Easter Monday Formation|72522|4|Described|p3, p5, p65, p113-114, p119-124, p127|Furongian|Ediacaran|Thomson Orogen. Maximum depositional age determined herein: 567+/-7 Ma. Depositional age determined from tuff in the Tibooburra Inlier (Greenfield et al, 2010). Occurs on low rounded hills west of the township of Tibooburra.|497+/-2.6 Ma depositional age from tuff (p113).|Warratta Group||Unconformably overlies Teltawongee Group. Intruded by the Tibooburra Granodiorite.|Dominated by metamudstone and metasandstone. Minor tuffaceous beds.|24-FEB-21
73552|Easter Monday Formation|73177|5|Briefly described|p1098-1099, 1112, 1115 Fig.17, 1116,1118|Late Cambrian|Late Cambrian|Thomson Orogen. Crops out near Tibooburra.|497.2 +/- 2.6 Ma (Black, 2006).|Warratta Group.||Possible equivalent to Yancannia Formation.|Includes a solitary laminated felsic tuff.|
82430|Eastlake Monzogranite|71628|4|Described|p2: 61-63, 65, 67-69; p3: 1, 4, 24,32-35|||Originally the Hillview Adamellite (Binns et al., 1967); subsequently the East Lake Adamellite (Leitch et al., 1971), Eastlake Adamellite (Landenberger, 1986), East Lake Monzogranite (Brown, 2003). Here spelled Eastlake Monzogranite after the homestead of that name. A N-S trending body, ~35 km S of Armidale and ~25 km SSE of Uralla. Geochemistry described. This ~292 Ma age may relate to the Shallow Lagoon Monzogranite.|292.1 +/- 2.9 Ma (Rosenbaum et al., 2012).|Eastlake Suite.||Intrudes the Sandon Association. Is 'intimately associated with' or abuts Shallow Lagoon Monzogranite and The Knobs Tonalite (Woodburn Complex: possibly intruded contemporaneously).|Plagioclase-rich biotite monzogranite; amphibole-bearing variants; weakly to moderately deformed.|
36472|Eastwood Granite|23550|4|Described|p504|||Fig 1 p502 and p509. of Wangrah Suite. Lachlan Fold Belt Province.||||||
36472|Eastwood Granite|71206|6|Mentioned|p373, 377|||Lachlan Fold Belt.||Wangrah Suite.|||Aluminous A-type granite.|
69441|Echo Hills Formation|68005|5|Briefly described|p35, p154.|Early Permian|Early Permian|||Unit in Manning Group.|||Siltstone and sandstone, coarse conglomerates and interbedded shales.|
69441|Echo Hills Formation|73202|4|Described|p625-626, p628-p634, p636-637, p639-640|Early Permian|Late Carboniferous|New England Orogen, southern. Described and mappd by Blair (1983). Deposited in a small transtensional strike-slip basin along the Monkey Creek Fault. Steeply dipping ~1700 m thick sequence, rapidly and episodically deposited with normal and reverse grading beds during initial basin formation. Overall transition from a steep-sided deep marine basin to a shallow marine or terrestrial basin. Sandstone facies are dominated by siliceous to dacitic volcanic rock fragments. Sandstone dykes suggest deformation or seismic events when the sediments were unlithified. Early Permian rhyolites erupted in the upper section of the formation (Ramleh Volcanics), constrains minimum age of deposition.|295.6 +/- 4.6 Ma U-Pb SHRIMP|Manning Group|Ramleh Volcanics|Interbedded with Ramleh Volcanics.|Diamictites and poorly sorted mass-flow deposits, clasts include locally sourced green chert and argillite. Individual channel-fill packages locally grade from diamictites and conglomerates into sandstones and siltstones.|
72984|Edgeworth tuff|62033|5|Briefly described|p25 (Table)|||Of Adamstown Formation (Newcastle Coal Measures). Overlain by Wave Hill seam; overlies Fern Valley seam. Geological Province: Sydney Basin. Informal name.||||||04-FEB-08
29505|Edinboro Formation|22857|5|Briefly described|p490 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Canangle Subgroup (Catombal Group). Fine-grained arenite and red mudstone. Max. thickness: 166m. Geological Province: Hervey Basin.||||||10-MAR-06
29505|Edinboro Formation|23214|3|Fully described|p237|Late Devonian|Late Devonian|Of Canangle Subgroup. Formerly part of the now superseded Columbine Sandstone. Dominantly red mudstone. Geological Province: Lambie Basin. Underlying unit: Macquarie Park Sandstone, overlying unit: Carlton Formation. Max. thickness: 166m.||||||17-JUL-08
29505|Edinboro Formation|43640|5|Briefly described|Map Legend||Devonian|||||||
29505|Edinboro Formation|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Catombal Group, Canangle Subgroup. Consists of red mudstone, fine quartzose sandstone, red to grey-green calcareous gritstone.||||||17-JUL-08
29505|Edinboro Formation|43782|6|Mentioned|map diagram|Famennian|Famennian|Of Canangle Subgroup, of Catombal Group.||||||17-JUL-08
26532|Edinglassie Coal Member|29942|4|Described|Fig.1|||Permian||||||
26532|Edinglassie Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26532|Edinglassie Coal Member|68004|6|Mentioned|p51 Table 5.|Late Permian|Late Permian|||||||
39340|Edithvale Formation|61964|3|Fully described|p14 Fig. 4, p134|Famennian|Frasnian|Of Cocoparra Group. Contains high proportion of polymictic paraconglomerates + sporadic polymictic orthoconglomerates; no fossils.Conformably overlies Hazeldene Sandstone; and the Barrat Formation in the Narriah Syncline. Thickness: >200m.See also p115.||||||14-OCT-08
39340|Edithvale Formation|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Poorly sorted pebbly sandstone, polymictic conglomerate, lithic sandstone, sandstone and siltstone; planar and trough corss bedded.||||||25-MAR-08
39340|Edithvale Formation|69160|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|||Poorly sorted pebbly sandstone, polymictic conglomerate, lithic sandstone, sandstone and siltstone, planar and trough cross-bedded.|
24260|Ednas Gneiss|6823|6|Mentioned|p205|Palaeoproterozoic|Palaeoproterozoic|||||Underlies the Thackaringa Group.||26-MAR-22
24260|Ednas Gneiss|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
24260|Ednas Gneiss|22771|6|Mentioned|Table12.2p45|||||||||
24260|Ednas Gneiss|22857|5|Briefly described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: ~1km. Geological Province: Willyama Fold Belt.||||||07-NOV-08
24260|Ednas Gneiss|22884|6|Mentioned|p41, p43 Fig. 3|||Correlates with similar George Mine Formation. Geological province: Broken Hill Domain.||||||26-MAR-09
24260|Ednas Gneiss|22965|6|Mentioned|Fig 1||Statherian|||||||
24260|Ednas Gneiss|23248|5|Briefly described|Fig2p169|||||||||
24260|Ednas Gneiss|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Rocks are leucocratic, high in silica and are usually albitic. Age: ~1710Ma. Geological Province: Broken Hill Domain.||||||07-FEB-11
24260|Ednas Gneiss|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|||||||
24260|Ednas Gneiss|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24260|Ednas Gneiss|42537|6|Mentioned|Fig.2 P5|||||||||
24260|Ednas Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
24260|Ednas Gneiss|42897|2|Defined|p333|Proterozoic||see also Fig.3, p321.||||||29-MAY-07
24260|Ednas Gneiss|43052|6|Mentioned|Fig.4.22|||||||||
24260|Ednas Gneiss|43086|6|Mentioned|Fig.3|||||||||
24260|Ednas Gneiss|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
24260|Ednas Gneiss|43267|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
24260|Ednas Gneiss|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
24260|Ednas Gneiss|43572|6|Mentioned|p5|||||||||
24260|Ednas Gneiss|46598|5|Briefly described|p302|||||||||
24260|Ednas Gneiss|50045|5|Briefly described|p116 Fig. 3|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Mulculca Formation; underlain by Redan Gneiss.||||||31-MAY-07
24260|Ednas Gneiss|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Redan Suite. Geological Province: Broken Hill Block.||||||07-NOV-08
24260|Ednas Gneiss|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.  Geological Province: Broken Hill Block.||||||07-NOV-08
24260|Ednas Gneiss|60485|5|Briefly described|p28 Fig. 2|||Of theThackaringa Group? Geological Province: Broken Hill Domain.||||||03-MAR-05
24260|Ednas Gneiss|61606|5|Briefly described|p4 Fig.2|||||||||
24260|Ednas Gneiss|61735|5|Briefly described|p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Part of the Redan Block. See also p636 Fig. 2.||||||04-JUN-15
24260|Ednas Gneiss|62536|6|Mentioned|p635-636|||Redan Block, Broken Hill area.||||||
24260|Ednas Gneiss|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
24260|Ednas Gneiss|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||||||19-DEC-21
24260|Ednas Gneiss|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
24260|Ednas Gneiss|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24260|Ednas Gneiss|63519|5|Briefly described|p10 Fig. 3|||Geological Province: Redan Sub-block.||||||11-JUN-08
24260|Ednas Gneiss|63866|5|Briefly described|p36|||Redan Subdomain of the Broken Hill Domain, Curnamona Province. Mistakenly referred to as the Ednas Formation on p36.||Willyama Supergroup||Overlies the Redan Gneiss.||
24260|Ednas Gneiss|64097|5|Briefly described|p304 Fig. 1, p309|Paleoproterozoic|Paleoproterozoic|Of the new Rantyga Group (equivalent rocks in the Redan geophysical zone to the Lady Brassey unit). Very poor outcropping.||||||07-FEB-11
24260|Ednas Gneiss|64316|5|Briefly described|p532, p533 Fig. 1|||Part of the amphibole-quartz-albite-magnetite Redan geophysical Zone forming a magnetic high regionally.  Geological Province: Broken Hill Block.||||||07-FEB-11
24260|Ednas Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Rantyga Group. Geological province: Broken Hill Domain.||||||07-FEB-11
24260|Ednas Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||07-FEB-11
24260|Ednas Gneiss|66302|5|Briefly described|p36 Fig.9, p39, p41|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Incorrectly referred to as the Ednas Formation on p41.||Rantyga Group||Overlies the Redan Gneiss. Overlain by Mulculca Formation.||
24260|Ednas Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.||Of Rantyga Group.||||
24260|Ednas Gneiss|70000|6|Mentioned|p34|Statherian|Statherian|||Unit in Rantyga Group.||||
24260|Ednas Gneiss|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.||Overlies Redan Gneiss. Is overlain by Mulculca Formation.|Quartz-albite-magnetite gneiss, sodic plagioclase-quartz-magnetite rock, minor albite-hornblende-quartz rock, minor quartzo-feldspathic composite gneiss.|
24260|Ednas Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Rantyga Group.||Overlies Redan Gneiss.|Albite-quartz +/- magnetite rock. Magnetite layers (up to 10s cm thick) impart a gneissic texture.|
24260|Ednas Gneiss|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|~1710 Ma|Rantyga Group||Overlies Redan Gneiss. Underlies Mulculca Formation.||
24260|Ednas Gneiss|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
24260|Ednas Gneiss|72461|5|Briefly described|p16 fig 9|||Redan sub-block of the Broken Hill Block.||Rantyga Group||Overlies the Redan Gneiss. Overlain by the Mulculca Formation.||
24260|Ednas Gneiss|73243|6|Mentioned|p53 Fig.2|||||||||
24260|Ednas Gneiss|73482|6|Mentioned|p422 Fig.3|||Redan sub-block.||Rantyga Group||||
24260|Ednas Gneiss|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|||Redan Geophysical Zone.||Rantyga Group||||
24944|Edols Conglomerate|22797|5|Briefly described|P838|||Parent is the Derriwong Group||||||
24944|Edols Conglomerate|22831|3|Fully described|p 43|Pridolian|Pridolian|Of the Derriwong Group.||||||27-OCT-08
24944|Edols Conglomerate|22857|4|Described|p450 App.1, Tb.A1.6|Silurian||Of the Derriwong Group. Mass-flow polymictic conglomerate and massive to planar-bedded medium-grained arenite. Max. thickness: ~50m. Geological Province: Bogan Gate Terrace.||||||
24944|Edols Conglomerate|23522|5|Briefly described|p253|Devonian|Devonian|||||||
24944|Edols Conglomerate|24417|3|Fully described|p67|Pridoli|Ludlow|Of Derriwong Group.  Previously named "Edols Sandstone".  Overlain by Cookeys Plains Formation. Maximum thickness: 200m.||||||
24944|Edols Conglomerate|36066|5|Briefly described|p9|||This is correct spelling of Edol.||||||
24944|Edols Conglomerate|40365|6|Mentioned|p240|||||||||
24944|Edols Conglomerate|42449|5|Briefly described|p12|||||||||
24944|Edols Conglomerate|43441|5|Briefly described|27|Early Devonian|Late Silurian|||||||08-JAN-10
24944|Edols Conglomerate|44160|5|Briefly described|Map Legend||Pridolian|||||||08-JAN-10
24944|Edols Conglomerate|50299|5|Briefly described|Map Legend|Devonian|Silurian|Of the Derriwong Group.||||||
24944|Edols Conglomerate|50385|5|Briefly described|Map Legend|Devonian|Silurian|Of Derriwong Group. Polymict conglomerate and massive medium-grained quartz and lithic sandstone||||||11-JUN-04
24944|Edols Conglomerate|50554|5|Briefly described|Map legend|Devonian|Silurian|Of the Derriwong Group.  Red-purple and cream polymictic conglomerate and massive to planar bedded  medium-grained sandstone, siltstone.  Overlies the Lake Cowal Volcanic Complex.||||||21-JUN-04
24944|Edols Conglomerate|60009|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Derriwong Group.  Underlies: Cookeys Plains Formation.||||||13-JUL-04
24944|Edols Conglomerate|60548|5|Briefly described|map legend|Devonian|Silurian|Of Derriwong Group.  Polymict conglomerate.||||||
24944|Edols Conglomerate|61894|6|Mentioned|p179 Fig.3|||||||||
24944|Edols Conglomerate|61964|6|Mentioned|p95|||Formerly considered to include the rocks now known as Manna Conglomerate (of the Ootha Group) by Scott (in Lyons and Wallace 1999).||||||27-OCT-08
24944|Edols Conglomerate|63290|6|Mentioned|p391, p395|Pridoli|Pridoli|Of Derriwong Group.||||||
79401|Edwardstown Tonalite|71708|3|Fully described|p336 Fig 1, p345-349, p355 App.1|Late Cambrian|Late Cambrian|New  name. U/Pb SHRIMP age on zircons.Previously described as unnamed dioritic body in Tumut 1:100 000 map sheet.  Occurs within a sandstone/siltstone matrix. Crops out over 500m2 within the Jackalass Slate, Tumut Trough. Previously considered to intrude Jackalass Slate. Now considered to be an allochthonous block. Sm-Nd and Hf isotopes discussed. Pre-dates the Macquarie Volcanic Province. Province: Eastern Lachlan Orogen. Name is derived from the historic parish of Edwardstown, south of Gundagai. Exposed in a cutting along Gocup road 1.5km north of the junction with Edwardstown.|501.2 +/- 2.6 Ma U-Pb [SHRIMP] magmatic age|||Nature of contact with Jackalass Slate is unknown; both units deeply weathered where observed.|Deeply weathered, medium grained, greeny grey, quartz bearing tonalite. Euhedral/subhedral sericitised feldspar (65-70 vol%), patchy carbonate alteration,	quartz (15-20 vol%). Minor altered ferromag. minerals; accessory apatite.|31-MAR-20
79401|Edwardstown Tonalite|73483|6|Mentioned|p415|Cambrian|Cambrian||501.2+/-2.6 Ma magmatic zircons|||||
34598|Efflux Siltstone Member|5253|6|Mentioned|p97|Devonian|Early Ludlow|Member of Frome Hill Formation. Equivalent to Upper Shale of Carr et al. 1990||||||
34598|Efflux Siltstone Member|22842|5|Briefly described|p29|Early Devonian|Late Silurian|||||||16-JAN-12
34598|Efflux Siltstone Member|68592|5|Briefly described|p898, p915-6, p1892|||Wollongong 1:250 000 map area. A unit in Frome Hill Formation of Bauer (1994).||Unit in Frome Hill Formation.||Locally overlies Folly Point Limestone Member.|Siliciclastic succession of siltstone, shale and minor medium-grained fossiliferous sandstone.|
34598|Efflux Siltstone Member|70661|3|Fully described|p31 tbl 1, p46-p48|Lochkovian|Pridoli|Name derived from "the Efflux" spring. Was informally referred to as upper shale of Bungonia Limestone previously. Up to 170m thick. Gently westerly dipping.Age based on fossil assemblage. Fossil assemblage, structure and metamorphism discussed.||Frome Hill Formation||Conformably overlies Folly Point Limestone Member, partly overlain  by  Sawtooth Ridge Limestone Member, Tangerang Formation|Poorly bedded, calcareous siliceous and sandy shale, siltstone chert and very fine grained sandstone.|
34598|Efflux Siltstone Member|71303|5|Briefly described|map legend|Lochkovian|Pridoli|||Of Frome Hill Formation.|||Poorly bedded calcareous, siliceous and sandy shale, siltstone, chert and very fine-grained sandstone. Fossiliferous sandstone grading to shale and white crinoidal mudstone locally.|
34598|Efflux Siltstone Member|71656|6|Mentioned|p31|Lochkovian|Pridoli|A new genus of ostracode, Bungonibeyrichia, from upper shale unit of Bungonia Limestone (of Copeland , 1981) is suggested as being from this unit.||Frome Hill Formation||Overlies Folley Point Limestone Member.|Fossiliferous siltstone.|
35104|Eight Foot Six Inch Bed|23055|6|Mentioned|p24,Fig13p25|||||||||
24945|Eight Mile Creek beds|39252|6|Mentioned|p22|||||||||
24945|Eight Mile Creek beds|43008|5|Briefly described|map legend|||||||||
24945|Eight Mile Creek beds|61392|5|Briefly described|p164 Fig. 1|Late Permian|Middle Permian|Of the Wildash Group.||||||07-FEB-11
24945|Eight Mile Creek beds|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Intermediate to acid lava, tuff and agglomerate. Conglomerate, well sorted to pebbly lithic arenite, siltstone and mudstone; richly fossilierous. Basaltic and andesitic to dacitic lava.||||||13-DEC-07
24945|Eight Mile Creek beds|63748|4|Described|p7 Fig. 3, p8, p19|Early Permian|Early Permian|Olgers et al (1974); now incl. some former Connolly Volcanics rocks (Van Noord 1999b). Conformable on Bromley Hills Fm along its northern border; unconformable on Silverwood Gp and Wallaby beds; unconformable below Marburg Subgroup. Detailed lithology.||||||07-FEB-11
24945|Eight Mile Creek beds|68679|5|Briefly described|p446-447, p452|Permian|Permian|Olgers et al. (1974); Dennis (1974). Extended by Van Noord (1999) to include parts of the Connolly Volcanics. Silver Spur Subprovince, Woolomin Province. Occurs 15km S of Warwick in a small, ~8 km2 outlier.||Wildash Group.||Overlies Bromley Hills Formation and (unconformably) the Wallaby beds. Unconformably overlies or is faulted against Silverwood Group. Is overlain unconformably by the Marburg Subgroup.|Mainly sedimentary lower half: conglomerate, pebbly lithic sandstone, well-sorted lithic sandstone, siltstone and mudstone; a rich early Permian marine fauna. The upper half comprises felsic to intermediate volcaniclastic rocks and lavas.|
83204|El Capitan Leucitite|73581|6|Mentioned|p26|||Paleomagnetism indicates lavas crystallised during a magnetic reversal.||||||
75831|Elby Glen Station serpentinite|65317|6|Mentioned|p631-632, p622 Fig. 1c, p635 Fig. 14|Early Permian|Late Carboniferous|Appears to be an informal name. Located within western margin of Nthn Hastings Block, New England Orogen.  Structures suggest Early Permian emplacement. Shown as Elby Glen Station Serpentinite in figs.||||||23-APR-12
25893|Ellenden Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Pink Granite. BMR map symbol: gil.||||||
25893|Ellenden Granite|24116|5|Briefly described|p104|Devonian|Devonian|||||||
25893|Ellenden Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
25893|Ellenden Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
25893|Ellenden Granite|30735|2|Defined|p39|Devonian|Devonian|||||||
25893|Ellenden Granite|30736|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25893|Ellenden Granite|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
25893|Ellenden Granite|33325|6|Mentioned|p19|||||||||
25893|Ellenden Granite|42726|5|Briefly described|Map legend|Silurian||||||||
25893|Ellenden Granite|42727|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Bega Batholith. Adamellite; I-type. BMR map symbol: Dge. Geol. Prov: Rocky Pic Block.||||||
25893|Ellenden Granite|42820|3|Fully described|p72|||Early Devonian age||||||
25893|Ellenden Granite|66300|5|Briefly described|p21, p23, p27. |Silurian|Silurian|Age is indistinguishable from the Woodlawn Volcanics and the leucogranite phase of the Lockhart Igneous Complex. Shallow-level intrusions.|423.4 +/- 3.3 Ma.|||||
25893|Ellenden Granite|67125|6|Mentioned|Slide 29.|Early Devonian|Early Devonian||c.370 Ma.|||Intrudes Pittmann Formation.||
25893|Ellenden Granite|68592|6|Mentioned|p24, p1567|||East of Lake George. May be a southern continuation of Wologorong Granite.||||||
25893|Ellenden Granite|69159|5|Briefly described|Map legend|Silurian|Silurian|Two un-names sub-units are separately mapped, including a leucocratic, medium-grained, equigranular granite with high K, Th and U radioelement response.||Unit in Thurralilly Suite.|||Leucocratic, medium-grained, equigranular, biotite+/-muscovite granite with a marginal phase of fine- to medium-grained, leucocratic, porphyritic, granite and microgranite.|
25893|Ellenden Granite|69270|6|Mentioned|p1|Late Silurian|Late Silurian|Dating: zircon U-Pb by SHRIMP, Bodorkos and Simpson (2008).|~423 Ma, magmatic crystallisation age|||||
25893|Ellenden Granite|71069|3|Fully described|p21 fig 7, p28, p38 fig 15, p40 fig 17|Ludlow|Wenlock|Named for the Ellenden Trigonometrical Station. Previously an unnamed granite within the Ellenden Suite. Contains two unnamed sub-units whose lithology is described on p190. Representatitve localities mentioned. Chemically equivalent to the extrusive Woodlawn Volcanics. Age derived from SHRIMP U-Pb, Bodorkos and Simpson, 2008.  Intruded in the Goulburn Basin as part of a larger magmatic system.  Distribution, geomorphology, geochemistry, geophysical characteristics, tectonic structure, primary structures/textures and metamorphism discussed. The granite is quarried for road materials. See also p41, p55 fig 20, p153, p174-p179, p181, p182, p185, p189-193.|423.4 +/- 3.3 Ma |Thurralilly Suite||Intrudes the Bendoc and Margules Groups. Part equivalent to the Lockhart Igneous Complex.Equivalent to the Gibraltar Granite, Butmaroo Granite, Gourock Granodiorite and Tallaganda Granodiorite.|White to cream, leucocratic,  fine to medium-grained, equigranular to porphyritic, biotite granite and microgranite. Fine grained mafic enclaves are present in places.|
25893|Ellenden Granite|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Thurralilly Suite.|||Leucocratic, fine- medium- to coarse-grained, equigranular, biotite +/- muscovite granite with a marginal phase of fine- to medium-grained, leucocratic, porphyritic granite and microgranite.|
25893|Ellenden Granite|71699|5|Briefly described|Map legend.|Silurian|Silurian|||Thurralilly Suite.|||Leucocratic, medium-grained, equigranular, biotite+/-muscovite granite with a marginal phase of fine- to medium-grained, leucocratic, porphyritic granite and microgranite.|
25893|Ellenden Granite|71700|3|Fully described|vi, viii, p7, p12, p17, CD|Pridoli|Ludlow|Named for the Ellenden Trigonometrical Station. A representative locality is given along the Bungendore-Tarago road about 10km northeast of Bungendore. This unit was previously assigned to an "Ellenden Suite" by Chappell et al. (1991) before being reassigned to the Thurralilly Suite. This unit is the only one in which economic activity occurs in the Thurralilly Suite. This unit includes two unnamed members; a granite phase and microgranite dykes and small intrusions. Distribution, geomorphic expression, outcrop, structure, metamorphism, geochemistry, geophysical charateristics, distinguishing features and economic geology are discussed. See also p45, p48, p50, p52, p63, p65, p71, p77, p81, p83-p84.|423.4 +/- 3.3 Ma (Bodorkos & Simpson 2008)|Thurralilly Suite||Intrudes the Adaminaby, Bendoc and Margules groups. (potentially) Equivalent to the Gibraltar Adamellite. Equivalent to the Butmaroo Granite.|Leucocratic, medium-grained, equigranular granite which features a porphyritic phase at its margins.|
31573|Ellenden Suite|42726|5|Briefly described|map legend||Silurian|||||||
31573|Ellenden Suite|44093|5|Briefly described|p203 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||07-MAR-05
31573|Ellenden Suite|71069|6|Mentioned|p174|||Obsolete, replaced by the Thurralilly Suite.||||||
32393|Ellersley Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Hyandra Creek Complex.||||||
32393|Ellersley Formation|23170|2|Defined|p208|Early Devonian|Early Devonian|of Hyandra Creek Group.||||||
32393|Ellersley Formation|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hyandra Creek Group.  Trachylatite.||||||
32393|Ellersley Formation|68003|5|Briefly described|p24 Fig.3-e, p143. |Lochkovian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Hyandra Group.|||Trachylatite.|
31635|Ellerslie Suite|42726|5|Briefly described|map legend||Silurian|||||||
31635|Ellerslie Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
26537|Elmside Formation|13996|6|Mentioned|p130, p137, p142|Lochkovian|Pridoli|Yass area. Previously the Upper Trilobite Bed. Contains latest Pridoli to Early Devonian Icriodus conodonts with North American affinity. Conulariid species listed. Bivalve taxa distribution Table.||||||
26537|Elmside Formation|22857|4|Described|p458 App.1, Tb.A1.6|Late Silurian|Late Silurian|Of the Barambogie Group. Sandstone. Mudstone, algal limestone; contains brachiopods, molluscs, stromatoporoids, corals, sponges, conodonts. Max. thickness: >62m. Geological Province: Canberra-Yass Shelf. ||||||
26537|Elmside Formation|23522|5|Briefly described|p248 Fig 4|Lochkovian|Pridoli|||||||
26537|Elmside Formation|24248|5|Briefly described|p52, p50 Fig.1|Lochkovian|Pridoli|Unconformably overlain by the Black Range Group. Overlies the Cowridge Siltstone.||||||
26537|Elmside Formation|24249|5|Briefly described|p90 Fig.3, p93|Pridoli|Pridoli|Underlain by Cowridge Siltstone.||||||12-JUN-08
26537|Elmside Formation|30069|5|Briefly described|p5|||||||||
26537|Elmside Formation|31852|5|Briefly described|p711|||See also P714,715,718,719. L.Dev.||||||
26537|Elmside Formation|32624|6|Mentioned|p724|||Coral species||||||
26537|Elmside Formation|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Nomenclature||||||
26537|Elmside Formation|33116|6|Mentioned|Fig.11|||Correlation||||||
26537|Elmside Formation|33325|5|Briefly described|Table 2|||||||||
26537|Elmside Formation|33326|6|Mentioned|p441|||Lochkovian. Fauna.||||||
26537|Elmside Formation|33732|6|Mentioned|p112|||||||||
26537|Elmside Formation|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26537|Elmside Formation|35386|3|Fully described|p39|||||||||
26537|Elmside Formation|35501|6|Mentioned|p156|||||||||
26537|Elmside Formation|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
26537|Elmside Formation|36775|6|Mentioned|p361|||||||||
26537|Elmside Formation|37727|4|Described|p57|||See also p8 and p31.||||||12-JUN-08
26537|Elmside Formation|38151|6|Mentioned|Table 1|||||||||
26537|Elmside Formation|38378|6|Mentioned|p134|||||||||
26537|Elmside Formation|38691|5|Briefly described|p167|||||||||
26537|Elmside Formation|39331|6|Mentioned|p46|||See Fig.5-4,5-5||||||
26537|Elmside Formation|40328|3|Fully described|p49|||||||||
26537|Elmside Formation|42015|6|Mentioned|p318|||||||||
26537|Elmside Formation|42029|5|Briefly described|Fig.1 P96|||||||||
26537|Elmside Formation|42032|6|Mentioned|p485|||||||||
26537|Elmside Formation|42033|6|Mentioned|p650|||||||||
26537|Elmside Formation|45075|5|Briefly described|p8|||Fauna||||||
26537|Elmside Formation|50230|5|Briefly described|Map legend|Lochkovian|Lochkovian|Of the Hattons Corner Group.  Medium- to thin-bedded quartz-lithic sandstone, mudstone.||||||
26537|Elmside Formation|60332|6|Mentioned|p937|Devonian|Silurian|||||||
26537|Elmside Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hattons Corner Group. Medium- to thin-bedded quartz-lithic sandstone, mudstone; algal limestone lenses in mudstone occur.||||||12-JUN-08
26537|Elmside Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Taemas. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26537|Elmside Formation|67820|6|Mentioned|p136 Fig.3|Devonian|Silurian|||Hattons Corner Group.||||
26537|Elmside Formation|68592|2|Defined|p559-61, p563, p602-6, p940-1, p1884-6|Lochkovian|Pridoli|See also p430 Fig.89. Named after former Elmside homestead. Link (1970, 1971); Link and Druce (1972); unit in their Barambogie Group. The upper part was formerly known as the Upper Trilobite Bed. Here included in redefined Hattons Corner Group. "Incomplete" type section, and other good exposures, described. 62-85m thick. Diverse fossil fauna listed, including the recently described, earliest-known holothurian body fossil Porosothyone picketti (Jell, 2010).||Unit in Hattons Corner Group.||Gradationally overlies Cowridge Siltstone. Is overlain unconformably by Sharpeningstone Conglomerate.|Basal fine- to coarse-grained, graded, lithic sandstone sequence gradationally overlain by a grey, laminated mudstone sequence containing rare, thin beds of graded lithic sandstone; mudstone sequence contains several massive, algal limestone lenses.|
26537|Elmside Formation|70192|5|Briefly described|Map Legend|Lochkovian|Pridoli|She. Includes one unnamed member of algal limestone. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hattons Corner Group|Includes one unnamed member.|Overlies Cowridge Siltstone.|Fine-coarse grained, graded lithic sandstone and laminated mudstone with rare, thin beds pf graded, lithic sandstone; minor massive, algal limestone.|
26537|Elmside Formation|70540|5|Briefly described|Map Legend|Devonian|Silurian|Includes one unnamed member of algal limestone.||Hattons Corner Group|Includes one unnamed member||Fine-coarse grained, graded lithic sandstone and laminated mudstone with rare, thin beds pf graded, lithic sandstone; minor massive, algal limestone.|
26537|Elmside Formation|70546|5|Briefly described|Map Legend|Devonian|Silurian|||Hattons Corner Group|||Fine to coarse grained, graded, lithic sandstone and laminated mudstone with rare, thin beds of graded lithic sandstone. Minor massive algal limestone.|
26537|Elmside Formation|71040|5|Briefly described|p5|Lochkovian|Pridoli|Associated with the Bowning (=Bindian) Orogeny.||||Is overlain unconformably by Sharpeningstone Conglomerate.||
26537|Elmside Formation|71656|4|Described|p12 Fig.2, p27|Lochkovian|Pridoli|Fossils of primitive plants, graptolites, brachiopods, bivalves, echinoderms, holothurian bodies, nautiloids, conodonts, trilobites, stromatoporpoids and corals have been identified in this formation. Includes the 'Upper Trilobite Bed' of earlier workers e.g. Fletcher 1938, 1946).||Hattons Corner Group||Hattons Corner Group. Partially overlies Cowridge Siltstone.|Fossiliferous mudstone.|
26537|Elmside Formation|73143|6|Mentioned|p8-9|Lochkovian|Lochkovian|Contains Cypricriodus hesperius conodonts previously reported as Caudicriodus woschmidti (Link and Druce, 1972), re-identified by Klapper and Johnson (1980) and by Drygant (2010), indicates earliest Lochkovian age. Lochkovian age rugose corals in upper part.|||||Includes limestone lenses.|
26537|Elmside Formation|73215|5|Briefly described|p995|Early Devonian|Early Devonian|||Topmost Hattons Corner Group.||Is overlain by Black Range Group.||
70482|Elmswood Ignimbrite Member|62095|2|Defined|p281 Appdx.|Early Carboniferous|Early Carboniferous|Of the Seaham Formation. Slightly welded, grey to purple ignimbrite in lower section; upper part is unwelded, beige to brown and of finer composition.Age: 326.4+/-2.6Ma. Thickness: 15m. Geol.Prov: Rouchel block, Tamworth Belt. See also Plate 1, p265.||||||25-MAY-06
70482|Elmswood Ignimbrite Member|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Seaham Formation||||
82442|Elsmore Leucomonzogranite|71628|3|Fully described|p19: 30, 32-37, 43, 78, 158, 169|||Nicholson (1965). Name is derived from the village of Elsmore, and the unit comprises two small outcrops to the S and SE, interpreted to be parts of a c.6 x 2.5 km body. Type locality is GR 37409820 to GR 38059780 along the Silver Mines Road. Lithology, mineralogy and geochemistry detailed. Hosts several lode cassiterite deposits (named), variably associated with Ag, W, Mo, Au, Cu, Pb and Zn. Has been mined for quartz crystals, monazite and kaolin.|250.3 +/- 1.8 Ma (SHRIMP: Cross and Blevin, 2013).|Elsmore Suite.||Intrudes Texas and Sandon beds.|White, medium- to coarse-grained, seriate to porphyritic leucomonzogranite to leucosyenogranite, with extensive greisenisation and silicification in parts. Pervasively altered. I-type.|
72759|Elura Limestone|61907|6|Mentioned|p143|||||||||
82205|Elura Limestone Member|73143|4|Described|p1-7, p9, p11, p14, p17-20|Lochkovian|Lochkovian|Lachlan Orogen. Cobar Superbasin, northern. Restricted to the northeast side of the Elura Thrust Fault Zone, Endeavor Mine District. The unit is 50-70m wide and 700m long, maximum vertical thickness over 500m. Represents a carbonate reef submerged and buried beneath turbidites during a regional transgressive event. Ten conodont species identified, Caudicriodus woschmidti and Cypricriodus hesperius from middle part of the unit are age diagnostic for the Cy. hesperius Biozone, early Lochkovian. Three rugose coral species identified including Nardophyllum karpinskiense. Six tabulate coral species identified. Subject to moderate-intense recrystallisation. Host to part of the Endeavor sulfide deposit. Drillcore section NP1047 nominated as type section.||Brookong Formation||Conformably underlies CSA Siltstone, interfingers with Brookong Formation.|Limestone with minor intercalated dark grey calcareous mudstone of reefal, back-reefal and outer-shelf facies; dominated by rudstone, boundstone, packstone and floatstone with minor grainstone. Contains rugose and tabulate corals and conodonts.|
77013|Emerald Beach Monzogranite|69639|4|Described|p3, p6, p8, p118, p128|Triassic|Triassic|New England Orogen. Sample locality, petrography, and geochronology is described. This is the most easterly granite on the Australian mainland. See also p139-p145, p223-p224, p237.|228.5 +/- 1.5 Ma (SHRIMP U-Pb)|||Intrudes the Coramba Formation. Overlain by the Bundamba Group.||
77013|Emerald Beach Monzogranite|71628|3|Fully described|p17: 2, 54, 92-94|||Chisholm et al. (2014), after unpublished work by Chappell and Bryant (1994). Previously Emerald Beach Adamellite. Named after a local beach. Occurs on the Solitary Islands and a small intrusion on a headland between Bare Bluff and Signal Hill; this latter location (at GR 63112630, Coffs Harbour 1:250,000) is the type locality (Korsch, 1978). Geochemistry described and discussed. Unaffiliated. Is associated with minor pyrite-Au mineralisation.|228.5 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|||Intrudes Coramba Beds.|Medium-grained, sparsely to strongly porphyritic, biotite monzogranite. Described in detail. I-type (discussed).|
73372|Emohruo Granite|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Westella Suite.|||Grey, fine- to medium-grained biotite granite/granodiorite with mafic enclaves/xenoliths, mylonitic.|
73372|Emohruo Granite|70602|6|Mentioned|p67 Fig 3|Early Devonian|Silurian|Age inferred from Byrock Granite.||Westella Suite||||
73372|Emohruo Granite|70941|3|Fully described|pviii-px, p9, p11 fig 6|Early Devonian|Late Silurian|Named for the Emohruo crutching shed. I type granite containing mafic enclaves.Distribution, geomorphology, structure, metamorphism, geochemistry, geophysical and distinguishing characteristics discussed. Type area named by not described. Intrudes Girilambone Group basement. Crystallisation age. See also p58 fig 23, p59,  p70-73, p140, p145, p149.|416.7 +/- 3.4 Ma (SHRIMP U/Pb)|Westella Suite||Intrudes Girilambone Group, equivalent to the Pendianna Tank and Byrock Granites|Fine to medium grained, equigranular biotite granite that is strongly foliated to mylonitic. Numerous fine grained, dark enclaves that are up to 10cm are present throughout the granite.|
73372|Emohruo Granite|71345|6|Mentioned|p30|||||||||
73372|Emohruo Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: very small non-magnetic unit with boundaries based on geological mapping. Minor radioelement high.|416.7 +/- 3.4 Ma.|Westella Suite.|||Fine- to medium-grained biotite granite/granodiorite with mafic xenoliths, strongly foliated to mylonitic.|
24953|Emu Hollow Dacite|34895|6|Mentioned|Fig.1|||||||||
24953|Emu Hollow Dacite|35412|6|Mentioned|p40|||||||||
24953|Emu Hollow Dacite|70684|5|Briefly described|p30|||5km S of Copper Hill, Molong area. Hornblende K-Ar age.|449 +/- 4 Ma (Chivas in Scott, 1978).|||||
41056|Enmore Monzogranite|24366|5|Briefly described|p8 Fig. 6|Early Permian|Early Permian|Of the Hillgrove Plutonic Suite.||||||
41056|Enmore Monzogranite|71628|4|Described|p2: 14-15, 24, 60; p3: 1, 4, 10, 35-39|||Brown (2003); originally Enmore Adamellite (Binns et al., 1967). Named after the locality of Enmore. A large (~18 x 4-5 km) pluton cropping out 25 km SE of Uralla and 30 km SSE of Armidale. Geochemistry described in some detail. Associated (via major shear zones, not genetically) with historically significant Au-Sb-W vein mineralisation.||Enmore Suite.||Intrudes Sandon Association and Girrakool beds. Abuts and is intruded by Barney House Gabbro. Adjacent to, and surrounds, Table Top Diorite; their relationship is ""unconstrained"".|Medium- to coarse-grained, weakly porphyritic to seriate biotite monzogranite; garnet- and orthopyroxene-bearing variants; weakly to strongly foliated.|
41569|Erigolia Granite|60303|5|Briefly described|p6 Fig. 1, p7|Early Silurian|Early Silurian|Geological Province: Lachlan Fold belt.  See also p9 Tb. 1.||||||
41569|Erigolia Granite|61964|3|Fully described|p14 Fig. 4, p41 Tb. 2, p53|Middle Silurian|Early Silurian|Of Koetong Suite (Koetong Supersuite). S-type:coarse- to med.-gr.leucocratic equigranular to sparsely porph.granite with metsed. xenoliths + bitotie-rich microgranular enclaves. Intrudes Clements Fm (Wagga Gp). Ages: ~428.2Ma, 428.0+/-3.4Ma. See also p38||||||
41569|Erigolia Granite|62367|5|Briefly described|p4 Fig. 2|Early Devonian|Silurian|||||||02-JUN-06
41569|Erigolia Granite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Coarse- to medium-grained leucocratic equigranular to sparsely porphyritic granite with metasedimentary xenoliths and biotite-rich microgranular enclaves.||||||10-APR-08
41569|Erigolia Granite|69161|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Koetong Suite.||Intrudes Clements Formation.|Coarse- to fine-grained leucocratic porphyritic granite.|
41569|Erigolia Granite|70296|5|Briefly described|p1, p5, p7-8, p10, p24|Llandovery|Llandovery|Cargelligo district. Includes inherited zircons.|429.2 +/- 3.4 Ma (SHRIMP U-Pb)|Koetong Supersuite|||S-type granite.|21-JAN-21
41569|Erigolia Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Coarse- to medium-grained, leucocratic, equigranular to sparsely porphyritic granite with metasedimentary xenoliths and biotite-rich microgranular enclaves.|
41569|Erigolia Granite|73082|5|Briefly described|p26|||SW West Wyalong district.|||||Heavily greisenised granite with quartz veins in the surrounding hornfels. Source of alluvial Sn in Erigolia and Taleeban.|
25898|Erimeran Granite|9548|5|Briefly described|Map Legend|Silurian|Silurian|Granite, microadamellite, microgranite, porphyry.||||||
25898|Erimeran Granite|22503|5|Briefly described|p643, Fig.1 p642||Late Silurian|See also p650||||||
25898|Erimeran Granite|22768|6|Mentioned|p170,172|||||||||
25898|Erimeran Granite|22857|5|Briefly described|p132, p170, p172|||Of the Cobar Supergroup. Geological Province: Wagga Marginal Basin.||||||
25898|Erimeran Granite|23245|6|Mentioned|p132|||||||||
25898|Erimeran Granite|23454|5|Briefly described|p27 Fig.1|Silurian|Silurian|||||||
25898|Erimeran Granite|29987|4|Described|p14|||||||||
25898|Erimeran Granite|31993|6|Mentioned|p678|||||||||
25898|Erimeran Granite|32087|6|Mentioned|p16|||||||||
25898|Erimeran Granite|32674|5|Briefly described|p31|||||||||
25898|Erimeran Granite|33875|6|Mentioned|p76|||Uranium mineralisation.||||||
25898|Erimeran Granite|34405|6|Mentioned|p126|||||||||
25898|Erimeran Granite|34406|6|Mentioned|p220|||||||||
25898|Erimeran Granite|34449|4|Described|Table 2-1|||U.Silurian - L.Devonian||||||
25898|Erimeran Granite|34469|6|Mentioned|p115|||Table P108. Silurian||||||
25898|Erimeran Granite|34544|6|Mentioned|p187|||||||||
25898|Erimeran Granite|34907|6|Mentioned|p296|||||||||
25898|Erimeran Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
25898|Erimeran Granite|35257|6|Mentioned|p157|||||||||
25898|Erimeran Granite|35287|4|Described|p3|||See also P2.||||||
25898|Erimeran Granite|35385|6|Mentioned|p56|||||||||
25898|Erimeran Granite|38335|6|Mentioned|p1733|||||||||
25898|Erimeran Granite|39064|6|Mentioned|p2|||||||||
25898|Erimeran Granite|39083|6|Mentioned|p30|||||||||
25898|Erimeran Granite|39214|4|Described|p14|||See also Table 11||||||
25898|Erimeran Granite|39618|6|Mentioned|p38|||||||||
25898|Erimeran Granite|39627|4|Described|p264|||||||||
25898|Erimeran Granite|39772|6|Mentioned|p20|||||||||
25898|Erimeran Granite|40328|4|Described|p205|||||||||
25898|Erimeran Granite|41126|6|Mentioned|p24|||||||||
25898|Erimeran Granite|41394|2|Defined|p32|Late Silurian|Middle Silurian|||||||
25898|Erimeran Granite|41395|6|Mentioned|Map legend|Silurian||||||||
25898|Erimeran Granite|41528|2|Defined|p28|Late Silurian|Middle Silurian|||||||
25898|Erimeran Granite|41529|6|Mentioned|Map legend|Middle Silurian||||||||
25898|Erimeran Granite|41821|6|Mentioned|p5 Fig.3|||Occurs in Nymagee, Kilparney, Bobadah, Gindoono sheet areas||||||
25898|Erimeran Granite|42313|6|Mentioned|p35|||||||||
25898|Erimeran Granite|42521|5|Briefly described|p15|||approx 419 Ma||||||
25898|Erimeran Granite|42566|3|Fully described|p34|||||||||
25898|Erimeran Granite|42568|5|Briefly described|Map legend|Late Silurian|Middle Silurian|||||||
25898|Erimeran Granite|42726|5|Briefly described|map legend|Silurian||||||||
25898|Erimeran Granite|42954|6|Mentioned|p68|||||||||
25898|Erimeran Granite|43032|5|Briefly described|Table 1.|||||||||
25898|Erimeran Granite|43089|5|Briefly described|Map Legend|||||||||
25898|Erimeran Granite|43389|14|Not recorded|Map Legend||Silurian|||||||
25898|Erimeran Granite|43479|14|Not recorded|p95||Ordovician|Intrudes Tellebang Group; O/lain by Cobar Group||||||
25898|Erimeran Granite|43757|6|Mentioned|p510|||||||||
25898|Erimeran Granite|45003|14|Not recorded|p22|||||||||
25898|Erimeran Granite|45087|5|Briefly described|p51|||Chemical analyses.||||||
25898|Erimeran Granite|46032|14|Not recorded|p.412||Late Ordovician|Overlain by Cobar Group. post U.Ord.||||||
25898|Erimeran Granite|46900|6|Mentioned|p16|||Refers Pogson & Felton(1977)||||||
25898|Erimeran Granite|46967|6|Mentioned|Fig.4|||||||||
25898|Erimeran Granite|61964|6|Mentioned|p37|||Located north of CARGELLIGO sheet area - appears to be unrelated to Koetong Suite granites. ||||||
25898|Erimeran Granite|65469|6|Mentioned|p144|Silurian|Silurian|Lachlan Orogen.|||||Granite|
25898|Erimeran Granite|67416|6|Mentioned|p84-86|Early Silurian|Early Silurian|Emplaced during the Benambran Orogeny. Younger ages (listed) probably due to Ar loss.|434 +/- 4 Ma (SHRIMP: Isaacs, 2000).|||Is overlain nonconformably by Tarran Volcanics.|S-type.|
25898|Erimeran Granite|69511|5|Briefly described|p23|Late Silurian|Late Silurian|Is texturally and compositionally similar to the Thule Granite.|427.2 +/- 2.4 Ma (Black, 2007).|||||
25898|Erimeran Granite|69801|6|Mentioned|p1, p18, p135|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Age is indistinguishable from nearby Urambie Granodiorite. Provided dates are SHRIMP U-Pb zircon ages and derived from Isaacs (2000) and (Black, 2007) respectively.|434 +/- 4 Ma to 427.1 +/- 2.4 Ma |Nymagee Igneous Complex||In contact with the Urambie Granodiorite but relationship is unknown.|Massive and foliated S-type granite.|
25898|Erimeran Granite|70751|5|Briefly described|p5, p8, p10-p12, p25-p28, p30, p38|Late Silurian|Late Silurian|An additional age of 434 +/- 4 Ma is derived by SHRIMP from Isaacs (2000); However this age was not supported by the present study which gave a date of 424.5 +/- 2.6 Ma (SHRIMP). SHRIMP dates are igneous crystallisation dates. Prospective for Sn-W mineralisation.|427.1 +/- 2.4 (SHRIMP, Black, 2007)|||Intrudes the Break O' Day Amphibolite. Overlain by the Tarran Volcanics.|Medium-grained, S-type granite.|
25898|Erimeran Granite|70828|5|Briefly described|p4-8,10,15,17|Ludlow|Ludlow|Intruded by porphyritic rhyolitic to microgranitic dykes, equivalent to Tarran Volcanics. Occurs to the WNW of Girilambone Group; in contact with Girilambone Group. Field relationships indicate the Erimeran Granite passes stratigraphically below Break O'Day Amphibolite.|424.5+\-2.6 Ma (zircon U-Pb)||||Rhyolite, felsic porphyry, microgranite|
25898|Erimeran Granite|70876|5|Briefly described|p16, p76|Silurian|Silurian|An additional age of 424.5 +/- 2.6 Ma is derived from Downes et al., 2016.|427.1 +/- 2.4 Ma (Black, 2007)|||||
25898|Erimeran Granite|70941|6|Mentioned|p9|||||||||
25898|Erimeran Granite|70950|6|Mentioned|p1030|Late Silurian|Late Silurian|Geological province: Central Lachlan Orogen. Intruded Ordovician basement, and upper Silurian to lowermost Devonian volcano-sedimentary sequences that overlie basement. U-Pb SHRIMP zircon dating indicates late Silurian age.||||||
25898|Erimeran Granite|71039|6|Mentioned|p14, p26|Late Silurian|Late Silurian|||||Intrudes the Mouramba Group.||
25898|Erimeran Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped S-type intrusion.|||||Porphyritic, massive, fine- to coarse-grained cordierite-biotite granite and monzogranite with lesser equigranular medium-grained biotite and muscovite biotite granite. Rhyolite quartz-feldspar porphyry and porphyritic microgranite dykes.|
25898|Erimeran Granite|72080|5|Briefly described|p4, p15|Late Silurian|Late Silurian|Surface exposure and subsurface interpretation shown p15.|424.5 +/- 2.6 Ma (Downes et al, 2016)|||Intrudes the Girilambone Group.|Granite.|07-JAN-22
25898|Erimeran Granite|72908|6|Mentioned|p5|Late Silurian|Late Silurian||~427-419 Ma|||||
25898|Erimeran Granite|72951|5|Briefly described|p1013, 1015-1016|Ludlow|Wenlock|Lachlan Orogen. Albury-Bega Terrane. S-type granite. SHRIMP U-Pb zircon isotope analyses from Black (2007). eHf = -6.9 +/- 0.6, and d18O = 9.39 +/- 0.56.|427.2 +/- 2.4 Ma||||Felsic porphyritic granite.|
25898|Erimeran Granite|72958|6|Mentioned|p5, p11, p46, p61|Pridoli|Ludlow|Part of a series of Silurian basement granites that underlie the Cobar Basin.|424.1 +/- 2.9 Ma|||Part of basement to Cobar Basin.||
25898|Erimeran Granite|73578|6|Mentioned|p1, p50|Pridoli|Homerian|Ages include 427.1 +/- 2.4 Ma (Black, 2007) and 424.5 +/- 2.6 Ma (Downes et al., 2016).|427.1 +/- 2.4 Ma, 424.5 +/- 2.6 Ma||||S-type granite.|
31574|Erimeran Suite|42726|5|Briefly described|map legend||Silurian|||||||
31574|Erimeran Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||07-MAR-05
24958|Erins Vale Formation|22578|6|Mentioned|p391|||||||||
24958|Erins Vale Formation|22857|5|Briefly described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Cumberland Subgroup (Illawarra Coal Measures). Fine to medium-grained bioturbated lithic sandstone. Max. thickness: 100m. Geological Province: Sydney Basin.||||||
24958|Erins Vale Formation|22969|5|Briefly described|p 24, Fig 3.1|||||||||
24958|Erins Vale Formation|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||29-NOV-04
24958|Erins Vale Formation|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Cumberland Subgroup. Geological Province: Sydney Basin.||||||
24958|Erins Vale Formation|24471|4|Described|p29 Fig.2, p32 Fig 4|Late Permian|Late Permian|Overlies Shoalhaven Group. Contains unamed coal. Overlain by Woonona Coal. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Wallis Creek Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
24958|Erins Vale Formation|29900|4|Described|p173|||||||||
24958|Erins Vale Formation|29901|6|Mentioned|p169|||||||||
24958|Erins Vale Formation|30006|4|Described|p8|||||||||
24958|Erins Vale Formation|31128|6|Mentioned|Table 1|||||||||
24958|Erins Vale Formation|31887|5|Briefly described|p5|||||||||
24958|Erins Vale Formation|32618|3|Fully described|p313|||Perm. Strat. table 1. See also P314-319||||||
24958|Erins Vale Formation|32849|6|Mentioned|Table 1|||Permian||||||
24958|Erins Vale Formation|34060|6|Mentioned|p24|||Perm. Table||||||
24958|Erins Vale Formation|34569|6|Mentioned|p9|||Correlates with Dempsey Beds. Permian||||||
24958|Erins Vale Formation|34605|4|Described|p374|||Fig.5.29||||||
24958|Erins Vale Formation|35065|6|Mentioned|p43|||||||||
24958|Erins Vale Formation|35794|6|Mentioned|p256|||||||||
24958|Erins Vale Formation|36042|6|Mentioned|Fig.18|||||||||
24958|Erins Vale Formation|36220|3|Fully described|p40|||See also Table 10 & P38.||||||
24958|Erins Vale Formation|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
24958|Erins Vale Formation|37089|6|Mentioned|p208|||||||||
24958|Erins Vale Formation|38615|6|Mentioned|p25|||||||||
24958|Erins Vale Formation|38656|6|Mentioned|Fig.1.5.14|||P281||||||
24958|Erins Vale Formation|39287|6|Mentioned|p20|||See also P33||||||
24958|Erins Vale Formation|39307|6|Mentioned|p438|||Foraminifera||||||
24958|Erins Vale Formation|39308|5|Briefly described|p514|||See also P515||||||
24958|Erins Vale Formation|39309|4|Described|p123|||See also Table 7.2||||||
24958|Erins Vale Formation|39661|6|Mentioned|p443|||See also Fig.1||||||
24958|Erins Vale Formation|40256|6|Mentioned|p306|||||||||
24958|Erins Vale Formation|40321|6|Mentioned|p19|||||||||
24958|Erins Vale Formation|40330|6|Mentioned|Fig.8|||||||||
24958|Erins Vale Formation|40744|6|Mentioned|Table 1|||||||||
24958|Erins Vale Formation|41514|6|Mentioned|p82|||||||||
24958|Erins Vale Formation|42737|5|Briefly described|map legend|Permian||||||||
24958|Erins Vale Formation|42787|5|Briefly described|p129|||||||||
24958|Erins Vale Formation|42896|3|Fully described|p18, Table 2|||Of Cumberland Subgroup.||||||12-MAR-09
24958|Erins Vale Formation|42925|5|Briefly described|Table 18||Late Permian|||||||
24958|Erins Vale Formation|42948|6|Mentioned|p50|||||||||
24958|Erins Vale Formation|43194|5|Briefly described|p129 Tb. 8.3, p130|Late Permian|Late Permian|Of Illawarra Coal Measures, western Sydney Basin. ||||||
24958|Erins Vale Formation|45090|6|Mentioned|p27|||Relationship of rock units||||||
24958|Erins Vale Formation|60281|5|Briefly described|p61, p63|Late Permian|Late Permian|Delta plain sandstone deposits.  Top is eroded and overlain, disconformably, by the Wilton Formation.  Max. thickness: ~37m.  Numerous hydrocarbon shows have been recorded.  Geological Province: Sydney Basin.||||||27-APR-05
24958|Erins Vale Formation|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Cumberland Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
24958|Erins Vale Formation|61609|6|Mentioned|p240 Tb. 1, p246 Fig. 5|Permian|Permian|Of Cumberland Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
24958|Erins Vale Formation|61612|6|Mentioned|p272, p277, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||12-MAR-09
24958|Erins Vale Formation|63832|6|Mentioned|p131 fig 2|||Of Sydney Basin.||Unit in Illawarra Coal Measures.||||
24958|Erins Vale Formation|64631|6|Mentioned|p44 Fig.2.|Capitanian|Wordian|SE Sydney Basin. Biostratigraphic age control at base and top.||Unit in Illawarra Coal Measures.||||
24958|Erins Vale Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Pheasants Nest Formation. Is overlain by Woonona Coal.||
24958|Erins Vale Formation|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Late Permian.||Of the Illawarra Coal Measures.||||
24958|Erins Vale Formation|69297|6|Mentioned|p502 fig 5.43|||Sydney Basin. ||||||
24958|Erins Vale Formation|73304|6|Mentioned|p74, p78|||Sydney Basin, southern. Base is identified as the base of the P4 glaciation.||Illawarra Coal Measures||||
24958|Erins Vale Formation|73421|5|Briefly described|p3, p5, p16, p18-19|Capitanian|Capitanian|Sydney Basin, southern.||Cumberland Subgroup|Kulnura Marine Tongue|Overlies Pheasant Nest Formation, underlies Wilton Formation|Siltsone with sandstone and pebble layers.|
24958|Erins Vale Formation|73625|6|Mentioned|p2|Permian|Permian|Southern coalfield, Sydney Basin.||Illawarra Coal Measures.||Overlies Pheasants Nest Formation. Is overlain by Marangaroo Conglomerate.||
37298|Ermelo Pyroclastics|23861|5|Briefly described|p3, p4 Fig. 2|Namurian|Namurian|Overlain by Clifden Formation.  Geological Province: New England Orogen.||||||
37298|Ermelo Pyroclastics|24010|5|Briefly described|p379|Carboniferous|Carboniferous|Age: 319+/-5Ma (K-Ar), 321.3+/-3.2Ma (SHRIMP U-Pb)||||||
37298|Ermelo Pyroclastics|24603|5|Briefly described|p868 Fig. 3 (caption)|Namurian|Namurian|Part of the Ermelo Dacite?  Age: 321.3+/-3.2Ma.  Geological Province: Tamworth Belt.||||||
37298|Ermelo Pyroclastics|24605|2|Defined|p932, Fig.1, p937, p949 App.1|Namurian|Namurian|Overlies the Spion Kop Conglomerate and disconformably overlies the Caroda Formation. Overlain by the lower parts of the Clifden Foramtion. Age: 321.3 +/- 3.2 Ma (U-Pb) and 319 +/- 5 Ma (K-Ar). Geological Province: New England Orogen.||||||
37298|Ermelo Pyroclastics|50613|5|Briefly described|p220|||Geological Province: Rocky Creek Syncline.||||||22-FEB-05
37298|Ermelo Pyroclastics|60299|5|Briefly described|p212 Fig.2c|Carboniferous|Carboniferous|Age: 321 Ma (U-Pb zircon, Roberts et al., 1995). Of Clifden Formation. Geological Province: Rocky Creek Block.||||||18-MAY-05
37298|Ermelo Pyroclastics|61214|6|Mentioned|p170, p172 Fig. 2|Namurian|Namurian|Of the Clifden Formation. Age: 321.3+/-3.2Ma (SHRIMP). Geological Province: Boomi Block predominantly (restricted to the northern Rocky Creek area). See also p173. ||||||
37298|Ermelo Pyroclastics|61767|4|Described|p71|Namurian|Namurian|Formerly known as Ermelo Dacite Tuff. Dark, hornblende pyroxene andesitic to dacitic pyroclastic fall or/and flow deposit. Conformably overlain by Clifden Fm. Conformably overlies the Spion Kop Conglomerate. Max. thickness: 250m. Geol. Prov: Tamworth Belt||||||25-JAN-06
37298|Ermelo Pyroclastics|65382|5|Briefly described|p714|Serpukhovian|Serpukhovian|Of Clifden Formation. Age of 321.3 +/- 3.2 given.||||||
37298|Ermelo Pyroclastics|65902|5|Briefly described|p204|Bashkirian|Serpukhovian|Of Clifden Formation. SHRIMP U-Pb zircon age of 321.3 +/- 2 Ma (Opdyke et al., 2000) and K-Ar hornblende age of 319 +/- 5 Ma (Roberts et al., 2003).||||||09-MAR-12
29585|Errowan Monzonite|22679|3|Fully described|p 37, 38|Ordovician|Ordovician|formerly Errowan Monzonite||||||
29585|Errowan Monzonite|23214|2|Defined|p95|Late Ordovician|Late Ordovician|Intrudes Forest Reefs Volcanics.||||||
29585|Errowan Monzonite|24398|5|Briefly described|p259 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
29585|Errowan Monzonite|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite clinopyroxene monzonite, altered quartz syenite, pyritized monzonite.||||||17-JUL-08
29585|Errowan Monzonite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29585|Errowan Monzonite|63286|6|Mentioned|p304|Ordovician|Ordovician|Renamed as the Errowan Intrusive Complex.||||||07-FEB-11
29585|Errowan Monzonite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
68031|Escott Zeolitite Member|50613|5|Briefly described|p215, P220 Fig. 10|Westphalian|Namurian|Informal? - see Escott Zeolitite.||||||11-SEP-21
35608|Essex Member|61964|2|Defined|p14 Fig. 4, p115, p128|Famennian|Famennian|Of Rankin Formation (Cocoparra Group) where these rocks were formerly undifferentiated, along with the Bywatha Conglomerate Member. Very thin to medium bedded, white to buff, fine- to med.-gr. qtz sst. Max.thickness: 300m. For palaeontology - see p261.||||||
35608|Essex Member|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Rankin Formation. Thin, medium bedded quartz sandstone, minor mudchip breccias, rounded to sub-angular quartz grains; marine trace fossils and rare shelly debris.||||||10-APR-08
35608|Essex Member|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Rankin Formation.|||Thin- to medium-bedded quartz sandstone, minor mudchip breccias, rounded to subangular quartz grains; marine trace fossils and rare shelly debris.|
35608|Essex Member|69163|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Rankin Formation.|||Thin- to medium-bedded quartz sandstone, minor mudchip breccias, rounded to subangular quartz grains; marine trace fossils and rare shelly debris.|
27676|Ettamogah Tuff Member|22857|4|Described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Babinda Volcanics (Kopyje Group, Cobar Supergroup). Max. thickness: 900m. Geological Province: Kopyje Shelf (Darling Basin).||||||
27676|Ettamogah Tuff Member|23173|6|Mentioned|Map Legend|||||||||
27676|Ettamogah Tuff Member|35287|6|Mentioned|p7|||||||||
27676|Ettamogah Tuff Member|39618|1|Redefined|p60|Early Devonian|Early Devonian|||||||
27676|Ettamogah Tuff Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27676|Ettamogah Tuff Member|41528|2|Defined|p47|Early Devonian||||||||
27676|Ettamogah Tuff Member|41529|6|Mentioned|Map legend|Early Devonian||||||||
27676|Ettamogah Tuff Member|42566|3|Fully described|p56|||||||||
27676|Ettamogah Tuff Member|42568|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
32326|Euchabil Gap Formation|22831|3|Fully described|p 66|||||||||
32326|Euchabil Gap Formation|22857|5|Briefly described|p448 App.1, Tb.A1.6|Devonian|Devonian|Of the Wallingalair Group. Siltstone and fine-grained quartzose arenite with claystone fragments; poorly preserved fossils. Max. thickness: 570m. Geological Province: Bogan gate Terrace.||||||
32326|Euchabil Gap Formation|24417|3|Fully described|p91|Early Devonian|Early Devonian|Of Trundle Group.  Parts previously included in Hervey Group, "Wallingalair Beds" and Wallingalair Group. Overlies the Coonardo Sandstone.||||||
32326|Euchabil Gap Formation|44160|5|Briefly described|map legend|Pragian|Pragian|of Wallingalair Group.||||||
32326|Euchabil Gap Formation|60009|5|Briefly described|Map Legend|Pragian|Pragian|Of the Trundle Group. Overlies: Coonardoo Sandstone.  Underlies: Beugamel Sandstone.||||||13-JUL-04
32326|Euchabil Gap Formation|62569|5|Briefly described|p607 Fig. 2|Late Devonian|Givetian|Of Wallingalair Group. Geological Province: Lachlan Fold Belt. Fig shows Early Devonian age but conclusions p612 imply Givetian or younger age, based on underlying Coonardoo Sandstone fossils.||||||21-AUG-12
27770|Eugowra Granite|22831|6|Mentioned|p 71|||||||||
27770|Eugowra Granite|23053|6|Mentioned|p23,69||Devonian|||||||
27770|Eugowra Granite|23214|3|Fully described|p207|Early Devonian|Early Devonian|Intrudes the Maura Formation. I-type granite. Of the Eugowra Batholith.||||||
27770|Eugowra Granite|24125|5|Briefly described|p3|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
27770|Eugowra Granite|24266|6|Mentioned|p1486|||Geological Province: Lachlan Fold Belt.||||||
27770|Eugowra Granite|24417|3|Fully described|p97|Devonian|Devonian|Of Eugowra Suite.  Intrudes Glenisla Volcanics.  Formerly included rocks now known as Lords, Milandra and Loch Lomond Granites and Clear Hills Monzodiorite.  Age: 394+/-2.1 Ma (SHRIMP U/Pb).||||||
27770|Eugowra Granite|24580|5|Briefly described|p828|Early Devonian|Early Devonian|Geological Province: Eastern Lachlan Fold Belt.||||||
27770|Eugowra Granite|29907|6|Mentioned|p10|||||||||
27770|Eugowra Granite|29985|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
27770|Eugowra Granite|33285|6|Mentioned|p27|||||||||
27770|Eugowra Granite|33732|6|Mentioned|p115|||||||||
27770|Eugowra Granite|33833|6|Mentioned|Fig.1|||||||||
27770|Eugowra Granite|34403|6|Mentioned|p147|||||||||
27770|Eugowra Granite|34405|6|Mentioned|p124|||||||||
27770|Eugowra Granite|34406|6|Mentioned|p222|||Buchan orogenic phase.||||||
27770|Eugowra Granite|39214|5|Briefly described|p18|||||||||
27770|Eugowra Granite|39331|6|Mentioned|Fig.7-3|||||||||
27770|Eugowra Granite|40130|5|Briefly described|p197|||||||||
27770|Eugowra Granite|40328|4|Described|p205|||||||||
27770|Eugowra Granite|40766|6|Mentioned|p26|||||||||
27770|Eugowra Granite|40882|5|Briefly described|p22|||See also P29||||||
27770|Eugowra Granite|40891|6|Mentioned|Fig.3|||||||||
27770|Eugowra Granite|42262|6|Mentioned|Fig. 2 P1810|||||||||
27770|Eugowra Granite|42726|5|Briefly described|map legend|Early Devonian||417.  Of the Eugowra Suite (Boggy Plain Supersuite).||||||08-FEB-05
27770|Eugowra Granite|43499|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
27770|Eugowra Granite|43510|14|Not recorded|p39,52-5,58,60,65||Middle Devonian|Manildra-Gooloogong area.Young Granite is probably S extension of unit.Also Gooloogong-Grenfell area||||||
27770|Eugowra Granite|43640|5|Briefly described|Map Legend||Devonian|||||||
27770|Eugowra Granite|43782|5|Briefly described|Map Legend|Emsian|Emsian|||||||
27770|Eugowra Granite|44093|5|Briefly described|p186 App. 1|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||07-MAR-05
27770|Eugowra Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|Of the Eugowra Suite.||||||13-JUL-04
27770|Eugowra Granite|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Boggy Plain Supersuite||||
27770|Eugowra Granite|71040|6|Mentioned|p17-18|Early Devonian|Early Devonian|Forbes area.||||||
27770|Eugowra Granite|71206|6|Mentioned|p379|||Lachlan Fold Belt.|||||Unfractionated I-type granite.|
31470|Eugowra Suite|22768|6|Mentioned|p178|||||||||
31470|Eugowra Suite|22857|5|Briefly described|p178|Early Devonian|Early Devonian|Of the Boggy Plain Supersuite.||||||
31470|Eugowra Suite|24417|3|Fully described|p94|Middle Devonian|Early Devonian|Previously included in Boggy Plain Supersuite.  Has also been referred to as "Eugowra Granite" by many authors.||||||
31470|Eugowra Suite|24580|5|Briefly described|p828|Early Devonian|Early Devonian|Age: 393.0 +/- 2.5 & 394.2 +/- 2.1 Ma. Geological Province: Eastern Lachlan Fold Belt.||||||
31470|Eugowra Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains the Eugowra and Clear Hills Granites.||||||08-FEB-05
31470|Eugowra Suite|60009|5|Briefly described|Map Legend|Emsian|Emsian|||||||13-JUL-04
30099|Eulendool Formation|22857|4|Described|p412 App. 1 Tb. A1.4.|Ordovician|Ordovician|Of the Tallebung Group. Thick-bedded, poorly sorted fine to coarse-grained quartz arenite and quartzite; thinly bedded to massive mudstone and siltstone; minor pebble and cobble conglomerate. Geological Province: Wagga Marginal Basin.||||||24-FEB-06
30099|Eulendool Formation|43089|5|Briefly described|Map Legend|||Of Tallebung Group.||||||20-OCT-08
30099|Eulendool Formation|61964|5|Briefly described|p30, p33|||Of MacRae and Pogson (1990). Name suggested for thick-bedded seq. (Trigg 1987) within former Tallebung Group. Probably refers to a composite of the sandstone-rich packages overlying/underlying Currawalla Shale. Written informally as "Eulendool Formation"||||||20-OCT-08
30099|Eulendool Formation|70950|6|Mentioned|p1029|Ordovician|Ordovician|Geological province: Central Lachlan Orogen. Formerly of Tallebung Group (of Trigg 1987; see Colquhoun, Hendrickx and Meakin 2005a). ||Unit of Wagga Group.||||
30099|Eulendool Formation|71069|6|Mentioned|p71|||||Tallebung Group||||
40557|Eulowrie Pyroclastic Member|24605|2|Defined|p931, p943, p953 App.1|Westphalian|Namurian|Of the Lark Hill Formation. Thickness in the type section: 23m. Age: 310.6 +/- 4Ma. Geological Province: New England Orogen.||||||
36152|Eura Bonny Granite|61964|3|Fully described|p14 Fig. 4, p40, p41 Tb. 2, p52|Early Silurian|Early Silurian|Of Koetong Suite (Koetong Supersuite).Highly weathered porphyritic biotite granite - lithological details included and compared with other granites of the Koetong Suite. Overlain by Gurragong Volcanics. Age: ~428.2Ma. ||||||
36152|Eura Bonny Granite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Highly weathered porphyritic biotite granite.||||||10-APR-08
36152|Eura Bonny Granite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian|||Unit in Koetong Suite.||Intrudes Clements Formation.|Highly weathered biotite granite and residual granitic soil.
|
36152|Eura Bonny Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Coarse-grained porphyritic biotite cordierite muscovite granite; poorly exposed.|
75927|Euradux Granite|69159|5|Briefly described|Map legend|Pragian|Pragian|Medium magnetic susceptibility. High radioelement response.||Unit in Braidwood Suite.|||Pink-grey, medium- to coarse-grained, massive, porphyritic, biotite granite.|07-SEP-15
75927|Euradux Granite|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Glenbog Suite.|||Pink-grey, medium- to coarse-grained, massive, porphyritic biotite granite; moderate magnetic susceptibility; high radioelement response.|
75927|Euradux Granite|71700|3|Fully described|vi, viii, p7, p26, p42, CD|Early Devonian|Early Devonian|Named for the Euradux road west of the pluton. The type locality is outcrop near GR 756633 6079583. Previously (Joplin et al, 1953; Best et al, 1964; Felton and Huleatt, 1975) this unit was not differentiated from the Braidwood Granodiorite. Ruker (1988) recognised and subdivided the granite from the Braidwood Granodiorite as the Brushy Hill Granodiorite. However, "Brushy Hill" had already been used for a formally defined unit and is compositionally a granite not a granodiorite, thus the new name Euradux Granite is proposed. Distribution, geomorphic expression, outcrop, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. Age is inferred from this units relationship with the Braidwood Granodiorite which is dated to be early Devonian. Intrusive relationship with the Braidwood Granodiorite is inferred only, as no boundary relationships have been observed.||Braidwood Suite||Intrudes the Braidwood Granodiorite. Equivalent to the Braidwood Granodiorite.|Pink to grey, medium- to coarse-grained, massive, porphyritic biotite granite.|
72812|Eurimbla Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Purplish to greenish, polymictic conglomerate. lithic sandstone, laminated quartzose siltstone and minor black siliceous mudstone, and volcaniclastic sandstone.||||||29-MAY-08
72812|Eurimbla Formation|68592|3|Fully described|p376, p384-5, p389, p408-26, p437, p464|Llandovery|Llandovery|See also p16, p73 Tb.5, p81, p1866. New name, after Eurimbla homestead N of Frogmore. Included in Kenyu Formation by Stevens (1955) and Gibbons (1960); recognised as a separate sequence by Bartolo (1994) and O'Sullivan (1993) who named the Eurimbla Conglomerate; asociated sandstone and siltstone were assigned as equivalents to Adaminaby Group, Kenyu Formation or Hawkins Volcanics. Generally small outcrops in the Frogmore and Boorowa area. No type section because of poor exposure; but >660m thick. Has a mixed mafic volcanic/quartzose provenance, suggesting nearby juxtaposition and local erosion of the Macquarie Arc and Adaminaby Group. Yass structural zone: deformation described. Conflicting ages from fossils discussed.||||Unconformably overlies Kenyu Formation. Is intruded by Licking Gully Granite. Is faulted against Hawkins Volcanics and probably the Hanaminno Limestone.|Purplish to greenish, polymictic conglomerate, lithic sandstone, laminated quartzose siltstone, and minor black siliceous mudstone and volcaniclastic sandstone; includes limestone.|
72812|Eurimbla Formation|70192|5|Briefly described|Map Legend|Llandovery|Llandovery|Sxe. Ungrouped Silurian formation. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||||Polymictic conglomerate, lithic sandstone and laminated quartzose siltstone and minor black siliceous mudstone and volcaniclastic sandstone.|
72812|Eurimbla Formation|70545|5|Briefly described|Map Legend|Silurian|Silurian||||||Polymictic conglomerate, lithic sandstone and laminated quartzose siltstone and minor black siliceous mudstone and volcaniclastic sandstone.|
72812|Eurimbla Formation|71656|5|Briefly described|p10 Fig.1, p12 Fig.2, p16|Llandovery|Llandovery|Presumed age based on Monograptus graptolite identification. Placed below the Douro Group on the correlation chart of Fig.2 with no relation to other units or group described. Early Ordovician conodonts found in a nearby chert are interpreted as being reworked.|||||Fossiliferous dark grey-black siltstone.|
80448|Eurolie granite|70718|5|Briefly described|p68-p71, p74, p76-77, p86, 122, 123|Early Devonian|Early Devonian|Informal name, interpreted from geophysics.Interpreted as I-type granite similar to Booroorban granite. Referred to as the Eurolie granodiorite on p74. This or Booroorbin granite was intersected in waterbore GW036235. Misspelt as Euorlie granite p122 (correct spelling also on same page).||Booroorban granite suite||Intruded by Booroorban granite, Oolambeyan granite, part of the Leeton Igneous Complex, some of the Willurah and the Singorimbah igneous intrusions. .||31-MAY-19
29575|Eurongilly Serpentinite|22638|2|Defined|p35||Late Silurian|Previously "Mooney Mooney Serpentinite"||||||
29575|Eurongilly Serpentinite|22857|5|Briefly described|p416 App. 1 Tb. A1.5|||On COOTAMUNDRA 1:250 000 sheet. Schistose serpentinite with dark isotropic aggregates surrounded by antigorite. ||||||
29575|Eurongilly Serpentinite|44192|5|Briefly described|Map Legend|Wenlockian|Llandoverian|||||||
29575|Eurongilly Serpentinite|44936|5|Briefly described|Map Legend||Silurian|||||||
29575|Eurongilly Serpentinite|50191|6|Mentioned|p6, 23, Fig. 8|Silurian|Silurian|||||||
29575|Eurongilly Serpentinite|71708|6|Mentioned|p336 Fig 1|||Adjacent to the Gilmore Fault zone.||||||
29575|Eurongilly Serpentinite|72084|5|Briefly described|p11, p25|||Forms in situ outcrops and displaced blocks. Highly magnetic. Appears as Eurongillie Serpentinite on p25.||||Is intruded by Wantabadgery Granite.|Fine-grained, light greenish-grey serpentinite; dominated by fine serpentine minerals with domains of disseminated magnetite. Locally has extensive carbonate alteration.|
29575|Eurongilly Serpentinite|73483|6|Mentioned|p407 Fig.1|||||||||
24965|Eurow Formation|23214|6|Mentioned|p231|||Superseded by Eurow Member.||||||
24965|Eurow Formation|23217|4|Described|p1, p10, p17-9||Famennian|(Conolly, 1965a).  Of the Hervey Group (formerly the only named unit within the "Cookamidgera Sub-group).  Max. thickness>680m. Geological Province: Parkes Syncline.||||||08-MAR-06
24965|Eurow Formation|23392|2|Defined|p14, p24||Famennian|Correlation with Culela Member. Of the Hervey Group. Geological Province: Lachlan Fold Belt. Max Thickness: 680m||||||
24965|Eurow Formation|24417|3|Fully described|p140|Famennian|Famennian|Of Hervey Group.  Originally of Connolly's (1965a) "Cookamidgera Sub-Group".  Pogson & Watkins (1998) proposed "Eurow Member" (of "Cookamidgera Fm.") - however formation status now retained.  Overlain by Wingara Fm; underlain by Bumberry Fm.||||||
24965|Eurow Formation|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
24965|Eurow Formation|33006|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
24965|Eurow Formation|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
24965|Eurow Formation|43499|14|Not recorded|Map Legend|||(Provisional Edition) Part of Cookamidgera Sub-Group||||||
24965|Eurow Formation|43507|2|Defined|p128,130,161||Late Devonian|Formation of Cookamidgera Subgroup (Hervey Group)||||||
24965|Eurow Formation|43510|2|Defined|p41-2,52,54-5,57-8|||||||||
24965|Eurow Formation|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
24965|Eurow Formation|43516|14|Not recorded|Map Legend||Late Devonian|||||||
24965|Eurow Formation|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hervey Group. Friable red sandstone and shale.||||||05-JUL-04
24965|Eurow Formation|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Hervey Group. Underlies: Wingara Formation.  Overlies: Bumberry Formation.||||||13-JUL-04
24965|Eurow Formation|68592|5|Briefly described|p1720|Famennian|Famennian|Lyons et al. (2000). In the Forbes 1:250 000 map area. Contains Late Famennian Culela fish fauna and Leptophloeum australe.||||Correlated with Koorawatha Formation.||
24965|Eurow Formation|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Hervey Group||||
80148|Eurunderee Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Werrie Basin. Shown only as Eurunderee. Ending assumed from references to other Coal Members in text.||Rowan Formation.||||28-SEP-17
30026|Eurundury Formation|43188|5|Briefly described|p205|||Mudgee - Gulgong region.||||||
37372|Eurydesma beds|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, fine- to medium-grained lithic arenite, dark calcareous siltstone; local limestone lenses. Thin-bedded, richly fossiliferous limestone.||||||12-DEC-07
37372|Eurydesma beds|63748|4|Described|p7 Fig. 3, p18|Early Permian|Early Permian|Unconformably overlain by Wallaby beds; faulted against older basement Silverwood Group rocks. Thickness: ~200m. Consists of conglomerate, fine-to medium-grained lithic arenite, dark calcareous siltstone and thin bedded limestone.||||||07-FEB-11
37372|Eurydesma beds|68679|5|Briefly described|p446, p452|Permian|Permian|Silver Spur Subprovince, Woolomin Province. Exposed over 5 km2 around Rokeby homestead, 17km SE of Warwick. ~200m thick.||Wildash Group.||Is faulted against Silverwood Group. Is overlain unconformably by Wallaby beds.|Conglomerate, fine- to medium-grained lithic sandstone, calcareous siltstone and thin-bedded limestone containing early Permian marine macrofossils.|
30351|Eusdale Granite|23214|3|Fully described|p254|Carboniferous|Carboniferous|Of the Bathurst Batholith.  Intrudes the Lambie Group. Formerly named Eusdale Stock and included in the Yetholme Granite, and then named Eusdale Adamellite.||||||
30351|Eusdale Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
30351|Eusdale Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
30351|Eusdale Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|of Bathurst Batholith.||||||
30351|Eusdale Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
26541|Eustah Granite|42712|4|Described|Table1p13; Fig3p9.|Carboniferous|Early Carboniferous|||||||
24966|Evans Head Coal Measures|22857|4|Described|p284, p542 App.1 Tb.A1.11|Late Triassic|Early Triassic|Sandstone, siltstone, claystone, conglomerate, very minor coal. Max. thickness: >50m. Geological Province: Ipswich Basin (under Clarence-Moreton Basin). See also p318-9 Figs. 22.10A,B.||||||
24966|Evans Head Coal Measures|22860|6|Mentioned|Fig20.2p278|||||||||
24966|Evans Head Coal Measures|22861|6|Mentioned|p284|||||||||
24966|Evans Head Coal Measures|23811|5|Briefly described|Map Legend|Norian|Norian|Thin- to thick-bedded, crossbedded, coarse-grained quartz to lithic arenite, thinly bedded, grey siltstone, claystone, minor coal as partings and as very thin bands.Geological Province: Clarence-Moreton Basin.||||||22-SEP-05
24966|Evans Head Coal Measures|23812|5|Briefly described|p31, p35 Tb.4|Late Triassic|Late Triassic|Together with the Red Cliff Coal Measures considered to be equivalent to the Ipswich Coal Measures. Unconformably overlies the Chillingham Volcanics. Max. thickness: 300m. Geological Province: Clarence-Moreton Basin.||||||
24966|Evans Head Coal Measures|30785|6|Mentioned|p398|||||||||
24966|Evans Head Coal Measures|30911|6|Mentioned|Map legend|Triassic|Triassic|||||||
24966|Evans Head Coal Measures|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
24966|Evans Head Coal Measures|33476|6|Mentioned|p99|||||||||
24966|Evans Head Coal Measures|34340|4|Described|p464|||Correlated with Red Cliff and Nymboida Coal Measures||||||
24966|Evans Head Coal Measures|37112|5|Briefly described|Table 1|||||||||
24966|Evans Head Coal Measures|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
24966|Evans Head Coal Measures|43383|14|Not recorded|p24|||||||||
24966|Evans Head Coal Measures|43468|14|Not recorded|Map Legend||Triassic|Provisional Edition||||||
24966|Evans Head Coal Measures|44093|5|Briefly described|p72|Late Triassic|Late Triassic|See also p73 Fig. 7.3. In Ipswich Basin.||||||
24966|Evans Head Coal Measures|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup.  Arenite, siltstone, claystone, minor coal. Equivalent to Ipswich Coal Measures.||||||20-JUL-04
24966|Evans Head Coal Measures|60281|5|Briefly described|p21-22, p25|Late Triassic|Early Triassic|Of the Ipswich Coal Measures. Sandstone, siltstone, claystone, conglomerate, very minor coal.  Max. thickness: >50m.  Geological Province: Ipswich Basin.  See also Figure 18 Appendix 1.||||||17-MAR-05
24966|Evans Head Coal Measures|60993|5|Briefly described|p8 |||Unconformably overlain by Raceview Formation. Geological Province: Clarence-Moreton Basin. Equivalent to Ipswich Coal Measures. ||||||
24966|Evans Head Coal Measures|60995|5|Briefly described|p52 Tb. 1|Late Triassic|Early Triassic|Of the Ipswich Coal Measures. May be misidentified Raceview Fm. Sandstone, siltstone, claystone, conglomerate, very minor coal. Max. thickness: >50m. Geol. Prov: Clarence-Moreton Basin.||||||
24966|Evans Head Coal Measures|61310|5|Briefly described|p16, Table C1 (p22-23)|Late Triassic|Late Triassic|Comprise shallow to steeply dipping sandstone and lesser conglomerate, mudrock and coal. Max. thickness: ~300m. Geological Province: Clarence-Moreton Basin. Along with Red Cliff Coal Measures are equivalent to Ipswich Coal Measures.||||||
24966|Evans Head Coal Measures|61772|6|Mentioned|p130 Fig. 5||Late Triassic|Coal Measures is C.M. in text.||||||24-SEP-08
24966|Evans Head Coal Measures|61775|6|Mentioned|p182 Fig. 1|||||||||
24966|Evans Head Coal Measures|66855|5|Briefly described|pp955-958.|Late Triassic|Late Triassic|Conglomerate clasts are felsic volcanic rocks similar to Chillingham Volcanics. The quartz sandstone is interpreted as Ripley Road Sandstone. Correlated with Red Cliff and Nymboida Coal Measures.Overlies basalt c.141 Ma and hyaloclastic andesitic breccia.|||||Tuffaceous mudstone intercalated with pebbly lithic sandstone and conglomerate; quartz sandstone, siltstone and carbonaceous shale.|
24966|Evans Head Coal Measures|68679|6|Mentioned|p388, p392|Late Triassic|Late Triassic|||||Equivalent to the Ipswich Coal Measures.||
24966|Evans Head Coal Measures|69297|5|Briefly described|p487 fig 5.38|Late Triassic|Late Triassic|Clarence-Moreton Basin. More than 50m thick. ||||Overlies the Nymboida Coal Measures. Overlain by the Redcliff Coal Measures.|Sandstone, siltstone, conglomerate and very minor coal.|
76099|Evelyn Creek Volcanics|67207|5|Briefly described|Map legend.|Ordovician|Cambrian|Regionally metamorphosed to greenschist facies.|||||Dark grey, foliated and folded mafic sills and dykes, medium-grained monzodiorite: alkaline geochemical affinity; brown to green, foliated and folded aphanitic mafic sills/flows, with amygdales and possible vesicles: alkali basalt to trachy-basalt.|25-SEP-13
76099|Evelyn Creek Volcanics|68822|6|Mentioned|p324|||Undated. Koonenberry Belt.||||||
80635|Evergreen Formation, lower|71805|6|Mentioned|p79|||Of Evans (1962) based on study of Glentulloch -1 well. Eromanga Basin. Depositional environment discussed.||||||01-SEP-20
39795|Evergreen Formation, upper|24159|6|Mentioned|p152|||Informal - see Evergreen Formation. Geological Province: Surat Basin.||||||
39795|Evergreen Formation, upper|61310|6|Mentioned|p22|||Informal - see Evergreen Formation||||||
39795|Evergreen Formation, upper|71805|5|Briefly described|p79|||Eromanga Basin.|||Includes the Boxvale Sandstone Member.|||
27152|Ewolong Formation|9548|5|Briefly described|Map Legend|Pragian|Pragian|Of the Yarra Yarra Creek Group. Underlies: Gwando Siltstone.||||||
27152|Ewolong Formation|22831|3|Fully described|p53|Pragian|Lochkovian|Yarra Yarra Creek Group||||||01-NOV-13
27152|Ewolong Formation|22857|4|Described|p446 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Yarra Yarra Creek Group. Max. thickness: 150m. Geological Province: Darling Basin.||||||
27152|Ewolong Formation|42449|6|Mentioned|p13|||Reserved 1977, D. Pogson last update May 1991.||||||
27152|Ewolong Formation|42566|2|Defined|p102|Early Devonian|Early Devonian|Age: late Early Devonian||||||
27152|Ewolong Formation|42568|5|Briefly described|Map legend|Pragian|Pragian|||||||
27152|Ewolong Formation|43441|6|Mentioned|29||Early Devonian|||||||08-JAN-10
27152|Ewolong Formation|44160|5|Briefly described|Map Legend||Lochkovian|||||||
27152|Ewolong Formation|70751|6|Mentioned|p12|Lochkovian|Lochkovian|||Yarra Yarra Creek Group||||
27152|Ewolong Formation|72958|6|Mentioned|p11|Lochkovian|Lochkovian|Cobar Basin. Nymagee area.||Yarra Yarra Creek Group, Cobar Supergroup||Overlain by Gwando Siltstone.||
28543|Excursion Creek Sandstone Member|22857|4|Described|p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Silverdale Formation. Coarse tuffs, tuffaceous sandstone, siltstone. Max. thickness: 104.9m. Geological Province: Canberra-Yass Shelf. ||||||
28543|Excursion Creek Sandstone Member|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Nomenclature||||||
28543|Excursion Creek Sandstone Member|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
28543|Excursion Creek Sandstone Member|35386|4|Described|p26|||||||||
28543|Excursion Creek Sandstone Member|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
28543|Excursion Creek Sandstone Member|40328|4|Described|p109|||||||||
28543|Excursion Creek Sandstone Member|45147|6|Mentioned|M152|||||||||
28543|Excursion Creek Sandstone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yanawe Formation (Douro Group). Quartzose biomicrite with crinoidal biomicrite sproadically developed. Coarse-grained volcaniclastite, tuffaceous sandstone and siltstone.||||||09-SEP-08
28543|Excursion Creek Sandstone Member|68592|2|Defined|p430 Fig.89,p432,p434-6, p514-5, p523-58|Ludlow|Ludlow|Link (1970, 1971) named this unit in his Laidlaw Formation. Moved into Silverdale Formation by Owen and Wyborn (1979); here transferred from Silverdale Formation (Hattons Corner Group) to Yanawe Formation (Douro Group). Type section described. 22-105m thick. Volcanic mass flows from the rapidly eroding Laidlaw Volcanics. Unfossiliferous; early Ludlow age inferred from stratigraphic relationships.||Unit in Yanawe Formation.||Conformably overlies Euralie Limestone Member. Is overlain conformably by Gums Road Limestone Member.|Medium- to very fine-grained, thin- to medium-bedded, massive volcaniclastic sandstone with rare, thin siltstone interbeds.|10-JAN-17
28543|Excursion Creek Sandstone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdwx[asterisk]. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Yanawe Formation||Is overlain by Gums Road Limestone Member. Overlies Euralie Limestone Member.|Medium-very fine grained, thin-medium bedded, massive volcanic sandstone with lesser siltstone and mudstone.|
28543|Excursion Creek Sandstone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Medium-very fine grained, thin-medium bedded, massive volcanic sandstone with lesser siltstone and mudstone.|
28543|Excursion Creek Sandstone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Medium to very fine grained, thin to medium bedded, massive volcanic sandstone with lesser siltstone and mudstone.|
38307|Fairbairns Lane seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
25904|Fairbridge Volcanics|13139|5|Briefly described|p8, p9 Fig. 4|Late Ordovician|Middle Ordovician|Contains the Yuranigh and Wahringa Limestone Members.  Overlie the Hensleigh Siltstone; overlain by Oakdale Formation. Geological Province: Western Molong Volcanic Belt.||||||12-APR-05
25904|Fairbridge Volcanics|13995|5|Briefly described|p70-71, p77|Ordovician|Ordovician|Northern Molong High. Contains late Darriwilian (Middle Ordovician) gastropods.|||Wahringa Limestone Member.|||
25904|Fairbridge Volcanics|22857|4|Described|p422 App. 1, Tb. A1.5|Late Ordovician|Early Ordovician|Of the Kenilworth Group. Max. thickness: 2100m - possibly reaches 4km in the Cudal area? See also p426 App. 1 Tb. A1.5.||||||
25904|Fairbridge Volcanics|23043|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of Cabonne Group.||||||01-SEP-08
25904|Fairbridge Volcanics|23170|2|Defined|p34|Gisbornian|Darriwilian|Age: Early Darriwilian - Late Bolindian (Ordovician). Lachlan Fold Belt.||||||
25904|Fairbridge Volcanics|23181|6|Mentioned|Fig.2|Late Ordovician|Ordovician|Max age is middle Ordovician.||||||
25904|Fairbridge Volcanics|23213|3|Fully described|p11, Fig.10|Gisbornian|Darriwilian|Age: Early Darriwilian to Late Gisbornian. Includes 'Cargo Volcanics', Blathery Creek Volcanics. Formerly included in Kenilworth Group. Now of Cabonne Group.||||||04-MAR-09
25904|Fairbridge Volcanics|23214|2|Defined|p24|Middle Devonian|Middle Devonian|Included as part of Kenilworth Group on 1:250 000 and 1:100 000 map sheets but should probably be part of the Cabonne Group. Includes Yaranigh Limestone Member. Type Locality GR 678900 6333150.||||||
25904|Fairbridge Volcanics|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
25904|Fairbridge Volcanics|23736|5|Briefly described|p12|Eastonian|Darriwilian|||||||
25904|Fairbridge Volcanics|23739|4|Described|p212|Late Ordovician|Middle Ordovician|Geological Province: Lachlan Fold Belt||||||
25904|Fairbridge Volcanics|24215|5|Briefly described|p805|||Geological Province:  Lachlan Fold Belt||||||
25904|Fairbridge Volcanics|24265|5|Briefly described|p1448||Ordovician|Geological Province: Lachlan Fold Belt.||||||04-MAR-09
25904|Fairbridge Volcanics|24266|5|Briefly described|p1470|Ordovician|Ordovician|Age: 447+/-5 Ma. Geological Province: Lachlan Fold Belt.||||||
25904|Fairbridge Volcanics|24398|4|Described|p262-263|Gisbornian|Darriwilian|See also p259 Fig. 2.  Basaltic andesite-latite-trachylatite (Pogson and Watkins, 1998). Contains the Wahringa and Yuranigh Limestone Members.  Overlies the Hensleigh Siltstone.  Geological Province: Lachlan Fold Belt.||||||01-SEP-08
25904|Fairbridge Volcanics|29362|2|Defined|p190|Middle Ordovician|Early Ordovician|Lower-Middle Ordovician.||||||
25904|Fairbridge Volcanics|30044|6|Mentioned|p17|||||||||
25904|Fairbridge Volcanics|30139|5|Briefly described|Table 1|||||||||
25904|Fairbridge Volcanics|31161|5|Briefly described|PA2|||||||||
25904|Fairbridge Volcanics|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25904|Fairbridge Volcanics|32672|6|Mentioned|p671|||||||||
25904|Fairbridge Volcanics|33116|4|Described|p201|||Ord.||||||
25904|Fairbridge Volcanics|33121|6|Mentioned|p85|||Correlation table. Early Ord.||||||
25904|Fairbridge Volcanics|33285|5|Briefly described|p30|||||||||
25904|Fairbridge Volcanics|33480|6|Mentioned|p240|||Age dating||||||
25904|Fairbridge Volcanics|34895|6|Mentioned|Fig. 1|||Also petrology P969||||||
25904|Fairbridge Volcanics|35118|6|Mentioned|Fig.5|||||||||
25904|Fairbridge Volcanics|35291|6|Mentioned|p17|||||||||
25904|Fairbridge Volcanics|35412|6|Mentioned|p10|||Location of Copper Hill copper mineralization.||||||
25904|Fairbridge Volcanics|35415|6|Mentioned|Fig.2|||Stratigraphic correlations.||||||
25904|Fairbridge Volcanics|39214|5|Briefly described|p19|||||||||
25904|Fairbridge Volcanics|40136|6|Mentioned|p24|||||||||
25904|Fairbridge Volcanics|40328|6|Mentioned|p148|||||||||
25904|Fairbridge Volcanics|43640|5|Briefly described|Map Legend||Ordovician|||||||
25904|Fairbridge Volcanics|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Kenilworth Group. Consists of porphyritic augite basalt, hornblende basaltic andesite; volcaniclastic horizons.||||||15-JUL-08
25904|Fairbridge Volcanics|43653|5|Briefly described|Map Legend||Ordovician|||||||
25904|Fairbridge Volcanics|43782|5|Briefly described|Map Legend|Gisbornian|Yapeenian|Of Kenilworth Group.||||||04-MAR-09
25904|Fairbridge Volcanics|50095|5|Briefly described|p109 Fig.2|Ordovician|Ordovician |||||||
25904|Fairbridge Volcanics|50097|4|Described|p41|Gisbornian|Darwillian|Unconformably overlies Hensleigh Silstone. Unconformably overlain by Catombol Group. Includes shallow water carbonates. Thickness: 2750 m. Geological Province: Lachlan Orogen. NSW||||||07-FEB-11
25904|Fairbridge Volcanics|60417|6|Mentioned|p155 Fig.2|Middle Ordovician||||||||
25904|Fairbridge Volcanics|60987|6|Mentioned|p154 Fig.1|Ordovician|Ordovician|||||||
25904|Fairbridge Volcanics|62478|4|Described|p88-89|Middle Ordovician|Early Ordovician|Volcaniclastic rocks. Phenocrysts of plagioclase, clinopyroxene and opaques. Age: 455.4 +/- 1.0Ma. Of the Copper Hill Intrusive Complex.||||||
25904|Fairbridge Volcanics|63278|5|Briefly described|p151|Late Ordovician|Middle Ordovician|Unconformably underlain by Hensleigh Siltstone. Geological Province: Molong Volcanic Belt, Lachlan Fold Belt. Consists of andesitic lavas, rare limestones yeilding conodonts. See also p151-152 for more information.||||||07-FEB-11
25904|Fairbridge Volcanics|63279|6|Mentioned|p175 Fig. 7|Ordovician|Early Ordovician|||||||
25904|Fairbridge Volcanics|63283|4|Described|p189-190 Tb. 1, p194 Fig. 2, p199|Gisbornian|Darriwilian|Includes; Wahringa Limestone Member, Yuranigh Limestone Member. Overlain by Reedy Creek Limestone. Age: 455-450Ma (basal basalt and pl-phyric basalt). Thickness: <2km. Divided into six units. See p200-202.||||||07-FEB-11
25904|Fairbridge Volcanics|63284|6|Mentioned|p249|Darriwilian|Darriwilian|Geological Province: Molong Volcanic Belt.||||||
25904|Fairbridge Volcanics|63285|6|Mentioned|p291 App. 1|||Underlain by Weemalla Formation. Geological Province: Molong Volcanic Belt.||||||
25904|Fairbridge Volcanics|63286|5|Briefly described|p308 Fig. 9|Late Ordovician|Middle Ordovician|Includes; Wahringa Limestone Member, Yaranigh Limestone Member. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
25904|Fairbridge Volcanics|63287|4|Described|p316, p317 Fig. 2, p319, p339-343|Gisbornian|Middle Ordovician|Of the Kenilworth Group. Overlain by Reedy Creek Limestone confomably to disconforambly. Geological Province: Molong Volcanic Belt. See p339 for more information on petrology.||||||07-FEB-11
25904|Fairbridge Volcanics|63289|6|Mentioned|p374|||||||||07-FEB-11
25904|Fairbridge Volcanics|63290|6|Mentioned|p397 Fig. 3(b)|Gisbornian|Middle Ordovician|Geological Province: Molong Volcanic Belt.||||||
25904|Fairbridge Volcanics|63293|5|Briefly described|p470, p468 Fig. 2, p473|Gisbornian|Darriwilian|Overlain by Reedy Creek Limestone. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
25904|Fairbridge Volcanics|64295|5|Briefly described|p198 Fig. 1|||Contains the Yuranigh and Wahronga Limestone Members. On the Molong Volcanic Belt.||||||01-SEP-08
25904|Fairbridge Volcanics|64826|5|Briefly described|p1040 Tb. 1|Gisbornian|Darriwilian|Of the Kenilworth Group. Contains the Wahringa Limestone Member and Yuranigh Limestone Member. Formerly Oakdale Formation.||||||04-MAR-09
25904|Fairbridge Volcanics|64963|5|Briefly described|p182 Fig. 2, p183|||Mapped as Oakdale Formation (Meakin and Morgan 1999) north of Wellington, but referred to as Cheesenmans Creek Formation by Percival and Glen (2007). ||||||
25904|Fairbridge Volcanics|67106|6|Mentioned|p673, 675-679, 681-683|||Molong Volcanic Belt. Age range determined as ~468 to 445 Ma.|464.6 +/- 3.2 Ma.|||||
25904|Fairbridge Volcanics|67107|5|Briefly described|p694|Middle Ordovician|Middle Ordovician|Copper Hill district.||||Is intruded by Copper Hill Intrusive Complex.|Andesitic volcanics and minor limestones.|
25904|Fairbridge Volcanics|67322|4|Described|p20 Fig.5, p23|Darriwilian|Darriwilian|Macquarie Arc. Named by Adriene (1971); described in detail by Morgan, Scott, and Percival, in Meakin and Morgan (1999). Conodont fauna suggest an early to mid-Darriwilian age. Occurs in the northern Molong Volcanic Belt.||Of the Cabonne Group.|Wahringa Limestone Member, Yuranigh Limestone Member||Includes allochthonous limestones.|21-FEB-18
25904|Fairbridge Volcanics|68592|5|Briefly described|p371, p378-9|||Molong-Wellington Volcanic Belt. Formerly part of Kenilworth Group which has been discontinued (Pogson et al., 2012) in favour of Cabonne Group.||Unit in Cabonne Group.|Includes Yuranigh and Wahringa, Limestone Members.|||
25904|Fairbridge Volcanics|69541|5|Briefly described|p646-647|Late Ordovician|Late Ordovician|Molong Volcanic Belt, Macquarie Arc. Zircons with subround and subangular shapes represent resorption during magma transport, not during sedimentary processes.|464.6 +/- 3.2 Ma: Glen et al. (2011).|||||
25904|Fairbridge Volcanics|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 2 volcanic units. Age: ranges from early Darriwilian (Da2) to latest Gisbornian. Molong Volcanic Belt.|c. 470-455 Ma|Cabonne Group|Yuranigh Limestone Member|||
25904|Fairbridge Volcanics|70684|5|Briefly described|p3, p12, p18-20, p25-30, p41, p74|Middle Ordovician|Middle Ordovician|Molong Volcanic Belt. Estimated thickness of c.2750m in the type area.|||Wahringa Limestone Member.|Is overlain unconformably by Reedy Creek Limestone and Hervey Group. Intruded by Copper Hill Complex. Is faulted against Oakdale Formation.|From the base: volcaniclastic and volcanic rocks, allochthonous limestone, monomictic conglomerate, autochthonous limestone, more volcaniclastic rocks (mainly breccias), lavas and pods of fossiliferous limestone.|
25904|Fairbridge Volcanics|70754|5|Briefly described|p447, p449, p450 Fig.2, p455, p458-459|Sandbian|Darriwilian|See also p465-466, p474-479. Contains the oldest documented lingulate brachiopods. Systematic palaeontological descriptions.|||Wahringa, Yuranigh, Limestone Members.|Is overlain ?unconformably by Reedy Creek Limestone.|Includes fossiliferous limestones.|
25904|Fairbridge Volcanics|72263|4|Described|p513,515-521,523-525|Ordovician|Middle Ordovician|Geological province: Lachlan Orogen. Crops out in the Molong Volcanic Belt. Also see 1:250 000 DUBBO and BATHURST maps (Morgan et al., 1999; Raymond et al., 1998). Thickness: up to 2km (Bakers Swamp area; Crawford et al., 2007a; Percival et al., 1999). Approximantely 9my hiatus with underlying Hensleigh Formation (fossil assemblages; Percival et al., 1999; Percival and Glen, 2007). Contains Early Darriwillian to Late Bolindian (~468-444 Ma) fossil assemblage. Limestone clasts in upper section of the unit indicate shallow marine environment proximal to a volcanic source. Intruded by Copper Hill Suite. Three main zircon age components at 444 Ma, 459 Ma and 470 Ma, interpreted to represent maximum depositional age, main age of volcanism and recycled material from Mitchell Fomation, respectively.||Unit of Cabonne Group.|Includes Yuranigh and Wahringa limestone members.|Overlain conformably by Reedy Creek Limestone or Cheesemans Creek Formation. Underlain unconformably by Hensleigh Formation.|Volcanic breccia, conglomerate and volcanic rocks, which are intercalated with finer volcaniclastic sandstones, volcanic sandstones and minor cherty siltstones.|16-JAN-20
25904|Fairbridge Volcanics|73154|6|Mentioned|p77 Fig.3, p92|Gisbornian|Darriwilian|Macquarie Arc, Phase 2. Molong Volcanic Belt, northern.||||||
25904|Fairbridge Volcanics|73264|6|Mentioned|p1390, p1391 Fig.13|Middle Ordovician|Early Ordovician|Lachlan Orogen, Macquarie Volcanic Province, phase 2.|459 Ma|||||
25904|Fairbridge Volcanics|73299|6|Mentioned|p1104 Fig.10, p1105|Late Ordovician|Ordovician|Macquarie Arc. Molong High. Middle to Upper Ordovician age.||||Underlies the Bowan Park Subgroup.||
25904|Fairbridge Volcanics|75070|6|Mentioned|p184|||||||||
33490|Fairholme Igneous Complex|63278|6|Mentioned|p145 Fig 1, p148|||Geological Province: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
33490|Fairholme Igneous Complex|63283|5|Briefly described|p185, p191 Tb. 2, p193, p199|Late Ordovician|Early Ordovician|Age: 480 and 445Ma (pillow basalt and hbd-phyric intrusive). Geological Province: Junee-Narromine Volcanic Belt. See p193.||||||07-FEB-11
33490|Fairholme Igneous Complex|63284|5|Briefly described|p255, p264-268, p245 Fig. 2|||Geological Province: Junee - Narromine Volcanic Belt. See also p264-268 for more information.||||||
33490|Fairholme Igneous Complex|67107|6|Mentioned|p695|Ordovician|Ordovician|Cowal district.||||||
33490|Fairholme Igneous Complex|67322|6|Mentioned|p21|||Described in detail by Crawford, Cooke, and Fanning (2007).||||||
33490|Fairholme Igneous Complex|70178|6|Mentioned|p4 fig. 2|Ordovician|Ordovician|Macquarie Arc.||||||
33490|Fairholme Igneous Complex|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
33490|Fairholme Igneous Complex|72495|6|Mentioned|p217-221, 228, 233, p235-236, 240|||Coincides in part with the south-western gravity high that is centered on 34degrees S. Best defined by geophysics with some exploration drillhole data.||||||26-MAR-20
80149|Faithful Coal Member|70791|5|Briefly described|p292, p293 Fig.17|Permian|Permian|Werris Creek coal mine: borehole WC030C. Appears as Faithfull Coal Member on p292.||Rowan Formation.||Is correlated with Bohena Coal Member (Mullaley Sub-basin).||28-SEP-17
31708|Falnash Granite|23214|4|Described|p257|Carboniferous|Carboniferous|Intrudes the Chesleigh Formation and the undifferentiated Turondale and Waterbeach Formations.||||||
31708|Falnash Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
31708|Falnash Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|of Bathurst Batholith.||||||
31708|Falnash Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
27403|Faraway Hills Quartzite|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (East).  Parent - Farnell Group .  Age - Ediacarian in text.||||||
27403|Faraway Hills Quartzite|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
27403|Faraway Hills Quartzite|22857|4|Described|Tb. 13.1 9 (insert p70-71)|Marinoan|Marinoan|Of the Farnell Group. Grey, silicified massive quartzite with white clay matrix. Age: ~580Ma. Max. thickness:40m. Geological Province: Adelaide Fold Belt. See also p400 App.1 Tb.A1.3.||||||
27403|Faraway Hills Quartzite|30261|4|Described|Table 1|||Marinoan age||||||
27403|Faraway Hills Quartzite|34563|4|Described|p65|||Stratigraphy P62.||||||
27403|Faraway Hills Quartzite|34812|3|Fully described|p102|||||||||
27403|Faraway Hills Quartzite|34814|6|Mentioned|Fig.2|||||||||
27403|Faraway Hills Quartzite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27403|Faraway Hills Quartzite|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
27403|Faraway Hills Quartzite|36960|6|Mentioned|Fig.2|||||||||
27403|Faraway Hills Quartzite|39214|5|Briefly described|p9|||||||||
27403|Faraway Hills Quartzite|41301|5|Briefly described|p92|||||||||
27403|Faraway Hills Quartzite|41429|5|Briefly described|p246|||||||||
27403|Faraway Hills Quartzite|41801|6|Mentioned|Fig.4|||||||||
27403|Faraway Hills Quartzite|60648|6|Mentioned|p48 Fig. 7|||||||||
27403|Faraway Hills Quartzite|66623|5|Briefly described|p13, p18, p428.|||Thick, extensive, quartz sandstone marker unit.||Unit in Farnell Group.||Overlies Picnic Creek Basalt. Is overlain by Fowlers Gap Formation.|Light-grey, medium- to coarse-grained, well-silicified quartzite, trace interstitial clay, trace lithic fragments, massive bedding.|
27403|Faraway Hills Quartzite|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Farnell Group.||||
27403|Faraway Hills Quartzite|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Farnell Group.||Overlies Sturts Meadows Silstone. Is overlain by Fowlers Gap Formation.|Massively-bedded, grey, medium- to coarse-grained quartzite; trace of interstitial clay and lithic fragments; disseminated limonite after sulfides.|07-SEP-15
35525|Farmcote Gneiss|24169|5|Briefly described|p677|Archean|Archean|||||||07-NOV-08
35525|Farmcote Gneiss|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|||||||
35525|Farmcote Gneiss|61258|6|Mentioned|p399|Paleoproterozoic|Paleoproterozoic|Age: >1704+/-3Ma and <1705+/-5Ma (Page et al 2000a,b). Geological Province: Broken Hill-Olary region (Redan Sub-block).||||||07-NOV-08
35525|Farmcote Gneiss|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
35525|Farmcote Gneiss|61735|5|Briefly described|p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1703+/-3 and 1705+/-3Ma U/Pb SHRIMP magmatic age.  Max metamorphic age 1605+/-3 Ma. Part of the Redan Block. See also p636 Fig. 2.||||||04-JUN-15
35525|Farmcote Gneiss|62536|5|Briefly described|p635-637, 639-640, 643|||Redan Block, Broken Hill area. Protolith magmatic age. Maximum metamorphic age 1605 +/- 3 Ma. Also referred to informally as Farmcote leucogneiss.|1705 +/- 3 Ma, 1703 +/- 3 Ma.|||||
35525|Farmcote Gneiss|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1705 +/- 4 Ma|||||19-DEC-21
35525|Farmcote Gneiss|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: >1704+/-3Ma, <1705+/-5Ma. Geological Province: Redan Sub-block||||||07-NOV-08
35525|Farmcote Gneiss|63866|5|Briefly described|p36|||Redan Subdomain of the Broken Hill Domain, Curnamona Province. |1705 +/- 5 Ma (Stevens, 2006)|||Overlies the Redan Gneiss.||
35525|Farmcote Gneiss|64097|2|Defined|p328 Appdx., p305 Fig. 2, p309|Paleoproterozoic|Paleoproterozoic|Top of Rantyga Group - equiv.to Lady Brassey Fm.+ Alma Gneiss(Thackaringa Gp) in Broken Hill/Euriowie Inliers.Overlies Mulculca Fm; overlain by Cues Fm. Max. age: 1705+/-5Ma (SHRIMP zircon). Thickness:~1-5km.||||||07-FEB-11
35525|Farmcote Gneiss|64316|5|Briefly described|p532, p533 Fig. 1, p539, p548|Paleoproterozoic|Paleoproterozoic|Informally named intrusive. Age:ca.1703Ma (SHRIMP U-Pb); crystallisation age reported as ca.1650Ma.Geol.Prov: Broken Hill Block/ Redan Geophysical Zone. Leucocratic felsic orthogneiss - composed of quartz-albitic plagioclase+/-K-feldspar+/- biotite||||||07-FEB-11
35525|Farmcote Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Rantyga Group. Age: 1705+/-4Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
35525|Farmcote Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1705+/-4Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
35525|Farmcote Gneiss|66302|5|Briefly described|p36 Fig.9, p39, p41|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Rantyga Group||Overlies the Mulculca Formation.||
35525|Farmcote Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.||Rantyga Group.||||
35525|Farmcote Gneiss|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
35525|Farmcote Gneiss|68126|6|Mentioned|p26, p30|||Oldest rocks in the Broken Hill Domain, Curnamona Province.|1705 +/- 5 Ma (Stevens et al., 2008).|||||
35525|Farmcote Gneiss|70000|5|Briefly described|p34-36|Statherian|Statherian|Intruded by A-type granite gneisses at c.1704 Ma.|1705 +/- 5 Ma (Stevens, Page and Crooks 2008).|Unit in Rantyga Group.||Correlated with Lady Brassey Formation.||
35525|Farmcote Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Rantyga Group.||Overlies Mulculca Formation.|Leucocratic albite-quartz rich metasedimentary rock, leucocratic quartz-K feldspar-plagioclase(+/- biotite, magnetite) gneiss and basic gneiss.|07-SEP-15
35525|Farmcote Gneiss|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|1705 +/- 4 Ma|Rantyga Group.||Overlies Mulculca Formation. Is overlain by Thackaringa Group.||
35525|Farmcote Gneiss|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|1705 +/- 4 Ma.|||||
35525|Farmcote Gneiss|72461|5|Briefly described|p16 fig 9|||Redan sub-block of the Broken Hill Block.|1704 +/- 3 Ma; 1705 +/- 5 Ma|Rantyga Group||Overlies the Mulculca Formation.||
35525|Farmcote Gneiss|73243|6|Mentioned|p53 Fig.2|||||||||
35525|Farmcote Gneiss|73482|5|Briefly described|p422 Fig.3|Statherian|Statherian|Redan sub-block.|1704+/-3 Ma, 1705+/-5 Ma|Rantyga Group||||
35525|Farmcote Gneiss|73575|5|Briefly described|p828 Fig.2|Statherian|Statherian|Redan Geophysical Zone.|<1703+/-3 Ma, 1705+/-5 Ma|Rantyga Group||||
24609|Farmers Creek Formation|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wallerawang Subgroup (Illawarra Coal Measures). Contains the Middle River seam. Claystone, carbonaceous claystone, mudstone, tuffaceous shale, coal. Max. thickness: 40m. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
24609|Farmers Creek Formation|38614|6|Mentioned|p14|||||||||
24609|Farmers Creek Formation|39232|4|Described|p111|||||||||
24609|Farmers Creek Formation|40332|6|Mentioned|Fig.4|||||||||
24609|Farmers Creek Formation|40806|2|Defined|p158|Permian|Permian|Prob. Permian||||||
24609|Farmers Creek Formation|42657|4|Described|p84|||||||||
24609|Farmers Creek Formation|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
24609|Farmers Creek Formation|43194|5|Briefly described|p116|Late Permian|Late Permian|Of Wallerawang Subgroup, Illawarra Coal Measures, western Sydney Basin. With Gap Sandstone, a lithofacies equivalent of the 'Tuffaceous coaly unit' (now Trinkey Formation) of the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
24609|Farmers Creek Formation|68004|5|Briefly described|p60 Table 6, p62.|Late Permian|Late Permian|Western Coalfield. Thickness from 20 m to 60 m. In parts of the Ulan area, it has been almost entirely eroded. Several thin coal layers may locally coalesce to form the "Woodford seam".||Unit in Wallerawang Subgroup.|Includes Middle River Coal Member and the "Woodford seam".|Overlies State Mine Creek Formation and Gap Sandstone. Is overlain by Katoomba Coal.|Claystone, carbonaceous claystone, siliceous claystone, siltstone, sandstone, coal and oil shale.|
35115|Fassifern coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal name. Of the Boolaroo Formation (Newcastle Coal Measures). ||||||
35115|Fassifern coal seam|23055|6|Mentioned|p26,29|||||||||
35115|Fassifern coal seam|68711|5|Briefly described|p118, p116 Tbl 2|||Informal unit.||Within Boolaroo Formation||||
31675|Federal Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31675|Federal Suite|44093|5|Briefly described|p198 App.1|Early Devonian|Late Silurian|In the Canberra Block. Geological Province: Lachlan Fold Belt.||||||
32686|Fencers Creek Conglomerate Member|22638|1|Redefined|p50|Early Silurian|Early Silurian|Of Blowering Formation.||||||
32686|Fencers Creek Conglomerate Member|22857|5|Briefly described|p452 App.1, Tb.A1.6|Silurian|Silurian|Of the Blowering Formation. Stretched pebble conglomerate, sandstone, claystone.||||||
32686|Fencers Creek Conglomerate Member|44192|5|Briefly described|Map Legend|Llandoverian|Llandoverian|Of Blowering Formation.||||||
32686|Fencers Creek Conglomerate Member|44936|5|Briefly described|Map Legend||Silurian|||||||
32686|Fencers Creek Conglomerate Member|60280|5|Briefly described|p2, p3 Fig. 1|Early Silurian|Early Silurian|Of the Brawlin Formation.||||||12-JAN-05
78693|Fenestella Shale Member|68493|3|Fully described|p6,  p14-21, p3 Fig.1, p5 Fig.2|Wordian|Wordian|Formerly 'Fenestella Shale' of Jones(1939). Formalised herein. Contains fenestellid bryozoa and brachiopods (spiniferides and productoids); bivalve molluscs next in abundance; minor gastropods, rostroconchs, corals, trilobites and echinoderms (crinoids and blastoids). 30-60 m thick. Type locality: Mulbring quarry at 32deg54'00"S, 151deg28'12"E. Deposited during Fielding et al.'s (2008) glacial episode P3.|ca. 271.4 Ma, CA-IDTIMS (Metcalfe et al. 2012). |Of the Branxton Formation.|||Consists of interbedded yellowish brown micaceous shale and siltstone, with sparse bands of very thin calcareous mudstone.|12-MAR-14
35171|Fennell Bay Member|23055|6|Mentioned|Fig23p37|||||||||
25907|Fentonville Tonalite|22815|4|Described|p51|Early Devonian|Late Silurian|||||||
25907|Fentonville Tonalite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
25907|Fentonville Tonalite|35109|2|Defined|p74|Early Devonian|Late Silurian|Late Silurian to Early Devonian. On P74 and/or P75||||||
25907|Fentonville Tonalite|36411|6|Mentioned|p268|||Refers White et al 1977 for definition.||||||
25907|Fentonville Tonalite|40328|4|Described|p205|||||||||
25907|Fentonville Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Jindabyne Suite.||||||
25907|Fentonville Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh12||||||
25907|Fentonville Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
75834|Fenwicks Creek Serpentinite|65317|6|Mentioned|p622 Fig. 1c|||||||||
76847|Feral gneiss|65681|4|Described|pp733-747.|Paleoproterozoic|Paleoproterozoic|An informal name used in this article for a felsic gneiss with a relatively minor outcrop area, northeast of Broken Hill airport. The name of this informal unit has been taken from Feral Park, a horsestud. Intensely folded; contains first tectonic foliation that anastomoses around the 35 mm megacrysts; myrmekite at grain margins.||Unit in Willyama Supergroup.||Intruded by Alma Gneiss.|Light-grey, leucocratic, megacrystic, felsic gneiss with non-aligned, euhedral to subhedral K-feldspar megacrysts in a coarse- to medium-grained groundmass of quartz, alkali feldspar, plagioclase, biotite and minor sillimanite.|14-MAY-13
29586|Fernside Monzodiorite|22679|4|Described|p 39, 40|||formerly Fernside Diorite||||||
29586|Fernside Monzodiorite|23214|2|Defined|p91|Late Ordovician|Late Ordovician|Intrudes Blayney Volcanics. Forms an elongate intrusion 3.5km in length and about 0.5km in width.||||||
29586|Fernside Monzodiorite|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Clinopyroxene monzonite and diorite.||||||17-JUL-08
29586|Fernside Monzodiorite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29586|Fernside Monzodiorite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
76950|Fife Monzogranite|71628|5|Briefly described|p17: 1-2, 20, 95-96|||Originally the Fife Adamellite of Kinney et al. (1985), after unpublished work by Leitch (1972). Named (possibly mistakenly) after Fife Knob; crops out on Bald Knob in a 5 x 1 km E-W intrusion, 16 km SW of Bellbrook. Part of Coastal Granite Association. Is associated with a single, minor Mo deposit.||Fife Suite.||Intrudes Parrabel beds.|Fine-grained, leucocratic biotite-hornblende monzogranite to monzogranite-syenogranite. Is cut by quartz and aplitic veins.|
40945|Fifeshire Shale|50230|5|Briefly described|map legend|Pragian|Pragian|Of the Murrumbidgee Group.  Overlies the Sugarloaf Creek Formation; underlies the Cavan Bluff Limestone.  Shale, siltstone, minor tuffaceous sandstone.||||||
40945|Fifeshire Shale|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Murrumbidgee Group. Shale, siltstone, minor tuffaceous sandstone.||||||
40945|Fifeshire Shale|68592|3|Fully described|p936, p975, p982-4, p986, p989-p93|Pragian|Pragian|New name suggested by Koluzs (1972), after Fifeshire property. These rocks were previously included in Cavan Bluff LImestone or Sugarloaf Creek Formation. This unit marks the major change from volcanic and volcaniclastic deposition (Black Range Group) to mainly carbonate deposition (Murrumbidgee Group) and is essentially transitional. Type section described. 30-85m thick.||Basal unit in Murrumbidgee Group.||Gradationally overlies Sugarloaf Creek Formation (Black Range Group). Is overlain conformably by Cavan Bluff Limestone.|Predominantly red-grey, massive to finely-laminated shale or mudstone, with lesser amounts of calcareous shale and fine- to very fine-grained, poorly sorted sandstone and irregularly spaced beds of silty, micritic limestone.|
40945|Fifeshire Shale|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dmf. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Murrumbidgee Group||Overlies Sugarloaf Creek Formation (Black Range Group). Is overlain by Cavan Bluff Limestone.|Red-grey, massive to finely laminated shale or mudstone with lesser amounts of calcareous shale and fine-very fine grained, irregularly spaced beds of silty micritic limestone.|
40945|Fifeshire Shale|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|||Red-grey, massive to finely laminated shale or mudstone with lesser amounts of calcareous shale and fine-very fine grained, irregularly spaced beds of silty micritic limestone.|
40945|Fifeshire Shale|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|||Red-grey, massive to finely laminated shale or mudstone with lesser amounts of calcareous shale and fine-very fine grained, irregularly spaced beds of silty micritic limestone.|
40945|Fifeshire Shale|71656|6|Mentioned|p12 Fig.2|Pragian|Pragian|Shown only in correlation chart (Fig.2).||Base of Murrumbidgee Group.||Overlies Sugarloaf Creek Formation, and Black Range Group.||
77333|Fifield Suite|69635|6|Mentioned|p70||||||Includes Honeybugle Complex.|||
77333|Fifield Suite|70751|6|Mentioned|p4, p6, p15|Ordovician|Ordovician|||||||
77333|Fifield Suite|71039|6|Mentioned|p6|Silurian|Silurian|||||||
77333|Fifield Suite|71693|5|Briefly described|Map legend; p2.|Silurian|Silurian|Is associated with Ni-Co-Sc laterites resulting from prolonged weathering in the Tertiary. Distribution inferred from drilling and geophysics.||||Intrudes Girilambone Group.|Alaskan-type ultramafic to mafic igneous rocks with minor monzonitic differentiates.|13-SEP-19
77333|Fifield Suite|72908|6|Mentioned|p4|Ordovician|Ordovician|||||||
77333|Fifield Suite|73578|6|Mentioned|p2|Ordovician|Ordovician|Cobar Basin.||||||
23591|Fifteen Mile Tank Conglomerate Member|22857|4|Described|p440 App.1, Tb.A1.6|Devonian|Devonian|Of the Boothumble Formation. Clast-supported pebble and cobble conglomerate and arenite. Max. thickness: 1000m. Geological Province: Mouramba Shelf.||||||
23591|Fifteen Mile Tank Conglomerate Member|41394|2|Defined|p63|Early Devonian||||||||
23591|Fifteen Mile Tank Conglomerate Member|41395|6|Mentioned|Map legend|Lochkovian||||||||
23591|Fifteen Mile Tank Conglomerate Member|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
23591|Fifteen Mile Tank Conglomerate Member|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Of Boothumble Formation?, Mouramba Group||||
75943|Figtree Creek Ignimbrite Member|65902|5|Briefly described|p203 Fig.7|Serpukhovian|Serpukhovian|Of Currabubula Formation. Overlies Coeypolly Conglomerate Member in the Werrie Syncline.||||||09-MAR-12
70081|Finch clay facies|22857|5|Briefly described|p544 App.1 Tb.A1.12|Albian|Albian|Not intended as a formal name. Contained within the Wallungulla Sandstone Member (Griman Creek Formation, Rolling Downs Group). Grey to buff, montmorillonite-rich claystone. Max. thickness: 6m. Geological Province: Surat Basin.||||||
70081|Finch clay facies|68069|5|Briefly described|p2.|Early Cretaceous|Early Cretaceous|Informal name.||Unit in Wallangulla Sandstone Member.|||Soft, grey to buff claystone; hardens and whitens upon drying; top metre hosts opal.|
70081|Finch clay facies|68593|5|Briefly described|p5, p33|Albian|Albian|Byrnes (1977). Lenses of the clay facies are 1.2 to 6m thick, but usually 1-2m. Hosts much of the precious black opal in the upper 1m or so. Source of a diverse range of fossils. Appears on p84 as Finch Claystone facies: a concatenation of the two informal names, Finch Claystone and Finch clay facies.||Wallangulla Sandstone Member.|||"Opal dirt", grey to buff montmorillonite-rich claystone; numerous clay beds interbedded with sandstone.|
70081|Finch clay facies|71601|6|Mentioned|p121|Albian|Albian|Geological province: Surat Basin.||Unit of Griman Creek Formation.||Overlain by Wallangulla Sandstone Member.||
35395|Fitz Creek beds|61392|5|Briefly described|p164 Fig. 1|Middle Permian|Middle Permian|Of the Wildash Group.||||||07-FEB-11
35395|Fitz Creek beds|63731|5|Briefly described|Map legend|Permian|Permian|Conglomerate, volcaniclastic arenite, rhyolitic tuff. Polymictic, granule to boulder conglomerate; minor arenite and tuff. Massive, poorly sorted, dark grey rhyolitic lithi-crystal tuff, lapilli tuff and crystal tuff.||||||
35395|Fitz Creek beds|63748|4|Described|p7 Fig. 3, p20-21|Late Permian|Middle Permian|Originally mapped as Connolly Volcanics (Olgers et al 1974). Unconformably on Silverwood Group rocks, mainly Connolly Volcanics. Locally intruded by part of Herries Granite.  Max. thickness: ~1770m. Dominated by conglomerate. In the Wandsworth Province.||||||07-FEB-11
35395|Fitz Creek beds|68679|5|Briefly described|p446, p453|Permian|Permian|Olgers et al. (1974) included these rocks in the Connolly Volcanics; recognised as a separate unit by Dennis (1974) and Van Noord (1999), the latter proposing this name for two irregular areas each ~2.5 km2 about 18km S of Warwick. Silver Spur Subprovince, Woolomin Province. Estimated 314-1770m thick. Conglomerates are most common, ranging from matrix-supported to graded or inversely graded clast-supported varieties. No fossils have been recovered. Lithologically similar to nearby Rhyolite Range beds.||Wildash Group.||Unconformably overlies or is faulted against Connolly Volcanics. Is intruded by Herries Granite. May correlate with Rhyolite Range beds.|Massive thick-bedded conglomerates. Massive, poorly-sorted rhyolitic lithic-crystal tuff, lapilli tuff and crystal tuff are interbedded with minor rhyolite lava and massive, very coarse-grained volcaniclastic sandstone.|
74779|Five Mile Creek Syenogranite|61789|4|Described|p303, 310-311|Triassic|Triassic|Previously mapped as Stanthorpe Adamellite.  Age: 242.2 Ma (Shaw 1994), probably Rb-Sr. Of Stanthorpe Granite Group.||||||14-OCT-08
74779|Five Mile Creek Syenogranite|61790|6|Mentioned|p318, p319, p320|||||||||
74779|Five Mile Creek Syenogranite|71628|5|Briefly described|p11: 38; p16: 8, 11|||Sivell and Passmore (1999) after unpublished work by Passmore (1998). Previously part of Stanthorpe Monzogranite. Renamed (this study) Five Mile Creek Syenogranite Phase (of Cullendore Syenogranite).||||||
82447|Flaggy Range Monzogranite Phase|71628|5|Briefly described|p4: 1, 4, 8, 10-11, 14-16, 38|||New subunit. Southern New England Orogen. Named after the local range of hills. Lithology and geochemistry much the same as the parent.||Banalasta Monzogranite.||Abuts Pringles and MacDonald River Monzogranites. Is intruded by Looanga and Bendemeer Monzogranites (Moonbi Supersuite), Fox Tor Quartz Diorite and ?Mountain Home Granite.|A more mafic phase than the eastern part of the parent.|
26556|Fleming Coal Member|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
26556|Fleming Coal Member|40331|6|Mentioned|p13|||||||||
25911|Flying Fox Gully Trachyandesite Member|29915|2|Defined|p66|Late Carboniferous|Middle Carboniferous|Middle or Upper Carboniferous||||||
83654|Focal Peak Volcanics|73581|5|Briefly described|p7||||||Albert Basalt, Kyogle Basalt||Scattered basaltic and felsic volcanic units. Includes numerous thin basal basalt lava units, interbedded with volcaniclastics.|
34596|Folly Point Limestone Member|5253|5|Briefly described|p97|Devonian|Early Ludlow|Bottom member of Frome Hill Formation. Equivalent to Middle Limestone of Carr et al. 1990.||||||16-JAN-12
34596|Folly Point Limestone Member|22842|4|Described|p29|Early Devonian|Late Silurian|||||||
34596|Folly Point Limestone Member|50234|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Frome Hill Formation (Bungonia Group).||||||
34596|Folly Point Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Frome Hill Formation (Bungonia Group).  Fossiliferous limestone interbedded with well-sorted, medium-grained, fossiliferous sandstone.||||||
34596|Folly Point Limestone Member|68592|3|Fully described|p898, p900, p914-6, p918-21, p1892|Pridoli|Pridoli|Name first published by James, Francis and Jennings (1979) referring to Carr et al.'s (1979) 'Middle Limestone' of the Bungonia Limestone. Bauer (1994) formally defined it as a unit of Frome Hill Formation. Type locality described. Thickness to 225m.||Basal unit in Frome Hill Formation.||Overlies Tangerang Formation unconformably or with faulted contact. Locally overlain conformably by Efflux Siltstone Member or Sawtooth Ridge Limestone Member.|Sequence of fossiliferous limestone (mostly biomicrite or biomicrudite, with common biosparrudite), interbedded with well-sorted, medium-grained, fossiliferous calcareous sandstone.|
34596|Folly Point Limestone Member|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Sbff. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Frome Hill Formation|||Fossiliferous limestone interbedded with well-sorted, medium-grained, fossiliferous calcareous sandstone.|
34596|Folly Point Limestone Member|70542|5|Briefly described|Map Legend|Silurian|Silurian|||Frome Hill Formation|||Fossiliferous limestone interbedded with well-sorted, medium-grained, fossiliferous calcareous sandstone.|
34596|Folly Point Limestone Member|70661|3|Fully described|p31 tbl 1, p44-p46|Lochkovian|Pridoli|Name derived from Folly Point (a bluff). Termed the middle limestone of Bungonia Limestone previously. Ranges from 25m thick to 250m thick.Likely deposited in marine barrier system. Has a gentle westerly dip and has no significant geomorphic expression. Metamorphism, geophysical characteristics and fossil assemblage described.||Frome Hill Formation||Faulted over Cardinal View Formation, conformably overlain by Efflux Siltstone Member and the Sawtooth Ridge Limestone Member, also overlain by Tangerang Formation|Fossiliferous limestone interbedded with well sorted, medium grained, fossiliferous calcareous sandstone. The limestone consists mostly of biomicrite or biomicrudite.|07-JUL-20
34596|Folly Point Limestone Member|71303|5|Briefly described|map legend|Ludlow|Ludlow|||Of Frome Hill Formation.|||Fossiliferous limestone, mostly biomicrite or biomicrudite; interbedded with well-sorted, medium-grained, fossiliferous calcareous sandstone.|
34596|Folly Point Limestone Member|71700|5|Briefly described|p16|Late Silurian|Late Silurian|Bungonia Shelf. Interpreted to have been deposited in a carbonate shelf system in varied environments including tidal flats, reefs and marine barriers.||Frome Hill Formation||Overlain by the Efflux Siltstone Member.||
37289|Folly Volcanics|24008|5|Briefly described|p355|Late Devonian|Middle Devonian|||||||
37289|Folly Volcanics|24009|6|Mentioned|p368|||Also referred to as Folly Basalt.||||||13-NOV-08
37289|Folly Volcanics|61730|6|Mentioned|p1027|Late Devonian|Middle Devonian|In the Glenrock station area. Geological Province: New England Orogen.||||||
37289|Folly Volcanics|68005|5|Briefly described|p52.|||Tamworth Belt.||Unit in Tamworth Group.||Intrudes and is interbedded with Silver Gully and Yarrimie Formations.|Mafic intrusions including quite thick dolerite sills, and altered basalts.|
37289|Folly Volcanics|73440|6|Mentioned|p129-130, p132|Late Devonian|Late Devonian|[Also written as Folly volcanics, p129]. Gamilaroi terrain.|||||Massive and pillowed basalts.|
25912|Forbes Group|13139|5|Briefly described|p9 Fig. 4|Early Silurian|Early Silurian|Geological Province: Junee-Narromine Volcanic Belt.||||||
25912|Forbes Group|22519|6|Mentioned|p7|Devonian|Ordovician|||||||
25912|Forbes Group|22768|6|Mentioned|p175|Late Silurian|Silurian|||||||
25912|Forbes Group|22831|5|Briefly described|p 34||Wenlockian|||||||
25912|Forbes Group|22857|5|Briefly described|p175, p450 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Max. thickness: 3.5m. Geological Province: Bogan Gate Terrace.||||||
25912|Forbes Group|23309|6|Mentioned|p390|||||||||
25912|Forbes Group|23334|5|Briefly described|9 Fig.4|Silurian|Early Silurian|||||||
25912|Forbes Group|23454|5|Briefly described|p32|Silurian|Silurian|||||||
25912|Forbes Group|24125|5|Briefly described|p3|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
25912|Forbes Group|24267|4|Described|p1508|Late Silurian|Silurian|Overlying Unit: Milpose Volcanics. Underlying Unit: Girilambone Group. Geological Province: Parkes-Narromine Belt||||||
25912|Forbes Group|24417|3|Fully described|p42|Silurian|Silurian|Originally termed "Forbes Beds".  Overlain by Douro Group.||||||
25912|Forbes Group|29907|6|Mentioned|p8|||||||||
25912|Forbes Group|29910|6|Mentioned|Map legend|Silurian|Silurian|||||||
25912|Forbes Group|31722|6|Mentioned|p136|||Stratigraphy||||||
25912|Forbes Group|32412|6|Mentioned|p86|||||||||
25912|Forbes Group|32917|6|Mentioned|p130|||Research on Sil. graptolites||||||
25912|Forbes Group|33118|5|Briefly described|p1|||M.-U. Sil. Formerly Forbes Beds.||||||
25912|Forbes Group|33121|3|Fully described|p65|||Mid.-Late Sil. See also PP66-71.||||||
25912|Forbes Group|33122|6|Mentioned|p149|||Refers Brunker (1972) & Sherwin (1973)||||||
25912|Forbes Group|33124|6|Mentioned|p227|||||||||
25912|Forbes Group|33125|6|Mentioned|p15|||Correlation chart||||||
25912|Forbes Group|35185|6|Mentioned|p231|||||||||
25912|Forbes Group|36066|6|Mentioned|p11|||||||||
25912|Forbes Group|37727|3|Fully described|p59|||Formerly Forbes Beds||||||
25912|Forbes Group|39214|5|Briefly described|p18|||||||||
25912|Forbes Group|39618|6|Mentioned|Fig.7|||||||||
25912|Forbes Group|39656|6|Mentioned|Fig.1|||||||||
25912|Forbes Group|40328|3|Fully described|p39|||||||||
25912|Forbes Group|40891|4|Described|p14|||Formerly Forbes Beds||||||
25912|Forbes Group|41793|6|Mentioned|p109|||||||||
25912|Forbes Group|42262|6|Mentioned|Fig. 2 P1810|||||||||
25912|Forbes Group|42489|5|Briefly described|Map legend|Ludlow|Wenlock|||||||
25912|Forbes Group|43263|6|Mentioned|Map Legend|Late Silurian||Age Middle-Late Silurian.||||||
25912|Forbes Group|43441|5|Briefly described|21, 24|||Age: Middle Silurian to Late Silurian||||||08-JAN-10
25912|Forbes Group|44093|5|Briefly described|p115|Silurian|Silurian|Clastic sediments. See also pp178-179 and p181, Appendix 1.||||||
25912|Forbes Group|44160|5|Briefly described|Map Legend|Ludlovian|Wenlock|||||||08-JAN-10
25912|Forbes Group|46522|2|Defined|p58|Late Silurian|Early Silurian|||||||
25912|Forbes Group|46525|6|Mentioned|p149|||||||||
25912|Forbes Group|46528|5|Briefly described|Map legend|Silurian||||||||
25912|Forbes Group|50299|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Mumbidgle Formation, Bocobidgle Conglomerate.||||||
25912|Forbes Group|60008|5|Briefly described|Map Legend|Silurian|Silurian|Sediments.||||||
25912|Forbes Group|60009|5|Briefly described|Map Legend|Ludlow|Wenlock|Includes: Mumbidgle Formation, Bocobidgle Conglomerate.||||||13-JUL-04
25912|Forbes Group|60548|5|Briefly described|map legend|Silurian|Silurian|||||||
25912|Forbes Group|62569|5|Briefly described|p607 Fig. 2|Late Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||10-AUG-07
25912|Forbes Group|63283|6|Mentioned|p192|Silurian|Silurian|Sedimentary rocks.||||||07-FEB-11
25912|Forbes Group|63288|6|Mentioned|p353, p355, p361||Wenlock|Includes Mumbidgil Formation.||||||
25912|Forbes Group|63289|6|Mentioned|p373 Fig. 7, p374, p380|Wenlock|Wenlock|Contains Silurian fossils.||||||07-FEB-11
25912|Forbes Group|63290|5|Briefly described|p395, p397 Fig. 3(b)|Silurian|Wenlock|Includes; Bocobidgle Conglomerate, Bocobidgle Formation. Sandstone in lower part of group contains rare defoemed metamorphic clasts and corse grained biotite and rounded volcanic quartz. Geological Province: Junee - Narromine Volcanic Belt.||||||
25912|Forbes Group|63291|6|Mentioned|p419 Fig. 2|||||||||
25912|Forbes Group|63293|6|Mentioned|p468 Fig. 2||Wenlock|Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
25912|Forbes Group|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
25912|Forbes Group|67107|6|Mentioned|p696|||Peak Hill, c.45km N of Parkes.||||||
25912|Forbes Group|67805|6|Mentioned|p73|Ordovician|Ordovician|||||||
25912|Forbes Group|67821|6|Mentioned|p150, p177|Silurian|Silurian|Strongly deformed sediments. Appears as Forbes group on p150.||||||08-FEB-18
25912|Forbes Group|67847|6|Mentioned|p24||||||Includes the Mumbidgle Formation.|||
25912|Forbes Group|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
25912|Forbes Group|70684|6|Mentioned|p54 Fig.27, p55, p74-75|Early Silurian|Early Silurian|Junee-Narromine Volcanic Belt. Wenlock.||||||
25912|Forbes Group|70751|6|Mentioned|p13|Wenlock|Wenlock|Forbes 1:250k map sheet area. Age is derived from graptolite fauna (Sherwin, 2010).||||Unconformably overlain by the Mineral Hill Volcanics.||
25912|Forbes Group|71040|6|Mentioned|p13, p15, p17-18|Silurian|Silurian|Eastern limb of the Forbes Anticline. Underwent considerable shortening from the Tabberabberan Orogeny.||||||
25912|Forbes Group|72495|5|Briefly described|p218, 225, 227,228,230-231,233,235-236|Late Silurian|Early Silurian|Highly deformed rocks. Exhibits low magnetisation and low Bouger gravity values. Densities of 2.65-2.67 t/m^3 and magnetic susceptibilities of zero were used for modelling.||||Faulted against the Parkes Volcanics and the Cotton Formation.|Includes sandstone and mudstone.|31-MAR-20
25912|Forbes Group|73154|6|Mentioned|p77 Fig.3|Wenlock|Wenlock|||||||
74591|Forest Lodge Quartz Monzodiorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Grey, medium-grained, porphyritic, quartz monzodiorite with large crystals of plagioclase and augite set in an equigranular mosaic of plagioclase, pyroxene (clinopyroxene and orthopyroxene), K-feldspar, and miarolitic cavities||Turrallo Suite||||06-APR-10
74591|Forest Lodge Quartz Monzodiorite|68592|2|Defined|p1056-8, p1168, p1650-63, p1666|Pragian|Pragian|See also p786, p795, p730 Fig.132, p821, p831-2, p834, p836, p839, p853, p868, p1042. New  name, after Forest Lodge property and homestead. This unit subsumes the Forest Lodge Granite (actually a quartz monzodiorite), as well as the Turrallo Quartz Diorite of Scheibner (1973) due to pronounced lithological similarity. Typically forms scattered low blocky to bouldery exposures with larger tors in places. Type and representative localities described. A xenolithic dacite porphyry component described by Scheibner (1973) is probably the Back Station Ignimbrite Member of Gundary Volcanics. Geochemistry detailed; remarkably similar geochemistry to Bushranger Volcanics (Crudine Group), 50km away, as well as Saltpetre Andesite Member (Quialigo Volcanics), which is suggested to be the extrusive equivalent of this unit. Geophysical properties described. Contact metamorphism occurs to rocks intruded. Inferred mid to late Pragian age from correlation with other units.||Unit in Turrallo Suite.||Intrudes Mount Fairy Group. Is overlain unconformably by Crookwell Basalt and Strathaird Formation. Correlated with Saltpetre Andesite Member.|Dark green-grey, quartz monzodiorite to borderline quartz monzonite, equigranular to porphyritic in plagioclase, and augite up to 8mm. Characteristic pale green plagioclase and salmon pink K-feldspar crystals. I-type.|
74591|Forest Lodge Quartz Monzodiorite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dff. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.||Turrallo Suite|||Quartz monzodiorite to borderline quartz monzonite; equigranular-porphyritic in plagioclase, augite and orthopyroxene, hornblende and rare biotite up to 8mm; K feldspar and green sericitised plagioclase crystals are distinctive.|
74591|Forest Lodge Quartz Monzodiorite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Turrallo Suite|||Quartz monzodiorite to borderline quartz monzonite; equigranular to porphyritic in plagioclase, augite, orthopyroxene, hornblende with rare biotite up to 8mm. Salmon pink K feldspar and green sericitised plagioclase crystals are distinctive.|
74591|Forest Lodge Quartz Monzodiorite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Turrallo Suite|||Quartz monzodiorite to borderline quartz monzonite; equigranular-porphyritic in plagioclase, augite and orthopyroxene, hornblende and rare biotite up to 8mm; K feldspar and green sericitised plagioclase crystals are distinctive.|
74591|Forest Lodge Quartz Monzodiorite|71069|6|Mentioned|p137 fig 44, p147, p170|||||||Intrudes the Rhyanna Formation and Covan Creek Formation. Overlain by the Bradfordville Volcaniclastic Member.||
29306|Forest Range Member|22736|6|Mentioned|p623|Namurian|Visean|after Hamilton 1982||||||
29306|Forest Range Member|38803|5|Briefly described|p106|||||||||
23600|Fosters Creek Conglomerate|22679|4|Described|p 26|||||||||
23600|Fosters Creek Conglomerate|22857|5|Briefly described|p472 App.1 Tb.A1.6|Devonian|Silurian|Of the Mumbil Group. Max. thickness: >100m. Geological Province: Hill End Trough. ||||||
23600|Fosters Creek Conglomerate|23214|4|Described|p142|Late Silurian|Late Silurian|Of Mumbil Group. Oligomictic boulder conglomerate, meta feldspathic quartz arenite and siltstone.||||||
23600|Fosters Creek Conglomerate|42712|4|Described|8, Table1 p14.|Early Devonian|Late Silurian|Within Campbells/Kildrummie Group. Unconformable on Rockley Volcanics, conformable below Campbells Formation.||||||
23600|Fosters Creek Conglomerate|43639|5|Briefly described|Map Legend||Silurian|||||||
23600|Fosters Creek Conglomerate|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group (east). Oligomictic boulder conglomerate, feldspathic quartz sandstone, siltstone.||||||17-JUL-08
23600|Fosters Creek Conglomerate|43782|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Mumbil Group.||||||11-JUN-08
23600|Fosters Creek Conglomerate|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Green-grey, massive matrix- to clast-supported polymictic conglom.+ pebbly sst. beds up to 2m thick, composed of well-rounded to angular clasts of crystal-rich to fine-gr.andesite, feldspathic sst., quartzose sst.+minor chert...||||||09-SEP-08
23600|Fosters Creek Conglomerate|68592|2|Defined|p398, p425-6, p608, p613, p627-31, p750|Ludlow|Wenlock|See also p376, p391. Wallace and Stuart-Smith (1994); named after Foster Creek homestead, 9km E of Trunkey. Type locality described. c.200-300m thick. Well-cleaved and dips steeply (~85 degrees) to SE. Probably Middle Silurian. Geophysical properties described. Unfossiliferous. Is correlated with Shivering Conglomerate. Basal conglomeratic units could be reworked material at the top of the Rockley Volcanics. Marks the first episode of sedimentation associated with the opening of the Hill End Trough.||Basal unit in Campbells Group.||Overlies Rockley Volcanics (?) unconformably and Triangle Formation disconformably. Is overlain conformably by Cuddyong Formation and Kangaloolah Volcanics, and by Wheeo Basalt.|Polymictic conglomerate: 2m thick beds of coarse-grained mixed-provenance (volcanic and quartzose) reworked detritus; clast- to matrix-supported; interbedded with medium-grained pebbly sandstone and cherty siltstone.|
23600|Fosters Creek Conglomerate|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Scf. Conglomerate, pebbly sandstone and cherty siltstone beds up to 2m thick. Feldspathic sandstone, quartzose sandstone and minor chert and cherty siltstone clasts set in a medium grained lithic feldspar quartz sandstone matrix. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Campbells Group||Erosional at base. Basal unit in Campbells Group. Is overlain by, and interfingers with, Cuddyong Formation.|Massive, matrix-clast supported, polymictic conglomerate, pebbly sandstone and cherty siltstone; well rounded-angular clasts include crystal rich-fine grained andesite, feldspathic sandstone, quartzose sandstone and minor chert and cherty siltstone.|
23600|Fosters Creek Conglomerate|70297|5|Briefly described|map legend|Silurian|Silurian|Presented as Fosters Creek Cgl.||||||
23600|Fosters Creek Conglomerate|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Campbells Group|||Massive, matrix- to clast-supported, polymictic conglomerate, pebbly sandstone and cherty siltstone; well rounded-angular clasts; beds up to 2m thick.|15-NOV-16
26560|Fountain Dale Tuff Member|9548|5|Briefly described|Map Legend|Pragian|Lochkovian|Of the Majuba Volcanics (Kopyje Group).||||||
26560|Fountain Dale Tuff Member|22857|4|Described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Majuba Volcanics (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin). ||||||
26560|Fountain Dale Tuff Member|42566|3|Fully described|p80|||Reserved as Fountain Dale.||||||
26560|Fountain Dale Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|Reserved as Fountain Dale.||||||
79848|Fountaindale Granodiorite|67416|5|Briefly described|p84-85, p87, p91|Wenlock|Wenlock|[New name]. Hosts gold mineralisation. Found 12km west of Mineral Hill. Re-Os date of 424.7 +/- 1.5 Ma for Mo in veins in altered wallrock. Located 12 km west of Mineral Hill.Trace element patterns typical of LFB Siluro-Devonian I-types.|424 Ma (lumped zircon age).||||Medium to fine grained biotite- and hornblende-bearing granodiorite.  Moderately oxidised calc-alkaline I-type of medium-K calc-alkaline character.  Ie Compositionally similar to other "intrusion related gold deposits".|21-JUN-17
79848|Fountaindale Granodiorite|70751|6|Mentioned|p8, p27-p28|Silurian|Silurian||420 +/- 2 Ma (LAICPMS, Norman, 2004)|||||
79848|Fountaindale Granodiorite|71039|6|Mentioned|p26|Early Devonian|Early Devonian|Interpreted from gravity and aeromagnetic data, this unit is entirely subsurface. Associated with potassic to calc-potassic alteration grading out to chlorite-magnetite rich propylitic alteration.|420 +/- 2 Ma|||||
79848|Fountaindale Granodiorite|73578|4|Described|p1, p3, p46-53|Ludfordian|Homerian|Lachlan Orogen. Of Blevin (2003). New U-Pb SHRIMP magmatic crystallisation age from zircon of 426.7 +/- 2.3 Ma reported, alongside a U-Pb titanite SHRIMP hydrothermal crystallisation age of 421.6 +/- 2.7 Ma which is inferred to record timing of alteration and mineralisation. Doesn't outcrop at the surface. Previous dating included ages of 420 +/- 2 Ma (U-Pb zircon LA-ICP-MS; Norman, 2004) and 424.7 +/- 1.5 Ma (Re-Os model age; Blevin, 2003).|426.7 +/- 2.3 Ma zircon SHRIMP||||Includes equigranular biotite-hornblende granodiorite; oxidised calc-alkaline I-type granite of intermediate character.|
77435|Four Bull Granodiorite|69639|4|Described|p1-p2, p5, p8, p26, p74-p78|Lopingian|Lopingian|New England Orogen. Sandy Flat-Bolivia region. Sample locality, petrography, and geochronology is described. See also p217, p220, p240.|258.4 +/- 1.3 Ma (SHRIMP U-Pb)|Herries Supersuite|||Medium- to fine-grained, mildly porphyritic pink/white granite.|
77435|Four Bull Granodiorite|70876|5|Briefly described|p81|||Provided age is a SHRIMP U-Pb zircon date.|258.4 +/- 1.3 Ma (Chisholm et al, 2014b)|Herries Supersuite||||
77435|Four Bull Granodiorite|71628|4|Described|p19: 37-39|||Chisholm et al. (2014) after unpublished work by Chappell and Bryant (1994) who named it Four Bull Monzogranite. Named after a local creek. Forms an irregular intrusion ~3 x 1 km, c.15 km E of Bolivia. Three geochemical analyses are described; discrepancies are discussed.|258.4 +/- 1.3 Ma (SHRIMP: Chisholm et al., 2014).|Four Bull Suite.||Intrudes Sandon Association.|White to pink, medium- to fine-grained, equigranular to mildly porphyritic, leucosyenogranite to leucomonzogranite, and possibly granodiorite.|
28559|Four Mile Creek Subgroup|22578|6|Mentioned|p398|||||||||
28559|Four Mile Creek Subgroup|22601|6|Mentioned|417|Permian|Permian|||||||
28559|Four Mile Creek Subgroup|24471|4|Described|p32 Fig.4|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to Tongarra Coal, Wilton Formation and Woonona Coal Member. Geological Province: Sydney Basin.||||||07-FEB-11
28559|Four Mile Creek Subgroup|42214|6|Mentioned|p460|||||||||
28559|Four Mile Creek Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
28559|Four Mile Creek Subgroup|73304|6|Mentioned|p62|||Includes Thornton Claystone.||||||
69885|Four Winds Ignimbrite Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Quialigo Volcanics (Bindook Group). Green-grey, lithic-crystal-rich dacitic welded ignimbrite and dacitic volcanic breccia.||||||18-JUN-08
69885|Four Winds Ignimbrite Member|68592|2|Defined|p1061, p1065, p1162-4, p1182-5|Pragian|Pragian|New name, after Four Winds property. These rocks were previously included in Gundary Beds or Towrang Beds. Poor outcrop. Type locality described. Thickness estimated to c.200m. Geochemistry unknown; geophysical properties briefly described. Mid Pragian age inferred from surrounding units. Is mineralogically and texturally distinct from Barrallier Ignimbrite.||Unit in Quialigo Volcanics.||Overlies Newacres Ignimbrite Member. Is overlain by Saltpetre Andesite Member. Correlated with Kerillon Tuff Member.|Greenish grey dacitic ignimbrite with up to 40% angular to sub-rounded clasts to 10cm; has characteristically lumpy weathering surfaces.|
69885|Four Winds Ignimbrite Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dkqf. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Quialigo Volcanics||Is overlain by, and also lenses out at base of, Saltpere Andesite Member. Overlies Newacres Ignimbrite Member.|Greenish grey, lithic-crystal rich, welded, dacitic ignimbrite and dacitic volcanic breccia.|
69885|Four Winds Ignimbrite Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Quialigo Volcanics|||Greenish grey, lithic-crystal rich, welded, dacitic ignimbrite and dacitic volcanic breccia.|
69885|Four Winds Ignimbrite Member|71700|5|Briefly described|p24, p26|||||Quialigo Volcanics||||
27409|Fowlers Gap Formation|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (East).  Parent - Farnell Group .  Age - Ediacarian in text.||||||
27409|Fowlers Gap Formation|22730|5|Briefly described|p559|Emsian||||||||
27409|Fowlers Gap Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
27409|Fowlers Gap Formation|22857|4|Described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Farnell Group. Purple, yellow shales bleached white in outcrop, interbedded with massive quartzite. Age: ~580Ma. Max. thickness: 1500m. Geological Province: Adelaide Fold Belt. See also p400 App.1 Tb.A1.3.||||||21-MAR-06
27409|Fowlers Gap Formation|23336|6|Mentioned|p16 Fig. 10|Precambrian|Precambrian|||||||
27409|Fowlers Gap Formation|30261|4|Described|Table 1|||Marinoan||||||
27409|Fowlers Gap Formation|33734|6|Mentioned|p495|||Correlation & trace fossils.||||||
27409|Fowlers Gap Formation|34812|3|Fully described|p104|||||||||
27409|Fowlers Gap Formation|34814|6|Mentioned|Table 1|||||||||
27409|Fowlers Gap Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27409|Fowlers Gap Formation|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
27409|Fowlers Gap Formation|36960|6|Mentioned|Fig.2|||||||||
27409|Fowlers Gap Formation|39214|6|Mentioned|Table 1|||||||||
27409|Fowlers Gap Formation|39885|6|Mentioned|p427|||||||||
27409|Fowlers Gap Formation|41301|5|Briefly described|p92|||||||||
27409|Fowlers Gap Formation|41429|5|Briefly described|p246|||||||||
27409|Fowlers Gap Formation|41801|6|Mentioned|p216|||See also Fig.4||||||
27409|Fowlers Gap Formation|46889|6|Mentioned|p272|||||||||
27409|Fowlers Gap Formation|60648|5|Briefly described|p42 Fig. 2|Precambrian|Precambrian|See also p53 Fig. 13.||||||
27409|Fowlers Gap Formation|66623|5|Briefly described|p13, p18. |||||||Overlies Faraway Hills Quartzite. Is overlain by Camels Hump Quartzite.|Purple and yellow shale (bleached white in outcrop) interbedded with dark-grey sandy siltstone; sporadic fine-grained quartzite beds with minimal clay material.|
27409|Fowlers Gap Formation|67562|6|Mentioned|p103 Fig.9|Precambrian|Precambrian|||||||
27409|Fowlers Gap Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Farnell Group.||||
27409|Fowlers Gap Formation|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Farnell Group.||Overlies Faraway Hills Quartzite. Is overlain by Camels Hump Quartzite.|Purple to yellow shale interbedded with dark grey sandy siltstone, sporadic fine-grained discontinuous quartzite beds with minor clay. A separately-mapped un-named subunit contains fine-grained, thinly-bedded quartzite horizons.|
82448|Fox Tor Quartz Diorite|71628|4|Described|p4: 8-9, 15, 47, 49; p19: 39-42, 136,171|||New name (this study); originally informal 'Fox Tor diorite' of Brown (2003); formalised by Stonestreet et al. (2006). Named after a local homestead; composition is almost exclusively quartz diorite. Is located 34 km WSW of Uralla and 20 km N of Bendemeer. Crops out as six irregular masses over 84 ha; forms tors and blocks. Geochemistry detailed.|239.7 +/- 6.7 Ma (K-Ar ?biotite).|Fox Tor Suite.||Intrudes Flaggy Range Monzogranite Phase (Banalasta Monzogranite) and Pringles Monzogranite.|Grey, medium- to coarse-grained, equigranular to slightly porphyritic, two-pyroxene-hornblende-biotite quartz diorite; locally flow-aligned and hybridised variants. I-type.|
26561|Foybrook Formation|22969|4|Described|Fig 4.1a||Late Permian|||||||
26561|Foybrook Formation|23060|6|Mentioned|5|||Geol province Sydney Basin||||||
26561|Foybrook Formation|29942|3|Fully described|p11|||||||||
26561|Foybrook Formation|29943|6|Mentioned|p39|||||||||
26561|Foybrook Formation|35767|6|Mentioned|p9|||||||||
26561|Foybrook Formation|35823|5|Briefly described|p29|||||||||
26561|Foybrook Formation|37087|6|Mentioned|p197|||||||||
26561|Foybrook Formation|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26561|Foybrook Formation|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26561|Foybrook Formation|40166|6|Mentioned|p366|||||||||
26561|Foybrook Formation|40256|6|Mentioned|Fig.3|||||||||
26561|Foybrook Formation|40330|6|Mentioned|Fig.4|||||||||
26561|Foybrook Formation|41054|6|Mentioned|Fig.3|||||||||
26561|Foybrook Formation|41604|4|Described|p5|||||||||
26561|Foybrook Formation|42648|6|Mentioned|p36|||||||||
26561|Foybrook Formation|42916|5|Briefly described|Table 1||Late Permian|||||||
26561|Foybrook Formation|42922|6|Mentioned|p38|||||||||
26561|Foybrook Formation|42946|6|Mentioned|p32|||||||||
26561|Foybrook Formation|43017|5|Briefly described|Fig.1,p372|||||||||
26561|Foybrook Formation|44093|6|Mentioned|p64 Photo 3|||In Sydney Basin.||||||
26561|Foybrook Formation|44244|4|Described|p236|Late Permian|Late Permian|Of the Vane Subgroup (Wittingham Coal Measures).  Includes Hebden, Barrett, Liddell, Arties, Pikes Gully and Lemington seams.  Underlies the Bulga Formation.  Max. thickness: >300m.||||||
26561|Foybrook Formation|45090|6|Mentioned|p219|||L. Tatarian||||||
26561|Foybrook Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Vane Subgroup (Wittingham Coal measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
26561|Foybrook Formation|61529|5|Briefly described|p857 Fig. 3a|||Of the Vane Subgroup (Wittingham Coal Measures). Overlain by Bulga Formation. See also p868.||||||17-FEB-06
26561|Foybrook Formation|61770|6|Mentioned|p111|||Of the Vane Supergroup. Unconformably overlian by Archerfield Sandstone.||||||25-SEP-08
26561|Foybrook Formation|68004|5|Briefly described|p51 Table 5, p155.|Late Permian|Late Permian|Upper Hunter Coalfield. Type section is 240 m thick.||Lower unit in Vane Subgroup.|Includes Edinglassie, Bengalla, Clanricard, Edderton and Wynn, Coal Members.|Overlies Saltwater Creek Formation. Is overlain by Bulga Formation.|Lithic sandstone, siltstone, shale, conglomerate and coal seams.|
26561|Foybrook Formation|69683|6|Mentioned|p411 Fig.2, p414-419 Figs.3-4|Late Permian|Late Permian|Appears to be mature for oil and gas generation.||Unit in Vane Subgroup.||||
26561|Foybrook Formation|73625|6|Mentioned|p2|Permian|Permian|Hunter coalfield, Sydney Basin.||Wittingham Coal Measures.||Overlies Mulbring Siltstone. Is overlain by Bulga Sandstone.||
80988|Frazer Beach Member|73625|6|Mentioned|p25|Permian|Permian|Sydney Basin. Records a widespread flooding or ponding event in southern temperate latitudes.||||"Equivalent to ""Marker Mudstone""."|A thin mudrock unit.|
31577|Free Damper Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31577|Free Damper Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||08-MAR-05
23602|Freyers Metasediments|6823|6|Mentioned|p205|||||Broeken Hill Group.||||
23602|Freyers Metasediments|22553|5|Briefly described|fig2p77,p78|Proterozoic|Proterozoic|||||||
23602|Freyers Metasediments|22575|6|Mentioned|p179 Fig.2|||Of the Pumamoota Subgroup, Broken Hill Group.||||||30-APR-13
23602|Freyers Metasediments|22771|6|Mentioned|Table12.2p45,47|||||||||
23602|Freyers Metasediments|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Purnamoota Subgroup (Broken Hill Group). Max. thickness: 500m. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
23602|Freyers Metasediments|22884|5|Briefly described|p45|||Of the Broken Hill Group. Geological province: Broken Hill Domain.||||||26-MAR-09
23602|Freyers Metasediments|22964|6|Mentioned|p56||Proterozoic|||||||
23602|Freyers Metasediments|22965|6|Mentioned|Fig 1||Statherian|Part of the Purnamoota Subgroup.||||||11-JUN-08
23602|Freyers Metasediments|22966|6|Mentioned|Fig1||Proterozoic|Rift stage of development.||||||
23602|Freyers Metasediments|22967|6|Mentioned|p39||Statherian|||||||
23602|Freyers Metasediments|23025|6|Mentioned|Fig1p75|||||||||
23602|Freyers Metasediments|23160|6|Mentioned|fig1|||||||||
23602|Freyers Metasediments|23248|5|Briefly described|Fig2p169|||||||||
23602|Freyers Metasediments|23461|5|Briefly described|p204 Fig.3|||||||||
23602|Freyers Metasediments|24307|5|Briefly described|p975|Proterozoic|Proterozoic|Parent: Broken Hill Group.   Previously included in the Purnamoota Subgroup, which has been abandoned by this study.||||||
23602|Freyers Metasediments|38969|4|Described|p209|||||||||
23602|Freyers Metasediments|39662|2|Defined|p428|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23602|Freyers Metasediments|39849|6|Mentioned|Table 2|||||||||
23602|Freyers Metasediments|40822|6|Mentioned|Fig.2|||||||||
23602|Freyers Metasediments|41093|6|Mentioned|p252|||||||||
23602|Freyers Metasediments|41145|6|Mentioned|Fig.4|||||||||
23602|Freyers Metasediments|41630|6|Mentioned|p53|||||||||
23602|Freyers Metasediments|41633|6|Mentioned|p139|||||||||
23602|Freyers Metasediments|42181|6|Mentioned|Fig,1 P252|||||||||
23602|Freyers Metasediments|42261|6|Mentioned|Fig 1 P530|||||||||
23602|Freyers Metasediments|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23602|Freyers Metasediments|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23602|Freyers Metasediments|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23602|Freyers Metasediments|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23602|Freyers Metasediments|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23602|Freyers Metasediments|42537|6|Mentioned|Fig.2 P5|||||||||
23602|Freyers Metasediments|42595|6|Mentioned|Fig. 2 P5|||||||||
23602|Freyers Metasediments|42897|5|Briefly described|Fig.3, P321|||||||||
23602|Freyers Metasediments|43052|6|Mentioned|Fig.4.22|||||||||
23602|Freyers Metasediments|43086|6|Mentioned|Fig.3|||||||||
23602|Freyers Metasediments|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23602|Freyers Metasediments|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23602|Freyers Metasediments|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23602|Freyers Metasediments|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23602|Freyers Metasediments|43271|5|Briefly described|Map Legend||Paleoproterozoic|of Purnamoota Sub-Group.||||||07-NOV-08
23602|Freyers Metasediments|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
23602|Freyers Metasediments|43572|6|Mentioned|Fig.3.2 p6|||||||||
23602|Freyers Metasediments|43583|5|Briefly described|Table 1,p2139|||||||||
23602|Freyers Metasediments|46598|5|Briefly described|p304|||||||||
23602|Freyers Metasediments|50045|5|Briefly described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Purnamoota Subgroup (Broken Hill Group). Overlain by Hores Gneiss and Silver King Formation. Underlain by Parnell Formation.||||||31-MAY-07
23602|Freyers Metasediments|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Purnamoota Subgroup (Broken Hill Group).  Geological Province: Broken Hill Block.||||||07-NOV-08
23602|Freyers Metasediments|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic||Of the Broken Hill Group.||||||07-NOV-08
23602|Freyers Metasediments|61735|5|Briefly described|p636 Fig. 2, p639 Tb.1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Max depositional age: ~1750Ma. Presented as Freyers only in Fig. 2||||||04-JUN-15
23602|Freyers Metasediments|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Geological province: Olary Domain.||||||
23602|Freyers Metasediments|62535|5|Briefly described|p666 Fig.3, p671-673|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Broken Hill Group.||Is overlain by Hores Gneiss.|Basal psammite unit, then fining upwards into the predominant pelitic rocks.|
23602|Freyers Metasediments|62536|5|Briefly described|p636, 639, 641, 646|||Broken Hill area. Appears only as Freyers on p636.|c.1690 Ma. MDA of ~1750 Ma.|Broken Hill Group.||||
23602|Freyers Metasediments|62993|6|Mentioned|p6, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Purnamoota Subgroup||||16-DEC-21
23602|Freyers Metasediments|63519|5|Briefly described|p6 Fig. 2, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Age: <1780Ma. Geological Province: Broken Hill Block-Euriowie Block. See also p22,  p29 Fig. 11..||||||07-NOV-08
23602|Freyers Metasediments|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province. ||Purnamoota Subgroup||Overlies the Parnell Formation.|Well-bedded pelite to psammopelite/psammite with rare mafic gneisses.|
23602|Freyers Metasediments|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Purnamoota Subgroup (Broken Hill Group, Willyama Supergroup). Geological Province: Broken Hill Block.||||||07-FEB-11
23602|Freyers Metasediments|64741|5|Briefly described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Purnamoota Subgroup (Broken Hill Group). Geological province: Broken Hill Domain.||||||07-FEB-11
23602|Freyers Metasediments|64742|6|Mentioned|p321 Fig.3, p323. |||||Unit in Broken Hill Group.|||Psammite.|
23602|Freyers Metasediments|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Purnamoota Subgroup (Broken Hill Group). Geological province: Broken Hill Domain.||||||07-FEB-11
23602|Freyers Metasediments|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Purnamoota Subgroup||Overlies the Parnell Gneiss. Overlain by the Hores Gneiss.||
23602|Freyers Metasediments|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.||Broken Hill Group.||||
23602|Freyers Metasediments|69999|6|Mentioned|p7 Photo 3|||||||||
23602|Freyers Metasediments|70014|5|Briefly described|Map legend|||Beds thin and planar; sporadic graded bedding. Sporadic zoned calc-silicate nodules.||Unit in Purnamoota Subgroup.||Overlies Parnell Formation. Is overlain by Hores Gneiss and Silver King Formation.|Mainly metasediments, ranging from well-bedded pelitic/psammopelitic schists with some psammitic intervals, to psammitic/psammopelitic or psammitic/pelitic metasediments. Minor tourmaline-quartz rocks. Rare basic gneiss and quartz-gahnite rock.|
23602|Freyers Metasediments|70405|6|Mentioned|p9 Table 1|Paleoproterozoic|Paleoproterozoic||1685 Ma|Purnamoota Subgroup||||
23602|Freyers Metasediments|70657|5|Briefly described|p15|Statherian|Statherian|Broken Hill Domain, Curnamona Province. See also mis-spelt Fryers Metasediments (p13 Fig.6).||Purnamoota Subgroup.||Overlies and is intruded by Parnell Gneiss. Is overlain by Hores Gneiss and Sundown Group.||
23602|Freyers Metasediments|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Purnamoota Subgroup.||||
23602|Freyers Metasediments|72461|5|Briefly described|p13, p16, p18|||Hosts three different types of mineralisation including: Tin hosted in feldspar pegmatite, Great Eastern Type copper-cobalt and Hores-type tungsten.||Broken Hill Group||Overlies the Parnell Gneiss. Overlain by the Hores Gneiss.|Metasediments with moderately graded bedding, ellipsoidal to lenticular metamorphosed concretions.|
23602|Freyers Metasediments|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian|Broken Hill block-Euriowie block.||Broken Hill Group||||
23602|Freyers Metasediments|73308|6|Mentioned|p607 Fig.1, 611, 618|||||Broken Hill Group.|||Includes BIFs and pelitic metasediments.|
23602|Freyers Metasediments|73482|6|Mentioned|p422 Fig.3|||||Broken Hill Group||||
23602|Freyers Metasediments|73512|6|Mentioned|p2|||||||||
23602|Freyers Metasediments|73524|5|Briefly described|p4, p18|Statherian|Statherian||c. 1750 Ma|Broken Hill Group|||Includes migmatitic paragneisses with metapelitic and subordinate psammo-pelitic units.|
23602|Freyers Metasediments|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p830, p831 Fig.5|Statherian|Statherian|Hosts intermittent quartz-gahnite and banded iron formation outcrops.|<1780 Ma|Purnamoota Subgroup||Overlies Parnell Formation, underlies Hores Gneiss||
80151|Friendly Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Werrie Basin. Shown only as Friendly. Ending assumed from references to other Coal Members in text.||Rowan Formation.||||28-SEP-17
35359|Frog Hollow Formation|23185|6|Mentioned|p159,Fig5p161|Eifelian|Emsian|||||||
35359|Frog Hollow Formation|24008|5|Briefly described|p355|Middle Devonian|Early Devonian|||||||
35359|Frog Hollow Formation|61766|5|Briefly described|p68|Early Devonian|Early Devonian|Coarse-grained mafic volcaniclastics.||||||
35359|Frog Hollow Formation|73440|6|Mentioned|p129-130, p132|Early Devonian|Early Devonian|Gamilaroi terrain.||||Underlain by Pitch Creek Volcanics.|Interbedded tuff, sandstone, mudstone and rare limestone.|
42437|Fullerton Gneiss|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tumboramboro Suite. Grey-brown metasedimentary composite gneiss with minor migmatite, quartzo-feldspathic segregation veins and pods of equigranular biotite-quartz-feldspar xenolithic granodiorite.||||||24-JUN-08
42437|Fullerton Gneiss|68592|2|Defined|p279, p1543, p1545-6, p1577-80, p1585-8|Early Devonian|Early Devonian|See also p105. New name, after Fullerton locality and property. Included in Wologorong-Tumboramboro Granite by Scheibner (1973). Occurs as an ovoid pod c.2km long by 600m wide. Type area described. Enclosed by, and partly assimilated into, Balmeringa Granite. This unit's protolith was probably the Abercrombie Formation which underwent very high-grade regional metamorphism and was partly assimilated by an unrelated granitic melt to form the Balmeringa Granite. Generally poorly exposed. Geochemistry and geophysical properties briefly described. No direct age; could be significantly older than the tentative age allocated.||Unit in Tumboramboro Suite.||Is overlain by Crookwell Basalt. Grades into the surrounding Balmeringa Granite.|Hard, grey-brown gneiss and gneissic granite to granodiorite; thick, pale, locally boudinaged pegmatite veins; fine-grained domains without gneissic banding but heavily recrystallised; pods of migmatite.|
42437|Fullerton Gneiss|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dtf. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Tumboramboro Suite|||Metasedimentary composite gneiss with minor migmatite, quartzo-feldspathic segregation veins and pods of equigranular, xenolithic, biotite granite to granodiorite; high K and Th, low-high U response; low magnetic susceptibility.|
42437|Fullerton Gneiss|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Tumboramboro Suite|||Metasedimentary composite gneiss with minor migmatite, quartzo-feldspathic segregation veins and pods of equigranular, xenolithic, biotite granite to granodiorite; high K and Th, low-high U response; low magnetic susceptibility.|
39276|Funeral Creek Limestone|24241|5|Briefly described|p15 Fig.2|Cambrian|Cambrian|Geological Province: Darling Basin.||||||
39276|Funeral Creek Limestone|66623|2|Defined|p110, pp128-129. |Late Cambrian|Late Cambrian|Defined in this study. Correlated with Nootumbulla Sandstone. A single resistant 20-30 m thick outcrop, demonstrably allochthonous and overturned, representing a shallow marine shelf-shoreline environment.||Unit in Kayrunnera Group.||Discordant relationships with surrounding Wheeney Creek Formation.|Single allochthonous block of bedded, brecciated intraclast bearing-limestone with brecciated tectonic contacts against conglomerate, metasandstone and slate units. Carbonate clasts are tabular and cm-scale; minor intercalated lenses of siltstone.|
39276|Funeral Creek Limestone|67322|5|Briefly described|p11-12; Fig.5|Stage 10|Stage 10|Defined by Greenfield and Percival, in Greenfield et al.(2010). The unit is approximately 20-30m thick. Age from conodonts. Occurs on Morden Station, in the Kayrunnera-Koonenberry region.||Of the Kayrunnera Group.|||An isolated overturned allochthonous pod of fossiliferous limestone with a distinctive brecciated appearance, composed of subrounded to tabular clasts of carbonate up to 20cm long.|21-FEB-18
39276|Funeral Creek Limestone|71284|5|Briefly described|p488|Stage 10|Stage 10|Central Koonenberry Belt.||Kayrunnera Group.||||
28226|Gaden Tonalite|22815|4|Described|p51|Early Devonian|Late Silurian|||||||
28226|Gaden Tonalite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
28226|Gaden Tonalite|35109|2|Defined|p74|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
28226|Gaden Tonalite|35263|6|Mentioned|Table 3|||||||||
28226|Gaden Tonalite|36411|6|Mentioned|p268|||Refers White et al 1977 for definition.||||||
28226|Gaden Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
28226|Gaden Tonalite|40328|4|Described|p206|||||||||
28226|Gaden Tonalite|41563|6|Mentioned|p506|||||||||
28226|Gaden Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Jindabyne Suite.||||||
28226|Gaden Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh13||||||
26565|Gairdners Creek Quartzite|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
26565|Gairdners Creek Quartzite|22857|5|Briefly described|Tb 13.1 (insert p70), p400 App.1 Tb A1.3|Marinoan|Marinoan|Of the Teamsters Creek Subgroup (Torrowangee Group). Age ~593+/-32Ma. Max. thickness: 4m. Geological Province: Adelaide Fold Belt.||||||15-JAN-15
26565|Gairdners Creek Quartzite|30261|4|Described|Table 1|||Marinoan age||||||15-JAN-15
26565|Gairdners Creek Quartzite|34812|3|Fully described|p90|||||||||
26565|Gairdners Creek Quartzite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26565|Gairdners Creek Quartzite|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
26565|Gairdners Creek Quartzite|36733|6|Mentioned|Table 5|||||||||
26565|Gairdners Creek Quartzite|37931|4|Described|p532|||See also P533.||||||
26565|Gairdners Creek Quartzite|38157|6|Mentioned|p265|||||||||
26565|Gairdners Creek Quartzite|39214|5|Briefly described|p9|||Blanket sand||||||
26565|Gairdners Creek Quartzite|41405|5|Briefly described|p204|||||||||
26565|Gairdners Creek Quartzite|68241|6|Mentioned|p24 Fig.3, p32, p33 Fig.3||||||||Diamictite.|
26565|Gairdners Creek Quartzite|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Teamsters Creek Subgroup.||||
26565|Gairdners Creek Quartzite|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Teamsters Creek Subgroup.||Overlies Alberta Conglomerate.|Massive to weakly bedded, well-sorted quartzite with local, well-rounded quartz cobbles.|
73371|Galambo Granite|69094|5|Briefly described|Map legend|Early Silurian|Early Silurian|Subsurface; shown on time-space plot, cross-sections and pre-Mesozoic geology diagram.|||||Hornblende granodiorite (dominant), adamellite, syenite, granite; strongly magnetic.|
73371|Galambo Granite|70602|6|Mentioned|p67 Fig 3,72|Silurian|Silurian|Age inferred from map symbol. Aeromagnetic map data given. Grouped with Mount Oxley Granite, Glenariff Granite, Knightvale Granite and 3 informal units: Rosses Tank Unit, Brevelon Unit, Mulgawarrina Unit.||||||
73371|Galambo Granite|70941|4|Described|pviii, p8 fig 4, p9, p11 fig 6|Early Silurian|Early Silurian|Named for Galambo property. Not subdivided due to a paucity of outcrop and drill data. Distribution, distinguishing characteristics, geomorphology, metamorphism, structure, geochemistry and geophysical characteristics discussed. Lithology discussed in further detail. Type hole proposed but may not be representative. Thickness is unknown. I type granite containing mafic enclaves. See also p58 fig 23p, p60-63, p70 fig 30, p113, p140 fig 58, p145.||||May intrude Girilambone Group.|Hornblende bearing granodiorite, leucoadamellite, biotite adamellite and syenite.|
73371|Galambo Granite|71345|2|Defined|p4,30-35|Early Devonian|Early Devonian|Type location/section: RAB hole CAC 5.5, 50-66 m (EOH) as proposed by Trigg (in Burton et al., 2012); collared at Lat -30.4719° Long 145.9353° GR 397800 6628430.  Named after the Galambo property, whose homestead is situated over the granite. This drillhole interval was proposed by Trigg (in Burton et al., 2012) as a type section due to the lack of outcrop and paucity of drill hole intercepts, however Berven (1997) described these rock chips samples as altered felsic volcanics. Distribution is based on results of a number of exploration drilling campaigns (Gould 1975; Rabone 1979; Lea 1991; Hoatson 1981; Berven 1997) and on aeromagnetic imagery (as a distinctive relative magnetic high). Roughly triangular in shape; located across parts of the Mount Oxley, Byrock, Gunderbooka and Bourke 1:100 000 map sheet areas (Hegarty 2011). Maximum interpreted extension is 32 km in an E-W direction (Trigg in Burton et al. 2012, pp. 60-63). The faulting along and near the northern boundary of the granite is part of the Louth-Eumarra Shear Zone (Glen et al. 1996, p. 49); field relationships may indicate granite emplacement occurring before faulting. See p31-32 for detailed lithological and petrographical descriptions. Hoastson (1981) described the Galambo Granite as I-type, while drillhole J14 encountered red-brown biotite adamellite that may of S-type affinities; if correct, this would be evidence that the Galambo Granite comprises at least two, unrelated igneous bodies. Preliminary age of 418 Ma reported from aircore chips in RAB drill hole CAC 5.5, 50¿66 m (EOH) (Fraser and Thorne, in prep.), which is similar in age to Early Devonian Tarcoon Suite, and within error of Mullagalah Quartz Diorite.|c. 418 Ma|||In fault contact, and intrudes into Girilambone Group.|Hornblende-bearing granodiorite. Leucoadamellite, biotite adamellite (Hoatson 1981) and syenite (Rabone 1979).|02-DEC-19
73371|Galambo Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: zone of moderate magnetic intensity features showing irregular texture with magnetite-depleted fractures patterns. Unit also includes smaller features which have similar characteristics in adjacent areas. Intrusive contacts vary from sharp contrast and structure-bounded margins to complex patterns suggesting partial unroofing.|||||Hornblende-biotite granodiorite, with less-magnetic zones of monzogranite and alteration.|
73371|Galambo Granite|71965|6|Mentioned|p910|||Geological province: Lachlan Orogen. I-type granite.||||||
73371|Galambo Granite|72522|4|Described|p1, p3, p5, p10, p13-17, p29, p133.|Lochkovian|Pridoli|Situated along the southern margin of the Louth-Eumarra Shear Zone, interpreted to represent the boundary between the Lachlan and Thomson orogens.Not known to crop out.  Date is a magmatic crystallisation age which is indistinguishable from previously reported ages of granites of the Tarcoon Suite along strike to the east.|417.8 +/- 3.2 Ma 206Pb/238U (204Pb-corrected)|Tarcoon Suite|||Typically a hornblende-bearing granodiorite. Dated sample highly weathered kaolinitic granite.|
73371|Galambo Granite|72951|5|Briefly described|p1013, 1017, 1022-1023|Lochkovian|Pridoli|Lachlan Orogen. Hermidale Terrane. I-type. SHRIMP U-Pb zircon isotope analyses from Fraser et al. (in prep). eHf = 1.9 +/- 0.5, and d18O = 6.39 +/- 0.17.|417.8 +/- 3.2 Ma||||Granite.|
37403|Gamboola Shale|23214|6|Mentioned|P127|||||||||
23607|Ganmain Granite|22508|5|Briefly described|p2||Silurian|Koetong Supersuite, Lachlan Fold Belt||||||
23607|Ganmain Granite|22638|4|Described|p52|||Probably Late Silurian.||||||
23607|Ganmain Granite|42726|5|Briefly described|map legend|Silurian||||||||
23607|Ganmain Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
23607|Ganmain Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
23607|Ganmain Granite|69801|5|Briefly described|p1, p4-p5, p39-43, p135-137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs between Junee and Narrandera. Sample locality, petrography, SHRIMP analyses and interpretation are detailed. Together with the Grong Grong Granite confirms the presence of Koetong Supersuite granites between Junee and Narrandera. Ganmain Granodiorite also used p148.|428.7 +/- 1.8 Ma|Tom Groggin Suite||Intrudes the Wagga Group.|Medium to coarse-grained, porphyritic, biotite s-type granite. Hosts abundant biotite rich enclaves and rare blocks of foliated metasandstone.|
23607|Ganmain Granite|70777|5|Briefly described|p1-p2, p9, p14, p80|Wenlock|Wenlock|Lachlan Orogen.|(428.7 +/- 1.8 Ma (Bodorkos et al., 2015)|||||
23607|Ganmain Granite|71889|4|Described|p7-p8, p24-p34, p67|Ludlow|Wenlock|Defined by Warren et al., 1995 and description updated by Eastlake (2016, 2017). Isolated exposures occur in the far eastern part of NARRANDERA, c. 5km east of Matong and west of the exposures mapped by Eastlake (2016, 2017) in COOLAMON. Includes rocks formerly assigned as Rosemorder Granite. The most extensive outcrops of this granite occurs around the Cobb Trigonometrical Station (GR 497052 6151831) across an area extending 600m to the northwest. Outcrops are mainly tors and large whale-backs. 1.5km south of the Cobb Trigonometrical Station there is extnesive exposure of granite that is more equigranular. Weathered granite outcropping north-northwest of the Ganmain granite may be a northerly extension. Geochemistry is briefly discussed. Trigg (2017) tentatively assigned cordierite poprhyitic granite outcropping on the Ranchero property to the Rosemorder Granite. This granite was previously included in the Ardlethan Granite (Pogson 1974; Chappell et al. 1991) geochemistry has since indicated that this is more likely to belong to the Ardlethan Granite than the Ganmain Granite; however, the author notes geochronology would be definitive in assigning the 'Ranchero" cordierite granite.|428.7 +/- 1.8 Ma (Bodorkos et al, 2015)||||Highly porphyritic medium- to coarse-grained biotite granite and medium-grained and locallly equigranular granite with small scattered phenocrysts.|
23607|Ganmain Granite|72084|4|Described|p2, p6 Fig.5a, p8, p28 Fig.30,p30-38,p46|Silurian|Silurian|Eastlake (2016). Forms rounded boulder outcrops and blocks. Petrography, geochemistry detailed. Geochemical plot. Has similarities with Wantabadgery Granite. Metamorphic effects detailed: photomicrographs.|428.7 +/- 1.8 Ma (Bodorkos et al., 2015).|||Intrudes Wagga Group.|Light grey, medium- to coarse-grained, inequigranular cordierite-biotite granite with biotite-rich schistose, and xenolithic quartz, enclaves; weakly K-feldspar-megacrystic felsic granite. Aplite dykes. S-type.|
41058|Gara Monzogranite|24366|5|Briefly described|p8 Fig. 6|Early Permian|Early Permian|Of the Hillgrove Plutonic Suite.||||||
41058|Gara Monzogranite|71628|4|Described|p3: 1, 4, 10, 24, 39-43|||Brown (2003). Previously Gara Adamellite (Binns et al., 1967). Named after a local homstead or the parish of Gara. A large (16 x 9 km) intrusion, cropping out ~20 km SE of Armidale. Exposed along the Gara River. Geochemistry described in some detail. Contains garnet in the more deformed rocks.|296.2 +/- 1.7 Ma (Landenberger et al., 1995).|Gara Suite.||Intrudes Girrakool beds.|Medium-grained biotite monzogranite-granodiorite; amphibole, orthopyroxene, and garnet bearing variants; massive to foliated. S-type.|
77016|Garibaldi Monzogranite|71628|5|Briefly described|p2: 5-6; p3: 1, 4, 43-45|||New unit, after Chappell and Bryant (1994 unpublished) and Landenberger et al. (2010). Previously a southern part of the Apsley River Diorite. Possibly named after the homestead 'Garrabaldi' or a local feature Garibaldi Rock, both to the SE. Crops out on the edge of Apsley River gorge, 23 km ESE of Walcha. Limited geochemistry described; has similarities with Murder Dog Monzogranite.||Garibaldi Suite.||Intrudes Agnes Greywacke.|Biotite monzogranite.|
27082|Garrawilla Volcanics|721|5|Briefly described|Map legend|Callovian|Rhaetian|Vesicular and non-vesicular, alkali olivine basalt, hawaiite, basanite, mugearite.  Geological Province: Surat Basin.||||||21-DEC-04
27082|Garrawilla Volcanics|12597|5|Briefly described|p492 Tb.1, p496|Early Jurassic|Early Jurassic|S Surat Basin. 180m thick.|201-171 Ma (K-Ar; Hawke and Bourke, 1984).||||Irregular sequence of basaltic flows and pyroclastic rocks with tuffaceous sandstone and claystone beds.|
27082|Garrawilla Volcanics|22857|4|Described|p295, p304, p546 App.1 Tb.A1.12|Early Jurassic|Early Jurassic|Flows of alkali-olivine basalt, alkali basalt, mugearite, hawaiite; pyroclastics of ash, lapilli tuff, volcanic agglomerate, conglomerate; small lava domes. Age: 208-175Ma (K/Ar). Max. thickness: 180m. Geol. Prov: Surat and Oxley Basins. See p309, 314-5||||||
27082|Garrawilla Volcanics|22861|6|Mentioned|Map26p282-3||Late Triassic|||||||
27082|Garrawilla Volcanics|22865|4|Described|p295,304,309,314|Middle Jurassic|Early Jurassic|Max Age: 201 Ma; Min Age: 171 Ma.||||||
27082|Garrawilla Volcanics|23053|5|Briefly described|p11,24,70|Late Jurassic|Early Jurassic|Max Age: 188.5 Ma.||||||
27082|Garrawilla Volcanics|23566|5|Briefly described|p116 Fig. 2|Jurassic|Jurassic|Geological Province: Gunnedah Basin.||||||17-SEP-08
27082|Garrawilla Volcanics|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
27082|Garrawilla Volcanics|24070|5|Briefly described|p303|Jurassic|Jurassic|Geological Province: Coonamble Embayment.||||||
27082|Garrawilla Volcanics|24092|5|Briefly described|p8 Fig.3|||||||||
27082|Garrawilla Volcanics|24237|5|Briefly described|p7|Jurassic|Jurassic|||||||
27082|Garrawilla Volcanics|24243|5|Briefly described|p3 Fig.2|Early Jurassic|Late Triassic|||||||
27082|Garrawilla Volcanics|29698|4|Described|p66|||||||||
27082|Garrawilla Volcanics|29699|4|Described|p131|||||||||
27082|Garrawilla Volcanics|29870|4|Described|p14|||||||||
27082|Garrawilla Volcanics|29909|6|Mentioned|Table 1|||||||||
27082|Garrawilla Volcanics|30135|6|Mentioned|Map legend|Jurassic|Triassic|Jurassic - Triassic||||||
27082|Garrawilla Volcanics|30610|1|Redefined|p323|Early Jurassic|Late Triassic|Upper Triassic - Lower Jurassic||||||
27082|Garrawilla Volcanics|30910|6|Mentioned|Map legend|Triassic|Triassic|||||||
27082|Garrawilla Volcanics|30911|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
27082|Garrawilla Volcanics|32482|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
27082|Garrawilla Volcanics|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
27082|Garrawilla Volcanics|33004|6|Mentioned|p123|||||||||
27082|Garrawilla Volcanics|33352|6|Mentioned|p176|||||||||
27082|Garrawilla Volcanics|33676|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
27082|Garrawilla Volcanics|33873|6|Mentioned|p5|||||||||
27082|Garrawilla Volcanics|35095|4|Described|p111|||||||||
27082|Garrawilla Volcanics|35416|6|Mentioned|p8|||Stratigraphy and palynological framework on Fig.2||||||
27082|Garrawilla Volcanics|36570|6|Mentioned|p38|||||||||
27082|Garrawilla Volcanics|36954|6|Mentioned|Fig.1|||||||||
27082|Garrawilla Volcanics|37818|6|Mentioned|Table 3|||||||||
27082|Garrawilla Volcanics|37856|6|Mentioned|Table I|||||||||
27082|Garrawilla Volcanics|38614|6|Mentioned|p12|||||||||
27082|Garrawilla Volcanics|38684|5|Briefly described|p18|Jurassic|Jurassic|Geological Province: New England Fold Belt||||||
27082|Garrawilla Volcanics|38784|6|Mentioned|p77|||||||||
27082|Garrawilla Volcanics|39063|6|Mentioned|Fig.6, p17|||||||||
27082|Garrawilla Volcanics|39666|6|Mentioned|p111|||||||||
27082|Garrawilla Volcanics|39913|6|Mentioned|Fig.1|||||||||
27082|Garrawilla Volcanics|40263|6|Mentioned|Table 2|||||||||
27082|Garrawilla Volcanics|40811|4|Described|p323|||||||||
27082|Garrawilla Volcanics|40869|6|Mentioned|Fig.2|||||||||
27082|Garrawilla Volcanics|40952|6|Mentioned|p8|||See also Fig.3||||||
27082|Garrawilla Volcanics|41264|6|Mentioned|p257|||||||||
27082|Garrawilla Volcanics|41266|6|Mentioned|Fig.3|||||||||
27082|Garrawilla Volcanics|41290|6|Mentioned|p226|||||||||
27082|Garrawilla Volcanics|41330|6|Mentioned|p21|||||||||
27082|Garrawilla Volcanics|41857|6|Mentioned|p394|||||||||
27082|Garrawilla Volcanics|42284|6|Mentioned|p111|||||||||
27082|Garrawilla Volcanics|42463|6|Mentioned|Fig.6 P173|||||||||
27082|Garrawilla Volcanics|42558|6|Mentioned|p6|||||||||
27082|Garrawilla Volcanics|42679|6|Mentioned|Fig.3 P3|||||||||
27082|Garrawilla Volcanics|42918|6|Mentioned|p45|||||||||
27082|Garrawilla Volcanics|42925|6|Mentioned|p86|||||||||
27082|Garrawilla Volcanics|42950|5|Briefly described|p41|||||||||
27082|Garrawilla Volcanics|43091|5|Briefly described|Map legend|||of Surat Basin||||||
27082|Garrawilla Volcanics|43194|5|Briefly described|p98 Tb 8.2, p122,p125 p127, p133 App. 1|Middle Triassic|Middle Triassic|Gunnedah Basin. Disconformably overlies Napperby and Deriah Formations.||||||
27082|Garrawilla Volcanics|43276|5|Briefly described|Map Legend||Early Jurassic|||||||
27082|Garrawilla Volcanics|43277|5|Briefly described|Map Legend||Early Jurassic|||||||
27082|Garrawilla Volcanics|43354|5|Briefly described|p105-108|Jurassic|Triassic|||||||
27082|Garrawilla Volcanics|43355|14|Not recorded|Map Legend||Jurassic|Provisional Edition||||||
27082|Garrawilla Volcanics|43356|14|Not recorded|Map Legend||Jurassic|Includes Comiala Shale||||||
27082|Garrawilla Volcanics|43357|14|Not recorded|155-161|Early Jurassic|Late Triassic|Potassium Argon Dating||||||
27082|Garrawilla Volcanics|43383|14|Not recorded|p25||Early Jurassic|||||||
27082|Garrawilla Volcanics|43393|14|Not recorded|p180|||Late Triassic or Early Jurassic||||||
27082|Garrawilla Volcanics|43405|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
27082|Garrawilla Volcanics|43407|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
27082|Garrawilla Volcanics|43410|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
27082|Garrawilla Volcanics|43479|14|Not recorded|p249,262|||Liass.||||||
27082|Garrawilla Volcanics|43494|5|Briefly described|p13|Early Jurassic|Late Triassic|Overlies Napperby Formation.||||||09-MAR-06
27082|Garrawilla Volcanics|43535|4|Described|p135,137-8|Early Jurassic|Late Triassic|Includes all intrusives and extrusive rocks including Garrawilla Lavas.||||||17-SEP-08
27082|Garrawilla Volcanics|43755|6|Mentioned|Fig.9,p556|||||||||
27082|Garrawilla Volcanics|44093|5|Briefly described|p192 App. 1|Mesozoic|Mesozoic|Geological Province: Lachlan Fold Belt.||||||
27082|Garrawilla Volcanics|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
27082|Garrawilla Volcanics|49010|6|Mentioned|Fig.4|||Coonamble Embayment||||||
27082|Garrawilla Volcanics|49011|6|Mentioned|Fig.3|||Coonamble Embayment||||||
27082|Garrawilla Volcanics|50616|6|Mentioned|p275|||||||||
27082|Garrawilla Volcanics|50629|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Surat Basin. Underlies: Purlawaugh Formation.  Overlies: Deriah Formation.||||||05-JUL-04
27082|Garrawilla Volcanics|60266|5|Briefly described|p2, p3 Tb. 1|Early Jurassic|Late Triassic|Basal unit of the Surat Basin. Unconformably overlies the Deriah Formation of the Gunnedah Basin.  Geological Province: Surat Basin.||||||08-DEC-04
27082|Garrawilla Volcanics|60267|4|Described|p15, p21, p26|Late Triassic|Late Triassic|Moderately porphyritic basalts with scattered olivine phenocrysts.  Overlain, mostly conformably, by the Pilliga Sandstone and, in places, the Purlawaugh Formation.  Intruded by the Glenrowan Intrusives. Geological Province: Surat Basin.||||||11-AUG-04
27082|Garrawilla Volcanics|61313|5|Briefly described|p88, p94 Fig. G7|Jurassic|Jurassic|Only locally present - as a 220m thick igneous intersection. Geological Province: Gunnedah Basin; locally forms basal unit of Surat Basin (39m thick). See also p95 Fig. G8, p98 Fig. G10.||||||
27082|Garrawilla Volcanics|61377|5|Briefly described|p142, p148 Tb. SU1|Early Jurassic|Early Jurassic|Labile sandstone, polymictic conglomerate, siltstone, mudstone. Geological Province: Surat Basin. See also p154 Fig. SU9.||||||07-FEB-11
27082|Garrawilla Volcanics|61776|5|Briefly described|p195, p199, p194 Fig. 3|Jurassic|Jurassic|Geological Province: Surat Basin. Alkali basalts.||||||17-SEP-08
27082|Garrawilla Volcanics|65112|6|Mentioned|Fig 11 p324|Late Triassic|Late Triassic|Underlies the Precipice Sandstone and Purlawaugh Formation (relationship to these units unknown).||||||14-SEP-09
27082|Garrawilla Volcanics|65113|5|Briefly described|Fig 4 p340|Late Triassic|Late Triassic|Shown as Garrawilla Volcanics and intrusions.||||||
27082|Garrawilla Volcanics|65114|5|Briefly described|p385 Fig.3|Late Triassic||and intrusives||||||
27082|Garrawilla Volcanics|65116|5|Briefly described|p451, 452, p442 Fig. 7|Early Jurassic|Late Triassic|Mafic tuffs and flows, Gunnedah Basin.. K-Ar ages: 203.2+/- 2.1 Ma and 177.9-/+1.9 Ma, pre-dated Surat Basin deposition.||||||
27082|Garrawilla Volcanics|65119|6|Mentioned|p516|Early Jurassic|Late Triassic|||||||
27082|Garrawilla Volcanics|66191|5|Briefly described|p484 Fig.1, p485 Fig.2|Early Jurassic|Late Triassic|Gunnedah Basin. Related to breakup of east Gondwana. Unconformably overlies the Deriah Formation.||||||
27082|Garrawilla Volcanics|66529|6|Mentioned|p12 Fig.5 |||Coonamble Embayment.||||Unconformably overlies Napperby Formation.||
27082|Garrawilla Volcanics|68003|4|Described|p14, pp48-50, p52, p54, pp56-59, p127.|Early Cretaceous|Middle Triassic|A lengthy period of intermittent volcanism. Outcrops mainly in the Coonabarabran-Mullaley-Gunnedah areas. Flows vary from one to eight metres thick; probably from several vents or fissures.|218-119 Ma.||Includes Glenrowan Intrusives, the Bulga Complex, Nombi Extrusives and Tambar Intrusives.|Unconformably overlies Napperby Formation. Is conformably overlain by Purlawaugh Formation.|Extrusives range from alkali basalt to soda trachyte; flows range from extremely vesicular to non-vesicular, fine-grained, with flow structure; ash cloud and debris flow deposits common, often interbedded with flows; some claystones.|
27082|Garrawilla Volcanics|68135|6|Mentioned|p52 fig 2b|Sinemurian|Hettangian|Surat Basin (NSW)||||||
27082|Garrawilla Volcanics|70036|5|Briefly described|Map legend|||Surat Basin. Included in a mapped unit of Late Triassic to Early Jurassic volcanic rocks: basalt, trachyte, nephelinite, phonolite, tuff and tuffaceous sandstone.||||||
27082|Garrawilla Volcanics|70791|5|Briefly described|p279|Mesozoic|Mesozoic|Gunnedah Basin.|||||Alkali volcanics.|
27082|Garrawilla Volcanics|70821|5|Briefly described|p80|||Coonamble Embayment. Tight aquitard.||||Unconformably overlies Napperby Formation. Is overlain unconformably by Purlawaugh Formation.||
27082|Garrawilla Volcanics|71890|4|Described|p5-p7, p17-p18, p31, p52|Toarcian|Norian|Surat Basin. Age equivalent of the Glenrowan Intrusives. Outcrops extensively south and east of Coonabarabran and south of Tooraweenah.|203 to 178 Ma|||Unconformably overlies the Napperby Formation. Conformably overlain by the Purlawaugh Formation or Pilliga Sandstone. Overlain by the Warrumbungle Volcanics.|Alkali basalt to sodic trachyte. Lava flows are flow-foliated, extremely vesicular to non-vesicular, porphyritic to equigranular and aphanatic. Pyroclastic flows are commonly interbedded with lava flows.|
27082|Garrawilla Volcanics|72298|5|Briefly described|p801|Triassic|Triassic|Coonamble Embayment (NSW).||||Unconformably overlies Napperby FZ. Is overlain unconformably by Purlawaugh FZ.||
27082|Garrawilla Volcanics|72921|5|Briefly described|p15 Fig.2.|Early Jurassic|Triassic|Shown as located in the Surat Basin in New South Wales.||||Shown as unconformably underlying Purlawaugh Formation||
25718|Gatelee Ignimbrite|22638|6|Mentioned|p64|||Correlates with Cowcumbala Rhyolite||||||
25718|Gatelee Ignimbrite|22768|5|Briefly described|p178||Early Devonian|||||||
25718|Gatelee Ignimbrite|22857|5|Briefly described|p178, p450 App.1, Tb.A1.6|Early Devonian|Early Devonian|Rhyodacitic ignimbrite, minor polymictic conglomerate. Max. thickness: >100m. ||||||
25718|Gatelee Ignimbrite|29454|4|Described|p11|||||||||
25718|Gatelee Ignimbrite|29648|4|Described|p11|||Lower-Middle Devonian||||||
25718|Gatelee Ignimbrite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
25718|Gatelee Ignimbrite|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25718|Gatelee Ignimbrite|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25718|Gatelee Ignimbrite|37529|5|Briefly described|p11|||||||||
25718|Gatelee Ignimbrite|37727|6|Mentioned|Fig.1|||||||||
25718|Gatelee Ignimbrite|39319|6|Mentioned|p357|||||||||
25718|Gatelee Ignimbrite|39331|4|Described|p41|||See also PP34, 42 & 43. Early Devonian||||||
25718|Gatelee Ignimbrite|40328|6|Mentioned|p37|||||||||
25718|Gatelee Ignimbrite|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
25718|Gatelee Ignimbrite|40498|6|Mentioned|p368|||||||||
25718|Gatelee Ignimbrite|40882|6|Mentioned|p25|||||||||
25718|Gatelee Ignimbrite|42045|6|Mentioned|p149|||||||||
25718|Gatelee Ignimbrite|42145|4|Described|Table 1 P624|||||||||
25718|Gatelee Ignimbrite|42313|1|Redefined|p144|Early Devonian||||||||
25718|Gatelee Ignimbrite|42314|5|Briefly described|Map|Early Devonian||||||||
25718|Gatelee Ignimbrite|42497|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
25718|Gatelee Ignimbrite|42726|5|Briefly described|map legend|Early Devonian||138.  Of the Boggy Plain Suite (Boggy Plain Supersuite).||||||08-FEB-05
25718|Gatelee Ignimbrite|42828|5|Briefly described|Fig.2 P128|||||||||
25718|Gatelee Ignimbrite|44093|5|Briefly described|p184 App. 1|Early Devonian|Early Devonian|Felsic volcanics. Geological Province: Lachlan Fold Belt.||||||
25718|Gatelee Ignimbrite|66197|6|Mentioned|p631 Fig.3a|||Silicic volcanics. Tumut Trough.||||||14-MAR-12
25718|Gatelee Ignimbrite|71040|6|Mentioned|p9|Early Devonian|Early Devonian|Tumut Trough. Post-dates deformation associated with Bindian (= Bowning) Orogeny; has a basal unconformity.||||||
23610|Gatum Gully Member|33476|6|Mentioned|Table 4|||||||||
23610|Gatum Gully Member|40505|6|Mentioned|p83|||||||||
23610|Gatum Gully Member|40773|6|Mentioned|p462|||||||||
26305|Gearys Gap Formation|40664|6|Mentioned|p248|||||||||
26305|Gearys Gap Formation|42727|5|Briefly described|map schematic section|Tertiary|Tertiary|Gravel, sand, silty clay; fluvial. Overlies Pittman Formation; underlies Ondyong Point Formation. See Lake George (Subsurface stratigraphy) schematic section and legend.||||||
26305|Gearys Gap Formation|42820|2|Defined|p57|early Miocene||||||||
26305|Gearys Gap Formation|47060|5|Briefly described|p163|||||||||
26305|Gearys Gap Formation|61155|5|Briefly described|p19|Late Pliocene|Late Miocene|Overlain by Lake George Formation (NSW). Thickness: 110m. Geological Province: Lake George.||||||11-APR-06
26305|Gearys Gap Formation|67125|5|Briefly described|Slide 36.|Cenozoic|Cenozoic|Tertiary. There is a deep weathering profile at the top of this unit.||||Unconformably overlies Pittmann Formation. Is overlain by Ondyong Point Formation.|Fluvial deposits of gravel, sand, silty clay.|
26305|Gearys Gap Formation|68592|6|Mentioned|p1841|||Mentioned in the context of estimating the thickness of Cenozoic fluvial sediments in northern Lake George, by correlation with this Formation.||||||
26305|Gearys Gap Formation|70377|4|Described|p853-855,p856-857, p858, 859, 866, 868|Piacenzian|Zanclean|Lake George Basin. Thickness at type section Core C354: Approximately 58m. Likely began accummulating in paleochannels of tributaries to present-day Yass River. Cosmogenic nuclide (10Be/25Al) burial ages  quartzite gravels + paleomagnetic and palynostratigraphic age constraints for Gearys Gap Formation. Sampled at 163.75 - 164.6 m (base of unit) for burial age. Minimum age from dating in overlying unit, and palynostratigraphy.|3.93 +\- 0.36 Ma burial age near base.|||Lowermost and oldest unit infilling Lake George. Underlain unconformably by Pittman Formation and upper Silurian volcanoclastics. Overlain by Ondyong Point Formation.|Deeply weathered, horizontally bedded sands and subrounded, poorly sorted quartz-rich gravels and minor silt and clay strata. Fluvial sands and gravels.|
26305|Gearys Gap Formation|71069|5|Briefly described|p21 fig 7, p33, p208, p209|Pliocene|Miocene|Named for Gearys Gap on the shore of Lake George. Believed to represent fluvial deposition by streams truncated by the Lake George Fault. Representatitve section nominated in BMR drillhole C354 at GR 71810 6113990. Thickness is variable but a maximum estimated thickness of 58m is given from BMR drillhole C354.Age derived on the basis of magnetostratigraphy and relationships with older material from drillhole C354. See also  p213-p214, p223.||Weereewa Group||Overlain by the Ondyong Point Formation, or the Bungendore Formation.|Deeply weathered, horizontally bedded sand and gravel with minor alluvial silt and clay interbeds.|
26305|Gearys Gap Formation|71691|5|Briefly described|Map legend.|Quaternary|Neogene|||Weereewa Group.||Is overlain by Ondyong Point Formation.|Horizontally bedded, fluvial, sand and gravel with minor silt and clay interbeds.|
30747|Genowlan Formation|43363|14|Not recorded|Map Legend|||(Provisional first edition)||||||
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.||||||
32273|Geordies Spur Gabbro|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Og3||||||
32273|Geordies Spur Gabbro|60078|6|Mentioned|Map Legend|Ordovician|Ordovician|||||||
70111|Georges Bore Granite Gneiss|64097|2|Defined|p328 Appdx., p305 Fig. 2, p317-318|Paleoproterozoic|Paleoproterozoic|Age: 1695 +/- 4 Ma. Mapped by Stroud (1986) as a coarse- to v.coarse-grained qtz-feldspar-biotite gneiss + abundant K-feldspar megacrysts and lesser fine- to med.gr.gneiss lacking megacrysts.Overlain/flanked by Himalaya Fm.+ in part by Broken Hill Group||||||07-FEB-11
70111|Georges Bore Granite Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1695+/-4Ma. Geological province: Broken Hill Domain. Written as Georges Bore only.||||||07-FEB-11
70111|Georges Bore Granite Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1695+/-4Ma. Geological province: Broken Hill Domain. Name presented only as Georges Bore.||||||07-FEB-11
70111|Georges Bore Granite Gneiss|68126|6|Mentioned|p30||||1695 +/- 4 Ma (Stevens et al. 2008).|||||
70111|Georges Bore Granite Gneiss|70000|6|Mentioned|p34|Statherian|Statherian|||Unit in Silver City Suite.||||
70111|Georges Bore Granite Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Silver City Suite.|||Megacryst-rich and megacryst-poor quartz-feldspar-biotite gneiss, and minor garnet-bearing gneiss.|
70111|Georges Bore Granite Gneiss|70657|4|Described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|1695 +/- 4 Ma|Silver City Suite||Intrudes Himalaya Formation (Thackaringa Group). ?Underlies Rasp Ridge Granite Gneiss.|Intrusive S-type felsic rocks (granite sills), metamorphosed to gneiss.|
70111|Georges Bore Granite Gneiss|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian||1695 +/- 4 Ma|||||
70111|Georges Bore Granite Gneiss|73308|6|Mentioned|p607 Fig.1||||1695 +/- 4 Ma.|||||
70111|Georges Bore Granite Gneiss|73482|5|Briefly described|p422 Fig.3|Statherian|Statherian||1695+/-4 Ma|Silver City Suite||||
70111|Georges Bore Granite Gneiss|73575|5|Briefly described|p828 Fig.2|Statherian|Statherian||1695+/-4 Ma||Silver City Suite|||
28570|Georges Knob Conglomerate Member|32801|6|Mentioned|Fig.5|||||||||
28570|Georges Knob Conglomerate Member|34340|3|Fully described|p462|||||||||
28570|Georges Knob Conglomerate Member|37112|5|Briefly described|Table 1|||||||||
28570|Georges Knob Conglomerate Member|61310|5|Briefly described|Table C1 (p22-23)|Middle Triassic|Middle Triassic|Of the Basin Creek Formation. Pebble conglomerate, minor claystone, siltstone, sandstone. Geological Province: Clarence-Moreton Basin||||||
83228|Getty Gabbro|73175|5|Briefly described|p1050 Fig.1, p1053, p1055 Tb.1, p1066|Cambrian|Ediacaran|Shows age of 535+/-19 in Fig 1, but appears to show apatite U/Pb LA-ICP-MS maximum emplacement age on monzodiorite of 280+/-120 Ma. Previously considered to be Neoproterozoic, but may include xenocrystic zircons from Cobar Basin sedimentary rocks, and so may actually be Permo-Triassic.|Previously 535 +/- 19 Ma|||||
37290|Ghangat Basalt|24008|5|Briefly described|p350|Late Devonian|Middle Devonian|||||||
69999|Ghanghat Basalt|61766|4|Described|p67|Late Devonian|Middle Devonian|Thick flows of commonly vesiculated structureless and pillowed basalt; thin intercalations of ash-fall tuff and siliceous green and purple laminated slts are present. Contains radiolarian rich slts. Gradational with Bulliac Fm. Geol. Prov: Tamworth Belt.||||||
42501|Ghost Rocks Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tumboramboro Suite. Grey-brown mylonitised muscovite-biotite-quartz-feldspar megacrystic granite. Rounded K-feldspar porphyroblasts (<50mm), and plagioclase crystals in a foliated groundmass of biotite and muscovite folia and ribbons of recryst.qtz.||||||
42501|Ghost Rocks Granite|68592|2|Defined|p88, p135, p650, p1543, p1589-92|Early Devonian|Early Devonian|New name, after Ghost Rocks locality. Crops out as regular large boulders. Type locality described. Has undergone middle to upper greenschist facies regional metamorphism. Geophysical properties described. No direct age; tentative age based on intrusive relationship.||Unit in Tumboramboro Suite.||Intrudes Cuddyong Formation. Is overlain by Crookwell Basalt. Is faulted against Tumboramboro Granite.|Brown, schistose to mylonitic biotite granite which has undergone considerable grainsize reduction leaving large K-feldspar porphyroclasts to 50mm.|
42501|Ghost Rocks Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dtg. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Tumboramboro Suite|||Mylonitised, megacrystic biotite granite; rounded K feldspar porphyroclasts and plagioclase crystals in a foliated groundmass of biotite and muscovite folia and ribbons of recrystallised quartz. Low-high K & U, low-medium Th; low mag susceptibility.|
42501|Ghost Rocks Granite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Tumboramboro Suite|||Mylonitised, megacrystic biotite granite; rounded K feldspar porphyroclasts and plagioclase crystals in a foliated groundmass of biotite and muscovite folia and ribbons of recrystallised quartz. Low-high K & U, low-medium Th; low mag susceptibility.|
82450|Giants Den Leucosyenogranite|71628|4|Described|p4: 1, 5, 9, 23-28, 39-40, 42, 44-45|||See also p4: 48, 50, 55. New unit, named after a local mountain (with a significant Sn deposit). Southern New England Orogen. Unclear how, or if, these rocks differ from Glenclair Syenogranite: almost indistinguishable geochemically. Crops out as broad sheets rather than tors. Geochemistry described.|288.7 +/- 1 Ma (SHRIMP: Cross and Blevin, 2013).|Glenclair Suite.||Abuts Glenclair Syenogranite, Pringles and Namoi Tops Monzogranites.|Fine- to medium-grained, porphyritic to even-grained leucosyenogranite; minor leucomonzogranite. S-type.|
26570|Gibraltar Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Gibraltar Adamellite etc? Bega Batholith.||||||
26570|Gibraltar Granite|64137|6|Mentioned|p1553 Fig.8 |||Neodymium isotope data.||||||
26570|Gibraltar Granite|71069|4|Described|p21 fig 7, p174, p175, p189|Ludlow|Wenlock|Name derived from Gibraltar Hill. Previously termed the Gibraltar Adamellite by Abell (1991). Petrography described briefly. Intruded into the Goulburn Basin as part of a larger magmatic system. See also  p193, p195-196.||Thurralilly Suite||Equivalent to the Ellenden Granite, Lockhart Igneous Complex, Butmaroo Granite, Tallaganda Granodiorite and the Gourock Granodiorite. Intrudes the Abercrombie Formation.|Strongly foliated, medium to coarse grained biotite granite with mafic rich xenoliths.|
26570|Gibraltar Granite|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Thurralilly Suite.|||Strongly foliated, medium- to coarse-grained biotite granite, with mafic-rich xenoliths.|
35899|Gibsonvale Formation|61964|2|Defined|p14 Fig. 4, p139, p154|Early Pliocene|Late Oligocene|Poorly lithified to friable quartzose conglom., pebbly sandstone + sandstone containing common detrital cassiterite; subrounded to rounded clasts; white vein clasts dominant with minor cassiterite+metased. lithic clasts. Contains tin-bearing deep leads.||||||03-NOV-15
35899|Gibsonvale Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Cream to white coarse-grained quartz sandstone to gravel, mottled red brown in places; hosts cassiterite concentrations.||||||
35899|Gibsonvale Formation|69160|5|Briefly described|Map legend|Tertiary|Tertiary||||||Cream to white coarse quartz sandstone to gravel, mottled red-brown in places; hosts cassiterite concentrations.|
73666|Gidyen Volcanic Member|63278|5|Briefly described|p156|||Of the Triangle Formation. Overlain by Mozart Chert. Geological Province: Rockley Volcanic Belt, LFB. Consists of massive pyroxene basalt lavas and breccias with clasts of lava and chert.||||||21-FEB-18
73666|Gidyen Volcanic Member|67322|5|Briefly described|p17-18|||Murray and Stewart (2001). Never formally defined and appears to represent an admixture of allochthonous debris indistinguishable from the Rockley Volcanics. Occurs in the Oberon-Rockley region.||Unit in Triangle Formation.||||21-FEB-18
82453|Gilgai Leucogranite|71628|4|Described|p4:1,17,19: p8: 44-45, 47-48; p15:87-88|||See also p19: 28, 31, 33, 35-36, 42-52, 78, 118-119, 142, 144, 169. New name (this study); previously Gilgai Granite (Korsch, 1977). Originally Howell Granite (Andrews et al., 1907). Copeton area, southern New England Orogen. Resistant; crops out as sheets, and tors to 10m diameter. Highly fractionated. Lithology, mineralogy, geochemistry and mineralisation are described in great detail. Has high to extremely high radiometric response. Is extensively mineralised: hosts lode and placer Sn deposits, base metals, disseminated As-U deposits, Mo veins and disseminations, and is a source of fluorite, quartz, silica, kaolin and dimension stone.|252.2 +/- 1.8 Ma (Cross and Blevin, 2010).|Gilgai Suite.||Intrudes Copeton and Tingha Monzogranites (the latter is discussed), Sandon beds, Wandsworth Volcanic Group. Abuts Tingha Monzogranite (boundary obscured).|Pink to grey, microgranitic to coarse-grained, porphyritic to equigranular biotite-(hornblende) leucogranite; contains abundant miarolitic cavities and granophyric intergrowths. I-type.|
25923|Gilgal Formation|22857|5|Briefly described|p456 App.1 Tb.1A1.6|Devonian|Silurian|Of the Toongi Group. Max. thickness: 600m. Shale, siltstone, tuff. Geological Province: Cowra Trough.||||||
25923|Gilgal Formation|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Toongi Group.||||||
25923|Gilgal Formation|23170|2|Defined|p116|Late Silurian|Late Silurian|of Toongi Group.||||||
25923|Gilgal Formation|29986|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25923|Gilgal Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
25923|Gilgal Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
25923|Gilgal Formation|40328|2|Defined|p126|Silurian|Silurian|||||||
25923|Gilgal Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
25923|Gilgal Formation|43500|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition) Part of Toongi Group||||||
25923|Gilgal Formation|48958|6|Mentioned|Plate 1|||||||||
25923|Gilgal Formation|68003|5|Briefly described|p24 Fig.3-e, p145. |Wenlock|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion. Subsurface distribution has a mottled aeromagnetic appearance.||Unit in Toongi Group.||Overlies Gullengumbel Formation. Is overlain by Berridong Siltstone.|Shale, siltstone, rhyolitic tuff, lithic sandstone, volcaniclastic sandstone, quartzose sandstone, phyllite.|
79855|Gillenbah Granite|71889|4|Described|p7-p8, p13-p15, p17-p20|Silurian|Silurian|Defined by Trigg, 2017 and is an elongate body extending in a southeasterly direction for over 60km from c. 10km west of Narrandera to c. 10km to the north-northeast of Lockhart. Outcrops south of Narrandera, southeast of Galore Hill, in the Morgans mine pit and as scattered outcrops of weathered granite for over a kilometre at the base of 'Strontian hills'. In the Morgans mine pit this unit is almost completely altered to kaolin and coarse-grained muscovite.This unit has previously been intersected in drill core (DH Esso Cuddel B19).  See also  p22, p36, p41, p56, p58.|c. 427 Ma (Bodorkos et al, in prep.)|||Overlain by the Cocoparra Group.|Mylonitic granite and medium- to coarse-grained granite with remamnet quartz and feldspar which is largely altered to kaolin.|
79855|Gillenbah Granite|72083|3|Fully described|p7-8, p11, p22-26, p53 Fig.8, p54|||New name; from Gillenbah locality a few kms SW of Narrandera. Previously known only from drill core. Extends c.60km SE from just S of Narrandera; exposed on the SW flanks of Galore Hill. Is obvious in magnetic imagery: has relatively low and uniform response. Outcrop photographs.|c.427 Ma (Bodorkos et al., in prep.).|||Is overlain by Galore Hill Formation (Cocoparra Group). Probably intrudes Wagga Group.|Mylonitic granite. Coarse grains of feldspar and muscovite; quartz and ?tourmaline also present.|
79855|Gillenbah Granite|73457|5|Briefly described|p4, p6|Ludlow|Wenlock|Sheared and unroofed before deposition of the Galore Hill Formation.|427+/-2.3 Ma (Bodorkos et al., 2021)|||Nonconformably underlies Galore Hill Formation||
36329|Gillieston Sequence|23540|5|Briefly described|p 421|||Also see p 423||||||
69147|Gilmore Hill Suite|60423|5|Briefly described|p372, Fig. 3|Late Devonian|Late Devonian|Sodic I Type granites. Of the Temora Complex/Narraburra Complex. Age: 365 +/- 4 Ma, Rb/Sr age. Geological Province: Lachlan Fold Belt.||||||30-APR-10
35360|Gilwhite Limestone|23185|6|Mentioned|Fig4p160,160,172|Eifelian|Emsian|||||||
82455|Girard Creek Diorite|71628|5|Briefly described|p9:5; p19: 52-53|||New (apparently not previously published) name, after unpublished work by Biddle (1977). Named after a local watercourse. Occurs ~9 km NE of Drake, and crops out poorly as small rounded tors in a 2 x 1 km area. The text states it intrudes (p9-5) and is intruded by (p19-52) the Bruxner Granodiorite.||Girard Creek Suite.||Intrudes Emu Creek Formation, Razorback Creek Mudstone and Drake Volcanics.|Light to dark grey, fine- to medium-grained, equigranular clinopyroxene-orthopyroxene-hornblende-biotite diorite to quartz diorite. Thrust-faulted and weakly jointed.|
27158|Girilambone Group|730|5|Briefly described|p15-19, p24, p22 Fig.5, p35 Fig.7, p59.|Ordovician|Cambrian|Metamorphosed and deformed clastic sedimentary rocks with chert, volcanics, limestone. Underlies, probably with angular unconformably, Mulga Downs Group. Unconformably overlain by Tertiary gravel near Coolabah. Low level mineralisation, including gold in quartz veins.||||||11-NOV-14
27158|Girilambone Group|9548|5|Briefly described|Map Legend|Ordovician|Cambrian|Quartzo-feldspathic schist, sandstone and siltstone.||||||06-JUL-04
27158|Girilambone Group|22508|6|Mentioned|p2||Late Ordovician|Lachlan Fold Belt||||||
27158|Girilambone Group|22519|5|Briefly described|p3|||||||||
27158|Girilambone Group|22555|5|Briefly described|p371, Fig.1p372|Caradoc|Llanvirn|||||||
27158|Girilambone Group|22557|6|Mentioned|p569|||||||||
27158|Girilambone Group|22580|6|Mentioned|p89|Ordovician|Cambrian|||||||
27158|Girilambone Group|22638|6|Mentioned|p16|Early Ordovician||Max age ?Cambrian. Correlative of the Jindalee Group.||||||
27158|Girilambone Group|22700|6|Mentioned|p785|||||||||
27158|Girilambone Group|22704|6|Mentioned|p52|Early Ordovician||||||||
27158|Girilambone Group|22768|6|Mentioned|Fig16.8p168||Ordovician|||||||
27158|Girilambone Group|22831|3|Fully described|p 11- 15||Early Ordovician|||||||
27158|Girilambone Group|22857|5|Briefly described|p76, p91 Fig. 14.7B|Ordovician|Late Cambrian|Ophiolitic rocks. May be Cambro-Ordovician in age? Part of the Girilambone Slope and Basin. Max. thickness: >4km. See also p406 App.1 Tb. A1.4, pages 412 and 414 App. 1 Tb. A1.5, and p168 Fig. 16.8.||||||
27158|Girilambone Group|22858|6|Mentioned|p78,81,Fig14.7bp90-1|||||||||
27158|Girilambone Group|22933|6|Mentioned|p24|||||||||
27158|Girilambone Group|23053|4|Described|p8,11,19,69,85|Late Ordovician|Cambrian|||||||
27158|Girilambone Group|23088|5|Briefly described|p652, 651|||||||||
27158|Girilambone Group|23095|5|Briefly described|p610 (table 1)|Ordovician|Cambrian|||||||
27158|Girilambone Group|23096|6|Mentioned|p601 (Fig 1)|||||||||
27158|Girilambone Group|23097|5|Briefly described|p594||Ordovician|||||||
27158|Girilambone Group|23101|5|Briefly described|p567 (Fig 1), p568||Ordovician|||||||
27158|Girilambone Group|23171|4|Described|p11,17-9,22||Early Ordovician|||||||
27158|Girilambone Group|23173|4|Described|Map Legend|Late Ordovician|Late Cambrian|||||||
27158|Girilambone Group|23213|5|Briefly described|Fig.10|Late Ordovician|Ordovician|Age: Middle Ordovician to Late Ordovician. of Cobar Trough.||||||
27158|Girilambone Group|23245|4|Described|p103,123,125,133|Ordovician|Cambrian|||||||
27158|Girilambone Group|23367|6|Mentioned|p15|||||||||
27158|Girilambone Group|23371|5|Briefly described|p34|Ordovician|Ordovician|||||||
27158|Girilambone Group|23454|5|Briefly described|p32|Ordovician|Ordovician|||||||
27158|Girilambone Group|23734|5|Briefly described|p12 Fig. 1|||Basement unit of sandstone, mudstone and chert.||||||20-OCT-08
27158|Girilambone Group|23736|5|Briefly described|p11|||||||||
27158|Girilambone Group|24007|5|Briefly described|p327|Ordovician|Ordovician|||||||
27158|Girilambone Group|24037|6|Mentioned|p424 Fig.1|||Geological Province: Lachlan Fold Belt.||||||
27158|Girilambone Group|24215|5|Briefly described|p802|||Geological Province: Lachlan Fold Belt||||||06-NOV-13
27158|Girilambone Group|24233|5|Briefly described|p253 Fig.1, p256|||Geological Province: Lachlan Orogen.||||||
27158|Girilambone Group|24266|5|Briefly described|p1469|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
27158|Girilambone Group|24267|4|Described|p1508|Ordovician|Cambrian|Overlain by Forbes Group. Geological Province: Parkes-Narromine Belt.||||||20-OCT-08
27158|Girilambone Group|24280|5|Briefly described|p1831|Ordovician|Cambrian|Geological Province: Lachlan Fold Belt.||||||09-MAR-05
27158|Girilambone Group|24417|2|Defined|p13|Late Ordovician|Late Ordovician|Originally named "Girilambone Series".  Also previously termed "Girilambone Beds" by Brunker (1969). Geological Province: Lachlan Fold Belt. Intruded by Billys Lookout Granite and intruded and overlain by Ina Volcanics. Age from Late Ordovician conodonts in Murda Formation.||||||27-JAN-11
27158|Girilambone Group|24600|5|Briefly described|p479|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
27158|Girilambone Group|29621|6|Mentioned|Table 1|||||||||
27158|Girilambone Group|29680|6|Mentioned|Fig.1|||||||||
27158|Girilambone Group|29947|6|Mentioned|p685|||||||||
27158|Girilambone Group|29948|6|Mentioned|Fig.12|||||||||
27158|Girilambone Group|31592|6|Mentioned|Fig. 1|||Pre U.Silurian||||||
27158|Girilambone Group|32087|4|Described|p7|||||||||
27158|Girilambone Group|33732|6|Mentioned|p114|||||||||
27158|Girilambone Group|34400|6|Mentioned|p6|||See also p12 - problematical.||||||23-SEP-18
27158|Girilambone Group|34402|6|Mentioned|p75|||Pre Ordovician basement or extension of Wagga Metamorphic Belt.||||||
27158|Girilambone Group|34404|4|Described|p98|||Interpretation p99.||||||20-OCT-08
27158|Girilambone Group|34405|6|Mentioned|p125|||See also p126.||||||23-SEP-18
27158|Girilambone Group|34406|5|Briefly described|p216|||Pre-Ordovician basement. See also p219.||||||20-OCT-08
27158|Girilambone Group|34449|4|Described|Table 2-1|||Pre-Silurian.||||||20-OCT-08
27158|Girilambone Group|35118|6|Mentioned|Fig.5|||||||||
27158|Girilambone Group|35287|6|Mentioned|Table 1|||||||||
27158|Girilambone Group|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
27158|Girilambone Group|37529|6|Mentioned|p4|||||||||
27158|Girilambone Group|37727|6|Mentioned|p47|||SSee also Fig.1.||||||
27158|Girilambone Group|38292|6|Mentioned|p3|||||||||
27158|Girilambone Group|39064|6|Mentioned|Fig.1|||||||||
27158|Girilambone Group|39083|5|Briefly described|p27|||||||||
27158|Girilambone Group|39084|6|Mentioned|Fig.1|||||||||
27158|Girilambone Group|39618|6|Mentioned|Table 1|||See also Table 2||||||
27158|Girilambone Group|40136|5|Briefly described|p25|||||||||
27158|Girilambone Group|40365|6|Mentioned|p236|||||||||
27158|Girilambone Group|40677|5|Briefly described|p24|||||||||
27158|Girilambone Group|40678|6|Mentioned|p2|||||||||
27158|Girilambone Group|40682|6|Mentioned|Fig.1|||||||||
27158|Girilambone Group|40762|6|Mentioned|p269|||||||||
27158|Girilambone Group|40766|5|Briefly described|p25|||||||||
27158|Girilambone Group|41138|6|Mentioned|Map legend|Ordovician|Cambrian|Cambro-Ordovician||||||
27158|Girilambone Group|41394|4|Described|p9|||||||||
27158|Girilambone Group|41410|6|Mentioned|p295|||||||||
27158|Girilambone Group|41452|6|Mentioned|p22|||||||||
27158|Girilambone Group|41528|2|Defined|p21|Early Silurian|Late Ordovician|||||||
27158|Girilambone Group|41529|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
27158|Girilambone Group|41594|6|Mentioned|p28|||See also p32.||||||23-SEP-18
27158|Girilambone Group|41872|6|Mentioned|p8|||||||||
27158|Girilambone Group|42045|6|Mentioned|p149|||||||||
27158|Girilambone Group|42077|5|Briefly described|p27|||||||||
27158|Girilambone Group|42144|6|Mentioned|p603|||||||||
27158|Girilambone Group|42171|5|Briefly described|p142|||See also Table 2||||||
27158|Girilambone Group|42313|6|Mentioned|p30|||||||||
27158|Girilambone Group|42332|5|Briefly described|p162|Ordovician|Cambrian|||||||
27158|Girilambone Group|42449|5|Briefly described|p12|||||||||
27158|Girilambone Group|42521|5|Briefly described|p13|||||||||
27158|Girilambone Group|42566|3|Fully described|p17|||||||||
27158|Girilambone Group|42568|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
27158|Girilambone Group|42596|5|Briefly described|Fig. 1 P24|||||||||
27158|Girilambone Group|42603|6|Mentioned|p53|||||||||
27158|Girilambone Group|42725|6|Mentioned|p10|||||||||
27158|Girilambone Group|42907|6|Mentioned|Fig.8, P8|||||||||
27158|Girilambone Group|42983|5|Briefly described|p342|||||||||
27158|Girilambone Group|43032|3|Fully described|p19|||||||||
27158|Girilambone Group|43089|5|Briefly described|Map Legend|||||||||
27158|Girilambone Group|43090|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
27158|Girilambone Group|43153|5|Briefly described|Map Legend||Ordovician|||||||
27158|Girilambone Group|43213|6|Mentioned|p63|||Written as Girilambone beds (or Group).||||||
27158|Girilambone Group|43263|6|Mentioned|Map Legend||Ordovician|||||||
27158|Girilambone Group|43276|5|Briefly described|Map Legend|Ordovician|Late Cambrian|||||||
27158|Girilambone Group|43277|5|Briefly described|Map Legend|Late Ordovician|Late Cambrian|Of Lachlan Fold Belt.||||||08-APR-09
27158|Girilambone Group|43384|14|Not recorded|Map Legend||Ordovician|||||||
27158|Girilambone Group|43441|3|Fully described|p3-6|Late Ordovician||Age:?Early - ?Late Ordovician.||||||08-JAN-10
27158|Girilambone Group|43479|14|Not recorded|p62,77||Ordovician|pre-Ord?||||||
27158|Girilambone Group|43757|5|Briefly described|p510|Ordovician|Cambrian|||||||
27158|Girilambone Group|43774|3|Fully described|p10-12||Ordovician|||||||
27158|Girilambone Group|44093|5|Briefly described|p50, p114|Ordovician|Cambrian|Geological Province: Lachlan Fold Belt.||||||
27158|Girilambone Group|44160|5|Briefly described|Map Legend|Llandoverian|Cambrian|||||||
27158|Girilambone Group|46032|2|Defined|p.411-414||Late Silurian|(H55-14/Cobar). Pre Upper Silurian.||||||20-OCT-08
27158|Girilambone Group|46524|6|Mentioned|p118|||||||||
27158|Girilambone Group|48958|6|Mentioned|p1|||||||||
27158|Girilambone Group|50385|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
27158|Girilambone Group|50554|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Murda Formation. Overlain by Lake Cowal Volcanic Complex.||||||06-NOV-13
27158|Girilambone Group|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Metasediments.||||||
27158|Girilambone Group|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|Includes: Murda Formation.||||||13-JUL-04
27158|Girilambone Group|60902|5|Briefly described|p876|Ordovician|Ordovician|Turbidites; spaced cleavage/stripey layering is widespread in parts of this unit.||||||
27158|Girilambone Group|61814|6|Mentioned|p7|||||||||
27158|Girilambone Group|61817|5|Briefly described|p80|Ordovician|Ordovician|||||||
27158|Girilambone Group|61905|5|Briefly described|p135 Fig. 1|||Geological Province: Cobar Basin.||||||
27158|Girilambone Group|61911|5|Briefly described|p155|Ordovician|Ordovician|Flysch sediments and medium-grained, quartz rich greywackes regionally metamorphosed to quartz-chlorite-sericite schists.||||||23-SEP-18
27158|Girilambone Group|61964|4|Described|p14 Fig. 4, p35|Middle Ordovician|Early Ordovician|Superseded "Girilambone Series". Very thinly interbedded, well-sorted metasiltstone and fine- to medium-grained metasandstone of pale tan brown with greenish to purplish hues; rocks strongly deformed.||||||27-JAN-11
27158|Girilambone Group|62035|6|Mentioned|p31|Late Ordovician|Early Ordovician|New mapping has shown this unit can be subdivided into Early, Middle and Late ordovician components - in the new Cobar-Bourke mapping project (2006)||||||
27158|Girilambone Group|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Phyllite and metamorphosed muddy sandstone, minor siltstone and chert.||||||20-OCT-08
27158|Girilambone Group|63185|5|Briefly described|p2 Fig. 2|Ordovician|Cambrian|Metasedimentary rocks.||||||12-APR-07
27158|Girilambone Group|63283|6|Mentioned|p206, p210|Ordovician|Ordovician|Deformed Ordovician sediments.||||||07-FEB-11
27158|Girilambone Group|63288|6|Mentioned|p360, p361|||Consists of turbidites.||||||
27158|Girilambone Group|63289|6|Mentioned|p372|||Geological Province: Junee - Narromine Volcanic Belt. Consists of quartz-rich turbidites that are tightly folded multiply cleaved and metamorphosed to upper greenschist facies.||||||07-FEB-11
27158|Girilambone Group|63290|5|Briefly described|p388, p395|Late Ordovician|Early Ordovician|Overlain by Bendoc Group and Edols Conglomerate. Quartz-rich.||||||20-OCT-08
27158|Girilambone Group|64568|5|Briefly described|Map legend|Ordovician|Ordovician|Phyllite and metamorphosed muddy sandstone, minor siltstone and chert.||||||
27158|Girilambone Group|64681|5|Briefly described|p1, p2, p3 Fig. 1|Ordovician|Ordovician|Turbidite - interbedded sandstones, siltstones, mudstone.||||||
27158|Girilambone Group|64962|5|Briefly described|p202|Paleozoic|Paleozoic|Dominantly metasedimentary rocks.||||||08-APR-09
27158|Girilambone Group|65384|6|Mentioned|S105|Ordovician|Cambrian|||||||
27158|Girilambone Group|65469|5|Briefly described|p14, p16-p20, p43, p52, |Late Ordovician|Early Ordovician|Lachlan Orogen. Deformed during the early Silurian Benambran Orogeny.  See also p55 fig 3-19,  p62, p67, p78, p94, p127, p133, p136, p139, p141, p142, p144, p146, p326-p327, p336, p346, p358, p360, p388, App A-VI 3, App A-VI 5.|||Includes the Whitefell Chert and the Alandoon Chert.||Turbidite deposits.|
27158|Girilambone Group|65756|5|Briefly described|p27, 30, 34, 35, 37|Ordovician|Ordovician|deep-marine turbidites||||||
27158|Girilambone Group|67106|6|Mentioned|p681, 683|||||||||
27158|Girilambone Group|67107|6|Mentioned|p700|||||||Is intruded by Fifield Complex.|Siliciclastic metasedimentary rocks.|
27158|Girilambone Group|67127|6|Mentioned|p172|Ordovician|Cambrian|Intruded by several 'Alaskan'-type intrusions of mafic-ultramafic rocks such as the Gilgai intrusion.|||||Metasedimentary rocks.|
27158|Girilambone Group|67322|4|Described|p4 Fig.2, p5, p13, p19-20; Fig.5|Darriwilian|Tremadocian|Hermidale Terrane. Complicated nomenclatural history: see Pogson (1991). Initially the Girilambone Series of Andrews (1915) which excluded the Ballast Beds that are now a constituent Formation of the Girilambone Group. First usage of Girilambone Group was by Russell and Lewis (1965). The most recent revision of the Girilambone Group is by Trigg and Burton et al. (in press). Maximum age determined from the constituent Narrama Formation, and minimum from  p20 Fig.5 (Strat. column). Occurs in the Sussex-Byrock region.|||Ballast Formation, Narrama Formation, Murda Formation, Break O'Day Amphibolite, Tritton Formation, Tottenham Subgroup.||Coarse- to fine-grained sandstones and siltstones of turbiditic origin, with associated pelagic sediments.|21-FEB-18
27158|Girilambone Group|67416|5|Briefly described|p83, p85-86, p89|Ordovician|Ordovician|At the Blind Calf historic diggings, hosts numerous Cu-Au-Bi lodes.|||||Quartz and quartzofeldspathic sandstones, pelites, cherts, and minor mafic volcanics.|
27158|Girilambone Group|67803|5|Briefly described|p34|Ordovician|Ordovician|The Wagga and Girilambone Groups and western Adaminaby Group (with overlying shales) constitute the Girilambone-Wagga Terrane in the Wagga Basin. These are in situ deposits.|||||Includes cherts and black shales.|
27158|Girilambone Group|67817|5|Briefly described|p117-119|Ordovician|Late Cambrian|Variably-metamorphosed quartzose turbidite succcession. Structure described. Hosts numerous Cu mineralisations. Tectonics discussed. Plateau ages: 435 Ma (Tottenham) or 480-500 Ma (Hartmans Pit).|||||Psammitic schist, pelitic schist, cleaved sandstone, quartzite and slate; subordinate chert, mafic schist; rare serpentinite. Lithologies vary with locality.|
27158|Girilambone Group|67821|5|Briefly described|p150, p187|Ordovician|Ordovician||||||Metasediments: turbidite package.|
27158|Girilambone Group|67847|6|Mentioned|p21, p54|Middle Ordovician|Early Ordovician|Wagga Basin. ||||||
27158|Girilambone Group|68003|6|Mentioned|p23. |Early Ordovician|Early Ordovician|||||||
27158|Girilambone Group|68466|6|Mentioned|p63, 65-66|Ordovician|Ordovician|Hermidale Terrane, central NSW. Extends N and E of Cobar.|||Narrama, Ballast Formations.|||
27158|Girilambone Group|68592|6|Mentioned|p298, p307-8|||||||||
27158|Girilambone Group|68822|5|Briefly described|p334, p335, p347, p349, p351|Early Ordovician|Early Ordovician|Interpillow cherts contain Chewtonian and Castlemainian 1 conodont Oepikodus evae (Percival et al. 2011). Contains mafic volcanics with a mean LA-ICPMS zircon age of 484 Ma (unpublished data and Jones 2012). |ca. 477 - 474 Ma (conodont)|||Overlain by the Bendoc Group.||10-NOV-14
27158|Girilambone Group|68823|5|Briefly described|pp376-378, p386, p388-400, p406, p409|Gisbornian|Lancefieldian|Source of Nurri Group sediments.|||||Comprises turbidites and cherts, with a minor mafic volcanic component.|
27158|Girilambone Group|69002|5|Briefly described|p7, p10, p11, p13, p14, Map 1b, Legend|||Comprises a region of low magnetic intensity having bedding/foliation linear magnetic fabric.|625-470 Ma detrital zircon age range.||||Comprises siliclastic metasedimentary rocks.|28-NOV-13
27158|Girilambone Group|69042|5|Briefly described|map legends|Ordovician|Ordovician|Og. Lachlan Orogen. Region of low magnetic intensity having bedding/foliation linear magnetic fabric. Siliciclastic metasediments. Misspelt as Girtilambone Group on separate map legend page.||||||
27158|Girilambone Group|69043|6|Mentioned|p11|Ordovician|Ordovician|||||||
27158|Girilambone Group|69094|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician||||Includes Lang and Ballast Formations.|||
27158|Girilambone Group|69095|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician||||Includes Lang and Ballast Formations.|||
27158|Girilambone Group|69540|6|Mentioned|p640-641||Early Ordovician|A correlation is suggested between the oldest part of this unit and the Warratta Group.||||||
27158|Girilambone Group|69541|5|Briefly described|p643, p648, p652-653|Middle Ordovician|Early Ordovician|Lachlan Orogen. Fergusson et al. (2005) reported 5 Permian to Cretaceous zircon grains out of 120; used to demonstrate zircon crystallisation in older rocks from younger hydrothermal or magmatic fluids. There is no overlying black shale equivalent to the Bendoc Group, which overlies the Adaminaby and Wagga Groups.|||Includes basal Narrama Formation.|Possibly correlated with Castlemaine Group.|Quartz-rich turbidites and interbedded cherts.|
27158|Girilambone Group|69635|5|Briefly described|p96-104, Table 1, p69, 70, 78, 84, 88 |Ordovician|Ordovician|North-western Lachlan Orogen. U-Pb SHRIMP zircon maximum depositional age. See also pages 108, 119, 120, 140, 148.|496.0+/-2.5 Ma||Includes Ballast Formation, Narrama Formation.|Intruded by Honeybugle Complex, Wilgaroon Granite (hornfels contact aureole).||
27158|Girilambone Group|69668|5|Briefly described|p927, p929 Fig.2, p930 Fig.3, p931, p948|Middle Ordovician|Early Ordovician|Hermidale terrane, central NSW. Geochemical similarity of cherts with those of the Adaminaby Group suggests both regions shared identical sources and depositional regimes, occupying near-identical tectonic settings in a back-arc basin.|||Includes Narrama and Ballast Formations.|||18-JUN-20
27158|Girilambone Group|70178|6|Mentioned|p3, p4 fig. 2|Ordovician|Ordovician||||||Phyllite and siliciclastic turbidite sequences.|
27158|Girilambone Group|70493|6|Mentioned|p63|Middle Ordovician|Early Ordovician|||||||
27158|Girilambone Group|70602|4|Described|p65-72,75|Middle Ordovician|Early Ordovician|Age constrained by detrital zircons and conodonts. Knightvale area, sericite schist, chert units mapped. Petrographic descriptions and structural map given. Aeromagnetic map data given, sericite schist unit depicted.|496+/-2.5Ma detrital zircon.||Includes Ballast Formation, Lang Formation, Narrama Formation, Brevelon Tank Quartzite.|Intruded by Tarcoon Plutonic Complex.|Metamorphosed turbidites, Bouma A,C sequences, deep marine environment; interbedded sandstone, siltstone, claystone, some chert horizons and a minor occurrence of mafic volcanic rocks; subgreenschist facies to localised amphibolite facies.|
27158|Girilambone Group|70684|6|Mentioned|p7 Fig.1, p54|Ordovician|Ordovician|||||||
27158|Girilambone Group|70718|5|Briefly described|p44|Late Ordovician|Early Ordovician|Wagga-Omeo Zone, Murray Basin.|||||Micaceous, quartzose and quartz-lithic sandstone, pelite and chert with minor intercalations of polymictic conglomerate, siltstone, quartzite and mafic-intermediate volcanics.|
27158|Girilambone Group|70744|6|Mentioned|p944-945|Middle Ordovician|Early Ordovician|Detrital zircon age distribution graph.||||||
27158|Girilambone Group|70751|4|Described|p4-p6, p12, p15, p25-p28|Ordovician|Ordovician|Age is poorly constrained in the study area though early to late Ordovician conodonts have been identified elsewhere. Deformed in the early Silurian by the Benambran Orogeny. Rocks corresponding to this group have a magnetic high. Numerical ages are Ar/Ar dates of muscovite derived from Fergusson et al, 2005.|435.2 +/- 2.6 Ma and 440.2 +/- 2.6 Ma||Includes the Break O'Day Amphibolite and Alandoon Chert.|Overlain by the Cobar Supergroup.|Turbiditic sedimentary rocks.|
27158|Girilambone Group|70821|5|Briefly described|p9,p11-12, p15, p28, p70, p109-110, p118|Middle Ordovician|Early Ordovician|Polyphase-deformed metasedimentary rocks and granite intrusions. Forms basement to south-eastern Thomson Orogen. Is exposed in the Gongolgon area. Electrical conductivity depends on the amount of pyrite and carbon contained in the rocks.|||Ballast Formation.||Metamorphosed turbidite sequences, subordinate meta-cherts, and minor mafic volcanic (and possibly intrusive) rocks.|
27158|Girilambone Group|70828|5|Briefly described|p2,4-8,10,14-15,17|Ordovician|Ordovician|Deformed by Late Ordovician to Early Silurian Benambran Orogeny (Burton et al., 2012). In contact with Erimeran Granite. Limited evidence of mid-ocean ridge type crust within Girilambone Group (Burton 2011, 2014, in prep).|||Includes Narrama Formation and the Break O'Day Amphibolite.|Intruded by Break O'Day Amphibolite.|Deep marine turbidites; pelitic to psammitic metasediments, minor chert.|11-DEC-19
27158|Girilambone Group|70941|3|Fully described|pviii-pxii, p4, p6|Middle Ordovician|Early Ordovician|Generally very poorly outcropping.  Named after the township of Girilambone. Previously referred to as the Girilambone Series. Forms the Bedrock of most of the Byrock and Sussex map area. Generally forms low rounded hills with scattered outcrop. Thickness estimated to be at least several kilometres based on thicknesses in other map sheets. Deposited in deep to very deep marine environment as turbidites or pelagic sediments.Distinguishing features, Structure, metamorphism, geochemistry, geophysical characteristics and fossil assemblage discussed. No type section discussed or given. Siltstones are difficult to distinguish from those of the Meryula Formation. Hosts the Wilga Downs disseminated and massive sulfide prospect close to the Meryula Formation. See also  p7 fig 3, p8 fig 4, p11 fig 6, p12-p16, p21, p64 fig 29, p76, p80, p80 fig 33, p81-p94, p97, p112, p113, p122, p126-p129, p131, p133, p135, p136, p137, p139, p140 fig 58, p143-145.|||Narrama, Lang, Ballast Formations|Unconformably overlain by the Coronga Peak Quartzite, Drouin Conglomerate Member, Kopyje Group. Tentatively correlated with the Wagga Group (and thus the Omeo Metamorphic Complex)|Micaceous and quartzose sandstone, siltstone and claystone turbidite deposits. Associated chert horizons and mafic volcanic rocks also occur. Slates, phyllites and schists also occur throughout this group. Quartz veins occur throughout this group.|
27158|Girilambone Group|70950|6|Mentioned|p1028-1029, 1044|Late Ordovician|Early Ordovician|Geological province: Central Lachlan Orogen. Turbiditic sedimentary rocks that form basement to the Lachlan Orogen. Includes Early to Late Ordovician conodonts in various areas.||||||
27158|Girilambone Group|71039|6|Mentioned|p4, p6, p27-p28|Ordovician|Ordovician|||||||09-MAR-23
27158|Girilambone Group|71069|6|Mentioned|p52, p58, p59|||Central Lachlan Orogen.||||Equivalent to the Adaminaby Group.||
27158|Girilambone Group|71285|5|Briefly described|p538-539, p549-551, p552|Middle Ordovician|Early Ordovician|Cobar region. Probable basement to the Cobar Basin. Origins and details of sulfur isotopes discussed. Subject to mid-greenschist facies metamorphism.|||||Fine- to coarse-grained turbiditic and pelagic sedimentary rocks with minor mafic volcanic/intrusive rocks.|
27158|Girilambone Group|71345|5|Briefly described|p6,10,22-23|Ordovician|Ordovician|Metasedimentary unit.||||Intruded by Sainsbury Park Granite, Glenariff Granite, Wilgaroon Granite, Galambo Granite.||
27158|Girilambone Group|71360|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Geophysical signature: broad areas of low magnetic intensity; rare discontinuous linear  trends with slightly elevated magnetic intensity occur parallel to regional foliation directions. Some lithologies (chert, sericite schist, quartzite) are mapped separately.|||Narrama, Ballast, Lang Formations.||Quartzite, ironstone, phyllite, sericite schist and talc schist, fine- to coarse-grained quartzose and quartz-lithic sandstone, siltstone, claystone and chert; minor basalt, dolerite, trachyte. Variably metamorphosed.|
27158|Girilambone Group|71693|5|Briefly described|Map legend; p2.|Ordovician|Ordovician|Turbiditic sedimentary sequence. Lower parts are associated with Besshi-style Cu-Zn(-Au) VAMS mineralisation.|||Includes Narrama, Murda, Lang, Ballast Formations.|Is intruded by Fifield Suite. Lateral equivalent of Clements Formation (Wagga Group).|Deformed and metamorphosed, micaceous, quartzose and quartz-lithic sandstone, metamudstone, chert; minor intercalations of polymictic conglomerate, siltstone, quartzite, and mafic and intermediate volcanic rocks.|13-SEP-19
27158|Girilambone Group|71700|5|Briefly described|p8, CD|Chewtonian|Bendigonian|Age derived from conodont faunas.|||Includes the Ballast Formation and Lang Formation.|||
27158|Girilambone Group|71860|6|Mentioned|p6|Ordovician|Ordovician|||||||
27158|Girilambone Group|71965|5|Briefly described|p894,896,902,904,912-913|Floian|Tremadocian|Geological province: Lachlan Orogen. Metamorphosed to greenschist or locally amphibolite facies (Burton et al., Campbell, 2012; Fraser et al., 2014).||||Overlain by Mulga Downs Group and Cobar Supergroup.|Deep marine turbidites, pelagic sediments and minor mafic rocks.|
27158|Girilambone Group|72080|4|Described|p2, p4-p10, p12-p14, p19|Ordovician|Ordovician|Gilligan et al (1994) assigned rocks in the Harts Tank area to this group and the now defunct Harts Tank beds.The oldest package of rocks in the Cobar district; interpreted to have been deposited in a deep marine setting as a turbidite. Deformed during the Benambran Orogeny dated between 440 and 435 Ma using Ar/Ar (Fergusson et al, 2005). Referred to as the Girilambone Beds on p7.|||Includes the Alandoon Chert, Ballast Formation, Narrama Formation, Lang Formation and the Whinfell Chert.|Overlain by the Cobar Supergroup. Intruded by the Erimeran Granite.|Metamorphosed, fine to medium-grained sandstone, siltstone and claystone with lesser chert and altered mafic volcanic rocks.|07-JAN-22
27158|Girilambone Group|72296|3|Fully described|ix-x, p2, p5-10, p13,p16, p20-21, p24-26|Middle Ordovician|Early Ordovician|See also p28, p31, p34, p37-38, p49, p53, p57-61, p68, p78, p81. Rayner (1961, 1969) after Andrews (1915). See p6 for the complicated evolution of the unit's name and constituents. Thickness estimated at several kilometres. Turbidites and pelagic sediments. Deformed (not strongly) 434 +/- 3.5 Ma (i.e. during the Benambran Orogeny); usually two or more cleavages. Constitutes bedrock over a large area of central northern NSW. Abundant quartz veins: quartz vein float is ubiquitous. Lithology, geophysical characteristics described in detail. Hosts VAMS mineralisation (banded pyrite +/- chalcopyrite deposits). Conodont species listed. RELATED UNITS (continued): Is faulted against the Doradilla Formation. Correlated with the Wagga Group.|||Narrama, Lang Formations.|Is overlain unconformably by the Kopyje Group. Is intruded by Midway Granite and presumably (no contacts observed) by Bobelah Granite and Mullagallah Quartz Diorite. See COMMENTS for more.|Brown to tan, interbedded micaceous and quartzose (locally feldspathic), very fine- to medium-grained metasandstone, metasiltstone and metaclaystone (phyllite, schist and slate); as well as chert, minor mafic volcanic rocks and rare ultramafic rocks.|
27158|Girilambone Group|72495|5|Briefly described|p217-218, p233-p235|Ordovician|Ordovician|Coincides with a north-western gravity high in the Junee-Narromine volcanic belt.|||||Quartz rich turbidites.|
27158|Girilambone Group|72522|6|Mentioned|p18.|Ordovician|Ordovician|Northern Lachlan Orogen. Younger parts of this Group may be equivalent to the Booda Formation.||||||
27158|Girilambone Group|72908|5|Briefly described|p3-5, p6-7 Tb.1, p9, p11, p24-25, p31|Ordovician|Ordovician|Lachlan Orogen, central. Age is poorly constrained in the study area. Deposited in marine conditions. Hosts the Blind Calf, Condobolin and Melrose deposits. See also p29.|||Lang Formation, Narrama Formation||Turbiditic sedimentary rocks with minor mafic units, deformed and metamorphosed.|
27158|Girilambone Group|72958|6|Mentioned|p5-7, p45-50, p57, p61|Ordovician|Ordovician|Underlies the eastern shelf sequences of the Cobar Basin. Unnamed tonalitic pluton intruding this group returned a SHRIMP U-Pb magmatic age of 424.9 +/- 2.0 Ma. Hosts 413.0 +/- 3.2 Ma rhyolitic dykes, which is comparable in age to the unnamed hornblende-phyric dacite sill, hosted within the Meryula Formation.|||Includes Ballast Formation.|Underlies Kopyje Group.||
27158|Girilambone Group|73059|5|Briefly described|p1060-1061|||Detrital zircon age plots.|||||Turbidites. Includes quartzites and quartzose sandstones.|
27158|Girilambone Group|73140|5|Briefly described|p495|Gisbornian|Late Cambrian|Proposed to be incorporated into a new Lachlan Supergroup.||Lachlan Supergroup|||Terrigenous turbiditic sequence.|
27158|Girilambone Group|73143|6|Mentioned|p2|Ordovician|Ordovician|||||||
27158|Girilambone Group|73154|6|Mentioned|p77 Fig.3|Middle Ordovician|Early Ordovician|||||||
27158|Girilambone Group|73174|6|Mentioned|p1035-1037, p1046|Ordovician|Ordovician|Lachlan Orogen[?].||||Overlain by Mount Boppy Conglomerate (Baledmund Formation, Kopyje Group).|Includes turbidites.|
27158|Girilambone Group|73175|6|Mentioned|p1051, p1059, p1063 Fig.10, p1064 Fig.11|Middle Ordovician|Early Ordovician|Lachlan Orogen.|||Narrama Formation|||
27158|Girilambone Group|73177|5|Briefly described|p1097, 1112-1114, 1115 Fig.17, 1118|Early Ordovician|Early Ordovician|Lachlan Orogen.|||Narrama Formation.|Possibly equivalent to Thomson beds.||
27158|Girilambone Group|73264|5|Briefly described|p1390 Fig.12, p1394|Middle Ordovician|Middle Ordovician|Lachlan Orogen, Hermidale Terrane. Age described as late Middle Ordovician.|||Ballast Formation, Narrama Formation.||Includes turbidites, sandstones.|
27158|Girilambone Group|73578|5|Briefly described|p1, p28, p39, p43, p50|Ordovician|Ordovician|||||Intruded by Wild Wave Granodiorite.||
82457|Gleamwoods Monzogranite|71628|5|Briefly described|p12: 1, 8-10, 17; p15: 33, 52|||New name, after a local homestead. Occurs 5 km NE of Eukey and ~12 km SW of Stanthorpe. The outcrop area is ca. 3 x 2 km and is deeply weathered and poorly exposed. Very limited geochemistry detailed; similar to Storm King Monzogranite.||Gleamwoods Suite.||Is entirely enclosed by the younger Jenners Monzogranite (Stanthorpe Complex).|Pale pinkish-grey, fine- to medium-grained, highly porphyritic monzogranite; locally, flow alignment of phenocrysts and granophyric groundmass; mafic inclusions are common. I-type.|
82458|Gleamwoods Suite|71628|5|Briefly described|p12: 8, 15|||New name. Assignation is tentative.||Sailor Jack Supersuite.|Gleamwoods, Storm King Monzogranites.|||
24286|Gleesons Limestone Member|5250|5|Briefly described|p42, p45, ||Early Caradoc|Member of  Fossil Hill Limestone. Includes brachiopod fauna.||||||16-JAN-12
24286|Gleesons Limestone Member|23214|3|Fully described|p41|Eastonian|Eastonian|Of Fossil Hill Limestone. 20m thick at type section. Overlying unit: Kalimna Limestone Member.||||||
24286|Gleesons Limestone Member|38219|2|Defined|p306|Late Ordovician|Late Ordovician|Part of Cliefden Caves Group. See also Fig.2.||||||
24286|Gleesons Limestone Member|41046|6|Mentioned|Fig.2|||||||||
24286|Gleesons Limestone Member|41508|6|Mentioned|p576|||||||||
24286|Gleesons Limestone Member|42479|5|Briefly described|p108|||||||||
24286|Gleesons Limestone Member|42603|5|Briefly described|Fig.4 P57|||||||||
24286|Gleesons Limestone Member|43571|5|Briefly described|p821|||||||||
24286|Gleesons Limestone Member|70754|5|Briefly described|p449, p455|Late Ordovician|Late Ordovician|Lingulides, probably infaunal, are occasionally preserved on bedding planes.||Fossil Hill Limestone.|||Includes thin-bedded terrigenous-rich limestones.|
40761|Glen Allyn Ignimbrite Member|50613|2|Defined|p213, p231 App. 1|Namurian|Namurian|Of the Willuri Formation.  Volcanic member of the Gunnan package (informal grouping of stratigraphically recognisable distinctive, mappable units). Overlies Taggarts Mountain Ignimbrite.  Max. thickness: 35m. Geol.Prov: New England Orogen.  See also p210||||||22-FEB-05
70279|Glen Bell Formation|65398|2|Defined|p1-22|Early Silurian|Late Ordovician|New name: of Brown (2009). Previously part of Woolomin Group; subsequently Wisemans Arm Formation. Type section 1700 m NNW of Glen Bell Homestead. Limestone, limestone breccia, limestone conglomerate and laminated calcareous sandstone, fine-grained laminated buff feldspathic or feldspatholithic sandstone, fine- to medium-grained porphyritic andesite and basalt. Intimately associated with Woodsreef Melange.  Formerly regarded as olistoliths in the Wisemans Arm Formation. Thickness to 50m. Fossil fauna listed. All boundaries are fault surfaces; interpreted as a discrete terrane (the Dunmore terrane).||||||
70279|Glen Bell Formation|66720|5|Briefly described|Map legend|Early Silurian|Late Ordovician||||Three un-named members are mapped separately: thinly bedded and laminated buff siltstone; limestones, massive micritic and rare fossiliferous, -breccia and -conglomerate; massive andesite and basalt.||Undifferentiated sandstone, argillite, limestone and mafic volcanic rocks.|15-NOV-13
70279|Glen Bell Formation|67322|5|Briefly described|Fig.5; p27-28, p39-40|Wenlock|Eastonian|Redefined. Originally of Brown (2009), who assigned to this unit rocks interpreted as olistoliths of limestones and laminated fine-grained feldspathic sandstones of the Wisemans Arm Formation; also included the 'Uralba Beds' of Hall (1975). Allochthonous limestone blocks within the Glen Bell Formation contain macro- and microfaunas of two distinct ages: Late Ordovician and Early Silurian (Llandovery to early Wenlock). Corals and conodonts (Eastonian) are evidence for the Late Ordovician age. Occurs in the Tamworth-Neminha region, New England Orogen.||||||21-FEB-18
70279|Glen Bell Formation|71091|6|Mentioned|p147|||Vickery et al. (2010). Includes the former "Uralba beds".||||||
28309|Glen Bower Formation|13996|6|Mentioned|p143|Silurian|Silurian|Taemas-Cavan area. Hosts two undescribed nautiloid species (named).||||||
28309|Glen Bower Formation|22486|6|Mentioned|p 6|||||||||
28309|Glen Bower Formation|22857|4|Described|p460 App.1 Tb.A1.6|Silurian|Silurian|Limestone, sandstone, siltstone, shale, mudstone; contains corals. Max. thickness:>1.1km. Geological Province: Canberra-Yass Shelf.||||||24-FEB-06
28309|Glen Bower Formation|32675|6|Mentioned|p8|||Strat. nomenclature||||||
28309|Glen Bower Formation|35070|6|Mentioned|p78|||||||||
28309|Glen Bower Formation|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
28309|Glen Bower Formation|35386|3|Fully described|p20|||||||||
28309|Glen Bower Formation|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
28309|Glen Bower Formation|36441|5|Briefly described|map legend|Ludlovian|Ludlovian|Interbedded limestone, sandstone and red shale, minor conglomerate. Unconformably underlies Laidlaw Volcanics; overlies Hawkins Volcanics. BMR map code: Sug.||||||
28309|Glen Bower Formation|40328|3|Fully described|p92|||||||||
28309|Glen Bower Formation|40689|3|Fully described|p18|||||||||
28309|Glen Bower Formation|45147|2|Defined|M119|early Ludlovian|early Ludlovian|Earliest Ludlovian||||||
28309|Glen Bower Formation|68592|2|Defined|p428, p431, p433-4, p436, p440, p472-92|Wenlock|Wenlock|See also p1875. Originally Glenbower Formation (Shearsby, 1905); later Glen Bower Beds (Fig.13) or Series (accompanying text) of Harper (1909). This became Glen Bower Beds within Douro Series of Best et al. (1964), renamed as Glen Bower Member of Douro Volcanics by Brunker and Offenberg (1970) and Offenberg (1974). Pogson and Baker (1974) published the Glen Bower Formation and Boambolo Formation, and Cramsie et al. (1978) published the three Members (Wyelba, Copplestone and Connell). Owen and Wyborn (1979) reverted to the single unit style of Brunker and Offenberg, but Feary (1984, 1986) "introduced considerable confusion" with his Ravenswood Subgroup containing the Glen Bower Formation and four others. That system is here rejected and the system used by Cramsie et al. is restored. Type and representative sections are described. Diverse fauna described.||Unit in Douro Group.|Includes Connell, Copplestone and Wyelba Members.|Conformably overlies Hawkins Volcanics. Equivalent to Yass Formation. Is overlain by Boambolo Formation. Is overlain unconformably by Laidlaw Volcanics.|Basal sandstones and mudstones, overlain by interbedded algal limestones and mudstones, followed by mudstones with very fine-grained sandstones and interbedded carbonates.|
28309|Glen Bower Formation|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdg[3 asterisks]. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Douro Group|Includes Connell Member, Copplestone Member, Wyelba Member.|Is overlain by Boambolo Formation. Overlies Hawkins Volcanics.|Laminated, tuffaceous mudstone; thinly bedded, interbedded quartz lithic sandstone and mudstone; coarse grained cross stratified-planar laminated quartzose sandstone. Algal and biohermal limestone, mudstone with carbonate nodules and lenses.|
28309|Glen Bower Formation|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|Includes Connell Member, Copplestone Member, Wyelba Member.||Laminated, tuffaceous mudstone; thinly bedded, interbedded quartz lithic sandstone and mudstone; coarse grained cross stratified-planar laminated quartzose sandstone. Algal and biohermal limestone, mudstone with carbonate nodules and lenses.|
28309|Glen Bower Formation|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|Includes Connell Member, Copplestone Member, Wyelba Member||Laminated, tuffaceous mudstone; thinly bedded, interbedded quartz lithic sandstone and mudstone. Coarse grained, cross stratified to planar laminated quartzose sandstone; algal and biohermal limestone, mudstone with carbonate nodules and lenses.|
28309|Glen Bower Formation|71656|5|Briefly described|p12 Fig.2, p22|Wenlock|Wenlock|Includes rugose and tabulate corals along with brachiopods, nautiloids and conodonts. Compared with Hattons Corner Assemblage.||Douro Group|Includes Connell Member?|Partially equivalent to Goobarragandra Volcanics, Hawkins Volcanics.|Fossiliferous strata.|
28309|Glen Bower Formation|73215|5|Briefly described|p993-994, 1002|||Yass Syncline.||Douro Group||Overlies Hawkins Volcanics. Is overlain by Laidlaw Volcanics.||
24610|Glen Davis Formation|22578|6|Mentioned|p398|||||||||
24610|Glen Davis Formation|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wallerawang Subgroup (Illawarra Coal Measures). Claystone, siltstone; minor coal, carbonaceous claystone; oil shale. Max. thickness: 14m. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
24610|Glen Davis Formation|39232|4|Described|p109|||||||||
24610|Glen Davis Formation|40256|6|Mentioned|Fig.3|||||||||
24610|Glen Davis Formation|40332|6|Mentioned|p21|||||||||
24610|Glen Davis Formation|40806|2|Defined|p155|Permian|Permian|Prob. Permian||||||
24610|Glen Davis Formation|42657|4|Described|p80|||||||||
24610|Glen Davis Formation|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
24610|Glen Davis Formation|68004|4|Described|p60 Table 6, p61.|Late Permian|Late Permian|Western Coalfield. From 17 to 26 m thick. In the far west, the two Coal Members coalesce to form a seam up to 13.6 m thick NW of Ulan.||Unit in Charbon Subgroup.|Includes Cockabutta Creek Sandstone Member and Bungaba Coal Member.|Overlies Newnes Formation. Is overlain by Denman Formation and Moolarben Coal Member.|Coal, carbonaceous claystone, claystone and siltstone and sandstone.|
74801|Glen Eden Granite|61804|5|Briefly described|p419-423, p424 Fig. 2, p425 Fig. 4|Early Triassic|Early Triassic|Age: 240+/-1Ma (Ar-Ar). Geological Province: New England Fold Belt. Porphyritic microleucogranite.||||||
74801|Glen Eden Granite|71628|6|Mentioned|p15:28|||Somarin and Ashley (1999). Renamed Glen Eden Microleucogranite in this study.||||||
82750|Glen Eden Microleucogranite|71628|4|Described|p15: 2-3, 28-31|||New name (this study); previously Glen Eden Granite of Somarin and Ashley (1999). Named after a molybdenum deposit of that name or a local homestead. No surface exposure; forms a series of dykes over 80m depth. This c.270 Ma date of molybdenite is likely too old. Geochemistry described. Is spatially associated with stockwork and vein Mo-Bi-W-Sn mineralisation.|270-265 Ma (Re-Os; Norman et al., 2004).|Glen Eden Suite.||Intrudes Emmaville Volcanics.|Three phases of intrusion are detailed: fine- to very fine-grained, biotite microgranite porphyry, micrographic granite, and aplite.|
80453|Glen Emu granite|70718|5|Briefly described|p65,66|||Informal name, interpreted from geophysics. Referred to as the Glen Emu granodiorite on p65 fig 35. Subsurface Balranald 1:250 000 sheet area.||Glen Emu granite suite|||Interpreted as granite or granodiorite.|31-MAY-19
80442|Glen Emu granite suite|70718|5|Briefly described|p3, p65-p67, p71, 82, 94, p121|Silurian|Silurian|Situated in a region that was previously interpreted as sedimentary troughs (Sniffin 1985) (along the Balranald and Booligal troughs). The Glen Emu granite suite is interpreted as stitching plutons in a suture zone between the Hay¿Booligal and Stawell zones. Informal name, derived from geophysics. Geophysical characteristics are discussed in some detail.|||Includes the Glen Emu granite, the Merritop granite, Cringadale granite and the Rata granite.||Interpreted as granites or granodiorites.|31-MAY-19
77012|Glen Esk Monzogranite|71628|4|Described|p17: 2, 54, 56-64, 89|||Initially the Glen Esk Adamellite of Leitch et al. (1982). Name altered to align with IUGS nomenclature. May be named after Glen Esk Road. Occurs ~40 km NW of Port Macquarie as a ~8 x 9 km intrusion. Has good outcrops, sometimes as pavements, in heavily forested areas. Geochemistry described. Is associated with limited Sn mineralisation (prospects named).|221.2 +/- 1.5 Ma (SHRIMP: Cross and Blevin, 2013).|Glen Esk Suite.||Intrudes Boonanghi beds.|Pinkish, medium coarse-grained, porphyritic monzogranite and leucogranite, granodiorite enclave variant and microleucogranite marginal facies. I-type.|
74017|Glen Esk Suite|71628|5|Briefly described|p17: 58, 62, 88|||||Glen Esk Supersuite.|Glen Esk, Gundle Monzogranites.|||
82460|Glen Esk Supersuite|71628|5|Briefly described|p17: 1-2, 27, 54-70, 72, 88|||New unit, incorporating some intrusions of the Coastal Granite Association. Emplaced over a period just under 10 m.y. Geochemistry summarised.||Coastal Granite Association.|Cairncross, Glen Esk, Tallawudjah Suites.||Dominated by white to pink, biotite-hornblende monzogranite to biotite leucomonzogranite, with lesser biotite-hornblende leucosyenogranite, and granodiorite; texturally heterogeneous. Borderline I-A-type.|
27417|Glen Gallic Subgroup|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wollombi Coal Measures (Singleton Supergroup). Max. thickness: 55m. Geological Province: Sydney Basin.||||||
27417|Glen Gallic Subgroup|22969|4|Described|Fig 4.1a||Late Permian|Wollombi Coal Measures||||||
27417|Glen Gallic Subgroup|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures. Geological Province: Sydney Basin||||||
27417|Glen Gallic Subgroup|41010|6|Mentioned|Table 1|||||||||
27417|Glen Gallic Subgroup|42078|6|Mentioned|Table 1 P5|||||||||
27417|Glen Gallic Subgroup|42916|5|Briefly described|Table 1||Late Permian|||||||
27417|Glen Gallic Subgroup|43257|5|Briefly described|Map Legend||Late Permian|Of Wollombi Coal Measures||||||
27417|Glen Gallic Subgroup|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wollombi Newcastle Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
82461|Glen Garry Microleucosyenogranite|71628|5|Briefly described|p11:16; p14: 1-8|||Originally Glen Garry Granite of Flinter et al. (1972); later Glen Garry Microleucogranite (Willis, 1987). Renamed here to reflect more accurately the composition of the intrusion. Name derived from a local homestead. Comprises numerous (at least 10 mapped) small bodies. Varies locally from highly resistant to highly susceptible to weathering. Geochemistry described. Has Mo (Bi) and Ag mineralisation.||Kingsgate Supersuite.||Intrudes Mount Mitchell Monzogranite, Coffs Harbour Association, Wandsworth Volcanic Group, and ?Kingsgate Syenogranite. Partly encloses Kingsgate Syenogranite.|Pinkish, fine- to medium-grained, equigranular (saccharoidal) leucosyenogranite and rarer leucomonzogranite. I-type.|
40559|Glen Idle Rhyolite Member|24605|3|Fully described|p931, p933 Fig.2, p939|Namurian|Namurian|Of the Clifden Formation. Overlain by the Peri Rhyolite Member. Geological Province: New England Orogen. Defined as Glen Idle Rhyolite.||||||
40559|Glen Idle Rhyolite Member|61214|5|Briefly described|p170, p171 Fig. 1|Carboniferous|Carboniferous|Of the Clifden Formation. Underlies the Peri Rhyolite Member/"Eastons Arm Rhyolite Member" horizon in the Clifden Formation at a single location in the north only. ||||||
38313|Glen Road seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
37292|Glen Ward beds|24008|6|Mentioned|p355|Late Silurian|Late Silurian|||||||
37292|Glen Ward beds|69601|6|Mentioned|p405|||||||Locally is overlain unconformably by Pitch Creek Volcanics.||
80152|Glenara Coal Member|70791|5|Briefly described|p285, p293 Fig.17|Permian|Permian|Werris Creek area. Has similarities with Bibblewindi Coal Member (Mullaley Sub-basin).||Skeletar Formation.||||
78509|Glenariff Granite|68823|6|Mentioned|p376 Fig.3, p377, p378 Fig.4|Pridoli|Pridoli||ca. 422 Ma|||||
78509|Glenariff Granite|69541|5|Briefly described|p645 Fig.1(b)|Late Silurian|Late Silurian|Lachlan Orogen.|422 Ma.|||||
78509|Glenariff Granite|70602|6|Mentioned|p67 Fig 3,72|Silurian|Silurian|Age inferred from  map symbol. Aeromagnetic map data given. Grouped with Galambo Granite, Mount Oxley Granite, Knightvale Granite and 3 informal units: Rosses Tank Unit, Brevelon Unit, Mulgawarrina Unit.||||||
78509|Glenariff Granite|71345|2|Defined|p4,22-24|Late Silurian|Late Silurian|Type location: Lat: -30.7267 Long: 146.5839 (GR 460165 6600615), the collar location for drill hole Glenariff DDH1. Named for the Glenariff homestead and station; the homestead is approximately 2.5km south of the southern margin of the granite. First mapped by Byrnes (1993), defined herein after Blevin (2011). Exposed in a few locations and intersected in drill hole Glenariff DDH1 (Blevin 2011); from magnetic data, DDH1 was drilled in a SE-trending 'tadpole'-shaped anomaly 45km long. Fractionated I-type granite (Blevin 2011). Black (2007) reported a SHRIMP U-Pb magmatic crystallisation age of 422.7+\-2.4 Ma. Anomalous Cu, Pb, Zn, Ag, Sn and W were reported from the Lindsay Park prospect (Byrnes 1993, Blevin 2011), which is on the southern margin of the granite at GR474205 6595205. Blevin (2011) considered the granite to have high metallogenic potential for Au-Bi-W-Mo. Poorly known due to the lack of exposure and lack of exploration drilling, despite its high metallogenic potential (Blevin 2011).|422.7+\-2.4 Ma (SHIRMP U-Pb; magmatic)|||Intrudes into Girilambone Group.|Pink, medium to coarse grained, quartz, biotite, alkali-feldspar granite, includes fluorite, zircon, apatite and opaques; sparse miarolitic cavities, though microgranite zones have well developed interconnected miarolitic textures.|02-DEC-19
78509|Glenariff Granite|71360|5|Briefly described|Map legend|Late Silurian|Late Silurian|Geophysical signature: elongate zone of moderate to high magnetic intensity which typically shows sharp contacts with metasedimentary rocks of low magnetic intensity; numerous dyke swarms and magnetite-depleted fractures transect the pluton. Some areas show muted and varied magnetic character which suggests partial unroofing. Sparse exposures of granite have high radioelement counts. Interpreted to occur also in the Mulgawarrina area.|422.7 +/- 2.4 Ma.||||Pink alkali feldspar granite with biotite; miarolitic upper margin; leucocratic biotite quartz monzonite reported.|
78509|Glenariff Granite|72296|6|Mentioned|p42|||||||||
78509|Glenariff Granite|72522|5|Briefly described|p8, p10.|Lochkovian|Silurian|Magmatic age by Black, 2007. Age indistinguishable from nearby dated granodiorite at Glen Idol prospect (421.9+/-3.5 Ma) and Brewarrina Granite (420.9+/-2.3 Ma).|422.7 +/- 2.4 Ma|||||
78509|Glenariff Granite|72951|5|Briefly described|p1013, 1017, 1022|Pridoli|Ludlow|Lachlan Orogen. Hermidale Terrane. I-type. SHRIMP U-Pb zircon isotope analyses from Black (2007). eHf = -0.2 +/- 1.5, and d18O = 6.33 +/- 0.32.|422.6 +/- 2.4 Ma||||Coarse-grained syenogranite.|
25013|Glenbog Granodiorite|22815|4|Described|p76|||||||||
25013|Glenbog Granodiorite|41133|6|Mentioned|p1124|||||||||
25013|Glenbog Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Glenbog Suite.||||||
25013|Glenbog Granodiorite|62070|5|Briefly described|p40,|Lochkovian|Lochkovian|Of Bega Batholith. SHRIMP U/Pb zircon ages.|412+/-3 Ma ,414+/- Ma U/Pb SHRIMP.|||||
25013|Glenbog Granodiorite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|Chappell et al. (1987). The type pluton for Glenbog Supersuite. Located E of Nimmitabel.||||||
25013|Glenbog Granodiorite|69270|5|Briefly described|p1, p15|Early Devonian|Early Devonian|Ages from zircons in mafic inclusions in Glenbog Granodiorite (Chen et al, 1990) are indistinguishable from new age of Anembo Granodiorite. Name presented once in text (p15) as Glenbog Granite (probably misspelt).|412+/-3 Ma and 412+/-2 Ma, zircons, U-Pb SHRIMP|||||
25013|Glenbog Granodiorite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. I-type. Hf and O18 isotope data included.|414 Ma|||||
41059|Glenburnie Leucomonzogranite|24366|6|Mentioned|p18 Fig. 11|||||||||
41059|Glenburnie Leucomonzogranite|69639|5|Briefly described|p1, p217|Cisuralian|Cisuralian|New England Orogen. An additional date of 297.7 +/- 2.9 Ma is derived from Jeon, 2012.|295.2 +/- 2.3 ( Black, 2007)|||||
41059|Glenburnie Leucomonzogranite|71628|4|Described|p1:6; p7-40; p8: 61, 67, 72, 77; p19: 2|||See also p19: 4, 54-57. Brown (2003) after Chappell and Bryant (2002[?], unpublished). Previously the Glenburnie Leucoadamellite of Binns et al. (1967) after work by Flood, and later Glenburnie Leucogranite (Green and Kridoharto, 1975). Southern New England Orogen. Named after a local homestead. Crops out along the New England Highway, 15 km SW of Uralla, as small rounded tors or blocky rubble. Comprises ?2 masses (discussed). Is interspersed with S-type granites. Lithology, mineralogy and geochemistry described in some detail.|297.7 +/- 2.9 Ma (SHRIMP; Jeon, 2012).|Glenburnie Suite.||Intrudes Sandon beds. Is intruded by Walcha Road Monzogranite; Manuka Farm and Terrible Vale, Porphyritic Microgranodiorites; Uralla Granodiorite; and Wilhelmshohe Tonalite.|Grey-blue to pale grey to buff, medium- to coarse-grained, equigranular to slightly porphyritic biotite-hornblende monzogranite and biotite leucomonzogranite. I-type.|
70280|Glencairn Formation|66720|5|Briefly described|Map legend|Late Devonian|Early Devonian|||Unit in Tamworth Group.|An un-named member, mapped separately, has dark grey micritic limestone and limestone with granule- to pebble-sized angular metasedimentary and volcanic clasts.||Volcaniclastic conglomerate, cross-bedded sandstone and minor siltstone with major limestone lenses.|
67900|Glenclair Suite|68005|5|Briefly described|p136.|Permian|Permian|||Unit in Bundarra Supersuite.|Includes Glenclair Monzogranite.|||
67900|Glenclair Suite|71628|5|Briefly described|p4: 3, 24-25, 29-30, 48, 55|||Bryant et al. (2001?). Named after a local homestead.||Bundarra Supersuite.|Giants Den Leucosyenogranite, Glenclair Syenogranite.|||
82451|Glenclair Syenogranite|71628|4|Described|p4: 1, 4-5, 7-9, 13, 23-33, 37,42,44-46|||See also p4: 50, 55. Southern New England Orogen. Named after a local homestead. Crops out ~12 km NW of Bendemeer; coincides with an almost circular mountain. Almost indistinguishable geochemically from Giants Den Leucosyenogranite; complicated (mapping) history outlined. Lithology described in detail.|288 Ma (U-Pb ion probe: Kemp et al., 2009).|Glenclair Suite.||Abuts Banalasta and Pringles Monzogranites, and Giants Den Leucosyenogranite (nature of all boundaries uncertain).|Medium- to coarse-grained, porphyritic biotite-muscovite (+/- cordierite, +/- garnet) syenogranite to leucosyenogranite with lesser monzogranite-leucomonzogranite.|
30043|Glendale Limestone Member|22857|5|Briefly described|p474 App.1 Tb.A1.6|Emsian|Pragian|Of the Carwell Creek Formation (Kandos Group). Limestone, dolomitic limestone and dolomite; rare conglomerre beds. Geological Province: Capertee Rise.||||||
30043|Glendale Limestone Member|23043|5|Briefly described|Map Legend|Emsian|Emsian|of Carwell Creek Formation, Kandos Group.||||||
30043|Glendale Limestone Member|23522|5|Briefly described|p248 Fig 4|Emsian|Pragian|||||||
30043|Glendale Limestone Member|43188|4|Described|p211,Table 3 p208|||Basal member of Carwell Creek Formation.||||||
30043|Glendale Limestone Member|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cudgegong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
29584|Glendale Quartz Monzonite|13139|5|Briefly described|p3 Fig. 2, p8|Late Ordovician|Late Ordovician|Age: 450-440Ma. Geological Province: Lachlan Orogen.||||||17-JUL-08
29584|Glendale Quartz Monzonite|22679|4|Described|p 37|||||||||
29584|Glendale Quartz Monzonite|23214|3|Fully described|p91|Late Ordovician|Late Ordovician|Originally included as part of the now superseded Prince of Wales Dioirite. Wholly enclosed with in the Tettenhall Monzodiorite.||||||
29584|Glendale Quartz Monzonite|23334|5|Briefly described|3 Fig.2|||||||||
29584|Glendale Quartz Monzonite|24398|6|Mentioned|p267|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
29584|Glendale Quartz Monzonite|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Quartz monzonite.||||||17-JUL-08
29584|Glendale Quartz Monzonite|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Quartz monzonite.||||||17-JUL-08
29584|Glendale Quartz Monzonite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29584|Glendale Quartz Monzonite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
28578|Glengeera Formation|22768|6|Mentioned|p179|||||||||
28578|Glengeera Formation|22857|4|Described|p179, p456 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Toongi Group. Purple sandstone, siltstone and shale, lithic sandstone, rhyolite, limestone. Max. thickness: 600m. Geological Province: Cowra Basin. ||||||
28578|Glengeera Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Toongi Group.||||||
28578|Glengeera Formation|23170|2|Defined|p122|Early Devonian|Early Devonian|of Toongi Group.||||||
28578|Glengeera Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
28578|Glengeera Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
28578|Glengeera Formation|40328|2|Defined|p126|Silurian|Silurian|||||||
28578|Glengeera Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
28578|Glengeera Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Purple sandstone, siltstone and shale.||||||
28578|Glengeera Formation|68003|5|Briefly described|p24 Fig.3-e, p144. |Pridoli|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Trealmont Quartzite.|Quartz sandstone, quartzofeldspathic sandstone, lithic sandstone, siltstone and shale, limestone.|
38201|Glengowan Shale Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Pinegrove Formation.   Geological Province: Sydney Basin||||||
38201|Glengowan Shale Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Pinegrove Formation. Geological Province: Sydney Basin||||||
38201|Glengowan Shale Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield. The rank 'Member' is missing in table 5.||Basal unit in Pinegrove Formation.||Overlies Eyriebower Coal Member. Is overlain by Wylies Flat Coal Member.||
76033|Glenhope granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Baconian Swamp Granite Suite.|||Interpreted S-type granites.|
76033|Glenhope granite|70718|4|Described|p75, p125|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics.||Baconian Swamp granite suite|||S-type granitic rocks.|31-MAY-19
78895|Gleniffer Monzogranite|69639|4|Described|p1, p5, p8, p100-p105, p217, p237|Cisuralian|Cisuralian|New England Orogen. Sample locality, petrography, and geochronology is described. SHRIMP dating supports its association with the Hillgrove Supersuite.|295.5 +/- 1.9 Ma (SHRIMP, magmatic cryst.)|Hillgrove Suite||Intrudes the Moombil Siltstone and the Nambucca beds.|Massive, undeformed, coarse-grained, inequigranular granite.|21-JAN-19
78895|Gleniffer Monzogranite|71628|4|Described|p3: 1, 46-48; p17:13|||Originally Glenifer Adamellite of Leitch et al. (1971). Spelling corrected to Gleniffer Adamellite (after the locality) in Milford (1996); changed again to Gleniffer Monzogranite in Chisholm et al. (2014). Irregularly shaped; crops out ~15 km W of Sawtell and several kms N of Bellingen. Limited geochemistry described.|295.5 +/- 1.9 Ma (Chisholm et al., 2014).|Hillgrove Supersuite.||Intrudes Moombil Sandstone. Is faulted against Buffers Creek Formation, McGraths Hump Metabasalt and Bellingen Slate (possibly intrudes this last).|Medium- to coarse-graned, weakly porphyritic, massive monzogranite and granodiorite. S-type.|
30051|Glenisla Volcanics|24417|2|Defined|P46|Silurian|Silurian|Of Douro Group.  Parts previously included in the Dulladerry Volcanics.  Intruded by Grenfell and Eugowra Granites.  Unconformably overlain by Dulladerry Volcanics; unconformably underlain by Kirribilli Formation.||||||
30051|Glenisla Volcanics|50628|5|Briefly described|Map Legend|Silurian|Silurian|Of the Douro Group. Quartz feldspar acid porphyry.||||||05-JUL-04
30051|Glenisla Volcanics|60009|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Douro Group.||||||13-JUL-04
30051|Glenisla Volcanics|64994|5|Briefly described|p7|Llandovery|Llandovery|Age: 432.2+/-2.8Ma (SHRIMP U-Pb zircon: Lyons et al 2000). Considered to be equivalent of Canowindra Volcanics.||||||07-FEB-11
30051|Glenisla Volcanics|68592|5|Briefly described|p442, p466|||SHRIMP U-Pb zircon age.|432 +/- 2.8 Ma; Black in Lyons et al. (2000).|||Stratigraphic equivalent to Hawkins and Canowindra Volcanics.||
34613|Glennie Ridge Granite|22831|4|Described|p 71||Late Devonian|previously included in Obley Granite as Glennie Ridge Granophyre.||||||
67908|Glenore Monzogranite|68111|5|Briefly described|p968 Tb.1|Anisian|Induan||250 - 247 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
67908|Glenore Monzogranite|71628|4|Described|p8: 3, 19, 22-25, 34-35|||Li et al. (2012); DMR NAND04 Nandewar Geology Integration and Upgrade Project. Previously Glenore Adamellite of Binns et al. (1967), after unpublished work by Neilson (1970). Named after a local property c.15km W of Guyra. A small (~19.5 km2) ovoid intrusion. Crops out as small rounded boulders. Both age determinations are Rb-Sr (biotite) by Shaw (1994). Geochemistry described.|249.2 Ma and 247.6 Ma.|Mount Duval Suite.||Entirely surrounded and intruded by Mount Duval Monzogranite.|Fine- to medium-grained, weakly porphyritic biotite-hornblende monzogranite; contains abundant leucocratric veins. I-type.|
25925|Glenrae Limestone Member|23214|3|Fully described|p37|Eastonian|Eastonian|Of Daylesford Limestone. 25m thick at type section. Overlain by Davys Plains Limestone. Underlain by Gerybong Limestone Member.||||||13-NOV-08
25925|Glenrae Limestone Member|33063|2|Defined|p81|Ordovician|Ordovician|||||||
25925|Glenrae Limestone Member|33065|6|Mentioned|Table 1|||Lithology.||||||
25925|Glenrae Limestone Member|33740|6|Mentioned|Fig.1|||||||||
25925|Glenrae Limestone Member|38219|6|Mentioned|Table 2|||||||||
25925|Glenrae Limestone Member|40136|6|Mentioned|p23|||||||||
25925|Glenrae Limestone Member|41046|6|Mentioned|Fig.2|||||||||
25925|Glenrae Limestone Member|42479|6|Mentioned|p111|||||||||
25925|Glenrae Limestone Member|70684|5|Briefly described|p39 Fig.17|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Daylesford Limestone.||||
25925|Glenrae Limestone Member|73210|5|Briefly described|p893, p897-898, p903|||Semeniuk (1973, 2011). Exhibits subaerial disconformities and diagenesis/pedogenesis.||Daylesford Limestone.|||Massively calcreted limestone.|14-DEC-22
69449|Glenreach Monzogranite|71628|5|Briefly described|p8: 3, 25-27|||This name is currently (2020) Reserved in the ASUD. Previously Glenreach Adamellite of Chesnut et al. (1973). Crops out as an irregularly shaped, ~11km elongate pluton 20km SSE of Tingha. Forms well-exposed small to large tors. Geochemistry very briefly described. Associated with small alluvial tin deposits.||Mount Duval Suite.||Intrudes Wandsworth Volcanics and abuts the Tingha Monzogranite.|Fine- to medium-grained, equigranular hornblende-biotite(-pyroxene) monzogranite; local porphyritic and pegmatitic variants, small aplitic dykes.|
26583|Glenrossal Granite|42726|5|Briefly described|map legend|Early Devonian||Of the Watch Box Suite (Candelo Supersuite).  Not intended as a formal name.||||||09-FEB-05
26583|Glenrossal Granite|71700|5|Briefly described|ix|Early Devonian|Early Devonian|Rocks in the Mayfield-Limekilns area previously identified as belonging to this unit have been remapped as Braidwood Granodiorite.||||||
27783|Glenrowan Intrusives|29698|4|Described|p68|||||||||
27783|Glenrowan Intrusives|33352|6|Mentioned|p177|||||||||
27783|Glenrowan Intrusives|50629|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Surat Basin.||||||
27783|Glenrowan Intrusives|60266|5|Briefly described|p2,  p3 Tb. 1|Early Jurassic|Late Triassic|Alkali dolerite.  Associated with the Garrawilla Volcanics.  Age: 177+/-1.9Ma and 203+/-2Ma (K-Ar).  Geological Province: Surat Basin.||||||08-DEC-04
27783|Glenrowan Intrusives|60267|4|Described|p15, p21, p26|Jurassic|Jurassic|Porphyritic olivine dolerite.  Probably overlain by Pilliga Sandstone (contacts not exposed).  Intrude the Garrawilla Volcanics.  Age: minimum of 148+/-1.6Ma.  Geological Province: Surat Basin.||||||
27783|Glenrowan Intrusives|61776|5|Briefly described|p194 Fig. 3|Jurassic|Jurassic|Geological Province: Surat Basin. Alkali dolerite and micro-syenodiorite.||||||17-SEP-08
27783|Glenrowan Intrusives|68003|5|Briefly described|p48, p51 Photo.3-o, p55 Fig.3-m, p128.|Cretaceous|Late Triassic|Gunnedah Basin. Widespread unit. Often found following seams of Permian coal.||Unit in Garrawilla Volcanics.||Intrudes the Garrawilla Volcanics extrusives.|Sills and dykes of alkali dolerite and microsyenodolerite; medium- to coarse-grained; lack flow structure.|
27783|Glenrowan Intrusives|70036|5|Briefly described|Map legend|||Surat Basin. Included in a mapped unit of Late Triassic to Early Jurassic intrusive rocks: dolerite, trachyte, phonolite, teschenite and syenite.||||||
27783|Glenrowan Intrusives|70791|6|Mentioned|p279|Mesozoic|Mesozoic|Gunnedah Basin.||||||
27783|Glenrowan Intrusives|71890|6|Mentioned|p5|||Surat Basin. Age equivalent of the Garrawilla Volcanics.||||||
30522|Glenrowe Granite|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Batholith.||||||
30522|Glenrowe Granite|23170|3|Fully described|p220|Early Devonian|Early Devonian|of Yeoval Batholith.||||||
79944|Glenroy Formation|71965|4|Described|p896,899,903-904,906-908,912-913|Middle Devonian|Early Devonian|Geological province: Thomson Orogen. Observed as a broad area of low and bland magnetic response, consistent with either a monotonous sequence of metasedimentary rocks (e.g. quartz-rich metasandstones), or the presence of a relatively young basin. Lithological constraints provided by scattered drillholes that have intersected low-grade metasedimetnary rocks including quartzite and phyllite. Minimum age provided by intrusion of Scalby Granite dated at 368.4+\-2.3 Ma; effects of possible contact metamorphism represented by slightly elevated magnetic response adjacent intrusion. Proposed to be correlable to Timbury Hills Formation of the Roma Shelf.||||Intruded by Scalby Granite.|Interbedded sandstone and siltstone.|
79944|Glenroy Formation|72522|4|Described|p1-2, p33-40.||Middle Ordovician|Age given is U-Pb SHRIMP maximum deposition age, Purdy et al., 2018. Older detrital zircon components are similar to Thomson beds, but ~460 Ma component distinguishes this unit and may indicate younger deposition. Unit is magnetically bland. Sample is a sand-rich interval within an otherwise mudstone-dominated sedimentary package.|459 +/- 6 Ma 206Pb/238U (204Pb-corrected)||||Fine grained sandstone sampled for dating.  Generally described as low-grade quartzites and phyllites with a single cleavage parallel, or at shallow angle, to bedding.|
82353|Gloucester Tops Granodiorite|71628|5|Briefly described|p6: 2, 4, 7-8, 13, 15-17|||New name (this study), after the Gloucester Tops pluton of Powell (1995). Named after a local geographic feature. Occurs 40 km W of Gloucester; not mapped in its entirety. Poor outcrops in swampy areas; local rounded boulders and low-level whalebacks. Limited geochemistry described. Minor sulfide mineralisation (pyrite and arsenopyrite).||Omadale Brook Suite.|||Fine- to medium-grained, amphibole granodiorite - tonalite - quartz monzodiorite. Characterised by conspicuous glomerophyric aggregates (< 1cm) of ferromagnesian minerals. I-type.|
82354|Glowang Granodiorite Phase|71628|5|Briefly described|p6: 2, 4, 6, 10-11, 13-15, 19|||New name; based on Powell's Glowang pluton (1995). Doubt exists as to whether it should be a separate unit. Named after the Glowang Trail, a local track. A small (1 km x 300m) elongate body. Largely recessive; weathering common. Very limited geochemistry described.|277.1 +/- 1.9 Ma (Waltenberg et al., 2015).|Barrington River Granodiorite.|||Dark grey, waxy, biotite-clinopyroxene-orthopyroxene granodiorite.|
76154|Gnaltaknoko Member|66623|2|Defined|p161, pp178-183, pp186-187.|Early Devonian|Late Silurian|Defined in this study. Possibly equivalent to Koonburra Creek Quartzite Member. Northern Mount Daubeny Basin. Basal clasts derived from underlying Ponto and Teltawongee Groups and units to the north. Sphericity of clasts increases up-sequence. 590 m thick, including 160 m of intercalated volcanics.|Between 425.0 +/- 7.0 Ma and 414.2 +/- 2.7 Ma.|Unit in Mount Daubeny Formation.||Unconformably overlies Ponto and Teltawongee Groups. Is intercalated with Wertago Volcanics. Is overlain by Mount Daubeny Formation sandstones.|Conglomerate; basal horizons containing boulders and angular rafts of sandstone, minor siltstone and quartzite; andesitic flows and related pyroclastics are intercalated; above these is quartzofeldspathic sandstone then polymict cobble conglomerate.|
76154|Gnaltaknoko Member|70037|5|Briefly described|p309 Fig.2, p311|||Northern margin of the Mount Daubeny Basin. Clasts sourced mainly from Ponto Group (in the NE), and almost exclusively from the Teltawongee Group (in the NW). Mis-spelt as Gnaltaknocko Member on p311.|c.425 Ma (Black, 2005 in Neef, 2012).|Basal Mount Daubeny Formation.||Distal equivalent to the Koonburra Creek Quartzite Member (in the S of the Basin).|A basal conglomerate containing at least two andesitic flows.|
76154|Gnaltaknoko Member|72522|6|Mentioned|p131.|||||Mount Daubeny Formation|||Includes conglomerate.|
27420|Goalen Head Gabbro|22815|4|Described|p88|||||||||
27420|Goalen Head Gabbro|23327|6|Mentioned|1009|||||||||
27420|Goalen Head Gabbro|29992|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
27420|Goalen Head Gabbro|29994|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
27420|Goalen Head Gabbro|41919|6|Mentioned|Fig.2|||||||||
27420|Goalen Head Gabbro|42726|5|Briefly described|map legend|||||||||
27420|Goalen Head Gabbro|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
27420|Goalen Head Gabbro|46574|5|Briefly described|Map Legend|Jurassic|Jurassic|Intrusive. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
27420|Goalen Head Gabbro|60007|5|Briefly described|Map legend|Paleozoic|Paleozoic|Age given as post-Devonian.||||||07-NOV-08
32525|Goat Mountain Alkali Granite|23043|5|Briefly described|Map Legend|Namurian|Namurian|of Gulgong Plutonic Suite.||||||
32525|Goat Mountain Alkali Granite|23170|2|Defined|p274|Carboniferous|Carboniferous|Age: SHRIMP 325.1+/- 3.3 Ma. of Gulgong Plutonic Suite.||||||
32525|Goat Mountain Alkali Granite|68003|5|Briefly described|p24 Fig.3-e. |Visean|Visean|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gulgong Plutonic Suite.||||
31578|Gobondery Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
27422|Gomiala Shale|32485|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
78375|Gongolgon Granite|69002|6|Mentioned|p12|Pragian|Pragian||c. 409, U-Pb SHRIMP|||||
78375|Gongolgon Granite|70210|5|Briefly described|p1, p8, p10, p38, p40-41|Early Devonian|Late Silurian|Cobar-Bourke district.|410.9 +/- 2.5 Ma.|||||
78375|Gongolgon Granite|70602|6|Mentioned|p66 Fig 2, p67,72|Early Devonian|Early Devonian|Aeromagnetic map data given.|410.0+/-2.5Ma|Tarcoon Plutonic Complex||||28-JUN-16
78375|Gongolgon Granite|71345|2|Defined|p4,14-15,17-21|Early Devonian|Early Devonian|Type location: Lat -30.3471 Long 146.8965; GR490049 6642742 (excellent exposure of weathered granite on the southern bank of the Bogan River adjacent to the weir) Also exposed sporadically in the Gongolgon village surrounds. Named for the village of Gongolgon. Described by Brunker (1968). Referred to informally as Gongolgon granite by Proksch (1982), Black (2006), Blevin (2011) and Hegarty (2011). Defined herein after Blevin (2011). The massive nature of the granite distinguishes it from foliated metasedimentary rocks in the area. Associated with a SWtrending gravity low and radioelement anomaly (red and white hues) extending 10km and 7km respectively. Highly evolved, volatile-rich, strongly fractionated, moderately oxidised I-type granite with high W, U, Th and REE; presence of tourmaline indicate late stages of crystallisation (Blevin et al., 2011). In contrast, Byrnes (1993) described the granite as S-type (based on description and presence of minor poikilitic andalusite in North Broken Hill Limited (1982); Barron (pers. comm. 1989, in Byrnes 1993) suggested a A-type affinity. Similar in age and geochemistry to the unfractionated Mount Kelly Granite. Black (2006) reported a SHRIMP U-Pb magmatic age of 410.9+\-2.5 Ma.|410.9+\-2.5 Ma (SHRIMP U-Pb, magmatic).||||Massive, coarse grained quartz-plagioclase-K feldspar granite, includes xenotime, apatite, zircon, possible topaz and secondary muscovite.|02-DEC-19
78375|Gongolgon Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: small elongate zone of low magnetic intensity with narrow linear trends interpreted as dykes. High radioelement concentrations in areas of outcrop.|410.9 +/- 2.5 Ma.|Tarcoon Plutonic Complex.|||Altered pink alkali-feldspar granite with tourmaline patches; local quartz-feldspar porphyry and porphyritic, graphic and miarolitic textures. I-type.|
26266|Gooandra Volcanics|22687|6|Mentioned|110|Early Silurian|Ordovician|Geol province Lachlan Fold Belt||||||
26266|Gooandra Volcanics|22768|6|Mentioned|p174|||||||||
26266|Gooandra Volcanics|22857|4|Described|p420 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Of the Kiandra Group? Fine feldspathic siltstone and shale, aphyric and feldspathic basalt, lava breccia, pillow lava; contains graptolites. Max. thickness: 3km. ||||||
26266|Gooandra Volcanics|24133|6|Mentioned|p57|||Geological Province: Lachlan Fold Belt.||||||
26266|Gooandra Volcanics|36443|5|Briefly described|map legend|Early Ordovician|Early Ordovician|BMR map codes Ogl: aphyric and feldsparphyric basalt, lava breccia, pillow lava, rhyolite, shale; Ogs: fine feldspathic siltstone and shale; Ogi: ophitic gabbro and dolerite.||||||
26266|Gooandra Volcanics|36512|6|Mentioned|p21|||||||||
26266|Gooandra Volcanics|39660|6|Mentioned|p449|||||||||
26266|Gooandra Volcanics|41423|5|Briefly described|p270|||||||||
26266|Gooandra Volcanics|42313|6|Mentioned|p34|||||||||
26266|Gooandra Volcanics|42820|5|Briefly described|p78|||||||||
26266|Gooandra Volcanics|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Ovg1||||||
26266|Gooandra Volcanics|44093|5|Briefly described|p183  App. 1|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
26266|Gooandra Volcanics|45147|2|Defined|M9|early Gisbornian|late Darriwilian|Late Darriwilian to Early Gisbornian||||||
26266|Gooandra Volcanics|60078|6|Mentioned|Map Legend|Late Ordovician|Middle Ordovician|||||||15-JUL-04
26266|Gooandra Volcanics|60308|6|Mentioned|p38|Llandovery|Llandovery|"Important stratigraphic unit with contentious age" Preferred age quoted.|435 Ma|||||
26266|Gooandra Volcanics|63278|6|Mentioned|p157|Gisbornian|Darriwilian |Geological Province: Kiandra Volcanic Belt, LFB. MORB-like lithologies.||||||07-FEB-11
26266|Gooandra Volcanics|63290|6|Mentioned|p403 Fig. 6c, p394 Tb. 1, p398|Late Silurian|Late Silurian|Geological Province: Tumut Block.||||||
26266|Gooandra Volcanics|66197|5|Briefly described|p631 Fig.3a|||Mafic volcanics. Underlies the Jackalass Slate and Bumbolee Creek Formation. Tumut Trough.||||||14-MAR-12
26266|Gooandra Volcanics|67322|4|Described|p26; Fig.5|Bolindian|Eastonian|Defined by Owen and Wyborn (1979). Occurs in the upper part of the Kiandra Group. Age is determined from p20 Fig.5 (Strat. column). Occurs in the Kiandra Volcanic Belt.||Of the Kiandra Group.||Overlies the Nine Mile Volcanics.|Volcaniclastic rocks; siliceous siltstone-dominated strata with volcaniclastic debris flows, gritstones and conglomerates; or siliceous siltstones with interbedded quartz sandstones and turbidite sequences.|22-FEB-18
26266|Gooandra Volcanics|68116|5|Briefly described|Appendix, Map 28.|Sandbian|Dariwilian|Minimum age written as Gisbornian in text.|||||Basaltic to andesitic lava and breccia, pillow lava; minor rhyolite, volcaniclastic siltstone and shale; ophitic gabbro; greenschist facies metamorphism; cleavage and schistosity well developed.|
26266|Gooandra Volcanics|68822|6|Mentioned|p335|||||||||
33689|Goobang Volcanics|24417|3|Fully described|p28|Late Ordovician|Late Ordovician|Of Northparkes Volcanic Group.||||||
33689|Goobang Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
33689|Goobang Volcanics|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|Of the Northparkes Volcanic Group.||||||13-JUL-04
33689|Goobang Volcanics|63278|6|Mentioned|p145 Fig. 1, p151|Silurian|Silurian|Previously assumed to be [Late] Ordovician, but geochemical correlation of some units in the area to Goonumbla Volcanics suggests these units may be Early Silurian (Llandovery).||||||25-MAR-20
33689|Goobang Volcanics|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
33689|Goobang Volcanics|63283|6|Mentioned|p192, p196 Fig. 4|||||||||07-FEB-11
33689|Goobang Volcanics|67107|6|Mentioned|p696|||Peak Hill, c.45km N of Parkes. Appears as Goobang volcanics.||||||
33689|Goobang Volcanics|70684|6|Mentioned|p3, p54|||Probably Silurian.||||||
33689|Goobang Volcanics|72495|6|Mentioned|p218, 225, 227, p231|Ordovician|Ordovician|Occurs to the east of the Parkes Thrust. Poorly exposed.||||Faulted under the Kirribilli Formation.||26-MAR-20
25929|Goobarragandra Volcanics|22638|1|Redefined|p32|Pridoli|Caradoc|429 +/- 16 Ma isochron. Volcanic equivalent of Young Ganodiorite. Previously "Goobarragandra porphyry"||||||
25929|Goobarragandra Volcanics|22687|6|Mentioned|111|||Geol province Lachlan Fold Belt||||||
25929|Goobarragandra Volcanics|22691|3|Fully described|P315, Fig2|Ludlow|Llandovery|Ages of unit are 429+/-16, 429+/-9 and 417+/-8 Ma.||||||02-JUN-08
25929|Goobarragandra Volcanics|22768|6|Mentioned|p174||Llandovery|Max Age: 429 (+/-) 16 Ma||||||
25929|Goobarragandra Volcanics|22857|4|Described|p174, p450 App.1, Tb.A1.6|Wenlockian|Wenlockian|Age: 429Ma +/-16Ma (Rb/Sr whole rock, Owen and Wyborn, 1979). Includes former "Fiery Range Porphyry" and "Wyora Porphyry" of  "Douro Group". Part of "Douro Group" in the Canberra-Yass Shelf region. Geological Province: Tumut Trough/Canberra-Yass Basin.||||||02-JUN-08
25929|Goobarragandra Volcanics|23214|6|Mentioned|p168|||Intruded by the Young Granodiorite.||||||
25929|Goobarragandra Volcanics|23309|6|Mentioned|p390|||||||||
25929|Goobarragandra Volcanics|23454|6|Mentioned|p27 Fig.1|||||||||
25929|Goobarragandra Volcanics|24005|6|Mentioned|p293|||||||||
25929|Goobarragandra Volcanics|36441|5|Briefly described|map legend|Late Silurian|Late Silurian|Extrusive. S-type. Dacite ignimbrite, agglomerate, tuff, sediments, intrusive porphyry. Includes interbedded marble, calc-silicate hornfels (Sg1). BMR map code: Sg.||||||
25929|Goobarragandra Volcanics|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Extrusive. Dacite ignimbrite, agglomerate, minor tuff, andesite and sediments. BMR map code: Sg.||||||
25929|Goobarragandra Volcanics|36534|6|Mentioned|p225|||||||||
25929|Goobarragandra Volcanics|37529|5|Briefly described|p8|||See also P5 & 6||||||
25929|Goobarragandra Volcanics|38548|6|Mentioned|p110|||||||||
25929|Goobarragandra Volcanics|40689|6|Mentioned|p3|||||||||
25929|Goobarragandra Volcanics|41563|6|Mentioned|p506|||||||||
25929|Goobarragandra Volcanics|42045|6|Mentioned|p147|||||||||
25929|Goobarragandra Volcanics|42145|4|Described|Table 1 P624|||||||||
25929|Goobarragandra Volcanics|42313|3|Fully described|p122|Middle Silurian||||||||
25929|Goobarragandra Volcanics|42314|5|Briefly described|Map|Middle Silurian||||||||
25929|Goobarragandra Volcanics|42497|5|Briefly described|Map Legend|Pridolian|Wenlockian|||||||
25929|Goobarragandra Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
25929|Goobarragandra Volcanics|42828|5|Briefly described|Table 1 P129|Late Silurian|Middle Silurian|||||||
25929|Goobarragandra Volcanics|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv5||||||
25929|Goobarragandra Volcanics|44093|5|Briefly described|p188 App. 1|Late Silurian|Late Silurian|Felsic volcanics. Geological Province: Lachlan Fold Belt.||||||
25929|Goobarragandra Volcanics|44192|5|Briefly described|Map Legend|Wenlockian|Llandoverian|||||||
25929|Goobarragandra Volcanics|44936|5|Briefly described|Map Legend||Silurian|||||||
25929|Goobarragandra Volcanics|45147|2|Defined|M127|Late Silurian|Late Silurian|||||||
25929|Goobarragandra Volcanics|49705|6|Mentioned|p3|||||||||
25929|Goobarragandra Volcanics|50191|6|Mentioned|p6, 21 Fig. 1|Silurian|Silurian|Intruded by the Young Granodiorite||||||02-AUG-04
25929|Goobarragandra Volcanics|50230|5|Briefly described|Map legend|Ludlow|Wenlock|Of the Douro Group.  Medium- to coarse-grained often welded porphyritic crystal vitric rhyolitic to dacitic ignimbrite.||||||10-MAY-04
25929|Goobarragandra Volcanics|50231|5|Briefly described|Map Legend|Ludlow|Wenlock|Of the Douro Group.||||||
25929|Goobarragandra Volcanics|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
25929|Goobarragandra Volcanics|63290|6|Mentioned|p402 Fig. 6(b)|Ordovician|Ordovician|Geological Province: Kiandra Volcanic Belt.||||||
25929|Goobarragandra Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Douro Group.Grey-blue massive, medium- to coarse-grained, often welded, porphyritic crystal-vitric rhyolitic to dacitic ignimbrite. Limestone breccia+volcaniclastic sst. Laminated mudstone. Volcaniclastic sst interbedded with laminated tuffaceous mudst||||||
25929|Goobarragandra Volcanics|66197|6|Mentioned|p631 Fig.3b|Silurian|Silurian|Canberra-Yass Basin. Silicic volcanics.||||||14-MAR-12
25929|Goobarragandra Volcanics|68592|2|Defined|p428, p431, p433-4, p437-55, p457, p519|Wenlock|Wenlock|See also p73, p125-6, p226, p269, p271, p1197, p1219, p1873. Originally Wyora Porphyry (and another un-named porphyry unit) of Joplin et al. (1953); both renamed as Goobarragandra Porphyry by Adamson in Booker, Rayner, Hall et al. (1960). Ashley et al. (1972) described their Goobarragandra Beds which were continuous with these earlier-named porphyries. Owen and Wyborn (1979) proposed the name Goobarragandra Volcanics to include all these units. Extended by Basden (1990); Warren et al. (1995) and Cramsie et al (1978). This study includes Goobarragandra Volcanics in Douro Group. Type locality described. At least 600m thick. Hosts three Pb-Zn-Ag-Cu skarn occurrences close to contact with Young Granodiorite. Prospective for aggregate. Isolated lenses of limestone have been quarried for lime. Thought to be comagmatic with Young Suite. Binalong structural zone: deformation and metamorphism described. Fossil fauna listed.|429 +/- 16 Ma (Rb-Sr whole rock).|Unit in Douro Group.||Is intruded by Micalong Swamp Basic Igneous Complex and Young Granodiorite. Is faulted against, and elsewhere unconformably overlain by, Mountain Creek Volcanics. Correlates with Hawkins Volcanics.|Medium- to coarse-grained, massive, often welded, porphyritic, crystal-rich, dacitic to rhyolitic ignimbrite; subordinate volcaniclastic sandstone, siltstone and mudstone; minor dacitic and rhyolitic lava; allochthonous limestone lenses. S-type.|
25929|Goobarragandra Volcanics|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdn. Includes five unnamed units: micritic and fossiliferous limestone and marble with interbedded mudstone; laminated mudstone and beds of sandstone; volcaniclastic sandstone interbedded with tuffaceous mudstone, and sandstone beds are locally pebbly; quartzose sandstone and mudstone; crystal-rich tuffaceous sandstone. On Yass and Boorowa 1:100 000 mapsheet portions of Time-Space Plot.||Douro Group|Includes five unnamed units.||Massive, medium-coarse grained, densely welded dacitic ignimbrite with common cooling columns. Minor pebbly volcanic sandstone and mudstone, crystal rich tuffaceous sandstone, limestone, quartzose - quartz lithic sandstone and laminated mudstone.|
25929|Goobarragandra Volcanics|70540|5|Briefly described|Map Legend|Silurian|Silurian|Includes five unnamed members; fossiliferous limestone and marble, quartz lithic sandstone, quartzose sandstone, tuffaceous sandstone and volcaniclastic sandstone.||Douro Group|||Massive, medium-coarse grained, crystal rich, densely-welded dacitic ignimbrite; minor pebbly volcanic sandstone and mudstone, crystal-rich tuffaceous sandstone, limestone, quartzose to quartz lithic sandstone and laminated mudstone.|26-AUG-16
25929|Goobarragandra Volcanics|70545|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|||Massive, medium-coarse grained, densely welded dacitic ignimbrite with common cooling columns. Minor pebbly volcanic sandstone and mudstone, crystal rich tuffaceous sandstone, limestone, quartzose - quartz lithic sandstone and laminated mudstone.|
25929|Goobarragandra Volcanics|71656|5|Briefly described|p12 Fig.2, p11, p19|Ludlow|Wenlock|Contains isolated limestone pods with Silurian age fossils lacking precision due to low yields of conodont fauna. Age based on macrofauna: corals, brachiopds.||Douro Group||Partially equivalent to Glen Bower Formation.|Volcanics containing isolated limestone pods.|
25929|Goobarragandra Volcanics|73215|4|Described|p991, 995-998, 1000-1002, 1003, 1004|Middle Silurian|Middle Silurian|Talmo-Taemas area, about 30 km W of Yass, NSW. Lachlan Orogen. Photographs, microphotographs, map, cross-section. Compositionally grouped with Bullenbalong Supersuite.|433-430 Ma.|Douro Group.||Is overlain by Talmo Formation. Equivalent to Hawkins Volcanics.|S-type. Mostly grey-green, massive dacitic ignimbrite; characterised by broken and fractured crystals. Lenses of mudstone and volcaniclastic sandstone. Local columnar jointing. Includes blocks of Late Ordovician graptolitic siltstone.|
25929|Goobarragandra Volcanics|73483|6|Mentioned|p407 Fig.1|||||||||
68172|Goodwood Mudstone|60281|5|Briefly described|Fig. 33 Appendix 1|Cretaceous|Cretaceous|Of the Maryborough Formation.  Geological Province: Maryborough Basin.||||||22-MAR-05
32590|Googodery Trachyte|23043|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|||||||
32590|Googodery Trachyte|23170|2|Defined|p313|Mesozoic|Mesozoic|||||||
32590|Googodery Trachyte|73299|6|Mentioned|p1105|Triassic|Triassic|||||||
40440|Gooligal Group|24580|5|Briefly described|p828|Pridoli|Pridoli|Overlain by the Gregra Group. Geological Province: Eastern Lachlan Fold Belt.||||||
23626|Gooloo granite|36600|6|Mentioned|p97 Table 1, p109|Carboniferous|Carboniferous|After McIlveen (1975). Granite in Gooloo Creek. Exposed below the Permian Conjola Subgroup, Sydney Basin. Granite is even and coarse-grained (5mm). 4% quartz, 62% K-feldspar, 27% plagioclase, biotite, hornblende each 3%, magnetite, sphene very minor accessories.||||||20-MAR-23
33409|Gooloogong Member|23217|6|Mentioned|p12|||(Young, 1999b).||||||08-MAR-06
33409|Gooloogong Member|23392|2|Defined|p13||Frasnian|Supersedes 'Gooloogong Beds' of Colwell (1974). Possible correlation with lower part of the Mount Cole Fm. Of the Hunter Formation. Geological Province: Lachlan Fold Belt. Max Thickness: 80m||||||
33409|Gooloogong Member|24417|3|Fully described|p134|Frasnian|Frasnian|Of Hunter Formation.  Supersedes "Gooloogong Beds".  Underlain by Peaks Formation.  Max. thickness: 80m.||||||
33409|Gooloogong Member|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hunter Formation (Hervey Group).||||||05-JUL-04
33409|Gooloogong Member|60009|5|Briefly described|Map Legend|Frasnian|Frasnian|Of the Hunter Formation (Hervey Group).||||||13-JUL-04
33409|Gooloogong Member|68592|6|Mentioned|p1738|Late Devonian|Late Devonian|Marginal marine. Possible correlate of Strathaird Formation.||Unit in Hunter Formation.||||
23627|Goona Volcanics|22768|5|Briefly described|p171|||||||||
23627|Goona Volcanics|22857|4|Described|p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Mount Hope Group (Cobar Supergroup). Max. thickness: 700m. Geological Province: Mount Hope Trough (Darling Basin). See also p171 photo 3.||||||
23627|Goona Volcanics|23048|6|Mentioned|p13|||||||||
23627|Goona Volcanics|23214|6|Mentioned|p360|||||||||
23627|Goona Volcanics|37772|4|Described|p8|||||||||
23627|Goona Volcanics|40269|4|Described|p150|||Mention P148||||||
23627|Goona Volcanics|40913|6|Mentioned|Map legend|Pragian|Pragian|||||||
23627|Goona Volcanics|41126|2|Defined|p65|early Pragian|early Pragian|Mention p56.||||||23-SEP-19
23627|Goona Volcanics|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
23627|Goona Volcanics|41821|3|Fully described|p31|Early Devonian||||||||
23627|Goona Volcanics|42144|6|Mentioned|Fig.3 P604|||||||||
23627|Goona Volcanics|42521|5|Briefly described|Fig.3b P16|||||||||
23627|Goona Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
23627|Goona Volcanics|43089|5|Briefly described|Map Legend|||of Mount Hope Group||||||
23627|Goona Volcanics|69511|5|Briefly described|p6|||Barron et al. (1982).||||Conformably overlies Mount Halfway Volcanics.||
23627|Goona Volcanics|70751|6|Mentioned|p17, p19, p30|||||Mount Hope Group||||
23627|Goona Volcanics|72908|6|Mentioned|p3|||Simpson (2014) (see also Downes, Blevin et al., 2016) proposed that the stratigraphy of the Mount Hope Group be simplified, with the Ambone, Regina, Goona and part of the Coando Volcanics being grouped into the Mount Halfway Volcanics.||Mount Hope Group||||
24296|Goonbri Formation|22857|4|Described|p520 App.1 Tb.A1.9, p315 Fig. 22.8|Early Permian|Early Permian|Of the Bellata Group. Dark organic-rich siltstone, thin coal, graded siltstone-claystone, laminated sandstone and siltstone. Max. thickness: >125m. Geological Province: Gunnedah Basin.||||||
24296|Goonbri Formation|22865|6|Mentioned|Fig22.8p315|||||||||
24296|Goonbri Formation|23050|5|Briefly described|p 82 Fig.17|Early Permian|Early Permian|of Gunnedah Basin.||||||
24296|Goonbri Formation|23566|5|Briefly described|p116 Fig. 2|Early Permian|Early Permian|Parent: Bellata Group. Geological Province: Gunnedah Basin||||||
24296|Goonbri Formation|23740|5|Briefly described|p1221|Permian|Permian|Geological Province: Gunnedah Basin||||||
24296|Goonbri Formation|24159|5|Briefly described|p150 Fig.3, p149|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Overlying Unit: Maules Creek Formation. Underlying Unit: Boggabri Volcanics and Werrie Basalt.||||||
24296|Goonbri Formation|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
24296|Goonbri Formation|40767|4|Described|p2|||||||||
24296|Goonbri Formation|41290|5|Briefly described|p225|||||||||
24296|Goonbri Formation|41451|6|Mentioned|p14|||||||||
24296|Goonbri Formation|42182|6|Mentioned|Table 1|||||||||
24296|Goonbri Formation|42284|5|Briefly described|Fig.11 P104|||||||||
24296|Goonbri Formation|42463|6|Mentioned|Fig.6 P173|||Table just says 'Goonbri'.||||||
24296|Goonbri Formation|43017|5|Briefly described|Fig.2,p374|||||||||
24296|Goonbri Formation|43194|1|Redefined|p98 Tb. 8.2, p100-103, p133 App. 1|Early Permian|Early Permian|See also references on p95, p128, p129 Tb.8.3. Gunnedah Basin. Now of Bellata Group. Unconformably overlies and onlaps Boggabri Volcanics and (where present) Leard Formation. Underlies Maules Creek Formation. Assigned Stage 3 palynological age.||||||
24296|Goonbri Formation|43582|6|Mentioned|Fig.5,p16||Early Permian|||||||
24296|Goonbri Formation|50629|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Gunnedah Basin.  Of the Bellata Group. Underlies: Porcupine Formation.  Overlies: Leard Formation.||||||05-JUL-04
24296|Goonbri Formation|61313|5|Briefly described|p91, p98 Fig.G10|Permian|Permian|Lacustrine unit; comprises dark organic rich siltstone, thin coal bands, graded siltstone/claystone, laminated siltstone and sandstone. Conformably overlies Leard Fm.; overlain by Maules Creek Fm. Max. thickness: 95m. Geol. Prov: Gunnedah Basin.||||||16-JUN-06
24296|Goonbri Formation|61377|5|Briefly described|p149 Fig. SU8|||Lacustrine deposits. Geological Province: Gunnedah Basin. See also p154 Fig. SU9. Presented as Goonbri only in Figure SU9.||||||07-FEB-11
24296|Goonbri Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Gunnedah Basin.||||||17-MAR-09
24296|Goonbri Formation|62357|5|Briefly described|p524 Fig. 7|Early Permian|Early Permian|Geological Province: Gunnedah Basin.||||||
24296|Goonbri Formation|63832|6|Mentioned|p131 fig 2|Artinskian|Sakmarian|Of Gunnedah Basin. Sixth (P2) glaciation.||||||
24296|Goonbri Formation|64631|5|Briefly described|p44 Fig.2.|Artinskian|Sakmarian|Gunnedah Basin. Biostratigraphic age control for base and top.||||||
24296|Goonbri Formation|65112|6|Mentioned|Fig 4 p314|Early Permian|Early Permian|Gunnedah Basin. Overlies the Leard Formation, underlies the Maules Creek Formation.||||||22-MAR-12
24296|Goonbri Formation|65113|5|Briefly described|Fig 4 p340|Early Permian|Early Permian|Gunnedah Basin. Overlies Werrie Basalt.||||||
24296|Goonbri Formation|65114|5|Briefly described|p385 Fig.3|Early Permian||||||||
24296|Goonbri Formation|65115|6|Mentioned|Fig 2 p403|Permian|Permian|Underlies the Maules Creek Formation in the Gunnedah Basin.||||||
24296|Goonbri Formation|65116|4|Described|p436, Fig.2,  Fig 6 p441|Early Permian|Early Permian|Underlies the Maules Creek Formation, overlies the Leard Formation in the Gunnedah Basin. Organic rich siltstone, with laminated claystone. Upward coarsens to fine and medium grained sandstone.||||||
24296|Goonbri Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Maules Creek Formation in the Gunnedah Basin.||||||
24296|Goonbri Formation|66191|5|Briefly described|p485 Fig.2, p485|Early Permian|Early Permian|Gunnedah Basin. Underlies the Maules Creek Formation, overlies both the Boggabri Volcanics and the Werrie Basalt. Lacustrine sediments inundated by the Maules Creek Formation.||||||
24296|Goonbri Formation|68003|5|Briefly described|p38 Fig.3-j, p40, p57 Fig.3-n.|Early Permian|Early Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Part-equivalent to Greta Coal Measures in the Sydney Basin.||Unit in Bellata Group.|||Fine-grained lacustrine sediments.|
24296|Goonbri Formation|68004|5|Briefly described|p23 Table 1, p31, p170.|||Gunnedah Basin. Known only from drill core. Lacustrine depositional environment. Moderate to high potential for coal seam methane. A potential oil source rock.||Unit in Bellata Group.|||Organic rich siltstone, thin layers of coal, laminites and fine- to medium-grained, moderately well-sorted sandstones.|
24296|Goonbri Formation|70791|5|Briefly described|p277-281, p283, p285-287, p292-294|Cisuralian|Cisuralian|Is assigned in this article to the Dalwood Group, "consistent with Hunter and Newcastle coalfield stratigraphy based on palynological ages and conformity relationships". Gunnedah Basin. Has two lateral facies variants (see Lithology). Maximum thickness over 100m. Sediment source is primarily from underlying Werrie Basalt and Boggabri Volcanics. Has microflora of APP22 age.||Bellata Group.||Nonconformably overlies Werrie Basalt and Boggabri Volcanics. Is overlain disconformably by Maules Creek Formation.|Bioturbated, sulfur-bearing, upward-fining package of conglomerate, sandstone and siltstone; thinly laminated, fine- to medium-grained sandstone and siltstone and featureless siltstone.|
24296|Goonbri Formation|70878|5|Briefly described|p718 Fig.13|Permian|Permian|Gunnedah Basin.||Bellata Group.||Overlies Leard Formation. Is overlain by Maules Creek Formation.||
24296|Goonbri Formation|71701|5|Briefly described|p170|||||||Overlain by the Maules Creek Formation.||
77251|Goondi Formation|68004|5|Briefly described|p44.|Early Permian|Early Permian|New name. Gilgandra Sub-basin, Gunnedah Basin. Direct equivalent of the Leard Formation further to the east. ||||Overlies Cobbora Formation. Is overlain by Mirrie Formation.|Colluvial/alluvial deposits from weathering of basement metasediments: subangular broken pieces of basement metasediments in a light grey sandstone matrix; clasts have tabular shape and bimodal sorting.|17-OCT-12
24297|Goonigal Group|22503|6|Mentioned|Fig.6 p649||Late Silurian|||||||
24297|Goonigal Group|22768|6|Mentioned|p180||Late Silurian|||||||
24297|Goonigal Group|22857|5|Briefly described|p180, p454 App.1. Tb.A1.6|Pridolian|Pridolian|Formerly the "Fairhill Formation" of Savage (1969). Greywacke and volcaniclastics. Overlain by rocks of the Gregra Group. See also p454 and p456 App.1, Tb.A1.6.||||||
24297|Goonigal Group|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|||||||
24297|Goonigal Group|23170|1|Redefined|p109|Pridoli|Ludlow|of Lachlan Fold Belt.||||||12-FEB-09
24297|Goonigal Group|23214|1|Redefined|p151|Late Silurian|Late Silurian|Includes some rocks previously included in Burgoon Subgroup, Cudal Group, Fairhill Formation and Manildra Group. Intruded by Gumble Granite. Max. thickness 1425m. Overlying unit: Grega Group, underlying unit: Cudal Group.||||||12-FEB-09
24297|Goonigal Group|23522|5|Briefly described|p248 Fig 4|Lochkovian|Ludlow|||||||
24297|Goonigal Group|24417|4|Described|p58|Late Silurian|Late Silurian|Only Moura Formation is present on FORBES 1:250 000.||||||
24297|Goonigal Group|40328|1|Redefined|p102|Silurian|Silurian|Also mentioned on P71 and P76||||||
24297|Goonigal Group|42032|6|Mentioned|Fig.11 P503|||||||||
24297|Goonigal Group|43494|6|Mentioned|p20|Silurian|Silurian|Overlies the Cudal Group units. Age is Pridolian.||||||16-MAR-06
24297|Goonigal Group|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|||||||
24297|Goonigal Group|60009|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes: Moura Formation.||||||13-JUL-04
24297|Goonigal Group|61859|6|Mentioned|p5 Fig.2, p6|||Formerly named the Fairhill Formation (Savage, 1968).||||||
24297|Goonigal Group|63289|6|Mentioned|p373 Fig. 7|Early Devonian|Silurian|||||||07-FEB-11
24297|Goonigal Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Manildra. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
24297|Goonigal Group|70297|4|Described|map legend|Pridoli|Pridoli|Cowra Trough.||||Conformably overlies Cudal Group; is conformably overlain by Grega Group.|Feldspar-lithic volcaniclastic sandstone, siltstone, shale, chert; pyroxene andesite lava; minor conglomerate, breccia, calcareous sandstone, rhyolite dykes; coarsens upwards.|
40939|Goonoonglah Monzodiorite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Porphyritic ex-pyroxene-biotite-hornblende-quartz monzodiorite, quartz monzodiorite, quartz alkali gabbro.  See also misspelt Goonooglah Monozodiorite.||||||13-DEC-05
40939|Goonoonglah Monzodiorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Goonoonglah Suite. Grey to dark green, med-gr., commonly porphyritic, pyroxene-biotite-hornblende quartz syenite, quartz monzonite + quartz monzodiorite, minor biotite-hornblende-quartz diorite and black, medium-gr. biotite-hornblende-augite gabbro.||||||
40939|Goonoonglah Monzodiorite|68592|2|Defined|p619, p1275, p1482, p1491-1507|Early Devonian|Early Devonian|Originally named the Bigga House Basic Igneous Complex (Hasan, 1957, 1959); changed to Bigga Mafic Complex following further mapping by Yacopetti (1987). Chappell et al. (1991) changed the name to Goonoonglah Gabbro (after Goonoonglah Creek) to avoid confusion with adjacent Bigga Granite; here renamed Goonoonglah Monzodiorite after more recent petrography. Type pluton for the mafic component of Keverstone Supersuite. Type locality and other good exposures described. Poorly exposed; occupies lower topographic areas. Lithologies and geochemistry described in considerable detail. Geophysical properties described. Very similar characteristics to Box Ridge Volcanics.|413 +/- 5 Ma (SHRIMP U-Pb zircon: Wilde, 2001).|Unit in Goonoonglah Suite.||Is intruded by Bigga and Yewrangara Granites.|A-type. Grey to dark-grey, medium-grained, massive, often porphyritic, quartz syenite, quartz monzonite and quartz monzodiorite; minor quartz diorite; black, massive gabbro. Some phases intrude others. All phases fractionated from a common magma.|
40939|Goonoonglah Monzodiorite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dng. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Goonoonglah Suite|||Medium grained, commonly porphyritic; pyroxene-biotite-hornblende-quartz syenite, quartz monzonite and quartz monzodiorite, minor biotite-hornblende-quartz diorite and medium grained, biotite-hornblende-augite gabbro; medium K, low Th and U;|
40939|Goonoonglah Monzodiorite|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Goonoonglah Suite|||Medium grained, commonly porphyritic; pyroxene-biotite-hornblende-quartz syenite, quartz monzonite and quartz monzodiorite, minor biotite-hornblende-quartz diorite and medium grained, biotite-hornblende-augite gabbro; medium K, low Th and U;|
70027|Gooramma Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Contains 6 named granites, a named granodiorite and a named monzodiorite.||||||25-JUN-08
70027|Gooramma Suite|68592|2|Defined|p845 Fig.141, p1306, p1397-8, p1421-58|Early Devonian|Early Devonian|See also p73, p973, p1669 Fig.344. New unit and name, after Parish of Gooramma. Blevin (2011) chose the Willawong Creek Granite as the type pluton. Constituent plutons generally form low rises and sometimes rocky hills; dykes (many of which are of un-named units) are typically found high in the landscape as rounded boulders and tors. Geochemistry described. Not isotopically dated: age from intrusive relationships and Boggy Plain Supersuite. Murringo Iron Prospect and Murringo Copper Prospect are close to Gooramma Suite units, but the relationship to mineralisation is uncertain. Binalong structural zone: deformation described.||Unit in Boggy Plain Supersuite.|Includes Burrowa Hills, Little Range, Macclesfield, Moonshine, Willawong Creek and Wyoming Granites; Hazeldean Granodiorite; and Crowther Monzodiorite.|Intrudes Young Granodiorite; Hawkins, Goobarragandra and Mountain Creek Volcanics; Licking Gully Granite and Kirawin Formation.|Mainly granite to granodiorite; several plutons also have quartz monzonite and quartz monzodiorite phases; dykes range from quartz monzonite to quartz monzodiorite to diorite; one small gabbro body; typically medium-grained and equigranular. I-type.|
70027|Gooramma Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Includes two unnamed members; dykes and small intrusions of medium grained, massive, porphyritic and equigranular quartz monzodiorite, diorite quartz monzonite; and an undescribed gabbro. On Yass and Boorowa 1:100 000 mapsheet portions of Time-Space Plot.|||Burrowa Hills Granite, Crowther Monzodiorite, Hazeldean Granodiorite, Little Range Granite, Macclesfield Granite, Moonshine Granite, Willawong Creek Granite, Wyoming Granite and two unnamed units.||Generally made up of equigranular to porphyritic hypersthene-augite-biotite-hornblende granites and granodiorites. Porphyritic leucocratic granites and microgranites are also present. Magnetic susceptibility is generally high amongst all members.|
70027|Gooramma Suite|70540|5|Briefly described|Map Legend|Devonian|Devonian|Includes an unnamed unit of dykes and small intrusions of medium grained, massive, porphyritic and equigranular monzodiorite, diorite, quartz monzonite, granite and tonalite.|||Includes Burrowa Hills Granite.|||
70027|Gooramma Suite|70545|5|Briefly described|Map Legend|Devonian|Devonian|Includes two unnamed members; dykes and small intrusions of medium grained, massive, porphyritic and equigranular quartz monzodiorite, diorite quartz monzonite and an undescribed gabbro.|||Burrowa Hills Granite, Crowther Monzodiorite, Hazeldean Granodiorite, Little Range Granite, Macclesfield Granite, Moonshine Granite, Willawong Creek Granite, Wyoming Granite.||Generally made up of equigranular to porphyritic hypersthene-augite-biotite-hornblende granites and granodiorites. Porphyritic leucocratic granites and microgranites are also present. Magnetic susceptibility is generally high amongst all members.|20-SEP-17
23631|Goran Conglomerate Member|38614|4|Described|p10|||||||||
23631|Goran Conglomerate Member|40321|6|Mentioned|p19|||||||||
23631|Goran Conglomerate Member|40680|5|Briefly described|p23|||||||||
23631|Goran Conglomerate Member|40767|6|Mentioned|Fig.10|||||||||
23631|Goran Conglomerate Member|43194|5|Briefly described|p98 Tb. 8.2, p115|Late Permian|Late Permian|Name used to describe part of an unnamed lithic conglomerate unit in the upper sequence of the Black Jack Formation. In a separate paper (Tadros, in press, summarised in Appendix 1) it is proposed that this name be abandoned.||||||
24298|Gospel Oak Shale|22503|6|Mentioned|Fig.6 p649||Late Silurian|||||||
24298|Gospel Oak Shale|22768|6|Mentioned|p179|||||||||
24298|Gospel Oak Shale|22857|4|Described|p179, p458 App.1, Tb.A1.6|Wenlockian|Llandovery|Of the Cudal Group. Red, green and brown shale, buff siltstone, shale with concretions. Max. thickness: 105m. Geological Province: Cowra Trough. ||||||
24298|Gospel Oak Shale|23214|2|Defined|p115|Wenlock|Llandovery|Of Cudal Group. Originally named Lower Avoca Valley Shale by Ryall (1964). 105m thick at type section. Overlying unit: Canowindra Volcanics, underlying unit: Liscombe Pools Limestone.||||||
24298|Gospel Oak Shale|40328|2|Defined|p79|Silurian|Silurian|Also mentioned on P10 and P71||||||
24298|Gospel Oak Shale|43640|5|Briefly described|Map Legend||Silurian|||||||
24298|Gospel Oak Shale|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of red, green and brown shale, buff siltstone, shale with concretions.||||||15-JUL-08
24298|Gospel Oak Shale|43782|5|Briefly described|Map Legend|Wenlock|Llandovery|Of Cudal Group.||||||04-MAR-09
24298|Gospel Oak Shale|64826|5|Briefly described|p1040 Tb. 1|Wenlock|Wenlock|Of the Cudal Group.||||||04-MAR-09
24298|Gospel Oak Shale|64994|5|Briefly described|p7|Ludlow|Wenlock|Of Pickett (1982). Contains graptolites.||||||07-FEB-11
24298|Gospel Oak Shale|67847|5|Briefly described|p33|Wenlock|Llandovery|Contains graptolite fauna which is briefly discussed. ||||Conformably overlain by the Canowindra Volcanics.||
24298|Gospel Oak Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group||||
41061|Gostwyck Monzogranite|24366|5|Briefly described|p8 Fig. 6|Early Permian|Early Permian|Of the Hillgrove Plutonic Suite.||||||
41061|Gostwyck Monzogranite|71628|4|Described|p3: 1, 4, 24, 48-51|||Brown (2003); previously Gostwyck Adamellite (Binns et al., 1967). Named after the parish of Gostwyck. Crops out 10 km E of Uralla and ~15 km S of Armidale. Pluton size is up to 6.5 x 4.5 km. Geochemistry described.|290 Ma (Rb-Sr biotite).|Gostwyck Suite.||Intrudes Sandon Association. Is overlain locally by Armidale beds.|Medium-grained biotite monzogranite; amphibole and pyroxene bearing variants; massive to weakly deformed. S-type.|
24299|Gourock Granodiorite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
24299|Gourock Granodiorite|40276|2|Defined|p15|Early Devonian|Early Devonian|||||||
24299|Gourock Granodiorite|42497|5|Briefly described|Map Legend|Zlichovian|Pragian|||||||
24299|Gourock Granodiorite|61818|5|Briefly described|p85|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
24299|Gourock Granodiorite|69270|4|Described|p2 Tb.1.1, p15, p20, p23, p27, p30-36|Late Silurian|Late Silurian|Goulburn Trough. Eastern Lachlan Orogen. The sample analysed was taken from roadside outcrop on northern side of Bald Peak Road in Tallaganda State Forest, and comprised strongly foliated, grey to cream, massive, medium- to coarse-grained hornblende-biotite granodiorite. Dating method: zircon U-Pb by SHRIMP, n=25. Previous dating: 373+/-6 Ma (K-Ar biotite age) and 380+/-6 Ma (biotite-whole rock Rb-Sr age), Wyborn and Owen (1986); affinity of Gourock Granodiorite to Early Devonian Glenbog Suite and Late Silurian Thurralilly Suite was not clear. SHRIMP analysis of Tinderry Granite (this volume) is indistinguishable from Gourock Granodiorite (this volume), and is also within error of ~425 Ma Kohinoor Volcanics of Hoskinstown Group (Fraser et al., in prep); much younger K-Ar and Rb-Sr ages of Wyborn and Owen (1986) reflect at least partial resetting of those isotopic systems, possibly during Carboniferous deformation; and, confirms its grouping with Thurralilly Suite (428-424 Ma: Bodorkos et al., 2010; Fitzherbert et al., 2011) along strike to the north (rather than Early Devonian Glenbog and Candello suites (413-410 Ma: Chen et al., 1990; Bodorkos and Simpson, 2008; Bodorkos et al., 2010) to east and west).|421.6+/-1.9 Ma, magmatic crystallisation||||granodiorite|
24299|Gourock Granodiorite|71069|4|Described|p28, p174, p175, p177-p179|Ludlow|Ludlow|Intrudes the Ordovician basement of the Goulburn Basin. Magmatic crystallisation age. Age from SHRIMP U-Pb, Chisholm et al, 2014. See also p189, p193, p194.|421.6 +/- 1.9 Ma |Thurralilly Suite||Equivalent to the Lockhart Igneous Complex and Ellenden Granite.|Grey to cream, massive, foliated, medium to coarse-grained hornblende-biotite granodiorite.|
25932|Govetts Leap Sandstone Member|31373|6|Mentioned|Table 1|||||||||
25932|Govetts Leap Sandstone Member|33683|6|Mentioned|Table 1|||Narrabeen Gp.||||||
25932|Govetts Leap Sandstone Member|33685|6|Mentioned|Table 2|||||||||
25932|Govetts Leap Sandstone Member|34205|2|Defined|p23|Triassic|Triassic|Caley Formation.||||||
25932|Govetts Leap Sandstone Member|34209|6|Mentioned|p141|||Table 1. Triassic.||||||
25932|Govetts Leap Sandstone Member|39293|5|Briefly described|p145|||||||||
25932|Govetts Leap Sandstone Member|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
25932|Govetts Leap Sandstone Member|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
25932|Govetts Leap Sandstone Member|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
73104|Gowan Brae monzogranite|62757|6|Mentioned|p16 Fig. 6|||See also "Gowan Brae monzogranite".||||||07-FEB-11
28211|Gowan Green Group|24126|6|Mentioned|p122|||||||||
28211|Gowan Green Group|32485|6|Mentioned|Map legend|Cambrian|Cambrian|Prob. Cambrian||||||
28211|Gowan Green Group|33611|6|Mentioned|p125|||||||||
28211|Gowan Green Group|43476|14|Not recorded|Map Legend||Cambrian|(Provisional Edition)||||||
82467|Graman Monzogranite|71628|4|Described|p4: 1, 3, 5, 20, 33-35|||New unit: unmodified from unpublished work by Chappell and Bryant (1994). Southern New England Orogen. Named after the locality or the parish in which it occurs. Approx. 63 km long (N-S) and up to 23 km wide; several satellite bodies. Geochemistry described and contrasted with Copeton Monzogranite. Associated with minor Au mineralisation.|288.6 +/- 2.9 Ma (SHRIMP: Rosenbaum et al., 2012).|Graman Suite.||Intrudes Texas beds. Is overlain by Pilliga Sandstone. Abuts Linton Monzogranite.|Coarse-grained, porphyritic biotite (+/- muscovite, +/- cordierite) monzogranite; locally cut by quartz tourmaline veins.|
81961|Grand High Tops Member|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Shawns Creek Formation|||Clast-supported polymictic volcaniclastic breccia; clasts of felsic coherent fragments and feldspar crystals, matrix formerly glass.|02-NOV-20
82469|Granite Hills Complex|71628|3|Fully described|p1:7; p15: 33, 79; p19: 58-72, 99|||New name (this study); previously known as Herries Adamellite/Herries Monzogranite/Herries Granite; and their rather complicated subdivisions are presented. Named after a local station. Comprises two bodies, 20 km SW of Warwick. Outcrop varies with constituent plutons. Type locality is 1.25 miles N of Braeside, from base to crest of the range (GR 498479) (Robertson, 1971). Geochemistry described. Various age determinations given. Is associated with very minor base metal mineralisation; has been a source of quarry materials.|c.256-247 Ma.||Clare Hills, Fairleigh, Herries, Palgrave Monzogranites.|Is faulted against Stanthorpe Complex. Is locally overlain by Marburg Formation.|Composite unit comprising pale pink to greyish pink, to grey, fine- to coarse-grained, slightly to moderately porphyritic, hornblende-biotite monzogranite. Mafic enclaves common. I-type.|
29590|Grants Corner Granodiorite|23214|3|Fully described|p157|Late Silurian|Late Silurian|Previously named Grants Corner Tonalite. Forms part of the Pine Mount Granodiorite of Stevens (1955) and the Pine Mount Intrusive Complex of Madsen (1970).  Intrudes Walli Volcanics. Geological Province: Wyangala Batholith||||||
29590|Grants Corner Granodiorite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of medium grained, slightly porphyritic, hornblende biotite granodiorite.||||||17-JUL-08
29590|Grants Corner Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyangla Batholith.||||||17-JUL-08
29590|Grants Corner Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|||Grants Corner Supersuite||||
31525|Grants Corner Suite|42726|5|Briefly described|map legend||Silurian|||||||
31524|Grants Corner Supersuite|42726|5|Briefly described|map legend|||||||||
31524|Grants Corner Supersuite|68592|6|Mentioned|p1318|||Brief comparison with Gunning Suite geochemistry.||||||
31524|Grants Corner Supersuite|70297|4|Described|map legend|Ludlow|Wenlock||||Padua Granodiorite, Grants Corner Granodiorite, Swan Ponds Tonalite||Unfractionated I-type equigranular to slightly porphyritic biotite-hornblende granodiorite; xenolith-rich porphyritic hornblende tonalite.|
76021|Grasmere Formation|66623|1|Redefined|pp74-75, p80 Fig. 21, pp85-87.  |Middle Cambrian|Middle Cambrian|Redefined; incorporates former Grasmere beds (Buckley 2000) and former Bendee beds (Stevens et al. 2000). Previously, portion of Wonnaminta beds (Warris 1967). No fossils identified. Extensively (thrust-)faulted. Prospective for VMS base metal mineralisation eg historic Grasmere Mine.||Unit in Ponto Group.||Overlies Weinteriga Formation. Is overlain by Noonthorangee Formation, separated by fine-grained porphyritic metabasalt of Bittles Tank Volcanics.|Sandy phyllite and meta-sandstone interbedded with felsic, laminated and cherty (airfall) tuff; and Bittles Tank Suite tholeiitic pillow lavas, basaltic flows, basalt and dolerite sills; quartz-magnetite rock.|
76021|Grasmere Formation|66918|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Ponto Group.||Map key suggests overlies Bittles Tank Volcanics.|Dominant magnetic mudstone (phyllite) and non-magnetic metasandstone, with lesser mafic phyllite and metamorphosed mafic volcanic members, minor laminated felsic tuff layers and quartz-magnetite beds.|25-SEP-13
76021|Grasmere Formation|67322|4|Described|p11, p39; Fig.5|Cambrian||Now includes the Bendee beds, part of the Palgamurtie Subgroup (obsolete) (Greenfield et al. 2010). Age determined from p20 Fig.5 (Strat. column) - not well constrained. Occurs in the Kayrunnera-Koonenberry region.||Of the Ponto Group.||Overlies Weinteriga Creek Formation. Is overlain by Noonthorangee Formation.|Phyllites with feldspathic tuff horizons, quartz-magnetite rocks and mafic units.|22-FEB-18
76021|Grasmere Formation|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|||Ponto Group|||Dominant magnetic metamudstone (phyllite) and non-magnetic metasandstone, with lesser mafic phyllite and metamorphosed mafic volcanic members, minor laminated felsic tuff layers and quartz-magnetite beds.|
76021|Grasmere Formation|70651|5|Briefly described|Map Legend|Cambrian|Cambrian|4 unnamed sub-units: Very fine-grained phyllite with lesser fine-grained sandy phyllite, intensely deformed. Fine- to medium-grained, massive to locally moderately deformed sandstone. Thin bands of very fine-grained massive to locally strongly banded/laminated, siliceous cherty tuff. Very fine-grained, well-banded to locally massive quartz and magnetite rock.||Ponto Group|Includes 4 unnamed sub-units.||Dominant magnetic metamudstone (phyllite) and non-magnetic metasandstone, with lesser mafic phyllite and metamorphosed mafic volcanic members, minor laminated felsic tuff layers and quartz-magnetite beds.|
82478|Grasstree Quartz Monzodiorite|71628|5|Briefly described|p17:5; p19: 72-74, 96|||Apparently a 'new' name for a unit identified as Pxg on the Grafton-Maclean 1:250,000 Metallogenic Sheet (Henley et al., 2001). The name may be invalid; [its proposed (yet another single-member) Suite certainly is, as Grasstree Suite is current in Queensland and has priority]. The unit's name is from a local watercourse. Occurs as several bodies ~24 km E and ESE of Sandy Flat. Geochemistry described. RELATED UNITS (continued): Is faulted against Dandahra Creek Leucosyenogranite, Sandon Association and Pi Pi Ignimbrite.||||Intrudes Drake Volcanics, Dundee Rhyodacite and Pheasant Creek Volcanics (Wandsworth Volcanic Group). Abuts Rocky River Monzogranite. See COMMENTS for more.|Pale grey to pinkish grey, very fine-grained, highly porphyritic biotite-hornblende quartz monzodiorite. A-type (tentative).|
75931|Grassy Gully Rhyolite Member|66300|5|Briefly described|p52, pp70-75.|Late Devonian|Late Devonian|This age is indistinguishable from that of Tullyangela Granite, indicating at least local exposure of plutonic equivalents of the Late Devonian volcanic succession in southern MOSS VALE area.|384.5 +/- 4.4 Ma.|Unit in Yalwal Volcanics.||Intruded by Bundundah Granite.|Cream-coloured, almost aphyric, extensively-sericitised rhyolite.|
75931|Grassy Gully Rhyolite Member|70661|3|Fully described|vii, viii, p6, p95, p96 fig 7|Frasnian|Middle Devonian|Temporally associated with the Tullyangela Granite. Named after grassy gully tributary of the Shoalhaven River. Previously termed Grassy Gully rhyolite or Grassy Gully Rhyolite, now demoted to member status. Distribution, depositional environment, metamorphism, geochemistry discussed. Lithology discussed in further detail. Hosts some gold deposits. Age from SHRIMP U-Pb, Bodorkos et al 2010). See also p101-p105, p245.|384.5 +/- 4.4 Ma |Yalwal Volcanics|||Flow banded, grey-pink fine grained, weakly porphyritic, spherulitic rhyolite. Phenocrysts include feldspar (altered to sericite) biotite, rare quartz and accessory zircon.|
75931|Grassy Gully Rhyolite Member|71303|5|Briefly described|map legend|Givetian|Givetian|||Of Yalwal Volcanics.|||Grey to pink, weakly porphyritic, locally spherulitic, flow-banded rhyolite, rhyolitic breccia; sericitised, silicified locally. Intercalated with sedimentary rocks and basalt.|
73425|Gravel Creek Member|66623|2|Defined|p12, p19, pp24-25.|||Newly defined. Outcrop is one continuous ridge west of Mount Arrowsmith. 264 m thick. Forms bare, moderate hills. Formerly part of Torrowangee Series (Mawson 1912), Wonominta beds (Warris 1964), Kara beds (Mills 1992), and herein part of Grey Range Group.||Unit in Kara Formation.|||Thickly-bedded sequence of dark-grey slate and calcareous psammite, overlain by lithic-feldspathic psammite; regionally metamorphosed to greenschist facies.|
73425|Gravel Creek Member|66917|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Basal unit in Kara Formation.|||A thickly-bedded sequence of dark grey slate and calcareous psammite, overlain by lithic-feldspathic psammite, originally mudstone and sandstone; regionally metamorphosed to greenschist facies.|
73425|Gravel Creek Member|67208|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Basal unit in Kara Formation.|||A thickly-bedded sequence of dark grey slate and calcareous metasandstone to impure limestone, overlain by lithic-feldspathic metasandstone; originally mudstone and sandstone.|
79339|Greengrove mafic intrusion|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|Included in general description for Unassigned mafic intrusions (Ben Bullen Igneous Complex and Greengrove mafic intrusion).|||||Small plutons of hornblende diorite, gabbro and dolerite. Irregular areas of olivine norite, and gabbroic anorthosite. Rare limestone blocks xenoliths at Ben Bullen.|19-MAY-16
29670|Greenslopes Porphyry|23214|4|Described|p175|Devonian|Silurian|Intrudes the Adaminaby Group and Rockley Volcanics.  Is a pink massive porphyry.||||||
29670|Greenslopes Porphyry|43639|5|Briefly described|Map Legend||Silurian|||||||
29670|Greenslopes Porphyry|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|||||||
29670|Greenslopes Porphyry|67847|6|Mentioned|p28|Devonian|Silurian|||||Intrudes the Triangle Formation and the Rockley Volcanics.||
29670|Greenslopes Porphyry|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Wologorong Supersuite||||
73424|Grey Range Group|66623|2|Defined|p v, pp12-29. |Late Neoproterozoic|Late Neoproterozoic|Defined in this study. About 5 km thick. Oldest rocks in the Koonenberry Belt area. Correlated with Farnell Group. Geophysical properties described. Formerly Torrowangee Series (Mawson 1912), Wonominta beds (Warris 1967), then Kara beds (Mills 1992).|||Includes Mount Arrowsmith Volcanics and Kara Formation.|Overlies Torrowangee Group. Is overlain by Nundora Formation of Teltawongee Group. Intruded by Bittles Tank Volcanics.|Shallow marine continental shelf sequence: metamorphosed mudstone, siltstone and well-sorted quartzose sandstone; minor dolomitic and calcareous beds. Interfingers with Mount Arrowsmith Volcanics.|
73424|Grey Range Group|66917|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Several un-named units are mapped separately.|||Includes Mount Arrowsmith Volcanics and Kara Formation.|||
73424|Grey Range Group|66918|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||Includes Mount Arrowsmith Volcanics and Kara Formation.|||
73424|Grey Range Group|66927|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
73424|Grey Range Group|67105|5|Briefly described|p651, 653-655, 661, 663|Ediacaran|Ediacaran|Koonenberry Belt.|||Kara Formation, Mount Arrowsmith Volcanics.|Equivalent to Farnell Group.|Metasedimentary (shallow marine) rocks including a series of laminated to cross-bedded feldspathic sandstone, and dominantly basaltic submarine lavas and related intrusives.|
73424|Grey Range Group|67207|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Includes Kara Formation and Mount Arrowsmith Volcanics.|Is overlain by Teltawongee Group.||
73424|Grey Range Group|67208|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Includes Kara Formation and Mount Arrowsmith Volcanics.|||
73424|Grey Range Group|67211|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Includes Kara Formation.|||
73424|Grey Range Group|67322|6|Mentioned|p11, p39|Neoproterozoic|Neoproterozoic|||||Intruded by the Bittles Tank Volcanics.||
73424|Grey Range Group|69961|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||Includes Kara Formation and Mount Arrowsmith Volcanics.|||
73424|Grey Range Group|70648|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic||||Includes Mount Arrowsmith Volcanics, Kara Formation.|||
73424|Grey Range Group|70650|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic||||Includes Mount Arrowsmith Volcanics, Kara Formation.|Intruded by diorite of Bittles Tank Formation.||
73424|Grey Range Group|70651|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic||||Includes Kara Formation.|||
73424|Grey Range Group|70744|5|Briefly described|p940|Neoproterozoic|Neoproterozoic|Koonenberry Belt. Late Neoproterozoic. Interpreted by Greenfield et al. (2010, 2011) as part of a rifted passive margin succession.|||||A thick succession of shallow-marine quartzose siliciclastics, minor carbonate and interbedded mafic volcanic rocks.|
73424|Grey Range Group|70749|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Southern Thomson and Koonenberry area.||||||
73424|Grey Range Group|70838|5|Briefly described|p268-272, p274, p276-278, p280-281|Ediacaran|Ediacaran|Possible tectonic settings discussed. Sedimentology and geochemistry suggest a continental (shallow-marine) rift setting for deposition of this Group. Deformed during the Delamerian Orogeny (c.500 Ma). Detrital zircon analyses: quartz-rich and cratonic source aged 1.3-1.0 Ga.|||Kara Formation, Mount Arrowsmith Volcanics.|Is faulted against Teltawongee, Gnalta and Ponto Groups.||
73424|Grey Range Group|71415|5|Briefly described|p10,15|Neoproterozoic|Neoproterozoic|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.|||Includes Mount Arrowsmith Volcanics.|Overlain by the Teltawongee Group and Ponto Group.||19-AUG-19
73424|Grey Range Group|71965|6|Mentioned|p894|Neoproterozoic|Neoproterozoic|Geological province: Koonenberry Belt, Delamerian Orogen. Record rifting and passive margin sedimentation.||||||
73424|Grey Range Group|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: southern Thomson Orogen.||||||
73424|Grey Range Group|72461|6|Mentioned|p19|Neoproterozoic|Neoproterozoic|Koonenberry Belt.||||||
73424|Grey Range Group|73177|5|Briefly described|p1098, 1114-1115 Figs.16-17|Neoproterozoic|Neoproterozoic|Delamerian Orogen.|||Mount Arrowsmith Volcanics, Kara Formation.||Metasedimentary rocks.|
73424|Grey Range Group|74367|6|Mentioned|p18|||Interpreted as the stratigraphic equivalent of the Farnell Group.|||Kara Formation|||
73901|Greymare Suite|63748|6|Mentioned|p28|Early Triassic|Permian|Includes the Greymare Granite.||||||07-FEB-11
73901|Greymare Suite|68679|5|Briefly described|p457, p464|Permian|Permian|Northern New England Batholith.|~280 Ma.|Clarence River Supersuite.|Greymare Granodiorite.|||
73901|Greymare Suite|71628|5|Briefly described|p18: 10|||||Greymare Supersuite.|Greymare Tonalite.|||
73900|Greymare Supersuite|63748|6|Mentioned|p28|Early Triassic|Permian|Includes the Greymare Suite.||||||07-FEB-11
73900|Greymare Supersuite|71628|5|Briefly described|p18: 1, 10||||||Greymare Suite.||I-type.|
25032|Grong Grong Granite|22508|5|Briefly described|p3||Silurian| Keotong Supersuite, Lachlan Fold Belt||||||
25032|Grong Grong Granite|32676|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
25032|Grong Grong Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
25032|Grong Grong Granite|36316|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
25032|Grong Grong Granite|40328|4|Described|p206|||||||||
25032|Grong Grong Granite|42726|5|Briefly described|map legend|Silurian||||||||
25032|Grong Grong Granite|69801|5|Briefly described|p1, p4-p5, p32-37, p135-136|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs between Junee and Narrandera; outcrop is generally poor. Sample locality, petrography, SHRIMP analyses and interpretation are detailed. Together with the Ganmain Granite confirms the presence of Koetong Supersuite granites between Junee and Narrandera.|430.6 +/- 1.8 Ma|Koetong Suite||Intrudes the Wagga Group.|Medium to coarse-grained, sparsely porphyritic, leucocratic, muscovite-biotite granite with some tourmaline.|
25032|Grong Grong Granite|71364|5|Briefly described|p5, p10|Silurian|Silurian|Wynn (1960).|||||Medium-grained, muscovite-biotite granite..|15-FEB-18
25032|Grong Grong Granite|71365|5|Briefly described|map legend|||Silurian?|||||Biotite granite.|15-FEB-18
25032|Grong Grong Granite|71889|5|Briefly described|p7, p22-p23|Silurian|Silurian|Interpreted to underlie much of the town of Grong Grong on the basis of new information gathered during road works, which shifted its boundary 1km to the southwest of the town.|||||S-type fesic granite.|
25032|Grong Grong Granite|72083|5|Briefly described|p9, p17-18, p40 Fig.6, p58 Fig.9|||Trigg (2016). Further exposures mapped around the N and W edges of Grong Grong township and along the Newell Highway.|||||Mostly medium-grained, muscovite-biotite granite; local rare to abundant biotite-rich (?)enclaves to 12cm in size; generally equigranular, local phenocrysts of feldspar to 2cm. Felsic, S-type.|
26595|Grose Subgroup|22447|4|Described|p624, Fig.1 p624||Early Triassic|Fluvial quartz to quartz-lithic||||||
26595|Grose Subgroup|22857|5|Briefly described|p526 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Narrabeen Group: includes the Banks Wall Sandstone, Mount York Claystone, Burra-Moko Head Sandstone and Caley Formation. Geological Province: Sydney Basin.||||||
26595|Grose Subgroup|22969|5|Briefly described|Fig 2.2||Early Triassic|||||||
26595|Grose Subgroup|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
26595|Grose Subgroup|31061|6|Mentioned|Table 1|||See also P1318||||||
26595|Grose Subgroup|31725|6|Mentioned|Table|||P10||||||
26595|Grose Subgroup|31886|6|Mentioned|Table 1|||||||||
26595|Grose Subgroup|42925|4|Described|p11, Table 1|||of Narrabeen Group||||||
26595|Grose Subgroup|42926|4|Described|map legend|Early Triassic|Late Permian|||||||
26595|Grose Subgroup|60281|5|Briefly described|Fig. 7 Appendix 1|Middle Triassic|Early Triassic|Of the Narrabeen Group.  Age: >240Ma.  Geological Province: Sydney Basin.||||||
26595|Grose Subgroup|61315|5|Briefly described|Table SY2|Early Triassic|Early Triassic|Of the Narrabeen Group. Geological Province: Sydney Basin||||||
26595|Grose Subgroup|69297|6|Mentioned|p501|Anisian|Olenekian|Sydney Basin. ||Narrabeen Group||Overlies the Caley Subgroup. Overlain by the Burralow Formation.||
28190|Grosses Plain Tonalite|22815|4|Described|p49|Early Devonian|Late Silurian|||||||
28190|Grosses Plain Tonalite|35263|6|Mentioned|Table.3|||||||||
28190|Grosses Plain Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
28190|Grosses Plain Tonalite|41563|6|Mentioned|p506|||||||||
28190|Grosses Plain Tonalite|41898|6|Mentioned|p1184|||||||||
28190|Grosses Plain Tonalite|41905|2|Defined|p92|Silurian||||||||
28190|Grosses Plain Tonalite|41933|5|Briefly described|Map legend|Late Silurian||||||||
28190|Grosses Plain Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Jindabyne Suite.||||||
28190|Grosses Plain Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh17||||||
28190|Grosses Plain Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
25936|Guapa Tank Rhyodacite Member|22857|5|Briefly described|p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Burthong Formation (Mouramba Group, Cobar Supergroup). Max. thickness: 900m. Geological Province: Mouramba Shelf. See also p440, App.1, Tb.A1.6.||||||
25936|Guapa Tank Rhyodacite Member|41394|2|Defined|p56|Early Devonian||Reserved as Guapa Tank Volcanic Member||||||
25936|Guapa Tank Rhyodacite Member|41395|6|Mentioned|Map legend|Lochkovian||||||||
25936|Guapa Tank Rhyodacite Member|41528|2|Defined|p67|Early Devonian||||||||
25936|Guapa Tank Rhyodacite Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
27790|Gulf Siltstone-Argillite Formation|38915|4|Described|p335|||||||||
27790|Gulf Siltstone-Argillite Formation|71628|6|Mentioned|p8: 86-87|||||||Is Intruded by Hell Hole Monzogranite. Abuts Emmaville Volcanics.||
82480|Gulf Station Leucosyenogranite|71628|5|Briefly described|p3:71; p19: 74-76|||New name (this study). First documented by Sturmfels (1971, unpublished). A very small ( 1 km2) intrusion about 28 km NW of Ebor. Crops out as low angular blocks and boulders. Named after a local creek. E of the Wongwibinda Fault. Geochemistry described.||Gulf Station Suite.||Intrudes ?Dyamberin beds. Is partly overlain by Doughboy Basalt.|Fine- to medium-grained biotite leucosyenogranite. Has undergone deformation, annealing, pervasive alteration, and is strongly jointed.|
31452|Gulgong Suite|42726|5|Briefly described|Map legend||Carboniferous|Of the Bathurst Supersuite.  Contains Gulgong, Havilah, Mudgee River and Wiagdon Granites.||||||07-FEB-05
31452|Gulgong Suite|44093|5|Briefly described|p211 App. 1|Late Carboniferous|Early Carboniferous| Geological Province: Lachlan Fold Belt.||||||
76156|Gum Creek Member|66623|2|Defined|p193, pp222-223.|Givetian|Givetian|As distinct from Gum Creek Basalt. Named as Gum Creek beds by Neef and Larsen (2003); defined in this study. Menamurtee Hills area. One of three contemporaneous basal units of Ravendale Formation; correlated with Turkaro Range Conglomerate Member and Rocky Tank Conglomerate Member. Interpreted to have formed from Tabberabberan uplift and erosion of Menamurtee Sandstone.||Basal unit in Ravendale Formation.||Overlies unconformably the Menamurtee Sandstone of the Wana Karnu Group.|Medium-grained quartzose sandstone similar to the Menamurtee Sandstone, and distinct from overlying white to buff planar-laminated and cross-bedded fluvial quartzose sandstones of undifferentiated Ravendale Formation.|
76156|Gum Creek Member|70651|5|Briefly described|Map Legend|Devonian|Devonian|||Ravendale Formation|||Medium-grained quartzose sandstone.
|
68693|Gum Vale beds|22857|6|Mentioned|p295, p544 App.1 Tb.A1.12|Early Cretaceous|Early Cretaceous|Known as Cadna-owie Formation outside the Tibooburra area. ||||||
68693|Gum Vale beds|44093|6|Mentioned|p68 (photo)|||Associated with Rolling Downs Group.||||||07-APR-05
68693|Gum Vale beds|66623|6|Mentioned|p449.|Neocomian|Neocomian|Formerly Gum Vale Beds. Equivalent to Cadna-owie Formation. A microfloral assemblage obtained from Wydjah well, near Mount Arrowsmith, was assigned (McMinn 1981) to the Foraminisporis wonthaggiensis subzone of Burger (1973) and Morgan (1980).||||||
68693|Gum Vale beds|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
39365|Gum Valley Volcanics|24123|5|Briefly described|p3|Devonian|Devonian|Geological Province: Sydney Basin.||||||
28254|Gumbardo Formation|22464|6|Mentioned|p9||Early Devonian|Adavale Basin. Overlain by Eastwood Beds||||||
28254|Gumbardo Formation|22518|6|Mentioned|p 10|||||||||
28254|Gumbardo Formation|22604|6|Mentioned|p442|||||||||
28254|Gumbardo Formation|22857|6|Mentioned|p201|||Andesite. Geological Province: Avadale Basin. ||||||
28254|Gumbardo Formation|22859|6|Mentioned|p201|||||||||
28254|Gumbardo Formation|23522|5|Briefly described|p250 Fig 6|Emsian||||||||
28254|Gumbardo Formation|23834|4|Described|p312|Emsian|Emsian| Geological Province: Adavale Basin. Maximum thickness: >43m.||||||
28254|Gumbardo Formation|29387|6|Mentioned|Table 1|||Refers to Galloway(1970). Lower Devonian.||||||
28254|Gumbardo Formation|29393|6|Mentioned|Table 1|||Lower Devonian.||||||
28254|Gumbardo Formation|29721|6|Mentioned|Table 38|||||||||
28254|Gumbardo Formation|30103|4|Described|p5|||Table 2 on p5. See also p6.||||||20-NOV-08
28254|Gumbardo Formation|30104|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|30544|6|Mentioned|Fig.5 P51|||Devonian||||||
28254|Gumbardo Formation|30691|4|Described|p7|||See also Table 6. Middle Devonian age||||||
28254|Gumbardo Formation|30853|1|Redefined|p27|Middle Devonian|Middle Devonian|See also Table 2.||||||
28254|Gumbardo Formation|30854|4|Described|Table 2|||Middle Devonian age||||||
28254|Gumbardo Formation|30855|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|31999|5|Briefly described|Table 1|||||||||
28254|Gumbardo Formation|32619|6|Mentioned|p462|||L.Dev.||||||
28254|Gumbardo Formation|33069|4|Described|p6|||Middle Devonian.||||||22-DEC-09
28254|Gumbardo Formation|33078|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|33079|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|33087|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||22-DEC-09
28254|Gumbardo Formation|33088|4|Described|Table 2|||Of the Adavale Group.||||||20-NOV-08
28254|Gumbardo Formation|33092|5|Briefly described|p5|||Stratigraphy||||||
28254|Gumbardo Formation|33326|6|Mentioned|p447|||Fauna.||||||
28254|Gumbardo Formation|33641|6|Mentioned|p59|||L.Dev.||||||
28254|Gumbardo Formation|33732|6|Mentioned|p103|||Emsian.||||||
28254|Gumbardo Formation|34065|4|Described|p7|||Middle Devonian.||||||20-NOV-08
28254|Gumbardo Formation|34217|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|34218|4|Described|Table 1|||See also Table 2, p8. Middle Devonian.||||||20-NOV-08
28254|Gumbardo Formation|37565|6|Mentioned|Fig.6|||||||||
28254|Gumbardo Formation|38226|6|Mentioned|p414|||||||||
28254|Gumbardo Formation|39445|5|Briefly described|Table 5|||See also p73.||||||20-NOV-08
28254|Gumbardo Formation|39478|6|Mentioned|Table 1|||||||||
28254|Gumbardo Formation|39480|6|Mentioned|p188|||||||||
28254|Gumbardo Formation|40762|6|Mentioned|p282|||||||||
28254|Gumbardo Formation|40787|6|Mentioned|p340|||||||||
28254|Gumbardo Formation|41097|6|Mentioned|Table 1|||||||||
28254|Gumbardo Formation|41167|6|Mentioned|p398|||||||||
28254|Gumbardo Formation|41198|5|Briefly described|p35|||Mention Table 1||||||
28254|Gumbardo Formation|41208|6|Mentioned|Fig.1|||||||||
28254|Gumbardo Formation|41289|6|Mentioned|p209|||||||||
28254|Gumbardo Formation|42031|5|Briefly described|Fig.8 P766|||||||||
28254|Gumbardo Formation|42999|5|Briefly described|p87,Table1.p90|||||||||
28254|Gumbardo Formation|43004|5|Briefly described|Table 1,p179|||||||||
28254|Gumbardo Formation|43008|5|Briefly described|map legend|||||||||
28254|Gumbardo Formation|43105|5|Briefly described|p11|||||||||
28254|Gumbardo Formation|43213|5|Briefly described|p93|Emsian|Emsian|Adavale Basin.||||Is overlain by Eastwood beds.|Continental felsic to mafic volcanics.|
28254|Gumbardo Formation|43461|14|Not recorded|p617,table p618||Early Devonian|||||||
28254|Gumbardo Formation|43914|14|Not recorded|p3,Fig.3|||K-Ar: 380 Ma.||||||
28254|Gumbardo Formation|44770|14|Not recorded|p111,diag.p113,114|||Part of Adavale Group.||||||
28254|Gumbardo Formation|44851|14|Not recorded|p172||Middle Devonian|Part of Adavale Group.||||||
28254|Gumbardo Formation|44888|14|Not recorded|p32|||||||||
28254|Gumbardo Formation|44889|14|Not recorded|p160||Silurian|K/Ar = Middle Devonian||||||
28254|Gumbardo Formation|46881|6|Mentioned|Table.1|||See also Table.2||||||
28254|Gumbardo Formation|48920|6|Mentioned|Fig.2|||See also Table 3||||||
28254|Gumbardo Formation|64783|1|Redefined|p88-91, p82, p84-87,92-94, 100, 103, 104|Emsian|Pragian|First named by Phillips Petroleum Company (1963) in PPC Gumbardo-1, and defined by them in 1964; the reference section being 3167.8 to 3912.1 m.  Redefined here as the section between 3148.5 and 3904 m, to exclude Ordovician volcanic rocks. Galloway (1970) included in the Formation the eastern-margin arkosic and labile arenites. Basal unit in Adavale Basin. Pragian to early-mid Emsian.|408.3 +/- 2.4 Ma and 401-8 +/- 2.1 Ma.|||Is unconformably overlain by Eastwood beds, Log Creek Formation or Etonvale Formation.|Includes volcanic and volcaniclastic rocks including arkosic and litho-feldspathic labile sandstones, and acidic volcanics (crystal tuffs and ignimbrite) with minor mafics.|15-NOV-17
28254|Gumbardo Formation|65214|6|Mentioned|p275|Devonian|Devonian|QLD, Adavale. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
28254|Gumbardo Formation|65756|5|Briefly described|p27|Early Devonian|Early Devonian|||||||
28254|Gumbardo Formation|67402|5|Briefly described|p165 tbl LPB1, p167|Emsian|Pragian|Adavale Basin. Deposited as fluvio-lacustrine rift infill continental sediments. See also p168 tbl ADV/WRR1, p170, fig ADV/WRR8, p172, p173, p175.||||Overlain by the Eastwood beds.|Andesitic basalt, rhyolite, trachyandesite and volcaniclastic arkosic and litho-feldspathic labile sandstones becoming more silty/muddy towards the northeast of the basin.|
28254|Gumbardo Formation|68731|5|Briefly described|p164, p174, p179, pp180-181 Tb 3.3|Early Devonian|Early Devonian|Adavale Basin. Evans et al. (1990), de Boer (1996), and Boreham and De Boer, (1998). Between 25.6-755.5 m thick. Suggested fluvial and perhaps fluvio-lacustrine depositional environment.|402 +/- 2 Ma; 408 +/- 4 Ma (McKillop et al. 2007)|||Unconformably overlain by the Log Creek Formation.|Comprises volcanic and volcaniclastic rocks. Volcaniclastics are feldspathic and lithofeldspathic labile sandstones. Volcanic rocks are mainly acidic, although there are some mafic volcanic rocks.|
28254|Gumbardo Formation|69541|5|Briefly described|p645 Fig.1(b), p654|Emsian|Pragian|Thomson Orogen. Oldest unit in the Adavale Basin. Subsurface.||||Is overlain by Eastwood beds.|Volcanic and volcaniclastic rocks.|
28254|Gumbardo Formation|70744|5|Briefly described|p939|Early Devonian|Early Devonian|Thomson Orogen basement (QLD).|c.409 Ma (estimated from Fig.7).|||||
28254|Gumbardo Formation|70823|5|Briefly described|p33|Devonian|Silurian|Cooper Basin.||||||
28254|Gumbardo Formation|71965|6|Mentioned|p913-914|Devonian|Devonian|Of Adavale Basin.||||||
28254|Gumbardo Formation|71966|5|Briefly described|p989,991,997,1000,1002|Early Devonian|Early Devonian|Of Adavale Basin. Volcanism associated with the opening of the Adavale Basin as a result of 408-403 Ma extension. Intersected in drillholes PPC Carlow 1 and PPC Gumbardo 1, and sample of rhyolitic ignimbrite analysed for SHRIMP U-Pb geochronology, and Lu and Hf isotopic analysis. Sample 1682891 yielded a 206Pb/238U age of 408.1+\-3.1 Ma, interpreted as the eruptive age of ths sample. Sample 1682892 yielded a weighted mean 206Pb/238U age of 402.9+\-2.9 Ma, interpreted as crystallisation age of the rock. SHRIMP U-Pb ages constrain the lower age and initial phases of basin opening to approximately Pragian (Draper 2006). Contains c. 475 ma inherited zircons, derived from local volcanic or plutonic source that was mixed into the ignimbirite during eruption or later phase of magmatic evolution. Hf and O isotope analysis indication derivation from a more juvelie source than Silurian granites.|||||Volcanic and volcaniclastic rocks including rhyolitic ignimbrite.|25-OCT-19
28254|Gumbardo Formation|72522|6|Mentioned|p1.|Early Devonian|Early Devonian|Located in the Adavale Basin c. 200km north of the central Thomson Orogen. Age of ignimbrites in this unit stated to be indistinguishable from Maximum depositional age of volcaniclastic sandstone in Paka Tank Trough (398+/-3 Ma).|||||Includes ignimbrites.|
28254|Gumbardo Formation|73179|4|Described|p1133, p1136-1143, p1147-1156|Emsian|Pragian|Adavale Basin. Deposited in a half-graben system that appears to be confined to a NNE-SSW-trending rift corridor. Found in the main depocentre of the basin and may extend [at depth] to the Warrabin and Quilpie troughs based on seismic interpretations. Used as a seismic marker horizon.  Maximum thickness: 755.5 m. Geochron are previously published SHRIMP ages, which are reportedly slightly older than new LA-ICP-MS ages.  [Article includes detailed thin section petrography, a series of new U-Pb LA-ICP-MS ages and whole-rock geochemistry]. Epiclastic sedimentary rocks both underlie and overlie volcanic units. Ignimbrites are interpreted as an outflow facies [relatively distal from source]. Similar ages for ignimbrites suggest short-lived volcanism at the initiation of the basin opening. Has inherited zircons but lacks inherited ages between 600 and 500 Ma, which is a prominent detrital zircon age in metasedimentary rocks of the Thomson Orogen; [thus,] little to no contribution of metasedimentary rocks in the petrogenesis of this unit. Volcanics have transitional I- to A-type affinities.|402.9 +/- 2.9 Ma, 408.1 +/- 3.1 Ma|||Unconformably overlain by Eastwood Beds.|Dominantly crystal-rich dacitic and rhyolitic ignimbrites with porphyritic rhyolite and rhyodacite, tuff, very fine- to coarse-grained sandstone, pelitic sandstone and epiclastic sandstone (lithic arkose - arkose). [+/- andesite and andesitic tuff].|19-SEP-22
28254|Gumbardo Formation|73307|5|Briefly described|p585|||Basal unit in Adavale Basin.|c.410 Ma (Draper, 2006).||||Fluvial sedimentation followed by a marine incursion resulting in mixed carbonate-siliciclastic deposition.|
82355|Gummi Plain Granodiorite|71628|4|Described|p6: 2-9, 12, 18-21, 23-25; p9-1|||New name, after the Gummi Plain pluton of Mason and Kavalieris (1984). One of three units that replaced Barrington Tops Granodiorite, in Bryant et al. (2003), after unpublished work by Chappell and Bryant (1994). Named after a local geographic feature. Crops out in Barrington Tops area, ~40 km W of Gloucester. Forms tors. Several other age determinations given and discussed. Geochemistry described.|267.8 +/- 1.4 Ma (Waltenberg et al., 2015).|Gummi Plain Suite.||Intrudes Tamworth, Parry and Manning Groups.|Black and white speckled to waxy, medium-grained hornblende-biotite-(pyroxene) granodiorite to tonalite; strongly altered, finer-grained, porphyritic marginal variant.|
26597|Gums Road Limestone Member|22857|4|Described|p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Silverdale Formation. Fossiliferous intrasparrudite, pelsparrudite, biomicrite, shale. Max. thickness: 23.7m. Geological Province: Canberra-Yass Shelf. ||||||
26597|Gums Road Limestone Member|24248|5|Briefly described|p54|Gorstian|Gorstian|Of the Silverdale Formation.||||||02-JUN-08
26597|Gums Road Limestone Member|30069|6|Mentioned|p9|||Table on P9||||||
26597|Gums Road Limestone Member|31852|6|Mentioned|p711|||Ludlovian. See also Figs. 1,2,4,5.||||||
26597|Gums Road Limestone Member|33116|6|Mentioned|Fig.11|||Correlation. Mb. Silverdale Fm.||||||
26597|Gums Road Limestone Member|34692|6|Mentioned|p186|||||||||
26597|Gums Road Limestone Member|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
26597|Gums Road Limestone Member|35386|3|Fully described|p27|||Part of Silverdale Formation||||||
26597|Gums Road Limestone Member|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
26597|Gums Road Limestone Member|37727|6|Mentioned|p85|||||||||
26597|Gums Road Limestone Member|39331|6|Mentioned|Fig.5-5|||||||||
26597|Gums Road Limestone Member|40328|4|Described|p110|||Also mentioned on p108.||||||02-JUN-08
26597|Gums Road Limestone Member|45075|5|Briefly described|p6|||Fauna||||||
26597|Gums Road Limestone Member|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Yanawe Formation (Douro Group).  Lies within an unnamed unit (Sdwc) of the Yanawe Formation underlying the basal Bowspring Limestone Member of Hattons Corner Group||||||
26597|Gums Road Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yanawe Formation (Douro Group).  Crinoidal stromatoporoid intrasparudites and coral pelsarrudites containing fragmental rugose and tabulate corals and stromatoporoids.||||||02-JUN-08
26597|Gums Road Limestone Member|68592|2|Defined|p430 Fig.89, p434-6, p441, p515, p523-58|Ludlow|Ludlow|See also p239, p1877. Link (1970, 1971) named this unit in his Silverdale Formation. Here transferred from Silverdale Formation (Hattons Corner Group) to Yanawe Formation (Douro Group). Type section described. 3-24m thick. Contains uneconomic limestone deposits. Contains abundant and diverse faunas. Early Ludlow age inferred from stratigraphic relationships.||Unit in Yanawe Formation.||Conformably overlies Excursion Creek Sandstone Member. Is overlain gradationally by Tullerah Sandstone Member.|Biomicrites, stromatoporoidal limestone, intrasparrudite, semi-nodular limestone with shale partings, conglomerate composed of rounded micrite cobbles and pebbles in a shaly matrix.|
26597|Gums Road Limestone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdwg[asterisk]. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Yanawe Formation||Is overlain by Tullerah Sandstone Member. Overlies Excurison Creek Sandstone Member.|Fossiliferous massive-bedded limestone (biomicrite, intrasparrudite, pelsparrudite, biomicrudite), quartzose biomicrudite, clayey biomcrite, shale partings and conglomerate.|
26597|Gums Road Limestone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Fossiliferous massive-bedded limestone (biomicrite, intrasparrudite, pelsparrudite, biomicrudite), quartzose biomicrudite, clayey biomcrite, shale partings and conglomerate.|
26597|Gums Road Limestone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Fossiliferous massive to bedded limestone (biomicrite, intrasparrudite, pelsparrudite and biomicrudite) quartzose biomicrite, clayey biomicrite, shale partings, conglomerate.|
26597|Gums Road Limestone Member|71656|6|Mentioned|p23|Silurian|Silurian|Not shown in correlation chart (Fig.2).||Yanawe Formation, Douro Group||Douro Group. Yanawe Formation.|Fossiliferous strata.|
27162|Gundagai Serpentinite|22638|1|Redefined|p13|Early Ordovician||Jindalee Group. ?Cambro- Early Ordovician||||||
27162|Gundagai Serpentinite|24215|5|Briefly described|p801|||Parent: Jindalee Group.    Geological Province:  Lachlan Fold Belt||||||
27162|Gundagai Serpentinite|35070|2|Defined|p25|Early Ordovician|Cambrian|Cambrian to Early Ordovician||||||
27162|Gundagai Serpentinite|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27162|Gundagai Serpentinite|36411|6|Mentioned|p269|||Refers Basden et al 1978 for definition.||||||
27162|Gundagai Serpentinite|37529|6|Mentioned|p4|||||||||
27162|Gundagai Serpentinite|40328|6|Mentioned|p41|||||||||
27162|Gundagai Serpentinite|40498|6|Mentioned|p417|||||||||
27162|Gundagai Serpentinite|42313|3|Fully described|p22|||||||||
27162|Gundagai Serpentinite|42314|5|Briefly described|Map|Cambrian||||||||
27162|Gundagai Serpentinite|44192|5|Briefly described|Map Legend|Early Ordovician|Cambrian|||||||
27162|Gundagai Serpentinite|67322|6|Mentioned|p20|Pridoli|Ludlow|Age constrained by that of the parent Jindalee Group: an Ordovician fragmented ophiolite sequence within a Silurian sedimentary matrix. On Tumut 1:100 000 and Cootamundra 1:250 000 sheets (Warren et al. 1995).||Of the Jindalee Group||||
27162|Gundagai Serpentinite|71708|6|Mentioned|p336 Fig 1, p345, p351|||Includes tonalitic clasts, supporting allochthonous origin for Edwardstown Tonalite, in Jackalass Slate. Interpreted to have belonged to a larger ultramafic massif called the Tumut Serpentinite Province by Graham (2000).||Potentially a satellite body of the Coolac Serpentinite|||Serpentine melange.|31-MAR-20
27162|Gundagai Serpentinite|73082|6|Mentioned|p16|||Gundagai area.|||||Contains auriferous quartz (+/- calcite, talc) veins.|
27162|Gundagai Serpentinite|73483|5|Briefly described|p407 Fig.1, p408-409|Ordovician|Cambrian|Also referred to as Gundagai Serpentinite Belt p407. Inferred Cambro-Ordovician age based on association with Jindalee Group.||Jindalee Group|||Serpentinite melange with tonalitic clasts.|
73406|Gundara Quartzite Member|62795|5|Briefly described|p347|Middle Ordovician|Middle Ordovician|Unit in Rowena Formation of Mutawintji Group. Planar- and cross-bedded quartzite with distinctive angular vein-quartz conglomerate, pebble bands and trace fossils including Skolithos.||||||
73406|Gundara Quartzite Member|64679|5|Briefly described|Map legend|Ordovician|Late Cambrian|Of the Rowena Formation (Mutawintji Group). Buff to white, planar- and cross-bedded quartzite with distinctive angular vein-quartz conglomerate, pebble bands and trace fossils.||||||16-FEB-09
73406|Gundara Quartzite Member|66623|2|Defined|pp134-138, pp147-150.|Early Ordovician|Early Ordovician|Mapped, named but not defined by Sharp (2004). Defined in this study. Forms prominent outcrop strike ridges. Maximum thickness c.500 m. Contains trace fossil Skolithos, and cross-bedding. Represents change from fluvial to marginal marine conditions with a large deltaic fan.||Unit in Rowena Formation.||Conformable within Rowena Formation.|Distinctive angular vein-quartz pebbly sandstone or conglomerate and quartzite.|
73406|Gundara Quartzite Member|67322|5|Briefly described|p9; Fig.5|Dapingian|Dapingian|Defined by Percival, in Greenfield et al. (2010). Age is determined from conodonts in the lower to middle part of the formation, as well as from a trilobite fossil (Patterson 2006) and fish plate impression (Young 2009) in the upper part. Occurs in the Mount Wright-Mutawintji region.||Of the upper Rowena Formation.|||A distinctive conglomerate with angular clasts of vein quartz.|22-FEB-18
23639|Gundaroo Sandstone|22518|6|Mentioned|p 3, 7|||Winduck Group, Darling Basin||||||
23639|Gundaroo Sandstone|22857|4|Described|p442 App.1, Tb.A1.6|Emsian|Pragian|Of the Winduck Group (Cobar Supergroup). Max. thickness: >900m. Geological Province: Winduck Shelf (Darling Basin). See also p201.||||||
23639|Gundaroo Sandstone|22859|6|Mentioned|p201|||||||||
23639|Gundaroo Sandstone|22887|2|Defined|p25, Fig.4 p11|Early Devonian|Early Devonian|||||||
23639|Gundaroo Sandstone|23173|6|Mentioned|Map Legend|||||||||
23639|Gundaroo Sandstone|23252|5|Briefly described|Map Legend|||of Winduck Group, Cobar Supergroup.||||||
23639|Gundaroo Sandstone|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|Of Winduck Group.||||||
23639|Gundaroo Sandstone|35925|5|Briefly described|p2|||To be defined by Glen et al.||||||
23639|Gundaroo Sandstone|37798|4|Described|p128|||See also Table 1.||||||
23639|Gundaroo Sandstone|38292|6|Mentioned|p3|||See also Fig.1.||||||
23639|Gundaroo Sandstone|39660|6|Mentioned|p449|||||||||
23639|Gundaroo Sandstone|40913|6|Mentioned|Map legend|Zlichovian|Pragian|Zlichovian-Pragian||||||
23639|Gundaroo Sandstone|41126|3|Fully described|p97|||||||||
23639|Gundaroo Sandstone|41138|6|Mentioned|Map legend|Pragian|Pragian|||||||
23639|Gundaroo Sandstone|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
23639|Gundaroo Sandstone|41821|3|Fully described|p46|||||||||
23639|Gundaroo Sandstone|42983|6|Mentioned|Fig.3,p345|||||||||
23639|Gundaroo Sandstone|43032|2|Defined|p140|Pragian||Of Winduck Group.||||||22-APR-09
23639|Gundaroo Sandstone|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Winduck Group (Cobar Supergroup).  Interbedded sandstone and recessive siltstone/mudstone.  Age is Pragian. Geological Province: Winduck Shelf.||||||
23639|Gundaroo Sandstone|61964|6|Mentioned|p140|Early Devonian|Early Devonian|||||||
23639|Gundaroo Sandstone|64967|5|Briefly described|p114 Fig. 2|Pragian|Pragian|Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). See also p115 Fig. 3.||||||
23639|Gundaroo Sandstone|65469|5|Briefly described|p15-p17|Pragian|Lochkovian|Lachlan Orogen.||Winduck Group|Includes the Booth Limestone Member|||
23639|Gundaroo Sandstone|70037|4|Described|p309 Fig.2, p311|Middle Devonian|Early Devonian|Glen (1979) initially placed this unit towards the top of the Amphitheatre Group, but reassigned it to the Winduck Group (Glen, 1982). Darling Basin. Mis-spelt as Grundaroo Sandstone on p311. c.90m thick. Sedimentary structures and fossils listed.||Upper part of Winduck Group.||Overlies Sawmill Tank Siltstone.|Lower unit contains sandstone with interbeds of shale. The overlying unit is mainly fine- and medium-grained sandstone, with vey fine interbeds of siltstone and shale.|
23639|Gundaroo Sandstone|70751|4|Described|p7, p12|Emsian|Pragian|Winduck Shelf. Hosts base metal-silver mineralisation.||Winduck Group|Includes the Booth Limestone Member.||Thinly to thickly-bedded sandstones and siltstones and minor limestones.|
23639|Gundaroo Sandstone|70950|4|Described|p1030,1033,1037|||Geological province: Winduck Shelf, Central Lachlan Orogen. Detailed mineralisation analysis provided. Basal unit comprises carbonaceous calcareous shales.||Unit of Winduck Group.|Includes, and overlies Booth Limestone Member.|Underlain unconformably by Thule Granite.|Thinly to thickly bedded sandstones and siltstones and minor limestones, some dolomitised.|
23639|Gundaroo Sandstone|72908|5|Briefly described|p5, p7, p16|Emsian|Pragian|Pragian to early Emsian in age. Hosts the Manuka deposit, formerly Wonawinta (carbonate-hosted Pb-Zn) deposit.||Winduck Group|Booth Limestone Member|Unconformably overlies Thule Granite|Includes thinly to thickly bedded sandstones and siltstones, carbonaceous shale, minor limestone units.|
23639|Gundaroo Sandstone|72958|6|Mentioned|p11|Emsian|Pragian|Cobar Basin. Nymagee area.||Winduck Group||Underlain by Sawmill Tank Siltstone. Overlain by Meadows Tank Formation (Mulga Downs Group). Equivalent to Buckambool Sandstone and Walters Range Group.||
23639|Gundaroo Sandstone|73174|6|Mentioned|p1037-1038|Emsian|Emsian|Winduck Shelf. Time-transgressive basal boundary. [Text suggest this unit overlies the Winduck Group and that it is Pragian in age; conflicts with other information].||Winduck Group, Cobar Supergroup||Underlain and equivalent to Sawmill Tank Sandstone.||
69883|Gundary Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Tirranna Andesite, Bradfordville Volcaniclastic, Komungla Rhyolite, and Back Station Ignimbrite Members. Rhyolitic to andesitic ignimbrites, lavas, intrusives and volcaniclastic rocks (no outcrop).||||||09-SEP-08
69883|Gundary Volcanics|66087|5|Briefly described|p3 Fig. 2|Early Devonian|Silurian|||Of the Mount Fairy Group.||||10-MAY-12
69883|Gundary Volcanics|68592|1|Redefined|p845 Fig.141, p846-7, p851-83, p889-91|Early Devonian|Early Devonian|See also p231, p265, p725-6, p728-30, p732, p745, p807, p827, p836, p897, p902, p916. New name. On p852 Fig.143, Gundary Volcanics incorrectly brackets Rhyanna Formation and Saltpetre Andesite Member as constituents. In the Strathaird area, west of Taralga, the unit was mapped as Turrallo Quartz Diorite by Scheibner (1973). Subsequently, Jones et al. (1995) defined the Gundary Formation, however their stratigraphy is at odds with recent Geological Survey of New South Wales mapping. Gundary Formation is here renamed Gundary Volcanics to reflect the large volume of primary volcanic rocks and was redefined due to the recognition of a regional depositional break and accompanying conglomerate unit (Bullamalita Conglomerate, Bindook Group). It is equivalent to the lower part of the Gundary Formation of Jones et al. (1995). Multiple type or representative sections provided: one for each named Member. Max thickness: ~1350 m. Metamorphism: apparently experienced two discrete phases of alteration. SHRIMP zircon U-Pb isotopic ages of Back Station Ignimbrite Member (414 +/- 4 Ma, Wilde 2002) and unconformably overlying Newacres Ignimbrite Member (Quialigo Volcanics, 411 +/- 3 Ma and 409 +/- 4 Ma, and 414.4 +/- 2.9, Black 2006); earliest Devonian brachiopod fauna near top of underlying Boxers Creek Formation. Thus age is most probably early Lochkovian (earliest Early Devonian). A dark green porphyry from an ignimbrite outcrop at Frogs Hole was quarried for dimension stone. Geophysical properties described. Basal units of Longreach and Gundary Volcanics correlate and may be distal equivalents. Is intruded by Forest Lodge Quartz Monzodiorite.|414 +/- 4 Ma (SHRIMP zircon U-Pb: Wilde, 2002).|Unit in Mount Fairy Group.|Includes Back Station Ignimbrite, Tirranna Andesite, Bradfordville Volcaniclastic and Komungla Rhyolite Members.|Erosionally overlies Rhyanna, Argyle and Covan Creek Formations. Overlies, interfingers with, and intrudes Boxers Creek Formation. Is unconformably overlain by Bullamalita Conglomerate.|Now defined as a succession of rhyolitic through basaltic volcanic, intrusive, clastic and volcaniclastic rocks; diverse composition and facies.|
69883|Gundary Volcanics|69159|5|Briefly described|Map legend|Lochkovian|Lochkovian|||Unit in Mount Fairy Group.|Includes Back Station Ignimbrite Member.||Rhyolitic to andesitic ignimbrite, lavas and intrusives.|07-SEP-15
69883|Gundary Volcanics|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfg[3 asterisks]. Includes 5 unnamed units: siliceous ironstone of microcrystalline quartz and disseminated fine-grained hematite; recrystallised limestone block, conodont-bearing; quartzose sandstone and quartzite with interbedded siltstone; laminated siltstone and mudstone with lesser sandstone and minor tuffaceous siltstone; dacitic to rhyolitic (volcaniclastic) sandstone, and minor conglomerate of porphyritic rhyolite and mudstone blocks. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group|Includes Back Station Ignimbrite Member, Komungla Rhyolite Member, Bradfordville Volcaniclastic Member, Tirranna Andesite Member and 5 unnamed units.|Overlies Boxers Creek Formation.|Crystal rich, pyroxene and hornblende dacitic welded ignimbrite, crystal-lithic rich, rhyolitic to dacitic volcanic sandstone and conglomerate. Porphyritic rhyolite and andesite with basalt. Quartzose-lithic quartz sandtsone, siltstone and mudstone.|
69883|Gundary Volcanics|70542|5|Briefly described|Map Legend|Devonian|Silurian|Includes five unnamed members consisting of: siliceous ironstone, recrystallised limestone, massive quartz sandstone and massive to laminated siltstone and mudstone.||Mount Fairy Group|Includes Back Station Ignimbrite Member, Komungla Rhyolite Member, Bradfordville Volcaniclastic Member, Tirranna Andesite Member and five unnamed members.||Crystal rich, pyroxene and hornblende dacitic welded ignimbrite, crystal-lithic rich, rhyolitic to dacitic volcanic sandstone and conglomerate. Porphyritic rhyolite and andesite with basalt. Quartz-lithic quartz sandstone, siltstone and mudstone.|
69883|Gundary Volcanics|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|Includes Back Station Ignimbrite Member, Bradfordville Volcaniclastic Member||Crystal rich, pyroxene and hornblende dacitic welded ignimbrite, crystal-lithic rich, rhyolitic to dacitic volcanic sandstone and conglomerate. Porphyritic rhyolite and andesite with basalt. Quartzose-lithic quartz sandstone, siltstone and mudstone.|14-NOV-16
69883|Gundary Volcanics|70661|6|Mentioned|p35|||||||||
69883|Gundary Volcanics|71040|5|Briefly described|p8 Fig.5|||Canberra Zone.|414 +/- 4 Ma; U-Pb zircon.|||||
69883|Gundary Volcanics|71069|6|Mentioned|p133, p135, p136 fig 44, p141, p143|Lochkovian|Lochkovian|Up to 1350m thick.Age based on SHRIMP age derived for the Back Station Ignimbrite Member. Erupted in shallow marine to subaerial environment. See also p144, p163, p170. ||Mount Fairy Group|Includes the Back Station Ignimbrite Member, Bradfordville Volcaniclastic Member and the Tirranna Andesite Member.|Unconformably overlies the Rhyanna Formation. Conformably overlies the Covan Creek Formation.  Overlies the Boxers Creek Formation.||
69883|Gundary Volcanics|71656|5|Briefly described|p13 Fig.2, p30|Early Devonian|Early Devonian|An allochthonous limestone in the Gundary Volcanics yielded more than 100 conodont elements suggesting a maximum age of Ludlow - Pridoli, but regional correlations suggest an Early Devonian depositional age.||Mount Fairy Group||Overlies Boxers Creek Formation.|Volcanics containing allochthonous limestone blocks.|
69883|Gundary Volcanics|71699|5|Briefly described|Map legend.|Devonian|Silurian|||Mount Fairy Group.|Back Station Ignimbrite Member.||Rhyolitic to andesitic ignimbrite, lava and intrusive rocks.|
69883|Gundary Volcanics|71700|2|Defined|vi, p7, p15, p23-p24, CD|Lochkovian|Lochkovian|Named for the Gundary Plains in GOULBURN250. A single type section was not nominated for the Gundary Volcanics in GOULBURN250 due to the high degree of variation and complexity within the unit, however, type sections were nominated for individual subunits. Units comprising the formation were previously mapped as the Gundary beds, Towrang Beds, Turallo Quartz Diorite or Gundary Formation. Recognised in the Braidwood100 sheet. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, Age is further constrained by SHRIMP ages for the underlying and overlying units. This unit has an estimated maximum thickness of approximately 1350m.|414 +/- 4 Ma (SHRIMP, Wilde, 2002)|Mount Fairy Group|Includes the Back Station Ignimbrite Member, Bradfordville Volcaniclastic Member, Tirranna Andesite Member, Komungla Rhyolite Member.|Overlies the Boxers Creek Formation. Unconformably overlain by the Newacres Ignimbrite Member (Quialigo Volcanics). Overlain by the Long Flat Volcanics. Faulted against the Abercrombie Formation.|Dacitic ignimbrite, rhyolitic volcaniclastics, andesitic to basalatic lavas and volcaniclastic rocks, high level intrusive rhyolite and less abundant conglomerate, sandstone, siltstone, quartzite and limestone.|
29581|Gundibindyal Granite|22638|4|Described|p68|Early Devonian|Late Silurian|||||||
29581|Gundibindyal Granite|44192|5|Briefly described|Map Legend|Lochkovian|Pridolian|||||||
29581|Gundibindyal Granite|44936|5|Briefly described|Map Legend||Early Devonian|||||||
29581|Gundibindyal Granite|69801|6|Mentioned|p2-p5, p45-50, p138|Devonian|Devonian|Eastern Lachlan Orogen. Occurs southwest of Stockinbingal. Sample locality, petrography, SHRIMP analyses and interpretation are detailed.|417.9 +/- 2.0 Ma (SHRIMP)|Gundibindyal Suite||Intrudes the Combaning Formation.|Slightly weathered, medium to coarse-grained, weakly porphyritic biotite I-type granite.|
29581|Gundibindyal Granite|73215|5|Briefly described|p994|||Tumut Trough.|418 +/- 2 Ma (Bodorkos et al.,2015).|||||
32685|Gundibindyal Suite|44192|6|Mentioned|Map Legend|Devonian|Devonian|||||||
24302|Gundillion Conglomerate|22815|4|Described|p102|||||||||
24302|Gundillion Conglomerate|22857|5|Briefly described|p216, p494 App.1 Tb.A1.7|Frasnian|Frasnian|Of the Minuma Range Group. Reddish-purple, poorly sorted coarse polytmictic conglomerate. Max. thickness: 150m. Geological Province: Lambie Basin.||||||03-FEB-06
24302|Gundillion Conglomerate|22859|6|Mentioned|p216|||||||||
24302|Gundillion Conglomerate|39028|6|Mentioned|Map legend|Famennian|Famennian|||||||
24302|Gundillion Conglomerate|40276|2|Defined|p23|Late Devonian|Late Devonian|||||||
24302|Gundillion Conglomerate|43233|5|Briefly described|Map Legend||Late Devonian|||||||
24302|Gundillion Conglomerate|61818|5|Briefly described|p85|Late Devonian|Late Devonian|Of the Minuma Range Group. Geological Province: Lachlan Fold Belt.||||||
24302|Gundillion Conglomerate|69159|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Minuma Range Group.|||Red to brown, polymictic, matrix to clast-supported pebble to cobble conglomerate fining upwards into coarse to very coarse-grained lithic-rich sandstones. Clasts include chert, mudstone, siltstone, fine-grained quartz sandstone, rhyolitic volcanics.|07-SEP-15
24302|Gundillion Conglomerate|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Minuma Range Group.|||Red to brown, polymictic, matrix- to clast-supported pebble to cobble conglomerate, fining upward to coarse-grained, lithic-rich sandstone; clasts include chert, mudstone, siltstone, fine-grained quartz sandstone, rhyolitic volcanics, sparse granite.|
24302|Gundillion Conglomerate|71700|2|Defined|vi, p7, p29, p45, p58, p119|Late Devonian|Late Devonian|Named for the Gundillion homestead at GR 738606 6039698. The type section is designated from GR 738390 639402 to GR 738386 639401. Synonymy and lithology is discussed in detail, see CD. Distribution, geomorphic expression, outcrop, depositional environment, structure, fossils, metamorphism, geophysical characteristics, distinguishing features and economic geology are discussed. The unit ranges in thickness from 2 to 150m thick at the type section. Late Devonian age is derived from unit relationships. Equivalent to the unnamed conglomerate member at the base of the Worange Point Member.||Minuma Range Group||Unconformably overlies the Toggannoggra Rhyolite Member. Conformably overlain by the Big Hole Formation and the Long Swamp Creek Formation. Faulted against the Tally Ho Ignimbrite Memebr.|Bedded sequence of red to brown, pebble to cobble conglomerate, finining upwards into coarse- to very coarse-grained, lithic-rich sandstones.|
24302|Gundillion Conglomerate|73181|6|Mentioned|p65-67|Frasnian|Frasnian|||Minuma Range Group||Overlain by Long Swamp Creek Formation and Big Hole Formation.||
82484|Gundle Monzogranite|71628|4|Described|p17: 1-2, 54, 56, 60-65, 89|||Initially Gundle Granite; subsequently Gundle Adamellite (Matthias, 1967 unpublished); name altered to align with IUGS nomenclature. Comprises at least four small bodies, ~5 km NW of Bellangry. Lithology and mineralogy detailed. Geochemistry described. Is associated with historically significant Sn mineralisation (several prospects named).|213 +/- 12 Ma (U-Pb LA-ICP-MS; Prichard, 2013).|Glen Esk Suite.||Intrudes Pappinbarra Formation and Boonanghi beds.|Off-white, green-grey to pale pink, coarse-grained biotite-hornblende monzogranite and biotite leucomonzogranite, grading into porphyritic, microgranitic and sugary-texture aplitic variants towards the margin.|
77553|Gunnedah Formation|66891|5|Briefly described|p183.|||Liverpool Plains. Low salinity groundwater rises through this unit before dissolving salt stores in the overlying Narrabri Formation, producing salinised catchments.||||Is overlain by Narrabri Formation.|Sands and gravels.|
77553|Gunnedah Formation|68240|6|Mentioned|p9-13, 22|Pliocene|Pliocene|Liverpool Plains. Meandering stream deposits. Uniformly fresh groundwater.|||||Interbedded clays with sand and gravel layers.|
31580|Gunning Suite|42726|5|Briefly described|map legend||Silurian|||||||
31580|Gunning Suite|44093|5|Briefly described|p202 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31580|Gunning Suite|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Willdamar Tonalite, Streamville Granodiorite, Gunning, Oolong and Mutmutbilly Granites, Little Redbank Granodiorite and Cumberoona Tonalite.||||||12-JUN-08
31580|Gunning Suite|66300|5|Briefly described|p92.|||I-type. Time-equivalent to Hovells and Burrawinda Suites in west-central GOULBURN area.|||Includes Gunning Granite and Cumberoona Tonalite.|||
31580|Gunning Suite|68592|2|Defined|p74 Tb.5, p231, p1312-53|Early Silurian|Early Silurian|Named by Chappell et al. (1991), after the town of Gunning, to include Gunning and Oolong Granites. Now expanded to include Mutmutbilly Granite; Cumberoona and Willdamar Tonalites; Litle Redbank and Streamville Granodiorites. These plutons were included in undifferentiated Wyangala Batholith in previously published geological maps (Brunker and Offenberg, 1970; Felton, 1974). Gunning Granite remains the type pluton. Plutons typically exhibit mildly to strongly developed schistosity; a number are intensely foliated adjacent to major faults. Geochemistry detailed. Probable late Early Silurian age. Wyangala structural zone: deformation described.|||Includes Gunning, Oolong and Mutmutbilly Granites; Little Redbank and Streamville Granodiorites; Cumberoona and Willdamar Tonalites.|Intrudes and contatc metamorphoses Abercrombie Formation. Is intruded by Wyangala Supersuite.|I-type. Typically grey to cream, medium- to coarse-grained, massive to foliated, equigranular to porphyritic hornblende-biotite granite, granodiorite and tonalite. Microdiorite enclaves common.|
31580|Gunning Suite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Error in Geological Reference Legend: shown as containing constituent 'Sgl' Micalong Swamp Basic Igneous Complex. Should be 'Sgl' Little Redbank Granodiorite. It is correctly shown ('Sgl' Little Redbank Granodiorite in Gunning Suite) in the Time-Space Plot, on the Crookwell 1:100 000 sheet portion. On Crookwell and Gunning 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Cumberoona Tonalite, Micalong Swamp Basic Igneous Complex, Mutmutbilly Granite, Oolong Granite, Streamville Granodiorite, Gunning Granite, Willdamar Tonalite.|||
31580|Gunning Suite|70541|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Mutmutbilly Granite, Oolong Granite, Gunning Granite|||
31580|Gunning Suite|70544|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Cumberoona Tonalite, Little Redbank Granodiorite, Streamville Granodiorite, Gunning Granite, Willdamar Tonalite|||
31580|Gunning Suite|70545|5|Briefly described|Map Legend |Silurian|Silurian||||Includes Streamville Granodiorite|||
31580|Gunning Suite|71069|6|Mentioned|p36|Late Silurian|Late Silurian|||||||
35027|Gunningbland Formation|13995|5|Briefly described|p84|Late Ordovician|Late Ordovician|Parkes Platform. Contains the trilobite genus Koksorenus, with links to N China and Kazakhstan.||||||
35027|Gunningbland Formation|23736|3|Fully described|p16|Eastonian|Eastonian|Previously Gunningbland Shale Member of the Goonumbla Volcanics. Of the Northparkes Group. Maximum thickness: 400m.||||||13-MAR-07
35027|Gunningbland Formation|24417|2|Defined|p24|Eastonian|Eastonian|Of Northparkes Volcanic Group. Formerly "Gunningbland Shale Member" of Goonumbla Volcanics - now raised to formation status.  Includes one informal subdivision, "Currajong Park Beds".  Overlies Billabong Creek Limestone.  Max. thick.: 400m.||||||
35027|Gunningbland Formation|60009|5|Briefly described|Map Legend|Eastonian|Eastonian|Of the Northparkes Volcanic Group. Interbedded with: Goonumbla Volcanics.||||||13-JUL-04
35027|Gunningbland Formation|61724|3|Fully described|p864 Fig.1, p867|Late Ordovician|Middle Ordovician|A sequence of volcanic siltstone, mudstone, sandstone and patchy limestone. Overlain by Wombin Volcanics; conformably overlies Billabong Creek Limestone. See also p870-872.||||||
35027|Gunningbland Formation|61893|5|Briefly described|p249|||||||Overlies Billabong Creek Limestone.|Includes intermittent limestones of Ea3 age.|
35027|Gunningbland Formation|62799|5|Briefly described|p413, p415|Late Ordovician|Late Ordovician|Formerly Gunningbland Shale Member of Goonumbla Volcanics. Contains trilobites of Eokosovopeltis-Pliomerina fauna of late Eastonian age.||||Overlies Billabong Creek Limestone.|Slope to basinal deposits, including lithic calcareous siltstones.|28-MAR-12
35027|Gunningbland Formation|63121|5|Briefly described|p226|Late Ordovician|Late Ordovician|Of Percival (1978).||||||
35027|Gunningbland Formation|63278|4|Described|p146 Fig. 2a|Eastonian|Eastonian|Of the Goonumbla Volcanics. Overlain by Goonumbla Volcanics, underlain by Billabong Creek Limestone. Geol Prov: Junee-Narromine Volcanic Belt, LFB. In Gunningbland area, this unit seperates the lower Goonumbla Volcanics from the upper Goonumbla Volcanics.||||||04-DEC-12
35027|Gunningbland Formation|63283|6|Mentioned|p194 Fig. 2|Eastonian|Eastonian|||||||07-FEB-11
35027|Gunningbland Formation|63286|5|Briefly described|p308 Fig. 9|Late Ordovician|Late Ordovician|Of the Goonumbla Volcanics. Underlain by Billabong Creek Limestone. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
35027|Gunningbland Formation|63290|5|Briefly described|p397 Fig. 3(b)|Eastonian|Eastonian|Overlain by Wombin Volcanics, underlain by Billabong Creek Limestone. Geological Province: Junee - Narromine Volcanic Belt.||||||
35027|Gunningbland Formation|63291|5|Briefly described|p421, p425|Bolindian|Darriwilian|Of Goonumbla Volcanics. Fossils give age of unit.||||||28-SEP-07
35027|Gunningbland Formation|63293|6|Mentioned|p468 Fig. 2|Eastonian|Eastonian|Of Goonumbla Volcanics. Overlain by Wombin Volcanics, underlain by Billabong Creek Limestone. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
35027|Gunningbland Formation|64015|5|Briefly described|p57, p58 Fig. 1|Late Ordovician|Late Ordovician|Overlies ?Billabong Creek Limestone. Contains assemblages of coral and conodont fauna.||||||28-AUG-08
35027|Gunningbland Formation|64826|5|Briefly described|p1040 Tb. 1|Eastonian|Gisbornian|Of Northparkes Group.||||||04-MAR-09
35027|Gunningbland Formation|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
35027|Gunningbland Formation|67107|5|Briefly described|p688, 693-694, 699|Late Ordovician|Middle Ordovician|Goonumbla district. Hosts Au-Cu skarn deposits; mineralised at c.440 Ma. Eastonian.||||Overlies Goonumbla Volcanics.|Limestone, calcareous sandstone. Mineralised zoned calc-silicate-rich skarn.|
35027|Gunningbland Formation|67322|4|Described|p22; Fig.5|Katian||Macquarie Arc. Sherwin and Percival, in Lyons et al. (2000), modified from Sherwin et al., (1987). Of late Eastonian age, defined by as yet-undescribed graptolites. Contains a diverse macrofossil fauna. Occurs in the Junee-Narromine region.||Of the Northparkes Group.||Conformably overlies the Billabong Creek Limestone. Overlain by the Goonumbla Volcanics.|Fine sandstones and siltstones with lenses of limestone.|22-FEB-18
35027|Gunningbland Formation|70684|5|Briefly described|p55, p56 Fig.29, p61-62, p74-75|Late Ordovician|Late Ordovician|Junee-Narromine Volcanic Belt. Eastonian.||Northparkes Group.||Is overlain by the upper part of Goonumbla Volcanics.|Lower part has volcaniclastic rocks, passing up into feldspar-rich siltstone with a deep-water fauna (listed). The upper part includes volcanic sandstones with local ash beds, shallowing-up to pinnacle reef limestones.|
35027|Gunningbland Formation|70754|5|Briefly described|p450 Fig.2, p451, p455, p457, p459-462|Late Ordovician|Late Ordovician|Moderately to abundantly fossiliferous. Some fossil species named. Systematic palaeontological descriptions.||||Overlies Billabong Creek Limestone. Is overlain by Goonumbla Volcanics.|Siltstone, limestone.|
35027|Gunningbland Formation|71091|6|Mentioned|p146-147|||||||Correlative of Malongulli Formation.|Includes limestones.|
35027|Gunningbland Formation|73154|5|Briefly described|p77 Fig.3|Eastonian|Eastonian|Junee-Narromine Belt.||||Overlies Billabong Creek Limestone, underlies Wombin Volcanics.|Limestone, siltstone.|
35027|Gunningbland Formation|73492|6|Mentioned|p693|||Exposed in the Parkes-Forbes area.||||||
82487|Gunny Bag Granite|71628|5|Briefly described|p17: 2, 98|||New name (this study), after a local creek. Occurs to the north of Mount Seaview, ~60 km ESE of Walcha, as a ~5 x 1 km intrusion. Unaffiliated.||Gunny Bag Suite.||Intrudes Sandon beds.|Porphyry and leucomonzogranite.|
26600|Guroba Formation|22529|5|Briefly described|1,4 fig 2|Lochkovian|Lochkovian|||||||
26600|Guroba Formation|22857|5|Briefly described|p470 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Cruding Group. Quartzofeldspathic arenite, siltstone, tuff and breccia. Max. thickness: 600m. Geological Province: Hill End Trough. ||||||
26600|Guroba Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
26600|Guroba Formation|23170|2|Defined|p165|Lochkovian|Lochkovian|of Crudine Group.||||||
26600|Guroba Formation|24126|6|Mentioned|p228|||Geological Province: Hill End Trough.||||||
26600|Guroba Formation|24394|5|Briefly described|p170 Fig. 1, p175|Pragian|Pragian|Predominantly volcanogenic turbidite with mass-flow paraconglomerates and minor pelitic units. Geological Province: Lachlan Fold Belt.  See also p171 Fig. 2.||||||
26600|Guroba Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
26600|Guroba Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
26600|Guroba Formation|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
26600|Guroba Formation|43494|4|Described|p26, p27||Devonian|Thick lithic, feldspathic sandstones with minor siltstone interbedded with thicker siltstone units. Conformably underlies Merrions Fm ;conformably overlies Dunmoogin Fm, interfingers with Waterbeach Formation east of Pyramul. Max.thickness: 1000m.||||||16-MAR-06
26600|Guroba Formation|68003|5|Briefly described|p24 Fig.3-e. |Lochkovian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Crudine Group.||Overlies Waterbeach Formation. Is overlain by Merrions Formation.||
26600|Guroba Formation|68592|6|Mentioned|p1038|||Northern Hill End Trough.||Unit in Crudine Group.||||
26600|Guroba Formation|73299|6|Mentioned|p1096 Fig.3, p1098 Fig.4, p1102 Fig.8|Devonian|Devonian|Hill End Trough.||||Overlies the Waterbeach Formation, underlies the Cunningham Formation, Merrions Formation.||
40131|Gurragong Volcanics|60303|5|Briefly described|p5, p6 fig. 1|Early Devonian|Silurian|Age is Middle Silurian to Early Devonian. Geological Province: Lachlan Fold Belt.||||||03-NOV-15
40131|Gurragong Volcanics|61964|2|Defined|p14 Fig. 4, p86-87|Pragian|Pridoli|Southerly extension of Ural Volcanics. A-type. Narrow belt of silicic volcanic, or shallow intrusion (details included). Overlie part of Weethalle Granite (south); partly below Cocoparra Group; unconformable contacts with Clements Fm. Ages are provisional.|417.9 +/-2.3, 418.6+/-2.3 Ma U/Pb SHRIMP|||||21-JAN-21
40131|Gurragong Volcanics|62034|5|Briefly described|p27|Devonian|Silurian|Interpreted to be the southern extension of the Ural Volcanics. Geological Province: Lachlan Orogen.||||||10-APR-06
40131|Gurragong Volcanics|62367|5|Briefly described|p4 Fig. 2, p5|Early Devonian|Late Silurian|Felsic rocks.||||||02-JUN-06
40131|Gurragong Volcanics|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Ural Volcanics (Rast Group). Undifferentiated silicic volcanic and intrusive rocks.||||||10-APR-08
40131|Gurragong Volcanics|63019|5|Briefly described|p920, p921 Fig.2|Pridoli|Pridoli|Of Rast Group. Geological Province: Lachlan Orogen.||||||23-JAN-07
40131|Gurragong Volcanics|69043|4|Described|p2, p5-6, p12-18, p21, p28, p34, p40|Lochkovian|Pridoli|See also p47, p50, p53, p56, p116. Colquhoun et al. (2005). Bears a strong petrographic and geochemical resemblance to the Walleroobie Volcanics to the S and E; their ages are indistinguishable. Other similar ages given. A "garnet porphyry" at the Ardlethan Mine, dated at 414.7 +/- 2.3 Ma, is probably a lateral equivalent; previously it was considered a carapace of the Ardlethan Granite.|416.5 +/- 2.4 Ma.|Rast Group.||Age-equivalent with Walleroobie Volcanics.|Includes a garnet-bearing crystal-rich volcaniclastic rock.|
40131|Gurragong Volcanics|69160|5|Briefly described|Map legend|Early Devonian|Early Devonian|The five facies are mapped separately.||Unit in Rast Group.||Unconformably overlies Clements Formation.|Silicic volcanic and intrusive rocks: porphyritic biotite garnet granite to very coarse porphyritic rhyolite; quartz-feldspar porphyry; porphyritic banded rhyolite, minor breccia; quartz-feldspar crystal-rich lithic ignimbrite; biotite ignimbrite.|
40131|Gurragong Volcanics|69801|6|Mentioned|p25|Early Devonian|Early Devonian|Central Lachlan Orogen, occurs in the Ardlethan mine area.||||||
40131|Gurragong Volcanics|70296|5|Briefly described|p1, p8-10, p24|Pridoli|Ludlow|Cargelligo district. 2 samples dated, volcanic breccia and porphyry. Similar in age to the Nyora Granite. Potentially related to the Ural Volcanics on the basis of dating.|417.9 +/- 2.3 Ma, 418.3+/-2.3 Ma (SHRIMP U-Pb)|||Overlies the Weethalle Granite.||21-JAN-21
40131|Gurragong Volcanics|70777|5|Briefly described|p1-p2, p80|Lochkovian|Lochkovian|Lachlan Orogen. Additional ages provided include 416.5 +/- 2.4 Ma (Bull, 2015) 417.9 +/- 2.3 Ma (Colquhoun et al., 2005) and 417.8 +/- 2.3 Ma (Bodorkos et al., 2013). Ages are very similar to the Walleroobie Volcanics and some facies are similar also (thus they may be equivalent).|418.6 +/- 2.3 Ma (Black, 2005)|||Equivalent to the Walleroobie Volcanics.|Minor coherent crystal-rich lavas overlain by pyroclastic deposits associated with more voluminous massive ignimbrites.|
40131|Gurragong Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Rast Group.|||Biotite ignimbrite, lithic quartz-feldspar ignimbrite, rhyolite lava, quartz-feldspar porphyry, megacrystic garnet granite.|
40131|Gurragong Volcanics|71889|5|Briefly described|p9|||Outcrops around Mooneys Lane, north of Ardlethan.|||||Rhyolite.|
40131|Gurragong Volcanics|72082|6|Mentioned|p3|||||||||
40131|Gurragong Volcanics|72084|6|Mentioned|p39|Early Devonian|Early Devonian||416.5 +/- 2.4 Ma (Bodorkos et al., 2013).|||||
35786|Gurrundah Granite|50232|5|Briefly described|Map legend|Pragian|Lochkovian|Part of the Wologorong Batholith.  Foliated cream to pink leucocratic biotite sodic granodiorite, quartz monzonite, granite.||||||
35786|Gurrundah Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Part of the Wologorong Batholith.||||||
35786|Gurrundah Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Parkesbourne Suite. Pinkish-grey, medium-grained porphyritic granite and granodiorite, porphyritic alkali feldspar granite and quartz monzonite.||||||
35786|Gurrundah Granite|68592|3|Fully described|p1543, p1557-60|Early Devonian|Early Devonian|New [?] name, after Parish of Gurrundah. Previously included in Wologorong Granite; current mapping indicates separation from that unit by metasedimentary rocks. No type area because of compositional diversity; a good exposure is described. Strong deformation in the W and SW weakens to the E. Geophysical properties described. No isotopic age; age inferred from intrusive relationship.||Unit in Parkesbourne Suite.||Intrudes Cuddyong Formation. Is overlain by Crookwell Basalt.|Northern body has medium-grained, porphyritic granite and granodiorite. Southern body has pinkish-grey to beige, porphyritic alkali feldspar granite, granite, and lesser quartz monzonite with local metasedimentary xenoliths and microgranite enclaves.|
35786|Gurrundah Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dpg. On Gunning 1:100 000 mapsheet portion of Time-Space Plot.||Parkesbourne Suite|||Medium-grained, porphyritic biotite granite and granodiorite, porphyritic alkali feldspar granite and quartz monzonite; low K, Th and U response; low magnetic susceptibility.|
35786|Gurrundah Granite|70541|4|Described|Map Legend|Devonian|Devonian|||Parkesbourne Suite|||Pinkish grey, medium grained, porphyritic, biotite granite and granodiorite, porphyritic alkali feldspar granite and quartz monzonite; low K, Th and U response; low magnetic susceptibility.|
35786|Gurrundah Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Parkesbourne Suite|||Medium-grained, porphyritic biotite granite and granodiorite, porphyritic alkali feldspar granite and quartz monzonite; low K, Th and U response; low magnetic susceptibility.|
82489|Guy Fawkes Granodiorite|71628|4|Described|p17: 2, 8, 13, 28-30, 90-92|||New name, after a local river, for I-type granites of the Chaelundi Complex. Occurs ~40 km NW of Dorrigo. Geochemistry described. Guy Fawkes Suite.|237.4 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Chaelundi Complex.||Intrudes Moombil Siltstone and Brooklana beds (Coffs Harbour Association). Is intruded by Chaelundi Mountain Monzogranite.|Medium to light greenish-grey, equigranular, medium-grained hornblende-biotite granodiorite, and (K-feldspar) porphyritic hornblende-biotite monzogranite. I-type.|
40991|Guygallon Volcanic Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Of the Flagstaff Formation. Volcanogenic sandstone, volcanic breccia and siltstone; ash lenses. Max. thickness: 230m. Geological Province: Tamworth Forearc Basin.||||||
40991|Guygallon Volcanic Member|44244|5|Briefly described|p81|Visean|Visean|Of the Flagstaff Formation.  Interfingers with Mount Rivers Ignimbrite Member.  Max. thickness: 230m.  Type section in text.  Geological Province: Gresford Block.||||||18-AUG-04
40991|Guygallon Volcanic Member|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Gresford Block.  Of the Flagstaff Formation.||||||
26601|Gwando Siltstone|9548|5|Briefly described|Map Legend|Pragian|Pragian|Of the Yarra Yarra Creek Group. Underlies: Myamely Sandstone.  Overlies: Ewolong Formation.||||||
26601|Gwando Siltstone|22831|4|Described|p 54|Pragian|Lochkovian|||||||
26601|Gwando Siltstone|22857|4|Described|p446 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Yarra Yarra Creek Group. Max. thickness: 700m. Geological Province: Darling Basin. ||||||
26601|Gwando Siltstone|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
26601|Gwando Siltstone|42449|6|Mentioned|p23|||Reserved 1977, D. Pogson. Last update May 1991.||||||
26601|Gwando Siltstone|42566|3|Fully described|p106|||||||||
26601|Gwando Siltstone|42568|5|Briefly described|Map legend|Pragian|Pragian|||||||
26601|Gwando Siltstone|43441|6|Mentioned|29||Early Devonian|||||||08-JAN-10
26601|Gwando Siltstone|44160|5|Briefly described|Map Legend||Lochkovian|||||||08-JAN-10
26601|Gwando Siltstone|70751|6|Mentioned|p12|Lochkovian|Lochkovian|||Yarra Yarra Creek Group||||
26601|Gwando Siltstone|72958|6|Mentioned|p11|Lochkovian|Lochkovian|Cobar Basin. Nymagee area.||Yarra Yarra Creek Group, Cobar Supergroup||Underlain by Ewolong Formation. Overlain by Myamley Sandstone.||
41062|Gwydir River Monzogranite|24366|5|Briefly described|p9, 16 Fig. 3|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.||||||
41062|Gwydir River Monzogranite|68111|5|Briefly described|p968 Tb.1|Anisian|Olenekian|Also 249 - 244 Ma; Rb-Sr (biotite) (Shaw 1994).|252.3 +/- 1.5 Ma, U-Pb SHRIMP (Cross et al. 2010).|Of the Uralla Supersuite.||||
41062|Gwydir River Monzogranite|69639|5|Briefly described|p32, p68, p95, p133, p219|Induan|Changhsingian|New England Orogen.|252.3 +/- 1.5 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
41062|Gwydir River Monzogranite|70217|5|Briefly described|p43, p73 tbl 14.1|Changhsingian|Changhsingian|New England Orogen. Previously the Gwydir River Adamellite. Age derived from Cross and Blevin, 2010.|252.3 +/- 1.5 Ma (SHRIMP U-Pb)|Mount Duval Suite||||
41062|Gwydir River Monzogranite|71628|4|Described|p8: 4, 27-33, 41, 99-101, 115|||Brown (2003), after unpublished work by Chappell and Bryant (1994). Previously Gwydir River Adamellite. Forms a large (195 km2) body, cropping out N of Yarrowyck, 35km W of Armidale, as whalebacks and tors and forming prominent hills. Metamorphic aureole described. Is said (p8-115) to be intruded by Yarrowyck Granodiorite. Several other age determinations given. Lithology described in detail. Geochemistry described. Very high radiometric response. Associated with minor Mo, As and Au mineralisation.|252.3 +/- 1.5 Ma (SHRIMP: Cross and Blevin, 2010).|Mount Duval Suite.||Intrudes Sandon beds, Yarrowyck Granodiorite(?) and locally Wandsworth Volcanics. Is intruded (gradational contact) by Myanbah Leucosyenogranite.|Medium- to coarse-grained, porphyritic to equigranular biotite-hornblende monzogranite to granodiorite; minor fine-grained sugar-textured leucomonzogranite to leucosyenogranite. I-type.|
26602|Gyarran Volcanics|22601|6|Mentioned|409|Permian|Permian|Geol province Sydney Basin. Overlying unit Skeletar Formation. Previously Skeletar Formation.||||||12-NOV-08
26602|Gyarran Volcanics|22857|4|Described|p526 App.1 Tb.A1.9|Permian|Permian|Of the Dalwood Group. Rhyolite, felsic to mafic volcanics, pyroclastics. Max. thickness: >218m. Geological Province: Sydney Basin.||||||
26602|Gyarran Volcanics|22969|4|Described|p 9, Fig 4.1a|||||||||
26602|Gyarran Volcanics|23350|5|Briefly described|260|Permian|Permian|Proposed that Gyarran Volcanics and Skeletar Formation combine to form the Dalwood Group (1994).||||||15-JUL-04
26602|Gyarran Volcanics|31706|6|Mentioned|p657|||Permian correlation chart.||||||12-NOV-08
26602|Gyarran Volcanics|31881|5|Briefly described|p340|||? equiv. Werrie Basalts.||||||
26602|Gyarran Volcanics|31882|6|Mentioned|p243|||||||||
26602|Gyarran Volcanics|34015|6|Mentioned|p328|||||||||
26602|Gyarran Volcanics|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
26602|Gyarran Volcanics|34292|6|Mentioned|p24|||Permian||||||
26602|Gyarran Volcanics|34445|5|Briefly described|p319|||||||||
26602|Gyarran Volcanics|34447|6|Mentioned|Table 5.2|||||||||
26602|Gyarran Volcanics|36042|6|Mentioned|Table 1|||||||||
26602|Gyarran Volcanics|36045|6|Mentioned|p330|||||||||
26602|Gyarran Volcanics|36069|6|Mentioned|p23|||||||||
26602|Gyarran Volcanics|37773|5|Briefly described|p18|||||||||
26602|Gyarran Volcanics|38837|6|Mentioned|p232|||||||||
26602|Gyarran Volcanics|39287|6|Mentioned|Fig. 2.5|||||||||
26602|Gyarran Volcanics|39288|6|Mentioned|p57|||See also Fig.3.3||||||
26602|Gyarran Volcanics|39346|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26602|Gyarran Volcanics|40246|6|Mentioned|p173|||||||||
26602|Gyarran Volcanics|40331|6|Mentioned|p3|||||||||
26602|Gyarran Volcanics|40883|6|Mentioned|p15|||||||||
26602|Gyarran Volcanics|41054|6|Mentioned|Fig.3|||||||||
26602|Gyarran Volcanics|41290|6|Mentioned|Fig.8|||||||||
26602|Gyarran Volcanics|41689|6|Mentioned|Table 1|||||||||
26602|Gyarran Volcanics|41834|6|Mentioned|p590|||||||||
26602|Gyarran Volcanics|42916|5|Briefly described|Table 1||Early Permian|||||||
26602|Gyarran Volcanics|42925|5|Briefly described|Table 1||Early Permian|||||||
26602|Gyarran Volcanics|43017|5|Briefly described|Fig.1,p372|||||||||
26602|Gyarran Volcanics|43194|5|Briefly described|p128, p129 Tb. 8.3|Early Permian|Early Permian|Hunter region, Sydney Basin. Contains Lochinvar, Allandale, Rutherford and Farley Formations. Equivalent to Dalwood Group in the Newcastle Coalfield and Werrie Basalt and Boggabri Volcanics (Gunnedah Basin).||||||
26602|Gyarran Volcanics|43257|5|Briefly described|Map Legend||Early Permian|Of Dalwood Group.||||||
26602|Gyarran Volcanics|43440|14|Not recorded|p91,82|||Correlated with Dalwood Group.||||||12-NOV-08
26602|Gyarran Volcanics|43477|14|Not recorded|p17,28,29,31,35,Pl.3|||||||||
26602|Gyarran Volcanics|43479|14|Not recorded|p218||Artinskian|||||||
26602|Gyarran Volcanics|44244|6|Mentioned|p232|Permian|Permian|Underlies Skeletar Formation.||||||
26602|Gyarran Volcanics|45088|6|Mentioned|p59|||Permain succession||||||
26602|Gyarran Volcanics|45090|6|Mentioned|p25|||Early Sakmarian. Correlation||||||
26602|Gyarran Volcanics|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: Sydney Basin/Hunter Valley area.||||||
26602|Gyarran Volcanics|61529|5|Briefly described|p854 Fig. 1b|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: Sydney Basin.||||||
26602|Gyarran Volcanics|61791|6|Mentioned|p325|||||||||
26602|Gyarran Volcanics|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Early Permian. ||||Overlain by the Greta Coal Measures. Overlies Seaham Formation.||
26602|Gyarran Volcanics|68003|5|Briefly described|p38 Fig.3-j, p40.|Early Permian|Early Permian|Hunter Coalfield (Sydney Basin), Brigalow Belt South Bioregion. Correlative of Werrie Basalt in Gunnedah and Werrie Basins. Thick volcanic sequence.||Unit in Dalwood Group.||||
26602|Gyarran Volcanics|68004|5|Briefly described|p23 Table 1, p51 Table 5.|||Hunter Coalfield. Is coeval with Dalwood Group. Equivalent to Boggabri Volcanics and Werrie Basalt in Gunnedah Basin.||||Overlies Seaham Formation. Is overlain by Greta Coal Measures.|Felsic to mafic volcanics and pyroclastics.|
26602|Gyarran Volcanics|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|||Unit in Dalwood Group.|Includes Lochinvar, Allandale, Rutherford and Farley Formations.|||
26602|Gyarran Volcanics|70791|5|Briefly described|p277, p293 Fig.17|Cisuralian|Cisuralian|Hunter Coalfield.||Dalwood Group.||||
26602|Gyarran Volcanics|73304|6|Mentioned|p75, p78||||||Farley Formation, Rutherford Formation, Allandale Formation, Lochinvar Formation|||
27044|Haedon Formation|22736|6|Mentioned|p629||Ordovician|||||||
27044|Haedon Formation|22750|5|Briefly described|p 228||Ordovician|||||||
27044|Haedon Formation|22857|4|Described|p434 App. 1 Tb. A1.5|Late Ordovician|Early Ordovician|Reworked limestone; massive bedded and oolitic limestone. Max. thickness: 150m. Geological Province: New England Fold Belt. ||||||
27044|Haedon Formation|23185|6|Mentioned|Fig1p156|||||||||
27044|Haedon Formation|41347|4|Described|Table 3|||||||||
27044|Haedon Formation|41348|5|Briefly described|Map legend|Ordovician|Cambrian|In the Tamworth Belt.||||||16-DEC-04
27044|Haedon Formation|41796|6|Mentioned|p304|||||||||
27044|Haedon Formation|42554|6|Mentioned|p35|||||||||
27044|Haedon Formation|44093|5|Briefly described|p227 App. 1|Ordovician|Cambrian|Geological Province: New England Fold Belt.||||||
27044|Haedon Formation|47056|6|Mentioned|Fig.2 P523|||||||||
27044|Haedon Formation|50094|3|Fully described|p315, p316 Fig.1, p317 Fig.2|Llanvirn|Arenig|Conglomerates, sandstone and intercalated limestone beds. Contains biostratigraphically important conodonts. Max. thickness: 100m. Unconformably overlies Pipeclay Creek formation. Unconformably overlain by Drik Drik Fm. Geol. Prov: New England Fold Belt.||||||23-JUN-06
27044|Haedon Formation|50168|6|Mentioned|p157 Fig.2|||Gamilaroi Terrane.||||||
27044|Haedon Formation|60417|6|Mentioned|p159|Middle Ordovician|Middle Ordovician|Contains conodonts.||||||
27044|Haedon Formation|61392|5|Briefly described|p165 Fig. 2|Gisbornian|Dariwillian|In the Gamilaroi terrane.||||||07-FEB-11
27044|Haedon Formation|67322|4|Described|Fig.5; p27|Darriwilian|Darriwilian|Tamworth Belt, New England Orogen. Of Cawood (1983). Maximum thickness is approximately 100m. Conodonts indicate a Darriwilian age for this formation. Occurs in the Tamworth-Neminha region.||||Unconformably overlain by the Drik Drik Formation. Unconformably overlies the Pipeclay Creek Formation.|Sandstones and boulder conglomerates with clasts of limestone, mudstone, basalt and andesite. Autochthonous massive and bedded limestones are intercalated with the conglomerates.|22-FEB-18
27044|Haedon Formation|68005|5|Briefly described|p49 Fig.3-M, p50, p51 Photo.3-J,K, p151.|Middle Ordovician|Middle Ordovician|Tamworth Belt. Deep marine sedimentary rocks: carbonate bank and submarine canyon deposits.||||Unconformably overlies Pipeclay Creek Formation.|Polymictic conglomerates, including more-or-less rounded extraformational clasts (granite, limestone, jasper and green argillite) and angular intraformational clasts (andesitic volcaniclastics); sedimentary breccia with angular clasts.|
27044|Haedon Formation|68822|5|Briefly described|p332|||Unconformably underlain by Cambrian argillite.||||Unconformably overlain by the Drik Drik Formation. Unconformably underlain by the Murrawong Creek Formation.|Consists of arc-derived andesite and basalt detritus in conglomerates and siltstones, ~ 100 m thick, which are interbedded with Middle Ordovician (Darriwilian 2-3, i.e. 470-463 Ma; Sadler et al. 2009) bedded and allochthonous limestone.|
37319|Halls Peak Volcanics|24011|6|Mentioned|p419|||||||||
37319|Halls Peak Volcanics|61914|5|Briefly described|p163|Permian|Permian|Sequence of moderately deformed, low-grade metamorphosed, felsic volcaniclastic and sedimentary rocks.||||||
37319|Halls Peak Volcanics|70096|6|Mentioned|p221-222|||Geological province: New England Orogen. Of Gunnedah Basin. SHRIMP U-Pb ages from volcanic samples indicate a Sakmarian age.||||||
37319|Halls Peak Volcanics|73197|6|Mentioned|p472 Tb.2|Sakmarian|Asselian|New England Orogen, southern.|295.3 +/- 2.0 Ma U-Pb zircon|||||
37319|Halls Peak Volcanics|73202|5|Briefly described|p626, p627 Fig.1, p639 Fig.10|Early Permian|Early Permian|New England Orogen, southern. I-type, mixed arc to depleted rift geochemical signature. Magmatic zircon age (SHRIMP) of 292.6 +/- 2.0 Ma.|295.7 +/- 2.2 Ma, 292.6 +/- 2.0 Ma||||Volcanic rocks.|
82492|Hannam Vale Granodiorite|71628|5|Briefly described|p17: 2, 74-75|||New name. A small (~9 km2) intrusion just W of Hannam Vale village.||The Brothers Suite.||Intrudes Camden Haven Group, Cowangara and Pappinbarra Formations.|Porphyritic microgranodiorite.|
28596|Happy Valley Granite|34544|5|Briefly described|p187|||||||||
28596|Happy Valley Granite|40328|4|Described|p207|||||||||
28596|Happy Valley Granite|45087|5|Briefly described|p39|||Chemical analyses||||||
28596|Happy Valley Granite|60086|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Maragle Bathylith (Batholith?).||||||07-NOV-08
25943|Harrisons Peak Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Biotite granite. BMR map symbol: gbx.||||||
25943|Harrisons Peak Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
25943|Harrisons Peak Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
25943|Harrisons Peak Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
25943|Harrisons Peak Granite|32820|6|Mentioned|p3|||Within Cullarin Anticlinorium||||||
25943|Harrisons Peak Granite|33325|6|Mentioned|PP18|||? pt. of Michelago Gp.||||||
25943|Harrisons Peak Granite|36413|2|Defined|p107|Early Devonian|Early Devonian|||||||
25943|Harrisons Peak Granite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite, massive, homogenous, medium grained. GSNSW map code: gh.||||||
25943|Harrisons Peak Granite|39800|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25943|Harrisons Peak Granite|40328|4|Described|p207|||||||||
25943|Harrisons Peak Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
25943|Harrisons Peak Granite|48878|4|Described|p.11,15,20,30,Pl.3|||Silurian-Devonian (Bowning Orogeny). (I55-16).||||||
25943|Harrisons Peak Granite|71069|4|Described|p10, p21 fig 7, p28, p39 fig 16|Ludlow|Wenlock|Named for Harrisons Peak. Previously referred to as the Harrisons Peak Massive Microcline Granite, the Harrison's Peak Granite before formal definition of the current name. May be compositionally equivalent to the Watch Box Granite. Age constrained by unit relationships and correlations. Petrography briefly discussed. Distribution, geomorphology, primary textures, geochemistry, tectonic structure, metamorphism and geophysical characteristics discussed. See also p200 fig 74, p201-p202. ||||Overlain by the Kohinoor Volcanics. Equivalent to the Urialla and Tinderry Granites. Intrudes the Abercrombie Formation.|Grey, cream to pink, medium to coarse grained, massive, equigranular biotite microcline granite.|
25943|Harrisons Peak Granite|71691|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped. Three facies variations are mapped separately.|||||Grey, cream to pink, medium- to coarse-grained, massive biotite granite.|
26606|Hartley Granite|42726|5|Briefly described|map legend|Carboniferous||24. Of the Hartley Suite.  Variation on the informal Hartley granodiorite.  Not intended as a formal name.||||||07-FEB-05
26606|Hartley Granite|73582|6|Mentioned|p119|||Joplin (1931).||||||
31451|Hartley Suite|42726|5|Briefly described|Map legend|Carboniferous|Carboniferous|Of the Bathurst Supersuite.  Includes the Wallerawang, Lett, Blaxland, Hartley Granites.||||||07-FEB-05
38464|Harts Paddock Diorite|24133|3|Fully described|p76|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
28130|Hartwood Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Ashflow unit. Max. thickness: 200m. Geological Province: Kopyje Shelf (Darling Basin).||||||
28130|Hartwood Tuff Member|23171|6|Mentioned|p31|||||||||
28130|Hartwood Tuff Member|23173|6|Mentioned|Map Legend|||||||||
28130|Hartwood Tuff Member|35287|6|Mentioned|p7|||||||||
28130|Hartwood Tuff Member|39618|2|Defined|p51|Early Devonian|Early Devonian|||||||
28130|Hartwood Tuff Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
28130|Hartwood Tuff Member|41528|2|Defined|p41|Early Devonian||||||||
28130|Hartwood Tuff Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
28130|Hartwood Tuff Member|42566|5|Briefly described|p69|||Baledmund Formation, Nymagee 1:100 000 sheet.||||||
78899|Hatchery Creek Group|67823|4|Described|p355-p368|Middle Devonian|Emsian|Of the Burrinjack area of NSW. New name; of Hunt and Young (2010). Previously Hatchery Creek Conglomerate"". ~1800m thick, forms an isolated outcrop of some 70km^2 near Wee Jasper, mostly lying on the Brindabella 1:100k map sheet. Maximum age constrained (Late Devonian) by invertebrate fauna in the underlying Murrumbidgee Group. Contains the placoderm: Sherbonaspis hillsi (Middle Devonian). Deposited in a humid alluvial fan environment. Type section at Cave Creek Road.|||Includes Corradigbee Formation, Wee Jasper Formation.|Disconformably underlain by the Murrumbidgee Group.||08-MAY-20
78899|Hatchery Creek Group|68592|4|Described|p73, p987-8, p1193-1202, p1907-8|Middle Devonian|Early Devonian|Originally Hatchery Creek Conglomerate of Joplin et al. (1953). Subsequent work divided this unit into two Formations and elevated it to Group status (Hunt and Young, 2010). Extended type section described. 1760m thick. Taemas structural zone: deformation described. Fossil fauna described.|||Includes Wee Jasper and Corradigbee Formations.|Overlies Taemas Limestone.||
78899|Hatchery Creek Group|70192|5|Briefly described|Map Legend|Emsian|Emsian|On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Wee Jasper Formation.|Overlies Taemas Limestone (Murrumbidgee Group).||
78899|Hatchery Creek Group|70540|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Wee Jasper Formation.|||
78899|Hatchery Creek Group|71656|4|Described|p12 Fig.2, p38|Eifelian|Emsian|Outcrop of the Hatchery Creek Group is largely confined to the Brindabella 1:100,000 mapsheet, where it is bounded by the Goodradigbee Valley to the east, the Burrinjuck Granite to the west, and Burrinjuck Reservoir to the north.|||Includes Wee Jasper Formation and Corradigbee Formation.|Overlies Murrumbidgee Group.|Including conglomeratic and sandstone facies and calcareous nodular mudstone.|
78899|Hatchery Creek Group|73215|5|Briefly described|p993, 995|Middle Devonian|Middle Devonian|Appears as Hatcherys Creek Group on p993.||||||
23644|Hathaway Conglomerate Member|22857|5|Briefly described|p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Burthong Formation (Mouramba Group, Cobar Supergroup). Max. thickness: 150m. Geological Province: Mouramba Shelf.||||||
23644|Hathaway Conglomerate Member|41528|2|Defined|p62|Early Devonian||||||||
23644|Hathaway Conglomerate Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
23644|Hathaway Conglomerate Member|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
23644|Hathaway Conglomerate Member|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Mouramba Group||||
80190|Hawks Nest beds|70217|5|Briefly described|p27|Devonian|Devonian|New England Orogen.||||Intruded by the Mount Ephraim Granodiorite.|Shale and greywacke.|
31589|Hawksview Suite|42726|5|Briefly described|map legend||Silurian|||||||
75829|Haydonville serpentinite|65317|5|Briefly described|p633-635, p622 Fig. 1c, p635 Fig. 14|Early Permian|Late Carboniferous|Appears to be an informal name for small lenses of serpentinite outcropping near Haydonville on the northern tip of the Hastings Block, New England Orogen.  Structures suggest Early Permian emplacement. Shown as Haydonville Serpentinite in figs.||||||
35616|Hazeldean Granodiorite|50231|5|Briefly described|Map Legend|Emsian|Pragian|||||||
35616|Hazeldean Granodiorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Dark grey, medium-grained, massive, porphyritic biotite-pyroxene? granodiorite.||||||25-JUN-08
35616|Hazeldean Granodiorite|68592|2|Defined|p1398, p1433-5|Early Devonian|Early Devonian|New unit and name, after Hazeldean property. A small arcuate body, 700m long and 100m wide. Crops out as small, rounded boulders and tors. Type locality described. No geochemical analysis, but assigned to the Gooramma Suite on the basis of mineralogy and petrophysics. Geophysical properties briefly described. Age from parent.||Unit in Gooramma Suite.||Intrudes Hawkins Volcanics (inferred).|Dark grey, medium-grained, massive, porphyritic granodiorite.|
35616|Hazeldean Granodiorite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgh. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Gooramma Suite|||Medium grained, massive, porphyritic granodiorite; high magnetic susceptibility.|
35616|Hazeldean Granodiorite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Medium grained, massive, porphyritic granodiorite; high magnetic susceptibility.|
37334|Hazeldene Sandstone|61964|2|Defined|p14 Fig. 4, p133|Frasnian|Frasnian|Of the Cocoparra Group. Fine- to medium-grained, moderately sorted, maroon sandstone with a significant detrital mica component. Overlies the basal Barrat Formation; conformably overlain by Edithvale Formation. See also p115, p117 Fig. 35.||||||
37334|Hazeldene Sandstone|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Medium- to fine-grained maroon quartz sandstone and minor pebbly sandstone, detrital mica.||||||
37334|Hazeldene Sandstone|69160|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.||Overlies Barrat Formation.|Medium- to fine-grained maroon quartz sandstone and minor pebbly sandstone, detrital mica.|
37334|Hazeldene Sandstone|71889|6|Mentioned|p50|||Outcrops near Ardlethan.|||||Fine sandstone and siltstone.|
37334|Hazeldene Sandstone|72083|5|Briefly described|p45|||A fine-grained recessive unit; one of few (listed) in the Group. A NE-dipping, laterally extensive unit across the NE corner of Ardlethan 1:100k sheet area. Crops out very poorly.||Cocoparra Group.||Overlies Ballast Formation. Probable correlative of Bogolong Formation (brief comment).|Medium-grained micaceous quartz sandstone; may include finer-grained lithologies that do not crop out.|
39364|Hazelgrove Formation|24123|5|Briefly described|p3|Devonian|Silurian|Geological Province: Sydney Basin.||||||
37912|Hazelvale Rhyodacite Member|24605|2|Defined|p933 Fig.2, p952 App.1|Namurian|Namurian|Of the Rocky Creek Conglomerate. Thickness at type locality: 5m. Geological Province: New England Orogen.||||||
37912|Hazelvale Rhyodacite Member|61214|5|Briefly described|p171 Fig. 1|Namurian|Namurian|Of the Rocky Creek Conglomerate. Geological Province: Darthula Block. See also p172 Fig. 2.  Presented only as Hazelvale in text of figure.||||||23-JAN-06
73653|Henleigh Siltstone|63279|4|Described|p167, p176-177|Bendigonian|Early Ordovician|Underlain conformably by Mitchell Formation. Thickness: ~310m. Contains Bendigonian graptolite fauna. Geol Prov: Molong Volcanic Belt. Consists of  laminated siltstone and shale, interbedded with volcaniclastic Sst and Conglom. See also p176-177.||||||
23648|Hennings Tank Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Ash flow unit. Geological Province: Kopyje Shelf (Darling Basin).||||||
23648|Hennings Tank Tuff Member|41528|2|Defined|p40|Early Devonian||||||||
23648|Hennings Tank Tuff Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
82497|Henry River Monzogranite|71628|4|Described|p3: 1, 4, 51-55; p8-92|||Originally Henry River Granite (Pogson and Hitchins, 1973); renamed here. Located ~30 km ESE of Glen Innes. The pluton's irregular outcrop is described. Dating has disproved Weber et al. (1978)'s interpretation that this unit intrudes Kingsgate Syenogranite. Limited geochemistry described.|293.1 +/- 5.1 Ma (Rosenbaum et al., 2012).|Henry River Suite.||Intrudes Sara beds. Is intruded by Red Range Microleucogranite. Is overlain by Wandsworth Volcanic Group.|Grey-blue, texturally heterogeneous, fine- to medium-grained biotite monzogranite-granodiorite; locally amphibole bearing; weakly to strongly foliated. S-type.|
77368|Herndale Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
82470|Herries Monzogranite|71628|4|Described|p19: 58-60, 62-71|||Brown et al. (2007). This name underwent several changes; now part of Granite Hills Complex. Named after the Herries Range. Crops out 20 km SW of Warwick. Deeply weathered and poorly exposed except in hilly country where it forms boulders, tors and whalebacks. Geochemistry described; assigned to Herries Suite. Is associated only with a single base metal deposit.|251.8 +/- 2.5 Ma (SHRIMP: Li et al., 2012).|Granite Hills Complex.||Intrudes Texas beds and Risdon Stud Formation. Abuts Fairleigh Monzogranite. Is overlain by the Marburg Formation.|Pale pink to greyish pink, medium- to coarse-grained, slightly to moderately porphyritic hornblende-biotite monzogranite; minor tonalite. I-type.|
25947|Hervey Group|22472|6|Mentioned|p49|Devonian|Devonian|||||||
25947|Hervey Group|22519|5|Briefly described|p8|Late Devonian|Late Devonian|||||||
25947|Hervey Group|22638|3|Fully described|p70|Famennian|Frasnian|Overlies Cootamundra Group.||||||15-JUL-08
25947|Hervey Group|22761|6|Mentioned|p355|||Geological Province - Lachlan Fold Belt.||||||
25947|Hervey Group|22831|2|Defined|p 74|Late Devonian|Early Devonian|||||||
25947|Hervey Group|22857|5|Briefly described|p213, p217, p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Formerly divided into "Bearmagil", "Nangar" and "Cookamidger Subgroups" by Conolly (1965a) but not recognised in recent mapping of subgroups. Max. thickness: 1615m. Geological Province: Hervey Basin. ||||||
25947|Hervey Group|22859|5|Briefly described|p213,217|||Consists of: Beargamil, Nangar and Cookamidgera Subgroups (Conolly 1965a).||||||
25947|Hervey Group|23053|6|Mentioned|p69||Late Devonian|||||||
25947|Hervey Group|23099|5|Briefly described|p582 (Fig 2)||Devonian|||||||
25947|Hervey Group|23214|2|Defined|p225|Late Devonian|Late Devonian|Consists of red sandstone/siltstone and mudstone sequences seperated by a thick sequence of red and white quartzitic sandstone and red siltstone. Max. thickness 1600m.||||||04-MAR-09
25947|Hervey Group|23217|5|Briefly described|p1-3|Famennian|Givetian|(Conolly, 1965b). Includes Mandagery Formation, Bumberry and Eurow Formations.  Overlies Moura Formation.||||||08-MAR-06
25947|Hervey Group|23309|6|Mentioned|p390|||||||||
25947|Hervey Group|23366|5|Briefly described|p13 fig.8|Devonian|Devonian|||||||
25947|Hervey Group|23392|2|Defined|p3|Late Devonian|Middle Devonian|Defined by Conolly (1965). Max Thickness: 1500m.||||||25-JUN-08
25947|Hervey Group|23522|5|Briefly described|p249 Fig 5||Late Devonian|||||||
25947|Hervey Group|24005|5|Briefly described|p293|Late Devonian|Middle Devonian|||||||
25947|Hervey Group|24007|4|Described|p330|Late Devonian|Late Devonian|||||||
25947|Hervey Group|24125|5|Briefly described|p3|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
25947|Hervey Group|24230|6|Mentioned|p173 Fig.2|||||||||
25947|Hervey Group|24233|5|Briefly described|p256, p258 Fig.6|Devonian|Devonian|Geological Province: Lachlan Orogen.||||||
25947|Hervey Group|24267|5|Briefly described|p1508|||Underlying Unit: Milpose Volcanics. Geological Province: Parkes-Narromine Belt||||||
25947|Hervey Group|24317|5|Briefly described|p14, p15 Fig.1|Late Devonian|Late Devonian|Fluvial (to shallow marine) sedimentary rocks.||||||
25947|Hervey Group|24334|5|Briefly described|p48 Tb.1|Famennian|Famennian|Age: 363 - 367 Ma.||||||
25947|Hervey Group|24417|3|Fully described|p125|Late Devonian|Late Devonian|||||||
25947|Hervey Group|24424|5|Briefly described|p539 Tb.4|Late Devonian|Late Devonian|Age: 354-365 Ma. Palaeomagnetic poles given.||||||04-FEB-05
25947|Hervey Group|24580|5|Briefly described|p827|Late Devonian|Late Devonian|Unconformably overlies the Young Granodiorite and the Eugowera Suite. Geological Province: Eastern Lachlan Fold Belt.||||||
25947|Hervey Group|29452|6|Mentioned|p218|||Late Devonian||||||
25947|Hervey Group|29453|6|Mentioned|p26|||||||||
25947|Hervey Group|29682|4|Described|p15|||||||||
25947|Hervey Group|29907|6|Mentioned|Fig.15|||||||||
25947|Hervey Group|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25947|Hervey Group|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25947|Hervey Group|29987|4|Described|p24|||||||||
25947|Hervey Group|29989|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25947|Hervey Group|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
25947|Hervey Group|30071|6|Mentioned|p373|||||||||
25947|Hervey Group|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
25947|Hervey Group|30793|6|Mentioned|p85|||||||||
25947|Hervey Group|31161|5|Briefly described|PA5|||||||||
25947|Hervey Group|32087|4|Described|p16|||||||||
25947|Hervey Group|32483|4|Described|p37|||U.Dev. Table 1||||||
25947|Hervey Group|32585|6|Mentioned|p211|||U.Dev.||||||
25947|Hervey Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25947|Hervey Group|32672|6|Mentioned|p674|||||||||
25947|Hervey Group|32865|5|Briefly described|p484|||Refers Conolly (1965)||||||
25947|Hervey Group|32986|5|Briefly described|p7|||U.Dev.||||||
25947|Hervey Group|33006|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25947|Hervey Group|33121|5|Briefly described|p90|||Refers Conolly (1965). ?Mid-Late Dev.||||||
25947|Hervey Group|33269|6|Mentioned|p46|||Refers Conolly (1965). Kaolinite||||||
25947|Hervey Group|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25947|Hervey Group|33285|5|Briefly described|p21|||||||||
25947|Hervey Group|33326|6|Mentioned|p442|||Fauna.||||||
25947|Hervey Group|33732|5|Briefly described|p114|||Table II||||||
25947|Hervey Group|33833|6|Mentioned|p401|||||||||
25947|Hervey Group|34109|3|Fully described|p161|||Red beds.||||||15-JUL-08
25947|Hervey Group|34403|6|Mentioned|p141|||Devonian. Mention P143,P148.||||||
25947|Hervey Group|34405|6|Mentioned|p125|||||||||
25947|Hervey Group|34406|6|Mentioned|p223|||||||||
25947|Hervey Group|34449|6|Mentioned|p128|||||||||
25947|Hervey Group|35070|2|Defined|p123|Late Devonian|Late Devonian|||||||
25947|Hervey Group|35072|6|Mentioned|p363|||||||||
25947|Hervey Group|35128|6|Mentioned|p361|||Appears on figure||||||
25947|Hervey Group|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25947|Hervey Group|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25947|Hervey Group|35244|6|Mentioned|p36|||||||||
25947|Hervey Group|35386|6|Mentioned|p59|||||||||
25947|Hervey Group|35609|4|Described|p11|||||||||
25947|Hervey Group|36066|4|Described|p10|||See also p4.||||||31-MAR-20
25947|Hervey Group|36534|6|Mentioned|p225|||||||||
25947|Hervey Group|37529|6|Mentioned|p13|||||||||
25947|Hervey Group|38368|6|Mentioned|p314|||||||||
25947|Hervey Group|38593|6|Mentioned|p87|||||||||
25947|Hervey Group|38899|6|Mentioned|p71|||||||||
25947|Hervey Group|39214|5|Briefly described|p17|||||||||
25947|Hervey Group|40130|6|Mentioned|p195|||||||||
25947|Hervey Group|40328|6|Mentioned|p205|||See also P213 and Plate3||||||
25947|Hervey Group|40365|6|Mentioned|p243|||See also Fig.13||||||
25947|Hervey Group|40791|5|Briefly described|p183|||||||||
25947|Hervey Group|40891|6|Mentioned|p17|||||||||
25947|Hervey Group|41869|5|Briefly described|p5|||||||||
25947|Hervey Group|42073|6|Mentioned|p293|||||||||
25947|Hervey Group|42141|6|Mentioned|p568|||||||||
25947|Hervey Group|42262|6|Mentioned|Fig. 2 P1810|||||||||
25947|Hervey Group|42313|6|Mentioned|p179|Late Devonian||||||||
25947|Hervey Group|42449|6|Mentioned|p10|||||||||
25947|Hervey Group|42489|5|Briefly described|Map legend|Carboniferous|Late Devonian|||||||
25947|Hervey Group|42566|6|Mentioned|p100|||||||||
25947|Hervey Group|42714|6|Mentioned|p24|||||||||
25947|Hervey Group|42921|5|Briefly described|p7|||||||||
25947|Hervey Group|43263|6|Mentioned|Map Legend|Early Carboniferous|Middle Devonian|||||||
25947|Hervey Group|43277|5|Briefly described|Map Legend||Late Devonian|Of Lachlan Fold Belt.||||||04-MAR-09
25947|Hervey Group|43383|14|Not recorded|p15||Late Devonian|||||||
25947|Hervey Group|43389|14|Not recorded|Map Legend||Late Devonian|||||||
25947|Hervey Group|43430|14|Not recorded|p143,145|||U.Dev above Taemas Formation||||||
25947|Hervey Group|43441|4|Described|31||Late Devonian|Fish Plates found near base||||||08-JAN-10
25947|Hervey Group|43461|14|Not recorded|p620,tb.p621-22||Late Devonian|table p635. U/C on Murrumbidgee Group||||||
25947|Hervey Group|43479|14|Not recorded|p132,134||Devonian|||||||
25947|Hervey Group|43499|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
25947|Hervey Group|43500|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
25947|Hervey Group|43507|2|Defined|p123-166||Late Devonian|Divided into Beargamil, Nangar and Cookamidgera Subgroups (q.v.for constituent formations).||||||04-MAR-09
25947|Hervey Group|43508|14|Not recorded|p117,118,125-131|||Occurence of quartz||||||
25947|Hervey Group|43509|14|Not recorded|p111,114-5,117-9,|||Plates I,II||||||
25947|Hervey Group|43510|14|Not recorded|p37-83|||Detailed Stratigraphy||||||
25947|Hervey Group|43511|14|Not recorded|p129,140||Late Devonian|||||||
25947|Hervey Group|43513|14|Not recorded|p70-72|||Some red beds||||||
25947|Hervey Group|43516|14|Not recorded|Map Legend||Late Devonian|||||||
25947|Hervey Group|43640|5|Briefly described|Map Legend||Devonian|||||||
25947|Hervey Group|43642|5|Briefly described|Map Legend|Devonian|Devonian|Inculdes; Bumberry Formation, Cookamidgera Formation, Eurow Member, Hunter Siltstone, Pipe Formation, Kadina Formation, Mandagery Sandstone and Peaks Sandstone.||||||15-JUL-08
25947|Hervey Group|43755|6|Mentioned|Fig.9,p556|||||||||
25947|Hervey Group|43782|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
25947|Hervey Group|44093|5|Briefly described|p178 App. 1|Early Carboniferous|Late Devonian|In the Parkes Zone (Hervey Basin). Geological Province: Lachlan Fold Belt.||||||10-MAR-05
25947|Hervey Group|44160|5|Briefly described|Map Legend||Famennian|||||||08-JAN-10
25947|Hervey Group|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
25947|Hervey Group|44936|5|Briefly described|Map Legend||Late Devonian|||||||
25947|Hervey Group|45147|6|Mentioned|M315|||||||||
25947|Hervey Group|46522|5|Briefly described|p69|||||||||
25947|Hervey Group|46525|6|Mentioned|Fig.1 p143|||||||||31-MAR-20
25947|Hervey Group|46528|5|Briefly described|Map legend|Late Devonian||||||||
25947|Hervey Group|48958|6|Mentioned|p5|||||||||
25947|Hervey Group|50191|6|Mentioned|p6, 21 Fig. 1|Late Devonian|Late Devonian|||||||
25947|Hervey Group|50231|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Cookamidgera Subgroup, Nangar Subgroup, Beargamil Subgroup.||||||
25947|Hervey Group|50299|5|Briefly described|Map Legend|Devonian|Devonian|Overlies: Carawandool Volcanics, Kadungle Volcanics.||||||
25947|Hervey Group|50628|5|Briefly described|Map Legend|Devonian|Devonian|||||||05-JUL-04
25947|Hervey Group|60008|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Sediments.||||||08-JUL-04
25947|Hervey Group|60009|5|Briefly described|Map Legend|Famennian|Givetian|||||||13-JUL-04
25947|Hervey Group|60280|5|Briefly described|p2, p3 Fig. 1|||||||||
25947|Hervey Group|60423|5|Briefly described|p371 Fig. 2, 372 Fig. 3|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
25947|Hervey Group|60548|5|Briefly described|map legend|Devonian|Devonian|||||||
25947|Hervey Group|62349|5|Briefly described|p73|Late Devonian|Late Devonian|Fluvial and possibly deltaic sediments. Geological Province: Lachlan Fold Belt.||||||03-JUL-06
25947|Hervey Group|62569|5|Briefly described|p605, p606 Fig.1|Late Devonian|Late Devonian|Unconformably underlain by Derriwong and Trundle Groups. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
25947|Hervey Group|63289|6|Mentioned|p373 Fig. 7|Late Devonian|Late Devonian|||||||07-FEB-11
25947|Hervey Group|63291|6|Mentioned|p419 Fig. 2|||||||||
25947|Hervey Group|63605|6|Mentioned|p999, p1003|||In NSW. Contains Remigolepis fragments.||||||07-FEB-11
25947|Hervey Group|64238|5|Briefly described|Map legend|Devonian|Devonian|Subdivided into Nangar, Cookamidgera and  Beargamil Sungroups.||||||
25947|Hervey Group|64826|5|Briefly described|p1039 Fig. 2, p1046|Late Devonian|Late Devonian|Contains the Mandagery and Kadina Formations.||||||04-MAR-09
25947|Hervey Group|65214|6|Mentioned|p281|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
25947|Hervey Group|66499|6|Mentioned|p64, p66, p69|||Fish fauna found in several horizons. Phyllolepids now known in highest fish horizons||||||
25947|Hervey Group|66589|6|Mentioned|p180|Famennian|Frasnian|Case studies cited; not visited in the field by the authors of this study.||||||
25947|Hervey Group|66623|6|Mentioned|p438.|||Marine incursions in this unit were contemporaneous with deposition of the Wana Karnu Group.||||||
25947|Hervey Group|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|||||24-APR-12
25947|Hervey Group|67823|5|Briefly described|p355, p365-366|Late Devonian|Middle Devonian|Upper Devonian minimum age.|||||Volcanics and sediments.|
25947|Hervey Group|67847|5|Briefly described|p60 fig 3.3.4|||Lambie Basin. Of the authors' proposed Kanimblan cycle. ||||||
25947|Hervey Group|68295|6|Mentioned|p28-29 Fig. 2.2, p43|||Siluro-Devonian-Carboniferous, Li et al. (1988).||||||
25947|Hervey Group|68298|5|Briefly described|p216, p234, p235, p236||Late Devonian|Largely non-marine Late Devonian sediments of central and western NSW. Connolly (1965) recognised three major lithological sequences. Famennian Bothriolepis-phyllolepid-Remigolepis-Groenlandasapis associations of placoderms, distinguished here as Jemalong-Canowindra fauna and Grenfell fauna. Also includes tetrapods and lungfishes.|||A lower Beargamil Subgroup, a middle Nangar Subgroup, and an upper Cookamidgera Subgroup (Connolly, 1965).|Includes faunas considered both older and younger than Worange Point Formation fauna.||
25947|Hervey Group|68592|3|Fully described|p443, p957, p988, p1197-8, p1698-1721|Late Devonian|Late Devonian|See also p73, p232. Conolly (1965); named after the Hervey Range. His three Subgroups (Beargamil, Cookamidgera and Nangar) have become obsolete due to problems in correlation, but the Formations remain. One of a number of sequences (also Lambie and Catombal Groups) which were previously collectively referred to as "Lambie Series" and "Lambie Stage", following Browne (1929). c.1200-1400m thick. No fossils found in current work, but a prolific fish fauna occurs in the Mandagery Formation at Canowindra. Mis-spelt as Harvey on p1197. Correlated with Lambie and Catombal Groups. Binalong structural zone: deformation described.|||Includes Koorawatha, Bumberry, Mandagery and Bendick Formations (in Goulburn 250 area); also Hunter Formation.|Overlies Young Granodiorite, Karoopa Granite nonconformably; Hawkins, Warrangong Volcanics and (locally) Douro Group unconformably. Faulted against Mountain Creek Volcanics and Crowther Monzodiorite.|Red and white, fine-grained sandstones and red siltstones with subordinate coarse-grained sandstones and conglomerate.|
25947|Hervey Group|70192|5|Briefly described|Map Legend|Famennian|Frasnian|On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Bendick Formation, Mandagery Formation, Bumberry Formation, Koorawatha Formation.||Composed primarily of quartzose-lithic quartz, quartz lithic sandstones and siltstones with some polymictic, massive and pebbly conglomerate in this area.|
25947|Hervey Group|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
25947|Hervey Group|70297|4|Described|map legend, on side 2 of map sheet|Famennian|Frasnian|Erosional base.|||Bumberry Formation, Eurow Formation, Hunter Formation, Pipe Formation, Kadina Formation, Mandagery Formation, Peaks Formation|With Lambie and Catombal Groups, overlies Dulladerry Volcanics.|Terrigenous to shallow marine, red to white and green, quartzose to lithic sandstone, siltstone, shale and conglomerate; sandstones commonly thick-bedded and massive to cross-stratified.|
25947|Hervey Group|70545|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Bumberry Formation, Bendick Formation, Koorawatha Formation, Mandagery Formation.||Composed primarily of quartzose-lithic quartz, quartz lithic sandstones and siltstones with some polymictic, massive and pebbly conglomerate in this area.|
25947|Hervey Group|70684|5|Briefly described|p25-26|Late Devonian|Late Devonian|||||Unconformably overlies Fairbridge Volcanics.|Includes fluviatile sandstone.|
25947|Hervey Group|71040|5|Briefly described|p12 Fig.7, p15-18, p25|Late Devonian|Late Devonian|Central NSW. Association with the Springdale Fault discussed.|||Weddin Sandstone, Cloughlan Shale.|Unconformably overlies Carawandool Volcanics and Wallingalair Group.||
25947|Hervey Group|71656|6|Mentioned|p12 Fig.2|Famennian|Frasnian|Shown only in correlation chart (Fig.2).|||Koorawatha Formation, Bumberry Formation Mandagery Formation, Bendick Formation.|Unconformably overlying Hatchery Creek Group.||
25947|Hervey Group|72082|6|Mentioned|p4|Devonian|Devonian|||||||
25947|Hervey Group|72084|5|Briefly described|p2, p39, p40 Fig.42, p49-54, p56|Late Devonian|Late Devonian|Temporal equivalents occur in the Curraburrama State Forest; lithologies described in detail; photographs; geochemical plots. An ignimbrite unit there is interpreted as an extrusive counterpart to the Narraburra Suite.  Interpreted to have been folded during the Carboniferous Kanimblan Orogeny.|c.368 Ma (Bodorkos, pers. comm. 2016).||||Thin-bedded to laminated quartz sandstone to siltstone; medium to thick-bedded, ferruginous lithic-quartz sandstone; (A-type) rhyolitic, coarse-tuff to lapilli-tuff; lithic sandstone, pebbly sandstone and pebble to cobble conglomerate.|29-AUG-19
25947|Hervey Group|72495|5|Briefly described|p217, 219, p226, 229, p235, 239, 241|Late Devonian|Late Devonian|Occurs as scattered outcrop in the core of the Tullamore Syncline. Appears in geophysics as a linear gravity low between the two highs in the Junee-Narromine Volcanic Belt. Modelling in one area suggests this group is 3.75km thick which is notably thicker than the interpreted 2km thickness for widely scattered outcrops.||||Thrusted under the Nyngan Intrusive Complex. In fault contact with the Raggatt Volcanics.|Fluvial sandstone, conglomerate, siltstone and mudstone.|31-MAR-20
25947|Hervey Group|73457|6|Mentioned|p2, p14|Late Devonian|Late Devonian|||||||
25055|Hexham Subgroup|22969|5|Briefly described|p 40|||Tomago Coal Measures||||||
25055|Hexham Subgroup|42214|6|Mentioned|Table 1 P462|||||||||
25055|Hexham Subgroup|43017|6|Mentioned|p379|||||||||
23649|Hianana Volcanics|22857|5|Briefly described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|Part of the Coombadhja Volcanic Complex within the Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
23649|Hianana Volcanics|23443|4|Described|p417|||||||||
23649|Hianana Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Coombadjha Volcanic Complex.  Volcanic breccia composed of block-sized fragments of porphyry; massive porphyritic lava with plagioclase phenocrysts and bedded volcaniclastic units composed of angular volcanic lithic and crystal fragments.||||||20-DEC-04
23649|Hianana Volcanics|23812|5|Briefly described|p29 Tb.3|Late Permian|Early Permian|Of Coombadjha Volcanic Complex. Maximum thickness: 200m.||||||
23649|Hianana Volcanics|23859|5|Briefly described|p937|||Of Coombadjha Volcanic Complex. Geological Province: New England Fold Belt.||||||
23649|Hianana Volcanics|41041|3|Fully described|p261|||||||||
23649|Hianana Volcanics|42378|5|Briefly described|Table 1 P6|||Coombadjha Volcanic Complex.||||||
23649|Hianana Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Coombadjha Volcanic Complex.||||||
23649|Hianana Volcanics|71628|5|Briefly described|p19:128|||||Coombadjha Volcanic Complex.||Is bounded by Moonta Gully Monzogranite.||
37297|High Valley andesite tuff|24010|6|Mentioned|p379|||Informal name.||||||
37297|High Valley andesite tuff|24603|6|Mentioned|p897 Fig. 17, p898|||Informal name.  Geological Province: Tamworth Belt.   In the Rocky Creek Block.||||||
37297|High Valley andesite tuff|60299|6|Mentioned|p231 Fig. 12|Carboniferous|Carboniferous|Informal. Of the Caroda Formation.||||||
37297|High Valley andesite tuff|65107|6|Mentioned|Fig 11, 286-7|Carboniferous|Carboniferous|Shown in a Carboniferous age pole path for Tamworth Belt rocks, Rocky Creek Block.||||||
27084|Hillcrest Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Babinda Volcanics (Kopyje Group, Cobar Supergroup). Max. thickness: 700m. Geological Province: Kopyje Shelf (Darling Basin).||||||
27084|Hillcrest Tuff Member|23173|6|Mentioned|Map Legend|||||||||
27084|Hillcrest Tuff Member|35287|6|Mentioned|p7|||||||||
27084|Hillcrest Tuff Member|39618|1|Redefined|p56|Early Devonian|Early Devonian|||||||
27084|Hillcrest Tuff Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27084|Hillcrest Tuff Member|41528|2|Defined|p46|Early Devonian||||||||
27084|Hillcrest Tuff Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
27084|Hillcrest Tuff Member|42566|4|Described|p53|||||||||
27084|Hillcrest Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
76953|Hillgrove Monzogranite|69639|6|Mentioned|p217|Artinskian|Artinskian||288 +/- 2.9 Ma (SHRIMP U-Pb)|Hillgrove Suite||||
76953|Hillgrove Monzogranite|71628|4|Described|p1: 14; p2: 9-10, 12, 62; p3: 1, 4, 6-8|||See also p3: 12, 24, 32, 56-60, 62. Ashley et al. (2007). Originally Hillgrove Blue Granite and Hillgrove Adamellite. Named after the local village 20 km E of Armidale. Generally poor outcrops of sparse rubbly piles and pavements. Spatial and temporal relationships with Bakers Creek Complex are unclear: various accounts given. Compositionally diverse geochemistry described in some detail. Associated with abundant (194 deposits) Sb-Au(W) deposits in the Hillgrove-Metz area; not genetically related to the intrusion. Other age determinations given; problems in dating zircon cores/rims discussed.|288 +/- 2.9 Ma (Rosenbaum et al., 2012).|Hillgrove Suite.||Intrudes Girrakool beds. Is adjacent to (?abuts) Baker Creek Diorite.|Massive to strongly foliated, medium- to coarse-grained, equigranular to porphyritic biotite monzogranite with minor granodiorite; locally amphibole-bearing and, independently, garnet-bearing; graphite locally evident.|
76953|Hillgrove Monzogranite|71703|6|Mentioned|p203, 204, p193 Fig 1, |||Note two different and separately dated samples  are among the oldest and youngest parts of the supersuite, indicating that some plutons are likely composite. Prob. location 294 Fig.  1 (Jeon et al., 2014) age 297.2+/-4.2 Ma.|Ages ~297 Ma, ~288 Ma.  |Of Hillgrove Supersuite.||||
76953|Hillgrove Monzogranite|73264|6|Mentioned|p1398|||||||||
67847|Hillgrove Supersuite|24513|5|Briefly described|p9|Late Carboniferous|Late Carboniferous|Intensely foliated S-type granite. Age: ~303Ma. Within southern New England Orogen.||||||
67847|Hillgrove Supersuite|62757|5|Briefly described|p1-2|Early Permian|Late Carboniferous|Plutonic suite of the New England Batholith. Includes Bakers Creek Diorite Complex. Age: ~300Ma. S-type granitoid.||||||07-FEB-11
67847|Hillgrove Supersuite|68005|6|Mentioned|p20, p60.|Early Permian|Late Carboniferous|Part of New England Batholith. Formerly a suite of Shaw and Flood (1982); redefined as a Supersuite by Bryant (2001). S-type.||||||
67847|Hillgrove Supersuite|68006|5|Briefly described|p27. |Early Permian|Late Carboniferous|New England Batholith, New England Fold Belt. Of Bryant (2001). S-type.||||||
67847|Hillgrove Supersuite|68679|5|Briefly described|p461|||Granitoids of this and the Uralla Supersuite separate the northern and southern parts of the Stanthorpe Supersuite.|||Hillgrove Suite.|||
67847|Hillgrove Supersuite|69188|5|Briefly described|p32|Permian|Permian||||Abroi Granodiorite.|||
67847|Hillgrove Supersuite|69639|5|Briefly described|p1, p3, p100, p112, p145, p217|Early Permian|Early Permian|New England Orogen. S-type supersuite.|||Includes the Hillgrove Suite and the Murder Dog Suite.|||
67847|Hillgrove Supersuite|70939|6|Mentioned|p823||||c.292 Ma.|||||
67847|Hillgrove Supersuite|71628|4|Described|p1:1, 6, 8, 11, 14, 18; p2:1-3, 5-6, 10|Permian|Permian|See also p2: 15, 22-26, 37, 39, 42, 46, 48, 52-55, 60, 62-64, 68-69, 71; p3: 1-99; p4-6; p5-1; p7-4; p8-3; p14-1; p17: 13, 32, 48-49; p19: 74-76, 152-155, 165. Blevin and Chappell (1993), Landenberger (1996). Southern New England Orogen. Generated in a variety of arc-related settings. Spatially associated with Bakers Creek Supersuite. A series of weakly to strongly deformed S-type granites. Age determination problems discussed in great detail. Geochemistry described. CONSTITUENTS (cont.): Mirani, Murder Dog, Rockvale, Shallow Lagoon, Tobermory, Winterbourne Monzogranites; Ingleba Leucomonzogranite; Abroi, Argyll, Dundurrabin, Tia Granodiorites. Also Abroi, Argyll, Blue Nobby, Campfire, Dundurrabin, Eastlake, Enmore, Gara, Garibaldi, Gleniffer, Gostwyck, Henry River, Kilburnie Suites.|300-290 Ma.||Blue Nobby, Campfire, Eastlake, Enmore, Gara, Garibaldi, Gleniffer, Gostwyck, Henry River, Hillgrove, Kilburnie, Kimberley Park, Kookabookra Monzogranites. See COMMENTS for more.||Mainly S-type granites, typically medium- to fine-grained, equigranular to mildly porphyritic (microcline), and commonly blue-grey (from opalescent blue quartz). Weakly to moderately deformed.|
67847|Hillgrove Supersuite|71703|4|Described|p191-194, 198, 202-205|Early Permian|Late Carboniferous|Main pulse of magmatism ~291 Ma (from 18 of 24 dated constituents). Hf isotope geochron p204. 288 Ma, Rosenbaum et al., 2012. Previously Hillgrove Plutonic Suite.||Of New England Batholith.|Includes Abroi Granodiorite, Tobermory, Rockvale, Hillgrove, Murder Dog, Blue Knobby Monzogranites, Tia Granodiorite, Cheyenne complex, Kilburnie Monzogranite, Dundurabbin, Wollomombi Granodiorite.||S-type granite plutons; biotite bearing granodiorite and monzogranite|
67847|Hillgrove Supersuite|72078|6|Mentioned|p5|||Geological province: New England Orogen. Unfractionated S-type granitic supersuite that is not prospective for Sn mineralisation.||||||
67847|Hillgrove Supersuite|73197|6|Mentioned|p471, 472 Tb.2|Artinskian|Kasimovian|New England Orogen, southern. Geosynchronous with rifting, intrudes accretionary wedge, S-type. [Written only as Hillgrove on p742 Tb.2, could be Hillgrove Suite?]. U-Pb zircon ages from Cawood et al., (2011a), Chisholm et al., (2014b), Craven et al., (2012), Jeon et al., (2014), Kemp et al., (2009), Kent (1994), McKibbin et al., (2017) and Rosenbaum et al., (2012).|303.0 +/- 3.0 Ma, 288.0 +/- 2.9 Ma U-Pb zircon||||Granitoids.|
67847|Hillgrove Supersuite|73202|6|Mentioned|p634 Fig.5|||||||||
67847|Hillgrove Supersuite|73264|6|Mentioned|p1398|Cisuralian|Cisuralian|New England Orogen. S-type granitoids. Contains large amount of Carboniferous zircon cores. Zircon eHf values of +4 to +7.|297-285 Ma||Hillgrove Granite.|||
67847|Hillgrove Supersuite|73570|6|Mentioned|p918|Early Permian|Late Carboniferous|New England Orogen.||||||
38204|Hillside Claystone Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Geological Province: Sydney Basin||||||
38204|Hillside Claystone Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Lucernia Coal. Geological Province: Sydney Basin||||||
30938|Hillston Volcanic Complex|22508|6|Mentioned|p13, map|||Lachlan Fold Belt||||||
30938|Hillston Volcanic Complex|22887|3|Fully described|p22, Fig.4 p11|Early Devonian|Early Devonian|||||||
30938|Hillston Volcanic Complex|23252|5|Briefly described|Map Legend||Devonian|of Mount Hope Group. Bimodal volcanism - part of the initial Cobar Basin development.||||||11-JAN-10
30938|Hillston Volcanic Complex|61964|6|Mentioned|p140|||||||||
30938|Hillston Volcanic Complex|62367|5|Briefly described|p4 Fig. 2|Early Devonian|Silurian|Inferred only.||||||
30938|Hillston Volcanic Complex|69162|5|Briefly described|Map legend|||Does not outcrop in map area. Is shown only in the interpretative cross-section.||||||
30938|Hillston Volcanic Complex|73505|6|Mentioned|p32|Devonian|Devonian|||||||
33124|Himalaya Suite|50606|5|Briefly described|p1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block. Age: ~1710Ma.||||||07-NOV-08
23650|Hollanders Formation|22857|5|Briefly described|p478 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Mumbil Group. Limestone, mudstone, arenite, siltstone. Max. thickness: 330m. Geological Province: Capertee Rise.||||||10-MAR-06
23650|Hollanders Formation|23214|3|Fully described|p145|Pridoli|Ludlow|Of Mumbil Group. Previously mapped as Tuglow Formation. Disconformably overlain by Drogheda Volcanics.  Max. thickness 330m.||||||17-JAN-06
23650|Hollanders Formation|42712|4|Described|8, Table1 p14.|Early Devonian|Late Silurian|Within Campbells/Kildrummie Group. Unconformable on Rockley Volcanics, conformable below Kowmung Volcaniclastics||||||
23650|Hollanders Formation|43639|5|Briefly described|Map Legend||Silurian|||||||
23650|Hollanders Formation|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|of Mumbil Group.||||||
23650|Hollanders Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
24312|Hollymount Formation|39848|2|Defined|p115|early Miocene|late Oligocene|Late Oligocene to Early Miocene||||||
24312|Hollymount Formation|40240|6|Mentioned|Fig.1|||||||||
24312|Hollymount Formation|40293|5|Briefly described|p460|||||||||
24312|Hollymount Formation|40742|5|Briefly described|p299|||||||||
24312|Hollymount Formation|41110|5|Briefly described|p223|||||||||
24312|Hollymount Formation|42820|6|Mentioned|p58|||||||||
24312|Hollymount Formation|61155|5|Briefly described|p19|Late Oligocene|Late Oligocene|Overlain by Bevendale, Wheeo, Bannister, Pomeroy and Divide Basalts.  Age: 26-24.5Ma.  In the Bathurst-Goulburn region. ||||||
24312|Hollymount Formation|64238|5|Briefly described|Map legend|Cenozoic|Cenozoic|Unconsolidated alluvial quartzose sand, polymictic gravel, and consolidated silcrete and quartz- and iron-cemented sandstone.||||||19-NOV-08
24312|Hollymount Formation|68592|5|Briefly described|p1840, p1845-6|Miocene|Miocene|Bishop (1984). Near Dalton. Age based on overlying basalt.||||Is overlain by Wheeo Basalt.|Undifferentiated alluvium; includes sand, clay and conglomerate; locally ferruginous; variably consolidated.|
33384|Home Rule Quartz Monzonite|23043|5|Briefly described|Map Legend|Namurian|Namurian|of Gulgong Plutonic Suite.||||||
33384|Home Rule Quartz Monzonite|23170|2|Defined|p275|Carboniferous|Carboniferous|Age: SHRIMP 314+/- 8 Ma. of Gulgong Plutonic Suite.||||||
70130|Homestead Gorge Formation|66623|2|Defined|pp192-193, pp199-200. |Early Devonian|Early Devonian|Defined in this study. Part of former Snake Cave Sandstone. Correlated with lower Muckabunnya Formation. c.37 km of strike length. Subdued outcrop, commonly with drainage developed along the unit. Thickness varies laterally from 20 m  to 550 m. Contains worm tubes and eurypterid or vertebrate tracks.||Unit in Wana Karnu Group.||Overlies New Tank Formation. Is overlain by Old Coach Road Formation.|Dominated by medium- to coarse-grained, white to cream, flaggy sandstones, rarely laminated and pebbly, with interbedded conglomerate.|
70130|Homestead Gorge Formation|66918|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Wana Karnu Group.||Overlies New Tank Formation.|Thick to very thick beds of white to buff quartz sandstone, pebbly in places, with horizons of vertical worm burrows.|25-SEP-13
70130|Homestead Gorge Formation|70650|5|Briefly described|Map Legend|Devonian|Devonian|||Wana Karnu Group|||Thick to very thick beds of white to buff, quartz sandstone, pebbly in places, with horizons of vertical worm burrows.|
82499|Honeysuckle Creek Leucosyenogranite|71628|4|Described|p8: 9, 100-101; p19: 76-79|||New name (this study). Originally Honeysuckle Creek Leucoadamellite of Binns et al. (1967), after unpublished work by Ransley (1970) who named the unit Honeysuckle Creek Leucoadamellite, and Joyce (1964). Named after a local watercourse. Occurs ~10 km SW of Yarrowyck as two NW-trending dyke-like bodies cropping out over ~6 km2 as abundant small tors and pavements. Emplaced along a major NNW-trending fracture system. Limited geochemical analyses described. Is associated with minor Mo mineralisation.||Honeysuckle Creek Suite.||Intrudes Sandon beds and ?Kurrajong Park Volcanics.|Pink to cream, fine- to medium-grained, equigranular biotite leucosyenogranite with lesser porphyritic and aphanitic variants. Has well-developed jointing. I-type.|
32687|Honeysuckle beds|22638|1|Redefined|p39|||Controversy over age. Previously "Honeysuckle beds", previously "Honeysuckle Metabasic Igneous Complex"||||||
32687|Honeysuckle beds|22687|3|Fully described|109,113,117,118,119|Late Silurian|Late Silurian|Geol province: Lachlan Fold Belt.||||||05-DEC-07
32687|Honeysuckle beds|22768|5|Briefly described|p155,174,184||Silurian|||||||
32687|Honeysuckle beds|22857|5|Briefly described|p174, p450 App.1, Tb.A1.6|Late Silurian|Early Silurian|Supersedes "Honeysuckle Metabasic Igneous Complex". Placed by Stuart-Smith (1990b) as above Blowering Fm but further study and age determination is required to solve controversy over timing of events. Contains radiolaria in cherts. See also p155 and p183.||||||
32687|Honeysuckle beds|44192|5|Briefly described|Map Legend|Llandoverian|Llandoverian|||||||
32687|Honeysuckle beds|44936|5|Briefly described|Map Legend||Silurian|||||||
32687|Honeysuckle beds|50191|5|Briefly described|p6, 21 Fig. 1|Silurian|Early Silurian|Interfingers with or overlies: Blowering Formation, Brawlin Formation.||||||
32687|Honeysuckle beds|66197|5|Briefly described|p631 Fig.3a|||Mafic volcanics. Tumut Trough.||||||13-MAR-12
32687|Honeysuckle beds|66768|6|Mentioned|p209  |||Sourced from subduction-related mafic melts in the Silurian.||||||
32687|Honeysuckle beds|69043|6|Mentioned|p63|||||||||
32687|Honeysuckle beds|71708|5|Briefly described|p335, p336 Fig 1, p337, p351|||Late-stage trough fill in the Tumut Trough of continental origin.||||In fault contact with Coolac Serpentinite.|Volcanic and sedimentary rocks. Includes basalts.|31-MAR-20
26620|Hopping Joe Granite|42726|5|Briefly described|map legend|Early Devonian||122.  Of the Hopping Joe Suite (Candelo Supersuite).  Not intended asa formal name.||||||09-FEB-05
31488|Hopping Joe Suite|42726|5|Briefly described|map legend||Early Devonian|Of theCandelo Supersuite.||||||09-FEB-05
70278|Horse Arm Formation|66720|5|Briefly described|Map legend|Late Devonian|Early Devonian||||Three un-named members are mapped separately: massive, porphyritic andesite; volcaniclastic sandstone; and black and green laminated siltstone with interbedded lithofeldspathic sandstone.||Volcanic breccia, andesite, conglomerate, sandstone, siltstone; rare limestone and calcareous sandstone.|
70278|Horse Arm Formation|71628|6|Mentioned|p7: 19, 31|||||||Is intruded by Inlet and Moonbi Monzogranites.||
35282|Hoskins Chert|24215|5|Briefly described|p801|||Formerly referred to as Hoskins Formation.  Superseded by Hoskins Chert.  Parent: Jindalee Group.    Geological Province:  Lachlan Fold Belt||||||
35282|Hoskins Chert|24417|3|Fully described|p7|Ordovician|Ordovician|Modified from Bowman (1977a).  Originally named "Hoskins Formation".  Of the Jindalee Group.||||||
35282|Hoskins Chert|60009|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Jindalee Group.||||||13-JUL-04
35282|Hoskins Chert|63289|5|Briefly described|p372|||Of Jindalee Group. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
35282|Hoskins Chert|67322|6|Mentioned|p20|Pridoli|Ludlow|Lyons, Duggan and Wallace in Lyons et al. (2000). Age from conodonts: an Ordovician fragmented ophiolite sequence within a Silurian sedimentary matrix. On the Forbes 1:250 000 Sheet, near Grenfell.||Of the Jindalee Group||||
35282|Hoskins Chert|68466|5|Briefly described|p66|||Crops out N and S of Grenfell. Sparse Darriwilian to Late Ordovician conodonts.||Jindalee Group.|||Includes conodont-bearing, salmon-coloured translucent cherts.|
35282|Hoskins Chert|69668|6|Mentioned|p932|Silurian|Silurian|Exposed north and south of Grenfell. Contains a sparse Darriwilian to Late Ordovician conodont fauna.||Unit in Jindalee Group.||||
35282|Hoskins Chert|71040|6|Mentioned|p17-18|Middle Ordovician|Middle Ordovician|Forbes area.||||||
35852|Hospital Porphyry|23329|3|Fully described|1043|Late Devonian|Middle Devonian|||||||
35852|Hospital Porphyry|60007|6|Mentioned|Map legend|Middle Devonian|Early Devonian|||||||
69895|Hovells Suite|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Rye Park, Wyangala, Reids Flat, Wywurri, Blanket Flat, Bigga, Foggs Hollow, Licking Gully and Ballyhooley Granites.||||||
69895|Hovells Suite|66300|6|Mentioned|p92.|||Eastern Lachlan Orogen. |||Includes Rye Park and Bigga Granites.|||
69895|Hovells Suite|66713|5|Briefly described|p5||Silurian|Unit in Wyangala Supersuite. Contains Ballyhooley Granite, Reids Flat Granite and Licking Gully Granite.||||||
69895|Hovells Suite|68592|2|Defined|p443, p464, p1228, p1253-6, p1260-1311|Early Devonian|Late Silurian|See also xxiv, p73 Tb.5, p230-1, p438. New name. Supersedes Wyangala Suite (Chappell et al., 1991) by also including other plutons on geochemical grounds (viz. Blanket Flat, Ballyhooley, Foggs Hollow, Rye Park, Julong and Wywurri Granites). Comprises 10 plutons which occupy most of the area between Boorowa/Bigga and Lake Wyangala (c. 810 km2). The type pluton is the Wyangala Granite. Geochemistry detailed. S-type. Generally form hilly areas; exposed as large tors and low rounded outcrops. All plutons show thin-section evidence of pervasive strain; some granites have broad protomylonitic zones recording W-over-E thrust movement. Yass and Wyangala structural zones: deformation described.||Unit in Wyangala Supersuite.|Includes Wyangala, Licking Gully, Reids Flat, Bigga, Blanket Flat, Ballyhooley, Foggs Hollow, Rye Park, Julong and Wywurri Granites.|Intrudes Adaminaby Group, Kenyu Formation, Hawkins Volcanics, Gunning and Burrawinda Suites.|Typically cream to grey, medium- to coarse-grained, massive to foliated, equigranular to porphyritic (often megacrystic) cordierite-muscovite-biotite granite and granodiorite. Characteristically megacrystic in K-feldspar. S-type.|
69895|Hovells Suite|70192|5|Briefly described|Map Legend|Pragian|Ludlow|On Boorowa and Yass 1:100 000 mapsheet portions of Time-Space Plot.|||Ballyhooley Granite, Licking Gully Granite, Foggs Hollow Granite, Bigga Granite, Julong Granite, Blanket Flat Granite, Wywurri Granite, Reids Flat Granite, Wyangala Granite, Rye Park Granite.|||
69895|Hovells Suite|70540|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Rye Park Granite.|||
69895|Hovells Suite|70544|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Foggs Hollow Granite, Bigga Granite, Julong Granite, Blanket Flat Granite, Reids Flat Granite|||
69895|Hovells Suite|70545|5|Briefly described|Map Legend |Devonian|Silurian||||Includes Ballyhooley Granite, Licking Gully Granite, Wywurri Granite, Reids Flat Granite, Wyangala Granite, Rye Park Granite|||
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.|
74213|Hulong Conglomerate Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yanowe Formation (Douro Group). Variecoloured polymictic pebble paraconglomerate sporadically grading to orthoconglomerate. Composed of clasts of chert, ?vitric tuff, ?siliceous mudstone in a matrix of medium- to very fine-grained quartz litharenite.||||||11-JUN-08
74213|Hulong Conglomerate Member|68592|2|Defined|p430 Fig.89, p431-2, p434-6, p523-558|Ludlow|Ludlow|Named after Hulong homestead, now part of Yanawe Station. Type locality described. 50-80m thick. Volcaniclastic debris-flow deposits. Unfossiliferous; age of early Early Ludlow inferred from stratigraphic relationships.||Basal unit in Yanawe Formation.||Overlies Laidlaw Volcanics. Is overlain conformably by Werong Breccia Member.|Varicoloured, largely monomictic, pebble paraconglomerate, sporadically grading to orthoconglomerate; clasts mostly subrounded and mainly (80%) of chert.|
74213|Hulong Conglomerate Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdwp. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Yanawe Formation||Overlies unnamed member of Yanawe Formation. Is overlain by Werong Breccia Member.|Largely monomictic, pebble paraconglomerate grading to orthoconglomerate; subrounded clasts of chert, tuffaceous mudstone with minor porphyritic volcanic rock in a matrix of medium-very fine grained quartz lithic sandstone.|
74213|Hulong Conglomerate Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Largely monomictic, pebble paraconglomerate grading to orthoconglomerate; subrounded clasts of chert, tuffaceous mudstone with minor porphyritic volcanic rock in a matrix of medium-very fine grained quartz lithic sandstone.|
74213|Hulong Conglomerate Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Largely monomictic, pebble paraconglomerate grading to orthoconglomerate, subrounded clasts of chert, tuffaceous mudstone and minor porphyritic volcanic rock in matrix of medium-very fine grained quartz lithic sandstone.|
74212|Humewood Volcanic Sandstone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yanawe Formation (Douro Gp). Variecoloured (green-grey and red-black), very coarse-grained crystal-rich volcaniclastite.||||||09-SEP-08
74212|Humewood Volcanic Sandstone Member|68592|2|Defined|p430 Fig.89, p434-6, p523-58|Ludlow|Ludlow|New name, after Humewood property. This unit lies within the Willow Bridge Tuff Member of Link (1970). Type locality described. 170-430m thick. Unfossiliferous; early Early Ludlow age inferred from stratigraphic relationships. Distal pyroclastic lacustrine? deposits.||Unit in Yanawe Formation.|||Varicoloured (green-grey and red-black), very coarse-grained, crystal-rich volcanic sandstone; sporadically thin-banded.|
74212|Humewood Volcanic Sandstone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdwd. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Yanawe Formation||Shown on Time-Space Plot as erosionally overlain by unnamed member of Yanawe Formation. Overlies Hulong Conglomerate Member.|Very coarse grained, crystal rich volcaniclastic sandstone; sporadically thinly banded with a fragmental texture and bimodal sorting; high magnetic susceptibility.|
74212|Humewood Volcanic Sandstone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Very coarse grained, crystal rich volcaniclastic sandstone; sporadically thinly banded with a fragmental texture and bimodal sorting; high magnetic susceptibility.|
74212|Humewood Volcanic Sandstone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Very coarse grained crystal rich volcaniclastic sandstone; sporadically thinly banded with a fragmental texture and bimodal sorting; high magnetic susceptibility.|
73520|Hummock Formation|66623|2|Defined|p110, pp124-125. |Late Cambrian|Late Cambrian|Defined in this study as comprising the lower (sandstone) sequence of the Cupala Creek Formation of Powell et al. (1982) which was included in Kayrunnera Group by Mills and Hicks (2000). Nuntherungie and Cupala Creek Basins. Generally an upward-fining, fluvial to shallow-marine, siliciclastic sequence, between 530-1000 m thick. Correlative of Morden Formation, Boshy Formation and Mutawintji Group.||Unit in Kayrunnera Group.||Overlies Williams Creek Conglomerate. Is overlain by Cupala Creek Formation.|White to red-maroon, well-laminated to festoon cross-bedded, medium- to fine-grained quartzite (originally quartz sandstone); minor siltstone and conglomerate interbeds near the base of the unit.|16-MAY-13
73520|Hummock Formation|67322|4|Described|p11; Fig.5|Series 3|Series 3|Redefined by Greenfield (in Greenfield et al. 2010) as a separate unit from the Cupala Creek Formation of Powell et al. (1982). Thickness varies between about 530m (Cupala Creek outlier), to over 1000m (Nuntherungie area). Age from its sole fossil, the brachiopod Billingsella. Occurs in the Kayrunnera-Koonenberry region.||Of the Kayrunnera Group.||Overlies Williams Creek Conglomerate conformably. Is overlain conformably by Cupala Creek Formation.|Quartzose sandstone- to quartzite-dominated.|22-FEB-18
31710|Hunter Formation|22857|5|Briefly described|p490 App.1 Tb.A1.7|Devonian|Devonian|Of the Hervey Group. Red and brown siltstone and mudstone, minor white and pink arenite. Max. thickness: 488m. Geological Province: Hervey Basin.||||||
31710|Hunter Formation|23214|3|Fully described|p227|Late Devonian|Late Devonian|Of Hervey Group.  Formerly Hunter Sandstone.  Red-brown siltstone and mudstone with minor thin interbeds of pinkish white sandstone.  Overlying unit: Mandgery Formation, Underlying unit: Peaks Formation.  Max. thickenss 488m.  Hervey Basin.||||||
31710|Hunter Formation|23217|6|Mentioned|p16|||Of the Hervey Group.||||||08-MAR-06
31710|Hunter Formation|23392|2|Defined|p9|Famennian|Famennian|Supersedes Hunter Siltstone and Bogan Gate Sandstone. Four fossil assemblages present. Correlates with Mount Cole Formation (Parkes 1:100 000). Of the Hervey Group. Geological Province: Lachlan Fold Belt. Max Thickness: 525m||||||
31710|Hunter Formation|24417|3|Fully described|p132|Famennian|Famennian|Of Hervey Group.  Formerly "Hunter Siltstone".  Max. thickness: 490m.||||||
31710|Hunter Formation|43782|5|Briefly described|Map Legend|Frasnian|Frasnian|of Hervey Group.||||||
31710|Hunter Formation|50258|5|Briefly described|p147, p153|Famennian|Famennian|Shallow, mainly marine deposits containing acanthodian fish jawbones.||||||
31710|Hunter Formation|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hervey Group.  Includes: Gooloogong Member. Red and brown siltstone, mudstone and minor sandstone. Overlies: Warrumba Volcanics.||||||14-JUL-04
31710|Hunter Formation|60009|5|Briefly described|Map Legend|Famennian|Frasnian|Of the Hervey Group.  Includes: Gooloogong Member.  Underlies: Weddin Sandstone.  Overlies: Peaks Formation.||||||13-JUL-04
31710|Hunter Formation|60548|5|Briefly described|map legend|Devonian|Devonian|Of Hervey Group.  Red and brown siltstone, mudstone, minor sandstone.||||||
31710|Hunter Formation|68592|5|Briefly described|p1717, p1738|Late Devonian|Late Devonian|||Unit in Hervey Group.|Includes Gooloogong Member.|Equivalent to Bumberry Formation.||
31710|Hunter Formation|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Hervey Group||||
30856|Huntingdale Volcanics|22529|6|Mentioned|8|Early Devonian|Early Devonian|||||||
68913|Hunton Group|60332|5|Briefly described|p946|Pridoli|Ludlow|Contains conodonts.||||||
39796|Hutton Sandstone, lower|24159|6|Mentioned|p152|||Geological Province: Surat Basin. Informal - see Hutton Sandsone.||||||
39796|Hutton Sandstone, lower|60999|6|Mentioned|p177|||Informal - see Hutton Sandstone. Broadly correlated with upper part of Koukandowie Formation. Geological Province: Surat Basin.||||||
31462|Hyde Creek Suite|22815|6|Mentioned|p74|||||||||
31462|Hyde Creek Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Bemboka Supersuite.  Contains the Hyde Creek Granite.||||||08-FEB-05
31462|Hyde Creek Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
27802|Illawarra Coal Measures|22488|6|Mentioned|p841 p847|||||||||
27802|Illawarra Coal Measures|22529|5|Briefly described|4 fig 2|Permian|Permian|Overlying unit Narrabeen Group, underlying unit Shoalhaven Group||||||
27802|Illawarra Coal Measures|22549|6|Mentioned|p526||Late Permian|||||||
27802|Illawarra Coal Measures|22578|5|Briefly described|p391, Fig.6 p396||Late Permian|||||||
27802|Illawarra Coal Measures|22728|5|Briefly described|p599 table1||Permian|||||||
27802|Illawarra Coal Measures|22745|6|Mentioned|Fig3,p128||Permian|Sydney Basin.||||||
27802|Illawarra Coal Measures|22857|4|Described|p265, p528 App.1 Tb.A1.9|Late Permian|Late Permian|Includes the Wallerawang, Charbon, Cullen Bullen, Nile, Sydney and Cumberland Subgroups. Disconformably overlain by Coal Cliff Sandstone (Narrabeen Group). Geological Province: Sydney Basin. See also pages 526 and 532 in App.1 Tb.A1.9.||||||
27802|Illawarra Coal Measures|22864|6|Mentioned|p265|||||||||
27802|Illawarra Coal Measures|22969|4|Described|p4, p 24|||||||||
27802|Illawarra Coal Measures|22970|5|Briefly described|Plate 6||Permian|||||||
27802|Illawarra Coal Measures|23013|6|Mentioned|p326|||||||||
27802|Illawarra Coal Measures|23043|5|Briefly described|Map Legend|Late Permian|Late Permian|of Sydney Basin.||||||
27802|Illawarra Coal Measures|23170|2|Defined|p298 Fig.61|Late Permian|Late Permian|Of Sydney Basin.||||||24-SEP-08
27802|Illawarra Coal Measures|23214|3|Fully described|p267|Late Permian|Late Permian|Previously referred to as Wallerawang Coal Measures, Lithgow Coal Measures and the Western Coal Measures. Max. thickness 50m. Overlying unit: Narrabeen Group, underlying unit: Shoalhaven Group. Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|23218|6|Mentioned|p28|||||||||
27802|Illawarra Coal Measures|23219|5|Briefly described|Map Legend|Permian||||||||
27802|Illawarra Coal Measures|23544|5|Briefly described|Fig 2 p358|||In the Sydeny Basin||||||
27802|Illawarra Coal Measures|23881|5|Briefly described|p69 Fig. 7.2|||Includes Bulli Coal, Eckersley Formation, Wongawilli Coal, Kembla Sandstone and Allans Creek Formation.  Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|23896|14|Not recorded|p249|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|24123|5|Briefly described|p3|||||||||
27802|Illawarra Coal Measures|24126|6|Mentioned|p201|||Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|24157|5|Briefly described|p209 Fig.19|||Geological Province: Sydney Basin||||||
27802|Illawarra Coal Measures|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||29-NOV-04
27802|Illawarra Coal Measures|24342|5|Briefly described|p51|Late Permian|Late Permian|Overlying unit: Narrabeen Group.  Includes Cumberland Subgroup and Sydney Subgroup. Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|24471|4|Described|p27|Late Permian|Late Permian|Geological Province: Sydney Basin. Conformably overlies Shoalhaven Group. Overlain by Narrabeen Group. Stratigraphically equivalent to Newcastle Coal Measures.||||||07-FEB-11
27802|Illawarra Coal Measures|24552|5|Briefly described|p5 Fig.2|Tatarian|Tatarian|Overlies Gerringong Volcanics. Geological Province: Southern Sydney Basin.||||||07-FEB-11
27802|Illawarra Coal Measures|29633|6|Mentioned|p437|||Permian/Triassic boundary||||||
27802|Illawarra Coal Measures|29635|6|Mentioned|p561|||See also P568.||||||
27802|Illawarra Coal Measures|29748|6|Mentioned|p8|||||||||
27802|Illawarra Coal Measures|29749|6|Mentioned|p12|||||||||
27802|Illawarra Coal Measures|29751|5|Briefly described|p5|||||||||
27802|Illawarra Coal Measures|29900|4|Described|Fig.3|||||||||
27802|Illawarra Coal Measures|29901|6|Mentioned|p169|||||||||
27802|Illawarra Coal Measures|29909|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|29944|4|Described|p236|||||||||
27802|Illawarra Coal Measures|29993|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27802|Illawarra Coal Measures|30006|4|Described|p6|||||||||
27802|Illawarra Coal Measures|30007|6|Mentioned|p61|||Permian||||||
27802|Illawarra Coal Measures|30109|6|Mentioned|Fig.1|||Permian age.||||||
27802|Illawarra Coal Measures|30228|6|Mentioned|p17|||Lithology Permian age.||||||
27802|Illawarra Coal Measures|30646|6|Mentioned|p42|||||||||
27802|Illawarra Coal Measures|30707|6|Mentioned|p2|||Refers also Table 1||||||
27802|Illawarra Coal Measures|31057|6|Mentioned|p2|||See also re potential use.||||||
27802|Illawarra Coal Measures|31061|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|31062|6|Mentioned|p478|||Triassic. On Table||||||
27802|Illawarra Coal Measures|31128|5|Briefly described|p5|||See also p3.||||||23-SEP-18
27802|Illawarra Coal Measures|31276|6|Mentioned|p143|||Refers to Hennelly (1958)||||||
27802|Illawarra Coal Measures|31297|6|Mentioned|Fig. 3|||See also Fig. 2||||||
27802|Illawarra Coal Measures|31298|6|Mentioned|p12|||||||||
27802|Illawarra Coal Measures|31326|6|Mentioned|p34|||Refers Kenny (1928)||||||
27802|Illawarra Coal Measures|31380|4|Described|p131|||||||||
27802|Illawarra Coal Measures|31381|6|Mentioned|p53|||||||||
27802|Illawarra Coal Measures|31559|6|Mentioned|p158|||||||||
27802|Illawarra Coal Measures|31563|6|Mentioned|p60|||||||||
27802|Illawarra Coal Measures|31613|6|Mentioned|p348|||||||||
27802|Illawarra Coal Measures|31649|6|Mentioned|p59|||||||||
27802|Illawarra Coal Measures|31802|5|Briefly described|p142|||Stratigraphy & age||||||
27802|Illawarra Coal Measures|31855|6|Mentioned|p14|||Stratigraphic table||||||
27802|Illawarra Coal Measures|31878|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|31880|6|Mentioned|p18|||||||||
27802|Illawarra Coal Measures|31884|6|Mentioned|Table 1|||Permian||||||
27802|Illawarra Coal Measures|31885|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|31886|6|Mentioned|p393|||||||||
27802|Illawarra Coal Measures|31887|5|Briefly described|p4|||Mention p3.||||||23-SEP-18
27802|Illawarra Coal Measures|31890|6|Mentioned|p77|||Permian||||||
27802|Illawarra Coal Measures|32045|6|Mentioned|Map legend|Permian|Permian|||||||
27802|Illawarra Coal Measures|32047|6|Mentioned|p4|||||||||
27802|Illawarra Coal Measures|32187|6|Mentioned|p4|||||||||
27802|Illawarra Coal Measures|32266|6|Mentioned|p24|||||||||
27802|Illawarra Coal Measures|32485|6|Mentioned|Map legend|Permian|Permian|||||||
27802|Illawarra Coal Measures|32537|6|Mentioned|p3|||||||||
27802|Illawarra Coal Measures|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
27802|Illawarra Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
27802|Illawarra Coal Measures|32672|6|Mentioned|p675|||||||||
27802|Illawarra Coal Measures|32801|6|Mentioned|Fig.1|||||||||
27802|Illawarra Coal Measures|32849|6|Mentioned|p7|||Permian||||||
27802|Illawarra Coal Measures|32938|6|Mentioned|p67|||Geology||||||
27802|Illawarra Coal Measures|32945|6|Mentioned|p84|||See also P85||||||
27802|Illawarra Coal Measures|32998|6|Mentioned|p113|||Stratigraphy||||||
27802|Illawarra Coal Measures|33006|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
27802|Illawarra Coal Measures|33128|5|Briefly described|p51|||||||||
27802|Illawarra Coal Measures|33129|6|Mentioned|p328|||||||||
27802|Illawarra Coal Measures|33131|6|Mentioned|Fig.9|||||||||
27802|Illawarra Coal Measures|33132|6|Mentioned|p1465|||||||||
27802|Illawarra Coal Measures|33282|6|Mentioned|Map legend|Permian|Permian|||||||
27802|Illawarra Coal Measures|33364|6|Mentioned|p43|||Boron & fresh water origin.||||||
27802|Illawarra Coal Measures|33489|6|Mentioned|p47|||Refers Duff (1967)||||||
27802|Illawarra Coal Measures|33683|6|Mentioned|Table 1|||Permian.||||||
27802|Illawarra Coal Measures|33685|6|Mentioned|Table 1|||Permian.||||||
27802|Illawarra Coal Measures|33867|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|33869|5|Briefly described|p66|||See also Fig.2.||||||
27802|Illawarra Coal Measures|33930|6|Mentioned|p15|||||||||
27802|Illawarra Coal Measures|34009|6|Mentioned|Table III|||||||||
27802|Illawarra Coal Measures|34038|6|Mentioned|p435|||||||||
27802|Illawarra Coal Measures|34039|6|Mentioned|p355|||||||||
27802|Illawarra Coal Measures|34040|6|Mentioned|p382|||Permian||||||
27802|Illawarra Coal Measures|34059|6|Mentioned|Map legend|Permian|Permian|||||||
27802|Illawarra Coal Measures|34060|6|Mentioned|p24|||Perm. Table||||||
27802|Illawarra Coal Measures|34110|6|Mentioned|p27|||||||||
27802|Illawarra Coal Measures|34130|6|Mentioned|p178|||||||||
27802|Illawarra Coal Measures|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
27802|Illawarra Coal Measures|34140|6|Mentioned|p45|||||||||
27802|Illawarra Coal Measures|34156|6|Mentioned|p387|||Permian||||||
27802|Illawarra Coal Measures|34158|6|Mentioned|p400|||||||||
27802|Illawarra Coal Measures|34204|6|Mentioned|p65|||||||||
27802|Illawarra Coal Measures|34205|3|Fully described|p10|||Now Nile Sub-Group & Charbon Sub-Group||||||
27802|Illawarra Coal Measures|34209|6|Mentioned|p137|||Permian. See also P140, Table 1.||||||
27802|Illawarra Coal Measures|34240|6|Mentioned|p395|||Permian||||||
27802|Illawarra Coal Measures|34283|6|Mentioned|Plate 6a|||Geomorphology||||||
27802|Illawarra Coal Measures|34287|6|Mentioned|p130|||Permian||||||
27802|Illawarra Coal Measures|34292|6|Mentioned|p25|||See also P27. Permian||||||
27802|Illawarra Coal Measures|34334|6|Mentioned|p357|||||||||
27802|Illawarra Coal Measures|34337|6|Mentioned|Table 5.18|||||||||
27802|Illawarra Coal Measures|34338|6|Mentioned|p400|||||||||
27802|Illawarra Coal Measures|34339|6|Mentioned|Fig.5.46|||Isopach map. See also Tectofacies map Fig.5.47||||||
27802|Illawarra Coal Measures|34399|6|Mentioned|p312|||||||||
27802|Illawarra Coal Measures|34400|6|Mentioned|p13|||Permian. Equivalent Newcastle and Tomago Coal Measures.||||||
27802|Illawarra Coal Measures|34404|6|Mentioned|Fig.3.5b|||||||||
27802|Illawarra Coal Measures|34434|6|Mentioned|p368|||||||||
27802|Illawarra Coal Measures|34444|6|Mentioned|Map legend|Permian|Permian|||||||
27802|Illawarra Coal Measures|34451|6|Mentioned|p198|||||||||
27802|Illawarra Coal Measures|34492|6|Mentioned|p67|||||||||
27802|Illawarra Coal Measures|34506|6|Mentioned|p408|||||||||
27802|Illawarra Coal Measures|34516|6|Mentioned|p16|||||||||
27802|Illawarra Coal Measures|34517|6|Mentioned|p46|||||||||
27802|Illawarra Coal Measures|34569|6|Mentioned|p7|||See also PP8,9. Permian||||||
27802|Illawarra Coal Measures|34585|4|Described|p30|Permian||Formerly Wollondilly or "Upper Coal Measures"? Upper C.M. superseded by current Singleton Subgroup.||||||
27802|Illawarra Coal Measures|34605|3|Fully described|p370|||See also pp371-379.||||||23-SEP-18
27802|Illawarra Coal Measures|34845|6|Mentioned|Fig.4|||||||||
27802|Illawarra Coal Measures|34884|6|Mentioned|p57|||||||||
27802|Illawarra Coal Measures|35065|5|Briefly described|p44|||||||||
27802|Illawarra Coal Measures|35095|6|Mentioned|p110|||||||||
27802|Illawarra Coal Measures|35138|6|Mentioned|p15|||||||||
27802|Illawarra Coal Measures|35145|6|Mentioned|Fig.2|||||||||
27802|Illawarra Coal Measures|35319|6|Mentioned|p473|||||||||
27802|Illawarra Coal Measures|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
27802|Illawarra Coal Measures|35524|5|Briefly described|p73|||||||||
27802|Illawarra Coal Measures|35767|6|Mentioned|p6|||||||||
27802|Illawarra Coal Measures|35794|6|Mentioned|p256|||||||||
27802|Illawarra Coal Measures|35878|6|Mentioned|p115|||||||||
27802|Illawarra Coal Measures|36042|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|36058|5|Briefly described|p3|||||||||
27802|Illawarra Coal Measures|36147|6|Mentioned|Fig.2|||||||||
27802|Illawarra Coal Measures|36148|6|Mentioned|p266|||||||||
27802|Illawarra Coal Measures|36172|6|Mentioned|Appendix|||||||||
27802|Illawarra Coal Measures|36207|6|Mentioned|Text Fig.2|||||||||
27802|Illawarra Coal Measures|36220|4|Described|p38|||See also Table 10.||||||
27802|Illawarra Coal Measures|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27802|Illawarra Coal Measures|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27802|Illawarra Coal Measures|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27802|Illawarra Coal Measures|36327|6|Mentioned|p3|||||||||
27802|Illawarra Coal Measures|36390|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27802|Illawarra Coal Measures|36593|6|Mentioned|p188|||See also Fig.2.||||||
27802|Illawarra Coal Measures|36594|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|36600|6|Mentioned|p105|||||||||
27802|Illawarra Coal Measures|36612|6|Mentioned|Fig.2|||||||||
27802|Illawarra Coal Measures|36899|6|Mentioned|Fig.3|||||||||
27802|Illawarra Coal Measures|36954|6|Mentioned|p113|||||||||
27802|Illawarra Coal Measures|37065|6|Mentioned|p32|||||||||
27802|Illawarra Coal Measures|37081|6|Mentioned|p156|||||||||
27802|Illawarra Coal Measures|37082|6|Mentioned|p161|||||||||
27802|Illawarra Coal Measures|37089|4|Described|p208|||||||||
27802|Illawarra Coal Measures|37090|6|Mentioned|p219|||||||||
27802|Illawarra Coal Measures|37091|5|Briefly described|p226|||||||||
27802|Illawarra Coal Measures|37092|6|Mentioned|p227|||||||||
27802|Illawarra Coal Measures|37093|6|Mentioned|p231|||||||||
27802|Illawarra Coal Measures|37168|6|Mentioned|Fig.2|||||||||
27802|Illawarra Coal Measures|37423|6|Mentioned|p21|||||||||
27802|Illawarra Coal Measures|37722|6|Mentioned|p23|||||||||
27802|Illawarra Coal Measures|37730|6|Mentioned|p18|||||||||
27802|Illawarra Coal Measures|37804|6|Mentioned|p55|||||||||
27802|Illawarra Coal Measures|37834|6|Mentioned|p48|||||||||
27802|Illawarra Coal Measures|38064|6|Mentioned|p41|||||||||
27802|Illawarra Coal Measures|38603|6|Mentioned|p79|||||||||
27802|Illawarra Coal Measures|38614|6|Mentioned|Fig.6|||||||||
27802|Illawarra Coal Measures|38615|6|Mentioned|p17|||||||||
27802|Illawarra Coal Measures|38656|5|Briefly described|Table1.5.5|||p220.||||||23-SEP-18
27802|Illawarra Coal Measures|38690|6|Mentioned|p288|||||||||
27802|Illawarra Coal Measures|38735|6|Mentioned|p76|||||||||
27802|Illawarra Coal Measures|38951|6|Mentioned|p409|||||||||
27802|Illawarra Coal Measures|38958|5|Briefly described|p493|||||||||
27802|Illawarra Coal Measures|39232|5|Briefly described|p111|||||||||
27802|Illawarra Coal Measures|39285|6|Mentioned|p9|||||||||
27802|Illawarra Coal Measures|39287|6|Mentioned|Fig. 2.5|||||||||
27802|Illawarra Coal Measures|39289|6|Mentioned|p78|||||||||
27802|Illawarra Coal Measures|39290|6|Mentioned|p99|||||||||
27802|Illawarra Coal Measures|39293|4|Described|p139|||||||||
27802|Illawarra Coal Measures|39296|6|Mentioned|Fig. 11.1|||||||||
27802|Illawarra Coal Measures|39299|6|Mentioned|p288|||||||||
27802|Illawarra Coal Measures|39306|6|Mentioned|p404|||See also P405||||||
27802|Illawarra Coal Measures|39307|6|Mentioned|Table 22.1|||||||||
27802|Illawarra Coal Measures|39308|6|Mentioned|p501|||||||||
27802|Illawarra Coal Measures|39309|3|Fully described|p125|||See also p121.||||||23-SEP-18
27802|Illawarra Coal Measures|39331|6|Mentioned|Fig.7-1|||||||||
27802|Illawarra Coal Measures|39442|6|Mentioned|p188|||||||||
27802|Illawarra Coal Measures|39450|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|39661|6|Mentioned|p443|||||||||
27802|Illawarra Coal Measures|39664|6|Mentioned|Table 8|||||||||
27802|Illawarra Coal Measures|39754|6|Mentioned|p1689|||||||||
27802|Illawarra Coal Measures|39757|6|Mentioned|p1601|||||||||
27802|Illawarra Coal Measures|40044|6|Mentioned|p382|||||||||
27802|Illawarra Coal Measures|40166|4|Described|p348|||||||||
27802|Illawarra Coal Measures|40256|6|Mentioned|p305|||||||||
27802|Illawarra Coal Measures|40270|6|Mentioned|p167|||||||||
27802|Illawarra Coal Measures|40285|6|Mentioned|p32|||||||||
27802|Illawarra Coal Measures|40321|6|Mentioned|p17|||||||||
27802|Illawarra Coal Measures|40516|6|Mentioned|p382|||||||||
27802|Illawarra Coal Measures|40519|6|Mentioned|p328|||||||||
27802|Illawarra Coal Measures|40602|6|Mentioned|p7|||||||||
27802|Illawarra Coal Measures|40625|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27802|Illawarra Coal Measures|40630|6|Mentioned|p178|||||||||
27802|Illawarra Coal Measures|40631|6|Mentioned|p162|||||||||
27802|Illawarra Coal Measures|40636|6|Mentioned|p43|||||||||
27802|Illawarra Coal Measures|40653|6|Mentioned|Fig.21|||||||||
27802|Illawarra Coal Measures|40654|6|Mentioned|p117|||||||||
27802|Illawarra Coal Measures|40744|4|Described|p326|||||||||
27802|Illawarra Coal Measures|40886|6|Mentioned|Fig.1|||||||||
27802|Illawarra Coal Measures|41054|6|Mentioned|p152|||||||||
27802|Illawarra Coal Measures|41580|6|Mentioned|p9|||||||||
27802|Illawarra Coal Measures|41595|6|Mentioned|Fig.2|||||||||
27802|Illawarra Coal Measures|41689|6|Mentioned|Table 1|||||||||
27802|Illawarra Coal Measures|41718|6|Mentioned|p235|||||||||
27802|Illawarra Coal Measures|41832|6|Mentioned|Fig.2|||||||||
27802|Illawarra Coal Measures|42008|6|Mentioned|p270|||||||||
27802|Illawarra Coal Measures|42310|5|Briefly described|p209|||||||||
27802|Illawarra Coal Measures|42379|5|Briefly described|p209|||||||||
27802|Illawarra Coal Measures|42430|6|Mentioned|p176|||||||||
27802|Illawarra Coal Measures|42526|6|Mentioned|Map legend|||||||||
27802|Illawarra Coal Measures|42642|6|Mentioned|p171|||||||||
27802|Illawarra Coal Measures|42648|4|Described|p31, p38|||||||||
27802|Illawarra Coal Measures|42657|3|Fully described|p73, 74|||||||||
27802|Illawarra Coal Measures|42713|5|Briefly described|Fig. P18|||||||||
27802|Illawarra Coal Measures|42737|5|Briefly described|map legend|Permian||||||||
27802|Illawarra Coal Measures|42767|5|Briefly described|Fig.5|||||||||
27802|Illawarra Coal Measures|42787|5|Briefly described|p128|||||||||
27802|Illawarra Coal Measures|42795|6|Mentioned|p21|||||||||
27802|Illawarra Coal Measures|42896|3|Fully described|p16, Table 2|||Permian age||||||
27802|Illawarra Coal Measures|42925|5|Briefly described|Table 18||Late Permian|||||||
27802|Illawarra Coal Measures|42926|4|Described|map legend||Late Permian|||||||
27802|Illawarra Coal Measures|42974|6|Mentioned|Fig.2,p192|||||||||
27802|Illawarra Coal Measures|43016|6|Mentioned|p366|||||||||
27802|Illawarra Coal Measures|43028|6|Mentioned|Fig.7,p618,p617|||||||||
27802|Illawarra Coal Measures|43146|5|Briefly described|p39|||see also p41,Fig.2.||||||
27802|Illawarra Coal Measures|43188|6|Mentioned|p221|||||||||
27802|Illawarra Coal Measures|43194|5|Briefly described|p106, p128, p129 Tb. 8.3|Late Permian|Late Permian|Western and Southern Coalfields, Sydney Basin. Contains Charbon, Cullen Bullen and Nile Subgroup (Western Coalfield), and Sydney and Cumberland Subgroups (Southern Coalfield). Correlates with the Black Jack Formation, Gunnedah Basin.||||||
27802|Illawarra Coal Measures|43263|6|Mentioned|Map Legend||Permian|||||||
27802|Illawarra Coal Measures|43319|14|Not recorded|Map Legend|||||||||
27802|Illawarra Coal Measures|43320|14|Not recorded|Table 1 p5||Permian|p8,16,17,25,27,28,30,31||||||
27802|Illawarra Coal Measures|43344|14|Not recorded|p13,18,20,21,53,63,||Permian|66-71,73,77,182||||||
27802|Illawarra Coal Measures|43345|14|Not recorded|p3,2-7,15||Permian|||||||
27802|Illawarra Coal Measures|43346|2|Defined|p1,3,5 Map|||||||||19-JAN-10
27802|Illawarra Coal Measures|43349|14|Not recorded|Map|||Now includes Lithgow Coal Measures||||||
27802|Illawarra Coal Measures|43359|14|Not recorded|Map Legend||Permian|Provisional first edition||||||
27802|Illawarra Coal Measures|43360|14|Not recorded|Map Legend||Permian|(Provisional first edition)||||||
27802|Illawarra Coal Measures|43361|14|Not recorded|Map Legend||Permian|(Provisional first edition)||||||
27802|Illawarra Coal Measures|43362|14|Not recorded|Map Legend||Permian|(Provisional first edition)Includes Charbon Sub-Group and Nile Sub-Group||||||
27802|Illawarra Coal Measures|43363|14|Not recorded|Map Legend||Permian|(Provisional first edition)||||||
27802|Illawarra Coal Measures|43383|14|Not recorded|p20,23,Fig.3|||||||||
27802|Illawarra Coal Measures|43384|14|Not recorded|Map Legend||Late Permian|||||||
27802|Illawarra Coal Measures|43385|14|Not recorded|p179||Late Permian|||||||
27802|Illawarra Coal Measures|43424|14|Not recorded|p11-15,17|||||||||
27802|Illawarra Coal Measures|43476|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
27802|Illawarra Coal Measures|43477|2|Defined|p22,24,26,41,49,|||p58-60,Pl.1. Equivalent to Newcastle Coal Measures.||||||24-SEP-08
27802|Illawarra Coal Measures|43479|14|Not recorded|p189,218|Tatarian|Kazanian|||||||
27802|Illawarra Coal Measures|43491|14|Not recorded|pVII/54||Permian|||||||
27802|Illawarra Coal Measures|43494|5|Briefly described|p11|Permian|Permian|Thickness: 30m.  Overlies the Gulgong Granite in the north.||||||09-MAR-06
27802|Illawarra Coal Measures|43515|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
27802|Illawarra Coal Measures|43516|14|Not recorded|Map Legend||Permian|||||||
27802|Illawarra Coal Measures|43545|14|Not recorded|p415|||From reprint. Correct reference not given||||||
27802|Illawarra Coal Measures|43676|6|Mentioned|p326|||||||||
27802|Illawarra Coal Measures|43782|5|Briefly described|Map Legend|Late Permian|Late Permian|||||||
27802|Illawarra Coal Measures|43873|14|Not recorded|p53|||||||||
27802|Illawarra Coal Measures|43984|14|Not recorded|p137|||Equivalent to Newcastle Coal Measures.||||||
27802|Illawarra Coal Measures|44093|6|Mentioned|p64 Photo 1|Permian|Permian|Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
27802|Illawarra Coal Measures|44507|14|Not recorded|p104,Fig.1|||||||||
27802|Illawarra Coal Measures|44676|14|Not recorded|p251|||||||||
27802|Illawarra Coal Measures|44834|14|Not recorded|p475|||||||||
27802|Illawarra Coal Measures|44861|4|Described|p226-229,232|||||||||
27802|Illawarra Coal Measures|45006|14|Not recorded|Tb.1,opp.p3|||||||||
27802|Illawarra Coal Measures|45090|6|Mentioned|p27|||Relationship of rock units||||||
27802|Illawarra Coal Measures|45138|6|Mentioned|p2|||||||||
27802|Illawarra Coal Measures|48744|6|Mentioned|p.88.|||||||||
27802|Illawarra Coal Measures|48995|6|Mentioned|p19|||||||||
27802|Illawarra Coal Measures|49644|5|Briefly described|Table|||||||||
27802|Illawarra Coal Measures|50116|5|Briefly described|p66 Fig.2|Permian|Permian|Overlain by the Narrabeen Group. Overlies the Shoalhaven Group. Geological Province: Sydney-Gunnedah Basin.||||||10-MAR-05
27802|Illawarra Coal Measures|60281|4|Described|p62|Late Permian|Late Permian|Sandstone, siltstone shale and coal seams, with minor conglomeratic and tuffaceous beds.  Age: 263-253Ma.  Max. thickness: >500m.  Geological Province: Sydney Basin.See also p6, p11, p61.||||||
27802|Illawarra Coal Measures|60299|6|Mentioned|p223|||||||||
27802|Illawarra Coal Measures|61209|5|Briefly described|p225 Fig. 7b|Paleozoic|Paleozoic|Geological Province: Sydney Basin.||||||07-NOV-08
27802|Illawarra Coal Measures|61315|5|Briefly described|p167,Table SY2|Late Permian|Late Permian|Includes the Cumberland, Sydney, Nile, Cullen Bullen, Charbon and Wallerawang Subgroups. Geological Province: Sydney Basin.||||||
27802|Illawarra Coal Measures|61609|6|Mentioned|p240 Tb. 1, p244, p247|Permian|Permian|Includes Sydney and Cumberland Subgroups. Geological Province: Sydney Basin.||||||07-FEB-11
27802|Illawarra Coal Measures|61610|5|Briefly described|p252, p252 Fig. 2|Permian|Permian|Includes Sydney and Cumberland Subgroups. Geological Province: Sydney Basin.||||||07-FEB-11
27802|Illawarra Coal Measures|61612|6|Mentioned|p274, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin. NSW.||||||17-MAR-09
27802|Illawarra Coal Measures|61772|6|Mentioned|p128||Late Permian|Geological Province: Sydney Basin.||||||24-SEP-08
27802|Illawarra Coal Measures|63461|5|Briefly described|p862|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||10-DEC-07
27802|Illawarra Coal Measures|63832|5|Briefly described|p131 fig 2, p136-137|Lopingian|Guadalupian|Southern Sydney Basin. The basal part shows no glacial indicators, suggesting a brief interglacial interval in the mid-Permian. Contains distal glaciomarine facies (outsized basement clasts in mudrock, glendonites) recording the final (P4) Paleozoic glaciation.|||Includes Nile, Charbon, Cullen Bullen and Wallerawang Subgroups; Wilton, Erins Vale, Allans Creek, Eckersley, Pheasants Nest, Newnes Formations; Bargo Claystone.||Continental proglacial and possibly subglacial facies.|13-DEC-17
27802|Illawarra Coal Measures|64631|5|Briefly described|p44 Fig.2, pp48-49.|Changhsingian|Wordian|SE, SW, NW Sydney Basin. Some units contain distal glaciomarine facies, eg glendonites and outsized basement clasts in mudrocks. Biostratigraphic  age control at base and top in SE.|||Includes Nile, Cullen Bullen, Charbon and Wallerawang Subgroups; and Wilton, Erins Vale, Newnes and Eckersley Formations.|Overlies Shoalhaven Group.||
27802|Illawarra Coal Measures|65490|6|Mentioned|p883|||||||||
27802|Illawarra Coal Measures|66577|6|Mentioned|pp995-996, p997 Fig.2.|Permian|Permian|The coal seams in this unit give rise to high-amplitude reflection horizons in seismic data.|||Includes Woonona, Tongarra, Wongawilli, Bulli Coals; Pheasants Nest, Erins Vale, Wilton, Allans Creek, Eckersley Formations; Darkes Forest, Kembla Sandstones; Bargo Claystone.|Overlies Shoalhaven Group. Is overlain by Narrabeen Group.||
27802|Illawarra Coal Measures|67500|6|Mentioned|p12 Tb.1, p13 Fig.1, p19||||||Includes Pheasants Nest Formation.|||01-MAY-12
27802|Illawarra Coal Measures|67560|6|Mentioned|p258, p261 Fig.3, p263-p269, p271-p272|Permian|Permian|Deposition displays some marine influence.||||Overlain by the Narrabeen Group.||
27802|Illawarra Coal Measures|67663|5|Briefly described|p518, p520 Tb.1|Triassic|Permian|Southern Sydney Basin. Late Permian.|||Includes Pheasants Nest Formation, Bargo Claystone, Erins Vale Formation, Baal Bone Formation, Marrangaroo Conglomerate.|Overlies Gerringong Volcanics and Shoalhaven Group. Is overlain by Narrabeen Group.||
27802|Illawarra Coal Measures|68003|5|Briefly described|p38 Fig.3-j, p42, p131.|Late Permian|Late Permian|Western Coalfield (Sydney Basin), Brigalow Belt South Bioregion. Correlative of Black Jack Group (Gunnedah Basin) and of Singleton Supergroup (Hunter Coafield). Prograding fluvio-deltaic system, fed from the New England region.|||Includes Nile, Cullen Bullen, Charbon and Wallerawang Subgroups.|Overlies Shoalhaven Group. Is overlain by Narrabeen Group.|Quartz-lithic sandstone, mudstone (sporadically carbonaceous), claystone, coal, torbanite, rhyolitic tuff, some lenses of polymictic conglomerate.|
27802|Illawarra Coal Measures|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.|||Includes Wallerawang, Charbon, Cullen Bullen and Nile Subgroups.|Is overlain by Narrabeen Group.||
27802|Illawarra Coal Measures|68202|6|Mentioned|p176|Permian|Permian|Sydney Basin. Swampy-deltaic conditions followed uplift of the New England Orogen in Late Permian.|||Bulli Coal.||Extensive coal deposits.|
27802|Illawarra Coal Measures|68204|6|Mentioned|p47, 54|Permian|Permian|Sydney Basin.||||||
27802|Illawarra Coal Measures|68592|5|Briefly described|p1779|Permian|Permian||||Includes Pheasants Nest Formation.|Overlies Shoalhaven Group. Broadly equivalent to Greta Coal Measures and Maitland Group.||
27802|Illawarra Coal Measures|69297|6|Mentioned|p499, p501, p503|Late Permian|Middle Permian|Sydney Basin. Deposited in a fluvial-deltaic environment. Has some potential as a gas or petroleum source rock.||||Unconformably overlies the Gerringong Volcanics. Overlies the Broughton Formation and the Budgong Sandstone. Unconformably overlain by the Narrabeen Group.|Sandstones, siltstones and coals.|
27802|Illawarra Coal Measures|69683|6|Mentioned|p410, p412|||Coal rank has potentially been influenced by igneous basement heat generation.||||||
27802|Illawarra Coal Measures|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian coal measures: conglomerate, quartzose and lithic sandstone, siltstone, carbonaceous and calcareous mudstone, tuff and coal.||||||
27802|Illawarra Coal Measures|70297|4|Described|map legend, on side 2 of map sheet|Lopingian|Guadalupian|Age: Late Permian. Coal measures. Sydney Basin.||||Overlies Shoalhaven Group. Is overlain by Narrabeen Group.|Shale, quartz-lithic sandstone, conglomerate, chert, sporadically carbonaceous mudstone, coal and torbanite seams.|
27802|Illawarra Coal Measures|70661|3|Fully described|vii, ix, p3, p4, p5, p140, P156|Late Permian|Late Permian|Sydney Basin. Name derived from illawarra region. Previously referred to as Illawarra beds, Bulli Coal Measures, previously included in the Upper Coal Measures before being formally defined as the Illawarra Coal Measures.  Predominantly fluvial and deltaic. Distribution, geomorphology, geochemistry, structure and fossil assemblage discussed. No type section exists. More than 500m thick in total. Deposited as alluvial fan, alluvial plain and deltaic depositional systems. Age derived from palynology and U-Pb SHRIMP dating (no ages given) of tuff horizons.  See also p177, p186-p193, p195, p196.|||Sydney, Cumberland, Wallarawang, Charbon, Nile, Cullen Bullen Subgroups, Wongawilli Seam|Conformably overlies Berry Siltstone, Nowra Sandstone, Broughton Formation disconformably overlain by Hawkesbury Sandstone, conformably overlain by Narrabeen Group|Interbedded lithic quartz sandstone,shale, siltstone, claystone and coal with minor tuff, conglomerate and intrusive units.|
27802|Illawarra Coal Measures|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Southern Sydney Basin.|||Includes Farmborough Claystone, Huntley Claystone, Bulli Coal Seam and Wongawilli Coal.|||
27802|Illawarra Coal Measures|71115|5|Briefly described|p178, 180, 182, 188|Permian|Permian|Southern Sydney Basin.|||Cumberland Subgroup.|Overlies Shoalhaven Group. Is overlain by the Narrabeen Group.||
27802|Illawarra Coal Measures|71303|5|Briefly described|map legend|Lopingian|Lopingian|Of Sydney Basin.|||||Thinly to thickly bedded lithic quartz sandstone, intercalated with thinly bedded shale and siltstone, coal seams; conglomerate lenses and thin vitric tuff layers locally. Coal seams up to metres thick.|
27802|Illawarra Coal Measures|71538|6|Mentioned|p54 fig 2|Lopingian|Lopingian|Sydney Basin. Deltaic depositional environment.||||Overlies the Broughtoun Formation. Overlain by the Hawkesbury Sandstone.||
27802|Illawarra Coal Measures|71542|6|Mentioned|p25|Permian|Permian|Of southern Sydney Basin.||||Underlain by Shoalhaven Group/Broughton Formation.||20-OCT-21
27802|Illawarra Coal Measures|73248|6|Mentioned|p301, p305, p310|Permian|Permian|Known in the Cumberland Basin only from borehole records.||||Underlain by Shoalhaven Group. Conformably overlain by Narrabeen Group.|Includes coals.|
27802|Illawarra Coal Measures|73304|6|Mentioned|p61, p65-66, p74, p76, p78-79|||Sydney Basin. Equivalent[?] to Newcastle Coal Measures. [Top?] boundary marks a major extinction of peat-producing plants. Some constituents include evidence of the P4 glacial episode.|||Thirroul Sandstone, Kembla Sandstone, Farmborough Claystone, Wongawilli Coal, Bulli Coal Seam|||
27802|Illawarra Coal Measures|73421|5|Briefly described|p2 Fig.1, p3, p5, p16|Changhsingian|Capitanian|Sydney Basin, southern.|||Sydney Subgroup, Cumberland Subgroup, Huntley Claystone, Farmborough Claystone|Overlies Broughton Formation, Shoalhaven Group, Underlies Narabeen Group|Sandstones, siltstone, claystone/shale and conglomerate intercalated with latite lava flows in lower part.|
27802|Illawarra Coal Measures|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.|||Cumberland Subgroup; Gerringong Volcanics (upper part).|Overlies Shoalhaven Group.||
27802|Illawarra Coal Measures|73625|6|Mentioned|p2|Permian|Permian|Western and Southern coalfields, Sydney Basin.|||Baal Bone, Eckersley, Erins Vale, Pheasants Nest, Wilton Formations; Angus Place Sandstone, Bargo Claystone, Bulli Coal, Katoomba Coal Member, Marangaroo Conglomerate, Nile Sub-group.|Overlies Berry Siltstone. Is overlain by Narrabeen Group.||
31839|Illunie Volcanics|23392|6|Mentioned|p6|||||||||
31839|Illunie Volcanics|24417|1|Redefined|p44|Ludlow|Wenlock|Of the Douro Group. Formerly "Illunie Rhyolite". Overlain by Warrumba Volcanics.||||||
31839|Illunie Volcanics|50628|5|Briefly described|Map Legend|Silurian|Silurian|Of the Douro Group.  Quartz-plagioclase-biotite phyric rhyodacite. Underlies: Warrumba Volcanics.||||||05-JUL-04
31839|Illunie Volcanics|60009|5|Briefly described|Map Legend|Wenlock|Wenlock|Of the Douro Group.||||||13-JUL-04
24315|Ina Volcanics|22857|4|Described|p446 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Part of Ootha Formation? Andesite and rhyolitic volcaniclastics, shales, sandstones, conglomerates, carbonates. Max. thickness: ~2km. ||||||
24315|Ina Volcanics|24417|3|Fully described|p48|Silurian|Silurian|Name now  includes "Cowal Member" as undifferentiated.  Age: 426+/-3.2Ma (SHRIMP U-Pb).||||||
24315|Ina Volcanics|35503|2|Defined|p205|Silurian|Silurian|New name refs Kemezys (1976)Prob. Silurian||||||
24315|Ina Volcanics|36534|6|Mentioned|p225|||||||||
24315|Ina Volcanics|40328|4|Described|p41|||||||||
24315|Ina Volcanics|50385|5|Briefly described|Map Legend|Silurian|Silurian|Rhyolitic crystal rich ignimbrite, felsic volcanic breccia||||||
24315|Ina Volcanics|50554|5|Briefly described|Map legend|Silurian|Silurian|Rhyolitic crystal-rich ignimbrite, felsic volcanic breccia.||||||24-JUN-04
24315|Ina Volcanics|60008|5|Briefly described|Map Legend|Silurian|Silurian|Felsic volcanics.||||||
24315|Ina Volcanics|60009|5|Briefly described|Map Legend|Wenlock|Wenlock|||||||13-JUL-04
82503|Ingleba Leucomonzogranite|71628|4|Described|p3: 1, 26, 61-64|||Probably named after the Inglebah [sic] homestead. A small intrusion 24 km SSW of Walcha; poor outcrop. Geochemistry described.|289 Ma (Rb-Sr biotite).|Kilburnie Suite (tentative).||Intrudes Sandon Association.|Medium- to coarse-grained biotite syenogranite-monzogranite. S-type.|
67905|Ingleba Monzogranite|71628|5|Briefly described|p3:4|||Landenberger et al. (2010), although on p3-61 of this study it is presented as having appeared as (the informal) Ingleba monzogranite.||Hillgrove Supersuite.||||
76004|Inlet Monzogranite|71628|4|Described|p7: 1, 4, 8, 18-24, 32, 35|||Brown et al. (2010). Previously the Inlet Monzonite of Cooper et al. (1963), then Inlet Quartz Monzonite of Chappell (1978). Named after the local property ""The Inlet"". Forms a small (13.2 km2) ovoid intrusion, ~7 km E of Attunga and ~21 km N of Tamworth. Excellent outcrops include a prominent hill, whalebacks and tors. Has a well-defined contact aureole (described). Several other age determinations given. Composition and geochemistry described in some detail; most mafic unit in the Supersuite. Hosts, and likely source of, a variety of vein and metasomatic Au, Cu, Mo and W mineralisation (briefly described).|251.3 +/- 1.3 Ma (SHRIMP: Jeon et al., 2014).|Inlet Suite.||Intrudes Silver Gully and Horse Arm Formations; Moore Creek and Sulcor Limestone Members.|Weakly zoned, equigranular to porphyritic, mafic-rich, quartz-poor monzogranite, with lesser quartz monzodiorite and granodiorite. Abundant enclaves. I-type.|
83835|Inspiration Point Formation|73582|2|Defined|p99, 105-106, 113-114, 119-120, 126|Pridolian|Wenlockian|Newly defined (this study). Named after Inspiration Point on the Jenolan Caves Road. Includes rocks given numerous, informal names in unpublished student theses and field compilations. Goulburn Basin. Occurs immediately E of Jenolan Caves, extending to at least the Black Range. Forms rugged topography intersected by deep valleys: hence no type section; a type area is specified N of Jenolan Caves. Total thickness is estimated at over 3220m. Lithologies described in detail.||||Conformably overlies Jenolan Caves Limestone. Is faulted against/overlain unconformably by Lambie Group. Correlated with lower to middle Mount Fairy Group.|Tuffaceous sandstone, limestone, siltstone, conglomerate and sandstone, with interbedded silicic lavas (spilite, quartz porphyry, silicic and dacitic flows).|
24317|Inverary Tonalite|40132|2|Defined|p238|Early Devonian|Early Devonian|||||||
24317|Inverary Tonalite|50234|5|Briefly described|Map Legend|Devonian|Devonian|Part of the Marulan Batholith.  See also Inverary Granite (in map strat. chart).||||||13-MAY-04
24317|Inverary Tonalite|68592|6|Mentioned|p1110, p1113, p1610, p1800|||Obsolete. Of Carr et al. (1979). Placed in Arthursleigh Suite by Chappell et al. (1991), but here is assigned to Carne Dacite Member (of the Tangerang Formation), with which it is compositionally and texturally identical.||||||
24317|Inverary Tonalite|70661|6|Mentioned|p78|||||||||
69820|Inverell Volcanics|63347|2|Defined|p5 Fig. 2, p30|Early Miocene|Early Miocene|Of the Delungra Volcanic Suite. Conformably overlie Mount Russell Volcanics. Age: 20Ma (K-Ar). Max. thickness: 80m; <20m in type area. Undersaturated alkaline olivine basalt/basinite and weathered volcaniclastic rocks. See also p6, p13.||||||
69820|Inverell Volcanics|73581|5|Briefly described|p14-15|Early Miocene|Early Miocene||19.8+/-0.2 Ma, 18.5+/-1.0 Ma K-Ar|||Conformably overlies Mount Russell Volcanics|Highly undersaturated olivine basalt up to 5 m thick, interbedded with volcaniclastic units.|
33969|Ironbark Formation|22578|6|Mentioned|p398|||Of Four Mile Creek Subgroup.||||||27-SEP-06
27165|Ironbong Dacite Member|22638|1|Redefined|p66||Early Devonian|Bethungra Formation||||||
27165|Ironbong Dacite Member|35608|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
27165|Ironbong Dacite Member|35609|2|Defined|p78|Early Devonian|Early Devonian|||||||
27165|Ironbong Dacite Member|39626|6|Mentioned|p275|||||||||
27165|Ironbong Dacite Member|44192|5|Briefly described|Map Legend||Lochkovian|||||||
26634|Isabella Granite|23214|4|Described|p258|Carboniferous|Carboniferous|||||||
26634|Isabella Granite|42712|4|Described|Table1p13; Fig3p9;12|Carboniferous|Early Carboniferous|Variation on Isabella Granodiorite.||||||
26634|Isabella Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
26634|Isabella Granite|43633|6|Mentioned|p18|||||||||
26634|Isabella Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
26634|Isabella Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
26634|Isabella Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
31592|Isabella Suite|42726|5|Briefly described|map legend||Carboniferous|||||||
31592|Isabella Suite|44093|5|Briefly described|p214 App. 1|Late Carboniferous|Late Carboniferous|Geological Province: Lachlan Fold Belt.||||||
70490|Isismede Ignimbrite Member|62095|2|Defined|p272 Appdx.|Early Carboniferous|Late Devonian|Oldest member of Merlewood Formation. Pale-red, partly reworked, unwelded ignimbrite. Age:ca352Ma. Max. thickness: 15m. Geological Province: Werrie block/Tamworth Belt. See also p251.||||||31-JAN-08
70490|Isismede Ignimbrite Member|70777|5|Briefly described|p2, p82|Early Carboniferous|Early Carboniferous|New England Orogen. Age derived from Roberts et al., 2006.|355.5 +/- 2 to 351.7 +/- 3.2 Ma|Merlewood Formation||||
31591|Island Bend Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
29576|Ivor Leucogranite|22638|4|Described|p78||Late Devonian|New name.||||||
29576|Ivor Leucogranite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
23664|Jackalass Slate|22638|6|Mentioned|p9|||||||||
23664|Jackalass Slate|22687|6|Mentioned|110|Early Silurian|Ordovician|Geol province Lachlan Fold Belt||||||
23664|Jackalass Slate|22768|5|Briefly described|p173-74|Early Silurian|Late Ordovician|||||||
23664|Jackalass Slate|22857|4|Described|p173, p452 App.1, Tb.A1.6|Silurian|Silurian|Age: 428Ma (U/Pb SHRIMP zircon). Major controversy has arisen in dating and interpreting rocks of the Tumut Trough which include this unit and the Bumbolee Creek Formation (see p173-174).||||||
23664|Jackalass Slate|24266|5|Briefly described|p1482|Silurian|Early Silurian|Geological Province: Lachlan Fold Belt. Overlying unit: Bumbolee Creek Formation.||||||09-MAR-05
23664|Jackalass Slate|37529|5|Briefly described|p8|||||||||
23664|Jackalass Slate|42045|6|Mentioned|Fig.2 P148|||||||||
23664|Jackalass Slate|42313|2|Defined|p88|Middle Silurian|Early Silurian|Age: late Early to early Middle Silurian||||||
23664|Jackalass Slate|42314|5|Briefly described|Map|Middle Silurian|Early Silurian|||||||
23664|Jackalass Slate|42828|5|Briefly described|Fig.2 P128|||||||||
23664|Jackalass Slate|44092|5|Briefly described|map legend|Early Silurian|Early Silurian|Smf3||||||
23664|Jackalass Slate|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
23664|Jackalass Slate|60280|5|Briefly described|p1-2|Early Silurian|Early Silurian|Together with the Bumbolee Creek Formation is the equivalent of the Brawlin Formation in the Tumut area.||||||12-AUG-04
23664|Jackalass Slate|63290|6|Mentioned|p403 Fig. 6(c)|Late Silurian|Late Silurian|Geological Province: Tumut Block.||||||
23664|Jackalass Slate|66197|5|Briefly described|p631 Fig.3a|||Deep marine shale. Underlies the Bumbolee Creek Formation, overlies the Gooandra Volcanics. Tumut Trough.||||||14-MAR-12
23664|Jackalass Slate|69043|5|Briefly described|p3, p5, p69-73, p118|Silurian|Silurian|Tumut Trough: S of Gundagai. Hosts (previously thought to be intruded by) an altered tonalite aged 501.2 +/- 2.6 Ma (ie Cambrian); now thought that both were incorporated in a Middle Silurian melange.|||||Part of a siltstone- and sandstone-matrix melange.|
23664|Jackalass Slate|71708|5|Briefly described|p337, 345, 355|Early Silurian|Early Silurian|Present in the Tumut Trough||||Intruded by an "older tonalite block", here called the Edwardstown Tonalite (p345)|Includes sandstone and siltstone.|
23664|Jackalass Slate|73082|6|Mentioned|p16-17|||Gundagai area.|||||Contains auriferous quartz (+/- calcite, talc) veins and auriferous shear zones.|
23664|Jackalass Slate|73154|6|Mentioned|p91|||||||||
36474|Jamon Granite|23550|5|Briefly described|p505|||A-type granite.||||||
34022|Jasdec Park Sandstone Member|22601|6|Mentioned|410|Permian|Permian|Geol province Sydney Basin. Of the Branxton Formation. Underlying unit Rowan Formation.||||||
34022|Jasdec Park Sandstone Member|23350|5|Briefly described|272|||Of the Branxton Formation.  See also p261 Fig. 2.  Sandstone is Sst in text.||||||15-JUL-04
34022|Jasdec Park Sandstone Member|70791|5|Briefly described|p283, p293 Fig.17|Guadalupian|Guadalupian|Hunter Coalfield. Has a disconformity at its base. The rank (Member) was omitted on p283.||Basal Branxton Formation.||||
76043|Jawbone Creek Granodiorite Suite|66934|6|Mentioned|Map legend|Early Devonian|Early Devonian|Informal name.|||Includes Wanganella and Windouran Swamp granodiorites.|||04-OCT-13
80457|Jawbone Creek granodiorite|70718|5|Briefly described|p61-p63, p64|||Informal name, interpreted from geophysics. Magnetic signatures suggest whole suite is I-type.||Jawbone Creek granodiorite suite||||30-MAY-19
73551|Jeffreys Flat Formation|66623|2|Defined|p46, pp98-101, pp104-107.|Early Ordovician|Late Cambrian|Defined in this study.Originally part of Torrowangee Series (Mawson 1912); named after Jeffreys Flat beds of Scheibner and Basden (1996). Correlated with Easter Monday Formation and possibly Yancannia Formation and Dullingari Group. Thickness c.4-5 km. Trace fossils only. Contains cross- and graded-bedding, ripple marks and flute casts.|Between c.510 Ma and c.422 Ma.|Unit in Warratta Group.||Overlies Depot Glen Formation. Is unconformably overlain by Namur Sandstone.|Variably cleaved phyllite and (commonly pyritic) slate, originally siltstone with minor sandstone beds; minor quartzite, conglomerate and limestone.|
73551|Jeffreys Flat Formation|66921|5|Briefly described|Map legend|Cambrian|Cambrian|Seven un-named sub-units are mapped separately.||Unit in Warratta Group.||Is overlain by Easter Monday Formation.|Variably cleaved phyllite and slate, originally siltstone with minor sandstone beds; local minor limestone and conglomerate.|
73551|Jeffreys Flat Formation|67105|6|Mentioned|p659|||||Warratta Group.|||Shallow-marine deposits, including diamictite, minor limestone.|
73551|Jeffreys Flat Formation|67207|5|Briefly described|Map legend.|Cambrian|Cambrian|Has six un-named sub-units of varying lithologies mapped separately.||Unit in Warratta Group.|||Variably cleaved phyllite and slate; originally siltstone with minor sandstone beds, local  minor limestone and conglomerate; local quartzo-feldspathic sandstone, impure limestone, slate with diagenetic pyrite, diamictite conglomerate.|
73551|Jeffreys Flat Formation|67209|5|Briefly described|Map legend.|Cambrian|Cambrian|Three un-named sub-units with differing lithologies are mapped separately.||Unit in Warratta Group.|||Variably cleaved phyllite and slate, originally siltstone with minor sandstone beds, local minor limestone and conglomerate; regionally metamorphosd to greenschist facies.|
73551|Jeffreys Flat Formation|67322|4|Described|p13; Fig.5|Cambrian||(Greenfield, in Greenfield et al.,2010). Lithologies imply shallowing from deep marine to shelfal environment. Age is based on the presence of branching to sinuous trace fossils from siltstone-sandstone interbeds. Occurs only in the Warratta Inlier.||Of the Warratta Group.||Overlies Yancannia Formation. Is overlain by Easter Monday Formation.|Pyritic siltstone-mudstone is overlain by impure limestone, diamictite (including boulders of felsic tuff), rippled sandstone beds and clean quartzite.|22-FEB-18
73551|Jeffreys Flat Formation|68823|5|Briefly described|p383|Middle Cambrian|Middle Cambrian|Age from a deformed felsic tuff; basement to Warratta Group.|510.4 +/- 3 Ma, SHRIMP (Greenfield 2010a)|||||
73551|Jeffreys Flat Formation|69001|5|Briefly described|p2 Fig.1B, p13, p59|Cambrian|Cambrian|Occurs within the Warratta Inlier. Approximately 2 km thick.||Of the Warratta Group.|||Comprises a turbidite sequence with pyritic siltstone and minor conglomerate and limestone.|
73551|Jeffreys Flat Formation|69002|5|Briefly described|p7, p8|Stage 5|Stage 4|Shallow water depositional environment. Age constrained by rounded boulders of deformed felsic tuff in a diamictite unit.|c. 510.4 +/- 3 Ma (Greenfield 2010b)|Of the Warratta Group.||Correlative of the Easter Monday Formation.||
73551|Jeffreys Flat Formation|69043|6|Mentioned|p11|||Thomson Orogen.||||||
73551|Jeffreys Flat Formation|69541|5|Briefly described|p648, p654|||Deep to shallow marine; cleaved and metamorphosed to greenschist facies. Three zircons from this [Cambrian] unit had ages of 148+/-6 Ma, 147+/-6 Ma and 142+/-6 Ma. Used to demonstrate zircon crystallisation in older rocks from younger hydrothermal or magmatic fluids.||Unit in Warratta Group.|||Phyllite, slate, lesser quartz- to quartz-feldspar sandstone; rarer conglomerate, and limestone.|
73551|Jeffreys Flat Formation|70749|5|Briefly described|p42-43|Ordovician|Cambrian|Warratta Inlier. Shelf to deep-marine deposits.|||||Variably deformed and metamorphosed siltstone, sandstone and mudstone.|
73551|Jeffreys Flat Formation|71415|5|Briefly described|p11,15|||Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Associated with marine deposition and volcanism post-delamarian Orogeny. Underwent deformation and metamorphism between c. 441-424 Ma, intruded by post-D1 monzodioritic sills and dykes between c. 423 and 416 Ma, and by Tibooburra Granodiorite. Contains zircon age populations at c. 575, 505 and 484 Ma (Greenfield, Gilmore and Mills 2010; Glen 2013).||Unit of Warratta Group.||||
73551|Jeffreys Flat Formation|71965|5|Briefly described|p897,900|||Geological province: Thomson Orogen. Occurs in the Warratta Inlier. Depositional environment: Shallow marine shelf to deep marine. Maximum depositional age at 510.4+\-3 Ma, based on the age of a rounded boulder.||Unit of Warratta Group.||Correlable with Easter Monday Formation.|Variably cleaved phyllitic slate, minor quartzite, conglomerate and limestone.|
73551|Jeffreys Flat Formation|73177|5|Briefly described|p1098-1099, 1110, 1112, p1113 Fig 15|Late Cambrian|Late Cambrian|See also p1115 Fig 17, 1118. Thomson Orogen. Crops out near Tibooburra. Underwent Benambran deformation c.450 Ma.|510.4 +/- 3.0 Ma (MDA; Greenfield et al., 2010).|Warratta Group.||Equivalent to Easter Monday Formation and Yancannia Formation.||
39362|Jeffries Formation|24123|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Sydney Basin.||||||
28225|Jemidee Microgranodiorite|37986|2|Defined|p314|Early Devonian|Early Devonian|||||||
28225|Jemidee Microgranodiorite|68592|5|Briefly described|p1610-1|||Hutton (1981). Mapped by Simpson (1979) as several bodies of unnamed rhyodacite. Has very irrregular contacts with adjacent Barrallier Ignimbrite. Similar to Carne and Bogungra Dacite Members; most are interpreted as small, high-level intrusive bodies emplaced at various times during eruption of the Bindook Group.||||Contact metamorphosed by Bullio Granite.|Pinkish-green, crystal-rich rhyodacite; massive, locally columnar jointed.|
28225|Jemidee Microgranodiorite|70661|6|Mentioned|p78|||||||||
82506|Jenners Monzogranite|71628|4|Described|p11: 4, 38-39; p12: 8, 15; p15:2, 34-35|Middle Triassic|Middle Triassic|See also p15: 51-56, 58, 61, 63-65, 68-69, 72, 77-78, 80, 82, 85, 97, 100, 115; p19: 19, 81-83, 88. New name, after a local watercourse. Comprises two large bodies and some smaller masses, from Stanthorpe to Bookookoorara. Exposure and outcrop forms vary. The relationship with adjacent units is discussed. Geochemistry detailed. Hosts several vein Au-Ag-polymetallic mineralisation (prospects named) and one Sn-W deposit. RELATED UNITS (continued): Encloses the older Gleamwoods and Storm King Monzogranites, and parts of Karonstadt Complex. Abuts Mount Lindesay Monzogranite and Mount Norman Leucomonzogranite.|241.2 Ma (Shaw and Flood, 1993).|Stanthorpe Complex.||Intrudes Undercliffe Falls Monzogranite. Abuts/is intruded by Ruby Creek Leucogranite. Bounds Bookookoorara Monzogranite. Is faulted against Severn River Monzogranite. See COMMENTS for more.|Pale pink, off-white to buff, or pale brown to brown, porphyritic coarse- to fine-grained (groundmass), biotite-(hornblende) K-feldspar-rich monzogranite to syenogranite; locally flow-aligned. I-type.|
82505|Jenners Suite|71628|5|Briefly described|p15: 35, 53, 68, 72, 77|Middle Triassic|Early Triassic|Ropers Creek Monzogranite Phase is geochemically assigned to this Suite.||Stanthorpe Supersuite.|Jenners, The Ram Swamp Monzogranites; Ropers Creek Monzogranite Phase.|||
77277|Jenny Lind Tonalite|71628|3|Fully described|p9: 31-34; p19:26|||Name reserved in ASUD by Blevin and used in this study. Originally Jenny Lind Granite of Thomson (1976). Subsequently Jenny Lind Granodiorite (Bryant et al., 1997). Named after a local creek. Crops out in mostly inaccessible country along the Clarence River, 12km NNW of Tabulam. Excellent exposures in riverside cliffs and slopes. Type locality is along the Clarence River between GR 447220 and GR 483215 (Drake 1:100 000 Geology Sheet). Geochemistry described. Is spatially associated with small, vein-hosted Au and Sb deposits, a small Mo deposit, and a small multi-vein base metal-precious metal deposit (all named).|255.3 +/- 1.2 Ma (SHRIMP: Waltenberg et al. 2016).|||Intrudes Emu Creek Formation and Drake Volcanics. Is overlain locally by Gatton Sandstone and Laytons Range Conglomerate.|Light grey, medium-grained, equigranular hornblende-biotite-pyroxene quartz diorite, quartz monzodiorite, tonalite, and granodiorite. I-type.|
77369|Jeralong Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
33682|Jerangle Metamorphic Complex|22576|6|Mentioned|p201|||||||||
33682|Jerangle Metamorphic Complex|22721|6|Mentioned|p501, Fig.1 p502|||||||||
33682|Jerangle Metamorphic Complex|22815|2|Defined|p32, fig13|||Age: Could be Early Ordovician to Late Cambrian||||||
33682|Jerangle Metamorphic Complex|22857|6|Mentioned|p135|Ordovician|Ordovician|Geological Province: Monara Forearc Basin. ||||||
33682|Jerangle Metamorphic Complex|23245|6|Mentioned|p135|||||||||
33682|Jerangle Metamorphic Complex|23550|5|Briefly described|p504|||Also see p502 Fig 1||||||
33682|Jerangle Metamorphic Complex|24310|5|Briefly described|p1044|||Geological Province: Lachlan Fold Belt||||||
33682|Jerangle Metamorphic Complex|43233|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
33682|Jerangle Metamorphic Complex|60904|5|Briefly described|p784 Fig. 10|||Of the Lachlan Orogen. See also Jerangle metamorphic complex.||||||
33682|Jerangle Metamorphic Complex|61413|6|Mentioned|p2 Fig.1.|||||||||
33682|Jerangle Metamorphic Complex|61964|6|Mentioned|p81|||Supersedes "Jerangle Igneous Complex". ||||||
26638|Jeremadra Granodiorite|35248|6|Mentioned|Fig.1|||||||||
26638|Jeremadra Granodiorite|42497|5|Briefly described|Map Legend|Zlichovian|Pragian|||||||
74243|Jeremy Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Grey to khaki laminated to very thinly-bedded chloritic siltst+mudst. with thin fine-gr. sst beds, schistose massive to diffusely bedded med.gr. poorly sorted chloritic feldspathic sst + minor poorly-sorted (bimodal) to well-sorted qtz-rich sst.||||||
74243|Jeremy Formation|68592|3|Fully described|p142, p390, p398-9, p408-26, p607, p611|Llandovery|Llandovery|See also p74 Tb.5, p86. Newly named & described; problematic stratigraphic history outlined. The southern extension of the Triangle Formation has been assigned to Jeremy Formation. Outcrops of Rockley Volcanics in the Isabella River area are reassigned to this unit. A representative locality is specified. Thickness to 1km. Has a mixed mafic volcanic/quartzose provenance, suggesting nearby juxtaposition and local erosion of the Macquarie Arc (Rockley Volcanics) and Adaminaby Group. Well-cleaved or strongly schistose; local crenulation cleavage or kink bands. Very similar to basal Fosters Creek Conglomerate. Peelwood structural zone: deformation and metamorphism described.||||Overlies Abercrombie Formation. Is overlain by Kildrummie Formation (probably faulted contact) and Cuddyong Formation (unconformably).|Grey to khaki, laminated to very thinly bedded chloritic schist, siltstone, and volcaniclastic sandstone; all contain a significant proportion of quartzose detritus.|23-SEP-16
74243|Jeremy Formation|70192|5|Briefly described|Map Legend|Llandovery|Llandovery|Sxy. Ungrouped Silurian formation. Includes one unnamed subunit of laminated to very thinly bedded chloritic siltstone and mudstone with thin, fine grained sandstone beds. Minor quartzofeldspathic sandstone is bimodal to well sorted. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Age max and min boundaries on Time-Space plot are marked with ?-?-?.|||Includes one unnamed unit.||Laminated-very thinly bedded chloritic siltstone and mudstone with fine grained sandstone beds; schistose massive-diffusely bedded, medium grained, poorly sorted chloritic feldspathic sandstone. Minor quartz rich-quartzofeldspathic sandstone.|
74243|Jeremy Formation|70543|5|Briefly described|Map Legend |Silurian|Silurian|Includes one unnamed subunit of laminated to very thinly bedded chloritic siltstone and mudstone with thin, fine grained sandstone beds. Minor quartzofeldspathic sandstone is  bimodal to well sorted.|||Includes one unnamed subunit.||Laminated-very thinly bedded chloritic siltstone and mudstone with fine grained sandstone beds; schistose massive-diffusely bedded, medium grained, poorly sorted chloritic feldspathic sandstone. Minor quartz rich-quartzofeldspathic sandstone.|
74243|Jeremy Formation|71656|6|Mentioned|p13 Fig.2|Llandovery|Llandovery|Shown only in correlation chart (Fig.2). Not assigned to any group.||||||
83470|Jerrabattgulla Creek Basalt|73581|6|Mentioned|p24|Oligocene|Eocene|Presently ungrouped. Also written as Jerrabattgulla Creek basalt.|~25-40 Ma||||Basalt.|
75048|Jerrabuttgulla Creek basalts|64827|3|Fully described|p1049-p1060|Miocene|Miocene|Informal name used throughout this paper, for basalt flows lying in the upper Shoalhaven River catchment. Age:~<23.7Ma, details discussed. Forms multiple lobes east of the Shoalhaven Fault scarp, the largest outcrop of at least 3 flows being 90m thick.||||||
40919|Jerrara Formation|50234|5|Briefly described|Map Legend|Llandovery|Llandovery|Thinly-bedded massive to laminated siltstone with minor graptolitic black shale horizons; ironstone; limestone.||||||13-MAY-04
40919|Jerrara Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Thinly-bedded massive to laminated siltstone with minor black graptolitic shale horizons; also contains ironstone and limestone subunits.||||||11-JUN-08
40919|Jerrara Formation|68592|2|Defined|p16, p74 Tb.5, p352,p367, p408-26, p1867|Llandovery|Llandovery|Formerly Jerrara Series; presumably named after the parish of Jerrara, County Argyle. E of Goulburn. Type locality described. Thickness >300m. Bedding surfaces have very fine-grained mica. Goulburn structural zone: deformation described. Fossil fauna described.||||Is faulted against Dignams Siltstone. Same age as Hanaminno Limestone. Correlated with State Circle Shale.|Uniform, massive to laminated dark grey shale that weathers to pale grey; very friable in places; minor black graptolitic shale; minor limestone, probably allochthonous, and ironstone.|
40919|Jerrara Formation|70192|5|Briefly described|Map Legend|Llandovery|Llandovery|Sxj. Ungrouped Silurian formation. Contains two unnamed members; one of ironstone and one of limestone. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.|||Includes two unnamed units.||Grey, thinly bedded, massive to laminated shale with minor black graptolitic shale horizon, minor limestone and ironstone present.|
40919|Jerrara Formation|70542|5|Briefly described|Map Legend|Silurian|Silurian|Contains two unnamed members; one of ironstone and one of limestone.|||||Grey, thinly bedded, massive to laminated shale with minor black graptolitic shale horizon, minor limestone and ironstone present.|
40919|Jerrara Formation|71069|6|Mentioned|p93|||||||||
40919|Jerrara Formation|71656|5|Briefly described|p10 Fig.1, p13 Fig.2, p16, 29, 30|Llandovery|Llandovery|Several species of monograptids described from what was then known as the Jerrara Series near Bungonia, and subsequently (Naylor 1939) provided expanded faunal lists from this area. Not assigned to a group.|||||Fossiliferous strata.|
40919|Jerrara Formation|71700|6|Mentioned|CD|Llandovery|Llandovery|||||||
26639|Jerrys Plains Subgroup|22607|6|Mentioned|p 57|||||||||
26639|Jerrys Plains Subgroup|22857|4|Described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wittingham Coal Measures (Singleton Supergroup). Includes Archerfield Sandstone. Numerous coal seams; claystone, tuff, siltstone, sandstone, conglomerate. Max. thickness: 800m. Geological Province: Sydney Basin.||||||
26639|Jerrys Plains Subgroup|22969|4|Described|Fig 4.1a||Late Permian|||||||
26639|Jerrys Plains Subgroup|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26639|Jerrys Plains Subgroup|39693|6|Mentioned|p18|||||||||
26639|Jerrys Plains Subgroup|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26639|Jerrys Plains Subgroup|40805|4|Described|p142|||||||||
26639|Jerrys Plains Subgroup|41010|6|Mentioned|p11|||||||||
26639|Jerrys Plains Subgroup|41054|6|Mentioned|p156|||||||||
26639|Jerrys Plains Subgroup|41604|6|Mentioned|Fig.2|||||||||
26639|Jerrys Plains Subgroup|41834|6|Mentioned|p590|||||||||
26639|Jerrys Plains Subgroup|41902|5|Briefly described|p5 Table 1|||||||||
26639|Jerrys Plains Subgroup|42078|6|Mentioned|p4|||||||||
26639|Jerrys Plains Subgroup|42648|6|Mentioned|p36, p37|||||||||
26639|Jerrys Plains Subgroup|42916|5|Briefly described|Table 1||Late Permian|||||||
26639|Jerrys Plains Subgroup|42922|6|Mentioned|p38|||||||||
26639|Jerrys Plains Subgroup|42965|6|Mentioned|p37|||||||||
26639|Jerrys Plains Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
26639|Jerrys Plains Subgroup|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Of Wittingham Coal Measures, Singleton Subgroup, Hunter region, Sydney Basin.||||||
26639|Jerrys Plains Subgroup|43257|5|Briefly described|Map Legend||Late Permian|Of Wittingham Coal Measures.||||||
26639|Jerrys Plains Subgroup|43752|6|Mentioned|p617|||||||||
26639|Jerrys Plains Subgroup|44244|2|Defined|p237|Late Permian|Late Permian|Of the Wittingham Coal Measures. Includes Burnamwood, Fairford, Mount Thorley, Milbrodale, Mount Ogilvie, Malabar, Althorpe and Mount Leonard Formations.  Max. thickness: 800m.Overlies the Archerfield Sandstone; underlies Denman Fm.  Type section in text||||||20-APR-05
26639|Jerrys Plains Subgroup|50268|5|Briefly described|Map Legend|Tatarian|Tatarian|Geological Province: Sydney Basin. Of the Wittingham Coal Measures. Overlies: Archerfield Sandstone.||||||25-SEP-08
26639|Jerrys Plains Subgroup|61529|5|Briefly described|p854 Fig. 1b|Late Permian|Late Permian|Of the Wittingham Coal Measures. Overlies Archerfield Sandstone. Geological Province: Sydney Basin.||||||
26639|Jerrys Plains Subgroup|61770|6|Mentioned|p111|||||||||
26639|Jerrys Plains Subgroup|68003|5|Briefly described|p38 Fig.3-j, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Unit in Wittingham Coal Measures.||Overlies Archerfield Sandstone. Is overlain by Denman Formation.||
26639|Jerrys Plains Subgroup|68004|5|Briefly described|p23 Table 1, p51 Table 5, p52, p155.|Late Permian|Late Permian|Hunter Coalfield. Table 5 shows Denman Formation as part of this unit.||Unit in Wittingham Coal Measures.|Includes Burnamwood, Fairford, Mount Thorley, Milbrodale, Mount Ogilvie, Malabar, Althorpe and Mount Leonard Formations.|Overlies Archerfield Sandstone. Is overlain by Denman Formation.||
26639|Jerrys Plains Subgroup|69683|5|Briefly described|p411 Fig.2, p415, p420-421|Late Permian|Late Permian|Predicted to have maturities suitable for oil and gas generation. Coals are predominantly vitrinite-rich; greater permeabilities may be due to well-developed cleat and fracture systems associated with these bright coals.||Unit in Wittingham Coal Measures.|Includes Burnamwood, Fairford, Mount Thorley, Milbrodale, Mount Ogilvie, Malabar, Althorpe and Mount Leonard Formations.|||
26639|Jerrys Plains Subgroup|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield.||Wittingham Coal Measures.||||
26639|Jerrys Plains Subgroup|73304|6|Mentioned|p65-67, p75-76|||[Also written as Jerrys Plains Sub-Group].||Whittingham Coal Measures, Singleton Supergroup|Fairford Formation|||
34631|Jerula Limestone Member|22831|4|Described|p 57|||Gleninga Formation||||||
34631|Jerula Limestone Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Gleninga Formation (Yarra Yarra Creek Group). Geological Province: Darling Basin.||||||
34631|Jerula Limestone Member|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
34631|Jerula Limestone Member|61894|6|Mentioned|p179 Fig.3|||||||||
34631|Jerula Limestone Member|66197|5|Briefly described|p635 Fig.5a|||Jemalong Trough. Shallow marine limestone.||||||14-MAR-12
34631|Jerula Limestone Member|66498|6|Mentioned|p45|||The name appears minus the lithology.||Gleninga Formation.||||
34631|Jerula Limestone Member|70751|6|Mentioned|p12|Pragian|Pragian|||Gleninga Formation||||
34631|Jerula Limestone Member|71039|6|Mentioned|p14|||Outcrops on Bogong Station and Boona Gap.||Yarra Yarra Creek Group|||Limestone.|
34631|Jerula Limestone Member|72958|6|Mentioned|p11|Pragian|Pragian|Cobar Basin. Nymagee area.||Gleninga Formation, Yarra Yarra Creek Group, Cobar Supergroup||||
31720|Jesse Limestone Member|22472|6|Mentioned|p38 Fig.3(a)|Middle Devonian|Early Devonian|||||||
31720|Jesse Limestone Member|22590|5|Briefly described|P752||Emsian|||||||
31720|Jesse Limestone Member|22857|5|Briefly described|p476 App.1 Tb.A1.6|Emsian|Pragian|Of the Limekilns Formation (Kandos Group). Geological Province: Capertee Rise.||||||09-MAR-06
31720|Jesse Limestone Member|23214|4|Described|p203|Emsian|Lochkovian|Of Limekilns Formation. Formerly Jesse Limestone and Diamond Creek Limestone.  Fossiliferous limestone.  Max. thickness: 60m.||||||
31720|Jesse Limestone Member|23738|5|Briefly described|p252||Devonian|Parent: Limekilns Formation.||||||
31720|Jesse Limestone Member|43641|5|Briefly described|Map Legend|Devonian|Devonian|of Limekilns Formation.||||||
31720|Jesse Limestone Member|43782|5|Briefly described|Map Legend|Emsian|Emsian|of Limekilns Formation.||||||
31720|Jesse Limestone Member|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Limekilns Formation||||
74030|Jibbinbar Granite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|White to pale brown, pale grey, or brown to reddish brown, fine- to medium-grained, mainly even-grained (allanite-titanite-)biotite syenogranite; commonly altered.||||||
74030|Jibbinbar Granite|63748|4|Described|p30-31|||In the Mount You You Suite. Intrudes Texas beds. Mainly white to pale brown, pale grey, or brown to reddish-brown, fine- to medium-grained, even-grained biotite syenogranite. See also p27 Fig.27||||||07-FEB-11
74030|Jibbinbar Granite|65668|5|Briefly described|p1, p2 Tb.1, p16-18|Permian|Permian|Stanthorpe area; New England Orogen. Formerly of the Ruby Creek Granite (Olgers, 1974). Redefined (Donchak et al., 2007) on age, geochemical and mineralogical grounds as part of Mount You You Supersuite. Age 298.1 +/- 2 Ma (SHRIMP U-Pb zircon). Buff, fine-medium grained altered leucocratic biotite syenogranite.||||||
74030|Jibbinbar Granite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, as well as Ballandean, Clare Hills, Fairleigh, Herries, Mount Bullaganang, Mount You You and Palgrave Granites; Boxwell and Greymare Granodiorites; are all mapped under the symbol, Pgn.||||||
74030|Jibbinbar Granite|68679|5|Briefly described|p445, p454-457, p466|Permian|Permian|Northern New England Batholith. ~7 km2. The oldest of several small leucogranite stocks. Had been mapped as Ruby Creek Granite (Robertson, 1974); differences listed. Appears as Jibbenbar Granite on p445. Associated with As mineralisation in quartz veins and lodes, with erratic Au values.|298.1 +/- 2.0 Ma (SHRIMP: Cross et al., 2009).|Mount You You Suite.|||Fine- to medium-grained, mainly even-grained, leucocratic biotite syenogranite; texturally heterogeneous; common granophyric intergrowths; enclaves of country rock near contact. Reduced, moderately-highly evolved, high-K, I-type.|
74030|Jibbinbar Granite|68901|5|Briefly described|p8, p6|Early Permian|Early Permian|New England Region. SHRIMP age derived from Cross et al, 2009.|298.1 +/- 2 Ma (SHRIMP U-Pb)|||||26-SEP-18
74030|Jibbinbar Granite|69639|5|Briefly described|p44, p220|Asselian|Gzhelian|New England Orogen.|298.1 +/- 2 Ma (Cross et al, 2009)|Mount You You Supersuite||||
74030|Jibbinbar Granite|70373|6|Mentioned|p790, p804|Early Permian|Late Carboniferous|Texas Orocline area.|~298 Ma||||S type granitoids.|
74030|Jibbinbar Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|298+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
74030|Jibbinbar Granite|71628|5|Briefly described|p5: 1|||Donchak et al. (2007). Now Jibbinbar Leucosyenogranite.||Mount You You Suite.||||
74030|Jibbinbar Granite|73202|6|Mentioned|p637|Asselian|Gzhelian|Anaiwan terrane (also spelt Anawian), western. I-type plutonism.|298.1 +/- 2 Ma|||||
82508|Jibbinbar Leucosyenogranite|71628|4|Described|p5: 1-4, 8-9; p19:150|Permian|Permian|Originally the Jibbinbar Granite (Donchak et al., 2007); the name is changed (?in this study) to reflect the dominant lithology. Named after the parish of Jibbinbar or Mount Jibbinbar where the unit crops out prominently. Occurs ~30 km SW of Stanthorpe; forms pavements, prominent bare rock outcrops, and numerous boulders. Geochemistry described. Associated with significant As (-Au, Ag) mineralisation: probably metahydrothemal rather than granite-related in origin.|298.1 +/- 2.0 Ma (SHRIMP: Cross et al., 2009).|Mount You You Suite.||Intrudes the Texas beds.|White to pale brown, pale grey, or brown to reddish brown; fine- to medium-grained, typically even-grained but locally porphyritic, biotite syenogranite; commonly altered. I-type.|
29245|Jillamatong Granodiorite|22606|6|Mentioned|P830|||||||||
29245|Jillamatong Granodiorite|22815|4|Described|p45|Silurian|Silurian|Must be older than 411.3+/-9.4 Ma.||||||
29245|Jillamatong Granodiorite|23439|6|Mentioned|p130|||||||||
29245|Jillamatong Granodiorite|23551|5|Briefly described|p495|||S-type granite. Kosciusko Batholith.||||||
29245|Jillamatong Granodiorite|24222|5|Briefly described|p11|||Of the Bullenbalong Suite. Chemistry of samples reported. S-type.  Geological Province: Lachlan Fold Belt.||||||24-JAN-06
29245|Jillamatong Granodiorite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
29245|Jillamatong Granodiorite|35109|2|Defined|p55|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
29245|Jillamatong Granodiorite|35263|6|Mentioned|p222|||||||||
29245|Jillamatong Granodiorite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
29245|Jillamatong Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
29245|Jillamatong Granodiorite|40328|4|Described|p207|||||||||
29245|Jillamatong Granodiorite|41888|5|Briefly described|p1184|||||||||
29245|Jillamatong Granodiorite|41898|5|Briefly described|p1184|||||||||
29245|Jillamatong Granodiorite|41905|2|Defined|p57|Silurian||||||||
29245|Jillamatong Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
29245|Jillamatong Granodiorite|43158|5|Briefly described|7,9,10|||||||||
29245|Jillamatong Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
29245|Jillamatong Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb16.||||||
29245|Jillamatong Granodiorite|49705|5|Briefly described|p40|||||||||
29245|Jillamatong Granodiorite|60078|6|Mentioned|Map Legend||Silurian|||||||
29245|Jillamatong Granodiorite|68310|6|Mentioned|p235, 239-241|||Kosciuszko Batholith. S-type.||||||
29245|Jillamatong Granodiorite|72571|5|Briefly described|p90, p92, p96-98, p100-101|||Of the Tasmanides of eastern Australia. Petrography of sample and zircon description and analyses are discussed in detail. S-type.||Bullenbalong Suite|||Cordierite granite with ilmenite.|
23668|Jilleon Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures). Upward coarsening sandstone; subordinate siltstone to medium-grained sandstone; thin coal seams, sideritic bands. Max. thickness: 280m. Geological Province: Sydney Basin.||||||
23668|Jilleon Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Craven Subgroup.    Geological Province: New England Fold Belt||||||
23668|Jilleon Formation|40872|6|Mentioned|Fig.2|||||||||
23668|Jilleon Formation|41054|6|Mentioned|p153|||||||||
23668|Jilleon Formation|44244|4|Described|p184-185, p168 Tb.2|Late Permian|Late Permian|Contains the Cloverdale coal seam.  Conformably overlies Wards River Conglomerate; conformably underlies Leloma Formation.  Max. thickness: 280m.  Geological Province: Myall Block.  Type section in text.||||||19-AUG-04
23668|Jilleon Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures).  Geological Province: Western Myall Block.||||||
74201|Jimberoo Formation|61964|3|Fully described|p123, p124-125|Late Devonian|Late Devonian|Previously known as "Stitts Member", later replaced by "Jimberoo Member". Now upgraded to formation status in Cocoparra Gp. Detailed lithology given.Conformable on Melbergen Sandstone; underlies Mailman Gap Mbr (Rankin Fm). Max. thickness: 1268m (calc)||||||14-OCT-08
74201|Jimberoo Formation|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Thin to medium bedded, coarse- to medium-grained red and white sandstone, minor red siltstone and grit beds.||||||
74201|Jimberoo Formation|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.||Overlies Melbergen Sandstone. Is overlain by Mailman Gap Member (Rankin Formation).|Thin- to medium-bedded, coarse- to medium-grained red and white sandstone, minor red siltstone and grit beds.|
74201|Jimberoo Formation|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|||Thin- to medium-bedded, coarse- to medium-grained red and white sandstone, minor red siltstone and grit beds.|
74201|Jimberoo Formation|71889|5|Briefly described|p48, p56|||Rankin Springs area. Misspelt as the Jinberoo Formation on p56.||Cocoparra Group||Equivalent to the Cocoparra Group, Upper.|Cross bedded and cross-laminated sandstone, pebbly sandstone and siltstone.|
74201|Jimberoo Formation|73457|5|Briefly described|p7|||||Mulga Downs Group|||Polymictic conglomerate.|
27440|Jindalee Group|22434|6|Mentioned|11|||Geol  province Lachlan Fold Belt||||||
27440|Jindalee Group|22638|4|Described|p13|Early Ordovician||?Cambro- Early Ordovician. Some units previously mapped as Jindalee Group now Yandilla Volcanics.||||||22-APR-09
27440|Jindalee Group|22687|5|Briefly described|110|Ordovician|Cambrian|||||||
27440|Jindalee Group|22768|6|Mentioned|p184|||||||||
27440|Jindalee Group|22857|5|Briefly described|p76, p91 Fig. 14.7B, p183|Ordovician|Cambrian|Disrupted sequence of mafic and ultramafic rocks, including serpentinites. May be Cambro-Ordovician in age? Part of the Girilambone Slope and Basin. See also p406 App. 1 Tb. A1.4 and p418 App. 1 Tb. A1.5||||||
27440|Jindalee Group|22858|6|Mentioned|p78,Fig14.7bp90-1|||||||||
27440|Jindalee Group|22933|6|Mentioned|p24|||||||||
27440|Jindalee Group|23087|5|Briefly described|p655 (Fig 1)|Ordovician|Cambrian|||||||
27440|Jindalee Group|23245|4|Described|p103,123,125,133|Ordovician|Cambrian|||||||
27440|Jindalee Group|23366|5|Briefly described|p13 fig.8|Ordovician|Cambrian|||||||
27440|Jindalee Group|24007|6|Mentioned|p325 Fig.2|||||||||
27440|Jindalee Group|24215|4|Described|p801|Ordovician|Ordovician|Geological Province:  Lachlan Fold Belt||||||
27440|Jindalee Group|24233|5|Briefly described|p253 Fig.1, p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
27440|Jindalee Group|24417|3|Fully described|p7|Ordovician|Ordovician|Includes Brangan Volcanics, Hoskins Chert and Wambidgee Serpentinite.||||||
27440|Jindalee Group|24600|5|Briefly described|p481|Ordovician|Ordovician|In the Molong volcanic province of the Lachlan Fold Belt.||||||
27440|Jindalee Group|37529|5|Briefly described|p4|||||||||
27440|Jindalee Group|40762|6|Mentioned|p272|||||||||
27440|Jindalee Group|42045|5|Briefly described|p197|||||||||
27440|Jindalee Group|42145|4|Described|Table 1 P624|||||||||
27440|Jindalee Group|42313|3|Fully described|p22|Early Ordovician|Cambrian|||||||
27440|Jindalee Group|42314|5|Briefly described|Map|Early Ordovician|Cambrian|||||||
27440|Jindalee Group|42828|5|Briefly described|Table 1 P129|Early Ordovician|Cambrian|||||||
27440|Jindalee Group|44093|5|Briefly described|p93|||Contains the Wambidgee Serpentinite. See also p116 footnote and pp181-184 Appendix 1. Geological Province: Lachlan Fold Belt.||||||30-MAR-05
27440|Jindalee Group|44192|5|Briefly described|Map Legend|Early Ordovician|Cambrian|||||||
27440|Jindalee Group|46522|6|Mentioned|p52|||||||||
27440|Jindalee Group|46524|6|Mentioned|p118|||||||||
27440|Jindalee Group|50191|6|Mentioned|p4, 19|Silurian|Ordovician|Ultramafic rocks.||||||02-AUG-04
27440|Jindalee Group|50628|5|Briefly described|Map Legend|Cambrian|Cambrian|Includes: Wambidgee Serpentinite.||||||
27440|Jindalee Group|60008|5|Briefly described|Map Legend|Ordovician|Cambrian|Serpentinite.||||||
27440|Jindalee Group|60009|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Includes: Brangan Volcanics, Hoskins Chert, Wambidgee Serpentinite.||||||13-JUL-04
27440|Jindalee Group|60280|5|Briefly described|p1. p3 Fig. 1|||||||||
27440|Jindalee Group|63278|6|Mentioned|p145 Fig. 1|Ordovician|Ordovician|||||||07-FEB-11
27440|Jindalee Group|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
27440|Jindalee Group|63289|6|Mentioned|p367, p373 Fig. 7|Late Ordovician|Middle Ordovician|||||||07-FEB-11
27440|Jindalee Group|63290|6|Mentioned|p405, p407|Gisbornian|Darriwilian|Consists of volcanic-chert rocks, MORB-like basalts. Cherts have been dated to Da3-Gi1 (Lyons and Percival 2002).||||||
27440|Jindalee Group|64963|5|Briefly described|p189|||Basement rocks in the Tumut Basin. Include rocks associated with cherts of Darriwilian-Gisbornian age.||||||22-APR-09
27440|Jindalee Group|65890|6|Mentioned|p157 Fig.2|Cambrian|Cambrian|||||||
27440|Jindalee Group|67322|4|Described|p20|Pridoli||Basden (1982, 1990); Warren et al. (1995). Extends from Tumut area north to Narromine. Late Middle to Late Ordovician age based on the discovery of conodonts from Hoskins Chert blocks within the Jindalee Group. All constituents are interpreted as blocks redeposited with Wenlock-Ludlow limestone and rare dacite clasts, and enclosed by a matrix no older than Ludlow-Pridoli!|||Brangan Volcanics, Hoskins Chert, Brungle Creek Metabasalt, Wermatong Metabasalt, Valley View Metabasalt Igneous Complex, Bullawyarra Schist, Wambidgee Serpentinite, Gundagai Serpentinite||A discontinuous belt of fragmented ophiolitic sequence of now-serpentinized harzburgites and other ultramafic rocks, gabbros, pillow basalts, and bedded and interpillow cherts, and jaspers within a younger sedimentary matrix.|22-FEB-18
27440|Jindalee Group|67847|6|Mentioned|p21-p22, p25, p59|Middle Ordovician|Middle Ordovician|Hosts the Mooney Mooney VHMS deposit. Has a Pb model age of ~355 Ma.  |||||Ophiolites.|
27440|Jindalee Group|68466|5|Briefly described|p66, 68|||Extends from Tumut area N to Narromine. A fragmented ophiolite sequence.|||Brangan Volcanics, Hoskins Chert.||Serpentinised harzburgites and other ultramafic rocks, gabbros, basalts, bedded and inter-pillow cherts, and jaspers within a sedimentary matrix (of probable Silurian age).|
27440|Jindalee Group|69043|4|Described|p2-3, p57-58, p61, p63, p69|Late Ordovician|Late Ordovician|Tumut Trough. Exposed in a N-S belt between Tumut and Narromine. Has conodonts of Middle to Late Ordovician age. Thought to have been incorporated in a Late Silurian melange.|||Bullawyarra Schist.|Is intruded by Blacks Flat Diorite.|A package of metamorphosed mafic and ultramafic rocks, serpentinites, and marine sedimentary rocks (jasper and chert).|
27440|Jindalee Group|69668|5|Briefly described|p932|Silurian|Silurian|Tumut-Cootamundra region.|||Includes Brangan Volcanics and Hoskins Chert.||Fragmented ophiolite sequence of now-serpentinised harzburgites and other ultramafic rocks, gabbros, pillow basalts and bedded and inter-pillow cherts, and jasper.|
27440|Jindalee Group|70684|5|Briefly described|p3, p7 Fig.1, p9 Fig.4(h), p14|Early Silurian|Early Silurian||||||Imbricated? local mafic rocks and cherts: an inferred ophiolitic package.|
27440|Jindalee Group|71708|6|Mentioned|p335|Ordovician|Ordovician||||||Ordovician basement|
27440|Jindalee Group|72495|6|Mentioned|p228, p233|Ordovician|Ordovician||||Includes the Brangan Volcanics.|Faulted against the Young Granodiorite.|Tholeiitic volcanics.|
27440|Jindalee Group|73215|6|Mentioned|p993|Ordovician|Ordovician|||||||
27440|Jindalee Group|73483|5|Briefly described|p407-409|Ordovician|Cambrian|Poorly defined, inferred to include the Wambidgee, Gundagai and unnamed serpentinites. Inferred Cambrian-Ordovician age based in part on Scheibner and Pearce (1978). Late Middle to early Late Ordovician age previously reported by Lyons and Percival (2002) from conodonts in chert.|||Gundagai Serpentinite, Wambidgee Serpentinite|Faulted against Blowering Formation|Includes serpentinites, basalts, gabbros, quartzites, mica schists, cherts and rare limestones. Metabasalts, metagabbros, metasedimentary rocks.|
31489|Jinden Suite|22815|6|Mentioned|p72|||||||||
31489|Jinden Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Candelo Supersuite.  Contains the Jinden Granite (informal name).||||||09-FEB-05
31489|Jinden Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
31489|Jinden Suite|44093|5|Briefly described|p222 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
31489|Jinden Suite|71700|6|Mentioned|CD||||||Includes the Jinden Adamellite.|||
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.|||
29577|Jingerangle Formation|22638|4|Described|p19||Late Ordovician|||||||
29577|Jingerangle Formation|22857|4|Described|p418 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Thinly bedded siltstone and mudstone, often silicified, minor arenite and claystone; contains graptolites. Geological Province: Springdale Block.||||||
29577|Jingerangle Formation|23737|6|Mentioned|p87|||||||||
29577|Jingerangle Formation|24417|3|Fully described|p33|Late Ordovician|Late Ordovician|||||||
29577|Jingerangle Formation|44192|5|Briefly described|Map Legend|Llandoverian|Eastonian|||||||
29577|Jingerangle Formation|60008|5|Briefly described|Map Legend|Silurian|Ordovician|Sediments and/or volcanics.||||||
29577|Jingerangle Formation|60009|5|Briefly described|Map Legend|Bolindian|Eastonian|||||||13-JUL-04
29577|Jingerangle Formation|60548|5|Briefly described|map legend|Ordovician|Ordovician|Interbedded siltstone and mudstone, often silicified minor sandstone, claystone.||||||
29577|Jingerangle Formation|61893|5|Briefly described|p235, p237, p243-244, p247-251, p254|Late Ordovician|Late Ordovician|Warren et al. (1995), Percival and Lyons (2000). Caragabal-Quandialla district. May be as young as Bolindian 2 (graptolites listed). Significant for containing the youngest, most diverse, Late Ordovician shelly macrofauna in central NSW.|||||Lower part consists of a succession of thinly-bedded siltstones and mudstones weathered to pink and white clays and orange-brown ochres. Higher beds have coarser silts to fine sands, partly silicified.|22-MAY-17
29577|Jingerangle Formation|63278|5|Briefly described|p145 Fig. 1|Bolindian|Bolindian|Of the Currumburrama Igneous Complex. Age from graptolite, nautiloid and sponge deep-water assemblage. Geological Province: Junee-Narromine Volcanic Belt, LFB. Consists of fine-grained spiculitic rocks.||||||07-FEB-11
29577|Jingerangle Formation|63293|6|Mentioned|p468 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
29577|Jingerangle Formation|67322|4|Described|p22-23; Fig.5|Hirnantian|Katian|Macquarie Arc. Described by Warren et al. (1995) and Percival and Lyons (in Lyons et al., 2000). Contains graptolites of probable Bolindian age. Occurs in the Junee-Narromine region near Quandialla.||Of the Cabonne Group.||Overlies Wombin Volcanics.|Predominantly a spiculitic facies of deep-water origin containing sponges, a diverse nautiloid fauna and graptolites.|22-FEB-18
29577|Jingerangle Formation|67847|5|Briefly described|p22|Early Silurian||Contains late Ordovician graptolite fossils. ||||Equivalent to the Bribbaree, Bronxhome and Trigalong Formations.||
29577|Jingerangle Formation|70684|6|Mentioned|p3|||Junee-Narromine Volcanic Belt.||||||
29577|Jingerangle Formation|70754|6|Mentioned|p451|||Forbes area. Graptolites and one lingulate brachiopod species occur in siltstone which was previously assigned to the Cotton Formation.||||||
29577|Jingerangle Formation|72082|5|Briefly described|p22|Late Ordovician|Late Ordovician|East of Barmedman; in the Cootamundra and Forbes 1:250K sheet areas. Similar to the Trigalong (and other) Formations.||||||
29577|Jingerangle Formation|72495|6|Mentioned|p225|Late Ordovician|Late Ordovician|||Included in Currumburrama Igneous Complex here.||||26-MAR-20
29577|Jingerangle Formation|73492|6|Mentioned|p693|Late Ordovician|Late Ordovician|||||||
78646|Jinglemoney Conglomerate|69159|5|Briefly described|Map legend|Lochkovian|Lochkovian|||Unit in Bindook Group.||Is overlain by Long Flat Volcanics.|Grey to brown, medium-bedded, poorly-sorted, peble to cobble conglomerate, interbedded with grey, medium-bedded, fine- to medium-grained sandstone. Clasts include quartz-rich sandstone and siltstone, mudstone, chert, quartz, rhyolitic ignimbrite.|02-SEP-15
78646|Jinglemoney Conglomerate|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Bindook Group.||Is overlain by Long Flat Volcanics.|Grey to brown, medium-bedded, poorly-sorted, pebble-cobble conglomerate interbedded with grey, medium-bedded, fine- to medium-grained sandstone; clasts of quartz-rich sandstone and siltstone, mudstone, chert, quartz grains, rhyolitic ignimbrite.|
78646|Jinglemoney Conglomerate|71700|3|Fully described|vi, p7, p23-p25, p27, p36-p37, CD|Early Devonian|Early Devonian|Named for the parish of Jinglemoney where it outcrops. A type locality is designated as outcrop along Bombay Creek near GR 738479 6074549. Distribution, geomorphic expression, outcrop,  depositional environment, structure, metamorphism and distinguishing features are discussed. This unit is estimated to be less than 200m thick at the type locality.This unit is sourced from unconformably underlying basement material and contemporaneous felsic volcanic material deposited by sheet wash fans or small scale fluvial channels. Interpreted to also be equivalent to the Larbert Conglomerate, Bullamalita Conglomerate and Sharpeningstone Conglomerate. Early Devonian age is derived from unit relationships.||Bindook Group||Unconformably overlies the Abercrombie Formation. Overlain by the Tally Ho Ignimbrite Member and the Toggannogra Rhyolite Member. Equivalent to the Brooklyn Conglomerate Member.|Medium-bedded, pebble to cobble conglomerate interbedded with normally graded and cross-bedded, medium-grained sandstone and pebbly sandstone.|
31530|Jingo Creek Suite|22815|6|Mentioned|p81|||||||||
31530|Jingo Creek Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31530|Jingo Creek Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
40791|Jo Doth Tuff Member|22857|5|Briefly described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Leloma Formation (Craven Subgroup, Gloucester Coal Measures). White to cream claystone. Max. thickness: 15m. Geological Province: Sydney Basin.||||||
40791|Jo Doth Tuff Member|44244|5|Briefly described|p188|Permian|Permian|Of the Leloma Formation.  Max. thickness: 15m.  Type section in text.  Geological Province: Myall Block.||||||
40791|Jo Doth Tuff Member|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Leloma Formation (Craven Subgroup, Gloucester Coal Measures).  Thick white claystone and minor sandstone sequence.  Geological Province: Western Myall Block.||||||
34262|Joaramin Ignimbrite|22678|4|Described|Fig1p712,722,725|||Of the Bindook Volcanic Complex. Max thickness: > 140 m (observed)||||||17-JAN-06
34262|Joaramin Ignimbrite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Of the Bindook Volcanic Complex.  Bluish grey, welded, dacitic ignimbrite containing fractured phenocrysts of plagioclase, quartz, hornblende, enstatite, with minor biotite set in a recrystallised quartzo-feldspathic groundmass.||||||12-MAY-04
34262|Joaramin Ignimbrite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Bindook Gp. Pale pink to green-grey, densely welded, crystal-rich, rhyolitic ignimbrite containing whole + fractured phenocrysts of plagioclase, quartz, orthoclase, minor biotite + trace hornblende set in fine-gr. recrystallised qtz-feldspathic matrix.||||||17-JUN-08
34262|Joaramin Ignimbrite|68592|2|Defined|p847, p1069-70, p1074-6, p1134-40, p1826|Pragian|Pragian|See also p218, p226-9, p236, p241, p269, p843. Originally these rocks were included in undifferentiated Bindook Porphyry (McElroy and Relph, 1961). Later included in the informal Brayton volcanics by O'Reilly (1972). First distinguished by Simpson (1990), and formally defined by Simpson, Carr and Jones (1997). Named after Joaramin Creek. Type section described. At least 140m thick. Encloses three small pods of Marulan Granite. Geochemistry detailed: I-type. Geophysical properties described. Intruded by Lockyersleigh Granite. Quarried for aggregate at Johnniefelds quarry, N of Marulan; with another approved quarry at Lynwood. Source of pottery and brick clay at Shelleys Flat. Associated with mineralisation at Carrington Fe mine.||Unit in Bindook Group.||Disconformably overlies Kerrawarra Dacite Member. Is overlain unconformably by Barrallier Ignimbrite and Strathaird Formation. Is faulted against Longreach Volcanics and Covan Creek Formation.|Rhyolitic, densely-welded ignimbrite, mostly coarse-grained and crystal-rich; minor volcanic sandstone, fine-grained and crystal-poor passing up to coarse-grained and bedded; discontinuous dacitic ignimbrite, a pod of porphyritic dacite/granodiorite.|
34262|Joaramin Ignimbrite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dkj. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Bindook Group||Overlies Kerrwarra Dacite Member (of Tangerang Formation).|Densely welded, crystal rich rhyolitic ignimbrite; whole and fractured phenocrysts are set in a fine-grained recrystallised matrix, very minor volcanic sandstone and porphyritic dacitic intrusions.|
34262|Joaramin Ignimbrite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Bindook Group|||Densely welded, crystal rich rhyolitic ignimbrite; whole and fractured phenocrysts are set in a fine-grained recrystallised matrix, very minor volcanic sandstone and porphyritic dacitic intrusions.|
34262|Joaramin Ignimbrite|70661|4|Described|p52 fig 5, p53, p69-p71|Pragian|Pragian|Named after Joaramin Creek property. Originally included in the undifferentiated Bindook Porphyry. Inferred extent of 11km^2, although full extent is obscured by the Tallong Conglomerate. Blocky, jointed outcrop forming a gently undulating landscape. Type section mentioned. Minimum thickness of 140m inferred. Subaerial depositional environment. Structure, metamorphism, geochemistry and geophysical characteristics described. Age derived from conodont and trilobite fossil assemblage.||Bindook Group||Overlies Tangerang Formation,Unconformably overlain by Tallong Conglomerate,overlain by Barralier Ignimbrite, intruded by Marulan Granite|Rhyolitic, densely welded ignimbrite characterised by the presence of prominent quartz and pink feldspars in a pale brown to grey matrix. Coarse grained and crystal rich, with some less crystal rich equivalents elsewhere.|
34262|Joaramin Ignimbrite|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Bindook Group.|||Rhyolitic, densely welded ignimbrite with prominent quartz and pink or pale green feldspar phenocrysts, in a pale brown to grey matrix.|
34262|Joaramin Ignimbrite|71656|6|Mentioned|p13 Fig.2|Emsian|Emsian|Shown only in correlation chart (Fig.2), as Emsian, but correlated with Murruin Formation which is interpreted to be Lochkovian to Emsian.||Bindook Group||Overlain by Barrallier Ignimbrite. Shown as lateral equivalent with Murruin Formation.||
76757|Johnniefelds granodiorite|70661|4|Described|p86-87, p78, p79 fig 6|Lochkovian|Early Devonian|Informal name, misspelt as Jonniefields granodiorite on p79 fig 6. Named after the Johnniefelds property. Originally included as part of the undifferentiated Marulan Batholith. It crops out poorly in a cleared area with low relief. No type locality given. Age: older than Pleasant Hill Granite, which contact metamorphoses it.||Arthursleigh Suite|||Bimodal, holocrystalline, medium to coarse grained granodiorite.|
76757|Johnniefelds granodiorite|71303|5|Briefly described|map legend|Pragian|Pragian|Shown as Jonniefelds Granodiorite in time-space plot.||Of Arthursleigh Suite.|||Bimodal holocrystalline, medium- to coarse-grained  biotite-hornblende granodiorite. Characterised by a contact metamorphic microstructure and a stong mineral lineation locally. Fine-grained enclaves common.|
26269|Jolly Nose Conglomerate|22616|6|Mentioned|Fig.1 p670|Triassic|Triassic|||||||
26269|Jolly Nose Conglomerate|22736|6|Mentioned|p611 Fig2||Triassic|||||||
26269|Jolly Nose Conglomerate|22857|5|Briefly described|p538 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Camden Haven Group. Pebble to cobble conglomerate; crossbedded quartz sandstone. Max. thickness: 100m. Geological Province: Lorne Basin.||||||
26269|Jolly Nose Conglomerate|36826|2|Defined|p93|Early Triassic|Early Triassic|||||||
26269|Jolly Nose Conglomerate|41348|5|Briefly described|Map legend|Triassic|Triassic|Of the Camden Haven Group.||||||16-DEC-04
26269|Jolly Nose Conglomerate|44093|5|Briefly described|p67 Fig. 6.6|Triassic|Triassic|Geological Province: Lorne Basin.||||||
26269|Jolly Nose Conglomerate|62058|5|Briefly described|map sheet|Early Triassic|Early Triassic|||Unit in Camden Haven Group.|||Lithic conglomerate.|
26269|Jolly Nose Conglomerate|63763|5|Briefly described|p4-5 Fig. 1|Early Triassic|Eary Triassic|Of Camden Haven Group. Lithic conglomerate.||||||03-FEB-09
26269|Jolly Nose Conglomerate|66090|2|Defined|p2, p4, pp8-10, p30.|Early Triassic|Late Permian|Named and defined by Leitch and Bocking (1980). Definition info provided here, where the unit is excluded from the Camden Haven Group, without explanation. Basal formation in northeastern part of Lorne Basin. Thickness max 140 m, and 100 m at type section. Composed of pebbles and cobbles probably derived from basement formations. Clast lithology is markedly different from lithologies of other conglomerates higher up in the sequence: identified by low content of jasper and quartz clasts, and >5 cobbles in 0.25 m2 area. Poor outcrops, usually weathered. Filled in a graben in NE of the Basin. Age: uncertain. Assumed to unconformably overlie Middle Ordovician to Late Carboniferous Watonga Formation; and is overlain by Laurieton Conglomerate (in part) containing Early Triassic macroflora.||||Overlies unconformably the Watonga Formation (Palaeozoic basement rocks). Is overlain by Laurieton Conglomerate or conformably by Coopernook Conglomerate Member.|Poorly outcropping, moderately to highly weathered, cobble-rich conglomerate. Clasts lithology dominated by ~80% lithic and quartzofeldspathic sandstone; other portion includes granitoids, quartzite and acid volcanic rocks.|19-OCT-15
26269|Jolly Nose Conglomerate|73197|6|Mentioned|p482|Late Triassic|Early Triassic|Lorne Basin. Lowermost horizon in the basin, possibly early Triassic (Pratt, 2010), zircons age peaks of 300 Ma and 220 Ma in volcanic clasts are consistent with latter Triassic extension (Richardson, 2013).|||||Conglomerate with sedimentary and volcanic cobble-sized clasts.|
69891|Joppa Siltstone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of De Drack Formation (Mount Fairy Group). Fawn, buff and khaki laminated siltstone with starved ripples of fine-grained sandstone in places. Rare thinly-bedded fine- to medium-grained lithic-quartz sandstone.||||||
69891|Joppa Siltstone Member|68592|2|Defined|p730 Fig.132, p760, p779, p785, p792-6|Early Silurian|Early Silurian|See also p106, p726, p728, p1672. New name. Crops out poorly, though wide extent in shallow subcrop. Type locality described. Folded and faulted. Well-developed slaty cleavage is affected by regular, steeply west-dipping, kink bands in footwall of west-dipping Yarra Fault. Thickness: 150-~700 m; unknown at type locality as fault-bounded and base not exposed. Stratigraphic correlation: presence of Bohemograptus sp. in siltstone suggests that it is partially equivalent to Kerrawary Siltstone. Quiet depositional conditions with little pyroclastic input. Is intruded by Bishopthorpe Dolerite and Forest Lodge Quartz Monzodiorite; is faulted against Warbisco Shale (Yarra Fault).||Top unit in De Drack Formation.||Overlies Kingsdale Limestone Member; conformably overlies and interfingers with Sooley Volcanic Member. Is conformably overlain by Covan Creek Formation.|Homogeneous sequence of laminated to medium-bedded fawn, cream, buff and khaki siltstone, mudstone and fine-grained quartzose sandstone with starved ripples in places; contains minimal volcaniclastic detritus; sometimes weathered to purplish colours.|
69891|Joppa Siltstone Member|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sfdj. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||De Drack Formation||Is overlain by Covan Creek Formation. Overlies Kingsdale Limestone Member. Overlies, and interfingers with, Sooley Volcanic Member. Interfingers with Woodlawn Volcanics.|Fawn, cream, buff and khaki laminated to medium bedded siltstone, mudstone and fine grained quartzose sandstone with starved ripples.|
69891|Joppa Siltstone Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||De Drack Formation|||Fawn, cream, buff and khaki laminated to medium bedded siltstone, mudstone and fine grained quartzose sandstone with starved ripples.|
69891|Joppa Siltstone Member|71069|5|Briefly described|p142, p144, p146, p147, p152|||Displays kink bands orientated at a high angle to the slat cleavage of silstone. Contains graptolite fossils. Has been quarried for limestone. ||De Drack Formation||Interfingers with the Woodlawn Volcanics.|Siltstone.|
69891|Joppa Siltstone Member|71656|5|Briefly described|p13 Fig.2, p29|Ludlow|Ludlow|The graptolite Bohemograptus bohemicus was found in an outcrop of the Joppa Siltstone Member behind the pumphouse at the Goulburn Waterworks Museum. This indicates a late Silurian age (early to mid-Ludlovian).||De Drack Formation, Mount Fairy Group||Partially overlies Kingsdale Limestone Member ?|Includes fossiliferous limestone.|
82509|Juhle Mountain Granodiorite|71628|4|Described|p17: 2, 75-78, 81|||New name (this study) after unpublished work by Knutson (1975). Forms a ~6 x 5 km intrusion, some 20 km SW of Laurieton. Named after a local mountain. Fresh outcrop is limited. Geochemistry described.|c.212 Ma.|The Brothers Suite.||Intrudes Pappinbarra Formation, Beechwood beds and Camden Haven Group.|Amphibole-biotite granodiorite to monzogranite with abundant granophyric variants. A-type.|
33794|Julong Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Massive to strongly foliated porphyritic muscovite-biotite granite.||||||
33794|Julong Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Burrawinda Suite. Massive to strongly foliated porphyritic muscovite-biotite granite. High K radioelement response.||||||
33794|Julong Granite|68592|2|Defined|p1268-9, p1274, p1284, p1287-9|Late Silurian|Late Silurian|See also p1255 Fig.220. New name, after Julong Creek within Parish Julong. This body was previously included in undifferentiated Wyangala Batholith (Brunker and Offenberg, 1970); later included in Wheeo Granite (Chappell et al., 1991). Here assigned to the Hovells Suite on geochemical grounds. Type locality described. Geochemistry detailed; geophysical properties described. Not isotopically dated.||Unit in Hovells Suite.||Intrudes Mulgowrie Granodiorite.|Grey, medium- to coarse-grained, massive to strongly foliated, porphyritic to megacrystic, cordierite-muscovite-biotite granite. S-type.|
33794|Julong Granite|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Soj. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Medium to coarse grained, massive-strongly foliated, porphyritic to megacrystic, cordierite-muscovite-biotite granite; high K response.|
33794|Julong Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Hovells Suite|||Medium to coarse grained, massive-strongly foliated, porphyritic to megacrystic, cordierite-muscovite-biotite granite; high K response.|
22044|Jumping Creek Granodiorite|42726|5|Briefly described|Map Legend|Early Devonian||||||||
29578|Junawarra Volcanics|22638|4|Described|p26|Early Silurian|Late Ordovician|||||||
29578|Junawarra Volcanics|22685|5|Briefly described|Fig1p729|Late Ordovician|Late Ordovician|Andesite and volcaniclastic rocks.||||||17-JAN-06
29578|Junawarra Volcanics|22857|4|Described|p418 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|Well-bedded andesitic tuffs and flow-banded intermediate lavas.||||||
29578|Junawarra Volcanics|44192|5|Briefly described|Map Legend||Bolindian|||||||
29578|Junawarra Volcanics|44936|5|Briefly described|Map Legend||Ordovician|||||||
29578|Junawarra Volcanics|50191|5|Briefly described|p5, 11, fig. 4|Silurian|Ordovician|||||||
29578|Junawarra Volcanics|63278|6|Mentioned|p145 Fig. 1, p149|||||||||07-FEB-11
29578|Junawarra Volcanics|67322|5|Briefly described|p23|Ordovician|Ordovician|Defined and Ordovician age assigned by Warren et al. (1995). Its geochemistry excludes this unit from the Macquarie Arc. Age is conjectural.|||||Tholeiitic geochemistry.|22-FEB-18
29578|Junawarra Volcanics|68822|6|Mentioned|p335|||||||||
29578|Junawarra Volcanics|70684|6|Mentioned|p3, p54 Fig.27|||||||||
29578|Junawarra Volcanics|72082|6|Mentioned|p4, p32-33|Early Silurian|Late Ordovician|Warren et al. (1995). Wyborn (1996) considered this unit to be geochemically distinct from rocks in the Dobroyde area and named the latter the informal Dobroyde volcanics.||||||08-JAN-20
29578|Junawarra Volcanics|72084|5|Briefly described|p2, p12, p15, p25, p41, p59|Early Silurian|Late Ordovician|Warren et al. (1996); they assigned a Late Silurian to Early Devonian age to the unit. Intermediate volcanic rocks. Crops out poorly on low hills. No iosotopic ages at time of publication. Outcrops on the Cootamundra 1:250 000 sheet in the far east area of Junee. Detailed lithological descriptions are provided for numerous outcrops.||||Is intruded by Wantabadgery Granite. Correlated with Gidginbung Volcanics.|Poorly-sorted, andesitic, pebble- to cobble-sized, matrix-supported breccia; dark greenish-grey, fine- to very coarse-grained volcaniclastic sandstone; jasper.|29-AUG-19
29578|Junawarra Volcanics|72495|5|Briefly described|p218, p227, p234|||Originally of Warrant et al, 1995 and initially included the Dobroyde Volcanics before being removed by Wyborn (1996) on the basis of different geochemical affinities. Locally outcrop along the western side of the Gilmore Fault Zone and Tullamore Fault.|||||Tholeiitic MORB-like rocks.|
29578|Junawarra Volcanics|72528|5|Briefly described|p1, p31-32, p36, p108, p123-5.|Wenlock|Wenlock|An outcrop is located approximately 12 km to the SE of Dobroyde. Part of the Macquarie Igneous Province. Compared with an unnamed andesite at Dobroyde, dated herein at 431.1+/-1.8 Ma. Similar ages but geochemically distinct units.|c. 432 Ma|||||
22048|Junee Reefs Granite|22638|3|Fully described|p53|||Previously "Ardlethan Granite", Wantabadgery Granite.||||||
22048|Junee Reefs Granite|22685|5|Briefly described|Fig1p729||Silurian|||||||
22048|Junee Reefs Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
22048|Junee Reefs Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
22048|Junee Reefs Granite|50191|6|Mentioned|p17|Silurian|Silurian|||||||
22048|Junee Reefs Granite|72082|5|Briefly described|p4, p33|Early Silurian|Early Silurian|Lithologically similar to the Wantabadgery Granite according to descriptions in Warren et al (1995).|431.2 +/- 2.4 Ma (SHRIMP: Geoscience Australia).|||Intrudes the Wagga Group. Abuts the eastern margin of the Wantabadgery Granite.|Grey, equigranular, porphyritic, quartz-feldspar-biotite-muscovite granite; tourmaline-bearing, locally pegmatitic, xenolith-rich.|08-JAN-20
29570|Kabadah Formation|22857|4|Described|p422 App. 1, Tb. A1.5|Early Silurian|Late Ordovician|Of the Cabonne Group. Mafic volcaniclastic arenite, siltstone, banded cherty siltstone, minor limestone; with graptolites, conodonts. Max. thickness: 1400m. Geological Province: Molong Volcanic Arc. ||||||
29570|Kabadah Formation|23043|5|Briefly described|Map Legend|Llandovery|Bolindian|of Cabonne Group.||||||
29570|Kabadah Formation|23170|2|Defined|p55|Llandovery|Late Ordovician|Cabonne Group.||||||
29570|Kabadah Formation|23213|5|Briefly described|p20, Fig.1|Early Silurian|Late Ordovician|||||||
29570|Kabadah Formation|23214|3|Fully described|p73|Early Silurian|Late Ordovician|Of Cabonne Group. Intruded by Gumble Granite. Primarily consists of interbedded grey to black tuffaceous sandstone and shale with minor chert bands. Max. thickness 800m||||||03-APR-13
29570|Kabadah Formation|24015|5|Briefly described|p13|Early Silurian|Late Ordovician|Arc volcaniclastic rocks.||||||
29570|Kabadah Formation|43494|3|Fully described|p16|Silurian|Ordovician|Of the Cabonne Group. Incl: former units: Kabadah Beds and Loombah, Bournewood and Yullundry  Formations, as well as Buckinbah Volcanics and Myrangle Formation. Mafic volcaniclastic sst, sltst, banded cherty slts, minor allochth. limestone.||||||01-OCT-09
29570|Kabadah Formation|43640|5|Briefly described|Map Legend||Ordovician|||||||
29570|Kabadah Formation|43782|5|Briefly described|Map Legend|Llandovery|Bolindian|of Cabonne Group.||||||
29570|Kabadah Formation|63277|5|Briefly described|p139||Early Silurian|Geol Prov: LFB. Comprises detrital fragments; mafic-intermediate volcanic rocks + ultramafic clasts, free crystals of pyroxene, chromite, volcanic quartz, garnet, clasts of welded S-type rhyolitic volcanic rock, + rare clasts of uplifted fold belt rock.||||||
29570|Kabadah Formation|63278|5|Briefly described|p152|Early Silurian|Late Ordovician|Geological Province: Molong Volcanic Belt, LFB. Age from Raymond et al. 1998; Morgan et al. 1999a. Calcareous sandstone contains fossil coral .||||||07-FEB-11
29570|Kabadah Formation|63283|6|Mentioned|p194 Fig. 2|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29570|Kabadah Formation|63288|3|Fully described|p353-354, p354 Fig. 1, p335-361|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt. Consists largely of volcaniclastic rocks, and has a high K-radiometric signiture. Deposited in a shallow water environmnet. See p353-359 for more information.||||||
29570|Kabadah Formation|63289|6|Mentioned|p374, p380|Landovery|Llandovery|Geological Province: Molong Volcanic Belt. Mixed quartz and volcanic detritus occurs. Contains Silurian fossils.||||||07-FEB-11
29570|Kabadah Formation|63290|5|Briefly described|p391, p393 Tb. 1, p404, p397 Fig. 3(b)|Landovery|Llandovery|Age: 443-428Ma. Lithologies; ultramafic, S-type igneous rocks, Ordovician volcanic rocks, Silurian volcanic rocks and Ordovician quartz-rich turbidites. Geological Province: Molong Volcanic Belt. ||||||
29570|Kabadah Formation|63293|6|Mentioned|p475, p468 Fig. 2|Llandovery|Llandovery|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29570|Kabadah Formation|66197|5|Briefly described|p632, p633 Fig.4c|Early Silurian|Early Silurian|Cowra Trough-Molong High. Shallow marine volcaniclastics that contain graptolites and corals. Underlies the Canowindra Volcanics.||||||14-MAR-12
29570|Kabadah Formation|67322|6|Mentioned|p25, p26|Early Silurian|Early Silurian|The Gunnars Dam beds of Percival and Glen (2007) are now regarded as blocks of Late Ordovician cherty spiculitic and graptolitic siltstone, emplaced into this Formation.||||||
29570|Kabadah Formation|67847|5|Briefly described|p4, p19-p20, p32|Late Silurian|Middle Silurian|Lachlan Orogen. Lithic fragments are correlated with the Cowra Granodiorite and the Canowindra Volcanics. Previous work on fossil assemblage indicated an early Silurian age and thus Bradley (in Pickett, 1982) included the Formation in the Cudal Group. Detailed discussion of previous age determinations of the unit is given on pages 32-33. |||||Mafic volcaniclastic rocks including quartz and lithic fragments.|
29570|Kabadah Formation|68003|5|Briefly described|p23, p24 Fig.3-e, p147. |Bolindian|Gisbornian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Cabonne Group.|||Mafic volcaniclastic sandstone, siltstone, banded cherty siltstone, minor limestone.|
29570|Kabadah Formation|70297|5|Briefly described|map legend|Early Silurian|Early Silurian||||||Mafic volcaniclastic sandstone, siltstone, shale, chert; minor limestone, conglomerate.|
29570|Kabadah Formation|70684|6|Mentioned|p9 Fig.4(g), p74|Early Silurian|Early Silurian|Cumnock-Yullundry district, Molong Volcanic Belt.||||||
29570|Kabadah Formation|73299|6|Mentioned|p1105|||Cowra Trough. [Map symbol suggests Ordovician-Silurian age]||||||
24324|Kadoona Dacite Member|22857|5|Briefly described|p480 App.1 Tb.A1.6|Silurian|Silurian|Of the Long Flat Volcanics. Porphyritic dacite, ignimbrite. Max. thickness: ~1000m.||||||10-MAR-06
24324|Kadoona Dacite Member|39028|6|Mentioned|Map legend|Pridolian|Pridolian|||||||
24324|Kadoona Dacite Member|40276|2|Defined|p6|Late Silurian|Late Silurian|||||||
24324|Kadoona Dacite Member|41133|4|Described|p1116|||||||||
24324|Kadoona Dacite Member|66300|5|Briefly described|p35, 41, 46.|Early Devonian|Early Devonian||413.4 +/- 2.6 Ma.|Said in this study to be a unit in Long Flat Volcanics.||Conformably overlain by Toggannoggra Rhyolite Member. Possibly laterally equivalent to Croppies Gunyah Rhyolite Member.||29-OCT-13
24324|Kadoona Dacite Member|69159|5|Briefly described|Map legend|Lochkovian|Lochkovian|||Unit in Long Flat Volcanics.||Overlies Larbert Conglomerate. Is overlain by Tooggannoggra Rhyolite Member and Croppies Gunyah Ignimbrite Member.|Green to grey, medium-grained, moderately fragmental and densely welded, crystal-rich dacitic ignimbrite; variable lithic clast content.|07-SEP-15
24324|Kadoona Dacite Member|69635|6|Mentioned|p18|||||Of Long Flat Volcanics.||||16-JUL-15
24324|Kadoona Dacite Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Long Flat Volcanics.|||Dark greenish-grey, fine- to medium-grained, densely-welded plagioclase-quartz-hornblende-pyroxene-phyric dacitic ignimbrite.|
24324|Kadoona Dacite Member|71700|3|Fully described|vi, p25-p26, p79, p110, CD|Early Devonian|Early Devonian|Name is derived from the homestead of Kadoona in ARALUEN100. A type locality is defined as outcrops at GR 739310 6037467 approximately 1.5 km northeast of the Kadoona homestead. Historically these rocks were included in the Long Flat Porphyries of Anderson (1893), then the Long Flat Volcanics. This unit was then included in the Bombay Volcanics before being formalised by Wyborn and Owen (1986) as a member of the Long Flat Volcanics. SHRIMP age is derived from Kemp, Hawkesworth and Paterson et al (2007). Age is confirmed by similar ages for other members of the Long Flat Volcanics.  Thickness is estimated at up to 1000m. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed.|414 +/- 5 Ma (SHRIMP U-Pb)|Long Flat Volcanics||Conformably overlies the Larbert Conglomerate. Conformably overlain by the Croppies Gunyah Rhyolite Member. Overlain by the Tally Ho Ignimbrite Member. Intruded by the Braidwood Granodiorite.|Greenish-grey, dacitic ignimbrite that is very poorly sorted and fragmented.|
24325|Kadungle Volcanics|22768|6|Mentioned|p178|||||||||
24325|Kadungle Volcanics|22831|2|Defined|p 59|Devonian|Lochkovian|Previously in the"Ootha Beds"||||||
24325|Kadungle Volcanics|22857|4|Described|p178, p448 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Trundle Group. Rhyolite lavas and ignimbrites, minor shale and arenite; contains brachiopods and corals. Max. thickness: 2000m. Geological Province: Bogan Gate Terrace.||||||
24325|Kadungle Volcanics|23053|6|Mentioned|p69||Early Devonian|||||||
24325|Kadungle Volcanics|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
24325|Kadungle Volcanics|24417|3|Fully described|p90|Early Devonian|Early Devonian|Of Trundle Group.  Originally included as part of the Byong Volcanics.  Includes the Bird Flat Volcanic Member.  Thickness range: 400-800m.||||||
24325|Kadungle Volcanics|36066|5|Briefly described|p10|||||||||
24325|Kadungle Volcanics|39660|6|Mentioned|p449|||||||||
24325|Kadungle Volcanics|40365|2|Defined|p326|Early Devonian|Early Devonian|||||||
24325|Kadungle Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
24325|Kadungle Volcanics|43441|5|Briefly described|20, 29|Early Devonian|Early Devonian|||||||08-JAN-10
24325|Kadungle Volcanics|44160|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||08-JAN-10
24325|Kadungle Volcanics|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Trundle Group.  Overlies: Pullabooka Formation.  Interfingers/bedded with: Carawandool Volcanics. Underlies: Hervey Group.||||||27-MAY-04
24325|Kadungle Volcanics|60009|5|Briefly described|Map Legend|Devonian|Devonian|Of the Trundle Group. Overlies: Coonardoo Sandstone.  Underlies: Bird Flat Volcanic Member, Beugamel Sandstone.||||||13-JUL-04
24325|Kadungle Volcanics|62569|5|Briefly described|p607 Fig. 2|Early Devonian|Early Devonian|Of Trundle Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
25098|Kahibah Formation|23055|6|Mentioned|Fig11p23|||||||||
25098|Kahibah Formation|29922|6|Mentioned|Appendix 4|||||||||
25098|Kahibah Formation|29926|6|Mentioned|Fig.3|||||||||
25098|Kahibah Formation|29942|4|Described|Fig.2|||||||||
25098|Kahibah Formation|34351|6|Mentioned|p344|||Fig.5.13||||||
25098|Kahibah Formation|39292|6|Mentioned|Fig. 6.2|||||||||
25098|Kahibah Formation|39308|6|Mentioned|Fig. 23.4|||||||||
25098|Kahibah Formation|41479|6|Mentioned|Fig.2|||||||||
25098|Kahibah Formation|43344|14|Not recorded|p85||Permian|||||||
25098|Kahibah Formation|43447|14|Not recorded|diag.p26|||Part of Cardiff Sub-Group||||||
25098|Kahibah Formation|43448|14|Not recorded|p224||Permian|On table only. Unit of Cardiff Subgroup (Newcastle Coal Measures)||||||
25098|Kahibah Formation|45090|6|Mentioned|p186|||Refers McKenzie (1962)||||||
25098|Kahibah Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Adamstown Subgroup|Included Hillsborough Tuff Member, Whitebridge Conglomerate Member.|||
77047|Kain Porphyry Member|66300|5|Briefly described|p36, pp41-45. |Early Devonian|Early Devonian|Supersedes the Kain Porphyry. Interpreted as a subvolcanic unit intruding the eruptive components of Long Flat Volcanics, and has the same age as them.|414.1 +/- 2.8 Ma.|Said in this study to be a unit in Long Flat Volcanics.|||Massive, medium-grained, crystal-rich porphyritic dacite.|
77047|Kain Porphyry Member|69159|5|Briefly described|Map legend|Lochkovian|Lochkovian|||Unit in Long Flat Volcanics.|||Green to grey, medium- to coarse-grained, crystal-rich, plagioclase-quartz-ferromagnesian-phyric coherent dacite.|07-SEP-15
77047|Kain Porphyry Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Long Flat Volcanics.|||Green to grey, medium- to coarse-grained, crystal-rich, plagioclase-quartz-ferromagnesian-phyric coherent dacite.|
77047|Kain Porphyry Member|71700|3|Fully described|vi, p25, p43, p79, CD|Early Devonian|Early Devonian|Named for the Kain homestead south of Jerrabattgulla Creek on the Captains Flat Road. The type locality for the Kain Porphyry Member is defined at GR 734946 6041479. Historically this unit was included in the Long Flat Porphyries (Anderson 1893), later renamed the Long Flat Volcanics (Best et al. 1964). White (1961) formalised Bombay Volcanics and this subdivision was also adopted by Felton and Huleatt (1975). Wyborn and Owen (1986) rejected the subdivision of the Bombay Volcanics and formalised the name Kain Porphyry as a member of the Long Flat Volcanics. SHRIMP age is derived from Bodorkos et al. 2010. Distribution, geomorphic expression, outcrop, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. Lithology is discussed in detail.|414.1 +/- 2.8 Ma (SHRIMP U-Pb)|Long Flat Volcanics||Intrudes the Tally Ho Ignimbrite Member, Croppies Gunyah Ignimbrite Member and the Toggannoggra Rhyolite Member.|Deep green, massive, medium to coarse grained, plagioclase and quartz-phyric coherent dacite.|
78580|Kaiwilta Member|67322|4|Described|p19; Fig.5|Floian|Floian|Defined by Trigg, in Burton et al.(in press). 45m thick. The Kaiwilta Member is enclosed within the turbidite sequence of the Narrama Formation at Dijou Mountain and Bald Hills. Age is determined from p20 Fig.5 (Strat. column). Occurs in the Sussex-Byrock region.||Of the Narrama Formation||Overlain by the Mount Dijou Volcanic Member.|Basaltic volcanics with a basal basaltic/basic volcanic horizon overlain by lithic quartz sandstone and minor siltstone. The top of the unit is marked by a 1-3m thick, laterally extensive horizon of thinly bedded chert.|22-FEB-18
78580|Kaiwilta Member|68466|6|Mentioned|p65|Early Ordovician|Early Ordovician|Hermidale Terrane.||Narrama Formation.||||
78580|Kaiwilta Member|69094|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Intercalated amygdaloidal basalt is mapped separately.||Unit in Narrama Formation.||Is overlain ?conformably by Mount Dijou Volcanic Member.|Medium- to coarse-grained, lithic, quartzose sandstone and minor quartzose siltstone, conodont-bearing chert, and intercalated amygdaloidal basalt.|
78580|Kaiwilta Member|69668|5|Briefly described|p929 Fig.2|Early Ordovician|Early Ordovician|Hermidale terrane, central NSW.||Unit in Narrama Formation.||Is overlain by Mount Dijou Volcanic Member.||
78580|Kaiwilta Member|70602|6|Mentioned|p67 Fig 3|Middle Ordovician|Early Ordovician|Age inferred.||Narrama Formation||||
78580|Kaiwilta Member|70828|5|Briefly described|p14|||Associated with quartz-magnetic rocks, and therefore characterised by complex magnetic patterns due to magnetic remanence of the basaltic and quartz-magnetic rocks (Dadd 2006, Trigg and Burton 2012 p31-39 in Burton, Trigg and Campbell 2012).||Unit of Narrama Formation.||Overlain by Mount Dijou Volcanic Member.||
78580|Kaiwilta Member|70941|2|Defined|pviii, p6, p8 fig 4|Chewtonian|Bendigonian|Named derived from Kaiwilta Parish. Previously a part of the undifferentiated Mount Dijou Volcanics. Distribution, distinguishing characteristics, structure, metamorphism, geochemistry , geomorphology and geophysical characteristics discussed.Conodont fossils present and the age is derived from these. Up to 45m thick.Type area mentioned and briefly described. Lithology in different areas discussed. Deposited in a deep water marine enviornment as an intra-plate oceanic seamount. Associated spatially with gold, minor sulfides also present. See also  p12, p16, p17, p21, p27-p31, p36, p37, p39-41, p111, p112, p123, p124 fig 54, p125, p134, p139, p140 fig 58, p141 ph78, p147.||Narrama Formation||Generally conformably overlain by Mount Dijou Volcanic Member (but faulted in places).Conformably overlies Narrama Formation|Intercalated basalt and amygdaloidal basalt, medium - coarse grained lithic quartz sandstone,minor siltstone and chert.|
78580|Kaiwilta Member|71360|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Mapped as the one unit with the Mount Dijou Volcanic Member and an un-named jasper unit, all of the Narrama Formation. Geophysical signature: irregular-shaped units of high magnetic intensity forming a curvilinear lenticular zone at surface (short wavelength), and a sub-parallel trend to the north at greater depth (longer wavelength).||Narrama Formation.|||Altered amygdaloidal basaltic pillow lavas and lavas, trachytic lavas, fragmental basaltic rocks, sandstone, siltstone, chert, magnetite-rich jasper.|
24328|Kalimna Limestone Member|23214|3|Fully described|p41|Eastonian|Eastonian|Of Fossil Hill Limestone. 9m thick at type section.  Overlying unit: Wyoming Limestone Member, underlying unit: Gleesons Limestone Member.||||||
24328|Kalimna Limestone Member|38219|2|Defined|p306|Late Ordovician|Late Ordovician|Part of Cliefden Caves Group. See also Fig.2.||||||
24328|Kalimna Limestone Member|41046|6|Mentioned|p143|||||||||
24328|Kalimna Limestone Member|42479|5|Briefly described|p108|||||||||
24328|Kalimna Limestone Member|42603|5|Briefly described|Fig.4 P57|||||||||
24328|Kalimna Limestone Member|70754|5|Briefly described|p449, p455|Late Ordovician|Late Ordovician|||Fossil Hill Limestone.|||Includes thin-bedded terrigenous-rich limestones.|
24328|Kalimna Limestone Member|73492|6|Mentioned|p706|||||Fossil Hill Limestone, lower part||||
25100|Kallinga Formation|40774|6|Mentioned|Fig.2|||||||||
77043|Kaloe Tonalite|69639|5|Briefly described|p1, p217, p223|Cisuralian|Cisuralian|New England Orogen.|291.9 +/- 2.0 Ma (Cawood et al, 2011)|Clarence River Supersuite||||
77043|Kaloe Tonalite|70876|5|Briefly described|p2, p77-p79|Permian|Permian|New England Orogen. An additional age of 293.1 +/- 1.8 Ma is derived from Ar-Ar hornblende completed by Bryant et al, 1997.|291.2 +/- 2 Ma (SHRIMP U-Pb)|Clarence River Supersuite||||
77043|Kaloe Tonalite|71628|4|Described|p1: 6; p5: 1; p10: 7; p18: 1-2, 13-17|||Originally Hanging Rock Adamellite; subsequently Kaloe Granodiorite and Kaloe Granite. Named after the parish, trig or mount. Forms a narrow, curvilinear body stretching ~32 km from N of Jackadgery to just N of Coombadjha. Has poor relief in generally low country. Lithology, mineralogy and geochemistry detailed. This age determination was the first evidence that I-type granites in the New England Orogen were emplaced contemporaneously with S-type granites of the Bundarra and Hillgrove Supersuites. Is associated spatially (not definitively) with a series of Cu deposits.|291.9 +/- 2 Ma (SHRIMP: Cawood et al., 2011).|Kaloe Suite.||Intrudes Silverwood Group.|Medium-grained, equigranular to weakly porphyritic, biotite-hornblende-(pyroxene) tonalite, with minor granodiorite; locally finer-grained variants. I-type.|
29513|Kandos Group|22529|5|Briefly described|1,4 fig 2|Early Devonian|Early Devonian|||||||
29513|Kandos Group|22590|6|Mentioned|Fig3 P754|Emsian|Lochkovian|||||||
29513|Kandos Group|22768|5|Briefly described|p179|Emsian|Lochkovian|||||||
29513|Kandos Group|22857|5|Briefly described|p179, p474 App.1 Tb.A1.6|Emsian|Lochkovian|Fine to coarse-grained clastics, limestone, dacite ignimbrite, volcaniclastics and lava. Max. thickness: 4km. Geological Province: Capertee Rise. See also p476 App.1 Tb.A1.6.||||||
29513|Kandos Group|23043|5|Briefly described|Map Legend|Eifelian|Lochkovian|||||||
29513|Kandos Group|23170|2|Defined|p125|Eifelian|Lochkovian|of Lachlan Fold Belt.  Conodont dating (Colquhuon 1995) suggests the group extends from the woschmidti Zone in the early Lochkovian to at least the paritus Zone of the earliest Eiflian.||||||
29513|Kandos Group|23214|3|Fully described|p205|Early Devonian|Early Devonian|Formerly referred to as Kandos Series. Thick sequences of siliciclastic, carbonates, volcaniclastics and silicic volcanics deposited in a shallow marine to subaerial environment.||||||
29513|Kandos Group|43188|4|Described|p205||Early Devonian|Capertee High.Age early Lochkovian to middle Emsian.||||||
29513|Kandos Group|43782|5|Briefly described|Map Legend|Emsian|Emsian|||||||
29513|Kandos Group|44093|5|Briefly described|p212 App. 1|Early Devonian|Early Devonian|Includes Carwell Creek Formation, Riversdale Volcanics, Roxburgh Formation, Yellowmans Creek Formation, Clandulla Limestone and Warrah Conglomerate. Geological Province: Lachlan Fold Belt.||||||24-MAR-05
29513|Kandos Group|66197|5|Briefly described|p633 Fig.4a|Emsian|Lochkovian|Capertee High-Hill End Trough. Shallow marine mixed clastic and carbonate rocks. Overlies the Riversdale and Dungeree Volcanics.||||||14-MAR-12
29513|Kandos Group|68003|5|Briefly described|p24 Fig.3-e. |Emsian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Carwell Creek Formation.|||
29513|Kandos Group|70297|5|Briefly described|map legend, on side 2 of map sheet|Emsian|Lochkovian|Age: Middle Devonian (early Lochkovian to earliest Eifelian). Deposited on shelf adjacent to Hill End Trough, the Capertee High. Erosional base.||||||
29513|Kandos Group|73299|6|Mentioned|p1096 Fig.3, p1098 Fig.4|||Capertree High.||||||
82513|Kangaroo Creek Sandstone Member|70820|6|Mentioned|p37|Cretaceous|Late Jurassic|Richmond River catchment area (Casino-Kyogle area) basement aquifer.||||Is overlain by the Bungawalbin Member.|A fluvial channel deposit containing quartzose sandstone in calcareous or argillaceous cement.|
30652|Kangaroo Mountain Basanite|43346|2|Defined|p4 Map|||||||||19-JAN-10
30652|Kangaroo Mountain Basanite|43349|14|Not recorded|Map|||||||||
70450|Kankool Ignimbrite Member|62095|2|Defined|p275-276 Appdx.|Late Carboniferous|Late Carboniferous|Of Currububula Fm. Supersedes Back Creek Tuff Mbr. Beige unwelded ignimbrite with fine to medium phenocrysts of plagioclase.... Overlain by Allawa Ig, Mbr. Age: ~310Ma. Thick: >10m. Geol.Prov: Werrie block/Tamworth Belt. See also Plate 1, p245 Figs. 4, 5.||||||31-JAN-08
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.|
73550|Kara Formation|66623|1|Redefined|pp19-25, p28, pp12-17.|Early Cambrian|Neoproterozoic|Redefined in this publication. Correlative of Farnell Group and by inference Wilpena Group. Has oncolites and possible lenticular stromatolites. Formerly part of Torrowangee Series (Mawson 1912), Wonominta beds (Warris 1967), then Kara beds (Mills 1992). Hosting clear extrusive and intrusive realationship with Mount Arrowsmith Volcanics (p28).||Unit in Grey Range Group.|Includes Gravel Creek Member.|Is overlain by Nundora Formation (Teltawongee Group) with gradational conformable contact. Locally intruded by gabbroic to wehrlitic sills of Mount Arrowsmith Volcanics.|Mustard-coloured, intercalated dolomite, quartzite, limestone, siltstone, sandstone units; metamorphosed to greenschist facies. Shows bedding, cross-bedding, ripple marks and laminations.|24-SEP-13
73550|Kara Formation|66917|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Several un-named units are mapped separately.||Unit in Grey Range Group.|Includes Gravel Creek Member.|Overlies Mount Arrowsmith Volcanics.|Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|66918|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Four un-named units are mapped separately.||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|66927|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Zones of low magnetic intensity with local narrow trends of moderate magnetic intensity which may relate to narrow mafic sills and flows.||||Overlies Mount Arrowsmith Volcanics.|Phyllite, quartzite, sandstone and siltstone; minor dolomitic and calcareous beds.|
73550|Kara Formation|67105|5|Briefly described|p654- 655, 659, 661|Ediacaran|Ediacaran|Wonnaminta Zone, Koonenberry Belt.||Grey Range Group.||Is overlain (probably disconformably) locally by the Nundora Formation.|Shallow-marine sedimentary rocks.|
73550|Kara Formation|67207|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding; massive yellow, dolomitised limestone with variable lithic component.|
73550|Kara Formation|67208|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Seven un-named sub-units with differing lithologies are mapped separately.||Lower unit in Grey Range Group|Includes basal Gravel Creek Member.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; oolitic limestones, quartzite, quartzose sandstones, minor basaltic volcanics.|
73550|Kara Formation|67211|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|67322|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|W flank of Mount Arrowsmith, northern end of the Koonenberry Belt.||||Overlain by the Pincally Formation.||22-FEB-18
73550|Kara Formation|69961|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70648|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|3 un-named units: Metasedimentary sequence dominated by metre-scale thick quartzite horizons; originally quartz-rich sandstone. Pink to grey limestone with variable lithic component; regionally metamorphosed to lower greenschist facies. Dark grey to green cryptocrystalline chert with discontinuous boudinaged lenses up to 2m thick.||Grey Range Group|Includes 3 un-named units.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70650|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|4 unnamed units: multiply deformed biotite-muscovite schist; originally interbedded mudstone and sandstone, with minor feldspathic sandstone, quartz-hematite-magnetite and dolomitic limestone lenses; regionally metamorphosed to lower amphibolite facies. Metasedimentary sequence dominated by metre scale thick quartzite horizons; originally quartz-rich sandstone; regionally metamorphosed to greenschist facies. Pink to grey limestone with variable lithic component; regionally metamorphosed to lower greenschist facies. Buff to red-brown, medium- to coarse-grained lithic-feldspathic sandstone; lithic clasts are mainly volcanic and are poorly-sorted and subangular; regionally metamorphosed to greenschist facies.||Grey Range Group|Includes 4 un-named units.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70651|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Unnamed sub-unit is a metasedimentary sequence dominated by metre-scale quartzite horizons; originally quartz-rich sandstone.||Grey Range Group|Includes unnamed sub-unit.||Variably cleaved phyllite and minor quartzite; interbedded sandstone and siltstone with minor dolomitic and calcareous beds; ripples, bioturbation, cross-bedding and load structures; regionally metamorphosed to greenschist facies.|
73550|Kara Formation|70838|4|Described|p268-272, p274-278, p280-281|Ediacaran|Ediacaran|Coeval with Mount Arrowsmith Volcanics. SHRIMP U-Pb zircon age from interbedded rhyolite. Detrital zircon analyses: exclusively Mesoproterozoic source. Provenance discussed: Musgrave Province preferred.|585 +/- 3.2 Ma (Black, 2007).|Grey Range Group.||Is overlain conformably by Nundora Formation (Teltawongee Group).|Finely laminated siltstone and sandstone with  minor chert and limestone.|
73550|Kara Formation|71262|6|Mentioned|p3, p5 Fig 2, p8 Fig 5, p9, p12|Neoproterozoic|Neoproterozoic|||||||
73550|Kara Formation|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic|[the basaltic metavolcanics included in this SA description may be Mount Arrowsmith Volcanics, or equivalent]|||||Phyllite, schist with metasandstone, meta-limestone and basaltic metavolcanics.|12-DEC-21
73550|Kara Formation|73177|5|Briefly described|p1113-1115 Figs.15-17|Neoproterozoic|Neoproterozoic|Delamerian Orogen. Proposed continental rift setting. An MDA of >900 Ma (Johnson et al., 2016) is also given.|585 +/- 3.2 Ma.|Grey Range Group.||||
73550|Kara Formation|74367|6|Mentioned|p16, p18|Cambrian|Neoproterozoic|||Grey Range Group||||
23685|Karalinga Formation|37986|2|Defined|p310|Silurian|Silurian|||||||
23685|Karalinga Formation|68592|6|Mentioned|p899, p913|||Wollongong 1:250 000 map area.||Unit in Bungonia Group.|Includes Tugalong Limestone Member.|||
23685|Karalinga Formation|70661|6|Mentioned|p31|||||Bungonia Group||||
23686|Karawina Formation|22857|4|Described|p478 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Mumbil Group. Arenite, conglomerate, siltstone. Max. thickness: 300m. Geological Province: Capertee Rise.||||||
23686|Karawina Formation|23214|3|Fully described|p145|Pridoli|Ludlow|Of Mumbil Group.  Composed of metamorphosed feldspathic quartz sandstone, conglomerate and metasiltstone. Max. thickness: 300m.||||||
23686|Karawina Formation|42712|4|Described|8, Table1 p14.|Early Devonian|Late Silurian|Within Campbells/Kildrummie Group. Unconformable on Rockley Volcanics, conformable below Campbells Formation||||||
23686|Karawina Formation|43639|5|Briefly described|Map Legend||Silurian|||||||
23686|Karawina Formation|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|of Mumbil Group.||||||
23686|Karawina Formation|68592|5|Briefly described|p650|Late Silurian|Late Silurian|||Unit in Mumbil Group.||Correlated with Cuddyong Formation (Campbells Group).||
23686|Karawina Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
23687|Karikeree Metadolerite|22736|6|Mentioned|p627|||||||||
23687|Karikeree Metadolerite|24124|5|Briefly described|p3|||||||||
23687|Karikeree Metadolerite|40134|2|Defined|p279|Late Permian|Late Permian|||||||
23687|Karikeree Metadolerite|41347|4|Described|p171|||||||||
23687|Karikeree Metadolerite|41348|5|Briefly described|Map legend|Early Paleozoic||||||||07-NOV-08
23687|Karikeree Metadolerite|44093|5|Briefly described|p237 App. 1|Early Permian|Early Permian|Geological Province: New England Fold Belt.||||||
23687|Karikeree Metadolerite|62058|4|Described|p4, p5, p29 Fig.11, map sheet|Permian|Permian|||||Intrudes Watonga Formation, Touchwood Formation and Thrumster Slate.|Holocrystalline medium-grained dolerite. Variably altered.|
23687|Karikeree Metadolerite|63763|2|Defined|p2, p4-5 Fig. 1, p14-15|Early Permian|Early Permian|Revised def. presented, for unit prev'ly defined by Leitch (1980a) - def.not formally formatted however. Emplaced as dykes in Port Macquarie Serpentinite, Thrumster Slate, and Touchwood + Watonga Fms. Intruded by Nobbys Beach Lamprophyre; lithol.detail.||||||03-FEB-09
23687|Karikeree Metadolerite|65940|6|Mentioned|p194|||Wauchope-Port Macquarie area, NSW.||||||
23687|Karikeree Metadolerite|66090|5|Briefly described|p18-19|Permian|Permian|Of Port Macquarie Block.||||||
40130|Karingal Rhyolite Member|61964|3|Fully described|p14 Fig. 4, p83-83, p79|Lochkovian|Lochkovian|Of Ural Volcanics (Rast Group). Grey, speckled, v. coarse-gr.boulder-forming porphyritic rhyolite; euhedral to rounded feldspar megacrysts; lithic + porphyritic enclaves. Age: 422+/-4Ma (Bull, in prep.) suggesting age is older than Early Devonian. ||||||
40130|Karingal Rhyolite Member|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Ural Volcanics (Rast Group). Grey, speckled, very coarse-grained boulder-forming porphyritic rhyolite; euhedral to rounded feldspar megacrysts; lithic and/or fine-grained porphyritic mafic enclaves.||||||
40130|Karingal Rhyolite Member|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Ural Volcanics.|||Grey to speckled very coarse-grained boulder-forming quartzofeldspathic coherent facies; euhedral to rare rounded megacrysts of feldspar with lithic and/or fine-grained mafic porphyritic enclaves containing traces of sulfide.|
82515|Karonstadt Complex|71628|4|Described|p11: 39; p15: 34, 40, 52, 58, 69,85,116|||See also p19: 80-89. New name (this study) applied to mafic and hybrid intermediate rocks spatially associated with the Undercliffe Falls Monzogranite, and includes the Warroo Monzogranite (herein the Warroo Monzogranite Phase). Named after a local property. Comprises numerous outcrops in the Bakers Hill - Liston area (locations elaborated in text). Crops out as residual boulders. Relationships, usually complex, with other units are described in detail. Possibly intruded simultaneously with Stanthorpe Complex. Lithologies and mineralogy described in considerable detail. Geochemistry described.|||Warroo Monzogranite Phase.|Complex boundary with Jenners and Undercliffe Falls Monzogranites, and Stanthorpe Complex.|Compositionally and texturally diverse intrusives incorporating layered olivine-clinopyroxene-orthopyroxene gabbros, dolerite, diorite, hybrid granites, and strongly porphyritic biotite-hornblende monzogranite.|
35615|Karoopa Granite|50231|5|Briefly described|Map Legend|Emsian|Emsian|||||||
35615|Karoopa Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Karoopa Suite. Pinkish-grey, fine- to medium-grained, massive, equigranular (occasionally porphyritic), leucocratic, pyroxene?-biotite granite, with rare miarolitic cavities, minor biotite tonalite. Microgranitic marginal phases. Intruded by dykes.||||||09-SEP-08
35615|Karoopa Granite|68592|2|Defined|p1250, p1398, p1400-3, p1462-5|Early Devonian|Early Devonian|New unit and name, after Karoopa Lane and nearby Karoopa property. Previously included as part of Illunie Rhyolite by Brunker and Offenberg (1970). Type locality described. Geochemistry detailed; geophysical properties described. Assigned to Boggy Plain Supersuite. Probably comagmatic with Black Range Group Volcanics.||Unit in Karoopa Suite.||Intrudes Young Granodiorite. Is overlain unconformably by Hervey Group (inferred).|Pinkish-grey, fine- to medium-grained, massive, equigranular to occasionally porphyritic, leucocratic, biotite granite; minor biotite tonalite phase; fine-grained and equigranular or microgranitic margins. I-type.|
35615|Karoopa Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dqk. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Karoopa Suite|||Fine-medium grained, massive, equigranular, leucocratic, biotite granite with rare miarolitic cavities; minor biotite tonalite; microgranitic marginal phases; intruded by massive, porphyritic rhyolite dykes; moderate-high magnetic susceptibility.|
35615|Karoopa Granite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Karoopa Suite|||Fine-medium grained, massive, equigranular, leucocratic, biotite granite with rare miarolitic cavities; minor biotite tonalite; microgranitic marginal phases; intruded by massive, porphyritic rhyolite dykes; moderate-high magnetic susceptibility.|
70496|Karralee Ignimbrite Member|62095|2|Defined|p277 Appdx. late carb||Late Carboniferous|Of Currabubula Formation. Purple to brown, welded to unwelded ignimbrite with rare coarse phenocrysts. Interbeded with less extensive unnamed rhyodacite flows .Age is Westphalian. Thick: ~10m. Geol.Prov: Werrie block/Tamworth Belt.  See also Plate 1.||||||31-JAN-08
33404|Kars Ultramafic Intrusive Complex|24417|3|Fully described|p39|Late Ordovician|Late Ordovician|Previously informally referred to as "Kars intrusive complex".||||||
33404|Kars Ultramafic Intrusive Complex|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Ultramafic rocks.||||||
33404|Kars Ultramafic Intrusive Complex|60009|5|Briefly described|Map Legend|Eastonian|Eastonian|||||||13-JUL-04
23689|Kataway Mudstone|22736|6|Mentioned|p628 Fig7||Tournaisian|||||||
23689|Kataway Mudstone|22857|4|Described|p500 App.1 Tb.A1.7|Tournaisian|Tournaisian|Unfossiliferous mudstone, interbeds of siltstone, single coarse feldspathic arenite. Max. thickness: 630m. Geological Province: Tamworth Forearc Basin.||||||
23689|Kataway Mudstone|36057|2|Defined|p346|Visean|Tournaisian|Tournaisian - Visean||||||
23689|Kataway Mudstone|36528|6|Mentioned|p176|||||||||
23689|Kataway Mudstone|39660|6|Mentioned|p449|||||||||
23689|Kataway Mudstone|40883|6|Mentioned|p5|||Mention Fig.2||||||
23689|Kataway Mudstone|42547|4|Described|p34|||||||||
23689|Kataway Mudstone|44093|5|Briefly described|p231 App. 1|Tournaisian|Late Devonian|Geological Province: New England Fold Belt.||||||
23689|Kataway Mudstone|44244|2|Defined|p200|Tournaisian|Tournaisian|Conformably overlies Wallanbah Formation; underlies Boolambayte Formation.  Max. thickness: >730m.  Geological Province: Myall Block.  Type section in text.||||||
23689|Kataway Mudstone|47056|6|Mentioned|Fig.2 P523|||||||||
23689|Kataway Mudstone|50132|6|Mentioned|p248  Fig.6|||Early Namurian age||||Overlies the Wallanbah Formation. Underlies the Boolambayte Formation.||
23689|Kataway Mudstone|50263|5|Briefly described|Map Legend|Visean|Visean|Overlies: Wallanbah Formation.  Geological Province: Eastern Myall Block.||||||
23689|Kataway Mudstone|63832|6|Mentioned|p131 Fig.2|Visean|Visean|Eastern Myall block, Southern New England Fold Belt.||||||
23689|Kataway Mudstone|64631|5|Briefly described|p44 Fig.2.|Visean|Tournaisian|Southern New England Fold Belt, eastern Myall Block. Biostratigraphic age control for base and top.||||Overlies Wallanbah Formation. Is overlain by Boolambayte Formation.||
23689|Kataway Mudstone|69793|6|Mentioned|p1121 Fig.12|Visean|Tournaisian|Myall Block, Tamworth Belt.||||||
73842|Kellys Creek Leucomonzogranite|71628|3|Fully described|p17: 2, 6, 35, 54, 59, 65-68, 70|||Chappell and Bryant (1994 unpublished); initially Kellys Creek Leucoadamellite (Korsch, 1978). Has precedence over Nymboi Granite of Li et al. (2012). Named after a local watercourse. Forms an ovoid, ~15 km2 intrusion about 8 km E of Clouds Creek. The type locality is near Kellys Creek where it cuts the intrusion. Geochemistry described and I- and A-types discussed. Highly variable mineralisation deposits (named) include gold, base metals and tin.|221.3 +/- 2.2 Ma (SHRIMP: Li et al., 2012).|Tallawudjah Suite.||Intrudes Coramba beds.|Medium- to fine-grained, porphyritic to equigranular biotite-(hornblende) leucomonzogranite. A-type.|
27172|Kellyville Laminite Member|22745|6|Mentioned|p138|||Sydney Basin.||||||
27172|Kellyville Laminite Member|35690|2|Defined|p178|Middle Triassic|Middle Triassic|||||||
27172|Kellyville Laminite Member|39298|5|Briefly described|p262|||See also P263||||||
27172|Kellyville Laminite Member|39626|6|Mentioned|p275|||||||||
27172|Kellyville Laminite Member|40602|4|Described|p22|||||||||
27172|Kellyville Laminite Member|42896|4|Described|p42, Fig.7|||of Ashfield Shale||||||
27172|Kellyville Laminite Member|42925|4|Described|p22|||of Ashfield Shale||||||
27172|Kellyville Laminite Member|70661|6|Mentioned|p211|Middle Triassic|Middle Triassic|Age derived from parent unit. Not present in the map sheet area (Moss Vale)||Ashfield Shale||||
32180|Kelvin Suite|22815|5|Briefly described|p84|||Consists of two plutons: Bombala and Gunningrah Tonalites.||||||
32180|Kelvin Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
29941|Kempfield Granodiorite|22679|4|Described|p 49|||||||||
29941|Kempfield Granodiorite|22798|6|Mentioned|p851 Fig.2|Devonian|Silurian|Siluro-Devonian.||||||
29941|Kempfield Granodiorite|23214|3|Fully described|p173|Late Silurian|Late Silurian|Originally included in the Barry Granite. Intrudes the Coombing Formation, Triangle and Campbells Formations. Geological Province: Wyangala Batholith.||||||
29941|Kempfield Granodiorite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Recrystallised biotite granodiorite.||||||17-JUL-08
29941|Kempfield Granodiorite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|||||||
29941|Kempfield Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
81816|Kengal Formation|73457|4|Described|ii, p1, p3, p5, p7-9, p14|Late Devonian|Early Devonian|Name is derived from 'Kengal', the Aboriginal place name for The Rock, southwest of Wagga Wagga. Interpreted as non-marine. Estimated to be 2150 m thick. Divided into six informal subunits (A-G) by Williams (2016), most extend laterally for over 10km. Included in the Mulga Downs Group by Williams (2016), Trigg (2019) however suggested the formation be left ungrouped. Maximum depositional age of 413.7+/-2.2 Ma from detrital zircons in subunit E (Huang 2019). Late Devonian age based on general correlation with other Late Devonian units. Exact nature of contact with Wallandoon Ignimbrite cannot be determined. Has been folded into a large anticline with a spaced foliation that is axial planar. Faults bound the formation to the NE, NW and SW. Full definition given in Trigg (2021).|413.7+/-2.2 Ma MDA (Huang, 2019)|||Unconformably overlies Adaminaby Group, overlies Wallandoon Ignimbrite|Comprises intercalated conglomerate, pebbly sandstone and siltstone.|
25678|Kensington Formation|721|5|Briefly described|Map legend|Sakmarian|Sakmarian|Conglomerate, siltstone, sandstone, rare basalt and limestone.  Geological Province: Tamworth Belt.||||||
25678|Kensington Formation|22857|4|Described|p506 App.1 Tb.A1.8|Late Carboniferous|Late Carboniferous|Conglomerate, siltstone, sandstone; rare basalt and limestone. Max. thickness: 1300m.||||||
25678|Kensington Formation|41009|3|Fully described|p5|||||||||
25678|Kensington Formation|42866|5|Briefly described|Table 2, P12|||||||||
25678|Kensington Formation|43091|5|Briefly described|Map legend|||||||||
25678|Kensington Formation|44093|5|Briefly described|p226 App. 1|Early Permian|Early Permian|Clastic sediments. Geological Province: New England Fold Belt.||||||
25678|Kensington Formation|65398|4|Described|p4 Fig.2, p6 Fig.3, p8, Fig 2-3, 6|Early Permian|Early Permian|Fossiliferous, shallow marine. Occurs as fault bounded blocks and slivers. Contains massive to foliated pebble orthoconglomerate, sandstone, radiolarian siltstone, black shale, pebbly mudstone, massive and conglomeratic limestone, rare basalt, tuff and claystone.||||||
25678|Kensington Formation|66720|5|Briefly described|Map legend|Early Permian|Early Permian||||||Massive pebble conglomerate, siltstone, sandstone, shale, pebbly mudstone, limestone; rare basalt, tuff and claystone.|
25678|Kensington Formation|68005|5|Briefly described|p49 Fig.3-M, p57, p136, p170.|Sakmarian|Sakmarian|Tamworth Belt. One of a number of units that occur in narrow fault slivers immediately west of the Peel Fault.|||||Conglomerate, siltstone, sandstone, rare basalt and limestone.|
25678|Kensington Formation|68822|6|Mentioned|p342|||Low metamorphic grade.||||||
82522|Kentucky Quartz Diorite|71628|4|Described|p8: 3, 49-55, 66-67, 77|||New name. Includes the Kentucky Diorite (Binns et al., 1967) and Kentucky Ponds Diorite (Flood, 1971), both small intrusions. Named after the local homestead, village or Parish. The most mafic unit in Uralla Supersuite. Geochemistry described|245.3 and 251.3 Ma (Rb-Sr biotite: Shaw, 1994).|Uralla Suite.||Intrudes Wandsworth Volcanic Group and Terrible Vale Porphyritic Microgranodiorite. Abuts Wilhelmshohe Tonalite (nature of the boundary uncertain).|Medium- to coarse-grained, weakly porphyritic, two-pyroxene-hornblende-biotite-quartz diorite; minor gabbro, quartz gabbro, quartz monzodiorite, and tonalite; locally contains appinitic diorite and felsic pegmatite.|
22086|Kerillon Tuff Member|22678|3|Fully described|p714-15,720,725|||Of the Tangerang Formation.||||||17-JAN-06
22086|Kerillon Tuff Member|50234|5|Briefly described|Map Legend|Pragian|Pragian|Of the Tangerang Formation (Bindook Volcanic Complex).  ?Underlies Kerrawarra Dacite Member.||||||16-JUN-08
22086|Kerillon Tuff Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tangerang Fm (Bindook Gp). Rhyolitic accretionary lapilli-bearing non-welded ignimbrite and volcaniclastic rocks overlain by coarse-grained welded, crystal-rich dacitic ignimbrite, and subordinate volcanic breccia, ashfall tuffs + tuffaceous sandstone.||||||16-JUN-08
22086|Kerillon Tuff Member|66300|5|Briefly described|p76, pp81-86.|||This age is indistinguishable from all existing SHRIMP zircon 238U/206Pb dates for the Bindook Group.|412.7 +/- 2.2 Ma.|Unit in Tangerang Formation.|||Dark-grey, medium-grained and moderately crystal-rich welded dacitic ignimbrite containing abundant volcanic lithic clasts and flattened pumice clasts defining a eutaxitic texture.|
22086|Kerillon Tuff Member|68592|2|Defined|p1061-4, p1083, p1121-7, p1657|Pragian|Lochkovian|Originally part of undifferentiated Tangerang Formation by Wass and Gould (1969) and later workers. The southernmost exposures were included in Aloes Tuff Member (Hall, 1981; Jones, Carr et al., 1984). This latter unit was abandoned (Simpson, 1990; Simpson, Carr and Jones, 1997) and the Kerillon Tuff Member was included as a mappable horizon in the Tangerang Formation. Type section and representative section described. c.2km thick. Geochemistry and geophysical properties described. A marker horizon. Includes abundant clasts of Carne Dacite Member. Age from fossils (conodonts and trilobites).||Unit in Tangerang Formation.||Is overlain by Barrallier Ignimbrite unconformably; Carne and Kerrawarra Dacite Members (the latter conformably). May correlate with Newacres and Four Winds, Ignimbrite Members (Quialigo Volcanics).|Basal massive medium-grained rhyolitic volcaniclastic rocks, accretionary-lapilli tuffs, fine-grained and planar-bedded volcaniclastics; dacitic ignimbrite, lesser volcanic breccia, ash-fall tuffs, accretionary-lapilli tuffs and tuffaceous sandstone.|
22086|Kerillon Tuff Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dkte. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Tangerang Formation||Is overlain by Kerrawarra Dacite Member.|Rhyolitic, accretionary lapili-bearing, non-welded ignimbrite and volcaniclastic rocks overlain by coarse-grained, welded, crystal-rich, dacitic ignimbrite with subordinate volcanic breccia, ash-fall tuff and tuffaceous sandstone.|
22086|Kerillon Tuff Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Tangerang Formation|||Rhyolitic, accretionary lapili-bearing, non-welded ignimbrite and volcaniclastic rocks overlain by coarse-grained, welded, crystal-rich, dacitic ignimbrite with subordinate volcanic breccia, ash-fall tuff and tuffaceous sandstone.|
22086|Kerillon Tuff Member|70661|3|Fully described|vii, p6, p51, p52 fig 5, p61-p64|Lochkovian|Lochkovian|Name derived from Kerillon Tuff Member. Originally included in undifferentiated Tangerang Formation. Distribution, structure, metamorphism, geochemistry, geophysical characteristics discussed. Forms blocky to bouldery outcrops. Type section mentioned. 365m thick in type section, estimated to be 2km thick. Deposited by violent phreatomagmatic eruptions in a marine to subaerial environment. The rhyolitic and dacitic subdivisions of this member are discussed in further detail.|412 +/- 2.2 Ma (SHRIMP U-Pb)|Tangerang Formation||Overlain by Kerrawarra Dacite Member, unconformably overlain by Barrallier Ignimbrite|Sequence of volcaniclastic rocks, tuffs and welded ignimbrites that can be divided into a lower rhyolitic and upper dacitic unit.|
22086|Kerillon Tuff Member|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Tangerang Formation.|||Rhyolitic and dacitic volcaniclastic and tuffaceous rocks; homogeneous and undifferentiated welded dacitic ignimbrite.|16-FEB-18
34259|Kerrawarra Dacite Member|22678|4|Described|Fig2p713,714,721,725|||Of the Tangerang Formation.||||||17-JAN-06
34259|Kerrawarra Dacite Member|50234|5|Briefly described|Map Legend|Pragian|Pragian|Of the Tangerang Formation (Bindook Volcanic Complex).  Overlies Kerillon Tuff Member.  Underlies Joaramin Ignimbrite.||||||16-JUN-08
34259|Kerrawarra Dacite Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Tangerang Fm (Bindook Gp). Dark grey, massive to flow banded, crystal-rich dacitic lava, phenocrysts of plagioclase, pyroxene+trace qtz set in originally glassy groundmass, minor autobrecciated dacite, discontinuous horizons of feldspathic siltst/sst..||||||16-JUN-08
34259|Kerrawarra Dacite Member|68592|2|Defined|p1061, p1128-33|Pragian|Pragian|Originally part of undifferentiated Bindook Porphyry (McElroy and Relph, 1961); later part of Carne Dacite Member (Jones, Carr et al., 1984). Distinguished as a separate entity by Simpson (1990); formally defined by Simpson, Carr and Jones (1997). Named after Kerrawarra property. Type and representative sections, and good exposures, are described. Over 700m thick. Interpreted as a probable lava flow of unusually large extent. Geochemistry and geophysical properties described.||Topmost unit in Tangerang Formation.||Conformably overlies Kerillon Tuff Member. Is overlain by Joaramin Ignimbrite and unconformably by Barrallier Ignimbrite. Is intruded by Carne Dacite Member.|Widespread, massive to flow-banded dark grey dacitic unit; compositionally and texturally homogeneous. Minor dacitic volcaniclastic sedimentary rocks.|
34259|Kerrawarra Dacite Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dktk. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Tangerang Formation||Is overlain by Joaramin Ignimbrite (of Bindook Group). Overlies Kerillon Tuff Member.|Massive - flow-banded, crystal rich dacitic lava with phenocrysts of plagioclase, pyroxene, hornblende and quartz set in an originally glassy groundmass. Minor autobrecciated dacite and discontinuous horizons of feldspathic siltstone and sandstone.|
34259|Kerrawarra Dacite Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Tangerang Formation|||Massive - flow-banded, crystal rich dacitic lava with phenocrysts of plagioclase, pyroxene, hornblende and quartz set in an originally glassy groundmass. Minor autobrecciated dacite and discontinuous horizons of feldspathic siltstone and sandstone.|
34259|Kerrawarra Dacite Member|70661|3|Fully described|p52 fig 5, p64-p67|Pragian|Pragian|Name derived from Kerrawarra property. Originally a part of the Bindook Porphyry, also included in the Carne Dacite Member. Forms low bouldery outcrops in the big hill area. Type section mentioned. Maximum thickness of 550m . Age constrained by Barralier Ignimbrite. Structure, metamorphism, geochemistry and geophysical characteristics discussed in some detail. ||Tangerang Formation||Conformably overlies Kerillon Tuff Member, overlain by Joaramin Ignimbrite, locally unconformably overlain by Barralier Ignimbrite, Intruded by Carne Dacite Member, Marulan Granite|Compositionally and texturally homogenous dark grey dacite. Dacitic volcaniclastic rocks consisting of interbedded shale, siltstone and sandstone composed of dacitic detritus. Flow banded and massive in places.|
34259|Kerrawarra Dacite Member|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Tangerang Formation.|||Homogeneous dark grey dacite; flow banded or autobrecciated locally. Minor intercalated dacitic volcaniclastic sedimentary rock. Sandstone, shale and siltstone, composed of dacitic detritus. Plant fragments abundant locally.|16-FEB-18
70251|Kerrawary Siltstone|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Grey, thickly- to very thickly-bedded siltstone with minor massive thinly- to medium-bedded fine- to medium-grained quartzose sandstone.||||||
70251|Kerrawary Siltstone|68592|2|Defined|p726-8, p752-3, p810-814, p818, p820-1|Late Silurian|Early Silurian|See also p236, p731 Fig.132, p833, p889, p908, p1889-1890. New name. The beds now separated as Kerrawary Siltstone in the type area were formerly split between upper part of Cobra Formation and base of Argyle Formation of Taralga Group (Scheibner 1973). Outcrops on the Hume Highway, east of Goulburn, were formerly an undifferentiated unit within Towrang Beds of Brunker and Offenberg (1970). Has very poor outcrop. Type area is in Kerrawary Creek and in an abandoned gravel quarry. True thickness probably 500-600 m in type area; folded. Depositional environment in bottom currents in possibly poorly aerated or anoxic waters. Mild hornfelsing next to Lockyersleigh Granite. Locally very fossiliferous, very fragmentary. Type area fossil names detailed. Age range is most probably early to late Ludlow. Distinguished by generally uniform lithology, marked bedding plane fissility, and dark grey weathering to off-white colour. Contains graptolites (listed), some inarticulate brachiopods and rare shelly fossils. Abundance of Bohemograptus subsp. provides a good marker.||Unit in Mount Fairy Group.||Overlies Cobra Formation ?conformably. Is gradationally overlain by Argyle and De Drack Formations. Equivalent to Cardinal View Formation. Is faulted against Warbisco Shale and Covan Creek Formation.|Mostly dark to pale grey carbonaceous siltstone, thick- to very thick-bedded and laminated, with minor fine- to medium-grained grey sandstone beds, thin- to medium-bedded, massive and moderately well sorted.|
70251|Kerrawary Siltstone|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sfy. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group||Overlies De Drack Formation. Overlies, and interfingers with, Cobra Formation. Is overlain by Covan Creek Formation and Argyle Formation.|Thick-very thickly bedded, laminated siltstone with minor massive, thin-medium bedded, fine-medium grained quartzose sandstone.|
70251|Kerrawary Siltstone|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|||Grey, thick - very thickly-bedded, laminated siltstone with minor massive, thin-medium bedded, fine-medium grained quartzose sandstone.|
70251|Kerrawary Siltstone|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|||Thick-very thickly bedded, laminated siltstone with minor massive, thin-medium bedded, fine-medium grained quartzose sandstone.|
70251|Kerrawary Siltstone|71069|6|Mentioned|p134, p138 fig 44, p144, p146|Ludlow|Ludlow|Up to 500m thick. Contains fossils of Bohemograptus bohemicus. See also p147, p162, p170, p172.||Mount Fairy Group||Conformably overlain by the Covan Creek Formation. Overlies the Cobra Formation. Conformably overlies and is a part equivalent of the De Drack Formation.||
70251|Kerrawary Siltstone|71656|4|Described|p13 Fig.2, p29-30, p53-56|Ludlow|Ludlow|Shown as Kerrawarry Formation p52. Also located on p55 Fig.6, p56 Fig.7. Include graptolites, brachiopods, ostracods. Graptolites constrain age to nilssoni and overlying scanicus zones of the early Ludlovian.||Mount Fairy Group||Mount Fairy Group. Overlies and is partially equivalent to Cobra Formation. Partially equivalent to Undifferentiated De Drack Formation and underlies the Argyle Formation.|Fossiliferous limestone.|
69867|Keverstone Supersuite|68592|2|Defined|p622, p678, p681, p690-1, p1482-1541|Early Devonian|Early Devonian|See also p74 Tb.5. New name, after Blevin (2011); named for Parish Keverstone. Comprises nine plutons: two un-named. Type pluton (felsic component) is Yewrangara Granite and type pluton (mafic component) is Goonoonglah Monzodiorite. Geochemistry detailed. Magmatism thought to result from high temperature melting of a quartzo-feldspathic source. A genetic link with Wrens Nest Trachyte and Box Ridge Volcanics is suggested from geochemical similarities. Plutons in the Supersuite host minor tin and traces of molybdenite; road construction material has also been obtained. Wyangala and Peelwood structural zones: deformation described.|413 +/- 5 Ma - 398 +/- 6 Ma (Wilde, 2001).||Includes Goonoonglah, Yewrangara and Whick Whack Suites.||A-type. Felsic plutons are biotite granite and leucogranite and minor biotite-quartz syenite. Mafic plutons are quartz syenite, quartz monzonite and quartz monzodiorite, with minor quartz diorite and gabbro.|
69867|Keverstone Supersuite|70297|5|Briefly described|map legend|Pragian|Lochkovian|Age: Lochkovian?|||Spring Road Granite|||
70498|Kewell Creek Volcanic Member|62095|1|Redefined|p281 Appdx., Plate 1, p259 Fig. 10|Late Carboniferous|Late Carboniferous|Of Seaham Fm. Interbedded, dacitic ashflow and ashfall ignimbrites, volcanic agglomerate, epiclastic ......... Similar to Birken Head Volcanic Member (Willuri Fm.). Overlain by Temi Fm. Age: 320.5+/-2.9Ma. Thickness: 155m in type section. Rouchel block...||||||
70498|Kewell Creek Volcanic Member|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Seaham Formation||||
25970|Khan Yunis Formation|22815|5|Briefly described|p102|Late Devonian|Late Devonian|||||||
25970|Khan Yunis Formation|22857|5|Briefly described|p217, p494 App.1 Tb.A1.7|Late Devonian|Fammenian|Of the Minuma Range Group. Coarse lithic arenite, siltstone, minor siltstone and shale. Max. thickness: 550m. ||||||
25970|Khan Yunis Formation|22859|5|Briefly described|p217||Famennian|||||||
25970|Khan Yunis Formation|23549|6|Mentioned|p528|||Mentioned only as stratigraphical nomenclature example.||||||05-APR-05
25970|Khan Yunis Formation|39028|6|Mentioned|Map legend|Famennian|Famennian|||||||
25970|Khan Yunis Formation|40276|2|Defined|p26|Late Devonian|Late Devonian|||||||
25970|Khan Yunis Formation|41385|6|Mentioned|Table 2|||||||||
25970|Khan Yunis Formation|42497|5|Briefly described|Map Legend|Famennian||||||||
25970|Khan Yunis Formation|43233|5|Briefly described|Map Legend||Late Devonian|||||||
25970|Khan Yunis Formation|68298|5|Briefly described|p234|||Non-marine rocks. A Famennian Bothriolepis-phyllolepid-Remigolepis-Groenlandasapis association of placoderms.||||||
25970|Khan Yunis Formation|71700|5|Briefly described|CD|Famennian|Famennian|Ages derived from fossil assemblage.||Minuma Range Group||||
25970|Khan Yunis Formation|73181|6|Mentioned|p65|Famennian|Famennian|Contains fish fossils.||Minuma Range Group||Underlain by Deua Formation.||
32248|Khancoban Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh4||||||
32248|Khancoban Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
31595|Khancoban Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
82525|Kia-Ora Syenogranite Phase|71628|4|Described|p11: 39; p16: 12, 14-16, 20|||New name (this study); previously Kia-Ora Syenogranite of Sivell and Passmore (1999) after unpublished work by Passmore (1998). Originally part of Undercliffe Falls Monzogranite. Named after a local homestead. Forms one larger (~1.5 x 0.2 km) mass and several smaller pods and dyke-like structures (?roof zone), ~13 km NE of Stanthorpe. Crops out as large boulders on high relief hills. Geochemistry described; is geochemically assigned to the Five Mile Creek Suite.||Cullendore Syenogranite.||Intrudes Undercliffe Falls Monzogranite and Thomkins Gully Monzogranite Phase. Is intruded by Herding Yard Creek Intrusives.|Light pink, medium-grained, mildly porphyritic, biotite syenogranite.|
40936|Kialla Quartz Diorite|50234|5|Briefly described|Map Legend|Emsian|Pragian|Part of the Wologorong Batholith.||||||21-JAN-21
40936|Kialla Quartz Diorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Mid greenish-grey, fine- to medium-grained, equigranular, massive quartz diorite and dark grey, coarse-grained, micropoikilitic, massive quartz gabbro. rare dark grey massive tonalite near western margin.||||||
40936|Kialla Quartz Diorite|68592|3|Fully described|p1657, p1682, p1690-5|Early Devonian|Late Silurian|New name, after Kialla Creek. Ungrouped. Type locality described. Geochemistry detailed; geophysical properties described. This numerical age is too old (the Campbells Group which it intrudes has yielded younger ages) and may reflect inherited zircons. Has an equivocal contact relationship with the surrounding Wologorong Granite: magma mingling occurs on a variety of scales, and may be responsible for some of the lithological and chemical variation in this unit.|425.4 +/- 2.4 Ma (SHRIMP U-Pb: Black, 2005).||||Rocks have variable texture; primary lithology from mid greenish-grey, fine- to medium-grained, equigranular massive quartz diorite, to dark grey, coarse-grained, micropoikilitic, massive quartz gabbro; rare dark grey, massive tonalite. I-tpe.|
40936|Kialla Quartz Diorite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dxk. Ungrouped Devonian intrusion. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.|||||Fine-medium grained, equigranular, massive quartz diorite and coarse grained, massive, micropoikilitic quartz gabbro. Rare massive tonalite near the western margin.|
40936|Kialla Quartz Diorite|70296|5|Briefly described|p1, p15, p16, p24|||Goulburn-Yass district.|425.4 +/- 2.4 Ma (SHRIMP U-Pb)|||||21-JAN-21
40936|Kialla Quartz Diorite|70542|5|Briefly described|Map Legend|Devonian|Devonian||||||Fine-medium grained, equigranular, massive quartz diorite and coarse grained, massive, micropoikilitic quartz gabbro. Rare massive tonalite near the western margin.|
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|||||||
35851|Kilbrechin Conglomerate  Member|23329|3|Fully described|1051 Appendix 3|||||||||
67906|Kilburnie Monzogranite|71628|4|Described|p3: 1, 4, 9-10, 25-26, 61-67|||Leitch et al. (2010). Originally Kilburnie Adamellite of Binns et al. (1967). Subsequently revised by Pogson and Hitchins (1973). Renamed Kilburnie Granodiorite by Gulson and Goodbeer (1979). Named after a local homestead. Crops out ~17 km SW of Walcha as rounded boulders and rare flat surfaces. Geochemistry described. Contains an unusual combination of ferrohornblende and pale green actinolite (discussed).|288.6 +/- 1.5 Ma (SHRIMP: Leitch et al., 2010).|Kilburnie Suite.||Intrudes Sandon Association. Abuts (?is intruded by) Campfire Monzogranite.|Grey-blue to whitish-grey, porphyritic biotite monzogranite; amphibole and garnet bearing variants; locally rapakivi and microgranitic textures; weakly to strongly deformed (described). S-type.|
67906|Kilburnie Monzogranite|71703|5|Briefly described|p203, 204|Artinskian|Artinskian|289 Ma; Cawood et al., 2011.[unclear whether this is location 74,  289.8+/-1.7 Ma or 79,  288.6+/-1.5 Ma, p193 Fig.1]||Of Hillgrove Supersuite.||||
25972|Killimicat Granite|22768|6|Mentioned|p178|||||||||
25972|Killimicat Granite|22857|6|Mentioned|p178|Early Devonian|Early Devonian|||||||
25972|Killimicat Granite|37529|6|Mentioned|p9|||||||||
25972|Killimicat Granite|42313|2|Defined|p159|Early Devonian||||||||
25972|Killimicat Granite|42314|5|Briefly described|Map|Early Devonian||||||||
25972|Killimicat Granite|42726|5|Briefly described|map legend|Early Devonian||440.  Of the Bogong Suite (Boggy Plain Supersuite).||||||08-FEB-05
25972|Killimicat Granite|42828|5|Briefly described|Table 1 P129|Early Devonian||||||||
77019|Kimberley Park Monzogranite|71628|5|Briefly described|p2: 37, 39; p3: 1, 4, 9, 67-70|||Originally Kimberley Park Adamellite (Binns et al., 1967). Named after a local homestead. A small intrusion, ~29 km E of Walcha. Poor outcrop. Geochemistry described.||Argyll Suite (tentative).||Intrudes Agnes Greywacke. Is 'spatially associated' with Moona Plains Complex.|Heterogeneous, fine- to medium-grained biotite monzogranite; amphibole and garnet bearing variants; weakly to strongly foliated.|
23699|Kimo Diorite|42313|2|Defined|p100|Middle Silurian|Middle Silurian|Reserved May 1982. Age: early Middle Silurian to Middle Silurian||||||
23699|Kimo Diorite|42314|5|Briefly described|Map legend|Middle Silurian||||||||
23699|Kimo Diorite|69635|4|Described|p48-52|||Tumut Trough, Eastern Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation age. Sample location originally considered to be in Long Tunnel Metabasic Igneous Complex.|419.1+/-2.7 Ma|||Interpreted to intrude Long Tunnel Metabasic Igneous Complex. Contacts not observed.|Sample: conchoidal-fracturing hornblende diorite. I-type.|16-JUL-15
23699|Kimo Diorite|73215|5|Briefly described|p994|||Tumut Trough.|420 +/- 3 Ma (Fraser et al., 2014).|||||
36402|Kimridge Volcanic Member|50234|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Covan Creek Formation (Mount Fairy Group).  Aphanitic devitrified siliceous volcanic rocks.||||||
22101|Kindee Conglomerate|22616|6|Mentioned|Fig.1 p670||Carboniferous|||||||
22101|Kindee Conglomerate|22736|2|Defined|p617|Visean|Tournaisian|southern Hastings Block unit||||||
22101|Kindee Conglomerate|22857|4|Described|p500 App.1 Tb.A1.7|Tournaisian|Tournaisian|Age is inferred. Lithic sandstone, conglomerate and intraformational breccia; minor siltstone and diamictite. Max. thickness: 1000m.||||||
22101|Kindee Conglomerate|44093|5|Briefly described|p67 Fig 6.6|Carboniferous|Carboniferous|Of the Southern Hastings Block. Geological Province: New England Fold Belt.||||||14-MAR-05
22101|Kindee Conglomerate|70939|6|Mentioned|p826, p828-829|Carboniferous|Carboniferous|Southern Hastings Block. Faulting discussed.||||||
80917|Kindee Creek Tonalite|71628|4|Described|p17: 2, 13, 30-32, 97|||Formalised in this study; previously Kindee Creek tonalite (Chisholm et al., 2014) and originally Hillview Granite of Daigle (1993, unpublished). Named after a local watercourse. A small, barely unroofed intrusion at the Birdwood Cu-Mo-Au-Sn prospect ~40 km WNW of Wauchope. The very limited geochemistry (one analysis) is described. Is associated with significant Cu, Ag, Pb, Zn, Mo, and minor Au, mineralisation.|227.3 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Kindee Creek Suite.||Intrudes Nevann Siltstone.|Medium-grained, porphyritic to equigranular tonalite, and possibly granodiorite, and monzogranite porphyry. I-type.|
23700|King Gunnia Calc-Silicate Member|22500|5|Briefly described|p 1, 4, 10|||Of the Paragon Group.||||||11-SEP-07
23700|King Gunnia Calc-Silicate Member|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-SEP-07
23700|King Gunnia Calc-Silicate Member|22771|6|Mentioned|Table12.2p45|||||||||
23700|King Gunnia Calc-Silicate Member|22884|5|Briefly described|p43 Fig. 3, p47|||Within a unit of the Paragon Group. Geological province: Broken Hill Domain. May correlate to the Telechie Sulphide Member.||||||26-MAR-09
23700|King Gunnia Calc-Silicate Member|22965|6|Mentioned|Fig 1||Statherian|Within the Cartwrights Creek Metasediments.||||||
23700|King Gunnia Calc-Silicate Member|22967|6|Mentioned|p39||Statherian|||||||
23700|King Gunnia Calc-Silicate Member|38969|4|Described|p210|||||||||
23700|King Gunnia Calc-Silicate Member|39662|2|Defined|p436|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|40290|6|Mentioned|Fig.2|||||||||
23700|King Gunnia Calc-Silicate Member|40822|6|Mentioned|Fig.2|||||||||
23700|King Gunnia Calc-Silicate Member|41093|6|Mentioned|p252|||||||||
23700|King Gunnia Calc-Silicate Member|41630|6|Mentioned|Fig.1.3|||||||||
23700|King Gunnia Calc-Silicate Member|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|42537|4|Described|p15|||||||||
23700|King Gunnia Calc-Silicate Member|43086|6|Mentioned|Fig.3|||||||||
23700|King Gunnia Calc-Silicate Member|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Cartwrights Creek Metasediments||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Cartwrights Creek Metasediments.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Cartwrights Creek Metasediments.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|43572|6|Mentioned|Fig.3.2 p6|||||||||
23700|King Gunnia Calc-Silicate Member|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of Cartwrights Creek Metasediments (Paragon Group, Willyama Supergroup).||||||31-MAY-07
23700|King Gunnia Calc-Silicate Member|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Cartwights Creek Metasediments (Paragon Group).  Geological Province: Broken Hill Block.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|61606|5|Briefly described|p4 Fig. 2|||Of Cartwrights Creek Metasediments.||||||
23700|King Gunnia Calc-Silicate Member|61735|5|Briefly described|p635 Fig. 1, p639 Tb. 1|Statherian||Of Cartwrights Creek Metasediments (Paragon Group). Age: 1647+/-8 Ma U/Pb SHRIMP minimum crystallisation and 1651+/-8 Ma stratigraphic age. Presented as King Gunnia CS only in Fig. 2.||||||04-JUN-15
23700|King Gunnia Calc-Silicate Member|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments (Paragon Group). Geological province: Broken Hill Domain.||||||
23700|King Gunnia Calc-Silicate Member|62535|5|Briefly described|p666 Fig.3, p671-672, p674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Appears as King Gunnia calc-silicate member on p671, p674.||Cartwrights Creek Metasediments.|||Metamorphosed, laminated dolomitic carbonate sediment.|
23700|King Gunnia Calc-Silicate Member|62536|5|Briefly described|p636, 639, 650-651|||Broken Hill area. Appears only as King Gunnia CS on p636. Up to 10m thick.|1647 +/- 8 Ma (min. crystall'n age).||||Laminated, sandy dolomitic (now tremolite-zoisite-rich) rocks.|
23700|King Gunnia Calc-Silicate Member|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Within the Paragon Group. Included in the dark, planar-layered amphibole-rich rocks of the Paragon Group.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|63519|5|Briefly described|p6 Fig. 2, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments. Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
23700|King Gunnia Calc-Silicate Member|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province||Cartwrights Creek Metasediments||Overlain by the Bijerkerno Metasediments.||
23700|King Gunnia Calc-Silicate Member|64097|5|Briefly described|p303|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments (Paragon Group).||||||07-FEB-11
23700|King Gunnia Calc-Silicate Member|64741|5|Briefly described|p301 Fig. 4, p311|Paleoproterozoic|Paleoproterozoic|Of Cartwrights Creek Metasediments (Paragon Group). Geological province: Broken Hill Domain. Has stratiform-stratabound Zn-dominated mineralisation||||||07-FEB-11
23700|King Gunnia Calc-Silicate Member|64742|6|Mentioned|p321 Fig.3.|||||Unit in Paragon Group.||||
23700|King Gunnia Calc-Silicate Member|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Paragon Group. Geological province: Broken Hill Domain.||||||07-FEB-11
23700|King Gunnia Calc-Silicate Member|66302|5|Briefly described|p36 Fig.9, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain. The rank [Member] is omitted.||Cartwright Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|70000|5|Briefly described|p37|Statherian|Statherian|Mis-spelt as King-Gunnia Calc-silicate Member.||Unit in Cartwrights Creek Metasediments.|||Thinly-bedded unit.|
23700|King Gunnia Calc-Silicate Member|70014|5|Briefly described|Map legend|||||Unit in Cartwrights Creek Metasediments.|||Layered, dark, graphitic, amphibole-rich rock. Layering thin (2-100mm), planar, continuous. Minor quartz and plagioclase-rich layers. Interpreted as a metamorphosed carbonaceous limestone.|
23700|King Gunnia Calc-Silicate Member|70657|5|Briefly described|p13 Fig.6, p15, p42, p65|Statherian|Statherian|Curnamona Province; Broken Hill Domain. Appears as King Gunnia Calc-silicate Member in Fig.6, and as King-gunnia Calc-Silicate Member [!] on p42.||Cartwrights Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Cartwrights Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|71968|5|Briefly described|p5,18,28|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. ||Unit of Cartwrights Creek Metasediments.||||
23700|King Gunnia Calc-Silicate Member|72461|6|Mentioned|p16 fig 9|||||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|73482|5|Briefly described|p422 Fig.3|||Shown as King Gunnia CS Member.||Cartwrights Creek Metasediments||||
23700|King Gunnia Calc-Silicate Member|73575|6|Mentioned|p828 Fig.2, p829 Fig.3|||||Cartwrights Creek Metasediments||||
32272|Kings Cross Formation|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv7||||||
32272|Kings Cross Formation|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
82761|Kings Plains Granodiorite|71628|5|Briefly described|p10: 1, 8-11|||Originally the Kings Plain Granite and included as Kings Plain [sic] Granodiorite in the Boxwell Suite by Blevin (unpublished), who has also reserved the name in ASUD. Renamed the Kings Plains [sic] Granodiorite in this study. Probably named after a local creek. Occurs as two narrow, elongate bodies ~10 km E of Bukkulla.||Kings Plains Suite.||Intrudes the Texas beds. It is bounded by (?intruded) Emmaville Volcanics.|Quartz-poor granodiorite.|
33795|Kings Vale Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Foliated to massive, leucocratic, biotite granite amd aplitic granite, muscovite biotite granite, containing miarolitic cavities. Cut by quartz-pyrite-arsenopyrite-gold veins.||||||
40921|Kingsdale Limestone Member|50234|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Sooley Volcanics (Mount Fairy Group).||||||
40921|Kingsdale Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of De Drack Formation (Mount Fairy Group). Grey, blue-grey to white, massive fossiliferous limestone (including micrite and grainstone) and dolomite, limestone breccia, and laminated to thinly bedded limestone and siltstone.||||||
40921|Kingsdale Limestone Member|68592|2|Defined|p726, p728, p760-1, p774-8, p782, p794|Wenlock|Wenlock|See also p730 Fig.132, p902, p913, p1672, p1888-9. New name. Was included in Towrang Beds by Pickett (1982), and previously mapped as undifferentiated Upper Silurian by Brunker and Offenberg (1970). Type and representative sections provided. Age from fossils: fauna described. Thickness: max 500 m, at type section 370 m; pinches out in northern part. Geomorphic expression: subdued topography commonly located in valleys, irregular karst surface (karst pinnacles), terra rossa soils and residual iron deposits. Depositional environment: calm, very shallow, water. Metamorphism: limestone is recrystallised to marble in places; sub-greenschist facies (anchi zone) from conodont colour alteration index. Geochemistry: unit is reasonably pure, with high lime (CaCO3 >92%) and generally low dolomite (MgCO3 <2%). Stratigraphically continuous and autochthonous limestone distinguishes this unit from other lithologies of De Drack Formation. Was source of lime for agricultural and building purposes. Near equivalent to Lookdown Limestone Member (Cardinal View Formation). Correlates with Bango and Sandhills Creek, Limestone Members.||Unit in De Drack Formation.||Overlies Joppa Siltstone Member. Is conformably overlain by Sooley Volcanic Member. Intruded by Bishopthorpe Dolerite. Is inferred faulted against Covan Creek Formation. See Comments for correlates.|Carbonate sequence: massive and bedded fossiliferous limestone (predominantly biomicrite) and marble, and laminated to thinly bedded limestone, marl, and buff siltstone.|
40921|Kingsdale Limestone Member|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sfdk. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||De Drack Formation||Is overlain by Joppa Siltstone Member and Sooley Volcanics Member|Grey, blue grey and white, massive to bedded, fossiliferous limestone and marble, includes biomicrite and grainstone , dolomite, limestone breccia, calc-arenite and buff siltstone.|
40921|Kingsdale Limestone Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||De Drack Formation|||Grey, blue grey and white, massive to bedded, fossiliferous limestone and marble, includes biomicrite and grainstone , dolomite, limestone breccia, calc-arenite and buff siltstone.|
40921|Kingsdale Limestone Member|70661|6|Mentioned|p36|||||De Drack Formation||||
40921|Kingsdale Limestone Member|71069|6|Mentioned|p25, p137 fig 44, p144, p146, p149-p151|Wenlock|Wenlock|Contains brachiopod fossils that are assigned to the Conchidium sp and Kirkidium sp. Up to 370m thick. Shallow marine depositional environment. Age derived from fossil assemblage. ||De Drack Formation|||Biohermal limestone, marl and shelly beds.|
40921|Kingsdale Limestone Member|71656|5|Briefly described|p13 Fig.2, p28-p29|Wenlock|Wenlock|Contains a macrofauna characteristic of a quite shallow water depositional environment, evidenced by the presence of megalodont bivalves in the Kingsdale Limestone Quarry (near Goulburn).||Near base of De Drack Formation, Mount Fairy Group||Mount Fairy Group. Partially underlies De Drack Formation.|Fossiliferous limestone.|
40921|Kingsdale Limestone Member|71700|5|Briefly described|p14|||Hosts Conchidium sp. ||De Drack Formation||||
30044|Kingsford Formation|22529|6|Mentioned|1|||||||||
30044|Kingsford Formation|22857|4|Described|p476 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of Queens Pinch Group. Arenite, limestone breccia, mudstone. Max. thickness: 250m. Geological Province: Capertee Rise.||||||
30044|Kingsford Formation|23043|5|Briefly described|Map Legend|Pragian|Pragian|of Queens Pinch Group.||||||
30044|Kingsford Formation|23170|2|Defined|p146|Early Devonian|Early Devonian|of Queens Pinch Group. Age; Macrofauna fossil assemblage dated at sulcatus-kindlei Zone age (early to middle Pragian).||||||
30044|Kingsford Formation|23522|5|Briefly described|p251|Devonian|Devonian|||||||
30044|Kingsford Formation|43188|4|Described|p211|Pragian|Lochkovian|Age late Lochkovian to early Pragian. Located north of Ilford. New name of Colquhoun.||||||
82536|Kingsgate Suite|71628|5|Briefly described|p14: 8, 13, 20, 32-33|||||Kingsgate Supersuite.|Kingsgate Syenogranite; Mount Jonblee, Oban River Leucomonzogranites.|||
82127|Kingsgate Supersuite|71628|5|Briefly described|p3:55; p8:93; p14: 1-33; p15: 2, 3,7,11|||See also p15: 24, 27, 31; p17: 7, 12; p19-38. New name, for a small number of leucocratic granites that crop out in the NE portion of the southern New England Orogen (from ~20 km NNE of Guyra to ~20 km S of Tenterfield). Geochemistry briefly summarised. Associated with Mo mineralisation.|||Red Range, Sandy Flat, Glen Garry, Kingsgate, Yellow Gap Suites.||Pale pink to white, fine- to very coarse-grained, equigranular with local marginal inequigranular-porphyritic variants, felsic, fractionated granites. I-type.|
82127|Kingsgate Supersuite|72528|6|Mentioned|p71.|||||||||
82126|Kingsgate Syenogranite|71628|4|Described|p3: 53, 55; p8-92; p11: 16-17, 19;|||See also p14: 1-2, 4, 7-13, 17, 21-23, 26; p15: 12-13, 15. Originally Kingsgate Granite and later Kingsgate Leucogranite. Renamed in this study in light of modal analyses. Has an irregular distribution (described) over c.40 km N-S. Crops out as large tors, minor whalebacks and rock platforms. Geochemistry described. Associated with historically significant Mo-W-Bi mineralisation (described). Hosts Au occurrence. Appears as Kingsgate Monzogranite on p15-14. RELATED UNITS (continued): Is largely enclosed by Glen Garry Microleucosyenogranite, Mount Mitchell and Wards Mistake Monzogranites, and Red Range Microleucogranite.|254.4 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Kingsgate Suite.||Abuts Sara beds and Emmaville Volcanics and partly bounds Mount Jonblee Leucomonzogranite. Intrudes Arranmor Ignimbrite and Dundee Rhyodacite. See COMMENTS for more.|Pink to white, coarse-grained, equigranular, biotite syenogranite, with minor leucosyenogranite; locally greisenous; minor chilled marginal variants and aplite veins. I-type.|
82126|Kingsgate Syenogranite|72528|6|Mentioned|p72, p109.|||Previously included rocks now known as Deepwater Syenogranite.||||||
24337|Kingsland Conglomerate Member|37987|2|Defined|p219|Carboniferous|Carboniferous|||||||
24337|Kingsland Conglomerate Member|38222|6|Mentioned|Fig.2|||||||||
70499|Kingsmill Peak Andesite Member|62095|5|Briefly described|Plate 1|Carboniferous|Carboniferous|Intrudes the Merlewood Formation.||||||01-FEB-07
31707|Kirribilli Formation|13139|5|Briefly described|p9 Fig. 4, p11|||Geological Province: Cowra Trough.||||||
31707|Kirribilli Formation|23334|5|Briefly described|9 Fig.4|Silurian|Ordovician|||||||
31707|Kirribilli Formation|23366|5|Briefly described|p13 fig.8|Ordovician|Ordovician|||||||
31707|Kirribilli Formation|24007|5|Briefly described|p326|Ordovician|Ordovician|||||||
31707|Kirribilli Formation|24215|5|Briefly described|p801|||Geological Province:  Lachlan Fold Belt||||||
31707|Kirribilli Formation|24233|5|Briefly described|p252, p253 Fig.1, p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
31707|Kirribilli Formation|24417|3|Fully described|p30|Late Ordovician|Middle Ordovician|originally named "Kirribilli Beds" by Sherwin et al (1987).||||||
31707|Kirribilli Formation|24600|5|Briefly described|p481|Ordovician|Ordovician|Contains quartz turbidites.  Associated with the Mugincoble Chert.  Geological Province: Lachlan Fold Belt.||||||
31707|Kirribilli Formation|50191|6|Mentioned|p25 Fig. 9|Ordovician|Ordovician|||||||
31707|Kirribilli Formation|50299|5|Briefly described|Map Legend|Ordovician|Ordovician|Siltstone, slate, phyllite and shale.||||||09-JUN-04
31707|Kirribilli Formation|50628|5|Briefly described|Map Legend|Ordovician|Ordovician|Fine to medium grained shale,  siltstone, limonitic sandstone. Intruded by: Cemetery Granite.  Underlies: Grenfell Granite, Warrumba Volcanics.||||||25-MAR-20
31707|Kirribilli Formation|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Metasediments.||||||
31707|Kirribilli Formation|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||13-JUL-04
31707|Kirribilli Formation|60548|5|Briefly described|map legend|Ordovician|Ordovician|Buff, olive green, mauve and light grey shale, carbonaceous in part, siltstone and coarse limonitic sandstone.||||||
31707|Kirribilli Formation|60902|5|Briefly described|p876|Ordovician|Ordovician|Turbidites; spaced cleavage/stripey layering is widespread in parts of this unit.||||||11-APR-06
31707|Kirribilli Formation|63278|6|Mentioned|p151|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt. Ordovician turbidites and cherts. See also p151.||||||07-FEB-11
31707|Kirribilli Formation|63283|6|Mentioned|p183 Fig. 1|||||||||07-FEB-11
31707|Kirribilli Formation|63289|4|Described|p372, p373 Fig. 7, p374|Ordovician|Ordovician|Quartz-rich turbidites. Structural interleaved with Hoskins Chert and Brangan Volcanics. Geological Province: Junee - Narromine Volcanic Belt. See p372374 for detailed structural and lithological information.||||||07-FEB-11
31707|Kirribilli Formation|63290|6|Mentioned|p386 Fig. 1(a), p391, p405|Ordovician|Ordovician|Consists of turbidites and siltstones. Geological Province: Junee - Narromine and Molong Volcanic Belts.||||||
31707|Kirribilli Formation|63291|6|Mentioned|p419 Fig. 2|||||||||
31707|Kirribilli Formation|64963|5|Briefly described|p180 Fig. 1, p185|Ordovician|Ordovician|Includes turbidites. Located between the Goonumbla-Triangle and Molong Volcanic Belts.||||||22-APR-09
31707|Kirribilli Formation|67107|6|Mentioned|p696|||Peak Hill, c.45km N of Parkes.||||||
31707|Kirribilli Formation|67322|5|Briefly described|p20|Silurian|Silurian|Raymond and Wallace, in Lyons et al.(2000). Recent age-dating of zircon grains using LA-ICPMS indicates a probable Silurian age (Quinn et al. unpubl.). Occurs in the Parkes-Forbes-Junee area.||||Possible equivalents are Bribbaree, Bronxhome and Trigalong Formations.|Poorly exposed quartz-rich turbiditic rocks.|22-FEB-18
31707|Kirribilli Formation|67847|4|Described|p4, p19-p25|Ludlow|Wenlock|Macquarie Arc, Lachlan Orogen. Intruded by the Bogolong Suite and the Caragabel Granite. Equivalent to the Bribbaree, Bronxhome, Trigalong and Mumbidgle Formations. ||||Conformably overlies the Brangan Chert. Disconformably overlain by the Ootha and Derriwong Groups.|Graded and massive, fine-grained, quartz-rich turbiditic sandstone interlayered with massive siltstone and shale.|
31707|Kirribilli Formation|68592|5|Briefly described|p10|Early Silurian|Late Ordovician||||||Quartzose sediments.|
31707|Kirribilli Formation|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
31707|Kirribilli Formation|70684|5|Briefly described|p9 Fig.4(h), p14, p54|Early Silurian|Early Silurian|Adaminaby Superterrane.||||Is inferred to be overlain by Mugincoble Chert.|Turbidites.|
31707|Kirribilli Formation|71040|6|Mentioned|p15-18, p25|Ordovician|Ordovician|Central NSW. Multiply-deformed with downward-facing folds and three cleavages. Has been thrust to the E over the Parkes Syncline during the Kanimblan Orogeny.||||||
31707|Kirribilli Formation|72082|6|Mentioned|p22|||Forbes 1:250K sheet area.||||Correlated with Mugincoble Chert.||
31707|Kirribilli Formation|72495|4|Described|p218, p221, 227-229, p231, 233-235|Ordovician|Ordovician|Adaminaby Superterrane, in contact with the Junee-Narromine Volcanic belt on its eastern margin via the Mugincoble fault. Includes rocks previously mapped as part of the Cotton Formation. Generally poorly exposed with a complex internal structure. Bedding is commonly either not apparent in outcrop or highly attenuated, parallel to a moderately to strongly developed cleavage or chlorite-white mica schistosity. Structure is discussed further in detail.|||Includes the Mugincoble Chert.|Faulted over the Goobang Volcanics.|Fine-grained, thinly bedded quartz rich turbidites (thinly to thickly interbedded siltstone, sandstone and shale).|25-MAR-20
27814|Kitchener Formation|22601|6|Mentioned|410|Permian|Permian|Parent Greta Coal Measures. Geol province Sydney Basin. Also known as Greta Seam||||||
27814|Kitchener Formation|22610|5|Briefly described|Fig 1|||Maximum thickness 12m||||||
27814|Kitchener Formation|22969|4|Described|Fig 4.1a||Early Permian|||||||
27814|Kitchener Formation|23540|5|Briefly described|p 419|||Of Greta Coal Measures.||||||20-FEB-07
27814|Kitchener Formation|33867|6|Mentioned|p6|||||||||
27814|Kitchener Formation|34015|4|Described|p325|||Permian||||||
27814|Kitchener Formation|37086|6|Mentioned|p185|||||||||
27814|Kitchener Formation|45090|5|Briefly described|p151|||||||||
27814|Kitchener Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
27814|Kitchener Formation|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Lochinvar area.||Unit in Greta Coal Measures.|Includes Kearsley Lens.|||
26666|Kiwarrak beds|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Hastings Block.||||||16-DEC-04
73373|Knightvale Granite|64681|6|Mentioned|p2|Early Silurian|Early Silurian|||||||
73373|Knightvale Granite|69002|6|Mentioned|p12|Homerian|Sheinwoodian||430 +/- 2.6 Ma, U-Pb SHRIMP|||||
73373|Knightvale Granite|69043|5|Briefly described|p3, p91|Silurian|Silurian|Thomson Orogen.|430.4 +/- 2.6 Ma (Blevin, 2011).||||I-type.|19-JAN-17
73373|Knightvale Granite|69094|5|Briefly described|Map legend|Early Silurian|Early Silurian|Subsurface; shown on time-space plot and pre-Mesozoic geology diagram.|||||Altered biotite-hornblende granodiorite with basalt xenoliths; strongly magnetic.|
73373|Knightvale Granite|70602|6|Mentioned|p67 Fig 3,72|Silurian|Silurian|Age inferred from  map symbol. Aeromagnetic map data given. Grouped with Galambo Granite, Mount Oxley Granite, Glenariff Granite and 3 informal units: Rosses Tank Unit, Brevelon Unit, Mulgawarrina Unit.||||||
73373|Knightvale Granite|70941|4|Described|pviii, pix, p9, p57-60, p70 fig 30|Early Silurian|Early Silurian|Named for Knightvale property. Previously informal name. No outcrop occurs and is only known through drillcore.Metamorphism, geochemistry, geophysical characteristics and structure discussed. Emplacement age. Probably associated with the  Benambran deformation. Contains minor disseminated pyrite and chalcopyrite. See also p114, p140 fig 58, p142, p145, p152.|430.4 +/- 2.6 Ma (SHRIMP, Black 2007)|||Intrudes the Girilambone Group, may correlate witht the Galambo Granite|Altered biotite-hornblende granodiorite with accessory magnetite and basalt xenoliths. Microgabbro and basalt also occurs.|
73373|Knightvale Granite|71345|6|Mentioned|p30|Silurian|Silurian|Similar in age and lithology to Galambo Granite.|c. 430 Ma|||||
73373|Knightvale Granite|71360|5|Briefly described|Map legend|Early Silurian|Early Silurian|Geophysical signature: small irregular features of moderate magnetic intensity within a zone of low magnetic intensity.|430.4 +/- 2.6 Ma.||||Strongly magnetic, altered, biotite-hornblende granodiorite with basic xenoliths. Less magnetic basic rocks with quartz and calcite veining are also present in drillholes.|
73373|Knightvale Granite|72951|5|Briefly described|p1013, 1017, 1022-1023|Wenlock|Wenlock|Lachlan Orogen. Hermidale Terrane. I-type. SHRIMP U-Pb zircon isotope analyses from Black (2007). eHf = 1.8 +/- 1.8, and d18O = 6.70 +/- 0.45.|430.4 +/- 2.6 Ma||||Medium-grained granodiorite.|
39822|Knowles Group|24247|6|Mentioned|p37|Famennian|Frasnian|||||||
27175|Kohinoor Volcanics|12185|5|Briefly described|map legend|Middle Silurian|Middle Silurian|Dacite, tuff, ash flows, agglomerate, minor shale. Underlies Captains Flat Formation. Overlies Copper Creek Shale and Rutledge Quartzite. BMR map symbol: Smk.||||||
27175|Kohinoor Volcanics|22721|6|Mentioned|p505|Late Silurian|Late Silurian|||||||
27175|Kohinoor Volcanics|22768|6|Mentioned|p177|||||||||
27175|Kohinoor Volcanics|22857|4|Described|p177, p474 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of Hoskinstown Group. Overlies the Copper Creek Shale? Max. thickness: 1300m. Geological Province: Captains Flat-Goulburn Trough.||||||
27175|Kohinoor Volcanics|23048|5|Briefly described|p2 fig5||Late Silurian|||||||
27175|Kohinoor Volcanics|23550|5|Briefly described|p504|||Also see Fig 1 p502||||||
27175|Kohinoor Volcanics|24266|5|Briefly described|p1477|Late Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||09-MAR-05
27175|Kohinoor Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
27175|Kohinoor Volcanics|29994|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
27175|Kohinoor Volcanics|30433|4|Described|p696|||||||||
27175|Kohinoor Volcanics|31017|6|Mentioned|p45|||||||||
27175|Kohinoor Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
27175|Kohinoor Volcanics|31020|5|Briefly described|p12|||Aslo mention Fig. 5.||||||
27175|Kohinoor Volcanics|31161|5|Briefly described|PA7|||||||||
27175|Kohinoor Volcanics|31411|5|Briefly described|p18|||||||||
27175|Kohinoor Volcanics|32414|6|Mentioned|p57|||||||||
27175|Kohinoor Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
27175|Kohinoor Volcanics|32672|6|Mentioned|p672|||||||||
27175|Kohinoor Volcanics|32820|6|Mentioned|p3|||Hoskinstown Gp.||||||
27175|Kohinoor Volcanics|33325|5|Briefly described|Table 2|||||||||
27175|Kohinoor Volcanics|34405|4|Described|p108|||||||||
27175|Kohinoor Volcanics|34406|6|Mentioned|p220|||||||||
27175|Kohinoor Volcanics|36413|2|Defined|p59|late Ludlovian|middle Ludlovian|Middle to Late Ludovian||||||
27175|Kohinoor Volcanics|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Of Hoskinstown Group. Underlies Captains Flat Formation and Carwoola Formation; overlies Copper Creek Shale. Rhyolitic to andesitic tuff, minor sediments. GSNSW map code: Sk.||||||
27175|Kohinoor Volcanics|37727|4|Described|p67|||See also P31.||||||
27175|Kohinoor Volcanics|38367|6|Mentioned|p30|||||||||
27175|Kohinoor Volcanics|40328|4|Described|p182|||||||||
27175|Kohinoor Volcanics|42497|5|Briefly described|Map Legend|Ludlovian|Ludlovian|||||||
27175|Kohinoor Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
27175|Kohinoor Volcanics|42727|5|Briefly described|map legend|Ludlow|Ludlow|Of Hoskinstown Group. Rhyodacitic ignimbrite, agglomerate and minor argillaceous sediments. Underlies Captains Flat Formation and Carwoola Formation; overlies Copper Creek Shale. BMR map symbol: Suk. Geol. Prov: Captains Flat Block.||||||
27175|Kohinoor Volcanics|42820|2|Defined|p48|Ludlow||Of Hoskinstown Group. Age inferred.||||||20-MAY-08
27175|Kohinoor Volcanics|46568|14|Not recorded|p.423,427,430|||(I55-16/Michelago). Contains Elliot's & Keating's shale lenses.||||||
27175|Kohinoor Volcanics|48873|14|Not recorded|Pl.1|||(I55-16/Michelago).||||||
27175|Kohinoor Volcanics|48878|2|Defined|p.8||Wenlockian|On many pages. p.1,5,7,11,13,16,17,19,20,22-29,31,38,39,45,47,49,51-55,Pl.1-4. 1200'-2500'. Wenlockian. (I55-16).||||||
27175|Kohinoor Volcanics|68592|5|Briefly described|p743, p803|||Stratigraphic position suggests that Kohinoor Volcanics in Captains Flat area (Davis 1990) is equivalent to at least the upper part of Woodlawn Volcanics.||Hoskinstown Group.||Overlies Copper Creek Shale; perhaps? overlain by Carwoola Formation (though not clearly stated on p743). Suggested equivalent to at least the upper part of Woodlawn Volcanics.|Felsic volcanic pile.|
27175|Kohinoor Volcanics|69270|5|Briefly described|p1, p4, p9, p16, p20, p23, p27, p30|Late Silurian|Late Silurian|Coeval mineralised felsic volcanic units: ~425 Ma Kohinoor Volcanics (Fraser et al., in prep) and ~423 Ma Woodlawn Volcanics (Black, 2006; Bodorkos and Simpson, 2008).|~425 Ma, zircon|Hoskinstown Group||is conformably overlain by Carwoola Formation||
27175|Kohinoor Volcanics|69635|4|Described|p11-17, 19, 21, 39|Pridoli|Wenlock|Eastern Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation age. Age previously based on correlations. Host the Captains Flat VHMS mineralisation.|425.7+/-3.4 Ma|Of Hoskinstown Group.||Overlain by Carwoola Formation. Correlated with Woodlawn Volcanics, Colinton Volcanics.|Green-grey, crystal-rich, medium-grained, porphyritic rhyolite, with plagioclase crystals and lesser quartz, in a microcrystalline groundmass.  Weak chlorite alteration.|
27175|Kohinoor Volcanics|71069|3|Fully described|p9, p21 fig 7, p26-p30, p35|Ludlow|Wenlock|Name derived from the Kohinoor Trigonometrical Station. Incorporates rocks of the discontinued Kohinoor Tuffs and Eastern Massive Fragmentals.  Hosts the Captains Flat VAMS mineralisation. Representative sections for each of the constituent members are proposed. Estimated maximum thickness of 1km. Deep marine depositional setting. Subdivided into four unnamed mappable members: andesite, feldspathic dacite, quartz dacite/rhyolite and volcaniclastic sandstone.Equivalent in part to the Captains Flat Formation, Woodlawn Volcanics, Sooley Volcanic and Wowagin Dacite Members, the Kangaloolah Volcanics and the Bells Creek Volcanics. Distribution, primary structures/textures, geochemistry, geomorphology, tectonic structure, metamorphism and geophysical characteristics are discussed in detail. Lithology discussed in detail. See also p38 fig 15, p39 fig 16, p45, p99, p99 fig 30, p100, p101 fig 31, p101, p102-103 fig 32, p105-p110, p113 oh 30, p115, p117, p119, p124-132, p154.|424.9 +/- 2.9 Ma (SHRIMP U-Pb)|Hoskinstown Group||Overlies the Harrisons Peak Granite. Overlain by the Sinclair Conglomerate Member. Interbedded conformably with the Captains Flat Formation.|Autobrecciated coherent dacitic, andesite and rhyolite lavas that are interbedded with massive to graded beds of polymictic volcanic conglomerate, sandstone, shale, siltstone and breccia.|
27175|Kohinoor Volcanics|71691|5|Briefly described|Map legend.|Silurian|Silurian|Four un-named facies are mapped separately.||Hoskinstown Group.||Is interbedded with/enclosed by Captains Flat Formation.|Coherent andesite, dacite, minor rhyolite and autoclastic breccia, interfingering/interbedded with volcanogenic sandstone to cobble conglomerate.|
27175|Kohinoor Volcanics|71700|5|Briefly described|p14|||Captains Flat map sheet area.||Hoskinstown Group||||
69888|Komungla Rhyolite Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Cream vesicular quartz-feldspar-phyric rhyolite, miarolitic quartz-feldspar-phyric micrographic rhyolite and aplite intrusive.||||||
69888|Komungla Rhyolite Member|68592|2|Defined|p851-4, p859, p861, p863, p868, p880-3|Lochkovian|Pridoli|See also p726, p739, p744, p816, p821, p827. New name. Porphyritic rhyolite in Komungla area was noted on first edition Goulburn 1:250 000 map sheet (Brunker and Offenberg 1970) and Goulburn metallogenic map sheet (Felton 1974). Massive rhyolitic units (Komungla Rhyolite Member), possibly sills or domes, occur within sedimentary rocks of Boxers Creek Formation; their nature and extent remains uncertain owing to poor outcrop. Type localities provided, though top not exposed. Thickness: western body ~1580 m; smaller bodies <~900 m. Sub-greenschist facies metamorphism.||Unit in Gundary Volcanics.||Intrudes(?) or is conformable with Covan Creek Formation and Boxers Creek Formation.|Inferred to be intrusive; high level intrusions consisting of homogeneous, sparsely porphyritic rhyolite; leucocratic, crystal-poor rhyolite in heavily recrystallised groundmass; also quartz-feldspar-phyric aplite.|20-SEP-16
69888|Komungla Rhyolite Member|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfgk. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Gundary Volcanics||Over and underlain by Back Station Ignimbrite Member.|Cream, vesicular, crystal poor, quartz-feldspar phyric rhyolite, with spherulites, sparse vesicles and miarolitic cavities.|
69888|Komungla Rhyolite Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Gundary Volcanics|||Cream, vesicular, crystal poor, quartz-feldspar phyric rhyolite, with spherulites, sparse vesicles and miarolitic cavities.|
69888|Komungla Rhyolite Member|71069|6|Mentioned|p140 tbl 4, p170|||||||Intrudes the Covan Creek Formation.||
69888|Komungla Rhyolite Member|71700|5|Briefly described|CD|||Recognised in the Braidwood100 sheet area.||Gundary Volcanics||||
37354|Koo-Lee Tuff Member|71542|4|Described|p23, 25, 28, 30-32, 34, 35|Late Permian|Late Permian|Of southern Sydney Basin. Type location: Eastern side of Mount Coolangatta at 120m elevation (56/291250E, 6141300N). Thickness: 2m. Interpreted to occur 85m from the base of, and within the Westley Park Sandstone Member. Named for the property of Koo-Lee on which it occurs. Contains the Permian Warthia stricta shelly marine gastropod, indicating emplacement in a shallow marine environment proximal to the source, probably by flow mechanism or as primary air-fall ash. Contains flat, slightly curved, platy, glass shards, suggestive of a phreatomagmatic Vulcanian, Plinian or Surtseyan eruption to the S or SE.See also Facies 6 description p 27-28. Also written as Koo Lee Tuff Member p30 and p34.||Unit of Gerringong Volcanics.||Within Westley Park Sandstone Member, Broughton Formation.|Slightly fossiliferous pyroclastic vitric tuff. Volcanic ash deposit including chaotic glass shards in a cryptocrystalline vitreous matrix.|20-OCT-21
37354|Koo-Lee Tuff Member|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanic Complex.|||Shoshonitic.|
28651|Koogah Formation|23350|5|Briefly described|264|||||||||
28651|Koogah Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28651|Koogah Formation|31880|6|Mentioned|p18|||||||||
28651|Koogah Formation|31881|4|Described|p329|||Permian Equiv. Greta C. M.||||||
28651|Koogah Formation|31882|5|Briefly described|p244|||||||||
28651|Koogah Formation|32482|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
28651|Koogah Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
28651|Koogah Formation|35065|5|Briefly described|p44|||||||||
28651|Koogah Formation|36940|6|Mentioned|p141|||||||||
28651|Koogah Formation|37087|6|Mentioned|p194|||||||||
28651|Koogah Formation|37558|6|Mentioned|p998|||||||||
28651|Koogah Formation|39331|6|Mentioned|Table 10-1|||||||||
28651|Koogah Formation|39569|6|Mentioned|p95|||||||||
28651|Koogah Formation|39664|6|Mentioned|p115|||||||||
28651|Koogah Formation|41264|6|Mentioned|p251|||Recently Leard Formation||||||
28651|Koogah Formation|41348|5|Briefly described|Map legend|Permian|Permian|Geological Province: Sydney-Bowen (Gunnedah ) Basin.||||||16-DEC-04
28651|Koogah Formation|43407|14|Not recorded|Map Legend||Early Permian|(Provisional Edition)||||||
28651|Koogah Formation|43417|4|Described|Map Legend||Permian|Equivalent of Greta Coal Measures||||||
28651|Koogah Formation|47056|6|Mentioned|Fig.2 P523|||||||||
28651|Koogah Formation|68003|5|Briefly described|p38 Fig.3-j, p40, p130.|Early Permian|Early Permian|Werrie Basin (South), Brigalow Belt South Bioregion. Coeval with Willow Tree Formation in the north of the Basin; and correlative of Bellata Group (Gunnedah Basin) and Greta Coal Measures (Hunter Coalfield).||||Overlies Werrie Basalt. Is overlain by Bickham Formation.|Coals, carbonaceous shales and sandstones.|
28651|Koogah Formation|68006|5|Briefly described|p39, pp93-94, pp127-128.|Permian|Permian|Southern Werrie Basin. Coal was extracted from the lowest of seven seams in this unit, until the mine closed in the 1930s. Contains seven potentially economic, export quality thermal coal seams. Also contains kaolinitic clays, partly calcinised by Burning Mountain burning coal seams; used in refractories.||||||
28651|Koogah Formation|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Early Permian coal measures: conglomerate, lithic sandstone, siltstone, claystone, carbonaceous claystone and coal.||||||
28651|Koogah Formation|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
38287|Kookabookra Monzogranite|23811|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Hillgrove Plutonic Suite.  Foliated, coarse-grained, slightly porphyritic biotite monzogranite, with metasedimentary enclaves, rare hornblende-rich enclaves and leucocratic phases.||||||20-DEC-04
38287|Kookabookra Monzogranite|23812|5|Briefly described|p14|Early Permian|Early Permian|Of Hillgrove Plutonic Suite.||||||
38287|Kookabookra Monzogranite|60079|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Hillgrove Suite.||||||
38287|Kookabookra Monzogranite|69639|6|Mentioned|p217|Sakmarian|Sakmarian||292 +/- 3 Ma (SHRIMP U-Pb)|Hillgrove Supersuite||||
38287|Kookabookra Monzogranite|71628|4|Described|p2:41; p3:1, 4, 10,70-74; p8:92; p14:17|||See also p19:12. Henley et al. (2001); formerly Kookabookra Adamellite (Binns, 1966). Named after the locality. Crops out over 120 km2, about 42 km SE of Glen Innes and a similar distance NE of Guyra. Affected by the Wongwibinda Fault (discussed). Geochemistry described in some detail. Associated with numerous vein-hosted Au deposits.|292 +/- 3 Ma (SHRIMP: Rosenbaum et al., 2012).|Kookabookra Suite.||Intrudes Rampsbeck Schists, Sara beds and Dyamberin beds (and faulted against this last). Is intruded by Black Knob and Wards Mistake Monzogranites and ?Oban River Leucomonzogranite.|Coarse-grained, weakly porphyritic biotite monzogranite with minor granodiorite; locally amphibole and, independently, garnet bearing; variably but typically mildly foliated.|
27176|Koolanock Sandstone|22601|6|Mentioned|407|Early Permian|Early Permian|||||||
27176|Koolanock Sandstone|22736|6|Mentioned|p629|Namurian|Visean|||||||
27176|Koolanock Sandstone|22857|4|Described|p512 App.1 Tb.A1.8|Westphalian|Westphalian|Upper, middle and lower sequences of spherulitic rhyolite volcanics, plant-bearing lithic arenite with devitrified rhyolite units and thick lithic arenite interbedded with thin bioturbated siltstone respectively. Max. thickness: >1500m. ||||||
27176|Koolanock Sandstone|23157|5|Briefly described|p110,115 fig2,7,8|||||||||
27176|Koolanock Sandstone|32868|6|Mentioned|p210|||||||||
27176|Koolanock Sandstone|36057|2|Defined|p349|Early Permian|Late Carboniferous|Late Carboniferous or Early Permian||||||
27176|Koolanock Sandstone|36528|6|Mentioned|p182|||||||||
27176|Koolanock Sandstone|38801|6|Mentioned|Fig.3|||||||||
27176|Koolanock Sandstone|39660|6|Mentioned|p450|||||||||
27176|Koolanock Sandstone|40883|6|Mentioned|p8|||||||||
27176|Koolanock Sandstone|42547|4|Described|p37|||||||||
27176|Koolanock Sandstone|42833|4|Described|p225|||||||||
27176|Koolanock Sandstone|43017|5|Briefly described|Fig.1,p372|||||||||
27176|Koolanock Sandstone|44093|5|Briefly described|p231 App. 1|Early Permian|Late Carboniferous|Geological Province: New England Fold Belt.||||||
27176|Koolanock Sandstone|44244|2|Defined|p216, p207 Fig. 41|Westphalian|Westphalian|Overlies Yagon Siltstone; underlies Muirs Creek Conglomerate.  Max. thickness: 1625m.  Geological Province: Myall Block.  Type section in text.||||||10-MAY-13
27176|Koolanock Sandstone|47056|6|Mentioned|Fig.2 P523|||||||||
27176|Koolanock Sandstone|50132|5|Briefly described|p248  Fig.6|||Early Namurian age||||Overlies the Yagon Siltstone.||
27176|Koolanock Sandstone|50263|5|Briefly described|Map Legend|Westphalian|Westphalian|Overlies: Yagon Siltstone.  Underlies: Muirs Creek Conglomerate.  Geological Province: Eastern Myall Block.||||||
27176|Koolanock Sandstone|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Serpukhovian|Myall Block, Tamworth Belt.||||||
24342|Koonburra Creek Quartzite Member|22857|5|Briefly described|p436 App 1, Tb.A1.6|||Pale-red coarse- to medium-grained arenite. Max. thickness: 75m. ||||||
24342|Koonburra Creek Quartzite Member|23336|5|Briefly described|p8 Fig. 5, p13|||Of the Mount Daubeny Formation. Max. thickness: 75m.||||||21-MAR-06
24342|Koonburra Creek Quartzite Member|42121|2|Defined|p102|Ordovician||||||||
24342|Koonburra Creek Quartzite Member|42298|6|Mentioned|p29|||||||||
24342|Koonburra Creek Quartzite Member|42364|5|Briefly described|p205|||See also Koonburra Creek Quartzite||||||
24342|Koonburra Creek Quartzite Member|61213|5|Briefly described|p320, p323 Fig. B|||Of the Mount Daubeny Formation. Geological Province: Darling Basin.||||||
24342|Koonburra Creek Quartzite Member|64671|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of Mount Daubeny Formation.  Polymictic basal conglomerate with a range of local and foreign clasts. Horizon of boulders and rafts of Mootwingee Group sandstones and quartzites near base.||||||01-DEC-08
24342|Koonburra Creek Quartzite Member|64680|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Mount Daubeny Formation.||||||01-DEC-08
24342|Koonburra Creek Quartzite Member|64682|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Mount Daubeny Formation.||||||
24342|Koonburra Creek Quartzite Member|66623|1|Redefined|p161, pp184-185. |Late Silurian|Late Silurian|Formerly Koonburra Creek Quartzite (Neef and Bottrill 1991), Koonburra Quartzite (Neef et al. 1996); formally redefined in this study. Southern margin of Mount Daubeny Basin. Possibly a fine-grained distal equivalent of Gnaltaknoko Member conglomerates. Forms a prominent 100m wide ridge for 12 km. Typically 14-36 m thick. No fossils identified. Deposited in sand-bed braided streams flowing to the southwest.||Basal unit in Mount Daubeny Formation.||Unconformably overlies Kara Formation and Wonnaminta Formation. Is overlain by undifferentiated beds of Mount Daubeny Formation.|Grey, fine-grained, commonly tabular cross-stratified, orthoquartzite; rare small clasts of vein quartz; very rare clasts of red arenite.|
24342|Koonburra Creek Quartzite Member|66929|6|Mentioned|Map legend|||||Unit in Mount Daubeny Formation.||||
24342|Koonburra Creek Quartzite Member|70037|5|Briefly described|p309 Fig.2, p311|||Darling Basin. Forms prominent exposures.||Basal Mount Daubeny Formation.||Distal equivalent to the Gnaltaknoko Member (in the N of the Basin).|A basal quartzite horizon.|
24342|Koonburra Creek Quartzite Member|70651|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Daubeny Formation|||Fine grained, commonly tabular cross-stratified quartzite.|
22128|Koonenberry Formation|66623|1|Redefined|pp74-75, p80 Fig. 21, pp92-93. |Middle Cambrian|Middle Cambrian|Redefined; formerly part of Wonominta beds (Warris 1967), then Koonenberry beds (Stevens et al. 2000). About 200 m thick. No fossils identified. Hosts the VMS style Ponto Copper Mine; syngenetic and stratiform mineralisation. Consistently magnetic along strike length due to magnetite-bearing basaltic tuffs.||Unit in Ponto Group.||Conformably overlies Noonthorangee Formation. Is conformably overlain by Yandenberry Formation.|Green and green-grey phyllite, metasiltstone and metasandstone; tholeiitic pillow lavas, basaltic flows, basalt and dolerite sills; basalts are trachytic to latitic and plagioclase-phyric; red-brown to black, very fine-grained quartz-magnetite rock.|24-SEP-13
22128|Koonenberry Formation|67322|5|Briefly described|p11; Fig.5|Cambrian|Cambrian|Age determined from p20 Fig.5 (Strat. column) where it appears as Koonenberry Fm.  - not well constrained. Occurs in the Kayrunnera-Koonenberry region.||Of the Ponto Group.||Overlies Noonthorangee Formation. Is overlain by Yandenberry Formation.|Green phyllites with minor basaltic flows, tuffaceous and quartz-magnetite rocks.|22-FEB-18
22128|Koonenberry Formation|69961|5|Briefly described|Map legend|Cambrian|Cambrian|The two facies assemblages are mapped separately.||Unit in Ponto Group.|||Green and grey metamudstone (phyllite), metasiltstone and metasandstone, dolerite sills, tholeiitic and pillow basalts, basaltic tuff and thin quartz-magnetite horizons; red-brown to black, well banded/laminated to massive quartz and magnetite rock.|
22128|Koonenberry Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|||Ponto Group|||Magnetic and non-magnetic green and green-grey metamudstone (phyllite), metasiltstone and metasandstone, dolerite sills, tholeiitic basalt, pillow basalt, basaltic tuff and thin quartz-magnetite horizons.|
80932|Kooranjie Conglomerate|70751|6|Mentioned|p12|Pridoli|Pridoli|||Possibly a member of Mount Knobby Formation?||||16-MAR-19
80932|Kooranjie Conglomerate|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Of Mount Knobby Formation?||Partly overlain by and equivalent to Mount Knobby Formation[?].||
37902|Kooringal Dacite Member|24605|2|Defined|p931, p948 App. 1|Visean|Visean|Of the Caroda Formation. Maximum Thickness: 50m. Geological Province: New England Orogen.||||||
37902|Kooringal Dacite Member|61214|5|Briefly described|p171 Fig. 1|Carboniferous|Carboniferous|||||||
72565|Kooringaroo Group|68592|5|Briefly described|p1840, p1846|Cenozoic|Cenozoic|Nott (1992). Near Bungonia.|||||Undifferentiated alluvium; includes sand, clay and conglomerate; locally ferruginous; variably consolidated.|
28654|Kopyje Group|730|5|Briefly described|p23 - p24.|Early Devonian|Early Devonian|Cobar Sub-basin, Darling Basin. Of Cobar Supergroup. Fringing, shallow-water facies. Lochkovian to mid Pragian. Inferred faulted against Amphitheatre Group to the west, and unconformably overlies Girilambone Group to the east. Includes Meryula Formation.||||||11-NOV-14
28654|Kopyje Group|9548|5|Briefly described|Map Legend|Pragian|Lochkovian|Includes: Baledmund Formation, Majuba Volcanics.||||||06-JUL-04
28654|Kopyje Group|22768|5|Briefly described|p171|Lochkovian|Pridoli|||||||
28654|Kopyje Group|22831|4|Described|p 38|Lochkovian|Pridolian|Of the Cobar Supergroup.||||||12-APR-07
28654|Kopyje Group|22857|5|Briefly described|p171, p442 App.1, Tb.A1.6|Early Devonian|Late Silurian|Of the Cobar Supergroup. Unconformably overlain by Yarra Yarra Creek Group. Max. thickness: 2km. Geological Province: Kopyje Shelf (Darling Basin). See also p444 App.1, Tb.A1.6.||||||12-APR-07
28654|Kopyje Group|23096|6|Mentioned|p601 (Fig 1)|||Cobar Supergroup||||||
28654|Kopyje Group|23171|5|Briefly described|p13,22,31,Fig15p45||Lochkovian|||||||
28654|Kopyje Group|23173|4|Described|Map Legend|||||||||
28654|Kopyje Group|23309|6|Mentioned|p390|||||||||
28654|Kopyje Group|23522|5|Briefly described|p249 Fig 5|Lochkovian|Ludlow|||||||
28654|Kopyje Group|23734|5|Briefly described|p12 Fig. 1|||Shelf sediments of sandstone and limestone.||||||
28654|Kopyje Group|35287|6|Mentioned|p6|||||||||
28654|Kopyje Group|38292|6|Mentioned|p3|||||||||
28654|Kopyje Group|39083|6|Mentioned|Fig.1|||||||||
28654|Kopyje Group|39618|3|Fully described|p40|||||||||
28654|Kopyje Group|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
28654|Kopyje Group|41138|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
28654|Kopyje Group|41394|6|Mentioned|p10|||||||||
28654|Kopyje Group|41410|5|Briefly described|p295|||||||||
28654|Kopyje Group|41528|2|Defined|p35|Early Devonian||||||||
28654|Kopyje Group|41529|6|Mentioned|Map legend|Early Devonian||||||||
28654|Kopyje Group|41821|6|Mentioned|p11 Fig.5|||Occurs Cobar, Wrightville, Canbelego, Nymagee, Bobadah, Gindoono sheet areas||||||
28654|Kopyje Group|41872|6|Mentioned|p8|||||||||
28654|Kopyje Group|42144|5|Briefly described|p604|||||||||
28654|Kopyje Group|42172|6|Mentioned|Fig.5 P167|||||||||
28654|Kopyje Group|42208|6|Mentioned|Fig.1 P304|||||||||
28654|Kopyje Group|42521|5|Briefly described|Fig.1 P14|||||||||
28654|Kopyje Group|42566|3|Fully described|p47|||||||||
28654|Kopyje Group|42568|5|Briefly described|Map legend|Pragian|Late Silurian|||||||
28654|Kopyje Group|42907|6|Mentioned|Fig.8, P8|||||||||
28654|Kopyje Group|42983|6|Mentioned|Fig.3,p345|||||||||
28654|Kopyje Group|43032|3|Fully described|p27|||Of the Cobar Supergroup.||||||12-APR-07
28654|Kopyje Group|43089|5|Briefly described|Map Legend|||Of the Cobar Supergroup.||||||12-APR-07
28654|Kopyje Group|43090|5|Briefly described|Map legend|Pragian|Lochkovian|Of the Cobar Supergroup.||||||12-APR-07
28654|Kopyje Group|43153|5|Briefly described|Map Legend||Lochkovian|||||||
28654|Kopyje Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
28654|Kopyje Group|43441|4|Described|20,24|Early Devonian|Late Silurian|||||||08-JAN-10
28654|Kopyje Group|43757|6|Mentioned|p510|||||||||
28654|Kopyje Group|43774|3|Fully described|p18-19||Devonian|||||||
28654|Kopyje Group|44093|5|Briefly described|p172 App. 1|Early Devonian|Late Silurian|In the Mineral Hill Zone. Geological Province: Lachlan Fold Belt.||||||
28654|Kopyje Group|44160|5|Briefly described|Map Legend|Lochkovian|Pridolian|||||||
28654|Kopyje Group|46900|5|Briefly described|p16|||Tectonics||||||
28654|Kopyje Group|63185|6|Mentioned|p3|Early Devonian|Late Silurian|Of the Cobar Supergroup. Includes polymictic conglomerates with lithic sandstone and minor siltstone.||||||12-APR-07
28654|Kopyje Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
28654|Kopyje Group|65469|5|Briefly described|p15, p43, p52, p55 fig 3-19|Early Devonian|Late Silurian|Lachlan Orogen. See also p62, p67, p133, p136, p139, p144, p145, p146, p335, p345, p355, p356, p366, p368, App A-VI 3.|||Includes the Meryula Formation, Florida Volcanics, Badinda Volcanics and the Baledmund Formation.|Unconformably overlies the Nymagee Igneous Complex.||
28654|Kopyje Group|66197|5|Briefly described|p634, p635 Fig.5a|Lochkovian|Pridoli|Jemalong Trough.||||Is overlain unconformably by Yarra Yarra Creek Group.|Includes silicic volcanics and volcaniclastics, shallow marine clastics; basal conglomerate.|14-MAR-12
28654|Kopyje Group|67416|6|Mentioned|p83-86|||Pogson and Felton (1978, in Pogson, 1991), who upgraded the previous Kopyje Beds of Brunker (1969, in Pogson, 1991). Included all the sedimentary and volcanic rocks on the Kopyje Shelf, eastern Cobar Basin. Assigned to Cobar Supergroup by Pogson and Felton (1978).||Cobar Supergroup.|Babinda, Majuba Volcanics; Baledmund Formation.|Equivalent to Mineral Hill Volcanics.||
28654|Kopyje Group|68823|5|Briefly described|p377, p378 Fig.4|Lochkovian|Ludlow|Deposited on the Kopyje Shelf. Coeval in its upper part with the Winduck Group.||Of the Cobar Supergroup|Includes Brookong and Meryula Formations.|Disconformably to paraconformably overlain by the Mulga Downs Group.||
28654|Kopyje Group|69002|6|Mentioned|Map 1b, Legend|Early Devonian|Late Silurian|Non-magnetic.|||||Sediments.|
28654|Kopyje Group|69042|6|Mentioned|map legends|Early Devonian|Late Silurian|Dck. Lachlan Orogen. Non-magnetic sediments.||||||
28654|Kopyje Group|69043|6|Mentioned|p11|Early Devonian|Late Silurian|||||||
28654|Kopyje Group|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Cobar Supergroup.|Includes Coronga Peak Quartzite and Meryula Formation.|||
28654|Kopyje Group|69095|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Cobar Supergroup.|Includes Coronga Peak Quartzite and Meryula Formation.|||
28654|Kopyje Group|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Late Silurian|Lachlan Orogen.||||||
28654|Kopyje Group|69635|5|Briefly described|p75, 105|Early Devonian|Late Silurian|||Of Cobar Supergoup.|Includes Coronga Peak Quartzite.|||
28654|Kopyje Group|69801|6|Mentioned|p1, p11|||Cobar Basin, Central Lachlan Orogen.||Cobar Supergroup|Includes the Baledmund Formation.|||
28654|Kopyje Group|70602|6|Mentioned|p67 Fig 3|Devonian|Devonian|||Cobar Supergroup||||
28654|Kopyje Group|70751|5|Briefly described|p1, p4-p6, p12, p15, p17, p21, p31|Devonian|Late Silurian|Cobar Superbasin, Kopyje Shelf.||Cobar Supergroup|Includes the Florida Volcanics, Baledmund Formation, Talingaboolba Formation, Babinda Volcanics, Majuba Volcanics and Mineral Hill Volcanics.|||
28654|Kopyje Group|70821|6|Mentioned|p11|Early Devonian|Late Silurian|Shelf facies. Typically non-magnetic.||||||
28654|Kopyje Group|70876|5|Briefly described|p1, p9, p76|||Lachlan Orogen. Deposited in a shallow marine environment.||Cobar Supergroup|Includes the Babinda Volcanics, Florida Volcanics, Majuba Volcanics and the Mineral Hill Volcanics.|||
28654|Kopyje Group|70941|3|Fully described|pviii, p4, p7 fig 3,|Early Devonian|Late Silurian|Named after Kopyje property. Contains rocks that belonged to the former Kopyje Beds and the Mallee Tank Beds.  Geomorphology, structute, metamorphism, geophysical characteristics, distinguishing features and fossil assemblage discussed. Maximum thickness of 1100m (based on Meryula Formation). Deposited in a near to shallow marine environment. Minor gold and base metal mineralisation is associated with this group. See also  p8 fig 4, p76, p77 fig 31,  p79-p81, p94, p122, p125, p126, p128 fig 55, p135, p136, p140 fig 58, p147.||Cobar Supergroup|Meryula Formation, Coronga Peak Quartzite|Unconformably overlies Girilambone Group||
28654|Kopyje Group|70950|5|Briefly described|p1028,1030,1033-1034,1044|Early Devonian|Silurian|Geological province: Kopyje, Shelf, Central Lachlan Orogen. Constituent volcanic units form the Canbelego Mineral Hill Volcanic Belt.|||Includes the Babinda Volcanics, Majuba Volcanics and Mineral Hill Volcanics.||Felsic volcanics, siltstone, limestone|
28654|Kopyje Group|71039|5|Briefly described|p6-p7, p10-p13, p24, p26, p28|Devonian|Silurian||||Includes the Florida Volcanics, Baledmund Formation, Babinda Volcanics, Meryula Formation, Coronga Peak Quartzite and the Majuba Volcanics.|Intruded by the Mount Walton Porphyry and the Yellow Mountain Granite.||
28654|Kopyje Group|71040|5|Briefly described|p9, p11, p12 Fig.7, p13, p19|Early Devonian|Late Silurian|N and NW of Condobolin, NSW. Deformation associated with Bindian (= Bowning) Orogeny described.||||Is overlain unconformably by Yarra Yarra Creek Group.||
28654|Kopyje Group|71285|5|Briefly described|p538-539|Early Devonian|Late Silurian|Cobar region.|||Meryula Formation.|||
28654|Kopyje Group|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Cobar Supergroup.|"Stony Tank Formation", Meryula Formation, Coronga Peak Quartzite.|||
28654|Kopyje Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|Talingaboolba, Brookong, Mount Knobby, Meryula, Baledmund Formations; Majuba, Mineral Hill, Florida, Babinda Volcanics; Harts Tank beds; Mount Susannah Conglomerate.|||
28654|Kopyje Group|71860|6|Mentioned|p6|Early Devonian|Late Silurian|||||||
28654|Kopyje Group|72080|5|Briefly described|p4-5, p6, p8-9, p13|Early Devonian|Late Silurian|Only Harts Tank area discussed.||Lowest part of Cobar Supergroup in area.|Includes the Baledmund Formation, Babinda Volcanics and the Harts Tank beds.|||07-JAN-22
28654|Kopyje Group|72296|5|Briefly described|p6|Devonian|Late Silurian|||Cobar Supergroup.||Unconformably overlies Girilambone Group.||
28654|Kopyje Group|72908|5|Briefly described|p4-5, p21, p23-24|Early Devonian|Silurian|Kopyje Shelf, Canbelego-Mineral Volcanic Belt.|||Badinda Volcanics, Majuba Volcanics, Mineral Hill Volcanics||Contains felsic-dominated volcanic units, and fine-grained terrigenous to shallow-marine sedimentary rocks.|
28654|Kopyje Group|72958|6|Mentioned|p5-6, p8-9, p11, p45, p52, p61|||Flanks the Cobar Basin. Nymagee area.|||Includes Meryula Formation.|Underlain by Girilambone Group.|Limestone-bearing shelf sequences.|
28654|Kopyje Group|73019|5|Briefly described|p429, 433|Early Devonian|Early Devonian|Glen (1994). Cobar Basin.||||Is overlain by the Amphitheatre Group.|Basal rift sequence of boulder conglomerate and massive sandstone, platform and reef limestone, back reef facies, and clastic open shelf sediments.|
28654|Kopyje Group|73143|5|Briefly described|p1-4, p8-9, p20|Lochkovian|Pridoli|Lachlan Orogen. Cobar Superbasin, northern. Shallow marine shelf sequence, deposited synchronously with extensive volcanism.|422-417 Ma||Brookong Formation, Meryula Formation||Includes volcanic units, limestone in uppermost part.|
28654|Kopyje Group|73174|5|Briefly described|p1035, p1037-1038|Lochkovian|Lochkovian|Cobar Basin, east [of Rookery Fault].||Cobar Supergroup||Underlain by Girilambone Beds [Group].|Limestone, shallow water siliciclastic sediments and locally distributed volcaniclastic sediments.|
28654|Kopyje Group|73578|6|Mentioned|p2|||Cobar Basin.||||||
24343|Koreelah Conglomerate Member|22857|5|Briefly described|p319 Fig.22.10B, p548 App.1 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Gatton Sandstone (Marburg Subgroup (Bundamba Group). Pebble to cobble conglomerate, sandstone. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin.||||||
24343|Koreelah Conglomerate Member|22865|6|Mentioned|Fig22.10bp319|||||||||
24343|Koreelah Conglomerate Member|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
24343|Koreelah Conglomerate Member|42248|2|Defined|App.1 p413||Triassic|||||||04-JAN-17
24343|Koreelah Conglomerate Member|42463|6|Mentioned|Fig.3 P170|||||||||
24343|Koreelah Conglomerate Member|43150|5|Briefly described|Map Legend|Jurassic||Of the Gatton Sandstone (Marburg Subgroup, Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||12-APR-05
24343|Koreelah Conglomerate Member|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
24343|Koreelah Conglomerate Member|60993|5|Briefly described|p6 Fig. 2, p18|||Of the Gatton Sandstone (Marburg Subgroup, Bundamba Group). Polymictic conglomerate in basal part of unit. Overlies Woogaroo Subgroup units. Geological Province: Clarence-Moreton Basin.||||||
24343|Koreelah Conglomerate Member|60995|4|Described|p65, p51 Fig. 3|Early Jurassic|Early Jurassic|Of Gatton Sandstone. Significant pebble-cobble conglomerate occurring in the coarse, lithic and quartz-lithic sandstones of the parent unit. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin. ||||||
24343|Koreelah Conglomerate Member|60996|5|Briefly described|p95|||Of Gatton Sandstone (Marburg Subgroup). Patches of conglomerate, sandstone and mudstone equivalent to the parent sandstone. Geological Province: Clarence-Moreton Basin.||||||
24343|Koreelah Conglomerate Member|60997|5|Briefly described|p140|||Of the Gatton Sandstone. Geological Province: Clarence-Moreton Basin. ||||||
24343|Koreelah Conglomerate Member|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Gatton Sandstone (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
24343|Koreelah Conglomerate Member|61310|5|Briefly described|Table C1 (p22-23)|Early Jurassic|Late Triassic|Of the Gatton Formation. Pebble to cobble conglomerate, sandstone. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin||||||
24343|Koreelah Conglomerate Member|63731|5|Briefly described|Map legend|Jurassic|Jurassic|Of the Gatton Sandstone (Marburg Subgroup).  Massive, polymictic, pebble to cobble conglomerate; coarse-grained sandstone.||||||
24343|Koreelah Conglomerate Member|63748|4|Described|p21-22|Early Jurassic|Early Jurassic|Grades eastwards into Gatton Sandstone (Marburg Subgroup from western margin of the Clarence-Moreton Basin. Massive to crudely-bedded, clast-supported, ploymictic, pebble to cobble conglom., massive matrix-supported sandy conglom. + thick-bedded sandstone||||||07-FEB-11
24343|Koreelah Conglomerate Member|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
24343|Koreelah Conglomerate Member|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Gatton Sandstone.||Overlies Ripley Road Sandstone.||
24343|Koreelah Conglomerate Member|71628|5|Briefly described|p16: 4,23; p19-24|||||Marburg Subgroup.||Overlies Wylie Creek Monzogranite Phase (Cullendore Syenogranite). May overlie Cullens Creek Granodiorite.||
24343|Koreelah Conglomerate Member|72528|5|Briefly described|p90.|Jurassic|Jurassic|||Bundamba Group||Unconformably overlies Cullens Creek Granite.||
67848|Koreelah Creek Granodiorite|71628|3|Fully described|p9: 1-3; p16: 4, 29-31; p19: 23-24,|||See also p19: 89-95, 174. Brown et al., (2001). Was included as (mis-spelled) Koreelan Creek Granodiorite in the Clarence River Plutonic Suite of Shaw and Flood (1981), and in a number of other publications. Renamed Koreelah Creek Granodiorite in this study to reflect the correct spelling of the watercourse. Occurs ~20 km E to NE of Liston. The type locality is excellently exposed at GR 320332, Drake 1:100,000 Geological Sheet (Thomson, 1976). Comprises four bodies. Was excluded from the Clarence River Supersuite by Brown et al. (2007). Lithologies and mineralogy described in considerable detail. Geochemistry detailed. Is spatially associated with historically significant Ag-Zn-Pb-As-Cu-Sb-Sn-Au (fissure vein) mineralisation, likely sourced from Rivertree Syenogranite.|246.3 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Koreelah Creek Suite.||Intrudes Emu Creek Formation, Drake Volcanics, Razorback Creek Mudstone. Intrusive relationship with Rivertree Syenogranite is equivocal. Is faulted against Cullendore Syenogranite.|Mottled grey and white, fine- to medium-grained, equigranular to seriate, hornblende-biotite-(pyroxene) granodiorite to quartz diorite and quartz monzodiorite, with minor tonalite and monzogranite; local porphyritic and foliated variants. I-type.|
72792|Koringaroo Group|62740|5|Briefly described|p364|Oligocene||Probably misspelt -probably should be Kooringaroo? Comprises three subgroups: Nadgigomar, Nerriga and Badgerys Sub-Groups. Age stated to be pre-Eocene to Middle Oligocene.||||||06-FEB-07
27815|Kotara Formation|22578|6|Mentioned|p401|||||||||
27815|Kotara Formation|23055|6|Mentioned|Fig5p12,15,18|||||||||
27815|Kotara Formation|29922|6|Mentioned|Appendix 4|||||||||
27815|Kotara Formation|29926|6|Mentioned|Fig.3|||||||||
27815|Kotara Formation|29942|4|Described|Fig.2|||||||||
27815|Kotara Formation|34351|5|Briefly described|p344|||Fig.5.13||||||
27815|Kotara Formation|37083|6|Mentioned|p164|||||||||
27815|Kotara Formation|39292|6|Mentioned|Fig. 6.2|||||||||
27815|Kotara Formation|39308|6|Mentioned|Fig.23.4|||||||||
27815|Kotara Formation|39609|6|Mentioned|Table 1|||||||||
27815|Kotara Formation|41479|6|Mentioned|Fig.2|||||||||
27815|Kotara Formation|43344|14|Not recorded|p85||Permian|||||||
27815|Kotara Formation|43447|14|Not recorded|diag.p26|||Cardiff Sub-Group||||||
27815|Kotara Formation|43448|14|Not recorded|p224,228,235||Permian|Unit of Cardiff Subgroup (Newcastle Coal Measures)||||||
27815|Kotara Formation|45090|6|Mentioned|p186|||Refers McKenzie (1962)||||||
27815|Kotara Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Adamstown Subgroup|Included Merewether Conglomerate Member.|||
69882|Kowmung Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Very thick bedded crystal-rich volcaniclastic rocks of rhyolitic to dacitic provenance, interbedded with siltstone and mudstone; rhyolitic lavas and proximal volcaniclastic rocks; 2 subunits - volc.sst.+conglom. and rhyolitic rocks.||||||11-JUN-08
69882|Kowmung Formation|68592|1|Redefined|p725-6, 757-8, p821, p742, p874, p884-91|Lochkovian|Early Silurian|See also p728, p731 Fig.132. Redefined after Powell and Fergusson (1979); Cas et al. (1981). Defined as interval of Kowmung Volcaniclastics (Powell and Fergusson 1979) occurring below 'Boulder Conglomerate Member' (now basal Murruin Formation) of Cas et al. (1981); thus it includes 'Quartzo-Feldspathic Sandstone Member' and 'Silicic Breccia Member' of these authors. As the unit now includes coherent rhyolite it was renamed Kowmung Formation. The equivalent sequence to the Kowmung Formation in the Jocks Creek area was originally called the Goker Volcaniclastics by Whalan (1986). Type (largely retained as the interval stratigraphically beneath 'Boulder Conglomerate Member' of Cas et al. 1981) and representative section described. Max. thickness: ~600 m. Sub-greenschist to lower greenschist facies metamorphism. Age: inferred likely early Lochkovian age.||Unit in Mount Fairy Group.||Conformably overlies Covan Creek and Cobra Formations; conformably overlain by a basal conglomerate of Murruin Formation; unconformably overlain by Lambie Group.|Flow-banded rhyolite and rhyolitic volcanic breccia; very thickly-bedded quartzofeldspathic sandstone, siltstone and mudstone.|
69882|Kowmung Formation|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfk[3 asterisks]. Includes two unnamed subunits; a crystal rich quartz-feldspar-phyric rhyolite with spherulites and lithophysae and a thinly-thickly bedded crystal rich lithic quartz volcaniclastic sandstone. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group|Includes two unnamed members.|Overlies Covan Creek Formation and Cobra Formation.|Massive, very thick bedded, medium-coarse grained, lithic quartzofeldspathic sandstone interbedded with siltstone and mudstone; massive to flow banded rhyolite; minor rhyolitic volcanic breccia and sandstone.|
69882|Kowmung Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed subunits; a crystal rich quartz-feldspar-phyric rhyolite with spherulites and lithophysae and a thinly-thickly bedded crystal rich lithic quartz volcaniclastic sandstone.||Mount Fairy Group|Includes two unnamed members||Massive, very thick bedded, medium-coarse grained, lithic quartzofeldspathic sandstone interbedded with siltstone and mudstone; massive to flow banded rhyolite; minor rhyolitic volcanic breccia and sandstone.|
69882|Kowmung Formation|71069|5|Briefly described|p133, p135, p144, p170|||New name, redefinition of the Kowmung Volcaniclastics which it replaced. Up to 590m thick. ||Mount Fairy Group||Conformably overlain by the Murruin Formation. Conformably overlies the Covan Creek Formation.|Rhyolite lava and volcanic breccia.|
69882|Kowmung Formation|71700|5|Briefly described|p23|||northern Goulburn Basin. ||||||
23706|Kruge Conglomerate Member|22857|5|Briefly described|p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Burthong Formation (Mouramba Group, Cobar Supergroup). Max. thickness: 350m. Geological Province: Mouramba Shelf. See also p440 App.1, Tb.A1.6.||||||
23706|Kruge Conglomerate Member|41394|2|Defined|p54|Early Devonian||||||||
23706|Kruge Conglomerate Member|41395|6|Mentioned|Map legend|Lochkovian||||||||
23706|Kruge Conglomerate Member|41528|2|Defined|p59|Early Devonian||||||||
23706|Kruge Conglomerate Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
23706|Kruge Conglomerate Member|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
23706|Kruge Conglomerate Member|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Mouramba Group||||
77631|Kyeamba Monzogranite|69371|6|Mentioned|p9, p14|Silurian|Silurian|||||||
31597|Kyeamba Suite|42726|5|Briefly described|map legend||Silurian|Not grouped into any Supersuite.|||Burrandana, Kyeamba, Mount Flakney Granites.|||19-JAN-17
31597|Kyeamba Suite|69043|6|Mentioned|p44|||[Said to be of Koetong Supersuite & Chappell et al.1991 given as reference, but Chappell et al. did not include Kyeamba Suite in their Koetong Supersuite]. The dating of Burrandana Granite, Kyeamba Suite at 417.7+/-2.8 Ma is said to cast doubt on the inclusion of this Suite in the Koetong Supersuite.||Koetong Supersuite?|Burrandana Granite.|||19-JAN-17
30553|Kynuna Granite|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Batholith.||||||
30553|Kynuna Granite|23170|3|Fully described|p220|Early Devonian|Early Devonian|of Yeoval Batholith.||||||
25142|Kyogle Basalt|30604|2|Defined|p66|Cenozoic|Cenozoic|||||||19-NOV-08
25142|Kyogle Basalt|30605|4|Described|p268|||Mineralogy.Refs Mason (1969) unpublished.||||||
25142|Kyogle Basalt|36411|6|Mentioned|p269|||Refs Duggan & Masson 1978 for definition.||||||
25142|Kyogle Basalt|40896|4|Described|p46|||||||||
25142|Kyogle Basalt|43161|6|Mentioned|32|||||||||
25142|Kyogle Basalt|69599|5|Briefly described|p640|||In NSW.||||Equivalent to the Albert Basalt in QLD.||
25142|Kyogle Basalt|73581|5|Briefly described|p7|||Attributed to Focal Peak Volcano based on geochemistry (Cotter, 1998).||Focal Peak Volcanics||Underlies Lamington Volcanics, Mount Gillies Volcanics||
24349|Kyong Formation|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|part of Willyama Supergroup||||||
24349|Kyong Formation|22575|6|Mentioned|p179 Fig.2|||of the Thackaringa Group||||||
24349|Kyong Formation|22771|6|Mentioned|Table12.2p45|||||||||
24349|Kyong Formation|22857|5|Briefly described|p45 Tb. 12.2|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Geological Province: Willyama Fold Belt.||||||05-MAR-13
24349|Kyong Formation|22967|6|Mentioned|p39||Statherian|||||||
24349|Kyong Formation|23248|5|Briefly described|Fig2p169|||||||||
24349|Kyong Formation|40290|2|Defined|p5|Proterozoic|Proterozoic|||||||
24349|Kyong Formation|42537|4|Described|p11|||||||||
24349|Kyong Formation|43052|6|Mentioned|Fig.4.22|||||||||
24349|Kyong Formation|43086|6|Mentioned|Fig.3|||||||||
24349|Kyong Formation|46598|5|Briefly described|p303|||||||||
24349|Kyong Formation|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Thackaringa Group (Willyama Supergroup). Overlain by Rasp Ridge Gneiss. Underlain by Alma Gneiss.||||||31-MAY-07
24349|Kyong Formation|50606|6|Mentioned|p3.2|||Of the Thackaringa Group. Geological Province: Broken Hill Block.||||||
24349|Kyong Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
24349|Kyong Formation|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group.  Geological Province: Broken Hill Domain.||||||03-MAR-05
24349|Kyong Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
24349|Kyong Formation|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
24349|Kyong Formation|63866|5|Briefly described|p36|||Broken Hill Domain, Curnamona Province.||Thackaringa Group||||
24349|Kyong Formation|70014|5|Briefly described|Map legend|||Minor basic gneiss, granular ferruginous and cupriferous quartz rock, garnet-quartz rock, garnet-haematite rock, very minor medium-grained quartz-feldspar-biotite-garnet gneiss, quartz magnetite rock, and poorly-layered calc-silicate rock.||Unit in Thackaringa Group.||Overlies Alma Gneiss. Is overlain by Rasp Ridge Gneiss.|Psammitic to pelitic metasediments intercalated with quartzo-feldspathic gneisses which form beds 1m to tens of metres thick and lenses. Gneisses include leucocratic and biotite-rich types, and some contain sillimanite and/or feldspar megacrysts.|
34075|Kywong beds|22612|6|Mentioned|423, 424 fig 2 tbl 1|Early Permian|Early Permian|Parent Manning Group. Max thickness 1600 m. Also on page 426. Geol province New England Orogen||||||
34075|Kywong beds|24040|5|Briefly described|p475|||Of the Manning Group. Geological Province: Barnard Basin||||||21-AUG-08
82541|Lachlan Supergroup|73140|5|Briefly described|p495|Gisbornian|Late Cambrian|New unit proposed to recognise similarities in age and composition between the Adaminaby, Castlemaine and Girilambone groups.|||Adaminaby Group, Castlemaine Group, Girilambone Group||Terrigenous turbiditic sequences.|
23711|Lady Brassey Formation|6823|6|Mentioned|p205|||||Thackaringa Group||||
23711|Lady Brassey Formation|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
23711|Lady Brassey Formation|22575|6|Mentioned|p179 Fig.2|||Of the Thackaringa Group.||||||11-JUN-08
23711|Lady Brassey Formation|22771|6|Mentioned|Table12.2p45,45|||||||||
23711|Lady Brassey Formation|22857|4|Described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Lateral equivalent of Alma Gneiss. Max. thickness: 600m. Geological Province: Willyama Supergroup.||||||07-NOV-08
23711|Lady Brassey Formation|22884|5|Briefly described|p41. p43 Fig,. 3|||Of the Thackaringa Group. Geological province: Broken Hill Domain.||||||24-FEB-10
23711|Lady Brassey Formation|22965|6|Mentioned|Fig 1||Statherian|Part of the Thackaringa Group.||||||
23711|Lady Brassey Formation|22966|6|Mentioned|Fig1||Proterozoic|Rift stage of development.||||||
23711|Lady Brassey Formation|22967|6|Mentioned|p39||Statherian|||||||
23711|Lady Brassey Formation|23025|6|Mentioned|Fig1p75|||||||||
23711|Lady Brassey Formation|23160|6|Mentioned|fig1|||||||||
23711|Lady Brassey Formation|23248|5|Briefly described|Fig2p169|||||||||
23711|Lady Brassey Formation|24307|5|Briefly described|p973|Proterozoic|Proterozoic|Parent: Thackaringa Group.   Geological Province: Broken Hill Block||||||
23711|Lady Brassey Formation|38969|4|Described|p206|||||||||
23711|Lady Brassey Formation|39662|2|Defined|p416|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23711|Lady Brassey Formation|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23711|Lady Brassey Formation|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23711|Lady Brassey Formation|39849|6|Mentioned|Table 2|||||||||
23711|Lady Brassey Formation|40290|6|Mentioned|Fig.2|||||||||
23711|Lady Brassey Formation|40822|6|Mentioned|Fig.2|||||||||
23711|Lady Brassey Formation|41093|6|Mentioned|p252|||||||||
23711|Lady Brassey Formation|41145|6|Mentioned|Fig.4|||||||||
23711|Lady Brassey Formation|41633|6|Mentioned|p141|||||||||
23711|Lady Brassey Formation|42261|6|Mentioned|Fig 1 P530|||||||||
23711|Lady Brassey Formation|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23711|Lady Brassey Formation|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23711|Lady Brassey Formation|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23711|Lady Brassey Formation|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23711|Lady Brassey Formation|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23711|Lady Brassey Formation|42537|4|Described|p9|||||||||
23711|Lady Brassey Formation|42595|4|Described|p3, p5|||||||||
23711|Lady Brassey Formation|42897|5|Briefly described|Table 1 P326|||see also Fig.3, P321||||||
23711|Lady Brassey Formation|43052|6|Mentioned|Fig.4.22|||||||||
23711|Lady Brassey Formation|43086|6|Mentioned|Fig.3|||||||||
23711|Lady Brassey Formation|43267|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
23711|Lady Brassey Formation|43268|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
23711|Lady Brassey Formation|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
23711|Lady Brassey Formation|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
23711|Lady Brassey Formation|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
23711|Lady Brassey Formation|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
23711|Lady Brassey Formation|43572|6|Mentioned|Fig.3.2 p6|||||||||
23711|Lady Brassey Formation|46598|5|Briefly described|p302|||||||||
23711|Lady Brassey Formation|50045|5|Briefly described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Thackaringa Group (Willyama Supergroup). Overlain by Alders Tank Formation. Underlain by Mulculca Formation.||||||31-MAY-07
23711|Lady Brassey Formation|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Himalaya Suite. Geological Province: Broken Hill Block. Intruded by Potosi Supersuite.||||||07-NOV-08
23711|Lady Brassey Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
23711|Lady Brassey Formation|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group.  Geological Province: Broken Hill Domain.||||||03-MAR-05
23711|Lady Brassey Formation|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.||||||07-NOV-08
23711|Lady Brassey Formation|61735|5|Briefly described|p635 Fig. 1, p637|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group (lower part). Age: </-1720Ma and >1704+/-3Ma.||||||30-JUN-09
23711|Lady Brassey Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Ages: 1703+/-3Ma and 1705+/-3Ma. Geological province: Olary Domain.||||||
23711|Lady Brassey Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Thackaringa Group.||||
23711|Lady Brassey Formation|62536|5|Briefly described|p636-637, 640|||Broken Hill area. Appears on p636 as L.Brass.||Thackaringa Group.|||Metasediments. Extensive quartz-albite metasedimentary rocks; some with climbing ripples indicate sandstone progenitors.|
23711|Lady Brassey Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
23711|Lady Brassey Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Thackaringa Group||||15-DEC-21
23711|Lady Brassey Formation|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
23711|Lady Brassey Formation|63110|6|Mentioned|p1132|||Albite-rich rocks.||||||11-JUN-08
23711|Lady Brassey Formation|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Age: <1704+/-3Ma, <1705+/-5Ma. Geological Province: Broken Hill Block-Euriowie Block.||||||24-FEB-10
23711|Lady Brassey Formation|63866|5|Briefly described|p36|||Broken Hill Domain, Curnamona Province.||Thackaringa Group||||
23711|Lady Brassey Formation|64097|5|Briefly described|p305 Fig. 2|Paleoproterozoic|Paleoproterozoic|At base of Thackaringa Group; part of the formation had formerly been referred to as "Farmcote gneiss" but  only in the Redan geophysical zone of Broken Hill Domain. Age: </-1720Ma. Also written as "Lady Brassey Formation".||||||30-APR-13
23711|Lady Brassey Formation|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group (Willyama Supergroup). Geological Province: Broken Hill Block.||||||07-FEB-11
23711|Lady Brassey Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Thackeringa Group. Geological province: Broken Hill Domain.||||||07-FEB-11
23711|Lady Brassey Formation|64742|6|Mentioned|p321 Fig.3. ||||<1720 Ma.|Unit in Thackaringa Group.||||
23711|Lady Brassey Formation|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackeringa Group. Geological province: Broken Hill Domain.||||||07-FEB-11
23711|Lady Brassey Formation|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Thackaringa Group||Overlies the Thorndale Composite Gneiss. Overlain by the Alders Tank Formation. Intruded by the Alma Gneiss.||
23711|Lady Brassey Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.||Thackaringa Group.||||
23711|Lady Brassey Formation|70000|5|Briefly described|p34-36|Statherian|Statherian|Protolith probably sandy marine shelf sediments with variable evaporitic or hypersaline component.||Unit in Thackaringa Group.||Correlated with Farmcote Gneiss.||
23711|Lady Brassey Formation|70014|5|Briefly described|Map legend|||In the SE, contains abundant leucocratic quartzo-feldspathic gneiss, and is magnetite-rich.||Unit in Thackaringa Group.||Overlies Mulculca Formation. Is overlain by Alders Tank Formation.|Well to poorly bedded leucocratic sodic plagioclase-quartz rocks, either massive, discrete units or thin to thick interbeds within psammitic to pelitic metasedimentary composite gneisses. Substantial conformable masses of basic gneiss.|
23711|Lady Brassey Formation|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Thackaringa Group.||Overlies Thorndale Composite Gneiss.|Sodic plagioclase-quartz rock forming massive units or interbeds within sedimentary composite gneiss; local conformable basic gneiss.|
23711|Lady Brassey Formation|70405|6|Mentioned|p9 table 1|Paleoproterozoic|Paleoproterozoic||1700 Ma|Thackaringa Group||||
23711|Lady Brassey Formation|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|~1705 Ma|Thackaringa Group||Overlies Thorndale Composite Gneiss. Underlies Alders Tank Formation. Intruded by Alma Gneiss of Silver City Suite.||
23711|Lady Brassey Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Thackaringa Group.||||
23711|Lady Brassey Formation|72461|6|Mentioned|p16 fig 9|||||Thackaringa Group||Overlain by the Cues Formation.||
23711|Lady Brassey Formation|73243|6|Mentioned|p66|Statherian|Statherian|Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.||Thackaringa Group|||Contains amphibolite sills.|
23711|Lady Brassey Formation|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Thackaringa Group||Underlies Alders Tank Formation||
23711|Lady Brassey Formation|73482|6|Mentioned|p422 Fig.3|||||Thackaringa Group||||
23711|Lady Brassey Formation|73524|6|Mentioned|p5 Fig.3|||||Thackaringa Group||||
23711|Lady Brassey Formation|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|Statherian|Statherian||<1720 Ma|Thackaringa Group||Overlies Thorndale Composite Gneiss, underlies Cues Formation||
35889|Lady Louise Suite|23347|2|Defined|p51 Tb. 1, p54-55|Statherian|Statherian|Of the Willyama Supergroup.  Age: 1.69 Ga. Intrudes Curnamona Gp, including Basso Suite. Widespread as sills+dykes in Olary Domain; includes amphibolites - more detail included.||||||29-AUG-13
35889|Lady Louise Suite|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Igneous suite. Geological Province: Olary Domain. Age: 1685 Ma.||||||28-APR-05
35889|Lady Louise Suite|61239|5|Briefly described|p54|||Includes mafic sills, orthogneiss.||||||
35889|Lady Louise Suite|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.69 Ga|||Intrudes the Curnamona Group, Saltbush Subgroup and Basso Suite.|Amphibolite and mesocratic hornblende granite.|
35889|Lady Louise Suite|62373|5|Briefly described|p502, p503 Fig.2|Paleoproterozoic|Paleoproterozoic|Suite of magmatic rocks. Age: ca. 1685 Ma. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
35889|Lady Louise Suite|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Intrudes the Ethiudna Subgroup (Curnamona Group). Geological Province: Olary Domain/Curnamona Province.||||||16-SEP-09
35889|Lady Louise Suite|62535|5|Briefly described|p671||||c.1685 Ma.|||Intrudes Wiperaminga Subgroup.|Mafic intrusions.|
35889|Lady Louise Suite|62592|5|Briefly described|p15, p16 Fig.2.2.|Statherian|Statherian|Olary Domain. Mafic-dominated fractionated set of intrusives.|c.1685 Ma.|||||
35889|Lady Louise Suite|62993|5|Briefly described|p4, 7,8,14,23,26,37 39,40,42|Paleoproterozoic|Paleoproterozoic|Olary Domain. At the Radium Hill tailings dam borrow pit, green amphibolitic bodies considered to be part of  the 'sedimentary amphibolites' of Sprigg (1954) are now considered to be sills of Lady Louise Suite.|~1685 Ma||Includes Woman-in-White Amphibolite|Intrudes Basso Suite|Mafic dykes.|19-DEC-21
35889|Lady Louise Suite|63102|4|Described|p13,31,35,38,40,43-44,50,53|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Mafic magmatic suite, locally differentiated into hornblende or biotite granite. Underwent extensional deformation during Willyama Supergroup deposition. Chronostratigraphic equivalent of Hores Gneiss and Parnell Formation (Broken Hill Group).|~1685 Ma||Includes Woman-in-White Amphibolite.|Intrudes Curnamona Group.|Partly differentiated amphibolite-granite sills.|
35889|Lady Louise Suite|63186|5|Briefly described|p67 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Olary Domain, Curnamona Province. Mafic rocks.||||||07-NOV-08
35889|Lady Louise Suite|63224|6|Mentioned|p12|||Geological Province: Curnamona Province.||||||07-FEB-08
35889|Lady Louise Suite|63866|5|Briefly described|p37, p41, p49||||1685 +/- 4 Ma (Page et al., 2005b)||Includes the Woman-in-White Amphibolite.|||
35889|Lady Louise Suite|64316|5|Briefly described|p534|Paleoproterozoic|Paleoproterozoic|Term used for rocks in the Olary Domain equivalent to the ca 1685Ma mafic magmatism of the Broken Hill Block.  Age: 1685+/-6Ma (SHRIMP U-Pb, Connor and Fanning 2001).||||||07-FEB-11
35889|Lady Louise Suite|64741|5|Briefly described|p301 Fig. 4, p310|Paleoproterozoic|Paleoproterozoic|Intrudes the lower section of Saltbush Group, up as far as Raven Hill Subgroup. Age: 1685Ma. Geological province: Olary Domain.||||||07-FEB-11
35889|Lady Louise Suite|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Intrudes the Saltbush Group. Age: 1685Ma. Geological province: Olary Domain.||||||07-FEB-11
35889|Lady Louise Suite|66302|5|Briefly described|p36 Fig.9, p38|Statherian|Statherian|Olary Domain, Curnamona Province. |ca. 1685 Ma||Includes the Woman-in-White Amphibolite|Intrudes the Saltbush Group.||
35889|Lady Louise Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Olary Domain, Curnamona Province.|1687 +/- 4 Ma.|Saltbush Group.|||Amphibolite and mafic gneiss.|
35889|Lady Louise Suite|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|1685 +/- 4 Ma||||Amphibolite.|
35889|Lady Louise Suite|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
35889|Lady Louise Suite|67653|6|Mentioned|p4|||Geological province: Curnamona Province. ||||||
35889|Lady Louise Suite|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
35889|Lady Louise Suite|68126|5|Briefly described|p6, p29-31|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.|1685 +/- 4 Ma (Page et al. in prep).||||Medium-grained, black, weakly layered, hornblende-plagioclase +/- garnet amphibolite with oxidised magnetite. Local metamorphic layering. Sometimes contains coarse epidotised hornblende.|
35889|Lady Louise Suite|69654|6|Mentioned|p3|||Curnamona Province.||||||
35889|Lady Louise Suite|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||U-Pb age 1685+/-4 Ma.||||Amphibolite, quartz-bearing, locally differentiated to hornblende granite, intrusive sills and dykes, metamorphosed and deformed. Granodiorite to monzogranite, A-type affinity.|
35889|Lady Louise Suite|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||U-Pb age 1685+/-4 Ma||||Amphibolite, quartz-bearing, locally differentiated to hornblende granite, intrusive sills and dykes, metamorphosed and deformed. Granodiorite to monzogranite, A-type affinity.|
35889|Lady Louise Suite|70405|4|Described|p36, p37|Paleoproterozoic|Paleoproterozoic|The intrusion of this unit into broken hill sediments may have provided the heat source to mobilise fluids for ore formation.|1685 Ma|Kalabity Supersuite||Intrudes Broken Hill Group, Raven Hill Subgroup, Wiperaminga Subgroup, Basso Suite, Ethiunda Subgroup, Oonartra Creek Formation|Mafic dykes and lenticular sills. Mafic iron rich tholeiites, fine-medium grained amphibolites and two-pyroxene mafic granulites. Commonly massive with little to no foliation present. Some are altered into chloritic schists.|
35889|Lady Louise Suite|70657|4|Described|p12, p13 Fig.6, p15-16, p21, p30-31, p45|Statherian|Statherian|See also p47, p50-51, p58, p62-63. Conor and Fanning (2001). Olary Domain, Curnamona Province. Age-equivalent to Hores Gneiss and Parnell Formation.|1685 Ma|In Willyama Supergroup.|Woman-in-White Amphibolite.|In Willyama Supergroup. Intrudes Basso Suite, Curnamona Group (Wiperaminga and Ethiudna Subgroups). Equivalent to Parnell Formation.|Mafic (amphibolite) intrusives, locally differentiated into hornblende or biotite granite.|
35889|Lady Louise Suite|70658|5|Briefly described|p1-2, 5, 8, 11, 15, 20, 29, 32, 39, 42|Paleoproterozoic|Paleoproterozoic|Olary and Broken Hill Domains, Curnamona Province. Geochemistry briefly described.|~1685 Ma.||Woman-in-White Amphibolite.|Intrudes Peryhumuck Formation. Associated with Saltbush Group.|Mafic metagranites. Includes a thick, differentiated amphibolite-granite composite sill.|
35889|Lady Louise Suite|72454|6|Mentioned|p2 Fig.2|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain. Shown only on p2 Fig.2.||||||
35889|Lady Louise Suite|72461|6|Mentioned|p6||||1685 +/- 4 Ma|||||
35889|Lady Louise Suite|73030|6|Mentioned|p2150|Statherian|Statherian||ca. 1700-1680|||||
35889|Lady Louise Suite|73482|6|Mentioned|p422 Fig.3||||||Parnell metadolerite, Silver King metadolerites|||
35889|Lady Louise Suite|73512|5|Briefly described|p2-4, p7|Statherian|Statherian|Curnamona Province, Broken Hill Block. Emplaced at ca 1685 Ma.|ca 1685 Ma||||Mafic igneous rocks including metabasite.|
32270|Lady Northcotts Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
31600|Lady Northcotts Suite|42726|5|Briefly described|map legend||Silurian|||||||
31600|Lady Northcotts Suite|44093|5|Briefly described|p188 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
27457|Lake Bathurst Limestone Member|22768|6|Mentioned|p179|||||||||
27457|Lake Bathurst Limestone Member|22857|5|Briefly described|p179, p472 App.1 Tb.A1.6|Middle Devonian|Early Devonian|Of the Mulwaree Group. Contains corals. Max. thickness: 80m. Geological Province: Captains Flat-Goulburn Trough. ||||||
27457|Lake Bathurst Limestone Member|30730|6|Mentioned|p11|||Early Devonian||||||
27457|Lake Bathurst Limestone Member|30735|4|Described|p48|||||||||
27457|Lake Bathurst Limestone Member|30736|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27457|Lake Bathurst Limestone Member|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
27457|Lake Bathurst Limestone Member|39331|6|Mentioned|p56|||||||||
27457|Lake Bathurst Limestone Member|68592|5|Briefly described|p1657, p1173|Emsian|Emsian|On the Braidwood 1:100 000 map sheet. This unit post-dates cessation of major volcanism in the Goulburn area. Early Emsian age from fossils.||Unit in Mulwaree Group.||||
27457|Lake Bathurst Limestone Member|69159|5|Briefly described|Map legend|Emsian|Emsian|||Top of Bongalaby Formation.|||Grey to blue-grey, fossiliferous, massive to well-bedded biomicrite; lesser sandy biomicrite, biosparite and calc-arenite; minor cross-bedded, coarse-grained, calcareous lithic-quartz-feldspar sandstone.|07-SEP-15
27457|Lake Bathurst Limestone Member|71040|6|Mentioned|p13, p19|Emsian|Emsian|Youngest unit in the Goulburn region to be involved in Tabberabberan Orogeny deformation.||||||
27457|Lake Bathurst Limestone Member|71656|5|Briefly described|p12 Fig.2, p40|Emsian|Pragian|Well-exposed and highly fossiliferous section along Bongalaby Creek, yielded a diverse and abundant fauna. Correlated with Taemas Limestone.||Bongalaby Formation|||Fossiliferous limestone.|
27457|Lake Bathurst Limestone Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Bongalaby Formation.|||Grey to blue-grey, fossiliferous, massive to well-bedded biomicrite with lesser sandy biomicrite, biosparite and calc-arenite; minor cross-bedded, coarse-grained, calcareous lithic-quartz-feldspar sandstone.|
27457|Lake Bathurst Limestone Member|71700|3|Fully described|vi, p27, CD|Emsian|Pragian|Named for the township of Lake Bathurst. A representative section is in the Bongaralaby Creek between GR 740912 6120710 and GR 740851 6121855. Philip and Pedder (1968) referred informally to the Lake Bathurst Limestone before it was formally defined as the Lake Bathurst Limestone Member by Felton (1974b). Distribution,  geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils, distinguishing features, economic geology and geological hazards are discussed. Bands of this limestone member vary in thickness up to 220m spread over an interval of about 1200m. May be partially equivalent to the Taemas Limestone.||Bongalaby Formation||Conformably overlies the Bongalaby Formation. Equivalent to the Cavan Bluff Limestone.|Grey to blue-grey biomicrite with lesser sandy biomicrite and biosparite. This limestone varies from massive, to well stratified and is composed mainly of calcareous mud and fossil debris bound by fossils.|
31522|Lake Bathurst Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31522|Lake Bathurst Suite|68592|6|Mentioned|p1675|||Invalid name by Chappell et al. (1991). Sole unit was their Lake Bathurst Granite. Now Glenbog Suite.||||||
33050|Lake Cowal Volcanic Complex|22797|5|Briefly described|p837||Late Ordovician|Overlying unit is the Manna Conglomerate||||||26-MAR-20
33050|Lake Cowal Volcanic Complex|24233|5|Briefly described|p255 Fig.4, p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
33050|Lake Cowal Volcanic Complex|24417|2|Defined|p17|Middle Ordovician|Middle Ordovician|Previously referred to as "Lake Cowal Volcanics" (Miles, 1993) and "Lake Cowal volcanic complex" (Miles & Brooker, 1998).  Poorly exposed.||||||
33050|Lake Cowal Volcanic Complex|50554|5|Briefly described|Map legend|Ordovician|Ordovician|Intermediate to mafic volcanics and intrusives.  Overlies the Girilambone Group; underlies Edols Conglomerate.||||||05-JUL-13
33050|Lake Cowal Volcanic Complex|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||13-JUL-04
33050|Lake Cowal Volcanic Complex|60548|5|Briefly described|map legend|Ordovician|Ordovician|||||||
33050|Lake Cowal Volcanic Complex|70178|6|Mentioned|p2 ,p5, p6|||Former name for Cowal Igneous Complex. Oldest age determinations  (~470 Ma) shown in Fig 3, p5, reported on 'early diorite', E42 area and 'pre-mineral diorite' E43 area as U-Pb SHRIMP on monazite (Zukowski 2009, 2010 unpub).|Most ages in 466-460 Ma range.|||||05-JAN-22
23712|Lakes Road Rhyolite Member|22601|6|Mentioned|407|Early Permian|Early Permian|Parent Alum Mountain Volcanics|274.1+/-3.4 Ma|||||06-SEP-18
23712|Lakes Road Rhyolite Member|22857|5|Briefly described|p504|Early Permian|Early Permian|Of the Alum Mountain Volcanics. Yellow to white spherulitic and fluidal rhyolite with minor albitised and silicified basalt. Max. thickness: 130m. ||||||
23712|Lakes Road Rhyolite Member|24118|5|Briefly described|p34|||Of Alum Mountain Volcanics.||||||
23712|Lakes Road Rhyolite Member|36057|2|Defined|p350|Early Permian|Late Carboniferous|Late Carboniferous - Early Permian.||||||
23712|Lakes Road Rhyolite Member|39660|6|Mentioned|p450|||||||||
23712|Lakes Road Rhyolite Member|42833|5|Briefly described|p230|||of Alum Mountain Volcanics||||||
23712|Lakes Road Rhyolite Member|44244|4|Described|p227|Early Permian|Early Permian|Of the Alum Mountain Volcanics.  Underlies the Markwell Coal Measures.  Max. thickness: 130m.  Type section in text.  Geological Province: Myall Block.||||||
23712|Lakes Road Rhyolite Member|50263|5|Briefly described|Map Legend|Sakmarian|Sakmarian|Overlies: Burdekins Gap Basalt Member.  Underlies: Markwell Coal Measures (u).  Geological Province: Eastern Myall Block.||||||
23712|Lakes Road Rhyolite Member|65114|5|Briefly described|p396|Kungurian|Artinskian|?Of Alum Mountain Volcanics. Rhyolitic unit; zircon SHRIMP age of 275.1 +/- 3.4 Ma||||||
23712|Lakes Road Rhyolite Member|73487|5|Briefly described|p567, p568 Fig.3, p571, p572 Fig.7, p584|Wordian|Kungurian|Myall blocks. Myall Syncline. Abbreviated as Lakes Rod RM p566, Lakes Road Rhyolite Mb p568. See also p577, p579, p580 Fig.9.|ca 274-272 Ma (Li et al., 2014)|Alum Mountain Volcanics, upper|||Rhyolite.|
25987|Lambs Valley Ignimbrite Member|22857|5|Briefly described|p508 App.1 Tb.A1.8|Visean|Visean|Of the Mowbray Formation (Gilmore Volcanic Group). Welded rhyodacitic ignimbrite. Max. thickness: 100m. Geological Province: Tamworth Forearc Basin.||||||
25987|Lambs Valley Ignimbrite Member|24121|5|Briefly described|p4|||Of Mowbray Formation. Shown as Lamb Valley Ignimbrite Member p159.||||||25-AUG-22
25987|Lambs Valley Ignimbrite Member|31228|2|Defined|p82|Carboniferous|Carboniferous|||||||
25987|Lambs Valley Ignimbrite Member|44093|5|Briefly described|p229 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
25987|Lambs Valley Ignimbrite Member|44244|4|Described|p93, p40|Carboniferous|Carboniferous|Of the Mowbray Formation and the same ignimbrite extends into the top of the Isismurra Formation.  Max. thickness: 100m.  Type section in text.  Geological Provinces: Gresford and Rouchel Blocks.||||||16-SEP-04
25987|Lambs Valley Ignimbrite Member|50268|5|Briefly described|Map Legend|Visean|Visean|Of the Mowbray Formation.  Geological Province: Gresford and Rouchel Blocks.  Overlies and Underlies: Isismurra Formation.||||||
25987|Lambs Valley Ignimbrite Member|73487|6|Mentioned|p566|||||||||
25988|Lanes Shaft Coal Member|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Narrow Plain Formation (Coorabin Coal Measures). Max. thickness: 12m. Geological Province: Ovens Graben.||||||
25988|Lanes Shaft Coal Member|35498|2|Defined|p144|Late Permian|Late Permian|||||||
25988|Lanes Shaft Coal Member|35503|6|Mentioned|p202|||Defined in Standing Committee Coalfield Geology NSW (1978)||||||
25988|Lanes Shaft Coal Member|36329|4|Described|p62|||||||||
25988|Lanes Shaft Coal Member|38293|5|Briefly described|p20|||||||||
25988|Lanes Shaft Coal Member|42966|5|Briefly described|p407|||See also misspelling - Lane's Shaft Coal Member||||||
25988|Lanes Shaft Coal Member|43841|6|Mentioned|8||Late Permian|Member of Coorabin Coal Measures||||||
25988|Lanes Shaft Coal Member|69798|5|Briefly described|p4 Fig.2, p7, p16|Permian|Permian|Oaklands Basin. Considered to be the only economical seam in the Coorabin Coal Measures. From 4m to 18m thick. Fluvial-point bar depositional environment.||Narrow Plain Formation.||||06-FEB-18
73367|Lang Formation|67322|5|Briefly described|p19-20|Darriwilian|Darriwilian|Burton et al. (in press) recognised the Lang Formation as a facies variant of the Ballast Formation. Conodonts from cherts have been found which are indicative of a late Darriwilian age (Stewart and Glen 1986; Iwata et al. 1995; Percival and Zhen 2007).||||Facies variant of the Ballast Formation.|Greater predominance of sandstone with lesser chert (than Ballast Formation); rare, very weathered volcanics.|22-FEB-18
73367|Lang Formation|69094|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Includes an un-named but separately-mapped Member of 'maroon to brown, highly altered, ferruginised, porphyritic basaltic volcanic rock'.||Unit in Girilambone Group.|||Variably metamorphosed quartzose sandstone, siltstone, claystone/shale, thin chert beds; radiolarian and conodont-bearing in finer-grained rocks (Darriwilian).|
73367|Lang Formation|69095|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|||Unit in Girilambone Group.|||Variably metamorphosed quartzose sandstone, siltstone, claystone/shale, thin chert beds; radiolarian and conodont-bearing finer-grained rocks (Darriwilian); local mafic to ultramafic layers.|
73367|Lang Formation|69541|5|Briefly described|p652|Early Ordovician|Early Ordovician|Chert units contain conodonts of late Darriwilian age.||Unit in Girilambone Group.||||
73367|Lang Formation|69635|6|Mentioned|p69 Fig 3.1|||Misspelt as Lang Formtion.||||||
73367|Lang Formation|70602|6|Mentioned|p66,Fig 2, p67,72|Middle Ordovician|Middle Ordovician|Aeromagnetic map data given.||Girilambone Group||||
73367|Lang Formation|70941|4|Described|pviii, px, p6, p8 fig 4|Darriwilian|Darriwilian|Named for Lang Trigonometric station. Distribution, distinguishing features, geomorphology, geochemistry, metamorphism and geophysical characteristics discussed. lithology discussed in great detail. No type section is given due to generally poor outcrop and the structural complexity of the unit. Estimated to be several km thick. Deposited as a turbidite package in a deep marine environment. See also p13 fig 7, p12, p26,  p27, p50-56, p126, p127, p133, p140 fig 58, p147.||Girilambone Group||Conformably overlies or is faulted against the Narrama Formation, Laterally equivalent to the Ballast Formation|Interbedded generally massive, fine to medium grained  quartz sandstone, fissile siltstone, claystone, shale and minor thinly bedded chert.|
73367|Lang Formation|71360|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Mapped (and lithology described) with part of the Ballast Formation as one unit. Geophysical signature: broad areas of low magnetic intensity with linear trends of moderate magnetic intensity occurring parallel to regional foliation directions.||Girilambone Group.|||Sandstone, siltstone, claystone and chert. Local thin flows and sills of vesicular basalt.|
73367|Lang Formation|71693|5|Briefly described|Map legend.|Ordovician|Ordovician|This unit and the Ballast Formation are mapped as one unit.||Girilambone Group.||Overlies Narrama Formation [??].|Interbedded quartz-rich sandstone, siltstone, slate and phyllite with minor thin chert horizons.|13-SEP-19
73367|Lang Formation|71700|5|Briefly described|p8|||Chert units in this formation may be equivalent to the Nattery Chert Member.||Girilambone Group||||
73367|Lang Formation|72080|5|Briefly described|p2, p4, p9, p12-p14|Darriwilian|Darriwilian|Age is derived from conodont fossils in the chert units.||Girilambone Group||Equivalent to the Alandoon Chert and the Ballast Formation.|Terrigenous turbidites with minor mafic volcanics and rare chert horizons.|07-JAN-22
73367|Lang Formation|72296|3|Fully described|p5-11,p13,p24-26,p29-30,p58-59,p75,p82|Middle Ordovician|Middle Ordovician|Burton et al. (2012). Named after Lang Trig Station; the rather complicated type area (no type section) is in this vicinity with the coordinates of a number of separate outcrops detailed. Thickness is estimated at a few kilometres. Outcrop distribution described. Forms low hilly country. Very similar to Narrama Formation; distinguishing features described. Turbidites and pelagic sediments. Several generations of deformation. Geophysical properties described. No macrofossils: Darriwilian age from conodonts (listed).||Girilambone Group.||Is faulted against (locally may conformably overlie) Narrama Formation. Correlated, and may locally interfinger, with Ballast Formation. Is intruded by Byrock Granite.|Interbedded metasandstone, metasiltstone, metaclaystone, phyllite and chert; chert beds are characteristically rare and thin. Commonly strongly ferruginised locally. White quartz veining ubiquitous. Lithologies elaborated on p25.|
73367|Lang Formation|72908|6|Mentioned|p9|Late Ordovician|Late Ordovician|Hosts sulfide-rich copper mineralisation in the Blind Calf area, crosscut by later mafic and felsic dykes.||Girilambone Group||||
69819|Langari Hill Volcanics|63347|2|Defined|p5 Fig. 2, p31|Middle Miocene|Middle Miocene|Of the Langari Hill Volcanic Suite. Unconformable over Maybole Volcanic Suite. Age: 14Ma (K-Ar). Max. thickness: 80m; 40m in type area. Olivine-bearing tholeiitic basalt with minor volcanoclastic rocks. See also p7.||||||
69819|Langari Hill Volcanics|73581|5|Briefly described|p14-15|Miocene|Miocene||20.5+/-0.3 Ma, 14.2+/-0.02 Ma K-Ar|||Overlies Maybole Volcanic Suite|Thloeiitic basalt.|
28669|Lapstone Complex|36042|6|Mentioned|p50|||Invalid variation of Lapstone Creek sandstone?||||||
28669|Lapstone Complex|41939|6|Mentioned|p34|||||||||
75929|Larbert Conglomerate|69159|5|Briefly described|Map legend|Lochkovian|Lochkovian|||Unit in Bindook Group.||Is overlain by Kadoona Dacite Member.|Cream to green, pebble to cobble conglomerate. Clasts include quartz-rich sandstone and siltstone, mudstone and chert.|02-SEP-15
75929|Larbert Conglomerate|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Bindook Group.|||Cream to green, pebble to cobble conglomerate; clasts include quartz-rich sandstone and siltstone, mudstone and chert.|
75929|Larbert Conglomerate|71700|5|Briefly described|vi, p7, p23-p25, p27, p36-p37, CD|Lochkovian|Wenlock|Named for the parish of Larbert. Due to limited exposure no type section is defined for this unit and a representative section only intermittently outcrops. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism and distinguishing features are discussed. A maximum thickness of 1km is estimated. Age is derived from dates of over and underlying units. This unit is also interpreted to be equivalent to the Jinglemoney Conglomerate and the Bullamalita Conglomerate.||Bindook Group||Unconformably overlies the Cardinal View Formation. Overlain by the Kadoona Dacite Member (Long Flat Volcanics). Equivalent to the Brooklyn Conglomerate Member.|Massive, clast- to matrix-supported, pebble conglomerate in which clasts are prediominantly chert, sandstone and siltstone.|
26684|Laytons Range Conglomerate|12597|5|Briefly described|p491, p492 Tb.1|Rhaetian|Rhaetian|S Clarence-Moreton Basin. Basal, high energy fluvial deposits on top of eroded surface of Ipswich and Nymboida Basins. Appears as Laytons Ranges Cgl in Tb.1.||Unit in Bundamba Group.|||Conglomerate, coarse lithic sandstone.|
26684|Laytons Range Conglomerate|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Rahetian|Of the Woogaroo Subgroup (Bundamba Group). Polymictic pebble-cobble conglomerate (basal rudite); minor sandstone. Max. thickness: 80m. Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|22865|6|Mentioned|Fig.22.10ap318|||||||||
26684|Laytons Range Conglomerate|23811|5|Briefly described|Map Legend|Rhaetian|Rhaetian|Of Woogaroo Subgroup.  Polymictic pebble and cobble ortho- and paraconglomerate; subordinate lenses/beds of coarse-grained, crossbedded sublithic to lithic sandstone.  Clasts incl. chert, volcanic and sedimentary rock.  Geol:Prov: Clarence-Moreton Basin.||||||20-DEC-04
26684|Laytons Range Conglomerate|23812|5|Briefly described|p35 Tb.4|Late Triassic|Late Triassic|Of Bundamba GRoup.  Maximum thickness: 80m.  Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|30911|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
26684|Laytons Range Conglomerate|31806|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
26684|Laytons Range Conglomerate|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
26684|Laytons Range Conglomerate|33476|4|Described|p102|||Mention p90.||||||22-MAY-08
26684|Laytons Range Conglomerate|33766|6|Mentioned|Map legend|Jurassic|Triassic|Jurassic - Triassic||||||
26684|Laytons Range Conglomerate|34340|3|Fully described|p465|||||||||
26684|Laytons Range Conglomerate|39279|6|Mentioned|Fig. 1|||||||||
26684|Laytons Range Conglomerate|39907|4|Described|p10|||Sedimentology||||||
26684|Laytons Range Conglomerate|41631|6|Mentioned|p9|||||||||
26684|Laytons Range Conglomerate|42248|6|Mentioned|p408|||||||||
26684|Laytons Range Conglomerate|42463|6|Mentioned|Fig.3 P170|||||||||
26684|Laytons Range Conglomerate|43150|5|Briefly described|Map Legend||Late Triassic|Of the Woogaroo Subgroup. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
26684|Laytons Range Conglomerate|43736|5|Briefly described|Table 1,p4|||||||||
26684|Laytons Range Conglomerate|44450|5|Briefly described|p9|Late Triassic|Late Triassic|Geological Province: New England Fold Belt.||||||
26684|Laytons Range Conglomerate|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup. Conglomerate and sandstone.||||||
26684|Laytons Range Conglomerate|60281|5|Briefly described|p30, Fig. 18 App 1|Late Triassic|Late Triassic|See also the informal Laytons Range conglomerate.  Of the Woogaroo Subgroup (Bundamba Group).  Conglomerate, minor sandstone.  Overlain by Raceview Formation. Max. thickness: 80m.  Geological Province: Clarence-Moreton Basin.||||||17-MAR-05
26684|Laytons Range Conglomerate|60993|5|Briefly described|p6|Late Triassic|Late Triassic|Of the Woogaroo Subgp. Previously mapped as Corindi Conglom., but this name now discarded. Incorporates the Aberdare Conglom. Pebble to boulder conglomerate; minor shale, siltstone, coal. Geol. Prov: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|60995|4|Described|p55-56, p51 Fig. 3|Late Triassic|Late Triassic|Of Woogaroo Subgp; equivalent of Aberdare Conglom. Pebble and cobble conglomerate, minor sandstone. Overlain by Raceview Fm or Gatton Sst.  Max. thickness: 80m. Geol. Prov: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|60996|5|Briefly described|p72|||Grades up into Raceview Formation and also unconformably overlain by Gatton Sandstone; near Baryulgil, overlain conformably by Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin. Equivalent of Aberdare Conglomerate.||||||
26684|Laytons Range Conglomerate|60997|5|Briefly described|p140|||Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
26684|Laytons Range Conglomerate|60999|5|Briefly described|p164|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6.||||||
26684|Laytons Range Conglomerate|61004|5|Briefly described|p232 Fig. 2|Triassic|Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|61006|5|Briefly described|p279 Tb. 1|Triassic|Triassic|Conglomerate, labile sandstone, mudstone. See also p279 Tb. 1.||||||
26684|Laytons Range Conglomerate|61310|5|Briefly described|p21, Table C1 (p22-23)|Late Triassic||Of the Woogaroo Subgroup. Pebble/cobble conglomerate, minor sandstone. Geological Province: Clarence-Moreton Basin||||||
26684|Laytons Range Conglomerate|64665|5|Briefly described|p59.|Late Triassic|Late Triassic|Clarence-Moreton Basin. ||||Is overlain by Raceview Formation.|High energy conglomerate and sandstone.|
26684|Laytons Range Conglomerate|67402|5|Briefly described|p165 tbl LPB1, p187, p188, p193|||Clarence-Moreton Basin.||Woogaroo Subgroup|||Conglomerates with minor coarse lithic sandstones.|
26684|Laytons Range Conglomerate|69297|5|Briefly described|p487 fig 5.38|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. More than 50m thick. ||Woogaroo Subgroup||Overlies the Redcliff Coal Measures. Overlain by the Raceview Formation.||
26684|Laytons Range Conglomerate|69594|5|Briefly described|p543-544|||Clarence-Moreton Basin (NSW). Is known as Aberdare Conglomerate in QLD. The basal shale-siltstone is <1m thick and consists of weathered needles of iron carbonate in a pinkish Fe-rich matrix; it forms a consistent marker bed in many boreholes.||Woogaroo Subgroup.||Is overlain by Raceview Formation.|Pebble to cobble conglomerate; some beds with rippled fine sandstone laminae, others extensively rooted, thin claystones in places; a pinkish grey shale and siltstone underlies conglomerate at base.|
26684|Laytons Range Conglomerate|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
26684|Laytons Range Conglomerate|71628|5|Briefly described|p9: 5, 11, 32; p19: 24, 147|Triassic|Triassic|Clarence-Moreton Basin.||Woogaroo Subgroup.||Overlies Purgatory Monzogranite, Bruxner and ?Cullens Creek Granodiorites and (locally) Dumbudgery Creek Complex and Jenny Lind Tonalite.||
26684|Laytons Range Conglomerate|73570|5|Briefly described|p911, p912 Fig.2, p913-915, p919-920|Rhaetian|Norian|Clarence-Moreton Basin, lower part. Paleocurrent directions are generally radial into the basin. Very local provenance from New England Orogen. Abbreviated as Laytons Conglomerate p917 Fig.5.||||Overlies Ipswich Coal Measures, underlies Raceview Formation||
35069|Leadville Quartz Monzonite|23043|5|Briefly described|Map Legend|Visean|Tournaisian|of Gulgong Plutonic Suite.||||||
35069|Leadville Quartz Monzonite|23170|2|Defined|p276|Early Carboniferous|Early Carboniferous|of Gulgong Plutonic Suite.||||||
35069|Leadville Quartz Monzonite|68003|5|Briefly described|p24 Fig.3-e, p141. |Tournaisian|Famennian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gulgong Plutonic Suite.|||Porphyritic quartz monzonite.|
22180|Leather Barrel Pyroxenite|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Og1||||||
22180|Leather Barrel Pyroxenite|60078|6|Mentioned|Map Legend|Late Ordovician|Middle Ordovician|||||||15-JUL-04
40925|Ledgeworth Facies|50230|5|Briefly described|Map legend|Wenlock|Wenlock|Informal name.  Of the Hawkins Volcanics (Douro Group).   Grey to white aphanitic vitric tuff.||||||10-MAY-04
25990|Leesville Granodiorite|22815|4|Described|p45|Silurian|Silurian|||||||
25990|Leesville Granodiorite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
25990|Leesville Granodiorite|35109|2|Defined|p59|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
25990|Leesville Granodiorite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
25990|Leesville Granodiorite|40328|4|Described|p208|||||||||
25990|Leesville Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
25990|Leesville Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb25.||||||
25990|Leesville Granodiorite|60078|6|Mentioned|Map Legend||Silurian|||||||
33861|Leeton Igneous Complex|22508|5|Briefly described|p5|||Lachlan Fold Belt. ?Middle Devonian||||||
33861|Leeton Igneous Complex|66934|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Informal name. Magnetic susceptibility and gravity readings are given.|||||Plutonic, dominantly silicic; includes altered porphyritic leucocratic granite with quartz, feldspar and biotite crystals in a matrix of perthite-microcline, and greisen granites composed of quartz and feldspar with miarolitic cavities and sulfides.|
33861|Leeton Igneous Complex|69798|5|Briefly described|p6, p9, p13|Silurian|Silurian|Gunn (2003). Part of the basement to Oaklands Basin. |||||Contains highly magnetic, low density granite.|
33861|Leeton Igneous Complex|70718|4|Described|p53, p72-p74, p86, p94, p115-116, p123|Middle Devonian|Middle Devonian|Thin section descriptions are provided in the appendix (p115-116). Unit description p123.||||Intrudes Booroorban granite, Eurolie granite. Intruded by  the Singorimbah igneous intrusions.|Series of nested plutons, dominantly silicic granites consisting of greisens, weakly greisenised leucocratic granites, leucocratic granites and leucocratic high-level granites.|31-MAY-19
23721|Legume Sandstone|33476|6|Mentioned|Table 6|||Refers Brunker pers comm||||||
23722|Leloma Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures). Siltstone, sandstone and coals. Max. thickness: 585m. Geological Province: Sydney Basin.||||||
23722|Leloma Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Craven Subgroup.    Geological Province: New England Fold Belt||||||
23722|Leloma Formation|40872|6|Mentioned|Fig.2|||||||||
23722|Leloma Formation|41054|6|Mentioned|p154|||||||||
23722|Leloma Formation|44244|4|Described|p168 Tb. 2, p186-188|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures).  Includes the Jo Doth Tuff Member.  Conformably overlies Jilleon Formation.  Max. thickness: 585m.  Type section in text.  Geological Province: Myall Block.||||||23-AUG-04
23722|Leloma Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures).  Geological Province: Western Myall Block.||||||
23723|Lerida Limestone Member|23173|6|Mentioned|Map Legend|||||||||
23723|Lerida Limestone Member|38292|6|Mentioned|p5|||||||||
23723|Lerida Limestone Member|41138|6|Mentioned|Map legend|Pragian|Pragian|||||||
23723|Lerida Limestone Member|43032|2|Defined|p80||Early Devonian|of lower Amphitheatre Group||||||
23723|Lerida Limestone Member|71039|5|Briefly described|p14|||Northwestern Amphitheatre Group. Conodont Alteration Index (CAI) in this member is recorded.||Biddabirra Formation|||Limestone.|23-SEP-19
23723|Lerida Limestone Member|72958|6|Mentioned|p5, p61||Pragian|Allochthonous, olistolithic. Contains Pragian conodonts at ca. 412-408 Ma (Mathieson et al., 2016; Walker et al., 2018). Northern stratigraphic equivalent of the Shume Formation.||Biddabirra Formation||Correlated to Shume Formation||
23723|Lerida Limestone Member|73174|5|Briefly described|p1037-1039|Lochkovian|Lochkovian|Cobar Basin. Contains a non-age-diagnostic fossil assemblage of corals, Favosites, stromatoporoids and crinoid stems. An early Lochkovian age was assigned based on the presence of Ozarkodina cf. eurekaensis (conodont).||CSA Siltstone, Amphitheatre Group, Cobar Supergroup||||
26686|Lett Granite|42726|5|Briefly described|map legend|Carboniferous||22.  Of the Hartley Suite (Bathurst Supersuite).||||||07-FEB-05
27463|Lewis Coal Member|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
27463|Lewis Coal Member|40331|6|Mentioned|p5|||||||||
27463|Lewis Coal Member|70791|5|Briefly described|p285, p293 Fig.17|Permian|Permian|Muswellbrook area. Has similarities with Bibblewindi Coal Member (Mullaley Sub-basin).||Skeletar Formation||||
28114|Lewis Ponds Granite|23214|3|Fully described|p255|Carboniferous|Carboniferous|Intrudes Anson Formation, Mullions Range Volcanics, Barnby Hills Shale and Bay Formation.||||||
28114|Lewis Ponds Granite|42726|5|Briefly described|map legend|Carboniferous||12.||||||
28114|Lewis Ponds Granite|43127|5|Briefly described|Fig.2 p6,Fig.3 p9|||||||||
28114|Lewis Ponds Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
28114|Lewis Ponds Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|||||||
28114|Lewis Ponds Granite|60424|5|Briefly described|p350 Fig. 1, 352 Fig. 3|Carboniferous|Carboniferous|Geological Province: Hill End Trough. I-Type, massive.||||||
28114|Lewis Ponds Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
26687|Liamena Rhyolite|29909|6|Mentioned|p139|||||||||
26687|Liamena Rhyolite|30910|6|Mentioned|Map legend|Permian|Permian|||||||
26687|Liamena Rhyolite|31726|6|Mentioned|Map legend|Permian|Permian|||||||
26687|Liamena Rhyolite|35095|6|Mentioned|p107|||Reference Kenny (1928).||||||
26687|Liamena Rhyolite|43355|14|Not recorded|Map Legend||Permian|Provisional Edition||||||
26687|Liamena Rhyolite|43356|14|Not recorded|Map Legend||Permian|||||||
26687|Liamena Rhyolite|43405|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
26687|Liamena Rhyolite|68003|5|Briefly described|p129.|Permian|Permian|Gunnedah Basin.|||||Rhyolite.|
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.||||||
35614|Licking Gully Granite|50231|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of the Wyangala Batholith.||||||
35614|Licking Gully Granite|61910|5|Briefly described|p152 Fig. 1|Late Silurian|Late Silurian|Part of the Wyangala Batholith. Geological Province: Lachlan Fold Belt.||||||
35614|Licking Gully Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Cream, coarse-grained, massive to weakly foliated, equigranular to occasionally porphyritic biotite granite. High K, Th and U radioelement response.||||||12-JUN-08
35614|Licking Gully Granite|64295|5|Briefly described|p199|||Part of Wyangala Batholith. Intrudes Kenyu Formation.||||||01-SEP-08
35614|Licking Gully Granite|66713|6|Mentioned|p3 Fig.2, p5  ||Silurian|Frogmore area. Unit in Hovells Suite.||||||
35614|Licking Gully Granite|68592|2|Defined|p1262-4, p1268-9, p1274, p1284, p1290-3|Late Silurian|Late Silurian|See also xxiv, p373, p376, p379, p384-5, p415, p443, p467, p1255 Fig.220, p1260. Named by Gibbons (1960) after Licking Gully. Has been called the Gunnary Granite by Chappell et al. (1991). The parent Wyangala Suite has been superseded by Hovells Suite which incorporates several new units on geochemical grounds. Type locality described. Geochemistry detailed; geophysical properties described. The metamorphic aureole has produced cordierite spotting in pelitic lithologies. Fractionated; a potential source of Sn-W mineralisation, although none is known.||Unit in Hovells Suite.||Intrudes Kenyu and Eurimbla Formations and Hawkins Volcanics. Contact metamorphosed Hanaminno Limestone.|Cream, coarse-grained, massive to somewhat foliated, equigranular to sporadically porphyritic, biotite granite; fine- to medium-grained, aplitic granite occurs at the margins. Minor grey, porphyritic biotite microgranite, generally as dykes.|
35614|Licking Gully Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Soc. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot. Includes one unnamed subunit of fine-medium grained, leucocratic, aplitic granite. ||Hovells Suite|Includes one unnamed sub-unit.||Coarse grained, massive-foliated, equigranular to sporadically porphyritic biotite granite. Minor porphyritic biotite microgranite with aplitic granite at margins; high K, medium to high Th and U response; low magnetic susceptibility.|
35614|Licking Gully Granite|70545|5|Briefly described|Map Legend |Devonian|Silurian|Includes one unnamed subunit of fine-medium grained, leucocratic, aplitic granite.||Hovells Suite|||Coarse grained, massive-foliated, equigranular to sporadically porphyritic biotite granite. Minor porphyritic biotite microgranite with aplitic granite at margins; high K, medium to high Th and U response; low magnetic susceptibility.|20-SEP-17
25167|Limekilns Formation|22472|5|Briefly described|p39|Devonian|Devonian|||||||
25167|Limekilns Formation|22486|6|Mentioned|p 1|||||||||
25167|Limekilns Formation|22529|6|Mentioned|8|Early Devonian|Early Devonian|||||||
25167|Limekilns Formation|22590|5|Briefly described|P750|||Formerly Limekilns Group, Equivalent to the Cunningham Formation||||||
25167|Limekilns Formation|22768|5|Briefly described|p179|Emsian|Pragian|||||||
25167|Limekilns Formation|22857|5|Briefly described|p179, p476 App.1 Tb.A1.6|Emsian|Pragian|Of Kandos Group. Shales and carbonates. Max. thickness: 360m. Geological Province: Capertee Rise. ||||||
25167|Limekilns Formation|23214|3|Fully described|p203, p201 Fig. 38|Emsian|Lochkovian|Modified from Limekilns Group. Bedded sequence of monotonous grey siltstone with minor fine grained sandstone. Max. thickness 510m.||||||17-JAN-06
25167|Limekilns Formation|23738|5|Briefly described|p252||Devonian|||||||
25167|Limekilns Formation|24019|6|Mentioned|p368|Pragian|Pragian|||||||
25167|Limekilns Formation|24394|5|Briefly described|p170 Fig.1, p171|||||||||
25167|Limekilns Formation|42051|6|Mentioned|p139|||||||||
25167|Limekilns Formation|43641|5|Briefly described|Map Legend||Devonian|||||||
25167|Limekilns Formation|43782|5|Briefly described|Map Legend|Emsian|Pragian|||||||
25167|Limekilns Formation|44093|5|Briefly described|p213 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
25167|Limekilns Formation|64296|5|Briefly described|p84 Tb 1|Early Devonian|Early Devonian|Trilobite fauna.||||||28-AUG-08
25167|Limekilns Formation|64994|5|Briefly described|p8|Pragian|Pragian|Overlies Merrions Formation. Contains the Pragian dacryocyanarid Nowakia acuarina.||||||07-FEB-11
25167|Limekilns Formation|70297|4|Described|map legend, on side 2 of map sheet|Emsian|Pragian|Age: Early Devonian (late Pragian to late Emsian). Ungrouped, this unit records a relatively deep water slope environment on the eastern side of the Hill End Trough.|||Jesse Limestone Member|Overlies Crudine Group.|Bedded grey siltstone with minor fine-grained sandstone and fossiliferous limestone.|
25167|Limekilns Formation|73143|6|Mentioned|p8|Lochkovian|Lochkovian|Only confirmed graptolite recorded from the basal Lochkovian Monograptus uniformis Biozone (Rickards and Wright, 2000) in Australia.||||||
77064|Linden Coal Member|71628|6|Mentioned|p13:10|||||||||
82545|Linden Hill Tonalite|71628|4|Described|p9:2; p18: 1, 17-20|||New name, after unpublished work by Hensel (1982). Originally Linden Hill Adamellite of Binns et al. (1967). Crops out ~7 km W of Walcha as a small (~1.5 x 0.5 km) intrusion. Geochemistry detailed.|250-246 Ma (Hensel, 1982).|Linden Hill Suite.||Intrudes Sandon Association.|Porphyritic biotite-hornblende tonalite; minor leucomonzogranite. I-type.|
38301|Linden seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
26690|Lintiss Vale Formation|22646|5|Briefly described|p 102|Early Cambrian|Neoproterozoic|Situated in the Adelaide Geosyncline - East.  Parent - Farnell Group||||||
26690|Lintiss Vale Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
26690|Lintiss Vale Formation|22857|4|Described|Tb. 13.1 (insert p70-71), p92|Marinoan|Marinoan|Of Farnell Gp. Sltst with qtz beds and minor carbonates. Contains a diverse trace fossil faunal assemblage. Quartzites at top of the Fm were included in "Acacia Downs Formation". Max. thickness: 1200m. Geol Prov: Adelaide Fold Belt. See p400 App.1 Tb.A1.3||||||
26690|Lintiss Vale Formation|22858|5|Briefly described|p92||Vendian|||||||
26690|Lintiss Vale Formation|30261|4|Described|Table 1|||Marinoan age||||||
26690|Lintiss Vale Formation|30375|6|Mentioned|p205|||Fossil content.||||||
26690|Lintiss Vale Formation|33004|6|Mentioned|p138|||||||||
26690|Lintiss Vale Formation|33734|6|Mentioned|p494|||Correlation.||||||
26690|Lintiss Vale Formation|34812|3|Fully described|p105|||||||||
26690|Lintiss Vale Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26690|Lintiss Vale Formation|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
26690|Lintiss Vale Formation|38157|6|Mentioned|p265|||||||||
26690|Lintiss Vale Formation|39214|6|Mentioned|Table 1|||||||||
26690|Lintiss Vale Formation|39885|6|Mentioned|p427|||||||||
26690|Lintiss Vale Formation|41429|5|Briefly described|p246|||||||||
26690|Lintiss Vale Formation|41801|6|Mentioned|p216|||||||||
26690|Lintiss Vale Formation|43781|6|Mentioned|p5|||||||||
26690|Lintiss Vale Formation|66623|5|Briefly described|p13, p18. |||||||Overlies Camels Hump Quartzite.|Light brown, green, grey and yellow siltstone with some quartzite and minor carbonate; very narrow beds of medium-grey, medium-grained, massive quartzite; rare thinly-bedded sandy limestone (<0.2 m thick).|
26690|Lintiss Vale Formation|70000|6|Mentioned|p34, p40|Neoproterozoic|Neoproterozoic|||Uppermost unit in Farnell Group.||||
26690|Lintiss Vale Formation|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Farnell Group.||Overlies Camels Hump Quartzite.|Upward-coarsening, brown, green, grey and yellow siltstone-sandstone with minor limestone; increasing thinly-bedded quartzite horizons up-section.|
82546|Linton Monzogranite|71628|4|Described|p4: 1, 3, 5, 13-14, 33-37|||New unit: formalised here after Linton monzogranite of Jeon et al. (2012). Unmodified from unpublished work by Chappell and Bryant (1994). Named after the town of Linton. 32 km NW and up to 34 km E-W. Southern New England Orogen. Geochemistry described; essentially indistinguishable from Copeton Monzogranite.|287.7 +/- 2.1 Ma (SHRIMP: Jeon et al., 2012,2014).|Copeton Suite.||Intrudes Texas beds. Is overlain by Marburg Formation and Pilliga Sandstone. Abuts Graman Monzogranite.|Coarse-grained, porphyritic and less commonly equigranular, biotite (+/- muscovite, +/- cordierite, +/- garnet) monzogranite and syenogranite; locally greisenous. S-type.|
29940|Little Bay Shale|22943|6|Mentioned|p509-10,516-7|||||||||
29940|Little Bay Shale|24343|5|Briefly described|p63, p65 Fig. 2|Middle Miocene|Middle Miocene|Overlain by Tupia Formation||||||
29940|Little Bay Shale|70587|5|Briefly described|Map Legend|Miocene|Miocene||||||Poorly consolidated shale|
31393|Little Broken Hill Gabbro|22553|6|Mentioned|p77|Cryogenian|Cryogenian|||||||
31393|Little Broken Hill Gabbro|24599|5|Briefly described|p491|Neoproterozoic|Neoproterozoic|Age: ca827Ma.  Geological Province: Curnamona Craton.||||||
31393|Little Broken Hill Gabbro|43572|6|Mentioned|Fig.3.23,p43|||See also colour plate after p36||||||
31393|Little Broken Hill Gabbro|61732|5|Briefly described|p37|Cryogenian|Cryogenian|In the Willyama Inlier. Age: 827+/-9Ma.||||||07-FEB-11
31393|Little Broken Hill Gabbro|61822|6|Mentioned|p107|||||||||
31393|Little Broken Hill Gabbro|62453|5|Briefly described|p15|||Age: 827 +/- 9Ma. Geological Province: Curnamona Province.||||||
31393|Little Broken Hill Gabbro|68822|6|Mentioned|p322 Fig.4|||||||||
31393|Little Broken Hill Gabbro|69003|6|Mentioned|p58|Proterozoic|Proterozoic||c.825 Ma.|||||
31393|Little Broken Hill Gabbro|69666|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Part of the Willouran Basic Province.||||||
31393|Little Broken Hill Gabbro|69999|6|Mentioned|p21|Neoproterozoic|Neoproterozoic|Broken Hill Block.||||||
31393|Little Broken Hill Gabbro|70000|5|Briefly described|p39|Neoproterozoic|Neoproterozoic|Early sign of Neoproterozoic rifting; intrudes the Paleoproterozoic basement. Correlated with the Gairdner Dyke Swarm in the Gawler Craton and Stuart Shelf in SA.|c.827 Ma.||||Tholeiitic dolerite dykes and gabbro.|
31393|Little Broken Hill Gabbro|70328|6|Mentioned|p160-161|Tonian|Tonian|Adelaide Geosyncline. Age from baddeleyite U-Pb analysis by Wingate et al., 1998.|827+\-9 Ma (Wingate et al., 1998).|||||
31393|Little Broken Hill Gabbro|70334|6|Mentioned|p45||||827+\-9 Ma (U-Pb)|||Contemporaneous with Gairdner Dolerite.||
31393|Little Broken Hill Gabbro|70405|6|Mentioned|p79|Neoproterozoic|Neoproterozoic||827 Ma ||||Gabbro dykes.|
31393|Little Broken Hill Gabbro|70657|6|Mentioned|p53|Tonian|Tonian|Considered to represent early stages of extensional rifting of the Adelaide Geosyncline.|~827 Ma.|||||
31393|Little Broken Hill Gabbro|71129|5|Briefly described|p103,106|Tonian|Tonian|Geological Province: Curnamona Province, Gawler Craton. Part of the Willouran Basic Province, which also includes Beda Basalt, and the Wooltana and Cadlareena volcanics, Wilangee Basalt and Gairdner Dolerite. Related to the Rodinian break-up (Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Basaltic volcanism interpreted to be result of mantle plume upwelling, causing doming in the continental lithosphere (Zhao et al., 1994). Dated at 827+\-9 Ma (Wingate et al., 1998).|827+\-9 Ma|||||
31393|Little Broken Hill Gabbro|72238|5|Briefly described|p42-43|Tonian|Tonian|Geological province: Curnamona Province. Pb-Pb zircon age of 827+\-9 Ma (Wingate et al. 1998).||||||
23732|Little Brown Mountain Granite|22815|5|Briefly described|p96|||||||||
23732|Little Brown Mountain Granite|42726|5|Briefly described|map legend|Middle Devonian||Informal usage.||||||
23732|Little Brown Mountain Granite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Mumbulla Suite.||||||
29591|Little Forest Granite|22679|3|Fully described|p 43||Silurian|||||||
29591|Little Forest Granite|23214|3|Fully described|p166|Late Silurian|Late Silurian|Originally named Little Forest Adamellite.  Intrudes the Adaminaby Group.  Geological Province: Wyangala Batholith||||||
29591|Little Forest Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Biotite granite, leucogranite.||||||17-JUL-08
29591|Little Forest Granite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyangla Batholith.||||||17-JUL-08
29591|Little Forest Granite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
26693|Little Mount Porphyry|30910|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
26693|Little Mount Porphyry|43405|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
29531|Little Plains Granite|22519|5|Briefly described|p8|Silurian|Silurian|||||||
29531|Little Plains Granite|23053|4|Described|p21-2,65||Wenlock|Max Age: 425 Ma.||||||
29531|Little Plains Granite|43277|5|Briefly described|Map Legend|Late Silurian||of Lachlan Fold Belt.Middle-Late Silurian.||||||
35343|Little Range Granite|50231|5|Briefly described|Map Legend|Emsian|Pragian|||||||
35343|Little Range Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Grey, medium-grained, massive, weakly porphyritic to equigranular biotite-hornblende-augite-ferroan enstatite granite.||||||25-JUN-08
35343|Little Range Granite|68592|3|Fully described|p1398, p1401-3, p1436-8|Early Devonian|Early Devonian|New unit and name, after Little Range property. Crops out as a very small circular intrusion (400m diameter). Type locality described. Geochemistry detailed; geophysical properties briefly described. Probably intrudes and is comagmatic with Mountain Creek Volcanics. Age from parent.||Unit in Gooramma Suite.|||Grey, medium-grained, massive, weakly porphyritic to equigranular, biotite-hornblende-augite-hypersthene granite. I-type.|
35343|Little Range Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgl. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Gooramma Suite|||Medium grained, massive, weakly porphyritic to equigranular, biotite-hornblende-augite-hypersthene granite; high magnetic susceptibility.|
35343|Little Range Granite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Medium grained, massive, weakly porphyritic to equigranular, biotite-hornblende-augite-hypersthene granite; high magnetic susceptibility.|
40986|Little Redbank Granodiorite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Massive porphyritic allanite (relic cores)-hornblende granodiorite and quartz-soda diorite.  See also Little Redbank Granite (in map strat. chart).||||||13-MAY-04
40986|Little Redbank Granodiorite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Gunning Suite. Blue-grey to dark grey , med- to coarse-gr., foliated, equigranular, hornblende-biotite granodiorite, minor aplite. Low K, Th and U radioelement response.||||||
40986|Little Redbank Granodiorite|68592|2|Defined|p1312-3, p1315-20, p1334-7, p1664|Early Silurian|Early Silurian|Formerly Little Redbank Tonalite (Yacopetti, 1987) and Little Redbank Granite (Chappell et al., 1991). Both these authors had included the Willdamar Tonalite and part of the Mulgowrie Granodiorite in their definitions. Present mapping has distinguished a western pluton, herein defined as the Little Redbank Granodiorite, and an eastern pluton now called the Willdamar Tonalite, separated by Mulgowrie Granodiorite. Type locality described. Geochemistry detailed; geophysical properties described. Not isotopically dated.||Unit in Gunning Suite.||Intrudes Adaminaby Group. Is intruded by Bishopthorpe Suite and Bigga Granite.|Blue-grey to dark-grey, medium- to coarse-grained, foliated, equigranular, hornblende-biotite granodiorite and tonalite. Narrow aplite veins, and mafic microgranitic enclaves up to 600mm long, are present. I-type.|
40986|Little Redbank Granodiorite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sgl. Error in Geological Reference Legend: shown as 'Sgl' Micalong Swamp Basic Igneous Complex. Should be 'Sgl' Little Redbank Granodiorite. It is correctly shown ('Sgl' Little Redbank Granodiorite) in the Time-Space Plot, on the Crookwell 1:100 000 sheet portion. This unit is shown on Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Gunning Suite|||Medium-coarse grained, foliated, equigranular, hornblende-biotite granodiorite and tonalite; minor aplite. low K, Th and U response; low magnetic susceptibility.|
40986|Little Redbank Granodiorite|70544|5|Briefly described|Map Legend|Devonian|Silurian|[Note that this is shown as part of the Micalong Suite on the Goulburn 1:250 000 map sheet key]||Gunning Suite|||Medium-coarse grained, foliated, equigranular, hornblende-biotite granodiorite and tonalite; minor aplite. low K, Th and U response; low magnetic susceptibility.|
28684|Little Tank Formation|42144|6|Mentioned|Fig.11 P615|||||||||
77259|Liverpool Range Volcanic Complex|68004|5|Briefly described|p156.|Tertiary|Tertiary|Hunter Coalfield. This unit caps a plateau which overlies gently WNW-dipping coal sequences which present a potential underground resource.||||Overlies Narrabeen Group.||
31599|Llanelly Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31599|Llanelly Suite|44093|5|Briefly described|p199 App. 1|Devonian|Late Silurian|Granite. Geological Province: Lachlan Fold Belt.||||||
76958|Llangothlin Monzogranite|69639|4|Described|p1, p6, p8, p32, p68, p95|Lopingian|Lopingian|New England Orogen. SHRIMP age is interpreted as a magmatic crystallisation age. Sample locality, petrography, and geochronology is described. See also p133-p138, p219-p220, p241.|253.1 +/- 1.5 Ma (SHRIMP)|Llangothlin Suite||Intrudes the Wandsworth Volcanics, Annalee Pyroclastics, Girrakool beds, Wards Mistake Monzogranite and the Yellow Cap Micromonzogranite.|Medium- to coarse-grained porphyritic hornblende-biotite granite (monzogranite).|
76958|Llangothlin Monzogranite|70217|5|Briefly described|p38, p73 tbl 14.1 |Changhsingian|Changhsingian|New England Orogen. Age derived from Chisholm et al, 2014b. |253.1 +/- 1.5 Ma (SHRIMP U-Pb)|Llangothlin Suite||||
76958|Llangothlin Monzogranite|71628|4|Described|p8: 4-6, 12-15, 17; p14:31|||Chisholm et al. (2014) after unpublished work by Chappell and Bryant (1994). Previously Llangothlin Adamellite of Binns et al. (1967) after unpublished work by Neilson (1965). Occurs N and E of Llangothlin village after which it is named. Covers ~48 km2 at high elevations, cropping out as small knolls. Petrology well-described; geochemistry described. Associated with stockwork and vein Mo(-Ag) mineralisation.|253.1 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Llangothlin Suite.||Intrudes Annalee Pyroclastics (Wandsworth Volcanics), and ?Girrakool beds, Wards Mistake Monzogranite and Yellow Gap Microleucomonzogranite.|Fine- to medium-grained, porphyritic to equigranular, biotite-hornblende monzogranite. I-type.|
74008|Llangothlin Suite|69639|6|Mentioned|p133|||||Uralla Supersuite|Includes the Llangothlin Monzogranite.|||
74008|Llangothlin Suite|70217|5|Briefly described|p38|||New England Orogen.||Uralla Supersuite|Includes the Wellingrove Granodiorite and the Llangothlin Monzogranite.|||
74008|Llangothlin Suite|71628|5|Briefly described|p8: 4-18, 118; p10:2; p12:2|||Borderline A-type granites.||Uralla Supersuite.|Llangothlin, Wellingrove Monzogranites; Aberfoyle River Porphyrite; Blackfellows Gully Leucomonzogranite.||Intermediate to felsic granites.|
35507|Lock Lomond Granite|24417|3|Fully described|p97|Early Devonian|Early Devonian|Of Milandra Granite.  Part of the Milandra Granite previously included in Eugowra Granite.||||||29-AUG-12
35507|Lock Lomond Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|Of the Eugowra Suite.||||||13-JUL-04
39352|Lockhart Igneous Complex|24116|5|Briefly described|p98|||||||||
39352|Lockhart Igneous Complex|24128|5|Briefly described|p56|||Geological Province: Lachlan Fold Belt.||||||
39352|Lockhart Igneous Complex|66300|5|Briefly described|pp17-28. |Silurian|Silurian|Lithologies in this unit display a variety of magma mixing and mingling relationships. Magmatic crystallisation age of this leucogranite phase (c.4 My younger than tonalite phase) is indistinguishable from Ellenden Granite and Woodlawn Volcanics.|424.4 +/- 3.2 Ma.|Unit in Thurralilly Suite.||Intrudes the Adaminaby Group.|Plutonic rocks ranging from olivine-bearing gabbro to leucogranite.|
39352|Lockhart Igneous Complex|68592|6|Mentioned|p24, p26|Silurian|Silurian|In the Braidwood 1:100 000 map area.||||||
39352|Lockhart Igneous Complex|69159|5|Briefly described|Map legend|Silurian|Silurian|Six un-named sub-units are mapped separately.||Unit in Thurralilly Suite.|||Weakly to strongly foliated, equigranular to porphyritic, biotite granite, granodiorite, leucogranite, hornblende+/-pyroxene olivine dolerite to gabbro and enclave-rich granodiorite to quartz diorite.|
39352|Lockhart Igneous Complex|69270|5|Briefly described|p1, p27|Late Silurian|Late Silurian|Tinderry Granite's Late Silurian age (423.3+/-2.2 Ma U-Pb, this volume) links temporally with other regional plutonic suites (e.g. Thurralilly Suite, which includes 428-424 Ma Lockhart Igneous Complex; Bodorkos et al., 2010). Dating: zircon U-Pb SHRIMP age.|428-424 Ma|Thurralilly Suite||||
39352|Lockhart Igneous Complex|71069|2|Defined|p21 fig 7, p28, p28 fig 10, p29|Ludlow|Wenlock|Named for the Lockhart property. Previously named the Lockhart Basic Intrusive Complex. Now incorporates rocks of the Boro Granite, Rossi Granodiorite and parts of the Butmaroo Granite.Tholeiitic geochemical affinity. Type locality given at GR 727672 6087400. Representative localities are given for each of the six unnamed sub-units. Ages are SHRIMP U-Pb from Bodorkos & Simpson, 2008. Lithology for constituent units given. Magmatism possibly related to rifting and the opening of the Goulburn Basin. Distribution, geomorphology, geochemistry, primary structures/textures, tectonic structure, metamorphism and geophysical characteristics discussed. See also p29 fig 11, p31, p36, p38 fig 15, p174-p189, p191.|424.4 +/- 3.2 Ma to 428.5 +/- 3.1 Ma |Thurralilly Suite||Part equivalent to the Briars Sharrow Gabbro, Ellenden Granite. Equivalent to the Butmaroo Granite, Tallaganda Granodiorite and Gourock Granodiorite.|Weakly to strongly foliated, equigranular to porphyritic biotite granite, granodiorite, leucogranite, hornblende-pyroxene-olivine dolerite to gabbro and enclave rich granodiorite to quartz dolerite.|
39352|Lockhart Igneous Complex|71691|5|Briefly described|Map legend.|Silurian|Silurian|Five un-named facies are mapped separately.||Thurralilly Suite.|||Weakly to strongly foliated, equigranular to porphyritic, biotite granite, granodiorite, leucogranite, hornblende +/- pyroxene olivine diorite to gabbro and enclave-rich granodiorite to quartz diorite.|
39352|Lockhart Igneous Complex|71699|5|Briefly described|Map legend.|Silurian|Silurian|Six un-named facies are mapped separately.||Thurralilly Suite.|||Weakly to strongly foliated, equigranular to  porphyritic, biotite granite, granodiorite, leucogranite, hornblende+/-pyroxene olivine diorite to gabbro and enclave-rich granodiorite to quartz diorite.|
39352|Lockhart Igneous Complex|71700|2|Defined|vi, viii, p7, p17-p18, p21-p22, CD|Late Silurian|Late Silurian|This unit is named for the "Lockhart" property. A type area for this unit was at approximately GR 727672 6087400 (Abell 1991). Numerous representative localities are also proposed.This unit was first named by Read (1961), the name was retained by Felton and Huleatt (1977) and Rigden (1976) mapped the area around Lockhart using this name. Abell (1991) formalised the name "lockhart Basic Intrusive Complex". This unit was formalised as the Lockhart Igneous Complex in this volume to include the Boro Granite, Rossi Granodiorite and the Butmaroo Granite. Distribution, geomorphic expression, outcrop, structure, geochemistry, geophysical characteristics and metamorphism are discussed. Lithology is described in detail. SHRIMP ages are derived from Bodorkos et al, 2010. See also p45, p47, p52-p53, p61, p65, p71, p74, p77-p78, p81, p83, p85.|424.4 +/- 3.2 Ma and 428.5 +/- 3.1 Ma|Thurralilly Suite||Intrudes the Abercrombie Formation.|Bi-modal intrusive and extrusive rocks including gabbro and dolerite.|
31604|Lockyersleigh Suite|42726|5|Briefly described|map legend||Carboniferous|||||||
31604|Lockyersleigh Suite|64238|5|Briefly described|Map legend|Carboniferous|Carboniferous|Contains the Lockyersleigh Granite.||||||
31604|Lockyersleigh Suite|68592|3|Fully described|p1754-8, p1760-7|Carboniferous|Early Carboniferous|Defined by Chappell et al. (1991) who included Lockyersleigh Adamellite and Chapmans Creek Granodiorite in the Suite. The Chapmans Creek Granodiorite has subsequently been incorporated as a marginal phase of the herein redefined Lockyersleigh Granite, the sole constituent (and hence type pluton) of this Suite.||Unit in Oberon Supersuite.|Includes Lockyersleigh Granite.||Undeformed, unfractionated, mafic, I-type granitoid.|
31604|Lockyersleigh Suite|70192|5|Briefly described|Map Legend|Carboniferous|Carbononiferous|On Taralga 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Lockyersleigh Granite.|||
31604|Lockyersleigh Suite|70542|5|Briefly described|Map Legend|Carboniferous|Carbononiferous||||Includes Lockyersleigh Granite.|||
34000|Loddon Sandstone|22578|5|Briefly described|p402, Fig.10 p400|||of Illawarra Coal Measures||||||
34000|Loddon Sandstone|24471|4|Described|p31 Fig.3|Late Permian|Late Permian|Overlies Lawrence Sandstone, overlain by Bulli Coal. Contains Cape Horn Coal Member and Balgownie Coal . Possibly stratigraphically equivalent to Moon Island Beach Formation. Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
34000|Loddon Sandstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
34000|Loddon Sandstone|68202|5|Briefly described|p177-185|Permian|Permian|Stratigraphic column; C, N, S, trace and rare earth elements, isotope data plots. Thin section photographs.||||Is overlain by Bulli Coal.|Includes fine-grained shale, massive to very finely laminated, dominated by clays with quartz and organic matter.|
34000|Loddon Sandstone|73304|6|Mentioned|p74, p77|||Sydney Basin, southern.||Illawarra Coal Measures||||
34000|Loddon Sandstone|73421|6|Mentioned|p19|Changhsingian|Wuchiapingian|Sydney Basin, southern.||Sydney Subgroup||||
27468|Loder Coal Member|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
27468|Loder Coal Member|40331|6|Mentioned|p5|||||||||
27468|Loder Coal Member|70791|5|Briefly described|p285, p293 Fig.17|Permian|Permian|Muswellbrook area. Has similarities with Bibblewindi Coal Member (Mullaley Sub-basin). Appears as Lodder in Fig.17.||Skeletar Formation||||
23737|Long Beach Formation|22815|5|Briefly described|p115|Early Miocene|Early Miocene|||||||
23737|Long Beach Formation|22943|6|Mentioned|p516-7||Early Miocene|||||||
23737|Long Beach Formation|23349|6|Mentioned|252|Oligocene|Oligocene|||||||
23737|Long Beach Formation|24343|5|Briefly described|p63, p65 Fig. 2|Early Miocene|Early Miocene|||||||
23737|Long Beach Formation|42786|4|Described|p359, p364|||see also Fig.1 P358||||||
35394|Long Mountain Breccia Member|61392|5|Briefly described|p163, p165 Fig. 1|||A separate unit that forms the lower 300m of the Bromley Hills Formation.||||||07-FEB-11
35394|Long Mountain Breccia Member|63731|5|Briefly described|Map legend||Silurian|Of Bromley Hills Volcanics (Silverwood Group). Polymictic megabreccia containing sedimentary as well as basaltic to andesitic clasts and cross-stratified pebbly arenite.||||||13-DEC-07
35394|Long Mountain Breccia Member|63748|4|Described|p9||Middle Devonian|Of Bromley Hills Formation (Silverwood Group). Thickness 350m. Geol.Prov: Silverwood province. Polymictic megabreccia capped by 60m of cross-stratified pebbly arenite.||||||07-FEB-11
35394|Long Mountain Breccia Member|68679|5|Briefly described|p447|Middle Devonian|Middle Devonian|Silverwood Province. 350m thick.||Basal Bromley Hills Formation.|||Polymict megabreccia containing basaltic to andesitic fragments and various clastic sedimentary blocks (debris flows initiated by catastrophic collapse along the margins of a stratovolcano), capped by 60m of cross-stratified pebbly sandstone.|
27292|Long Swamp Creek Formation|22815|4|Described|p102|Late Devonian|Late Devonian|||||||
27292|Long Swamp Creek Formation|22857|5|Briefly described|p216, p494 App. 1 Tb.A1.7|Frasnian|Frasnian|Of the Minuma Range Group. Grey-brown mudstone and shale interbeds, with lithic quartz arenite, locally feldspathic. Max. thickness: 150m. Geological Province: Lambie Shelf. NOTE: Not to be confused with Long Swamp Formation (Illawarra Coal Measures). ||||||
27292|Long Swamp Creek Formation|22859|5|Briefly described|p216|||||||||
27292|Long Swamp Creek Formation|39028|6|Mentioned|Map legend|Famennian|Famennian|||||||
27292|Long Swamp Creek Formation|40276|2|Defined|p23|Late Devonian|Late Devonian|||||||
27292|Long Swamp Creek Formation|42497|5|Briefly described|Map Legend|Frasnian|Frasnian|||||||
27292|Long Swamp Creek Formation|43233|5|Briefly described|Map Legend||Late Devonian|||||||
27292|Long Swamp Creek Formation|68298|5|Briefly described|p214, 215|||Contains marine sediments and fish fauna.||||||
27292|Long Swamp Creek Formation|71700|5|Briefly described|CD|Late Devonian|Late Devonian|Ages derived from fossil assemblage.||Minuma Range Group||Unconformably overlain by the Curmulee Conglomerate. Conformably overlain by the Gundillion Conglomerate.||
27292|Long Swamp Creek Formation|73181|6|Mentioned|p65-66|Frasnian|Frasnian|Contains invertebrate fossils.||Minuma Range Group||Underlain by Gundillion Conglomerate. Overlain by Curmulee Conglomerate. Equivalent to Long Swamp Creek Formation.||
24613|Long Swamp Formation|22578|6|Mentioned|p398|||||||||
24613|Long Swamp Formation|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Charbon Subgroup (Illawarra Coal Measures). Claystone, siltstone, mudstone, thin coal; bioturbation. Max. thickness: 40m. Geological Province: Sydney Basin. NOTE: Not to be confused with Long Swamp Creek Formation (Minuma Range Group). ||||||
24613|Long Swamp Formation|23214|4|Described|p268|Late Permian|Late Permian|Of Illawarra Coal Measures.  Consists mostly of claystone and mudstone commonly interlaminated and thinly interbedded.  Geological Province: Sydney Basin. Maximum thickness: 20m.||||||
24613|Long Swamp Formation|39232|4|Described|p109|||See also P108||||||
24613|Long Swamp Formation|40256|6|Mentioned|p305|||||||||
24613|Long Swamp Formation|40332|6|Mentioned|p21|||||||||
24613|Long Swamp Formation|40806|2|Defined|p154|Permian|Permian|Prob. Permian||||||
24613|Long Swamp Formation|42657|4|Described|p78|||||||||
24613|Long Swamp Formation|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
24613|Long Swamp Formation|43641|5|Briefly described|Map Legend||Permian|||||||
24613|Long Swamp Formation|43782|6|Mentioned|Map diagram|Late Permian|Late Permian|of Illawarra Coal Measures.||||||
24613|Long Swamp Formation|68004|5|Briefly described|p61.|Late Permian|Late Permian|Western Coalfield. Over 60 m thick in the east, thinning near the western margin of the Basin. West of Wollar Hingeline, forms a thin layer within the Ulan Coal.|||||Bioturbated claystone and siltstone, tuff, sandstone and thin discontinuous coal layers.|
23738|Long Tunnel Metabasic Igneous Complex|22857|4|Described|p452 App.1, Tb.A1.6|Middle Silurian|Silurian|Metabasalt, meta-andesite, minor keratophyre, serpentinite and sediments. Basement of the Tumut Trough.||||||
23738|Long Tunnel Metabasic Igneous Complex|37529|5|Briefly described|p7|||||||||
23738|Long Tunnel Metabasic Igneous Complex|42045|6|Mentioned|Fig.2 P148|||||||||
23738|Long Tunnel Metabasic Igneous Complex|42313|2|Defined|p57|Late Silurian|Middle Silurian|Age: early Middle Silurian to Late Silurian||||||
23738|Long Tunnel Metabasic Igneous Complex|42314|5|Briefly described|Map|Early Silurian|Middle Silurian|||||||
23738|Long Tunnel Metabasic Igneous Complex|69635|5|Briefly described|p48, 49|||Tumut Trough, Eastern Lachlan Orogen. Location of Kimo Diorite sample originally considered to be in this unit. Abbreviated as Long Tunnel Igneous Complex p1.|419.1+/-2.7 Ma minimum age|||Interpreted to be intruded by Kimo Diorite.||
38203|Longford Creek Siltstone Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Geological Province: Sydney Basin||||||
38203|Longford Creek Siltstone Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Lucernia Coal. Geological Province: Sydney Basin||||||
38203|Longford Creek Siltstone Member|68004|5|Briefly described|p51 Table 5, p53.|Late Permian|Late Permian|Upper Hunter Coalfield. The rank 'Member' is missing in table 5.||Unit in Lucernia Coal.||Overlies Rombo Coal Member. Is overlain by Eyriebower Coal Member.||
36331|Longreach Volcanics|50234|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Mount Fairy Group.  Includes: Bulls Pit Limestone Member.||||||
36331|Longreach Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Amygdaloidal glomeroporphyritic basalt lava, minor siltstone,siliceous volcanic breccia and fine-grained vitric rhyolitic tuff.||||||03-JUN-08
36331|Longreach Volcanics|68592|2|Defined|p726, p728, p842-50, p868, p916|Lochkovian|Lochkovian|New name. Originally informally termed 'Longreach Volcanics' by O'Reilly (1972). Limited distribution and crops out poorly. Type section/locality/area: reasonable outcrop occurs. Thickness: ~900 m, estimate difficult due to poor outcrop and faulting. Shallowing marine depositional environment. Is intruded by Lockyersleigh Granite and Billyrambija Dolerite. Albite-epidote hornfels facies conditions developed in aureole to Lockyersleigh Granite. Age: possible early Lochkovian age is indicated by conodont faunas from Brayton Limestone Member.||Unit in Mount Fairy Group.|Includes Brayton Limestone Member.|Faulted lower contact with Covan Creek Formation and upper contact with Barrallier and Joaramin Ignimbrites. Is disconformably overlain by Crookwell Basalt.|Porphyritic basaltic to (?)calc-alkaline andesitic lavas and associated volcanic conglomerate and minor interbedded siltstone; rhyolitic vitric tuff occurs at or near base of sequence.|
36331|Longreach Volcanics|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfl. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Mount Fairy Group|Includes Brayton Limestone Member.||Massive-flow banded, amygdaloidal, glomeroporphyritic basalt to andesite, minor siltstone, siliceous volcanic breccia and fine grained vitric, rhyolitic tuff; rare limestone.|
36331|Longreach Volcanics|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|Includes Brayton Limestone Member||Massive-flow banded, amygdaloidal, glomeroporphyritic basalt to andesite, minor siltstone, siliceous volcanic breccia and fine grained vitric, rhyolitic tuff; rare limestone.|
36331|Longreach Volcanics|71069|6|Mentioned|p133, p140 tbl 4, p163|||||Mount Fairy Group||||
36331|Longreach Volcanics|71656|5|Briefly described|p13 Fig.2, p30|Pragian|Lochkovian|Sampling of this unit exposed in the Longreach limestone quarry on the Goulburn 1:100,000 mapsheet, yielded four conodont elements.||Mount Fairy Group|Includes Brayton Limestone Member.|Laterally equivalent to Rhyanna Formation, Gundary Volcanics.|Volcanics containing fossiliferous limestone.|
41066|Looanga Monzogranite|24366|5|Briefly described|p16 Fig. 3|Early Triassic|Late Permian|Of the Moonbi Plutonic Suite.||||||
41066|Looanga Monzogranite|68005|5|Briefly described|p67, p133.|Permian|Permian|Listed on p.133 as a unit in Moonbi Supersuite.||Unit in Southern Moonbi Supersuite.|||Medium- to coarse-grained equigranular biotite(-hornblende) monzogranite.|
41066|Looanga Monzogranite|68111|5|Briefly described|p968 Tb.1|Anisian|Anisian||ca. 247 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
41066|Looanga Monzogranite|71628|4|Described|p4:15; p7: 1, 27-30; p19:136|||Originally Looanga Adamellite (Chesnut et al., 1973). Subsequently Looanga Leucoadamellite (Flinter, 1982) then Looanga Monzogranite (Brown, 2003 after Chappell and Bryant, 1994). Named for the parish of Looanga. Forms a narrow, elongated 26 km2 mass ~15 km NE of Bendemeer. Excellent exposures along New England Highway; pavements and tors in neighbouring farmland. Geochemistry described; has similarities with felsic phases of Bendemeer Monzogranite.|246.7 Ma (Rb-Sr biotite: Shaw and Flood, 1993).|Moonbi Suite.||Intrudes Flaggy Range Monzogranite Phase (Banalasta Monzogranite).|Grey to pale grey, medium- to coarse-grained, porphyritic, leucocratic biotite-hornblende monzogranite. I-type.|
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.|
25692|Looney Intrusive Complex|730|6|Mentioned|p22 Fig.5.|||||||||11-NOV-14
25692|Looney Intrusive Complex|22519|5|Briefly described|p8|||||||||
25692|Looney Intrusive Complex|22831|4|Described|p48|Early Devonian|Early Devonian|||||||01-NOV-13
25692|Looney Intrusive Complex|40365|2|Defined|p326|Early Devonian|Early Devonian|||||||
25692|Looney Intrusive Complex|40682|6|Mentioned|Fig.1|||||||||
25692|Looney Intrusive Complex|42912|6|Mentioned|Fig.1|||||||||
25692|Looney Intrusive Complex|44160|5|Briefly described|Map Legend||Lochkovian|||||||08-JAN-10
83554|Lord Howe Volcanic Complex|73554|5|Briefly described|Map legend, back of map|Neogene|Neogene|||||||
31715|Lords Granite|24417|3|Fully described|p95|Early Devonian|Early Devonian|Of Eugowra Suite.  Previously included in the Eugowra Granite.||||||
31715|Lords Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|Of the Eugowra Suite.||||||13-JUL-04
31715|Lords Granite|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Boggy Plain Supersuite||||
82510|Lorne Forest Granodiorite|71628|5|Briefly described|p17: 2, 76, 78-79, 81, 83|||New name, after work by Knutson (1975). Named after the Lorne State Forest. Forms a ~23 km2 body c.12 km NW of Laurieton.||The Brothers Suite.||Intrudes Pappinbarra, Hyndmans Creek and Mingaletta Formations.|Porphyritic hornblende quartz monzonite and hornblende micromonzogranite.|
23741|Lostock Sandstone Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Of the Flagstaff Formation. Calcareous sandstone, grey mudstone, coarse lithic sandstone. Max. thickness: 930m. Geological Province: Tamworth Forearc Basin.||||||
23741|Lostock Sandstone Member|40883|6|Mentioned|p7|||||||||
23741|Lostock Sandstone Member|43576|6|Mentioned|p350|||||||||
23741|Lostock Sandstone Member|44244|4|Described|p72-73|Visean|Visean|Of the Flagstaff Formation.  Contains the Verulam Oolite Member (of the Wootton beds).  Overlies the Bandon Grove Limestone Member; underlies the Chichester Formation.  Max. thickness: 930m.  Type section in text.  Geological Province: Gresford Block.||||||
23741|Lostock Sandstone Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Flagstaff Formation.  Grey, cross-stratified lithic sandstone with thin interbeds of of grey mudstone containing the Verulam Oolite Member.  Geological Province: Gresford Block.||||||
27183|Loughmore Formation|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Coorabin Coal Measures. Pebble sandstone, siltstone and claystone. Max. thickness: 13m. Geological Province: Ovens Graben.||||||
27183|Loughmore Formation|35498|2|Defined|p144|Late Permian|Late Permian|||||||
27183|Loughmore Formation|35503|6|Mentioned|p202|||Defined in Standing Committee Coalfield Geology NSW (1978)||||||
27183|Loughmore Formation|38293|5|Briefly described|p20|||||||||
27183|Loughmore Formation|42966|4|Described|p64|||of Coorabin Coal Measures||||||
27183|Loughmore Formation|69798|5|Briefly described|p4 Fig.2|Permian|Permian|Oaklands Basin.||Coorabin Coal Measures.|Coreen Creek Coal Member.|||
79635|Louth Group|70821|5|Briefly described|p9, p12|Late Ordovician|Late Ordovician|Age given as Upper Ordovician? Interpreted as broad areas of complex trends of low to moderate magnetic intensity.|||||Siliciclastic metasedimentary rocks with intercalated mafic horizon flows, sills and dykes.|
78367|Louth Volcanics|69001|6|Mentioned|p24|||||||||
78367|Louth Volcanics|69002|6|Mentioned|p15, p16||Pridoli|See also Louth volcanics. Contains a concordant 422 Ma zircon in volcanogenic sandstone which provides a maximum age for ?most/all of the Louth Volcanics.|< 422 Ma?|||||
78367|Louth Volcanics|69042|6|Mentioned|map|||Accidentally capitalised on map face? Shown as informal Louth volcanics in map legends.||||||06-NOV-13
78367|Louth Volcanics|70602|6|Mentioned|p67,75|Paleozoic|Paleozoic|Age inferred from Map Unit.||||||28-JUN-16
78367|Louth Volcanics|70821|5|Briefly described|p12|Early Devonian|Late Silurian|Louth area. Characterised by linear trends of moderate to high magnetic intensity.|||||Basalt and basaltic andesites, volcanoclastic rocks and dolerite.|
78367|Louth Volcanics|71860|6|Mentioned|p6|||||||||
78367|Louth Volcanics|71965|5|Briefly described|p896,899,901-902,904,912-914|Silurian|Ordovician|Geological province: Thomson Orogen. Siliciclastic and volcanic-dominated sequences and mafic intrusions, that can be observed as curvilinear trends of moderate to high magnetic intensity and small discrete magnetic highs. Magnetic trends indicate one generation of tight to isoclinal folding, with later open folding. Sandstone samples from drill hole L2 yielded a maximum depositional age of c. 422 Ma (sample Louth A, in Glen et al., 2013), consistent with presence of Pridoli to Lochkovian conodonts (Brunker 1968). Contains basalts with MORB signatures, and mafic-intrusives with calc-alkaline affinities. Reflects voluminous and widespread magmatism from late Silurian to early Devonian.|c. 422 Ma||||Gabbro, basalt/andesite, volcaniclastic sediments, carbonaceous mudstone, limestone; mafic intrusions include stocks, sills, dykes and diatremes.|29-OCT-19
78367|Louth Volcanics|71966|6|Mentioned|p990|Early Devonian|Early Devonian|Geological province: southern Thomson Orogen.|c. 415-400 Ma|||||
78367|Louth Volcanics|72951|6|Mentioned|p1010|||||||||
78367|Louth Volcanics|73175|4|Described|p1049-1053, p1055, 1059-1063, p1066|Triassic|Early Devonian|Thomson Orogen, southern. Consists of two main belts of high magnetic intensity that are complexly folded. Formed in a deep-water marine setting synchronous with sedimentation. Two groups of temporally and compositionally distinct igneous rocks are distinguished. Calc-alkaline assemblage assigned a Lower Devonian age of ca 415-410 Ma forms a semi-coherent stratigraphic assemblage, U-Pb LA-ICPMS zircon ages of 411 +/- 6.3 Ma and 414 +/- 9.3 Ma, eNd (t) values of 2.6 and 3.1. Alkaline assemblage assigned a Permian-Triassic age of 260-240 Ma, 261 +/- 8.2 Ma and 242 +/- 7.9 Ma U-Pb LA-ICPMS zircon ages, eNd (t) values of 1.2 - 3.1. Alkaline group forms small, discrete magnetic anomalies interpreted as diatremes and plug-like bodies, previously considered Neoproterozoic but contains abundant xenocrystic zircons. Consistent Nd model ages of 960-830 Ma. Location in text includes p1064 Fig.11.|414 +/- 9.3 Ma, 243 +/- 5.6 Ma LA-ICP-MS, zircon||||Alkaline intrusives and volcanics, typically doleritic to gabbroic, with breccia. Calc-alkaline rocks include dolerite and gabbro, are more intensely altered and deformed. Includes tuffs, interlayered sedimentary rock, volcanogenic sedimentary rocks.|26-SEP-22
78367|Louth Volcanics|73179|6|Mentioned|p1152|Emsian|Pragian|Geochron is a maximum depositional age for a volcaniclastic sandstone.|402.0 +/- 5.2 Ma||||Includes volcaniclastic sandstone.|19-SEP-22
78374|Louth volcanics|69002|5|Briefly described|p3, p14, Map 1b, Legend|Devonian|Ordovician|See also Louth Volcanics. Informal name. Represented by zones of both linear and irregular magnetic anomalies. Age based on conodonts in limestone fragments.|||||Comprises volcanics, volcaniclastics, and dolerite.|
78374|Louth volcanics|69042|5|Briefly described|map legends|Devonian|Ordovician|LV. Thomson Orogen. Zones containing both linear and irregular magnetic anomalies. Volcanics, volcaniclastics and dolerite. Age shown as ?Ordovician-Devonian.||||||
78374|Louth volcanics|69043|6|Mentioned|p11|||Thomson Orogen.||||||
78374|Louth volcanics|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Late Silurian|Thomson Orogen.||||||
29592|Lucan Complex|23214|3|Fully described|p162||Late Silurian|Intrudes the Swan Ponds Tonalite. Geological Province: Wyangala Batholith||||||
29592|Lucan Complex|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of granodiorite, porphyritic tonalite, rhyodacite.||||||17-JUL-08
29592|Lucan Complex|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyangala Batholith.||||||17-JUL-08
29592|Lucan Complex|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
26001|Lucas Creek Granite|22815|5|Briefly described|p44|Silurian|Silurian|||||||
26001|Lucas Creek Granite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
26001|Lucas Creek Granite|35109|4|Described|p81|||||||||
26001|Lucas Creek Granite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
26001|Lucas Creek Granite|36443|5|Briefly described|map legend|Lochkovian|Pridolian|Of Kosciusko Batholith. Leucogranite, adamellite. BMR map code: Slg.||||||
26001|Lucas Creek Granite|40328|4|Described|p208|||||||||
26001|Lucas Creek Granite|42726|5|Briefly described|map legend|Silurian||358.  Of the Bullenbalong Suite (Bullenbalong Supersuite).||||||08-FEB-05
26001|Lucas Creek Granite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
26001|Lucas Creek Granite|44092|5|Briefly described|map legend|Silurian|Silurian|glw4||||||
26001|Lucas Creek Granite|45147|2|Defined|M231|Late Silurian|Late Silurian|Refers previous undefined usage. Probably Late Silurian.||||||19-FEB-13
26001|Lucas Creek Granite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Murrumbidgee Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
26001|Lucas Creek Granite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||15-JUL-04
26002|Lumga Siltstone|22857|4|Described|p440 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Walters Range Group (Cobar Supergroup). Thin-bedded siltstone, interbedded quartz-rich medium-graimed arenite, minor flaggy arenite. Max. thickness: >300m. Geological Province: Darling Basin. ||||||
26002|Lumga Siltstone|41394|2|Defined|p98|Pragian||Reserved as Lumga Formation||||||
26002|Lumga Siltstone|41395|6|Mentioned|Map legend|Pragian||||||||
26002|Lumga Siltstone|61964|5|Briefly described|p104|||Of the Walters Range Group on KILPARNEY 1:100k sheet.||||||23-SEP-19
26002|Lumga Siltstone|70751|6|Mentioned|p12|Pragian|Lochkovian|||Walters Range Group||||
26002|Lumga Siltstone|72958|6|Mentioned|p11|Emsian|Lochkovian|Cobar Basin. Nymagee area.||Walters Range Group||Overlain by Crowl Creek Formation (Mulga Downs Group). Overlain by and equivalent to Yar Sandstone and Whoey Tank Formation. Equivalent to Winduck Group.||
26003|Luton Formation|721|5|Briefly described|Map legend|Tournaisian|Tournaisian|Of the Parry Group.  Lithic, feldspathic and calcareous sandstones and siltstones interbedded with mudstones.||||||
26003|Luton Formation|22572|6|Mentioned|p108||Carboniferous|||||||
26003|Luton Formation|22857|5|Briefly described|p496 App.1 Tb.A1.7|Tournaisian|Tournaisian|Of the Parry Group. Lithic, feldspathic and calcareous sandstone and sitlstone interbedded with mudstone. Max. thickness: 560m. Geological Province: Tamworth Forearc Basin.||||||
26003|Luton Formation|23051|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Parry Group.||||||
26003|Luton Formation|23185|6|Mentioned|Fig5p161||Famennian|||||||
26003|Luton Formation|23522|5|Briefly described|p249 Fig 5|Early Carboniferous|Late Devonian|||||||
26003|Luton Formation|24010|5|Briefly described|p379|Early Carboniferous|Early Carboniferous|||||||
26003|Luton Formation|24605|5|Briefly described|p932 Fig.1|Tournaisian|Tournaisian|Geological Province: New England Orogen.||||||
26003|Luton Formation|24614|6|Mentioned|p204|||Overlies the Mandowa Formation.||||||07-FEB-11
26003|Luton Formation|30133|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26003|Luton Formation|30135|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26003|Luton Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26003|Luton Formation|31802|6|Mentioned|p134|||Latest Dev. - Early Carb. Equiv. Tangaratta Fm.||||||
26003|Luton Formation|31999|6|Mentioned|p151|||Table 1||||||
26003|Luton Formation|32602|5|Briefly described|p66|||Fammenian. Fauna||||||
26003|Luton Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26003|Luton Formation|32672|6|Mentioned|p674|||||||||
26003|Luton Formation|32865|4|Described|p481|||Dev.-Carb.||||||
26003|Luton Formation|32866|6|Mentioned|p9|||Fossil content||||||
26003|Luton Formation|32867|6|Mentioned|p26|||||||||
26003|Luton Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
26003|Luton Formation|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
26003|Luton Formation|34349|4|Described|p246|||||||||
26003|Luton Formation|34555|6|Mentioned|p240|||||||||
26003|Luton Formation|36057|6|Mentioned|p350|||||||||
26003|Luton Formation|36528|6|Mentioned|p175|||||||||
26003|Luton Formation|37987|2|Defined|p226|Carboniferous|Carboniferous|||||||
26003|Luton Formation|38215|6|Mentioned|p278|||||||||
26003|Luton Formation|38222|6|Mentioned|Fig.2|||||||||
26003|Luton Formation|39331|6|Mentioned|Table 10-1|||||||||
26003|Luton Formation|39468|6|Mentioned|Fig.2|||||||||
26003|Luton Formation|40328|6|Mentioned|p198|||||||||
26003|Luton Formation|41009|6|Mentioned|Fig.2|||||||||
26003|Luton Formation|41990|6|Mentioned|p13|||||||||
26003|Luton Formation|42547|4|Described|p15|Tournaisian|Tournaisian|Rocky Creek Syncline. Age: early to late Tournaisian||||||
26003|Luton Formation|42728|4|Described|p6|||||||||
26003|Luton Formation|43091|5|Briefly described|Map legend|||Of Parry Group.||||||04-FEB-08
26003|Luton Formation|43383|14|Not recorded|p17|||||||||
26003|Luton Formation|43428|14|Not recorded|p141|||||||||
26003|Luton Formation|43429|14|Not recorded|Map Legend|||>4000ft thick. Turbidites at base, up to traction current deposits at top||||||
26003|Luton Formation|43434|2|Defined|Map Legend||Carboniferous|Equivalent to Tangaratta Formation||||||
26003|Luton Formation|43435|2|Defined|Map Legend||Carboniferous|||||||
26003|Luton Formation|43436|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
26003|Luton Formation|43479|14|Not recorded|p177||Tournaisian|||||||
26003|Luton Formation|43538|14|Not recorded|p2|||Lower Carboniferous fauna.||||||
26003|Luton Formation|45097|6|Mentioned|p24|||Fauna Corrrelation chart||||||
26003|Luton Formation|46803|6|Mentioned|Fig. 3|||||||||
26003|Luton Formation|47056|6|Mentioned|Fig.2 P523|||||||||
26003|Luton Formation|63832|5|Briefly described|p131 fig 2|Tournaisian|Tournaisian|Rocky Creek Syncline, Southern New England Fold Belt.||||Is overlain by Namoi Formation.|Includes continental coal-bearing successions deposited between P1 and P2 glaciations.|13-DEC-17
26003|Luton Formation|64631|5|Briefly described|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Belt, Rocky Creek Syncline. Some biostratigraphic age control within unit. Time transgressive top?||||Is overlain by Namoi Formation.||
26003|Luton Formation|65214|6|Mentioned|p280|Devonian|Devonian|NSW, Tamworth and Keepit. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26003|Luton Formation|68003|5|Briefly described|p32 Fig.3-h, p34 Photo.3-d, p138.|Tournaisian|Tournaisian|Tamworth Belt (North), New England Fold Belt. Coeval with Tulcumba Sandstone.||Unit in Parry Group.||Overlies Mandowa Mudstone. Is overlain by Namoi Formation.|Calcareous and arkosic arenite, siltstone and claystone with orthoconglomerate towards the base; rare limestone lenses and tuff; laminite extensively developed in the north.|
26003|Luton Formation|68005|5|Briefly described|p26 Fig.3-C, p54, p148, p170.|Tournaisian|Tournaisian|Central Block, New England Fold Belt. Occurs north of Barraba. Broadly equivalent to Tangaratta Formation and Tulcumba Sandstone.||||Overlies Mandowa Mudstone. Is overlain by Tulcumba Sandstone.|Calcareous and arkosic arenite, siltstone and claystone with orthoconglomerate towards the base; rare limestone lenses and tuff; laminite extensively developed in the north.|
26003|Luton Formation|69793|6|Mentioned|p1121 Fig.12|Tournaisian|Tournaisian|Rocky Creek Block, Tamworth Belt.||||||
26003|Luton Formation|70050|5|Briefly described|p325, p327, p364, p366|Tournaisian|Tournaisian|Type locality is Slaughterhouse Creek near Gravesend, NSW. Contains Cionodendron coral fossils (illustrations and systematic palaeontology), including the holotype of C. columen. |||||Includes fossiliferous limestone beds at the top of the Formation.|
26003|Luton Formation|70728|5|Briefly described|p265|Tournaisian|Tournaisian|Geological province: North Tamworth terrane, New England Orogen.||||Overlain by Namoi Formation.||
26003|Luton Formation|70907|6|Mentioned|p774 Fig.2|||||||||
36776|Lynwood Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Part of the Marulan Batholith.||||||12-MAY-04
82565|MacDonald River Monzogranite|71628|5|Briefly described|p4: 1, 5, 8-10, 14-15, 37-39|||New unit. Incorporates more mafic parts previously part of Banalasta and Pringles Monzogranites. Named after a local watercourse. Occurs on the very S margin of Bundarra Supersuite; unmapped: defined by geochemical characteristics. Southern New England Orogen. Only generic Supersuite lithology described. Geochemistry described.||MacDonald River Suite.||Intrudes Woolomin beds. Abuts Banalasta and Pringles Monzogranites.|Coarse-grained biotite (+/- muscovite, +/- cordierite) monzogranite.|
35406|Macclesfield Granite|50231|5|Briefly described|Map Legend|Emsian|Pragian|||||||
35406|Macclesfield Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Pinkish, medium-grained, massive, porphyritic biotite granite.||||||09-SEP-08
35406|Macclesfield Granite|68592|3|Fully described|p1398, p1401-3, p1439|Early Devonian|Early Devonian|New unit and name, after Macclesfield property. Type locality described. Geochemistry detailed; geophysical properties described. Age from parent. Thought to intrude Mountain Creek Volcanics.||Unit in Gooramma Suite.|||Pinkish, medium-grained, massive, porphyritic, leucocratic granite. I-type.|
35406|Macclesfield Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgm. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Gooramma Suite|||Medium grained, massive, porphyritic, leucocratic granite; moderate-high magnetic susceptibility.|
35406|Macclesfield Granite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Medium grained, massive, porphyritic, leucocratic granite; moderate-high magnetic susceptibility.|
73750|Maccullochs Range beds|63632|5|Briefly described|649|Early Devonian|Late Silurian|Attributed to the Winduck Interval of Bembrick (1997). Almost entirely alluvial-fan deposits - grey and grey-brown, fine-grained sheet-flood sandstones - 4 lithofacies distinguishable; fossils rare.  Min. age probably Pragian. Geol. prov: Darling Basin||||||16-OCT-07
73750|Maccullochs Range beds|66589|6|Mentioned|p179|Praghian|Lochkovian|Case studies cited; not visited in the field by the authors of this study.||||||
81953|Macha Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|Includes the Belougery Split Rock Member and the Danu Rhyolite Member and two other unnamed sub-units.||Orange to white weathering, porphyritic to equigranular quartz trachyte to rhyolite lava deposits and intrusions with minor autobreccia.|02-NOV-20
38266|Mackenzie Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Coarse-grained, porphyritic hornblende-biotite monzogranite.  An I-tyope granitoid.||||||20-DEC-04
38266|Mackenzie Monzogranite|23812|5|Briefly described|p19 Tb.2, p71|Early Triassic|Early Triassic|Age: 244-238Ma (Rb-Sr).||||||
38266|Mackenzie Monzogranite|68111|5|Briefly described|p968 Tb.1|Wuchiapingian|Changhsingian|U-Pb SHRIMP geochronology (Geoscience Australia dataset).|251.7 +/- 2.1 Ma|Of the Stanthorpe Supersuite.||||
27825|Mackeys Creek Shale|22857|4|Described|p456 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Cudal Group. Quartzose shale, siltstone, minor sandstone. Max. thickness: 200m. Geological Province: Cowra Trough. ||||||
27825|Mackeys Creek Shale|23043|5|Briefly described|Map Legend|Ludlow|Wenlock|of Cudal Group.||||||
27825|Mackeys Creek Shale|23170|2|Defined|p105|Ludlow|Ludlow|of Cudal Group.||||||
27825|Mackeys Creek Shale|23214|3|Fully described|p123|Ludlow|Ludlow|Of Cudal Group. Parts of this unit were previously included in the Nora Formation and the Mandagery Cherts. 150m thick at type section.  Overlying unit: Goonigal Group, underlying unit: Kurrajong Park Formation.||||||
27825|Mackeys Creek Shale|32986|6|Mentioned|p6|||Geological map. Ludlovian||||||
27825|Mackeys Creek Shale|33116|6|Mentioned|Fig.12|||Correlation||||||
27825|Mackeys Creek Shale|33326|6|Mentioned|p443|||Fauna.||||||
27825|Mackeys Creek Shale|37727|5|Briefly described|p69|||||||||
27825|Mackeys Creek Shale|40328|3|Fully described|p84|||||||||
27825|Mackeys Creek Shale|43494|6|Mentioned|p20, p21|Silurian|Silurian|Overlain by Jews Creek Volcanics. Contains Monograptus bohemicus fossils.||||||16-MAR-06
27825|Mackeys Creek Shale|43640|5|Briefly described|Map Legend||Silurian|||||||
27825|Mackeys Creek Shale|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|of Cudal Group.||||||
27825|Mackeys Creek Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group||||
27826|Macquarie Park Sandstone|22857|5|Briefly described|p492 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Black Rock Subgroup (Catombal Group). Arenite and siltstone. Max. thickness: 550m. Geological Province: Lambie Shelf.||||||
27826|Macquarie Park Sandstone|23043|5|Briefly described|Map Legend|Famennian|Famennian|Of Black Rock Subgroup, Catombal Group.||||||17-JUL-08
27826|Macquarie Park Sandstone|23170|2|Defined|p251|Famennian|Famennian|Of Black Rock Subgroup.||||||17-JUL-08
27826|Macquarie Park Sandstone|23214|2|Defined|p235|Late Devonian|Late Devonian|Of Black Rock Subgroup. Supersedes Columbine Sandstone and includes Coffee Hill Member. Max. thickness 160m.||||||
27826|Macquarie Park Sandstone|24247|5|Briefly described|p37|Late Devonian|Late Devonian|See also p40 Fig.3. Fossil evidence suggests age is Famennian. Parent: Black Rock Subgroup (Catombal Group)||||||
27826|Macquarie Park Sandstone|32151|6|Mentioned|p209|||Refers Conolly in Packham (1969)||||||
27826|Macquarie Park Sandstone|32708|6|Mentioned|Fig.6|||||||||
27826|Macquarie Park Sandstone|32865|6|Mentioned|p483|||Fauna||||||
27826|Macquarie Park Sandstone|33732|4|Described|p120|||See also P119.||||||
27826|Macquarie Park Sandstone|34109|4|Described|p159|||See also Fig.3.17||||||
27826|Macquarie Park Sandstone|35246|6|Mentioned|p172|||||||||
27826|Macquarie Park Sandstone|43509|14|Not recorded|p113,Pl.I||Late Devonian|Unit of Catombal Group||||||
27826|Macquarie Park Sandstone|43511|14|Not recorded|p139||Late Devonian|||||||
27826|Macquarie Park Sandstone|43512|2|Defined|p73,77-9,82-7,94,||Late Devonian|White & red orthoquartzites, protoquartzites and lithic ss, white & red siltstones and shaly bands. p96-106||||||22-JAN-13
27826|Macquarie Park Sandstone|43513|14|Not recorded|p72|||||||||
27826|Macquarie Park Sandstone|43640|5|Briefly described|Map Legend||Devonian|||||||
27826|Macquarie Park Sandstone|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Catombal Group, Black Rock Subgroup. Consists of massive to bedded, fine to medium-grained quartz sandstone.||||||06-AUG-08
27826|Macquarie Park Sandstone|43782|6|Mentioned|Map diagram|Famennian|Frasnian|Of Black Rock Subgroup.||||||17-JUL-08
27826|Macquarie Park Sandstone|68592|5|Briefly described|p1737-8|Late Devonian|Late Devonian|Pogson and Watkins (1998) incorporated the Columbine Sandstone into this unit.||Unit in Catombal Group.||Is correlated with Strathaird Formation.||
27826|Macquarie Park Sandstone|71600|5|Briefly described|p23 Fig 1|Devonian|Devonian|Geological province: Lachlan Fold Belt.||Unit of Catombal Group.|||Massive to bedded, fine to medium-grained quartz sandstone and red mudstone|
27826|Macquarie Park Sandstone|73299|6|Mentioned|p1104 Fig.10, p1105|Late Devonian|Late Devonian|Molong High.||Catombal Group||Overlies the Brymedura Sandstone.||
35078|Macquarie River basalts|23043|6|Mentioned|Map Diagram|Tertiary|Tertiary|||||||
41630|Macqueen Member|22857|5|Briefly described|p498 App.1 Tb.A1.7|Visean|Tournaisian|Green lithic sandstone, siltstone, calcareous skeletal mudstone and wackestone. Max. thickness: 64m. Geological Province: Tamworth Forearc Basin.||||||
41630|Macqueen Member|44244|4|Described|p23|Visean|Tournaisian|Reduced from formation status as "Macqueen Formation"  to member of the Dangarfield Formation.  Conformably overlies the Kingsfield Formation.  Max. thickness: 64m.||||||
76023|Macs Tank Ultramafic|63793|5|Briefly described|p18, pp37-38,  p62.|||Outcrop now within Mutawintji National Park. Elevated values of Cu, Cr and Ni. Abundant magnesite occurs west of the body. Well serpentinised and highly magnetic. Numerous small doleritic intrusions appear associated with Mount Wright Fault or splays from it.|||||Contains numerous small intrusions/inclusions of doleritic rock.|19-JAN-15
76023|Macs Tank Ultramafic|66623|1|Redefined|p194, pp224-229.|||Named  by Buckley (2002); formerly  Macs Tank Serpentinite (Crawford et al. 1997); subsequently Macs Tank Ultramafic Complex (Sharp 2004); redefined in this study. A 3 x 1.5 km outcrop in Mutawintji National Park. Relatively undeformed: probably intruded along the Mount Wright Fault after the Delamerian Orogeny. Possibly correlated with Cliffs Tank Complex.||||Probable intrusion into Ponto Group.|Serpentinised pyroxene-olivine ultramafic body; rare small inclusions or intrusions of dolerite.|
76023|Macs Tank Ultramafic|66918|5|Briefly described|Map legend|Paleozoic|Paleozoic||||||Serpentinised pyroxene-olivine ultramafic; occasional small inclusions/intrusions of dolerite.|
76023|Macs Tank Ultramafic|70650|5|Briefly described|Map Legend|Paleozoic|Paleozoic||||||Serpentinised pyroxene-olivine ultramafic; occasional small inclusions/intrusions of dolerite.
|
34756|Madron Formation|22892|6|Mentioned|p41|||||||||
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.||||||
36824|Magistrate Volcanic Member|23859|2|Defined|p241 Appendix 1|Late Permian|Permian|See also page 931. Type locality 403900E, 6749700N. Of Emmaville Volcanics. Overlain by Dundee Rhyodacite. Underlain by Dummy Creek Conglomerate. New England Fold Belt. Max. thickness: >450 m.||||||28-JAN-09
36824|Magistrate Volcanic Member|70876|5|Briefly described|p82|Late Permian|Late Permian|Provided age is a SHRIMP U-Pb zircon date.|252.5 +/- 1.5 Ma (Black, 2006)|Emmaville Volcanics||||
36824|Magistrate Volcanic Member|71628|5|Briefly described|p14:12|||||Emmaville Volcanics.||Partly bounds the Mount Jonblee Leucomonzogranite.||
35610|Mailman Gap Member|61964|4|Described|p14 Fig. 4, p117 Fig. 35, p126|Famennian|Famennian|Supersedes "Mailman Gap Conglom.Mbr". Base of Rankin Fm(Cocoparra Gp). Coarse-gr.qtz-lithic sst + increasing pebble content downwards; basal seq.of polymictic pebble-cobble orthoconglom.grading into paracongloms.Conform.on Jimberoo Fm.Max.thickness: 599m||||||29-AUG-12
35610|Mailman Gap Member|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Includes Mailman Gap, Byawatha Conglomerate and Essex Members. Cross bedded pebbly sandstone with thin conglomerate bands (dominant vein quartz clasts), sandstone, and lithic sandstone.||||||25-MAR-08
35610|Mailman Gap Member|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Rankin Formation.||Overlies Jimberoo Formation.|Cross-bedded pebbly sandstone with thin conglomerate bands (dominant vein quartz clasts), sandstone and lithic sandstone.|
35610|Mailman Gap Member|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Rankin Formation.||Overlies (?faulted contact) Bootheragandra Group.|Cross-bedded pebbly sandstone with thin conglomerate bands (dominant vein quartz clasts), sandstone and lithic sandstone.|
35610|Mailman Gap Member|69163|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Rankin Formation.||Overlies (?faulted contact) Bootheragandra Group.|Cross-bedded pebbly sandstone with thin conglomerate bands (dominant vein quartz clasts), sandstone and lithic sandstone.|
35610|Mailman Gap Member|71040|5|Briefly described|p28 Fig.15, p31|Devonian|Devonian|Diagram of major faults and contractional deformation related to Tabberabberan Orogeny. Age is now considered Lower to Middle Devonian.||Rankin Formation.|||Clasts dominantly quartzite and vein quartz; small percentage of cleaved clasts.|
26007|Majors Creek Formation|22736|6|Mentioned|p627-9|Namurian|Visean|||||||
26007|Majors Creek Formation|22857|5|Briefly described|p514 App.1 Tb.A1.8|Namurian|Namurian|Arenite-dominated sequence; minor ash beds and carbonaceous shale at top.||||||
26007|Majors Creek Formation|23720|5|Briefly described|Map Legend|||Lithic sandstone, cherty mudstone.||||||15-DEC-04
26007|Majors Creek Formation|24124|5|Briefly described|p3||Carboniferous|||||||
26007|Majors Creek Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26007|Majors Creek Formation|31806|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26007|Majors Creek Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26007|Majors Creek Formation|34293|2|Defined|p44|Carboniferous|Carboniferous|See also PP43,44||||||
26007|Majors Creek Formation|36528|6|Mentioned|p180|||||||||
26007|Majors Creek Formation|36961|6|Mentioned|Fig.5|||||||||
26007|Majors Creek Formation|38803|6|Mentioned|p106|||||||||
26007|Majors Creek Formation|39214|6|Mentioned|p43|||||||||
26007|Majors Creek Formation|40883|6|Mentioned|p2|||||||||
26007|Majors Creek Formation|41347|4|Described|Table 5|||||||||
26007|Majors Creek Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Hastings Block.||||||16-DEC-04
26007|Majors Creek Formation|42002|6|Mentioned|p92|||||||||
26007|Majors Creek Formation|42547|4|Described|p39|||||||||
26007|Majors Creek Formation|43755|6|Mentioned|Fig.1,p548||Carboniferous|||||||
26007|Majors Creek Formation|44093|5|Briefly described|p67 Fig 6.6|Carboniferous|Late Devonian|In the Northern Hastings Block. See also p233 Appendix 1. Geological Province: New England Fold Belt.||||||
26007|Majors Creek Formation|44450|4|Described|p24 Table 5|Late Carboniferous|Late Carboniferous|Geological Province: Hastings Block.||||||
26007|Majors Creek Formation|45097|6|Mentioned|p27|||Brachiopods. Correlation chart||||||
26007|Majors Creek Formation|47056|6|Mentioned|Fig.2 P523|||||||||
26007|Majors Creek Formation|47059|5|Briefly described|p145|||||||||
26007|Majors Creek Formation|61771|5|Briefly described|p116|||Exposed in the Parrabel Dome. Geological Province: Northern Hastings Terrane.||||||25-JAN-06
26007|Majors Creek Formation|63832|6|Mentioned|p131 fig 2|Serpukhovian|Visean|Northern Hastings block, Southern New England Fold Belt.||||||
26007|Majors Creek Formation|64631|5|Briefly described|p44 Fig.2.|Serpukhovian|Visean|Southern New England Fold Belt: northern Hastings Block. Some biostratigraphic age control near top.||||Is overlain by Kullatine Formation.||
26007|Majors Creek Formation|65317|6|Mentioned|p634 Fig.13|||||||||
26007|Majors Creek Formation|70939|6|Mentioned|p826, p828, p837|Carboniferous|Carboniferous|Northern Hastings Block. Appears as Major Creek Formation on p826.||||||
27473|Majuba Volcanics|9548|5|Briefly described|Map Legend|Pragian|Lochkovian|Of the Kopyje Group. Includes: Long Panel Tuff Member, Fountain Dale Tuff Member.||||||06-JUL-04
27473|Majuba Volcanics|22768|6|Mentioned|p170|||||||||
27473|Majuba Volcanics|22857|4|Described|p170, p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Kopyje Group. Lavas and pyroclastics - interfinger with Baledmund Formation. Max. thickness: 2km. Geological Province: Kopyje Shelf (Darling Basin). ||||||
27473|Majuba Volcanics|23171|6|Mentioned|p15|||||||||
27473|Majuba Volcanics|35219|6|Mentioned|p16|||||||||
27473|Majuba Volcanics|35287|6|Mentioned|p7|||||||||
27473|Majuba Volcanics|39618|6|Mentioned|p40|||||||||
27473|Majuba Volcanics|41528|6|Mentioned|p17|||See also P110||||||
27473|Majuba Volcanics|42566|3|Fully described|p72|||||||||
27473|Majuba Volcanics|42568|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
27473|Majuba Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
27473|Majuba Volcanics|43089|5|Briefly described|Map Legend|||of Kopyje Group||||||
27473|Majuba Volcanics|65469|6|Mentioned|p16|||Lachlan Orogen.||||||
27473|Majuba Volcanics|67416|6|Mentioned|p84 Fig.1|||Canbelego-Mineral Hill Volcanic Belt.||Kopyje Group.|||I-type.|
27473|Majuba Volcanics|70751|5|Briefly described|p5, p7, p17, p21-p22|||||Kopyje Group||Interfingers with the Baledmund Formation.|Thick felsic volcanic rocks.|
27473|Majuba Volcanics|70876|5|Briefly described|p9|||Lachlan Orogen.||Kopyje Group|||Felsic, I-type volcanics.|
27473|Majuba Volcanics|70950|6|Mentioned|p1030,1034,1044|||Geological province: Central Lachlan Orogen. Forms part of the Canbelego-Mineral Hill Volcanic Belt.||Unit of Kopyje Group.||Interfingers with Baledmund Formation.|Felsic volcanic, volcaniclastic sandstone and siltstones|
27473|Majuba Volcanics|71039|5|Briefly described|p11-p12, p25|Devonian|Silurian|Preserve zeolite to epizone greenschist facies rift basin metamorphic mineral assemblages, but there are significant areas of biotite-zone greenschist facies metamorphism associated with syn-volcanic plutons. In contact with the Baledmund Formation although the nature of the contact is not made clear.||Kopyje Group||||
27473|Majuba Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Kopyje Group.|||In the north: feldspar +/- quartz phyric, locally flow-banded rhyolitic to dacitic lavas. In the south: dacitic lava, moderately crystal-rich rhyolite, poorly sorted often pumiceous volcaniclastic sandstone and siltstone.|
27473|Majuba Volcanics|72908|5|Briefly described|p5, p8 Tb.1, p24, p30|Early Devonian|Late Silurian|Hosts the Yellow Mountain deposit.||Kopyje Group|||Felsic-dominated volcanic unit, includes derived sedimentary rocks.|
27473|Majuba Volcanics|72958|6|Mentioned|p11|Lochkovian|Pridoli|Cobar Basin. Nymagee area.||||Underlain by Mount Susannah Conglomerate. Equivalent to Baledmund Formation, Mineral Hill Volcanics and Talingaboolba Formation. Intruded[?] by Yellow Mountain Granite.||
27473|Majuba Volcanics|73174|6|Mentioned|p1038|||Kopyje Shelf.|||||Rhyolite and rhyodacite ashflow and airfall tuffs.|
27473|Majuba Volcanics|73578|5|Briefly described|p1, p3, p32, p34-37|Early Devonian|Early Devonian|This unit hasn't been dated directly but it interfingers with first-cycle volcaniclastic rocks of the ca 420 Ma Baledmund Formation. Intruded by unnamed dacitic porphyry at Gindoono. New SHRIMP U-Pb zircon age for the dacitic porphyry intrusion provides a minimum age of 423.0 +/- 2.6 Ma for the Majuba Volcanics.||||Interfingers with the Baledmund Formation.|I-type volcanics.|
80701|Malara Quartz Monzodiorite|71628|4|Described|p7: 1; p19: 72, 95-97|||New name, after Malara Creek. Occurs ~19 km W of Baryulgil as a ~4 x 1.5 km (poorly constrained) intrusion. Geochemistry described. Included in the Moonbi Plutonic Suite by Shaw and Flood (1981). Is spatially (probably not genetically) associated with Au mineralisation.|~252 Ma (Waltenberg et al., 2017 unpubl.).|Grasstree Suite (tentative).||Intrudes Drake Volcanics.|Pale to medium grey, fine- and locally medium-grained, moderately to slightly porphyritic hornblende-biotite and biotite quartz monzodiorite. A-type.|
80701|Malara Quartz Monzodiorite|72528|5|Briefly described|p2, p4 Tb.1.2, p84-89, p110, p127.|Early Triassic|Lopingian|Magmatic crystallisation age determined. Geographically close to Bungulla Supersuite rocks, but geochemically very distinct. Situated southeast of Tenterfield. Hosts orogenic Au deposits  and a historic alluvial gold field. Shown as part of the New England Orogen.|251.2+/-1.3 Ma U-Pb SHRIMP|Grasstree Suite.||Intrudes Drake Volcanics|Dated sample is a medium-fine grained, grey, porphyritic biotite quartz monzodiorite. Includes Au-mineralised quartz monzondiorite. Oxidised I-type.|01-FEB-21
27474|Mallee Tank Group|29621|6|Mentioned|Table 1|||||||||
27474|Mallee Tank Group|29680|6|Mentioned|Fig.1|||||||||
27474|Mallee Tank Group|29947|6|Mentioned|Fig.1|||||||||
27474|Mallee Tank Group|29948|6|Mentioned|Fig.12|||||||||
27474|Mallee Tank Group|29987|4|Described|p20|||||||||
27474|Mallee Tank Group|31592|6|Mentioned|Fig. 1|||U.Sil.-L.Dev.||||||
27474|Mallee Tank Group|32087|6|Mentioned|p10|||||||||
27474|Mallee Tank Group|33121|6|Mentioned|p90|||Correlated with Amphitheatre Beds. See also Fig.8.||||||
27474|Mallee Tank Group|33342|4|Described|p175|||Late Sil.-Early Dev.||||||
27474|Mallee Tank Group|34400|6|Mentioned|p5|||||||||
27474|Mallee Tank Group|34404|6|Mentioned|Fig.3.8|||?Upper Silurian - Lower Devonian||||||
27474|Mallee Tank Group|34449|6|Mentioned|p128|||||||||
27474|Mallee Tank Group|34469|6|Mentioned|p115|||Upper Silurian||||||
27474|Mallee Tank Group|35163|6|Mentioned|Map legend|Early Devonian|Late Silurian|||||||
27474|Mallee Tank Group|35287|6|Mentioned|Table 1|||||||||
27474|Mallee Tank Group|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area||||||
27474|Mallee Tank Group|39618|6|Mentioned|Table 1|||||||||
27474|Mallee Tank Group|41528|6|Mentioned|Fig.3|||||||||
27474|Mallee Tank Group|42172|4|Described|Fig.5 P167|||||||||
27474|Mallee Tank Group|43032|5|Briefly described|Table 1.|||||||||
27474|Mallee Tank Group|43383|14|Not recorded|p11,13||Late Silurian|Unconformable on Cobar Group||||||
27474|Mallee Tank Group|43385|14|Not recorded|p172||Late Silurian|||||||
27474|Mallee Tank Group|43389|14|Not recorded|Map Legend|Devonian|Silurian|||||||
27474|Mallee Tank Group|46032|2|Defined|p.411-414|Early Devonian|Late Silurian|Overlies Cobar Group & Girilambone Group. Fossiliferous.||||||
23757|Mammy Johnsons Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Dewrang Group. Massive and thickly bedded lithic sandstone; strings of pebble conglomerate and coarse sandstone. Max. thickness: 300m. Geological Province: Sydney Basin.||||||
23757|Mammy Johnsons Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Dewrang Group.    Geological Province: New England Fold Belt||||||
23757|Mammy Johnsons Formation|40872|6|Mentioned|Fig.2|||||||||
23757|Mammy Johnsons Formation|41054|6|Mentioned|p152|||||||||
23757|Mammy Johnsons Formation|44244|2|Defined|p172-174, p168 Tb. 2|Late Permian|Late Permian|Of the Dewrang Group.  Conformably overlies the Weismantels Formation; underlies Waukivory Creek Formation.  Max. thickness: 300m.  Type section in text.  Geological Province: Myall Block.||||||23-AUG-04
23757|Mammy Johnsons Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Dewrang Group.  Geological Province: Western Myall Block.||||||
77429|Manar Ignimbrite Member|66300|5|Briefly described|p35, 41, 46.|Early Devonian|Early Devonian||413.0 +/- 2.3 Ma.|Said in this study to be a unit in Long Flat Volcanics.||Overlies Croppies Gunyah Rhyolite Member.||29-OCT-13
77429|Manar Ignimbrite Member|69159|5|Briefly described|Map legend|Pragian|Lochkovian|||Unit in Long Flat Volcanics.||Overlies Croppies Gunyah Ignimbrite Member.|Green to grey, fine- to medium-grained, mainly crystal-rich and highly fragmented, densely welded rhyolitic ignimbrite; variable lithic clast content.|07-SEP-15
77429|Manar Ignimbrite Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Long Flat Volcanics.|||Green to grey, fine- to medium-grained, mainly crystal-rich and highly fragmented, densely welded, rhyolitic ignimbrite; variable lithic clast content.|
77429|Manar Ignimbrite Member|71700|3|Fully described|vi, p25-p26, p79, CD|Early Devonian|Early Devonian|Named for the Manar Homestead. A type locality is nominated on the Kings Highway at GR 745269 6091809. A representative locality occurs at GR 748564 6094011. Historically included in the Manar Porphyry defined by Joplin et al (1953) and the Long Flat Porphyries of Anderson (1893). Potentially equivalent to the Wongabel Rhyodacite Member, Newacres Ignimbrite Member and the Four Winds Ignimbrite Member. Mistakenly referred to as the Manar Rhyolite Member on the CD. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. SHRIMP age is consistent with dates for other members of the Long Flat Volcanics. This unit has an estimated thickness of less than 500m.|413 +/- 2.3 Ma (SHRIMP U-Pb)|Long Flat Volcanics||Overlies the Croppies Gunyah Ignimbrite Member. Overlain by the Toggannoggra Rhyolite Member.|Greenish-grey, medium-grained, densely welded rhyolitic ignimbrite.|
31704|Mandagery Formation|23214|3|Fully described|p229|Late Devonian|Late Devonian|Of Hervey Group. Previously named Mandagery Sandstone.  Consists of fine to medium grained white sandstone with thin red and green siltstone and shale.  Max. thickness 750m. Overlying unit: Pipe Formation, underlying unit: Kadina Formation.||||||
31704|Mandagery Formation|23217|4|Described|p1, p6-9|Frasnian|Frasnian|(Conolly, 1965a). Replaces Mandagery Sandstone. Contains the famous Canowindra fish fossils. Overlies Kadina Formation; underlies Mount Cole Formation.  Probably late Frasnian in age. Geological Province: Parkes Syncline.||||||08-MAR-06
31704|Mandagery Formation|23392|6|Mentioned|p7|||Broad correlation of Peaks Formation but on Parkes sheet only.||||||
31704|Mandagery Formation|24417|3|Fully described|p130|Frasnian|Frasnian|Of Hervey Group.  Formerly "Mandagery Sandstone".  Overlain by Mount Cole Formation; underlain by Boulton Formation.  Max. thickness: 900m.||||||
31704|Mandagery Formation|43782|5|Briefly described|Map Legend|Famennian|Frasnian|Of the Hervey Group.||||||27-OCT-08
31704|Mandagery Formation|50231|5|Briefly described|Map Legend|Famennian|Frasnian|Of the Nangar Subgroup (Hervey Group).  Overlies: Bendick Formation.  Underlies: Bumberry Formation.||||||13-MAY-04
31704|Mandagery Formation|60009|5|Briefly described|Map Legend|Frasnian|Frasnian|Of the Hervey Group. Underlies Mount Cole Formation.  Overlies Boulton Formation.||||||27-OCT-08
31704|Mandagery Formation|61964|6|Mentioned|p129|Frasnian|Frasnian|Contains large lingulide brachiopods. ||||||
31704|Mandagery Formation|62569|5|Briefly described|p612|Late Devonian|Late Devonian|A marginal marine lingulid facies. Contains the Canowindra fish fauna remains - BATHURST map sheet area. ||||||
31704|Mandagery Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Basal unit of Nangar Subgroup (Hervey Group). White, thick bedded, coarse-gr. pebbly to conglom., quartzose to lithic-quartz sst; overlain by massive, thick bedded, medium- to fine-gr. quartzose sst; thinly bedded planar-lam.,flaggy sst + minor red siltst||||||
31704|Mandagery Formation|64826|5|Briefly described|p1040 Tb. 1|Famennian|Frasnian|Of the Hervey Group.||||||04-MAR-09
31704|Mandagery Formation|68592|2|Defined|p35, p232, p1707-12|Frasnian|Frasnian|Originally Mandagery Sandstone of Conolly (1965), after Mandagery railway station. Renamed Mandagery Formation (Pogson and Watkins, 1998) to reflect the greater component of siltstone and shale away from the type area. Typically forms prominent ridges. Type area and representative exposures are described. c.700m thick. Geophysical properties briefly described. A prolific Late Frasnian fish fauna has been obtained from this unit at Canowindra. Quartzite has been quarried at Douglas Gap for dimension stone and aggregate; has potential also as source of silica.||Unit in Hervey Group.||Conformably overlies Bendick Formation. Is overlain conformably by Bumberry and Koorawatha Formations. Is correlated with upper part of Peaks Formation.|Basal white, thick-bedded, coarse-grained, pebbly to conglomeratic, quartzose to lithic-quartz sandstone, overlain by massive, thick-bedded quartzose sandstone and thinly-bedded, planar-laminated, flaggy quartzose sandstone and minor red siltstone.|
31704|Mandagery Formation|70192|5|Briefly described|Map Legend|Frasnian|Frasnian|Dhm. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hervey Group||Overlies Bendick Formation. Is overlain by Bumberry Formation.|Basal, thickly bedded, coarse grained, pebbly-conglomeratic quartzose-lithic quartz sandstone. Overlain by massive, thick bedded, medium-fine grained quartzose sandstone and thinly bedded, planar laminated quartzose sandstone and minor siltstone.|
31704|Mandagery Formation|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Hervey Group||||
31704|Mandagery Formation|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Hervey Group|||Basal, thickly bedded, coarse grained, pebbly-conglomeratic quartzose-lithic quartz sandstone. Overlain by massive, thick bedded, medium-fine grained quartzose sandstone and thinly bedded, planar laminated quartzose sandstone and minor siltstone.|
31704|Mandagery Formation|71656|6|Mentioned|p12 Fig.2|Frasnian|Frasnian|Shown only in correlation chart (Fig.2).||Hervey Group||Overlies Bendick Formation, underlies Bumberry Formation.||
81817|Mandaring Formation|73457|4|Described|ii, p1, p3, p5, p13-14|Late Devonian|Late Devonian|Exposure is confined to the property of 'Mandaring', which gives the formation its name. Previously shown as a non-marine Upper Devonian sequence (Adamson and Loudon, 1966; Degeling, 1977). Divided into three subunits (units A, B, C) by Trigg (2019). Maximum thickness of ca. 350 m. Easterly dipping. Boundary between the top of the unit and the Adaminaby Group to the east is inferred to be a fault. Late Devonian age suggested is dependant on general correlation with other 'Lambie' facies sequences. Formal definition is given in Trigg (2021).||||Nonconformably overlies Thologolong Granite in northern part, unconformably overlies Adaminaby Group in southern part|Mostly comprises medium-grained quartz sandstone and locally also pebbly sandstone and pebble to cobble conglomerate. Thinly interbedded fine-grained red sandstone and siltstone occur near the base of the sequence.|
26010|Mandowa Mudstone|721|5|Briefly described|Map legend|Tournaisian|Famennian|Of the Parry Group. Grey, thinly bedded, laminated and massive mudstone with subordinate thin siltstone and fine sandstone.||||||04-FEB-08
26010|Mandowa Mudstone|22572|6|Mentioned|p112|||||||||
26010|Mandowa Mudstone|22639|5|Briefly described|p276|Late Devonian|Late Devonian|||||||
26010|Mandowa Mudstone|22857|5|Briefly described|p496 App.1 Tb.A1.7|Famennian|Fammenian|Of the Parry Group. Laminated and massive mudstone with subordinate thin siltstone and fine sandstone. Max. thickness: 650m. Geological Province: Tamworth Forearc Basin.||||||
26010|Mandowa Mudstone|23051|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of Parry Group.||||||14-APR-08
26010|Mandowa Mudstone|23185|6|Mentioned|Fig1p156|Famennian|Famennian|||||||
26010|Mandowa Mudstone|23522|5|Briefly described|p249 Fig 5|Famennian|Famennian|||||||
26010|Mandowa Mudstone|24366|5|Briefly described|p17 Fig. 3|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||
26010|Mandowa Mudstone|24614|6|Mentioned|p190, p204|Famennian|Famennian|Underlies the Luton Formation.||||||07-FEB-11
26010|Mandowa Mudstone|30133|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26010|Mandowa Mudstone|30135|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26010|Mandowa Mudstone|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
26010|Mandowa Mudstone|31802|5|Briefly described|p134|||||||||
26010|Mandowa Mudstone|31999|5|Briefly described|p151|||Table 1||||||
26010|Mandowa Mudstone|32286|6|Mentioned|Fig. 1|||||||||
26010|Mandowa Mudstone|32482|6|Mentioned|Map legend|Carboniferous|Devonian|Carb.-Dev.||||||
26010|Mandowa Mudstone|32602|6|Mentioned|p67|||||||||
26010|Mandowa Mudstone|32671|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian-Carboniferous||||||
26010|Mandowa Mudstone|32672|6|Mentioned|p674|||||||||
26010|Mandowa Mudstone|32865|5|Briefly described|p480|||See also P481. Fauna||||||
26010|Mandowa Mudstone|32866|6|Mentioned|Fig.11|||||||||
26010|Mandowa Mudstone|34085|6|Mentioned|Cor.chart|||Famennian||||||
26010|Mandowa Mudstone|34349|6|Mentioned|p246|||||||||
26010|Mandowa Mudstone|34555|3|Fully described|p240|||||||||
26010|Mandowa Mudstone|35761|6|Mentioned|Table 1|||||||||
26010|Mandowa Mudstone|36057|6|Mentioned|p350|||||||||
26010|Mandowa Mudstone|36961|6|Mentioned|p208|||See also Fig.3.||||||
26010|Mandowa Mudstone|37987|2|Defined|p214|Carboniferous|Devonian|Carboniferous - Devonian.||||||14-APR-08
26010|Mandowa Mudstone|38215|6|Mentioned|p276|||||||||
26010|Mandowa Mudstone|39214|4|Described|p33|||Late Dev.||||||
26010|Mandowa Mudstone|39331|6|Mentioned|Table 10-1|||||||||
26010|Mandowa Mudstone|39468|6|Mentioned|Fig.2|||||||||
26010|Mandowa Mudstone|40246|6|Mentioned|Table 1|||||||||
26010|Mandowa Mudstone|41009|6|Mentioned|Fig.2|||||||||
26010|Mandowa Mudstone|41238|6|Mentioned|p82|||||||||
26010|Mandowa Mudstone|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Of the Parry Group.||||||16-DEC-04
26010|Mandowa Mudstone|41389|6|Mentioned|p27|||||||||
26010|Mandowa Mudstone|42547|4|Described|p18|Devonian||||||||
26010|Mandowa Mudstone|42728|4|Described|p5|||||||||
26010|Mandowa Mudstone|42849|6|Mentioned|p541|||Contains the Kiah Limestone Member which overlies the Keepit Conglomerate.||||||09-MAY-05
26010|Mandowa Mudstone|43091|5|Briefly described|Map legend|||Of Parry Group.||||||04-FEB-08
26010|Mandowa Mudstone|43344|14|Not recorded|p91||Devonian|Unit of Manilla Group.||||||14-APR-08
26010|Mandowa Mudstone|43406|14|Not recorded|p49|||||||||
26010|Mandowa Mudstone|43407|14|Not recorded|Map Legend|Carboniferous|Devonian|(Provisional Edition)||||||
26010|Mandowa Mudstone|43409|14|Not recorded|Map Legend||Late Devonian|Late Upper Devonian||||||
26010|Mandowa Mudstone|43417|14|Not recorded|Map Legend|||||||||
26010|Mandowa Mudstone|43418|14|Not recorded|Map Legend|||||||||
26010|Mandowa Mudstone|43428|14|Not recorded|p141|||||||||
26010|Mandowa Mudstone|43429|14|Not recorded|Map Legend|||||||||
26010|Mandowa Mudstone|43434|14|Not recorded|Map Legend||Late Devonian|||||||
26010|Mandowa Mudstone|43435|14|Not recorded|Map Legend||Late Devonian|||||||
26010|Mandowa Mudstone|43436|14|Not recorded|Map Legend||Devonian|(Provisional Edition)||||||
26010|Mandowa Mudstone|43455|14|Not recorded|p460(Tb.)||Late Devonian|||||||
26010|Mandowa Mudstone|43461|14|Not recorded|p619||Famennian|U.Famennian||||||
26010|Mandowa Mudstone|43479|14|Not recorded|p136,151||Late Devonian|||||||
26010|Mandowa Mudstone|43575|6|Mentioned|p276||Late Devonian|||||||
26010|Mandowa Mudstone|45097|6|Mentioned|Fig.|||Correlation chart||||||
26010|Mandowa Mudstone|46803|6|Mentioned|Fig. 3|||||||||
26010|Mandowa Mudstone|47056|6|Mentioned|Fig.2 P523|||||||||
26010|Mandowa Mudstone|48926|6|Mentioned|p56|||P56 et seq.||||||
26010|Mandowa Mudstone|50132|5|Briefly described|p246 Fig. 4, p247 Fig. 5, p248 Fig.6|Late Devonian|Late Devonian|New England Fold Belt, Manilla area||||Overlies the Keepit Conglomerate. Underlies the Tulcumba Sandstone.||
26010|Mandowa Mudstone|61765|6|Mentioned|p58 Fig. 1|||Includes Kiah Limestone Member. Geological Province: Tamwoth Belt.||||||07-FEB-11
26010|Mandowa Mudstone|61769|6|Mentioned|p95, p99 Fig. 4||Late Devonian|||||||
26010|Mandowa Mudstone|65214|6|Mentioned|p282|Devonian|Devonian|NSW, Keepit. Appears in text as Mandowa Ms. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26010|Mandowa Mudstone|65902|5|Briefly described|p199, p203 Fig.7|Fammenian|Fammenian|Overlies Keepit Conglomerate. Overlain by Tulcumba Sandstone. Dated by ammonoids.||||||09-MAR-12
26010|Mandowa Mudstone|66720|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Parry Group.|Includes Borah Limestone Member and an un-named but separately mapped member with fine-grained buff lithic sandstone.||Thinly bedded, laminated and massive mudstone with subordinate thin siltstone and fine-grained sandstone beds.|
26010|Mandowa Mudstone|68003|5|Briefly described|p32 Fig.3-h, pp138-139. |Famennian|Famennian|Tamworth Belt (North), New England Fold Belt.||Unit in Parry Group.|Includes Kiah Limestone Member.|Overlies Keepit Conglomerate. Is overlain by Tulcumba Sandstone, Tangaratta and Luton Formations.|Grey, thinly bedded, laminated and massive mudstone with subordinate thin siltstone and fine sandstone; limestone, sandstone, tuff.|
26010|Mandowa Mudstone|68005|5|Briefly described|p49 Fig.3-M, p54, p148, p170.|Late Devonian|Late Devonian|Tamworth Belt.||Unit in Parry Group.|Includes Kiah Limestone and Hyde Greywacke Member.|Conformably overlies Keepit Conglomerate. Is overlain by Tangaratta and Luton Formations.|Grey, thinly bedded, laminated and massive mudstone with subordinate thin siltstone and fine sandstone; scattered limestone bodies; andesite.|
26010|Mandowa Mudstone|70907|6|Mentioned|p774 Fig.2|||||||||
26010|Mandowa Mudstone|71628|6|Mentioned|p18:20|||||Parry Group.||||
26010|Mandowa Mudstone|73181|6|Mentioned|p60|Famennian|Famennian|Contains abundant L. Australe and rare trilobites used for temporal constraint.||||||
22253|Mandurama Ponds Granodiorite|22679|4|Described|p 46|Silurian|Silurian|||||||
22253|Mandurama Ponds Granodiorite|23214|3|Fully described|p166|Late Silurian|Late Silurian|Originally named Sunnyside Granodiorite. Intrudes the Adaminaby Group. Intruded by Roseburg and Little Forest Granite. Geological Province: Wyangala Batholith. I-type granodiorite.||||||
22253|Mandurama Ponds Granodiorite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Hornblende alllanite biotite granodiorite.||||||17-JUL-08
22253|Mandurama Ponds Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyanagala Batholith.||||||17-JUL-08
22253|Mandurama Ponds Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
22254|Manfred Sandstone|22799|6|Mentioned|p16|||||||||
22254|Manfred Sandstone|22893|2|Defined|p13-17|||Age, thickness discussed but exact figures are not known. Age inferred as Late Devonian to Early Carboniferous.||||||
22254|Manfred Sandstone|44188|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Mulga Downs Group. Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Medium- to coarse-grained quartzitic arenite with quartzite in the basal section.||||||15-MAY-08
80702|Mann River Leucogranite|71628|4|Described|p17: 1-2, 4, 11-12|||New name (this study), after a local watercourse. The ~10 x 4.5 km intrusion occurs ~9 km SW of Jackadgery, ~40 km W of Grafton. Has excellent outcrops as tors and pavements in rugged forested country. Very limited (one sample) geochemistry described. Is associated with numerous Au deposits (named) which are unlikely to be genetically related to this unit.|~240 Ma (Waltenberg and Blevin, 2017, unpub.)|Dandahra Creek Suite.||Intrudes Gundahl Complex.|Pinkish-brown, porphyritic leucomonzogranite; fine-grained, highly porphyritic marginal variant. A-type.|
80702|Mann River Leucogranite|72528|5|Briefly described|p2, p3 Tb.1.2, p96-101, p127.|Ladinian|Ladinian|Magmatic crystallisation age determined. Situated west of Grafton. Au-bearing vein system cross-cuts the leucogranite, allowing a maximum age to be derived for the Dalmorton Gold Field. Shown as part of the New England Orogen.|239.1+/-1.2 Ma|Dandahra Creek Suite||Intrudes into Gundahl Complex.|Outcrop is pale pinkish brown, very fine-grained, porphyritic leucogranite with phenocrysts of pale pink alkali feldspar. The outcrop has some secondary 'iron' staining.|
26011|Manna Conglomerate|22434|6|Mentioned|11 fig 14|Devonian|Silurian|Geol Province Lachlan Fold Belt||||||
26011|Manna Conglomerate|22797|5|Briefly described|P838|||Equivalent of Edols Conglomerate, parent is the Derriwong Group||||||
26011|Manna Conglomerate|22857|5|Briefly described|p446 App.1, Tb.A1.6|Early Devonian|Silurian|Part of Derriwong Group? Formerly the "Womboyne Conglomerate" of Bunker (1972a). Max. thickness: ~5km. ||||||
26011|Manna Conglomerate|23099|5|Briefly described|p582|Devonian|Silurian|||||||
26011|Manna Conglomerate|24417|2|Defined|p62|Early Devonian|Late Silurian|Originally named "Womboyne Conglomerate" (Brunker 1972a) however this name was preoccupied. Other authors previously included the unit as part of the now superseded "Condobolin Formation" and also as part of Edols Conglomerate.||||||
26011|Manna Conglomerate|35503|2|Defined|p205|Silurian|Silurian|New name refs Kemezys (1976)Prob. Silurian||||||
26011|Manna Conglomerate|40328|4|Described|p41|||Replaces Wamboyne Conglomerate. May be southern extension of Derriwong Group.||||||
26011|Manna Conglomerate|60009|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Ootha Group. Underlies Mulguthrie Formation, Yarnel Volcanics.||||||26-MAR-08
26011|Manna Conglomerate|61964|4|Described|p14 Fig. 4, p95-96, p35|Lochkovian|Pridoli|Of Ootha Group. Originally named "Womboyne Conglomerate" (Brunker 1972), previously included as part of "Condobolin Formation " (Connolly 1965). Also considered part of Edols Conglomerate (Scott in Lyons and Wallace 1999). Max.thickness:1000m (est.)||||||
26011|Manna Conglomerate|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Ootha Group. Pebble conglomerate with quartz and quartzite clasts, massive medium-grained quartz and lithic quartz sandstone.||||||10-APR-08
26011|Manna Conglomerate|64568|5|Briefly described|Map legend|Silurian|Silurian|Of the Ootha Group. Polymictic conglomerate, and massive medium-grained quartz and lithic sandstone.||||||24-SEP-08
26011|Manna Conglomerate|66197|5|Briefly described|p635 Fig.5b|Early Devonian|Late Silurain|Jemalong Trough. Deep marine shale and sandstone. Underlies the Pullabooka Formation.||||||14-MAR-12
26011|Manna Conglomerate|71040|5|Briefly described|p16|Early Devonian|Late Silurian|Currowong Syncline.||Ootha Group.||||
26011|Manna Conglomerate|72084|5|Briefly described|p39-40, p49|Devonian|Silurian|Pinnacle Mountain area.|||||Clasts include quartzite, shale, limestone, granite, possibly mafic volcanic lithic fragments, and quartz and feldspar crystals.|
25202|Mannering Park Tuff Member|29922|6|Mentioned|p49|||||||||
25202|Mannering Park Tuff Member|29926|6|Mentioned|Fig.3|||||||||
25202|Mannering Park Tuff Member|34351|6|Mentioned|p348|||Fig.5.13||||||
25202|Mannering Park Tuff Member|37083|6|Mentioned|p164|||||||||
25202|Mannering Park Tuff Member|39292|6|Mentioned|Fig. 6.2|||||||||
25202|Mannering Park Tuff Member|39666|6|Mentioned|Table 20|||||||||
25202|Mannering Park Tuff Member|41479|6|Mentioned|Fig.2|||||||||
25202|Mannering Park Tuff Member|43447|14|Not recorded|diag.p26|||Moon Island Beach Sub-Group||||||
25202|Mannering Park Tuff Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Catherine Hill Bay Formation.||||
31616|Mannus Creek Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31616|Mannus Creek Suite|69801|6|Mentioned|p104, p137|Devonian|Wenlock|Central Lachlan Orogen. Chappell et al (1991) assigned the three original constituents. Subsequently in 1999 Chappell et al merged the three plutons into the Bogandyera Granite and renamed the Mannus Creek Suite as the Bogyandera Suite.|||Includes the Munderoo Granodiorite, Bogandyera Granite and the Prison Farm Granodiorite.|||
26012|Manooka Limestone Member|5250|5|Briefly described|p42 |Mid Caradoc|Early Caradoc|Member of  Daylesford Limestone, Overlies Bourimbla Limestone Member. Overlain by Gerybong Limestone Member.||||||
26012|Manooka Limestone Member|23214|3|Fully described|p37|Late Ordovician|Late Ordovician|Of Daylesford Limestone. 16m thick at type section. For lithology description see Semeniuk (1973a,b).||||||
26012|Manooka Limestone Member|33063|2|Defined|p80|Ordovician|Ordovician|Mb. Daylesford Lst.||||||
26012|Manooka Limestone Member|33064|4|Described|p450|||See also PP451-453. Stratigraphy||||||
26012|Manooka Limestone Member|33065|6|Mentioned|Table 1|||Lithology||||||
26012|Manooka Limestone Member|33737|6|Mentioned|p167|||||||||
26012|Manooka Limestone Member|33740|6|Mentioned|Fig.1|||||||||
26012|Manooka Limestone Member|38219|6|Mentioned|Table 2|||||||||
26012|Manooka Limestone Member|40136|6|Mentioned|p23|||||||||
26012|Manooka Limestone Member|42479|5|Briefly described|p111|||||||||
26012|Manooka Limestone Member|70684|5|Briefly described|p39 Fig.17|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Daylesford Limestone.||||
26012|Manooka Limestone Member|73210|5|Briefly described|p893, 900 Fig.7, 902|||Semeniuk (1973, 2011). Exhibits subaerial disconformities and diagenesis/pedogenesis. Summary profile of a subaerial disconformity.||Daylesford Limestone.||Overlies Bourimbla Limestone Member. Is overlain by Gerybong Limestone Member.||
27477|Mantappa Dolomite|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (East).  Parent - Farnell Group .  Age - Ediacarian in text.||||||
27477|Mantappa Dolomite|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
27477|Mantappa Dolomite|22857|4|Described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Farnell Group. Brown to buff, finely laminated dolomite. Age: 590Ma. Max. thickness: 2m. Geological Province: Adelaide Fold Belt. See also p400 App.1 Tb.A1.3.||||||
27477|Mantappa Dolomite|30261|4|Described|Table 1|||Marinoan age||||||
27477|Mantappa Dolomite|33004|6|Mentioned|p138|||||||||
27477|Mantappa Dolomite|34812|3|Fully described|p100|||||||||
27477|Mantappa Dolomite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27477|Mantappa Dolomite|35255|6|Mentioned|p15|||||||||
27477|Mantappa Dolomite|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
27477|Mantappa Dolomite|37931|4|Described|p533|||||||||
27477|Mantappa Dolomite|39214|5|Briefly described|p9|||||||||
27477|Mantappa Dolomite|41405|5|Briefly described|p205|||||||||
27477|Mantappa Dolomite|41429|5|Briefly described|p246|||||||||
27477|Mantappa Dolomite|41801|6|Mentioned|Fig.4|||||||||
27477|Mantappa Dolomite|66623|5|Briefly described|p18. |||||Unit in Farnell Group.||Is overlain by Sturts Meadows Siltstone.|Pale grey to white, finely laminated dolomite.|
27477|Mantappa Dolomite|68241|6|Mentioned|p21, p24 Fig.3, p32, p33 Fig.3|||Cooper et al. (1978).|||||Comprises a 2m thick finely laminated buff dolomite.|
27477|Mantappa Dolomite|70000|5|Briefly described|p34, p40|Neoproterozoic|Neoproterozoic|||Basal unit in Farnell Group.|||Cap dolomite.|
27477|Mantappa Dolomite|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Farnell Group.||Unconformably overlies Nunduro Conglomerate. Is overlain by Sturts Meadows Siltstone.|Pale grey to white, poorly bedded to finely laminated dolomite.|
82567|Manuka Farm Porphyritic Microgranodiorite|71628|4|Described|p8: 3, 56-57, 61-64; p19:55|||New name. Originally Wilsons Creek Porphyrite of Binns et al. (1967), after unpublished work by Ransley (1970). Referred to as Terrible Vale Porphyritic Microtonalite by Flood in Binns et al. (1967), and later (Flood, 1971) as Manuka Farm Tonalite Porphyrite. Later still, Green and Kridoharto (1975) referred to it as Manuka Adamellite and Manuka adamellite. Named after 'Manuka Farm' homestead. Crops out as large, grey tors. Limited geochemistry briefly described. Associated with Au mineralisation.||Uralla Suite.||Intrudes Sandon beds, Glenburnie Leucomonzogranite and Wandsworth Volcanic Group. Abuts (is probably intruded by) Khatoun Tonalite.|Texturally heterogeneous,fine- to medium-grained, commonly porphyritic possibly quartz-poor granodiorite - quartz monzodiorite, ranging from pyroxene-dominant to hornblende-biotite dominant ferromagnesian assemblages.|
29522|Marangulla Syenite|13139|5|Briefly described|p3 Fig. 2|||Geological Province: Lachlan Orogen.||||||
29522|Marangulla Syenite|23214|3|Fully described|p95|Late Ordovician|Late Ordovician|Intrudes the Weemalla Formation.||||||
29522|Marangulla Syenite|23334|5|Briefly described|3 Fig.2|||||||||
29522|Marangulla Syenite|24268|6|Mentioned|p1537 Fig.3|||Geological Province: Lachlan Fold Belt||||||
29522|Marangulla Syenite|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Syenite.||||||17-JUL-08
29522|Marangulla Syenite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29522|Marangulla Syenite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
26013|Marble Arch Limestone Member|22857|5|Briefly described|p480 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the De Drack Formation.||||||
26013|Marble Arch Limestone Member|40276|2|Defined|p5|Late Silurian|Late Silurian|||||||
26013|Marble Arch Limestone Member|68592|5|Briefly described|p760|||Defined on Araluen 1:100 000; Wyborn and Owen (1988).||Unit in De Drack Formation.|||Limestone.|
26013|Marble Arch Limestone Member|71069|6|Mentioned|p146|||||De Drack Formation||||
70244|Mares Forest Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Rhyolitic volcaniclastics with minor discontinuous lenses of massive, poorly sorted volcanogenic pebbly sandstone; 2 volcaniclastic subunits...||||||09-SEP-08
70244|Mares Forest Volcanics|68592|2|Defined|p742, p750, p886-7, p890-1, p892-7, p922|Early Devonian|Early Devonian|See also p726, p728. New name. Wombeyan Volcanics redefined during Goulburn mapping as Mares Forest Volcanics, and petrographic descriptions noted conspicuous orthoclase (Simpson 2006). Was included in Bindook Porphyry Complex by Scheibner (1973), although he recognised rock types around Mares Forest differed from those in remainder of Complex. Simpson, Carr and Jones (1997) regarded the volcanic rocks as possible lateral time equivalents of basal units of Bindook Volcanic Complex. Cas et al. (1981) used an informal term, 'Wollondilly volcanics'. Type locality noted. Thickness: ~3900 m, though top is faulted. Plateau-forming. Metamorphism: consistent with sub-greenschist facies. Age: inferred to be Early Devonian on lithostratigraphic grounds. Possible correlatives with other volcanic units within Gundary Volcanics, Kowmung Formation and Bindook Group.||Unit in Mount Fairy Group.||Unconformably overlies and is faulted against Wombeyan Limestone. Intruded by Columba Granite.|Predominantly fine-grained, non-welded, relatively crystal-poor rhyolitic ignimbrite and less abundant, medium-grained, poorly sorted, relatively crystal-rich, generally rhyolitic ignimbrite.|
70244|Mares Forest Volcanics|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfm. Includes three unnamed subunits; a non-welded rhyolitic ignimbrite, a fine-medium grained, thick bedded, massive lithic quartz sandstone and a welded pumiceous rhyolitic ignimbrite. Related units inferred from Time-Space Plot.||Mount Fairy Group||Erosional at base.|Fine grained, non-welded, crystal poor, rhyolitic ignimbrite; lesser medium-grained, poorly sorted, crystal rich, rhyolitic ignimbrite + interbedded massive coarse-grained + pebbly sandstone; minor lithic quartz sandstone, rare rhyolite-dacite.|
70244|Mares Forest Volcanics|70543|5|Briefly described|Map Legend |Devonian|Silurian|Includes three unnamed subunits; a non-welded rhyolitic ignimbrite, a fine-medium grained, thick bedded, massive lithic quartz sandstone and a welded pumiceous rhyolitic ignimbrite.||Mount Fairy Group|||Fine grained, non-welded, crystal poor, rhyolitic ignimbrite; lesser medium-grained, poorly sorted, crystal rich, rhyolitic ignimbrite + interbedded massive coarse-grained + pebbly sandstone; minor lithic quartz sandstone, rare rhyolite-dacite.|
70244|Mares Forest Volcanics|71069|6|Mentioned|p135, p144|||||||Unconformably overlies the Wombeyan Limestone.||
69897|Margules Group|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Poidevins and Mundoonen Sandstones.||||||
69897|Margules Group|66087|6|Mentioned|p3 Fig. 2|Ordovician|Ordovician|||||||
69897|Margules Group|67322|5|Briefly described|p17; Fig.5|Silurian|Late Ordovician|Scott et al., in Thomas et al. (in press). Southern half of the Goulburn 1:250 000 mapsheet. Paleontological evidence is lacking. Occurs in the Goulburn region.|||Dignams Siltstone, Poidevins Sandstone, Mundoonen Sandstone.|Interfingers with and conformably overlies Warbisco Shale.||22-FEB-18
69897|Margules Group|68592|3|Fully described|p322-3, p326-7, p339, p344-69, p420-1|Early Silurian|Late Ordovician|See also xxiv, p71, p73 Tb.5, p116-8, p275 Fig.57, p280, p282, p731, p742. Named after a Trig station between Yass and Gunning. Over 1300m thick terrigenous turbiditic sediments. Locally, consists of stacked, NE-trending, elongate fault slices in an en echelon array, and overturned folds. Frogmore and Goulburn structural zones: deformation described.|||Includes Mundoonen and Poidevins Sandstones; Dignams Siltstone.|Overlies Warbisco Shale gradationally; is overlain by Hawkins Volcanics; is unconformably overlain by Mount Fairy Group|Grey to yellowish-brown, lithic-quartz and quartzose sandstone; black, buff, greenish laminated to medium-bedded siltstone and lesser mudstone; olive, grey and buff, laminated to medium-bedded siltstone, minor mudstone and quartzose sandstone.|
69897|Margules Group|69159|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Mundoonen Sandstone.|||
69897|Margules Group|70192|5|Briefly described|Map Legend|Bolindian|Bolindian|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 Dignams Siltstone, Mundoonen Sandstone, Poidevins Sandstone.|Overlies Bendoc Group.||06-SEP-16
69897|Margules Group|70540|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Mundoonen Sandstone.|||
69897|Margules Group|70541|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Mundoonen Sandstone.|||
69897|Margules Group|70542|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Dignams Siltstone, Poidevins Sandstone|||
69897|Margules Group|70543|5|Briefly described|Map Legend |Ordovician|Ordovician||||Includes Poidevins Sandstone|||
69897|Margules Group|70545|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Mundoonen Sandstone.|||
69897|Margules Group|70546|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Mundoonen Sandstone|||
69897|Margules Group|71069|3|Fully described|p9, p21 fig 7, p22, p23, p40 fig 17, p51|Bolindian|Bolindian|Name derived from the Margules Trigonometrical Station. No synonmy or type section is available for the group as a whole, although there are reference sections given for its constituent units.  Thickened during the Benambran Orogeny. Estimated thickness ranges from 1200m to in excess of 2400m.Generally forms prominent ridges and outcrops, though in some places forms rubbly outcrop and is only well exposed in creeks.  Interpreted to have been deposited as turbidite seqeuences in a slope to basin-plain setting. Distribution, tectonic structure and metamorphism discussed. See also  p53 fig 19, p71, p72, p76 fig 27, p77, p82, p84, p87-92, p100, p105-p107, p114, p120, p134, p144, p169, p172.|||Includes the Mundoonen Sandstone, Dignams Siltstone and Poidevins Sandstone.|Conformably (gradationally) overlies the Warbisco Shale. Unconformably overlain by the Hoskinstown Group.Overlain by the Covan Creek Formation. Is faulted against the Hawkins Volcanics.|Siliciclastic turbidite sequences consisting of fine to very coarse grained, thinly to very thickly bedded lithic quartz sandstone, laminated to medium-bedded siltstone, lesser mudstone and black shale.|
69897|Margules Group|71656|5|Briefly described|p12,p13 Fig.2|Bolindian|Bolindian||||Includes Mundoonen Sandstone, Poidevins Sandstone.|Overlies Bendoc Group.||
69897|Margules Group|71691|5|Briefly described|Map legend.|Ordovician|Ordovician||||Mundoonen Sandstone.|Overlies Bendoc Group. Is overlain by Hoskinstown Group.||
69897|Margules Group|71699|5|Briefly described|Map legend.|Ordovician|Ordovician||||Mundoonen Sandstone.|Overlies Bendoc Group.||
69897|Margules Group|71700|3|Fully described|vi, p5, p7, p9-p10, p36-p38|Llandovery|Eastonian|Albury-Bega Terrane. Named for the Margules Trigonometrical Station between Yass and Gunning. There is no type section for this group, however, representative sections have been established for constituent units. Distribution, geomorphic expression, outcrop, structure, metamorphism, depositional environment, age evidence and distinguishing features are discussed. It is interpreted that this unit and its constituents were deposited by discrete submarine fans, producing sand-rich packages with a more restricted lateral extent than the sheet-like sandstone of the Adaminaby Group. See also  p45-p46, p48-p50, p82, p90, p107, CD.|||Includes the Mundoonen Sandstone, Poidevins Sandstone and Dignams Siltstone.|Conformably overlies the Warbisco Shale and the Bendoc Group. Unconformably overlain by the Mount Fairy Group and the Woodlawn Volcanics.|Quartzose sandstone and siltstone.|
69897|Margules Group|73140|5|Briefly described|p495|Bolindian|Bolindian|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.|||New Country Sandstone, Akuna Mudstone, Gungoandra Siltstone, Willandra Sandstone, Dignams Siltstone, Poidevins Sandstone, Mundoonen Sandstone|Overlies Bendoc Group|Represents resumption of terrigenous-derived turbiditic sedimentation.|
23764|Marobee Conglomerate|22857|4|Described|p414 App.1 Tb.A1.5|Ordovician|Ordovician|Of the Tallebung Group. Quartzite, mudstone, siltstone, conglomerate. Max. thickness: 500m. Geological Province: Wagga Marginal Basin.||||||24-FEB-06
23764|Marobee Conglomerate|41394|2|Defined|p27|Ordovician||||||||
23764|Marobee Conglomerate|41395|6|Mentioned|Map legend|Ordovician||||||||
23764|Marobee Conglomerate|61964|5|Briefly described|p30|||Of Trigg (1987) - for a conglomerate sequence within the former Tallebung Group. Previously included in the Boothumble beds of Brunker (1973). ||||||
23766|Marooba Formation|22857|4|Described|p442 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Winduck Group (Cobar Supergroup). Max. thickness: >600m. Geological Province: Winduck Shelf (Darling Basin). ||||||
23766|Marooba Formation|22887|3|Fully described|p26, Fig.4 p11|Early Devonian|Early Devonian|||||||
23766|Marooba Formation|23252|5|Briefly described|Map Legend|||of Winduck Group, Cobar Supergroup.||||||
23766|Marooba Formation|40913|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
23766|Marooba Formation|41126|3|Fully described|p98|||||||||
23766|Marooba Formation|61964|6|Mentioned|p140|Early Devonian|Early Devonian|||||||
39353|Maroota Sand|24117|5|Briefly described|p3|Tertiary|Tertiary|Geological Basin: Sydney Basin.||||||
39353|Maroota Sand|73248|5|Briefly described|p304, p307|||Lies on the Hornsby Plateau surface east of the Hawkesbury valley. Possibly the distal component of the Rickabys Creek Gravel. Overlain by a 44.7 +/- 1 Ma basalt unit.||||||
39353|Maroota Sand|75059|6|Mentioned|p8|Cenozoic|Cenozoic|NW Cumberland Basin, Sydney area.||||||
29532|Marra Creek Formation|22773|6|Mentioned|Fig24.10p355||Holocene|||||||
29532|Marra Creek Formation|23053|4|Described|p7,12,Fig11p34,49-56||Holocene|||||||
29532|Marra Creek Formation|24042|5|Briefly described|p513, 523|Holocene|Holocene||6 - 0 ka|||||11-SEP-12
29532|Marra Creek Formation|43276|5|Briefly described|Map Legend||Holocene|||||||
29532|Marra Creek Formation|43277|5|Briefly described|Map Legend||Holocene|||||||
29532|Marra Creek Formation|68003|5|Briefly described|pp91-92.|Holocene|Holocene|Coonamble Embayment. River, swamp and marsh deposits. Stratigraphic equivalent of the current alluvial system within the Brigalow Belt South Bioregion. Age from Watkins and Meakin (1996).|6.4 +/- 0.6 ka.|||Overlies Bugwah Formation.|Medium silt to clay.|
29532|Marra Creek Formation|68069|5|Briefly described|Map legend.|Quaternary|Quaternary|Has several facies: channel, meander plain, backplain, floodplain, floodbasin and lake; each mapped separately.|||||Unconsolidated pale to dark grey silt, clay, sandy silt, clayey silt; carbonate nodules common; boulders and pebbles along channels; cracking soils common.|
29532|Marra Creek Formation|68593|5|Briefly described|p1-3, p13-14, p17-20, p48|Holocene|Holocene|Watkins and Meakin (1996). Consists of narrow channels flanked by relatively narrow meander belts and broad backplains. Channel, meander, backplain, channelised backplain, flood basin backplain, ridge-bounded flood basin, flood basin and lake facies are described in some detail.|6.4 - 0 ka (Thermoluminescence; Watkins, 1992).|||Overlies Bugwah Formation.|Unconsolidated Quaternary alluvium surrounding silcrete-capped ridges: clay, silt, sandy silt, carbonate nodules.|
29532|Marra Creek Formation|73492|6|Mentioned|p691|||||||||
22270|Marrar Dyke|22638|4|Described|p80||Late Silurian|New name. Does not crop out.||||||
22270|Marrar Dyke|44192|5|Briefly described|Map Legend|Tertiary|Frasnian|||||||
36827|Marrawarra Rhyolite Member|23859|2|Defined|p242 Appendix 1|Late Permian|Permian|See also page 932. Type Locality 407000E 6740000N. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
37317|Martinsburg Slate|24011|6|Mentioned|p408|||||||||
69871|Marulan Supersuite|68592|4|Described|p901, p1318-20, p1611, p1613-4, p1600-73|Early Devonian|Early Devonian|See also p74 Tb.5. Chappell et al. (1991). Represents the culmination of Early Devonian magmatic activity in E part of the Goulburn Basin. A close genetic relationship with the Bindook Group is proposed. Geochemical differences with Gunning Suite are briefly described. Bungonia structural zone: deformation described.|||Includes Arthursleigh, Bangadilly, Bogungra, Koo-rilla and Mandari Suites.|Intrudes Bungonia Group.||
69871|Marulan Supersuite|70661|3|Fully described|p75-p77, p83|Early Devonian|Early Devonian|Name derived from township of Marulan. Originally described as the Marulan Batholith before being formally defined. Three suites have been redefined or rendered obsolete leaving only the Arthursleigh and Mandari Suite.Type Suite mentioned. Typically occurs as poorly exposed tors and low pavement outcrop. Forms a gently undulating landscape across a north-south trending belt. Structure, metamorphism, geochemistry discussed. |||Arthursleigh Suite, Mandari Suite|Intrudes Adaminaby Group, Bindook Group|I type granites and granodiorites with less abundant tonalite. Many plutons are compositionally uniform but vary in grainsize and texture and may be compositionally zoned.|
69871|Marulan Supersuite|72528|5|Briefly described|p25, p108.|Lochkovian|Lochkovian|Age range from Banshea Granite and Pleasant Hills Granite, Arthursleigh Suite and 3 other granites in the supersuite.|414.8+/-2.6 Ma to 412.6+/-2.2 Ma.||Includes Arthursleigh Suite.||Includes porphyritic granite.|
82571|Maryland Granodiorite|71628|3|Fully described|p19: 26, 97-100, 102|||New name (this study). Originally Maryland granite (Saint-Smith, 1911). Named after a local homestead. Forms a 6 x 3 km intrusion ~15 km NNW of Stanthorpe. Crops out poorly as small tors in grazing land. Thomson (1976) proposed a type locality on Wylie Creek Road (GR 030424, Drake 1:100,000 Sheet). Geochemistry detailed. Previously within the Herries Supersuite.|252.4 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Maryland Suite.||Intrudes Silverwood Group. Is faulted against and intruded by Cullendore Syenogranite. Is overlain by Marburg Formation.|Medium-grey, medium-grained, uneven-grained to slightly porphyritic hornblende-biotite granodiorite to monzogranite; mafic inclusions are common. I-type.|
74782|Maryland River Quartz Monzodiorite|61789|4|Described|p303, p306|Late Permian||Medium-grained, seriate, biotite quartz monzonite - quartz diorite. Mineralogically separate to Maryland Granite. Older than Undercliffe Falls Monzogranite. Intrudes Permian felsic volcanics.||||||
74782|Maryland River Quartz Monzodiorite|61790|6|Mentioned|p315, p318, p319, p320|||||||||
74782|Maryland River Quartz Monzodiorite|71628|5|Briefly described|p16: 8, 20; p19: 100-103, 163-164|||Passmore (1998, unpublished). Not to be confused with the similarly-named Maryland Granodiorite. Named after a local watercourse, along which it is best exposed as unweathered boulders. Forms a small (1 x 0.8 km), horseshoe-shaped intrusion ~12 km NE of Stanthorpe. Mineralogy detailed, geochemistry described and briefly discussed.||Maryland River Suite.||Is intruded by dykes of Thomkins Gully Monzogranite Phase.|Greyish-blue, medium-grained, seriate, biotite-(hornblende) quartz monzodiorite, characterised by magmatic-schistose and alkali granite enclaves. ?A-type (contaminated).|
25216|Matong Granodiorite|22815|4|Described|p56|Silurian|Silurian|||||||
25216|Matong Granodiorite|41905|2|Defined|p50|Silurian||Reserved as Matong Granite||||||
25216|Matong Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
25216|Matong Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Dalgety Suite.||||||
25216|Matong Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb20.||||||
25216|Matong Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
26020|Matthews Gap Dacitic Tuff Member|24603|5|Briefly described|p896 Fig. 17|Late Carboniferous|Late Carboniferous|Age: 309+/-3Ma (Gulson et al, 1990).  Geological Province: Tamworth Belt.  See also p898.||||||
26020|Matthews Gap Dacitic Tuff Member|29915|2|Defined|p67|Late Carboniferous|Middle Carboniferous|Middle or Upper Carboniferous||||||
26020|Matthews Gap Dacitic Tuff Member|42214|4|Described|p459|||||||||
26020|Matthews Gap Dacitic Tuff Member|62095|5|Briefly described|p267|Late Carboniferous|Late Carboniferous|Uppermost member in the Pokolbin Hills Volcanics. Age: 309+/-3Ma.||||||31-JAN-08
26020|Matthews Gap Dacitic Tuff Member|69635|5|Briefly described|p189, 193|Late Carboniferous|Late Carboniferous|309+/-3 Ma (U-Pb zircon) and 302+/-4  Ma (K-Ar hornblende) by Gulson et al. (1990).||Of Pokolbin Hills Volcanics.||either overlying (Brakel, 1972) or underlying (Willey, 2010) the ignimbrite member.||
26020|Matthews Gap Dacitic Tuff Member|73304|5|Briefly described|p62|Kasimovian|Moscovian|Sydney Basin, northern. Dating by U-Pb CA-TIMS (Gulson et al., 1990).|309 +/- 3 Ma|Patterson Volcanics||||
76034|Maude granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Baconian Swamp Granite Suite.|||Interpreted S-type granites.|
76034|Maude granite|70718|4|Described|p75-p76, p124|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics. Magnetic highs have correpsonding gravity lows.||Baconian Swamp granite suite|||S-type granitic rocks.|31-MAY-19
69815|Maybole Volcanic Suite|63347|2|Defined|p27, p5 Fig. 2, p6,p15, p22|Early Oligocene|Middle Eocene|Includes the Maybole Volcanics.Unconformably overlain by Langari Hill Volcanics. Age: 40-32Ma (K-Ar). Lithologies include mafic flows, tuffs, intrusions and volcaniclastic rocks of alkaline affinity.||||||16-FEB-23
69815|Maybole Volcanic Suite|73581|5|Briefly described|p10, p14-16|Oligocene|Eocene|Described by Vickery et al., (2007). List of fission track and K-Ar ages provided. Mantle and lower crustal xenoliths and megacrystal suites are relatively common in alkaline lavas. Includes minor alkaline endmember fractionates, zircon and sapphire megacrysts (U-Pb ages 45-32 Ma; Abduryim et al., 2012).|43.9+/-0.6 Ma, 31.3+/-5.5 Ma fission track|||Underlies Langarai Hill Volcanics|Main unit is undersaturated alkali olivine to transitional basalt with minor lithic volcaniclastic and epiclastic units including sapphire-bearing basal units. Rare plugs, sills and dykes, including a phonolite plug.|
69817|Maybole Volcanics|63347|2|Defined|p5 Fig. 2, p27|Early Oligocene|Middle Eocene|Of Maybole Volcanic Suite. Unconformable below Delungra V.S/Langari Hill V.S. Max.thickness: >400m; 100m in type area. Alkali olivine and transit.basalt flows+plugs and red and white sapphire-bearing tuffs + minor corundum-bearing volcaniclastic rocks.||||||
23774|Mayers Flat Limestone Member|36057|2|Defined|p345|Early Carboniferous|Early Carboniferous|||||||
23774|Mayers Flat Limestone Member|39660|6|Mentioned|p450|||||||||
23774|Mayers Flat Limestone Member|42547|5|Briefly described|p34|||||||||
23774|Mayers Flat Limestone Member|44244|4|Described|p199|Tournaisian|Tournaisian|Of the Wallanbah Formation.  Max. thickness: 20m.  Type section in text.  Geological Province:  Myall Block.||||||25-AUG-04
23775|Mayfair Granite|22638|1|Redefined|p30|Llandovery|Ashgillian|Wallundry Suite. 431 +/- 4 Ma Rb-Sr date. New name.||||||17-JUL-07
23775|Mayfair Granite|42726|5|Briefly described|map legend|Silurian||||||||
23775|Mayfair Granite|44192|5|Briefly described|Map Legend||Llandoverian|||||||
22284|McCabes Granite|22638|2|Defined|p30|Llandovery|Ashgillian|Wallundry Suite. 431 +/- 4 Ma Rb-Sr date. New name. Previously "Woodlands Granite"||||||
22284|McCabes Granite|44192|5|Briefly described|Map Legend||Llandoverian|||||||
37576|McCarty Limestone|23309|5|Briefly described|p94|Llandovery|Llandovery|Of Cowombat Siltstone.||||||
36964|McGraths Hump Metabasalt|22857|5|Briefly described|p516 App.1 Tb.A1.8|Early Permian|Carboniferous|Metabasaltic pillow lava and massive flows, dolerite intrusives; minor siltstone and diamictite. Max. thickness: 1900m. ||||||
36964|McGraths Hump Metabasalt|23720|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Metabasaltic pillow lavas and massive flows, dolerite intrusives and minor siltstone and diamictite.||||||15-DEC-04
36964|McGraths Hump Metabasalt|24127|5|Briefly described|p5|||||||||
36964|McGraths Hump Metabasalt|44093|5|Briefly described|p243 App. 1|Early Permian|Early Permian|Geological Province: New England Fold Belt.||||||
36964|McGraths Hump Metabasalt|44450|3|Fully described|p22 Table 4|Early Permian|Late Carboniferous|Geological Province: Nambucca Block. Max. thickness: 2000 m||||||
36964|McGraths Hump Metabasalt|71628|5|Briefly described|p2:34; p3:46|||Nambucca Block. Contact-metamorphosed by Dorrigo Mountain Complex intrusion.||||Is intruded by Dorrigo Mountain Complex. Is faulted against Gleniffer Monzogranite.||
31610|McKeahnie Suite|42726|5|Briefly described|map legend||Silurian|||||||
75068|McMillan Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
75068|McMillan Formation|65388|6|Mentioned|p199|||South West Bowen Basin? Grades laterally  to NE into Moranbah Coal Measures.||||||
25223|Meadow Flat Shale|39364|6|Mentioned|p51|||||||||
80168|Medowie Clay Member|68811|6|Mentioned|p63, p167 tbl 29|Quaternary|Quaternary|Age assumed from map symbol. Aquitard.||||Overlain by the Tomago Sandbeds.||14-APR-20
27486|Melbergen Sandstone|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27486|Melbergen Sandstone|61964|3|Fully described|p14 Fig. 4,  p123|Famennian|Frasnian|Of Cocoparra Gp. Previously Melbergen Sandstone Member of Cocoparra Gp (Conolly 1962). Lith.details included. Conformably overlies Confreys Fm; conformably underlies Jimberoo Fm; also conformable below Miocene Tullibigeal Leucitite. Max. thickness:1158m.||||||14-OCT-08
27486|Melbergen Sandstone|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Thin to medium bedded, red to white medium-grained orthoquartzite.||||||25-MAR-08
27486|Melbergen Sandstone|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.||Overlies Confreys Formation. Is overlain by Jimberoo Formation.|Thin- to medium-bedded red to white fine- to medium-grained orthoquartzite.|
27486|Melbergen Sandstone|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|||Thin- to medium-bedded red to white fine- to medium-grained orthoquartzite.|
27486|Melbergen Sandstone|71889|5|Briefly described|p48, p54, p64|||Rankin Springs area. Rocks previously assigned to the Narrandera Sandstone are now recognised as extensions of this unit.||Cocoparra Group||Equivalent to the Narrandera Sandstone.|Quartz rich sandstone and lithic quartz sandstone.|
27486|Melbergen Sandstone|73457|6|Mentioned|p6|||||Mulga Downs Group||||
31301|Melgra Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Quartzite.||||||
24377|Meloola Volcanics|22831|4|Described|p 46|Early Devonian|Late Silurian|||||||
24377|Meloola Volcanics|22857|4|Described|p448 App.1, Tb.A1.6|Pridolian|Pridolian|Of the Derriwong Group. Fine-grained siliceous volcanics, minor arenite, siltstone, conglomerate; contains corals, conodonts. Max. thickness: 230m. Geological Province: Bogan Gate Terrace.||||||
24377|Meloola Volcanics|23522|5|Briefly described|p253|Devonian|Devonian|||||||
24377|Meloola Volcanics|40365|2|Defined|p326|Early Devonian|Early Devonian|||||||
24377|Meloola Volcanics|42449|3|Fully described|p12|||||||||
24377|Meloola Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
24377|Meloola Volcanics|43441|5|Briefly described|27|Early Devonian|Late Silurian|||||||08-JAN-10
24377|Meloola Volcanics|44160|5|Briefly described|Map Legend||Pridolian|||||||08-JAN-10
24377|Meloola Volcanics|61894|5|Briefly described|p181|Pridoli|Pridoli|Condobolin area. The article states (twice) that this unit is "of Cookeys Plains Formation, Derriwong Group", which could only be the case if it were named Meloola Volcanics Member [which it isn't].||Derriwong Group.||||
24377|Meloola Volcanics|62070|5|Briefly described|p37|Pridoli|Ludlow|Occurs near Condobolin, NSW .Includes coral Squameofavosites squamuliferus.||||||
24377|Meloola Volcanics|68297|5|Briefly described|p181|Pridoli|Pridoli|Fifield, NSW. Limestones include small vertebrate fossil fauna.||||||
39132|Melougel Ignimbrite|61964|3|Fully described|p14 Fig. 4, p85, p80|Early Devonian|Late Silurian?|Chemically a member of Ural Volcanics (Rast Group). A-type. Dk. grey elongated tors of very crystal-rich, densely welded ignimbrite + some broken phenocrysts and faint, relict strung-out shards and pumice fragments. Unconformable below ?Barrat Formation||||||
39132|Melougel Ignimbrite|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Ural Volcanics (Rast Group). Crystal-rich, densley welded ignimbrite, rare pumice clasts.||||||10-APR-08
39132|Melougel Ignimbrite|63019|5|Briefly described|p920, p921 Fig.2|Lochkovian|Lochkovian|Of Rast Group. Geological Province: Lachlan Orogen.||||||23-JAN-07
39132|Melougel Ignimbrite|69161|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Rast Group.|||Crystal-rich, densely-welded ignimbrite, rare pumice clasts.|
33758|Menamurtee Sandstone|24345|4|Described|p83, p84-85 Fig. 2|Eifelian|Emsian|||||||
33758|Menamurtee Sandstone|63632|6|Mentioned|p654|Emsian|Emsian|||||||
33758|Menamurtee Sandstone|66623|1|Redefined|pp192-195, pp208-212. |Middle Devonian|Early Devonian|Formerly Mootwingee Series (Andrews 1922), undifferentiated Mulga Downs Group (Rose 1974), Menamurtee Dome Sequence (Neef et al. 1996), part of Snake Cave Sandstone (Buckley 2000), Muckabunnya beds of Neef & Larsen (2002). Redefined in this study. Meenamurtee Hills, Koonenberry Belt. Forms prominent high strike ridges. Thickness more than 3700 m. Coeval with Muckabunnya Formation units e to h; laterally equivalent to top half of Wana Karnu Group. Contains fossil fish fragments. Upper parts may be Ravendale Formation equivalents.||Unit in Wana Karnu Group.|Includes Moona Vale Conglomerate Member.|Locally overlies unit c of Muckabunnya Sandstone. Is overlain unconformably by Gum Creek Member and Eyre Formation.|Medium- to coarse-grained, pebbly, massive grey lithic and quartzose sandstone; brown weathered veneer; subangular vein quartz and minor rounded quartzite pebbles scattered and as lags; rare conglomerate beds to 5m thick; local kaolinite-rich beds.|
33758|Menamurtee Sandstone|67562|5|Briefly described|p102 Fig.8, p106-107, p111-113|Eifelian||Strata coeval with units 4-8 of the Copper Mine Range sequence were renamed as the Menamurtee Sandstone (Neef and Larsen 2003). Contains fragments of the Wuttagoonaspis fletcheri found ~ 100m above the base of this unit indicates a minimum  Eifelian age.|||Moona Vale Conglomerate Member.|Overlies Muckabunnya Beds. Unconformably overlain by the Gum Creek Beds.||23-JAN-17
33758|Menamurtee Sandstone|70651|5|Briefly described|Map Legend|Devonian|Devonian|||Wana Karnu Group|Includes Moona Vale Conglomerate [Member?].||Medium- to coarse-grained, pebbly, massive grey lithic and quartzose sandstone, local kaolinite-rich bends and rare conglomerate beds up to 5m thick.|
33758|Menamurtee Sandstone|71040|6|Mentioned|p14|Emsian|Emsian|Age from fossil fish.||||||
26028|Merlewood Formation|721|5|Briefly described|Map legend|Visean|Visean|Coarse, crossbedded feldspathic and lithic sandstone, minor conglomerate, mudstone, limestone.  Geological Province: Tamworth Belt.||||||21-DEC-04
26028|Merlewood Formation|22572|6|Mentioned|p108||Carboniferous|||||||
26028|Merlewood Formation|22736|6|Mentioned|p630||Visean|||||||
26028|Merlewood Formation|22857|4|Described|p496 App.1 Tb.A1.7|Visean|Visean|Coarse, cross-bedded feldspathic and lithic arenite and minor conglomerate, mudstone, limestone. Max. thickess: 1500m. Geological Province: Tamworth Forearc Basin.||||||
26028|Merlewood Formation|23102|5|Briefly described|p561|||||||||
26028|Merlewood Formation|23185|6|Mentioned|Fig1p156|Carboniferous|Carboniferous|||||||
26028|Merlewood Formation|24010|6|Mentioned|p379 Fig. 5|||||||||
26028|Merlewood Formation|24348|5|Briefly described|p133|Carboniferous|Carboniferous|||||||
26028|Merlewood Formation|24366|6|Mentioned|p5|||||||||
26028|Merlewood Formation|24603|5|Briefly described|p866, p875||Visean|Contains volcanolithic sandstone, pyroclastics and three thick pyroxene andesite units (~200m).  See also p869 Fig. 4a, p886 Fig.11, p872 Tb. 1.  Geological Province: Tamworth Belt.||||||
26028|Merlewood Formation|30070|6|Mentioned|Fig.2|||Devonian age.||||||
26028|Merlewood Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26028|Merlewood Formation|31519|6|Mentioned|Fig. 1|||||||||
26028|Merlewood Formation|31586|6|Mentioned|p6|||Equiv. in part to Cannindah Lst.||||||
26028|Merlewood Formation|31587|6|Mentioned|p63|||Rugose corals||||||
26028|Merlewood Formation|32286|4|Described|p49|||||||||
26028|Merlewood Formation|32482|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
26028|Merlewood Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26028|Merlewood Formation|32866|6|Mentioned|p13|||Fossil content||||||
26028|Merlewood Formation|32867|6|Mentioned|p66|||||||||
26028|Merlewood Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
26028|Merlewood Formation|34081|6|Mentioned|p260|||||||||
26028|Merlewood Formation|34083|3|Fully described|p247|||Previously Lower Kuttung Series.||||||14-APR-08
26028|Merlewood Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
26028|Merlewood Formation|34086|6|Mentioned|p263|||||||||
26028|Merlewood Formation|36528|6|Mentioned|p178|||||||||
26028|Merlewood Formation|36961|6|Mentioned|p210|||See also Fig.3.||||||
26028|Merlewood Formation|37919|6|Mentioned|Fig.2|||||||||
26028|Merlewood Formation|37987|2|Defined|p229|Visean|Visean|||||||
26028|Merlewood Formation|38222|5|Briefly described|p358|||||||||
26028|Merlewood Formation|38818|6|Mentioned|p167|||||||||
26028|Merlewood Formation|39214|4|Described|p33|||||||||
26028|Merlewood Formation|39299|6|Mentioned|p279|||||||||
26028|Merlewood Formation|39331|6|Mentioned|Table 10-1|||||||||
26028|Merlewood Formation|39468|6|Mentioned|Fig.2|||||||||
26028|Merlewood Formation|39572|6|Mentioned|Fig.2|||||||||
26028|Merlewood Formation|40177|6|Mentioned|p51|||||||||
26028|Merlewood Formation|40246|6|Mentioned|Table 1|||||||||
26028|Merlewood Formation|40883|6|Mentioned|p13|||||||||
26028|Merlewood Formation|41009|6|Mentioned|Fig.2|||||||||
26028|Merlewood Formation|41279|6|Mentioned|Fig.3|||||||||
26028|Merlewood Formation|41347|4|Described|Table 3|||||||||
26028|Merlewood Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Temi Syncline.||||||16-DEC-04
26028|Merlewood Formation|41800|6|Mentioned|p499|||||||||
26028|Merlewood Formation|41990|6|Mentioned|Fig.2 P12|||||||||
26028|Merlewood Formation|42002|6|Mentioned|p94|||||||||
26028|Merlewood Formation|42547|4|Described|p21|||Werrie Syncline.||||||
26028|Merlewood Formation|43091|5|Briefly described|Map legend|||||||||
26028|Merlewood Formation|43383|14|Not recorded|p17,18|||||||||
26028|Merlewood Formation|43407|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition) Middle Carboniferous||||||
26028|Merlewood Formation|43409|14|Not recorded|Map Legend|||||||||
26028|Merlewood Formation|43417|14|Not recorded|Map Legend|||(Werrie Basin) Lower horizons equivalent Waverley Formation||||||
26028|Merlewood Formation|43418|14|Not recorded|Map Legend|||||||||
26028|Merlewood Formation|43432|14|Not recorded|p203||Visean|||||||
26028|Merlewood Formation|43479|14|Not recorded|p158,159,177||Visean|||||||
26028|Merlewood Formation|43538|14|Not recorded|p1,2||Visean|Lower Carboniferous fauna.||||||
26028|Merlewood Formation|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
26028|Merlewood Formation|44833|14|Not recorded|p117|||||||||
26028|Merlewood Formation|44835|4|Described|p45-47,Pl.1||Carboniferous|Formerly called Upper Kuttung Series.||||||
26028|Merlewood Formation|45097|6|Mentioned|p24|||Correlation chart. Fossils.||||||
26028|Merlewood Formation|46803|6|Mentioned|Fig. 3|||||||||
26028|Merlewood Formation|47056|6|Mentioned|Fig.2 P523|||||||||
26028|Merlewood Formation|50132|6|Mentioned|p247 Fig. 5|Carboniferous|Carboniferous|||||||
26028|Merlewood Formation|61769|6|Mentioned|p99 Fig. 4|||||||||
26028|Merlewood Formation|62095|4|Described|p251, p272 Appdx.|Carboniferous|Carboniferous|Includes Kingshill Peak Andesite, Isismede , Burnewang and Wheelihans Gap Ig. Mmbrs. Predominantly pink, zeolitic, volcanolithic sst. and conglomerate with.... Conformableover Goonoo Goonoo Fm; disconformable below Currabubula Fm. Geol.Prov: Werrie block.||||||31-JAN-08
26028|Merlewood Formation|63832|6|Mentioned|p131 fig 2|Serpukhovian|Visean|Werrie Syncline, Southern New England Fold Belt.||||||
26028|Merlewood Formation|64631|5|Briefly described|p44 Fig.2.|Serpukhovian|Visean|Southern New England Fold Belt, Werrie Syncline. Some biostratigraphic and radiometric age control within unit.||||Overlies Namoi Formation.||
26028|Merlewood Formation|65107|6|Mentioned|Fig 11, 286-7|Carboniferous|Carboniferous|Shown in a Carboniferous age pole path for Tamworth Belt rocks,Werrie Block.||||||
26028|Merlewood Formation|65902|4|Described|p195, 199-201, 202-4, Figs.5, 7|Carboniferous|Carboniferous|Previously referred to as Lower Kuttung Series (Carey, 1937).|||Includes Kyndalyn Member.|Overlies Namoi Formation; overlain by Currabubula Formation.|Predominantly non-marine lithic sandstone, conglomerate, minor siltstone and heavy-mineral sandstone.|09-MAR-12
26028|Merlewood Formation|66498|6|Mentioned|p47, 49||||||Kyndalyn Member.|||
26028|Merlewood Formation|66720|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous||||Includes Kyndalyn Mudstone Member and an un-named but separately mapped unit of massive fine-grained limestone.||Coarse-grained, cross-bedded, feldspathic and lithic sandstone; minor conglomerate, mudstone and limestone; rare andesite.|
26028|Merlewood Formation|68003|5|Briefly described|p32 Fig.3-h, p134. |Visean|Visean|Tamworth Belt (South); New England Fold Belt. Coeval with Isismurra Formation. SHRIMP AS3 ages from un-named ignimbrites.|348.1 +/- 1.8 to 326.8 +/- 1.9 Ma.||Includes Kyndalyn Mudstone Member.||Coarse cross-bedded feldspathic and lithic sandstone; red-pink ignimbrites, unwelded, locally pumiceous; minor conglomerate, mudstone and limestone.|
26028|Merlewood Formation|68005|5|Briefly described|p49 Fig.3-M, p56, pp141-142, p170.|Visean|Visean|Werrie Block, Tamworth Belt. A marine to terrestrial transition sequence.|||Includes Kyndalyn Mudstone Member and Kingsmill Peak Andesite Member.||Limestone, andesite, dacite, ignimbrites, conglomerate, sandstone and siltstone with rare coal.|
26028|Merlewood Formation|68006|6|Mentioned|p115.|||Tamworth Belt. Contains extensive but thin and impure beds of limestone.||||||
26028|Merlewood Formation|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Tournaisian|Werrie Block, Tamworth Belt.|||Includes Kyndalyn Member.|||
26028|Merlewood Formation|70050|5|Briefly described|p334, p347, p358, p365|Visean|Visean|Babbinboon area.|||Kyndalyn Mudstone Member.|||
26028|Merlewood Formation|70728|5|Briefly described|p265,271-273|Serphukovian|Tournaisian|Geological province: North Tamworth terrane, New England Orogen.||||Overlain by Currabubula Formation or Coepolly Conglomerate. Underlain by Namoi Formation or Goonoo Goonoo Formation.||
26028|Merlewood Formation|70777|5|Briefly described|p2, p8, p82|Early Carboniferous|Early Carboniferous|Werrie Block, New England Orogen.|||Includes the Isismede Ignimbrite Member.|||
26028|Merlewood Formation|70907|5|Briefly described|p773, p774 Fig.2|Carboniferous|Carboniferous|||||Overlies Namoi Formation.|Mainly lithic sandstones and conglomerate.|
23787|Merrastone Formation|721|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, breccia, lithic sandstone, siltstone, mudstone.||||||
23787|Merrastone Formation|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Early Permian|Conglomerate, breccia, lithic sandstone, siltstone, mudstone. Max. Thickness: 375m.||||||
23787|Merrastone Formation|23790|5|Briefly described|p6 Fig. 5|||||||||
23787|Merrastone Formation|41009|3|Fully described|p6|||||||||
23787|Merrastone Formation|43091|5|Briefly described|Map legend|||||||||
23787|Merrastone Formation|71628|6|Mentioned|p8-40|||||||May be intruded by The Basin Monzogranite (no contacts observed).||
31493|Merricumbene Suite|22878|6|Mentioned|p83|||||||||
31493|Merricumbene Suite|42726|5|Briefly described|map legend||Early Devonian|Of the (Cobargo Supersuite.  Includes Merricumbene Granite (informal name).||||||09-FEB-05
31493|Merricumbene Suite|44093|5|Briefly described|p222 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
31719|Merriganowry Shale Member|22857|5|Briefly described|p490 App.1 Tb.A1.7|Middle Devonian|Middle Devonian|Of the Dulladerry Volcanics. Geological Province: Dulladerry Rift.||||||
31719|Merriganowry Shale Member|23214|4|Described|p224|Givetian|Givetian|Of Dulladerry Volcanics. Shale, volcaniclastic sandstone and rhyolite lava.||||||
31719|Merriganowry Shale Member|24417|5|Briefly described|p128|||Of Dulladerry Volcanics.||||||
31719|Merriganowry Shale Member|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Dulladerry Volcanics. Consists of slumped shale with graded interbeds of rhyolitic sandstone, minor rhyolite lava.||||||17-JUL-08
31719|Merriganowry Shale Member|43782|5|Briefly described|Map Legend|Givetian|Givetian|Of Dulladerry Volcanics.||||||17-JUL-08
31719|Merriganowry Shale Member|62569|5|Briefly described|p610 Fig. 4|Late Devonian|Middle Devonian|Of Dulladerry Volcanics. ||||||
31719|Merriganowry Shale Member|67823|6|Mentioned|p366|||||Of the Dulladerry Volcanics||||
31719|Merriganowry Shale Member|70297|5|Briefly described|map legend|Middle Devonian|Middle Devonian|||Dulladerry Volcanics||||
29917|Merrions Formation|22451|6|Mentioned|p24|||||||||
29917|Merrions Formation|22472|4|Described|p39|Early Devonian|Early Devonian|Formerly Merrions Tuff||||||
29917|Merrions Formation|22529|4|Described|1,4 fig 2, 8|Early Devonian|Early Devonian|||||||
29917|Merrions Formation|22590|3|Fully described|p750-757, p753, Fig1||Pragian|Formerly Merrions Tuff. Type section sampled/dated at 4 stratigraphic levels: basal arenite P; intermediate arenite member D, dacitic lava H, upper arenite member E Agerage of unit is 411.9+/-5 Ma to  407.1 +/- 6.9 Ma.||||||10-SEP-18
29917|Merrions Formation|22679|5|Briefly described|p 34||Early Devonian|||||||
29917|Merrions Formation|22768|5|Briefly described|p179-80||Eifelian|||||||
29917|Merrions Formation|22857|5|Briefly described|p179, p180, p470 App.1 Tb.A1.6|Eifelian|Eifelian|Of the Crudine Group. Lavas, tuffs and breccias. Age: 349-338Ma (Cas, Flood and Shaw, 1976). Max. thickness: 660m. Geological Province: Hill End Trough and Capertee Rise. See also p478 App.1 Tb.A1.6 and p239.||||||
29917|Merrions Formation|22863|6|Mentioned|p239|Visean|Tournaisian|Max Age: 349 Ma; Min Age: 338 Ma.||||||
29917|Merrions Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
29917|Merrions Formation|23170|2|Defined|p171-174,|Pragian|Lochkovian|Of Crudine Group. Ages reported from Appendix 2 of Bathurst Explan notes. The 405 +/-5 Ma age is from Cas (1978).|top 405.5+/-4.4 Ma, 411+/-3 Ma SHRIMP (Black 1996)|||||10-SEP-18
29917|Merrions Formation|23214|3|Fully described|p193-194, App2 p393|Lochkovian|Lochkovian|Of Crudine Group. Formerly Merrions Tuff. Originally mapped as Paling Yard Tuff and Winburn Tuff. Max. thickness 662m. type section described. Top age constrained by fauna in overlying Limekilns and Cunningham Formations. SHRIMP dating from Jagodzinski et al.in prep,  & Black (1996) gives ages of 410+/-2 Ma, 411+/-3 Ma. Younger radiometric ages listed in Appendix 2, from Cas (1978),  are not discussed in the text.||||||10-SEP-18
29917|Merrions Formation|23738|5|Briefly described|p251|Devonian|Devonian|||||||
29917|Merrions Formation|23851|5|Briefly described|p797|Early Devonian|Early Devonian|||||||
29917|Merrions Formation|24394|4|Described|p169, p170|Pragian|Pragian|Underlying unit: Waterbeach Formation.  Maximum thickness: 615m.  Geological Province: Lachlan Fold Belt.||||||
29917|Merrions Formation|43494|4|Described|p27||Devonian|Supersedes Merrions Tuff. Uppermost unit in Crudine Gp. Conformable over Waterbeach Fm in SE and Guroba Fm in NW.  Conformable over Waterbeach Fm in SE and Guroba Fm in NW; overlain by Cunningham Fm. Max. thick: 700m.||||||16-MAR-06
29917|Merrions Formation|43639|5|Briefly described|Map Legend||Devonian|||||||
29917|Merrions Formation|43641|5|Briefly described|Map Legend||Devonian|||||||
29917|Merrions Formation|43653|5|Briefly described|Map Legend||Devonian|||||||
29917|Merrions Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
29917|Merrions Formation|49916|5|Briefly described|p510|Silurian|Silurian|Age: 413.4+/-5.5Ma and 411.8+/-5.5Ma.||||||
29917|Merrions Formation|62569|6|Mentioned|p612|Early Devonian|Early Devonian|Contains fish plates remains. ||||||
29917|Merrions Formation|64994|5|Briefly described|p1, p8, p9|pragian|Pragian|Overlain by Limekilns Formation. Geological province: Lachlan Orogen/Hill End Trough - marks the top of the Trough and can be correlated with Riversdale Volcanics on the adjacent Capertee High. Volcaniclastics.||||||07-FEB-11
29917|Merrions Formation|66197|5|Briefly described|p633 Fig.4a|Emsian|Lochkovian|Top of Crudine Group. Capertee High-Hill End Trough. Deep marine volcaniclastics. Underlies the Cunningham Formation. Age: 405 - 412 Ma ?mid-Pragian.||||||13-MAR-12
29917|Merrions Formation|68003|5|Briefly described|p24 Fig.3-e. |Lochkovian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Crudine Group.||Overlies Guroba Formation. Is overlain by Cunningham Formation.||
29917|Merrions Formation|68592|4|Described|p1038, p1059, p1147|Lochkovian|Lochkovian|Northern Hill End Trough. Formerly Merrions Tuff. SHRIMP U-Pb zircon ages by Jagodzinski and Black (1999).|411.9 +/- 5.0 Ma to 407.1 +/- 6.9 Ma.|Unit in Crudine Group.||May correlate with Bushranger Volcanics and Barrallier Ignimbrite.|Includes submarine mass-flow facies.|
29917|Merrions Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
29917|Merrions Formation|71700|5|Briefly described|CD|Early Devonian|Early Devonian|Hill End Trough. Potentially equivalent to the subaqueous ignimbrites of the Bindook Group.||Crudine Group|||Volcaniclastic rocks.|
29917|Merrions Formation|73299|5|Briefly described|p1093, p1096 Fig.3, p1098 Fig.4, p1101|Early Devonian|Late Silurian|Lachlan Orogen, Hill End Trough. Thickness variations determined a northwest- to southeast-trending axis of the basin (Cas, 1977). Disharmonic folding southeast of Hill End. Locations in text include p1102 Fig.8 and p1108. [Map symbol suggests Devonian age]||||Overlies the Waterbeach Formation, Guroba Formation, underlies the Cunningham Formation.|Volcaniclastic.|
22317|Merriown Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
80452|Merritop granite|70718|5|Briefly described|p65, 66|||Informal name, interpreted from geophysics. Referred to as the Merritop granodiorite on p65 fig 35, p66.||Glen Emu granite suite|||Interpreted as granite or granodiorite.|31-MAY-19
26029|Merrygoen Ironstone Member|30610|2|Defined|p323|Middle Jurassic|Early Jurassic|Lower to Middle Jurassic.||||||
26029|Merrygoen Ironstone Member|35095|6|Mentioned|p108Table 1|||||||||10-MAR-19
41247|Merton Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Hornfels.||||||
26275|Merumbago Granodiorite|22815|4|Described|p54|||||||||
26275|Merumbago Granodiorite|38500|6|Mentioned|Fig.2|||||||||
26275|Merumbago Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
26275|Merumbago Granodiorite|41133|6|Mentioned|p1123|||||||||
26275|Merumbago Granodiorite|41905|2|Defined|p39|Early Silurian||||||||
26275|Merumbago Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
26275|Merumbago Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Finister Suite.||||||
26275|Merumbago Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh20||||||
74755|Merungi Gap Conglomerate Member|61964|2|Defined|p120-123|Late Devonian|Late Devonian|Revised stratigraphy of Cocoparra Gp recently added this unit at top of Naradhan Sandstone. Primarily a polymictic orthoconglomerate with clasts to cobble size + matrix of v.coarse-gr. quartz lithic sst. See also misspelt Meringi Gap Conglomerate Member.||||||23-OCT-08
31606|Micaligo Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
70032|Micalong Suite|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes the Micalong Swamp Basic Igneous Complex of gabbro and dolerite.||||||16-JUN-08
70032|Micalong Suite|68592|2|Defined|p1214-23|Wenlock|Wenlock|New name, after Micalong Creek. These basic intrusions were first noted by Best et al. (1964), and mapped by Owen and Wyborn (1979) as their Micalong Swamp Basic Igneous Complex, which is here included in the Micalong Suite. Type pluton locality described. Deeply weathered; exposed mostly as boulder float in red soil. Geochemistry detailed.  Age of 428.8 +/- 1.9 Ma (SHRIMP U-Pb zircon) for Young Granodiorite intrusion by Black (pers. comm. in Lyons et al. 2000); an intrusive feeder dyke of Goobarragandra Volcanics was dated 429 +/- 9 Ma, and a Burrinjuck Granite intrusion at 415 +/- 8 Ma (both by Owen and Wyborn, 1979). A K-Ar hornblende isotopic age of 430 +/- 9 Ma was obtained from a Micalong Suite pluton by Owen and Wyborn (1979).|<415 +/- 8 Ma (K-Ar biotite isotopic age).||Includes Micalong Swamp Basic Igneous Complex.|Intrudes Goobarragandra Volcanics. Is intruded by Young Granodiorite and Burrinjuck Granite.|Plutons include dolerite, gabbro and tonalite as well as quartz diorite and leucogranodiorite, with very minor hornblende pyroxenite. Gabbro and diorite typically well jointed; local steeply dipping spaced cleavage. I-type.|
70032|Micalong Suite|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Error in Geological Reference Legend: shown as containing constituent 'Sim' Little Redbank Granodiorite. Should be 'Sim' Micalong Swamp Basic Igneous Complex. It is correctly shown ('Sim' Micalong Swamp Basic Igneous Complex in Micalong Suite) in the Time-Space Plot, on the Yass 1:100 000 sheet portion.|||Includes Micalong Swamp Basic Igneous Complex.|||
70032|Micalong Suite|70540|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Micalong Swamp Basic Igneous Complex.|||
27194|Micalong Swamp Basic Igneous Complex|22691|6|Mentioned|P315||Llandovery|Age of unit is 430+/-9 Ma||||||
27194|Micalong Swamp Basic Igneous Complex|23454|6|Mentioned|p27 Fig.1|||||||||
27194|Micalong Swamp Basic Igneous Complex|33959|6|Mentioned|p235|||||||||
27194|Micalong Swamp Basic Igneous Complex|36441|5|Briefly described|map legend|Late Silurian|Late Silurian|Extrusive. Gabbro, hornblende magnetite gabbro, dolerite, leucogabbro, gabbro pegmatite, anorthosite, quartz gabbro. BMR map code: Sbm.||||||
27194|Micalong Swamp Basic Igneous Complex|36443|5|Briefly described|map legend|Pridolian|Late Silurian|Gabbro, dolerite, leucogabbro, gabbro pegmatite. BMR map code: Sbm.||||||
27194|Micalong Swamp Basic Igneous Complex|37529|5|Briefly described|p6|||||||||
27194|Micalong Swamp Basic Igneous Complex|42145|5|Briefly described|p636|||||||||
27194|Micalong Swamp Basic Igneous Complex|42313|3|Fully described|p84|Middle Silurian||Age: early Middle Silurian||||||
27194|Micalong Swamp Basic Igneous Complex|42314|5|Briefly described|Map|Middle Silurian||||||||
27194|Micalong Swamp Basic Igneous Complex|42497|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
27194|Micalong Swamp Basic Igneous Complex|42828|5|Briefly described|Table 1 P129|Late Silurian|Middle Silurian|||||||
27194|Micalong Swamp Basic Igneous Complex|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sg1||||||
27194|Micalong Swamp Basic Igneous Complex|45147|2|Defined|M292|Late Silurian|Late Silurian|||||||
27194|Micalong Swamp Basic Igneous Complex|50230|5|Briefly described|Map legend|Wenlock|Wenlock|Equigranular gabbro to dolerite.||||||
27194|Micalong Swamp Basic Igneous Complex|60078|6|Mentioned|Map Legend|Late Silurian|Late Silurian|||||||
27194|Micalong Swamp Basic Igneous Complex|64238|5|Briefly described|Map legend|Silurian|Silurian|Part of  Micalong Suite. Equigranular gabbro and dolerite. High magnetic susceptibility.||||||16-JUN-08
27194|Micalong Swamp Basic Igneous Complex|68592|2|Defined|p17, p441-3, p454, p1214-23|Wenlock|Wenlock|Named after Micalong Swamp which occurs in the headwaters of Micalong Creek. These basic intrusions were mapped by Owen and Wyborn (1979) as their Micalong Swamp Basic Igneous Complex, which is here included in the Micalong Suite. MacDonald (1979) extended the unit's distribution by mapping a small gabbro pluton 3.8km W of Burrinjuck Dam. No type section, but two representative areas described. Mostly exposed as boulder float in red soil. Geochemistry detailed; geophysical properties described. Owen and Wyborg (1979) obtained a K-Ar hornblende age of 430 +/- 9 Ma; this is at odds with several intrusions dated between 429 Ma to 415 Ma (details given). The authors conclude a mid Wenlock age is probable.||Unit in Micalong Suite.||Intrudes Goobarragandra Volcanics. Is intruded by Young Granodiorite and Burrinjuck Granite.|Dolerite, gabbro, tonalite, quartz diorite and leucogranodiorite, with very minor hornblende pyroxenite. Gabbro and diorite typically well jointed; local steeply dipping spaced cleavage.|
27194|Micalong Swamp Basic Igneous Complex|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sim. Error in Geological Reference Legend: shown as 'Sim' Little Redbank Granodiorite. Should be 'Sim' Micalong Swamp Basic Igneous Complex. It is correctly shown ('Sim' Micalong Swamp Basic Igneous Complex) in the Time-Space Plot, on the Yass 1:100 000 sheet portion.||Micalong Suite.|||Dark grey equigranular gabbro, diorite and quartz diorite; medium-high magnetic susceptibility.|
27194|Micalong Swamp Basic Igneous Complex|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Micalong Suite|||Dark grey equigranular gabbro, diorite and quartz diorite; medium-high magnetic susceptibility.|
27194|Micalong Swamp Basic Igneous Complex|71069|6|Mentioned|p179|||||||Part equivalent to the Lockhart Igneous Complex.||
83329|Middle Beach Member|73136|5|Briefly described|p193, p198|Upper Pleistocene|Upper Pleistocene|Lord Howe Island, east coast. Part of alloformation N2. Overlies the comparatively more consolidated dunes of alloformation N1. Eolianite. May have been deposited during an interstadial, perhaps marine oxygen isotope stage 5a. [Written as Middle Beach member on p192].|0.1-0.08 Ma thermoluminescence|Neds Beach Formation||Equivalent[?] to Cobby Corner Member.|Miliolid-rich, very pale brown to white, poorly lithified dune sands.|31-AUG-22
83329|Middle Beach Member|73554|4|Described|Map legend, back of map|Quaternary|Quaternary|Lord Howe Island. Underlies the higher elevation parts of the settlement.||Neds Beach Formation|||White, miliolid-rich (microscopic marine organisms), fine-grained calcarenite, displaying well developed medium- to large-scale cross-bedding.|
35168|Middle Bed|23055|6|Mentioned|Fig13p25|||of Victoria Tunnel Coal Seam, Newcastle Coal Measures.||||||
80914|Middle Brother Granodiorite|71628|4|Described|p17: 2, 76, 78-83|||New name (this study). Previously Middle Brother Diorite (Li et al., 2012) and Middle Brother monzodiorite (Cross and Blevin, 2013). Named after Middle Brother Mountain, 6 km SW of Laurieton. Distribution of this unit is not consistently defined. At least 28 km2. Several age determinations given. Lithologies described in detail. Geochemistry detailed.|212.5 +/- 1.6 Ma (Cross and Blevin, 2013).|The Brothers Suite.||Intrudes Beechwood beds, Mingaletta Formation and Camden Haven Group.|Hornblende-biotite-(pyroxene) granodiorite, two-pyroxene diorite to monzodiorite, and monzogranite. A-type.|
82128|Middle Creek granodiorite|72528|6|Mentioned|p11.|Wenlock|Wenlock|Informal name used in company reports for unnamed porphyritic granodiorite dated herein with U-Pb SHRIMP magmatic crystallisation age of 430.9+/-2.1 Ma|430.9+/-2.1 Ma|||||
22324|Middledale Gabbroic Diorite|22638|4|Described|p29|Llandovery|Ashgillian|Wallundry Suite. 431 +/- 4 Ma Rb-Sr date.||||||
22324|Middledale Gabbroic Diorite|44192|5|Briefly described|Map Legend||Llandoverian|||||||
22324|Middledale Gabbroic Diorite|44936|5|Briefly described|Map Legend||Silurian|||||||
22324|Middledale Gabbroic Diorite|60423|5|Briefly described|p371, 372 Fig. 3|Early Devonian|Early Devonian|Age: 417 Ma (U/Pb). Of the Narraburra Complex. Geological Province: Lachlan Fold Belt.||||||
22324|Middledale Gabbroic Diorite|64571|5|Briefly described|p827|||Zircons from this unit have an age of 417Ma.||||||15-DEC-08
22324|Middledale Gabbroic Diorite|65890|4|Described|157, 167|Lochkovian|Pridoli|~3 sq. km high-level mafic stock in Lachlan Orogen near Temora NSW. Investigated and proposed as Phanerozoic standard material for zircon dating methods. U-Pb IDTIMS age of 416.75+/-0.24Ma 95pct confidence limits; revised to 416.8 +/-1.1 Ma with uncertainites.|416.75+/-0.24;416.8 +/-1.8 Ma U-Pb SHRIMP, ID-TIMS|||Intrudes Bronxhome Formation, Combaning Formation.|Medium- to coarse-grained. Composed dominantly of labrodoritic plagioclase and brown pargasitic hornblende (partially replaced by chlorite). Augite and hyperstene, hematite, ilmenite, magnetite. Strongly magnetic.|14-APR-11
22324|Middledale Gabbroic Diorite|70876|5|Briefly described|p77|Devonian|Devonian|Lachlan Orogen. Additional ages provided from Iles et al, 2015 are: 416.1 +/- 1.6 Ma, 414.8 +/- 1.8 Ma, 414.8 +/- 1.7 Ma 414.1 +/- 1.6 Ma.|416.8 +/- 1.3 Ma (Black et al, 2004)|||||
78457|Midway Granite|68823|5|Briefly described|p378 Fig.4, p393, p402|Carnian|Ladinian|Comprises a small stock about 300 m in diameter. Youngest granite in (this part of) Thomson Orogen. SHRIMP zircon age.|235 Ma +/- 1.4 Ma, (Burton et al 2007)|||||
78457|Midway Granite|69042|6|Mentioned|map, map legends|Devonian||||||||
78457|Midway Granite|69043|6|Mentioned|p11|||||||||
78457|Midway Granite|69541|5|Briefly described|p645 Fig.1(b), p648, p649-652|||Thomson Orogen. Has an age of 235 Ma in Fig.1 (b).|351 +/- 1.4 Ma (Black).|||||
78457|Midway Granite|69635|5|Briefly described|p119, 120, 69|Middle Triassic|Middle Triassic|Porphyritic dykes associated with this unit intersected in drill core DDH DR20 (Aberfoyle). Granite and quartz-feldspar porphyry dyke ages from (Burton et al., 2007).|235+/-1.4 Ma;  dyke 230.7+/-1.4 Ma|||||
78457|Midway Granite|70210|5|Briefly described|p1, p6-7, p38, p40-41|Middle Triassic|Middle Triassic|Cobar-Bourke district. Closely related to Sn mineralisation.|235.1 +/- 1.4 Ma.|||||
78457|Midway Granite|70821|5|Briefly described|p9-10, p12, p13 Tb.2.1|Late Triassic|Late Triassic|Related to tin and base metal mineralisation at Doradilla (described in detail).|235.1 +/- 1.4 Ma (Burton et al., 2007).||||Leucocratic granite. S-type.|01-DEC-16
78457|Midway Granite|71360|5|Briefly described|Map legend|Middle Triassic|Middle Triassic|Geophysical signature: outcrops are too small to be recognised in regional geophysical data and occur at the centre of a cluster of linear and concentric trends with moderate to high magnetic intensity. The outcrops lie within a narrow zone of elevated radiometric values, and occur within a zone of low gravity values. Ages are of granodiorite and quartz-feldspar porphyry, respectively.|235.1 +/- 1.4 Ma; 230.7 +/- 1.4 Ma.||||Granodiorite and quartz-feldspar porphyry.|
78457|Midway Granite|71860|5|Briefly described|p7, p13|||Age is a SHRIMP U-Pb date.|235.1 +/- 1.4 Ma (Burton et al, 2007)||||Leucocratic, fractionated, moderately reduced, metaluminous I-type granite.|
78457|Midway Granite|71965|5|Briefly described|p914|Triassic|Triassic|Of Lachlan Orogen. Similar emplacement age to Permo-Triassic intrusions such as small alkaline stocks, diatremes, plugs and dykes scattered across the southern Thomson Orogen and west of the Koonenberry Belt.||||||
78457|Midway Granite|72296|5|Briefly described|p6|Triassic|Triassic|Doradilla area.||||Intrudes the Girilambone Group.|Granite and associated quartz-feldspar porphyry dykes.|
78457|Midway Granite|72951|5|Briefly described|p1013, 1018, 1022-1023, 1029, 1030|Late Triassic|Late Triassic|Lachlan Orogen. Hermidale Terrane. Extremely fractionated I-type granite, associated with Sn mineralisation at the Doradilla prospect. SHRIMP U-Pb zircon isotope analyses from Black (2006). eHf = 4.0 +/- 0.6, and d18O = 6.24 +/- 0.18. Described as 'Midway granites' p1029, 1030.|235.2 +/- 1.5 Ma||||Felsic granodiorite.|
78457|Midway Granite|73175|6|Mentioned|p1063, p1064 Fig.11, p1065|Triassic|Triassic|A-type granites. U-Pb age from Black, 2006. Written as Midway Granites p1063.|235 +/- 1.4 Ma U-Pb|||||
78373|Midway granite|69002|6|Mentioned|p10, Map 1b|Carnian|Ladinian|Comprises a small stock about 300m in diameter, within the Louth Eumarra shear zone. Presented as Midway Granite on Map 1b.|235 +/- 1.4 Ma, SHRIMP II (Burton et al. 2007)|||||22-SEP-13
40757|Mihi Rhyolite Member|50613|2|Defined|p209, p227 App. 1|Namurian|Namurian|Of the Willuri Formation. Volcanic member of the Piney Range package (informal grouping of stratigraphically recognisable distinctive, mappable units). Age: 320+/-4.5Ma (SHRIMP). Max. thickness: 90m. Geol.Prov: New England Orogen. Type section included.||||||22-FEB-05
22326|Mila Granodiorite|22815|4|Described|p83|||||||||
22326|Mila Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Mila Suite.||||||
31609|Mila Suite|22815|6|Mentioned|p82|||||||||
31609|Mila Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31609|Mila Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
31609|Mila Suite|44093|5|Briefly described|p204 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
31714|Milandra Granite|23392|6|Mentioned|p22|||||||||
31714|Milandra Granite|24417|3|Fully described|p96|Emsian|Emsian|Of Eugowra Suite.  Previously included in the Eugowra Granite.  Age: 390+/-2.5Ma (SHRIMP U/Pb).||||||
31714|Milandra Granite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Leucocratic biotite magnetite granite.||||||05-JUL-04
31714|Milandra Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|Of the Eugowra Suite.||||||13-JUL-04
23790|Milbrodale Formation|40805|2|Defined|p139|Permian|Permian|Previously used as Fairford Claystone Tongue||||||
23790|Milbrodale Formation|41010|6|Mentioned|p13|||Mention Fig.2||||||
23790|Milbrodale Formation|42078|6|Mentioned|Table 1 P5|||||||||
23790|Milbrodale Formation|42648|6|Mentioned|p37|||||||||
23790|Milbrodale Formation|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Jerrys Plains Subgroup (Wittingham Coal Measures)..||||||25-AUG-04
23790|Milbrodale Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Jerrys Plain Subgroup (Wittingham Coal Measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
23790|Milbrodale Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. Averages less than 1 m thick. Occurs throughout the coalfield, usually associated with the base of the Woodlands Hill seam. Mis-spelt as Millbrodale Formation on p52.||Unit in Jerrys Plains Subgroup.||Overlies Mount Thorley Formation. Is overlain by Mount Ogilvie Formation.|A waxy white tuffaceous claystone to cherty siltstone.|
23790|Milbrodale Formation|69683|6|Mentioned|p411 Fig.2, p415-416 Fig.3|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.||||
38481|Milby Chert Member|61964|4|Described|p14 Fig. 4, p28|Chewtonian|Chewtonian|Of the Clements Formation (Wagga Group). Thin bedded dark to light grey chert or brown chert to siliceous mudstone; forms low outcrops. Includes an unnamed Orodovician chert member of Scott and Sherwin (2000). For palaeontology - see p258.||||||20-OCT-08
38481|Milby Chert Member|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Clements Formation (Wagga Group). Dark grey to black radiolarian- and conodont-bearing chert (Chewtonian).||||||10-APR-08
38481|Milby Chert Member|65469|5|Briefly described|p18|Early Ordovician|Early Ordovician|Lachlan Orogen.||Clements Formation||||
38481|Milby Chert Member|67322|5|Briefly described|p18; Fig.5|Dapingian||Named by Colquhoun, Hendrickx and Meakin (in Colquhoun et al. 2005). Contains late Bendigonian to early Castlemainian conodonts. Vertical stratigraphic relationships are obscure. Occurs in the Cargelligo region.||Of the Clements Formation|||A relatively poorly exposed and laterally impersistent chert which forms lenticular bodies that pass into sandstone, mudstone and shale of the turbiditic sequence.|22-FEB-18
38481|Milby Chert Member|68466|6|Mentioned|p65-66, 69|Early Ordovician|Early Ordovician|Albury-Bega Terrane.||Clements Formation.||||
38481|Milby Chert Member|68592|5|Briefly described|p307|||Central Lachlan Orogen.||Unit in Clements Formation.||Correlative of Mummel Chert Member (Abercrombie Formation).||
38481|Milby Chert Member|69668|6|Mentioned|p929 Fig.2, p931|Early Ordovician|Early Ordovician|Cargelligo area, Albury-Bega terrane. Contains late Bendigonian to early Castlemainian conodont Oepikodus evae.||Unit in Clements Formation.||||
38481|Milby Chert Member|73140|6|Mentioned|p495 Fig.1, Fig.3|Bendigonian|Bendigonian|Age based on conodonts.||Abercrombie Formation||||
34363|Mile Road beds|22736|4|Described|p611|Frasnian|Givetian|New unit at base of southern Hastings Block||||||
34363|Mile Road beds|22857|4|Described|p484 App.1 Tb.A1.6|Givetian|Givetian|Siltstone, arenite, limestone and conglomerate; contain corals. Geological Province: Tamworth Forearc Basin. See also p500 App.1 Tb.A1.7.||||||
34363|Mile Road beds|44093|5|Briefly described|p67 Fig 6.6|Devonian|Devonian|||||||
25236|Milk Shanty Formation|22857|4|Described|p452 App.1, Tb.A1.6|Devonian|Devonian|Of the Byron Range Group. Siltstone, sandstone and conglomerate. Max. thickness: 170m. Geological Province: Bogan Gate Terrace. ||||||
25236|Milk Shanty Formation|23522|5|Briefly described|p248 Fig 4|Early Devonian|Early Devonian|||||||
25236|Milk Shanty Formation|30790|6|Mentioned|p1|||Devonian. Member Byron Range Group. See Fig.1||||||
25236|Milk Shanty Formation|32583|6|Mentioned|p373|||||||||
25236|Milk Shanty Formation|33325|5|Briefly described|Table 4|||||||||
25236|Milk Shanty Formation|33327|5|Briefly described|p173|||See also Fig.2. Byron Ra. Gp.||||||
25236|Milk Shanty Formation|33732|5|Briefly described|p111|||||||||
25236|Milk Shanty Formation|34184|6|Mentioned|p5|||Devonian||||||
25236|Milk Shanty Formation|34403|4|Described|p145|||||||||
25236|Milk Shanty Formation|34405|6|Mentioned|Fig.3.15|||||||||
25236|Milk Shanty Formation|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
25236|Milk Shanty Formation|60086|5|Briefly described|Map legend|Late Devonian|Middle Devonian|Of the Byron Range Group. Conglomerate, sandstone, siltstone.||||||19-JUL-04
25236|Milk Shanty Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Ravine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26740|Mill Creek Siltstone|31806|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
26740|Mill Creek Siltstone|33476|4|Described|p102|||Mention Table and P99||||||
26740|Mill Creek Siltstone|33766|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
26740|Mill Creek Siltstone|34340|4|Described|p466|||||||||
26740|Mill Creek Siltstone|35264|6|Mentioned|p16|||||||||
26740|Mill Creek Siltstone|41631|6|Mentioned|p9|||||||||
26740|Mill Creek Siltstone|42248|6|Mentioned|Fig.2 P399|||||||||
26740|Mill Creek Siltstone|43383|14|Not recorded|p24|||||||||
26740|Mill Creek Siltstone|43468|14|Not recorded|Map Legend|Jurassic|Triassic|Provisional Edition||||||
26740|Mill Creek Siltstone|43881|14|Not recorded|p6-7,11,31-3,133|Jurassic|Triassic|Top formation of Bundamba Group||||||
26740|Mill Creek Siltstone|44450|5|Briefly described|p36|Late Triassic|Late Triassic|Of Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
26740|Mill Creek Siltstone|60995|5|Briefly described|p55 Fig. 6|||Of McElroy (1963, 1969) and Brunker and Chesnut (1976).  Of the former Marburg Formation. Term now abandoned and replaced by Raceview Formation. Overlay Laytons Range Conglomerate. ||||||
26740|Mill Creek Siltstone|60997|5|Briefly described|p140 Fig. 2|||Reploaced by Raceview Formation (and Ripley Road Sandstone?). ||||||
26740|Mill Creek Siltstone|69639|6|Mentioned|p106, p224|Late Triassic|Late Triassic|Clarence-Moreton Basin.||Bundamba Group||Overlies the Tallawudjah Leucomonzogranite.||
27195|Millambri Formation|13139|6|Mentioned|p10|||||||||
27195|Millambri Formation|22857|5|Briefly described|p127, p424 App.1 Tb.A1.5|Early Silurian|Early Silurian|Of the Cabonne Group. Immature volcaniclastic arenite and siltstone, conglomerate lenses. Disconformably overlain by Cudal Group. Max. thickness: 1250m. See also p127.||||||
27195|Millambri Formation|23214|1|Redefined|p59|Llandovery|Bolindian|Of Cabonne Group. Divided into informal "upper" and "lower" members. Age derived from fossil assemblages. Max. thickness 1250m.||||||03-FEB-05
27195|Millambri Formation|23245|5|Briefly described|p127||Llandovery|||||||
27195|Millambri Formation|24398|4|Described|p265|Bolindian|Bolindian|See also p259 Fig. 2. Geological Province: Lachlan Fold Belt.||||||17-JUL-08
27195|Millambri Formation|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
27195|Millambri Formation|32590|6|Mentioned|Fig.1|||||||||
27195|Millambri Formation|32671|6|Mentioned|Map legend|Silurian|Ordovician|Ordovician-Silurian||||||
27195|Millambri Formation|32821|6|Mentioned|p10|||||||||
27195|Millambri Formation|33006|6|Mentioned|Map legend|Early Silurian|Late Ordovician|Upper Ordovician to Lower Silurian||||||
27195|Millambri Formation|33116|6|Mentioned|Fig.6|||Ord. Correlation||||||
27195|Millambri Formation|33125|6|Mentioned|p15|||Correlation chart||||||
27195|Millambri Formation|33282|6|Mentioned|Map legend|Early Silurian|Late Ordovician|Upper Ordovician - Lower Silurian||||||
27195|Millambri Formation|33285|6|Mentioned|p20|||||||||
27195|Millambri Formation|34404|2|Defined|p82|Early Silurian|Late Ordovician|Upper Ordovician - Early Silurian||||||
27195|Millambri Formation|34405|5|Briefly described|p122|||||||||
27195|Millambri Formation|34406|6|Mentioned|p218|||||||||
27195|Millambri Formation|34498|6|Mentioned|p150|||See also P153. Upper Ordovician||||||
27195|Millambri Formation|35118|6|Mentioned|Fig.5|||||||||
27195|Millambri Formation|35244|6|Mentioned|p35|||||||||
27195|Millambri Formation|36534|6|Mentioned|p223|||||||||
27195|Millambri Formation|37727|4|Described|p73|||See also P29.||||||
27195|Millambri Formation|38219|6|Mentioned|Table 2|||||||||
27195|Millambri Formation|39331|6|Mentioned|p61|||||||||
27195|Millambri Formation|39655|6|Mentioned|Plate 1|||||||||
27195|Millambri Formation|39657|6|Mentioned|M30|||||||||
27195|Millambri Formation|39663|6|Mentioned|Table 1|||||||||
27195|Millambri Formation|40136|5|Briefly described|p31|||[Originally entered for NT. CEBMar95]||||||
27195|Millambri Formation|40328|3|Fully described|p114|||Also mentioned on P3||||||
27195|Millambri Formation|43384|14|Not recorded|Map Legend||Ordovician|||||||
27195|Millambri Formation|43385|14|Not recorded|p169||Late Ordovician|Ref.to Stevens 1957||||||
27195|Millambri Formation|43433|14|Not recorded|p192|||||||||
27195|Millambri Formation|43479|14|Not recorded|p79,95f,105,116|Llandoverian|Caradoc|||||||
27195|Millambri Formation|43494|6|Mentioned|p17|Early Silurian|Ordovician|Similar composition to that of the Kabadah Formation sandstones.||||||16-MAR-06
27195|Millambri Formation|43515|14|Not recorded|Map Legend|Early Silurian|Late Ordovician|(Provisional Edition)||||||
27195|Millambri Formation|43516|14|Not recorded|Map Legend|Early Silurian|Late Ordovician|||||||
27195|Millambri Formation|43548|14|Not recorded|p250|||Equivalent to Angullong Tuff||||||
27195|Millambri Formation|43640|5|Briefly described|Map Legend||Ordovician|||||||
27195|Millambri Formation|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Consists of  immature volcaniclastic sandstone and siltstone; conglomerate lenses.||||||17-JUL-08
27195|Millambri Formation|43782|5|Briefly described|Map Legend|Llandovery|Bolindian|of Cabonne Group.||||||
27195|Millambri Formation|60417|6|Mentioned|p155 Fig.2||Late Ordovician|||||||
27195|Millambri Formation|63278|5|Briefly described|p145 Fig. 1, p154|Ordovician|Ordovician|Underlain by Rockdale Formation. Geological Province: Lachlan Fold Belt. Consists of turbidites composed of volcaniclastic sandstone and conglomerate containing clasts of volcanics.||||||07-FEB-11
27195|Millambri Formation|63286|5|Briefly described|p294 Fig. 1, p308 Fig. 9|Llandovery|Bolindian|Consists of volcanic sandstone, siltstone and conglomerate. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
27195|Millambri Formation|63287|4|Described|p318 Fig. 3, p317 Fig. 2, p335|Bolindian|Bolindian|Of Cabonne Group. Conformably underlain by Malongulli Formation. Geological Province: Molong Volcanic Belt.  Consists of volcaniclastic conglomerate, basaltic andestie and siltstone.||||||07-FEB-11
27195|Millambri Formation|63290|6|Mentioned|p398|||||||||
27195|Millambri Formation|67322|5|Briefly described|p20 Fig.5, p24|Ordovician|Ordovician|Macquarie Arc. Modified by Ryall (1966), from the usage of Stevens (1957) to include only the upper turbiditic sand-dominated part of his original Millambri Formation. Youngest unit in the Belubula River Valley area, assigned a late Ordovician age (but lacking in palaeontological evidence).||Of the Cabonne Group.|||Composed of volcaniclastic sandstone and conglomerate containing clasts of andesitic volcanics.|22-FEB-18
27195|Millambri Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
27195|Millambri Formation|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3).||Cabonne Group||||
27195|Millambri Formation|70684|6|Mentioned|p3, p18, p33, p35 Fig.15||||||||Sandstone, siltstone.|
29520|Millamolong Porphyry|13139|5|Briefly described|p3 Fig. 2|||Geological Province: Lachlan Orogen.||||||12-APR-05
29520|Millamolong Porphyry|23214|2|Defined|p85|Late Ordovician|Late Ordovician|Intrudes the Weemalla Formation.||||||
29520|Millamolong Porphyry|23334|5|Briefly described|3 Fig.2|||||||||
29520|Millamolong Porphyry|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Feldspar porphyry.||||||17-JUL-08
29520|Millamolong Porphyry|43782|6|Mentioned|Map Legend|Eastonian|Eastonian|||||||
29520|Millamolong Porphyry|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
78647|Millendale Formation|69159|5|Briefly described|Map legend|Llandovery|Llandovery||||||Grey, cream, brown to buff, medium- to thickly-bedded medium-grained quartz-rich sandstone interbedded with grey to pink siltstone, grading to grey siltstone and mudstone with fine-grained quartzose sandstone laminae towards the top of the Formation.|17-FEB-14
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|||||||||
30036|Millie Group|22857|5|Briefly described|p520 App.1 Tb.A1.9||Permian|Includes Watermark and Porcupine Formations. ||||||
30036|Millie Group|23566|5|Briefly described|p116 Fig. 2|Late Permian|Late Permian|Includes the Watermark Formation and Porcupine Formation. Geological Province: Gunnedah Basin.||||||01-SEP-15
30036|Millie Group|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Encompasses Watermark and Porcupine Formations. Age Upper Stage 4 to Lower Stage 5c. Formal definition published in an article released immediately prior, however a summary of new nomenclature is provided in Appendix 1.||||||13-NOV-13
30036|Millie Group|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin.  Includes: Watermark Formation, Porcupine Formation.||||||
30036|Millie Group|68003|5|Briefly described|p38 Fig.3-j, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Correlative of Maitland Group (Hunter Coalfield); Shoalhaven Group (Western Coalfield); and Bickham, Borambil Creek and Toll Bar Formations (Werrie Basin).|||Includes Porcupine and Watermark Formations.|Overlies Bellata Group. Is overlain by Black Jack Group.||
30036|Millie Group|68004|5|Briefly described|p23 Table 1.|||Gunnedah Basin. Equivalent to the Maitland Group and the upper part of the Shoalhaven Group, Sydney Basin.|||Includes Porcupine and Watermark Formations.|Overlies Bellata Group. Is overlain by Black Jack Group.||
30036|Millie Group|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian marine sequences: conglomerate, quartzose sandstone, siltstone, calcareous mudstone and limestone.||||||
30036|Millie Group|70791|5|Briefly described|p276-277, p293 Fig.17|Guadalupian|Guadalupian|Gunnedah Basin. Marine.|||Porcupine, Watermark Formations.|||
30036|Millie Group|70878|5|Briefly described|p712, p715-718|Permian|Permian|NW Sydney Basin. 34.20m thick in Santos Brawboy 1 well.|||Porcupine, Watermark Formations.|Overlies Bellata Group. Is overlain by Black Jack Group.||
74041|Milligans Road Formation|66090|2|Defined|p1, p4, pp8-9, pp28-29.|Early Jurassic|Late Triassic|Defined in this study. Identified by the presence of airfall tuff beds. The tuffs are believed to be associated with felsic igneous rocks in the immediate vicinity, including the Werrikimbe Volcanics to the NW. Type section is the Bago Road - Milligans Road intersection to a quarry 200 m to the SW. Thickness from 12 to 27 m. Age: exposures occur in fault-bounded blocks and neither top or base is exposed, therefore unit boundaries cannot be determined.|||||A sequence of interbedded mudstone, carbonaceous mudstone and poor coaly bands, occasional granule to pebble conglomerate, tuffaceous sandstone and airfall tuff.|12-OCT-15
74041|Milligans Road Formation|73570|6|Mentioned|p914, p915 Fig.4, p916, p918, p919 Fig.6|Late Triassic|Late Triassic|Lorne Basin.||||||
30024|Millsville Formation|22529|5|Briefly described|6|Ludlow|Wenlock|||||||
30024|Millsville Formation|22590|6|Mentioned|Fig3 P754||Pridoli|Actually spelt Millsville Fm.||||||
30024|Millsville Formation|22857|4|Described|p476 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Tannabutta Group. Age: 417+/-3Ma, 412.6+/-4.3Ma (U/Pb SHRIMP). Max. thickness: 250m. Geological Province: Capertee Rise. ||||||
30024|Millsville Formation|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|of Tannabutta Group.||||||
30024|Millsville Formation|23170|2|Defined|p71|Ludlow|Silurian|= 'Millsville beds'. Tannabutta Group.||||||
30024|Millsville Formation|43188|4|Described|p205,Table 2 p201|Ludlovian|Wenlockian|Capertee High. Representative section location given.||||||
30024|Millsville Formation|44093|5|Briefly described|p211 App. 1|Ludlovian|Wenlockian|Geological Province: Lachlan Fold Belt.||||||
30024|Millsville Formation|66197|6|Mentioned|p633 Fig.4a||Late Silurian|Deep marine clastics. Overlies Willow Glen Formation; is overlain by Queens Pinch Group.||||||14-MAR-12
73514|Millthorpe Volcanics|63278|5|Briefly described|p147 Fig. 2b, p156|Late Ordovician|Late Ordovician|Geological Province: Molong Volcanic Belt, LFB. Crawford et al. (2007a), correlate the Byng Volcanics with a geochemically similar upper part of Blaney Volcanics and distinguish this new unit.||||||07-FEB-11
73514|Millthorpe Volcanics|63283|2|Defined|p203-204, p214 App. 2|Bolindian|Late Ordovician|Underlain by upper Blayney Volcanics in west of Browns Creek mine, and by Cowringa Limestone Member. Thickness; probably 900m. See also p214 App. 2.||||||10-SEP-15
73514|Millthorpe Volcanics|63284|6|Mentioned|p268|||||||||
73514|Millthorpe Volcanics|63286|6|Mentioned|p308 Fig. 9|Llandovery|Llandovery|Geological Province: Molong Volcanic Belt. Consists of shoshonitic lavas.||||||07-FEB-11
73514|Millthorpe Volcanics|63290|5|Briefly described|p396 Fig. 3|Bolindian|Bolindian|Underlain by Blayney Volcanics. Geological Province: Molong Volcanic Belt.||||||
73514|Millthorpe Volcanics|63293|6|Mentioned|p469 Fig. 2|Bolindian|Bolindian|Underlain by Blayney Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73514|Millthorpe Volcanics|67322|5|Briefly described|Fig.5; p25|Late Ordovician|Late Ordovician|Macquarie Arc. Crawford, Meffre et al. (2007) set up this unit for more evolved rocks which were previously included in the Byng Volcanics. Age is determined from p20 Fig.5 (Strat. column). Occurs in the Blayney region. ||||Overlies the Blayney Volcanics.|Evolved basaltic to basaltic andesitic lavas and volcaniclastic rocks.|22-FEB-18
73514|Millthorpe Volcanics|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3).||Cabonne Group||||
73514|Millthorpe Volcanics|70684|6|Mentioned|p75|Late Ordovician|Late Ordovician|Blayney district, Molong Volcanic Belt.||||||
73514|Millthorpe Volcanics|73154|5|Briefly described|p77 Fig.3|Bolindian|Bolindian|Macquarie Arc, Phase 4. Molong Volcanic Belt.||||Overlies upper Blayney Volcanics.|Intermediate-mafic lava.|
29555|Milmiland Granite|22519|5|Briefly described|p8|Early Devonian|Early Devonian|||||||
29555|Milmiland Granite|23053|4|Described|p22-3,70,78||Early Devonian|Max Age: 394 (+/-) 2 Ma.||||||
29555|Milmiland Granite|43277|5|Briefly described|Map Legend||Early Devonian|of Lachlan Fold Belt.||||||
29555|Milmiland Granite|71206|6|Mentioned|p373|||This unit is apparently known also as Mount Arthur Granite. Lachlan Fold Belt.|||||Aluminous A-type granite.|
33693|Milroy Granite|24417|3|Fully described|p99|Early Devonian|Early Devonian|Of Bogalong Suite.  Unit previously included in "Bogalong Granite" and also referred to as "Glenroy Granite" (Duggan et al, 1999).||||||
33693|Milroy Granite|60009|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Bogalong Suite.||||||13-JUL-04
34494|Milton Grove Formation|22799|6|Mentioned|p16|||||||||
34494|Milton Grove Formation|22893|2|Defined|p17-19 table3|||Age, thickness discussed but exact figures are not known. Age inferred as Late Devonian to Early Carboniferous.||||||
27678|Minchinbury Sandstone|22745|6|Mentioned|Fig14,p138|||Wianamatta Group, Sydney Basin.||||||
27678|Minchinbury Sandstone|22857|4|Described|p530 App.1 Tb.A1.9|Middle Triassic|Middle Triassic|Of the Wianamatta Group. Fine to medium-grained lithic sandstone. Max. thickness: <3m. Geological Province: Sydney Basin. ||||||
27678|Minchinbury Sandstone|22969|5|Briefly described|p 26|||||||||
27678|Minchinbury Sandstone|29361|6|Mentioned|p3|||On table.||||||
27678|Minchinbury Sandstone|30132|6|Mentioned|Table 1|||||||||
27678|Minchinbury Sandstone|30286|6|Mentioned|p1099|||Stratigraphy||||||
27678|Minchinbury Sandstone|31056|5|Briefly described|p3|||||||||
27678|Minchinbury Sandstone|31296|6|Mentioned|p29|||Refers Lovering||||||
27678|Minchinbury Sandstone|31725|6|Mentioned|p10|||On table||||||
27678|Minchinbury Sandstone|32187|6|Mentioned|p6|||||||||
27678|Minchinbury Sandstone|32801|6|Mentioned|Fig.10|||||||||
27678|Minchinbury Sandstone|34243|6|Mentioned|p423|||Plant microfossils||||||
27678|Minchinbury Sandstone|34274|6|Mentioned|p121|||Triassic. See also P120||||||
27678|Minchinbury Sandstone|34305|2|Defined|p418|Triassic|Triassic|||||||
27678|Minchinbury Sandstone|34306|5|Briefly described|p443|||||||||
27678|Minchinbury Sandstone|35098|6|Mentioned|Fig.3|||||||||
27678|Minchinbury Sandstone|35312|6|Mentioned|p3|||||||||
27678|Minchinbury Sandstone|35502|6|Mentioned|Fig.1|||Also on Table 1||||||
27678|Minchinbury Sandstone|35690|1|Redefined|p181|Middle Triassic|Middle Triassic|||||||
27678|Minchinbury Sandstone|36042|6|Mentioned|Fig.22|||||||||
27678|Minchinbury Sandstone|39287|6|Mentioned|p50|||See also Fig.2.18||||||
27678|Minchinbury Sandstone|39298|4|Described|p257|||See also PP264-265||||||
27678|Minchinbury Sandstone|39306|6|Mentioned|p390|||See also P428||||||
27678|Minchinbury Sandstone|39626|6|Mentioned|p276|||||||||
27678|Minchinbury Sandstone|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
27678|Minchinbury Sandstone|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
27678|Minchinbury Sandstone|40602|3|Fully described|p24|||||||||
27678|Minchinbury Sandstone|40625|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
27678|Minchinbury Sandstone|40629|6|Mentioned|p191|||||||||
27678|Minchinbury Sandstone|40653|6|Mentioned|p121|||||||||
27678|Minchinbury Sandstone|42737|5|Briefly described|map legend|Triassic||||||||
27678|Minchinbury Sandstone|42896|3|Fully described|p45, Table 2|||of Wianamatta Group||||||
27678|Minchinbury Sandstone|42925|3|Fully described|p24|||of Wianamatta Group||||||
27678|Minchinbury Sandstone|42926|4|Described|map legend||Middle Triassic|||||||
27678|Minchinbury Sandstone|43194|6|Mentioned|p131|Triassic|Triassic|Sydney Basin.||||||
27678|Minchinbury Sandstone|43317|4|Described|Table 1 p13|||See also Lexicon||||||
27678|Minchinbury Sandstone|43318|14|Not recorded|opp p6||Late Triassic|||||||
27678|Minchinbury Sandstone|43319|14|Not recorded|Map Legend|||||||||
27678|Minchinbury Sandstone|43320|14|Not recorded|Table 1 p13,14|||Part of Liverpool Subgroup||||||
27678|Minchinbury Sandstone|43344|14|Not recorded|p22,51,55,57,58||Triassic|||||||
27678|Minchinbury Sandstone|43365|14|Not recorded|p169-210||Triassic|||||||
27678|Minchinbury Sandstone|43383|14|Not recorded|p23|||Liverpool Sub-Group||||||
27678|Minchinbury Sandstone|43385|14|Not recorded|p182 Table|||Ref.to Lovering 1954 (Keuper-L.Triassic?)||||||
27678|Minchinbury Sandstone|43395|14|Not recorded|map||Triassic|||||||
27678|Minchinbury Sandstone|45090|6|Mentioned|p221|||Triassic||||||
27678|Minchinbury Sandstone|60281|6|Mentioned|p64|Triassic|Triassic|Sandy barrier island complex.||||||
27678|Minchinbury Sandstone|65195|5|Briefly described|p4, p4 Fig.2|Triassic|Triassic|Of Wianamatta Group. Quartz-lithic sandstone. Overlies Ashfield Shale. Disconformably overlain by Miocene basalts and Tertiary alluvial deposits.||||||
27678|Minchinbury Sandstone|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Wianamatta Group.||||
27678|Minchinbury Sandstone|67663|6|Mentioned|p521|Triassic|Triassic|||Of the Wianamatta Group||||
27678|Minchinbury Sandstone|70661|3|Fully described|p214-p217|Middle Triassic|Middle Triassic|Named for Minchinbury station. Generally thin unit with poor outcropping and little to no geomorphic expression. Type section mentioned. Generally around 4m thick, may be up to 10m thick in places. Distribution, structure, geochemistry, fossil assemblage and distinguishing characteristics discussed. Deposited in a beach or offshore marine depositional environment.||Wianamatta Group||Conformably overlies Ashfield Shale. Conformably overlain by by Bringelly Shale.|Lithic quartz sandstone. Lithic grains are mostly quartzose but minor argillaceous and intermediate volcanic fragments do occur. The sandstone is generally well bedded with low angle cross bedding present.|
27678|Minchinbury Sandstone|71303|5|Briefly described|map legend|Middle Triassic|Middle Triassic|Of Sydney Basin.||Of Wianamatta Group.|||Thin sequence of buff to mid-brown, lithic-quartz sandstone; blue-grey when fresh. Sequence thicker locally, comprising sandstone interbedded with siltstone and minor claystone. Cross bedding; generally low angle.|
27678|Minchinbury Sandstone|73248|6|Mentioned|p301|Middle Triassic|Middle Triassic|||Wianamatta Group||||
27678|Minchinbury Sandstone|73304|6|Mentioned|p76|||||||||
27678|Minchinbury Sandstone|75059|6|Mentioned|p4, 9-10|Middle Triassic|Middle Triassic|Sydney Basin.||Wianamatta Group.||Overlies Ashfield Shale. Is overlain by Bringelly Shale.||
23795|Mingaletta Formation|22616|6|Mentioned|Fig.1 p670||Carboniferous|||||||
23795|Mingaletta Formation|22736|2|Defined|p621-6,28,29|Permian|Visean|revised from Hamilton 1982.  Base of formation moved down to base of Forest Range Member, replacing upper section of Cooperabung Formation.||||||
23795|Mingaletta Formation|22857|4|Described|p512 App.1 Tb.A1.7|Namurian|Namurian|Of the Manning Group. Arenite, siltstone, conglomerate, vitric tuff, coal-bearing beds. ?Unconformably overlies Hyndmans Creek Formation. Max. thickness: >2000m. Geological Province: Tamworth Forearc Basin. See also p500 App.1 Tb.A1.8.||||||
23795|Mingaletta Formation|24124|5|Briefly described|p3|||||||||
23795|Mingaletta Formation|38803|2|Defined|p106|Middle Carboniferous|Middle Carboniferous|See also P105||||||
23795|Mingaletta Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Hastings Block.||||||16-DEC-04
23795|Mingaletta Formation|43755|6|Mentioned|Fig.1,p548||Carboniferous|||||||
23795|Mingaletta Formation|44093|5|Briefly described|p67 Fig 6.6|Carboniferous|Carboniferous|In the South Hastings Block. See also p232 Appendix 1. Geological Province: New England Fold Belt.||||||
23795|Mingaletta Formation|65940|6|Mentioned|p194|||Wauchope-Port Macquarie area, NSW.||||||
23795|Mingaletta Formation|66090|6|Mentioned|p4, p8, pp18-19 map.|Late Carboniferous|Late Carboniferous|Southern Hastings Block. Part of the floor of the Lorne Basin.||||||
23795|Mingaletta Formation|70939|5|Briefly described|p824, p826, p828-829|Carboniferous|Carboniferous|Southern Hastings Block.|326.3 +/- 3.9 Ma.|||||
23795|Mingaletta Formation|71628|5|Briefly described|p17: 78, 80, 84|||Hastings Block. Ungrouped.||||Is intruded by Lorne Forest, North Brother and Middle Brother Granodiorites.||
27687|Mingelo Volcanics|22831|6|Mentioned|p 26|||||||||
27687|Mingelo Volcanics|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
27687|Mingelo Volcanics|24265|5|Briefly described|p1450||Ordovician|Geological Province: Lachlan Fold Belt||||||
27687|Mingelo Volcanics|40891|4|Described|p9|||Mention Fig.3||||||
27687|Mingelo Volcanics|42489|5|Briefly described|Map legend|Bolindian|Eastonian|||||||
27687|Mingelo Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
27687|Mingelo Volcanics|46522|1|Redefined|p38|Late Ordovician|Late Ordovician|Up to 1000 m thick.||||Conformably overlain by Cotton Formation, Burrandong Creek Member.||07-SEP-18
27687|Mingelo Volcanics|46523|6|Mentioned|p85|||||||||
27687|Mingelo Volcanics|46524|4|Described|p103|||See also Appendix 1 p129.||||||07-SEP-18
27687|Mingelo Volcanics|46525|6|Mentioned|Fig.1 p143|||||||||07-SEP-18
27687|Mingelo Volcanics|46528|5|Briefly described|Map legend|Late Ordovician||||||||
27687|Mingelo Volcanics|63278|6|Mentioned|p145 Fig. 1, p151|||Geological Province: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
27687|Mingelo Volcanics|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
27687|Mingelo Volcanics|63283|5|Briefly described|p189-190|Gisbornian|Darriwilian|Age: 463-455Ma (suggested). Geological Province: Junee-Narromine Volcanic Belt. Consists of basaltic andesite lavas, ranging from vesicular and formerly glassy, to massive, with plagioclase, augite and rare altered olivine phenocrysts. Strong compositional affinities with the Goonumbla Volcanics basal mafic unit basaltic andesites and with the upper unit of the Fairbridge Volcanics in the Molong Volcanic Belt.|||||Consists of basaltic andesite lavas, ranging from vesicular and formerly glassy, to massive, with plagioclase, augite and rare altered olivine phenocrysts. Dominantly a high-K calc alkaline to shoshonitic suite.|07-SEP-18
27687|Mingelo Volcanics|67107|6|Mentioned|p696, 701|Ordovician|Ordovician|Sherwin (1996). A fault-controlled elongated (3.3km x 600m) N-S striking alteration zone; hosts the Peak Hill Au-Cu deposits in a high-sulfidation epithermal deposit. Interpreted to belong to the Goonumbla Volcanics.||Goonumbla Volcanics.||||
27687|Mingelo Volcanics|67805|5|Briefly described|p73|Ordovician|Ordovician|Thin, N-S trending slice of andesitic volcanics. Host to gold ore at Peak Hill. Chemically and petrographically similar to early Goonumbla Volcanics.||||||
27687|Mingelo Volcanics|67821|5|Briefly described|p150, p173, p177|Early Silurian|Late Ordovician|Host to Peak Hill and Wyoming gold deposits. Equated with the Goonumbla Volcanics. Strongly deformed and hydrothermally altered (described in some detail).||||||08-FEB-18
27687|Mingelo Volcanics|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
27687|Mingelo Volcanics|72495|6|Mentioned|p218, 225, p234|Ordovician|Ordovician|Occurs to the east of the Parkes Thrust. Age inferred from geochemical similarity to the Northparkes Volcanic Group. Interpreted to be cut by west-northwest trending faults which appear as demagnetisation zones in aeromagnetics data.||||||
27687|Mingelo Volcanics|73492|6|Mentioned|p691, p707|||Temporal correlative with Goonumbla Volcanics based on Katian age of calcareous interbeds in volcanics from drill hole WNDD0001 correlated with the Mingelo Volcanics.||||||
24381|Minnalong Sandstone|40365|2|Defined|p327|Early Cretaceous|Late Jurassic|Late Jurassic to earliest Cretaceous||||||
79636|Minoru Plains Volcanics|70821|6|Mentioned|p12|||Not encountered in outcrop or boreholes in this study. Characterised by linear trends of moderate to high magnetic intensity.||||||
79636|Minoru Plains Volcanics|71251|6|Mentioned|p3|||N and S of Cunnamulla. Map symbol ( Emp) implies Cambrian age suspected or inferred.||||||26-APR-18
79636|Minoru Plains Volcanics|71864|6|Mentioned|p3|||||||||
28758|Minyon Falls Rhyolite Member|34340|6|Mentioned|Table 6.1|||||||||
28758|Minyon Falls Rhyolite Member|43881|2|Defined|p6-7,49,56||Tertiary|Top member of Nimbin Rhyolite (Minyon Falls area)||||||
82574|Mirani Monzogranite|71628|5|Briefly described|p3: 1, 4, 75-76|||New name: formalising the ""Mirani monzogranite"" of Brown (2003). Named after Mirani homestead. Occurs ~30 km S of Armidale and ~20 km SSE of Uralla. No geochemistry available; very low magnetic susceptibility, and moderate to strong radiometric response.||Mirani Suite.||Intrudes Sandon Association.|Medium- to coarse-grained, equigranular to locally porphyritic, biotite monzogranite; weakly to strongly foliated. S-type.|
26743|Mirrabooka Formation|13996|5|Briefly described|p143-145|Silurian|Silurian|Contains a diverse Wenlock-aged trilobite fauna in its lower parts, and a rich Ludlow fauna in the upper part. Biogeographic implications.||||Overlies Boree Creek Formation. Equivalent to Borenore and Molong Limestones.||
26743|Mirrabooka Formation|22520|6|Mentioned|p17|||||||||
26743|Mirrabooka Formation|22857|5|Briefly described|p468 App.1 Tb.A1.6|Silurian|Silurian|Of the Mumbil Group. Fine quartzose arenite, minor cherty or sandy layers. Max. thickness: 500m. ||||||
26743|Mirrabooka Formation|23214|3|Fully described|p128|Ludlow|Wenlock|Of Mumbil Group. Previously included in Molong Beds, Panuara Formation and Panuara Group. 500m thick at type section.||||||
26743|Mirrabooka Formation|24249|5|Briefly described|p87, p90 Fig.3|Ludlow|Ludlow|Overlain by Wallace Shale, in Cheeseman's Creek district.||||||15-FEB-07
26743|Mirrabooka Formation|29791|6|Mentioned|p89|||||||||
26743|Mirrabooka Formation|30073|6|Mentioned|p54|||||||||
26743|Mirrabooka Formation|32624|6|Mentioned|p718|||Coral species||||||
26743|Mirrabooka Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
26743|Mirrabooka Formation|32672|6|Mentioned|p672|||||||||
26743|Mirrabooka Formation|33116|4|Described|p212|||Sil. See also pp213-215.||||||15-FEB-07
26743|Mirrabooka Formation|33121|6|Mentioned|p85|||Late Sil. Correlation table||||||
26743|Mirrabooka Formation|33285|6|Mentioned|p18|||Mid.-Late Sil.||||||
26743|Mirrabooka Formation|33611|6|Mentioned|p132|||||||||
26743|Mirrabooka Formation|37727|3|Fully described|p79|||||||||
26743|Mirrabooka Formation|38368|6|Mentioned|p314|||||||||
26743|Mirrabooka Formation|39214|5|Briefly described|p19|||||||||
26743|Mirrabooka Formation|39331|5|Briefly described|p68|||M-U Silurian. See also p61.||||||15-FEB-07
26743|Mirrabooka Formation|40328|3|Fully described|p147|||||||||
26743|Mirrabooka Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
26743|Mirrabooka Formation|43782|5|Briefly described|Map Legend|Ludlow|Wenlock|Of Mumbil Group.||||||15-FEB-07
26743|Mirrabooka Formation|48971|6|Mentioned|p31|||See also p32, p33, p34, p40.||||||15-FEB-07
26743|Mirrabooka Formation|61894|5|Briefly described|p180 |||Orange district.|||||Contains fossiliferous limestone lenses.|
26743|Mirrabooka Formation|63083|6|Mentioned|p218|Ludlow|Wenlock|In the Orange-Molong district. Lateral equivalent to Borenore/Molong Limestones.||||||07-FEB-11
26743|Mirrabooka Formation|63287|6|Mentioned|p317 Fig. 2, p321 Fig. 4, p335|Pridoli|Wenlock|Of Mumbil Group. Undelain by Quarry Creek Limestone and Boree Creek Formation. Geological Province: Molong Volcanic Belt. Consists of fine grained quartz sandstone and shale with limestone nera the top.||||||07-FEB-11
26743|Mirrabooka Formation|64826|5|Briefly described|p1040 Tb. 1|Ludlow|Wenlock|Of the Mumbil Group.||||||10-FEB-09
26743|Mirrabooka Formation|64994|5|Briefly described|p7|Wenlock|Wenlock|Of Percival (2001). Includes shales containing graptolites.||||||07-FEB-11
26743|Mirrabooka Formation|67651|5|Briefly described|p413-416,423-424,430,432,435-436,439|Ludlow|Wenlock|Broadly contemporaneous to Borenore and Molong limestones. Conodonts in limestone beds (tentatively correlated to Limestone I of Sherwin 1971) nearby Bunyarra homestead (Locality PL1988) indicates early Wenlock (Pterospathodus amorphognathoides biozone); graptolites in siltstone at a similar stratigraphic level assigned Ludlow age (Lobograptus scanicus-Saetograptus leintwardinensis biozones). Combined with sharp, nongradational boundaries between the limestone and siltstone, the limestones are likely autochthonous. See also p442,445,450,453-454,456,459,462,464,468,470,472,475-476,478,480,482,485.||||Laterally grades into Molong or Borenore limestones. Overlain by Wallace Shale. Underlain unconformably by Boree Creek Formation.||
26743|Mirrabooka Formation|68297|5|Briefly described|p179|Ludlow|Wenlock|NSW. Includes bone fragments, probably Acanthodian, in limestone (Turner & Pickett 1982).||||||
26743|Mirrabooka Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
26743|Mirrabooka Formation|73299|6|Mentioned|p1104 Fig.10|Late Silurian|Early Silurian|Molong High.||||Overlies the Oakdale Formation, underlies the Wallace Shale.||
77260|Mirrie Formation|68004|5|Briefly described|p44 Table 3, p45.|Early Permian|Early Permian|New name. Gilgandra Sub-basin, Gunnedah Basin. 7 m thick.||||Overlies Goondi Formation. Is overlain by Maules Creek Formation.|Pebble conglomerate in a black carbonaceous claystone matrix; clasts from basement metasediments and matrix is from organic-rich swamp or lake sediments.|
29688|Mishurley Creek Granite|22638|4|Described|p44|Early Silurian||Previously "Billabong Creek Pluton"||||||
29688|Mishurley Creek Granite|44192|5|Briefly described|Map Legend|Wenlockian|Llandoverian|||||||
29688|Mishurley Creek Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
29688|Mishurley Creek Granite|50191|6|Mentioned|p21 Fig. 1|Silurian|Silurian|||||||
29688|Mishurley Creek Granite|69801|6|Mentioned|p2, p138|Devonian|Silurian|Eastern Lachlan Orogen. Indistinguishable in age to the Yammatree Granite.|419.3 +/- 2.2 Ma (SHRIMP)|||Intrudes the Frampton Volcanics.||
29688|Mishurley Creek Granite|73215|5|Briefly described|p994|||Tumut Trough.|419 +/- 2 Ma (Black, 2007).|||||
34936|Mitchell Cave beds|22952|6|Mentioned|Table1p179||Pleistocene|||||||
33382|Mitchell Formation|13139|6|Mentioned|p10|||||||||
33382|Mitchell Formation|22857|4|Described|p426 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Latitic conglomerate, sandstone, siltstone; minor latite. Max. thickness: >1000m. ||||||
33382|Mitchell Formation|23043|5|Briefly described|Map Legend|Bendigonian|Warendan|||||||
33382|Mitchell Formation|23170|2|Defined|p23 Fig.3, p6|Lancefieldian|Early Ordovician|Submarine massive flows. Lachlan Fold Belt.||||||09-MAY-13
33382|Mitchell Formation|23213|2|Defined|p10, Fig.10|Lancefieldian||formerly 'Mitchell Grit' and 'Mitchell Breccia'. Oldest rocks in the Molong Volcanic Belt. Only recognised in Bakers Swamp area so far. of Northern Molong Volcanic Belt.||||||
33382|Mitchell Formation|23739|5|Briefly described|p213 Fig. 1|Early Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt.||||||
33382|Mitchell Formation|24398|5|Briefly described|p261|Lancefieldian|Lancefieldian|See also p259 Fig. 2.  Volcaniclastic conglomerate and sandstone with minor flows and intrusions.  Overlain conformably by Hensleigh Siltstone.  Geological Province: Lachlan Fold Belt.||||||
33382|Mitchell Formation|50097|4|Described|p41|Early Ordovician||Min Thickness: 1100  m. Conglomerate with mainly latite clasts interpreted as a downslope mass flow from a volcanic centre, with interbedded sandstone turbidites. Conformably overlain by Hensleigh Silstone. Geol Prov: Lachlan Orogen. NSW||||||07-FEB-11
33382|Mitchell Formation|63121|5|Briefly described|p225 Fig. 2|Bendigonian|Late Cambrian|Max. age is early Bendigonian. In Bakers Swamp area, south of Wellington, NSW.||||||13-MAR-07
33382|Mitchell Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p151|Early Ordovician|Early Ordovician|Overlain conformably and transitionally by Hensleigh Siltstone. Geological Province: Monlong Volcanic Belt, Lachlan Fold Belt. Consists of mainly volcaniclastics with minor lavas. Carbonate clasts occur sporadically in uppermost part.||||||07-FEB-11
33382|Mitchell Formation|63279|4|Described|p171 Fig. 4, p174-176|Ordovician|Ordovician|Overlain conformably by Hensleigh Siltstone. Thickness: 1100m +. Geological Province: Molong Volcanic Belt. Consists of volcaniclastic rocks and minor lavas. Age range around ca 500Ma. See also p174-176.||||||
33382|Mitchell Formation|63283|6|Mentioned|p191 Tb. 2|Early Ordovician|Early Ordovician|Age: 485Ma (andesite clast).||||||07-FEB-11
33382|Mitchell Formation|63286|6|Mentioned|p310-311|Early Odrovician|Early Ordovician|Geological Province: Molong Volcanic Belt. Consists of high-K calc-alkaline lavas.||||||07-FEB-11
33382|Mitchell Formation|63287|6|Mentioned|p317 Fig. 2|Early Ordovician|Early Ordovician|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
33382|Mitchell Formation|63293|5|Briefly described|p467, p468 Fig. 2|Early Ordovician|Early Ordovician|Overlain by Hensleigh Siltstone. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
33382|Mitchell Formation|65756|5|Briefly described|p27|Early Ordovician|Early Ordovician|||||||
33382|Mitchell Formation|67106|5|Briefly described|p672-676, 678-679, 681-683|Early Ordovician|Early Ordovician|Molong Volcanic Belt, Lachlan Orogen. Zircon analyses detailed.||||Is overlain transitionally by Hensleigh Siltstone.|Debris flow detritus and rare pillow basalts.|
33382|Mitchell Formation|67107|6|Mentioned|p687, 701-702|||Parkes district, Junee-Narromine Volcanic Belt. The oldest identified unit in the Macquarie Arc above basement. May be analogous to Mount Read Volcanics in TAS.||||||
33382|Mitchell Formation|67322|5|Briefly described|Fig.5; p23|Floian|Tremadocian|Macquarie Arc. Defined by Morgan and Scott, in Meakin and Morgan (1999). Conodont fauna at the boundary and in the lower part of the overlying Hensleigh Formation are mid to late Bendigonian in age. Bakers Swamp area.||||Conformably overlain by the Hensleigh Siltstone.|Volcaniclastic.|22-FEB-18
33382|Mitchell Formation|68592|5|Briefly described|p370|Early Ordovician|Early Ordovician|South of Wellington. Is not included in the much younger Cabonne Group.||||Is overlain conformably by Hemsleigh Siltstone.||
33382|Mitchell Formation|70684|5|Briefly described|p3, p12, p18-21, p74|Early Ordovician|Early Ordovician|Northern Molong Volcanic Belt. Possibly over 1100m thick. Subaqueous debris-flow deposits: proximal apron deposits on the flanks of a seamount. Late Lancefieldian to earliest Bendigonian.||||Is overlain conformably by Hensleigh Siltstone.|Bedded volcaniclastic sandstone, shales and massive to poorly bedded conglomerate to angular sedimentary breccias and minor lavas; rare limestones at the top of the unit.|
33382|Mitchell Formation|72263|4|Described|p513,515-526|Early Ordovician|Early Ordovician|Geological province: Lachlan Orogen. Crops out in the Molong Volcanic Belt. Considered oldest unit in the Macquarie Arc. Also see 1:250 000 DUBBO and BATHURST maps (Morgan et al., 1999; Raymond et al., 1998). Minimum thickness of 1100m. Basal contact is a juxtaposition against Neurera Fault and Silurian-Devonian volcanic and sedimentary rocks. Age constraint provided by Sponge Archaeoscyphia and graptolites from carbonate breccias in uppermost Mitchell Formation and overlying Hensleigh Formation (~482-476 Ma; (Percival et al., 1999; Percival and Glen, 2007). Weighted mean Pb/Pb age of 479.8+\-3.8 Ma from a volcaniclastic sample reflect age of volcanic component (regarded as lowest stratigraphic part of the Macquarie Arc). Rock samples were possibly contaminated in laboratory and yielded anomalous Silurian zircon ages. U-Pb-Hf isotopic analysis indicates that initiation of Macquarie Arc within an intra-oceanic setting, outboard of the Gondwana margin.|482-476 Ma|||Overlain conformably by Hensleigh Formation. Fault contact with Oakdale Formation.|Coarse-grained volcaniclastic rocks (including breccias and conglomerates) and fine-grained volcaniclastic sandstone (with thinly bedded layers).|
33382|Mitchell Formation|73059|6|Mentioned|p1064|Early Ordovician|Early Ordovician|Near the base of the Macquarie Arc succession. See also reference to Mitchell Breccia (p1054).||||||
33382|Mitchell Formation|73154|6|Mentioned|p93|||Abundance of detrital zircons, interpreted as volcaniclastic apron of an emergent high-K calc-alkaline volcano (Glen et al., 2007a)||||||
33382|Mitchell Formation|73264|6|Mentioned|p1391 Fig.13|Middle Ordovician|Early Ordovician|Lachlan Orogen, Macquarie Volcanic Province, phase 1.||||||
33382|Mitchell Formation|73299|6|Mentioned|p1105|Ordovician|Ordovician|Macquarie Arc.||||||
25246|Mitchie Well Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Cryogenian|||||||
25246|Mitchie Well Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Eurowie Subgroup (Torrowangee Group). Lenticular grey limestone interbedded with laminated calcareous siltstone. Age: <700Ma. Max. thickness: 2130m. Geological Province: Adelaide Fold Belt. See also p400 App. 1 Tb.A1.3.||||||
25246|Mitchie Well Formation|30261|4|Described|Table 1|||Sturtian-Marinoan age||||||
25246|Mitchie Well Formation|34812|3|Fully described|p79|||||||||
25246|Mitchie Well Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25246|Mitchie Well Formation|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
25246|Mitchie Well Formation|36733|6|Mentioned|Table 5|||||||||
25246|Mitchie Well Formation|37931|4|Described|p534|||||||||
25246|Mitchie Well Formation|39214|5|Briefly described|p7|||||||||
25246|Mitchie Well Formation|41405|5|Briefly described|p204|||||||||
25246|Mitchie Well Formation|46889|6|Mentioned|p272|||||||||
25246|Mitchie Well Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Euriowie Subgroup.||||
25246|Mitchie Well Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Euriowie Subgroup.||Is overlain by Floods Creek Formation.|Fine-grained sandstone and siltstone with regularly-spaced, fine-grained, discontinuous, marly, gritty limestone beds and pods. A separately mapped un-named subunit also contains minor diamictite clasts.|08-SEP-15
27489|Mittagong Formation|22745|6|Mentioned|p136|||Sydney Basin. 20 m.||||||
27489|Mittagong Formation|22857|4|Described|p530 App.1 Tb.A1.9|Middle Triassic|Middle Triassic|Interbedded shale, laminite and medium-grained quartz sandstone. Max. thickness: 10m. Geological Province: Sydney Basin.||||||
27489|Mittagong Formation|22969|6|Mentioned|p 26|||||||||
27489|Mittagong Formation|24117|5|Briefly described|p3|||Geological Basin: Sydney Basin.||||||
27489|Mittagong Formation|29361|6|Mentioned|p4|||||||||
27489|Mittagong Formation|29901|4|Described|Table 1|||||||||
27489|Mittagong Formation|30132|6|Mentioned|Table 1|||||||||
27489|Mittagong Formation|30286|6|Mentioned|p1099|||Stratigraphy||||||
27489|Mittagong Formation|31128|6|Mentioned|p7|||||||||
27489|Mittagong Formation|31296|6|Mentioned|p42|||Refers Branagan (1969)||||||
27489|Mittagong Formation|31887|5|Briefly described|p9|||||||||
27489|Mittagong Formation|32187|6|Mentioned|p6|||||||||
27489|Mittagong Formation|34033|6|Mentioned|p61|||||||||
27489|Mittagong Formation|34205|6|Mentioned|p34|||||||||
27489|Mittagong Formation|34209|6|Mentioned|Table 1|||Triassic. See P148.||||||
27489|Mittagong Formation|34305|6|Mentioned|Table 5.26|||||||||
27489|Mittagong Formation|35690|6|Mentioned|p19|||||||||
27489|Mittagong Formation|36042|6|Mentioned|Fig.27|||||||||
27489|Mittagong Formation|36220|6|Mentioned|p91|||||||||
27489|Mittagong Formation|39287|6|Mentioned|p50|||||||||
27489|Mittagong Formation|39293|5|Briefly described|p160|||||||||
27489|Mittagong Formation|39298|4|Described|p259|||||||||
27489|Mittagong Formation|39306|6|Mentioned|p425|||See also P426||||||
27489|Mittagong Formation|40602|3|Fully described|p20|||||||||
27489|Mittagong Formation|40603|6|Mentioned|p4|||||||||
27489|Mittagong Formation|40625|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
27489|Mittagong Formation|40629|6|Mentioned|p184|||||||||
27489|Mittagong Formation|40651|6|Mentioned|Table 6|||||||||
27489|Mittagong Formation|40653|6|Mentioned|p121|||||||||
27489|Mittagong Formation|40654|6|Mentioned|p116|||||||||
27489|Mittagong Formation|41299|6|Mentioned|p118|||||||||
27489|Mittagong Formation|41939|5|Briefly described|p23|||||||||
27489|Mittagong Formation|42737|5|Briefly described|map legend|Triassic||||||||
27489|Mittagong Formation|42896|3|Fully described|p38, Table 2|||||||||
27489|Mittagong Formation|42925|3|Fully described|p16|||see also Table 1||||||
27489|Mittagong Formation|42926|4|Described|map legend||Middle Triassic|||||||
27489|Mittagong Formation|43320|14|Not recorded|Table 1 p13|||Part of Liverpool Subgroup||||||
27489|Mittagong Formation|43383|14|Not recorded|p23|||Liverpool Sub-Group||||||
27489|Mittagong Formation|45090|6|Mentioned|p72|||Palynological zones||||||
27489|Mittagong Formation|60281|6|Mentioned|p63|||Max. thickness: 15m.||||||
27489|Mittagong Formation|60726|5|Briefly described|p3.|||Up to 15m thick.||||Overlies the Hawkesbury Sandstone, underlies the Ashfield Shale.||
27489|Mittagong Formation|61315|5|Briefly described|Table SY2|Middle Triassic|Middle Triassic|Geological Province: Sydney Basin||||||
27489|Mittagong Formation|65195|6|Mentioned|p7, p4 Fig.2|Triassic|Triassic|||||||
27489|Mittagong Formation|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Hawkesbury Sandstone.||||
27489|Mittagong Formation|67850|5|Briefly described|p51 Table 1, p54 Fig.5. |||Exposed in the Spring Creek Monocline.||||||
27489|Mittagong Formation|70587|5|Briefly described|Map Legend|Triassic|Triassic ||||||Interbedded Shale, laminite and medium-grained quartz sandstone.|
27489|Mittagong Formation|70661|3|Fully described|p202-p206, p213|Middle Triassic|Early Triassic|Name likely derived from town of Mittagong. Some rocks from this formation incorporated into the Wianamatta Series, also previously referred to as the Passage Beds. Generally poorly outcropping. Type section mentioned. Up to 15m thick. Fossil assemblage, distinguishing characteristics and structure discussed.||||Conformably overlies Hawkesbury Sandstone, Disconformably? overlain by Ashfield Shale|Fine to medium grained quartzose, cross laminated and sometimes cross bedded sandstone. Sandstone is interbedded with finely laminated siltstone and fine sandstone.|
27489|Mittagong Formation|71303|5|Briefly described|map legend|Middle Triassic|Middle Triassic|Of Sydney Basin.|||||Quartzose, off-white, fine to medium-grained sandstone; pebbly locally. Cross-bedded locally.Lesser grey, micaceous siltstone.|
27489|Mittagong Formation|73248|6|Mentioned|p301, p309|Middle Triassic|Middle Triassic|||||Underlain by Hawkesbury Sandstone.|Shale and sandstone.|
27489|Mittagong Formation|75059|6|Mentioned|p4|Triassic|Triassic|Sydney Basin.||||Overlies Hawkesbury Sandstone.|Shales and sandstones.|
28760|Mittagong Syenites|40811|6|Mentioned|p323|||The syenites at Mittagong. Informal name.||||||
26745|Mogendoura Granodiorite|35248|6|Mentioned|Fig.1|||||||||
26745|Mogendoura Granodiorite|36600|6|Mentioned|p102|||||||||
26745|Mogendoura Granodiorite|42497|5|Briefly described|Map Legend|Eifelian|Pragian|||||||
82577|Moggs Swamp Complex|71628|3|Fully described|p19: 12, 17, 105-108|||New (not previously published) name, after Hensel (1982) and Stolz (1976), both unpublished. Potentially named after a local feature. Crops out as two small bodies ~40 km SE of Guyra. Type locality proposed by Stolz (1976, unpublished) is GR 510282, Grafton 1;250,000 sheet). Lithologies and mineralogy described in detail. Geochemistry described. Hosts minor stockwork Au mineralisation.||Moggs Swamp Suite.||Intrudes Oban River Leucomonzogranite.|Medium-grained, locally porphyritic, biotite-hornblende-clinopyroxene-(orthopyroxene) quartz diorite - quartz-poor tonalite to quartz-poor granodiorite - quartz monzodiorite enclosing quartzo-feldspathic veins and pegmatite.|
23803|Mograni Limestone Member|36057|2|Defined|p344|Tournaisian|Tournaisian|Prob. Tournaisian||||||
23803|Mograni Limestone Member|36528|6|Mentioned|p175|||||||||
23803|Mograni Limestone Member|38215|6|Mentioned|Fig.2|||||||||
23803|Mograni Limestone Member|39660|6|Mentioned|p450|||||||||
23803|Mograni Limestone Member|42547|4|Described|p34|||||||||
23803|Mograni Limestone Member|44244|4|Described|p198-199|Tournaisian|Tournaisian|Of the Wallanbah Formation.  Max. thickness: 75m.  Type section in text.  Geological Province: Myall Block.||||||25-AUG-04
78891|Moira Formation|69635|4|Described|p156-163, p69, 139|Late Devonian|Middle Devonian|Southern Thomson Orogen. U-Pb SHRIMP zircon maximum depositional age.|414+/-7 Ma|Of Mulga Downs Group||Unconformably overlies Booda Formation. Transitionally overlain by Mount Oxley Formation.|Includes both fine-grained red sandstone, and feldspathic coarse-grained sandstone to granule conglomerate.|
78891|Moira Formation|70602|6|Mentioned|p66, Fig 2|Devonian|Devonian|||Mulga Downs Group||||
78891|Moira Formation|72522|5|Briefly described|p18.|Late Devonian|Middle Devonian|||Mulga Downs Group||Unconformably overlies Booda Formation in Oxley Range.|Includes relatively flat-lying conglomerates and sandstones.|
34521|Molineaux-Lowan Sands|10010|5|Briefly described|p14 Fig. 5f, p16|||Geological Province: Murray Basin. Includes surficial deposits such as mobile sand sheets, source-bordering dunes and lunettes.||||||13-AUG-07
34521|Molineaux-Lowan Sands|22799|3|Fully described|p46|Holocene|Late Pleistocene|||||||
34521|Molineaux-Lowan Sands|65552|5|Briefly described|p5 Fig. 3, p6|Quaternary|Quaternary|Forms part of a series of aeolian-fluvio-lacustrine units that overlie Bungunnia Limestone and Blanchetown Clay in the uppermost Murray Basin.||||||
34521|Molineaux-Lowan Sands|73118|6|Mentioned|p37|||Glenelg Zone, Western Victoria. Drill core summary log.||||Overlies Loxton-Parilla Sands.||
26036|Monash Formation|22495|6|Mentioned|P220|||||||||
26036|Monash Formation|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|Consists of: Coombool Member, Merreti Member and Pyap Member.||||||
26036|Monash Formation|22799|2|Defined|p18|Albian|Aptian|||||||
26036|Monash Formation|22857|5|Briefly described|p318, p548 App.1 Tb.A1.12|||Max. thickness: 279m in type area in SA. Geological Province: Berri Basin. See also p350 Fig.24.5.||||||
26036|Monash Formation|22865|6|Mentioned|p318|||(Thornton 1972).||||||
26036|Monash Formation|22887|4|Described|p30, Table 5 p31|Early Cretaceous|Early Cretaceous|See also Fig.5 p12. Renmark Trough.||||||
26036|Monash Formation|22893|6|Mentioned|table5 fig4||Early Cretaceous|||||||
26036|Monash Formation|23836|4|Described|p93|Cretaceous|Cretaceous|Geological Province: Murray Basin.||||||
26036|Monash Formation|24551|5|Briefly described|p270|||Geological Province: Murray Basin.||||||
26036|Monash Formation|33488|2|Defined|p8|Early Cretaceous|Early Cretaceous|See also PP9-11||||||
26036|Monash Formation|33490|4|Described|p10|||Cretaceous. See also P23||||||
26036|Monash Formation|35200|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
26036|Monash Formation|35232|6|Mentioned|Table.2|||||||||
26036|Monash Formation|39211|6|Mentioned|Fig.23|||||||||
26036|Monash Formation|42133|6|Mentioned|Fig.7 P315|||||||||
26036|Monash Formation|42966|2|Defined|p71|Albian|Aptian|||||||
26036|Monash Formation|43052|5|Briefly described|Table 2.1|||||||||
26036|Monash Formation|43218|4|Described|Fig.3,p22|Albian|Aptian|||||||
26036|Monash Formation|44133|5|Briefly described|p94, 127|Cretaceous|Cretaceous|Geological Province: Berri Basin. Unconformably overlies Urana Formation. Unconformably overlain by Renmark Group. ||||||
26036|Monash Formation|44191|5|Briefly described|Map Legend||Early Cretaceous|||||||
26036|Monash Formation|49038|5|Briefly described|p23|||||||||
26036|Monash Formation|49040|6|Mentioned|p8|||||||||
26036|Monash Formation|61314|5|Briefly described|p129|Early Cretaceous|Early Cretaceous|Comprises three sequences of strata: the Pyap, Merreti and Coombool Members. Geological Province: western Murray Basin.||||||
26036|Monash Formation|68189|6|Mentioned|p25|||Of the Murray Basin.|||Includes the Coombool Member.|||
26036|Monash Formation|68715|6|Mentioned|p31 Fig.5|Albian|Aptian|Berri Basin.||||||
26036|Monash Formation|73228|6|Mentioned|p50-54|Early Cretaceous|Early Cretaceous|Berri Basin. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1, and Overland Corner 1 drillholes. Type section is subsurface in North Renmark 1 (Thornton, 1972).|||Coombool Member, Merreti Member, Pyap Member|Unconformably underlain by Urana Formation. Overlain by Warina Sand, Renmark Group.||
26036|Monash Formation|73229|6|Mentioned|p66-68|Early Cretaceous|Early Cretaceous|Berri Basin.|||Coombool Member, Merreti Member, and Pyap Member|||
31607|Monga Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31607|Monga Suite|44093|5|Briefly described|p220 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
31607|Monga Suite|71206|6|Mentioned|p373, 377, 387|||Lachlan Fold Belt. Sr/Nd plot.|||Monga Granite.||Aluminous A-type granite.|
77038|Mongamula Monzogranite|71206|6|Mentioned|p373|||The name Mongamula [sic] appears in a list of Suites; almost certainly placed in the wrong column.|||||Aluminous A-type granite.|
24384|Monkellan Granodiorite|36413|2|Defined|p92|Devonian|Devonian|||||||
24384|Monkellan Granodiorite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Michelago Igneous Complex. Biotite granodiorite. GSNSW map code: gcm.||||||
24384|Monkellan Granodiorite|39626|6|Mentioned|p276|||||||||
24384|Monkellan Granodiorite|40328|4|Described|p209|||||||||
22365|Montagu Dacite Member|49690|4|Described|Tb.4, p9, p11,|Late Silurian|Late Silurian|Type section nominated 15km east of Cooma from GR 059830 (base) to GR 048825 (top). Up to 800m thick.|||||Bouldery outcrops of coarse, grey dacite with large hornblende phenocrysts.|14-FEB-14
28764|Montague Island Complex|42855|5|Briefly described|p620|||Variation on old name Montague Island Granite?||||||
83274|Monza gabbro|73154|6|Mentioned|p84, p89 Tb.2, p90-91, p92 Fig.8, p94|Miaolingian|Miaolingian|Entirely sub-surface body. Zircon ages of Monza gabbro from samples MZ0807 and MZ0810, shown as from Monza Intrusive Complex p78 Tb.1. Juvenile Hf isotope signature. See also Monza Gabbro.|503.2+/-3.2 Ma, 503.4+/-3.7 Ma zircon U-Pb SHRIMP|||||
79107|Mooculta Granite|69635|6|Mentioned|p165|||Coherent, rhyolitic sills in DDH T17 may be related to this unit.||||||
79107|Mooculta Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: typically non-magnetic. An arcuate outer zone of moderate magnetic intensity on the N and W margins is interpreted as aureole/granite contact zone.|||||Biotite granodiorite with pelitic metasedimentary xenoliths.|
79107|Mooculta Granite|71965|5|Briefly described|p904,910|||Geological province: Thomson Orogen. Concealed S-type granite occurring immediate north of the Mount Oxley Fault.||||||
79335|Mooki Coal Member|70791|5|Briefly described|p275, p283, p286-287, p292-294|Cisuralian|Cisuralian|New name. Mullaley Sub-basin. 0.5-3m thick. Borehole cross-sections and long-sections; correlations. Coal properties not described. In situ coal estimates.||||||
24616|Moolarben Coal Member|38614|6|Mentioned|Fig.6|||||||||
24616|Moolarben Coal Member|40806|2|Defined|p157|Permian|Permian|Prob. Permian||||||
24616|Moolarben Coal Member|42657|4|Described|p82|||of State Mine Creek Formation||||||
24616|Moolarben Coal Member|68004|5|Briefly described|p60 Table 6, p61, p157.|Late Permian|Late Permian|Western Coalfield. c.3 m thick. Uneconomic, but coalesces with Bungaba Coal Member (Glen Davis Formation) to form a 13.6 m thick layered seam NW of Ulan. See also references to Moolarben Seam (pp217-220).||Unit in State Mine Creek Formation.|||Dull coal with minor bright layers, mainly in the lower part, and numerous carbonaceous claystone layers.|
80459|Moolpa granite|70718|5|Briefly described|p48, p78-p79|Late Devonian|Late Devonian|Bendigo Zone, Murray Basin. Informal name [Only known from geophysical interpretation]. Size and rough shape of magnetic anomalies is provided.  Interpreted lithology and age  based on similar geophysical signature to outcropping Lake Boga and Pyramid Hill granites.||Cunninyeuk granite suite|||Interpreted to be S-type granite , with metamorphic aureole.|02-JUN-19
38288|Moombil Siltstone|22857|5|Briefly described|p516 App.1 Tb.A1.8|Carboniferous|Carboniferous|Included in the informal "Coffs Harbour Association". Black marine siltstone; rare lithofeldspathic wacke and granule conglomerate. Several kilometres thick. Geological Province: Texas-Coffs Harbour Slope and Basin.||||||
38288|Moombil Siltstone|23720|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Part of the "Coffs Harbour Association".  Black massive siltstone, rare lithofeldspathic wacke and granule conglomerate.||||||08-DEC-04
38288|Moombil Siltstone|23811|5|Briefly described|Map Legend|Westphalian|Tournaisian|Part of the "Coffs Harbour Association".  Black massive siltstone, rare lithofeldspathic wacke and granule conglomerate.||||||08-DEC-04
38288|Moombil Siltstone|23812|5|Briefly described|p10, p12 Tb.1|Late Carboniferous|Early Carboniferous|Included in the informal "Coffs Harbour Association".||||||
38288|Moombil Siltstone|24127|5|Briefly described|p4|||||||||
38288|Moombil Siltstone|24129|5|Briefly described|p4|Carboniferous|Carboniferous|||||||
38288|Moombil Siltstone|44450|3|Fully described|p14 Table 1|Late Carboniferous|Late Carboniferous|Geological Province: Coffs Harbour Block.||||||
38288|Moombil Siltstone|69639|6|Mentioned|p100|Westphalian|Tournaisian|||Coffs Harbour Association||Intruded by the Gleniffer Monzogranite.||
38288|Moombil Siltstone|71628|5|Briefly described|p2: 20, 45, 49, 54; p3: 27, 46; p17:8|Carboniferous|Carboniferous|See also p17: 28, 51, 91. Coffs Harbour Block. Appears as Moombil Sandstone on p2-20 and p3: 27-28, 46.||Coffs Harbour Association.||Is intruded by Charon Creek Quartz Diorite; Big Bull Gabbro; Collett, Chaelundi Mountain and Gleniffer Monzogranites; Dundurrabin, Guy Fawkes, Tyringham East Granodiorites.||
79358|Moombooldool Granite|72083|5|Briefly described|p9, p18-19, p34 Fig.5|||Of Trigg, 2016. A large, very poorly outcropping, coarse-grained granite body, largely exposed in the W part of Ardlethan 1:100K sheet area. Relatively little evidence is present of contact metamorphic effects.|c.430 Ma (Main et al., in prep.).|||Intrudes Wagga Group.|Fine- to medium-grained, subequigranular to subporphyritic tourmaline-muscovite granite.|31-AUG-19
75962|Moona Plains Gabbro|71628|6|Mentioned|p2:37|||Reserved name. The author prefers Moona Plains Complex as it has precedence (Binns et al., 1967) and better reflects the complexity of compositions within the intrusion.||||||
33759|Moona Vale Conglomerate Member|23469|5|Briefly described|p 328|||||||||
33759|Moona Vale Conglomerate Member|24345|4|Described|p83, p84 Fig. 2|||Supersedes Moona Vale Conglomerate.    Thickness: 350m at type section.    Geological Province: Moona Vale Trough.||||||
33759|Moona Vale Conglomerate Member|63632|6|Mentioned|p657|Paleoproterozoic|Paleoproterozoic|Alluvial fan deposits formed from debris flows.||||||07-NOV-08
33759|Moona Vale Conglomerate Member|64169|5|Briefly described| p20 Fig. 9|Devonian|Devonian|Of the Snake Cave Sandstone.  Written informally as Moona Vale conglomerate member.||||||
33759|Moona Vale Conglomerate Member|66623|1|Redefined|pp192-193, pp208-212. |Middle Devonian|Early Devonian|Formerly Mootwingee Series (Andrews 1922), undifferentiated Mulga Downs Group (Rose 1974), Menamurtee Dome Sequence (Neef et al. 1996), part of Snake Cave Sandstone (Buckley 2000), Muckabunnya beds of Neef & Larsen (2002). Redefined in this study. Correlates with Muckabunnya Formation units e to h. Occurs about 2300 m above the base of the Menamurtee Sandstone. It is alternatively suggested that this Member and overlying strata are equivalent to Ravendale Formation. Forms low rises.||Unit in Menamurtee Sandstone.|||Massive, clast-supported unit with rounded to angular boulders of well-cemented sandstones, quartzite and less common felsic porphyry, to 1.5 m in diameter; progressive decrease in size northwards; coarse sandstone matrix; rare sandstone lenses.|
33759|Moona Vale Conglomerate Member|67562|5|Briefly described|p106-107, p111-112|||Maximum thickness ~ 520m. East of Mt Daubeny, and adjacent to the eastern margin of the Koonenberry Fault, a 450m thick breccia unit, comprising clasts of ?alluvial fan deposited, lightly indurated sandstone is thought to be coeval with this member. ||Menamurtee Sandstone.||Unconformably overlies unit 2 of the Muckabunnya Beds.||23-JAN-17
41069|Moonbi Monzogranite|24366|5|Briefly described|p11 Fig. 9|Early Triassic|Late Permian|Of the Moonbi Plutonic Suite.||||||
41069|Moonbi Monzogranite|65398|5|Briefly described|p5 Tb.1, p9, Fig 2|Early Triassic|Late Permian|Unit in Moonbi Supersuite. A stitching pluton across Peel Fault. Coarsely-porphyritic biotite-hornblende monzogranite and minor monzonite. Age of 247-249 Ma (Rb-Sr biotite: Shaw and Flood, 1992).||||||
41069|Moonbi Monzogranite|66720|5|Briefly described|Map legend|Early Triassic|Late Permian|||Unit in Moonbi Supersuite.|||Coarsely-porphyritic biotite-hornblende monzogranite; minor monzonite.|
41069|Moonbi Monzogranite|68005|5|Briefly described|p67, p134.|Permian|Permian|Listed on p.134 [and in the database] as a unit in Moonbi Suite.||Unit in Southern Moonbi Supersuite.|||Coarsely porphyritic biotite-hornblende monzogranite and minor monzonite.|
41069|Moonbi Monzogranite|68006|5|Briefly described|pp143-144, p165.|||Has skarns in surrounding limestones which should be assessed for economic mineralisation.||Unit in Moonbi Supersuite.||||
41069|Moonbi Monzogranite|68111|5|Briefly described|p968 Tb.1|Olenekian|Olenekian||250 - 247 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
41069|Moonbi Monzogranite|68679|5|Briefly described|p458, p461 Fig.5.132|||Tamworth district. Geochemical plots.||Moonbi Supersuite.||||
41069|Moonbi Monzogranite|69639|6|Mentioned|p211, p218|Induan|Changhsingian|Intrudes the peel Fault.|251.1 +/- 1.8 Ma (SHRIMP, Jeon, 2012)|||||
41069|Moonbi Monzogranite|71628|4|Described|p1:14; p7: 1, 4, 8, 10, 13-14, 19, 22-23|||See also p7: 30-37, 41, 44-45. DMR NAND04 Nandewar Geology Integration and Upgrade Project (2003), after unpublished work by Barnes and Willis (1989). Originally Moonbi Adamellite of White (1964), after unpublished work by Chappell (1959, 1966). Named after the locality of Moonbi. Extends from ~3km NE of Tamworth to 2km SW of Bendemeer. Forms subdued topography. Metamorphic aureole described. Zoning, petrology, mineralogy and geochemistry detailed. Chemically similar to Bendemeer Monzogranite. Associated with three small Mo(W) deposits.|251.1 +/- 1.8 Ma (SHRIMP: Jeon et al., 2014).|Moonbi Suite.||Intrudes Bendemeer Monzogranite, Tamworth Group, Silver Gully, Wisemans Arm, Cara and Horse Arm Formations, Woodsreef Melange, Woolomin and Sandon Associations.|Weakly zoned, medium- to coarse-grained, coarsely porphyritic, hornblende-biotite monzogranite to granodiorite. Abundant enclaves. I-type.|
41069|Moonbi Monzogranite|73264|6|Mentioned|p1398 Fig.20, p1399|Triassic|Permian|New England Orogen.|251 Ma|Moonbi Supersuite||||
29249|Moonbi Suite|22580|6|Mentioned|p99|Early Triassic|Late Permian|||||||
29249|Moonbi Suite|22857|6|Mentioned|p204 Fig. 17.2, p239|||Plutonic suite within the New England Batholith. See also p243 Fig. 18.4.||||||
29249|Moonbi Suite|22859|6|Mentioned|Fig17.2p204|||||||||
29249|Moonbi Suite|22863|6|Mentioned|p239|||||||||
29249|Moonbi Suite|23544|5|Briefly described|p372|||||||||
29249|Moonbi Suite|23549|5|Briefly described|p518, p520|||Of Moonbi Supersuite. Comprises two plutons - Moonbi and Bendemeer plutons. Geological Province: New England Orogen.||||||05-APR-05
29249|Moonbi Suite|38683|5|Briefly described|p13|Early Triassic|Late Permian|Geological Province: New England Fold Belt. Age: ~250Ma||||||
29249|Moonbi Suite|38822|6|Mentioned|p193|||Geological Province: New England Fold Belt||||||
29249|Moonbi Suite|38823|6|Mentioned|p207|||||||||
29249|Moonbi Suite|38824|6|Mentioned|p212|||Geological Province: New England Fold Belt||||||
29249|Moonbi Suite|38839|6|Mentioned|p244|||Geological Province: New England Fold Belt||||||
29249|Moonbi Suite|38905|6|Mentioned|p305|||Geological Province: New England Fold Belt||||||
29249|Moonbi Suite|41133|6|Mentioned|p1124|||||||||
29249|Moonbi Suite|42780|5|Briefly described|p419|||age of 247-249 Ma.||||||
29249|Moonbi Suite|42876|6|Mentioned|p142|||||||||
29249|Moonbi Suite|42984|5|Briefly described|p365|||||||||
29249|Moonbi Suite|43017|5|Briefly described|Fig.2,p374|||||||||
29249|Moonbi Suite|44093|5|Briefly described|p226 App. 1|Triassic|Permian|Orogenic granite. Age: <250Ma. Geological Province: New England Fold Belt.||||||
29249|Moonbi Suite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Includes: Undercliffe Falls Monzogranite, Mount Mitchell Monzogranite, Newton Boyd Granodiorite.||||||
29249|Moonbi Suite|60422|5|Briefly described|p386|Early Triassic|Late Permian|Of the New England Batholith. Also classified as Supersuites (Chappell and Bryant).||||||
29249|Moonbi Suite|68004|5|Briefly described|p67, p117.|Early Triassic|Late Permian|New England Fold Belt. May include an intrusive complex of this age at Bald Hill, in the Werrie Basin. Also called Moonbi Plutonic Suite on p117. Has recognised porphyry copper-gold potential.|||||Fractionated, I-type, oxidised granites.|
29249|Moonbi Suite|68005|6|Mentioned|p133, p134.|Permian|Permian|There is inconsistency with subdivisions of the Moonbi Supersuite in this article. This unit and the (?informal) Southern Moonbi Supersuite are both given as parents to the Bendemeer Monzogranite. ||Unit in Moonbi Supersuite.||||
29249|Moonbi Suite|71280|5|Briefly described|p410|Early Triassic|Permian||||||I-type plutonic rocks.|
29249|Moonbi Suite|71628|5|Briefly described|p1:14; p7: 11, 28, 30, 33; p11:17|||Chappell et al. (1987); previously the Bendemeer Suite (Chappell, 1978).||Moonbi Supersuite.|Bendemeer, Moonbi, Looanga Monzogranites.|||
29249|Moonbi Suite|73202|6|Mentioned|p637, p638 Fig.9, p639 Fig.10|Lopingian|Lopingian|New England Orogen, southern. Intrudes the Peel-Manning Fault System.|ca 256 Ma|||||
29249|Moonbi Suite|73264|6|Mentioned|p1399|||||||||
36465|Moonbi Supersuite|23549|5|Briefly described|p516 Fig. 1, p519|||Geological Province: New England Batholith.||||||05-APR-05
36465|Moonbi Supersuite|23763|5|Briefly described|p543 Fig. 1|Early Triassic|Late Permian|Previously the Moonbi suite.  Includes the Ruby Creek granite, Stanthorpe leucomonzogranite, and Bungulla monzogranite.  Geological Province: New England Fold Belt.||||||
36465|Moonbi Supersuite|23812|5|Briefly described|p24|Early Triassic|Late Permian|||||||
36465|Moonbi Supersuite|24512|5|Briefly described|p6, p7|||Granite. Of the New England Batholith. The northern part is highly prospective for Sn and Au deposits. Includes Stanthorpe Group of granites.||||||02-MAY-05
36465|Moonbi Supersuite|24513|5|Briefly described|p10|Early Triassic|Late Permian|High-K hornblende-biotite (+/-augite) I-type granite.||||||03-MAY-05
36465|Moonbi Supersuite|60422|6|Mentioned|p386, Fig. 1|Early Triassic|Late Permian|Of the New England Batholith. ||||||
36465|Moonbi Supersuite|61783|4|Described|p295-296|||Component of the New Engalnd Batholith. Granites.||||||
36465|Moonbi Supersuite|62534|6|Mentioned|p22|||||||||07-FEB-11
36465|Moonbi Supersuite|62757|5|Briefly described|p1-2, p13 Fig. 5|Early Triassic|Late Permian|Plutonic suite of the New England Batholith. Age: 251-243Ma. Mafic granitoids.||||||07-FEB-11
36465|Moonbi Supersuite|63748|5|Briefly described|p25, p47|||Includes the Walcha Road Monzogranite.||||||07-FEB-11
36465|Moonbi Supersuite|65398|5|Briefly described|p4 Fig.2, p9, Fig 2-3|Early Triassic|Late Permian|Of Bryant (2001). Includes Inlet Monzonite, Attunga Creek Monzogranite and Moonbi Monzogranite. Results in large contact aureoles of albite-epidote to upper hornblende facies. Age: 247-249 Ma (Rb-Sr biotite).||||||
36465|Moonbi Supersuite|66720|6|Mentioned|Map legend|Early Triassic|Late Permian||||Includes Moonbi, Inlet and Attunga Creek Monzogranites.|||
36465|Moonbi Supersuite|68005|5|Briefly described|p20, p32, p60, pp67-68, pp133-134, p170.|Early Triassic|Late Permian|Part of New England Batholith. I-type. Formerly a suite of Shaw and Flood (1982); redefined as a Supersuite by Bryant (2001) who subdivided it into a Northern Moonbi Supersuite and a Southern Moonbi Supersuite. Are these meant to be formal names?  There is inconsistency between these and the formal Moonbi Suite, eg as to what unit is the parent of Bendemeer Monzogranite [currently it is the Moonbi Suite].|||Includes Moonbi Suite.|||
36465|Moonbi Supersuite|68006|5|Briefly described|p20 Fig.3-A, p135, p143, p146, p155.|Early Triassic|Late Permian|New England Batholith, New England Fold Belt. Of Bryant (2001). I-type. May be favourable for porphyry copper-gold or porphyry-related gold only deposits. Covers the Weabonga Gold Field. Has W-Mo veins and disseminations internally and along the margins of its granites. A number of oxidised granites have high potential as a source of garnet.|||Includes Moonbi Monzogranite, Inlet Monzonite, Attunga Creek and Moonbi Granites.|||
36465|Moonbi Supersuite|68111|5|Briefly described|p968 Tb.1||||||Includes Inlet, Looanga, Attunga Creek, Moonbi, and Bendemeer Monzogranites, Oban River Leucomonzogranite, Red Range Microleucogranite, Limbri Leucomonzogranite, and Kingsgate Leucogranite.|||
36465|Moonbi Supersuite|68679|5|Briefly described|p458, p461-462|||Tamworth district. Geochemistry discussed; geochemical plots.|||Moonbi, Bendemeer Monzogranites, Inlet Monzonite.|||
36465|Moonbi Supersuite|69188|5|Briefly described|p1, p60|||The Highlands Complex is described as "geochemically unique, and a poor fit in the Moonbi Supersuite, to which it is sometimes ascribed".|||Highlands Complex.|||
36465|Moonbi Supersuite|69323|5|Briefly described|p20,70|Late Permian|Late Permian|Geological province: New England Orogen.|||Includes Attunga Creek Monzogranite, Inlet Monzonite, Walcha Road Monzogranite, Red Range Leucoadamellite, Oban River Leucoadamellite, Bendemeer Monzogranite.|||
36465|Moonbi Supersuite|69541|6|Mentioned|p646|||New England Batholith.|||Includes Inlet Suite.|||
36465|Moonbi Supersuite|69639|5|Briefly described|p1-p2, p9-p10, p26, p94|||New England Orogen. See also p133, p198, p211-p212, p217-p221.|||Includes the Kingsgate Leucogranite, Oban Suite, Walcha Road Monzogranite, Congi Creek Monzogranite, Inlet Monzonite, Bendemeer Monzogranite and the Red Range Leucomonzogranite.|||
36465|Moonbi Supersuite|70217|6|Mentioned|p60, p75|||New England Orogen.||||||
36465|Moonbi Supersuite|71628|4|Described|p1:6-7; p3:41; p4: 9, 11, 15; p5: 1-2,7|Early Triassic|Permian|See also p7: 1-51; p8: 2-3, 23, 97, 105; p9: 3, 41; p10: 1, 7; p11: 1, 3-5, 11, 17, 19, 40; p13: 2, 7, 25; p14: 8, 13, 23, 29; p15: 1, 5-6, 9, 16, 20, 23, 26, 34, 46-47, 53, 73, 77, 83, 93, 98, 107; p16: 21, 26; p17: 1, 5; p18-18; p19: 18, 39-41, 60, 98, 131, 136, 138, 142, 154. Chappell and Bryant (1994) significantly expanded this unit to include many of the leucocratic granites in the Tenterfield-Stanthorpe region. These authors in 1996 differentiated the Stanthorpe Granite Group from the Moonbi Granite Group in the south. Redefined in this study to include only those units in the southen part of the southern New England Orogen, N and NE of Tamworth. The highly anomalous geochemistry is described in some detail. Includes Attunga Creek, Moonbi, Callaghans Creek, Inlet, Limbri, Walcha Road Suites.|254 - 248 Ma.||Looanga, Bendemeer, Inlet, Moonbi, Walcha Road Monzogranites; Limbri Leucomonzogranite; Callaghans Creek Quartz Monzodiorite.|Intrudes Banalasta Monzogranite.|Dark grey to pale grey, medium- to coarse-grained, equigranular to strongly porphyritic, massive plagioclase-rich biotite-hornblende-(pyroxene) monzogranite, locally transitional into granodiorite. Mafic and felsic variants.|
36465|Moonbi Supersuite|72528|6|Mentioned|p71.|||||||||
36465|Moonbi Supersuite|73264|6|Mentioned|p1398 Fig.20, p1399|Triassic|Permian|New England Orogen. I-type granitoids.|~250 Ma||Bendemeer Monzogranite, Moonbi Monzogranite|||
36465|Moonbi Supersuite|73570|6|Mentioned|p918|Late Permian|Late Permian|New England Orogen.||||||
34753|Mooneba Formation|22892|6|Mentioned|p41|Quaternary|Quaternary|Age: 3740yrs Bp.||||||
35404|Moonshine Granite|50231|5|Briefly described|Map Legend|Emsian|Emsian|||||||
35404|Moonshine Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Grey to pinkish, medium-grained, massive, generally equigranular ferroan enstatite-augite-biotite-hornblende granite and granodiorite; minor marginal lecuocratic, porphyritic granite to microgranite.||||||
35404|Moonshine Granite|68592|2|Defined|p1398, p1401-3, p1442-5|Early Devonian|Early Devonian|New unit and name, after Moonshine property. Forms a series of broad rises; is exposed as scattered groups of boulders and large tors. Type locality described. Geochemistry detailed; geophysical properties described. Contains a large xenolithic block of Young Granodiorite. Age from parent.||Unit in Gooramma Suite.||Intrudes (and is probably comagmatic with) Mountain Creek Volcanics.|Grey to pinkish, medium-grained, massive, generally equigranular, hypersthene-augite-biotite-hornblende granite to granodiorite with an irregularly developed marginal phase of leucocratic, porphyritic granite to microgranite. I-type.|
35404|Moonshine Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgo. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Gooramma Suite|||Medium grained, massive, generally equigranular, hypersthene-augite-biotite-hornblende granite to granodiorite. Minor marginal leucocratic, porphyritic granite to microgranite; high to very high magnetic susceptibility.|
35404|Moonshine Granite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Medium grained, massive, generally equigranular, hypersthene-augite-biotite-hornblende granite to granodiorite. Minor marginal leucocratic, porphyritic granite to microgranite; high to very high magnetic susceptibility.|
38285|Moonta Gully Monzogranite|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Medium-grained, mildly porphyritic, grey biotite-hornblende monzogranite.||||||20-DEC-04
38285|Moonta Gully Monzogranite|23812|5|Briefly described|p22 Tb.2|Late Permian|Late Permian|||||||
38285|Moonta Gully Monzogranite|69639|4|Described|p1-2, p5, p8, p21|Induan|Changhsingian|New England Orogen. Sample locality, petrography, and geochronology is described. See also p56-p61, p219, p222, p237.|253.6 +/- 1.6 Ma (SHRIMP)|Moonta Gully Suite||Intruded by the Dandahra Creek Leucogranite. Intrudes the Gundahl Complex.|Massive, inequigranular, medium-grained granodiorite.|
38285|Moonta Gully Monzogranite|71628|4|Described|p17:4; p19: 127-130|||Barnes and Willis (1989); previously Moonta Gully Adamellite (McPhie, 1986). Named after a local watercourse. Occurs ~25 km NW of Jackadgery. Forms a narrow (up to 1.5 km wide), discontinuous annulus around Coombadjha Volcanic Complex [CVC]; interpreted as being emplaced following cauldron collapse after eruption of CVC. Crops out as boulders and bluffs.|253.6 +/- 1.6 Ma (SHRIMP: Chisholm et al., 2014).|Moonta Gully Suite.||Intrudes Silverwood Group and Gundahl Complex. Abuts Drake Volcanics. Surrounds (much of) Coombadjha Volcanic Complex: Pheasant Creek and Hianana Volcanics, Pi Pi Ignimbrite, and Dundee Rhyodacite.|Grey, medium-grained, porphyritic but locally equigranular, biotite-hornblende monzogranite to granodiorite. I-type.|
34397|Mooraback beds|22736|6|Mentioned|p611 Fig2||Permian|||||||
34397|Mooraback beds|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Macleay Group. Thickness is tens of metres. Geological Province: Barnard Basin (Nambucca Basin).||||||
34397|Mooraback beds|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|Geological Province: New England Fold Belt.||||||
75832|Mooral Creek serpentinite|65317|5|Briefly described|p633, p622 Fig. 1c, p635 Fig. 14|Early Permian|Late Carboniferous|Appears to be an informal name. Located in the southern Hastings Block, New England Orogen.  Structures suggest Early Permian emplacement. Shown as Mooral Creek Serpentinite p622 and in figs.||||||
22380|Moorilda Monzonite|22679|4|Described|p 40||Late Ordovician|Intrudes Blayney Volcanics.||||||17-JUL-08
22380|Moorilda Monzonite|22704|6|Mentioned|p66|||||||||
22380|Moorilda Monzonite|23214|2|Defined|p94|Late Ordovician|Late Ordovician|Intrudes the Blayney Volcanics. Only four known outcrops. Magnetic anomaly suggests the unit is more extensive with depth.||||||
22380|Moorilda Monzonite|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Clinopyroxene monzonite, altered monzonite.||||||17-JUL-08
22380|Moorilda Monzonite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
22380|Moorilda Monzonite|63283|6|Mentioned|p204|Late Ordovician|Late Ordovician|Intrudes Millthorpe Volcanics. Age of emplacement: ca 440 Ma.Geological Province: Molong Volcanic Belt.||||||07-FEB-11
22380|Moorilda Monzonite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
22382|Mooroona Granite|22638|4|Described|p73||Late Devonian|||||||
22382|Mooroona Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
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.|
23810|Morden Formation|22857|5|Briefly described|p122, p410 App. 1 Tb. A1.4.|||Base of Kayrunnera Group? Hard white medium-grained quartzite with silty laminations; thin limestone lenses. Overlain by Boshy Formation. Max. thickness: 6m.||||||
23810|Morden Formation|23245|6|Mentioned|p122|||||||||
23810|Morden Formation|41587|4|Described|p908|||||||||
23810|Morden Formation|41810|6|Mentioned|p107|||||||||
23810|Morden Formation|62793|5|Briefly described|p270|Late Cambrian|Late Cambrian|Basal unit of Kayrunnera Group, Northern Koonenberry Belt. Non-fossiliferous quartzite, 1 - 6 m thick.||||Unconformably overlies Teltawongee beds. Underlies Boshy Formation.||21-MAR-12
23810|Morden Formation|63790|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of Kayrunnera Group. Basal cross-bedded calcareous pebbly quartzites and quartzites, east of Koonenberry Fault.||||||
23810|Morden Formation|64671|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of Kayrunnera Gp. Well-laminated quartzose sandstones and quartzites, mostly white, some red and maroon. Festoon cross-bedding in some units. Minor siltstone and conglomerate interbeds. Lacking detrital mica. Mindyallen trilobite remains near base.||||||26-NOV-08
23810|Morden Formation|64684|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of Kayrunnera Group. Well-laminated quartzose sandstones and quartzites, mostly white, some red and maroon. Festoon cross-bedding in some units. Minor siltstone and conglomerate interbeds. Lacking detrital mica. Mindyallan trilobite at base.||||||08-DEC-08
23810|Morden Formation|66623|3|Fully described|p110, pp114-116. |Late Cambrian|Middle Cambrian|Kayrunnera Basin. A thin (less than 10 m) basal unit forming prominent strike-persistent outcrops. Contains worm-burrows. Has weak cleavage and minor folding. Represents base of  a marine sedimentary cycle from uplift and erosion of Delamerian highlands. Correlative of Hummock Formation.|Post-Delamerian Orogeny, c.500 Ma.|Unit in Kayrunnera Group.||Unconformably overlies Teltawongee Group rocks. Is conformably overlain by Boshy Formation.|Prominent metre-wide outcrops of medium-grained pure quartzite, calcareous cement sporadically developed in the upper section; sporadic crossbeds.|05-DEC-12
23810|Morden Formation|66929|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Mindyallan trilobite remains near base.|||||Well-laminated quartzose sandstones and quartzites; mostly white, some red and maroon; local festoon cross-bedding; minor siltstone and conglomerate interbeds.|
23810|Morden Formation|66933|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Mindyallan trilobite remains near base.||Unit in Kayrunnera Group.|||Well-laminated quartzose sandstones and siltstones; mostly white, some red and maroon; local festoon cross-bedding; minor siltstone and conglomerate interbeds; lacking detrital mica.|
23810|Morden Formation|67322|4|Described|p11; Fig.5|Series 3|Series 3|Defined by Webby et al. (1988). Between 1-6m thick but regionally extensive. Age determined from p20 Fig.5 (Strat. column). SE of Koonenberry Mountain.||Basal unit of the Kayrunnera Group.||Conformably overlain by the Boshy Formation.|Unfossiliferous medium-grained quartzite.|22-FEB-18
23810|Morden Formation|70648|5|Briefly described|Map Legend|Ordovician|Cambrian|||Kayrunnera Group|||Prominent metre-wide outcrops of cross-bedded calcareous pebbly quartzite.
|
23810|Morden Formation|70838|4|Described|p269 Fig.3, p270-272, p275, p277-278|Cambrian|Cambrian|Kayrunnera Basin, SE Koonenberry Belt. Sediments were not extensively reworked; have not travelled far. Detrital zircon analyses. Provenance discussed. Appears as Modern Formation on p277.||Basal Kayrunnera Group.||Is overlain conformably by Boshy Formation.|Grains of sub-angular quartz and feldspar embedded in calcite cement.|
23810|Morden Formation|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
82581|Morgans Creek Leucomonzogranite|71628|4|Described|p9: 3; p19: 130-133, 176|||Barnes and Willis (1989). Originally Morgans Creek Adamellite of Flinter et al. (1972) after unpublished work by Cook (1971). Renamed Morgans Creek Leucoadamellite by Flinter et al. (1982). Named after a local watercourse. Occurs 15 km N of Drake. The intrusion covers a 4.5 x 6 km area. Has features typical of high level plutons. Mineralogy detailed. Geochemistry described. Appears also as Morgans Creek Monzogranite on p19-131. Is associated with minor Mo mineralisation (deposits named).|240.8 +/- 1.3 Ma (SHRIMP: Chisholm et al., 2014).|Morgans Creek Suite.||Intrudes Navies Creek member (Drake Volcanics). Is faulted against Razorback Creek Mudstone.|Pinkish, coarse-grained, equigranular to porphyritic (biotite) leucomonzogranite; aplitic, microgranitic, graphic and pegmatitic marginal variants. I-type.|
39366|Moripo Dacite|24124|5|Briefly described|p3|Devonian|Devonian|||||||
37393|Morland Granodiorite|50234|5|Briefly described|Map strat. chart|Emsian|Emsian|Part of the Marulan Batholith.  Not represented in Map legend; [Djg] on map strat. chart.||||||13-MAY-04
25266|Morley Member|36413|6|Mentioned|p38|||||||||
82583|Mornington Complex|71628|5|Briefly described|p2: 41-44; p3-71; p19-74|||Originally the Mornington Diorite (Binns, 1966); herein the Mornington Complex, after Hensel (thesis, 1982), reflecting compositional variation. Named after a local homestead; ~38 km ENE of Guyra. Eastern boundary is cut by the Wongwibinda Fault. Assigned to the Bakers Creek Suite by Landenberger (1996) and to the Bakers Creek Supersuite by Landenberger et al. (2010). Geochemistry detailed.|c.280 Ma (Sr87/Sr86: Hensel, 1982).|||Intrudes Wongwibinda Complex and ?Dyamberin beds. Abuts Abroi Granodiorite.|Fine- to medium-grained quartz diorite; lesser gabbro, tonalite and monzogranite.|
33739|Mortray Hill Granite Complex|24233|5|Briefly described|p255 Fig.4|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
33739|Mortray Hill Granite Complex|24417|3|Fully described|p100|Early Devonian|Early Devonian|Of Bogalong Suite.  Previously included in "Bogalong Granite".  Constituent units "Mortray Hill Granite", "Lucy Hill Granite", "Rosehill Granite" and "Hill Sixty Granite" are discontinued.||||||
33739|Mortray Hill Granite Complex|60009|5|Briefly described|Map legend|Lochkovian|Lochkovian|Of the Bogalong Suite.||||||13-JUL-04
28778|Moruya Tonalite|23549|5|Briefly described|p521.|||Of the Moruya Suite.  Predominantly tonalites and granodiorites.||||||05-APR-05
28778|Moruya Tonalite|35248|4|Described|p239|||See also P236.||||||
28778|Moruya Tonalite|36600|6|Mentioned|p101|||||||||
28778|Moruya Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
28778|Moruya Tonalite|42855|5|Briefly described|p623|||||||||
38897|Mossgiel Granite|70718|5|Briefly described|p43, p65-p66, p71|Silurian|Silurian|Intersected in Mossgiel-1 drillhole. SHRIMP age  form Wilde (2000) . SHRIMP age is interpreted as the emplacement age of this granite. Shown as Mossgiel Granite p43, but not subsequently.|427+/- 7 Ma (SHRIMP U-Pb)|||Overlain by the Wana Karnu Group|S-type granitic rocks.|
23812|Mostyn Vale Formation|721|5|Briefly described|Map legend|Famennian|Frasnian|Of the Parry Group.  Pebbly lithic wacke, diamictite, lithic wacke, orthoconglomerate, olistostromal volcanic breccia, rhyodacitic to basaltic lavas, tuffs, agglomerates, rare limestone.||||||
23812|Mostyn Vale Formation|22736|5|Briefly described|p630|Famennian|Frasnian|||||||
23812|Mostyn Vale Formation|22857|4|Described|p219, p498 App.1 Tb.A1.7|Famennian|Frasnian|Of the Parry Group. Disconformably overlain by Keepit Conglomerate. Max. thickness: 2000m. Geological Province: Tamworth Forearc Basin.||||||24-FEB-06
23812|Mostyn Vale Formation|22859|5|Briefly described|p219||Frasnian|||||||
23812|Mostyn Vale Formation|23185|5|Briefly described|Fig1p156,157,162|Famennian||||||||
23812|Mostyn Vale Formation|23522|5|Briefly described|p249 Fig 5|Famennian|Frasnian|||||||
23812|Mostyn Vale Formation|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||14-APR-08
23812|Mostyn Vale Formation|24008|5|Briefly described|p360|Late Devonian|Late Devonian|||||||
23812|Mostyn Vale Formation|24605|5|Briefly described|p935 Fig.4|Frasnian|Frasnian|Geological Province: New England Orogen.||||||
23812|Mostyn Vale Formation|24614|6|Mentioned|p190|||||||||07-FEB-11
23812|Mostyn Vale Formation|41009|3|Fully described|p3|||||||||
23812|Mostyn Vale Formation|42728|5|Briefly described|p5|||||||||
23812|Mostyn Vale Formation|42849|6|Mentioned|p539|||||||||
23812|Mostyn Vale Formation|43091|5|Briefly described|Map legend|||Of Parry Group.||||||04-FEB-08
23812|Mostyn Vale Formation|50132|5|Briefly described|p246 Fig. 4, p247 Fig. 5, p248 Fig.6|Late Devonian|Late Devonian|New England Fold Belt, Manilla area||||Underlies the Keepit Conglomerate.||27-MAR-12
23812|Mostyn Vale Formation|50629|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Parry Group. Geological Province: New England Orogen.||||||04-FEB-08
23812|Mostyn Vale Formation|61769|5|Briefly described|p95, p96, p97, p99 Fig. 4, p102||Late Devonian|Unit has been thrust over Currabubula Formation. Consists of lava flows, coarse volcanic breccias and tuffs, lavas are basalt to basaltic andesites.||||||
23812|Mostyn Vale Formation|63774|6|Mentioned|p1079, p1085|Devonian|Devonian|Geological Province: Tamworth Belt.||||||17-MAR-09
23812|Mostyn Vale Formation|65214|6|Mentioned|p280|Devonian|Devonian|NSW, Tamworth and Keepit. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23812|Mostyn Vale Formation|65902|4|Described|p195 Fig.2, p199, p203 Fig.7|Fammenian|Frasnian|Disconformably overlain by Keepit Conglomerate. Agglomerate, conglomerate, breccia and pebbly sandstone containing allochthonous blocks ranging in composition from vesicular andesite to basalt, tuffs and limestone. Dated by ammonoid Cheiloceras acutum.||||||09-MAR-12
23812|Mostyn Vale Formation|66720|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Parry Group.|Includes two un-named but separately mapped units: volcanic agglomerate olistoliths; lava and volcaniclastic olistoliths.||Pebbly and conglomeratic lithic wacke, diamictite, lithic wacke; olistoliths of orthoconglomerate, and andesitic to basaltic (rare rhyodacitic) lavas, volcaniclastics and agglomerates, rare limestone.|
23812|Mostyn Vale Formation|68003|5|Briefly described|p32 Fig.3-h, p139.|Famennian|Late Devonian|Tamworth Belt (North), New England Fold Belt. Coeval with Lowana Formation and Noumea beds.||Unit in Parry Group.||Is overlain by Keepit Conglomerate.|Pebbly lithic wacke, diamictite, lithic wacke, orthoconglomerate, olistostromal volcanic breccia, rhyodacite to basaltic lavas, tuffs, agglomerates, rare limestone.|
23812|Mostyn Vale Formation|68004|6|Mentioned|p125.|||Mineral potential and level of certainty are discussed.||||||
23812|Mostyn Vale Formation|68005|5|Briefly described|p49 Fig.3-M, p54, p59, p149, p170.|Late Devonian|Late Devonian|Tamworth Belt. Occurs to the west of Keepit Dam. Moderate to strong magnetic response.||Basal unit in Parry Group.||Overlies Yarrimie Formation. Is overlain by Keepit Conglomerate.|Reworked andesitic volcanics and basalts: pebbly lithic wacke, diamictite, lithic wacke, orthoconglomerate, olistostromal volcanic breccia, rhyodacitic to basaltic lavas, tuffs, agglomerates, rare limestone.|
23812|Mostyn Vale Formation|68006|5|Briefly described|p149, p168.|||Tamworth Belt. Contains a few examples of anomalous base metal prospects. Hosts the Croydon magnetite deposit, 20 km from Manilla.|||||Rhyodacitic to basaltic lavas extruded in a deep marine setting.|
23812|Mostyn Vale Formation|68297|5|Briefly described|p186, 194|Late Devonian|Frasnian|NSW. Includes Late Devonian vertebrate fossil assemblages.||||||22-JAN-13
23812|Mostyn Vale Formation|68298|5|Briefly described|p216||Frasnian|Includes Frasnian conodonts in limestones in allochthonous blocks (Wright et al., 1990).||||||
23812|Mostyn Vale Formation|68822|6|Mentioned|p336, p347|||Proximal correlative of the Baldwin Formation. Fan fringe depositional environment.||||||
23812|Mostyn Vale Formation|70661|6|Mentioned|p118 |||Fossilised corals defining a global transgressive event in Australia. |||||Fossiliferous limestone.|
22394|Mother Shipton Monzodiorite|22638|2|Defined|p28|Early Silurian|Late Ordovician|New name. Type locality: Mother Shipton Hill.||||||05-APR-20
22394|Mother Shipton Monzodiorite|44192|5|Briefly described|Map Legend|Llandoverian|Bolindian|||||||
22394|Mother Shipton Monzodiorite|50191|5|Briefly described|p17|Late Ordovician|Late Ordovician|Intrudes: Temora Volcanics.||||||
22394|Mother Shipton Monzodiorite|72082|5|Briefly described|p4, p25, p30, p32|Early Silurian|Late Ordovician|Age is derived from work by Warren et al (1995) although the reasoning behind her determination is not provided. Source of the gold in the Temora Gold Field; as hydrothermal quartz veins (the Mother Shipton lode), and weathering products as alluvial deposits (the "Temora lead"). Only known outcrop occurs on Mother Shipton Hill on the southeastern side of Temora.||||Intrudes (and ?co-magmatic with) Temora Volcanics.|Dioritic intrusion.|31-MAR-20
22394|Mother Shipton Monzodiorite|72495|6|Mentioned|p227,p 241|Late Ordovician|Late Ordovician|Source of gold at Temora. Age inferred from geochemistry (A. Crawford, pers. Comms, 2006).Is shoshonitic with 'Late Ordovician' chemistry (Wyborn 1996, unpubl.).||||Intrudes ?Temora Volcanics.||05-APR-20
81166|Mount Agony Formation|71538|5|Briefly described|p52-p55, p61-p62|Cisuralian|Cisuralian|Sydney Basin. Referred to throughout the text as "MAF". This name is new and corresponds to the uppermost shallow marine part of the former Pebbley Beach Formation.  Subdivided informally into two units: a lower sand-rich approximately 5m thick upper shoreface deposit and an upper mud-dominated lower shoreface deposit. Potential as source rocks for oil and gas.||Shoalhaven Group||Overlies the Pebbley Beach Formation. Disconformably overlies the Tallong Formation and the Yadboro Formation. Overlain by the Snapper Point Formation.||
31548|Mount Arthur Suite|42726|5|Briefly described|map legend||Silurian|||||||
31548|Mount Arthur Suite|44093|5|Briefly described|p180 App. 1|Early Devonian|Silurian|Mount is Mt in text of Table. Geological Province: Lachlan Fold Belt.||||||
31548|Mount Arthur Suite|71206|6|Mentioned|p373, 377, 387|||Lachlan Fold Belt. Sr/Nd plot.|||Mount Arthur Granite.||Aluminous A-type granite.|
27498|Mount Boppy Conglomerate Member|22768|6|Mentioned|p170|||||||||
27498|Mount Boppy Conglomerate Member|22857|5|Briefly described|p170, p444 App.1, Tb.A1.6|Early Devonian|Lochkovian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Max. thickness: <200m. Geological Province: Kopyje Shelf (Darling Basin). ||||||
27498|Mount Boppy Conglomerate Member|23171|6|Mentioned|p31|||||||||
27498|Mount Boppy Conglomerate Member|23173|6|Mentioned|Map Legend|||||||||
27498|Mount Boppy Conglomerate Member|35287|6|Mentioned|p7|||||||||
27498|Mount Boppy Conglomerate Member|39618|3|Fully described|p49|||||||||
27498|Mount Boppy Conglomerate Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27498|Mount Boppy Conglomerate Member|46900|6|Mentioned|Fig.2|||Stratigraphic table||||||
27498|Mount Boppy Conglomerate Member|70941|6|Mentioned|p78 fig 32, p94, p145|Late Silurian|Late Silurian|Hosts the Mount Boppy gold deposit in Canbelego.||Baledmund Formation||Overlain by the Baledmund Formation.|Conglomerate, sandstone and siltstone.|
27498|Mount Boppy Conglomerate Member|73174|5|Briefly described|p1038, p1040-1042, p1044|||Kopyje Shelf. Basal member of the formation. <200 m thick. Breccia clasts interpreted as derived from the underlying Girilambone Beds [Group]. Also referred to as Mt Boppy Conglomerate in figures.||Baledmund Formation, Kopyje Group, Cobar Supergroup||Underlain by Girilambone Beds [Group].|Sedimentary breccia with sub-angular fragments of vein quartz, quartz schist, and phyllite.|23-NOV-22
26048|Mount Bright Rhyolitic Ignimbrite Member|29915|2|Defined|p65|Carboniferous|Carboniferous|||||||
26048|Mount Bright Rhyolitic Ignimbrite Member|32378|6|Mentioned|p113|||||||||
26048|Mount Bright Rhyolitic Ignimbrite Member|42214|6|Mentioned|p460|||||||||
26048|Mount Bright Rhyolitic Ignimbrite Member|69635|4|Described|p188-195|Late Carboniferous|Late Carboniferous|New England Orogen.  U-Pb SHRIMP zircon magmatic crystallisation age.|311.2+/-1.8 Ma|Of Pokolbin Hills Volcanics.||Probably predates Matthews Gap Dacitic Tuff Member.|Relatively crystal-poor, fairly fine-grained, pumice-rich, densely welded ignimbrite. Dominant phenocrysts are quartz and plagioclase with less K-feldspar. Very high emplacement temperature, and a subaerial setting indicated.|
26048|Mount Bright Rhyolitic Ignimbrite Member|71628|5|Briefly described|p19: 134|||||Pokolbin Hills Volcanics.||Nonconformably overlies Mount View Range Granodiorite.||
82585|Mount Bullaganang Leucosyenogranite|71628|3|Fully described|p5: 1, 3-6, 8, 10; p19-103|Permian|Permian|Originally the Bullaganang Granite (Donchak et al., 2007). Renamed in this study the Mount Bullaganang Leucosyenogranite to reflect the feature from which it was named as well as its composition; the higher ranking units are renamed accordingly. Type locality is at MGA 344868 6836729 (Texas 1:100 000 sheet). Crops out ~50 km WNW of Stanthorpe as a small (18 km2) ovoid stock. Resistant unit, comprising the core of Mount Bullaganang and forms abundant boulders and rock pavements. Limited geochemistry described. Spatially associated with Cu and Cu-Au mineralisation.|291.5 +/- 2.2 Ma (SHRIMP: Donchak et al., 2007).|Mount Bullaganang Suite.||Intrudes Texas beds.|Pale pink to pale brownish pink, medium-grained, uneven-grained, leucocratic biotite syenogranite. I-type.|
82586|Mount Bullaganang Supersuite|71628|4|Described|p5: 1-11; p15-79; p19-104|Permian|Permian|Originally the Bullaganang Supersuite (Donchak et al., 2007); the constituent Bullaganang Granite (Donchak et al., 2007) is renamed in this study to Mount Bullaganang Leucosyenogranite to reflect the feature from which it was named as well as its composition; the higher ranking units are renamed accordingly. Comprises a small number of Early Permian granites in the NW part of the southern New England Orogen, W and NW of Ballandean. Most were previously included in Ruby Creek Leucogranite. Broadly contemporaneous with Hillgrove Supersuite and Kaloe Tonalite. Geochemistry briefly summarised.|298-291 Ma (various authors cited).||Mount You You, Mount Bullaganang Suites. Jibbinbar, Mount Bullaganang Leucosyenogranites; Mount You You, Treverton Leucogranites.||Fine- to medium-grained, pale pink to pale grey (fresh), inequigranular to porphyritic, commonly leucocratic biotite monzogranite-syenogranite. I-type.|
40756|Mount Byar Ignimbrite Member|50613|2|Defined|p209, p227 App. 1|Late Carboniferous|Late Carboniferous|Of Willuri Formation.  Volcanic member of the Kaputar package (informal grouping of stratigraphically recognisable distinctive, mappable units. Overlies the Plagyan Ignimbrite Mbr and beds a and b of Piney Range Mbr.  Max. thickness: ~20m. Mount is Mt in||||||22-FEB-05
26049|Mount Carrington Rhyolite|33106|6|Mentioned|Fig.1|||||||||
26049|Mount Carrington Rhyolite|33476|2|Defined|p26|Permian|Carboniferous|Permian - Carboniferous||||||
26049|Mount Carrington Rhyolite|33766|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
26049|Mount Carrington Rhyolite|35803|6|Mentioned|p321|||||||||
26049|Mount Carrington Rhyolite|36961|6|Mentioned|Fig.5|||||||||
26049|Mount Carrington Rhyolite|37252|6|Mentioned|Map legend|Permian|Permian|||||||
26049|Mount Carrington Rhyolite|40505|6|Mentioned|p83|||||||||
26049|Mount Carrington Rhyolite|40773|4|Described|p458|||||||||
33416|Mount Cole Formation|23217|4|Described|p1, 5, 6, 9-13|Frasnian||Supersedes "Pipe Formation" and "Nyrang Formation"of Conolly (1965a). Overlies Mandagery Formation. Thickness in type section: 344m.||||||08-MAR-06
33416|Mount Cole Formation|23392|6|Mentioned|p12|||Correlates with Hunter Formation.||||||
33416|Mount Cole Formation|24417|2|Defined|p135|Frasnian|Frasnian|Of Hervey Group.  Formerly referred to as "Pipe Formation" and "Nyrang Formation".  Overlain by Bumberry Formation; underlain by Mandagery Formation.  Max. thickness: 344m.||||||
33416|Mount Cole Formation|60009|5|Briefly described|Map Legend|Famennian|Frasnian|Of the Hervey Group. Underlies: Bumberry Formation.  Overlies: Mandagery Formation.||||||13-JUL-04
33416|Mount Cole Formation|62569|6|Mentioned|p612|||Mentioned only in the context of "the Mandagery-Mt Cole Formation transition in the Parkes Syncline and west of Canowindra". Contains a lingulid-fish association at the transition point. Mount is Mt in text. ||||||
33416|Mount Cole Formation|68592|5|Briefly described|p1717|||In the Forbes 1:250 000 map area.||Unit in Hervey Group.||Correlated with lower part of Bumberry Formation.||
72573|Mount Darling Basalt|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Green to black, massive to pillowed, fine-grained basalt.||||||28-MAY-08
72573|Mount Darling Basalt|68592|2|Defined|p73 Tb.5, p374-5, p386-8, p397-8, p400-6|Ordovician|Ordovician|New name. Distinctly different geochemistry from the spatially associated Cabonne Group; previously equated with the Kenyu Formation. Ocean island basalt affinity. A type locality is given. Frogmore structural zone: deformation described.||||Faulted against Adaminaby Group and Wyangala Granite. Is intruded by Wyangala Granite.|Green to black, massive to pillowed, fine-grained alkali basalt; locally slightly porphyritic.|
72573|Mount Darling Basalt|70192|5|Briefly described|Map Legend|Late Ordovician|Early Ordovician|[Theta]xd. Ungrouped Ordovician formation. Age max and min boundaries on Time-Space plot extent is uncertain, and are marked with extended arrow and '?'. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||||Massive to pillowed, fine grained basalt; slightly porphyritic in places.|
72573|Mount Darling Basalt|70544|5|Briefly described|Map Legend|Ordovician|Ordovician||||||Massive to pillowed, fine grained basalt; slightly porphyritic in places.|
72573|Mount Darling Basalt|70545|5|Briefly described|Map Legend|Ordovician|Ordovician||||||Green to black, massive to pillowed, fine grained basalt; slightly porphyritic in places.|
77051|Mount Dijou Volcanic Member|67322|4|Described|p19; Fig.5|Floian|Floian|Described in detail by Trigg and Burton, in Burton et al. (in press), after Brunker (1968). Felton (1981) also recorded the presence of mafic volcanics apparently interbedded with the Girilambone Group on the Canbelego 1:100 000 sheet area. Occurs in the Sussex-Byrock region.||Of the Narrama Formation||Overlies the Kaiwilta Member.|Amygdaloidal pillow basaltic and trachytic lavas with inter-pillow chert.|22-FEB-18
77051|Mount Dijou Volcanic Member|68466|5|Briefly described|p65-66|Early Ordovician|Early Ordovician|Hermidale Terrane. Contains Floian conodonts.||Narrama Formation.|||Amygdaloidal pillow basaltic and trachytic lavas and inter-pillow chert.|
77051|Mount Dijou Volcanic Member|69094|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|The trachyte or trachytic basalt with pale yellow weathered surface is mapped separately.||Unit in Narrama Formation.||Overlies ?conformably Kaiwilta Member.|Deformed and altered amygdaloidal pillow basalt and lavas, trachytic lavas, fragmental basaltic rocks, minor chert and quartzose sandstone.|
77051|Mount Dijou Volcanic Member|69635|6|Mentioned|p69 Fig 3.1|||||||||
77051|Mount Dijou Volcanic Member|69668|5|Briefly described|p929 Fig.2, p931|Early Ordovician|Early Ordovician|Hermidale terrane, central NSW. The chert contains Oepikodus evae conodonts of Floian age.||Unit in Narrama Formation.||Overlies Kaiwilta Member.|Includes amygdaloidal pillow basaltic and trachytic lavas, with inter-pillow chert.|
77051|Mount Dijou Volcanic Member|70602|6|Mentioned|p67 Fig 3|Middle Ordovician|Early Ordovician|Age inferred.||Narrama Formation||||
77051|Mount Dijou Volcanic Member|70828|5|Briefly described|p6,14|Early Ordovician|Early Ordovician|Whole-rock geochemical data supports an oceanic island origin (Dadd 2006, Trigg and Burton 2012 p31-39 in Burton, Trigg and Campbell 2012). Associated with quartz-magnetic rocks, and therefore characterised by complex magnetic patterns due to magnetic remanence of the basaltic and quartz-magnetic rocks (Dadd 2006, Trigg and Burton 2012 p31-39 in Burton, Trigg and Campbell 2012).||Unit of Narrama Formation.||Underlain by Kaiwilta Member.|Alkali basalt and trachyte.|
77051|Mount Dijou Volcanic Member|70941|3|Fully described|pviii, pxii, p4, p6, p8 fig 4|Chewtonian|Bendigonian|Named for Dijou Mountain. Previously part of the Mount Dijou Volcanics, herein formally redefined. Distribution, geomorphology, geochemistry, geophysical characteristics(in detail), distinguishing characteristics.  Lithology elaborated on in detail. No type section available or described. Age derived from conodont fossil assemblage. Deposited in a deep water marine environment as an intra-plate oceanic seamount. Very minor gold and silver mineralisation occurs. See also p12, p16, p17, p21, p28, p30-41, p111, p112, p125, p124 fig 54, p134, p135, p139, p140 fig 58, p145, p147, p149, P155.||Narrama Formation||Conformably overlies the Kaiwilta Member. May also overlie the Narrama Formation where Kaiwilta Member is absent.|Amygdaloidal pillow basalts, basalt flows, trachyte, basaltic breccia and minor intercalated sedimentary rocks.|
77051|Mount Dijou Volcanic Member|71360|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Mapped as the one unit with the Kaiwilta Member and an un-named jasper unit, all of the Narrama Formation. Geophysical signature: irregular-shaped units of high magnetic intensity forming a curvilinear lenticular zone at surface (short wavelength), and a sub-parallel trend to the north at greater depth (longer wavelength).||Narrama Formation.|||Altered amygdaloidal basaltic pillow lavas and lavas, trachytic lavas, fragmental basaltic rocks, sandstone, siltstone, chert, magnetite-rich jasper.|
77051|Mount Dijou Volcanic Member|72296|5|Briefly described|p7|||||Girilambone group.|||Pillow lavas and interpreted basaltic breccias.|
77051|Mount Dijou Volcanic Member|73175|6|Mentioned|p1059-1060, p1065|Early Ordovician|Early Ordovician|Lachlan Orogen, northern. eNd (480 Ma) value of +3.6. Nd model ages of ca 860 Ma. Mount Dijou Volcanic Member spelt as Mt Dijou Volcanic Member. Written as only Mt Dijou on p1060 Fig.8, p1061, p1064 Fig. 11, p1065. Lower Ordovician alkali basalt from Mt Dijou.||Narrama Formation|||Basalts.|
22411|Mount Durham Tuff Member|22857|5|Briefly described|p506 App.1 Tb.A1.8|Westphalian|Namurian|Of the Seaham Formation. Tuffaceous arenite, felsic tuff. Max. thickness: 200m. Geological Province: Tamworth Forearc Basin.||||||
22411|Mount Durham Tuff Member|24603|5|Briefly described|897 Fig. 17|Late Carboniferous|Late Carboniferous|Age: 309+/-3Ma (Gulson et al, 1990).  Mount is Mt. in text of figure's caption.  Geological Province: Tamworth Belt.  In the Gresford Block.||||||
22411|Mount Durham Tuff Member|44244|6|Mentioned|p105, p107|||Of the Seaham Formation.  Geological Province: Gresford Block.||||||
22411|Mount Durham Tuff Member|60289|5|Briefly described|p1|Late Carboniferous|Late Carboniferous|Of Seaham Formation. Geological Province: Cranky Corner Basin.||||||
22411|Mount Durham Tuff Member|60290|3|Fully described|p15, 17, 37|Late Carboniferous|Late Carboniferous|Of Seaham Formation. Max. thickness: 354 m. Age: 306.5+/-2.1 Ma. Coarse-grained, granular, pebbly, porphyritic ignimbrite. Rhyolite to rhyodacite. Geological Province: Cranky Corner Basin.||||||07-FEB-11
22411|Mount Durham Tuff Member|60291|4|Described|p51, 55|Late Carboniferous|Late Carboniferous|Of Seaham Formation. Dacite, rhyolite, trachyte. Welded ignimbrite. Petrology described.||||||
22411|Mount Durham Tuff Member|60293|6|Mentioned|p107|||Of Seaham Formation. Vitritinite reflectance of organic matter described.||||||
22411|Mount Durham Tuff Member|60298|5|Briefly described|p179, 183|Stephanian|Westphalian|Partly welded ignimbrite. Age: 306.5+/-2.1 Ma (SHRIMP zircon U-Pb). Of the Seaham Formation. Geological Province: Cranky Corner Basin.||||||17-DEC-07
22411|Mount Durham Tuff Member|60299|5|Briefly described|p208|Carboniferous|Carboniferous|Of Seaham Formation. Age: ~311 Ma (U-Pb zircon, Roberts et al., 1995). Geological Province: Gresford Block.||||||
22411|Mount Durham Tuff Member|60300|5|Briefly described|p239|Carboniferous|Carboniferous|Of Seaham Formation. Geological Province: Cranky Corner Basin.||||||
22411|Mount Durham Tuff Member|62095|6|Mentioned|p268|Late Carboniferous|Late Carboniferous|Age: 306.5+/-2.1Ma.||||||
22411|Mount Durham Tuff Member|65107|5|Briefly described|p276, 289, fig 4 p279, Fig 11 p286-7|Kasimovian|Kasimovian|Member of the Seaham Formation, Gresford Block. Age: 306.5+/-2.1 Ma. Provides segments that agree with east to west pole path (for the Gresford Block) for the New England Orogen.||||||
22411|Mount Durham Tuff Member|73487|6|Mentioned|p566|Moscovian|Moscovian|Gresford Block.||||||
41070|Mount Duval Monzogranite|24366|5|Briefly described|p13|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.||||||
41070|Mount Duval Monzogranite|66660|3|Fully described|p342-p349|Changhsingian|Wuchiapingian|New England Batholith; Central Block, New England Orogen. Intrudes Sandon beds. Medium to coarse grained, massive and non-foliated, mesocratic grey granitoid, in places K-feldspar porphyritic. Distinguished in field from Newholme Monzogranite on basis of enclave proportions: igneous 66%, metasedimentary 26%, quartz 8%.|SHRIMP U-Pb zircon age 252.8 +/- 1.5 Ma.|||||07-OCT-15
41070|Mount Duval Monzogranite|68111|5|Briefly described|p968 Tb.1|Anisian|Induan||252 - 245 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
41070|Mount Duval Monzogranite|69188|5|Briefly described|p1-2, p4, p47-50, p52 Fig.2.34, p79|Permian|Permian|Indistinguishable in age from Newholme Monzogranite.|253.7 +/- 1.4 Ma (magmatic age)||||Medium- to coarse-grained monzogranite.|16-APR-20
41070|Mount Duval Monzogranite|69323|5|Briefly described|p41,71|||Geological province: New England Orogen.|253.7+/-1.4 Ma (Cross and Blevin, 2013)|Unit of Uralla Supersuite.||||
41070|Mount Duval Monzogranite|69639|5|Briefly described|p32, p68, p95, p133, p219|Induan|Changhsingian|New England Orogen.|253.7 +/- 1.7 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
41070|Mount Duval Monzogranite|70217|5|Briefly described|p43, p73 tbl 14.1|Changhsingian|Wuchiapingian|New England Orogen. Age derived from Cross and Blevin, 2013. |253.7 +/- 1.4 Ma (SHRIMP U-Pb)|Mount Duval Suite||||
41070|Mount Duval Monzogranite|71628|4|Described|p8: 3, 18-22, 24, 32-39, 42, 48, 109|||DMR NAND04 Nandewar Geology Integration and Upgrade project, after unpublished work by Neilson (1970) and Chappell and Bryant (1994). Named after the geographical feature 10km NNW of Armidale. Forms a large (~110 km2) crescent-shaped intrusion, c.32 x 5 km, with excellent exposures as whalebacks, tors and flat pavements. Contains enclaves and inclusions of Boorolong Granodiorite. Encloses Newholme Monzogranite. Geochemistry, geophysics described. Associated with several small deposits of Ag, Sb, Sn and Pb; also vein gold-antimony-arsenic deposits near contact with Tilbuster Granodiorite.|253.7 +/- 1.4 Ma (SHRIMP: Cross and Blevin, 2010).|Mount Duval Suite.||Intrudes Sandon beds, Wandsworth Volcanic Group, Glenore Monzogranite, and Boorolong and Exmouth Granodiorites (?and completely surrounds these last two). Is intruded by Tilbuster Granodiorite.|Medium-grained, porphyritic biotite-hornblende monzogranite; plagioclase phenocrysts to 15mm and orthoclase to 25mm. Abundant enclaves, of sedimentary and granite xenoliths and fragments of Boorolong Granodiorite. I-type.|
67902|Mount Duval Suite|70217|5|Briefly described|p43|||New England Orogen.||Uralla Supersuite|Includes the Webbs Consols Leucogranite, Mount Duval Monzogranite, the Tingha Granite and the Gwydir River Monzogranite.|||
67902|Mount Duval Suite|71628|5|Briefly described|p8: 1, 3-4, 18-49, 97, 100, 102, 118|||Crops out mainly W of Armidale and Guyra, but E of Bundarra Supersuite. Appears as Mt Duval Suite on p8-19.||Uralla Supersuite.|Mount Duval, Glenore, Newholme, The Basin, Glenreach, Tingha, Gwydir River Monzogranites; Exmouth, Boorolong Granodiorites.||Intermediate to felsic granites.|
81943|Mount Exmouth Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|||Green, white weathering, basalt to basaltic trachyandesite, porphyritic to aphanitic coherent and volcaniclastic units.|02-NOV-20
26052|Mount Fairy Group|22768|6|Mentioned|p176||Ludlow|||||||
26052|Mount Fairy Group|22857|5|Briefly described|p176, p472 App.1 Tb.A1.6|Ludlovian|Ludlovian|Geological Province: Captains Flat-Goulburn Trough.||||||
26052|Mount Fairy Group|23048|5|Briefly described|p6 fig9|Late Silurian|Silurian|||||||
26052|Mount Fairy Group|24116|5|Briefly described|p43|Silurian|Silurian|||||||
26052|Mount Fairy Group|24128|5|Briefly described|p148|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
26052|Mount Fairy Group|24317|5|Briefly described|p14, p15 Fig.1|Early Devonian|Late Silurian|Shallow to deep marine sedimentary rocks. Includes the Covan Creek Formation.||||||
26052|Mount Fairy Group|30730|6|Mentioned|p10|||Geological map||||||
26052|Mount Fairy Group|30735|2|Defined|p16|Silurian|Silurian|||||||
26052|Mount Fairy Group|30736|6|Mentioned|Map legend|Silurian|Silurian|||||||
26052|Mount Fairy Group|35503|6|Mentioned|p202|||Redefined in Felton and Huleatt (1977)||||||
26052|Mount Fairy Group|36413|6|Mentioned|Table 3|||||||||
26052|Mount Fairy Group|39331|6|Mentioned|p57|||||||||
26052|Mount Fairy Group|39800|6|Mentioned|Map legend|Silurian|Silurian|||||||
26052|Mount Fairy Group|40276|6|Mentioned|p3|||||||||
26052|Mount Fairy Group|40328|4|Described|p184|||||||||
26052|Mount Fairy Group|42727|5|Briefly described|map legend|Pridoli|Ludlow|Includes Covan Creek Formation, Currawang Basalt and Woodlawn Volcanics. Unconformably overlies Birkenburn beds. Geol. Prov: Rocky Pic Block.||||||
26052|Mount Fairy Group|42820|5|Briefly described|p46|||||||||
26052|Mount Fairy Group|43659|6|Mentioned|p4||Late Silurian|||||||
26052|Mount Fairy Group|44093|5|Briefly described|p209 App. 1|Early Devonian|Late Silurian|Mount is Mt in text of Table. See also p221 Appendix 1. Geological Province: Lachlan Fold Belt.||||||
26052|Mount Fairy Group|50232|5|Briefly described|Map legend|Ludlow|Ludlow|Interfingered with rocks of the Campbells Group.  Includes the Woodlawn Volcanics, Currawang Basalt and Covan Creek Formation.||||||
26052|Mount Fairy Group|50234|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Donganelly Formation, Joppa Formation, Sooley Volcanics, De Drack Formation, Currawang Basalt, Covan Creek Formation, Boxers Creek Formation, Gundary Formation, Longreach Volcanics.||||||
26052|Mount Fairy Group|62070|5|Briefly described|p37, p39, p40,|Late Silurian|Late Silurian|Includes limestone in basal formations.|||Includes De Drack Formation.|Includes the Palerang Formation||
26052|Mount Fairy Group|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes 14 constituent formations.||||||
26052|Mount Fairy Group|66087|4|Described|p5, p3 Fig. 2|Early Devonian|Middle Silurian||||Includes Boxers Creek, De Drack and Covan Creek Formations; Gundary and Woodlawn Volcanics, and Currawang Basalt.|Overlain by Bindook Group.|Felsic volcanics, that host massive sulfide related mineralisation (VHMS) and reduced gold skarn type mineralisation.|10-MAY-12
26052|Mount Fairy Group|66300|6|Mentioned|p29, p34. |Late Silurian|Late Silurian|Eastern Lachlan Orogen. Includes the mineralised Woodlawn-Currawang bimodal volcanic succession.|||Includes Woodlawn Volcanics.|||
26052|Mount Fairy Group|67820|6|Mentioned|p136 Fig.3|Lochkovian|Wenlock||||Gundary, Boxers Creek, Covan Creek, Donganelly, De Drack, Joppa Formations; Currawang Basalt; Woodlawn, Sooley Volcanics.|||
26052|Mount Fairy Group|68592|1|Redefined|p725-897, p902-3, p908, p913, p916|Early Devonian|Late Silurian|See also xxiii, p74 Tb.5, p107-108, p118, p232, p235, p238, p257, p269, p298, p326, p350, p360, p362-363, p624,. Modified after Felton and Huleatt (1977). Expanded to incorporate Taralga Group (Scheibner 1973) and part of Kowmung Volcaniclastics (Cas et al. 1981). 'Mount Fairy Series' by Garretty (1936) appeared on first edition Canberra 1:250 000 geological map sheet (Joplin et al. 1953). Modified to 'Mount Fairy Beds' on second edition Canberra 1:250 000 geological map sheet (Best et al. 1964). Some olistostromes E of Taralga are likely sourced from Bungonia Group. Thickness is highly variable, 1575 - 5150 m. Sub-greenschist and possibly lowest greenschist facies regional metamorphism. Age ranges from mid Wenlock to mid Lochkovian indicated by available palaeontology and age dating. Structure: bounded to E and W by faults. Mineralisation: hosts significant Pb-Zn-Cu-Ag+/-Au. Geol. Prov: Goulburn Basin. Contemporaneous with Campbells Group. Lower part is equivalent to Bungonia Group;  is intruded by Bishopthorpe Dolerite. Geophysical properties described. Goulburn structural zone: deformation described. Inferred displacement of c.35 km by Mulwaree Fault.|||Gundary, Longreach, Mares Forest, Woodlawn Volcanics; Argyle, Boxers Creek, Cobra, Covan Creek, De Drack, Kowmung, Rhyanna Formations; Currawang Basalt, Kerrawary Siltstone, Shivering Conglomerate.|Unconformably overlies, or is faulted against, Adaminaby, Bendoc and Margules Groups. Is unconformably overlain by Lambie Group; is erosionally overlain by Bindook Group.|Lower: conglomerate (basal), siltstone, mudstone, sandstone, marl, limestone, shale, interfinger with felsic to bimodal volcanics. Middle: basement-derived, quartzose package. Upper: felsic to intermediate, mafic (minor) lavas and volcaniclastics.|
26052|Mount Fairy Group|69159|5|Briefly described|Map legend|Devonian|Silurian||||Includes Woodlawn and Gundary Volcanics; Covan Creek, De Drack and Boxers Creek Formations; Currawang Basalt.|||
26052|Mount Fairy Group|69635|6|Mentioned|p11, 12, 19, 25||||||Includes Covan Creek Formation.|||16-JUL-15
26052|Mount Fairy Group|70192|5|Briefly described|Map Legend|Lochkovian|Wenlock|On Taralga, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Argyle, Boxers Creek, De Drack, Rhyanna, Kowmung, Covan Creek & Cobra Formations; Currawang Basalt; Gundary, Longreach, Mares Forest & Woodlawn Volcanics; Shivering Conglomerate; Kerrawary Siltstone.|||
26052|Mount Fairy Group|70297|5|Briefly described|map legend|Ludlow|Ludlow||||Argyle Formation|||
26052|Mount Fairy Group|70541|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Currawang Basalt, Covan Creek Formation, Woodlawn Volcanics.|||
26052|Mount Fairy Group|70542|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Argyle, Boxers Creek, De Drack Formations, Currawang Basalt, Gundary Volcanics, Rhyanna Formation, Longreach Volcanics, Covan Creek Formation, Woodlawn Volcanics, Kerrawary Siltstone|||
26052|Mount Fairy Group|70543|5|Briefly described|Map Legend |Devonian|Silurian||||Includes Argyle, De Drack, Rhyanna Formations, Gundary Volcanics, , Shivering Conglomerate, Kowmung Formation, Mares Forest Volcanics, Covan Creek Formation, Cobra Formation, Kerrawary Siltstone|||
26052|Mount Fairy Group|70601|5|Briefly described|p28, p55|Late Silurian|Late Silurian|Post-Benambran Orogeny.|||||Quartzose and lithic sandstones, felsic volcanics and limestones.|
26052|Mount Fairy Group|70661|6|Mentioned|p35||||||De Drack Formation|||
26052|Mount Fairy Group|71069|3|Fully described|p9, p21 fig 7, p23, p24, p26 fig 9, p27|Lochkovian|Wenlock|Name derived from the Mount Fairy locale on Braidwood100. Thickness ranges between 1575m to 5150m. No type section for the group has been proposed.  Previously the Mount Fairy Series and Mount Fairy Beds. Hosts VAMS mineralisation, gold vein deposits and small scale skarn-related deposits. Goulburn Basin. Age range defined by fossil assemblage, SHRIMP dating of the Back Station Ignimbrite Member and the overlying Bindook Group.Distribution, geomorphology, geochemistry, tectonic structure, metamorphism and fossil assemblage discussed. Also includes the Gundary Volcanics, Kerrawary Siltstone,  Argyle Formation, Cobra Formation, Rhyanna Formation and the Boxers Creek Formation.  Intruded by the Lockyersleigh and Abercorn Granites, in addition to the Billyrambija Dolerite Member and the Bishopthorpe, Turallo, Candello and Thurralilly Suites. Equivalent to the Hoskinstown Group and parts of the Campbells Group and Kangaloolah Volcanics. See also p28, p35, p36, p40 fig 17, p41, p42, p76 fig 27, p90, p99, p100, p106, p114, p115, p118, p120, p123, p125, p133-146,  p149, p163, p169.|||Includes the Currawang Basalt, Covan Creek Formation, Woodlawn Volcanics, De Drack Formation, Sandhills Creek Limestone Member, Shivering Conglomerate|Unconformably overlies or is faulted against the Adaminaby, Bendoc and Margules groups. Unconformably overlain by the Crookwell Basalt, Bullamalita and Tallong Conglomerates and the Lambie Group.|Conglomerate, thinly bedded siltstone, mudstone and fine-grained sandstone with biohermal limestone lenses and black shale.  Felsic to bimodal volcanic sequences of rhyolite, rhyodacite, dacite, dacitic ignimbrite, basalt and andesite also occur.|
26052|Mount Fairy Group|71656|3|Fully described|p10 Fig.1, p28, p30|Lochkovian|Wenlock||||Longreach Volcanics, Rhyanna Formation, Gundary Volcanics, Boxers Creek, Covan Creek, Argyle, De Drack Formations, Kerrawary Siltstone, Cobra Formation, Shivering Conglomerate.|Partially equivalent to Campbells Group and Crudine Group.||
26052|Mount Fairy Group|71691|5|Briefly described|Map legend.|Silurian|Silurian||||Covan Creek, De Drack Formations; Currawang Basalt; Woodlawn Volcanics.|||
26052|Mount Fairy Group|71699|5|Briefly described|Map legend.|Devonian|Silurian||||De Drack, Covan Creek, Boxers Creek Formations; Woodlawn, Gundary Volcanics; Currawang Basalt.|||
26052|Mount Fairy Group|71700|3|Fully described|vi, viii, p7, p10, p14-p16, p23-p24|Lochkovian|Wenlock|Goulburn Basin. Named for the locality of Mount Fairy at GR 736400 6105000. A composite section is found in the Woodlawn-Currawang-Tarago area.The Mount Fairy Series was used originally by Garretty (1936). The name Mount Fairy Group was first used by Joplin et al, 1953 before being subsequently modified to Mount Fairy Beds by Best et al, 1964. The Mount Fairy Group was formalised and defined by Felton and Huleatt (1977) and expanded by Thomas and Pogson (2012) to include rocks above the Covan Creek Formation. Also includes the Mares Forest Volcanics, Kowmung Formation, Rhyanna Formation, Longreach Volcanics, Argyle Formation, Kerrawary Siltstone and Shivering Conglomerate. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils, potential correlations and economic geology are discussed. This group has an estimated thickness of up to 5150m. Lithologies for constituent units are descirbed in detail. Hosts the Woodlawn VAMS deposit.  See also p28, p36-p38, p41, p45, p46-p51, p58-p60, p62-p64, p75, p79-p80, p84, p85, p116, p123, CD.|||Includes the De Drack Formation, Sandhills Creek Limestone Member, Woodlawn Volcanics, Currawang Basalt, Covan Creek Formation, Boxers Creek Formation, Gundary Volcanics.|Unconformably overlain by the Bindook Group. Disconformably overlain by the Mulwaree Group. Unconformably overlies the Adaminaby, Bendoc and Margules groups.||
26052|Mount Fairy Group|73582|5|Briefly described|p99, 105, 114, 118, 126|Early Devonian|Late Silurian|Goulburn Basin. Exposed in a NNE-trending belt on the E side of the Goulburn 1:250,000 sheet.||||Correlated with Inspiration Point Formation.|Clastic sedimentary rocks, interfingering with silicic lavas and volcaniclastics; graptolitic black shales; coarse-grained turbidites.|
26760|Mount Flakney Granite|22508|5|Briefly described|p2||Silurian|Koetong Supersuite, Lachlan Fold Belt||||||13-JUN-13
26760|Mount Flakney Granite|24119|5|Briefly described|p3|Silurian|Silurian|||||||
26760|Mount Flakney Granite|42726|5|Briefly described|map legend|Silurian||544.||Kyeamba Suite.||||19-JAN-17
26760|Mount Flakney Granite|69371|5|Briefly described|p9, p14-17|Silurian|Silurian|Shows a high K anomaly in airborne radiometric data.||||||08-DEC-17
26760|Mount Flakney Granite|69801|6|Mentioned|p2, p136-137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs between Wagga Wagga and Holbrook. Same age as the nearby Nest Hill Granite.|432.3 +/- 5.4 Ma (Ickert and Williams, 2011)||||S-type granite.|
32376|Mount Foster Monzonite|22519|5|Briefly described|p7|||||||||
32376|Mount Foster Monzonite|23053|4|Described|p23-4,70||Early Devonian|||||||
32376|Mount Foster Monzonite|43277|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
75830|Mount George serpentinite|65317|6|Mentioned|p630-631, p622 Fig. 1c, p635 Fig. 14|Early Permian|Late Carboniferous|Appears to be an informal name for serpentinites near Mt George township. Located on SW margin of Hastings Block, New England Orogen.  Structures suggest Early Permian emplacement. Shown as Mt George Serpentinite in figs.||||||
31205|Mount Gibraltar Microsyenite|43479|14|Not recorded|p263||Late Jurassic|at Bowral about 160-165 m.y||||||
31205|Mount Gibraltar Microsyenite|43870|14|Not recorded|p341||Early Jurassic|178 Ma||||||
31205|Mount Gibraltar Microsyenite|73197|6|Mentioned|p468|Serpukhovian|Serpukhovian|New England Orogen, southern, Sydney Basin. Earliest zircon ages in plutonic rocks of the New England Orogen [in section called 'Zircon inheritance']. Shown as Mount Gibraltar Syenite p465 Fig.4.|325 Ma zircon age||||Plutonic rock.|
23819|Mount Halfway Volcanics|22857|4|Described|p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Mount Hope Group (Cobar Supergroup). Rhyolite to dacitic lavas, ignimbrites, igniturbidites, tuffs, agglomerate interbedded with arenite, siltstone. Max. thickness: >2km. Geological Province: Mount Hope Trough (Darling Basin).||||||
23819|Mount Halfway Volcanics|22887|6|Mentioned|Fig.4 p11|||||||||
23819|Mount Halfway Volcanics|23048|6|Mentioned|p13|||||||||
23819|Mount Halfway Volcanics|23214|6|Mentioned|p360|||Of Mount Hope Group.||||||
23819|Mount Halfway Volcanics|37772|4|Described|p7|||||||||
23819|Mount Halfway Volcanics|40269|5|Briefly described|p148|||||||||
23819|Mount Halfway Volcanics|40913|6|Mentioned|Map legend|Devonian|Devonian|||||||
23819|Mount Halfway Volcanics|41126|2|Defined|p51|early Lochkovian|early Lochkovian|||||||
23819|Mount Halfway Volcanics|41528|2|Defined|p99|Early Devonian||||||||
23819|Mount Halfway Volcanics|41529|6|Mentioned|Map legend|Lochkovian||||||||
23819|Mount Halfway Volcanics|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
23819|Mount Halfway Volcanics|41821|2|Defined|p25|Early Devonian||||||||
23819|Mount Halfway Volcanics|42144|6|Mentioned|Fig.3 P604|||||||||
23819|Mount Halfway Volcanics|42521|5|Briefly described|Fig.3b P16|||||||||
23819|Mount Halfway Volcanics|42726|5|Briefly described|map legend|Early Devonian||Actually spelt Mt Halfway Volcanics.||||||
23819|Mount Halfway Volcanics|43089|5|Briefly described|Map Legend|||of Mount Hope Group||||||
23819|Mount Halfway Volcanics|69511|4|Described|p1, p3, p5-13, p18, p22, p44, p48|Late Silurian|Late Silurian|Barron et al. (1982). Most widespread Formation in the Group. Up to ~2km thick. Youngs to the S. Referred to as "The Peaks Porphyry" by MacRae (1987, 1989). The inference (MacRae, 1989) that it is co-magmatic with the Gilgunnia Granite, to which it is chemically and petrographically related (Blevin and Jones, 2004), is confirmed by this age determination.|422.8 +/- 2.6 Ma (SHRIMP U-Pb zircon).|Mount Hope Group.||Conformably overlies Coando Volcanics. Overlies Thule Granite (inferred). Is overlain conformably by Goona Volcanics. Interfingers with Amphitheatre Group.|S-type. Includes quartz-feldspar-phyric volcaniclastic rhyolite.|
23819|Mount Halfway Volcanics|70751|5|Briefly described|p5, p8, p10, p17-p19|Late Silurian|Late Silurian|The most areally extensive unit of the Mount Hope Group. See also p25, p27-p28, p30, p38.|422.8 +/- 2.6 Ma (SHRIMP, Chisholm et al, 2014)|Mount Hope Group|||Rhyolitic and dacitic volcanic rocks in addition to volcaniclastic rocks which include pumice breccias and peperites.|
23819|Mount Halfway Volcanics|70876|5|Briefly described|p1, p17, p76|Devonian|Silurian|Cobar Basin. S-type geochemistry.|422.8 +/- 2.6 Ma (Chisholm et al., 2014a)|||||
23819|Mount Halfway Volcanics|70950|5|Briefly described|p1029,1032,1033,1035, 1038, 1047|||Geological province: Central Lachlan Orogen. Detailed mineralisation analysis provided. Also shown as Mount Halfway Group p1035, fig 3.||Unit of Mount Hope Group.|||Crystal lithic tuff, felsic volcanics, quartz feldspar porphyry, tuffaceous sedimentary rocks.|
23819|Mount Halfway Volcanics|71039|6|Mentioned|p25|||||||||
23819|Mount Halfway Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|Lithology continued: Volcaniclastic facies include vitric crystal, sandstone, siltstone, mudstone, pumice breccia and rare peperite.||Mount Hope Group.|||Medium-grained, crystal-rich plagioclase, quartz +/- K-feldspar rhyolitic/dacitic lava with microspherulitic/poikilitic to perlitic matrix. Vesicular to amygdular variants, locally well-developed columnar jointing and flow foliation. See Comments.|
23819|Mount Halfway Volcanics|72908|5|Briefly described|p3, p6-7 Tb.1, p11-13, p25, p30|Lochkovian|Late Silurian|Simpson (2014) (see also Downes, Blevin et al., 2016) proposed that the stratigraphy of the Mount Hope Group be simplified, with the Ambone, Regina, Goona and part of the Coando Volcanics being grouped into the Mount Halfway Volcanics. Hosts the Great Central, BMW prospect, and MD 2-Siegals deposits.|422.8+/-2.6 Ma, 418.7+/-3.1 Ma U-Pb SHRIMP zircon|Mount Hope Group|||Includes sheared and altered felsic volcaniclastic rocks, altered felsic volcanic rocks.|
23819|Mount Halfway Volcanics|72951|5|Briefly described|p1013, 1015-1016, 1021|Pridoli|Ludlow|Lachlan Orogen. Albury-Bega Terrane. S-type. SHRIMP U-Pb zircon isotope analyses from Chisholm et al. (2014). eHf = -5.9 +/- 1.4, and d18O = 9.78 +/- 0.23.|422.8 +/- 2.6 Ma||||Porphyritic quartz-feldspar rhyolite.|
23819|Mount Halfway Volcanics|73578|6|Mentioned|p7, p14, p21|Pridoli|Ludfordian|Age of 422.8 +/- 2.6 Ma reported by Chisholm et al. (2014).|422.8 +/- 2.6 Ma|||||
70240|Mount Hannibal Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Grey, medium-grained, massive, equigranular, biotite-hornblende granite; weakly porphyritic at margins. High to very high magnetic susceptibility.||||||
70240|Mount Hannibal Granite|68592|2|Defined|p1639-41|Early Devonian|Early Devonian|New name, after Mount Hannibal property. Not previously distinguished from undifferentiated Bindook Group. Mapped and described, but not named, by Erickson (1986). Distribution, type locality and geophysical properties described. Age from intrusive relationships and mineralogical similarities.||Unit in Arthursleigh Suite.||Intrudes Bindook Group.|Uniform internal composition. Grey, medium-grained (1-5mm), equigranular, massive, biotite-hornblende granite. I-type.|
70240|Mount Hannibal Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dah. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Arthursleigh Suite|||Grey, medium-grained, massive, equigranular biotite hornblende granite. Weakly porphyritic at margins and has a high magnetic susceptibility.|
70240|Mount Hannibal Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Arthursleigh Suite|||Grey, medium-grained, massive, equigranular biotite hornblende granite. Weakly porphyritic at margins and has a high magnetic susceptibility.|
70502|Mount Helen Rhyodacite Member|62095|2|Defined|p277 Appdx.|Late Carboniferous|Late Carboniferous|Of the Currabubula Formation. Grey to purple rhyodacite lava. Thickness at type locaiity: 20m. In the Werrie block/Tamworth Belt.  See also Plate 1.  Mount is Mt in text.||||||31-JAN-08
37913|Mount Hook Rhyolite Member|24605|2|Defined|p931, p952 App.1|Namurian|Namurian|Of the Rocky Creek Conglomerate. Thickness in type section: 45m. Geological Province: New England Orogen. Mount is Mt. in text.||||||
37913|Mount Hook Rhyolite Member|61214|5|Briefly described|p170, p171 Fig. 1|Namurian|Namurian|Of Rocky Creek Conglomerate. Mount is Mt in text. Geological Province: Darthula Block. Presented as only Mt Hook in text of Fig. 2.||||||
25281|Mount Hope Group|22508|6|Mentioned|p7|||In the Lachlan Fold Belt.||||||27-OCT-08
25281|Mount Hope Group|22768|6|Mentioned|p170-71|||||||||
25281|Mount Hope Group|22857|5|Briefly described|p170, p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Cobar Supergroup. Complex volcanics and sedimentary sequence. See also p442 App.1 Tb.A1.6.||||||
25281|Mount Hope Group|22887|3|Fully described|p21, Fig.4 p11|Early Devonian|Early Devonian|||||||
25281|Mount Hope Group|23048|6|Mentioned|p13|||||||||
25281|Mount Hope Group|23214|6|Mentioned|p360|||||||||
25281|Mount Hope Group|23252|5|Briefly described|Map Legend|||Of The Hillston Volcanic Complex..||||||03-JUN-08
25281|Mount Hope Group|37772|4|Described|p1|||||||||
25281|Mount Hope Group|40269|4|Described|p144|||||||||
25281|Mount Hope Group|40913|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
25281|Mount Hope Group|41126|2|Defined|p24|Early Devonian|Early Devonian|||||||
25281|Mount Hope Group|41394|6|Mentioned|p10|||See also p95.||||||27-OCT-08
25281|Mount Hope Group|41528|2|Defined|p98|Early Devonian||||||||
25281|Mount Hope Group|41529|6|Mentioned|Map legend|Lochkovian||||||||
25281|Mount Hope Group|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
25281|Mount Hope Group|41821|3|Fully described|p22|Early Devonian||||||||
25281|Mount Hope Group|42144|5|Briefly described|p604|||||||||
25281|Mount Hope Group|42408|6|Mentioned|p415|||||||||
25281|Mount Hope Group|42521|5|Briefly described|p15, Figs|||||||||
25281|Mount Hope Group|42566|5|Briefly described|Fig.5 P11|||||||||
25281|Mount Hope Group|43089|5|Briefly described|Map Legend|||Of Cobar Supergroup.||||||27-OCT-08
25281|Mount Hope Group|43263|6|Mentioned|Map Legend||Early Devonian|Written as Mt Hope Group.||||||27-OCT-08
25281|Mount Hope Group|61964|6|Mentioned|p98, p104|Early Devonian|Early Devonian|On the MOUNT ALLEN 1:100k sheet. May overlie the Bootheragandra Group (Square Head Formation)?||||||27-OCT-08
25281|Mount Hope Group|62367|6|Mentioned|p5, p10|Early Devonian|Early Devonian|Of the Cobar Supergroup. Massive Early Devonian sulphide mineralisation is associated with this unit. Geological Province:  Mount Hope Trough.||||||02-JUN-06
25281|Mount Hope Group|63891|5|Briefly described|p237|||Includes Mount Hope Volcanics. Interpreted as overlying Thule Granite and underlying Broken Range Group. Mount is Mt in text.||||||27-OCT-08
25281|Mount Hope Group|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, App A-VI 3.||||||
25281|Mount Hope Group|69511|5|Briefly described|p1, p6-7, p14, p22|||Blevin and Jones (2004).||Cobar Supergroup.|Mount Halfway, Mount Kennan, Mount Hope, Volcanics.|Overlies Thule Granite (inferred).||
25281|Mount Hope Group|70751|4|Described|p1, p5-p6, p10-p13, p15|Devonian|Late Silurian|Cobar Superbasin, Mount Hope Trough. Present study shows that this unit is not contemporaneous with or comagmatic with the Ural Volcanics. See also p17, p19, p27-p28, p30-p31.||Cobar Supergroup|Includes the Mount Halfway Volcanics, Mount Kennan Volcanics, Double Peak Volcanics, Ambone Volcanics, Coando Volcanics, Goona Volcanics, Nombiginni Volcanics and Regina Volcanics.||S-type granitic rocks.|
25281|Mount Hope Group|70950|5|Briefly described|p1028-1029,1033-1035, 1036|Early Devonian|Late Silurian|Geological province: Mount Hope Trough, Central Lachlan Orogen. Felsic volcanic and derived sedimentary rocks. Detailed mineralisation analysis provided.|||Includes Mount Halfway Volcanics, Mount Kennan Volcanics, Double Peak Volcanics and Regina Volcanics||Crystal lithic tuff, felsic volcanics, quartz-feldspar porphyry, tuffaceous sedimentary rocks|
25281|Mount Hope Group|71039|6|Mentioned|p6, p20, p25-p26|Devonian|Silurian|||||||
25281|Mount Hope Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|Nombiginni, Mount Kennan, Mount Halfway, Volcanics.|||
25281|Mount Hope Group|72908|5|Briefly described|p3-4, p11-14|Lochkovian|Pridoli|Mount Hope Trough.|||Mount Halfway Volcanics, Mount Kennan Volcanics, Nombiginni Volcanics, Ambone Volcanics, Regina Volcanics, Goona Volcanics, Coando Volcanics, Double Peak Volcanics.|||
25281|Mount Hope Group|72958|6|Mentioned|p6, p8, p11, 61|Lochkovian|Pridoli|Cobar Basin. Nymagee area.|409 +/- 4 Ma LA-ICP-MS U-Pb zircon|||Partly[?] overlain by Buckambool Sandstone (Winduck Group). Intruded[?] by Gilgunnia Granite, Mount Allen Granite. Equivalent to Amphitheatre Group, Broken Range Group.|Includes felsic volcanic rocks.|
25281|Mount Hope Group|73174|6|Mentioned|p1039|Emsian[?]|Lochkovian|A-type. Crops out to the south of the main basin. Geochron are magmatic ages from Bull et al. (2008).|415 +/- 5 Ma, 409 +/- 4 Ma LA-ICP-MS|||||
25281|Mount Hope Group|73578|6|Mentioned|p2|||Cobar Basin.||||||
38240|Mount Hutton tuff|23717|6|Mentioned|p123 Tb.4|||Mount is Mt. in text.||||||
38240|Mount Hutton tuff|62033|5|Briefly described|p25 (Table)|||Of the Boolaroo Formation (Newcastle Coal Measures). Overlies Lower Pilot seam; overlain by Upper Pilot seam. Geological Province: Sydney Basin. Informal name. Mount is Mt in text.||||||14-MAR-07
38269|Mount Jonblee Leucomonzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Includes the Petries Sugarloaf mass.  Medium- to coarse-grained, saccharoidal, pale pink  to buff leucomonzogranite; includes buff leucomonzogranite spotted with occasional biotite flakes.   An I-type granitoid.||||||20-DEC-04
38269|Mount Jonblee Leucomonzogranite|23812|5|Briefly described|p19 Tb.2, p101|Early Triassic|Early Triassic|Age: 242Ma (Rb-Sr).||||||
38269|Mount Jonblee Leucomonzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca. 243 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38269|Mount Jonblee Leucomonzogranite|69639|4|Described|p1, p5, p8, p50-p55|Lopingian|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described. See also p68, p80, p221, p236.|254.6 +/- 1.5 Ma (SHRIMP)|Bolivia Range Suite||Intrudes the Wandsworth Volcanic Group and the Bungulla Monzogranite. Intruded by (inferred) the Cottesbrook Monzogranite.|Pink, equigranular to coarse-grained, porphyritic leucoadamellite.|
38269|Mount Jonblee Leucomonzogranite|70217|5|Briefly described|p74 tbl 14.1|Changhsingian|Wuchiapingian|New England Orogen.|254.6 +/- 1.5 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
38269|Mount Jonblee Leucomonzogranite|71628|4|Described|p8:80; p11: 9-11, 16; p14: 1, 8, 12-15|||See also p14: 28, 33; p15: 9, 25. Henley et al. (2001); Barnes (unpubl. 1987). Incorporates Mt Jonblee Leucoadamellite and Petries Sugarloaf Leucoadamellite of Brunker and Chesnut (1976). Named after a local prominent hill. Occurs as two elongate plutons, ~20 km S of Tenterfield and ~5 km and 11 km E of Bolivia. Geochemistry described. Is associated with Mo-W-Bi +/- base metals, Au, Ag mineralisation (briefly described). RELATED UNITS (continued): Is also partly bound (?intruded) by Cottesbrook and Mount Mitchell Monzogranites and Kingsgate Syenogranite.|254.6 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Kingsgate Suite.||Intrudes Wandsworth Volcanic Group, Sandy Flat Leucomonzogranite and Bungulla Monzogranite. Is partly bound by Emmaville Volcanics. See COMMENTS for more.|Pale pink to buff, medium- to coarse-grained, equigranular, saccharoidal, biotite leucomonzogranite, less commonly leucosyenogranite; finer-grained saccharoidal, inequigranular and microgranitic marginal variant. I-type.|
77135|Mount Kelly Granite|68823|5|Briefly described|p376 Fig.3, p394|Emsian|Lochkovian|Within the Louth-Eumarra Shear Zone. Inferred magmatic SHRIMP zircon age.|408.8 +/- 2.4 Ma (Black 2006)|||||
77135|Mount Kelly Granite|69002|6|Mentioned|p12|Pragian|Pragian||c. 409, U-Pb SHRIMP|||||
77135|Mount Kelly Granite|69635|5|Briefly described|p134, 136|Early Devonian|Early Devonian||408.8+/-2.4 Ma (Black, 2006)|Of Tarcoon Suite. ||||
77135|Mount Kelly Granite|70210|5|Briefly described|p1, p9, p38, p40-41|Early Devonian|Late Silurian|Cobar-Bourke district.|408.8 +/- 2.4 Ma.|||||
77135|Mount Kelly Granite|70602|6|Mentioned|p67 Fig 3,72|Early Devonian|Silurian|Age inferred from Tarcoon Plutonic Complex Granitoids. Aeromagnetic map data given.||Tarcoon Plutonic Complex||||
77135|Mount Kelly Granite|71345|2|Defined|p4,14-16,18|Early Devonian|Early Devonian|Type location: Lat -30.2049 Long 146.8881; GR489224 6658510. Named for Mount Kelly (GR488846 6654971). Described by Brunker (1969) from tors of biotite-bearing leucocratic granite near Moorwari homestead. Referred to informally as Mount Kelly granite by Proksch (1982), Black (2006), Blevin (2011) and Hegarty (2011). Exposure is restricted to approximately 4 x 2 km including Mount Kelly and the type locality. Exposed as whalebacks, tors and low out outcrop at Mount Kelly and along the Gongolgon-Brewarrina road (Blevin 2011). Magnetic anomaly is a ellipsoid shape 11km E-W and 5Km N-S. Subdued magnetic anomaly, suggesting a lower magnetic signature than granites of the Tarcoon Suite to the west or thicker floodplain cover. Broadly similar geochemical, petrographical and geophysical signatures to Tarcoon Suite, but is ~9my younger. Similar in age and geochemistry to the more fractionated Gongolgon Granite (~12km to the south). Geochemistry: I-type, unfractionated, moderately-oxidised granite (Blevin 2011). Black (2006) reported SHRIMP U-Pb magmatic age of 408.8+\-2.4 Ma|408.8+\-2.4 Ma (SHIRMP U-Pb; magmatic)||||Medium grained, equigranular grey/pale pink syenogranite, with dark quartz, grey plagioclase, very pale pink alkali feldspar and biotite.|02-DEC-19
77135|Mount Kelly Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: horseshoe-shaped area of moderate magnetic intensity with irregular texture that corresponds to an area of low gravity values.|408.8 +/- 2.4 Ma.|Tarcoon Plutonic Complex.|||Medium-grained, equigranular syenogranite, aplite.|
77135|Mount Kelly Granite|72951|5|Briefly described|p1013, 1018, 1022-1023, 1027, 1030|Pragian|Lochkovian|Lachlan Orogen. Hermidale Terrane. I-type. SHRIMP U-Pb zircon isotope analyses from Black (2006). eHf = 8.5 +/- 0.5, and d18O = 5.52 +/- 0.16. Sourced from Macquarie Arc-like material.|408.9 +/- 2.4 Ma||||Granite.|
28308|Mount Kennan Volcanics|22508|6|Mentioned|p4|||Lachlan Fold Belt||||||
28308|Mount Kennan Volcanics|22857|4|Described|p442 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Mount Hope Group. Rhyolite lavas and pyroclastics enbedded with arenite and siltstone. Max. thickness: 1000m. Geological Province: Mount Hope Trough (Darling Basin).||||||
28308|Mount Kennan Volcanics|37772|6|Mentioned|Fig.2|||||||||
28308|Mount Kennan Volcanics|40269|4|Described|p144|||||||||
28308|Mount Kennan Volcanics|40913|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
28308|Mount Kennan Volcanics|41126|2|Defined|p25|early Lochkovian|early Lochkovian|||||||
28308|Mount Kennan Volcanics|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
28308|Mount Kennan Volcanics|41821|3|Fully described|p24|Early Devonian||||||||
28308|Mount Kennan Volcanics|42144|5|Briefly described|p605|||||||||
28308|Mount Kennan Volcanics|42313|6|Mentioned|p219|||||||||
28308|Mount Kennan Volcanics|42408|5|Briefly described|p415|||||||||
28308|Mount Kennan Volcanics|42521|5|Briefly described|p15, Figs|||||||||
28308|Mount Kennan Volcanics|42726|5|Briefly described|map legend|Early Devonian||Actually spelt Mt Kennan Volcanics.||||||
28308|Mount Kennan Volcanics|43089|5|Briefly described|Map Legend|||of Mount Hope Group||||||
28308|Mount Kennan Volcanics|61964|5|Briefly described|p80|Lochkovian|Lochkovian|A-type. To the north of CARGELLIGO 1:250k sheet area on MT ALLEN 1:100k.||||||
28308|Mount Kennan Volcanics|69511|5|Briefly described|p22|||Contains clasts of metasedimentary rock purportedly derived from the Thule Block [Granite].||Basal Mount Hope Group.||||
28308|Mount Kennan Volcanics|70751|5|Briefly described|p5, p11, p17, p19, p30|||||Mount Hope Group||Intruded by the Boolahbone Granite.||23-SEP-19
28308|Mount Kennan Volcanics|70950|6|Mentioned|p1029,1034,1036|||Geological province: Central Lachlan Orogen.||Unit of Mount Hope Group.|||Felsic volcaniclastic rocks, conglomerate, sandstone, slate, siltstone, breccia.|
28308|Mount Kennan Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|The lavas have micropoikilitic, microspherulitic, flow-banded matrix.||Mount Hope Group.|||Plagioclase phyric dacitic and quartz feldspar phyric rhyolitic lavas; intercalated with volcanic crystal-lithic breccia, sandstone, siltstone and other non-volcanic feldspathic litharenite to sublitharenite.|
28308|Mount Kennan Volcanics|72908|5|Briefly described|p3, p8 Tb.1, p14|||Hosts the Wagga Tank deposit.||Mount Hope Group|||Includes felsic volcanic rocks and siltstone-slate units.|
30853|Mount Knowles Group|22451|5|Briefly described|p23|||Mount is written Mt in text||||||
30853|Mount Knowles Group|22472|6|Mentioned|p47 Fig.6(e)|||Mount is written Mt in text||||||
30853|Mount Knowles Group|22529|6|Mentioned|1, 4 fig 2|Late Devonian|Late Devonian|||||||
30853|Mount Knowles Group|22857|5|Briefly described|p492 App.1 Tb.A1.7|Late Devonian|Late Devonian|Max. thickness: >1700m. Geological Province: Lambie Shelf.||||||
30853|Mount Knowles Group|23043|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
30853|Mount Knowles Group|23170|2|Defined|p238|Late Devonian|Late Devonian|of Lachlan Fold Belt.||||||
30853|Mount Knowles Group|24580|6|Mentioned|p828 Fig.1|||Mount is Mt. in text. Group is Gp in text. Geological Province: Eastern Lachlan Fold Belt.||||||
30853|Mount Knowles Group|67847|5|Briefly described|p60 fig 3.3.4|||Lambie Basin. Of the authors' proposed Kanimblan cycle. ||||||
30853|Mount Knowles Group|73299|6|Mentioned|p1096 Fig.3, p1101 Fig.6-7, p1106|Famennian|Frasnian|Capertree High. Locations in text include p1100 Fig.5.|||Buckaroo Conglomerate, Bumberra Formation, Lawsons Creek Shale, Derale Sandstone.|||
23823|Mount Leonard Formation|24423|5|Briefly described|p270|Late Permian|Late Permian|Contains megaspores described here.||||||
23823|Mount Leonard Formation|40805|2|Defined|p141|Permian|Permian|||||||
23823|Mount Leonard Formation|41010|6|Mentioned|p13|||||||||
23823|Mount Leonard Formation|42078|6|Mentioned|Table 1 P5|||||||||
23823|Mount Leonard Formation|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Jerrys Plains Subgroup.  Includes the Whybrow seam.||||||
23823|Mount Leonard Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Jerrys Plain Subgroup (Wittingham Coal Measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
23823|Mount Leonard Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. Generally <12 m thick. Contains the Whybrow seam.||Uppermost unit in Jerrys Plains Subgroup.||Overlies Althorpe Formation. Is overlain by Denman Formation.|Massive sandstone, conglomerate, interbedded thin coal seams.|
23823|Mount Leonard Formation|69683|6|Mentioned|p411 Fig.2, p415 Fig.3|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.||||
82590|Mount Lindesay Monzogranite|71628|4|Described|p1:15; p11: 4, 38; p12:11; p15: 2, 4|Middle Triassic|Early Triassic|See also p15: 35-36, 49, 52, 56-72, 75, 77, 82, 100, 106, 115; p16-3; p19: 20, 83, 163. New name, after the Mount Lindesay Highway. Occurs S of Undercliffe Falls Monzogranite. Extensive unit: covers ~550 km2. A composite unit, whose subunits do not qualify as Phases according to stratigraphic naming conventions (discussed); it is thus not assigned to any one Suite. See individual 'Phases' for geochemistry. RELATED UNITS (continued): Bounds the Bookookoorara  Monzogranite. Partially encloses (?is intruded by) Quartz Pot Creek and Boonoo Monzogranites and Donnellys Castle Leucomonzogranite. Is faulted against Rocky River Monzogranite and Surface Hill Leucomonzogranite. Abuts The Ridge, The Ram Swamp and Severn River Monzogranites, Thomkins Gully Monzogranite Phase, Ruby Creek Leucogranite, Mount Norman Leucomonzogranite.||Stanthorpe Complex.|Carrolls Creek, Thulimbah, Ropers Creek, Monzogranite Phases; Gosling Swamp, Basket Swamp, Leucomonzogranite Phases.|Intrudes Silverwood Group, Drake Volcanics, Gilgurry Mudstone, Wallangarra Volcanics, Undercliffe Falls, Bungulla, Jenners Monzogranites. See COMMENTS for more.|Composite unit comprising pale pink, texturally and compositionally heterogeneous biotite-(hornblende) monzogranite-syenogranite; leucocratic variants locally prevalent.|
82592|Mount Mackenzie Monzogranite|71628|3|Fully described|p11:11; p15: 2, 15-21|||Henley et al. (2001) after unpublished work by Barnes (1987). Originally the Mackenzie Adamellite of Shaw (1969) and later Mackenzie Leucoadamellite of Flinter (1982). Named after a prominent local topographic feature. The type locality is on the Woodside loop road, 6.5 km SW of Tenterfield (Shaw, 1964). Occurs several kms SW of Tenterfield as a c.15 x 11 km ovoid body. Crops out as pavements and large tors. The Nonnington Leucomonzogranite may be a marginal variant of this unit. Geochemistry described. Associated with ten small Mo-dominant deposits (listed), and has been quarried for dimension stone.|251.7 +/- 2.1 Ma (SHRIMP: Black, 2007).|Bolivia Range Suite.||Intrudes Wandsworth Volcanic Group.|Pinkish, coarse-grained, seriate to porphyritic hornblende-biotite leucocratic monzogranite. I-type.|
28804|Mount Manara Conglomerate|34071|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
28804|Mount Manara Conglomerate|43379|14|Not recorded|Map Legend||Late Devonian|Unit of Mulga Downs Group||||||
28804|Mount Manara Conglomerate|43438|14|Not recorded|Map Legend|||Upper Devonian unit of Mulga Downs Group||||||
78380|Mount Merrere Conglomerate|69002|6|Mentioned|p11, p15|Early Devonian|Early Devonian|Spelt as Mt Merrere Conglomerate in the text. Inferred to be a shallow water unit of the Cobar Supergroup, rather than part of the Girilambone Group, as inferred by Brunker (1968).||Of the Cobar Supergroup.|||Includes clasts of quartzite, chert and sandstone.|
78380|Mount Merrere Conglomerate|73174|6|Mentioned|p1045-1046|||Detrital spectra does not include the 470-460 Ma Macquarie Arc peak that is common in other Cobar Basin rocks.||||||
31612|Mount Misery Suite|42726|5|Briefly described|map legend||Silurian|||||||
38283|Mount Mitchell Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Of Moonbi Plutonic Suite.  Coarse-grained, porphyritic to equigranular, biotite-hornblende monzogranite and leucogranite.||||||20-DEC-04
38283|Mount Mitchell Monzogranite|23812|5|Briefly described|p21 Tb.2, p65|Early Triassic|Late Permian|Of Moonbi Plutonic Suite.||||||
38283|Mount Mitchell Monzogranite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Moonbi Suite. Monzogranite and leucogranite.||||||
38283|Mount Mitchell Monzogranite|68111|5|Briefly described|p968 Tb.1|Anisian|Olenekian||249 - 243 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38283|Mount Mitchell Monzogranite|69639|4|Described|p1, p5, p8-p14, p16, p218, p221|Lopingian|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described.|253.7 +/- 1.5 Ma (SHRIMP U-Pb)|Stanthorpe Supersuite||Intrudes the Wandsworth Volcanic Group. Intruded by the Kingsgate Leucogranite.|Medium- to coarse-grained adamellite with mafic clots.|
38283|Mount Mitchell Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Changhsingian|Changhsingian|New England Orogen.|253.7 +/- 1.5 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
38283|Mount Mitchell Monzogranite|71628|4|Described|p3:54; p7:1; p11: 1, 15-22; p14: 3-4|||See also p14: 6-9, 12, 22; p17-1; p19: 137-138, 140. Barnes (1987). Originally presented as Mt [sic] Mitchell Adamellite of Flinter et al. (1972). Included in the Moonbi Plutonic Suite by Shaw and Flood (1981). Probably named after the local Mount Mitchell State Forest. Similarities with Henry River Monzogranite. A large (up to 40 x 15 km) composite pluton. Crops out as knolls, tors, pavements and whalebacks. Petrology, mineralogy and geochemistry described in some detail. Is associated with Mo, Au and Ag mineralisation (prospects named). RELATED UNITS (continued): Abuts Wandsworth Volcanic Group, Kingsgate Syenogranite, Red Range Microleucogranite and Mount Jonblee Leucomonzogranite. Partly bounds Mount Jonblee Leucomonzogranite. Is faulted against Newton Boyd Granodiorite.|253.7 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Mount Mitchell Suite.|Bruisers Creek Granodiorite Phase.|Intrudes Coffs Harbour Association and Sara beds. Surrounds (?is intruded by) Glen Garry Microleucosyenogranite and Kingsgate Syenogranite. See COMMENTS for more.|Coarse-grained, porphyritic to equigranular, biotite-hornblende monzogranite; local mafic and leucocratic variants, including unmapped fragments of the Glen Garry Microleucosyenogranite. I-type.|
81948|Mount Naman Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|Includes the Bluff Mountain Trachyte Member, Spire Trachyte Member, Timor Rock Trachyte Member, Breadknife Trachyte Member, Uringery Trachyte Member and 2 unnamed subunits.||Pale orange-white, fine-grained porphyritic to equigranular trachydacite to rhyolite coherent and volcaniclastic rocks.|02-NOV-20
82597|Mount Norman Leucomonzogranite|71628|5|Briefly described|p12:11; p15: 34-35, 43-44, 52, 58,65-66|||See also p15: 74-77, 82, 88, 99, 103, 115. New name, after a local topographic feature. Covers ~205 km2 between Bald Rock to Mount Stirling. A resistant unit: crops out in various forms including huge domes and inselbergs. Geochemistry described; is geochemically assigned to the Amiens Suite. Is spatially associated with minor Sn and Ag mineralisation.||Stanthorpe Complex.||Intrudes Wallangarra Volcanics. Partially encloses Quartz Pot Creek Monzogranite. Abuts Amiens Leucomonzogranite, Ruby Creek Leucogranite and Mount Lindesay, Severn River, The Ram Swamp Monzogranites.|Pale pink to pale brown, or brown to reddish brown, medium- to coarse-grained (groundmass), strongly, coarsely porphyritic, biotite leucomonzogranite to leucosyenogranite. Locally contains mafic enclaves to ~15m. I-type.|
26055|Mount Ogilvie Formation|29942|3|Fully described|p11|||||||||
26055|Mount Ogilvie Formation|35767|6|Mentioned|p8|||||||||
26055|Mount Ogilvie Formation|37087|6|Mentioned|p197|||||||||
26055|Mount Ogilvie Formation|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26055|Mount Ogilvie Formation|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26055|Mount Ogilvie Formation|40166|6|Mentioned|Table 1|||||||||
26055|Mount Ogilvie Formation|40256|6|Mentioned|Fig.3|||Mention Fig.4||||||
26055|Mount Ogilvie Formation|40805|2|Defined|p139|Permian|Permian|||||||
26055|Mount Ogilvie Formation|41010|6|Mentioned|p13|||Mention Fig.2||||||
26055|Mount Ogilvie Formation|41054|6|Mentioned|Fig.3|||||||||
26055|Mount Ogilvie Formation|42078|6|Mentioned|Table 1 P5|||||||||
26055|Mount Ogilvie Formation|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Jerrys Plains Subgroup.  Includes the Saxonvale Member and Glen Munro and Woodlands Hill seams.||||||
26055|Mount Ogilvie Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Jerrys Plain Subgroup (Wittingham Coal Measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
26055|Mount Ogilvie Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. About 100 m thick. Includes Woodlands Hill seam at the base, and the Glen Munro seam.||Unit in Jerrys Plains Subgroup.||Overlies Milbrodale Formation. Is overlain by Malabar Formation.|Sandstone, siltstone, carbonaceous siltstone, minor claystone; two named coal seams.|
26055|Mount Ogilvie Formation|69683|6|Mentioned|p411 Fig.2, p415-419 Figs.3-4|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.|Includes Saxonvale Member.|||
73697|Mount Olive Diorite|63286|5|Briefly described|p300, p304|Llandovery|Late Ordovician|Mount is Mt in text. Age:445 to 432Ma of crystallisation. Consists of quartz, hornblende and plagioclase-phyric dorite.||||Overlies Coombing Formation.||25-MAY-22
73697|Mount Olive Diorite|67106|6|Mentioned|p681|||||||||
73697|Mount Olive Diorite|73154|6|Mentioned|p84|||See also Mount Olive diorite p79.||||||
34470|Mount Oxley Formation|22768|6|Mentioned|Fig16.6p165|||Shown as Mount Oxley F. : probably Fault rather than Formation; see also Fig 16.7 p167.||||||16-JUL-15
34470|Mount Oxley Formation|69635|5|Briefly described|p156, p139|||||||Transitionally overlies Moira Formation.|Includes sandstone.|
34470|Mount Oxley Formation|70602|6|Mentioned|p66, Fig 2|Devonian|Devonian|||Mulga Downs Group||||
34470|Mount Oxley Formation|72522|5|Briefly described|p18.|Late Devonian|Middle Devonian|||Mulga Downs Group||Unconformably overlies Booda Formation in Oxley Range.|Includes relatively flat-lying conglomerates and sandstones.|
24403|Mount Painter Volcanics|22768|6|Mentioned|p176|||||||||
24403|Mount Painter Volcanics|22857|4|Described|p176, p462 App.1 Tb.A1.6|Wenlockian|Wenlockian|Of the Hawkins Suite. Large dacitic ignimbrite. Max. thickness: >1km. Geological Province: Canberra-Yass Shelf. ||||||
24403|Mount Painter Volcanics|35325|4|Described|p483|||Chemical analysis P484||||||
24403|Mount Painter Volcanics|35326|6|Mentioned|p485|||Geochemistry||||||
24403|Mount Painter Volcanics|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24403|Mount Painter Volcanics|37728|4|Described|Table 2|||||||||
24403|Mount Painter Volcanics|37752|6|Mentioned|Fig.2|||||||||
24403|Mount Painter Volcanics|38035|6|Mentioned|p92|||||||||
24403|Mount Painter Volcanics|38664|5|Briefly described|p11|||||||||
24403|Mount Painter Volcanics|39947|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24403|Mount Painter Volcanics|39975|6|Mentioned|Fig.1|||||||||
24403|Mount Painter Volcanics|41356|4|Described|p16|||See also P49||||||
24403|Mount Painter Volcanics|42497|5|Briefly described|Map legend|Wenlockian|Wenlockian|Actually spelt Mt Painter Volcanics.||||||
24403|Mount Painter Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
24403|Mount Painter Volcanics|42727|5|Briefly described|map legend|Wenlock|Wenlock|Of Hawkins Volcanic Suite. Dacitic ignimbrite with lithic xenoliths and dacitic autoliths, tuff and ashstone. Under Yarralumla Formation and over Walker Volcanics; intruded by Federal Golf Course Tonalite. BMR map symbol: Smp. Geol. Prov: Canberra Block.||||||
24403|Mount Painter Volcanics|42820|2|Defined|p26|late Wenlock||of Hawkins Volcanic Suite. Age late Early Silurian (late Wenlock)||||||
24403|Mount Painter Volcanics|43158|4|Described|3,13|||||||||
24403|Mount Painter Volcanics|43159|4|Described|Fig.2p4,p3,p9.|||of Hawkins Suite.||||||
24403|Mount Painter Volcanics|43481|6|Mentioned|3|||||||||
24403|Mount Painter Volcanics|45147|6|Mentioned|M137|||||||||
24403|Mount Painter Volcanics|49043|5|Briefly described|p7|||Formerly Mount Painter Porphyry||||||
24403|Mount Painter Volcanics|49690|5|Briefly described|p18-19|Silurian|Silurian|S-type volcanics: contains accessory cordierite or garnet.||||Underlies the Deakin Volcanics||
24403|Mount Painter Volcanics|68592|6|Mentioned|p428, p443, p457|||Abell (1991) after Opik (1954, 1958). Equivalent to, but not yet formally included in, the Douro Group.||||||
31723|Mount Pleasant Basalt Member|13139|5|Briefly described|p3 Fig. 2, p10|Late Ordovician|Late Ordovician|Of the Weemalla Formation. Max. thickness: 300m. Geological Province: Eastern Molong Volcanic Belt. See also p9 Fig. 4.||||||17-JUL-08
31723|Mount Pleasant Basalt Member|22679|2|Defined|p 15|Ordovician|Ordovician|Cabonne Group. Replaces Mount Pleasant Andesite and Mount Pleasant Basalt||||||
31723|Mount Pleasant Basalt Member|22857|5|Briefly described|p426 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Weemalla Formation. Porphyritic trachybasalt, pillow lava.||||||
31723|Mount Pleasant Basalt Member|23214|2|Defined|p57|Darriwilian|Darriwilian|Formerly referred to as Mount Pleasant Andesite and Mount Pleasant Basalt. Of Cabonne Group. Entirely enclosed in the Weemalla Formation. Type locality at Pleasant Hill.||||||17-JUL-08
31723|Mount Pleasant Basalt Member|23334|6|Mentioned|3 Fig.2|||||||||
31723|Mount Pleasant Basalt Member|24268|4|Described|p1535|Early Ordovician|Late Cambrian|Age: 479.2 +/- 1.1 Ma (Ar/Ar). Geological Province: Lachlan Fold Belt||||||
31723|Mount Pleasant Basalt Member|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Weemalla Formation, Cabonne Group. Consists of prophyritic trachybasalt, pillow lava.||||||17-JUL-08
31723|Mount Pleasant Basalt Member|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Weemalla Formation (Cabonne Group). Porphyritic trachybasalt, pillow lava.||||||17-JUL-08
31723|Mount Pleasant Basalt Member|43782|5|Briefly described|Map Legend|Darriwilian|Darriwilian|Of Weemalla Formation, Cabonne Group.||||||17-JUL-08
31723|Mount Pleasant Basalt Member|60417|5|Briefly described|p156|||Of Forest Reefs Volcanics. Previously of Weemalla Formation.||||||
31723|Mount Pleasant Basalt Member|63283|5|Briefly described|p195 Fig. 2, p202, p208|Gisbornian|Gisbornian|Of the Forest Reefs Volcanics. Geological Province: Molong Volcanic Belt. Consists of pillowed high-K to shosonitic basalts.||||||
31723|Mount Pleasant Basalt Member|63284|6|Mentioned|p268|||Mount is Mt in text.||||||
31723|Mount Pleasant Basalt Member|63285|4|Described|p292 App. 1, p280|||Of Forest Reefs Volcanics. Thickness: 480m. Geological Province: Molong Volcanic Belt. Consists of plagioclase-clinopyroxene +/- olivine +/- apatite-phyric basaltic andesites. Found in the lower part of Forest Reefs Volcanics.||||||
31723|Mount Pleasant Basalt Member|63286|4|Described|p294 Fig. 1, p297-298, p301-302, p307|Eastonian|Gisbornian|Mount is Mt in text. Of the Forest Reefs Volcanics. Age of emplacement: inferred from early Darriwillian detrital zircons in Coombing Formation and poorly preserved Late Darriwillian to late Gisbornian graptolites in  overlying black mudstone. Consists of pillow and massive basalts. Unit occurs near the base of Forest Reefs Volcanics.See also p297-298.||||||07-FEB-11
31723|Mount Pleasant Basalt Member|63293|6|Mentioned|p469 Fig. 2|Gisbornian|Gisbornian|Of Forest Reefs Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
31723|Mount Pleasant Basalt Member|67322|5|Briefly described|p25; Fig.5|Sandbian|Sandbian|Previously of the Weemalla Formation by Wyborn (in Pogson and Watkins 1998), but as noted by Percival and Glen (2007), based on stratigraphic revisions by Zhen and Percival (2004b), the Weemalla Formation is not present in the Forest Reefs area east of the Wongalong Fault. Age is determined from p20 Fig.5 (Strat. column). Occurs in the Forest Reefs-Junction Reefs region.||Of the Forest Reefs Volcanics.||||22-FEB-18
31723|Mount Pleasant Basalt Member|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 2 volcanic units. Age: ranges from early Darriwilian (Da2) to latest Gisbornian. Molong Volcanic Belt.|c. 449-443 Ma|Weemalla Formation||||
31723|Mount Pleasant Basalt Member|73154|6|Mentioned|p77 Fig.3|Gisbornian|Gisbornian|Macquarie Arc, Phase 2. Molong Volcanic Belt.||Forest Reefs Volcanics||||
76985|Mount Poole Monzogranite|69801|4|Described|p3-p5, p129-133, p138|Devonian|Devonian|Eastern Lachlan orogen. Intersected in drillcore from  the Walz and McCloys mine in the Yambulla goldfield of far southeastern New South Wales. Previously assigned a Late Silurain to Early Devonian age. Associated with gold mineralisation during the Tabberabberan Orogeny. Sample locality, petrography, SHRIMP analyses and interpretation are detailed. |402.5 +/- 2.8 Ma (SHRIMP)|Wallagaraugh Suite|||Medium- to coarse-grained, equigranular granite featuring red alkali feldspar, red plagioclase, quartz and minor chloritised biotite.|
76985|Mount Poole Monzogranite|72528|5|Briefly described|p108.|Emsian|Emsian|Age is indistinguishable from the Whipstick Monzogranite c. 30km NE.|402.5+/-2.6 Ma|||||
26056|Mount Rivers Ignimbrite Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Micaceous sandstone; minor siltstone and chert; volcanic breccia, ignimbrite. Passes laterally into Guygallon Volcanic Member. Max. thickness: 71m. Geological Province: Tamworth Forearc Basin.||||||09-MAR-06
26056|Mount Rivers Ignimbrite Member|31228|2|Defined|p78|Carboniferous|Carboniferous|||||||
26056|Mount Rivers Ignimbrite Member|36528|6|Mentioned|p178|||||||||
26056|Mount Rivers Ignimbrite Member|43576|6|Mentioned|p351|||||||||
26056|Mount Rivers Ignimbrite Member|44244|5|Briefly described|p40, p81|Visean|Visean|Of the Flagstaff Fromation.  Geological Province: Gresford Block.  Type section in text.||||||25-AUG-04
26056|Mount Rivers Ignimbrite Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Flagstaff Formation. Brown to purple dacitic ignimbrite with interbedded volcanic breccia, sandstone, siltstone and chert. Geological Province: Gresford Block||||||
26056|Mount Rivers Ignimbrite Member|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Gresford Block.  Of the Flagstaff Formation.||||||
30984|Mount Royal Formation|22519|6|Mentioned|p6|||Mount is written Mt. in text||||||
30984|Mount Royal Formation|22831|2|Defined|p 16||Lancefieldian|||||||
30984|Mount Royal Formation|22857|5|Briefly described|p414 App. 1 Tb. A1.5|Ordovician||Of the Tottenham Subgroup (Girilambone Group). Basic schist with pods of banded magnetite quartzite. Geological Province: Girilambone Slope and Basin.||||||
30984|Mount Royal Formation|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
30984|Mount Royal Formation|43441|3|Fully described|p7|||Age: ?Early Ordovician||||||08-JAN-10
30984|Mount Royal Formation|44160|5|Briefly described|Map Legend||Lancefieldian|||||||
30984|Mount Royal Formation|67322|5|Briefly described|p20|Darriwilian|Tremadocian|Defined by Sherwin (1996) based on underground sections and drill core examined by Suppel (1977). Age assumed to Tottenham Subgroup. Moderately strongly metamorphosed and unfossiliferous. Occurs in the Condobolin - West Wyalong region.||Of the Tottenham Subgroup||||22-FEB-18
69821|Mount Russell Volcanics|63347|2|Defined|p5 Fig. 2, p28, p6|Early Miocene|Late Oligocene|Of Delungra Volc.Suite.Thick: 200m (inferred).Uconform.over Warialda Trough units; conform.under Inverell Volcs. Age:24-19Ma.Qtz-bearing tholeiitic basalt; dolerite (lavas and plugs) + minor volcaniclastic deposits, clayst. + rare diamond-bearing gravels.||||||10-DEC-07
69821|Mount Russell Volcanics|73581|5|Briefly described|p14|Early Miocene|Late Oligocene|Dominates the Delungra Volcanic Suite. Strongly weathered in many cases, forming rich soil profiles and bauxite deposits.|22.6+/-0.5 Ma K-Ar|Delungra Volcanic Suite||Conformably underlies Inverell Volcanics|Quartz-bearing tholeiitic basalt along with some volcaniclastic units and minor plugs.|
34614|Mount Susannah Conglomerate|22831|3|Fully described|p 38|||||||||
34614|Mount Susannah Conglomerate|23522|5|Briefly described|p253|Devonian|Devonian|||||||
34614|Mount Susannah Conglomerate|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
34614|Mount Susannah Conglomerate|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Kopyje Group.|||Coarse lithic conglomerate and minor coarse-grained lithic sandstone.|
34614|Mount Susannah Conglomerate|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Cobar Supergroup||Partly overlain by Majuba Volcanics, Mineral Hill Volcanics and Talingaboolba Formation.||
69972|Mount Terrible Volcanic Complex|61801|5|Briefly described|p403-406|||U-Pb zircon dating of 18 grains assumed to have been from the Mount Terrible Volcanic Complex, and appear to be from a simple igneous source produced two age groupings: 300+/-8 Ma and 337+/- 9 Ma.|300+/-8 Ma U-Pb SHRIMP.|||Werrie Basalt, Boggabri Volcanics correlated on geochemical similarity.||24-SEP-18
23836|Mount Thorley Formation|40805|2|Defined|p138|Permian|Permian|||||||
23836|Mount Thorley Formation|41010|6|Mentioned|p13|||||||||
23836|Mount Thorley Formation|42078|6|Mentioned|Table 1 P5|||||||||
23836|Mount Thorley Formation|42922|6|Mentioned|Fig.14|||actually spelt Mt Thorley Formation||||||
23836|Mount Thorley Formation|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Jerrys Plains Group.  Includes the Arrowfield, Bowfield and Warkworth seams.||||||25-AUG-04
23836|Mount Thorley Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Jerrys Plain Subgroup (Wittingham Coal Measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
23836|Mount Thorley Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. Includes the Warkworth, Bowfield and Arrowfield coal seams. About 100 m thick.||Unit in Jerrys Plains Subgroup.||Overlies Fairford Formation. Is overlain by Milbrodale Formation.|Sandstone, siltstone and coal seams.|
23836|Mount Thorley Formation|69683|6|Mentioned|p411 Fig.2, p415-419 Figs.3-4|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.||||
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.|
26059|Mount Walton Porphyry|42566|2|Defined|p97|Early Devonian|Early Devonian|||||||
26059|Mount Walton Porphyry|42568|5|Briefly described|Map legend|Pragian|Lochkovian|Reserved as Mount Walton.||||||
26059|Mount Walton Porphyry|43089|5|Briefly described|Map Legend|||||||||
26059|Mount Walton Porphyry|67416|6|Mentioned|p85, p91|||Temporally and chemically related to volcanics in the Canbelego-Mineral Hill Volcanic Belt. Contains fluorite.||||||
26059|Mount Walton Porphyry|70876|6|Mentioned|p76|||Lachlan Orogen.||||||
26059|Mount Walton Porphyry|71039|6|Mentioned|p26|Early Devonian|Early Devonian|I-type.||||Intrudes the Kopyje Group.||
26059|Mount Walton Porphyry|71693|5|Briefly described|Map legend.|Devonian|Devonian||||||I-type. Massive medium-grained crowded pink two-feldspar porphyry typically with accessory fluorite.|
27508|Mount York Claystone|22745|6|Mentioned|p130|||Sydney Basin.||||||
27508|Mount York Claystone|22857|5|Briefly described|p526 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Grose Subgroup (Narrabeen Group). Red-brown claystone. Max. thickness: 13m. Geological Province: Sydney Basin.||||||
27508|Mount York Claystone|23218|6|Mentioned|p15, 28|||||||||
27508|Mount York Claystone|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
27508|Mount York Claystone|29749|4|Described|p12|||||||||
27508|Mount York Claystone|31061|6|Mentioned|Table 1|||||||||
27508|Mount York Claystone|31373|4|Described|Table 2|||||||||
27508|Mount York Claystone|31725|6|Mentioned|p7|||||||||
27508|Mount York Claystone|31886|6|Mentioned|p394|||||||||
27508|Mount York Claystone|36042|6|Mentioned|p52|||||||||
27508|Mount York Claystone|37804|6|Mentioned|Table 1|||||||||
27508|Mount York Claystone|39293|4|Described|p147|||||||||
27508|Mount York Claystone|39308|6|Mentioned|p500|||||||||
27508|Mount York Claystone|42925|3|Fully described|p11|||of Grose Subgroup||||||
27508|Mount York Claystone|42926|4|Described|map legend||Early Triassic|||||||
27508|Mount York Claystone|45090|5|Briefly described|p203|||Refers Goldbery (1966) & Goodwin (1970)||||||
73979|Mount You You Suite|63748|5|Briefly described|p30|Early Triassic|Permian|Of Mount You You Supersuite. Includes Mount You You Granite.||||||07-FEB-11
73979|Mount You You Suite|68679|5|Briefly described|p454, p457-459|Permian|Late Carboniferous|Northern New England Batholith. Comprises several small stocks of leucogranite. Geochemistry described.|~298 Ma.|Stanthorpe Supersuite.|Mount You You, Jibbinbar, Treverton Granites.|||
73979|Mount You You Suite|71628|5|Briefly described|p5: 2, 7, 10|||Donchak et al. (2007) included this unit within the Mount You You Supersuite. Brown et al. (2014) placed this Suite in the Bullaganang Supersuite. In this study, this Suite is placed in the Mount Bullaganang Supersuite.||Mount Bullaganang Supersuite.|Jibbinbar Leucosyenogranite; Mount You You, Treverton Leucogranites.|||
31613|Mount Youngal Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
32249|Mount Youngal Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh5||||||
32249|Mount Youngal Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
32033|Mountain Creek Suite|22768|5|Briefly described|p178|||||||||
32033|Mountain Creek Suite|22857|5|Briefly described|p178|Early Devonian|Early Devonian|Geological Province: Canberra-Yass Shelf. ||||||
32033|Mountain Creek Suite|43158|4|Described|Fig1p2; p4,13|||||||||
32033|Mountain Creek Suite|43159|4|Described|p1,6|||||||||
82779|Mountain Home Granite|71628|5|Briefly described|p4: 9, 15, 47; p19: 135-137|||Genske et al. (2012). A blind pluton, inferred from geophysical modelling. Named after a local homestead. Located ~25 km WSW of Uralla.||Mountain Home Suite.||Intrudes (?the boundary between) Banalasta and Pringles Monzogranites (Bundarra Supesuite).|Felsic intrusive, not exposed at the surface. ?I-type granite.|
29589|Moura Formation|22857|4|Described|p454 App.1, Tb.A1.6|Pridolian|Pridolian|Of the Goonigal Group. Feldspathic-lithic arenite and interbedded shale, minor conglomerate. Geological Province: Cowra Trough.||||||
29589|Moura Formation|23214|3|Fully described|p155|Pridoli|Pridoli|Of Goonigal Group.  Previously Moura Beds. Consists of well-banded lithic sandstone with lesser intercalated shale, siltstone and minor conglomerate.||||||
29589|Moura Formation|23217|5|Briefly described|p4, p5|||Unconformably underlies Hervey Group.||||||08-MAR-06
29589|Moura Formation|24417|3|Fully described|p58||Late Silurian|Originally named "Moura Beds". Of Goonigal Group.  Overlies Kirribilli Formation.||||||
29589|Moura Formation|24580|5|Briefly described|p828|||Intruded by the Eugowra Suite. Geological Province: Eastern Lachlan Fold Belt. Correlated lithologically with the Pridoli Gooligal Group.||||||
29589|Moura Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
29589|Moura Formation|43782|5|Briefly described|Map Legend|Pridoli|Pridoli|of Goonigal Group.||||||
29589|Moura Formation|60008|5|Briefly described|Map legend|Devonian|Silurian|Sediments and/or volcanics.||||||08-JUL-04
29589|Moura Formation|60009|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Goonigal Group.||||||13-JUL-04
29589|Moura Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Goonigal Group||||
25736|Mouramba Group|22508|6|Mentioned|p5||Early Devonian|Lachlan Fold Belt||||||
25736|Mouramba Group|22768|5|Briefly described|p170|||||||||
25736|Mouramba Group|22857|5|Briefly described|p170, p438 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Cobar Supergroup. Interfingers with and is overlain by the lower Amphitheatre Group in Priory and Cobar Blocks. Max. thickness: 5km. Geological Province: Mouramba Shelf. ||||||
25736|Mouramba Group|23171|6|Mentioned|p15,22|||(MacRae 1987).||||||
25736|Mouramba Group|23173|4|Described|Map Legend|||||||||
25736|Mouramba Group|23734|5|Briefly described|p12 Fig. 1|||Parent: Nurri Group.  Sandstone and conglomerate.||||||
25736|Mouramba Group|41394|3|Fully described|p45|Early Devonian||||||||
25736|Mouramba Group|41395|6|Mentioned|Map legend|Lochkovian||||||||
25736|Mouramba Group|41528|1|Redefined|p47|Early Devonian||Mention p17.||||||20-JUN-19
25736|Mouramba Group|41529|6|Mentioned|Map legend|Lochkovian||||||||
25736|Mouramba Group|42144|6|Mentioned|p603|||||||||
25736|Mouramba Group|42521|5|Briefly described|p15 and Figs|||||||||
25736|Mouramba Group|42566|5|Briefly described|Fig.5 P11|||||||||
25736|Mouramba Group|43089|5|Briefly described|Map Legend|||of Cobar Supergroup||||||
25736|Mouramba Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
25736|Mouramba Group|65469|5|Briefly described|p16, p43, p52, p55 fig 3-19|Early Devonian|Late Silurian|Lachlan Orogen. Extensive sericite alteration occurs within this group.  See also p62, p67, p138, p139, p357, App A-VI 3.|||Includes the Roset Sandstone|||
25736|Mouramba Group|70751|5|Briefly described|p4-p6, p12, p15|Early Devonian|Late Silurian|Cobar Superbasin, Mouramba Shelf.||Cobar Supergroup|Includes the Burthong Formation, Roset Sandstone.|||
25736|Mouramba Group|70950|6|Mentioned|p1028-1029,1040, 1041|Early Devonian|Late Silurian|Geological province: Mouramba Shelf, Central Lachlan Orogen. Misspelt as Moramba Group on p1041.|||Includes Burthong Formation.|||
25736|Mouramba Group|71039|5|Briefly described|p6, p8, p13-p14, p17, p24, p26, p28|Devonian|Silurian||||Includes the Burthong Formation.|Intruded by the Erimeran Granite.|Arkosic sandstone and conglomerate overlain by fine to medium-grained sandstone.|10-MAR-23
25736|Mouramba Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|Burthong, Boothumble Formations.|||
25736|Mouramba Group|72908|6|Mentioned|p4-5, p17, p19|Early Devonian|Late Silurian|Mouramba Shelf.|||Burthong Formation|||
25736|Mouramba Group|72958|6|Mentioned|p6, p8, p11, p37|Lochkovian|Pridoli|Cobar Basin. Nymagee area. Intruded by the 415.0 +/- 3.2 Ma Nymagee felsic dyke swarm, which is comparable in age to the unnamed hornblende-phyric dacite sill, hosted within the Meryula Formation.||Cobar Supergroup|Roset Sandstone, Boothumble Formation, Fifteen Mile Tank Conglomerate Member, Whitlock Conglomerate Member, Kruge Conglomerate Member, Hathaway Conglomerate Member|Equivalent to Amphitheatre Group, Rast Group.||
25736|Mouramba Group|73578|6|Mentioned|p2|||Cobar Basin.||||||
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.|
26060|Mowbray Formation|22857|5|Briefly described|p508 App.1 Tb.A1.8|Visean|Visean|Of the Gilmore Volcanic Group. Lithic arenite and conglomerate, rhyolitic and dacitic ignimbrite and tuff. Disconformably overlain by Mount Johnstone Formation. Max. thickness: ~200m. Geological Province: Tamworth Forearc Basin.||||||09-MAR-06
26060|Mowbray Formation|24121|5|Briefly described|p4, p154. p159|Carboniferous|Carboniferous|Includes Breckin and Lambs Valley Ignimbrite Members.||||||25-AUG-22
26060|Mowbray Formation|31228|2|Defined|p82|Namurian|Namurian|||||||
26060|Mowbray Formation|42547|5|Briefly described|p31|||||||||
26060|Mowbray Formation|44244|2|Defined|p92, p40|Carboniferous|Carboniferous|Of the Gilmore Volcanic Gp.  Includes Breckin Ignimbrite and Lambs Valley Ignimbrite Members.  Conformably overlies Newtown Fm; disconformably underlies Mount Johnstone Fm. Max. thick: >198m.  Type section in text.  Geol. Prov: Gresford Block.||||||25-AUG-04
26060|Mowbray Formation|50147|5|Briefly described|Map legend|Visean|Visean|Of the Gilmore Volcanic Group.  Yellow to red lithic sandstone and conglomerate with interbedded rhyolitic and rhyodacitic ignimbrite and tuff.||||||
26060|Mowbray Formation|50268|5|Briefly described|Map Legend|Visean|Visean|Of the Gilmore Volcanic Group.  Geological Province: Rouchel and Gresford Blocks.  Includes: Lambs Valley Ignimbrite Member, Breckin Ignimbrite Member.||||||
26060|Mowbray Formation|61768|6|Mentioned|p83 Fig. 2, p86|||Includes; Breckin Ignimbrite and Lambs Valley Ignimbrite.||||||13-MAY-08
26060|Mowbray Formation|73487|6|Mentioned|p566, p574 Fig.8, p583|||||||||
73667|Mozart Chert|63278|5|Briefly described|p147 Fig. 2b, p156|Early Gisbornian|Late Darriwilian|Of the Triangle Formation (Murry and Stewart (2001)).Underlain by Gidyen Volcanic Member, overlain by Rockley Volcanics. Geological Province: Rockley Volcanic Belt, LFB. Age based on conodonts.||||||07-FEB-11
73667|Mozart Chert|63283|6|Mentioned|p195 Fig. 2|Late Ordovician|Middle Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||07-FEB-11
73667|Mozart Chert|63290|5|Briefly described|p396 Fig. 3|Gisbornian|Darriwilian|Overlain by Rockley Volcanics, underlain by Gidyen Volcanics. Geological Province: Rockley - Gulgong Volcanic Belt.||||||
73667|Mozart Chert|63293|6|Mentioned|p469 Fig. 2|Gisbornian|Darriwilian|Overlain by Rockley Volcanics, underlain by Gidyen Volcanics. Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
73667|Mozart Chert|67322|5|Briefly described|p17-18|Sandbian|Darriwilian|Albury-Bega Terrane. Originally defined by Murray and Stewart (2001) as a member of the Triangle Formation, but this has been reassigned to the Adaminaby Group due to its identical appearance and age compared to the Numeralla Chert and equivalent facies such as the Nattery Chert Member of the Abercrombie Formation. Occurs in the Oberon-Rockley region.||Of the Adaminaby Group||||22-FEB-18
73667|Mozart Chert|67847|5|Briefly described|p27||||||||Imbricated cherts.|
73667|Mozart Chert|68466|6|Mentioned|p66|||Oberon district.||||Correlates with the Nattery Chert Member (Abercrombie Formation).||
73667|Mozart Chert|68592|5|Briefly described|p371, p376, p397|||Rockley-Gulgong Volcanic Belt. Contains late Darriwilian to early Gisbornian conodont fauna.||Unit in Cabonne Group.||Is overlain by Rockley Volcanics.||
73667|Mozart Chert|69668|6|Mentioned|p931|||Oberon district.||||Correlates with Nattery Chert Member.||
73667|Mozart Chert|70684|6|Mentioned|p75|Late Ordovician|Middle Ordovician|Oberon district, Rockley-Gulgong Volcanic Belt.||||||
76152|Muckabunnya Formation|66623|1|Redefined|p36, pp192-195, pp205-208. |Middle Devonian|Early Devonian|Formerly Mootwingee Series (Andrews 1922), undifferentiated Mulga Downs Group (Rose 1974), part of Snake Cave Sandstone (Buckley 2000), Muckabunnya beds of Neef & Larsen (2002). Redefined in this study. Equivalent to much of Wana Karnu Group. Outcrops east of Koonenberry Fault as high strike ridges with local cliffs. 3000m thick. Abundant Skolithos in unit b.||Unit in Wana Karnu Group.||Unconformable over Copper Mine Range, Bunker Creek and Cupala Creek Formations. Overlain conformably locally by Menamurtee Sandstone; unconformably by Namur Sandstone, Ravendale and Eyre Formations.|Medium- to coarse-grained, poorly to well sorted, quartz-rich sandstone with local pebbly intervals; very minor shale; clay and mica rich matrix common; planar cross-beds, sporadic ripples; some rutilated and fibrolitic detrital quartz.|
76152|Muckabunnya Formation|70651|5|Briefly described|Map Legend|Devonian|Devonian|||Wana Karnu Group|Includes unnamed units h, c and b.||Unit h: Coarse- and fine- laminated sandstone with pebble lags. Unit c: Pebbly, medium-grained and coarse-grained sandstone. Unit b: finely laminated quartzose sandstone.|
73681|Muddy Lake Diorite|63278|5|Briefly described|p148|Ordovician|Ordovician|Intrudes a part of Cowal Igneous Complex. Age: 456+/-5Ma (K-Ar, Perkins et al. 1995a).||||||24-AUG-12
73681|Muddy Lake Diorite|70178|5|Briefly described|p4 fig. 2, p8, p9, p10, p20 |Ordovician|Ordovician|Numerous gold deposits described occuring along margins. These deposits are often structurally controlled though some intrusion related and porphyritic deposits occur.|470 Ma- 456 Ma|Included in unnamed diorite and monzonite of Cowal Igneous Complex||Intrudes sediments of Cowal Igneous Complex.|Elongate, diorite sill intruded by and with mafic-intermediate (diorite) dykes, sills and stocks.  Veins of quartz-carbonate-pyrite-base metal, sericite-carbonate-pyrite and quartz-pyrite-calcite-chlorite along margins; quartz-sulfide breccias.|
73681|Muddy Lake Diorite|72495|5|Briefly described|p225|Darriwilian|Darriwilian|K-Ar date is derived from Perkins 1993, cited in Miles and Brooker, 1998.|456 +/- 5 Ma (Hornblende K-Ar)|||Intrudes the Cowal Igneous Complex.||05-APR-20
28823|Mudgee River Granite|22857|6|Mentioned|p231|Late Carboniferous|Early Carboniferous|||||||
28823|Mudgee River Granite|22863|6|Mentioned|p231|||||||||
28823|Mudgee River Granite|23043|5|Briefly described|Map Legend|Namurian|Visean|||||||
28823|Mudgee River Granite|23170|4|Described|p266|Carboniferous|Carboniferous|of Lachlan Fold Belt.||||||
28823|Mudgee River Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
28823|Mudgee River Granite|32045|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
28823|Mudgee River Granite|32046|6|Mentioned|p142|||See also P143||||||
28823|Mudgee River Granite|32047|6|Mentioned|p16|||||||||
28823|Mudgee River Granite|32485|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
28823|Mudgee River Granite|42726|5|Briefly described|map legend|Carboniferous||7.  Of the Gulgong Suite (Bathurst Supersuite).||||||07-FEB-05
28823|Mudgee River Granite|43476|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
32286|Mudgingar Granite|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Batholith.||||||
32286|Mudgingar Granite|23170|3|Fully described|p222|Early Devonian|Early Devonian|of Yeoval Batholith.||||||
32286|Mudgingar Granite|68003|5|Briefly described|p24 Fig.3-e, p142. |Pragian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion. Part of the Yeoval Batholith.|||||Medium- to coarse-grained pink granite; includes aplitic dykes.|
24407|Mugga Mugga Porphyry Member|22857|4|Described|p462 App.1 Tb.A1.6|Silurian|Silurian|Of Deakin Volcanics. Compact blue and mauve-grey porphyritic rhyodacite, volcaniclastic and waterlaid epiclastic tuff, tuffaceous shale. Age: 414+/-9Ma (Rb/Sr). Max. thickness: 300m. ||||||
24407|Mugga Mugga Porphyry Member|36633|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
24407|Mugga Mugga Porphyry Member|37728|4|Described|Table 2|||||||||
24407|Mugga Mugga Porphyry Member|38664|5|Briefly described|p12|||||||||
24407|Mugga Mugga Porphyry Member|42727|5|Briefly described|map legend|Ludlow|Ludlow|Of Deakin Volcanics. Rhyodacite lava. BMR map symbol: Sum. Geol. Prov: Canberra Block.||||||
24407|Mugga Mugga Porphyry Member|42820|2|Defined|p33|early Ludlow||of Deakin Volcanics. Age early Ludlovian||||||
24407|Mugga Mugga Porphyry Member|43159|5|Briefly described|Fig.2p4,p6,p10||Late Silurian|of Deakin Volcanics, Laidlaw Suite.||||||
25303|Mulbring Siltstone|22601|2|Defined|412, 413, 417, 419|Permian|Permian|Geol province Sydney Basin. Underlying unit Branxton Formation where Muree Formation is not separately recognised||||||19-JAN-17
25303|Mulbring Siltstone|22610|4|Described|Fig 5||Late Permian|Age 264.1 +/- 2.2Ma,  Maximum Thickness 330m||||||
25303|Mulbring Siltstone|22663|5|Briefly described|NSW97 - 1 Fig.2||Late Permian|||||||01-MAR-10
25303|Mulbring Siltstone|22857|4|Described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Maitland Group. Siltstone, claystone, minor fine-grained sandstone. Max. thickness: 393m. Geological Province: Sydney Basin.||||||
25303|Mulbring Siltstone|22969|4|Described|p 21, Fig 2.2||Late Permian|Maitland Group. Max. thickness: >393 m.||||||
25303|Mulbring Siltstone|22970|5|Briefly described|Plate 6|Late Permian||||||||
25303|Mulbring Siltstone|23540|5|Briefly described|p 417|||Also see Fig 3 p 420||||||
25303|Mulbring Siltstone|24079|5|Briefly described|p433 Fig.6|Permian|Permian|Of Maitland Group. Geological Province: Sydney Basin.||||||
25303|Mulbring Siltstone|24121|5|Briefly described|p4, p30|Permian|Permian|||||||25-AUG-22
25303|Mulbring Siltstone|30340|6|Mentioned|p2529|||||||||
25303|Mulbring Siltstone|30341|5|Briefly described|p136|||Upper Permian age||||||
25303|Mulbring Siltstone|31124|5|Briefly described|Table 1|||Petrology. See also Fig. 1, 2 & P17.||||||
25303|Mulbring Siltstone|31125|6|Mentioned|p16|||Refers geology||||||
25303|Mulbring Siltstone|31251|6|Mentioned|p73|||Refers Ludbrook (1956)||||||
25303|Mulbring Siltstone|31375|6|Mentioned|p4|||||||||
25303|Mulbring Siltstone|32266|6|Mentioned|p24|||||||||
25303|Mulbring Siltstone|32671|6|Mentioned|Map legend|Permian|Permian|||||||
25303|Mulbring Siltstone|32945|6|Mentioned|p83|||Permian||||||
25303|Mulbring Siltstone|33702|6|Mentioned|Fig.1|||||||||
25303|Mulbring Siltstone|33711|6|Mentioned|Table 2|||||||||
25303|Mulbring Siltstone|33867|4|Described|p6|||||||||
25303|Mulbring Siltstone|34043|6|Mentioned|p451|||||||||
25303|Mulbring Siltstone|34345|3|Fully described|p333|||Stratigraphic column Fig.5.10. Permian.||||||
25303|Mulbring Siltstone|34444|6|Mentioned|Map legend|Permian|Permian|||||||
25303|Mulbring Siltstone|34445|6|Mentioned|Fig.5.3|||||||||
25303|Mulbring Siltstone|34447|5|Briefly described|p319|||Fossils. See also Table 5.2||||||
25303|Mulbring Siltstone|34448|5|Briefly described|p432|||Permian||||||
25303|Mulbring Siltstone|34465|4|Described|Fig.5.10|||Strat. column||||||
25303|Mulbring Siltstone|34466|6|Mentioned|Fig.5.22|||||||||
25303|Mulbring Siltstone|34845|6|Mentioned|Fig.4|||||||||
25303|Mulbring Siltstone|35284|6|Mentioned|Fig.1|||||||||
25303|Mulbring Siltstone|36009|6|Mentioned|Table 1|||||||||
25303|Mulbring Siltstone|36042|6|Mentioned|Table 1|||||||||
25303|Mulbring Siltstone|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25303|Mulbring Siltstone|37082|6|Mentioned|p161|||||||||
25303|Mulbring Siltstone|37086|6|Mentioned|p185|||||||||
25303|Mulbring Siltstone|37087|6|Mentioned|p192|||||||||
25303|Mulbring Siltstone|37773|6|Mentioned|Fig.3|||||||||
25303|Mulbring Siltstone|37922|6|Mentioned|p483|||||||||
25303|Mulbring Siltstone|38614|6|Mentioned|p14|||||||||
25303|Mulbring Siltstone|38656|5|Briefly described|Fig.1.5.13|||P280||||||
25303|Mulbring Siltstone|39214|6|Mentioned|p29|||Permian marine||||||
25303|Mulbring Siltstone|39287|6|Mentioned|Fig.2.2|||See also Fig.2.5||||||
25303|Mulbring Siltstone|39288|4|Described|p64|||||||||
25303|Mulbring Siltstone|39292|6|Mentioned|p104|||||||||
25303|Mulbring Siltstone|39304|6|Mentioned|p366|||||||||
25303|Mulbring Siltstone|39307|6|Mentioned|p438|||||||||
25303|Mulbring Siltstone|39308|6|Mentioned|p491|||See also Fig.23.4||||||
25303|Mulbring Siltstone|39346|6|Mentioned|Map legend|Late Permian|Middle Permian|Middle to Late Permian||||||
25303|Mulbring Siltstone|39830|6|Mentioned|Map legend|Late Permian|Middle Permian|Middle to Late Permian||||||
25303|Mulbring Siltstone|40166|6|Mentioned|p346|||See also Fig.2||||||
25303|Mulbring Siltstone|40224|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
25303|Mulbring Siltstone|40256|6|Mentioned|p301|||||||||
25303|Mulbring Siltstone|40636|6|Mentioned|p43|||||||||
25303|Mulbring Siltstone|40872|6|Mentioned|p37|||||||||
25303|Mulbring Siltstone|41010|6|Mentioned|Fig.1|||||||||
25303|Mulbring Siltstone|41054|6|Mentioned|Fig.3|||||||||
25303|Mulbring Siltstone|41474|6|Mentioned|p59|||||||||
25303|Mulbring Siltstone|41514|6|Mentioned|p82|||||||||
25303|Mulbring Siltstone|41580|5|Briefly described|p7|||||||||
25303|Mulbring Siltstone|41604|6|Mentioned|p2|||||||||
25303|Mulbring Siltstone|41834|6|Mentioned|p590|||||||||
25303|Mulbring Siltstone|41902|5|Briefly described|p5 Table 1|||||||||
25303|Mulbring Siltstone|41903|6|Mentioned|Map legend|Late Permian||||||||
25303|Mulbring Siltstone|42214|6|Mentioned|p467|||||||||
25303|Mulbring Siltstone|42378|5|Briefly described|p19|||||||||
25303|Mulbring Siltstone|42780|6|Mentioned|Table 1 P417|||||||||
25303|Mulbring Siltstone|42916|5|Briefly described|Table 1|Late Permian|Middle Permian|||||||
25303|Mulbring Siltstone|42925|5|Briefly described|Table 1||Late Permian|||||||
25303|Mulbring Siltstone|43050|5|Briefly described|p12|||||||||
25303|Mulbring Siltstone|43194|5|Briefly described|p104, p128, p129 Tb. 8.3|Middle Permian|Middle Permian|Of Maitland Group, Hunter and Newcastle Coalfields, Sydney Basin. Correlative of Watermark Formation, Gunnedah Basin.||||||13-NOV-13
25303|Mulbring Siltstone|43257|5|Briefly described|Map Legend||Permian|Age Middle Permian. Of Maitland Group.||||||
25303|Mulbring Siltstone|43344|14|Not recorded|p84||Permian|||||||
25303|Mulbring Siltstone|43383|14|Not recorded|p20|||||||||
25303|Mulbring Siltstone|43440|14|Not recorded|p32,35,62,65,72,83,|||p90||||||
25303|Mulbring Siltstone|43447|14|Not recorded|p20,28,48|||Part of Maitland Group||||||
25303|Mulbring Siltstone|43451|14|Not recorded|Map Legend|||||||||
25303|Mulbring Siltstone|44244|4|Described|p233|Early Permian|Early Permian|Of the Maitland Group.  Overlies the Muree Sandstone.  Max. thickness: 330m.  Type section in text.  Geological Province: Sydney Basin.||||||25-AUG-04
25303|Mulbring Siltstone|45088|6|Mentioned|p59|||Permian||||||
25303|Mulbring Siltstone|45090|6|Mentioned|p26|||Isopach map P49||||||
25303|Mulbring Siltstone|50268|5|Briefly described|Map Legend|Tatarian|Kazanian|Geological Province: Sydney Basin.  Of the Maitland Group.  Overlies: Branxton Formation, Muree Sandstone.  Underlies: Saltwater Creek Formation.||||||
25303|Mulbring Siltstone|60281|4|Described|p9, p59|Late Permian|Late Permian|Of Maitland Gp.  Succession of grey siltstone and minor claystone.  Conformably overlies either Muree Fm. or Branxton Fm.; unconformably overlain by Narrabeen Gp. sediments. Overlain by Wittingham C.M. and Saltwater Creek Fm. Max. thick: 393m.||||||
25303|Mulbring Siltstone|61201|6|Mentioned|p7|||||||||
25303|Mulbring Siltstone|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Maitland Group. Geological Province: Sydney Basin||||||
25303|Mulbring Siltstone|61529|5|Briefly described|p853, p854 Fig. 1b|Late Permian|Late Permian|Of the Maitland Group. Overlain by Vane Subgroup (Wittingham Coal Measures); overlies Branxton Formation (Maitland Group). Geological Province: Sydney Basin.||||||
25303|Mulbring Siltstone|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||17-MAR-09
25303|Mulbring Siltstone|61770|6|Mentioned|p110|||||||||
25303|Mulbring Siltstone|63172|6|Mentioned|p307|||A NSW stratigraphic unit.||||||07-FEB-11
25303|Mulbring Siltstone|63832|5|Briefly described|p131 fig 2, p136|Roadian|Roadian|Hunter Valley, Of Sydney Basin. Seventh (P3) glaciation. Dominantly glaciomarine deposits.||Unit in Maitland Group.||||13-DEC-17
25303|Mulbring Siltstone|64631|5|Briefly described|p44 Fig.2, p49.|Roadian|Roadian|Sydney Basin. Distal glaciomarine deposits. Biostratigraphic age control at base?||Probably of Maitland Group||Is overlain by Tomago Coal Measures. Appears to be disconformable on Branxton Formation.||
25303|Mulbring Siltstone|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||Maitland Group.||Overlies Muree Sandstone. Is overlain by Tomago Coal Measures.||
25303|Mulbring Siltstone|68003|5|Briefly described|p38 Fig.3-j, p41, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Uppermost unit in Maitland Group.||Overlies Muree Sandstone. Is overlain by Vane Subgroup.|Fine-grained offshore sediments: siltstone, claystone, minor fine-grained sandstone.|
25303|Mulbring Siltstone|68004|5|Briefly described|p23 Table 1, P51|||Hunter and Newcastle Coalfields. About 300 m thick.||Upper unit in Maitland Group.||Overlies Muree Sandstone or Branxton Formation. Is overlain by Vane Subgroup and Tomago Coal Measures.|Mainly siltstone with subordinate claystone and thin sandy lenses.|
25303|Mulbring Siltstone|68493|5|Briefly described|p3 Fig.1, p5 Fig.2, p6|Lopingian|Lopingian|Sydney Basin. Marine shelf depositional environment. Up to 330 m thick at type section. Ice-rafted material present.|shown as ~260.0 Ma at base in fig2.|Of the Maitland Group.||Overlies the Muree Sandstone. Overlain by the Tomago Coal Measures.|Consists of relatively uniform sandy claystone, shale and cherty shale.|06-SEP-18
25303|Mulbring Siltstone|69297|6|Mentioned|p501, p502 fig 5.43, p503|Capitanian|Capitanian|Sydney Basin. Has good oil and gas source rock potential.||Maitland Group||Overlies the Muree Sandstone. Overlain by the Tomago Coal Measures.||
25303|Mulbring Siltstone|69683|6|Mentioned|p411 Fig.2|Late Permian|Middle Permian|||Unit in Maitland Group.||||
25303|Mulbring Siltstone|70661|6|Mentioned|p181|Capitanian|Capitanian|Hunter Valley (North Sydney Basin).|264.1 +/- 2.2 Ma (SHRIMP)|Maitland Group|||Equivalent to Berry Siltstone|
25303|Mulbring Siltstone|70791|5|Briefly described|p277|Guadalupian|Guadalupian|Hunter Coalfield.||Maitland Group.||||
25303|Mulbring Siltstone|70878|5|Briefly described|p712, p723|Permian|Permian|This age is a recalculation and re-analysis of the samples used by Roberts et al. (1996) for their age of 264.1 +/- 2.2 Ma. Calibration of palynological ages (D. ericianus Zone).|264.12 +/- 0.17 Ma (CA-IDTIMS).|||||
25303|Mulbring Siltstone|73304|5|Briefly described|p75-76|Capitanian|Capitanian|Sydney Basin, northern. Hunter Valley. Includes evidence of the P3 glacial episode. Age by interpolation between dates for the Jerrys Plains Sub-Group and Rowan Formation in the northern Sydney Basin.|c. 263 Ma|Maitland Group||||
25303|Mulbring Siltstone|73421|6|Mentioned|p18|Capitanian|Capitanian|Sydney Basin, northern. Previously correlated with Berry Siltstone based on sedimentary facies and marine faunas. Contains the Echinalosia runnegari Zone. Dated to 264.12+/-0.17 Ma by Laurie et al., (2016).|264.12+/-0.17 Ma|||||
25303|Mulbring Siltstone|73625|6|Mentioned|p2|Permian|Permian|Hunter and Newcastle coalfields, Sydney Basin.||||Overlies Muree Sandstone. Is overlain by Foybrook Formation (Wittingham Coal Measures) or lower Tomago Coal Measures.||
28825|Mulcatcha Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
28825|Mulcatcha Formation|22857|5|Briefly described|Tb 13.1 (insert p70-71), p398 Tb A1.3|Sturtian|Sturtian|Of the Yancowinna Subgroup (Torrowangee Group). Flaggy, quartzose sandstone with some lenticular boulder beds. Age: ~700Ma. Max. thickness: 850m. Geological Province: Adelaide Fold Belt. ||||||
28825|Mulcatcha Formation|30261|4|Described|Table 1|||Sturtian.||||||
28825|Mulcatcha Formation|33004|6|Mentioned|Plate 5|||Shown on photo 5||||||
28825|Mulcatcha Formation|34812|3|Fully described|p69|||||||||
28825|Mulcatcha Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
28825|Mulcatcha Formation|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
28825|Mulcatcha Formation|36733|6|Mentioned|Table 5|||||||||
28825|Mulcatcha Formation|37931|4|Described|p532|||||||||
28825|Mulcatcha Formation|38157|6|Mentioned|p261|||||||||
28825|Mulcatcha Formation|39214|6|Mentioned|Table 1|||||||||
28825|Mulcatcha Formation|41405|5|Briefly described|p204|||||||||
28825|Mulcatcha Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Yancowinna Subgroup.|[Includes Kantappa Quartzite Member].|||
28825|Mulcatcha Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Yancowinna Subgroup.|Includes Kantappa Quartzite Member.|Is overlain by Yangalla and Waukeroo Formations.|Flaggy, quartzose sandstone with lenticular boulder and arkosic sandstone beds.|07-SEP-15
29225|Mulculca Formation|6823|6|Mentioned|p205|Palaeoproterozoic|Palaeoproterozoic|||||Underlies the Thackaringa Group.||26-MAR-22
29225|Mulculca Formation|22553|5|Briefly described|fig2p77,p78|Proterozoic|Proterozoic|||||||
29225|Mulculca Formation|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
29225|Mulculca Formation|22771|6|Mentioned|Table12.2p45|||||||||
29225|Mulculca Formation|22857|4|Described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: 1.5km. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
29225|Mulculca Formation|22965|6|Mentioned|Fig 1||Statherian|||||||
29225|Mulculca Formation|23248|5|Briefly described|Fig2p169|||||||||
29225|Mulculca Formation|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|||||||
29225|Mulculca Formation|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
29225|Mulculca Formation|42537|6|Mentioned|Fig.2 P5|||||||||
29225|Mulculca Formation|42595|4|Described|p3, p5|||||||||
29225|Mulculca Formation|42897|2|Defined|p334|Proterozoic||see also Fig.3, p321.||||||29-MAY-07
29225|Mulculca Formation|43052|6|Mentioned|Fig.4.22|||||||||
29225|Mulculca Formation|43086|6|Mentioned|Fig.3|||||||||
29225|Mulculca Formation|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
29225|Mulculca Formation|43267|5|Briefly described|Map Legend||Paleoproterozoic|of Willyama Supergroup.||||||07-NOV-08
29225|Mulculca Formation|43270|5|Briefly described|Map Legend||Paleoproterozoic|of Willyama Supergroup.||||||07-NOV-08
29225|Mulculca Formation|43273|5|Briefly described|Map Legend||Paleoproterozoic|of Willyama Supergroup.||||||07-NOV-08
29225|Mulculca Formation|43572|6|Mentioned|p5|||||||||
29225|Mulculca Formation|46598|5|Briefly described|p302|||||||||
29225|Mulculca Formation|50045|5|Briefly described|p116 Fig. 3|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Thackaringa Group; underlain by Ednas Gneiss.||||||31-MAY-07
29225|Mulculca Formation|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Redan Suite. Geological Province: Broken Hill Block.||||||07-NOV-08
29225|Mulculca Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.  Geological Province: Broken Hill Block.||||||07-NOV-08
29225|Mulculca Formation|60485|5|Briefly described|p29|||Of the Thackaringa Group? Geological Province: Broken Hill Domain.||||||03-MAR-05
29225|Mulculca Formation|61606|5|Briefly described|p4 Fig.2|||||||||18-MAY-06
29225|Mulculca Formation|61735|5|Briefly described|p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Part of the Redan Block. See also p636 Fig. 2.||||||30-JUN-09
29225|Mulculca Formation|62536|5|Briefly described|p635-636|||Redan Block, Broken Hill area.||||||
29225|Mulculca Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
29225|Mulculca Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||||||19-DEC-21
29225|Mulculca Formation|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
29225|Mulculca Formation|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29225|Mulculca Formation|63519|5|Briefly described|p10 Fig. 3|||Geological Province: Redan Sub-block.||||||11-JUN-08
29225|Mulculca Formation|63866|5|Briefly described|p36|||Redan Subdomain of the Broken Hill Domain, Curnamona Province. ||Willyama Supergroup||Overlies the Redan Gneiss.||
29225|Mulculca Formation|64097|5|Briefly described|p304 Fig. 1, p309|Paleoproterozoic|Paleoproterozoic|Of the Rantyga Group (Willyama Supergroup). Overlies Ednas Gneiss; underlies Farmcote Gneiss. Geological province: Broken Hill Domain/Curnamona province.||||||07-FEB-11
29225|Mulculca Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Rantyga Group. Geological province: Broken Hill Domain.||||||07-FEB-11
29225|Mulculca Formation|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||07-FEB-11
29225|Mulculca Formation|66302|5|Briefly described|p36 Fig.9, p39, p41|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Rantyga Group||Overlies the Ednas Gneiss. Overlain by the Farmcote Gneiss.||
29225|Mulculca Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.||Rantyga Group.||||
29225|Mulculca Formation|70000|6|Mentioned|p34|Statherian|Statherian|||Unit in Rantyga Group.||||
29225|Mulculca Formation|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.||Overlies Ednas Gneiss. Is overlain by Lady Brassey Formation.|Abundant metasedimentary composite gneiss, variable sodic plagioclase-quartz-magnetite rock, quartz-albite-magnetite gneiss, minor quartz-magnetite rock common, minor basic gneiss, albite-hornblende-quartz rock.|
29225|Mulculca Formation|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Rantyga Group.||Overlies Ednas Gneiss.|Albite-quartz(+/- magnetite) rock, quartz-magnetite rock up-sequence; minor basic gneiss and albite-quartz-amphibole magnetite rock.|
29225|Mulculca Formation|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|~1710-1705 Ma|Willyama Supergroup.||Overlies Ednas Gneiss. Underlies Farmcote Gneiss.||
29225|Mulculca Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
29225|Mulculca Formation|72461|5|Briefly described|p16 fig 9|||Redan sub-block of the Broken Hill Block.||Rantyga Group||Overlies the Ednas Gneiss. Overlain by the Farmcote Gneiss.||
29225|Mulculca Formation|73243|6|Mentioned|p53 Fig.2|||||||||
29225|Mulculca Formation|73482|6|Mentioned|p422 Fig.3|||Redan sub-block.||Rantyga Group||||
29225|Mulculca Formation|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|||Redan Geophysical Zone.||Rantyga Group||||
26063|Mulga Downs Group|730|5|Briefly described|p6, p7, p9, p15, p19, p24, p34, p70.||Devonian|Cross-bedded sandstone, conglomerate, siltstone. Outliers form prominent hills and ranges. Mildly deformed by Kanimblan tectonism. Overlies Girilambone Group, probably unconformably. Early source of building stone near Bourke.||||||11-NOV-14
26063|Mulga Downs Group|5252|5|Briefly described|p61, p62, p63. |Late Devonian|Middle Devonian|Sandstones and, less commonly, quartz pebble conglomerates. Overlies paraconformably, locally unconformably, the Winduck Group.||||||
26063|Mulga Downs Group|9250|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes Ravendale Formation.||||||
26063|Mulga Downs Group|22503|6|Mentioned|p643|Late Devonian|Middle Devonian|||||||
26063|Mulga Downs Group|22508|6|Mentioned|p6|||Lachlan Fold Belt||||||
26063|Mulga Downs Group|22518|5|Briefly described|p 6, 7|||||||||
26063|Mulga Downs Group|22580|5|Briefly described|p87|Carboniferous|Middle Devonian|||||||
26063|Mulga Downs Group|22646|6|Mentioned|p 107|||western New South Wales||||||
26063|Mulga Downs Group|22671|5|Briefly described|p832|Late Devonian|Middle Devonian|Fluvial quartz sandstone with minor conglomerate and shale.||||||17-JAN-06
26063|Mulga Downs Group|22683|6|Mentioned|93,96|Devonian|Devonian|||||||
26063|Mulga Downs Group|22730|5|Briefly described|p557,8|Early Carboniferous|Emsian|Represented in Nudooka area by Coco Range Sandstone and Nundooka Sandstone.||||||
26063|Mulga Downs Group|22768|6|Mentioned|p153,169|||||||||
26063|Mulga Downs Group|22773|5|Briefly described|Fig24.5p350|||||||||
26063|Mulga Downs Group|22799|2|Defined|p16|Early Carboniferous|Devonian|||||||
26063|Mulga Downs Group|22857|6|Mentioned|p153, p200|Early Carboniferous|Devonian|Divided into 5 formations and 2 members. Conformably overlies the Cobar Supergroup. Max. thickness: >5km. Geological Province: Barka Basin, Kanmantoo Fold Belt. See also p211. Mentioned in terms of equivalents on p350 Fig. 24.5.||||||
26063|Mulga Downs Group|22859|4|Described|p200,207,211-12|Early Carboniferous|Devonian|||||||
26063|Mulga Downs Group|22887|5|Briefly described|p27, Fig.4 p11||Early Devonian|See also p13||||||
26063|Mulga Downs Group|22893|5|Briefly described|p12 fig4|Late Carboniferous|Middle Devonian|||||||
26063|Mulga Downs Group|23101|5|Briefly described|p567 (Fig 1)|||||||||
26063|Mulga Downs Group|23171|5|Briefly described|p11,15-6,21|Late Devonian|Early Devonian|||||||
26063|Mulga Downs Group|23173|4|Described|Map Legend|Late Devonian|Emsian|||||||
26063|Mulga Downs Group|23252|5|Briefly described|Map Legend|||||||||
26063|Mulga Downs Group|23309|6|Mentioned|p390|||||||||
26063|Mulga Downs Group|23336|3|Fully described|p5, p14-15|Early Carboniferous|Emsian|Fluviatile deposits. Overlain by Eyrian Formation and Rolling Downs Group. max. thickness: 2km.||||||21-MAR-06
26063|Mulga Downs Group|23380|3|Fully described|p105-120|Late Devonian|Early Devonian|8 informal constituent units described. of Wonaminta Block. Age: Emsian - Famennian.||||||
26063|Mulga Downs Group|23469|5|Briefly described|p 321|||Comprises the Snake Cave Sandstone, Waverly Creek beds and the Ravendale Formation.||||||10-MAY-12
26063|Mulga Downs Group|23522|5|Briefly described|p249 Fig 5|Devonian|Devonian|||||||
26063|Mulga Downs Group|23734|5|Briefly described|p12 Fig. 1|||Sandstone.||||||
26063|Mulga Downs Group|23835|4|Described|p399|Devonian|Devonian|Maximum thickness:  4700m.||||||
26063|Mulga Downs Group|23836|5|Briefly described|p92|Early Devonian|Early Devonian|Geological Province: Murray Basin.||||||
26063|Mulga Downs Group|24580|6|Mentioned|p829|||Geological Province: Eastern Lachlan Fold Belt.||||||
26063|Mulga Downs Group|29621|6|Mentioned|p11|||||||||
26063|Mulga Downs Group|29947|6|Mentioned|p685|||||||||
26063|Mulga Downs Group|29984|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|29987|5|Briefly described|p23|||||||||
26063|Mulga Downs Group|29991|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|30663|6|Mentioned|p25|||||||||
26063|Mulga Downs Group|30683|6|Mentioned|Table 1|||||||||
26063|Mulga Downs Group|31161|5|Briefly described|PA5|||||||||
26063|Mulga Downs Group|31618|6|Mentioned|p104|||||||||
26063|Mulga Downs Group|32087|6|Mentioned|Table 3|||||||||
26063|Mulga Downs Group|32619|6|Mentioned|p459|||Flora||||||
26063|Mulga Downs Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
26063|Mulga Downs Group|32672|6|Mentioned|p674|||||||||
26063|Mulga Downs Group|32677|5|Briefly described|p6|||||||||
26063|Mulga Downs Group|32853|6|Mentioned|p59|||Rich fish fauna. ?Emsian-Eifelian||||||
26063|Mulga Downs Group|32865|5|Briefly described|p485|||Late Dev. to Early Carb.||||||
26063|Mulga Downs Group|32918|4|Described|p12|||||||||11-JAN-10
26063|Mulga Downs Group|33004|6|Mentioned|p199|||||||||
26063|Mulga Downs Group|33121|6|Mentioned|Fig.8|||May extend into Middle Dev.||||||
26063|Mulga Downs Group|33732|4|Described|p100|||||||||
26063|Mulga Downs Group|34035|6|Mentioned|p544|||U.Dev.||||||
26063|Mulga Downs Group|34057|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|34071|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|34109|3|Fully described|p164|||See also PP165-169||||||
26063|Mulga Downs Group|34400|5|Briefly described|p5|||Correlated with Ravendale Formation. See also P11,24.||||||
26063|Mulga Downs Group|34401|5|Briefly described|p71|||Late Devonian fish plates. See also p72.||||||04-NOV-13
26063|Mulga Downs Group|34403|6|Mentioned|p148|||||||||
26063|Mulga Downs Group|34404|6|Mentioned|Fig.3.8|||Devonian - ?Lower Carboniferous||||||
26063|Mulga Downs Group|34405|6|Mentioned|Fig.3.9|||Correlation Table||||||
26063|Mulga Downs Group|34406|6|Mentioned|p225|||||||||
26063|Mulga Downs Group|34418|6|Mentioned|p501|||||||||
26063|Mulga Downs Group|34449|4|Described|p21|||U.Devonian||||||
26063|Mulga Downs Group|34469|6|Mentioned|p107|||Upper Devonian. See P116||||||
26063|Mulga Downs Group|34550|5|Briefly described|Table 2.1|||?Late Devonian||||||
26063|Mulga Downs Group|34563|6|Mentioned|p70|||Refers Conolly (1962). Stratigraphy.||||||
26063|Mulga Downs Group|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|35185|6|Mentioned|p220|||||||||
26063|Mulga Downs Group|35232|6|Mentioned|Table 2|||||||||
26063|Mulga Downs Group|35385|6|Mentioned|p19|||Refers Joklik(1950). See also P38.||||||
26063|Mulga Downs Group|35609|6|Mentioned|p13|||||||||
26063|Mulga Downs Group|35925|4|Described|p5|||||||||
26063|Mulga Downs Group|36214|6|Mentioned|p57|||||||||
26063|Mulga Downs Group|36317|6|Mentioned|p147|||||||||
26063|Mulga Downs Group|37272|6|Mentioned|p237|||||||||
26063|Mulga Downs Group|37798|6|Mentioned|p128|||||||||
26063|Mulga Downs Group|38292|6|Mentioned|p3|||||||||
26063|Mulga Downs Group|38593|6|Mentioned|p85|||See also P88.||||||
26063|Mulga Downs Group|38692|6|Mentioned|p128|||||||||
26063|Mulga Downs Group|39064|6|Mentioned|p2|||||||||
26063|Mulga Downs Group|39084|6|Mentioned|Fig.1|||||||||
26063|Mulga Downs Group|39618|6|Mentioned|p121|||||||||
26063|Mulga Downs Group|39978|6|Mentioned|p65|||||||||
26063|Mulga Downs Group|40130|6|Mentioned|p195|||||||||
26063|Mulga Downs Group|40291|6|Mentioned|p15|||||||||
26063|Mulga Downs Group|40387|6|Mentioned|p146|||||||||
26063|Mulga Downs Group|40595|6|Mentioned|Fig.7|||||||||
26063|Mulga Downs Group|40676|6|Mentioned|p28|||||||||
26063|Mulga Downs Group|40728|6|Mentioned|p173|||||||||
26063|Mulga Downs Group|40913|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
26063|Mulga Downs Group|41018|6|Mentioned|p239|||||||||
26063|Mulga Downs Group|41126|3|Fully described|p107|||Mention P23||||||
26063|Mulga Downs Group|41138|6|Mentioned|Map legend|Carboniferous|Devonian|Carboniferous - Devonian||||||
26063|Mulga Downs Group|41276|6|Mentioned|p62|||||||||
26063|Mulga Downs Group|41385|6|Mentioned|p374|||||||||
26063|Mulga Downs Group|41394|2|Defined|p104|Eifelian|Emsian|||||||
26063|Mulga Downs Group|41395|6|Mentioned|Map legend|Middle Devonian||||||||
26063|Mulga Downs Group|41410|5|Briefly described|p295|||||||||
26063|Mulga Downs Group|41528|5|Briefly described|p20|||||||||
26063|Mulga Downs Group|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
26063|Mulga Downs Group|41821|3|Fully described|p53|Early Carboniferous|Early Devonian|||||||
26063|Mulga Downs Group|41872|6|Mentioned|p8|||||||||
26063|Mulga Downs Group|42033|6|Mentioned|p653|||||||||
26063|Mulga Downs Group|42140|6|Mentioned|p559|||||||||
26063|Mulga Downs Group|42144|5|Briefly described|p603|||||||||
26063|Mulga Downs Group|42172|4|Described|Fig.4 P166|||See also Fig 5||||||
26063|Mulga Downs Group|42208|5|Briefly described|p304|||||||||
26063|Mulga Downs Group|42467|5|Briefly described|Map Legend|||||||||
26063|Mulga Downs Group|42521|5|Briefly described|p15 and Figs|||||||||
26063|Mulga Downs Group|42547|5|Briefly described|p59|||||||||
26063|Mulga Downs Group|42566|5|Briefly described|Fig.5 P11|||||||||
26063|Mulga Downs Group|42581|6|Mentioned|p48|||||||||
26063|Mulga Downs Group|42907|6|Mentioned|Fig.8, P8|||||||||
26063|Mulga Downs Group|42954|6|Mentioned|p68|||||||||
26063|Mulga Downs Group|42955|5|Briefly described|p70|||||||||
26063|Mulga Downs Group|42966|5|Briefly described|Fig. 25 p47|||||||||
26063|Mulga Downs Group|42983|5|Briefly described|p342|||||||||
26063|Mulga Downs Group|43032|3|Fully described|p149|||||||||
26063|Mulga Downs Group|43089|5|Briefly described|Map Legend|||||||||
26063|Mulga Downs Group|43090|5|Briefly described|Map legend|Carboniferous|Middle Devonian|||||||
26063|Mulga Downs Group|43192|5|Briefly described|p65,Table1 p61|Early Carboniferous|Late Devonian|||||||
26063|Mulga Downs Group|43202|6|Mentioned|p17|||||||||
26063|Mulga Downs Group|43263|6|Mentioned|Map Legend|Early Carboniferous|Late Devonian|||||||
26063|Mulga Downs Group|43366|14|Not recorded|Map Legend|||||||||
26063|Mulga Downs Group|43367|14|Not recorded|Map Legend|||||||||11-JAN-10
26063|Mulga Downs Group|43368|14|Not recorded|Map Legend|||||||||
26063|Mulga Downs Group|43369|14|Not recorded|Map Legend|||||||||
26063|Mulga Downs Group|43371|14|Not recorded|Map Legend||Late Devonian|||||||11-JAN-10
26063|Mulga Downs Group|43379|14|Not recorded|Map Legend||Late Devonian|||||||
26063|Mulga Downs Group|43380|14|Not recorded|Map Legend||Late Devonian|||||||
26063|Mulga Downs Group|43381|14|Not recorded|Map Legend||Late Devonian|||||||
26063|Mulga Downs Group|43383|14|Not recorded|p13-15||Late Devonian|Disconformable on Amphitheatre Beds||||||
26063|Mulga Downs Group|43384|14|Not recorded|Map Legend||Late Devonian|||||||
26063|Mulga Downs Group|43387|14|Not recorded|Map Legend|||||||||
26063|Mulga Downs Group|43388|14|Not recorded|Map Legend||Late Devonian|||||||
26063|Mulga Downs Group|43389|14|Not recorded|Map Legend||Late Devonian|Includes Bulgoo Ss,Keginni Ss, Meadows Tank Conglomerate,Merrimerriwa Formation,Yathong Formation||||||
26063|Mulga Downs Group|43398|14|Not recorded|Map Legend||Late Devonian|||||||
26063|Mulga Downs Group|43438|14|Not recorded|Map Legend|||Upper Devonian consists of Mount Manara Conglomerate||||||
26063|Mulga Downs Group|43461|14|Not recorded|p619,Table p621,625||Famennian|||||||
26063|Mulga Downs Group|43479|14|Not recorded|p134,151||Late Devonian|||||||
26063|Mulga Downs Group|43501|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
26063|Mulga Downs Group|43507|14|Not recorded|p124-126,129|||||||||
26063|Mulga Downs Group|43509|14|Not recorded|p112|||||||||
26063|Mulga Downs Group|43510|14|Not recorded|p37-8,46|||||||||
26063|Mulga Downs Group|43511|14|Not recorded|p129||Late Devonian|||||||
26063|Mulga Downs Group|43757|6|Mentioned|p511||Early Devonian|Age: approx. 390-380 Ma||||||
26063|Mulga Downs Group|43774|6|Mentioned|Fig.1,p2|||||||||
26063|Mulga Downs Group|43841|5|Briefly described|7||Carboniferous|||||||
26063|Mulga Downs Group|43859|4|Described|14,15, Fig6p22-23|Late Devonian|Middle Devonian|Unconformable on Winduck Group.||||||15-DEC-08
26063|Mulga Downs Group|44093|5|Briefly described|p54|Early Carboniferous|Devonian|See also p146 Appendix 1. Geological Province: Barka Basin/Kanmantoo Fold Belt.||||||
26063|Mulga Downs Group|44133|6|Mentioned|p45|Devonian|Devonian|||||||
26063|Mulga Downs Group|44188|5|Briefly described|Map Legend|Late Devonian|Early Devonian|Includes Milton Grove beds, Manfred Sandstone, Hughies Bore beds. Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt.||||||15-MAY-08
26063|Mulga Downs Group|44191|5|Briefly described|Map Legend|Early Carboniferous|Early Devonian|||||||
26063|Mulga Downs Group|46973|6|Mentioned|p51|||||||||
26063|Mulga Downs Group|47026|6|Mentioned|Fig.5|||||||||
26063|Mulga Downs Group|47050|6|Mentioned|p239|||||||||
26063|Mulga Downs Group|49038|6|Mentioned|p22|||||||||
26063|Mulga Downs Group|49040|6|Mentioned|p6|||||||||
26063|Mulga Downs Group|50618|5|Briefly described|p249, p249 Fig. 3|Late Devonian|Late Devonian|Quartzitic sandstone.||||||
26063|Mulga Downs Group|60520|5|Briefly described|Map legend|Late Devonian|Middle Devonian|Undifferentiated in this context.  Geological Province: Barka Basin.||||||18-OCT-04
26063|Mulga Downs Group|60648|6|Mentioned|p40-41|Early Carboniferous|Emsian|Includes the Coco Range and Nundooka Sandstones. Geological Province: Darling Basin.||||||
26063|Mulga Downs Group|61311|5|Briefly described|p43 table D1|Early Carboniferous|Middle Devonian|Includes the Meadows Tank and Merrimerriwa Formations. Geological Province: Darling Basin.||||||
26063|Mulga Downs Group|61314|5|Briefly described|p120, p128|Carboniferous|Middle Devonian|Fluvial/lacustrine red bed facies - massive sandstone and interbedded red siltstone and shale. Overlies the Amphitheatre Group (Cobar Supergroup). Max. thickness: 2000m. Geological Province: Murray Basin.||||||
26063|Mulga Downs Group|61964|5|Briefly described|p113-114|Late Devonian|Late Devonian|Possibly a correlative of Cocoparra Group. Max. thickness: 3212m.||||||
26063|Mulga Downs Group|62659|6|Mentioned|p612|||||||||
26063|Mulga Downs Group|63632|5|Briefly described|649|Frasnian|Emsian|||||||
26063|Mulga Downs Group|63793|6|Mentioned|p19 Table 1. |||||||||
26063|Mulga Downs Group|64681|5|Briefly described|p1, p3 Fig. 1|Late Devonian|Middle Devonian|Quartz-rich sedimentary rocks.||||||15-DEC-08
26063|Mulga Downs Group|64685|5|Briefly described|Map Legend|Carboniferous|Late Devonian|Includes Snake Cave Sandstone.||||||01-DEC-08
26063|Mulga Downs Group|64962|5|Briefly described|p202|Late Devonian|Early Devonian|Partly overlies Cobar Supergroup.||||||08-APR-09
26063|Mulga Downs Group|64964|5|Briefly described|p159, p163 Fig. 4|||Includes Bundycoola, Meadows Tank, Merrimerriwa, Crowl Formations and Mt Jack beds. Thickness: >6km(est.).See also p165 Fig. 6.||||||
26063|Mulga Downs Group|64967|5|Briefly described|p113, p114 Fig. 2, p121|Late Devonian|Early Devonian|Spans the informally named Snake Cave and Ravendale Intervals used in this study to indicate lithostratigraphic subdivisions.||||||04-JUL-13
26063|Mulga Downs Group|65214|6|Mentioned|p278|Devonian|Devonian|NSW, Cobar. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26063|Mulga Downs Group|65469|5|Briefly described|p14-p17, p22, p43|Famennian|Emsian|Lachlan Orogen. Deposited in sag basin setting during thermal subsidence of the Kanimblan Cycle. See also p52, p55 fig 3-19, p62, p67, p136, p339, App A-VI 3. ||||Unconformably overlies the Winduck Group.||
26063|Mulga Downs Group|65759|5|Briefly described|Throughout the article.|Late Devonian|Early Devonian|In Darling Basin, western NSW. Originally called Mulga Downs Stage (Mulholland 1940); redefined as Mulga Downs Group by Rayner (cited in Conolly et al. 1969) and subsequently. 5 major lithofacies; braided fluvial, meandering fluvial, estuarine tidal channel to near shore, fluvial and shallow lacustrine, and braided-delta plain. Article concludes that the Group has excellent reservoir potential and stratigraphic-trap configuration.||||||
26063|Mulga Downs Group|66498|6|Mentioned|p45|||Darling Basin, western NSW. Contains fossils of the thelodont Turinia australiensis, as do N'Dhala Member (Pertnjara Group) and other boreholes in WA.||||||
26063|Mulga Downs Group|66499|6|Mentioned|p59|||Part of Darling Basin, western NSW, contains diverse placoderm assemblages||||||
26063|Mulga Downs Group|66623|6|Mentioned|p195, p216. |||Darling Basin. Correlated with Wana Karnu Group.||||||
26063|Mulga Downs Group|67823|6|Mentioned|p366|||||||||
26063|Mulga Downs Group|67870|4|Described|p58, p62, p64-67, p69, p72-75, p77-79|Late Devonian|Middle Devonian|Darling Basin. A very thick succession of mainly fluvial deposits; minor marine incursions. Potential reservoir rocks; some source potential from organic-rich shale and limestone. Detailed modelling shows 89-100% of kerogen transformed and early expulsion of oil and minor gas.|||Snake Cave Sandstone; Ravendale, Bulgoo, Bundycoota Formations.|Unconformably overlies Winduck and Amphitheatre Groups.|Red beds. Conglomerate, sandstone, siltstone, shale, limestone.|
26063|Mulga Downs Group|68297|5|Briefly described|p192|Middle Devonian|Emsian|Includes Emsian vertebrate fossil fauna. See also Mulga Downs Formation p183.||||||
26063|Mulga Downs Group|68298|5|Briefly described|p210, p222, p223||Early Devonian|Fish fauna reported to contain typical European 'Old Red Sandstone' Late Devonian fish fauna (Rade 1964) was accordingly included as a Late Devonian-Carboniferous sequence in Packham (1969). However, Ritchie (1969) revealed fauna of almost entirely endemic genera suggesting Early or Middle Devonian age (Ritchie 1973). Wuttagoonaspis fauna contains abundant and diverse placoderm fauna (Ritchie, 1973). Also present are crossopterygians, acanthodians and the thelodont Turinia. Fluviatile. Presence or duration of a hiatus at the base of this unit is uncertain. Maximum age provided by underlying marine unit.||||Overlies Winduck Formation, Cobar Supergroup.||
26063|Mulga Downs Group|68592|6|Mentioned|p1198|Eifelian|Eifelian|||||||
26063|Mulga Downs Group|68823|5|Briefly described|pp375-379, p395, p399, p402, p409|Famennian|Emsian|Lambie Shelf. Upper Darling Basin. c.3-4 km thick, SW of Cobar. Has continuous, parallel seismic reflections.||||Disconformably to paraconformably overlies the Winduck Group and Kopyje Group.|Largely fluviatile sandstone, siltstone and shale.|
26063|Mulga Downs Group|69002|6|Mentioned|p15, p16, Map 1b, Legend|Late Devonian|Middle Devonian||||||Comprises non-magnetic massive fluviatile sandstones: mainly flat lying but linear magnetic trends over some bed-dip ridges.|
26063|Mulga Downs Group|69042|5|Briefly described|map legends|Late Devonian|Late Devonian|Dmd. Nelyambo Trough, Lachlan Orogen. Non-magnetic massive fluviatile sandstones. Mainly flat lying, but linear magnetic trends over some bed-dip ridges||||||
26063|Mulga Downs Group|69043|6|Mentioned|p11|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|69511|6|Mentioned|p22|||||||Is faulted against the Thule Granite.||
26063|Mulga Downs Group|69541|6|Mentioned|p645 Fig.1(b), p655|Late Devonian|Early Devonian|Lachlan Orogen.||||||
26063|Mulga Downs Group|69635|5|Briefly described|p148, 156, 69|Late Devonian|Middle Devonian|Age constrained by fish fossils in other units of this group.|||Includes Moira Formation, Mount Oxley Formation.|Unconformably overlies Booda Formation.||
26063|Mulga Downs Group|70000|6|Mentioned|p32, p34, p40|Devonian|Devonian||||Includes Nundooka Sandstone and Coco Range Beds.|||
26063|Mulga Downs Group|70015|5|Briefly described|Map legend|Devonian|Devonian|Only outcrop areas are shown. Mineral deposits (if any) are shown.|||||Quartzitic fluvial and alluvial sedimentary rocks: arenite and quartzite, minor conglomerate, shale.|
26063|Mulga Downs Group|70383|6|Mentioned|p51|Devonian|Devonian|Cobar area. Thought to be a source of fossiliferous (fish) sandstone boulders in the Bulldog Shale.||||||
26063|Mulga Downs Group|70602|5|Briefly described|p66,Fig 2, 67,72,75|Late Devonian|Early Devonian|Aeromagnetic map data given.|||Includes Mount Oxley Formation, Moira Formation.|Unconformably overlies Booda Formation.|Medium- to coarse-grained fluvial sedimentary rocks.|
26063|Mulga Downs Group|70718|5|Briefly described|p20, p43, p54, p102|Early Carboniferous|Early Devonian|Darling Basin. A deep to shallow marine depositional environment is interpreted for this group. Intersected by Booligal-2. Some uncertainty about whether the rocks in Mossgiel 1 should be assigned to this group or Wana Karnu Group [a lateral equivalent]. Radiometric age interpreted as the depositional ages of tuff and shales. A fossil fish suggests Emsian to Eifelian age.|398.5+/- 7.9 and 409.8+/- 8.1 Ma (K-Ar)|Cobar Supergroup||Overlies the Winduck Group, Mossgeil Granite..|Quartz fluvial and alluvial sediments of arenites and quartzites with minor conglomerate and shale.|02-JUN-19
26063|Mulga Downs Group|70751|4|Described|p4, p6, p11-p15, p28-p29|Late Devonian|Early Devonian|Cobar Superbasin, Winduck Shelf. Fossil control for this unit is poor. Age of this unit is a matter of debate with some authors suggesting Early Devonian ( Glen et al,(1992), Early Carboniferous to Late Devonian (Powell et al, 1987). Sherwin (2013) revised the age of the group from the Pragian-Emsian boundary to no younger than the Eifelian.|||Includes the Meadows Tank Formation, Merrimerriwa Formation, Bulgoo Formation, Bundycoola Formation and Crowl Creek Formation.|Overlies the Winduck Group. Equivalent to the Cocoparra Group.||
26063|Mulga Downs Group|70821|5|Briefly described|p9, p11, p15, p28, p111-112, p118|Late Devonian|Early Devonian|Upper part of the Darling Basin. Crops out in the Campamooka Mountains. Sediments occupying the Paka Tank Trough. Electrically resistant basement.|||||Predominantly fluviatile sandstone. Typically flat-lying and non-magnetic.|
26063|Mulga Downs Group|70941|6|Mentioned|p9|Late Devonian|Middle Devonian|Shallow marine depositional environment. Deformed by the Kanimblan Orogeny.|||||Quartzose sandstone.|
26063|Mulga Downs Group|70950|6|Mentioned|p1028|Early Devonian|Early Devonian|Geological province: Yathong Trough, Central Lachlan Orogen. ||||||
26063|Mulga Downs Group|71039|6|Mentioned|p6-p7, p16, p23-24|Devonian|Silurian|Devonian||||||10-MAR-23
26063|Mulga Downs Group|71040|5|Briefly described|p6-7, p14-15, p25, p28, p31|Eifelian|Emsian|Cobar Basin. Fluvial deposits. Age had been previously assessed as upper Lower to Upper Devonian; the upper limit may be Emsian. Contains conglomerate wedges thinning to the N, sourced from Tabberabberan Orogeny uplifted areas to the S. Underwent 16% shortening in Kanimbla Orogeny.|||Bundycoola Formation.|Overlies Winduck Group conformably (locally disconformably).||
26063|Mulga Downs Group|71263|6|Mentioned|p18 Fig 2|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|71360|5|Briefly described|Map legend|||Geophysical signature: non-magnetic unit generally not distinguishable in aeromagnetic data. These areas are low in radioelements. Boundaries shown are based on existing geological mapping. Age given as ?Middle Devonian -  Carboniferous.|||||Thick-bedded quartzose sandstone with granule to pebble conglomerate and fine-grained intervals.|
26063|Mulga Downs Group|71693|5|Briefly described|Map legend; p2.|Devonian|Devonian|||||Overlies Winduck Group.|Quartzitic fluvial and alluvial sedimentary rocks; arenite and quartzite, minor conglomerate, shale.|
26063|Mulga Downs Group|71860|6|Mentioned|p6|Late Devonian|Late Devonian|||||||
26063|Mulga Downs Group|71965|6|Mentioned|p894,896,901-904|Devonian|Devonian|Geological province: Lachlan Orogen. ||||Underlain by Girilambone Group.||
26063|Mulga Downs Group|72522|5|Briefly described|p18, p20.|Late Devonian|Middle Devonian|Contains fish fossils indicative of a Middle to Late Devonian age.|||Includes Mount Oxley Formation, Moira Formation.|Overlies Booda Formation.||24-FEB-21
26063|Mulga Downs Group|72908|6|Mentioned|p4|Early Devonian|Silurian|Winduck Shelf.||||||
26063|Mulga Downs Group|72915|6|Mentioned|p5|||Map symbol suggests Devonian age.||||||
26063|Mulga Downs Group|72958|6|Mentioned|p10, p11|Eifelian|Emsian|Cobar Basin. Nymagee area.|||Crowl Creek Formation, Bundycoola Formation, Bulgoo Formation, Merrimerriwa Formation, Meadows Tank Formation|Underlain by the Gundaroo Sandstone (Winduck Group) and Lumga Siltstone, Yar Sandstone and Whoey Tank Formation (all of the Walters Range Group).||
26063|Mulga Downs Group|73174|6|Mentioned|p1036|||||||||
26063|Mulga Downs Group|73175|6|Mentioned|p1050, p1066|||Thomson Orogen, southern. Low magnetic intensity.|||||Clastic sedimentary rocks.|
26063|Mulga Downs Group|73177|5|Briefly described|p1099, 1112|Late Devonian|Early Devonian|Widely distributed. Underwent significant (5 km N-over-S thrusting) displacement along the Olepoloko Fault, likely a result of the Alice Springs Orogeny.|||||Fluvial and alluvial sedimentary rocks.|
26063|Mulga Downs Group|73181|6|Mentioned|p60|||Darling Basin. Contains L. australe.||||||
26063|Mulga Downs Group|73264|5|Briefly described|p1395, p1407|Late Devonian|Early Devonian|Lachlan Orogen. Late Early Devonian minimum age.|||Meadows Tank Formation, Keginni Conglomerate Member, Calytria Quartzite Member||Includes fluviatile sandstones.|
26063|Mulga Downs Group|73457|5|Briefly described|p1-2, p4, p6-7, p14|Late Devonian|Late Devonian|Included in the Upper Devonian here, the exact age is debated. Williams (2016) included the Kenegal Formation in the Mulga Downs Group, Trigg (2019) however suggested that the formation be left ungrouped.|||Galore Hill Formation, Melbergen Sandstone, Keginni Conglomerate Member, Jimberoo Formation||Includes a basal quartz pebble conglomerate, and polymictic conglomerate higher in the group.|
33798|Mulgowrie Granite|50232|5|Briefly described|Map legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
33798|Mulgowrie Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith.||||||
33798|Mulgowrie Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Burrawinda Suite. Foliated to massive, porph. to megacrystic biotite granite + biotite granodiorite, containing sedimentary xenoliths. Massive to foliated porphyritic +/- biotite allanite granite, monzodiorite, granodiorite.||||||
33798|Mulgowrie Granite|68592|5|Briefly described|p231, p257-9, p270, p1664, p1667|||Geophysical properties described. Potential for quarrying for dimension stone. See also references for Mulgowrie Granodiorite (p134, p1288-1289, p1333, p1354-1364) which would seem to be the preferred name.||Unit in Burrawinda Suite.||Is intruded by Bishopthorpe Suite.|S-type.|
77436|Mulgowrie Granodiorite|66300|5|Briefly described|p92.|||S-type.|427.8 +/- 2.7 Ma.|Unit in Burrawinda Suite.||||
77436|Mulgowrie Granodiorite|68592|2|Defined|p134, p1288-9, p1333, p1354-64|Ludlow|Wenlock|New name, after Mulgowrie Creek. Previously part of undifferentiated Wyangala Batholith (Brunker and Offenberg, 1970) and later Wheeo Granite (Chappell et al., 1991). The type pluton for the Burrawinda Suite. Extends 50 km N-S and up to 11 km E-W. Type localities described. Metamorphism described; has a well-developed N to NW trending foliation dipping steeply to the W. Geochemistry and geophysical properties described. SHRIMP U-Pb zircon age. Has been used as a minor, local source of road construction materials. See also references to Mulgowrie Granite (p231, p257-259, p270, p1664, p1667) which would seem to be the less-preferred name.|427.8 +/- 2.7 Ma (Bodorkos and Simpson, 2008).|Unit in Burrawinda Suite.||Intrudes Adaminaby Group. Encloses Cumberoona Tonalite. Is intruded by Gunning, Narrawa and Julong Granites.|Dark grey to cream to white, medium- to coarse-grained, foliated, porphyritic (occasionally megacrystic) to equigranular, cordierite-muscovite-biotite granodiorite (with sporadic mafic enclaves and sedimentary xenoliths), tonalite and granite.|
77436|Mulgowrie Granodiorite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Swm. On Crookwell and Gunning 1:100 000 mapsheet portions of Time-Space Plot.||Burrawinda Suite|||Medium-coarse grained, foliated, porphyritic to equigranular, cordierite-muscovite-biotite granodiorite, tonalite and granite; granodiorite locally contains mafic enclaves and sedimentary xenoliths; low to high K and medium-high Th response.|
77436|Mulgowrie Granodiorite|70541|4|Described|Map Legend|Devonian|Silurian|||Burrawinda Suite|||Medium to coarse grained, foliated, porphyritic to equigranular, cordierite-muscovite-biotite granodiorite, tonalite and granite; granodiorite locally contains mafic enclaves and sedimentary xenoliths; low to high K and medium to high Th response.|
77436|Mulgowrie Granodiorite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Burrawinda Suite|||Medium-coarse grained, foliated, porphyritic to equigranular, cordierite-muscovite-biotite granodiorite, tonalite and granite; granodiorite locally contains mafic enclaves and sedimentary xenoliths; low to high K and medium-high Th response.|
33419|Mulguthrie Formation|24417|2|Defined|p66|Early Devonian|Late Silurian|Of Ootha Group.  Previously mapped as an undifferentiated unit within the "Ootha Formation".  Overlain by Yarra Yarra Creek Group;  underlain by Manna Conglomerate.||||||
33419|Mulguthrie Formation|50554|5|Briefly described|Map legend|Devonian|Silurian|Of the Ootha Subgroup (Derriwong Group).||||||
33419|Mulguthrie Formation|60009|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Ootha Group. Overlies: Manna Conglomerate.||||||13-JUL-04
81788|Mullagalah Quartz Diorite|71345|5|Briefly described|p30, 33|Early Devonian|Early Devonian|Similar in age and lithology to Galambo Granite. See Cooper 2001; Gilmore et al. in prep. b. Hergarty (2011) included Mullagalah Quartz Diorite as part of Galambo Granite on geophysical grounds.|414.9+\-4.2 Ma||||Quartz-biotite-hornblende bearing, I-type quartz diorite|02-DEC-19
81812|Mullengandra Monzodiorite|73457|6|Mentioned|p10|Early Devonian|Early Devonian|||||||
78648|Mullens Granite|69159|5|Briefly described|Map legend|Pragian|Pragian|||Unit in Glenbog Suite.|||Grey, green to pink, medium- to coarse-grained, massive, equigranular to occasionally weakly porphyritic, biotite-hornblende granite.|07-SEP-15
78648|Mullens Granite|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Glenbog Suite.|||Grey, green to pink, medium- to coarse-grained, massive, equigranular to weakly porphyritic, biotite-hornblende granite.|
78648|Mullens Granite|71700|3|Fully described|vi, ix, p7, p26, p44, p79, p82-p83, CD|Early Devonian|Early Devonian|Named for the Mullens Creek which joins the Croppies Gunyah Creek. Representative outcrops of the Mullens Granite occur in paddocks on either side of the track into the Pine Bank property, between GR 751273 6104734 to 751386 6104591. Previous mapping by Joplin et al. (1953), Best et al. (1964), Felton and Huleatt (1975) included the Mullens Granite within a group of elongate plutons collectively known as the Boro Granite that extended from Lake Bathurst to the southern boundary of ARALUEN100. Included in the Glenbog Suite on the basis of lithological and geochemical grounds. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics and distinguishing features are discussed.  Age is interpreted to be Early Devonian on the basis of dating of the geochemically similar Boro Granite at 411.5 +/- 3.1 Ma (Bodorkos and SImpson, 2008).||Glenbog Suite||Intrudes the Abercrombie Formation. Equivalent to the Boro Granite and Bundong Granite.|Grey, green to pink, medium- to coarse-grained, massive, equigranular to occasionally weakly porphyritic, biotitehornblende granite.|
26064|Mulwaree Group|22857|5|Briefly described|p472 App.1 Tb.A1.6|Middle Devonian|Early Devonian|Geological Province: Captains Flat-Goulburn Trough. See also p480 App.1 Tb.A1.6.||||||
26064|Mulwaree Group|23048|5|Briefly described|p6,7|Middle Devonian|Early Devonian|||||||
26064|Mulwaree Group|30730|6|Mentioned|p10|||Geological map||||||
26064|Mulwaree Group|30735|2|Defined|p46|Devonian|Devonian|||||||
26064|Mulwaree Group|30736|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26064|Mulwaree Group|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
26064|Mulwaree Group|39331|6|Mentioned|p56|||See p57.||||||07-SEP-15
26064|Mulwaree Group|42177|6|Mentioned|p213|||||||||
26064|Mulwaree Group|44093|5|Briefly described|p221 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
26064|Mulwaree Group|67820|6|Mentioned|p136 Fig.3|Devonian|Devonian|||||||
26064|Mulwaree Group|68592|5|Briefly described|p30, p1160|Emsian|Pragian|On Braidwood 1:100 000 sheet area.|||Includes Tarago Conglomerate.||Limestone and clastic red-bed sequences.|
26064|Mulwaree Group|69159|5|Briefly described|Map legend|Emsian|Pragian||||Includes Tarago Conglomerate and Bongalaby Formation.|||07-SEP-15
26064|Mulwaree Group|71040|6|Mentioned|p19|Early Devonian|Early Devonian|Braidwood region.||||||
26064|Mulwaree Group|71069|6|Mentioned|p135||||||Includes the Tarago Conglomerate|||
26064|Mulwaree Group|71656|4|Described|p10 Fig.1, p12 Fig.2, p40-41|Emsian|Pragian|Includes microfossils (in part numerous fish scales and teeth) in late strata with conodonts in the early strata of the Bongalaby Formation.|||Includes Bongalaby Formation, Tarago Congolomerate.|Unconformably overlies Douro Group.|Fosiliferous limestone, conglomerate|
26064|Mulwaree Group|71699|5|Briefly described|Map legend.|Devonian|Devonian||||Tarago Conglomerate, Bongalaby Formation.|||
26064|Mulwaree Group|71700|2|Defined|vi, p7, p13, p27,  p36-p37|Emsian|Late Pragian|Named for the Mulwaree River. See constituent units for type sections. Garretty (1936) applied the term Red Bed Stage to rocks of the Mulwaree Group near Tarago. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils, distinguishing features, economic geology and environmental hazards are discussed. Thickness varies up to 800m on the western limb of the Bongaralaby Syncline. Age is derived on the basis of palaeontological data. This group is potentially equivalent to parts of the Black Range and Murrumbidgee groups. See also p45, p47-p49, p51-p52, p59, p63, p76, CD.|||Includes the Tarago Conglomerate and the Bongalaby Formation.|Disconformably overlies the Mount Fairy Group. Unconformably overlies the Covan Creek Formation.|Red-bed sequence of low-grade metamorphosed sandstones, siltstones, conglomerates and limestones.|
31608|Mumbedah Suite|42726|5|Briefly described|map legend||Carboniferous|||||||
31608|Mumbedah Suite|44093|5|Briefly described|p216 App. 1|Late Carboniferous|Late Carboniferous|Geological Province: Lachlan Fold Belt.||||||18-MAR-05
23848|Mumbulla Granite|22815|4|Described|p95,96|||||||||
23848|Mumbulla Granite|38320|6|Mentioned|p191|||||||||
23848|Mumbulla Granite|40646|6|Mentioned|p23|||||||||
23848|Mumbulla Granite|40776|6|Mentioned|p504|||||||||
23848|Mumbulla Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
23848|Mumbulla Granite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Mumbulla Suite.||||||
23848|Mumbulla Granite|71206|6|Mentioned|p373, 377, 384|||Lachlan Fold Belt. Geochemistry graphs.||Mumbulla Suite.|||Aluminous A-type granite.|
23848|Mumbulla Granite|72313|6|Mentioned|p459 Table 2|||Lachlan Orogen. A-type. Hf isotope data included.|388 Ma|||||
30468|Mumbulla Suite|22815|5|Briefly described|p95|||||||||
30468|Mumbulla Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
30468|Mumbulla Suite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
30468|Mumbulla Suite|60423|6|Mentioned|p377 Fig. 5|||A-Type Suite. Geological Province: Lachlan Fold Belt.||||||
30468|Mumbulla Suite|63605|5|Briefly described|p992 Fig. 1|||||||||07-FEB-11
30468|Mumbulla Suite|67779|6|Mentioned|p66.|||Lachlan Fold Belt. A-type granites. Has remarkable chemical similarity with Tin Camp Granite, McArthur Basin.||||||
30468|Mumbulla Suite|67847|5|Briefly described|p60 fig 3.3.4|Middle Devonian|Middle Devonian|A-type intrusive rocks. ||||||
30468|Mumbulla Suite|70351|6|Mentioned|p55|||||||||
30468|Mumbulla Suite|71206|6|Mentioned|p373, 375, 377, 380-382, 385, 387|||Lachlan Fold Belt. Granites contain rare enclaves, xenocrysts and phenocrysts. Contains both abundant brick-red K-feldspar and cream-white K-feldspar. Very felsic. Geochemistry discussed. Sr/Nd plot.|||Mumbulla, Dr George Mountain, Granites.||Aluminous A-type granite.|
30468|Mumbulla Suite|73431|6|Mentioned|p374 Fig.8|||A-type granites.||||||
69901|Mummel Chert Member|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Abercrombie Formation. Varicoloured medium-bedded to laminated chert interbedded with grey massive to laminated siltstone, mudstone and fine-grained sandstone.||||||
69901|Mummel Chert Member|67322|5|Briefly described|p14, p17; Fig.5|Floian|Floian|Defined by Thomas and Scott, in Thomas et al. (in press). Includes conodonts (photographed) indicative of a late Bendigonian to Chewtonian age (Percival et al. 2003). Occurs in the Goulburn area.||Of the Abercrombie Formation||Overlies the Willigam Sandstone Member.||22-FEB-18
69901|Mummel Chert Member|68466|5|Briefly described|p65-68, 70|Early Ordovician|Early Ordovician|Albury-Bega Terrane. Conodonts indicate Floian age. Photomicrographs.||Abercrombie Formation.|||A thin-bedded, chert-dominated unit.|
69901|Mummel Chert Member|68592|3|Fully described|p274-5, p279, p282-4, p287,p296-7,p304-8|Early Ordovician|Early Ordovician|See also p272, p1860. A marker horizon. Type section specified with measured section in Fig.62. Less than 1m thick. Conodont fauna detailed.||Unit in Abercrombie Formation.|||One or more thin intervals of grey, brown, black and cream laminated to thinly-bedded chert, cherty mudstone and siltstone, interbedded with thin-bedded to laminated siltstone and mudstone with minor sandstone.|
69901|Mummel Chert Member|69159|5|Briefly described|Map legend|Bendigonian|Bendigonian|||Unit in Abercrombie Formation.|||Grey, brown, black or cream, medium-bedded to laminated chert, interbedded with grey to khaki, massive to laminated, siltstone, mudstone and fine-grained sandstone.|07-SEP-15
69901|Mummel Chert Member|69668|5|Briefly described|p929 Fig.2, p930 Fig.3, p931, p943|Early Ordovician|Early Ordovician|Goulburn-Braidwood area, Albury-Bega terrane. Contains late Floian conodonts including Oepikodus evae. Similar age to Budhang Chert in the Oberon district. Chert geochemistry discussed.||Unit in Abercrombie Formation.|||A thin-bedded, chert-dominated unit.|
69901|Mummel Chert Member|70192|5|Briefly described|Map Legend|Bendigonian|Bendigonian|[Theta]aam. On Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Abercrombie Formation||Within undifferentiated Abercrombie Formation.|Laminated to thinly bedded chert, cherty mudstone and siltstone, interbedded with thin bedded-laminated siltstone and mudstone with minor cross-laminated quartzose sandstone.|06-SEP-16
69901|Mummel Chert Member|70541|4|Described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Grey, brown, black and cream laminated to thinly bedded chert, cherty mudstone and siltstone, interbedded with thin-bedded to laminated silstone and grey-black mudstone with minor cross-laminated quartzose sandstone.|
69901|Mummel Chert Member|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Laminated to thinly bedded chert, cherty mudstone and siltstone, interbedded with thin bedded-laminated siltstone and mudstone with minor cross-laminated quartzose sandstone.|
69901|Mummel Chert Member|70544|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Laminated-thinly bedded chert, cherty mudstone and siltstone, interbedded with thin bedded-laminated siltstone and mudstone with minor cross laminated quartzose sandstone.|
69901|Mummel Chert Member|71069|6|Mentioned|p21, p52, p53 fig 19, p54 fig 20|Middle Ordovician|Early Ordovician|Contains early Ordovician Oepikodus evae zone fossils. See also p58-p60, p62, p63, p68.||Abercrombie Formation||Conformably overlain by the Nattery Chert Member||
69901|Mummel Chert Member|71656|6|Mentioned|p12 Fig.2, p11|Bendigonian|Bendigonian|Age based on conodonts. Ranges in age from the Early Ordovician (possibly late Tremadocian to Floian, equivalent to Bendigonian). Sponges also present.||Abercrombie Formation, Adaminaby Group||Adaminaby Group. Within Abercrombie Formation.|Contains siliceous siltstones.|
69901|Mummel Chert Member|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|||Abercrombie Formation.|||Grey, brown, black or cream, medium-bedded to laminated chert interbedded with grey to khaki, massive to laminated siltstone, mudstone and fine-grained sandstone.|
69901|Mummel Chert Member|71700|2|Defined|vi, p7-p8, p39, p43, p56, CD|Bendigonian|Lancefieldian|Albury-Bega Terrane. Named for the locality of Mummel. A type section is defined in Thomas and Pogson (2012). Distribution, geomorphic expression, outcrop characteristics, structure, metamorphism, geophysical characteristics, fossils, distinguishing features, stratigraphic correlation and economic geology are discussed.||Abercrombie Formation||Overlies the Willigam Sandstone Member. Overlain by the Peach Tree Chert Member.|Grey, brown, black or cream, laminated to medium-bedded chert and cherty mudstone and siltstone. Chert horizons are hosted within an interval of thin-bedded to laminated siltstone and mudstone with lesser cross-laminated quartzose sandstone.|19-OCT-22
69901|Mummel Chert Member|73140|6|Mentioned|p495 Fig.1, Fig.3|Bendigonian|Bendigonian|Age based on conodonts.||Abercrombie Formation||||
33123|Mundi Mundi Suite|24197|6|Mentioned|p63|||Part of the Mindi Mundi Batholith. Geological Province: Broken Hill Block.||||||07-FEB-11
33123|Mundi Mundi Suite|50045|6|Mentioned|p117|Calymmian|Calymmian|Geological Province: Broken Hill Block. Age: 1590 Ma.||||||17-MAY-07
33123|Mundi Mundi Suite|50606|5|Briefly described|p1.2, 1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block. Age: 1600Ma.||||||07-NOV-08
33123|Mundi Mundi Suite|69999|6|Mentioned|p4, p11|||||||||
33123|Mundi Mundi Suite|70000|5|Briefly described|p31, p33-34, p39|Calymmian|Calymmian|One of several late syn- to post-orogenic (c.1595-1580 Ma) granites which intrude all levels of Curnamona Province. Associated with Fe-rich breccias in the Silverton to Purnamoota areas.||||Intrudes Paragon Group.|Abundant, sill-like 'Umberumberka-type' granites.|
33123|Mundi Mundi Suite|70015|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Mineral deposits (if any) are shown.|||||Equigranular, pink to grey, leucocratic muscovite + biotite + microcline granite with scattered, euhedral microcline phenocrysts.|
33123|Mundi Mundi Suite|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
33123|Mundi Mundi Suite|73482|6|Mentioned|p421|||||||||
33123|Mundi Mundi Suite|73512|6|Mentioned|p2-3|Calymmian|Calymmian|Curnamona Province, Broken Hill Block. Emplaced during and following the Olarian Orogeny.||||||
34754|Mungay Formation|22892|6|Mentioned|p41|Quaternary|Quaternary|Age: 6425-8530yrs Bp.||||||
33191|Murda Formation|24215|5|Briefly described|p804 Fig. 3|||Geological Province:  Lachlan Fold Belt||||||
33191|Murda Formation|24417|2|Defined|p17|Late Ordovician|Late Ordovician|Of Girilambone Group.  Overlain by Manna Conglomerate.  Max. thickness: 750m.  Geological Province: Lachlan Fold Belt.||||||
33191|Murda Formation|50554|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Girlilambone Group.  Magnetite quartz sandstone, red siltstone, phyllite, chert.||||||24-JUN-04
33191|Murda Formation|60009|5|Briefly described|Map Legend|Eastonian|Darriwilian|Of the Girilambone Group.||||||13-JUL-04
33191|Murda Formation|61964|5|Briefly described|p36|Late Ordovician|Late Ordovician|Of Girilambone Group. Contains conodonts. ||||||
33191|Murda Formation|67322|5|Briefly described|p20|Late Ordovician|Late Ordovician|Defined by Scott (in Lyons et al. 2000). Age determination is based on conodonts. Occurs in the Condobolin - West Wyalong region. ||Of the Girilambone Group|||Magnetite-bearing massive red sandstone with minor white sandstone, siltstone and chert.|22-FEB-18
33191|Murda Formation|71693|5|Briefly described|Map legend.|Ordovician|Ordovician|||Girilambone Group.|||Magnetite-quartz sandstone, red siltstone, phyllite, chert.|
69452|Murder Dog Monzogranite|69639|4|Described|p1, p6, p8, p145-p150, p217, p237|Permian|Carboniferous|New England Orogen. Sample locality, petrography, and geochronology is described.|298 +/- 2 Ma (SHRIMP, magmatic cryst.)|Murder Dog Suite|||Coarse-grained and inequigranular, I-type granite.|
69452|Murder Dog Monzogranite|71628|4|Described|p3: 1, 4, 45, 76-79; p19:152|||Chisholm et al. (2014); previously Murder Dog Adamellite (Pogson and Hitchins, 1973). Named after a locality of that name. Crops out 25-30 km E of Nundle and ~65 km SE of Tamworth. Typically poor exposure; forms low bouldery outcrops and large tors. Geochemistry described; has similarities with Garibaldi Monzogranite.|298.0 +/- 2.0 Ma (SHRIMP: Chisholm et al., 2014).|Murder Dog Suite.||Intrudes Brandy Springs beds.|Greenish-grey to light grey, texturally heterogeneous, fine- to coarse-grained, inequigranular biotite monzogranite; amphibole and garnet bearing variants; weakly to strongly deformed. S-type.|
69452|Murder Dog Monzogranite|71703|5|Briefly described|p203|Cisuralian|Cisuralian|see also Chisholm et al., 2014.|298 +/- 2 Ma.|Of Hillgrove Supersuite.||Spatially associated with Bakers Creek Suite.||
35097|Murdering Gully Tuff Member|23055|5|Briefly described|p23|||||||||
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.|
22482|Murrabrine Quartz Diorite|22815|4|Described|p68|Early Devonian|Late Silurian|||||||
22482|Murrabrine Quartz Diorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Cobargo Suite.||||||
38848|Murrawombie Schist|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
38848|Murrawombie Schist|72296|6|Mentioned|p9|||Berthelsen (1998), for rocks that appeared to form basement to the ore body at the Tritton mine.||||||
23854|Murrawong Creek Formation|22750|5|Briefly described|p 228|Cambrian|Cambrian|||||||
23854|Murrawong Creek Formation|22857|4|Described|p434 App. 1 Tb. A1.5|Late Cambrian|Middle Cambrian|Arenite, granule to boulder conglomerate, clasts of limestone; trilobites, brachiopods, conodonts. Max. thickness: 500m. Geological Province: New England Fold Belt. ||||||
23854|Murrawong Creek Formation|41347|4|Described|Table 3|||||||||
23854|Murrawong Creek Formation|41348|5|Briefly described|Map legend|Ordovician|Cambrian|In the Tamworth Belt.||||||16-DEC-04
23854|Murrawong Creek Formation|41796|6|Mentioned|p304|||See also P308||||||
23854|Murrawong Creek Formation|44093|5|Briefly described|p227 App. 1|Ordovician|Cambrian|Geological Province: New England Fold Belt.||||||22-MAR-05
23854|Murrawong Creek Formation|47056|6|Mentioned|Fig.2 P523|||||||||
23854|Murrawong Creek Formation|50094|5|Briefly described|p315, p316 Fig.1, p317 Fig.2|Late Cambrian|Middle Cambrian|Geological Province: New England Fold Belt.||||||
23854|Murrawong Creek Formation|50168|6|Mentioned|p157 Fig.2|||Gamilaroi Terrane.||||||
23854|Murrawong Creek Formation|61392|5|Briefly described|p165 Fig. 2|Late Cambrian|Middle Cambrian|In the Gamilaroi terrane.||||||07-FEB-11
23854|Murrawong Creek Formation|61762|6|Mentioned|p14 Tab. 1|Ordovician|Cambrian|Consists of conglomerate, sandstone and volcanic-derived mudstone. Forearc Basin environment.||||||
23854|Murrawong Creek Formation|62791|6|Mentioned|p236|Cambrian|Cambrian|Floran-Undillan. Contains lingulate brachiopods indistinguishable from material in Dolodrook River limestones in eastern Victoria, which are somewhat younger (Mindyallan-Idamean).||||||
23854|Murrawong Creek Formation|67322|4|Described|p3 Fig.1; Fig.5; p27, p28|Middle Cambrian|Middle Cambrian|Tamworth Belt, New England Orogen. (Cawood 1983; Leitch and Cawood 1987). >450m thick. Shelly fauna in the lowermost unit are of Middle Cambrian age. Occurs in the Tamworth-Neminha area. ||||Conformably overlain by the Pipeclay Creek Formation.|Consists largely of volcaniclastic sandstones interbedded with conglomeratic units, the lowermost of which is 65 m thick and dominated by coarse-grained allochthonous limestone blocks.|22-FEB-18
23854|Murrawong Creek Formation|68005|5|Briefly described|p49 Fig.3-M, p50, p151, p170.|Middle Cambrian|Middle Cambrian|Tamworth Belt. Deep marine sedimentary rocks: base of slope fore-arc complex.||||Is overlain by Pipeclay Creek Formation.|Fine to coarse bedded sandstone, limestone conglomerate, argillite and chert.|
23854|Murrawong Creek Formation|68822|5|Briefly described|p329, p343|Drumian|Stage 5|Has a faulted base and lies unconformably below Ordovician strata.  Derived from a low-K calcalkaline western source, which was largely mafic to intermediate but silicic at the base.|ca. 505 - 500 Ma|||Overlain by the Pipeclay Creek Formation. Unconformably overlain by the Haedon Formation.|Consists of beds of sandstone and conglomerate, the latter containing arc-derived clasts of mafic, intermediate and, at the base, silicic volcanics.|
23854|Murrawong Creek Formation|69573|6|Mentioned|p655, 657, 659, 661, 665, 668|||Tamworth area. Contains exotic middle-Cambrian limestone clasts (?intra-oceanic island arc remnants).||||||
23854|Murrawong Creek Formation|70752|6|Mentioned|p125, p141|Middle Cambrian|Middle Cambrian|Organophosphatic brachiopod faunas have been described from allochthonous limestone blocks of this unit.||||||
23854|Murrawong Creek Formation|73440|6|Mentioned|p146|Silurian|Ordovician|Reflects deep marine settings.|||||Deep marine tuffs, turbidites and conglomerates.|
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.|
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|||
31614|Murringo Suite|42726|5|Briefly described|map legend||Silurian|||||||
31614|Murringo Suite|44093|5|Briefly described|p195 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||22-MAR-05
74371|Murruin Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Bindook Gp. Polymictic, massive, mainly clast-supported boulder conglom., + clasts of silicic volcs. and less abundant limest., marble, granite; passes up into volcanic sst. of plagioclase, qtz., pyroxene, minor biotite + prominent dk green vitriclasts||||||18-JUN-08
74371|Murruin Formation|68592|2|Defined|p884, p889-90, p892-7, p1060-1, p1147-55|Pragian|Pragian|See also p741-2. Newly defined, after Murruin Range. Was upper part of former Kowmung Volcaniclastics. The [informal] 'Boulder Conglomerate Member' and overlying 'Lenticle Tuff Member' of Cas et al. (1981) are now included in this unit, with the upper part considered as a possible reworked equivalent of the Barrallier Ignimbrite. Type section described. 230m thick. Joaramin Ignimbrite clasts in the basal conglomerate suggests the base of the Bindook Group is time-transgressive, being considerably younger in the north. Interpreted as sub-aqueous mass-flow deposits.||Unit in Bindook Group.||Conformably overlies Kowmung Formation. Is overlain unconformably by Strathaird Formation. Upper part is correlated with Barrallier Ignimbrite.|Basal clast-supported boulder conglomerate overlain by a massive, dark blue-grey, crystal-rich vitriclast-bearing dacitic volcaniclastic sandstone.|
74371|Murruin Formation|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dkm. Includes two unnamed subunits: massive, clast-matrix supported, boulder conglomerate with clasts of quartz-feldspar-phyric rhyolite, limestone and leucocratic granite; massive, crystal rich, volcaniclastic sandstone. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Bindook Group|Includes two unnamed members.|Erosional at base.|Polymictic, massive, mainly clast-supported boulder conglomerate and massive, crystal rich, dacitic, volcaniclastic sandstone.|
74371|Murruin Formation|70543|5|Briefly described|Map Legend |Devonian|Devonian|Includes two unnamed subunits: massive, clast-matrix supported, boulder conglomerate with clasts of quartz-feldspar-phyric rhyolite, limestone and leucocratic granite; massive, crystal rich, volcaniclastic sandstone.||Bindook Group|Includes two unnamed members||Polymictic, massive, mainly clast-supported boulder conglomerate and massive, crystal rich, dacitic, volcaniclastic sandstone.|
74371|Murruin Formation|71069|6|Mentioned|p135, p143|||Contains conodont fauna fossils. ||Bindook Group ||||
74371|Murruin Formation|71656|5|Briefly described|p13 Fig.2, p39, p40|Pragian|Lochkovian|54 identifiable conodont elements, including three specimens of Flajsella stygia which has a very restricted range in the middle part of the Lochkovian Stage of the Early Devonian. However sample came from clasts providing only a maximum age that may not necessarily reflect the true depositional age of the Murruin Formation. Fig. 2 shows Pragian age for this unit.||Bindook Group||Partially equivalent to Barralier Ignimbrite and Joaramin Ignimbrite.|Limestone clasts in conglomerate.|
74371|Murruin Formation|71700|5|Briefly described|p23|||northern Goulburn Basin. ||||||
27854|Murrumbidgee Group|5252|6|Mentioned|p88||Early Devonian|||||||
27854|Murrumbidgee Group|22768|6|Mentioned|p178|Emsian|Pragian|||||||
27854|Murrumbidgee Group|22857|5|Briefly described|p178, p460 App.1,Tb.A1.6|Emsian|Pragian|Geological Province: Canberra-Yass Shelf.||||||
27854|Murrumbidgee Group|23309|6|Mentioned|p390|||||||||
27854|Murrumbidgee Group|23522|5|Briefly described|p251|Emsian|Pragian|Age: c.940 Ma [??409Ma?].||||||01-MAR-10
27854|Murrumbidgee Group|23898|4|Described|p269|Early Devonian|Early Devonian|Stated to span most of the 15Ma Esmian Stage. Geological Province: Lachlan Fold Belt.||||||20-MAY-08
27854|Murrumbidgee Group|24005|5|Briefly described|p292 Fig.1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||20-MAY-08
27854|Murrumbidgee Group|24250|5|Briefly described|p103, p104 Fig.1|Early Devonian|Early Devonian|||||||
27854|Murrumbidgee Group|24580|5|Briefly described|p827|Emsian|Pragian|Overlies the Black Range Volcanics. Maximum Thickness: 800m. Geological Province: Eastern Lachlan Fold Belt.||||||
27854|Murrumbidgee Group|29648|6|Mentioned|p19|||||||||
27854|Murrumbidgee Group|29989|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27854|Murrumbidgee Group|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
27854|Murrumbidgee Group|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
27854|Murrumbidgee Group|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27854|Murrumbidgee Group|30069|6|Mentioned|p7|||||||||
27854|Murrumbidgee Group|30125|6|Mentioned|p3|||Refer, to Pedder(1967).Early Emsian-early Eifelian possibly.||||||
27854|Murrumbidgee Group|30731|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27854|Murrumbidgee Group|30814|6|Mentioned|Table 2|||||||||
27854|Murrumbidgee Group|31161|5|Briefly described|PA7|||||||||
27854|Murrumbidgee Group|32483|4|Described|p31|||Lower Devonian. Strat. table 1.||||||18-JUN-08
27854|Murrumbidgee Group|32583|6|Mentioned|p371|||Correlated with Lick Hole Fm.||||||
27854|Murrumbidgee Group|32585|4|Described|p207|||||||||
27854|Murrumbidgee Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
27854|Murrumbidgee Group|32672|6|Mentioned|p673|||||||||
27854|Murrumbidgee Group|33326|6|Mentioned|p442|||Emsian & early Eifelian. Fauna.||||||
27854|Murrumbidgee Group|33732|4|Described|p112|||||||||
27854|Murrumbidgee Group|33959|6|Mentioned|p234|||||||||
27854|Murrumbidgee Group|34184|6|Mentioned|p7|||Conodonts. Refers Pedder, Jackson & Philip(1969).||||||
27854|Murrumbidgee Group|34692|5|Briefly described|p186|||||||||
27854|Murrumbidgee Group|34886|6|Mentioned|p103|||||||||
27854|Murrumbidgee Group|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27854|Murrumbidgee Group|35386|3|Fully described|p40|||Overlies Black Range Group. Age discussed p56.||||||18-JUN-08
27854|Murrumbidgee Group|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
27854|Murrumbidgee Group|36441|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Taemas Limestone, Majurgong Formation and Cavan Limestone.||||||
27854|Murrumbidgee Group|37273|6|Mentioned|p247|||||||||
27854|Murrumbidgee Group|38593|6|Mentioned|p85|||||||||
27854|Murrumbidgee Group|40328|6|Mentioned|p1|||||||||
27854|Murrumbidgee Group|40728|6|Mentioned|p173|||||||||
27854|Murrumbidgee Group|41430|6|Mentioned|p17|||||||||
27854|Murrumbidgee Group|42577|4|Described|p25|||||||||
27854|Murrumbidgee Group|42994|6|Mentioned|p4|||||||||
27854|Murrumbidgee Group|43159|5|Briefly described|Fig.2 p4.||Early Devonian|||||||
27854|Murrumbidgee Group|43430|14|Not recorded|p143,map p.144,p144||Early Devonian|L.Dev.above Black Range Gp||||||
27854|Murrumbidgee Group|43431|14|Not recorded|p1262||Early Devonian|Lower Devonian, not Middle Devonian as previously regarded.||||||
27854|Murrumbidgee Group|43461|14|Not recorded|p622|Emsian|Siegenian|||||||
27854|Murrumbidgee Group|43530|14|Not recorded|p1025|Emsian|Siegenian|U.Siegenian-U.Emsian||||||
27854|Murrumbidgee Group|44093|5|Briefly described|p196 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
27854|Murrumbidgee Group|45078|6|Mentioned|p1|||Lower to Upper Emsian(?to Eifelian) age.||||||
27854|Murrumbidgee Group|45147|3|Fully described|M310|||Age on pM314.||||||01-MAR-10
27854|Murrumbidgee Group|46973|6|Mentioned|Fig.17|||||||||
27854|Murrumbidgee Group|47038|6|Mentioned|p121|||||||||
27854|Murrumbidgee Group|48926|6|Mentioned|p40|||P40 et seq.||||||
27854|Murrumbidgee Group|50230|5|Briefly described|Map legend|Emsian|Pragian|Overlies the Black Range Group.||||||
27854|Murrumbidgee Group|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes Majurgong Formation, Fifeshire Shale, Cavan Bluff Limestone, and Taemas Limestone with its 8 limestone members.||||||
27854|Murrumbidgee Group|65214|6|Mentioned|p272|Devonian|Devonian|NSW, Taemas. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27854|Murrumbidgee Group|66197|5|Briefly described|p631 Fig.3b, p632|Emsian|Pragian|Canberra-Yass Basin. Shallow marine limestone. Overlies the Sugarloaf Creek and Kirawin Formations.||||||14-MAR-12
27854|Murrumbidgee Group|66498|6|Mentioned|p45|||Taemas-Wee Jasper area.|||Bloomfield Limestone.|||
27854|Murrumbidgee Group|67820|6|Mentioned|p136 Fig.3|Devonian|Devonian|||||||
27854|Murrumbidgee Group|67823|5|Briefly described|p355, p356 Fig.1, p358, p361, p363-365|Emsian|Pragian|Contains abundant invertebrate fauna of maximum Emsian age.|||Includes Taemas Limestone.|Overlies Kirawin Formation. Disconformably overlain by the Hatchery Creek Group.|Shale/limestone interbeds alternating with more massive limestones.|08-MAY-20
27854|Murrumbidgee Group|68297|6|Mentioned|p186|Devonian|Devonian||||Said to include Receptaculites Limestone Member [of Taemas Limestone]|||
27854|Murrumbidgee Group|68592|4|Described|p980-1037, p1196, p1857-8, p1893-1904|Emsian|Pragian|See also p73, p238-9, p755, p957, p1909. Originally Murrumbidgee Beds of Jenkins (1878); name changed to Murrumbidgee Series by David (1932), and subdivided into 3 stages by Browne (1959). Later renamed Murrimbidgee Group by Pedder et al. (1970) who raised the stages to Formations. 900-1280m thick. Its rich and diverse faunas, from late Pragian to late Emsian, are described. Potential source of large reserves of limestone suitable for industrial use or agricultural lime. Taemas structural zone: deformation described. Pleistocene megafauna are preserved in cave-fill deposits in limestones of this unit.|||Includes Taemas and Cavan Bluff Limestones, Majurgong Formation and Fifeshire Shale.|Conformably overlies Sugarloaf Creek Formation (Black Range Group). Is overlain conformably by Wee Jasper Formation. Faulted against Mountain Creek Volcanics.||
27854|Murrumbidgee Group|70192|5|Briefly described|Map Legend|Emsian|Pragian|On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Cavan Bluff Limestone, Fifeshire Shale, Majurgong Formation, Taemas Limestone.|Overlies Black Range Group.||
27854|Murrumbidgee Group|70540|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Cavan Bluff Limestone, Fifeshire Shale, Majurgong Formation, Taemas Limestone.|||
27854|Murrumbidgee Group|70546|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Cavan Bluff Limestone, Fifeshire Shale, Majurgong Formation, Taemas Limestone|||
27854|Murrumbidgee Group|71040|6|Mentioned|p32|Early Devonian|Early Devonian|SW of Yass. Exhibits four deformations that formed in contractional to contractional/strike-slip regimes.||||||
27854|Murrumbidgee Group|71656|4|Described|p9, p10, p12, Fig.2, p32, p33-38|Emsian|Pragian|The Taemas-Wee Jasper area at the southern boundary of the Yass 1:100,000 mapsheet includes the heritage listed site known as 'Shearsby's Wallpaper', world-famous fossil fish sites (Young 2011), and much researched and diverse invertebrate fauna.|||Fifeshire Shale, Cavan Bluff Limestone, Majurgong Formation, Taemas Limestone.|Overlies Black Range Group and partially underlies Hatchery Creek Group.|Fossiliferous limestone and shales.|
27854|Murrumbidgee Group|71700|5|Briefly described|CD||||||Includes the Cavan Bluff Limestone and the Taemas Limestone.|Overlies the Black Range Group. Potentially equivalent (in part) to the Mulwaree Group.||
27854|Murrumbidgee Group|73215|5|Briefly described|p994-995|||Talmo-Taemas area.|||Cavan Bluff, Taemas Limestones; Majurgong Formation.||Well-bedded sedimentary units of shallow-marine limestone and fluvial deposits. Displays refolded folds and overprinted stylolitic cleavages.|
24413|Murrumbogie Intrusive Complex|730|6|Mentioned|p22 Fig.5.|||||||||11-NOV-14
24413|Murrumbogie Intrusive Complex|22831|4|Described|p 23|Late Silurian|Late Ordovician|Erosional contact with overlying Derriwong Group (Late-Silurian-Early Devonian) found in trench dug at foot of Derriwong Group escarpment.||||||01-NOV-13
24413|Murrumbogie Intrusive Complex|40365|2|Defined|p328|Early Devonian|Early Devonian|||||||01-NOV-13
24413|Murrumbogie Intrusive Complex|40682|5|Briefly described|p2|||||||||
24413|Murrumbogie Intrusive Complex|42912|6|Mentioned|Fig.1|||||||||
24413|Murrumbogie Intrusive Complex|43441|5|Briefly described|13|||?Late Ordovician||||||08-JAN-10
24413|Murrumbogie Intrusive Complex|44160|5|Briefly described|Map Legend||Eastonian|||||||08-JAN-10
31611|Murrumbucka Suite|22719|6|Mentioned|p492|||||||||
31611|Murrumbucka Suite|22779|6|Mentioned|p 179|||||||||
31611|Murrumbucka Suite|22815|5|Briefly described|p55|Silurian|Silurian|||||||
31611|Murrumbucka Suite|24222|5|Briefly described|p18|||Includes the Murrumbucka Tonalite. Geological Province: Lachlan Fold Belt.||||||24-JAN-06
31611|Murrumbucka Suite|42726|5|Briefly described|map legend||Silurian|||||||
31611|Murrumbucka Suite|43233|5|Briefly described|Map Legend||Silurian|Murrumbidgee Batholith.||||||
26067|Murrumbucka Tonalite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Tonalite. BMR map symbol: tmu.||||||
26067|Murrumbucka Tonalite|22815|4|Described|p62|||||||||
26067|Murrumbucka Tonalite|24222|6|Mentioned|p14|||Of the Murrumbucka Suite. Probably derived from mixed igneous and sedimentary sources.  Geological Province: Lachlan Fold Belt.||||||12-SEP-05
26067|Murrumbucka Tonalite|29953|6|Mentioned|p3|||||||||
26067|Murrumbucka Tonalite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
26067|Murrumbucka Tonalite|31581|3|Fully described|p182|||Refers Snelling (1960)||||||
26067|Murrumbucka Tonalite|32820|6|Mentioned|p3|||Murrumbidgee Batholith||||||
26067|Murrumbucka Tonalite|32905|6|Mentioned|Fig.1|||||||||
26067|Murrumbucka Tonalite|32906|6|Mentioned|Fig.1|||||||||
26067|Murrumbucka Tonalite|34544|5|Briefly described|p185|||See also P186||||||
26067|Murrumbucka Tonalite|36413|2|Defined|p79|Silurian|Silurian|||||||
26067|Murrumbucka Tonalite|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Biotite-hornblende tonalite. GSNSW map code: gmt.||||||
26067|Murrumbucka Tonalite|40328|4|Described|p209|||||||||
26067|Murrumbucka Tonalite|43233|5|Briefly described|Map Legend||Late Silurian|Possible Silurian age. Of Murrumbucka Suite.||||||
26067|Murrumbucka Tonalite|45003|14|Not recorded|p81|||||||||
26067|Murrumbucka Tonalite|45147|6|Mentioned|M194|||||||||
26067|Murrumbucka Tonalite|49705|6|Mentioned|p17|||||||||
26067|Murrumbucka Tonalite|65779|5|Briefly described|p291|||Biotite-rich. Includes hornblende-bearing xenoliths correlated with parts of Cooma Complex. North of the main Cooma Complex.||||||
26067|Murrumbucka Tonalite|73154|5|Briefly described|p77, p79, p84|Wenlock|Llandovery|Lachlan Orogen. Of the Murrumbidgee Batholith. 429+/-3 Ma age is for an amphibolite sheet, syn-magmatic relationship with the host Murrumbucka Tonalite inferred by Healy et al. (2004) dates the unit. Amphibolite bodies interpreted as remnants of syn-plutonic doleritic and gabbroic dykes that mingled and hybridised with the host tonalite. Misspelt as Murumbucka Tonalite p79.|429+/-3 Ma crystallisation age||||Includes interspersed amphibolite bodies, strongly deformed.|
70503|Murrurundi Ignimbrite Member|62095|2|Defined|p277 Appdx.|Late Carboniferous|Late Carboniferous|Of the Currabubula Formation. Unwelded red to pink ignimbrite. Overlain by Cohens Gully Ignimbrite Member. Thickness in type section: 70m. Age is probably Westphalian. Geol. Prov: Werrie Block/Tamworth Belt. See also Plate 1, p256 Fig. 7.||||||
77168|Murulla beds|68003|5|Briefly described|p38 Fig.3-j, p130.|Late Permian|Late Permian|Hunter Coalfield, Werrie Basin, Brigalow Belt South Bioregion.||Unit in Singleton Supergroup? or equivalent to ?||Overlies Bickham Formation.|Coal seams, claystone, siltstone, sandstone, conglomerate.|11-SEP-12
77168|Murulla beds|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian coal measures: conglomerate, quartzose and lithic sandstone, siltstone, carbonaceous and calcareous mudstone, tuff and coal.||||||
22487|Musical Tonalite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb28.||||||
22487|Musical Tonalite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
72958|Mutawintji Group|62787|4|Described|p77, p76 Fig. 1|Early Ordovician|Early Ordovician|Includes Tabita Formation and Yandaminta Quartzite. Unconformably overlie Kara Beds.||||||07-FEB-11
72958|Mutawintji Group|62793|5|Briefly described|p269, p270|Early Ordovician|Late Cambrian|Overlies deformed Late Proterozoic to Middle Cambrian Teltawongee beds in Central Koonenberry Belt.|||Comprises Nootumbulla Sandstone, Bynguano Quartzite and Rowena Formation in ascending order.||Marine sedimentary rocks, some fossiliferous limestones.|21-MAR-12
72958|Mutawintji Group|62795|5|Briefly described|p347, p348, p349 Fig.2|Ordovician|Late Cambrian|Formerly Mootwingee Group. Unconformably overlies Gnalta Group and unconformably underlies Snake Cave Sandstone. Comprises Nootumbulla Sandstone, Bynguano Quartzite, Rowena Formation. 2300 m thick.||||||
72958|Mutawintji Group|63121|5|Briefly described|p223-224|Early Ordovician|Late Cambrian|Supersedes Mootwingee Group as a result of a request by the Mutawintji people - to change the spelling  to reflect correct pronunciation.||||||13-MAR-07
72958|Mutawintji Group|64679|5|Briefly described|Map legend|Ordovician|Late Cambrian|Comprises Nuchea Conglomerate, Nootumbulla Sandstone, Bynguano Quartzite and Rowena Formation.||||||
72958|Mutawintji Group|66623|1|Redefined|p58, p99, pp134-151. |Middle Ordovician|Late Cambrian|Formerly part of Torrowangee Series (Mawson 1912), Mootwingee Series (Andrews 1922), redefined by Kenny (1934), Warris (1967), and expanded in this study. A Post-Delamerian fluvio-deltaic sequence. Up to 2300 m thick. Folding in late Ordovician/early Silurian. Correlates with Warratta, Pimbilla Tank and Kayrunnera Groups.|||Includes Nuchea and Bilpa Conglomerates, Nootumbulla Sandstone, Bynguano Quartzite and Gundara Quartzite Member, Rowena and Scropes Range Formations.|Unconformably overlies Gnalta, Teltawongee, Ponto and Grey Range Groups. Is unconformably or disconformably overlain by Wana Karnu Group.|Predominantly quartzite with pebbly sandstones, basal conglomerates and occasional micaceous siltstones; occasional local calcareous beds eg fossiliferous marls at the top of the sequence.|
72958|Mutawintji Group|66918|5|Briefly described|Map legend|Ordovician|Cambrian||||Includes Nuchea Conglomerate, Scropes Range and Rowena Formations, Nootumbulla Sandstone and Bynguano Quartzite.||Folded and weakly cleaved metasedimentary rocks; basal conglomerate overlain by fluvial to shallow marine sandstone and siltstone, fossiliferous marls at the top of the sequence; regionally metamorphosed to prehnite-pumpellyite facies.|
72958|Mutawintji Group|67105|5|Briefly described|p653-654, 659, 661, 663|Early Ordovician|Late Cambrian|Wonnaminta Zone (arc and forearc), Koonenberry Belt. Post-Delamerian Orogeny, Lachlan Orogenic Cycle deposits.|491 - 476 Ma.||Bilpa Conglomerate.||Dominantly fluvial to deltaic sedimentary sequence.|
72958|Mutawintji Group|67208|5|Briefly described|Map legend.|Ordovician|Cambrian||||||Folded and weakly cleaved metasedimentary rocks; basal conglomerate overlain by fluvial to shallow marine sandstone and siltstone; fossiliferous marl at the top of the sequence; regionally metamorphosed to prehnite-pumpellyite facies.|20-SEP-13
72958|Mutawintji Group|67322|4|Described|p8-12; Fig.5|Middle Ordovician|Iverian|Formerly spelt Mootwingee Group (redefined by Greenfield, Mills, and Percival, in Greenfield et al. 2010). Occurs in the Mount Wright-Mutawintji region, central Koonenberry Belt. Represents a rapid transition from fluviatile to shallow marine environments, with significant clastic influx from an extensive delta.|||Nuchea Conglomerate, Nootumbulla Sandstone, Bynguano Quartzite, Rowena Formation, Bilpa Conglomerate, Scropes Range Formation.|Correlated with Pimbilla Tank Group. Lower to middle parts correlate with Kayrunnera Group.|Basal conglomerate, overlain by sandstone, quartzite, siltstone and shale.|22-FEB-18
72958|Mutawintji Group|70648|5|Briefly described|Map Legend|Ordovician|Cambrian||||Includes Rowena Formation.||Folded and weakly cleaved metasedimentary rocks; basal conglomerate overlain by fluvial to shallow marine sandstone and siltstone, fossiliferous marls at the top of the sequence; regionally metamorphosed to prehnite-pupellyite facies.|
72958|Mutawintji Group|70650|5|Briefly described|Map Legend|Ordovician|Cambrian||||Includes Rowena Formation, Bynguano Quartzite, Nootumbulla Sandstone, Scropes Range Formation, Nuchea Conglomerate.||Folded and weakly cleaved metasedimentary rocks; basal conglomerate overlain by fluvial to shallow marine sandstone and siltstone, fossiliferous marls at the top of the sequence; regionally metamorphosed to prehnite-pumpellyite facies.|
72958|Mutawintji Group|70651|5|Briefly described|Map Legend|Ordovician|Cambrian||||Includes Scropes Range Formation.||Folded and weakly-cleaved metasedimentary rocks; basal conglomerate overlain by fluvial to shallow marine sandstone and siltstone, fossiliferous marls at the top of the sequence; regionally metamorphosed to prehnite-pumpellyite facies.|
72958|Mutawintji Group|70749|6|Mentioned|p43|Ordovician|Cambrian|Southern Thomson and Koonenberry area.||||||
72958|Mutawintji Group|70838|5|Briefly described|p268-271, p274, p277-278, p280-281|Cambrian|Cambrian|NW Koonenberry Belt. Possible tectonic settings discussed. Deposition in small post-orogenic pull-apart basins.|||Bilpa Conglomerate, Nootumbulla Sandstone.|Unconformably overlies and is faulted against Gnalta Group.|Generally consists of overall fining-upward sequences of conglomerate, turbiditic sandstone, mudstone and fossiliferous limestone.|
72958|Mutawintji Group|71262|6|Mentioned|p9 Fig 7|Ordovician|Cambrian|||||||
72958|Mutawintji Group|71284|6|Mentioned|p488|Early Ordovician|Late Cambrian|Southern Koonenberry Belt. Successive fluviatile, deltaic and shallow-marine deposits.||||||
72958|Mutawintji Group|71593|6|Mentioned|p189|||||||||
72958|Mutawintji Group|71966|6|Mentioned|p990|Ordovician|Cambrian|Geological province: southern Thomson Orogen.||||||
72958|Mutawintji Group|73059|6|Mentioned|p1061|||Koonenberry Belt.|||Bilpa Conglomerate.|||
72958|Mutawintji Group|73177|5|Briefly described|p1110, 1113|Middle Ordovician|Middle Ordovician|Contains Darriwilian trilobite and fish fossils, giving a maximum age for the Benambran deformation.|||||Fluvial to shallow marine.|
35613|Mutmutbilly Granite|50232|5|Briefly described|Map legend|Pridoli|Ludlow|Part of the Wyangala Batholith.  Grey, porphyritic, microgranular, biotite soda granite and soda granodiorite with miarolitic cavities.||||||
35613|Mutmutbilly Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Gunning Suite. Light grey, med- to coarse-gr., porphyritic biotite granite and granodiorite with a minor component of small microdiorite xenoliths and miarolitic cavities.  Margins comprise porphyritic microgranite and rhyolite. Low K, Th, U...||||||09-SEP-08
35613|Mutmutbilly Granite|68592|2|Defined|p1312-3, p1316-9, p1338-40|Early Silurian|Early Silurian|Nmew name, after Parish of Mutmutbilly. Type area described. Crops out as boulders and blocks in undulating terrain. Geochemistry detailed; geophysical properties described. No isotopic dating.||Unit in Gunning Suite.||Intrudes Abercrombie Formation.|Light grey, sometimes with a greenish or brownish tint, massive, porphyritic granite and granodiorite; minor small microdiorite enclaves. Chilled margins are of porphyritic microgranite and rhyolite.|
35613|Mutmutbilly Granite|70192|4|Described|Map Legend|Ludlow|Wenlock|Sgm. On Gunning 1:100 000 mapsheet portion of Time-Space Plot.||Gunning Suite|||Light grey, medium to coarse grained porphyritic, biotite granite and granodiorite; margins of porphyritic microgranite and rhyolite; minor small microdiorite xenoliths and miarolitic cavities; low radioelement response.|
35613|Mutmutbilly Granite|70541|4|Described|Map Legend|Devonian|Silurian|||Gunning Suite|||Light grey, medium to coarse grained porphyritic, biotite granite and granodiorite; margins of porphyritic microgranite and rhyolite; minor small microdiorite xenoliths and miarolitic cavities; low radioelement response.|
83553|Mutton Bird Point Formation|73554|4|Described|Map legend, back of map|Neogene|Neogene|Lord Howe Island. Part of the Lord Howe Volcanic Complex. Deposits emplaced underwater; includes pillow basalts. Intruded by many dykes of various compositions and textures, most of which strike toward Mount Lidgbird. Located on the south-eastern coast including at Mutton Bird Point, Boat Harbour and George Bay. [Also written as Mutton Bird Point Breccia in accompanying information on the back of the map; probably accidental].||Lord Howe Volcanic Complex|||Basaltic breccia and hyaloclastite (glassy) breccia and basalt pillow lava deposits.|
83553|Mutton Bird Point Formation|73581|6|Mentioned|p28 Fig.8|||||||||
30467|Myalla Road Syenite Complex|22815|2|Defined|p105|Middle Jurassic|Middle Jurassic|K/Ar Ages: Range from 161Ma to 171Ma.||||||
30467|Myalla Road Syenite Complex|22857|6|Mentioned|p295|||Bentonite of possible ceramic clay quality.||||||
30467|Myalla Road Syenite Complex|22865|6|Mentioned|p295|||||||||
30467|Myalla Road Syenite Complex|43233|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|||||||
28274|Myamley Sandstone|22831|3|Fully described|p 54|||Yarra Yarra Creek Group||||||
28274|Myamley Sandstone|22857|4|Described|p446 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Yarra Yarra Creek Group. Max. thickness: 400m. Geological Province: Darling Basin. ||||||
28274|Myamley Sandstone|42449|6|Mentioned|p23|||Reserved 1977, D. Pogson. Last update May 1991.||||||
28274|Myamley Sandstone|42566|4|Described|p107|||||||||
28274|Myamley Sandstone|42568|5|Briefly described|Map legend|Pragian|Pragian|||||||
28274|Myamley Sandstone|43441|6|Mentioned|29||Early Devonian|||||||08-JAN-10
28274|Myamley Sandstone|44160|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||
28274|Myamley Sandstone|61894|6|Mentioned|p179 Fig.3|||||||||
28274|Myamley Sandstone|70751|6|Mentioned|p12|Lochkovian|Lochkovian|||Yarra Yarra Creek Group||||
28274|Myamley Sandstone|72958|6|Mentioned|p11|Lochkovian|Lochkovian|Cobar Basin. Nymagee area.||Yarra Yarra Creek Group, Cobar Supergroup||Underlain by Gwando Siltstone. Overlain by Daalboro Sandstone.||
82600|Myanbah Leucosyenogranite|71628|4|Described|p8: 4, 28, 30, 98-101; p19: 79, 142|||New name (this study) better to reflect its composition. Previously Myanbah Leucomonzogranite of DMR NAND04 Nandewar Geology Integration and Upgrade project, after unpublished work by Chappell and Bryant (1994). Originally Myanbah Leucoadamellite (Binns et al., 1967 after unpublished work by Ransley, 1970). Named after Myanbah Creek. A small ( 2 km2) intrusion c. 6km WSW of Yarrowyck. Crops out as moderately sized tors and large domes, many highly weathered. Unassigned to a Suite. Geochemistry described; has many similarities with The Basin Monzogranite.||Myanbah Suite.||Intrudes Sandon beds and Gwydir River Monzogranite (gradational contact).|Medium-grained, sugary-textured, biotite leucosyenogranite to K-feldspar-rich leucomonzogranite. I-type.|
31523|Myocum Suite|22815|5|Briefly described|p79|||Consists of 4 plutons.||||||
31523|Myocum Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31523|Myocum Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
31523|Myocum Suite|44093|5|Briefly described|p222 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
31523|Myocum Suite|68592|6|Mentioned|p1674|Early Devonian|Early Devonian|||Unit in Glenbog Supersuite.||||
26792|Myra beds|22857|5|Briefly described|p484 App.1 Tb.A1.6|Early Paleozoic|Early Paleozoic|Slate, phyllite, chert, jasper, metabasalt, minor lithic wacke. Max. thickness: ?>4.5km. See also p203.||||||07-NOV-08
26792|Myra beds|22859|6|Mentioned|p203|||||||||
26792|Myra beds|23720|5|Briefly described|Map Legend|||Of the "Woolomin Association".  Slate, phyllite, chert, jasper, metabasalt, minor lithic wacke.||||||15-DEC-04
26792|Myra beds|41348|5|Briefly described|Map legend|Early Paleozoic|Early Paleozoic|Part of the "Woolomin Association".||||||07-NOV-08
26792|Myra beds|44450|3|Fully described|p12 Table 1|Early Paleozoic|Early Paleozoic|Geological Province: New England Fold Belt. Max. thickness >4500 m.||||||07-NOV-08
26792|Myra beds|65317|5|Briefly described|p632 Fig.10|Early Palaeozoic|Early Palaeozoic||||||Alkalic volcanics, limestone, chert.|23-APR-12
26792|Myra beds|71628|5|Briefly described|p17-89; p18-3|||||Woolomin Association.||Is intruded by Big Hill Creek Granite.||
23857|Myrtle Grove Formation|42033|6|Mentioned|p655|||||||||
23857|Myrtle Grove Formation|43363|14|Not recorded|Map Legend|||(Provisional first edition)||||||
27052|Nacka Nacka Metabasic Igneous Complex|22857|4|Described|p132, p414 App. 1 Tb. A1.5|Darriwilian|Yapeenian|Meta-andesites, amphibolites, metagabbro. Age: 465+/-6Ma and 467+/-6Ma (K/Ar hornblende)||||||
27052|Nacka Nacka Metabasic Igneous Complex|23245|6|Mentioned|p132|||||||||
27052|Nacka Nacka Metabasic Igneous Complex|37529|5|Briefly described|p4|||||||||
27052|Nacka Nacka Metabasic Igneous Complex|40678|6|Mentioned|p2|||||||||
27052|Nacka Nacka Metabasic Igneous Complex|42045|6|Mentioned|p149|||||||||
27052|Nacka Nacka Metabasic Igneous Complex|42313|3|Fully described|p30|Middle Ordovician||K/Ar dating: 465+/-6Ma, 467+/-6Ma. Age: Middle Ordovician (pre-Gisbornian)||||||
27052|Nacka Nacka Metabasic Igneous Complex|42314|5|Briefly described|Map|Middle Ordovician||||||||
27052|Nacka Nacka Metabasic Igneous Complex|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Ovg2||||||
27052|Nacka Nacka Metabasic Igneous Complex|44093|5|Briefly described|p67 Fig 6.6|Ordovician|Ordovician|Of Basden (1992). See also pp129 Table 10.1.||||||
27052|Nacka Nacka Metabasic Igneous Complex|63290|6|Mentioned|p403 Fig. 6(c)|Late Silurian|Late Silurian|Geological Province: Wagga Metamorphic Belt. Sillimanite/ K feldspar zone.||||||
27052|Nacka Nacka Metabasic Igneous Complex|67322|5|Briefly described|p20|Ordovician|Ordovician|Tumut area. Age is based on K-Ar dating of hornblende. Attributed to an ocean floor setting (ridge or backarc basin).|~466 Ma (Basden, 1990).||||Tholeiitic mafic volcanics and contains hornblende.|22-FEB-18
22498|Nagero Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
22501|Nalbaugh Granodiorite|22815|4|Described|p82|||||||||
22501|Nalbaugh Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Nalbaugh Suite.||||||
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.||||||
36469|Nallawa Suite|23549|4|Described|p523-524|||A major member of the Boggy Plain Supersuite.  It is part of the Yeovil Batholith. Geological Province: Lachlan Fold Belt .  See also the misspelt Nullawa Suite.||||||11-JUL-13
29689|Nambucca beds|22736|6|Mentioned|p611 Fig2||Permian|||||||
29689|Nambucca beds|22857|5|Briefly described|p516 App.1 Tb.A1.8|Middle Permian|Middle Permian|Max. thickness: >4km. Geological Province: Barnard Basin (Nambucca Basin). ||||||
29689|Nambucca beds|23720|5|Briefly described|Map Legend|||Includes the Bellingen Slate as well as unnamed metasediments, phyllites and volcanics, the Pee Dee beds and Parrabel beds.||||||15-DEC-04
29689|Nambucca beds|43018|6|Mentioned|p390|||||||||
29689|Nambucca beds|43755|6|Mentioned|Fig.1,p548||Permian|||||||
29689|Nambucca beds|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|See also p232 Appendix 1. Geological Province: New England Fold Belt.||||||22-MAR-05
29689|Nambucca beds|44450|3|Fully described|p22 Table 4|Early Permian|Early Permian|Geological Province: Nambucca Block. Max. thickness: 4000m.||||||
29689|Nambucca beds|61770|6|Mentioned|p110|||||||||
29689|Nambucca beds|65114|5|Briefly described|p383 Tb.1|Cisuralian||Listed as Early Permian; 294-291 Ma; Tectonic unit: Southern New England Orogen, Barnard Basin, slivers in Texas Block||||||
29689|Nambucca beds|69188|5|Briefly described|p22, p27|Permian|Late Carboniferous||||Pee Dee beds.|Is intruded by the Valla Adamellite.||
29689|Nambucca beds|70939|6|Mentioned|p826|Permian|Permian|Northern Hastings Block.||||||
29689|Nambucca beds|71628|5|Briefly described|p17: 15, 18, 20, 33, 38|||||||Is intruded by Botumburra Range and Carrai Granodiorites, Valla Monzogranite and Round Mountain Leucomonzogranite.||
29689|Nambucca beds|72528|5|Briefly described|p102.|Permian|Permian|||||Intruded by Botumburra Range Monzogranite.||
22502|Nambucurra Granodiorite|22893|4|Described|p12 table3|||Age: thought to be Early Devonian. no outcrops on the mapping area.||||||
22502|Nambucurra Granodiorite|44188|5|Briefly described|Map Legend||Early Devonian|Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Hornblende-bearing porphyritic granodiorite.||||||15-MAY-08
80154|Namoi Coal Member|70791|6|Mentioned|p289|Permian|Permian|||||||
82609|Namoi Tops Monzogranite|71628|4|Described|p4: 1, 3-5, 17, 24, 39-43, 45, 51,55,58|||New unit: modified from unpublished work by Chappell and Bryant (1994). A composite unit; includes rocks previously ascribed to various other units (mentioned). Named after a local topographic high. Southern New England Orogen. Geochemistry described. Associated with several Sn deposits.|292.3 +/- 1.5 Ma (SHRIMP: Cawood et al., 2011).|Copeton Suite.||Intrudes Cara and ?Whitlow Formations and Sandon beds. Abuts the Copeton, Rocky Glen and Pringles Monzogranites and Giants Den Leucosyenogranite.|Heterogeneous unit comprising white to light grey, medium[- to coarse-grained, weakly to coarsely porphyritic and equigranular biotite-(?) monzogranite. S-type.|
41276|Nandewar Volcanic Complex|50629|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
41276|Nandewar Volcanic Complex|63347|6|Mentioned|p2|||||||||
41276|Nandewar Volcanic Complex|68003|5|Briefly described|p73 Fig.3-q, pp78-79, p126.|Miocene|Miocene|Brigalow Belt South Bioregion. Two main eruptive centres, at Killarney Gap (21 - 20 Ma) and Mount Kaputar (18 - 16 Ma). Named as Nandewar Volcanic field on p.126.|21 - 16 Ma.||||Rhyolite plugs and flows (Killarney Gap) and basalts, alkali rhyolites and trachytes (Mount Kaputar), tuff; minor interbedded diatomite.|
41276|Nandewar Volcanic Complex|68004|6|Mentioned|p212.|||||||||
41276|Nandewar Volcanic Complex|68005|6|Mentioned|p169 Plan 1, p170.|Tertiary|Tertiary|||||||
41276|Nandewar Volcanic Complex|68006|5|Briefly described|p20 Fig.3-A, p100, p120, p164.|Tertiary|Tertiary|High quality diatomite has been extracted from this unit in the Barraba area. Volcanic opal has been recovered from this unit.|c. 18 Ma.||||Includes basaltic and trachytic lava flows and pyroclastic tuffs.|
41276|Nandewar Volcanic Complex|70036|5|Briefly described|Map legend|||Included in a mapped unit of Tertiary volcanic rocks: trachyte, basalt, nephelinite, syenite, rhyolite, monzonite and tuff.||||||
41276|Nandewar Volcanic Complex|70791|5|Briefly described|p279|Miocene|Miocene|Gunnedah Basin.||||||
26071|Nangahrah Formation|721|5|Briefly described|Map legend|Late Devonian|Silurian|Of the Woolomin Group.  Low-grade, regionally metamorphosed. multiply deformed cherts, siliceous mudrocks, olistostromal chert, pillow basalt, minor limestone, in basaltic clastic matrix.||||||21-DEC-04
26071|Nangahrah Formation|22857|4|Described|p484 App.1 Tb.A1.6|Late Devonian|Middle Silurian|Of the Woolomin Group. Locally interfingers with Bobs Creek Formation. Cherts, mudrocks, pillow basalt. Geological Province: Woolomin Basin. ||||||
26071|Nangahrah Formation|23050|4|Described|p15 Table 1|Late Devonian|Silurian|Age: Middle Silurian to latest Devonian; part possibly as old as Ordovician; part possibly as young as early carboniferous.||||||
26071|Nangahrah Formation|23051|5|Briefly described|Map Legend|Middle Devonian|Early Silurian|of Woolomin Group.||||||
26071|Nangahrah Formation|41328|2|Defined|p13|Early Carboniferous|Middle Devonian|Reserved as Nangarah||||||
26071|Nangahrah Formation|41329|5|Briefly described|p5|||||||||
26071|Nangahrah Formation|42554|5|Briefly described|p38|||||||||
26071|Nangahrah Formation|42631|5|Briefly described|Fig.1 P265|||||||||
26071|Nangahrah Formation|42748|6|Mentioned|Fig.3 P9|Devonian|Silurian|||||||
26071|Nangahrah Formation|42866|5|Briefly described|Table 2, P12|||||||||
26071|Nangahrah Formation|43091|5|Briefly described|Map legend|||||||||
26071|Nangahrah Formation|65398|1|Redefined|p4-6, p8, p10, p14; Tb.1, Fig 2-6|Late Devonian|Late Silurian|Of the Woolomin Group. Laterally persistent; low-grade regionally metamorphosed, abundant multiply-deformed chert, jasper, siliceous argillite, minor wacke and mafic volcanic rocks.||||||
26071|Nangahrah Formation|66720|5|Briefly described|Map legend|Late Devonian|Late Silurian|||Unit in Woolomin Group.|||Massive to bedded chert, jasper, siliceous argillite, minor diamictite and conglomerate; rare basalt.|
26071|Nangahrah Formation|68003|5|Briefly described|p140.|Devonian|Silurian|||Unit in Woolomin Group.|||Low grade regionally metamorphosed, multiply deformed chert, lithic and volcaniclastic wacke, breccia, basic volcanics, siltstone, mudstone and rare limestone.|
26071|Nangahrah Formation|68005|4|Described|pp26-28, p157, p170.|Early Carboniferous|Middle Devonian|Central Block, New England Fold Belt. Forms a narrow, elongate belt of sediments parallel to Peel Fault. Text says age is from radiolarian biostratigraphy: Appendix 4 gives age as Silurian with no further explanation. Low radiometric response; magnetic response is higher than Bobs Creek Formation. Low grade regionally metamorphosed and multiply deformed.||Unit in Woolomin Group.||Overlies Woodsreef Melange. Is overlain by Bobs Creek Formation, gradationally to thrust fault contact.|Basal metabasalt overlain by chert, lithic and volcaniclastic wacke, breccia, basic volcanics, siltstone, mudstone and rare limestone.|
27517|Naradhan Sandstone|22857|5|Briefly described|p212-213, p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Cocoparra Group. Massive quartzose sandstone. Max. thickness: 520m. Geological Province: Barka Basin. See also p488 App.1 Tb.A1.7.||||||
27517|Naradhan Sandstone|22859|5|Briefly described|p212|||||||||
27517|Naradhan Sandstone|32676|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27517|Naradhan Sandstone|34109|4|Described|Table 3.11|||See also p172.||||||25-MAR-08
27517|Naradhan Sandstone|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27517|Naradhan Sandstone|36316|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27517|Naradhan Sandstone|43507|14|Not recorded|p125|||||||||
27517|Naradhan Sandstone|43511|4|Described|p129,132,134,139-145||Late Devonian|p147-48||||||
27517|Naradhan Sandstone|44534|5|Briefly described|map legend||Late Devonian|SI 55-6. Upper Dev., part of the Cocoparra Group, O/lies the Barrat Conglomerate, U/lies the Confreys Shale Member.||||||
27517|Naradhan Sandstone|61964|3|Fully described|p14 Fig. 4, p114, p117 Fig. 35, p118-119|Frasnian|Frasnian|Of Cocoparra Group. Medium- to thick-bedded, coarse- to med.-gr. qtz sst grading upwards to finer sst; off-white through to light maroon. Overlain by Merungi Gap Conglomerate Member, Confreys Formation; overlies Barrat Formation. Max. thickness: 778m. ||||||
27517|Naradhan Sandstone|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. White to maroon, medium- to coarse-grained quartz sandstone, medium to thick bedded.||||||
27517|Naradhan Sandstone|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.||Overlies Barrat Formation. Is overlain by Confreys Formation.|White to maroon, medium- to coarse-grained quartz sandstone, medium- to thick-bedded.|
27517|Naradhan Sandstone|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|||White to maroon, medium- to coarse-grained quartz sandstone, medium- to thick-bedded.|
27517|Naradhan Sandstone|71889|5|Briefly described|p8, p48-p50, p52-p54|||Originally defined by Connolly (1962, 1965)  in the eastern and northern margins of the Cocoparra Syncline. Outcrops on the Cargelligo 1:250k sheet area. The former Narrandera Sandstone is now recognised as the southern continuation of this unit. An unnamed informal unit is recognised in places between this formation and the Barrat Formation.||Cocoparra Group||Equivalent to and conformably overlies the Barrat Formation.|Quartz sandstones.|
27517|Naradhan Sandstone|72083|5|Briefly described|p45|||North of Rankin Springs.||Cocoparra Group.||Overlies Barrat Formation. Is overlain by Confreys Formation.||
29826|Nargong Volcanics|22857|5|Briefly described|p458 App.1, Tb.A1.6|Silurian|Silurian|Of the Cudal Group. Andesite, porphyritic in plagioclase, augite and rare orthopyroxene, sericitised andesite. Max. thickness: 750m. Geological Province: Cowra Trough.||||||10-MAR-06
29826|Nargong Volcanics|23214|3|Fully described|p113|Wenlock|Wenlock|Of Cudal Group. Originally mapped as part of Walli Volcanics.||||||17-JUL-08
29826|Nargong Volcanics|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of andesite, porphyritic in plagioclase, augite and rare orthopyroxene; sericitised andesite.||||||17-JUL-08
29826|Nargong Volcanics|43782|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Cudal Group.||||||17-JUL-08
29826|Nargong Volcanics|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group|||Two major felsic to intermediate volcaniclastic and pyroclastic units.|19-MAY-16
23864|Naringla Granodiorite|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Complex.||||||
23864|Naringla Granodiorite|23170|3|Fully described|p217|Early Devonian|Early Devonian|of Yeoval Complex, Yeoval Batholith.||||||
23864|Naringla Granodiorite|24519|6|Mentioned|p90|||Mafic phase of the Yeoval Complex.||||||25-MAY-05
23864|Naringla Granodiorite|39658|4|Described|M58|||See also M56||||||
23864|Naringla Granodiorite|40882|6|Mentioned|Table 1|||||||||
22512|Narooma Chert|22815|2|Defined|p15,16|Early Cambrian|Late Cambrian|New Name. Bed thickness not known.||||||20-JUL-15
22512|Narooma Chert|22857|4|Described|p135, p432 App. 1 Tb. A1.5.|Early Ordovician|Late Cambrian|Of the Wagonga Group. Overlies Kianga Basalt. Max. thickness: 600m. ||||||
22512|Narooma Chert|23213|5|Briefly described|Fig.10 p24|Chewtonian|Bendigonian|Age: Middle Bendigonian to Chewtonian.||||||
22512|Narooma Chert|23245|5|Briefly described|p135|Early Ordovician|Late Cambrian|||||||
22512|Narooma Chert|43233|5|Briefly described|Map Legend|Gisbornian|Late Cambrian|of Wagonga Group.||||||
22512|Narooma Chert|44093|5|Briefly described|p225 App. 1|Ordovician|Cambrian|Of the Wagonga Group. Geological Province: Lachlan Fold Belt.||||||
22512|Narooma Chert|60902|3|Fully described|p860, p865, p866, p879 App.1|Middle Cambrian|Middle Cambrian|Of Wagonga Group. Divided into lower and upper cherts, the latter interbedded with shales bearing Eastonian graptolites. Conformably overlain by Bogolo Formation (and former Kianga Basalt). Geological Province: Narooma Terrane. See also p861 Fig. 2a.||||||02-OCT-15
22512|Narooma Chert|61731|5|Briefly described|p1035-1040|||Geological Province: Lachlan fold Belt/Narooma Terrane.||||||
22512|Narooma Chert|66196|4|Described|p618, 616, 617|Late Ordovician|Cambrian|500-700m thick. Includes Darriwilian to Gisbornian conodonts. Pelagic deep-sea environment. Upper is light-grey and black siliceous mudstone and contains white clay-rich beds. Contains conodonts.||||||
22512|Narooma Chert|67322|4|Described|Fig.5; p26-27, p39|Late Ordovician|Late Cambrian|Narooma Terrane. Defined by Glen (1994). Ribbon chert contains conodonts that range from the late Cambrian to Darriwilian-Gisbornian. Occurs in the Narooma region.||Of the Wagonga Group.||Overlain gradationally by the Bogolo Formation.|Lower part consists of ribbon chert containing conodonts. Upper part has extensively bioturbated chert beds alternating with shale and siltstone beds that contain Eastonian graptolites.|22-FEB-18
22512|Narooma Chert|67849|6|Mentioned|p22 Fig.1.|||||Unit in Wagonga Group.||||
22512|Narooma Chert|68255|6|Mentioned|p1051|Ordovician|Cambrian|||Of the Wagonga Group||||
22512|Narooma Chert|68309|5|Briefly described|p225-226|Late Ordovician|Middle Cambrian|Stratigraphic relations deceptive due to subduction-related thrust faulting.||Wagonga Group.||Is overlain by Bogolo Formation.|Chert, shale, siltstone.|
22512|Narooma Chert|68466|5|Briefly described|p65-67, 69-70|Late Ordovician|Late Cambrian|Narooma Terrane. Graptolites are occasionally common in black shales in the upper parts of this unit.||Wagonga Group.||Is overlain by Bogolo Formation.|Slates interbedded with ribbon cherts (with a diverse conodont fauna), pale yellow translucent cherts darkening upwards. In upper parts, chert beds alternate with Eastonian graptolite-bearing shale and siltstone.|
22512|Narooma Chert|69668|5|Briefly described|p929 Fig.2, p932|Late Ordovician|Late Cambrian|Narooma terrane.||Unit in Wagonga Group.||Is overlain by Bogolo Formation.|Slates interbedded with ribbon cherts, pale yellow to black as silt content increases up-section, with Furongian to Darriwilian conodonts; overlain by chert beds to 30cm thick alternating with shale and siltstone containing Eastonian graptolites.|
22512|Narooma Chert|70026|5|Briefly described|p40-41, p44|||Geological province: Lachlan Orogen. Highly deformed; abundant upright to steep, west-inclined, tight to isoclinal, eastverging folds as well as west-dipping thrust faults.||Unit of Wagonga Group.||Overlain conformably by Bogolo Formation where present, or gradatonally with Adaminaby Group.|Chert and mudstone, including altered basalt.|17-JUL-19
22512|Narooma Chert|70493|6|Mentioned|p56|Late Cambrian|Late Cambrian|Narooma Zone, Lachlan Orogen.||||Is overlain by Adaminaby Group.||
22512|Narooma Chert|70601|5|Briefly described|p23, p26-27, p42-50, p53-54, p57|Ordovician|Late Cambrian|Proposed origins discussed. Deposited on "Seamount Basalt". Late Cambrian to Eastonian conodonts and Eastonian graptolites.||Wagonga Group||Conformably overlies and is interbedded with Adaminaby Group. Overlies "Seamount Basalt". Underlies Bogolo Formation conformably.|Black siliceous mudstone; 5-10cm black shale, 0.5-4cm cherts, silt laminations, mudstones and rare sandstones interbedded; very fine-grained highly deformed black phyllitic chert with isotropic phosphatic lenses. Conodont fauna.|
22512|Narooma Chert|73059|5|Briefly described|p1053 Fig.2, 1059|Late Ordovician|Late Ordovician|Is shown on p1059 as overlying and underlying the Adaminaby Group.||||Overlies Adaminaby Group.|Chert and mudstone.|
77554|Narrabri Formation|66891|5|Briefly described|p183.|||Liverpool Plains. Low salinity groundwater rises through the underlying Gunnedah Formation before dissolving salt stores in this unit, producing salinised catchments.||||Overlies Gunnedah Formation.|Black and grey cracking clays occurring as shoestrings and lenses.|
77554|Narrabri Formation|68240|6|Mentioned|p9-13|Pleistocene|Pleistocene|Liverpool Plains. Braided stream deposits. Groundwater is saline.|||||Predominantly black, grey and brown clays, with laterally discontinuous channel deposits resulting in shoestring sand lenses.|
24420|Narrabundah Ashstone Member|22768|6|Mentioned|p176|||||||||
24420|Narrabundah Ashstone Member|22857|4|Described|p176, p462 App.1 Tb.A1.6|Silurian|Silurian|Strongly jointed massive tuffaceous arenite and fine to medium-grained tuff at top of Canberra Formation. Max. thickness: 70m. ||||||
24420|Narrabundah Ashstone Member|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24420|Narrabundah Ashstone Member|37728|4|Described|Table 2|||||||||
24420|Narrabundah Ashstone Member|38664|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24420|Narrabundah Ashstone Member|39947|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24420|Narrabundah Ashstone Member|42727|5|Briefly described|map legend|Wenlock|Wenlock|Of Canberra Formation. Tuffaceous sandstone, tuff and ashstone. BMR map symbol: Smn. Geol. Prov: Canberra Block.||||||
24420|Narrabundah Ashstone Member|42820|2|Defined|p21|Early Silurian||Of Canberra Formation.||||||22-MAY-08
24420|Narrabundah Ashstone Member|43158|6|Mentioned|3||Early Silurian|Member of Canberra Formation||||||
24420|Narrabundah Ashstone Member|49043|5|Briefly described|p7|||||||||
24420|Narrabundah Ashstone Member|73211|6|Mentioned|p909, p911|||||Canberra Formation||||
31617|Narraburra Suite|24417|6|Mentioned|p111|||||||||
31617|Narraburra Suite|42726|5|Briefly described|map legend||Late Devonian|||||||
31617|Narraburra Suite|44093|5|Briefly described|p182 App. 1|Early Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
31617|Narraburra Suite|44192|5|Briefly described|Map Legend|||||||||
31617|Narraburra Suite|60423|5|Briefly described|p372 Fig. 3|Late Devonian|Late Devonian|Of the Narraburra Complex. Age: 358 +/- 9 Ma. Peralkaline granites. Geological Province: Lachlan Fold Belt.||||||30-APR-10
31617|Narraburra Suite|71206|6|Mentioned|p373, 383-384|||Lachlan Fold Belt. Geochemistry discussed.|||Narraburra, Pinehurst, Boginderra Granites.||Peralkaline granites.|
31617|Narraburra Suite|72084|5|Briefly described|p54, p55 Fig.57, p56|||Similar geochemistry to the ignimbrite unit of the Hervey Group in the Curraburrama State Forest. Geochemical plots. Interpreted as the intrusive counterpart to the ignimbrite unit in the Curraburrama State Forest.|375.3 +/- 4.1 Ma (Kemp et al., 2005).||||Peralkaline A-type granites.|
33406|Narragudgil Volcanics|22434|4|Described|11|Ordovician|Ordovician|Geol province Lachlan Fold Belt||||||
33406|Narragudgil Volcanics|24215|5|Briefly described|p806|||Geological Province:  Lachlan Fold Belt||||||
33406|Narragudgil Volcanics|24417|3|Fully described|p37|Early Silurian||Previously have been included as part of the Bland Diorite (Wyborn, 1996) and the Gidginbung Volcanics (Warren et al 1995).||||||
33406|Narragudgil Volcanics|50385|5|Briefly described|Map Legend|Ordovician|Ordovician|Gabbro, andesite, diorite, basaltic andesite. Metamorphosed to greenschist and amphibolite.||||||
33406|Narragudgil Volcanics|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||13-JUL-04
33406|Narragudgil Volcanics|63278|6|Mentioned|p145 Fig. 1|Ordovician|Ordovician|||||||07-FEB-11
33406|Narragudgil Volcanics|63289|6|Mentioned|p372|Late Ordovician|Late Ordovician|Geological Province: Junee - Narromine Volcanic Belt. Minor inferred tholeiitic basalts.||||||07-FEB-11
33406|Narragudgil Volcanics|63290|6|Mentioned|p407|Ordovician|Ordovician|Intruded by dykes containing zircons with U/Pb SHRIMP ages of 443+/-10Ma (Duggan 2000). Geological Province: Junee - Narromine Volcanic Belt.||||||
33406|Narragudgil Volcanics|67322|4|Described|p20|Telychian||Defined by Duggan, in Lyons et al. (2000). West Wyalong area. The minimum age is based on an intrusion. Attributed to an ocean floor setting (ridge or backarc basin).|Minimum age 433.7 +/- 2.3 Ma|||Is intruded by Bland Diorite.|Mafic tholeiitic rocks that are geochemically primitive, display low K2O, and have a flat REE pattern.|22-FEB-18
33406|Narragudgil Volcanics|68822|6|Mentioned|p335|Telychian||Predates the Early Silurian Bland Diorite (433.7 +/- 2.3 Ma).||||||
33406|Narragudgil Volcanics|70684|6|Mentioned|p3|||||||||
33406|Narragudgil Volcanics|72495|5|Briefly described|p217, p234|||Coincides with a small part of the south-western gravity high that was centered on 34degrees S. Probably Ordovician.|||||Tholeiitic volcanics.|05-APR-20
73364|Narrama Formation|67322|4|Described|p14, p19; Fig.5|Middle Ordovician|Early Ordovician|Hermidale Terrane. New name, defined by Burton et al. (in press). Contains index conodonts spanning late Lancefieldian to early Castlemainian in age. Occurs in the Sussex-Byrock region. Mis-spelt three times as Narrawa on p14.||Of the Girilambone Group|Kaiwilta Member, Mount Dijou Volcanic Member|Overlain by the Whinfell Chert Member (Ballast Formation).|Thick to thin bedded quartz-rich turbiditic sandstone grading to siltstone, interbedded with thin chert horizons; basaltic volcanics of oceanic intraplate affinity.|22-FEB-18
73364|Narrama Formation|68466|5|Briefly described|p65-67|Middle Ordovician|Early Ordovician|Hermidale Terrane. Conodonts indicate Floian age.|||Kaiwilta, Mount Dijou Volcanic, Members.||Dominated by thick- to thin-bedded quartz-rich sandstone locally grading to siltstone; thin (sometimes laterally extensive) chert horizons present.|
73364|Narrama Formation|69094|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Also includes three un-named but separately-mapped sub-units.|||Includes Kaiwilta Member and Mount Dijou Volcanic Member.||Undivided: variably metamorphosed quartzose and micaceous sandstone, siltstone, claystone, phyllite, minor chert, local mafic volcanic rocks, and slate and schist; radiolarians and conodonts in fine-grained rocks.|
73364|Narrama Formation|69095|5|Briefly described|Map legend|Early Ordovician|Early Ordovician||||||Variably metamorphosed quartzose and micaceous sandstone, siltstone, claystone, phyllite, minor chert, local mafic volcanic rocks, slate and schist; radiolarians and conodonts in fine-grained rocks.|
73364|Narrama Formation|69541|5|Briefly described|p652|Early Ordovician|Early Ordovician|Chert beds contain conodonts of late Lancefieldian to latest Chewtonian age.||Basal unit in Girilambone Group.|||Includes thin chert beds.|
73364|Narrama Formation|69635|4|Described|p88-104, p69|Early Ordovician|Early Ordovician|North-western Lachlan Orogen. Age from conodonts: late Lancefieldian to Chewtonian, but top and base unconstrained. U-Pb SHRIMP zircon maximum depositional age given.|496.0+/-2.5 Ma|Of Girilambone Group.|Includes Budgery Sandstone Member.||Sample: very hard, dark grey, medium grained, poorly sorted, feldspathic sandstone. Generally turbidites quartz-mica rich rather than feldspathic. Includes mafic rocks of both ocean island basalt (OIB) and mid-ocean ridge basalt (MORB) affinity.|
73364|Narrama Formation|69668|5|Briefly described|p929 Fig.2, p930 Fig.3, p931|Early Ordovician|Early Ordovician|Hermidale terrane, central NSW. Contains Floian conodonts Paracordylodus gracilis and Oepikodus evae.||Unit in Girilambone Group.|Includes Kaiwilta Member and Mount Dijou Volcanic Member.|Is overlain by Ballast Formation.|Mainly thick- to thin-bedded quartz-rich sandstone locally grading to siltstone; thin, sometimes laterally extensive, chert horizons.|
73364|Narrama Formation|70602|5|Briefly described|p66,Fig 2, 67,72|Middle Ordovician|Early Ordovician|Aeromagnetic map data given.||Girilambone Group|Includes Budgery Sandstone Member, Kaiwilta Member, Mount Dijou Volcanic Member, informal Jasper unit.||Contains rare thick packages of medium-grained metasandstone quartzite termed the Budgery Sandstone Member.|
73364|Narrama Formation|70828|5|Briefly described|p14|||||Unit of Girilambone Group.|Includes Mount Dijou Volcanic Member and Kaiwilta Member.|||
73364|Narrama Formation|70941|2|Defined|pviii- pxii, p4 ph4, p6|Chewtonian|Lancefieldian|Name derived from Narrama Parish. Rocks of this unit were previously just referred to as Girrilambone Group. Contains a number of unnamed informal subunits. Generally poor outcropping and forms low hills; some exposure occurs in gullies. Type locality is nominated and briefly described. Age derived from fossil assemblage. Thickness is unknown but estimated to be a few kilometres thick. Lithology discussed in great detail. Deposited as turbidites in a deep water marine environment. Structure, metamorphism, geochemistry, geophysical characteristics, fossil assemblage and distinguishing characteristics discussed. Hosts minor copper mineralisation at the Tritton copper mine. Contains an informal unit of Jasper. See also   p7 fig 3, p8 fig 4,  p13 fig 7, p12, p16-31, p38-41, p61 fig 28, p63, p69 ph 36, p84, p91, p117, p124 fig 54, p125-p128, p130, p133, p135, p136, p139, p140 fig 58, p142, p143, p145, p147, p149.||Girilambone Group||Conformably overlain (or faulted against) the Ballast Formation or Lang Formation. Unconformably overlain by the Meryula Formation. Probable correlative of the Lower Clements Formation (Wagga Group)|Turbiditic sequence of interbedded, medium grained, cleaved,  very fine- coarse grained, moderately -well sorted sandstone and siltstone/slate/phyllite/schist, cherty siltstone and minor thin chert beds. Localised jasper and quartzite also occur.|
73364|Narrama Formation|71345|6|Mentioned|p31|||References: Trigg in Burton et al. 2012, pp. 60-63; Bervin 1997. See p31, this study.|||||Micaceous cross-laminated siltstone (in outcrop); schistose siltstones intersected in drillholes.|
73364|Narrama Formation|71360|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Geophysical signature: broad areas of low magnetic intensity; rare discontinuous linear  trends with slightly elevated magnetic intensity occur parallel to regional foliation directions.||Girilambone Group.|Kaiwilta Member, Budgery Sandstone Member and Mount Dijou Volcanic Member.||Fine- to coarse-grained, quartzose and quartz-lithic sandstone, with siltstone, claystone, chert and minor basic volcanic rock. The degree of metamorphism varies.|
73364|Narrama Formation|71693|5|Briefly described|Map legend.|Ordovician|Ordovician|||Girilambone Group.||Is overlain by Lang and Ballast Formations [?].|Interbedded sandstone, siltstone, slate, phyllite, schist with rare chert horizons.|13-SEP-19
73364|Narrama Formation|72080|5|Briefly described|p2, p4, p9, p12-p13|Chewtonian|Lancefieldian|Early Ordovician age is derived from conodont fossils in the rare chert units up to 2 m thick.||Girilambone Group|||Terrigenous turbidites with minor mafic volcanics and rare chert horizons.|07-JAN-22
73364|Narrama Formation|72296|1|Redefined|6ix-x, p5-17, p19-22, p24-28, p31, p39|Early Ordovician|Early Ordovician|See also p41, p49, p51, p57-59, p61-62, p65-66, p68, p71, p75, p77, p81-82. Burton et al. (2012). Named after the Parish of Narrama, where one of the type areas is located. See p9 for the various locally-named units which have been suppressed in favour of the Narrama Formation. No type section because of structural complexity and poor exposure; type locality is between 31 degrees 21'41" S, 146 degrees 18'26" E and 31 degrees 22'05" S, 146 degrees, 17'46" E. Very similar to Lang Formation; distinguishing features described. Thickness estimated at a few kilometres. Occurs over most of the COOLABAH 100K sheet area. Forms low hilly country; exposure generally poor. Strongly ferruginised ("ironstone"). No macrofossils; age from conodonts. Hosts significant VAMS Cu mineralisation (described in detail) and orogenic gold veins. Numerous photographs. Deformed at 434 +/- 3.5 Ma (Fergusson et al., 2005). Conodont species listed.|496 +/- 2.5 Ma (MDA: Fraser et al., 2014).|Girilambone Group.|Budgery Sandstone, Birrimba, Members.|Is faulted against (locally may conformably underlie) Lang Formation. Is intruded by Byrock Granite and Coolabah Monzodiorite. Equivalent to lower part of the Clements Formation.|Interbedded medium-grained, cleaved sandstone and siltstone/slate/phyllite, cherty siltstone and minor thin cherts with common vein quartz float; contains very coarse- and coarse-grained metasandstone. Mafic volcanic rocks are distinctive.|
73364|Narrama Formation|72908|6|Mentioned|p11|Early Ordovician|Early Ordovician|Hosts minor copper mineralisation at the Melrose deposit.||Girilambone Group||||
73364|Narrama Formation|73175|6|Mentioned|p1059|||Lachlan Orogen, northern.||Girilambone Group|Mount Dijou Volcanic Member|||
73364|Narrama Formation|73177|5|Briefly described|p1113-1115 Figs.15-17|Ordovician|Ordovician|Eastern Lachlan Orogen.||Girilambone Group.||||
73364|Narrama Formation|73264|6|Mentioned|p1390 Fig.12|Middle Ordovician|Middle Ordovician|Hermidale Terrane. Shown as Narrama Fm.||Girilambone Group||||
79859|Narrandera Sandstone|71889|5|Briefly described|p8, p48, p64|||Originally defined by Trigg (2017). Obsolete name as it is recognised in this study as a southerly continuation of the Melbergen Sandstone.||Cocoparra Group||Overlies the Bogolong Formation. Equivalent to the Melbergen Sandstone.||
79859|Narrandera Sandstone|72083|3|Fully described|p7, p39-41, p45-50, p56-57|||New name, after the town which is built at least in part on the Formation; a subdivision of previously undifferentiated Cocoparra Group. Stratigraphy doubtful: this unit, as well as the Bogolong Formation, may be parts of the Barrat Formation; discussed. A suitable type area is a quarry/borrow pit on the S side of the Old Wagga Road at GR 465920 6153580 on Narrandera 1:100k sheet. Interpreted to have been deposited in a moderately high energy braided stream environment. Estimated thickness c.250-300m. Forms broad but isolated rises separated by areas of no outcrop. The basal conglomerate is lithologically indistinguishable from the underlying Barrat Formation. No fossils found.||Cocoparra Group.||Conformably overlies Bogolong Formation. Probable correlative of Bygoo Hills sandstone.|Well-laminated to locally massive, medium-grained quartz-rich sandstone; conglomerate to pebbly sandstone commonly developed at the base to 5m.|31-AUG-19
25331|Narrangullen Rhyolite|30069|6|Mentioned|p12|||Map on P12.||||||
25331|Narrangullen Rhyolite|32585|6|Mentioned|Fig.3|||||||||
25331|Narrangullen Rhyolite|33732|6|Mentioned|p112|||||||||
25331|Narrangullen Rhyolite|34403|6|Mentioned|p141|||Alternative name for Mountain Creek Volcanics||||||
25331|Narrangullen Rhyolite|34405|6|Mentioned|Fig.3.12|||||||||
25331|Narrangullen Rhyolite|43344|14|Not recorded|p119,120||Devonian|||||||
25331|Narrangullen Rhyolite|45078|6|Mentioned|p2|||On locality map P2.||||||
25331|Narrangullen Rhyolite|45147|6|Mentioned|M179|||||||||
25331|Narrangullen Rhyolite|68592|6|Mentioned|p948|||Browne (1959), replacing the name Mountain Creek Volcanics of Joplin et al. (1953) after Walpole (1949). Discarded, as the latter has priority.||||||
33802|Narrawa Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Leucocratic massive porphyritic biotite granite with miarolitic? cavities.||||||26-NOV-13
33802|Narrawa Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Burrawinda Suite. Cream to white, coarse-grained, equigranular, leucocratic granite. High K and low Th radioelement response.||||||26-NOV-13
33802|Narrawa Granite|68592|2|Defined|p1354-5, p1365-7|Late Silurian|Early Silurian|New name, after Narrawa Parish and Narrawa Creek. Formerly included (Chappell et al., 1991) in Wallah Granite. Crops out as two rather small plutons forming low hills and rises. Type locality described. Geophysical properties described. Not isotopically dated; age from parent unit and intrusive relationships.||Unit in Burrawinda Suite.||Intrudes Mulgowrie Granodiorite and Wallah Granite.|Cream to white, coarse-grained, equigranular, leucocratic granite; has undergone low greenschist facies metamorphism.|
33802|Narrawa Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Swn. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Burrawinda Suite|||Coarse grained, equigranular, leucocratic granite. High K and low Th response.|
33802|Narrawa Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Burrawinda Suite|||Coarse grained, equigranular, leucocratic granite. High K and low Th response.|
80155|Narrawolga Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Werrie Basin. Shown only as Narrawolga. Ending assumed from references to other Coal Members in text.||Rowan Formation.||||28-SEP-17
68843|Narromine Igneous Complex|24518|6|Mentioned|p66|||High-K monzogabbros, monzodiorites and more evolved rocks.||||||
68843|Narromine Igneous Complex|63277|6|Mentioned|p138|Early Ordovician|Early Ordovician|From the Maquarie Arc. Consists dominantly of dacitic porphyries, dorites and granodiorites. Geological Province: Lachlan Fold Belt.||||||27-SEP-07
68843|Narromine Igneous Complex|63278|6|Mentioned|, p148, p145 Fig. 1, p146 Fig. 2a|Odrovician|Early Ordovician|Geological Province: Junee-Narromine Volcanic Belt, LFB. Consists of lavas and volcaniclastics. Intrudes by mid-Ordovician monzodioritic to granodioritic rocks.||||||07-FEB-11
68843|Narromine Igneous Complex|63279|6|Mentioned|p167|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt. North part of province.||||||
68843|Narromine Igneous Complex|63283|5|Briefly described|p193, p185, p188, p194 Fig.2, p191 Tb. 2|Middle Ordovician|Early Ordovician|Age: 448Ma (dacite and granodiorite). Geological Province: Junee-Narromine Volcanic Belt. Consists of basaltic and andesitic volcanics and volcaniclastic sedimentary rocks intruded by large plutons with ages between 465-445Ma.||||||07-FEB-11
68843|Narromine Igneous Complex|63284|5|Briefly described|p244-254, p246 Fig. 3, p245 Fig. 2|||Geological Province: Junee - Narromine Volcanic Belt. Consists of basaltic and andesitic volcanics and volcaniclastic sedimentary rocks intruded by large plutons. See also p244-254.||||||
68843|Narromine Igneous Complex|63286|6|Mentioned|p307, p308 Fig. 9|Late Ordovician|Middle Ordovician|Gological Province: Junee - Narromine Volcanic Belt. Consists of high-K calc-alkaline lavas.||||||07-FEB-11
68843|Narromine Igneous Complex|63292|6|Mentioned|p449|||||||||
68843|Narromine Igneous Complex|63293|5|Briefly described|p467, p468 Fig. 2, p471|Late Ordovician|Early Ordovician|Age: 465Ma (granodiorite from E39). Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
68843|Narromine Igneous Complex|64963|5|Briefly described|p182 Fig. 2, p184|Late Ordovician|Middle Ordovician|Ages: 463-459Ma (U-Pb zircon, Crawford et al 2007c); 449-441Ma (U-Pb zircon, Crawford et al 2007c). ||||||
68843|Narromine Igneous Complex|67106|6|Mentioned|p673, 676, 679, 681|Early Silurian|Early Ordovician|Junee-Narromine Volcanic Belt.|||Copper Hill Suite.|||
68843|Narromine Igneous Complex|67322|5|Briefly described|p21|Hirnantian|Darriwilian|Junee-Narromine Volcanic Belt. The monzonite suite was emplaced between 465-460 Ma and the dacitic-granodiorite suite c.445 Ma (Crawford, Cooke and Fanning, 2007).|465-445 Ma.||||Comprises two petrologically and geochemically distinct suites; the earlier one dominated by monzodiorite with subsidiary monzonite and monzogabbro, and the later characterised by dacitic dykes and a granodiorite stock.|22-FEB-18
68843|Narromine Igneous Complex|67805|6|Mentioned|p73|||||||||
68843|Narromine Igneous Complex|70684|6|Mentioned|p3, p54, p74|Ordovician|Ordovician|Junee-Narromine Volcanic Belt.||||||
68843|Narromine Igneous Complex|72495|5|Briefly described|p217-219, 223, 228, 238, 239|Late Ordovician|Early Ordovician|Coincides with individual highs to the south of the Canonbar Igneous Complex in the Junee-Narromine volcanic belt. Best defined by geophysics with some exploration drillhole data. This body is 40 x 15km^2 and is completely buried beneath Tertiary and Mesozoic sediments.|||||Consists of basaltic and andesitic lavas and volcaniclastic rocks intruded by two sets of intrusives rocks: plutons varying in composition from gabbro to quartz monzodiorite and a younger set of dacitic and granodioritic porphyries|30-MAR-20
68843|Narromine Igneous Complex|73154|5|Briefly described|p75, p84, p92|Llandovery|Middle Ordovician|Inferred emplacement ages of several intrusions cluster around 459 Ma and 463 Ma (Crawford et al., 2007a, 2007b). Pb/U SHRIMP ages of 467+/-5 and 471+/-6 Ma interpreted by Crawford et al., (2007a, 2007b) as inherited zircon cores, may instead represent early to mid Ordovician magmatic episode.|441-445 Ma, 459 Ma and 463 Ma zircon, SIMS U-Pb||Copper Hill suite||Includes granodiorite and dacite.|
68843|Narromine Igneous Complex|73492|6|Mentioned|p691, p693|Ordovician|Ordovician|||||||
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.||||||
24423|Narwonah Rhyolite|22831|6|Mentioned|p 67|||||||||
24423|Narwonah Rhyolite|40365|2|Defined|p328|Early Devonian|Early Devonian|||||||
24423|Narwonah Rhyolite|43441|6|Mentioned|30||Middle Devonian|now included in Dulladerry Rhyolite||||||08-JAN-10
29252|Nash Hill Volcanics|22434|6|Mentioned|12|||Geol province Lachlan Fold Belt||||||
29252|Nash Hill Volcanics|22831|6|Mentioned|p 26|||||||||
29252|Nash Hill Volcanics|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
29252|Nash Hill Volcanics|24417|3|Fully described|p27|Bolindian||Now includes Back Yamma Volcanics and also re-includes Bushmans Volcanics.  Of Northparkes Volcanic Group.||||||
29252|Nash Hill Volcanics|39684|6|Mentioned|Fig.1|||||||||
29252|Nash Hill Volcanics|40891|4|Described|p7|||Modified from Nash Hill Andesite||||||
29252|Nash Hill Volcanics|42489|5|Briefly described|Map legend|Bolindian|Eastonian|||||||
29252|Nash Hill Volcanics|46522|1|Redefined|p30|Late Ordovician||Supersedes Nash Hill Andesite.||||||
29252|Nash Hill Volcanics|46524|5|Briefly described|p103|||See also Appendix 1 P129||||||
29252|Nash Hill Volcanics|46525|6|Mentioned|Fig.1 P143|||||||||
29252|Nash Hill Volcanics|46528|5|Briefly described|Map legend|Ordovician||||||||
29252|Nash Hill Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
29252|Nash Hill Volcanics|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|Of the Northparkes Volcanic Group.||||||13-JUL-04
29252|Nash Hill Volcanics|63278|6|Mentioned|p145 Fig. 1, p151|Silurian|Silurian|||||||07-FEB-11
29252|Nash Hill Volcanics|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
29252|Nash Hill Volcanics|63283|5|Briefly described|p185 Tb. 1, p192-193, p196 Fig. 4, p210|Early Silurian|Early Silurian|Structurally and conformably interfinger with Cotton Formation. Geological Province: Junee-Narromine Volcanic Belt. Unit has a strong and distinctive Th signal on regional radiometrics. See p192-193. Consists of autobrecciated lavas.||||||07-FEB-11
29252|Nash Hill Volcanics|63287|6|Mentioned|p343|Early Silurian|Early Silurian|Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
29252|Nash Hill Volcanics|63288|6|Mentioned|p358, p359, p360, p361|Early Silurian|Early Silurian|Belived to be compositionally similar to the Fifield Complexes.||||||
29252|Nash Hill Volcanics|63289|6|Mentioned|p373 Fig. 7|Silurian|Silurian|||||||07-FEB-11
29252|Nash Hill Volcanics|63290|5|Briefly described|p395, p397 Fig. 3(b)|Llandovery|Llandovery|Of Northparkes Group. Consists volcaniclastic bands with quartz detritus in the bands. Geological Province: Junee - Narromine Volcanic Belt.||||||
29252|Nash Hill Volcanics|63293|6|Mentioned|p467, p468 Fig. 2|Llandovery|Llandovery|Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
29252|Nash Hill Volcanics|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
29252|Nash Hill Volcanics|67107|6|Mentioned|p696, 700|||Peak Hill, c.45km N of Parkes.||||||
29252|Nash Hill Volcanics|70684|6|Mentioned|p3, p54-55, p74-75|Early Silurian|Early Silurian|Probably Llandovery.||||||
29252|Nash Hill Volcanics|71040|6|Mentioned|p17-18|Silurian|Ordovician|Forbes area.||||||
29252|Nash Hill Volcanics|72495|5|Briefly described|p218, 225, 227, p235|Llandovery|Llandovery|Occurs to the east of the Parkes Thrust, within the Parkes township. Age interpreted from geochemical data and the interpreted interfinger relationship with the Cotton Formation.||||Interfingers with the Cotton Formation.||
29252|Nash Hill Volcanics|73154|6|Mentioned|p77|Llandovery|Llandovery|Macquarie Arc, Junee-Narromine Volcanic Belt.|||||Mainly intermediate-mafic lava.|
69899|Nattery Chert Member|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Abercrombie Formation. Varicoloured medium-bedded to laminated chert interbedded with cherty siltstone and mudstone, minor graded and cross-laminated fine-grained quartzose sandstone.||||||11-JUN-08
69899|Nattery Chert Member|67322|5|Briefly described|p14, p17; Fig.5|Middle Ordovician|Middle Ordovician|Defined by Thomas and Pogson, in Thomas et al.(in press). This member correlates with the Numeralla Chert in southern NSW. Age based on conodonts (photographs) identified in thin sections of chert that occur in horizons interbedded with sandstone-dominated units. Occurs in the Goulburn area.||Of the Abercrombie Formation. ||Correlates with the Numeralla Chert.||22-FEB-18
69899|Nattery Chert Member|68466|5|Briefly described|p65-68, 70|Middle Ordovician|Middle Ordovician|Albury-Bega Terrane. Goulburn region. Very similar in age, lithology and outcrop to the Numeralla Chert.||Abercrombie Formation.||Correlated with Mozart Chert and Doongala Chert Member.|Includes cherty siltstone with grazing trail trace fossils.|
69899|Nattery Chert Member|68592|2|Defined|p282-4, p287, p291-3, p295-7, p309-19|Middle Ordovician|Middle Ordovician|See also p116-8, p272, p274-5, p277-8, p286 Fig.59, p1861-2. New name after Nattery Hill. Formerly identified with Numeralla Chert (Murray and Stewart, 2001 and Fergusson and Fanning, 2002). Also called Beacons Hill Chert on the provisional Boorowa and Gunning 1:100 000 geological sheets. Type section described. 10-50m thick. An important regional marker unit. Microfauna, esp. conodonts, detailed.||Unit in Abercrombie Formation.||Equivalent to Numeralla Chert. Locally overlain by Bumballa Formation.|Beds and laminae of honey-coloured, brown to grey chert in intervals up to 13m, separated by mudstone, siltstone and sandstone.|
69899|Nattery Chert Member|69159|5|Briefly described|Map legend|Darriwilian|Darriwilian|||Unit in Abercrombie Formation.|||Varicoloured, medium-bedded to laminated, chert, interbedded with cherty siltstone and mudstone, minor graded and cross-laminated fine-grained quartzose sandstone.|07-SEP-15
69899|Nattery Chert Member|69668|5|Briefly described|p929 Fig.2, p930 Fig.3, p931|Middle Ordovician|Middle Ordovician|Thomas and Pogson (2012). Goulburn-Braidwood area, Albury-Bega terrane. Similar age (late Darriwilian), lithology and outcrop characteristics to Numeralla Chert.||Unit in Abercrombie Formation.||||
69899|Nattery Chert Member|70192|5|Briefly described|Map Legend|Darriwilian|Darriwilian|Includes one unnamed member of grey, laminated to very thinly bedded siltstone and chert mudstone. On Boorowa, Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Abercrombie Formation|Includes one unnamed unit.|Is overlain by Warbisco Shale (of Bendoc Group).|Brown to grey medium bedded to laminated chert, interbedded with cherty siltstone, mudstone and minor graded and cross laminated, fine grained quartzose sandstone.|19-OCT-22
69899|Nattery Chert Member|70540|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Medium bedded to laminated chert, interbedded with cherty siltstone, mudstone and minor graded to cross laminated fine grained quartzose sandstone.|
69899|Nattery Chert Member|70541|4|Described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Honey-coloured, brown to grey, medium bedded to laminated chert, interbedded with cherty siltstone, mudstone and minor graded to cross laminated fine grained quartzose sandstone.|
69899|Nattery Chert Member|70542|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Honey coloured, brown to grey medium bedded to laminated chert, interbedded with cherty siltstone, mudstone and fine to medium grained quartzose sandstone.|
69899|Nattery Chert Member|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Brown to grey medium bedded to laminated chert, interbedded with cherty siltstone, mudstone and minor graded and cross laminated, fine grained quartzose sandstone.|
69899|Nattery Chert Member|70544|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||medium bedded-laminated chert interbedded with cherty siltstone, mudstone and minor graded and cross-laminated fine grained quartzose sandstone.|
69899|Nattery Chert Member|70545|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Medium bedded-laminated chert interbedded with cherty siltstone, mudstone and minor graded and cross-laminated fine grained quartzose sandstone.|
69899|Nattery Chert Member|70661|3|Fully described|p7, p8 fig 2, p16, p17|Middle Ordovician|Middle Ordovician|Name derived from Nattery Hill and Nattery Trigonometrical station, up to-78m thick.Only two lenses outcrop in the Moss Vale map area. Forms low ridges locally, steeply dipping, westerly younging. Sub greenschist to greenschist facies metamorphism.Fossil assemblage discussed in detail.||Abercrombie Formation||Conformably overlies Adaminaby Group, Conformably overlain by Bumballa Formation, equivalent to the Numeralla Chert, Doongala Chert Member, partly equivalent to the Sunlight Creek Formation|Horizons of well bedded chert, mudstone and sandstone intercalated with turbiditic sandstone. Chert rich horizons are 0.8 to 20m thick. Turbidites are similar to those elsewhere in the Adaminaby Group.|
69899|Nattery Chert Member|71069|2|Defined|p21, p22, p40 fig 17, p51, p52|Darriwilian|Darriwilian|Named for the Nattery Hill. Previously referred to as the Numeralla Chert.Contains an unnamed shale, siltstone and cherty mudstone unit.  Contains conodont fossils (Periodon aculeatus and Pygodus serra). Type section is located in a quarry at GR 759260 6135840. Generally 10-50m thick, though it may be up to 70m thick. Generally crops out as rubbly, hackly and blocky exposure or as tabular outcrops in road cuttings and quarries. Lithology discussed in detail. Age derived from conodont fossil assemblage. Fossils include the conodonts Pygodus serra, Periodon aculeatus and Pygodus anserinus, other fossils include radiolarians, sponge spicules, rare brachiopods and bioturbation. Interpreted to have been deposited in a deep marine setting with periodic input for turbidity currents. This member is quarried for road materials in some places.Primary structures/textures, tectonic structure, metamorphism and geophysical characteristics discussed. Equivalent to the Numeralla Chert and the Doongala Chert Member. May be equivalent in part to the Sunlight Creek Formation. See also  p53 fig 19, p55 fig 20, p58-62, p66 fig 21, p68-70, p73 fig 26, p76 fig 27, p78, p79, p81, p84.||Abercrombie Formation||Conformably overlies the Mummel Chert Member. Conformably overlain by the Bumballa Formation or the Warbisco Shale. Overlain by the Bendoc Group or the upper Abercrombie Formation.|Grey, brown and khaki chert beds that thicken up section and are interbedded with quartzose sandstone, siltstone, shale and cherty mudstone.|
69899|Nattery Chert Member|71303|5|Briefly described|map legend|Sandbian|Darriwilian|||Of Adaminaby Group.|||Well bedded dark grey chert, mudstone and sandstone, intercalated with turbiditic horizons of similar lithology to the surrounding Adaminaby Group.|
69899|Nattery Chert Member|71656|6|Mentioned|p12 Fig.2, p14|Gisbornian|Darriwilian|Now includes rocks formerly regarded as Sunlight Creek Formation. Age from conodonts. Also includes radiolaria, sponge spicules, brachiopods.||Near top of Abercrombie Formation, Adaminaby Group||May be overlain by Warbisco Shale, Bumballa Formation in places.|Fossiliferous chert.|
69899|Nattery Chert Member|71691|5|Briefly described|Map legend.|Ordovician|Ordovician|||Abercrombie Formation.|||Varicoloured, medium-bedded to laminated chert interbedded with cherty siltstone and mudstone: minor graded and cross-laminated fine-grained quartzose sandstone; grey to cream quartz sandstone to quartzite with lesser siltstone to mudstone.|
69899|Nattery Chert Member|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|||Abercrombie Formation.|||Varicoloured, medium-bedded to laminated chert; interbedded with cherty siltstone and mudstone, minor graded and cross-laminated fine-grained quartzose sandstone.|
69899|Nattery Chert Member|71700|4|Described|vi, p7-p9, p39-p40, p43, p46, p55-p56|Gisbornian|Darriwilian|Albury-Bega Terrane. A type section is defined in Thomas and Pogson (2012). Appears as the Nattery Chert on p7. Typically around 80m thick in the Braidwood 1:100k sheet area. See also CD.||Abercrombie Formation||Conformably overlain by the Warbisco Shale. Conformably overlies the Peach Tree Chert Member. Equivalent to the Numeralla Chert and Doongala Chert.||
69899|Nattery Chert Member|73140|5|Briefly described|p495 Fig.1, Fig.3|Darriwilian|Darriwilian|Age based on conodonts.||Abercrombie Formation||Underlies Bumballa Formation, Warbisco Shale||
30034|Nea Subgroup|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Black Jack Group. Includes the Trinkey and Wallala Formations. Geological Province: Gunnedah Basin.||||||
30034|Nea Subgroup|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Black Jack Group. Encompasses newly defined Trinkey and Wallala Formations. Age Upper Stage 5 to Upper Stage 5c. Formal definition published in an article released immediately prior, however a summary of new nomenclature is provided in Appendix 1.||||||13-NOV-13
30034|Nea Subgroup|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Black Jack Group. Underlies: Digby Formation.  Overlies: Brothers Subgroup.||||||05-JUL-04
30034|Nea Subgroup|68003|5|Briefly described|p38 Fig.3-j, p41, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Formed by southward-prograding major fluvio-deltaic systems.||Unit in Black Jack Group.|Includes Wallala and Trinkey Formations.|Overlies Coogal Subgroup. Is overlain by Digby Formation.||
30034|Nea Subgroup|68004|5|Briefly described|p23 Table 1. |||Gunnedah Basin. Largely equivalent to the Wollombi and Newcastle Coal Measures and the Wallerawang Subgroup, Sydney Basin.||Upper unit in Black Jack Group.|Includes Wallala and Trinkey Formations.|Overlies Coogal Subgroup. Is overlain by Digby Formation.||
30034|Nea Subgroup|70791|5|Briefly described|p277|Lopingian|Lopingian|Gunnedah Basin.||Black Jack Group.|Wallala, Trinkey Formations.|||
28856|Neath Sandstone|22601|6|Mentioned|410|Permian|Permian|Parent Greta Coal Measures. Geol province Sydney Basin||||||
28856|Neath Sandstone|22610|5|Briefly described|p 123|||Maximum thickness 18m||||||
28856|Neath Sandstone|22969|4|Described|Fig 4.1a||Early Permian|||||||
28856|Neath Sandstone|23540|5|Briefly described|p 419|||Of the Greta Coal Measures.||||||20-FEB-07
28856|Neath Sandstone|33867|6|Mentioned|p5|||||||||
28856|Neath Sandstone|34015|4|Described|p325|||Permian||||||
28856|Neath Sandstone|37086|6|Mentioned|p185|||||||||
28856|Neath Sandstone|45090|5|Briefly described|p151|||||||||
28856|Neath Sandstone|60297|5|Briefly described|p176|Permian|Permian|Base of Greta Coal Measures.||||||
28856|Neath Sandstone|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
28856|Neath Sandstone|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Lochinvar area.||Unit in Greta Coal Measures.||||
79789|Nebine Metamorphics|71251|4|Described|p2-3, p8-9, p11, p13, p20, p24, p48|||Thomson Orogen. Multiply-deformed metasedimentary rocks (greenschist) forming an extensive, geophysically-bland basement to the Eromanga Basin. Core and thin-section photographs. Has an elevated and highly variable natural gamma signal. HyLogger data.|~520 Ma (Kositcin et al., 2015).|||Is overlain by Cadna-owie Formation.|Green quartz-muscovite-biotite-chlorite schist (topmost 35m strongly weathered). Quartz commonly forms irregular milky segregations up to 5cm in diameter, often with some albite. Grain size variation in psammitic layers with larger grains is ~1mm.|
79789|Nebine Metamorphics|71864|6|Mentioned|p3-p4|||||||||
79789|Nebine Metamorphics|71965|4|Described|p896,899,903-904,906-908,910-913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Occurs adjacent Werewilka Formation. Generally low and featureless in magnetic response with some broad magnetic striping. Age constraints: 520+\-10 Ma (MDA); 435+\-3 Ma (Minimum DA, overlying sediments). Possible "on-strike" stratigraphic equivalent to Werewilka Formation, separated by the Caiwarro Fault Zone.|520+\-10 Ma (MDA)|||Correlable with Warratta Group, Tongo Formation, Twin Tanks Metamorphics, Thomson beds, Werewilka Formation.|Biotite-muscovite phyllite and garnet-plagioclase-muscovite-biotite-quartz schist, laminated quartz-mica schist, locally up to amphibolite facies.|29-OCT-19
79789|Nebine Metamorphics|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Thomson Orogen. Intersected in GSQ Mitchell 1 drillhole, samples analysed yielded a maximum depositional age of c. 520 Ma|<520 Ma|||||
79789|Nebine Metamorphics|72522|4|Described|p1-2, p33, p41-48|Cambrian|Cambrian|Very similar lithology to the Glenroy Formation except slightly higher metamorphic grade and multiple deformation fabrics exist in this unit. Dated sample is lower metamorphic grade than Nebine Metamorphics further north and may represent a younger unit. Nebine Metamorphics also identified in AOP Alba 1, GSQ Mitchell (MDA ~520 Ma), along the Nebine Ridge. Date ref. Kositcin et al., 2015; Purdy et al., 2016.|435+/-4 Ma U-Pb SHRIMP max.dep.||||Includes siltstone sampled for dating; quartz-muscovite-biotite-chlorite schist in GSQ Eulo 1.|
79789|Nebine Metamorphics|73600|6|Mentioned|p202, p204|||||||||
82619|Neds Beach Formation|73136|4|Described|p192-193, p195, p198|Pleistocene|Pleistocene|Lord Howe Island. Beach and shallow marine beds. Covers much of the northern part of the island and extends below sea level. Maximum thickness: 40 m. Includes thick dune units with a maximum height of 40 m above sea level. Preliminarily thought to be of last glacial age but more recently approximated as being deposited in the Last Interglacial around 125,000 years ago. The thick dune units and basal beach unit comprise the lower of two alloformations, called N1, which is assigned to marine oxygen isotope stage 5e. These dune units are separated by protosols. Above this, the N2 alloformation is composed of the Middle Beach Member and Cobbys Corner Member, which are assigned to marine oxygen isotope stage 5a. Found in the lagoon below Holocene sediments and above basalt and is less diagenetically altered than the underlying Searles Point Formation. Much of the eolianite preserves its original depositional form and the orientation of exposed foreset beds indicate that deposition occurred under variable onshore winds, similar to the modern setting. A small outcrop of calcarenite that appears to correspond to this unit is found within a talus slope (Big Slope) indicating the talus has persisted for at least 120,000 years.|[ca.] 0.125 Ma||Middle Beach Member, Cobbys Corner Member|Underlain by the Searles Point Formation.|Calcarenites of skeletal carbonate grainstones comprising grains of coralline algae, molluscs, foraminifera, bryozoans, and some volcanic grains with only rare coral. Predominately deposited as eolianite that comprise cross-bedded units 3-25 m thick.|22-NOV-22
82619|Neds Beach Formation|73554|4|Described|Map legend, back of map|Quaternary|Quaternary|Lord Howe Island. Composes most of the flat-lying areas of the island. Very well exposed from Neds Beach to Brodies Point. Deposited approximately 10,000 to 30,000 years ago as dunes around existing hills.|ca 0.03 - 0.01 Ma||Cobbys Corner Member, Middle Beach Member|Underlain by Searles Point Formation.|Brown to yellow calcarenite with cross-bedding. Consists of coralline algae fragments, coral, foraminifera and molluscs. Common clay-rich palaeosols may contain bird bones, land snail shells, rhizoliths and solution pipes.|
35162|Neegulbah Bed|23055|6|Mentioned|Fig13p25|||||||||
31615|Nelligen Suite|42726|5|Briefly described|map legend||Silurian|||||||
27679|Nelungaloo Volcanics|13139|5|Briefly described|p10|Lancefieldian|Lancefieldian|||||||
27679|Nelungaloo Volcanics|22519|5|Briefly described|p6|||||||||
27679|Nelungaloo Volcanics|22831|4|Described|p 11||Early Ordovician|||||||
27679|Nelungaloo Volcanics|22857|5|Briefly described|p416 App. 1 Tb. A1.5|||Aphanitic and porphyritic basaltic lavas.||||||
27679|Nelungaloo Volcanics|23213|6|Mentioned|p23, Fig.10|Bendigonian|Lancefieldian|Age: early Middle Lancefieldian to Early Bendigonian. of Junee-Narromine Volcanic Belt.||||||
27679|Nelungaloo Volcanics|23538|4|Described|p 457-458|||Also see p461 and Fig 1 p458.||||||
27679|Nelungaloo Volcanics|23736|6|Mentioned|p11|Lancefieldian|Lancefieldian|||||||
27679|Nelungaloo Volcanics|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
27679|Nelungaloo Volcanics|24267|4|Described|p1506|Late Ordovician|Early Ordovician|Age: 438.5 +/- 3.6Ma (U/Pb) and Early Ordovician (Graptolites). Overlying Unit: Goonumbla Volcanics. Geological Province: Parkes-Narromine Belt||||||
27679|Nelungaloo Volcanics|24417|3|Fully described|p29|Early Ordovician|Late Cambrian|Previously included the "Yarrimbah Chert Member", now the Yarrimbah Formation.  Overlain by Yarrimbah Formation.||||||
27679|Nelungaloo Volcanics|24518|5|Briefly described|p66|Early Ordovician|Early Ordovician|Intruded by the porphyritic rocks of the Condobolin Road Intrusive Complex.||||||
27679|Nelungaloo Volcanics|29907|6|Mentioned|p6|||||||||
27679|Nelungaloo Volcanics|29910|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
27679|Nelungaloo Volcanics|32591|6|Mentioned|Fig.2|||||||||
27679|Nelungaloo Volcanics|33121|3|Fully described|p55|||Early Ord. Andesites||||||
27679|Nelungaloo Volcanics|33125|6|Mentioned|p15|||Correlation chart||||||
27679|Nelungaloo Volcanics|35118|6|Mentioned|Fig.5|||||||||
27679|Nelungaloo Volcanics|35415|5|Briefly described|p15|||Age discussed on graptolite find. Late Cambrian-Early Ordovician.||||||
27679|Nelungaloo Volcanics|39214|5|Briefly described|p17|||||||||
27679|Nelungaloo Volcanics|40136|5|Briefly described|p33|||||||||
27679|Nelungaloo Volcanics|40746|5|Briefly described|p359|||||||||
27679|Nelungaloo Volcanics|40891|3|Fully described|p2|||Mention Fig.3||||||
27679|Nelungaloo Volcanics|42262|5|Briefly described|p1817|||See also Fig.2 P1810.||||||
27679|Nelungaloo Volcanics|42479|6|Mentioned|Fig. 2 P110|||||||||
27679|Nelungaloo Volcanics|42489|5|Briefly described|Map legend|Chewtonian|Lancefieldian|||||||
27679|Nelungaloo Volcanics|42718|6|Mentioned|p1|||||||||
27679|Nelungaloo Volcanics|43263|6|Mentioned|Map Legend||Ordovician|||||||
27679|Nelungaloo Volcanics|43441|5|Briefly described|11, 21||Early Ordovician|||||||08-JAN-10
27679|Nelungaloo Volcanics|44093|5|Briefly described|p178 App. 1|Ordovician|Ordovician|Of the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
27679|Nelungaloo Volcanics|44160|5|Briefly described|Map Legend|Chewtonian|Lancefieldian|||||||
27679|Nelungaloo Volcanics|46522|1|Redefined|p7|Early Ordovician||||||||
27679|Nelungaloo Volcanics|46523|6|Mentioned|p88|||||||||
27679|Nelungaloo Volcanics|46524|4|Described|p99|||||||||
27679|Nelungaloo Volcanics|46525|6|Mentioned|Fig.1 P143|||||||||
27679|Nelungaloo Volcanics|46528|5|Briefly described|Map legend|Ordovician||||||||
27679|Nelungaloo Volcanics|50299|5|Briefly described|Map Legend|Ordovician|Ordovician|Aphanitic and porphyritic basaltic lavas||||||09-JUN-04
27679|Nelungaloo Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
27679|Nelungaloo Volcanics|60009|5|Briefly described|Map Legend|Lancefieldian|Lancefieldian|||||||13-JUL-04
27679|Nelungaloo Volcanics|61724|3|Fully described|p864 Fig.1, p866|Early Ordovician|Early Ordovician|Consists of coherent andesite and associated volcaniclastic rocks; presence of graptolites indicates a deep marine origin. Overlain by Yarrimbah Formation. Min. age: 481+/-4 Ma. Max. thickness: 1.5 km (est.). See also p868-869.||||||03-SEP-18
27679|Nelungaloo Volcanics|63121|5|Briefly described|p225 Fig. 2|Early Ordovician|Late Cambrian|Max. age is Lancefieldian. In the "Yarrimbah" area NW of Parkes, NSW.||||||13-MAR-07
27679|Nelungaloo Volcanics|63278|4|Described|p149, p145 Fig. 1, p146 Fig. 2a|Early Ordovician|Early Ordovician|Overlain by Yarrimbah Fm. Age: 481+/-4Ma. (Simpson et al. 2005). Geol Prov: Junee-Narromine Volcanic Belt, LFB. Oldest Ordovician rocks in the Junee-Narromine Volcanic Belt. Consists of andesitic lavas and volcaniclastic sediments.||||||07-FEB-11
27679|Nelungaloo Volcanics|63279|5|Briefly described|p168-172, p169 Fig. 2, p171 Fig. 4|Lancefieldian|Lancefieldian|Overlain by Yarrimbah Formation. Geological Province: Junee-Narromine Volcanic Belt. Oldest rocks in province, and consists of volcanic and volcaniclastic rocks. Intrusive monzonites give age of 484.3+/-3.6Ma. See also p168-172.||||||
27679|Nelungaloo Volcanics|63283|5|Briefly described|p185, p191 Tb. 2, p194 Fig. 2|Early Ordovician|Early Ordovician|Overlain by Yarrimbah Formation. Age: 480Ma (basalt and andesite). Geological Province: Junee-Narromine Volcanic Belt. Small monzodiorite intrusions, age is post 445ma magmatisim.||||||07-FEB-11
27679|Nelungaloo Volcanics|63284|6|Mentioned|p247, 257, p258|Early Ordovician|Early Ordovician|In the Narromine Igneous Complex.||||||
27679|Nelungaloo Volcanics|63286|6|Mentioned|p308 Fig. 9|Early Odrovician|Early Ordovician|Geological Province: Junee - Narromine Volcanic Belt. Consists of high-K calc-alkaline lavas.||||||07-FEB-11
27679|Nelungaloo Volcanics|63290|6|Mentioned|p397 Fig. 3(b)|Early Ordovician|Early Ordovician|Geological Province: Junee - Narromine Volcanic Belt.||||||
27679|Nelungaloo Volcanics|63291|4|Described|p421, p423, p425 Fig.5|Early Ordovician|Early Ordovician|Overlain by Yarrimbah Fm. Age: ~496-480Ma (see fig 5). Geol Prov: Junee - Narromine Vol Belt. Comprising mainly plag+clinopyx+olivine+Fe+Ti oxide-phyric, high-K calc-alkaline to shoshonitic andesites and volcaniclastic sedementary rocks. Min thickness of 650m.||||||03-SEP-18
27679|Nelungaloo Volcanics|63293|5|Briefly described|p467, p468 Fig. 2|Early Ordovician|Early Ordovician|Overlain by Yarrimbah Formation. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
27679|Nelungaloo Volcanics|64015|5|Briefly described|p58 Fig. 1, p59|||||||||
27679|Nelungaloo Volcanics|65756|5|Briefly described|p27|Early Ordovician|Early Ordovician|Macquarie Arc, Lachlan orogen||||||
27679|Nelungaloo Volcanics|67106|6|Mentioned|p673, 675, 681-682|||Junee-Narromine Volcanic Belt.||||Is overlain unconformably by Yarrimbah Formation.||
27679|Nelungaloo Volcanics|67107|5|Briefly described|p687-688, 693, 696, 701-702|Early Ordovician|Early Ordovician|The oldest recognized unit in the Molong Volcanic Arc. May be analogous to Mount Read Volcanics in TAS.|484.3 +/- 2.9 Ma (SHRIMP: Butera et al., 2001).|||Faulted against Wombin and Goonumbla Volcanics.||
27679|Nelungaloo Volcanics|67322|5|Briefly described|Fig.5; p22|Early Ordovician|Early Ordovician|Macquarie Arc. (Sherwin 1973; Sherwin, in Lyons et al. 2000). Age is determined from p20 Fig.5 (Strat. column). Occurs in the Junee-Narromine region.  ||||Overlain ?disconformably by the Yarrimbah Formation.||22-FEB-18
27679|Nelungaloo Volcanics|67821|5|Briefly described|p150|Ordovician|Ordovician|||Goonumbla Volcanic Complex.|||Volcanics and volcaniclastics.|
27679|Nelungaloo Volcanics|67847|5|Briefly described|p56|Early Ordovician|Early Ordovician|Geochemically similar to the Cowal Igneous Complex.||||||
27679|Nelungaloo Volcanics|70278|5|Briefly described|p1609, 1611-1612, 1627|Early Ordovician|Early Ordovician|Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW. Over 650m thick.||Goonumbla Volcanic Complex.||Is overlain unconformably by Goonumbla Volcanics. Is overlain by Yarrimbah Formation.|Includes andesitic lavas overlain by volcanic conglomerate, volcanic sandstone, and the clastic sedimentary rocks of the Yarrimbah Formation.|
27679|Nelungaloo Volcanics|70684|5|Briefly described|p3, p12, p54-60, p74-74|Early Ordovician|Early Ordovician|Originally recognised by Sherwin (1979). W of Parkes, Junee-Narromine Volcanic Belt. Subaqueous debris-flow / turbidite deposits. Is intruded by a 481 +/- 4 Ma monzonite (age corrected by Williams in Simpson et al., 2005: previously 484.3 +/- 2.9 Ma: U-Pb SHRIMP zircon; Butera et al., 2001).||||Is overlain unconformably by Yarrimbah Formation.|Mainly andesitic and basaltic andesitic lavas and intercalated volcaniclastic sediments: volcanic breccia, pebbly sandstone, planar laminated siltstone.|
27679|Nelungaloo Volcanics|72495|5|Briefly described|p218-219, p222, p225, 227, p231-232|Early Ordovician|Early Ordovician|Outcrops in the core of the Forbes Anticline, which is probably faulted. Most recently described by Simpson et al, 2005 and were further described by Glen et al (2007) and Percival and Glen (2007).||||Overlain by the Yarrimbah Formation.||26-MAR-20
27679|Nelungaloo Volcanics|73154|6|Mentioned|p74, p77 Fig.3, p78|Early Ordovician|Early Ordovician|Macquarie Arc, Phase 1. Junee-Narromine Volcanic Belt. Dominantly high-K calc-alkaline volcanics. Intruded by monzodiorite and monzonite intrusions informally termed as Nettlebecks Lane monzodiorite with zircon U-Pb ages of 477.4+/-1.5 Ma and 477.2+/-4.2 Ma.||||Intruded by Nettlebecks Lane Monzodiorite.||
27679|Nelungaloo Volcanics|73287|4|Described|p661-662, p665 Fig.2|Early Ordovician|Early Ordovician|Macquarie Arc. Basal unit of the Goonumbla Volcanic Complex. Estimated to be 600-650m thick. Intruded by minor, unmineralised monzodiorite porphyries at 481 +/- 4 Ma. Low-angle unconformity with the overlying Goonumbla Volcanics.|482-471 Ma|Goonumbla Volcanic complex||Unconformably underlies the Goonumbla Volcanics|Coherent andesite overlain by conglomerates, sandstones. 600-650m thick.|
69633|Neriga Province Volcanics|61155|5|Briefly described|p19|Early Oligocene|Middle Eocene|Overlain by Airly Province Volcanics.  In the Bathurst-Goulburn region. ||||||
83270|Nettlebecks Lane Monzodiorite|73154|4|Described|p74-76, p78, p80, p84, p89 Fig.6, p90-91|Early Ordovician|Early Ordovician|Macquarie Arc, Phase 1. Informally termed here as Nettlebecks Lane Monzodiorite. Emplacement age interpreted to be around 477 Ma. Described with zircon U-Pb SHRIMP igneous crystallisation age 484+/-3 Ma by Butera et al., (2001), high-K, calc-alkaline affinity. Constrains timing of Phase 1 magmatism of the Macquarie Arc. Intrudes Nelungaloo Volcanics in the core of the Forbes anticline. Very high U content of zircons limits confidence in crystallisation age, revised age of ~477 Ma. Zircon inheritance claimed to be recognised by Glen et al. (2011) based on a 534 Ma zircon. Nettlebecks Lane monzodiorite pluton on p78.|484+/-3 Ma, 477+/-2 Ma, 477+/-4 Ma zircon U-Pb|||Intrudes Nelungaloo Volcanics.|Zoned monzodiorite stock.|
22526|Nevann Siltstone|22736|2|Defined|p619,29|Visean|Tournaisian|southern Hastings Block unit||||||
22526|Nevann Siltstone|22857|4|Described|p500 App.1 Tb.A1.7|Tournaisian|Tournaisian|Laminated siltstone, minor lithic sandstone. Max. thickness: 550m.||||||
22526|Nevann Siltstone|44093|5|Briefly described|p67 Fig 6.6|Carboniferous|Carboniferous|Of the Southern Hastings Block. Geological Province: New England Fold Belt.||||||
22526|Nevann Siltstone|69323|5|Briefly described|p2,55|Carboniferous|Carboniferous|Geological province: New England Orogen.||||Intruded by 'Kindee Creek tonalite'.||
22526|Nevann Siltstone|70939|6|Mentioned|p826, p828|Carboniferous|Carboniferous|Southern Hastings Block.||||||
22526|Nevann Siltstone|71628|5|Briefly described|p17:30|||Hastings Block.||Quintoc Group.||Is intruded by Kindee Creek Tonalite.|Agglomerate-tuff, coarse tuffaceous silts, ultrafine silts, and banded mudstone.|
31618|Neville Suite|42726|5|Briefly described|map legend||Silurian|||||||
31618|Neville Suite|44093|5|Briefly described|p201 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
22530|New Building Granodiorite|22815|5|Briefly described|p74|||||||||
22530|New Building Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of New Building Suite.||||||
31463|New Building Suite|22815|6|Mentioned|p74|||||||||
31463|New Building Suite|42726|5|Briefly described|map legend||Early Devonian|of the Bemboka Supersuite.  Contains New Building granite.||||||08-FEB-05
31463|New Building Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
40237|New England Suite|38822|6|Mentioned|p193|||Superseded by the New England Supersuite. Geological Province: New England Fold Belt||||||
40237|New England Suite|71628|6|Mentioned|p3: 40, 49, 77-78; p8: 1, 9, 51, 62, 67|||See also p8: 93, 104; p19: 13, 44, 55, 154. Hensel et al. (1982). They also called it the New England Super-suite.||||||
29686|New England Supersuite|43017|5|Briefly described|Fig.2,p374|||||||||
29686|New England Supersuite|71628|5|Briefly described|p8: 74|||"Puzzingly mentioned as ""Uralla and Moonbi Supersuites combined""."|||||Granites.|
70132|New Tank Formation|66623|2|Defined|pp192-193, pp197-199. |Early Devonian|Early Devonian|Defined in this study. Partly synonymous with lower Snake Cave Sandstone (Carroll 1982). Mutawintji National Park. Correlated with lower Muckabunnya Formation. Outcrops boldly, forming strike ridges. Thickness varies widely up to c.400 m. Shows variety of cross-bedding; rare bioturbation.||Basal unit in Wana Karnu Group.||Unconformably overlies Rowena Formation. Is overlain by Homestead Gorge Formation.|White to buff pebbly sandstone, thick to very thick beds; sandstone and conglomerate; fining upwards; basal conglomerate with grey quartzite pebbles and cobbles; conglomerates contain quartzite and vein quartz clasts.|
70132|New Tank Formation|66918|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Wana Karnu Group.||Is overlain by Homestead Gorge Formation.|Thick to very thick beds of white to buff pebbly sandstone, sandstone and conglomerate.|
70132|New Tank Formation|70650|5|Briefly described|Map Legend|Devonian|Devonian|||Wana Karnu Group|||Thick to very thick beds of white to buff pebbly sandstone, sandstone and conglomerate.|
70029|Newacres Ignimbrite Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Quialigo Volcanics (Bindook Group). Cream to grey quartz-feldspar phyric sryctal-rich welded rhyolitic ignimbrite.||||||18-JUN-08
70029|Newacres Ignimbrite Member|66300|5|Briefly described|p76, 85.|||Age indistinguishable from Marulan Granite (416.7 +/- 3.1Ma) and from Kerillon Tuff (412.7 +/- 2.2 Ma).|414.4 +/- 2.9 Ma to 409 +/- 4 Ma.|Unit in Quialigo Volcanics.||||29-OCT-13
70029|Newacres Ignimbrite Member|68592|2|Defined|p882-3, p1061, p1162-4, p1174-81, p1657|Pragian|Lochkovian|See also p742, p862. New name, after Newacres property, for rhyolitic to dacitic ignimbrites which were included in the Gundary Formation by Jones et al. (1995). Previously included in Gundary Beds or Towrang Beds. Type locality described. Estimated at 600m thick. Geochemistry described; geophysical properties briefly described. Other SHRIMP zircon U-Pb age determinations are 411 +/- 3 Ma (Wilde, 2002) and 414.4 +/- 2.9 Ma (Black, 2006), which may both includes inherited zircons.|409 +/- 4 Ma SHRIMP zircon U-Pb (Wilde, 2002).|Unit in Quialigo Volcanics.||Overlies Bullamalita Conglomerate locally. Is overlain by Saltpetre Andesite, or Four Winds Ignimbrite, Members. May correlate with Kerillon Tuff Member (Tangerang Formation).|Poorly stratified, densely welded rhyolitic ignimbrites: a crystal-rich group and a less crystal-rich group.|
70029|Newacres Ignimbrite Member|70192|5|Briefly described|Map Legend|Pragian|Lochkovian|Dkqn. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Quialigo Volcanics||Is overlain by Four Winds Ignimbrite Member and Saltpetre Andesite Member.|Cream to grey quartz-feldspar phyric crystal-rich welded rhyolitic ignimbrite.|
70029|Newacres Ignimbrite Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Quialigo Volcanics|||Cream to grey quartz-feldspar phyric crystal-rich welded rhyolitic ignimbrite.|
70029|Newacres Ignimbrite Member|71069|6|Mentioned|p143|Lochkovian|Lochkovian||414 +/- 2.9 Ma (SHRIMP U-Pb)|Quialigo Volcanics||||
70029|Newacres Ignimbrite Member|71700|5|Briefly described|p24-p26, CD|Pragian|Lochkovian|Occurs in the Goulburn250 sheet area. An additional SHRIMP U-Pb age of 414.4 +/- 2.9 Ma is derived from Black (2006).|411 +/- 3 Ma and 409 +/- 4 Ma (Wilde, 2002)|Quialigo Volcanics||Equivalent to the Croppies Gunyah Ignimbrite Member and the Manar Ignimbrite Member.||
27861|Newcastle Coal Measures|22516|5|Briefly described|p17||Late Permian|||||||
27861|Newcastle Coal Measures|22578|5|Briefly described|p391, Fig.5 p395||Late Permian|||||||
27861|Newcastle Coal Measures|22601|6|Mentioned|417|Permian|Permian|Geol province Sydney Basin||||||
27861|Newcastle Coal Measures|22745|6|Mentioned|Fig3,p128||Permian|Sydney Basin.||||||
27861|Newcastle Coal Measures|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Includes Moon Island Beach Formation, Awaba Tuff, Boolaroo Formation, Warners Bay Tuff, Adamstown Formation, Nobbys Tuff and Lambton Formation. Geological Province: Sydney Basin. See also p264 (photo 1).||||||
27861|Newcastle Coal Measures|22864|6|Mentioned|p264|||||||||
27861|Newcastle Coal Measures|22969|4|Described|p4, 24|||Max. thickness: 1200 m.||||||
27861|Newcastle Coal Measures|22970|5|Briefly described|Plate 6||Permian|||||||
27861|Newcastle Coal Measures|23055|4|Described|p1,21-3,Fig11p23,43||Late Permian|||||||
27861|Newcastle Coal Measures|23214|6|Mentioned|p267|||||||||
27861|Newcastle Coal Measures|23350|5|Briefly described|259|||||||||
27861|Newcastle Coal Measures|23438|4|Described|p25|||||||||
27861|Newcastle Coal Measures|23450|6|Mentioned|p527 Fig.1|||||||||
27861|Newcastle Coal Measures|23540|5|Briefly described|p 417|||||||||
27861|Newcastle Coal Measures|23544|5|Briefly described|p372|||In the Sydney Basin||||||
27861|Newcastle Coal Measures|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Geological Province: Sydney Basin||||||
27861|Newcastle Coal Measures|24040|5|Briefly described|p470 Fig.2, p484|Late Permian|Late Permian|Geological Province: Lachlan Fold Belt||||||21-AUG-08
27861|Newcastle Coal Measures|24079|5|Briefly described|p432|Permian|Permian|Geological Province: Sydney Basin.||||||
27861|Newcastle Coal Measures|24121|5|Briefly described|p4, p61, p73, 99, 115, 132, 227|||||||||25-AUG-22
27861|Newcastle Coal Measures|24157|3|Fully described|p188 Tb.1|Permian|Permian|Underlain by Waratah Sandstone. Recognised as equivalent of the Wollombi Coal Measures. Geological Province: Sydney Basin||||||14-MAR-07
27861|Newcastle Coal Measures|24158|4|Described|p170|Late Permian|Late Permian|Geological Province: Sydney Basin. Max Thickness: 8m||||||
27861|Newcastle Coal Measures|24423|5|Briefly described|p230 Fig.3|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||
27861|Newcastle Coal Measures|24424|6|Mentioned|p538|Late Permian|Late Permian|||||||
27861|Newcastle Coal Measures|24471|4|Described|p27|Late Permian|Late Permian|Geological Province: Sydney Basin. Overlain by Narrabeen Group.  Stratigraphically equivalent to Illawarra Coal Measures.||||||07-FEB-11
27861|Newcastle Coal Measures|24479|5|Briefly described|p41|||Parts equivalent to the Wollombi Coal Measures.||||||
27861|Newcastle Coal Measures|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
27861|Newcastle Coal Measures|29748|6|Mentioned|Fig.3|||||||||
27861|Newcastle Coal Measures|29752|6|Mentioned|p36|||||||||
27861|Newcastle Coal Measures|29827|6|Mentioned|p20|||||||||
27861|Newcastle Coal Measures|29918|6|Mentioned|p17|||||||||
27861|Newcastle Coal Measures|29922|6|Mentioned|Appendix 3|||||||||
27861|Newcastle Coal Measures|29926|6|Mentioned|Fig.3|||||||||
27861|Newcastle Coal Measures|29941|6|Mentioned|p13|||||||||
27861|Newcastle Coal Measures|29942|4|Described|Fig.2|||||||||
27861|Newcastle Coal Measures|30340|6|Mentioned|Table 3|||Tatarian age||||||
27861|Newcastle Coal Measures|30341|6|Mentioned|p136|||Upper Permian age||||||
27861|Newcastle Coal Measures|30545|6|Mentioned|Fig.2|||Tatarian||||||
27861|Newcastle Coal Measures|30547|6|Mentioned|p426|||Correlation||||||
27861|Newcastle Coal Measures|30555|6|Mentioned|Fig.21.5|||||||||
27861|Newcastle Coal Measures|30743|6|Mentioned|p32|||Upper Permian age. Correlation||||||
27861|Newcastle Coal Measures|31124|6|Mentioned|p17|||Equivalent in age to Singleton C.M.||||||
27861|Newcastle Coal Measures|31125|6|Mentioned|p16|||Geology||||||
27861|Newcastle Coal Measures|31129|5|Briefly described|p125|||See also P128-133.||||||
27861|Newcastle Coal Measures|31297|6|Mentioned|Fig. 2|||||||||
27861|Newcastle Coal Measures|31380|6|Mentioned|p131|||||||||
27861|Newcastle Coal Measures|31381|6|Mentioned|p53|||||||||
27861|Newcastle Coal Measures|31549|6|Mentioned|p158|||Refers McKenzie (1962) & Diessel (1968)||||||
27861|Newcastle Coal Measures|31551|6|Mentioned|Table 1|||Refers Rattigan (1966) & Duff (1967)||||||
27861|Newcastle Coal Measures|31559|6|Mentioned|p158|||||||||
27861|Newcastle Coal Measures|31563|6|Mentioned|p143|||||||||
27861|Newcastle Coal Measures|31649|6|Mentioned|p59|||||||||
27861|Newcastle Coal Measures|31706|6|Mentioned|p657|||Permian correlation chart||||||
27861|Newcastle Coal Measures|31855|6|Mentioned|p14|||Stratigraphic table||||||
27861|Newcastle Coal Measures|31883|6|Mentioned|Table 1|||||||||
27861|Newcastle Coal Measures|31884|6|Mentioned|Table 1|||Permian||||||
27861|Newcastle Coal Measures|31885|6|Mentioned|p1439|||Table 1. Refers Robinson (1969)||||||
27861|Newcastle Coal Measures|31887|6|Mentioned|p3|||||||||
27861|Newcastle Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
27861|Newcastle Coal Measures|32672|6|Mentioned|p675|||||||||
27861|Newcastle Coal Measures|32833|6|Mentioned|p108|||||||||
27861|Newcastle Coal Measures|32834|6|Mentioned|Table 3|||||||||
27861|Newcastle Coal Measures|32835|6|Mentioned|p4|||Flora||||||
27861|Newcastle Coal Measures|32840|6|Mentioned|Table 1|||||||||
27861|Newcastle Coal Measures|32920|6|Mentioned|p93|||||||||
27861|Newcastle Coal Measures|32937|6|Mentioned|p54|||Geology||||||
27861|Newcastle Coal Measures|32945|6|Mentioned|p83|||See also P85. Permian||||||
27861|Newcastle Coal Measures|33128|5|Briefly described|p51|||Permian||||||
27861|Newcastle Coal Measures|33129|6|Mentioned|Table 1|||Adapted from Packham (1969)||||||
27861|Newcastle Coal Measures|33131|6|Mentioned|p77|||Mention Fig. 9||||||
27861|Newcastle Coal Measures|33132|6|Mentioned|p1465|||||||||
27861|Newcastle Coal Measures|33334|6|Mentioned|p6|||See also P7. Perm.||||||
27861|Newcastle Coal Measures|33683|6|Mentioned|Table 1|||Narrabeen Gp.||||||
27861|Newcastle Coal Measures|33685|6|Mentioned|p6|||Permian. See also P7.||||||
27861|Newcastle Coal Measures|33686|6|Mentioned|p15|||||||||
27861|Newcastle Coal Measures|33701|6|Mentioned|Fig.1|||Tatarian||||||
27861|Newcastle Coal Measures|33711|6|Mentioned|Table 2|||||||||
27861|Newcastle Coal Measures|33867|4|Described|p7|||||||||
27861|Newcastle Coal Measures|33986|6|Mentioned|p30|||Table||||||
27861|Newcastle Coal Measures|34009|6|Mentioned|Table III|||||||||
27861|Newcastle Coal Measures|34015|6|Mentioned|p323|||Permian||||||
27861|Newcastle Coal Measures|34020|4|Described|p43|||||||||
27861|Newcastle Coal Measures|34037|6|Mentioned|Table 5.27|||||||||
27861|Newcastle Coal Measures|34038|6|Mentioned|p435|||||||||
27861|Newcastle Coal Measures|34039|6|Mentioned|p355|||||||||
27861|Newcastle Coal Measures|34040|6|Mentioned|p384|||Permian||||||
27861|Newcastle Coal Measures|34059|6|Mentioned|Map legend|Permian|Permian|||||||
27861|Newcastle Coal Measures|34106|6|Mentioned|p401|||||||||
27861|Newcastle Coal Measures|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
27861|Newcastle Coal Measures|34140|6|Mentioned|p45|||||||||
27861|Newcastle Coal Measures|34156|6|Mentioned|p387|||||||||
27861|Newcastle Coal Measures|34171|6|Mentioned|p16|||||||||
27861|Newcastle Coal Measures|34270|6|Mentioned|Table 1|||||||||
27861|Newcastle Coal Measures|34271|6|Mentioned|p12|||||||||
27861|Newcastle Coal Measures|34287|6|Mentioned|p130|||Permian. See also PP135, 164||||||
27861|Newcastle Coal Measures|34292|6|Mentioned|Table 1|||See also PP27,32. Permian||||||
27861|Newcastle Coal Measures|34300|6|Mentioned|p13|||||||||
27861|Newcastle Coal Measures|34302|6|Mentioned|p13|||||||||
27861|Newcastle Coal Measures|34339|6|Mentioned|Fig.5.46|||See also Fig.5.47 - Tectofacies map. Isopach map||||||
27861|Newcastle Coal Measures|34351|3|Fully described|p339|||See also pp340-345.||||||14-MAR-07
27861|Newcastle Coal Measures|34399|6|Mentioned|p312|||||||||
27861|Newcastle Coal Measures|34400|6|Mentioned|p9|||||||||
27861|Newcastle Coal Measures|34437|6|Mentioned|p406|||||||||
27861|Newcastle Coal Measures|34444|6|Mentioned|Map legend|Permian|Permian|||||||
27861|Newcastle Coal Measures|34447|6|Mentioned|Table 5.2|||||||||
27861|Newcastle Coal Measures|34448|5|Briefly described|Table 5.31|||Permian||||||
27861|Newcastle Coal Measures|34465|6|Mentioned|p334|||||||||
27861|Newcastle Coal Measures|34466|6|Mentioned|p350|||||||||
27861|Newcastle Coal Measures|34492|6|Mentioned|p67|||||||||
27861|Newcastle Coal Measures|34511|6|Mentioned|p47|||||||||
27861|Newcastle Coal Measures|34516|6|Mentioned|p16|||||||||
27861|Newcastle Coal Measures|34517|6|Mentioned|p46|||||||||
27861|Newcastle Coal Measures|34605|6|Mentioned|p376|||||||||
27861|Newcastle Coal Measures|34982|6|Mentioned|p49|||||||||
27861|Newcastle Coal Measures|35065|6|Mentioned|p43|||||||||
27861|Newcastle Coal Measures|35138|6|Mentioned|p17|||||||||
27861|Newcastle Coal Measures|35238|6|Mentioned|Fig.5|||||||||
27861|Newcastle Coal Measures|35268|6|Mentioned|p9|||||||||
27861|Newcastle Coal Measures|35284|6|Mentioned|Fig.12|||||||||
27861|Newcastle Coal Measures|35319|6|Mentioned|Table 1|||||||||
27861|Newcastle Coal Measures|35416|6|Mentioned|Fig.2|||Stratigraphy and palynological framework shown||||||
27861|Newcastle Coal Measures|35767|6|Mentioned|p8|||||||||
27861|Newcastle Coal Measures|35803|6|Mentioned|p321|||||||||
27861|Newcastle Coal Measures|35873|6|Mentioned|p45|||||||||
27861|Newcastle Coal Measures|35901|6|Mentioned|p5|||||||||
27861|Newcastle Coal Measures|35913|6|Mentioned|p36|||||||||
27861|Newcastle Coal Measures|35914|6|Mentioned|p8|||||||||
27861|Newcastle Coal Measures|36009|6|Mentioned|Table 1|||||||||
27861|Newcastle Coal Measures|36042|6|Mentioned|p19|||See also Table 1.||||||
27861|Newcastle Coal Measures|36172|6|Mentioned|Appendix|||||||||
27861|Newcastle Coal Measures|36327|6|Mentioned|p3|||||||||
27861|Newcastle Coal Measures|36390|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27861|Newcastle Coal Measures|36593|6|Mentioned|p187|||||||||
27861|Newcastle Coal Measures|37000|6|Mentioned|p23|||||||||
27861|Newcastle Coal Measures|37065|6|Mentioned|p32|||||||||
27861|Newcastle Coal Measures|37081|6|Mentioned|p156|||||||||
27861|Newcastle Coal Measures|37082|6|Mentioned|p160|||||||||
27861|Newcastle Coal Measures|37083|4|Described|p165|||||||||
27861|Newcastle Coal Measures|37084|6|Mentioned|p176|||||||||
27861|Newcastle Coal Measures|37085|6|Mentioned|p180|||||||||
27861|Newcastle Coal Measures|37086|5|Briefly described|p183,185,189,Fig.1,3||Permian|Now not regarded as part of Singleton Group.||||||
27861|Newcastle Coal Measures|37087|6|Mentioned|p195|||||||||
27861|Newcastle Coal Measures|37088|6|Mentioned|p205|||||||||
27861|Newcastle Coal Measures|37102|6|Mentioned|p264|||||||||
27861|Newcastle Coal Measures|37400|6|Mentioned|p313|||||||||
27861|Newcastle Coal Measures|37446|6|Mentioned|p187|||||||||
27861|Newcastle Coal Measures|37804|6|Mentioned|p55|||||||||
27861|Newcastle Coal Measures|37922|5|Briefly described|p483|||||||||
27861|Newcastle Coal Measures|37966|6|Mentioned|p4|||||||||
27861|Newcastle Coal Measures|38064|6|Mentioned|p41|||||||||
27861|Newcastle Coal Measures|38656|6|Mentioned|p138|||||||||
27861|Newcastle Coal Measures|38712|6|Mentioned|p63|||||||||
27861|Newcastle Coal Measures|38958|5|Briefly described|p493|||||||||
27861|Newcastle Coal Measures|39266|6|Mentioned|p221|||||||||
27861|Newcastle Coal Measures|39268|6|Mentioned|Fig. 5|||||||||
27861|Newcastle Coal Measures|39272|6|Mentioned|p297|||||||||
27861|Newcastle Coal Measures|39287|6|Mentioned|p20|||See also Fig.2.5||||||
27861|Newcastle Coal Measures|39288|6|Mentioned|p64|||||||||
27861|Newcastle Coal Measures|39292|3|Fully described|p101|||||||||
27861|Newcastle Coal Measures|39294|6|Mentioned|p163|||||||||
27861|Newcastle Coal Measures|39299|6|Mentioned|p288|||||||||
27861|Newcastle Coal Measures|39306|6|Mentioned|Fig. 21.2|||||||||
27861|Newcastle Coal Measures|39307|6|Mentioned|Table 22.1|||||||||
27861|Newcastle Coal Measures|39308|6|Mentioned|p458|||||||||
27861|Newcastle Coal Measures|39609|6|Mentioned|p2|||||||||
27861|Newcastle Coal Measures|39653|6|Mentioned|p69|||||||||
27861|Newcastle Coal Measures|39664|6|Mentioned|Table 8|||||||||
27861|Newcastle Coal Measures|39666|6|Mentioned|p89|||||||||
27861|Newcastle Coal Measures|39777|6|Mentioned|p141|||||||||
27861|Newcastle Coal Measures|39811|6|Mentioned|Map legend|Permian|Permian|||||||
27861|Newcastle Coal Measures|39812|6|Mentioned|Map legend|Permian|Permian|||||||
27861|Newcastle Coal Measures|40087|6|Mentioned|p237|||||||||
27861|Newcastle Coal Measures|40166|4|Described|p346|||||||||
27861|Newcastle Coal Measures|40256|6|Mentioned|p303|||||||||
27861|Newcastle Coal Measures|40321|6|Mentioned|p17|||||||||
27861|Newcastle Coal Measures|40335|6|Mentioned|p100|||||||||
27861|Newcastle Coal Measures|40396|5|Briefly described|p13|||||||||
27861|Newcastle Coal Measures|40602|6|Mentioned|p7|||||||||
27861|Newcastle Coal Measures|40625|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27861|Newcastle Coal Measures|40630|6|Mentioned|p178|||||||||
27861|Newcastle Coal Measures|40631|6|Mentioned|p162|||||||||
27861|Newcastle Coal Measures|40633|6|Mentioned|Fig.1-D|||||||||
27861|Newcastle Coal Measures|40635|6|Mentioned|p39|||||||||
27861|Newcastle Coal Measures|40636|6|Mentioned|p43|||||||||
27861|Newcastle Coal Measures|40807|6|Mentioned|p161|||||||||
27861|Newcastle Coal Measures|40883|6|Mentioned|p9|||||||||
27861|Newcastle Coal Measures|40963|6|Mentioned|p265|||||||||
27861|Newcastle Coal Measures|40971|6|Mentioned|p206|||||||||
27861|Newcastle Coal Measures|41054|6|Mentioned|p151|||||||||
27861|Newcastle Coal Measures|41130|4|Described|p47|||||||||
27861|Newcastle Coal Measures|41226|6|Mentioned|Table 1|||||||||
27861|Newcastle Coal Measures|41463|6|Mentioned|p37|||||||||
27861|Newcastle Coal Measures|41474|6|Mentioned|p63|||||||||
27861|Newcastle Coal Measures|41476|6|Mentioned|p75|||||||||
27861|Newcastle Coal Measures|41477|6|Mentioned|p79|||||||||
27861|Newcastle Coal Measures|41479|6|Mentioned|p93|||||||||
27861|Newcastle Coal Measures|41480|6|Mentioned|p9|||||||||
27861|Newcastle Coal Measures|41596|6|Mentioned|p106|||||||||
27861|Newcastle Coal Measures|41689|6|Mentioned|Table 1|||||||||
27861|Newcastle Coal Measures|41902|6|Mentioned|p22|||||||||
27861|Newcastle Coal Measures|41911|6|Mentioned|p147|||||||||
27861|Newcastle Coal Measures|42091|6|Mentioned|p284|||||||||
27861|Newcastle Coal Measures|42182|4|Described|p297|Late Permian|Late Permian|See also Table 1||||||04-NOV-04
27861|Newcastle Coal Measures|42214|6|Mentioned|p460|||||||||
27861|Newcastle Coal Measures|42526|6|Mentioned|Map legend|||||||||
27861|Newcastle Coal Measures|42641|6|Mentioned|p115|||||||||
27861|Newcastle Coal Measures|42648|4|Described|p33|||||||||
27861|Newcastle Coal Measures|42713|5|Briefly described|Fig. P18|||||||||
27861|Newcastle Coal Measures|42767|5|Briefly described|p5|||see also Fig.5||||||
27861|Newcastle Coal Measures|42780|5|Briefly described|Fig.2 P412|||||||||
27861|Newcastle Coal Measures|42965|6|Mentioned|p38|||||||||
27861|Newcastle Coal Measures|42992|6|Mentioned|p36|||||||||
27861|Newcastle Coal Measures|43017|5|Briefly described|Fig.1,p372|||||||||
27861|Newcastle Coal Measures|43194|5|Briefly described|p115, p129 Tb. 8.3, p130|Late Permian|Late Permian|May correlate with the upper lithic sequence (now Nea Subgroup) of the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
27861|Newcastle Coal Measures|43317|5|Briefly described|Table 1 p7|||||||||
27861|Newcastle Coal Measures|43318|14|Not recorded|opp p6|||||||||
27861|Newcastle Coal Measures|43319|14|Not recorded|Map Legend|||||||||
27861|Newcastle Coal Measures|43320|14|Not recorded|Table 1 p9,26-28,30||Permian|||||||
27861|Newcastle Coal Measures|43322|14|Not recorded|p7|||SI 56-5 Broken Bay||||||
27861|Newcastle Coal Measures|43344|14|Not recorded|p11,18,20,21,78,79,|||84,85,89,164||||||
27861|Newcastle Coal Measures|43370|4|Described|p1,3,4,6,9|||||||||
27861|Newcastle Coal Measures|43376|14|Not recorded|p149|||||||||
27861|Newcastle Coal Measures|43383|14|Not recorded|p20,Fig.5|||||||||
27861|Newcastle Coal Measures|43384|14|Not recorded|Map Legend||Late Permian|||||||
27861|Newcastle Coal Measures|43385|14|Not recorded|p179||Late Permian|||||||
27861|Newcastle Coal Measures|43408|14|Not recorded|Map Legend|||||||||
27861|Newcastle Coal Measures|43409|14|Not recorded|Map Legend|||Black Jack Formation is an equivalent||||||
27861|Newcastle Coal Measures|43424|14|Not recorded|p11-17|||||||||
27861|Newcastle Coal Measures|43425|14|Not recorded|p3||Permian|||||||
27861|Newcastle Coal Measures|43440|14|Not recorded|p32,34,44,48,59,63,|||p71,72,90||||||
27861|Newcastle Coal Measures|43447|14|Not recorded|Table 1,p15,20,23,|||diag.p26,27-29,32,37,43,46,47,49||||||
27861|Newcastle Coal Measures|43448|4|Described|p221-227,Pl.2,3,231,|||See base card table for new divisions. p233-236||||||
27861|Newcastle Coal Measures|43450|14|Not recorded|p9,10,11,16,17,24|||||||||
27861|Newcastle Coal Measures|43451|14|Not recorded|Map Legend|||||||||
27861|Newcastle Coal Measures|43477|2|Defined|p12-17,19-26,39,40,|||p46,47,49,51,52,55-62,Pl.1,5||||||
27861|Newcastle Coal Measures|43479|14|Not recorded|p190,199,208,218-9||Tatarian|||||||
27861|Newcastle Coal Measures|43491|4|Described|pVII/44,52||Permian|||||||
27861|Newcastle Coal Measures|43508|14|Not recorded|p122|||||||||
27861|Newcastle Coal Measures|43545|14|Not recorded|p417|||From reprint. Correct reference not shown||||||
27861|Newcastle Coal Measures|43881|14|Not recorded|p87-88,99|||p87-88(proximate anals.)||||||
27861|Newcastle Coal Measures|43917|14|Not recorded|p30|||||||||
27861|Newcastle Coal Measures|43984|14|Not recorded|p135-138,140|||||||||
27861|Newcastle Coal Measures|44040|14|Not recorded|p23|||||||||
27861|Newcastle Coal Measures|44219|14|Not recorded|p31||Tatarian|||||||
27861|Newcastle Coal Measures|44244|5|Briefly described|p276, p292|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||25-AUG-04
27861|Newcastle Coal Measures|44248|14|Not recorded|p34|||||||||
27861|Newcastle Coal Measures|44265|14|Not recorded|p113|||||||||
27861|Newcastle Coal Measures|44347|14|Not recorded|p85|||Fossil 'Leaia' sp. found near Belmont, very similar to that in Upper Bowen Coal Measures.||||||
27861|Newcastle Coal Measures|44610|14|Not recorded|p49|||||||||
27861|Newcastle Coal Measures|44855|14|Not recorded|p18||Permian|||||||
27861|Newcastle Coal Measures|44861|14|Not recorded|p227,232,246|||||||||
27861|Newcastle Coal Measures|44998|14|Not recorded|p104|||Correlated with Condren Member (W.A.).||||||
27861|Newcastle Coal Measures|45025|6|Mentioned|p61|||||||||
27861|Newcastle Coal Measures|45071|6|Mentioned|p68|||See also P77||||||
27861|Newcastle Coal Measures|45088|6|Mentioned|p59|||Permian||||||
27861|Newcastle Coal Measures|45090|6|Mentioned|p26|||Relationship of rock units||||||
27861|Newcastle Coal Measures|45095|6|Mentioned|p35|||||||||
27861|Newcastle Coal Measures|45138|6|Mentioned|p3|||||||||
27861|Newcastle Coal Measures|46849|6|Mentioned|p195|||||||||
27861|Newcastle Coal Measures|48926|6|Mentioned|p9|||P9 et seq.||||||
27861|Newcastle Coal Measures|49644|5|Briefly described|Table|||||||||
27861|Newcastle Coal Measures|50112|5|Briefly described|p117|Late Permian|Late Permian|Includes Lambton Formation.||||||04-MAY-05
27861|Newcastle Coal Measures|60281|4|Described|p62|Late Permian|Late Permian|Greywacke, siltstone, mudstone, lithic sandstone and coal units.  Overlie the Tomago Coal Measures.  Age: 256.5-252.5Ma.  Geological Province: Sydney Basin.  See also p6, p8, p61.||||||
27861|Newcastle Coal Measures|60297|6|Mentioned|p168 Fig.1|Permian|Permian|||||||
27861|Newcastle Coal Measures|60726|5|Briefly described|p1-3, p10, throughout text.|Late Permian|Late Permian||||Boolaroo, Lambton Formations; Dudley Coal Seam.|||
27861|Newcastle Coal Measures|61315|5|Briefly described|p167, Table SY1|Late Permian|Late Permian|Includes Lambton Formation, Nobbys Tuff, Adamstown Subgroup, Warners Bay and Boolaroo Formations, Awaba Tuff and Moon Island Beach Formation. Geological Province: Sydney Basin.||||||
27861|Newcastle Coal Measures|61529|5|Briefly described|p857 Fig. 3a|||Overlies Tomago Coal Measures. Geological Province: Sydney Basin. See also p868.||||||
27861|Newcastle Coal Measures|61612|6|Mentioned|p274, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||17-MAR-09
27861|Newcastle Coal Measures|61770|6|Mentioned|p110, p111|||||||||
27861|Newcastle Coal Measures|62033|4|Described|p24, p25 (Table)|||Replaces entire Wollombi C. M. nomenclature in northern Sydney Basin - as ratified by Coalfield Geology Council (2004) - also recommending Amoco Wybong DDH1 be adopted as 'Reference Bore' for Newcastle. C.M. in the Hunter Valley (formerly Wollombi C.M.).||||||04-FEB-08
27861|Newcastle Coal Measures|63832|6|Mentioned|p131 fig 2|Lopingian|Lopingian|Of Sydney Basin.||||||
27861|Newcastle Coal Measures|63868|6|Mentioned|p17, p21, p26|||Of NSW.||||||07-FEB-11
27861|Newcastle Coal Measures|64631|6|Mentioned|p44 Fig.2.|Changhsingian|Wuchiapingian|NE Sydney Basin.||||Overlies Tomago Coal Measures. Time equivalent to Wallarawang Subgroup, Eckersley Formation.||
27861|Newcastle Coal Measures|65107|6|Mentioned|p278|Late Permian|Late Permian|Provides constraint on Australia's Later Permian "westward loop" pole path. Pre Mesozoic. No radiometric date||||||
27861|Newcastle Coal Measures|66891|5|Briefly described|p179. |Late Permian|Late Permian|Frequent and complex faulting in this unit has resulted from east-west compression. Lies 100-200 m below the surface in the mid-Wybong Creek catchment; outcrops in the southeast.||||Is overlain by Narrabeen Group.||
27861|Newcastle Coal Measures|67500|6|Mentioned|p19|||||||||
27861|Newcastle Coal Measures|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Late Permian.||||Unconformably overlain by the Narrabeen Group. Underlain by the Tomago Coal Measures.||
27861|Newcastle Coal Measures|67786|5|Briefly described|p94-96|Permian|Permian|Sydney Basin. Late Permian. Alluvial fan and braided river systems.|||Moon Island Beach, Boolaroo, Adamstown, Lambton Subgroups.|Overlies Tomago Coal Measures. Is overlain by Narrabeen Group.|Includes several tuffaceous units (ash fall and ash flow).|
27861|Newcastle Coal Measures|67788|6|Mentioned|p22, 30|Permian|Permian|Mentioned in a list of units containing braided and low-sinuosity river deposits. S-flowing trunk axial channels, up to 70m deep.||||||
27861|Newcastle Coal Measures|68003|5|Briefly described|p41, p42.|Late Permian|Late Permian|Northern Sydney Basin. Formed by southward-prograding major fluvio-deltaic systems. Referred to as 'Newcastle-Tomago Coal Measures sequence' (p42) where both units were eroded off the Lochinvar Anticline before the Munmorah Conglomerate was unconformably deposited.||||||
27861|Newcastle Coal Measures|68004|5|Briefly described|p23 Table 1. |||Newcastle Coalfield.||||Overlies Tomago Coal Measures. Is overlain by Narrabeen Group.||
27861|Newcastle Coal Measures|68202|6|Mentioned|p176|Permian|Permian|Sydney Basin. Swampy-deltaic conditions followed uplift of the New England Orogen in Late Permian.|||||Extensive coal deposits.|
27861|Newcastle Coal Measures|68493|5|Briefly described|p3 Fig.1, p5, p5 Fig.2, p6|Permian|Permian|Youngest Permian strata in the Hunter Valley. Sydney Basin. Alluvial fan depositional environment with extensive swamps.|||Includes Moon Island Beach Formation, Awaba Tuff, Boolaroo Formation, Warners Bay Tuff, Adamstown Formation, Nobbys Tuff, Lambton Formation, Waratah Sandstone.|Overlies Maitland Group and Tomago Coal Measures. Is overlain by Narrabeen Group.|Coarsening-upward sequence of low sand:shale ratio. Conglomerates within this unit have well-rounded clasts of chert, sandstone, siltstone, quartzite, and volcanic rocks. Felsic tuff layers also occur within the sequence.|
27861|Newcastle Coal Measures|68711|3|Fully described|p113-119, p116 Tbl 2|||Top redefined as above the uppermost coal, usually the Vales Point seam. This redefinition first proposed by Uren (1977). Base redefined as the top of the Waratah Sandstone.  Note: Table 2 wrongly shows Waratah Sandstone as still part of the Newcastle Coal Measures. |||Includes Lambton Formation, Nobbys Tuff, Adamstown Formation, Warners Bay Tuff, Boolaroo Formation, Awaba Tuff, Moon Island Beach Formation|Overlies Waratah Sandstone. Overlain by Narrabeen Group.||
27861|Newcastle Coal Measures|69297|6|Mentioned|p499, p501, p502 fig 5.43, p503|Late Permian|Middle Permian|Sydney Basin. Deposited in a fluvial-deltaic environment. Has some potential as a gas or petroleum source rock.||Singleton Group||Overlies the Tomago Coal Measures.|Sandstones, siltstones and coals.|
27861|Newcastle Coal Measures|69683|5|Briefly described|p410 Fig.1, p411 Fig.2, p414, p420 Fig.5|Late Permian|Late Permian|||Unit in Singleton Supergroup.|Includes Lambton, Adamstown, Boolaroo and Moon Island Beach Formations; Nobbys, Warners Bay and Awaba Tuffs.||Coal seams, tuffaceous claystone, siltstone, sandstone, conglomerate.|
27861|Newcastle Coal Measures|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Singleton Supergroup|Includes Moon Island Beach, Boolaroo, Adamstown, Lambton Subgroups; Waratah Sandstone.|||04-OCT-16
27861|Newcastle Coal Measures|70791|5|Briefly described|p277|Lopingian|Lopingian|Hunter Coalfield.||Singleton Supergroup.||||
27861|Newcastle Coal Measures|70837|5|Briefly described|p245-246|Permian|Permian|Of Northern Sydney Basin.|||Includes Moon Island Beach Formation, Coepwe, Awaba, Nalleen and Nobbys tuffs, and Great Northern Coal Seam.|||
27861|Newcastle Coal Measures|70878|5|Briefly described|p710, p712, p715|Permian|Permian|Hunter Valley. 251.08m thick in Amoco Wybong 1 well. Calibration of palynological ages.|||Awaba, Warners Bay, Nobbys Tuffs; Lambton, Adamstown Formations.|Overlies Wittingham Coal Measures. Is overlain by Narrabeen Group.||
27861|Newcastle Coal Measures|71115|6|Mentioned|p186|Permian|Permian|Sydney Basin. Mentioned in connection with dual-polarity dykes dated at 79.6 +/- 1.8 Ma and 78.0 +/- 2.2 Ma (K/Ar, whole rock), and their relationship with paleomagnetism in the Gerringong Volcanics.||||||
27861|Newcastle Coal Measures|71542|6|Mentioned|p26|Permian|Permian|SHRIMP zircon data, combined with correlation based on brachiopod zones, suggested the Gerringong Volcanics is older than 253 Ma.||||||
27861|Newcastle Coal Measures|71701|5|Briefly described|p159, p169-170||||||Includes the Bulli Coal Seam and the Nobbys Tuff.|||08-FEB-23
27861|Newcastle Coal Measures|73304|6|Mentioned|p61, p65-67, p70-71, p75, p77-79|||Sydney Basin, northern. End-Permian mass extinction is recognised at the top of this unit. Middle portion contains the Wuchiapingian-Changhsingian boundary. Equivalent[?] to Illawarra Coal Measures. [Top?] boundary marks a major extinction of peat-producing plants.||Singleton Supergroup|Nobbys Tuff, Awaba Tuff, Moon Island Beach Formation, Mannering Park Tuff, Cowper Tuff|||
27861|Newcastle Coal Measures|73625|6|Mentioned|p2|Permian|Permian|Newcastle coalfield, Sydney Basin.||||Overlies Waratah Sandstone. Is overlain by Narrabeen Group.||
78602|Newholme Monzogranite|66660|3|Fully described|p342-p349|Changhsingian|Wuchiapingian|New name. Central Block, New England Orogen. Occurs at the southern margin of the Mount Duval Monzogranite; distinguishable by its high radiometric response. 10km NNW Armidale. Medium to coarse grained, massive and non-foliated, mesocratic grey granitoid, in places K-feldspar porphyritic.. Distinguished from Mount Duval Monzogranite on basis of enclaves: igneous 21%, metasedimentary 61%, quartz 18%.|SHRIMP U-Pb zircon age 253.7 +/- 1.4 Ma.|Of Uralla Supersuite.||Intrudes the Sandon beds. Overlain by Tertiary basaltic lavas and intruded by Miocene (16.5 Ma K-Ar) basalt plugs.||07-OCT-15
78602|Newholme Monzogranite|69188|5|Briefly described|p1-2, p4, p51-54, p79|Early Triassic|Permian|Indistinguishable in age from Mount Duval Monzogranite; recognised as a separate entity in the Mount Duval pluton on the basis of geophysics, petrography and geochemistry. Also appears as Newholme monzogranite on p51.|252.8 +/- 1.5 Ma (magmatic age)||||Medium- to coarse-grained, sparsely porphyritic (K-feldspar phenocrysts to 6mm) monzonite.|16-APR-20
78602|Newholme Monzogranite|69639|5|Briefly described|p32, p68, p95, p133, p219|Induan|Changhsingian|New England Orogen.|252.8 +/- 1.5 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
78602|Newholme Monzogranite|70217|5|Briefly described|p73 tbl 14.1|Changhsingian|Changhsingian|New England Orogen. Age derived from Cross and Blevin, 2010.|252.8 +/- 1.5 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
78602|Newholme Monzogranite|71628|4|Described|p8: 3, 33-36, 37-40|||Vickery et al. (2010) after work by Brown (2003) and others. Previously regarded as part of Mount Duval Monzogranite. Named after the Newholme property. ~10km NNW of Armidale. Crops out as whalebacks and tors. Exceptionally enriched in K2O, Th and U. Associated with Au-Sb-Ag-As mineralisation near contact with Mount Duval Monzogranite.|252.8 +/- 1.5 Ma (SHRIMP: Cross and Blevin, 2013).|Mount Duval Suite.||Intrudes Sandon beds. Is enclosed by Mount Duval Monzogranite (no contact observed).|Grey, medium- to coarse-grained, locally porphyritic, biotite-hornblende monzogranite; locally contains leucomonzogranite dykes.|
24618|Newnes Formation|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Charbon Subgroup (Illawarra Coal Measures). Lithic sandstone, siltstone, claystone. Max. thickness: 14m. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
24618|Newnes Formation|39232|4|Described|p109|||||||||
24618|Newnes Formation|40256|6|Mentioned|p305|||||||||
24618|Newnes Formation|40806|2|Defined|p155|Permian|Permian|Prob. Permian||||||
24618|Newnes Formation|42657|4|Described|p78|||||||||
24618|Newnes Formation|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
24618|Newnes Formation|63832|5|Briefly described|p137|Late Permian|Late Permian|Shows stratigraphically highest evidence of Permian glaciation in eastern Australia, indicating westward retreat of glaciers.||Illawarra Coal Measures|||Continental proglacial and possibly subglacial facies.|13-DEC-17
24618|Newnes Formation|64631|6|Mentioned|p49.|Changhsingian|Wordian|Sydney Basin. Contains stratigraphically highest evidence of Permian glaciation of eastern Australia.||Unit in upper Illawarra Coal Measures.||||
24618|Newnes Formation|68004|5|Briefly described|p60 Table 6, p61.|Late Permian|Late Permian|Western Coalfield. From 8 to 14.5 m thick.||Unit in Charbon Subgroup.||Overlies Ulan Coal and Irondale Coal. Is overlain by Glen Davis Formation.|Fine- to medium-grained, lithic sandstone, with interbedded siltstone and claystone (west of Wollar Hingeline) and upward-fining lithic sandstone (east of the Wollar Hingeline).|
24618|Newnes Formation|73304|6|Mentioned|p77|||Sydney Basin. Includes the youngest glacial facies in the basin.||Charbon Sub-group|||Includes glacial facies.|
29789|Newport Formation (NSW)|22549|6|Mentioned|p526||Early Triassic|||||||
29789|Newport Formation (NSW)|22745|5|Briefly described|p133|||Narrabeen Group, Sydney Basin. 90 m.||||||
29789|Newport Formation (NSW)|22749|6|Mentioned|p185,190-91|||||||||
29789|Newport Formation (NSW)|22833|6|Mentioned|p653|||of Sydney Basin.||||||
29789|Newport Formation (NSW)|22857|5|Briefly described|p530 App.1 Tb.A1.9|Middle Triassic|Early Triassic|Of the Gosford Subgroup (Narrabeen Group). Interbedded laminite, shale, quartz to lithic-quartz sandstone; minor red claystone. Max. thickness: 50m. Geological Province: Sydney Basin.||||||
29789|Newport Formation (NSW)|22969|4|Described|p 6, Fig 4.1b|Middle Triassic|Early Triassic|||||||
29789|Newport Formation (NSW)|23881|5|Briefly described|p69 Fig. 7.2|||Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
29789|Newport Formation (NSW)|29901|4|Described|Table 1|||||||||
29789|Newport Formation (NSW)|30007|6|Mentioned|p61|||||||||
29789|Newport Formation (NSW)|30132|6|Mentioned|Table 1|||||||||
29789|Newport Formation (NSW)|30707|6|Mentioned|p6|||Refers Bunny & Herbert (1971)||||||
29789|Newport Formation (NSW)|31061|6|Mentioned|Table 1|||||||||
29789|Newport Formation (NSW)|31276|6|Mentioned|p150|||Palynology. Interpretative section.||||||
29789|Newport Formation (NSW)|31297|5|Briefly described|p4|||See also P6, Fig. 3||||||
29789|Newport Formation (NSW)|31725|6|Mentioned|p10|||On table||||||
29789|Newport Formation (NSW)|31884|6|Mentioned|Table 1|||Triassic||||||
29789|Newport Formation (NSW)|31886|6|Mentioned|Table 1|||||||||
29789|Newport Formation (NSW)|31887|5|Briefly described|p8|||||||||
29789|Newport Formation (NSW)|32101|6|Mentioned|p107|||Refers Bunny & Herbert (1971), Ward (1972)||||||
29789|Newport Formation (NSW)|32537|4|Described|p7|||Description of sediments||||||
29789|Newport Formation (NSW)|32719|5|Briefly described|p212|||Climatic conditions. Correlation. Section P209.||||||
29789|Newport Formation (NSW)|32799|6|Mentioned|p9|||||||||
29789|Newport Formation (NSW)|32800|6|Mentioned|p384|||||||||
29789|Newport Formation (NSW)|32801|6|Mentioned|p254|||||||||
29789|Newport Formation (NSW)|32802|6|Mentioned|p19|||||||||
29789|Newport Formation (NSW)|33683|4|Described|Table 1|||Narrabeen Gp.||||||
29789|Newport Formation (NSW)|33685|5|Briefly described|p397|||||||||
29789|Newport Formation (NSW)|33867|6|Mentioned|Table 1|||||||||
29789|Newport Formation (NSW)|34205|6|Mentioned|Table 6|||Correlation with Burralow Formation||||||
29789|Newport Formation (NSW)|34236|6|Mentioned|p17|||||||||
29789|Newport Formation (NSW)|34336|6|Mentioned|Fig.5.33|||||||||
29789|Newport Formation (NSW)|35280|6|Mentioned|p148|||||||||
29789|Newport Formation (NSW)|35416|6|Mentioned|Fig.2|||Stratigraphy and palynological framework shown||||||
29789|Newport Formation (NSW)|35488|6|Mentioned|p74|||||||||
29789|Newport Formation (NSW)|35502|6|Mentioned|p182|||||||||
29789|Newport Formation (NSW)|35647|6|Mentioned|p51|||||||||
29789|Newport Formation (NSW)|35690|6|Mentioned|p61|||||||||
29789|Newport Formation (NSW)|35874|5|Briefly described|p1|||||||||
29789|Newport Formation (NSW)|36042|6|Mentioned|Fig.25|||||||||
29789|Newport Formation (NSW)|36220|4|Described|p73|||See also P65 & Table 20.||||||
29789|Newport Formation (NSW)|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
29789|Newport Formation (NSW)|37757|6|Mentioned|p19|||||||||
29789|Newport Formation (NSW)|37804|6|Mentioned|Table 1|||||||||
29789|Newport Formation (NSW)|38784|6|Mentioned|p78|||||||||
29789|Newport Formation (NSW)|39287|6|Mentioned|Fig. 2.18|||||||||
29789|Newport Formation (NSW)|39293|6|Mentioned|p152|||||||||
29789|Newport Formation (NSW)|39296|6|Mentioned|p186|||||||||
29789|Newport Formation (NSW)|39300|6|Mentioned|p313|||||||||
29789|Newport Formation (NSW)|39306|5|Briefly described|Fig. 21.11|||See also P411,414,422,389||||||
29789|Newport Formation (NSW)|40602|4|Described|p13|||||||||
29789|Newport Formation (NSW)|40603|6|Mentioned|p5|||||||||
29789|Newport Formation (NSW)|40625|6|Mentioned|Map legend|||Early to Middle Triassic||||||
29789|Newport Formation (NSW)|40652|6|Mentioned|p128|||||||||
29789|Newport Formation (NSW)|40653|6|Mentioned|p121|||||||||
29789|Newport Formation (NSW)|42737|5|Briefly described|map legend|Triassic||||||||
29789|Newport Formation (NSW)|42896|3|Fully described|p29, Table 2|||of Gosford Subgroup||||||
29789|Newport Formation (NSW)|42925|5|Briefly described|Table 18||Middle Triassic|||||||
29789|Newport Formation (NSW)|42926|4|Described|map legend||Middle Triassic|||||||
29789|Newport Formation (NSW)|43072|6|Mentioned|p55|||NSW?||||||
29789|Newport Formation (NSW)|45090|6|Mentioned|p71|||Relationship in Narrabeen Gp.||||||
29789|Newport Formation (NSW)|60281|5|Briefly described|Fig. 15 Appendix 1|||Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
29789|Newport Formation (NSW)|61315|5|Briefly described|Table SY2|Middle Triassic|Middle Triassic|Of Narrabeen Group. Lower part contains quartzose sandstones which are top-sealed by the shaly laminite at the top of the unit. The shaly laminite may provide a secondary reservoir seal in the offshore part of the basin. Geological Province: Sydney Basin.||||||
29789|Newport Formation (NSW)|73304|6|Mentioned|p66, p74, p76|||Sydney Basin, southern.||Narrabeen Group||Possible underlain by Garie Formation.||
25341|Newton Boyd Granodiorite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Of Moonbi Plutonic Suite.  Medium- to coarse-grained, equigranular to porphyritic biotite granodiorite and monzogranite; includes altered granitoid; coares-to medium-grained, equigranular to porphyritic to irregularly textured, granular felsic rock.||||||20-DEC-04
25341|Newton Boyd Granodiorite|23812|5|Briefly described|p21 Tb.2, p10|Early Triassic|Late Permian|Of Moonbi Plutonic Suite.||||||
25341|Newton Boyd Granodiorite|35173|2|Defined|p106|Late Paleozoic|Late Paleozoic|Prob. Late Palaeozoic||||||07-NOV-08
25341|Newton Boyd Granodiorite|36411|6|Mentioned|p269|||Refs Korsch 1978 for definition.||||||
25341|Newton Boyd Granodiorite|42719|5|Briefly described|p14|||||||||
25341|Newton Boyd Granodiorite|42866|5|Briefly described|Table 2, P12|||||||||
25341|Newton Boyd Granodiorite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Moonbi Suite.  Monzogranite and granodiorite.||||||
25341|Newton Boyd Granodiorite|70876|5|Briefly described|p2-p3, p58-p64, p79-p81, p94|Triassic|Permian|New England Orogen. SHRIMP date is interpreted as a magmatic crystallisation age. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|252.8 +/- 1 Ma (SHRIMP U-Pb)|Herries Suite||||
25341|Newton Boyd Granodiorite|71628|4|Described|p7: 1; p11-21; p17: 1, 31, 44|||See also p19: 137-141, 165. Korsch et al. (1978). Previously mapped as part of Mount Mitchell Monzogranite. Named after a local river. Is located near Newton Boyd, ~50 km E of Armidale. Forms a recessive and deeply weathered intrusion of ~8 x 4 km. Because of its substantially older age, it is not included in the Coastal Granite Association. Lithology, mineralogy and geochemistry detailed. Is associated with two mineral deposits (named): vein Sb, As (Au, Ag) and vein Au.|252.8 +/- 1.0 Ma (SHRIMP: Waltenberg et al., 2016)|Newton Boyd Suite.||Intrudes Brooklana beds. Is faulted against Sara beds and Bruisers Creek Granodiorite Phase (of Mount Mitchell Monzogranite).|Medium- to coarse-grained, equigranular to porphyritic, biotite quartz monzodiorite and granodiorite, possibly with minor monzogranite; commonly weathered; extensively mylonitised on the western margin. I-type.|
26078|Newtown Formation|22857|4|Described|p508 App.1 Tb.A1.8|Visean|Visean|Of the Gilmore Volcanic Group. Red to purple lithic arenite; red, purple, green siltstone; pebble conglomerate. Max. thickness: 650m. Geological Province: Tamworth Forearc Basin.||||||
26078|Newtown Formation|24121|5|Briefly described|p4, p34, p154, 159|||||||||25-AUG-22
26078|Newtown Formation|31228|2|Defined|p80|Namurian|Visean|Visean - Namurian||||||
26078|Newtown Formation|40883|6|Mentioned|p13|||||||||
26078|Newtown Formation|44244|2|Defined|p88, p87|Carboniferous|Carboniferous|Of the Gilmore Volcanic Group.  Contains the basal Martins Creek Ignimbrite Member and Vacy Ignimbrite Member.  max. thickness: 565m.  Type section in text.  Geological Province: Gresford Block.||||||
26078|Newtown Formation|50147|5|Briefly described|Map legend|Visean|Visean|Of the Gilmore Volcanic Group.  Red to purple lithic sandstone, red, purple or green siltstone, pebble conglomerate with interbedded andesitic, and rhyodacitic to dacitic ignimbrite.  Geological Province: Gresford Block||||||
26078|Newtown Formation|50268|5|Briefly described|Map Legend|Visean|Visean|Overlies: Isismurra Formation, Wallaringa Formation, Flagstaff Formation. Underlies: Mowbray Formation and Isismurra Formation.  Of the Gilmore Volcanic Group.||||||27-MAY-08
26078|Newtown Formation|61768|6|Mentioned|p83 Fig. 2, p86|||Includes; Vacy Ignimbrite and Martian Creek Ignimbrite Member.||||||13-MAY-08
26078|Newtown Formation|73197|6|Mentioned|p467|Carboniferous|Carboniferous|New England Orogen, southern. Forearc basin, volcanic rocks sourced from the Currabubula-Connors Arc.|||||Volcanic rocks, predominantly ignimbrite.|
26078|Newtown Formation|73487|6|Mentioned|p566|||||||||
80454|Niemur granodiorite|70718|5|Briefly described|p61-p64|||Informal name, interpreted from geophysics. Intrudes the Bendigo Zone of the Murray Basin. Magnetic signatures suggest whole suite is I-type. Deniliquin 1:250 000 sheet area.||Jawbone Creek granodiorite suite||||03-APR-18
27092|Nile Subgroup|22857|5|Briefly described|p528App.1 Tb.A1.9|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
27092|Nile Subgroup|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|||||||
27092|Nile Subgroup|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
27092|Nile Subgroup|38614|6|Mentioned|Fig.6|||||||||
27092|Nile Subgroup|39232|4|Described|p111|||||||||
27092|Nile Subgroup|40166|6|Mentioned|p348|||See also Table 1||||||
27092|Nile Subgroup|40332|6|Mentioned|Fig.4|||||||||
27092|Nile Subgroup|40806|1|Redefined|p148|Permian|Permian|Prob. Permian||||||
27092|Nile Subgroup|41330|6|Mentioned|p19|||||||||
27092|Nile Subgroup|42657|6|Mentioned|p75|||||||||
27092|Nile Subgroup|42925|5|Briefly described|Table 18||Late Permian|||||||
27092|Nile Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
27092|Nile Subgroup|43194|5|Briefly described|p108, p129 Tb. 8.3|Late Permian|Late Permian|Western Coalfield, Sydney Basin. Correlated with the basal (coal bearing) lithic unit in the Black Jack Formation (now named Pamboola Formation) in the Gunnedah Basin.||||||
27092|Nile Subgroup|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin||||||
27092|Nile Subgroup|63832|5|Briefly described|p131 fig 2|Guadalupian|Guadalupian|Of Sydney Basin. Final (P4) Paleozoic glaciation.||Unit in Illawarra Coal Measures.||||13-DEC-17
27092|Nile Subgroup|64631|5|Briefly described|p44 Fig.2.|Capitanian|Wordian|NW, SW Sydney Basin.||Unit in Illawarra Coal Measures.||Overlies Berry Siltstone.||
27092|Nile Subgroup|68003|5|Briefly described|p38 Fig.3-j.|Late Permian|Late Permian|Western Coalfield, Brigalow Belt South Bioregion.||Basal unit in Illawarra Coal Measures.||Overlies Berry Siltstone and Budgong Sandstone. Is overlain by Cullen Bullen Subgroup.||
27092|Nile Subgroup|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Basal unit in Illawarra Coal Measures.|Includes Mount Marsden Claystone, Coorongooba Creek Sandstone, and Gundangaroo Formation.|Is overlain by Cullen Bullen Subgroup.||
27092|Nile Subgroup|70661|6|Mentioned|p187|||Not present in map area (Moss Vale)||Illawarra Coal Measures||||
26079|Nine Mile Volcanics|22857|4|Described|p117, p420 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Kiandra Group. Feldspathic arenite, shale, chert, high-K porphyritic basalt, basaltic tuff. Max. thickness: 1050m. ||||||
26079|Nine Mile Volcanics|22968|6|Mentioned|P106||Gisbornian|||||||
26079|Nine Mile Volcanics|23309|6|Mentioned|App1|||||||||
26079|Nine Mile Volcanics|24268|6|Mentioned|p1543 Fig.8|||Geological Province: Lachlan Fold Belt||||||
26079|Nine Mile Volcanics|24280|5|Briefly described|p1831|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
26079|Nine Mile Volcanics|31019|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26079|Nine Mile Volcanics|33004|6|Mentioned|p166|||||||||
26079|Nine Mile Volcanics|33325|5|Briefly described|Table 1|||Gisbornian||||||
26079|Nine Mile Volcanics|34404|4|Described|p92|||||||||
26079|Nine Mile Volcanics|36443|5|Briefly described|map legend|Late Ordovician|Darriwillian|Of Kiandra Group. BMR map codes Okt: basaltic tuff, minor chert and feldspathic arenite; Okl: high potassium porphyritic basalt. Interfingers with Temperance Formation. Geol. Prov: Molong Volcanic Arc.||||||
26079|Nine Mile Volcanics|36512|6|Mentioned|p21|||See also P26.||||||
26079|Nine Mile Volcanics|36534|6|Mentioned|p223|||||||||
26079|Nine Mile Volcanics|39447|6|Mentioned|p5|||||||||
26079|Nine Mile Volcanics|40136|5|Briefly described|p34|||See also P26||||||
26079|Nine Mile Volcanics|40328|6|Mentioned|p67|||Also mentioned P68||||||
26079|Nine Mile Volcanics|40497|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26079|Nine Mile Volcanics|40498|6|Mentioned|p330|||||||||
26079|Nine Mile Volcanics|41905|6|Mentioned|p27|||||||||
26079|Nine Mile Volcanics|42313|6|Mentioned|p132|||||||||
26079|Nine Mile Volcanics|45147|2|Defined|M32|Gisbornian|Gisbornian|||||||
26079|Nine Mile Volcanics|46524|6|Mentioned|p123|||||||||
26079|Nine Mile Volcanics|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Conformably overlies Kiandra Beds. Of the Molong Volcanic Rise. Geological Province: Lachlan Pre-Cratonic Province.||||||20-MAY-08
26079|Nine Mile Volcanics|60308|6|Mentioned|p38|||"Important stratigraphic unit with contentious age" Preferred age quoted.|450 Ma|||||
26079|Nine Mile Volcanics|60423|6|Mentioned|p380|||Shoshonitic.||||||
26079|Nine Mile Volcanics|60452|6|Mentioned|p53|||||||||
26079|Nine Mile Volcanics|63278|4|Described|p157|Gisbornian|Darriwilian |Of Kiandra Gp. Underlain by Temperance Volcanics. Geol Prov: Kiandra Volcanic Belt, LFB. Consists of volcaniclastic sandstone, siltstone and conglomerate. Age provided by graptolites resembles Gisbornian. Sills intrude the unit.||||||07-FEB-11
26079|Nine Mile Volcanics|63283|6|Mentioned|p206|Ordovician|Ordovician|||||||07-FEB-11
26079|Nine Mile Volcanics|63290|6|Mentioned|p394 Tb. 1, p398, p402 Fig. 6(b)|Ordovician|Ordovician|Geological Province: Kiandra Volcanic Belt. High metamorphic albite-actinolite-biotite grade rocks.||||||
26079|Nine Mile Volcanics|67322|4|Described|p26; Fig.5|Late Ordovician|Late Ordovician|Defined by Owen and Wyborn (1979). Contains late Gisbornian graptolites. Occurs in the Kiandra Volcanic Belt.||Of the Kiandra Group.||Overlies the Temperance Formation. Overlain by the Gooandra Volcanics.|Fine grained sequence with black shale and volcaniclastic laminations; rare limestone blocks.|22-FEB-18
72992|Nobbys Beach Lamprophyre|63763|3|Fully described|p8, p15|Permian|Permian|Emplaced in Port Macquarie Serpentinite, Karikeree Metadolerite and Watonga Formation; cut by Sea Acres Dolerite. Fine-grained, dark green lamprophyre in narrow dykes (more lith. detail included).||||||03-JUL-14
28870|Nobbys Coal|23055|6|Mentioned|p1,14,Fig11p23|||||||||
28870|Nobbys Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Lambton Formation.   Geological Province: Sydney Basin||||||
28870|Nobbys Coal|39292|6|Mentioned|Fig.6.6|||||||||
28870|Nobbys Coal|39308|5|Briefly described|p470|||See also P467||||||
28870|Nobbys Coal|39609|5|Briefly described|p4|||||||||
28870|Nobbys Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Nobbys coal seam instead. See also p113.||Of Lambton Subgroup||||
28870|Nobbys Coal|73304|6|Mentioned|p75|||||Lambton Formation, Newcastle Coal Measures||||
35126|Nobbys coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within Lambton Formation (Newcastle Coal Measures).||||||
35126|Nobbys coal seam|23055|6|Mentioned|p36|||||||||
35126|Nobbys coal seam|68711|5|Briefly described|p119, p116 Tbl 7|||Informal unit.||Within Lambton Formation||||
27863|Nombi Extrusives|29698|4|Described|p67|||||||||
27863|Nombi Extrusives|68003|5|Briefly described|p48. |||Identified by Bean (1974) but not mapped because of its local extent.||Unit in Garrawilla Volcanics.||||
23876|Nombiginni Volcanics|22857|4|Described|p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Mount Hope Group (Cobar Supergroup). Rhyolite and rhyodacite lavas, subordinate arenite. Max. thickness: 1.5km. Geological Province: Mount Hope Trough (Darling Basin). ||||||
23876|Nombiginni Volcanics|37772|4|Described|p7|||||||||
23876|Nombiginni Volcanics|40269|4|Described|p148|||||||||
23876|Nombiginni Volcanics|40913|6|Mentioned|Map legend|Pragian|Pragian|||||||
23876|Nombiginni Volcanics|41126|2|Defined|p46|early Lochkovian|early Lochkovian|||||||
23876|Nombiginni Volcanics|41821|6|Mentioned|p15|||Occurs in the Mount Allen sheet area||||||
23876|Nombiginni Volcanics|42144|6|Mentioned|Fig.3 P604|||||||||
23876|Nombiginni Volcanics|42521|5|Briefly described|Fig.3b P16|||||||||
23876|Nombiginni Volcanics|43089|5|Briefly described|Map Legend|||Of Mount Hope Group.||||||27-OCT-08
23876|Nombiginni Volcanics|61964|6|Mentioned|p80|||A-type. To the north of CARGELLIGO 1:250k sheet area on MT ALLEN 1:100k.||||||
23876|Nombiginni Volcanics|70751|6|Mentioned|p8, p10, p17, p19, p24, p28, p30, p38|Silurian|Silurian||419.1 +/- 3 Ma (SHRIMP, this study)|Mount Hope Group|||S-type rhyolitic volcanics.|
23876|Nombiginni Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Mount Hope Group.|||Plagioclase-phyric dacite and minor quartz-plagioclase phyric rhyolite lavas (A-type). Locally amygdular with micropoikilitic to spherulitic matrix, intercalated with subordinate arenite.|
23876|Nombiginni Volcanics|72908|6|Mentioned|p3, p14|Early Devonian|Late Silurian|Hosts the Mount Allen gold mine.||Mount Hope Group|||Includes fine-grained clastic and volcaniclastic rocks.|
38270|Nonnington Leucomonzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Fine- to medium-grained, equigranular, saccharoidal, biotite-poor leucomonzogranite (probably leucogranite phase of the Mackenzie Monzogranite).   An I-type granitoid.||||||20-DEC-04
38270|Nonnington Leucomonzogranite|23812|5|Briefly described|p19 Tb.2|Early Triassic|Early Triassic|Age:241Ma (Rb-Sr).||||||
38270|Nonnington Leucomonzogranite|68111|5|Briefly described|p969 Tb.1|Ladinian|Ladinian||ca. 240 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38270|Nonnington Leucomonzogranite|71628|3|Fully described|p15: 2-3, 15-16, 18-22, 25|||Henley et al. (2001) after Barnes (1987). Originally Nonnington Leucoadamellite (Shaw, 1969). Regarded as a marginal variant of the Mount Mackenzie Monzogranite. Occurs as three small bodies within Mount Mackenzie Monzogranite. The type area is on the Woodside loop road, 11 km SW of Tenterfield (Shaw, 1964). Weathers rapidly but has excellent outcrop. Geochemistry described. Contains only one (vein Sn) mineral deposit.|240.5 Ma (Rb-Sr biotite: Shaw, 1994).|Bolivia Range Suite.|||Fine- to medium-grained, equigranular saccharoidal to seriate, biotite leucomonzogranite. I-type.|
76142|Noonthorangee Formation|66623|1|Redefined|pp74-75, pp89-91.  |Middle Cambrian|Middle Cambrian|Redefined; formerly portion of Wonominta beds (Warris 1967), then Noonthorangee Subgroup (Buckley 2000). Unlike the former Noonthorangee Subgroup, it has no formal members, and intrusive and extrusive rocks are now included in Bittles Tank Volcanics. Three feldspathic air-fall tuffs have been dated. Thickness c. 2 km.|508.6 +/- 3.2 Ma to 512 +/- 3.1 Ma (Black, 2005).|Unit in Ponto Group.||Believed to overlie Grasmere Formation, although thrust faulting affects the boundary. Is overlain by Koonenberry Formation.|Meta-mudstone-phyllite, locally grading into metasiltstone or metasandstone; locally interbedded with felsic, laminated and cherty (airfall) tuff; some calcareous phyllites and quartz-magnetite rocks.|
76142|Noonthorangee Formation|67322|4|Described|p11, p39; Fig.5|Late Cambrian|Early Cambrian|Ages from SHRIMP U-Pb zircon analyses of three feldspathic tuff horizons in this Formation. Blue Rock Well Basalt, Blue Rock Well Phyllite, Blue Rock Well Sandstone, Blue Rock Formation and Gum Creek Basalt were previously part of the Noonthorangee Subgroup (obsolete)- now included in Noonthorangee Formation (Greenfield et al., 2010). Occurs in the Kayrunnera-Koonenberry region.|508.6 +/- 3.2; 511.7 +/-3.5; 512.0 +/- 3.1|Of the Ponto Group.||Overlies Grasmere Formation. Is overlain by Koonenberry Formation. Correlated with Cannela Formation.|Similar to the underlying Grasmere Formation (i.e. phyllites with feldspathic tuff horizons, mafic units) but lacking its strong magnetic character.|22-FEB-18
76142|Noonthorangee Formation|69961|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Ponto Group.|||Green to dark blue-grey metamudstone (phyllite), lesser metasandstone, minor felsic tuff and weakly magnetic foliated pale to dark green-grey tholeiitic metabasalt, some feldspar-phyric, with vesicular or pillow structures.|
76142|Noonthorangee Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|||Ponto Group|||Predominantly non-magnetic green to dark blue-grey metamudstone (phyllite), lesser metasandstone, minor felsic tuff and weakly magnetic foliated pale to dark green-grey tholeiitic metabasalt, some feldspar-phyric with vesicular or pillow structures.|
76142|Noonthorangee Formation|70651|5|Briefly described|Map Legend|Cambrian|Cambrian|3 unnamed sub-units: White to buff-brown, fine- to medium-grained metasandstone, massive to locally moderately deformed sandstone with local cross-bedding textures. Buff to yellow-brown, thin bands of very fine-grained massive to locally strongly banded/laminated, siliceous cherty tuff. Red-brown to black, very fine-grained, well-banded/laminated to locally massive quartz and magnetite rock.||Ponto Group|Includes 3 unnamed sub-units.||Predominantly non-magnetic green to dark blue-grey metamudstone (phyllite), lesser metasandstone, minor felsic tuff and weakly magnetic foliated pale to dark green-grey tholeiitic metabasalt, some feldspar-phyric with vesicular or pillow structures.|
76142|Noonthorangee Formation|70838|5|Briefly described|p269-272, p274, p276|Cambrian|Cambrian|Koonenberry Belt. Is sandwiched conformably between two tuff units dated at 512.0 +/- 3.1 Ma and 508.6 +/- 3.3 Ma. Detrital zircon analyses: most detrital zircons are in the range of 600-540 Ma or older; youngest population at 516 +/- 9 Ma.|c.510 Ma.|Ponto Group.||||
76142|Noonthorangee Formation|73177|5|Briefly described|p1113-1115 Figs.15-17, 1116 Tb.2|Cambrian|Cambrian||516 +/- 9 Ma.|Ponto Group.||||30-AUG-22
76142|Noonthorangee Formation|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
23878|Norholm Sandstone Member|22857|5|Briefly described|p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Boothumble Formation (Cobar Supergroup). Arenite. Max. thickness: 650m. Geological Province: Mouramba Shelf. ||||||
23878|Norholm Sandstone Member|41394|2|Defined|p75|Early Devonian||||||||
23878|Norholm Sandstone Member|41395|6|Mentioned|Map legend|Lochkovian||||||||
23878|Norholm Sandstone Member|61964|5|Briefly described|p64|||Of the Boothumble Formation. Subaerial alluvial fan sequence. Conformably overlain by Crossleys Tank Formation. On the KILPARNEY map sheet. ||||||
82615|North Britain Monzogranite|71628|6|Mentioned|p8:85|||Proposed as a replacement for Hell Hole Monzogranite, to avoid any confusion with Hell Hole Creek Monzogranite used in the Tantangara area.||||||
82511|North Brother Granodiorite|71628|4|Described|p17: 2, 78, 80, 83-86|||New name (this study) after unpublished work by Richardson (2013). Named after North Brother Mountain, immediately W of Laurieton. Commonly deeply weathered and closely jointed. Inexplicably called North Brother Monzogranite on p.80. Lithology described in detail. Geochemistry described.|212.4 +/- 4.4 Ma (SHRIMP: Richardson et al., 2006)|The Brothers Suite.||Intrudes Camden Haven Group, Mingaletta Formation, Beechwood beds and Walibree Formation.|Fine- to medium-grained, porphyritic two-pyroxene-amphibole microgranite to granodiorite. A-type.|
28874|North Mooney Complex|22638|1|Redefined|p37|Ludlow|Llandovery|426 +/- 6 Ma Potassium-argon date. Age could have been reset by deformation.||||||
28874|North Mooney Complex|22687|6|Mentioned|111 fig 2,119|||Geol province Lachlan Fold Belt||||||
28874|North Mooney Complex|22768|6|Mentioned|p174,184||Llandovery|Max Age: 426 (+/-) 6 Ma||||||
28874|North Mooney Complex|22857|5|Briefly described|p174, p183|Late Silurian|Early Silurian|Age: 426+/-6Ma (K/Ar hornblende, Basden, 1982).||||||
28874|North Mooney Complex|23454|5|Briefly described|p32|Ordovician|Ordovician|426+/-6Ma||||||
28874|North Mooney Complex|29453|6|Mentioned|p26|||||||||
28874|North Mooney Complex|29682|4|Described|p12|||||||||
28874|North Mooney Complex|30172|6|Mentioned|Fig.19|||||||||
28874|North Mooney Complex|35070|2|Defined|p40|Early Silurian|Early Silurian|Prob.Early Silurian||||||
28874|North Mooney Complex|35185|6|Mentioned|p230|||||||||
28874|North Mooney Complex|35194|6|Mentioned|p67|||||||||
28874|North Mooney Complex|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28874|North Mooney Complex|35522|5|Briefly described|p45|||||||||
28874|North Mooney Complex|35608|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
28874|North Mooney Complex|35609|5|Briefly described|p15|||||||||
28874|North Mooney Complex|36051|5|Briefly described|p411|||||||||
28874|North Mooney Complex|36411|6|Mentioned|p269|||Refers Basden et al 1978 for definition.||||||
28874|North Mooney Complex|40328|6|Mentioned|Fig.12(E1)|||||||||
28874|North Mooney Complex|41798|5|Briefly described|p5|||||||||
28874|North Mooney Complex|42145|4|Described|Table 1 P624|||||||||
28874|North Mooney Complex|42313|6|Mentioned|p78|||||||||
28874|North Mooney Complex|42828|4|Described|p130|||||||||
28874|North Mooney Complex|44192|5|Briefly described|Map Legend||Llandoverian|||||||
28874|North Mooney Complex|44936|5|Briefly described|Map Legend||Silurian|||||||
28874|North Mooney Complex|50191|6|Mentioned|p6, 21 Fig. 1|Silurian|Early Silurian|||||||
28874|North Mooney Complex|69043|4|Described|p2, p5-6, p63-68, p118|Ludlow|Wenlock|Tumut Trough, eastern Lachlan Orogen. The origin of this unit is controversial: several models outlined. This age determination agrees with previous K-Ar hornblende ages of 426 +/- 6 Ma and 425 +/- 6 Ma (Webb, 1980).|426.8 +/- 2.2 Ma (magmatic crystallisation age).||||Mafic-ultramafic rocks including diorite and pegmatitic gabbro.|19-JAN-17
28874|North Mooney Complex|71040|5|Briefly described|p8 Fig.5, p10|||Tumut Trough.|427 +/- 2 Ma (Bodorkos et al., 2013).|Coolac Ophiolite Suite.||||
28874|North Mooney Complex|71708|4|Described|p335-338, p340,342-344,348, p351-352|Ludlow|Ludlow|SHRIMP zircon dating on gabbros supports previous K-Ar ages of 426 +/- 6 Ma and 425 +/- 6 Ma. Provides Min age for Coolac Serpentinite. These rocks have MORB-arc tholeitte compositions.|426.8+/-2.2 U-Pb SHRIMP magmatic crystallisation|||Intrudes Coolac Serpentinite. Sits adjacent to, and intrudes the Honeysuckle beds.|Includes pyroxenite, wehrlite, pegmatite gabbro, basalt.|31-MAR-20
28874|North Mooney Complex|73215|5|Briefly described|p994|||Tumut Trough.|427 +/- 3 Ma (Bodorkos et al., 2013).|||Intrudes Blowering Formation.||
28874|North Mooney Complex|73483|5|Briefly described|p407, p409, p416|Silurian|Silurian|Intrudes the Coolac Serpentinite Belt. K-Ar hornblende ages of 425+/-6 Ma and 426+/-6 Ma from gabbros (Webb, 1980), U-Pb SHRIMP age of 427+/-2 Ma on pegmatitic zircons (Bodorkos et al., 2013).|427+/-2 Ma U-Pb zircon, 425+/-6 Ma K-Ar hornblende||||Includes gabbro.|
29253|North Peak porphyry|34449|6|Mentioned|p128|||||||||
80169|North Stockton Sandbeds|68811|6|Mentioned|p62,63,  p126 tbl 13, p167 tbl 25|Holocene|Holocene|||||||14-APR-20
22567|Northam Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
23880|Northcotte Formation|22750|5|Briefly described|p 228||Early Devonian|Tamworth Group||||||
23880|Northcotte Formation|23185|6|Mentioned|Fig5p161|Emsian|Emsian|||||||
23880|Northcotte Formation|23522|5|Briefly described|p249 Fig 5|Emsian|Emsian|||||||
23880|Northcotte Formation|38686|5|Briefly described|Table 1|||||||||
23880|Northcotte Formation|41347|6|Mentioned|p162|||||||||
23880|Northcotte Formation|41348|5|Briefly described|Map legend|Devonian|Devonian|Of the Tamworth Group.||||||16-DEC-04
23880|Northcotte Formation|47056|6|Mentioned|Fig.2 P523|||||||||
23880|Northcotte Formation|50168|6|Mentioned|p157 Fig.2|||Gamilaroi Terrane.||||||
23880|Northcotte Formation|61392|5|Briefly described|p165 Fig. 2|Emsian|Emsian|In the Gamilaroi terrane.||||||07-FEB-11
23880|Northcotte Formation|65214|6|Mentioned|p275|Devonian|Devonian|NSW, Nundle. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23880|Northcotte Formation|68005|4|Described|p49 Fig.3-M, p50, p151, p170.|Emsian|Pragian|Tamworth Belt. Equivalent to part of Bog Hole Formation, which is oddly shown as a member on p151.||Unit in Tamworth Group.|Includes Nemingha Limestone and Northcotte Limestone Member.|Overlies Drik-Drik Formation. Is overlain by Wogarda Argillite.|Green sandstone and siltstone, tuff, minor argillite; rare limestone.|
23880|Northcotte Formation|73440|6|Mentioned|p132|||||||||
28875|Northern Limestone|41863|6|Mentioned|p19|||||||||
35020|Northparkes Volcanic Group|24233|5|Briefly described|p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
35020|Northparkes Volcanic Group|24417|2|Defined|p19|Middle Ordovician|Middle Ordovician|New group.||||||
35020|Northparkes Volcanic Group|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||13-JUL-04
35020|Northparkes Volcanic Group|60308|6|Mentioned|p38|Late Ordovician|Late Ordovician|"Important stratigraphic unit with contentious age" Preferred age quoted.|445 Ma|||||
35020|Northparkes Volcanic Group|63278|6|Mentioned|p150|||Established by Percival (2000).||||||07-FEB-11
35020|Northparkes Volcanic Group|63289|6|Mentioned|p372|||||||||07-FEB-11
35020|Northparkes Volcanic Group|63291|6|Mentioned|p421|||Previous name for Northparkes Group.||||||28-SEP-07
35020|Northparkes Volcanic Group|67322|6|Mentioned|p22|||Of Percival, in Lyons et al. (2000). Renamed Northparkes Group.||||||
35020|Northparkes Volcanic Group|72495|5|Briefly described|p222|Ordovician|Ordovician|Originally introduced by Percival (2000), the authors of the present study substitute it with the Northparkes Group.||||||30-MAR-20
26082|Nowranie Creek Formation|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Coorabin Coal Measures. Coarse sandstone, siltstone, carbonaceous shale. Max. thickness: 7m. Geological Province: Ovens Graben.||||||
26082|Nowranie Creek Formation|35498|2|Defined|p145|Late Permian|Late Permian|||||||
26082|Nowranie Creek Formation|35503|6|Mentioned|p202|||Defined in Standing Committee Coalfield Geology NSW (1978)||||||
26082|Nowranie Creek Formation|38293|6|Mentioned|p20|||||||||
26082|Nowranie Creek Formation|42966|4|Described|p64|||of Coorabin Coal Measures||||||
26082|Nowranie Creek Formation|69798|5|Briefly described|p4 Fig.2|Permian|Permian|Oaklands Basin. Fluvial-point bar and lacustrine depositional environment.||Coorabin Coal Measures.||||06-FEB-18
24434|Noyeau Hollow Andesite|39655|4|Described|M4|||||||||
24434|Noyeau Hollow Andesite|39663|6|Mentioned|Table 2|||||||||
31299|Nubingerie Formation|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Gregra Group.  Sandstone, shale, siltstone, tuffaceous sediment, rhyolite, ash tuff.||||||
33380|Nubrigyn Member|22768|6|Mentioned|p179|||||||||
33380|Nubrigyn Member|22857|5|Briefly described|p179, p470 App.1 Tb.A1.6|Pragian|Lochkovian|Of the Cunningham Formation. Composed of arenites, rudites and olistostromes with olistoliths up to 1km in length. Max. thickness: 400m. Geological Province: Hill End Trough.||||||
33380|Nubrigyn Member|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Cunningham Formation.||||||
33380|Nubrigyn Member|23170|2|Defined|p185|Emsian|Lochkovian|of Cunningham Formation.||||||
33380|Nubrigyn Member|50095|5|Briefly described|p150|Pragian; Kindlei Zone (conodont)|Pragian; Sulcatus Zone (conodont)|Of Cunningham Formation. Contains Pandorinellina exigua exigua (conodont).||||||11-FEB-08
41602|Nuchea Conglomerate|50618|5|Briefly described|p249 Fig. 2|Early Ordovician|Early Ordovician|Of the Mootwingee Group.||||||
41602|Nuchea Conglomerate|64679|5|Briefly described|Map legend|Ordovician|Late Cambrian|Of the Mutawintji Group. Polished pebble to cobble quartzite conglomerate interbedded with red coarse-grained lithic sandstone.||||||27-NOV-08
41602|Nuchea Conglomerate|66623|2|Defined|p58, p122, pp135-143. |Late Cambrian|Late Cambrian|Formerly part of Torrowangee Series (Mawson 1912), Mootwingee Series (Andrews 1922) redefined by Kenny (1934); included by name in Nootumbulla Sandstone by Sharp (2004); defined in this study. Clasts derived from distant sources to the west, possibly Willyama Complex rocks of the Curnamona Craton. Possibly correlates with Williams Creek Conglomerate (Kayrunnera Group) and Owen Conglomerate in Tasmania. From 50 to 110 m thick. Poorly cemented: outcrops usually as pebble scree.||Unit in Mutawintji Group.||Unconformably or disconformably overlies Gnalta Group basement. Locally overlies Bilpa Conglomerate. Is overlain by Scropes Range Formation and Nootumbulla Sandstone.|Medium- to coarse-grained conglomerate with highly polished and very well-rounded blue-grey, strongly recrystallised quartzite pebbles, cobbles and boulders to 60 cm diameter; minor interbedded red quartzose pebbly sandstone lenses.|25-SEP-13
41602|Nuchea Conglomerate|66918|5|Briefly described|Map legend|||||Unit in Mutawintji Group.||Is overlain by Scropes Range Formation.|Conglomerate with highly polished and rounded blue-grey quartzite pebbles and boulders; regionally metamorphosed to prehnite-pumpellyite facies.|
41602|Nuchea Conglomerate|67322|4|Described|p8, p12; Fig.5|Stage 9||First distinguished by Sharp (2004); defined by Greenfield and Percival, in Greenfield et al. (2010). Thickness is approximately 50-109 m. Age determined from p20 Fig.5 (Strat. column). Occurs in the Mount Wright-Mutawintji region; also in Scropes Range.||Basal unit of the Mutawintji Group.||Conformably overlies Bilpa Conglomerate. Overlain conformably by the Nootumbulla Sandstone or Scropes Range Formation.|Clast-supported monomict conglomerate of fluvial origin with well-polished and highly-rounded blue-grey orthoquartzite and metaquartzite pebbles, cobbles, and boulders.|22-FEB-18
41602|Nuchea Conglomerate|70650|5|Briefly described|Map Legend|Ordovician|Cambrian|||Mutawintji Group|||Conglomerate with highly polished and rounded blue-grey quartzite pebbles and boulders.
|
77137|Nullawa Member|68069|5|Briefly described|Map legend.|Quaternary|Quaternary|Has three facies mapped separately: channel, crevasse splay and backplain.||Unit in Bugwah Formation.|||Unconsolidated red-brown, beige and grey sand, silt, silty clay and clay; carbonate nodules.|
77137|Nullawa Member|68593|4|Described|p1-3, p13, p15-17, p45, p48, p83|Pleistocene|Pleistocene|Newly named unit. Composed of the same constituents as Bugwah Formation but has different geomorphological features: expressed as a dendritic, medial to distal fluvial distributary system. Channel, splay and backplain facies described in some detail. Age based on a single thermoluminescence dating by Price (2003); conflicts with age of parent unit. Probably remobilised by aeolian processes. Sand and loam are extracted from the Heathfield pit.|2.6 +/- 0.15 ka (Burton, 2011).|Basal Bugwah Formation.|||Unconsolidated Quaternary alluvium surrounding silcrete-capped ridges.|
73515|Nullawonga Latite Member|63278|6|Mentioned|p145 Fig. 1, p147 Fig. 2b|Bolindian|Bolindian|Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
73515|Nullawonga Latite Member|63283|6|Mentioned|p195 Fig. 2, p202|Bolindian|Bolindian|Of the Forest Reeefs Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
73515|Nullawonga Latite Member|63285|6|Mentioned|p281|||Geological Province: Molong Volcanic Belt. Unit is a ring-dyke complex.||||||
73515|Nullawonga Latite Member|63286|4|Described|p298, p294 Fig. 1, p302, p308 Fig. 9|Lalandovery|Llandovery|Of the Forest Reefs Volcanics .Age: 443Ma, age of emplacement. Consists of latitic lava, breccia and ignimbrite. See also p298 for more petrologiacl information.||||||07-FEB-11
73515|Nullawonga Latite Member|67106|6|Mentioned|p679|||Molong Volcanic Belt.||Forest Reefs Volcanics.||||
73515|Nullawonga Latite Member|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3). Shown as Nullawonga Latite Mbr.||Forest Reefs Volcanics||||
30855|Nulling Member|22529|5|Briefly described|p6|||Parent Piambong Formation||||||
30855|Nulling Member|22857|4|Described|p470 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Piambong Formation (Chelsleigh Group). Rhyodacite-dacite flows, volcanic arenite, quartz-rich conglomerate. Geological Province: Hill End Trough. ||||||
30855|Nulling Member|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Chesleigh Group.||||||
30855|Nulling Member|23170|5|Briefly described|p75|||of Piambong Formation. Supercedes 'Nulling Formation'.||||||
76963|Numbla Vale Monzogranite|72571|5|Briefly described|p90, p92, p96-98, p100|||Of the Tasmanides of eastern Australia. Petrography of sample and zircon description and analyses are discussed in detail. S-type.|||||Biotite and cordierite granites with magnetiyte and ilmenite.|
33831|Numeralla Chert Member|22545|6|Mentioned|p504||Darriwilian|||||||
33831|Numeralla Chert Member|73140|5|Briefly described|p495 Fig.1, Fig.3|Darriwilian|Darriwilian|Age based on conodonts.||Abercrombie Formation||Underlies Sunlight Creek Formation||
29562|Nundle Suite|38822|5|Briefly described|p193, 194|Permian|Permian|Geological Province: New England Fold Belt. Age: 264-273Ma||||||
29562|Nundle Suite|42984|5|Briefly described|p365|||||||||
29562|Nundle Suite|68005|5|Briefly described|p63, p135.|Early Permian|Early Permian|Felsic intrusives.||Unit in Clarence River Supersuite.|Includes Barrington Tops, Mount Ephraim and Rockisle Granodiorites and Duncans Creek Trondhjemite.||Porphyries, granitoids, leucocratic sills and dykes.|
29562|Nundle Suite|68006|6|Mentioned|p135.|||Equivalent to Clarence River Supersuite.||||||
29562|Nundle Suite|69601|5|Briefly described|p403-404, p408-409|||New England Orogen. Defined by Hensel et al. (1982) as a suite of low-K granites spatially associated with the Peel Fault system.|281 Ma; 273 Ma.||Barrington Tops Granodiorite, Mount Ephraim Granite.||I-type granites.|
29562|Nundle Suite|70217|5|Briefly described|p11, p17, p22|||New England Orogen. ||Clarence River Supersuite|Includes the Barrington Tops Granodiorite.|||
29562|Nundle Suite|71628|5|Briefly described|p1:5; p3: 2, 77; p6: 1, 6, 16; p9:1|||See also p18: 1, 4, 8, 18, 21; p19-152. Hensel et al. (1985). This study lists (p9-1) Mount Ephraim, Gogs Top, Duncans Creek, Linden Hill, Barrington Tops and Rockisle as original constituents, but unhelpfully omits every lithology.|||See Comments.||Low-K granitoids.|
25356|Nundooka Sandstone|22518|5|Briefly described|Table 1, p 6||Late Devonian|Mulga Downs Group||||||
25356|Nundooka Sandstone|22553|5|Briefly described|p78|Devonian|Devonian|||||||
25356|Nundooka Sandstone|22730|4|Described|p557-9, 563,66|Famennian|Frasnian|contains 6 informal units...||||||
25356|Nundooka Sandstone|22857|4|Described|p210, p486 App.1 Tb.A1.7|Famennian|Frasnian|Arenite. Max. thickness: >1425m. Geological Province: Ravendale Basin.||||||
25356|Nundooka Sandstone|22859|5|Briefly described|p210|||||||||
25356|Nundooka Sandstone|23336|4|Described|p15, p18 Fig. 15|Famennian|Frasnian|Of the Mulga Downs Group. Subdivided into the Lower Friable Arenite, Lower Light-Grey Arenite, Quartzose Arenite, Central Light-grey Arenite, Marker Bed and Upper Light-Grey Arenite - together these attain a max. thickness of 1800m. See also p26.||||||21-MAR-06
25356|Nundooka Sandstone|23380|5|Briefly described|p109|Late Devonian|Middle Devonian|Equivalent to Ravendale Formation and upper Mulga Downs Group. Age: Givetian - Famennian. of Wonaminta Block.||||||
25356|Nundooka Sandstone|23833|5|Briefly described|p256 Table 1|Carboniferous|Devonian|||||||
25356|Nundooka Sandstone|29991|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25356|Nundooka Sandstone|30683|6|Mentioned|Table 1|||||||||
25356|Nundooka Sandstone|30908|6|Mentioned|Map legend|Carboniferous|Late Devonian|Carboniferous - Upper Devonian||||||
25356|Nundooka Sandstone|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25356|Nundooka Sandstone|32672|6|Mentioned|p674|||||||||
25356|Nundooka Sandstone|33004|6|Mentioned|Fig.8|||||||||
25356|Nundooka Sandstone|33732|6|Mentioned|p103|||||||||
25356|Nundooka Sandstone|34469|6|Mentioned|p107|||Devonian. P116||||||
25356|Nundooka Sandstone|34563|4|Described|p69|||Nundooka sandstone-Stratigraphy p62||||||
25356|Nundooka Sandstone|34812|3|Fully described|p141|||||||||
25356|Nundooka Sandstone|35199|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25356|Nundooka Sandstone|43263|6|Mentioned|Map Legend|Early Carboniferous|Late Devonian|||||||
25356|Nundooka Sandstone|43501|14|Not recorded|Map Legend|Carboniferous|Devonian|(Provisional Edition)||||||
25356|Nundooka Sandstone|43502|14|Not recorded|Map Legend|Carboniferous|Late Devonian|(Provisional Edition)||||||
25356|Nundooka Sandstone|44093|5|Briefly described|p140 App. 1|Early Carboniferous|Middle Devonian|Overlies Coco Range Sandstone. Geological Province: Kanmantoo Fold Belt: Bancannia Zone: Bancannia Block.||||||
25356|Nundooka Sandstone|46889|6|Mentioned|Table1|||||||||
25356|Nundooka Sandstone|47026|6|Mentioned|Fig.5|||||||||
25356|Nundooka Sandstone|60648|4|Described|p43|Famennian|Frasnian|Of the Mulga Downs Group. Contains a Marker Bed of quartzose fine arenite, and successions of light brown fine-grained arenite 2-5m thick.  May overlie Coco Range Sandstone. Max. thickness: 1420m at type section.  Geological Province: Darling Basin.||||||28-APR-05
25356|Nundooka Sandstone|61311|6|Mentioned|p51|||Geological Province: Darling Basin.||||||
25356|Nundooka Sandstone|63632|6|Mentioned|p658|||Geological Province: western Darling Basin. Alluvial fan deposits.||||||16-OCT-07
25356|Nundooka Sandstone|64967|5|Briefly described|p114 Fig. 2|Famennian|Frasnian|Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). See also p115 Fig. 3.||||||
25356|Nundooka Sandstone|65759|5|Briefly described|p114 Fig.2, p131|Famennian|Givetian|1070m thick, part of Mulga Downs Group, uncomformably overlies Coco Range Beds, fluvial. Includes Marker Bed Unit.||||||
25356|Nundooka Sandstone|66589|6|Mentioned|p180|Famennian|Frasnian|Case studies cited; not visited in the field by the authors of this study.||||||
25356|Nundooka Sandstone|66623|6|Mentioned|p216.|||Correlated with Ravendale Formation on western margin of Bancannia Trough.||||||
25356|Nundooka Sandstone|67562|6|Mentioned|p97 Fig.4, p102 Fig.8, p103, p109, p115|Tournaisian||Appears as Nundooka Formation in Fig.8. > 1425m thick (base and top are unexposed).|||||Comprises six east-dipping sublitharenite-rich units.|23-JAN-17
25356|Nundooka Sandstone|70000|5|Briefly described|p40|Devonian|Devonian|Darling Basin, N and W Broken Hill Province. Weakly folded during the c.320 Ma Kanimblan Orogeny.||Unit in Mulga Downs Group.|||Fluvial sedimentary rocks.|
37338|Nundora Formation|66623|2|Defined|pp39-40, p17, p34. |Middle Cambrian|Early Cambrian|This unit is defined in this publication. Formerly part of Packsaddle Series (Andrews 1922), Wonominta Beds (Warris 1967), Complex (Scheibner 1972) and beds (McIntyre & Wyatt 1978), Teltawongee beds (Mills 1992). Exposed over 25 km2. Over 2.5 km thick.|Maximum from detrital zircons: 652 Ma|Unit in Teltawongee Group.||Overlies Kara Formation (Grey Range Group) with gradational conformable contact.  Is unconformably overlain by Namur Sandstone.|Maroon, turbiditic silty and muddy, massive sandstones; graded bedded; erosional basal contact with rip-up clasts, coarse-grained basal sand, detrital muscovite to 3 mm. Unfossiliferous. Shows climbing ripples, laminations and rare muddy tops|03-OCT-13
37338|Nundora Formation|67105|5|Briefly described|p655|Cambrian|Cambrian|Occurs W of the Koonenberry Fault. Contains detrital zircons likely derived from the Curnamona Province.||Teltawongee Group.||Locally overlies  (probably disconformably) the Kara Formation.|Includes a sequence of steeply-dipping laminated slate and graded sandstone beds.|
37338|Nundora Formation|67322|5|Briefly described|p10; Fig.5|Cambrian|Cambrian|Defined by Mills in Greenfield et al., (2010). Age determined from p20 Fig.5 (Strat. column) - not well constrained. Occurs in the Kayrunnera-Koonenberry region.||Of the Teltawongee Group.||||22-FEB-18
37338|Nundora Formation|68731|6|Mentioned|p212|Early Cambrian|Early Cambrian|Early Cambrian(?) age. A detrital zircon age pattern with a major peak at 1178 +/- 17 Ma has been found from a sample of this Formation.||Of the Teltawongee Group.||||17-JUL-14
37338|Nundora Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|||Teltawongee Group|||Maroon, turbiditic silty and muddy, massive sandstone, 20cm to 3m thick; erosional basal contact with rare rip-up clasts, slightly coarser basal sand, common detrital muscovite to 3mm; climbing ripples and laminations in upper parts of many units.|
37338|Nundora Formation|70749|5|Briefly described|p52-53|||Koonenberry Belt. Deposited during the Petermann Orogeny. Contains abundant 1300-900 Ma aged detrital zircons sourced from the Musgrave Province. Multiply deformed.||||||
37338|Nundora Formation|70838|5|Briefly described|p268-270, p272, p277|Cambrian|Cambrian|SE Koonenberry Belt. Appears as Nundorra Fm. on p270.||Teltawongee Group.||Overlies Kara Formation conformably.|Characterised by repetitive sequences of immature sandstone (up to 3m thick locally) overlain by an upward-fining sequence (locally absent) of fine sandstone, siltstone and mudstone. Ubiquitous large (<5mm) detrital white mica grains.|
37338|Nundora Formation|73059|6|Mentioned|p1061|||Detrital zircon ages mentioned.||Teltawongee Group.||||
26814|Nunduro Conglomerate|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
26814|Nunduro Conglomerate|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Teamsters Creek Subgroup (Torrowangee Group). Siltstone with pebbles, cobbles, blocks, boulders (olistoliths). Age: ~593+/-32Ma. Max. thickness: 70m. Geological Province: Adelaide Fold Belt. See also p400 App. 1 Tb.A1.3.||||||10-MAR-06
26814|Nunduro Conglomerate|30261|4|Described|Table 1|||Marinoan age||||||
26814|Nunduro Conglomerate|34812|3|Fully described|p95|||||||||
26814|Nunduro Conglomerate|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26814|Nunduro Conglomerate|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
26814|Nunduro Conglomerate|36733|6|Mentioned|Table 5|||||||||
26814|Nunduro Conglomerate|37931|4|Described|p533|||||||||
26814|Nunduro Conglomerate|38157|6|Mentioned|p265|||||||||
26814|Nunduro Conglomerate|39214|5|Briefly described|p9|||||||||
26814|Nunduro Conglomerate|41405|5|Briefly described|p205|||||||||
26814|Nunduro Conglomerate|68241|6|Mentioned|p21, p24 Fig.3, p32, p33 Fig.3|||||||Underlain by the Dering Siltstone. Equivalent to the Cottons Breccia.|Breccia.|
26814|Nunduro Conglomerate|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Teamsters Creek Subgroup.||||
26814|Nunduro Conglomerate|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Teamsters Creek Subgroup.||Overlies Dering Siltstone. Is overlain unconformably by Mantappa Dolomite.|Quartzite clast-dominated conglomerate with a pebbly silty matrix; some slumping and rare large clasts (up to 20 m).|
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.||||||
78460|Nurri Group and possible equivalents 78460|69042|5|Briefly described|map legends|Early Devonian|Late Silurian|Dcn. Belt of linear trends of low to moderate magnetic intensity. Sediments and tuff of the Nurri Group and possible equivalents.||||||
76036|Nyangay granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Baconian Swamp Granite Suite.|||Interpreted S-type granites.|
76036|Nyangay granite|70718|4|Described|p75, p127|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics. Age derived from cross cutting relationship of the Oolambeyan and Eurolie granites. Also misspelt as the Nyangan granite on p127.||Baconian Swamp granite suite|||S-type granitic rocks.|31-MAY-19
26087|Nymagee Igneous Complex|730|6|Mentioned|p16.|||Intrudes Girilambone Group.||||||11-NOV-14
26087|Nymagee Igneous Complex|23053|6|Mentioned|p19|||||||||
26087|Nymagee Igneous Complex|23171|5|Briefly described|p12,18||Silurian|Max Age: 440 Ma.||||||
26087|Nymagee Igneous Complex|23173|4|Described|Map Legend|||||||||
26087|Nymagee Igneous Complex|35287|4|Described|p3|||See also p2.||||||20-SEP-19
26087|Nymagee Igneous Complex|39083|6|Mentioned|p30|||||||||
26087|Nymagee Igneous Complex|39214|4|Described|p14|||||||||
26087|Nymagee Igneous Complex|39618|2|Defined|p30|Middle Silurian|Middle Ordovician|Middle Ordovician - Middle Silurian||||||
26087|Nymagee Igneous Complex|39627|4|Described|p263|||||||||
26087|Nymagee Igneous Complex|40624|6|Mentioned|Map legend|Early Silurian|Early Ordovician|Ordovician to Silurian||||||
26087|Nymagee Igneous Complex|40677|5|Briefly described|p24|||||||||
26087|Nymagee Igneous Complex|41394|6|Mentioned|p9|||||||||
26087|Nymagee Igneous Complex|41528|2|Defined|p26|Middle Silurian|Early Silurian|||||||
26087|Nymagee Igneous Complex|41529|6|Mentioned|Map legend|Middle Silurian||||||||
26087|Nymagee Igneous Complex|41821|6|Mentioned|p11 Fig.5|||Occurs in Nymagee and Canbelego sheet areas||||||
26087|Nymagee Igneous Complex|42566|5|Briefly described|p44|||||||||
26087|Nymagee Igneous Complex|43032|5|Briefly described|p23|||||||||
26087|Nymagee Igneous Complex|43089|5|Briefly described|Map Legend|||||||||
26087|Nymagee Igneous Complex|43757|5|Briefly described|p510|||Rb-Sr age: 440 Ma||||||
26087|Nymagee Igneous Complex|46900|6|Mentioned|p15|||||||||
26087|Nymagee Igneous Complex|50553|5|Briefly described|p1337|||Contains granite in which jointing is described.||||||
26087|Nymagee Igneous Complex|63290|6|Mentioned|p399|Early Silurian|Early Silurian|Age: ca 440Ma (Pogson and Hilyard, 1981) poorly dated.||||||
26087|Nymagee Igneous Complex|65469|6|Mentioned|p15-p17|Middle Silurian|Early Silurian|Lachlan Orogen.|||Includes the Erimeran Granite,|Unconformably overlain by the Kopyje Group.||
26087|Nymagee Igneous Complex|67416|6|Mentioned|p85-86||||~425 Ma.|||||
26087|Nymagee Igneous Complex|69801|6|Mentioned|p1, p18, p135-136|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Probably emplaced contemporaneous with the Urambie Granodiorite. Indistinguishable in age from the Koetong Supersuite granites on CARGELLIGO.|c. 427-423 Ma (Chisholm et al., 2014)||Includes the Erimeran Granite.|||
26087|Nymagee Igneous Complex|70751|5|Briefly described|p8-p10, p12, p27, p38|Silurian|Silurian|A SHRIMP date of 428.1 +/- 4.3 Ma is derived from this study.|c. 425 Ma (Isaacs, 2000)|||||
26087|Nymagee Igneous Complex|70941|6|Mentioned|p9|||||||||
26087|Nymagee Igneous Complex|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped S-type intrusion.|||||Massive, porphyritic, biotite-muscovite granite and muscovite-biotite monzogranite; lesser massive equigranular muscovite-biotite monzogranite. Strongly foliated, coarse, biotite-muscovite granite and monzogranite.|
26087|Nymagee Igneous Complex|72958|6|Mentioned|p11|Wenlock|Wenlock|Basement to Cobar Basin||||||
78521|Nymboi Granite|68111|5|Briefly described|p969 Tb.1, p969, p970-p973, p976|Ladinian|Anisian|New name. Dating detailed. Included in group of units described as consisting of biotite, quartz, feldspar and minor hornblende. Sample NE1072 discussed.|221.3 +/- 2.2 Ma, U-Pb SHRIMP (Li et al. 2012).|||||21-OCT-14
78521|Nymboi Granite|71628|5|Briefly described|p17:65|||Li et al. (2012) for an intrusion initially named Kellys Creek Leucoadamellite (Korsch, 1978). This latter name has precedence; the unit is now named Kellys Creek Leucomonzogranite.|221.3 +/- 2.2 Ma (SHRIMP: Li et al., 2012).|||||
40931|O'Briens Creek Sandstone Member|22857|4|Described|p460 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Yass Formation. Cross-stratified sandstone, mudstone. Max. thickness: 130m. Geological Province: Canberra-Yass Shelf. ||||||
40931|O'Briens Creek Sandstone Member|50230|4|Described|Map legend|Wenlock|Wenlock|Of the Yass Formation (Douro Group).  Interbedded with the Clifton Limestone Member within the Yass Formation.  Overlies the Hawkins Volcanics.||||||10-MAY-04
40931|O'Briens Creek Sandstone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yass Formation (Douro Gp). Brown-beige to off-white, v. coarse- to med.-grained quartzofeldspathic sandstone, poorly sorted, sub-rounded to angular grains. Sparsely fossiliferous (brachiopods, gastropods, crinoid stems).||||||
40931|O'Briens Creek Sandstone Member|68592|2|Defined|p433-5,p440,p480,p497-501,p503-10,p521|Early Silurian|Early Silurian|See also p428, p430 Fig.89. Formerly O'Briens Creek Sandstone of Link (1970, 1971); Link and Druce (1972), a Formation in their Yass Group. Subsequently, Owen and Wyborn (1979) reduced it to Member status in their similarly-downgraded Yass Formation. Type section described. Up to 500m thick. Fluvial to nearshore shallow marine. Sparse fauna: brachiopods, gastropods, ostracods, bivalves and trilobites.||Unit in Yass Formation.||Overlies Hawkins Volcanics. Is overlain gradationally by Cliftonwood Limestone Member or Laidlaw Volcanics. Correlated with Wyelba Member (Glen Bower Formation).|Upward-coarsening sequence of medium- to coarse-grained, quartzose and quartzo-feldspathic sandstone and mudstone; cross-bedding, ripple marks, mud cracks and rain prints present.|
40931|O'Briens Creek Sandstone Member|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdyo. On Yass 1:100 000 mapsheet portion of Time-Space Plot.||Yass Formation|||Fine-very coarse grained, poorly sorted, quartz-quartzofelspathic to lithic sandstones with subrounded to angular grained; sparsely fossiliferous; sporadic subcrop of laminated siltstone-thinly laminated mudstone are stratigraphically down sequence.|
40931|O'Briens Creek Sandstone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|Sparsely fossiliferous: brachiopods, gastropods, crinoid stems.||Yass Formation|||Fine-very coarse grained, poorly sorted, quartz-quartzofelspathic to lithic sandstones with subrounded to angular grained; sparsely fossiliferous; sporadic subcrop of laminated siltstone-thinly laminated mudstone are stratigraphically down sequence.|25-AUG-16
40931|O'Briens Creek Sandstone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yass Formation|||Fine-very coarse grained, poorly sorted, quartz-quartzofeldspathic to lithic sandstones with subrounded to angular grains; sparsely fossiliferous. Sporadic subcrop of laminated siltstone-thinly laminated mudstone are stratigraphically down sequence.|
23882|O'Briens Monchiquite|36220|4|Described|p96|||||||||
23882|O'Briens Monchiquite|42896|5|Briefly described|p55|||||||||
28886|Oakley Limestone Member|23214|3|Fully described|p37|Late Ordovician|Late Ordovician|Of Daylesford Limestone. Not present of Daylesford Limestone type section. For lithology description see Semeniuk (1973a,b).||||||
28886|Oakley Limestone Member|33063|2|Defined|p80|Ordovician|Ordovician|See also P81. Mb. Daylesford Lst.||||||
28886|Oakley Limestone Member|33064|4|Described|p450|||Stratigraphy P454. Strat.column P453.||||||
28886|Oakley Limestone Member|33065|6|Mentioned|Table 1|||Lithology||||||
28886|Oakley Limestone Member|38219|6|Mentioned|Table 2|||||||||
28886|Oakley Limestone Member|42479|5|Briefly described|p111|||||||||
28886|Oakley Limestone Member|70684|5|Briefly described|p39 Fig.17|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Daylesford Limestone.||||
38276|Oban River Leucomonzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Coarse- to very coarse-grained, leucocratic, equigranular, biotite monzogranite, phases of fine- to very fine-grained saccharoidal, pink, equigranular microleucogranite.  An I-type granitoid.||||||20-DEC-04
38276|Oban River Leucomonzogranite|23812|5|Briefly described|p14|Early Triassic|Late Permian|Age: 248Ma (Rb-Sr).||||||
38276|Oban River Leucomonzogranite|68111|5|Briefly described|p968 Tb.1|Olenekian|Olenekian||ca. 248 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
38276|Oban River Leucomonzogranite|69639|5|Briefly described|p1, p26, p94, p218-p219, p221|Triassic|Lopingian|New England Orogen.|252.1 +/- 1.4 Ma (Cross and Blevin, 2013)|Oban Suite||Intrudes the Wards Mistake Monzogranite.||
38276|Oban River Leucomonzogranite|71628|4|Described|p3:72; p8:92; p14: 1, 15-23, 26, 31-32|||See also p19: 12, 105. Henley et al. (2001) after unpublished work by Chappell and Bryant (1994). Originally the Oban River Leucoadamellite (Binns et al., 1967 after unpublished work by Neilson, 1965). Named after a local stream. Occurs ~35 km NE of Guyra, forming cliffs and granite peaks and large rounded tors. Mineralogy, geochemistry detailed. Is associated with vein Au-Ag-Bi-W, sheeted vein Sn, and disseminated Sn deposits (named), as well as numerous placer Sn, Au, sapphire and topaz deposits (named). RELATED UNITS (continued): Is intruded by Black Knob Monzogranite and Moggs Swamp Complex. DESCRIPTION (continued): Locally includes a pink, fine- to very fine-grained, equigranular, saccharoidal microleucogranite, medium-grained variants, and a porphyritic marginal variant.|252.1 +/- 1.4 Ma (SHRIMP: Cross and Blevin, 2013).|Kingsgate Suite.||Intrudes Sara beds, Wards Mistake Monzogranite, and possibly Red Range Microleucogranite, Yellow Gap Microleucomonzogranite and Kookabookra Monzogranite. See COMMENTS for more.|Pink to white, coarse- to very coarse-grained, equigranular biotite leucomonzogranite and leucosyenogranite. I-type. See COMMENTS for more.|
31534|Oberon Suite|42726|5|Briefly described|map legend||Carboniferous|||||||
31534|Oberon Suite|44093|5|Briefly described|p207 App. 1|Late Carboniferous|Early Carboniferous|Geological Province: Lachlan Fold Belt.||||||
31534|Oberon Suite|68592|6|Mentioned|p1754|||In the Bathurst 1:250 000 map area. The type Suite in the Oberon Supersuite.||Unit in Oberon Supersuite.||||
31533|Oberon Supersuite|42726|5|Briefly described|map legend|||||||||
31533|Oberon Supersuite|68592|2|Defined|p74 Tb.5, p650, p1621, p1754-78|Carboniferous|Early Carboniferous|The Carboniferous plutons of the Goulburn 250 map area were previously assigned to "ungrouped" Tuglow and Lockyersleigh Suites by Chappell et al. (1991); and have been "grouped" with Oberon and Redfern Suites by Blevin (2011). Named after township of Oberon. Included Columba Granite (Phipps, 1950; Chappell et al., 1991), which is moved into Arthursleigh Suite because of elongate shape, similar geochemistry and geophysical response. The Oberon Suite is the type suite. Geochemistry detailed. Goulburn structural zone: deformation described.|||Includes Lockyersleigh and Tuglow Suites (Goulburn 250 map area); also Oberon and Redfern Suites.|Intrudes Cuddyong Formation.|Entirely felsic plutons: predominantly pink, medium- to coarse-grained, equigranular to locally megacrystic K-feldspar granite; with less abundant, usually marginal, more equigranular granodiorite containing more hornblende. Undeformed. I-type.|
31533|Oberon Supersuite|70297|4|Described|map legend, on side 2 of map sheet|Carboniferous|Carboniferous|Age: Middle to Late Carboniferous.|||Black Springs Granite, Burraga Granite, Duckmaloi Granite, Isabella Granite, Kanangra Granite, Oberon Granite, Rossdhu Granite, Sloggets Granite||Oxidised to reduced, occasionally strongly fractionated, I-type biotite-hornblende granite, leucogranite, and granodiorite. Equigranular to occasionally porphyritic.|19-MAY-16
31533|Oberon Supersuite|70661|6|Mentioned|p125, p128, p133|||Blevin et al (2010) suggest that this supersuite and supersuite classification of carboniferous granites in the sydney basin are generally unclear.|||Touga Granite, Bundundah Granite, Sloping Rock Monzogranite|||
27053|Obley Granite|22519|6|Mentioned|p7|||||||||
27053|Obley Granite|22831|4|Described|p70|Givetian|Eifelian|||||||01-NOV-13
27053|Obley Granite|23053|6|Mentioned|p23,69||Devonian|||||||
27053|Obley Granite|39658|6|Mentioned|M56|||||||||
27053|Obley Granite|42726|5|Briefly described|map legend|Early Devonian||412.  Of the Yeoval Suite (Boggy Plain Supersuite).||||||08-FEB-05
27053|Obley Granite|43441|5|Briefly described|30|Late Devonian|Middle Devonian|K-Ar dates doubtful||||||08-JAN-10
27053|Obley Granite|44160|5|Briefly described|Map Legend|Givetian|Eifelian|||||||08-JAN-10
31622|Ogilvies Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
35053|Old Armidale group|23050|4|Described|p77|||||||||
70129|Old Coach Road Formation|66623|2|Defined|pp192-193.|Middle Devonian|Early Devonian|Defined in this study. Part of former Snake Cave Sandstone. Correlated with Muckabunnya Formation. Mutawintji National Park. Coarse clastics form prominent strike ridges. Thickness is difficult to determine. Contains many trace fossils, worm tubes and burrows.||Unit in Wana Karnu Group.||Overlies Homestead Gorge Formation. Is overlain by Shell Hill Formation.|White to buff, thick-bedded quartz sandstone; pebbly sandstone and conglomerate. In the north, medium- to coarse-grained, planar sandstones, pebbly sandstones and conglomerate. In the south, conglomerates have coarse sandy or clay-siltstone matrix.|
70129|Old Coach Road Formation|66918|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Wana Karnu Group.||Overlies Shell Hill Formation. Is overlain by Bengoro Ridge Formation.|Dominated by medium- to coarse-grained, white to cream, flaggy sandstones, rarely laminated and pebbly, with interbedded conglomerate.|
70129|Old Coach Road Formation|70650|5|Briefly described|Map Legend|Devonian|Devonian|||Wana Karnu Group|||Dominated by medium- to coarse-grained, white to cream flaggy sandstone, rarely laminated and pebbly, with interbedded conglomerate.|
69703|Old Cork beds|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Geological region: Diamantina.||||||
69703|Old Cork beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.|||||Fluviatile and lacustrine grey mudstone, and white limestone, minor sandy siltstone, silty sandstone, calcareous sandstone; duricrusted.|
69703|Old Cork beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
69703|Old Cork beds|69599|5|Briefly described|p584, p599|Eocene|Paleocene|Old Cork Basin. Maximum thickness 78m. The limestones contains freshwater gastropods and ostracods. Capped by silcrete and laterite of the Canaway profile. RELATED UNITS (continued): Also correlated (at least partly) with Moonie, Eyre, Glendower, Edkins, Springvale and Marion Formations.||||Unconformably overlies Winton Formation. Is overlain unconformably by Mueller Sandstone. Correlated (at least partly) with Werite beds; Mueller and Moses Sandstones; see COMMENTS for more.|Dominated by limestone and mudstone, with subordinate silty sandstone, calcareous sandstone and sandy siltstone. Surface exposures are commonly silicified; contains abundant wood fragments.|
35067|Old Leake Quartz Monzonite|23043|5|Briefly described|Map Legend|Tournaisian|Tournaisian|of Gulgong Plutonic Suite.||||||
35067|Old Leake Quartz Monzonite|23170|2|Defined|p270|Early Carboniferous|Late Devonian|Age: SHRIMP date 357.6+/- 4.8 Ma. of Gulgong Plutonic Suite.||||||
35067|Old Leake Quartz Monzonite|68003|5|Briefly described|p24 Fig.3-e, p141. |Famennian|Famennian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gulgong Plutonic Suite.|||Mafic quartz monzonite.|
35067|Old Leake Quartz Monzonite|68004|5|Briefly described|p122, p196.|||Likely source of zinc-lead skarn mineralisation at Leadville. Oxidised and highly magnetic. Has high potential and a certainty level of C.|||||I-type, felsic and fractionated.|
27527|Olivedale Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Ash flow unit. Geological Province: Kopyje Shelf (Darling Basin).||||||
27527|Olivedale Tuff Member|35287|6|Mentioned|p7|||||||||
27527|Olivedale Tuff Member|39618|6|Mentioned|Table 9|||||||||
27527|Olivedale Tuff Member|42566|3|Fully described|p67|||Previously incorrectly identified as part of the 'Ballast Chert' (Brunker, 1968), or 'Ballast Group (Rayner, 1969).|||||Massive blue grey to white, crystal - vitric tuff containing small chloritic 'clots' or wisps.|24-SEP-19
27527|Olivedale Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
82352|Omadale Brook Granodiorite|71628|4|Described|p6: 2, 4-8, 10, 12, 16-25; p9: 1-2|||New name (this study), after the Omadale Brook pluton of Mason and Kavalieris (1984). One of three units that replaced Barrington Tops Granodiorite, in Bryant et al. (2003), after unpublished work by Chappell and Bryant (1994). Is excluded from Clarence River Supersuite in this study. Named after a local watercourse. Occurs ~40 km W of Gloucester. Poor outcrop in swampy areas, with local rounded boulders and low-level whalebacks. Geochemistry described.|272.5 +/- 1.65 Ma (Waltenberg et al., 2015).|Omadale Brook Suite.||Intrudes Woolooma Formation.|Waxy, medium-grained orthopyroxene-clinopyroxene-(hornblende-biotite) granodiorite; porphyritic, finer-grained chilled marginal phase. I-type.|
82351|Omadale Brook Suite|71628|5|Briefly described|p6: 7, 10, 14, 16, 23|||Apparently a petrographic, rather than stratigraphic, subdivision of the Barrington Tops Complex by Mason and Kavalieris (1984) which in this study is formalised stratigraphically. Includes Omadale Brook, Barrington River and Gloucester Tops Granodiorites.||Barrington Tops Supersuite.|Omadale Brook, Barrington River, Gloucester Tops Granodiorites.|||
77371|Onavale Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
24437|Ondyong Point Formation|42727|5|Briefly described|map schematic section|Tertiary|Tertiary|Sand, clay, silt; fluvio-lacustrine facies. Overlies Gearys Gap Formation; underlies Bungendore Formation. Point is Pt in text. See Lake George (Subsurface stratigraphy) schematic section and chart.||||||
24437|Ondyong Point Formation|42820|2|Defined|p58|late Miocene||||||||
24437|Ondyong Point Formation|47060|5|Briefly described|p163|||Reserved R.Abell 1984.||||||
24437|Ondyong Point Formation|67125|5|Briefly described|Slide 36.|Cenozoic|Cenozoic|Tertiary. A change from coarse to fine grained sediments probably indicates the effect of movement of the Lake George Fault, damming the flow of Taylors Creek to form Lake George. Pollen suites indicate a cool temperate rainforest 3 - 5 Ma, interspersed with grassland.||||Overlies Gearys Gap Formation. Is overlain by Bungendore Formation.|Fluvio-lacustrine cyclic deposits of clay/silt and sand.|
24437|Ondyong Point Formation|70377|5|Briefly described|p855, p856, p858 Fig 4, p859, p868|Quaternary|Piacenzian|Lake George Basin. Thickness at type section Core C354: 52 m (from 54-106 m depth). Burial age from cosmogenic nuclides from sample taken from 89.3-90.45m. Maximum age inferred from palynoflora in underlying unit plus burial age.|burial age 2.97+/- 0.23 Ma|||Overlain by Bungendore Formation. Underlain by Gearys Gap Formation.|Fluvio-lacustrine sands, silts and clays|23-MAY-19
24437|Ondyong Point Formation|71069|5|Briefly described|p21 fig 7, p33, p208, p209, p211-212|Pliocene|Pliocene|Name derived from Ondyong Point. Fluvial to lacustrine depositional environment. ||Weereewa Group||Overlies the Gearys Gap Formation (possibly disconformably), conformably overlain by the Bungendore Formation.|Sand that is coarse grained and normally graded, silt and clay.|
24437|Ondyong Point Formation|71691|5|Briefly described|Map legend.|Quaternary|Neogene|||Weereewa Group.||Overlies Geary Gap Formation. Is overlain by Bungendore Formation.|Horizontally bedded sand, silt and clay, fluvio-lacustrine sediments, with some well-rounded aeolian sand;  red-brown ferruginous profiles occur sporadically throughout (does not crop out).|
24440|Onslow Granodiorite|36413|2|Defined|p93|Devonian|Devonian|||||||
24440|Onslow Granodiorite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Michelago Igneous Complex. Biotite-hornblende granodiorite. GSNSW map code: gco.||||||
24440|Onslow Granodiorite|39626|6|Mentioned|p276|||||||||
24440|Onslow Granodiorite|39627|6|Mentioned|Table 1|||||||||
24440|Onslow Granodiorite|40328|4|Described|p210|||||||||
76037|Oolambeyan granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Baconian Swamp Granite Suite.|||Interpreted S-type granites.|
76037|Oolambeyan granite|70718|4|Described|p75-p76, p125|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics. Magnetic highs have correpsonding gravity lows. Age derived from cross cutting relationship of the Oolambeyan and Eurolie granites.||Baconian Swamp granite suite||Cross-cuts the Eurolie granite.|S-type granitic rocks.|
31296|Orchard Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group. Micaceous fine sandstone.||||||29-JUN-04
35392|Ormoral Volcanics|61392|4|Described|p163-165, p167|Middle Devonian|Early Devonian|Of Silverwood Group (Keinjan Terrane). Consists of high-level mafic intrusive rocks, subaqueous mafic extrusives, syn-eruptive hydroclastic facies, resedimented subaerial lapillistones and proximal high-density turbidites. Max. thickness: 620m||||||07-FEB-11
35392|Ormoral Volcanics|63731|5|Briefly described|Map legend|Devonian|Silurian|Of Silverwood Group. Almalgamated volcaniclastic arenite, basaltic to andesitic lavas and volcaniclastic arenite and siltstone with interbedded peperite.||||||
35392|Ormoral Volcanics|63748|4|Described|p7 Fig. 3, p8|Middle Devonian|Middle Devonian|Of Silverwood Group. Conformable on Bald Hill Fm. Max.thickness: ~620m. Geol.Prov:Silverwood province. Include dolerite, anorthosite, basalt, basaltic andesite + backarc andesite.||||||07-FEB-11
35392|Ormoral Volcanics|68679|5|Briefly described|p445-447|Middle Devonian|Middle Devonian|Van Noord (1999). Silverwood Province. Low-K tholeiitic submarine extrusives. Up to ~620m thick. Deposited in a deep-marine intra-arc basin. Unfossiliferous.||Silverwood Group.||Conformably overlies Bald Hill Formation. Is overlain unconformably by Bromley Hills Formation.|Hypabyssal rocks include dolerite, anorthosite, basalt, basaltic andesite and andesite. Extrusive rocks include pillow lava, hyaloclastite and peperite sporadically interbedded with proximal, epiclastic high-density turbidites.|
35392|Ormoral Volcanics|73600|6|Mentioned|p204|Devonian|Devonian|New England Orogen.||||||
77622|Ottery Monzogranite|71628|5|Briefly described|p8: 4, 87-89|||New name (this study). Originally the Ottery Adamellite-Porphyrite of Wood (1982). Named after the Ottery As-Sn Mine/Prospect. A small (<1 km x several hundred metres) body ~7km NE of Emmaville. Geochemistry described. Spatially associated with historically significant Sn and As mineralisation (likely sourced from Mole Leucogranite).||Wards Mistake Suite.||Intrudes between Emmaville Volcanics and Gulf Siltstone-Argillite Formation; also adjacent to Dundee Rhyodacite.|Porphyritic biotite-hornblende monzogranite; locally micrographic; extensively altered.|
39261|Ourimperee Ignimbrite Member|50613|2|Defined|p213, p230 App. 1|Namurian|Namurian|Of the Willuri Formation.  Volcanic member of the Gunnan package (informal grouping of stratigraphically recognisable distinctive, mappable units. Max. thickness: 115m in type section.  geol.Prov: New England Orogen.  See also p210 Fig. 4.||||||22-FEB-05
24448|Owendale Intrusive Complex|730|6|Mentioned|p22 Fig.5.|||||||||11-NOV-14
24448|Owendale Intrusive Complex|22519|5|Briefly described|p6|||||||||
24448|Owendale Intrusive Complex|22831|4|Described|p 21|Early Devonian|Late Ordovician|||||||
24448|Owendale Intrusive Complex|23053|6|Mentioned|p75|||||||||
24448|Owendale Intrusive Complex|40365|2|Defined|p329|Early Devonian|Early Devonian|||||||
24448|Owendale Intrusive Complex|40682|5|Briefly described|p2|||||||||
24448|Owendale Intrusive Complex|41871|6|Mentioned|p1|||||||||
24448|Owendale Intrusive Complex|42077|5|Briefly described|p21|||||||||
24448|Owendale Intrusive Complex|42912|6|Mentioned|Fig.1|||||||||
24448|Owendale Intrusive Complex|43441|5|Briefly described|12, 21|||Age: ?Late Ordovician||||||08-JAN-10
24448|Owendale Intrusive Complex|44160|5|Briefly described|Map Legend||Eastonian|||||||08-JAN-10
26827|Oxley Metamorphics|23720|5|Briefly described|Map Legend|||Part of the "Sandon Association".||||||08-DEC-04
26827|Oxley Metamorphics|31694|6|Mentioned|p344|||||||||
26827|Oxley Metamorphics|38804|5|Briefly described|p95|||||||||
26827|Oxley Metamorphics|41347|5|Briefly described|p409|||||||||
26827|Oxley Metamorphics|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Part of the "Sandon Association".||||||16-DEC-04
26827|Oxley Metamorphics|42803|6|Mentioned|Fig.1 P112|||||||||
26827|Oxley Metamorphics|42872|5|Briefly described|p103|||||||||
26827|Oxley Metamorphics|42997|5|Briefly described|p39|||||||||
26827|Oxley Metamorphics|44450|3|Fully described|p12 Table 1|Early Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||
26827|Oxley Metamorphics|71628|5|Briefly described|p3:86|||Korsch (1977); regarded these as metamorphosed equivalents of the Sandon Association.|||||More mafic.|
26093|Paddys River Volcanics|12185|5|Briefly described|map legend|Middle Silurian|Middle Silurian|Dacite, acid tuff, lenses of limestone, calcaroues shale, phyllite. BMR map symbol: Smp.||||||
26093|Paddys River Volcanics|22768|5|Briefly described|p176|||||||||
26093|Paddys River Volcanics|22857|4|Described|p176, p464 App. 1 Tb.A1.6|Wenlockian|Wenlockian|Of the Hawkins Suite. Dacitic ignimbrites and tuffs, dacitic lava.||||||
26093|Paddys River Volcanics|23866|5|Briefly described|p120|||Intruded by Shannons Flat Granodiorite. Geological Province: Murrumbidgee Batholith.||||||03-OCT-07
26093|Paddys River Volcanics|24005|5|Briefly described|p293|Silurian|Silurian|Geological Province: Lachlan Fold Belt||||||
26093|Paddys River Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
26093|Paddys River Volcanics|29994|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
26093|Paddys River Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
26093|Paddys River Volcanics|31111|6|Mentioned|p172|||See also P174, 176, 178, 182, 186, 188.||||||
26093|Paddys River Volcanics|33325|5|Briefly described|Table 2|||Unconformable on Ord. rocks P13.||||||
26093|Paddys River Volcanics|34405|6|Mentioned|p114|||||||||
26093|Paddys River Volcanics|36441|5|Briefly described|map legend|Wenlockian|Wenlockian|Extrusive. Grey green dacite ignimbrite, limestone and shale lenses, minor rhyolite and andesite. Unconformably overlies Adaminaby Beds and Nungar Beds; intruded by Shannons Flat Adamellite. BMR map code: Smp.||||||
26093|Paddys River Volcanics|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
26093|Paddys River Volcanics|37727|4|Described|p77|||||||||
26093|Paddys River Volcanics|37728|4|Described|Table 2|||||||||
26093|Paddys River Volcanics|38035|6|Mentioned|p93|||||||||
26093|Paddys River Volcanics|40328|4|Described|p116|||||||||
26093|Paddys River Volcanics|41356|4|Described|p22|||||||||
26093|Paddys River Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
26093|Paddys River Volcanics|42820|5|Briefly described|p7|||||||||
26093|Paddys River Volcanics|43159|6|Mentioned|Fig.2p4,p3.|||||||||
26093|Paddys River Volcanics|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv1||||||
26093|Paddys River Volcanics|45147|2|Defined|M137|late Wenlockian|late Wenlockian|||||||
26093|Paddys River Volcanics|60078|6|Mentioned|Map Legend|Late Silurian|Late Silurian|||||||
26093|Paddys River Volcanics|68592|6|Mentioned|p428, p443, p457|Silurian|Silurian|Best et al. (1964). Equivalent to, but not yet formally included in, the Douro Group.||||||
26093|Paddys River Volcanics|71040|6|Mentioned|p11|Late Silurian|Late Silurian|Brindabella-Tantangara region. Locally affected by the Bindian (=Bowning) Orogeny.||||||
29593|Padua Granodiorite|23214|3|Fully described|p159|Late Silurian|Late Silurian|Forms part of the Pine Mount Granodiorite of Stevens (1955) and the Pine Mount Intrusive Complex of Madsen (1970).  Intrudes Walli Volcanics. Geological Province: Lachlan Fold Belt||||||
29593|Padua Granodiorite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of medium grained, equigranular, biotite hornblende granodiorite.||||||17-JUL-08
29593|Padua Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyangala Batholith.||||||17-JUL-08
29593|Padua Granodiorite|63289|6|Mentioned|p367, p368 Fig. 5a|Silurian|Silurian|Silurian granite.||||||07-FEB-11
29593|Padua Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|||Grants Corner Supersuite||||
31526|Padua Suite|42726|5|Briefly described|map legend||Silurian|||||||
78466|Paleozoic ultramafics, undivided 78466|69042|6|Mentioned|map legends|||MS. Narrow horizons of moderate to high magnetic intensity. Ultramafics, mafic schist, magnetite quartzite. Age unknown.||||||
26829|Pallal Conglomerate Member|23051|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|of Parry Group.||||||
26829|Pallal Conglomerate Member|30133|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26829|Pallal Conglomerate Member|37987|6|Mentioned|p228|||||||||
26829|Pallal Conglomerate Member|38222|6|Mentioned|Fig.2|||||||||
26829|Pallal Conglomerate Member|43436|14|Not recorded|Map Legend|||(Provisional Edition)||||||
26829|Pallal Conglomerate Member|68003|5|Briefly described|p138.|Devonian|Carboniferous|Tamworth Belt (North), New England Fold Belt.||Unit in Namoi Formation.|||Cross-bedded, coarse-grained wacke, lenticular orthoconglomerate and siltstone.|
26829|Pallal Conglomerate Member|68005|5|Briefly described|p56, p146.|Visean|Visean|Possibly formed in a submarine canyon. The rank 'Member' is omitted on p56.||Unit in Namoi Formation.|||Cross-bedded, coarse-grained wacke, lenticular orthoconglomerate and siltstone. Contains angular sedimentary blocks up to three metres in diameter.|
30029|Pamboola Formation|22857|4|Described|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Brothers Subgroup (Black Jack Group). Includes Melvilles Coal Member. Lithic sandstone, siltstone, claystone, conglomerate and intercalated coals. Max. thickness: 89m. Geological Province: Gunnedah Basin.||||||
30029|Pamboola Formation|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Of Brothers Subgroup. New, formal name for the 'basal lithic unit' in Black Jack Formation (now Black Jack Group). Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||13-NOV-13
30029|Pamboola Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Brothers Subgroup.||||||
30029|Pamboola Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Brothers Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Lithic sandstone, siltstone, coal, conglomerate and claystone.||||||
30029|Pamboola Formation|65116|4|Described|p444, Fig 6 p441|Late Permian|Late Permian|Of Black Jack Group. Lithic sandstone, siltstone, claystone and coal.||||||
30029|Pamboola Formation|68003|5|Briefly described|p38 Fig.3-j, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Correlative of Vane Subgroup (minus Bulga Formation) in the Hunter Coalfield, and of the Nile Subgroup (Western Coalfield).||Basal unit in Brothers Subgroup.||Overlies Watermark Formation. Is overlain by Brigalow and Arkarula Formations.|Includes lithic sandstone, siltstone.|
30029|Pamboola Formation|68004|5|Briefly described|p23 Table 1. |||Gunnedah Basin. Largely equivalent to the Vane and Nile Subgroups, and the Pheasants Nest Formation, in the Sydney Basin.||Basal unit in Brothers Subgroup.||Overlies Watermark Formation. Is overlain by Brigalow and Arkarula Formations.||
30029|Pamboola Formation|70791|5|Briefly described|p277|Permian|Permian|Gunnedah Basin.||Brothers Subgroup.||||
30029|Pamboola Formation|70878|5|Briefly described|p717 Fig.12, p718 Fig.13|Permian|Permian|Gunnedah Basin. This is shown in the Santos Brawboy 1 well completion report as underlying Arkarula Formation, but subsequent reinterpretation has that latter unit replaced by Brigalow Formation.||Black Jack Group.||Overlies Watermark Formation. Is overlain by Hoskissons Coal.||
30029|Pamboola Formation|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Overlies Watermark Formation. Is overlain by Arkaroola Formation.||
26830|Pangee Road Volcanic Breccia Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Agglomerate or breccia unit. Max. thickness: 200m. Geological Province: Kopyje Shelf (Darling Basin).||||||
26830|Pangee Road Volcanic Breccia Member|42566|3|Fully described|p70|||Variation on Pangee Road Agglomerate.||||||
26830|Pangee Road Volcanic Breccia Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
22625|Pappinbarra Formation|22616|6|Mentioned|Fig.1 p670||Carboniferous|||||||
22625|Pappinbarra Formation|22736|2|Defined|p619-23,27,29|Visean|Tournaisian|southern Hastings Block unit||||||
22625|Pappinbarra Formation|22857|4|Described|p500 App.1 Tb.A1.7|Visean|Tournaisian|Includes "Taree Limestone". Turbiditic lithic sandstone and interbedded hard grey siltstone, conglomerate, tuff, calcareous sandstone and limestone, bioturbation. Max. thickness: >1355m.||||||
22625|Pappinbarra Formation|44093|5|Briefly described|p67 Fig 6.6|Carboniferous|Carboniferous|Of the Southern Hastings Block. Geological Province: New England Fold Belt.||||||
22625|Pappinbarra Formation|66090|6|Mentioned|p4, p8, pp18-19 map.|Early Carboniferous|Early Carboniferous|Southern Hastings Block. Part of the floor of the Lorne Basin.||||||
22625|Pappinbarra Formation|70939|6|Mentioned|p826, p828|Carboniferous|Carboniferous|Southern Hastings Block.||||||
22625|Pappinbarra Formation|71628|5|Briefly described|p17: 55, 61, 74-75, 78|||Hastings Block. Appears as Pappinbarra beds on p55.||Quintoc Group.||Is intruded by Cairncross and Gundle Monzogranites, Hannam Vale, Juhle Mountain and Lorne Forest Granodiorites.||
27533|Paradise Porphyry|22815|4|Described|p94|||||||||
27533|Paradise Porphyry|23329|3|Fully described|1043|Late Devonian|Middle Devonian|||||||
27533|Paradise Porphyry|29992|6|Mentioned|Map legend|Carboniferous|Carboniferous|Post DevonianProb. Carboniferous||||||
27533|Paradise Porphyry|29994|6|Mentioned|Map legend|Carboniferous|Carboniferous|Post DevonianProb. Carboniferous||||||
27533|Paradise Porphyry|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
27533|Paradise Porphyry|60007|6|Mentioned|Map legend|Middle Devonian|Early Devonian|||||||
38315|Parkers Road seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
25742|Parkes Volcanics|22434|6|Mentioned|12|||Geol province Lachlan Fold Belt||||||
25742|Parkes Volcanics|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
25742|Parkes Volcanics|24417|3|Fully described|p26|Bolindian||Previously named "Parkes Andesite".  Now includes the former "Daroobalgie Volcanics".  Of Northparkes Volcanic Group.  Overlain by Cotton Formation.||||||
25742|Parkes Volcanics|40891|4|Described|p7|||Mention Fig.2||||||
25742|Parkes Volcanics|42489|5|Briefly described|Map legend|Bolindian|Eastonian|||||||
25742|Parkes Volcanics|42920|6|Mentioned|Fig.2|||||||||
25742|Parkes Volcanics|46522|1|Redefined|p29|Late Ordovician||Supersedes Parkes Andesite.||||||
25742|Parkes Volcanics|46524|5|Briefly described|p103|||See also Appendix 1 p129.||||||07-SEP-18
25742|Parkes Volcanics|46525|6|Mentioned|Fig.1 P143|||||||||
25742|Parkes Volcanics|46528|5|Briefly described|Map legend|Late Ordovician||||||||
25742|Parkes Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
25742|Parkes Volcanics|60009|5|Briefly described|Map Legend|Bolindian|Darriwilian|Of the Northparkes Volcanic Group.||||||13-JUL-04
25742|Parkes Volcanics|63278|6|Mentioned|p145 Fig. 1, p151|Odrovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
25742|Parkes Volcanics|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
25742|Parkes Volcanics|63283|5|Briefly described|p185 Tb. 1, p191 Tb. 2, p196 Fig. 4|Late Ordovician|Middle Ordovician|Age: 465Ma (pl-phyric andesite). Geological Province: Junee-Narromine Volcanic Belt. Consist of plagioclase-phyric basaltic andesites and andesites with subordinate augite phenocrysts. See p192.||||||07-SEP-18
25742|Parkes Volcanics|63290|6|Mentioned|p389, p397 Fig. 3(b)|Darriwilian|Darriwilian|Of Northparkes Group. Geological Province: Junee - Narromine Volcanic Belt.||||||
25742|Parkes Volcanics|64681|6|Mentioned|p16 Fig. 12|||||||||
25742|Parkes Volcanics|67106|6|Mentioned|p673|||Junee-Narromine Volcanic Belt.||||||
25742|Parkes Volcanics|67107|6|Mentioned|p696|||Peak Hill, c.45km N of Parkes.||||||
25742|Parkes Volcanics|67322|5|Briefly described|Fig.5; p22|Ordovician|Ordovician|Macquarie Arc. Recognised and defined by Sherwin et al. (1987) and Krynen et al. (1990); later described by Meffre et al. (2007). Age is determined from p20 Fig.5 (Strat. column) - not well constrained. Compositionally distinct from Nelungaloo and Goonumbla Volcanics; closer affinities with Cargo and Walli Volcanics. Occurs in the Junee-Narromine region.||Of Northparkes Group?|||Moderately plagioclase-phyric basaltic andesites and andesites with subordinate augite phenocrysts.|22-FEB-18
25742|Parkes Volcanics|70684|6|Mentioned|p54 Fig.27, p55, p74-75|Middle Ordovician|Middle Ordovician|Junee-Narromine Volcanic Belt.||||||
25742|Parkes Volcanics|72495|5|Briefly described|p218, 225, 227, p231|Ordovician|Ordovician|Occurs to the east of the Parkes Thrust as scattered outcrop surrounded by regolith. Age inferred from geochemical similarity to the Northparkes Volcanic Group. Strongly deformed in the vicinity of the London-Victoria goldmine. Includes Daraboolgie Volcanics.|||||Andesite, basaltic andesite and conglomerate.|26-MAR-20
25742|Parkes Volcanics|73154|5|Briefly described|p77 Fig.3|Darriwilian|Darriwilian|Macquarie Arc, Phase 2. Junee-Narromine Belt.|||||Intermediate-mafic lava.|
25742|Parkes Volcanics|73492|6|Mentioned|p707|||||||||
35788|Parkesbourne Granite|50232|5|Briefly described|Map legend|Early Devonian|Early Devonian|Part of the Wologorong Batholith.  Foliated to massive , cream biotite leucocratic muscovite biotite sodic granite and soda syenite.||||||13-MAY-04
35788|Parkesbourne Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Part of the Wologorong Batholith.||||||
35788|Parkesbourne Granite|67820|5|Briefly described|p137|||Of Wologorong Batholith. Reduced and moderately fractionated; potential for Sn mineralisation.||||||
35788|Parkesbourne Granite|68592|6|Mentioned|p112, p270|Early Devonian|Early Devonian|Truncates the Mummel Anticline south of Woodhouselee. 2-4 km-wide gravity highs around the flanks of this unit are ascribed to contact metamorphic aureoles: enhanced density due to mild hornfelsing.||||||
35788|Parkesbourne Granite|70296|6|Mentioned|p19|Ludlow|Wenlock|Caused contact metamorphism in Campbells Group. Must be only marginally younger than Kangaloolah Volcanics.|425.5+/-2.4 Ma.|||||21-JAN-21
69872|Parkesbourne Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes the Wologorong, Gurrundah and Dawsons Granites.  Rocks are granites and granodiorite.||||||
69872|Parkesbourne Suite|66087|6|Mentioned|p3 Fig. 2|Devonian|Devonian||||Includes Wologorong Granite.|||10-MAY-12
69872|Parkesbourne Suite|68592|2|Defined|p29, p113, p1228, p1542, p1550-68|Devonian|Devonian|New name, after locality of Parkesbourne. These plutons form the southern part of the Wologorong Batholith which was called the Wologorong-Tumboramboro Granite by Schneibner (1973). Extensive outcrops as large boulders and tors in the north; heavily obscured by regolith in the south. Type pluton is the Wologorong Granite. Geochemistry detailed and discussed. Low mineral potential; quarried locally for construction material and decorative aggregate.|425.5 +/- 2.4 Ma SHRIMP U-Pb; Black, 2005).|Unit in Wologorong Supersuite.|Includes Wologorong, Dawsons and Gurrundah Granites.|Intrudes Abercrombie and Cuddyong Formations. Is intruded by Bishopthorpe Suite.|Leucocratic, fine- to coarse-grained, equigranular to sparsely porphyritic, muscovite-biotite granite and granodiorite; minor quartz monzonite, aplite and rhyolite dykes. Largely unstrained to strongly foliated to mylonitic. S-type.|
69872|Parkesbourne Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|On Taralga, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Dawsons Granite, Gurrundah Granite, Wologorong Granite.|||
69872|Parkesbourne Suite|70541|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Dawsons Granite, Gurrundah Granite, Wologorong Granite.|||
69872|Parkesbourne Suite|70542|5|Briefly described|Map Legend|Early Devonian|Early Devonian||||Includes Dawsons Granite, Gurrundah Granite, Wologorong Granite.|||
69872|Parkesbourne Suite|70543|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Wologorong Granite|||
27217|Parkvale Gabbro|22768|6|Mentioned|p170|||||||||
27217|Parkvale Gabbro|22857|6|Mentioned|p170|||Of the Cobar Supergroup?||||||10-NOV-14
27217|Parkvale Gabbro|35287|5|Briefly described|p9|||||||||
27217|Parkvale Gabbro|41528|6|Mentioned|p110|||||||||
27217|Parkvale Gabbro|42566|2|Defined|p98|Early Devonian|Early Devonian|Two bodies near Bobadah.||||Intrudes Majuba Volcanics.|Dark blue-green coarsely crystalline horneblende-biotite gabbro.|24-SEP-19
27217|Parkvale Gabbro|42568|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
27217|Parkvale Gabbro|43089|5|Briefly described|Map Legend|||||||||
27217|Parkvale Gabbro|68823|6|Mentioned|p401|||In Bobadah 1:1000 geological sheet area, Lachlan Orogen; mapped by Pogson (1991).||||||
27217|Parkvale Gabbro|70751|6|Mentioned|p27|||Within-plate tholeiitic character.||||||
67895|Parlour Mountain Leucomonzogranite|69639|5|Briefly described|p2, p32, p95, p219|Lopingian|Lopingian|New England Orogen.|254.7 +/- 1.6 Ma (Cross and Blevin, 2010)|Uralla Supersuite||||
67895|Parlour Mountain Leucomonzogranite|70217|5|Briefly described|p74 tbl 14.1|Wuchiapingian|Wuchiapingian|New England Orogen. Age derived from Cross and Blevin, 2010.|254.7 +/- 1.6 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
67895|Parlour Mountain Leucomonzogranite|71628|4|Described|p19: 141-145|||DMR NAND04 Nandewar Geology Integration and Upgrade project, after Chappell and Bryant (1994, unpublished). Named after a local geographical feature. Located ~5 km SW of Baldersleigh. Forms a series of ridges, hills and valley flats over 32 km2; crops out as tors and whalebacks. Constitutes the subvolcanic intrusive mass in a collapsed caldera structure. Lithology and mineralogy detailed; geochemistry described. Is associated with diverse Sn, As, Mo and W mineralisation, mostly small and low grade.|254.7 +/- 1.6 Ma (SHRIMP: Cross and Blevin, 2010).|Parlour Mountain Suite.||Intrudes Sandon beds; and Baldersleigh and Abington Volcanics (Wandsworth Volcanic Group).|Medium- to coarse-grained, equigranular, K-feldspar-rich biotite leucomonzogranite with minor leucosyenogranite, microgranite, and coarser-grained variants. I-type.|
26096|Parnell Formation|6823|5|Briefly described|p205, 206, 207, 233, 234|Palaeoproterozoic|Palaeoproterozoic|Age is derived from Page and Laing (1992).|1693 +/- 5 Ma (SHRIMP U-Pb, magmatic age)|||||26-MAR-22
26096|Parnell Formation|22553|5|Briefly described|fig2p77,p80|Proterozoic|Proterozoic|||||||
26096|Parnell Formation|22771|5|Briefly described|Table12.2p45,45,47|||||||||
26096|Parnell Formation|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Purnamoota Subgroup (Broken Hill Group). Age: 1693+/-5Ma (Page and Laing, 1992). Max. thickness: 500m. Geological Province: Willyama Fold Blt. ||||||07-NOV-08
26096|Parnell Formation|22884|5|Briefly described|p47||Statherian|Middle unit of Broken Hill Group. Age of unit is 1693+/-5 Ma. Geological province: Broken Hill Domain.||||||26-MAR-09
26096|Parnell Formation|22964|4|Described|p55,58||Statherian|||||||
26096|Parnell Formation|22965|6|Mentioned|p14,Fig1||Statherian|Part of the Purnamoota Subgroup.||||||
26096|Parnell Formation|22966|5|Briefly described|p3,4 Fig1||Proterozoic|Rift stage of development.||||||
26096|Parnell Formation|22967|6|Mentioned|p31,42,37||Statherian|||||||
26096|Parnell Formation|23025|6|Mentioned|Fig1p75|||||||||
26096|Parnell Formation|23223|5|Briefly described|p42|||Equivalent to amphibolite in BS-ECM. of Purnamoota Subgroup.||||||
26096|Parnell Formation|23248|5|Briefly described|Fig2p169|||||||||
26096|Parnell Formation|23347|6|Mentioned|p51 Tb. 1|||Geological province: Broken Hill Domain.||||||24-MAR-09
26096|Parnell Formation|23461|5|Briefly described|p204 Fig. 3|||Of Broken Hill Group||||||11-JUN-08
26096|Parnell Formation|23565|5|Briefly described|p195|||Of Broken Hill Group.||||||
26096|Parnell Formation|24197|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Potosi Supersuite. Geological province: Broken Hill Inlier.||||||07-FEB-11
26096|Parnell Formation|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|Of the Broken Hill Group.   Previously included in the Purnamoota Subgroup, which has been abandoned by this study.||||||18-JUN-08
26096|Parnell Formation|38969|4|Described|p208|||||||||
26096|Parnell Formation|39662|2|Defined|p426|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26096|Parnell Formation|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26096|Parnell Formation|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26096|Parnell Formation|39849|6|Mentioned|Table 2|||||||||
26096|Parnell Formation|40290|6|Mentioned|Fig.2|||||||||
26096|Parnell Formation|40822|6|Mentioned|Fig.2|||||||||
26096|Parnell Formation|41093|6|Mentioned|p252|||||||||
26096|Parnell Formation|41145|6|Mentioned|Fig.4|||||||||
26096|Parnell Formation|41630|6|Mentioned|p26|||||||||
26096|Parnell Formation|41633|6|Mentioned|p139|||||||||
26096|Parnell Formation|41651|5|Briefly described|p188|||||||||
26096|Parnell Formation|41870|6|Mentioned|p120|||||||||
26096|Parnell Formation|42181|4|Described|p251|||See also Fig.1||||||
26096|Parnell Formation|42261|6|Mentioned|Fig 1 P530|||||||||
26096|Parnell Formation|42286|6|Mentioned|p7|||||||||
26096|Parnell Formation|42323|5|Briefly described|p4|||||||||
26096|Parnell Formation|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26096|Parnell Formation|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26096|Parnell Formation|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26096|Parnell Formation|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26096|Parnell Formation|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
26096|Parnell Formation|42537|6|Mentioned|Fig.2 P5|||||||||
26096|Parnell Formation|42595|6|Mentioned|Fig. 2 P5|||||||||
26096|Parnell Formation|42897|5|Briefly described|p320|||||||||
26096|Parnell Formation|43052|6|Mentioned|Fig.4.22|||||||||
26096|Parnell Formation|43086|6|Mentioned|Fig.3|||||||||
26096|Parnell Formation|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
26096|Parnell Formation|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
26096|Parnell Formation|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
26096|Parnell Formation|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
26096|Parnell Formation|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Sub-Group.||||||07-NOV-08
26096|Parnell Formation|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Purnamoota Subgroup.||||||07-NOV-08
26096|Parnell Formation|43572|6|Mentioned|p5||Paleoproterozoic|||||||07-NOV-08
26096|Parnell Formation|43583|4|Described|Table 1,p2139,2140|||||||||
26096|Parnell Formation|46598|4|Described|p304|||||||||
26096|Parnell Formation|50045|5|Briefly described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Purnamoota Subgroup (Broken Hill Group). Overlain by Freyers Metasediments; underlain by Allendale Metasediments.||||||31-MAY-07
26096|Parnell Formation|50606|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Potosi Suite. Geological Province: Broken Hill Block. Age: 1696 +/- 6Ma (U-Pb).||||||07-NOV-08
26096|Parnell Formation|50619|5|Briefly described|p175|Paleoproterozoic|Paleoproterozoic|Of the Purnamoota Subgroup (Broken Hill Group).  Geological Province: Broken Hill Block.||||||07-NOV-08
26096|Parnell Formation|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Intrusive rocks.  Age: 1693+/-5Ma.  Geological Province: Broken Hill Domain.||||||
26096|Parnell Formation|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
26096|Parnell Formation|61735|5|Briefly described|p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Crystallisation age: 1693+/-5Ma and >/-1682+/-9Ma. metamorphic age 1594+/-7 Ma. Presented as Parnell only in Fig. 2.||||||04-JUN-15
26096|Parnell Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Age: 1693+/-5Ma. Geological province: Olary Domain.||||||
26096|Parnell Formation|62373|6|Mentioned|p502, p503 Fig.2|||In Broken Hill region, NSW||||||
26096|Parnell Formation|62473|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group.||||||17-JUN-09
26096|Parnell Formation|62535|5|Briefly described|p666 Fig.3, p671-672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1693 +/- 5 Ma.|Broken Hill Group.||||
26096|Parnell Formation|62536|4|Described|p633, 636, 639-640, 645-646, 658|||Broken Hill area. Most of the many small Broken Hill-type Pb-Zn-Ag deposits occur in or very close to this unit. Metamorphosed at 1594 +/- 7 Ma.|1682 +/- 9 Ma (min. crystall'n age).|Broken Hill Group.||Overlies Ettlewood Calc-Silicate Member.|Felsic metavolcaniclastic rocks. Amphibolite common. Contains many Corruga-type tungsten deposits (i.e. scheelite with Cu, Pb, +/- Zn in calc-silicate rocks).|
26096|Parnell Formation|62592|5|Briefly described|p16 Fig.2.2. |Statherian|Statherian|Broken Hill Domain, Curnamona Province.|1693 +/- 5 Ma.|||||
26096|Parnell Formation|63102|5|Briefly described|p12-14,30,34,39,53-54|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province. Suite of mafic sills or flows.  Chronostratigraphic equivalent of Lady Louise Suite.|1693+\-5 Ma|||Intrudes Broken Hill Group.||
26096|Parnell Formation|63186|5|Briefly described|p67 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Olary Domain, Curnamona Province.||||||07-NOV-08
26096|Parnell Formation|63519|5|Briefly described|Abstract, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Gp. Age: 1693+/-5Ma, >1688+/-9Ma. Comprises quartzo-feldspathic gneiss. Some embedded metasediments and bounding amphibolites. Hosts the Allendale mine. See also p10 Fig. 3, p13, p29 Fig. 11. ||||||07-NOV-08
26096|Parnell Formation|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province. ||Purnamoota Subgroup||Overlies the Allendale Metasediments. Overlain by the Freyers Metasediments.|Amphibolite/mafic granulite associated with garnetiferous quartzo-feldspathic gneiss.|
26096|Parnell Formation|64097|5|Briefly described|p302 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group (Willyama Supergroup).  Age: 1693 +/- 5 Ma on Potosi-type gneiss.||||||07-FEB-11
26096|Parnell Formation|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Purnamoota Subgroup (Broken Hill Group, Willyama Supergroup). Geological Province: Broken Hill Block. Contains quartz-feldspathic garnet-rich Potosi-type gneisses.||||||07-FEB-11
26096|Parnell Formation|64741|6|Mentioned|p309|||Part of this unit is now named Parnell Gneiss. Name no longer in use.||||||07-FEB-11
26096|Parnell Formation|64742|6|Mentioned|p321 Fig.3. |||||Unit in Broken Hill Group.||||
26096|Parnell Formation|66302|5|Briefly described|p38-40|||Broken Hill Domain, Curnamona Province. Interpreted as the product of bimodal rhyodacitic to tholeiitic basaltic volcanism. [see also Parnell Gneiss]. Time equivalent of the Rasp Ridge granite gneiss.||||Overlies the Ettlewood Calc-silicate Member. Overlain by the Freyers Metasediments.|Amphibolite-mafic granulite and garnetiferous quartzofeldspathic gneiss.|
26096|Parnell Formation|68126|6|Mentioned|p30||||1693 +/- 4 Ma (Stevens et al., 2008).|||||
26096|Parnell Formation|69999|6|Mentioned|p16||||||||Includes orthopyroxene-bearing mafic gneiss.|
26096|Parnell Formation|70014|5|Briefly described|Map legend|||Quartzo-feldspathic gneiss is mostly medium-grained quartz-plagioclase-K feldspar-biotite-garnet ("Potosi") gneiss, and is interpreted as a dacitic to rhyodacitic metavolcanic. The basic gneisses are typically thinly layered with abundant garnet or pyroxene, and are interpreted as Fe-rich altered tholeiitic metavolcanics. The "lode horizon" rocks are commonly associated with Broken Hill type stratiform Pb-Zn-Ag mineralisation: quartz-gahnite, garnet-quartz, quartz-garnet rocks, and BIF. Tourmaline-quartz rocks and garnet-epidote-amphibole calc-silicate rocks are associated with basic gneisses.||Unit in Purnamoota Subgroup.||Overlies Allendale Metasediments. Is overlain by Freyers Metasediments.|Extensive bodies of basic gneiss, lenticular masses of garnet-bearing quartzo-feldspathic gneiss, and "lode horizon" rocks, intercalated with pelitic to psammopelitic and psammitic metasediments.|
26096|Parnell Formation|70657|5|Briefly described|p12, p16, p30, p41, p58|Statherian|Statherian|Related in time to the ~1685 Ma felsic S-type magmatism in the Broken Hill Group. Also represented in the Olary Domain by differentiated sills of the Lady Louise Suite (e.g. Woman-in-White Amphibolite).|~1685 Ma.|||Equivalent to Lady Louise Suite.|A suite of mafic and felsic sills or flows; amphibolites.|
26096|Parnell Formation|72461|5|Briefly described|p13, p16-17|||Appears as Parnell Gneiss on p16. Potentially a volcanic sandstone prior to metamorphism. Petrographic Description is provided.||Broken Hill Group||Overlies the Allendale Metasediments. Overlain by the Freyers Metasediments.|Quartzo-feldspathic gneiss and amphibolite.|
26096|Parnell Formation|73512|6|Mentioned|p2|||||||||
26096|Parnell Formation|73524|6|Mentioned|p5 Fig.3|||||Broken Hill Group||||
26096|Parnell Formation|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p831 Fig.5, p839|Statherian|Statherian||<1693+/-4 Ma, 1682+/-9 Ma|Purnamoota Subgroup||Overlies Allendale Metasediments, underlies Freyers Metasediments||
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.|
40948|Patmore Limestone Member|50230|4|Described|Map legend|Emsian|Emsian|Of the Taemas Limestone.  Overlies the Receptaculites Limestone Member; underlies the Warroo Limestone Member.  Massive crinoidal limestone.||||||
40948|Patmore Limestone Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Taemas Limestone (Murrumbidgee Group). Massive crinoidal limestone.||||||18-JUN-08
40948|Patmore Limestone Member|68592|2|Defined|p982, p984 Fig.162, p985, p1028-30|Emsian|Emsian|New name, after Patmore homestead. Refers to rocks previously included in either Receptaculites Limestone Member or Warroo Limestone Member. Forms a prominent marker horizon. Type section described. 34-42m thick. Early Emsian age from confining units.||Unit in Taemas Limestone.||Conformably overlies Receptaculites Limestone Member. Is overlain conformably by Warroo Limestone Member.|Light grey, thin, discontinuously developed, massive, medium- to thick-bedded crinoidal limestone.|
40948|Patmore Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmtp. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Taemas Limestone||Overlies Receptaculites Limestone Member. Is overlain by Warroo Limestone Member.|Light grey, massive, medium-thick bedded crinoidal limestone.|
40948|Patmore Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Light grey, massive, medium-thick bedded crinoidal limestone.|
40948|Patmore Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Light grey, massive, medium-thick bedded crinoidal limestone.|
40948|Patmore Limestone Member|71656|6|Mentioned|p12 Fig.2|Emsian|Emsian|Shown only in correlation chart (Fig.2).||Probably of Taemas Limestone, Murrumbidgee Group||Overlies Receptaculites Limestone Member and underlies Waroo Limestone Member.|Fossiliferous limestone.|
27534|Patonga Claystone|22745|6|Mentioned|p130|||Sydney Basin.||||||
27534|Patonga Claystone|22749|6|Mentioned|p 195|||||||||
27534|Patonga Claystone|22833|6|Mentioned|p653|||of Sydney Basin.||||||
27534|Patonga Claystone|22857|4|Described|p520 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Narrabeen Group. Siltstone and claystone; minor sandstone. Max. thickness: 167m. Geological Province: Sydney Basin. See also p524 App.1 Tb.A1.9.||||||
27534|Patonga Claystone|22969|4|Described|Fig 4.1a||Early Triassic|||||||
27534|Patonga Claystone|24424|5|Briefly described|p538|Early Triassic|Early Triassic|Age: 235-245 Ma. Palaeomagnetic poles given. Geological Province: Sydney Basin.||||||
27534|Patonga Claystone|30007|6|Mentioned|Fig.1|||||||||
27534|Patonga Claystone|30565|6|Mentioned|p120|||||||||
27534|Patonga Claystone|31276|6|Mentioned|p148|||Palynology||||||
27534|Patonga Claystone|31297|6|Mentioned|p6|||||||||
27534|Patonga Claystone|31884|6|Mentioned|Table 1|||Triassic||||||
27534|Patonga Claystone|33683|4|Described|p79|||Narrabeen Gp.||||||
27534|Patonga Claystone|33685|6|Mentioned|Table 2|||||||||
27534|Patonga Claystone|33867|6|Mentioned|Table 1|||||||||
27534|Patonga Claystone|36042|6|Mentioned|Fig.22|||||||||
27534|Patonga Claystone|37804|6|Mentioned|Table 1|||||||||
27534|Patonga Claystone|37818|6|Mentioned|p82|||||||||
27534|Patonga Claystone|39287|6|Mentioned|Fig. 2.18|||||||||
27534|Patonga Claystone|39294|4|Described|p165|||||||||
27534|Patonga Claystone|39308|6|Mentioned|Fig. 23.12|||||||||
27534|Patonga Claystone|40263|6|Mentioned|Table 2|||||||||
27534|Patonga Claystone|40602|6|Mentioned|p15|||||||||
27534|Patonga Claystone|40625|6|Mentioned|Map legend|Early Triassic|Early Triassic|Early to Middle Triassic||||||
27534|Patonga Claystone|41010|6|Mentioned|Table 1|||||||||
27534|Patonga Claystone|42916|5|Briefly described|Table 1||Early Triassic|||||||
27534|Patonga Claystone|43194|5|Briefly described|p130|Triassic|Triassic|Fine grained red and green overbank sediments deposited in the northern Sydney Basin.||||||
27534|Patonga Claystone|43257|5|Briefly described|Map Legend||Early Triassic|Of Clifton Subgroup||||||13-JUN-13
27534|Patonga Claystone|43755|6|Mentioned|Fig.9,p556|||||||||
27534|Patonga Claystone|45090|6|Mentioned|p71|||Narrabeen Gp. relationships||||||
27534|Patonga Claystone|60299|6|Mentioned|p223|||Palaeopole position given.||||||
27534|Patonga Claystone|67028|6|Mentioned|p371 Tb. 5|Triassic|Triassic|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|245-251 Ma magnetic age range|||||10-AUG-15
27534|Patonga Claystone|67029|6|Mentioned|p383 Fig. 5|||Embleton & McElhinny, 1982. Used for comparison of poles of magnetic overprint in the Cretaceous.||||||24-APR-12
27534|Patonga Claystone|68003|5|Briefly described|p42.|Triassic|Triassic|Northern Sydney Basin. Deposition from SE-flowing streams.|||||Fine-grained red and green overbank sediments.|
27534|Patonga Claystone|70647|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Sydney Basin.||Clifton Subgroup|||Red-brown claystone and siltstone, light green-grey fine-grained sandstone.|
69900|Peach Tree Chert Member|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Abercrombie Formation. Varicoloured thin to medium-bedded chert interbedded with quartzose sandstone, siltstone and mudstone.||||||
69900|Peach Tree Chert Member|67322|5|Briefly described|p14, p17, p20 Fig.5|Darriwilian|Darriwilian|Named by Thomas, Pogson and Percival (in Thomas et al. in press) contains early to mid Darriwilian conodonts (Percival and Zhen 2007). Occurs north of Goulburn.||Of the Abercrombie Formation||||22-FEB-18
69900|Peach Tree Chert Member|68466|6|Mentioned|p65, 68|Middle Ordovician|Middle Ordovician|Albury-Bega Terrane. Occurs N of Goulburn. Conodonts indicate mid-Darriwilian age.||Abercrombie Formation.||||
69900|Peach Tree Chert Member|68592|2|Defined|p278, p282-4, p291, p296-7, p309-12,p316|Middle Ordovician|Middle Ordovician|See also p118, p272, p274-5, p1861. New name, after Peach Tree Waterhole (Abercrombie River). Formerly (Murray and Stewart, 2001) included in Numeralla Chert, which is the equivalent of the younger Nattery Chert Member. Type area described. Thickness to 20m, usually <10m. Conodont fauna detailed.||Unit in Abercrombie Formation.|||Numerous honey-coloured, brown and dark grey chert bands up to 30cm thick in a sequence of interbedded to interlaminated siltstone and mudstone, commonly cherty, and fine- to medium-grained sandstone.|
69900|Peach Tree Chert Member|69159|5|Briefly described|Map legend|Darriwilian|Darriwilian|||Unit in Abercrombie Formation.|||Dark grey, honey-coloured and brown, thin- to medium-bedded, chert interbedded with quartzose sandstone, siltstone and mudstone.|07-SEP-15
69900|Peach Tree Chert Member|69668|6|Mentioned|p929 Fig.2, p930 Fig.3, p931|Middle Ordovician|Middle Ordovician|Thomas and Pogson (2012). Goulburn-Braidwood area, Albury-Bega terrane. Contains early- to middle-Darriwilian conodonts.||Unit in Abercrombie Formation.||||
69900|Peach Tree Chert Member|70192|5|Briefly described|Map Legend|Darriwilian|Darriwilian|[Theta]aap. On Taralga, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Abercrombie Formation||Within undifferentiated Abercrombie Formation.|Thin-medium bedded chert and cherty mudstone, interbedded with siltstone, mudstone and fine to medium grained quartzose sandstone.|
69900|Peach Tree Chert Member|70541|4|Described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Honey-coloured, brown to grey, thin to medium bedded chert and cherty mudstone, interbedded with siltstone, mudstone and fine to medium grained quartzose sandstone.|
69900|Peach Tree Chert Member|70542|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Honey coloured, brown to grey, thin to medium bedded chert and cherty mudstone, interbedded with siltstone, mudstone and fine-medium grained quartzose sandstone.|
69900|Peach Tree Chert Member|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Thin-medium bedded chert and cherty mudstone, interbedded with siltstone, mudstone and fine to medium grained quartzose sandstone.|
69900|Peach Tree Chert Member|71069|6|Mentioned|p21, p52, p53 fig 19, p55 fig 20|Middle Ordovician|Early Ordovician|Contains conodont fossils (Pygodus anitae, Periodon macro-dentata and Histiodella sp.) See also  p58-p60, p62, p68, p76 fig 27.||Abercrombie Formation||||
69900|Peach Tree Chert Member|71656|5|Briefly described|p13 Fig.2, p13-14|Darriwilian|Darriwilian|Taralga area. Many conodonts varieties are evident in this member.||Abercrombie Formation, Adaminaby Group||Adaminaby Group.|Fossiliferous chert.|
69900|Peach Tree Chert Member|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|||Abercrombie Formation.|||Dark grey, honey-coloured and brown, thin- to medium-bedded chert interbedded with quartzose sandstone, siltstone and mudstone.|
69900|Peach Tree Chert Member|71700|4|Described|vi, p8, p43, p56, CD|Darriwilian|Darriwilian|Albury-Bega Terrane. A type section is defined in Thomas and Pogson (2012).||Abercrombie Formation||Overlain by the Nattery Chert Member. Overlies the Mummel Chert Member.|Chert.|
69900|Peach Tree Chert Member|71889|6|Mentioned|p12|Darriwilian|Darriwilian|||||||
69900|Peach Tree Chert Member|73140|6|Mentioned|p495 Fig.1, Fig.3|Darriwilian|Darriwilian|Age based on conodonts.||Abercrombie Formation||||
80106|Peak Rhyolite|70941|6|Mentioned|p78, p78 fig 32, p152|Ludlow|Ludlow|Rhyolite within the Chesney Formation, Cobar Supergroup.|423.2 +/- 3.5 Ma (Black, 2007) SHRIMP age.|Chesney Formation?||Intrudes the Chesney Formation.||25-SEP-17
80106|Peak Rhyolite|72958|6|Mentioned|p5, p38, p60|Lochkovian|Ludlow|Syn-rift phase volcanic unit of the Nurri Group.|418.1 +/- 3.0 Ma|Nurri Group||Equivalent to Stones Tank Tuff Member.|Rhyolite domes/flows.|
80106|Peak Rhyolite|73174|5|Briefly described|p1038-1039|Lochkovian|Gorstian[?]|Uncertain whether it is intrusive or extrusive due to discordant contact; generally considered extrusive. Geochron are magmatic ages from Black (2005) and Bodorkos et al. (2013).|423.2 +/- 3.5 Ma, 418.1 +/- 3.0 Ma SHRIMP||||Relatively unaltered, flow-banded, amygdaloidal rhyolite.|
31703|Peaks Formation|22857|5|Briefly described|p490 App.1 Tb.A1.7|Devonian|Devonian|Of the Hervey Group. Red shale, mudstone and siltstone; white to pink-red-brown arenite; conglomerate lenses. Max. thickness: 128m. Geological Province: Hervey Basin.||||||
31703|Peaks Formation|23214|3|Fully described|p227|Late Devonian|Late Devonian|Of the Hervey Group. Previously Peaks Sandstone. 128m thick at type section. Geological Province: Hervey Basin. Overlying unit: Hunter Formation, Underlying unit: Canowindra Volcanics.||||||28-FEB-07
31703|Peaks Formation|23217|6|Mentioned|p6|||On GRENFELL 1:100,000 sheet.||||||08-MAR-06
31703|Peaks Formation|23392|2|Defined|p3|Frasnian|Givetian|Fossil assemblage includes placoderm fish and plant remains. Broad correlation with Kadina and Clagger Fms (Parkes 1:100 000) and Mandagery Formation. Max Thickness: 860m||||||
31703|Peaks Formation|24417|3|Fully described|p126|Middle Devonian|Middle Devonian|Of Hervey Group.  Supersedes "Peaks Sandstone" and "Bogan Gate Sandstone".  Max. thickness: 860m.||||||
31703|Peaks Formation|43782|5|Briefly described|Map Legend|Frasnian|Frasnian|of Hervey Group.||||||
31703|Peaks Formation|60009|5|Briefly described|Map Legend|Frasnian|Frasnian|Of the Hervey Group.  Includes: Mogongong Conglomerate Member. Underlies: Hunter Formation.||||||13-JUL-04
31703|Peaks Formation|68592|5|Briefly described|p1707|||In the Forbes 1:250 000 map area.||Basal unit in Hervey Group.||Is correlated with Bendick Formation.||
31703|Peaks Formation|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Hervey Group||||
32399|Peakview Tonalite|22815|4|Described|p87|||||||||
32399|Peakview Tonalite|43233|5|Briefly described|Map Legend|Devonian|Silurian|Unassigned pluton, Bega Batholith.||||||
36962|Pee Dee beds|22857|5|Briefly described|p516 App.1 Tb.A1.8|Permian||Slaty siltstone, lithic sandstone, minor diamictite.||||||
36962|Pee Dee beds|23720|5|Briefly described|Map Legend|||Of Nambucca beds.  Slaty siltstone, lithic sandstone, minor diamictite.||||||15-DEC-04
36962|Pee Dee beds|44450|5|Briefly described|p20|||Of Nambucca beds. Geological Province: Nambucca Block.||||||24-AUG-05
36962|Pee Dee beds|69188|5|Briefly described|p22|Permian|Late Carboniferous|||Nambucca beds.||||
36962|Pee Dee beds|71628|5|Briefly described|p17: 20, 42|||Nambucca Block.||||Is intruded by Carrai Granodiorite and Yarrahapinni Monzogranite.||
24619|Peera Peera Formation|13497|5|Briefly described|p65, p114|||Simpson Basin. Up to 190m thick.||||Equivalent to the Cuddapan Formation.||
24619|Peera Peera Formation|22839|6|Mentioned|P33|||Lateral equivalent of the Cuddapan Formation||||||
24619|Peera Peera Formation|22857|5|Briefly described|p310|Late Triassic|Late Triassic|Geological Province: Eromanga Basin.||||||
24619|Peera Peera Formation|22865|6|Mentioned|p310||Late Triassic|||||||
24619|Peera Peera Formation|22883|5|Briefly described|P31, Fig2||Late Triassic|Correlated to the Cuddapan Formation, underlying unit is Walkandi Formation.||||||16-SEP-08
24619|Peera Peera Formation|24204|5|Briefly described|p262, 263 Fig.4|Late Triassic|Late Triassic|Shale, coal, sandstone. Overlies Walkandi Formation (unconformable). Geological Province: Simpson Basin.||||||
24619|Peera Peera Formation|36922|6|Mentioned|Fig.3|||Note with Fig.4 states name should be P.P.beds. Misspelling of Peera Perra?||||||
24619|Peera Peera Formation|36941|6|Mentioned|Table 1|||||||||
24619|Peera Peera Formation|37287|6|Mentioned|p36|||||||||
24619|Peera Peera Formation|37776|6|Mentioned|Fig.2|||||||||
24619|Peera Peera Formation|38108|6|Mentioned|Table 1|||Misspelling of Peera Perra?||||||
24619|Peera Peera Formation|41063|2|Defined|p45|Late Triassic|Late Triassic|||||||
24619|Peera Peera Formation|41099|6|Mentioned|Fig.9|||||||||
24619|Peera Peera Formation|41176|6|Mentioned|p206|||||||||
24619|Peera Peera Formation|41183|6|Mentioned|p310|||||||||
24619|Peera Peera Formation|42008|5|Briefly described|p265,266, 267, 268, 275|Late Triassic|Late Triassic|Simpson Desert Basin. Correlated with Cuddapan Formation. Also shown as Peera Perra Formation on p266.||||||09-APR-15
24619|Peera Peera Formation|42062|5|Briefly described|p27|||||||||
24619|Peera Peera Formation|42463|6|Mentioned|Fig.4 P171|||||||||
24619|Peera Peera Formation|42746|4|Described|p6, Fig.2 p4|||||||||
24619|Peera Peera Formation|43052|5|Briefly described|Table 2.1|||||||||
24619|Peera Peera Formation|44133|5|Briefly described|p94|Late Triassic|Late Triassic|Conformably overlies: Walkandi Formation. Maximum Thickness: 190m. ||||||
24619|Peera Peera Formation|62376|5|Briefly described|p84|Late Triassic|Middle Triassic|Geological Province: Pedirka Basin.||||||09-FEB-10
24619|Peera Peera Formation|63979|6|Mentioned|p31|||Geological province: Simpson Basin. Correlate of Cuddapan Formation.||||||07-FEB-11
24619|Peera Peera Formation|64778|6|Mentioned|p13, 28|Triassic|Triassic|Simpson Desert Basin. Potential hydrocarbon source.||||||
24619|Peera Peera Formation|65238|5|Briefly described|p7 Fig. 8, p9|Late Triassic|Middle Triassic|Unconformably overlies Walkandi Formation. Max. thickness: 200m. Geological province: Simpson Desert Basin. Lacustrine, low energy, meandering deposits comprising thick, broadly upward-fining succession. Very detailed lithology included. See also p10.||||||
24619|Peera Peera Formation|65489|5|Briefly described|p53, p55-63, p137, p149-151|Late Triassic|Middle Triassic|Simpson Basin. 190m thick. Hydrocarbon source rock; hosts oil show and gas indication. Poor quality reservoirs; intrafomational siltstone and shale form seals.||||Conformably overlies Walkandi Formation. Correlated with Cuddapan Formation (Cooper Basin). Probably correlates with Tinchoo Formation.|Basal grey shale and siltstone with minor thin sandstone and coal, a fining upward sandy middle unit, and black highly carbonaceous silty shale at the top.|
24619|Peera Peera Formation|69454|5|Briefly described|p38:3-4, 8-13, 14 Fig.38.9|Rhaetian|Carnian|Pedirka Basin (subsurface only). 190m thick in Walkandi-1. Meandering fluvial, lacustrine/paludal deposits. May be equivalent to uppermost part of the Tinchoo Formation. Hosts minor coal resources with fair to good mixed oil-gas source potential. Sandstones have fair to good reservoir potential, with intra-formational shale seals.||||Overlies Purni Formation unconformably, and Walkandi Formation disconformably or unconformably. Is overlain unconformably by Poolowanna Formation. Correlated with Cuddapan Formation (Eromanga Basin).|Shale, siltstone, minor coal and sandstone at base, overlain by cyclical upward-fining sandstone, capped by highly carbonaceous shale with occasional thin sandstone beds.|12-JUL-16
24619|Peera Peera Formation|69457|6|Mentioned|p41:5 Fig.41.4; 41:16|Triassic|Triassic|Fair to good source rocks.||||||12-JUL-16
24619|Peera Peera Formation|69673|5|Briefly described|p152, 159, 160, 161, 149|Triassic|Triassic|190m thick. Source rock potential.||||Unconformably overlies Purni Formation, unconformably overlain by Poolowanna Formation|Shale, siltstone, minor sandstone and coal. Black silty and highly carbonaceous shale with occasional thin sandstone interbeds.|21-SEP-17
24619|Peera Peera Formation|69946|4|Described|p8-9, p36, p51-52|Late Triassic|Late Triassic|Defined by Moore (1986); previously Peera Peera beds of Wiltshire (1978). Type section is the interval 2593 - 2768m in Poolowanna 1. Up to 190m thick. Simpson Basin.||||Conformably overlies Walkandi Formation. Correlated with Cuddapan Formation.|Lowermost (of three) units is siltstone and shale with minor thin sandstone and rare coal; then upward-fining sandstone cycles; topped by black carbonaceous shale, coal and thin sandstone interbeds.|
24619|Peera Peera Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Walkandi Formation conformably and Purni Formation unconformably. Is overlain unconformably by Poolowanna Formation.||
24619|Peera Peera Formation|71321|6|Mentioned|p15|||Of Simpson Basin.||||Overlies the Walkandi Formation. Overlain by the Poolowanna Formation.||24-OCT-19
24619|Peera Peera Formation|71342|4|Described|Ch4 p25, Ch5 p8-p9|Triassic|Triassic|Simpson Basin. Originally the informal Peera Peera beds of Wiltshire (1978) before being defined by Moore (1986). A type section in Poolowanna 1 is mentioned. This unit was subdivided into three facies by Moore in 1986. A maximum thickness of 190m is recorded in Walkandi 1. Deposited in a high-sinuosity fluvial environment. See also Ch5 p30, Ch5 p36, Ch5 p51-p52, Ch9 p18, Ch11 p6, Ch12 p2-p3, Ch12 tbl 12.1, Ch12 p6, Ch12 p10-p14, Ch14 p4-p7.||||Conformably overlies the Walkandi Formation. Overlain by the Poolowanna Formation.|Siltstone and shale, minor thin sandstone and rare coal. Black carbonaceous shale, coal and thin sandstone interbeds also occurs.|
24619|Peera Peera Formation|72476|6|Mentioned|p36 Fig.9, p37|Triassic|Triassic|Simpson Basin. Time-temperature thermal history diagram. Only 200m thickness preserved.||||||
24619|Peera Peera Formation|73281|6|Mentioned|p1, Appendix (DIP)|Triassic|Triassic|Pedirka Basin. Petroleum source rocks. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
35787|Pejar Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Part of the Wologorong Batholith.  Cream biotite leucogranite with porphyritic plagioclase phenocrysts.||||||12-MAY-04
28916|Pelton Coal Member|22610|5|Briefly described|Fig 1, 5|||||||||
28916|Pelton Coal Member|23540|5|Briefly described|p 420|||||||||
28916|Pelton Coal Member|37086|6|Mentioned|p188|||||||||
28916|Pelton Coal Member|45090|5|Briefly described|p152|||||||||
28916|Pelton Coal Member|60297|5|Briefly described|p177|Permian|Permian|Of the Greta Coal Measures.||||||
26099|Pendergast Tonalite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
26099|Pendergast Tonalite|35109|2|Defined|p78|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
26099|Pendergast Tonalite|35263|6|Mentioned|Table 3|||||||||
26099|Pendergast Tonalite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
26099|Pendergast Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
26099|Pendergast Tonalite|40328|4|Described|p210|||||||||
26099|Pendergast Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh16||||||
26099|Pendergast Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
73374|Pendianna Tank Granite|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Westella Suite.|||Grey, medium-grained biotite granite with sparse biotite-rich enclaves.|
73374|Pendianna Tank Granite|70941|3|Fully described|pviii, pix, p9, p58 fig 23, p71, p73|Early Devonian|Late Silurian|Named for Pendianna Tank. Previously an informal name. Outcrops as low pavements and tors. Type locality mentioned.  Distribution, metamorphism, geochemistry, geophysical characteristics and distinguishing characteristics discussed. I type granite containing mafic enclaves. Intrudes Girilambone Group basement. Age inferred from similarities to the Byrock Granite. Has contact metamorphosed the Girilambone Group.  See also  p74, p75, p131, p140, p145.||Westella Suite||Equivalent to the Byrok Granite. Intrudes the Girilambone Group.|Grey granite composed of quartz, plagioclase, K-feldspar and biotite. Grains are roughly 2mm wide. Biotite shows radiation haloes. Possible amphibole occurs along with apatite, zircon and trace opaques. Sporadic mafic enclaves occur.|
73374|Pendianna Tank Granite|71345|6|Mentioned|p30|||||||||
73374|Pendianna Tank Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: very small non-magnetic unit with boundary based on geological mapping. Minor radioelement high.||Westella Suite.|||Medium-grained biotite granite with sparse biotite clumps. I-type.|
39262|Penryn Rhyolite Member|50613|2|Defined|p211, p228-229 App. 1|Namurian|Namurian|Of the Willuri Formation. Basal member of theTulcumba package (informal grouping of stratigraphically recognisable distinctive, mappable units) overlying the Piney Range package; underlies Birken Head Volcanic Member. Max. thickness: 50m;10m in type sect.||||||22-FEB-05
26840|Peri Rhyodacite Tuff Member|721|5|Briefly described|Map legend|Namurian|Namurian|of the Clifden Formation.  Rhyodacitic vitric tuff.  Geological Province: Tamworth Belt.||||||21-DEC-04
26840|Peri Rhyodacite Tuff Member|22857|4|Described|p506 App.1 Tb.A1.8|Late Carboniferous|Late Carboniferous|Of the Clifden Formation. Rhyodacitic vitric tuff. Max. thickness: 10m. ||||||
26840|Peri Rhyodacite Tuff Member|30135|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|Part of Clifden Formation||||||
26840|Peri Rhyodacite Tuff Member|43091|5|Briefly described|Map legend|||||||||
26840|Peri Rhyodacite Tuff Member|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||22-MAR-05
76989|Pericoe Monzogranite|69801|6|Mentioned|p129|||Eastern Lachlan Orogen.||Kameruka Supersuite||||
32184|Pericoe Suite|22815|6|Mentioned|p70|||||||||
32184|Pericoe Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
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.||||||
25393|Petroi Metabasalt|40258|2|Defined|p261|Early Permian|Early Permian|Underlying rocks include Early Permian fossils.||||||
25393|Petroi Metabasalt|41234|6|Mentioned|p33|||||||||
25393|Petroi Metabasalt|42480|5|Briefly described|p549, p5610|||Nambucca Slate Belt||||||
25393|Petroi Metabasalt|61772|6|Mentioned|p128||Early Permian|In New England Orogen.||||||24-SEP-08
25393|Petroi Metabasalt|71628|6|Mentioned|p17:18|||||||||
26100|Pheasants Nest Formation|22433|6|Mentioned|p12 Table 1|||in the Sydney Basin||||||
26100|Pheasants Nest Formation|22488|5|Briefly described|p841-2|||||||||
26100|Pheasants Nest Formation|22578|5|Briefly described|p394, Fig.6 p396|||of Illawarra Coal Measures||||||
26100|Pheasants Nest Formation|22857|4|Described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Cumberland Subgroup (Illawarra Coal Measures). Contains the Unanderra and Figtree coal seams. Interbedded lithic sandstone, coal, carbonaceous claystone, siltstone and claystone. Max. thickness: 75m. Geological Province: Sydney Basin.||||||
26100|Pheasants Nest Formation|22969|4|Described|p 25, Fig 3.1|||Lachlan Fold Belt.||||||
26100|Pheasants Nest Formation|23442|5|Briefly described|p168|||Sydney Basin||||||
26100|Pheasants Nest Formation|23544|5|Briefly described|Fig 2 p358|||In the Cumberland Subgroup||||||
26100|Pheasants Nest Formation|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Of the Illawarra Coal Measures.||||||
26100|Pheasants Nest Formation|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Cumberland Subgroup. Geological Province: Sydney Basin.||||||
26100|Pheasants Nest Formation|24471|5|Briefly described|p30|Late Permian|Late Permian|Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Wallis Creek Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
26100|Pheasants Nest Formation|29900|4|Described|p175|||||||||
26100|Pheasants Nest Formation|29901|5|Briefly described|p169|||||||||
26100|Pheasants Nest Formation|29944|6|Mentioned|Fig.18|||||||||
26100|Pheasants Nest Formation|30006|4|Described|p7|||Permian||||||
26100|Pheasants Nest Formation|31128|6|Mentioned|p7|||||||||
26100|Pheasants Nest Formation|31887|5|Briefly described|p5|||||||||
26100|Pheasants Nest Formation|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
26100|Pheasants Nest Formation|32849|6|Mentioned|Table 1|||Permian||||||
26100|Pheasants Nest Formation|34569|6|Mentioned|p9|||Permian. See Fig.2||||||
26100|Pheasants Nest Formation|34605|3|Fully described|p372|||See also P374||||||
26100|Pheasants Nest Formation|35189|6|Mentioned|p385|||||||||
26100|Pheasants Nest Formation|36042|6|Mentioned|p20|||||||||
26100|Pheasants Nest Formation|36220|3|Fully described|p40|||See also Table 10 & P38.||||||
26100|Pheasants Nest Formation|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
26100|Pheasants Nest Formation|37089|6|Mentioned|p208|||||||||
26100|Pheasants Nest Formation|38615|6|Mentioned|p22|||||||||
26100|Pheasants Nest Formation|38690|4|Described|p293|||||||||
26100|Pheasants Nest Formation|39287|6|Mentioned|p20|||See also Fig.2.13||||||
26100|Pheasants Nest Formation|39308|5|Briefly described|p514|||||||||
26100|Pheasants Nest Formation|39309|4|Described|p121|||See also Table 7.2||||||
26100|Pheasants Nest Formation|39661|6|Mentioned|p443|||||||||
26100|Pheasants Nest Formation|40256|6|Mentioned|p306|||||||||
26100|Pheasants Nest Formation|41857|6|Mentioned|p392|||||||||
26100|Pheasants Nest Formation|42737|5|Briefly described|map legend|Permian||||||||
26100|Pheasants Nest Formation|42787|5|Briefly described|p129|||||||||
26100|Pheasants Nest Formation|42896|2|Defined|p16, Table 2|Late Permian|Middle Permian|Of Cumberland Subgroup.||||||12-MAR-09
26100|Pheasants Nest Formation|42925|5|Briefly described|Table 18||Late Permian|||||||
26100|Pheasants Nest Formation|43194|5|Briefly described|p108|Late Permian|Late Permian|Correlated with the basal (coal bearing) lithic unit in the Black Jack Formation (now named Pamboola Formation) in the Gunnedah Basin.||||||
26100|Pheasants Nest Formation|45090|6|Mentioned|p27|||||||||
26100|Pheasants Nest Formation|60281|5|Briefly described|p62-63|Late Permian|Late Permian|At base of the Illawarra Coal Measures.  Coarse sandstone at the base grading to siltstone and coal at the top. Overlies Budgong Sandstone. Geological Province: Sydney Basin. See also p60.||||||27-APR-05
26100|Pheasants Nest Formation|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Cumberland Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
26100|Pheasants Nest Formation|61609|6|Mentioned|p240 Tb. 1, p246 Fig. 5|Permian|Permian|Of Cumberland Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
26100|Pheasants Nest Formation|63832|5|Briefly described|p136|Guadalupian|Guadalupian|Southern Sydney Basin. Shows no dispersed gravel or other glacial indicators, suggesting a brief interglacial interval in the mid-Permian.||Unit in Illawarra Coal Measures.||||13-DEC-17
26100|Pheasants Nest Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Is overlain by Erins Vale Formation.||
26100|Pheasants Nest Formation|67500|6|Mentioned|p12 Tb.1|||||Of the Illawarra Coal Measures.|Includes Berkeley, Minnamurra, Calderwood, and Five Islands, Latite Members.|||02-MAY-12
26100|Pheasants Nest Formation|67663|6|Mentioned|p518|Triassic|Permian|Late Permian. Interbedded with 4 latite flows of Gerringong Volcanics.||Of the Illawarra Coal Measures.||||
26100|Pheasants Nest Formation|68592|5|Briefly described|p1781|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Shoalhaven Group conformably (transitionally).|Thinly interbedded sandstone and siltstone with carbonaceous partings which contain no marine fauna and which pass upwards to coal-bearing strata.|
26100|Pheasants Nest Formation|69297|6|Mentioned|p502 fig 5.43|||Sydney Basin. ||||Unconformably overlain by the Newcastle Coal Measures.||
26100|Pheasants Nest Formation|71115|5|Briefly described|p180, 182|Permian|Permian|Southern Sydney Basin.||Cumberland Subgroup.|Unanderra, Fig Tree, Coal Members; Five Islands, Calderwood, Minnamurra, Berkeley, Latite Members.|Overlies Broughton Formation.||
26100|Pheasants Nest Formation|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
26100|Pheasants Nest Formation|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.||Cumberland Subgroup.||Overlies Broughton Formation.||
26100|Pheasants Nest Formation|73625|6|Mentioned|p2|Permian|Permian|Southern coalfield, Sydney Basin.||Illawarra Coal Measures.||Overlies Broughton Formation. Is overlain by Erins Vale Formation.||
72762|Phils Creek Formation|61910|5|Briefly described|p152|Late Ordovician|Late Ordovician|Deep marine turbiditic sequence of fine-grained sediments and shales. Geological Province: Lachlan Fold Belt.||||||
34937|Phosphate Mine beds|22952|6|Mentioned|Table1p179|||||||||
23902|Pi Pi Ignimbrite|22857|5|Briefly described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|||||||
23902|Pi Pi Ignimbrite|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Coombadjha Volcanic Complex.  Black densely welded dacitic ignimbrite, with generally less than 25% crystal fragments (predominantly plagioclase) with well-developed foliation of platy, grey, relict pumice fragments.||||||20-DEC-04
23902|Pi Pi Ignimbrite|23812|5|Briefly described|p29 Tb.3|Late Permian|Early Permian|Of Coombadjha Volcanic Complex.  Maximum thickness: 320m.||||||
23902|Pi Pi Ignimbrite|23859|5|Briefly described|p937|||Of Coombadjha Volcanic Complex. Geological Province: New England Fold Belt.||||||
23902|Pi Pi Ignimbrite|41041|3|Fully described|p263|||||||||
23902|Pi Pi Ignimbrite|42378|5|Briefly described|Table 1 P6|||Coombadjha Volcanic Complex.||||||
23902|Pi Pi Ignimbrite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Coombadjha Volcanic Complex.||||||20-JUL-04
23902|Pi Pi Ignimbrite|71628|5|Briefly described|p15:5; p19: 72, 128|||||Wandsworth Volcanic Group.||Is intruded by Billyrimba Leucomonzogranite. Is faulted against Grasstree Quartz Monzodiorite. Is bounded by Moonta Gully Monzogranite.||
30646|Piambong Formation|22529|5|Briefly described|p1|||||||||
30646|Piambong Formation|22590|6|Mentioned|Fig3 P754||Pridoli|||||||
30646|Piambong Formation|22857|4|Described|p470 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Chesleigh Group. Volcanic and quartzose arenite and siltstone, rhyolitic and felsic breccia, vitric tuff, latite, quartz latite. Max. thickness: 750m. Geological Province: Hill End Trough.||||||
30646|Piambong Formation|23043|5|Briefly described|Map Legend|Lochkovian|Ludlow|of Chesleigh Group.||||||
30646|Piambong Formation|23170|2|Defined|p75|Early Devonian|Late Silurian|of Chesleigh Group.||||||
30646|Piambong Formation|24394|5|Briefly described|p170|Pridoli|Pridoli|Of Chesleigh Formation.  Referred to by Packham et al (2001) as the "tuffaceous unit of the Chesliegh Formation".||||||
30646|Piambong Formation|50124|5|Briefly described|p126, p130|Late Silurian|Late Silurian|Now includes felsic volcaniclastic rocks of the upper Chesleigh Formation (Colquhoun et al. 1999b). Geological Province: eastern Lachlan Fold Belt.||||||
30646|Piambong Formation|68003|5|Briefly described|p24 Fig.3-e, p146. |Pridoli|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Upper unit in Chesleigh Group.||Overlies Biraganbil Formation.|Rhyolitic, felsitic and latitic volcaniclastic and quartz lithic sandstone, siltstone, breccia; crystal and vitric tuff, minor lava.|
30646|Piambong Formation|68004|5|Briefly described|p119.|Late Silurian|Middle Silurian|Hosts known Kuroko VHMS occurrences. Has high potential and a certainty level of C.||||||
30646|Piambong Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Chesleigh Group||||
30646|Piambong Formation|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4|Early Devonian|Late Silurian|Hill End Trough. Locations in text include p1102 Fig.8. [Map symbol suggests Silurian age]||||Overlies the Biraganbil Formation, underlies the Cookman Formation, Turondale Formation.||
23904|Pigeon Square Gabbro|40328|4|Described|p210|||||||||
29629|Pigna Barney Ophiolitic Complex|42997|5|Briefly described|p36|||||||||
29629|Pigna Barney Ophiolitic Complex|69601|5|Briefly described|p403, p405-406, p408-409|||Cross (1983). New England Orogen. Spatially associated with the Pola Fogal (Hornblendite-Tonalite) Suite; geochronological results suggest a related geological history with that unit. Probable island-arc source.|||||Strongly deformed, serpentinised ultramafic and mafic igneous rocks; also contains blueschists, amphibolites, greenschists, basaltic to silicic volcanics, sedimentary rocks, and blocks of tectonically disrupted granites from the Pola Fogal Suite.|
27536|Pilleuil Andesite|22768|6|Mentioned|p178|||||||||
27536|Pilleuil Andesite|22857|5|Briefly described|p178, p458 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Black Range Group. Massive andesite flows. Geological Province: Canberra-Yass Shelf.||||||10-MAR-06
27536|Pilleuil Andesite|30069|6|Mentioned|p7|||||||||
27536|Pilleuil Andesite|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Strat. Nomenclature. Black Ra. Gp.||||||
27536|Pilleuil Andesite|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27536|Pilleuil Andesite|35386|4|Described|p46|||||||||
27536|Pilleuil Andesite|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
27536|Pilleuil Andesite|37727|6|Mentioned|p40|||||||||
27536|Pilleuil Andesite|40882|6|Mentioned|p27|||||||||
27536|Pilleuil Andesite|45147|6|Mentioned|M178|||||||||
27536|Pilleuil Andesite|50230|5|Briefly described|Map legend|Lochkovian|Lochkovian|Of the Black Range Group. Overlies the Sharpeningstone Conglomerate. Andesite lava and tuff.||||||17-JUN-08
27536|Pilleuil Andesite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Black Range Group. Andesite lava and tuff.||||||17-JUN-08
27536|Pilleuil Andesite|68592|2|Defined|p81, p430 Fig.89, p926-35, p943-7|Lochkovian|Lochkovian|Link (1970, 1971); Link and Druce (1972); unit in their Bowning Group. Formally published and described by Cramsie et al. (1975, 1978) who placed it in the Black Range Group. Named after the homestead and porperty of Pilleuil (no longer current), 500m S of Bowning. Forms undulating to hilly country. A suitable type section is proposed and described here, although the top of the unit is not preserved. Over 380m thick. Geochemistry detailed; geophysical properties described. Close geochemical/genetic association with Boggy Plain Supersuite. A SHRIMP U-Pb zircon age of 419.7 +/- 3.1 Ma (Black, 2005) is considered too old and due to inherited zircons.||Unit in Black Range Group.||Overlies Sharpeningstone Conglomerate disconformably, and Hattons Corner Group unconformably. Is intruded by Waynes Knob Rhyolite. Equivalent to Rolling Grounds Latite and Mountain Creek Volcanics.|Blue-grey, massive, fine-grained, feldspar- and pyroxene-phyric andesite lavas; outcrops are commonly highly jointed and often deeply weathered. Rare thin lenses of fine-grained, grey, massive volcanic-rich sandstone occur throughout. I-type.|
27536|Pilleuil Andesite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dbp. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Black Range Group||Unconformably overlies Sharpeningstone Conglomerate. Is overlain by Waynes Knob Rhyolite.|Fine grained, massive feldspar and pyroxene-phyric andesite; rare thin lenses of fine grained, massive, volcaniclastic sandstone.|
27536|Pilleuil Andesite|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Blue-grey, fine-grained, massive feldspar- and pyroxene-phyric andesite; rare thin lenses of fine-grained, massive, volcaniclastic sandstone.|29-AUG-16
27536|Pilleuil Andesite|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Fine grained, massive, feldspar and pyroxene-phyric andesite; rare thin lenses of grey, fine grained, massive, volcaniclastic sandstone.|
27536|Pilleuil Andesite|73215|5|Briefly described|p994|||Yass Syncline.||Black Range Group.||Overlies Hattons Corner Group.||
82557|Pilot Coal, Lower|73304|6|Mentioned|p75|||Below the Mount Hutton Tuff. Above the Hartley Hill Coal.||Boolaroo Formation, Newcastle Coal Measures||||
82556|Pilot Coal, Upper|73304|6|Mentioned|p65, p75|||||Boolaroo Formation, Newcastle Coal Measures||||
73404|Pimbilla Tank Group|66623|2|Defined|p16, pp152-159. |Ordovician|Cambrian|Defined in this study. Contemporaneous in part with, and an offshore equivalent of, the upper Mutawintji Group. Diverse marine macrofauna and conodont microfauna, which have been subject to minimal post-lithification burial and stress. Thickness in excess of 454 m. Has large secondary folds due to Silurian deformation.|||Includes Yandaminta Quartzite, Tabita and Pingbilly Formations.|Fault-bound against Gnalta Group.|Grey-green mudstone; white quartzite; limestone, primarily coquinaite, interbedded silty shale and siltstone; very minor thin limestone beds; micaceous mudstone with fine-grained subangular quartz grains, sporadic interbeds of siltstone.|
73404|Pimbilla Tank Group|66917|5|Briefly described|Map legend|Early Ordovician|Early Ordovician||||Includes Yandaminta Quartzite, Tabita and Pingbilly Formations.||Folded and weakly cleaved metasedimentary rocks, dominantly mudstone with minor sandstone, fossiliferous limestone, quartzite and basal pebbly conglomerate. Regionally metamorphosed to prehnite-pumpellyite facies.|
73404|Pimbilla Tank Group|67208|5|Briefly described|Map legend.|Ordovician|Ordovician||||Includes Yandaminta Quartzite, Tabita and Pingbilly Formations.||Folded and weakly cleaved metasedimentary rocks; dominantly mudstone with minor sandstone, fossiliferous limestone, quartzite and basal pebbly conglomerate; regionally metamorphosed to prehnite-pumpellyite facies.|
73404|Pimbilla Tank Group|67322|5|Briefly described|p10; Fig.5|Floian|Floian|Koonenberry Belt. Defined by Percival, in Greenfield et al. (2010). Represents post Delamarian Orogeny rock units that correlate with the Mutawintji Group. Occurs in the Mount Arrowsmith region.|||Tabita Formation, Yandaminta Quartzite, Pingbilly Formation.|Unconformably overlies or is faulted against Wyarra Shale. Correlates with Mutawintji Group.||22-FEB-18
73404|Pimbilla Tank Group|70749|6|Mentioned|p43|Ordovician|Cambrian|Southern Thomson and Koonenberry area.||||||
73404|Pimbilla Tank Group|71284|6|Mentioned|p488|Floian|Floian|Mount Arrowsmith area, far western Koonenberry Belt.||||||
73404|Pimbilla Tank Group|71966|6|Mentioned|p990|Ordovician|Cambrian|Geological province: southern Thomson Orogen.||||||
73404|Pimbilla Tank Group|73567|6|Mentioned|p68|Ordovician|Ordovician|Gnalta Shelf.||||||
73420|Pimpara Member|66917|5|Briefly described|Map legend|Cambrian|Cambrian|Separates the lower and upper units of upward-coarsening red-brown flaggy sandstone and conglomerate of the Wydjah Formation.||Unit in Wydjah Formation.|||Boldly outcropping impure dolomite interbedded with recessive blue-grey shale and siltstone.|
40891|Pincally Formation|12066|5|Briefly described|p13|Middle Cambrian|Middle Cambrian|Of Gnalta Group. Conformably overlain by the Wydjah Formation.||||||
40891|Pincally Formation|22857|5|Briefly described|p90 Fig. 14.7B|||Geological Province: Bancannia Block in the Adelaide Fold Belt||||||
40891|Pincally Formation|62787|4|Described|p77, p76 Fig. 1, p79, p80, p81, p82|Middle Cambrian|Early Cambrian|See p77 for detailed info.||||||07-FEB-11
40891|Pincally Formation|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Shale, sandstone, conglomerate, limestone.||||||10-SEP-07
40891|Pincally Formation|64671|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Blue grey shale, siltstone, tuffaceous lithic sandstone and minor limestone. Occurs west of Mt Arrowsmith.||||||26-NOV-08
40891|Pincally Formation|64687|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Blue grey shale, siltstone, tuffaceous lithic sandstone and minor limestone. Fault bounded and unconformable to the east, against Ordovician formations, unconformably overlain by Cretaceous rocks to the west.||||||
40891|Pincally Formation|66623|3|Fully described|pp67-70, pp56-58. |Early Cambrian|Early Cambrian|Defined by Warris (1967); included in Gnalta Group by Brock and Percival (2006) based on palaeontological studies. Toyonian to Ordian-early Templetonian. Stratigraphic equivalent of Coonigan Formation; contemporaneous with First Discovery Limestone Member. Maximum thickness c. 300 m. Limestones contain a diverse fauna. Algal oncolites occur in the limestones.||Unit in Gnalta Group.||Wydjah Formation overlies.  Recent sediment obscure underlying unit.|Mainly friable, poorly-outcropping grey-green phyllitic siltstone and shale; thin-bedded limestones and cross-bedded sandstones with carbonate matrix.|27-SEP-13
40891|Pincally Formation|66917|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Gnalta Group.|||Poorly-outcropping, grey-green slaty shale and dark grey siltstone, grey-green lithic sandstone and minor limestone.|
40891|Pincally Formation|66929|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian||||||Blue grey shale, siltstone, tuffaceous lithic sandstone; minor limestone.|
40891|Pincally Formation|66933|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
40891|Pincally Formation|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Gnalta Group.|||Poorly outcropping, grey-green slaty shale, dark grey siltstone, grey-green lithic sandstone and minor limestone.|
40891|Pincally Formation|67322|4|Described|p9; Fig.5|Stage 5|Stage 4|Warris (1967, 1969); revised by Brock and Percival (2006). At least 260m thick; base not exposed. Age from diverse shallow-marine macrofauna closely comparable with First Discovery Limestone Member. Occurs in the Mount Arrowsmith region.||Of the Gnalta Group.||Overlies the Kara Formation. Conformably overlain by the Wydjah Formation. Equivalent to First Discovery Limestone Member.|Composed principally of poorly exposed grey-green phyllitic siltstone and fissile shale, with a carbonate lens in the lower third and three prominent thin-bedded limestones in the upper third of the unit.|22-FEB-18
40891|Pincally Formation|70752|5|Briefly described|p127, p135-137, p139, p141|Middle Cambrian|Middle Cambrian|Koonenberry Belt. Linguliformean brachiopods have close affinity with those in Giles Creek Dolostone (NT). Systematic palaeontological descriptions. Ordian-early Templetonian.||||Is overlain by Wydjah Formation.||
81957|Pincham Syenite|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|||Sub-equigranular quartz syenite. Areas of magmatic quartz-hematite-apatite and resorbed primary syenite.|02-NOV-20
37909|Pine Cliffs Rhyolite Member|24605|3|Fully described|p931, p941|Namurian|Namurian|Of the Clifden Formation. Overlies the Bexley Rhyolite Member. Geological Province: New England Orogen. Defined as Pine Cliffs Rhyolite.||||||
37909|Pine Cliffs Rhyolite Member|61214|5|Briefly described|p171 Fig. 1|Carboniferous|Carboniferous|Of the Clifden Formation. ||||||
27054|Pinehurst Granite|22638|4|Described|p74||Late Devonian|New name.||||||
27054|Pinehurst Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
27054|Pinehurst Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
27054|Pinehurst Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.||Narraburra Suite.||||
27054|Pinehurst Granite|72084|6|Mentioned|p55 Fig.57|||A-type geochemical discrimination diagrams.||||||
40758|Piney Range Member|50613|2|Defined|p227-228 App. 1|Namurian|Namurian|Of Willuri Fm. Of the Piney Range package (informal grouping of stratigraphically recognisable mappable units) - contains 3 beds of purple ignimbrite (beds a, b and c).  Beds a and b overlain by Mount Byar Ignim.Mbr.  Ages: 317.7+/-2.4, 317+/-3.5Ma.||||||24-FEB-05
23906|Pinnacles Lens|42786|4|Described|p359|||||||||
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.||||||
82622|Piora Member|70820|6|Mentioned|p37|Cretaceous|Late Jurassic|Richmond River catchment area (Casino-Kyogle area) basement aquifer.||||Is overlain conformably by the Rappville Member.|Sandstone and claystone with minor carbonaceous material. A confined aquifer with low permeability below 150m.|
26845|Pipe Formation|22831|4|Described|p 80 -81|||Nangar Subgroup||||||03-MAR-22
26845|Pipe Formation|22857|5|Briefly described|p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Hervey Group. Red, green and buff shale; minor finely bedded white to red arenite. Max. thickness: 250m. Geological Province: Hervey Basin.||||||
26845|Pipe Formation|23214|3|Fully described|p230|Late Devonian|Late Devonian|Of Hervey Group. Geological Province: Hervey Basin. 270m at type section.||||||
26845|Pipe Formation|23217|6|Mentioned|p10|||replaced by Mount Cole Formation. See also  "Pipe Formation".||||||08-MAR-06
26845|Pipe Formation|23392|6|Mentioned|p12|||Superseded by Mount Cole Formation||||||
26845|Pipe Formation|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26845|Pipe Formation|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26845|Pipe Formation|30071|6|Mentioned|Fig.3|||||||||
26845|Pipe Formation|33006|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26845|Pipe Formation|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26845|Pipe Formation|33833|6|Mentioned|Fig.1|||||||||
26845|Pipe Formation|34109|4|Described|Table 3.10|||||||||
26845|Pipe Formation|43441|5|Briefly described|31||Late Devonian|||||||08-JAN-10
26845|Pipe Formation|43499|14|Not recorded|Map Legend|||(Provisional Edition) Part of Nangar Sub-Group||||||
26845|Pipe Formation|43500|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Part of Nangar Sub-Group||||||
26845|Pipe Formation|43507|2|Defined|p128-9,137,146-152,||Late Devonian|Formation of Nangar Subgroup (Hervey Group) p156||||||
26845|Pipe Formation|43509|14|Not recorded|p113|||||||||
26845|Pipe Formation|43510|2|Defined|p41-2,47-49-52,54-7,|||p77||||||
26845|Pipe Formation|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
26845|Pipe Formation|43516|14|Not recorded|Map Legend||Late Devonian|Part of Nangar Sub Group||||||
26845|Pipe Formation|43640|5|Briefly described|Map Legend||Devonian|||||||
26845|Pipe Formation|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Hervey Group. Consists of  red, green and buff shale; minor finely bedded white to red sandstone.||||||06-AUG-08
26845|Pipe Formation|43782|5|Briefly described|Map Legend|Famennian|Famennian|of Hervey Group.||||||
26845|Pipe Formation|44160|5|Briefly described|Map Legend||Famennian|||||||08-JAN-10
26845|Pipe Formation|48958|6|Mentioned|Plate 1|||||||||
26845|Pipe Formation|62569|5|Briefly described|p606 Fig. 1E|Late Devonian|Late Devonian|Of the Hervey Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
26845|Pipe Formation|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Hervey Group||||
29938|Pipers Flat Formation|13139|5|Briefly described|p9 Fig. 4|Early Silurian|Early Silurian|Geological Province: Rockley-Gulgong Volcanic Belt.||||||12-APR-05
29938|Pipers Flat Formation|22472|6|Mentioned|p36|||||||||
29938|Pipers Flat Formation|22486|4|Described|p 1, 3, 5, 7|||||||||
29938|Pipers Flat Formation|22857|4|Described|p430 App. 1 Tb. A1.5|Llandovery|Llandovery|Thinly bedded graptolitic shales. Disconformably overlain by Tanwarra Shale. Max. thickness: 375m. ||||||
29938|Pipers Flat Formation|23214|2|Defined|p112|Llandovery|Llandovery|Newly recognised  unit.  Consists of steeply west dipping sequence of medium bedded volcaniclastic sandstone with interbeds of thinly bedded graptolite shale. Max thickness 375m.||||||19-MAY-16
29938|Pipers Flat Formation|23334|5|Briefly described|9 Fig.4|Early Silurian|Early Silurian|||||||
29938|Pipers Flat Formation|43782|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||
29938|Pipers Flat Formation|63278|5|Briefly described|p146 Fig. 2a, p157|Early Silurian|Early Silurian|Overlain by Tanwarra Shale. Geological Province: Rockley-Gulgong Volcanic Belt, LFB. Comprising olny slate and interbedded siltstones with mid to late Llandovery graptoloites.||||||07-FEB-11
29938|Pipers Flat Formation|63290|5|Briefly described|p392 Tb. 1, p404, p397 Fig. 3(b)|Llandovery|Llandovery|Overlian by Tanwarra Shale. Geological Province: Rockley-Gulgong Volcanic Belt. Contains mid-late Llandovery (ca 436-428Ma) graptolites.||||||
29938|Pipers Flat Formation|63293|6|Mentioned|p468 Fig. 2|Llandovery|Llandovery|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
29938|Pipers Flat Formation|64826|5|Briefly described|p1041 Tb. 1|Llandovery|Llandovery|||||||
29938|Pipers Flat Formation|68592|5|Briefly described|p420, p426|Early Silurian|Early Silurian|Sofala district. Comparable lithology and graptolite fauna as Jerrara Formation.||||Disconformably overlies Sofala Volcanics. Is overlain disconformably by the Mumbil Group. Possible correlative of Jeremy Formation.||
29938|Pipers Flat Formation|70297|5|Briefly described|map legend, on side 2 of map sheet|Early Silurian|Early Silurian|Ungrouped Early Silurian formations. Deposited in moderate to deep-water environment.|||||Medium-bedded volcaniclastic sandstone with interbeds of thinly bedded graptolite shale.|
29938|Pipers Flat Formation|70684|6|Mentioned|p74|Early Silurian|Early Silurian|Sofala district, Rockley-Gulgong Volcanic Belt.||||||
29938|Pipers Flat Formation|73299|6|Mentioned|p1102 Fig.8|||Hill End Trough, eastern. [Map symbol suggests Silurian age]||||||
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.|
34004|Pitch Creek Volcanics|22571|6|Mentioned|p19|Devonian|Silurian|New England Orogen. Gamilaroi terrane||||||
34004|Pitch Creek Volcanics|23522|5|Briefly described|p249 Fig 5|Pragian|Silurian|||||||
34004|Pitch Creek Volcanics|24008|5|Briefly described|p355|Early Devonian|Late Silurian|||||||
34004|Pitch Creek Volcanics|44447|5|Briefly described|p131, p133 Fig.2, p135|Early Devonian||c. 2200m of subaqueously extruded quartz keratophyre, soda trachyte, dacite, rhyodacite and andesitic lavas. Overlain by Glen Ward Beds. Age: ?Early Devonian||||||
34004|Pitch Creek Volcanics|50168|5|Briefly described|p160, p160 Tb.1|Early Silurian||Gamilaroi Terrane. Minimum age constrained by the intrusive Pola Fogal Suite.||||Intruded by the Pola Fogal Suite.|Felsic lavas.|06-FEB-18
34004|Pitch Creek Volcanics|65214|6|Mentioned|p275|Devonian|Devonian|NSW, Pigna. Appears in text as Pitch Ck Volcanics. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
34004|Pitch Creek Volcanics|69601|5|Briefly described|p405-407|||Mayer (1972). Relationship with Glen Ward beds not certain; may be interbedded or interdigitate.||||Faulted against Pola Fogal Hornblendite-Tonalite Suite. Locally overlies Glen Ward beds unconformably.|A partly disrupted pile of intermediate-silicic volcanics: quartz keratophyres, keratophyres, keratophyric breccias, and andesitic extrusives and intrusives.|
34004|Pitch Creek Volcanics|73440|6|Mentioned|p129-132, p141-142, p145|Devonian|Silurian|[Written as Pitch Creek Volcanics and Pitch Creek volcanics; Pitch Creek intrusives are also mentioned on p129]. Of Stratford and Aitchison (1996, 1997). Lowermost unit of the Gamilaroi terrain.||||Overlain by Frog Hollow Formation.|Felsic volcanic rocks, basaltic breccia, tuffs, and trondhjemites.|
27221|Pitt Town Sand|35098|4|Described|p5|||||||||
27221|Pitt Town Sand|42925|2|Defined|p39||early Pleistocene|||||||
27221|Pitt Town Sand|42926|4|Described|map legend||Pleistocene|||||||
27221|Pitt Town Sand|73248|6|Mentioned|App. p3|Pleistocene|Pliocene?||||||Fluvial deposit.|
37911|Plagyan Ignimbrite Member|24605|2|Defined|p933 Fig. 2, p951 App.1|Namurian|Namurian|Of the Rocky Creek Conglomerate. Maximum Thickness: 2.5km. Age: 319.0 +/- 2.7 Ma (U-Pb) and 326.4 +/- 2.9 Ma. Geological Province: New England Orogen.||||||
37911|Plagyan Ignimbrite Member|50613|5|Briefly described|p209|Namurian|Namurian|Part of the Kaputar package of the Willuri Formation.  Overlain by Bideroie, The Calpe and Mount Byar Ignimbrite Members. Age: 319+/-2.7Ma (Roberts et al 2003).  Max. thickness: 300m.  Geological Province: Rocky Creek Syncline.||||||24-FEB-05
37911|Plagyan Ignimbrite Member|61214|5|Briefly described|p170, p171 Fig. 1|Namurian|Namurian|Of Rocky Creek Conglomerate. Contains multiple rhyolitic and dacitic ignimbrites. Geological Province: Boomi Block (in Rocky Creek Syncline) and in Carrol-Nandewar Block. See also p172 Fig. 2 (presented as Plagyan Ignimbrite only)||||||
75932|Pleasant Hill Granite|66300|5|Briefly described|pp76-81, 85.|||Eastern Lachlan Orogen. This age is slightly younger than the Marulan Granite (another unit in the Arthursleigh Suite), but indistinguishable from those of the Bindook Group felsic volcanics which this unit intrudes.|412.6 +/- 2.2 Ma.|Unit in Arthursleigh Suite.||Intrudes Bindook Group.|Includes massive, medium- to coarse-grained (3.5 - 5.5 mm) equigranular leucocratic granodiorite.|29-OCT-13
75932|Pleasant Hill Granite|70661|3|Fully described|vii, p6, p31, p75, p78, p79 fig 6|Lochkovian|Lochkovian|Originally placed in the now defunct Koorilla Suite, geochemical characterisation (Bodorkos et al 2010) showed it belonged in the Arthursleigh Suite. Named after the Pleasant Hill. Originally included as part of the undifferentiated Marulan batholith, was then renamed Mount Pleasant Adamellite before finally being named the Pleasant Hill Granite.  Metamorphism, geochemistry, geophysical characteristics and distribution discussed.  Type section mentioned. Age from SHRIMP U-Pb, Bodorkos et al 2010. See also  p87-p89, p145, p245.|412.6 +/- 2.2 Ma|Arthursleigh Suite||Intrudes Adaminaby Group, Bindook Group, intrudes Johnniefelds granodiorite, intruded by Arthursleigh Tonalite|Coarse to very coarse grained holocrystalline, equigranular biotite, hornblende granite to granodiorite. Primary minerals include quartz, plagioclase, K feldspar, biotite and hornblende.|
75932|Pleasant Hill Granite|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Arthursleigh Suite.|||Coarse- to very coarse-grained holocrystalline equigranular biotite-hornblende granite to granodiorite.|
68215|Plumbago Creek beds|44093|5|Briefly described|p233 App. 1|Early Permian|Early Permian|Geological Province: New England Fold Belt.||||||
68215|Plumbago Creek beds|61772|6|Mentioned|p128, p128 Fig. 2||Early Permian|In New England Orogen.||||||
37356|Poidevins Sandstone|50234|5|Briefly described|Map Legend|Llandovery|Llandovery|Quartz sandstone, quartzite, turbiditic quartz-lithic-micaceous sandstone with minor interbedded siltstone.  Overlies: Dignams Siltstone (Bendoc Group).||||||13-MAY-04
37356|Poidevins Sandstone|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Margules Group. Grey to brown med. to v. thickly bedded fine- to very coarse-gr. quartzose to feldspar-lithic-quartz sandstone, interbedded with green-grey to dk. grey siltstone; grey-green massive to laminated siltstone.||||||
37356|Poidevins Sandstone|67322|4|Described|p17|Early Silurian|Late Ordovician|Thomas and Simpson, in Thomas et al.(in press). At least 1200m thick. The Poidevins Sandstone (and possibly the Mundoonen Sandstone) may correlate with the Lower Silurian Cobbannah or Yalmy groups. Age determined from p20 Fig.5 (Strat. column) and correlative stratigraphy. Occurs in the Goulburn region.||||Conformably overlies the Dignams Siltstone. May correlate with the Mundoonen Sandstone, and Cobbannah or Yalmy Groups.|Fine to very coarse-grained quartzose sandstone with minor grey-green siltstone.|22-FEB-18
37356|Poidevins Sandstone|68592|2|Defined|p298, p322, p325-7, p339, p343-68, p420|Early Silurian|Late Ordovician|See also p12, p116-8. Named after Poidevins Creek. Originally the rocks were called Burra Burra Creek Formation (Scheibner, 1973). Representative section described. Forms low rubbly outcrop. Over 1200m thick. Correlative of Mundoonen, New Country and Willandra Sandstones.||Unit in Margules Group.||Conformably overlies Dignams Siltstone and Warbisco Shale (Bendoc Group). Is overlain unconformably by Shivering Conglomerate and Argyle Formation, and locally by Crookwell Basalt.|Grey to brown, medium- to very thick-bedded, quartzose sandstone (sublitharenite to subarkose), interbedded with siltstone and lesser mudstone of variable hue.|
37356|Poidevins Sandstone|70192|5|Briefly described|Map Legend|Bolindian|Bolindian|[Theta]mp. Includes one unnamed subunit of massive-laminated siltstone. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.||Margules Group|Includes one unnamed unit.||Medium-very thickly bedded, fine-very coarse grained, quartzose to feldspar lithic quartz sandstone interbedded with siltstone and mudstone; graded bedding and ripple cross-lamination are common; bimodal sorting in places.|
37356|Poidevins Sandstone|70542|5|Briefly described|Map Legend|Ordovician|Ordovician|||Margules Group |||Medium-very thickly bedded, fine-very coarse grained, quartzose to feldspar lithic quartz sandstone interbedded with siltstone and mudstone; graded bedding and ripple cross lamination are common; bimodal sorting in places.|
37356|Poidevins Sandstone|70543|5|Briefly described|Map Legend |Ordovician|Ordovician|Includes one unnamed subunit of massive-laminated siltstone||Margules Group|Includes one unnamed sub unit.||Medium-very thickly bedded, fine-very coarse grained, quartzose to feldspar lithic quartz sandstone interbedded with siltstone and mudstone; graded bedding and ripple cross-lamination are common; bimodal sorting in places.|
37356|Poidevins Sandstone|71069|5|Briefly described|p72, p75, p76 fig 27, p87-90, p93|||||Margules Group||Conformably (Gradationally) overlies the Warbisco Shale and Dignams Siltstone. Unconformably overlain by the Shivering Conglomerate and the Argyle Formation. Equivalent to the Mundoonen Sandstone.|Amalgamated, medium to thick, massive quartzose sandstone.|
37356|Poidevins Sandstone|71656|6|Mentioned|p13 Fig.2|Bolindian|Bolindian|Shown only in correlation chart (Fig.2).||Margules Group||Margules Group. Overlies Bendoc Group (Warbisco Shale).|Sandstone.|
37356|Poidevins Sandstone|71700|5|Briefly described|CD|||||Margules Group||Equivalent to the Mundoonen Sandstone.||
37356|Poidevins Sandstone|73140|5|Briefly described|p495 Fig.1, Fig.7|Bolindian|Bolindian|Uncertainty indicated for minimum age.||Margules Group||Overlies Warbisco Shale, Dignams Siltstone||
26106|Pokolbin Hills Volcanics|29915|2|Defined|p62|Middle Carboniferous|Middle Carboniferous|||||||
26106|Pokolbin Hills Volcanics|36528|6|Mentioned|p182|||||||||
26106|Pokolbin Hills Volcanics|38837|5|Briefly described|p232|Late Carboniferous|Late Carboniferous|Geological Province: New England Fold Belt||||||
26106|Pokolbin Hills Volcanics|39308|6|Mentioned|p478|||||||||
26106|Pokolbin Hills Volcanics|42214|6|Mentioned|p460|||||||||
26106|Pokolbin Hills Volcanics|42547|4|Described|p32|||||||||
26106|Pokolbin Hills Volcanics|44450|5|Briefly described|p147 Fig 43|Late Carboniferous|Late Carboniferous|Geological Province: Sydney Basin.||||||
26106|Pokolbin Hills Volcanics|62095|5|Briefly described|p267|||Uppermost member is Matthews Gap Dacitic Tuff Member. Overlain by Seaham Formation.||||||31-JAN-08
26106|Pokolbin Hills Volcanics|69635|5|Briefly described|p188, 189, 193|||New England Orogen. Basement to Sydney Basin.|||Includes Mount Bright Rhyolitic Ignimbrite Member, Matthews Gap Dacitic Tuff Member.|Correlated with the Paterson Volcanics.||
26106|Pokolbin Hills Volcanics|71628|5|Briefly described|p19: 134||||||Mount Bright Rhyolitic Ignimbrite Member.|Nonconformably overlies Mount View Range Granodiorite.||
78174|Pola Fogal Complex|68822|5|Briefly described|p332|Llandovery||Age derived from minimum age of  tonalite in the Complex.|>436 Ma (Kimbrough et al. 1993)|||||17-SEP-13
35621|Ponto Group|24345|5|Briefly described|p85|Cambrian|Cambrian|Geological Province:  Wonominta Block.||||||
35621|Ponto Group|24599|5|Briefly described|p494 Fig. 2|Cambrian|Cambrian|Metasediments and volcanics.||||||
35621|Ponto Group|50618|5|Briefly described|p248|Middle Cambrian|Early Cambrian|Of Stevens et al (2000). Upgrading of Ponto beds?? Geological Province: Wonominta Block.||||||
35621|Ponto Group|63789|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Baroorangee Creek Subgroup. In the Koonenberry Fault area.||||||27-NOV-08
35621|Ponto Group|63793|4|Described|p18, p22, p34-38, p76-77.|||Stevens et al. (2000). Formerly part of Wonominta beds (Warris 1967), Ponto beds (Mills 1992). High grade metamorphic rocks, multiply deformed; no primary textures preserved.  Unfossiliferous. White quartz veins abundant. Hosts Grasmere copper mine. Much of outcrop area has not been prospected.|||Includes Baroorangee Creek Subgroup.|Faulted against Kara beds. Is unconformably overlain by Ravendale Formation.|Phyllites and fine-grained mica-schists, with lesser tholeiitic pillow lavas and tuffs, thinly laminated quartzofeldspathic tuffs and weakly calcareous and dolomitic pelites.|19-JAN-15
35621|Ponto Group|64169|5|Briefly described|p18, p19|||Supersedes Ponto beds. Subdivided into: Nutherangie, Palgamurtie and Baroorangee Creek Subgroups. Geol. prov: Mount Daubeny Basin/Koonenberry Belt. In western half of GRASMERE sheet - atypical rocks characterise Baroorangee Creek Subgroup.||||||14-MAY-08
35621|Ponto Group|64671|5|Briefly described|Map legend|||Tentatively subdivided into Barroorangee Creek, Palgamurtie and Noonthorangee Subgroups. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-gr. turbiditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalt...||||||07-MAY-13
35621|Ponto Group|64680|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Includes Noonthorangee, Palgamurtie, and Baroorangee Creek Subgroups. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turbiditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalts.||||||
35621|Ponto Group|64682|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Noonthorangee Subgroup. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalts, and laminated siliceous tuffs.||||||
35621|Ponto Group|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Palgamurtie Subgroup.||||||
35621|Ponto Group|64686|5|Briefly described|Map Legend|Ordovician|Middle Cambrian|Includes Palgamurtie and Barooangee Creek Subgroups. Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turbiditic quartzofeldspathic arenites. Massive to well-cleaved tholeiitic metabasalts, + laminated siliceous tuffs||||||
35621|Ponto Group|64687|5|Briefly described|Map Legend|||||||||
35621|Ponto Group|65381|5|Briefly described|p689, 691, Fig 2|Middle Cambrian|Early Cambrian|Of the Wertago zone, Broken Hill; distal turbidites with minor tholeiitic volcanics.||||||07-MAR-12
35621|Ponto Group|66623|1|Redefined|p10, p57, pp74-97. |Cambrian|Cambrian|Formerly part of Wonominta beds (Warris 1967); named the Ponto beds (Mills 1972); renamed Ponto Group (Stevens et al. 2000); redefined this study. Fault-bounded, highly-deformed rocks, c.5.5 km thick. No fossils found. Characteristically forms low relief rises. Similar calc-alkaline chemistry as the coeval lower Gnalta Group. Equivalent age and geochemistry to the Kars Zone in the Loch Lillly - Kars Belt. Bittles Tank Volcanics correlated with Glenelg Complex of Victoria's Stavely Belt. Hosts several small copper deposits. Geophysical properties described.|Tuffs aged 512-509 Ma (Black 2005). ||Includes Baroorangee Creek, Weinteriga Creek, Grasmere, Cannela, Noonthorangee, Koonenberry, Yandenberry Formations and Bittles Tank Volcanics.|Is unconformably overlain by Mutawintji Group and the Mount Daubeny Formation.|Predominant fine-grained distal sequence of metamorphosed mudstone, siltstone and sandstone; minor tholeiitic pillow lavas and sills, exhalative (quartz-magnetite rocks) units, and felsic air-fall tuffs.|
35621|Ponto Group|66917|5|Briefly described|Map legend|Cambrian|Cambrian|Does not crop out in the map area.|||||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic psammites; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|66918|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Baroorangee Creek Formation, Bittles Tank Volcanics and Grasmere Formation.||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic psammites; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|66922|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Cannela Formation.||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic psammites; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|66927|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
35621|Ponto Group|66929|5|Briefly described|Map legend|||Variable strong to weak magnetic signature. Unfossiliferous.|||Includes Baroorangee Creek, Palgamurtie and Noonthorangee Subgroups.||Thick dark grey and maroon phyllite units interbedded with well-indurated, fine-grained turbiditic quartzofeldspathic arenites; massive to well-cleaved tholeiitic metabasalts and laminated siliceous tuffs.|
35621|Ponto Group|66933|5|Briefly described|Map legend|Ordovician|Middle Cambrian|Variable strong to weak magnetic signature.|||Includes Noonthorangee and Palgamurtie Subgroups.||Thick dark grey and maroon phyllite units interbedded with well-indurated fine-grained turbiditic quartzofeldspathic arenites; massive to well-cleaved tholeiitic metabasalts and laminated siliceous tuffs.|
35621|Ponto Group|67105|5|Briefly described|p650-651, 653-654, 658-659, 661-663|Cambrian|Cambrian|See also p665-666. East of the Gnalta Group, Koonenberry Belt. Deep-water environment; fore-arc sequence. Tectonic settings discussed. Upper greenschist to amphibolite (muscovite-biotite schist) grade. Strongly deformed.|511.7 +/- 3.5 Ma (SHRIMP II zircon: Black, 2005).||Bittles Tank Volcanics.||Deep-marine sedimentary package (mudstone and siltstone) with tholeiitic lavas and extensive laminated cherty felsic tuffs. Includes magnetic phyllite with intercalated calc-silicate horizons.|
35621|Ponto Group|67107|6|Mentioned|p697, 701|||Mentioned in a graph of Pb isotope data for the Lachlan Orogen.|||Bittles Tank Formation.||Includes metamorphosed marine clastic rocks with mafic dykes and flows of fundamentally tholeiitic composition.|
35621|Ponto Group|67207|5|Briefly described|Map legend.|Cambrian|||||Includes Cannela Formation.|Map key shows: overlies Teltawongee Group, is overlain by Warratta Group[?].|Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|25-SEP-13
35621|Ponto Group|67208|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Bittles Tank Volcanics and Yandenberry Formation.||Dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|67322|4|Described|p3 Fig.1, p11, p39; Fig. 5|Late Cambrian|Middle Cambrian|Koonenberry Belt, Delamerian Orogen. Of Mills (in Greenfield et al., 2010). At least 5500 m thick. Unfossiliferous. Age from tuffs in Noonthorangee Formation - not well constrained. Occurs in the Kayrunnera-Koonenberry region.|||Weinteriga Creek, Grasmere, Noonthorangee, Koonenberry, Yandenberry, Cannela and Baroorangee Creek Formations; Bittles Tank Volcanics.|Intruded by the Bittles Tank Volcanics.|Variably metamorphosed, fine-grained marine clastic rocks (phyllites, schists, fine-grained sandstones and mudstones). In the middle are extrusive rocks, including enriched MORB tholeiitic pillow lavas, basaltic flows and basic tuffs.|22-FEB-18
35621|Ponto Group|68822|6|Mentioned|p330|||Contains c 510 Ma tuff bands.||||||
35621|Ponto Group|69001|6|Mentioned|p2 Fig.1B|Cambrian|Cambrian||||Includes the Cannela Formation.|||
35621|Ponto Group|69043|5|Briefly described|p4, p100, p104|||Fore-arc eruptive deposits from the subduction-related Mount Wright volcanic arc; coeval with Cymbric Vale Formation to the W. Other similar age determinations given.|511.7 +/- 3.5 Ma (Black, 2005).|||||
35621|Ponto Group|69961|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Noonthorangee, Koonenberry and Yandenberry Formations and Bittles Tank Volcanics.||Undifferentiated: dark grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|
35621|Ponto Group|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|In the Koonenberry Belt, quartzofeldspathic sandstone, metabasalt, trachyandesite and dacitic tuff are intercalated. Crops out in N part of the Kars Zone. Interpreted equivalent to sedimentary and volcanic rocks in the Wirryilka, Loch Lilly and Kars (geophysical basement) Zones.|||||Thickly bedded dark grey phyllite units.|
35621|Ponto Group|70037|6|Mentioned|p11|||||||||
35621|Ponto Group|70210|5|Briefly described|p1, p38|Middle Cambrian|Middle Cambrian|Koonenberry-Tibooburra district. Four felsic tuffs from this unit and Cymbric Vale Formation have indistinguishable SHRIMP ages of c.511 Ma.|||Canella Beds.|||
35621|Ponto Group|70296|6|Mentioned|p1-2, p19-21, p24|||Koonenberry District. Four samples dated. Three are felsic tuffs. SHRIMP ages include 511.4 +/- 3.7 Ma; 509.4 +/- 3.4 Ma; 512.8 +/- 3.3 Ma and 497.5 +/- 3.3 Ma for a felsic tuff or volcanic flow. Dated tuffs correlated with dated tuff in Cymbric Vale Formation, suggesting both units saw the same volcanic event at ~511.1+/-1.7 Ma.|||Includes the Mount Daubeny Formation [?].|||22-JAN-21
35621|Ponto Group|70648|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Bittles Tank Volcanics, Yandenberry Formation, Koonenberry Formation, Noonthorangee Formation.||Dark grey to maroon phyllite interbedded with upward fining quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|20-JAN-22
35621|Ponto Group|70650|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Bittles Tank Volcanics, Grasmere Formation, Baroorangee Creek Formation.|Intruded by diorite of Bittles Tank Formation.|Dark grey to maroon phyllite interbedded with upward fining quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies.|20-JAN-22
35621|Ponto Group|70651|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Bittles Tank Volcanics, Noonthorangee Formation, Grassmere Formation, Weinteriga Creek Formation, Baroorangee Creek Formation.||Dark-grey to maroon phyllite interbedded with upward fining quartzo-feldspathic metasandstone; originally interbedded siltstone and minor sandstone; regionally metamorphosed to greenschist facies;  mafic intrusions, and extrusive mafic lavas.|
35621|Ponto Group|70749|6|Mentioned|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.||||||
35621|Ponto Group|70838|4|Described|p266,p268-272,p274-275,p277-278,p280-281|Cambrian|Cambrian|Koonenberry Belt. Suggested deposition in deep water at the foot of a continental slope. Texturally immature: possible tectonic settings discussed (convergent margin preferred). Coeval with Teltawongee Group. Maximum depositional age is poorly constrained. Deformed during the Delamerian Orogeny (c.500 Ma). Cut by an undeformed felsic body dated 496.3 +/- 3.1 Ma (Black, 2005). Detrital zircon analyses.|c.508 Ma (maximum deposition age).||Noonthorangee Formation, Bittles Tank Volcanics.|Faulted against Grey Range Group.|Texturally immature, finely bedded mudstones and siltstones metamorphosed at greeenschist to lower-amphibolite facies.|
35621|Ponto Group|71262|5|Briefly described|p3, p5 Fig 2,  p8 Fig 5, p9, p12|Cambrian|Cambrian||||Includes Bittles Tank Volcanics?||Includes magnetite-rich members.|
35621|Ponto Group|71415|5|Briefly described|p11,15|Cambrian|Cambrian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Sedimentary sequence related to c. 510 Ma volcanics of the Mount Wright Arc. Underwent deformation and greenschist facies metamorphism during c. 500 Ma Delamarian Orogeny.||||Overlies the Grey Range Group.||19-AUG-19
35621|Ponto Group|71593|5|Briefly described|p188-p189|Early Cambrian|Early Cambrian|Koonenberry Province. Hosts Besshi-type VHMS Cu-Zn prospects in E-MORB-like mafic volcanics.|c. 511-506 Ma||||Mafic volcanics.|
35621|Ponto Group|71965|5|Briefly described|p894|Cambrian|Cambrian|Geological province: Koonenberry Belt, Delamerian Orogen. Volcanism c. 510 Ma associated with development of the Mount Wright continental magmatic arc (Greenfield et al., 2010; Greenfield et al., 2011).||||||
35621|Ponto Group|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Delamarian Orogen.||||||
35621|Ponto Group|72522|6|Mentioned|p131.|||Part of the basement to Mount Daubeny Basin||||Intruded by Wertago Volcanics.||
35621|Ponto Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Dark-grey to maroon phyllite interbedded with fining-upward quartzo-feldspathic metasandstone; regionally metamorphosed to greenschist facies.|09-DEC-21
35621|Ponto Group|73177|5|Briefly described|p1098, 1114-1115 Figs.16-17|Middle Cambrian|Early Cambrian|||Grey Range Group.|Bittles Tank Volcanics, Noonthorangee Formation.|||
35621|Ponto Group|73430|6|Mentioned|p494|Middle Cambrian|Early Cambrian|Koonenberry Belt. Deformed in Delamerian Orogeny.|||||Sedimentary unit.|
22680|Pooncarie Ironstone|22893|3|Fully described|p37,38 table8|Pleistocene|Pliocene|||||||
22680|Pooncarie Ironstone|44188|5|Briefly described|Map Legend|Pleistocene|Pliocene|Geological province: Murray Basin. Medium- to coarse-ghrained oolitic goethiyic ironstone, angular quartz grain nuclei, interstitial quartz grains and massive radiating crystals of goethite; sporadically developed non-oolitic (weathered) ironstone.||||||15-MAY-08
73111|Port Macquarie Serpentinite|63763|3|Fully described|p3, p4-5 Fig. 1, p15|Early Cambrian|Early Cambrian|Proposed that this name is extended to other known serpentinite bodies in the Port Macquarie Block, including "Burrawan serpentinite" and "Lake Innes mass" (Leitch 1980a).Age: ~530Ma.  Lithological detail included. See also p7 Fig. 2.||||||
73111|Port Macquarie Serpentinite|65940|6|Mentioned|p194|||Wauchope-Port Macquarie area, NSW.||||||
73111|Port Macquarie Serpentinite|67322|5|Briefly described|Fig.5; p28|Late Ordovician|Late Ordovician|Defined by Och, Leitch and Caprarelli (2007). Although undated, the ultramafic protolith is interpreted to be as old as Early Cambrian on the basis of correlation with comparable serpentinised rocks in the southern New England Orogen, dated at 530 Ma using zircons from plagiogranite blocks. Occurs in the Port Macquarie region.|||||Consists of massive and schistose serpentinite together with rodingite (highly altered mafic rocks, possibly originally dykes), surrounded by broken formation of the Watonga Formation.|22-FEB-18
33742|Porters Mount Quartz Diorite|24417|3|Fully described|p105|Early Devonian|Early Devonian|Previously referred to as "Porters Mount Tonalite".  Age: 399.7+/-2.6Ma (SHRIMP U/Pb).||||||
33742|Porters Mount Quartz Diorite|60009|5|Briefly described|Map Legend|Emsian|Pragian|||||||13-JUL-04
33742|Porters Mount Quartz Diorite|66197|5|Briefly described|p635 Fig.5b|Eifelian|Emsian|Jemalong Trough. Age: 399.7 +/- 2.6 Ma.||||||13-MAR-12
33742|Porters Mount Quartz Diorite|71040|6|Mentioned|p16|Devonian|Devonian|Currowong Syncline.||||||
37915|Pound Rock Rhyodacite Member|24605|2|Defined|p931, p953 App.1|Namurian|Namurian|Of the Rocky Creek Conglomerate. Thickness at type locality: 45m. Age: 320 +/- 2.8 Ma. Geological Province: New England Orogen.||||||
37915|Pound Rock Rhyodacite Member|50613|6|Mentioned|p215|||In the Darthula Block.||||||
37915|Pound Rock Rhyodacite Member|61214|5|Briefly described|p170, p171 Fig. 1|Namurian|Namurian|Of Rocky Creek Conglomerate. Geological Province: Darthula Block. See also p172 Fig. 2 (presented as only Pound Rock in text of figure).||||||
22689|Powder Horn Hill Microgranite|22638|1|Redefined|p69|Early Silurian||Possibly the fine-grained equivalent of Gundibindyal Granite||||||
22689|Powder Horn Hill Microgranite|44192|5|Briefly described|Map Legend||Lochkovian|||||||
25414|Prairie Sand|30289|4|Described|p269|||||||||
80636|Precipice Sandstone, Lower|71805|4|Described|p83, p84, p86-p89, p77 fig.3||Sinemurian|Surat Basin. See Precipice Sandstone. Cored in Woleebee Creek GW4. Wireline logs exist for the core and for this unit. Highly varied and greater thickness (<5-115m) than the Upper Precipice Sandstone. Outcrops in the Carnarvon Gorge section of the Carnarvon National Park. An informal lacustrine shale unit seperates this unit and the Upper Precipice Sandstone.||||Overlain by the Precipice Sandstone, Upper.|Fine-grained heterolithic and coarse-grained sandstone.|16-MAY-19
80637|Precipice Sandstone, Upper|71805|4|Described|p80-p82, p84, p86-p89, p77 Fig.3|Toarcian||Surat Basin. See Precipice Sandstone. Cored in Woleebee Creek GW4. Includes fossilised worm burrows including Teichichnid forms which suggest a Triassic age. Wireline logs exist for the core and for this unit. Thickness varies fgrom 10-75m. Part of this unit is interpreted as tidal on the basis of sedimentary structures.||||Overlies the Precipice Sandstone, Lower.|Thinly-bedded sandstone and siltstone in which ripple marks, worm trails and leaf impressions are common.|16-MAY-19
41571|Preston Formation|60303|5|Briefly described|p5, p6 Fig. 1|Early Devonian|Late Silurian|Hosts the Brown Reef deposits - dominant sulphide is pyrite.  Geological Province: Rast Trough (Lachlan Fold Belt).||||||
41571|Preston Formation|61964|3|Fully described|p14 Fig. 4, p67-69|Lochkovian|Pridoli|Of Rast Gp. Muddy marine basinal seq.originally mapped as Ural Volcanics using nomenclature such as "Boothumble beds", "Preston beds" and "Yelkin beds" . Conformable below Ural Volcs; overlies Crossleys Tank Fm. Max.thickness: >1500m.Palaeontology - p260||||||14-OCT-08
41571|Preston Formation|62034|5|Briefly described|p27|Devonian|Silurian|Hosts the large Browns Reef polymetallic deposit.  Conformably overlain by the Ural Volcanics.  Geological Province: Lachlan Orogen.||||||04-JUL-06
41571|Preston Formation|62367|5|Briefly described|p4 Fig. 2|Early Devonian|Silurian|Of the Rast Group. Hosts large low-grade Browns Reef base metal deposit.||||||02-JUN-06
41571|Preston Formation|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Rast Group. Interbedded mudstone, quartz sandstone, lithic sandstone with rare conglomerate lenses and rhyolite sills.||||||03-NOV-15
41571|Preston Formation|63019|5|Briefly described|p920, p921 Fig.2|Lochkovian|Lochkovian|Volcaniclastic and fossiliferous sandstone. Conformably overlies Crossleys Tank Formation east of Ural Range.||||||
41571|Preston Formation|63891|5|Briefly described|p237|||Underlies Ural Volcanics. Lithology (together with Crossleys Tank Formation): basin-fill sequences of quartz-rich turbidites consisting of volcaniclastic and fossiliferous sandstones.||||||
41571|Preston Formation|65469|5|Briefly described|p18|Late Silurian|Late Silurian|Lachlan Orogen.||||||
41571|Preston Formation|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian|The five facies are mapped separately as un-named sub-units: slate or mudstone; crystal-rich quartzofeldspathic sandstone; lithic-feldspathic sandstone; rhyolite intrusions; quartz-rich sandstone, massive and thick-bedded.||Unit in Rast Group.||Is faulted against Clements Formation. Overlies Crossleys Tank Formation.|Interbedded mudstone, quartz sandstone, lithic sandstone with rare conglomerate lenses and rhyolite sills.|
41571|Preston Formation|70950|6|Mentioned|p1033,1045, 1046|||Geological province: Central Lachlan Orogen. Detailed mineralisation analysis provided.||Unit of Rast Group.|||Medium- to coarse-grained sandstones, conglomerate and carbonaceous siltstone to shale; granule conglomerate, fine to medium-grained sandstone, carbonaceous radiolarian siltstone and porphyritic coherent rhyolite.|
41571|Preston Formation|71039|6|Mentioned|p22, p29|||||||||
41571|Preston Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Rast Group.||Overlies Crossleys Tank Formation. Is overlain by Ural Volcanics.|Volcaniclastic and fossiliferous sandstone. Interbedded mudstone, quartz sandstone, lithic sandstone with rare conglomerate lenses and rhyolite sills.|
22697|Pretty Point Tonalite|22815|4|Described|p74|||||||||
22697|Pretty Point Tonalite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Why Worry Suite.||||||
82601|Primley Monzogranite|71628|5|Briefly described|p8: 4, 102-103|||New name (this study) after unpublished work by Smith (1973) who had called it Primley Adamellite. Named after Primley homestead. A small (~3 km2) intrusion ~12 km NW of Armidale. Crops out as sheets and tors. Unassigned to a Suite.||Primley Suite.||Intrudes Sandon beds.|Medium-grained, porphyritic, hornblende-biotite monzogranite.|
41071|Pringles Monzogranite|24366|5|Briefly described|p11, 16 Fig. 3|Early Permian|Early Permian|Of the Bundarra Plutonic Suite.||||||
41071|Pringles Monzogranite|62757|5|Briefly described|p2, p5 Fig. 2|Early Permian|Early Permian|Of the Bundarra Supersuite.Surrounds the intruding Fox Tor Diorite. S-type granitoid. Megacrystic quartz-plagioclase-K-feldspar-biotite-muscovite-cordierite monzogranite.||||||07-FEB-11
41071|Pringles Monzogranite|65398|5|Briefly described|p5 Tb.1, p8, Fig 3|Early Permian|Early Permian|S-type granite of the Bundarra Supersuite. Equigranular to porphyritic, coarse-grained biotite-muscovite-cordierite leucogranite. Age of 277 Ma (K-Ar; Hartono, 1984) and 270-273 (Shaw and Flood, 1981).||||||
41071|Pringles Monzogranite|66720|5|Briefly described|Map legend|Early Permian|Early Permian||||Includes two un-named, separately mapped units: carapace-phase of fine-grained, leucocratic quartz-feldspar-biotite granite; pyritic phase, similar but with rare pyritic aggregates and joint fills.||Equigranular to porphyritic biotite-muscovite-cordierite granite.|
41071|Pringles Monzogranite|68005|5|Briefly described|p62, p136.|Early Permian|Late Carboniferous|Boundaries have been refined using radiometric imagery.||Unit in Banalasta Suite.|||Approximately equigranular biotite-muscovite-cordierite granite.|
41071|Pringles Monzogranite|69188|4|Described|p2, p4, p55-59, p79|Permian|Permian|Watson Creek area, near Bendemeer. The microgranite is intimately spatially associated with phyllic to greisenous alteration, tourmalinisation, and veining associated with hard rock tin mineralisation (at Giants Den) and related placers and stream deposits. See also reference to Pringles Monzonite (p55).|288.7 +/- 1.6 Ma (magmatic age)|Bundarra Supersuite.||Adjacent to Banalasta Adamellite.|Porphyritic biotite-bearing microgranite. Reduced; S-type.|16-APR-20
41071|Pringles Monzogranite|69323|5|Briefly described|p35,69|Cisularian|Cisularian|Geological province: New England Orogen. Date derived from Cross and Blevin, 2013 is a SHRIMP age.|288.7+\-1.6 Ma (Cross and Blevin, 2013)|Unit of Bundarra Supersuite.||||03-DEC-19
41071|Pringles Monzogranite|70217|5|Briefly described|v, p72|Artinskian|Sakmarian|New England Orogen. SHRIMP ages are derived from this volume. S-type affinity.|288.7 +/- 1.6 Ma (SHRIMP U-Pb)|Bundarra Supersuite||||04-OCT-17
41071|Pringles Monzogranite|71628|4|Described|p4: 1, 3-5, 7-10, 12, 20, 23-25, 29-30|||See also p4: 38-53, 55-58; p19: 39, 42. Brown (2003). Its definition has varied markedly over time: history is given. Redefined in this study. Named after a local watercourse. Occurs ~20 km N of Bendemeer and ~35 km W of Uralla. Southern New England Orogen. Likely a composite unit; geochemically heterogeneous. Forms a variety of outcrops, mostly weathered. Characterised by a featureless, moderate Th-U and high K response. Appears as Pringle Monzogranite on p4-5. Geochemistry described. Unmineralised but used as a source of dimension stone. RELATED UNITS (continued): Abuts the Banalasta, Namoi Tops, Rocky Glen and MacDonald River Monzogranites, Glenclair Syenogranite and Giants Den Leucosyenogranite.||Pringles Suite.|Roumalla Monzogranite Phase, Tilmunda Syenogranite Phase.|Intrudes Sandon beds and Banalasta Monzogranite. Is intruded by Fox Tor Quartz Diorite and ?Mountain Home Granite. See COMMENTS for more.|Coarse-grained, porphyritic to even-grained, K-feldspar-rich biotite (+/- muscovite, +/- cordierite) monzogranite and leucocratic syenogranite. S-type.|
41071|Pringles Monzogranite|72078|5|Briefly described|p4|Permian|Permian|Geological province: New England Orogen. Also referred to as Pringels pluton in text. U-Pb SHRIMP date for zircon is derived from Cross and Blevin 2013. Features minor scattered Sn-W mineralisation.|288.7 +/- 1.6 Ma (SHRIMP U-Pb)|Unit of Bundarra Spersuite.||||14-JAN-20
26857|Prison Farm Granodiorite|40328|4|Described|p210|||||||||
26857|Prison Farm Granodiorite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
26857|Prison Farm Granodiorite|45087|5|Briefly described|p48|||Chemical analyses||||||
26857|Prison Farm Granodiorite|69801|6|Mentioned|p104|||Central Lachlan Orogen. Obsolete terminology?, incorporated into the Bogandyera Granite?||Mannus Creek Suite||||25-NOV-19
26112|Prospect Picrite|22857|5|Briefly described|p309 (photo 2)|||Large sill-like basin-shaped intrusion of strongly differentiated picrite in lower part and alkaline dolerite in upper part. Age: 168Ma (Evernden and Richards, 1962). Overlain by Ashfield Shale (Wianamatta Group). Max. thickness: 130m. ||||||
26112|Prospect Picrite|42925|2|Defined|p57|Middle Jurassic|Early Jurassic|||||||
26112|Prospect Picrite|42926|4|Described|map legend||Jurassic|||||||
26112|Prospect Picrite|70587|5|Briefly described|Map Legend|Jurassic|Jurassic||||||Picrite, dolerite and minor basalt.|
31422|Pullabooka Formation|24417|3|Fully described|p80|Early Devonian|Early Devonian|Of Trundle Group.  Originally named "Pullabooka beds".  Intruded by Dalrida Granite.  Conformably overlain by Carawandool Volcanics; underlain by Derriwong Group.||||||
31422|Pullabooka Formation|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Trundle Group.  Overlies: Cookeys Plains Formation.  Underlies: Carawandool Volcanics.||||||
31422|Pullabooka Formation|60009|5|Briefly described|Map Legend|Pragian|Lochkovian|Of the Trundle Group. Underlies: Carawandool Volcanics.||||||13-JUL-04
31422|Pullabooka Formation|60548|5|Briefly described|map legend|Devonian|Devonian|Of Trundle Group.  Massive to poorly bedded quartz sandstone and quartzite, minor siltstone and shale.||||||19-NOV-04
31422|Pullabooka Formation|62569|6|Mentioned|p612|Early Devonian|Early Devonian|Contains fish plates remains. ||||||
31422|Pullabooka Formation|66197|5|Briefly described|p634, p635 Fig.5b|||Jemalong Trough. Deep marine shale and sandstone. Underlies the Carawandool Volcanics, overlies the Yiddah Formation or the Manna Conglomerate.||||||13-MAR-12
31422|Pullabooka Formation|71040|5|Briefly described|p16-17|Early Devonian|Early Devonian|Currowong Syncline.||Trundle Group.||||
28944|Purgatory Creek Limestone|34220|6|Mentioned|p297|||||||||
28944|Purgatory Creek Limestone|40328|6|Mentioned|p191|||||||||
28944|Purgatory Creek Limestone|71628|6|Mentioned|p19:146|||||||||
82628|Purgatory Monzogranite|71628|5|Briefly described|p19: 146-148|||Originally Purgatory Creek adamellite of Gutsche (1969). Renamed in this study to align with IUGS nomenclature. Crops out 7 km ESE of Jackadgery as a series of small bodies, heavily weathered. Is associated with the Paddy Doughty Cu (As, Zn, Au) mine.||Purgatory Suite.||Intrudes Willowie Creek beds and Gundahl Complex. Is overlain by Laytons Range Conglomerate.|Medium- to coarse-grained, equigranular, biotite-leucogranite, microgranite, and aplite; heavily weathered.|
68901|Purnamoota Road Gneiss|6823|5|Briefly described|p203, 205, 226-227, 228, 233, 236|Paleoproterozoic|Paleoproterozoic|Previous name? or revived here? Interpreted as granitic intrusion into metasedimentary rocks. Previously considered to be part of Hores Gneiss. Herein considered to be part of the Potosi Gneiss? Crystallisation age for LF granite at Purnamoota Road; 1586+/-9 Ma. Shown as Purnamoota Gneiss p205 Fig.2, p228, 233, 235. Also shown as 'Purnamoota Road Gneisses (Potosi Gneiss assigned to Hores Gneiss)' p226.|ca. 1640-1660 Ma?, 1586+/-9 Ma cryst.|||||26-MAR-22
68901|Purnamoota Road Gneiss|60657|5|Briefly described|p13 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1680-1660Ma. Geological Province: Curnamona Craton.||||||07-NOV-08
68901|Purnamoota Road Gneiss|64316|5|Briefly described|p534|Mesoproterozoic|Paleoproterozoic|One of the "Lf leucocratic gneisses", a group of felsic gneisses. Ages: 1573+/-29Ma (Nutman and Ehlers et al 1996) and 1597+/-3Ma (Page et al 2005a) - both SHRIMP zircon ages.||||||07-FEB-11
68901|Purnamoota Road Gneiss|66302|6|Mentioned|p39|||||||||
22707|Purnim Volcanic Member|22519|6|Mentioned|p7|||of Troffs Formation||||||
22707|Purnim Volcanic Member|22520|6|Mentioned|p18|||of Troffs Formation||||||
22707|Purnim Volcanic Member|22831|3|Fully described|p 63||Early Devonian|||||||
22707|Purnim Volcanic Member|22857|5|Briefly described|p448 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Troffs Formation (Trundle Group). Andesitic lavas. Max. thickness: 300m. Geological Province: Bogan Gate Terrace.||||||
22707|Purnim Volcanic Member|43441|5|Briefly described|30||Early Devonian|||||||08-JAN-10
22707|Purnim Volcanic Member|44160|5|Briefly described|Map Legend||Pragian|||||||08-JAN-10
29552|Purnoo Conglomerate Member|22578|6|Mentioned|p394|||||||||
29552|Purnoo Conglomerate Member|42974|5|Briefly described|p192|||Of Nowra Sandstone.||||||12-MAR-09
29552|Purnoo Conglomerate Member|61609|5|Briefly described|p240, p241|Permian|Permian|Fisher (1972). Of Nowra Sandstone. Underlain by Wandrawandian Siltstone and Snapper Point Formation in the west. Attributed to shallow marine setting after a period of low sea level.||||||07-FEB-11
29552|Purnoo Conglomerate Member|70661|4|Described|p137, p139, p165, p169, p170, p174-p176|Permian|Permian|Named after Purnoo Lookout. Overlies a ravinement surface. 0.5 -1.8m thick. Basal to the Nowra sandstone, generally recessive outcrop. Type section mentioned. Age from parent unit.||Nowra Sandstone||Conformably overlies Wandrawandian Formation, Snapper Point Formation, may be overlain by Berry Siltstone|Clast to matrix supported pebble-cobble conglomerate. Clasts range from well rounded to angular. Angular boulders occur where it is basal to the Nowra Sandstone. The matrix is poorly sorted quartz sandstone to granule conglomerate.|
29552|Purnoo Conglomerate Member|71303|5|Briefly described|map legend|Guadalupian|Guadalupian|Of Sydney Basin.||Of Nowra Sandstone.|||Very poorly sorted, predominantly matrix-supported pebble to cobble conglomerate. Clasts subangular to mostly well rounded, comprising mainly quartzite with lesser white quartz, black chert, sandstone and igneous lithologies.|
26861|Puxtrees Coal Member|37773|6|Mentioned|p19|||||||||
26861|Puxtrees Coal Member|39346|6|Mentioned|Map legend|Permian|Permian|||||||
26861|Puxtrees Coal Member|40331|6|Mentioned|p13|||||||||
26861|Puxtrees Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area. Appears as Puxtrees Lower and Puxtrees Upper.||Rowan Formation. ||||
30047|Pyangle Pass Granite|22529|6|Mentioned|4 fig 2|Visean|Visean|||||||
30047|Pyangle Pass Granite|23043|5|Briefly described|Map Legend|Namurian|Visean|||||||
30047|Pyangle Pass Granite|23170|2|Defined|p278|Carboniferous|Carboniferous|Age: Middle Carboniferous.||||||
30047|Pyangle Pass Granite|43188|5|Briefly described|p221, Fig.2 p197||Carboniferous|of Langworthy (1986)(B.Sc.Hons.)||||||
30047|Pyangle Pass Granite|73299|6|Mentioned|p1096 Fig.3|Carboniferous|Carboniferous|||||||
38277|Pyes Creek Leucomonzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Coarse-grained, equigranular leucomonzogranite.  An I-type granitoid.||||||20-DEC-04
38277|Pyes Creek Leucomonzogranite|23812|5|Briefly described|p20 Tb.2|Permian|Permian|||||||
38277|Pyes Creek Leucomonzogranite|70217|4|Described|v, p1 tbl 1.1, p49-p54, p75, p76, p87|Changhsingian|Wuchiapingian|New England Orogen. SHRIMP ages are derived from this volume. Petrography, zircon morphology and SHRIMP results discussed in detail. Coeval with other granites of the Uralla Supersuite.|253.1 +/- 1.4 Ma (SHRIMP U-Pb)|Uralla Supersuite||Intruded by the Bolivia Range Leucomonzogranite. Intrudes the Wandsworth Volcanics.|Seriate, medium-grained granite composed of approximately 40 percent quartz, 20 percent plagioclase, 20 percent alkali feldspar and 10 percent biotite.|
38277|Pyes Creek Leucomonzogranite|71628|3|Fully described|p15: 2, 9, 22-25|||Henley et al. (2001) after unpublished work by Barnes (1987). Originally Pyes Creek Adamellite (Shaw, 1969); later Pyes Creek Leucoadamellite of Pogson and Hitchins (1973). The type locality is just over 1 km S of the road junction from Stannum, Bolivia and Clive (Shaw, 1969). Named after a local watercourse. Occurs approx. 10 km WNW of Bolivia locality, 6 km NE of Stannum and 30 km SSW of Tenterfield. Limited geochemistry briefly described.|253.1 +/- 1.4 Ma (SHRIMP: Waltenberg et al., 2015)|Bolivia Range Suite.||Intrudes Emmaville Volcanics and Bolivia Range Leucomonzogranite.|Coarse-grained, equigranular, K-feldspar-rich leucomonzogranite; finer-grained marginal variants.|
30904|Pyramid Hill Arenite|43399|2|Defined|p197,198,203-205,207||Early Carboniferous|||||||
30904|Pyramid Hill Arenite|43406|14|Not recorded|p41,42,45,48||Tournaisian|Formation of Parry Group (L.Carb)||||||
30904|Pyramid Hill Arenite|43446|14|Not recorded|p6049||Tournaisian|||||||
30904|Pyramid Hill Arenite|68005|5|Briefly described|p148.|Carboniferous|Carboniferous|||Unit in Tangaratta Formation.|||Lenses of labile sandstones and lithic wackes with minor conglomerate interbedded with Tangaratta Formation.|
30897|Pyramid Hill Arenite Member|43400|14|Not recorded|map|Early Carboniferous|Late Devonian|||||||
30897|Pyramid Hill Arenite Member|43406|14|Not recorded|p42||Tournaisian|Part of Parry Group (L.Carb)||||||
33671|Quaama Granodiorite|22815|4|Described|p68|Early Devonian|Late Silurian|||||||
33671|Quaama Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Cobargo Suite.||||||
28252|Quarantine Bay Member|30938|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28252|Quarantine Bay Member|32127|4|Described|p248|||Refers Steiner (1972)||||||
28252|Quarantine Bay Member|33268|4|Described|p262|||||||||
28252|Quarantine Bay Member|33269|6|Mentioned|Table 1|||Refers Steiner (1966)||||||
28252|Quarantine Bay Member|35526|6|Mentioned|p87|||Refers Steiner (1972)||||||
28252|Quarantine Bay Member|42050|6|Mentioned|Fig.3 P229|||||||||
82631|Quartz Pot Creek Monzogranite|71628|5|Briefly described|p12: 1, 11-12; p15: 33, 57, 65, 75|||New name, after a local watercourse. Crops out in Bookookoorara Creek 3 km N of Bald Rock. An irregularly-shaped intrusion 2 km x 700m; deeply weathered and poorly exposed.||Sailor Jack Supersuite.||Is entirely enclosed by the (?younger) Mount Norman Leucomonzogranite, and Mount Lindesay Monzogranite (Stanthorpe Complex).|Coarsely porphyritic, hornblende-biotite monzogranite to granodiorite. I-type.|
30152|Queens Pinch Group|22529|6|Mentioned|1,4 fig 2|||||||||
30152|Queens Pinch Group|22590|6|Mentioned|Fig3 P754|Emsian|Lochkovian|||||||
30152|Queens Pinch Group|22857|4|Described|p476 App.1 Tb.A1.6|Early Devonian|Early Devonian|Siliclastic and carbonate mass flow, hemipelagic deposits and felsic to mafic volcanics. Max. thickness: 1700m. Geological Province: Capertee Rise.||||||
30152|Queens Pinch Group|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|||||||
30152|Queens Pinch Group|23170|2|Defined|p143|Emsian|Lochkovian|of Lachlan Fold Belt.||||||
30152|Queens Pinch Group|44093|5|Briefly described|p211 App. 1|Early Devonian|Early Devonian|Includes Tinja Formation and Sutchers Creek Formation. Geological Province: Lachlan Fold Belt.||||||29-MAR-05
30152|Queens Pinch Group|66197|5|Briefly described|p633 Fig.4a|Emsian|Pragian|Capertee High-Hill End Trough. Shallow marine clastics, limestone and silicic volcanics. Overlies the Toolamanang Formation or the Millsville Formation.||||||13-MAR-12
30152|Queens Pinch Group|68003|5|Briefly described|p24 Fig.3-e. |Emsian|Pragian|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Sutchers Creek Formation.|||
30152|Queens Pinch Group|73299|6|Mentioned|p1096 Fig.3, p1108|Early Devonian|Early Devonian||||Mullamuddy Formation, Taylors Hill Formation, Warratra Formation, Ingleburn Formation, Sutchers Creek Formation.||Includes limestone markers.|
69864|Quialigo Volcanics|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Bindook Group. Includes 6 named members and 3 unnamed subunits. Rhyolitic and dacitic crystal-rich ignimbrite, feldspar-pyroxene-phyric andesite, feldspar-phyric basalt, minor volcanic conglomerate, slate, laminated siltstone and lithic sandstone.||||||16-DEC-15
69864|Quialigo Volcanics|66300|6|Mentioned|p76.|||||Of Bindook Group|Includes Newacres Ignimbrite Member.|||24-OCT-13
69864|Quialigo Volcanics|68592|2|Defined|p1060-2, p1067-72, p1075-8, p1162-92|Pragian|Lochkovian|See also p265, p269, p807, p845 Fig.141, p846, p851, p858-9, p872-3, p875, p878, p1654-7, p1667. New name, after Quialigo Creek. These rocks were originally included within the Gundary Beds (Brunker, Offenberg et al., 1970), the Towrang Beds (Brunker and Offenberg, 1970) or Gundary Formation (Jones, Carr et al., 1995). Now combined with the Bindook Volcanic Complex into the redefined Bindook Group (Thomas and Pogson, 2012). Goulburn area. No type section because of lithological variation and poor exposure; a suggested type locality is described. Thickness probably over 2000m. Also includes six un-named lithological subdivisions, described in some detail. Calc-alkaline. Geochemistry and geophysical properties detailed. Another age determination is 414.4 +/- 2.9 Ma, SHRIMP U-Pb zircon (Black 2006).|411 +/- 3 Ma, 409 +/- 4 Ma (Wilde, 2002).|Unit in Bindook Group.|Saltpetre Andesite Member; Four Winds and Newacres, Ignimbrite Members.|Overlies Bullamalita Conglomerate. Is overlain unconformably by Lambie Group. Partial corrrelative of Tangerang Formation.|A diverse sequence of andesitic pyroclastic rocks and volcanic sandstone and conglomerate; thin horizons of andesitic-basaltic lavas, and minor more quartzose sedimentary rocks blanketed by rhyolitic ignimbrites, topped by andesite lava and breccia.|
69864|Quialigo Volcanics|69159|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Bindook Group.|Includes Saltpetre Andesite Member.||Rhyolitic to dacitic ignimbrite and volcanic sandstone; green-grey, moderately to strongly crystal-rich, pyroxene-plagioclase-phyric andesite.|16-DEC-15
69864|Quialigo Volcanics|70192|5|Briefly described|Map Legend|Pragian|Lochkovian|Dkq. Includes six unnamed members consisting of feldspathic sandstone, plagioclase-augite phyric basalt, lithic sandstone, plagioclase-clinopyroxene phyric andesite, coarse grained quartzite, and andesitic volcaniclastic breccia. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Bindook Group|Includes Four Winds Ignimbrite Member, Newacres Ignimbrite Member, Saltpetre Andesite Member and six unnamed members.|Overlies Bullamalita Conglomerate.|Rhyolitic + dacitic, crystal rich ignimbrite and dacitic breccia, pyroxene-feldspar-phyric andesite and andesitic breccia. Feldspar-pyroxene-phyric basalt minor volcanic conglomerate, laminated siltstone and lithic sandstone.|
69864|Quialigo Volcanics|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes six unnamed members consisting of feldspathic sandstone, plagioclase-augite phyric basalt, lithic sandstone,  plagioclase-clinopyroxene phyric andesite, coarse grained quartzite and andesitic volcaniclastic breccia.||Bindook Group|Includes Four Winds Ignimbrite Member, Newacres Ignimbrite Member, Saltpetre Andesite Member and six unnamed members.||Rhyolitic + dacitic, crystal rich ignimbrite and dacitic breccia, pyroxene-feldspar-phyric andesite and andesitic breccia. Feldspar-pyroxene-phyric basalt minor volcanic conglomerate, laminated siltstone and lithic sandstone.|
69864|Quialigo Volcanics|70661|6|Mentioned|p51, p53|||||||||
69864|Quialigo Volcanics|71040|5|Briefly described|p8 Fig.5, p13, p33|||Canberra Zone. Has an arc-to-backarc magmatic affinity. Deformed by the Tabberabberan Orogeny.|414 +/- 3 Ma to 409 +/- 4 Ma; U-Pb zircon.|||Is overlain unconformably by the Lambie Group.||
69864|Quialigo Volcanics|71069|6|Mentioned|p143, p154, p163|Lochkovian|Lochkovian|Age derived from SHRIMP age for constituent Newacres Ignimbrite Member. Incorporates rocks that were previously a part of the Woodlawn Volcanics. ||Bindook Group|Includes the Newacres Ignimbrite Member.|||
69864|Quialigo Volcanics|71656|6|Mentioned|p13 Fig.2|||Shown only in correlation chart (Fig.2).||Bindook Group||Overlies Bullamalita Conglomerate.||
69864|Quialigo Volcanics|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Bindook Group.|Saltpetre Andesite Member.||Rhyolitic to dacitic ignimbrite and volcanic sandstone; green-grey, moderately to strongly crystal-rich, pyroxene-plagioclase-phyric andesite.|
69864|Quialigo Volcanics|71700|3|Fully described|vi, p7, p24, p62, CD|Pragian|Lochkovian|Named for the Quialigo Creek east of the Goulburn-Winmdellama road. The lithological diversity and poor exposure has meant that no single type or representative section has been proposed. Historically, units now assigned to the Quialigo Volcanics were included in either"Gundary Beds" (Brunker et al. 1970; Felton 1974a) or"Towrang Beds" (Brunker & Offenberg 1970; Offenberg 1974). Subsequently these rocks were mapped as"Gundary Formation" by Jones et al. (1995). Occurs in the Goulburn 250k map sheet in the northwest of the Braidwood 1:100k sheet. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics and  distinguishing features are discussed.  A maximum thickness of 350m is preserved south of Lake Bathurst village. This unit is interpreted to be equivalent to the Long Flat Volcanics.||Bindook Group|Includes the Saltpetre Andesite Member, Newacres Ignimbrite Member and the Four Winds Ignimbrite Member,|Disconformably overlies the Boxers Creek Formation. Overlies the Gundary Volcanics and Bullamalita Conglomerate. Unconformably overlain by the Tarago Conglomerate.|Minor basalt, more common andesite, and voluminous dacite and rhyolite.|
22719|Quintoc Group|43755|6|Mentioned|Fig.1,p548||Carboniferous|||||||
22719|Quintoc Group|44093|5|Briefly described|p232 App. 1|Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||
22719|Quintoc Group|71628|5|Briefly described|p17: 55, 75, 78|||Hastings Block.|||Hyndmans Creek Formation, Pappinbarra beds.|||
23932|Quondolo Formation|22815|5|Briefly described|p115|Tertiary|Tertiary|||||||
23932|Quondolo Formation|22943|6|Mentioned|p516|||||||||
23932|Quondolo Formation|23349|6|Mentioned|252|||||||||
23932|Quondolo Formation|42786|4|Described|p359, p368|||see also Fig.1 P358||||||
27688|Quondong Limestone|5250|6|Mentioned|p42, p50, p54-57||Late Ordovician|Includes brachiopod fauna.||||||
27688|Quondong Limestone|13995|5|Briefly described|p73|Ordovician|Ordovician|Bowan Park, western side of the Molong High. Contains Eastonian bryozoans.||||||
27688|Quondong Limestone|23214|2|Defined|p38|Eastonian|Eastonian|Of Bowan Park Limestone Subgroup. Alternating units of limestone, marl and minor terrigenous mudstone. Max. thickness 34m.||||||
27688|Quondong Limestone|24417|6|Mentioned|p24|||||||||
27688|Quondong Limestone|33063|1|Redefined|p81|Ordovician|Ordovician|Redefinition of Quondong Fm. (Semeniuk, 1970)||||||
27688|Quondong Limestone|33064|5|Briefly described|p449|||O'lies Daylesford Lst. disconformably.||||||
27688|Quondong Limestone|33065|4|Described|p130|||See also P131. Biogenic structures||||||
27688|Quondong Limestone|33737|6|Mentioned|p168|||||||||
27688|Quondong Limestone|33740|6|Mentioned|Fig.1|||||||||
27688|Quondong Limestone|35118|6|Mentioned|Fig.5|||||||||
27688|Quondong Limestone|38219|6|Mentioned|Table 2|||||||||
27688|Quondong Limestone|40136|5|Briefly described|p37|||||||||
27688|Quondong Limestone|41046|6|Mentioned|p144|||||||||
27688|Quondong Limestone|42479|5|Briefly described|p111|||||||||
27688|Quondong Limestone|42603|6|Mentioned|p60|||Bowan Park Group||||||
27688|Quondong Limestone|63278|5|Briefly described|p153|||Of Bowan Park Limestone Subgroup. Underlain by Daylesford Limestone. Contains shelly fauna. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
27688|Quondong Limestone|67322|5|Briefly described|Fig.5; p23, p24|Katian|Katian|Semeniuk (1970, 1973). Age from T. blandus conodonts (Semeniuk 1970, 1973). Occurs in the Bowan Park region.||Of the Bowan Park Limestone Subgroup.||||22-FEB-18
27688|Quondong Limestone|70684|5|Briefly described|p39 Fig.17, p40-41|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian. Shelly faunas indicate water depth of c.30-50m.||Bowan Park Subgroup.||Overlies Daylesford Limestone.||
27688|Quondong Limestone|73209|5|Briefly described|p882|Late Ordovician|Late Ordovician|Bowan Park, NSW.|||||Fossiliferous limestone.|
27688|Quondong Limestone|73210|6|Mentioned|p893 Fig.2|||||||||
27688|Quondong Limestone|73299|6|Mentioned|p1104 Fig.10|Late Ordovician|Late Ordovician|Molong High.||||||
27688|Quondong Limestone|73492|6|Mentioned|p696, p703|||T. blandus Biozone.||Bowan Park Limestone Subgroup||||
31297|Rabbit Creek Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Spherulitic rhyolite, siltstone.||||||
82633|Racehorse Porphyry|71628|5|Briefly described|p19: 148-149|||New (previously unpublished) name; its origin is unclear, involving unpublished students' work (Vickery, 1972; Parker, 1982). Located ~19 km NNE of Torrington; forms a small ( ~800 x 200 m) intrusion. Is possibly a cupola of Mole Leucogranite. The very limited geochemistry is briefly described. Hosts a single (Heffernans tin) deposit: Sn, Pb (Au, Ag, Zn).||Racehorse Suite.||Intrudes Bondonga beds.|Biotite porphyry; extensively altered, locally greisenous.|
81967|Rain Hill Monzodiorite|73154|6|Mentioned|p78|||||||||
81808|Rain Hill Quartz Monzonite|67107|6|Mentioned|p689|||Gidginbung-Temora district. Co-magmatic with epithermal mineralization.|434 +/- 2.3 Ma (hornblende, Ar/Ar).|||||
81808|Rain Hill Quartz Monzonite|72495|6|Mentioned|p227|||Ar-Ar date is derived from Wormald 1993 [actually 1991], cited in Wyborn 1996. Intrudes andesites and latites with probable shoshonitic affinity at Gidginbung.|434.9 +/- 2.3 Ma (Hornblende Ar-Ar)|||||31-MAR-20
80565|Ralpine Valley Sandstone Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Long Flat Volcanics.|||Grey, green to purple, thick- to very thick-bedded, very coarse-grained, poorly-sorted volcaniclastic sandstone to granule conglomerate, with rare interbedded grey, buff to green siltstone and grey to pink cobble conglomerate.|
80565|Ralpine Valley Sandstone Member|71700|3|Fully described|vi, p25, p42-p44, p86, CD|Early Devonian|Early Devonian|Named for the Ralpine Valley property in Tallaganda National Park. The type locality is designated as low road cuttings on the side of the Mulloon Fire Trail between GR 735491 6077381 and GR 735034 6076991. Felton and Huleatt (1975) mapped this unit as the most southerly exposure of the Early Devonian Tarago Conglomerate. This stratigraphic correlation was based mostly on the interpretation that it overlay the"Palerang Formation", which was thought to be a Late Silurian Covan Creek Formation equivalent. Exposed in the Tallaganda State Forest. Derived from reworked material of the Toggannoggra Rhyolite Member. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geophysical characteristics, distinguishing features and economic geology are discussed. This unit has an estimated thickness of 280m. Lithology is discussed in detail.||Long Flat Volcanics||Overlies the Toggannoggra Rhyolite Member. Faulted against (or unconformably overlies) the Abercrombie Formation. Intruded by the Ballallaba Granite.|Grey, green to purple, thick- to very thick-bedded, coarse- to very coarse-grained, poorly sorted volcaniclastic sandstone and granule/pebble conglomerate, with rare interbedded grey, buff to green siltstone and grey to pink cobble conglomerate.|
81736|Ralvona granite''|69801|5|Briefly described|p2, p4-p5, p78-83, p135-136|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs west of Holbrook. Previously the invalid Black Rock Granite (Chappell et al., 1991) (Invalid as 'Black Rock' is used elsewhere in NSW). Petrography, zircon characteristics, SHRIMP analyses and interpretation are detailed.  Probably intrudes the Wagga Group.|429 +/- 2.9 Ma||||Medium- to coarse-grained, leucocratic, tourmaline bearing, two-mica granite.|
83041|Ramleh Volcanics|73202|4|Described|p625-626, p628-630, p632-637, p640|Early Permian|Late Carboniferous|New England Orogen, southern. Only recorded volcanics interbedded with the Manning Group, first described and named by Blair (1983). Predominantly on the western edge of the Echo Hills Formation basin, occurs in the uppermost stratigraphic position with lower intrusions probably representing feeder dykes. Contacts with the Echo Hills Formation are preferentially weathered, one exposed contact displays autoclastic breccia consistent with eruption into wet, soft sediments. Slightly peraluminous. Contains two zircon populations, Carboniferous population may be inherited from the underlying accretionary complex, younger age of 291.7 +/- 2.9 Ma may be a more accurate crystallisation age. Suggested to be comagmatic with the Hillgrove Plutonic Supersuite.|295.6 +/- 4.6 Ma U-Pb SHRIMP|Echo Hills Formation||Interbedded with Echo Hills Formation.|Columnar jointed rhyolite flows with distinct flow banding, typically aphanitic and glassy with rare quartz and plagioclase phenocrysts, glomeroporphyritic; discontinuous sills and dykes intrude lower sections of the Echo Hills Formation.|
36966|Rampsbeck Schist|23720|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of Wongwibinda Metamorphic Complex.  Biotite+/-sillimanite+/-cordierite+/-almandine+/-orthoclase schist, quartzite, amphibolite.||||||15-DEC-04
36966|Rampsbeck Schist|44450|3|Fully described|p12 Table 1|Late Carboniferous|Late Carboniferous|Geological Province: New England Fold Belt.||||||
36966|Rampsbeck Schist|71628|5|Briefly described|p2:41; p8:92|||Upper amphibolite facies.||Wongwibinda Complex.||Is intruded by Mornington Complex and Wards Mistake Monzogranite.||
28263|Ranch Member|23214|3|Fully described|p37|Late Ordovician|Late Ordovician|Of Daylesford Limestone. 34m thick at type section. For lithology descriptions see Semeniuk (1973 a,b).||||||
28263|Ranch Member|24398|5|Briefly described|p259 Fig. 2|Eastonian|Eastonian|Of Bowan Park Limestone.  Geological Province: Lachlan Fold Belt.||||||
28263|Ranch Member|33063|2|Defined|p80|Ordovician|Ordovician|Mb. Daylesford Lst.||||||
28263|Ranch Member|33064|4|Described|p450|||Strat. column P4551||||||
28263|Ranch Member|33065|6|Mentioned|Table 1|||Lithology||||||
28263|Ranch Member|33740|6|Mentioned|Fig.1|||||||||
28263|Ranch Member|38219|6|Mentioned|Table 2|||||||||
28263|Ranch Member|40136|6|Mentioned|p23|||||||||
28263|Ranch Member|41046|6|Mentioned|Fig.2|||||||||
28263|Ranch Member|42479|5|Briefly described|p111|||||||||
28263|Ranch Member|63278|4|Described|p153|||Of the Daylesford Limestone, Bowen Park Limestone Subgroup. Basal unit of the sucession. Very-low-diversity faunal assemblages, dominated by lingulid and rhynchonellid brachiopods. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
28263|Ranch Member|63283|6|Mentioned|p199, p208|Late Ordovician|Late Ordovician|Of the Bowan Park Limestone Subgroup. Geological Province: Molong Volcanic Block. Basal unit of the subgroup.||||||07-FEB-11
28263|Ranch Member|63287|5|Briefly described|p333|Eastonian|Gisbornian|Of the Daylasford Limestone. Age:453+/-4.1Ma. Consists of volcaniclastic detritus and sandstone. Found at the base of bowan Park Limestone Subgroup.||||||07-FEB-11
28263|Ranch Member|63293|5|Briefly described|p470|||Of Daylesford Limestone. Age: 453Ma (LAICPMS zircon in Sst). Has dacite clasts and quartz and hornblende phenocrysts in a sandstone of unit.||||||07-FEB-11
28263|Ranch Member|67106|5|Briefly described|p674, 676-677, 679, 681-683|||Molong Volcanic Belt. Ages and putative sources of zircons detailed.|>c.455 Ma.|Daylesford Limestone.||Overlies Cargo Volcanics.||
28263|Ranch Member|70684|5|Briefly described|p39-41|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian. Basal unit of the Bowan Park Limestone Subgroup. Has a characteristically low-diversity fossil fauna.||Daylesford Limestone.||Is overlain by Bourimbla Limestone Member.|Coarse-grained sandstone to conglomerate, containing volcanic detritus including dacite clasts. Has a distinctive basal red sandstone with quartz grains, siltstone interbeds and rhynchonellide brachiopods.|
28263|Ranch Member|70754|5|Briefly described|p450, p455|Late Ordovician|Late Ordovician|Intertidal deposits. Contains only a few specimens of lingulide brachiopods.||Daylesford Limestone.|||Thin-bedded marls.|
28263|Ranch Member|73210|6|Mentioned|p900 Fig.7|||||Daylesford Limestone?||||
70113|Rantyga Group|62993|6|Mentioned|p35|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup||||19-DEC-21
70113|Rantyga Group|64097|4|Described|p303, p309|Paleoproterozoic|Paleoproterozoic|Of Stevens (2006a) for Redan Sub-block rocks. Of Willyama Supergp. Includes Redan Gneiss (lower), Ednas Gneiss, Mulculca Fm.+Farmcote Gneiss (upper/equiv.to Lady Brassey Fm). Abundant albite-quartz-magnetite rocks +/- amphibole||||||07-FEB-11
70113|Rantyga Group|64741|5|Briefly described|p301 Fig. 4, p305, p307|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Geological province: Broken Hill Domain. New name introduced by Stevens (2006) to include the 4 formations contained in the Redan Domain.||||||07-FEB-11
70113|Rantyga Group|66302|6|Mentioned|p36 Fig.9, p39, p41|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Willyama Supergroup|Includes the Redan Gneiss, Ednas Gneiss, Mulculca Formation, Farmcote Gneiss|||
70113|Rantyga Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Broken Hill Domain, Curnamona Province. Deposited during intra-continental extension.||Willyama Supergroup.|Farmcote, Redan, Ednas Gneisses; Mulculca Formation.|||
70113|Rantyga Group|68126|6|Mentioned|p26||||c.1710-1700 Ma (maximum depositional age).|||||
70113|Rantyga Group|69999|6|Mentioned|p4|||||||||
70113|Rantyga Group|70000|5|Briefly described|p31, p33-35|Statherian|Statherian|Among the oldest outcropping units in the Broken Hill Domain. Protolith was shallow marine, siliciclastic sedimentary rock with an evaporative component, and tholeiitic lavas or subvolcanic intrusions. Age range from bottom and top Formations.|1705-1710 Ma.|Unit in Willyama Supergroup.|Includes Redan, Ednas and Farmcote Gneisses; Mulculca Formation.||Quartz-albite-magnetite +/- hornblende gneiss; basic gneiss.|
70113|Rantyga Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.|||Includes Redan, Ednas and Farmcote Gneisses; Mulculca Formation.||Albite-quartz-magnetite +/- hornblende +/- K feldspar +/- biotite +/- clinopyroxene gneiss and minor basic gneiss.|
70113|Rantyga Group|70657|5|Briefly described|p6 Fig.1, p11 Fig.5, p15|Statherian|Statherian|Broken Hill Domain, Curnamona Province.|1710 +/- 4 Ma -1705 +/- 4 Ma.|Lower Willyama Supergroup|Redan, Ednas, Farmcote Gneisses; Mulculca Formation.|Is overlain by Thackaringa Group.||
70113|Rantyga Group|70658|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|Broken Hill region.||Willyama Supergroup.||||
70113|Rantyga Group|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
70113|Rantyga Group|72461|5|Briefly described|p16 fig 9|||Redan sub-block of the Broken Hill Block.|||Includes the Redan Gneiss, Ednas Gneiss, Mulculca Formatio and the Farmcote Gneiss.|||
70113|Rantyga Group|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian|Redan sub-block.|1710-1705 Ma|Willyama Supergroup||||
70113|Rantyga Group|73308|6|Mentioned|p607 Fig.1||||1710-1705 Ma.|Willyama Supergroup.||||
70113|Rantyga Group|73482|5|Briefly described|p422 Fig.3|||Redan sub-block.||Willyama Supergroup|Farmcote Gneiss, Mulculca Formation, Edna Gneiss, Redan Gneiss|||
70113|Rantyga Group|73512|6|Mentioned|p2-3|Statherian|Statherian|Curnamona Province, Broken Hill Block, Redan Zone. Fluviatile to shallow marine successions.||||||
70113|Rantyga Group|73575|5|Briefly described|p828 Fig.2|||Redan Geophysical Zone.||Willyama Supergroup|Redan Gneiss, Ednas Gneiss, Mulculca Formation, Farmcote Gneiss|||
82623|Rappville Member|70820|6|Mentioned|p37|Cretaceous|Cretaceous|Richmond River catchment area (Casino-Kyogle area) basement aquitard.||||Conformably overlies the Piora Member (aquifer).||
70120|Rasp Ridge Granite Gneiss|64097|1|Redefined|p329 Appdx., p302, p305 Fig. 2|Paleoproterozoic|Paleoproterozoic|Supersedes Rasp Ridge Gneiss of Stevens et al (1993), herein modified. Age: 1683 +/- 3 Ma. Now interpreted as a syn-sedimentary granitic intrusion (concordant metagranite), as is Alma Granite Gneiss also.||||||17-SEP-15
70120|Rasp Ridge Granite Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1683+/-3Ma. Geological province: Broken Hill Domain. Written as Rasp Ridge only.||||||07-FEB-11
70120|Rasp Ridge Granite Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1683+/-3Ma. Geological province: Broken Hill Domain. Name presented only as Rasp Ridge.||||||07-FEB-11
70120|Rasp Ridge Granite Gneiss|70000|6|Mentioned|p34|Statherian|Statherian|||Unit in Silver City Suite.||||
70120|Rasp Ridge Granite Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Silver City Suite.||Overlies Wondervale Well Granite Gneiss.|Quartz-K feldspar-plagioclase-biotite +/- garnet +/- sillimanite gneiss; feldspar megacrysts rare, but sporadic to abundant in a few gneissic lenses.|
70120|Rasp Ridge Granite Gneiss|70657|4|Described|p12, p13 Fig.6, p15, p46|Statherian|Statherian|Curnamona Province: Broken Hill Domain. Abbreviated to Rasp Ridge Gneiss (p12, p46) and to the basic Rasp Ridge (p15). |1683 +/- 3 Ma (Stevens et al., 2000).|Silver City Suite||Intrudes Himalaya Formation (Thackaringa Group). ?Underlies Wondervale Well Granite Gneiss. ?Overlies Georges Bore Granite Gneiss.|Intrusive S-type felsic rocks (granite sills) metamorphosed to gneiss.|
70120|Rasp Ridge Granite Gneiss|73243|6|Mentioned|p52 Fig.1, p68, p72, p76|Statherian|Statherian|[Folded granite gneiss lithology interpreted/assumed as being the Rasp Ridge Granite Gneiss in text]|1683 +/- 3 Ma||||Granite gneiss, folded.|
70120|Rasp Ridge Granite Gneiss|73308|6|Mentioned|p607 Fig.1||||1683 +/- 3 Ma.|||||
70120|Rasp Ridge Granite Gneiss|73482|5|Briefly described|p422 Fig.3, p430|Statherian|Statherian||1683+/-3 Ma|Silver City Suite|||Granite gneiss.|
70120|Rasp Ridge Granite Gneiss|73512|6|Mentioned|p2|||||||||
70120|Rasp Ridge Granite Gneiss|73575|5|Briefly described|p826, p828 Fig.2, p829 Fig.3, p832|Statherian|Statherian|Stratabound. Shown as a single intrusive sill, emplaced before initial deformation. Mapped as the Upper Granite Gneiss and the Lower Granite Gneiss before 1978, and shown as Hangingwall Gneiss and Footwall Gneiss by Webster (2006). See also Rasp Ridge Gneiss p831 Fig.5, p835.|1683+/-3 Ma||Silver City Suite||A single, folded intrusive granitic sill.|
23935|Rast Group|22508|6|Mentioned|p3|||Cobar Supergroup, Lachlan Fold Belt||||||
23935|Rast Group|22768|5|Briefly described|p170|||||||||
23935|Rast Group|22857|5|Briefly described|p170, p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Cobar Supergroup. Deep water turbiditic sediments. Overlies the Boothumble Formation. Max. thickness: 6km. Geological Province: Rast Trough (Darling Basin).||||||
23935|Rast Group|41394|2|Defined|p80|Early Devonian||||||||
23935|Rast Group|41395|6|Mentioned|Map legend|Early Devonian||||||||
23935|Rast Group|41821|6|Mentioned|p11 Fig.5|||Occurs in Kilparney sheet area||||||
23935|Rast Group|42144|5|Briefly described|p605|||See also Fig.3||||||
23935|Rast Group|42521|5|Briefly described|p16, Figs|||||||||
23935|Rast Group|42566|5|Briefly described|Fig.5 P11|||||||||
23935|Rast Group|43089|5|Briefly described|Map Legend|||Of Cobar Supergroup.||||||03-JUN-08
23935|Rast Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
23935|Rast Group|61964|3|Fully described|p14 Fig. 4, p61|Emsian|Pridoli|Of Cobar Supergroup. Nomenclatural history is included. Sedimentary + volcanic sequences. May? unconformably overlie Wagga Group + Weethalle Granite and be, in turn, unconformably overlain by Cocoparra Group. Max. thickness: >2000m.  Geophysics (p224).||||||
23935|Rast Group|62367|5|Briefly described|p4 Fig. 2|Early Devonian|Silurian|Includes Ural Volcanics and Preston Formation.||||||
23935|Rast Group|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes Crossleys Tank and Preston Formations, Ural and Gurragong Volcanics and Melougel Ignimbrite.||||||
23935|Rast Group|63019|5|Briefly described|p920, p921 Fig.2|Emsian|Ludlow|Conformable over Boothumble Formation (KILPARNEY), not exposed on CARGELLIGO. Comprises Crossleys Tank and Preston Formations, and Ural Volcanics on CARGELLIGO; and Gurragong Volcanics, Melougel Ignimbrite and Nyora Granite (not exposed on this sheet).||||||
23935|Rast Group|63891|5|Briefly described|p236|||Includes Ural Volcanics. Overlies Boothumble Formation.||||||
23935|Rast Group|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, App A-VI 3.||||||
23935|Rast Group|69043|6|Mentioned|p12||||||Gurragong Volcanics.|||
23935|Rast Group|69160|5|Briefly described|Map legend|Early Devonian|Early Devonian||||Includes Gurragong Volcanics.||Undifferentiated predominantly felsic volcanic, volcaniclastic and sedimentary rocks.|
23935|Rast Group|69161|5|Briefly described|Map legend|Early Devonian|Early Devonian||||Includes Crossleys Tank Formation, Ural Volcanics and Melougel Ignimbrite.||Undifferentiated predominantly felsic volcanic, volcaniclastic and sedimentary rocks.|
23935|Rast Group|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian||||Includes Crossleys Tank and Preston Formations and Ural Volcanics.|Is overlain by Walters Range Group.|Undifferentiated predominantly felsic volcanic, volcaniclastic and sedimentary rocks.|
23935|Rast Group|70751|6|Mentioned|p4, p6, p12, p15|Devonian|Late Silurian|Cobar Superbasin, Rast Trough.||Cobar Supergroup||||
23935|Rast Group|70950|4|Described|p1028,1030,1033,1045, 1046|Early Devonian|Late Silurian|Geological province: Rast Trough, Central Lachlan Orogen. Detailed mineralisation analysis provided.|||Includes Preston Formation, Ural Volcanics.||Basal syn-rift succession of coarse basement-derived sedimentary rocks, quartz-rich sandstones, basal siliclastic and volcaniclastic rocks and finally A-type (transitional to I-type) submarine to subaerial felsic volcanic rocks.|
23935|Rast Group|71039|6|Mentioned|p6, p23|Devonian|Silurian|||||||
23935|Rast Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|Ural Volcanics, Preston Formation, Gurragong Volcanics, Crossleys Tank Formation.||A sedimentary and volcanic sequence. See constituents for details.|
23935|Rast Group|72908|6|Mentioned|p4|Early Devonian|Silurian|Rast Trough.||||||
23935|Rast Group|72958|6|Mentioned|p6, p8, p11, p61|Lochkovian|Pridoli|Cobar Basin. Nymagee area. Deep-water unit.|||Includes Ural Volcanics.|Part equivalent to Mouramba Group, Kopyje Group.||
23935|Rast Group|73175|6|Mentioned|p1062|||Cobar Basin, southern part.|||Ural Volcanics|||
23935|Rast Group|73578|6|Mentioned|p2|||Cobar Basin.||||||
76042|Rata granite|66934|5|Briefly described|Map legend|Devonian|Silurian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Glen Emu Granite Suite.|||Interpreted S-type granite/granodiorite.|
76042|Rata granite|70718|5|Briefly described|p65, p121|Silurian|Silurian|Informal name, interpreted from geophysics.Aeromag character: Low-amplitude, approximately -30 nT trough, approximately 7×40 km wide. Adjacent anomalies to the east, interpreted as magnetic metamorphic aureoles, extend approximately 8 km from the granite boundary have a peak amplitude of approximately 20 nT. Gravity character:  Associated Bouguer gravity trough with amplitude of approximately -110 ¿ms-2. Magnetic metamorphic aureoles have associated Bouguer gravity high with peak amplitude of approximately 20 ¿ms-2. Interpreted as S-type granite or granodiorite. Referred to as the Rata granodiorite on p65 fig 35.||Glen Emu granite suite||||31-MAY-19
35163|Rathmines Bed|23055|6|Mentioned|Fig13p25|||Tuff marker bed in Upper Pilot coal seam, Newcastle Coal Measures.||||||
27546|Receptaculites Limestone Member|22857|5|Briefly described|p462 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Taemas Limestone. Massive fossiliferous bedded limestone. Max. thickness: 180m. Geological Province: Canberra-Yass Shelf. ||||||
27546|Receptaculites Limestone Member|23898|5|Briefly described|p272 Fig.3|||||||||
27546|Receptaculites Limestone Member|24250|5|Briefly described|p105, p109 Fig.5|Early Devonian|Early Devonian|Of the Taemas Limestone (Murrumbidgee Group). Maximum Thickness: 180m. Overlain by Warroo Limestone Member (conformable). Underlain by Bloomfield Limestone Member (conformable).||||||18-JUN-08
27546|Receptaculites Limestone Member|32483|6|Mentioned|p33|||Refers Browne (1959)||||||
27546|Receptaculites Limestone Member|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27546|Receptaculites Limestone Member|35386|4|Described|p54|||||||||
27546|Receptaculites Limestone Member|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
27546|Receptaculites Limestone Member|42994|6|Mentioned|p14|||||||||
27546|Receptaculites Limestone Member|50230|4|Described|Map legend|Emsian|Emsian|Of the Taemas Limestone (Murrumbidgee Group).  Overlies the Cockatoo Point and Bloomfield Limestone Members.  Massive fossiliferous limestone.||||||
27546|Receptaculites Limestone Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Taemas Limestone (Murrumbidgee Group). Massive fossiliferous limestone.||||||18-JUN-08
27546|Receptaculites Limestone Member|64992|5|Briefly described|p60 Fig. 1, p61|Devonian|Devonian|Part of Taemas-Wee Jasper succession. Of Taemas Fm. Contains Dipnorhynchus kurikae (lungfish) and Speonesudrion iani. The Bloomfield Limestone-Receptaculites Limestone members contact is richest area for dipnoans in Taemas Fm.||||||26-MAR-09
27546|Receptaculites Limestone Member|65214|6|Mentioned|p272|Devonian|Devonian|NSW, Taemas. Appears in text as Receptaculites Limestone Mb. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27546|Receptaculites Limestone Member|68297|6|Mentioned|p186|Emsian|Emsian|Includes shark scales||Said to be of [Taemas Limestone,] Murrumbidgee Group||||
27546|Receptaculites Limestone Member|68592|2|Defined|p982, p984 Fig.162, p985-6, p1024-7|Emsian|Emsian|See also p1899-1903. Originally Receptaculites Limestone of Browne (1959), a prominent unit in her Taemas Stage. When the latter was raised to Formation status by Offenberg (1974), this became the Receptaculites Limestone Member. Type locality described. About 180m thick. Notable for large, frequently silicified examples of Receptaculites australis, as well as a rich and diverse fauna: listed and described.||Unit in Taemas Limestone.||Conformably overlies Bloomfield Limestone Member or Cockatoo Point Limestone Member. Is overlain conformably by Patmore Limestone Member or Warroo Limestone Member.|Blue-grey, well-bedded to massive limestones, predominantly sparse or packed biomicrites; shale content varies considerably.|
27546|Receptaculites Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmtr. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Taemas Limestone||Overlies Bloomfield Limestone Member and Cockatoo Point Limestone Member. Is overlain by Patmore Limestone Member.|Blue-grey, well bedded-massive, fossiliferous limestone.|
27546|Receptaculites Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, well-bedded to massive, fossiliferous limestone.|
27546|Receptaculites Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, well bedded-massive, fossiliferous limestone.|
27546|Receptaculites Limestone Member|71656|3|Fully described|p12 Fig.2, p34-37|Emsian|Emsian|Large specimens of the postulated dasycladacean alga Receptaculites australis are (or were - many having been removed by collectors) characteristic of this unit and give the member its name. Also includes rugose corals, sponges, ostracodes, gastropods, bivalves, fish, bryzoa.||Probably of Taemas Limestone, Murrumbidgee Group||Overlies Cuckatoo Point Member and underlies Patmore Limestone Member.|Fossiliferous limestone.|
25434|Red East Member|23214|3|Fully described|p49|Eastonian|Eastonian|Of Regans Creek Limestone. 60+m thick at type section.||||||
25434|Red East Member|32151|3|Fully described|p202|||||||||
25434|Red East Member|38219|5|Briefly described|p301|||||||||
25434|Red East Member|40136|6|Mentioned|p38|||||||||
25434|Red East Member|42479|5|Briefly described|p109|||||||||
38271|Red Range Microleucogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Fine- to very fine-grained, equigranular pink microleucogranite (phase of Kingsgate Leucogranite).  An I-type granitoid.||||||20-DEC-04
38271|Red Range Microleucogranite|23812|4|Described|p20 Tb.2, p105|Early Triassic|Early Triassic|Age: 245Ma (Rb-Sr). Geological Province: Clarence-Moreton Basin.||||||
38271|Red Range Microleucogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca. 245 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Moonbi Supersuite.||||
38271|Red Range Microleucogranite|69639|5|Briefly described|p1, p10, p16, p26, p94, p218-p219|Lopingian|Lopingian|New England Orogen. Mistakenly referred to as the Red Range Leucomonzogranite on p10. Regarded as the finer-grained carapace of the Kingsgate Leucogranite pluton.|253.2 +/- 1.5 Ma (Cross and Blevin, 2013)|Oban Suite||Intrudes the Wards Mistake Monzogranite.||
38271|Red Range Microleucogranite|71628|4|Described|p3: 53, 55; p8-92; p11-16; p14: 1, 4|||See also p14: 7-10, 16-17, 20-27, 33; p15: 13, 27. Weber et al. (1978). Previously Red Range Granite (Flinter et al., 1972); also Red Range Leucoadamellite (Flinter, 1982). Named after a locality E of Glen Innes. Comprises numerous irregular outcrops extending ~60 km NNE from Capoompeta. Crops out as weathered pavements and boulders. Only recently unroofed, causing mixed interpretations of field relationships (discussed); may be the marginal facies of Kingsgate Syenogranite. Petrology, mineralogy and geochemistry detailed. Associated with many historically significant Mo-W-Bi mineralisations (listed). RELATED UNITS (continued): Possibly intruded by Oban River Leucomonzogranite.|253 +/- 1.5 Ma (Cross and Blevin, 2013).|Red Range Suite.||Intrudes Henry River, Wards Mistake Monzogranites, Emmaville Volcanics and Coffs Harbour Association. Abuts Mount Mitchell Monzogranite and Kingsgate Syenogranite. See COMMENTS for more.|Fine- to very fine-grained, saccharoidal, equigranular to weakly porphyritic, biotite leucosyenogranite to leucomonzogranite; minor medium-grained biotite-hornblende leucomonzogranite-leucosyenogranite, granophyre, and pegmatite. I-type.|
38271|Red Range Microleucogranite|72078|6|Mentioned|p4|Permian|Permian|Geological province: New England Orogen. U-Pb SHRIMP date for zircon is derived from Cross and Blevin 2013).  Features minor scattered Sn-W mineralisation.|253.2+\-1.5 Ma (SHRIMP U-Pb)|||||14-JAN-20
33125|Redan Suite|50606|5|Briefly described|p1.3, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block. Age: 1820Ma.||||||07-NOV-08
26868|Redbank Creek Coal Member|29942|4|Described|Fig.1|||Permian||||||
26868|Redbank Creek Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26868|Redbank Creek Coal Member|39666|6|Mentioned|p66|||||||||
26868|Redbank Creek Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26868|Redbank Creek Coal Member|40805|6|Mentioned|Table 1|||||||||
26868|Redbank Creek Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Malabar Formation.||||
22737|Redbank Falls Monzodiorite|22638|4|Described|p68|Early Devonian||||||||
22737|Redbank Falls Monzodiorite|44192|5|Briefly described|Map Legend||Lochkovian|||||||
31535|Redfern Suite|42726|5|Briefly described|map legend||Carboniferous|||||||
31535|Redfern Suite|68592|6|Mentioned|p1754|||||Unit in Oberon Supersuite.||||
28959|Redhead Conglomerate Member|29922|6|Mentioned|p1791|||||||||
28959|Redhead Conglomerate Member|29926|6|Mentioned|Fig.3|||||||||
28959|Redhead Conglomerate Member|34351|6|Mentioned|p344|||Fig.5.13||||||
28959|Redhead Conglomerate Member|37083|6|Mentioned|p164|||||||||
28959|Redhead Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
28959|Redhead Conglomerate Member|39609|6|Mentioned|Table 1|||||||||
28959|Redhead Conglomerate Member|41130|4|Described|p48|||||||||
28959|Redhead Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
28959|Redhead Conglomerate Member|43447|14|Not recorded|p34,diag.p26|||Part of Cardiff Sub-Group||||||
28959|Redhead Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Glebe Formation||||
26121|Reedy Creek Limestone|13139|5|Briefly described|p9 Fig. 4|Eastonian|Eastonian|||||||
26121|Reedy Creek Limestone|22857|4|Described|p426 App. 1 Tb. A1.5|Eastonian|Eastonian|Of the Barrajin Group. Bedded to massive limestone, tuffaceous arenite and shale, potassic lava. Max. thickness: 850m. ||||||
26121|Reedy Creek Limestone|23181|6|Mentioned|Fig.2|||Correlative of Cliefden Caves Limestone Subgroup.||||||
26121|Reedy Creek Limestone|23213|3|Fully described|p19, Fig.10|Eastonian|Eastonian|Age: Early Eastonian to Middle Eastonian. Extensive fossil assemblage present. of Barrajin Group.||||||19-MAY-16
26121|Reedy Creek Limestone|23214|2|Defined|p47|Eastonian|Eastonian|Of Barrajin Group. Type Section GR 675450 6328450 (base) to GR 674500 6329100 (top).  Limestone with minor, interbedded tuffaceous sandstone and siltstone, marl and calcarenite. Max thickness 850m.||||||04-MAR-09
26121|Reedy Creek Limestone|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
26121|Reedy Creek Limestone|23739|5|Briefly described|p215|Eastonian|Eastonian|||||||
26121|Reedy Creek Limestone|24215|5|Briefly described|p804 Fig. 3|||Geological Province:  Lachlan Fold Belt||||||
26121|Reedy Creek Limestone|24247|6|Mentioned|p45|Late Ordovician|Late Ordovician|||||||
26121|Reedy Creek Limestone|29362|2|Defined|p190|Late Ordovician|Late Ordovician|||||||
26121|Reedy Creek Limestone|30044|6|Mentioned|p17|||||||||
26121|Reedy Creek Limestone|30139|5|Briefly described|Table 1|||||||||
26121|Reedy Creek Limestone|32151|6|Mentioned|p206|||Stromatoporoids||||||
26121|Reedy Creek Limestone|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26121|Reedy Creek Limestone|32672|6|Mentioned|p672|||||||||
26121|Reedy Creek Limestone|33116|4|Described|p202|||Ord.||||||
26121|Reedy Creek Limestone|33121|6|Mentioned|p85|||Correlation Table. Late Ord.||||||
26121|Reedy Creek Limestone|33285|6|Mentioned|p30|||Late Ord.||||||
26121|Reedy Creek Limestone|33735|6|Mentioned|p206|||||||||
26121|Reedy Creek Limestone|33737|6|Mentioned|p167|||||||||
26121|Reedy Creek Limestone|33741|6|Mentioned|Fig.1|||Ordovician. Fauna.||||||
26121|Reedy Creek Limestone|34404|4|Described|p81|||||||||
26121|Reedy Creek Limestone|34575|6|Mentioned|p637|||See also PP638,653 etc. Ordovician.||||||01-SEP-08
26121|Reedy Creek Limestone|34692|6|Mentioned|p184|||||||||
26121|Reedy Creek Limestone|34895|6|Mentioned|Fig. 1|||||||||
26121|Reedy Creek Limestone|35118|6|Mentioned|Fig.5|||||||||
26121|Reedy Creek Limestone|35291|6|Mentioned|p17|||||||||
26121|Reedy Creek Limestone|35412|6|Mentioned|Fig.9|||||||||
26121|Reedy Creek Limestone|35415|6|Mentioned|Fig.2|||Stratigraphic correlations.||||||
26121|Reedy Creek Limestone|38219|6|Mentioned|p301|||||||||
26121|Reedy Creek Limestone|39331|6|Mentioned|Fig.6-1|||||||||
26121|Reedy Creek Limestone|39663|6|Mentioned|Table 1|||||||||
26121|Reedy Creek Limestone|40136|5|Briefly described|p37|||||||||
26121|Reedy Creek Limestone|40328|6|Mentioned|p148|||||||||
26121|Reedy Creek Limestone|42479|4|Described|p109|||||||||
26121|Reedy Creek Limestone|43640|5|Briefly described|Map Legend||Ordovician|||||||
26121|Reedy Creek Limestone|43782|5|Briefly described|Map Legend|Eastonian|Eastonian|Of Barrajin Group.||||||01-SEP-08
26121|Reedy Creek Limestone|44988|14|Not recorded|p13||Early Ordovician|(Middle Ordovician)||||||
26121|Reedy Creek Limestone|48926|6|Mentioned|p23|||P23 et seq.||||||
26121|Reedy Creek Limestone|63278|5|Briefly described|p146 Fig. 2a, p152|Late Ordovician|Late Ordovician|Underlain by Yuranigh Limestone Member. Geological Province: Molong Volcanic Belt, LFB. Consists of limestone.||||||07-FEB-11
26121|Reedy Creek Limestone|63283|6|Mentioned|p194 Fig. 2, p200|Eastonian|Eastonian|Overlian by Cheesemans Creek Formation. Geological Province: Molong Volcanic Belt. Consists of limestone.||||||07-FEB-11
26121|Reedy Creek Limestone|63286|6|Mentioned|p308 Fig. 9|Late Ordovician|Late Ordovician|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
26121|Reedy Creek Limestone|63287|4|Described|p317 Fig. 2, p349|Eastonian|Eastonain|Of Barrajin Group.Underlain conformably to disconfomably Fairbridge Volcanics. Geological Province: Molong Volcanic Belt. Consists of Limestone.||||||07-FEB-11
26121|Reedy Creek Limestone|63290|5|Briefly described|p397 Fig. 3(b)|Eastonian|Eastonian|Overlain by Cheesemans Creek Formation. Geological Province: Molong Volcanic Belt.||||||
26121|Reedy Creek Limestone|63293|5|Briefly described|p470, p468 Fig. 2|Eastonian|Gisbornian|Overlain by Cheesmans Creek Formation, underlain by Fairbridge Volcanics and Oakdale Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
26121|Reedy Creek Limestone|64295|5|Briefly described|p200 Fig. 2, p202|||||||||
26121|Reedy Creek Limestone|64826|5|Briefly described|p1040 Tb. 1|Eastonian|Eastonian|Of Cabonne Group.||||||04-MAR-09
26121|Reedy Creek Limestone|64963|5|Briefly described|p182 Fig. 2, p184, p190|||Within the Molong Volcanic Belt.||||||22-APR-09
26121|Reedy Creek Limestone|67106|6|Mentioned|p673, 679|||Molong Volcanic Belt.||||||
26121|Reedy Creek Limestone|67322|5|Briefly described|Fig.5; p23|Katian|Katian|Macquarie Arc. Ross (1961); Adrian (1971). Occurs in the North Molong Volcanic Belt.||Of the Cabonne Group.||Overlies Yuranigh Limestone Member (of Fairbridge Volcanics) unconformably. Correlative of the Cliefden Caves Limestone Subgroup. Overlain by the Cheesemans Creek Formation.||22-FEB-18
26121|Reedy Creek Limestone|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
26121|Reedy Creek Limestone|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Post-phase 2 volcanic hiatus. Age: deposited from early to late Eastonian. Shown as Reedy Ck Limestone.|c. 455-450 Ma|Cabonne Group||||
26121|Reedy Creek Limestone|70684|5|Briefly described|p18-19, p27-30, p41, p74|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Up to c.850m thick. Crops out over 24km along strike, N and S of Molong.||||Conformably overlies Fairbridge Volcanics. Is overlain by Cheesemans Creek Formation. Intruded by Copper Hill Complex.|Fossiliferous, thin-bedded, mud-rich calcarenites overlain by more massive and pure carbonates up-section.|
26121|Reedy Creek Limestone|70754|5|Briefly described|p448-449, p450 Fig.2, p451|Late Ordovician|Late Ordovician|Some fossil species named.||||Overlies ?unconformably Fairbridge Volcanics. Is overlain by Cheesemans Creek Formation. Coeval with Cliefden Caves Limestone Subgroup.||
26121|Reedy Creek Limestone|72263|5|Briefly described|p516-517|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen.||||Underlain conformably by Fairbridge Volcanics.||
26121|Reedy Creek Limestone|73209|5|Briefly described|p880|Late Ordovician|Late Ordovician||||||Bedded to massive limestone.|
22748|Reefton Dolerite|22638|3|Fully described|p80||Late Devonian|New name.||||||31-MAR-20
22748|Reefton Dolerite|24101|6|Mentioned|p110 Fig.3|||Geological Province: Lachlan Fold Belt||||||
22748|Reefton Dolerite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
22748|Reefton Dolerite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
24470|Reevesdale Basalt|40132|2|Defined|p239|late Eocene|late Eocene|||||||
24470|Reevesdale Basalt|64238|5|Briefly described|Map legend|Cenozoic|Cenozoic|Alkali olivine basalt and nephelinite.||||||19-NOV-08
24470|Reevesdale Basalt|68592|2|Defined|p37, p228-9, p1787-9, p1798-1803, p1909|Eocene|Eocene|Carr, Jones et al. (1979); after Reevesdale property. A proposed type section, which adds to the type locality of Carr, Jones et al. (1979), is described. Thickness variable: up to 58m maximum. Bungonia region. Geophysical properties described. A hard-rock quarry for aggregate at Ardmore Park was approved in 2009. K-Ar dating by Wellman and McDougall (1974); Jones, (1986) respectively.|47.3 +/- 1.2 Ma and 45.4 +/- 1.1 Ma|||Correlated with Tomboye, Endrick River, Crookwell Basalts and Monaro Volcanics.|Dark grey to black, ophitic, hard and generally massive alkali olivine basalt; numerous stacked flat-lying lavas with zones of amygdales on upper flow surfaces; also numerous unmapped thin basalt and dolerite dykes.|
24470|Reevesdale Basalt|69159|5|Briefly described|Map legend|Eocene|Eocene||||||Grey to black, fine- to medium-grained, olivine basalt and red to orange pisolitic ironstone.|07-SEP-15
24470|Reevesdale Basalt|70192|5|Briefly described|Map Legend|Eocene|Eocene|Czr. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.|||||Fine-medium grained alkali olivine basalt with minor basalt and dolerite dykes.|
24470|Reevesdale Basalt|70542|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Fine-medium grained alkali olivine basalt with minor basalt and dolerite dykes.|
24470|Reevesdale Basalt|70661|6|Mentioned|p231, p232|||||||Correlated with the Robertson Basalt||
24470|Reevesdale Basalt|71699|5|Briefly described|Map legend.|Neogene|Paleogene||||||Grey to black, fine- to medium-grained, olivine basalt and red to orange, pisolitic ironstone.|
24470|Reevesdale Basalt|71700|2|Defined|vi, p7, p33, CD|Cenozoic|Middle Eocene|Named for the property of Reevesdale in Goulburn100. A type section defined by M.M. Scott (in Thomas & Pogson 2012) includes the type locality of Carr, Jones et al. (1980) and follows a transect of local maximum change in elevation of the unit at the surface (Wray et al. 1993), from a base at Inverary Creek at GR 771590 6135020 to a top at Inverary Trigonometrical Station at GR 772240 6133480. Outcrops in the Braidwood 1:100k sheet area. Middle Eocene maximum age is derived from correlations of fossil pollen which occurs below this basalt (Truswell and Owen (1988). Distribution, geomorphic expression, depositional environment, distinguishing features, economic geology, metamorphism and geophysical characteristics are discussed.  This unit has an estimated maximum thickness of 30m directly northeast of Lake Bathurst. Thickness in drilling is estimated between 8 and 58m. K-Ar dates are derived from Wellman and McDougall, 1974 and Jones, 1986.|47.3 +/- 1.2 Ma and 45.4 +/- 1.1 Ma (K-Ar dates)|||Equivalent to the Crookwell Basalt, Endrick River Basalt and the Tomboye Basalt.|Fine- to medium-grained alkali olivine basalt.|
24470|Reevesdale Basalt|73581|5|Briefly described|p22-23|Eocene|Eocene|Southern Highlands Volcanic Province. List of K-Ar ages provided from Ruxton and Taylor (1982), and Wellman and McDougall (1974b).|47.3 Ma, 45.5 Ma, 43.8 Ma, 42.9 Ma K-Ar||||Low-K tholeiite to alkali basalt. High-Ti mineralogy and mantle xenoliths.|
26869|Regans Creek Limestone|5250|6|Mentioned|p45, p50||Late Ordovician|Includes Ashton Member, Checkers Member. ||||||
26869|Regans Creek Limestone|22857|5|Briefly described|p424 App.1 Tb.A1.5|Ordovician|Ordovician|Of the Barrajin Group. Thick-bedded to massive wackestone, limey mudstone, calcarenite, siliceous nodules. Max. thickness: 158m.||||||
26869|Regans Creek Limestone|23213|6|Mentioned|p19|||||||||
26869|Regans Creek Limestone|23214|3|Fully described|p48|Eastonian|Eastonian|Of Barrajin Group. Age determined by fossil assembleges.||||||
26869|Regans Creek Limestone|24398|5|Briefly described|p264, p259 Fig. 2|Eastonian|Eastonian|Contains the Ashton Member.  Geological Province: Lachlan Fold Belt.||||||
26869|Regans Creek Limestone|32151|3|Fully described|p198|||U.Gisbornian? - L.Eastonian? p196||||||09-MAY-12
26869|Regans Creek Limestone|32590|6|Mentioned|p10|||||||||
26869|Regans Creek Limestone|33006|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle and Upper OrdovicianM - U||||||
26869|Regans Creek Limestone|33282|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle and Upper Ordovician||||||09-MAY-12
26869|Regans Creek Limestone|33735|6|Mentioned|p206|||||||||
26869|Regans Creek Limestone|33737|6|Mentioned|p168|||||||||
26869|Regans Creek Limestone|33741|6|Mentioned|Fig.1|||Ordovician. Fauna.||||||
26869|Regans Creek Limestone|34404|4|Described|p81|||||||||
26869|Regans Creek Limestone|34575|6|Mentioned|p637|||Ordovician. See also PP638,640,643 etc.||||||
26869|Regans Creek Limestone|35118|6|Mentioned|Fig.5|||||||||
26869|Regans Creek Limestone|38219|5|Briefly described|p300|||||||||
26869|Regans Creek Limestone|39331|6|Mentioned|Fig.6-1|||||||||
26869|Regans Creek Limestone|39657|6|Mentioned|M30|||||||||
26869|Regans Creek Limestone|39663|6|Mentioned|Table 1|||||||||
26869|Regans Creek Limestone|40136|5|Briefly described|p38|||See also p30||||||16-JAN-12
26869|Regans Creek Limestone|40328|6|Mentioned|Plate 4|||||||||
26869|Regans Creek Limestone|42479|4|Described|p109|||||||||
26869|Regans Creek Limestone|42561|6|Mentioned|p87|||||||||
26869|Regans Creek Limestone|43515|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(Provisional Edition) (M.-U.Ord)||||||
26869|Regans Creek Limestone|43516|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(M.-U.Ord)||||||
26869|Regans Creek Limestone|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Barrajin Group. Consists of thick-bedded to massive, wackestone and packstone, limey mudstone, calcarenite, silicious nodules.||||||17-JUL-08
26869|Regans Creek Limestone|43782|5|Briefly described|Map Legend|Eastonian|Gisbornian|of Barrajin Group.||||||
26869|Regans Creek Limestone|44086|14|Not recorded|p97-99,102,105,107,|Late Ordovician|Early Ordovician|Pl.IV. See also Lexicon. (Upper Middle Ordovician-Late Ordovician)||||||
26869|Regans Creek Limestone|48926|6|Mentioned|p22|||P22 et seq.||||||
26869|Regans Creek Limestone|63287|4|Described|p317 Fig. 2, p320, p322 Fig. 5, p347|Eastonian|Gisbornian|Of Barrajin Group. Overlain by Malongulli Formation. Geological Province: Molong Volcanic Belt. Consists of limestone.||||||09-MAY-12
26869|Regans Creek Limestone|64963|5|Briefly described|p182 Fig. 2|||Within the Molong Volcanic Belt.||||||22-APR-09
26869|Regans Creek Limestone|67322|5|Briefly described|p24|Katian||Age based on the correlative Cliefden Caves Limestone Subgroup, along strike to the south.||||Correlative of the Cliefden Caves Limestone Subgroup.||22-FEB-18
26869|Regans Creek Limestone|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
26869|Regans Creek Limestone|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Post-phase 2 volcanic hiatus. Age: deposited from early to late Eastonian. Shown as Regans Ck Limestone.||Cabonne Group||||
26869|Regans Creek Limestone|70754|6|Mentioned|p448|||||||||
26869|Regans Creek Limestone|73209|5|Briefly described|p880|Late Ordovician|Late Ordovician||||||Thick-bedded to massive wackestone, limey mudstone, calcarenite.|
23938|Regina Volcanics|22857|4|Described|p440 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Mount Hope Group (Cobar Supergroup). Max. thickness: 400m. Geological Province: Mount Hope Trough.||||||
23938|Regina Volcanics|37772|4|Described|p6|||||||||
23938|Regina Volcanics|40269|4|Described|p147|||||||||
23938|Regina Volcanics|40913|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
23938|Regina Volcanics|41126|2|Defined|p38|early Lochkovian|early Lochkovian|||||||
23938|Regina Volcanics|41821|6|Mentioned|p15|||Occurs in the Mount Allen sheet area||||||
23938|Regina Volcanics|42144|5|Briefly described|Fig.3|||||||||
23938|Regina Volcanics|42521|5|Briefly described|Fig.3b P16|||||||||
23938|Regina Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
23938|Regina Volcanics|43089|5|Briefly described|Map Legend|||of Mount Hope Group||||||
23938|Regina Volcanics|43202|5|Briefly described|Table 2,p20.|||||||||
23938|Regina Volcanics|70751|6|Mentioned|p5, p9-p10, p17, p19, p28, p30, p38||||418.7 +/- 3.1 (SHRIMP, this study)|Mount Hope Group||||
23938|Regina Volcanics|70950|5|Briefly described|p1029,1032|||Geological province: Central Lachlan Orogen. Suggested by Simpson (2014) to be part of Mount Halfway Volcanics.||Unit of Mount Hope Group.|||Volcaniclastic-rich host sequence, that includes crystal-rich siliceous volcaniclastic sandstone/breccia and pumice breccia.|
23938|Regina Volcanics|72908|6|Mentioned|p3, p30|||Simpson (2014) (see also Downes, Blevin et al., 2016) proposed that the stratigraphy of the Mount Hope Group be simplified, with the Ambone, Regina, Goona and part of the Coando Volcanics being grouped into the Mount Halfway Volcanics.||Mount Hope Group||||
28960|Reids Mistake Formation|22578|6|Mentioned|Fig.9 p399, p402|||of Newcastle Coal Measures||||||
28960|Reids Mistake Formation|23055|6|Mentioned|Fig11p23|||See also Reids Mistake Tuff, p25.||||||
28960|Reids Mistake Formation|24040|5|Briefly described|p484|||Geological Province: Sydney Basin - at Swansea south of Newcastle. Shows a general tilting of tree stumps in its tuffaceous rocks.||||||21-AUG-08
28960|Reids Mistake Formation|24471|5|Briefly described|p33|Late Permian|Late Permian|Of Illawarra Coal Measures. Stratigraphically correlates to Eckersley Formation. Geological Province: Sydney Basin.||||||07-FEB-11
28960|Reids Mistake Formation|29922|6|Mentioned|Appendix 4|||||||||
28960|Reids Mistake Formation|29926|6|Mentioned|Fig.3|||||||||
28960|Reids Mistake Formation|29942|4|Described|Fig.2|||||||||
28960|Reids Mistake Formation|34351|6|Mentioned|p346|||Fig.5.13||||||
28960|Reids Mistake Formation|35319|3|Fully described|p473|||||||||
28960|Reids Mistake Formation|35803|6|Mentioned|p319|||Discussion re volcanism.||||||
28960|Reids Mistake Formation|37083|6|Mentioned|p164|||||||||
28960|Reids Mistake Formation|39292|6|Mentioned|Fig. 6.2|||||||||
28960|Reids Mistake Formation|39308|6|Mentioned|Fig. 23.4|||||||||
28960|Reids Mistake Formation|39609|6|Mentioned|Table 1|||||||||
28960|Reids Mistake Formation|41479|6|Mentioned|Fig.2|||||||||
28960|Reids Mistake Formation|42767|6|Mentioned|p5|||||||||
28960|Reids Mistake Formation|45090|6|Mentioned|p186|||Stratigraphic table||||||
28960|Reids Mistake Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Boolaroo Subgroup|Included Seahampton Sandstone Member.|||
70325|Rhyanna Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Greenish-grey, thin- to medium-bedded, siltstone grading up from fine-gr.sandstone at bed bases, interbedded with silicified vitric and fine-gr. felsic tuff; rare olistostrome deposits; 2 subunits.||||||09-SEP-08
70325|Rhyanna Formation|68592|2|Defined|p833-41, p852 Fig.143, p856-7, p861-3|Lochkovian|Lochkovian|See also p725-6, p728, p730-2 Fig.132, p734, p757, p866, p868-70, p873-4, p887, p889-91, p1890-1. New name. Previously included in Argyle Formation, Whipbird Creek Formation and lower Lambie Group (Scheibner 1973), undifferentiated Upper Silurian and Lambie Group (Brunker and Offenberg 1970), undifferentiated Taralga Group (Powell and Fergusson 1979), Towrang Beds (Pickett 1982), and Adaminaby Group and Gundary Formation by Branagan and Packham (2000). Type section is thickest section (~1250 m) and all lithologies are present, however base not well exposed, and top is an erosional unconformity. Representative, and other, exposures of 'lower' portion are provided. Deposition in a moderately deep marine environment by turbidity currents and mass flow processes, with ash-rich volcaniclastic detritus from an intermediate to mafic volcanic source. Metamorphism: low grade greenschist facies regionally; contact metamorphosed by (intruding) Forest Lodge Quartz Monzodiorite sills. Early Lochkovian age. Is a deepwater distal facies equivalent of Gundary Volcanics; 'upper' sequence is inferred equivalent to 'upper' portion of Gundary Volcanics (Bradfordville Volcaniclastic Member and upper part of Back Station Ignimbrite Member) which overlie 'lower' Rhyanna Formation. In Fig.143, Gundary Volcanics incorrectly brackets Rhyanna Formation as a constituent. Fossil fauna listed.||Unit in Mount Fairy Group.||Conformably overlies Argyle and Covan Creek Formations. Is unconformably (erosionally) overlain by Lambie Group; is overlain by Bradfordville Volcaniclastic Member.|Broadly subdivided into a 'lower' sequence of rhythmically bedded, volcaniclastic sandstone-siltstone-mudstone and an 'upper' sequence of massive, silicified, volcanic mudstone; largely turbiditic; olistostrome horizon.|
70325|Rhyanna Formation|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfh. Includes two unnamed subunits of massive-faintly planar laminated volcanic mudstone and olisostrome with megaclasts of quartzose to quartz lithic sandstone, siltstone, limestone and mafic igneous rock. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group|Includes two unnamed members.|Overlies Argyle Formation. Is overlain by Bradfordville Volcaniclastic Member, and undifferentiated Gundary Volcanics.|very thin-thickly bedded, fine-medium grained, normally graded, ash rich, volcaniclastic sandstone and siltstone. Massive volcaniclastic mudstone; generally massive-planar laminated, thin-thick bedded, silicified volcanic mudstone.|
70325|Rhyanna Formation|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|||Fine-medium grained, normally graded, ash rich, volcaniclastic sandstone and siltstone and mudstone. The mudstone is massive-planar laminated, thin-thickly bedded, silicified. Minor fine-grained lithic-quartz sandstone present.|
70325|Rhyanna Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed subunits of massive-faintly planar laminated volcanic mudstone and olisostrome with megaclasts of quartzose to quartz lithic sandstone, siltstone, limestone and mafic igneous rock.||Mount Fairy Group|Includes two unnamed members||very thin-thickly bedded, fine-medium grained, normally graded, ash rich, volcaniclastic sandstone and siltstone. Massive volcaniclastic mudstone; generally massive-planar laminated, thin-thick bedded, silicified volcanic mudstone.|
70325|Rhyanna Formation|71069|5|Briefly described|p134, p135, p137-138 fig 44, p143, p170|||Replaces the Whipbird Creek Formation.Up to 1250m thick. Contains condont fossils. ||Mount Fairy Group||Intruded by the Forest Lodge Quartz Monzodiorite. Unconformably overlain by the Gundary Volcanics. Conformably overlies the Covan Creek Formation and Argyle Formation.|Massive, silicified volcanic mudstone.|
70325|Rhyanna Formation|71656|5|Briefly described|p13 Fig.2, p30|Lochkovian|Pridoli|Various ages obtained from fossils in allochthonous blocks and clasts.The youngest fossils indicate an earliest Devonian depositional age for this unit.||Mount Fairy Group||Mount Fairy Group. Partially equivalent to Gundary Volcanics.|Allochthonous limestone blocks emplaced as an olistostrome.|
74781|Ridge Monzogranite|61789|5|Briefly described|p303, p305|||Previously identified as Stanthorpe Adamellite. Granular, medium-grained, seriate, biotite-bearing monzogranite. Intrudes Permian felsic volcanics. Intruded by Undercliffe Falls Monzogranite. Not believed to be regionally extensive.||||||27-OCT-08
74781|Ridge Monzogranite|61790|6|Mentioned|p321|||One of a group of hybrid monzogranite suites. ?Abbreviated to Ridge Monzogranite.||||||
26871|Ripley Road Sandstone|12597|5|Briefly described|p491, p492 Tb.1, p496|Pliensbachian|Hettangian|Clarence-Moreton Basin. Up to 1200m thick.||Unit in Woogaroo Subgroup.|||Massive, cross-bedded, fine- to coarse-grained, sub-labile to quartzose sandstone.|
26871|Ripley Road Sandstone|13516|5|Briefly described|p159 fig 8|Early Jurassic|Early Jurassic|From Clarence-Moreton Basin.||Of Woogaroo Subgroup||||
26871|Ripley Road Sandstone|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Rhaetian|Of the Woogaroo Subgroup (Bundamba Group). Quartz arenite, granule conglomerate. Max. thickness: 150m. Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|22865|6|Mentioned|Fig.22.10ap318|||||||||
26871|Ripley Road Sandstone|23435|5|Briefly described|p66|||of Woogaroo Subgroup.||||||
26871|Ripley Road Sandstone|23799|5|Briefly described|p46|Late Triassic|Late Triassic|See also p48 Fig. 3.  Of the Woogaroo Subgroup.  Overlies Raceview Formation.  Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|23811|5|Briefly described|Map Legend|Pliensbachian|Hettangian|Of Woogaroo Subgroup.  Thick-bedded, fine- to medium- to very coarse-grained quartz-rich sandstone and quartz-rich granule conglomerate.  A grey clay matrix is characteristic of fresh rock.  Geological Province: Clarence-Moreton Basin.||||||09-MAY-13
26871|Ripley Road Sandstone|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Late Triassic|Of Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|23843|5|Briefly described|p456 Table 1|Jurassic|Late Triassic|Of Woogaroo Sub-Group. Geological Province:Moreton Basin.  Maximum thickness: 400m.||||||
26871|Ripley Road Sandstone|24081|5|Briefly described|p451|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group.  Geological Province: Nambour Basin.||||||
26871|Ripley Road Sandstone|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|29385|6|Mentioned|p82|||Jurassic.||||||
26871|Ripley Road Sandstone|30086|5|Briefly described|p4|||Triassic age. Part of Bundamba Group.||||||
26871|Ripley Road Sandstone|30302|6|Mentioned|p415|||Refers to Staines(1964)||||||
26871|Ripley Road Sandstone|30458|6|Mentioned|p2|||||||||
26871|Ripley Road Sandstone|30463|6|Mentioned|p466|||See also P471||||||
26871|Ripley Road Sandstone|30464|6|Mentioned|p3|||||||||
26871|Ripley Road Sandstone|30465|6|Mentioned|p4|||||||||
26871|Ripley Road Sandstone|30466|6|Mentioned|p14|||Triassic age||||||
26871|Ripley Road Sandstone|30470|6|Mentioned|p459|||||||||
26871|Ripley Road Sandstone|30472|6|Mentioned|p132|||Pollen distribution||||||
26871|Ripley Road Sandstone|30474|6|Mentioned|p251|||Correlation chart||||||
26871|Ripley Road Sandstone|30475|6|Mentioned|Fig.14.3|||||||||
26871|Ripley Road Sandstone|30477|6|Mentioned|p461|||||||||
26871|Ripley Road Sandstone|30915|6|Mentioned|p100|||||||||
26871|Ripley Road Sandstone|31118|4|Described|p320|||||||||
26871|Ripley Road Sandstone|31259|6|Mentioned|p325|||Refers Staines (1964)||||||
26871|Ripley Road Sandstone|32136|6|Mentioned|p5|||Miospores||||||
26871|Ripley Road Sandstone|32176|6|Mentioned|p2|||Bundamba Gp. See also P3, Figs. 2&3.||||||
26871|Ripley Road Sandstone|32179|6|Mentioned|p3|||Trias.||||||
26871|Ripley Road Sandstone|32180|6|Mentioned|Table 1|||||||||
26871|Ripley Road Sandstone|32492|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
26871|Ripley Road Sandstone|33381|6|Mentioned|p118|||See also P122||||||
26871|Ripley Road Sandstone|33476|6|Mentioned|p99|||||||||
26871|Ripley Road Sandstone|34010|6|Mentioned|Cor. chart|||U.Triassic||||||
26871|Ripley Road Sandstone|34354|6|Mentioned|p3|||Triassic. See also P12.||||||
26871|Ripley Road Sandstone|34505|6|Mentioned|p3|||Bundamba Group. See Figs.8,9,10,11||||||
26871|Ripley Road Sandstone|35101|6|Mentioned|p51|||||||||
26871|Ripley Road Sandstone|35866|6|Mentioned|p399|||||||||
26871|Ripley Road Sandstone|36243|6|Mentioned|Table 8A|||||||||
26871|Ripley Road Sandstone|36779|6|Mentioned|p7|||||||||
26871|Ripley Road Sandstone|36825|6|Mentioned|p12|||||||||
26871|Ripley Road Sandstone|37111|6|Mentioned|Table 1|||||||||
26871|Ripley Road Sandstone|37122|5|Briefly described|Table 1|||||||||
26871|Ripley Road Sandstone|37375|4|Described|p474|||||||||
26871|Ripley Road Sandstone|37456|6|Mentioned|p268|||||||||
26871|Ripley Road Sandstone|37463|6|Mentioned|p483|||||||||
26871|Ripley Road Sandstone|37616|6|Mentioned|p33|||||||||
26871|Ripley Road Sandstone|38074|5|Briefly described|Table 1|||||||||
26871|Ripley Road Sandstone|38076|6|Mentioned|Table 3|||||||||
26871|Ripley Road Sandstone|38306|6|Mentioned|p512|||||||||
26871|Ripley Road Sandstone|38307|4|Described|p522|||||||||
26871|Ripley Road Sandstone|38441|6|Mentioned|Map legend|Early Jurassic|Rhaetian|Rhaetian - Early Jurassic||||||
26871|Ripley Road Sandstone|39445|5|Briefly described|Table 10|||||||||
26871|Ripley Road Sandstone|39907|4|Described|p14|||Sedimentology||||||
26871|Ripley Road Sandstone|39943|6|Mentioned|Table 10A|||||||||
26871|Ripley Road Sandstone|40623|5|Briefly described|p107|||||||||
26871|Ripley Road Sandstone|41591|6|Mentioned|p18|||||||||
26871|Ripley Road Sandstone|41631|4|Described|p10|||See also Fig.2||||||
26871|Ripley Road Sandstone|41906|3|Fully described|Table 2 P16|||||||||
26871|Ripley Road Sandstone|42248|6|Mentioned|p397|||||||||
26871|Ripley Road Sandstone|42316|6|Mentioned|p8|||||||||
26871|Ripley Road Sandstone|42336|5|Briefly described|Table 1 P5|||||||||
26871|Ripley Road Sandstone|42405|6|Mentioned|Table 3 P.7|||||||||
26871|Ripley Road Sandstone|42463|6|Mentioned|Fig.3 P170|||||||||
26871|Ripley Road Sandstone|42525|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group (Bundama Group).||||||15-JUL-04
26871|Ripley Road Sandstone|42869|5|Briefly described|Table 1, P33|||of Woogaroo Subgroup||||||
26871|Ripley Road Sandstone|42893|6|Mentioned|p11|||||||||
26871|Ripley Road Sandstone|42894|5|Briefly described|Fig.1 P20|||||||||
26871|Ripley Road Sandstone|43001|6|Mentioned|p122|||||||||
26871|Ripley Road Sandstone|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||12-APR-05
26871|Ripley Road Sandstone|43736|5|Briefly described|Table 1,p4|||||||||
26871|Ripley Road Sandstone|43910|4|Described|p1,3,10,16-18,Fig.2|||||||||
26871|Ripley Road Sandstone|44450|5|Briefly described|p27|||Underlying unit Raceview Formation. Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|44734|14|Not recorded|p5,6,12,13,16,17,19|||||||||
26871|Ripley Road Sandstone|44774|2|Defined|p30-32||Late Triassic|Conformably overlies Raceview Formation. Upper limit hard to delineate, possible upward gradation into Marburg Sandstone.||||||
26871|Ripley Road Sandstone|44775|4|Described|p9||Late Triassic|||||||
26871|Ripley Road Sandstone|44776|14|Not recorded|p4||Late Triassic|||||||
26871|Ripley Road Sandstone|44884|4|Described|p2,3,Fig.1|||||||||
26871|Ripley Road Sandstone|45110|6|Mentioned|p83|||||||||
26871|Ripley Road Sandstone|48917|3|Fully described|p16|||See also p13. Stratigraphic table. Refers Staines (1964)||||||10-JUN-22
26871|Ripley Road Sandstone|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup.  Arenite and conglomerate.||||||
26871|Ripley Road Sandstone|60281|5|Briefly described|p27, Fig.18 App 1|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Quartz sandstone, granule conglomerate.  Overlies the Raceview Formation; overlain by Gatton Sandstone.  Max. thickness: 150m. Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|60993|4|Described|p4-5, p6 Fig. 2|Early Jurassic|LateTriassic|Of the Woogaroo Subgroup. Formely known as the "Helidon Sandstone" which is now interpreted as a facies variant within the unit. Overlies The Raceview Fm. Geol. Prov: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|60995|4|Described|p61, p51 Fig. 3|Late Triassic|Late Triassic|Of Woogaroo Subgp. Sandstone and quartz-rich granule conglomerate. Conformably overlies Raceview Fm; overlain by Calamia Mbr. Max. thick: 150m. Part of this unit is equivalent to "Olive Gap Fm". Geol. Prov: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|60996|5|Briefly described|p72|||Quartzose sandstone forming an extensive blanket overlying the Raceview Formation. Geological Province: Clarence-Moreton Basin. Equivalent to Precipice Sandstone of the Surat Basin.||||||09-MAY-13
26871|Ripley Road Sandstone|60997|5|Briefly described|p139 Fig. 1|Sinemurian|Rhaetian|Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
26871|Ripley Road Sandstone|60999|5|Briefly described|p164, p172|Early Jurassic|Late Triassic|Of the Woogaroo Subgroup. Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6.||||||
26871|Ripley Road Sandstone|61002|5|Briefly described|p201|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin. See also p199 Fig. 3.||||||
26871|Ripley Road Sandstone|61004|5|Briefly described|p232 Fig. 2|Jurassic|Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|61005|5|Briefly described|p242|||See also p255 Figs. 23, 24 and 25. ||||||
26871|Ripley Road Sandstone|61006|5|Briefly described|p277, p289|Jurassic|Triassic|Formerly the Pillar Valley Fm. Quartzose sandstone (sheet-like braided-stream deposits) with potential as reservoir rocks. This unit is the most extensive potential reservoir in the basin. Geol. Prov: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|61310|5|Briefly described|p21, table C1 (p22-23)|||Of the Woogaroo Subgroup. Comprises a sandstone sequence with minor mudrock and conglomerate intervals, and minor coal.  Max. thickness: 500m. Geological Province: Clarence-Moreton Basin||||||
26871|Ripley Road Sandstone|64289|5|Briefly described|p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
26871|Ripley Road Sandstone|64665|5|Briefly described|p53 Fig.2, p59.|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Correlates with lower part of Landsborough Sandstone (Southern Nambour Basin), and Myrtle Creek Sandstone (Northern Nambour Basin).||Upper unit in Woogaroo Subgroup.||Overlies Raceview Formation. Is overlain by Gatton Sandstone.||
26871|Ripley Road Sandstone|64856|5|Briefly described|p80, 81|||Moreton Basin. Grades laterally into Precipice Sandstone to west.| | ||||31-JAN-13
26871|Ripley Road Sandstone|65096|6|Mentioned|p373|||Clarence-Moreton Basin. Compared with the Jurassic sandstones east of the Kumbarilla Ridge and west of the Toowoomba Strait [accidently capitalised as Jurassic Sandstone] and the Precipice Sandstone of the Surat Basin, to the west.||||||
26871|Ripley Road Sandstone|66855|5|Briefly described|p956.|||Clarence-Moreton Basin.||||Unconformably overlies Evans Head Coal Measures.|Massive quartz sandstone.|
26871|Ripley Road Sandstone|67402|5|Briefly described|p165 tbl LPB1|Hettangian||Clarence-Moreton Basin. Deposited in a high energy environment. Approximately 70m thick. Sandstones are often reservoirs and potential reservoirs for the storage of carbon dioxide with an average porosity of 18% and an average permeability of 735 mD. See also p187, p188, p190, p190 fig CLM6, p192, p193, p195.||Woogaroo Subgroup||Overlies the Raceview Formation. Overlain by the Gatton Sandstone.|Massive, cross-bedded, fine to coarse-grained, sub-labile to quartzose sandstone.|
26871|Ripley Road Sandstone|69297|5|Briefly described|p487 fig 5.38, p488, p490|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. Between 100-150m thick. In the onshore Clarence-Moreton Basin has great potential as a hydrocarbon reservoir rock. ||Woogaroo Subgroup||Overlies the Raceview Formation. Overlain by the Gatton Sandstone.||
26871|Ripley Road Sandstone|69594|4|Described|p519, p534-535, p543-547, p572|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Formerly the Helidon Sandstone. The Triassic-Jurassic boundary is at the base of this unit.||Woogaroo Subgroup.||Overlies Raceview Formation. Is overlain by Gatton Sandstone. Merges with Precipice Sandstone in the Surat Basin.|Sheet-like, quartzose, cross-bedded sandstone.|
26871|Ripley Road Sandstone|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||||||
26871|Ripley Road Sandstone|70821|5|Briefly described|p80|||Clarence-Moreton Basin. Aquifer: generally artesian.||Woogaroo Subgroup.||Overlies Raceview Formation. Is overlain by Koreelah Conglomerate Member (Gatton Sandstone).||
26871|Ripley Road Sandstone|71805|5|Briefly described|p75-p76|Sinemurian|Hettangian|Clarence-Moreton Basin. Referred to as the Ripley Road Formation on p75. This unit is a time equivalent to the Precipice Sandstone, Poolowanna Formation and the Helidon Formation.||Woogaroo Subgroup||Overlain by the Gatton Sandstone.||
26871|Ripley Road Sandstone|72298|6|Mentioned|p802|||Clarence-Moreton Basin. Has supplied small supplies of groundwater for irrigation.||||||
26871|Ripley Road Sandstone|72921|5|Briefly described|p15 Fig.2.|Early Jurassic|Triassic|Shown as located within the Clarence-Moreton Basin.||||Underlies Gatton Sandstone.||
26871|Ripley Road Sandstone|73570|6|Mentioned|p912 Fig.2, p913-914, p915 Fig.4|Rhaetian|Rhaetian|Clarence-Morton Basin.||||||
27552|Riversdale Volcanics|22529|5|Briefly described|7|Pragian|Pragian|||||||
27552|Riversdale Volcanics|22590|6|Mentioned|Fig3 P754|Emsian|Pragian|||||||
27552|Riversdale Volcanics|22857|4|Described|p474 App.1 Tb.A1.6|Pragian|Pragian|Of the Kandos Group. Age: 410+/-8 and 389+/-8Ma (U/Pb zircon). Contains brachiopods. Max. thickness: 1250m. Geological Province: Capertee Rise.||||||03-MAR-06
27552|Riversdale Volcanics|23043|5|Briefly described|Map Legend|Pragian|Pragian|of Kandos Group.||||||
27552|Riversdale Volcanics|23170|2|Defined|p133|Early Devonian|Early Devonian|Of the Kandos Group.||||||28-NOV-06
27552|Riversdale Volcanics|23522|5|Briefly described|p248 Fig 4|Emsian|Pragian|||||||
27552|Riversdale Volcanics|24394|5|Briefly described|p171|Pragian|Pragian|Geological Province: Hill End Trough.||||||
27552|Riversdale Volcanics|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
27552|Riversdale Volcanics|30329|6|Mentioned|p30|||On table P30||||||
27552|Riversdale Volcanics|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
27552|Riversdale Volcanics|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
27552|Riversdale Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
27552|Riversdale Volcanics|34059|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
27552|Riversdale Volcanics|36285|4|Described|p56|||See also Fig.2.& 3.||||||
27552|Riversdale Volcanics|37727|5|Briefly described|p83|||||||||
27552|Riversdale Volcanics|39331|6|Mentioned|Fig.0-3|||||||||
27552|Riversdale Volcanics|39663|6|Mentioned|Table 1|||||||||
27552|Riversdale Volcanics|40328|5|Briefly described|p139|||||||||
27552|Riversdale Volcanics|42379|4|Described|p205|Early Devonian||Names supersedes Riversdale Rhyolite.||||||
27552|Riversdale Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
27552|Riversdale Volcanics|43043|4|Described|p94|||Pragian age. Supersedes Riversdale Rhyolite of Wright (1966)||||||
27552|Riversdale Volcanics|43188|4|Described|p207,Table 3 p208||Pragian|Type section location given. Of Kandos Group.||||||
27552|Riversdale Volcanics|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
27552|Riversdale Volcanics|44093|5|Briefly described|p212 App. 1|Early Devonian|Early Devonian|Of the Kandos Group. Geological Province: Lachlan Fold Belt.||||||
27552|Riversdale Volcanics|64994|5|Briefly described|p8|Pragian|Pragian|Geological province: Capertee High. Top of the unit can be correlated with the top of Merrions Formation in Hill End Trough.||||||07-FEB-11
27552|Riversdale Volcanics|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cudgegong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27552|Riversdale Volcanics|66197|5|Briefly described|p633 Fig.4a|Pragian|Pragian|Capertee High-Hill End Trough. Silicic volcanics. Underlies the Kandos Group. Age: 410 +/ - 7 Ma.||||||14-MAR-12
27552|Riversdale Volcanics|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4, p1099|Early Devonian|Early Devonian|Capertree High. Locally thickens from west to east and north to south, potentially occupied a volcanic subsidence feature (Pemberton et al., 1994). Locations in text include p1100 Fig.5.||||Overlies the Roxburgh Formation, Tanabutta Group, underlies the Carwell Creek Formation.||
82640|Rivertree Syenogranite|71628|3|Fully described|p9: 3; p15-40; p16: 1-2, 4, 6, 13,25-32|Early Triassic|Early Triassic|See also p19: 89-91, 95, 131, 133, 174. New name (this study). Previously called Rivertree Granodiorite (Offenberg, 1968) and Rivertree Granite (Thomson, 1973). Named after a local Station. Crops out over ~20 km2 about 32 km E of Stanthorpe as well-exposed cliffs and tors. The type locality is at GR 286314 (Drake 1:100,000 sheet) (Thomson, 1976). Lithology not given on p9-3. Distinctive geochemistry described. Other, younger ages are given. Is associated with historically economically significant Ag-Zn-Pb-As-Cu-Sb-Sn-Au mineralisation, briefly described.|249.1 +/- 1.3 Ma (SHRIMP: Chisholm et al., 2014).|Rivertree Suite.|Jacks Creek Monzogranite Phase.|Intrudes Razorback Creek Mudstone, Emu Creek Formation and Drake Volcanics. The intrusive relationship with Koreelah Creek Granodiorite is equivocal. Is faulted against Cullendore Syenogranite.|Pink to grey, coarse-grained, porphyritic, less commonly equigranular, biotite-(hornblende) syenogranite; aplitic to porphyritic dykes. I-type.|
24473|Roach Island Tuff|36958|3|Fully described|p159|||Interbedded tuffs, thin rubbly lavas, fragmental material. Overlain by North Ridge Basalt, Neds Beach Calcarenite.||||||14-MAR-06
24473|Roach Island Tuff|61943|5|Briefly described|Map Legend|||Interbedded Tuff, thin lavas and fragmental materials. Overlain by: North Ridge Basalt.||||||
24473|Roach Island Tuff|73136|6|Mentioned|p190-191, p194|||Lord Howe Island. Composes the Admiralty Islands, Malabar Point, and Stevens Point. Forms well-rounded slopes on Admiralty Islands.||||||
24473|Roach Island Tuff|73554|4|Described|Map legend, back of map|Neogene|Neogene|Lord Howe Island. Part of the Lord Howe Volcanic Complex. Oldest known unit in the area. Found on the north side of Malabar Hill and extends north to the Admiralty Islands. Colour varies including yellow and red. Visible up to 60 m above sea level. Well exposed contact with the overlying North Ridge Basalt at Malabar Hill. Commonly intruded by basaltic dykes.||Lord Howe Volcanic Complex||Overlain by North Ridge Basalt.|A mix of tuff, thin basaltic lava flow deposits and fragmental rocks.|
24473|Roach Island Tuff|73581|6|Mentioned|p28 Fig.8|||||||||
28287|Robertson Basalt|29901|4|Described|Table 1|||||||||
28287|Robertson Basalt|31057|6|Mentioned|p8|||Re potential use.||||||
28287|Robertson Basalt|36220|4|Described|p95|||||||||
28287|Robertson Basalt|36221|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
28287|Robertson Basalt|37253|6|Mentioned|Table 1|||||||||
28287|Robertson Basalt|42896|4|Described|p56|||||||||
28287|Robertson Basalt|61155|5|Briefly described|p19|Middle Eocene|Middle Eocene|Of the Mittagong Province Volcanics. In the Bathurst-Goulburn region. ||||||
28287|Robertson Basalt|70661|4|Described|p229- 234|Eocene|Eocene|Presumably named for the town of Robertson. Previously referred to as the Robertson Flow. Distribution, geomorphology, geochemistry, geophysical characteristics and economic geology discussed. No type section proposed. Generally thought to be more than 100m thick. Deposited as multiple subaerial lava flows, possibly originating from a number of fissures.|37.4-55.4 Ma (K-Ar)|||Correlated with the Reevesdale Basalt.|Fine grained, dense, alkali olivine basalt with a groundmass of labradorite, augite and magnetite. Flow textures are common and columnar jointing is well developed.|
28287|Robertson Basalt|71303|5|Briefly described|map legend|Eocene|Eocene||||||Grey to black fine-grained alkali olivine basalt; basanite locally. Typically deeply weathered with extensive  development of red-brown soils.|
28287|Robertson Basalt|73248|6|Mentioned|p309|Eocene?|Eocene?|Observed to overlay a surface cut across the Wianamatta Group and Hawkesbury Sandstone just beyond the southern end of the Woronora Plateau.||||Underlain by Wianamatta Group and Hawkesbury Sandstone.||
28287|Robertson Basalt|73581|5|Briefly described|p22-23|Eocene|Paleocene|Southern Highlands Volcanic Province. Low-degree partial melts of a high Ni and Cr primary or near primary source. List of K-Ar ages provided from Carr and Facer (1980) and Wellman and McDougall (1974b).|63.8-35.1 Ma K-Ar||||Contains high-K, nepheline- and analcime-bearing basanite and alkali basalt.|
70506|Rockford Ignimbrite Member|62095|2|Defined|p245 Figs.4,5, p274 and p276 Appdx.|Late Carboniferous|Late Carboniferous|Of Currabubula Fm. Purple to beige, unwelded to possibly slightly welded ignimbrite; groundmass micropoikilitic. Overlain by Allawa Ig. Mbr; underlain by Back Creek Ig. Mbr. Thickness: up to 20m.  Geol. Prov: Werrie block/Tamworth Belt. see also Plate 1.||||||31-JAN-08
76965|Rockvale Monzogranite|71628|3|Fully described|p3: 1, 4, 6-7, 14-15, 24, 79-86, 93, 95|||See also p13-24; p17-24. Originally Rockvale Adamellite-Granodiorite (Binns et al., 1967). Later appeared as Rockvale Granodiorite-adamellite (Korsch and Harrington, 1981), Rockvale Granodiorite (Korsch, 1981), Rockvale Adamellite (Gilligan et al., 1992), and Rockvale Monzogranite (Landenberger et al., 2010). Named from the parish of Rockvale or the Rockvale Station. Crops out ~30 km ENE of Armidale and a similar distance W of Ebor. Crops out as rubbly corestones. Geochemistry described in some detail; similar to Abroi Granodiorite, and indistinguishable from Tobermory Monzogranite. Several age determinations are given and briefly discussed. Spatially (probably not genetically) associated with numerous hydrothermal Sb (+/- As, Ag), Ag-As (+/- base metals), and Au(-W, -Bi) bearing veins.|292.6 +/- 2.4 Ma (SHRIMP: Cawood et al., 2011).|Rockvale Suite.||Intrudes Girrakool beds. Abuts Abroi Monzogranite. Is intruded by Billygoat Hill Complex.|Heterogeneous, medium-grained, weakly porphyritic biotite monzogranite, minor granodiorite; locally amphibole and, independently, garnet bearing; weakly to strongly deformed. S-type.|
76965|Rockvale Monzogranite|71703|4|Described|p191-192, 194, 195, 196-205|||S-type granite. Least deformed of the 3 plutons in the Hillgrove Supersuite. U-Pb geochron p198. Called Rockvale Granodiorite p192. Age this paper: 295.9 +/-2.1 Ma.|Recalc. 296.7+/-2.3 Ma (McKibbin et al.2017) |Of Hillgrove Supersuite.||Intrudes Girrakool Beds, Wongwibinda Metamorphic Complex. Adjacent to Abroi Granodiorite.|K feldspar quartz plagioclase biotite opaque +/- garnet muscovite granodiorite with accessory zircon, monazite and apatite.|
76965|Rockvale Monzogranite|73202|6|Mentioned|p637|Sakmarian|Asselian|New England Orogen, southern. Zircon U-Pb crystallisation age from McKibbin et al., (2017).|295.6 +/- 2.4 Ma U-Pb zircon|Hillgrove Plutonic Supersuite||||
73933|Rockvale Suite|71628|5|Briefly described|p3: 15, 82, 85, 93|||||Hillgrove Supersuite.|Rockvale, Tobermory Monzogranites, Abroi Granodiorite.|||
72991|Rocky Beach Metamorphic Melange|62058|4|Described|p11-18, map sheet|||Och et al.(2003). Considerable details of lithology and mineralogy.|||||Lenses of melange: rounded phacoids of eclogite, blueschist, omphacitite and tremolite marble embedded in a chlorite-actinolite schist matrix; surrounded by serpentinite.|
72991|Rocky Beach Metamorphic Melange|63763|3|Fully described|p2, p4-5 Fig. 1, p8-10|Middle Ordovician||Of Och et al (2003). More complete definition presented. Eclogite, omphacitite, blueschist, galucophane-phengite schist, tremolite marble and rare slate. See also p7 Fig. 2, p16.||||||
72991|Rocky Beach Metamorphic Melange|67322|5|Briefly described|Fig.5; p28|Late Ordovician|Late Ordovician|(Och et al., 2003). Undated, but believed to be of similar age as the enclosing serpentinite (Port Macquarie Serpentinite): Early Cambrian. Occurs at Rocky Beach in the Port Macquarie region.||||Enclosed within Port Macquarie Serpentinite.|Chloro-actinolite schist containing blocks of high pressure metamorphic rocks including blueschist and lawsonite eclogite; surrounded by broken formation of the Watonga Formation.|22-FEB-18
29588|Rocky Bridge Granodiorite|22679|4|Described|p 49|||||||||
29588|Rocky Bridge Granodiorite|22798|6|Mentioned|p851 Table.1|||||||||
29588|Rocky Bridge Granodiorite|23214|3|Fully described|p171|Silurian|Silurian|Originally included with Neville Granite (now Sunset Hills Granite). Intrudes the Adaminaby Group. Hornblende-biotite granodiorite. Geological Province: Wyangala Batholith.||||||
29588|Rocky Bridge Granodiorite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Hornblende biotite granodiorite.||||||17-JUL-08
29588|Rocky Bridge Granodiorite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|||||||
29588|Rocky Bridge Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
82645|Rocky Glen Monzogranite|71628|5|Briefly described|p4: 1, 5, 51, 57-58|||New unit, named after the Rocky Glen homestead. Previously part of Pringles Monzogranite. Southern New England Orogen. Crops out ~7 km S of Kingstown and ~40 km WNW of Uralla. Extends ~6 km N-S and ~2.5 km E-W. No lithological or geochemical descriptions available.||Rocky Glen Suite.||Intrudes Sandon Association. Abuts Roumalla Monzogranite Phase (Pringles Monzogranite) and Namoi Tops Monzogranite.|Coarse-grained biotite (+/- muscovite, +/- cordierite) monzogranite; possibly minor syenogranite.|
32475|Rocky Ponds Group|24417|3|Fully described|p114|Middle Devonian|Middle Devonian|Includes Dulladerry Volcanics and Warrumba Volcanics.||||||06-MAY-08
32475|Rocky Ponds Group|50628|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Coomaloo Ignimbrite Member, Walloy Rhyolite Member, Adelargo Basalt Member, Warrumba Volcanics.||||||
32475|Rocky Ponds Group|60008|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Felsic to mafic volcanics.||||||08-JUL-04
32475|Rocky Ponds Group|60009|5|Briefly described|Map Legend|Givetian|Eifelian|||||||13-JUL-04
32475|Rocky Ponds Group|63289|6|Mentioned|p373 Fig. 7|Middle Devonian|Middle Devonian|||||||07-FEB-11
32475|Rocky Ponds Group|64826|5|Briefly described|p1040 Tb. 1|Givetian|Givetian|Contains the Dulladerry Volcanics.||||||05-APR-20
32475|Rocky Ponds Group|66768|5|Briefly described|p211|Middle Devonian|Middle Devonian|Parkes-Grenfell area. Contains Dulladerry Volcanics and Warrumba Volcanics.||||||
32475|Rocky Ponds Group|67847|5|Briefly described|p60 fig 3.3.4|||Dulladerry Rift. ||||||
32475|Rocky Ponds Group|68592|5|Briefly described|p33|Middle Devonian|Middle Devonian|Dulladerry Rift.|||Includes Dulladerry and Warrumba Volcanics.||A-type bimodal volcanics and associated plutons.|
32475|Rocky Ponds Group|69043|6|Mentioned|p74|||Eastern Province, Lachlan Orogen.|||Dulladerry Volcanics.|||
32475|Rocky Ponds Group|70297|5|Briefly described|map legend|Frasnian|Givetian|Erosional base.|||Dulladerry Volcanics|||
32475|Rocky Ponds Group|71700|5|Briefly described|p29|Middle Devonian|Middle Devonian||||Includes the Dulladerry Volcanics and Warrumba Volcanics.|||
32475|Rocky Ponds Group|72495|6|Mentioned|p229|Middle Devonian|Middle Devonian|[age from 1979, 1997 references].||||||05-APR-20
68865|Rocky River Monzogranite|60422|5|Briefly described|p387 Fig. 2, p388 Tb. 1|||Of the Bungulla-type granite (Moonbi Supersuite).  Very coarse to coarse-grained monzogranite, crowded porphryitic monzogranite.||||||
68865|Rocky River Monzogranite|71628|4|Described|p11: 1-2, 7, 11, 14, 23-35, 45; p12-16|||See also p15: 33, 57, 94-95, 105, 109; p19-72. Formalised in this study; after Rocky River monzogranite of Mustard (2001, 2004). Named after Rocky (Timbarra) River. Occurs 30-40 km E of Tenterfield, over 335 km2 of the Timbarra Plateau. Geochemistry described. Associated with hard-rock and alluvial Au deposits (named); probably not genetically related to the Monzogranite. RELATED UNITS (continued): Is faulted against Wandsworth Volcanic Group, Bungulla and Mount Lindesay Monzogranites and Stanthorpe Monzogranite (also intruded by the last).|244 Ma (Rb-Sr biotite: Shaw, 1994).|Rocky River Suite.|Bulldog Diggings, Ewingar, McLeods Creek, Monzogranite Phases; Long Creek Quartz Monzonite Phase.|Intrudes Silverwood Group, Drake Volcanics and Gilgurry Mudstone. Abuts Sandy Creek Monzogranite and Grasstree Quartz Monzodiorite. See COMMENTS for more.|Medium- to very coarse-grained, porphyritic (K-feldspar to 75mm) biotite-hornblende monzogranite; minor quartz monzonite. Considerable compositional, lithological and mineralogical variation (elaborated). I-type.|
33761|Rocky Tank Conglomerate Member|50129|4|Described|p16, p23|Givetian|Givetian|Of the Waverly Creek Formation. Conformably overlain by the Ramparts Sandstone Member. Unconformably overlies the Snake Cave Sandstone. Thickness at Type Section: 58m. Geological Province: Bancannia Trough, Darling Basin.||||||
33761|Rocky Tank Conglomerate Member|63632|6|Mentioned|p654||Givetian|||||||16-OCT-07
33761|Rocky Tank Conglomerate Member|66623|3|Fully described|p121, p216, pp219-220.|Early Givetian|Early Givetian|Cupala Creek Basin. Formerly (Neef 2004a) the basal unit in Waverly Creek Formation (no longer recognised); in this study, presented as one of three contemporaneous basal units of Ravendale Formation. Correlated with Turkaro Range Conglomerate Member and Gum Creek Member. Thickness from 33 m to 120 m.||Basal unit in Ravendale Formation.||Unconformably overlies Cupala Creek Formation.|Basal part of the conglomerate contains cobbles and boulders of quartzite, vein quartz and grey quartzose sandstone; upper horizons contain beds of coarse-grained sandstone with conglomeratic lenses; clasts to 34 cm.|
33761|Rocky Tank Conglomerate Member|66918|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Ravendale Formation.|||Conglomerate containing cobbles and boulders of grey quartzose sandstone, quartzite and vein quartz; up-sequence are coarse-grained sandstones with conglomeratic lenses.|
33761|Rocky Tank Conglomerate Member|67562|5|Briefly described|p98, p102, p104, p111|||~ 33m thick. Is apparently misnamed as Rocky Creek Conglomerate in the same paragraph on p102.||Of the Waverly Creek Formation.||Unconformably overlies Snake Cave Sandstone.||23-JAN-17
33761|Rocky Tank Conglomerate Member|70650|5|Briefly described|Map Legend|Devonian|Devonian|||Ravendale Formation|||Conglomerate containing cobbles and boulders of grey quartzose sandstone, quartzite and vein quartz; up-sequence are coarse-grained sandstones with conglomeratic lenses.|20-JAN-22
33761|Rocky Tank Conglomerate Member|70651|5|Briefly described|Map Legend|Devonian|Devonian|||Ravendale Formation|||Conglomerate containing cobbles and boulders of grey quartzose sandstone, quartzite and vein quartz; up-sequence are coarse-grained sandstone with conglomeratic lenses.|
22776|Rollans Road Formation|22616|6|Mentioned|Fig.1 p670|Carboniferous|Devonian|||||||
22776|Rollans Road Formation|22736|2|Defined|p614-16,29,30|Tournaisian|Famennian|southern Hastings Block unit||||||
22776|Rollans Road Formation|22857|4|Described|p500 App.1 Tb.A1.7|Tournaisian|Famennian|Medium and thin-bedded dark siltstone, volcaniclastic arenite, minor conglomerate. Interdigitated by Cowangara Formation. Max. thickness: ~1km.||||||
22776|Rollans Road Formation|44093|5|Briefly described|p67 Fig 6.6|Carboniferous|Devonian|Of the Southern Hastings Block. Geological Province: New England Fold Belt.||||||24-MAR-05
22776|Rollans Road Formation|70939|6|Mentioned|p824, p826, p828, p830|Carboniferous|Devonian|Relative timing of deposition and faulting discussed.||||||
22776|Rollans Road Formation|71628|6|Mentioned|p17-97|||||||Is intruded by Forbes River Porphyrite.||
26126|Rolling Grounds Latite|22857|5|Briefly described|p464 App.1 Tb.A1.6|Early Devonian|Early Devonian|Porphyritic latite and andesitic lava. Max. thickness: <250m. ||||||
26126|Rolling Grounds Latite|29456|6|Mentioned|p424|||||||||
26126|Rolling Grounds Latite|36050|6|Mentioned|p399|||||||||
26126|Rolling Grounds Latite|36443|5|Briefly described|map legend|Lochkovian|Lochkovian|Of Boggy Plain I-type Suite. Extrusive. Latite, minor andesite. Disconformably overlies Kellys Plain Volcanics. BMR map code: Dlr.||||||
26126|Rolling Grounds Latite|40328|6|Mentioned|p62|||||||||
26126|Rolling Grounds Latite|40882|6|Mentioned|p22|||||||||
26126|Rolling Grounds Latite|45147|2|Defined|M176|Lochkovian|Lochkovian|||||||
26126|Rolling Grounds Latite|68592|5|Briefly described|p932-5, p947|||Owen and Wyborn (1979). Tantangara 1:100 000 sheet area. Mentioned as having geochemical affinities with Boggy Plain Supersuite.||||Equivalent to Pilleuil Andesite.||
33797|Romner Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Foliated, muscovite-biotite granite.||||||
33797|Romner Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Whick Whack Suite. Foliated muscovite-biotite granite. High K, Th and U radioelement response.||||||
33797|Romner Granite|68592|3|Fully described|p29, p1480, p1482, p1508-11, p1515-7|Early Devonian|Early Devonian|New name; not recognised previously: included in undifferentiated Wyangala Batholith by Brunker and Offenberg (1970) and in Binda Granite by Chappell et al. (1991). Regarded as part of Hovells Suite by Blevin (2011); here assigned to Whick Whack Suite. Type locality described. Crops out as tors to 4m high.||Unit in Whick Whack Suite.||Intrudes Binda Granite.|Grey to white, medium- to coarse-grained, foliated biotite granite. A-type. Geochemistry and geophysical properties briefly described.|
33797|Romner Granite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dwr. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Whick Whack Suite|||Medium-coarse grained, foliated biotite granite; high K, medium-high Th and low-high U response and low magnetic susceptibility.|
33797|Romner Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Whick Whack Suite|||Medium-coarse grained, foliated biotite granite; high K, medium-high Th and low-high U response and low magnetic susceptibility.|
27299|Rook Tuff|22553|6|Mentioned|p77,p83|Cryogenian|Cryogenian|part of the Adelaidean sequence||||||
27299|Rook Tuff|22589|6|Mentioned|p129||Neoproterozoic|||||||
27299|Rook Tuff|22631|6|Mentioned|p177|Cryogenian|Cryogenian|||||||
27299|Rook Tuff|22772|4|Described|p65,Table13.1|Cryogenian|Cryogenian|Max Age: 802 (+/-) 10 Ma.||||||
27299|Rook Tuff|22857|5|Briefly described|p65, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Curdimurka Subgroup (Callanna Group). Age: 802+/-10Ma (Fanning, Ludwig et al, 1986). See also p399 App.1 Tb.A1.3.||||||
27299|Rook Tuff|22907|5|Briefly described|41|||Age 802 + - 10 Ma||||||
27299|Rook Tuff|23314|6|Mentioned|335|||||||||
27299|Rook Tuff|23557|5|Briefly described|p98|Cryogenian|Cryogenian|Age: 802+/-10Ma (U-Pb).||||||
27299|Rook Tuff|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|Age: 802+/-10 Ma||||||
27299|Rook Tuff|24175|4|Described|p9|Neoproterozoic III|Neoproterozoic|Of Curdimurka Subgroup.  Overlain by Dunns Mine Limestone; overlies Dome Sandstone.  Max. thickness: 60m.  Age: 802+/-10Ma (U-Pb zircon, Fanning et al, 1986).||||||
27299|Rook Tuff|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Parent: Curdimurka Subgroup.  Age: 802+/-10Ma (Concordant U-Pb zircon)||||||
27299|Rook Tuff|24400|5|Briefly described|p155, p156|Neoproterozoic|Neoproterozoic|Of Callanna Group. Overlies Wooltana Volcanics. Age: 802+/-10Ma.||||||18-APR-13
27299|Rook Tuff|24401|5|Briefly described|p100|Neoproterozoic|Neoproterozoic|Age: 802+/-10Ma. Geological Province: Adelaide Geosyncline||||||03-MAR-05
27299|Rook Tuff|24604|5|Briefly described|p915|Neoproterozoic|Neoproterozoic|Age: 802 +/- 10 Ma.||||||
27299|Rook Tuff|37854|2|Defined|p10|Adelaidean|Adelaidean|Prob.Late Willouran||||||
27299|Rook Tuff|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27299|Rook Tuff|40294|6|Mentioned|p9|||||||||
27299|Rook Tuff|41363|5|Briefly described|p19|||||||||
27299|Rook Tuff|41402|6|Mentioned|p42|||||||||
27299|Rook Tuff|41403|4|Described|p61|||||||||
27299|Rook Tuff|42222|5|Briefly described|p12|||||||||
27299|Rook Tuff|42223|6|Mentioned|Fig.2 P36|||||||||
27299|Rook Tuff|42238|5|Briefly described|p72|||||||||
27299|Rook Tuff|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup. Age of 802+/-10 Ma.||||||
27299|Rook Tuff|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline. 802 +/- 10 Ma.||||||
27299|Rook Tuff|60718|5|Briefly described|p49 Fig. 2, p50|Adelaidean|Adelaidean|Unconformably overlies Dome Sandstone. Geological Province: Adelaide Geosyncline.||Of Curdimurka Subgroup (Callanna Group).||Unconformably overlies Dome Siltstone.||15-APR-11
27299|Rook Tuff|61153|5|Briefly described|p344-345 Fig. 1|||Of the Callanna Group. Age: 802+/-10Ma (Fanning et al 1986). Geological Province: Adelaide Geosyncline. See also p352.||||||25-JAN-06
27299|Rook Tuff|61238|4|Described|p45, p48|Neoproterozoic|Neoproterozoic|Of the Callanna Group (Curdimurka Subgroup). Geological Province: Adelaide Geosyncline. Age: 802+/-10 Ma. Occurs in one isolated locality.||||||14-MAY-07
27299|Rook Tuff|61732|5|Briefly described|p4 Fig. 3|Willouran|Willouran|Of the Callanna Group.  Age: 802+/-10Ma. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||07-FEB-11
27299|Rook Tuff|62453|3|Fully described|p12 Fig. 8, 24|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex/Stuart Shelf. Age: 802 +/- 10Ma (Fanning et al., 1986). Of the Callanna Group. Overlies Coominaree Dolomite.||||||30-AUG-18
27299|Rook Tuff|62664|5|Briefly described|p138 Fig.2, p139, p151.|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma (Fanning et al. 1986)|Unit in Curdimurka Subgroup.|||Thin dacitic volcaniclastic unit.|
27299|Rook Tuff|62893|6|Mentioned|p17|||Willouran Ranges. Early Adelaidean.||||||
27299|Rook Tuff|63224|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Geosyncline and Arrowie Basin.||||||07-FEB-08
27299|Rook Tuff|63562|5|Briefly described|p345|Cryogenian|Cryogenian|Adelaide Rift Complex. Mentioned as a possible, though unlikely, distal source of zircons in Grant Bluff Formation (Georgina Basin) and Cyclops Member (Amadeus Basin).|802 Ma (Fanning et al., 1986).||||Felsic.|
27299|Rook Tuff|64647|5|Briefly described|p44, p46|Willouran|Willouran|Age: 802+/-10Ma (Fanning et al. 1996).||||||
27299|Rook Tuff|64793|6|Mentioned|p283, p285|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma (Fanning et al., 1986).|Curdimurka Subgroup||||
27299|Rook Tuff|64796|5|Briefly described|p183 Fig.2, p184|Cryogenian|Cryogenian||802 +/- 10 Ma (U-Pb zircon; Fanning et al., 1986)|Unit in Curdimurka Subgroup.||||
27299|Rook Tuff|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Adelaide Rift Complex. Lithology/rank not shown on diagram.||||||
27299|Rook Tuff|64801|6|Mentioned|p111|Tonian|Tonian||802 +/- 10 Ma (Fanning et al., 1986).|Callanna Group.||||
27299|Rook Tuff|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Of Curdimurka Subgroup. Dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986).||||||19-MAR-12
27299|Rook Tuff|65366|5|Briefly described|p23 Fig. 3, p24|Cryogenian|Cryogenian|Of Curdimurka Subgroup. Dated at 802 +/- 10 Ma, U-Pb (Fanning, 1986). Overlies the Coominaree Dolomite.||||||19-MAR-12
27299|Rook Tuff|65410|5|Briefly described|p72.|Neoproterozoic|Neoproterozoic|Age suggests that sedimentation in the Adelaide Geosyncline and Centralian Superbasin began before 800 Ma.|802 +/- 10 Ma (U-Pb; Fanning et al. 1986).|Unit in Callanna Group.||||
27299|Rook Tuff|66522|5|Briefly described|p19.|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma.|Unit in Curdimurka Subgroup.||||
27299|Rook Tuff|67536|5|Briefly described|Map Legend|Cryogenian|Cryogenian||ca. 802 +/- 10 Ma||||Felsic volcanic rocks.|
27299|Rook Tuff|67979|5|Briefly described|p528|Cryogenian|Cryogenian|Age date from Willouran Ranges.|802+/-10 Ma, U-Pb zircon, Fanning et al. 1986|Curdimurka Subgroup||||
27299|Rook Tuff|69019|5|Briefly described|p37.|Neoproterozoic|Neoproterozoic||802 +/- 10 Ma (U-Pb zircon: Fanning et al. 1986).|Unit in Curdimurka Subgroup.||||
27299|Rook Tuff|69666|5|Briefly described|p33|Neoproterozoic|Neoproterozoic|Willouran Ranges.|802 +/- 10 Ma (U-Pb zircon: Fanning et al. 1986).|Curdimurka Subgroup.||||
27299|Rook Tuff|69873|5|Briefly described|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.|802 +/- 10 Ma (Fanning et al., 1986).|Unit in Curdimurka Subgroup.||||21-DEC-15
27299|Rook Tuff|70819|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Clare Valley.|802 +/- 10 Ma (U-Pb).|Curdimurka Subgroup.||||
27299|Rook Tuff|72238|5|Briefly described|p42|Tonian|Tonian|Of Adelaide Geosycline.|802+\-10 Ma (Fanning et al., 1986)|||||
27299|Rook Tuff|72492|5|Briefly described|p2 Fig.1, p2|Neoproterozoic|Neoproterozoic|In Willouran Ranges. Dates from Fanning et al., 1986.|802 +/- 10 Ma|Curdimurka Subgroup||Overlies Dome Sandstone and underlies Dunns Mine Limestone.|Includes siltstone with porphyritic dacite lenses.|
27299|Rook Tuff|73188|6|Mentioned|p315|Tonian|Tonian||ca 800 Ma|||||
27299|Rook Tuff|73222|6|Mentioned|p7|Tonian|Tonian|Willouran Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Underlain by Dome Sandstone. Overlain by Dunns Mine Limestone. Possibly equivalent to Wirrawilka Beds.||
27299|Rook Tuff|73262|6|Mentioned|p581, p583|Tonian|Tonian|Marks the second phase of [Rodinian] rifting. Geochron from Fanning et al. (1986).|802 +/- 10 Ma|Callanna Group, Warrina Supergroup||||
27299|Rook Tuff|74367|5|Briefly described|p7 Fig.6, p8, p12, p18-20|Tonian|Tonian|Coeval with Oodla Wirra Volcanics.|802+/-10 Ma U-Pb SHRIMP igneous zircon|Curdimurka Subgroup||||
25746|Rookery Limestone Member|22857|5|Briefly described|p442 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Meryula Formation (Kopyje Group, Cobar Supergroup). Max. thickness: <300m. Geological Province: Kopyje Shelf (Darling Basin).||||||
25746|Rookery Limestone Member|23171|6|Mentioned|p31|||||||||
25746|Rookery Limestone Member|23173|6|Mentioned|Map Legend|||||||||
25746|Rookery Limestone Member|23522|5|Briefly described|p253|Middle Devonian|Early Devonian|||||||
25746|Rookery Limestone Member|35287|6|Mentioned|p7|||||||||
25746|Rookery Limestone Member|36118|6|Mentioned|p67|||||||||
25746|Rookery Limestone Member|39618|1|Redefined|p77|Early Devonian|Early Devonian|||||||
25746|Rookery Limestone Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25746|Rookery Limestone Member|43032|5|Briefly described|Table 1.|||||||||
25746|Rookery Limestone Member|65469|6|Mentioned|p15, p17|||Lachlan Orogen.||Meryula Formation||||
25746|Rookery Limestone Member|70941|6|Mentioned|p147|Lochkovian|Lochkovian|Age based on conodont faunas.||Meryula Formation||||
25746|Rookery Limestone Member|71039|6|Mentioned|p13|||||Meryula Formation||||
25746|Rookery Limestone Member|73174|6|Mentioned|p1039|Lochkovian|Lochkovian|Contains late Lochkovian age-diagnostic conodont.||Meryula Formation, Kopyje Group, Cobar Supergroup||||24-NOV-22
27890|Rose Valley Member|40664|3|Fully described|p233|Miocene|Miocene|||||||13-JUN-13
27890|Rose Valley Member|42035|5|Briefly described|Table 1 P130|||||||||
23946|Roseburg Granite|22679|4|Described|p 42||Silurian|||||||
23946|Roseburg Granite|23214|3|Fully described|p165|Late Silurian|Late Silurian|Intrudes the Adaminaby Group. Medium grained, porphyritic, biotite-muscovite granite. Geological Province: Wyangala Batholith||||||
23946|Roseburg Granite|42726|5|Briefly described|map legend|Silurian||||||||
23946|Roseburg Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Foliated porphyritic biotite corderite granite.||||||17-JUL-08
23946|Roseburg Granite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Wyangala Batholith.||||||17-JUL-08
23946|Roseburg Granite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian S-type granitoids.||||||
23946|Roseburg Granite|73431|6|Mentioned|p363 Fig.1, p365, p373 Fig.8, p374|Silurian|Silurian|Lachlan Orogen. S-type granite.|||||Granite.|
31629|Roseburg Suite|42726|5|Briefly described|map legend||Silurian|||||||
81257|Roseleigh rhyolite|72084|5|Briefly described|p57-59|||Informal name, for a previously unrecorded unit of rhyolite mapped on Leahy Road, c.900m SSE of Roseleigh Manor (whence the name). N-S outcrop; outcrops of similar lithology are described. Photographs, photomicrographs.||||Is surrounded by Wantabadgery Granite.|Crystal-rich, quartz-feldspar-phyric rhyolite lava or shallow sill. Fairly detailed description.|
33387|Rosemeath Formation|23329|2|Defined|1051 Appendix 3|Early Carboniferous|Late Devonian|||||||
26127|Roset Sandstone|22857|4|Described|p438 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Mouramba Group. Max. thickness: 1.1km. Geological Province: Mouramba Shelf. ||||||
26127|Roset Sandstone|41394|2|Defined|p58|Early Devonian||Reserved as Roset Sandstone Member||||||
26127|Roset Sandstone|41395|6|Mentioned|Map legend|Lochkovian||||||||
26127|Roset Sandstone|41528|2|Defined|p68|Early Devonian||||||||
26127|Roset Sandstone|41529|6|Mentioned|Map legend|Lochkovian||||||||
26127|Roset Sandstone|43089|5|Briefly described|Map Legend|||of Mouramba Group||||||
26127|Roset Sandstone|65469|5|Briefly described|p16|Early Devonian|Late Silurian|Lachlan Orogen.||Mouramba Group||||
26127|Roset Sandstone|70751|6|Mentioned|p12|Pridoli|Pridoli|||Mouramba Group||||
26127|Roset Sandstone|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Mouramba Group||||
38306|Roseville seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
29669|Rossdhu Granite|23214|3|Fully described|p260|Carboniferous|Carboniferous|Intrudes the Adaminaby Group. A course, equigranular, biotite - muscovite - garnet leucogranite with S-type affinities.||||||
29669|Rossdhu Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
29669|Rossdhu Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
29669|Rossdhu Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
24477|Rossi Granodiorite|24128|5|Briefly described|p143|||Geological Province: Lachlan Fold Belt.||||||
24477|Rossi Granodiorite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
24477|Rossi Granodiorite|40276|2|Defined|p14|Early Devonian|Early Devonian|||||||
24477|Rossi Granodiorite|42497|5|Briefly described|Map Legend|Zlichovian|Pragian|||||||
24477|Rossi Granodiorite|42727|5|Briefly described|map legend|Early Devonian|Early Devonian|Of Bega Batholith. Granodiorite; I-type. Intrudes Birkenburn beds and Lockhart Basic Igneous Complex. BMR map symbol: Dgr. Geol. Prov: Rocky Pic Block.||||||
24477|Rossi Granodiorite|42820|5|Briefly described|p73|||||||||
24477|Rossi Granodiorite|71069|6|Mentioned|p178, p179|||Obsolete, now included as part of the Lockhart Igneous Complex.|||||Granodiorite.|
31632|Rossi Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31632|Rossi Suite|44093|5|Briefly described|p209 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31632|Rossi Suite|71069|6|Mentioned|p174|||Obsolete, replaced by the Thurralilly Suite.||||||
27891|Rosyth Limestone|13996|5|Briefly described|p143|Silurian|Silurian|Hosts a small trilobite fauna.||||Equivalent to Boree Creek Formation.||
27891|Rosyth Limestone|30073|6|Mentioned|p54|||On geological map P54. Silurian age.||||||
27891|Rosyth Limestone|32149|6|Mentioned|p659|||U.Llandovery. New coral species.||||||
27891|Rosyth Limestone|32150|6|Mentioned|p4|||Refers Walker (1959)||||||
27891|Rosyth Limestone|32153|6|Mentioned|p54|||Refers McLean (1974)||||||
27891|Rosyth Limestone|33061|6|Mentioned|p26|||Refers Walker (1959) Correlation||||||
27891|Rosyth Limestone|35137|6|Mentioned|p87|||||||||
27891|Rosyth Limestone|37727|6|Mentioned|p9|||See also P79.||||||
27891|Rosyth Limestone|39331|6|Mentioned|Fig.6-3|||||||||
27891|Rosyth Limestone|40328|3|Fully described|p161|||||||||
27891|Rosyth Limestone|43344|14|Not recorded|p139||Silurian|||||||
27891|Rosyth Limestone|63083|6|Mentioned|p218|||In the orange district, central NSW. Laterally equivalent to Boree Creek Formation. Contains Wenlock trilobite fauna.||||||07-FEB-11
27891|Rosyth Limestone|63287|6|Mentioned|p317 Fig. 2|Early Silurian|Early Silurian|Of Waugoola Group. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
27891|Rosyth Limestone|67651|5|Briefly described|p414-415|||||Unit of Boree Creek Limestone.||||
27891|Rosyth Limestone|68592|6|Mentioned|p1889|Wenlock|Llandovery|Boree Creek area, W of Orange. Contains the rugose coral Cyathactis variabilis; a similar organism occurs in the Kingsdale Limestone Member.||||||
27891|Rosyth Limestone|71656|6|Mentioned|p29|Wenlock|Llandovery|Assigned to the Pterospathodus amorphognathoides conodont Zone, which spans the Llandovery-Wenlock boundary. Situated in the Boree Creek area, west of Orange.|||||Fossiliferous limestone.|
24478|Rothery Tuff|39655|4|Described|M4|||||||||
24478|Rothery Tuff|39663|6|Mentioned|Table 2|||||||||
24479|Rothlyn Formation|22768|6|Mentioned|p176|||||||||
24479|Rothlyn Formation|22815|3|Fully described|p41, fig10,16|Late Silurian|Late Silurian|Includes rocks formerly in Bransby Beds||||||
24479|Rothlyn Formation|22857|5|Briefly described|p176, p464 App. 1 Tb.A1.6|Silurian|Silurian|Includes the portion of the former "Bransby Beds" (Richardson, 1979) not included in Colinton Volcanics. Of the Bredbo Group. Max. thickness: >1500m. Geological Province: Canberra-Yass Shelf. See also p468 App.1 Tb.A1.6.||||||
24479|Rothlyn Formation|42726|5|Briefly described|map legend|Silurian||V65.||||||
24479|Rothlyn Formation|43233|5|Briefly described|Map Legend||Late Silurian|of Bredbo Group||||||
24479|Rothlyn Formation|49690|5|Briefly described|p4-11, p15-19, p20, 21, p24, p28-29|Late Silurian|Late Silurian|New Name. Includes former Bransby Beds and previously undifferentiated Late Silurian rocks. Divided into 18 subunits: see tb.4. 700 m thick minimum.|407 +/- 3 Ma (K/Ar).||Includes Billilingra Dacite Member, Montagu Dacite Member and Cloyne Limestone Member.|Conformably overlies the Colinton Volcanics. Includes some units formerly mapped as Bransby Beds.|Sedimentary rocks and interbedded volcanics ranging in composition from rhyolite and biotite dacite to hornblende-biotite dacite; minor basalt is also present.|11-NOV-14
24479|Rothlyn Formation|69635|4|Described|p43-47, 35, 1|Lochkovian|Pridoli|Eastern Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation age. Dacite sampled.|420.2+/-2.9 Ma|Of Bredbo Group.||Overlies the Colinton Volcanics. Correlated with dacite high in Captains Flat Formation and rhyolite from upper Woodlawn Volcanics.|Sample: Black microlitic rhyolite with sparse quartz, feldspar and biotite phenocrysts up to 4 mm.|
32244|Rough Creek Tonalite|22768|6|Mentioned|p175|||||||||
32244|Rough Creek Tonalite|22857|6|Mentioned|p175|||||||||
32244|Rough Creek Tonalite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb29||||||
32244|Rough Creek Tonalite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
32244|Rough Creek Tonalite|63290|6|Mentioned|p403 Fig. 6(c)|Silurian|Silurian|Tonalite.||||||
82648|Roumalla Monzogranite Phase|71628|5|Briefly described|p4: 1, 5, 24, 46-53|||Previously (Bryant and Chappell, 2010) the Roumalla Monzogranite. Named after a local homestead. Herein assigned as a subunit of Pringles Monzogranite. Extends ~15 km W-E. Southern New England Orogen. Geochemistry described.||Pringles Monzogranite.||Intrudes Sandon beds. Abuts Rocky Glen, Banalasta and Namoi Tops Monzogranites and possibly Tilmunda Syenogranite Phase.|Equigranular to seriate, leucocratic, K-feldspar-rich, biotite monzogranite, and possibly syenogranite. S-type.|
25452|Round Flat Tonalite|22815|4|Described|p49,51|Early Devonian|Late Silurian|Rb/Sr age: 412.7 +/-9.2 Ma.||||||
25452|Round Flat Tonalite|23549|5|Briefly described|p516.|||Of the Jindabyne Suite.||||||16-FEB-05
25452|Round Flat Tonalite|35109|2|Defined|p69|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
25452|Round Flat Tonalite|35263|6|Mentioned|Table 3|||Variation of Roundflat?||||||
25452|Round Flat Tonalite|36411|6|Mentioned|p270|||Refers White et al 1977 for definition.||||||
25452|Round Flat Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
25452|Round Flat Tonalite|40328|4|Described|p210|||||||||
25452|Round Flat Tonalite|41905|6|Mentioned|p93|||||||||
25452|Round Flat Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Jindabyne Suite.||||||
25452|Round Flat Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh10||||||
25452|Round Flat Tonalite|49705|5|Briefly described|p38|||This ref. is not a publication! BMR records became publications in July 1991.||||||
25452|Round Flat Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
76966|Round Mountain Leucomonzogranite|69639|5|Briefly described|p3, p112, p118, p124, p128, p223-p224|Triassic|Triassic|New England Orogen.|238 +/- 1.6 Ma (Cross and Blevin, 2013)|||||
76966|Round Mountain Leucomonzogranite|71628|4|Described|p17: 1-2, 5, 13-15, 32-36, 90, 98|||Previously Round Mountain Leucoadamellite (Leitch et al., 1971). Renamed to align with IUGS nomenclature. Named after Round Mountain; occurs ~5 km SW of Ebor. Has excellent outcrop as tors and pavements, with pervasive jointing (050). Geochemistry detailed. Is associated with lode Sn deposits and disseminated stockwork Mo occurrences (named).|238.0 +/- 1.7 Ma (SHRIMP: Cross and Blevin, 2013).|Round Mountain Suite.||Intrudes Sandon Association, Nambucca beds, Dyamberin beds and Abroi Granodiorite.|White to pink, fine- to medium-grained, equigranular to weakly porphyritic, biotite leucomonzogranite with minor hornblende-biotite leucomonzogranite; contains small pods of pegmatite; intruded by felsic dyke swarms and veins. I-type.|
27559|Round Top Formation|22857|4|Described|p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Byron Range Group. Quartzite, siltstone. Max. thickness: 30m. Geological Province: Bogan Gate Terrace.||||||
27559|Round Top Formation|23522|5|Briefly described|p248 Fig 4|Early Devonian|Early Devonian|||||||
27559|Round Top Formation|30790|6|Mentioned|p1|||Devonian. Member Byron Range Group||||||
27559|Round Top Formation|33325|5|Briefly described|Table 4|||||||||
27559|Round Top Formation|33327|5|Briefly described|p173|||See also Fig.2. Byron Ra. Gp.||||||
27559|Round Top Formation|33732|5|Briefly described|p111|||||||||
27559|Round Top Formation|34184|5|Briefly described|p5|||Devonian||||||
27559|Round Top Formation|34403|4|Described|p145|||||||||
27559|Round Top Formation|34405|6|Mentioned|Fig.3.15|||||||||
27559|Round Top Formation|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
27559|Round Top Formation|60086|5|Briefly described|Map legend|Late Devonian|Middle Devonian|Of the Byron Range Group.  Quartzite, siltstone.||||||19-JUL-04
27559|Round Top Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Ravine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
28979|Rouse Hill Siltstone Member|35690|2|Defined|p177|Middle Triassic|Middle Triassic|||||||
28979|Rouse Hill Siltstone Member|39298|5|Briefly described|p262|||||||||
28979|Rouse Hill Siltstone Member|39626|6|Mentioned|p276|||||||||
28979|Rouse Hill Siltstone Member|40602|4|Described|p22|||||||||
28979|Rouse Hill Siltstone Member|42896|4|Described|p41, Fig.7|||of Ashfield Shale||||||
28979|Rouse Hill Siltstone Member|42925|4|Described|p22|||of Ashfield Shale||||||
28979|Rouse Hill Siltstone Member|70661|6|Mentioned|p211|Middle Triassic|Middle Triassic|Age derived from parent unit. Not present in the map sheet area (Moss Vale)||Ashfield Shale||||
26878|Rowan Formation|22601|6|Mentioned|410|Permian|Permian|Parent Greta Coal Measures. Geol province Sydney Basin. Overlying unit Jasdec Park Sandstone Member||||||
26878|Rowan Formation|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Greta Coal Measures. Coal seams, siltstone, sandstone. Max. thickness: >110m. Geological Province: Sydney Basin.||||||
26878|Rowan Formation|22969|4|Described|Fig 4.1a||Early Permian|||||||
26878|Rowan Formation|23350|4|Described|270|Early Permian|Early Permian|Contains the Ayrdale Sandstone Member.  Age: 268.9+/-2Ma.||||||14-JUL-04
26878|Rowan Formation|31881|4|Described|p340|||Refers Basden (1969)||||||
26878|Rowan Formation|31882|6|Mentioned|p244|||Gyarran Volcanics||||||
26878|Rowan Formation|34015|4|Described|p328|||Permian member of Greta C.M.||||||
26878|Rowan Formation|34345|6|Mentioned|Fig.5.7|||||||||
26878|Rowan Formation|36940|6|Mentioned|p141|||||||||
26878|Rowan Formation|37087|6|Mentioned|p194|||||||||
26878|Rowan Formation|37773|4|Described|p18|||||||||
26878|Rowan Formation|39288|6|Mentioned|p61|||||||||
26878|Rowan Formation|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
26878|Rowan Formation|39664|6|Mentioned|p117|||||||||
26878|Rowan Formation|40331|6|Mentioned|p3|||||||||
26878|Rowan Formation|41054|6|Mentioned|Fig.3|||||||||
26878|Rowan Formation|41834|6|Mentioned|p590|||||||||
26878|Rowan Formation|41902|5|Briefly described|p5 Table 1|||||||||
26878|Rowan Formation|42182|5|Briefly described|p298|||||||||
26878|Rowan Formation|42916|5|Briefly described|Table 1|Middle Permian|Early Permian|||||||
26878|Rowan Formation|43017|5|Briefly described|Fig.1,p372|||||||||
26878|Rowan Formation|43194|5|Briefly described|p103, p129 Tb. 8.3|Early Permian|Early Permian|Of Greta Coal Measures, Sydney Basin. Correlative of Maules Creek Formation in the Gunnedah Basin.||||||
26878|Rowan Formation|43257|5|Briefly described|Map Legend||Permian|Age Middle Permian. Of Greta Coal Measures.||||||
26878|Rowan Formation|44244|5|Briefly described|p232|Permian|Permian|Of the Greta Coal Measures.  Sandstone, siltstone, claystone, coal and minor conglomerate.  Overlies the Skeletar Formation.||||||
26878|Rowan Formation|45090|5|Briefly described|p152|||See also P26||||||
26878|Rowan Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
26878|Rowan Formation|61529|5|Briefly described|p854 Fig. 1b|Late Permian|Late Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin.||||||
26878|Rowan Formation|68003|5|Briefly described|p38 Fig.3-j, p131.|Late Permian|Late Permian|Hunter Coalfield (Sydney Basin), Brigalow Belt South Bioregion.||Upper unit in Greta Coal Measures.||Overlies Skeletar Formation. Is overlain by Branxton Formation.|Coal seams, siltstone, sandstone.|
26878|Rowan Formation|68004|5|Briefly described|p23 Table 1.|||Hunter Coalfield.||Upper unit in Greta Coal Measures.||Overlies Skeletar Formation. Is overlain by Branxton Formation.|Sandstone, siltstone and coal seams.|
26878|Rowan Formation|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Muswellbrook area.||Unit in Greta Coal Measures.|Includes Ayrdale Sandstone Member.|||
26878|Rowan Formation|70096|5|Briefly described|Supp4|||Of northern Sydney Basin. CA IDTIMS date of 271.60+\-0.08 Ma (Metcalfe et al., 2014; see supplementary information). See also supplementary files in appendix for additional stratigraphic and locality information.||Unit of Greta Coal Measures.||||
26878|Rowan Formation|70791|5|Briefly described|p277, p286-287, p293 Fig.17|Cisuralian|Cisuralian|Hunter Coalfield and north Werrie Basin.||Greta Coal Measures.|Narrawolga, Aberglen, Britton, Cintra, Doyles Hill, Eurunderee, Friendly, Faithful, Hilltop, Fleming, Hallett, Muswellbrook, Saint Heliers, Puxtrees, Thiess, Brougham, Coal Measures;Ayrdale Sandstone.|||
26878|Rowan Formation|70837|5|Briefly described|p246|Lopingian|Guadalupian|Of Northern Sydney Basin. CA-TIMS ages of 271.6 Ma (Metcalfe etal., 2015). ||||||
26878|Rowan Formation|70878|5|Briefly described|p712, p720-721|Permian|Permian|Muswellbrook area. Calibration of palynological ages. Other ages given.|271.60 +/- 0.11 Ma.|Topmost Greta Coal Measures.||Is overlain by Branxton Formation.|Includes tuff layers.|
26878|Rowan Formation|71701|5|Briefly described|p169|||Sydney Basin.|||Includes the Greta Coal Measures.|||
26878|Rowan Formation|73304|5|Briefly described|p61, p65-66, p75-76, p78-79|Roadian|Roadian|Sydney Basin. Includes evidence of the [Permian] greenhouse crisis. Age from near the top of the formation.|271.60 +/- 0.33 Ma U-Pb CA-TIMS.|Greta Coal Measures||||
26878|Rowan Formation|73421|6|Mentioned|p17|Roadian|Roadian|Sydney Basin, northern. Lower Roadian. Equated with uppermost part of the Pebbley Beach Formation by Metcalfe et al., (2015) and Briggs (1998).|271.6 +/- 0.08 Ma CA-TIMS|Greta Coal Measures, upper part.||||
29693|Rowen Brae Porphyry|23214|2|Defined|p81|Late Ordovician|Late Ordovician|Intrudes the Fairbridge Volcanics and lower portion of the Weemalla Formation. Dark grey dacite to latite porphyry.||||||
29693|Rowen Brae Porphyry|43640|5|Briefly described|Map Legend||Ordovician|||||||
29693|Rowen Brae Porphyry|43782|6|Mentioned|Map Legend|Eastonian|Eastonian|||||||
29693|Rowen Brae Porphyry|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
26323|Roxburgh Formation|22529|5|Briefly described|7|Lochkovian|Lochkovian|||||||
26323|Roxburgh Formation|22590|6|Mentioned|Fig3 P754|Pragian|Lochkovian|||||||
26323|Roxburgh Formation|22857|4|Described|p474 App.1 Tb.A1.6|Lochkovian|Lochkovian|Of the Kandos Group. Arenite, rare volcaniclastic conglomerate and accretionary lapilli tuff horizons. Max. thickness: 750m. Geological Province: Capertee Rise.||||||14-NOV-13
26323|Roxburgh Formation|23043|5|Briefly described|Map Legend|Pragian|Lochkovian|of Kandos Group.||||||
26323|Roxburgh Formation|23170|2|Defined|p132|Early Devonian|Early Devonian|of Kandos Group.||||||
26323|Roxburgh Formation|23522|5|Briefly described|p248 Fig 4|Pragian|Lochkovian|||||||
26323|Roxburgh Formation|36285|2|Defined|p56|Early Devonian|Early Devonian|See also Fig.2.& 3.||||||
26323|Roxburgh Formation|39660|6|Mentioned|p450|||||||||
26323|Roxburgh Formation|42379|3|Fully described|p204|Early Devonian||Used by Pemberton 1980. Age: Pragian?||||||
26323|Roxburgh Formation|43043|3|Fully described|p91|||Approximate Pragian age||||||
26323|Roxburgh Formation|43188|4|Described|p207,Table 3 p208|Pragian|Lochkovian|Representative sections locations given.Age late Lochkovian to ?early Pragian. Of Kandos Group.||||||
26323|Roxburgh Formation|44093|5|Briefly described|p212 App. 1|Early Devonian|Early Devonian|Of the Kandos Group. See also p56 Photo 5. Geological Province: Lachlan Fold Belt.||||||
26323|Roxburgh Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cudgegong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26323|Roxburgh Formation|73299|6|Mentioned|p1096 Fig.3, p1098 Fig.4, p1099|||Capertree High. Rapidly thins eastwards from the Razorback Fault. [Map symbol suggests Devonian age]||||Overlies the Tanabutta Group, underlies the Riversdale Volcanics.||
81636|Ruby Creek Leucogranite|71628|4|Described|p1-7; p5: 1-2, 11; p11-11; p12: 5, 10|Middle Triassic|Middle Triassic|See also p12: 12, 17; p15: 2-3, 5, 32, 34-35, 37, 40-41, 43, 49-50, 53, 55, 57-58, 62, 65-67, 70, 72-73, 75-92, 97, 99, 101-103, 112; p16: 1, 9; p19: 6, 59, 63, 83, 88, 118-119, 131, 133, 150, 159-160, 162. Flinter (1982); previously Ruby Creek Adamellite, granite, Adamellite-Granite, Granite and Leucoadamellite. Named after a local watercourse. Widely distributed (~225 km2) throughout the Stanthorpe Complex (location and brief description of the larger masses given); also occurs as dykes, pods and irregular stocks. Exposure is variable, with flatter terrain characterised by poor sandy (quartz) soil. Cut by NNE-trending vertical joints. Lithology, mineralogy, geochemistry and mineralisation (named Sn-W-Mo deposits) are detailed. Is geochemically assigned to the Ruby Creek Suite within the Stanthorpe Supersuite. RELATED UNITS (continued): Abuts Amiens and Mount Norman Leucomonzogranites; Mount Lindesay, Severn River, Jenners and The Ram Swamp Monzogranites. Partly encloses (?is intruded by) Donnellys Castle Leucomonzogranite.|241.9 +/- 1.2 Ma (SHRIMP: Chisholm et al., 2014).|Stanthorpe Complex.||Intrudes Texas beds; Wallangarra Volcanics; Bungulla, Passchendaele, Waroo, Ballandean, Jenners, Mount Marley Monzogranites; Warroo Monzogranite Phase?. See COMMENTS for more.|Pink to white, rarely pale to medium grey, very fine- to medium-grained, weakly porphyritic (marginal) to equigranular, biotite leucomonzogranite to leucosyenogranite; abundant miarolitic enclaves. I-type.|
81636|Ruby Creek Leucogranite|72078|6|Mentioned|p4|Triassic|Triassic|Geological province: New England Orogen. U-Pb SHRIMP date for zircon derived from Chisholm et al. 2014. Together with the Stanthorpe Granite forms the Ruby Creek Sn-W district.|241.9+\-1.2 Ma (SHRIMP U-Pb)|||||14-JAN-20
82409|Ruby Creek Suite|71628|5|Briefly described|p15: 35, 49, 76, 84|Middle Triassic|Early Triassic|||Stanthorpe Supersuite.|Ruby Creek Leucogranite, Donnellys Castle Leucomonzogranite (tentative).|||
35165|Rudd Bed|23055|6|Mentioned|Fig13p25|||Tuff marker bed in Upper Pilot coal seam.||||||
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|||||||
80085|Rutledge Conglomerate Member|71069|2|Defined|p114-116, p23, 24, p39 fig 16, p41, 87|Late Silurian|Wenlock|Named for the Rutledge Trigonometrical Station. Previously mapped as an unnamed conglomerate of the Copper Gossan beds. Previously referred to as the Rutledge Quartzite Member. A new type section has been proposed in this study at GR 723149 6056672 to 723036 6056564. 100m thick at the type section to in excess of 300m thick east of Foxlow Creek.  Deposited in a subaerial to shallow marine, alluvial fan environment. Previously referred to as the Rutledge Quartzite Member of the Copper Creek Shale. Intepreted to have been deposited as a subearial to shallow marine fan. Directly correlates with unnamed basal conglomerate of the Mount Fairy Group.Age determined by its stratigraphic relationships. Distribution,  geomorphology, tectonic structure, primary structures/textures, metamorphism and geophysical characteristics discussed. See also p100, 101 fig 31, p102-103 fig 32, p105, p106, p110, p120.||Base of Captains Flat Formation||Overlain by the Captains Flat Formation|Massive to normally graded, medium to thickly bedded, cream to brown, fine to coarse grained quartz arenite to lithic arenite and well rounded to angular, clast-supported, pebble conglomerate.|22-SEP-17
80085|Rutledge Conglomerate Member|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Captains Flat Formation.|||Cream to brown, poorly sorted, pebble conglomerate to medium-grained lithic sandstone; occasionally imbricated; clasts/lithics include black shale, chert, quartz sandstone, siltstone and quartzite.|
26884|Saddleback Latite Member|22488|5|Briefly described|p841|||||||||
26884|Saddleback Latite Member|22857|5|Briefly described|p532 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Broughton Formation (Shoalhaven Group). Latite members of Broughton Formation and Pheasants Nest Formation (Illawarra C.M.) together form Gerringong volcanic facies. Geol. Prov: Sydney Basin.||||||
26884|Saddleback Latite Member|23544|5|Briefly described|Table 1 p360.|||In the Broughton Formation.||||||
26884|Saddleback Latite Member|29900|6|Mentioned|p175|||||||||
26884|Saddleback Latite Member|29901|4|Described|Table 1|||||||||
26884|Saddleback Latite Member|31128|6|Mentioned|Table 1|||||||||
26884|Saddleback Latite Member|31887|6|Mentioned|p4|||||||||
26884|Saddleback Latite Member|32938|6|Mentioned|p67|||Geology.||||||
26884|Saddleback Latite Member|36220|4|Described|p37|||See also Table 1.||||||
26884|Saddleback Latite Member|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
26884|Saddleback Latite Member|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
26884|Saddleback Latite Member|38690|4|Described|p291|||||||||
26884|Saddleback Latite Member|40270|6|Mentioned|Table 1|||||||||
26884|Saddleback Latite Member|40519|6|Mentioned|Fig.3|||||||||
26884|Saddleback Latite Member|45090|6|Mentioned|p171|||Refers Hanlon et al. (1953)||||||
26884|Saddleback Latite Member|67500|5|Briefly described|p12 Tb.1|Late Permian|Late Permian|Between 18-35m thick.||Of the Broughton Formation and Gerringong volcanic facies.|||Pillowed, coarsely porphyritic flow, with phenocrysts of labradorite and augite.|01-MAY-12
26884|Saddleback Latite Member|71115|5|Briefly described|p178-180, 182-185, 187-188, 195|Permian|Permian|Southern Sydney Basin. Note revised stratigraphic location of this Member and Dapto Latite Member. Geochemically similar to Dapto Latite Member. Paleomagnetic results tabulated, discussed.||Gerringong Volcanics.||Overlies Dapto Latite Member. Is overlain by Cambewarra Latite Member.|Dark-coloured latite, aphanitic to porphyritic with short prismatic pyroxene phenocrysts in texture, with a crystalline groundmass.|
26884|Saddleback Latite Member|73494|5|Briefly described|p542-543|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanics.|||Shoshonitic basalt. Porphyritic (usually plagioclase); locally vesicular or amygdaloidal.|
41588|Sailor Jack Granite|63732|5|Briefly described|Map legend|Early Triassic|Early Triassic|Grey, pinkish grey, or pale pink to pink, fine- to medium-grained, moderately to highly porphyritic hornblende-biotite monzogranite to clinopyroxene-biotite-hornblende granodiorite; locally granophyric; high magnetic response.||||||31-AUG-21
41588|Sailor Jack Granite|63748|3|Fully described|p36, p85-86 Appdx. 1|Early Triassic|Late Permian|In the Sailor Jack Suite. Intrudes Texas beds and Wallangarra Volcanics. Grey, pinkish grey or pale pink to pink, fine- to medium-grained, moderately to highly porphyritic. Contains widespread pink K-feldspar and accessory titanite. See also p27 Fig. 27.||||||07-FEB-11
41588|Sailor Jack Granite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Bungulla Monzogranite, and Ruby Creek, Dormans Flat and Stanthorpe Granites, are all mapped under the symbol, Rgn.||||||
41588|Sailor Jack Granite|68679|5|Briefly described|p453, p455, p457-459|Early Triassic|Permian|Northern New England Batholith. ~30 km2. Geochemistry described. Is similar chemically, but not mineralogically or texturally, to the Dormans Flat Granite. Photographs, geochemical plot.||Sailor Jack Suite.||Intrudes the Wallangarra Volcanics and Texas beds.|Grey to pink, fine- to medium-grained, porphyritic; cpx-biotite-hornblende granodiorite (~20% mafics) to hornblende-biotite monzogranite (~5% mafics); granophyric intergrowths locally. Strongly oxidised-reduced, moderately evolved, high-K, I-type.|
41588|Sailor Jack Granite|68901|6|Mentioned|p8 Fig. iii|Early Triassic|Late Permian|||||||27-SEP-18
41588|Sailor Jack Granite|69639|4|Described|p1, p5, p8, p44-p50, p220, p241|Lopingian|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described. Distinguishiable mineralogically and texturally but not chemically from the Ballandean Granite.|253.1 +/- 1.5 Ma (SHRIMP U-Pb)|Sailor Jack Suite||Intrudes the Texas Beds and Wallangara Volcanics (Wandsworth Volcanic Group).|Equigranular to inequigranular, medium- to coarse-grained granite.|
41588|Sailor Jack Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|253+/-1.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
41588|Sailor Jack Granite|71628|6|Mentioned|p12: 1, 12|||Donchak et al. (2007). Now Sailor Jack Monzogranite.||||||
82413|Sailor Jack Monzogranite|71628|3|Fully described|p5-1; p12: 1-2, 4-5, 7, 10, 12-19|||See also p15-57; p19: 6, 8. New name. Originally mapped as part of Stanthorpe Adamellite then Stanthorpe Monzogranite; later Sailor Jack Granite (Donchak et al., 2007). Probably named after Sailor Jack homestead. Type area is near MGA 379891 6796872, on Sailor Jack Station. It is unclear whether granodiorite or monzogranite dominates. Crops out over 30 km2 about 13 km W of Wallangarra. Forms tors, scattered boulders and pavements. Geochemistry described.|253.1 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Sailor Jack Suite.||Intrudes Texas beds (and locally is faulted against it), Wallangarra Volcanics and Ballandean Monzogranite.|Pale pink to pale grey, fine- to medium-grained, moderately to highly porphyritic hornblende-biotite monzogranite to clinopyroxene-biotite-hornblende granodiorite; locally granophyric. I-type.|
73887|Sailor Jack Suite|63748|5|Briefly described|p36, p43|Early Triassic|Late Permian|Of the Ballandean Supersuite. Includes Sailor Jack Granite.||||||07-FEB-11
73887|Sailor Jack Suite|68679|5|Briefly described|p457-458|Early Triassic|Permian|Northern New England Batholith.||Stanthorpe Supersuite.|Dormans Flat, Sailor Jack, Granites.|||
73887|Sailor Jack Suite|69639|5|Briefly described|p44, p220|||New England Orogen.||Ballandean Supersuite||||
73887|Sailor Jack Suite|71628|5|Briefly described|p12: 1, 3-4, 6, 8, 10-11, 13, 15|||Donchak et al. (2007); they initially included it in their Ballandean Supersuite. Reassigned to Sailor Jack Supersuite in this study. Appears erroneously as Sailor Jack Group on p12-6.||Sailor Jack Supersuite.|Sailor Jack Granite.; Accommodation Creek, Blacksmiths Creek, Passchendaele Monzogranites.|||
82412|Sailor Jack Supersuite|71628|5|Briefly described|p1-7; p12: 1-19; p15: 33, 52-53, 65, 75|Early Triassic|Permian|See also p19: 159-160. New unit; includes intermediate granites in the Ballandean-Tenterfield-Stanthorpe area. Apparently previously included in the Bungulla Monzogranite. Geochemically most similar to Llangothlin Suite.|||Sailor Jack, Dormans Flat, Gleamwoods, Quartz Pot Creek, Strathaven Suites: Accommodation Creek, Blacksmiths Creek, Storm King, Monzogranites.||Typically grey, pinkish-grey, pale pink to pink, fine-medium grained, porphyritic granodiorite to monzogranite. K-feldspar phenocrysts range from pink to white; ferromagnesians primarily hornblende and biotite. I-type.|
79108|Sainsbury Park Granite|69635|4|Described|p134-138, p69, 131|Early Devonian|Early Devonian|North-western Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation age. Shown as Sainsbury Park granite p136.|417.3+/-2.8 Ma|Of Tarcoon Suite. ||Age indistinguishable from Bobelah Granite, Compton Downs Granite.|Sample: Highly weathered quartz-biotite granite with a kaolinitic matrix with some feldspar pseudomorphs. The granite is massive, but is cut by narrow, 040deg-trending mylonitic shear-bands.|16-JUL-15
79108|Sainsbury Park Granite|70602|5|Briefly described|p65,66 Fig 2|Early Devonian|Late Silurian||417.3+/-2.6Ma|Tarcoon Plutonic Complex||Intrudes Girilambone Group.|I-type granite.|
79108|Sainsbury Park Granite|70821|5|Briefly described|p9-10, p13 Tb.2.1|Early Devonian|Early Devonian||417.3 +/- 2.6 Ma (Fraser et al., 2014).||||Granite.|01-DEC-16
79108|Sainsbury Park Granite|71345|2|Defined|p4,6,10-12|Early Devonian|Early Devonian|Type location: Lat -30.2602 Long 146.5418 (GR 455921 6652277) in a drainage gutter 125m south of the dam. Described by Proksch (1982) as a 'non-magnetic granite which crops out in the main homestead tank' at Sainsbury Park. Referred to as 'Sainsbury granites' by Hoatson (1982). Defined herein after Blevin (2011). Named for the Sainsbury Park homestead. [Misspelt as Sainsbury Pak Granite on p6]. Exposures on Bourke 1:250 000 map sheet lies over two blobby magnetic anomalies, together measure approximately 4 km N-S and 1.5km E-W. Recessive and poorly outcropping. Exposure limited to incised creek channels and under silcrete-capped breakaway. Massive with occasional thin 040° trending mylonitic zones (parallel to regional trends). SHRIMP U-Pb dating of zircons yielded magmatic age of 417.3+\-2.6 Ma (Fraser et al. 2014).|417.3+\-2.6 Ma (SHIRMP U-Pb; magmatic)|Unit of Tarcoon Suite.||Intrudes Girilambone Group.|Quartz-biotite granite with a kaolinitic matrix with some feldspar pseudomorphs (outcrop). Medium-grained, crystalline, magnetic, quartz (with green hue) - biotite - hornblende? 'quartz-mica-diorite' (drillcore).|02-DEC-19
79108|Sainsbury Park Granite|71860|5|Briefly described|p7|||Age is a SHRIMP U-Pb date.|417.3 +/- 2.6 Ma (Fraser et al, 2014)||||Granite.|
79108|Sainsbury Park Granite|72522|4|Described|p1, p10, p13, p15, p29, p133.|Lochkovian|Pridoli|Magmatic age by Fraser et al., 2014.|417.3 +/- 2.8 Ma|Tarcoon Suite|||Includes granite.|
75579|Saint Andrews beds|22831|4|Described|p36|Early Devonian|Silurian|Introduced Brunker (1972). Possibly n isolated roof pendant of Toongi Group sediments.|Inferred from intrusive relationship.|||Intruded and entirely surrounded by Obley Granite, of Yeoval Granite Complex.|Hornfelsed siltstone and shale with laminae. Calc-silicate hornfels near Minore prospect.|
75579|Saint Andrews beds|43441|5|Briefly described|27,23, 21|Early Devonian|Silurian|||||||
75579|Saint Andrews beds|44160|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
75579|Saint Andrews beds|68003|5|Briefly described|p143.|Devonian|Silurian|Lachlan Fold Belt. See also reference to Saint Andrews Beds (p24 Fig.3-e).|||||Fine- to medium-grained sandy and calc-silicate hornfels.|
26130|Saint Marys Formation|35098|4|Described|p1|||||||||
26130|Saint Marys Formation|41391|6|Mentioned|p46|||||||||
26130|Saint Marys Formation|42925|2|Defined|p29|early Miocene|late Oligocene|Saint is St in text.||||||03-OCT-07
26130|Saint Marys Formation|42926|4|Described|map legend|Miocene|Oligocene|Saint is St in text.||||||03-OCT-07
26130|Saint Marys Formation|70587|5|Briefly described|Map Legend|Miocene|Oligocene||||||Laterised sand and clay with ferricrete bands and minor silcrete.|
26130|Saint Marys Formation|70647|5|Briefly described|Map Legend|Neogene|Paleogene||||||Laterised sand and clay with ferricrete bands and silcrete.|
26130|Saint Marys Formation|73248|6|Mentioned|p302, App. p2|lower Miocene|upper Oligocene|[Written as St Marys Formation].||||||
25462|Salamagundia Granite|42726|5|Briefly described|map legend|Silurian||||||||
24487|Salisbury Sandstone|22857|5|Briefly described|p508 App.1 Tb.A1.8|Carboniferous|Carboniferous|Disconformably overlies Chichester Formation. Well-bedded medium-grained lithic arenite; lenses of conglomerate and mudstone. Max. thickness: 650m.||||||
24487|Salisbury Sandstone|36528|6|Mentioned|p179|||||||||
24487|Salisbury Sandstone|40883|6|Mentioned|Fig.2|||||||||
24487|Salisbury Sandstone|42547|4|Described|p32|||||||||
24487|Salisbury Sandstone|44093|5|Briefly described|p229 App. 1|Late Carboniferous|Early Carboniferous|In the Gresford Block. Geological Province: New England Fold Belt.||||||
24487|Salisbury Sandstone|44244|2|Defined|p120-121|Namurian|Visean|Overlies the Chichester Formation; underlies the Booral Formation.  max. thickness: >650m.  Type section in text.  Geological Province: Gresford Block.||||||
24487|Salisbury Sandstone|50147|5|Briefly described|Map legend|Namurian|Visean|Geological Province: Gresford Block.||||||
24487|Salisbury Sandstone|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Gresford Block, Tamworth Belt.||||||
24487|Salisbury Sandstone|71628|6|Mentioned|p6-22|||||Dewrang Group.||||
69884|Saltpetre Andesite Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Quialigo Volcanics (Bindook Group). Green-grey flow banded feldspar-pyroxene-phyric andesite; commonly vesicular and vuggy.||||||18-JUN-08
69884|Saltpetre Andesite Member|68592|2|Defined|p1061, p1071 Fig.174a, p1162-4, p1186-92|Pragian|Pragian|See also p852 Fig.143, p858, p878, p1056, p1654-7. New name, after Saltpetre Creek. Previously included in Gundary Beds, Towrang Beds and Gundary Formation. Type locality described. Similar geochemistry to Bushranger Volcanics and Forest Lodge Quartz Monzodiorite; suggested to be the extrusive equivalent of the latter. Geochemistry detailed; geophysical properties described. On p852 Fig.143, Gundary Volcanics incorrectly brackets Saltpetre Andesite Member as a constituent. Mid to late Pragian age from surrounding units.||Unit in Quialigo Volcanics.||Overlies the Newacres and Four Winds Ignimbrite Members, and Bullamalita Conglomerate.|Greenish grey, massive to commonly flow-banded porphyritic andesite, commonly amygdaloidal, with varying textures; sporadic monomictic andesite breccias and minor immature volcaniclastic rocks.|
69884|Saltpetre Andesite Member|69159|5|Briefly described|Map legend|Pragian|Lochkovian|||Unit in Quialigo Volcanics.|||Green-grey, moderately to strongly crystal-rich, pyroxene-plagioclase-phyric andesite.|02-SEP-15
69884|Saltpetre Andesite Member|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dkqs. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Quialigo Volcanics||Overlies Newacres Ignimbrite Member. Overlies Four Winds Ignimbrite Member, which also lenses out at base of this unit.|Green-grey, flow banded, commonly amygdaloidal, pyroxene-feldspar-phyric andesite.|
69884|Saltpetre Andesite Member|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Quialigo Volcanics|||Green-grey, flow banded, commonly amygdaloidal, pyroxene-feldspar-phyric andesite.|
69884|Saltpetre Andesite Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Quialigo Volcanics.|||Green-grey, moderately to strongly crystal-rich, pyroxene-plagioclase-phyric andesite.|
69884|Saltpetre Andesite Member|71700|5|Briefly described|vi, p24, CD|Middle Pragian|Middle Pragian|Named for the Saltpetre Creek at GR 748800 6136000. A representative locality is at GR 749885 6137660 in GOULBURN250. The andesite was included in the"Gundary Formation" by Jones et al. (1995) above a volcanic conglomerate unit now recognised as the Bullamalita Conglomerate (Thomas & Pogson 2012). Historically, the rocks were included in either"Gundary Beds" (Brunker et al. 1970; Felton 1974a) or"Towrang Beds" (Brunker & Offenberg 1970; Offenberg 1974). Occurs in the Goulburn 250k map sheet in the northwest of the Braidwood 1:100k sheet. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics and distinguishing features are discussed. This unit is estimated to be about 220m thick. Age is derived from dating of over- and underlying formations.||Quialigo Volcanics||Disconformably overlies the Four Winds Ignimbrite Member, Newacres Ignimbrite Member and the Bullamalita Conglomerate. Overlies the Boxers Creek Formation.|Moderately to strongly crystal-rich, porphyritic andesite.|
27561|Saltwater Creek Formation|22601|6|Mentioned|412, 413|Permian|Permian|Parent Wittingham Coal Measures. Geol province Sydney Basin. Overlying unit Vane Subgroup||||||
27561|Saltwater Creek Formation|22857|4|Described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Vane Subgroup (Wittingham Coal Measures, Singleton Supergroup). Sandstone, siltstone, minor coaly bands. Max. thickness: 100m. Geological Province: Sydney Basin.||||||
27561|Saltwater Creek Formation|22969|6|Mentioned|p 22|||||||||
27561|Saltwater Creek Formation|29941|6|Mentioned|p13|||||||||
27561|Saltwater Creek Formation|29942|3|Fully described|p12|||||||||
27561|Saltwater Creek Formation|29943|6|Mentioned|p39|||||||||
27561|Saltwater Creek Formation|29944|6|Mentioned|FIg.18|||||||||
27561|Saltwater Creek Formation|30005|6|Mentioned|p81|||||||||
27561|Saltwater Creek Formation|31124|5|Briefly described|Table 1|||Petrology. See also P17 & Fig. 1, 2.||||||
27561|Saltwater Creek Formation|31125|6|Mentioned|p16|||Geology||||||
27561|Saltwater Creek Formation|34448|5|Briefly described|p432|||Permian||||||
27561|Saltwater Creek Formation|34466|3|Fully described|p351|||||||||
27561|Saltwater Creek Formation|34569|6|Mentioned|p10|||Permian||||||
27561|Saltwater Creek Formation|35823|6|Mentioned|p31|||||||||
27561|Saltwater Creek Formation|37087|6|Mentioned|p197|||||||||
27561|Saltwater Creek Formation|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27561|Saltwater Creek Formation|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27561|Saltwater Creek Formation|40166|6|Mentioned|Table 1|||||||||
27561|Saltwater Creek Formation|41010|6|Mentioned|Fig.1|||||||||
27561|Saltwater Creek Formation|41054|6|Mentioned|Fig.3|||||||||
27561|Saltwater Creek Formation|41604|5|Briefly described|p5|||||||||
27561|Saltwater Creek Formation|41834|6|Mentioned|p590|||||||||
27561|Saltwater Creek Formation|41902|5|Briefly described|p5 Table 1|||||||||
27561|Saltwater Creek Formation|42916|5|Briefly described|Table 1||Late Permian|||||||
27561|Saltwater Creek Formation|42946|6|Mentioned|p32|||||||||
27561|Saltwater Creek Formation|43017|5|Briefly described|Fig.1,p372|||||||||
27561|Saltwater Creek Formation|43257|5|Briefly described|Map Legend||Late Permian|Of Wittingham Coal Measures.||||||
27561|Saltwater Creek Formation|44244|4|Described|p234, p291|Late Permian|Late Permian|Basal unit of the Wittingham Coal Measures.  Underlies the Vane Subgroup.  max. thickness: 40m; 16m in type section.  Geological Province: Sydney Basin.||||||26-AUG-04
27561|Saltwater Creek Formation|45090|6|Mentioned|p26|||Relationship of rock units||||||
27561|Saltwater Creek Formation|50268|5|Briefly described|Map Legend|Tatarian|Tatarian|Geological Province: Sydney Basin.  Overlies: Maitland Group.  Underlies: Vane Subgroup.  Of the Wittingham Coal Measures.||||||
27561|Saltwater Creek Formation|60281|5|Briefly described|p59-60|Late Permian|Middle Permian|Shallow marine and shoreface facies.  Overlies the Mulbring Formation.  Geological Province: Sydney Basin.||||||
27561|Saltwater Creek Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wittingham Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
27561|Saltwater Creek Formation|61529|5|Briefly described|p854 Fig. 1b|Late Permian|Late Permian|Of the Wittingham Coal Measures. Geological Province: Sydney Basin.||||||03-FEB-06
27561|Saltwater Creek Formation|68003|5|Briefly described|p130.|Permian|Permian|Hunter Coalfield, Sydney Basin.||Unit in Wittingham Coal Measures.|||Sandstone, siltstone, minor coal bands.|
27561|Saltwater Creek Formation|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield. Thickness varies from 10 to 100 m.||Basal unit in Wittingham Coal Measures.||Overlies Mulbring Siltstone. Is overlain  by Vane Sub-group.|Passes upwards from dark marine siltstone to quartz-lithic sandstone with minor siltstone and claystone bands.|
27561|Saltwater Creek Formation|69683|6|Mentioned|p411 Fig.2, p416 Fig.3|Late Permian|Late Permian|||Unit in Wittingham Coal Measures.||||
32683|Sandal Member|50385|5|Briefly described|Map Legend|Silurian|Silurian|Of Burcher Greywacke. Sandstone, siltstone, chert.||||||
67995|Sandon Association|61003|5|Briefly described|p224-225|Carboniferous|Devonian|Informal name. Part of the Tablelands Complex of Korsch (1977).||||||
67995|Sandon Association|63774|6|Mentioned|p1075, p1078, p1080, p1084, p1085|||||||||
67995|Sandon Association|71280|6|Mentioned|p402|||Armidale district. Also referred to as Sandon Beds (p402, p404, p411-412).||||||
67995|Sandon Association|71628|5|Briefly described|p3: 5, 25, 35, 49, 61, 64, 75, 86|Carboniferous|Devonian|See also p4-58; p7: 15, 31, 39; p8-107; p13: 4, 10, 21; p17: 4-5, 33; p18-18; p19: 37, 72, 151. RELATED UNITS (continued): Callaghans Creek Quartz Monzodiorite; Moonbi and Walcha Road Monzogranites; Linden Hill Tonalite; Rockisle Granodiorite; Highlands Complex; Round Mountain Leucomonzogranite; Dandahra Creek Leucosyenogranite (also faulted against this last). Is faulted against Grasstree Quartz Monzodiorite.||||Is intruded by the (western) Hillgrove Supersuite, eg Campfire, Enmore, Gostwyck, Kilburnie, Mirani, Rocky Glen Monzogranites; Ingleba Leucomonzogranite. See COMMENTS for more.|Mainly lithic-rich sandstone with abundant chert, metabasite with rare limestone.|
28301|Sandon beds|721|5|Briefly described|Map legend|Late Carboniferous|Late Devonian|Low-grade, regionally metamorphosed, multiply deformed lithic wacke, paraconglomerate, siltstone, mudstone, minro chert, jasper, spillite.||||||21-DEC-04
28301|Sandon beds|22857|6|Mentioned|p204|||||||||
28301|Sandon beds|22859|6|Mentioned|p204-05|||||||||
28301|Sandon beds|23050|4|Described|p14 Table 1|Early Carboniferous|Early Carboniferous|Age: Early Carboniferous (Tournisian to early Visean) based on radiolaria.||||||
28301|Sandon beds|23051|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
28301|Sandon beds|23720|5|Briefly described|Map Legend|||Part of the "Sandon Association".||||||08-DEC-04
28301|Sandon beds|23790|5|Briefly described|p10 Fig. 2|Early Carboniferous|Early Carboniferous|Geological Province: Central Block||||||
28301|Sandon beds|24366|5|Briefly described|p7, 9|Early Carboniferous|Early Carboniferous|||||||
28301|Sandon beds|35020|6|Mentioned|p345|Early Carboniferous|Early Carboniferous|||||||
28301|Sandon beds|37509|6|Mentioned|p504|||||||||
28301|Sandon beds|38222|6|Mentioned|Fig.2|||||||||
28301|Sandon beds|41009|6|Mentioned|p6|||||||||
28301|Sandon beds|41329|6|Mentioned|p6|||||||||
28301|Sandon beds|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Part of the "Sandon Association".||||||16-DEC-04
28301|Sandon beds|42297|5|Briefly described|p3|Late Devonian||||||||
28301|Sandon beds|42378|6|Mentioned|Table 1 P11|||||||||
28301|Sandon beds|42554|5|Briefly described|p43|||||||||
28301|Sandon beds|42629|5|Briefly described|p360|||||||||
28301|Sandon beds|42729|5|Briefly described|p12|||Early Carboniferous||||||
28301|Sandon beds|42748|6|Mentioned|Fig.3 P9|Carboniferous||||||||
28301|Sandon beds|42866|5|Briefly described|Table 2, P12|||||||||
28301|Sandon beds|42901|5|Briefly described|p411, Fig.12 p412|||||||||
28301|Sandon beds|43091|5|Briefly described|Map legend|||||||||
28301|Sandon beds|43745|6|Mentioned|Fig.4,p13|||||||||
28301|Sandon beds|44093|5|Briefly described|p76 (photo)|Paleozoic|Paleozoic|Age: middle Palaeozoic. Unconformably overlies Armidale beds. Of the Armidale Block. Geological Province: New England Fold Belt.||||||07-NOV-08
28301|Sandon beds|44450|3|Fully described|p12 Table 1|Early Carboniferous|Late Devonian|Overlain by Dummy Creek Conglomerate. Geological Province: New England Fold Belt.||||||31-MAY-07
28301|Sandon beds|50016|5|Briefly described|p353|Carboniferous|Carboniferous|See also  Sandon Beds. Geological Province: New England Fold Belt||||||31-MAY-07
28301|Sandon beds|62534|5|Briefly described|p6, p11 (legend)|Early Carboniferous|Early Carboniferous|||||||07-FEB-11
28301|Sandon beds|62757|5|Briefly described|p3 Fig. 1|Early Carboniferous|Early Carboniferous|||||||07-FEB-11
28301|Sandon beds|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Cambrian|In Central Block and Woodsreef Melange.||||||31-MAY-07
28301|Sandon beds|66660|4|Described|p344|||Deformed and metamorphosed accretionary complex rocks: metagreywacke, metasiltstone, metabasalt. Intruded by the Mount Duval Monzogranite and the Newholme Monzogranite.||||||
28301|Sandon beds|68005|5|Briefly described|p18, p22, pp33-34, p155, p170.|Carboniferous|Carboniferous|Anaiwan terrane, Central Block, New England Fold Belt. Texas-Sandon association: a thick sequence of deep marine deposition; locally highly deformed; uppermost part of subduction complex.||||Overlies Whitlow Formation.|Turbidites only locally abundant; typically thin-bedded, coarse lithic wacke or conglomerate horizons, siltstone, mudstone with subordinate chert, jasper and spilite.|
28301|Sandon beds|68006|5|Briefly described|p25, p127.|Early Carboniferous|Late Devonian|Deposited in a deep marine setting; forms part of a subduction complex. Kaolinisation of this unit resulted in the Wades Brickworks deposit.||||Overlies Whitlow Formation.||
28301|Sandon beds|69188|5|Briefly described|p60|Early Carboniferous|Late Devonian|Part of the Central Complex in the New England region.||||Is intruded by the Highlands Complex.||
28301|Sandon beds|71628|5|Briefly described|p2-68; p4: 9, 17, 40, 47, 51; p7-39|Early Carboniferous|Late Devonian|See also p8: 8, 28, 32-34, 37, 39, 43-44, 61, 66, 72, 99, 102-103, 107, 109, 115; p13: 4, 10, 15, 17, 21; p17: 89, 98; p19: 1, 9, 33, 43, 55, 76, 141. RELATED UNITS (continued): Is also intruded by Blackfellows Gully, Glenburnie, Parlour Mountain and Elsmore Leucomonzogranites; Gilgai Leucogranite; Balala, Uralla, Shalimar, Tilbuster, Yarrowyck Granodiorites; Manuka Farm, Terrible Vale, Porphyritic Microgranodiorites; Myanbah and Honeysuckle Creek Leucosyenogranites; Highlands Complex; Big Hill Creek and Gunny Bag Granites; Bannaweera Gabbro.||||Is intruded by Shallow Lagoon, Banalasta, Namoi Tops, Pringles, Walcha Road, Gwydir River, Mount Duval, Newholme, Primley and Copeton Monzogranites. See COMMENTS for more.|Deformed and metamorphosed sediments (cherts and argillites).|
82655|Sandy Creek Monzogranite|71628|4|Described|p11: 2-11, 24-26, 33, 15: 92-96|||See also p12: 16, p15: 32, 106, 109-110; p16-20. New name, this study, after Sandy Creek Syenogranite of Mustard (2004). Comprises a narrow zone between his Rocky River monzogranite and Surface Hill syenogranite. Previously mapped as part of Bungulla Monzogranite. Named after a tributary of the Rocky (Timbarra) River. Occurs 30 km E of Tenterfield. Geochemistry detailed; is geochemically assigned to the Surface Hill Suite within the Stanthorpe Supersuite. Also appears as Sandy Creek monzogranite on p15-109.|251.6 +/- 2.8 Ma (SHRIMP: Mustard, 2001 unpubl.).|Stanthorpe Complex.||Is intruded by Surface Hill Leucomonzogranite. Abuts Rocky River Monzogranite.|Phenocryst-poor, fine- to coarse-grained, seriate to weakly porphyritic, leucocratic biotite-hornblende monzogranite-syenogranite. Comprises three variants (""zones""); detailed. I-type.|
82537|Sandy Flat Leucomonzogranite|71628|3|Fully described|p11: 3, 10-11, 13; p14: 1, 12, 27-30|||See also p15-9. New name (this study). Originally Sandy Flat Adamellite (Shaw, 1964); later Sandy Flat Leucoadamellite (Flinter, 1982) and subsequently Sandy Flat Monzogranite (Henley et al., 2001 after Barnes, 1987 unpublished). Named after a locality 21 km S of Tenterfield. The type locality is 1 km NE of Sandy Flat (Shaw, 1964). Occurs as a ca. 15 x 3 km NNE-trending elongate intrusion. Has excellent exposure as whalebacks and an absence of tors. Geochemistry described. Is associated with only minor mineralisation: base metals and an Au deposit.|253.6 +/- 1.1 Ma (SHRIMP: Chisholm et al., 2014).|Sandy Flat Suite.||Intrudes Dundee Rhyodacite (Wandsworth Volcanic Group). Is intruded by Mount Jonblee Leucomonzogranite and Bungulla Monzogranite.|Pink, coarse-grained, even-textured, biotite-(+/- hornblende) leucomonzogranite. I-type.|
26134|Sapling Flat Igneous Complex|32820|6|Mentioned|p3|||Cullarin Anticlinorium||||||
26134|Sapling Flat Igneous Complex|36413|2|Defined|p97|Devonian|Silurian|Siluro-Devonian age||||||
26134|Sapling Flat Igneous Complex|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Danswell Creek Granodiorite and Wangrah Adamellite.||||||
26134|Sapling Flat Igneous Complex|39626|6|Mentioned|p276|||||||||
26134|Sapling Flat Igneous Complex|39627|6|Mentioned|p268|||||||||
26134|Sapling Flat Igneous Complex|40328|4|Described|p210|||||||||
26134|Sapling Flat Igneous Complex|69270|6|Mentioned|p23||||||Tinderry Granite|||
83461|Sassafras Basalt|73581|5|Briefly described|p22-23|Eocene|Eocene|Southern Highlands Volcanic Province. List of K-Ar ages provided from Young and McDougall (1985).|50.9-41.2 Ma K-Ar||||Low-K tholeiite to alkali basalt. High-Ti mineralogy and mantle xenoliths.|
25465|Sassafras basalt|40591|4|Described|p324|||||||||
27652|Sawmill Tank Siltstone|22857|5|Briefly described|p442 App.1, Tb.A1.6|Pragian|Pragian|Of the Winduck Group. Thinly bedded siltstone, arenite. Geological Province: Winduck Shelf.||||||
27652|Sawmill Tank Siltstone|23173|6|Mentioned|Map Legend|||||||||
27652|Sawmill Tank Siltstone|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|Of Winduck Group.||||||
27652|Sawmill Tank Siltstone|35925|5|Briefly described|p2|||To be defined by Glen et al.||||||
27652|Sawmill Tank Siltstone|37798|4|Described|p128|||See also Table 1.||||||
27652|Sawmill Tank Siltstone|38292|6|Mentioned|p3|||||||||
27652|Sawmill Tank Siltstone|39660|6|Mentioned|p450|||||||||
27652|Sawmill Tank Siltstone|41138|6|Mentioned|Map legend|Pragian|Pragian|||||||
27652|Sawmill Tank Siltstone|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27652|Sawmill Tank Siltstone|41821|4|Described|p45|||||||||
27652|Sawmill Tank Siltstone|43032|2|Defined|p137|Early Devonian||Of Winduck Group||||||22-APR-09
27652|Sawmill Tank Siltstone|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Winduck Group (Cobar Supergroup).  Comprises mostly siltstone/ mudstone and ripple , cross-laminated fine sandstone.  Age is Pragian. Geological Province: Winduck Shelf.||||||
27652|Sawmill Tank Siltstone|64967|5|Briefly described|p114 Fig. 2|Pragian|Lochkovian|Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). See also p115 Fig. 3.||||||
27652|Sawmill Tank Siltstone|65469|5|Briefly described|p15-p17|Lochkovian|Lochkovian|Lachlan Orogen.||Winduck Group||||
27652|Sawmill Tank Siltstone|70037|4|Described|p309 Fig.2, p311|Early Devonian|Early Devonian|Glen (1979) initially placed this unit towards the top of the Amphitheatre Group, but reassigned it to the Winduck Group (Glen, 1982). Darling Basin. 500m thick.||Winduck Group.||Overlies Buckambool Sandstone. Is overlain by Gundaroo Sandstone.|Mainly siltstone and shale with thin interbeds of sandstone.|
27652|Sawmill Tank Siltstone|70751|6|Mentioned|p12|Pragian|Lochkovian|||Winduck Group||||
27652|Sawmill Tank Siltstone|72958|6|Mentioned|p11|Pragian|Lochkovian|Cobar Basin. Nymagee area.||Winduck Group||Underlain by and equivalent to Buckambool Sandstone. Overlain by Gundaroo Sandstone. Equivalent to Walters Range Group.||
27652|Sawmill Tank Siltstone|73174|6|Mentioned|p1037, p1039|Emsian|Emsian|Winduck Shelf. Time-transgressive basal and upper boundaries. Contains age-diagnostic brachiopod.||Winduck Group, Cobar Supergroup||Underlain by and equivalent to Buckambool Sandstone. Overlain by and equivalent to Gundaroo Sandstone.||
34600|Sawtooth Ridge Limestone Member|5253|6|Mentioned|p97|Devonian|Early Ludlow|Topmost member of Frome Hill Formation. Equivalent to Upper Limestone of Carr et al. 1990.||||||
34600|Sawtooth Ridge Limestone Member|22842|5|Briefly described|p29|Early Devonian|Late Silurian|||||||16-JAN-12
34600|Sawtooth Ridge Limestone Member|68592|5|Briefly described|p898, p915, p1892|||A unit in Frome Hill Formation of Bauer (1994). See also reference to Sawtooth Ridge Limestone (p1096-1097).||Unit in Frome Hill Formation.||Locally overlies Folly Point Limestone Member.|Mass-flow units containing pebbles of limestone.|
34600|Sawtooth Ridge Limestone Member|70661|3|Fully described|p31 tbl 1, p48, p49|Devonian|Devonian|Named after Sawtooth Ridge. Informally referred to previously as the upper limestone of the Bungonia Limestone.Up to 170m thick. Age partly derived from fossil assemblage. Deposited in a relatively shallow marine environment. Westerly dipping.||Frome Hill Formation||Conformably overlies Efflux Siltstone Member, Folly Point Limestone Member|Moderately bedded, sparsley fossiliferous micrite with interbeds of finely laminated algal micrite and lenses of calcareous and siliceous siltstone. The limestone contains up to 2% detrital quartz and is locally highly silicified.|
34600|Sawtooth Ridge Limestone Member|71303|5|Briefly described|map legend|Lochkovian|Ludlow|||Of Frome Hill Formation.|||Bedded, sparsely fossiliferous micrite with interbeds of finely laminated algal micrite and lenses of calcareous and siliceous siltstone. Intercalated lensoidal 'mass-flow' units containing fossil and limestone clasts locally.|
34600|Sawtooth Ridge Limestone Member|71656|6|Mentioned|p31|Lochkovian|Pridoli|Devonian brachiopod Cyrtina identified from this the latest unit of the Frome Hill Formation.||top of the Frome Hill Fromation, Bungonia Group|||Fossiliferous limestone.|
28989|Saxa Shale Member|29870|6|Mentioned|p13|||||||||
28989|Saxa Shale Member|30610|2|Defined|p325|Late Triassic|Late Triassic|Part of Talbragar Formation||||||
28989|Saxa Shale Member|35095|6|Mentioned|Table 1|||Reference Dulhunty 1973.||||||
28989|Saxa Shale Member|37757|6|Mentioned|p29|||||||||
23958|Saxonvale Member|40805|2|Defined|p140|Permian|Permian|Previously used as Saxonvale Claystone||||||
23958|Saxonvale Member|41010|6|Mentioned|Fig.2|||||||||
23958|Saxonvale Member|42648|6|Mentioned|p37|||||||||
23958|Saxonvale Member|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Mount Ogilvie Formation (Jerrys Plains Subgroup).||||||
23958|Saxonvale Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Mount Ogilvie Formation.||||
23958|Saxonvale Member|69683|6|Mentioned|p411 Fig.2|Late Permian|Late Permian|||Unit in Mount Ogilvie Formation.||||
40230|Scaham Formation|38801|5|Briefly described|p123 Fig.3|Stephanian|Namurian|Geological Province: New England Fold Belt||||||
33684|Schneiders Granite|24417|2|Defined|p113|Middle Devonian|Middle Devonian|||||||
33684|Schneiders Granite|60009|5|Briefly described|Map Legend|Eifelian|Eifelian|||||||13-JUL-04
74760|Scotts Craig Conglomerate|61964|2|Defined|p109, 104|Pragian|Pragian|Of Walters Range Group. Marker unit of pebbly sandstone to conglomerate. Thickness: 10-60cm. Gradational contact with underlying Yar Sst. Top obscured or faulted. See also misspelt Scotts Graig Conglomerate (p14 Fig. 4).||||||09-OCT-08
74760|Scotts Craig Conglomerate|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Walters Range Group.||Overlies Yar Sandstone.|Pebbly sandstone to conglomerate; trough cross-bedded with abundant clasts of vein quartz.|
75944|Scropes Range Formation|66623|1|Redefined|pp134-138, pp150-151.|Early Ordovician|Late Cambrian|Formerly part of Torrowangee Series (Mawson 1912), Mootwingee Series (Andrews 1922); type section defined by Packham (1968); mapped as Scopes (sic) Range Beds by Rose (1969); redefined and renamed in this study. Barren, recessive outcrops. Thickness varies laterally between c.1340 m and 2012 m. Correlated with Nootumbulla and Rowena Formations and Bynguano Quartzite; parts correlate in time with Pimbilla Tank, Warratta and Kayrunnera Groups.||Unit in Mutawintji Group.||Overlies Nuchea Conglomerate. Locally is overlain disconformably by Wana Karnu Group.|Weakly cleaved, white to maroon, red-bed, fluviatile, cross-bedded quartz sandstones in the southwest, grading to shallow marine quartz sandstones containing glauconite, trace fossils and marine macrofossils in the northeast.|25-SEP-13
75944|Scropes Range Formation|66918|5|Briefly described|Map legend|||||Unit in Mutawintji Group.||Map key suggests: Overlies Nuchea Conglomerate, is overlain by Nootumbulla Sandstone.|Weakly cleaved white to maroon fluviatile cross-bedded quartz sandstone, grading to shallow marine (increasing glauconite, trace fossils and trilobites); regionally metamorphosed to prehnite-pumpellyite facies.|25-SEP-13
75944|Scropes Range Formation|67322|4|Described|p12-13; Fig.5|Early Ordovician|Late Cambrian|Koonenberry Belt. Redefined by Greenfield (in Greenfield et al., 2010) from earlier mis-spelt usage of Scopes Range Beds. Age determined from p20 Fig.5 (Strat. column). 1385-2012 m thick. Occurs in the Bilpa-Comarto, Scropes Range regions.||Unit of the Mutawintji Group.||Locally, conformably overlies Nuchea Conglomerate. Correlated with Nootumbulla Sandstone, Bynguano Quartzite, Rowena Formation.|Formation consists of white to maroon cross-bedded (fluvial) quartz sandstone in the southwest, grading to (shallow marine) quartz sandstones to the northeast.|22-FEB-18
75944|Scropes Range Formation|70650|5|Briefly described|Map Legend|Ordovician|Cambrian|||Mutawintji Group|||Weakly cleaved white to maroon fluviatile cross-bedded quartz sandstone, gradation to shallow marine (increasing glauconite, trace fossils and trilobites).|
75944|Scropes Range Formation|70651|5|Briefly described|Map Legend|Ordovician|Cambrian|||Mutawintji Group|||Weakly cleaved white to maroon fluviatile cross-bedded quartz sandstone, gradation to shallow marine (increasing glauconite, trace fossils and trilobites).|
75944|Scropes Range Formation|75070|6|Mentioned|p184-185 Figs.7-8|||Broken Hill region. Appears as Scropes Formation. Mentioned in discussion of detrital zircon provenances.||||||
73110|Sea Acres Dolerite|63763|3|Fully described|p4-5 Fig. 1, p16|Late Triassic|Late Triassic|Previously mapped with Karikeree Metadolerite; now grouped separately due to chemical differences. Cuts most of local units. Dykes of fine- to medium-grained, dark green plagioclase-phyric dolerite, undeformed; more lith. detail incl. See also p7 Fig. 2.||||||
22827|Seal Rocks Formation|23157|5|Briefly described|p110,115 fig2,7,8|Carboniferous|Carboniferous|||||||
83331|Searles Point Formation|73136|4|Described|p192-193, p198|Middle Pleistocene[?]|Middle Pleistocene[?]|Lord Howe Island. Prominent at Searles Point and exposed at Hells Gates. Older and more diagenetically altered than the overlying Neds Beach Formation. Overlies basalt. Surface is generally heavily karstified and cave deposits and solutional features are common. Contains caves that extend down to the contact with the underlying basalt. Outcrop shows that the unit fills a bedrock valley on the southern side of North Bay. Much of the unit appears to have been deposited in marine oxygen isotope stage 7. Well-indurated and often recrystallised calcarenite, containing pore-filling sparite and microsparite, is yellow to pale brown. Also includes flowstones. Contact with overlying Neds Beach Formation is exposed near Old Settlement Beach. Max height of 75 m above sea level. [Written as Searles Beach Formation on p192].||||Overlain by the Neds Beach Calcarenite.|Diagenetically altered calcarenite comprising grains of coralline algae, molluscs, foraminifera, bryozoans, and some volcanic grains with only rare coral. Consists of eolianite units bounded by clay-rich brown and terra rossa palaeosols.|
83331|Searles Point Formation|73554|4|Described|Map legend, back of map|Quaternary|Quaternary|Lord Howe Island. Exposed at the base of the cliff at the southern end of Neds Beach. Possibly up to 130,000 years old. Contains fossil Meiolania (extinct stem-turtle), bird eggs, bird bones and marine shells, and land snails have been identified within the top of the unit (indicating some soil and vegetation were present at that time).|ca 0.13 Ma|||Overlain by Neds Beach Formation.|Yellow to pale brown calcarenite displaying medium- to large-scale cross-bedding and exposed relict speleothem such as stalactites and stalagmites and clay-rich palaeosol units.|
35101|Seven Foot Bed|23055|6|Mentioned|p24,Fig13p25|||||||||
82596|Severn River Monzogranite|71628|3|Fully described|p15: 4, 7, 34-36, 43, 46, 96-105|Middle Triassic|Middle Triassic|See also p15: 49, 55, 58, 65, 70, 73-75, 82, 115; p16-3; p19: 8, 19. New name, for a series of more mafic granites with considerable textural, mineralogical and chemical variability. These subunits do not 'technically' qualify as Phases according to stratigraphic naming conventions. Historically part of Stanthorpe Monzogranite. Named after the Severn River. Comprises several masses (locations and lithologies described) that outcrop irregularly from ~6 km N of Bullecourt to ~2 km SE of Wallangarra. Typically deeply weathered, with poor outcrop from soil cover. Geochemistry described; that of the individual 'Phases' is described separately; is geochemically assigned to Severn River Suite within Stanthorpe Supersuite. Is spatially associated with numerous typically small Sn deposits (named), and several gemstone occurrences in the Severn River area. RELATED UNITS (continued): Abuts Amiens, Mount Norman Leucomonzogranites, Ruby Creek Leucogranite and Mount Lindesay Monzogranite. Partly encloses (?is intruded by) Donnellys Castle Leucomonzogranite. Entirely encloses Mount Marley Monzogranite.|246.9 +/- 2.0 Ma (SHRIMP: Donchak et al., 2007).|Stanthorpe Complex.|Glenbrae, Eukey, Severnlea, Malachi, Cannon Creek, Broadwater, Applethorpe, Monzogranite Phases.|Intrudes Texas beds, Wallangarra Volcanics, Ballandean and Bungulla Monzogranites. Is faulted against Jenners Monzogranite. See COMMENTS for more.|Heterogeneous, pink to pinkish grey, moderately porphyritic, medium- to fine-grained (locally quenched), biotite-(hornblende) monzogranite-?syenogranite to leucocratic biotite monzogranite; locally contains miarolitic cavities and pegmatite. I-type.|
82595|Severn River Suite|71628|5|Briefly described|p15: 35, 73, 98|Middle Triassic|Early Triassic|Is geochemically assigned to the Stanthorpe Supersuite.||Stanthorpe Complex.|Mount Marley Monzogranite, Severn River Monzogranite.|||
82604|Shalimar Granodiorite|71628|4|Described|p7: 17-18; p8: 103-106|||New name (this study); originally Shalimar Tonalite (Binns et al., 1967) after unpublished work by Flood. Named after a local homestead. Forms a small (4 x 2 km) intrusion 5km SE of Wollun. Crops out as rounded boulders and prominent grey tors. Geochemistry described; similar to Callaghans Creek Quartz Monzodiorite. Several age determinations given.|238.1 to 247.0 Ma.|Uralla Supersuite.||Intrudes Sandon beds.|Grey, fine- to medium-grained, porphyritic, hornblende-biotite-quartz monzodiorite to quartz-poor granodiorite, with minor monzogranite. I-type.|
23964|Shannon Harbour Coal Member|37094|5|Briefly described|p240|||||||||
31633|Shannons Flat Suite|22815|6|Mentioned|p62|||||||||
31633|Shannons Flat Suite|42726|5|Briefly described|map legend||Silurian|||||||
31633|Shannons Flat Suite|43233|5|Briefly described|Map Legend||Silurian|Murrumbidgee Batholith.||||||
31633|Shannons Flat Suite|44093|5|Briefly described|p190 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||29-MAR-05
31633|Shannons Flat Suite|68592|5|Briefly described|p1253-4|||Chappell et al. (1991). Includes 4 plutons in the ACT-Cooma area.||Unit in Wyangala Supersuite.|||Non-fractionated granitoids.|
26891|Shannonvale Granodiorite|29988|6|Mentioned|Map legend|Permian|Permian|||||||
26891|Shannonvale Granodiorite|30787|6|Mentioned|p49|||Differentiation index||||||
26891|Shannonvale Granodiorite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
26891|Shannonvale Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26891|Shannonvale Granodiorite|35257|6|Mentioned|Fig.11|||||||||
26891|Shannonvale Granodiorite|38842|6|Mentioned|p286|||||||||
26891|Shannonvale Granodiorite|38905|6|Mentioned|p305|||||||||
26891|Shannonvale Granodiorite|42378|6|Mentioned|Table 1 P9|||||||||
26891|Shannonvale Granodiorite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wards Mistake Adamellite (Uralla Suite).||||||
26891|Shannonvale Granodiorite|71628|6|Mentioned|p8-91; p14: 8, 23|||Flinter (1982) after unpublished work by Dunlop (1966) and others. Flinter (1982) equated this unit with the more southern Wards Mistake Adamellite. Both now constitute the Wards Mistake Monzogranite.||||||
26892|Sharpeningstone Conglomerate|22857|4|Described|p458 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Black Range Group. Tuffaceous conglomerate, sandstone, siltstone. Redeposited fossiliferous limestone clasts. Max. thickness: 170m. Geological Province: Canberra-Yass Shelf. ||||||
26892|Sharpeningstone Conglomerate|24249|5|Briefly described|p90 Fig.3|Pridoli|Pridoli|||||||
26892|Sharpeningstone Conglomerate|30069|6|Mentioned|p7|||||||||
26892|Sharpeningstone Conglomerate|31852|6|Mentioned|p711|||See also Figs. 1,2,4,5. Gedinnian. Browning Group||||||
26892|Sharpeningstone Conglomerate|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Strat. Nomenclature||||||
26892|Sharpeningstone Conglomerate|33325|5|Briefly described|Table 2|||See also Table 3.||||||
26892|Sharpeningstone Conglomerate|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26892|Sharpeningstone Conglomerate|35386|4|Described|p46|||||||||
26892|Sharpeningstone Conglomerate|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
26892|Sharpeningstone Conglomerate|37727|6|Mentioned|p32|||||||||
26892|Sharpeningstone Conglomerate|38691|5|Briefly described|Fig.1|||||||||
26892|Sharpeningstone Conglomerate|39331|6|Mentioned|p46|||See Fig.5-3,5-4,5-5||||||
26892|Sharpeningstone Conglomerate|40328|6|Mentioned|p49|||||||||
26892|Sharpeningstone Conglomerate|45075|6|Mentioned|p8|||Fauna||||||
26892|Sharpeningstone Conglomerate|45147|6|Mentioned|M175|||||||||
26892|Sharpeningstone Conglomerate|50230|5|Briefly described|Map legend|Lochkovian|Lochkovian|Of the Black Range Group.  Overlain by Pilleuil Andesite.  Polymictic pebble to cobble conglomerate, pebbly sandstone and mudstone.||||||
26892|Sharpeningstone Conglomerate|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Black Range Group. Polymictic pebble to cobble conglomerate, pebbly sandstone and mudstone.||||||
26892|Sharpeningstone Conglomerate|68592|2|Defined|p81, p430 Fig.89, p926-30, p937-42|Lochkovian|Lochkovian|A conglomerate sequence around Bowning included in the Black Range Series of Brown (1940). This name published by Link (1970, 1971); Link and Druce (1972) as a unit in their Bowning Group which was renamed as Black Range Group by Pogson and Baker (1974); Cramsie et al. (1978). Named after Sharpeningstone Creek. Type section described. Over 168m thick. Forms gently undulating countryside. Geophysical properties described. Age based on stratigraphic grounds. Fossil fauna listed. Probable time-correlative of Brooklyn Conglomerate Member. Polymetallic vein  mineralisation (Pb, Ag and minor Cu) occurred in shafts of the [old] Bradford and Party Workings, S of Bowning.||Unit in Black Range Group.||Unconformably overlies Elmside Formation (Hattons Corner Group). Is overlain disconformably by Pilleuil Andesite. Is intruded by Waynes Knob Rhyolite.|Grey to maroon, medium- to very thick-bedded, poorly sorted, polymictic pebble- to cobble conglomerate and pebbly sandstone interbedded sporadically with mudstone and fine-grained lithic sandstone.|
26892|Sharpeningstone Conglomerate|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dbh. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Black Range Group||Unconformable base. Is unconformably overlain by Pilleuil Andesite.|Medium-very thickly bedded, poorly sorted, polymictic, pebble to cobble conglomerate to pebbly sandstone interbedded with subordinate mudstone and fine grained, lithic sandstone, especially towards top.|
26892|Sharpeningstone Conglomerate|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Medium-very thickly bedded, poorly sorted, polymictic, pebble to cobble conglomerate to pebbly sandstone interbedded with subordinate mudstone and fine grained, lithic sandstone, especially towards top.|
26892|Sharpeningstone Conglomerate|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Medium-very thick bedded, poorly sorted, polymictic, pebble-cobble conglomerate to pebbly sandstone, interbedded with subordinate mudstone and fine grained lithic sandstone, especially towards the top of the sequence.|
26892|Sharpeningstone Conglomerate|71040|5|Briefly described|p5|Pragian|Lochkovian|Associated with the Bowning (=Bindian) Orogeny.||||Unconformably overlies Elmside Formation.||
26892|Sharpeningstone Conglomerate|71656|5|Briefly described|p12 Fig.2, p31|Lochkovian|Lochkovian|Reworked clasts in the Sharpeningstone Conglomerate, derived from underlying Silurian strata (and hence providing evidence of the Bowning Orogeny) contain fragments of corals.||Black Range Group||Underlies Mountain Creek Volcanics.|Reworked clasts contain fragments of corals.|
26892|Sharpeningstone Conglomerate|71700|5|Briefly described|p23, p27|||Occurs on the Goulburn 250k map sheet. Overlies an unconformity at Mount Bowning near Yass.||Black Range Group||||
26892|Sharpeningstone Conglomerate|73215|6|Mentioned|p994|||Yass Syncline.||Black Range Group.||||
32274|Shaw Hill Gabbro|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Og5||||||
32274|Shaw Hill Gabbro|60078|6|Mentioned|Map Legend|Ordovician|Ordovician|||||||
32274|Shaw Hill Gabbro|60308|6|Mentioned|p38|Llandovery|Llandovery|"Important stratigraphic unit with contentious age" Preferred age quoted.|437 Ma|||||
81958|Shawns Creek Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|Includes the Crualch Member, Chalkers Ridge Member, Grand High Tops Member.||Crystal, vitric and scoria tuff, crystal vitric breccia, burnt wood-bearing pyroclastic deposits.|02-NOV-20
28997|Sheep Station Creek Complex|23720|5|Briefly described|Map Legend||Late Permian|Massive and foliated granite, gabbro, granodiorite.||||||15-DEC-04
28997|Sheep Station Creek Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28997|Sheep Station Creek Complex|31695|6|Mentioned|Fig. 1|||||||||
28997|Sheep Station Creek Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
28997|Sheep Station Creek Complex|35257|6|Mentioned|p75|||||||||
28997|Sheep Station Creek Complex|44450|5|Briefly described|p35|||Geological Province: Coffs Harbour Block.||||||
28997|Sheep Station Creek Complex|71628|4|Described|p2:1, 3, 20, 26, 44-49; p3:1, 3, 10, 27|||See also p17: 47-48, 50. Binns et al. (1967). Formerly assigned to the Hillgrove Supersuite and Chaelundi Complex. Named after a local watercourse. Crops out as 17 distinct masses, ~7 km NW of Dundurrabin. Assigned to the Bakers Creek Suite by Landenberger (1996) and to the Bakers Creek Supersuite by Landenberger et al. (2010). Diverse geochemistry detailed. Spatially associated with several mineral deposits; genetic relationships need further evaluation.|289.4 +/- 3.1 Ma (Rosenbaum et al., 2012).|Bakers Creek Supersuite.|Gumtree Monzogranite, Big Bull Gabbro.|Intrudes along the boundary between Moombil Siltstone and Brooklana beds.|Tholeiitic gabbro associated with a diverse range of calc-alkaline rocks: olivine gabbro, quartz gabbro, diorite, amphibole-biotite granodiorite, monzogranite and leucomonzogranite.|
70128|Shell Hill Formation|66623|2|Defined|pp192-193, pp202-203. |Middle Devonian|Early Devonian|Defined in this study. Formerly part of upper Snake Cave Sandstone. Correlated with Muckabunnya Formation and Menamurtee Sandstone. Thin unit; strike length of 25 km in Mutawintji National Park. Outcrop is poor to modest. Thickness varies around c.250 m. Contains 11 taxa of fish fossils, many new forms. Planar bedding universally preserved.||Unit in Wana Karnu Group.||Overlies Old Coach Road Formation. Is overlain by Bengoro Ridge Formation.|White to buff, poorly sorted, weakly indurated quartz sandstone, pebbly sandstone, siltstone and conglomerate; flakes of detrital mica common; commonly ferruginised as in the basal red siltstone with fine interbeds of red sandstone.|
70128|Shell Hill Formation|66918|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Wana Karnu Group.||Map key suggests: overlies Homestead Gorge Formation, is overlain by Old Coach Road Formation.|White to buff, poorly-sorted, lightly indurated quartz sandstone, pebbly sandstone, siltstone and conglomerate.|25-SEP-13
70128|Shell Hill Formation|70650|5|Briefly described|Map Legend|Devonian|Devonian|||Wana Karnu Group|||White to buff, poorly-sorted, lightly indurated quartz sandstone, pebbly sandstone, siltstone and conglomerate.|
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.|
70025|Shivering Conglomerate|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Matrix to clast-supported pebble to boulder conglomerate composed of rounded to angular clasts of grey laminated chert, siltstone, shale and quartzose sandstone, set in a medium-grained lithic-quartz sandstone matrix.||||||03-JUN-08
70025|Shivering Conglomerate|68592|2|Defined|p397-8, p726-7, p731 Fig.132, p746-52|Late Silurian|Middle Silurian|See also p326, p350, p363, p376. New name. Type locality given. Was included in Cobra Formation by Scheibner (1973) as a basal chert pebble conglomerate; Matthews (1985) regarded this as a tectonic breccia occurring where contact between Cobra Formation and underlying Ordovician sequence was a fault (also Valentine et al. 2006). Conglomerate marking base of Cobra Formation of Scheibner (1973) now defined as a separate unit, Shivering Conglomerate, and is composed of material derived from underlying rock. Thickness: ~25 - ~100 m. Contains Late Ludlow to Wenlock pentamerid brachiopods; rare silicified siltstone bands host brachiopod and coralline fossils. Min age: mid Wenlock to early Ludlow, as early Ludlow conodont fauna in marl of overlying Cobra Formation. Massive bedding and poor sorting suggest mass flow deposition.||Discontinuous basal unit in Mount Fairy Group.||Unconformably overlies Adaminaby and Bendoc Groups, Poidevins Sandstone and Rockley Volcanics; conformably overlain by Cobra Formation and De Drack Formation.|Pebble to boulder conglomerate; mainly meta-sandstone clasts (typically <60 mm, up to boulder size >256 mm) set in a medium- to coarse-grained, silicified, lithic-quartz sandstone matrix; poorly sorted, massive bedding; pebbly sandstone intervals.|
70025|Shivering Conglomerate|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sfi. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group||Is overlain by Cobra Formation. Unconformable at base.|Matrix-clast supported, pebble to boulder conglomerate and pebbly sandstone; clasts of laminated chert and lesser siltstone, shale, and rounded, medium grained quartzose sandstone set in a medium-coarse, silicified, lithic-quartz sandstone matrix.|
70025|Shivering Conglomerate|70543|5|Briefly described|Map Legend |Devonian|Silurian|||Mount Fairy Group|||Matrix-clast supported, pebble to boulder conglomerate and pebbly sandstone; clasts of laminated chert and lesser siltstone, shale, and rounded, medium grained quartzose sandstone set in a medium-coarse, silicified, lithic-quartz sandstone matrix.|
70025|Shivering Conglomerate|71069|6|Mentioned|p90, p138 fig 44|||Up to 20m thick. ||Mount Fairy Group||Overlain by the Cobra Formation.||
70025|Shivering Conglomerate|71656|5|Briefly described|p13 Fig.2, p28|Ludlow|Wenlock|The only fossiliferous site known from this unit is located on the Oberon 1:100,000 mapsheet, immediately north of the boundary with the Taralga 1:100,000 mapsheet.||Base of Mount Fairy Group||Overlain by Cobra Formation, De Drack Formation.|Heavily silicified, with poorly preserved macrofauna including a small rugose coral with long septa, resembling Palaeophyllum. Cross-sections of brachiopods observed in outcrop indicate the presence of pentamerides.|
22842|Shortland Formation|43017|5|Briefly described|Fig.1,p372|||||||||
22842|Shortland Formation|63832|5|Briefly described|p137|Late Permian|Late Permian|Shows stratigraphically highest evidence of Permian glaciation in eastern Australia, indicating westward retreat of glaciers.||Tomago Coal Measures||||14-DEC-17
22842|Shortland Formation|64631|6|Mentioned|p49.|Wuchiapingian|Wordian|Sydney Basin. Contains stratigraphically highest evidence of Permian glaciation of eastern Australia.||Unit in Tomago Coal Measures.||||
81962|Siding Spring Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic||||Includes the Belar Member and the Central Valley Breccia Member.||Scoria- or felsic clast-rich tuffs, volcaniclastic breccia, conglomerate, sandstone and mudstone.|02-NOV-20
70121|Silver City Suite|62728|5|Briefly described|p26|||Of Potosi Supersuite. Suite of gneisses outcropping in the Broken Hill Domain. Geological Province: Broken Hill Domain/Curnamona Province.||||||07-FEB-11
70121|Silver City Suite|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|||Includes Alma Gneiss|||15-DEC-21
70121|Silver City Suite|63866|5|Briefly described|p38, p41|||Named by Stevens (2006) to include the Alma Gneiss, Rasp Ridge Gneiss and three other newly identified magmatic units.|||Includes the Alma Gneiss, Rasp Ridge Gneiss, Georges Bore Granite, Stephens Creek Granite Gneiss and the Wondervale Well Granite Gneiss.|Intrudes the Thackaringa Group and/or the Broken Hill Group.||
70121|Silver City Suite|64097|2|Defined|p328 Appdx., p304 Fig. 1, p323|Paleoproterozoic|Paleoproterozoic|Formerly mapped in Thackaringa Gp - revised as separate suite comprising Alma, Georges Bore, Stephens Ck, Wondervale Well + Rasp Ridge Granite Gneisses -all intrude Thackaringa and/or Broken Hill Gps.Geochemically discussed as part of Potosi Supersuite||||||07-FEB-11
70121|Silver City Suite|64741|5|Briefly described|p301 Fig. 4, p302, p310|Paleoproterozoic|Paleoproterozoic|Includes Alma Gneiss, Georges Bore, Stephens Creek, Wondervale Well and Rasp Ridge Granite Gneisses. Geological province: Broken Hill Domain. Granite sills/metagranites. Peraluminous S-type.||||||07-FEB-11
70121|Silver City Suite|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Alma Gneiss, Georges Bore, Stephens Creek, Wondervale Well, Rasp Ridge and unnamed dolerite sills, dykes. Age range: 1704+/-3Ma to 1683+/-3Ma. Granite sills||||||07-FEB-11
70121|Silver City Suite|66302|5|Briefly described|p35, p36 Fig.9|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Formed by the melting of lower Willyama Supergroup or underlying rocks. |1705-1685 Ma||Includes the Rasp Ridge Gneiss, Georges Bore Granite, Oakdale Granite Gneiss and the Stephens Creek Granite Gneiss.|Intrudes the Thackaringa Group and Broken Hill Group.|S-type granites.|
70121|Silver City Suite|67581|6|Mentioned|p44 Fig.8, p45|||||Willyama Supergroup.||||
70121|Silver City Suite|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
70121|Silver City Suite|68126|5|Briefly described|p26, p29-30|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|c.1705-1685 Ma (Stevens et al. 2008).|||||
70121|Silver City Suite|69999|6|Mentioned|p4|||||||||
70121|Silver City Suite|70000|5|Briefly described|p31, p33-34, p36-37|Statherian|Statherian|Interpreted to have acted as a thermal driver for deposition of BIF and massive Pb-Zn-Ag sulfide mineralisation.|1695-1683 Ma.|Unit in Willyama Supergroup.|Includes Alma, Georges Bore, Stephens Creek, Wondervale Well and Rasp Ridge, Granite Gneisses.|Intrudes Broken Hill Group.|Granite sills.|
70121|Silver City Suite|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Alma, Georges Bore, Stephens Creek, Wondervale Well and Rasp Ridge Granite Gneisses.||Metagranitic rocks: quartz-feldspar-biotite gneiss (some megacrystic), +/- garnet, sillimanite; granitic to pegmatitic leucosome veins/patches.|17-SEP-15
70121|Silver City Suite|70657|4|Described|p12, p13 Fig.6, p15, p45|Statherian|Statherian|Stevens et al. (in prep). Curnamona Province: Broken Hill Domain.|1704 +/- 3 Ma -1683 +/- 3 Ma||Alma Gneiss, Georges Bore Granite Gneiss, Rasp Ridge Granite Gneiss, Wondervale Well Granite Gneiss, Stephens Creek Granite Gneiss.|Intrudes Broken Hill, Thackaringa Groups (Willyama Supergroup). Hores Gneiss is of similar age.|S-type felsic intrusive rocks; granite sills.|
70121|Silver City Suite|70658|5|Briefly described|p2, 15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Result of melting of lower part of rift in-fill.|~1705-1685 Ma.||Alma Gneiss.|Associated with Thackaringa and Broken Hill Groups.|Granite sills.|
70121|Silver City Suite|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
70121|Silver City Suite|73030|6|Mentioned|p2150|Statherian|Statherian||ca. 1700-1680|||||
70121|Silver City Suite|73243|6|Mentioned|p53 Fig.2||||||||Meta-granites.|
70121|Silver City Suite|73482|5|Briefly described|p422 Fig.3||||||Rasp Ridge Granite Gneiss, Wondervale Well Granite Gneiss, Stephens Creek Granite Gneiss, Georges Bore Granite Gneiss|||
70121|Silver City Suite|73512|5|Briefly described|p2-3|Statherian|Statherian|Curnamona Province, Broken Hill Block. Emplaced at ca 1700-1685 Ma.|ca 1704-1683 Ma||||Includes Potosi-type gneisses, and granitic rocks.|
70121|Silver City Suite|73524|5|Briefly described|p3|Statherian|Statherian|Proposed to have been emplaced during early rifting/basin opening.|1705-1685 Ma||Alma Gneiss, Rasp Ridge Gneiss|Intrudes lower Willyama Supergroup|Granitic sills, metamorphosed.|
70121|Silver City Suite|73575|5|Briefly described|p826, p828 Fig.2, p829 Fig.3|||||||Alma Granite Gneiss, Georges Bore Granite Gneiss, Stephens Creek Granite Gneiss, Wondervale Well Granite Gneiss, Rasp Ridge Granite Gneiss|Granite gneiss sills.|
79118|Silver King Metadolerites|69999|6|Mentioned|p20|Paleoproterozoic|Paleoproterozoic|||Unit in upper Broken Hill Group.||||
79118|Silver King Metadolerites|70000|5|Briefly described|p34, p36|Statherian|Statherian|||Unit in Purnamoota Subgroup.|||Basic gneiss from syn-depositional, high-Fe tholeiitic dykes and sills; locally very abundant.|
79118|Silver King Metadolerites|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Purnamoota Subgroup.|||Basic gneisses emplaced in uppermost Broken Hill Group, includes intervening metasedimentary rocks.|
79118|Silver King Metadolerites|73243|6|Mentioned|p52 Fig.1||||||||Sills.|
79118|Silver King Metadolerites|73308|6|Mentioned|p607 Fig.1|||||||||
29002|Silverspur Series|48940|6|Mentioned|Fig.14|||Refers Wade (1941)||||||
25478|Sinclair Conglomerate Member|22857|4|Described|p474 App.1 Tb.A1.6|Silurian|Silurian|Of the Captains Flat Formation (Hoskinstown Group). Lithic tuff and conglomerate in eastern area. Max. thickness: 130m. Geological Province: Captains Flat-Goulburn Trough. ||||||
25478|Sinclair Conglomerate Member|23048|5|Briefly described|fig5||Late Silurian|||||||
25478|Sinclair Conglomerate Member|31017|6|Mentioned|p47|||||||||
25478|Sinclair Conglomerate Member|31020|6|Mentioned|p12|||||||||
25478|Sinclair Conglomerate Member|32820|6|Mentioned|p3|||||||||
25478|Sinclair Conglomerate Member|36413|2|Defined|p68|Late Silurian|Late Silurian|||||||
25478|Sinclair Conglomerate Member|36414|5|Briefly described|map legend|Pridolian|Pridolian|Of Captains Flat Formation, Hoskinstown Group. Interbedded shale and reworked lithic tuff, minor conglomerate. GSNSW map code: Sfs.||||||
25478|Sinclair Conglomerate Member|40328|5|Briefly described|p181|||||||||
25478|Sinclair Conglomerate Member|42727|5|Briefly described|map legend|Pridoli|Pridoli|Of Captains Flat Formation. Lithic tuff and minor shale and conglomerate. BMR map symbol: Suf4. Geol. Prov: Captains Flat Block.||||||
25478|Sinclair Conglomerate Member|42820|2|Defined|p52|Late Silurian||Of Captains Flat Formation.||||||20-MAY-08
25478|Sinclair Conglomerate Member|48878|4|Described|p.10,Pl.3||Late Silurian|Upper Silurian. (I55-16). Pages, 7,15.||||||
25478|Sinclair Conglomerate Member|68592|6|Mentioned|p1160|||Possibly equivalent to Bullamalita Conglomerate.||Unit in Captains Flat Formation.||||
25478|Sinclair Conglomerate Member|69635|5|Briefly described|p32|||Shown as Sinlair Conglomerate and said to be high in Captains Flat Formation.||Of Captains Flat Formation||||
25478|Sinclair Conglomerate Member|71069|3|Fully described|p9, p10, p27, p28, p30, p38 fig 15|Pridoli|Ludlow|Named for the Sinclair Trigonometrical Station. Refined in this study to include rocks of the informal Newton beds. A type locality for this member has been proposed from GR 722033 6063086 to 722724 6063283. Estimated thickness ranging from 40m to 170m. Interpreted to be marine debris flow deposits. SHRIMP age derived from the dacite horizon. Possibly continues into the Lochkovian. Forms major ridges to the North of Captains Flat township. Distribution, geomorphology, primary structures/textures, tectonic structure and geophysical characterisitics discussed. Lithology discussed in detail. Age is SHRIMP U-Pb from Fraser et al. 2014. See also p39 fig 16, p100, p101 fig 31, p101, p102 fig 32, p105, p107, p111, p114, p117-p122.|419.6 +/- 2.6 Ma|Captains Flat Formation.||Paraconformably overlies the Kohinoor Volcanics. Overlain by the Carwoola Formation.  Interbedded with the Captains Flat Formation. Laterally equivalent to the Carwoola and Covan Creek Formations.|Pebble to boulder conglomerate, volcaniclastic sandstone, feldspathic arenite, coarse grained to pebbly litharenite and feldspathic litharenite that interfingers with a dacite horizon.|
25478|Sinclair Conglomerate Member|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Captains Flat Formation.|||Massive, cream to grey, thick-bedded lithartenite to feldspathic litharenite; lesser beds of cream to brown, poorly sorted, polymictic to monomictic, pebble to boulder conglomerate with clasts of sedimentary, volcanic and rare plutonic lithologies.|
81161|Singorimbah igneous intrusions|70718|5|Briefly described|p86-89, p95, p129|Neogene|Paleogene|No outcrop. Interpreted as Middle Cenozoic as TMI inversion modelling indicates it intrudes Murray Basin sediments. Aeromag. Character :Roughly circular 2-5 km wide anomalies with peak amplitude of approximately 100-600 nT. It is interpreted as a igneous intrusion with an intermediate to mafic volcanic susceptibility.||||Intrude the Eurolie granite and Leeton igneous complex.|Intermediate to mafic volcanic?|02-JUN-19
29005|Skains Hill Granodiorite|39409|6|Mentioned|Table XVII|||||||||
31453|Sloggets Suite|42726|5|Briefly described|map legend|Carboniferous|Carboniferous|38.||||||
31453|Sloggets Suite|44093|5|Briefly described|p207 App. 1|Late Carboniferous|Early Carboniferous|Geological Province: Lachlan Fold Belt.||||||29-MAR-05
75934|Sloping Rock Monzogranite|70661|3|Fully described|vii, viii, p6, p126 fig 10, p133, p134|Carboniferous|Carboniferous|Named for Sloping Rock Bluff. Originally called the Sloping Rock Adamellite. Distribution and metamorphism discussed. Type locality mentioned.||Oberon Supersuite||Intrudes Yalwal Volcanics|Leucocratic, aphyric and medium grained monzogranite containing aggregates of biotite. Miarolitic cavities are ubiquitous. Xenoliths of country rock, particularly of rhyolite are present throughout this unit.|16-FEB-18
75934|Sloping Rock Monzogranite|71303|5|Briefly described|map legend|Carboniferous|Late Devonian||||||Leucocratic aphyric and medium-grained feldspar-quartz-biotite monzogranite. Abundant miarolitic cavities. Xenoliths of country rock locally.|
82658|Smoky Cape Syenogranite|71628|4|Described|p17: 2, 9, 54, 67, 72-73, 77, 86, 99-103|||New name (this study). Previously published as Smokey Cape Adamellite, Smoky Cape Adamellite, Smokey Cape Leucoadamellite; also Smokey Cape Monzogranite (unpublished). Name derived from a local headland near South West Rocks. Comprises three epizonal bodies. Lithologies, mineralogy and geochemistry described in considerable detail. Unaffiliated. Has been quarried for dimension stone.|218.4 +/- 1.6 Ma (SHRIMP: Cross and Blevin, 2013).|Smoky Cape Suite.||Intrudes Kempsey beds.|White to pink, coarse-grained, equigranular biotite-hornblende syenogranite (three un-named phases described) with a fine-grained, porphyritic margin, and granophyric carapace. A-type.|
29213|Snowball Metabasic Igneous Complex|22857|4|Described|p452 App.1, Tb.A1.6|Silurian|Silurian|Basaltic lavas and tuffs, minor sediments. Basement of the Tumut Trough.||||||24-FEB-06
29213|Snowball Metabasic Igneous Complex|37529|5|Briefly described|p7|||||||||
29213|Snowball Metabasic Igneous Complex|42313|3|Fully described|p59||Middle Silurian|Age: early Middle Silurian||||||
29213|Snowball Metabasic Igneous Complex|42314|5|Briefly described|Map|Early Silurian|Middle Silurian|||||||
29213|Snowball Metabasic Igneous Complex|44093|5|Briefly described|p183 App. 1|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
29213|Snowball Metabasic Igneous Complex|67847|5|Briefly described|p56|Early Silurian|Early Silurian|Hosts the Snowball mine.||||||
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.|
80313|Soldiers Quarry Member|72528|6|Mentioned|p125.|||Example in 'calibrations and data processing' appendix.||||||
23979|Solitary Hill Granite|22638|3|Fully described|p74||Late Devonian|New name.||||||
23979|Solitary Hill Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
23979|Solitary Hill Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
23979|Solitary Hill Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.||||||
23979|Solitary Hill Granite|72084|6|Mentioned|p55 Fig.57|||A-type geochemical discrimination diagrams.||||||
70456|Sooley Volcanic Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of De Drack Formation (Mount Fairy Group). Grey, massive, crystal-poor, rhyolitic volcanic sst. interbedded with fine- to v. coarse-gr.rhyolitic volcaniclastic sst, siltst.+ mudstone; grey to pale green fine- to medium-gr. feldspar-phyric qtz.andesite.||||||
70456|Sooley Volcanic Member|68592|2|Defined|p760-1, p778-86, p790-1, p794, p1672|Pridoli|Ludlow|See also p269, p726, p728, p730 Fig.132. New name. Previously mapped as undifferentiated Upper Silurian by Brunker and Offenberg (1970). Low undulating topography. Type and representative sections described. Distinguished by volcanic composition and its limited geographic extent. Total thickness: estimated maximum is 800 m. Shallow marine depositional environment. Lower greenschist facies metamorphism. Conodont fauna provide an age range of Ludlow-Pridoli and therefore a maximum age for volcanic rocks at this site.||Unit in De Drack Formation.||Conformably overlies Kingsdale Limestone Member; is overlain by and interfingers with Joppa Siltstone Member; is intruded by Bishopthorpe Dolerite and Forest Lodge Quartz Monzodiorite.|Rhyolitic volcaniclastic rocks; fine-grained, matrix-rich volcanic sandstones, porphyritic quartz andesite, and rhyolitic to dacitic lava facies with a more limited extent.|
70456|Sooley Volcanic Member|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sfds. Includes 3 unnamed units of: feldpar-phyric, quartz andesite; rhyolite to dacite; rhyolitic, volcanic/volcaniclastic sandstone, siltstone and minor grey mudstone. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||De Drack Formation|Includes three unnamed units.|Is overlain by, and interfingers with, Joppa Siltstone Member. Overlies Kingdale Limestone Member.|Massive-crystal poor, rhyolitic volcanic sandstone interbedded with fine to very coarse-grained rhyolitic volcaniclastic sandstone, siltstone and mudstone, fine-medium grained, feldspar phyric, quartz andesite and porphyritic rhyolite and dacite.|
70456|Sooley Volcanic Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||De Drack Formation|||Massive-crystal poor, rhyolitic volcanic sandstone interbedded with fine to very coarse-grained rhyolitic volcaniclastic sandstone, siltstone and mudstone, fine-medium grained, feldspar phyric, quartz andesite and porphyritic rhyolite and dacite.|
70456|Sooley Volcanic Member|71069|6|Mentioned|p26, p29, p35, p125, p127|||Northern Goulburn Basin. Less than 1000m thick. Deposited in a shallow marine environment that deepened before deposition of the overlying unit.  See also p137 fig 44, p140 tbl 4, p144, p146, p147, p151, p154.||De Drack Formation||Partly equivalent to the Kohinoor Volcanics. Equivalent to the Woodlawn Volcanics.||
70456|Sooley Volcanic Member|71656|5|Briefly described|p13 Fig.2, p29|Pridoli|Ludlow|Conodont from an allochthonous limestone block surrounded by Sooley Volcanic Member rocks yielded a single specimen most likely referrable to the distinctive conodont Belodella anomalis, ranging from the mid-Ludlovian up to the Pridolian.||upper De Drack Formation.|||Surrounds allochthonous limestone.|
70456|Sooley Volcanic Member|71700|5|Briefly described|p14|||||De Drack Formation||||
30524|Sorronto Granite|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Batholith.||||||
30524|Sorronto Granite|23170|3|Fully described|p221|Early Devonian|Early Devonian|of Yeoval Batholith.||||||
82512|South Brother Microgranite|71628|5|Briefly described|p17: 2, 78, 86-87|||New name (this study), after South Brother Mountain, ~17 km SW of Laurieton. Crops out over ~6 km2. Geochemistry described.||The Brothers Suite.||Intrudes Beechwood beds and Camden Haven Group.|(Perthitic alkali-feldspar)-porphyritic, riebeckite microgranite. Characterised by marked secondary alteration. A-type.|
34757|South Casino Gravel|22892|6|Mentioned|table9 p69|Quaternary|Quaternary|||||||
29012|Southern Limestone|41863|6|Mentioned|p19|||||||||
23982|Spa Creek Siltstone|42567|4|Described|p136|||Reserved J.Nott Aug 1990.||||||
23982|Spa Creek Siltstone|62740|4|Described|p366-367|Oligocene|Oligocene|Of Nadgigomar Sub-Group (Koringaroo Group). Overlies Old Timberlight Conglomerate. Thickness: 60m. Well-sorted, organic-rich, purple-brown silts and localised patches of sand: very well laminated silts, rarely horizontal.||||||15-JAN-08
22872|Specimen Hill Gabbroic Diorite|22638|3|Fully described|p30||Early Silurian|Wallundry Suite. New name.||||||
22872|Specimen Hill Gabbroic Diorite|44192|5|Briefly described|Map Legend||Llandoverian|||||||
22872|Specimen Hill Gabbroic Diorite|44936|5|Briefly described|Map Legend||Silurian|||||||
22872|Specimen Hill Gabbroic Diorite|65890|6|Mentioned|p158 Fig.4|||Highly magnetic mafic stock, to the south of the Middledale Gabbroic Diorite.||||||13-APR-11
23984|Speldon Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Gloucester Coal Measures. Well-bedded pebbly sandstone, bioturbated mudstone, pebble conglomerate, coarse lithic sandstone. Max. thickness: 80m. Geological Province: Sydney Basin.||||||
23984|Speldon Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Gloucester Coal Measures.    Geological Province: New England Fold Belt||||||
23984|Speldon Formation|40872|6|Mentioned|Fig.2|||||||||
23984|Speldon Formation|40883|6|Mentioned|p9|||||||||
23984|Speldon Formation|41054|6|Mentioned|p152|||See also Fig.2||||||
23984|Speldon Formation|43017|5|Briefly described|Fig.1,p372|||||||||
23984|Speldon Formation|44244|2|Defined|p179, p168 Tb. 2|Late Permian|Late Permian|Of the Gloucester Coal Measures, dividing the lower Avon Subgroup from the upper Craven Subgroup.  Max. thickness: 76.8m.  Type section in text.  Geological Province: Myall Block.||||||26-AUG-04
23984|Speldon Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Geological Province: Western Myall Block.||||||
32268|Spicers Creek Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb27.||||||
32268|Spicers Creek Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
81950|Spire Trachyte Member|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Mount Naman Formation|||Flow-foliated, porphyritic, fine-grained, aegerine-augite trachyte forming blocky outcrop, well developed columnar jointing.|02-NOV-20
26906|Spring Road Granite|42726|5|Briefly described|map legend|Middle Devonian||260. Wyangala Batholith.||||||
26906|Spring Road Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Foliated biotite and tonalitic granite, minor porphyritic microgranite, quartz diorite and biotite granodiorite.||||||13-MAY-04
26906|Spring Road Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Whick Whack Suite. Cream to grey, medium- to coarse-grained, foliated to protomylonitic, equigranular to weakly porphyritic biotite granite. Low K, Th and U radioelement response.||||||
26906|Spring Road Granite|68592|2|Defined|p1482, p1508-11, p1518-22|Early Devonian|Early Devonian|Part of this pluton was named the Spring Road Adamellite by Gibson (1973) and Yacopetti (1987). Chappell et al. (1991) first used the name Spring Road Granite and assigned this unit to their Spring Road Suite. All these workers included parts of the unit in Blackmans Creek Granite. Blevin (2011) included it in his Whick Whack Suite. Type locality described. Poorly exposed; occupies lower topographic areas. Has strongly developed, partly protomylonitic, foliation dipping to W. Geochemistry and geophysical properties described. Alluvial gold has been obtained within the outcrop area, but its origin is uncertain. Road construction material has been locally extracted.||Unit in Whick Whack Suite.||Intrudes Adaminaby Group. Is intruded by Blackmans Creek Granite. Abuts Bigga and Blanket Flat Granites.|Cream to grey, medium- to coarse-grained, foliated to protomylonitic, equigranular to occasionally porphyritic, hornblende-biotite granite and leucogranite. A-type.|
26906|Spring Road Granite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dws. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Whick Whack Suite|||Medium-coarse grained, foliated-protomylonitic, equigranular-porphyritic, hornblende biotite granite and leucogranite; low-medium K and Th, low U response and low magnetic susceptibility.|
26906|Spring Road Granite|70297|5|Briefly described|map legend|||||Keverstone Supersuite|||Medium- to coarse-grained, foliated to protomylonitic, equigranular to pophyritic, hornblende-biotite granite and leucogranite.|
26906|Spring Road Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Whick Whack Suite|||Medium-coarse grained, foliated-protomylonitic, equigranular-porphyritic, hornblende biotite granite and leucogranite; low-medium K and Th, low U response and low magnetic susceptibility.|
26906|Spring Road Granite|71206|6|Mentioned|p373, 384|||Lachlan Fold Belt. Geochemistry graphs.||Spring Road Suite.|||Aluminous A-type granite.|
31634|Spring Road Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
31634|Spring Road Suite|68592|6|Mentioned|p1508|||Chappell et al. (1991); consisted of Spring Road Granite which was later assigned to the Whick Whack Suite (Blevin, 2011).||||||
31634|Spring Road Suite|71206|6|Mentioned|p373|||Lachlan Fold Belt.|||Spring Road Granite.||Aluminous A-type granite.|
77252|Springfield Seam|43194|5|Briefly described|p133 App. 1|Late Permian|Late Permian|Informal name? Within Trinkey Formation (Nea Subgroup, Black Jack Group)||||||
77252|Springfield Seam|68004|5|Briefly described|p153.|Late Permian|Late Permian|Southern Mullaley Sub-basin, Gunnedah Basin. Thickness to 2.5 m; interbanded stony coal and tuff units make this a very high ash coal with limited to no development potential.||Unit in Black Jack Group.|||Interbanded stony coal and tuff.|
77044|Springponds Tonalite|68592|2|Defined|p1610-1, p1613, p1642-5|Early Devonian|Early Devonian|New name, after Springponds property: a composite of the original Springponds Granodiorite and Wylora Quartz Gabbro as described by Carr et al. (1979), based on similarity in composition, texture and geophysical response. Type locality described. Geochemistry and geophysical properties described. It is the most mafic of the Arthursleigh Suite plutons in the Goulburn 1:250 000 map area. Carr et al. (1980) obtained an age for the former Wylora Quartz Gabbro of 395 +/- 8 Ma. Is in contact with Marulan Granite (in the N) and Lumley Granite (in the S).|406 +/- 7 Ma (K-Ar biotite; Carr et al., 1980).|Unit in Arthursleigh Suite.||Intrudes Barrallier Ignimbrite.|Variable composition. Greenish-grey, medium-grained, equigranular to weakly porphyritic tonalite and quartz diorite. The weakly porphyritic rocks are finer grained and contain micrographic quartz and orthoclase. I-type.|
77044|Springponds Tonalite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Das. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Arthursleigh Suite|||Greenish grey, medium-grained, massive, equigranular to weakly porphyritic tonalite and quartz diorite. Low radioelement response and high magnetic susceptibility.|
77044|Springponds Tonalite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Arthursleigh Suite|||Greenish grey, medium-grained, massive, equigranular to weakly porphyritic tonalite and quartz diorite. Low radioelement response and high magnetic susceptibility.|
79857|Sprys Tank Granite|72083|5|Briefly described|p20|Silurian|Silurian|Formerly the Mine granite (Trigg (2016). Similar to the Rosemorder Granite.|428.1 +/- 2.8 Ma (Bodorkos et al., 2013).|||||
33859|Square Head Formation|22508|4|Described|p5||Lochkovian|In the Lachlan Fold Belt. Previously Square Head beds. Late Lochkovian.||||||26-MAR-08
33859|Square Head Formation|22768|6|Mentioned|p172|||||||||
33859|Square Head Formation|22857|5|Briefly described|p172, p448 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Cobar Supergroup. Pebbly arenite, lithic arenite, conglomerate and cobble conglomerate. Contains brachiopods. Correlates with Boothumble Formation. Geological Province: Darling Basin. ||||||
33859|Square Head Formation|61964|3|Fully described|p14 Fig. 4, p97-98|Lochkovian|Pridoli|Supersedes "Square Head beds". Of Bootheragandra Group. Comprises several conglomeratic and quartz sandstone unnamed units: Max. thickness: >1200m.||||||03-NOV-15
33859|Square Head Formation|62405|5|Briefly described|Map legend|Early Devonian|Late Silurian|Of the Bootheragandra Group. Undifferentiated quartz sandstone, pebble to cobble conglomerate (quartzite clasts dominant) and slate.||||||
33859|Square Head Formation|69162|5|Briefly described|Map legend|Silurian|Silurian|Six facies are mapped as separate but un-named sub-units.||Unit in Bootheragandra Group.|||Undifferentiated quartz sandstone, pebble to cobble conglomerate (quartzite clasts dominant) and slate.|
33859|Square Head Formation|69163|5|Briefly described|Map legend|Silurian|Silurian|Four facies are mapped as separate but un-named sub-units.||Unit in Bootheragandra Group.||Is faulted against Rankin Formation.|Undifferentiated quartz sandstone, pebble to cobble conglomerate (quartzite clasts dominant) and slate.|
33859|Square Head Formation|69164|5|Briefly described|Map legend|Silurian|Silurian|Five facies are mapped as separate but un-named sub-units.||Unit in Bootheragandra Group.||Is faulted against Clements Formation (Wagga Group) and Walters Range Group.|Undifferentiated quartz sandstone, pebble to cobble conglomerate (quartzite clasts dominant) and slate.|
33859|Square Head Formation|71889|4|Described|p7, p46-p48, p67|||Exposed on the flanks of Square Nob from the Barellan Road, in the middle of the Beness Syncline and on a sweeping curve on the Colinroobie Road. [An unconformable contact with the Barrat Formation is mentioned although the relative position of the two units is not elucidated]. Thin sections were described by K. Bull.|||||Foliated tuffaceous mudstone with quartz crystal fragments and possible lithic grains. Very fine-grained sandstone and siltstone with abundant lithic grains of claystone siltstone and very fine-grained arenite.|
33859|Square Head Formation|72083|4|Described|p7, p27-37, p40 Fig.6|Early Devonian|Late Silurian|At least 800m thick. Forms Beness Hill with ridges, cliffs and terraces: a syncline of this Formation is interpreted to extend to Square Nob. Other scattered outcrops mentioned. Unfossiliferous. Well-illustrated: maps, outcrop photographs, photomicrograph. Age range from regional correlation with other units of the Supergroup. Deformed in Early Devonian: ?Bindian Orogeny; discussed.||Cobar Supergroup.||Unconformably overlies Wagga Group.|Basal crowded matrix- to clast-supported, mainly sub-angular metasandstone/quartzite clasts conglomerate; flaggy-bedded, medium- to coarse-grained lithic quartz sandstone; and an upper coarse-cobble, clast-supported conglomerate unit.|
41072|Standbye Monzogranite|24366|6|Mentioned|p7|||||||||
41072|Standbye Monzogranite|68005|5|Briefly described|p67, p134.|Permian|Permian|Listed on p.134 as a unit in Moonbi Supersuite.||Unit in Southern Moonbi Supersuite.|||Coarsely porphyritic hornblende-biotite monzogranite with inequigranular groundmass.|
73988|Stanthorpe Supersuite|63748|5|Briefly described|p36-37|Early Triassic|Permian|Includes Stanthorpe and Bungulla Suites.||||||07-FEB-11
73988|Stanthorpe Supersuite|65455|6|Mentioned|p7|||New England Fold Belt. Has high U.||||||09-MAY-12
73988|Stanthorpe Supersuite|68111|5|Briefly described|p968 Tb.1|||Consistently mis-spelt as Stanthrope in Table 1. Also includes Dandahra Creek Leucogranite.|||Includes Mackenzie, Mount Mitchell, Sandy Flat, Undercliffe Falls, and Bungulla Monzogranites; Stanthorpe Granite; Nonnington, Mount Jonblee, Bolivia Range, and Billyrimba Leucomonzogranites;|||
73988|Stanthorpe Supersuite|68679|5|Briefly described|p454, p456-466|||Northern New England Batholith. Comprises a northern and southern part separated by Uralla and Hillgrove Supersuite granitoids. Geochemistry described. Associated with disseminated Au at Timbarra.|||Bungulla, Clare Hills, Herries, Sailor Jack, Stanthorpe, Ballandean, Mingimarny, Bullaganang, Mount You You, Suites.|||
73988|Stanthorpe Supersuite|69639|5|Briefly described|p1-p2, p9, p16, p20-p21, p26|Lopingian|Lopingian|New England Orogen. See also p50, p80, p157, p163, p175, p181-p182, p187, p218-p219, p221-p222.|||Includes the Stanthorpe Suite, Mount Mitchell Monzogranite, Bungulla Suite and the Bolivia Range Suite.|||
73988|Stanthorpe Supersuite|70217|5|Briefly described|v, vi, p60, p66, p74 tbl 14.1, p75, p76|Early Triassic|Late Permian|New England Orogen. Granites of this supersuite are I-type, felsic, fractionated and variably mineralised. Also includes the Billyrimba Leucomonzogranite, Ruby Creek Granite, Cullendore Granite, Stanthorpe Granite, Rivertree Granite, Bookookoorara Monzogranite, MacKenzie Monzogranite, Sandy Flat Monzogranite, Mount Mitchell Monzogranite, Mount Jonblee Leucomonzogranite and the Clive Monzogranite.  |255-238 Ma||Includes the Bolivia Range Suite, Morgans Creek Monzogranite.|||
73988|Stanthorpe Supersuite|70876|4|Described|p2, p58|Early Triassic|Early Triassic|New England Orogen. Donchak et al (2013) incorporated into this supersuite the Herries, Bullaganang, Ballandean and Mount You You supersuites despite their varied ages; the authors therefore suggest revisiting the defintion of this supersuite.|c. 248-245 Ma||Includes the Herries Suite.|||
73988|Stanthorpe Supersuite|71628|5|Briefly described|p5: 3, 6-7, 11; p7: 1-2; p9-1; p11: 1-3|Middle Triassic|Late Permian|See also p11: 5, 11, 25, 40; p12: 3, 9; p14: 2, 32; p15: 1-116; p16: 1-3, 10, 26; p18-10; p19: 37, 91, 131, 138, 144, 175. Redefined to exclude granites of the Cullendore Supersuite, and the Bungulla Type of Blevin and Chappell (1996). Previously included Bungulla Suite. The Supersuite is subdivided into several spatio-temporal groups (detailed). Geochemistry summarised; contrasted with Jibbinbar Leucosyenogranite.|256-241 Ma.||Stanthorpe Complex; Bolivia Range, Clive, Glen Eden, Surface Hill Suites.||Pale pink, mainly medium- to coarse-grained monzogranite-leucomonzogranite, in some cases transitional to syenogranite-leucosyenogranite. I-type.|
73988|Stanthorpe Supersuite|72528|5|Briefly described|p71, p109.|Triassic|Permian||c.254 to c.237 Ma||Includes Deepwater Syenogranite.|||
73988|Stanthorpe Supersuite|73570|6|Mentioned|p918|Middle Triassic|Middle Triassic|New England Orogen.||||||
31637|Stanton Rock Suite|22815|6|Mentioned|p81|||||||||
31637|Stanton Rock Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31637|Stanton Rock Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
25699|State Mine Creek Formation|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wallerawang Subgroup (Illawarra Coal Measures). Contains the Moolarben coal seam. Claystone, mudstone, siltstone; thin coal. Max. thickness: 30m. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
25699|State Mine Creek Formation|38614|6|Mentioned|Fig.6|||||||||
25699|State Mine Creek Formation|39232|4|Described|p110|||||||||
25699|State Mine Creek Formation|40332|6|Mentioned|Fig.4|||||||||
25699|State Mine Creek Formation|40806|2|Defined|p157|Permian|Permian|Prob. Permian||||||
25699|State Mine Creek Formation|42657|5|Briefly described|p82|||||||||
25699|State Mine Creek Formation|68004|5|Briefly described|p60 Table 6, p61.|Late Permian|Late Permian|Western Coalfield. From 5 to 10 m thick at the west, gradually thickening eastwards. ||Unit in Charbon Subgroup.|Includes Moolarben and Turill Coal Members, and the "Lennox seam" or the "Goulburn seam" at the top.|Overlies Moolarben Coal Member. Is overlain by Middle River Coal Member or by Gap Sandstone.|Claystone, mudstone, siltstone, minor sandstone and coal seams; common worm burrows and plant remains.|
70114|Stephens Creek Granite Gneiss|63866|5|Briefly described|p38|Statherian|Statherian||1689 +/- 5 Ma (lower) and 1686 +/- 4 Ma (upper)|Silver City Suite||Intrudes the Thackaringa Group and/or the Broken Hill Group.||
70114|Stephens Creek Granite Gneiss|64097|2|Defined|p329 Appdx., p305 Fig. 2, p316|Paleoproterozoic|Paleoproterozoic|Age: 1689 +/- 5 Ma (lower part), 1686 +/- 4 Ma (upper part). Overlain by Allendale Metsediments or Parnell Formation. This granite gneiss body is zoned - 3 granite type rocks(details incl.)||||||07-FEB-11
70114|Stephens Creek Granite Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Ages: 1686+/-4Ma, 1689+/-5Ma. Geological province: Broken Hill Domain. Written as Stephens Creek only.||||||07-FEB-11
70114|Stephens Creek Granite Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1686+/-4Ma, 1689+/-5Ma. Geological province: Broken Hill Domain. Name presented only as Stephens Creek.||||||07-FEB-11
70114|Stephens Creek Granite Gneiss|66302|6|Mentioned|p41|Statherian|Statherian||1689 +/-5 to 1686 +/- 4 Ma |Silver City Suite||||
70114|Stephens Creek Granite Gneiss|68126|6|Mentioned|p30||||1689+/-5 Ma; 1686+/-4 Ma (Stevens et al. 2008).|||||
70114|Stephens Creek Granite Gneiss|69999|6|Mentioned|p17|||Thackaringa Group lithologies occur within this unit.||||||
70114|Stephens Creek Granite Gneiss|70000|6|Mentioned|p34|Statherian|Statherian|||Unit in Silver City Suite.||||
70114|Stephens Creek Granite Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Silver City Suite.||Is overlain by Wondervale Well Granite Gneiss.|Quartz-feldspar-biotite +/- sillimanite gneiss. K-feldspar megacrysts abundant in the middle parts, decreasing to few megacrysts in the upper parts.|17-SEP-15
70114|Stephens Creek Granite Gneiss|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province: Broken Hill Domain. |1689 +/- 5 Ma; 1686 +/- 4 Ma.|Silver City Suite||Intrudes Allendale Metasediments (Broken Hill Group). ?Overlies Wondervale Well Granite Gneiss.|Intrusive S-type felsic rocks, metamorphosed to gneiss.|
70114|Stephens Creek Granite Gneiss|72461|6|Mentioned|p16 fig 9||||1689 +/- 5 Ma, 1686 +/- 4 Ma|||||
70114|Stephens Creek Granite Gneiss|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian||1689 +/- 5 Ma, 1686 +/- 4 Ma|||||
70114|Stephens Creek Granite Gneiss|73308|6|Mentioned|p607 Fig.1, 610, 612||||1689 +/- 5 Ma.|||||
70114|Stephens Creek Granite Gneiss|73482|5|Briefly described|p422 Fig.3|Statherian|Statherian||1689+/-5 Ma, 1686+/-4 Ma|Silver City Suite||||
70114|Stephens Creek Granite Gneiss|73575|5|Briefly described|p828 Fig.2|Statherian|Statherian||1689+/-5 Ma||Silver City Suite|||
24505|Stockinbingal Formation|22638|3|Fully described|p65|||Thought equivalent to the Bethungra Formation. 1000 m thick. Unconformably overlies the Frampton Volcanics.||||||
24505|Stockinbingal Formation|22685|5|Briefly described|p728,Fig1p729|Early Devonian|Early Devonian|Dacite, rhyolite, siltstone and sandstone.||||||17-JAN-06
24505|Stockinbingal Formation|22857|4|Described|p450 App.1, Tb.A1.6|Early Devonian|Early Devonian|Dacitic to rhyolitic tuffs. Max. thickness: 1000m. Geological Province: Bogan Gate Terrace.||||||14-JAN-10
24505|Stockinbingal Formation|35608|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
24505|Stockinbingal Formation|35609|2|Defined|p78|Early Devonian|Early Devonian|||||||
24505|Stockinbingal Formation|39626|6|Mentioned|p276|||||||||
24505|Stockinbingal Formation|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
24505|Stockinbingal Formation|44192|5|Briefly described|Map Legend||Lochkovian|||||||
32522|Stockinbingal and Bethungra Formations|44192|6|Mentioned|Map Legend|Early Devonian|Early Devonian|||||||
32522|Stockinbingal and Bethungra Formations|44936|5|Briefly described|Map Legend||Early Devonian|||||||
39829|Stockrington Tuff Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Adamstown Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
39829|Stockrington Tuff Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Tickhole Formation. ||||
22896|Stone Boat Hill Granite|22638|4|Described|p75||Late Devonian|Previously "Katunga Granite".||||||
22896|Stone Boat Hill Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
27235|Stones Tank Tuff Member|22857|5|Briefly described|p436 App.1, Tb.A1.6|Pragian|Lochkovian|Of the lower Amphitheatre Group (Cobar Supergroup). ||||||
27235|Stones Tank Tuff Member|23171|5|Briefly described|p51|||Said to be intercalated with the lower Amphitheatre Formation [probably meant Group], and in faulted contact with Burthong Formation at the Stones Tank prospect. Brief discussion of mainly gold and silver mineralisation associated with steep, easterly dipping shear zone (Stones Tank shear) on the western margin of the volcanics.||||||27-MAY-20
27235|Stones Tank Tuff Member|23173|6|Mentioned|Map Legend|||||||||
27235|Stones Tank Tuff Member|35287|5|Briefly described|p6, p4 Fig. 2, p10|Early Devonian|Early Devonian|New name. Of Mouramba Formation|||||Felsic tuffs and minor rhyolitic lavas.|26-MAY-20
27235|Stones Tank Tuff Member|39618|2|Defined|p97|Early Devonian|Early Devonian|Named after Stones Tank. Representative suite of volcanics can be seen west of GR240640. max thickness  of 900m estimated. Actual thickness may be much less.|||||Laminated + welded rhyodacitic crystal and crystal-vitric tuff + minor flow-banded, pyritic, vughy, porphyritic rhyolite.Interbedded turffaceous arenite + siltstone.|27-MAY-20
27235|Stones Tank Tuff Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
27235|Stones Tank Tuff Member|41528|6|Mentioned|p50|||||||||
27235|Stones Tank Tuff Member|72958|5|Briefly described|p5, p7, p37-42, p60|Lochkovian|Ludlow|Lachlan Orogen. Age from rhyolite DD13ST104. Interpreted to have been erupted on the seafloor in a deep-water environment (Felton, 1981). Stratigraphic relationships remain unclear. Previously (1981) considered to be within the Mouramba Group, with interfingering relationship. Previously thought to be undatable due to secondary alteration of these rocks.|421.7 +/- 2.1 Ma SHRIMP U-Pb|Amphitheatre Group, 'lower', Amphitheatre Group||Equivalent to Peak Rhyolite, Nurri Group. In faulted contact with Burthong Formation.|Laminated and welded rhyodacitic crystal-vitric tuff, flow banded porphyritic rhyolite.|
82634|Strathaven Monzogranite|71628|5|Briefly described|p12: 1-2, 17-19|||New name (this study), after Blevin (pers. comm., 2014) informally assigned the name Strathaven Complex to the unit identified as Po on the Grafton-Maclean 1:250 000 Metallogenic Sheet (Henley et al., 2001). The mis-spelled Strathhaven Complex is reserved in the ASUD. Named after a local homestead. Occurs as three small bodies with poor outcrop, 20 km W of Tenterfield. Geochemistry described||Strathaven Suite.||Intrudes Texas beds. Appears to be bounded locally by Wandsworth Volcanic Group.|Pale grey to pale pinkish-grey, fine-grained, moderately porphyritic hornblende-biotite monzogranite to ?granodiorite. I-type.|
31295|Strathgled Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Fine to coarse cherty tuff, rhyolitic tuff.||||||
22906|Streamville Granodiorite|22679|4|Described|p 45|||||||||
22906|Streamville Granodiorite|23214|3|Fully described|p161|Silurian|Silurian|Intrudes the Adaminaby Group.  Biotite-hornblende granodiorite with and even grain size of 1-2mm. Reduced I-type granitoid. Geological Province: Wyangala Batholith.||||||15-JUL-08
22906|Streamville Granodiorite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of hornblende biotite granodorite, felsic granodiorite, fine grained granite.||||||15-JUL-08
22906|Streamville Granodiorite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Hornblende biotite granodiorite, felsic granodiorite, fine grained granite.||||||17-JUL-08
22906|Streamville Granodiorite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of Wyangala Batholith.||||||12-JUN-08
22906|Streamville Granodiorite|50231|5|Briefly described|Map Legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
22906|Streamville Granodiorite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Hornblende-biotite granodiorite, felsic granodiorite and fine grained granite.||||||
22906|Streamville Granodiorite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Gunning Suite. Grey, medium-grained, partly foliated, equigranular hornblende-biotite granodiorite.||||||12-JUN-08
22906|Streamville Granodiorite|68592|2|Defined|p1312-3, p1316-20, p1276, p1346-9|Early Silurian|Early Silurian|Originally the Streamville Granite of Close (1978), after Streamville Creek; subsequently Streamville Granodiorite (Chappell et al., 1991). Forms hilly terrain around Lake Wyangala. Type area described. Geochemistry detailed; geophysical properties described. Not isotopically dated.||Unit in Gunning Suite.||Intrudes Adaminaby Group. Is intruded by Bigga Granite.|Mainly grey, medium-grained, partly foliated, equigranular, hornblende-biotite granodiorite with a small biotite granite core; mafic enclaves and other hornfelsic sedimentary inclusions are characteristic of the margins of the body. I-type.|
22906|Streamville Granodiorite|69539|6|Mentioned|p608 Fig.2|||||||||
22906|Streamville Granodiorite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sgs. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Gunning Suite|||Medium grained, partly foliated, equigranular, hornblende-biotite granodiorite with biotite granite core; low magnetic susceptibility.|
22906|Streamville Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
22906|Streamville Granodiorite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Gunning Suite|||Medium grained, partly foliated, equigranular, hornblende-biotite granodiorite with biotite granite core; low magnetic susceptibility.|
22906|Streamville Granodiorite|70545|5|Briefly described|Map Legend |Silurian|Silurian|||Gunning Suite|||Medium-coarse grained, partly foliated, equigranular, hornblende-biotite granodiorite with biotite granite core; low magnetic susceptibility.|
22909|Stringy Road Granodiorite|22815|4|Described|p85|||||||||
22909|Stringy Road Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Xmas Suite.||||||
82661|Stroud Mountain Microgranite|71628|5|Briefly described|p19: 156-157|||New name, after work by Sutherland and Graham (2003). Named after the topographic feature of the same name. Located 4 km NE of Stroud. Comprises one large (7 x 1 km) and several smaller bodies.||Stroud Mountain Suite.||Intrudes Booral and McInnes Formations.|Pink to grey, porphyritic microgranite.|
33413|Stump Hole Granite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Medium to coarse grained biotite granite.||||||05-JUL-04
27576|Sturts Meadows Siltstone|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (East).  Parent - Farnell Group.  Age - Ediacarian in text.||||||17-SEP-15
27576|Sturts Meadows Siltstone|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
27576|Sturts Meadows Siltstone|22857|4|Described|Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Of the Farnell Group. Finely laminated siltstone. Age: ~580Ma. Max. thickness: 200m. Geological Province: Adelaide Fold Belt. See also p400 App. 1 Tb.A1.3.||||||
27576|Sturts Meadows Siltstone|30261|4|Described|Table 1|||Marinoan age||||||
27576|Sturts Meadows Siltstone|34812|3|Fully described|p102|||||||||
27576|Sturts Meadows Siltstone|34814|6|Mentioned|p281|||||||||
27576|Sturts Meadows Siltstone|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27576|Sturts Meadows Siltstone|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
27576|Sturts Meadows Siltstone|36960|6|Mentioned|p191|||||||||
27576|Sturts Meadows Siltstone|39214|5|Briefly described|p9|||||||||
27576|Sturts Meadows Siltstone|41301|5|Briefly described|p92|||See also Fig.1||||||
27576|Sturts Meadows Siltstone|41429|5|Briefly described|p246|||||||||
27576|Sturts Meadows Siltstone|41801|6|Mentioned|Fig.4|||||||||
27576|Sturts Meadows Siltstone|46889|6|Mentioned|p272|||||||||
27576|Sturts Meadows Siltstone|66623|5|Briefly described|p13, p18. |||||||Overlies Mantappa Dolomite. Is overlain by Picnic Creek Basalt.|Monotonous sequence of finely laminated, medium to dark green-grey siltstone; thin discontinuous buff-coloured sandy-limestone beds to 0.8 m in upper sequence.|
27576|Sturts Meadows Siltstone|68241|5|Briefly described|p21, p24 Fig.3, p33 Fig.3|||> 3270m thick.||||Intertongued with the Mount Arrowsmith Volcanics.||
27576|Sturts Meadows Siltstone|70000|6|Mentioned|p34, p40|Neoproterozoic|Neoproterozoic|||Unit in Farnell Group.||||
27576|Sturts Meadows Siltstone|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Farnell Group.||Overlies Mantappa Dolomite. Is overlain by Faraway Hills Quartzite.|Homogeneous, finely laminated, green-grey siltstone; discontinuous buff-coloured sandy limestone beds to 0.8m in upper sequence.|
35164|Styles Bed|23055|6|Mentioned|Fig13p25|||marker tuff within Upper Pilot coal seam.||||||
26152|Sugarloaf Creek Formation|22768|6|Mentioned|p178||Pragian|||||||
26152|Sugarloaf Creek Formation|22857|4|Described|p178, p462 App.1 Tb.A1.6|Pragian|Lochkovian|Max. thickness: 1.2km. Geological Province: Canberra-Yass Shelf. See also p464 App.1 Tb.A1.6.||||||
26152|Sugarloaf Creek Formation|24005|5|Briefly described|p292 Fig.1|Early Devonian|Early Devonian|Of Black Range Group. Geological Province: Lachlan Fold Belt||||||
26152|Sugarloaf Creek Formation|36441|5|Briefly described|map legend|Pragian|Lochkovian|Lithic arenite, siltstone and shale. Underlies Cavan Limestone; overlies Kirawin Formation. BMR map code: Dls.||||||
26152|Sugarloaf Creek Formation|40124|6|Mentioned|Fig.1|||||||||
26152|Sugarloaf Creek Formation|42497|5|Briefly described|Map Legend|Pragian|Pragian|||||||
26152|Sugarloaf Creek Formation|42577|5|Briefly described|p25|||||||||
26152|Sugarloaf Creek Formation|45147|2|Defined|M306|early Pragian|late Lochkovian|Late Lochkovian to Early Pragian||||||
26152|Sugarloaf Creek Formation|50230|4|Described|Map legend|Pragian|Pragian|Of the Black Range Group.  Overlies Kirawin Formation; overlain by Fifeshire Shale and Cavan Bluff Limestone.||||||
26152|Sugarloaf Creek Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Black Range Group. Tuffaceous sandstone, shale, siltstone and minor conglomerate.||||||17-JUN-08
26152|Sugarloaf Creek Formation|64992|5|Briefly described|p60 Fig. 1|Devonian|Devonian|Part of the Taemas-Wee Jasper succession. Volcanics||||||26-MAR-09
26152|Sugarloaf Creek Formation|66197|5|Briefly described|p631 Fig.3b|||Canberra-Yass Basin. Shallow marine/subaerial clastics. Underlies the Murrumbidgee Group, overlies the Mountain Creek Volcanics.||||||14-MAR-12
26152|Sugarloaf Creek Formation|68592|2|Defined|p926-30, p936, p975-9, p989|Pragian|Pragian|Originally Sugarloaf Creek Tuff (Edgell, 1949); formalised by Joplin et al. (1953). Widely used (with Tuff or Tuffs as the lithological component) since, despite Browne (1959) including these rocks in her broadly-encompassing Mountain Creek Tuffs (superseded). The current name, Sugarloaf Creek Formation, avoids incorrect genetic implications and has also been widely used since its introduction by Pedder et al. (1970). The upper contact is here redefined with the fornal recognition of the Fifeshire Shale (basal Murrumbidgee Group). Named after Sugarloaf Creek. Type section, and representative section for the distinctive eastern outcrops, are described. From 740m to c.1000m thick. The top of this unit marks a major change from volcanic and volcaniclastic deposition (Black Range Group) to mainly carbonate deposition (Murrumbidgee Group). Geophysical properties described. Only one fossil (a fish plate) found. Inferred age from sparse biostratigraphic relationships.||Unit in Black Range Group.||Conformably and gradationally overlies Kirawin Formation. Is overlain gradationally by Fifeshire Shale or Cavan Bluff Limestone (Murrumbidgee Group).|Off-white, grey and red, fine- to very coarse-grained (locally pebbly), poorly sorted, massive or parallel laminated, volcaniclastic sandstone interbedded with lesser shale and tuffaceous mudstone.|
26152|Sugarloaf Creek Formation|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dbs. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Black Range Group||Overlies Kirawin Formation. Is overlain by Fifeshire Shale and Cavan Bluff Limestone (of Murrumbidgee Group).|Fine-very coarse grained (locally pebbly), poorly sorted, massive or parrallel laminated, volcanic sandstone interbedded with subordinate amounts of shale and tuffaceous mudstone.|24-JAN-23
26152|Sugarloaf Creek Formation|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Fine-very coarse grained(locally pebbly), poorly sorted, massive or parrallel laminated, volcanic sandstone interbedded with subordinate amounts of shale and tuffaceous mudstone.|
26152|Sugarloaf Creek Formation|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Fine to very coarse grained, poorly sorted, massive or parallel laminated, volcanic sandstone interbedded with subordinate amounts of shale and tuffaceous mudstone.|
26152|Sugarloaf Creek Formation|71656|6|Mentioned|p12 Fig.2, p31-32|Pragian|Pragian|The only fossil definitely known from this unit is an undescribed fish plate assigned to the placoderm Groenlandaspis? collected from material excavated during roadworks near the entrance to ""Fifeshire"" property on the lakeside road from Good Hope.",,||Black Range Group||Overlies Kirawin Formation and underlies Fifeshire Shale, Murrumbidgee Group.||
26152|Sugarloaf Creek Formation|73215|5|Briefly described|p994|||Talmo-Taemas area.||||Overlies Mountain Creek Volcanics. Is overlain by Cavan Bluff Limestone.||
29029|Sulcor Limestone Member|721|5|Briefly described|Map legend|Frasnian|Givetian|Of the Yarrimie Formation (Tamworth Group).  Oliststromal limestone lenses.||||||
29029|Sulcor Limestone Member|22857|5|Briefly described|p482 App.1 Tb.A1.6|Givetian|Givetian|Of the Yarrimie Formation (Tamworth Group). Contains sponges, corals, conodonts. Max. thickness: 120m. Geological Province: Tamworth Forearc Basin. ||||||
29029|Sulcor Limestone Member|30650|6|Mentioned|p315|||||||||
29029|Sulcor Limestone Member|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
29029|Sulcor Limestone Member|31999|6|Mentioned|Table 1|||||||||
29029|Sulcor Limestone Member|32619|6|Mentioned|p460|||Fauna||||||
29029|Sulcor Limestone Member|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
29029|Sulcor Limestone Member|34403|6|Mentioned|p149|||||||||
29029|Sulcor Limestone Member|34554|6|Mentioned|p234|||Faunas||||||
29029|Sulcor Limestone Member|34692|5|Briefly described|p188|||||||||
29029|Sulcor Limestone Member|38802|4|Described|p115|||||||||
29029|Sulcor Limestone Member|43091|5|Briefly described|Map legend|||of Tamworth Group||||||
29029|Sulcor Limestone Member|43428|14|Not recorded|p138|||List of fauna||||||
29029|Sulcor Limestone Member|43431|14|Not recorded|p1264|||Northeastern N.S.W.||||||
29029|Sulcor Limestone Member|61765|4|Described|p58 Fig. 1, p59 Fig. 3, p60-61|Emsian|Emsian|Of Silvergully Formation. Max thickness: >475m. Geological Province: Tamworth Belt. See p60-61 for more detailed information.||||||07-FEB-11
29029|Sulcor Limestone Member|65940|6|Mentioned|p204,206-207|Emsian|Emsian|Near Tamworth, NSW. Also referred to as Sulcor Limestone on p204, 206. Contains Phillipsastrea maculosa (serotinus Zone, type locality, Mawson and Talent, 2000), Favosites aff. F. salebrosus (Pohler, 2002), P. tumulosus (Yanet, 1965), P. rariporosus (Dubatolov, 1963).||||||
29029|Sulcor Limestone Member|66720|5|Briefly described|Map legend|Late Devonian|Early Devonian|||Unit in Yarrimie Formation.|||Massive biohermal coralline limestone, crinoidal, minor calcareous sedimentary rocks.|
29029|Sulcor Limestone Member|68006|6|Mentioned|p114.|Early Devonian|Early Devonian|||Unit in Tamworth Group.||||
29029|Sulcor Limestone Member|71628|6|Mentioned|p7: 19|||||||Is intruded by Inlet Monzogranite.||
73708|Sundew Basalt|63286|5|Briefly described|p295, p298, p304|Llandovery|Llandovery|Coarsely phorphyritic basaltic trachyandesite intrusions, also have lower clinopyroxene and higher plagioclase phenocrysts abundances. Age ~439 Ma.||||||04-NOV-14
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||
25502|Sunny Ridge beds|35118|6|Mentioned|p436|||||||||
31636|Sunnyside Suite|42726|5|Briefly described|map legend||Silurian|||||||
29827|Sunset Hills Granite|22503|6|Mentioned|Fig.7 p650|||||||||
29827|Sunset Hills Granite|22679|4|Described|p48|||||||||
29827|Sunset Hills Granite|22798|5|Briefly described|p850,851 Table.1|Early Devonian|Late Silurian|Age: K/Ar 378.8 +/-8.5Ma.||||||
29827|Sunset Hills Granite|23214|3|Fully described|p172|Silurian|Silurian|Formerly named Neville Granite. Also previously shown as part of the Barry Granodiorite. Intrudes the Adaminaby Group, Coombing Formation and Kangaloolah Volcanics. Geological Province: Wyangala Batholith.||||||
29827|Sunset Hills Granite|23335|5|Briefly described|p14, p15 Tb. 1|||||||||27-OCT-04
29827|Sunset Hills Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Biotite granodiorite, hornblende biotite granodiorite, biotite granite, leucogranite.||||||17-JUL-08
29827|Sunset Hills Granite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|||||||
29827|Sunset Hills Granite|63286|6|Mentioned|p300|Early Silurian|Early Silurian|Age: 430+/-4Ma (U-Pb SHRIMP: Lennox et al. 2005).||||||07-FEB-11
29827|Sunset Hills Granite|63290|6|Mentioned|p403|Early Silurian|Early Silurian|Age: ca 430Ma (U/Pb . Lennox et al. 2005).||||||
29827|Sunset Hills Granite|69539|5|Briefly described|p608 Fig.1, p614-615|Silurian|Silurian|Dating by K-Ar, 40Ar/39Ar and Rb-Sr on hornblende and biotite consistently produce ages of 379-363 Ma; reflects resetting due to Tabberabberan event.|430.1 +/- 3.7 Ma (U-Pb zircon).|||||
29827|Sunset Hills Granite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
29827|Sunset Hills Granite|73431|5|Briefly described|p365-366, p367 Tb.1, p368, p372, p374|Silurian|Silurian|Lachlan Orogen. S-type granite with abundant zircon xenocrysts. Coeval with Davies Creek Granite, part of Browns Creek Igneous Complex. Previous ages include 363+/-2 Ma Rb/Sr biotite, 378.8+/-8.5 Ma K/Ar biotite and 371+/-4 Ma Ar/Ar biotite from Lennox et al., (1998), Ar/Ar biotite ages may be a post-magmatic thermal event. Appears as Sunset Hill Granite p373 Fig.8, Sunset Hills Gr. p363 Fig.1. Location in text includes p363 Fig.1.|430.1+/-3.7 Ma zircon U/Pb SHRIMP, 363+/-2 Ma|||Intrudes Adaminaby Group|Granite.|
82656|Surface Hill Leucomonzogranite|71628|3|Fully described|p11: 3, 25-26, 34; p15: 3, 32, 36, 40|Early Triassic|Early Triassic|See also p15: 57, 61-62, 66, 80, 92-95, 105-114. New name to reflect better the primary lithology. Historically regarded as part of Stanthorpe Monzogranite. Probably named after a local hill or the locality of that name. Occurs ~30 km E of Tenterfield as a c.24 x 10 km unit. Its shape suggests limited unroofing. Numerous age determinations given. Geochemistry is described in great detail; is assigned geochemically to the Stanthorpe Supersuite. Hosts many Au deposits (named) and minor Mo, Bi and As mineralisation. DESCRIPTION (continued): Miarolitic cavities. Detailed descriptions by various workers.|249.7 - 247.8 Ma (Mustard, 2001).|Stanthorpe Complex.|Dinner Creek, Plateau, Microgranite Phases; Nelson Creek Leucomonzogranite Phase.|Intrudes Sandy Creek Monzogranite. Is faulted against Mount Lindesay Monzogranite and Dundee Rhyodacite.|Medium- to coarse-grained biotite leucomonzogranite-leucosyenogranite, strongly porphyritic biotite microgranite, very fine-grained microgranite; locally aplitic and pegmatitic. Locally fine- or very fine-grained. I-type. See COMMENTS for more.|
82657|Surface Hill Suite|71628|5|Briefly described|p15: 2, 4, 35-36, 47-48, 61, 93, 107|Middle Triassic|Early Triassic|Of Stanthorpe Supersuite. Basket Swamp Leucomonzogranite Phase (of Branch Swamp Monzogranite) is geochemically assigned to this Suite.||Stanthorpe Complex.|Branch Swamp, Surface Hill Leucomonzogranite, [?]Sandy Creek Monzogranites.|||
29032|Sutchers Creek Formation|22451|6|Mentioned|p24|||||||||
29032|Sutchers Creek Formation|22529|6|Mentioned|4 fig 2|Emsian|Emsian|Parent Queens Pinch Group. Underlying unit Ingleburn Formation.||||||28-AUG-08
29032|Sutchers Creek Formation|22590|6|Mentioned|Fig3 P754||Emsian|Actually spelt Sutchers Ck Formation.||||||28-AUG-08
29032|Sutchers Creek Formation|22857|4|Described|p476 App.1 Tb.A1.6|Emsian|Emsian|Of the Queens Pinch Group. Arenite, mudstone, limestone; corals, brachiopods, conodonts. Max. thickness: 180m. Geological Province: Capertee Rise. ||||||
29032|Sutchers Creek Formation|23043|5|Briefly described|Map Legend|Emsian|Emsian|Of Queens Pinch Group.||||||28-AUG-08
29032|Sutchers Creek Formation|23170|2|Defined|p149|Emsian||Of Queens Pinch Group.||||||28-AUG-08
29032|Sutchers Creek Formation|23522|5|Briefly described|p252|Devonian|Devonian|||||||
29032|Sutchers Creek Formation|24611|6|Mentioned|p196|Emsian|Emsian|||||||
29032|Sutchers Creek Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
29032|Sutchers Creek Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
29032|Sutchers Creek Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian.||||||28-AUG-08
29032|Sutchers Creek Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
29032|Sutchers Creek Formation|33326|6|Mentioned|p431|||Fauna.||||||
29032|Sutchers Creek Formation|33732|5|Briefly described|p118|||||||||
29032|Sutchers Creek Formation|33948|6|Mentioned|p82|||||||||
29032|Sutchers Creek Formation|35491|6|Mentioned|p135|||||||||
29032|Sutchers Creek Formation|41000|6|Mentioned|p279|||||||||
29032|Sutchers Creek Formation|42033|6|Mentioned|p654|||||||||
29032|Sutchers Creek Formation|42051|6|Mentioned|p143|||||||||
29032|Sutchers Creek Formation|43188|4|Described|p216,Table 4 p212||Early Devonian|Early Devonian (early Emsian) age.||||||
29032|Sutchers Creek Formation|43461|14|Not recorded|Table p621||Eifelian|||||||
29032|Sutchers Creek Formation|43476|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
29032|Sutchers Creek Formation|43519|14|Not recorded|Tb p119,120||Eifelian|||||||
29032|Sutchers Creek Formation|43530|14|Not recorded|p1028,1034||Emsian|U.Emsian||||||
29032|Sutchers Creek Formation|43541|14|Not recorded|p263,271|||To be definded formally in later publ.Youngest Dev.beds in Queens Pinch area,12 miles SE of Mudgee||||||
29032|Sutchers Creek Formation|44093|5|Briefly described|p197 App. 1|Early Devonian|Early Devonian|Of the Queens Pinch Group. Geological Province: Lachlan Fold Belt.||||||29-MAR-05
29032|Sutchers Creek Formation|48926|6|Mentioned|p29|||P29 et seq.||||||
29032|Sutchers Creek Formation|64296|5|Briefly described|p84, p85, p91|||In Queens Pinch belt. Has a 'serotinus' conodont fauna.||||||28-AUG-08
29032|Sutchers Creek Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Mudgee. Appears just as Sutchers Creek. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
29032|Sutchers Creek Formation|68003|5|Briefly described|p24 Fig.3-e. |Emsian|Pragian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Queens Pinch Group.||||
29032|Sutchers Creek Formation|71924|6|Mentioned|p1, 3|||Queens Pinch, near Mudgee. Has fauna different to Cunningham Formation. But fauna similar to Jesse Limestone. Brachiopod fauna similar to Ingleburn Formation.||||Correlated with Ingleburn Formation.||
29032|Sutchers Creek Formation|73299|6|Mentioned|p1096 Fig.3, p1097 Fig.4|Early Devonian|Early Devonian|||Queens Pinch Group||||
26154|Sutton Granodiorite|24128|5|Briefly described|p3|||Geological Province: Lachlan Fold Belt.||||||
26154|Sutton Granodiorite|42727|5|Briefly described|map legend|Early Devonian|Pridoli|Granodiorite, adamellite and porphyry, I-type. Intrudes Pittman Formation with associated spotted and porphyroblastic hornfels (contact metamorphism).  BMR map symbol: Sgs. Geol. Prov: Cullarin Block.||||||
26154|Sutton Granodiorite|42820|2|Defined|p66|Late Silurian||age of 410 +/- 4 Ma||||||
31639|Sutton Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
31639|Sutton Suite|44093|5|Briefly described|p203 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
29672|Swallow Creek Porphyry|13139|5|Briefly described|p3 Fig. 2|||Geological Province: Lachlan Orogen.||||||
29672|Swallow Creek Porphyry|23214|2|Defined|p86|Late Ordovician|Ordovician|Formerly Swallow Keratophyre. Intrudes the Weemalla Formation and the Fairbridge Volcanics.||||||
29672|Swallow Creek Porphyry|23334|5|Briefly described|3 Fig.2|||||||||
29672|Swallow Creek Porphyry|43640|5|Briefly described|Map Legend||Ordovician|||||||
29672|Swallow Creek Porphyry|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Consists of hornblende andesite.||||||17-JUL-08
29672|Swallow Creek Porphyry|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Hornblende andesite.||||||17-JUL-08
29672|Swallow Creek Porphyry|43782|6|Mentioned|Map Legend|Eastonian|Eastonian|||||||
29672|Swallow Creek Porphyry|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
82663|Swan Brook Granite|71628|5|Briefly described|p19: 157-158|||New name, after a local watercourse. Occurs as a cluster of small outcrops at the location of Swanbrook, ~13 km ENE of Inverell. Limited (two analyses) detailed.||Swan Brook Suite.||Intrudes Texas beds.|Felsic intrusive.|
31527|Swan Ponds Suite|42726|5|Briefly described|map legend||Silurian|||||||
29594|Swan Ponds Tonalite|22679|4|Described|p 46|||||||||
29594|Swan Ponds Tonalite|23214|2|Defined|p160|Late Silurian|Late Silurian|I-type tonalite. Intrudes the Cabonne, Cudal and Adminaby Groups.  Intruded by the Lucan Complex, Garland Granodiorite and the Wyangala Granite. Geological Province: Wyangala Batholith||||||
29594|Swan Ponds Tonalite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of xenolith -rich porphyritic hornblende tonalite.||||||17-JUL-08
29594|Swan Ponds Tonalite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Xenolith-rich porphyritic hornblende tonalite.||||||17-JUL-08
29594|Swan Ponds Tonalite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyangala Batholith.||||||17-JUL-08
29594|Swan Ponds Tonalite|68592|5|Briefly described|p1305|Late Silurian|Late Silurian|In the Bathurst 1:250 000 map sheet area.||||Is intruded by Wyangala Granite.||
29594|Swan Ponds Tonalite|70297|5|Briefly described|map legend|Silurian|Silurian|||Grants Corner Supersuite||||
37332|Swastika Siltstone|61964|3|Fully described|p14 Fig. 4, p134-135, p115|Frasnian|Frasnian|Tentatively assigned to Cocoparra Group. Poorly outcropping, highly weathered /eroded. Weathered, ferruginous red-orange brown laminated siltstone+ minor fine-grained lithic quartz sandstone; contains distinctive plant fossils.Palaeontology - p260||||||
37332|Swastika Siltstone|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Red-brown laminated siltstone and minor quartz sandstone, rare plant fossils.||||||
37332|Swastika Siltstone|69164|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|||Red-brown laminated siltstone and minor quartz sandstone, rare plant fossils.|
26920|Swatchfield Monzonite|42712|4|Described|Table 1 p14|Ordovician|Ordovician|Intrudes Rockley Volcanics||||||
26920|Swatchfield Monzonite|63278|5|Briefly described|p156|Early Silurian|Late Ordovician|Intrudes the Rockely Volcanics. Age: 437+/-8Ma (U/Pb zircon).||||||07-FEB-11
26920|Swatchfield Monzonite|63289|6|Mentioned|p371|Llandovery|Bolindian|Age: 439+/-8Ma (Zircon U-Pb: Meffre 2003). Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
26920|Swatchfield Monzonite|63290|6|Mentioned|p392 Tb. 1|||In the Rockley Volcanics. Age: 437+/-8Ma (laser ablation ICPMS, Meffre 2003). Geological Province: Rockley-Gulgong Volcanic Belt.||||||
26920|Swatchfield Monzonite|63293|6|Mentioned|p471, p474, p476|||Intrudes Rockley Volcanics. Age: 437+/-8Ma (Meffre 2003).||||||07-FEB-11
26920|Swatchfield Monzonite|64963|5|Briefly described|p182 Fig. 2|||Age: 437+/-8Ma (U-Pb zircon, Percival and Glen 2007)||||||
26920|Swatchfield Monzonite|67106|6|Mentioned|p681|||South of Oberon, southern Rockley-Gulgong Volcanic Belt.|437 +/- 8 Ma (zircon: Meffre, 2003).|||||
26920|Swatchfield Monzonite|67847|4|Described|p4, p26 fig 4.2, p28, p29, p31-p32|Llandovery|Bolindian|Name derived from the Swatchfield property. At least 437 +/- 8 Ma (La-ICPMS U-Pb zircon) although this age is interpreted by Glen et al., 2007b to be several million years too young; however Meffre 2003 and Meffre et al., 2007 give a similar age. ||||Intrudes the Rockley Volcanics and Triangle Formation.|Monzodiorite dominated by plagioclase, clinopyroxene, hornblende and minor alkali feldspar and quartz.|
26920|Swatchfield Monzonite|68592|5|Briefly described|p376, p397|Early Silurian|Early Silurian|In Bathurst 1:250 000 map sheet area. ICP-MS U-Pb zircon age.|437 +/- 8 Ma: Crawford et al. (2007).|||Intrudes Rockley Volcanics.||
26920|Swatchfield Monzonite|69541|6|Mentioned|p648|Early Silurian|Late Ordovician|A sample for dating contained 2 Cretaceous grains out of 20: mentioned to demonstrate zircon crystallisation in older rocks from younger hydrothermal or magmatic fluids.||||||
75961|Table Top Diorite|71628|5|Briefly described|p2: 59-61; p3-36|||A provisional name, awaiting change from further studies, after unpublished Hensel (1982). Named after the local Table Top Homestead. Small outcrops occur ~27 km SSE of Armidale and ~7 km ESE of Enmore. Geochemistry described.||Bakers Creek Supersuite.||Intrudes Girrakool beds. Is adjacent to, and within, Enmore Monzogranite; their relationship is 'unconstrained'.|Microdiorite.|
72990|Tacking Point Gabbro|62058|5|Briefly described|map sheet|Late Permian|Late Permian||||||Gabbro, pyroxenite, diorite, pegmatite.|
72990|Tacking Point Gabbro|63763|3|Fully described|p4-5 Fig. 1, p14|Late Triassic|Early Permian|Intruded by Karikeree Metadolerite. Coarse-grained, ranging from near-black (melanocratic gabbro) to pale grey (leucocratic gabbro); contains schlieren of pyroxenite, coarse pegmatitic segregations and uncommon narrow aplite dykes. See also p7 Fig. 2.||||||
72990|Tacking Point Gabbro|73440|6|Mentioned|p127, p145-146|Middle Devonian|Middle Devonian||390 Ma|||||
28268|Talaterang Group|22591|5|Briefly described|p 58|||Sydney Basin||||||
28268|Talaterang Group|22857|4|Described|p504 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Massive to thickly bedded fluvioglacial conglomerate; locally possible tillite, siltstone. Geological Province: Kanimblan Highlands.||||||
28268|Talaterang Group|22969|4|Described|p 17, Fig 2.2||Early Permian|Sydney Basin Province.||||||
28268|Talaterang Group|23544|5|Briefly described|Fig 2 p358|||In the Sydney Basin||||||
28268|Talaterang Group|24079|5|Briefly described|p433 Fig. 6|Late Carboniferous|Late Carboniferous|Geological Province: Sydney Basin.||||||
28268|Talaterang Group|24552|5|Briefly described|p9|Sakmarian|Sakmarian|Disconformably overlain by Shoalhaven Group. Geological Province: Southern Sydney Basin.||||||07-FEB-11
28268|Talaterang Group|29752|3|Fully described|p16|||||||||
28268|Talaterang Group|31081|2|Defined|p51|Paleozoic|Paleozoic|||||||07-NOV-08
28268|Talaterang Group|31128|5|Briefly described|p5|||Also mention on P3.||||||
28268|Talaterang Group|36042|6|Mentioned|Table 1|||||||||
28268|Talaterang Group|36594|6|Mentioned|Table 1|||||||||
28268|Talaterang Group|37924|4|Described|p488|||||||||
28268|Talaterang Group|39287|6|Mentioned|Fig. 2.2|||||||||
28268|Talaterang Group|39289|6|Mentioned|Fig. 4.1|||||||||
28268|Talaterang Group|39290|3|Fully described|p83|||Palaeogeography P85||||||
28268|Talaterang Group|39293|6|Mentioned|p137|||||||||
28268|Talaterang Group|39308|6|Mentioned|p519|||||||||
28268|Talaterang Group|42974|6|Mentioned|p191|||||||||
28268|Talaterang Group|43194|5|Briefly described|p128, p129 Tb. 8.3|Early Permian|Late Carboniferous|Southern Sydney Basin. Non-marine fluvio-glacial conglomerates.||||||
28268|Talaterang Group|45097|6|Mentioned|p28|||Terrestrial valley-fill sediments. Late Carb.||||||
28268|Talaterang Group|60281|1|Redefined|p55|Early Permian|Early Permian|Redefined to comprise the Clyde Coal Measures, Pigeon House Creek Siltstone and Wasp Head Formation. Overlain by the Shoalhaven Group.  Geological Province: Sydney Basin.||||||11-APR-08
28268|Talaterang Group|60285|4|Described|p181|Sakmarian|Sakmarian|Deposited during intial phase of basin development. Geological Province: Sydney Basin.||||||
28268|Talaterang Group|61610|6|Mentioned|p252 Fig. 2|Permian|Permian|Geological Province: Sydney Basin.||||||07-FEB-11
28268|Talaterang Group|62043|6|Mentioned|p438 Fig.2. |Sakmarian|Sakmarian|Southern Sydney Basin.|||Includes Clyde Coal Measures and Wasp Head Formation.|Is overlain by Shoalhaven Group.||
28268|Talaterang Group|63773|5|Briefly described|p1058 Fig. 2, p1069|Early Permian|Early Permian|Includes Clyde Cola Measures and Wasp Head Formation. Geological Province: Sydney Basin.||||||07-APR-09
28268|Talaterang Group|64877|6|Mentioned|p295-296|Permian|Permian||||Wasp Head Formation, Clyde Coal Measures.|||
28268|Talaterang Group|65114|5|Briefly described|p383 Tb.1, p395|Early Permian||Listed as Early Permian; 292 Ma; Tectonic unit: Southern and western Sydney Basin; deposited in north-trending extensional basins||||||
28268|Talaterang Group|66577|5|Briefly described|p995, p997 Fig.2.|Early Permian|Early Permian|Basal sediments in southern Sydney Basin, consisting of fluvial sedimentary rocks, interpreted to have been deposited in N-S rift-related grabens.|||Includes Clyde Coal Measures and Wasp Head Formation.|Overlain by Shoalhaven Group.||
28268|Talaterang Group|67663|6|Mentioned|p518, p520 Tb.1|Late Carboniferous|Late Carboniferous|Southern Sydney Basin.||||Unconformably overlain by Clyde Coal Measures and Wasp Head Formation.|Thick fluvioglacial conglomerates, diamictites and varves.|
28268|Talaterang Group|68003|5|Briefly described|p40.|Early Permian|Early Permian|Southern Sydney Basin.|||Includes Clyde Coal Measures, Pigeon House Creek Siltstone and Wasp Head Formation.|||
28268|Talaterang Group|68592|5|Briefly described|p1779, p1785-6|Permian|Permian||||Includes Clyde Coal Measures and Wasp Head Formation.|Is overlain disconformably by Tallong Conglomerate (Shoalhaven Group).||
28268|Talaterang Group|69297|6|Mentioned|p501|Artinskian|Artinskian|Sydney Basin. |||Includes the Clyde Coal Measures and the Wasp Head Formation.|||
28268|Talaterang Group|70661|6|Mentioned|p137|||||||||
28268|Talaterang Group|71542|5|Briefly described|p25|Permian|Permian|Of southern Sydney Basin.||||Overlain by Shoalhaven Group/Pebbley Beach Formation.||20-OCT-21
28268|Talaterang Group|73421|5|Briefly described|p3, p5|Sakmarian|Asselian|Sydney Basin, southern. Marine sediments.|||Wasp Head Formation|Underlies Shoalhaven Group|Includes sandstone with pebble layers and cross bedding, conglomerate and siltstone.|
28268|Talaterang Group|73494|5|Briefly described|p541|Permian|Permian|Southern Sydney Basin. Early Permian.|||Wasp Head Formation.|Is overlain by Conjola Subgroup (Shoalhaven Group).|Southern Sydney Basin. Fluvio-glacial deposits.|
28268|Talaterang Group|73582|6|Mentioned|p122|Permian|Late Carboniferous|Herbert (1980); see also Tye et al. (1996). SW edge of the Sydney Basin.|||||Fluvioglacial drainage.|
26159|Talgarry Sand Member|30996|2|Defined|p48|late Holocene|late Holocene|See also P50,51. Time eq. of Coonambidgal Fm.||||||
26159|Talgarry Sand Member|42966|6|Mentioned|p239|||of Lake Victoria Sand||||||
29039|Talingaboolba Formation|9548|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Lithic-quartz sandstone and siltstone.||||||
29039|Talingaboolba Formation|22768|6|Mentioned|p170-71|||||||||
29039|Talingaboolba Formation|22831|3|Fully described|p 40|Lochkovian|Pridolian|Kopyje Group||||||
29039|Talingaboolba Formation|22857|4|Described|p170-171, p446 App.1, Tb.A1.6|Lochkovian|Lochkovian|Previously combined with Mineral Hill Volcanics in the "Ootha Group" (McClatchie, 1971). Possibly equivalent to the Condobolin Formation. Max. thickness: >1km. Geological Province: Darling Basin. ||||||
29039|Talingaboolba Formation|23309|6|Mentioned|p390|||||||||
29039|Talingaboolba Formation|23522|5|Briefly described|p253|Devonian|Devonian|||||||
29039|Talingaboolba Formation|24477|6|Mentioned|p20|||sandstone, grits.||||||
29039|Talingaboolba Formation|29987|4|Described|p19|||||||||
29039|Talingaboolba Formation|30769|6|Mentioned|p34|||||||||
29039|Talingaboolba Formation|32087|4|Described|p11|||||||||
29039|Talingaboolba Formation|32674|6|Mentioned|p31|||||||||
29039|Talingaboolba Formation|33004|6|Mentioned|p173|||||||||
29039|Talingaboolba Formation|35287|5|Briefly described|p14|||See also Fig.4.||||||
29039|Talingaboolba Formation|36066|5|Briefly described|p4|||||||||
29039|Talingaboolba Formation|37727|6|Mentioned|p86|||||||||
29039|Talingaboolba Formation|39214|6|Mentioned|Table 11|||||||||
29039|Talingaboolba Formation|40328|6|Mentioned|p36|||See also P42||||||
29039|Talingaboolba Formation|40365|6|Mentioned|p240|||See also P295||||||
29039|Talingaboolba Formation|42144|5|Briefly described|p604|||||||||
29039|Talingaboolba Formation|42449|6|Mentioned|p13|||||||||
29039|Talingaboolba Formation|42521|5|Briefly described|p15, Fig 3 p16|||||||||
29039|Talingaboolba Formation|42566|6|Mentioned|Fig.3 P6|||||||||
29039|Talingaboolba Formation|43089|5|Briefly described|Map Legend|||||||||
29039|Talingaboolba Formation|43263|6|Mentioned|Map Legend||Early Devonian|||||||
29039|Talingaboolba Formation|43441|5|Briefly described|25|Early Devonian|Late Silurian|||||||08-JAN-10
29039|Talingaboolba Formation|44093|5|Briefly described|p173 Aoo. 1|Early Devonian|Late Silurian|In the Mineral Hill Zone. Geological Province: Lachlan Fold Belt.||||||
29039|Talingaboolba Formation|44160|5|Briefly described|Map Legend||Lochkovian|||||||
29039|Talingaboolba Formation|65469|6|Mentioned|p103, p115|||Lachlan Orogen.||||||
29039|Talingaboolba Formation|67416|5|Briefly described|p84 Fig.1, p86-89, p90-91|Early Devonian|Early Devonian||~418 Ma.|||Overlies Mineral Hill Volcanics (unconformably) or faulted against. Is overlain paraconformably by Yarra Yarra Creek Group.|Conglomerate, coarse sandstone, sandstone, siltstone. Extensively leached to kaolinite. Not mineralised.|
29039|Talingaboolba Formation|70751|6|Mentioned|p12, p17, p21|Pridoli|Pridoli|||||||
29039|Talingaboolba Formation|71039|6|Mentioned|p12|||||||Overlies the Mineral Hill Volcanics.||
29039|Talingaboolba Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Kopyje Group.|||Mass flow lithic conglomerate, lithic and quartz-lithic sandstone, vitric-rich volcanic mudstone and siltstone, aphyric dacite; minor limestone.|
29039|Talingaboolba Formation|72083|5|Briefly described|p36|Early Devonian|Early Devonian|Fossils indicate a stratigraphic break in the Lochkovian, consistent with the age of the Bindian Orogeny.||Cobar Supergroup.||Is overlain by Yarra Yarra Group probably unconformably.||
29039|Talingaboolba Formation|72958|6|Mentioned|p11|Lochkovian|Pridoli|Cobar Basin. Nymagee area.||Cobar Supergroup||Partly underlain by Mount Susannah Conglomerate. Partly underlain by and equivalent to Mineral Hill Volcanics. Equivalent to Majuba Volcanics.||
24511|Tallaganda Granodiorite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
24511|Tallaganda Granodiorite|40276|2|Defined|p14|Early Devonian|Early Devonian|||||||
24511|Tallaganda Granodiorite|69159|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Thurralilly Suite.|||Grey to cream, coarse-grained, massive to protomylonitic, equigranular to sparsely porphyritic, muscovite-biotite-K-feldspar-plagioclase-quartz granite to granodiorite.|
24511|Tallaganda Granodiorite|71069|4|Described|p21 fig 7, p28, p39 fig 16, p175|Ludlow|Wenlock|Named for the Tallaganda State Forest.  Previously grouped as part of the Boro Granite. Intrudes the Ordovician basement of the Goulburn Basin. Distribution, geomorphology, geochemistry, tectonic structure, metamorphism and geophysical characteristics discussed. See also p177, p179, p189, p193-p195.||Thurralilly Suite||Equvialent to the Lockhart Igneous Complex, Gibraltar Granite, Butmaroo Granite, Gourock Granodiorite and the Ellenden Granite.|Grey to cream, medium to coarse-grained, massive to strongly foliated, equigranular, hornblende granodiorite; biotite granodiorite with abundant metasedimentary xenoliths.|
24511|Tallaganda Granodiorite|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Thurralilly Suite.|||Grey to cream, medium- to coarse-grained, often strongly foliated, equigranular to sparsely porphyritic, hornblende granodiorite and lesser biotite granite to granodiorite.|
24511|Tallaganda Granodiorite|71699|5|Briefly described|Map legend.|Silurian|Silurian|||Thurralilly Suite.|||Grey to cream, medium-grained, massive to protomylonitic, equigranular muscovite-biotite-K-feldspar-plagioclase-quartz granodiorite.|
24511|Tallaganda Granodiorite|71700|3|Fully described|vi, viii, p7, p17, p45, CD|Late Silurian|Late Silurian|Named for the Tallaganda State Forest. A type locality is designated at GR 729413 6068184.This unit was previously grouped as a part of the Boro Granite by Best et al. (1964), Felton and Huleatt (1975) and Richardson and Barron (1977) before being formalised as the Tallaganda Granodiorite by Wyborn and Owen (1986). Distribution. geomorphic expression, outcrop, structure, metamorphism, geochemistry, geophysical characteristics and distinguishing features are discussed. Age is derived from SHRIMP age of the geochemically and structurally similar ages for the Lockhart Igneous Complex and the Ellenden Granite. Intrudes Ordovician basement below the southernmost part of the Goulburn basin. See also p52-p53, p77-p78, p81, p83.||Thurralilly Suite||Intrudes the Adaminaby Group. Equivalent to the Lockhart Igneous Complex.|Grey to cream, medium-grained, strongly-foliated, equigranular biotite granodiorite. Black to brown metasedimentary xenoliths are abundant.|
32034|Tallawang Granite|23043|5|Briefly described|Map Legend|Eifelian|Emsian|||||||
32034|Tallawang Granite|23170|3|Fully described|p223|Early Devonian|Early Devonian|of Lachlan Fold Belt.||||||
32034|Tallawang Granite|66713|6|Mentioned|p2 Fig.1, p13|||Age < 415 +/- 11 Ma (Fanning, 1997): a rhyolite cut by this unit. Appears as Tallawang Granodiorite in Fig.1.||||||
32034|Tallawang Granite|67847|5|Briefly described|p59|Early Devonian|Early Devonian|Intrusion into the Dungeree Volcanics resulted in the formation of the Tallawang magnetic skarn. ||||Intrudes the Dungeree Volcanics.||
32034|Tallawang Granite|68003|5|Briefly described|p24 Fig.3-e, p142. |Emsian|Emsian|Lachlan Fold Belt, Brigalow Belt South Bioregion. Part of the Yeoval Batholith.|||||Fine- to medium-grained biotite granite, alkali granite, quartz monzonite, granophyre.|
32034|Tallawang Granite|70036|5|Briefly described|Map legend|Devonian|Devonian|Lachlan Fold Belt. |||||Includes granite.|
80916|Tallawudjah Leucosyenogranite|71628|4|Described|p17: 2, 54, 59, 68-70, 94|||Chisholm et al. (2014) after Chappell and Bryant (1994 unpublished). Name changed in this study to Tallawudjah Leucosyenogranite to reflect modal data. Initially Tallawudjah Leucoadamellite (Korsch, 1978). Named after a local watercourse. Forms a small (0.6 x ~1.5 km) intrusion 5 km SW of Glenreagh village. Geochemistry described.|229.9 +/- 1.4 Ma (Chisholm et al., 2014).|Tallawudjah Suite.||Intrudes Coramba beds. Is partly overlain by Bundamba Group.|Porphyritic biotite-hornblende leucosyenogranite, and possibly leucomonzogranite; commonly altered. A-type.|
82680|Tallawudjah Suite|71628|5|Briefly described|p17: 66, 69|||||Glen Esk Supersuite.|Tallawudjah Leucosyenogranite, Kellys Creek Leucomonzogranite.|||
76756|Tallowa Gully granite|70661|5|Briefly described|p126 fig 10, p132, p134-p135|Carboniferous|Carboniferous|Named after Tallowa Gully. Forms a "scarp" at the bottom of Tallowa Gully. No type section given. Age is tentative. Petrographically similar to Marulan batholith and Bundanoon Granite.||||Overlain by Snapper Point Formation|Quartz, feldspar and minor biotite granite porphyry.|
76756|Tallowa Gully granite|71303|5|Briefly described|map legend|Carboniferous|Late Devonian||||||Porphyritic medium-grained biotite granite (poorly known).|
73700|Tallwood Intrusive Complex|63286|5|Briefly described|p304, p310|Llandovery|Late Ordovician|Age: 439Ma. Consists of porphyritic mafic intrusions that are predominantly equigranular.||||||07-FEB-11
30216|Tallwood Monzodiorite|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|Reserved as Tallwood Monzonite.||||||
79109|Tally Ho Ignimbrite Member|69635|6|Mentioned|p18|||||Of Long Flat Volcanics.||||16-JUL-15
79109|Tally Ho Ignimbrite Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Long Flat Volcanics.|||Green to grey, medium-grained, moderately fragmental and densely welded, crystal-rich dacitic ignimbrite; variable lithic clast content.|
79109|Tally Ho Ignimbrite Member|71700|3|Fully described|vi, p24-p26, p58, p63, p66, p79|Early Devonian|Early Devonian|Named for the Tally Ho Road. A type locality is nominated at GR 741168 6071935 along the eastern slopes of Tallaganda State Park. These rocks were included in the Long Flat Porphyries of Anderson (1893) which were renamed the Long Flat Volcanics (Best et al, 1964). White (1961) thereafter formalised the Bombay Volcanics in which this unit was included. Whites subdivision was continued by Felton and Huleatt (1975). Potentially equivalent to the Wongabel Rhyodacite Member. Mistakenly referred to as the Tally Ho Dacite Member in the CD. Thickness is estimated between 500 and 600m within the Gingamona Syncline. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics and distinguishing features are discussed.|413.4 +/- 2.6 Ma (SHRIMP U-Pb)|Long Flat Volcanics||Overlies the Kadoona Dacite Member. Overlain by the Croppies Gunyah Ignimbrite Member and the Toggannoggra Rhyolite Member. Intruded by the Kain Porphyry Member.|Green-grey, porphyritic ignimbrite of dacitic composition whicch retains a faint welded fabric in places.|
82682|Talmo Formation|73215|4|Described|p991, 994-1004|||Talmo-Taemas area, about 30 km W of Yass, NSW. Lachlan Orogen. Named after a local property. Over 1,200m thick. No type section; locations of representative sections for both the lower limestone/mudstone component and for the upper mudstone/interbedded quartz sandstone component are given. Photographs, map, cross-section. The problematic structural pattern (folds, faults and dips) is discussed. A caldera collapse is postulated.||||Overlies Goobarragandra Volcanics. Is overlain by and partly faulted against Mountain Creek Volcanics. May be equivalent to Yass and Yarralumla Formations.|A clastic-carbonate succession, including interbedded limestone and mudstone, with local massive mudstone and quartz-rich turbidites. Lithologies described in some detail.|
29042|Tamby Creek Formation|22610|5|Briefly described|Fig 5||Silesian|Age 305.3 +/-3.2Ma||||||
29042|Tamby Creek Formation|22857|5|Briefly described|p536 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Andesite and andesite breccia interbedded with lithic sandstone, conglomerate and tuff. Max. thickness: 130m. Geological Province: Sydney Basin.||||||
29042|Tamby Creek Formation|23540|5|Briefly described|Fig 3 p 420|||Also see p 425||||||
29042|Tamby Creek Formation|32094|6|Mentioned|p383|||||||||
29042|Tamby Creek Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis elongata||||||
29042|Tamby Creek Formation|35284|6|Mentioned|p37|||||||||
29042|Tamby Creek Formation|37922|5|Briefly described|p481|||||||||
29042|Tamby Creek Formation|38217|6|Mentioned|p272|||||||||
29042|Tamby Creek Formation|38837|6|Mentioned|p232|||||||||
29042|Tamby Creek Formation|39288|6|Mentioned|p57|||||||||
29042|Tamby Creek Formation|39304|6|Mentioned|Fig. 19.2|||||||||
29042|Tamby Creek Formation|44244|6|Mentioned|p272|Early Permian|Early Permian|||||||
29042|Tamby Creek Formation|46849|6|Mentioned|Fig. 8|||||||||
29042|Tamby Creek Formation|60289|5|Briefly described|p2|Late Carboniferous|Late Carboniferous|Of Dalwood Group. Overlies Seaham Formation. Underlies Beckers Formation. Geological Province: Cranky Corner Basin.||||||
29042|Tamby Creek Formation|60290|3|Fully described|p15, 18, 34-35, 38-39|Late Carboniferous|Late Carboniferous|Basal unit of Dalwood Gp. Overlies Seaham Fm. Unconformably overlain by Beckers Fm. Thick: 82 m. Interbedded volcanic congloms + intermediate to felsic tuffs. Age: 304-300 Ma. G.P: Cranky Corner Basin.||||||07-FEB-11
29042|Tamby Creek Formation|60291|4|Described|p51, 53 Tb.1|Late Carboniferous|Late Carboniferous|Distal Tuff, volcanic conglomerate, sandstone. Coastal alluvial fan, proximal volcanism. Petrology described.||||||26-MAR-13
29042|Tamby Creek Formation|60292|4|Described|p65|Late Carboniferous|Late Carboniferous|Overlies Seaham Formation. Overlain by Beckers Formation. Petrography and geochemistry described.||||||02-MAY-13
29042|Tamby Creek Formation|60293|5|Briefly described|p108 Fig. 1|Late Carboniferous|Late Carboniferous|Overlies: Seaham Formation. Overlain by Beckers Formation.||||||17-JUN-05
29042|Tamby Creek Formation|60294|5|Briefly described|p116 Fig.1|Late Carboniferous|Late Carboniferous|Overlies Seaham Formation. Overlain by Beckers Formation.||||||
29042|Tamby Creek Formation|60295|4|Described|p127, p133 Fig.9|Asselian|Westphalian|Of Dalwood Group. Overlies Seaham Formation. Overlain by Beckers Formation. Age: 300-304 Ma. Volcanogenic. Geological Province: Cranky Corner Basin.||||||
29042|Tamby Creek Formation|60296|5|Briefly described|p155, p156 Fig.1|||Of Dalwood Group. Geological Province: Cranky Corner Basin||||||
29042|Tamby Creek Formation|60297|5|Briefly described|p167|Permian|Permian|Of the Dalwood Group. Geological Province: Cranky Corner Basin.||||||
29042|Tamby Creek Formation|60298|5|Briefly described|p180, 185|Stephanian|Stephanian|Age: 304-300 Ma (SHRIMP zircon U-Pb). Coarse volcanic-derived conglomerates with interbeds of volcaniclastic sandstone.||||||17-DEC-07
29042|Tamby Creek Formation|60299|5|Briefly described|p207, 218|||Palaeomagnetism measured.||||||
29042|Tamby Creek Formation|60300|5|Briefly described|p242 Tb.1|Early Permian|Late Carboniferous|Of the Dalwood Group. Overlies Seaham Formation. Overlain by Beckers Formation. Tuff, tuffaceous sandstone and volcanic conglomerate.||||||
29042|Tamby Creek Formation|62095|5|Briefly described|p268|Late Carboniferous|Late Carboniferous|Includes tuffs interbedded with conglomerates containing intermediate and basaltic clasts.  Age: 304-3+-Ma.||||||31-JAN-08
29042|Tamby Creek Formation|63832|5|Briefly described|p131 fig 2, p135|Kasimovian|Moscovian|Cranky Corner/Gresford Block, Southern New England Fold Belt.||||Conformably overlies Seaham Formation.||14-DEC-17
29042|Tamby Creek Formation|64631|5|Briefly described|p44 Fig.2.|Kazimovian|Moscovian|Southern New England Fold Belt, Cranky Corner/Gresford Block. Some biostratigraphic age control.||||Overlies Seaham Formation.||
29042|Tamby Creek Formation|65382|6|Mentioned|p717 App. 2|Pennsylvanian||Gresford Block, NSW. Top has radiometric age of 302 Ma.||||||
29042|Tamby Creek Formation|69793|6|Mentioned|p1121 Fig.12|Gzhelian|Moscovian|Gresford Block, Tamworth Belt.||||||
29042|Tamby Creek Formation|70096|5|Briefly described|Supp2|||Of northern Sydney Basin. "Evidence of glacial facies, based on core examination and description" in the basal part of Beckers Formation as intersected in Tangorin-1 core (Stevenson 2003; from Fielding er al., 2008a; see supplementary information) is reassigned as part of Tamby Creek Formation. Includes angular volcanic orthoconglomerate clasts interpreted to be locally derived, rather than glacial transport. See also supplementary files in appendix for additional stratigraphic and locality information. ||||||
29042|Tamby Creek Formation|73197|6|Mentioned|p469, p473|Gzhelian|Carboniferous|Cranky Corner Basin. Zircon content in the upper part of the formation derived from the interior of the continent, dated tuff horizon at top of the formation has a large increase in inherited zircons ranging from the Archean to Carboniferous (Claoue-Long and Korsch, 2003).|300 Ma||||Includes a tuff horizon at the top of the formation.|
29042|Tamby Creek Formation|73487|6|Mentioned|p563, p585|||Gresford Block, Cranky Corner Basin. Written only as Tamby Creek p566.|ca 300 Ma near top|||||
27094|Tangerang Formation|22678|3|Fully described|p711-15||Early Devonian|Of the Bindook Volcanic Complex. Includes the Kerillon Tuff, Carne Dacite and Kerrawarra Dacite Members.||||||17-JAN-06
27094|Tangerang Formation|22842|6|Mentioned|p31|||Unconformably overlies Bungonia Group.||||||16-JUN-08
27094|Tangerang Formation|22857|5|Briefly described|ERRATA sheet for p482|Devonian|Devonian|Supersedes Tangerang Volcanics and "Tangerang Volcanics". Contains Windellama Limestone, Carne Dacite and Aloes Tuff Members.||||||
27094|Tangerang Formation|23522|5|Briefly described|p248 Fig 4|Devonian|Pridoli|||||||
27094|Tangerang Formation|24019|6|Mentioned|p353, p636||Lochkovian|||||||
27094|Tangerang Formation|39568|1|Redefined|p77|Early Devonian|Early Devonian|||||||
27094|Tangerang Formation|42033|6|Mentioned|p651|||||||||
27094|Tangerang Formation|42142|5|Briefly described|p578|||See also Fig.3||||||
27094|Tangerang Formation|42210|5|Briefly described|p172|||See also Fig.1||||||
27094|Tangerang Formation|42931|5|Briefly described|p495|||||||||
27094|Tangerang Formation|50234|5|Briefly described|Map Legend|Pragian|Pragian|Of the Bindook Volcanic Complex.  Includes: Kerrawarra Dacite Member, Kerillon Tuff Member, Carne Dacite Member, Devils Pulpit Member, Brooklyn Conglomerate Member.||||||
27094|Tangerang Formation|62070|5|Briefly described|p38,|Pragian|Lochkovian|Basal limestones in Yass and Windellema areas.|||||includes quartz-rich siltstone and sandstone. Also basal limestones.|
27094|Tangerang Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Bindook Group. Includes 7 members. Massive to well-bedded tuffaceous sst., volcanic breccia+siltstone, qtz.sst., minor basal conglom., rare allochthanous limest.blocks; rhyolitic non-welded ignimb., welded dacite ignimb., massive to flow-banded dacite.||||||09-SEP-08
27094|Tangerang Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Bungonia. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27094|Tangerang Formation|66300|6|Mentioned|p76, pp81-86.|||||Unit in Bindook Group.|Includes Kerillon Tuff Member.|||
27094|Tangerang Formation|68592|2|Defined|p902,p907-8, p1061, p1066-71, p1079-1133|Pragian|Lochkovian|See also p732, p741, p840, p1613, p1628, p1904-5. Informally named Tangerang volcanics by Gould (1966) and Wass and Gould (1969); redefined as Tangerang Formation by Jones, Carr et al. (1984). The original type section has been mostly buried by limestone quarrying operations. A number of representative sections and exposures for the various facies are described. Geochemistry detailed; geophysical properties described. Records transition from shallow marine to predominantly fluvio-lacustrine environments. Up to 2600m thick. Contains a mid Lochkovian conodont fauna (or possibly Pridoli) at the base, and trilobite fauna suggest most of the Formation is Pragian. Fauna listed and described.||Unit in Bindook Group.|Includes Carne, Kerrawarra and Bogungra, Dacite Members; Kerillon Tuff, Windellama Limestone, Brooklyn Conglomerate and Devils Pulpit, Members.|Unconformably overlies Adaminaby Group and Bungonia Group. Is overlain unconformably by Joaramin + Barrallier Ignimbrites, Lambie + Shoalhaven Groups. Intruded by several units of Arthursleigh Suite.|Dacitic and rhyolitic pyroclastics, lavas and shallow intrusions; tuffaceous sandstone and siltstone, quartzose sandstone; subordinate conglomerate and limestone. Includes welded ignimbrite. I-type.|
27094|Tangerang Formation|69159|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Bindook Group.|Includes Windellama Limestone Member and Devils Pulpit Member.||Massive to well-bedded volcanic sandstone and siltstone, volcanic breccia, quartzose sandstone and siltstone; basal limestone.|
27094|Tangerang Formation|70192|5|Briefly described|Map Legend|Pragian|Lochkovian|Dkt[3 asterisks]. Includes four unnamed members consisting of: fossiliferous allochthonous limestone blocks; quartz sandstone and mudstone and rare pebbly sandstone; siltstone and minor quartz sandstone with shallow marine in-situ fauna; sparsely fossiliferous, immature volcanic sandstone, vitric mudstone, non-fossiliferous pebbly sandstone towards top. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Bindook Group|Includes Brooklyn Conglomerate, Carne Dacite Member, Kerillon Tuff Member, Kerrawarra Dacite Member, Bogungra Dacite Member, Devils Pulpit Member, Windellama Limestone and four unnamed members.|Erosional at base. Is overlain by Joaramin Ignimbrite.|Massive-well bedded, tuffaceous sandstone, volcanic breccia, siltstone, quartz sandstone, rhyolitic non-welded ignimbrite, welded dacitic ignimbrite, massive-flow banded dacite lava, intrusive dacite, minor basal conglomerate, rare limestone blocks.|
27094|Tangerang Formation|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes four unnamed members consisting of fossiliferous limestone, well sorted medium grained quartz sandstone, fossiliferous siltstone and immature sparsely fossiliferous volcanic sandstone.||Bindook Group|Includes Brooklyn Conglomerate, Carne Dacite Member, Kerillon Tuff Member, Kerrawarra Dacite Member, Bogungra Dacite Member, Devils Pulpit Member, Windellama Limestone and four unnamed members.||Massive-well bedded, tuffaceous sandstone, volcanic breccia, siltstone, quartz sandstone, rhyolitic non-welded ignimbrite, welded dacitic ignimbrite, massive-flow banded dacite lava, intrusive dacite, minor basal conglomerate, rare limestone blocks.|
27094|Tangerang Formation|70661|3|Fully described|p51, p52 fig 5, p53 - p59|Pragian|Lochkovian|Name derived from Tangerang Creek. Synonymous with Tangerang Volcanics. Distribution, geomorphology, structure,  fossil assemblage, metamorphism, geochemistry , economic geology and geophysical characteristics all discussed. A number of representative sections discussed. Maximum thickness of 2600m estimated. Deposited in moderately deep- shallow marine  and deltaic environments through to some subaerial deposition. Intruded by Marulan Granite, Arthursleigh Suite, unconformably (or faulted over) overlying Adaminaby Group. See also p61, p64, p81, p243, p245.|412 +/- 2.2 Ma (SHRIMP U-Pb)|Bindook Group|Kerillon Tuff Member, Carne Dacite Member, Devils Pulpit Member, Kerrawarra Dacite Member, Brooklyn Conglomerate Member, Windellama Limestone Member, Bogungra Dacite Member|(either faulted against, disconformably or conformably) overlies Bungonia Group, unconformably overlain by Barrallier Ignimbriate, overlain by Joaramin Ignimbrite, Lambie Group, Shoalhaven Group.|Dacitic and rhyolitic pyroclastic rocks, lavas and shallow intrusions, tuffaceous sandstone and siltstone, quartzose sandstone and subordinate conglomerate and limestone.|
27094|Tangerang Formation|71303|5|Briefly described|map legend|Pragian|Lochkovian|||Of Bindook Group.|Includes Devils Pulpit Member, Kerillon Tuff Member, Kerrawarra Dacite Member, Carne Dacite Member.||Dacitic and rhyolitic pyroclastic rock, lava and shallow intrusions, tuffaceous sandstone and siltstone, quartzose sandstone.|16-FEB-18
27094|Tangerang Formation|71656|5|Briefly described|p13 Fig.2, p11, p38-39|Pragian|Lochkovian|Shown in Fig.2 as Pragian to Emsian. Corals, brachiopods, trilobites and other fossiliferous fauna implied Lochovian age in 1986. Mawson and Talent (1999) inferred a Pragian age from the fossils they described 375m above the base of the formation.||Bindook Group|Includes Windellama Limestone Member||Contains limestone pods.|
27094|Tangerang Formation|71699|5|Briefly described|Map legend.|Devonian|Devonian|Four facies, including the two formal Members, are mapped separately.||Bindook Group.|Windellama Limestone Member, Devils Pulpit Member.||Massive to well-bedded volcanic sandstone and siltstone, volcanic breccia, quartzose sandstone and siltstone; basal limestone.|
27094|Tangerang Formation|71700|2|Defined|vi, p7, p10, p23-p24,|Late Lochkovian|Middle Lochkovian|Named for the Tangerang Creek in Mossvale100. The original type section of Jones et al (1984) has been largely buried by quarrying and landscape restoration. Three representative sections were nominated in Goulburn100 (Thomas and Pogson, 2012). Another representative section for the lower part of the Formation is in Windellama Creek. The Tangerang volcanics was previously recognised as an informal unit by Gould (1966) and Wass and Gould (1969). This unit was upgraded and formally defined as the Tangerang Formation by Jones et al (1984) and subsequent workers (Jones et al. 1986; Simpson, Carr and Jones 1997). In Braidwood rocks of this formation was previously assigned to the Jacqua and Burburba formations. Also includes the Carne Dacite Member, Bogungra Dacite Member, Kerillon Tuff Member and Kerrawarra Dacite Member. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geophysical characteristics, fossils, economic geology and distinguishing features are discussed.  A maximum thickness of 2600m was estimated by Simpson, Carr and Jones (1997). This unit is interpreted as a temporal correlative of the Quialigo Volcanics. See also p27, p43, p57, p62, CD.||Bindook Group|Includes the Brooklyn Conglomerate Member, Windellama Limestone Member and the Devils Pulpit Member.|Unconformably overlies (or is faulted against) the Abercrombie Formation. Faulted against the Cardinal View Formation.|Dacitic and rhyolitic pyroclastic rocks, lavas and shakllow intrusions, tuffaceous sandstone and siltstone, quartzose sandstones and subordinate conglomerate and limestone.|
34101|Tangorin Coal Member|22610|6|Mentioned|p 127|||||||||
30466|Tanja Syenite Complex|22815|4|Described|p106,107 table1|||||||||
30466|Tanja Syenite Complex|43233|5|Briefly described|Map Legend|Late Cretaceous|Early Cretaceous|||||||
30153|Tannabutta Group|22529|4|Described|6|Pridoli|Wenlock|||||||
30153|Tannabutta Group|22590|6|Mentioned|Fig3 P754|Pridoli|Ludlow|||||||
30153|Tannabutta Group|22768|6|Mentioned|p177|Late Silurian|Silurian|||||||
30153|Tannabutta Group|22857|5|Briefly described|p177, p476 App.1 Tb.A1.6|Late Silurian|Middle Silurian|Correlative of the Mumbil Group. Max. thickness: 3km. Geological Province: Capertee Rise.||||||
30153|Tannabutta Group|23043|5|Briefly described|Map Legend|Pridoli|Ludlow|||||||
30153|Tannabutta Group|23170|3|Fully described|p61|Silurian|Silurian|Age: Middle to Late Silurian (?Wenlock to late Pridoli). Lachlan Fold Belt.||||||
30153|Tannabutta Group|23309|6|Mentioned|p390|||||||||
30153|Tannabutta Group|50124|6|Mentioned|p125 Fig.2|Early Devonian|Late Silurian|Geological Province: eastern Lachlan Fold Belt.||||||
30153|Tannabutta Group|68003|5|Briefly described|p24 Fig.3-e, pp146-147. |Pridoli|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion. Mis-spelt as Tanabutta Group on p24.|||Includes Dungeree Volcanics.||Limestone and limestone breccia; shale, slate and volcanic-rich sandstone; mafic to intermediate intrusion; rhyolite lava, frequently flow-banded.|
30153|Tannabutta Group|70036|5|Briefly described|Map legend|||Lachlan Fold Belt. Included in a mapped unit of Silurian and Devonian sedimentary and volcanic rocks including strongly to moderately deformed felsic to andesitic metasedimentary rocks, conglomerate, sandstone, siltstone, mudstone, shale, tuff, basalt, andesite and rhyolite.||||||
26163|Tantangara Formation|22815|5|Briefly described|p35|Llandovery|Llandovery|||||||
26163|Tantangara Formation|22857|4|Described|p134, p420 App. 1 Tb. A1.5|Early Silurian|Early Silurian|Of the Yalmy Group. Coarse to fine quartz arenite, siltstone and shale. Max. thickness: 2km. Geological Province: Yalmy Basin.||||||
26163|Tantangara Formation|22968|6|Mentioned|P108|||Parent is Yalmy Group||||||
26163|Tantangara Formation|23245|5|Briefly described|p134||Early Silurian|||||||
26163|Tantangara Formation|23309|6|Mentioned|p390|||||||||
26163|Tantangara Formation|23454|5|Briefly described|p28|Llandovery|Llandovery|||||||
26163|Tantangara Formation|36443|5|Briefly described|map legend|Llandoverian|Llandoverian|Coarse to fine quartz arenite, siltstone and shale, grading from proximal flysch in west to distal flysch in east. Includes massive quartzite (Saq). BMR map code: Sa.||||||
26163|Tantangara Formation|40136|6|Mentioned|p34|||||||||
26163|Tantangara Formation|40498|6|Mentioned|p365|||||||||
26163|Tantangara Formation|43233|5|Briefly described|Map Legend||Llandovery|Of Yalmy Group.||||||20-MAY-08
26163|Tantangara Formation|44092|5|Briefly described|map legend|Early Silurian|Early Silurian|Slf1||||||
26163|Tantangara Formation|44093|5|Briefly described|p189 App. 1|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
26163|Tantangara Formation|45147|2|Defined|M66|early Llandoverian|early Llandoverian|||||||
26163|Tantangara Formation|60078|6|Mentioned|Map Legend|Early Silurian|Early Silurian|||||||
26163|Tantangara Formation|63290|5|Briefly described|p388, p395, p396 Fig. 3|Llandovery|Llandovery|Of Yalmy Group. Overlain by Peppercorn Formation unconformably.||||||08-DEC-16
26163|Tantangara Formation|68592|5|Briefly described|p13, p30|Llandovery|Llandovery|Owen and Wyborn (1979). Derived from erosion of a deformed and uplifted backarc region.||||Unconformably overlies Kiandra Group.||
34615|Tantitha Ultramafic Complex|22831|4|Described|p 23|||||||||
29046|Tanwarra Shale|5253|6|Mentioned|p100.|||||||||
29046|Tanwarra Shale|22472|5|Briefly described|p37|Silurian|Silurian|of the Mumbil Group||||||
29046|Tanwarra Shale|22486|4|Described|p 1, 2, 3, 5, 6, 7|Ludlovian|Wenlockian|Hill End Trough||||||
29046|Tanwarra Shale|22590|6|Mentioned|P750|Ludlow|Wenlock|||||||
29046|Tanwarra Shale|22768|6|Mentioned|p180|||||||||
29046|Tanwarra Shale|22857|4|Described|p180, p472 Tb A1.6, p478 Tb A1.6|Llandovery|Llandovery|Of Mumbil Group. Mudstone, siltstone, limestone, lithic arenite; corals, trilobites, graptolites. Conformably underlies Bells Creek Volcanics; disconformably overlies Pipers Flat Formation. Max.thickness: 375m. Geol.Prov: Hill End Trough and Capertee Rise||||||
29046|Tanwarra Shale|23043|5|Briefly described|Map Legend|Ludlow|Wenlock|of Mumbil Group.||||||
29046|Tanwarra Shale|23170|2|Defined|p97|Ludlow|Wenlock|of Mumbil Group.||||||
29046|Tanwarra Shale|23214|3|Fully described|p139|Ludlow|Wenlock|Of Mumbil Group. First defined by Packham (1968b). Prodominantly black and brown mudstone, siltstone, limestone and lithic sandstone. Max. thickness 375m.||||||
29046|Tanwarra Shale|23738|5|Briefly described|p251|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
29046|Tanwarra Shale|24394|5|Briefly described|p170|Ludlow|Wenlock|||||||
29046|Tanwarra Shale|29669|6|Mentioned|p604|||||||||
29046|Tanwarra Shale|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
29046|Tanwarra Shale|30099|6|Mentioned|Fig.2|||||||||
29046|Tanwarra Shale|32621|6|Mentioned|p1|||||||||
29046|Tanwarra Shale|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
29046|Tanwarra Shale|32708|6|Mentioned|Fig.3|||||||||
29046|Tanwarra Shale|33006|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
29046|Tanwarra Shale|33282|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
29046|Tanwarra Shale|33285|5|Briefly described|p20|||Early Sil.||||||
29046|Tanwarra Shale|33948|6|Mentioned|p79|||||||||
29046|Tanwarra Shale|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
29046|Tanwarra Shale|34404|6|Mentioned|Fig.3.5b|||Lower Silurian||||||
29046|Tanwarra Shale|34405|4|Described|p105|||Late Early Silurian or Early Middle Silurian||||||
29046|Tanwarra Shale|34406|6|Mentioned|p221|||||||||
29046|Tanwarra Shale|34572|6|Mentioned|p89|||See also Table 1. Silurian||||||
29046|Tanwarra Shale|35137|6|Mentioned|p88|||||||||
29046|Tanwarra Shale|35166|6|Mentioned|p121|||||||||
29046|Tanwarra Shale|35185|6|Mentioned|p245|||||||||
29046|Tanwarra Shale|35877|6|Mentioned|p126|||||||||
29046|Tanwarra Shale|36285|6|Mentioned|Fig.6|||||||||
29046|Tanwarra Shale|37727|4|Described|p87|||See also P30.||||||
29046|Tanwarra Shale|39331|6|Mentioned|Table 7.1|||See also Fig.0-3||||||
29046|Tanwarra Shale|40136|6|Mentioned|p39|||[Originally entered for Tas. CEBMar95]||||||
29046|Tanwarra Shale|40328|3|Fully described|p179|||||||||
29046|Tanwarra Shale|43188|6|Mentioned|p205|||Sofala district.||||||
29046|Tanwarra Shale|43263|6|Mentioned|Map Legend|Late Silurian||Age Middle-Late Silurian.||||||
29046|Tanwarra Shale|43344|14|Not recorded|p139,152||Silurian|||||||
29046|Tanwarra Shale|43515|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition)||||||
29046|Tanwarra Shale|43516|14|Not recorded|Map Legend|Early Silurian|Early Silurian|(L.-M.Sil)||||||
29046|Tanwarra Shale|43517|2|Defined|p112-122,147-159||Silurian|Type section in parish of Sofala. Slight U/C on Sofala Volcanics. Map Plate XII||||||
29046|Tanwarra Shale|43641|5|Briefly described|Map Legend||Silurian|||||||
29046|Tanwarra Shale|43782|5|Briefly described|Map Legend|Ludlow|Wenlock|of Mumbil Group.||||||
29046|Tanwarra Shale|44093|5|Briefly described|p213 App. 1|Early Devonian|Silurian|Of the Mumbil Group. Geological Province: Lachlan Fold Belt.||||||
29046|Tanwarra Shale|63278|5|Briefly described|p157|||Underlain by Pipers Flat Formation. Geological Province: Rockley-Gulgong Volcanic Belt, LFB. Consists of upward-deepening sucuession, basal conglomerates to traction-current sandstones into shales with graptoloites.||||||07-FEB-11
29046|Tanwarra Shale|63290|6|Mentioned|p392 Tb. 1|Ludlow|Wenlock|Geological Province: Rockley-Gulgong Volcanic Belt. Passes up through conglomerate, sandstone, limestone and into shale with graptolites (Pickett et al. 1996).||||||
29046|Tanwarra Shale|68592|6|Mentioned|p426|||||||Overlies Sofala Volcanics.||
29046|Tanwarra Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
29046|Tanwarra Shale|71924|5|Briefly described|p2|||Of Packham 1968, Sherwin 1994. Hill End Trough. Includes important faunas.||||||
29046|Tanwarra Shale|73299|6|Mentioned|p1102 Fig.8|||Hill End Trough, eastern. [Map symbol suggests Silurian age]||||||
26327|Taplow Limestone Member|5250|6|Mentioned|p47||Late Ordovician|Member of Fossil Hill Limestone. ||||||
26327|Taplow Limestone Member|23214|3|Fully described|p41|Eastonian|Eastonian|Of Fossil Hill Limestone. Max. thickness 10m.||||||
26327|Taplow Limestone Member|38219|2|Defined|p307|Late Ordovician|Late Ordovician|Part of Cliefden Caves Group. See also Fig.2.||||||
26327|Taplow Limestone Member|41046|6|Mentioned|Fig.2|||||||||
26327|Taplow Limestone Member|42479|5|Briefly described|p108|||||||||
26327|Taplow Limestone Member|42603|5|Briefly described|Fig.4 P57|||||||||
26164|Tara Granodiorite|22815|4|Described|p59|Silurian|Silurian|||||||
26164|Tara Granodiorite|23551|5|Briefly described|p490|||Lachlan Fold Belt||||||
26164|Tara Granodiorite|33779|4|Described|p168|||Map||||||
26164|Tara Granodiorite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
26164|Tara Granodiorite|33852|6|Mentioned|p501|||Date given.||||||
26164|Tara Granodiorite|35109|2|Defined|p44|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
26164|Tara Granodiorite|35192|6|Mentioned|p280|||||||||
26164|Tara Granodiorite|36411|6|Mentioned|p270|||Refers White et al 1977 for definition.||||||
26164|Tara Granodiorite|38327|6|Mentioned|Table 4|||||||||
26164|Tara Granodiorite|38500|4|Described|p90|||||||||
26164|Tara Granodiorite|39721|6|Mentioned|p48|||See also Table 2. Sr Isotopes||||||
26164|Tara Granodiorite|40328|4|Described|p210|||||||||
26164|Tara Granodiorite|41133|6|Mentioned|p1118|||||||||
26164|Tara Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Tara Suite.||||||
26164|Tara Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh8||||||
26164|Tara Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
26164|Tara Granodiorite|68310|6|Mentioned|p240|||Berridale Batholith. 24 km2. An I-type granite completely surrounded by the older (intruded) S-type Cootralantra Granodiorite.||||||
26164|Tara Granodiorite|72571|5|Briefly described|p90-91, p95-101|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail. I-type.|||||Hornblende granite with titanite, allanite and magnetite.|
31641|Tara Suite|22719|6|Mentioned|p485|||||||||
31641|Tara Suite|22815|5|Briefly described|p53,59|Silurian|Silurian|||||||
31641|Tara Suite|42726|5|Briefly described|map legend||Silurian|||||||
31641|Tara Suite|72571|6|Mentioned|p90-91, p103|||Of the Tasmanides of eastern Australia.||||||
25516|Tarago Conglomerate|22768|5|Briefly described|p177,179||Early Devonian|||||||
25516|Tarago Conglomerate|22857|4|Described|p177, p179, p472 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Mulwaree Group. Polymictic boulder conglomerate, arenite and siltstone. Max. thickness: 300m. Geological Province: Captains Flat-Goulburn Trough.||||||07-SEP-15
25516|Tarago Conglomerate|23048|5|Briefly described|p7 fig9||Early Devonian|||||||
25516|Tarago Conglomerate|24116|5|Briefly described|p88|||||||||
25516|Tarago Conglomerate|30730|6|Mentioned|p10|||Geological map||||||
25516|Tarago Conglomerate|30735|6|Mentioned|p46|||||||||
25516|Tarago Conglomerate|30736|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25516|Tarago Conglomerate|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
25516|Tarago Conglomerate|31982|5|Briefly described|p703|||||||||
25516|Tarago Conglomerate|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25516|Tarago Conglomerate|34692|6|Mentioned|p183|||||||||
25516|Tarago Conglomerate|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
25516|Tarago Conglomerate|39331|6|Mentioned|p56|||See P57||||||
25516|Tarago Conglomerate|40328|6|Mentioned|p184|||See also P186||||||
25516|Tarago Conglomerate|42820|5|Briefly described|p86|||||||||
25516|Tarago Conglomerate|68592|5|Briefly described|p1160|Early Devonian|Early Devonian|Age is poorly constrained.||Unit in Mulwaree Group.||Probably equivalent to Bullamalita Conglomerate.|Clast-supported boulder conglomerate with a distinctive red sandstone matrix, alternating with red sandstone and siltstone-rich intervals; possibly fluvial deposits.|
25516|Tarago Conglomerate|69159|5|Briefly described|Map legend|Pragian|Pragian|||Unit in Mulwaree Group.||Is overlain by Bongalaby Formation.|Purple, maroon and red, clast to matrix supported, polymictic, pebble to boulder conglomerate; lesser interbedded coarse-grained to pebbly sandstone and maroon to purple, laminated to thinly-bedded, fine-grained sandstone and siltstone.|07-SEP-15
25516|Tarago Conglomerate|71040|6|Mentioned|p19|Early Devonian|Early Devonian|Braidwood region.||||||
25516|Tarago Conglomerate|71069|6|Mentioned|p135|||||Mulwaree Group||Unconformably overlies the Mount Fairy Group.||
25516|Tarago Conglomerate|71656|6|Mentioned|p12 Fig.2|Pragian|Pragian|Shown only in correlation chart (Fig.2).||Mulwaree Group||Underlies Bongalaby Formation.||
25516|Tarago Conglomerate|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Mulwaree Group.|||Purple, maroon-red, clast- to matrix-supported, polymictic pebble to boulder conglomerate with lesser interbedded, medium- to very thick-bedded, coarse-grained to pebbly sandstone and maroon-purple thin-bedded, fine-grained sandstone and siltstone.|
25516|Tarago Conglomerate|71700|2|Defined|vi, p7, p27, p52|Late Pragian|Late Pragian|Named for the village of Tarago. A type section was designated by Felton and Huleatt (1977) in the Mulwaree River from GR 739413 6113184 to GR 739613 6113184 where it is estimated to be 200m thick. Garretty (1936) used the term "Red Bed Stage" to refer to this unit. Rocks previously mapped by Felton and Huleatt (1975) as Tarago Conglomerate are now considered to be Bongalaby Formation; other rocks mapped as this member by the same author are now regarded as Ralpine Valley Sandstone Member of the Long Flat Volcanics. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features, economic geology and geological hazards are discussed. This unit is sestimated to be 300m thick near Tarago. Lithology is discussed in detail. Age is inferred on the basis of unit relationships.||Mulwaree Group||Overlain by the Bongalaby Formation. Unconformably overlies the Boxers Creek Formation, Covan Creek Formation and the Quialigo Volcanics.|Clast- to matrix-supported, polymictic, pebble to boulder conglomerate with lesser interbedded, medium- to very thick-bedded, coarse-grained to pebbly, sandstone and laminated to thin-bedded siltstone and fine-grained sandstone.|
24009|Tarakan Formation|721|5|Briefly described|Map legend|Early Permian|Early Permian|Quartzose and lithic sandstone, orthoconglomerate, minor mudstone and siltstone.  Geological Province: Tamworth Belt.||||||21-DEC-04
24009|Tarakan Formation|22857|5|Briefly described|p506 App.1 Tb.A1.8|Sakmarian|Sakmarian|Quartzose and lithic sandstone, orthoconglomerate; minor mudstone and siltstone. Max. thickness: 600m. ||||||
24009|Tarakan Formation|41009|3|Fully described|p5|||||||||
24009|Tarakan Formation|42229|5|Briefly described|p4|||||||||
24009|Tarakan Formation|43091|5|Briefly described|Map legend|||||||||
24009|Tarakan Formation|44093|5|Briefly described|p226 App. 1|Early Permian|Early Permian|Clastic sediments. Geological Province: New England Fold Belt.||||||
24009|Tarakan Formation|68005|5|Briefly described|p49 Fig.3-M, p137, p170.|Artinskian|Asselian|Tamworth Belt. One of a number of units that occur in narrow fault slivers immediately west of the Peel Fault.|||||Quartzose and lithic sandstone, orthoconglomerate, minor mudstone and siltstone.|
32505|Tarban mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
77133|Tarcoon Suite|69635|5|Briefly described|p122, 127, 134, 159|Early Devonian|Early Devonian||~417-408 Ma||Includes Bobelah Granite, Sainsbury Park Granite, Compton Downs Granite, Mount Kelly Granite.|||
77133|Tarcoon Suite|71345|5|Briefly described|p6,10,15,30,33|Early Devonian|Early Devonian|I type granitic suite. Similar in age and lithology to Galambo Granite.|||Includes Compton Downs, Sainsbury Pak and Bobelah granites.|||
77133|Tarcoon Suite|71965|6|Mentioned|p904,910|||Geological province: Lachlan Orogen. I-type granite.||||||
77133|Tarcoon Suite|72522|4|Described|p1, p3, p10, p13, p15-16, p29, p133.|Lochkovian|Pridoli|Occurs in the northern Lachlan Orogen. Magmatic age of Galambo Granite discussed with reference to previous dating of other units in this Suite. Age of the Suite compared with Wertago Volcanics, 400km to the west.|416-418 Ma||Galambo Granite, Bobelah Granite, Sainsbury Park Granite and Compton Downs Granite.|Intrudes Girilambone Group.|Includes kaolinitised, weathered granite.|
25517|Tarlo Formation|22857|4|Described|p217, p494 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Lambie Group. Red quartz and lithic arenite, red siltstone, red, purple, green and grey shale, mudstone. Thickness: >>1000m. Geological Province: Lambie Basin.||||||
25517|Tarlo Formation|22859|6|Mentioned|p217|||||||||
25517|Tarlo Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
25517|Tarlo Formation|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
25517|Tarlo Formation|32865|6|Mentioned|p483|||||||||
25517|Tarlo Formation|32999|3|Fully described|p43|||Refers Brunker et al. (1970) P39||||||
25517|Tarlo Formation|34481|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian - Early Carboniferous||||||
25517|Tarlo Formation|35655|6|Mentioned|p209|||Stratigraphy. See also mention on Fig.2, geology Myrtleville area.||||||
25517|Tarlo Formation|50234|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Lambie Group.  Overlies: Wiarborough Formation, Cookbundoon Formation.||||||
25517|Tarlo Formation|63633|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Lambie Group. Red sandstone, lithic sandstone, red siltstone; red, purple, green and grey shales; mudstone; quartzite in lower part.||||||
25517|Tarlo Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Lambie Group. Purplish-reddish to fawn, thinly bedded, fine- to medium-grained, often flaggy lithic-quartz sandstone, interbedded with purplish to red, fine-grained sandstone and siltstone.||||||
25517|Tarlo Formation|68592|2|Defined|p35, p1722-3, p1727, p1749-53|Early Carboniferous|Famennian|Brunker et al. (1970), after Tarlo River. Extends almost 80 km in the core of the Cookbundoon Syncline. Very subdued topography; forms deep soil. Proposed type section is described, as well as "typical exposures" of Offenberg (1974). Very near to 3000m thick. Unfossiliferous. Has slaty cleavage in finer lithologies. Geochemistry unknown; geophysical properties described. Minimum age is poorly constrained: Famennian to very early Carboniferous. Shows elevated uranium radiometric responses. Has been quarried for road surfacing.||Unit in Lambie Group.||Conformably overlies Cookbundoon Formation and Cowpers Creek Conglomerate. Is correlated with Koorawatha Formation and Morgans Gully Siltstone.|Reddish purple or green, massive or thinly bedded siltstone interbedded with generally thinly to medium-bedded, fine- to medium-grained lithic-quartz sandstone; sparse interbeds of similar but off-white to brown, lithic-quartz sandstone packets.|
25517|Tarlo Formation|70192|5|Briefly described|Map Legend|Carboniferous|Famennian|Dlt. Includes an unnamed sub unit of thin-thickly bedded, fine-medium grained, moderately sorted, commonly laminate, sporadically cross bedded, lithic quartz sandstone. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Lambie Group|Includes one unnamed subunit.|Overlies Cookbundoon Formation.|Thinly-medium bedded and sporadically thickly bedded, fine-medium grained, lithic quartz sandstone interbedded with massive-thinly bedded siltstone.|
25517|Tarlo Formation|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed member of thin-thickly bedded, fine-medium grained, moderately sorted, sporadically cross bedded lithic quartz sandstone.||Lambie Group|||Thinly to medium bedded with sporadic thick bedding, fine to medium grained lithic-quartz sandstone interbedded with massive or thinly bedded siltstone.|
25517|Tarlo Formation|70543|5|Briefly described|Map Legend|Devonian|Devonian|Includes an unnamed sub unit of thin-thickly bedded, fine-medium grained, moderately sorted, commonly laminate, sporadically cross bedded, lithic quartz sandstone.||Lambie Group|Includes one unnamed subunit||Thinly-medium bedded and sporadically thickly bedded, fine-medium grained, lithic quartz sandstone interbedded with massive-thinly bedded siltstone.|
25517|Tarlo Formation|71656|6|Mentioned|p13 Fig.2|Famennian|Frasnian|Shown only in correlation chart (Fig.2).||Lambie Group||Overlies Cookbundoon Formation.||
24013|Tarran Volcanics|22768|6|Mentioned|p172|||||||||
24013|Tarran Volcanics|22857|5|Briefly described|p172, p448 App.1, Tb.A1.6|Devonian|Devonian|Of the Cobar Supergroup. Predominantly crystal and lithic-crystal tuffs. Max. thickness: ~100m. Geological Province: Darling Basin. ||||||
24013|Tarran Volcanics|23454|5|Briefly described|p27 Fig.1|Silurian|Silurian|||||||
24013|Tarran Volcanics|41394|2|Defined|p40|Early Devonian||||||||
24013|Tarran Volcanics|41395|6|Mentioned|Map legend|Lochkovian||||||||
24013|Tarran Volcanics|41528|2|Defined|p103|Early Devonian||||||||
24013|Tarran Volcanics|41529|6|Mentioned|Map legend|Lochkovian||||||||
24013|Tarran Volcanics|41821|6|Mentioned|p11 Fig.5|||Occurs in Nymagee sheet area||||||
24013|Tarran Volcanics|42566|3|Fully described|p87|||||||||
24013|Tarran Volcanics|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
24013|Tarran Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
24013|Tarran Volcanics|43089|5|Briefly described|Map Legend|||of Cobar Supergroup||||||
24013|Tarran Volcanics|43263|6|Mentioned|Map Legend||Early Devonian|||||||
24013|Tarran Volcanics|43757|6|Mentioned|p510|||||||||
24013|Tarran Volcanics|67416|6|Mentioned|p84 Fig.1, p86-87||||433 +/- 4 Ma (Isaacs, 2000).|||Nonconformably overlies Erimeran Granite.||
24013|Tarran Volcanics|70751|5|Briefly described|p8-p9, p11-p12, p25, p28, p38|Silurian|Silurian|An additional date of 415 +/- 3.9 Ma is recorded from this study.|433.1 +/- 4.4 Ma (SHRIMP, Isaacs, 2000)|||Overlies the Erimeran Granite.|A-type volcanics.|
24013|Tarran Volcanics|70828|5|Briefly described|p4|Silurian|Silurian|Equivalent to felsic porphyries that intruded the Erimeran Granite in Early Devonian (Pogson 1991a).|415+\-3.9 Ma (zircon U-Pb)|||||
24013|Tarran Volcanics|71039|6|Mentioned|p6, p26-27|Devonian|Silurian|Defined by MacRae (1987). Intruded by Nymagee felsic dykes dated at 415 +/- 2.7 Ma (Downes et al, 2016).||||||10-MAR-23
24013|Tarran Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|||Massive, medium- to fine-grained rhyolitic crystal, lithic-crystal and partly bedded vitric tuff, minor rhyolite lava, pebble conglomerate and lithic breccia.|
24013|Tarran Volcanics|72958|6|Mentioned|p11|Lochkovian|Lochkovian|Cobar Basin. Nymagee area. Equivalent to the informal Nymagee felsic dykes.||||||
24515|Tarrangatta Schist|37871|4|Described|p7|||||||||
24515|Tarrangatta Schist|39858|6|Mentioned|Map legend|Silurian|Ordovician|Silurian - Ordovician||||||
22954|Tarrawonga Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
31648|Tea Tree Suite|42726|5|Briefly described|Map Legend||Carboniferous|||||||
31648|Tea Tree Suite|44093|5|Briefly described|p214 App. 1|Late Carboniferous|Late Carboniferous|Geological Province: Lachlan Fold Belt.||||||25-JAN-06
70560|Telephone Creek Formation|61820|5|Briefly described|p96, p97|Early Cretaceous||Age based on plant macrofossil and microfossil evidence. Maybe Late Jurassic in age.||||||02-JUN-06
37348|Teltawongee Group|23889|5|Briefly described|p35 Fig. 30|Cambrian|Cambrian|||||||
37348|Teltawongee Group|65381|5|Briefly described|p689 Fig.2|Middle Cambrian|Early Cambrian|Variation on Teltawongee beds.||||||
37348|Teltawongee Group|66623|1|Redefined|p17, pp30-49, p348.|Early Cambrian|Early Cambrian|Formerly part of Packsaddle Series (Andrews 1922), Wonominta beds (Warris 1967) and Complex (Scheibner 1972), part of Teltawongee beds (Mills 1992). Approximate equivalents with Kanmantoo Group. Low hills and rises. Geophysical properties described.|504.5 +/- 2.6 Ma (Black 2006).||Includes Nundora, Copper Mine Range, Wonnaminta, Bunker Creek and Depot Glen Formations.|Overlies Kara Formation of Grey Range Group. Intruded by Bittles Tank Volcanics. Capped by Cordillo Silcrete.|Mainly monotonous sequence of dirty turbiditic, metamorphosed, graded-bedded sandstones of uniform grainsize range and composition, and siltstone; presence of detrital muscovite flakes is characteristic.|
37348|Teltawongee Group|66917|5|Briefly described|Map legend|Cambrian|Cambrian|Does not crop out in the map area.|||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|66918|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|66921|6|Mentioned|Map legend|||Does not outcrop in map area. Position in cross-section is based on geological interpretation and geophysical modelling.|||Includes Depot Glen Formation.|||
37348|Teltawongee Group|66922|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Depot Glen Formation.||Well cleaved and folded dark grey to buff-brown fine- to medium-grained turbiditic silty and muddy sandstones, several metres thick, with detrital muscovite to 3 mm; minor grey, green and maroon slate units; metamorphosed to greenschist facies.|
37348|Teltawongee Group|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Narrow, single and paired moderately-magnetic trends which are continuous over many kilometres; mainly occur within Teltawongee Group formations further south (in the Cotham Lake map sheet area).||||||
37348|Teltawongee Group|67105|5|Briefly described|p653-655, 659, 661, 663, 665|Early Cambrian|Early Cambrian|Kayrunnera Zone, Koonenberry Belt.|||Nundora, Wonnaminta, Bunker Creek, Copper Mine Range, Depot Glen Formations.||Metasedimentary rocks; an extensive package of turbiditic sandstones and siltstones.|
37348|Teltawongee Group|67207|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Depot Glen Formation.|Overlies Grey Range Group. Is overlain by Ponto Group.|Well cleaved and folded dark grey to buff-brown, fine- to medium-grained turbiditic silty and muddy sandstones, several metres thick; minor grey, green slate and maroon slate units; regionally metamorphosed to greenschist facies.|
37348|Teltawongee Group|67208|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Wonnaminta, Depot Glen and Bunker Creek Formations.||Well cleaved and folded, dark grey to buff-brown, fine- to medium-grained turbiditic silty and muddy sandstones, several metres thick, with detrital muscovite to 3 mm; minor grey, green and maroon slate units; greenschist facies.|
37348|Teltawongee Group|67209|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Depot Glen Formation.|||
37348|Teltawongee Group|67210|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Bunker Creek Formation.|||
37348|Teltawongee Group|67211|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Bunker Creek Formation.||Well cleaved and folded dark grey to buff-brown, fine- to medium-grained, turbiditic silty and muddy sandstones, several metres thick, with detrital muscovite to 3 mm; minor grey, green and maroon slate units; metamorphosed to greenschist facies.|
37348|Teltawongee Group|67322|4|Described|p3 Fig.1, p10-13; Fig.5|Cambrian|Cambrian|Koonenberry Belt. Defined by Mills, in Greenfield et al. (2010); previously Teltawongee Beds (Mills, 1992). Occurs in the Wonnaminta and Kayrunnera areas.|||Wonnaminta, Nundora, Bunker Creek, Depot Glen and Copper Mine Range Formations.|Intruded by the Bittles Tank Volcanics.|Consists of weakly metamorphosed graded bedded turbiditic sandstones.|22-FEB-18
37348|Teltawongee Group|68823|6|Mentioned|p376 Fig.3|Cambrian|Cambrian|Separated from Warratta Group by Olepoloko Fault. Mis-spelt as Teltawangee on p400.||||||
37348|Teltawongee Group|69001|6|Mentioned|p2 Fig.1B|Cambrian|Cambrian||||Includes the Depot Glen Formation.|||
37348|Teltawongee Group|69002|6|Mentioned|Map 1b, Legend|Cambrian|Cambrian|Comprises a broad area of low magnetic intensity.|||||Metasediments.|
37348|Teltawongee Group|69042|5|Briefly described|map legends|Cambrian|Cambrian|ETG. Delamerian Orogen. Broad area of low magnetic intensity. Metasediments.||||||
37348|Teltawongee Group|69043|5|Briefly described|p4, p11, p100-101, p104|||NE of the Koonenberry Fault. Deeper-water sedimentary rocks.|||Depot Glen Formation.|||
37348|Teltawongee Group|69541|5|Briefly described|p645 Fig.1(b)|Cambrian|Cambrian||515 Ma.|||||
37348|Teltawongee Group|69961|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Wonnaminta, Depot Glen and Bunker Creek Formations.||Undifferentiated well-cleaved and folded dark grey to buff-brown, fine- to medium-grained turbiditic silty and muddy sandstones, with detrital muscovite to 3mm; minor grey, green and maroon slate units; regionally metamorphosed to greenschist facies.|
37348|Teltawongee Group|70037|6|Mentioned|p11|||||||||
37348|Teltawongee Group|70210|6|Mentioned|p1|||Koonenberry-Tibooburra district.|||Depot Glen beds.|||
37348|Teltawongee Group|70602|6|Mentioned|p75|Cambrian|Cambrian|||||||
37348|Teltawongee Group|70648|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Copper Mine Range Formation, Bunker Creek Formation, Nundora Formation, Wonnaminta Formation.|||
37348|Teltawongee Group|70650|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|70651|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Wonnaminta Formation.|||
37348|Teltawongee Group|70744|5|Briefly described|p945|Middle Cambrian|Early Cambrian|Koonenberry Belt. The NE part of this unit is interpreted as a subduction complex.|||||Widespread quartzose turbidites.|
37348|Teltawongee Group|70749|6|Mentioned|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.||||||
37348|Teltawongee Group|70838|4|Described|p266, p268-272, p274-278, p280-281|Early Cambrian|Early Cambrian|Koonenberry Belt. Coeval with Ponto Group. Texturally immature: possible tectonic settings discussed (convergent margin preferred). The maximum depositional age is poorly defined from rare trace fossils. Minimum age from intrusion. Deformed during the Delamerian Orogeny (c.500 Ma). Detrital zircon analyses.|>515 +/- 2.7 Ma (Black, 2007).||Bunker Creek, Depot Glen, Wonnaminta and Nundora Formations.|Is faulted against Grey Range Group. Is intruded by Williams Creek Granite. Is overlain unconformably by Kayrunnera Group.|Monotonous packages of poorly sorted sandstone, siltstone and mudstone. Ubiquitous large (<5mm) detrital white mica grains.|
37348|Teltawongee Group|71262|5|Briefly described|p3, p5 Fig 2, p8 Fig 5, p9, p12|Cambrian|Cambrian||||Includes Depot Glen Formation and Bunker Creek Formation|||
37348|Teltawongee Group|71263|6|Mentioned|p18 Fig 2|Cambrian|Cambrian|||||||
37348|Teltawongee Group|71284|5|Briefly described|p487|||Milparinka area, Koonenberry Belt.|||||Includes felsic tuff horizons.|
37348|Teltawongee Group|71415|5|Briefly described|p11,15|Cambrian|Cambrian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Sedimentary sequence related to c. 510 Ma volcanics of the Mount Wright Arc. Underwent deformation and greenschist facies metamorphism during c. 500 Ma Delamarian Orogeny.||||Overlies the Grey Range Group.||19-AUG-19
37348|Teltawongee Group|71593|5|Briefly described|p188|||Koonenberry Province.||||Overlain by the Mount Wright Volcanics. Intruded by the Williams Peak Granite.|Turbiditic sedimentary rocks.|
37348|Teltawongee Group|71860|6|Mentioned|p6|Cambrian|Cambrian|||||||
37348|Teltawongee Group|71965|5|Briefly described|p894,896,901,913|Cambrian|Cambrian|Geological province: Delamerian Orogen. Turbidite deposition to the east, closer to the Thomson Orogen boundary; separated by Olepoloko Fault. Contemporaneous with Mount Wright continental magmatic arc development, and associated c. 510 Ma Gnalta Group and Ponto Group volcanism.||||||
37348|Teltawongee Group|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Delamarian Orogen.||||||
37348|Teltawongee Group|72522|4|Described|p3, p119, p125, p131.|Middle Cambrian|Early Cambrian||||Includes Depot Glen Formation.|Unconformably overlain by Easter Monday Formation. Intruded by Wertago Volcanics.||
37348|Teltawongee Group|72951|6|Mentioned|p1010|||Delamarian Orogen. Koonenberry Belt.||||||
37348|Teltawongee Group|73059|5|Briefly described|p1061|||Considered to be the subduction complex equivalent to the convergent margin arc and forearc deposits represented by the Mount Wright Volcanics. Variation in detrital zircon ages in this unit's constituents indicates their variety of provenances prior to the Delamerian Orogeny.|525-505 Ma.||Nundora, Copper Mine Range Formations.||Deep-marine turbidite succession.|
37348|Teltawongee Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Well-cleaved and folded dark-grey to buff-brown fine- to medium-grained turbiditic silty and muddy sandstones; minor grey, green and maroon slate units; regionally metamorphosed to greenschist facies.|09-DEC-21
37348|Teltawongee Group|73177|5|Briefly described|p1097-1100, 1109 Fig.13(a), 1113|Early Cambrian|Early Cambrian|See also p1114-1115 Figs.16-17. Northern Delamerian Orogen. Has many similarities to the Warratta Group.|||Bunker Creek Formation.|Is overlain by Warratta Group. Is intruded by Williams Peak Granite.||
22967|Temora Volcanics|22638|4|Described|p23|Silurian||||||||
22967|Temora Volcanics|22857|4|Described|p418 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|Lavas and pillow lavas, tuffaceous rocks including lapilli tuffs; andesite, trachyandesite, latite, basaltic andesite and associated volcaniclastic arenite, siltstone and conglomerate.||||||
22967|Temora Volcanics|23309|6|Mentioned|p390|||||||||
22967|Temora Volcanics|24233|5|Briefly described|p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
22967|Temora Volcanics|44093|5|Briefly described|p180 App. 1|Ordovician|Ordovician|Of the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
22967|Temora Volcanics|44192|5|Briefly described|Map Legend||Bolindian|||||||
22967|Temora Volcanics|44936|5|Briefly described|Map Legend||Ordovician|||||||
22967|Temora Volcanics|50191|6|Mentioned|p5, 16 Fig. 4|Silurian|Ordovician|||||||
22967|Temora Volcanics|63278|6|Mentioned|p145 Fig. 1, p149|||Geological Province: Junee-Narromine Volcanic Belt, LFB. Consists of lavas and volcaniclastis rocks, siltstone, sandstone, conglomerate (Warren et al. 1995).||||||07-FEB-11
22967|Temora Volcanics|67322|6|Mentioned|p23|Silurian|Silurian|Defined and Ordovician age assigned by Warren et al. (1995). Contain sparse fossils indicating a Silurian age.|||||Shoshonitic.|
22967|Temora Volcanics|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
22967|Temora Volcanics|72082|1|Redefined|p4, p24-31|Middle Devonian|Silurian|Name derived from the township of Temora. Originally shown as an unnamed diorite body in Fitzpatrick (1976). Warren et al. (1995), who gave no type locality; generally poorly exposed. Herein designated as a road cutting on Loftus Street in Temora at Lat. 34degrees 26'37"S, Long. 147degrees 32'41"E. An easily accessible reference section is given on the eastern side of Mother Shipton Hill. Thickness unknown. Forms a NNW-trending elongate belt through E Temora. Geochemistry and fossil assemblage are described. Fossils are basis for age. Bedding vertical or dipping steeply to W. Age range from corals. Marine nearshore to subaerial deposits with input from volcanic islands. Hosted many historical gold mines.||||Is possibly overlain unconformably by Combaning Formation. Is intruded by (and ?co-magmatic with) Mother Shipton Monzodiorite.|Lavas: andesite, trachyandesite, latite, basaltic andesite; associated volcaniclastic sandstone, siltstone, conglomerate; and lapilli tuff. Several historical rock types that are no longer available (due to housing expansion) are decribed in detail.|25-MAR-20
22967|Temora Volcanics|72495|5|Briefly described|p218, 227, p234, p236|||Described by Warren et al, 1995. Crops out as two belts, partly intruded and overlain by younger rocks with a length of 46km and combined width of <6km.||||Faulted against the Wagga Group.|Lavas (basaltic andesite, andesite and trachyandesite) and volcaniclastic rocks including siltstone, sandstone and conglomerate in addition to lapilli tuff.|
22967|Temora Volcanics|72528|6|Mentioned|p32.|||Part of the Macquarie Igneous Province.||||||
27908|Temperance Formation|22857|4|Described|p420 App. 1 Tb. A1.5|Ordovician|Ordovician|Of the Kiandra Group. Interbedded basaltic tuff, chert, feldspathic arenite; minor agglomerate; contains radiolaria. Max. thickness: 5km.||||||
27908|Temperance Formation|22968|5|Briefly described|P104|||Basal Formation of the Kiandra Group, overlying unit is Nine Mile Volcanics||||||
27908|Temperance Formation|24551|5|Briefly described|p106|||||||||
27908|Temperance Formation|36443|5|Briefly described|map legend|Late Ordovician|Early Ordovician|Of Kiandra Group. Units of varying combinations of interbedded basaltic tuff, chert, feldspathic arenite, agglomerate, bedded chert, and tuff. Interfingers with Nine Mile Volcanics and Nungar Beds. Overlies Boltons Beds. BMR map codes: Otd, Otc, Ott, Otb||||||
27908|Temperance Formation|40136|5|Briefly described|p41|||See also P26||||||
27908|Temperance Formation|45147|2|Defined|M21|late Gisbornian|early Gisbornian|Late Darriwilian to Late ? Gisbornian||||||
27908|Temperance Formation|63278|4|Described|p157|Gisbornian|Darriwilian |Of Kiandra Gp. Overlain by Nine Mile Volcanics. Geol Prov: Kiandra Volcanic Belt, LFB. Interbedded volcanic sandstone, siltstone and cherts. Part of the formation is mid-Darriwilian to early Gisbornian in age due to conodonts present.||||||07-FEB-11
27908|Temperance Formation|63290|6|Mentioned|p394 Tb. 1|Gisbornian|Darriwilian|Geological Province: Kiandra Volcanic Belt.||||||
27908|Temperance Formation|67322|4|Described|p26; Fig.5|Late Ordovician|Late Ordovician|Defined by Owen and Wyborn (1979). Contains conodonts of late Darriwilian age. Occurs in the Kiandra Volcanic Belt.||Of the Kiandra Group.||Overlain by the Nine Mile Volcanics. Overlies Blueys Creek Formation.|Bedded chert sequence with thin mafic volcaniclastic layers becoming progressively more dominant up section.|22-FEB-18
27584|Tenandra Formation|22857|5|Briefly described|p458 App.1, Tb.A1.6|Silurian|Silurian|Of the Cudal Group. Shale, siliceous arenite, coarse quartzofeldspathic arenite, minor laminated chert. Max. thickness: >370m. Geological Province: Cowra Trough.||||||
27584|Tenandra Formation|23214|3|Fully described|p113|Ludlow|Wenlock|Reinstated into the Cudal Group. 370m thick at type section is thought to be a minimum thickness. Absence of fossils suggest deep marine deposition environment.||||||
27584|Tenandra Formation|31852|6|Mentioned|p718|||U.Sil.-L.Dev. See also Fig.4.||||||
27584|Tenandra Formation|33006|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27584|Tenandra Formation|33282|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27584|Tenandra Formation|33285|6|Mentioned|p12|||||||||
27584|Tenandra Formation|34404|6|Mentioned|Fig.3.3b|||||||||
27584|Tenandra Formation|34405|6|Mentioned|p122|||||||||
27584|Tenandra Formation|34406|6|Mentioned|p221|||||||||
27584|Tenandra Formation|37727|4|Described|p88|||||||||
27584|Tenandra Formation|39655|6|Mentioned|Plate 1|||||||||
27584|Tenandra Formation|40328|4|Described|p122|||||||||
27584|Tenandra Formation|43461|14|Not recorded|Table p621||Ludlovian|||||||
27584|Tenandra Formation|43515|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
27584|Tenandra Formation|43516|14|Not recorded|Map Legend||Late Silurian|||||||
27584|Tenandra Formation|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of shale, siliceous sandstone, coarse quartzo-feldspathic sandstone; minor laminated chert.||||||17-JUL-08
27584|Tenandra Formation|43782|5|Briefly described|Map Legend|Ludlow|Wenlock|Of Cudal Group.||||||17-JUL-08
27584|Tenandra Formation|70297|5|Briefly described|map legend|Silurian|Silurian|Shown as Tenandra Fm.||Cudal Group||||
32507|Tenterfield mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
77620|Terimbone Monzogranite|69639|4|Described|p1, p5, p8, p32-p36|Lopingian|Lopingian|New England Orogen. SHRIMP age is interpreted as a magmatic crystallisation date. Sample locality, petrography, and geochronology is described. I-type geochemistry. See also p68, p95, p133, p219-p220, p236.|253.1 +/- 1.5 Ma (SHRIMP U-Pb)|Wards Mistake Suite||Intruded by the Mole Granite.|Medium- to coarse-grained, equigranular monzogranite.|
77620|Terimbone Monzogranite|70217|5|Briefly described|p73 tbl 14.1, p75|Changhsingian|Wuchiapingian|New England Orogen. Age derived from Chisholm et al, 2014b. |253.1 +/- 1.5 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
77620|Terimbone Monzogranite|71628|4|Described|p8: 4, 89-91; p19-111|||New name (this study), after the local Terimbone Tableland; Terembone Granodiorite, reserved in the ASUD by Blevin, appears to be a mis-spelling. Forms at least two roof pendants within the Mole Leucogranite ~3km ENE of Torrington. Very limited geochemistry is briefly described. Spatially associated with Sn and As mineralisation, likely sourced from Mole Leucogranite.|253.1 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Wards Mistake Suite.||Is enclosed by Mole Leucogranite.|Medium- to coarse-grained, broadly equigranular, biotite-(hornblende) monzogranite.|
36362|Termeil Complex|23544|5|Briefly described|p372|||Age: 245+/-6Ma K-Ar whole rock (Facer and Carr, 1979).||||||
36362|Termeil Complex|68822|6|Mentioned|p339|Ladinian|Anisian|Southern Sydney Basin.|ca. 241 +/- 4 Ma|||||
36362|Termeil Complex|73197|6|Mentioned|p475 Fig.6, p478|Lopingian|Guadalupian|Attributed to the Currarong Arc.|||||Mafic intrusives.|
36362|Termeil Complex|73421|4|Described|p1, p2 Fig.1, p5-7, p10-11, p14-17|Kungurian|Kungurian|Sydney Basin, southern. Exposed in a coastal strip between Merry Beach and Termeil Point. Contacts with surrounding rocks are obscurred. Northern contact appears concordant with overlying Snapper Point Formation. Mineralogy indicates an oxidised, hydrous melt. Undated monzo-diorite intrusion that is syndepositional with the Snapper Point Formation at Snake Bay is interpreted as a continuation of the Termeil Complex. Location in text includes p12 Fig.7. Termeil monzo-diorite used p14 Tb.2|278.9+/-3.7 Ma U-Pb zircon crystallisation age|||Intrudes Snapper Point Formation|Mafic monzonitic intrusion, dominant lithology of coarse-grained monzo-diorite, cut by irregular pegmatite veins and patches. Relationship between variants is diverse. Locally contains distinct spidery felsic residual melt segregations.|
82495|Terrible Vale Porphyritic Microgranodiorite|71628|4|Described|p7-40; p8: 50-51, 61, 64-70, 72; p19-55|||New name, after a local homestead. Includes the former Terrible Vale Porphyritic Microtonalite (Flood, 1971), Harnham Grove Porphyritic Microtonalite and Salisbury Waters Porphyrite (Binns et al., 1967). Comprises two masses c.12km S of Uralla. Crops out as small tors and rounded boulders. Geochemistry described; similar to Uralla Granodiorite. RELATED UNITS (continued): Is also intruded by Wilhelmshohe Tonalite and possibly Kentucky Quartz Diorite.|247.7 Ma and 250.2 Ma (Rb-Sr; Shaw, 1994).|Uralla Suite.||Intrudes Sandon beds, Wandsworth Volcanic Group and Glenburnie Leucomonzogranite. Is intruded by Walcha Road Monzogranite, Uralla Granodiorite (gradationally). See COMMENTS for more.|A texturally heterogeneous sequence ranging from two-pyroxene dacite-tuffasite and fragmental dacite to fine-grained porphyritic and medium-grained equigranular quartz-poor granodiorite - quartz monzodiorite, possibly with minor monzogranite. I-type.|
28255|Terrigal Formation|22745|6|Mentioned|Fig3,p128||Scythian|Sydney Basin.||||||
28255|Terrigal Formation|22749|6|Mentioned|p 194|||||||||
28255|Terrigal Formation|22857|4|Described|p520 App.1 Tb.A1.9|Early Triassic|Late Permian|Of the Narrabeen Group. Interbedded fine to medium-grained sandstone and siltstone, minor claystone. Max. thickness: 330m. Geological Province: Sydney Basin. See also p524 App.1 Tb.A1.9.||||||
28255|Terrigal Formation|22969|4|Described|Fig 4.1a|Middle Triassic|Early Triassic|||||||
28255|Terrigal Formation|23256|6|Mentioned|p50|||||||||
28255|Terrigal Formation|24117|5|Briefly described|p49|||Of Narrabeen Group. Geological Basin: Sydney Basin.||||||
28255|Terrigal Formation|30007|6|Mentioned|Fig.1|||||||||
28255|Terrigal Formation|31297|6|Mentioned|p4|||||||||
28255|Terrigal Formation|32537|6|Mentioned|p11|||||||||
28255|Terrigal Formation|33685|6|Mentioned|p395|||||||||
28255|Terrigal Formation|35488|6|Mentioned|p73|||||||||
28255|Terrigal Formation|35502|6|Mentioned|Table 1|||||||||
28255|Terrigal Formation|35833|6|Mentioned|p35|||||||||
28255|Terrigal Formation|36042|6|Mentioned|Fig.22|||||||||
28255|Terrigal Formation|36616|6|Mentioned|p4|||||||||
28255|Terrigal Formation|39287|6|Mentioned|Fig. 2.18|||||||||
28255|Terrigal Formation|39293|6|Mentioned|p152|||||||||
28255|Terrigal Formation|39295|3|Fully described|p171|||See also PP172-176||||||
28255|Terrigal Formation|39306|6|Mentioned|p414|||See also P415,422||||||
28255|Terrigal Formation|39308|5|Briefly described|p454|||See also Figs 23.3, 23.12 & P458||||||
28255|Terrigal Formation|40602|3|Fully described|p15|||||||||
28255|Terrigal Formation|40603|6|Mentioned|p5|||||||||
28255|Terrigal Formation|40625|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Early to Middle Triassic||||||
28255|Terrigal Formation|40629|6|Mentioned|p186|||||||||
28255|Terrigal Formation|40630|6|Mentioned|p174|||||||||
28255|Terrigal Formation|40653|6|Mentioned|p121|||||||||
28255|Terrigal Formation|41010|6|Mentioned|Table 1|||||||||
28255|Terrigal Formation|43072|6|Mentioned|p55|||||||||
28255|Terrigal Formation|43194|5|Briefly described|p131|Triassic|Triassic|Fluvio-deltaic deposits of the upper Narrabeen Group, Sydney Basin.||||||
28255|Terrigal Formation|43257|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
28255|Terrigal Formation|61315|5|Briefly described|Table SY1|MiddleTriassic|Middle Triassic|Of the Narrabeen Group. Geological Province: Sydney Basin||||||
28255|Terrigal Formation|66090|6|Mentioned|p24.|Early Triassic|Early Triassic|Sydney Basin. Contains Protohaploxypinus samoilovichii and Aratrisporites tenuispinosus Assemblages, similar to flora in the Laurieton Conglomerate, Lorne Basin.||||||
28255|Terrigal Formation|67663|5|Briefly described|p520 Tb.1, p522|Triassic|Triassic|||||Unconformably overlain by the Hawkesbury Sandstone.||
28255|Terrigal Formation|68003|6|Mentioned|p43.|Triassic|Triassic|||Unit in upper part of Narrabeen Group.||||
28255|Terrigal Formation|68004|6|Mentioned|p23 Table 1.|||Newcastle Coalfield.||Unit in Narrabeen Group.||||
28255|Terrigal Formation|70125|5|Briefly described|p386 Fig.1, p387-390, p392-393, p397-399|Middle Triassic|Early Triassic|See also p405. Origins and ages of sediments detailed. Fluvial flood-plain and channel-bar volcanolithic (dark) sediments in a foreland basin. Detrital zircons are dominated by 350-225 Ma ages of the New England Orogen. Appears on p397 as Terrigal (Gosford) Formation [it is a unit in the Gosford Subgroup].||||||
28255|Terrigal Formation|70647|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Sydney Basin.||Gosford Subgroup|||Interbedded laminite, shale and fine- to coarse-grained quartz- to quartz-lithic sandstone; minor red claystone.|
28255|Terrigal Formation|73264|6|Mentioned|p1402 Fig.23|||Shown as Terrigal Fm.||||||
28255|Terrigal Formation|73570|5|Briefly described|p914, p915 Fig.4, p916, p918-919|Middle Triassic|Middle Triassic|Sydney Basin. Marine-deltaic.||Narrabeen Group|||Includes sandstone.|
77376|Teston Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
73699|Tettenhall Intrusive Complex|63286|6|Mentioned|p304, 296, 297|Ordovician|Ordovician|Consists of gabbroic to monzonitic intrusions; dominantly equigranular.||||||07-FEB-11
29916|Tettenhall Monzodiorite|13139|5|Briefly described|p3 Fig. 2|||Geological Province: Lachlan Orogen.||||||
29916|Tettenhall Monzodiorite|22679|4|Described|p 36|Ordovician|Ordovician|Formerly Prince of Wales Diorite||||||
29916|Tettenhall Monzodiorite|23214|2|Defined|p88|Late Ordovician|Late Ordovician|Originally named Prince of Wales Diorite. Intrudes Weemalla Formation and fully encloses the Glendale Quartz Monzonite. Age 439 +/- 1Ma (Ar/Ar), 439 +/- 3Ma (Rb/Sr).||||||17-JUL-08
29916|Tettenhall Monzodiorite|23334|5|Briefly described|3 Fig.2|||||||||
29916|Tettenhall Monzodiorite|24398|5|Briefly described|p259 Fig. 2|Late Ordovician|Late Ordovician|Supersedes Prince of Wales Monzodiorite. Geological Province: Lachlan Fold Belt.||||||17-JUL-08
29916|Tettenhall Monzodiorite|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Consists of prophyritic and aphyric monzonite and diorite.||||||17-JUL-08
29916|Tettenhall Monzodiorite|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Porphyritic and aphyric monzonite and doirite.||||||17-JUL-08
29916|Tettenhall Monzodiorite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
29916|Tettenhall Monzodiorite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
25749|Thackaringa Group|6823|6|Mentioned|p203-205, 206, 233, 234, 236|Palaeoproterozoic|Palaeoproterozoic||ca >1690 Ma|Willyama Supergroup|Includes the Rasp Ridge Gneiss, Alma Gneiss.|Overlies the Thorndale Composite Gneiss, Clevedale Migmatite, Mulculca Formation, Ednas Gneiss and the Redan Gneiss.||26-MAR-22
25749|Thackaringa Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill Domain||||||
25749|Thackaringa Group|22575|6|Mentioned|p179 Fig.2|||In the Broken Hill Block.||||||16-JAN-07
25749|Thackaringa Group|22588|6|Mentioned|p85|||||||||
25749|Thackaringa Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
25749|Thackaringa Group|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|22720|6|Mentioned|p 168|||||||||
25749|Thackaringa Group|22771|5|Briefly described|p40,Table12.2p45,45|||||||||
25749|Thackaringa Group|22789|6|Mentioned|p50|||||||||
25749|Thackaringa Group|22857|4|Described|p40, p45 Tb.12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: 3000m. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
25749|Thackaringa Group|22884|5|Briefly described|p40 Fig. 1, p41, p43 Fig. 3||Statherian|Age of lower unit is 1699+/-10 Ma. Geological province: Broken Hill Domain.||||||26-MAR-09
25749|Thackaringa Group|22956|6|Mentioned|p147||Proterozoic|||||||
25749|Thackaringa Group|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|22960|6|Mentioned|p90,92||Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|22962|6|Mentioned|p74||Statherian|||||||
25749|Thackaringa Group|22963|5|Briefly described|p69||Paleoproterozoic|Broad correlation with the Fullarton River Group of the Mt Isa Maronan Supergroup.||||||07-NOV-08
25749|Thackaringa Group|22964|6|Mentioned|p56||Proterozoic|||||||
25749|Thackaringa Group|22965|6|Mentioned|p11,14,Fig1||Paleoproterozoic|Contains the Himalaya, Cues, Alders Tank and Lady Brassy Formations.||||||07-NOV-08
25749|Thackaringa Group|22966|5|Briefly described|p2,4||Proterozoic|||||||
25749|Thackaringa Group|22967|5|Briefly described|p25,6,39,41,2||Statherian|||||||
25749|Thackaringa Group|23025|5|Briefly described|p75-6|||||||||
25749|Thackaringa Group|23039|6|Mentioned|p166||Statherian|||||||
25749|Thackaringa Group|23160|6|Mentioned|fig1|||||||||
25749|Thackaringa Group|23223|5|Briefly described|p39|||Described in article as 'Thackaringa group - quartzofeldspathic suite (TG-QS)'. Of the Willyama Supergroup. In the Curnamona Province.||||||16-JAN-07
25749|Thackaringa Group|23248|6|Mentioned|p170, 179|||||||||
25749|Thackaringa Group|23346|6|Mentioned|48|||||||||
25749|Thackaringa Group|23347|6|Mentioned|p51 Tb. 1, p52|||Geological province: Broken Hill Domain. Presented only as Thackaringa in Table 1. Equivalent to parts of Wiperaminga Subgroup.||||||24-MAR-09
25749|Thackaringa Group|23390|6|Mentioned|p8|||||||||
25749|Thackaringa Group|23461|5|Briefly described|p202|||||||||
25749|Thackaringa Group|23912|6|Mentioned|p779|||||||||
25749|Thackaringa Group|24197|5|Briefly described|p29, p62|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Leucocratic, high in silica and usually albitic; includes lacustrine sedimentary rocks, felsic metavolcanic rocks, shallow granite sills and several varieties of iron formations. Age: ~1710Ma. Geol.Province: Broken Hill Domain.||||||07-FEB-11
25749|Thackaringa Group|24307|4|Described|p973|Proterozoic|Proterozoic|||||||
25749|Thackaringa Group|38969|4|Described|p204|||||||||
25749|Thackaringa Group|39662|1|Redefined|p414|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|39674|6|Mentioned|p204|||||||||
25749|Thackaringa Group|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|39849|6|Mentioned|p87|||||||||
25749|Thackaringa Group|39883|6|Mentioned|p382|||||||||
25749|Thackaringa Group|40290|6|Mentioned|p1|||||||||
25749|Thackaringa Group|40595|6|Mentioned|p78|||||||||
25749|Thackaringa Group|40822|6|Mentioned|Fig.2|||||||||
25749|Thackaringa Group|41093|4|Described|p251|||||||||
25749|Thackaringa Group|41145|5|Briefly described|p827|||||||||
25749|Thackaringa Group|41630|5|Briefly described|p6|||||||||
25749|Thackaringa Group|41633|6|Mentioned|p150|||||||||
25749|Thackaringa Group|41651|5|Briefly described|p190|||||||||
25749|Thackaringa Group|41652|5|Briefly described|p192|||||||||
25749|Thackaringa Group|42171|6|Mentioned|p142|||||||||
25749|Thackaringa Group|42181|6|Mentioned|Fig,1 P252|||||||||
25749|Thackaringa Group|42261|6|Mentioned|Fig 1 P530|||||||||
25749|Thackaringa Group|42286|6|Mentioned|p7|||||||||
25749|Thackaringa Group|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42537|3|Fully described|p8|||||||||
25749|Thackaringa Group|42595|6|Mentioned|Fig. 2 P5|||||||||
25749|Thackaringa Group|42720|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25749|Thackaringa Group|42813|6|Mentioned|p9|||||||||
25749|Thackaringa Group|42897|5|Briefly described|Fig.3, P321|||||||||
25749|Thackaringa Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
25749|Thackaringa Group|43052|6|Mentioned|p84|||||||||
25749|Thackaringa Group|43086|6|Mentioned|Fig.3|||||||||
25749|Thackaringa Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
25749|Thackaringa Group|43264|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43267|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43268|5|Briefly described|Map Legend||Paleoproterozoic|Within the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
25749|Thackaringa Group|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
25749|Thackaringa Group|43572|6|Mentioned|p5|||||||||
25749|Thackaringa Group|43583|5|Briefly described|Table 1, p2139|||||||||
25749|Thackaringa Group|43595|5|Briefly described|p355|||||||||
25749|Thackaringa Group|46598|4|Described|p303|||||||||
25749|Thackaringa Group|50045|4|Described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geol Prov: Broken Hill Block. Of  Willyama Supergroup. Conformably overlain by Broken Hill Group; underlain by Thorndale Composite Gneiss and Mulculca Formation. Age: c.1710 Ma. Includes 7 named units.||||||31-MAY-07
25749|Thackaringa Group|50606|5|Briefly described|p1.1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Intruded by Potosi Supersuite.||||||
25749|Thackaringa Group|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.  Interbedded psammite, pelite and quartz-albitite.  Conformably overlain by the Broken Hill Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
25749|Thackaringa Group|60485|5|Briefly described|p28 Fig. 2|||Geological Province: Broken Hill Domain.||||||03-MAR-05
25749|Thackaringa Group|61258|5|Briefly described|p399|Paleoproterozoic|Paleoproterozoic|Includes the Himalaya and Alma Formations. Geological Province: Broken Hill-Olary region.||||||07-NOV-08
25749|Thackaringa Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1700Ma. Geological Province: Broken Hill.||||||07-NOV-08
25749|Thackaringa Group|61605|5|Briefly described|p769|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Broken Hill domain.||||||07-NOV-08
25749|Thackaringa Group|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||18-MAY-06
25749|Thackaringa Group|61735|5|Briefly described|p635 Fig. 1, p636, 640|Paleoproterozoic|Paleoproterozoic|Oldest recognised part of the Willyama Supergroup. Age: 1730-1720Ma. See also p636 Fig. 2. Regional metamorphism 1595+/-6 Ma U/Pb SHRIMP.||||||04-JUN-15
25749|Thackaringa Group|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Contains Lady Brassey, Cues and Himalaya Formations, Geological province: Olary Domain.||||||
25749|Thackaringa Group|62373|5|Briefly described|p503|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Migmatised, quartz-feldspathic rocks and albite-quartz rocks. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
25749|Thackaringa Group|62473|5|Briefly described|p72|Paleoproterozoic|Paleoproterozoic|Age: 1710-1700ma. Geological province: Broken Hill Domain.||||||17-JUN-09
25749|Thackaringa Group|62535|5|Briefly described|p665, p667, p670, p672-674|Paleoproterozoic|Paleoproterozoic|Hosts Broken Hill-type base metal deposits.|c.1720 Ma.||Lady Brassey, Cues, Himalaya Formations.|||
25749|Thackaringa Group|62536|4|Described|p633, 635-638, 640, 642, 647, 653, 658|||Broken Hill area. A minimum age for the lower part of this unit is 1704 +/- 3 Ma. Contains various metal ores (listed).|1720 Ma (MDA).|Willyama Supergroup.|Himalaya, Cues, Alders Tank, Lady Brassey Formations; Alma Gneiss.|Overlies Thorndale Composite Gneiss. Is intruded by Alma Gneiss and Farmcote leucogneiss.||
25749|Thackaringa Group|62592|5|Briefly described|p14, p16, p16 Fig.2.2.|||Broken Hill Domain, Curnamona Province. This unit, representing a >10 m.y. gap, is missing from the Olary Domain.||Unit in Willyama Supergroup.|Includes Thorndale Composite, Redan and Ednas Gneisses; Clevedale Migmatite; Mulculca, Lady Brassey, Kyong, Alders Tank, Cues and Himalaya Formations.|Is intruded by Alma and Rasp Ridge Gneisses.||
25749|Thackaringa Group|62728|5|Briefly described|p25 Fig. 2|||Includes the Thackeringa Group metasediments. Geological Province: Curnamona Province.||||||07-FEB-11
25749|Thackaringa Group|62993|5|Briefly described|p35, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup|Includes Himalaya Formation, Cues Formation, Alders Tank Formation, Lady Brassey Formation|||19-DEC-21
25749|Thackaringa Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
25749|Thackaringa Group|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.|||Includes Himalaya Fm, Kyong Fm, Cues Fm, Alders Tank Fm, Lady Brassey Fm, Thorndale Composite Gneiss, Mulculca Fm, Clevedale Migmatite, Ednas Gneiss and Regan Gneiss.|||
25749|Thackaringa Group|63110|6|Mentioned|p1129 Fig. 8, p1131|||Comprises metasedimentary rocks with intrusive, shallow level granitoids.||||||
25749|Thackaringa Group|63186|5|Briefly described|p66, p67, p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Age: 1705Ma. Geological Province: Broken Hill Domain, Curnamona Province. Intruded by Rasp Ridge and Hores Gneisses. Lower section includes Cues Formation.||||||07-NOV-08
25749|Thackaringa Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metasediments, composite gneiss, albite-rich rocks, granitic gneiss, amphibolite, minor quartz-magnetite rocks and metasediments in Broken Hill Domain; equivalent metasediments in Olary Domain.||||||07-NOV-08
25749|Thackaringa Group|63519|5|Briefly described|p5, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Alma Gneiss, Lady Brassey, Alders Tank, Cues Formations and Himalaya Formations, and Rasp Ridge Gneiss. Albite rock. ||||||07-NOV-08
25749|Thackaringa Group|63866|5|Briefly described|p36, p38, p40|||Broken Hill Domain, Curnamona Province.|1705-1693 Ma||Includes the Lady Brassey Formation, Cues Formation and the Himalaya Formation.|||
25749|Thackaringa Group|64097|5|Briefly described|p302, p306|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Includes Alma Gneiss, Lady Brassey Fm.(both basal), Alders Tank,Cues and Himalaya Formations. Overlies Thorndale Composite Gneiss; underlies Broken Hill Group. Max. age: ca 1720Ma. Abundant albitised metasediment.||||||07-FEB-11
25749|Thackaringa Group|64250|6|Mentioned|p25 fig 10|||||Unit in Willyama Supergroup.||||
25749|Thackaringa Group|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the lower Willyama Supergroup. Includes Lady Brassey, Cues and Himalaya Fms. Migmatised quartzo-feldspathic rocks and albititeswith progressive increase in poelitic-trubiditic component up into the broken Hill Group above. Geol.Prov: Broken Hill Block.||||||07-FEB-11
25749|Thackaringa Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
25749|Thackaringa Group|64725|6|Mentioned|p58 Fig.2. |||||||||
25749|Thackaringa Group|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Overlain by Broken Hill Group. Geological province: Broken Hill Domain.||||||07-FEB-11
25749|Thackaringa Group|64742|5|Briefly described|p320 Fig.2, p328.|||Broken Hill Domain. Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Willyama Supergroup.|Includes Lady Brassey, Cues, and Himalaya Formations.|||29-MAR-12
25749|Thackaringa Group|64743|6|Mentioned|pp339-340, p344 Fig.5. |Paleoproterozoic|Paleoproterozoic|||Unit in Willyama Supergroup.||Is overlain by Broken Hill Group.||
25749|Thackaringa Group|64744|5|Briefly described|p353 Fig.4, p354. |Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Is intruded by Alma and Rasp Ridge Gneisses. Is overlain by Broken Hill Group.|Psammopelitic schists and gneisses.|
25749|Thackaringa Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Lady Brassey, Alders Tank, Cues and Himalaya Formations. Geological province: Broken Hill Domain.||||||07-FEB-11
25749|Thackaringa Group|65681|6|Mentioned|pp733-734,|Paleoproterozoic|Paleoproterozoic|||Unit in Willyama Supergroup.|Previously regarded as including Rasp Ridge Gneiss.|||16-MAY-13
25749|Thackaringa Group|65925|5|Briefly described|Appendix 2.||||Includes metavolcanics 1699+/-10 Ma. ||||Gneiss, quartz-feldspar-biotite, foliated; calc-albitite and quartz-plagioclase rich metasediment; metavolcanics 1699+/-10 Ma; ironstone; calc-silicate; minor Pb-Zn-Ag-Cu mineralisation; minor amphibolite.|
25749|Thackaringa Group|66302|5|Briefly described|p35, p36 Fig.9, p37, p38, p39, p40|Statherian|Statherian|Olary and Broken Hill Domains, Curnamona Province.|1705-1693 Ma (Conor, 2006)|Willyama Supergroup|Includes the Thorndale Composite Gneiss, Clevedale Migmatite, Lady Brassey Formation, Alders Tank Formation, Cues Formation and Himalaya Formation.|Overlain by the Broken Hill Group. Intruded by the Silver City Suite.||
25749|Thackaringa Group|66857|5|Briefly described|p971, p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Thought to have equivalents in the (informally-named) Quartzo-feldspathic Suite of the Olary Domain.|c.1700 Ma (Ashley et al. 1997).|Unit in Willyama Supergroup.||Overlies Thorndale Composite Gneiss. Is overlain by Broken Hill Group.||
25749|Thackaringa Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Broken Hill Domain, Curnamona Province. Deposited during intra-continental extension.|||Himalaya, Cues, Lady Brassey Formations; Thorndale Composite Gneiss.|Is overlain by Broken Hill Group.||
25749|Thackaringa Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
25749|Thackaringa Group|68126|5|Briefly described|p6, p26, p29-30|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|c.1710-1700 Ma (maximum depositional age).|Willyama Supergroup.||Is overlain by Broken Hill Group.||
25749|Thackaringa Group|69999|5|Briefly described|p3, p9 Photo 11, p14, p16-18, p20|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Basal, early-rift fluviatile to shallow marine sedimentation. Orthopyroxene -bearing rather than garnet-bearing, unlike Broken Hill Group: discussed.||||||
25749|Thackaringa Group|70000|5|Briefly described|p31, p33-37|Statherian|Statherian|||Unit in Willyama Supergroup.|Includes Lady Brassey, Cues and Himalaya Formations.|Is overlain conformably by Broken Hill Group.|Contains a sequence of variably albitic, psammite-dominated metasedimentary rocks.|
25749|Thackaringa Group|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.||Overlies Thorndale Composite Gneiss and Mulculca Formation. Is overlain by Broken Hill Group.|Characterised by a wide variety of quartzo-feldspathic lithologies, including quartz-feldspar-biotite gneisses and leucocratic plagioclase-quartz rocks, as well as composite gneiss, lesser metasediment, and sporadic to abundant basic gneiss bodies.|
25749|Thackaringa Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Lady Brassey, Cues and Himalaya Formations.|Is overlain by Broken Hill Group.|Sodic plagioclase-quartz rocks at top and base, with intervening metasedimentary rocks and composite gneiss; intruded by granitic and basic gneiss.|
25749|Thackaringa Group|70405|6|Mentioned|p15, p43 Table 3, p92|Mesoproterozoic|Paleoproterozoic|Correlated with Curnamona group previously (now known to be incorrect).|1700 Ma|Wilyama Supergroup|Includes Cues Formation, Himalaya Formation, Alders Tank Formation, Lady Brassey Formation||Low magnetic intensity.|
25749|Thackaringa Group|70657|4|Described|p6 Fig.1, p10 Fig.4, p11 Fig.5, p12|Statherian|Statherian|See also p13 Fig.6, p15. Curnamona Province; Mulyungarie, Broken Hill Domains. Shown as Thackaringa Group + Thorndale Composite Gneiss + Clevedale Migmatite in Fig.4.|~1705-1700 Ma|Lower Willyama Supergroup|Includes Thorndale Composite Gneiss; Lady Brassey, Alders Tank, Cues, Himalaya Formations.|Overlies Redan and Farmcote Gneisses (Rantyga Group). Underlies Allendale Metasediments (Broken Hill Group). Intruded by Silver City Suite.||
25749|Thackaringa Group|70658|5|Briefly described|p2, 15-|Paleoproterozoic|Paleoproterozoic|Broken Hill region.|1705-1700 Ma.|Willyama Supergroup.|Lady Brassey, Alders Tank, Cues, Himalaya Formations.|Associated with Silver City Suite.||
25749|Thackaringa Group|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
25749|Thackaringa Group|72004|6|Mentioned|p84|||Broken Hill region. May have been volcanics, altered in an alkaline environment, most likely an evaporitic setting.|||Includes Himalaya Formation.|Overlain by Willyama Supergroup.||
25749|Thackaringa Group|72435|6|Mentioned|p715|||||||||
25749|Thackaringa Group|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain.  Shown only on p2 Fig.2 and p8 Fig.6.||Willyama Supergroup||||
25749|Thackaringa Group|72461|4|Described|p5-6, p13, p16|||Some of the oldest sedimentary rocks in the  Curnamona Craton (Broken Hill Block). Hosts Great Eastern-type Copper Cobalt mineralisation.||Willyama Supergroup|Includes the Himalaya Formation, Lady Brassey Formation, Cues Formation.|Overlain by the Broken Hill Group.||
25749|Thackaringa Group|73021|5|Briefly described|p224||||~1710 Ma to ~1704 +/- 3 Ma.|Willyama Supergroup.|Cues Formation.|||
25749|Thackaringa Group|73243|6|Mentioned|p52 Fig.1, p53 Fig.2, p59, p65-66, p76|Statherian|Statherian|Broken Hill block-Euriowie block. Amphibolite bodies are mostly concordant or near-concordant with bedding, interpreted as sills emplaced during or immediately after deposition of the Broken Hill Group. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.|~1705-1700 Ma|Willyama Supergroup|Cues Formation, Lady Brassey Formation||Contains amphibolite sills.|
25749|Thackaringa Group|73308|6|Mentioned|p606-607||||c.1705-1700 Ma.|Willyama Supergroup.||||
25749|Thackaringa Group|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Willyama Supergroup, lower|Lady Brassey Formation, Alders Tank Formation, Cues Formation, Himalaya Formation|||
25749|Thackaringa Group|73482|5|Briefly described|p422 Fig.3, p425-426, p430, p432-433|||Hosts pegmatitic masses. See also p423.||Willyama Supergroup|Lady Brassey Group, Cues Formation, Himalaya Formation||Metasediments.|
25749|Thackaringa Group|73512|5|Briefly described|p2-7|Statherian|Statherian|Curnamona Province, Broken Hill Block. Fluviatile to shallow marine successions. Monozite U-Pb SHRIMP age of 1636.8 +/- 4.4 Ma reflects an amphibolite-facies pre-Olarian metamorphic event.||Willyama Supergroup|Cues Formation|Overlain by Broken Hill Group.|Includes metapelites.|
25749|Thackaringa Group|73524|5|Briefly described|p2, p5 Fig.3|||Rift-phase metasediments.||lower Willyama Supergroup|Cues Formation, Lady Brassey Formation, Thorndale Composite Gneiss, Clevedale Migmatite|||16-FEB-23
25749|Thackaringa Group|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p830, p838|||||Willyama Supergroup|Lady Brassey Formation, Cues Formation, Himalaya Formation|Overlies Thorndale Composite Gneiss, underlies Broken Hill Formation, Allendale Metasediments||
76047|Thalaka granite|66934|5|Briefly described|Map legend|Early Devonian|Early Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Thalaka Granite Suite.|||Interpreted S-type granite.|
76047|Thalaka granite|70718|5|Briefly described|p59-61, p64, 115, 119, 120|Wenlock|Ordovician|Name derived from the Thalaka locality. No outcrop. Relatively low magnetic susceptibility. Geophysically similar to the Cunninyeuk Granite. Interpreted as S-type granite.||Thalaka granite suite||Intruded by the Windouran Swamp granodiorite.||30-MAY-19
80440|Thalaka granite suite|70718|5|Briefly described|p59-61, p64, 71, 95, 119|||Name derived from the Thalaka locality. No known outcrop or intersecting drillcore and interpreted entirely from geophysics. Magnetic signature suggests S-type granites.|||Includes the Thalaka granite and Yadabal Lagoon granite.|||30-MAY-19
22979|Thanowring Granite|22638|4|Described|p73||Late Devonian|||||||
22979|Thanowring Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
67910|The Basin Monzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca. 245 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
67910|The Basin Monzogranite|71628|4|Described|p8: 3, 40-43, 100-101; p19-142|||See also . DMR NAND04 Nandewar Geology Integration and Upgrade project; Li et al. (2012); after unpublished work by Chappell and Bryant (1994). Originally The Basin Adamellite (Chesnut et al., 1973). Named after ""The Basin"" homestead. Occurs 20km ESE of Bundarra and 45km W of Guyra. It is ~10km long and 100m to 4km wide. Forms topographic lows; crops out as tors and pavements, often deeply weathered. Geochemistry described; has many similarities with Myanbah Leucosyenogranite. Hosts minor Sb (As, W) and Mo mineralisation.|245.2 Ma (Rb-Sr biotite: Shaw, 1994).|Mount Duval Suite.||Intrudes Sandon beds.|Medium to coarse biotite-hornblende-(pyroxene) monzogranite; minor porphyritic and typically leucocratic finer-grained variants. Characteristically red-orange from iron-stained weathering. Small (2-30cm) enclaves are ubiquitous. Rare aplitic dykes.|
77628|The Brothers Suite|71628|4|Described|p1-2; p17: 1-2, 54, 71-87, 100, 103|Late Triassic|Late Triassic|See also p19-156. Blevin (year not given). Includes the Laurieton Granites group of Chappell and Bryant (1994 unpublished), and appears to have replaced The Brothers Granitoids of Raymond (year not given). Laurieton area. A series of high-level/subvolcanic laccoliths, plugs, sills and dykes. Geochemistry described. Appears also as the Brothers Suite.|213-212 Ma (SHRIMP: Cross and Blevin, 2013).|Coastal Granite Association.|Middle Brother, North Brother, Lorne Forest, Juhle Mountain, Hannam Vale, Cataract Creek, Granodiorites; South Brother Microgranite.||Variable composition: granodiorite to monzogranite, diorite to quartz monzonite, microgranite, and locally graphic leucogranite and granophyre. Invariably porphyritic. Spatially associated with rhyolites. A-type granites.|
40755|The Calpe Ignimbrite Member|50613|5|Briefly described|p209, p219 Fig. 9|Namurian|Namurian|Defined as Calpe Ignimbrite Member in Appendix 1 (p227) but is named after the property The Calpe.  Names used interchangeably in this study.||||||
24023|The Gap Sandstone|38614|6|Mentioned|p14|||||||||
24023|The Gap Sandstone|40806|2|Defined|p158|Permian|Permian|Prob. Permian||||||
32496|The Pinnacle Dolerite|22638|3|Fully described|p79||Late Devonian|New name.||||||
32496|The Pinnacle Dolerite|44192|5|Briefly described|Map Legend|Devonian|Devonian|||||||
82507|The Ram Swamp Monzogranite|71628|5|Briefly described|p15: 35, 58, 65, 77-78, 82, 116; p19-20|||New name, after a local aqueous feature (several kilometres SW of Boonoo Boonoo). The unit was first delineated by Thomson (1973, 1976). Forms an irregular branching mass c.8 x 5 km. Very limited geochemistry is described; is geochemically assigned to the Jenners Suite.||Stanthorpe Complex.||Abuts (is entirely enclosed by) Mount Lindesay and Boonoo Monzogranites, Mount Norman Leucomonzogranite and Ruby Creek Leucogranite.|Pale pink to pink, or pale grey (locally), medium-grained, porphyritic biotite-(hornblende) monzogranite; rapakivi textures are locally well-developed. I-type.|
82684|The Ridge Monzogranite|71628|5|Briefly described|p11: 38; p15: 57-58, 69; p16: 8, 19-20|||See also p16: 162-164. New name, after unpublished work by Passmore (1998) who named it Ridge Monzogranite. Previously mapped as part of Stanthorpe Monzogranite. Named after the property ""The Ridge"||The Ridge Suite.||Is intruded by Thomkins Gully Monzogranite Phase, and Undercliffe Falls Monzogranite. Abuts Mount Lindesay Monzogranite and Five Mile Creek Syenogranite Phase. See COMMENTS for more.|Medium-grained, seriate, K-feldspar-rich, biotite monzogranite. I-type.|
24518|The Secrets Andesite|39656|4|Described|M13|||||||||
24518|The Secrets Andesite|39663|6|Mentioned|Table 4|||||||||
37917|The Tops Rhyolite Member|50613|6|Mentioned|p215|Namurian|Namurian|Age: 315Ma. Of Lark Hill Formation.||||||24-AUG-12
34356|The Valley Tank Arenite Member|22518|6|Mentioned|p 10, Fig 3|||||||||
34356|The Valley Tank Arenite Member|22730|4|Described|p559,60,62,68|Eifelian|Emsian|1 of 5 sub-units of the Coco Range Sandstone.  Variation on reserved name The Valley Tank Sandstone Member.||||||
34356|The Valley Tank Arenite Member|22857|5|Briefly described|p486 App.1 Tb.A1.7|Middle Devonian|Early Devonian|Of the Coco Range Sandstone. Coarse-grained arenite and pebbly arenite followed by friable silty mudstone and arenite. Geological Province: Ravendale Basin.||||||
34356|The Valley Tank Arenite Member|60648|5|Briefly described|p44 Fig. 4|Eifelian|Emsian|Of the Coco Range Sandstone.  See also The Valley Tank Member, The Valley Tank Arenite and The Valley Tank Pebbly Arenite Member.  Coarse-grained pebbly arenite.  Geological Province: Darling Basin.||||||09-MAR-06
34356|The Valley Tank Arenite Member|67562|5|Briefly described|p103 Fig.9|||~ 150m thick. Also discussed as The Valley Tank Member, p101.||Of the Coco Range Sandstone.||||01-OCT-15
72979|Thirroul Sandstone|24471|5|Briefly described|p31 Fig.3|Late Permian|Late Permian|Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
72979|Thirroul Sandstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
72979|Thirroul Sandstone|73304|6|Mentioned|p61, p70, p74, p78|Wuchiapingian|Capitanian|Sydney Basin, southern. Correlates to the Capitanian-Wuchiapingian/Guadalupian-Lopingian boundary. Corresponds to the middle of the P4 glacial episode, and is coincident with the Emeishan large igneous province and the major regression and low sea level stand at that time.||Illawarra Coal Measures||||
29054|Thirty Foot Coal|41054|6|Mentioned|p152|||||||||
34622|Tholeiitic Gabbro|22831|4|Described|p 24|Ordovician|Ordovician|||||||
82686|Thomkins Gully Monzogranite Phase|71628|5|Briefly described|p11: 36-39, 41, 44; p15: 34, 57-58, 69|||See also p16: 8, 14, 18-23; p19: 101, 162-163. New name (this study), after a local geographic feature. Previously part of Undercliffe Falls Monzogranite. Forms a narrow elongate body exposed as whalebacks and boulders. Relationship with adjacent units is not determined (discussed). Geochemistry described; is geochemically assigned to the Five Mile Creek Suite.||Cullendore Syenogranite.||Intrudes Maryland River Quartz Monzodiorite and The Ridge Monzogranite. Is intruded by Kia-Ora Syenogranite Phase. Abuts Mount Lindesay Monzogranite (Stanthorpe Complex).|Medium-grained, mildly porphyritic to equigranular, biotite-hornblende monzogranite. Contains ellipsoidal mafic enclaves. ?A-type.|
37408|Thompsons Volcanics|23214|5|Briefly described|p142|||Of Burraga Group. Formerly included in part of Kangaloolah Volcanics.||||||
77373|Thornfield Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
24027|Thornton Claystone|22601|6|Mentioned|417, 419|Permian|Permian|Parent Tomago Coal Measures||||||
24027|Thornton Claystone|22610|5|Briefly described|Fig 5||Early Permian|Age 266.1 +/- 0.4Ma||||||
24027|Thornton Claystone|42214|4|Described|p460|||||||||
24027|Thornton Claystone|42780|5|Briefly described|p418|||||||||
24027|Thornton Claystone|71538|6|Mentioned|p54|Permian|Permian|Sydney Basin. |ca. 266 Ma (Gulson et al., 1990)|Tomago Coal Measures||||
24027|Thornton Claystone|73304|5|Briefly described|p62|Wordian|Wordian|Dating by U-Pb CA-TIMS (Gulson et al., 1990).|266 +/- 0.4 Ma|||||
29056|Three Peaks Siltstone Member|9548|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Baledmund Formation (Kopyje Group).||||||
29056|Three Peaks Siltstone Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Thin-bedded siltstone and fine-grained lithic-quartz arenite. Geological Province: Kopyje Shelf (Darling Basin).||||||
29056|Three Peaks Siltstone Member|35287|6|Mentioned|p7|||||||||
29056|Three Peaks Siltstone Member|39618|6|Mentioned|Table 9|||||||||
31643|Three Rocks Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
32251|Three Rocks Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh7||||||
32251|Three Rocks Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
82166|Three Sisters Sill|72522|5|Briefly described|p131.|Lochkovian|Lochkovian|Of Black, 2005. Compared with Wertago Volcanics age.|414.2+/-2.7 Ma|||||
24029|Throsby Granite|22815|4|Described|p80|||||||||
24029|Throsby Granite|42726|5|Briefly described|map legend|Early Devonian||Formal name not intended.||||||
24029|Throsby Granite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Myocum Suite.||||||
24030|Thrumster Slate|22616|6|Mentioned|Fig.1 p670||Early Permian|||||||
24030|Thrumster Slate|22736|6|Mentioned|p627|Permian|Devonian|||||||
24030|Thrumster Slate|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Early Permian|Slate, meta-sandstone and meta-granule conglomerate. Max. Thickness: >650m. Geological Province: Barnard Basin.||||||
24030|Thrumster Slate|24124|5|Briefly described|p3|||||||||
24030|Thrumster Slate|40134|2|Defined|p278|Early Permian|Early Permian|||||||
24030|Thrumster Slate|41347|4|Described|Table 6|||||||||
24030|Thrumster Slate|41348|5|Briefly described|Map legend|Permian|Permian|Slate, met-sandstone and meta-granule conglomerate.||||||16-DEC-04
24030|Thrumster Slate|43755|6|Mentioned|Fig.1,p548||Permian|||||||
24030|Thrumster Slate|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|See also p237 Appendix 1. Geological Province: New England Fold Belt.||||||
24030|Thrumster Slate|62058|4|Described|p4, p5, map sheet|Early Permian|Early Permian|Outcrops between Innes Estate and Cowarra Faults. >650m thick. Resembles the Early Permian Nambucca Slate Belt.||||Intruded by Karikeree Metadolerite.|Slate, metasiltstone and metaconglomerate; laminated limestone.|
24030|Thrumster Slate|63763|5|Briefly described|p4-5 Fig. 1, p14|Early Permian|Early Permian|Slate, slaty sandstone, rare limestone.||||||
24030|Thrumster Slate|65940|6|Mentioned|p194|||Wauchope-Port Macquarie area, NSW.||||||
75928|Thurralilly Suite|66300|6|Mentioned|p17, p23. |Silurian|Silurian|Eastern Lachlan Orogen.|||Includes Lockhart Igneous Complex.|||
75928|Thurralilly Suite|69159|5|Briefly described|Map legend|Silurian|Silurian||||Includes Tallaganda Granodiorite, Lockhart Igneous Complex, Ellenden and Butmaroo Granites.|||
75928|Thurralilly Suite|69270|5|Briefly described|p1, p15-16, p23, p27, p30, p34|Late Silurian|Late Silurian|Most plutonic rocks of Anembo Range have been assigned to Late Silurian Thurralilly Suite by Fitzherbert et al. (2011). Tinderry Granite's Late Silurian age (423.3+/-2.2 Ma U-Pb, this volume) links temporally with other regional plutonic suites (e.g. Thurralilly Suite, which includes 428-424 Ma Lockhart Igneous Complex; Bodorkos et al., 2010).|||Lockhart Igneous Complex|||
75928|Thurralilly Suite|71069|3|Fully described|p9, p21 fig 7, p24, p26 fig 9, p28, p29|Ludlow|Wenlock|Name derived from Thurralilly parish. Replaces the Ellenden, Butmaroo and Rossi Suites. Type locality for type pluton (Lockhart Igneous Complex) is given.  Intrudes the basement beneath basin sequences.Intrusive equivalent of the Woodlawn Volcanics. Foliation developed during the Tabberabberan Orogeny. Distribution, geomorphology,  geochemistry, tectonic structure and metamorphism discussed. See also p31, p36, p38 fig 15, p39 fig 16, p40-p43, p45, p99, p111, p130, p135, p162, p174-p179, p189, p193, p195, p197, p202. |||Includes the  Butmaroo Granite, Gourock Granodiorite, Gibraltar Granite, Lockhart Igneous Complex, Tallaganda Granodiorite, Ellenden Granite, Briars Sharrow Gabbro.|Intrudes the Adaminaby and Mount Fairy Groups. Equivalent to the Currawang Basalt.|Bimodal plutonic rocks.|
75928|Thurralilly Suite|71691|5|Briefly described|Map legend.|Silurian|Silurian||||Briars Sharrow Gabbro; Gibraltar, Ellenden Granites; Tallaganda Granodiorite; Lockhart Igneous Complex.|||
75928|Thurralilly Suite|71699|5|Briefly described|Map legend.|Silurian|Silurian||||Lockhart Igneous Complex, Tallaganda Granodiorite, Ellenden and Butmaroo Granites.|||
75928|Thurralilly Suite|71700|2|Defined|vi, viii, ix, p7, p12, p17, p45, p48|Late Silurian|Middle Silurian|Named for the Parish of Thurralilly. The type pluton for this suite is the Lockhart Igneous Complex. This suite incorporates the "Ellenden", "Rossi", and "Butmaroo" suites of Chappell et al (1991). Distribution, geomorphic expression, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features, and economic geology are discussed. Lithology of this units constituents are discussed. Exposed in the Goulburn Structural Zone. Granites previously mapped as Boro Granite have been recognised in this volume as belonging to the Thurralilly Suite. See also p50, p52-p53, p67, p76-p77, p83-p84, CD.|||Includes the Lockhart Igneous Complex, Butmaroo Granite, Ellenden Granite, Gibraltar Adamellite and the Tallaganda Granodiorite.|Faulted against the Glenbog Suite.||
29579|Thurungly Granite|22638|4|Described|p75||Late Devonian|Previously "Gilmore Hill Granite".||||||
29579|Thurungly Granite|24007|6|Mentioned|p329|Devonian|Devonian|||||||
29579|Thurungly Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
29579|Thurungly Granite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
73401|Tibooburra Suite|66623|2|Defined|pp54-55, pp160-175. |Late Silurian|Late Silurian|Defined in this study. Consists of three penecontemporaneous granodiorite phases, probably the same intrusion at depth, united by age, lithology and geochemistry; and several un-named units. Forms prominent hills of stacked, rounded tors.|427.7 +/- 2.3 Ma - 420 Ma (Black 2006, 2007).||Includes Creswells Tank, Dynamite Tank and Tibooburra Granodiorites.|Intrudes Easter Monday Formation.|Monzodiorite, diorite, granodiorite.|
73401|Tibooburra Suite|66920|5|Briefly described|Map legend|Silurian|Silurian|||||||
73401|Tibooburra Suite|66921|6|Mentioned|Map legend|Silurian|Silurian||||Includes Tibooburra Granodiorite.|||
73401|Tibooburra Suite|66922|5|Briefly described|Map legend|Silurian|Silurian||||Includes Tibooburra Granodiorite.||Predominantly I-type Suite dominated by undeformed, massive, medium-grained hornblende granodiorite with smaller bodies of diorite, dacite, pegmatite and aplite.|
73401|Tibooburra Suite|66927|5|Briefly described|Map legend|Silurian|Silurian|Low to moderate magnetic zones. Intrusive boundaries contrast strongly with magnetised aureole zones.||||Includes Tibooburra, Creswells Tank and Dynamite Creek Granodiorites.|Hornblende granodiorite with smaller bodies of dacite, pegmatite and aplite.|
73401|Tibooburra Suite|67207|5|Briefly described|Map legend.|Silurian|Silurian||||Includes Tibooburra Granodiorite.|||
73401|Tibooburra Suite|67209|5|Briefly described|Map legend.|Silurian|Silurian||||Includes Creswells Tank, Dynamite Tank and Tibooburra Granodiorites.|Intrudes the Warratta Group.|Predominantly I-type suite dominated by undeformed, massive, medium-grained hornblende granodiorite with smaller bodies of diorite, dacite, pegmatite and aplite.|
73401|Tibooburra Suite|67211|5|Briefly described|Map legend.|Silurian|Silurian|||||Intrudes Easter Monday Formation.|Predominantly I-type suite dominated by undeformed, massive, medium-grained hornblende granodiorite with smaller bodies of diorite, dacite, pegmatite and aplite.|
73401|Tibooburra Suite|68823|5|Briefly described|p394|Pridoli|Gorstian||427-420 Ma (Black 2006, 2007; Vickery 2010)||||I-type granites.|
73401|Tibooburra Suite|69001|6|Mentioned|p2 Fig.1B, p58, p97, p105 Fig.43|Silurian|Silurian|||||||
73401|Tibooburra Suite|69002|5|Briefly described|p7, p9, p13|Pridoli|Gorstian||~427-420 Ma, U-Pb SHRIMP II (Black 2006; 2007)|||Intrudes the Warratta Group.|I-type granite.|
73401|Tibooburra Suite|69042|5|Briefly described|map, map legends|Devonian|Silurian|Thomson Orogen?||||||
73401|Tibooburra Suite|69043|6|Mentioned|p11|||Thomson Orogen.||||||
73401|Tibooburra Suite|70210|6|Mentioned|p1|||Koonenberry-Tibooburra district.||||||
73401|Tibooburra Suite|70649|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Tibooburra Granodiorite.||Predominantly I-type suite dominated by undeformed, massive, medium-grained hornblende granodiorite with smaller bodies of diorite, dacite, pegmatite and aplite.|
73401|Tibooburra Suite|70652|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Tibooburra Granodiorite.||Predominantly I-type suite dominated by undeformed, massive, medium-grained hornblende granodiorite with smaller bodies of diorite, dacite, pegmatite and aplite.|
73401|Tibooburra Suite|70749|5|Briefly described|p43|Silurian|Silurian|Southern Thomson and Koonenberry area.|~428-420 Ma.|||||
73401|Tibooburra Suite|71415|5|Briefly described|p11,16-17|||Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.|||Includes Tibooburra Granodiorite.|||
73401|Tibooburra Suite|71965|4|Described|p897,909,913-914|Pridoli|Ludlow|Geological province: Thomson Orogen. Outcropping I-type granitic suite in the southern Thomson Orogen. Reflects voluminous and widespread magmatism from late Silurian to early Devonian.|427.7 +/- 2.4 Ma to 420 .2 +/- 3.3 Ma||Includes Tibooburra, Dynamite Tank and Creswells Tank granodiorites.|Inrudes into the Easter Monday Formation.|Quartz-feldspar-biotite-hornblende granodiorite and associated dykes and sills.|29-OCT-19
73401|Tibooburra Suite|71966|5|Briefly described|p989-990, p1000|Early Devonian|Late Silurian|Geological province: Thomson Orogen. Intrusion associated with c. 430-395 Ma magmatism in the southern Thomson Orogen. Age equivalent with Hungerford Granite.|c. 428-420 Ma|||||25-OCT-19
73401|Tibooburra Suite|72522|6|Mentioned|p119.|Pridoli|Ludlow||c. 420-427 Ma||Includes Dynamite Tank Granodiorite, Creswells Tank Granodiorite, Tibooburra Granodiorite, and felsic dykes.||Includes felsic dykes.|
73401|Tibooburra Suite|72914|6|Mentioned|p16|||Early members had I-type affinities||||||
73401|Tibooburra Suite|72951|6|Mentioned|p1012, p1024, p1029-1031|Silurian|Silurian|Thomson Orogen, southwest. I-type. Surface expression of a gravity high observed under the Warratta Group is interpreted to be the Tibooburra Suite. Heterogeneous mantle source with variable amounts of crustal contamination, possibly including the Mount Wright Arc. Referred to as Tibooburra granites on p1030?|ca 420 Ma||Tibooburra Granodiorite, Dynamite Tank Granodiorite|Intrudes the Warrata Group.|Granites.|
73401|Tibooburra Suite|73177|5|Briefly described|p1110, 1115 Fig.17|Silurian|Silurian|Southern Thomson Orogen. Gives a minimum age for the Benambran deformation.|427.7 +/- 2.3 Ma (Black, 2006).|||Intrudes Warratta Group.||29-AUG-22
73401|Tibooburra Suite|73179|6|Mentioned|p1153|late Silurian|late Silurian|||||||
27913|Tickhole Formation|23055|6|Mentioned|Fig11p23|||||||||
27913|Tickhole Formation|29922|6|Mentioned|Appendix 4|||||||||
27913|Tickhole Formation|29926|6|Mentioned|Fig.3|||||||||
27913|Tickhole Formation|29942|4|Described|Fig.2|||Permian||||||
27913|Tickhole Formation|33867|6|Mentioned|p11|||||||||
27913|Tickhole Formation|34351|5|Briefly described|p344|||Fig.5.13||||||
27913|Tickhole Formation|37083|6|Mentioned|p164|||||||||
27913|Tickhole Formation|39292|6|Mentioned|Fig. 6.2|||||||||
27913|Tickhole Formation|39308|6|Mentioned|p467|||||||||
27913|Tickhole Formation|39609|6|Mentioned|Table 1|||||||||
27913|Tickhole Formation|41479|6|Mentioned|Fig.2|||||||||
27913|Tickhole Formation|43344|14|Not recorded|p85||Permian|||||||
27913|Tickhole Formation|43447|14|Not recorded|diag.p26|||Part of Cardiff Sub-Group||||||
27913|Tickhole Formation|43448|14|Not recorded|p224||Permian|On table only. Unit of Cardiff Subgroup (Newcastle Coal Measures)||||||
27913|Tickhole Formation|45090|6|Mentioned|p186|||Refers McKenzie (1962)||||||
27913|Tickhole Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Adamstown Subgroup|Included Stockrington Tuff Member, Charlestown Conglomerate Member.|||
77324|Tiilungra Limestone Member|68005|5|Briefly described|p147.|Carboniferous|Carboniferous|||Unit in Namoi Formation.|||Coarse, crossbedded feldsarenite, siltstone, conglomerate, calcareous mudstone, oolitic & bioclastic limestone.|17-OCT-12
81862|Tilligerry Mud Member|68811|5|Briefly described|p63|Holocene|Pleistocene|Forms a confining layer in some parts.||||Overlies Tomago Sandbeds. Is overlain by North Stockton Sandbeds.|Estuarine mud.|
82646|Tilmunda Syenogranite Phase|71628|5|Briefly described|p4: 1, 5, 24, 29-30, 47-49, 51-57|||Originally the Tilmunda Adamellite of Chesnut et al. (1973). Chappell (1978) referred to it as Tilmunda Granite. Herein assigned as a subunit of Pringles Monzogranite. Named after a local homestead. Southern New England Orogen. Sparse outcrop in gently undulating, mostly cleared country. Geochemistry described.||Pringles Monzogranite.||Is intruded by Fox Tor Quartz Diorite. Abuts Glenclair Syenogranite, Giants Den Leucosyenogranite and Namoi Tops Monzogranite.|Coarse-grained, equigranular to seriate, leucocratic biotite syenogranite-monzogranite. I-type.|
68871|Timbarra Tablelands suite|60422|5|Briefly described|p386, p391|||Previously Timbarra Tablelands pluton - now assigned this new informal name.||||||
68871|Timbarra Tablelands suite|63748|6|Mentioned|p25|||Informal name.||||||07-FEB-11
23006|Timbrebongie Granite|22519|5|Briefly described|p7|||||||||
23006|Timbrebongie Granite|22831|4|Described|p 73|||||||||
23006|Timbrebongie Granite|43441|5|Briefly described|31|Late Devonian|Middle Devonian|||||||08-JAN-10
23006|Timbrebongie Granite|44160|5|Briefly described|Map Legend|Givetian|Eifelian|||||||08-JAN-10
23006|Timbrebongie Granite|68003|5|Briefly described|p24 Fig.3-e, p142. |Pragian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion. Part of the Yeoval Batholith.|||||Biotite-rich coarse-grained granite.|
81951|Timor Rock Trachyte Member|72700|5|Briefly described|Mapsheet 1|Cenozoic|Cenozoic|||Mount Naman Formation|||Flow-foliated porphyritic anorthoclase, arfvedsonite trachyte.|02-NOV-20
79954|Tinchelooka Diorite|71965|5|Briefly described|p902-903|Emsian|Emsian|Geological province: Thomson Orogen. Intersected in drillhole TRI-RMD08-01, dated at 401.8+\-3.1 Ma (Bodorkos et al., 2013).|401.8+\-3.1 Ma|||Intrudes into Twin Tanks Metamorphics.||
79954|Tinchelooka Diorite|72951|5|Briefly described|p1013, 1021, 1026-1028, 1031|Emsian|Emsian|Thomson Orogen, southern, inboard. I-type. SHRIMP U-Pb zircon isotope analyses from Bodorkos et al. (2013). Spatially associated with the Culgoa lineament, central southern Thomson Orogen. eHf = 4.9 +/- 0.5 and -1.9 +/- 1.8, and d18O = 6.25 +/- 0.27.|401.8 +/- 3.1 Ma||||Porphyritic monzodiorite.|
25532|Tinda Mountain Conglomerate Member|9548|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Kopyje Group.||||||06-JUL-04
25532|Tinda Mountain Conglomerate Member|35287|6|Mentioned|p7|||||||||
25532|Tinda Mountain Conglomerate Member|39618|6|Mentioned|Table 9|||||||||
26173|Tinderry Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Biotite granite. BMR map symbol: gbt.||||||
26173|Tinderry Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
26173|Tinderry Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
26173|Tinderry Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
26173|Tinderry Granite|32820|6|Mentioned|p3|||Cullarin Anticlinorium||||||
26173|Tinderry Granite|33325|6|Mentioned|p18|||Age. Michelago Gp.||||||
26173|Tinderry Granite|34544|6|Mentioned|p186|||||||||
26173|Tinderry Granite|35318|6|Mentioned|p470|||||||||
26173|Tinderry Granite|36413|2|Defined|p105|Early Devonian|Early Devonian|||||||
26173|Tinderry Granite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite, massive, homogeneous, medium grained. GSNSW map code: gt.||||||
26173|Tinderry Granite|39800|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
26173|Tinderry Granite|40328|4|Described|p211|||||||||
26173|Tinderry Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
26173|Tinderry Granite|42820|6|Mentioned|p86|||||||||
26173|Tinderry Granite|48878|14|Not recorded|p.20||Early Devonian|390 m.yrs. (Lower Devonian). (I55-16).||||||
26173|Tinderry Granite|69270|4|Described|p2 Tb.1.1, p15, p20, p23-29, p31|Late Silurian|Late Silurian|Goulburn Trough. Eastern Lachlan Orogen. The sample analysed was grey to cream-brown texturally homogeneous, fine- to medium-grained biotite granite, and was taken from outcrop on north side of Tinderry Road, 200 m outside of Tinderry National Park. Occasional sedimentary-derived xenoliths present on the margins of pluton were noted by Richards (1967); however, none were seen in collected sample. Richardson (1976) suggested Tinderry Granite is a southern continuation of Watch Box Granite, which outcrops only 2 km along strike to the north. Dating method: zircon U-Pb by SHRIMP, n=23. Previous dating: 378 Ma (K-Ar biotite age, Evernden and Richards, 1962); Richardson (1976) suggested this age is too young and Tinderry Granite is more likely Early Devonian, while Scheibner and Basden (1996) included the pluton in Late Silurian-Devonian granites. SHRIMP analysis of Tinderry Granite (this volume) is indistinguishable from Gourock Granodiorite (this volume), and is also within error of ~425 Ma Kohinoor Volcanics of Hoskinstown Group (Fraser et al., in prep). Tinderry Granite links temporally with other regional plutonic suites (e.g. Thurralilly Suite, which includes 428-424 Ma Lockhart Igneous Complex; Bodorkos et al., 2010).|423.3+/-2.2 Ma, magmatic crystallisation|Sapling Flat Igneous Complex|||granite|
26173|Tinderry Granite|71069|6|Mentioned|p201|Wenlock|Wenlock||423.0 +/- 1.8 Ma (SHRIMP, Chisholm et al. 2014)|||Equivalent to the Harrisons Peak Granite.||
31646|Tinderry Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
31646|Tinderry Suite|44093|5|Briefly described|p199 App. 1|Devonian|Late Silurian|Granite. Geological Province: Lachlan Fold Belt.||||||
38354|Tingha Monzogranite|23812|6|Mentioned|p22 Tb.2|||||||||
38354|Tingha Monzogranite|24480|6|Mentioned|p6|||||||||
38354|Tingha Monzogranite|62534|5|Briefly described|p11 (legend), p16|Early Triassic|Early Triassic|Of the Uralla Supersuite. Adjacent to Gilgai Granite. See also p32.||||||07-FEB-11
38354|Tingha Monzogranite|68005|5|Briefly described|pp65-66, p66 Figs.3-P,Q, p135.|Permian|Permian|I-type granite. Ages: 249 Ma (Shaw and Flood 1991: Rb-Sr biotite); 237 Ma (Stroud 1989: K-Ar). Uniform low magnetic response; variably moderate to high radiometric response.|249-237 Ma.|Unit in Uralla Supersuite.||Is intruded by Gilgai Granite.|Moderate to large K-feldspar crystals within a gradational groundmass including biotite and hornblende.|
38354|Tingha Monzogranite|68006|5|Briefly described|p31, p140, p151.|||Associated with tin occurrences. The Gilgai Granite has introduced disseminations, pipes, veins and joint fills of tin, molybdenum and polymetallic mineralisation. Spelt Tinga on p151.||||Is intruded by Gilgai Granite.||
38354|Tingha Monzogranite|68111|5|Briefly described|p968 Tb.1|Wuchiapingian|Changhsingian|Also c.249 Ma, Rb-Sr (biotite) (Shaw 1994).|251.3 +/- 1.7 Ma (U-Pb SHRIMP; Cross et al. 2010).|Of the Uralla Supersuite.||||
38354|Tingha Monzogranite|69639|5|Briefly described|p32, p68, p95, p133, p219|Induan|Changhsingian|New England Orogen.|251.3 +/- 1.7 Ma (SHRIMP U-PB)|Uralla Supersuite||||
38354|Tingha Monzogranite|70217|5|Briefly described|p73 tbl 14.1|Triassic|Permian|New England Orogen. See also reference to Tingha Granite (p43). Age derived from Cross and Blevin, 2010.|251.3 +/- 1.7 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
38354|Tingha Monzogranite|71628|4|Described|p8: 3, 25-26, 43-49; p19: 42-44, 46, 48|||Hosts significant Sn, Ag, Pb, Zn and Mo mineralisation (discussed).|251.3 +/- 1.7 Ma (SHRIMP: Blevin unpubl.)|Mount Duval Suite.||Intrudes Sandon beds, Copeton Monzogranite, Wandsworth Volcanic Group and possibly Gilgai Leucogranite (complex boundary discussed). Abuts Glenreach Monzogranite.|Coarse-grained, porphyritic to megacrystic (plagioclase and white K-feldspar to 60mm}, biotite-hornblende-(pyroxene) monzogranite; rare syenogranite and granodiorite. Igneous enclaves (2-20cm) locally abundant. I-type.|
38354|Tingha Monzogranite|72078|6|Mentioned|p4|Permian|Permian|Geological province: New England Orogen. U-Pb SHRIMP dates for zircon derived from Cross and Blevin 2010. Together with the Elsmore Granite and the Gilgai Granite forms the Tingha Sn-W district.| 251.3+\-1.7 Ma (SHRIMP U-Pb)|||||14-JAN-20
29595|Tintern Granodiorite|23214|3|Fully described|p158|Late Silurian|Late Silurian|Forms part of the Pine Mount Granodiorite of Stevens (1955) and the Pine Mount Intrusive Complex of Madsen (1970).  Intrudes Walli Volcanics. Geological Province: Wyangala Batholith. Leucocratic, medium grained biotite granodiorite.||||||
29595|Tintern Granodiorite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of leucocratic, medium grained, biotite granodiorite.||||||17-JUL-08
29595|Tintern Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyangala Batholith.||||||17-JUL-08
29595|Tintern Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
69886|Tirranna Andesite Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Green-grey massive to amygdaloidal pyroxene-phyric andesite affected by strong qtz-sericite + chlorite+/-pyrite alteration. Massive matrix-supported volcanic conglom.containing rounded scoriaceous andesite clasts...||||||09-SEP-08
69886|Tirranna Andesite Member|68592|2|Defined|p847, p851, p853-9, p862, p873, p875-9|Early Devonian|Early Devonian|See also p132, p726, p729 Fig.132, p827. New name. Geomorphic expression: flat to undulating topography, and isolated outcrops on hilltops. Type locality and representative section located. Thickness: at least 1 km thick, although top not exposed. Could be either lavas or shallow intrusive bodies. Lower greenschist facies metamorphism. Age: most probably earliest Lochkovian. Possibly correlate with Longreach Volcanics; ||Unit in Gundary Volcanics.||Locally conformably overlies Boxers Creek Formation; overlain by Back Station Ignimbrite Member; overlain by Bullamalita Conglomerate and Quialigo Volcanics with probable erosional disconformity.|Locally developed sequence of porphyritic, andesitic to basaltic lava deposits and volcaniclastic rocks.|20-SEP-16
69886|Tirranna Andesite Member|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sfgt. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Gundary Volcanics||Overlies Boxers Creek Formation. Is overlain by Back Station Ignimbrite Member.|Massive-amygdaloidal, plag-pyroxene phyric andesite with strong quartz-sericite and chlorite-pyrite alteration. Massive matrix-supported volcanic conglomerate and breccia with massive-vesicular andesite and quartz-feldspar phyric rhyolite blocks.|
69886|Tirranna Andesite Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||Gundary Volcanics|||Massive-amygdaloidal, plag-pyroxene phyric andesite with strong quartz-sericite and chlorite-pyrite alteration. Massive matrix-supported volcanic conglomerate and breccia with massive-vesicular andesite and quartz-feldspar phyric rhyolite blocks.|
69886|Tirranna Andesite Member|71069|6|Mentioned|p136 fig 44|Early Devonian|Early Devonian|Approximately 100m thick. ||Gundary Volcanics||Overlies the Boxers Creek Formation.||
69886|Tirranna Andesite Member|71700|5|Briefly described|CD|||Recognised in the Braidwood100 sheet area.||Gundary Volcanics||||
76971|Tobermory Monzogranite|71628|4|Described|p2:28; p3: 1, 4, 14-15, 17, 71-72, 80|||See also p3: 82, 84-85, 91-96; p8: 5, 92. Rosenbaum (2012). Previously Tobermory Adamellite (Binns, 1996). Named after a homestead of that name. Crops out ~30 km E of Guyra as small, rubbly corestones. Is cut by two major faults into three slivers. Geochemistry described; indistinguishable from Rockvale Monzogranite. Younger age determinatons suggest resetting of biotite.|292.4 +/- 2.9 Ma (Rosenbaum et al., 2012).|Rockvale Suite.||Intrudes Girrakool beds and Days Creek Gabbro. Encloses (probably intruded by) Days Creek Gabbro. Is intruded by Wards Mistake Monzogranite and Aberfoyle River Porphyrite. Abuts Abroi Monzogranite.|Medium-grained biotite monzogranite-granodiorite; rare garnet-bearing variants; weakly to strongly foliated.|
76971|Tobermory Monzogranite|71703|4|Described|p191-192, 194, 195, 196-205|||S-type granite. U-Pb geochron p198.||Of Hillgrove Supersuite.||Intrudes Girrakool Beds, Wongwibinda Metamorphic Complex.  Adjacent to Abroi Granodiorite.|K feldspar quartz plagioclase biotite opaque +/- garnet muscovite granodiorite with accessory zircon, monazite and apatite.|
24527|Toggannoggra Rhyolite Member|22857|5|Briefly described|p480 App.1 Tb.A1.6|Silurian|Silurian|Of the Long Flat Volcanics. Porphyritic rhyolite, ignimbrite. Max. Thickness: >1000m.||||||09-MAR-06
24527|Toggannoggra Rhyolite Member|39028|6|Mentioned|Map legend|Pridolian|Pridolian|||||||
24527|Toggannoggra Rhyolite Member|40276|2|Defined|p7|Late Silurian|Late Silurian|||||||
24527|Toggannoggra Rhyolite Member|66300|5|Briefly described|p35, 41, 46.|Early Devonian|Early Devonian||412.3 +/- 2.3 Ma.|Unit in Long Flat Volcanics.||Conformably overlies Kadoona Dacite Member. Possibly laterally equivalent to Croppies Gunyah Rhyolite Member.||29-OCT-13
24527|Toggannoggra Rhyolite Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Long Flat Volcanics.|||Cream, grey to black, medium-grained, moderately crystal-rich, densely-welded rhyolitic ignimbrite. Minor intercalated non-welded tuff and volcanic sandstone, rare siltstone.|
24527|Toggannoggra Rhyolite Member|71700|3|Fully described|vi, p24-p26, p43, p58, p63, p70, p79, CD|Early Devonian|Early Devonian|Named for the Toggannoggra homestead on the eastern Captains Flat Road. The type locality is defined north of the homestead at GR 736164 6052840. Historically these rocks have been included in the Long Flat Porphyries (Anderson 1893), later renamed the Long Flat Volcanics (Best et al. 1964). White (1961) formalised the name Bombay Volcanics for dacitic to rhyolitic volcanics within the Bombay area and this subdivision was also adopted by Felton and Huleatt (1975). Wyborn and Owen (1986) rejected the subdivision of the Bombay Volcanics and formalised the Toggannoggra Rhyolite Member. Age is a SHRIMP U-Pb zircon date and is consistent with ages obtained for other members of the Long Flat Volcanics. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. This unit is estimated to be around 1000m thick. Lithology is discussed in detail. Misspelt as the Togganoggra Rhyolite Member on the CD. Intruded by the Kain Porphyry Member.|412.3 +/- 2.3 Ma (Bodorkos & Simpson, 2008)|Long Flat Volcanics||Conformably overlies the Tally Ho Ignimbrite Member. Overlies the Manar Ignimbrite Member. Unconformably overlain by the Gundillion Conglomerate. Overlain by the Ralpine Valley Sandstone Member.|Homogeneous, moderately crystal-rich, densely welded, porphyritic ignimbrite.|
33379|Tolga Member|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Cunningham Formation.||||||
33379|Tolga Member|23170|2|Defined|p183|Lochkovian|Lochkovian|of Cunningham Formation.||||||
33379|Tolga Member|23738|5|Briefly described|p252|Devonian|Devonian|Parent: Cunningham Formation.||||||
33379|Tolga Member|68003|5|Briefly described|p24 Fig.3-e, p143. |Lochkovian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Cunningham Formation|||Calcareous sandstone and siltstone; shale.|
33379|Tolga Member|73299|6|Mentioned|p1103, p1105|Early Devonian|Silurian|Hill End Trough, western. Overturned bedding at type section from pre-Upper Devonian deformation. [Map symbol suggests Devonian age]||||Overlies the Cuga Burga Volcanics, underlies the Cunningham Formation.||
82606|Tolleys Gully Leucomonzogranite|71628|5|Briefly described|p8: 4, 72, 110-112|||New name (this study). First published as Tollys Gully Leucoadamellite (Binns et al., 1967), after unpublished work by Ransley (1970) where he named it the Tolley's Gully Leucoadamellite. Subsequently named Tollys Gully Leucomonzogranite in DMR NAND04 Nandewar Geology Integration and Upgrade project, after unpublished work by Chappell and Bryant (1994). The renaming in this study accords with the correct (Australian Gazetteer) spelling of the watercourse, Tolleys Gully. Unassigned to a Suite. A very small (~1 km2) intrusion c.10km NW of Uralla, with poor outcrops of sloping rock platforms and large scattered tors.||Tolleys Gully Suite.||Intrudes Uralla Granodiorite.|Fine-grained, equigranular, biotite leucomonzogranite.|
80963|Tolligo Granodiorite|71039|6|Mentioned|p26|Early Devonian|Early Devonian|Interpreted from gravity and aeromagnetic data, this unit is entirely subsurface.||||||
80721|Tollingo Granodiorite|71693|5|Briefly described|Map legend.|Early Devonian|Late Silurian||||||I-type. Medium-grained, white, hornblende-biotite granodiorite with prominent poikilitic texture comprising plagioclase, quartz and ferromagnesians set in alkali feldspar chadacrysts.|16-MAR-19
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.|
26175|Tomboye Basalt|30735|2|Defined|p51|Tertiary|Tertiary|||||||
26175|Tomboye Basalt|30736|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26175|Tomboye Basalt|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
26175|Tomboye Basalt|61155|5|Briefly described|p19|Late Eocene|Middle Eocene|Of the Monaro Province Volcanics.Age: 42-39Ma.  In Southeastern NSW.||||||
26175|Tomboye Basalt|68592|6|Mentioned|p1802|||Felton and Huleatt (1977). Occurs in the Shoalhaven River catchment.||||Is correlated with the Reevesdale Basalt.||
26175|Tomboye Basalt|69159|5|Briefly described|Map legend|Eocene|Paleocene||||||Grey to black, fine- to medium-grained, weakly porphyritic and sometimes vesicular, olivine basalt.|07-SEP-15
26175|Tomboye Basalt|71699|5|Briefly described|Map legend.|Neogene|Paleogene||||||Grey to black, fine- to medium-grained, weakly porphyritic and in places vesicular, olivine basalt.|
26175|Tomboye Basalt|71700|2|Defined|vi, p7, p33, CD|Middle Eocene|Middle Eocene|Named for the Tomboye homestead at GR 770690 6094649. The type section is defined at the Tomboye Trigonometrical Station (GR 767517 6096388. Distribution, geomorphic expression, outcrop,  depositional environment, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. K-Ar dates are derived from Carr, 1966; Wellman and McDougall, 1974; Jones, 1986.|40.36 +/- 1.2 Ma to 43.6 +/- 1.3 (K-Ar dates)|||Unconformably overlies the Abercrombie Formation. Equivalent to the Reevesdale Basalt and the Endrick River Basalt.|Grey to black, weakly porphyritic and sometimes vesicular olivine basalt.|
26175|Tomboye Basalt|73581|5|Briefly described|p22|Eocene|Eocene|Southern Highlands Volcanic Province. Misspelt as Tomboyne Basalt p23. List of K-Ar ages provided from Wellman and McDougall (1974b).|44.8, 41.2 Ma, 40.8 Ma, 40.7 Ma K-Ar||||Low-K tholeiite to alkali basalt. High-Ti mineralogy and mantle xenoliths.|
75837|Toms Creek serpentinite|65317|5|Briefly described|p632-633, p622 Fig. 1c, p635 Fig. 14|Early Permian|Late Carboniferous|Appears to be an informal name. Located in the southern Hastings Block, New England Orogen.  Structures suggest Early Permian emplacement. Shown as Toms Creek Serpentinite in figs.||||||
27587|Tongarra Coal|22578|6|Mentioned|p398, Fig.10 p400|||||||||
27587|Tongarra Coal|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Sydney Subgroup||||||
27587|Tongarra Coal|24157|5|Briefly described|p209 Fig.19|||Parent: Bargo Claystone (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
27587|Tongarra Coal|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Overlies: Lower Shoreface Wilton Formation.||||||
27587|Tongarra Coal|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||
27587|Tongarra Coal|24471|4|Described|p29 Fig.2|Late Permian|Late Permian|Within Wilton Formation. Thickness: 3.8 m. Of Illawarra Coal Measures. Possibly Stratigraphically equivalent to part of Four Mile Creek Subgroup.  Geological Province: Sydney Basin.||||||07-FEB-11
27587|Tongarra Coal|29900|6|Mentioned|p169|||||||||
27587|Tongarra Coal|29901|4|Described|Table 1|||||||||
27587|Tongarra Coal|29944|6|Mentioned|Fig.18|||||||||
27587|Tongarra Coal|30006|5|Briefly described|p12|||Permian||||||
27587|Tongarra Coal|31128|6|Mentioned|Table 1|||||||||
27587|Tongarra Coal|31887|5|Briefly described|p5|||||||||
27587|Tongarra Coal|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
27587|Tongarra Coal|33869|6|Mentioned|Fig.2|||||||||
27587|Tongarra Coal|36042|6|Mentioned|Fig.19|||||||||
27587|Tongarra Coal|36220|4|Described|p52|||See also Table 1 & P49.||||||
27587|Tongarra Coal|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
27587|Tongarra Coal|37090|6|Mentioned|p222|||||||||
27587|Tongarra Coal|39287|6|Mentioned|p33|||||||||
27587|Tongarra Coal|39308|5|Briefly described|p512|||||||||
27587|Tongarra Coal|39309|6|Mentioned|p127|||||||||
27587|Tongarra Coal|39661|6|Mentioned|p445|||Replaces Brimstone seam. See also Fig.1||||||
27587|Tongarra Coal|40256|6|Mentioned|p306|||||||||
27587|Tongarra Coal|41226|6|Mentioned|Fig.6|||||||||
27587|Tongarra Coal|42737|5|Briefly described|map legend|Permian||||||||
27587|Tongarra Coal|42787|5|Briefly described|p127, Fig.3 p128|||||||||
27587|Tongarra Coal|42896|4|Described|p20|||of Sydney Subgroup||||||
27587|Tongarra Coal|42925|5|Briefly described|Table 18||Late Permian|||||||
27587|Tongarra Coal|42947|6|Mentioned|p47|||||||||
27587|Tongarra Coal|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
27587|Tongarra Coal|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Wilton Formation. Is overlain by Bargo Claystone.||
27587|Tongarra Coal|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
27587|Tongarra Coal|73421|6|Mentioned|p16, p18-19|Wuchiapingian|Wuchiapingian|Sydney Basin, southern.||Sydney Subgroup||Overlies Wilton Formation, underlies Bargo Claystone||
79955|Tongo Formation|71965|5|Briefly described|p896,900-902,911,913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Characterised by linear trends of moderate magnetic intensity in the Gumbalara Zone. No known outcrop or drillcore; lithology, age and affinity are unknown. Interpreted to be overlain by non-magnetic Cobar Supergroup equivalents, which infers the Tongo Formation to be of Silurian age or older.||||Correlable with Warratta Group, Twin Tanks Metamorphics, Thomson beds, Werewilka Formation and Nebine Metamorphics.||
82472|Tongo intrusion|72914|6|Mentioned|p16|||Informal name for the granodiorite at the base of the Tongo 1 well? See also p12 for description.|425 Ma prelimU-Pb SHRIMP age|||Intrudes Tongo Formation?|Magnetic, medium-K, I-type granodiorite that is unfractionated.|
30025|Toolamanang Formation|22529|5|Briefly described|6|||||||||
30025|Toolamanang Formation|22590|6|Mentioned|Fig3 P754||Ludlow|Actually spelt Toolamanang Fm.||||||
30025|Toolamanang Formation|22857|4|Described|p476 App.1 Tb.A1.6|Pridoli|Wenlockian|Of the Tannabutta Group. Arenite, mudstone, fragmental basalt blocks. Max. thickness: 3km. Geological Province: Capertee Rise.||||||
30025|Toolamanang Formation|23043|5|Briefly described|Map Legend|Pridoli|Ludlow|of Tannabutta Group.||||||
30025|Toolamanang Formation|23170|2|Defined|p69|Late Silurian|Silurian|Supersedes 'Toolamarang Volcanics'. Tannabutta Group.||||||
30025|Toolamanang Formation|43188|4|Described|p199,Table 1 p200|Ludlovian|Wenlockian|Capertee High. Lateral equivialent to Windamere Volcanics. See also Table 2 p201.||||||
30025|Toolamanang Formation|44093|5|Briefly described|p211 App. 1|Ludlovian|Wenlockian|Geological Province: Lachlan Fold Belt.||||||
30025|Toolamanang Formation|66197|5|Briefly described|p629, p633 Fig4a||Late Silurian|Capertee High-Hill End Trough. Deep marine clastics, basaltic clasts. ?Underlies the Queens Pinch Group; overlies Willow Glen Formation.||||||14-MAR-12
26178|Toongi Group|22768|6|Mentioned|p179-80|||||||||
26178|Toongi Group|22831|4|Described|p 37|Lochkovian|Early Silurian|||||||
26178|Toongi Group|22857|4|Described|p179, p456 App.1, Tb.A1.6|Lochkovian|Wenlockian|Predominantly arenites. Contains conodonts. Overlain by rocks of the Gregra Group. Max. thickness: ~8km. Geological Province: Cowra Trough. See also p454 App.1, Tb.A1.6.||||||
26178|Toongi Group|23043|5|Briefly described|Map Legend|Lochkovian|Ludlow|||||||
26178|Toongi Group|23170|2|Defined|p114|Early Devonian|Late Silurian|of Lachlan Fold Belt.||||||
26178|Toongi Group|23309|6|Mentioned|p390|||||||||
26178|Toongi Group|24126|6|Mentioned|p39|||||||||
26178|Toongi Group|29986|6|Mentioned|Map legend|Devonian|Silurian|Silurian-Devonian||||||
26178|Toongi Group|29993|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
26178|Toongi Group|31161|5|Briefly described|PA3|||||||||
26178|Toongi Group|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
26178|Toongi Group|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
26178|Toongi Group|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
26178|Toongi Group|32672|6|Mentioned|p672|||||||||
26178|Toongi Group|34403|6|Mentioned|p147|||||||||
26178|Toongi Group|34405|5|Briefly described|p124|||Fig.3.9||||||
26178|Toongi Group|34406|6|Mentioned|p220|||Probably Silurian||||||
26178|Toongi Group|37727|6|Mentioned|p35|||||||||
26178|Toongi Group|40328|2|Defined|p124|Silurian|Silurian|||||||
26178|Toongi Group|40365|6|Mentioned|p239|||See also P245||||||
26178|Toongi Group|42726|5|Briefly described|map legend|||||||||
26178|Toongi Group|42993|5|Briefly described|p61|||||||||
26178|Toongi Group|43441|5|Briefly described|21, 28|Early Devonian|Late Silurian|In part overlain unconformably by the Dulladerry Rhyolite||||||08-JAN-10
26178|Toongi Group|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
26178|Toongi Group|43500|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
26178|Toongi Group|44093|5|Briefly described|p195 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
26178|Toongi Group|44160|5|Briefly described|Map Legend|Lochkovian|Ludlovian|||||||08-JAN-10
26178|Toongi Group|48958|6|Mentioned|Plate 1|||||||||
26178|Toongi Group|50590|5|Briefly described|Map Legend|Silurian|Silurian|||||||
26178|Toongi Group|67127|6|Mentioned|p111|Devonian|Silurian|Cut by a pipe-like body that hosts the Toongi deposit.|||||Sedimentary rocks.|
26178|Toongi Group|68003|5|Briefly described|p24 Fig.3-e, pp144-145. |Pridoli|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Gullengumbel, Gilgal, Wambangalong, Belowrie, Whylandra, Whychetella, Wirrabilla, Dowd and Glengeera Formations; Berridong Siltstone; Toongi Hall Tuff; Trealmont Quartzite.|Is overlain by Hyandra Group.|Sandstone, shale, siltstone, fine-grained angular conglomerate, chert, rhyolite, tuff.|
26178|Toongi Group|68004|6|Mentioned|p119.|||Outcropping and subcropping units of this Group have moderate epithermal VHMS potential and a level of certainty C.||||||
26178|Toongi Group|70036|5|Briefly described|Map legend|||Lachlan Fold Belt. Included in a mapped unit of Silurian and Devonian sedimentary and volcanic rocks including strongly to moderately deformed felsic to andesitic metasedimentary rocks, conglomerate, sandstone, siltstone, mudstone, shale, tuff, basalt, andesite and rhyolite.||||||
76035|Toopuntul granite|66934|5|Briefly described|Map legend|Late Devonian|Late Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Baconian Swamp Granite Suite.|||Interpreted S-type granites.|
76035|Toopuntul granite|70718|4|Described|p75, p126|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics. Age derived from cross cutting relationship of the Oolambeyan and Eurolie granites.||Baconian Swamp granite suite|||S-type granitic rocks.|31-MAY-19
78976|Toorale gabbro|69540|6|Mentioned|p639-641|||Inferred Neoproterozoic age (Glen et al., 2013) is called into question on the basis of the zircons used.||||||
78976|Toorale gabbro|69541|6|Mentioned|p644, p648|||||||||
36828|Top-Crossing Sandstone Member|23859|2|Defined|p242 Appendix 1|Late Permian|Permian|See also page 933. Type locality 404000E 6742800N. Of Emmaville Volcanics. Geological Province: New England Fold Belt. Max. thickness: 400 m.||||||
27589|Torrington Pendant|29988|6|Mentioned|Map legend|Permian|Carboniferous|Permo-Carboniferous||||||
23028|Torwood Granodiorite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Grey, massive, equigranular, medium- to coarse-grained biotite-pyroxene-hornblende granodiorite. High magnetic response.||||||19-JUN-08
23028|Torwood Granodiorite|68592|2|Defined|p1111-2, p1611, p1632, p1646-9|Early Devonian|Early Devonian|Distinguished as a separate pluton from the undifferentiated Marulan Batholith by Hall (1981); formally defined by Jones (1986). Named after Torwood property. A small pluton of c. 2 km2 in Lumley Park area. Type locality described. Geochemistry and geophysical properties described.||Unit in Arthursleigh Suite.||Truncates Bogungra Dacite Member (Tangerang Formation). Is overlain nonconformably by Lambie Group.|Uniform internal composition. Pale grey, medium- to coarse-grained, equigranular granodiorite and tonalite. Includes scattered small sub-spherical enclaves of quartz monzodiorite and rare fine-grained quartz monzogabbro. I-type.|
23028|Torwood Granodiorite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dat. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Arthursleigh Suite|||Pale grey, medium - coarse-grained, equigranular granodiorite and tonalite. Low to medium K, low Th and U responses; high magnetic susceptibility.|
23028|Torwood Granodiorite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Arthursleigh Suite|||Pale grey, medium - coarse-grained, equigranular granodiorite and tonalite. Low to medium K, low Th and U responses; high magnetic susceptibility.|
30980|Tottenham Subgroup|22831|4|Described|p 15, 16||Ordovician|Girilambone Group||||||
30980|Tottenham Subgroup|22857|5|Briefly described|p414 App. 1 Tb. A1.5|Ordovician|Cambrian ?|Of the Girilambone Group. ||||||
30980|Tottenham Subgroup|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
30980|Tottenham Subgroup|43441|4|Described|Fig.3 p22|||formerly Tottenham Formation. Age:?Early Ordovician||||||08-JAN-10
30980|Tottenham Subgroup|44160|5|Briefly described|Map Legend|Chewtonian|Lancefieldian|||||||
30980|Tottenham Subgroup|67322|5|Briefly described|p20|Darriwilian|Tremadocian|Age assumed to be constrained by the parent Girilambone Group. Occurs in the Condobolin - West Wyalong region.||Of the Girilambone Group|Mount Royal Formation, Bogan Schist, Carolina Forest Formation|||
24040|Touchwood Formation|22736|6|Mentioned|p616,627|Tournaisian|Famennian|||||||
24040|Touchwood Formation|22857|4|Described|p500 App.1 Tb.A1.7|Late Devonian|Late Devonian|Siltstone, arenite, paraconglomerate, basalt, breccia and keratophyric andesite. Max. thickness: ?1km. See also p502 App.1 Tb.A1.7.||||||24-FEB-06
24040|Touchwood Formation|24124|5|Briefly described|p3|||||||||
24040|Touchwood Formation|40134|2|Defined|p276|Middle Paleozoic|Middle Paleozoic|||||||07-NOV-08
24040|Touchwood Formation|41347|4|Described|Table 6|||||||||
24040|Touchwood Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|Siltstone, sandstone, paraconglomerate, basaltic breccia, keratophyric andesite.||||||16-DEC-04
24040|Touchwood Formation|43755|6|Mentioned|Fig.2,p550|Famennian|Frasnian|||||||
24040|Touchwood Formation|44093|5|Briefly described|p67 Fig 6.6|Early Carboniferous|Devonian|In the Southern Hastings Block. See also p237 Appendix 1. Geological Province: New England Fold Belt.||||||30-MAR-05
24040|Touchwood Formation|62058|4|Described|p4, p5, map sheet|Late Devonian|Late Devonian|Lies between Lake Innes and Innes Estate Faults. West-younging sequence > 600m thick with top 250m being andesite. All the clasts are quartz-poor and volcanic. Corals in the conglomerate are Late Devonian.||||Intruded by Karikeree Metadolerite.|Siltstone, sandstone, paraconglomerate, basalt breccia and andesite. A massive volcanic breccia horizon 50m thick is intercalated between sandstone/siltstone below and coarse sandstone above.|
24040|Touchwood Formation|63763|5|Briefly described|p4-5 Fig. 1|Devonian|Devonian|Siltstone, sandstone, paraconglomerate, breccia, andesite. See also p7 Fig. 2.||||||
24040|Touchwood Formation|65940|5|Briefly described|p193-198,203-206,208-209,211-212|||Wauchope-Port Macquarie area, NSW. Type section: a disused quarry on the eastern side of Aston Street, north of the Hibbard - Port Macquarie road (Hastings River Drive) at GR 490000 6522560 (m), Port Macquarie 1:25,000 sheet (9435-2S) (see Leitch 1980). Thickness: at least 600m. Exposed between the Lake Innes and Innes Estate faults. Lower part of stratigraphy is dominantly thin-bedded and graded sandstone and laminated siltstone, upper part contains rare paraconglomerate beds, and basaltic and andesitic clasts. Contains fossil assemblages in clasts indicating a Pragian-Emsian age, possibly down to the latest Silurian (see p196-197). |||||Siltstone, sandstone, paraconglomerate, basalt breccias and andesite.|
24040|Touchwood Formation|70939|6|Mentioned|p826, p828|Devonian|Devonian|Southern Hastings Block.||||||
23031|Towamba Granodiorite|22815|4|Described|p77|||||||||
23031|Towamba Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Glenbog Suite.||||||
23031|Towamba Granodiorite|68592|6|Mentioned|p1675|Early Devonian|Early Devonian|||Unit in Glenbog Suite.||||
77045|Towgon Grange Tonalite|70876|4|Described|p2-p3, p53-p58, p78-p79, p94|Permian|Permian|New England Orogen. An additional age of c. 257.5 Ma is derived from Ar-Ar hornblende dating by Bryant et al, 1997a. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|255.4 +/- 1.2 Ma (SHRIMP U-Pb)|Clarence River Supersuite|||Very coherent, medium-grained tonalite of predominantly unclouded plagioclase, biotite, amphibole and small amounts of alkali feldspar.|
77045|Towgon Grange Tonalite|71628|4|Described|p9: 9, 13, 18, 25, 31, 33-34, 35-42|||See also p18-13. Waltenberg et al. (2016). Originally Gordonbrook Granodiorite (Gutsche, 1969) but renamed Towgon Grange Granodiorite (Brunker and Chesnut, 1976) because Gordonbrook Serpentinite has priority. Renamed again better to reflect the dominant composition. Named after a locality. Crops out ~15 km NNW of Jackadgery. Outcrops vary; on valley floors forms scattered, relatively fresh exfoliated masses. Lithologies, petrography and mineralogy discussed in detail. Geochemistry detailed. Spatially associated with minor Hg, Au, Cu, Fe, Sb and U mineralisation.|255.4 +/- 1.2 Ma (SHRIMP: Waltenberg et al., 2016)|Towgon Grange Suite.||Intrudes Willowie Creek beds (= Silverwood Group).|Medium- to coarse-grained, equigranular to weakly porphyritic, hornblende-biotite-(clinopyroxene-orthopyroxene) tonalite to quartz diorite, with minor diorite and granodiorite; fine-grained, porphyritic marginal variants. I-type.|
72989|Town Beach Diorite|63763|3|Fully described|p4-5 Fig. 1, p8, p14|Late Triassic|Early Permian|Small hornblende diorite pluton and associated dykes. See also p7 Fig. 2.||||||03-FEB-09
77000|Towneys Creek Monzogranite|69270|5|Briefly described|p15, p20|Early Devonian|Early Devonian|Considered contemporaneous with Anembo Granodiorite based on field relationships (Richardson, 1976).|396 Ma, biotite K-Ar date, Richardson 1976|||adjacent to Anembo Granodiorite||
29533|Trangie Formation|22773|6|Mentioned|Fig24.10p355|Late Pleistocene|Late Pliocene|||||||
29533|Trangie Formation|23053|4|Described|p7,12,Fig11p34,38-41|Late Pleistocene|Late Pliocene|||||||
29533|Trangie Formation|24042|5|Briefly described|p513|Eocene|Eocene|||||||
29533|Trangie Formation|43276|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|||||||
29533|Trangie Formation|43277|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|of Great Australian Basin.||||||
29533|Trangie Formation|50616|5|Briefly described|p287|Pleistocene|Pleistocene|Of the Darling River Plain.||||||
29533|Trangie Formation|68003|5|Briefly described|p92 Fig.3-v and Table 3-b, p103.|Pleistocene|Pleistocene|Coonamble Embayment. Thermoluminescence ages from Watkins (1992).|467 +/- 150 to 127 +/- 16 ka.|||Overlies Mount Charlotte Silcrete. Is overlain by Carrabear Formation.||
39263|Tranquille Dacite Member|50613|2|Defined|p213, p230 App. 1, 210 Fig. 4.|Namurian|Namurian|Of the Willuri Formation.  Volcanic member of the Gunnan package (informal grouping of stratigraphically recognisable distinctive, mappable units). Overlain by Yarralumbla Ignim. Mbr. max. thickness: 130m in type section. Geol. Prov: New England Orogen.||||||14-NOV-13
27303|Transmission Limestone Member|5250|5|Briefly described|p42, p45||Early Caradoc|Member of  Fossil Hill Limestone. Includes brachiopod fauna.||||||16-JAN-12
27303|Transmission Limestone Member|23214|3|Fully described|p41|||Of Cliefden Caves Limestone Subgroup. 21m thick at type section.||||||
27303|Transmission Limestone Member|24398|4|Described|p264, p259 Fig. 2|Eastonian|Eastonian|Of Fossil Hill Limestone.   Geological Province: Lachlan Fold Belt.||||||
27303|Transmission Limestone Member|38219|2|Defined|p308|Late Ordovician|Late Ordovician|Part of Cliefden Caves Group. See also Fig.2.||||||
27303|Transmission Limestone Member|41046|6|Mentioned|p144|||||||||
27303|Transmission Limestone Member|42479|5|Briefly described|p109|||||||||
77148|Tremaine Tuff Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Lightly welded crystal vitric tuff. Heulandite-rich.|
77148|Tremaine Tuff Member|68005|5|Briefly described|p139.|Stephanian|Namurian|Informal name.||Unit in Currabubula Formation.|||Lightly-welded crystal-vitric tuff; heulandite-rich.|
25553|Trevallyn Conglomerate Member|31228|5|Briefly described|p77|||Stratigraphy||||||
25553|Trevallyn Conglomerate Member|32869|5|Briefly described|p167|||Depositional environment||||||
25553|Trevallyn Conglomerate Member|44244|6|Mentioned|p48|||Of the Ararat Formation.  Previously regarded as belonging to the Bingleburra Formation.  Geological Province: Gresford Block.||||||
25553|Trevallyn Conglomerate Member|44833|14|Not recorded|p110||Early Carboniferous|Faunal units.||||||
25553|Trevallyn Conglomerate Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Ararat Formation.  Geol. Province: Gresford Block||||||
29502|Triangle Formation|22679|3|Fully described|p 11|Ordovician|Late Ordovician|Maximum thickness >3000.||||||04-MAR-09
29502|Triangle Formation|22857|4|Described|p428 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Kenilworth Group. Quartz arenite, siltstone, slate, phyllite, chert, carbonaceous slate, metabasalt, actinolite schist. Max. thickness: 1200m. ||||||
29502|Triangle Formation|23170|6|Mentioned|p34||Darriwilian|Of Kenilworth Group.||||||17-JUL-08
29502|Triangle Formation|23214|2|Defined|p29|Ordovician|Ordovician|Of Kenilworth Group. Orginally Triangle Group.  Consists of two unnamed units. Geological Province: Lachlan Fold Belt.||||||04-MAR-09
29502|Triangle Formation|23245|6|Mentioned|p134||Early Ordovician|||||||
29502|Triangle Formation|24215|5|Briefly described|p804|||Geological Province:  Lachlan Fold Belt||||||
29502|Triangle Formation|43639|5|Briefly described|Map Legend||Ordovician|||||||
29502|Triangle Formation|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Kenilworth Group. Volcanic and quartz sandstone, phyllite, metabasalt, chert, slate.||||||
29502|Triangle Formation|43782|5|Briefly described|Map Legend|Gisbornian|Darriwilian|of Kenilworth Group.||||||
29502|Triangle Formation|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p156|Late Ordovician|Middle Ordovician|Overlain by Rockley Volcanics (Rockely area). Geological Province: Rockley-Gulgong Volcanic Belt, LFB.||||||07-FEB-11
29502|Triangle Formation|63283|6|Mentioned|p195 Fig. 2, p205|Late Ordovician|Middle Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||07-FEB-11
29502|Triangle Formation|63286|6|Mentioned|p308 Fig. 9|Darriwilian|Darriwilian|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
29502|Triangle Formation|63289|5|Briefly described|p369, p371|Middle Ordovician|Middle Ordovician|Conformably overlies Adaminaby and Bendoc Groups. Intruded by Swatchfield Monzonite. Geological Province: Rockley - Gulgong Volcanic Belt. Consists of volcaniclastics sedimenarty rocks and volcanics.||||||07-FEB-11
29502|Triangle Formation|63290|5|Briefly described|p395, p396 Fig. 3|Late Ordovician|Middle Ordovician|Overlain by Campbells Formation and Rockley Volcanics. Geological Province: Rockley - Gulgong Volcanic Belt. Volcanic and volcaniclastic rocks.||||||
29502|Triangle Formation|63293|6|Mentioned|p469 Fig. 2|Gisbornian|Darriwilian|Overlain by Rockley Volcanics. Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
29502|Triangle Formation|64826|5|Briefly described|p1041 Tb. 1|Darriwilian|Darriwilian|Of the Kenilworth Group.||||||04-MAR-09
29502|Triangle Formation|67106|6|Mentioned|p673|||Rockley-Gulgong Volcanic Belt.||||||
29502|Triangle Formation|67322|4|Described|p17-18|Devonian|Silurian|The Triangle Formation originally included the Budhang and Mozart Cherts (subsequently reassigned to the Adaminaby Group) (Percival and Glen 2007). Occurs in the Oberon-Rockley region. Discussion of possible regional geology scenarios. Contains Gisbornian conodonts in clasts within a younger matrix.|||Includes Gidyen Volcanic Member.|Is overlain by the Rockley Volcanics.|Quartz siltstone with conglomerate, debris flow and olistostromal horizons.|22-FEB-18
29502|Triangle Formation|67847|4|Described|p19-p20, p25, p26 fig 4.2, |Early Gisbornian|Darriwillian|Lachlan Orogen, (the southern part of the Rockley-Gulgong belt of the Macquarie Arc). See also references to the Triangle Group of Stanton 1956 (which precedes the formation). A type area is mentioned at the intersection with the Rockley and Burraga Road and also briefly described. Mistakenly referred to as the Triangle Creek Formation on p29. Hosts the Lucky Draw deposit in laminated quartz-albite rocks.  See also p27-p30, p32, p59.||||Overlies the Campbells Group. Conformably overlain by the Rockley Volcanics. Overlain by the Kangaloolah Volcanics. Intruded by the Swatchfield Monzonite and the Greenslopes Porphyry.|Chert, immature arc-derived volcaniclastic sandstones, siltstones and conglomerates.|
29502|Triangle Formation|68592|5|Briefly described|p371, p424-5, p630|||Rockley-Gulgong Volcanic Belt. Fossils of Middle and Late Silurian have been found in this unit, implying a significant hiatus.||Unit in Cabonne Group.||Is overlain disconformably by Fosters Creek Conglomerate.||
29502|Triangle Formation|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 2 volcanic units. Age: ranges from early Darriwilian (Da2) to latest Gisbornian. Rockley-Gulgong Volcanic Belt.|c. 470-455 Ma|Cabonne Group||||
29502|Triangle Formation|70684|6|Mentioned|p3, p75|Late Ordovician|Middle Ordovician|Rockley district, Rockley-Gulgong Volcanic Belt.||||||
29502|Triangle Formation|73154|5|Briefly described|p77 Fig.3|Gisbornian|Darriwilian|Macquarie Arc, Phase 2. Rockley-Gulgong Volcanic Belt.|||||Intermediate-mafic lava, conglomerate, shale.|
23046|Trigalong Formation|22638|4|Described|p22|Early Devonian|Late Ordovician|New name.||||||
23046|Trigalong Formation|22857|5|Briefly described|p418 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Thinly bedded siltstone and minor sandstone.||||||
23046|Trigalong Formation|44192|5|Briefly described|Map Legend|Llandoverian|Eastonian|||||||
23046|Trigalong Formation|44936|5|Briefly described|Map Legend||Ordovician|||||||
23046|Trigalong Formation|50191|6|Mentioned|p16||Late Ordovician|||||||
23046|Trigalong Formation|67322|5|Briefly described|p20|||Warren et al. (1995). Occurs in the Parkes-Forbes-Junee area. Probably Ordovician.||||Possible equivalent of the Kirribilli Formation.|Quartz-rich turbiditic rocks.|22-FEB-18
23046|Trigalong Formation|67847|5|Briefly described|p21-p22|||||||Equivalent to the Kirribilli, Cotton and Jingerangle Formations.|Inter-bedded sandstones, siltstones and slate.|
23046|Trigalong Formation|70684|6|Mentioned|p54 Fig.27|Ordovician|Ordovician|Adaminaby Superterrane.||||||
23046|Trigalong Formation|70718|5|Briefly described|p44|Llandovery|Eastonian|Wagga-Omeo Zone, Murray Basin. The source of the ages is not provided. |428.2 -456.1 Ma ||||Thinly bedded siltstone with minor sandstone.|
23046|Trigalong Formation|72082|1|Redefined|p4, p6-23, p25|Early Silurian|Late Ordovician|Originally included in undifferentiated late Silurian to early Devonian sedimentary rocks in Fitzpatrick (1976). Defined by Warren et al. (1995); named after the Parish of Trigalong, County of Bland. Thickness unknown. The type area is herein allocated as being within the quarried ground in Wilesmiths Quarry at Lat. 34degrees 28'50"S, Long. 147degrees 32'23"E and a larger quarried area c.500m to the NNW. A reference area is a road cutting along Reinholds Lane, c.7.5 km by road S of Temora. Generally poorly exposed. Forms flat to gently undulating country exept for NNW-trending ridges on the S outskirts of Temora. Numerous photographs and photomicrographs. Deformation detailed. Definitive evidence for age is lacking; based on similarity with other units (described in great detail). Has similar age, lithology, metamorphic facies, bedding strike/dip, folding and interpreted turbiditic depositional environment, to the Bribbaree, Bronxhome and Illabo Formations. More units with similar lithologies are described. Quarried for construction material. Hosted historical gold workings (listed).||||Is faulted against the Combaning Formation.|Sub- to low-greenschist facies, laminated to thinly bedded, finely micaceous, metapelites (claystone, sandy claystone, mudstone), metasiltstone (can be siliceous), phyllite and lesser fine-grained quartzose metasandstone. Quartz veins prevalent.|08-JAN-20
23046|Trigalong Formation|72495|6|Mentioned|p218|Ordovician|Ordovician|Adaminaby Superterrane.|||||Turbidite.|
24537|Trilobite Hill Limestone Member|5250|6|Mentioned|p42, p54, p57||Late Ordovician|Member of Vandon Limestone. Includes brachiopod fauna.||||||
24537|Trilobite Hill Limestone Member|23213|5|Briefly described|p19|||Distinctive lithology like the Reedy Creek Limestone.||||||
24537|Trilobite Hill Limestone Member|23214|3|Fully described|p40|Eastonian|Eastonian|Of Vandon Limestone. Previously "island unit" of Percival (1976). Max. thickness 29m.||||||
24537|Trilobite Hill Limestone Member|24417|6|Mentioned|p24|||Of Cliefden Caves Limestone Subgroup.||||||
24537|Trilobite Hill Limestone Member|38219|2|Defined|p311|Late Ordovician|Late Ordovician|See also Fig.2 and P301.||||||
24537|Trilobite Hill Limestone Member|41046|6|Mentioned|p144|||||||||
24537|Trilobite Hill Limestone Member|42479|5|Briefly described|p109|||||||||
38847|Tritton Formation|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
38847|Tritton Formation|67322|5|Briefly described|p20|Darriwilian|Tremadocian|Fogarty (1998). Age from parent Girilambone Group. Occurs in the Condobolin - West Wyalong region.||Of the Girilambone Group|||Clastic rocks: phyllite, sandstone, quartzwacke and quartz-mica schist.|22-FEB-18
38847|Tritton Formation|72296|5|Briefly described|p9|||Smith (1973). Girilambone mine area. See p9 for the evolving use of this name. ||||Conformably overlies Caro Schist.|Metasedimentary rocks.|
26957|Truganini Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Ash flow unit. Geological Province: Kopyje Shelf (Darling Basin).||||||
26957|Truganini Tuff Member|35287|6|Mentioned|p7|||||||||
26957|Truganini Tuff Member|39618|6|Mentioned|Table 9|||||||||
26957|Truganini Tuff Member|42566|3|Fully described|p66|||Previously included in Babinda Volcanics.|||||Massive blue grey to white, crystal - vitric tuff containing small chloritic 'clots' or wisps.|24-SEP-19
26957|Truganini Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
29079|Trundle Group|22519|6|Mentioned|p3|||||||||
29079|Trundle Group|22520|6|Mentioned|p18|||||||||
29079|Trundle Group|22638|6|Mentioned|p62|||Equivalent of the Combaning Formation||||||
29079|Trundle Group|22768|4|Described|p178|Emsian|Pragian|||||||
29079|Trundle Group|22831|2|Defined|p 58|Pragian|Lochkovian|||||||
29079|Trundle Group|22857|5|Briefly described|p178, p448 App.1, Tb.A1.6|Early Devonian|Early Devonian|Max. thickness: 2000m. Geological Province: Bogan Gate Terrace.||||||
29079|Trundle Group|23522|5|Briefly described|p249 Fig 5|Emsian|Lochkovian|||||||
29079|Trundle Group|23898|6|Mentioned|p287|Emsian|Pragian|||||||
29079|Trundle Group|24417|3|Fully described|p78|Early Devonian|Early Devonian|Now includes rocks previously mapped as Wallingalair Group.  Formerly referred to as "Trundle Beds".  Overlain by Hervey Group (para); overlies Derriwong Group (para).  Max. thickness: 2300m.||||||
29079|Trundle Group|24580|6|Mentioned|p828|||Geological Province: Eastern Lachlan Fold Belt.||||||
29079|Trundle Group|34449|6|Mentioned|p128|||||||||
29079|Trundle Group|36066|4|Described|p10|||||||||
29079|Trundle Group|37258|6|Mentioned|p2|||||||||
29079|Trundle Group|40365|6|Mentioned|p241|||||||||
29079|Trundle Group|40891|6|Mentioned|p19|||||||||
29079|Trundle Group|42456|6|Mentioned|p10|||||||||
29079|Trundle Group|42714|6|Mentioned|p24|||||||||
29079|Trundle Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
29079|Trundle Group|43441|4|Described|20, 29||Early Devonian|||||||08-JAN-10
29079|Trundle Group|44093|5|Briefly described|p178 App. 1|Early Devonian|Silurian|In the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
29079|Trundle Group|44160|5|Briefly described|map legend|Emsian|Lochkovian|||||||
29079|Trundle Group|46522|6|Mentioned|p65|||||||||
29079|Trundle Group|50077|5|Briefly described|p13|Early Devonian|Early Devonian|||||||
29079|Trundle Group|50299|5|Briefly described|Map Legend|Devonian|Devonian|||||||
29079|Trundle Group|60008|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Sediments and/or volcanics.||||||08-JUL-04
29079|Trundle Group|60009|5|Briefly described|Map Legend|Emsian|Lochkovian|||||||13-JUL-04
29079|Trundle Group|60548|5|Briefly described|map legend|Devonian|Devonian|||||||
29079|Trundle Group|61894|6|Mentioned|p179 Fig.3|||||||||
29079|Trundle Group|62569|5|Briefly described|p606|Devonian|Silurian|Unconformably underlies Hervey Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
29079|Trundle Group|63289|6|Mentioned|p373 Fig. 7|Early Devonian|Early Devonian|||||||07-FEB-11
29079|Trundle Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
29079|Trundle Group|66498|6|Mentioned|p43|||||||||
29079|Trundle Group|71040|5|Briefly described|p12 Fig.7, p16, p26|Early Devonian|Early Devonian||||Pullabooka Formation, Carawandool Volcanics.|||
24046|Trungley Hall Granite|22638|4|Described|p75||Late Devonian|New name.||||||
24046|Trungley Hall Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
24046|Trungley Hall Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
24046|Trungley Hall Granite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
30219|Trunkey Creek Slate|43127|6|Mentioned|p12|||||||||
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.|
31015|Tucklan Formation|13139|5|Briefly described|p9 Fig. 4, p10|Late Ordovician|Late Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||12-APR-05
31015|Tucklan Formation|22466|6|Mentioned|P8||Ordovician|||||||
31015|Tucklan Formation|22857|4|Described|p430 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Dark mudstone, basalt-latite boulder conglomerate or breccia, lithic arenite, rare chert.||||||
31015|Tucklan Formation|23043|5|Briefly described|Map Legend|Bolindian|Eastonian|of Cabonne Group.||||||
31015|Tucklan Formation|23170|1|Redefined|p46|Late Ordovician|Eastonian|Age: Middle Eastonian - Late Ordovician. Cabonne Group.||||||
31015|Tucklan Formation|23181|5|Briefly described|p1,5,6, Fig.1||Late Ordovician|Age from conodont samples: late Eastonian.||||||
31015|Tucklan Formation|23213|5|Briefly described|p21, Fig.10|Eastonian|Eastonian|Age: early Eastonian to Late Eastonian. Contain conodont fauna comparable to Oakdale Formation.||||||
31015|Tucklan Formation|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
31015|Tucklan Formation|24463|4|Described|p321|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||24-FEB-06
31015|Tucklan Formation|43494|4|Described|p8|Ordovician|Ordovician|Supersedes Tucklan Beds of Offenberg et al (1971). Consists of basalt, volcaniclastic sandstone and siltstone, micaceous schist, black slaty shale and chert. Overlies the Adaminably Group. Adjacent to Gulgong Granite.||||||09-MAR-06
31015|Tucklan Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p157|Late Ordovician|Late Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt, LFB. Age determined from conodonts found in discrete limestone lenses, Eastonian.||||||07-FEB-11
31015|Tucklan Formation|63283|6|Mentioned|p205|||Geological Province: Rockley-Gulgong Volcanic Belt.||||||07-FEB-11
31015|Tucklan Formation|63290|6|Mentioned|p397 Fig. 3(b)|Late Ordovician|Late Ordovician|Geological Province: Rockley - Gulgong Volcanic Belt.||||||
31015|Tucklan Formation|63293|6|Mentioned|p468 Fig. 2|Bolindian|Gisbornian|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
31015|Tucklan Formation|67322|4|Described|p25-26|Ordovician|Ordovician|Redefined by Colquhoun, Meakin and Henderson, in Meakin and Morgan (1999). E margin of the Hill End Trough. Age from fossils and the high potassium response (typical of Ordovician rocks in the Macquarie Arc) on ternary U-K-Th radioelement imagery.||Of the Cabonne Group|||Consists of mass-flow deposits, conglomerates, and minor allochthonous limestones.|22-FEB-18
31015|Tucklan Formation|68003|5|Briefly described|p24 Fig.3-e, p28 Photo.3-a, p147.|Eastonian|Darriwilian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Cabonne Group.|||Dark mudstone, basalt to latite boulder conglomerate or breccia, lithic sandstone, rare chert; basalt, ?andesite to dolerite and latite unit; black radiolarian chert unit; limestone, minor allodapic facies, unit.|
31015|Tucklan Formation|68592|6|Mentioned|p371|||Rockley-Gulgong Volcanic Belt.||Unit in Cabonne Group.||||
31015|Tucklan Formation|70684|6|Mentioned|p3, p74|Late Ordovician|Late Ordovician|Rockley-Gulgong Volcanic Belt.||||||
31015|Tucklan Formation|70754|5|Briefly described|p450 Fig.2, p451, p457|Katian|Katian|South of Dunedoo. Some fossil species named. Systematic palaeontological descriptions.|||||Siltstone. Also contains allochthonous limestones of late Eastonian age.|
83217|Tueloga beds|73496|5|Briefly described|Map legend|Ordovician|Ordovician|Parts either have magnetic responses to 10 nT but mostly less than 5 nT; or 10 to 30 nT, or are reversely magnetised.|||||Sandstone with lesser siltstone and mudstone, strongly layered, probably includes pyrrhotite-rich layers; deep marine turbidite fan deposits; gravity response higher than adjacent plutons.|
83217|Tueloga beds|73497|6|Mentioned|Map legend|Ordovician|Ordovician|Marine.|||||Contact metamorphosed, magnetic responses to 10 nT, but mostly less than 5 nT.|
83217|Tueloga beds|73505|5|Briefly described|p2, p6-7, p14, p19-20, p28, p35|Ordovician|Ordovician|Newly named unit in Swan Hill and parts of Balranald and Deniliquin 1:250 000 map areas. Named after Tueloga Railway Station. Distributed mostly north of the Governor Fault, comprises consistently magnetic rocks separated from the equivalent Castlemaine Group. Typical magnetic response about 2 nT, but units may reach 30 nT; may be remnantly magnetised. Includes two moderately magnetic units in NSW interpreted as metasediments. Gravity repsonse largely defines the regional.||||Overlies Dja Dja Wrung Supergroup, equivalent to Castlemaine Group|Metasediments.|
35029|Tuena Formation|23048|5|Briefly described|p9 fig14||Early Devonian|||||||
24048|Tugalong Limestone Member|37986|2|Defined|p310|Silurian|Silurian|||||||
24048|Tugalong Limestone Member|40774|6|Mentioned|Fig.2|||||||||
24048|Tugalong Limestone Member|68592|5|Briefly described|p899, p913|||Wollongong 1:250 000 map area.||Unit in Karalinga Formation.||Time equivalent to Lookdown Limestone Member (Cardinal View Formation).||
24048|Tugalong Limestone Member|70661|6|Mentioned|p31|||||Bungonia Group||||
26958|Tuggerah Formation|22745|6|Mentioned|p129|||Sydney Basin.||||||
26958|Tuggerah Formation|22857|4|Described|p520 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Narrabeen Group. Medium to coarse-grained sandstone interbedded with siltstone and claystone. Max. thickness: 98m. Geological Province: Sydney Basin. See also p524 App.1 Tb.A1.9.||||||
26958|Tuggerah Formation|22969|4|Described|Fig 4.1a||Early Triassic|||||||
26958|Tuggerah Formation|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
26958|Tuggerah Formation|29915|6|Mentioned|p68|||||||||
26958|Tuggerah Formation|30286|6|Mentioned|p1099|||Stratigraphic table||||||
26958|Tuggerah Formation|31276|6|Mentioned|p147|||Palynology||||||
26958|Tuggerah Formation|31297|6|Mentioned|p6|||||||||
26958|Tuggerah Formation|31426|6|Mentioned|Fig.1|||||||||
26958|Tuggerah Formation|31884|6|Mentioned|Table 1|||Triassic||||||
26958|Tuggerah Formation|32803|6|Mentioned|p95|||||||||
26958|Tuggerah Formation|33683|4|Described|Table 1|||||||||
26958|Tuggerah Formation|33685|6|Mentioned|Table 2|||||||||
26958|Tuggerah Formation|33867|6|Mentioned|Table 1|||||||||
26958|Tuggerah Formation|33986|6|Mentioned|p30|||Table||||||
26958|Tuggerah Formation|34009|6|Mentioned|Table III|||||||||
26958|Tuggerah Formation|34107|6|Mentioned|p217|||Triassic||||||
26958|Tuggerah Formation|34121|6|Mentioned|p397|||||||||
26958|Tuggerah Formation|34241|6|Mentioned|p404|||||||||
26958|Tuggerah Formation|34301|6|Mentioned|p403|||||||||
26958|Tuggerah Formation|34336|5|Briefly described|p391|||On Table 5.16.||||||
26958|Tuggerah Formation|34339|6|Mentioned|p442|||Clay minerals||||||
26958|Tuggerah Formation|34437|6|Mentioned|p406|||Contains Ostracods||||||
26958|Tuggerah Formation|35062|6|Mentioned|p279|||||||||
26958|Tuggerah Formation|35690|6|Mentioned|p61|||||||||
26958|Tuggerah Formation|36042|6|Mentioned|Fig.22|||See also Fig.24.||||||
26958|Tuggerah Formation|36391|6|Mentioned|p156|||||||||
26958|Tuggerah Formation|37804|6|Mentioned|Table 1|||||||||
26958|Tuggerah Formation|39287|6|Mentioned|Fig. 2.18|||||||||
26958|Tuggerah Formation|39294|4|Described|p165|||||||||
26958|Tuggerah Formation|39306|6|Mentioned|p413|||||||||
26958|Tuggerah Formation|39308|6|Mentioned|Fig. 23.12|||||||||
26958|Tuggerah Formation|40625|6|Mentioned|Map legend|Early Triassic|Early Triassic|Early to Middle Triassic||||||
26958|Tuggerah Formation|40629|6|Mentioned|p186|||||||||
26958|Tuggerah Formation|41010|6|Mentioned|p17|||See also Table 1||||||
26958|Tuggerah Formation|41639|6|Mentioned|p9|||||||||
26958|Tuggerah Formation|42916|5|Briefly described|Table 1||Early Triassic|||||||
26958|Tuggerah Formation|43194|5|Briefly described|p130|Triassic|Triassic|Fine grained red and green overbank sediments deposited in the northern Sydney Basin.||||||
26958|Tuggerah Formation|43257|5|Briefly described|Map Legend||Early Triassic|Of Clifyon Subgroup||||||
26958|Tuggerah Formation|43317|5|Briefly described|Table 1 p10|||||||||
26958|Tuggerah Formation|43318|14|Not recorded|opp p6||Late Triassic|See also Lexicon||||||
26958|Tuggerah Formation|43320|14|Not recorded|Table 1 p11,12||Triassic|Part of Clifton Subgroup||||||
26958|Tuggerah Formation|43342|14|Not recorded|Table 1 p107|||||||||
26958|Tuggerah Formation|43344|14|Not recorded|p21|||Unit of Narrabeen Group||||||
26958|Tuggerah Formation|43352|14|Not recorded|p 209-223||Triassic|||||||
26958|Tuggerah Formation|43383|14|Not recorded|p22|||||||||
26958|Tuggerah Formation|43385|14|Not recorded|p182 Table||Triassic|||||||
26958|Tuggerah Formation|43395|14|Not recorded|p74|||||||||
26958|Tuggerah Formation|43508|14|Not recorded|p122|||petrographic analyses||||||
26958|Tuggerah Formation|44610|14|Not recorded|p47,49|||||||||
26958|Tuggerah Formation|45090|6|Mentioned|p122|||Phosphate deposits||||||
26958|Tuggerah Formation|61315|5|Briefly described|Table SY1|Eary Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
26958|Tuggerah Formation|68003|5|Briefly described|p42.|Triassic|Triassic|Northern Sydney Basin. Deposition from SE-flowing streams.|||||Fine-grained red and green overbank sediments.|
26958|Tuggerah Formation|70647|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Sydney Basin.||Clifton Subgroup|||Grey to green-grey laminite, red-brown claystone and siltstone, interbedded with fine- to medium-grained green-grey sandstone.|04-OCT-16
31649|Tuglow Suite|42726|5|Briefly described|Map Legend||Carboniferous|||||||
31649|Tuglow Suite|44093|5|Briefly described|p216 App. 1|Late Carboniferous|Late Carboniferous|Geological Province: Lachlan Fold Belt.||||||
31649|Tuglow Suite|64238|5|Briefly described|Map legend|Carboniferous|Carboniferous|Contains the Kanangra and Abercorn Granites.||||||
31649|Tuglow Suite|68592|3|Fully described|p1754-8, p1768-77||Early Carboniferous|Assigned to the former Tuglow Granite (name since replaced by Kanangra Granite) by Chappell et al. (1991), after the Tuglow area. The previously unassigned pluton, the Abercorn Granite, is also included due to proximity and compositional similarity with Kanangra Granite. Geochemistry detailed; shares many similarities with Lockyersleigh Suite.||Unit in Oberon Supersuite.|Includes Kanangra and Abercorn Granites.|Intrudes Abercrombie Formation and Warbisco Shale, Mount Fairy and Lambie Groups.|Pink-cream, medium- to coarse-grained leucocratic granites; massive and undeformed.|
31649|Tuglow Suite|70192|5|Briefly described|Map Legend|Carboniferous|Carboniferous|On Taralga 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Abercorn Granite, Kanangra Granite.|||
31649|Tuglow Suite|70543|5|Briefly described|Map Legend|Carboniferous|Carboniferous||||Includes Abercorn Granite, Kanangra Granite|||
28291|Tugrabakh Limestone Member|36057|1|Redefined|p345|Tournaisian|Tournaisian|Prob. Tournaisian||||||
28291|Tugrabakh Limestone Member|39660|6|Mentioned|p450|||||||||
28291|Tugrabakh Limestone Member|42547|5|Briefly described|p34|||||||||
28291|Tugrabakh Limestone Member|44244|4|Described|p199|Tournaisian|Tournaisian|Of the Wallanbah Formation.  Max. thickness: 40m.  Type section in text.  Geological Province: Myall Block.||||||
26185|Tulcumba Sandstone|721|5|Briefly described|Map legend|Tournaisian|Tournaisian|Of the Parry Group.  Coarse crossbedded feldsarenite, siltstone, conglomerate, calcareous mudstone, oolitic and bioclastic limestone.||||||
26185|Tulcumba Sandstone|22736|6|Mentioned|p630|||||||||
26185|Tulcumba Sandstone|22857|5|Briefly described|p496 App.1 Tb.A1.7|Torunaisian|Tournaisian|Of the Parry Group. Coarse, crossbedded felsarenite, siltstone, conglomerate, calcareous mudstone, oolitic and bioclastic limestone. Max. thickness: 230m. Geological Province: Tamworth Forearc Basin.||||||
26185|Tulcumba Sandstone|23185|6|Mentioned|Fig1p156|Carboniferous|Carboniferous|||||||
26185|Tulcumba Sandstone|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt||||||
26185|Tulcumba Sandstone|24366|5|Briefly described|p17 Fig. 3|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt.||||||
26185|Tulcumba Sandstone|24603|5|Briefly described|p867|Tournaisian|Tournaisian|See also p869 Fig. 4 and p886 Fig. 11.  Geological Province: Tamworth Belt.||||||
26185|Tulcumba Sandstone|24605|5|Briefly described|p935 Fig. 4|Tournaisian|Tournaisian|Geological Province: New England Orogen.||||||
26185|Tulcumba Sandstone|30070|6|Mentioned|Fig.2|||Devonian age.||||||
26185|Tulcumba Sandstone|30135|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26185|Tulcumba Sandstone|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26185|Tulcumba Sandstone|31519|6|Mentioned|p920|||||||||
26185|Tulcumba Sandstone|31802|6|Mentioned|p134|||Source area.  See also unconformities P143.||||||
26185|Tulcumba Sandstone|31999|6|Mentioned|Table 1|||||||||
26185|Tulcumba Sandstone|32286|6|Mentioned|Fig. 1|||||||||
26185|Tulcumba Sandstone|32482|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26185|Tulcumba Sandstone|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26185|Tulcumba Sandstone|32672|6|Mentioned|p674|||||||||
26185|Tulcumba Sandstone|32865|6|Mentioned|p480|||Carb.||||||
26185|Tulcumba Sandstone|32866|6|Mentioned|p3|||Fossil content||||||
26185|Tulcumba Sandstone|33728|6|Mentioned|p48|||||||||
26185|Tulcumba Sandstone|34080|6|Mentioned|p248|||||||||
26185|Tulcumba Sandstone|34081|6|Mentioned|p258|||||||||
26185|Tulcumba Sandstone|34083|5|Briefly described|p247|||||||||
26185|Tulcumba Sandstone|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
26185|Tulcumba Sandstone|34086|6|Mentioned|p261|||Assemblages||||||
26185|Tulcumba Sandstone|34262|6|Mentioned|p242|||||||||
26185|Tulcumba Sandstone|34347|6|Mentioned|p15|||Tournaisian. See also P17.||||||
26185|Tulcumba Sandstone|34555|5|Briefly described|p240|||||||||
26185|Tulcumba Sandstone|36057|6|Mentioned|p350|||||||||
26185|Tulcumba Sandstone|36296|6|Mentioned|p165|||||||||
26185|Tulcumba Sandstone|36528|6|Mentioned|p175|||||||||
26185|Tulcumba Sandstone|36961|6|Mentioned|p208|||See also Fig.3.||||||
26185|Tulcumba Sandstone|37987|2|Defined|p225|Carboniferous|Carboniferous|||||||
26185|Tulcumba Sandstone|38215|6|Mentioned|Fig.2|||||||||
26185|Tulcumba Sandstone|38222|5|Briefly described|p358|||||||||
26185|Tulcumba Sandstone|39331|6|Mentioned|Table 10-1|||||||||
26185|Tulcumba Sandstone|39468|6|Mentioned|Fig.2|||||||||
26185|Tulcumba Sandstone|40245|6|Mentioned|p199|||||||||
26185|Tulcumba Sandstone|40246|6|Mentioned|Table 1|||||||||
26185|Tulcumba Sandstone|40883|6|Mentioned|p13|||||||||
26185|Tulcumba Sandstone|41009|6|Mentioned|Fig.2|||||||||
26185|Tulcumba Sandstone|41279|6|Mentioned|Fig.3|||||||||
26185|Tulcumba Sandstone|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Of the Parry Group.||||||16-DEC-04
26185|Tulcumba Sandstone|41542|6|Mentioned|p239|||||||||
26185|Tulcumba Sandstone|41826|6|Mentioned|p311|||||||||
26185|Tulcumba Sandstone|42547|4|Described|p20|||Werrie Syncline.||||||
26185|Tulcumba Sandstone|43091|5|Briefly described|Map legend|||Of Parry Group.||||||17-SEP-08
26185|Tulcumba Sandstone|43383|14|Not recorded|p17|Early Carboniferous|Tournaisian|||||||
26185|Tulcumba Sandstone|43407|14|Not recorded|Map Legend||Early Carboniferous|(Provisional Edition)||||||
26185|Tulcumba Sandstone|43409|14|Not recorded|Map Legend||Tournaisian|||||||
26185|Tulcumba Sandstone|43417|14|Not recorded|Map Legend|||||||||
26185|Tulcumba Sandstone|43418|14|Not recorded|Map Legend|||||||||
26185|Tulcumba Sandstone|43432|14|Not recorded|p202,203,211||Early Carboniferous|||||||
26185|Tulcumba Sandstone|43435|14|Not recorded|Map Legend|||||||||
26185|Tulcumba Sandstone|43455|14|Not recorded|p460(Tb.)||Carboniferous|||||||
26185|Tulcumba Sandstone|43479|14|Not recorded|p157,158,177||Tournaisian|||||||
26185|Tulcumba Sandstone|43538|14|Not recorded|p2,3|||Lower Carboniferous fauna||||||
26185|Tulcumba Sandstone|44360|14|Not recorded|p33||Early Carboniferous|||||||
26185|Tulcumba Sandstone|44379|14|Not recorded|p10,15||Tournaisian|Ref. to Campbell and Engel 1963. (lower or early upper Tournaisian.)||||||
26185|Tulcumba Sandstone|44833|14|Not recorded|p116,117|||||||||
26185|Tulcumba Sandstone|44835|14|Not recorded|p45||Carboniferous|||||||
26185|Tulcumba Sandstone|44858|14|Not recorded|p90||Tournaisian|||||||
26185|Tulcumba Sandstone|45063|6|Mentioned|p272|||Brachiopods. Tournaisian||||||
26185|Tulcumba Sandstone|45088|5|Briefly described|p62|||Correlation||||||
26185|Tulcumba Sandstone|45097|6|Mentioned|p14|||Zone. Correlation chart||||||
26185|Tulcumba Sandstone|46803|6|Mentioned|p143|||See also Fig. 3||||||
26185|Tulcumba Sandstone|47056|6|Mentioned|Fig.2 P523|||||||||
26185|Tulcumba Sandstone|48926|6|Mentioned|p57|||P41 et seq.||||||
26185|Tulcumba Sandstone|50132|5|Briefly described|p246 Fig. 4, p247 Fig. 5, p248 Fig.6|Early Carboniferous|Early Carboniferous|New England Fold Belt, Manilla area||||Overlies the Mandowa Mudstone. Underlies the Namoi Formation at Keepit Dam.||
26185|Tulcumba Sandstone|61776|6|Mentioned|p197|||||||||
26185|Tulcumba Sandstone|63832|5|Briefly described|p131 fig 2|Tournaisian|Tournaisian|Werrie Syncline, Southern New England Fold Belt.||||Is overlain by Namoi Formation.||14-DEC-17
26185|Tulcumba Sandstone|64631|5|Briefly described|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Belt, Werrie Syncline. Some biostratigraphic age control at top of unit.||||Is overlain by Namoi Formation.||
26185|Tulcumba Sandstone|65902|4|Described|p195 Fig.2, p199, p203 Fig.7|Tournaisian|Tournaisian|Overlies Mandowa Mudstone. Overlain by Rangari Limestone or, where this is absent, Namoi Formation. Shallow marine feldspathic sandstone. Ammonoids and conodonts date to late Tournaisian.||||||09-MAR-12
26185|Tulcumba Sandstone|66720|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|||Unit in Parry Group.|Includes Rangari Limestone Member.||Coarse- to fine-grained, cross-bedded feldspathic to quartzofeldspathic sandstone, siltstone, polymict conglomerate, calcareous mudstone, and limestone.|
26185|Tulcumba Sandstone|68003|5|Briefly described|p32 Fig.3-h, p138. |Tournaisian|Tournaisian|Tamworth Belt (North), New England Fold Belt. Coeval with Luton Formation.||Unit in Parry Group.|Includes Rangari Limestone Member.|Overlies Mandowa Mudstone. Is overlain by Namoi Formation.|Coarse, cross-bedded feldsarenite, siltstone, conglomerate, calcareous mudstone, oolitic and bioclastic limestone.|
26185|Tulcumba Sandstone|68005|4|Described|p49 Fig.3-M, p54, p147, p170.|Early Carboniferous|Early Carboniferous|Tamworth Belt. Broadly equivalent to Luton Formation north of Barraba.||Unit in Parry Group.|Includes Rangrai Limestone Member.|Overlies Tangaratta and Luton Formations. Locally overlies the Mandowa Mudstone unconformably. Is overlain by Namoi Formation.|Basal conglomerate; fining up into sandstones and limestones towards the top of the unit.|
26185|Tulcumba Sandstone|69793|6|Mentioned|p1121 Fig.12|Tournaisian|Tournaisian|Werrie Block, Tamworth Belt.||||||
26185|Tulcumba Sandstone|70050|6|Mentioned|p318|||Werrie Syncline.||||||
26185|Tulcumba Sandstone|70728|5|Briefly described|p265|Tournaisian|Tournaisian|Geological province: North Tamworth terrane, New England Orogen.||||Overlain by Namoi Formation.||
26185|Tulcumba Sandstone|70907|5|Briefly described|p773, p774 Fig.2|Carboniferous|Carboniferous|||||Is overlain by Namoi Formation.||
26185|Tulcumba Sandstone|71628|6|Mentioned|p18-20|||||Parry Group.||||
24539|Tullamore Intrusive Complex|730|6|Mentioned|p22 Fig.5.|||||||||11-NOV-14
24539|Tullamore Intrusive Complex|40365|2|Defined|p330|Early Devonian|Early Devonian|||||||
24539|Tullamore Intrusive Complex|40682|6|Mentioned|Fig.1|||||||||
24539|Tullamore Intrusive Complex|42912|6|Mentioned|Fig.1|||||||||
79334|Tullamullen Coal Member|70791|5|Briefly described|p275, p283, p286-287, p293-294|Cisuralian|Cisuralian|New name. Mullaley Sub-basin. 0.5-4m thick. Borehole cross-sections and long-sections; correlations. Coal properties not described. In situ coal estimates.||||||
26960|Tullerah Sandstone Member|22857|4|Described|p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Silverdale Formation. Crystal tuff, tuffaceous sandstone. Max. thickness: 3.9m. Geological Province: Canberra-Yass Shelf. ||||||
26960|Tullerah Sandstone Member|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
26960|Tullerah Sandstone Member|35386|4|Described|p28|||Part of Silverdale Formation||||||
26960|Tullerah Sandstone Member|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
26960|Tullerah Sandstone Member|40328|4|Described|p110|||||||||
26960|Tullerah Sandstone Member|45075|6|Mentioned|p6|||||||||
26960|Tullerah Sandstone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yanawe Formation (Douro Group). Crystal tuffs and tuffaceous sandstone, being a matric-rich micaceous quartz felsarenite, with minor volcanic fragments.||||||25-AUG-16
26960|Tullerah Sandstone Member|68592|2|Defined|p430 Fig.89, p434-5, p515, p523-58|Ludlow|Ludlow|Link (1970, 1971) named this unit in his Silverdale Formation. Here transferred from Silverdale Formation (Hattons Corner Group) to Yanawe Formation (Douro Group). Type section described. 2.3m thick in type section. Unfossiliferous. Early Ludlow age inferred from stratigraphic relationships. Mis-spelt as Tullerah Road Sandstone Member on p434.||Topmost unit in Yanawe Formation.||Gradationally overlies Gums Road Limestone Member. Is overlain conformably by Bowspring Limestone Member (Silverdale Formation).|White-grey, medium- to very fine-grained, arkosic to volcanic sandstone; beds typically 5-20cm thick, internally massive and featureless.|
26960|Tullerah Sandstone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdwt[asterisk]. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Yanawe Formation (upper unit)||Is overlain by Bowspring Limestone Member (Silverdale Formation). Overlies Gums Road Limestone Member.|Thin-medium bedded, massive, medium-very fine grained arkosic to volcaniclastic sandstone.|
26960|Tullerah Sandstone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||White-grey, thin-medium bedded, massive, medium-very fine grained arkosic to volcaniclastic sandstone.|25-AUG-16
26960|Tullerah Sandstone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Medium bedded, massive, medium-very fine grained arkosic and volcaniclastic sandstone.|
35612|Tullibigeal Leucitite|61964|2|Defined|p14 Fig. 4, p144-151|Late Miocene|Middle Miocene|Originally "Lake Cudgelligo Leucite Basalt" (Stonier 1894), then "Weja Hill Leucitite" (Scott 2000b). Detailed lith.included. Parts overlie Kikoira Granite, Wagga Gp units, Melbergen Sst, Jimberoo Fm and Mailman Gap Member (Cocoparra Group). Age: 14-10Ma.||||||09-OCT-08
35612|Tullibigeal Leucitite|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Fine-grained, dark grey to black olivine-phyric leucitite.||||||25-MAR-08
35612|Tullibigeal Leucitite|64568|5|Briefly described|Map legend|Cenozoic|Cenozoic|Fine-grained dark-grey to black olivine-phyric leucitite; with 3 unnamed subunits of: leucitite; scoriaceous leucitite clasts and fine-grained; and, microcrystalline leucitite/abundant micro-phenocrysts of leucitite/traces of olivine phenocrysts.||||||19-NOV-08
35612|Tullibigeal Leucitite|69160|5|Briefly described|Map legend|Tertiary|Tertiary||||||Fine-grained dark grey to black olivine-phyric leucitite.
|
35612|Tullibigeal Leucitite|69161|5|Briefly described|Map legend|Tertiary|Tertiary||||||Fine-grained dark grey to black olivine-phyric leucitite.|
35612|Tullibigeal Leucitite|69164|5|Briefly described|Map legend|Tertiary|Tertiary||||||Fine-grained dark grey to black olivine-phyric leucitite.|
35612|Tullibigeal Leucitite|71693|5|Briefly described|Map legend; p2.|Neogene|Paleogene|Sub-aerial eruptions; subsequently leached to form magnesite deposits.|||||Fine-grained grey to black olivine-phyric leucitite (emplaced as lava) with sporadic sandstone country-rock clasts, basal thermally oxidised scoria breccia.|
74597|Tumboramboro Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Tumboramboro Suite. Coarse-grained, massive to protomylonitic, equigranular to sparsely porphyritic muscovite-biotite granite to granodiorite.||||||
74597|Tumboramboro Granite|68592|2|Defined|p88, p611, p1542-7, p1593, p1664, p1672|Early Devonian|Early Devonian|See also p104-5, p277, p293-4. This name was first used by students working in the Abercrombie River area (Dunnet, 1961; Gemuts, 1961; Grady, 1961). Subsequent, mis-spelt, variations include Tamboramboro Granodiorite (Packham, 1968); Tamboramboro Granite (various authors in Packham, 1969); Tamberamboro Granite (Stevens, 1972); Wologorong-Tumboramboro Granite (Scheibner, 1973). Published here for the first time using the correct geographic name. The northern tip of the unit was referred to as Wologorong Granite by Wallace et al. (in Pogson and Watkins, 1998). Type pluton for Tumboramboro Suite. Exposed as large tors and boulders, river-cut platforms and tombstone-style outcrops. Type locality described. Lithologies and deformation structures described in detail. Apparent magma mixing and contemporanerous emplacement with Burridgee Diorite. Geochemistry briefly described; geophysical properties descibed.||Unit in Tumboramboro Suite.||Intrudes Abercrombie and Cuddyong Formations and Burridgee Diorite. Is intruded by Bishopthorpe Suite and Burridgee Diorite. Is faulted against, and abuts Balmeringa Granite, probably gradationally.|Pale grey to cream, coarse-grained, equigranular, muscovite- or biotite-rich granites to biotite-rich granodiorite. Either weakly peraluminous S-type granites or heavily sediment-contaminated I-type.|
74597|Tumboramboro Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dtt. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.||Tumboramboro Suite|||Medium-coarse grained, massive-protomylonitic, equigranular-sparsely porphyritic, muscovite-biotite granite to granodiorite. Low to high K, Th and U; low magnetic susceptibility.|
74597|Tumboramboro Granite|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Wologorong Supersuite||||
74597|Tumboramboro Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Tumboramboro Suite|||Medium-coarse grained, massive to protomylonitic, equigranular to sparsely porphyritic, muscovite-biotite granite to granodiorite, low to high K, Th and U. Low magnetic susceptibility.|
74597|Tumboramboro Granite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Tumboramboro Suite|||Medium-coarse grained, massive-protomylonitic, equigranular-sparsely porphyritic, muscovite-biotite granite to granodiorite. Low to high K, Th and U; low magnetic susceptibility.|
69874|Tumboramboro Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes Tumboramboro and Ghost Rocks Granites, Fullerton Gneiss, Cooks Vale and Balmeringa Granites, and unnamed porphyritic rhyolite dykes...||||||09-SEP-08
69874|Tumboramboro Suite|68592|2|Defined|p1228, p1542, p1569-99|Early Devonian|Early Devonian|New unit, after Tumboramboro Granite. Makes up the northern part of Wologorong Batholith. Fullerton Gneiss is included because of its close geographic and intimate geological relationship with Balmeringa Granite. Geochemistry and deformation structures, particularly the Turkey Hill Shear Zone, detailed. No known resources.||Unit in Wologorong Supersuite.|Includes Tumboramboro, Ghost Rocks, Cooks Vale and Balmeringa Granites and Fullerton Gneiss.|Intrudes Abercrombie and Cuddyong Formations. Is overlain by Crookwell Granite.|Pale-grey to cream, medium- to coarse-grained, equigranular to sparsely porphyritic, muscovite-biotite and biotite granite and granodiorite; unstrained to mylonitic; metasedimentary xenoliths common. Granitic and rhyolitic dykes. S-type.|
69874|Tumboramboro Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Includes one unnamed member of porphyritic rhyolite dykes. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Balmeringa Granite, Cooks Vale Granite, Fullerton Gneiss, Ghost Rocks Granite, Tumboramboro Granite.|||
69874|Tumboramboro Suite|70542|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Tumboramboro Granite.|||
69874|Tumboramboro Suite|70543|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed member of porphyritic rhyolite dykes.|||Includes Balmeringa Granite, Cooks Vale Granite,Fullerton Gneiss, Ghost Rocks Granite, Tumboramboro Granite|||
69874|Tumboramboro Suite|70544|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Cooks Vale Granite|||
26961|Tumut Pond Group|22857|5|Briefly described|p454 App.1, Tb.A1.6|Silurian|Silurian|Contains graptolites. Geological Province: Tumut Trough.||||||10-MAR-06
26961|Tumut Pond Group|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
26961|Tumut Pond Group|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
26961|Tumut Pond Group|31161|5|Briefly described|PA5|||||||||
26961|Tumut Pond Group|32671|6|Mentioned|Map legend|Silurian|Ordovician|Ordovician-Silurian||||||
26961|Tumut Pond Group|32672|6|Mentioned|p672|||||||||
26961|Tumut Pond Group|33001|6|Mentioned|p64|||||||||
26961|Tumut Pond Group|33004|6|Mentioned|p175|||||||||
26961|Tumut Pond Group|33325|5|Briefly described|Table 2|||Age uncertain P11.||||||
26961|Tumut Pond Group|33874|6|Mentioned|p5|||||||||
26961|Tumut Pond Group|34404|6|Mentioned|p92|||Silurian||||||
26961|Tumut Pond Group|34405|5|Briefly described|p114|||Fig.3.13||||||
26961|Tumut Pond Group|35070|6|Mentioned|p165|||||||||
26961|Tumut Pond Group|37727|4|Described|p91|||Formerly Tumut Pond Beds||||||
26961|Tumut Pond Group|40328|4|Described|p45|||||||||
26961|Tumut Pond Group|40497|6|Mentioned|Map legend|Silurian|Silurian|||||||
26961|Tumut Pond Group|40498|6|Mentioned|p364|||See also P416||||||
26961|Tumut Pond Group|60086|5|Briefly described|Map legend|Silurian|Silurian|||||||19-JUL-04
29524|Tunbridge Wells Diorite|13139|5|Briefly described|p3 Fig. 2|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
29524|Tunbridge Wells Diorite|23214|3|Fully described|p86|Late Ordovician|Late Ordovician|Intrudes the Weemalla Formation.  Newcrest Mining Ltd. considered this to be an earlier part of the Cadia Hill Monzonite intrusive suite; No geochemical data available. Identified as Phase 4.||||||
29524|Tunbridge Wells Diorite|43640|5|Briefly described|Map Legend||Ordovician|||||||
29524|Tunbridge Wells Diorite|43782|6|Mentioned|Map Legend|Eastonian|Eastonian|||||||
29524|Tunbridge Wells Diorite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
38124|Tupia Formation|24343|2|Defined|p68 App. 1|Miocene|Miocene|Max. known thickness: 5.4m.   Overlies Little Bay Shale||||||
23064|Turill Coal Member|68004|5|Briefly described|p61.|Late Permian|Late Permian|Western Coalfield. From 1.5 to 4 m thick. Is 600 metres deep at Cassilis. See also reference to "Turill seam" p220.||Unit in State Mine Creek Formation.|||Dull coal with bright layers and numerous thin carbonaceous claystone layers in lower half, and moderately thick carbonaceous and tuffaceous claystone layers in the upper half.|
76174|Turkaro Range Conglomerate Member|66623|2|Defined|p147, pp216-222. |Givetian|Givetian|Defined in this study; one of three contemporaneous basal units of Ravendale Formation. Correlated with Rocky Tank Conglomerate Member and Gum Creek Member. About 380 m thick. Contains Skolithos tube trace fossils. Represents the first stage of a new sedimentary sequence after the Tabberabberan Orogeny. ||Basal unit in Ravendale Formation.||Unconformably overlies Wana Karnu Group; overlies Grey Range Group with a strong angular discordance.|Upward fining basal red-bed sequence of conglomerates, sandstones and siltstones; boulders of Teltawongee Group sandstones to 1 m in basal conglomerates; minor pale buff sandstones to 600 mm thick occur intermittently in middle of the sequence.|
76174|Turkaro Range Conglomerate Member|70648|5|Briefly described|Map Legend|Devonian|Devonian|||Ravendale Formation|||Upward fining basal red-bed sequence of conglomerate, sandstone and siltstone, minor buff sandstone with skolithos tubes.|20-JAN-22
29082|Turon River Grits|22472|6|Mentioned|p38 Fig.3(a)|Late Devonian|Devonian|of the Lambie Group||||||
29082|Turon River Grits|22857|5|Briefly described|p492 App.1 Tb.A1.7|Devonian|Devonian|Of the Lambie Group. Oligomictic to polymictic conglomerate, coarse arenite and mudstone. Max. thickness: 140m. Geological Province: Lambie Basin.||||||
29082|Turon River Grits|23214|3|Fully described|p242|Late Devonian|Late Devonian|Of Lambie Group, Lambie Basin. Massive clast-supported conglomerate.  Overlying unit: Morgans Gully Siltstone, Underlying unit: Slowmans Creek Conglomerate. Max. thickness: 140m.||||||
29082|Turon River Grits|32708|6|Mentioned|Fig.2|||||||||
29082|Turon River Grits|35166|6|Mentioned|Fig.3|||||||||
29082|Turon River Grits|43641|5|Briefly described|Map Legend||Devonian|||||||
29082|Turon River Grits|43782|5|Briefly described|Map Legend|Famennian|Famennian|of Lambie Group.||||||
29082|Turon River Grits|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Lambie Group||||
32519|Turondale and Waterbeach Formations undiff.|43639|5|Briefly described|Map Legend|Devonian|Devonian|||||||
32519|Turondale and Waterbeach Formations undiff.|43641|5|Briefly described|Map Legend||Devonian|Crudine Group.||||||
32519|Turondale and Waterbeach Formations undiff.|43653|5|Briefly described|Map Legend||Devonian|of Crudine Group||||||
32519|Turondale and Waterbeach Formations undiff.|43654|5|Briefly described|Map Legend||Devonian|Of Crudine Group. Feldspathic volcaniclastics, greywacke, slate.||||||17-JUL-08
32519|Turondale and Waterbeach Formations undiff.|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
27918|Tuross Head Tonalite|22606|6|Mentioned|P827|||||||||
27918|Tuross Head Tonalite|22778|5|Briefly described|p 168|||Moruya Suite.||||||15-DEC-08
27918|Tuross Head Tonalite|22815|4|Described|p89,90|||||||||
27918|Tuross Head Tonalite|22933|6|Mentioned|p13|||||||||
27918|Tuross Head Tonalite|23439|6|Mentioned|p126|||||||||
27918|Tuross Head Tonalite|23549|5|Briefly described|p521|||Of the Moruya Suite. Quartz diorites.||||||15-DEC-08
27918|Tuross Head Tonalite|35109|6|Mentioned|p71|||||||||
27918|Tuross Head Tonalite|35248|4|Described|p238|||Mention Fig.1||||||
27918|Tuross Head Tonalite|39240|6|Mentioned|Fig.6|||||||||
27918|Tuross Head Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
27918|Tuross Head Tonalite|41456|5|Briefly described|p2|||||||||
27918|Tuross Head Tonalite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Moruya Suite.||||||
27918|Tuross Head Tonalite|50553|5|Briefly described|p1334|||Part of Moruya Batholith. Jointing described.||||||
27918|Tuross Head Tonalite|64571|6|Mentioned|p834|||||||||
27918|Tuross Head Tonalite|66575|6|Mentioned|p961,|||A 20:80 ration of mantle and lower crustal components could produce elemental and isotopic compositions similar to this unit.||||||
67914|Turrallo Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes the Forest Lodge Quartz Monzodiorite and an unnamed unit. Mainly quartz monzodiorite and monzonite.||||||19-JUN-08
67914|Turrallo Suite|68592|2|Defined|p74 Tb.5, p1650-63, p1666-7, p1669|Early Devonian|Early Devonian|See also p803, p827, p845 Fig.141, p852 Fig.143. First used, mis-spelt, as Turallo, in Chappell et al. (1991); their Forest Lodge Suite is also included in the current definition. Named after Turrallo Creek, 12km SW of Taralga. The Forest Lodge Quartz Monzodiorite is the type pluton. Includes five main bodies and several smaller intrusions and dykes. Predominantly intermediate in composition. Geochemistry detailed. Typically crop out as scattered low blocks and boulders, with larger tors in places. Goulburn structural zone: deformation described.|||Includes Forest Lodge Quartz Monzodiorite.|Intrudes Woodlawn Volcanics and Boxers Creek Formation. Locally overlain by Crookwell Basalt.|Monzodioritic to dioritic intrusions: mineralogy typically includes clinopyroxene, orthopyroxene and hornblende.|
67914|Turrallo Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Includes one unnamed member of porphyritic quartz monzodiorite to diorite with phenocrysts up to 5mm of plagioclase with lesser augite and hornblende; miarolitic cavities present. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Forest Lodge Quartz Monzodiorite and one unnamed member.|||
67914|Turrallo Suite|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed subunit of quartz monzodiorite to diorite with phenocrysts of plagioclase and lesser augite and hornblende.|||Includes Forest Lodge Quartz Monzodiorite and one unnamed member.|||
67914|Turrallo Suite|70543|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed member of porphyritic quartz monzodiorite to diorite with phenocrysts up to 5mm of plagioclase with lesser augite and hornblende; miarolitic cavities present.|||Includes Forest Lodge Quartz Monzodiorite and one unnamed member|||
67914|Turrallo Suite|71069|6|Mentioned|p135, p156, p163|Early Devonian|Early Devonian|Misspellt as Turallo Suite on p135.||||Intrudes the Woodlawn Volcanics, Mount Fairy Group.|Dioritic intrusions.|
67914|Turrallo Suite|71700|5|Briefly described|p24|||Rhyolitic to dacitic pyroclastic rocks, andesite lavas and proximal volcaniclastics in Braidwood 1:100k are interpreted to be related to this suite.|||||Quartz monzodiorite intrusions.|
82690|Tuting Monzogranite|71628|4|Described|p17: 1; p19: 164-166|||Name is formalised in this study; appeared informally as Tuting monzogranite in Anchor Resources Limited (2014). Previously included within Billys Creek Granodiorite. Named after Tuting trig on a hill/mountain of that name. Occurs 3 km N of Dundurrabin. This 250 Ma age determination is anomalous and needs verification. Is associated with W-Mo-Cu-(Au-Bi-Te) mineralisation.|250 Ma (U-Pb; Anchor Resources Limited 2014).|Tuting Suite.||Intrudes Brooklana beds.|Biotite monzogranite.|
32250|Twins Creek Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh6||||||
32250|Twins Creek Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
83262|Two-Thirty breccia complex|73287|5|Briefly described|p659, p664, p667-668, p671-672, p675-677|Llandovery|Llandovery|Occurs in a subvertical pipe like structure with three major breccia facies and four cemented breccia subfacies described. Identified cement phases indicate five phases of cementation and brecciation. Two-Thirty porphyry interpreted as projenitor of the breccia complex, includes clasts from the Goonumbla Volcanics and Two-Thirty porphyry. Dated molybdenite is coeval with the post-mineralisation zero porphyry, interpreted as product of a late hydrothermal overprint. Location in text includes p680.|438.9+/-1.4 Ma Re-Os (Mo)|||Intrudes the Goonumbla Volcanics.|Comprises dominantly polymict magmatic-hydrothermal breccias with significant variation, containing cemented, igneous cemented and tectonic-hydrothermal breccia facies; contains Cu-Au (Mo) mineralisation and variable syn-brecciation alteration.|
83259|Two-Thirty intrusive complex|73287|4|Described|p659,664, 666, p670 Tb.6, 675, 677-678|Llandovery|Ordovician|Intrusive phases divided into pre-, syn-, and post-mineralisation. Syn-mineralisation porphyries emplaced between 448 +/- 4.5 Ma and 447.1 +/- 4.5 Ma. Additional zircon U-Pb ages: 447.3+/-4.5 Ma, 448.0+/-4.5 Ma. Includes mafic, aplite and minor pebble dykes. Location in text includes p659, p673 Fig.10, p674 Fig.11, p680. Two-Thirty Intrusive complex used on p663.|450.5+/-4.5 Ma, 438.8+/-4.4 Ma zircon U-Pb||Two-Thirty porphyry, Zero porphyry|Intrudes the Goonumbla Volcanics.|Contains ten intrusive phases, including six monzonite to quartz-monzonite porphyries, some are hornblende-biotite bearing and K-feldspar-phyric, variably altered and with disseminated mineralisation in parts.|
83264|Two-Thirty porphyry|73287|5|Briefly described|p659, p667, p669-670, p676-677, 679-680|Ordovician|Ordovician|Interpreted to be progenitor of the Two-Thirty breccia complex, predates mineralisation. Location in text includes p668 Fig.6, p671 Fig.8, p672, p673 Fig.10, p674 Fig.11. See also Two-Thirty Porphyry.|448.0+/-4.5 Ma zircon U-Pb|Two-Thirty intrusive complex|||Brick red, moderately crystal crowded, feldspar phyric monzonite porphyry with euhedral K-feldspar and plagioclase; pervasive potassic alteration and hematite dusting; contains xenoliths, disseminated and veinlet mineralisation.|
37916|Tycannah Rhyodacite Member|24605|2|Defined|p931, p953 App.1|Westphalian|Westphalian|Of the Lark Hill Formation. Thickness: ~5m. Geological Province: New England Orogen.||||||
80918|Tyringham East Granodiorite|71628|4|Described|p17: 2, 51-53|||Previously the informal Tyringham East granite of Chisholm et al. (2014), after the Tyringham East anomaly/intrusive of Anchor Resources Limited (2014). Renamed and formalised in this study. Named after the Tyringham East prospect. Occurs ~3 km W of Dorrigo. The limited (one analysis) geochemistry is described. Is associated with intrusion-related gold system (Au-Bi-Te-[Mo-W]).|236.5 +/- 1.6 Ma (SHRIMP: Chisholm et al., 2014).|Billys Creek Suite.||Intrudes Moombil Siltstone.|Dark grey, massive, fine- to medium-grained granite; probably granodiorite or tonalite; extensive biotite or sericite alteration. I-type.|
32528|Ulan Quartz Monzonite|23043|5|Briefly described|Map Legend|Namurian|Visean|of Gulgong Plutonic Suite.||||||
32528|Ulan Quartz Monzonite|23170|2|Defined|p272|Carboniferous|Carboniferous|Age: SHRIMP date 323+/- 7 Ma. of Gulgong Plutonic Suite.||||||
32528|Ulan Quartz Monzonite|68003|5|Briefly described|p24 Fig.3-e, p42, p140.|Visean|Visean|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gulgong Plutonic Suite.||Is overlain by Narrabeen Group.|Megacrystic biotite subporphyritic quartz monzonite.|
32528|Ulan Quartz Monzonite|68004|6|Mentioned|p137, p210.|||Hosts a number of residual kaolin deposits in the Gulgong area.||||||
28302|Ulandra Granite|22638|2|Defined|p45|Early Silurian||||||||12-FEB-09
28302|Ulandra Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
28302|Ulandra Granite|40328|4|Described|p211|||||||||
28302|Ulandra Granite|42726|5|Briefly described|map legend|Silurian||||||||
28302|Ulandra Granite|44192|5|Briefly described|Map Legend|Wenlockian|Llandoverian|||||||
28302|Ulandra Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
28302|Ulandra Granite|50191|6|Mentioned|p21 Fig. 1|Silurian|Silurian|||||||
28302|Ulandra Granite|69801|6|Mentioned|p52|||Eastern Lachlan Orogen. Rocks mapped as belonging to this granite are now regarded as Yammatree Granite.||||||
31650|Ulandra Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
31650|Ulandra Suite|44093|5|Briefly described|p182 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
31650|Ulandra Suite|44192|5|Briefly described|Map Legend|||||||||
31650|Ulandra Suite|69801|6|Mentioned|p52||||||Ulandra Granite|||
25564|Ulinbawn Conglomerate Member|22857|5|Briefly described|p440 App.1, Tb.A1.6|Devonian|Devonian|Of the Rast Group (Cobar Supergroup). Muddy cobble conglomerate and siltstone. Max. thickness: 30m.||||||
25564|Ulinbawn Conglomerate Member|41394|2|Defined|p73|Early Devonian||Reserved as Ulinbawn Member||||||
25564|Ulinbawn Conglomerate Member|41395|6|Mentioned|Map legend|Lochkovian||||||||
25564|Ulinbawn Conglomerate Member|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
25564|Ulinbawn Conglomerate Member|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Of Boothumble Formation?||Equivalent to Boothumble Formation, Mount Knobby Formation||
70038|Ulinda Sandstone Member|22857|5|Briefly described|p518 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Digby Formation. Max. thickness: 73m. Geological Province: Gunnedah Basin.||||||
70038|Ulinda Sandstone Member|43194|5|Briefly described|p133 App. 1|Early Triassic|Early Triassic|Newly defined member within the Digby Formation. Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||
29086|Ulladulla Mudstone|29752|6|Mentioned|p29|||||||||
29086|Ulladulla Mudstone|30153|6|Mentioned|p154|||Fauna. See also P156||||||
29086|Ulladulla Mudstone|30449|6|Mentioned|p16|||Brachiopods||||||
29086|Ulladulla Mudstone|30450|6|Mentioned|Table 1|||Permian. Sydney Basin||||||
29086|Ulladulla Mudstone|31081|2|Defined|p65|late Artinskian|late Artinskian|See also P66-69Prob.Late Artinskian||||||
29086|Ulladulla Mudstone|32769|6|Mentioned|Fig.1|||||||||
29086|Ulladulla Mudstone|32943|6|Mentioned|p87|||See also Fig.2 & P105||||||
29086|Ulladulla Mudstone|32945|6|Mentioned|p79|||See also PP83-89. Permian. Conjola Subgroup.||||||
29086|Ulladulla Mudstone|34084|6|Mentioned|p368|||Perm.||||||
29086|Ulladulla Mudstone|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
29086|Ulladulla Mudstone|34211|6|Mentioned|p32|||||||||
29086|Ulladulla Mudstone|34568|6|Mentioned|p218|||Permian||||||
29086|Ulladulla Mudstone|34569|6|Mentioned|p11|||Permian||||||
29086|Ulladulla Mudstone|35145|6|Mentioned|p84|||||||||
29086|Ulladulla Mudstone|35490|6|Mentioned|p118|||||||||
29086|Ulladulla Mudstone|36042|6|Mentioned|Fig.13|||||||||
29086|Ulladulla Mudstone|38227|6|Mentioned|p426|||||||||
29086|Ulladulla Mudstone|38505|6|Mentioned|Fig.7|||||||||
29086|Ulladulla Mudstone|38586|6|Mentioned|p25|||||||||
29086|Ulladulla Mudstone|38917|6|Mentioned|p173|||||||||
29086|Ulladulla Mudstone|39267|6|Mentioned|p236|||||||||
29086|Ulladulla Mudstone|41666|6|Mentioned|p15|||||||||
29086|Ulladulla Mudstone|41902|6|Mentioned|p20|||||||||
29086|Ulladulla Mudstone|43345|14|Not recorded|p3 Table 1||Permian|||||||
29086|Ulladulla Mudstone|43346|14|Not recorded|p2|||||||||
29086|Ulladulla Mudstone|43475|14|Not recorded|p553||Permian|||||||
29086|Ulladulla Mudstone|43491|14|Not recorded|pVII/50||Permian|||||||
29086|Ulladulla Mudstone|45090|5|Briefly described|p164|||Age & correlation||||||
29086|Ulladulla Mudstone|48940|6|Mentioned|p99|||||||||
33389|Umagarlee Monzodiorite|23043|5|Briefly described|Map Legend|Namurian|Tournaisian|||||||
33389|Umagarlee Monzodiorite|23170|4|Described|p267|Carboniferous|Carboniferous|of Lachlan Fold Belt.||||||
25566|Umbiella nephelinite|33349|6|Mentioned|p683|||||||||
26966|Unanderra Coal Member|29900|5|Briefly described|p168|||||||||
26966|Unanderra Coal Member|29901|4|Described|Table 1|||||||||
26966|Unanderra Coal Member|30006|6|Mentioned|p7|||||||||
26966|Unanderra Coal Member|32849|6|Mentioned|Table 1|||Permian||||||
26966|Unanderra Coal Member|33869|6|Mentioned|Fig.2|||||||||
26966|Unanderra Coal Member|36220|6|Mentioned|p38|||See also Table 10 & P38.||||||
26966|Unanderra Coal Member|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
26966|Unanderra Coal Member|37089|6|Mentioned|p208|||||||||
26966|Unanderra Coal Member|39661|6|Mentioned|Fig.1|||||||||
26966|Unanderra Coal Member|42182|5|Briefly described|p300|||||||||
26966|Unanderra Coal Member|42787|6|Mentioned|Table 1 P126|||||||||
26966|Unanderra Coal Member|45090|6|Mentioned|p224|||L. Tatarian||||||
26966|Unanderra Coal Member|71115|5|Briefly described|p180|Permian|Permian|Southern Sydney Basin.||Pheasants Nest Formation.||Overlies Berkeley Latite Member (Gerringong Volcanics). Is overlain by Figtree Coal Member.||
24054|Underbank Mudstone Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Of the Flagstaff Formation. Fossiliferous grey to black mudstone interbedded with fine to medium-grained lithic sandstone. Max. thickness: 520m. Geological Province: Tamworth Forearc Basin.||||||
24054|Underbank Mudstone Member|40883|6|Mentioned|p7|||||||||
24054|Underbank Mudstone Member|43576|6|Mentioned|p350|||||||||
24054|Underbank Mudstone Member|44244|4|Described|p68|Visean|Visean|Of the Flagstaff Formation.  Fossiliferous grey to black mudstone interbedded witn fine to medium-grained lithic sandstone.  Max. thickness: 520m; 430m in type section.  Type section in text.  Geological Province: Gresford Block.||||||
24054|Underbank Mudstone Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Flagstaff Formation. Grey to black, thinly bedded fossiliferous mudstone and minor interbedded lithic sandstone. Geological Province: Gresford Block||||||
41352|Undercliffe Falls Monzogranite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Moonbi Suite.  Previously known as Bungulla Porphyritic Adamellite.||||||
41352|Undercliffe Falls Monzogranite|61790|6|Mentioned|p318, p319, p320|||Not intended as a formal name, more of a petrology descriptor, phase of Undercliffe Falls Adamellite.||||||27-OCT-08
41352|Undercliffe Falls Monzogranite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Greyish pink to pinkish grey, mediuym- to fine-grained (groundmass), coarsely porphyritic titanite-hornblende-biotite monzogranite to granodiorite; with pink K-feldspar megacrysts; mafic enclaves common; high magnetic response.||||||30-JAN-09
41352|Undercliffe Falls Monzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca 245, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
41352|Undercliffe Falls Monzogranite|69639|5|Briefly described|p80, p157, p192, p222|||New England Orogen. Considered to be identical to the Bungulla Monzogranite and geochemically similar to the Bookookoorara Monzogranite. In contact with the Cullendore Granite, although the relationship between the two is unclear.||||||
41352|Undercliffe Falls Monzogranite|71628|4|Described|p7: 1; p11: 1-2, 5, 7, 9, 12, 14, 24|||See also p11: 35-46; p15: 1, 32-33, 37-38, 40, 52-54, 56-57, 59, 68-69, 115-116; p16: 1-4, 6-14, 16, 18-20, 22; p19: 80-83, 87, 102. Barnes (1987). Included in the Moonbi Plutonic Suite by Shaw and Flood (1981). Referred to more recently by NSWGS (e.g. Henley et al., 2001) as Bungulla Monzogranite. Named after a local geographic feature. Comprises two masses, Undercliffe Falls and Boorook (described). Forms whalebacks and tors in gently undulating hills. Geochemistry described; similar to Bungulla Monzogranite. RELATED UNITS (continued): Is intruded by Mount Lindesay and Jenners Monzogranites (Stanthorpe Complex) and Cullendore Syenogranite. Abuts Stanthorpe Complex.|245.4 Ma (Rb-Sr biotite: Shaw and Flood, 1993).|Bungulla Suite.||Intrudes and is faulted against Drake Volcanics and Razorback Creek Mudstone. May intrude The Ridge Monzogranite. Has a complex boundary with Karonstadt Complex (detailed). See COMMENTS for more.|Medium- to coarse-grained, strongly porphyritic biotite-hornblende granodiorite-monzogranite characterised by abundant pink, and locally white, K-feldspar phenocrysts, enclaves and megascopic titanite. Described in great detail. I-type.|
67894|Uralla Supersuite|24513|5|Briefly described|p10|Early Triassic|Late Permian|Speckled black and white and equiganular granites.||||||25-MAY-05
67894|Uralla Supersuite|62534|5|Briefly described|p11 (legend), p16|Early Triassic|Late Permian|Includes Tingha Monzogranite, Wellingrove Granodiorite and Wards Mistake Monzogranite. I-type. Occurs as scattered bodies throughout the survey area.||||||07-FEB-11
67894|Uralla Supersuite|62757|5|Briefly described|p1-2, p13 Fig. 5|Early Triassic|Late Permian|Plutonic suite of the New England Batholith. Age: 251-243Ma. Transitional between S-type and I-type. Mafic granitoids.||||||07-FEB-11
67894|Uralla Supersuite|63347|5|Briefly described|p2|Middle Triassic|Late Permian|I-type granites of the New England Batholith. Geological Province: New England Orogen.||||||
67894|Uralla Supersuite|66660|6|Mentioned|p347|||New England Batholith. Contains the Mount Duval Monzogranite and the Newholme Monzogranite.||||||
67894|Uralla Supersuite|68005|5|Briefly described|p20, p60, pp64-66, pp134-135, pp169-170.|Early Triassic|Late Permian|Part of New England Batholith. Formerly a suite of Shaw and Flood (1982); redefined as a Supersuite by Bryant (2001). Transitional between S- and  I-type. Includes an association of leucogranites which host historically important metalliferous deposits and are the source of significant alluvial deposits. Bryant et al. (2002) have tentatively reclassified the Gilgai, Mole, Elsmore, Webbs Consols and Dumboy-Gragin Granites as part of this unit.|||Includes Tingha Monzogranite.||Compositionally diverse: from gabbro and diorite through to monzogranite.|
67894|Uralla Supersuite|68006|5|Briefly described|p20 Fig.3-A.|Early Triassic|Late Permian|New England Batholith, New England Fold Belt. Of Bryant (2001). I-type.|||Includes Mole, Gilgai and Tingha Granites.|||
67894|Uralla Supersuite|68111|5|Briefly described|p968 Tb.1|||Also includes Kentucky Diorite as well as Tingha, Mount Duval, Glenore, Gwydir River, and The Basin Monzogranites.|||Includes Parlour Mountain Granite, Booralong and Botumburra Range Adamellites; Yarrowyck and Uralla Granodiorites; Terrible Vale Porphyritic Microtonalite, Shalimar and Back Creek Tonalites;|||
67894|Uralla Supersuite|68679|6|Mentioned|p461|||Granitoids of this and the Hillgrove Supersuite separate the northern and southern parts of the Stanthorpe Supersuite.||||||
67894|Uralla Supersuite|69188|6|Mentioned|p1, p48, p61, p72|||Aggregates of amphibole, biotite and opaques, often with relict primary pyroxene, are typical of granitoids of this Supersuite. Geochemically similar to the Culaden Granodiorite.||||||
67894|Uralla Supersuite|69323|5|Briefly described|p1,6,13,34,69-71|Late Permian|Late Permian|Geological province: New England Orogen. I-type granitic supersuite. Also includes Gwydir River Adamellite, Parlour Mountain Granite, Tingha Adamellite, Mount Duval Monzogranite.|||Includes Balala Suite, Uralla Suite, Manuka Farm Porphyritic Microtonalite, Uralla Granodiorite, Wilhelmshohe Tonalite, Wongalee Leucogranite, Yarrowyck Suite.|||03-DEC-19
67894|Uralla Supersuite|69639|5|Briefly described|p1-p2, p32, p68, p94, p218-p220|||New England Orogen. Also includes Mount Duval Monzogranite, Newholme Monzogranite, Yarrowyck Granodiorite, Khatoun Tonalite and Llangothlin Suite.|||Includes the Wards Mistake Suite, Gwydir River Monzogranite, Tingha Monzogranite, Parlour Mountain Leucomonzogranite.||I-type granitic rocks.|
67894|Uralla Supersuite|70217|5|Briefly described|v, vi, p38, p43, p44|||New England Orogen. Nominally I-type geochemistry. Also includes the Tingha Monzogranite, Newholme Monzogranite, Terimbone Monzogranite, Khatoun Tonalite, Wards Mistake Monzogranite, Cottesbrook Monzogranite, Parlour Mountain Leucomonzogranite and the Yarrowyck Granodiorite. See also p49, p73 tbl 14.1, p75, p76.|255-251 Ma (Cross and Blevin, 2010)||Includes the Llangothlin Suite, Mount Duval Suite, Pyes Creek Leucomonzogranite|||
67894|Uralla Supersuite|71628|4|Described|p1:8, 14; p3-41; p7: 3-4, 15, 17-18|Early Triassic|Permian|See also p8: 1-119; p9-3; p10: 1-2, 7; p12-2; p13-1; p14: 1-2, 8, 12, 32; p18-18; p19: 2, 10, 28, 33, 39-41, 44, 55, 57, 79, 113, 142, 154, 169. A heterogeneous collection of granites in the central portion of the southern New England Orogen. Bryant et al. (2002) recognised four distinct spatially controlled sub-groupings within this unit. Geochemistry summarised.|255-251 Ma.|Hillgrove Supersuite.|Uralla, Mount Duval, Myanbah, Wards Mistake, Llangothlin, Primley, Shalimar, Tolleys Gully, Yarrowyck Suites.|Intrudes Tablelands Complex.|Speckled black and white, fine to coarse, equigranular to porphyritic, compositionally diverse granites: gabbro, quartz gabbro, quartz diorite, tonalite, granodiorite, to (leuco)monzogranite and (leuco)syenogranite. Reduced or contaminated I-type.|
26971|Uranquinty Granite|42497|5|Briefly described|Map legend|Wenlockian|Llandoverian|||||||
27247|Urialla Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Biotite granite. BMR map symbol: gbu.||||||
27247|Urialla Granite|24128|5|Briefly described|p122|||Geological Province: Lachlan Fold Belt.||||||
27247|Urialla Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
27247|Urialla Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
27247|Urialla Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
27247|Urialla Granite|32820|6|Mentioned|p3|||Cullarin Anticlinorium||||||
27247|Urialla Granite|33325|6|Mentioned|p18|||Michelago Gp.||||||
27247|Urialla Granite|36413|2|Defined|p109|Devonian|Silurian|Siluro-Devonian age||||||
27247|Urialla Granite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Biotite granite, massive, medium grained. GSNSW map code: gu.||||||
27247|Urialla Granite|39626|6|Mentioned|p276|||||||||
27247|Urialla Granite|39800|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
27247|Urialla Granite|40328|4|Described|p211|||||||||
27247|Urialla Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
27247|Urialla Granite|42727|5|Briefly described|map legend|Early Devonian|Pridoli|Adamellite; I-type. BMR map symbol: Sgu. Geol. Prov: Cullarin Block.||||||
27247|Urialla Granite|42820|5|Briefly described|p69|||Probable Late Silurian.||||||20-MAY-08
27247|Urialla Granite|71069|6|Mentioned|p201|||||||Equivalent to the Harrisons Peak Granite.||
31653|Urialla Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
81952|Uringery Trachyte Member|72700|5|Briefly described|Mapsheet 1|Cenozoic|Cenozoic|||Mount Naman Formation|||Porphyritic trachyte with minor aegerine and aenigmatite, Common radial columnar joints.|02-NOV-20
79961|Utah Lake Suite|71965|6|Mentioned|p902|||Geological province: Thomson Orogen. ||||||
26191|Vacy Ignimbrite Member|22857|5|Briefly described|p508 App.1 Tb.A1.8|Visean|Visean|Of the Newtown Formation (Gilmore Volcanic Group). Grey dacitic ignimbrite. Max. thickness: 20m. Geological Province: Tamworth Forearc Basin.||||||
26191|Vacy Ignimbrite Member|24121|5|Briefly described|p4, p34, p154|||Of Newtown Formation.||||||25-AUG-22
26191|Vacy Ignimbrite Member|31228|2|Defined|p81|Carboniferous|Carboniferous|||||||
26191|Vacy Ignimbrite Member|44244|5|Briefly described|p92|||Red, white and grey dacitic ignimbrite of the Newtown Formation.  Type section in text.  Geological Province: Gresford Block.  See also p88.||||||
26191|Vacy Ignimbrite Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Newtown Formation (Gilmore Volcanic Group).  Red micaceous rhyodacitic ignimbrite and grey micaceous dacitic ignimbrite.  Geological Province: Gresford Block||||||
26191|Vacy Ignimbrite Member|50268|5|Briefly described|Map Legend|Visean|Visean|Of the Newtown Formation.  Geological Province: Gresford Block.||||||
26191|Vacy Ignimbrite Member|73487|6|Mentioned|p566, p574 Fig.8|||See also Vacy Ignimbrite p583.||||||
40926|Vale View Facies|50230|5|Briefly described|Map legend|Wenlock|Wenlock|Informal name.  Of the Hawkins Volcanics (Douro Group).  Porphyritic vitric tuff with phenocrysts of quartz in an aphanitic matrix.||||||10-MAY-04
25576|Vales Point Coal|22578|6|Mentioned|Fig.9 p399, p402|||||||||
25576|Vales Point Coal|23055|6|Mentioned|p22,Fig11p23|||||||||
25576|Vales Point Coal|24158|5|Briefly described|p172 Fig.3|||Of the Newcastle Coal Measures. Geological Province: Sydney Basin||||||
25576|Vales Point Coal|35873|6|Mentioned|Fig.39|||||||||
25576|Vales Point Coal|39294|6|Mentioned|Fig. 9.2|||||||||
25576|Vales Point Coal|41463|6|Mentioned|Fig.1|||||||||
25576|Vales Point Coal|73304|6|Mentioned|p75|||||Moon Island Beach Formation, Newcastle Coal Measures||||
25576|Vales Point Coal|73625|6|Mentioned|p2|Permian|Permian|Newcastle coalfield, Sydney Basin.||||||
70050|Vales Point coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam in the Moon Island Beach Formation (Newcastle Coal Measures).||||||
70050|Vales Point coal seam|68711|5|Briefly described|p113, p117, 118, p116 Tb 2|||Informal unit. Downgraded from Vales Point Coal Member. Has been found to converge with the Wallarah coal seam. Now generally marks top of Newcastle Coal Measures. Also discussed as Vales Point seam p113. Misspelt as Vale Point coal seam p118.||Within Moon Island Beach Formation||||
76972|Valla Monzogranite|69639|6|Mentioned|p3, p118, p128, p223|Triassic|Triassic|New England Orogen.|230.7 +/- 1.6 Ma|||||
76972|Valla Monzogranite|71628|4|Described|p17: 2, 13-14, 35-43, 45|||Previously the Valla Adamellite of Leitch et al. (1971). The name was changed to Valla Monzogranite by Chappell and Bryant (1994, unpublished) to align with IUGS nomenclature. Named after the locality of Valla. Crops out ~8 km NW of Nambucca Heads, and several kilometres W of Valla Beach. The locations of several outcrop bodies are described. Lithology and mineralogy detailed; limited geochemistry described. Is associated with significant Mo, As, Au, Ag, Sb mineralisation (31 known deposits); named and discussed.|230.7 +/- 1.6 Ma (SHRIMP: Cross and Blevin, 2013).|Valla Suite.||Intrudes Nambucca beds.|Equigranular to porphyritic, fine-grained biotite granodiorite and medium-grained biotite leucomonzogranite; locally aplitic and pegmatitic variants; abundant porphyritic and microgranite dykes. I-type.|
74025|Valla Suite|71628|5|Briefly described|p17-38|||||Carrai Supersuite.|Valla Monzogranite.|||
38314|Valley View seam|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Of the Gloucester Basin Coal Measures.   Geological Province: New England Fold Belt||||||
27304|Vandon Limestone|5250|6|Mentioned|p42, p50, p57||Late Ordovician|Includes Trilobite Hill Limestone Member. ||||||
27304|Vandon Limestone|13995|5|Briefly described|p70|Ordovician|Ordovician|Probable mid-Eastonian age. Exhibits the first appearances of clathrodictyid stromatoporoids, with biogeographic relationships mainly with Asia.||Cliefden Caves Limestone Group.||||
27304|Vandon Limestone|22503|6|Mentioned|Fig.4 p646|||||||||
27304|Vandon Limestone|23214|2|Defined|p46|Eastonian|Eastonian|Of Cliefden Caves Limestone Subgroup. Composite type section. Max. thickness 51m.||||||
27304|Vandon Limestone|23736|6|Mentioned|p19|||||||||
27304|Vandon Limestone|38219|2|Defined|p309|Late Ordovician|Late Ordovician|Referred to as Large Flat Limestone member.(Osbourne,78). See Fig.2.||||||
27304|Vandon Limestone|41046|6|Mentioned|p144|||||||||
27304|Vandon Limestone|41108|6|Mentioned|Fig.2|||||||||
27304|Vandon Limestone|42479|4|Described|p108 (p7 & p8)|||||||||
27304|Vandon Limestone|42603|6|Mentioned|p60|||||||||
27304|Vandon Limestone|42612|5|Briefly described|Fig.2 P29|||||||||
27304|Vandon Limestone|43569|6|Mentioned|p477||Late Ordovician|||||||
27304|Vandon Limestone|43571|6|Mentioned|p821|||||||||
27304|Vandon Limestone|63278|5|Briefly described|p154|||Of the Cliefden Caves Limestone Subgroup. Top unit of the Cliefden Caves Limestone Subgroup.||||||07-FEB-11
27304|Vandon Limestone|63290|6|Mentioned|p400 Fig. 5(c)|||||||||
27304|Vandon Limestone|67322|5|Briefly described|Fig.5; p24|Katian|Katian|Macquarie Arc. Described by Webby and Packham (1982). Conodonts obtained throughout the limestone are of early Eastonian age. Occurs in the Cliefden Caves region. ||Of the Cliefden Caves Limestone Subgroup.||Overlies the Belubula Limestone. Overlain by the Malongulli Formation.||22-FEB-18
27304|Vandon Limestone|73208|6|Mentioned|p870 Fig.2|Late Ordovician|Late Ordovician|||Cliefden Caves Limestone Subgroup.||||
27304|Vandon Limestone|73209|5|Briefly described|p879-881, 883|Late Ordovician|Late Ordovician|The (composite) type section is in the Cliefden Caves area.||Cliefden Caves Limestone Subgroup||Overlies Belubula Limestone. Is overlain by Malongulli Formation.|Thinly-bedded, fossiliferous limestone.|
27304|Vandon Limestone|73210|6|Mentioned|p893 Fig.2|||||||||
27304|Vandon Limestone|73492|6|Mentioned|p703|Katian|Katian|T. blandus Biozone.||Cliefden Caves Limestone Subgroup||||
26973|Vane Subgroup|22601|6|Mentioned|413|Permian|Permian|Geol province Sydney Basin. Underlying unit Saltwater Creek Formation||||||
26973|Vane Subgroup|22857|4|Described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wittingham Coal Measures (Singleton Supergroup). Includes the Saltwater Creek Formation. Coal seams, siltstone, lithic sandstone, shale, conglomerate. Max. thickness: >250m. Geological Province: Sydney Basin.||||||
26973|Vane Subgroup|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26973|Vane Subgroup|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26973|Vane Subgroup|40805|6|Mentioned|Fig.2|||||||||
26973|Vane Subgroup|41010|6|Mentioned|Fig.1|||||||||
26973|Vane Subgroup|41054|6|Mentioned|p156|||||||||
26973|Vane Subgroup|41604|6|Mentioned|Fig.2|||||||||
26973|Vane Subgroup|41834|6|Mentioned|p590|||||||||
26973|Vane Subgroup|42648|6|Mentioned|p36|||||||||
26973|Vane Subgroup|42916|5|Briefly described|Table 1||Late Permian|||||||
26973|Vane Subgroup|42922|6|Mentioned|p38|||||||||
26973|Vane Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
26973|Vane Subgroup|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Of Wittingham Coal Measures, Singleton Subgroup, Hunter region, Sydney Basin.||||||
26973|Vane Subgroup|43257|5|Briefly described|Map Legend||Late Permian|Of Wittingham Coal Measures.||||||
26973|Vane Subgroup|44244|4|Described|p234|Late Permian|Late Permian|Of the Wittingahm Coal Measures.  Includes the Foybrook and Bulga Formations. Overlies Saltwater Creek Formation; underlies Archerfield Sandstone.  max. thickness: 360m.  Geological Province: Sydney basin.||||||26-AUG-04
26973|Vane Subgroup|50268|5|Briefly described|Map Legend|Tatarian|Tatarian|Geological Province: Sydney Basin.  Overlies: Saltwater Creek Formation.  Underlies: Archerfield Sandstone.  Of the Wittingham Coal Measures.||||||
26973|Vane Subgroup|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wittingham Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
26973|Vane Subgroup|61529|5|Briefly described|p854 Fig. 1b|Late Permian|Late Permian|Of the Wittingham Coal Measures. Includes Foybrook Formation. Overlain by Bulga Formation; overlies Maitland Group. Geological Province: Sydney Basin.||||||17-FEB-06
26973|Vane Subgroup|61770|6|Mentioned|p111|||Includes Foybrook and Bulga Formations.||||||25-SEP-08
26973|Vane Subgroup|68003|5|Briefly described|p38 Fig.3-j, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion. Correlative of Pamboola Formation (Gunnedah Basin), and of Nile Subgroup (Western Coalfield).||Basal unit in Wittingham Coal Measures.|Includes Bulga Formation.|Overlies Mulbring Siltstone. Is overlain by Archerfield Sandstone.|Coal seams, siltstone, lithic sandstone, shale, conglomerate.|
26973|Vane Subgroup|68004|5|Briefly described|p23 Table 1.|Late Permian|Late Permian|Hunter Coalfield.||Unit in lower part of Wittingham Coal Measures.|Includes Bulga Formation.|Overlies Mulbring Siltstone. Is overlain  by Archerfield Sandstone.||
26973|Vane Subgroup|69683|5|Briefly described|p411 Fig.2, p415, p421 Tb.4|Late Permian|Late Permian|Predicted to have maturities suitable for oil and gas generation.||Unit in Wittingham Coal Measures.|Includes Foybrook and Bulga Formations.|||
26973|Vane Subgroup|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield.||Wittingham Coal Measures.|Bulga Formation.|||
26973|Vane Subgroup|73304|6|Mentioned|p75|||||Whittingham Coal Measures, Singleton Supergroup||||
23103|Velyama Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
26192|Victoria Pass Claystone Member|31373|6|Mentioned|Table 1|||||||||
26192|Victoria Pass Claystone Member|33683|6|Mentioned|Table 1|||Narrabeen Gp.||||||
26192|Victoria Pass Claystone Member|33685|6|Mentioned|Table 2|||||||||
26192|Victoria Pass Claystone Member|34205|2|Defined|p22|Triassic|Triassic|||||||
26192|Victoria Pass Claystone Member|34209|6|Mentioned|p140|||See also P141. Triassic.||||||
26192|Victoria Pass Claystone Member|39293|6|Mentioned|Fig. 8.2|||||||||
26192|Victoria Pass Claystone Member|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
26192|Victoria Pass Claystone Member|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
35119|Victoria Tunnel coal seam|23055|6|Mentioned|p34|||||||||
35119|Victoria Tunnel coal seam|68711|5|Briefly described|p118, p116 Tbl 2|||Informal unit.||Within Adamstown Formation||||
27248|Vineyard Lookout Volcanic Agglomerate Member|29915|2|Defined|p66|Late Carboniferous|Middle Carboniferous|Middle or Upper Carboniferous||||||
33675|Waalima Granodiorite|22815|4|Described|p88|||||||||
33675|Waalima Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Unassigned pluton, Bega Batholith.||||||
30505|Wahringa Limestone Member|13139|5|Briefly described|p9 Fig. 4|Late Ordovician|Middle Ordovician|Of the Fairbridge Volcanics.  Geological Province: Western Molong Volcanic Belt.||||||
30505|Wahringa Limestone Member|13995|5|Briefly described|p70-71|Ordovician|Ordovician|Northern Molong High. Contains an early Gisbornian stromatoporoid assemblage including Labechia banksi, also known from the Sassafras Formation in Tasmania. Also contains the tabulate coral Billingsaria, resembling North American and Siberian species.||Fairbridge Volcanics.||||
30505|Wahringa Limestone Member|22857|5|Briefly described|p422 App. 1, Tb. A1.5|Ordovician|Ordovician|Of the Fairbridge Volcanics (Kenilworth Group). Carbonates around volcanic islands. Contains shelfal invertebrate fossils. Geological Province: Molong Volcanic Arc.||||||
30505|Wahringa Limestone Member|23043|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of Cabonne Group.||||||01-SEP-08
30505|Wahringa Limestone Member|23170|2|Defined|p37|Gisbornian|Darriwilian|Age: Late Darriwilian - Early Gisbornian (Ordovician). Fairbridge Volcanics. Autochthonous limestone lens.||||||
30505|Wahringa Limestone Member|23181|6|Mentioned|Fig.2|Late Ordovician|Ordovician|Max age is Middle Ordovician.||||||
30505|Wahringa Limestone Member|23213|2|Defined|p16 Fig.10|Gisbornian|Darriwilian|Initially plotted in "Cargo Andesite". In Bakers Swamp Area. Age: Late Darriwilian to Middle Gisbornian.||||||
30505|Wahringa Limestone Member|23214|5|Briefly described|p24|||Geological Province: Lachlan Fold Belt.||||||01-SEP-08
30505|Wahringa Limestone Member|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
30505|Wahringa Limestone Member|23736|5|Briefly described|p12|Eastonian|Darriwilian|Parent: Fairbridge Volcanics||||||
30505|Wahringa Limestone Member|23739|4|Described|p214|Late Ordovician|Late Ordovician|Parent: Fairbridge Volcanics. Geological Province: Lachlan Fold Belt.||||||01-SEP-08
30505|Wahringa Limestone Member|24215|5|Briefly described|p805|||Parent:  Fairbridge Volcanics. Geological Province: Lachlan Fold Belt||||||01-SEP-08
30505|Wahringa Limestone Member|24398|4|Described|p263, p259 Fig. 2|Gisbornian|Darriwilian|Of Fairbridge Volcanics.  See also Wahringa Member.  Geological Province: Lachlan Fold Belt.||||||
30505|Wahringa Limestone Member|50097|4|Described|p41|Gisbornian|Darwillian|Thickness: 88 m.  Of Fairbridge Volcanics. Contains diverse conodont, sponge, stromatoporoid and brachipod fauna. Geological Province: Lachlan Orogen. NSW.||||||07-FEB-11
30505|Wahringa Limestone Member|60417|5|Briefly described|p158|||Of Fairbridge Volcanics. Contains conodonts.||||||
30505|Wahringa Limestone Member|61893|6|Mentioned|p236|Late Ordovician|Late Ordovician|The upper part contains the late Gisbornian zonal index conodont, B. compressa.||||||
30505|Wahringa Limestone Member|63278|5|Briefly described|p146 Fig. 2a, p151|Late Ordovician|Middle Ordovician|Underlain by the informal bolder beach conglomerate. Consists of limestone. Geological Province: Molong Volcanic Belt, LFB. See also p151.||||||07-FEB-11
30505|Wahringa Limestone Member|63283|5|Briefly described|p194 Fig. 2, p199-200|Gisbornian|Darriwilian|Underlain by Hensleigh Siltstone. Thickness: 88m. Geological Province: Molong Volcanic Belt. Consists of limestone.||||||07-FEB-11
30505|Wahringa Limestone Member|63286|6|Mentioned|p308 Fig. 9|Gisbornian|Darriwilian|Of the Fairbridge Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
30505|Wahringa Limestone Member|63293|5|Briefly described|p470, p468 Fig. 2|Gisbornian|Darriwilian|Overlain by Yuranigh Limestone Member. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
30505|Wahringa Limestone Member|64295|5|Briefly described|p200 Fig. 2|||Of Fairbridge Volcanics. Contains conodonts.||||||01-SEP-08
30505|Wahringa Limestone Member|64826|5|Briefly described|p1041 Tb. 1|Gisbornian|Gisbornian|Of Fairbridge Volcanics (Kenilworth Group).||||||04-MAR-09
30505|Wahringa Limestone Member|67106|6|Mentioned|p673-675|||Molong Volcanic Belt.||||||
30505|Wahringa Limestone Member|67322|5|Briefly described|Fig.5; p23|Katian|Darriwilian|Morgan, Percival and Scott, in Meakin and Morgan (1999). Age defined by conodont fauna from the late Darriwilian to late Gisbornian. Occurs in the North Molong Volcanic Belt.||Of the Fairbridge Volcanics||Upper beds correlate with the Yuranigh Limestone Member.||22-FEB-18
30505|Wahringa Limestone Member|68592|6|Mentioned|p379|||Macquarie Arc; Dubbo 1:250 000 map area.||Unit in Fairbridge Volcanics.||||
30505|Wahringa Limestone Member|70684|5|Briefly described|p19-20, p26-27, p74|Late Ordovician|Middle Ordovician|Molong Volcanic Belt. About 88m thick at the type section.||Fairbridge Volcanics.|||From the base: a fossiliferous, pink and cream coloured limestone, passing up into a muddy orange brown dirty limestone (richly fossiliferous), and topped by a massive grey limestone with occasional stromatoporoid fossils.|
30505|Wahringa Limestone Member|70754|5|Briefly described|p449, p450 Fig.2, p452, p455, p458-459|Sandbian|Darriwilian|See also p465-466, p474-479. Bakers Swamp district. Shallow-water high energy deposits. Lingulate species listed. Systematic palaeontological descriptions.||Fairbridge Volcanics.|||Dominantly ooidal grainstones and bioclastic calcarenites.|
27656|Walbrook Metabasalt Member|42712|4|Described|Table1p14; Fig3p10.|Early Devonian|Late Silurian|Member of Campbells Formation||||||
41073|Walcha Road Monzogranite|24366|5|Briefly described|p7|Early Triassic|Late Permian|Of the Moonbi Plutonic Suite.||||||
41073|Walcha Road Monzogranite|63748|6|Mentioned|p47|Early Triassic|Early Triassic|Pluton of the Moonbi Supersuite. Age: 249+/-1Ma.||||||07-FEB-11
41073|Walcha Road Monzogranite|68005|5|Briefly described|pp67-68, p134.|Permian|Permian|Listed on p.134 as a unit in Moonbi Supersuite. Mottled, high K with lower Th and U radiometric responses. Complex jointing and regolith effects producing a U-rich deep blue smear, are also evident in the imagery.||Unit in Southern Moonbi Supersuite.|||Monzogranite: high K sphene-magnetite-bearing I-type granitoid.|
41073|Walcha Road Monzogranite|68006|6|Mentioned|p146.|||Quartz vein deposits of W-Mo have been reported proximal to this unit.||||||
41073|Walcha Road Monzogranite|68111|5|Briefly described|p968 Tb.1|Induan|Wuchiapingian|Geoscience Australia dataset, 2007. Also 249 +/- 3 Ma (La-ICP-MS U-Pb; Jackson et al. 2004).|253.8 +/- 1.8 Ma (U-Pb SHRIMP).|Of the Moonbi Supersuite.||||
41073|Walcha Road Monzogranite|69323|5|Briefly described|p21,70|Lopingian|Lopingian|Geological province: New England Orogen. Previous SHRIMP U-Pb dating includes 253.8+\-1.8 Ma (Black, 2006) and 251.8+\-3.0 Ma (Jeon, 2012).|253.8+\-1.8 Ma; 251.8+\-3.0 Ma|Unit of Moonbi Supersuite.||||
41073|Walcha Road Monzogranite|69639|4|Described|p2, p6, p8-p9, p198-p204|Lopingian|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described. Previously dated by Shaw and Flood (2009) at 249 +/- 3 Ma which is the same age obtained by Jackson et al (2004). Previous SHRIMP U-Pb ages of 253.8 +/- 1.8 Ma and 251.8 +/- 3 Ma were derived from Black (2006) and Jeon (2012), respectively. See also  p217-p218, p238.|252.0 1+/- 1.4 Ma (SHRIMP U-Pb, magmatic.)|Moonbi Supersuite|||Coarsely porphyritic hornblende-biotite monzogranite with an equigranular groundmass.|
41073|Walcha Road Monzogranite|70210|5|Briefly described|p2|Permian|Permian|New England district. The first (and only) mention in the text (on p2) is as Walcha Road Adamellite (Monzogranite). See references to Walcha Road Adamellite (p2, p30, p34-35, p38, p40-41).|253.8 +/- 1.8 Ma.|||||
41073|Walcha Road Monzogranite|71628|4|Described|p1-15; p7: 1, 4, 15-18, 37-51; p8: 56|||See also p8: 66, 69, 71; p19: 54-55. Previously the Walcha Road Adamellite (Binns et al., 1967). Named after the locality of the same name. The largest pluton in the Supersuite (~420 km2); located ~10km E of Bendemeer. Crops out as whalebacks and tors. Metamorphic aureole detailed. Several other age determinations given. Petrology, mineralogy and geochemistry described in detail. Hosts the Rimbanda (Sn) prospect. RELATED UNITS (continued): Abuts Callaghans Creek Quartz Monzodiorite.|252.0 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Walcha Road Suite.|Congi Creek, Campbells Hill, Monzogranite Phases.|Intrudes Sandon Association and Sandon beds; Banalasta Monzogranite; Glenburnie Leucomonzogranite; Terrible Vale Porphyritic Microgranodiorite; Wandsworth Volcanic Group. See COMMENTS for more.|Zoned, variably porphyritic, hornblende-biotite monzogranite, and minor granodiorite. I-type.|
23120|Walibree Formation|22736|2|Defined|p616,17,627|Tournaisian|Famennian|north and south Hastings Block unit||||||
23120|Walibree Formation|22857|4|Described|p500 App.1 Tb.A1.7|Famennian|Famennian|Siltstone overlying dacitic volcanics. Sediment similar to Touchwood Formation. Max. thickness: 1700m.||||||24-FEB-06
23120|Walibree Formation|70939|6|Mentioned|p826, p828|Devonian|Devonian|Southern Hastings Block. Appears as Wallibree Formation on p826.||||||
23120|Walibree Formation|71628|6|Mentioned|p17-84|||||||Is intruded by North Brother Granodiorite.||
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.|||
30035|Wallala Formation|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Nea Subgroup (Black Jack Group). Fining-upwards sequence of lithic conglomerate, sandstone, siltstone, claystone, coal; minor tuff and tuffaceous sediments. Max. thickness: 55.5m. Geological Province: Gunnedah Basin.||||||
30035|Wallala Formation|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Nea Subgroup. New, formal name for the 'lithic conglomeratic unit' in Black Jack Formation (now Black Jack Group). Formal definition published in an article released immediately prior to this article, however new nomenclature is summarised in Appendix 1.||||||13-NOV-13
30035|Wallala Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Nea Subgroup.||||||
30035|Wallala Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Nea Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Lithic conglomerate, sandstone and siltstone.||||||
30035|Wallala Formation|65116|5|Briefly described|p447, 449, fig 6, p441|Late Permian|Late Permian|?Of Black Jack Group. Lithic conglomerate, sandstone, siltstone, claystone and coal.||||||
30035|Wallala Formation|68003|5|Briefly described|p38 Fig.3-j, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion.||Lower unit in Nea Subgroup.||Overlies Clare Sandstone. Is overlain by Trinkey Formation.||
30035|Wallala Formation|68004|5|Briefly described|p23 Table 1. |||Gunnedah Basin.||Lower unit in Nea Subgroup.||Overlies Clare Sandstone. Is overlain by Trinkey Formation.||
30035|Wallala Formation|70791|5|Briefly described|p277|Lopingian|Lopingian|Gunnedah Basin.||Nea Subgroup.||||
30035|Wallala Formation|70878|5|Briefly described|p715, p717-718, p724|Permian|Permian|Gunnedah Basin.|255.40 +/- 0.09 Ma.|Black Jack Group.||Overlies Clare Sandstone or Benelabri Formation. Is overlain by Trinkey Formation.||
30035|Wallala Formation|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Overlies Clare Sandstone. Is overlain by Trinkey Formation.||
25682|Wallanbah Formation|22736|6|Mentioned|p628 Fig7||Tournaisian|||||||
25682|Wallanbah Formation|22857|4|Described|p500 App.1 Tb.A1.7|Tournaisian|Tournaisian|Lithic arenite, minor interbedded mudstone, limestone and conglomerate at the top. Max. thickness: 1800m.||||||
25682|Wallanbah Formation|36057|2|Defined|p344|Tournaisian|Tournaisian|Prob. Tournaisian||||||
25682|Wallanbah Formation|36528|6|Mentioned|p175|||||||||
25682|Wallanbah Formation|39660|6|Mentioned|p450|||||||||
25682|Wallanbah Formation|40883|6|Mentioned|p5|||||||||
25682|Wallanbah Formation|42547|4|Described|p34|||||||||
25682|Wallanbah Formation|44093|5|Briefly described|p231 App. 1|Tournaisian|Late Devonian|Geological Province: New England Fold Belt.||||||
25682|Wallanbah Formation|44244|2|Defined|p197|Tournaisian|Tournaisian|Includes Mograni Limestone, Tugrabakh Limestone and Mayers Flat Limestone Members..  Overlies the Darts Creek Mudstone; underlies Kataway Mudstone.  Max. thickness: 1800m.  Geological Province: Myall Block.||||||
25682|Wallanbah Formation|47056|6|Mentioned|Fig.2 P523|||||||||
25682|Wallanbah Formation|50132|6|Mentioned|p248  Fig.6|||Early Namurian age||||Underlies the Kataway Mudstone.||
25682|Wallanbah Formation|50263|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Overlies: Bundook beds, Darts Creek Mudstone.  Underlies: Kataway Mudstone.  Geological Province: Eastern Myall Block.||||||
25682|Wallanbah Formation|61766|5|Briefly described|p68|Tournaisian|Tournaisian|Overlies unnamed Late Devonian-Early Carboniferous unit which itself overlies the Bulliac Formation. Conformably overlies the Darts Creek Formation. Geological Province: Tamworth Belt.||||||
25682|Wallanbah Formation|63832|6|Mentioned|p131 Fig.2|Tournaisian|Tournaisian|Eastern Myall block, Southern New England Fold Belt.||||||
25682|Wallanbah Formation|64631|5|Briefly described|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Belt, eastern Myall Block. Biostratigraphic age control for base and top.||||Is overlain by Kataway Mudstone.||
25682|Wallanbah Formation|69793|6|Mentioned|p1121 Fig.12|Tournaisian|Tournaisian|Myall Block, Tamworth Belt.||||||
80311|Wallandoon Ignimbrite|73457|5|Briefly described|p8-9|Early Devonian|Early Devonian|Exact nature of contact with Kengal Formation cannot be determined.|412.6+/-2.5 Ma (Bodorkos et al., 2021)|||Underlies Kengal Formation|Includes weathered crystal-rich volcaniclastic rocks.|
26979|Wallaya Dolerite|34434|6|Mentioned|Fig.5.25|||||||||
26979|Wallaya Dolerite|36220|5|Briefly described|p97|||||||||
26979|Wallaya Dolerite|36221|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic||||||
26979|Wallaya Dolerite|37253|6|Mentioned|Table 1|||||||||
26979|Wallaya Dolerite|45003|14|Not recorded|p233|||See also Lexicon||||||
27603|Walleroobie Volcanics|22638|3|Fully described|p56|||Mid- Silurian age on Cargelligo- Narrandera 1: 250 000 map sheet||||No contacts located. Wagga Group assumed to underlie unconformably.||10-MAR-16
27603|Walleroobie Volcanics|22857|5|Briefly described|p448 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Dacite ignimbrites, rhyolite, garnet dacite, quartz-feldspar and quartz-feldspar-garnet porphyries, rhyolite lavas.||||||
27603|Walleroobie Volcanics|29993|5|Briefly described|Map legend|Early Devonian|Early Devonian|Silurian-Devonian|||||Quartz-feldspar porphyry, rhyolite|10-MAR-16
27603|Walleroobie Volcanics|44192|5|Briefly described|Map Legend||Ludlovian|||||||
27603|Walleroobie Volcanics|44936|5|Briefly described|Map Legend||Silurian|||||||
27603|Walleroobie Volcanics|61964|5|Briefly described|p86, p88|||On the COOTAMUNDRA 1:250k sheet.  Similar garnet-bearing quartz-feldspar porphyry and rhyolite to Gurragong Volcanics. ||||||
27603|Walleroobie Volcanics|69043|4|Described|p1-2, p5-6, p15, p21, p28, p34, p40, p47|Early Devonian|Early Devonian|See also p50-56, p115-116, p123. E of Ardlethan. Bears a strong petrographic and geochemical resemblance to the Gurragong Volcanics to the N and W; their ages are indistinguishable. A "garnet porphyry" at the Ardlethan Mine, dated at 414.7 +/- 2.3 Ma, is probably a lateral equivalent; previously it was considered a carapace of the Ardlethan Granite.|418.7 +/- 1.8 Ma.|||Overlies Wagga Group, presumably unconformably. Correlated with Gurragong Volcanics.|Massive, medium-grey, garnet-biotite-bearing quartz-feldspar porphyry of rhyolitic composition.|
27603|Walleroobie Volcanics|70777|4|Described|p1-p4, p14, p24-p31, p80, p96|Lochkovian|Pridoli|Lachlan Orogen. Time equivalent and may be associated with the Boblegigbie Granite. SHRIMP age of 418.3 +/- 2.3 Ma (this volume) interpreted to be the magmatic crystallisation age of the rhyolite. Petrography, zircon description and U-Pb isotopic results discussed in detail. Ages are very similar to the Gurragong Volcanics and some facies are similar (thus they may be equivalent).|418.7 +/- 1.8 Ma (SHRIMP, Bodorkos et al., 2013)|||Equivalent to the Gurragong Volcanics.|Crystal-rich, garnet-bearing ignimbrites and porphyritic rhyolite.|
27603|Walleroobie Volcanics|71889|6|Mentioned|p7|||||||||
27603|Walleroobie Volcanics|72082|6|Mentioned|p3-4|||||||||
27603|Walleroobie Volcanics|72083|5|Briefly described|p26|||An exposure of "porphyry" mapped by Wynn (1962) is reinterpreted and discussed.||||Unconformably overlies Wagga Group.|Includes rhyolite with well-developed flow-banding, and crystal-rich (?)volcaniclastic sandstone to granule conglomerate.|
27603|Walleroobie Volcanics|72084|6|Mentioned|p39||||418.3 +/- 2.3 Ma (Bodorkos et al., 2016).|||||
33399|Walloy Rhyolite Member|24417|4|Described|p121|Middle Devonian|Middle Devonian|Of Warrumba Volcanics.  Underlain by Kirribilli Formation.||||||
33399|Walloy Rhyolite Member|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Warrumba Volcanics (Rocky Ponds Group).||||||05-JUL-04
33399|Walloy Rhyolite Member|60009|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Warrumba Volcanics (Rocky Ponds Group).||||||13-JUL-04
35075|Wallumbilla Formation, lower|23053|6|Mentioned|p28|||||||||
35075|Wallumbilla Formation, lower|67784|6|Mentioned|p28 table 1|||||||||
81947|Wallumburrawang Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|Includes two unnamed subunits.||Orange to white weathering, porphyritic to equigranular, trachyandesite to trachyte coherent and volcaniclastic rocks, lava flow deposits, lava domes and intrusions.|02-NOV-20
29582|Wallundry Suite|22638|4|Described|p29|Llandovery|Ashgillian|431 +/- 4 Ma (from Middledale Gabbroic Diorite intrusion)||||||
29582|Wallundry Suite|44192|5|Briefly described|Map Legend|||||||||
29582|Wallundry Suite|50191|6|Mentioned|p5, 13, 21|Silurian|Ordovician|||||||
29582|Wallundry Suite|72082|5|Briefly described|p22|Early Silurian|Early Silurian|||||Intrudes the Bronxhome Formation.||
24072|Walters Range Group|22508|5|Briefly described|p5||Early Devonian|Some units previously in Cocoparra Group now in Walters Range Group.||||||
24072|Walters Range Group|22768|5|Briefly described|p170|||||||||
24072|Walters Range Group|22857|5|Briefly described|p170, p440 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Cobar Supergroup. Max. thickness: 1.5km. Geological Province: Cobar Basin. ||||||
24072|Walters Range Group|37772|6|Mentioned|Fig.2|||||||||
24072|Walters Range Group|40269|6|Mentioned|Fig.3|||||||||
24072|Walters Range Group|40913|6|Mentioned|Map legend|Zlichovian|Pragian|Zlichovian-Pragian||||||
24072|Walters Range Group|41126|2|Defined|p86|Pragian|Pragian|||||||
24072|Walters Range Group|41394|2|Defined|p94|Pragian||||||||
24072|Walters Range Group|41395|6|Mentioned|Map legend|Pragian||||||||
24072|Walters Range Group|41528|6|Mentioned|p132|||||||||
24072|Walters Range Group|41821|6|Mentioned|p11 Fig.5|||In Mount Allen and Kilparney area||||||
24072|Walters Range Group|42144|6|Mentioned|p605|||||||||
24072|Walters Range Group|42521|5|Briefly described|Fig.3b P16|||||||||
24072|Walters Range Group|42566|5|Briefly described|Fig.5 P11|||||||||
24072|Walters Range Group|43089|5|Briefly described|Map Legend|||Of Cobar Supergroup.||||||03-JUN-08
24072|Walters Range Group|43263|6|Mentioned|Map Legend||Pragian|||||||
24072|Walters Range Group|43757|6|Mentioned|p510|||||||||
24072|Walters Range Group|44093|5|Briefly described|p167 App. 1|Early Devonian|Early Devonian|Clastic sediments. Geological Province: Lachlan Fold Belt.||||||
24072|Walters Range Group|61964|3|Fully described|p14 Fig. 4, p104-112|Pragian|Pragian|Includes Yar Sst + Scotts Craig Conglom. in CARGELLIGO sheet + undiff'd units; and Lumga Siltst. + Whoey Tank Fm on KILPARNEY 1:100k sheet.  Paraconformable below Mulga Downs Group. Age: Pragian411.2-407Ma[ from 2004 timescale], from shelly faunas in Lumga Siltstone, low in Group. Thickness: >800m. Lith.details. Geophysics (p227-228)||||||19-SEP-18
24072|Walters Range Group|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes Yar Sandstone and several unnnamed units.||||||10-APR-08
24072|Walters Range Group|63019|5|Briefly described|p920, p921 Fig.2|Pragian|Pragian|Shallow marine, sedimentary rocks. ?Possibly overlies upper Ural Volcanics.||||||
24072|Walters Range Group|63891|5|Briefly described|p237|||Shallow-marine, sedimentary. Mapped as age-equivalent and possibly overlying upper Ural Volcanics (KILPARNEY 1:100K).||||||
24072|Walters Range Group|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, App A-VI 3.||||||
24072|Walters Range Group|69163|5|Briefly described|Map legend|Early Devonian|Early Devonian||||Includes Yar Sandstone.||Undifferentiated medium- to coarse-grained quartz sandstone, medium- to small-scale trough cross-bedding.|
24072|Walters Range Group|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian||||Includes Yar Sandstone and Scotts Craig Conglomerate.|Overlies Rast Group. Unconformably overlies Clements Formation (Wagga Group). Is faulted against Square Head Formation (Bootheragandra Group).|Undifferentiated medium- to coarse-grained quartz sandstone, medium- to small-scale trough cross-bedding.|
24072|Walters Range Group|70751|5|Briefly described|p4, p6, p12, p15|Devonian|Late Silurian|Cobar Superbasin, Mouramba Shelf.||Cobar Supergroup|Includes the Lumga Siltstone, Yar Sandstone and Whoey Tank Formation.|||
24072|Walters Range Group|71039|6|Mentioned|p6, p23|Devonian|Silurian|||||||
24072|Walters Range Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|||Thin-bedded, parallel-laminated, medium-grained quartz sandstone and siltstone, overlain by cross-bedded quartz sandstone and intercalated siltstone; sporadic feldspathic-lithic sandstone and conglomerate. Sporadic Skolithos horizons towards top.|
24072|Walters Range Group|72908|6|Mentioned|p4|Early Devonian|Silurian|Mouramba Shelf.||||||
24072|Walters Range Group|72958|6|Mentioned|p8, p11, p19, p25|Emsian|Lochkovian|Cobar Basin. Nymagee area.|||Lumga Siltstone, Whoey Tank Formation, Yar Sandstone|Overlain by Crowl Creek Formation (Mulga Downs Group). Equivalent to Winduck Group.|Limestone-bearing shelf sequences.|
24072|Walters Range Group|73578|6|Mentioned|p2|||Cobar Basin.||||||
25590|Wambangalong Formation|22857|5|Briefly described|p456 App.1, Tb.A1.6|Devonian|Silurian|Of the Toongi Group. Sandstone, shale. Max. thickness: 700m. Geological Province: Cowra Trough.||||||
25590|Wambangalong Formation|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Toongi Group.||||||
25590|Wambangalong Formation|23170|2|Defined|p117|Late Silurian|Late Silurian|of Toongi Group.||||||
25590|Wambangalong Formation|29986|6|Mentioned|Map legend|Devonian|Silurian|Silurian-Devonian||||||
25590|Wambangalong Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
25590|Wambangalong Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
25590|Wambangalong Formation|40328|2|Defined|p130|Silurian|Silurian|||||||
25590|Wambangalong Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
25590|Wambangalong Formation|43500|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition) Part of Toongi Group||||||
25590|Wambangalong Formation|48958|6|Mentioned|Plate 1|||||||||
25590|Wambangalong Formation|68003|5|Briefly described|p24 Fig.3-e, p144. |Ludlow|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Berridong Siltstone. Is overlain by Belowrie Formation.|Quartzose sandstone, siltstone, shale, phyllite.|
26198|Wambidgee Serpentinite|22638|1|Redefined|p13|Early Ordovician||Jindalee Group. ?Cambro- Early Ordovician. Previously "Fontenoy Sepentinite"||||||
26198|Wambidgee Serpentinite|22857|5|Briefly described|p418 App. 1 Tb. A1.5|||Of the Jindalee Group. Antigorite serpentinite with minor antigorite-carbonate rock and antigorite-carbonate-talc rock; massive serpentinite pods. ||||||
26198|Wambidgee Serpentinite|23366|5|Briefly described|p12, p13 fig.8|Ordovician|Cambrian|||||||22-FEB-05
26198|Wambidgee Serpentinite|24215|5|Briefly described|p801|||Parent:  Jindalee Group.   Geological Province:  Lachlan Fold Belt||||||
26198|Wambidgee Serpentinite|24417|3|Fully described|p9|Late Ordovician|Middle Ordovician|Of Jindalee Group.||||||
26198|Wambidgee Serpentinite|30172|6|Mentioned|p43|||||||||
26198|Wambidgee Serpentinite|35070|2|Defined|p23|Early Ordovician|Cambrian|Cambrian to Early Ordovician||||||
26198|Wambidgee Serpentinite|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
26198|Wambidgee Serpentinite|35608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26198|Wambidgee Serpentinite|35609|4|Described|p14|||||||||
26198|Wambidgee Serpentinite|36411|6|Mentioned|p270|||Refers Basden et al 1978 for definition.||||||
26198|Wambidgee Serpentinite|36534|6|Mentioned|p225|||||||||
26198|Wambidgee Serpentinite|40328|6|Mentioned|p41|||||||||
26198|Wambidgee Serpentinite|44093|6|Mentioned|p116 footnote|||Of the Jindalee Group. Age: 401-400Ma (U/Pb SHRIMP Graham, Franklin et al, 1996) but contradicts other findings/observations. Requires scrutiny.||||||
26198|Wambidgee Serpentinite|44192|5|Briefly described|Map Legend|Early Ordovician|Cambrian|||||||
26198|Wambidgee Serpentinite|50191|6|Mentioned|p23, 25|Ordovician|Ordovician|Of the Jindalee Group?||||||
26198|Wambidgee Serpentinite|50628|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Jindalee Group. Serpentinite, talc-carbonate rocks.||||||05-JUL-04
26198|Wambidgee Serpentinite|60009|5|Briefly described|Map Legend|Gisbornian|Darriwilian|Of the Jindalee Group.||||||13-JUL-04
26198|Wambidgee Serpentinite|67127|6|Mentioned|p173|Cambrian|Cambrian|Source of Ni-Co-Sc mineralisation.||||Intrudes the Jindalee Beds.||
26198|Wambidgee Serpentinite|67322|5|Briefly described|p20|Pridoli|Ludlow|Age constrained by that of the parent Jindalee Group: an Ordovician fragmented ophiolite sequence within a Silurian sedimentary matrix. On Tumut 1:100 000 and Cootamundra 1:250 000 sheets (Warren et al. 1995).||Of the Jindalee Group||||22-FEB-18
26198|Wambidgee Serpentinite|71708|6|Mentioned|p336 Fig 1, p349, 351|Early Ordovician||Intruded by a granite dyke age 483.5+/-2.3 Ma U-Pb zircon. Related to the Coolac Serpentinite. Interpreted to have belonged to a larger ultramafic massif called the Tumut Serpentinite Province by Graham (2000).||||Intruded by an oceanic granitic dyke. Genetically related to the Coolac Serpentinite.||31-MAR-20
26198|Wambidgee Serpentinite|72296|5|Briefly described|p78|Ordovician|Ordovician|Thuddungra area, near Young. Associated with lateritic Ni-Co +/- Sc mineralisation derived from this unit in the Cenozoic. The style and setting of mineralisation is comparable to lateritic mineralisation in the COOLABAH 100K sheet area. Misprinted as Wambidgee Serpentine.|||||Originally harzburgite.|
26198|Wambidgee Serpentinite|73483|6|Mentioned|p406-407, p409, p416|Ordovician|Cambrian|Inferred Cambro-Ordovician age based on association with Jindalee Group. Also referred to as Wambidgee Serpentinite Belt which has a U-Pb zircon age of 486+/-3.2 Ma from plagiogranite in the Western Wambidgee Serpentinite Melange, has been inferred as part of the Cambro-Ordovician Jindalee Group.|486+/-3.2 Ma|Jindalee Group||||
36404|Wambrook Dolerite|50126|2|Defined|p76, p83 App.2|Late Eocene|Late Eocene|Of the Monaro Volcanics. Age: 40.6 +/- 0.4 Ma (K/Ar). Maximum Thickness: ~20m. Contains large phenocrysts of titanaugite. Previously considered to be Bondo Dolerite.||||||27-MAY-04
70131|Wana Karnu Group|64679|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Subdivided into Formations 1 to 5 comprising mainly sandstone and conglomerate; some siltstone.||||||27-NOV-08
70131|Wana Karnu Group|66623|1|Redefined|p vii, pp192-212. |Middle Devonian|Early Devonian|Formerly Mootwingee Series (Andrews 1922), Mootwingee Stage (Kenny 1934), Snake Cave Sandstone (Warris 1967), Wana Karnu Group (informal) (Sharp 2004); redefined in this study. Deposition in a large, complex braided river to delta system. Contains sedimentary structures, worm tube forms, and fish fossils. Correlated with Mulga Downs Group and Coco Range beds, and the Menamurtee Sandstone. |||Includes Muckabunnya, New Tank, Homestead Gorge, Old Coach Road, Shell Hill and Bengoro Ridge Formations, and Menamurtee Sandstone.|Paraconformably or disconformably overlies the Rowena Formation. Is unconformably or paraconformably overlain by Ravendale Formation.|White to buff, coarse fluviatile sandstones and interbedded conglomerates with variable quartz and quartzite pebble contents.|
70131|Wana Karnu Group|66918|5|Briefly described|Map legend|Devonian|Devonian||||Includes New Tank, Homestead Gorge, Shell Hill, Old Coach Road and Bengoro Ridge Formations.||Thick-bedded, laminated and cross-bedded medium-grained fluvial quartzose sandstones and quartzites; some beds with scattered round vein quartz and quartzose pebbles, and mudcasts.|
70131|Wana Karnu Group|67105|6|Mentioned|p661|Devonian|Devonian|||||||
70131|Wana Karnu Group|67208|5|Briefly described|Map legend.|Devonian|Devonian||||||Thick-bedded, laminated and cross-bedded medium-grained fluvial quartzose sandstones and quartzites; some beds with scattered rounded vein quartz and quartzose pebbles and mud clasts.|
70131|Wana Karnu Group|69541|5|Briefly described|p655|Late Devonian|Late Devonian|Koonenberry Belt, Delamerian Orogeny.||||Equivalent to Mulga Downs Group. Is overlain by Ravendale Sandstone.||
70131|Wana Karnu Group|70013|5|Briefly described|Map legend|Carboniferous|Devonian|Mapped, and description of lithologies combined, with [overlying] Ravendale Formation.||||Is overlain by Ravendale Formation.|Quartz sandstone, conglomerate and siltstone. Pebbles of vein quartz and quartzite. Cross-, trough- and planar-bedded. Rare horizons contain vertical worm-tubes (?Skolithos) indicating marine incursions.|
70131|Wana Karnu Group|70648|5|Briefly described|Map Legend|Devonian|Devonian||||||Thick-bedded, laminated and cross-bedded medium-grained fluvial quartzose sandstones and quartzite; some beds with scattered rounded vein quartz, quartzose pebbles and mudclasts.|
70131|Wana Karnu Group|70650|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Bengoro Ridge Formation, Shell Hill Formation, Old Coach Road Formation, Homestead Gorge Formation, New Tank Formation.||Thick-bedded, laminated and cross-bedded medium-grained fluvial quartzose sandstones and quartzites; some beds with scattered rounded vein quartz and quartzose pebbles and mudclasts.|
70131|Wana Karnu Group|70651|5|Briefly described|Map Legend|Devonian|Devonian|Includes 2 unnamed sub-units: Sandstone variant. Matrix-supported conglomerate variant; clasts dominated by quartzite and vein quartz.|||Includes 2 unnamed sub-units, Menamurtee Sandstone and Muckabunnya Formation.||Thick-bedded, laminated and cross-bedded medium-grained fluvial quartzose sandstone and quartzite; some beds with scattered rounded vein quartz and quartzose pebbles and mudclasts.|
70131|Wana Karnu Group|70718|4|Described|p43, p54, p102-103|Middle Devonian|Early Devonian|Possibly intersected in Mossgiel-1 drillhole.Radiometric age interpreted as the depositional ages of tuff and shales. A fossil fish suggests Emsian to Eifelian age. Some uncertainty about whether the rocks in Mossgiel 1 should be assigned to this group or Mulga Downs Group [a lateral equivalent].|398.5+/- 7.9 and 409.8+/- 8.1 Ma (K-Ar)|||Overlies the Mossgiel Granite.|Thinly interbedded red-brown, green-grey, fine- to very fine-grained quartzlithic sandstone with green-grey claystone and siltstone in Mossgiel 1. Includes tuff and shales.|02-JUN-19
70131|Wana Karnu Group|71040|5|Briefly described|p14|||Koonenberry Belt.||||Is overlain unconformably by Ravendale Formation.||
70131|Wana Karnu Group|71262|6|Mentioned|p9 Fig 7|Devonian|Devonian|||||||
70131|Wana Karnu Group|72461|6|Mentioned|p7|Devonian|Devonian|Forms the gorges and escarpments of the Mutawintji National Park.||||||
70131|Wana Karnu Group|75063|6|Mentioned|p108|Midle Devonian|Early Devonian|Bancannia Trough. Fluvial to estuarine or marginal marine environment(s) of deposition. Overlaps in age with Ooloo Hill Formation.|||||Mature, clastic sediments and local limestone units.|
23130|Wandeen Formation|22638|4|Described|p42|Silurian||Previously mapped as Jindalee "beds"||||||
23130|Wandeen Formation|22768|6|Mentioned|p174||Silurian|||||||
23130|Wandeen Formation|22857|4|Described|p174, p452 App.1, Tb.A1.6|Middle Silurian|Silurian|Basalt, basaltic andesite, mafic volcanogenic epiclastic arenites.||||||
23130|Wandeen Formation|44192|5|Briefly described|Map Legend||Llandoverian|||||||
23130|Wandeen Formation|44936|5|Briefly described|Map Legend||Silurian|||||||
23130|Wandeen Formation|60280|5|Briefly described|p2, p3 Fig. 1|||||||||
82695|Wandera Leucosyenogranite|71628|3|Fully described|p19: 166-168|||New name, after 'Wandera leucosyenogranite' of Waltenberg et al. (2015). Named after the locality of Wandera. A small (~4 x 1-1.5 km), deeply weathered intrusion. The type locality is the eastern floor and wall of the quarry on Wandera Lane (GR 322430, 67156870, Inverell 1:100,00 sheet) (Waltenberg et al., 2015). The very limited (one analysis) geochemistry is described.|288.7 +/- 1.4 (SHRIMP: Waltenberg et al., 2015).|Wandera Suite.||Intrudes Texas beds.|Medium- to coarse-grained leucosyenogranite. S-type (tentative).|
80192|Wandera leucosyenogranite|70217|4|Described|v, p1 tbl 1.1, p5-p10, p72, p87|Artinskian|Sakmarian|New England Orogen. Informal name. Interpreted as an S-type granite on the basis of its geochemistry. SHRIMP ages are derived from this volume. In depth description of zircons used for dating are provided. The age of 288.7 +/- 1.4 Ma is an unusual age for granite emplacement in the New England Orogen. On the basis of age and geochemical similarities with constituents of the Bundarra Supersuite, this unit is interpreted to be related to that supersuite.|288.7 +/- 1.4 Ma (SHRIMP U-Pb)|Bundarra Supersuite|||Coarse-grained, felsic, leucosyenogranite composed of 50 percent alkali feldspar, 40 percent quartz, 10 percent plagioclase and minor biotite.|04-OCT-17
80192|Wandera leucosyenogranite|71628|6|Mentioned|p19-166|||Waltenberg et al. (2015). [In this study, the author mistakenly states that Waltenberg et al. named the unit as the ""Wandera Leucosyenogranite""]. Now the Wandera Leucosyenogranite.||||||
29113|Wandsworth Volcanic Group|721|5|Briefly described|Map legend|Late Permian|Late Permian|Undifferentiated rock of this group is represented on this sheet - rhyolitic to rhyodacitic ashflow tuffs and rare lavas, rare trachyte, and andesite.||||||
29113|Wandsworth Volcanic Group|22490|4|Described|4|Late Permian|Late Permian|Geol province New England Fold Belt.||||||24-SEP-08
29113|Wandsworth Volcanic Group|22580|6|Mentioned|p97,p99||Late Permian|||||||
29113|Wandsworth Volcanic Group|22857|5|Briefly described|p262, p536 App.1 Tb.A1.9|Early Triassic|Late Permian|Contains the Coombadhja Volcanic Complex. Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|22864|5|Briefly described|p262,264|||||||||
29113|Wandsworth Volcanic Group|23050|4|Described|p14 Table 1|Late Permian|Late Permian|Age: unconformably overlies Sandon beds and is intruded by Early Triassic granites.||||||
29113|Wandsworth Volcanic Group|23051|5|Briefly described|Map Legend|Late Permian|Early Permian|||||||
29113|Wandsworth Volcanic Group|23544|6|Mentioned|p372|||||||||
29113|Wandsworth Volcanic Group|23720|5|Briefly described|Map Legend|||Includes the Annalee Pyroclastics and other volcanics, and the Dummy Creek Conglomerate.||||||15-DEC-04
29113|Wandsworth Volcanic Group|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Includes the Gilgurry Mudstone, Drake Volcanics, Dundee Rhyodacite and Coombadja Volcanic Complex.  Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|23790|5|Briefly described|p10 Fig. 2|Late Permian|Late Permian|Geological Province: Central Block.||||||28-OCT-08
29113|Wandsworth Volcanic Group|23811|5|Briefly described|Map Legend|Permian|Early Permian|Includes the Tent Hill, Emmaville, Wallangarra and Drake Volcanics, Gibraltar Ignimbrite and the Coombadjha Volcanic Complex, as well as undifferentiated Wandsworth Volcanic group and seven informally (geographic) named masses of the Dundee Rhyodacite.||||||31-MAY-07
29113|Wandsworth Volcanic Group|23812|4|Described|p25, p26 Tb.3|Early Triassic|Late Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|23859|5|Briefly described|p930|Late Permian|Late Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|24366|5|Briefly described|p9, 17 Fig. 3|Late Permian|Late Permian|||||||
29113|Wandsworth Volcanic Group|24480|5|Briefly described|p7|Late Permian|Late Permian|||||||
29113|Wandsworth Volcanic Group|42378|2|Defined|p2-30|Early Triassic|Late Permian|Encompasses 8 named units and undifferentiated Permian volcanics.||||||
29113|Wandsworth Volcanic Group|42559|6|Mentioned|p10|||||||||
29113|Wandsworth Volcanic Group|42719|5|Briefly described|p7|||||||||
29113|Wandsworth Volcanic Group|42729|5|Briefly described|p12|||||||||
29113|Wandsworth Volcanic Group|42748|6|Mentioned|Fig.3 P9|Permian||||||||
29113|Wandsworth Volcanic Group|43017|5|Briefly described|Fig.2,p374|||||||||
29113|Wandsworth Volcanic Group|43091|5|Briefly described|Map legend|||||||||
29113|Wandsworth Volcanic Group|44093|5|Briefly described|p233 App. 1|Late Permian|Early Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|44450|3|Fully described|p25|Permian|Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|60079|5|Briefly described|Map Legend|Late Permian|Permian|Includes: Dundee Rhyodacite.||||||
29113|Wandsworth Volcanic Group|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|||||||
29113|Wandsworth Volcanic Group|61772|6|Mentioned|p128, p133, p131||Late Permian|Thick, bedded felsic volcanic rocks. In southern New England Orogen.||||||27-MAY-08
29113|Wandsworth Volcanic Group|61773|6|Mentioned|p138|||||||||
29113|Wandsworth Volcanic Group|61793|6|Mentioned|p341|Late Permian|Late Permian|Geological Province: New England Fold Belt.||||||07-FEB-11
29113|Wandsworth Volcanic Group|61796|5|Briefly described|p385, p386 Fig. 1|Late Permian|Late Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|61804|5|Briefly described|p419|Permian|Permian|Felsic rocks. Geological Province: New England Fold Belt.||||||28-OCT-08
29113|Wandsworth Volcanic Group|62534|4|Described|p6, p7|Early Triassic|Late Permian|Of Barnes et al (1991). Comprises Emmaville and Tent Hill Volcanics and Dundee Rhyodacite - each characterised by distinctive magnetic and/or radiometric features.||||||07-FEB-11
29113|Wandsworth Volcanic Group|62757|5|Briefly described|p3 Fig. 1|Late Permian|Late permian|Felsic volcanic units.||||||07-FEB-11
29113|Wandsworth Volcanic Group|63347|5|Briefly described|p2|Late Permian|Late Permian|Geological Province: New England Orogen.||||||
29113|Wandsworth Volcanic Group|63748|6|Mentioned|p16, p50|Late Permian|Middle Permian|Of Barnes et al (1991) in New South Wales - see Wandsworth Group, although the two terms are used interchangeably in the text.||||||07-FEB-11
29113|Wandsworth Volcanic Group|65398|5|Briefly described|p4 Fig.2, p8-9, Fig 2-3|Late Permian|Late Permian|Thermally metamorphosed ignimbritic, rhyolitic and rhyodacitic volcaniclastic rocks: ashflow tuffs, local sandstone and conglomerate. Unconformably overlies Cara Formation; is intruded by Attunga Creek Monzogranite.||||||
29113|Wandsworth Volcanic Group|65668|6|Mentioned|p2, p32|Late Permian|Late Permian|Includes the Wallangarra and Emmaville Volcanics, considered to be closely related (Barnes et al., 1991 and Purdy, 2003). Age c.254 Ma. Dominantly calc-alkaline, terrestrial ignimbrites to shallow marine volcanics, deposited over large areas of the central New England region.||||||
29113|Wandsworth Volcanic Group|66720|5|Briefly described|Map legend|Early Triassic|Late Permian|The volcanic and sedimentary rocks are mapped separately, but with no Member status or names.|||||Rhyolitic to rhyodacitic volcaniclastic rocks; undifferentiated interbedded pebble conglomerate and feldspathic and lithic sandstone.|
29113|Wandsworth Volcanic Group|68005|5|Briefly described|p18, pp42-46, p69 Fig.3-S, pp151-153.|Late Permian|Late Permian|Central Block, New England Fold Belt. A coherent group of terrestrial and shallow marine felsic volcanics.|||Includes Emmaville and Wallangarra Volcanics, Gibraltar Ignimbrite.||Undifferentiated felsic volcanics, minor sediments and granites. Dominantly ignimbritic rhyolites and rhyodacites (dark crystal-lithic tuffs); rhyodacitic lavas, minor dacite, andesite, trachyte; interbedded fine-grained tuff and volcaniclastics.|
29113|Wandsworth Volcanic Group|68006|5|Briefly described|p20 Fig.3-A, p26, p115.|||Central Block, New England Fold Belt. Of Barnes et al. (1991).|||Includes Emmaville Volcanics and Glenmore Formation.||Thick sequences of predominantly rhyolitic to rhyodacitic, and minor andesitic, tuffs and ignimbrites.|
29113|Wandsworth Volcanic Group|68111|5|Briefly described|p968 Tb.1, p973||||||Includes Drake Volcanics, Dundee Rhyodacite, Emmaville Volcanics, and Wallangarra Volcanics.|||
29113|Wandsworth Volcanic Group|68553|6|Mentioned|Map legend|Permian|Permian|||||||
29113|Wandsworth Volcanic Group|68679|5|Briefly described|p451, p453|Permian|Permian|Barnes et al. (1991). Wandsworth Province. Largely undeformed.|||Wallangarra Volcanics, Dundee Rhyodacite.|Correlated with the Texas beds.||
29113|Wandsworth Volcanic Group|68822|6|Mentioned|p339|Late Permian|Late Permian|||||||
29113|Wandsworth Volcanic Group|69188|5|Briefly described|p1, p60, p64|||Same age as Culaden Granodiorite.|||Emmaville Volcanics.|Is overlain by Dundee Rhyodacite.||
29113|Wandsworth Volcanic Group|69323|5|Briefly described|p1,3,13-33,41,70-71, 76|Lopingian|Lopingian|Geological province: New England Orogen. Commonly abbreviated WVG in text. Traditionally regarded as having the Drake Volcanics at its base, but not anymore based on the age of the Drake Volcanics (264.4+\-2.5 Ma; Cross and Blevin 2010), and that it has a distinct chemical composition to the Wandsworth Volcanic Group.|||Includes Emmaville Volcanics, Emmaville Volcanics, 'Uralla volcanics', 'Attunga Creek volcanics', 'Kurrajong Park volcanics'.|||03-DEC-19
29113|Wandsworth Volcanic Group|69639|4|Described|p2, p8-p9, p16, p21|Lopingian|Lopingian|New England Orogen. Contact metamorphosed by the Attunga Creek Monzogranite. Also intruded by Mount Jonblee Leucomonzogranite, Mole Granite, Kingsgate Leucogranite, Wards Mistake Monzogranite and the Mount Mitchell Monzogranite. See also p26, p38, p44, p50, p62, p94, p212, p218-p222.|255.8 +/- 1.5 Ma (Chisholm et al, 2014)||Includes the Dundee Rhyodacite, Attunga Creek volcanics and the Wallangara Volcanics.|Intruded by the Attunga Creek Monzogranite, Dandahra Creek Leucogranite, Bolivia Range Leucomonzogranite.||
29113|Wandsworth Volcanic Group|70217|5|Briefly described|p38, p43, p49, p75|||New England Orogen. Ages derived from Cross and Blevin, 2010, 2013 and from Chisholm et al, 2014a. |256-252 Ma||Includes the Wandsworth Volcanics.|Intrudes the Webbs Consols Leucogranite. Intruded by the Pyes Creek Leucomonzogranite.||
29113|Wandsworth Volcanic Group|70876|5|Briefly described|p2, p64, p70, p79, p81|Late Permian|Middle Permian|New England Orogen. Previously included the Drake Volcanics; in this study they are recognised as a distinct unit on the basis of geochronology. Represents extensive terrestrial and shallow marine volcanism. Previously this group has been dated either Triassic or Permian but recent modern U-Pb dating techniques have placed the group firmly in the Permian.|||Includes the Wallangarra Volcanics, Emmaville Volcanics and Dundee Rhyodacite.|||
29113|Wandsworth Volcanic Group|71628|5|Briefly described|p3-52; p7: 2, 5, 40; p8: 16, 34, 40, 44|||See also p8: 50, 56, 61, 65-66, 72, 76, 80, 86-87, 92; p10-3; p11: 10-11, 20, 23, 26; p12: 5, 18; p13-4; p14: 3, 7, 12, 28; p15: 5, 9, 12, 22, 25, 29, 31, 106; p17: 4-5; p19: 43, 72, 77, 110, 141, 144-145, 159-160. A pendant of these rocks occurs in the Attunga Creek Monzogranite; probably comagmatic and representing cauldron collapse. See also Wandsworth Volcanics (p8: 13, 25, 28; p10-9; p11-11; p15-67; p19: 55, 77, 142). CONSTITUENTS (continued): Nioka Porphyritic Dacite; Arranmor, Pi Pi Ignimbrites; Georges Mountain Volcanics; Coombadjha Volcanic Complex. RELATED UNITS (continued): Is intruded by Walcha Road, Mount Duval, Cottesbrook, Llangothlin, Wards Mistake Monzogranites; Khatoun and Wilhelmshohe Tonalites; Manuka Farm and Terrible Vale Porphyritic Microgranodiorites; Uralla Granodiorite; Glen Garry Microleucosyenogranite; Mount Jonblee, Billyrimba, Bolivia Range, Clive and Sandy Flat Leucomonzogranites; Gilgai and Mole Leucogranites; Deepwater Syenogranite and Kentucky Quartz Diorite. May be intruded by The Basin and Tingha Monzogranites (no contacts observed). Abuts Mount Mitchell and Strathaven Monzogranites.|||Annalee Pyroclastics; Dummy Creek Conglomerate; Dundee Rhyodacite; Abington, Baldersleigh, Emmaville, Pheasant Creek, Tent Hill, Wallangarra Volcanics. See COMMENTS for more.|Overlies Henry River and (locally) Wellingrove Monzogranites. Is faulted against Rocky River Monzogranite and Dandahra Creek Leucosyenogranite. See COMMENTS for more.|Includes felsic volcanics.|
29113|Wandsworth Volcanic Group|72528|6|Mentioned|p71.|||Field relationships indicate a close temporal correlation with Deepwater Syenogranite.|||Includes Emmaville Volcanics.|||
70002|Wang Wauk Formation|61766|4|Described|p68|Early Carboniferous|Late Devonian|Consists of grey lithic feldspathic sandstone, siltstone and mudstone. Supersedes Wang Wauk beds. Conformably overlain by Darts Creek Mudstone. See also Wang Wauk formation.  Geological Province: Tamworth Belt.||||||09-APR-10
37906|Wanganui Andesite Member|24605|2|Defined|p931, p949 App.1|Namurian|Namurian|Of the Clifden Formation. Thickness at type section: 10m. Age: 319.2 +/- 2.8 Ma. Geological Province: New England Orogen.||||||
37906|Wanganui Andesite Member|65902|5|Briefly described|p203-4|Bashkirian|Serpukhovian|Of Clifden Formation. Dated at 319.2 +/- 2.8 Ma (Roberts et al., 2003).||||||09-MAR-12
31494|Wangrah Suite|23550|3|Fully described|p503-504|||A-type granites. Also see Fig 1 p502 and p509. Lachlan Fold Belt.||||||
31494|Wangrah Suite|24456|6|Mentioned|p328|||Granite. Geological Province: Lachlan Fold Belt.||||||09-MAR-05
31494|Wangrah Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Cobargo Supersuite. Includes the Wangarabell Granite (informal name).||||||09-FEB-05
31494|Wangrah Suite|71206|6|Mentioned|p373, 375, 377, 381, 387|||Lachlan Fold Belt. Granites contain phenocrysts, rapakivi texture and microgranular enclaves, with considerable textural heterogeneity at all scales. Geochemistry discussed. Sr/Nd plot.|||Danswell Creek, Wangrah, Dunskeig, Eastwood Granites.||Aluminous A-type granite.|
27925|Wankeroo Formation|34812|3|Fully described|p70|||||||||
29571|Wansey Formation|22857|4|Described|p456 App.1 Tb.1A1.6|pridoli|Pridolian|Of the Goonigal Group. Andesitic lithic tuffs and richly fossiliferous arenite, shale and conglomerate, breccia. Max. thickness: 600m. Geological Province: Cowra Trough. ||||||
29571|Wansey Formation|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|of Goonigal Group.||||||
29571|Wansey Formation|23170|2|Defined|p113|Pridoli|Pridoli|of Goonigal Group.||||||
29571|Wansey Formation|23214|3|Fully described|p154|Pridoli|Pridoli|Of Goonigal Group. Formerly named Wansey Tuff. Max. thickness 160m||||||
29571|Wansey Formation|24417|5|Briefly described|p59|||Of Coonigal Group.||||||
29571|Wansey Formation|43494|4|Described|p22|Pridolian|Pridolian|Supersedes Wansey Tuff. Consists of volcaniclastic sandstone and conglomerate of andesitic composition, interbedded with shale to the north. Conformably overlies Burgoon Formation; conformable beneath Maradana Shale. Thickness in type section: 570m.||||||16-MAR-06
29571|Wansey Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
29571|Wansey Formation|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|of Goonigal Group.||||||
29571|Wansey Formation|66197|5|Briefly described|p634, p633 Fig.4c|Pridoli|Pridoli|Cowra Trough-Molong High. Shallow marine sandstone. Underlies the Maradana Shale, overlies the Burgoon Formation.||||||14-MAR-12
29571|Wansey Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Goonigal Group||||
29571|Wansey Formation|73299|6|Mentioned|p1105|||Cowra Trough. [Map symbol suggests Silurian age]||||||
26202|Warbro Formation|22736|6|Mentioned|p611 Fig2||Permian|||||||
26202|Warbro Formation|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Macleay Group. Max. thickness: 1070m. Geological Province: Barnard Basin (Nambucca Basin).||||||
26202|Warbro Formation|23720|5|Briefly described|Map Legend|||Of Macleay Group. Grey micaceous siltstone, sandstone, rare mudstone, thin conglomeratic crinoidal limestone.||||||24-SEP-08
26202|Warbro Formation|24124|5|Briefly described|p3|||||||||
26202|Warbro Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
26202|Warbro Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
26202|Warbro Formation|34293|2|Defined|p49|Permian|Permian|||||||
26202|Warbro Formation|34556|4|Described|p266|||Permian||||||
26202|Warbro Formation|36961|6|Mentioned|Fig.5|||||||||
26202|Warbro Formation|38685|6|Mentioned|p27|||Geological Province: New England Fold Belt||||||
26202|Warbro Formation|38837|6|Mentioned|p233|||||||||
26202|Warbro Formation|40590|6|Mentioned|p333|||||||||
26202|Warbro Formation|41347|6|Mentioned|p368|||||||||
26202|Warbro Formation|41348|5|Briefly described|Map legend|Permian|Permian|Of the Macleay Group.||||||16-DEC-04
26202|Warbro Formation|43018|6|Mentioned|p390|||||||||
26202|Warbro Formation|43385|14|Not recorded|p179,180||Sakmarian|||||||
26202|Warbro Formation|43755|6|Mentioned|Fig.1,p548||Permian|||||||
26202|Warbro Formation|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|See also p232 Appendix 1. Geological Province: New England Fold Belt.||||||
26202|Warbro Formation|44450|5|Briefly described|p24|Early Permian|Early Permian|Geological Province: New England Fold Belt.||||||
26202|Warbro Formation|47059|4|Described|p151|||Cf. Warbro Beds p145, 147||||||
26202|Warbro Formation|61771|5|Briefly described|p116|||Geological Province: Northern Hastings Terrane.||||||
26202|Warbro Formation|61772|6|Mentioned|p130|||||||||
26202|Warbro Formation|63832|6|Mentioned|p131 fig 2|Kungurian|Artinskian|Northern Hastings block, Southern New England Fold Belt.||||||
26202|Warbro Formation|64631|5|Briefly described|p44 Fig.2.|Kungurian|Artinskian|Southern New England Fold Belt: northern Hastings Block. Biostratigraphic age control for base and top.||||Overlies Yessabah Limestone.||
26202|Warbro Formation|65317|5|Briefly described|p633, 635, p634 Fig.13|Permian|Permian|Includes 'Haydonville serpentinite' lenses. Also mis-spelt as Wabro Formation p635.||||||23-APR-12
26202|Warbro Formation|70939|6|Mentioned|p826, p828, p830|Permian|Permian|Northern Hastings Block.||||||
30528|Warderie Volcanic Member|22857|5|Briefly described|p466 App.1 Tb.A1.6|Silurian|Silurian|Of the Dripstone Formation (Mumbil Group). Intermediate lavas, intrusives, conglomerates and breccias. Max. thickness: 400m.||||||
30528|Warderie Volcanic Member|23043|5|Briefly described|Map Legend|Wenlock|Wenlock|of Dripstone Formation, Mumbil Group.||||||
30528|Warderie Volcanic Member|23170|2|Defined|p83|Wenlock|Wenlock|of Dripstone Formation, Mumbil Group.||||||
30528|Warderie Volcanic Member|71600|6|Mentioned|p23 Fig 1|Silurian|Silurian|Geological province: Lachlan Fold Belt.||Unit of Mumbil Group.||||
34073|Wards Creek beds|22612|5|Briefly described|423,425 fig 2 tble 1|Early Permian|Early Permian|Parent Manning Group.  Max thickness 600 m. Also on pages 426-429, 432. Overlying unit Giro Diamictite. Geol province New England Orogen||||||
38284|Wards Mistake Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Late Permian|Of Uralla Plutonic Suite.  Coarse- to medium-grained, hornblende-biotite monzogranite and granodiorite.||||||20-DEC-04
38284|Wards Mistake Monzogranite|23812|4|Described|p22 Tb.2, p14|Late Permian|Late Permian|Of Uralla Plutonic Suite.||||||
38284|Wards Mistake Monzogranite|62534|5|Briefly described|p11 (legend), p17|Early Triassic|Late Permian|Of the Uralla Supersuite.||||||07-FEB-11
38284|Wards Mistake Monzogranite|68111|5|Briefly described|p968 Tb.1|Anisian|Olenekian||248 - 244 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
38284|Wards Mistake Monzogranite|69639|4|Described|p1, p5, p8, p16, p32|Lopingian|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described. See also p68, p94-p99, p133, p218-p220, p240.|253.3 +/- 1.4 Ma (SHRIMP)|Wards Mistake Suite||Intruded by the Oban River Leucomonzogranite, Red Range Microleucogranite, Llangothlin Monzogranite and Kingsgate Leucogranite. Intrudes the Wandsworth Volcanic Group.|Medium-grained, equigranular monzogranite.|
38284|Wards Mistake Monzogranite|70217|5|Briefly described|p73 tbl 14.1|Changhsingian|Wuchiapingian|New England Orogen. Age derived from Chisholm et al, 2014b.|253.3 +/- 1.4 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
38284|Wards Mistake Monzogranite|71628|4|Described|p2: 28, 31; p3: 52, 72, 93; p8: 4-6|||See also p8: 12-15, 82, 85-86, 89-98; p14: 7-8, 16, 18, 20-25, 31-33; p15-12; p19: 12, 152. Henley et al. (2001). Originally the Wards Mistake Adamellite (Binns and Richards, 1965 after unpublished work by Neilson, 1965). Named after the locality, ~20km ENE of Guyra. Crops out almost 100km N-S; the largest more mafic I-type intrusion in the southern New England Orogen. Forms large whalebacks, tors and flat pavements in undulating hilly country and open woodlands. Several younger age determinations are given. Lithology described in great detail. Geochemistry detailed. Is spatially associated with minor mineralisation (W-Bi-Sn-Mo greisens, Au veins, Sn and base metal veins), mostly suspected as sourced from subsurface leucogranites. RELATED UNITS (continued): Also intrudes Hillgrove Supersuite (Tobermory and Kookabookra Monzogranites). Is intruded by Llangothlin Monzogranite, Oban River Leucomonzogranite, Red Range Microleucogranite. Abuts Sara beds and Kingsgate Syenogranite. Contains an outlier of Black Knob Monzogranite.|253.3 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Wards Mistake Suite.||Intrudes Girrakool beds, Rampsbeck Schist, Wandsworth Volcanic Group (Emmaville Volcanics, Nioka Porphyritic Dacite), Bakers Creek Supersuite (Days Creek Gabbro). See COMMENTS for more.|Medium-grained, typically equigranular hornblende-biotite-(pyroxene) monzogranite to granodiorite. Conspicuously jointed. I-type.|
38284|Wards Mistake Monzogranite|72528|5|Briefly described|p71, p109.|Lopingian|Lopingian|Date by Chisholm et al., 2014a. Presumed to intrude Deepwater Syenogranite (p109), but the nature of the boundary has not been fully examined (p71).|253.3+/-1.4 Ma|||Shares boundaries with Deepwater Syenogranite.|Includes monzogranite.|
67903|Wards Mistake Suite|69639|5|Briefly described|p32, p68, p95, p133|||New England Orogen.||Uralla Supersuite|Includes the Wards Mistake Monzogranite, Cottesbrook Monzogranite and the Terimbone Monzogranite.|||
67903|Wards Mistake Suite|71628|5|Briefly described|p8: 1, 4, 79-98; p14-1|||Northernmost, and most homogeneous, Suite in the Supersuite.||Uralla Supersuite.|Wards Mistake, Hell Hole, Ottery, Terimbone, Cottesbrook Monzogranites; Culaden Granodiorite.||Intermediate granites.|
29580|Wargin Granite|22638|3|Fully described|p54|||Previously mapped as Ungarie Granite. Probably Late Silurian||||||
29580|Wargin Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
29580|Wargin Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
29580|Wargin Granite|70217|6|Mentioned|p90|||New England Orogen.||||||
29580|Wargin Granite|70777|4|Described|p1, p3-p4, p52-p55, p98, p100|Wenlock|Wenlock|Lachlan Orogen. A zircon age of 428 +/- 2.5 Ma is also given in this volume. Both ages provided in this volume are interpreted to be magmatic crystallisation ages. Low magnetic susceptibility (12 x 10^-5 SI). Previously the sample dated in this study was mapped as the most southerly portion of the Ungarie Granite (Chappell et al., 1991). Warren et al (1995) subsequently included this outcrop within the newly defined Wargin Granite, which was separated from the Ungarie Granite to the north on the basis of its distinctive texture and abundance of metasedimentary xenoliths. Petrography, zircon description, U-Pb SHRIMP dates and geochronological interpretation are discussed. This granite is interpreted to be an S-type. See also p57-p62, p79.|430.1 +/- 2.2 Ma (Monazite, this volume) |Koetong Supersuite||Intrudes the Wagga Group.|Migmatitic, fine to medium-grained, sub-equigranular, plagioclase-poor muscovite-biotite granite. Hosts abundant xenoliths chiefly composed of metapelite.|
26985|Warialda Sandstone|29869|6|Mentioned|p34|||Ref Rade 1954||||||
26985|Warialda Sandstone|30133|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
26985|Warialda Sandstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
26985|Warialda Sandstone|34254|5|Briefly described|p490|||||||||
26985|Warialda Sandstone|43436|14|Not recorded|Map Legend||Jurassic|(Provisional Edition) See also Lexicon||||||
77262|Warkworth Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Mount Thorley Formation.||||
70510|Warlands Creek Volcanic Member|62095|2|Defined|p279 Appdx., Plate 1, p260 Tb. 1|Permian|Permian|Of Woodton Fm. Supersedes Warlands Creek Tuff Mbr. Also synonymous with Barangarook Tuff Mbr (misspelt - should be Barongarook Tuff Mbr). Beige to grey welded ignimbrite, partly flow-foliated. Age is Asselian. Thickness at type section: 25m.||||||31-JAN-08
35095|Warners Bay Tuff|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Newcastle Coal Measures. Tuff, tuffaceous sandstone, tuffaceous siltstone, claystone, chert. Max. thickness:15m. Geological Province: Sydney Basin.||||||
35095|Warners Bay Tuff|23055|6|Mentioned|p22, fig 11, fig 13|||||||||
35095|Warners Bay Tuff|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Of the Newcastle Coal Measures. Geological Province: Sydney Basin||||||14-MAR-07
35095|Warners Bay Tuff|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Of the Newcastle Coal Measures. Geological Province: Sydney Basin||||||14-MAR-07
35095|Warners Bay Tuff|24471|4|Described|p27|Late Permian|Late Permian|Geochemical correlation with Farmborough Claystone Member. Of Newcastle Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
35095|Warners Bay Tuff|62033|5|Briefly described|p25 (Table)|||Of the Newcastle Coal Measures. Overlies Adamstown Formation; overlain by Boolaroo Formation. Geological Province: Sydney Basin.||||||14-MAR-07
35095|Warners Bay Tuff|68493|6|Mentioned|p5 Fig.2|Lopingian|Lopingian|||Of the Newcastle Coal Measures.|||Felsic tuff, tuffaceous sedimentary rock.|
35095|Warners Bay Tuff|68711|3|Fully described|p118, 113, 115, p116 Tb 2, p114 Fig. 2|||Renamed from Warners Bay Formation. Thickness: 0.5-15m; 8.77 in type section in BHP Floraville Bore. Type and standard sections described.||Of Newcastle Coal Measures||Conformably overlies Adamstown Formation. Overlain by Boolaroo Formation.|Tuff, tuffaceous sandstone, tuffaceous siltstone, claystone, chert.|15-JAN-15
35095|Warners Bay Tuff|69683|6|Mentioned|p411 Fig.2|Late Permian|Late Permian|||Unit in Newcastle Coal Measures.||||
35095|Warners Bay Tuff|70878|5|Briefly described|p710, p712|Permian|Permian|Hunter Valley. 5.42m thick in Amoco Wybong 1 well.||Newcastle Coal Measures.||||
35095|Warners Bay Tuff|73304|6|Mentioned|p75|||||Newcastle Coal Measures||||
83869|Waroo beds|67908|6|Mentioned|p282-283|Cisuralian|Cisuralian|Texas Orocline, New England Orogen. New name. Early Permian. Shallow-dipping.|||||Thick arenite layers interlayered with thin siltstone bands.|
29512|Warraberry Member|22857|5|Briefly described|p490 App.1 Tb.A1.7|Middle Devonian|Middle Devonian|Of the Dulladerry Volcanics. Geological Province: Dulladerry Rift.||||||
29512|Warraberry Member|23043|5|Briefly described|Map Legend|Givetian|Givetian|of Dulladerry Volcanics.||||||
29512|Warraberry Member|23170|4|Described|p231|Middle Devonian|Middle Devonian|of Dulladerry Volcanics.||||||
29512|Warraberry Member|23214|3|Fully described|p222|Middle Devonian|Middle Devonian|Of Dulladerry Volcanics. Overlying unit: Curumbenya Ignimbrite Member. Rhyolite lava, polymict breccia, basalt, volcaniclastic sandstone/siltstone.||||||
29512|Warraberry Member|24417|3|Fully described|p116|Middle Devonian|Middle Devonian|Of Dulladerry Volcanics.||||||
29512|Warraberry Member|43640|5|Briefly described|Map Legend||Devonian|||||||
29512|Warraberry Member|43782|5|Briefly described|Map Legend|Givetian|Givetian|of Dulladerry Volcanics.||||||
29512|Warraberry Member|60009|5|Briefly described|Map Legend|Eifelian|Eifelian|Of the Dulladerry Volcanics (Rocky Ponds Group).||||||13-JUL-04
29512|Warraberry Member|70297|5|Briefly described|map legend|Middle Devonian|Middle Devonian|||Dulladerry Volcanics||||
75066|Warragamba Formation|61609|6|Mentioned|p240 Tb. 1, p244|Permian|Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||07-FEB-11
30039|Warrah Conglomerate|22529|5|Briefly described|7|Early Devonian|Early Devonian|Parent Kandos Group||||||
30039|Warrah Conglomerate|22590|6|Mentioned|Fig3 P754||Lochkovian|Actually spelt Warrah Cngl.||||||
30039|Warrah Conglomerate|22857|4|Described|p476 App.1 Tb.A1.6|Lochkovian|Lochkovian|Of the Kandos Group. Contains corals and stromatoporoids. Max. thickness: 280m. Geological Province: Capertee Rise.||||||
30039|Warrah Conglomerate|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Kandos Group.||||||
30039|Warrah Conglomerate|23170|2|Defined|p126|Lochkovian|Pridoli|of Kandos Group. Age: Clandulla Limestone conformably overlying has conodont fauna indicative of Lochkovian age, therefore WC is a similiar to slightly older age (possibly extending into the latest Pridoli).||||||
30039|Warrah Conglomerate|23522|5|Briefly described|p248 Fig 4|Lochkovian|Lochkovian|||||||
30039|Warrah Conglomerate|43188|4|Described|p205,Table 3 p209|Lochkovian|Lochkovian|Representative section location given. Age early Lochkovian. Of Kandos Group.||||||
30039|Warrah Conglomerate|44093|5|Briefly described|p212 App. 1|Early Devonian|Early Devonian|Of the Kandos Group. Geological Province: Lachlan Fold Belt.||||||
30039|Warrah Conglomerate|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cudgegong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
33418|Warrangong Volcanics|24417|3|Fully described|p75|Early Devonian|Early Devonian|Of the Black Range Group.  Previously included as part of "Illunie Rhyolite".  Overlain by Hervey Group.||||||
33418|Warrangong Volcanics|44936|5|Briefly described|Map Legend||Early Devonian|||||||
33418|Warrangong Volcanics|50231|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Black Range Group.||||||
33418|Warrangong Volcanics|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Black Range Group. Andesite, hornblende dacite, rhyolite.||||||05-JUL-04
33418|Warrangong Volcanics|60009|5|Briefly described|Map Legend|Pragian|Pragian|Of the Black Range Group.||||||13-JUL-04
33418|Warrangong Volcanics|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Black Range Group. Fine- to medium-grained, massive, generally porphyritic, dacitic ignimbrite, flow banded ferroan enstatite-augite latite, minor olivine?-augite basalt.||||||17-JUN-08
33418|Warrangong Volcanics|68592|2|Defined|p845 Fig.141, p926-35, p959-64|Early Devonian|Early Devonian|Bacchin et al. (1999). These rocks were formerly included in the Illunie Rhyolite by Brunker and Offenberg (1970) and Warren et al. (1996). Named after Warrangong Hills and Parish of Warrangong. Type area is the general area of the Warrangong Hills, NW of Koorawatha. Thickness unknown. In the Goulburn 250 map, occurs as a few isolated roof pendants in Crowther Monzodiorite. Distribution in other map areas described. Geochemistry, lithology detailed; geophysical properties described. Devitrified and strongly recrystallised. Possibly comagmatic with Crowther Monzodiorite and Broula Granite. Likely age from petrological similarities with other units. Quarried for construction materials 4.5km W of Koorawatha.||Unit in Black Range Group.||Is intruded by Crowther Monzodiorite and Broula Granite (both of Boggy Plain Supersuite). Is correlated with Mountain Creek Volcanics. Is overlain unconformably by Hervey Group.|Includes welded, porphyritic dacitic ignimbrite; fine-grained, flow-banded latite; and coarse-grained basalt.|
33418|Warrangong Volcanics|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dbw. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Black Range Group|||Fine-medium grained, massive, generally porphyritic, dacite; flow banded ferroan enstatite-augite latite and minor olivine?-augite basalt.|
33418|Warrangong Volcanics|70297|4|Described|map legend|Early Devonian|Early Devonian|||Black Range Group|||Andesite to dacite, rhyolite, volcaniclastic rocks, diorite, granite.|
33418|Warrangong Volcanics|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Fine-medium grained, massive, generally porphyritic, dacite; flow banded ferroan enstatite-augite latite and minor olivine?-augite basalt.|
73409|Warratta Group|66623|2|Defined|pp98-109, pp v-vi, p239.|Early Ordovician|Late Cambrian|New group, first defined in this study. Formerly part of Torrowangee Series (Mawson 1912); these have been repeatedly subdivided; the informal Easter Monday beds (Thalhammer et al. 1998) and Jeffreys Flat beds (Scheibner and Basden 1996) are now included in this unit. Possibly correlative with Dullingari Group. Thickness c.4-5 km. Has experienced a major deformational event resulting in penetrative foliation, inclined folding and reverse faulting. Hosts orogenic gold mineralisation. Geophysical properties described.|497 +/- 2.6 Ma (Black 2006).||Includes basal Yancannia, Jeffreys Flat and Easter Monday Formations.|Significant intrusions from Tibooburra Suite and Evelyn Creek volcanics.|Variably deformed and metamorphosed sequence of marine shelf to deep marine, interbedded siltstone, sandstone and mudstone.|
73409|Warratta Group|66920|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Easter Monday Formation.|||
73409|Warratta Group|66921|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Jeffreys Flat and Easter Monday Formations.|||
73409|Warratta Group|66922|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Jeffreys Flat Formation.||Variably deformed and metamorphosed sequence of interbedded siltstone, sandstone and mudstone.|
73409|Warratta Group|66927|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
73409|Warratta Group|67105|5|Briefly described|p653-654, 659, 661|Early Ordovician|Late Cambrian|Kayrunnera Zone, northern Koonenberry Belt. Post-Delamerian Orogeny, Lachlan Orogenic Cycle deposits. The sequence deepens from W to E.|497 +/- 2.6 Ma (SHRIMP II: Black, 2006).||Jeffreys Flat, Easter Monday, Yancannia Formations.||Interbedded siltstone, sandstone and mudstone; local limestone, turbidites. Includes felsic tuff.|
73409|Warratta Group|67207|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Jeffreys Flat and Easter Monday Formations.|Overlies Ponto Group.||
73409|Warratta Group|67209|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Jeffreys Flat and Easter Monday Formations.|||
73409|Warratta Group|67210|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Yancannia Formation.|Is unconformably overlain by Rolling Downs Group.|Variably deformed and metamorphosed sequence of interbedded siltstone, sandstone and mudstone.|
73409|Warratta Group|67211|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes Yancannia and Easter Monday Formations.|Is overlain by Rolling Downs Group.|Variably deformed and metamorphosed sequence of interbedded siltstone, sandstone and mudstone; regionally metamorphosed to lower greenschist facies.|
73409|Warratta Group|67322|5|Briefly described|p3 Fig.1;Fig.5; p39|Late Cambrian|Middle Cambrian|Newly defined: Greenfield, in Greenfield et al. (2010). Koonenberry Belt. Includes rocks deposited in the Warratta and Tibooburra Inliers after the Delamerian Orogeny. Age from p20 Fig.5 (Strat. column) - not well constrained.|||Easter Monday Formation, Jeffreys Flat Formation, Yancannia Formation|||22-FEB-18
73409|Warratta Group|68823|5|Briefly described|p376 Fig.3, pp382-385, p378 Fig.4, p401|Jiangshanian|Guzhangian|Deposition postdates Delamerian Orogeny. Mis-spelt Waratta p.383. Youngest detrital zircon age of 503 +/- 6 Ma gives maximum age of this unit. Separated from Teltawongee [mis-spelt as Teltawangee p.400] Group by Olepoloko Fault.|ca 500-490 Ma||Includes Easter Monday Formation.|Intruded by the Tibooburra Granodiorite.|Shallow to deep marine, interbedded, sandy, silty and muddy strata.|
73409|Warratta Group|69001|6|Mentioned|p2 Fig.1B|Cambrian|Cambrian||||Includes the Easter Monday Formation and the Jeffreys Flat Formation.|||
73409|Warratta Group|69002|5|Briefly described|p7, p8, p9, Map 1b|Ordovician|Cambrian|Late Cambrian to Early Ordovician age. Occurs in the northwestern corner of the Thomson Orogen.|||Includes the Easter Monday Formation and Jeffreys Flat Formation.|Intruded by the Tibooburra Suite.||23-JUL-15
73409|Warratta Group|69042|5|Briefly described|map legends|Ordovician|Cambrian|YF. Thomson Orogen? Belts of narrow trends having moderate magnetic intensity. Metasediments.||||||
73409|Warratta Group|69043|6|Mentioned|p11|Ordovician|Cambrian|||||||
73409|Warratta Group|69540|6|Mentioned|p640-641|Early Ordovician|Late Cambrian|Post-dates the Late Cambrian Delamerian Orogeny. Deformed by Benambran Orogeny; absence of earlier structures casts doubt on the proposed amalgamation of the Thomson with the Lachlan Orogens (Glen et al., 2013).||||||
73409|Warratta Group|69541|5|Briefly described|p644 Fig.1(a), p652, p654|Early Ordovician|Early Cambrian|Koonenberry Belt, Delamerian Orogeny. Potential correlate with Les Jumelles beds.|||Includes Easter Monday, Jeffreys Flat and Yancannia Formations.|||
73409|Warratta Group|69961|5|Briefly described|Map legend|Cambrian|Cambrian|No outcrop in map area.|||Includes Yancannia Formation.||Undifferentiated: variably deformed and metamorphosed sequence of interbedded siltstone, sandstone and mudstone.|
73409|Warratta Group|70602|6|Mentioned|p75 Fig11|Ordovician|Cambrian|||||||
73409|Warratta Group|70649|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Easter Monday Formation.||Variably deformed and metamorphosed sequence of interbedded siltstone, sandstone and mudstone.|
73409|Warratta Group|70652|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Easter Monday Formation.|||
73409|Warratta Group|70749|5|Briefly described|p42-44, p51-52, p54|Cambrian|Cambrian|Southern Thomson and Koonenberry area. Includes both shallow-marine to shelf and deeper water (turbidite) facies; general deepening of depositional environment to the E.|497.2 +/- 2.6 Ma.||Easter Monday, Jeffreys Flat, Yancannia Formations.|||
73409|Warratta Group|70821|5|Briefly described|p9, p12|Early Ordovician|Late Cambrian|Occurs N of the Olepoloko Fault. Electrical conductivity depends on the amount of pyrite and carbon contained in the rocks.|||||Shallow- to deep-marine clastic sedimentary rocks of low to very low metamorphic grade.|
73409|Warratta Group|71262|5|Briefly described|p3, p6|Early Ordovician|Late Cambrian||||||Marine sedimentary rocks.|
73409|Warratta Group|71263|6|Mentioned|p16-18|Ordovician|Cambrian||||Includes Yancannia Formation.|||
73409|Warratta Group|71284|5|Briefly described|p487-488|Early Ordovician|Furongian|Tibooburra area, Koonenberry Belt. Largely unfossiliferous. Deeper water marine succession.|||||Includes felsic tuff horizons.|
73409|Warratta Group|71415|5|Briefly described|p11,15-17|Early Ordovician|Cambrian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Associated with marine deposition and volcanism post-delamarian Orogeny. Includes metasedimentary units with maximum depositional ages of c. 465 Ma (Greenfield, Gilmore and Mills 2010). Underwent deformation and metamorphism between c. 441-424 Ma, intruded by post-D1 monzodioritic sills and dykes between c. 423 and 416 Ma, and by Tibooburra Granodiorite. Appears as the Warratta Formation on p17.|||Includes Easter Monday and Jeffreys Flat formations.|||19-AUG-19
73409|Warratta Group|71860|6|Mentioned|p6|Ordovician|Cambrian|||||||
73409|Warratta Group|71965|5|Briefly described|p896-902,909,911,913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Forms an elongate belt adjacent to the Olepoloko Fault and truncated to the north by Orientos Fault; known to outcrop in the Warratta and Tibooburra Inliers. Can be extrapolated north and south following broad, linear magnetic trends. Maximum depositional age provided tuff ages in the Easter Monday Formation (497.2+\-2.6 Ma); minimum depositional age provided by Wolgolla Granite intrusion (429.1+\-8.5 Ma). Deposited immediately after Delamerian Orogeny, likely during Larapinta extensional event, which liked the central and eastern basins via the Lapapinta Sea.|497.2 +/- 2.6 Ma (Dep. Tuff age)||Includes Easter Monday, Jeffreys Flat and Yancannia formations.|Correlable with Tongo Formation, Twin Tanks Metamorphics, Thomson beds, Werewilka Formation and Nebine Metamorphics.|Sandstone, siltstone and mudstone.|29-OCT-19
73409|Warratta Group|71966|5|Briefly described|p990,1000|Furongian|Furongian|Geological province: southern Thomson Orogen. Turbidite deposition synchronous with widespread I- and S-type magmatism in the Thomson Orogen.|497.2+\-2.6 Ma|||Correlable with Thomson beds.||
73409|Warratta Group|72522|4|Described|p3, p62-63, p65, p94, p112-114, p119.|Late Cambrian|Late Cambrian|Thomson Orogen. Regarded as post-dating late Cambrian deformation associated with ther Delamerian Orogeny. Age 498 Ma from tuff in Easter Monday Formation.|c. 502 Ma maximum depositional age||Includes Yancannia Formation?, Easter Monday Formation||Includes metamudstone and metasandstone and minor tuffaceous beds.|
73409|Warratta Group|72951|6|Mentioned|p1009-1012, p1024, p1029-1032|Early Ordovician|Late Cambrian|Thomson Orogen, southwest. Very restricted outcrop. Distinct, relatively high magnetic character that suggests a more extensive sub-surface extent. Spelt Warrata Group on p1031.||||Intruded by the Tibooburra Suite, Cuttaburra granite, and Evelyn Creek volcanics.|Metasediments.|
73409|Warratta Group|73177|4|Described|p1097-1099, 1112-1114, 1115-1118|Cambrian|Cambrian|Greenfield et al. (2010). Thomson Orogen. Has many similarities to the Teltawongee Group and Saint Arnaud Group. Underwent synorogenic (Benambran) deformation c.460-420 Ma.|c.497 Ma (MDA).||Yancannia, Jeffreys Flat, Easter Monday Formations; Cuttaburra Sandstone.|Overlies Teltawongee Group. Probable equivalent to Saint Arnaud Group. Intruded by Tibooburra Suite.|Variably metamorphosed and deformed sequences of interbedded mudstone, siltstone and sandstone.|29-AUG-22
78456|Warraweena Volcanics|68731|6|Mentioned|p213 Fig 3.118, p215|Neoproterozoic|Neoproterozoic|Considered late Neoproterozoic on the basis of zircon ages (Glen et al. 2010).||||||
78456|Warraweena Volcanics|69042|6|Mentioned|map|||Accidentally capitalised  on map face? Shown as informal Warraweena volcanics in map legends. ||||||
78456|Warraweena Volcanics|69043|6|Mentioned|p11|||Thomson Orogen. Also appears as Warraweena volcanics.||||||
78456|Warraweena Volcanics|69635|5|Briefly described|p164, p69 Fig 3.1, p3|||Intersected by drilling ~20 km NE of DDH T17. Shown as Warraweena volcanics in Fig 3.1|||||Calc-alkaline basaltic andesites.|
78456|Warraweena Volcanics|70602|6|Mentioned|p67,72,75|Paleozoic|Paleozoic|Age inferred from  map symbol. Aeromagnetic map data given. Appears as Warraweena volcanics on p75.||||||28-JUN-16
78456|Warraweena Volcanics|70744|5|Briefly described|p936 Fig.4, p939, p942|Neoproterozoic|Neoproterozoic|NW New South Wales. Subsurface Thomson Orogen. Has volcanic arc geochemical signature. Discussion over Late Neoproterozoic or Ordovician age.|?577 +/- 6 Ma.|||||
78456|Warraweena Volcanics|70821|6|Mentioned|p11-12|||Occurs S of the Culgoa Shear Zone/magnetic lineament. Characterised by linear trends of moderate to high magnetic intensity. Age is poorly constrained;  a sample with calcalkaline affinity was dated at 577 Ma (Glen et al., 2013).||||||
78456|Warraweena Volcanics|71860|6|Mentioned|p6|||||||||
78456|Warraweena Volcanics|71965|5|Briefly described|p896,899,904-905,912-914|Middle Devonian|Early Devonian|Geological province: Thomson Orogen. Does not occur in outcrop, but can be observed as linear anomalies of moderate to high magnetic intensity. Intersected in drill holes ACDWE008, 009 and 010. Glen et al. (2010, 2013) interpreted SHRIMP U-Pb zircon crystallisation age of 576.9+\-5.6 Ma, but defined a detrital spectrum of younger concordant grains that gave a peak at c. 504 Ma. Hack et al. (2018) reported ages of  417+\-3.5 Ma and  414+\-4 Ma from samples from ACDWE009 and 008 respectively. Reflects voluminous and widespread magmatism from late Silurian to early Devonian.|||||Massive, porphyritic and amygdaloidal coherent andesite to basaltic andesite lavas; volcaniclastic sandstone and conglomerate.|
78456|Warraweena Volcanics|73175|6|Mentioned|p1051, p1060 Fig.8, p1061, p1065|Devonian|Silurian|Age constraints from Hack et al., (2018) with Nd model ages of ca 830-760. Location in text includes p1062 Fig.9, p1064 Fig.11.|ca 420-415 Ma|||||
31775|Warree Creek Formation|23214|3|Fully described|p238|Late Devonian|Late Devonian|Of Canagle Subgroup. Geological Province: Lambie Basin. Underlying unit: Carlton Formation. Max. thickness: 185m.  Massive red or green mudstone. Formerly Warree Creek Shale.||||||
31775|Warree Creek Formation|43640|5|Briefly described|Map Legend|Devonian|Devonian|Canangle Subgroup, Catombal Group.||||||
31775|Warree Creek Formation|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Canangle Subgroup, Catombal Group. Consists of lenticular conglomerate, green sandstone and siltstone, green and red friable shale.||||||17-JUL-08
31775|Warree Creek Formation|43782|6|Mentioned|map diagram|Famennian|Famennian|of Canangle Subgroup, Catombal Group. [Misspelling of Waree Creek Formation/Shale.]||||||07-FEB-22
31656|Warri Suite|42726|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
25602|Warriewood silt loam|35488|6|Mentioned|p74|||||||||
25603|Warroo Limestone Member|22857|4|Described|p460 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Taemas Limestone. Fossiliferous thinly bedded limestone, shaly limestone, massive limestone. Max. thickness: 113m. Geological Province: Canberra-Yass Shelf.||||||
25603|Warroo Limestone Member|24250|5|Briefly described|p105, p109 Fig.5, p110|Early Devonian|Early Devonian|Of the Taemas Limestone (Murrumbidgee Group). Maximum Thickness: 110m. Overlain by Crinoidal Limestone Member (unconformable). Underlain by Receptaculites Limestone Member (conformable)||||||18-JUN-08
25603|Warroo Limestone Member|24551|6|Mentioned|p621|||||||||
25603|Warroo Limestone Member|32483|6|Mentioned|p33|||Refers Browne (1959)||||||
25603|Warroo Limestone Member|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25603|Warroo Limestone Member|35386|4|Described|p54|||||||||
25603|Warroo Limestone Member|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
25603|Warroo Limestone Member|42994|6|Mentioned|p4|||||||||
25603|Warroo Limestone Member|50230|4|Described|Map legend|Emsian|Emsian|Of the Taemas Limestone (Murrumbidgee Group).  Overlies the Patmore Limestone Member; underlies the Crinoidal Limestone Member.  Thinly-bedded fossiliferous limestone, massive limestone and impure silty limestone.||||||10-MAY-04
25603|Warroo Limestone Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Taemas Limestone (Murrumbidgee Group). Thinly bedded fossiliferous limestone; massive limestone and impure silty limestone.||||||
25603|Warroo Limestone Member|64992|5|Briefly described|p60 Fig. 1, p62|Devonian|Devonian|Part of the Taemas-Wee Jasper succession. Of the Taemas Formation. A well-bedded carbonate unit containing many silicified specimens  similar to those in Receptaculites Limestone Member; trilobites and brachiopods also...||||||30-MAR-09
25603|Warroo Limestone Member|68592|2|Defined|p982,p984 Fig.162,p985-6,p1031-3,p1903-4|Emsian|Emsian|Originally Warroo Limestone of Browne (1959), the uppermost unit in her Taemas Stage. When the latter was raised to Formation status (Offenberg, 1974), it became Warroo Limestone Member. Type locality described. 113-124m thick. Fauna, including silicified brachiopods, bivalves, rugose and tabulate corals, listed. Early to mid Emsian.||Unit in Taemas Limestone.||Conformably overlies Patmore Limestone Member and Receptaculites Limestone Member. Is overlain disconformably by Crinoidal Limestone Member.|Lower part is blue-grey, thinly-bedded, richly fossiliferous limestone and impure flaggy limestone; upper part is blue-grey, massive, thickly-bedded, sparsely fossiliferous limestone dominated by corals and stromatoporoids.|
25603|Warroo Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmtw. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Taemas Limestone||Overlies Patmore Limestone Member. May be overlain by Crinoidal Limestone Member, nature of contact unclear.|Blue-grey, thinly bedded, richly fossiliferous limestone and impure flaggy limestone overlain by massive, thickly bedded, sparsely fossiliferous limestone.|
25603|Warroo Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, thinly bedded, richly fossiliferous limestone and impure flaggy limestone overlain by massive, thickly bedded, sparsely fossiliferous limestone.|
25603|Warroo Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, thinly bedded, richly fossiliferous limestone and impure flaggy limestone overlain by massive, thickly bedded, sparsely fossiliferous limestone.|
25603|Warroo Limestone Member|71656|5|Briefly described|p12 Fig.2, p37,p38|Emsian|Emsian|Includes conodonts, a trilobite, bivalves, fish fossils.||Probably of Taemas Limestone, Murrumbidgee Group||Overlies Patmore Limestone Member.|Fossiliferous limestone.|
82516|Warroo Monzogranite Phase|71628|5|Briefly described|p15: 34, 52; p19: 80-81, 83-84, 87-89|||New name (this study); previously Warroo Monzogranite of Sivell and Passmore (1999). Named after a local property. Occurs ~10 km NW of Liston. Crops out with excellent exposures as small boulders or blocks in rocky knoll or nubbin-like masses. The text has this unit intruding and intruded by Ruby Creek Leucogranite. Geochemistry described.||Karonstadt Complex.||Intrudes Jenners Monzogranite, Stanthorpe Complex.|Medium-grained, strongly porphyritic, granophyric, leucocratic, biotite-hornblende monzogranite. I-type.|
32474|Warrumba Volcanics|23392|6|Mentioned|p14|||||||||
32474|Warrumba Volcanics|24417|3|Fully described|p119|Middle Devonian|Middle Devonian|Of Rocky Ponds Group.  Has been previously included in "Illunie Rhyolite".  Underlain by Illunie Volcanics.||||||
32474|Warrumba Volcanics|24580|5|Briefly described|p828|Frasnian|Givetian|Unconformably overlies the Young Granodiorite. Unconformably overlain by the Hervey Group. Age: 348.4 +/- 3.4 Ma (this appears to be incorrect - OLR - 29-JAN-2014) & 382.7 +/- 2.8 Ma. Geological Province: Eastern Lachlan Fold Belt.||||||29-JAN-14
32474|Warrumba Volcanics|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Rocky Ponds Group. Overlies: Illunie Volcanics, Kirribilli Formation.  Underlies: Weddin Sandstone, Peak Formation, Hunter Formation.||||||05-JUL-04
32474|Warrumba Volcanics|60009|5|Briefly described|Map Legend|Givetian|Eifelian|Of the Rocky Ponds Group. Includes: Walloy Rhyolite Member, Coomaloo Ignimbrite Member, Adelargo Member.||||||13-JUL-04
32474|Warrumba Volcanics|62569|5|Briefly described|p609|||Overlain by Hervey Group. Crystallisation age: 382+/-2.8Ma (Raymond 2000a).  ||||||
32474|Warrumba Volcanics|63891|5|Briefly described|p236|||Volcanic analogue of A type intrusion. Geol Prov: Eastern Lachlan Orogen.||||||28-MAY-08
32474|Warrumba Volcanics|66768|5|Briefly described|p211-212||Givetian|In Rocky Ponds Group. Felsic lavas, ignimbrite and epiclastic rocks. 383 +/- 3 Ma U/Pb zircon age (Raymond 2000).||||||
32474|Warrumba Volcanics|68592|5|Briefly described|p33|Middle Devonian|Middle Devonian|Dulladerry Rift.||Unit in Rocky Ponds Group.|||A-type bimodal volcanics and associated plutons.|
32474|Warrumba Volcanics|71700|5|Briefly described|p29|Middle Devonian|Middle Devonian|||Rocky Ponds Group||||
77165|Warrumbungle Volcanic Complex|68003|5|Briefly described|p73 Fig.3-q, pp79-81, pp125-126.|Miocene|Miocene|Brigalow Belt South Bioregion. A NW-SE elongate ellipsoidal area. Strongly bimodal volcanism: older (18-15 Ma) distal basalt, and younger (15-13 Ma) central trachyte shield. Plugs and domes form spectacular scenery.|18 - 13 Ma.||||Alkali basalt, trachyandesite, potassic trachyte, tuff, tristanite; gravels, poorly consolidated sandstone, siltstone and carbonaceous claystone; occasional diatomite; beige silcrete.|
77165|Warrumbungle Volcanic Complex|70791|5|Briefly described|p279|Miocene|Miocene|Gunnedah Basin.||||||
77165|Warrumbungle Volcanic Complex|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic||||Includes Mount Exmouth, Wingabutta Fmns, Damnation Gully Gabbro, Burbie , Wallumburrawang , Mount Naman , Macha, Bingie Grumble, Shawn Creek, Siding Spring Formations, Pincham Syenite.||Undifferentiated mafic to felsic coherent and volcaniclastic rocks, lava flow and autobreccia deposits.|02-NOV-20
80446|Warwaegae granite|70718|5|Briefly described|p75|Middle Devonian|Middle Devonian|Hay-Booligal Zone. Informal name, derived from geophysics. Age derived from cross cutting relationship of the Oolambeyan granite and older Eurolie granite.||Baconian Swamp granite suite||||03-APR-18
31491|Watch Box Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Candelo Supersuite.  Includes the Glenrossal and Warri Granites (informal names).||||||09-FEB-05
31491|Watch Box Suite|44093|5|Briefly described|p220 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
24084|Watonga Formation|22616|6|Mentioned|Fig.1 p670|Devonian|Silurian|||||||
24084|Watonga Formation|22736|6|Mentioned|p627|Devonian|Silurian|||||||
24084|Watonga Formation|22857|4|Described|p484 App.1 Tb.A1.6|Silurian|Silurian|Cherts, slate, minor meta-arenite, rare metabasalt. Max. thickness: ?>1km. Geological Province: Woolomin Basin.||||||24-FEB-06
24084|Watonga Formation|24124|5|Briefly described|p3|||||||||
24084|Watonga Formation|40134|2|Defined|p274|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
24084|Watonga Formation|41237|5|Briefly described|p75|||||||||
24084|Watonga Formation|41347|4|Described|Table 6|||||||||
24084|Watonga Formation|41348|5|Briefly described|Map legend|Early Paleozoic||Slate, chert, minor slaty sandstone and rare metabasalt.||||||07-NOV-08
24084|Watonga Formation|44093|5|Briefly described|p67 Fig 6.6|Devonian|Devonian|Of the Port Macquarie Block. Geological Province: New England Fold Belt.||||||
24084|Watonga Formation|62058|4|Described|p3-5,p7,p18,p14 fig 5,p21,p23-26,p29|Late Devonian|Late Devonian|E of Lake Innes Fault. Part of an accretionary subduction complex. See also map sheets.||||Intruded by Karikeree Metadolerite.|Abundant chert (up to 100m thick units) and slate, uncommon metasandstone, rare metabasalt. Boudinage in more competent rocks; bedding in chert, that is irregularly folded, of a lensoidal, discontinuous nature. Unit is mostly broken formation.|
24084|Watonga Formation|63119|5|Briefly described|p209, p215|Late Silurian|Silurian|Unconformably overlain by Camden Haven Group. Chert-rich unit.||||||
24084|Watonga Formation|63763|3|Fully described|p2, p4-5 Fig. 1, p10-13|Late Carboniferous|Middle Ordovician|Includes pillow and massive basalt, rare dolerite dykes as well as mudstone, sandstone; a dominantly chert unit and undifferentiated rocks of slate, mudstone, sandstone, conglomerate and minor basalt. See also p7 Fig. 2, p14, p17.||||||
24084|Watonga Formation|65940|6|Mentioned|p193-194|||Wauchope-Port Macquarie area, NSW. Structurally dismembered unit, containing Middle-Late Ordovician conodonts in chert (Och et al., 2007).||||||
24084|Watonga Formation|66090|6|Mentioned|p4, p8, pp18-19 map.|Late Carboniferous|Ordovician|Port Macquarie Block, floor of the NE Lorne Basin. Low-grade regionally metamorphosed rocks.||||Is overlain unconformably by Jolly Nose Conglomerate.||
24084|Watonga Formation|67322|5|Briefly described|Fig.5, p28|Late Ordovician|Middle Ordovician|Och, Leitch and Caprarelli (2007). Conodonts in cherts establish a maximum age range for these rocks, extending from the late Darriwilian to possibly as young as the end of the Eastonian. Occurs in the Port Macquarie region, New England Orogen.||||Surrounds the Port Macquarie Serpentinite.|Mostly broken formation: disrupted sequence of once-stratified basalt, chert, siliceous mudstone, siltstone, sandstone and conglomerate.|22-FEB-18
24084|Watonga Formation|68466|6|Mentioned|p66|||Is well exposed along the coastline immediately S of Port Macquarie. Conodont ages range from late Darriwilian to end-Eastonian.|||||Broken formation: disruption of once-stratified sequence of basalt, ribbon chert, siliceous mudstone, siltstone, sandstone and conglomerate. Cherts are discontinuous and lensoidal, usually 5-200mm thick, highly variable in colour, with conodonts.|
24084|Watonga Formation|69668|5|Briefly described|p932, p942-943|Eastonian|Darriwilian|Described by Och et al. (2007). Mid north coast of NSW: Port Macquarie Block, New England Orogen. Age range from conodonts in chert. Chert geochemistry discussed. Ghosts of radiolarians preserved in some cherts.|||||Broken formation: disrupted sequence of basalt, ribbon chert, siliceous mudstone, siltstone, sandstone and conglomerate.|18-JUN-20
24084|Watonga Formation|70939|6|Mentioned|p826|Devonian|Devonian|Southern Hastings Block.||||||
24084|Watonga Formation|73440|6|Mentioned|p127|Ordovician|Ordovician||||||Includes isoclinally folded chert pendants.|
75069|Watta Formation|61612|6|Mentioned|p274, p277|Late Permian|Late Permian|||||||
24085|Watties Bore Formation|13995|5|Briefly described|p81, p95|Middle Ordovician|Early Ordovician|Webby et al. (1988). Slopes of the Gnalta Shelf. Contains a trilobite fauna belonging to the SE China Province.|||||Shale-rich.|
24085|Watties Bore Formation|22857|5|Briefly described|p91 Fig. 14.7B, p122|Early Ordovician|Late Cambrian|Of the Kayrunnera Group? Finely laminated siltstone and shale. Max. thickness: >2000m. See also p410 App. 1 Tb. A1.4.||||||
24085|Watties Bore Formation|22858|6|Mentioned|Fig14.7bp90-1|Ordovician|Late Cambrian|||||||
24085|Watties Bore Formation|23245|5|Briefly described|p122|||||||||
24085|Watties Bore Formation|23889|5|Briefly described|p5|||Of Kayrunnera Group.||||||
24085|Watties Bore Formation|41587|4|Described|p908|||||||||
24085|Watties Bore Formation|41810|6|Mentioned|p107|||||||||
24085|Watties Bore Formation|62793|5|Briefly described|p270|Early Ordovician|Late Cambrian|Youngest unit of Kayrunnera Group, Northern Koonenberry Belt. Contains thin limestones forming sedimentary breccias in which simple protoconodonts of Upper Cambrian type have been reported.||||Overlies Boshy Formation.||21-MAR-12
24085|Watties Bore Formation|63790|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Kayrunnera Group. Massive to well-laminated shales and siltstones, khaki primary colour weathering yellow. Minor calcareous and dolomitic members of brecciated or olistolithic character. Moderatly well-cleaved.||||||
24085|Watties Bore Formation|64671|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of Kayrunnera Gp.Massive to well-laminated shales + siltstones, khaki primary colour weathering yellow. Minor calcareous+dolomitic members. Highly cleaved on Nuntherungie. Trilobites near tip of exposed sequence indicate proximity to Cambro-Ordovician bou||||||26-NOV-08
24085|Watties Bore Formation|64684|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of Kayrunnera Group. Massive to well-laminated shales and siltstones, khaki primary colour weathering yellow. Minor calcareous and dolomitic members. Highly cleaved.||||||01-DEC-08
24085|Watties Bore Formation|66623|3|Fully described|p110, pp118-119. |Early Ordovician|Late Cambrian|Kayrunnera Basin. Defined by Webby et al. (1988) from rocks in the Kayrunnera beds of Brunker et al. (1971). Strongly weathered with recessive outcrops. At least 2000 m thick. Contains eleven trilobite species, protoconodonts and brachiopods. Mindyallan to basal Tremadocian.||Unit in Kayrunnera Group.||Conformably overlies Boshy Formation. Top of unit is fault-bounded against the Teltawongee Group.|Khaki coloured, variably-cleaved slate; originally massive to well-laminated marine mudstone, siltstone and minor calcareous to dolomitic breccias.|05-DEC-12
24085|Watties Bore Formation|66929|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Trilobites near top of exposed sequence indicate proximity to Ordovician boundary.|||||Massive to well-laminated shales and siltstones; khaki weathering to yellow; minor calcareous and dolomitic members; locally highly cleaved.|
24085|Watties Bore Formation|66933|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Highly cleaved on Nuntherungie. Trilobites near top of exposed sequence indicate proximity to Cambro-Ordovician boundary.||Unit in Kayrunnera Group.|||Massive to well-laminated shales and siltstones; khaki weathering to yellow; minor calcareous and dolomitic members.|
24085|Watties Bore Formation|67322|4|Described|p12; Fig.5|Tremadocian|Late Cambrian|Defined by Webby et al.(1988). Age determined from trilobite fossils present at two levels (separated by about 100m) close to the top of the Formation. About 2000m thick. SE of Koonenberry Mountain. ||Of the Kayrunnera Group.||Conformably overlies Boshy Formation. Correlated with Bynguano Quartzite.|Consists of shales and siltstones, with some well-bedded and laminated impure shaly limestones and minor limestone breccia lenses.|22-FEB-18
24085|Watties Bore Formation|70648|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Age from trilobites.||Kayrunnera Group|||Khaki, variably cleaved slate; originally massive- to well-laminated marine mudstone, siltstone and minor calcareous to dolomitic breccias; Late Cambrian to Early Ordovician trilobite fossils.|
26990|Wattle Park Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
26990|Wattle Park Granite|71206|6|Mentioned|p373|||Named by Chappell et al. (1991). The pluton was named Wattle Park Granite, also in 1991, by Wormald. Lachlan Fold Belt.||||||
27607|Watts Sandstone|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Included in both the Apple Tree Flat Subgroup (Wollombi Coal Measures, Singleton Supergroup) and the Charbon Subgroup (Illawarra Coal Measures). Max. thickness: 60m in the Hunter region. Geological Province: Sydney Basin. See also p528 App.1 Tb.A1.9.||||||
27607|Watts Sandstone|22969|4|Described|Fig 4.1a, p 53||Late Permian|Wollombi Coal Measures||||||
27607|Watts Sandstone|24157|5|Briefly described|p187, p188 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures. Geological Province: Sydney Basin||||||
27607|Watts Sandstone|29942|4|Described|Fig.1|||Permian||||||
27607|Watts Sandstone|29944|6|Mentioned|Fig.18|||||||||
27607|Watts Sandstone|31375|6|Mentioned|p3|||Stratigraphy||||||
27607|Watts Sandstone|33867|6|Mentioned|p7|||||||||
27607|Watts Sandstone|35926|6|Mentioned|p15|||||||||
27607|Watts Sandstone|36042|6|Mentioned|Fig.19|||||||||
27607|Watts Sandstone|38614|6|Mentioned|Fig.6|||||||||
27607|Watts Sandstone|39232|6|Mentioned|p105|||See also P110||||||
27607|Watts Sandstone|39287|6|Mentioned|Fig. 2.15|||||||||
27607|Watts Sandstone|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27607|Watts Sandstone|39666|6|Mentioned|p66|||||||||
27607|Watts Sandstone|39693|6|Mentioned|p17|||||||||
27607|Watts Sandstone|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27607|Watts Sandstone|40166|6|Mentioned|p347|||See also Table 1||||||
27607|Watts Sandstone|40256|6|Mentioned|p304|||||||||
27607|Watts Sandstone|40321|6|Mentioned|Fig.3|||||||||
27607|Watts Sandstone|40805|6|Mentioned|Fig.2|||||||||
27607|Watts Sandstone|41010|4|Described|p13|||||||||
27607|Watts Sandstone|41902|6|Mentioned|p23|||||||||
27607|Watts Sandstone|42078|6|Mentioned|Fig.2 P3|||||||||
27607|Watts Sandstone|42182|6|Mentioned|p299|||||||||
27607|Watts Sandstone|42657|5|Briefly described|p81|||||||||
27607|Watts Sandstone|42916|5|Briefly described|Table 1||Late Permian|||||||
27607|Watts Sandstone|43017|5|Briefly described|Fig.1,p372|||||||||
27607|Watts Sandstone|43194|5|Briefly described|p129 Tb. 8.3, p130|Late Permian|Late Permian|Of Singleton Supergroup, Hunter region, Sydney Basin.||||||
27607|Watts Sandstone|43257|5|Briefly described|Map Legend||Late Permian|Of Wollombi Coal Measures||||||
27607|Watts Sandstone|45090|5|Briefly described|p63|||Lithology, relationships, correlation & age||||||
27607|Watts Sandstone|60281|6|Mentioned|p9|||||||||
27607|Watts Sandstone|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wollombi Newcastle Coal Measures. Good reservoir potential in uppermost sections. Geological Province: Sydney Basin/Hunter Valley area.||||||
27607|Watts Sandstone|62033|5|Briefly described|p24, p25 (Table)|||Base of Newcastle Coal Measures was raised to top of Watts Sandstone by the resolution to replace Wollombi Coal Measure nomenclature with Newcastle Coal Measure nomenclature as ratified by Coalfield Geology Council in 2004. Name retained in Hunter Valley.||||||14-MAR-07
27607|Watts Sandstone|68003|5|Briefly described|p38 Fig.3-j, p41, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Unit in Wittingham Coal Measures (Singleton Supergroup).||Overlies Denman Formation. Is overlain by Wollombi Coal Measures.|Medium- to coarse-grained sandstone.|
27607|Watts Sandstone|68004|5|Briefly described|p23 Table 1, p51 Table 5, p52, p61.|Late Permian|Late Permian|Hunter and Western Coalfields. Equivalent to Waratah Sandstone in Newcastle Coalfield. 30 to 60 m thick. Resistant; forms prominent linear outcrop.||Basal unit in Wollombi Coal Measures.||Overlies Denman Formation. Is overlain by Abbey Green Coal.|A distinctive massive, medium-grained, even textured sandstone; coal-barren.|
27607|Watts Sandstone|69683|6|Mentioned|p411 Fig.2|Late Permian|Late Permian|||Unit in Singleton Supergroup.||||
27607|Watts Sandstone|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield.||Wittingham Coal Measures.||||
27607|Watts Sandstone|73304|6|Mentioned|p75|||||Singleton Supergroup||||
27607|Watts Sandstone|73625|6|Mentioned|p2|Permian|Permian|Hunter coalfield, Sydney Basin.||||Overlies Denman Formation. Is overlain by Wollombi Coal Measures.||
34395|Wauchope Formation|22736|6|Mentioned|p611 Fig2||Early Permian|See also Wauchope Limestone p625.||||||
34395|Wauchope Formation|22857|6|Mentioned|p514 App.1 Tb.A1.8|Permian|Permian|||||||
34395|Wauchope Formation|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|Geological Province: New England Fold Belt.||||||
27608|Waukeroo Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
27608|Waukeroo Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Yancowinna Subgroup (Torrowangee Group). Lenticular paraconglomerate, siltstone, sandstone. Age: ~700Ma. Max. thickness: 1500m. Geological Province: Adelaide Fold Belt. See also p398 App.1 Tb.A1.3.||||||
27608|Waukeroo Formation|30261|4|Described|Table 1|||Sturtian age||||||
27608|Waukeroo Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27608|Waukeroo Formation|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
27608|Waukeroo Formation|37931|4|Described|p533|||||||||
27608|Waukeroo Formation|38157|6|Mentioned|p261|||||||||
27608|Waukeroo Formation|39214|6|Mentioned|Table 1|||||||||
27608|Waukeroo Formation|41405|5|Briefly described|p204|||||||||
27608|Waukeroo Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Yancowinna Subgroup.||||
27608|Waukeroo Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Yancowinna Subgroup.||Overlies Mulcatcha Formation. Is overlain by Wammerra Formation (Euriowie Subgroup).|Lenticular paraconglomerate and diamictite, interbedded with quartzite siltstone and arkosic sandstone.|07-SEP-15
24087|Waukivory Creek Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Avon Subgroup (Gloucester Coal Measures). Very coarse to medium-grained trough-bedded lithic sandstone, laminated sandstone and mudstone; numerous coals; minor claystone. Max. thickness: 326m. Geological Province: Sydney Basin.||||||
24087|Waukivory Creek Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Avon Subgroup.    Geological Province: New England Fold Belt||||||
24087|Waukivory Creek Formation|40872|6|Mentioned|Fig.2|||||||||
24087|Waukivory Creek Formation|41054|6|Mentioned|p152|||||||||
24087|Waukivory Creek Formation|44244|2|Defined|p175, p168 Tb. 2|||Of the Avon Subgroup.  Overlies Mammy Johnsons Formation; conformably underlies Dog Trap Creek Formation.  Max. thickness: 326m.  Type section in text.  Geological Province: Myall Block.||||||
24087|Waukivory Creek Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Avon Subgroup (Gloucester Coal Measures).  Geological Province: Western Myall Block.||||||
78864|Wave Hill coal seam|68711|5|Briefly described|p118, p116 Tbl 4|||Informal unit.||Within Adamstown Formation||||
25608|Waverley Formation|22857|4|Described|p498 App.1 Tb.A1.7|Visean|Tournaisian|Disconformably overlain by Isismurra Formation. Max. thickness: 1550m. Geological Province: Tamworth Forearc Basin. See also p509 App.1 Tb. A1.8.||||||
25608|Waverley Formation|24603|6|Mentioned|p896 Fig. 17|||Age: 350.9+/-3.8Ma (Roberts et al, 1995a).  Geological Province: Tamworth Belt.  In the Rouchel Block.||||||
25608|Waverley Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25608|Waverley Formation|32529|5|Briefly described|p198|||Refers Manser (1968)||||||
25608|Waverley Formation|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25608|Waverley Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25608|Waverley Formation|32866|6|Mentioned|p13|||Fossil content||||||
25608|Waverley Formation|32867|6|Mentioned|p19|||||||||
25608|Waverley Formation|32869|5|Briefly described|p167|||Depositional environment. See also Figs 2, 3B||||||
25608|Waverley Formation|36296|6|Mentioned|p155|||||||||
25608|Waverley Formation|36390|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25608|Waverley Formation|36528|6|Mentioned|p175|||||||||
25608|Waverley Formation|39623|6|Mentioned|p33|||||||||
25608|Waverley Formation|39979|6|Mentioned|p62|||||||||
25608|Waverley Formation|40883|6|Mentioned|p5|||||||||
25608|Waverley Formation|41279|6|Mentioned|Fig.2|||||||||
25608|Waverley Formation|42547|4|Described|p25|||||||||
25608|Waverley Formation|43417|4|Described|Map Legend||Late Carboniferous|||||||
25608|Waverley Formation|43576|6|Mentioned|Fig.1,p348|||||||||
25608|Waverley Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
25608|Waverley Formation|44093|5|Briefly described|p228 App. 1|Tournaisian|Late Devonian|Geological Province: New England Fold Belt.||||||
25608|Waverley Formation|44244|2|Defined|p25-30|Visean|Tournaisian|Overlies the Goonoo Goonoo Mudstone; disconformably underlies the Ayr Conglomerate Member (Isismurra Formation).  Max. thickness: 1550m.  Type section in text.  Geological Province: Rouchel Block.||||||30-AUG-04
25608|Waverley Formation|45088|2|Defined|p26|Early Carboniferous|Early Carboniferous|See also Plate 2||||||
25608|Waverley Formation|45097|6|Mentioned|p25|||Brachiopod fauna. Correlation chart||||||
25608|Waverley Formation|46803|6|Mentioned|Fig. 3|||||||||
25608|Waverley Formation|50099|5|Briefly described|p9, p21|Early Carboniferous|Early Carboniferous|Conformably overlies the Goonoo Goonoo Mudstone; disconformably underlies the Isismurra Formation. Max. thickness: >1500m. Geological Province: Tamworth Belt/New England Orogen.||||||26-JUN-05
25608|Waverley Formation|50268|5|Briefly described|Map Legend|Visean|Tournaisian|Geological Province: Rouchel Block.  Overlies: Goonoo Goonoo Mudstone, Dangerfield Formation.||||||
25608|Waverley Formation|60299|5|Briefly described|p212 Fig. 2c|Carboniferous|Carboniferous|Age: 351 Ma (U-Pb zircon, Roberts et al., 1995). Geological Province: Rouchel Block.||||||
25608|Waverley Formation|62095|5|Briefly described|p250, p264|Tournaisian|Tournaisian|Parts are now mapped as Merlewood Formation. Geological Province: Rouchel Block/Tamworth Belt. See also Plate 1.||||||02-MAY-13
25608|Waverley Formation|63832|6|Mentioned|p131 fig 2|Tournaisian|Tournaisian|Rouchel block, Southern New England Fold Belt.||||||
25608|Waverley Formation|64631|6|Mentioned|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Belt, Rouchel Block.||||Shown as laterally equivalent to Dangarfield Formation.||
25608|Waverley Formation|65107|5|Briefly described|p275, Fig9 p283, Fig11 p286-7, Fig4 p279|Tournaisian|Tournaisian|Age: 350.9+/-4.0 Ma, from SHRIMP U-Pb zircons. From the Rouchel Block. Is used to constrain the older "eastward" loop of the New England Orogen (NEO)paleopole path.||||||16-JAN-12
25608|Waverley Formation|69793|6|Mentioned|p1121 Fig.12|Tournaisian|Tournaisian|Rouchel Block, Tamworth Belt.||||||
25608|Waverley Formation|70217|6|Mentioned|p90|||New England Orogen.||||||
25608|Waverley Formation|70777|4|Described|p2, p4, p8, p73-p77, p82|Early Carboniferous|Early Carboniferous|New England Orogen. SHRIMP zircon age from this volume is derived from a polymictic andesite breccia clast that is itself a clast within the conglomerate of this unit; thus this is a maximum depositional age.  An additional SHRIMP U-Pb age of 350.9 +/- 4 Ma is derived from an andesite low in this succession by Roberts et al., 1995. Early carboniferous age is supported by the presence of Late Tournaisian to Early Visean brachiopods, ammonoids and conodont fossils in the interfingering Dangarfield Formation. |355 +/- 2.2 Ma (zircons, this volume)|||Overlies the Kingsfield Formation. Interfingers with the Dangarfield Formation.|Coarse-grained volcanolithic conglomerate containing porphyritic clasts of andesitic breccia.|
27609|Weddin Sandstone|22638|4|Described|p72|||Nangar Subgroup. 460 m thick.||||||
27609|Weddin Sandstone|22831|5|Briefly described|p 66|||||||||
27609|Weddin Sandstone|22857|5|Briefly described|p490 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Hervey Group. White and red arenite; conglomerate, siltstone. Max. thickness: 457m. Geological Province: Hervey Basin.||||||
27609|Weddin Sandstone|23392|5|Briefly described|p14|||of Conolly (1965) Superseded by Weddin Formation||||||
27609|Weddin Sandstone|24125|5|Briefly described|p44|||Of the Hervey Group.  Geological Province: Lachlan Fold Belt.||||||
27609|Weddin Sandstone|24417|3|Fully described|p144|Late Devonian|Late Devonian|Now includes some rocks previously included in the "Mandagery Sandstone", Bumbery Formation and Eurow Formation.  Of the Hervey Group.||||||
27609|Weddin Sandstone|29907|6|Mentioned|Fig.15|||||||||
27609|Weddin Sandstone|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27609|Weddin Sandstone|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
27609|Weddin Sandstone|30071|6|Mentioned|Fig.2|||||||||
27609|Weddin Sandstone|32865|6|Mentioned|p484|||Fauna||||||
27609|Weddin Sandstone|33121|4|Described|p78|||?Mid.-Late Dev. Refers Conolly (1965)||||||
27609|Weddin Sandstone|33732|5|Briefly described|p114|||||||||
27609|Weddin Sandstone|35070|6|Mentioned|Fig.6|||||||||
27609|Weddin Sandstone|36066|6|Mentioned|p10|||||||||
27609|Weddin Sandstone|43441|5|Briefly described|32||Late Devonian|In Tullamore Syncline area||||||08-JAN-10
27609|Weddin Sandstone|43499|14|Not recorded|Map Legend|||(Provisional Edition) Part of Nangar Sub-Group. In Tullamore Syncline||||||
27609|Weddin Sandstone|43500|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Part of Nangar Sub-Group||||||
27609|Weddin Sandstone|43507|2|Defined|p128-9,145,148,151||Late Devonian|Formation of Nangar Subgroup (Hervey Group) (petrographic analyses) p165||||||
27609|Weddin Sandstone|43508|14|Not recorded|p118,120,124-5,127-8|||Occurrence of polycrystalline and undulatory quartz discussed. p129-134||||||
27609|Weddin Sandstone|43509|14|Not recorded|p113|||||||||
27609|Weddin Sandstone|43510|2|Defined|p41,45,66,68-73,|||p77-80||||||
27609|Weddin Sandstone|43513|14|Not recorded|p72|||||||||
27609|Weddin Sandstone|44192|5|Briefly described|Map Legend||Frasnian|||||||
27609|Weddin Sandstone|48958|6|Mentioned|Plate 1|||||||||
27609|Weddin Sandstone|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hervey Group.  Includes: Carlachy Sandstone Member, Cudgelbar Sandstone Member.||||||
27609|Weddin Sandstone|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hervey Group. Conglomerate and cross bedded quartz sandstone.  Overlies: Warrumba Volcanics.||||||05-JUL-04
27609|Weddin Sandstone|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Hervey Group. Includes: Culela Member, Carlachy Sandstone Member, Cudgelbar Sandstone Member. Overlies: Cloghnan Shale.  Underlies: Cookamidgera Subgroup.||||||13-JUL-04
27609|Weddin Sandstone|60548|5|Briefly described|map legend|Devonian|Devonian|Of Hervey Group.  Massive to cross bedded, pink quartz sandstone with pebbly horizons.||||||19-NOV-04
27609|Weddin Sandstone|62569|5|Briefly described|p607|||Within Hervey Group of Conolly (1965). Its lower part is now represented by Beugamel Sandstone (Wallingalair Group). See also "Weddin Sandstone". ||||||
27609|Weddin Sandstone|71040|5|Briefly described|p16|Late Devonian|Late Devonian|Currowong Syncline.||Hervey Group.||||
78900|Wee Jasper Formation|67823|5|Briefly described|p356-359, p362-364, p366|Middle Devonian|Early Devonian|New name; of Hunt and Young (2010). Formerly Wee Jasper Limestone. Root casts, extensive bioturbation and rare wood tissue occur in the red siltstones at the top of the conglomeratic cycles within this Formation.||Of Hatchery Creek Group.||Is overlain by Corradigbee Formation.|Red beds.|
78900|Wee Jasper Formation|68592|2|Defined|p989, p1193-1202|Early Devonian|Early Devonian|Essentially identical with former Hatchery Creek Conglomerate (Joplin et al., 1953); this latter unit was raised to Group status (Hunt and Young, 2010) to include the previously unrecognised Corradigbee Formation. Composite type section described. About 1500m thick. Former correlation with Hervey Group no longer tenable. Latest Emsian to early Eifelian age.||Unit in Hatchery Creek Group.||Conformably overlies Taemas Limestone (Murrumbidgee Group). Overlain by Corradigbee Formation. Is faulted against Burrinjuck Granite and Goobarragandra Volcanics.|Multiple fining-up cycles consisting of red-brown basal pebble conglomerate; red-purple cross-bedded sandstone; and red siltstone, extensively bioturbated with root casts and woody fragments.|
78900|Wee Jasper Formation|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dyw. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hatchery Creek Group||Overlies Taemas Limestone (Murrumbidgee Group).|Fining-upward cycles of red-purple-brown conglomerate, cross bedded sandstone and siltstone.|
78900|Wee Jasper Formation|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Hatchery Creek Group|||Fining-upward cycles of red-purple-brown conglomerate, cross bedded sandstone and siltstone.|
78900|Wee Jasper Formation|71656|5|Briefly described|p12 Fig.2, p38|Emsian|Emsian|Coarser sandstone than the overlying Corradigbee Formation. Non-marine. Location is bounded by the Goodradigbee Valley to the east, the Burrinjuck Granite to the west, and Burrinjuck Reservoir to the north.||Hatchery Creek Group.||Conformably overlies Taemas Limestone (Murrumbidgee Group) and underlies Corradigbee Formation.|Includes clastic conglomeratic and sandstone facies.|
28136|Weedallion Granophyre|22638|4|Described|p77||Late Devonian|||||||
28136|Weedallion Granophyre|35608|6|Mentioned|Map legend|Early Devonian|Middle Silurian|Middle Silurian to Early Devonian||||||
28136|Weedallion Granophyre|35609|6|Mentioned|p39|||||||||
28136|Weedallion Granophyre|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
28136|Weedallion Granophyre|44936|5|Briefly described|Map Legend||Late Devonian|||||||
29503|Weemalla Formation|13139|5|Briefly described|p3 Fig. 2, p9 Fig. 4|Late Eastonian|Darriwilian|Contains the Mount Pleasant Basalt Member. Conformably underlies Forest Reefs Volcanics. Geological Province: Eastern Molong Volcanic Belt.||||||17-JUL-08
29503|Weemalla Formation|22679|4|Described|p 8|Gisbornian|Darriwilian|Cabonne Group.||||||17-JUL-08
29503|Weemalla Formation|22857|4|Described|p426 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Feldspathic siltstone, arenite, minor conglomerate, calcareous mudstone, lavas, sills. Overlain by Forest Reef Volcanics. Max. thickness: 1350m.||||||07-SEP-09
29503|Weemalla Formation|23090|5|Briefly described|p642|||||||||
29503|Weemalla Formation|23170|6|Mentioned|p34|||||||||
29503|Weemalla Formation|23213|6|Mentioned|p13|||Correlates with Fairbridge Volcanics in the Cabonne Group. of Cabonne Group.||||||
29503|Weemalla Formation|23214|2|Defined|p54|Middle Devonian|Late Ordovician|Of Cabonne Group. Originally included as part of Malongulli Formation. At some locations the formation is subdivided in to unnamed units. Max. thickness 3500m.||||||
29503|Weemalla Formation|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
29503|Weemalla Formation|24007|6|Mentioned|p342|||||||||
29503|Weemalla Formation|24398|5|Briefly described|p265, p259 Fig. 2|Eastonian|Darriwilian|Overlies Coombing Formation. Geological Province: Lachlan Fold Belt. See also p267.||||||17-JUL-08
29503|Weemalla Formation|43640|5|Briefly described|Map Legend||Ordovician|||||||
29503|Weemalla Formation|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Includes Mount Pleasent Basalt Member. Consists of feldspathic siltstones, sandstone; minor conglomerate, calcareous mudstone, lavas and sills.||||||17-JUL-08
29503|Weemalla Formation|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Includes Mount Pleasent Basalt Member. Feldspathic siltstones, sandstone; minor conglomerate, calcareous mudstone, lavas and sills.||||||17-JUL-08
29503|Weemalla Formation|43782|5|Briefly described|Map Legend|Bolindian|Darriwilian|Of Cabonne Group.||||||17-JUL-08
29503|Weemalla Formation|60417|4|Described|p153, 157|Gisbornian|Darriwilian|Conformably overlain by Forest Reefs Volcanics. Siltstone and shale, with some calcareous units. Turbidites. Contains conodonts described here.||||||
29503|Weemalla Formation|60443|4|Described|p763 FIg.2, p765 Fig.3|Ordovician|Ordovician|Conformably overlain by Forest Reefs Volcanics. Max. thickness: ~1000 m. Fine grained, laminated and variably calcareous feldspathic sandstone, siltstone and minor conglomerate. Geological Province: Lachlan Fold Belt.||||||
29503|Weemalla Formation|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p155|Late Ordovician|Middle Ordovician|Conformably overlain by Forest reef  Volcanics. Geological Province: Molong Volcanic Belt, LFB. Early Darriwilian age suggested by conodonts at the base of unit.||||||07-FEB-11
29503|Weemalla Formation|63283|5|Briefly described|p195 Fig. 2, p202|Late Ordovician|Middle Ordovician|Overlain by Forest Reefs Volcanics. Geological Province: Molong Volcanic Belt. Consists of feldspathic turbidites.||||||07-FEB-11
29503|Weemalla Formation|63285|4|Described|p291 App. 1, p275 Fig. 2, p275|Eastonian|Darriwilian|Of Cabonne Group. Conformably overlain by Forest Reefs Volcanics and Fairbridge Volcanics. Age: ~468-447Ma. Geological Province: Molong Volcanic Belt. Consists of feldspathic sandstone and black mudstone.||||||
29503|Weemalla Formation|63286|5|Briefly described|p294 Fig. 1,p295, p308 Fig. 9|Late Ordovician|Middle Ordovician|Overlain conformably by Forest Reefs Volcanics and by Walli Formation and Cargo Volcanics. Consists of volcanic sandstone, siltstone and conglomerate. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29503|Weemalla Formation|63290|5|Briefly described|p396 Fig. 3|Gisbornian|Middle Ordovician|Overlain by Forest Reefs Volcanics. Geological Province: Molong Volcanic Belt.||||||
29503|Weemalla Formation|63293|5|Briefly described|p469 Fig. 2|Gisbornian|Darriwilian|Overlain by Forest Reefs Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
29503|Weemalla Formation|64015|6|Mentioned|p60|Darriwilian|Darriwilian|||||||
29503|Weemalla Formation|64963|5|Briefly described|p183|||Relatively deep marine deposits.||||||22-APR-09
29503|Weemalla Formation|67106|6|Mentioned|p673|||Molong Volcanic Belt.||||||
29503|Weemalla Formation|67107|5|Briefly described|p689, 691|Late Ordovician|Middle Ordovician|With Forest Reefs Volcanics, hosts the Cadia system of world-class Au-Cu deposits.||||Is overlain by Forest Reefs Volcanics. Is intruded by Cadia Intrusive Complex.|Sedimentary rocks.|
29503|Weemalla Formation|67322|5|Briefly described|p24-25, Fig.5|Darriwilian|Darriwilian|Oldest unit recognised in the Cadiangullong Creek valley. Name formalised by Wyborn, Krynen and Pogson, in Pogson and Watkins (1998), after an unpublished thesis mapping by J.Taylor. Graptolite and conodont assemblages indicate a Darriwilian age. Occurs in the Cadia region. Not present in the Forest Reefs area E of the Wongalong fault.||||Conformably overlain by the Forest Reefs Volcanics.|Includes calcareous mudstone beds.|22-FEB-18
29503|Weemalla Formation|67821|5|Briefly described|p157, p159|||Cadia area. Also appears as Weemalla Sediments on p159.|||||Siltstone.|08-FEB-18
29503|Weemalla Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
29503|Weemalla Formation|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 2 volcanic units. Age: ranges from early Darriwilian (Da2) to latest Gisbornian. Hosts Au-rich skarns at Junction Reefs. Molong Volcanic Belt.|c. 470-455 Ma|Cabonne Group|Mount Pleasant Basalt Member|||
29503|Weemalla Formation|70684|6|Mentioned|p3, p33-34, p47, p75|Late Ordovician|Middle Ordovician|Molong Volcanic Belt.||||||
29503|Weemalla Formation|72503|6|Mentioned|p31|||H. holodentata biozone[?] documented in the basal part of the unit.||||||
29503|Weemalla Formation|73431|6|Mentioned|p364-365, p366 Fig.3|Ordovician|Ordovician|Lachlan Orogen.||||Faulted against Browns Creek Intrusive Complex||
77796|Weereewa Group|71069|4|Described|p21 fig 7, p33, p208-209|Cenozoic|Cenozoic|Name derived from the indigenous name for Lake George (Weereewa). Distribution, geochemistry and geophysical characteristics discussed. Maximum thickness of 165m. See also  p211, p213, p216.|||Includes the Gearys Gap Formation, Ondyong Point Formation and the Bungendore Formation.|||
77796|Weereewa Group|71691|5|Briefly described|Map legend.|Quaternary|Neogene||||Bungendore, Ondyong Point, Gearys Gap Formations.|||
25610|Weethalle Granite|42726|5|Briefly described|map legend|||See also the informal Weethalle granite.||||||26-MAR-08
25610|Weethalle Granite|60303|6|Mentioned|p9 Tb. 1|||||||||
25610|Weethalle Granite|61964|3|Fully described|p14 Fig. 4, p38, p41 Tb. 2, p56-57|Middle Silurian|Early Silurian|Of Koetong Suite (Koetong Sup'ste).S-type, fractionated: coarse-med.-gr.porph. biotite granite with biotite-rich microgran.enclaves.Incl: 3 main rock type groups: muscovite-bearing, cordierite-bearing + a distinctive porph'tic microgranite.Age: ~428.2Ma||||||
25610|Weethalle Granite|62034|5|Briefly described|p26|Silurian|Silurian|Geological Province: Lachlan Orogen.||||||10-APR-06
25610|Weethalle Granite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Grey, coarse- to medium-grained porphyritic biotite granite with biotite-rich microgranular enclaves.||||||
25610|Weethalle Granite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian|||Unit in Koetong Suite.|||Grey, coarse- to medium-grained biotite granite.|
25610|Weethalle Granite|70296|5|Briefly described|p1, p8, p10, p24|Wenlock|Wenlock|Has a circular shape in the regional geomagnetics of the Cargelligo district.|426.9 +/- 2.4 Ma (SHRIMP U-Pb)|||Overlain by the Gurragong Volcanics.||21-JAN-21
25610|Weethalle Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Coarse- to medium-grained, compositionally zoned, porphyritic biotite granite comprising cordierite-biotite, biotite-muscovite and porphyritic tourmaline-muscovite microgranite varieties.|
76178|Weinteriga Creek Formation|66623|1|Redefined|pp74-75, pp84-85. |Middle Cambrian|Middle Cambrian|Redefined; formerly portion of Wonominta beds (Warris 1967), then Weinteriga Creek beds (Buckley 2000). Outcrops as generally subdued rounded hills and ridges. No fossils identified. Absence of tuffs and basalts implies Mount Wright Volcanic Arc was not active at the time.||Unit in Ponto Group.||Basal contact is not observed. Is overlain by Grasmere Formation, separated by a tightly folded metabasalt.|Turbiditic sandy phyllites, fine- to medium-grained, strongly foliated and kink-banded, weathers to yellow-brown colour; quartz-magnetite rock. Quartz veins to more than 1 m wide are a prominent feature.|
76178|Weinteriga Creek Formation|67322|5|Briefly described|p11; Fig.5|Cambrian||Age determined from p20 Fig.5 (Strat. column) - not well constrained. Occurs in the Kayrunnera-Koonenberry region.||Basal unit of the Ponto Group.||Overlain by the Grasmere Formation.|Predominantly sandy phyllites.|22-FEB-18
76178|Weinteriga Creek Formation|70651|5|Briefly described|Map Legend|Cambrian|Cambrian|Unnamed sub-unit of red-brown to black, very fine-grained, well-banded/laminated to locally massive quartz and magnetite rock; milky white quartz veining within the unit locally contains boxworks after pyrite.||Ponto Group|Includes unnamed sub-unit.||Predominantly non-magnetic metasandstone and metasiltstone; lesser weakly chloritic and magnetic metamudstone (phyllite); rare narrow bands of quartz-magnetite rock.
|
24090|Weismantels Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Dewrang Group. Thick, moderately high sulphur bituminous coal and laminated mudstone. Correlative of Muree Sandstone. Max. thickness: 20m. Geological Province: Sydney Basin.||||||
24090|Weismantels Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Dewrang Group.    Geological Province: New England Fold Belt||||||
24090|Weismantels Formation|40872|6|Mentioned|p33|||||||||
24090|Weismantels Formation|41054|6|Mentioned|p152|||||||||
24090|Weismantels Formation|42491|6|Mentioned|p6|||Stroud-Gloucester Trough.||||||
24090|Weismantels Formation|43017|5|Briefly described|Fig.1,p372|||||||||
24090|Weismantels Formation|44244|2|Defined|p171, p168 Tb. 2|Late Permian|Late Permian|Of the Dewrang Group.  Overlies Durallie Road Formation; underlies Mammy Johnsons Formation.  Max. thickness: 50m.  Type section in text.  Geological Province: Myall Block.||||||
24090|Weismantels Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Dewrang Group.  Geological Province: Western Myall Block.||||||
39133|Weja Dolomite|61964|3|Fully described|p151, p197-199|Pleistocene|Pliocene|Sourced from Wagga Gp metased. rocks - polygenetic, unconsolidated, polymictic dolomitic pebble orthoconglom. Distributed in a zone within  "Featureless sandplain". Commercial value as acid soil neutraliser ||||||
39133|Weja Dolomite|62405|5|Briefly described|Map legend|Cenozoic|Cenozoic|Dolomite-rich pedogenic carbonate over fluvially deposited dolomitic carbonate pebbles and cobbles, over massive carbonate.||||||19-NOV-08
39133|Weja Dolomite|64568|5|Briefly described|Map legend|Cenozoic|Cenozoic|Regolithic dolomite-rich carbonate accumulations, being: pedogenic dolomite; over fluvially deposited dolomitic carbonate pebbles and cobbles; over massive dolomite-rich carbonate.||||||19-NOV-08
36831|Welcome Volcanic Member|23859|2|Defined|p242 Appendix 1|Late Permian|Late Permian|See also page 933. Type locality 399000E 6755000N. Of Emmaville Volcanics. Geological Province: New England Fold Belt. Max. thickness: <400 m.||||||
36831|Welcome Volcanic Member|71628|5|Briefly described|p14-12; p15-9|||||Emmaville Volcanics.||Is overlain conformably by Dundee Rhyodacite. Is intruded by Bolivia Range Leucomonzogranite. Partly bounds the Mount Jonblee Leucomonzogranite.||
70511|Well Gully Ignimbrite Member|62095|2|Defined|p282 Appdx., Plate 1|Late Carboniferous|Late Carboniferous|Of the Seaham Formation. Grey to beige unwelded ignimbrite. Overlies Kewell Creek Volcanic Member. Age: 305.7+/-2.7Ma. Max. thickness: 15m. Geological Province: Rouchel Block/Tamworth Belt.||||||31-JAN-08
70511|Well Gully Ignimbrite Member|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Seaham Formation||||
82702|Wellingrove Monzogranite|71628|4|Described|p8: 4, 16-18; p19-170|||New name (this study). Previously Wellingrove Granodiorite (Pogson and Hitchins, 1973). From the village of that name. Comprises a series of NW-striking dyke-like bodies and irregular masses ~20km NW of Glen Innes. Geochemistry described.|256.1 +/- 1.4 Ma (SHRIMP: Waltenberg et al., 2015)|Llangothlin Suite.||Intrudes Emmaville Volcanics. Is overlain locally by Wandsworth Volcanic Group.|Irregularly textured, medium- to coarse-grained, porphyritic to equigranular, hornblende-biotite monzogranite, with minor syenogranite. Small round mafic enclaves are abundant. I-type (borderline A-type).|
24093|Wenham Formation|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of Craven Subgroup (Gloucester Coal Measures). Contains Bowens Road coal seam at top, Bowens Road Lower coal seam at base. Fine-grained sst; wavy and contorted bedding, plant debris laminations; palaeosols. Max. thickness: 24m. Geol. Prov: Sydney Basin.||||||
24093|Wenham Formation|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Craven Subgroup.    Geological Province: New England Fold Belt||||||
24093|Wenham Formation|40872|6|Mentioned|Fig.2|||||||||
24093|Wenham Formation|44244|2|Defined|p181, p168 Tb. 2|Late Permian|Late Permian|Of the Craven Subgroup.  Contains the Bowens Road coal seam.  Max. thickness: 23.9m.  Type section in text.  Geological Province: Myall Block.||||||30-AUG-04
24093|Wenham Formation|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures).  Coal, bright at base dull at top, and medium-grained lithic sandstone.  Geological Province: Western Myall Block.||||||
80455|Werai granodiorite|70718|5|Briefly described|p61-p63, p64|||Informal name, interpreted from geophysics. Deniliquin 1:250 000 sheet area. Also intrudes the Bendigo Zone of the Murray Basin. Magnetic signatures suggest whole suite is I-type.||Jawbone Creek granodiorite suite||Intrudes the Yadabal Lagoon granite.||30-MAY-19
79962|Werewilka Formation|71251|6|Mentioned|p3, p48|||Yowah-Cunnamulla area. Has a stripy magnetic domain. Map symbol suggests age inferred to be Cambrian.||||||26-APR-18
79962|Werewilka Formation|71864|6|Mentioned|p3|||||||||
79962|Werewilka Formation|71965|5|Briefly described|p896,899,901,903-906,908,910-911,913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Marker unit through the southern Thomson Orogen and defines a broad fold with an E-W to NE-SW-trending axial planes and a faulted hinge marked by the Caiwarro fault zone; possible "on-strike" stratigraphic equivalent, and adjacent to Nebine Metamorphics. Observed as elongate domains of distinctly stripy magnetic appearance related to narrow parallel zones of alternating high and low magnetic character. Age constraints: c. 506 Ma (MDA); 455.6+\-2.4 Ma (intrusion).|c. 506 Ma (MDA)|||Laterally grades into Lycosa Formation and Thomson beds. Correlable with Warratta Group, Tongo Formation, Twin Tanks Metamorphics, Nebine Metamorphics.|Interbedded sandstone, siltstone and calc-silicates.|29-OCT-19
79962|Werewilka Formation|72915|6|Mentioned|p5|||Map symbol suggests Cambrian age.||||||
40935|Werong Breccia Member|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Yanawe Formation (Douro Group). Subdivided into the Werong Breccia Cobble facies (underlying) and the overlying Werong Breccia Pebble facies.||||||10-MAY-04
40935|Werong Breccia Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yanawe Fm (Douro Gp). Variecoloured polymictic para-breccia. Angular clasts (boulders to pebbles) including ignimbrite, volcaniclastite, vitriv tuff and sst. in green-grey, medium- to coarse-grained volcaniclastite + microcrystalline matrix.||||||09-SEP-08
40935|Werong Breccia Member|68592|2|Defined|p430 Fig.89, p431-2, p434-5, p523-58|Ludlow|Ludlow|Named after Werong property. Representative localities for the boulder facies and the pebble facies are described. 45-72m thick. Volcaniclastic debris-flow deposits. Unfossiliferous; early Early Ludlow age from stratigraphic relationships.||Unit in Yanawe Formation.||Overlies Hulong Conglomerate Member conformably, and Laidlaw Volcanics disconformably.|Varicoloured, poorly sorted, polymictic, clast-supported breccia; upward-coarsening sequence comprising a lower pebble and cobble facies overlain by an upper boulder facies.|
40935|Werong Breccia Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdwb. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Yanawe Formation||Shown on Time-Space Plot as within unnamed member of Yanawe Formation.|Poorly sorted, pebble-boulder, clast supported, polymictic breccia; clasts are subangular and include sandstone, crystal rich volcaniclastite, porphyritic dacite?, crystal rich ignimbrite and microcrystalline vitric tuff, set in chloritic mudstone.|
40935|Werong Breccia Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Poorly sorted, pebble-boulder, clast supported, polymictic breccia; clasts are subangular and include sandstone, crystal rich volcaniclastite, porphyritic dacite?, crystal rich ignimbrite and microcrystalline vitric tuff, set in chloritic mudstone.|
40935|Werong Breccia Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|Lithology description continued: Microcrystalline vitric tuff set in a matrix of quartz-feldspar-lithic sandy chloritic mudstone.||Yanawe Formation|||Poorly sorted, pebble to boulder, clast supported, polymictic breccia; clasts generally subangular, include sandstone, crystal rich volcaniclastite, porphyritic dacite?, crystal rich ignimbrite, and see comments|
34400|Werrikimbe Volcanics|22736|5|Briefly described|p611 Fig2, p612||Triassic|||||||
34400|Werrikimbe Volcanics|22857|4|Described|p269, p281, p542 App.1 Tb.A1.11|Late Triassic|Late Triassic|Rhyolitic and dacitic ignimbrites. Age: 223.9 and 225.4Ma (Rb/Sr: Flood, Leitch and Shaw, 1993). Geological Province: New England Fold Belt. ||||||
34400|Werrikimbe Volcanics|22861|6|Mentioned|p281,285||Late Triassic|Max Age: 225.4 Ma.||||||
34400|Werrikimbe Volcanics|22864|6|Mentioned|p269|||||||||
34400|Werrikimbe Volcanics|44093|5|Briefly described|p67 Fig 6.6|Triassic|Triassic|Ignimbrite/dacite. Geological Province: New England Fold Belt.||||||
34400|Werrikimbe Volcanics|62095|5|Briefly described|p250 Fig. 1|Triassic|Triassic|||||||
34400|Werrikimbe Volcanics|66090|6|Mentioned|p29.|Early Jurassic|Late Triassic|NW of the Lorne Basin. Possibly associated with the ashfall tuffs in the Milligans Road Formation within that Basin.||||||
34400|Werrikimbe Volcanics|70939|5|Briefly described|p824-p826, p829-836, p838|Late Triassic|Late Triassic|Timing of deposition and faulting discussed. Appears as Werrikimbi Volcanics on p824 and p832.|226 Ma.|||||10-JAN-19
34400|Werrikimbe Volcanics|71628|6|Mentioned|p17: 89, 97|||||||Is intruded by Big Hill Creek Granite and Forbes River Porphyrite.||
34400|Werrikimbe Volcanics|73487|6|Mentioned|p585|Late Triassic|Late Triassic|Misspelt as Werrikimbi Volcanics p574 Fig.8.||||||
76155|Wertago Volcanics|66623|2|Defined|pp180-183, pp187-191. |Early Devonian|Silurian|Defined in this study. Andesite flows previously referred to Mount Daubeny Formation (Mills and Hicks 2000). Sills to 100 m thick and plugs to 500 m diameter. Widely-spread unit forming hilly terrain. Includes calc-alkaline lava flows and pyroclastics with high level sills and dykes. Hosts epithermal copper mineralisation. |Between 425 +/-7 Ma and 417.7 +/- 1.9 Ma.|||Cuts across Mount Daubeny Formation and the underlying basement Ponto and Teltawongee Groups, but not the Wana Karnu Group.|Trachytic, dacitic and rhyolitic intrusions. Four main mappable units: a coarse-grained amphibole-bearing intrusion; quartz-feldspar porphyritic rhyolitic to rhyodacitic sills and dykes; dacite intrusions; dark amygdaloidal andesitic flows.|
76155|Wertago Volcanics|70651|5|Briefly described|Map Legend|Devonian|Silurian|Unnamed sub-unit is  a felsic volcanic and volcaniclastic variant.|||Includes unnamed sub-unit.||Trachytic, dacitic and rhyolitic plugs, sills and dykes; includes amphibole-rich intrusions of unknown geochemical affinity.|
76155|Wertago Volcanics|70749|5|Briefly described|p43|Devonian|Silurian|Southern Thomson and Koonenberry area.|425.0 +/- 7.0 Ma.|||||30-APR-18
76155|Wertago Volcanics|71966|6|Mentioned|p990|Late Silurian|Late Silurian|Geological province: southern Thomson Orogen.|425+\-7 Ma|||||
76155|Wertago Volcanics|72522|4|Described|p3, p5 Tb.1.1, p131-135.|Lochkovian|Pridoli|Kayrunnera Zone, Koonenberry Belt. U-Pb SHRIMP age. Previous dating of intrusive rhyolite dyke gave age of 417.7+/-1.9 Ma (Black, 2006). Age compared with Tarcoon Suite, 400km to east.|417.7 +/- 3.9 Ma magmatic crystallisation|||Intrudes Ponto Group, Teltawongee Group, basal Mount Daubeny Formation.|Includes dacite (sampled for dating) and rhyolitic dykes, sills and plugs.|
76155|Wertago Volcanics|73177|5|Briefly described|p1110|||Mount Daubeny Basin.|425.0 +/- 7 Ma.||||Deformed basal pyroclastic and extrusive units.|
34741|West 16-mile Tank dolomite|22893|5|Briefly described|p32|||Within Loxton Sands.||||||
35128|West Borehole coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within Lambton Formation (Newcastle Coal Measures).||||||
35128|West Borehole coal seam|23055|6|Mentioned|p36|||||||||
35128|West Borehole coal seam|68711|5|Briefly described|p119, p116 Tbl 2|||Informal unit. The west Borehole Coal/seam is said to be the combination of Nobbys, Dudley, Yard and Borehole Coal/seams.[???]. See also p113.||Within Lambton Formation||||
37905|West Lynne Rhyodacite Member|24605|2|Defined|p936 Fig.5, p948 App.1|Visean|Visean|Of the Caroda Formation. Maximum Thickness: 3m. Geological Province: New England Orogen.||||||
73375|Westella Suite|69002|6|Mentioned|p12|Early Devonian|Early Devonian||~416 Ma||Includes the Byrock Granite.|||28-NOV-13
73375|Westella Suite|69043|5|Briefly described|p3, p91|Silurian|Silurian|Thomson Orogen. Two dates given: 416.8+/-2.5 Ma & as per age field. Source of dates unclear -  ?Black 2007.|416.7 +/- 3.4 Ma (Burton et al., 2012).||||I-type.|19-JAN-17
73375|Westella Suite|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian||||Includes Pendianna Tank, Emohruo and Byrock Granites.|||
73375|Westella Suite|70602|5|Briefly described|p67 Fig 3|Early Devonian|Silurian|Age inferred from Byrock Granite.|||Includes Emohruo Granite, Pendiana Tank Granite, Byrock Granite.|||
73375|Westella Suite|70941|4|Described|pviii, p9, p66-67, p140|Early Devonian|Late Silurian|Named for Westella property. Constituent units occur rarely as whalebacks and tors in very flat, low elevation country. The Byrock Granite is the type pluton for this suite. Distribution, structure, geophysical response and geochemistry discussed. Age derived from ages for constituent units. Has contact metamorphosed the Girilambone Group.|Ca. 416 Ma (SHRIMP U/Pb)||Byrock Granite, Pendianna Tank Granite, Emohruo Granite|Intrudes the Girilambone Group|Grey to white, fine to medium grained, medium to coarse grained granites consisting of quartz, K-feldspar, plagioclase and biotite with biotite rich enclaves occuring throughout.|
73375|Westella Suite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian||||Byrock, Emohruo and Pendianna Granites.|||
27929|Westerly Leucogranite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Leucogranite. BMR map symbol: gmt.||||||
27929|Westerly Leucogranite|34544|6|Mentioned|p186|||||||||
27929|Westerly Leucogranite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Leucogranite. S-type. BMR map code: Smw.||||||
27929|Westerly Leucogranite|40328|4|Described|p212|||Also mentioned on P203||||||
27929|Westerly Leucogranite|44092|5|Briefly described|map legend|Silurian|Silurian|glw5||||||
27929|Westerly Leucogranite|45147|3|Fully described|M200|||||||||
27929|Westerly Leucogranite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
35791|Wet Lagoon Volcanics|24317|5|Briefly described|p14|Late Silurian|Late Silurian|||||||
35791|Wet Lagoon Volcanics|50124|5|Briefly described|p132|||Of the Campbells Group. Geological Province: eastern Lachlan Fold Belt.||||||
35791|Wet Lagoon Volcanics|50232|5|Briefly described|Map legend|Ludlow|Wenlock|Of the Campbells Group.  Porphyritic rhyolitic to dacitic volcanic sandstone. Minor porphyritic to dacitic lava.||||||13-MAY-04
35791|Wet Lagoon Volcanics|50234|5|Briefly described|Map Legend|Pridoli|Wenlock|Of the Campbells Group.||||||
35791|Wet Lagoon Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Crystal-rich to crystal-lithic rhyolitic to dacitic volcanic sandstone. Minor porhyritic rhyolitic to dacitic lava. Volcaniclastic sandstone, siltstone, mudstone, and shale. Rare calcareous sedimentary rocks and limestone.||||||11-JUN-08
35791|Wet Lagoon Volcanics|67820|6|Mentioned|p136 Fig.3|Silurian|Silurian|||Campbells Group.||||
35791|Wet Lagoon Volcanics|68592|2|Defined|p166-70, p269, p608, p612, p616, p660-6|Late Silurian|Silurian|See also p102-3, p151-3. New name; after Wet Lagoon, 18km N of Lake George. Previously referred to as Coopers Creek Dacite (Gould, 1974; Farrell, 1986) and Coopers Creek Volcanics (Farrell and Offler, 1989), and mapped as Woodlawn Volcanics by Stuart-Smith (1992). Also previously known as Clare Vale Beds. Reasons for new name given. Type area described. Estimated thickness over 1000m. Regionally metamorphosed twice (Tabberabberan and Kanimblan Orogenies) to the biotite zone of greenschist metamorphism. Strongly silicified and chlorite-sericite-carbonate altered. Geophysical properties described. Hosts base metal  mineralisation (Lucky Hit-Gurrundah deposit detailed).||Unit in Campbells Group.||Overlain by and interfingers with Cuddyong Formation. Faulted against Abercrombie Fm. Correlated with Kangaloolah and Woodlawn Volcanics, Wowagin Dacite Mbr and Sooley Volcanic Mbr (De Drack Fm).|A sequence of crystal-rich to crystal-lithic rhyolitic to dacitic proximal volcaniclastic rocks with some coherent facies (lavas or sills) and thin, predominantly fine-grained sedimentary intercalations; minor massive ironstone outcrops.|
35791|Wet Lagoon Volcanics|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Scw. Includes three unnamed units of: dacitic to rhyolitic volcanic sandstone and minor laminated mustone to siltstone; rhyolitic volcanic sandstone with porphyritic dacite to rhyolite (sills or flows); tuffaceous siltstone, mudstone and quartzo-feldspathic sandstone. On Gunning 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Campbells Group|Includes three unnamed units.|Is within undifferentiated Cuddyong Formation.|Crystal rich-crystal lithic rhyolitic to dacitic volcanic sandstone; minor porphyritic rhyolite to dacite lavas and sills; lesser interbedded volcaniclastic sandstone, siltstone and mudstone; rare volcaniclastic conglomerate.|
35791|Wet Lagoon Volcanics|70541|4|Described|Map Legend|Devonian|Silurian|Includes three unnamed members: massive, dacitic to rhyolitic sandstone with minor laminated to medium-bedded siltstone and mudstone; lithic rhyolitic volcanic sandstone with minor tuffaceous siltstone and mudstone; tuffaceous siltstone and mudstone with massive, moderately sorted tuffaceous quartzofeldspathic sandstone.||Campbells Group|Includes three unnamed members.||Crystal rich to crystal-lithic rhyolitic to dacitic volcanic sandstone; minor porphyritic rhyolite to dacite (lavas or sills); lesser interbedded volcaniclastic sandstone, siltstone and mudstone; rare volcanic conglomerate also present.|
35791|Wet Lagoon Volcanics|70542|5|Briefly described|Map Legend|Devonian|Silurian|Includes one unnamed member of tuffaceous siltstone, mudstone and quartzo-feldspathic sandstone.||Campbells Group|||Crystal rich-crystal lithic rhyolitic to dacitic volcanic sandstone; minor porphyritic rhyolite to dacite lavas and sills; lesser interbedded volcaniclastic sandstone, siltstone and mudstone; rare volcaniclastic conglomerate.|
35791|Wet Lagoon Volcanics|71069|6|Mentioned|p36|||Hosts VAMS mineralisation in the southern Hill End Trough. ||Campbells Group||||
70514|Wheelihans Gap Ignimbrite Member|62095|2|Defined|p254, p273 Appdx.|Visean|Early Carboniferous|Of Merlewood Formation. Fine unwelded to slightly welded, grey, purple or beige ignimbrite with rare phenocrysts of plagioclase, minor quartz and opaque minerals. Geological Province: Werrie block/Tamworth Belt.||||||30-MAY-06
73405|Wheeney Creek Formation|66623|2|Defined|p110, pp131-133. |Early Ordovician|Early Ordovician|Defined in this study. Age-correlation with Yandaminta Quartzite, Tabita and Rowena Formations. Up to 500 m thick. Outcrops as strike-persistent ridges and characteristic jagged edged quartzite hills.||Unit in Kayrunnera Group.||Is overlain unconformably by Ravendale Formation.|Variably cleaved, fault-bound discontinuous lenses of metasedimentary rocks including polymictic conglomerate, ridge-forming quartzite, interbedded metasandstone and slate, fossiliferous limestone, intraclast limestone and dolomite.|
73405|Wheeney Creek Formation|67322|5|Briefly described|p11-12; Fig.5|Floian|Floian|Defined by Greenfield, in Greenfield et al. (2010). Up to 500m thick. Conodont assemblages from limestone are identical to those in the Yandaminta Quartzite and Tabita Formation (Bendigonian to early Castlemainian). Occurs between Koonenberry Fault to the W and Big Wallaby Tank Fault to the E, in the Kayrunnera-Koonenberry region.||Of the Kayrunnera Group.|||Discontinuous lenses of polymictic conglomerate, quartzite, interbedded psammite and slate, fossiliferous limestone, intraclast limestone and dolomite.|22-FEB-18
73405|Wheeney Creek Formation|69961|5|Briefly described|Map legend|Ordovician|Cambrian|||Unit in Kayrunnera Group.|||Fault-bound, discontinuous lenses of polymictic conglomerate, quartzite, interbedded sandstone and siltstone, fossiliferous and intraclast limestones and dolomite. Conglomerate and limestones are mapped separately.|
73405|Wheeney Creek Formation|70648|5|Briefly described|Map Legend|Ordovician|Cambrian|||Kayrunnera Group|||Weakly cleaved, fault-bound discontinuous lenses of sedimentary rocks including polymictic conglomerate, ridge-forming quartzite, interbedded sandstone and siltstone, fossiliferous limestone (conodonts), intraclast limestone and dolomite.|
24570|Wheeo Basalt|39848|2|Defined|p115|early Miocene|late Oligocene|Late Oligocene to Early Miocene||||||
24570|Wheeo Basalt|40240|5|Briefly described|p107|||||||||
24570|Wheeo Basalt|40293|6|Mentioned|p459|||||||||
24570|Wheeo Basalt|40742|5|Briefly described|p298|||||||||
24570|Wheeo Basalt|41110|5|Briefly described|p223|||||||||
24570|Wheeo Basalt|50232|5|Briefly described|Map legend|Miocene|Miocene|Black alkali basalt to basanite flows, containing porphyritic olivine and T-augite, with flow-banding, vesicles and doleritic textures.||||||
24570|Wheeo Basalt|50233|5|Briefly described|Map Legend|Miocene|Miocene|Black alkali basalt to basanite flows, containing porphyritic olivine and Ti-augite, with flow banding, vesicles and doleritic textures.||||||
24570|Wheeo Basalt|50234|5|Briefly described|Map Legend|Miocene|Miocene|Black alkali basalt to basanite flows, containing porphyritic olivine and Ti-augite, with flow banding, vesicles and doleritic textures.||||||11-MAY-04
24570|Wheeo Basalt|61155|5|Briefly described|p19|Early Miocene|Late Oligocene|In the Bathurst-Goulburn region. ||||||
24570|Wheeo Basalt|64238|5|Briefly described|Map legend|Cenozoic|Cenozoic|Alkali olivine basalt and basanite, doleritic in part, with local concentrations of ultramafic xenoliths.||||||19-NOV-08
24570|Wheeo Basalt|68592|2|Defined|p237, p398, p630, p1787-9, p1814-8|Miocene|Miocene|See also p37, p116-8. Bishop (1984) named several basalts which had been grouped by Wellman and McDougall (1974) in their Abercrombie Province. Since they are all believed to be from a single series of related flows, they have all been placed in the one Formation and named after the most extensive of Bishop's units. Type section described. Generally at a slightly lower level than the older Crookwell Basalt; flowed over a more dissected landscape, i.e. along valleys. Associated with poor quality sapphires at Mount Werong. K-Ar age determinations discussed. Has been used for dimension stone and crushed aggregate. Sapphires of uncertain origin have been found in association with these basalts.|24-14 Ma.|||Unconformably overlies Rockley Volcanics, Fosters Creek Conglomerate.|Hard, black, locally vesicular, olivine basalt verging on basanite; ultramafic xenocrysts and xenoliths common. Terraced; very jointed and locally deeply weathered series of basalt flows.|
24570|Wheeo Basalt|70192|5|Briefly described|Map Legend|Miocene|Miocene|Czw. On Crookwell, Taralga and Gunning 1:100 000 mapsheet portions of Time-Space Plot.|||||Alkali, olivine phyric basalt to basanite, doleritic in part with local concentrations of ultramafic xenoliths and xenocrysts.|
24570|Wheeo Basalt|70541|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Black, alkali olivine phyric basalt to basanite, doleritic in part with local concentrations of ultramafic xenoliths and xenocrysts.|
24570|Wheeo Basalt|70542|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Black, alkali olivine phyric basalt to basanite, doleritic in part with local concentrations of ultramafic xenoliths and xenocrysts.|
24570|Wheeo Basalt|70543|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Alkali, olivine phyric basalt to basanite, doleritic in part with local concentrations of ultramafic xenoliths and xenocrysts.|
24570|Wheeo Basalt|70544|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Alkali olivine basalt-basanite, doleritic in part with local concentrations of ultramafic xenoliths and xenocrysts.|
24570|Wheeo Basalt|70545|5|Briefly described|Map Legend|Neogene|Palaeogene||||||Alkali, olivine phyric basalt to basanite, doleritic in part with local concentrations of ultramafic xenoliths and xenocrysts.|
24570|Wheeo Basalt|71069|6|Mentioned|p76 fig 27|||||||||
24570|Wheeo Basalt|73581|5|Briefly described|p22|Miocene|Miocene|Grabben Gullen Volcanic Province. Grouping of multiple distinct and dissected erosional outcrops of basalt within valley floors. The basalt is alkaline, verging on basanite.|21.0-14.4 Ma K-Ar||||Moderately vesicular, flow-laminated, olivine- and titanaugite-phyric basalt. Common Cr-spinel and lherzolite mantle xenoliths.|
69869|Whick Whack Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes the Yarra, Spring Road, Romner and Burnt Hill Granites.||||||
69869|Whick Whack Suite|68592|1|Redefined|p650, p1482-9, p1508-26|Early Devonian|Early Devonian|Blevin (2011); redefined here to include Romner Granite which Blevin regarded as part of Hovells Suite. Named after the locality of Whick Whack. Geochemistry described. No significant mineralisation: traces of Mo, and alluvial gold of uncertain origin. ||Unit in Keverstone Supersuite.|Includes Yarra, Spring Road, Burnt Hill and Romner Granites.|Intrudes Adaminaby Group, Cuddyong Formation and Binda Granite. Is intruded by Blackmans Creek Granite.|Pinkish to cream to grey, fine- to coarse-grained, massive, foliated to protomylonitic, equigranular to sporadically porphyritic, biotite granite, hornblende-biotite granite and leucogranite; minor biotite-quartz syenite. A-type.|
69869|Whick Whack Suite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Burnt Hill Granite, Romner Granite, Spring Road Granite, Yarra Granite.|||
69869|Whick Whack Suite|70544|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Burnt Hill Granite, Romner Granite, Spring Road Granite, Yarra Granite|||
24097|Whinfell Chert|22555|6|Mentioned|p375|||of Ballast Formation||||||
24097|Whinfell Chert|23171|6|Mentioned|p11|||(Felton 1981).||||||
24097|Whinfell Chert|23173|4|Described|Map Legend|||||||||
24097|Whinfell Chert|39618|2|Defined|p27|Early Silurian|Cambrian|Cambrian - Early Silurian||||||
24097|Whinfell Chert|40624|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
24097|Whinfell Chert|65469|6|Mentioned|p15, 17, 20|Late Ordovician|Middle Ordovician|Lachlan Orogen||Girilambone Group||||06-NOV-17
24097|Whinfell Chert|72080|5|Briefly described|p6, p12|Darriwilian|Darriwilian|Occurs to the north of the Harts Tank area. Potential correlative of the Alandoon Chert.||Girilambone Group||Equivalent to the Ballast Formation.||07-JAN-22
76995|Whipstick Monzogranite|72528|5|Briefly described|p1, p3 Tb.1.1, p18-p24, p108, p124.|Emsian|Emsian|Magmatic crystallisation age determined. Provides  a maximum age for molybdenum-bismuth mineralisation hosted by the pluton. Age is indistinguishable from the 402.5 +/-2.8 Ma Mount Poole Monzogranite (Bodorkos et al., 2015) of the Kameruka Supersuite some 30 km to the southwest. This pluton is one of many that comprise the Bega Batholith.|403.9+/-2.6 Ma U238/Pb206 (Pb204-corrected)|Whipstick Suite||Intrudes Adaminaby Group and underlies Merrimbula Group and is intruded by the Jingera Rock Syenite.|Dated sample is a very felsic, medium-grained equigranular leucocratic granite. Includes coarse-grained leucocratic syenogranite.|
31660|Whipstick Suite|22815|6|Mentioned|p81|||||||||
31660|Whipstick Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
31660|Whipstick Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
31660|Whipstick Suite|44093|5|Briefly described|p202 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31660|Whipstick Suite|72528|6|Mentioned|p18.|Emsian|Emsian|Age from Whipstick Monzogranite.|||Includes Whipstick Monzogranite|Intrudes Adaminaby Group and underlies Merrimbula Group and is intruded by the Jingera Rock Syenite.|Includes coarse-grained leucocratic syenogranite.|
23186|Whitbarrow Creek Complex|23171|6|Mentioned|p12,28|||Previously known as the Gilgai complex (Jones 1991).||||||
23186|Whitbarrow Creek Complex|23173|4|Described|Map Legend|Late Ordovician|Late Ordovician|||||||
70473|White Rocks Ignimbrite Member|62095|2|Defined|p274 Appdx.|Late Carboniferous|Late Carboniferous|Of Currabubula Fm. Supersedes White Rocks Tuff Member (Dawson 1988 and Davies 1988) and Castle Mountain Tuff Mbr. (Cherry 1987).  Welded rhyodacitic ig. Overlies Cana Creek Tuff Mbr; overlain by Bindawalla Ig.Mbr. in Castle Mt.Dome area. Age: 315.3+/-3Ma.||||||26-MAR-07
35789|Whiteheads Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Part of the Wologorong Batholith.||||||
24099|Whitlock Conglomerate Member|22857|5|Briefly described|p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Burthong Formation (Mouramba Group, Cobar Supergroup). Max. thickness: 400m. Geological Province: Mouramba Shelf.||||||
24099|Whitlock Conglomerate Member|41528|2|Defined|p57|Early Devonian||||||||
24099|Whitlock Conglomerate Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
24099|Whitlock Conglomerate Member|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
24099|Whitlock Conglomerate Member|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Mouramba Group||||
26212|Whitlow Formation|721|5|Briefly described|Map legend|Late Carboniferous|Late Devonian|Low-grade, regionally metamorphosed, multiply deformed, thickly bedded, coarse-grained and minor fine-grained lithic wacke, subordinate siltstone and minor granule conglomerate.||||||
26212|Whitlow Formation|22857|4|Described|p502 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Max. thickness: ?1km. Geological Province: Texas-Coffs Harbour Slope and Basin.||||||
26212|Whitlow Formation|23050|4|Described|p15 Table 1|Early Carboniferous|Early Carboniferous|Age: Late Tournisian to early Visean age based on age equivalent Sandon beds.||||||
26212|Whitlow Formation|23051|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
26212|Whitlow Formation|23790|5|Briefly described|p10 Fig. 2|Early Carboniferous|Early Carboniferous|Geological Province: Central Block||||||
26212|Whitlow Formation|24366|5|Briefly described|p7, 17 Fig. 3|Early Carboniferous|Early Carboniferous|||||||
26212|Whitlow Formation|41328|2|Defined|p11|Middle Carboniferous|Early Carboniferous|Reserved as Whitlow||||||
26212|Whitlow Formation|41329|6|Mentioned|p6|||||||||
26212|Whitlow Formation|42554|5|Briefly described|p45|||||||||
26212|Whitlow Formation|42748|6|Mentioned|Fig.3 P9|Carboniferous||||||||
26212|Whitlow Formation|43091|5|Briefly described|Map legend|||||||||
26212|Whitlow Formation|43582|6|Mentioned|p4|||||||||
26212|Whitlow Formation|62534|5|Briefly described|p6, p11 (legend)|Early Carboniferous|Early Carboniferous|Intruded Dumboy-Gragin Granite.||||||07-FEB-11
26212|Whitlow Formation|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Cambrian|In Central Block and Woodsreef Melange.||||||10-DEC-07
26212|Whitlow Formation|67669|6|Mentioned|p14|||Geological province: New England Fold Belt.||||||
26212|Whitlow Formation|68003|5|Briefly described|p31, p32 Fig.3-h, p140.|Early Carboniferous|?Late Devonian|Central Block, New England Fold Belt. Coeval with Texas beds.||||Overlies Cara Formation.|Low grade regionally metamorphosed, multiply deformed, thickly-bedded feldspathic and volcanic lithic wacke, interbedded siltstone, fine wacke and minor conglomerate and rare olistostromal limestone; some siltstone and wacke are tuffaceous.|
26212|Whitlow Formation|68005|5|Briefly described|p18, p22, pp31-32, p155, p169, p170.|Early Carboniferous|Early Carboniferous|Anaiwan terrane, Central Block, New England Fold Belt. Deep marine deposition. Low grade, regionally metamorphosed, multiply deformed; locally highly deformed; part of subduction complex. Thickness unknown because of poor exposure and thrust repetition.||||Unconformably overlies Cara Formation. Is intruded by Dumboy-Gragin Granite and Bundarra Supersuite. Is overlain by Texas and Sandon beds.|Thick-bedded, coarse-grained and minor fine-grained feldspathic volcaniclastic arenites and wackes with subordinate siltstone and conglomerate; rare olistostromal beds and oolitic detritus within volcaniclastic arenites.|
26212|Whitlow Formation|68006|5|Briefly described|p20 Fig.3-A, p25. |||Central Block, New England Fold Belt. Hosts small, discontinuous limestone lenses of dubious economic importance.||||Unconformably overlies Cara Formation. Is overlain by Texas and Sandon beds.||
26212|Whitlow Formation|69639|6|Mentioned|p211, p218|Carboniferous|Carboniferous|||||Intruded by the Attunga Creek Monzogranite.||
26212|Whitlow Formation|70036|5|Briefly described|Map legend|||Central Block, New England Fold Belt. Included in a mapped unit of Silurian to Carboniferous strongly deformed, andesitic to rhyolitic metasedimentary rocks, lithic sandstone, argillite, chert and jasper.||||||
26212|Whitlow Formation|71628|5|Briefly described|p4: 9, 15, 17, 24, 29, 40; p19-27|||||||Is intruded by Banalasta, Copeton and ?Namoi Tops Monzogranites; and Dumboy-Gragin Leucosyenogranite.|Tuffaceous chert, siltstone, mudstone, sandstone and conglomerate.|
24100|Whoey Tank Formation|22857|4|Described|p440 App.1, Tb.A1.6|Emsian|Pragian|Of the Walters Range Group (Cobar Supergroup). Max. thickness: >200m. Geological Province: Darling Basin. ||||||
24100|Whoey Tank Formation|41394|2|Defined|p95|Pragian||||||||
24100|Whoey Tank Formation|41395|6|Mentioned|Map legend|Pragian||||||||
24100|Whoey Tank Formation|61964|5|Briefly described|p104|||Of the Walters Range Group 0n KILPARNEY 1:100k sheet.||||||
24100|Whoey Tank Formation|70751|6|Mentioned|p12|Pragian|Pragian|||Walters Range Group||||
24100|Whoey Tank Formation|72958|6|Mentioned|p11|Emsian|Pridoli|Cobar Basin. Nymagee area.||Walters Range Group||Underlain by and equivalent to Lumga Siltstone. Equivalent to Yar Sandstone and in part to Winduck Group. Overlain by Crowl Creek Formation (Mulga Downs Group).||
31661|Why Worry Suite|22815|5|Briefly described|p74|||Part of the Bega Batholith.  Comprises Why Worry and Pretty Point Tonalites, separated by a narrow discontinuous screen of metasediments of the Adaminaby Group.||||||16-FEB-05
31661|Why Worry Suite|42726|5|Briefly described|Map Legend||Early Devonian|||||||
31661|Why Worry Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||
31661|Why Worry Suite|66575|6|Mentioned|p949,|||Bega Batholith. I-Type.||||||
31661|Why Worry Suite|72571|6|Mentioned|p101|||||||||
31661|Why Worry Suite|73264|6|Mentioned|p1393, p1405|Early Devonian|Early Devonian|Lachlan Orogen, eastern. I-type.|400 Ma|||||
31661|Why Worry Suite|73514|6|Mentioned|p8|||Lachlan Fold Belt.|||||I-type.|
23193|Why Worry Tonalite|22815|4|Described|p74|||||||||
23193|Why Worry Tonalite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Why Worry Suite.||||||
27000|Whylandra Formation|22857|5|Briefly described|p456 App.1, Tb.A1.6|Devonian|Silurian|Of the Toongi Group. Greywacke and shale. Max. thickness: 1280m. Geological Province: Cowra Trough.||||||10-MAR-06
27000|Whylandra Formation|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Toongi Group.||||||
27000|Whylandra Formation|23170|2|Defined|p119|Late Silurian|Late Silurian|of Toongi Group.||||||
27000|Whylandra Formation|29986|6|Mentioned|Map legend|Devonian|Silurian|Devonian-Silurian||||||
27000|Whylandra Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
27000|Whylandra Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
27000|Whylandra Formation|40328|3|Fully described|p131|||||||||
27000|Whylandra Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
27000|Whylandra Formation|43500|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition) Part of Toongi Group||||||
27000|Whylandra Formation|48958|6|Mentioned|Plate 1|||||||||
27000|Whylandra Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Greywacke and shale.||||||
27000|Whylandra Formation|68003|5|Briefly described|p24 Fig.3-e, p144. |Ludlow|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Belowrie Formation. Is overlain by Toongi Hall Tuff.|Lithic sandstone, volcaniclastic sandstone, siltstone, tuffaceous siltstone.|
27932|Whynot Coal Member|29942|4|Described|Fig.1|||Permian||||||
27932|Whynot Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27932|Whynot Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27932|Whynot Coal Member|40805|6|Mentioned|Table 1|||||||||
27932|Whynot Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Malabar Formation.||||
24103|Widden Brook Conglomerate|22857|5|Briefly described|p524 App.1 Tb.A1.9|Early Triassic|Late Permian|Of the Clifton Subgroup (Narrabeen Group). Conglomerate and sandstone. Max. thickness: 38m. Geological Province: Sydney Basin.||||||
24103|Widden Brook Conglomerate|22969|6|Mentioned|p 41|||||||||
24103|Widden Brook Conglomerate|36042|6|Mentioned|Fig.22|||||||||
24103|Widden Brook Conglomerate|39287|6|Mentioned|p42|||||||||
24103|Widden Brook Conglomerate|39293|6|Mentioned|Fig. 8.11|||||||||
24103|Widden Brook Conglomerate|41010|6|Mentioned|p17|||See also Table 1||||||
24103|Widden Brook Conglomerate|41902|6|Mentioned|p3|||||||||
24103|Widden Brook Conglomerate|42916|5|Briefly described|Table 1||Early Triassic|||||||
24103|Widden Brook Conglomerate|43194|5|Briefly described|p118-119, p130|Early Triassic|Early Triassic|Of Narrabeen Group, Hunter Valley region, Sydney Basin. Equivalent to the informal 'lower lithic conglomerate unit' of the Digby Formation, Gunnedah Basin. ||||||
24103|Widden Brook Conglomerate|43257|5|Briefly described|Map Legend|Early Triassic|Late Permian|Of Clifton Subgroup||||||
24103|Widden Brook Conglomerate|43360|14|Not recorded|Map Legend|||(Provisional first edition)||||||
24103|Widden Brook Conglomerate|43361|14|Not recorded|Map Legend|||(Provisional first edition)||||||
24103|Widden Brook Conglomerate|61315|5|Briefly described|Table SY1|Eary Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
24103|Widden Brook Conglomerate|68003|5|Briefly described|p42.|Early Triassic|Early Triassic|Hunter Valley. Thick conglomerate sequences formed by large alluvial fans, generated by erosion in the uplifted New England Fold Belt.||||||
29142|Wilangee Basalt|22553|6|Mentioned|p77,p83|||part of the Adelaidean sequence||||||
29142|Wilangee Basalt|22752|6|Mentioned|p 275|||||||||
29142|Wilangee Basalt|22772|5|Briefly described|p53,63,65,Table13.1|Cryogenian|Cryogenian|||||||
29142|Wilangee Basalt|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of Wendalpa Subgroup (Poolamacca Group). Includes pillow basalts. Overlies the Boco Formation. Correlative of Wooltana Volcanics of South Australia. Max. thickness: ~160m. Geol. Prov: Adelaide Fold belt. See also p398 and p400 App. 1 Tb A1.3.||||||
29142|Wilangee Basalt|34812|3|Fully described|p63|||||||||
29142|Wilangee Basalt|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
29142|Wilangee Basalt|36411|6|Mentioned|p270|||Refs Cooper et al 1978 for definition of modified name.||||||
29142|Wilangee Basalt|37931|4|Described|p533|||||||||
29142|Wilangee Basalt|39214|6|Mentioned|Table 1|||||||||
29142|Wilangee Basalt|39885|6|Mentioned|p431|||||||||
29142|Wilangee Basalt|40291|6|Mentioned|p11|||||||||
29142|Wilangee Basalt|40595|6|Mentioned|p77|||||||||
29142|Wilangee Basalt|41403|4|Described|p53|||||||||
29142|Wilangee Basalt|43052|6|Mentioned|p172|||||||||
29142|Wilangee Basalt|43269|5|Briefly described|Map Legend||Neoproterozoic|of Wendalpa Group.||||||
29142|Wilangee Basalt|46889|6|Mentioned|p272|||||||||
29142|Wilangee Basalt|69666|6|Mentioned|p24, p26, p36|Neoproterozoic|Neoproterozoic|Broken Hill area. Part of the Willouran Basic Province.||||||
29142|Wilangee Basalt|70000|5|Briefly described|p34, p40|Neoproterozoic|Neoproterozoic|The Delamerian-Ross Orogeny produced low-grade metamorphism, with a chlorite-actinolite +/- biotite metamorphic assemblage.||Unit in Wendalpa Subgroup.||Overlies Boco Formation.|Continental flood basalt.|
29142|Wilangee Basalt|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Wendalpa Subgroup.||Overlies Boco Formation.|Black, variably altered, amygdaloidal, vesicular basalt with plagioclase, actinolite and magnetite.|07-SEP-15
29142|Wilangee Basalt|71129|5|Briefly described|p103|Tonian|Tonian|Geological Province: Curnamona Province, Gawler Craton. Part of the Willouran Basic Province, which also includes Beda Basalt, and the Wooltana and Cadlareena volcanics, Little Broken Hill Gabbro, and Gairdner Dolerite. Related to the Rodinian break-up (Zhao et al., 1994, Li et al., 1999, Wang et al., 2010). Basaltic volcanism interpreted to be result of mantle plume upwelling, causing doming in the continental lithosphere (Zhao et al., 1994).||||||
29142|Wilangee Basalt|72461|6|Mentioned|p16 fig 9|||||||||
31300|Wilbertree Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Fine sandstone.||||||
83659|Wild Cattle Trachyandesite|73581|6|Mentioned|p7|||Marker unit separating the Governors Chair Volcanics and Superbus Basalt, absent in places. Originally described as a melanotrachyte.||||||
25625|Wild Wave Granodiorite|22700|5|Briefly described|p785|||Age: 418+/-2 Ma.||||||
25625|Wild Wave Granodiorite|23171|5|Briefly described|p12,39||Ludlow|Max Age: 418 (+/-) 2 Ma (Rb-Sr).||||||
25625|Wild Wave Granodiorite|23173|4|Described|Map Legend|Ludlovian|Ludlovian|||||||
25625|Wild Wave Granodiorite|39083|4|Described|p27|||||||||
25625|Wild Wave Granodiorite|42144|6|Mentioned|p603|||||||||
25625|Wild Wave Granodiorite|42521|5|Briefly described|p15|||Age: 418 +/- Ma.||||||23-APR-09
25625|Wild Wave Granodiorite|42566|6|Mentioned|p25|||||||||
25625|Wild Wave Granodiorite|43032|5|Briefly described|p23|||Age of 418 +/-2 Ma.||||||23-APR-09
25625|Wild Wave Granodiorite|43153|5|Briefly described|Map Legend|Silurian|Ordovician|||||||
25625|Wild Wave Granodiorite|43774|3|Fully described|p15-16||Silurian|Age: 418+/-12 Ma.||||||23-APR-09
25625|Wild Wave Granodiorite|68823|5|Briefly described|p376 Fig.3, p377, p378 Fig.4|Lochkovian|Pridoli|Near Cobar. Lachlan Orogen.|418 +/- 2 Ma, Rb-Sr (Glen et al. 1983)|||||
25625|Wild Wave Granodiorite|69541|6|Mentioned|p645 Fig.1(b)|Late Silurian|Late Silurian|Lachlan Orogen.||||||
25625|Wild Wave Granodiorite|70941|6|Mentioned|p9|||||||||
25625|Wild Wave Granodiorite|71039|5|Briefly described|p27|Early Devonian|Early Devonian|I-type.|418 +/- 2 Ma (Rb-Sr, Glen et al, 1983)|||Overlain by the Meryula Formation.||10-MAR-23
25625|Wild Wave Granodiorite|72958|6|Mentioned|p5, p46, p61|Pridoli|Wenlock|Part of a series of Silurian basement granites that underlie the Cobar Basin.|424.1 +/- 2.4 Ma|||||
25625|Wild Wave Granodiorite|73578|4|Described|p1, p3, p28, p39-44, p50|Pridoli|Gorstian|New U-Pb SHRIMP magmatic crystallisation age from zircon of 424.1 +/- 2.8 Ma reported. Forms clasts within pebble conglomerates of the lowermost Cobar Basin. A previous biotite Rb-Sr age of 418 +/- 2 Ma was obtained by Glen et al. (1983).|424.1 +/- 2.8 Ma zircon SHRIMP|||Intrudes the Girilambone Group.|I-type igneous rocks including coarse-grained biotite granodiorite.|
27615|Wilgaroon Granite|730|5|Briefly described|p20, p15, p17, p36, p60, p61.|||Sheared, greisenized granodiorite and porphyritic microgranite. Samples contain 5% K2Oand 20 - 40 ppm Sn. May coalesce at depth with Tinderra Granite. Associated hornfels has slightly anomalous tin values.||||||11-NOV-14
27615|Wilgaroon Granite|23171|5|Briefly described|p12-3,30|||||||||
27615|Wilgaroon Granite|23173|4|Described|Map Legend|||||||||
27615|Wilgaroon Granite|35287|5|Briefly described|p3|||||||||
27615|Wilgaroon Granite|35383|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
27615|Wilgaroon Granite|35385|3|Fully described|p17|||||||||
27615|Wilgaroon Granite|36411|6|Mentioned|p270|||Refers Baker 1978 for definition.||||||
27615|Wilgaroon Granite|38292|6|Mentioned|p3|||||||||
27615|Wilgaroon Granite|40328|4|Described|p212|||||||||
27615|Wilgaroon Granite|42566|6|Mentioned|p25|||||||||
27615|Wilgaroon Granite|42726|5|Briefly described|map legend|Silurian||||||||
27615|Wilgaroon Granite|43032|5|Briefly described|Table 1.|||||||||
27615|Wilgaroon Granite|43090|5|Briefly described|Map legend||Silurian|||||||
27615|Wilgaroon Granite|43153|5|Briefly described|Map Legend|Silurian|Ordovician|||||||
27615|Wilgaroon Granite|43774|3|Fully described|p13-15||Silurian|||||||
27615|Wilgaroon Granite|68823|6|Mentioned|p376 Fig.3, p377|Devonian|Late Silurian|North of Cobar.||||||
27615|Wilgaroon Granite|69635|4|Described|p113-118, p69|Early Devonian|Silurian|North-western Lachlan Orogen.  U-Pb SHRIMP zircon magmatic crystallisation age (tentative).|408+/-17 Ma|||Interpreted to intrude the Ordovician Girilambone Group (hornfels contact aureole)|S-type granite with muscovite-biotite granite, greisenous granodiorite and porphyritic microgranite lithologies. Sample: massive, medium- to coarse-grained, weakly chlorite altered, quartz-K-feldspar-biotite-muscovite granite with little variation.|
27615|Wilgaroon Granite|70602|6|Mentioned|p67 Fig 3|Early Devonian|Silurian|Age inferred from map symbol.||||||
27615|Wilgaroon Granite|71345|2|Defined|p4,25-29|Emsian|Ludlow|Type location: OXCOPJG0774, a large tor measuring 20m wide x 3 m high at Lat: -30.9764 Long: 145.7059 (GR GR676418 6572292). Named for the Wilgaroon homestead. First described and defined by Baker et al., 1975. Byrnes (1993) interpreted the granite to lie at the northern end of the Wagga tin belt. Exposed on both the Cobar and Bourke 1:250 000 map sheet areas (see p25 for more detail about distribution). Coincident magnetic and gravity lows in the area of the type localities; rwo NW trending magnetic lows approximately 4km long between White Tank and Darling Downs. Fraser et al., 2014 reported a SHRIMP U-Pb zircon age of 408+\-16 Ma. Felsic intrusives associated with mineralisation at the Arrawa (Cu, W, Bi with lesser Pb, Zn, Sn, Mo) and Wilgaroon (Chinamans) (Au with lesser Pb, Ag) prospects may be related to the Wilgaroon Granite (Byrnes 1993).|408+\-16 Ma (SHRIMP U-Pb, magmatic)|||Intrudes into Girilambone Group.|S-type quartz-muscovite-biotite granite with griesenous phases and porphyritic microgranite; massive to weakly foliated. Variably sheared.|02-DEC-19
27615|Wilgaroon Granite|71360|5|Briefly described|Map legend|Late Silurian|Late Silurian|Part of the Wagga Batholith. Geophysical signature: small NW-trending non-magnetic unit with high radioelement counts. The unit is located near the Tinderra Granite (Cobar 1:250 000 map sheet) in an area of low gravity values.|||||Medium-grained, leucocratic, muscovite-biotite S-type granite, greisenous granodiorite, and porphyritic microgranite.|
27615|Wilgaroon Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped S-type intrusion.|||||Altered biotite-muscovite microgranite to granodiorite, deformed to gneiss in shear zones. Muscovite-biotite granite, greisenous granodiorite, porphyritic microgranite.|
24106|Wilkerboon Conglomerate Member|22857|5|Briefly described|p440 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Roset Sandstone (Mouramba Group, Cobar Supergroup).||||||
24106|Wilkerboon Conglomerate Member|41528|2|Defined|p73|Early Devonian||||||||
24106|Wilkerboon Conglomerate Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
38898|Wilkurra Granite|73177|5|Briefly described|p1113 Fig.15, 1115 Fig.17, 1117|Silurian|Silurian|Western Lachlan Orogen. Contains 500-490 Ma zircon grains (cf Saint Arnaud Group).|425-420 Ma.|||||
39534|Willandra Sandstone|61964|2|Defined|p14 Fig. 4, p33|Bolindian|Eastonian|Of Bendoc Group. Detailed lithology presented. Sequence also informally referred to as "Eulendool Formation" (MacRae and Pogson (1990). Overlies Currawalla Shale.  Palaeontology (p259)||||||
39534|Willandra Sandstone|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Bendoc Group. Grey to black, medium-grained, medium bedded quartz-rich sandstone, interbedded black quartzofeldspathic muddy sandstone and graptolitic black shale.||||||10-APR-08
39534|Willandra Sandstone|64568|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Bendoc Group.Grey to black, medium-grained, medium bedded quartz-rich sandstone, interbedded black quartzofeldspathic muddy sandstone and graptolitic black shale.||||||
39534|Willandra Sandstone|64963|5|Briefly described|p184|||Renewed quartz-rich trubidites deposited in a mega-fan environment, west of West Wyalong.||||||
39534|Willandra Sandstone|65469|5|Briefly described|p18|Late Ordovician|Late Ordovician|Lachlan Orogen.||||Overlies the Currawalla Shale.||
39534|Willandra Sandstone|67322|4|Described|p19; Fig.5|Late Ordovician|Late Ordovician|Approximately 800m thick. Named by Hendrickx and Colquhoun, in Colquhoun et al. (2005). Black shale beds within the Willandra Sandstone contain late Eastonian to early Bolindian graptolite fauna. Reginally extensive in the Cargelligo region.||Of the Bendoc Group||Interfingers with and overlies the Currawalla Shale.|Quartz-rich sandstone, white to pale grey, and poorly/moderately sorted with subangular/rounded quartz and lithic grains; minor poorly sorted black sandstone is also distributed throughout the unit; rare gritty lithic sandstone; black shale beds.|22-FEB-18
39534|Willandra Sandstone|68466|6|Mentioned|p65|Late Ordovician|Late Ordovician|Albury-Bega Terrane.||||||
39534|Willandra Sandstone|68592|4|Described|p320, p351, p363-4|Late Ordovician|Late Ordovician|Cargelligo region.||Unit in Bendoc Group.||Conformably overlies Currawalla Shale. Correlative of New Country and Poidevins Sandstones.|Contains subordinate black graptolitic shale in metre-thick packages throughout.|
39534|Willandra Sandstone|69160|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Bendoc Group.||Overlies Currawalla Shale.|Grey to black, medium-grained, medium-bedded quartz-rich sandstone, interbedded black quartzofeldspathic muddy sandstone and graptolitic black shale.|
39534|Willandra Sandstone|69540|5|Briefly described|p640|Bolindian|Bolindian|Central NSW.|||||Quartz-rich turbidites.|
39534|Willandra Sandstone|69668|6|Mentioned|p929 Fig.2|Late Ordovician|Late Ordovician|Cargelligo area, Albury-Bega terrane.||||Overlies Currawalla Shale.||
39534|Willandra Sandstone|71069|5|Briefly described|p72, p74, p87|Early Silurian|Late Ordovician|Preserved thickness of 800m. Generally recessive outcrop characteristics except where it is contact metamorphosed. Contains fossils of flattened spherical sponges (c. Hindia).||Bendoc Group||Conformably overlies the Currawalla Shale. Is equivalent to the New Country Sandstone and members of the Margules Group.|Grey, medium to coarse grained, moderate to poorly sorted quartzose sandstone. These are interbedded with packages of graptolitic black shale and distinctive black medium to coarse grained, poorly sorted lithic-quartz sandstone.|
39534|Willandra Sandstone|71700|5|Briefly described|CD|||||||Equivalent to the Mundoonen Sandstone and the New Country Sandstone.||
39534|Willandra Sandstone|71889|5|Briefly described|p9, p11, p16-p17|Late Ordovician|Late Ordovician|Outcrops in Buckingbong State Forest.||||Overlies the Currawalla Shale.|Very coarse-grained lithic-rich turbidites consisting of dark-coloured lithic sandstone and thin beds of black shale intercalated within.|
39534|Willandra Sandstone|72084|5|Briefly described|p7-8|||Forms ridges of the Malebo Range.||||Overlies, and is intercalated with, Currawalla Shale.|Grey to bluish-grey, foliated, lithic-bearing fine- to medium-grained metaquartz-arenite.|
39534|Willandra Sandstone|73140|5|Briefly described|p495|Bolindian|Bolindian|Proposed to be reassigned from the Bendoc Group to Margules Group. Age based on graptolites. Uncertainty indicated for minimum age.||Margules Group||Overlies Currawalla Shale||
39534|Willandra Sandstone|73457|6|Mentioned|p8|Ordovician|Ordovician|||||||
70517|Willawarra Rhyodacite Member|62095|2|Defined|p280 Appdx., Plate 1, p254 Figs. 4,5.|Asselian|Asselian|Top unit in Woodton Fm. Supersedes Willawarra Dacite (Lowe 1971) and Willawarra Rhyodacite (Kelk 1986). At least two flows of beige and white finely flow-banded rhyodacite lava and minor breccia. Disconformable under either Temi Fm. or Werrie Basalt.||||||
35405|Willawong Creek Granite|50231|5|Briefly described|Map Legend|Emsian|Emsian|||||||21-JAN-21
35405|Willawong Creek Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Grey to pinkish-grey, medium-grained, massive, equigranular to weakly porphyritic ferroan enstatite?-augite-biotite-hornblende granite and granodiorite.||||||25-JUN-08
35405|Willawong Creek Granite|68592|2|Defined|p935, p956, p1400-3, p1446-9|Early Devonian|Early Devonian|New unit and name, after Willawong Creek. Forms prominent rocky hills. Type locality described. A SHRIMP U-Pb zircon age of 418.9 +/- 2.8 Ma (Black, 2005) is considered too old and due to inherited zircons. It cannot be older than late Lochkovian (the age of the Mountain Creek Volcanics). Geochemistry detailed; geophysical properties described. Is adjacent to the Murringo Iron Prospect, but their relationship is uncertain.||Unit in Gooramma Suite.||Intrudes (and is probably comagmatic with) Mountain Creek Volcanics. Is faulted against Young Granodiorite and Hawkins Volcanics.|Grey, medium-grained, massive, generally equigranular (or rarely weakly porphyritic) orthopyroxene (ferroan enstatite?)-augite-biotite-hornblende granite to granodiorite. I-type.|21-JAN-21
35405|Willawong Creek Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgw. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Gooramma Suite|||Medium grained, massive, equigranular to weakly porphyritic, orthopyroxene-augite-biotite-hornblende granite to granodiorite; high to very high magnetic susceptibility.|
35405|Willawong Creek Granite|70296|5|Briefly described|p1, p14, p24|Lochkovian|Ludlow|Goulburn-Yass district. Constrains the age of the Bowning Orogeny.|418.9 +/- 2.8 Ma (SHRIMP U-PB)|||||21-JAN-21
35405|Willawong Creek Granite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Medium grained, massive, equigranular to weakly porphyritic, orthopyroxene-augite-biotite-hornblende granite to granodiorite; high to very high magnetic susceptibility.|
35405|Willawong Creek Granite|73215|5|Briefly described|p994|||Talmo-Taemas area.|419 +/- 3 Ma (Black, 2005).|||||
74586|Willdamar Tonalite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Gunning Suite. Bluish-grey, medium-grained, foliated, equigranular hornblende-biotite granodiorite to tonalite.  Low K, Th and U radioelement response.||||||12-JUN-08
74586|Willdamar Tonalite|68592|2|Defined|p1312-4, p1316-20, p1350-3, p1664|Early Silurian|Early Silurian|Named after Willdamar property. Formerly Willdamar Granodiorite. Referred to as Willdamar Granodiorite in the Bishopthorpe Suite chapter (see p1672). Previously part of Little Redbank Tonalite (Yacopetti, 1987) which was called Little Redbank Granite by Chappell et al. (1991). Present mapping has distinguished a western pluton, now defined as Little Redbank Granodiorite, separated by Mulgowrie Granodiorite from an eastern pluton here named Willdamar Tonalite. Crops out as scattered tors with some pavement outcrops in creeks. Type locality and other good exposures described. Geochemistry detailed; geophysical properties described. Not isotopically dated.||Unit in Gunning Suite.||Intrudes Adaminaby Group. Is intruded by Bigga Granite and Bishopthorpe Suite.|Bluish-grey, medium-grained, foliated, equigranular, hornblende-biotite tonalite and minor fine-grained, foliated, biotite granodiorite. Tourmaline-bearing veins and two roof pendants occur. I-type.|
74586|Willdamar Tonalite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sgw. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Gunning Suite|||Medium grained, foliated, equigranular, hornblende-biotite tonalite and minor biotite granodiorite; low K, Th and U response.|
74586|Willdamar Tonalite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Gunning Suite|||Medium grained, foliated, equigranular, hornblende-biotite tonalite and minor biotite granodiorite; low K, Th and U response.|
73407|Williams Creek Conglomerate|66623|2|Defined|p110, pp120-123. |Late Cambrian|Late Cambrian|Nuntherungie and Cupala Creek Basins. Defined in this study as the basal unit of the Cupala Creek Formation of Powell et al. (1982); initially part of Torrowangee Series of Mawson (1912). Correlative of Bilpa and Nuchea Conglomerates to the west. Thickness varies from 10 to 100 m. No fossils identified. Represents first post-Delamerian Orogeny deposition of sediments.||Basal unit in Cupala Creek Formation.||Basal unit of Cupala Creek Formation. Unconformably overlies Teltawongee Group. Has gradational contact with overlying Hummock Formation.|Variably cleaved, polymictic basal conglomerate with a wide range of local and foreign clasts, interbedded with red to maroon quartzose pebbly sandstone.|
73407|Williams Creek Conglomerate|67322|4|Described|p11; Fig.5|Series 3||Defined by Greenfield, in Greenfield et al.(2010); previously recognised as an unnamed basal conglomerate facies of the Cupala Creek Formation by Powell et al. (1982). Up to 100 m thick. Occurs in the Kayrunnera-Koonenberry region.||Basal unit of the Kayrunnera Group.||?Unconformably overlies the Copper Mine Range Formation (Ponto Group) Is overlain conformably by Hummock Formation.|Coarse polymictic conglomerate with well-rounded clasts of sandstone, mafic volcanics, and chert.|22-FEB-18
73407|Williams Creek Conglomerate|70838|4|Described|p269 Fig.3, p270-272, p275, p277-278|Cambrian|Cambrian|Nuntherungie Basin, SE Koonenberry Belt. Detrital zircon analyses. Provenance discussed.||Kayrunnera Group.||Is overlain by Cupala Creek Formation.|Poorly sorted and polymict, with angular to sub-rounded pebbles of pelite, psammite and granitic material and granules of quartz.|
73407|Williams Creek Conglomerate|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
73403|Williams Peak Granite|66623|2|Defined|pp49-51, p v. |Middle Cambrian|Middle Cambrian|Defined in this publication. Six outcrops, very weathered, around Williams Peak. Includes porphyritic sills with chilled margins and angular country rock xenoliths. Superficially resembles arkosic sandstone; characteristic salmon-coloured weathering. Possible correlation with Evelyn Creek volcanics intruding the Depot Glen Formation and Easter Monday Formation.|515.1 +/- 2.7 Ma.|||Intrudes eastern Teltawongee Group (Bunker Creek Formation).|Porphyritic rhyodacitic rock containing phenocrysts of feldspar and volcanic quartz (to 3 mm) in a fine-grained matrix; pale-cream to buff-brown dacitic rock devoid of phenocrysts.|
73403|Williams Peak Granite|67105|6|Mentioned|p655||||515.1 +/- 2.7 Ma|||Intrudes Bunker Creek Formation (Teltawongee Group).||
73403|Williams Peak Granite|67322|5|Briefly described|p10-11|Stage 4|Stage 3|Unit defined by Gilmore, in Greenfield et al. (2010).|515.1 +/- 2.7 Ma (U-Pb SHRIMP: Black, 2007).|||Intrudes Bunker Peak Formation (Teltawongee Group).||22-FEB-18
73403|Williams Peak Granite|70749|5|Briefly described|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.|515.1 +/- 2.7 Ma.|||||
73403|Williams Peak Granite|70838|5|Briefly described|p268, p270, p274|Cambrian|Cambrian|Shown as a unit in the Teltawongee Group. Appears as Williams Creek Granodiorite (p268) and Williams Peak Granodiorite (p274).|515 +/- 2.7 Ma (Black, 2007).|||Intrudes Bunker Creek Formation (Teltawongee Group).||
73403|Williams Peak Granite|71415|6|Mentioned|p15|Cambrian|Cambrian||c. 515 Ma|||||
73403|Williams Peak Granite|71593|5|Briefly described|p188|||Koonenberry Province.|c. 515 Ma|||Intrudes the Teltawongee Group.||
73403|Williams Peak Granite|71966|6|Mentioned|p990|Series 2|Series 2|Geological province: southern Thomson Orogen.|515.1+\-2.7 Ma|||||
73403|Williams Peak Granite|73177|5|Briefly described|p1100|||Northern Delamerian Orogen.|515.1 +/- 2.7 Ma (Black, 2007).|||Intrudes Teltawongee Group.||
73403|Williams Peak Granite|73430|6|Mentioned|p494|Cambrian|Cambrian|Koonenberry Belt. Syn-tectonic granite.|515+/-2.4 Ma (Black, 2007)||||Granite.|
69907|Willigam Sandstone Member|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Abercrombie Formation. Grey, poorly sorted, lithic-feldspar-quartz sandstone and interbedded siltstone. Graded bedding and ripple cross-lamination is common in sandstone beds.||||||28-MAY-08
69907|Willigam Sandstone Member|67322|4|Described|p17; Fig.5|Early Ordovician|Early Ordovician|Defined by Thomas and Scott, in Thomas et al.(in press). Age from conodonts in overlying Mummel Chert Member. Occurs in the Goulburn-Taralga region.||Of the Abercrombie Formation (Adaminaby Group).||Overlain by the Mummel Chert Member.|Quartzo-feldspathic sandstone.|22-FEB-18
69907|Willigam Sandstone Member|68466|6|Mentioned|p65|Early Ordovician|Early Ordovician|Albury-Bega Terrane.||Abercrombie Formation.||||
69907|Willigam Sandstone Member|68592|2|Defined|p282-4, p287, p289-90, p297-8, p300-3|Early Ordovician|Early Ordovician|See also xxiv, p112, p272, p274-5, p307. New name, after Willigam Hill. Representative section on Tarlo River specified. c.900m thick. Turbidites in a deep-marine setting. Occupies the core of the Mummel Anticline. Hosts the Mummel copper mine Cu-Pb-Zn sulfides in quartz veins. Characterised by the conodont Oepikodus evae.||Unit in Abercrombie Formation.|||Sublitharenite to subfelsarenite: distinctive in its prominent feldspar and lithic component, interbedded with siltstone and mudstone or shale.|
69907|Willigam Sandstone Member|69159|5|Briefly described|Map legend|Lancefieldian|Lancefieldian|||Unit in Abercrombie Formation.|||Grey-brown, khaki and olive, thinly- to thickly-bedded, fine- to coarse-grained, micaceous lithic-feldspar-quartz sandstone, interbedded with siltstone. Graded bedding and ripple cross-lamination are common.|07-SEP-15
69907|Willigam Sandstone Member|69668|6|Mentioned|p929 Fig.2|Middle Ordovician|Early Ordovician|Goulburn-Braidwood area, Albury-Bega terrane.||Unit in Abercrombie Formation.||||
69907|Willigam Sandstone Member|70192|5|Briefly described|Map Legend|Lancefieldian|Lancefieldian|[Theta]aaw. On Taralga, and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Abercrombie Formation||Within undifferentiated Abercrombie Formation.|Poorly sorted, feldspar lithic quartz sandstone and wacke, interbedded with siltstone, mudstone and shale; graded beddding and ripple cross lamination are common in sandstone beds.|
69907|Willigam Sandstone Member|70542|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Grey, poorly sorted, feldspar lithic quartz sandstone and wacke, interbedded with siltstone, mudstone and shale; graded bedding and ripple cross lamination are common in sandstone beds.|
69907|Willigam Sandstone Member|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|||Abercrombie Formation|||Poorly sorted, feldspar lithic quartz sandstone and wacke, interbedded with siltstone, mudstone and shale; graded beddding and ripple cross lamination are common in sandstone beds.|
69907|Willigam Sandstone Member|71069|5|Briefly described|p19, p21, p51, p52, p53 fig 19||Lancefieldian|Age based on conodont age determinations from overlying chert intervals. Misspellt on p56 and 61 as the Willigams Sandstone Member. See also  p54 fig 20, p55, p56, p58-p61, p63.||Abercrombie Formation||Is equivalent to the Pinnak Sandstone.|Immature, micaceous, lithic, quartzofeldspathic sandstone and siltstone.|
69907|Willigam Sandstone Member|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|||Abercrombie Formation.|||Grey-brown, khaki and olive, thin- to thick-bedded, fine- to coarse-grained, micaceous lithic-feldspar-quartz sandstone, interbedded with siltstone; graded bedding and ripple cross-lamination are common.|
69907|Willigam Sandstone Member|71700|3|Fully described|vi, x, p7-p8, p30, p40|Early Bendigonian|Lancefieldian|Albury-Bega Terrane. This units name is derived from the Willigam Hill. A representatitve section was defined in Thomas and Pogson 2012 along the Tarlo River about 3.5 km south of Willigam Hill from GR 745160 6178070 to GR 744125 6178740. Defined by Thomas and Pogson (2012). This unit has a minimum thickness of 1100m in Goulburn 250k and 1375m in Braidwood 100k. Distribution, geomorphic expression, outcrop, metamorphism, geophysical characteristics, fossils and structure are discussed. Lithology is described in some detail in the CD. A detailed stratigraphic section through this unit has not yet been measured, however in the eastern part of Braidwood100 a maximum thickness of 1375m is preserved and in Goulburn 250k 900m of section is preserved. Overlain gradationally, or interfingers with undifferentiated Abercrombie Formation.  Sourced from a low- to medium-grade metamorphic source terrain in the Ross-Delamerian Orogen. Appears as Willigams Sandstone Member on p44 and p84. Seperated from the Comerong Volcanics and Merrimbula Group by the Mongarlowe Fault. See also p43, p44, p54-p56, p66, p84 and CD.||Abercrombie Formation||Overlain by the Mummel Chert Member. Faulted against the Comerong Volcanics. Equivalent to the Adaminaby Group (in part).|Grey-brown, khaki and olive, thinly to thickly bedded, fine- to coarse-grained, micaceous lithic-feldspar-quartz sandstone, interbedded with siltstone.|
69907|Willigam Sandstone Member|73140|6|Mentioned|p495 Fig.1, Fig.3|Lancefieldian|Lancefieldian|Uncertainty indicated for maximum age.||Abercrombie Formation||||
27934|Willoona Tonalite|31580|6|Mentioned|p272|||See also Table 1-4 analysis||||||
27934|Willoona Tonalite|31581|3|Fully described|Table 1|||Analysis||||||
27934|Willoona Tonalite|32906|6|Mentioned|p239|||||||||
27934|Willoona Tonalite|36413|6|Mentioned|p77|||||||||
27934|Willoona Tonalite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Xenolith-rich tonalite and granodiorite. S-type. BMR map code: Smo.||||||
27934|Willoona Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
27934|Willoona Tonalite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb3.||||||
27934|Willoona Tonalite|45147|3|Fully described|M194|||||||||
27934|Willoona Tonalite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
29148|Willow Tree Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
29148|Willow Tree Formation|31882|5|Briefly described|p245|||||||||
29148|Willow Tree Formation|31883|6|Mentioned|p594|||See also Table 1||||||
29148|Willow Tree Formation|32482|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
29148|Willow Tree Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
29148|Willow Tree Formation|33686|6|Mentioned|p21|||||||||
29148|Willow Tree Formation|36961|6|Mentioned|Fig.3|||||||||
29148|Willow Tree Formation|37087|6|Mentioned|p194|||||||||
29148|Willow Tree Formation|37856|6|Mentioned|Table I|||||||||
29148|Willow Tree Formation|39288|5|Briefly described|p59|||||||||
29148|Willow Tree Formation|39308|6|Mentioned|p494|||Cored ddh||||||
29148|Willow Tree Formation|39468|6|Mentioned|Fig.2|||||||||
29148|Willow Tree Formation|41264|6|Mentioned|p251|||Recently Leard Formation||||||
29148|Willow Tree Formation|43407|14|Not recorded|Map Legend||Early Permian|(Provisional Edition)||||||
29148|Willow Tree Formation|61201|4|Described|p2, 5 Table 1, 6-7|Early Permian|Early Permian|Geological Province: Werrie Basin. Max, Thickness: 300m+. Shale, lithic sandstone, conglomerate, grit, ironstone, coal. Previously Willow Tree and Werris Creek Coal Measures. Overlies: Werrie Basalt. Underlies: Borambil Creek Formation.||||||
29148|Willow Tree Formation|61776|5|Briefly described|p194 Fig. 3|Early Permian|Early Permian|Geological Province: Werrie Basin. Lithic conglomerate, sandstone, siltstone, and coal.||||||
29148|Willow Tree Formation|68003|5|Briefly described|p38 Fig.3-j, p40, p129.|Early Permian|Early Permian|Werrie Basin (North), Brigalow Belt South Bioregion. Coeval with Koogah Formation in the south of the Basin; and correlative of Maules Creek Formation (Gunnedah Basin) and Greta Coal Measures (Hunter Coalfield).||||Overlies Warrigundi Complex and Werrie Basalt. Is overlain by Borambil Creek Formation.|Shale, lithic sandstone, conglomerate, coal.|
29148|Willow Tree Formation|68004|5|Briefly described|p66, 153.|||Werrie Basin. Correlative of Maules Creek Formation (Gunnedah Basin) and Greta Coal Measures (Hunter Coalfield). The Werris Creek deposit is limited, but c.3.9 Mt remains at Werris Creek Colliery site (now rehabilitated).||||Overlies Werrie Basalt. Is overlain by Borambil Creek Formation.|A terrestrial coal-bearing unit.|
29148|Willow Tree Formation|68006|5|Briefly described|pp92-94.|Early Permian|Early Permian|Werrie Basin. Contains nine coal seams, mined underground at Werris Creek Colliery from 1925 to 1963. Could produce very low sulfur export thermal coal. Potential for coal seam methane in synclines such as the Fairfield and Quirindi. Equivalent to Maules Creek Formation.||||||
29148|Willow Tree Formation|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Early Permian coal measures: conglomerate, lithic sandstone, siltstone, claystone, carbonaceous claystone and coal.||||||
82704|Willowrie Diorite|71628|4|Described|p19: 39, 171-172|||Originally Willowie Diorite of Dawson et al. (2004). Later the informal Willowrie diorite of Brown (2006); formalised in this study as Willowrie Diorite. Age from (Dawson in Stonestreet et al.,2006). Probably named after Willowrie Road in the general area, SW of Ashford. Is located ~14 km SW of Ashford. Crops out as tors over a circular 1.3 x 1.2 km area. Distinguished by a distinctive intense magnetic anomaly (described). Diamonds occur in the area.|244.3+/-2.5 Ma K-Ar.|Willowrie Creek Suite.||Intrudes Bundarra Supersuite and Texas beds.|Fine- to medium-grained diorite and microdiorite plug.|
77159|Willows Formation|24042|3|Fully described|p523 Appendix 1, p515|Late Pleistocene|Late Pleistocene|Type locality in quarry adjacent to Willows homestead.|56 - 38 ka (thermoluminescence)|||Overlain by Marra Creek Formation (6-0 ka). Also pre-dates Carrabear Formation (27-12 ka)|red, red-brown silty loam, predominantly alluvial; ~15% aeolian|
77159|Willows Formation|68003|5|Briefly described|p90.|Quaternary|Quaternary|Of Young et al. (2002). A formation within the Namoi alluvial system.|56 - 38 ka.||||Fine-grained red-brown silty loam deposits with 15% aeolian component.|
81160|Willurah igneous intrusions|70718|5|Briefly described|p77-78, p127, p3, p86|Mesozoic|Middle Devonian|No outcrop. Aeromag. Character: Eleven discrete, roughly circular (1-3 km wide), low amplitude (5-35 nT peaks) anomalies. Interpreted as an igneous intrusion.||||Intrudes the Booroorban granite suite, but not the overlying Murray Basin sediments.||02-JUN-19
39257|Willuri Formation|24605|6|Mentioned|p946|||||||||
39257|Willuri Formation|50613|2|Defined|p204-224, p226 App. 1|Westphalian|Namurian|Of the Currangandi Group.  Consists of 4 stratigraphically recognisable packages: Kaputar, Piney Range, Tulcumba and Gunnan - informal units containing individual successions of distinctive mappable volcanic units. Age range: ca. 320 to ca. 308Ma.||||||28-MAR-13
39257|Willuri Formation|62095|5|Briefly described|p266|||In the Carroll-Nandewar region of the Tamworth Belt.  Includes Birken Head Volcanic Member.||||||
39257|Willuri Formation|65902|4|Described|p193, 196, 197, 203-4, Figs.2, 7|Carboniferous|Carboniferous|Includes Yarrari Pyroclastic Member. Volcanigenic non-marine succession. Correlated with Currabubula Formation.||||||09-MAR-12
39257|Willuri Formation|68003|5|Briefly described|p32 Fig.3-h, pp131-133. |Late Carboniferous|Late Carboniferous|Tamworth Belt (West), New England Fold Belt. Coeval with Seaham and Currabubula Formations to the south.|||Includes Plagyan Rhyodacite.||Ignimbrites (rhyolitic, dacitic and andesitic), pyroxene andesite, rhyolite flows, dacite dome; rhyolitic agglomerate and conglomerate; interbedded ash-rich siltstone, volcanolithic sandstone and conglomerate; volcanic breccia.|
39257|Willuri Formation|68005|5|Briefly described|p49 Fig.3-M, p57, pp137-139, p170.|Stephanian|Namurian|Tamworth Belt. Informal (at time of publishing) name for all sedimentary rocks between the Kelvin-Plagyan and Hunter-Mooki thrusts. At least 11 ignimbrite members have been associated with Birken Head Rhyolite and 3 with Penryn Rhyolite.|||Includes Plagyan Rhyodacite; Bunaleer and Tranquille Dacites; Gunnan and Ourinperee Ignimbrites; Penryn, Yarralumba and Birken Head Rhyolites.||Ignimbrites (rhyolitic, dacitic and andesitic), rhyolite flows, dacite dome, rhyolitic agglomerate and conglomerate; interbedded ash-rich siltstone, medium- to coarse-grained volcanilithic sandstone and thick-bedded conglomerate.|
39257|Willuri Formation|69793|6|Mentioned|p1121 Fig.12, p1122|Moscovian|Serpukhovian|Nandewar Block, Tamworth Belt.||||||
39257|Willuri Formation|73197|6|Mentioned|p467|Carboniferous|Carboniferous|New England Orogen, southern. Forearc basin, volcanic rocks sourced from the Currabubula-Connors Arc.|||||Volcanic rocks, predominantly ignimbrite.|
30452|Wiltagoona Sandstone|22857|4|Described|p442 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Winduck Group (Cobar Supergroup). Quartz-rich arenite interbedded with mudrock. Max. thickness: 5km. Geological Province: Winduck Shelf (Darling Basin).||||||
30452|Wiltagoona Sandstone|23171|5|Briefly described|p15|Pragian|Lochkovian|||||||
30452|Wiltagoona Sandstone|23173|6|Mentioned|Map Legend|||||||||
30452|Wiltagoona Sandstone|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|Winduck Group||||||
30452|Wiltagoona Sandstone|43774|1|Redefined|p28-35|Pragian|Lochkovian|||||||
30452|Wiltagoona Sandstone|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Winduck Group (Cobar Supergroup). Thin to thick-bedded sequence of quartz sandstone interbedded with mudstone. Contains a marker sandstone zone. Age is Pragian. Geological Province: Winduck Shelf.||||||06-NOV-13
30452|Wiltagoona Sandstone|65469|5|Briefly described|p14|Lochkovian|Lochkovian|Lachlan Orogen.||Winduck Group||||
30452|Wiltagoona Sandstone|68823|6|Mentioned|p377, p378 Fig.4, p379|Lochkovian|Lochkovian|||||||
30452|Wiltagoona Sandstone|69002|6|Mentioned|p14|||||||||
30452|Wiltagoona Sandstone|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Early Devonian|Lachlan Orogen.||||||
30452|Wiltagoona Sandstone|73174|6|Mentioned|p1038|Pragian|Lochkovian|Winduck Shelf. Time-transgressive basal and upper boundaries. Records syn-rift development. Deposited above storm base in a shallow water environment. [Misspelt as Wittagoona Sandstone on p1037].||Winduck Group, Cobar Supergroup|||Interbedded sandstones and mudstones.|23-NOV-22
24110|Windamere Volcanics|22529|5|Briefly described|6|||||||||
24110|Windamere Volcanics|22590|6|Mentioned|Fig3 P754|Pridoli|Ludlow|||||||
24110|Windamere Volcanics|22857|4|Described|p476 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Tannabutta Group. Dacite and rhyolite lavas and autoclastics. Macrofauna. Max. thickness: 1500m. Geological Province: Capertee Rise. ||||||
24110|Windamere Volcanics|23043|5|Briefly described|Map Legend|Pridoli|Ludlow|of Tannabutta Group. Not shown on face of map or Time/Space diagram.||||||
24110|Windamere Volcanics|23170|2|Defined|p68|Late Silurian|Late Silurian|U/Pb SHRIMP dates 417 +/-3Ma (Fresh Dacite Age) Tannabutta Group.||||||
24110|Windamere Volcanics|40106|6|Mentioned|p593|||||||||
24110|Windamere Volcanics|43043|5|Briefly described|Fig.2,p93|||||||||
24110|Windamere Volcanics|43188|4|Described|p204,Table 2 p201|Ludlovian|Wenlockian|Capertee High. Representative section location given.||||||
24110|Windamere Volcanics|44093|5|Briefly described|p211 App. 1|Ludlovian|Wenlockian|Geological Province: Lachlan Fold Belt.||||||
27007|Winders Hill Granodiorite|32945|6|Mentioned|Fig.1|||Permian||||||
27007|Winders Hill Granodiorite|34444|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27007|Winders Hill Granodiorite|44244|6|Mentioned|p259 Fig. 51|||||||||
27007|Winders Hill Granodiorite|71628|5|Briefly described|p19: 172-173|||Rasmus et al. (1969). Named after a local geographical feature. Comprises a small (<1 km) intrusion, ~7 km ENE of Greta.||Winders Hill Suite.|||Granodiorite.|
23219|Windover Quartz Monzodiorite|22638|2|Defined|p29|Llandovery|Ashgillian|Wallundry Suite. 431 +/- 4 Ma Rb-Sr date. New name.||||||
23219|Windover Quartz Monzodiorite|44192|5|Briefly described|Map Legend||Llandoverian|||||||
23219|Windover Quartz Monzodiorite|70876|5|Briefly described|p77|Devonian|Devonian|Lachlan Orogen.|412.9 +/- 2.0 Ma (Iles, 2012)|||||
25683|Winduck Group|730|6|Mentioned|p23.|Early Devonian|Early Devonian|Cobar Sub-basin, Darling Basin. Fringing, shallow-water facies.||||||11-NOV-14
25683|Winduck Group|5252|4|Described|p61; p62 Fig.2; p63; throughout article.|Pragian|Lochkovian|Of Cobar Supergroup. Conformable but diachronous with underlying Amphitheatre Group; overlain paraconformably / locally unconformably by Mulga Downs Group. Quartzose sandstones with interbedded siltstones. Fauna includes brachiopods, trilobites, bivalves||||||
25683|Winduck Group|22518|4|Described|Table 1, p 4, 7, 10|||In the Darling Basin.||||||20-OCT-08
25683|Winduck Group|22768|6|Mentioned|p170||Pragian|||||||
25683|Winduck Group|22773|5|Briefly described|Fig24.5p350|Early Devonian|Silurian|||||||
25683|Winduck Group|22857|5|Briefly described|p170, p442 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Cobar Supergroup. Shallow marine deposits. Max. thickness: 6km. Geological Province: Winduck Shelf (Darling Basin). Equivalents mentioned on p350 Fig. 24.5. ||||||
25683|Winduck Group|22859|6|Mentioned|p211|||||||||
25683|Winduck Group|22887|4|Described|p23, Fig.4 p11|Early Devonian|Early Devonian|See also Fig.5 p13||||||
25683|Winduck Group|22893|6|Mentioned|fig4 p9|Devonian|Devonian|Describing an equivalent to this unit.||||||
25683|Winduck Group|23101|5|Briefly described|p567 (Fig 1)|||||||||
25683|Winduck Group|23171|6|Mentioned|p15||Pragian|||||||
25683|Winduck Group|23173|4|Described|Map Legend|Pragian|Pragian|||||||
25683|Winduck Group|23252|5|Briefly described|Map Legend||Early Devonian|of the Cobar Supergroup.||||||
25683|Winduck Group|23522|5|Briefly described|p249 Fig 5|Early Devonian|Early Devonian|||||||
25683|Winduck Group|23734|5|Briefly described|p12 Fig. 1|||Shelf sediments of sandstone, siltstone and limestone.||||||
25683|Winduck Group|24588|5|Briefly described|p31 Fig.15|Emsian|Emsian|Geological Province: Lachlan Fold Belt.||||||
25683|Winduck Group|37772|6|Mentioned|Fig.2|||||||||
25683|Winduck Group|37798|6|Mentioned|p128|||||||||
25683|Winduck Group|38292|6|Mentioned|p3|||||||||
25683|Winduck Group|40269|6|Mentioned|Fig.3|||||||||
25683|Winduck Group|40676|6|Mentioned|p28|||||||||
25683|Winduck Group|40913|6|Mentioned|Map legend|Zlichovian|Pragian|Zlichovian-Pragian||||||
25683|Winduck Group|41126|2|Defined|p95|Early Devonian|Early Devonian|||||||
25683|Winduck Group|41138|6|Mentioned|Map legend|Pragian|Pragian|||||||
25683|Winduck Group|41276|6|Mentioned|p73|||||||||
25683|Winduck Group|41394|6|Mentioned|p11|||||||||
25683|Winduck Group|41528|6|Mentioned|p19|||||||||
25683|Winduck Group|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
25683|Winduck Group|41821|3|Fully described|p42|||||||||
25683|Winduck Group|41872|6|Mentioned|p8|||||||||
25683|Winduck Group|42144|6|Mentioned|p603|||||||||
25683|Winduck Group|42172|5|Briefly described|Fig.5 P167|||||||||
25683|Winduck Group|42456|6|Mentioned|p8|||in Cobar Supergroup||||||
25683|Winduck Group|42566|5|Briefly described|Fig.5 P11|||||||||
25683|Winduck Group|42907|6|Mentioned|Fig.8, P8|||||||||
25683|Winduck Group|42966|5|Briefly described|p48, Fig.25|||||||||
25683|Winduck Group|42983|6|Mentioned|Fig.3,p345|||||||||
25683|Winduck Group|43032|2|Defined|p131|Middle Devonian|Early Devonian|Of Cobar Supergroup.||||||20-OCT-08
25683|Winduck Group|43089|5|Briefly described|Map Legend|||of Cobar Supergroup||||||
25683|Winduck Group|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||
25683|Winduck Group|43263|6|Mentioned|Map Legend||Pragian|||||||
25683|Winduck Group|43757|6|Mentioned|p510|||||||||
25683|Winduck Group|43774|4|Described|p27-28||Devonian|||||||
25683|Winduck Group|43859|5|Briefly described|15, Fig6p22-23|Middle Devonian|Early Devonian|Conformable on Amphitheatre Group, unconformable under Mulga Downs Group||||||
25683|Winduck Group|44093|5|Briefly described|p169 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
25683|Winduck Group|47026|6|Mentioned|Fig.5|||||||||
25683|Winduck Group|49038|6|Mentioned|p22|||||||||
25683|Winduck Group|49040|6|Mentioned|p6|||||||||
25683|Winduck Group|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Cobar Supergroup.  Comprises Gundaroo Sandstone, Sawmill Tank Siltstone, Buckambool and Wiltagoona Sandstones.  Age is Pragian. Geological Province: Winduck Shelf.||||||18-OCT-04
25683|Winduck Group|61213|5|Briefly described|p318, p319 Fig. 3|Early Devonian|Early Devonian|Synerogenic. Almost entirely non-marine; comprises four large alluvial fans. Possibly interfingers with Amphitheatre Group. Max. thickness: >2.5km in McCullochs Range. Geological Province: Darling Basin.||||||
25683|Winduck Group|61817|5|Briefly described|p80|Early Devonian|Early Devonian|Interbedded sandstone and mudstone.  Geological Province: Cobar Basin.||||||
25683|Winduck Group|61964|5|Briefly described|p66, p67|Lochkovian|Lochkovian|Of the Cobar Supergroup.  On THE MEADOWS map sheet. Includes fauna assemblages similar to those of the former "Square Head Beds" of the current Crossleys Tank Formation. Geological Province: Cobar Basin. See also p104.||||||
25683|Winduck Group|64967|5|Briefly described|p113, p114 Fig. 2, p121|Early Devonian|Late Silurian|Age is Pragian. Geological province: Darling Basin/Blantyre Sub-basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113)||||||
25683|Winduck Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cobar. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
25683|Winduck Group|65469|5|Briefly described|p14-p17, p22, p43, |Pragian|Pridoli|Lachlan Orogen. Misspelt as the Winduck group on p22. See also p52, p55 fig 3-19, p62, p67, p136, p339.||Cobar Supergroup|Includes the Wiltagoona Sandstone, Buckambool Sandstone, Sawmill Tank Siltstone and the Gundaroo Sandstone.|Unconformably overlain by the Mulga Downs Group. Equivalent to the Cocoparra Group.||
25683|Winduck Group|67870|5|Briefly described|p58, p62, p64-66, p68-69, p72-77|Early Devonian|Late Silurian|Eastern and central Darling Basin. Fluvial sedimentary rocks. Potential hydrocarbon source rocks in upper parts. Detailed modelling shows 100% of kerogen transformed and early expulsion of oil and minor gas.||||Is overlain unconformably by Snake Cave Sandstone (Mulga Downs Group).|Lower part: sandstone, shale, minor limestone. Upper part: siltstone, organic-rich (3% TOC) shale, marl, micritic limestone.|
25683|Winduck Group|68298|5|Briefly described|p223|||Shallowing-up marine sequence above which the fluviatile Mulga Downs Group shows bedding concordance, but with local angular unconformities, and there is no palaeontological control on the duration of a hiatus, if present.||Cobar Supergroup||Is overlain by Mulga Downs Group, with bedding concordance and local angular unconformities.||
25683|Winduck Group|68823|5|Briefly described|pp376-378 Figs.3,4, p383, pp397-399|Pragian|Lochkovian|Winduck Shelf. Lachlan and Thomson Orogens. Shallow water strata. Coeval with the upper part of the Kopyje Group. Possible low magnetic character.||Of the Cobar Supergroup.||Disconformably to paraconformably overlain by the Mulga Downs Group.||23-JUL-15
25683|Winduck Group|69002|6|Mentioned|p14, p16, Map 1b, Legend|Middle Devonian|Early Devonian|||||||
25683|Winduck Group|69042|5|Briefly described|map legends|Middle Devonian|Early Devonian|Dw. Thomson or Lachlan Orogen? Non-magnetic sandstone with very weak linear magnetic trends related to local resistent ridges||||||
25683|Winduck Group|69043|6|Mentioned|p11|Middle Devonian|Early Devonian|||||||
25683|Winduck Group|69511|6|Mentioned|p22|||||||Is faulted against the Thule Granite.||
25683|Winduck Group|69541|6|Mentioned|p644 Fig.1(a)|Early Devonian|Late Silurian|Lachlan Orogen.||Unit in Cobar Supergroup.||||
25683|Winduck Group|69635|6|Mentioned|p69 Fig 3.1|||||||||
25683|Winduck Group|70037|5|Briefly described|p309 Fig.2, p310-311, p327|Middle Devonian|Early Devonian|Central and eastern Darling Basin. Deltaic/shoreline deposits (Glen, 1982) over 200m thick.|||Buckambool Sandstone, Sawmill Tank Siltstone, Gundaroo Sandstone.|Overlies or interfingers with Amphitheatre Group.||
25683|Winduck Group|70602|6|Mentioned|p67 Fig 3|Devonian|Devonian|||Cobar Supergroup||||
25683|Winduck Group|70718|4|Described|p20, p43, p54, p102-103|Pragian|Lochkovian|Darling Basin. A maximum thickness of 6000m is given. A deep to shallow marine depositional environment is interpreted for this group. Multiple lithological descriptions from various sources are provided. Bedforms of this group includes parallel-laminated and commonly rippled to cross-laminated, cross-bedded and occasionally hummocky with cross-stratification. Intersected by Booligal-2 and possibly intersected in Mossgiel-1.. Misspelt as Winduck Formation p43,  Windick Group on p54. Age interpreted as the depositional age of  2 tuffs within the Group.|401.7+/- 8.2 and 417.8+/- 8.3 Ma (K-Ar)|Cobar Supergroup||Overlies the Amphitheatre Group. Overlain by the Mulga Downs Group.|Well-sorted, fine- to medium-grained quartzose sandstone with lesser interbedding siltstone and mudstone shelf sediments; tuffs.|02-JUN-19
25683|Winduck Group|70751|4|Described|p4, p6-p7, p11-p15, p28|Pragian|Late Silurian|Cobar Superbasin, Winduck Shelf. Locally rich in marine fossils indicative of an early Devonian age, however; a Pridolian age cannot be discounted based on fossils near Cobar.||Cobar Supergroup|Includes the Buckambool Sandstone, Sawmill Tank Siltstone and Gundaroo Sandstone.|Overlain by the Mulga Downs Group.||24-SEP-19
25683|Winduck Group|70821|5|Briefly described|p11|Early Devonian|Late Silurian|Shelf facies. Typically non-magnetic.||||||
25683|Winduck Group|70950|5|Briefly described|p1028,1030,1033, 1037|Early Devonian|Early Devonian|Geological province: Winduck Shelf, Central Lachlan Orogen. Detailed mineralisation analysis provided.|||Includes Gundaroo Sandstone.||Dolomitic limestone, calcareous carbonaceous shale, arkosic sandstone, granite|
25683|Winduck Group|71039|5|Briefly described|p6, p14|Devonian|Silurian|Glen (1987) reported that this unit is essentially unmetamorphosed.|||Includes the Booth Limestone Member.|||
25683|Winduck Group|71040|5|Briefly described|p6-7, p15, p25|Pragian|Lochkovian|Cobar Basin. Shallow-marine to fluvial deposits. Presented as Winduck on p7. Has broad to open upright folds, with associated vertical faults.||||Is overlain by Mulga Downs Group conformably (locally disconformably).||
25683|Winduck Group|71263|6|Mentioned|p18 Fig 2|Middle Devonian|Early Devonian|||||||
25683|Winduck Group|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Cobar Supergroup.|Belah Formation"".|||
25683|Winduck Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.||Is overlain by Mulga Downs Group.|Cross-bedded (including hummocky cross-stratified), parallel laminated and commonly ripple cross-laminated, well-sorted, fine- to medium-grained quartzose sandstone with lesser interbedded siltstone and mudstone; deposited in a shelf environment.|
25683|Winduck Group|71860|6|Mentioned|p6|Middle Devonian|Early Devonian|||||||
25683|Winduck Group|72908|6|Mentioned|p4-5, p14, p16, p25, p30|Emsian|Lochkovian|Winduck Shelf. Lochkovian to early Emsian in age.|||Buckambool Sandstone, Gundaroo Sandstone|||
25683|Winduck Group|72958|6|Mentioned|p8-9, p19, p25|||Flanks the Cobar Basin. Nymagee area.|||Gundaroo Sandstone, Booth Limestone Member, Sawmill Tank Siltstone, Buckambool Sandstone|Partly underlain by Amphitheatre Group and Mount Hope Group. Partly overlain by Meadows Tank Formation and Crowl Creek Formation (both of Mulga Downs Group). Partly equivalent to Walters Range Group.|Limestone-bearing shelf sequences.|
25683|Winduck Group|73174|5|Briefly described|p1035-1036, p1038-1039|Emsian|Lochkovian|Cobar Basin, west [of Rookery Fault], Winduck Shelf. Formed in shallow-water conditions. Interfingers with the Amphitheatre Group representing increasing water depth to the east. Geochron are magmatic ages from Wilde (1998). [Misspelt as Windruck Group on p1037].|417 +/- 11 Ma, 411 +/- 6 Ma SHRIMP|Cobar Supergroup|Gundaroo Sandstone, Sawmill Tank Siltstone, Buckambool Sandstone, Wiltagoona Sandstone|Underlain by Lower Amphitheatre Group. Equivalent to Amphitheatre Group.|Predominantly sandstone.|
25683|Winduck Group|73175|6|Mentioned|p1050, p1066|||Thomson Orogen, southern. Low magnetic intensity.|||||Clastic sedimentary rocks.|
25683|Winduck Group|73177|6|Mentioned|p1099|Middle Devonian|Early Devonian|||||||
25683|Winduck Group|73578|6|Mentioned|p2|||Cobar Basin.||||||
35790|Winduella Tonalite|50232|5|Briefly described|Map legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
35790|Winduella Tonalite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Burrawinda Suite. Grey porphyritic biotite tonalite, relict calcic cores in plagioclase. Diorite enclaves, and sedimentary xenoliths of Adaminaby Group rocks are found close to the foliated (faulted) eastern margin. High Th radioelement response.||||||12-JUN-08
35790|Winduella Tonalite|66300|5|Briefly described|p92.|||S-type.|427.9 +/- 3.0 Ma.|Unit in Burrawinda Suite.||||
35790|Winduella Tonalite|68592|2|Defined|p291, p1329, p1354-8, p1375-8|Ludlow|Wenlock|New name, after Parish of Winduella. Previously included in undifferentiated Wyangala Batholith (Brunker and Offenberg, 1970) and later in the Wheeo Granite (Chappell et al., 1991). Type area described. Encloses recrystallised Abercrombie Formation rocks. Has a well-developed N to NW trending foliation dipping steeply to the W. Has undergone moderate to high greenschist facies regional metamorphism. Geochemistry and geophysical properties described. SHRIMP U-Pb zircon age. Is overlain by diamond- and sapphire-bearing alluvial deposits, sourced from Cenozoic basalt.|427.9 +/- 3.0 Ma (Bodorkos and Simpson, 2008).|Unit in Burrawinda Suite.|||S-type. Grey, medium- to coarse-grained, equigranular to porphyritic biotite tonalite; contains sporadic microgranite and aplite dykes; metasedimentary xenoliths and dioritic enclaves common. Well-developed foliation decreases to the W.|
35790|Winduella Tonalite|70192|4|Described|Map Legend|Ludlow|Wenlock|Swd. On Gunning 1:100 000 mapsheet portion of Time-Space Plot.||Burrawinda Suite|||Grey, medium to coarse grained, foliated equigranular to porphyritic, biotite tonalite with metasedimentary and vein quartz xenoliths and grey dioritic igneous enclaves; sporadic microgranite and aplite dykes. Th response can be high.|
35790|Winduella Tonalite|70541|4|Described|Map Legend|Devonian|Silurian|||Burrawinda Suite|||Grey, medium to coarse grained, foliated equigranular to porphyritic, biotite tonalite with metasedimentary and vein quartz xenoliths and grey dioritic igneous enclaves; sporadic microgranite and aplite dykes. Th response can be high.|
81944|Wingabutta Formation|72700|5|Briefly described|Mapsheet 1 and 2|Cenozoic|Cenozoic|||Warrumbungle  Volcanic Complex|||Dark to medium green, white weathering, porphyritic to aphanitic basalt (hawaiite) lava deposits and minor autobreccia.|02-NOV-20
33407|Wingara Formation|23217|4|Described|p1, p18-20||Late Devonian|Of the Hervey Group. Previously Cookamidgera Formation (in part). Max. thickness: >200m.||||||07-MAR-06
33407|Wingara Formation|23392|6|Mentioned|p3||Late Devonian|of Young 1999. No fossil assemblage but Famennian fossils in unit below. Age by strat. position. Of the Hervey Group. Geological Province: Lachlan Fold Belt. Max Thickness: 60m||||||
33407|Wingara Formation|24417|3|Fully described|p141|Late Devonian|Late Devonian|Of Hervey Group.  Previously included in Eurow Formation, Cookamidgera Formation and Cookamidgera Sub-Group  Underlain by Eurow Formation.||||||
33407|Wingara Formation|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Hervey Group. Overlies: Eurow Formation.||||||13-JUL-04
69705|Winmatti beds|61155|5|Briefly described|p16|Holocene|Pleistocene|Overlies the Uluru Clay. Age: <1.5Ma. Geological Province: East Amadeus Basin.||||||
69705|Winmatti beds|69458|5|Briefly described|p42:24|Pleistocene|Pleistocene|Lake Amadeus. 2-3m thick. Deposition began at about 1 Ma and marks the transition from a surface-water dominated system to a groundwater-controlled playa, as a result of increasing aridity.||||Overlies Uluru Clay.|Interlayered red quartz aeolian sand and gypsum.|12-JUL-16
76973|Winterbourne Monzogranite|71628|4|Described|p2: 24; p3: 1, 96-99|||Landenberger et al. (2010). Previously the Winterbourne Adamellite (Binns et al., 1967). Named after a local homestead. Crops out ~37 km SSE of Armidale and 23 km NE of Walcha. A small (up to 4 x 1.5 km) intrusion. Geochemistry described.|292.5 +/- 2.9 Ma (SHRIMP: Rosenbaum et al., 2012).|Winterbourne Suite.||Intrudes Coffs Harbour Association.|Fine- to medium-grained, massive to weakly foliated, plagioclase-rich biotite monzogranite-granodiorite; locally garnet bearing. Rare sedimentary enclaves. S-type.|
27009|Wirchilleba Granite|29987|5|Briefly described|p15|||||||||
27009|Wirchilleba Granite|34449|6|Mentioned|Table 2-1|||||||||
27009|Wirchilleba Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
27009|Wirchilleba Granite|43389|14|Not recorded|Map Legend||Silurian|||||||
26225|Wirrilah Conglomerate Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||
26225|Wirrilah Conglomerate Member|35287|6|Mentioned|p7|||||||||
26225|Wirrilah Conglomerate Member|39618|6|Mentioned|Table 9|||||||||
26225|Wirrilah Conglomerate Member|42566|2|Defined|p62|Early Devonian|Early Devonian|Age: mid Early Devonian. Previously included in 'Barrow Range Beds' of Brunker (1968). Max thickness ~150m.|||||Grades from a sedimentary breccia - unsorted, clast-supported, subangular to subrounded, pebble to cobble conglomertate -  upwards to a quartzo-feldspathic sandstone with large scale crossbedding.|24-SEP-19
26225|Wirrilah Conglomerate Member|42568|5|Briefly described|Map legend|Early Devonian|Late Silurian|||||||
26225|Wirrilah Conglomerate Member|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
26225|Wirrilah Conglomerate Member|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Equivalent to Cauldwell Vale Conglomerate Member.||
25639|Wirrinya Granite|24417|3|Fully described|p111|Middle Devonian|Early Devonian|||||||
25639|Wirrinya Granite|29907|2|Defined|Appendix 1|Early Devonian|Early Devonian|Prob.Early Devonian||||||
25639|Wirrinya Granite|29910|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
25639|Wirrinya Granite|36411|6|Mentioned|p270|||Refers Bowman 1977.||||||
25639|Wirrinya Granite|40328|4|Described|p212|||||||||
25639|Wirrinya Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
25639|Wirrinya Granite|60009|5|Briefly described|Map Legend|Eifelian|Eifelian|||||||13-JUL-04
25639|Wirrinya Granite|60548|5|Briefly described|map legend|Devonian|Devonian|Granite.||||||
25639|Wirrinya Granite|71040|6|Mentioned|p16|Devonian|Devonian|Currowong Syncline.||||||
25639|Wirrinya Granite|72084|5|Briefly described|p56|Middle Devonian|Middle Devonian|Not yet isotopically dated; age based on correlation with intrusions of similar chemistries (Lyons et al., 2000). Mentioned as a possible source for the ignimbrite unit in a sequence of Hervey Group equivalents in the Curraburrama State Forest, c.23km to the SW.|||||A-type.|
27937|Wisemans Arm Formation|721|5|Briefly described|Map legend|Late Carboniferous|Late Devonian|Andesitic lithic wacke, siltstone and conglomerate, with olistoliths of andesite, limestone and chert.  Geological Province: Djungati Terrane.||||||21-DEC-04
27937|Wisemans Arm Formation|13996|6|Mentioned|p132|Silurian|Silurian|Northern NSW. Contains Telychian-Sheinwoodian tabulate corals.||||||
27937|Wisemans Arm Formation|22857|5|Briefly described|p434 App. 1 Tb. A1.5||Late Ordovician|Max. thickness: >1.2km. Geological Province: Woolomin Basin. See also p484 App.1 Tb.A1.6.||||||
27937|Wisemans Arm Formation|23185|6|Mentioned|Fig1p156|||||||||
27937|Wisemans Arm Formation|24366|6|Mentioned|p7|||||||||
27937|Wisemans Arm Formation|36071|4|Described|p8|||||||||
27937|Wisemans Arm Formation|38194|4|Described|p383|||||||||
27937|Wisemans Arm Formation|38229|5|Briefly described|p445|||||||||
27937|Wisemans Arm Formation|38683|5|Briefly described|p11|Early Devonian|Early Devonian|Geological Province: New England Fold Belt||||||
27937|Wisemans Arm Formation|38686|4|Described|p54|Devonian|Devonian|Geological Province: New England Fold Belt||||||
27937|Wisemans Arm Formation|39441|6|Mentioned|p30|||||||||
27937|Wisemans Arm Formation|40762|6|Mentioned|p278|||||||||
27937|Wisemans Arm Formation|40883|6|Mentioned|p3|||||||||
27937|Wisemans Arm Formation|40960|6|Mentioned|p215|||||||||
27937|Wisemans Arm Formation|41237|4|Described|p75|||||||||
27937|Wisemans Arm Formation|41328|6|Mentioned|p12|||||||||
27937|Wisemans Arm Formation|41329|5|Briefly described|p5|||||||||
27937|Wisemans Arm Formation|41347|4|Described|Table 4|||Mention P364||||||
27937|Wisemans Arm Formation|41348|5|Briefly described|Map legend|Devonian|Devonian|Sandstone, granule to boulder conglomerate, and siltstone, with olistoliths of chert, limestone, basalt, andesite and siltstone.||||||16-DEC-04
27937|Wisemans Arm Formation|41612|6|Mentioned|p141|||||||||
27937|Wisemans Arm Formation|41796|6|Mentioned|p307|||||||||
27937|Wisemans Arm Formation|42554|5|Briefly described|p39|||||||||
27937|Wisemans Arm Formation|42901|5|Briefly described|Fig.12 P412|||see also Fig.11 P411||||||
27937|Wisemans Arm Formation|43091|5|Briefly described|Map legend|||||||||
27937|Wisemans Arm Formation|44093|5|Briefly described|p122|Early Carboniferous|Early Carboniferous|Sequence of relatively deep-water redeposited epiclastic sediments, ashfall tuffs and slide blocks (olistoliths).||||||
27937|Wisemans Arm Formation|44450|5|Briefly described|p6|Early Devonian|Early Devonian|Geological Province: New England Fold Belt.||||||
27937|Wisemans Arm Formation|50090|5|Briefly described|p421|Late Ordovician|Late Ordovician|Contains limestone olistoliths which contain conodont fauna.  Geological Province: New England Fold Belt.||||||
27937|Wisemans Arm Formation|61764|4|Described|p46, p46|||Shares many similarities with Dinoga Formation. Authors consider there is little justification for considering rocks at Mandalay (property east of Peel Fault) as distinct from Wisemans Arm Formation.||||||29-NOV-13
27937|Wisemans Arm Formation|63119|5|Briefly described|p214|||Of the Tablelands Complex. Contains osteoliths of Eastonian age. Age: early Devonian? Geological Province: Tamworth Belt.||||||13-MAR-07
27937|Wisemans Arm Formation|65398|1|Redefined|p1-22|Carboniferous|Carboniferous|Defined by Leitch and Cawood (1980); revised by Vickery and Brown (in prep.). Fault bounded assemblage of metasediments. Possibly a suspect terrane; sediment sources unidentified. Massive thick, coarse-grained labile pebbly sandstone and laminated siltstone, with subordinate siliceous argillite, jasper and chert; conglomerate lenses occur. Age is poorly constrained and contentious. Faulted against Woolomin Group and Cara Formation.||||||
27937|Wisemans Arm Formation|66720|5|Briefly described|Map legend|Late Carboniferous|||||Includes two un-named but separately mapped units: granule- to pebble-, clast- and matrix-supported conglomerates; white olistostromal chert lenses.||Massive andesitic lithic wacke, argillite, siltstone and conglomerate; rare chert and jasper olistoliths.|
27937|Wisemans Arm Formation|67322|5|Briefly described|p27, p39, p40|Wenlock|Eastonian|Leitch and Cawood (1980) sensu Furey-Greig (1999, 2003). The Uralba Beds (predominantly limestone clasts) used to be incorporated into the Wisemans Arms Formation (sensu Furey-Greig 2003), but are now part of the Glen Bell Formation (Brown 2009). Occurs in the Halls Creek district (Manilla region) north of Tamworth.||||||22-FEB-18
27937|Wisemans Arm Formation|68005|5|Briefly described|pp17-18, p22, pp29-30, p154, p169, p170.|Devonian|Devonian|Djungati terrane, Central Block, New England Fold Belt. Deep marine deposition.|||||Mainly siltstone, finely laminated or massive; subordinate sandstone beds, the thicker ones being pebbly; granule to boulder conglomerates, clast supported, dominantly volcanic-derived; olistoliths of chert and intermediate volcanic blocks common.|
27937|Wisemans Arm Formation|68006|5|Briefly described|p20 Fig.3-A, p25, p99. |||Central Block, New England Fold Belt. Hosts small, discontinuous limestone lenses of dubious economic importance.||||Is overlain by, and faulted against, Cara Formation.||
27937|Wisemans Arm Formation|71628|5|Briefly described|p7: 5, 31|||Appears as Wiseman Arm Formation on p7-5.||||Is intruded by Attunga Creek and Moonbi Monzogranites.||
39410|Witchetella Formation|24126|6|Mentioned|p221|||||||||
23235|Wog Wog Complex|22815|5|Briefly described|p106|||Age suspected to be Jurassic or Cretaceous.||||||
23235|Wog Wog Complex|43233|5|Briefly described|Map Legend|Late Cretaceous|Early Cretaceous|||||||
81719|Wolgolla Granite|71965|5|Briefly described|p898,910,913|Late Silurian|Late Silurian|Geological province: Thomson Orogen. Of Warburton Basin; Ella Belt. Dated from drillholes TEA Roseneath 1 (419.4+\-7 Ma; Siegel, 2015) and DIO Wolgolla 1 (418.8+\-2.8 Ma; Siegel, 2015). See also Wollgolla Granite p911 Fig 15.||||Intrudes into Lycosa Formation.||22-NOV-19
81719|Wolgolla Granite|72951|6|Mentioned|p1024, 1027, 1030|Lochkovian|Pridoli|Thomson Orogen, southwest. S-type granite. Siegel (2015) reports U-Pb, O and Hf isotopic data from Wolgolla 1 well.|419.0 +/- 2.7 Ma|||||
81113|Wollomombi Granodiorite|71703|6|Mentioned|p204|||Hf isotopes discussed. Said to be of Kemp et al. 2009.||Of Hillgrove Supersuite.||||18-JUN-19
26228|Wollong Siltstone Member|33867|6|Mentioned|p6|||||||||
26228|Wollong Siltstone Member|34345|2|Defined|p331|Permian|Permian|||||||
26228|Wollong Siltstone Member|39288|6|Mentioned|p63|||||||||
26228|Wollong Siltstone Member|41275|6|Mentioned|p27|||||||||
26228|Wollong Siltstone Member|45090|5|Briefly described|p157|||||||||
36825|Wollundi Mudstone Member|23859|2|Defined|p241 Appendix 1|Late Permian|Permian|See also page 931. Type locality 4397300E 6750400N. Of Emmaville Volcanics. Overlying unit Dundee Rhyodacite. Underlying unit Dummy Creek Conglomerate. New England Fold Belt. Max. thickness: >150 m.||||||
69873|Wologorong Supersuite|68592|2|Defined|p74 Tb.5,p650-1,p1256-8,p1356-7,p1542-99|Early Devonian|Late Silurian|New name, after Wologorong Granite and parish of Wologorong. Comprises those granites that form the Wologorong Batholith, including the Wologorong Granite which was unintentionally included in the Bemboka Supersuite by Chappell et al. (1991) due to a typographical error. The type pluton is the Wologorong Granite. Geochemistry detailed and discussed: heterogeneous character suggests this unit is the transition between S-type and I-type granites. Some plutons intrude Late Silurian rocks, rather than Ordovician as previously suggested. Another age is 405 +/- 11 Ma (Shaw et al., 1982: whole-rock Rb-Sr). Low mineral potential; locally quarried for construction materials. Peelwood and Goulburn structural zones: deformation described.|425.5 +/- 2.4 Ma (SHRIMP U-Pb).||Includes Parkesbourne and Tumboramboro Suites and Davies Creek Granite.|Intrudes Cuddyong Formation. Is intruded by Bishopthorpe Suite.|K-feldspar-rich, muscovite-bearing granite; medium- to coarse-grained biotite granite; fine-grained granodiorite. Generally massive. Transitional S- to I-type eastwards.|20-MAY-16
69873|Wologorong Supersuite|70297|4|Described|map legend, on side 2 of map sheet|Pragian|Pragian|Age: Pragian? (Early Devonian).|||Davies Creek Granite, Greenslopes Porphyry, Tumboramboro Granite|?Intrudes Crudine Group.|Reduced, unfractionated, S-type biotite granite, leucogranite, monzogranite and porphyritic granite.|20-MAY-16
69873|Wologorong Supersuite|71069|6|Mentioned|p24|Early Devonian|Early Devonian||||Includes the Wologorong Suite|||
29162|Wolumla Conglomerate Member|22815|4|Described|p100, fig32|||||||||
29162|Wolumla Conglomerate Member|32127|6|Mentioned|p262|||Refers Hall (1960)||||||
29162|Wolumla Conglomerate Member|33268|6|Mentioned|Table 1|||||||||
29162|Wolumla Conglomerate Member|33269|4|Described|p47|||Lithology||||||
29162|Wolumla Conglomerate Member|33732|5|Briefly described|p113|||||||||
29162|Wolumla Conglomerate Member|34109|4|Described|p157|||||||||
29162|Wolumla Conglomerate Member|39665|6|Mentioned|Table 1|||||||||
29162|Wolumla Conglomerate Member|40276|6|Mentioned|p27|||||||||
29162|Wolumla Conglomerate Member|42050|5|Briefly described|p228|||||||||
29162|Wolumla Conglomerate Member|42158|6|Mentioned|p2|||||||||
29162|Wolumla Conglomerate Member|42848|6|Mentioned|p530|||||||||09-MAY-05
29162|Wolumla Conglomerate Member|46579|2|Defined|p.109||Late Devonian|Basal unit of Merrimbula Formation. Massive purplish conglomerate with arkosic matrix. (J55-4/Pambula; J55-8/Eden).U Dev. Overlies Bega Granite. Underlies red shales etc.||||||05-FEB-08
29162|Wolumla Conglomerate Member|63605|5|Briefly described|p999|||Basal part of Twofold Bay Formation. Max. thickness: ~70m. In the Eden area; 180m at Wolumla Peak.||||||07-FEB-11
29162|Wolumla Conglomerate Member|70661|6|Mentioned|p110, p112|||||||||
29162|Wolumla Conglomerate Member|73181|6|Mentioned|p64-65|||Stretched pebbles define a high-strain zone.||Twofold Bay Formation, Merrimbula Group||||
25698|Wombiana Formation|22679|4|Described|p 25||Silurian|Mumbil Group||||||
25698|Wombiana Formation|22857|5|Briefly described|p468 App.1 Tb.A1.6|Wenlockian|Wenlockian|Of the Mumbil Group. Siltstone, limestone, marble. Geological Province: Molong Rise.||||||09-MAR-06
25698|Wombiana Formation|23214|4|Described|p139|Late Silurian|Late Silurian|Of Mumbil Group. Contains limestone and siltstone.||||||
25698|Wombiana Formation|24268|6|Mentioned|p1536 Fig.2|||Geological Province: Lachlan Fold Belt||||||
25698|Wombiana Formation|43653|5|Briefly described|Map Legend||Silurian|||||||
25698|Wombiana Formation|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group (northwest). Siltstone, limestone.||||||17-JUL-08
25698|Wombiana Formation|43782|5|Briefly described|Map Legend|Ludlow|Wenlock|Of Mumbil Group.||||||17-JUL-08
25698|Wombiana Formation|49794|4|Described|p14, p8|||Used 1977 [?]. Reserved Jan 1978, SJ Richardson. Defn card supplied. NLR Jan 1984.||||||
25698|Wombiana Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
24582|Wombin Volcanics|22434|6|Mentioned|12|||Geol province Lachlan Fold Belt||||||
24582|Wombin Volcanics|22659|5|Briefly described|p 281|||||||||
24582|Wombin Volcanics|22831|4|Described|p 28|Early Silurian|Late Ordovician|||||||
24582|Wombin Volcanics|22857|5|Briefly described|p416 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|Dominantly red andesitic lavas. Max. thickness: 700m. ||||||
24582|Wombin Volcanics|23538|6|Mentioned|p 457|||||||||
24582|Wombin Volcanics|23736|6|Mentioned|p13 Fig. 2|||||||||
24582|Wombin Volcanics|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
24582|Wombin Volcanics|24230|5|Briefly described|p171|||||||||
24582|Wombin Volcanics|24267|5|Briefly described|p1506|||Underlying Unit: Goonumbla Volcanics. Geological Province: Parkes-Narromine Belt||||||
24582|Wombin Volcanics|24417|3|Fully described|p26|Early Silurian|Late Ordovician|Previously referred to as "Wombin Group".  Of Northparkes Volcanic Group.||||||
24582|Wombin Volcanics|40365|2|Defined|p331|Late Silurian|Late Silurian|||||||
24582|Wombin Volcanics|40791|5|Briefly described|p182|||||||||
24582|Wombin Volcanics|40891|3|Fully described|p9|||Mention Fig.2||||||
24582|Wombin Volcanics|42171|6|Mentioned|p144|||||||||
24582|Wombin Volcanics|42262|6|Mentioned|p1817|||Part of Goonumbla Volcanics. See also Fig.2 P1810.||||||
24582|Wombin Volcanics|42489|5|Briefly described|Map legend|Llandovery|Bolindian|||||||
24582|Wombin Volcanics|43263|6|Mentioned|Map Legend|Early Silurian|Late Ordovician|||||||
24582|Wombin Volcanics|43441|5|Briefly described|17, 21|Late Silurian|Late Ordovician|included as a member of Goonumbla Volcanics||||||08-JAN-10
24582|Wombin Volcanics|44093|5|Briefly described|p178 App. 1|Ordovician|Ordovician|Of the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
24582|Wombin Volcanics|44160|5|Briefly described|Map Legend||Bolindian|||||||08-JAN-10
24582|Wombin Volcanics|46522|1|Redefined|p26|Early Silurian||||||||
24582|Wombin Volcanics|46523|6|Mentioned|p89|||||||||
24582|Wombin Volcanics|46524|4|Described|p102|||See also Appendix 1 P129||||||
24582|Wombin Volcanics|46525|6|Mentioned|Fig.1 P143|||||||||
24582|Wombin Volcanics|46528|5|Briefly described|Map legend|||||||||
24582|Wombin Volcanics|50299|5|Briefly described|Map Legend|Ordovician|Ordovician|Predominantly red andesitic lavas.||||||09-JUN-04
24582|Wombin Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
24582|Wombin Volcanics|60009|5|Briefly described|Map Legend|Bolindian|Eastonian|Of the Northparkes Volcanic Group.||||||13-JUL-04
24582|Wombin Volcanics|61724|3|Fully described|p864 Fig.1, p874-876|Early Silurian|Late Ordovician|Predominantly volcanic sandstone and polymictic volcanic breccia, some significant grey trachyandesite in addition to red/brown trachyte and ignimbrite; rare mudst. Overlies Goonumbla Volcs, Billabong Creek Limestone and Gunningbland Fm. Max. age: 450Ma||||||
24582|Wombin Volcanics|61821|5|Briefly described|p101|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
24582|Wombin Volcanics|62478|4|Described|p89|Early Silurian|Ordovician|Overlies Goonumbla Volcanics. Of the Goonumbla Volcanic Complex. Volcaniclastic rocks, trachyandesitic to trachytic lavas.||||||
24582|Wombin Volcanics|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a|||Underlain by Goonumlba Volcanics. Geological Province: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
24582|Wombin Volcanics|63279|6|Mentioned|p168 Fig. 1|Ordovician|Ordovician|Geological Province: Junee-Narromine Volcanic Belt.||||||
24582|Wombin Volcanics|63283|5|Briefly described|p184, p185 Tb. 1, p186-187, p196 Fig. 4|Early Silurian|Late Ordovician|Of Northparkes Group. Underlain by Goonumbla Volcanics. Age: 445Ma. Geological Province: Junee-Narromine Volcanic Belt. Consists of trachyandesitic and trachytic lavas and sills. Youngest age: 437+/-3.5Ma (SHRIMP).  See p187.||||||07-FEB-11
24582|Wombin Volcanics|63284|6|Mentioned|p247|Late Ordovician|Late Ordovician|In the Narromine Igneous Complex.||||||
24582|Wombin Volcanics|63286|6|Mentioned|p308 Fig. 9||Early Silurian|Geological Province: Junee - Narromine Volcanic Belt. Consists of shoshonitic lavas.||||||07-FEB-11
24582|Wombin Volcanics|63288|6|Mentioned|p358|||Geological Province: Junee - Narromine Volcanic Belt. Consists of felsic lavas.||||||
24582|Wombin Volcanics|63290|5|Briefly described|p398, p402 Fig. 6(a), p397 Fig. 3(b)|Bolindian|Eastonian|Overlain by Cotton Formation, underlain by Gunningbland Formation. Geological Province: Junee - Narromine Volcanic Belt. Consists of a sequence of volcaniclastic sandstone and lavas.||||||
24582|Wombin Volcanics|63291|4|Described|p421, p423|Late Ordovician|Late Ordovician|Of Northparkes Gp. Conformably underlain by Goonumbla Vol.  Age: ~444-436Ma. Thick: 700-1000m. Comprises dark-red polymetric volcanic breccia + volcaniclastic units, with less abundant porphyritic trachyandesite, flow-banded trachyte lavas + ignimbrites.||||||14-NOV-13
24582|Wombin Volcanics|63293|5|Briefly described|p473, p474, p468 Fig. 2|Bolindian|Eastonian|Overlain by Cotton Formation, underlain by Bunningbland Formation. Geological Province: Junee - Narromine Volcanic Belt. Host for Northparkes intrusion.||||||07-FEB-11
24582|Wombin Volcanics|64015|5|Briefly described|p58 Fig. 1|||||||||
24582|Wombin Volcanics|64963|6|Mentioned|p182 Fig. 2|||||||||
24582|Wombin Volcanics|67106|6|Mentioned|p673, 679|||Junee-Narromine Volcanic Belt. Appears as Wombin Formation on p679.||||||
24582|Wombin Volcanics|67107|5|Briefly described|p688, 693, 696, 701|Late Ordovician|Late Ordovician|Goonumbla district, 20km NW of Parkes. Junee-Narromine Volcanic Belt. Eastonian to Llandovery. Intruded by a monzonite dated 450.8 +/- 4.2 Ma.||||Is intruded by the Goonumbla Volcanic Complex. Faulted against Nelungaloo Volcanics.||
24582|Wombin Volcanics|67322|5|Briefly described|Fig.5; p22|Katian||Simpson et al. (2005). Macquarie Arc. Age from surrounding units. Occurs in the Junee-Narromine region.||Of the Northparkes Group.||Overlies Gunningbland Formation and Goonumbla Volcanics. Overlain by the Jingerangle Formation.||22-FEB-18
24582|Wombin Volcanics|70278|5|Briefly described|p1609, 1611-1613, 1616-1617, 1619-1620|Late Ordovician|Late Ordovician|See also p1622, 1624, 1627, 1633. Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW. 700-1,000m thick. Drill hole logs. Photographs, numerous photomicrographs.|438.9 +/- 4.7 Ma (SHRIMP; Butera et al., 2001).|Goonumbla Volcanic Complex.|||Typically dark red, hematite-dusted glassy lavas, ignimbrites, polymictic volcanic breccias, and other volcanic sedimentary rocks with less abundant porphyritic trachyandesitic and flow-banded trachytic lavas.|
24582|Wombin Volcanics|70684|5|Briefly described|p13, p54-56, p61, p65, p68, p74-75|Late Ordovician|Late Ordovician|Junee-Narromine Volcanic Belt. Bolindian. Intruded by several monzonite and quartz monzonite bodies, which host the Northparkes porphyry Cu-Au deposit (described in detail). Unfossiliferous. Lithology described in some detail. Appears as Wombin Formation on p68.||Northparkes Group.||Overlies Goonumbla Volcanics.|Mainly coarse-grained, texturally immature volcaniclastic rocks, numerous bodies of coarsely porphyritic trachyandesite, and smaller volumes of trachyte lava and ignimbrite.|
24582|Wombin Volcanics|72495|5|Briefly described|p218, 220, 222, 240|Late Ordovician|Late Ordovician|Hosts the Endeavour Cu deposits at Goonumbla within intruding magnetite-rich quartz monzonite porphyries.  Similar aeromag pattern to Raggatt Volcanics. Continuity between the two beneath the Tullamore Syncline is suggested.||Northparkes Group|||Hematite-rich volcanic and volcaniclastic rocks.|30-MAR-20
24582|Wombin Volcanics|73154|5|Briefly described|p77 Fig.3|Bolindian|Late Ordovician|Macquarie Arc, Phase 4. Junee-Narromine Belt.||||Overlies Gunningbland Formation, underlies Cotton Formation.|Intermediate-mafic lava, siltstone, sandstone.|
24582|Wombin Volcanics|73287|4|Described|p662, p665 Fig.2, p678|Llandovery|Late Ordovician|Macquarie Arc. Interpreted as voluminous subaerial to subaqueous explosive eruptions and sector collapse of volcanic edifices. 700-1000m thick.|444-434 Ma|Goonumbla Volcanic complex||Conformably overlies the Goonumbla Volcanics|Intermediate to felsic volcanics including ignimbrites, porphyritic trachyandesites and trachytic lavas, polymict volcaniclastic breccias and volcanic sandstones. Intruded by numerous monzonites and quartz monzonites.|
29164|Wombramurra Formation|34555|4|Described|p241|||||||||
29164|Wombramurra Formation|43399|2|Defined|p189,197,199,200,||Early Carboniferous|202-205,207 (Early L.Carb)||||||
29164|Wombramurra Formation|43400|14|Not recorded|map opp.p.188||Early Carboniferous|||||||
29164|Wombramurra Formation|43406|14|Not recorded|p42,50||Tournaisian|Part of Parry Group (L.Carb)||||||
29164|Wombramurra Formation|43407|14|Not recorded|Map Legend|Carboniferous|Devonian|(Provisional Edition)||||||
29164|Wombramurra Formation|68005|5|Briefly described|p148.|Carboniferous|Carboniferous|Appendix 4 (p.148) invalidly lists this unit as a member of Tangaratta Formation, a unit of equal rank.||Unit in Parry Group.|||Zone of lenses of polymictic conglomerate and lithic wackes interbedded with Tangaratta Formation.|
35166|Wommara Bed|23055|6|Mentioned|Fig13p25|||Marker tuff in the Fern Valley coal seam of the Newcastle Coal Measures.||||||
31659|Wondalga Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
31659|Wondalga Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||31-MAR-05
70112|Wondervale Well Granite Gneiss|63866|5|Briefly described|p38|Statherian|Statherian||1685 +/- 5 Ma|Silver City Suite||Intrudes the Thackaringa Group and/or the Broken Hill Group.||
70112|Wondervale Well Granite Gneiss|64097|2|Defined|p329 Appdx., p305 Fig. 2, p317|Paleoproterozoic|Paleoproterozoic|Overlain by Purnamoota Subgroup (Broken Hill Gp). Age: 1685 +/- 5 Ma - identical to Hores Gneiss. Concordant meta-granite - coarse- to medium-grained qtz-feldspar-biotite gneiss+some zones with poikiliblastic garnets.||||||07-FEB-11
70112|Wondervale Well Granite Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1685+5Ma. Geological province: Broken Hill Domain. Written as Wondervale Well only.||||||07-FEB-11
70112|Wondervale Well Granite Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Silver City Suite. Age: 1685+/-5Ma. Geological province: Broken Hill Domain. Name presented only as Wondervale Well.||||||07-FEB-11
70112|Wondervale Well Granite Gneiss|66302|6|Mentioned|p41|Statherian|Statherian||1685 +/- 5 Ma |Silver City Suite||||
70112|Wondervale Well Granite Gneiss|68126|6|Mentioned|p30||||1685 +/- 5 Ma (Stevens et al. 2008).|||||
70112|Wondervale Well Granite Gneiss|70000|6|Mentioned|p34|Statherian|Statherian|||Unit in Silver City Suite.||||
70112|Wondervale Well Granite Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Silver City Suite.||Overlies Stephens Creek Granite Gneiss.|Complexly zoned body: inner zone is biotite-rich and biotite-garnet gneiss; outer zone is leucocratic biotite-poor gneiss.|
70112|Wondervale Well Granite Gneiss|70657|4|Described|p13 Fig.6|Statherian|Statherian|Curnamona Province: Broken Hill Domain. |~1685 Ma|Silver City Suite||Intrudes Allendale Metasediments (Broken Hill Group). Overlies Rasp Ridge Granite Gneiss. Underlies Stephens Creek Granite Gneiss.|Intrusive S-type felsic rocks, metamorphosed to gneiss.|
70112|Wondervale Well Granite Gneiss|72461|6|Mentioned|p16 fig 9||||1685 +/- 5 Ma|||||
70112|Wondervale Well Granite Gneiss|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian||1685 +/- 5 Ma|||||
70112|Wondervale Well Granite Gneiss|73308|6|Mentioned|p607 Fig.1||||1685 +/- 5 Ma.|||||
70112|Wondervale Well Granite Gneiss|73482|5|Briefly described|p422 Fig.3|Statherian|Statherian||1685+/-5 Ma|Silver City Suite||||
70112|Wondervale Well Granite Gneiss|73575|5|Briefly described|p828 Fig.2|Statherian|Statherian||1685+/-5 Ma||Silver City Suite|||
26333|Wongabel Rhyodacite Member|22857|5|Briefly described|p480 App.1 Tb.A1.6|Silurian|Silurian|Of Long Flat Volcanics. Porphyritic rhyodacite, ignimbrite. Max. thickness: ?300m. ||||||
26333|Wongabel Rhyodacite Member|39028|6|Mentioned|Map legend|Pridolian|Pridolian|||||||
26333|Wongabel Rhyodacite Member|40276|2|Defined|p7|Late Silurian|Late Silurian|||||||
26333|Wongabel Rhyodacite Member|71700|5|Briefly described|p26, CD|||Occurs in the Araluen 1:100k sheet area. Potentially equivalent to the Manar Ignimbrite Member or the Tally Ho Ignimbrite Members of the Long Flat Volcanics.||||||
81255|Wongajong conglomerate|72083|5|Briefly described|p35|||Trigg (2015). A 20m-thick exposure, SE of Ardlethan.||||Is overlain by the Cocoparra Group. May be equivalent to the Square Head Formation.||
41076|Wongalee Leucogranite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Medium to coarse-grained biotite leucogranite.||||||
41076|Wongalee Leucogranite|24366|6|Mentioned|p13|||||||||
41076|Wongalee Leucogranite|69323|5|Briefly described|p34,69|||Geological province: New England Orogen.||Unit of Uralla Supersuite.||||
41076|Wongalee Leucogranite|71628|5|Briefly described|p8: 4, 112-114, 116; p19-1|||Brown et al. (1990). Previously Wongalee Complex of Binns et al. (1967) after unpublished work by Ransley (1970). Unassigned to a Suite. Named after Wongalee homestead. A small (~2 km wide) intrusion ~20 km WNW of Uralla. Forms high (up to 350m) topographical relief.||Wongalee Suite.||Intrudes Yarrowyck and Balala Granodiorites.|Medium-grained biotite-leucomonzogranite-leucosyenogranite.|
76005|Wonnaminta Formation|66623|2|Defined|pp41-42, p31, p35. |Cambrian|Cambrian|Defined in this study. Same history of naming as Nundora Formation. Equivalent to Nundora, Bunker Creek and Copper Mine Range Formations. Exposed over c.436 km2. About 3.5 km thick. Faulted at top and bottom. Contains rare hexactinellid sponge spicules.||Unit in Teltawongee Group.||Intruded by Bittles Tank Volcanics.|A monotonous sequence of grey, medium- to fine-grained, dirty, turbiditic, muscovite-bearing quartzo-feldspathic sandstones; sharp bases, fining up to siltstone and sporadic mudstone in upper parts of many bedding units.|
76005|Wonnaminta Formation|66917|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Grey, fine- to medium-grained, dirty, turbiditic sandstone; basal erosional contact, with sand grains to 1 mm, detrital muscovite to 3 mm; up-section are climbing ripples, laminations and rare muddy tops (outcrops west of Koonenberry Fault).|
76005|Wonnaminta Formation|66918|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Grey, fine- to medium-grained, dirty, turbiditic sandstone; basal erosional contact, with sand grains to 1 mm, detrital muscovite to 3 mm; up-section are climbing ripples, laminations and rare muddy tops (outcrops west of Koonenberry Fault).|
76005|Wonnaminta Formation|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Zone of low magnetic intensity with minor curvilinear trends of moderate magnetic intensity.||||Overlies Depot Glen Formation.|Quartzo-feldspathic sandstone; minor phyllite and slate.|
76005|Wonnaminta Formation|67105|6|Mentioned|p655, 661|Cambrian|Cambrian|Occurs W of the Koonenberry Fault.||Teltawongee Group.||||
76005|Wonnaminta Formation|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Grey, fine- to medium-grained, dirty, turbiditic sandstone; basal erosional contact, with sand grains to 1 mm, detrital muscovite to 3 mm; up-section are climbing ripples, laminations, and rare muddy tops.|
76005|Wonnaminta Formation|67322|5|Briefly described|p10, p39; Fig.5|Cambrian|Cambrian|Defined by Mills in Greenfield et al., (2010). Age determined from p20 Fig.5 (Strat. column): Series 2. Occurs in the Kayrunnera-Koonenberry region.||Of the Teltawongee Group.||||22-FEB-18
76005|Wonnaminta Formation|69961|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Teltawongee Group.|||Grey, fine- to medium-grained, dirty, turbiditic sandstone; sand to 1 mm, detrital muscovite to 3 mm; basal erosional contact; climbing ripples, laminations and rare muddy tops are common in the upper parts of many bedding units.|
76005|Wonnaminta Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|Un-named unit is phyllitic, slaty metamudstone; magnetite-bearing north of Wonnaminta homestead.||Teltawongee Group|Includes un-named unit.||Grey, fine- to medium-grained, dirty, turbiditic sandstone; basal erosional contact, with sand grains to 1mm, detrital muscovite to 3mm; climbing ripples and laminations in the upper parts of many bedding units.|
76005|Wonnaminta Formation|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|||Teltawongee Group|||Grey, fine- to medium-grained, dirty, turbiditic sandstone; basal erosional contact, with sand grains to 1mm, detrital muscovite to 3mm; climbing ripples, laminations, and rare muddy tops are common in the upper parts of many bedding units.|
76005|Wonnaminta Formation|70651|5|Briefly described|Map Legend|Cambrian|Cambrian|Outcrops west of Koonenberry Fault: Phyllitic, slaty-metamudstone; magnetite bearing north of Woonaminta homestead. Massive, quartz rich, metasandstone horizons, thicker than 1m, within turbidite sequence of Woonaminta Formation.||Teltawongee Group|Includes 2 unnamed sub-units.||Grey, fine to medium-grained, dirty, turbiditic sandstone; basal erosional contact, with sand grains to 1mm, detrital muscovite to 3mm; climbing ripples, laminations, and rare muddy tops are common in the upper parts of many bedding units.|
76005|Wonnaminta Formation|70838|4|Described|p268-272, p274, p276|Cambrian|Cambrian|SE Koonenberry Belt. High-energy deep-water deposits. Detrital zircon analyses.||Teltawongee Group.||Is faulted against Kara Formation.|Characterised by repetitive sequences of immature sandstone (up to 3m thick locally) overlain by an upward-fining sequence (locally absent) of fine sandstone, siltstone and mudstone. Ubiquitous large (<5mm) detrital white mica grains.|
76005|Wonnaminta Formation|73177|6|Mentioned|p1113-1114 Figs.15-16|Cambrian|Cambrian|||||||
76005|Wonnaminta Formation|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
82435|Woodburn Complex|71628|5|Briefly described|p1-11; p2: 3, 61-69, 71; p3: 3, 10|||See also p3: 33-34, 86. Originally the Woodburn Diorite (Binns et al., 1967), after the Woodburn homestead. The name Woodburn Complex is used here to reflect the heterogeneous nature of the constituent rock types. A fairly small (~6 km x 1.5 km) Complex ~24 km SE of Uralla. Problems in determining its distribution and composition/affinities are discussed. Geochemistry described in some detail.||Bakers Creek Supersuite.||Intrudes the 'Sandon Association'. Is 'intimately associated with' Eastlake Monzogranite (possibly intruded contemporaneously).|Mafic igneous Complex comprising fine- to coarse-grained, leucocratic olivine gabbro, leucogabbro, biotite-hornblende monzogranite, and tonalite. Contains a variety of more felsic compositions: granophyres, monzogranites.|
27623|Woodlands Hill Coal Member|29942|4|Described|Fig.1|||Permian||||||
27623|Woodlands Hill Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27623|Woodlands Hill Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27623|Woodlands Hill Coal Member|40805|6|Mentioned|Table 1|||||||||
27623|Woodlands Hill Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Mount Ogilvie Formation.||||
31412|Woodton Formation|62095|2|Defined|p278 Appdx., p250, Plate 1|Asselian|Asselian|Synonymous with Kankool Fm (Lowe 1971); Inglewood Fm (Kelk 1986), Tara Fm. (Hockley 1966, Dawson 1988) SHRIMP age =290.5+/-2.8Ma (Asselian according to Roberts 2006, but Sakmarian in ICS scheme).  >230m at type section; ~900m on western Temi Syncline.||||||22-AUG-18
31412|Woodton Formation|63832|6|Mentioned|p131 fig 2|Sakmarian|Sakmarian|Werrie Syncline, Southern New England Fold Belt.||||||
31412|Woodton Formation|64631|5|Briefly described|p44 Fig.2.|Sakmarian|Sakmarian|Southern New England Fold Belt, Werrie Syncline. Some biostratigraphic and radiometric age control near base and top of unit respectively.||||Is overlain by Temi Formation.||
31412|Woodton Formation|65114|5|Briefly described|p395|||Includes Brogans Rhyodacite Member. Stratigraphically below the Temi Formation and Werrie Basalt||||||
31412|Woodton Formation|69793|6|Mentioned|p1121 Fig.12|Sakmarian|Asselian|Werrie Block, Tamworth Belt.||||||
31412|Woodton Formation|70373|6|Mentioned|p802|Permian|Asselian|Roberts et al. 2006. Glaciogenic succession, Werrie Block.||||Correlated with Alum Rock beds.||
31412|Woodton Formation|70728|5|Briefly described|p265|Sakmarian|Asselian|Geological province: North Tamworth terrane, New England Orogen.||||Overlain by Temi Formation. Underlain by Currabubula Formation.||
31412|Woodton Formation|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
27097|Woolomin Group|721|5|Briefly described|Map legend|Late Devonian|Silurian|Includes Bobs Creek Formation.  Age may be as young as Early Carboniferous?||||||
27097|Woolomin Group|22612|6|Mentioned|424 fig 2, 429|Dinantian|Silurian|||||||
27097|Woolomin Group|22857|4|Described|p434 App. 1 Tb. A1.5|Late Devonian|Middle Silurian|Chert, jasper, slate, arenite, basalt and dolerite. Geol. Prov: Woolomin Basin (Kanmantoo Fold Belt). Max. thickness: ?>4.5km. See also p203 and p484 App.1 Tb.A1.6.||||||03-MAR-06
27097|Woolomin Group|22859|6|Mentioned|p203-04|||||||||
27097|Woolomin Group|23050|4|Described|p15 Table1|Late Devonian|Silurian|Age: Middle Silurian to Late Devonian, part possibly as young as Early Carboniferous.||||||
27097|Woolomin Group|23051|5|Briefly described|Map Legend|Late Devonian|Early Silurian|||||||
27097|Woolomin Group|23790|5|Briefly described|p11 Fig. 2|Early Devonian|Silurian|Geological Province: Central Block||||||
27097|Woolomin Group|24366|5|Briefly described|p7, 17 Fig. 3|Early Devonian|Silurian|||||||
27097|Woolomin Group|41328|1|Redefined|p12|Early Carboniferous|Middle Devonian|||||||
27097|Woolomin Group|41990|6|Mentioned|Fig.2 P12|||||||||
27097|Woolomin Group|42376|6|Mentioned|p33|||||||||
27097|Woolomin Group|42554|5|Briefly described|p39|||||||||
27097|Woolomin Group|42629|5|Briefly described|p358|||||||||
27097|Woolomin Group|42748|6|Mentioned|Fig.3 P9|Devonian||||||||
27097|Woolomin Group|42866|5|Briefly described|Table 2, P12|||||||||
27097|Woolomin Group|43091|5|Briefly described|Map legend|||||||||
27097|Woolomin Group|43384|14|Not recorded|Map Legend||Silurian|||||||
27097|Woolomin Group|43385|14|Not recorded|p171||Silurian|||||||
27097|Woolomin Group|43397|14|Not recorded|p209,212|||||||||
27097|Woolomin Group|43400|14|Not recorded|p173,176,209||Early Devonian|Ref.to Voisey 1958. =Woolomin Beds||||||
27097|Woolomin Group|43582|5|Briefly described|p4|Early Carboniferous|Late Devonian|||||||
27097|Woolomin Group|43852|14|Not recorded|p197|||||||||
27097|Woolomin Group|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Cambrian|In Central Block and Woodsreef Melange.||||||31-MAY-07
27097|Woolomin Group|65398|1|Redefined|p1-22|Late Devonian|Late Silurian|Fault-bounded slices of tightly folded deep water marine metasedimentary and minor metavolcanic rocks. Contains the Nangahrah and Bobs Creek Formations. Age from conodonts and radiolaria. Faulted against Cara and Wisemans Arm Formations.||||||
27097|Woolomin Group|66720|6|Mentioned|Map legend|Late Devonian|Late Silurian||||Includes Nangahrah and Bobs Creek Formations.|||
27097|Woolomin Group|68003|5|Briefly described|p31, p32 Fig.3-h, p140. |Late Devonian|Silurian|Central Block, New England Fold Belt. Lateral equivalent of Bobs Creek and Nangahrah Formations.|||Includes Bobs Creek and Nangahrah Formations.||Low grade regionally metamorphosed, multiply deformed chert, wacke, basic volcanics and mudstone.|
27097|Woolomin Group|68004|5|Briefly described|p122.|||New England Fold Belt. Outcropping and subcropping marine intermediate to mafic volcanic/sedimentary rock packages. Hosts probable Besshi and/or Cyprus type VHMS occurrences. High potential with a certainty level of C.||||||
27097|Woolomin Group|68005|4|Described|pp17-18, p22, pp26-31, pp156-157, p169.|Late Devonian|Middle Silurian|Djungati terrane, Central Block, New England Fold Belt. Defined by Aitchison et al. (1988). Oldest and most westerly sedimentary package in the Block. Sediments were disrupted during latest Devonian to Early Carboniferous.|||Includes Bobs Creek and Nangahrah Formations.||Low grade regionally metamorphosed, multiply deformed chert, wacke, basic volcanics and mudstone.|
27097|Woolomin Group|68006|5|Briefly described|p20 Fig.3-A, p25, p149.|Late Devonian|Middle Silurian|Oldest and most western sedimentary package in the Central Block, New England Fold Belt. Sediments from volcanic arc with little terrigenous input. Deformed Late Devonian/Early Carboniferous. Limited potential for small Besshi-Cyprus VHMS-type mineralisation.||||Is overlain by, and faulted against, Cara Formation.||
27097|Woolomin Group|68822|5|Briefly described|p347|Devonian|Silurian|Conodont (Ishiga et al. 1988) and radiolarian identifications (Aitchison et al. 1992a) indicate an age range from Middle or latest Silurian into the Late Devonian.|||||Sandstone poor, dominated by the repetition of fault slices consisting of basal basalts that pass up into red cherts, siltstones, and only locally sandstone beds.|
27097|Woolomin Group|70036|5|Briefly described|Map legend|||Central Block, New England Fold Belt. Included in a mapped unit of Silurian to Carboniferous strongly deformed, andesitic to rhyolitic metasedimentary rocks, lithic sandstone, argillite, chert and jasper.||||||
27097|Woolomin Group|71628|5|Briefly described|p4-17||||||Bobs Creek Formation.|Is intruded by Copeton Monzogranite.||
27097|Woolomin Group|73197|5|Briefly described|p468|Devonian|Silurian|New England Orogen, southern. Referred to as Woolomin Group by Spry (1953, 1955), also refered to as the Djungati Terrane (Buckman et al., 2015; Flood and Aitchison, 1988). Earliest part of accretionary complex, dominated by ocean floor sedimentary rocks.|||||Cohesive sequence of basalt and chert.|
41245|Wooloo Limestone Member|50590|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Cabonne Group.  Bedded to massive limestone.||||||29-JUN-04
77049|Woomargama Granite|69801|5|Briefly described|p2, p4-p5, p85-89, p91, p94, p135-137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs south of Holbrook. Sample locality, petrography, zircon characteristics, SHRIMP analyses and interpretation are detailed.|428.2 +/- 1.9 Ma|Koetong Suite||Intruded by the Holbrook Granite.|Medium- to coarse-grained, bluish-grey biotite-muscovite granite which hosts abundant enclaves of quartzite through pelitic migmatitic schist and biotite-rich enclaves.|
32529|Worobil Alkali Granite|23043|5|Briefly described|Map Legend|Namurian|Namurian|of Gulgong Plutonic Suite.||||||
32529|Worobil Alkali Granite|23170|2|Defined|p273|Carboniferous|Carboniferous|of Gulgong Plutonic Suite.||||||
32529|Worobil Alkali Granite|68003|5|Briefly described|p24 Fig.3-e. |Visean|Visean|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gulgong Plutonic Suite.||||
70457|Wowagin Dacite Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of De Drack Formation (Mount Fairy Group). Grey to greenish grey, medium-grained, flow-banded rhyodacite to dacite lava.||||||
70457|Wowagin Dacite Member|68592|2|Defined|p726, p728, p730 Fig.132, p760, p786-91|Late Silurian|Early Silurian|New name. Previously mapped as Carboniferous porphyries and undifferentiated Lambie Group (Scheibner 1973); Carboniferous? Syenite (Brunker and Offenberg 1970); and Strathaird Formation (Lambie Group) (Felton 1974). Product of a newly recognised Late Silurian felsic volcanic centre. Geomorphic expression and outcrop: generally forms boldly outcropping hills and ridges. Type section: occurs across a ridge between a base and an upper contact with undifferentiated De Drack Formation; basal contact is better exposed at another location. Thickness: 270 m thick at type section, but thins to north and south. Erupted in a moderately deep to deep marine environment. Lower greenschist facies metamorphism. Age: overlying upper portion of De Drack Formation includes a graptolite fauna, possibly late Wenlock to early Ludlow age. Has distinguishing features from surrounding lithologies. Minor quartz phenocrysts (in geographically separated dacite) differentiate Wowagin Dacite Member from andesite in Sooley Volcanic Member.||Unit in De Drack Formation.||Correlates with Sooley Volcanic Member; occupies similar stratigraphic position to the more extensive Woodlawn Volcanics.|Grey and greenish-grey, porphyritic, medium-grained, spherulitic, flow-banded, moderately crystal-rich, coherent rhyodacite (to the north) and dacite lava (to the south).|
70457|Wowagin Dacite Member|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sfdw. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||De Drack Formation||Is within undifferentiated De Drack Formation.|Medium grained, spherulitic, flow banded, porphyritic rhyodacite and dacite.|
70457|Wowagin Dacite Member|70542|5|Briefly described|Map Legend|Devonian|Silurian|||De Drack Formation|||Grey to greenish grey, medium grained, spherulitic, flow banded, porpyhritic rhyodacite and dacite.|
70457|Wowagin Dacite Member|70543|5|Briefly described|Map Legend|Devonian|Silurian|||De Drack Formation|||Medium grained, spherulitic, flow banded, porphyritic rhyodacite and dacite.|
70457|Wowagin Dacite Member|71069|6|Mentioned|p26, p29, p35, p125, p137 fig 44|||Northern Goulburn Basin.See also p140 tbl 4, p144, p146, p147, p151, p154.||De Drack Formation||Partly equivalent to the Kohinoor Volcanics. Equivalent to the Woodlawn Volcanics.||
70457|Wowagin Dacite Member|71700|5|Briefly described|p14|||||De Drack Formation||||
74577|Wrens Nest Trachyte|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Grey, fine-grained, aphyric to sparsely porphjyritic quartz trachyte to rhyolite. Groundmass typically contains abundant microlites of aegirine and less abundant arfvedsonite which define a crude flow foliation.||||||
74577|Wrens Nest Trachyte|68592|2|Defined|p608,p610,p613, p618-22, p678-9, p683-91|Early Devonian|Early Devonian|New name, after Wrens Nest Creek. These rocks were formerly included in Box Ridge Volcanics (Brunker and Offenberg, 1970; amended Pogson and Watkins, 1998). Type locality described. Layers/sills from 130-360m thick for a total unit thickness of c.950m. Trace elements, geochemistry (in particular) detailed: two groups recognised. Forms bouldery outcrops in prominent wooded ridges. Unclear if extrusive or intrusive: favoured interpretation is a series of superimposed but partly discordant sills. Geophysical properties described. Age based on geochemical similarities with other dated units.||Unit in Campbells Group.||Intercalated paraconformably with Cuddyong Formation. Is correlated with Box Ridge Volcanics, and is equivalent of Keverstone Supersuite A-type granites.|Dominantly fine-grained grey trachyte with scattered quartz and feldspar phenocrysts, and peralkaline rhyolite.|
74577|Wrens Nest Trachyte|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Sct. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Campbells Group||Is enveloped by undifferentiated Cuddyong Formation.|Fine grained, aphyric to sparsely porphyritic quartz trachyte to rhyolite; microlites define a crude flow foliation.|
74577|Wrens Nest Trachyte|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Campbells Group|||Fine grained, aphyric to sparsely porphyritic quartz trachyte to rhyolite; microlites define a crude flow foliation.|
31664|Wullwye Suite|22815|5|Briefly described|p53,60|Silurian|Silurian|||||||
31664|Wullwye Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
31664|Wullwye Suite|72571|5|Briefly described|p90-91, p101|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail.|||||Felsic, medium-grained, biotite granite with magnetite and no titanite.|
80444|Wyam Creek granite|70718|5|Briefly described|p78-p79|Late Devonian|Late Devonian|Informal name, interpreted from geophysics. Size and rough shape of magnetic anomaly are provided.Only member ofthe suite with roughly circular morphology. Interpreted lithology and age  based on similar geophysical signature to outcropping Lake Boga and Pyramid Hill granites.||Cunninyeuk granite suite|||Interpreted to be S-type granite , with metamorphic aureole.|02-JUN-19
24127|Wyangle Formation|22638|6|Mentioned|p9|||||||||
24127|Wyangle Formation|22687|6|Mentioned|110|Late Silurian|Late Silurian|Geol province Lachlan Fold Belt||||||
24127|Wyangle Formation|22768|6|Mentioned|p174-75|||||||||
24127|Wyangle Formation|22857|4|Described|p174-175, p452, App.1, Tb.A1.6|Middle Silurian|Silurian|Andesitic tuffs and lavas, quartz-poor lithic sandstone, conglomerate, cherty siltstone.||||||
24127|Wyangle Formation|36534|6|Mentioned|p225|||||||||
24127|Wyangle Formation|37529|5|Briefly described|p7|||||||||
24127|Wyangle Formation|39319|6|Mentioned|p357|||||||||
24127|Wyangle Formation|42045|4|Described|p153|||||||||
24127|Wyangle Formation|42145|4|Described|Table 1 P624|||See also Fig.2||||||
24127|Wyangle Formation|42313|2|Defined|p96|Middle Silurian|Early Silurian|Age: late Early to early Middle Silurian||||||
24127|Wyangle Formation|42314|5|Briefly described|Map|Middle Silurian|Early Silurian|||||||
24127|Wyangle Formation|42497|5|Briefly described|Map Legend|Wenlockian|Wenlockian|||||||
24127|Wyangle Formation|42828|5|Briefly described|Table 1 P129|Middle Silurian||||||||
24127|Wyangle Formation|44093|6|Mentioned|p29|||Mentioned with Blowering Formation as sedimentary and volcanic sequences.||||||
24127|Wyangle Formation|66197|5|Briefly described|p631 Fig.3a|Wenlock|Llandovery|Tumut Trough. Deep marine shale and sandstone. Underlies the Blowering Formation, overlies the Brungle Creek Metabasalt.||||||14-MAR-12
40892|Wyarra Shale|12066|5|Briefly described|p13|||Of the Gnalta Group. Conformably overlies the Wydjah Formation.||||||11-SEP-07
40892|Wyarra Shale|22857|5|Briefly described|p90 Fig. 14.7B, p404 App. 1 Tb. A1.4|Middle Cambrian|Early Cambrian|Red shale; siltstone and carbonate interbeds; tuffaceous greywacke, grey shale. ||||||
40892|Wyarra Shale|62787|4|Described|p77, p80, p81|Middle Cambrian|Early Cambrian|Of Gnalta Group. Conformably overlies Wydjah Formation and is faulted against Yandaminta Quartzite. Strongley cleaved maroon and purple shales with somekhaki-coloured beds. Thickness: ~50m.||||||07-FEB-11
40892|Wyarra Shale|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Shale, sandstone, conglomerate, limestone.||||||10-SEP-07
40892|Wyarra Shale|64671|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Khaki, blue and purple shales, minor sandstones and limestones. Occurs west of Mt Arrowsmith.||||||01-DEC-08
40892|Wyarra Shale|64687|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Khaki, blue and purple shales, minor sandstones and limestones. Fault bounded and unconformable to the east, against Ordovician formations, unconformably overlain by Cretaceous rocks to the west.||||||27-NOV-08
40892|Wyarra Shale|66623|3|Fully described|pp56-58, pp72-73. |Early Cambrian|Early Cambrian|Defined informally by Warris (1967); included in Gnalta Group by Brock and Percival (2006) based on palaeontological studies. Ordian - early Templetonian. Forms low hills and scree-covered slopes. Thickness about 50 m. Unfossiliferous.||Unit in Gnalta Group.||Overlies Wydjah Formation. Is unconformably overlain or faulted against Yandaminta Quartzite.|Maroon and purple shale, strongly cleaved, sporadic khaki-coloured beds.|
40892|Wyarra Shale|66917|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Gnalta Group.||Overlies Wydjah Formation.|Khaki, blue and purple slate and shale, minor sandstone and limestone.|
40892|Wyarra Shale|66929|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian||||||Khaki, blue and purple shales; minor sandstones and limestones.|
40892|Wyarra Shale|66933|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
40892|Wyarra Shale|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Gnalta Group.|||Khaki, blue and purple slate and shale, minor sandstone and limestone.|
40892|Wyarra Shale|67322|4|Described|p10; Fig.5|Drumian|Stage 5|Unit defined by Brock and Percival (2006). Approximately 50m thick. Age determined from p20 Fig.5 (Strat. column). Occurs in the Mount Arrowsmith region.||Of the Gnalta Group.||Conformably overlies Wydjah Formation. Is overlain unconformably by or faulted against Pimbilla Tank Group.|Dominated by strongly cleaved, unfossiliferous maroon, purple, and khaki shales. Distinguished from Wydjah Formation by the absence of sandstones.|22-FEB-18
27625|Wybeena Metamorphics|23720|5|Briefly described|Map Legend|||Part of the "Sandon Association".||||||08-DEC-04
27625|Wybeena Metamorphics|31694|6|Mentioned|p344|||||||||
27625|Wybeena Metamorphics|38804|6|Mentioned|Fig.1|||||||||
27625|Wybeena Metamorphics|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Part of the "Sandon Association".||||||16-DEC-04
27625|Wybeena Metamorphics|42803|6|Mentioned|Fig.1 P112|||||||||
27625|Wybeena Metamorphics|42872|5|Briefly described|p103|||||||||
27625|Wybeena Metamorphics|44450|3|Fully described|p12 Table 1|Early Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||
27625|Wybeena Metamorphics|71628|6|Mentioned|p3-86|||Korsch (1977); regarded these as metamorphosed equivalents of the Sandon Association.|||||Chert-rich.|
32504|Wyberba mass|42378|6|Mentioned|Table 1 p6|||Informal subdivision of Dundee Rhyodacite.||||||
34693|Wydjah Formation|12066|5|Briefly described|p13|Cambrian|Cambrian|Of Gnalta Group. Conformably overlies the Pincally Formation, conformably overlain by Wyarra Shale. Includes the Pimpira Member.||||||11-SEP-07
34693|Wydjah Formation|22857|5|Briefly described|p90 Fig. 14.7B, p404 App. 1 Tb. A1.4|||Contains the Pimpira Member. ||||||
34693|Wydjah Formation|22858|6|Mentioned|p99|||||||||
34693|Wydjah Formation|62787|4|Described|p77, p76 Fig. 1, p79, p81|Middle Cambrian|Early Cambrian|Of Gnalta Group. Includes Pimpira Member. Conformably overlies Pincally Formation. Thick: 270m. Interbedded dolostones, phyllitic siltstones and shales, and upward-coarsening sequence of sandstones. See p 79 for detailed info.||||||07-FEB-11
34693|Wydjah Formation|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Shale, sandstone, conglomerate, limestone.||||||10-SEP-07
34693|Wydjah Formation|64671|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Red to grey mudstone, conglomerate, limestone and shale. Occurs west of Mt Arrowsmith.||||||25-NOV-08
34693|Wydjah Formation|64687|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Red to grey mudstone, conglomerate, limestone and shale. Fault bounded and unconformable to the east, against Ordovician formations, unconformably overlain by Cretaceous rocks to the west.||||||27-NOV-08
34693|Wydjah Formation|66623|3|Fully described|pp56-58, pp69-71. |Early Cambrian|Early Cambrian|Defined by Warris (1967); included in Gnalta Group by Brock and Percival (2006) based on palaeontological studies. Ordian-early Templetonian. Stratigraphic equivalent of First Discovery Limestone Member; broadly contemporaneous with Coonigan Formation. Conglomerate clasts include schist, altered volcanics and sandstone. About 250 m thick. Small shelly fossils occur in dolostone beds.||Unit in Gnalta Group.|Includes Pimpara Member.|Overlies Pincally Formation. Is overlain by Wyarra Shale.|Polymictic pebble conglomerate; red-brown, medium- to very coarse-grained silicified quartz sandstone; phyllitic cleaved siltstone with rare, thin dolomitic beds.|
34693|Wydjah Formation|66917|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Gnalta Group.|Includes Pimpara Member.|Overlies Pincally Formation. Is overlain by Wyarra Shale.|Lower and upper units of upward-coarsening red-brown flaggy sandstone and conglomerate, separated by dolostone, siltstone and shale of the Pimpara Member.|
34693|Wydjah Formation|66929|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian||||||Red to grey mudstone, conglomerate, limestone and shale.|
34693|Wydjah Formation|66933|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
34693|Wydjah Formation|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Gnalta Group.|Includes Pimpira Member.||Lower and upper units of upward-coarsening red-brown flaggy sandstone and conglomerate; separated by dolostone, siltstone and shale of the Pimpira Member.|
34693|Wydjah Formation|67322|4|Described|p9-10; Fig.5|Stage 5|Stage 5|Thickness is approximately 250m: 87m for the lower unit, 74m for the Pimpira Member, and 89m for the upper unit. Age from Pelagiella madianensis in basal beds of Pimpira Member. Occurs in the Mount Arrowsmith region.||Of the Gnalta Group.|Pimpira Member|Conformably overlies Pincally Formation. Conformably overlain by the Wyarra Shale.|Basal distinctive cross-bedded, white quartz-rich sandstone. This Formation is subdivisible into a lower and upper upwards-coarsening sand-dominated sequence (both culminating in conglomeratic layers), separated by the dolomitic Pimpira Member.|22-FEB-18
34693|Wydjah Formation|70752|5|Briefly described|p127, p135-137, p139, p141|Middle Cambrian|Middle Cambrian|Koonenberry Belt. Linguliformean brachiopods have close affinity with those in Giles Creek Dolostone (NT). Systematic palaeontological descriptions. Ordian-early Templetonian.||||Overlies Pincally Formation.||
40927|Wyelba Member|50230|4|Described|Map legend|Wenlock|Wenlock|Of the Yass Formation (Douro Group).  Laminated tuffaceous mudstone, interbedded sandstone and mudstone, coarse-grained sandstone.  Overlies Hawkins Volcanics.||||||10-MAY-04
40927|Wyelba Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Ravenswood Formation (Douro Gp). Laminated tuffaceous mudstone, interbedded sandstone and mudstone, coarse-grained sandstone, cross-stratified to planar laminated.||||||02-JUN-08
40927|Wyelba Member|68592|2|Defined|p428, p433, p436, p440, p473-6, p478-81|Wenlock|Wenlock|See also p484. Cramsie et al. (1978). Raised to Formation status by Feary (1984, 1986); here returned to Member status, to include the clastic succession below the first carbonates, of Glen Bower Formation. Type section described. c.145m thick. Barrier lagoon to beach or barrier island deposits. Unfossiliferous.||Basal unit in Glen Bower Formation.||Is overlain conformably by Copplestone Member. Correlated with O'Briens Creek Sandstone Member (Yass Formation).|Laminated tuffaceous mudstone; thinly-bedded, interbedded quartz-lithic sandstone and mudstone; coarse-grained, cross-stratified to planar laminated, quartzose sandstone.|
40927|Wyelba Member|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdgw. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Glen Bower Formation||Is overlain by Copplestone Member. Overlies Hawkins Volcanics.|Laminated tuffaceous mudstone; thinly bedded, interbedded quartz lithic sandstone and mudstone; coarse grained, cross stratified to planar laminated quartzose sandstone.|
40927|Wyelba Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Glen Bower Formation|||Laminated tuffaceous mudstone; thinly bedded, interbedded quartz lithic sandstone and mudstone; coarse grained, cross stratified to planar laminated quartzose sandstone.|
40927|Wyelba Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Glen Bower Formation|||Laminated tuffaceous mudstone, thinly bedded, interbedded quartz lithic sandstone and mudstone; coarse grained, cross stratified to planar laminated quartzose sandstone.|
30527|Wylinga Member|6969|5|Briefly described|p17|Early Wenlock|Early Wenlock|Basal member of the Dripstone Formation.  Geological Province: Lachlan Fold Belt.||||||
30527|Wylinga Member|22857|4|Described|p466 App.1 Tb.A1.6|Silurian|Silurian|Of the Dripstone Formation (Mumbil Group). Volcanics with limestone lenses. Max. thickness: 25m. ||||||
30527|Wylinga Member|23043|5|Briefly described|Map Legend|Wenlock|Wenlock|of Dripstone Formation, Mumbil Group.||||||
30527|Wylinga Member|23170|2|Defined|p82|Wenlock|Wenlock|of Dripstone Formation, Mumbil Group. Superceded 'Wylinga Formation'.||||||
30527|Wylinga Member|23225|6|Mentioned|p17|||of Dripstone Formation.||||||
30527|Wylinga Member|68003|5|Briefly described|p146.|Silurian|Silurian|Lachlan Fold Belt. Parent [Dripstone Formation] not specified.||Unit in Mumbil Group.|||Felsic crystal-lithic sandstone, fossiliferous limestone.|
24589|Wylora Quartz Gabbro|40132|2|Defined|p238|Early Devonian|Early Devonian|||||||
24589|Wylora Quartz Gabbro|68592|5|Briefly described|p1610, p1642, p1644|||Carr et al. (1979). Now incorporated, with Springponds Granodiorite, into Springponds Tonalite on the basis of similar composition, texture and geophysical response.|395 +/- 8 Ma (K-Ar isotopic: Carr et al., 1980).|||||
36328|Wyndham Sequence|23540|5|Briefly described|p 421|||Also see p 423||||||
27668|Wynn Coal Member|29942|4|Described|Fig.1|||Permian||||||
27668|Wynn Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27668|Wynn Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Foybrook Formation.||||
35708|Wyoming Granite|50231|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of the Wyangala Batholith.||||||
35708|Wyoming Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Gooramma Suite. Pinkish-grey, coarse-grained, massive, equigranular (to occasionally porphyritic) leucocratic granite.||||||
35708|Wyoming Granite|66623|6|Mentioned|p388.|||Lachlan Orogen. Has similar slopes of REE pattern as Tibooburra Suite.||Unit in Wyangala Batholith.||||
35708|Wyoming Granite|68592|2|Defined|p1305-6, p1398, p1400-3, p1450|Early Devonian|Early Devonian|New unit and new name, after Wyoming property. Previously included within their Whistle Waa Granite by Chappell et al. (1991). Forms scattered boulder outcrops across the crest and slopes of a broad hill. Type locality described. Geochemistry detailed; geophysical properties described. Not isotopically dated: age from intrusive relationship and geochemical affinity.||Unit in Gooramma Suite.||Intrudes Wyangala Granite.|Pinkish-grey, coarse-grained, massive, equigranular (to weakly porphyritic) leucocratic granite. I-type.|
35708|Wyoming Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dgy. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Gooramma Suite|||Coarse grained, massive, equigranular to weakly porphyritic leucocratic granite; high magnetic susceptibility.|
35708|Wyoming Granite|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Gooramma Suite|||Coarse grained, massive, equigranular to weakly porphyritic leucocratic granite; high magnetic susceptibility.|
26334|Wyoming Limestone Member|5250|5|Briefly described|p42, p45  ||Early Caradoc|Member of  Fossil Hill Limestone. Includes brachiopod fauna.||||||16-JAN-12
26334|Wyoming Limestone Member|23214|3|Fully described|p41|Eastonian|Eastonian|Of Fossil Hill Limestone. 27m thick at type section.||||||
26334|Wyoming Limestone Member|38219|2|Defined|p307|Late Ordovician|Late Ordovician|Part of Cliefden Caves Group. See also Fig.2.||||||
26334|Wyoming Limestone Member|41046|6|Mentioned|p144|||||||||
26334|Wyoming Limestone Member|41508|6|Mentioned|Abb.1|||||||||16-JAN-12
26334|Wyoming Limestone Member|42479|5|Briefly described|p108|||||||||
26334|Wyoming Limestone Member|42603|5|Briefly described|Fig.4 P57|||||||||
26334|Wyoming Limestone Member|43571|5|Briefly described|p821|||||||||
26334|Wyoming Limestone Member|63278|5|Briefly described|p154|||Of the Fossil Hill Limestone. Contains calcarenites. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
26334|Wyoming Limestone Member|70754|5|Briefly described|p449, p455, p462|Late Ordovician|Late Ordovician|Systematic palaeontological descriptions.||Fossil Hill Limestone.|||Includes thin-bedded terrigenous-rich limestones, calcarenite.|
35342|Wywurri Granite|50231|5|Briefly described|Map Legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
35342|Wywurri Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Cream to light grey, medium- to coarse-grained, massive to mildly foliated, equigranular to occasionally pophyritic cordierite-muscovite-biotite granite with leucocratic, finer-grained. High K and U, mod.to low Th radioelement response.||||||10-SEP-14
35342|Wywurri Granite|66185|5|Briefly described|p397, p398 Fig.2, p399|||In the Wyangala Batholith. Intrudes Reids Flat Granite (426-419.5Ma). Massive to foliated, grey to beige, equigranular to porphyritic, cordierite-muscovite-biotite granite and soda granite.||||||
35342|Wywurri Granite|68592|2|Defined|p1262-4, p1268-9, p1274, p1284, p1308-11|Late Silurian|Late Silurian|See also p1255 Fig.220. New name, after Wywurri property. The pluton was included in undifferentiated Wyangala Batholith by Stevens (1955) and Brunker and Offenberg (1970); Chappell et al. (1991) did not separate it from the Reids Flat Granite. Here assigned to the Hovells Suite on geochemical grounds. Type locality described. Geochemistry detailed; geophysical properties described. Not isotopically dated.||Unit in Hovells Suite.||Intrudes Reids Flat Granite and Adaminaby Group.|Cream to light grey, fine- to coarse-grained, equigranular to sporadically porphyritic, massive to mildly foliated, cordierite-muscovite-biotite granite. Not fractionated. S-type.|
35342|Wywurri Granite|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Son. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Fine-coarse grained, equigranular-sporadically porphyritic, massive to mildly foliated cordierite-muscovite-biotite granite with leucocratic, finer grained marginal phases. High K and U, medium to high Th; low magnetic susceptibility.|
35342|Wywurri Granite|70545|5|Briefly described|Map Legend |Devonian|Silurian|||Hovells Suite|||Fine-coarse grained, equigranular-sporadically porphyritic, massive to mildly foliated cordierite-muscovite-biotite granite with leucocratic, finer grained marginal phases. High K and U, medium to high Th; low magnetic susceptibility.|
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.||||||
31667|Yabba Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
76048|Yadabal Lagoon granite|66934|5|Briefly described|Map legend|Early Devonian|Early Devonian|Informal name. Magnetic susceptibility and gravity readings are given.||Unit in Thalaka Granite Suite.|||Interpreted S-type granite.|
76048|Yadabal Lagoon granite|70718|5|Briefly described|p59- 61, p64, 95, 119, 120|Middle Silurian|Ordovician|Name derived from Yadabal Lagoon. Relatively low magnetic susceptibility.||Thalaka granite suite||Intruded by the Wanganella granodiorite.||30-MAY-19
23277|Yalgatta Granodiorite|22815|4|Described|p76,77|||||||||
23277|Yalgatta Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Glenbog Suite.||||||
23277|Yalgatta Granodiorite|68592|6|Mentioned|p1675|Early Devonian|Early Devonian|||Unit in Glenbog Suite.||||
36151|Yalgogrin Granite|60303|5|Briefly described|p9 Tb. 1|||||||||21-JAN-21
36151|Yalgogrin Granite|61964|3|Fully described|p14 Fig. 4, p50-51, p37, p38, p41 Tb. 2|Middle Silurian|Early Silurian|Of Koetong Suite (Koetong Supersuite). Nomenclatural history included. S-type. Detailed lith. Age: ~428.2Ma, 432.1+/-2.8Ma (SHRIMP).||||||14-OCT-08
36151|Yalgogrin Granite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Biotite-cordierite granite, grey, coarse- to medium-grained, porphyritic, locally megacrystic, biotite-rich microgranular enclaves and abundant metasedimentary xenoliths.||||||10-APR-08
36151|Yalgogrin Granite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian|||Unit in Koetong Suite.||Intrudes Clements Formation.|Biotite-cordierite granite, grey, coarse- to medium-grained, porphyritic, locally megacrystic, abundant metasedimentary enclaves.|
36151|Yalgogrin Granite|70296|6|Mentioned|p1, p5, 6-7, p10, p24|Llandovery|Llandovery|Cargelligo district. Includes inherited components.|430 +/- 2.9 Ma (SHRIMP U-Pb)|Koetong Supersuite|||S-type granite.|21-JAN-21
36151|Yalgogrin Granite|70777|4|Described|p1, p3-p4, p39-p41,|Wenlock|Wenlock|Lachlan Orogen. New zircon date is indistinguishable from dates previously obtained (430 +/- 2.9 Ma, Black, 2005; Colquhoun et al., 2005); Both dates are interpreted to be the ages of magmatic crystallisation. Previously mapped as the Kikoira Granite; however, this was considered inappropriate as Chappell et al., 1991 had previously named a different pluton the Kikoira Granite. Chappell et al (1991) mapped this pluton as the Bland Granite, this name however, was also invalid as Bowman (1977) had previously mapped a different pluton as the Bland Diorite; subsequently it was recognised that this granite is a southern extension of the Yalgogrin Granite. Petrography, zircon description and U-PB SHRIMP dates are discussed in some detail. This granite is interpreted to be an S-type. See also p43-p46, p51, p79-p80, p95-p96.|428.5 +/- 2.3 Ma (SHRIMP, this volume)|Koetong Supersuite||Coeval with the Ungarie and Buddigower Granites. Intrudes the Wagga Group.|Coarse-grained, foliated biotite granite.|13-SEP-19
36151|Yalgogrin Granite|71693|5|Briefly described|Map legend; p2.|Silurian|Silurian|Associated with structurally controlled low sulfide Au mineralisation.||Koetong Supersuite.|||Coarse- to medium-grained, grey, porphyritic, locally megacrystic, biotite-cordierite granite with abundant metasedimentary enclaves.|
36151|Yalgogrin Granite|73082|6|Mentioned|p27|||Ariah Park district. Quartz reefs in this unit have historically been worked for tin, gold and wolframite.||||||
81818|Yambla Formation|73457|4|Described|ii, p1, p3, p5, p9-15|Late Devonian|Late Devonian|Comprises a sequence that forms the crest and western slopes of the Great Yambla Ridge and Table Top Ridge. Noted by Joplin (1944, p.205), brief lithological description given by Willis (1974). Estimated to be 1700 m thick. Interpreted to unconformably overlie the Budginigi Ignimbrite. Western boundary is inferred to be faulted. Trigg (2019) informally described a lower conglomeratic subunit and an upper sandstone and pebbly sandstone subunit. Distinctive pits on surfaces of the upper sandstone subunit are probable weathering features. Initially deposited in a very high energy environment, interpreted as non-marine. Upper subunit has maximum depositional age of 377+/-3.0 Ma (Huang, 2019), unit is interpreted to be entirely Late Devonian in age, in part from a general correlation with other 'Lambie' facies sequences. Further details are given in Trigg (2019), with a full definition in Trigg (2021).|377+/-3.0 Ma LA-ICP-MS MDA (Huang, 2019)|||Unconformably overlies Adaminaby Group and Budginigi Ignimbrite, nonconformably overlies Granya Granite|Fining-upwards sequence of cobble conglomerate in lower part composed mostly of rounded metasandstone clasts, locally intercalated with thin sandstone and siltstone; recessive sandstone and pebbly sandstone in upper part.|
40932|Yanawe Formation|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Douro Group. Overlies the Laidlaw Volcanics; underlies Hattons Corner Group.||||||29-MAY-08
40932|Yanawe Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Douro Gp. Includes Excursion Creek, Tullerah Sst, Hulong Conglom., Gums Road Limest., Euralie Limest., Humewood Volcanic Sst. + Werong Breccia Members. Volcaniclastic sst, pebble-boulder volc.conglom. tuffaceous or volc mudst. calcareous mudst.+...||||||09-SEP-08
40932|Yanawe Formation|68592|2|Defined|p432,p434-6,p441-2,p515-6,p520,p523-58|Ludlow|Wenlock|See also p239, p427-8, p430 Fig.89, p1869. New name. Includes the sedimentary rocks between the last primary volcanic rocks of the Laidlaw Volcanics and the base of the Bowspring Limestone Member (Silverdale Formation). Represents volcaniclastic debris flow, fluvial, pyroclastic lacustrine and ashfall depositions overlain by a marine transgression. Diachronous base. Limestone units are not considered economic because of their limited thickness and impure interbedded nature. See individual Members for type localities. 30-800m thick. Probably mid-Wenlock to early Ludlow.||Unit in Douro Group.|Includes Gums Road and Euralie, Limestone Members; Excursion Creek and Tullerah, Sandstone Members; Werong Breccia Member; Humewood Volcanic Sandstone Member; Hulong Conglomerate Member.|Overlies Laidlaw and Hawkins Volcanics, and locally Yass Formation, disconformably. Is overlain conformably by redefined Silverdale Formation (Hattons Corner Group).|Lower terrestrial sequence of volcaniclastic sandstone and mudstone, siliceous mudstone and pebble conglomerate, pebble to boulder breccia; upper marine sequence of volcanic sandstone, siltstone and mudstone, 2 horizons of fossiliferous limestone.|
40932|Yanawe Formation|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdw[3 asterisks]. Includes three unnamed members; a siliceous/tuffaceous mudstone, quartz lithic volcanic sandstone and arkosic-volcanic rich sandstone. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Douro Group|Includes 7 named Members: Werong Breccia, Humewood Volcanic Sandstone, Euralie Limestone, Gums Road Limestone, Hulong Conglomerate, Tullerah Sandstone, & Excursion Creek Sandstone; & 3 unnamed units.|Unconformably overlies Laidlaw Volcanics. Is overlain by Silverdale Formation.|Volcaniclastic sandstone, siltstone and mudstone, pebble-boulder conglomerate and breccia, siliceous volcanic mudstone, calcareous mudstone and lenses of fossiliferous limestone.|
40932|Yanawe Formation|70540|5|Briefly described|Map Legend|Silurian|Silurian|Includes three unnamed members; a siliceous/tuffaceous mudstone, quartz lithic volcanic sandstone and arkosic-volcanic rich sandstone.||Douro Group|Includes Werong Breccia Member, Humewood Volcanic Sandstone Member, Euralie, Gums Road Limestone Members, Hulong Conglomerate Member, Tullerah Sandstone Member, Excursion Creek Sandstone Member.||Volcaniclastic sandstone, siltstone and mudstone, pebble-boulder conglomerate and breccia, siliceous volcanic mudstone, calcareous mudstone and lenses of fossiliferous limestone.|
40932|Yanawe Formation|70546|5|Briefly described|Map Legend|Silurian|Silurian|Includes three unnamed members; siliceous or tuffaceous mudstone, quartz lithic volcanic sandstone and arkosic-volcanic rich sandstone.||Douro Group|Includes Werong Breccia Member, Humewood Volcanic Sandstone Member, Euralie , Gums Road Limestone Members Hulong Conglomerate Member, Tullerah Sandstone Member, Excursion Creek Sandstone Member||Volcaniclastic sandstone, siltstone and mudstone, pebble to boulder conglomerate and breccia, siliceous volcanic mudstone, calcareous mudstone and lenses of fossiliferous limestone.|
40932|Yanawe Formation|71656|5|Briefly described|p12 Fig.2, p19, p21-23|Ludlow|Wenlock|Corals and stromatoporoids are included in description of this unit.||Top of Douro Group|Includes Euralie Limestone  Member, Gums Road Limestone Member.|Overlies Laidlaw Volcanics and underlies Silverdale Formation and Bowspring Limestone Member.|Fossiliferous strata.|
40932|Yanawe Formation|73215|5|Briefly described|p994, 1003|||Yass Syncline.||Douro Group.||Overlies Laidlaw Volcanics. Is overlain by Hattons Corner Group.||
73418|Yancannia Formation|66623|2|Defined|pp98-101, pp108-109.|Early Ordovician|Late Cambrian|Defined in this study. Formerly part of Wonominta Beds (Warris 1967). Correlated with Jeffreys Flat and Easter Monday Formations. Unfossiliferous, highly weathered and recessive. Channels contain mud flows with cobbles of older rocks, including Ponto Group. White quartz veins common.||Unit in Warratta Group||Is unconformably overlain by Rolling Downs Group.|Well-sorted and fine-grained, weakly cleaved metamudstone (slate and shaly slate), lesser metasiltstone and minor metasandstone.|
73418|Yancannia Formation|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Regularly spaced continuous linear trends lie within broad zones of low to moderate magnetic intensity which are elongated in west-northwest to northwest directions.||||Is overlain by Easter Monday Formation.||
73418|Yancannia Formation|67105|6|Mentioned|p661|||||Warratta Group.||||
73418|Yancannia Formation|67210|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Warratta Group.||Is overlain by Rolling Downs Group.|Weakly cleaved slate and minor metasandstone, showing original bedding and facing in some outcrops; regionally metamorphosed to lower greenschist or prehnite-pumpellyite facies.|
73418|Yancannia Formation|67211|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Warratta Group.|||Weakly cleaved slate and minor metasandstone, showing original bedding and facing in some outcrops; regionally metamorphosed to lower greenschist or prehnite-pumpellyite facies.|
73418|Yancannia Formation|67322|5|Briefly described|p13; Fig.5|Cambrian|Cambrian|(Mills, in Greenfield et al. 2010). Age is determined from p20 Fig.5 (Strat. column). Restricted to base of Yancannia Range.||Of the Warratta Group.|||Mostly mudstone or siltstone of low metamorphic grade.|22-FEB-18
73418|Yancannia Formation|69002|6|Mentioned|p8, p13, p15, Map 1b|Ordovician|Cambrian|Suggested Cambro-Ordovician age inferred from the distribution of this formation on map 1b.||||||28-NOV-13
73418|Yancannia Formation|69042|5|Briefly described|map|Ordovician|Cambrian|Probably part of the unit shown as YF - Warratta Group. Probably not the unit shown as YF2. Thomson Orogen?  Zones of low magnetic intensity. Sediments/metasediments, Yancannia area. Age shown as ?Ordovician-Devonian.||||||04-NOV-13
73418|Yancannia Formation|69043|6|Mentioned|p11|||Thomson Orogen.||||||
73418|Yancannia Formation|69541|5|Briefly described|p654|Late Cambrian|Late Cambrian|Cleaved; prehnite-pumpellyite to lower greenschist metamorphic grade.||Unit in Warratta Group.|||Mudstone, siltstone; minor sandstone.|
73418|Yancannia Formation|69961|5|Briefly described|Map legend|Cambrian|Cambrian|No outcrop in map area.||Unit in Warratta Group.|||Weakly cleaved slate and minor metasandstone, showing original bedding and facing in some outcrops; regionally metamorphosed to lower greenschist or prehnite-pumpellyite facies.|
73418|Yancannia Formation|70749|5|Briefly described|p42-43|Ordovician|Cambrian|Yancannia area. Shelf to deep-marine deposits.|||||Variably deformed and metamorphosed siltstone, sandstone and mudstone.|
73418|Yancannia Formation|71263|5|Briefly described|p15-20, p22-p24|Early Ordovician|Late Cambrian|Geological province: Thomson Orogen. Deformed by Benambran (461-428 Ma) through Kanimblan Alice Springs orogenies. U-Pb dating of detrital zircons provide maximum depositional age of 497+\-13 Ma. Deposition is inferred to be in a proximal, low-energy, deep-marine environment. Characterised by negative aeromagnetic anomalies. Includes pyrrhotite mineralisation.||Of Warratta Group.|||Deformed fine-grained turbiditic metasediments, with considerable quantities of detrital micas, feldspars and lithic fragments|29-MAY-19
73418|Yancannia Formation|71965|4|Described|p897-898|||Geological province: Thomson Orogen. Depositional environment: distal, outer shelf. Outcrops and drillhole intersections confirm presence to the south in the White Cliff Area, following N-S trending magnetic lineations that define the Warratta Group.||Unit of Warratta Group.||Correlable with Easter Monday Formation.|Weakly cleaved metamudstone, lesser metasiltstone and minor metasandstone.|
73418|Yancannia Formation|72522|4|Described|p3, p5 Tb.1.1, p112-118.|Furongian|Fortunian|Thomson Orogen. Maximum depositional age, U-Pb SHRIMP from sample in BH2A, ~40km SE of surface outcrops. Isotopic ratio used for this age is 206Pb/238U (204Pb-corrected). Minimum age from possible correlation with Easter Monday Formation (depositional age 497+/-2.6 Ma).|533 +/- 8 Ma (2 sigma) maximum depositional age|Warratta Group||Of Warratta Group (p112, p114) or may correlate with Warratta Group (p113)?|Dated sample is medium-grained metasandstone.|
73418|Yancannia Formation|73177|4|Described|p1097-1099, 1103-1113, 1114 Fig.16|Late Cambrian|Late Cambrian|See also p1115 Fig.17, 1118. Greenfield, Gilmore and Mills (2010). Previously described as part of the Wonominta Beds (Warris, 1967 and others). Southern Thomson Orogen. Located ~120 km SE of Tibooburra, adjacent to the Olepoloko Fault. Deposition in a proximal, low-energy, deep-marine environment.This MDA is based on a tuff in the correlative Easter Monday Formation. Deformation described in great detail; deforming events and their dates are listed.|497 +/- 13 Ma (max deposition age).|Warratta Group.||Correlative of Jeffreys Flat and Easter Monday Formations.|Deformed, fine-grained, quartz and lithic-rich, turbiditic low-grade metasediments; well-sorted, cleaved metamudstone with lesser amounts of metasiltstone and minor metasandstone.|
76100|Yandenberry Formation|66623|2|Defined|pp74-75, p80 Fig. 21, pp93-94.  |Middle Cambrian|Middle Cambrian|Defined in this study. Formerly part of Wonominta beds (Warris 1967). Incorporates former Belah and Yandenberry beds (Stevens et al. 2000). No fossils identified. Subject to tight isoclinal folding. Exposed over 50 km strike length and up to 3.5 km wide.||Unit in Ponto Group.||Overlies Koonenberry Formation. Faulted contact with Teltawongee Group. Intruded by minor gabbros of Bittles Tank Volcanics.|Turbiditic micaceous metasandstones, metasiltstones and metamudstones (phyllites); a single outcrop of very fine-grained, massive to locally strongly banded/laminated, siliceous cherty tuff.|
76100|Yandenberry Formation|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Ponto Group.|||Turbiditic, micaceous, metasandstone, metasiltstone and metamudstone (phyllite) and very rare felsic tuff horizons; metasandstone units make up about half of the type section.|
76100|Yandenberry Formation|67322|5|Briefly described|p11; Fig.5|Cambrian|Cambrian|First defined by Mills, in Greenfield et al. (2010). Unfossiliferous; age from parent unit. Occurs in the Kayrunnera-Koonenberry region.||Of the Ponto Group.||Overlies Koonenberry Formation.||22-FEB-18
76100|Yandenberry Formation|69961|5|Briefly described|Map legend|Cambrian|Cambrian|The two facies assemblages are mapped separately.||Unit in Ponto Group.|||Turbiditic, micaceous metasandstone, lesser metasiltstone and metamudstone (phyllite), very rare felsic tuff horizons; thin bands of buff to yellow-brown, massive to locally strongly banded/laminated, siliceous cherty tuff.|
76100|Yandenberry Formation|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|||Ponto Group|||Turbiditic, micaceous metasandstone, metasiltstone and metamudstone (phyllite) and very rare felsic tuff horizons; metasandstone units make up about half of the type section.|
23286|Yandilla Volcanics|22638|4|Described|p43|||Previously mapped as Jindalee Group||||||
23286|Yandilla Volcanics|22857|4|Described|p452 App.1, Tb.A1.6|Silurian|Silurian|High-K meta-andesite, metabasalt, metamorphosed tuffs. Max. thickness: >500m. ||||||
23286|Yandilla Volcanics|44192|5|Briefly described|Map Legend||Llandoverian|||||||
27260|Yandyguinula Member|22857|5|Briefly described|p474 App.1 Tb.A1.6|Silurian|Silurian|Of Captains Flat Formation. Alternating thin beds of siltstone and shale. Max. thickness: 60m. Geological Province: Captains Flat-Goulburn Trough.||||||
27260|Yandyguinula Member|32820|6|Mentioned|p3|||Hoskinstown Gp.||||||
27260|Yandyguinula Member|36413|2|Defined|p67|Late Silurian|Late Silurian|||||||
27260|Yandyguinula Member|36414|5|Briefly described|map legend|Pridolian|Pridolian|Of Captains Flat Formation, Hoskinstown Group. Alternating thin beds of siltstone and shale. GSNSW map code: Sfy.||||||
27260|Yandyguinula Member|37727|5|Briefly described|p95|||||||||
27260|Yandyguinula Member|40328|5|Briefly described|p181|||||||||
27260|Yandyguinula Member|48878|4|Described|p.9,Pl.3||Late Silurian|Near base of Captains Flat Formation. Upper Silurian. See page, 7. "Yandy Member" - Defn. on Tech.File I/55-16.||||||
27260|Yandyguinula Member|71069|5|Briefly described|p105 |||Obsolete name, now just included as part of the Captains Flat Formation.||Captains Flat Formation|||Thin bedded turbidite sequence.|
73399|Yanna Tank Formation|66623|2|Defined|p225, pp230-232, pp269-270.|Permian|Permian|Defined in this study. Correlated with Urana and Cape Jervis Formations. Contains glacial drop-stones and erratics; polished and striated quartzite boulders, and black manganiferous chert from ?Victoria. Glaciated Devonian pavement and monadnocks occur.||||Capped by Cordillo Silcrete.|Poorly exposed, weakly consolidated, deeply weathered gritty sandstones with occasional large, isolated boulders. Drillholes reveal fine-grained yellow sands, dark grey-maroon siltstones and claystones, and uncommon solid pebbles.|29-MAY-13
73399|Yanna Tank Formation|69001|6|Mentioned|p14, p62|||Periglacial sedimentary rocks. Of the southern Koonenberry Belt.||||||
70042|Yard coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within Lambton Formation (Newcastle Coal Measures).||||||
70042|Yard coal seam|68711|5|Briefly described|p119, p116 Tbl 4|||Informal unit. ||Within Lambton Formation||||
33420|Yarnel Volcanics|24417|3|Fully described|p64|Early Devonian|Late Silurian|Of Ootha Group.  Includes Bogandillian Chert Member.  Underlain by Manna Conglomerate.  Max. thickness: 400m.||||||
33420|Yarnel Volcanics|50554|5|Briefly described|Map legend|Devonian|Silurian|Of the Ootha Subgroup (Derriwong Group).  Rhyolitic tuff.||||||
33420|Yarnel Volcanics|60009|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Ootha Group. Overlies: Manna Conglomerate.||||||13-JUL-04
33420|Yarnel Volcanics|70751|6|Mentioned|p17, p21|||Canbelego-Mineral Hill Volcanic Belt.||Ootha Group||||
29299|Yarra Yarra Creek Group|9548|5|Briefly described|Map Legend|Zlichovian|Pragian|Includes: Gleninga Formation, Inverleith Sandstone, Daalboro Sandstone, Myamely Sandstone, Gwando Siltstone, Ewolong Formation.||||||
29299|Yarra Yarra Creek Group|22768|5|Briefly described|Fig16.8p168,171|Emsian|Pragian|||||||
29299|Yarra Yarra Creek Group|22831|4|Described|p52|Devonian|Devonian|||||||31-OCT-13
29299|Yarra Yarra Creek Group|22857|5|Briefly described|p444 App.1, Tb.A1.6|Emsian|Pragian|Unconformably overlies Kopyje Group. Max. thickness: 1.8m. Geological Province: Darling Basin. See also p168 Fig. 16.8.||||||
29299|Yarra Yarra Creek Group|23309|6|Mentioned|p390|||||||||
29299|Yarra Yarra Creek Group|23522|5|Briefly described|p249 Fig 5|Emsian|Lochkovian|||||||
29299|Yarra Yarra Creek Group|23898|6|Mentioned|p287|Emsian|Pragian|||||||
29299|Yarra Yarra Creek Group|24417|4|Described|p77|Early Devonian|Early Devonian|Of Pogson and Felton (1978).||||||
29299|Yarra Yarra Creek Group|35287|5|Briefly described|p14|||||||||
29299|Yarra Yarra Creek Group|36066|5|Briefly described|p4|||||||||
29299|Yarra Yarra Creek Group|40365|6|Mentioned|p241|||||||||
29299|Yarra Yarra Creek Group|41821|6|Mentioned|p11 Fig.5|||Occurs in Bobadah and Gindoono sheet areas||||||
29299|Yarra Yarra Creek Group|42144|5|Briefly described|p604|||||||||
29299|Yarra Yarra Creek Group|42449|4|Described|p23|||||||||
29299|Yarra Yarra Creek Group|42456|6|Mentioned|p10|||||||||
29299|Yarra Yarra Creek Group|42521|5|Briefly described|p16|||||||||
29299|Yarra Yarra Creek Group|42566|3|Fully described|p100|||||||||
29299|Yarra Yarra Creek Group|42568|5|Briefly described|Map legend|Pragian|Pragian|||||||
29299|Yarra Yarra Creek Group|43089|5|Briefly described|Map Legend|||||||||
29299|Yarra Yarra Creek Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
29299|Yarra Yarra Creek Group|43441|5|Briefly described|20, 28|Early Devonian|Early Devonian|||||||08-JAN-10
29299|Yarra Yarra Creek Group|44093|5|Briefly described|p172 App. 1|Early Devonian|Late Silurian|In the Mineral Hill Zone. Geological Province: Lachlan Fold Belt.||||||
29299|Yarra Yarra Creek Group|44160|5|Briefly described|Map Legend|Emsian|Lochkovian|||||||
29299|Yarra Yarra Creek Group|50554|5|Briefly described|Map legend|Devonian|Devonian|Includes the Darbeys Ridge Conglomerate.||||||
29299|Yarra Yarra Creek Group|60008|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Sediments and/or volcanics.||||||08-JUL-04
29299|Yarra Yarra Creek Group|60009|5|Briefly described|Map Legend|Pragian|Pragian|Includes: Darbys Ridge Conglomerate.||||||13-JUL-04
29299|Yarra Yarra Creek Group|61894|6|Mentioned|p179 Fig.3|||||||||
29299|Yarra Yarra Creek Group|62569|6|Mentioned|p608|Pragian|Pragian|||||||
29299|Yarra Yarra Creek Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
29299|Yarra Yarra Creek Group|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. Shows significant sericite alteration. See also p62, p67, p145, p146, p364, App A-VI 3.||||||
29299|Yarra Yarra Creek Group|66197|5|Briefly described|p634, p635 Fig.5a|Emsian|Lochkovian|Jemalong Trough. Shallow marine and fluvial clastics. Unconformably overlies the Kopyje and Derriwong Groups.||||||14-MAR-12
29299|Yarra Yarra Creek Group|67416|6|Mentioned|p85-86|Lochkovian|Lochkovian|||||Paraconformably overlies Talingaboolba Formation.|Coarse pebbly sandstones, sandstones, siltstones, and minor local limestone.|
29299|Yarra Yarra Creek Group|70751|5|Briefly described|p4, p6, p12, p15|Emsian|Lochkovian|Cobar Superbasin, Winduck Shelf.||Cobar Supergroup|Includes the Gleninga Formation, Inverleith Sandstone, Daalboro Sandstone, Myamley Sandstone, Gwando Siltstone and Ewolong Formation.|||24-SEP-19
29299|Yarra Yarra Creek Group|71039|6|Mentioned|p6, p8, p14, p24|Devonian|Silurian|There is very little petrographic data for this group. Sherwin (1996) described wide spread folding and extensive grain-suturing and recrystallisation of quartz within regional fold hinges.|||Includes the Jerula Limestone Member.|||10-MAR-23
29299|Yarra Yarra Creek Group|71040|5|Briefly described|p4 Fig.2, p9, p11, p12 Fig.7, p13-14|Emsian|Lochkovian|See also p17, p26, p31. Yarra Yarra Creek and Murda Synclines. Post-dates the Bindian (=Bowning) Orogeny; folded by Tabberabberan (and/or Kanimblan) Orogeny.|c.410 Ma.|||Unconformably overlies Kopyje Group.||
29299|Yarra Yarra Creek Group|71693|5|Briefly described|Map legend.|Devonian|Devonian||||||Cross-bedded, medium- and coarse-grained, pebbly quartz-lithic to quartzose sandstone, pebble to cobble conglomerate; ripple cross-laminated, fine-grained quartz sandstone, siltstone, claystone, minor algal limestone, red siltstone.|
29299|Yarra Yarra Creek Group|72908|6|Mentioned|p4|Early Devonian|Silurian|Winduck Shelf.||||||
29299|Yarra Yarra Creek Group|72958|6|Mentioned|p11|Emsian|Lochkovian|Cobar Basin. Nymagee area.||Cobar Supergroup|Gleninga Formation, Jerula Limestone Member, Inverleith Sandstone, Daalboro Sandstone, Myamley Sandstone, Gwando Siltstone, Ewolong Formation|||
76974|Yarrahapinni Monzogranite|69639|5|Briefly described|p3, p118, p128, p223-p224|Triassic|Triassic|New England Orogen. Misspelt as the Yarraphapinni Monzogranite on p118 and p128. Sample locality, petrography, and geochronology is described.|228.4 +/- 1.7 Ma|||||
76974|Yarrahapinni Monzogranite|71628|3|Fully described|p17: 2, 13, 40, 42-46|||Originally Yarrahapinni Adamellite (Leitch et al., 1971). Named after a local mountain. Occurs ~4 km W of Scotts Head and ~5 km SE of Macksville. Crops out as several masses (locations described). Lithology and mineralogy detailed; geochemistry described. Is associated with significant Mo, Ag, As and Sb mineralisation (prospects named); morphological types described.|228.4 +/- 1.7 Ma (SHRIMP: Cross and Blevin).|Yarrahapinni Suite.||Intrudes Pee Dee beds and Kempsey beds.|Medium-grained, equigranular to porphyritic, leucocratic biotite-hornblende granodiorite-monzogranite to biotite leucomonzogranite. I-type.|
73986|Yarrahapinni Suite|71628|5|Briefly described|p17-43|||||Carrai Supersuite.|Yarrahapinni Monzogranite.|||
39264|Yarralumba Ignimbrite Member|50613|2|Defined|p213, p230 App. 1, p210 Fig. 4|Namurian|Namurian|of the Willuri Formation.  Volcanic member of the Gunnan package (informal grouping of stratigraphically recognisable distinctive, mappable units). Overlies Tranquille Dacite Member; underlies Taggarts Mountain Ignim.Member.  Max. thic: 175m;>135 in type||||||22-FEB-05
77322|Yarralumba Rhyolite|68005|5|Briefly described|p139.|Stephanian|Namurian|||Unit in Willuri Formation.|||Beige, pink or grey, rhyolitic ignimbrite, agglomerate, conglomerate, coarse resedimented rhyolitic sandstone and minor rhyolite flows.|
25666|Yarramanbully Limestone Member|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
25666|Yarramanbully Limestone Member|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
25666|Yarramanbully Limestone Member|38802|4|Described|p115|||||||||
36830|Yarramundi Andesite Member|23859|2|Defined|p242 Appendix 1|Late Permian|Late Permian|See also page 933. Type Locality 390000E, 6745500N. Of Emmaville Volcanics. Geological Province: New England Fold Belt.||||||
36830|Yarramundi Andesite Member|71628|6|Mentioned|p15-9|||||||Is intruded by Bolivia Range Leucomonzogranite.||
79381|Yarranjerry Granite|70777|4|Described|p2-p4, p32-p37, p81, p96|Lochkovian|Lochkovian|Lachlan Orogen. Anadditional age of 411 +/- 11 Ma is provided (this volume); Ages are derived from SHRIMP U-Pb dating and are interpreted to be the ages of magmatic crystallisation. Characterised by low magnetic susceptibility. Petrography, zircon description and U-Pb isotopic results are provided in detail. S-type geochemistry.|414.3 +/- 2 Ma (Zircon, this record)||||Pale pink, medium-grained leucocratic granite that contains clots of aggregated biotite.|
79381|Yarranjerry Granite|72082|6|Mentioned|p4|Devonian|Devonian|||||||
40760|Yarrari Pyroclastic Member|50613|2|Defined|p230, p231|||Of the Willuri Formation.  Volcanic member of the Tulcumba package (informal grouping of stratigraphically recognisable distinctive, mappable units). Age: 307.8+/-3.7Ma (mean). Max. thickness: >310m; 75m in type section.  Geol. Prov: New England Orogen.||||||28-MAR-13
40760|Yarrari Pyroclastic Member|65902|6|Mentioned|p203 Fig.7|Kasimovian|Kasimovian|Of Willuri Formation. Age 307.8 +/- 3.7 Ma.||||||09-MAR-12
34001|Yarras Complex|22571|5|Briefly described|p13|Middle Devonian|Early Devonian|New England Orogen. Birpai terrane. 377 +/- 8 Ma trondjhemite sample.||||||05-NOV-07
34001|Yarras Complex|73264|5|Briefly described|p1390|Late Devonian|Middle Devonian||377+/-9 Ma zircon||||Ophiolite.|
33692|Yarrimbah Formation|23736|5|Briefly described|p15|Early Ordovician|Early Ordovician|||||||
33692|Yarrimbah Formation|24417|3|Fully described|p30|Early Ordovician|Early Ordovician|Formerly included in Nelungaloo Volcanics as "Yarrimbah Chert Member".  Underlain by Nelungaloo Volcanics.||||||
33692|Yarrimbah Formation|60009|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|||||||13-JUL-04
33692|Yarrimbah Formation|61724|3|Fully described|p864 Fig.1, p866|Early Ordovician|Early Ordovician|Fine-grained volcaniclastic rocks; presence of graptolites indicates a deep marine origin. Overlies Nelungaloo Volcanics; unconformably overlain by Goonumbla Volcanics. Max. thickness: up to 600m. See also p868-869.||||||23-SEP-18
33692|Yarrimbah Formation|63121|5|Briefly described|p223, p225 Fig. 2, p226|Ordovician|Ordovician|Contains Ordovician brachiopods (Lingulide); and graptolites in upper part - laminated siliceous mudstones. Age is Lancefieldian to Bendigonian. In the "Yarrimbah" area NW of Parkes, NSW.||||||13-MAR-07
33692|Yarrimbah Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a|Early Ordovician|Early Orodvician|Geol Prov: Junee-Narromine Volcanic Belt, LFB. Consists of volcaniclastic sandstone and conglomerate in lower parts, overlain by silicious mudstone/ chert. Clasts amoung comglomerate, rare limestone with microfossils. See p149-150.||||||07-FEB-11
33692|Yarrimbah Formation|63279|5|Briefly described|p167, p168, p168 Fig. 1, p170 Fig. 3|Bendigonian|Lancefieldian|Supersedes Yarrimbah Chert. Underlain by Nelungaloo Volcanics. Thickness: ~400m. Geol Prov: Junee-Narromine Volcanic Belt. Age from graptolites present in unit. See p172-174.||||||
33692|Yarrimbah Formation|63283|5|Briefly described|p185, p194 Fig. 2|Bendigonian|Early Ordovician|Underlain by Nelungaloo Volcanics. Geological Province: Junee-Narromine Volcanic Belt. Consists of an upward-finning sequence.||||||07-FEB-11
33692|Yarrimbah Formation|63290|6|Mentioned|p397 Fig. 3(b)|Bendigonian|Lancefieldian|Geological Province: Junee - Narromine Volcanic Belt.||||||
33692|Yarrimbah Formation|63291|4|Described|p421, p425|Early Ordovician|Early Ordovician|Underlain by Nelungaloo Volcanics. Age: ~485-481Ma. Geological Province: Junee - Narromine Volcanic Belt. Consists of volcanic conglomerate, corse-grained volcanic sandstone and sedimentary units.||||||
33692|Yarrimbah Formation|63293|5|Briefly described|p467, p468 Fig. 2|Early Ordovician|Early Ordovician|Underlain by Nelungaloo Volcanics. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
33692|Yarrimbah Formation|64015|5|Briefly described|p58 Fig. 1, p59|||||||||
33692|Yarrimbah Formation|67106|6|Mentioned|p673-676, 678-679, 681|||Junee-Narromine Volcanic Belt.||||Unconformably overlies Nelungaloo Volcanics.||
33692|Yarrimbah Formation|67322|5|Briefly described|p22; Fig.5|Floian|Tremadocian|Macquarie Arc. (Sherwin in Lyons et al. 2000, modified from Sherwin et al. 1987). Contains graptolites of late Lancefieldian to mid Bendigonian age. Occurs in the Junee-Narromine region.||||Overlies the Nelungaloo Volcanics. Unconformably overlain by the Goonumbla Volcanics.|Mostly siliceous siltstones; basal conglomerate.|22-FEB-18
33692|Yarrimbah Formation|70278|5|Briefly described|p1611, 1627 Fig.16|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.|c.485-482 Ma.|||Overlies Nelungaloo Volcanics.|Clastic sedimentary rocks.|
33692|Yarrimbah Formation|70684|4|Described|p3, p12, p21, p54-56, p58-61, p74-75|Early Ordovician|Early Ordovician|Junee-Narromine Volcanic Belt. The type locality is a shallow gravel pit just SW of Yarrimbah homestead. Thickness of several hundred metres estimated. Lithologically very similar to Hensleigh Siltstone, and only slightly older. Lancefieldian 3 to Bendigonian 2 age from graptolites (listed). Lithology contrasted with Nelungaloo Volcanics. Measured section through upper part of the Formation.||||Unconformably overlies Nelungaloo Volcanics.|Metre-thick packets of granule conglomerate interbedded with siliceous siltstones and mudstones containing graptolites.|
33692|Yarrimbah Formation|72495|6|Mentioned|p218-219, p222, 227,232|Early Ordovician|Early Ordovician|Outcrops in the core of the Forbes Anticline, which is probably faulted. Most recently described by Simpson et al, 2005 and were further described by Glen et al (2007) and Percival and Glen (2007). Also appears as the Yarrimbah Chert on p227.||||Overlies the Nelungaloo Volcanics.||26-MAR-20
33692|Yarrimbah Formation|73154|5|Briefly described|p77 Fig.3|Early Ordovician|Early Ordovician|Macquarie Arc, Phase 1. Junee-Narromine Belt.|||||Includes conglomerate, intermediate-mafic lava, sandstone.|
23300|Yathella Serpentinite|22519|5|Briefly described|p6|||||||||
23300|Yathella Serpentinite|22831|3|Fully described|p 24-25|Early Carboniferous|Ordovician|||||||
23300|Yathella Serpentinite|22857|5|Briefly described|p414 App. 1 Tb. A1.5|||Chlorite with minor antigorite and magnetite.||||||
23300|Yathella Serpentinite|24417|6|Mentioned|p40|||||||||
23300|Yathella Serpentinite|43441|4|Described|15,16|||Boundary with Girilambone Group may be fault or stratigraphic. Age: ?Late Ordovician||||||08-JAN-10
23300|Yathella Serpentinite|44160|5|Briefly described|Map Legend||Darriwilian|||||||08-JAN-10
38118|Yegi Conglomerate|61964|3|Fully described|p14 Fig. 4, p103-104|Pridoli|Pridoli|Tog. with Boothumble Fm, forms a transgressive sequence incl. alluvial fan clastics; includes: cobble-pebble conglom., pebbly lithic-qtz sst+ muddy lithic-qtz sst. Unconform.below Tullibigeal Leucitite. Overlain by Rast Gp.  Age: <418.7Ma.||||||20-OCT-08
38118|Yegi Conglomerate|62405|5|Briefly described|Map legend|Early Devonian|Silurian|Of the Bootheragandra Group. Lithic quartz sandstone and matrix-supported cobble conglomerate with metasedimentary and vein quartz clasts.||||||
38118|Yegi Conglomerate|69161|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Bootheragandra Group.|||Lithic quartz sandstone and matrix-supported cobble conglomerate with metasedimentary and vein quartz clasts.|
82539|Yellow Gap Microleucomonzogranite|71628|5|Briefly described|p8: 12-13, 92; p14: 1-2, 17, 31-33|||New name (this study). Originally Yellow Gap Microadamellite (Neilson, 1970 unpublished) and later Yellow Gap Micromonzogranite (Chappell and Bryant, 1994 unpublished). Named after a local geographic feature. Occurs as two to four outcrops covering 6 km2; forms small tors and flat rock pavements. Differing interpretations of relationships with adjacent units are given. Geochemistry described.||Yellow Gap Suite.||Intrudes Wards Mistake Monzogranite. Is intruded by Llangothlin Monzogranite and possibly Oban River Leucomonzogranite. See COMMENTS.|Fine-grained, equigranular, biotite K-feldspar-rich leucomonzogranite, rarely leucosyenogranite. I-type.|
82709|Yellow Gully Leucosyenogranite|71628|5|Briefly described|p19: 23, 25, 173-176|||New name (after work by Brown et al., 2007) for two bodies of felsic granite 9 km SSW of Rivertree. They were previously included in Cullens Creek Granite by Thomson (1973, 1976) and in Stanthorpe Monzogranite by Brown et al. (2007, 2014). Named after a local watercourse. Lithology and mineralogy detailed. Geochemistry described.||Yellow Gully Suite.||Intrudes Razorback Creek Mudstone and Drake Volcanics.|Medium- to coarse-grained biotite syenogranite with ferromagnesian-free and granophyric variants. I-type.|
30041|Yellowmans Creek Formation|22529|5|Briefly described|7|Early Devonian|Early Devonian|||||||
30041|Yellowmans Creek Formation|22590|6|Mentioned|Fig3 P754||Lochkovian|Actually spelt Yellowmans Ck Formation||||||
30041|Yellowmans Creek Formation|22857|4|Described|p476 App.1 Tb.A1.6|Lochkovian|Lochkovian|Of the Kandos Group. Shale, mudstone, arenite. Max. thickness: 500m. Geological Province: Capertee Rise. ||||||
30041|Yellowmans Creek Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Kandos Group.||||||
30041|Yellowmans Creek Formation|23170|2|Defined|p130|Middle Devonian|Early Devonian|of Kandos Group. Age: U/Pb SHRIMP Zircon date:" 418.8 +/-2.6 Ma.||||||
30041|Yellowmans Creek Formation|23522|5|Briefly described|p248 Fig 4|Lochkovian|Lochkovian|||||||
30041|Yellowmans Creek Formation|43188|4|Described|p207,Table 3 p209|Lochkovian|Lochkovian|Type section location given. Age middle Lochkovian. Of Kandos Group.||||||
30041|Yellowmans Creek Formation|44093|5|Briefly described|p212 App. 1|Early Devonian|Early Devonian|Of the Kandos Group. Geological Province: Lachlan Fold Belt.||||||
30041|Yellowmans Creek Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cudgegong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
30041|Yellowmans Creek Formation|73299|6|Mentioned|p1096 Fig.3, p1100 Fig.5|Early Devonian|Early Devonian|Capertree High.||||||
30523|Yennora Granite|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Batholith.||||||
30523|Yennora Granite|23170|4|Described|p219|Early Devonian||of Yeoval Batholith.||||||
26246|Yeo Yeo Rhyodacite Member|22638|5|Briefly described|p31|||Of the Frampton Volcanics.||||||24-AUG-04
26246|Yeo Yeo Rhyodacite Member|22857|5|Briefly described|p452 App.1, Tb.A1.6|Silurian|Silurian|Of the Frampton Volcanics. Notable tuff unit. Geological Province: Edge of Tumut Trough.||||||
26246|Yeo Yeo Rhyodacite Member|35070|6|Mentioned|p74|||||||||
26246|Yeo Yeo Rhyodacite Member|35608|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Late Silurian||||||
26246|Yeo Yeo Rhyodacite Member|35609|2|Defined|p77|Late Silurian|Middle Silurian|Middle to Late Silurian||||||
26246|Yeo Yeo Rhyodacite Member|39626|6|Mentioned|p276|||||||||
26246|Yeo Yeo Rhyodacite Member|44192|5|Briefly described|Map Legend||Llandoverian|||||||
30531|Yeoval Complex|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|of Yeoval Batholith.||||||
30531|Yeoval Complex|23170|3|Fully described|p215|Early Devonian|Early Devonian|of Yeoval Batholith.||||||
30531|Yeoval Complex|24519|6|Mentioned|p90|||Of the Yeoval Batholith, eastern side.||||||
30531|Yeoval Complex|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Yeoval Batholith.||||||
30531|Yeoval Complex|66713|5|Briefly described|p13|Eifelian|Emsian|75 km NNW of Orange. In the Boggy Plains Supersuite. Contains Cu-Mo mineralisation. 3 U-Pb SHRIMP zircon ages: 397+/-4, 398+/-4 and 399+/-4 Ma (Black, 1998 cited in Wyborn et al., 1999).||||||
30531|Yeoval Complex|68003|5|Briefly described|p24 Fig.3-e, p142. |Pragian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion. Part of the Yeoval Batholith.||||Intrudes Tantitha Intrusive Complex.|Pink microgranite, biotite-ferrohastingsite granite, red biotite microgranite.|
30531|Yeoval Complex|68004|5|Briefly described|p117.|Early Devonian|Early Devonian|Mineral potential and level of certainty are discussed.|||||A fractionated, I-type, felsic and oxidised intrusive complex.|
30531|Yeoval Complex|73179|6|Mentioned|p1152|Eifelian|Emsian|Lachlan Orogen, eastern. Geochron from Black (1998).|397 +/- 4 Ma, 398 +/- 4 Ma, 399 +/- 4 Ma||||Includes granite.|
31486|Yeoval Suite|22768|6|Mentioned|p178|||||||||
31486|Yeoval Suite|22857|5|Briefly described|p178|Early Devonian|Early Devonian|Of the Boggy Plains Supersuite.||||||
31486|Yeoval Suite|23549|5|Briefly described|p529|||Of the Boggy Plain Supersuite.  Has considerable mineralisation.||||||
31486|Yeoval Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains the Obley and Yeoval Granites.||||||08-FEB-05
31486|Yeoval Suite|44093|5|Briefly described|p180 App. 1|Early Devonian|Late Silurian|Orogenic granite. Geological Province: Lachlan Fold Belt.||||||
31486|Yeoval Suite|66713|6|Mentioned|p2 Fig.1 |||||||||
31486|Yeoval Suite|69564|6|Mentioned|p3|||Lachlan Orogen.||||||
31486|Yeoval Suite|70036|5|Briefly described|Map legend|Devonian|Devonian|Lachlan Fold Belt. |||||Includes granite.|
23307|Yerna Granite|22638|4|Described|p77||Late Devonian|Previously "Gladstone Granite".||||||
23307|Yerna Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
23307|Yerna Granite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
25672|Yessabah Limestone|22736|6|Mentioned|p611 Fig2||Permian|||||||
25672|Yessabah Limestone|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Macleay Group. Geological Province: Barnard Basin.||||||09-MAR-06
25672|Yessabah Limestone|23720|5|Briefly described|Map Legend|||Of Macleay Group.  Bioclastic crinoidal limestone and calcareous mudstone.||||||15-DEC-04
25672|Yessabah Limestone|24124|5|Briefly described|p3|||||||||
25672|Yessabah Limestone|29990|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25672|Yessabah Limestone|30911|6|Mentioned|Map legend|Permian|Permian|||||||
25672|Yessabah Limestone|31802|6|Mentioned|p143|||L.Permian. Unconformity||||||
25672|Yessabah Limestone|31806|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25672|Yessabah Limestone|32671|6|Mentioned|Map legend|Permian|Permian|||||||
25672|Yessabah Limestone|32672|6|Mentioned|p675|||||||||
25672|Yessabah Limestone|32943|6|Mentioned|p105|||||||||
25672|Yessabah Limestone|32944|6|Mentioned|p708|||Se also P709||||||
25672|Yessabah Limestone|32945|6|Mentioned|p88|||Permian||||||
25672|Yessabah Limestone|34293|2|Defined|p48|Devonian|Devonian|Refers De Koninck (1898)||||||
25672|Yessabah Limestone|34556|4|Described|p265|||Permian||||||
25672|Yessabah Limestone|34590|6|Mentioned|p300|||Permian||||||
25672|Yessabah Limestone|34692|5|Briefly described|p188|||||||||
25672|Yessabah Limestone|35062|6|Mentioned|p279|||||||||
25672|Yessabah Limestone|35862|6|Mentioned|p277|||||||||
25672|Yessabah Limestone|36042|6|Mentioned|Fig.7|||||||||
25672|Yessabah Limestone|36961|6|Mentioned|Fig.5|||||||||
25672|Yessabah Limestone|38685|6|Mentioned|p27|||Geological Province: New England Fold Belt||||||
25672|Yessabah Limestone|38916|6|Mentioned|p346|||||||||
25672|Yessabah Limestone|39287|6|Mentioned|Fig. 2.2|||||||||
25672|Yessabah Limestone|40246|6|Mentioned|p173|||||||||
25672|Yessabah Limestone|40590|6|Mentioned|p333|||Mention P338||||||
25672|Yessabah Limestone|41347|6|Mentioned|p368|||||||||
25672|Yessabah Limestone|41348|5|Briefly described|Map legend|Permian|Permian|Of the Macleay Group.||||||16-DEC-04
25672|Yessabah Limestone|42547|5|Briefly described|p39|||||||||
25672|Yessabah Limestone|42866|5|Briefly described|Table 2, P12|||||||||
25672|Yessabah Limestone|43017|5|Briefly described|p376|||||||||
25672|Yessabah Limestone|43018|6|Mentioned|p390|||||||||
25672|Yessabah Limestone|43385|14|Not recorded|p179,180||Sakmarian|SH56-10, SH 56-14||||||
25672|Yessabah Limestone|43475|14|Not recorded|p553||Permian|||||||
25672|Yessabah Limestone|43479|14|Not recorded|p162||Carboniferous|||||||
25672|Yessabah Limestone|43755|6|Mentioned|Fig.1,p548||Permian|||||||
25672|Yessabah Limestone|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|See also p232 Appendix 1. Geological Province: New England Fold Belt.||||||
25672|Yessabah Limestone|44450|5|Briefly described|p24|Early Permian|Early Permian|Of Macleay Group. Underlying unit Youdale Formation. Geological Province: Hastings Block.||||||
25672|Yessabah Limestone|47056|6|Mentioned|Fig.2 P523|||||||||
25672|Yessabah Limestone|47059|4|Described|p146|||Age earliest Permian||||||
25672|Yessabah Limestone|48600|14|Not recorded|p30|||Anidanthus springsurensis found.||||||
25672|Yessabah Limestone|63832|5|Briefly described|p131 fig 2|Artinskian|Artinskian|Northern Hastings Block, Southern New England Fold Belt.|||||Fluvial sandstones, conglomerates and commonly carbonaceous mudrocks with plant fossils. Alluvial facies and pyroclastic rocks underlie glacial deposits of C3.|14-DEC-17
25672|Yessabah Limestone|64631|5|Briefly described|p44 Fig.2.|Artinskian|Artinskian|Southern New England Fold Belt: northern Hastings Block. Biostratigraphic age control for base and top.||||Overlies Youdale Formation. Is overlain by Warbro Formation.||
25672|Yessabah Limestone|65317|6|Mentioned|p635, p634 Fig.13|||Also mis-spelt as Yesabah Limestone, p635.||||||23-APR-12
25672|Yessabah Limestone|70939|6|Mentioned|p825-826, p828-831, p833, p835|Permian|Permian|||||||
31670|Yewrangara Suite|42726|5|Briefly described|Map Legend||Middle Devonian|||||||
31670|Yewrangara Suite|44093|5|Briefly described|p202 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31670|Yewrangara Suite|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes the Yewrangara and Blackmans Creek Granites, and an upper unnamed units of biotite leucogranite and microgranite.||||||
31670|Yewrangara Suite|68592|2|Defined|p1482-9, p1527-41|Early Devonian|Early Devonian|Yacopetti (1987), after Yewrangara property; published by Chappell et al. (1991). Subsequently modified by Blevin (2011) to include Blackmans Creek Granite; and again here to include two small, unnamed leucocratic granitoids referred to by Yacopetti (1987) as the Fire Trail Microgranites. Plutons crop out as large tors and whalebacks on prominent hills. Geochemistry described. Hosts Reids Flat Tin Prospect. Alluvial gold, adjacent to Blackmans Creek Granite, is of uncertain origin. Has been a source of local road materials.||Unit in Keverstone Supersuite.|Includes Yewrangara and Blackmans Creek Granites.|Intrudes Adaminaby Group; Blanket Flat, Spring Road and Bigga Granites; Goonoonglah Microdiorite and (probably) Sentry Box Granite.|Cream to grey, medium- to occasionally coarse-grained, massive to mildly foliated, equigranular to weakly porphyritic, hornblende-biotite granite, arfvedsonite-biotite granite and biotite granite; minor biotite leucogranite and microgranite. A-type.|
31670|Yewrangara Suite|70192|5|Briefly described|Map Legend|Emsian|Emsian|Includes one unnamed unit of fine-medium grained, massive, equigranular biotite leucogranite and microgranite, with high K and Th, variable U. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Blackmans Creek Granite, Yewrangara Granite and one unnamed unit.|||
31670|Yewrangara Suite|70544|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed unit of fine-medium grained, massive, equigranular biotite leucogranite.|||Includes Blackmans Creek Granite, Yewrangara Granite and one unnamed unit.|||
31670|Yewrangara Suite|71206|6|Mentioned|p373, 377, 387|||Lachlan Fold Belt. Sr/Nd plot.|||Yewrangara Granite.||Aluminous A-type granite.|
23308|Yiddah Formation|22434|6|Mentioned|11 fig 14|Devonian|Silurian|Geol province Lachlan Fold Belt||||||
23308|Yiddah Formation|22638|3|Fully described|p60|Early Devonian|Late Silurian|New name. Probably equivalent to the Combaning Formation.||||||
23308|Yiddah Formation|22857|5|Briefly described|p450 App.1, Tb.A1.6|Early Devonian|Late Silurian|Siltstone, arenite, minor conglomerate and felsic volcanic rocks; contains trilobites, brachiopods, lamellibranchs, corals. Geological Province: Bogan Gate Terrace.||||||
23308|Yiddah Formation|24417|3|Fully described|p65|Early Devonian|Late Silurian|Of Ootha Group.  Overlies the Manna Conglomerate.||||||
23308|Yiddah Formation|44093|5|Briefly described|p178 App. 1|Early Devonian|Silurian|In the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
23308|Yiddah Formation|44192|5|Briefly described|Map Legend|Lochkovian|Ludlovian|||||||
23308|Yiddah Formation|44936|5|Briefly described|Map Legend|Devonian|Silurian|Derriwong Group.||||||
23308|Yiddah Formation|50191|5|Briefly described|p6|Early Devonian|Late Silurian|Of the Derriwong Group.||||||
23308|Yiddah Formation|50385|5|Briefly described|Map Legend|Devonian|Silurian|Of Derriwong Group. Sandstone, siltsone, minor conglomerate||||||
23308|Yiddah Formation|60009|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Ootha Group.||||||13-JUL-04
23308|Yiddah Formation|66197|5|Briefly described|p634, p635 Fig.5b|Early Devonian|Late Silurian|Jemalong Trough. Deep marine shale and sandstone. Underlies the Pullabooka Formation.||||||14-MAR-12
23308|Yiddah Formation|71040|5|Briefly described|p16|Early Devonian|Late Silurian|Currowong Syncline.||Ootha Group.||||
23308|Yiddah Formation|72082|6|Mentioned|p4|Devonian|Silurian|||||||
23308|Yiddah Formation|72084|5|Briefly described|p2, p39, p40 Fig.42, p54|Early Devonian|Late Silurian|Medial-fan turbidite facies deposits overlain by high-energy alluvial fan facies intercalated with minor pyroclastic deposits. Forms hills and ridges.|425.9 +/- 3.7 Ma (Main et al., in prep.).||||Includes poorly sorted, very crystal-rich, quartz-feldspar-garnet, rhyolitic, coarse tuff to lapilli tuff.|
31669|Young Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
31669|Young Suite|44093|5|Briefly described|p187 App. 1|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
31669|Young Suite|44192|5|Briefly described|Map Legend|||||||||
31669|Young Suite|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Hume Park Granite and Young Granodiorite as well as 6 unnamed granitic subunits.||||||
31669|Young Suite|68592|2|Defined|p443,p1225-9, p1232-4, p1239-52, p1262-3|Early Silurian|Early Silurian|See also p73 Tb.5, p139. Chappell et al. (1988, 1991). Named after the Young Granodiorite. Geochemistry detailed. Has close geochemical affinity with volcanics of the Douro Group: thought to be comagmatic with Goobarragandra and Hawkins Volcanics. Yass structural zone: deformation described. Noticeable lack of contact metamorphic aureoles is discussed.||Unit in Bullenbalong Supersuite.|Includes Young Granodiorite, Hume Park Granite.|Intrudes Douro Group. Is intruded by Boggy Plain Supersuite.|Grey, massive, equigranular medium- to coarse-grained muscovite-biotite granite and granodiorite; altered cordierite, microgranitic enclaves, vein quartz. Minor phases include leucogranite, porphyritic microgranite and sheeted rhyolite dykes. S-type.|
31669|Young Suite|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|On Yass and Boorowa 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Young Granodiorite.|||
31669|Young Suite|70540|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Hume Park Granite, Young Granodiorite.|||
31669|Young Suite|70545|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Young Granodiorite|||
31669|Young Suite|70546|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Hume Park Granite|||
70041|Young Wallsend coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within Lambton Formation (Newcastle Coal Measures).||||||
70041|Young Wallsend coal seam|68711|5|Briefly described|p119, p116 Tbl 5|||Informal unit. The Young Wallsend Coal/seam is said to be the combination of Nobbys and Dudley Coal/seams.[???]||Within Lambton Formation||||
23319|Yurammie Granodiorite|22815|4|Described|p72|||||||||
23319|Yurammie Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Candelo Suite.||||||
31726|Yuranigh Limestone Member|13139|5|Briefly described|p9 Fig. 4|Late Ordovician|Late Ordovician|Of the Fairbridge Volcanics.  Geological Province: Western Molong Volcanic Belt.||||||
31726|Yuranigh Limestone Member|22857|5|Briefly described|p426 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Of Fairbridge Volcanics. Bioturbated limestone, calcareous siltstone, lithic arenite; with corals.||||||
31726|Yuranigh Limestone Member|23170|6|Mentioned|p37|||of Fairbridge Volcanics.||||||
31726|Yuranigh Limestone Member|23181|6|Mentioned|Fig.2||Late Ordovician|||||||
31726|Yuranigh Limestone Member|23213|3|Fully described|p18, Fig.10|Gisbornian|Gisbornian|Age: Middle to Late Gisbornian. of Fairbridge Volcanics.||||||
31726|Yuranigh Limestone Member|23214|2|Defined|p26|Late Ordovician|Late Ordovician|Of Fairbridge Volcanics. Type Section - GR 675300 6332800 to GR 674950 66332800.||||||
31726|Yuranigh Limestone Member|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
31726|Yuranigh Limestone Member|23739|4|Described|p215|Late Ordovician|Middle Ordovician|Parent: Fairbridge Volcanics. Geological Province: Lachlan Fold Belt.||||||01-SEP-08
31726|Yuranigh Limestone Member|24215|5|Briefly described|p804 Fig. 3|||Geological Province:  Lachlan Fold Belt.||||||01-SEP-08
31726|Yuranigh Limestone Member|24398|5|Briefly described|p264, p259 Fig. 2|Gisbornian|Gisbornian|Of Fairbridge Volcanics. Geological Province: Lachlan Fold Belt.||||||01-SEP-08
31726|Yuranigh Limestone Member|43640|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Fairbridge Volcanics.||||||01-SEP-08
31726|Yuranigh Limestone Member|43782|5|Briefly described|Map Legend|Gisbornian|Gisbornian|of Fairbridge Volcanics, Kenilworth Group.||||||
31726|Yuranigh Limestone Member|63278|5|Briefly described|p146 Fig. 2a, p152|Late Ordovician|Late Ordovician|Overlain by Reedy Creek Limestone. Geological Province: Molong Volcanic Belt, LFB. Consists of limestone. Upper part of unit includes brachiopods and a section contatning conodonts.||||||07-FEB-11
31726|Yuranigh Limestone Member|63283|6|Mentioned|p194 Fig. 2, p200|Gisbornian|Darriwilian|Of Fairbridge Volcanics. Geological Province: Molong Volcanic Belt. Consists of limestone.||||||07-FEB-11
31726|Yuranigh Limestone Member|63290|5|Briefly described|p397 Fig. 3(b)|Eastonian|Gisbornian|Underlain by Fairbridge Volcanics. Geological Province: Molong Volcanic Belt.||||||
31726|Yuranigh Limestone Member|63293|6|Mentioned|p468 Fig. 2|Eastonian|Gisbornian|Underlain by Wahringa Limestone Member. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
31726|Yuranigh Limestone Member|64295|5|Briefly described|p202|||Of Fairbridge Volcanics. In the Molong area.||||||01-SEP-08
31726|Yuranigh Limestone Member|64826|5|Briefly described|p1041 Tb. 1|Gisbornian|Gisbornian|||||||
31726|Yuranigh Limestone Member|67106|6|Mentioned|p673|||Molong Volcanic Belt.||||||
31726|Yuranigh Limestone Member|67322|5|Briefly described|p23; Fig.5|Late Ordovician|Late Ordovician|Scott and Pogson, in Pogson and Watkins (1998). Age is determined from diverse fossil fauna. Occurs in the North Molong Volcanic Belt.||Of the Fairbridge Volcanics.||Correlative of the upper beds of the Wahringa Limestone Member. Overlain unconformably by the Reedy Creek Limestone.||22-FEB-18
31726|Yuranigh Limestone Member|68592|6|Mentioned|p379|||Macquarie Arc; Bathurst 1:250 000 map area.||Unit in Fairbridge Volcanics.||||
31726|Yuranigh Limestone Member|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 2 volcanic units. Age: ranges from early Darriwilian (Da2) to latest Gisbornian. Shown as Yuranigh Limestone Mbr.||Fairbridge Volcanics||||
31726|Yuranigh Limestone Member|70684|5|Briefly described|p19, p28, p74|Late Ordovician|Late Ordovician|Molong Volcanic Belt.||Fairbridge Volcanics.||||
31726|Yuranigh Limestone Member|70754|5|Briefly described|p449, p450 Fig.2|Gisbornian|Gisbornian|Contemporaneous with upper part of Wahringa Limestone Member. Contains a moderately diverse shelly fauna.||Fairbridge Volcanics.||||
83267|Zero porphyry|73287|5|Briefly described|p663, 666, p670 Tb.6, p674 Fig.11|Llandovery|Llandovery|Post-mineralisation porphyry, also coeval with dated molybdenite in Two-Thirty breccia. Zero porphyries used on p670, named for their similarity with late-, post-mineralisation monzonite porphyries at Northparkes intrusive complex described by Lickfold et al. (2003, 2007). 455.5+/-4.4 Ma U-Pb zircon age interpreted as inherited from Goonumbla Volcanics. Written as zero-porphyry p670, p677-679 and zero porphyry p668 Fig.6, p670, p673 Fig.10, p677-680.|438.8+/-4.4 Ma zircon U-Pb|Two-Thirty intrusive complex|||Variable from aphanitic to crystal crowded monzonite, typically with a gradational contact, highly variable alteration.|
78471|diatreme 78471|69042|6|Mentioned|map legends|||Diatremes. Small normal and reversely magnetised alkali basalt vents, dykes or minor flows. Age shown as ?Permian, Triassic, Tertiary.||||||
78468|granite - high magnetic intensity 78468|69042|6|Mentioned|map legends|Devonian|Silurian|MG. Areas of granite and intermediate intrusives having high magnetic intensity.||||||
78469|granite - low magnetic intensity 78469|69042|6|Mentioned|map legends|Devonian|Silurian|NMG. Areas of granites (both S-type and some I-types) having low magnetic intensity.||||||
78470|granite, gneiss, schist - curved trends, low magnetic intensity 78470|69042|6|Mentioned|map legends|||SPG. Curved magnetic trends of low intensity. Undifferentiated granite, gneiss and schist. Age: ?Devonian.||||||
78465|intermediate igneous - moderate magnetic intensity 78465|69042|6|Mentioned|map legends|Devonian|Ordovician|II. Areas of moderate magnetic intensity. Possible intermediate plutonic/volcanic unit. Age shown as ?Ordovician-Devonian||||||
78459|possible equivalents of  Amphitheatre and Winduck Groups 78459|69042|6|Mentioned|map legends|||PZsn. Possible Devonian siliciclastic sediment equivalents of Amphitheatre and Winduck Groups. Broad featureless areas of very low magnetic intensity sediments.  Age: ?Ordovician - Devonian.||||||
78461|sediments - non-magnetic 78461|69042|6|Mentioned|map legends|Early Devonian|Late Silurian|Dck. Kopyje Group and possible equivalents.||||||
