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
28|Abbey Green Coal|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Apple Tree Flat Subgroup. Equivalent to Lambton Formation (Newcastle Coal Measures).  Geological Province: Sydney Basin||||||
28|Abbey Green Coal|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Apple Tree Flat Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
28|Abbey Green Coal|29942|3|Fully described|p11|||||||||
28|Abbey Green Coal|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. Very widespread Formation.||Lower unit in Apple Tree Flat Sub-group.||Overlies Watts Sandstone. Is overlain by Charlton Formation.|Bright to vestigial coal rich in carbonaceous shale.|
32|Abercorn Granite|30731|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
32|Abercorn Granite|32999|3|Fully described|p44|||||||||
32|Abercorn Granite|34481|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
32|Abercorn Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
32|Abercorn Granite|63633|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Granite, adamellite, porphyritic granite.||||||02-FEB-09
32|Abercorn Granite|64238|5|Briefly described|Map legend|Carboniferous|Carboniferous|Of the Tuglow Suite. Pink to cream, massive, equigranular to medium-grained leucocratic biotite granite.||||||
32|Abercorn Granite|68592|2|Defined|p756, p1754-5, p1768-9, p1771-3|Carboniferous|Carboniferous|Originally the Gurnang Granite (Sylvester, 1966). Renamed Abercorn Granite by Scheibner (1973) after the local Parish. Assigned to the Oberon Supersuite by Chappell et al. (1991) but without a Suite. Included here in the Tuglow Suite due to its proximity and compositional similarity with the Kanangra Granite. Type area defined here. Poor exposure and weathered outcrop. Geochemistry unknown; geophysical properties described. Age assumed on basis of lithological similarity with nearby Kanangra Granite.||Unit in Tuglow Suite.||Intrudes Abercrombie Formation, Warbisco Shale and Mount Fairy Group. Correlative of Kanangra Granite.|Pink-cream, equigranular, medium-grained leucocratic granite; massive and undeformed (post-Kanimbla).|
32|Abercorn Granite|70192|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Cta. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Tuglow Suite|||Leucocratic, medium grained, massive, equigranular, biotite granite.|
32|Abercorn Granite|70543|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||Tuglow Suite|||Leucocratic, medium grained, massive, equigranular, biotite granite.|
39|Aberdare Conglomerate|12597|5|Briefly described|p491, p492 Tb.1|Rhaetian|Rhaetian|N Clarence-Moreton Basin. Basal, high energy fluvial deposits on top of eroded surface of Ipswich and Nymboida Basins.||Unit in Woogaroo Subgroup.|||Conglomerate, coarse lithic sandstone.|
39|Aberdare Conglomerate|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Woogaroo Subgroup||||
39|Aberdare Conglomerate|22757|5|Briefly described|Table5,p10|Late Triassic|Late Triassic|Ipswich-Moreton Basin. 380+ m.||||||
39|Aberdare Conglomerate|23799|5|Briefly described|p46|Late Triassic|Late Triassic|Of Woogaroo Group.  Overlain by Raceview Formation.  Geological Province: Clarence-Moreton Basin.  See also p48 Fig. 3.||||||
39|Aberdare Conglomerate|23843|5|Briefly described|p456 Table 1|Jurassic|Late Triassic|Of Woogaroo Sub-Group. Geological Province:Moreton Basin.  Maximum thickness: 40m.||||||
39|Aberdare Conglomerate|24081|5|Briefly described|p451|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group.  Geological Province: Nambour Basin.||||||
39|Aberdare Conglomerate|29385|6|Mentioned|p82|||Jurassic||||||
39|Aberdare Conglomerate|30086|5|Briefly described|p4|||Triassic. Part of Bundamba Group.||||||
39|Aberdare Conglomerate|30087|4|Described|p3|||See also P4. Unit of Bundamba Group||||||27-SEP-05
39|Aberdare Conglomerate|30302|6|Mentioned|p415|||Refers Staines(1964)||||||
39|Aberdare Conglomerate|30458|6|Mentioned|p1|||Late Triassic (Norian or Rhaetian). See also P39-40.||||||
39|Aberdare Conglomerate|30459|6|Mentioned|p309|||Triassic age||||||
39|Aberdare Conglomerate|30461|6|Mentioned|p100|||||||||
39|Aberdare Conglomerate|30464|6|Mentioned|p4|||Triassic microfossils||||||
39|Aberdare Conglomerate|30465|6|Mentioned|p4|||Triassic microfossils||||||
39|Aberdare Conglomerate|30470|6|Mentioned|p459|||||||||
39|Aberdare Conglomerate|30472|6|Mentioned|p132|||Pollen distribution.||||||
39|Aberdare Conglomerate|30474|6|Mentioned|p251|||Correlation chart P251||||||
39|Aberdare Conglomerate|30475|6|Mentioned|Fig.14.3|||||||||
39|Aberdare Conglomerate|30477|6|Mentioned|p461|||||||||
39|Aberdare Conglomerate|30478|6|Mentioned|p272|||||||||
39|Aberdare Conglomerate|30701|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||11-JAN-10
39|Aberdare Conglomerate|30915|6|Mentioned|p100|||||||||
39|Aberdare Conglomerate|30916|6|Mentioned|p99|||||||||
39|Aberdare Conglomerate|31118|4|Described|p320|||||||||
39|Aberdare Conglomerate|32136|6|Mentioned|p5|||Miospores||||||
39|Aberdare Conglomerate|32176|6|Mentioned|p2|||See also P3&4 & Figs. 2&3||||||
39|Aberdare Conglomerate|32179|6|Mentioned|p3|||Trias.||||||
39|Aberdare Conglomerate|32180|5|Briefly described|p6|||||||||
39|Aberdare Conglomerate|32491|5|Briefly described|p19||Late Triassic|||||||
39|Aberdare Conglomerate|32492|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
39|Aberdare Conglomerate|32801|6|Mentioned|p266|||||||||
39|Aberdare Conglomerate|33381|4|Described|p110|||See also P116-118. Triassic. Overlies Ipswich Coal Measures||||||28-NOV-05
39|Aberdare Conglomerate|33476|6|Mentioned|p99|||||||||
39|Aberdare Conglomerate|34010|6|Mentioned|Cor. chart|||Jurassic||||||
39|Aberdare Conglomerate|34235|6|Mentioned|p91|||||||||
39|Aberdare Conglomerate|34354|6|Mentioned|p3|||See also P12. Triassic.||||||
39|Aberdare Conglomerate|34457|6|Mentioned|p484|||Correlates with Borallon Beds||||||
39|Aberdare Conglomerate|34505|6|Mentioned|p3|||Bundamba Group. See also Figs.8-11||||||
39|Aberdare Conglomerate|35007|6|Mentioned|p76|||||||||
39|Aberdare Conglomerate|35079|6|Mentioned|p424|||||||||
39|Aberdare Conglomerate|35101|6|Mentioned|p51|||||||||
39|Aberdare Conglomerate|36237|6|Mentioned|Map legend|Late Jurassic|Late Triassic|Late Triassic to Early Jurassic||||||
39|Aberdare Conglomerate|36243|6|Mentioned|Table 8A|||||||||
39|Aberdare Conglomerate|36351|6|Mentioned|p373|||||||||
39|Aberdare Conglomerate|36354|4|Described|p371|||||||||
39|Aberdare Conglomerate|36779|6|Mentioned|p7|||||||||
39|Aberdare Conglomerate|36825|6|Mentioned|p12|||||||||
39|Aberdare Conglomerate|36899|6|Mentioned|p1085|||See also P1095.||||||
39|Aberdare Conglomerate|37122|5|Briefly described|Table 1|||||||||
39|Aberdare Conglomerate|37456|6|Mentioned|p268|||||||||
39|Aberdare Conglomerate|37463|6|Mentioned|p483|||||||||
39|Aberdare Conglomerate|37616|6|Mentioned|p33|||||||||
39|Aberdare Conglomerate|37812|6|Mentioned|p657|||||||||
39|Aberdare Conglomerate|38074|5|Briefly described|Table 1|||||||||
39|Aberdare Conglomerate|38076|6|Mentioned|Table 3|||||||||
39|Aberdare Conglomerate|38306|6|Mentioned|p509|||||||||
39|Aberdare Conglomerate|38307|4|Described|p521|||||||||
39|Aberdare Conglomerate|38441|6|Mentioned|Map legend|Rhaetian|Rhaetian|||||||
39|Aberdare Conglomerate|39445|5|Briefly described|Table 10|||||||||
39|Aberdare Conglomerate|39907|6|Mentioned|p8|||||||||
39|Aberdare Conglomerate|39943|6|Mentioned|Table 10A|||||||||
39|Aberdare Conglomerate|40434|6|Mentioned|p25|||||||||
39|Aberdare Conglomerate|40623|5|Briefly described|p34|||||||||
39|Aberdare Conglomerate|41591|5|Briefly described|p19|||||||||
39|Aberdare Conglomerate|41906|3|Fully described|Table 2 P17|||||||||
39|Aberdare Conglomerate|42248|6|Mentioned|p397|||||||||
39|Aberdare Conglomerate|42316|6|Mentioned|p5|||||||||
39|Aberdare Conglomerate|42336|5|Briefly described|p6|||||||||
39|Aberdare Conglomerate|42405|6|Mentioned|Table 3 P.7|||||||||
39|Aberdare Conglomerate|42525|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group (Bundamba Group).||||||27-AUG-08
39|Aberdare Conglomerate|42869|5|Briefly described|Table 1, P33|||Of Woogaroo Subgroup.||||||27-AUG-08
39|Aberdare Conglomerate|42893|5|Briefly described|Fig.2 P7|||||||||
39|Aberdare Conglomerate|42894|5|Briefly described|Fig.1 P20|||||||||
39|Aberdare Conglomerate|43150|5|Briefly described|Map Legend||Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||12-APR-05
39|Aberdare Conglomerate|43736|5|Briefly described|Table 1,p4|||||||||
39|Aberdare Conglomerate|43881|14|Not recorded|p134|||Orange card has 'conglomerate' listed||||||
39|Aberdare Conglomerate|43910|14|Not recorded|p1,3,14,17-18,Fig.2|||||||||
39|Aberdare Conglomerate|43991|6|Mentioned|p46|||Ref.to Wilson 1960||||||
39|Aberdare Conglomerate|43993|14|Not recorded|p97,102|||||||||
39|Aberdare Conglomerate|44026|14|Not recorded|p123|||||||||
39|Aberdare Conglomerate|44091|14|Not recorded|p51||Triassic|||||||
39|Aberdare Conglomerate|44432|14|Not recorded|p53||Late Triassic|||||||
39|Aberdare Conglomerate|44510|2|Defined|p252-7,260,Fig.35-6|||Unconformably overlies Ipswich Coal Measures.||||||
39|Aberdare Conglomerate|44542|14|Not recorded|p36|||||||||
39|Aberdare Conglomerate|44678|14|Not recorded|p1|||||||||
39|Aberdare Conglomerate|44734|14|Not recorded|p5,11-13,19|||Pine Mountain area.||||||
39|Aberdare Conglomerate|44771|14|Not recorded|p1,Fig.3,4|||Part of Bundamba Group.||||||
39|Aberdare Conglomerate|44774|2|Defined|p30,31||Late Triassic|Lowest unit of Bundamba Group. Conformably overlain by Raceview Formation, disconformably overlies Blackstone Formation. Now given formation status.||||||
39|Aberdare Conglomerate|44775|4|Described|p7,9,map 2||Late Triassic|||||||
39|Aberdare Conglomerate|44776|14|Not recorded|p3-5,Figs.3-5||Late Triassic|Member of Bundamba Group.||||||
39|Aberdare Conglomerate|44783|14|Not recorded|p13,16,17|||||||||
39|Aberdare Conglomerate|44884|4|Described|p1,2,3,4, Figs.1,7|||||||||
39|Aberdare Conglomerate|44885|14|Not recorded|p2,3,Fig.3|||||||||
39|Aberdare Conglomerate|45110|3|Fully described|Table 17|||||||||
39|Aberdare Conglomerate|48917|5|Briefly described|p13|||Stratigraphic Table. Upper Triassic||||||
39|Aberdare Conglomerate|60726|6|Mentioned|p16.|Late Triassic|Late Triassic|Ipswich area. Contains fossil Samarura sp.||||||
39|Aberdare Conglomerate|60993|5|Briefly described|p4, p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup. Pebble conglomerate, shale, siltstone; pink to brown claystone; minor coal. Overlain by Ripley Road Sandstone. Geol. Prov: Clarence-Moreton Basin.||||||
39|Aberdare Conglomerate|60995|6|Mentioned|p54|||Equivalent to Laytons Range Conglomerate (Woogaroo Subgroup) in the type area.||||||
39|Aberdare Conglomerate|60996|5|Briefly described|p72, p74|||Unconformably overlain by Gatton Sandstone. Geological Province: Clarence-Moreton Basin. Equivalent of Laytons Range Conglomerate.||||||
39|Aberdare Conglomerate|60999|5|Briefly described|p164|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin. See also p169.||||||
39|Aberdare Conglomerate|61002|5|Briefly described|p202|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
39|Aberdare Conglomerate|61005|6|Mentioned|p253, p254|||Equivalent to Laytons Range Conglomerate. See also p255 Figs. 23, 24 and 25. ||||||
39|Aberdare Conglomerate|61006|5|Briefly described|p278 Fig. 2|Triassic|Triassic|Conglomerate, labile sandstone, mudstone. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1.||||||
39|Aberdare Conglomerate|61310|6|Mentioned|p31|||Geological Province: Clarence-Moreton Basin.||||||
39|Aberdare Conglomerate|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
39|Aberdare Conglomerate|64665|5|Briefly described|p53 Fig.2, p59.|Late Triassic|Late Triassic|Clarence-Moreton Basin.||Basal unit in Woogaroo Subgroup.||Is overlain by Raceview Formation.|High energy conglomerate and sandstone.|
39|Aberdare Conglomerate|64856|6|Mentioned|p80|Rhaetian|Norian|Moreton Basin. Grades laterally into Precipice Sandstone to west. Base of Bundamba Group.| | ||||28-NOV-17
39|Aberdare Conglomerate|67402|5|Briefly described|p165 tbl LPB1|Norian|Norian|Clarence-Moreton Basin. See also p187, p188, p193, p223, p225.||Woogaroo Subgroup||Overlies the Blackstone Formation. Overlain by the Raceview Formation.|Conglomerates with minor coarse lithic sandstones.|
39|Aberdare Conglomerate|68679|5|Briefly described|p394|||||Woogaroo Subgroup.||Disconformably overlies Blackstone Formation (Brassall Subgroup).||
39|Aberdare Conglomerate|69594|4|Described|p519, p534, p543-547, p572|Late Triassic|Late Triassic|Northern Clarence-Moreton Basin. Is known as Laytons Range Conglomerate in NSW. In many places the unit is a single thin conglomerate; locally wedges out. 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.||Unconformably overlies Ipswich Coal Measures. Is overlain by Raceview Formation; both are equivalent to the Eddystone beds.|Pebble to cobble polymict 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.|
39|Aberdare Conglomerate|69790|6|Mentioned|p1063 Fig.2|Triassic|Triassic|Northern Clarence-Moreton Basin area.||||||
48|Aberfoyle River Porphyrite|23720|5|Briefly described|Map Legend|Permian|Permian|Of Uralla Plutonic Suite.  Porphyritic hornblende-biotite microgranite.||||||15-DEC-04
48|Aberfoyle River Porphyrite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
48|Aberfoyle River Porphyrite|44450|5|Briefly described|p57 Fig 8|||Geological Province: New England Fold Belt.||||||
48|Aberfoyle River Porphyrite|71628|4|Described|p8: 4-7; p14-32|||Binns et al. (1967). Previously Aberfoyle River Adamellite Porphyrite of Leitch et al. (1971) after unpublished work by Neilson (1970). One of several porphyritic intrusives around the margin of Wards Mistake Monzogranite. Named after the Aberfoyle River. Located 15km E of Guyra. Forms a small, E-W trending intrusion ~8km x 0.5-1.5km. Excellent outcrop comprises small, blocky rubble. Geochemistry described.||Llangothlin Suite.||Intrudes Girrakool beds and Tobermory Monzogranite.|Strongly porphyritic hornblende-biotite microgranite. I-type.|
63|Abroi Granodiorite|23720|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Hillgrove Plutonic Suite.  Gneissic biotite granodiorite.||||||15-DEC-04
63|Abroi Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
63|Abroi Granodiorite|31694|6|Mentioned|p349|||||||||
63|Abroi Granodiorite|31802|5|Briefly described|p142|||250 m.y. Refers Binns (1966)||||||
63|Abroi Granodiorite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
63|Abroi Granodiorite|35257|6|Mentioned|Fig.21|||||||||
63|Abroi Granodiorite|35664|6|Mentioned|p117|||Age dates.||||||
63|Abroi Granodiorite|36948|6|Mentioned|p51|||||||||
63|Abroi Granodiorite|36961|6|Mentioned|p219|||||||||
63|Abroi Granodiorite|39214|5|Briefly described|p40|||||||||
63|Abroi Granodiorite|42984|5|Briefly described|p370|||||||||
63|Abroi Granodiorite|44450|6|Mentioned|p11|||Within the Wongwibinda Metamorphic Complex. Geological Province: New England Fold Belt.||||||30-APR-10
63|Abroi Granodiorite|68822|6|Mentioned|p338|Sakmarian|Sakmarian||ca. 293 Ma|||||
63|Abroi Granodiorite|69188|5|Briefly described|p32|Permian|Permian|||Hillgrove Supersuite.||Is intruded by Round Mountain Leucoadamellite.||
63|Abroi Granodiorite|69930|6|Mentioned|255|||Southern New England Fold Belt. Deep-level intrusion; displays weak gneissic foliation parallel to that in surrounding metasediments.||||||
63|Abroi Granodiorite|71280|5|Briefly described|p403 Fig.2|||Wongwibinda Metamorphic Complex. Has southern and northern outcrops. Other similar ages given.|290.2 +/- 2.5 Ma (Cawood et al., 2011).|Hillgrove Plutonic Suite.|||S-type granites.|
63|Abroi Granodiorite|71628|4|Described|p2: 17, 41; p3: 1, 4, 6, 10, 12-18, 40|||See also p3: 71, 80-81, 85, 91-92, 94-95; p17: 32-33. Presumably named after a local homestead; ~42 km ENE of Armidale. A large intrusion, extending 43km N-S; crops out as large flat rock platforms (""whalebacks""). Geochemistry detailed; similar to Rockvale Monzogranite. Relative timing of this unit and Mornington Complex discussed. Deformation and relationship with Wongwibinda Complex described. Is faulted against Dyamberin beds. Associated (not genetically) with one Sb (Ag) deposit. Age of intrusion also given as ~290 Ma.|300  +/- 4  Ma (U-Pb TIMS: Collins et al., 1993).|Rockvale Suite.||Intrudes Girrakool beds. Is intruded by Round Mountain Leucomonzogranite. Abuts Tobermory and Rockvale Monzogranites and Mornington Complex and (?is intruded by) Camperdown Complex. See COMMENTS.|Mafic igneous complex comprising medium- to coarse-grained two-pyroxene gabbro, pyroxene diorite, porphyritic hornblende diorite, tonalite and mafic granodiorite; fine-grained and porphyritic marginal variants. Mafic enclaves.|
63|Abroi Granodiorite|71703|4|Described|p191-192, 194-205|||S-type granite. U-Pb geochron p198. Samples WO514, WO603 dated by LA-ICPMS-U-Pb.|290.5 +/-16 Ma, 292.6+/-2.5 Ma|Of Hillgrove Supersuite.||Intrudes Girrakool Beds, Wongwibinda Metamorphic Complex. Northern lobe adjacent to Tobermory Monzogranite. Sthn lobe adjacent to Rockvale Granodiorite.|K-feldspar quartz plagioclase biotite opaque +/- garnet muscovite granodiorite with accessory zircon, monazite and apatite.|
69|Acacia Downs Siltstone|33729|6|Mentioned|p83|||||||||
69|Acacia Downs Siltstone|33734|6|Mentioned|p494|||Early? Cambrian.||||||
69|Acacia Downs Siltstone|43501|14|Not recorded|Map Legend||Early Cambrian|(Provisional Edition)||||||
69|Acacia Downs Siltstone|43502|14|Not recorded|Map Legend||Early Cambrian|(Provisional Edition)||||||23-DEC-09
77|Ace Intrusive Complex|48958|6|Mentioned|p13|||||||||
90|Acton Shale|12185|5|Briefly described|map legend|Upper Ordovician|Upper Ordovician|Siliceous graptolitic slate. BMR map symbol: Oua.||||||15-AUG-07
90|Acton Shale|29992|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
90|Acton Shale|29994|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
90|Acton Shale|30332|6|Mentioned|Table 1|||Refers Opik (1958).||||||
90|Acton Shale|31019|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
90|Acton Shale|31111|6|Mentioned|p46|||See also P50, 52, 54, 58, 62||||||
90|Acton Shale|33325|5|Briefly described|Table 1|||Gisbornian - Eastonian||||||20-MAR-07
90|Acton Shale|34404|4|Described|p89|||Ordovician? Bolindian. Mention p97.||||||15-MAY-18
90|Acton Shale|34405|6|Mentioned|p119|||Lower Silurian||||||
90|Acton Shale|37728|6|Mentioned|p17|||||||||
90|Acton Shale|39331|6|Mentioned|Fig.5-11|||||||||
90|Acton Shale|40136|6|Mentioned|p37|||||||||
90|Acton Shale|40328|6|Mentioned|p57|||||||||
90|Acton Shale|41356|4|Described|p8|||See also P13||||||
90|Acton Shale|42497|5|Briefly described|Map legend|Eastonian|Eastonian|||||||
90|Acton Shale|42820|5|Briefly described|p7|||refers to Opik (1954,1958)||||||
90|Acton Shale|43344|14|Not recorded|p110,112,113||Late Ordovician|||||||
90|Acton Shale|43385|14|Not recorded|p169,170,171||Late Ordovician|||||||
90|Acton Shale|43472|14|Not recorded|p420-1,432-3,436|||fig.1||||||
90|Acton Shale|43473|14|Not recorded|Fig.1,opp.p1080||Late Ordovician|||||||
90|Acton Shale|43479|14|Not recorded|p79,95|Caradocian|Llandeilian|||||||
90|Acton Shale|44970|2|Defined|p1,7,11,12,17-19,22,||Late Ordovician|p23,29,31,42,69,85,86,map. Conformably overlies Pittman Formation||||||
90|Acton Shale|48878|14|Not recorded|p.6||Late Ordovician|Compared to Bullongong Shale Member (slightly older). Upper Ordovician.||||||21-MAR-07
90|Acton Shale|63290|5|Briefly described|p385|Late Ordovician|Late Ordovician|Included in Bendoc Group. Overlain by State Circle Shale and Black Mountain Sandstone uncomformably. Consists of black shales.||||||11-DEC-07
90|Acton Shale|67322|4|Described|p16, p20 Fig.5|Late Ordovician|Late Ordovician|Opik (1958). Albury-Bega Terrane. Includes graptolites of Gisbornian, Eastonian, and possibly earliest Bolindian age. Long considered as a member of the Pittman Formation (cf. Strusz and Henderson 1971; Abel 1991), it is suggested that its preferred correlation is with the Warbisco Shale of the Bendoc Group. Occurs in the Canberra-Queanbeyan region.||Of the Bendoc Group.||Overlies the Pittman Formation (Adaminaby Group). Is correlated with Warbisco Shale.||21-FEB-18
90|Acton Shale|73140|6|Mentioned|p495 Fig.6|||Proposed to be superseded and replaced by Warbisco Shale in the Bendoc Group.||||||
90|Acton Shale|73211|6|Mentioned|p909|Katian|Sandbian|Canberra region.|458-453Ma|||Underlain by Pittman Fomation.||
98|Adaminaby Group|12100|5|Briefly described|p819|Middle Ordovician|Early Ordovician|Eastern Lachlan Fold Belt area; upward fining succession with an upward decrease in lithic content.||||||08-MAY-12
98|Adaminaby Group|13139|5|Briefly described|p9 Fig. 4|Middle Ordovician|Middle Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||12-APR-05
98|Adaminaby Group|22472|5|Briefly described|p36|Ordovician|Ordovician|||||||
98|Adaminaby Group|22503|5|Briefly described|p645, Fig.3b|Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22529|5|Briefly described|1|Early Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22530|6|Mentioned|p693||Llanvirn|||||||
98|Adaminaby Group|22545|4|Described|p498-507, Fig.5||Ordovician|||||||
98|Adaminaby Group|22577|6|Mentioned|p120||Ordovician|||||||
98|Adaminaby Group|22624|5|Briefly described|p678, Fig.3 p679|Ordovician|Ordovician|See also Fig.4 p679||||||
98|Adaminaby Group|22628|6|Mentioned|fig1p108|Ordovician|Ordovician|||||||
98|Adaminaby Group|22679|3|Fully described|p 6|Ordovician|Ordovician|Lachlan Fold Belt. Overlain by Coombing Formation.||||||01-SEP-08
98|Adaminaby Group|22704|6|Mentioned|p63|||Also Fig6(b),p61. Previously Abercrombie beds||||||
98|Adaminaby Group|22708|5|Briefly described|p210|Ordovician|Ordovician|||||||
98|Adaminaby Group|22798|5|Briefly described|p856|Late Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22815|3|Fully described|p18,19,122|Ordovician|Ordovician|Equivalent to Pinnak Sandstone.||||||30-OCT-14
98|Adaminaby Group|22832|5|Briefly described|Fig.1b p634|Ordovician|Ordovician|Quartz turbidite, See also p636.||||||
98|Adaminaby Group|22842|6|Mentioned|p25||Ordovician|||||||
98|Adaminaby Group|22857|4|Described|p112, p422 App. 1, Tb. A1.5|Early Ordovician|Early Ordovician|A turbiditic sequence of interbedded arenite-siltstone-shale/slate together with chert beds. Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|22876|5|Briefly described|p16|Early Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22878|5|Briefly described|p29|Ordovician|Ordovician|||||||
98|Adaminaby Group|22879|5|Briefly described|map|Early Ordovician|Early Ordovician|||||||
98|Adaminaby Group|22880|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes: Pinnak Sandstone.||||||01-OCT-04
98|Adaminaby Group|22881|5|Briefly described|map|Ordovician|Ordovician|||||||
98|Adaminaby Group|22968|4|Described|P19, P99|Ordovician|Early Ordovician|Overlying unit is Bendoc Group.||||||04-MAR-09
98|Adaminaby Group|22971|5|Briefly described|p 17||Ordovician|of Lachlan Fold Belt.||||||
98|Adaminaby Group|23020|5|Briefly described|Map legend||Ordovician|||||||
98|Adaminaby Group|23021|5|Briefly described|Map legend|Ordovician|Early Ordovician|||||||
98|Adaminaby Group|23028|5|Briefly described|Map legend|Ordovician|Early Ordovician|Overlying unit is Bendoc Group.||||||01-SEP-08
98|Adaminaby Group|23029|5|Briefly described|Map legend|Ordovician|Early Ordovician|Overlying units are the Bendoc Group and the Kiandra Group.||||||01-SEP-08
98|Adaminaby Group|23030|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
98|Adaminaby Group|23043|5|Briefly described|Map Legend|Gisbornian|Yapeenian|||||||11-JAN-10
98|Adaminaby Group|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
98|Adaminaby Group|23170|2|Defined|p29 Fig.3|Ordovician|Darriwilian|Age: Late Darriwillian (Ordovician) - Ordovician.||||||
98|Adaminaby Group|23181|5|Briefly described|p1,7||Darriwilian|formerly 'Lue Beds'. Age from conodonts in chert.||||||
98|Adaminaby Group|23202|6|Mentioned|Fig.1|||||||||
98|Adaminaby Group|23213|5|Briefly described|Fig.10 p24|Darriwilian|Darriwilian|Includes some Darriwilian fossils. of Rockley-Gulgong Volcanic Belt.||||||
98|Adaminaby Group|23214|2|Defined|p19|Ordovician|Ordovician|Includes rocks previously mapped as Adaminaby Beds/beds, Triangle Group and Abercrombie Beds. Type Section refer to Glen et al 1990. Age determined by fossil assemblages (Fell, 1984). Geological Province: Lachlan Fold Belt. Max. thickness: >1500m.||||||05-MAR-12
98|Adaminaby Group|23245|5|Briefly described|p112,134||Early Ordovician|||||||
98|Adaminaby Group|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
98|Adaminaby Group|23309|5|Briefly described|p53-58 Fig 1.3||Ordovician|||||||
98|Adaminaby Group|23327|4|Described|1009|Ordovician|Ordovician|||||||
98|Adaminaby Group|23329|6|Mentioned|1042|Ordovician|Ordovician|||||||
98|Adaminaby Group|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
98|Adaminaby Group|23335|5|Briefly described|p15 Tb. 1, p19|Ordovician|Ordovician|||||||
98|Adaminaby Group|23464|5|Briefly described|p245|Ordovician|Ordovician|||||||
98|Adaminaby Group|23541|5|Briefly described|p398|||also see p396 Fig 1. In the Lachlan Fold Belt||||||
98|Adaminaby Group|23615|6|Mentioned|p64|Ordovician|Ordovician|||||||
98|Adaminaby Group|23850|5|Briefly described|p793|||||||||
98|Adaminaby Group|23860|5|Briefly described|p944|Ordovician|Ordovician|Overlying unit Bendoc Group.||||||
98|Adaminaby Group|23938|5|Briefly described|p11|Middle ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt. See also p71 Fig. 25, p75 Fig. 27. .||||||
98|Adaminaby Group|24003|5|Briefly described|p258|Late Ordovician|Late Ordovician|||||||
98|Adaminaby Group|24004|5|Briefly described|p277|||||||||
98|Adaminaby Group|24006|5|Briefly described|p312|Ordovician|Ordovician|||||||
98|Adaminaby Group|24007|5|Briefly described|p336|Ordovician|Ordovician|||||||
98|Adaminaby Group|24037|6|Mentioned|p423|||Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24133|4|Described|p35|Ordovician|Ordovician|Formerly Adaminaby Beds.  Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24146|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24177|6|Mentioned|p48|||||||||
98|Adaminaby Group|24215|5|Briefly described|p804 Fig. 3|||Geological Province:  Lachlan Fold Belt||||||
98|Adaminaby Group|24233|5|Briefly described|p253 Fig.1, p256|||Geological Province: Lachlan Orogen.||||||
98|Adaminaby Group|24317|5|Briefly described|p14, p15 Fig.1|Ordovician|Ordovician|||||||
98|Adaminaby Group|24329|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Includes the Hotham beds||||||
98|Adaminaby Group|24339|5|Briefly described|p47 Fig. 4|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt. Age: 445 +/- 2 Ma (Ar/Ar)||||||
98|Adaminaby Group|24383|6|Mentioned|p88 Fig.57|||Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24463|5|Briefly described|p319|||Overlain by Sofala Volcanics.  Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|24551|5|Briefly described|p96, p100|Middle Ordovician|Early Ordovician|Only includes Pinnak Sandstone in Victoria.||||||
98|Adaminaby Group|24575|5|Briefly described|p711|Middle Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|24576|5|Briefly described|p727|Middle Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt||||||
98|Adaminaby Group|42294|4|Described|p24|||Intended as a redefinition to replace Adaminaby beds.||||||
98|Adaminaby Group|42712|4|Described|5, 12, 19|Late Ordovician|Early Ordovician|Previously called the Triangle Group. Overlain by and interfingers with Rockley Volcanics.||||||04-MAR-09
98|Adaminaby Group|43233|5|Briefly described|Map Legend||Early Ordovician|||||||11-JAN-10
98|Adaminaby Group|43312|5|Briefly described|Map Legend|||||||||
98|Adaminaby Group|43313|5|Briefly described|Map Legend|||||||||
98|Adaminaby Group|43314|5|Briefly described|Map Legend||Early Devonian|||||||
98|Adaminaby Group|43315|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||03-MAY-05
98|Adaminaby Group|43494|5|Briefly described|p8, p15|Ordovician|Ordovician|Consists of slaty white and purplish siltstone and fine-grained massive quartz sandstone, with some siltstone. Overlain by the Tucklan Formation.||||||09-MAR-06
98|Adaminaby Group|43633|5|Briefly described|p17||Early Ordovician|||||||
98|Adaminaby Group|43639|5|Briefly described|Map Legend||Ordovician|||||||
98|Adaminaby Group|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Consists of quartz sandstone, siltstone, slate, phyllite, black carbonaceous slate, chert.||||||15-JUL-08
98|Adaminaby Group|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Quartz sandstone, siltstone, slate phyllite, black carbonaceous slate, shale.||||||
98|Adaminaby Group|43782|5|Briefly described|Map Legend|Darriwilian|Yapeenian|||||||
98|Adaminaby Group|44093|5|Briefly described|p50|Ordovician|Ordovician|See also p189 and 190 Appendix 1.||||||
98|Adaminaby Group|44184|5|Briefly described|Map Legend||Early Ordovician|||||||
98|Adaminaby Group|44185|5|Briefly described|Map legend.|Middle Ordovician|Early Ordovician||||Includes Pinnak Sandstone.|||30-OCT-14
98|Adaminaby Group|44187|5|Briefly described|Map Legend||Early Ordovician|||||||
98|Adaminaby Group|50230|5|Briefly described|Map legend|Ordovician|Ordovician|Sandstone and siltstone.  Includes the Beacons Hill Chert.  Overlain by the Bendoc Group.||||||
98|Adaminaby Group|50231|5|Briefly described|Map Legend|Late Ordovician|Middle Ordovician|Includes: Beacons Hill Chert.  Underlies: Bendoc Group.||||||
98|Adaminaby Group|50232|5|Briefly described|Map legend|Late Ordovician|Middle Ordovician|Contains the Nattery Chert.  Overlain by the Bendoc Group.||||||
98|Adaminaby Group|50233|5|Briefly described|Map Lagend|Gisbornian|Ordovician|Overlain by the Bendoc Group.||||||
98|Adaminaby Group|50234|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes: Nattery Chert.||||||
98|Adaminaby Group|60503|5|Briefly described|p27, p28 Fig. 9|Early Ordovician|Early Ordovician|Includes Pinnak Sandstone and metamorphics. Turbidites; largely metamorphosed to schists and gneisses of biotite grade. Geological Province: Lachlan Fold Belt. See also p45 Tb. 2. ||||||
98|Adaminaby Group|60504|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes Pinnak Sandstone||||||
98|Adaminaby Group|60505|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Includes the Pinnak Sandstone||||||
98|Adaminaby Group|60506|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Includes the Pinnak Sandstone||||||
98|Adaminaby Group|60507|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Includes the Pinnak Sandstone||||||
98|Adaminaby Group|60508|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Pinnak Sandstone.||||||20-OCT-04
98|Adaminaby Group|60536|6|Mentioned|p552|||||||||
98|Adaminaby Group|60542|5|Briefly described|p45|Early Silurian|Early Ordovician|In ORBOST is represented by only the Pinnak Sandstone, also referred to as Hotham slates and Mallacoota beds. Geological Province: Lachlan Fold Belt. ||||||
98|Adaminaby Group|60902|5|Briefly described|p859, p868|Early Ordovician|Early Ordovician|Includes Numeralla Chert. Craton-derived turbidites adjacent to Wagonga Group rocks. Overlain by Bendoc Group. Geological Province: Bega Terrane.||||||11-APR-06
98|Adaminaby Group|60904|5|Briefly described|p782|Middle Ordovician|Early Ordovician|Includes the Numeralla Chert. Sandstone.||||||
98|Adaminaby Group|60988|5|Briefly described|p144 Fig.1, p146|Late Ordovician|Late Ordovician|Includes rocks formerly known as the "Bombala Beds".|||||Undifferentiated sediments, turbidites, sandstone, mudstone, shale.|
98|Adaminaby Group|61160|5|Briefly described|p44, p35 Tb. 5.2|||Geological Province: Lachlan Fold Belt.||||||
98|Adaminaby Group|61161|5|Briefly described|p78, p76-77 Fig 6.1|Middle Ordovician|Early Ordovicioan|Includes mainly Pinnak Sandstone. Also been called Hotham Group, Hotham slates and Mallacoota beds. Geol. Prov: Lachlan Fold Belt.||||||
98|Adaminaby Group|61163|5|Briefly described|p7, p38 Tb. 6.2|Ordovician|Ordovician|Overlain by Bendoc Group. Geological Province: Lachlan Fold Belt. Variously named Hotham slates, Pinnak Sandstone and Mallacoota beds in different parts of the eastern LFB.||||||
98|Adaminaby Group|61164|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||05-MAR-12
98|Adaminaby Group|61165|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61166|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61167|5|Briefly described|map legend|Middle Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||07-FEB-11
98|Adaminaby Group|61168|5|Briefly described|map legend|Late Ordivician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61169|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61170|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||07-FEB-11
98|Adaminaby Group|61171|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61172|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61173|5|Briefly described|map legend|Middle Ordovician|Early Ordivician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61174|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||07-FEB-11
98|Adaminaby Group|61175|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61176|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61177|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61178|5|Briefly described|map legend|Middle Ordovician|Early Ordovician|Includes Pinnak Sandstone.||||||
98|Adaminaby Group|61187|5|Briefly described|p4, p5 Fig.3, p26 Fig.2, p29 Fig.4. |Early Ordovician|Early Ordovician|Benambra Terrane. Correlative of Castlemaine Supergroup (Bendigo Zone, Melbourne Terrane).|||Includes Hotham beds and Pinnak Sandstone.||Mainly turbidite sandstones.|
98|Adaminaby Group|61413|5|Briefly described|p7, p46, p82 Fig.103.|Early Ordovician|Early Ordovician|Suggested term for Early Ordovician turbidites in southeastern Lachlan Fold Belt.|||Includes Numeralla Chert.||Turbidites.|
98|Adaminaby Group|61731|5|Briefly described|p1037, p1038 Fig.1c|Ordovician|Ordovician|Conformably overlain by Wagonga Group.||||||
98|Adaminaby Group|61762|6|Mentioned|p19 Fig. 2(a)||Ordovician|||||||
98|Adaminaby Group|61964|5|Briefly described|p20|||Similar in age and lithology (quartz sandstone turbidite sequences) to Wagga Group but separated by the Gilmore Fault Zone. However, for this study these sequences have been mapped as Wagga Group pending further work. In the eastern Lachlan Orogen.||||||
98|Adaminaby Group|62070|5|Briefly described|p34 Fig.1, p38, p39,|Darriwilian|Bendigonian|||||Overlain by the Bendoc Group.|Predominantly quartz-rich turbidite succession with minor chert horizons.|
98|Adaminaby Group|63283|5|Briefly described|p205, p206|Ordovician|Early Ordovician|Includes; Budhang Chert. Geological Province: Rockley-Gulgong Volcanic Belt and Kiandra Volcanic Belt.||||||07-FEB-11
98|Adaminaby Group|63285|6|Mentioned|p275 Fig. 2|||Geological Province: Molong Volcanic Belt. Consists of quartz-rich sandstone, siltstone, minor siliceous siltstone and rare black mudstone.||||||
98|Adaminaby Group|63286|6|Mentioned|p294 Fig. 1|||Consists of quartz-rich sandstone, siltstone and chert.||||||07-FEB-11
98|Adaminaby Group|63289|4|Described|p364, p369, p372, p374|Gisbornian|Darriwilian|Conformably overlain by Triangle Formation and Coombing Formation. Geol Province: Kiandra Volcanic Belt. Consists of metamorphosed quartz-rich turbidites. Age constrained by conodonts and graptolites. Multiply deformed. See p374 for petrological info.||||||02-OCT-15
98|Adaminaby Group|63290|5|Briefly described|p388, p395, p396 Fig. 3|Middle Ordovician|Ordovician|Includes; Numeralla Chert, Chakola Formation. Overlain by Bendoc Group in eastern subprovince. Sandstones in group are matrix-rich, quartz-feldspar-mica sandstones.||||||05-MAR-12
98|Adaminaby Group|63635|6|Mentioned|p39|||In NSW. Correlation between mainland Australia and Tasmania discussed.||||||
98|Adaminaby Group|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Abercrombie Formation with its one sandstone member and 3 chert members.||||||
98|Adaminaby Group|64295|5|Briefly described|p198 Fig. 1, p199|Middle Ordovician|Early Ordovician|||||||
98|Adaminaby Group|64616|6|Mentioned|p343 Fig.23|||||||||
98|Adaminaby Group|64826|5|Briefly described|p1037|Ordovician|Ordovician|Includes quartz-rich turbidites.||||||04-MAR-09
98|Adaminaby Group|65469|6|Mentioned|p20|||East of the Macquarie Arc, Lachlan Orogen. ||||||
98|Adaminaby Group|65900|5|Briefly described|p162||Ordovician|Tabberabbera Zone.  Turbidite, intruded by I-type granites.||||||10-MAY-12
98|Adaminaby Group|65969|5|Briefly described|p3, p13|||Overlies Heathcote Volcanic Group. Metaturbidites.||||||
98|Adaminaby Group|66087|6|Mentioned|p3 Fig. 2, p4 Fig.3|Ordovician|Ordovician|||||||
98|Adaminaby Group|66182|6|Mentioned|p323 Fig.5|Middle Ordovician|Early Ordovician|Turbidites.||||||11-MAY-12
98|Adaminaby Group|66185|4|Described|p397, p396 Fig. 1|Late Ordovician|Early Ordovician|Backarc extensional setting. Thin quartz rich psammites (turbidites), minor black carbonaceous shale units. A thick package between the Wyangala Granite and the Reids Flat and Wywurri Granites.||||||
98|Adaminaby Group|66196|5|Briefly described|p616,617|Middle Ordovician|Early Ordovician|Turbidites. Overlies the Howqua Chert.||||||
98|Adaminaby Group|66300|5|Briefly described|p17, p23, p52, 64.|Ordovician|Ordovician|Eastern Lachlan Orogen.||||Intruded by Lockhart Igneous Complex, Touga Granite, Tullyangela Granite.|Turbiditic sedimentary rocks.|24-OCT-13
98|Adaminaby Group|66713|5|Briefly described|p3 Fig.2, p3, p5, p10|||Quartz-rich, turbiditic sedimentary rocks. Underlies the Bendoc Group. Includes Abercrombie Formation.||||||
98|Adaminaby Group|67106|6|Mentioned|p681|||||||||
98|Adaminaby Group|67107|6|Mentioned|p686||||||||Quartz-rich turbiditic sedimentary rocks.|
98|Adaminaby Group|67322|4|Described|p2,p4 Fig.2,p5,p13,p15-16,p25,p28;Fig.5|Early Ordovician|Late Cambrian|Albury-Bega Terrane and Macquarie Arc. First named by Fairbridge (1953), according to Glen (1994); current definition dates from Glen et al. (1990). Green to grey-green laminated slates and siltstones interbedded with sandstones of variable thickness. Includes chert bearing fossils of late Darriwilian age. Has at least five distinct conodont-based zones. Maximum age from p20 Fig.5 (Strat. column). Occurs in the Cooma-Mallacoota region, and Sofala-Dunedoo-Mudgee and Canberra-Queanbeyan regions.|||Budhang, Mozart and Numeralla Cherts; Abercrombie, Pittman and Chakola Formations; Pinnak Sandstone.|Conformably overlain by the Coomber Formation and Bendoc Group. Equivalent to Pinnak Sandstone.|Turbiditic sandstone sequence punctuated by 2-3 prominent and regionally extensive chert-rich horizons, of which the lowermost is more sporadic, consisting of thinly bedded cherts, sometimes interlayered with turbiditic sandstones.|
98|Adaminaby Group|67802|6|Mentioned|p28, p30|Middle Ordovician|Lower Ordovician|Tabberabbera Zone. Sediment derived from the south and west.||||Is overlain conformably by Bendoc Group.|A thick pile of turbidites.|
98|Adaminaby Group|67803|4|Described|p34|Ordovician|Ordovician|This unit is split in two. The western half in the Wagga Basin is in situ. The eastern half (east of the Macquarie Arc) is allochthonous, constituting (with overlying shales) the Bega Terrane. Deposited as a submarine fan, draining the northern part of the Ross Orogen.||||||
98|Adaminaby Group|67820|6|Mentioned|p135|||Has a gross domal distribution in the Kiawarra and Murrumbateman areas; this and a gravity low suggest a concealed (?mineralising) granite body at depth.||||||
98|Adaminaby Group|67847|5|Briefly described|p19, p21, p22, p26 fig 4.2|Middle Ordovician|Early Ordovician|Lachlan Orogen. See also p27-p30, p54, p59.|||||Quartz-rich turbidites.|
98|Adaminaby Group|67849|4|Described|p21, p22, p23, p27, p30. |Middle Ordovician|Early Ordovician|Lachlan Orogen. Turbidite sequences. Dominant part of an westward-dipping accretionary complex in the Batemans Bay area. Kubler Index measurements show this unit experienced much the same metamorphic conditions as Wagonga Group. Underplating and associated metamorphism occurred c.460-440 Ma.||Unit in Narooma Accretionary Complex.||Conformably overlies, and interfingers with, Wagonga Group.|Includes sandstones and minor chert lenses.|
98|Adaminaby Group|68255|4|Described|p1049-p1059, p106-p1064|Givetian|Ordovician|Lower to Middle Ordovician. Sequences within this unit have reached lower greenschist metamorphic grade. Intruded by the Buckenbowra Granodiorite around 395.8 +/- 8.1 Ma.|> 395.8 +/- 8.1 Ma|||Lenses of this group interfinger the Wagonga Group. Intruded by the Buckenbowra Granodiorite. Unconformably underlain by the Comerong Volcanics and Merrimbula Group.|Comprises a monotonous sequence of turbidites and minor black shale comprising well-bedded quartzose meta sandstone, meta siltstone and slate.|20-JUL-15
98|Adaminaby Group|68309|5|Briefly described|p225-226, 232-233|Middle Ordovician|Early Ordovician|Tectonic slices occur in the Wagonga Group; emplaced by thrust faulting during subduction. Extends ~30km inland, W of Batemans Bay (Bega Terrane).||||Is overlain conformably by Wagonga Group (locally thrust-faulted against).||
98|Adaminaby Group|68466|5|Briefly described|p64-66, 70|Middle Ordovician|Early Ordovician|Albury-Bega Terrane.|||Numeralla Chert.|Is overlain by Bendoc Group.|Turbiditic sandstones and cherts.|
98|Adaminaby Group|68592|2|Defined|p269-319, p320, p323-5, p338, p344,|Middle Ordovician|Early Ordovician|See also xxiv, p71, p73 Tb.5, p136-7, p182, p230, p235, p241-2, p255, p348, p350, p355, p357, p361-3, p376, p384-5, p408-9, p411-3, p416, p421, p425-6, p443, p731, p743, p750, p771, p819, p835. Originally Adaminaby Beds of Fairbridge (1953) after Adamson (1955) and defined by Richardson (1979); divided into Adaminaby Group and Warbisco Shale by Glen et al. (1990). Adaminaby Group was defined by Lewis et al. (1994) incorporating Mallacoota Beds of Fenton et al. (1982). Reference areas described. Thickness estimated up to 5 km. Geophysical properties described. Frogmore, Wyangala, Peelwood, Goulburn and Bungonia structural zones: deformation and metamorphism described. Is intruded by Banshea Granite and Wyangala Supersuite. Quarried locally. Major source of sediment for Covan Creek Formation. Palaeontology detailed. Hosts gold mineralisation in the Dalton area; Pb-Ag-Zn at Rye Park (Wallah Wallah mine: detailed).|||Includes Abercrombie and Chakola Formations, Numeralla Chert and Pinnak Sandstone.|Is overlain conformably by Bendoc Group, unconformably (or faulted) by Bungonia Group, and unconformably by Shivering Conglomerate. Equivalent to Wagga Group and Girilambone Group.|Uniform sequence of interbedded, turbiditic, quartzose to lithic-feldspar-quartz sandstone, siltstone and mudstone; minor chert intervals.|
98|Adaminaby Group|68822|5|Briefly described|p334, p349, p351|||Overlain by an Upper Ordovician sequence. The youngest conodonts are Darriwilian 4-Gisbornian-1, based on the presence of Pygodus serra, P.anserinus and Periodon aculeatus.|||Includes the Pinnak Sandstone.|Overlain by the Bendoc Group.||
98|Adaminaby Group|69002|6|Mentioned|p13|||||||Overlain by the Bendock Group.||
98|Adaminaby Group|69159|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|69270|6|Mentioned|p1, p4||||||Abercrombie Formation|||
98|Adaminaby Group|69539|6|Mentioned|p607-608|||||||||
98|Adaminaby Group|69541|5|Briefly described|p652-653|Late Ordovician|Early Ordovician|Top of the Group is early Gisbornian.|||Includes Chakola Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|69564|5|Briefly described|p3|Ordovician|Ordovician||||||Stacked turbidites.|
98|Adaminaby Group|69668|5|Briefly described|p927, p929 Fig.2, p930 Fig.3, p931, p948|Middle Ordovician|Early Ordovician|Albury-Bega terrane. Geochemical similarity of cherts with those of the Girilambone Group suggests both regions shared identical sources and depositional regimes, occupying near-identical tectonic settings in a back-arc basin.|||Includes Abercrombie Formation, Numeralla Chert..||Turbiditic sandstones and cherts.|18-JUN-20
98|Adaminaby Group|69801|5|Briefly described|p98|Ordovician|Ordovician|Central Lachlan Orogen.||||Intruded by the Thologolong Granite.|Sedimentary rocks.|
98|Adaminaby Group|70026|4|Described|p37,39-41,49,51-p52|Ordovician|Latest Cambrian|Geological province: Lachlan Orogen. Highly deformed with tight folds, foliations, quartz veining and fault breccia (Miller and Gray 1996, 1997; Fergusson and Frikken 2003; Glen et al. 2004; Prendergast 2007; Prendergast and Offler 2012). Detrital zircon ages from the sandstone turbidites at Melville Point, NSW mainly in the ranges 600-500 Ma and 1200-1000 Ma, similar to those reported from Ordovician turbidites elsewhere in the Lachlan Orogen (Fergusson et al. 2013). Cambrian basaltic breccia unit and associated limestones occur adjacent to and within disrupted quartz turbidites at Burrewarra Point (Fergusson & Frikken 2003).||||Underlain by (or interfingers with) Wagonga Group and gradationally by the Narooma Chert.|Quartzose turbidites; thick-bedded sandstone with thin-bedded mudstone and chert.|17-JUL-19
98|Adaminaby Group|70178|6|Mentioned|p3, p13|Ordovician|Ordovician||||||Siliciclastic turbidites.|
98|Adaminaby Group|70192|5|Briefly described|Map Legend|Gisbornian|Lancefieldian|On Boorowa, Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Abercrombie Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|70297|5|Briefly described|map legend, on side 2 of map sheet|Gisbornian|Bendigonian|Age: Middle Ordovician to earliest Late Ordovician. Includes thick sequence of thin, rhythmically bedded, quartz-rich fine- to coarse-grained turbidites, and chert with minor black carbonaceous shale of a distal turbidite fan, deposited in a deep water environment. Small structurally controlled low sufide (orogenic) gold, and copper-dominated structurally  controlled high sulfide (orogenic) base metal +/- gold veins.|||Mozart Chert Member, Budhang Chert Member|Is overlain by Bendoc Group.|Turbiditic sequence of quartz-rich sandstone, mudstone, shale; carbonaceous shale, greywacke; chert, quartzite, phyllite, slate.|17-MAY-16
98|Adaminaby Group|70493|5|Briefly described|p53-64|Ordovician|Ordovician|Lachlan Orogen. Numerous geochemical diagrams. Most sediments underwent one cycle of erosion; some have been recycled. Sediments were derived from a mainly felsic granodioritic, probably shoshonitic, source in a collisional, not subduction-related, setting.||||Overlies Howqua and Narooma Cherts. Is overlain by Bendoc Group.|Turbidites; lower part dominated by sandy turbidite facies with thin intervals of bedded chert, and an upper part with a thick (300-400m) unit of black shale largely lacking sandstone.|
98|Adaminaby Group|70540|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70541|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70542|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70543|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation|||
98|Adaminaby Group|70544|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation|||
98|Adaminaby Group|70545|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation.|||
98|Adaminaby Group|70546|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Abercrombie Formation|||
98|Adaminaby Group|70601|4|Described|p23, p25-27, p39-57|Gisbornian|Early Ordovician|Onshore geology. Conformable junction with overlying Narooma Chert. Above zone of melting where Moruya Suite granites extend onshore. Conodont age ca 485Ma. Outcrops extensively from the NSW coast to the eastern boundary of the Melbourne Zone.||Narooma Accretionary Complex.|Pinnak Sandstone, Chakola Formation, Numeralla Chert.|Underlies Warbisco Shale (Bendoc Group), Bogolo Formation, Numeralla Chert. Overlies Howqua Chert, "Melville Chert".|Quartz turbidites with crenulation cleavage that overprints a bedding-parallel slaty cleavage; siliceous shale, gradational, generally upward-fining sequence of siltstone, black shale and sandstone with thin cross-laminated quartzic silt layers.|18-JAN-19
98|Adaminaby Group|70629|6|Mentioned|p986|Late Ordovician|Early Ordovician|Melbourne Zone.||||||
98|Adaminaby Group|70661|3|Fully described|vii, viii, p3, p4, p7, p8 fig 2, p9|Gisbornian|Bendigonian|Named after the town of Old Adaminaby. Outcrops primarily in the southwest of the map, sporadically outcrops in the northwest. Estimated to be at least 1000m thick, may be 3-5km thick. Lithology in different map areas discussed in greater detail. Deposited in submarine fan or fan apron system below storm wave base.  Equivalent to the Wagga Group, Girilambone Group. See also p10, p11, p12, p13, p14, p15, p16, p17, p19,p21- p26, p41, p101, p130, p145, p243.||||Conformably overlain by Bindook Group, Bendoc Group, faulted against Merrimbula Group, intruded by Bundundah Granite, conformably overlies Howqua Chert, Unconformably overlain by Shoalhaven Group.|Thin to thickly bedded micaceous quartz-rich metasandstone, metasiltstone, medium to fine grained, poorly sorted and subangular to subrounded turbiditic sandstone, hornfels, shale, slate, phyllite and minor interbedded chert.|26-JUL-17
98|Adaminaby Group|70684|5|Briefly described|p7 Fig.1, p14-15|Ordovician|Ordovician|||||Is overlain by Bendoc Group.|Deformed turbidites.|
98|Adaminaby Group|70718|5|Briefly described|p43-p44|Late Ordovician|Early Ordovician|Tabberabbera  and Wagga-Omeo Zones, Murray Basin. Turbidite succession.|||Includes the Pinnak Sandstone.||Sandstone, mudstone, shale, carbonaceous shale, greywacke, chert, quartzite and phyllite.|
98|Adaminaby Group|70727|6|Mentioned|p172|Ordovician|Ordovician|Geological province: Hill End Zone, Eastern Lachlan Orogen.||||Passive intruded by Wyangala Granite.||
98|Adaminaby Group|70744|5|Briefly described|p944-945|Late Ordovician|Late Ordovician|SE Lachlan Orogen. Detrital zircon age distribution graph.||||||
98|Adaminaby Group|70754|5|Briefly described|p447|Darriwilian|Darriwilian|Contains rare linguloid and acrotretoid brachiopods.|||||Includes deep-water cherts.|
98|Adaminaby Group|71040|6|Mentioned|p10 Fig.6, p19|Ordovician|Ordovician|||||||
98|Adaminaby Group|71069|3|Fully described|p9, p19, p21 fig 7, p22, p31|Ordovician|Ordovician|Name derived from Old Adaminaby. Previously termed the Adaminaby Beds. Reference sections mentioned [However there is some ambiguity as to whether or not these are suitable]. Distributed widely across the Lachlan Orogen where it usually forms low, weathered outcrop. Possible source of gold in placer deposits near the map sheet (Captains Flat) area.Estimated thicknesses ranging from 2000-5000m. Structure, metamorphism and fossil assemblages discussed.  Age poorly constrained, [author states that is believed to be older than Ordovician, but no evidence is provided]. Equivalent to the Wagga and Girilambone Groups. Deposited in a submarine fan or fan apron system below storm-wave base, probably in an outer slope or basin plain setting. Lithology shows elements of being a bouma sequence and is thus interpreted to indicate depositon from turbidity currents. Intruded by the Harrisons Peak Granite. See also  p39 fig 16, p40 fig 17, p42, p51, p52, p55-p58, p60, p61, p65-67, p72, p75, p76 fig 27, p77, p80, p82, p88, p92, p93, p95, p100, p105-p107, p120, p125, p134, p144, p172, p178, p183, p184, p201, p202.|||Includes the Abercrombie Formation, Peach Tree Chert Member, Mummel Chert Member, Willigam Sandstone Member, Numeralla Chert, Chakola Formation and the Pinnak Sandstone|Conformably overlain by the Bendoc Group and the Warbisco Shale. Unconformably overlain by the Hoskinstown Group. Overlain by the Covan Creek Formation.|Interbedded quartzose to lithic-feldspar-quartz sandstone, siltstone and mudstone with minor but conspicuous chert rich intervals.|
98|Adaminaby Group|71303|5|Briefly described|map legend|Late Ordovician|Early Ordovician||||Includes Nattery Chert Member.||Thin- to thick-bedded micaceous quartz-rich sandstone and shale (turbidites), shales and slates, phyllite and minor interbedded chert. Rocks variably regionally metamorphosed to lower greenschist facies with hornfelsing near intrusions.|
98|Adaminaby Group|71656|4|Described|p10 Fig.1, p11-14, p12, 13 Fig 2|Gisbornian|Early Ordovician||||Includes Abercrombie Formation.|Underlies Bendoc Group.|Strata include chert bodies.|
98|Adaminaby Group|71691|5|Briefly described|Map legend.|Ordovician|Ordovician||||Abercrombie Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|71699|5|Briefly described|Map legend.|Ordovician|Ordovician||||Abercrombie Formation.|Is overlain by Bendoc Group.||
98|Adaminaby Group|71700|3|Fully described|vi, ix, x, p5, p7-p10, p36-p41, p43,  CD|Ordovician|Ordovician|Albury-Bega Terrane. Named for the town of old Adaminaby. A type section has not been defined but a number of reference sections have been proposed over time [see CD]. Originally the "Adaminaby Beds" of Fairbridge (1953) , the unit and the Bendoc Group were subsequently seperated into the Birkenburn Beds and Merigan Black Shale by Felton and Huleatt (1975) before being divided into the Adaminaby Group and the overlying Warbisco Shale by Glen et al (1990). The unit was thereafter formally defined by Lewis et al (1994) incorporating the Mallacoota Beds. Distribution, geomorphic expression, outcrop characteristics, depositional environment, structural geology, geochemistry, fossils, mineralisation and estimated thicknesses are discussed. Structural geology and metamorphism are discussed. See also p45, p48-p50, p57, p63-p64, p66, p71, p74, p79, p81-p83, p85-p86, p90, p114, p116-p119.|||Includes the Abercrombie Formation, Numeralla Chert, Chakola Formation and Pinnak Sandstone.|Conformably overlain by the Bendoc Group. Unconformably overlain by the Bindook Group, Mount Fairy Group and the Woodlawn Volcanics. Intruded by the Tallaganda Granodiorite.|Interbedded quartzose to lithic-feldspar-quartz sandstone, siltstone and mudstone with conspicuous chert rich intervals.|
98|Adaminaby Group|71889|6|Mentioned|p12|Darriwilian|Darriwilian|||||Equivalent to the Wagga Group.|Black shales.|
98|Adaminaby Group|72263|5|Briefly described|p514-515,524|Early Ordovician|Early Ordovician|Geological province: Lachlan Orogen. Deposited on a passive margin. Juxtaposed against, and surrounds the Macquarie Arc. Zircon analysis by Glen et al. (2011) on the Mitchell Formation, yielded zircon ages of ~494 Ma, and combined with Hf isotope analysis from this study (Zhang et al., 2019), suggests that the samples studied by Glen et al., 2011 were likely to be of Adaminaby Group instead (similar to Adaminaby zircon data presented by Meffre et al., 2007), with a peri-Gondwanan afinity.|||||Quartz-rich turbidites, cherts and black shales.|
98|Adaminaby Group|72296|6|Mentioned|p6||||||Pinnak Sandstone.|||
98|Adaminaby Group|72528|5|Briefly described|p11, p18, p25.|Ordovician|Ordovician|||Campbells Group||Underlies Lambie Group and is intruded by Whipstick Monzogranite and Bandshea Granite||
98|Adaminaby Group|73059|5|Briefly described|p1053 Fig.2, 1055, 1059-1061, 1063|Ordovician|Ordovician|Detrital zircons aged ~510-485 Ma attributed to a Delamerian Fold Belt source.||||Overlies Wagonga Group, Howqua Chert. Is overlain by Bendoc Group and Narooma Chert.|Quartz-lithic sandstones unit overlain by quartz-rich sandstones unit.|
98|Adaminaby Group|73140|5|Briefly described|p495|Gisbornian|Late Cambrian|Proposed to incorporate and supersede the Wagga Group. Also proposed to be incorporated into a new Lachlan Supergroup.||Lachlan Supergroup|Abercrombie Formation|Underlies Bendoc Group|Terrigenous turbiditic sequence.|
98|Adaminaby Group|73186|6|Mentioned|p227, p229-230, p236-237, p239-240, p242|Ordovician|Early Ordovician|Tabberabera Zone and Omeo Zone.|||||Turbidites with deep water chert, includes sandstones, mudstones and hemipelagic black slates.|
98|Adaminaby Group|73211|6|Mentioned|p909|Upper Ordovician|Middle Ordovician|Referred to as the foundation of the Lachlan Orogen/Fold Belt.||||||
98|Adaminaby Group|73264|6|Mentioned|p1390 Fig.12, p1392, p1393 Fig.15|Middle Ordovician|Early Ordovician|Lachlan Orogen. Age described as Early and late-Middle Ordovician.|||||Turbidites.|
98|Adaminaby Group|73299|5|Briefly described|p1094 Fig.2, p1095-1096, p1098|Ordovician|Ordovician|Lachlan Orogen. Generally strongly deformed with abundant tight to isoclinal mesoscopic folds. Poorly constrained early folds east of Mudgee prior to the dominant deformation, Capertree High. Locations in text include p1100 Fig.5.|||||Turbidites.|
98|Adaminaby Group|73431|5|Briefly described|p362-366, p370, p372, p374-375|Ordovician|Early Ordovician|Lachlan Orogen. Passive margin sequence along the east Gondwana continental margin. Coeval with, and in faulted contact with the Macquarie Arc. Location in text includes p371 Fig.7.||||Intruded by Sunset Hills Granite|Quartz and clay-rich turbidites, shales.|
98|Adaminaby Group|73440|6|Mentioned|p146||||||||Includes quartz-rich turbidites.|
98|Adaminaby Group|73457|5|Briefly described|p4, p6 Fig.4, p8-12, p13 Fig.8, p14|Ordovician|Ordovician|||||Unconformably underlies Galore Hill Formation, Kengal Formation, Yambla Formation, faulted against Granya Granite|Metasedimentary rock.|
98|Adaminaby Group|73497|5|Briefly described|Map legend|Ordovician|Ordovician||||||Marine turbiditic sandstone, siltstone and shale: magnetic response below limit of detection.|
98|Adaminaby Group|73505|6|Mentioned|p35|||||||||
98|Adaminaby Group|75070|6|Mentioned|p183|||||||||
107|Adamstown Subgroup|22969|4|Described|Fig 4.1a||Late Permian|||||||
107|Adamstown Subgroup|24121|5|Briefly described|p4, p99, p115, p227, p231|||Of Newcastle Coal Measures.||||||25-AUG-22
107|Adamstown Subgroup|39609|6|Mentioned|Table 1|||||||||
107|Adamstown Subgroup|42214|6|Mentioned|Table 1 P462|||||||||
107|Adamstown Subgroup|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Newcastle Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
107|Adamstown Subgroup|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||Newcastle Coal Measures.||Overlies Lambton Subgroup. Is overlain by Boolaroo Subgroup.||
107|Adamstown Subgroup|68711|5|Briefly described|p118, p116 Tbl 2|||Of McKenzie and Britten (1969). Replaced by Adamstown Formation. ||Formerly of Newcastle Coal Measures|Included Kotara Formation, Fern Valley Coal, Glebe Formation, Wave Hill Coal, Kahibah Formation, Montrose Coal, Tickhole Formation, Australasian Coal|||
107|Adamstown Subgroup|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Newcastle Coal Measures|||Conglomerate, tuff, sandstone, siltstone, claystone, black coal.|
134|Adelong Norite|29992|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
134|Adelong Norite|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
134|Adelong Norite|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
134|Adelong Norite|33959|6|Mentioned|p235|||||||||
134|Adelong Norite|37529|5|Briefly described|p6|||||||||
134|Adelong Norite|40328|4|Described|p202|||||||||
134|Adelong Norite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
134|Adelong Norite|40498|6|Mentioned|p385|||||||||
134|Adelong Norite|42313|3|Fully described|p51|Late Silurian|Early Silurian|||||||
134|Adelong Norite|42314|5|Briefly described|Map|Middle Silurian|Early Silurian|||||||
134|Adelong Norite|42497|5|Briefly described|Map legend|Ludlovian|Ludlovian|||||||
134|Adelong Norite|42828|5|Briefly described|Fig.2 P128|||||||||
134|Adelong Norite|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sg2||||||
134|Adelong Norite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
134|Adelong Norite|60086|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
210|Alandoon Chert|23173|4|Described|Map Legend|Late Ordovician|Early Ordovician|||||||
210|Alandoon Chert|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
210|Alandoon Chert|42566|3|Fully described|p32|||Reserved as Alandoon||||||
210|Alandoon Chert|42568|5|Briefly described|Map legend|Ordovician|Ordovician|||||||
210|Alandoon Chert|43089|5|Briefly described|Map Legend|||of Girilambone Group||||||
210|Alandoon Chert|65469|5|Briefly described|p15, p16|Middle Ordovician|Middle Orodovician|Lachlan Orogen.||Girilambone Group||||
210|Alandoon Chert|67322|5|Briefly described|p19|Middle Ordovician|Early Ordovician|Age determined from the Ballast Formation. Occurs in the Sussex-Byrock region.||Of Girilambone Group.||Correlative of Whinfell Chert Member, and of chert units in Ballast Formation.||
210|Alandoon Chert|70751|6|Mentioned|p12|Darriwillian|Darriwillian|||Girilambone Group||||
210|Alandoon Chert|72080|4|Described|p2, p4-p6, p11, p12, p14|Darriwilian|Darriwilian|Sampled for conodonts.Contains conodonts which form the basis of the Middle Ordovician age thus suggesting a potential correlation with the Whinfell Chert.||Girilambone Group||Equivalent to the Ballast Formation and the Lang Formation.||07-JAN-22
221|Albert Basalt|30604|6|Mentioned|p68|||||||||
221|Albert Basalt|30687|5|Briefly described|p65|||See also P66,77. Tertiary age||||||
221|Albert Basalt|30689|5|Briefly described|p76|||Also mention Table on P76||||||
221|Albert Basalt|31130|6|Mentioned|Fig. 2|||L. Miocene||||||
221|Albert Basalt|32923|5|Briefly described|p27|||Analysis P29.||||||
221|Albert Basalt|32924|6|Mentioned|p111|||Extrusive of Focal Peak Shield Volcano.||||||
221|Albert Basalt|33290|4|Described|p37|||Anal. p39.||||||23-JUL-08
221|Albert Basalt|35050|6|Mentioned|p130|||||||||
221|Albert Basalt|35296|6|Mentioned|p12|||Re stratigraphy||||||
221|Albert Basalt|36806|5|Briefly described|p131|||||||||
221|Albert Basalt|39445|5|Briefly described|Table 14|||||||||
221|Albert Basalt|39969|6|Mentioned|p2|||||||||
221|Albert Basalt|40623|5|Briefly described|p39|||||||||
221|Albert Basalt|40896|4|Described|p45|||||||||
221|Albert Basalt|43005|5|Briefly described|p213|||||||||
221|Albert Basalt|43161|6|Mentioned|32|||||||||
221|Albert Basalt|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
221|Albert Basalt|44813|14|Not recorded|p80,86,90||Tertiary|20-0 Ma.||||||
221|Albert Basalt|48917|6|Mentioned|p38|||One map symbol for all units of Lamington Volcanics||||||
221|Albert Basalt|61007|6|Mentioned|p293|||||||||
221|Albert Basalt|69599|5|Briefly described|p631, p640|||Focal Peak volcano, between the Main Range and Tweed volcanoes. Table of chemical analyses.|25-20 Ma.|||Underlies the Beechmont Basalt. Equivalent to the Kyogle Basalt in NSW.||
221|Albert Basalt|73450|4|Described|p92, p96, p98|||Associated with the Focal Peak volcano. Comprises numerous thin flows averaging about 10 m thick with maximum thickness of 440 m; thins to the northeast.|||||Alkaline to subalkaline basalts; commonly microphenocrystic in olivine and/or plagioclase with sparse amygdales.|
221|Albert Basalt|73581|5|Briefly described|p7|||||Focal Peak Volcanics||Underlies Lamington Volcanics||
234|Albury Gneiss|30909|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
234|Albury Gneiss|31278|6|Mentioned|Fig. 2|||||||||
234|Albury Gneiss|31800|6|Mentioned|p205|||||||||
234|Albury Gneiss|34544|6|Mentioned|p183|||||||||
234|Albury Gneiss|35278|6|Mentioned|p362|||||||||
234|Albury Gneiss|40328|4|Described|p202|||||||||
234|Albury Gneiss|40497|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
234|Albury Gneiss|40498|6|Mentioned|p392|||||||||
234|Albury Gneiss|45003|14|Not recorded|p16,26|||||||||
234|Albury Gneiss|70910|14|Not recorded|p46|||Refers to Joplin (1947).||||||
237|Alcheringa Coal|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Horshoe Creek (spelt Horshoe Creek) Subgroup.   Geological Province: Sydney Basin||||||
237|Alcheringa Coal|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Horseshoe Creek Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
237|Alcheringa Coal|29942|3|Fully described|p11|||||||||
237|Alcheringa Coal|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Horseshoe Creek Sub-group.||Overlies Clifford Formation. Is overlain by Strathmore Formation.|A distinctive coal-rich sequence with tuffaceous claystone beds.|
279|Allandale Formation|22591|6|Mentioned|p 66|||||||||
279|Allandale Formation|22610|5|Briefly described|Fig 1|||Maximum thickness 300m.||||||12-NOV-08
279|Allandale Formation|22857|5|Briefly described|p522 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Conglomerate, lithic sandstone. Max. thickness: 150m. Geological Province: Sydney Basin.||||||
279|Allandale Formation|22970|5|Briefly described|Plate 6|Permian||||||||
279|Allandale Formation|23540|6|Mentioned|p 420|||||||||
279|Allandale Formation|24079|5|Briefly described|p432|Early Permian|Late Carboniferous|Of Dalwood Group.  Geological Province: Sydney Basin.||||||
279|Allandale Formation|24121|5|Briefly described|p4, p139|||Of Dalwood Group. Spelt Allendale Formation p139.||||||25-AUG-22
279|Allandale Formation|24547|6|Mentioned|p24|||Of the Dalwood Group. Fossils indicate a broad correlation with some parts of the Golden Valley Group.||||||10-MAY-04
279|Allandale Formation|29436|6|Mentioned|p317|||Permian||||||
279|Allandale Formation|29437|6|Mentioned|p136|||||||||
279|Allandale Formation|29728|6|Mentioned|p394|||||||||
279|Allandale Formation|29744|6|Mentioned|p5|||||||||
279|Allandale Formation|29752|6|Mentioned|p34|||||||||
279|Allandale Formation|29915|6|Mentioned|p68|||||||||
279|Allandale Formation|30340|6|Mentioned|Table 3|||||||||
279|Allandale Formation|30341|5|Briefly described|p135|||Permian age||||||
279|Allandale Formation|30450|6|Mentioned|p49|||See also Table 1. Permian age||||||
279|Allandale Formation|30545|6|Mentioned|Fig.2|||Sakmarian. See also P24||||||
279|Allandale Formation|31081|6|Mentioned|p58|||See also Fig. 2||||||
279|Allandale Formation|31298|6|Mentioned|p16|||||||||
279|Allandale Formation|31598|6|Mentioned|p46|||||||||
279|Allandale Formation|31883|6|Mentioned|Table 1|||||||||
279|Allandale Formation|32094|6|Mentioned|p383|||||||||
279|Allandale Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis Konincki||||||
279|Allandale Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
279|Allandale Formation|32840|6|Mentioned|Table 5|||||||||
279|Allandale Formation|32943|6|Mentioned|p86|||Eurydesma cordatum also in fig.2 & pp94,99,105.||||||20-SEP-18
279|Allandale Formation|32945|6|Mentioned|p74|||See also p83,87 & Fig.1.||||||20-SEP-18
279|Allandale Formation|32946|6|Mentioned|p910|||Bivalves.||||||20-SEP-18
279|Allandale Formation|33701|6|Mentioned|Fig.1|||Sakmarian.||||||
279|Allandale Formation|33711|6|Mentioned|p382|||See also Table 2||||||
279|Allandale Formation|33867|5|Briefly described|p4|||||||||
279|Allandale Formation|34043|6|Mentioned|p449|||||||||
279|Allandale Formation|34099|6|Mentioned|p17|||Perm.||||||
279|Allandale Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
279|Allandale Formation|34170|6|Mentioned|p45|||Lower Permian||||||
279|Allandale Formation|34292|6|Mentioned|Table 1|||Permian||||||
279|Allandale Formation|34444|6|Mentioned|Map legend|Permian|Permian|||||||
279|Allandale Formation|34445|4|Described|p320|||Permian. Synon. "Allandale Stage" of Dalwood Group.||||||12-NOV-08
279|Allandale Formation|34447|5|Briefly described|p318|||Permian. Dalwood Group. See Fig.5.2||||||
279|Allandale Formation|34448|4|Described|p431|||Permian||||||
279|Allandale Formation|34512|6|Mentioned|p52|||Lower Permian||||||
279|Allandale Formation|34533|6|Mentioned|p1289|||||||||
279|Allandale Formation|34568|6|Mentioned|p218|||Permian||||||
279|Allandale Formation|34569|6|Mentioned|p11|||Upper Ordovician||||||
279|Allandale Formation|35284|6|Mentioned|Fig.1.|||||||||
279|Allandale Formation|35530|6|Mentioned|p3|||Location of Bivalvia fossils.||||||
279|Allandale Formation|35862|6|Mentioned|p267|||||||||
279|Allandale Formation|36042|6|Mentioned|Table 1|||||||||
279|Allandale Formation|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
279|Allandale Formation|37082|6|Mentioned|p160|||||||||
279|Allandale Formation|37086|6|Mentioned|p183|||||||||
279|Allandale Formation|37087|6|Mentioned|p192|||||||||
279|Allandale Formation|37092|6|Mentioned|p229|||||||||
279|Allandale Formation|37922|5|Briefly described|p483|||||||||
279|Allandale Formation|38204|6|Mentioned|p79|||||||||
279|Allandale Formation|38837|6|Mentioned|p232|||||||||
279|Allandale Formation|38917|6|Mentioned|p164|||||||||
279|Allandale Formation|39262|6|Mentioned|p122|||||||||
279|Allandale Formation|39287|6|Mentioned|p20|||See also Fig.2.5||||||
279|Allandale Formation|39288|4|Described|p57|||||||||
279|Allandale Formation|39304|5|Briefly described|p364|||Fauna. See also Fig. 19.2||||||
279|Allandale Formation|39307|6|Mentioned|p438|||Foraminifera||||||
279|Allandale Formation|39833|6|Mentioned|p297|||||||||
279|Allandale Formation|40166|6|Mentioned|Table 1|||See also Fig.2||||||
279|Allandale Formation|40636|6|Mentioned|p43|||||||||
279|Allandale Formation|40997|6|Mentioned|p413|||||||||
279|Allandale Formation|41315|6|Mentioned|p148|||||||||
279|Allandale Formation|41580|5|Briefly described|p7|||||||||
279|Allandale Formation|41902|5|Briefly described|p5 Table 1|||||||||
279|Allandale Formation|42000|6|Mentioned|p55|||||||||
279|Allandale Formation|42250|6|Mentioned|p26|||||||||
279|Allandale Formation|42925|5|Briefly described|Table 1||Early Permian|||||||
279|Allandale Formation|42994|6|Mentioned|p234|||||||||
279|Allandale Formation|43017|5|Briefly described|Fig.1,p372|||||||||
279|Allandale Formation|43018|5|Briefly described|Table 1,p386|||||||||
279|Allandale Formation|43050|5|Briefly described|p9|||||||||
279|Allandale Formation|43194|5|Briefly described|p129 Tb. 8.3|Early Permian|Early Permian|Of Gyarran Volcanics (Hunter region) and Dalwood Group (Newcastle region), Sydney Basin.||||||
279|Allandale Formation|43257|5|Briefly described|Map Legend||Early Permian|Of Dalwood Group.||||||
279|Allandale Formation|43344|14|Not recorded|p84,88||Permian|Formerly Allandale Stage||||||
279|Allandale Formation|43385|14|Not recorded|p179,180||Sakmarian|||||||
279|Allandale Formation|43440|14|Not recorded|p36,73,74,91|||||||||
279|Allandale Formation|43447|4|Described|p16,Table 1||Permian|Part of Dalwood Group.||||||12-NOV-08
279|Allandale Formation|43448|14|Not recorded|p224|||On table only. Unit of Dalwood Group||||||
279|Allandale Formation|43460|14|Not recorded|p96,100|||||||||
279|Allandale Formation|43471|14|Not recorded|p235,251|||Megadesmus, Astartila||||||
279|Allandale Formation|43474|14|Not recorded|p1,fig.1,10,22,25,||Sakmarian|p34,36,53,55,60,61,71,84,92,96||||||
279|Allandale Formation|43475|14|Not recorded|p552||Permian|||||||
279|Allandale Formation|43479|14|Not recorded|p218|Artinskian|Sakmarian|||||||
279|Allandale Formation|43491|14|Not recorded|pVII/44||Permian|||||||
279|Allandale Formation|44040|14|Not recorded|p27|||||||||
279|Allandale Formation|44135|6|Mentioned|p43|||A unit in NSW.||||||07-DEC-09
279|Allandale Formation|44219|14|Not recorded|p29,31||Sakmarian|See also p32,33,35-7,43.||||||
279|Allandale Formation|44348|14|Not recorded|p56|||||||||
279|Allandale Formation|44372|6|Mentioned|p40|||||||||
279|Allandale Formation|44855|14|Not recorded|p18|Permian|Carboniferous|||||||
279|Allandale Formation|44859|14|Not recorded|p69||Early Permian|||||||
279|Allandale Formation|45006|14|Not recorded|Tb.1,opp.p3|||||||||
279|Allandale Formation|45031|14|Not recorded|p25,49-51,64,67||Permian|||||||
279|Allandale Formation|45090|6|Mentioned|p7|||Time correlation chart||||||
279|Allandale Formation|46849|6|Mentioned|p195|||||||||
279|Allandale Formation|47041|6|Mentioned|Fig.2|||||||||
279|Allandale Formation|48926|6|Mentioned|p40|||p41 etc.||||||20-SEP-18
279|Allandale Formation|49644|5|Briefly described|Table|||||||||
279|Allandale Formation|60281|5|Briefly described|p54 |Early Permian|Early Permian|Of the Dalwood Group (lower part). Consists of lithic sandstone and conglomerate containing abundant invertebrate fossils. Overlies the Lochinvar Formation.  Age: 290-286Ma.  Thickness at type section: 150m.  Geological Province: Sydney Basin.||||||
279|Allandale Formation|60290|5|Briefly described|p43|||Contains Eurydesma. Laterally equivalent to Cranky Corner Sandstone.||||||07-FEB-11
279|Allandale Formation|60295|5|Briefly described|p132|Sakmarian|Sakmarian|||||||
279|Allandale Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Correlated with Cranky Corner Sandstone, lower Pebbley Beach Formation, Bundella Formation, Callytharra Formation and Golden Valley Group. Geological Province: Sydney Basin.||||||18-MAY-05
279|Allandale Formation|60330|5|Briefly described|p264|||Overlain by Rutherford Formation with a sharp contact. Dark green volcanolithic sandstone. Geological Province: Sydney Basin.||||||
279|Allandale Formation|60386|6|Mentioned|p296|Artinskian||Bowen/Sydney Basin. Non-marine.||||||
279|Allandale Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: Sydney Basin/ Newcastle area.||||||
279|Allandale Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||13-MAR-09
279|Allandale Formation|61791|6|Mentioned|p325|||||||||
279|Allandale Formation|63172|6|Mentioned|p301|||Of the Dalwood Group in NSW.||||||07-FEB-11
279|Allandale Formation|63832|5|Briefly described|p131 fig 2|Artinskian|Sakmarian|Of Sydney Basin. Sixth (P2) glaciation.||Unit in Dalwood Group.||||13-DEC-17
279|Allandale Formation|64631|5|Briefly described|p44 Fig.2.|Sakmarian|Sakmarian|Sydney Basin. Biostratigraphic age control at top.||Unit in Dalwood Group.||Overlies Lochinvar Formation. Is overlain by Rutherford Formation.||
279|Allandale Formation|68003|5|Briefly described|p38 Fig.3-j.|Early Permian|Early Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Unit in Dalwood Group.||Overlies Lochinvar Formation. Is overlain by Rutherford Formation.||
279|Allandale Formation|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields.||Unit in Dalwood Group.||Overlies Lochinvar Formation. Is overlain by Rutherford Formation.||
279|Allandale Formation|68493|4|Described|p1, p3 Fig.1, p5 Fig.2, p7, p10, p11|Sakmarian|Sakmarian|Shell bed containing the large bivalve Eurydesma specimens. Approximately 150m thick. Deposited mostly during Fielding et al.'s glacial episode P2. Correlation with the International Time Chart is challenging.||Of the Dalwood Group.||Overlies the Lochinvar Formation. Overlain by the Rutherford Formation. Correlative of the Cranky Corner Sandstone and Millfield Farm Formation.|Dominated by interbedded lithic sandstone and conglomerate, and commonly contains abundant invertebrate fossils. Contains a 20 m thick marker bed of dolerite boulder conglomerate.|20-SEP-18
279|Allandale Formation|69297|6|Mentioned|p501|Artinskian|Artinskian|Sydney Basin. ||Dalwood Group||Overlies the Lochinvar Formation. Overlain by the Rutherford Formation.||
279|Allandale Formation|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|||Unit in Gyarran Volcanics.||||
279|Allandale Formation|70096|5|Briefly described|p220-221;Supp1-3|||Of northern Sydney Basin. Comprises volcanic boulder conglomerates in the upper part of the section. See also supplementary files in appendix for additional stratigraphic and locality information.||Unit of Dalwood Group.|Includes Eurydesma beds.|Overlain by Rutherford Formation.||
279|Allandale Formation|73304|6|Mentioned|p75|||||Gyarran Volcanics||||
291|Allaru Mudstone|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|Eromanga Basin. 150-400m thick. Mis-spelt as Allura Mudstone in Tb.1.|||||Calcareous mudstone with interbeds of calcareous siltstone and fine-grained, partly calcareous labile sandstone; contains a rich marine fauna of bivalves, ammonites, gastropods and belemnites.|
291|Allaru Mudstone|13497|5|Briefly described|p115 fig 6.33|Early Cretaceous|Early Cretaceous|Eromanga Basin. Mis-spelt as the  Alluru Mudstone on p146. See also p144 fig 9.2, p145, p146, p148-p154 .||Marree Subgroup||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||
291|Allaru Mudstone|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Albian|In Eromanga Basin.||||||
291|Allaru Mudstone|22747|6|Mentioned|p15|||||||||
291|Allaru Mudstone|22857|5|Briefly described|p296-7 Tb.22.1, p314|Albian|Albian|Of the Rolling Downs Group. Black and grey claystone. Max. thickness: ~100m. (inc. Toolebuc Mudstone). Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6, p544 App.1 Tb.A1.12.||||||
291|Allaru Mudstone|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Albian|||||||
291|Allaru Mudstone|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Mackunda Formation, underlying unit is Toolebuc Formation||||||
291|Allaru Mudstone|22912|5|Briefly described|33|||Geological province: Eromanga  Basin.||||||30-JAN-07
291|Allaru Mudstone|23054|6|Mentioned|Fig5p22|||||||||
291|Allaru Mudstone|23056|6|Mentioned|12 table 2|||||||||
291|Allaru Mudstone|23065|5|Briefly described|18|||Geological province: Carpentaria Basin. Of the Rolling Downs Group.||||||30-JAN-07
291|Allaru Mudstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Of the Marree Subgroup (Neales River Group).||||||30-JAN-07
291|Allaru Mudstone|23155|4|Described|p32|Albian|Albian|Allaru Mudstone is laterally equivalent to the middle and upper parts of the Oodnadatta Formation, and the name Allaru Mudstone is only used when Toolebuc Formation is present.  The unit is Albian in age based on spore-pollen assemblages.||||||29-APR-10
291|Allaru Mudstone|23375|4|Described|Fig2 p265||Albian|Laterally equivalent to upper Oodnadatta Formation. In the Eromanga Basin.||||||30-JAN-07
291|Allaru Mudstone|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
291|Allaru Mudstone|23425|4|Described|Table 9.7 p394||Albian|Also see p378. Of Rolling Downs Group. Overlain by Normanton Formation; underlain by Toolebuc Formation - conformable. Geological Province Carpentaria Basin. Max. thickness 700 m.||||||16-SEP-08
291|Allaru Mudstone|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
291|Allaru Mudstone|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
291|Allaru Mudstone|23916|6|Mentioned|p534|Albian|Albian|||||||
291|Allaru Mudstone|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
291|Allaru Mudstone|24048|5|Briefly described|p76|||||||||
291|Allaru Mudstone|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group. Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|24085|5|Briefly described|p33, p36|Albian|Albian|||||||
291|Allaru Mudstone|24092|5|Briefly described|p8 Fig.3|||Of Rolling Downs Group. Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|24175|5|Briefly described|p28, p17 Fig. 3|Albian|Albian|Supersedes Allaru Member.  Transitionally overlain by Mackunda Formation.  Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
291|Allaru Mudstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Cooper Basin.||||||
291|Allaru Mudstone|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
291|Allaru Mudstone|29591|6|Mentioned|Table 72|||||||||
291|Allaru Mudstone|30019|6|Mentioned|p2|||||||||
291|Allaru Mudstone|30020|5|Briefly described|p30|||||||||
291|Allaru Mudstone|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30103|6|Mentioned|p6|||||||||
291|Allaru Mudstone|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30446|6|Mentioned|p38|||||||||
291|Allaru Mudstone|30539|6|Mentioned|p28|||Late middle Albian age||||||
291|Allaru Mudstone|30584|4|Described|Table 1|||||||||
291|Allaru Mudstone|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30691|4|Described|p17|||See also Table4,6.Lower Cretaceous. Part of Wilgunya Sub-group.||||||30-JAN-07
291|Allaru Mudstone|30804|5|Briefly described|Table 2|||||||||
291|Allaru Mudstone|30853|5|Briefly described|Table 3|||Albian age.||||||
291|Allaru Mudstone|30854|4|Described|Table 4|||Upper Albian age||||||
291|Allaru Mudstone|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Unit of Rolling Downs Group||||||
291|Allaru Mudstone|30856|4|Described|Table 3|||Lower Cretaceous||||||
291|Allaru Mudstone|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|31098|6|Mentioned|p10|||||||||
291|Allaru Mudstone|31121|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31145|5|Briefly described|Table 1|||L. Cretaceous||||||
291|Allaru Mudstone|31164|14|Not recorded|p8||Albian|Blue grey mudstone minor calcareous labilie sandstone and cone-in-cone limestone,marine.||||||
291|Allaru Mudstone|31168|6|Mentioned|p10|||||||||
291|Allaru Mudstone|31208|6|Mentioned|Fig. 7|||||||||
291|Allaru Mudstone|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone and labile sandstone.||||||02-DEC-04
291|Allaru Mudstone|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
291|Allaru Mudstone|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
291|Allaru Mudstone|31432|4|Described|Table 1|||L.Cretaceous||||||
291|Allaru Mudstone|31433|5|Briefly described|p6|||L.Cretaceous||||||
291|Allaru Mudstone|31434|3|Fully described|Table 1|||See also p8. L.Cretaceous||||||17-JUL-06
291|Allaru Mudstone|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32274|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32275|5|Briefly described|p9|||||||||
291|Allaru Mudstone|32277|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32314|6|Mentioned|Fig. 4|||||||||
291|Allaru Mudstone|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|32395|4|Described|p6|||Stratigraphic table||||||
291|Allaru Mudstone|32396|6|Mentioned|p6,8||Early Cretaceous|Palynomorphs ? Cenomanian. Marine.||||||
291|Allaru Mudstone|32553|4|Described|p38|||||||||
291|Allaru Mudstone|32705|6|Mentioned|p188|||||||||
291|Allaru Mudstone|32796|6|Mentioned|p303|||||||||
291|Allaru Mudstone|33016|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33017|6|Mentioned|p5|||||||||
291|Allaru Mudstone|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
291|Allaru Mudstone|33069|4|Described|p7|||L.-U. Cret. Rolling Downs Gp.||||||22-DEC-09
291|Allaru Mudstone|33072|4|Described|Table 1|||L.Cret.||||||
291|Allaru Mudstone|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33075|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
291|Allaru Mudstone|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||22-DEC-09
291|Allaru Mudstone|33088|4|Described|Table 3|||L.Cret.||||||
291|Allaru Mudstone|33089|4|Described|Table 2|||L.Cret.||||||
291|Allaru Mudstone|33092|6|Mentioned|p6|||Strat. table.||||||
291|Allaru Mudstone|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33150|4|Described|p8|||L.Cret.||||||
291|Allaru Mudstone|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
291|Allaru Mudstone|33175|6|Mentioned|p280|||||||||
291|Allaru Mudstone|33176|6|Mentioned|p171|||||||||
291|Allaru Mudstone|33177|6|Mentioned|p12|||||||||
291|Allaru Mudstone|33178|6|Mentioned|p11|||||||||
291|Allaru Mudstone|33179|6|Mentioned|Table 3|||||||||
291|Allaru Mudstone|33182|6|Mentioned|Fig.1|||L. Cretaceous||||||
291|Allaru Mudstone|33183|5|Briefly described|p227|||Underlies Normanton Formation.||||||30-JAN-07
291|Allaru Mudstone|33368|6|Mentioned|p24|||Geol.Map.||||||
291|Allaru Mudstone|33372|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|33414|6|Mentioned|p212,213,Tb.|||part of Wilgunya Sub-Group||||||
291|Allaru Mudstone|33448|6|Mentioned|p6|||||||||
291|Allaru Mudstone|33449|6|Mentioned|p7|||||||||
291|Allaru Mudstone|33561|6|Mentioned|p102|||||||||
291|Allaru Mudstone|33638|5|Briefly described|Table 1|||Lower Cret.||||||
291|Allaru Mudstone|33639|5|Briefly described|p11|||L.Cret. See also Table 4||||||
291|Allaru Mudstone|33640|4|Described|Table 2|||L.Cret.||||||
291|Allaru Mudstone|33642|5|Briefly described|p145,147,151,Table 1|||||||||
291|Allaru Mudstone|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|33648|6|Mentioned|p21|||Strat.||||||
291|Allaru Mudstone|33772|6|Mentioned|p13|||||||||
291|Allaru Mudstone|33773|6|Mentioned|p17|||||||||
291|Allaru Mudstone|33825|6|Mentioned|Table 4|||||||||
291|Allaru Mudstone|33832|5|Briefly described|p11|||Strat. and correlation||||||17-JUL-06
291|Allaru Mudstone|33900|6|Mentioned|p21|||||||||
291|Allaru Mudstone|33964|4|Described|p6|||||||||
291|Allaru Mudstone|34065|4|Described|p6|||L.Cret.||||||
291|Allaru Mudstone|34091|4|Described|Table 1|||L.Cretaceous. Of the Rolling Downs Group.||||||30-JAN-07
291|Allaru Mudstone|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34218|5|Briefly described|Table 2|||Lower Cretaceous.||||||
291|Allaru Mudstone|34356|6|Mentioned|p21|||Lower Cretaceous.||||||
291|Allaru Mudstone|34485|6|Mentioned|Table 1|||See also Table 2. Lower Cretaceous||||||
291|Allaru Mudstone|34486|4|Described|Table 1|||See also Table 2. Lower Cretaceous||||||
291|Allaru Mudstone|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|34611|4|Described|Fig.65|||Wilgunya Sub-Group.||||||16-SEP-08
291|Allaru Mudstone|34619|6|Mentioned|p.160, Pl.22||Early Cretaceous|||||||
291|Allaru Mudstone|34811|4|Described|Table 1|||||||||
291|Allaru Mudstone|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35139|4|Described|Table.2|||||||||
291|Allaru Mudstone|35239|6|Mentioned|p258|||||||||
291|Allaru Mudstone|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35560|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
291|Allaru Mudstone|35811|5|Briefly described|Table 3|||||||||
291|Allaru Mudstone|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
291|Allaru Mudstone|36012|3|Fully described|Table 5|||See also p20.||||||17-JUL-06
291|Allaru Mudstone|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|36243|6|Mentioned|Table 6A|||||||||
291|Allaru Mudstone|36251|4|Described|p3|||||||||
291|Allaru Mudstone|36552|6|Mentioned|Fig.25|||||||||
291|Allaru Mudstone|36571|6|Mentioned|p98|||See also Table 4.||||||
291|Allaru Mudstone|37263|6|Mentioned|Fig.14|||||||||
291|Allaru Mudstone|37451|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|37608|3|Fully described|Table 1|||See also Table 2||||||
291|Allaru Mudstone|38226|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|38372|6|Mentioned|p651|||||||||
291|Allaru Mudstone|38373|6|Mentioned|p622|||||||||
291|Allaru Mudstone|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
291|Allaru Mudstone|38780|6|Mentioned|p17|||||||||
291|Allaru Mudstone|38814|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlies Toolebuc Formation.||||||25-AUG-04
291|Allaru Mudstone|39070|4|Described|p365|||||||||
291|Allaru Mudstone|39211|5|Briefly described|Fig.3|||See also Figs 9,11-16,19 etc. Correlation||||||
291|Allaru Mudstone|39445|5|Briefly described|Table 11|||||||||
291|Allaru Mudstone|39478|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|39575|6|Mentioned|p103|||||||||
291|Allaru Mudstone|39708|6|Mentioned|p478|||||||||
291|Allaru Mudstone|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
291|Allaru Mudstone|39846|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|39847|5|Briefly described|p40|||||||||
291|Allaru Mudstone|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|39943|6|Mentioned|Table 8A|||||||||
291|Allaru Mudstone|39989|4|Described|p424|||||||||
291|Allaru Mudstone|40121|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|40199|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|40249|6|Mentioned|p41|||||||||
291|Allaru Mudstone|40452|6|Mentioned|p2|||||||||
291|Allaru Mudstone|40623|5|Briefly described|p111|||||||||
291|Allaru Mudstone|40648|6|Mentioned|p12|||||||||
291|Allaru Mudstone|40670|6|Mentioned|Fig.9|||||||||
291|Allaru Mudstone|40675|6|Mentioned|Table 8A|||||||||
291|Allaru Mudstone|40687|3|Fully described|p418|||||||||
291|Allaru Mudstone|40801|6|Mentioned|p42|||||||||
291|Allaru Mudstone|40833|6|Mentioned|p468|||||||||
291|Allaru Mudstone|40926|6|Mentioned|p18|||||||||
291|Allaru Mudstone|41012|5|Briefly described|p137|||||||||
291|Allaru Mudstone|41060|6|Mentioned|Fig.3|||Generalized stratigrapgy||||||
291|Allaru Mudstone|41062|6|Mentioned|Fig.5|||||||||
291|Allaru Mudstone|41063|6|Mentioned|p40|||||||||
291|Allaru Mudstone|41064|6|Mentioned|Fig.4|||||||||
291|Allaru Mudstone|41084|5|Briefly described|Fig.2|||||||||
291|Allaru Mudstone|41086|3|Fully described|p98, Fig.3|||||||||
291|Allaru Mudstone|41087|3|Fully described|p127|||||||||
291|Allaru Mudstone|41088|6|Mentioned|p141|||||||||
291|Allaru Mudstone|41097|6|Mentioned|Table 1|||||||||
291|Allaru Mudstone|41099|6|Mentioned|Fig.9|||||||||
291|Allaru Mudstone|41117|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|41121|6|Mentioned|p179|||||||||
291|Allaru Mudstone|41165|5|Briefly described|p362|||See also Fig.15||||||
291|Allaru Mudstone|41175|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|41176|6|Mentioned|Table 2|||||||||
291|Allaru Mudstone|41177|6|Mentioned|p225|||||||||
291|Allaru Mudstone|41178|6|Mentioned|p242|||||||||
291|Allaru Mudstone|41182|5|Briefly described|Fig.2|||||||||
291|Allaru Mudstone|41183|6|Mentioned|Fig.3 p308|||||||||
291|Allaru Mudstone|41187|6|Mentioned|Fig.2|||||||||
291|Allaru Mudstone|41214|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|41216|6|Mentioned|Fig.18|||||||||
291|Allaru Mudstone|41266|6|Mentioned|Fig.3|||||||||
291|Allaru Mudstone|41306|6|Mentioned|p4|||||||||
291|Allaru Mudstone|41307|6|Mentioned|p5|||||||||
291|Allaru Mudstone|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
291|Allaru Mudstone|41523|3|Fully described|p279|||See also p281.||||||
291|Allaru Mudstone|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
291|Allaru Mudstone|41568|5|Briefly described|p15|||||||||
291|Allaru Mudstone|42003|6|Mentioned|p141|||||||||
291|Allaru Mudstone|42061|5|Briefly described|p157|||See also Fig.11||||||
291|Allaru Mudstone|42071|6|Mentioned|p117|||See also Fig.2A p116||||||
291|Allaru Mudstone|42084|6|Mentioned|Fig.3 P356|||||||||
291|Allaru Mudstone|42085|6|Mentioned|Fig.2 P374|||||||||
291|Allaru Mudstone|42397|6|Mentioned|Fig.2 P3|||||||||
291|Allaru Mudstone|42429|6|Mentioned|Fig.10 P156|||||||||
291|Allaru Mudstone|42446|4|Described|p14|||||||||
291|Allaru Mudstone|42447|6|Mentioned|Fig.1|||||||||
291|Allaru Mudstone|42496|5|Briefly described|p136, Fig.3 p132|||||||||
291|Allaru Mudstone|42520|5|Briefly described|p6|||||||||
291|Allaru Mudstone|42588|5|Briefly described|p115|||||||||
291|Allaru Mudstone|42637|5|Briefly described|p11|||||||||
291|Allaru Mudstone|42673|5|Briefly described|Fig.2, P184|||||||||
291|Allaru Mudstone|42746|6|Mentioned|Fig.6 P8|||||||||
291|Allaru Mudstone|42749|6|Mentioned|Fig.2 P27|||||||||
291|Allaru Mudstone|42804|5|Briefly described|p115|||||||||
291|Allaru Mudstone|43002|5|Briefly described|Fig.2,p135|||||||||
291|Allaru Mudstone|43004|5|Briefly described|Table 1,p179|||||||||
291|Allaru Mudstone|43105|6|Mentioned|p15|||||||||
291|Allaru Mudstone|43114|5|Briefly described|p16|||||||||
291|Allaru Mudstone|43122|5|Briefly described|Fig.2.|||||||||
291|Allaru Mudstone|43591|6|Mentioned|p40|||||||||
291|Allaru Mudstone|43602|6|Mentioned|191|||In Eromanga Basin, Rolling Downs Group||||||
291|Allaru Mudstone|43630|6|Mentioned|p70|||also Fig.4||||||
291|Allaru Mudstone|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44017|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44020|14|Not recorded|Tb.1,2||Early Cretaceous|Of Rolling Downs Gruop.||||||
291|Allaru Mudstone|44031|14|Not recorded|p3,Tb.1,p8||Cretaceous|||||||
291|Allaru Mudstone|44034|4|Described|Tb.1,p2,4,5,9,10|||||||||
291|Allaru Mudstone|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44082|6|Mentioned|p3,4,10,12,20,24,28||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
291|Allaru Mudstone|44091|14|Not recorded|p60|||Part of Wilgunya Sub-Group.||||||
291|Allaru Mudstone|44098|14|Not recorded|p98||Cretaceous|||||||
291|Allaru Mudstone|44112|6|Mentioned|p82|||||||||
291|Allaru Mudstone|44133|5|Briefly described|p104 Fig. 9.11, 122|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Conformably underlies: Mackunda Formation.||||||
291|Allaru Mudstone|44308|14|Not recorded|p11|||||||||
291|Allaru Mudstone|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
291|Allaru Mudstone|44807|14|Not recorded|p3,Tb.1,p8||Cretaceous|||||||
291|Allaru Mudstone|45103|6|Mentioned|p8|||||||||
291|Allaru Mudstone|45110|6|Mentioned|Table 18|||||||||
291|Allaru Mudstone|45132|6|Mentioned|p17|||||||||
291|Allaru Mudstone|45145|3|Fully described|Table 5|||||||||
291|Allaru Mudstone|45161|6|Mentioned|p67|||||||||
291|Allaru Mudstone|46791|5|Briefly described|p48|||||||||
291|Allaru Mudstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
291|Allaru Mudstone|46939|6|Mentioned|Fig.1|||See also Table 1.||||||
291|Allaru Mudstone|47042|6|Mentioned|p171|||||||||
291|Allaru Mudstone|48920|3|Fully described|p61|||Cretaceous age||||||
291|Allaru Mudstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
291|Allaru Mudstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
291|Allaru Mudstone|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
291|Allaru Mudstone|50332|5|Briefly described|p22|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone.||||||07-FEB-11
291|Allaru Mudstone|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone, labile sandstone.||||||19-JUL-04
291|Allaru Mudstone|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Toolebuc Formation. Overlain by the Mackunda Formation. Geological Province: Eromanga Basin.||||||
291|Allaru Mudstone|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Mudstone, calcareous siltstone.||||||
291|Allaru Mudstone|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Toolebuc Formation. Overlain by Mackunda Formation. Interfingers laterally with Oodnadatta Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
291|Allaru Mudstone|61014|6|Mentioned|p533 Fig.2.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Wallumbilla Formation.||
291|Allaru Mudstone|61312|5|Briefly described|p75, p79 Table E2|Cretaceous|Cretaceous|Of Rolling Downs Group. In Queensland, consists of mainly blue-grey mudstone with interbeds of thin calcareous siltstone. Forms marine deposits in deeper parts of the Eromanga Basin. Absent in NSW. Overlies Toolebuc Formation. See also p64, p67 Fig. E5||||||
291|Allaru Mudstone|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
291|Allaru Mudstone|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|62028|5|Briefly described|p10 Fig. 1|||||||||
291|Allaru Mudstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin?||||||11-FEB-10
291|Allaru Mudstone|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Age: ~96-~94Ma. Geological Province: Northern Gulf of Carpentaria, Southern Cape York and Burketown Depression.||||||01-MAR-10
291|Allaru Mudstone|63113|6|Mentioned|p1219 Fig.8. |||||||Overlies Lawn Hill Formation.||
291|Allaru Mudstone|63979|2|Defined|p49, p51-52, Fig. 44|Albian|Albian|Top unit of Wilgunyah Subgroup (Rolling Downs Gp). Formerly Allaru Member (Wilgunyah Fm). Conformable on Toolebuc Formation or Wallumbilla Formation;conformable below Mackunda Fm. Max.thick: 400m. Detailed lithology provided. Geol.prov: Eromanga Basin|||||Primarily blue-grey mudstone (partly pyritic) and interbedded calcareous siltstone, cone-in-cone limestone and lesser sandstone.|29-APR-16
291|Allaru Mudstone|64048|6|Mentioned|p64 Tb. 2|||Geological Province: Eromanga Basin.||||||07-FEB-11
291|Allaru Mudstone|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Overlies Toolebuc Formation; is overlain by Mackunda Formation.||10-DEC-15
291|Allaru Mudstone|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
291|Allaru Mudstone|64820|5|Briefly described|pS6 Fig. 4|Albian|Albian|Of the Rolling Downs Group. Medium-grained galuconitic sandstone grading up into interbedded siltstone and sandstone. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
291|Allaru Mudstone|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||17-FEB-10
291|Allaru Mudstone|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Toolebuc Formation. Overlain by Mackunda Formation.||||||08-MAR-12
291|Allaru Mudstone|65489|5|Briefly described|p49, p55, p58-59, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 300m thick. Appears as Allaru Formation on p155. Regional seal.||||Overlies Toolebuc Formation. Is overlain by Mackunda Formation.||
291|Allaru Mudstone|65925|5|Briefly described|Appendix 2.|||||||||
291|Allaru Mudstone|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin. ||Unit in Rolling Downs Group.|||Deeper marine shale and mudstone.|
291|Allaru Mudstone|66623|3|Fully described|p242, pp256-257, pp264-266.|Albian|Albian|Formerly a member of Wilgunya Formation (Casey 1959), Allaru Member (Vine and Day 1965), reinstated as a Formation (Vine et al. 1967). Very poorly exposed: mudstone-dominated and masked by silcrete gibbers. Thickness from 87 m to 270 m. Wide range of fossils. Partly equivalent to Griman Creek and Oodnadatta Formations,Yalpunga Formation, lower half of Yalpunga Beds, and to the diachronous base of Mackunda Formation.||Unit in Rolling Downs Group.||Is conformably overlain by Winton Formation. In QLD, overlies Toolebuc Formation and underlies Mackunda Formation. Gradationally overlies Coreena Member (Wallumbilla Formation).|Blue shale with interbedded buff to grey, calcareous, fossiliferous fine silty sandstone, siltstone and mudstone; local gypsiferous concretions of calcareous, chocolate-brown shale exhibit cone-in-cone structures.|07-JUN-13
291|Allaru Mudstone|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Carpentaria and Eromanga Basins.||||||
291|Allaru Mudstone|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.||Overlies Coreena Member of Wallumbilla Formation. Is overlain by Cordillo Silcrete.|Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|
291|Allaru Mudstone|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|||Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|
291|Allaru Mudstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Late Cretaceous|Late Cretaceous|See also p86-87, p92-93, p94 Fig.12.4, p95 Fig.12.5, p96. Eromanga/Carpentaria Basins. Widespread shallow-marine deposits.||||Overlies Toolebuc Formation. Is overlain by Mackunda, Normanton Formations.|Mudstone, calcareous siltstone.|
291|Allaru Mudstone|67402|4|Described|p26, p26 tbl RRM4, p29, p29 fig PSA4|Albian|Albian|Eromanga Basin. Maximum thickness of 400m in the Eromanga Basin but may be up to 700m thick in the Carpentaria Basin. Proven regional seal for hydrocarbons. See also PSA5, p108-p112, p113 fig ERO12, p115 tbl ERO2, p123, p176, p177, p179 fig CRP/KRM6, p181.||Rolling Downs Group||Overlies the Wallumbilla Formation. Overlain by the Mackunda Formation.|Consists primarily of marine mudstone interbedded with calcareous siltstone, very fine-grained, laminated sandstone, shale and limestone.|
291|Allaru Mudstone|67784|6|Mentioned|p28-29, p33|Albian|Albian|See also references to Allaru Formation (p25-26, p32).||||||08-FEB-18
291|Allaru Mudstone|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Hydrocarbon seal.|||||Shaly limestone, marl, organic-rich (10% TOC) limestone, sandstone.|
291|Allaru Mudstone|68206|6|Mentioned|p32|Albian|Albian|NE Eromanga Basin. See also references to Allaru Formation (p31, 33).||||||
291|Allaru Mudstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
291|Allaru Mudstone|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Toolebuc Formation. Is overlain conformably by Mackunda Formation.||
291|Allaru Mudstone|68731|6|Mentioned|pp209-211|||||||||
291|Allaru Mudstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (NE). Shallow marine.||Of the Rolling Downs Group.||||
291|Allaru Mudstone|69019|5|Briefly described|p85 Fig.21.|Albian|Albian|Southern Eromanga Basin.||||Overlies Toolebuc Formation. Is overlain by Winton and Mackunda Formations.||
291|Allaru Mudstone|69023|6|Mentioned|p89 Fig.20, p102, p105|Albian|Albian|||||Lateral equivalent of Oodnadatta Formation.||
291|Allaru Mudstone|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
291|Allaru Mudstone|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. This unit is a good potential seal. ||Rolling Downs Group||Overlies the Toolebuc Formation. Overlain by the Normanton Formation.|Mudstone, siltstone and claystone.|
291|Allaru Mudstone|69454|6|Mentioned|p38:3|||Eromanga Basin.||||||12-JUL-16
291|Allaru Mudstone|69455|6|Mentioned|p39:4 Fig.39.3|Early Cretaceous|Early Cretaceous|||||||12-JUL-16
291|Allaru Mudstone|69457|3|Fully described|p41:2-3;41:5 Fig.41.4;41:6-8,10-12,17-18|Early Cretaceous|Early Cretaceous|Vine and Day (1965); Vine et al. (1967). Widely distributed: Eromanga and Carpentaria Basins. Entirely subsurface in NT. Quiet water, shallow-marine deposits; generally 200-300m thick, up to 400m. Laterally equivalent to middle and upper parts of Oodnadatta Formation; this latter name was previously used to describe the Allaru Mudstone in the NT. Late Albian to ?early Cenomanian age range from palynoflora. The basal part of this unit contains a 40m thick gas-charged interval, and has untested unconventional petroleum potential.||Wilgunya Subgroup.||Conformably overlies Toolebuc or Wallumbilla Formations. Is overlain conformably by Mackunda Formation. Correlative of Oodnadatta Formation.|Mostly blue-grey, partly pyritic mudstone with calcareous siltstone interbeds, cone-in-cone limestone; minor sandstone and limestone. Contains a rich fossil assemblage.|12-JUL-16
291|Allaru Mudstone|69582|5|Briefly described|p22, p25-p26, p29, p65-p66|Upper Cretaceous|Lower Cretaceous|Eromanga Basin. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Toolebuc Formation. Overlain by the Normation Formation and the Mackunda Formation.|Mudstone.|
291|Allaru Mudstone|69594|4|Described|p518-519, p521-522, p526, p529-530|Albian|Albian|See also p531 Fig.7.11, p574. Vine et al. (1967); Vine and Day (1965). Carpentaria, Eromanga Basins. Generally 200-300m thick; up to 350-400m. Generally poor surface expression. Contains rich shallow-marine late Albian macrofauna and microfauna (listed and photographs). Seismic interpretations suggest a significant intraformational unconformity. Appears as Allaru Formation in Fig.7.11.||Rolling Downs Group.||Conformably overlies Toolebuc Formation. Is overlain (conformably) by Normanton, Winton and Mackunda Formations. Is correlated with the Oodnadatta Formation.|Claystone, siltstone, cone-in-cone calcareous mudstone, minor limestone, labile volcanic-derived sandstone, glauconitic sandstone and sporadic coquinite.|
291|Allaru Mudstone|69673|5|Briefly described|ix, p155 fig 127, p156|||Prospective for unconventional hydrocarbons. 200-300m thick.||Wilgunya Subgroup||Overlies Toolebuc Formation, overlain by Mackunda Formation|Mudstone, in parts pyritic with thin interbeds of calcareous siltstone, cone in cone limestone and minor very fine grained sandstone and concretionary limestone.|
291|Allaru Mudstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
291|Allaru Mudstone|69946|3|Fully described|p23, p26-27, p57, p94|Early Cretaceous|Early Cretaceous|Of Casey (1959), who assigned it as the uppermost Member of the Wilgunya Formation. Renamed Allaru Member by Vine and Day (1965); raised to Formation status as Allaru Mudstone by Vine et al. (1967). Type section is on the Richmond-Winton Road, from Richmond S to Twenty-Mile Creek. Its extent is limited by definition to the extent of the Toolebuc Formation. Generally 100-240m thick, to >600m. Late Albian. Wireline log correlations.||||Conformably overlies Toolebuc Formation. Is overlain conformably by Mackunda Formation. Passes laterally into Oodnadatta Formation.|Grey mudstone with thin calcareous siltstone and minor thin, very fine-grained sandstone interbeds identical to the Oodnadatta Formation.|
291|Allaru Mudstone|69947|5|Briefly described|p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
291|Allaru Mudstone|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Toolebuc Formation. Is overlain by Mackunda Formation.||
291|Allaru Mudstone|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Overlies Toolebuc Formation.|Mudstone and calcareous siltstone.|
291|Allaru Mudstone|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Mudstone, calcareous siltstone.|20-JAN-22
291|Allaru Mudstone|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|||Regressive marine and non-marine grey claystone with silty and sandy intervals up-sequence.|20-JAN-22
291|Allaru Mudstone|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p23, p30, p33|Early Cretaceous|Early Cretaceous|See also p80, p82. Surat Basin. Not an equivalent of Oodnadatta Formation.  87m thick in Toompine 1 well; 212.5m thick in Mirintu 1 petroleum well. Low-energy marine deposits. Biotas include benthic and nektonic molluscs, turtles, fish, pliosaurs and a dinosaur. Hydrostratigraphic properties.||Rolling Downs Group.||Conformably overlies Toolebuc Formation or Wallumbilla Formation. Is overlain conformably by Mackunda Formation.|Includes minor calcareous labile (volcanic) sandstone. Includes coquinite beds and hummocky crossbeds.|
291|Allaru Mudstone|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||
291|Allaru Mudstone|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
291|Allaru Mudstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Toolebuc Formation. Overlain by the Mackunda Formation.||24-OCT-19
291|Allaru Mudstone|71342|3|Fully described|Ch3 p4, Ch4 p25|Albian|Albian|Eromanga Basin. Originally named by Casey (1959) as the uppermost member of the Wilgunya Formation. Vine and Day (1965) assigned the name Allaru Member before Vine et al (1967) elevated the mudstone to formation status. Replaces the obsolete Tambo Formation. Casey (1959) assigned the type section on the Richmond-Winton road from Richmond south to Twenty-Mile Creek in Queensland. This unit is generally 100-240m thick in the Cooper region but reaches thicknesses in excess of 600m in the Patchawarra Trough. Deposited in a low energy, shallow marine environment. Spore-pollen zone is given in Ch5 p57. Forms a seal for the Coorikiana Sandstone. See also  Ch5 p23-p27, Ch5 p57, Ch7 p13, Ch11 p5.||||Conformably overlies the Toolebuc Formation. Conformably overlain by the Mackunda Formation.|Grey mudstone with thin calcareous siltstone and minor thin, very fine-grained sandstone interbeds identical to the Oodnadatta Formation.|
291|Allaru Mudstone|71382|5|Briefly described|p4, p9, p11, p13, p16-p17|||Eromanga Basin. Intersected in GSQ Julia 1 from 0-156.65m for a total of 156.65m thickness. Deposited during widespread shallow marine conditions. Temp log and stratlog are provided. Lithology is described in detail on p22. See also p21-p23, p25, p27, App 3, 4.||||Overlies the Toolebuc Formation.|Mudstone interbedded with sandstone.|07-OCT-22
291|Allaru Mudstone|71601|6|Mentioned|p120, p121|Albian|Albian|NW Qld. Includes dinosaur fossils provisionally assigned to Minmi.||||||
291|Allaru Mudstone|71855|4|Described|p2, p4-p5, p9-p10, p13, p15, p27|Cretaceous|Cretaceous|Eromanga and Carpentaria basins. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure is discussed. See also p33-p35, p50, p52-p53, p56-p57, p61-p62, p75.||||Conformably (gradationally) overlies the Toolebuc Formation.|Light grey, predominantly non-calcareous mudstone, and calcareous in part mudstone.|
291|Allaru Mudstone|71863|5|Briefly described|p4-p5, p7-p9|Albian|Albian|Eromanga Basin and Carpentaria basins. Deposited in a marine incursion.||Rolling Downs Group||Conformably overlies the Toolebuc Formation. Overlain by the Normanton Formation, Mackunda Formation and the Winton Formation.||
291|Allaru Mudstone|72297|5|Briefly described|p753|||Eromanga Basin.||||Conformably overlies the Toolebuc Formation.||
291|Allaru Mudstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin.||Rolling Downs Group.||Overlies Toolebuc FZ. Is overlain by Mackunda or Normanhurst FZ.||
291|Allaru Mudstone|72913|6|Mentioned|p8.|||Two wells intersected this cover unit.|||||Includes mudstone.|
291|Allaru Mudstone|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
291|Allaru Mudstone|73083|6|Mentioned|p62, p77|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
291|Allaru Mudstone|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Leaky aquitard.||Rolling Downs Group||Underlain by Toolebuc Formation. Overlain by Normanton Formation.||
291|Allaru Mudstone|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Toolebuc Formation. Is overlain by Normanton Formation.||
291|Allaru Mudstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
291|Allaru Mudstone|73249|5|Briefly described|p319, p321||Albian|Eromanga Basin.||||Lateral equivalent to the Oodnadatta Formation, overlies the Allaru Formation, underlies the Mackunda Formation.|Siltstone and mudstone dominated.|
291|Allaru Mudstone|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Toolebuc Formation. Overlain by Mackunda Formation. Equivalent to Oodnadatta Formation.||
291|Allaru Mudstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
291|Allaru Mudstone|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Toolebuc Formation. Overlain by Mackunda Formation. Equivalent to Oodnadatta Formation.||
291|Allaru Mudstone|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 100 Ma|||Overlies Toolebuc Formation, underlies Mackunda Formation||
317|Alma Granite Gneiss|29864|6|Mentioned|p284|||||||||
317|Alma Granite Gneiss|64097|5|Briefly described|p302, 328|Paleoproterozoic|Paleoproterozoic|Superseded Alma Gneiss. Of Thackaringa Gp. Underlies Cues Fm. Previous correlations with lower Stephens Creek Granite Gneiss invalid. Age:1704 +/- 3 Ma.Now interpreted as syn-sed. granitic intrusion (metagranite), as is Rasp Ridge Granite Gneiss also||||||14-MAY-13
317|Alma Granite Gneiss|64741|6|Mentioned|p310|||See Alma Gneiss for detailed information.||||||07-FEB-11
317|Alma Granite Gneiss|70000|5|Briefly described|p34, p36|Statherian|Statherian|The oldest of the sill-like granitic plutons of the Silver City Suite. Intrusion under shallow cover was syn-depositional.|1704 +/- 3 Ma (Page, Stevens and Gibson 2005).|Unit in Silver City Suite.||Intrudes Cues Formation.||
317|Alma Granite Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Silver City Suite.|||Quartz-feldspar-biotite +/- garnet gneiss, with feldspar megacrysts, or aggregates of quartz+feldspar; minor basic gneiss, calc-silicate and metasedimentary rock.|
317|Alma Granite Gneiss|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian||1704 +/- 3 Ma|||||
317|Alma Granite Gneiss|73308|6|Mentioned|p607 Fig.1||||1704 +/- 3 Ma.|||||
317|Alma Granite Gneiss|73482|5|Briefly described|p430|Statherian|Statherian|Abbreviated as Alma p422 Fig.3.|1704+/-3 Ma||||Granite gneiss.|
317|Alma Granite Gneiss|73512|6|Mentioned|p2|||||||||
317|Alma Granite Gneiss|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p836|Statherian|Statherian|See also Alma Gneiss p826.|1704+/-3 Ma||Silver City Suite||Intrusive sill.|
335|Althorpe Formation|40805|2|Defined|p141|Permian|Permian|Previously used as Althorpe Claystone Member||||||
335|Althorpe Formation|41010|6|Mentioned|p13|||||||||
335|Althorpe Formation|42078|6|Mentioned|Table 1 P5|||||||||
335|Althorpe Formation|42648|6|Mentioned|p37|||||||||
335|Althorpe Formation|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Jerrys Plain Subgroup.||||||
335|Althorpe 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.||||||
335|Althorpe Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. About 2 m thick. Usually found overlying Redbank Creek seam.||Unit in Jerrys Plains Subgroup.||Overlies Malabar Formation. Is overlain by Mount Leonard Formation.|Tuffaceous claystone.|
335|Althorpe Formation|69683|6|Mentioned|p411 Fig.2, p415 Fig.3|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.||||
335|Althorpe Formation|70878|5|Briefly described|p710, p712|Permian|Permian|Hunter Valley. 1.39m thick in Amoco Wybong 1 well.||Wittingham Coal Measures.|||Includes tuff layers.|
342|Alum Mountain Volcanics|22580|6|Mentioned|p97|||||||||
342|Alum Mountain Volcanics|22601|2|Defined|407|Early Permian||||||||
342|Alum Mountain Volcanics|22612|6|Mentioned|423-425|Early Permian|Early Permian|Parent Tamworth Belt. Max thickness 530 m||||||
342|Alum Mountain Volcanics|22857|4|Described|P258, p504 App.1 Tb.A1.8|Early Permian|Early Permian|Contains Lakes Road Rhyolite and Burdekins Gap Basalt Members. Flows of albitised alkaline olivine basalt and massive to flow-banded rhyolite with interbedded pebble conglomerate and coal seams at base. Max. thickness: 2040m in Stroud-Gloucester Syncline.||||||
342|Alum Mountain Volcanics|22864|6|Mentioned|p258||Permian|||||||
342|Alum Mountain Volcanics|23102|5|Briefly described|p562|||||||||
342|Alum Mountain Volcanics|23157|6|Mentioned|p109||Permian|||||||
342|Alum Mountain Volcanics|23459|5|Briefly described|p157|Early Permian|Early Permian|ca 280Ma||||||
342|Alum Mountain Volcanics|23540|5|Briefly described|p 420|||Also see p 425. Divided into upper and lower.||||||
342|Alum Mountain Volcanics|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Max. thickness: 2000m.   Geological Province: New England Fold Belt||||||
342|Alum Mountain Volcanics|24040|5|Briefly described|p469, p475|Permian|Permian|Geological province: Gloucester and Myall Basins.  See also the informal Alum Mountains volcanics (Fig. 1). Contains basalts previously mapped with the Dalwood Group.||||||21-AUG-08
342|Alum Mountain Volcanics|24118|5|Briefly described|p3|Permian|Permian|||||||
342|Alum Mountain Volcanics|31802|4|Described|p137|||||||||
342|Alum Mountain Volcanics|32324|6|Mentioned|Table 8.1|||||||||
342|Alum Mountain Volcanics|32379|6|Mentioned|Fig.3|||||||||
342|Alum Mountain Volcanics|32671|6|Mentioned|Map legend|Permian|Permian|||||||
342|Alum Mountain Volcanics|32868|6|Mentioned|p210|||||||||
342|Alum Mountain Volcanics|34059|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
342|Alum Mountain Volcanics|34072|6|Mentioned|Fig.4.5|||Contains Rhacopteris. Carb.||||||
342|Alum Mountain Volcanics|34085|6|Mentioned|Cor.chart|||Stephanian - Sakmarian||||||
342|Alum Mountain Volcanics|34168|5|Briefly described|p254|||Carboniferous||||||
342|Alum Mountain Volcanics|34169|6|Mentioned|p252|||Correlation||||||
342|Alum Mountain Volcanics|34238|6|Mentioned|p10|||||||||
342|Alum Mountain Volcanics|34239|6|Mentioned|p264|||||||||
342|Alum Mountain Volcanics|34374|6|Mentioned|p255|||||||||
342|Alum Mountain Volcanics|34445|6|Mentioned|p319|||||||||
342|Alum Mountain Volcanics|34556|6|Mentioned|p269|||||||||
342|Alum Mountain Volcanics|35050|6|Mentioned|p130|||||||||
342|Alum Mountain Volcanics|35803|6|Mentioned|p321|||||||||
342|Alum Mountain Volcanics|36045|6|Mentioned|p330|||||||||
342|Alum Mountain Volcanics|36057|1|Redefined|p350|Early Permian|Late Carboniferous|Late Carboniferous - Early Permian.||||||12-NOV-08
342|Alum Mountain Volcanics|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
342|Alum Mountain Volcanics|37099|5|Briefly described|p255|||||||||
342|Alum Mountain Volcanics|38801|6|Mentioned|p121|||||||||
342|Alum Mountain Volcanics|38816|6|Mentioned|p9|||||||||
342|Alum Mountain Volcanics|38837|6|Mentioned|p233|||||||||
342|Alum Mountain Volcanics|39308|5|Briefly described|p489|||||||||
342|Alum Mountain Volcanics|39660|6|Mentioned|p449|||||||||
342|Alum Mountain Volcanics|41054|5|Briefly described|p155|||||||||
342|Alum Mountain Volcanics|41461|5|Briefly described|p13|||||||||
342|Alum Mountain Volcanics|42547|5|Briefly described|p36|||||||||
342|Alum Mountain Volcanics|42798|6|Mentioned|p55|||||||||
342|Alum Mountain Volcanics|42833|3|Fully described|p225|||see also Fig.1 p224 and Fig.2 p225.||||||21-AUG-08
342|Alum Mountain Volcanics|43017|5|Briefly described|Fig.1,p372|||||||||
342|Alum Mountain Volcanics|43432|14|Not recorded|p209|||Equivalent||||||
342|Alum Mountain Volcanics|43437|14|Not recorded|p169-175||Carboniferous|||||||
342|Alum Mountain Volcanics|43447|14|Not recorded|Table 1&2,p10,11,14||Carboniferous|||||||
342|Alum Mountain Volcanics|43451|14|Not recorded|Map Legend||Carboniferous|||||||
342|Alum Mountain Volcanics|43479|14|Not recorded|p162||Carboniferous|||||||
342|Alum Mountain Volcanics|44093|5|Briefly described|p230 App. 1|Early Permian|Early Permian|Bimodal volcano-sedimentary sequence.||||||
342|Alum Mountain Volcanics|44244|2|Defined|p224, p164|Early Permian|Early Permian|Overlies Muirs Creek Conglomerate and Johnsons Creek Conglomerate; disconformably underlies Markwell Coal Measures or Bulahdelah Formation, and Dewrang Group..  Max. thickness: 2040m.  Type section in text.  Geological Province: Myall Block.||||||16-JAN-12
342|Alum Mountain Volcanics|45097|6|Mentioned|p26|||Glossopteris flora low in formation||||||
342|Alum Mountain Volcanics|50099|5|Briefly described|p11|Early Permian|Early Permian|Suite of bimodal volcanics dominantly basaltic, with subordinate andesite, dacite and rhyolite. Underlies Gloucester Coal Measures. Geological Province: Tamworth Belt/New England Orogen.||||||
342|Alum Mountain Volcanics|50147|5|Briefly described|Map legend|Early Permian|Early Permian|Geological Province: Western Myall Block.||||||
342|Alum Mountain Volcanics|50263|5|Briefly described|Map Legend|Sakmarian|Sakmarian|Geological Province: Western Myall Block.||||||
342|Alum Mountain Volcanics|61772|6|Mentioned|p128 Fig. 1||Carboniferous|In text, Volcanics is V. In New England Orogen.||||||
342|Alum Mountain Volcanics|61791|6|Mentioned|p325, p326 Fig. 2|Permian|Carboniferous|||||||
342|Alum Mountain Volcanics|61801|6|Mentioned|p403, p404|||||||||
342|Alum Mountain Volcanics|63832|6|Mentioned|p131 fig 2|Kungurian|Sakmarian|Myall block, Southern New England Fold Belt. Sixth (P2) glaciation.||||||
342|Alum Mountain Volcanics|64631|5|Briefly described|p44 Fig.2.|Artinskian|Sakmarian|Southern New England Fold Belt, Myall Block. Shown in 2 parts with significant hiatus/unconformity within the Artinskian. Some biostratigraphic and radiometric age control within both parts. ||||||
342|Alum Mountain Volcanics|65107|5|Briefly described|p289|Early Permian|Early Permian|age:274.1+/-3.4Ma from SHRIMP U-PB zircons. Constrains Paleomag results from Myall block and New England Orogen (NEO) paleo pole path, with Nerong Volcanics||||||24-NOV-09
342|Alum Mountain Volcanics|65114|5|Briefly described|p383 Tb.1, p396|Cisuralian||ca 275 Ma; Tectonic unit: Gloucester Basin and Myall Basin; presumably part of an originally more extensive volcanic suite||||||21-SEP-09
342|Alum Mountain Volcanics|69793|6|Mentioned|p1121 Fig.12|Artinskian|Artinskian|Myall Block, Tamworth Belt.||||||
342|Alum Mountain Volcanics|70329|5|Briefly described|p1-6|Permian|Permian|Southernmost New England Orogen. Sourced from a depleted upper asthenosphere. Exposures form an oval ridge. Maximum thickness is 1800m. Paleomagnetic data tabulated.|271.8 +/- 1.8 Ma (Li et al., 2014).||||Basalt, andesite, dacite, rhyolite flows, breccias, welded-ash flows and ash-fall tuffs. Metamorphosed to lower than greenschist facies.|
342|Alum Mountain Volcanics|70939|5|Briefly described|p832|Permian|Permian|Indicates extension in the Southern New England Orogen was still active at c.274 Ma. Appears as Alum Mt Volcanics.|274 +/- 3.4 Ma: U-Pb zircon: Roberts et al. (1995)|||||
342|Alum Mountain Volcanics|71115|5|Briefly described|p192-194|Permian|Permian|Gloucester Syncline, Myall Block, New England Orogen. Paleomagnetism, and paleomagnetic poles for c.265 Ma, discussed.|271.8 +/- 1.8 Ma (40Ar/39Ar; Li et al., 2014).||||Basaltic to rhyolitic flow deposits and ash-fall tuffs.|
342|Alum Mountain Volcanics|71264|6|Mentioned|p582 Fig.5|||Gloucester and Myall Synclines.||||||
342|Alum Mountain Volcanics|73197|6|Mentioned|p475 Fig.6|Lopingian|Guadalupian|New England Orogen, southern.|||||Volcanics.|
342|Alum Mountain Volcanics|73202|5|Briefly described|p262, p627 Fig.1, p639 Fig.10|Early Permian|Early Permian|Gloucester Basin, base. Resulted from large degrees of asthenospheric melting and has flat REE patterns, eNd = +5.61 to +8.73 (Caprarelli and Leitch, 2001). 274.1 +/- 3.4 Ma SHRIMP magmatic zircon age (Roberts et al., 1995), 271.8 +/- 1.8 Ma age from Li et al., 2014).|274.1 +/- 3.4 Ma, 271.8 +/- 1.8 Ma||||Consists of basalt, andesite, dacite and rhyolite.|
342|Alum Mountain Volcanics|73303|6|Mentioned|p67|Kungurian|Kungurian|Sydney Basin. 'upper Echinolosia preovalis' brachiopod range-zone dated at 276.8 +/- 3.4 Ma U-Pb SHRIMP (Black et al., 2003; Roberts et al., 1995).|276.8 +/- 3.4 Ma U-Pb SHRIMP|Brooweena Formation||||
342|Alum Mountain Volcanics|73487|5|Briefly described|p563-567, p570-571, p574, p576-577, p584|Artinskian|Asselian|Myall blocks. Gloucester Synclines. Hiatus-bound. Correlated with a different volcanic succession in the Myall Syncline. See also p568 Fig.3, p581 Fig.10.|ca 274 Ma, ca 272 Ma||Lakes Road Rhyolite Member||Ignimbritic in parts. Includes rhyolites.|
344|Alum Rock Conglomerate|22601|2|Defined|405, 403-405, 407|Permian|Permian|||||||
344|Alum Rock Conglomerate|30914|6|Mentioned|Map legend|Permian|Devonian|Devonian ? - Permian||||||
344|Alum Rock Conglomerate|37252|6|Mentioned|Map legend|Permian|Permian|||||||
344|Alum Rock Conglomerate|38806|6|Mentioned|p72|||||||||
344|Alum Rock Conglomerate|39252|5|Briefly described|p16|||||||||
344|Alum Rock Conglomerate|39445|5|Briefly described|Table 7|||See also p90, p93, Fig.8 and Table 8. Earliest Permian.||||||12-DEC-07
344|Alum Rock Conglomerate|42559|6|Mentioned|p9|||Used by Lucas in 1958. Superseded informally by Alum Rock beds herein.||||||
344|Alum Rock Conglomerate|43008|5|Briefly described|map legend|||||||||
344|Alum Rock Conglomerate|43745|6|Mentioned|p16|Sakmarian|Sakmarian|(Early Sak.-Late Sak.)||||||
344|Alum Rock Conglomerate|44543|2|Defined|p29|||Overlies Thanes Creek Slate. Lower Permian fossils.||||||
344|Alum Rock Conglomerate|44565|2|Defined|p230-233|||||||||
344|Alum Rock Conglomerate|48940|6|Mentioned|p49|||Refers Lucas (1958)||||||
344|Alum Rock Conglomerate|61772|6|Mentioned|p128||Early Permian|In New England Orogen.||||||27-MAY-08
344|Alum Rock Conglomerate|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, locally pebbly arenite, and minor siltstone; rhyolitic to locally dacitic breccia, tuff and some lava with minor calcareous arenite and limestone.||||||
344|Alum Rock Conglomerate|63732|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, locally pebbly sandstone, and siltstone; rhyolitic to locally dacitic breccia, tuff and lava; minor calcareous arenite and limestone; locally fossiliferous.||||||
344|Alum Rock Conglomerate|63748|4|Described|p17, p49, p68|Sakmarian|Asselian|Of Lucas (1958); forms narrow outlier within Texas beds. Age: 291.3+/-2.8Ma. Lower conglomerate, pebbly arenite, arenite + minor siltstone, and upper rhyolitic to locally dacitic breccia, tuff with some lava with minor calcareous arenite and limestone.||||||07-FEB-11
344|Alum Rock Conglomerate|64098|5|Briefly described|p337|||Includes volcanic rocks.||||||
344|Alum Rock Conglomerate|65107|6|Mentioned|p287|Permian|Permian|Permian inlier in the Texas beds.||||||
344|Alum Rock Conglomerate|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; SHRIMP zircon ages on rhyolite from this unit yielded ages of 293.7 +/- 3.4 and 291.3 +/- 2.8 Ma||||||21-SEP-09
344|Alum Rock Conglomerate|67908|6|Mentioned|p283|Permian.|Permian.|Texas Orocline. Early Permian. Appears in text as Alum Rock Formation.|||||Conglomerate layers and interbedded arenite, siltstone and volcaniclastic layers.|
344|Alum Rock Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Bondonga, Pikedale, Silver Spur and Terrica beds, are all mapped under the symbol, Par.||||||
344|Alum Rock Conglomerate|68679|4|Described|p452, p455|Permian|Permian|First mapped by Lucas (1958). Forms a narrow, 20km long NW-trending belt, 30km NW of Stanthorpe; Silver Spur Subprovince, Woolomin Province. Contains Asselian-Sakmarian brachiopods at base and top.|291.3 +/- 2.8 Ma (SHRIMP: Roberts et al., 1996).|||Unconformably overlies Texas beds.|Lower half is brownish bedded conglomerate (mainly pebbles from Texas beds), pebbly lithic to volcaniclastic sandstone and minor siltstone; upper half is rhyolitic to dacitic breccia, tuff and some lava with minor calcareous sandstone and limestone.|
344|Alum Rock Conglomerate|68901|6|Mentioned|p8 Fig.iii|Permian|Permian|||||||26-SEP-18
344|Alum Rock Conglomerate|73421|6|Mentioned|p17|Sakmarian|Asselian|New England Orogen, southern. U-Pb zircon SHRIMP ages of 293.7+/-2.8 Ma and 291.3+/-2.8 Ma U-Pb (Roberts et al., 1996) adjusted to approx. 296 Ma and 294 Ma due to use of the SL13 standard, supports late Asselian to earliest Sakmarian age.|Approx. 294 Ma and 296 Ma U-Pb zircon SHRIMP|||||
344|Alum Rock Conglomerate|73487|5|Briefly described|p563, p582 Fig.11, p574 Fig.8, p585-586|Cisuralian|Cisuralian|New England Orogen, eastern limb of Texas Orocline. Referred to as Alum Rock Conglomerate volcanics p585-586.|ca 293 Ma (Roberts et al., 1996)||||Includes volcanic rocks.|
357|Amboyne Granodiorite|22815|4|Described|p44|Silurian|Silurian|Intruded Yalmy Group.||||||
357|Amboyne Granodiorite|22876|5|Briefly described|p28|||Bullenbalong Suite||||||
357|Amboyne Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Bullenbalong Suite. G71. Cordierite-garnet-biotite granodiorite. S-Type.||||||26-OCT-04
357|Amboyne Granodiorite|23309|5|Briefly described|p63, 113, 121, 303, 338, 465||Early Silurian|(G71). Age: U/Pb Zircon 430+/-3Ma, K/Ar Biotite 427+/-3 / 415+/-8 / 407+/-13Ma.  Includes McKillops Bridge Granodiorite (G72). Of Bullenbalong Suite.||||||
357|Amboyne Granodiorite|23615|3|Fully described|p154, p153 Tb. 2|Silurian|Silurian|Of Bullenbalong Suite.  See also p231 App 2.  Intrudes the Bendoc and Yalmy Groups.  Age 407+/-13Ma (Evernden & Richards, 1962) and 427+/-3Ma Henley and Webb, 1990).; 427+/-3Ma (Henley & Webb, 1990).||||||
357|Amboyne Granodiorite|23938|5|Briefly described|p54 Tb. 4|||See also p127.||||||25-SEP-08
357|Amboyne Granodiorite|24551|5|Briefly described|p132 Fig.5.23, p234, 728 Table 8.11, 440|||||||||
357|Amboyne Granodiorite|40761|6|Mentioned|p239|||||||||
357|Amboyne Granodiorite|41850|6|Mentioned|p431|||||||||
357|Amboyne Granodiorite|41905|2|Defined|p77|Silurian||||||||
357|Amboyne Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
357|Amboyne Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
357|Amboyne Granodiorite|42647|3|Fully described|p47|||||||||
357|Amboyne Granodiorite|42827|6|Mentioned|p431|||||||||
357|Amboyne Granodiorite|43206|5|Briefly described|map legend||Wenlock|Of Bullenbalong Suite.||||||
357|Amboyne Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||11-JAN-10
357|Amboyne Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb13.||||||
357|Amboyne Granodiorite|44185|5|Briefly described|Map legend.|Silurian|Silurian|S-type.||||||
357|Amboyne Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
357|Amboyne Granodiorite|60503|6|Mentioned|p78|Llandovery|Llandovery|Age: 427+/-3Ma. ||||||
357|Amboyne Granodiorite|61160|5|Briefly described|p120|Silurian|Silurian|Age: 430Ma. ||||||
357|Amboyne Granodiorite|61181|5|Briefly described|p16|||Contains a barite-calcite lode close to its faulted contact with Warbisco Shale on the Deddick River; the lode is reported to be 1m wide and near vertical. ||||||
357|Amboyne Granodiorite|68115|5|Briefly described|p4, p6.|Paleozoic|Paleozoic|Orth et al. (1995). Now includes the former Deddick Granodiorite (of Chappell et al. 1991) on its western side. Deddick Zone.||||||11-FEB-13
357|Amboyne Granodiorite|68116|5|Briefly described|Appendix, Maps 28, 36.|Wenlock|Llandovery||||||Biotite-cordierite granodiorite: medium grained; dark grey; abundant inclusions; S-type.|
357|Amboyne Granodiorite|75072|6|Mentioned|p236|||Deddick Valley, East Victoria. Contains mid-crustal metasedimentary xenoliths with U-Pb zircon age peaks at c.430 Ma.||||||
381|Amphitheatre Group|730|4|Described|p23, p24, p27, p32.|Devonian|Devonian|Cobar Sub-basin, Darling Basin. Three deep-water turbidite sequences; lower thin-bedded unit is CSA Siltstone. Middle unit is sandier and more thickly-bedded, called Biddabirra Formation. Probably faulted over Kopyje Group.||||||11-NOV-14
381|Amphitheatre Group|5252|5|Briefly described|p61; p62 Fig.2; p63; throughout article.|Early Devonian|Pridoli|Of Cobar Supergroup, Cobar Basin. Includes outcrop of thin sandstones and reddish purple siltstones. Conformable but diachronous with overlying Winduck Group.||||||
381|Amphitheatre Group|22518|4|Described|Table 1, p 4, 10||Late Silurian|Darling Basin||||||
381|Amphitheatre Group|22768|5|Briefly described|p170-71|||||||||
381|Amphitheatre Group|22773|5|Briefly described|Fig24.5p350|Early Devonian|Silurian|||||||
381|Amphitheatre Group|22857|4|Described|p170, p436 App.1, Tb.A1.6|Devonian|Devonian|Of the Cobar Supergroup. Geological Province: Cobar Basin. Equivalents mentioned on p350 Fig. 24.5.||||||
381|Amphitheatre Group|22887|5|Briefly described|Fig.5 p12|Middle Devonian||||||||
381|Amphitheatre Group|22893|6|Mentioned|p90 fig4|||Name given to Cobar Supergroup rocks when describing Dolmoreve No.1 drill hole.||||||
381|Amphitheatre Group|22935|5|Briefly described|p253||Early Devonian|||||||
381|Amphitheatre Group|23054|6|Mentioned|p24|||||||||
381|Amphitheatre Group|23095|5|Briefly described|p610 (table 1)|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|23096|6|Mentioned|p602|||Cobar Supergroup||||||
381|Amphitheatre Group|23098|5|Briefly described|p587|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|23101|5|Briefly described|p567 (Fig 1)|||||||||
381|Amphitheatre Group|23171|5|Briefly described|p15,22,40|||||||||
381|Amphitheatre Group|23173|4|Described|Map Legend|Lochkovian||||||||
381|Amphitheatre Group|23522|5|Briefly described|p249 Fig 5|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|23734|5|Briefly described|p12 Fig. 1|||Includes upper and lower mudstones and sandstones, the Biddabirra Formation, Shume Formation and the CSA Siltstone.||||||
381|Amphitheatre Group|24241|5|Briefly described|p15 Fig.2|Devonian|Silurian|Geological Province: Darling Basin.||||||17-MAR-05
381|Amphitheatre Group|29680|6|Mentioned|Fig.1|||||||||
381|Amphitheatre Group|29947|4|Described|p685|||||||||
381|Amphitheatre Group|29948|6|Mentioned|Fig.12|||||||||
381|Amphitheatre Group|29984|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|29987|6|Mentioned|p25|||||||||
381|Amphitheatre Group|30075|6|Mentioned|Fig.2|||||||||
381|Amphitheatre Group|32087|6|Mentioned|p17|||||||||
381|Amphitheatre Group|32619|6|Mentioned|p459|||Fauna||||||
381|Amphitheatre Group|32853|6|Mentioned|p58|||||||||
381|Amphitheatre Group|32865|6|Mentioned|p485|||||||||
381|Amphitheatre Group|32918|6|Mentioned|p12|||Refers Rade (1963 unpubl.)||||||
381|Amphitheatre Group|33004|6|Mentioned|p190|||||||||
381|Amphitheatre Group|33732|4|Described|p100|||||||||
381|Amphitheatre Group|34035|6|Mentioned|p544|||||||||
381|Amphitheatre Group|34057|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
381|Amphitheatre Group|34109|6|Mentioned|p165|||||||||
381|Amphitheatre Group|34400|5|Briefly described|p8|||Lower Devonian. See also P11.||||||
381|Amphitheatre Group|34403|4|Described|p148|||||||||
381|Amphitheatre Group|34404|6|Mentioned|Fig.3.8|||Lower - ?Middle Devonian||||||
381|Amphitheatre Group|34405|6|Mentioned|Fig.3.9|||Correlation Chart||||||
381|Amphitheatre Group|34406|6|Mentioned|p223|||||||||
381|Amphitheatre Group|34449|4|Described|p21|||L.- M.Devonian||||||
381|Amphitheatre Group|35232|6|Mentioned|p10|||||||||
381|Amphitheatre Group|35287|6|Mentioned|Table 1|||||||||
381|Amphitheatre Group|35385|6|Mentioned|Table 1|||Comparison of past and present stratigraphic schemes for the Cobar area.||||||08-APR-09
381|Amphitheatre Group|35925|4|Described|p1|||||||||
381|Amphitheatre Group|36214|6|Mentioned|p57|||||||||
381|Amphitheatre Group|37798|6|Mentioned|p128|||||||||
381|Amphitheatre Group|38064|6|Mentioned|p39|||||||||
381|Amphitheatre Group|38292|3|Fully described|p3|||||||||
381|Amphitheatre Group|38593|6|Mentioned|p90|||||||||
381|Amphitheatre Group|39083|6|Mentioned|p30|||||||||
381|Amphitheatre Group|39618|6|Mentioned|Table 1|||||||||
381|Amphitheatre Group|40130|6|Mentioned|p205|||||||||
381|Amphitheatre Group|40595|6|Mentioned|Fig.7|||||||||
381|Amphitheatre Group|40676|6|Mentioned|p28|||||||||
381|Amphitheatre Group|41085|6|Mentioned|p88|||||||||
381|Amphitheatre Group|41090|6|Mentioned|Fig.1|||||||||
381|Amphitheatre Group|41126|6|Mentioned|p107|||||||||
381|Amphitheatre Group|41138|6|Mentioned|Map legend|Pragian|Lochkovian|Pragian-Lochkovian||||||
381|Amphitheatre Group|41276|6|Mentioned|p62|||||||||
381|Amphitheatre Group|41394|2|Defined|p59|middle Pragian|late Lochkovian|||||||
381|Amphitheatre Group|41395|6|Mentioned|Map legend|Pragian|Lochkovian|||||||
381|Amphitheatre Group|41410|5|Briefly described|p295|||||||||18-JAN-10
381|Amphitheatre Group|41528|2|Defined|p75|Early Devonian||||||||
381|Amphitheatre Group|41529|6|Mentioned|Map legend|Early Devonian||||||||
381|Amphitheatre Group|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
381|Amphitheatre Group|41821|4|Described|p32|||||||||
381|Amphitheatre Group|41872|6|Mentioned|p8|||||||||
381|Amphitheatre Group|42033|6|Mentioned|p652|||||||||
381|Amphitheatre Group|42144|5|Briefly described|p603|||||||||
381|Amphitheatre Group|42208|6|Mentioned|Fig.1 P305|||||||||
381|Amphitheatre Group|42521|5|Briefly described|p15, Figs|||||||||
381|Amphitheatre Group|42566|5|Briefly described|Fig.5 P11|||||||||
381|Amphitheatre Group|42907|6|Mentioned|Fig.8, P8|||||||||
381|Amphitheatre Group|42966|5|Briefly described|Fig. 25 p47|||||||||
381|Amphitheatre Group|42983|6|Mentioned|p343|||||||||
381|Amphitheatre Group|43032|3|Fully described|p64|||Of Cobar Supergroup.||||||08-APR-09
381|Amphitheatre Group|43089|5|Briefly described|Map Legend|||Of Cobar Supergroup.||||||08-APR-09
381|Amphitheatre Group|43090|5|Briefly described|Map legend|Pragian|Lochkovian|Of Cobar Supergroup.||||||08-APR-09
381|Amphitheatre Group|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||
381|Amphitheatre Group|43202|6|Mentioned|p17|||||||||
381|Amphitheatre Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
381|Amphitheatre Group|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
381|Amphitheatre Group|43369|14|Not recorded|Map Legend|||||||||
381|Amphitheatre Group|43379|14|Not recorded|Map Legend|Early Devonian|Middle Devonian|||||||
381|Amphitheatre Group|43380|14|Not recorded|Map Legend|Early Devonian|Middle Devonian|||||||
381|Amphitheatre Group|43381|14|Not recorded|Map Legend|Early Devonian|Middle Devonian|||||||
381|Amphitheatre Group|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
381|Amphitheatre Group|43388|14|Not recorded|Map Legend||Early Devonian|||||||
381|Amphitheatre Group|43389|14|Not recorded|Map Legend||Early Devonian|||||||
381|Amphitheatre Group|43398|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Siluro-Dev.- L.Dev)||||||
381|Amphitheatre Group|43461|14|Not recorded|p619, table p621|Siegenian|Gedinnian|||||||
381|Amphitheatre Group|43479|14|Not recorded|p123,151|Middle Devonian|Early Devonian|||||||
381|Amphitheatre Group|43491|14|Not recorded|pV/14||Middle Devonian|||||||
381|Amphitheatre Group|43510|14|Not recorded|p46|||See also Lexicon||||||
381|Amphitheatre Group|43684|5|Briefly described|p253||Early Devonian|||||||
381|Amphitheatre Group|43757|5|Briefly described|p510|||||||||
381|Amphitheatre Group|43774|1|Redefined|p44-47||Devonian|||||||
381|Amphitheatre Group|43859|5|Briefly described|15|||Conformable under Winduck Group.||||||08-APR-09
381|Amphitheatre Group|44133|6|Mentioned|p45|Devonian|Devonian|||||||
381|Amphitheatre Group|46032|14|Not recorded|p.413|Middle Devonian|Early Devonian|= Amphitheatre Beds. (H55-14/Cobar).||||||
381|Amphitheatre Group|46973|6|Mentioned|p51|||||||||
381|Amphitheatre Group|47050|6|Mentioned|p244|||||||||
381|Amphitheatre Group|49038|6|Mentioned|p22|||||||||
381|Amphitheatre Group|49040|6|Mentioned|p6|||||||||
381|Amphitheatre Group|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Cobar Supergroup.  Informally divided into upper anf lower units. Geological Province: Cobar Basin.||||||
381|Amphitheatre Group|61213|5|Briefly described|p317 Fig. 2|Early Devonian|Early Devonian|Possibly interfingers with Winduck Group. Geological Province: Darling Basin.||||||
381|Amphitheatre Group|61311|5|Briefly described|p43 Table D1|Early Devonian|Late Silurian|Turbitdite sequence of rocks. Geological Province: Darling Basin.||||||
381|Amphitheatre Group|61314|5|Briefly described|p120|Early Devonian|Early Devonian|Of the Cobar Supergroup. Geological Province: Murray Basin.||||||
381|Amphitheatre Group|61817|5|Briefly described|p80|Early Devonian|Early Devonian|Deep-water turbidites.  Geological Province: Cobar Basin.||||||
381|Amphitheatre Group|61905|5|Briefly described|p136|||||||||
381|Amphitheatre Group|61964|6|Mentioned|p67|||Of the Cobar Supergroup. On THE MEADOWS map sheet area.||||||
381|Amphitheatre Group|63632|5|Briefly described|649|||Marine deposits comprising deep shelf and basin facies, westwards.||||||
381|Amphitheatre Group|64962|5|Briefly described|p202||Early Devonian|Geological province: Cobar Basin. Upper section comprises deep-water turbidites; lower section consists of turbidites, very minor volcanic rocks and minor limestone. Low-grade metasedimentary rocks host the McKinnon s mine.||||||
381|Amphitheatre Group|64967|5|Briefly described|p112 Fig. 1, p113, p114 Fig. 2|Emsian|Late Silurian|Geol.province: Darling Basin/Blantyre Sub-basin. Deeper marine deposits.Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113).||||||08-APR-09
381|Amphitheatre Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cobar. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
381|Amphitheatre Group|65469|5|Briefly described|p14-p17, p43|Early Devonian|Late Silurian|Lachlan Orogen. Informally sub-divided into an upper and lower component on p43, p55 and p62. See also p52, p55 fig 3-19, p62, p67, p81, p131, p341.|||Includes the CSA Siltstone, Shume Formation and the Biddabirra Formation.|||
381|Amphitheatre Group|67870|5|Briefly described|p58, p62|Early Devonian|Early Devonian|Western Darling Basin. Marine shelf and basin deposits.||||Is overlain unconformably by Mulga Downs Group.||
381|Amphitheatre Group|68823|6|Mentioned|p376 Fig.3, p377, p378 Fig.4, p404|Early Devonian|Late Silurian|Makes up most of the Cobar Basin. Lachlan and western Thomson Orogens. Sediments sourced mostly from the west; locally from Thule Granite to the south.|||Includes the Alley Sandstone Member.||Siliciclastic turbidites.|
381|Amphitheatre Group|69002|5|Briefly described|p11, p14, p15, Map 1b, Legend|Early Devonian|Early Devonian||||Includes the Biddabirra Formation.||Comprises siliclastic sedimentary rocks.|
381|Amphitheatre Group|69042|5|Briefly described|map legends|Early Devonian|Early Devonian|Dcs. Cobar Basin, Lachlan Orogen. Includes non-magnetic metasediments.||||||
381|Amphitheatre Group|69043|6|Mentioned|p11|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|69511|5|Briefly described|p1-2, p6, p14, p22|||Contains Lochkovian trilobites and brachiopods. Hosts an unnamed granite dated at c.423 Ma.||||Interfingers with Mount Halfway Volcanics. Is intruded by the 422.5 Ma Gilgunnia Granite. Is faulted against the Thule Granite.||
381|Amphitheatre Group|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Late Silurian|Lachlan Orogen.||||||
381|Amphitheatre Group|70037|5|Briefly described|p309 Fig.2, p310-311, p327|Early Devonian|Late Silurian|Rayner (1962). Previously the Amphitheatre Stage of Andrews (1913). Darling Basin. Marine deposits.||||Is overlain by or interfingers with Winduck Group.|Thin- to medium-bedded sandstone and thinly laminated siltstone, thin limestone beds and minor felsic volcanics; overlain by thin- to medium-bedded sandstone and siltstone overlain by coarse-grained beds.|
381|Amphitheatre Group|70383|6|Mentioned|p51|Devonian|Devonian|Cobar area. Thought to be a source of fossiliferous (fish) sandstone boulders in the Bulldog Shale.||||||
381|Amphitheatre Group|70602|6|Mentioned|p67 Fig 3|Devonian|Devonian|||Cobar Supergroup||||
381|Amphitheatre Group|70718|5|Briefly described|p20|Early Devonian|Early Devonian|Darling Basin. A deep to shallow marine depositional environment is interpreted for this group.||Cobar Supergroup||Overlain by the Winduck Group.|Clastic sediments.|
381|Amphitheatre Group|70751|5|Briefly described|p1, p5-p6, p12-p13, p15, p25-p26, p31|Devonian|Late Silurian|Cobar Superbasin, Kopyje Shelf. Can be subdivided into the informal lower and upper parts which are seperated by the Shume Formation.||Cobar Supergroup|||Fine- to medium-grained turbidites including quartz-rich and quartz-lithic sandstones and siltstones.|
381|Amphitheatre Group|70821|5|Briefly described|p11|Early Devonian|Late Silurian|Deep-water turbidites. Typically non-magnetic.||Cobar Supergroup.||||01-DEC-16
381|Amphitheatre Group|70876|5|Briefly described|p1, p16, p20, p76|||Cobar Basin. Deposited in a deep water marine environment.||Cobar Supergroup|Includes the Shume Formation.|Nonconformably overlies the Thule Granite.|Turbidite deposits.|
381|Amphitheatre Group|70941|6|Mentioned|p78 fig 32|Early Devonian|Early Devonian|||||Overlies the Great Cobar Slate and the CSA Siltstone.||
381|Amphitheatre Group|70950|5|Briefly described|p1028-1029,1033-1034,1038-1039, 1040|Early Devonian|Silurian|Geological province: Cobar Basin, Central Lachlan Orogen. Detailed mineralisation analysis provided.|||Includes Shume Formation.||Deep water fine- to medium-grained turbidites; Greywacke, siltstone, shale, felsic volcaniclastic units|
381|Amphitheatre Group|71039|5|Briefly described|p3, p6, p14-p16, p18-p19, p28|||Referred to as the Lower Amphitheatre Group on p14. Divided into the Northwestern, Northeastern and Southern portions in this study. See also p21, p23-26.|||Includes the Biddabirra Formation and the CSA Siltstone.|Intruded by the Gilgunnia Granite and the Boolahbone Granite.||09-MAR-23
381|Amphitheatre Group|71285|5|Briefly described|p538-539, p548-p549|Early Devonian|Late Silurian|Cobar region. Part of the Cobar Basin fill.||Cobar Supergroup.|Biddabirra Formation, CSA Siltstone.|||07-DEC-18
381|Amphitheatre Group|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Cobar Supergroup.|Biddabirra Formation.|||
381|Amphitheatre Group|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.||Cobar Supergroup.|Shume Formation, CSA Siltstone, Biddabirra Formation.|||
381|Amphitheatre Group|71860|6|Mentioned|p6|Early Devonian|Early Devonian|||||||
381|Amphitheatre Group|72908|5|Briefly described|p3-4, p18, p21|Lochkovian|Pridoli|Cobar Basin. Early Lochkovian minimum age.|||lower Amphitheatre Group, Shume Formation, upper Amphitheatre Group||Fine- to medium-grained turbidites.|
381|Amphitheatre Group|72958|6|Mentioned|p9, p11-12, p21, p29, p37|Pragian|Pridoli|Cobar Basin. Nymagee area. Present in the deepest part of the basin. Previously (McRae, 1987, Mathieson et al., 2016), considered the Shume Formation (of this Group) to be deposited in the Lochkovian to Pragian, on the basis of correlation with Pragian conodonts in the Lerida Limestone Member (Biddabirra Formation). This minimum age interpretation appears to be supported in the final discussion p60-61, although the maximum depositional age is only constrained as Pridoli, by dating of volcanics in autochthonous blocks.|||Shume Formation, 'upper' Amphitheatre Group, 'lower' Amphitheatre Group|Overlain by Buckambool Sandstone (Winduck Group). Equivalent to Mount Hope Group, Broken Range Group and Mouramba Group.||
381|Amphitheatre Group|73019|5|Briefly described|p429|Early Devonian|Early Devonian|Cobar Basin.||||Overlies Kopyje Group.|Deep-water turbidites.|
381|Amphitheatre Group|73143|5|Briefly described|p1-3, p8|Devonian|Silurian|Lachlan Orogen. Cobar Superbasin, northern. Host to the Endeavour Zn-Pb-Ag deposit. Upper and Lower Amphitheatre Group shown on p2.|||CSA Siltstone, Biddabirra Formation, Lower Amphitheatre Group, Upper Amphitheatre Group||Includes siltstone and limestone units.|
381|Amphitheatre Group|73174|5|Briefly described|p1036-1039|Early Devonian|Early Devonian|Cobar Basin. Interfingers with the Winduck Group representing increasing water depth to the east. Contains age-diagnostic brachiopod.||Cobar Supergroup|Biddabirra Formation, Alley Sandstone Member, CSA Siltstone, Shume Formation|||
381|Amphitheatre Group|73578|6|Mentioned|p2, p4, p11, p18|||Cobar Basin. [Written as Amphitheatre Group (lower) and Amphitheatre Group (upper) on p2].||Cobar Supergroup|Shume Formation|||
379|Amphitheatre Group, lower|22857|5|Briefly described|p436 App.1, Tb.A1.6|Pragian|Lochkovian|Informal - see Amphitheatre Group. Of the Cobar Supergroup. Interfingers with and overlies Mouramba Group in the Priory and Cobar Blocks. Geological Province: Cobar Basin. See also p440 App.1, Tb.A1.6.||||||
379|Amphitheatre Group, lower|23171|6|Mentioned|p15-6|||||||||21-JAN-05
379|Amphitheatre Group, lower|23173|4|Described|Map Legend|Lochkovian|Pridoli|||||||21-JAN-05
379|Amphitheatre Group, lower|24019|5|Briefly described|p353|||Informal name. Of Cobar Supergroup.||||||16-MAR-05
379|Amphitheatre Group, lower|41872|6|Mentioned|Fig.8|||||||||
379|Amphitheatre Group, lower|43032|4|Described|p76|||Intended as informal name.||||||21-JAN-05
379|Amphitheatre Group, lower|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|Informal name for unit of Amphitheatre Group||||||21-JAN-05
379|Amphitheatre Group, lower|60520|5|Briefly described|Map legend|Early Devonian|Early Devonian|Informal subdivision of the Amphitheatre Group.  Geological Province: Cobar Basin.||||||
379|Amphitheatre Group, lower|70950|5|Briefly described|p1029,1033-1034,1039,1041|||Geological province: Central Lachlan Orogen. See also Amphitheatre Group. Includes a sequence of quartz-rich to quartz-lithic sandstones and siltstones. Detailed mineralisation analysis provided. ||||Separated from upper Amphitheatrer Group by Shume Formation|Greywacke, siltstone, shale, felsic volcaniclastic units|
379|Amphitheatre Group, lower|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.|
379|Amphitheatre Group, lower|72908|5|Briefly described|p3, p7-8 Tb.1, p17, p19, p30|Early Devonian|Late Silurian|Cobar Basin. Earliest Devonian minimum age. Hosts the Hera and Nymagee deposits adjacent to the boundary with the Mouramba Group.||Amphitheatre Group|||Sequence of quartz-rich to quartz-lithic sandstones and siltstones. Includes deformed quartz-lithic greywacke, siltstones, shales and minor felsic volcanic units.|
379|Amphitheatre Group, lower|72958|5|Briefly described|p5, p8, p29, p37, p60|||Cobar Basin, syn-rift phase. Is the southern stratigraphic equivalent of the deep-water Nurri Group. [Also written as Amphitheatre Group (lower); Fig.1.1]||Amphitheatre Group|Stones Tank Tuff Member|||
379|Amphitheatre Group, lower|73174|5|Briefly described|p1037|||Cobar Basin. Represents syn-rift phase of sedimentation. Deposited as deep water turbidites. Thickness ranges from 1.5 km in the south to >7 km in the north.||||Lateral equivalent to Nuri Group.|Thin-bedded, sandstone-siltstone-mudstone turbidites with interbedded felsic volcanic horizons. Sandstones are generally quartz-rich with lithic clasts.|24-NOV-22
427|Andersons Flat beds|22857|5|Briefly described|p270, p536 App.1 Tb.A1.9|Early Permian|Early Permian|Shallow water deposits of the New England Orogen - sandstone, sitlstone, shale. Geological Province: New England Fold Belt. See also p256.||||||
427|Andersons Flat beds|22864|6|Mentioned|p256,270|||||||||
427|Andersons Flat beds|41348|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of the Manning Group.||||||16-DEC-04
427|Andersons Flat beds|68005|5|Briefly described|p154.|Permian|Permian|||Unit in Manning Group.|||Lithofeldspathic sandstone, conglomerate and mudstone.|
502|Appin Formation|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||
502|Appin Formation|24471|4|Described|p29 Fig.2|Late Permian|Late Permian|Overlies Wilton Formation. Overlain by American Creek Coal. Thickness: 35-40 m. Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
502|Appin Formation|29900|6|Mentioned|Table 1|||||||||
502|Appin Formation|30006|6|Mentioned|p13|||||||||
502|Appin Formation|32618|6|Mentioned|Table 1|||Perm. Strat. table||||||
502|Appin Formation|32849|6|Mentioned|Table 1|||Permian||||||
502|Appin Formation|34060|6|Mentioned|p24|||Perm. Table||||||
502|Appin Formation|34569|6|Mentioned|p8|||See P9. Permian||||||
502|Appin Formation|36220|6|Mentioned|p49|||||||||
502|Appin Formation|37089|6|Mentioned|p208|||||||||
502|Appin Formation|37090|6|Mentioned|Fig.2|||||||||
502|Appin Formation|39661|6|Mentioned|Fig.1|||||||||
502|Appin Formation|45090|6|Mentioned|p216|||Tatarian.||||||
504|Apple Tree Flat Subgroup|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wollombi Coal Measures (Singleton Supergroup). Max. thickness: 30m. Geological Province: Sydney Basin.||||||
504|Apple Tree Flat Subgroup|22969|4|Described|Fig 4.1a||Late Permian|Wollombi Coal Measures||||||
504|Apple Tree Flat Subgroup|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures.||||||
504|Apple Tree Flat Subgroup|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures. Geological Province: Sydney Basin||||||
504|Apple Tree Flat Subgroup|41010|6|Mentioned|Table 1|||||||||
504|Apple Tree Flat Subgroup|42078|6|Mentioned|Table 1 P5|||||||||
504|Apple Tree Flat Subgroup|42916|5|Briefly described|Table 1||Late Permian|||||||
504|Apple Tree Flat Subgroup|43257|5|Briefly described|Map Legend||Late Permian|Of Wollombi Coal Measures||||||
504|Apple Tree Flat Subgroup|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wollombi Newcastle Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
520|Arable Tonalite|22815|4|Described|p55|Silurian|Silurian|||||||
520|Arable Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||of Murrumbucka Suite.||||||11-JAN-10
520|Arable Tonalite|49705|5|Briefly described|p17|||Variation of Arable Granodiorite, same page?||||||
554|Ardlethan Granite|22508|5|Briefly described|p3||Pridolian|Age: 410 +/- 2.5 Ma. In the Lachlan Fold Belt.||||||27-OCT-08
554|Ardlethan Granite|22699|6|Mentioned|p121|||||||||
554|Ardlethan Granite|23549|5|Briefly described|p529|||Of Koetong Supersuite. Considered as a felsic 'specialised' granite - resulting from extensive fractional crystallisation; responsible for tin mineralisation in Ardlethan, NSW.||||||05-APR-05
554|Ardlethan Granite|24263|6|Mentioned|p1394|||Geological Province: Wagga Belt||||||
554|Ardlethan Granite|24266|6|Mentioned|p1486|||Geological Province: Lachlan Fold Belt.||||||
554|Ardlethan Granite|24270|6|Mentioned|p1612|||Geological Province: Lachlan Fold Belt. Of the Koetong Supersuite.||||||
554|Ardlethan Granite|24271|5|Briefly described|p1620|Late Silurian|Late Silurian|Geological Province: Wagga tin belt. Age: 410+/-2.5 Ma. Of the Koetong Supersuite.||||||
554|Ardlethan Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
554|Ardlethan Granite|30076|6|Mentioned|Fig.1|||||||||
554|Ardlethan Granite|31858|6|Mentioned|p3|||Tin deposits||||||
554|Ardlethan Granite|32579|6|Mentioned|p37|||||||||
554|Ardlethan Granite|32676|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
554|Ardlethan Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
554|Ardlethan Granite|35257|6|Mentioned|p154|||||||||
554|Ardlethan Granite|35412|6|Mentioned|p7|||Location of tin deposits.||||||
554|Ardlethan Granite|36316|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
554|Ardlethan Granite|36317|6|Mentioned|p126|||||||||
554|Ardlethan Granite|37590|6|Mentioned|p18|||||||||
554|Ardlethan Granite|38335|6|Mentioned|p1728|||||||||
554|Ardlethan Granite|38339|5|Briefly described|p11|||||||||
554|Ardlethan Granite|39083|6|Mentioned|p30|||||||||
554|Ardlethan Granite|39772|6|Mentioned|p22|||||||||
554|Ardlethan Granite|40328|4|Described|p202|||||||||
554|Ardlethan Granite|40498|6|Mentioned|p368|||||||||
554|Ardlethan Granite|40589|6|Mentioned|p343|||||||||
554|Ardlethan Granite|41415|6|Mentioned|Fig.1|||||||||
554|Ardlethan Granite|41433|5|Briefly described|p159|||||||||
554|Ardlethan Granite|42179|6|Mentioned|Fig.2 P234|||||||||
554|Ardlethan Granite|42726|5|Briefly described|map legend|Silurian||No.538.||||||19-JAN-17
554|Ardlethan Granite|61964|6|Mentioned|p52, p241|||To the south-southwest of CARGELLIGO map sheet area - in the NARRANDERA sheet area - links with Eura Bonny Granite pluton on CARGELLIGO. The mineralising event at Ardlethan is dated at 410+/-2.5Ma by Richards et al (Rb-Sr supported by K-Ar).||||||27-OCT-08
554|Ardlethan Granite|62367|6|Mentioned|p10|Early Devonian|Late Silurian|Age: 410+/-2.5Ma (Rb-Sr and K-Ar, Richards et al 1982).||||||31-MAY-06
554|Ardlethan Granite|69019|6|Mentioned|p29 Fig.9.|||Geochemistry is briefly described.||||||
554|Ardlethan Granite|69023|6|Mentioned|p26|||Blevin and Chappell (1995). An Australian standard S-type granite. Geochemistry outlined.||||||
554|Ardlethan Granite|69043|4|Described|p1-2, p5-6, p12, p15, p18, p21, p24-30|Early Devonian|Early Devonian|See also p34, p36-37, p40, p44, p47, p53, p116. Bald Hill Prospect, S of Ardlethan. A garnet-bearing porphyry, previously thought to be a carapace of this intrusion, is now considered to be a lateral equivalent of the Gurragong and Walleroobie Volcanics. Previously thought to belong to Koetong Supersuite; possible only if the latter was emplaced over 10-15 m.y. An earlier determination of the Granite was a muscovite whole-rock Rb-Sr age of 410 +/- 2.5 Ma (Richards et al., 1982).|414.7 +/- 2.3 Ma.|Ardlethan Suite.|||S-type. Felsic and fractionated. Includes leucocratic syenogranite.|
554|Ardlethan Granite|69801|6|Mentioned|p2, p25-26, p136|Devonian|Early Devonian|Central Lachlan Orogen. Associated with tin mineralisation in the Ardlethan area about 90km North-northwest of the Collingullie Granite.|414.7 +/- 2.3 Ma (SHRIMP)||||Felsic and highly fractionated S-type granitic rocks.|
554|Ardlethan Granite|70777|5|Briefly described|p2, p9, p14, p16, p22, p37, p80|Lochkovian|Lochkovian|Lachlan Orogen. Rock exposure previously mapped as this unit has subsequently been redefined as the new Beckom South Granite on the basis of its seperation by ordovician and late devonian rocks.|414.7 +/- 2.3 Ma (Bodorkos et al., 2015)|||||
554|Ardlethan Granite|71213|5|Briefly described|p94|Silurian|Silurian|Crops out around Yarran Waterholes in the southern section of Bland Shire.  Regarded as co-magmatic with Kikoira Granite, Ungarie Granite.|||||Biotite-muscovite granite with large feldspar phenocrysts.|25-JUN-17
554|Ardlethan Granite|71364|5|Briefly described|p5, p10|Late Silurian|Late Silurian|Harper (1913). Source of tin at Ardlethan, Bygoo, Bald Hill. Deeply weathered. Crops out as large, conspicuous tors.|||||Pink to pale grey, feldspar-phyric muscovite-biotite granite, granophyre, greisen and "quartz-tourmaline rock".|15-FEB-18
554|Ardlethan Granite|71365|5|Briefly described|map legend|||Silurian?|||||Porphyritic muscovite-biotite granite.|15-FEB-18
554|Ardlethan Granite|71889|5|Briefly described|p7, p31-p34, p73|Lochkovian|Lochkovian|Trigg (2017) assigned a cordierite granite on the 'Ranchero' property to the Ganmain Granite; however, more recent geochemistry seems to indicate this 'Ranchero' granite most likely belongs to the Ardlethan Granite. Trigg notes geochronological work would be more conclusive in assigning this granite as the Ganmain and Ardlethan granites have significantly different ages.|414.7 +/- 2.3 Ma (Bodorkos et al, 2013)|||||
554|Ardlethan Granite|72083|5|Briefly described|p20-22, p37, p39|Devonian|Devonian|An outcrop of this unit, mapped by Trigg (?2016) is here tentatively included in the Rosemorder Granite; discussion.|c.413 Ma (Bodorkos et al.,in prep.).||||Porphyritic granite.|
581|Argyll Granodiorite|23720|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Hillgrove Plutonic Suite.  Biotite granodiorite, gneissic in part.||||||15-DEC-04
581|Argyll Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
581|Argyll Granodiorite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
581|Argyll Granodiorite|41348|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of the Hillgrove Plutonic Suite.||||||16-DEC-04
581|Argyll Granodiorite|44450|6|Mentioned|p11|||Geological Province: New England Fold Belt.||||||
581|Argyll Granodiorite|71628|5|Briefly described|p2: 37; p3: 1, 4, 10, 19-22, 68-69|||Binns et al. (1967), after a local homestead. An elliptical (5 x 3 km) NNE-trending intrusion 30 km due E of Walcha. Geochemistry described in some detail. Contains garnet as a contaminant from surrounding sedimentary rocks.||Argyll Suite.||Intrudes Agnes Greywacke. Encloses a body of Moona Plains Complex.|Fine- to medium-grained, weakly porphyritic to granular biotite granodiorite-monzogranite; orthopyroxene, amphibole and garnet bearing variants; weakly deformed to gneissic.|
640|Arsenic Ridge Quartz Monzodiorite|22815|4|Described|p49|Early Devonian|Silurian|||||||
640|Arsenic Ridge Quartz Monzodiorite|35109|2|Defined|p78|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
640|Arsenic Ridge Quartz Monzodiorite|35263|6|Mentioned|Table 3|||||||||
640|Arsenic Ridge Quartz Monzodiorite|36411|6|Mentioned|p267|||Refs White et al 1977 for definition.||||||
640|Arsenic Ridge Quartz Monzodiorite|40882|6|Mentioned|p28|||||||||
640|Arsenic Ridge Quartz Monzodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Boggy Plain Suite.||||||11-JAN-10
654|Arthursleigh Tonalite|41420|5|Briefly described|p389|||Pluton of Maraluan Batholith (Early Devonian to Carboniferous). Heterogenous with well-dev'd unusual zonation from relatively mafic core to a felsic rim of adamellite; has a contact zone >4km wide in Late Ord strata along its eastern margin.||||||07-AUG-08
654|Arthursleigh Tonalite|68592|5|Briefly described|p1610-2|||Clenhall et al. (1988). Named after Arthursleigh homestead. Chosen by  Chappell et al. (1991) as the type pluton for the Arthursleigh Suite. Occurs in the deeply incised Wollondilly River, exposed over several hundreds of metres of relief.||Unit in Arthursleigh Suite.|Intrudes Bindook Group.||Zoned or compositionally varied.|
654|Arthursleigh Tonalite|70661|3|Fully described|p13, p31, p75, p88, p90, p91|Early Devonian|Early Devonian|Produced a 4km wide contact metamorphic zone.Named after Arthursleigh property. Originally mapped as undifferentiated Marulan Batholith. Forms low rolling hills with some extensive gully erosion. Structure, metamorphism, geochemistry and geophysical characteristics discussed.||Arthursleigh Suite||Intrudes Adaminaby Group, Bungonia Group, Bindook Group, Pleasant Hill Granite|Tonalite to granodiorite with concentric zoning. Is generally holocrystalline and mostly equigranular to locally porphyritic.|
654|Arthursleigh Tonalite|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Arthursleigh Suite.|||Concentrically-zoned, Biotite-hornblende bearing pluton varying from mostly tonalite in the middle to granodiorite on the edges. Mafic enclaves common throughout, country rock xenoliths abundant locally.|16-FEB-18
705|Ashford Coal Measures|22857|4|Described|p263, p538 App.1 Tb.A1.9|Early Permian|Early Permian|Arenite, argillite, cobble conglomerate; interbedded coal. Max. thickness: 300m. Equivalent of Greta Coal Measures. Geological Province: New England Fold Belt.||||||
705|Ashford Coal Measures|22864|6|Mentioned|p263|Artinskian|Artinskian|Stage B - 268-258 Ma.||||||20-AUG-18
705|Ashford Coal Measures|23050|4|Described|p14 Table 1|Early Permian|Early Permian|Age: Early Permian. Greta Coal Measures equivalent.||||||
705|Ashford Coal Measures|23051|5|Briefly described|Map Legend|Early Permian|Early Permian|||||||
705|Ashford Coal Measures|30133|6|Mentioned|Map legend|Permian|Permian|||||||
705|Ashford Coal Measures|30911|6|Mentioned|Map legend|Permian|Permian|||||||
705|Ashford Coal Measures|31694|6|Mentioned|p347|||||||||
705|Ashford Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
705|Ashford Coal Measures|32672|6|Mentioned|p675|||||||||
705|Ashford Coal Measures|32920|5|Briefly described|p90|||||||||
705|Ashford Coal Measures|32944|6|Mentioned|p699|||See also p709. Lower Permian.||||||05-AUG-08
705|Ashford Coal Measures|34292|6|Mentioned|p28|||Permian||||||
705|Ashford Coal Measures|34350|6|Mentioned|p16|||See pp17,18. Permian. Correlation with Greta Coal Measures.||||||05-AUG-08
705|Ashford Coal Measures|34400|6|Mentioned|p9|||Permian||||||
705|Ashford Coal Measures|34556|4|Described|p269|||||||||
705|Ashford Coal Measures|35767|6|Mentioned|p56|||||||||
705|Ashford Coal Measures|36172|6|Mentioned|Appendix|||||||||
705|Ashford Coal Measures|36961|6|Mentioned|Table 1|||||||||
705|Ashford Coal Measures|37065|6|Mentioned|p29|||||||||
705|Ashford Coal Measures|37100|4|Described|p259|||||||||
705|Ashford Coal Measures|38064|6|Mentioned|p40|||||||||
705|Ashford Coal Measures|38806|6|Mentioned|p72|||||||||
705|Ashford Coal Measures|38958|5|Briefly described|p490|||||||||
705|Ashford Coal Measures|40245|6|Mentioned|Table 2|||||||||
705|Ashford Coal Measures|40246|6|Mentioned|p173|||||||||
705|Ashford Coal Measures|42182|5|Briefly described|p302|||||||||
705|Ashford Coal Measures|42748|6|Mentioned|Fig.3 P9|Permian||||||||
705|Ashford Coal Measures|42923|6|Mentioned|p43|||||||||
705|Ashford Coal Measures|43017|5|Briefly described|Fig.2,p374|||||||||
705|Ashford Coal Measures|43344|14|Not recorded|p11||Permian|New England central zone.||||||
705|Ashford Coal Measures|43384|14|Not recorded|Map Legend|Early Permian||||||||
705|Ashford Coal Measures|43436|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
705|Ashford Coal Measures|43984|14|Not recorded|p139|||Correlated with Greta Coal Measures.||||||
705|Ashford Coal Measures|44093|5|Briefly described|p238 App. 1|Early Permian|Early Permian|Age: Late Early Permian. Continental, coal measures. Geological Province: New England Fold Belt.||||||
705|Ashford Coal Measures|44565|2|Defined|p230-232|||See also Lexicon. Gangamopteris and Glosssopteris.||||||
705|Ashford Coal Measures|48784|14|Not recorded|?|||||||||
705|Ashford Coal Measures|48940|6|Mentioned|p18|||||||||
705|Ashford Coal Measures|61772|6|Mentioned|p128 Fig. 2, p130||Early Permian|In text, Coal Measures is C.M. Geological Province: Bowen Basin.||||||
705|Ashford Coal Measures|62534|6|Mentioned|p7|Early Permian|Early Permian|||||||07-FEB-11
705|Ashford Coal Measures|63347|5|Briefly described|p5 Fig. 2|Early Permian|Early Permian|Geological Province: New England Orogen. Felsic to andesitic volcanic and volcaniclastic rocks.||||||04-JUN-07
705|Ashford Coal Measures|63733|5|Briefly described|Map legend|Early Permian|Early Permian|Fluvial sandstone, argillite, cobble conglomerate and interbedded coal horizons.||||||11-DEC-07
705|Ashford Coal Measures|68005|4|Described|p18, p22, pp36-42, p153, p170.|Early Permian|Early Permian|Central Block, New England Fold Belt. In part thrust under granite on its western side. Correlated with Greta Coal Measures of the Sydney Basin. 170 m thick at old colliery at Ashford. Intense multiphase structural deformation has reduced the coal fabric to a highly friable, non-cohesive material with greatly increased fines content.|||Includes Ashford, Bonshaw and Bukkulla Members.|Unconformably overlies Texas beds. Thrust faulted against Bundarra Supersuite.|Fluvial sandstones and shales, interbedded cobble conglomerate and coal horizons.|
705|Ashford Coal Measures|68006|5|Briefly described|p26, pp84-92.|Permian|Permian|A NE-striking belt, immediately east of northern Bundarra Supersuite, hosting significant coal deposits. Thrust at least 1.5 km under granite to its west by the Severn Thrust Fault. Resource discussed in detail.|||Includes Ashford and Bonshaw seams.||Fluvial sandstones and shales and interbedded cobble conglomerate and coal horizons.|
714|Ashleigh Member|23214|4|Described|p110|Wenlock|Llandovery|Limestone and black shale facies of Glendalough Formation.||||||
714|Ashleigh Member|35258|4|Described|p125|||||||||
776|Austinmer Sandstone Member|29900|5|Briefly described|Fig.4|||||||||
776|Austinmer Sandstone Member|29901|6|Mentioned|p163|||||||||
776|Austinmer Sandstone Member|31128|6|Mentioned|Table 1|||||||||
776|Austinmer Sandstone Member|36220|4|Described|p52|||||||||
776|Austinmer Sandstone Member|39309|5|Briefly described|p127|||||||||
776|Austinmer Sandstone Member|42787|5|Briefly described|p132|||of Bargo Claystone||||||
776|Austinmer Sandstone Member|42896|4|Described|p21|||of Bargo Claystone||||||
781|Australasian Coal|22578|6|Mentioned|Fig.9 p399, p402|||||||||
781|Australasian Coal|23055|6|Mentioned|Fig4p11,22|||||||||
781|Australasian Coal|24471|4|Described|p32 Fig.4, p33|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to American Creek Coal. Geological Province: Sydney Basin.||||||07-FEB-11
781|Australasian Coal|39308|6|Mentioned|Fig.23.4|||||||||
781|Australasian Coal|39609|6|Mentioned|Table 1|||||||||
781|Australasian Coal|40516|6|Mentioned|p395|||||||||
781|Australasian Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Australasian coal seam instead. See also p113.||Of Adamstown Subgroup||||
781|Australasian Coal|73304|6|Mentioned|p75|||||Adamstown Formation, Newcastle Coal Measures||||
795|Avon Lea Mudstone Member|23214|3|Fully described|p107|Llandovery|Llandovery|Basal unit of Cadia Coach Shale. 12m thick at type section.  Massive grey mudstone characterised by very sparsley distributed white, sand sized feldspar grains.||||||
795|Avon Lea Mudstone Member|35258|4|Described|p118|||||||||
802|Avon Subgroup|22857|5|Briefly described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Gloucester Coal Measures. Geological Province: Sydney Basin.||||||
802|Avon Subgroup|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Gloucester Coal Measures.  Geological Province: New England Fold Belt.||||||05-AUG-08
802|Avon Subgroup|40872|6|Mentioned|Fig.2|||||||||
802|Avon Subgroup|41054|6|Mentioned|p152|||||||||
802|Avon Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
802|Avon Subgroup|44244|5|Briefly described|p168 Tb. 2, p175|Late Permian|Late Permian|Of the Gloucester Coal Measures.  Comprises Waukivory Creek and Dog Trap Creek Formations.  Max. thickness: 420m.  Geological Procince: Myall Block.  See also p276.||||||13-JUL-04
802|Avon Subgroup|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Gloucester Coal Measures.  Geological Province: Western Myall Block.||||||
808|Awaba Tuff|22601|6|Mentioned|417, 419|Permian|Permian|||||||
808|Awaba Tuff|22610|5|Briefly described|Fig 5||Early Permian|Age: 256 +/-4Ma.||||||21-AUG-08
808|Awaba 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: 20m. Geological Province: Sydney Basin.||||||
808|Awaba Tuff|23055|6|Mentioned|p22,Fig13p25|||||||||
808|Awaba Tuff|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Of the Newcastle Coal Measures.  Equivalent to the Nalleen Tuff Member (Dights Creek Coal).   Geological Province: Sydney Basin||||||21-AUG-08
808|Awaba Tuff|24040|5|Briefly described|p484|Late Permian|Late Permian|Part of an upper subgroup of the Newcastle Coal Measures.  Age: 256+/-4ma (Gulson et al, 1990; U-Pb zircon).||||||21-AUG-08
808|Awaba Tuff|24157|4|Described|p195, p188 Tb.1|Permian|Permian|Of the Newcastle Coal Measures. Overlain by Great Northern seam. Underlain by Fassifern seam. Geological Province: Sydney Basin. Maximum Thickness: 30m||||||14-MAR-07
808|Awaba Tuff|24158|5|Briefly described|p172 Fig.3, p173 Fig.4|||Max. Thickness: 12m. Geological Province: Sydney Basin.||||||21-AUG-08
808|Awaba Tuff|24471|4|Described|p27, p43|Late Permian|Late Permian|Geochemical correlation with Burragorang Claystone Member. Of Newcastle Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
808|Awaba Tuff|29922|6|Mentioned|Appendix 4|||||||||
808|Awaba Tuff|33867|6|Mentioned|Fig.4|||||||||
808|Awaba Tuff|41463|6|Mentioned|p42|||||||||
808|Awaba Tuff|41477|6|Mentioned|p79|||||||||
808|Awaba Tuff|41479|6|Mentioned|p93|||||||||
808|Awaba Tuff|42214|4|Described|p460|||||||||
808|Awaba Tuff|42767|6|Mentioned|p5|||||||||
808|Awaba Tuff|43344|14|Not recorded|p85||Late Permian|Included in Eleebana Formation||||||
808|Awaba Tuff|45090|6|Mentioned|p83|||Tabel of Perm. igneous rocks||||||
808|Awaba Tuff|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Newcastle Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
808|Awaba Tuff|62033|5|Briefly described|p24, p25 (Table)|||Of the Newcastle Coal Measures. Overlain by Great Northern seam and underlain by Fassifern seam. Geological Province: Sydney Basin.||||||14-MAR-07
808|Awaba Tuff|67786|5|Briefly described|p94, 96, 101|Permian|Permian|Newcastle area, Sydney Basin.||Moon Island Beach Subgroup.||Overlies Bolton Point Conglomerate. Is overlain by Great Northern seam.|Extensive tuffaceous unit; cross-stratification common (ash flow or reworked ash fall material).|
808|Awaba Tuff|68493|4|Described|p5 Fig.2|Lopingian|Lopingian|Isotopic U-Pb age from Metcalfe et al. (2012).|ca. 253 Ma|Of the Newcastle Coal Measures.|||Felsic tuff, tuffaceous sedimentary rock.|
808|Awaba Tuff|68711|3|Fully described|p113, 115 Tb 1, p116 Tb 2, p114 Fig. 2|||Elevated from Member to Formation. Replaces Awaba Tuff Member. Named after township W of Toronto. Thickness: 2-20m; 9.34m in type section in BHP Coal Point Bore (details given for type and standard sections).||Of Newcastle Coal Measures. ||Overlies Boolaroo Formation. Overlain by Moon Island Beach Formation.|Tuff, tuffaceous sandstone, tuffaceous siltstone, claystone, chert, usually contains abundant mica in basal 0.2-0.4 m.|14-JAN-15
808|Awaba Tuff|69683|6|Mentioned|p411 Fig.2|Late Permian|Late Permian|||Unit in Newcastle Coal Measures.||||
808|Awaba Tuff|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. CA-TIMS ages of 253.21, 253.12 and 253.14 Ma (Metcalfe etal., 2015). Corresponding to APP5 zone (Lopingian).||Unit of Newcastle Coal Measures.||||
808|Awaba Tuff|70878|5|Briefly described|p706, p723-724|Permian|Permian|Newcastle and Hunter Coalfields, Sydney Basin. A widespread and relatively thick unit. 2.91m thick in Amoco Wybong 1 well. Four CA-IDTIMS U-Pb zircon ages, all within 0.02 Ma, are given. Calibration of palynological ages.|253.14 +/- 0.06 Ma (Metcalfe et al., 2015).|Newcastle Coal Measures.||||
808|Awaba Tuff|71701|5|Briefly described|p159, p169-p170|||Sydney Basin.|253.14 +/- 0.04 Ma, 253.25 +/- 0.04 Ma||||Intermediate volcanic tuff.|10-FEB-23
808|Awaba Tuff|73304|5|Briefly described|p62, p65-68, p70, p75|Changhsingian|Changhsingian|[Also written as Awaba tuff]. CA-ID-TIMS U-Pb ages of 253.25 +/- 0.30 Ma, 253.14 +/- 0.30 Ma, 253.21 +/- 0.30 Ma. Age of 256 +/- 4 Ma from BHP DDH N1561 corehole reported by Gulson et al. (1990).|ca 253.2 Ma [see comments]|Newcastle Coal Measures||Underlain by Fassifern Seam. Overlain by West Wallarah Seam.||
808|Awaba Tuff|73472|6|Mentioned|p129|Changhsingian|Changhsingian|Sydney Basin.|253.21-253.14 Ma|||||
819|Ayr Conglomerate Member|22857|5|Briefly described|p508 App.1 Tb.A1.8|Early Carboniferous|Early Carboniferous|Of the Isismurra Formation. Basal conglomerate, poorly sorted with interbeds and matrix of lithic arenite; large amount of arc-derived clasts. Max. thickness: 180m. Geological Province: Tamworth Forearc Basin.||||||
819|Ayr Conglomerate Member|32869|3|Fully described|p168|||Isismurra Fm.||||||
819|Ayr Conglomerate Member|36528|6|Mentioned|p177|||||||||
819|Ayr Conglomerate Member|40883|6|Mentioned|p5|||||||||
819|Ayr Conglomerate Member|41542|6|Mentioned|p234|||||||||
819|Ayr Conglomerate Member|44244|5|Briefly described|p34-35|||Of the Isismurra Formation.  Disconformably overlies Dangarfield and Waverley Formations; conformably overlain by Native Dog Member and Curra Keith Tongue.  Max. thickness: 180m.  Geological Province: Rouchel Block.||||||16-SEP-04
819|Ayr Conglomerate Member|50099|5|Briefly described|p10|Early Carboniferous|Early Carboniferous|Of the Isismurra Formation. Disconformably overlies the Waverly Formation; conformably overlain by the Native Dog Member and Curra Keith Tongue. Max. thickness: 180m. Geological Province: Tamworth Belt/New England Orogen.||||||
819|Ayr Conglomerate Member|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Rouchel Block.  Of the Isismurra Formation.  Underlies: Curra Keith Tongue, Native Dog Member.||||||
819|Ayr Conglomerate Member|62095|5|Briefly described|p258 Fig. 9|||Of the Isismurra Formation. Geological Province: Rouchel block/Tamworth Belt.||||||
821|Ayrdale Sandstone Member|23350|4|Described|268|Permian|Permian|Also informally referred to as Ayrdale Sandstone.  of the Rowan Formation.||||||14-JUL-04
821|Ayrdale Sandstone Member|36940|6|Mentioned|p141|||||||||
821|Ayrdale Sandstone Member|37773|5|Briefly described|p22|||||||||
821|Ayrdale Sandstone Member|40331|6|Mentioned|Fig.4|||||||||
821|Ayrdale Sandstone Member|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Muswellbrook area.||Unit in Rowan Formation.||||
821|Ayrdale Sandstone Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Rowan Formation. ||||
829|Babego Tuff 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).||||||
829|Babego Tuff Member|35287|6|Mentioned|p7|||||||||
829|Babego Tuff Member|39618|6|Mentioned|Table 9|||||||||
829|Babego Tuff Member|42566|3|Fully described|p71|||||||||
829|Babego Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
845|Back Creek Group|13516|6|Mentioned|p147, fig 5|Late Permian|Early Permian|From Denison Trough, Bowen Basin||||||
845|Back Creek Group|22593|6|Mentioned|Table 1|||||||||
845|Back Creek Group|22757|4|Described|p8|Late Permian|Early Permian|Also Table3,p9, Table4,p10. Thickness: 400 m. Unconformable on Kuttung Formation. Conformably under Blackwater Group.||||||10-DEC-07
845|Back Creek Group|22857|6|Mentioned|p315 Fig. 22.8|||Geological Province: Gunnedah and Bowen Basins.||||||
845|Back Creek Group|22865|6|Mentioned|Fig22.8p315|||||||||
845|Back Creek Group|22973|5|Briefly described|p9 Fig.2 (d)|Late Permian|Late Permian|||||||
845|Back Creek Group|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
845|Back Creek Group|22987|6|Mentioned|p299|||||||||
845|Back Creek Group|22988|5|Briefly described|p303|||||||||
845|Back Creek Group|23002|5|Briefly described|p417|Permian|Permian|||||||
845|Back Creek Group|23003|5|Briefly described|p423 Table 1|Permian|Permian|||||||
845|Back Creek Group|23004|5|Briefly described|p431 Table 1|Permian|Permian|||||||
845|Back Creek Group|23037|4|Described|p19,23,4,9,40,1,9,50||Permian|Overlain by Goodedulla beds. Underlain by Mount Benmore Volcanics.||||||10-DEC-07
845|Back Creek Group|23042|4|Described|p12,35,48, 50-60, 115||Permian|Underlying unit Mount Bensmore Volcanics.||||||
845|Back Creek Group|23050|6|Mentioned|p81|||||||||
845|Back Creek Group|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
845|Back Creek Group|23161|4|Described|p26 table4 fig11||Early Permian|||||||
845|Back Creek Group|23430|5|Briefly described|p514-515|||Bowen Basin Province.||||||
845|Back Creek Group|24077|5|Briefly described|p410 Tb. 2|Late Permian|Early Permian|Geological Province: Bowen Basin.  See also p411 Tb. 3.||||||
845|Back Creek Group|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|BCG (acronym in figure) interpreted to represent Back Creek Group.  Age: >259Ma.  Geological Province: Bowen Basin.||||||
845|Back Creek Group|24159|5|Briefly described|p148 Fig.2, p147|Late Permian|Early Permian|Geological Province: Bowen Basin. Overlain by the Kianga Formation. Unconformably overlies the Kuttung Volcanics||||||
845|Back Creek Group|24241|5|Briefly described|p18|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
845|Back Creek Group|24615|5|Briefly described|CD|Permian|Permian|[Pb].  Predominantly massive, cleaved mudstone and siltstone (commonly with concretions), minor sandstone.||||||
845|Back Creek Group|29387|6|Mentioned|Table 4|||||||||
845|Back Creek Group|29591|6|Mentioned|p96|||||||||
845|Back Creek Group|29721|6|Mentioned|p65|||||||||
845|Back Creek Group|29735|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|29964|6|Mentioned|p5|||Permian||||||
845|Back Creek Group|30449|6|Mentioned|p1|||Faunal sequence||||||
845|Back Creek Group|30450|5|Briefly described|Fig.1|||Permian age.||||||
845|Back Creek Group|30451|6|Mentioned|p49|||See also P50||||||
845|Back Creek Group|30508|6|Mentioned|p85|||No workable coal. Stratigraphic information||||||
845|Back Creek Group|30546|6|Mentioned|p107|||Correlation. Permian age||||||
845|Back Creek Group|30696|4|Described|Table 3|||Lower-Upper Permian age||||||
845|Back Creek Group|30698|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|30699|6|Mentioned|p53|||Early to late Permian||||||
845|Back Creek Group|30701|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
845|Back Creek Group|30914|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|31079|6|Mentioned|p5|||||||||
845|Back Creek Group|31116|6|Mentioned|p11|||||||||
845|Back Creek Group|31401|6|Mentioned|p30|||||||||
845|Back Creek Group|31656|4|Described|Table 1|||Permian||||||
845|Back Creek Group|31659|6|Mentioned|Table 2|||Correlation||||||
845|Back Creek Group|31690|5|Briefly described|p36|||Refers Derrington et al. (1959)||||||
845|Back Creek Group|31979|4|Described|Table 1|||See also Table 2. L.-U.Perm.||||||
845|Back Creek Group|31983|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
845|Back Creek Group|31984|6|Mentioned|Map legend|Late Permian|Early Permian|Lower to Upper Permian||||||
845|Back Creek Group|32141|6|Mentioned|p154|||||||||
845|Back Creek Group|32193|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
845|Back Creek Group|32276|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|32493|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
845|Back Creek Group|32496|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
845|Back Creek Group|32556|4|Described|Table 3|||L.-U.Perm.||||||
845|Back Creek Group|32577|4|Described|p23|||Early & Late Perm.||||||
845|Back Creek Group|32797|6|Mentioned|p10|||||||||
845|Back Creek Group|32840|6|Mentioned|p6|||||||||
845|Back Creek Group|32944|6|Mentioned|Fig.3|||||||||
845|Back Creek Group|33090|4|Described|Table 3|||Permian||||||
845|Back Creek Group|33091|5|Briefly described|p8|||Stratigraphy||||||
845|Back Creek Group|33094|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|33390|6|Mentioned|p3|||On Table.||||||
845|Back Creek Group|33451|6|Mentioned|Map legend|Permian|Permian|||||||
845|Back Creek Group|33774|3|Fully described|p33|||Map.||||||23-SEP-08
845|Back Creek Group|34138|6|Mentioned|Cor.Chart|||Sakmarian - Kazanian||||||
845|Back Creek Group|34314|4|Described|Table 2|||L.- U.Permian. See also pp10,12.||||||03-SEP-18
845|Back Creek Group|34331|6|Mentioned|p458|||L.- U.Permian||||||
845|Back Creek Group|34389|4|Described|Table 2|||Permian.||||||
845|Back Creek Group|34390|4|Described|Table 2|||Permian||||||
845|Back Creek Group|34392|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
845|Back Creek Group|34480|6|Mentioned|p489|||Lower, Upper Permian. See also P492||||||
845|Back Creek Group|34574|5|Briefly described|p115|||Lower part 260 my. Correlation||||||
845|Back Creek Group|34613|4|Described|p8|||Permian||||||
845|Back Creek Group|35008|6|Mentioned|p178|||||||||
845|Back Creek Group|35141|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|35266|6|Mentioned|p190|||||||||
845|Back Creek Group|35426|3|Fully described|p653|||||||||
845|Back Creek Group|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
845|Back Creek Group|35811|6|Mentioned|Fig.3|||||||||
845|Back Creek Group|35822|6|Mentioned|p40|||||||||
845|Back Creek Group|35873|6|Mentioned|p2|||||||||
845|Back Creek Group|35940|6|Mentioned|Fig.2|||||||||
845|Back Creek Group|36103|6|Mentioned|p145|||||||||
845|Back Creek Group|36241|6|Mentioned|p115|||||||||
845|Back Creek Group|36570|6|Mentioned|p77|||||||||
845|Back Creek Group|36739|2|Defined|p1|Permian|Permian|||||||
845|Back Creek Group|36925|4|Described|p179|||||||||
845|Back Creek Group|37070|6|Mentioned|p69|||||||||
845|Back Creek Group|37071|4|Described|p83|||||||||
845|Back Creek Group|37075|5|Briefly described|Table 1|||||||||
845|Back Creek Group|37076|6|Mentioned|p119|||||||||
845|Back Creek Group|37079|6|Mentioned|p137|||||||||
845|Back Creek Group|37121|5|Briefly described|Table 1|||||||||
845|Back Creek Group|37138|6|Mentioned|p94|||||||||
845|Back Creek Group|37565|6|Mentioned|p7|||||||||
845|Back Creek Group|37612|6|Mentioned|Fig.1|||See also P282||||||
845|Back Creek Group|37749|6|Mentioned|p184|||||||||
845|Back Creek Group|37858|6|Mentioned|p82|||||||||
845|Back Creek Group|37859|6|Mentioned|p68|||||||||
845|Back Creek Group|38081|5|Briefly described|Table 1|||||||||
845|Back Creek Group|38153|6|Mentioned|p368|||||||||
845|Back Creek Group|38204|4|Described|p71|||||||||
845|Back Creek Group|38365|6|Mentioned|Fig.2|||||||||
845|Back Creek Group|38447|6|Mentioned|Map legend|Late Permian|Early Permian|Late Permian to Early Permian||||||
845|Back Creek Group|38518|6|Mentioned|Fig.3|||||||||
845|Back Creek Group|39212|5|Briefly described|p10|||Coal deposits. p24 gas reservoir. See also p23.||||||03-SEP-18
845|Back Creek Group|39220|6|Mentioned|p43|||See also P44||||||
845|Back Creek Group|39252|6|Mentioned|Fig.13|||||||||
845|Back Creek Group|39260|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|39261|6|Mentioned|Fig.6|||||||||
845|Back Creek Group|39264|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|39267|6|Mentioned|p232|||||||||
845|Back Creek Group|39268|6|Mentioned|p269|||||||||
845|Back Creek Group|39269|6|Mentioned|Fig.1|||||||||
845|Back Creek Group|39445|6|Mentioned|Table 8|||||||||
845|Back Creek Group|39494|6|Mentioned|Fig.5|||||||||
845|Back Creek Group|39943|6|Mentioned|Table 6A|||||||||
845|Back Creek Group|40030|6|Mentioned|Fig.5|||||||||
845|Back Creek Group|40093|3|Fully described|p26|||||||||
845|Back Creek Group|40094|6|Mentioned|p22|||||||||
845|Back Creek Group|40096|6|Mentioned|p2|||||||||
845|Back Creek Group|40249|6|Mentioned|p41|||||||||
845|Back Creek Group|40544|6|Mentioned|Fig.6|||||||||
845|Back Creek Group|40571|4|Described|p31|||||||||
845|Back Creek Group|40574|5|Briefly described|p4|||||||||
845|Back Creek Group|40623|5|Briefly described|p80|||Briefly described p104.||||||03-SEP-18
845|Back Creek Group|40675|6|Mentioned|p306|||Mention Table 6A||||||
845|Back Creek Group|40767|6|Mentioned|p17|||||||||
845|Back Creek Group|40968|4|Described|p277|||||||||
845|Back Creek Group|41034|5|Briefly described|p366|||||||||
845|Back Creek Group|41188|5|Briefly described|p231|||||||||
845|Back Creek Group|41191|6|Mentioned|p283|||||||||
845|Back Creek Group|41210|5|Briefly described|Fig.3|||||||||
845|Back Creek Group|41246|6|Mentioned|Map legend|Permian||||||||
845|Back Creek Group|41247|6|Mentioned|Fig.7|||||||||
845|Back Creek Group|41290|6|Mentioned|Fig.6|||||||||
845|Back Creek Group|41666|6|Mentioned|p1|||||||||
845|Back Creek Group|41725|6|Mentioned|Fig.2|||||||||
845|Back Creek Group|41809|6|Mentioned|p63|||||||||
845|Back Creek Group|41922|4|Described|Table 1, P8|||||||||
845|Back Creek Group|41923|6|Mentioned|p21|||||||||
845|Back Creek Group|42091|6|Mentioned|p289|||||||||
845|Back Creek Group|42250|6|Mentioned|p26|||||||||
845|Back Creek Group|42258|4|Described|p275|||||||||
845|Back Creek Group|42463|6|Mentioned|Fig.5 P172|||||||||
845|Back Creek Group|42547|5|Briefly described|p46|||||||||
845|Back Creek Group|42614|5|Briefly described|p13|||Bowen Basin||||||
845|Back Creek Group|42634|5|Briefly described|Table 2 P10|||||||||
845|Back Creek Group|42641|6|Mentioned|p108|||||||||
845|Back Creek Group|42701|4|Described|p60|||||||||
845|Back Creek Group|42932|5|Briefly described|Fig.15|||||||||
845|Back Creek Group|42994|6|Mentioned|p263|||||||||
845|Back Creek Group|43000|4|Described|p107|||||||||
845|Back Creek Group|43002|5|Briefly described|Fig.2,p135|||||||||
845|Back Creek Group|43003|5|Briefly described|p168|||||||||
845|Back Creek Group|43017|5|Briefly described|Fig.2,p374|||||||||
845|Back Creek Group|43050|6|Mentioned|p55|||||||||
845|Back Creek Group|43099|5|Briefly described|p10|||||||||
845|Back Creek Group|43204|5|Briefly described|Map Legend|Late Permian|Late Permian|Clermont Basin||||||23-DEC-11
845|Back Creek Group|43213|5|Briefly described|p10, p74, p158-159, p239|Permian|Permian|Bowen Basin. Marine and transitional deposits, containing marine fossils and ice-rafted dropstones.|||Includes Blenheim Subgroup.|Overlies Bathampton Metamorphics and Greybank Volcanics.|Quartzose sandstone, quartzose pebble conglomerate.|
845|Back Creek Group|43474|14|Not recorded|p6,fig.2,22,68|Kazanian|Artinskian|||||||
845|Back Creek Group|43582|6|Mentioned|p28|||||||||
845|Back Creek Group|43714|6|Mentioned|p30|||||||||
845|Back Creek Group|43861|5|Briefly described|25, 28||Permian|||||||
845|Back Creek Group|43883|14|Not recorded|p18 Fig.4-3|||||||||
845|Back Creek Group|43982|14|Not recorded|Map Legend|||||||||
845|Back Creek Group|43988|14|Not recorded|Map Legend||Permian|||||||
845|Back Creek Group|43990|14|Not recorded|Map Legend|||||||||
845|Back Creek Group|43991|14|Not recorded|p46,50||Permian|Consists of several formations basal oneis Cracow Limestone, overlain by Gyranda Formation.||||||
845|Back Creek Group|43994|14|Not recorded|Map Legend|||||||||
845|Back Creek Group|43995|14|Not recorded|Table p9|Permian|Carboniferous|Comprises Mount Steel Formation, Passion Hill Formation, Acacia Formation, Orange Creek Formation, Oxtrack Formation.||||||
845|Back Creek Group|43998|4|Described|p6,11,12,18,map|Late Permian|Early Permian|=Middle Bowen Beds||||||
845|Back Creek Group|44000|14|Not recorded|p57|||||||||
845|Back Creek Group|44022|14|Not recorded|Map Legend||Permian|||||||
845|Back Creek Group|44118|14|Not recorded|Map Legend||Late Permian|||||||
845|Back Creek Group|44169|14|Not recorded|Tb.1,p6-8,map|||||||||
845|Back Creek Group|44170|4|Described|p6-8,12,22,29,31,35|Late Permian|Early Permian|Tb.1,map.||||||
845|Back Creek Group|44218|14|Not recorded|p17-19|Kazanian|Artinskian|||||||
845|Back Creek Group|44242|14|Not recorded|p14|||||||||
845|Back Creek Group|44245|5|Briefly described|Map Legend||Permian|||||||
845|Back Creek Group|44331|14|Not recorded|Map Legend|Late Permian|Early Permian|||||||
845|Back Creek Group|44381|14|Not recorded|p5,8,9|||||||||
845|Back Creek Group|44390|14|Not recorded|p16||Permian|||||||
845|Back Creek Group|44409|14|Not recorded|Map Legend||Permian|||||||
845|Back Creek Group|44419|14|Not recorded|p272||Permian|||||||
845|Back Creek Group|44424|14|Not recorded|p293-301|||||||||
845|Back Creek Group|44426|14|Not recorded|p11|||Equivalent of Middle Bowen Beds.||||||
845|Back Creek Group|44490|14|Not recorded|p48|||Fossils.||||||
845|Back Creek Group|44514|2|Defined|p27,28|||Contains Mount Steel Formation, Passion Hill Formation, Acacia Formation, Orange Creek Formation, Oxtrack Formation.||||||
845|Back Creek Group|44571|2|Defined|p204-205,207|||Overlies Camboon Andesite.||||||
845|Back Creek Group|44618|14|Not recorded|p511||Permian|Ref. to Malone et al. 1965||||||
845|Back Creek Group|44635|4|Described|p6-8,12,22,29,31,35,||Permian|Tb.1,map. Includes: Blenheim, Gebbie and Tiverton Formations.||||||
845|Back Creek Group|44640|14|Not recorded|p31|||||||||
845|Back Creek Group|44697|14|Not recorded|p91|||||||||
845|Back Creek Group|45031|14|Not recorded|p6-11, Fig.3||Permian|||||||
845|Back Creek Group|45043|14|Not recorded|p244||Permian|||||||
845|Back Creek Group|45071|6|Mentioned|p25|||||||||
845|Back Creek Group|45073|6|Mentioned|p58|||Geological history||||||
845|Back Creek Group|45095|6|Mentioned|p8|||||||||
845|Back Creek Group|45110|3|Fully described|Table 14|||See also Fig.5 and p24.||||||10-DEC-07
845|Back Creek Group|45151|5|Briefly described|Table 10|||See also Table 11 and p15.||||||03-SEP-18
845|Back Creek Group|48600|14|Not recorded|p8|||||||||
845|Back Creek Group|48881|14|Not recorded|p1,12,14,24-26,28,|||p33-4,45,48.  =Middle Bowen Beds.||||||
845|Back Creek Group|48898|2|Defined|p30|Late Permian|Early Permian|Lower - Upper Permian. See also pp1,2,7,8 etc.||||||10-DEC-07
845|Back Creek Group|48900|6|Mentioned|p84|||Table opposite. Lower - Upper Permian.||||||
845|Back Creek Group|48919|6|Mentioned|Table 3|||||||||
845|Back Creek Group|48922|4|Described|Table 2|||L.-U.Perm.||||||
845|Back Creek Group|49644|5|Briefly described|Table|||||||||
845|Back Creek Group|50213|5|Briefly described|Map legend|Permian|Permian|Includes Moah Creek beds, Boomer Formation and unnamed sediments.||||||
845|Back Creek Group|50214|5|Briefly described|Map Legend|Permian|Permian|Includes the Buffel Formation.||||||17-MAY-04
845|Back Creek Group|50215|5|Briefly described|Map Legend|Late Permian|Early Permian|Includes Barfield and Flat Top Formations and the Gyranda Subgroup (Wiseman and Banana Formations).||||||18-JUN-09
845|Back Creek Group|50273|5|Briefly described|Map legend|Late Permian|Early Permian|Includes: Buffel, Oxtrack, Barfield and Flat Top Formations.||||||18-MAY-04
845|Back Creek Group|50301|5|Briefly described|Map Legend|Late Permian|Early Permian|Includes: Buffel Formation, Oxtrack Formation, Barfield Formation, Flat Top Formation.||||||
845|Back Creek Group|50317|5|Briefly described|Map Legend|Permian|Permian|Includes Moah Creek beds.||||||09-JUN-04
845|Back Creek Group|50597|5|Briefly described|Map Legend|Permian|Permian|Undivided sedimentry rocks.||||||
845|Back Creek Group|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Overlies: Rookwood Volcanics, Mount Benmore Volcanics. Underlies: Duaringa Formation.||||||30-JUN-04
845|Back Creek Group|60115|5|Briefly described|p21 Fig. 1|Late Permian|Early Permian|Includes the Blair Athol Coal Measures. Geological Province: Bowen Basin and Comet Ridge.||||||04-FEB-08
845|Back Creek Group|60282|6|Mentioned|p6, p23|||Undivided only in this sheet area.  Passes laterally in to the Barfield Formation in the BANANA region.  References mostly made to Undivided Back Creek Group.||||||12-APR-05
845|Back Creek Group|60386|6|Mentioned|p296|Artinskian|Artinskian|Shown as Back CK GRP, Bowen/Sydney Basin. Deltaic - nearshore - shelf.||||||
845|Back Creek Group|60445|5|Briefly described|p6. p18, p25|||Consists of calcareous sandstone and mudstone. Intruded by Bundarra Granodiorite. Overlies Carmila beds.||||||16-MAY-06
845|Back Creek Group|60472|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Includes: Exmoor Formation, Blenheim Formation, Gebbie Formation, Tiverton Formation.||||||
845|Back Creek Group|60475|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Predominantly massive, cleaved mudstone and siltstone, minor lithic sandstone.||||||
845|Back Creek Group|60479|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Predomiantly massive, cleaved mudstone and siltstone (commonly with concretions), minor lithic sandstone.||||||29-SEP-04
845|Back Creek Group|60480|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Includes: Boomer Formation, Yatton Limestone.||||||
845|Back Creek Group|60481|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Includes: Boomer Formation.||||||
845|Back Creek Group|60557|5|Briefly described|p20 Fig. 5c, p25|||Much of the outcrop of this unit west of the Fitzroy River was previously mapped as the Rannes beds.  Contains the Boomer Formation and Moah Creek beds.  Geological Province: Bowen Basin.||||||09-JUN-05
845|Back Creek Group|60659|5|Briefly described|p20|Late Permian|Early Permian|Includes Tiverton, Gebbie, Blenheim and Exmoor Formations. Geological Province: Bowen Basin.||||||07-FEB-11
845|Back Creek Group|61035|4|Described|p11, p15, p42, p68|Permian|Permian|Unconformably overlain by Styx Coal Measures. Geological Province: Bowen Basin. General lithology consists of sandstone, mudstone + subordinate carbonates, lower part is mudstone-dominated sequence.||||||07-FEB-11
845|Back Creek Group|61377|5|Briefly described|p150|Late Permian|Early Permian|Two lithologies: lower (marine) shale, sltst, minor sst, limest, coal (parts fossiliferous); upper (marginal marine to non-marine) dominantly sst, minor shale and sltst. Unconformable on Kuttung Fm; conformable below Kianga Fm.||||||07-FEB-11
845|Back Creek Group|61612|6|Mentioned|p270 Fig. 1|Late Permian|Early Permian|Includes Blair Athol Coal Measures. Geological Province: Bowen Basin.||||||13-MAR-09
845|Back Creek Group|61777|5|Briefly described|p224|||Sedimentary rocks.||||||07-FEB-11
845|Back Creek Group|61832|5|Briefly described|p187|Permian|Permian|Mudstone, sandstone, limestone. Geological Province: Bowen Basin.||||||
845|Back Creek Group|61917|5|Briefly described|Map legend|Late Permian|Early Permian|`||||||16-MAR-06
845|Back Creek Group|64197|6|Mentioned|p630 Fig.7|Permian|Permian|||||Underlies the Blackwater Group; overlies the Reids Dome Beds.||
845|Back Creek Group|64665|6|Mentioned|p62.|||Styx Basin.||||Is overlain unconformably by Styx Coal Measures.||
845|Back Creek Group|64855|6|Mentioned|p33|||Taroom Trough. Age information not given but implied to be Permian.||||||22-FEB-10
845|Back Creek Group|64859|6|Mentioned|p195, 196, 225|Permian|Permian|Gas source rocks.||||||
845|Back Creek Group|65003|6|Mentioned|p34|||||||||
845|Back Creek Group|65119|5|Briefly described|Fig 2 p503, Table 1 p504, fig 7-8,16-19|Late Permian|Early Permian|Bowen Basin. Carbon shale interbedded with coal, sandstone and siltstone. Tuffaceous siltstone and shale, tuff and sandstone. Upper part up to 2934 m thick. Lower part up to ~90m thick. Age: 251-268 Ma (form Fielding , 1990). Fission Track age: ~106-138 Ma.||||||03-SEP-18
845|Back Creek Group|65388|4|Described|p159-191, p20, 26, 27, 28, 31, 33, 35|Kungurian|Asselian|Bowen Basin. Name first used by Derrington and others (1959) and Derrington and Morgan (1960) for the Permian succession in the Cracow-Theodore area. Includes Buffel Formation, Yatton Limestone, Pindari, Oxtrack, Barfield, Flat Top, Boomer Formations. Previously mapped partly as Rannes beds and partly as Boomer Formation. Includes brachiopod and other fossils. Cleaved mudstones. Overlies Carmila beds, Mount Benmore Volcanics. Intruded by microsyenite at Mount Bora. Intruded by unnamed gabbro. See also pages 48, 55, 70, 74, 76,77, 84, 85, 106, 110, 138, 141, 144, 232, 339, 432-433, 437, 438, 439, 441, 446, 447.||||||
845|Back Creek Group|65706|4|Described|p11, p12; Tb.1 p14,15,16|Late Permian|Early Permian|Bowen Basin. Parts of this unit probably equivalent to Carmila beds and Calen Coal Measures; possibly unconformable on Lizzie Creek Volcanic Group.|||Includes Collinsville Coal Measures, Tiverton Formation, Gebbie Formation and Blenheim Formation.|Conformably underlies Blackwater Group.|Quartzose to lithic sandstone, siltstone, mudstone, carbonaceous shale, calcareous sandstone and siltstone, conglomerate, coal, limestone and sandy coquinite.|
845|Back Creek Group|66084|5|Briefly described|Map legend|Permian|Permian|Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.||||||
845|Back Creek Group|66086|5|Briefly described|Map legend|Permian|Permian|Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.||||||
845|Back Creek Group|66188|6|Mentioned|443,fig 17|Late Permian|Early Permian|Bowen Basin||||||
845|Back Creek Group|66615|6|Mentioned|p3, p4 Fig.2, p5 Fig.3, p7 Fig.4, p8, p9|||Bowen Basin. Overlies Early Permian Volcanics.||||||
845|Back Creek Group|67133|6|Mentioned|p2, p5, p8, p19|||Samples of this unit were analysed by XRD and optical microscopy for this study. Early to Middle Permian.|||Peawaddy Formation.|||
845|Back Creek Group|67402|6|Mentioned|p19 fig WSD3, WSD4|Early Permian|Early Permian|Bowen Basin. Potential seal or reservoir for carbon dioxide storage. See also p43 tbl HPB1, p48 fig BWS1, p50 fig BWS4, p53, p55, p56 tbl BWS2, p57, p61, p62, p80, p80 tbl BWN1, p82-p84, p144, p165 tbl LPB1. |||Includes the Tiverton Formation, Gebbie Formation, Collinsville Coal Measures, Blenheim Formation, Exmoor Formation|||
845|Back Creek Group|67669|5|Briefly described|p11|Late Permian|Early Permian|Of Bowen Basin.||||Overlain by Black Water Group.||
845|Back Creek Group|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||||Is overlain by Blackwater Group.||
845|Back Creek Group|68004|5|Briefly described|p67, p173.|Late Permian|Early Permian|Gunnedah-Bowen Basin. Initial deposits of this unit were in graben structures formed during an Early Permian rift phase. Later deposits occurred during a phase of thermal subsidence. Targeted for oil/gas exploration; only minor fluorescence and low level gas shows. Unlike early deposits, upper parts have excellent reservoir potential. See also reference to Back Creek Formation p175.|||||Sandstones interbedded with (marine) shales.|
845|Back Creek Group|68006|6|Mentioned|p79.|Permian|Permian|Has good quality reservoir sandstones, prospective for petroleum.||||||
845|Back Creek Group|68008|5|Briefly described|p156-157, p292|||Formerly the Rannes beds.||||Overlies, and elsewhere is thrust under, Rookwood Volcanics.||
845|Back Creek Group|68359|5|Briefly described|p3, p7-10, p14-16, p18, p21-24, App.3, 8|Late Permian|Early Permian|Strathmuir Synclinorium, Bowen Basin. Gives high U-Th-K radiometric responses. Early to Late Permian. Predominantly marine to shallow-marine facies. Exhibits a "hot" radiogenic signature on ternary radiometric images: may be a suitable heat source for geothermal energy. The higher heat production value is attributed to radiogenic altered siltstone and claystone beds. Detailed lithologies and photographs of core; detailed lithology and geophysics log; thermal profile and heat flow model.||||Unconformably overlies Glenprairie beds. Is overlain by Styx Coal Measures.|Dominantly massive cleaved mudstone and minor lithic sandstone. Bioturbation common.|05-MAR-19
845|Back Creek Group|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin|||Includes Black Alley Shale, Peawaddy Formation, Colinlea Sandstone, Reids Dome beds.|Overlain unconformably by Blackwater Group. Underlain unconformably by Joe Joe Group.|Mudstone, siltstone, tuff, sandstone, coquinite, minor conglomerate, shale, and coal.|
845|Back Creek Group|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.|||Includes Black Alley Shale, Peawaddy Formation, Colinlea Sandstone.|Overlain by the Blackwater Group. Underlain by the Joe Joe Group.|Mudstone, sandstone, siltstone, coquinite, tuff and minor conglomerate.|
845|Back Creek Group|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Bowen Basin.||||Is overlain conformably by Blackwater Group.||
845|Back Creek Group|68679|5|Briefly described|p308, p311-313, p338, p343-344, p346-347|Permian|Permian|See also p349, p351, p353, p355, p357-360, p364, p373-374 Figs.5.66-68, p380, p419, p469. Bowen Basin. At its eastern margin, the Marlborough Province has been thrust over this Group during the Hunter-Bowen Orogeny. RELATED UNITS (continued): Is folded with and thrust against Leura Volcanics. Is thrust against and probably overlies Goodedulla beds.|||Barfield, Blenheim, Gebbie, Tiverton Formations; Moonlight Sandstone.|Overlies Mount Benmore Volcanics, Reids Dome beds. Is overlain by Blackwater Group. Is thrust under Rookwood Volcanics. Abuts the Carmila beds. Equivalent to Moah Creek beds. See COMMENTS  for more.||
845|Back Creek Group|68731|6|Mentioned|p173 Fig 3.85|||||||||
845|Back Creek Group|68900|6|Mentioned|p4|Permian|Permian|Drummond Basin.||||||
845|Back Creek Group|68901|6|Mentioned|p2 Fig i|Permian|Permian|||||||26-SEP-18
845|Back Creek Group|69379|5|Briefly described|map legend|Permian|Permian||||Colinlea Sandstone|||
845|Back Creek Group|69582|5|Briefly described|p57, p60|||Connors Arch. Thermal conductivity and geothermal energy potential are discussed. Intersected in GSQ St Lawrence 1.||||Conformably overlies the Carmila beds. Overlain by the Styx Coal Measures.|Massive cleaved mudstone and lithic sandstonee, deposited within a predominantly shallow marine environment.|
845|Back Creek Group|69594|6|Mentioned|p550|Permian|Permian|||||Is onlapped by the Styx Coal Measures.||
845|Back Creek Group|69599|5|Briefly described|p635|Permian|Permian|In the Nebo area, is intruded by Mount Bora.||||||
845|Back Creek Group|69681|6|Mentioned|p82|||||||||
845|Back Creek Group|69952|6|Mentioned|p75|Permian|Permian|||||||
845|Back Creek Group|70673|6|Mentioned|p9|Permian|Permian|||||||
845|Back Creek Group|70815|6|Mentioned|p3|||Bowen Basin.||||||
845|Back Creek Group|70856|5|Briefly described|Map Legend|Permian|Permian||||Includes Reids Dome beds, Cattle Creek Formation, Aldebaran Sandstone.|||
845|Back Creek Group|70857|5|Briefly described|Map Legend|Permian|Permian||||Includes Colinlea Sandstone, Peawaddy Formation, Black Alley Shale|Overlies Joe Joe Group, overlain by Blackwater Group||
845|Back Creek Group|71264|6|Mentioned|p581 Fig.4|Permian|Permian|Bowen Basin.||||||
845|Back Creek Group|72297|6|Mentioned|p700|||||||Is overlain unconformably by the Styx Coal Measures.||
845|Back Creek Group|73036|5|Briefly described|Map legend|Late Permian|Early Permian||||Includes Exmoor Formation, Blenheim Formation, Gebbie Formation, Tiverton Formation.||Quartzose to sublabile sst, siltst, mudst, rare limestone. Carbonaceous + micaceous labile sst, siltst, shale, coquinite, minor conglomerate. Quartzose to lithic ssst, sandy siltst, siltst, carbonaceous shale, calcareous sst + siltst; fossiliferous.|
845|Back Creek Group|73037|5|Briefly described|Map legend|Late Permian|Early Permian||||Exmoor Formation, Blenheim Formation, Gebbie Formation and Tiverton Formation||Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.|
845|Back Creek Group|73038|5|Briefly described|Map legend|Late Permian|Early Permian||||Includes Exmoor Formation.||Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.|
845|Back Creek Group|73040|5|Briefly described|Map legend|Late Permian|Early Permian||||||Quartzose to lithic sandstone, siltstone, carbonaceous shale, minor coal and sandy coquinite.|
845|Back Creek Group|73246|6|Mentioned|p189-190|Upper Permian|Lower Permian|Bowen Basin.|||Blenheim Subgroup, Exmoor Formation, German Creek Formation, Gebbie Subgroup, Collinsville Coal Measures, Tiverton Subgroup|Overlain by Blackwater Group including Moranbah Coal Measures and Fair Hill Formation.|Mudstone, sandstone, limestone and coal.|
845|Back Creek Group|73450|6|Mentioned|p55-56, p106|Permian|Permian|Bowen Basin.||||||
875|Bagdad Formation|13996|6|Mentioned|p128|Silurian|Silurian|Midwestern NSW. Contains Llandovery conodonts.||||||
875|Bagdad Formation|22857|4|Described|p426 App. 1 Tb. A1.5|Llandovery|Llandovery|Of the Ashburnia Group. Limestone, sandstone, conglomerate, siltstone. Max. thickness: 104m.||||||
875|Bagdad Formation|23214|2|Defined|p105|Llandovery|Llandovery|Of Ashburnia Group. Originally included in the Panuara Formation (subsequently Panuara Group).  104m Thick at type section.||||||
875|Bagdad Formation|35258|4|Described|p112|||||||||
875|Bagdad Formation|41048|6|Mentioned|p23|||||||||
875|Bagdad Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
875|Bagdad Formation|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Ashburnia Group. Consists of green feldspathic sandstone, calcareous siltstone, limestone and limestone conglomerate.||||||15-JUL-08
875|Bagdad Formation|43782|6|Mentioned|Map diagram|Llandovery|Llandovery|Of Ashburnia Group.||||||15-JUL-08
875|Bagdad Formation|63290|5|Briefly described|p401 Fig. 5(d)|Llandovery|Llandovery|Of Ashburnia Group. Overlain by Cadia Coach Shale, underlain by Bridge Creek Limestone Member.||||||
875|Bagdad Formation|70297|5|Briefly described|map legend, on side 2 of map sheet|Early Silurian|Early Silurian|Age: early to middle Llandovery.||Ashburnia Group||||
875|Bagdad Formation|70684|6|Mentioned|p50 Fig.24, p51-52|||||Ashburnia Group.|Bridge Creek, Wire Gully, Limestone Members.|||
917|Balala Granodiorite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Fine to coarse-grained hornblende-biotite granodiorite and minor diorite.||||||21-DEC-04
917|Balala Granodiorite|24366|5|Briefly described|p13|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.||||||
917|Balala Granodiorite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
917|Balala Granodiorite|30787|6|Mentioned|p49|||Differtiation index||||||
917|Balala Granodiorite|30789|6|Mentioned|Fig.1B|||Petrology & Geochemistry||||||
917|Balala Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
917|Balala Granodiorite|31140|6|Mentioned|p55|||||||||
917|Balala Granodiorite|43091|5|Briefly described|Map legend|||||||||
917|Balala Granodiorite|69323|4|Described|p1,3,6,34-40,69,71, 76|Cisuralian|Cisuralian|Geological province: New England Orogen. Appears to pre-date Bundarra Supersuite (c. 286 Ma), but geochemically and petrographically indistinguishable from the ~255 Ma I-type Uralla Supersuite. Shaw and Flood (1993) reported a Rb-Sr biotite age of c. 275 Ma. SHRIMP U-Pb zircon geochronology of GA 2121504 (biotite- and amphibole-bearing granodiorite) yielded an interpreted (weighted mean 206Pb/238U) magmatic crystallisation age of 295.3+\-1.7 Ma. This new SHRIMP age is older than expected based on existing literature, and is indistinguishable from the 295.2+\-2.3 Ma Glenburnie Adamellite, and confirms I-type plutonism in the southern NEO during the earliest Permian, prior to emplacement of the Bundarra Supersuite. Sample details, SHRIMP analyses, zircon characteristics and geochronology results are discussed.|295+\-1.7 Ma (SHRIMP U-Pb; this study)|Unit of Balala Suite.||Intruded by Yarrowyck Granodiorite and Wongalee Leucogranite.||03-DEC-19
917|Balala Granodiorite|69639|5|Briefly described|p1, p8, p217|Cisuralian|Cisuralian|New England Orogen.|295 +/- 1.7 Ma; Chisholm et al, 2014)|||||
917|Balala Granodiorite|71628|4|Described|p1: 6; p4: 9; p6: 16; p8: 113,115; p19:|||See also p19:1-5, 9-10, 55, 57. Binns et al. (1967), after work by Ransley (1970) and Flood (1971). Probably named after a local homestead. Crops out poorly as low whalebacks and small boulders about 8 km W of Uralla. Southern New England Orogen. Is interspersed with S-type granites. Mineralogy and geochemistry detailed.|295.4 +/- 1.8 Ma (SHRIMP: Chisholm et al., 2014).|Balala Suite.||Intrudes Sandon beds. Abuts Banalasta Monzogranite (relative ages uncertain). Is intruded by Wongalee, Yarrowyck Granodiorites. Is bounded (?intruded) by Bannaweera Gabbro.|Somewhat reduced I-type granitoids: texturally heterogeneous, fine- to medium-grained, equigranular, hornblende-biotite-(pyroxene) granodiorite, with minor monzogranite.|
920|Balarang Conglomerate|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
920|Balarang Conglomerate|32482|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
920|Balarang Conglomerate|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
920|Balarang Conglomerate|32865|6|Mentioned|p481|||||||||
920|Balarang Conglomerate|43407|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
920|Balarang Conglomerate|43417|4|Described|Map Legend||Late Devonian|||||||
939|Bald Hill Claystone|22549|6|Mentioned|p526||Triassic|||||||
939|Bald Hill Claystone|22745|6|Mentioned|p133|||Narrabeen Group, Sydney Basin.||||||
939|Bald Hill Claystone|22749|5|Briefly described|p185-86,Table1p187||Early Triassic|||||||
939|Bald Hill Claystone|22833|6|Mentioned|p653|||of Narrabeen Group.||||||
939|Bald Hill Claystone|22857|5|Briefly described|p530 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Dominantly red shale and fine to medium-grained sandstone. Max. thickness: <20m. Geological Province: Sydney Basin.||||||
939|Bald Hill Claystone|22969|4|Described|Fig 4.1a|Early Triassic|Early Triassic|||||||
939|Bald Hill Claystone|23881|5|Briefly described|p69 Fig. 7.2|||Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
939|Bald Hill Claystone|29633|4|Described|p435|||||||||
939|Bald Hill Claystone|29901|4|Described|Table 2|||||||||
939|Bald Hill Claystone|30006|4|Described|p64|||||||||
939|Bald Hill Claystone|30007|6|Mentioned|p61|||||||||
939|Bald Hill Claystone|30132|6|Mentioned|Table 1|||||||||
939|Bald Hill Claystone|30707|6|Mentioned|p6|||See also Fig.2||||||
939|Bald Hill Claystone|31061|3|Fully described|p1320|||Partly equiv. Wentworth Falls Claystone Member.||||||19-AUG-08
939|Bald Hill Claystone|31128|6|Mentioned|p10|||||||||
939|Bald Hill Claystone|31276|6|Mentioned|p148|||Palynology||||||
939|Bald Hill Claystone|31297|6|Mentioned|p4|||Pt. Gosford Subgroup. See also P6, Fig. 3||||||
939|Bald Hill Claystone|31426|6|Mentioned|Fig.1|||||||||
939|Bald Hill Claystone|31613|6|Mentioned|p348|||||||||
939|Bald Hill Claystone|31725|6|Mentioned|p7|||||||||
939|Bald Hill Claystone|31878|4|Described|p823|||Triassic. Clifton Subgroup. Table 1||||||
939|Bald Hill Claystone|31880|6|Mentioned|p18|||||||||
939|Bald Hill Claystone|31881|6|Mentioned|p335|||Triassic. Refers Laughnan et al.(1964)||||||
939|Bald Hill Claystone|31884|6|Mentioned|Table 1|||Triassic||||||
939|Bald Hill Claystone|31886|6|Mentioned|p394|||||||||
939|Bald Hill Claystone|31887|5|Briefly described|p8|||||||||
939|Bald Hill Claystone|32187|6|Mentioned|p4|||||||||
939|Bald Hill Claystone|32537|5|Briefly described|p3|||||||||
939|Bald Hill Claystone|32719|6|Mentioned|p212|||"Red bed" depositoion.||||||
939|Bald Hill Claystone|32799|6|Mentioned|p8|||||||||
939|Bald Hill Claystone|32800|6|Mentioned|p384|||||||||
939|Bald Hill Claystone|32801|6|Mentioned|p252|||||||||
939|Bald Hill Claystone|32802|6|Mentioned|p19|||||||||
939|Bald Hill Claystone|33682|6|Mentioned|p22|||||||||
939|Bald Hill Claystone|33683|4|Described|Table 1|||||||||
939|Bald Hill Claystone|33685|5|Briefly described|p397|||||||||
939|Bald Hill Claystone|33867|6|Mentioned|Table 1|||||||||
939|Bald Hill Claystone|34009|6|Mentioned|Table III|||Triassic||||||
939|Bald Hill Claystone|34058|5|Briefly described|p395|||Triassic||||||
939|Bald Hill Claystone|34139|6|Mentioned|Table|||PP23-24||||||
939|Bald Hill Claystone|34205|6|Mentioned|Table 6|||Correlated with Burralow Formation||||||
939|Bald Hill Claystone|34301|4|Described|p403|||Petrography||||||
939|Bald Hill Claystone|34303|4|Described|p14|||See also pp15-16.||||||19-AUG-08
939|Bald Hill Claystone|34336|6|Mentioned|Table 5.15|||Triassic||||||
939|Bald Hill Claystone|34337|4|Described|p394|||Triassic.||||||
939|Bald Hill Claystone|34339|6|Mentioned|p442|||Re-sorted laterite attributes.||||||
939|Bald Hill Claystone|34506|6|Mentioned|p408|||||||||
939|Bald Hill Claystone|35095|6|Mentioned|p110|||||||||
939|Bald Hill Claystone|35874|6|Mentioned|p7|||||||||
939|Bald Hill Claystone|36042|6|Mentioned|Fig.22|||||||||
939|Bald Hill Claystone|36220|4|Described|p69|||See also p65 and Table 20.||||||19-AUG-08
939|Bald Hill Claystone|36221|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
939|Bald Hill Claystone|36222|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
939|Bald Hill Claystone|36223|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic.||||||
939|Bald Hill Claystone|36391|6|Mentioned|p157|||||||||
939|Bald Hill Claystone|36593|5|Briefly described|Table 2|||See also Fig.2||||||
939|Bald Hill Claystone|36594|6|Mentioned|Table 1|||See also Table II.||||||
939|Bald Hill Claystone|39293|5|Briefly described|p153|||||||||
939|Bald Hill Claystone|39296|4|Described|p184|||||||||
939|Bald Hill Claystone|39306|6|Mentioned|p389|||Coniferous forests. See also P414,417,418||||||
939|Bald Hill Claystone|39308|6|Mentioned|p494|||See also PP505 & 524. Cored ddh||||||
939|Bald Hill Claystone|39450|6|Mentioned|Table 1|||||||||
939|Bald Hill Claystone|40516|6|Mentioned|Fig.3|||||||||
939|Bald Hill Claystone|40601|6|Mentioned|Photo 11|||||||||
939|Bald Hill Claystone|40602|3|Fully described|p9|||||||||
939|Bald Hill Claystone|40625|6|Mentioned|Map legend|Early Triassic|Early Triassic|Early to Middle Triassic||||||
939|Bald Hill Claystone|40629|6|Mentioned|p186|||||||||
939|Bald Hill Claystone|40631|6|Mentioned|p160|||||||||
939|Bald Hill Claystone|40652|6|Mentioned|p128|||||||||
939|Bald Hill Claystone|40653|6|Mentioned|p121|||||||||
939|Bald Hill Claystone|42737|5|Briefly described|map legend|Triassic||||||||
939|Bald Hill Claystone|42896|3|Fully described|p29, Table 2|||Of Clifton Subgroup (Narrabeen Group).||||||19-AUG-08
939|Bald Hill Claystone|42925|5|Briefly described|Table 18||Early Triassic|||||||
939|Bald Hill Claystone|42926|4|Described|map legend||Early Triassic|||||||
939|Bald Hill Claystone|43028|6|Mentioned|Fig.7,p618|||of Narrabeen Group||||||
939|Bald Hill Claystone|43194|5|Briefly described|p131|Triassic|Triassic|Thick claystone - siltstone red beds deposited in the Sydney Basin during the Triassic.||||||
939|Bald Hill Claystone|43317|6|Mentioned|Table 3 p12|||||||||
939|Bald Hill Claystone|43323|14|Not recorded|p63,71|||Fossils (I56-9)||||||
939|Bald Hill Claystone|43342|14|Not recorded|Table 1 p107|||||||||
939|Bald Hill Claystone|43344|14|Not recorded|p21,68-70||Triassic|Unit of Narrabeen Group||||||
939|Bald Hill Claystone|43345|14|Not recorded|p3,5,7,9,15||Triassic|||||||
939|Bald Hill Claystone|43383|14|Not recorded|p22|||Part of Clifton Sub-Group||||||
939|Bald Hill Claystone|43385|14|Not recorded|p182 Table||Triassic|Ref. to Hanlon et al.,1953 (L.Bunter)||||||
939|Bald Hill Claystone|43392|14|Not recorded|p224||Triassic|O/lies Bulgo Sandstone||||||
939|Bald Hill Claystone|43395|14|Not recorded|p76|||||||||
939|Bald Hill Claystone|43449|14|Not recorded|p11,opp.12,Pl.2|||||||||
939|Bald Hill Claystone|43980|14|Not recorded|Pl.1|||||||||
939|Bald Hill Claystone|45090|6|Mentioned|p71|||Relationships in Narrabeen Gp.||||||
939|Bald Hill Claystone|45095|6|Mentioned|p137|||Refers McElroy (1969)||||||
939|Bald Hill Claystone|60281|5|Briefly described|p9|||Of the Narrabeen Group.  Provides an effective reservoir seal for the Narrabeen Group.||||||
939|Bald Hill Claystone|61315|5|Briefly described|Table SY2|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Acts as an effective reservoir seal at the top of the Narrabeen Group. Geological Province: Sydney Basin||||||
939|Bald Hill Claystone|64829|5|Briefly described|p1100 Fig. 15|Early Triassic|Early Triassic|At Long Reef, NSW. Palaeosol with Long Reef pedotype.||||||07-FEB-11
939|Bald Hill Claystone|66577|6|Mentioned|pp996-1000.|Triassic|Triassic|Provides a continuous reflection in the seismic data and is thus used in many diagrams in this article.||Unit in Narrabeen Group.||Overlies Bulgo Sandstone. Is overlain by Garie Formation.||
939|Bald Hill Claystone|67560|5|Briefly described|p258, p260-p272|Triassic|Triassic|Constrained by the age of the Narrabeen Group. ~ 106m thick. May have originated from the erosion and deposition of volcanic/lateritic materials in dominantly fresh (?lacustrine) water. Indicated by its low resistivity.||Of the Narrabeen Group.||Overlain gradationally by Garie Formation. Underlain by Bulgo Sandstone.|Iron-rich (red beds); dark grey claystones grading upwards into mainly chocolate claystones and dark, often green-grey, sandstone.|
939|Bald Hill Claystone|68003|5|Briefly described|p43.|Triassic|Triassic|Sydney Basin. Possibly terrestrial piedmont deposits.||Unit in upper part of Narrabeen Group.|||Thick claystone-siltstone red beds.|
939|Bald Hill Claystone|70661|6|Mentioned|p193, p195|||||Narrabeen Group||||
939|Bald Hill Claystone|73304|6|Mentioned|p74, p76|||Sydney Basin, southern.||Narrabeen Group||||
949|Baldwin Formation|5254|5|Briefly described|p122 Fig.1, p123||Late Devonian|Overlies Yarrimie Formation? Massive to thickly bedded, dark grey greywacke with subordinate arenite.||||||
949|Baldwin Formation|22572|5|Briefly described|p108||Devonian|Noumea-Lowana correlates||||||
949|Baldwin Formation|22736|6|Mentioned|p630|Famennian|Frasnian|||||||
949|Baldwin Formation|22768|5|Briefly described|p182||Late Devonian|||||||
949|Baldwin Formation|22857|5|Briefly described|p498 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Parry Group. Interpreted by Korsch and Harrington (1981) to rest unconformably on Tamworth Group. Max. thickness: >1500m. Geological Province: Tamworth Forearc Basin. See also p182 and p219.||||||
949|Baldwin Formation|22859|5|Briefly described|p219-20|||||||||
949|Baldwin Formation|23157|6|Mentioned|p126||Late Devonian|||||||
949|Baldwin Formation|23185|6|Mentioned|Fig1p156,Fig2p158||Famennian|||||||
949|Baldwin Formation|23522|5|Briefly described|p249 Fig 5|Famennian||||||||
949|Baldwin Formation|24009|5|Briefly described|p368 Fig.1|Late Devonian|Late Devonian|Maximum thickness: ~1000m.||||||14-APR-08
949|Baldwin Formation|24366|5|Briefly described|p17 Fig. 3|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||
949|Baldwin Formation|24614|6|Mentioned|p190|Famennian|Famennian|||||||07-FEB-11
949|Baldwin Formation|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
949|Baldwin Formation|31694|6|Mentioned|p341|||||||||
949|Baldwin Formation|31947|6|Mentioned|p31|||||||||
949|Baldwin Formation|31999|4|Described|Table 1|||||||||
949|Baldwin Formation|32286|6|Mentioned|Fig. 1|||||||||
949|Baldwin Formation|32482|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
949|Baldwin Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
949|Baldwin Formation|32672|6|Mentioned|p674|||||||||
949|Baldwin Formation|32865|6|Mentioned|p481|||L.Famennian||||||
949|Baldwin Formation|33101|6|Mentioned|Fig.1|||||||||
949|Baldwin Formation|33873|6|Mentioned|p5|||||||||
949|Baldwin Formation|34093|6|Mentioned|p278|||Dev.||||||
949|Baldwin Formation|34262|6|Mentioned|p242|||||||||
949|Baldwin Formation|34400|5|Briefly described|p8|||Upper Devonian||||||
949|Baldwin Formation|34555|3|Fully described|p238|||||||||
949|Baldwin Formation|35137|6|Mentioned|Fig.1|||||||||
949|Baldwin Formation|35192|6|Mentioned|Fig.1|||||||||
949|Baldwin Formation|35761|5|Briefly described|p64|||Stratigraphy discussed. See also Table 1.||||||
949|Baldwin Formation|35783|6|Mentioned|Fig.1|||Mineral deposits and geology of Nundle gold field.||||||
949|Baldwin Formation|36961|6|Mentioned|p208|||||||||
949|Baldwin Formation|37987|6|Mentioned|p219|||||||||
949|Baldwin Formation|38064|5|Briefly described|p40|||||||||
949|Baldwin Formation|38229|5|Briefly described|p452|||||||||
949|Baldwin Formation|38686|5|Briefly described|p56|||Geological Province: New England Fold Belt. Of the Parry Group, lower||||||
949|Baldwin Formation|38802|4|Described|p115|||Formerly Baldwin Agglomerate.||||||14-APR-08
949|Baldwin Formation|38821|5|Briefly described|p185|||||||||
949|Baldwin Formation|39214|4|Described|p35|||||||||
949|Baldwin Formation|39331|6|Mentioned|Table 10-1|||||||||
949|Baldwin Formation|39438|6|Mentioned|Table 5|||||||||
949|Baldwin Formation|39468|6|Mentioned|Fig.2|||||||||
949|Baldwin Formation|40246|6|Mentioned|p167|||||||||
949|Baldwin Formation|40883|6|Mentioned|p2|||See also P13||||||
949|Baldwin Formation|40960|6|Mentioned|p218|||||||||
949|Baldwin Formation|41009|6|Mentioned|p4|||Mention Fig.2||||||
949|Baldwin Formation|41238|5|Briefly described|p88|||||||||
949|Baldwin Formation|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Of the Parry Group.||||||16-DEC-04
949|Baldwin Formation|41796|6|Mentioned|p301|||||||||
949|Baldwin Formation|42376|5|Briefly described|Fig.1 P34|||||||||
949|Baldwin Formation|42547|6|Mentioned|p21|||||||||
949|Baldwin Formation|42728|5|Briefly described|p5|||||||||
949|Baldwin Formation|42849|6|Mentioned|p539|||Overlies the Tamworth Group.||||||09-MAY-05
949|Baldwin Formation|42887|6|Mentioned|p268|||||||||
949|Baldwin Formation|42997|5|Briefly described|p36|||||||||
949|Baldwin Formation|43147|5|Briefly described|p54|||||||||
949|Baldwin Formation|43344|14|Not recorded|p10,92,93||Late Devonian|||||||
949|Baldwin Formation|43383|14|Not recorded|p14||Late Devonian|||||||
949|Baldwin Formation|43384|14|Not recorded|Map Legend||Late Devonian|||||||
949|Baldwin Formation|43385|14|Not recorded|p174,175||Late Devonian|||||||
949|Baldwin Formation|43397|14|Not recorded|p209,210,212,map||Devonian|||||||
949|Baldwin Formation|43399|2|Defined|p189-90,193,195-6,||Late Devonian|p204||||||
949|Baldwin Formation|43400|14|Not recorded|p178,180,185,map||Late Devonian|||||||
949|Baldwin Formation|43406|14|Not recorded|p42-50|||Base of Parry Group||||||
949|Baldwin Formation|43407|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
949|Baldwin Formation|43409|14|Not recorded|Map Legend|||U.Dev turbidites;very quartz poor.Leptophloeum australe, Platclymenia.||||||
949|Baldwin Formation|43417|6|Mentioned|Map Legend|||Occurs north of Liverpool Range.||||||
949|Baldwin Formation|43418|14|Not recorded|Map Legend|||||||||
949|Baldwin Formation|43428|14|Not recorded|p135,140|||||||||
949|Baldwin Formation|43435|14|Not recorded|Map Legend|||||||||
949|Baldwin Formation|43446|14|Not recorded|p6041||Late Devonian|||||||
949|Baldwin Formation|43447|14|Not recorded|p4|||||||||
949|Baldwin Formation|43455|14|Not recorded|p460,462||Late Devonian|Contains Cheiloceras (index ammonoid)||||||
949|Baldwin Formation|43461|14|Not recorded|p619||Late Devonian|||||||
949|Baldwin Formation|43479|14|Not recorded|p136,150-1,157,216||Late Devonian|||||||
949|Baldwin Formation|43785|6|Mentioned|p369|||||||||
949|Baldwin Formation|43860|5|Briefly described|2, Fig1p3||Late Devonian|= Noumea beds||||||
949|Baldwin Formation|44379|14|Not recorded|p10||Late Devonian|||||||
949|Baldwin Formation|45088|6|Mentioned|p12|||Refers Crook (1961).||||||14-APR-08
949|Baldwin Formation|47056|6|Mentioned|Fig.2 P523|||||||||
949|Baldwin Formation|48600|14|Not recorded|Plate 3|||||||||
949|Baldwin Formation|48926|6|Mentioned|p56|||P57 etc.||||||24-FEB-10
949|Baldwin Formation|50132|6|Mentioned|p246 Fig. 4|Late Devonian|Late Devonian|New England Fold Belt, Manilla area||||||
949|Baldwin Formation|50168|5|Briefly described|p157 Fig.2, p158 Fig.3, p159|Late Devonian|Late Devonian|Gamilaroi Terrane. Well-preserved uppermost Devonian (Famennian) radiolarians have been recovered from this unit (T. Naka, pers. comm.).||||Underlain by the Yarrimie Formation.||06-FEB-18
949|Baldwin Formation|61765|6|Mentioned|p58, p58 Fig. 1|Late Devonian|Late Devonian|Geological Province: Tamworth Belt.||||||07-FEB-11
949|Baldwin Formation|61769|6|Mentioned|p96||Late Devonian|||||||
949|Baldwin Formation|63118|5|Briefly described|p202 Fig. 1|Late Devonian|Late Devonian|||||||
949|Baldwin Formation|65214|6|Mentioned|p282|Devonian|Devonian|NSW, Nundle and Tamworth. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
949|Baldwin Formation|66720|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Parry Group.|Includes Browning Vale Andesite Member and four un-named members mapped separately: sandstone-rich facies; mudstone-siltstone facies; conglomerates; and porphyritic andesite olistoliths and sills.||Lithic wacke and conglomerate with mudstone and siltstone.|
949|Baldwin Formation|68005|5|Briefly described|p54.|Late Devonian|Late Devonian|Of Crook (1961a); subsequently the Noumea beds, Lowana Formation, Eungai Mudstone and Mostyn Vale Formation (McKelvey and White, 1964; Brown, 1982).||Basal unit in Parry Group.||||
949|Baldwin Formation|68297|6|Mentioned|p194|Frasnian|Frasnian|Tamworth Trough||||||
949|Baldwin Formation|68822|6|Mentioned|p336, p347|||Downslope correlative of the Mostyn Vale Formation. Forearc basin depositional environment.||||||
949|Baldwin Formation|70907|6|Mentioned|p774 Fig.2|||||||||
949|Baldwin Formation|71628|6|Mentioned|p18: 20|||||Parry Group.||||
954|Baledmund Formation|9548|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Kopyje Group.  Includes: Three Peaks Siltstone Member, Mount Susannah Conglomerate Member.||||||06-JUL-04
954|Baledmund Formation|22768|5|Briefly described|p170|||||||||
954|Baledmund Formation|22831|6|Mentioned|p 38|||||||||
954|Baledmund Formation|22857|4|Described|p170, p444 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Kopyje Group (Cobar Supergroup). Laminated siltstone and fine-grained sandstone. Includes the Mount Boppy Conglomerate Member. Max. thickness: ~2km. Geological Province: Kopyje Shelf (Darling Basin).||||||
954|Baledmund Formation|23171|5|Briefly described|p15,31,Fig9p34|||||||||
954|Baledmund Formation|23173|4|Described|Map Legend|Lochkovian|Pridoli|||||||
954|Baledmund Formation|23522|5|Briefly described|p253|Middle Devonian|Early Devonian|||||||
954|Baledmund Formation|35287|6|Mentioned|p7|||||||||
954|Baledmund Formation|36118|6|Mentioned|p67|||||||||
954|Baledmund Formation|39618|2|Defined|p41|Early Devonian|Early Devonian|||||||
954|Baledmund Formation|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
954|Baledmund Formation|41394|6|Mentioned|p34|||||||||
954|Baledmund Formation|41528|2|Defined|p37|Early Devonian||Mention P110||||||
954|Baledmund Formation|41529|6|Mentioned|Map legend|Lochkovian||||||||
954|Baledmund Formation|42566|3|Fully described|p58|||||||||
954|Baledmund Formation|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
954|Baledmund Formation|43032|6|Mentioned|p27|||||||||
954|Baledmund Formation|43089|5|Briefly described|Map Legend|||of Kopyje Group||||||
954|Baledmund Formation|43441|6|Mentioned|25|||||||||08-JAN-10
954|Baledmund Formation|46900|6|Mentioned|Fig.2|||Stratigraphic table||||||
954|Baledmund Formation|65469|5|Briefly described|p15-p17|Early Devonian|Late Silurian|Lachlan Orogen.||Kopyje Group|Includes the Boomerang Tank Limestone Member.|||
954|Baledmund Formation|67416|5|Briefly described|p84 Fig.1, p85|||||Kopyje Group.|||Dominantly clastic (lesser pyroclastics).|
954|Baledmund Formation|69801|4|Described|p1, p4-p5, p11-p16, p135|Early Devonian|Silurian|Cobar Basin, Central Lachlan Orogen. An immature felsic volcaniclastic south-southeast of Canbelego yields a zircon age of 419.3 +/- 2.8 Ma, this is interpreted as a max depositional age but could represent the true depositional age on the basis of brachiopod and conodont assemblages elsewhere in the unit. Brachiopod assemblages in the lower part of the formation are late Silurian/early Devonian belonging to the Rietzella Capricornae zone. Conodonts are hosted in limestone and belong to the Pedavis pesavis zone. SHRIMP analyses and interpretation are detailed.|419.3 +/- 2.8 Ma (Max dep age)|Kopyje Group||Interfingered with the Florida Volcanics.|Dominantly siltstone and lesser quartz arenite and limestone. Sample dated is a massive, granule to pebble sized, texturally immature volcaniclastic sandstone. Minor volcaniclastic agglomerate.|
954|Baledmund Formation|70751|4|Described|p6, p7-8, p10-12, p17, 21,22,23,24,27,38|Early Devonian|Late Silurian|Canbelego-Mineral Hill Volcanic Belt. Additional dates derived via SHRIMP include 428.2 +/- 3.9 Ma (Spandler, 1998) and 417.6 +/- 3.2 Ma (this study- derived from volcaniclastic sandstone.|419.3 +/- 2.8 Ma (SHRIMP, Bodorkos et al, 2015)|Kopyje Group||Interfingers with the Babinda Volcanics, Florida Volcanics and the Majuba Volcanics.|Includes fine-grained sedimentary rocks, volcaniclastic sandstone..|24-SEP-19
954|Baledmund Formation|70828|5|Briefly described|p4-5|||Part of the Baledmund Formation is a fault-bounded inlier, of which occurs 5km  NE of the Break O'Day Amphibolite.||Unit of Cobar Supergroup.|||Siltstone with minor sandstone, pebbly sandstone, tuff.|
954|Baledmund Formation|70876|4|Described|p1, p9, p76|Devonian|Silurian|Lachlan Orogen. SHRIMP age is derived from Bodorkos et al, 2015. SHRIMP age is interpreted as the maximum depositional age for this unit.|419.3 +/- 2.8 Ma (SHRIMP U-Pb)|||Interfingers with (and is overlain by) the Babinda Volcanics.||
954|Baledmund Formation|70941|5|Briefly described|p78, p78 fig 32, p94, p137|||Misspellt as the Balledmund Formation on p144. |||Mount Boppy Conglomerate Member.|Correlative of the Meryula Formation. Overlies the Mount Boppy Conglomerate Member. Overlain by the Florida Volcanics.|Siltstone, arenite, tuff, cherty siltsone and limestone.|
954|Baledmund Formation|70950|6|Mentioned|p1030|||Shallow marine sedimentary rocks||||Interfingers with Babinda Volcanics, MajubaVolcanics|Fine-grained terrigenous to shallow marine sedimentary rocks.|
954|Baledmund Formation|71039|5|Briefly described|p11-p12, p27|Devonian|Silurian|Consistently preserve zeolite to epizone greenschist facies rift basin metamorphic mineral assemblages. The majority of this unit shows partial recrystallisation to the secondary assemblage of sericite, chlorite, clay minerals, iron oxide and silica. CAI indicates burial metamorphism temperatures between 200-250 degrees C. In contact with the Majuba Volcanics although the relationship is not made clear.||Kopyje Group||||08-MAR-23
954|Baledmund Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|Boulder to granule polymictic conglomerate and sedimentary/volcanic breccia are variably developed.||Kopyje Group.|||Thinly laminated, rarely calcareous, siltstone and minor interbedded well-sorted fine-grained lithic-quartz sandstone. Locally abundant vitric, tuffaceous to crystal lithic sandstone-siltstone, reflecting distal airfall/water lain deposits.|
954|Baledmund Formation|72080|5|Briefly described|p5-p6, p9, p13|Early Devonian|Late Silurian|Harts Tank area.||Kopyje Group|Includes the Beloura Tank Limestone.|Interfingers with the Babinda Volcanics.|Basal conglomerate fining up into pebbly sandstone, sandstone, siltstone and limestone with intercalated felsic volcaniclastic rocks.|07-JAN-22
954|Baledmund Formation|72908|5|Briefly described|p5, p8 Tb.1, p23, p30|Late Silurian|Late Silurian|Hosts the Pipeline Ridge deposit.|419.3+/-2.8 Ma U-Pb SHRIMP zircon|Kopyje Group|||Fine-grained terrigenous to shallow-marine sedimentary rocks.|
954|Baledmund Formation|72958|6|Mentioned|p11|Lochkovian|Pridoli|Cobar Basin. Nymagee area.||||Equivalent to Babinda Volcanics and Majuba Volcanics. Intruded[?] by Mount Walton porphyry.||
954|Baledmund Formation|73174|6|Mentioned|p1036-1040, p1044|Lochkovian|Lochkovian|Kopyje Shelf. Contains age-diagnostic conodont and trilobite.||Kopyji Group, Cobar Supergroup|Boomerang Tank Limestone Member, Mount Boppy Conglomerate Member|Underlain by Girilambone Beds [Group]. Equivalent to Meryula Formation and Brookong Formation.||
954|Baledmund Formation|73578|6|Mentioned|p32, p35|Lochkovian|Pridoli|A maximum depositional age of 419.3 +/- 2.8 Ma was reported by Bodorkos et al. (2015).|419.3 +/- 2.8 Ma|||Interfingers with the Majuba Volcanics.||
965|Balickera Conglomerate|24121|5|Briefly described|p151||||||||coarse polymictic boulder conglomerate.|
965|Balickera Conglomerate|30074|6|Mentioned|p27|||||||||
965|Balickera Conglomerate|31228|6|Mentioned|p83|||Refers Rattigan (1967).||||||
965|Balickera Conglomerate|32379|6|Mentioned|p10|||||||||
965|Balickera Conglomerate|32836|6|Mentioned|Table 1|||Palaeobotany||||||
965|Balickera Conglomerate|34085|6|Mentioned|Cor.chart|||Namurian||||||
965|Balickera Conglomerate|34238|6|Mentioned|p8|||See also Fig.2||||||
965|Balickera Conglomerate|36528|6|Mentioned|p179|||||||||
965|Balickera Conglomerate|39666|6|Mentioned|p103|||||||||
965|Balickera Conglomerate|40883|6|Mentioned|p8|||||||||
965|Balickera Conglomerate|42547|4|Described|p31|||||||||
965|Balickera Conglomerate|44244|6|Mentioned|p94|||Of Rattigan (1967a).  Together with the Italia Raod Formation is the equivalent of the Mount Johnstone Formation.  Contains tuff and ignimbrite.||||||19-AUG-04
965|Balickera Conglomerate|44253|5|Briefly described|p6||Carboniferous|Unit of King's Hill Group.||||||
965|Balickera Conglomerate|44254|2|Defined|p76,77,81-83||Stephanian|||||||
965|Balickera Conglomerate|44255|14|Not recorded|p120|||Unit of King's Hill Group.||||||
965|Balickera Conglomerate|45097|6|Mentioned|Fig.|||Carboniferous correlation chart||||||
965|Balickera Conglomerate|50132|6|Mentioned|p246 Fig. 4|Late Carboniferous|Late Carboniferous|New England Fold Belt, Raymond Terrace area||||||
965|Balickera Conglomerate|71233|5|Briefly described|p104 Fig.1, p105, p106 Fig.2|Carboniferous|Carboniferous|Hunter Valley. 418m thick. The type section appears to be the Balickera canal excavation joining the Williams River (E of Seaham) to Grahamstown Reservoir (Rattigan, 1967).||||Is overlain conformably by Italia Road Formation.||
991|Ballengara Member|38803|5|Briefly described|p105|||||||||
997|Ballimore Formation|22833|6|Mentioned|p654|||of Sydney Basin.||||||
997|Ballimore Formation|30610|1|Redefined|p323|Early Jurassic|Late Triassic|Upper Triassic - Lower Jurassic||||||
997|Ballimore Formation|32045|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
997|Ballimore Formation|32485|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
997|Ballimore Formation|35095|6|Mentioned|Table 1|||||||||
997|Ballimore Formation|37757|6|Mentioned|p29|||||||||
997|Ballimore Formation|39298|6|Mentioned|p255|||||||||
997|Ballimore Formation|40328|6|Mentioned|p124|||See also P130||||||
997|Ballimore Formation|42993|5|Briefly described|p61|||||||||
997|Ballimore Formation|43476|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
997|Ballimore Formation|50616|5|Briefly described|p275|Triassic|Triassic|||||||
1000|Ballyhooley Granite|42726|5|Briefly described|map legend|Silurian||May be related to Bally Hooley Ignimbrite, reserved MAR-89.||||||
1000|Ballyhooley Granite|50231|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of the Wyangala Batholith.||||||
1000|Ballyhooley Granite|61910|5|Briefly described|p152 Fig. 1|Late Silurian|Late Silurian|Part of the Wyangala Batholith. Geological Province: Lachlan Fold Belt.||||||
1000|Ballyhooley Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Grey, coarse-grained, foliated, equigranular biotite granodiorite in a zoned pluton with medium-grained, foliated, often prophyritic biotite granodiorite stocks. Moderately high K.Th and U radioelement response.||||||09-SEP-08
1000|Ballyhooley Granite|66713|4|Described|p3 Fig.2, p5, p12||Homerian|Frogmore area. Variably foliated, coarse-grained, equigranular, S-type muscovite-biotite granite to biotite granite, weakly reduced and moderately to strongly fractionated. U-Pb SHRIMP zircon age 425 +/- 3 Ma (Lennox and Zwingmann, 2007). In Hovells Suite.||||||
1000|Ballyhooley Granite|67820|6|Mentioned|p135|||Reduced and moderately to highly fractionated. Potential for Sn-W mineralisation. The probable source of the (chiefly) W mineralisation at the Phoenix mine.||||||
1000|Ballyhooley Granite|68592|3|Fully described|p1258-9, p1262-4, p1266-71, p1274, p1284|Late Silurian|Late Silurian|See also xxiv, p325, p342, p1255 Fig.220. Named (after Ballyhooley property) by Gibbons (1960) for some granites included in the undifferentiated Wyangala Batholith by Stevens (1955) and Brunker and Offenberg (1970); published by Chappell et al. (1991). Subsequent mapping by Bartolo (1994) and O'Sullivan (1993) included many minor stocks to this unit. Here assigned to the Hovells Suite on geochemical grounds. Type locality described. The main pluton forms a prominent group of hills E of Hovells Creek. Geochemistry detailed; geophysical properties described. Contact metamorphism has produced chiastolite porphyroblasts in the vicinity. Potential source of Sn-W mineralisation. Age by Lennox and Zwingmann, reported in Downes et al. (2011).|425 +/- 3 Ma (SHRIMP U-Pb zircon).|Unit in Hovells Suite.||Intrudes Adaminaby Group, Reids Flat Granite, Kenyu Formation and Warbisco Shale.|Subcircular compositional zonation: the core comprises grey, medium- to coarse-grained, foliated, equigranular, muscovite-biotite granite; surrounded by grey, medium- to coarse-grained, biotite granodiorite. Foliated.|
1000|Ballyhooley Granite|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Sob. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Zoned pluton with a core of medium-coarse grained, foliated, equigranular, muscovite-biotite granite, surrounded by a zone of medium-coarse grained commonly porphyritic, biotite granodiorite; high K and medium to high Th and U responses.|
1000|Ballyhooley Granite|70545|5|Briefly described|Map Legend |Devonian|Silurian|||Hovells Suite|||Zoned pluton with a core of medium-coarse grained, foliated, equigranular, muscovite-biotite granite, surrounded by a zone of medium-coarse grained commonly porphyritic, biotite granodiorite; high K and medium to high Th and U responses.|
1000|Ballyhooley Granite|71069|6|Mentioned|p75|||Chiastolite porphyroblasts occur near where this unit intrudes in the Goulburn 250 Map Sheet.||||||
1001|Balmoral Coal Member|23350|5|Briefly described|263|||See also Balmoral Coal - names used interchangeably in text.||||||15-JUL-04
1001|Balmoral Coal Member|36940|6|Mentioned|p141|||||||||
1001|Balmoral Coal Member|37773|6|Mentioned|p19|||||||||
1001|Balmoral Coal Member|39346|6|Mentioned|Map legend|Permian|Permian|||||||
1001|Balmoral Coal Member|40331|6|Mentioned|p5|||See also Fig.4||||||
1001|Balmoral Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Skeletar Formation.||||
1029|Bandandra sand|39512|6|Mentioned|p2|||||||||
1037|Bangadilly Granite|42726|5|Briefly described|Map Legend|Early Devonian|Early Devonian|60.   I-type, felsic, unfractionated. Of the Bangadilly Suite.  Not intended as a formal name||||||17-FEB-12
1037|Bangadilly Granite|70661|3|Fully described|p75 - p77, p79 fig 6, p92-p94|Early Devonian|Early Devonian|Previously the sole member of the Bangadilly suite. Named after Bangadilly property. Originally included in the undifferentiated Marulan Batholith. Previously termed the Bangadilly Adamellite or Bangadilly Granodiorite, name changed to better suite the lithology of this unit and avoid confusion. Outcrops in rivers and creeks. No type section proposed.  Distribution,  metamorphism, geochemistry and geophysical characteristics discussed. Mistakenly referred to as the Bungadilly Granite on p6. Lithology discussed further. Equivalent to the other plutons of the Arthursleigh Suite.||Arthursleigh Suite||Intrudes Adaminaby Group, Bindook Group, overlain by Berry Siltstone|Varies from coarse grained, biotite adamellite to a medium-coarse grained, homogenous, biotite-hornblende granodiorite. The adamellite is characterised by perthitic Kfeldspar crystals. Aplite veins are common.|
1037|Bangadilly Granite|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Arthursleigh Suite.|||Coarse-grained biotite granite to a medium- to coarse-grained biotite-hornblende granodiorite.|
1051|Bango Limestone Member|22691|6|Mentioned|P321||Silurian|||||||
1051|Bango Limestone Member|22768|6|Mentioned|p176|||||||||
1051|Bango Limestone Member|22857|4|Described|p176, p460 App.1 Tb.A1.6|Middle Silurian|Middle Silurian|Of the Hawkins Volcanics. Contains corals, gastropods, brachiopods, crinoids. Max. thickness: 90m. Geological Province: Canberra-Yass Shelf.||||||
1051|Bango Limestone Member|24417|5|Briefly described|p46|||Of Douro Group.||||||
1051|Bango Limestone Member|30069|6|Mentioned|p5|||||||||
1051|Bango Limestone Member|32675|6|Mentioned|p8|||Refers Link (1970,1971)||||||
1051|Bango Limestone Member|35070|6|Mentioned|p78|||P107 also.||||||
1051|Bango Limestone Member|35384|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
1051|Bango Limestone Member|35386|3|Fully described|p15|||||||||
1051|Bango Limestone Member|36411|6|Mentioned|p267|||Refers Cramsie et al 1978 for redefinition.||||||
1051|Bango Limestone Member|37529|6|Mentioned|p8|||||||||
1051|Bango Limestone Member|40328|6|Mentioned|p59|||Also mentioned on P87||||||
1051|Bango Limestone Member|42313|6|Mentioned|p125|Wenlockian||Member of Douro Group. Age: middle Wenlockian.||||||
1051|Bango Limestone Member|50230|5|Briefly described|Map legend|Early Silurian|Early Silurian|Of the Hawkins Volcanics (Douro Group).  Grey fossiliferous limestone.  Overlies the Mundoonen Sandstone but contact not clear.||||||
1051|Bango Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Hawkins Volcanics (Douro Group). Grey fossiliferous limestone.||||||02-JUN-08
1051|Bango Limestone Member|66197|6|Mentioned|p630|Wenlock|Wenlock|Of Hawkins Volcanics.||||||14-MAR-12
1051|Bango Limestone Member|68592|2|Defined|p433, p435, p440, p456-8, p469-71|Wenlock|Wenlock|See also p356, p428, p430 Fig.89, p778, p1874. Pogson and Baker (1974); Cramsie et al. (1978); formerly Bango Beds (Shearsby, 1912), Bango Series (Brown, 1940). Type section is Bango Limestone Quarry, where it is 50 m thick; quarried for burnt lime. Three small limestone bodies. Recrystallised fossils include tabulate and solitary rugose corals, gastropods, crinoids; rare brachiopods and stromatoporoids.||Unit in Hawkins Volcanics.||Probably correlates (similar age and lithology) with the Kingsdale Limestone Member (Hawkins Volcanics)|Grey or white, massive, recrystallised fossiliferous limestone.|
1051|Bango Limestone Member|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdhb. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hawkins Volcanics||Shown on Time-Space Plot as within unnamed member of Hawkins Volcanics.|Massive, recrystallised, fossiliferous limestone.|
1051|Bango Limestone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Hawkins Volcanics|||Massive, recrystallised, fossiliferous limestone.|
1051|Bango Limestone Member|71069|6|Mentioned|p95|||||Hawkins Volcanics||||
1051|Bango Limestone Member|71656|5|Briefly described|p12 Fig.2, p21|Wenlock|Wenlock|Common on weathered surfaces in the Bango Quarry is a halysitid coral. Recrystallisation hinders species determination. No diagnostic fossils identified but the fauna is assigned to a Wenlockian to basal Ludlovian assemblage. Unit is shown as Wenlock in Fig.2.||Hawkins Volcanics||Douro Group. Within Hawkins Volcanics.|Pervasive recrystallisation of the limestone|
1051|Bango Limestone Member|71700|6|Mentioned|CD|||||Hawkins Volcanics||Overlies the Mundoonen Sandstone.||
1065|Banks Wall Sandstone|22745|6|Mentioned|p130|||Sydney Basin.||||||
1065|Banks Wall Sandstone|22857|5|Briefly described|p526 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Grose Subgroup (Narrabeen Group). Quartzose sandstone. Max. thickness: 114.6m. Geological Province: Sydney Basin.||||||
1065|Banks Wall Sandstone|23218|6|Mentioned|p28|||||||||
1065|Banks Wall Sandstone|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
1065|Banks Wall Sandstone|29749|4|Described|p11|||||||||
1065|Banks Wall Sandstone|31061|6|Mentioned|Table 1|||||||||
1065|Banks Wall Sandstone|31373|6|Mentioned|Table 2|||||||||
1065|Banks Wall Sandstone|31725|6|Mentioned|p7|||||||||
1065|Banks Wall Sandstone|31886|6|Mentioned|p394|||||||||
1065|Banks Wall Sandstone|32801|6|Mentioned|p254|||||||||
1065|Banks Wall Sandstone|32802|6|Mentioned|p22|||||||||
1065|Banks Wall Sandstone|36042|6|Mentioned|Fig.24|||||||||
1065|Banks Wall Sandstone|37804|6|Mentioned|Table 1|||||||||
1065|Banks Wall Sandstone|39287|6|Mentioned|p44|||||||||
1065|Banks Wall Sandstone|39293|4|Described|p151|||See also P154.||||||
1065|Banks Wall Sandstone|39306|6|Mentioned|p389|||See also P415||||||
1065|Banks Wall Sandstone|39308|6|Mentioned|p500|||See also PP501 & 504||||||
1065|Banks Wall Sandstone|42663|6|Mentioned|p11|||See misspelling Bansk Wall Sandstone.||||||
1065|Banks Wall Sandstone|42925|3|Fully described|p12|||of Grose Subgroup||||||
1065|Banks Wall Sandstone|42926|4|Described|map legend||Early Triassic|||||||
1065|Banks Wall Sandstone|43047|5|Briefly described|p272|||||||||
1065|Banks Wall Sandstone|43194|5|Briefly described|p119, 130|Early Triassic|Early Triassic|Broad correlative of the informal middle 'lithic sandstone unit' and 'upper quartzose unit'  of the Digby Formation, Gunnedah Basin.||||||
1065|Banks Wall Sandstone|45090|6|Mentioned|p71|||Relationship in Narrabeen Gp.||||||
1065|Banks Wall Sandstone|65195|5|Briefly described|p3-4, p7-12, p15, p22-27, p33|Early Triassic|Early Triassic|Of Narrabeen Group. Originally named by Goldberry (1972); renamed by Bembrick and Holland (1972). Predominantly quartzose, but also contains abundant ironstone bands, occasional conglomerates and numerous claystone lenses several metres thick. Friable, hence susceptible to erosion. Includes Wentworth Falls Claystone Member.||||||
1065|Banks Wall Sandstone|68003|5|Briefly described|p42.|Triassic|Triassic|Western Sydney Basin. Quartzose sediments from uplifted Lachlan Fold Belt to the west.||||||
1073|Banshea Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Banshea Adamellite, Banshee Adamellite.||||||
1073|Banshea Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Cream to pink to pale green, coarse-grained, inequigranular to strongly porphyritic, biotite-hornblende granite; finer-grained, more mafic granite occurs at north-east margin.||||||09-SEP-08
1073|Banshea Granite|68592|3|Fully described|p183, p194, p236, p1610-3, p1615-20|Early Devonian|Early Devonian|See also p756. Chappell et al. (1991) after Scheibner (1973). First mapped in detail and defined as Banshea Adamellite by Sylvester (1966). The most detailed work was done by Budd (1992). Here placed in Arthursleigh Suite. Named after Banshea State Forest. Apparently no type locality; representative exposures described. Better exposed on the edge of the Jenolan Plateau. Geochemistry detailed; geophysical properties described. Hosts the Ruby Creek Pb-Zn-Ag mine (detailed) and other minor base metal occurrences; has been linked with the chalcopyrite-pyrite-tetrahedrite mineralisation in the Hell Hole Mine in the Cobra Formation. Various age determinations by previous workers ranged from 431 Ma to Carboniferous (details given). It is pre Late Devonian: thought to be mid to late Early Devonian. Has petrographic similarities with Barrallier Ignimbrite.|413 +/- 9 Ma K-Ar biotite; minimum age.|Unit in Arthursleigh Suite.||Intrudes Adaminaby Group. Is overlain nonconformably by Lambie Group. Possible/mininal contact metamorphism of Cobra and Abercrombie Formations rocks.|Variable composition. Mainly greenish-grey porphyritic granite with subordinate cream, coarse-grained, inequigranular granite and black to pink/green, fine-grained, hornblende-rich granite; minor pink, fine-grained aplitic phases. I-type.|
1073|Banshea Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dab. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Arthursleigh Suite|||Porphyritic, biotite-hornblende granite with subordinate, coarse grained, inequigranular, hornblende-biotite granite and fine grained, hornblende rich granite; minor aplitic phases; low K, Th and U responses; low magnetic susceptibility.|
1073|Banshea Granite|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Arthursleigh Suite|||Porphyritic, biotite-hornblende granite with subordinate, coarse grained, inequigranular, hornblende-biotite granite and fine grained, hornblende rich granite; minor aplitic phases; low K, Th and U responses; low magnetic susceptibility.|
1073|Banshea Granite|70661|6|Mentioned|p75 - p77|||||||Intrudes Adaminaby Group, Overlain by Lambie Group.||
1073|Banshea Granite|71206|6|Mentioned|p379|||Lachlan Fold Belt.|||||Fractionated I-type granite.|
1073|Banshea Granite|72528|4|Described|p1, p3 Tb.1.1, p25-30, p108, p124.|Lochkovian|Lochkovian|New magmatic crystallisation zircon age from 30 km NNE of Taralga confirms that this pluton is part of the Arthursleigh Suite within the Marulan Supersuite. Previous Rb-Sr and K-Ar dating also discussed. Constrains the age of the Ruby Creek silver prospect.|413.3+/-1.8 Ma 238U/206Pb (207Pb-corrected)|Arthursleigh Suite||Intrudes Adaminaby Group (Campbells Group) and underlies Lambie Group.|Dated sample is porphyritic granite.|01-FEB-21
1077|Bar Beach Formation|22578|6|Mentioned|p401|||||||||
1077|Bar Beach Formation|23055|6|Mentioned|Fig11p23|||||||||
1077|Bar Beach Formation|29922|6|Mentioned|p49|||||||||
1077|Bar Beach Formation|29926|6|Mentioned|Fig.3|||||||||
1077|Bar Beach Formation|34351|5|Briefly described|p343|||Fig.5.13||||||
1077|Bar Beach Formation|37083|6|Mentioned|p164|||||||||
1077|Bar Beach Formation|39292|6|Mentioned|Fig. 6.2|||||||||
1077|Bar Beach Formation|39308|6|Mentioned|Fig. 23.4|||||||||
1077|Bar Beach Formation|39609|5|Briefly described|p3|||See also Table 1||||||
1077|Bar Beach Formation|41479|6|Mentioned|Fig.2|||||||||
1077|Bar Beach Formation|43344|14|Not recorded|p85||Late Permian|Table only||||||
1077|Bar Beach Formation|43447|14|Not recorded|diag p26,34|||Part of Lambton Sub-Group||||||
1077|Bar Beach Formation|43448|14|Not recorded|p224||Permian|Table only. Unit of Lambton Subgroup (Newcastle Coal Measures)||||||
1077|Bar Beach Formation|45090|6|Mentioned|p186|||Refers McKenzie (1962)||||||
1077|Bar Beach Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Lambton Subgroup|Included Signal Hill Conglomerate Member|||
1078|Baralaba Coal Measures|13516|5|Briefly described|p145 fig 3, p157|Late Permian|Late Permian|From Taroom Shelf, Bowen Basin. Age: APP5005 - APP6||||||
1078|Baralaba Coal Measures|22439|5|Briefly described|p15, Fig.2|Late Permian|Late Permian|Geological province: Taroom Trough, Bowen Basin.||||||25-AUG-08
1078|Baralaba Coal Measures|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|23003|5|Briefly described|p423 Table 1|Permian|Permian|Of the Blackwater Group.||||||26-AUG-08
1078|Baralaba Coal Measures|23004|5|Briefly described|p431 Table 1|Permian|Permian|Of the Blackwater Group.||||||26-AUG-08
1078|Baralaba Coal Measures|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
1078|Baralaba Coal Measures|23359|6|Mentioned|77|||||||||
1078|Baralaba Coal Measures|24159|5|Briefly described|p147|Late Permian|Late Permian|Parent: Blackwater Group. Geological Province: Bowen Basin.||||||
1078|Baralaba Coal Measures|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pwb].  Feldspathic and lithic sandstone, siltstone, mudstone, coal, conglomerate, tuff.||||||
1078|Baralaba Coal Measures|29411|5|Briefly described|p201|||||||||
1078|Baralaba Coal Measures|29723|6|Mentioned|p17|||||||||
1078|Baralaba Coal Measures|29727|6|Mentioned|p455|||||||||
1078|Baralaba Coal Measures|30137|4|Described|p2|||Upper Permian age.||||||
1078|Baralaba Coal Measures|30140|6|Mentioned|p2|||Upper Permian age||||||
1078|Baralaba Coal Measures|30141|5|Briefly described|p135|||||||||
1078|Baralaba Coal Measures|30448|6|Mentioned|p100|||||||||
1078|Baralaba Coal Measures|30451|3|Fully described|p62|||See also p63,64||||||26-AUG-08
1078|Baralaba Coal Measures|30460|6|Mentioned|p3|||See also P16,18,22,24,27. Fig.2||||||
1078|Baralaba Coal Measures|30546|6|Mentioned|p107|||Upper Permian age. Correlation||||||
1078|Baralaba Coal Measures|30743|3|Fully described|p21|||See also p22-34. Refers Reid (1944), Goscombe (1968)||||||26-AUG-08
1078|Baralaba Coal Measures|30916|6|Mentioned|p98|||||||||
1078|Baralaba Coal Measures|31079|6|Mentioned|p5|||See also Fig. 6||||||
1078|Baralaba Coal Measures|31088|6|Mentioned|p398|||||||||
1078|Baralaba Coal Measures|31116|4|Described|p11|||Upper Permian.||||||26-AUG-08
1078|Baralaba Coal Measures|31261|6|Mentioned|p518|||||||||
1078|Baralaba Coal Measures|31380|6|Mentioned|p131|||Refers Rigby(1972)||||||
1078|Baralaba Coal Measures|31391|6|Mentioned|p34|||See also P36.U.Permian||||||
1078|Baralaba Coal Measures|31531|6|Mentioned|Table 1|||U.Permian||||||
1078|Baralaba Coal Measures|31647|6|Mentioned|p354|||||||||
1078|Baralaba Coal Measures|31649|6|Mentioned|p57|||||||||
1078|Baralaba Coal Measures|32832|6|Mentioned|p4||Permian|||||||
1078|Baralaba Coal Measures|32834|6|Mentioned|p26|||See also Table 3||||||
1078|Baralaba Coal Measures|32835|6|Mentioned|p1|||Flora||||||
1078|Baralaba Coal Measures|32840|6|Mentioned|p10|||||||||
1078|Baralaba Coal Measures|32944|6|Mentioned|Fig.3|||Permian||||||
1078|Baralaba Coal Measures|33128|4|Described|p50|||Geochemistry. See also p52 and Figs. 2 and 5.||||||26-AUG-08
1078|Baralaba Coal Measures|33363|5|Briefly described|p115|||Upper Permian.||||||25-AUG-08
1078|Baralaba Coal Measures|33711|6|Mentioned|Table 3|||||||||
1078|Baralaba Coal Measures|33774|3|Fully described|p38|||Map||||||
1078|Baralaba Coal Measures|34094|5|Briefly described|p1-4,Figs.2,3,4||Late Permian|||||||
1078|Baralaba Coal Measures|34095|5|Briefly described|p3-6,26,Figs.5,6||Late Permian|||||||
1078|Baralaba Coal Measures|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
1078|Baralaba Coal Measures|34235|6|Mentioned|p92|||||||||
1078|Baralaba Coal Measures|34574|6|Mentioned|p115|||||||||
1078|Baralaba Coal Measures|35138|6|Mentioned|Fig.2-3|||||||||
1078|Baralaba Coal Measures|35266|6|Mentioned|p192|||||||||
1078|Baralaba Coal Measures|35426|3|Fully described|p659|||||||||
1078|Baralaba Coal Measures|35873|4|Described|p12|||||||||
1078|Baralaba Coal Measures|35901|6|Mentioned|p2|||||||||
1078|Baralaba Coal Measures|35937|6|Mentioned|p619|||||||||
1078|Baralaba Coal Measures|36172|6|Mentioned|Appendix|||||||||
1078|Baralaba Coal Measures|36241|6|Mentioned|p130|||||||||
1078|Baralaba Coal Measures|36243|6|Mentioned|Table 4A|||||||||
1078|Baralaba Coal Measures|36327|6|Mentioned|p8|||||||||
1078|Baralaba Coal Measures|36333|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|36739|6|Mentioned|p19|||||||||
1078|Baralaba Coal Measures|36825|6|Mentioned|p19|||||||||
1078|Baralaba Coal Measures|36925|6|Mentioned|Fig.1|||||||||
1078|Baralaba Coal Measures|36954|6|Mentioned|p114|||||||||
1078|Baralaba Coal Measures|37065|6|Mentioned|p32|||||||||
1078|Baralaba Coal Measures|37070|4|Described|p73|||||||||
1078|Baralaba Coal Measures|37075|5|Briefly described|Table 1|||||||||
1078|Baralaba Coal Measures|37400|6|Mentioned|Table 2|||||||||
1078|Baralaba Coal Measures|37858|6|Mentioned|p82|||||||||
1078|Baralaba Coal Measures|38153|6|Mentioned|p373|||||||||
1078|Baralaba Coal Measures|38358|6|Mentioned|p11|||||||||
1078|Baralaba Coal Measures|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1078|Baralaba Coal Measures|38603|6|Mentioned|p81|||||||||
1078|Baralaba Coal Measures|38951|6|Mentioned|p408|||||||||
1078|Baralaba Coal Measures|38958|5|Briefly described|p493|||||||||
1078|Baralaba Coal Measures|38971|4|Described|p543|||||||||
1078|Baralaba Coal Measures|39212|6|Mentioned|p14|||||||||
1078|Baralaba Coal Measures|39252|6|Mentioned|p26|||See also P28||||||
1078|Baralaba Coal Measures|39260|5|Briefly described|Fig.2|||||||||
1078|Baralaba Coal Measures|39261|6|Mentioned|Fig.6|||||||||
1078|Baralaba Coal Measures|39266|6|Mentioned|p221|||||||||
1078|Baralaba Coal Measures|39267|6|Mentioned|p240|||||||||
1078|Baralaba Coal Measures|39445|5|Briefly described|Table 8|||See also Table 9.||||||25-AUG-08
1078|Baralaba Coal Measures|39777|6|Mentioned|p151|||||||||
1078|Baralaba Coal Measures|39943|6|Mentioned|Table 6A|||||||||
1078|Baralaba Coal Measures|40087|6|Mentioned|p234|||See also P237||||||
1078|Baralaba Coal Measures|40092|5|Briefly described|p51|||||||||
1078|Baralaba Coal Measures|40096|6|Mentioned|p2|||||||||
1078|Baralaba Coal Measures|40539|6|Mentioned|p164|||||||||
1078|Baralaba Coal Measures|40860|6|Mentioned|p109|||||||||
1078|Baralaba Coal Measures|41130|4|Described|p56|||||||||
1078|Baralaba Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
1078|Baralaba Coal Measures|41666|6|Mentioned|p26|||||||||
1078|Baralaba Coal Measures|41689|6|Mentioned|Table 1|||||||||
1078|Baralaba Coal Measures|42091|6|Mentioned|p284|||||||||
1078|Baralaba Coal Measures|42187|6|Mentioned|p319|||||||||
1078|Baralaba Coal Measures|42212|6|Mentioned|p329|||||||||
1078|Baralaba Coal Measures|42249|6|Mentioned|p23|||||||||
1078|Baralaba Coal Measures|42250|6|Mentioned|Fig.4 P31|||||||||
1078|Baralaba Coal Measures|42251|5|Briefly described|p39|||||||||
1078|Baralaba Coal Measures|42256|6|Mentioned|Fig.1 P243|||||||||
1078|Baralaba Coal Measures|42309|6|Mentioned|p257|||||||||
1078|Baralaba Coal Measures|42431|6|Mentioned|p234|||||||||
1078|Baralaba Coal Measures|42641|6|Mentioned|p115|||||||||
1078|Baralaba Coal Measures|42648|6|Mentioned|p40|||||||||
1078|Baralaba Coal Measures|42865|5|Briefly described|p18|||||||||
1078|Baralaba Coal Measures|42932|6|Mentioned|p4|||||||||
1078|Baralaba Coal Measures|43000|5|Briefly described|p113|||||||||
1078|Baralaba Coal Measures|43017|5|Briefly described|Fig.3,p375|||||||||
1078|Baralaba Coal Measures|43987|14|Not recorded|p270|||Banana-Cracow area||||||
1078|Baralaba Coal Measures|44118|14|Not recorded|Map Legend||Late Permian|||||||
1078|Baralaba Coal Measures|44129|14|Not recorded|p95-96||Permian|||||||
1078|Baralaba Coal Measures|44169|2|Defined|Tb.1,p6,8,12,map|||||||||21-DEC-11
1078|Baralaba Coal Measures|44170|2|Defined|p6,12-16,2,25,31,||Late Permian|Tb.1||||||
1078|Baralaba Coal Measures|44218|14|Not recorded|p19||Tatarian|||||||
1078|Baralaba Coal Measures|44242|14|Not recorded|p14|||||||||
1078|Baralaba Coal Measures|44243|14|Not recorded|p648-650||Late Permian|||||||
1078|Baralaba Coal Measures|44337|5|Briefly described|Map Legend||Late Permian|Lithology.||||||
1078|Baralaba Coal Measures|44381|14|Not recorded|p6,9|||||||||
1078|Baralaba Coal Measures|44426|14|Not recorded|p11||Late Permian|Prolific plant remains.||||||
1078|Baralaba Coal Measures|44578|14|Not recorded|p8||Late Permian|||||||
1078|Baralaba Coal Measures|44629|14|Not recorded|p560|||Cracow area. No age given.||||||
1078|Baralaba Coal Measures|44630|14|Not recorded|p493,494||Late Permian|||||||
1078|Baralaba Coal Measures|44631|14|Not recorded|p205||Late Permian|||||||
1078|Baralaba Coal Measures|44639|14|Not recorded|p56,65|||||||||
1078|Baralaba Coal Measures|44640|14|Not recorded|p30|||||||||
1078|Baralaba Coal Measures|44720|14|Not recorded|p388|||||||||
1078|Baralaba Coal Measures|44721|14|Not recorded|p28-36||Early Permian|||||||
1078|Baralaba Coal Measures|44814|14|Not recorded|p483|||||||||
1078|Baralaba Coal Measures|45031|14|Not recorded|p9||Permian|||||||
1078|Baralaba Coal Measures|45071|3|Fully described|Table 12|||||||||
1078|Baralaba Coal Measures|45095|6|Mentioned|p9|||||||||
1078|Baralaba Coal Measures|46949|6|Mentioned|Fig.3|||||||||
1078|Baralaba Coal Measures|48600|14|Not recorded|p9|||||||||
1078|Baralaba Coal Measures|48900|6|Mentioned|p84|||Table opposite.||||||
1078|Baralaba Coal Measures|48919|4|Described|p28|||See also p29.||||||25-AUG-08
1078|Baralaba Coal Measures|48947|5|Briefly described|p8|||||||||
1078|Baralaba Coal Measures|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Feldspathic and lithic sandstone, siltstone, mudstone, coal, conglomerate and tuff.||||||18-JUN-09
1078|Baralaba Coal Measures|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Blackwater Group. Feldspathic and lithic sandstone, siltstone, mudstone, coal, conglomerate and tuff.  Contains the Kaloola Member.||||||
1078|Baralaba Coal Measures|60115|5|Briefly described|p20, p21 Fig. 1|Late Permian|Early Permian|Geological Province: Bowen Basin. Contains thickly developed coal seams up to 6m thick. Primary target for coal seam gas.||||||04-FEB-08
1078|Baralaba Coal Measures|60282|5|Briefly described|p7|||Overlie the Gyranda Formation.||||||
1078|Baralaba Coal Measures|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||13-MAR-09
1078|Baralaba Coal Measures|61617|6|Mentioned|p346 Tb. 3|||Net coal thickness: 19-35m. Geological Province: Bowen Basin.||||||11-FEB-09
1078|Baralaba Coal Measures|61782|6|Mentioned|p281|||||||||
1078|Baralaba Coal Measures|62357|5|Briefly described|p524 Fig. 7, p534|Late Permian|Late Permian|Geological Province: Bowen Basin. ||||||
1078|Baralaba Coal Measures|63713|6|Mentioned|p1523|||||||Equivalent to Bandana Formation.||
1078|Baralaba Coal Measures|64665|5|Briefly described|p52.|Late Permian|Late Permian|Bowen Basin. Low ash coal with good coking properties; high-volatile bituminous to anthracite.||||||
1078|Baralaba Coal Measures|64856|3|Fully described|p41-42, p56, p58, p60-63, p66-68, p102|Late Permian|Late Permian|Reid (1944) who later (1945) amended the name to 'Baralaba-Kianga Coal Measures' before reverting to the original form. Bowen Basin. Datum for the top of the Permian. Conformably overlies Burunga Formation. Transitional with overlying Rewan Group; locally overlain unconformably by Precipice Sandstone. Contains Kaloola Member. Age from palynoflora (APP5 and APP6). 556m thick. Sand-, silt-, mudstones; coal and tuff.| | ||||28-NOV-17
1078|Baralaba Coal Measures|64857|4|Described|p121-124, 134, p113 Fig.3|Late Permian|Late Permian|Bowen Basin. Coaly formation overlying the Wiseman Formation. Stated in article to be Permian, implied to be Late Permian because lies stratigraphically above Flat Top Formation.||||||
1078|Baralaba Coal Measures|64858|5|Briefly described|p182, p180 Fig.2, p186 Fig.11|Late Permian|Late Permian|Bowen Basin. Overlies Burunga Formation? Overlies Wiseman Formation in NE Taroom Trough.||||||30-NOV-09
1078|Baralaba Coal Measures|64859|5|Briefly described|p196, 226|Permian|Permian|Terrestrial coals, mudstones and sandstones. Minor gas source rocks.||||||
1078|Baralaba Coal Measures|65003|5|Briefly described|p2, p6, p27, p31, 32, 33-35||Permian|Of Bowen Basin. ||||Eastern equivalent of the Rangal Coal Measures. Unconformably overlain by the Rewan Formation||
1078|Baralaba Coal Measures|65112|6|Mentioned|p316; Fig 4 p314|Triassic|Late Permian|Part of Supersequence F. Unit in the Taroom Trough.||||Overlies the Burunga Formation, underlies the Rewan Group.||22-MAR-12
1078|Baralaba Coal Measures|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Taroom Trough. Overlies the Burunga Formation. Shown as Baralaba CM.||||||10-NOV-09
1078|Baralaba Coal Measures|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||21-SEP-09
1078|Baralaba Coal Measures|65115|5|Briefly described|p418, 420, Fig 2 p403|Tatarian|Tatarian|Underlies the Rewan Group in the Taroom Trough, Bowen Basin. Deltaic-fluvial coal measures. Part of Supersequence F.||||||
1078|Baralaba Coal Measures|65116|5|Briefly described|p447, Fig 2 P436|Late Permian|Late Permian|Underlies the Rewan Group and overlies the Burunga Formation in the Taroom Trough Bowen Basin.||||||
1078|Baralaba Coal Measures|65118|5|Briefly described|p483, Fig 2 p479|Permian|Permian|Underlies the Rewan Group in the Taroom Trough,Bowen Basin.||||||
1078|Baralaba Coal Measures|65119|6|Mentioned|p526, Fig 6 p512, Fig 14 p521|Late Permian|Late Permian|Unit in Blackwater Group. With Bandanna Formation, is the principal producer of liquid hydrocarbons in the Bowen and Surat Basins. Present in Flinton 1 well||||||07-MAR-12
1078|Baralaba Coal Measures|65388|4|Described|p196-198, p161 Fig. 62, p163, 193, 194|Late Permian|Late Permian|Conformably overlies Wiseman Formation of Gyranda Subgroup, Blackwater Group, Bowen Basin. Includes Kaloola Member. Top is mostly transitional with overlying Rewan Group, but unconformable in places. Palynofloras are identified with unit APP5 passing into APP6 near the top (Price, 1997). No formal type section and rocks crop out poorly. The lower 214m of the unit was intersected by GSQ Mundubbera 5 (Gray and Heywood, 1978), but there is no complete section.||||||
1078|Baralaba Coal Measures|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p6|||Southern Taroom Trough, Bowen Basin.||Of the Rewan Group ?||||
1078|Baralaba Coal Measures|67365|5|Briefly described|p83.|Late Permian|Late Permian|At Dawson Valley, contains up to 10 seams of thick, gassy coals with aggregate thickness of up to 30 m, at depths ranging from 300-1,000 m. Current (2009) CSG production of Dawson Valley operations is c.15 TJ per day. At the Peat gas field near Wandoan, 4 major coal seams with an aggregate thickness of 18.3 m produce (2009) 15 TJ per day. These same 4 seams supply CSG at the Scotia gas field to the north.||||||
1078|Baralaba Coal Measures|67402|5|Briefly described|p21, p45, p52, p57 tbl BWS3|Wuchiapingian|Wuchiapingian|Bowen Basin. Generally greater than 100m thick. See also p165 tbl LPB1, p272, p273.||||Overlain by the Rewan Group. Overlies the Burunga Formation.|Intraformational siltstones, mudstones and tuffs.|
1078|Baralaba Coal Measures|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Rewan Formation. Underlain by Gyranda Formation.||
1078|Baralaba Coal Measures|68139|6|Mentioned|p32|Permian|Permian|Bowen Basin. Group 5 coals. Hosts coal seam gas-producing fields.||||||
1078|Baralaba Coal Measures|68679|5|Briefly described|p353, p377, p381, p383-384|Permian|Permian|Mallett et al. (1983). Connors-Auburn Province. Denison Trough and Roma Shelf, Bowen Basin. 556m thick. Non-marine alluvial plain sediments. Properties of the coal are described in some detail.|||Kaloola Tuff Member.|Overlies Wiseman and Burunga Formations. Is overlain by the Rewan Group.|Fine- to medium-grained feldspatholithic sandstone, siltstone, mudstone, carbonaceous mudstone, siltstone, coal, tuff.|
1078|Baralaba Coal Measures|70330|6|Mentioned|p11 Fig.1|Late Permian|Late Permian|Bowen Basin. Appears as Rangal-Baralaba-Bandana Coal Measures.||||||
1078|Baralaba Coal Measures|70815|6|Mentioned|p3-4, 6-7, 11|||Bowen Basin. Vitrinite reflectance values mapped.||||||
1078|Baralaba Coal Measures|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Bowen Basin.|||Includes Kaloola member.|||
1078|Baralaba Coal Measures|70940|5|Briefly described|p844|Permian|Permian|Burunga Anticline, southern Bowen Basin.|252.5 Ma (Metcalfe et al., 2014).|Blackwater Group.||Overlies Yarrabee Tuff.||
1078|Baralaba Coal Measures|71276|6|Mentioned|p295-296|||||||Overlies Yarrabee Tuff.||
1078|Baralaba Coal Measures|72297|5|Briefly described|p694-695, p703, p744, p750|Permian|Permian|SE Bowen Basin. Numerous coal seams often split and coalesce. Indicative properties tabulated. Petroleum source, from coals. Produces structurally-trapped free CSG on the Burunga Anticline E of Wandoan, at Scotia and Peat.|||||Coal rank ranges from low-volatile bituminous to semianthracite, then decreases southwards through coking range.|
1078|Baralaba Coal Measures|73163|6|Mentioned|p468|||Bowen Basin.||||Overlies the Yarrabee Tuff.||02-FEB-22
1078|Baralaba Coal Measures|73305|6|Mentioned|p548 Fig.1|Late Permian|Late Permian|Bowen Basin. Taroom Trough, northeast.||||||
1078|Baralaba Coal Measures|73450|6|Mentioned|p55|||Bowen Basin.||||||
1078|Baralaba Coal Measures|73625|6|Mentioned|p5 Fig.3, p20-21|Permian|Permian|Eastern Bowen Basin.|||Kaloola Member.|Overlies Flat Top Formation. Is overlain by 'Marker Mudstone'/Rewan Group. Equivalent to Bandanna Formation.||
1090|Bardool Conglomerate|24237|5|Briefly described|p6 Fig.2|Middle Triassic|Middle Triassic|Geological Province: Clarence-Moreton Basin.||||||
1090|Bardool Conglomerate|29869|6|Mentioned|p38|||||||||
1090|Bardool Conglomerate|32801|6|Mentioned|p258|||||||||
1090|Bardool Conglomerate|32803|6|Mentioned|Fig. 1|||||||||
1090|Bardool Conglomerate|34340|2|Defined|p459|Triassic|Triassic|Nymboidea Coal Measures. See also p460.||||||
1090|Bardool Conglomerate|34593|6|Mentioned|p539|||Mesozoic||||||
1090|Bardool Conglomerate|36570|6|Mentioned|p25|||||||||
1090|Bardool Conglomerate|37112|5|Briefly described|Table 1|||||||||
1090|Bardool Conglomerate|43881|14|Not recorded|p2,6-7,12,19-22,||Triassic|49-51,78-80,133,147,157, Map 12. Part of Nymboida Coal Measures.||||||
1090|Bardool Conglomerate|61310|5|Briefly described|Table C1 (p22-23)|Middle Triassic|Middle Triassic|Of the Nymboida Coal Measures. Cobble conglomerate, lithic sandstone, claystone, siltstone. Max. thickness: >1070m. Geological Province: Clarence-Moreton Basin.||||||
1090|Bardool Conglomerate|73306|5|Briefly described|p565-566, 573|Late Triassic|Middle Triassic||c.237 Ma.|Nymboida Coal Measures.|Dalmally Basalt Member.|Overlies Cloughers Creek Conglomerate. Is overlain by Copes Creek Tuff.||
1098|Bargo Claystone|22578|5|Briefly described|p391, Fig.10 p400|||of Illawarra Coal Measures||||||
1098|Bargo Claystone|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Sydney Subgroup||||||
1098|Bargo Claystone|24157|5|Briefly described|p209 Fig.19|||Parent: Illawarra Coal Measures. Geological Province: Sydney Basin||||||
1098|Bargo Claystone|24471|4|Described|p31 Fig.3, p32 Fig.4, p33|Late Permian|Late Permian|Deltaic. Overlies Wilton Formation. Overlain by Darkes Forest Sandstone. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Dempsey Formation. Geological Province: Sydney Basin.||||||07-FEB-11
1098|Bargo Claystone|29900|6|Mentioned|Table 2|||||||||
1098|Bargo Claystone|29901|4|Described|Table 1|||||||||
1098|Bargo Claystone|29942|6|Mentioned|p16|||||||||
1098|Bargo Claystone|29944|6|Mentioned|Fig.18|||||||||
1098|Bargo Claystone|30006|4|Described|p13|||Permian||||||
1098|Bargo Claystone|31887|5|Briefly described|p5|||||||||
1098|Bargo Claystone|33334|6|Mentioned|Table 3|||Perm.||||||
1098|Bargo Claystone|34060|6|Mentioned|p24|||Table. Permian||||||
1098|Bargo Claystone|34569|5|Briefly described|p8|||Permian. Correlation. See Fig.2||||||
1098|Bargo Claystone|36042|6|Mentioned|Fig.20|||||||||
1098|Bargo Claystone|36220|5|Briefly described|p52|||See also Table 1 & P49.||||||
1098|Bargo Claystone|37087|6|Mentioned|p198|||||||||
1098|Bargo Claystone|39232|6|Mentioned|p105|||||||||
1098|Bargo Claystone|39287|6|Mentioned|Fig. 2.15|||||||||
1098|Bargo Claystone|39309|5|Briefly described|p127|||||||||
1098|Bargo Claystone|40166|6|Mentioned|p348|||See also Table 1||||||
1098|Bargo Claystone|40321|6|Mentioned|p19|||||||||
1098|Bargo Claystone|40744|6|Mentioned|Table 1|||||||||
1098|Bargo Claystone|42787|5|Briefly described|p133|||||||||
1098|Bargo Claystone|42896|4|Described|p21|||Of Sydney Subgroup.||||||13-MAR-07
1098|Bargo Claystone|42925|5|Briefly described|Table 18||Late Permian|||||||
1098|Bargo Claystone|43194|5|Briefly described|p129 Tb. 8.3, p130|Late Permian|Late Permian|Of Illawarra Coal Measures, western Sydney Basin. ||||||
1098|Bargo Claystone|45090|6|Mentioned|p189|||Refers Bowman (1970)||||||
1098|Bargo Claystone|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
1098|Bargo Claystone|61612|6|Mentioned|p274, p277, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||13-MAR-09
1098|Bargo Claystone|63832|5|Briefly described|p131 Fig.2|Lopingian|Lopingian|Sydney Basin. Final (P4) Paleozoic glaciation.||Unit in Illawarra Coal Measures.||||13-DEC-17
1098|Bargo Claystone|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Tongarra Coal. Is overlain by Darkes Forest Sandstone.||
1098|Bargo Claystone|67663|6|Mentioned|p520 Tb.1, p520|Permian|Permian|Late Permian.||Of the Illawarra Coal Measures.||||
1098|Bargo Claystone|68003|6|Mentioned|p41.|Late Permian|Late Permian|Sydney Basin. A marine incursion interrupting coal formation.||||||
1098|Bargo Claystone|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
1098|Bargo Claystone|73421|5|Briefly described|p3, p16, p19-20|Wuchiapingian|Wuchiapingian|Sydney Basin, southern. Bargo Tuff in lower part of unit dated to 254.86+/-0.30 Ma by Metcalfe et al., (2015), same age is also shown with the Huntley Claystone p16.|254.86+/-0.30 Ma CA-TIMS|Sydney Subgroup||Overlies Wilton Formation, Tongarra Coal, underlies Darkes Forest Sandstone|Siltstone, sandstone and claystone/shale.|
1098|Bargo Claystone|73625|6|Mentioned|p2|Permian|Permian|Southern coalfield, Sydney Basin.||Illawarra Coal Measures.||Overlies Wilton Formation. Is overlain by Eckersley Formation.||
1137|Barokaville Formation|23053|6|Mentioned|p52|||(Taylor 1976).||||||
1137|Barokaville Formation|24042|5|Briefly described|p511|||||||||
1137|Barokaville Formation|35187|6|Mentioned|p57|||||||||
1137|Barokaville Formation|35372|5|Briefly described|p107|||See also Table 1.||||||
1214|Barrow Range Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Max. thickness: 100m. Geological Province: Kopyje Shelf (Darling Basin).||||||
1214|Barrow Range Member|23171|6|Mentioned|p31|||||||||
1214|Barrow Range Member|23173|6|Mentioned|Map Legend|||||||||
1214|Barrow Range Member|35287|6|Mentioned|p7|||||||||
1214|Barrow Range Member|39618|3|Fully described|p46|||||||||
1214|Barrow Range Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
1214|Barrow Range Member|41528|6|Mentioned|p35|||||||||
1218|Barry Granodiorite|22503|5|Briefly described|Fig.7 p650, p651|Early Devonian|Silurian|||||||
1218|Barry Granodiorite|22679|4|Described|p 47|||||||||
1218|Barry Granodiorite|22798|4|Described|p850,851 Table.1|Early Devonian|Late Silurian|Age: K/Ar 410.2 +/-11.6Ma.||||||
1218|Barry Granodiorite|23100|5|Briefly described|p575 (Fig 1)||Silurian|||||||
1218|Barry Granodiorite|23202|6|Mentioned|Fig.1||Silurian|||||||
1218|Barry Granodiorite|23214|3|Fully described|p172|Late Silurian|Late Silurian|Formerly named Barry Granite and included Sunset Hills Granite. Intrudes the Adaminaby Group, Coombing Formation and Blayney Volcanics.||||||
1218|Barry Granodiorite|34907|6|Mentioned|p294|||||||||
1218|Barry Granodiorite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Hornblende biotite granodiorite.||||||17-JUL-08
1218|Barry Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|||||||
1218|Barry Granodiorite|69539|5|Briefly described|p608 Fig.1, p614|Silurian|Silurian|Dating by K-Ar, 40Ar/39Ar and Rb-Sr on hornblende and biotite consistently produce ages of 416-407 Ma; reflects resetting due to Bowning event.|425.8 +/- 1.9 Ma (U-Pb zircon).|||||
1218|Barry Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
1218|Barry Granodiorite|73431|6|Mentioned|p365, p367 Tb.1, p372|Devonian|Silurian|Lachlan Orogen. Previous ages include 425.8+/-1.9 Ma zircon Pb-evaporation (Lennox et al., 2005), and 408.2+/-11 Ma hornblende K/Ar, 413+/-8 Ma Ar/Ar hornblende, 410.2+/-11.6 Ma K/Ar hornblende (Lennox et al., 1998).|425.8+/-1.9 Ma zircon, 408.2+/-11 Ma K/Ar|||||
1232|Baryulgil Serpentinite|36961|6|Mentioned|p213|||||||||
1232|Baryulgil Serpentinite|38755|6|Mentioned|p65 Fig.1|||Geological Province: Coffs Harbour Block||||||
1232|Baryulgil Serpentinite|38806|6|Mentioned|p76|||||||||
1232|Baryulgil Serpentinite|39673|6|Mentioned|Fig.2|||||||||
1232|Baryulgil Serpentinite|40245|6|Mentioned|p182|||||||||
1232|Baryulgil Serpentinite|40508|6|Mentioned|p62|||||||||
1232|Baryulgil Serpentinite|40514|6|Mentioned|p7|||||||||
1232|Baryulgil Serpentinite|40960|6|Mentioned|p226|||||||||
1232|Baryulgil Serpentinite|42997|6|Mentioned|p42|||||||||
1232|Baryulgil Serpentinite|43745|6|Mentioned|Fig.4,p13|||||||||
1232|Baryulgil Serpentinite|44093|5|Briefly described|p132 Tab. 10.1|Middle Devonian|Late Silurian|Of New England Super-terrane. Geological Province: New England Fold Belt.||||||07-APR-05
1232|Baryulgil Serpentinite|60937|6|Mentioned|p424 Fig. 2|||||||||
1237|Basin Creek Formation|23812|5|Briefly described|p147|||Of Nymboida Coal Measures. Geological Province: Clarence-Moreton Basin.||||||
1237|Basin Creek Formation|24237|5|Briefly described|p6 Fig.2|Middle Triassic|Middle Triassic|Geological Province: Clarence-Moreton Basin.||||||
1237|Basin Creek Formation|29869|6|Mentioned|p37|||||||||
1237|Basin Creek Formation|30784|6|Mentioned|p70|||||||||
1237|Basin Creek Formation|32801|6|Mentioned|p258|||||||||
1237|Basin Creek Formation|32803|6|Mentioned|Fig. 1|||||||||
1237|Basin Creek Formation|34340|4|Described|p462|||Triassic.||||||
1237|Basin Creek Formation|35647|6|Mentioned|p51|||||||||
1237|Basin Creek Formation|37112|6|Mentioned|p298|||||||||
1237|Basin Creek Formation|37755|6|Mentioned|p79|||||||||
1237|Basin Creek Formation|37757|6|Mentioned|p3|||||||||
1237|Basin Creek Formation|38304|6|Mentioned|p83|||||||||
1237|Basin Creek Formation|41059|6|Mentioned|p170|||||||||
1237|Basin Creek Formation|42719|5|Briefly described|p15|||||||||
1237|Basin Creek Formation|43881|14|Not recorded|p6-7,12-16,22-27,|||p50-1,80-5,90-1,99-105,171-2.Incs George's Knob Clm Mbr & Farquhar's Ck Seam.See Basin Ck Felsite||||||
1237|Basin Creek Formation|60991|5|Briefly described|p39, p43, p47-49  |Middle Triassic|Middle Triassic|Leaves assigned to three gymnosperm genera are described.||Nymboida Coal Measures.||||
1237|Basin Creek Formation|60992|6|Mentioned|p1, p9 |Late Triassic|Early Triassic|Detailed analysis of leaf morphology of Dicroidium, and related problems of establishing species boundaries.||Nymboidea Coal Measures.||||
1237|Basin Creek Formation|61310|5|Briefly described|Table C1 (p22-23)|Middle Triassic|Middle Triassic|Of the Nymboida Coal Measures. Includes Georges Knob Conglomerate Member. Lithic sandstone, claystone, siltstone, pebble conglomerate, coal. Geological Province: Clarence-Moreton Basin.||||||
1237|Basin Creek Formation|63117|5|Briefly described|p156, p157|Middle Triassic|Middle Triassic|||||||
1237|Basin Creek Formation|64298|5|Briefly described|p113, p115, p116|Middle Triassic|Middle Triassic|Geological Province: Nymboida Sub-basin.||||||24-JUL-08
1237|Basin Creek Formation|73306|5|Briefly described|p565-566|Middle Triassic|Middle Triassic|||Nymboida Coal Measures.||Overlies Copes Creek Tuff.||
1244|Bathurst Granite|22503|5|Briefly described|p645|||||||||
1244|Bathurst Granite|22545|6|Mentioned|p498,503, Fig.1|||||||||
1244|Bathurst Granite|22679|4|Described|p 52||Carboniferous|||||||
1244|Bathurst Granite|22798|6|Mentioned|Fig.1||Carboniferous|||||||
1244|Bathurst Granite|22857|6|Mentioned|p217, p231|Late Carboniferous||||||||
1244|Bathurst Granite|22859|6|Mentioned|p217|||||||||
1244|Bathurst Granite|22863|6|Mentioned|p231,239|||||||||
1244|Bathurst Granite|23091|5|Briefly described|p636||Late Carboniferous|||||||
1244|Bathurst Granite|23214|3|Fully described|p249|Carboniferous|Carboniferous|Mafic I-type granite. Intrudes the Dunkeld Granite and is intruded by the Tarana Granite. Suggested intrusive age: 325-330Ma from Rb/Sr biotite/bulk rock pairs (Shaw & Flood, 1993)||||||06-DEC-10
1244|Bathurst Granite|23218|5|Briefly described|Diagram p4, Map. p17|Carboniferous|Carboniferous|||||||
1244|Bathurst Granite|24263|6|Mentioned|p1388 Fig.7||Carboniferous|||||||
1244|Bathurst Granite|24266|6|Mentioned|p1479|||Geological Province: Lachlan Fold Belt.||||||
1244|Bathurst Granite|24269|4|Described|p1554|Late Carboniferous|Late Carboniferous|Age: 310 +/- 7Ma (K-Ar) and (Rb-Sr). Geological Province: Lachlan Fold Belt||||||
1244|Bathurst Granite|24424|5|Briefly described|p539 Tb.4|Namurian|Visean|Age: 319-332 Ma. Palaeomagnetic poles given.||||||
1244|Bathurst Granite|29902|6|Mentioned|p6|||||||||
1244|Bathurst Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
1244|Bathurst Granite|30329|6|Mentioned|p30|||On table P30||||||
1244|Bathurst Granite|30734|6|Mentioned|p54|||||||||
1244|Bathurst Granite|31993|6|Mentioned|p680|||||||||
1244|Bathurst Granite|32047|6|Mentioned|p18|||Refers Stevens (1972)||||||
1244|Bathurst Granite|32087|6|Mentioned|p16|||||||||
1244|Bathurst Granite|32088|6|Mentioned|p10|||||||||
1244|Bathurst Granite|32412|6|Mentioned|p92|||||||||
1244|Bathurst Granite|32708|6|Mentioned|Fig.1|||||||||
1244|Bathurst Granite|32999|6|Mentioned|p9|||||||||
1244|Bathurst Granite|33004|6|Mentioned|p112|||||||||
1244|Bathurst Granite|33006|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
1244|Bathurst Granite|33007|5|Briefly described|p12|||History & genesis. See also PP16 & 17||||||
1244|Bathurst Granite|33220|6|Mentioned|Fig.4c|||||||||
1244|Bathurst Granite|33282|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
1244|Bathurst Granite|33285|6|Mentioned|p22|||Late Carb.||||||
1244|Bathurst Granite|33326|6|Mentioned|p444|||||||||
1244|Bathurst Granite|33742|5|Briefly described|p115|||Early - Middle Carb. Sulphide mineralization P132||||||
1244|Bathurst Granite|33948|6|Mentioned|p79|||||||||
1244|Bathurst Granite|34109|6|Mentioned|p151|||||||||
1244|Bathurst Granite|34255|6|Mentioned|p202|||Carb.||||||
1244|Bathurst Granite|34400|6|Mentioned|p8|||||||||
1244|Bathurst Granite|34403|6|Mentioned|p134|||||||||
1244|Bathurst Granite|34404|6|Mentioned|p83|||||||||
1244|Bathurst Granite|34405|6|Mentioned|p104|||||||||
1244|Bathurst Granite|34572|6|Mentioned|p81|||Carboniferous. See also PP86,87,89 etc.||||||
1244|Bathurst Granite|34692|6|Mentioned|p185|||||||||
1244|Bathurst Granite|34706|6|Mentioned|p392|||||||||
1244|Bathurst Granite|35017|6|Mentioned|p231|||||||||
1244|Bathurst Granite|35072|6|Mentioned|p363|||||||||
1244|Bathurst Granite|35128|6|Mentioned|p361|||Appears on figure||||||
1244|Bathurst Granite|35185|6|Mentioned|p240|||||||||
1244|Bathurst Granite|35257|6|Mentioned|p12|||See also Fig.24.||||||
1244|Bathurst Granite|35318|4|Described|p467|||Structural geology||||||
1244|Bathurst Granite|35654|5|Briefly described|p221|||Discussion re folding.||||||
1244|Bathurst Granite|36175|6|Mentioned|p340|||||||||
1244|Bathurst Granite|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
1244|Bathurst Granite|36391|6|Mentioned|p80|||Also P87,88,90,96||||||
1244|Bathurst Granite|36528|6|Mentioned|Fig.6|||||||||
1244|Bathurst Granite|38064|6|Mentioned|p40|||||||||
1244|Bathurst Granite|38216|6|Mentioned|p254|||Carboniferous||||||
1244|Bathurst Granite|38837|6|Mentioned|p230|||||||||
1244|Bathurst Granite|39214|5|Briefly described|p21|||See P23||||||
1244|Bathurst Granite|39331|6|Mentioned|p86|||See also Figs 0-3, 7-1, 7-3||||||
1244|Bathurst Granite|39664|6|Mentioned|Photo 5|||||||||
1244|Bathurst Granite|40328|6|Mentioned|p175|||See also P163||||||
1244|Bathurst Granite|40762|6|Mentioned|Fig.18|||||||||
1244|Bathurst Granite|40766|6|Mentioned|p27|||||||||
1244|Bathurst Granite|41746|6|Mentioned|p451|||See also Fig.2||||||
1244|Bathurst Granite|42384|6|Mentioned|p10|||||||||
1244|Bathurst Granite|42413|6|Mentioned|p49|||||||||
1244|Bathurst Granite|42547|4|Described|p43|||||||||
1244|Bathurst Granite|42712|4|Described|Table 1,p13; p7,16|Carboniferous|Carboniferous|||||||
1244|Bathurst Granite|42726|5|Briefly described|map legend|Carboniferous|Carboniferous|15.  Of the Bathurst Suite (Bathurst Supersuite).||||||07-FEB-05
1244|Bathurst Granite|42842|6|Mentioned|p9|||||||||
1244|Bathurst Granite|43127|5|Briefly described|p4,Fig.2,Fig.3|||Middle Carboniferous||||||
1244|Bathurst Granite|43344|14|Not recorded|p10,138,139,144,149||Carboniferous|See also Lexicon||||||
1244|Bathurst Granite|43383|14|Not recorded|Fig.3|||||||||
1244|Bathurst Granite|43515|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(Provisional Edition) (L-M.Carb)||||||
1244|Bathurst Granite|43516|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(L-M.Carb)||||||
1244|Bathurst Granite|43517|14|Not recorded|not on card|||||||||
1244|Bathurst Granite|43633|6|Mentioned|p17|||||||||
1244|Bathurst Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
1244|Bathurst Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
1244|Bathurst Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
1244|Bathurst Granite|43654|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of Bathurst Batholith. Coarse grained, porphyritic biotite granite.||||||17-JUL-08
1244|Bathurst Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of Bathurst Batholith.||||||17-JUL-08
1244|Bathurst Granite|44244|6|Mentioned|p301|||||||||
1244|Bathurst Granite|45086|6|Mentioned|p55|||See also P56.||||||
1244|Bathurst Granite|46967|6|Mentioned|Fig.4|||||||||
1244|Bathurst Granite|50113|5|Briefly described|p108|Early Carboniferous|Early Carboniferous|Part of the Bathurst Batholith. Geological Province: Lachlan Fold Belt||||||
1244|Bathurst Granite|61762|6|Mentioned|p15 Fig. 1, p17, p18|||||||||
1244|Bathurst Granite|62349|6|Mentioned|p72, p73|||Part of the Bathurst Batholith.  Geological Province: Lachlan Fold Belt.||||||
1244|Bathurst Granite|62368|6|Mentioned|p398 Fig.14|||||||||
1244|Bathurst Granite|63290|6|Mentioned|p391|||||||||
1244|Bathurst Granite|67847|6|Mentioned|p25, p27|||Lachlan Orogen, eastern (Rockley-Gulgong) belt.||||||
1244|Bathurst Granite|68004|6|Mentioned|p21. |Early Carboniferous|Early Carboniferous|||||||
1244|Bathurst Granite|68592|6|Mentioned|p1544|||Mentioned in the context of Carboniferous deformation in the Hill End Trough, north of this unit.||||||
1244|Bathurst Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
1244|Bathurst Granite|72495|6|Mentioned|p235|||Occurs to the south of Orange.||||||
1244|Bathurst Granite|73299|6|Mentioned|p1099|||||||||
1244|Bathurst Granite|73431|6|Mentioned|p363 Fig.1|Carboniferous|Carboniferous|||||||
1282|Bay Formation|22679|6|Mentioned|p 33|||||||||
1282|Bay Formation|22857|4|Described|p470 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Crudine Group. Massive to well bedded quartzofeldspathic arenite, siltstone, tuff. Age: 405 and 408Ma (U/Pb SHRIMP zircon). Max. thickness: 450m. Geological Province: Hill End Trough.||||||
1282|Bay Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||11-JAN-10
1282|Bay Formation|23170|2|Defined|p174|Lochkovian|Lochkovian|of Crudine Group.||||||
1282|Bay Formation|23214|3|Fully described|p194|Lochkovian|Lochkovian|Of Crudine Group. Consists of interbedded fine to coarse sandstone, pebbly sandstone, siltstone, shale, schist, tuff and rare quartz-feldspar porphyry. Max. thickness 1300m.||||||
1282|Bay Formation|29906|6|Mentioned|p12|||||||||
1282|Bay Formation|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
1282|Bay Formation|30099|6|Mentioned|Fig.2|||||||||
1282|Bay Formation|31852|6|Mentioned|p719|||||||||
1282|Bay Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
1282|Bay Formation|32047|6|Mentioned|p17|||||||||
1282|Bay Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Dev.||||||
1282|Bay Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
1282|Bay Formation|33006|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian to Lower Devonian||||||
1282|Bay Formation|33282|6|Mentioned|Map legend|Early Devonian|Late Silurian|U.Sil.-L.Dev.||||||
1282|Bay Formation|33732|5|Briefly described|p116|||||||||
1282|Bay Formation|34059|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
1282|Bay Formation|34403|4|Described|p135|||See also P136.||||||
1282|Bay Formation|34405|6|Mentioned|Fig.3.9|||||||||
1282|Bay Formation|37488|6|Mentioned|p251|||||||||
1282|Bay Formation|37727|6|Mentioned|Fig.1|||||||||
1282|Bay Formation|39331|6|Mentioned|Fig.7-3|||||||||
1282|Bay Formation|43127|5|Briefly described|p4,Fig.2,Fig.3||Early Devonian|||||||
1282|Bay Formation|43476|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Provisional Edition)||||||
1282|Bay Formation|43515|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Provisional Edition)||||||
1282|Bay Formation|43516|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
1282|Bay Formation|43517|14|Not recorded|p150,152,154,160-1|||Map Plate XII||||||
1282|Bay Formation|43525|14|Not recorded|map p124, Tb p127|||||||||
1282|Bay Formation|43639|5|Briefly described|Map Legend||Devonian|||||||
1282|Bay Formation|43653|5|Briefly described|Map Legend||Devonian|||||||
1282|Bay Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
1282|Bay Formation|60424|5|Briefly described|p350 Fig. 1, p351 Fig. 2|Devonian|Devonian|Geological Province: Hill End Trough. Feldspathic sandstone and siltstone||||||
1282|Bay Formation|66197|5|Briefly described|p633 Fig.4b|||Molong High-Hill End Trough. Deep marine volcaniclastics. Underlies the Cunningham Formation, overlies the Barnby Hills Shale.||||||13-MAR-12
1282|Bay Formation|68592|6|Mentioned|p1038|||Northern Hill End Trough.||Unit in Crudine Group.||||
1282|Bay Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
1282|Bay Formation|73299|6|Mentioned|p1102 Fig.8|Early Devonian|Late Silurian|Hill End Trough, western. [Map symbol suggests Devonian age]||||Overlies the Barnby Hills Shale, underlies the Cunningham Formation.||
1282|Bay Formation|73431|6|Mentioned|p363 Fig.1, p365, p367 Tb.1, p368, p372|Devonian|Devonian|Lachlan Orogen. Previous U/Pb (SHRIMP) zircon weighted mean age of 411.3+/-4.9 Ma with 56-715 Ma cores (Atton, 2013).|411.3+/-4.9 Ma zircon U/Pb SHRIMP||||Volcanic unit.|
1288|Bayswater Coal Member|29942|4|Described|Fig.1|||Permian||||||
1288|Bayswater Coal Member|29943|6|Mentioned|p37|||Permian||||||
1288|Bayswater Coal Member|29944|6|Mentioned|Fig.18|||||||||
1288|Bayswater Coal Member|31375|6|Mentioned|p3|||Stratigraphy||||||
1288|Bayswater Coal Member|37087|6|Mentioned|p197|||||||||
1288|Bayswater Coal Member|38614|6|Mentioned|p14|||||||||
1288|Bayswater Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1288|Bayswater Coal Member|39666|6|Mentioned|p84|||||||||
1288|Bayswater Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1288|Bayswater Coal Member|40060|6|Mentioned|p63|||||||||
1288|Bayswater Coal Member|40321|6|Mentioned|p19|||||||||
1288|Bayswater Coal Member|40805|6|Mentioned|Table 1|||||||||
1288|Bayswater Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Burnamwood Formation.||||
1299|Baywulla Formation|30451|4|Described|p28|||Part of Caswell Creek Group||||||
1299|Baywulla Formation|31519|6|Mentioned|p914|||||||||
1299|Baywulla Formation|31586|6|Mentioned|p2|||Refers Maxwell (1960,1961), Jull (1965,1969)||||||
1299|Baywulla Formation|31659|6|Mentioned|p54|||Part of Caswell Creek Group.||||||
1299|Baywulla Formation|31706|6|Mentioned|p651|||L.Carb. correlation chart||||||
1299|Baywulla Formation|32866|6|Mentioned|p30|||||||||
1299|Baywulla Formation|32867|6|Mentioned|p56|||||||||
1299|Baywulla Formation|32868|6|Mentioned|p200|||||||||
1299|Baywulla Formation|33728|6|Mentioned|p52|||||||||
1299|Baywulla Formation|33774|14|Not recorded|p19|||Stratigraphy||||||
1299|Baywulla Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
1299|Baywulla Formation|34155|6|Mentioned|p94|||Lower Carboniferous. Caswell Creek Group.||||||
1299|Baywulla Formation|34287|6|Mentioned|p111|||||||||
1299|Baywulla Formation|36528|6|Mentioned|p173|||||||||
1299|Baywulla Formation|39445|5|Briefly described|Table 6|||||||||
1299|Baywulla Formation|42547|4|Described|p51|||||||||
1299|Baywulla Formation|42583|6|Mentioned|p66|||||||||
1299|Baywulla Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
1299|Baywulla Formation|43983|14|Not recorded|p1-3,9,Figs.1,2|||||||||
1299|Baywulla Formation|44091|14|Not recorded|p37,47,Tb.3||Early Carboniferous|||||||
1299|Baywulla Formation|44360|2|Defined|p1-4,13,15,21-8,30-4|Namurian|Visean|Map. Unit of Caswell Creek Group. (late Visean-?early Namurian)||||||
1299|Baywulla Formation|44369|2|Defined|p168-171|||Limestone, Subgreywacke, conglomerate.||||||
1299|Baywulla Formation|44370|14|Not recorded|Tb.7,p219|||||||||
1299|Baywulla Formation|44372|6|Mentioned|p5-7||Visean|Overlies Tellebang Fromation. Underlies Branch Creek Formation.||||||
1299|Baywulla Formation|44379|14|Not recorded|p15|||Ref. to McKellar 1967.||||||
1299|Baywulla Formation|44486|14|Not recorded|p210,212,215|||Lithostrotion arundineum,Eth.||||||
1299|Baywulla Formation|44487|14|Not recorded|p199|||Cannindah Limestone proposed in lieu of Baywulla Formation in Monto-Old Cannindah area.||||||
1299|Baywulla Formation|44515|2|Defined|p29,30|||Overlies Black Mountain Formation.||||||
1299|Baywulla Formation|44833|14|Not recorded|p119-120|||Early Carboniferous faunal zones.||||||
1299|Baywulla Formation|44874|14|Not recorded|p102|||||||||
1299|Baywulla Formation|45097|6|Mentioned|Fig.|||Carboniferous correlation chart||||||
1299|Baywulla Formation|46803|6|Mentioned|p148|||See also Fig. 4||||||
1299|Baywulla Formation|48926|6|Mentioned|p40|||See also P41 etc.||||||24-FEB-10
1299|Baywulla Formation|48940|6|Mentioned|p101|||||||||
1299|Baywulla Formation|66498|6|Mentioned|p47, 49|||Vertebrate microfauna fossils listed.||||||
1299|Baywulla Formation|68297|5|Briefly described|p197|Visean|Visean|Near Rockhampton.||||||
1299|Baywulla Formation|70050|6|Mentioned|p327, p337, p347|Visean|Visean|Monto area. Contains Cionodendron coral fossils (illustrations and systematic palaeontology).||||||
1304|Beacon Mudstone|30914|6|Mentioned|Map legend|Permian|Devonian|Devonian ? - Permian||||||
1304|Beacon Mudstone|31586|5|Briefly described|p6|||Correlation of Visean coral horizons||||||
1304|Beacon Mudstone|31587|5|Briefly described|p60|||Distribution of Lithostrotion||||||
1304|Beacon Mudstone|31802|6|Mentioned|p137|||Refers Lucas in Hill & Denmead (1960) M. - U.Pal.||||||
1304|Beacon Mudstone|34074|5|Briefly described|p258|||L.Carb.||||||
1304|Beacon Mudstone|34350|6|Mentioned|p17|||Carboniferous||||||
1304|Beacon Mudstone|34556|6|Mentioned|p269|||Lower Carboniferous||||||
1304|Beacon Mudstone|36961|6|Mentioned|Fig.5|||||||||
1304|Beacon Mudstone|37100|6|Mentioned|p259|||||||||
1304|Beacon Mudstone|37508|6|Mentioned|p503|||||||||
1304|Beacon Mudstone|37509|6|Mentioned|p504|||||||||
1304|Beacon Mudstone|40246|6|Mentioned|p164|||||||||
1304|Beacon Mudstone|40435|6|Mentioned|p52|||||||||
1304|Beacon Mudstone|40514|6|Mentioned|p5|||||||||
1304|Beacon Mudstone|42547|5|Briefly described|p41|||||||||
1304|Beacon Mudstone|44091|14|Not recorded|p40||Early Carboniferous|||||||
1304|Beacon Mudstone|44360|14|Not recorded|p33||Early Carboniferous|||||||
1304|Beacon Mudstone|44543|2|Defined|p28,30|||Overlies Thanes Creek Slate.||||||
1304|Beacon Mudstone|44564|2|Defined|p166|||On NSW and QLD cards||||||
1304|Beacon Mudstone|44565|14|Not recorded|p232||Early Carboniferous|On NSW and QLD cards.||||||
1304|Beacon Mudstone|44786|14|Not recorded|p193-202||Early Carboniferous|||||||
1304|Beacon Mudstone|44832|14|Not recorded|p8|||||||||
1304|Beacon Mudstone|45097|6|Mentioned|p23|||Refers Lucas (1959)||||||
1304|Beacon Mudstone|48940|6|Mentioned|Fig.14|||Refers Lucas (1959,1960)||||||
1304|Beacon Mudstone|50536|6|Mentioned|p11.1|||||||||
1321|Beargamil Subgroup|22638|4|Described|p70|||Hervey Group||||||
1321|Beargamil Subgroup|22831|5|Briefly described|Table 24|||||||||
1321|Beargamil Subgroup|22859|6|Mentioned|p213|||||||||
1321|Beargamil Subgroup|23214|6|Mentioned|p226|||Of Hervey Group. Name discontinued. Geological Province: Hervey Basin||||||
1321|Beargamil Subgroup|30071|6|Mentioned|Fig.3|||||||||
1321|Beargamil Subgroup|40328|6|Mentioned|p202|||||||||
1321|Beargamil Subgroup|43441|5|Briefly described|31||Late Devonian|||||||08-JAN-10
1321|Beargamil Subgroup|43507|2|Defined|p123-145,156,165||Late Devonian|Subgp of Hervey Group;Contains Clagger Ss,Kadina Fm,Hunter Silts,Peaks Ss,Bendick Fm&Bogan Gate Ss||||||
1321|Beargamil Subgroup|43510|14|Not recorded|p37,41-2,45-47,49,52|||Constituent formations defined.  p58,60,63,65-6,70,74,77-80||||||
1321|Beargamil Subgroup|43513|14|Not recorded|p71,73|||||||||
1321|Beargamil Subgroup|44192|5|Briefly described|Map Legend|||||||||
1321|Beargamil Subgroup|50231|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Hervey Group.  Includes: Bendick Formation.||||||10-MAY-04
1321|Beargamil Subgroup|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Hervey Group. Contains the Bendick Formation.||||||
1321|Beargamil Subgroup|68298|5|Briefly described|p216||Late Devonian|Of Connolly (1965), central and western NSW sediments. Lithological correlation with Connolly's eastern province (Lambie and Catombal Groups) in which basal equivalents of Beargamil Subgroup are marine.||Hervey Group||Is overlain by Nangar Subgroup.||
1321|Beargamil Subgroup|68592|6|Mentioned|p1698|||Conolly (1965). Obsolete due to problems in correlation.||Unit in Hervey Group.||||
1347|Beckers Formation|22857|5|Briefly described|p536 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Massive to bedded silty tuffite. Max. thickness: 120m.||||||31-MAR-06
1347|Beckers Formation|23540|5|Briefly described|p 420|||Age: 287.1+/-2.4Ma (SHRIMP). Also see p425.||||||
1347|Beckers Formation|32094|6|Mentioned|p383|||||||||
1347|Beckers Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis elongata||||||
1347|Beckers Formation|35284|6|Mentioned|p37|||||||||
1347|Beckers Formation|36042|6|Mentioned|Fig.11|||||||||
1347|Beckers Formation|38217|6|Mentioned|p272|||||||||
1347|Beckers Formation|38837|6|Mentioned|p232|||||||||
1347|Beckers Formation|39262|6|Mentioned|p122|||||||||
1347|Beckers Formation|39288|6|Mentioned|p57|||||||||
1347|Beckers Formation|39304|6|Mentioned|Fig. 19.2|||||||||
1347|Beckers Formation|42000|6|Mentioned|p64|||||||||
1347|Beckers Formation|46849|6|Mentioned|Fig. 8|||||||||
1347|Beckers Formation|60289|5|Briefly described|p2|Early Permian|Early Permian|Of Dalwood Group. Overlies Tamby Creek Formation. Underlies Cranky Corner Sandstone. Geological Province: Cranky Corner Basin.||||||22-FEB-05
1347|Beckers Formation|60290|3|Fully described|p19, 24, 36, 40|Early Permian|Early Permian|Of Dalwood Gp. Unconformably overlies Tamby Creek Fm after a ~13 million year hiatus. Overlain by Cranky Corner Sst. Thick: 130 m. Sst + siltst , conglomerate. Age: c. 287 Ma. Geol Prov: Cranky Corner Basin.||||||07-FEB-11
1347|Beckers Formation|60291|4|Described|p51, 53 Tb.1|Early Permain|Early Permain|Of Dalwood Group. Sandstone, bioturbated carbonaceous mudstone/siltstone with 10 m thick basal conglomerate. Shoreface and shelf environments. Geological Province: Cranky Corner Basin. Petrology descirbed.||||||
1347|Beckers Formation|60292|4|Described|p65, p89 Fig.5|Early Permian|Early Permian|Overlies Tamby Creek Formation. Overlain by Cranky Corner Sandstone. Geological Province: Cranky Corner Basin. Petrography and geochemistry described.||||||
1347|Beckers Formation|60293|5|Briefly described|p108 Fig.1|||Overlies Tamby Creek Formation. Overlain by Cranky Corner Sandstone. Vitrinite reflectance of organic matter described.||||||
1347|Beckers Formation|60294|5|Briefly described|p115, p116 Fig.1|Early Permian|Early Permian|Overlies Tamby Creek Formation. Overlain by Cranky Corner Sandstone. Geological Province: Cranky Corner Basin.||||||
1347|Beckers Formation|60295|4|Described|p127, p133 Fig.9|Sakmarian|Asselian|Of Dalwood Group. Overlies Tamby Creek Formation. Overlain by Cranky Corner Sandstone. Plant microfossils indicate a shallow marine environment. Age: 287 Ma. Geological Province: Cranky Corner Basin.||||||
1347|Beckers Formation|60296|5|Briefly described|p155, p156 Fig.1|Sakmarian|Asselian|Of the Dalwood Group. Correalted with Lochinvar Formation, Wasp Head Formation, Woody Island Formation and Quamby Formation. Geological Province: Cranky Corner Basin.||||||
1347|Beckers Formation|60297|5|Briefly described|p167|Permian|Permian|Of the Dalwood Group. Geological Province: Cranky Corner Basin.||||||
1347|Beckers Formation|60298|5|Briefly described|p179, 180, 188|Sakmarian|Asselian|Age: 287.1+/-2.4 Ma (SHRIMP zircon U-Pb). Fossiliferous siltstones and sandstones. Geological Province: Cranky Corner Basin.||||||17-DEC-07
1347|Beckers Formation|60299|5|Briefly described|p207, 218|||Palaeomagnetism measured.||||||
1347|Beckers Formation|60300|5|Briefly described|p242 Tb.1|Early Permian|Early Permian|Of the Dalowood Group. Overlies Tamby Creek Formation. Overlain by Cranky Corner Sandstone. Includes bioturbated siltstone.||||||
1347|Beckers Formation|63832|5|Briefly described|p131 fig 2|Sakmarian|Asselian|Cranky Corner/Gresford block, Southern New England Fold Belt. Fifth (P1) glaciation.||Unit in Dalwood Group.||||13-DEC-17
1347|Beckers Formation|64631|5|Briefly described|p44 Fig.2.|Sakmarian|Asselian|Southern New England Fold Belt, Cranky Corner/Gresford Block. Some biostratigraphic and radiometric age control.||Unit in Dalwood Group.||Is overlain by Cranky Corner Sandstone.||
1347|Beckers Formation|68493|6|Mentioned|p10 Fig.4|Sakmarian|Asselian|||||Correlative of Lochinvar Formation, of Sydney Basin.||
1347|Beckers Formation|69793|6|Mentioned|p1121 Fig.12|Sakmarian|Sakmarian|Gresford Block, Tamworth Belt.||||||
1347|Beckers Formation|70096|5|Briefly described|p221;Supp1|||Of northern Sydney Basin. SHRIMP U-Pb age of 287+\-2.4 Ma. See also supplementary files in appendix for additional stratigraphic and locality information.||||Overlain by Cranky Corner Sandstone. Underlain by Tamby Creek Formation.||
1347|Beckers Formation|70373|6|Mentioned|p802|Permian|Asselian|Facer & Foster 2003. Glaciogenic succession, Cranky Corner Block.||||Correlated with Alum Rock beds.||28-SEP-16
1347|Beckers Formation|73487|6|Mentioned|p585||||ca 287 Ma, base|||||
1362|Bee Conglomerate Member|22857|4|Described|p436 App. 1, Tb.A1.6|Early Devonian|Early Devonian|Of the Chesney Formation (Nurri Group, Cobar Supergroup). Geological Province: Cobar Basin.||||||
1362|Bee Conglomerate Member|23171|6|Mentioned|p15|||||||||
1362|Bee Conglomerate Member|23173|6|Mentioned|Map Legend|||||||||
1362|Bee Conglomerate Member|35219|6|Mentioned|Fig.2|||||||||
1362|Bee Conglomerate Member|35287|6|Mentioned|p6|||||||||
1362|Bee Conglomerate Member|39618|3|Fully described|p87|||||||||
1362|Bee Conglomerate Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
1362|Bee Conglomerate Member|41138|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
1362|Bee Conglomerate Member|42983|6|Mentioned|Fig.3,p345|||||||||
1362|Bee Conglomerate Member|43032|3|Fully described|p47|||of Chesney Formation||||||
1362|Bee Conglomerate Member|46900|6|Mentioned|p16|||Refers Pogson & Felton(1977), part of Chesney Formation||||||
1362|Bee Conglomerate Member|70941|6|Mentioned|p78 fig 32|Late Silurian|Late Silurian|||Chesney Formation||Overlain by the Chesney Formation.||
1379|Beechwood beds|22736|6|Mentioned|p611 Fig2||Permian|||||||
1379|Beechwood beds|22857|5|Briefly described|p514 App.1 Tb.A1.8, p258|Early Permian|Early Permian|Tens of metres thick.||||||
1379|Beechwood beds|22864|6|Mentioned|p258|||||||||
1379|Beechwood beds|41347|6|Mentioned|p368|||||||||
1379|Beechwood beds|41348|5|Briefly described|Map legend|Permian||Of the Macleay Group.||||||16-DEC-04
1379|Beechwood beds|43755|6|Mentioned|Fig.1,p548||Permian|||||||
1379|Beechwood beds|44093|5|Briefly described|p67 Fig. 6.6|Permian|Permian|See also p232 Appendix 1. Geological Province: New England Fold Belt.||||||
1379|Beechwood beds|61771|6|Mentioned|p116, p118|Permian|Permian|||||||
1379|Beechwood beds|71628|5|Briefly described|p17: 75, 80, 84, 86|||Hastings Block.||Macleay Group.||Is intruded by Juhle Mountain, North Brother and Middle Brother Granodiorites, and South Brother Microgranite.||
1410|Belbora beds|41348|5|Briefly described|Map legend|Carboniferous|Devonian|In the Hastings Block.||||||16-DEC-04
1410|Belbora beds|61766|5|Briefly described|p67|||Informal status (Mayer 1972). Included along with Ghanghat Spilite and Bulliac beds within an undifferentiated unit termed Bundook beds. Authors have upgraded this unit to Belbora Formation. Geological Province: Tamworth Belt.||||||
1417|Belford Formation|22969|5|Briefly described|p 21|||Branxton Formation||||||
1417|Belford Formation|31081|6|Mentioned|p65|||See also P69 & Fig. 2||||||
1417|Belford Formation|32943|6|Mentioned|p87|||See also P105||||||
1417|Belford Formation|33711|6|Mentioned|Table 2|||||||||
1417|Belford Formation|34345|6|Mentioned|p329|||||||||
1417|Belford Formation|35160|6|Mentioned|p2|||||||||
1417|Belford Formation|35284|6|Mentioned|Fig.1|||||||||
1417|Belford Formation|39267|6|Mentioned|p238|||See also P246||||||
1417|Belford Formation|42994|6|Mentioned|p234|||||||||
1417|Belford Formation|43017|5|Briefly described|Fig.1,p372|||||||||
1417|Belford Formation|43385|14|Not recorded|p179||Kungurian|(Early Permian)||||||
1417|Belford Formation|43448|14|Not recorded|p224,225||Permian|Unit of Branxton Subgroup (of Maitland Group)||||||
1417|Belford Formation|43477|14|Not recorded|p15,18,42,43|||||||||
1417|Belford Formation|43479|14|Not recorded|p218||Artinskian|||||||
1417|Belford Formation|45006|14|Not recorded|Tb.1,opp.p3|||||||||
1417|Belford Formation|49644|5|Briefly described|Table|||||||||
1417|Belford Formation|60281|6|Mentioned|p58|||||||||23-MAR-05
1423|Bellbird Creek Formation|22815|4|Described|p100, fig31,32|||Age: Frasnian||||||
1423|Bellbird Creek Formation|22857|4|Described|p216, p494 App. 1 Tb.A1.7|Frasnian|Frasnian|Of the Merrimbula Group. Max. thickness: 375m. Geological Province: Lambie Shelf / Lambie Basin.||||||
1423|Bellbird Creek Formation|22859|5|Briefly described|p216|||||||||
1423|Bellbird Creek Formation|22878|6|Mentioned|p50|||||||||
1423|Bellbird Creek Formation|23309|6|Mentioned|p186|||||||||
1423|Bellbird Creek Formation|23522|5|Briefly described|p260|Early Devonian|Early Devonian|Of Merrimbula Group.||||||
1423|Bellbird Creek Formation|30938|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
1423|Bellbird Creek Formation|32127|3|Fully described|p264|||Refers Steiner (1966)||||||
1423|Bellbird Creek Formation|32129|6|Mentioned|p5|||||||||
1423|Bellbird Creek Formation|32865|6|Mentioned|p483|||Fauna. See also P484||||||
1423|Bellbird Creek Formation|33268|6|Mentioned|Table 1|||||||||
1423|Bellbird Creek Formation|33269|4|Described|p47|||Lithology||||||
1423|Bellbird Creek Formation|33732|5|Briefly described|p113|||||||||
1423|Bellbird Creek Formation|35277|5|Briefly described|p121|||||||||
1423|Bellbird Creek Formation|35526|6|Mentioned|Table 2|||Fossil types and localities||||||
1423|Bellbird Creek Formation|38899|6|Mentioned|p71|||||||||
1423|Bellbird Creek Formation|39313|6|Mentioned|p280|||||||||
1423|Bellbird Creek Formation|40276|6|Mentioned|p27|||||||||
1423|Bellbird Creek Formation|40646|6|Mentioned|p29|||||||||
1423|Bellbird Creek Formation|41385|6|Mentioned|p373|||||||||
1423|Bellbird Creek Formation|41641|5|Briefly described|p191|||||||||
1423|Bellbird Creek Formation|42050|5|Briefly described|p228|||||||||
1423|Bellbird Creek Formation|42158|6|Mentioned|p2|||||||||
1423|Bellbird Creek Formation|42827|5|Briefly described|p191|||of Merimbula Group||||||
1423|Bellbird Creek Formation|42848|4|Described|p532|Late Devonian|Late Devonian|Of Merrimbula Group. Contains the Ettrema Limestone Member. Consists of marine interbedded sandstone and mudstone with rare plant and marine fossils. Overlain by the Conjola Subgroup (Shoalhaven Group). Max. thickness: 1740m. See also p531 Fig. 3.||||||05-SEP-14
1423|Bellbird Creek Formation|43233|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
1423|Bellbird Creek Formation|43461|14|Not recorded|p625|||||||||
1423|Bellbird Creek Formation|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Merrimbula Group (Lambie Shelf). Geological Province: Lambian Transitional Province.||||||
1423|Bellbird Creek Formation|63605|5|Briefly described|p993 Fig.2, p999-1000|Frasnian|Frasnian|Middle unit of Merrimbula Gp.Overlies Twofold Bay Fm.Thickness: 350m. Lower marine transgression deposits (barrier island, littoral + shallow marine) to subaqueous deltaic phase; and upper deltaic tidal flat deposits;+ invertebrate marine fossil assemblage||||||05-SEP-14
1423|Bellbird Creek Formation|66499|5|Briefly described|p61, p62 Fig.6|Frasnian|Frasnian|Deposited during late Frasnian sea level maximum transgression. Includes invertebrate fossils.||Of Merrimbula Group||Stratigraphically above [?overlies] Twofold Bay Formation||
1423|Bellbird Creek Formation|68298|5|Briefly described|p214-215, p232; p234|Frasnian|Frasnian|A marine interval that contains invertebrate fauna, and has fish faunas in both overlying and underlying units.||Merrimbula Group||Is overlain by Worange Point Formation. Overlies Twofold Bay Formation.||
1423|Bellbird Creek Formation|68592|5|Briefly described|p34|Frasnian|Frasnian|||Unit in Merrimbula Group.|Is correlated with Strathaird Formation and Gibbons Creek Sandstone.||Marine clastic sequence.|
1423|Bellbird Creek Formation|70661|3|Fully described|p101, p107 fig 8, p112-p116|Frasnian|Frasnian|Named for the Bellbird Creek on the South coast of NSW. Distribution, geomorphology, geochemistry and fossil assemblage all discussed. Type section mentioned.Maximum thickness of 1740m in Ettrema Creek. Lithology discussed in greater detail (p113-114) . Deposited in a transgressive marine regime with barrier island, littoral, shallow marine and subaqeous deltaic depositional environments represented.||Merrimbula Group|Ettrema Limestone Member.|Faulted against Adaminaby Group, disconformably overlies Yalwal Volcanics, overlies Twofold Bay Formation, unconformably overlain by Shoalhaven Group, intruded by Bundundah Granite|Cross bedded quartzose sandstone, tuffaceous sandstone with minor shale, claystone, siltstone, conglomerate, limestone and rare basalt.|
1423|Bellbird Creek Formation|71303|5|Briefly described|map legend|Frasnian|Frasnian|||Of Merrimbula Group.|Includes Ettrema Limestone Member.||White, red-brown and green-grey, current-bedded, quartzose, fine- to very coarse-grained sandstone, red shale, siltstone and conglomerate. Rare marine microfossils and macroflora. Rare tuffaceous sandstone and intermediate dykes.|
1423|Bellbird Creek Formation|71700|5|Briefly described|CD|||||Merrimbula Group||||
1423|Bellbird Creek Formation|73181|6|Mentioned|p64-65, p67|Frasnian|Frasnian|Includes marine fossils. Contains invertebrate fossils; the brachiopods Cyphoterorhynchus, Productella and Cyrtospirifer.||Merrimbula Group||Underlain by Twofold Bay Formation. Overlain by Worange Point Formation.|Marine.|
1432|Belmont Conglomerate Member|29922|6|Mentioned|p49|||||||||
1432|Belmont Conglomerate Member|29926|6|Mentioned|p2|||||||||
1432|Belmont Conglomerate Member|33867|6|Mentioned|Fig.3|||||||||
1432|Belmont Conglomerate Member|34351|6|Mentioned|p346|||Fig.5.13||||||
1432|Belmont Conglomerate Member|37083|6|Mentioned|p164|||||||||
1432|Belmont Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
1432|Belmont Conglomerate Member|39308|6|Mentioned|p467|||||||||
1432|Belmont Conglomerate Member|39609|6|Mentioned|Table 1|||||||||
1432|Belmont Conglomerate Member|39666|6|Mentioned|Table 20|||||||||
1432|Belmont Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
1432|Belmont Conglomerate Member|43447|14|Not recorded|diag.p.26|||Part of Boolaroo Sub-Group||||||
1432|Belmont Conglomerate Member|45090|6|Mentioned|p186|||Stratigraphic table||||||
1432|Belmont Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Croudace Bay Formation.||||
1435|Belmore Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1435|Belmore Granite|42726|5|Briefly described|map legend|Silurian||||||||
1435|Belmore Granite|60086|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Maragle Bathylith (Batholith?).||||||07-NOV-08
1437|Beloura Tank Limestone Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Contains brachiopods,trilobites, lamellibranchs, cephalopds, corals, etc. Geological Province: Kopyje Shelf (Darling Basin).||||||
1437|Beloura Tank Limestone Member|35287|6|Mentioned|p7|||||||||
1437|Beloura Tank Limestone Member|39618|6|Mentioned|Table 9|||||||||
1437|Beloura Tank Limestone Member|41528|2|Defined|p39|Early Devonian||||||||
1437|Beloura Tank Limestone Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
1437|Beloura Tank Limestone Member|65469|6|Mentioned|p16|||Lachlan Orogen.||||||
1437|Beloura Tank Limestone Member|71039|6|Mentioned|p13|||||||||
1444|Belubula Limestone|5250|6|Mentioned|p42, p43, p45, p48|Mid Caradoc|Early Caradoc|Includes brachiopod faunas. Protected lagoon environment.||||||
1444|Belubula 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.||||
1444|Belubula Limestone|23214|2|Defined|p45|Eastonian|Eastonian|Of Cliefden Caves Limestone Subgroup. Age derived from fossil assembleges. Max. thickness 290m.||||||
1444|Belubula Limestone|23736|6|Mentioned|p19|||||||||
1444|Belubula Limestone|38219|2|Defined|p308|Late Ordovician|Late Ordovician|See also p298.||||||26-AUG-08
1444|Belubula Limestone|41046|6|Mentioned|p144|||||||||
1444|Belubula Limestone|41108|5|Briefly described|p211|||||||||
1444|Belubula Limestone|42479|4|Described|p108, p8|||||||||
1444|Belubula Limestone|42603|5|Briefly described|p60|||||||||
1444|Belubula Limestone|42612|5|Briefly described|Fig.2 P29|||||||||
1444|Belubula Limestone|43569|6|Mentioned|Fig.2,p477||Late Ordovician|||||||
1444|Belubula Limestone|43571|6|Mentioned|p821|||||||||
1444|Belubula Limestone|60989|6|Mentioned|p114|Late Ordovician|Late Ordovician|Cliefden Caves. Shell beds contain trimerellide brachiopods.||||||
1444|Belubula Limestone|63290|6|Mentioned|p400 Fig. 5(c)|||||||||
1444|Belubula Limestone|67322|5|Briefly described|Fig.5, p24|Katian|Katian|Macquarie Arc. Webby and Packham (1982). Contains early Eastonian conodonts.||Unit in Cliefden Caves Limestone Subgroup.||Overlies Fossil Hill Limestone; is overlain by Vandon Limestone.|Massive-bedded limestone.|21-FEB-18
1444|Belubula Limestone|73208|5|Briefly described|p870 Fig.2, 872 Fig.4, p874|Late Ordovician|Late Ordovician|||Cliefden Caves Limestone Subgroup.||Overlies Dunhill Bluff Limestone Member.|Poorly fossiliferous, massive-bedded, mud-rich carbonates derived from cyanobacterial structures.|13-DEC-22
1444|Belubula Limestone|73209|5|Briefly described|p880-881, 883|Late Ordovician|Late Ordovician|The type section is in the Cliefden Caves area.||Cliefden Caves Limestone Subgroup||Overlies Fossil Hill Limestone. Is overlain by Vandon Limestone.|Massively bedded limestone.|
1444|Belubula Limestone|73210|6|Mentioned|p893 Fig.2|||||||||
1445|Belubula Shale|22857|5|Briefly described|p458 App.1, Tb.A1.6|Silurian|Silurian|Of the Cudal Group. Brown, maroon and green shale; arenite. Max. thickness: 435m. Geological Province: Cowra Trough.||||||
1445|Belubula Shale|23214|3|Fully described|p120|Ludlow|Ludlow|Of Cudal Group. Consists of brown, red and grey shale. Unit can be sub-divided into four informal units. Max. thickness 435m.||||||
1445|Belubula Shale|31852|6|Mentioned|p718|||See also Fig. 4. Ludlovian||||||
1445|Belubula Shale|33006|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
1445|Belubula Shale|33282|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
1445|Belubula Shale|34404|6|Mentioned|Fig.3.3b|||||||||
1445|Belubula Shale|34405|6|Mentioned|Fig.3.9|||||||||
1445|Belubula Shale|37727|4|Described|p38|||||||||
1445|Belubula Shale|39655|6|Mentioned|Plate 1|||||||||
1445|Belubula Shale|40328|3|Fully described|p74|||||||||
1445|Belubula Shale|43461|14|Not recorded|p621||Ludlovian|||||||
1445|Belubula Shale|43515|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
1445|Belubula Shale|43516|14|Not recorded|Map Legend||Late Silurian|||||||
1445|Belubula Shale|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of brown, maroon and green shale; sandstone.||||||15-JUL-08
1445|Belubula Shale|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Cudal Group.||||||15-JUL-08
1445|Belubula Shale|63287|5|Briefly described|p317 Fig. 2|Ludlow|Ludlow|Of the Cudal Group. Underlain by Ghost Hill Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
1445|Belubula Shale|67847|5|Briefly described|p33|Late Ludlow|Late Ludlow|Age constrained on the basis of graptolite fossils. ||||||
1445|Belubula Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group||||
1446|Belvedere Formation|22831|6|Mentioned|p 52|||||||||
1446|Belvedere Formation|29986|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
1446|Belvedere Formation|29987|6|Mentioned|Table 3|||||||||
1446|Belvedere Formation|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
1446|Belvedere Formation|32087|6|Mentioned|p18|||||||||
1446|Belvedere Formation|36066|6|Mentioned|p6|||||||||
1446|Belvedere Formation|42449|3|Fully described|p28|||||||||
1446|Belvedere Formation|43441|6|Mentioned|29|||Of Conolly, 1965, then part of Hervey Group||||||08-JAN-10
1446|Belvedere Formation|43500|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
1446|Belvedere Formation|43507|2|Defined|p128,130,161-166||Late Devonian|Basal formation of Cookamidgera Subgroup (Hervey Group)||||||
1446|Belvedere Formation|43510|2|Defined|p41,45,74-77|||||||||
1446|Belvedere Formation|48958|6|Mentioned|Plate 1|||||||||
1448|Bemboka Granodiorite|22815|4|Described|p73|||||||||
1448|Bemboka Granodiorite|40646|5|Briefly described|p39|||||||||
1448|Bemboka Granodiorite|41563|6|Mentioned|p506|||||||||
1448|Bemboka Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
1448|Bemboka Granodiorite|49705|5|Briefly described|p3|||||||||
1451|Ben Boyd Formation|22815|3|Fully described|p101, fig31,32|||This sequence previously included in the Worange Point Formation.||||||
1451|Ben Boyd Formation|22857|5|Briefly described|p217, p494 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Merrimbula Group. A point bar sequence of massive mudstone and arenite. Max. thickness: 850m. Geological Province: Lambie Basin.||||||
1451|Ben Boyd Formation|22859|5|Briefly described|p217|||||||||
1451|Ben Boyd Formation|23309|6|Mentioned|p186,187|||of Merrimbula Group.||||||
1451|Ben Boyd Formation|42158|6|Mentioned|p2|||Reserved as Ben Boyd||||||
1451|Ben Boyd Formation|42848|6|Mentioned|p532|||||||||
1451|Ben Boyd Formation|43233|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
1451|Ben Boyd Formation|71700|5|Briefly described|CD|||||Merrimbula Group||||
1451|Ben Boyd Formation|73181|6|Mentioned|p64|||[Written as 'Ben Boyd' Formation].||Merrimbula Group||Underlain by Worange Point Formation.||
1466|Bendethera Limestone Member|22857|5|Briefly described|p480 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the De Drack Formation.||||||
1466|Bendethera Limestone Member|39028|6|Mentioned|Map legend|Ludlovian|Ludlovian|||||||
1466|Bendethera Limestone Member|40276|2|Defined|p4|Late Silurian|Late Silurian|||||||
1466|Bendethera Limestone Member|68592|5|Briefly described|p760|||Defined on Araluen 1:100 000; Wyborn and Owen (1986).||Unit in De Drack Formation.|||Limestone.|
1466|Bendethera Limestone Member|71069|6|Mentioned|p146|||||De Drack Formation||||
1468|Bendick Formation|22638|3|Fully described|p70|||Of the Beargamil Subgroup.Thickness:  90 m.||||||25-JUN-08
1468|Bendick Formation|22857|5|Briefly described|p490 App.1 Tb.A1.7|Devonian|Devonian|Of the Hervey Group. Max. thickness: 350m. Geological Province: Hervey Basin.||||||
1468|Bendick Formation|35070|3|Fully described|p125|||||||||
1468|Bendick Formation|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1468|Bendick Formation|35608|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
1468|Bendick Formation|43507|2|Defined|p126,128,135|||Formation of Upper Devonian Beargamil Subgroup||||||
1468|Bendick Formation|43510|2|Defined|p41,42,63-65|||||||||
1468|Bendick Formation|44192|5|Briefly described|Map Legend||Frasnian|||||||
1468|Bendick Formation|44936|5|Briefly described|Map Legend||Late Devonian|Of Hervey Group.||||||
1468|Bendick Formation|50231|5|Briefly described|Map Legend|Frasnian|Frasnian|Of the Beargamil Subgroup (Hervey Group).  Underlies: Mandagery Formation.||||||13-MAY-04
1468|Bendick Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Beargamil Subgroup (Hervey Group). Red, partly planar/ripple x-lam.siltst.+ fine-gr.sst, tog. with subordinate med. to thick bedded, poorly sorted, massive polymictic conglom.+ pebbly coarse-gr. lithic-qtz. to qtz-lithic sst; vein qtz pebbles+minor vol||||||
1468|Bendick Formation|68592|4|Described|p1698-9, p1704-7|Frasnian|Frasnian|Conolly (1965), after Bendick Trigonometrical Station. Type section described. 30-80m thick. Geochemistry unknown; geophysical properties briefly described. Fossils are poorly preserved fish plates and worm burrows. Is correlated with Boulton Formation and lower part of Peaks Formation.||Basal unit in Hervey Group.||Overlies Young Granodiorite nonconformably and Hawkins Volcanics unconformably. Is overlain conformably by Mandagery Formation. Is faulted against Mountain Creek Volcanics and Crowther Monzodiorite.|Red siltstone and fine-grained sandstone; pebbly, coarse-grained lithic-quartz to quartz-lithic sandstone; subordinate red to fawn, granule to pebble, polymictic conglomerate.|
1468|Bendick Formation|70192|5|Briefly described|Map Legend|Frasnian|Frasnian|Dhe. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hervey Group||Unconformable at base. Is overlain by Mandagery Formation.|Partly planar and ripple cross laminated siltstone and fine grained sandstone; subordinate medium-thickly bedded, poorly sorted, massive polymictic conglomerate and pebbly coarse grained lithic-quartz to quartz-lithic sandstone.|
1468|Bendick Formation|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Hervey Group|||Partly planar and ripple cross laminated siltstone and fine grained sandstone; subordinate medium-thickly bedded, poorly sorted, massive polymictic conglomerate and pebbly coarse grained lithic-quartz to quartz-lithic sandstone.|
1468|Bendick Formation|71656|6|Mentioned|p12 Fig.2|Frasnian|Frasnian|Shown only in correlation chart (Fig.2).||Base of Hervey Group||Underlies Mandagery Formation.||
1474|Bendoc Group|5258|6|Mentioned|164|||Includes Sunlight Creek Formation at base.||||||22-JAN-10
1474|Bendoc Group|22530|6|Mentioned|p695||Late Ordovician|||||||
1474|Bendoc Group|22545|6|Mentioned|p504|||||||||
1474|Bendoc Group|22577|6|Mentioned|p120,122||Ordovician|||||||
1474|Bendoc Group|22624|5|Briefly described|p678, Fig.3 p679|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|22628|6|Mentioned|p115,p118|||||||||
1474|Bendoc Group|22704|6|Mentioned|p49||Late Ordovician|||||||
1474|Bendoc Group|22708|5|Briefly described|p210|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|22815|4|Described|p24,122, fig10|Ordovician|Ordovician|||||||
1474|Bendoc Group|22832|4|Described|Fig.1b p634|Late Ordovician|Late Ordovician|See also p637.||||||
1474|Bendoc Group|22857|5|Briefly described|p134, p420 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Pelagic/hemipelagic black slates and mudstones and pelagic cherts.||||||
1474|Bendoc Group|22876|5|Briefly described|p15|Ordovician|Ordovician|500-440Ma||||||
1474|Bendoc Group|22877|5|Briefly described|map|Silurian|Silurian|||||||
1474|Bendoc Group|22878|5|Briefly described|p29|Ordovician|Ordovician|||||||
1474|Bendoc Group|22879|5|Briefly described|map|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|22880|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Warbisco Shale||||||01-OCT-04
1474|Bendoc Group|22881|5|Briefly described|Map legend|Ordovician|Ordovician|||||||06-OCT-04
1474|Bendoc Group|22968|4|Described|P19, P30, P103|Late Ordovician|Ordovician|Graptolite fauna ranges from late Darriwilian to Bolindian, underlying unit is Adaminaby Group||||||
1474|Bendoc Group|22971|4|Described|p 17|Late Ordovician|Ordovician|Included in the "Hotham beds" in WANGARATTA region. Geological Province:  Lachlan Fold Belt.||||||19-JAN-06
1474|Bendoc Group|23020|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|23021|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|23028|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Underlying unit is Adaminaby Group.||||||01-SEP-08
1474|Bendoc Group|23029|5|Briefly described|Map legend|Ordovician|Ordovician|Underlying unit is the Adaminaby Group||||||
1474|Bendoc Group|23030|5|Briefly described|Map legend|Ordovician|Ordovician|Overlying unit is the Yalmy Group||||||
1474|Bendoc Group|23214|5|Briefly described|p3|Ordovician|Ordovician|||||||
1474|Bendoc Group|23245|5|Briefly described|p134||Late Ordovician|||||||
1474|Bendoc Group|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
1474|Bendoc Group|23454|5|Briefly described|p28|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|23615|3|Fully described|p67, 19|Late Ordovician|Late Ordovician|Includes Blueys Creek Formation, Sunlight Creek Formation, Warbisco Shale and Akuna Mudstone. Age within the 'deep marine Ordovician sedimentation' period: 500-438Ma.  Geological Province: Lachlan Fold Belt.||||||16-AUG-18
1474|Bendoc Group|23850|5|Briefly described|p793|||Overlies the Pinnak Sandstone.||||||26-APR-06
1474|Bendoc Group|23860|5|Briefly described|p944|||Underlying unit Adaminaby Group.||||||
1474|Bendoc Group|23938|5|Briefly described|p11, p31-32 Fig. 12.|Late Ordovician|Late Ordovician|Consists of mainly deep marine siltstone and black shale. See also p139 Tb. 1 Appendix.||||||25-SEP-08
1474|Bendoc Group|24002|5|Briefly described|p228 Fig.2|Ordovician|Ordovician|||||||
1474|Bendoc Group|24004|5|Briefly described|p278|Ordovician|Ordovician|||||||
1474|Bendoc Group|24037|6|Mentioned|p423|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24098|5|Briefly described|p27 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24133|4|Described|p37|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24146|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|24177|5|Briefly described|p48|Ordovician|Ordovician|||||||
1474|Bendoc Group|24215|5|Briefly described|p806|||Geological Province:  Lachlan Fold Belt||||||
1474|Bendoc Group|24317|5|Briefly described|p14, p15 Fig.1|Late Ordovician|Late Ordovician|Overlain by Mundoonen Sandstone.||||||
1474|Bendoc Group|24339|6|Mentioned|p46 Fig. 3|||Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24551|3|Fully described|p105, 7, 606, 230, 118 Fig. 5.1|Silurian|Darriwilian |Includes the Sunlight Creek Formation, Warbisco Shale, New Country Sandstone and Akuna Mudstone.||||||
1474|Bendoc Group|24575|5|Briefly described|p711, p716 Tb. 1|Late Ordovician|Middle Ordovician|Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24576|6|Mentioned|p727|||Geological Province: Lachlan Fold Belt||||||
1474|Bendoc Group|24600|5|Briefly described|p481|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|42294|5|Briefly described|p24|||Reserved in 1985.||||||
1474|Bendoc Group|42647|4|Described|p19|||Reserved for use in NSW.||||||
1474|Bendoc Group|43206|5|Briefly described|map legend|Llandovery|Gisbornian|||||||
1474|Bendoc Group|43228|5|Briefly described|p9||Late Ordovician|||||||
1474|Bendoc Group|43233|5|Briefly described|Map Legend|Llandovery|Gisbornian|||||||
1474|Bendoc Group|43312|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||
1474|Bendoc Group|43313|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||
1474|Bendoc Group|43314|5|Briefly described|Map Legend|Bolindian|Gisbornian|||||||
1474|Bendoc Group|43315|5|Briefly described|Map Legend|Bolindian|Gisbornian|Includes Sunlight Creek Formation, Warbisco Shale and Akuna Mudstone.||||||03-MAY-05
1474|Bendoc Group|44093|5|Briefly described|p190 App. 1|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
1474|Bendoc Group|44184|5|Briefly described|Map Legend||Late Ordovician|||||||
1474|Bendoc Group|44185|5|Briefly described|Map legend.|Late Ordovician|Late Ordovician||||||Marine: black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone.|
1474|Bendoc Group|50230|5|Briefly described|Map legend|Bolindian|Gisbornian|Includes the Warbisco Shale.  Overlies the Adaminaby Group; overlain by Mundoonen Sandstone.||||||10-MAY-04
1474|Bendoc Group|50231|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Includes: Warbisco Shale.  Overlies: Adaminaby Group.||||||
1474|Bendoc Group|50232|5|Briefly described|Map legend|Eastonian|Gisbornian|Overlies the Adaminaby Group.  Includes the Warbisco Shale and Malay Creek Formation.||||||
1474|Bendoc Group|50233|5|Briefly described|Map Lagend|Bolindian|Gisbornian|Overlies the Adaminably Group||||||
1474|Bendoc Group|50234|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes: Dignams Siltstone, Warbisco Shale, Bumballa Formation.  Overlies Adaminaby Group; underlies the Poidevins Sandstone.||||||13-MAY-04
1474|Bendoc Group|60503|5|Briefly described|p84, p45 Tb. 2|Late Ordovician|Late Ordovician|Comprises Blueys Creek, Sunlight Creek, Warbisco, New Country and Akuna Formations, of which the second,third and fourth units are present in BENAMBRA. Characterised by deep marine shales, mudstones and chert. Overlies the Adaminaby Group. See also p48.||||||05-SEP-05
1474|Bendoc Group|60504|5|Briefly described|Map Legend|Bolindian|Darriwilian|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone||||||
1474|Bendoc Group|60505|5|Briefly described|Map legend|Bolindian|Darriwilian|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone.||||||
1474|Bendoc Group|60506|5|Briefly described|Map legend|Bolindian|Darriwilian|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone||||||
1474|Bendoc Group|60507|5|Briefly described|Map Legend|Late Ordovician|Early Ordovician|Includes: Sunlight Creek Formation, Warbisco Shale, New Country Sandstone.||||||06-OCT-04
1474|Bendoc Group|60508|5|Briefly described|Map legend|Ordovician|Ordovician|Black shale, sandstone: nonmagnetic except where altered (0-20 nT); very low total count, K, Th, elsewhere similar to Pinnak Sandstone.||||||
1474|Bendoc Group|60536|6|Mentioned|p552|Silurian||||||||
1474|Bendoc Group|60541|4|Described|p12, p51, p19 Tb.1|Llandovery|Late Ordovician|Comprises Sunlight Cr. and Blueys Creek Fms, Warbisco Shale and Akuna Mudstone. Accumulated deep anoxic seafloor shales, mudstones and cherts interbedded with occasional thin bedded quartz-rich sandstones. Age: 500-438Ma. Geol.Prov: Lachlan Fold Belt.||||||12-JAN-06
1474|Bendoc Group|60542|4|Described|p45-46, p12|Llandovery (Early Sil)|Late Ordovician|Characterised by black shales, black and dark grey mudstones and cherts with rare pale coloured sandstones. Comprises: Blueys Creek and Sunlight Creek Formations, Warbisco Shale and Akuna Mudstone.||||||
1474|Bendoc Group|60902|5|Briefly described|p870|Late Ordovician|Late Ordovician|Black shales. Overlies Adaminaby Group and Wagga Group.||||||11-APR-06
1474|Bendoc Group|61160|3|Fully described|p12, p48, p17 Fig. 3.5|Late Ordovician|Late Ordovician|In eastern Victoria, comprises: Sunlight Creek Fm., Warbisco Shale, New Country Sst. and Akuna Mudstone (divisions that could not be achieved in BOGONG due to structural complexity). Conformable on Pinnak Sst., and in places, faulted against it.||||||
1474|Bendoc Group|61161|5|Briefly described|p82, p6, p78 p76-77 Fig 6.1|Late Ordovician|Middle Ordovician|Includes Warbisco Shale, Sunlight Creek Formation, Akuna Mudstone and New Country Sandstone. Nonmagnetic. Deep marine: graphitic mudstone; thin bedded quartz wacke. Faulted against Adaminaby and Cobbannah Groups; overlies Pinnak Sandstone. GSV mapcode: Ob||||||
1474|Bendoc Group|61163|3|Fully described|p79, p10 Fig. 31|Late Ordovician|Late Ordovician|Includes Sunlight Creek Fm, Warbisco Shale, New Country Sandstone, Akuna Mudstone. Marine sedimentary rocks. Overlies Adaminaby Group. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). See also p14 Fig. 3.2, p38 Tb. 6.2.||||||
1474|Bendoc Group|61164|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||
1474|Bendoc Group|61165|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||
1474|Bendoc Group|61166|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||
1474|Bendoc Group|61167|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone, siltstone and sandstone: laminated and siliceous black mudstone and siltstone; thin bedded buff quartzose sandstone and dark grey siltstone; deep marine. GSV map code: Ob.||||||07-FEB-11
1474|Bendoc Group|61168|5|Briefly described|map legend|Late Ordivician|Late Ordivician|Mudstone and sandstone: nonmagnetic (<5 nT, kv = 0-15 x10^-6 cgs); no mapped gravity response; low total radioelement, K and Th, moderate U. GSV map code: Ob.||||||
1474|Bendoc Group|61169|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61170|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||07-FEB-11
1474|Bendoc Group|61171|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61172|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61173|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Warbisco Shale. Sandstone, siltstone, mudstone, black shale, chert; insufficient gravity data to determine response; nonmagnetic (k up to 5 x10^-6 cgs); varying moderate K, Th, U and total radioelements. GSV map code: Ob.||||||
1474|Bendoc Group|61174|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||07-FEB-11
1474|Bendoc Group|61175|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61176|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61177|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone. Deep-marine hemipelagic and turbidite deposits. GSV map code: Ob.||||||
1474|Bendoc Group|61178|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Includes Akuna Mudstone, New Country Sandstone, Warbisco Shale and Sunlight Creek Formation. Siltstone, minor black shale: nonmagnetic; moderate to high gravity; low to moderate total radioelement. GSV map code: Ob.||||||
1474|Bendoc Group|61187|5|Briefly described|p4, p5 Fig.3, p26 Fig.2, p29 Fig.4. |Late Ordovician|Late Ordovician|Benambra Terrane, Eastern Victoria. Correlative of Warbisco Shale, and Mount Easton Shale in the Melbourne Zone, Melbourne Terrane.|||||Mainly siltstone and black shale.|
1474|Bendoc Group|61196|5|Briefly described|p17|Ordovician|Ordovician|Graphitic mudstone and thin-bedded quartz wackes included. Conformably overlies the Pinnak Sandstone. Age is Late Ordovician.||||||25-JAN-06
1474|Bendoc Group|61762|6|Mentioned|p18, p19 Fig. 2(a)|Ordovician|Ordovician|||||||
1474|Bendoc Group|61964|3|Fully described|p14 Fig. 4, p30|Bolindian|Gisbornian|Includes Willandra Sst+Currawalla Shale. Incorporates black-shale dominated component of former Tallebung Gp. Black shale-dominated successions.Overlies Wagga Gp; overlain by Cobar Supergp + Boothumble Fm. Intruded byYalgogrin, Kikoira+Ungarie Granites||||||
1474|Bendoc Group|62070|5|Briefly described|p34 Fig.1, p38|Late Ordovician|Darriwilian|Age: late Darriwilian to latest Ordovician.||||Overlies the Adaminaby Group.|Black shale overlain by siltstone.|
1474|Bendoc Group|62405|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Currawalla Shale and Willandra Sandstone. Interbedded quartz sandstone, siltstone, black carbonaceous mudstone and minor quartz pebble conglomerate.||||||10-APR-08
1474|Bendoc Group|63285|6|Mentioned|p275 Fig. 2|||Geological Province: Molong Volcanic Belt. Consists of quartz-rich sandstone, siltstone, minor siliceous siltstone and rare black mudstone.||||||
1474|Bendoc Group|63286|6|Mentioned|p294 Fig. 1|||Consists of quartz-rich sandstone, siltstone and chert.||||||07-FEB-11
1474|Bendoc Group|63289|5|Briefly described|p363, p369, p380|Bolindian|Gisbornian|Conformably overlain by Triangle Formation. Consists of black shale and siltstone.||||||07-FEB-11
1474|Bendoc Group|63290|4|Described|p385, p388, p396 Fig. 3|Early Silurian|Late Ordovician|Includes Acton Shale, Sunlight Creek Formation, Waribisco Shale, Akuna Formation, Gungoandra Siltstone. Underlain by Girlambone Group, Wagga Group and Adaminaby Group.||||||18-SEP-08
1474|Bendoc Group|63635|5|Briefly described|p39|Darriwilian||Overlies Pinnak Sandstone. Correlation between mainland Australia and Tasmania discussed.||||||
1474|Bendoc Group|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Warbisco Shale, Bumballa Formation and Dignams Siltstone.||||||28-MAY-08
1474|Bendoc Group|64295|5|Briefly described|p198 Fig. 1, p199|Late Ordovician|Late Ordovician|||||||
1474|Bendoc Group|64568|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Currawalla Shale and Willandra Sandstone. Unnamed section is of interbedded quartz sandstone, siltstone, black carbonaceous mudstone and minor quartz-pebble conglomerate.||||||24-SEP-08
1474|Bendoc Group|65469|5|Briefly described|p18, p20|Late Ordovician|Late Ordovician|Lachlan Orogen. Replaces rocks previously mapped as Tallebung Group east of Nymagee. ||||Overlies the Wagga Group.|Black shales and local sandstones.|
1474|Bendoc Group|66713|5|Briefly described|p3|Late Ordovician|Late Ordovician|Black shale units with thin bedded mudstones and rare turbidites. Overlies the Adaminaby Group.||||||
1474|Bendoc Group|67322|4|Described|p4 Fig.2, p5, p13, p16, p28, p20 Fig.5|Late Ordovician|Middle Ordovician|Albury-Bega Terrane. Age determined from  p20 Fig.5 (Strat. column). This is supported due to the presence of graptolites of Upper Ordovician age. Occurs in the Cooma-Mallacoota, Canberra-Queanbeyan, and Goulburn regions.|||Warbisco Shale, Currawalla Shale, Acton Shale, Sunlight Creek Formation, Akuna Mudstone, Willandra Sandstone.|Conformably overlies the Adaminaby and Wagga Groups. Overlies the Chakola and Bumballa Formations. Overlain by the Margules Group.|Graptolitic black shales with relatively minor sandstone.|
1474|Bendoc Group|67802|5|Briefly described|p28|Late Ordovician|Late Ordovician|In fault zones throughout Benambra Terrane in Victoria. Useful dating stratum due to abundant graptolites.||||Is conformable with underlying Adaminaby Group, but usually occurs in faulted contact.|Black shale, sandstone, mudstone, sometimes bioturbated. The change from quartz-turbidite to black shale correlated to relative rise of sea level.|03-OCT-14
1474|Bendoc Group|67847|6|Mentioned|p83|||May be associated with the Cobram mineralisation. ||||||
1474|Bendoc Group|68116|5|Briefly described|Appx, Maps 18-20, 26-27, 34-36, 44-45.|Hirnantian|Darriwilian|Minimum age written as Bolindian in text.|||||Black shale, cherty shale, stripy thin-bedded sandstone and siltstone, laminated siltstone.|06-SEP-16
1474|Bendoc Group|68466|6|Mentioned|p70|Late Ordovician|Late Ordovician|||||Overlies Adaminaby Group.|Includes black shales containing prolific graptolites.|
1474|Bendoc Group|68592|3|Fully described|p316, p320-43, p348, p350, p354, p358|Late Ordovician|Late Ordovician|See also xxiv, p71, p73 Tb.5, p116-8, p230, p269, p272, p275 Fig.57, p277-8, p280, p282, p287, p291-3, p298, p302, p310, p362, p364, p366-7, p376, p384, p419, p421, p426, p731, p742-3, p753, p750, p753, p756, p758, p771, p793, p813, p819. Glen et al. (1990), VandenBerg et al. (1992). Named after Bendoc region of East Gippsland, Vic. Includes black shales formerly attributed to Abercrombie Beds (Packham, 1968), Adaminaby Group (Raymond et al. 1998) and Bubalahla Formation (Scheibner, 1973). c.450m thick. Near-complete reference section in Mountain Creek, NE Victoria; reference sections in NSW described. Quarried (eg Carrick Hill) for road materials. Covan Creek Formation sandstone composition suggests derivation predominantly from deformed and uplifted Adaminaby Group quartzose turbidites and chert, and Bendoc Group black shale. Frogmore, Wyangala, Peelwood, Goulburn and Bungonia structural zones: deformation described. Is intruded by Lockyersleigh Granite.|||Includes Warbisco Shale and (in NSW) Bumballa Formation and (in Vic) Sunlight Creek Formation, New Country Sandstone and Akuna Mudstone.|Conformably overlies Abercrombie Formation. Is overlain conformably by Margules Group and unconformably by Shivering Conglomerate, Cobra, Argyle and Strathaird Formations.|Siliceous black shale, generally with turbiditic sandstone, blackshale and siltstone at the base.|
1474|Bendoc Group|68822|5|Briefly described|p351|Upper Ordovician|Upper Ordovician|Graptolite ages range from Gisbornian 1 to Bolindian 3 (VanderBerg and Cooper 1992; Percival et al. 2011).||||Underlain by the Adaminaby Group and Girilambone Group.|Black shale sequence.|
1474|Bendoc Group|69002|6|Mentioned|p13|||Contains Late Ordovician black shales.||||Underlain by the Wagga Group and the Adaminaby Group.||
1474|Bendoc Group|69159|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Warbisco Shale and Bumballa Formation.|||
1474|Bendoc Group|69160|5|Briefly described|Map legend|Ordovician|Ordovician||||Includes Currawalla Shale and Willandra Sandstone.||Interbedded quartz sandstone, siltstone, black carbonaceous mudstone and minor quartz pebble conglomerate.|
1474|Bendoc Group|69540|5|Briefly described|p640||||||Includes Currawalla Shale.||Black shale. Contains intercalated sequences of quartz-rich turbidites up to 200m thick.|
1474|Bendoc Group|69541|5|Briefly described|p652-653|Late Ordovician|Late Ordovician|||||Overlies Adaminaby and Wagga Groups.|Black to buff coloured shale, siltstone +/- sandstone.|
1474|Bendoc Group|69564|6|Mentioned|p3||||||||Black shale.|
1474|Bendoc Group|69635|6|Mentioned|p148|Ordovician|Ordovician|||||||
1474|Bendoc Group|69668|5|Briefly described|p927|Late Ordovician|Late Ordovician||||||Includes black shales.|
1474|Bendoc Group|70026|5|Briefly described|p40|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen. |||||Black shale.|
1474|Bendoc Group|70178|6|Mentioned|p3|Ordovician|Ordovician||||||Siliciclastic turbidites.|
1474|Bendoc Group|70192|5|Briefly described|Map Legend|Bolindian|Gisbornian|[Theta]b. Undifferentiated member composed of siliceous shale with interbedded, thinly bedded, ripple cross-laminated and thick bedded quartzose sandstone and siltstone. On Boorowa, Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Bumballa Formation, Warbisco Shale and one undifferentiated unit.|Overlies Adaminaby Group. Is overlain by Margules Group.||
1474|Bendoc Group|70297|4|Described|map legend, on side 2 of map sheet|Early Ordovician|Early Ordovician|Max age: Gisbornian? Min age: Bolindian? Small slivers of siliceous black shale and variably developed quartzose sandstone and siltstone. Small structurally controlled low sufide (orogenic) gold, and copper-dominated structurally  controlled high sulfide (orogenic) base metal +/- gold veins.|||Bumballa Formation, Warbisco Shale|Overlies Adaminaby Group.|Black shale and slate, siliceous mudstone, chert, siltstone, fine-grained quartz sandstone to quartzite; massive to laminated, commonly graptolitic, deep marine.|18-MAY-16
1474|Bendoc Group|70493|6|Mentioned|p56||Late Ordovician|Lachlan Orogen.||||Overlies Adaminaby Group.||
1474|Bendoc Group|70540|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Warbisco Shale.|||
1474|Bendoc Group|70541|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Bumballa Formation, Warbisco Shale.|||
1474|Bendoc Group|70542|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician||||Includes Bumballa Formation, Warbisco Shale|||
1474|Bendoc Group|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|Undifferentiated member composed of siliceous shale with interbedded, thinly bedded, ripple cross-laminated and thick bedded quartzose sandstone and siltstone.|||Includes Bumballa Formation, Warbisco Shale and one undifferentiated member.|||
1474|Bendoc Group|70544|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Warbisco Shale|||
1474|Bendoc Group|70545|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Warbisco Shale.|||
1474|Bendoc Group|70601|5|Briefly described|p23, p25-27, p43, p45, p48-55, p57|Bolindian|Gisbornian|Albury-Bega Basin: Inland Zone. Uppermost unit is stratigraphically equivalent to Bogolo Formation.|||Warbisco Shale, Sunlight Creek Formation, Akuna Mudstone, Chakola Formation.|Overlies Numeralla Chert, Adaminaby Group. Underlies Akuna Mudstone, Bogolo Formation.|Black shales, minor turbidites, minor sandstones, chert.|
1474|Bendoc Group|70661|3|Fully described|vii, viii, p12, p13, p14|Eastonian|Gisbornian|Name derived from town of Bendoc, occurs over a vast area of NSW and VIC. Deposited in a deep marine environment with a mixture of hemipelagic and turbiditic sediments.Reference section in Mountain Creek, Victoria. Total thickness of 420m estimated in Moss Vale map sheet. Fossil assemblage described. See also p19, p20 fig 3, p21, p145.|||Bumballa Formation, Warbisco Shale, Sunlight Creek Formation, New Country Sandstone, Akuna Mudstone|Overlain by Bungonia group, Bindook group, Tallong Conglomerate, overlies Nattery Chert Member, overlies Adaminaby Group conformably,  also faulted against Adaminaby Group|Turbiditic sandstone, minor thin chert horizons that passes up into black  siliceous shales.|
1474|Bendoc Group|70684|5|Briefly described|p7 Fig.1, p15|||||||Overlies Adaminaby Group.|Black shales.|
1474|Bendoc Group|70718|4|Described|p43-p44|Late Devonian|Llandovery|Tabberabbera Zone, Murray Basin. Deposited in a deep marine setting. Hosts numerous small orogenic gold deposits.|||||Black shale, slate, siliceous mudstone, chert, siltstone, fine-grained quartz sandstone and quartzite.|02-JUN-19
1474|Bendoc Group|70751|6|Mentioned|p4-p6, p12, p15|Ordovician|Ordovician||||Includes the Currawalla Shale.|||
1474|Bendoc Group|70950|6|Mentioned|p1028-1029|Late Ordovician|Late Ordovician|Geological province: Central Lachlan Orogen. Turbiditic sedimentary rocks that form basement to the Lachlan Orogen|||Includes Currawalla Formation.|||
1474|Bendoc Group|71039|6|Mentioned|p6|Ordovician|Ordovician|||||||
1474|Bendoc Group|71040|6|Mentioned|p3, p10 Fig.6|Late Ordovician|Middle Ordovician|Marked by closely spaced thrust faults.||||||
1474|Bendoc Group|71069|3|Fully described|p9, p21 fig 7, p22, p23, p40 fig 17|Llandovery|Gisbornian|Lachlan Orogen. Name derived from the Bendoc region of Victoria. Previously mapped as part of the Adaminaby and Wagga Groups. Also mapped previously as the Bubalahla Formation, Merigan Black Shale, Birkenburn Beds, Copper Creek Shale and Tallebung Group or Beds. No single type section exists for the Bendoc Group, although a representative section has been proposed. Thickened during the Benambran Orogeny. Hosts VAMS mineralisation. Thickness estimated to range from 450 to over 900m.In deeply weathered areas forms low rounded hills associated with low outcrop, although good exposure is found in quarries and road cuttings. Also overlain by the Covan Creek Formation and unconformably overlain by the Hoskinstown Group.  Contains abundant graptolite fossils, also contains flattened spherical sponges, phosphatic brachiopods, burrows and conodonts.  Distribution, Metamorphism, Tectonic Structure and Geochemistry discussed. See also p41, p45, p51, p52, p53 fig 19, p56, p58, p61, p62, p68, p71-p77, p76 fig 27, p80, p81, p84, p85, p87, p92, p93, p95, p100, p105-p107, p116, p125, p126, p134, p144, p172.|||Includes the Warbisco Shale, Bumballa Formation, Sunlight Creek Formation, Akuna Mudstone, Gungoandra Siltstone, Currawalla Shale, New Country Sandstone and the Willandra Sandstone.|Conformably overlies the Adaminaby Group and the Wagga Group. Conformably overlain by the Margules Group and Yalmy Group.|Siliciclastic turbidite sequences of thick-bedded quartzose sandstone, black shale, siltstone and black carbonaceous to siliceous graptolitic shale.|
1474|Bendoc Group|71303|5|Briefly described|map legend|Late Ordovician|Late Ordovician||||Includes Bumballa Formation, Warbisco Shale.|||
1474|Bendoc Group|71656|4|Described|p10 Fig.1, p11, p14|Sandbian|Darriwilian|Contains poorly preserved graptolites in the early strata (Bumballa Formation).  Conodonts also present in  cherts.|||Bumballa Formation, Warbisco Shale.|Overlies Adaminaby Group. Underlies Margules Group.|Fossiliferous including graptolite bearing shales, conodont bearing cherts.|
1474|Bendoc Group|71691|5|Briefly described|Map legend.|Ordovician|Ordovician||||Warbisco Shale, Bumballa Formation.|Overlies Adaminaby Group. Is overlain by Margules Group.||
1474|Bendoc Group|71693|5|Briefly described|Map legend; p2.|Ordovician|Ordovician|This unit is mapped separately (with the symbol Obe), as well as in combination with the Clements Formation (with the symbol Owac_Obe) where these two units are fault-imbricated. Turbiditic sedimentary sequence.||||Overlies Clements Formation (Wagga Group).|Black shale and slate, siliceous mudstone, chert, siltstone, fine-grained quartz sandstone to quartzite; massive to laminated, commonly graptolitic, deposited as deep marine sediments.|
1474|Bendoc Group|71699|5|Briefly described|Map legend.|Ordovician|Ordovician||||Bumballa Formation, Warbisco Shale.|Overlies Adaminaby Group. Is overlain by Margules Group.||
1474|Bendoc Group|71700|3|Fully described|vi, viii, ix, p5, p7, p9-p11,  p36-p40,|Late Ordovician|Ordovician|Lachlan Orogen. VandenBerg et al (1992) described an almost complete reference section in Mountain Creek Additionally Thomas and Pogson (2012) proposed several represnetative sections in the Goulburn 1:250k sheet. The name is derived from the Bendoc region of East Gippsland, Victoria. Seperated by Felton and Huleatt (1975) from the Adaminaby Group as the "Merigan Black Shale". Rocks of this unit were previously included in the "Abercrombie Beds" (Packham 1968) and Adaminaby Group (Raymond et al. 1998). Scheibner (1973a) made the first attempt to map the shale-rich rocks as the "Bubalahla Formation". The Bendoc Group was subsequently mapped by Lewis et al (1994). Distribution, Geomorphic expression, outcrop, thickness, structure, geophysical characteristics, fossils and geochemistry are described. Thickness estimates for this group are difficult due to internal deformation and a lack of complete stratigraphic contacts; however, in the least-deformed sections thickness reaches up to 900m.Faulted against the Abercrombie Formation. See also p45-p46, p48, p50, p57, p60, p64, p71, p79, p82-p83, p90, p107, p110 and CD.|||Includes the Bumballa Formation, Warbisco Shale, Sunlight Creek Formation, New Country Sandstone and Akuna Mudstone.|Conformably overlies the Adaminaby Group. Conformably overlain by the Margules Group. Unconformably overlain by the Mount Fairy Group and the Woodlawn Volcanics.|Siliceous black shale which overlies a sequence of turbiditic, thin-bedded, ripple cross-laminated, and thick -bedded quartzose sandstone, black shale and siltstone (Bumballa Formation).|
1474|Bendoc Group|71889|6|Mentioned|p9, p12||||||Includes the Currawalla Shale.|||
1474|Bendoc Group|72082|5|Briefly described|p4|Ordovician|Ordovician||||||Metasedimentary sequences.|
1474|Bendoc Group|72083|6|Mentioned|p10||||||Currawalla Shale.|||
1474|Bendoc Group|72084|5|Briefly described|p2, p6 Fig.5a, p7, p9|Late Ordovician|Late Ordovician||||Currawalla Shale.||Metasedimentary sequence.|
1474|Bendoc Group|72296|5|Briefly described|p59|||Largely pelagic sequence.|||||Black muds.|
1474|Bendoc Group|72908|6|Mentioned|p4, p28|Ordovician|Ordovician||||||Contains black shale/carboniferous units.|
1474|Bendoc Group|73059|5|Briefly described|p1059|Late Ordovician|Late Ordovician|Tabberabbera Zone.||||Overlies Adaminaby Group.||
1474|Bendoc Group|73140|5|Briefly described|p495|Bolindian|Gisbornian|Following the division of the late Ordovician sequence in the Goulburn area by Thomas and Pogson (2012), it is proposed that the New Country Sandstone, Akuna Mudstone, Gungoandra Siltstone and Willandra Sandstone are reassigned from the Bendoc Group to Margules Group.|||Warbisco Shale, Bumballa Formation, Currawalla Shale, Sunlight Creek Formation|Overlies Adaminaby Group, underlies Margules Group|Defined by marked reduction in terrigenous sedimentation.|
1474|Bendoc Group|73186|6|Mentioned|p227, p229 Fig.2, p237, p242|Late Ordovician|Late Ordovician|Lachlan Orogen, Tabberabera Zone, Omeo Zone, Bega and eastern Victoria. 700 m thick.|||||Black shale.|
1474|Bendoc Group|73211|6|Mentioned|p909|Upper Ordovician|Middle Ordovician|Referred to as the foundation of the Lachlan Orogen/Fold Belt.||||||
1474|Bendoc Group|73431|6|Mentioned|p363 Fig.1|Late Ordovician|Late Ordovician||||||Sediments.|
1489|Bennetts Creek Volcanics|22857|4|Described|p466 App.1 Tb.A1.6|Silurian|Silurian|Felsic volcanics, shales and limestone lenses, conglomerates.||||||
1489|Bennetts Creek Volcanics|23454|6|Mentioned|p29|||||||||
1489|Bennetts Creek Volcanics|33780|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
1489|Bennetts Creek Volcanics|35109|2|Defined|p20|Llandoverian|Llandoverian|Llandoverian to Early Devonian ?||||||
1489|Bennetts Creek Volcanics|36411|6|Mentioned|p267|||Refers White et al 1977 for definition.||||||
1489|Bennetts Creek Volcanics|40328|5|Briefly described|p139|||||||||
1489|Bennetts Creek Volcanics|41905|6|Mentioned|p30|||||||||
1489|Bennetts Creek Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
1489|Bennetts Creek Volcanics|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv9||||||
1489|Bennetts Creek Volcanics|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
1498|Bergalia Formation|22477|4|Described|p173,177, Fig.3||Oligocene|||||||
1498|Bergalia Formation|22815|5|Briefly described|p115|Tertiary|Tertiary|||||||
1498|Bergalia Formation|29746|6|Mentioned|p2|||||||||
1498|Bergalia Formation|32126|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
1498|Bergalia Formation|32129|6|Mentioned|p7|||Refers Bembrick (1972)||||||
1498|Bergalia Formation|32673|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
1498|Bergalia Formation|34225|6|Mentioned|p552|||||||||
1498|Bergalia Formation|34341|6|Mentioned|p553|||||||||
1498|Bergalia Formation|35289|3|Fully described|p41|||||||||
1498|Bergalia Formation|36411|6|Mentioned|p267|||Refers Chalker & Bembrick 1977 for redefinition.||||||
1498|Bergalia Formation|42786|5|Briefly described|p364|||see also Fig.1 p358||||||26-NOV-15
1498|Bergalia Formation|43465|14|Not recorded|Map Legend||Tertiary|||||||
1498|Bergalia Formation|61155|5|Briefly described|p19|Late Oligocene|Early Oligocene|Sedimentary deposits. Overlain by Moruya Province Volcanics (Colia Basalts [misspelling of Coila Basalt]). In Southeastern NSW.||||||26-NOV-15
1498|Bergalia Formation|71408|6|Mentioned|p1027|Oligocene|Oligocene|Batemans Bay region. Fluvial gravels are quartz-dominated unlike the catchment geology.||||||
1504|Berkeley 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.||||||
1504|Berkeley Latite Member|23544|5|Briefly described|Fig 2 p358|||In the Gerringong Volcanics||||||
1504|Berkeley Latite Member|29900|4|Described|Table 1|||||||||
1504|Berkeley Latite Member|29901|4|Described|Table 1|||||||||
1504|Berkeley Latite Member|31128|6|Mentioned|Table 1|||||||||
1504|Berkeley Latite Member|36220|3|Fully described|p46|||See also Table 10 & P38.||||||
1504|Berkeley Latite Member|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
1504|Berkeley Latite Member|39309|6|Mentioned|p123|||||||||
1504|Berkeley Latite Member|42737|5|Briefly described|map legend|Permian||||||||
1504|Berkeley Latite Member|71115|5|Briefly described|p178-180, 182-185, 187-188|Permian|Permian|Southern Sydney Basin. Limited in exposure, and more poorly developed columnar jointing than other Members. Paleomagnetic results tabulated, discussed.|258 +/- 5 Ma (Evernden and Richards, 1962).|Gerringong Volcanics.||Overlies Minnamurra Latite Member. Is overlain by Unanderra Coal Member (Pheasants Nest Formation).|Basaltic. Varies from aphanitic to porphyritic with plagioclase laths up to 10mm long, and pyroxene phenocrysts up to 5mm across.|
1504|Berkeley 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.|
1516|Berrico Creek Formation|22736|6|Mentioned|p628 Fig7|Namurian|Visean|||||||
1516|Berrico Creek Formation|22857|4|Described|p512 App.1 Tb.A1.8|Visean|Visean|Grey and brown lithic arenite, mudstone; minor conglomerate, discontinuous limestone. Max. thickness: >300m. ||||||
1516|Berrico Creek Formation|32324|6|Mentioned|Table 8.1|||||||||
1516|Berrico Creek Formation|32379|6|Mentioned|Fig.3|||||||||
1516|Berrico Creek Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
1516|Berrico Creek Formation|32868|6|Mentioned|p200|||||||||
1516|Berrico Creek Formation|35492|6|Mentioned|p141|||||||||
1516|Berrico Creek Formation|35856|5|Briefly described|p189|||||||||
1516|Berrico Creek Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
1516|Berrico Creek Formation|36528|6|Mentioned|p178|||||||||
1516|Berrico Creek Formation|36599|6|Mentioned|Fig.1|||||||||
1516|Berrico Creek Formation|39302|6|Mentioned|p348|||||||||
1516|Berrico Creek Formation|39979|6|Mentioned|p62|||||||||
1516|Berrico Creek Formation|40883|6|Mentioned|Fig.2|||||||||
1516|Berrico Creek Formation|41348|5|Briefly described|Map legend|Carboniferous||In the Tamworth Belt.||||||16-DEC-04
1516|Berrico Creek Formation|42547|4|Described|p35|||||||||
1516|Berrico Creek Formation|44093|5|Briefly described|p190 App. 1|Late Devonian|Late Devonian|Geological Province: New England Fold Belt.||||||
1516|Berrico Creek Formation|44244|2|Defined|p131, p142|Visean|Visean|Includes the Buggs Creek Volcanic Member which conformably overlies the Conger Formation. Underlies the Faulkland Formation conformably.  Max. thickness: 300m+.  Type section in text.  Geological Procince: Myall Block.||||||16-SEP-04
1516|Berrico Creek Formation|50147|5|Briefly described|Map legend|Visean|Visean|Grey to brown lithic sandstone, conglomerate, thinly bedded dark grey mudstone with discontinuous limestone, and a basal rhyodacitic ignimbrite.||||||
1516|Berrico Creek Formation|63832|6|Mentioned|p131 fig 2|Visean|Visean|Western Myall block, Southern New England Fold Belt.||||||
1516|Berrico Creek Formation|64631|5|Briefly described|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt, western Myall Block. Biostratigraphic age control at base and top.||||Shown as underlying Faulkland and Karuah Formations, and overlying Nerong Volcanics.||
1516|Berrico Creek Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Myall Block, Tamworth Belt.||||||
1517|Berridale Granite|34404|6|Mentioned|p96|||||||||
1517|Berridale Granite|34405|6|Mentioned|p119|||||||||
1517|Berridale Granite|34544|5|Briefly described|p195|||See also P187||||||
1517|Berridale Granite|35044|6|Mentioned|p25|||||||||
1517|Berridale Granite|35109|6|Mentioned|p33|||Now referred to as the Berridale Batholith.||||||
1517|Berridale Granite|43344|14|Not recorded|p126|||Cooma area||||||
1517|Berridale Granite|45087|5|Briefly described|p40|||Chemical analyses||||||
1517|Berridale Granite|60007|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Included in undifferentiated granites of the Berridale Batholith.||||||
1520|Berridong Siltstone|22857|5|Briefly described|p456 App.1 Tb.1A1.6|Devonian|Silurian|Of the Toongi Group. Siltstone, lithic sandstone. Max. thickness: 400m. Geological Province: Cowra Trough.||||||
1520|Berridong Siltstone|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Toongi Group.||||||11-JAN-10
1520|Berridong Siltstone|23170|2|Defined|p117|Late Silurian|Late Silurian|of Toongi Group.||||||
1520|Berridong Siltstone|29986|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
1520|Berridong Siltstone|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
1520|Berridong Siltstone|32485|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
1520|Berridong Siltstone|40328|2|Defined|p125|Silurian|Silurian|||||||
1520|Berridong Siltstone|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
1520|Berridong Siltstone|43500|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition) Part of Toongi Group||||||
1520|Berridong Siltstone|48958|6|Mentioned|Plate 1|||||||||
1520|Berridong Siltstone|68003|5|Briefly described|p24 Fig.3-e, p145. |Ludlow|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Gilgal Formation. Is overlain by Wambangalong Formation.|Siltstone, lithic sandstone, phyllite.|
1524|Berrigan Granite|22857|5|Briefly described|p213|Devonian|Devonian|Massive, pink, biotite, felsic, fractionated I-type granite. Geological Province: Barka Basin.||||||
1524|Berrigan Granite|22859|5|Briefly described|p213|||||||||
1524|Berrigan Granite|30909|6|Mentioned|Map legend|Silurian|Silurian|Prob. Silurian||||||
1524|Berrigan Granite|33553|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1524|Berrigan Granite|34418|6|Mentioned|p502|||?Late Silurian||||||
1524|Berrigan Granite|40328|4|Described|p202|||||||||
1524|Berrigan Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
1524|Berrigan Granite|44340|14|Not recorded|p.5|||I/55-14. Upper Silurian?||||||
1524|Berrigan Granite|44341|14|Not recorded|map legend|||Coarse pink porphyritic granite. Upper Silurian?||||||
1524|Berrigan Granite|69798|6|Mentioned|p6, p13-14, p17|||Part of the basement to Oaklands Basin. Appears to have been significantly displaced by fault(s).||||||
1574|Bickham Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
1574|Bickham Formation|31881|6|Mentioned|p331|||See also Figs 1 & 2 & Table 1||||||
1574|Bickham Formation|31882|6|Mentioned|Table 1|||||||||
1574|Bickham Formation|32482|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1574|Bickham Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
1574|Bickham Formation|35284|6|Mentioned|p37|||||||||
1574|Bickham Formation|37558|6|Mentioned|p998|||||||||
1574|Bickham Formation|41348|5|Briefly described|Map legend|Permian||||||||16-DEC-04
1574|Bickham Formation|43407|14|Not recorded|Map Legend||Late Permian|(Provisional Edition)||||||
1574|Bickham Formation|43417|14|Not recorded|Map Legend||Permian|||||||
1574|Bickham Formation|68003|5|Briefly described|p38 Fig.3-j, p40, p41, p130.|Early Permian|Early Permian|Werrie Basin (South), Brigalow Belt South Bioregion. Coeval with Borambil Creek and Toll Bar Formations in the north of the Basin. Correlative of Millie Group (Gunnedah Basin), Maitland Group (Hunter Coalfield), and Shoalhaven Group (Western Coalfield).||||Overlies Koogah Formation. Is overlain by Murulla beds.|Sandstones and conglomerates.|
1574|Bickham Formation|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian marine sequences: conglomerate, quartzose sandstone, siltstone, calcareous mudstone and limestone.||||||
1574|Bickham Formation|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
1574|Bickham Formation|70791|6|Mentioned|p293 Fig.17|Permian|Permian|Werrie Basin.||||||
1601|Big Table Top Formation|23540|4|Described|p 420|||In Cranky Corner Basin. Also see p 424||||||20-FEB-07
1601|Big Table Top Formation|39288|6|Mentioned|Fig.3.3|||||||||
1601|Big Table Top Formation|60290|5|Briefly described|p15|Permian|Permian|Of Maitland Group. Overlies Greta Coal Measures. Geological Province: Cranky Corner Basin.||||||07-FEB-11
1608|Bigga Granite|22679|4|Described|p 43||Silurian|||||||
1608|Bigga Granite|23214|3|Fully described|p167|Late Silurian|Late Silurian|Previously termed Bigga Adamellite.  Intrudes the Adaminaby Group and Streamville Granodiorite. Coarse grained, porphyritic, biotite - rich granite. Geological Province: Wyangala Batholith||||||
1608|Bigga Granite|34544|6|Mentioned|p188|||Refers Hasan (1956, 1959)||||||
1608|Bigga Granite|42726|5|Briefly described|map legend|Silurian||||||||
1608|Bigga Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangla Batholith. Coarse foliated cordierite biotite granite.||||||17-JUL-08
1608|Bigga Granite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of Wyangala Batholith.||||||12-JUN-08
1608|Bigga Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Leucocratic massive to protomylonitic megacrystic perthite porphyritic biotite granite.||||||13-MAY-04
1608|Bigga Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Blue-grey, coarse-grained, massive to protomylonitic, porphyritic, often megacrystic biotite granite. High K, Th and U radioelement response.||||||12-JUN-08
1608|Bigga Granite|66300|6|Mentioned|p92.||||430 +/- 6 Ma (Wilde, 2001).|Unit in Hovells Suite.||||
1608|Bigga Granite|67820|6|Mentioned|p136|||Weakly to moderately fractionated and reduced; may have potential for Sn-W mineralisation.||||||
1608|Bigga Granite|68592|2|Defined|p1260, p1262-4, p1268-9, p1272-7|Early Devonian|Early Devonian|See also p99-101, p1255 Fig.220, p1284, p1664. Hasan (1957, 1959). Named after the village of Bigga. Renamed Bigga Adamellite by Gibson (1973), and by Close (1978) whose mapping extended the pluton to the N. Reclassified to meet standard nomenclature by Pogson and Watkins (1998) back to Bigga Granite. The parent Wyangala Suite (Chappell et al., 1991) has been superseded by Hovells Suite which incorporates several new units on geochemical grounds. Occupies a very hilly area; crops out as numerous large tors. No previous type locality; one is proposed here. Geochemistry detailed; geophysical properties described. Has a broad protomylonitic zone on the E margin recording W-over-E thrust movement. Age determination discussed.|408 +/- 13 Ma (SHRIMP U-Pb zircon: Wilde, 2001).|Unit in Hovells Suite.||Intrudes Adaminaby Group, Little Redbank and Streamville Granodiorites, Willdamar Tonalite, Goonoonglah Monzodiorite. Is intruded by Blackmans Creek and Yewrangara Granites and Bishopthorpe Suite.|Blue-grey, coarse-grained, porphyritic, commonly megacrystic, massive to protomylonitic biotite granite. Foliated. Metasedimentary and vein quartz xenoliths to 200mm are common. Not fractionated. S-type.|
1608|Bigga Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Soi. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Coarse grained, porphyritic, commonly megacrystic, massive-protomylonitic biotite granite; high K and Th, low to high U response; low magnetic susceptibility.|
1608|Bigga Granite|70297|5|Briefly described|map legend|Silurian|Silurian|||Wyangala Supersuite||||
1608|Bigga Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Hovells Suite|||Coarse grained, porphyritic, commonly megacrystic, massive-protomylonitic biotite granite; high K and Th, low to high U response; low magnetic susceptibility.|
1617|Biggam Tonalite|22815|5|Briefly described|p51|Early Devonian|Late Silurian|||||||
1617|Biggam Tonalite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
1617|Biggam Tonalite|35109|2|Defined|p77|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
1617|Biggam Tonalite|35263|6|Mentioned|Table 3|||||||||
1617|Biggam Tonalite|36411|6|Mentioned|p267|||Refers White et al 1977 for definition.||||||
1617|Biggam Tonalite|40328|4|Described|p202|||||||||
1617|Biggam Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Jindabyne Suite.||||||
1617|Biggam Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh11||||||
1617|Biggam Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
1669|Bimbimbie Granodiorite|22815|4|Described|p56|Silurian|Silurian|Rb/Sr Age: 414.8+/-3.7 Ma.||||||
1669|Bimbimbie Granodiorite|33852|6|Mentioned|Fig.2|||Date on Table 1.||||||
1669|Bimbimbie Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
1669|Bimbimbie Granodiorite|40328|4|Described|p202|||||||||
1669|Bimbimbie Granodiorite|41905|2|Defined|p94|Silurian||||||||
1669|Bimbimbie Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
1669|Bimbimbie Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
1669|Bimbimbie Granodiorite|42647|5|Briefly described|p41|||||||||
1669|Bimbimbie Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Currowong Suite.||||||
1669|Bimbimbie Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh22||||||
1669|Bimbimbie Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
1669|Bimbimbie Granodiorite|72571|5|Briefly described|p90-91, p94, p96, p98-100|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail.||Currowong Suite|||Mafic hornblende granite with magnetite, albanite and no titanite.|
1674|Binda Granite|42726|5|Briefly described|map legend|Silurian||||||||
1674|Binda Granite|50232|5|Briefly described|Map legend|Pridoli|Ludlow|Part of the Wyangala Batholith.  Foliated to massive, biotite granite, biotite tonalite, biotite-quartz monzonite, and muscovite-biotite granodiorite, albite granite, with miarolitic cavities.||||||
1674|Binda Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith.||||||
1674|Binda Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Crooked Corner Suite.  Foliated to massive biotite granite, biotite tonalite, biotite-quartz monzonite + mucovite-biotite granodiorite, + albite granite with miarolitic cavities. Intruded by dykes of dolerite, microgranite, aplite, rhyolite, qtz. veins||||||25-JUN-08
1674|Binda Granite|68592|2|Defined|p1466-70, p1475-81, p1664|Early Devonian|Early Devonian|Named by Chappell et al. (1991); previously assigned to the Wyangala Batholith by Stevens (1955). Placed within Crooked Corner Suite by Blevin (2011). Very poor outcrops. Type area described. Lithology, and geochemistry (similar to Asylum Granite), detailed; geophysical properties described. SHRIMP U-Pb zircon age. Quartz veins and aplite dykes host disseminated pyrite-arsenopyrite-gold mineralisation: the Caledonia and Wheel of Fortune mines and the Markdale workings.|405 +/- 12 Ma (Wilde, 2001).|Unit in Crooked Corner Suite.||Intrudes Cuddyong and Abercrombie Formations. Is intruded by Romner Granite and Bishopthorpe Suite.|Medium- to coarse-grained, equigranular to porphyritic, massive to recrystallised and foliated, hornblende-biotite granite and borderline tonalite/granodiorite; minor leucogranite and dykes and sills of aplite, microgranite and rhyolite. I-type.|
1674|Binda Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Drb. Includes three unnamed members: aplite; porphyritic biotite-muscovite microgranite and flow banded rhyolite dykes; medium-coarse grained, equigranular-porphyritic biotite leucogranite. On Crookwell and Gunning 1:100 000 mapsheet portions of Time-Space Plot.||Crooked Corner Suite|Includes three unnamed subunits.||Medium-coarse grained, equigranular-porphyritic, massive-foliated hornblende-biotite granite and borderline tonalite/granodiorite with metasedimentary xenoliths, megacrystic biotite clots and mafic enclaves; aplite, microgranite and rhyolite dykes.|
1674|Binda Granite|70541|4|Described|Map Legend|Devonian|Devonian|||Crooked Corner Suite|||Medium-coarse grained, equigranular-porphyritic, massive-foliated, hornblende-biotite granite and borderline tonalite/granodiorite with metasedimentary xenoliths, megacrystic biotite clots and mafic enclaves; aplite, microgranite and rhyolite dykes.|
1674|Binda Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|Includes three unnamed members: Aplite; porphyritic biotite-muscovite microgranite and flow banded rhyolite dykes;  medium-coarse grained, equigranular-porphyritic biotite leucogranite.||Crooked Corner Suite|Includes three unnamed subunits||Medium-coarse grained, equigranular-porphyritic, massive-foliated hornblende-biotite granite and borderline tonalite/granodiorite with metasedimentary xenoliths, megacrystic biotite clots and mafic enclaves; aplite, microgranite and rhyolite dykes.|
1689|Bingie Bingie Gabbro|42726|5|Briefly described|map legend|||Reserved as Bingie Bingie.||||||
1690|Bingleburn Formation|31228|6|Mentioned|p77|||||||||
1690|Bingleburn Formation|44093|5|Briefly described|p229 App. 1|Visean|Tournaisian|Geological Province: New England Fold Belt.||||||
1691|Bingleburra Formation|22857|4|Described|p498 App.1 Tb.A1.7|Tournaisian|Tournaisian|Mudstone, siltstone, occasional crinoidal and oolitic limestone, fine-grained sandstone. Max. thickness: 375m. Geological Province: Tamworth Forearc Basin.||||||03-FEB-06
1691|Bingleburra Formation|31228|6|Mentioned|p77|||Stratigraphy||||||
1691|Bingleburra Formation|31519|6|Mentioned|Fig. 1|||||||||
1691|Bingleburra Formation|31706|6|Mentioned|p651|||L.Carb. correlation chart||||||
1691|Bingleburra Formation|31802|6|Mentioned|p136|||Refers Roberts (1961)||||||
1691|Bingleburra Formation|32141|6|Mentioned|p148|||Tournaisian||||||
1691|Bingleburra Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
1691|Bingleburra Formation|32866|6|Mentioned|p8|||Fossil content||||||
1691|Bingleburra Formation|32867|6|Mentioned|p30|||||||||
1691|Bingleburra Formation|32869|5|Briefly described|p167|||Lithology & depositional environment. See also Fig.2||||||
1691|Bingleburra Formation|33728|6|Mentioned|p50|||||||||
1691|Bingleburra Formation|34072|6|Mentioned|Fig.4.5|||Fossils||||||
1691|Bingleburra Formation|34077|5|Briefly described|p252|||||||||
1691|Bingleburra Formation|34085|6|Mentioned|Cor.chart|||Tournaisian - Visean||||||
1691|Bingleburra Formation|34086|6|Mentioned|p262|||||||||
1691|Bingleburra Formation|34238|6|Mentioned|Table 1|||||||||
1691|Bingleburra Formation|36057|6|Mentioned|p352|||||||||
1691|Bingleburra Formation|37068|6|Mentioned|p59|||||||||
1691|Bingleburra Formation|39302|6|Mentioned|p341|||||||||
1691|Bingleburra Formation|40883|6|Mentioned|p5|||||||||
1691|Bingleburra Formation|42547|4|Described|p28|||||||||
1691|Bingleburra Formation|43383|14|Not recorded|p18|||||||||
1691|Bingleburra Formation|43432|14|Not recorded|p206||Early Carboniferous|||||||
1691|Bingleburra Formation|43447|4|Described|Table 1&2,p6,7,10||Tournaisian|||||||
1691|Bingleburra Formation|43451|14|Not recorded|Map Legend|||||||||
1691|Bingleburra Formation|43479|14|Not recorded|p158,177|Visean|Tournaisian|||||||
1691|Bingleburra Formation|43536|14|Not recorded|p682,683|||||||||
1691|Bingleburra Formation|43576|6|Mentioned|Fig.1,p348|||||||||
1691|Bingleburra Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
1691|Bingleburra Formation|43983|14|Not recorded|p12|||||||||
1691|Bingleburra Formation|44244|4|Described|p47|Tournaisian|Famennian|Max. thickness: >375m.  Type section in text.  Geological Procince: Gresford Block||||||13-JUL-04
1691|Bingleburra Formation|44360|14|Not recorded|p33||Early Carboniferous|||||||
1691|Bingleburra Formation|44833|14|Not recorded|p107-121|||Faunal zones.||||||
1691|Bingleburra Formation|45088|6|Mentioned|p63|||Refers Roberts (1961,1963,1965)||||||
1691|Bingleburra Formation|45097|6|Mentioned|p25|||Brachiopods. Carboniferous correlation chart||||||
1691|Bingleburra Formation|46803|6|Mentioned|p147|||See also Fig. 3||||||
1691|Bingleburra Formation|47056|6|Mentioned|Fig.2 P523|||||||||
1691|Bingleburra Formation|48924|6|Mentioned|p14||Late Carboniferous|L.Carb.||||||
1691|Bingleburra Formation|50147|5|Briefly described|Map legend|Carboniferous|Carboniferous|Brown and grey, thinly bedded mudstone and siltstone with thin interbeds of lithic sandstone, oolitic and crinoidal limestone.  Geol. Province: Gresford Block||||||
1691|Bingleburra Formation|66498|6|Mentioned|p49|||Vertebrate fossils listed.||||||
1691|Bingleburra Formation|68297|5|Briefly described|p197|Tournasian|Tournasian|Includes shark faunas||||||
1691|Bingleburra Formation|69793|6|Mentioned|p1121 Fig.12|Tournaisian|Tournaisian|Gresford Block, Tamworth Belt.||||||
1700|Binna Burra Rhyolite|22773|5|Briefly described|p345|||||||||
1700|Binna Burra Rhyolite|22857|5|Briefly described|p345|Cenozoic|Cenozoic|In the border region of Lamington National Park. Included in the central-volcano provinces of NSW. At least 5 individual flows each up to 100m thick occur in the type area near Binna Burra.||||||19-NOV-08
1700|Binna Burra Rhyolite|30604|6|Mentioned|p66|||||||||
1700|Binna Burra Rhyolite|30687|4|Described|p64|||See also p65,67,76,77. Miocene age.||||||03-SEP-18
1700|Binna Burra Rhyolite|30689|5|Briefly described|p76|||Also mention Table on p76.||||||03-SEP-18
1700|Binna Burra Rhyolite|31130|6|Mentioned|Fig. 2|||Lower Miocene||||||
1700|Binna Burra Rhyolite|32924|6|Mentioned|p113|||Refers McTaggart (1961)||||||
1700|Binna Burra Rhyolite|33290|4|Described|p37|||See also p38.||||||03-SEP-18
1700|Binna Burra Rhyolite|33751|6|Mentioned|p147|||||||||
1700|Binna Burra Rhyolite|35156|6|Mentioned|p8|||||||||
1700|Binna Burra Rhyolite|35296|6|Mentioned|p12|||Re stratigraphy.||||||
1700|Binna Burra Rhyolite|36806|6|Mentioned|p131|||||||||
1700|Binna Burra Rhyolite|39969|6|Mentioned|Fig.22|||||||||
1700|Binna Burra Rhyolite|40623|5|Briefly described|p39|||||||||
1700|Binna Burra Rhyolite|40780|5|Briefly described|p9|||||||||
1700|Binna Burra Rhyolite|40896|4|Described|p6|||||||||
1700|Binna Burra Rhyolite|42317|5|Briefly described|p2|||||||||
1700|Binna Burra Rhyolite|43161|4|Described|12, 19|||Dated: 20.5 to 23.5 Ma||||||
1700|Binna Burra Rhyolite|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
1700|Binna Burra Rhyolite|44813|14|Not recorded|p80||Tertiary|=Mount Lindsay Rhyolite.||||||
1700|Binna Burra Rhyolite|44818|6|Mentioned|p275|||||||||
1700|Binna Burra Rhyolite|44871|2|Defined|p140|Tertiary|Tertiary|Of Lamington Group.||||||
1700|Binna Burra Rhyolite|48917|6|Mentioned|p38|||Refers McTaggart (1961).||||||
1700|Binna Burra Rhyolite|69599|5|Briefly described|p631, p633 Fig.8.35, p640-641|||Northern side of the Tweed volcano, centred on Mount Warning. Resistant; forms cliff lines and waterfalls. Table of chemical analyses; REE diagram and comment. An age determination of 13.0 +/- 0.5 Ma (Wellman and McDougall, 1974) is "clearly aberrant".|23.9 +/- 0.2 Ma.|||Approximate equivalent of Nimbin Rhyolite in NSW.|Peraluminous or high-silica rhyolite.|
1700|Binna Burra Rhyolite|73450|4|Described|p99-101|Chattian|Chattian|Associated with the Tweed Volcano. Up to 500 m thick. Five separate lava flows have been identified, each up to 100 m thick. Separated from the Binna Burra Rhyolite by basalt (at least locally). Yielded an Ar-Ar sanidine age of 23.9 +/- 0.2 Ma (Cohen, 2007) and K-Ar feldspar ages of 20.8 +/- 0.4 Ma and 20.9 +/- 0.4 Ma (Ewart, 1982).|23.9 +/- 0.2 Ma Ar-Ar||||Coherent felsic lava and minor pyroclastic deposits including ash flow tuff and ash fall tuff.|
1700|Binna Burra Rhyolite|73581|5|Briefly described|p6|Oligocene|Oligocene|Tweed Volcano. Original K-Ar age of 20.9 Ma (Ewart, 1982) was reanalysed and produced an Ar-Ar age of 23.9+/-0.2 Ma (Cohen, 2007). Overlies Beechmont Basalt/Lismore Basalt.|23.9+/-0.2 Ma Ar-Ar (Cohen, 2007)||||Rhyolitic tuff and rhyolite lavas up to 100 m thick.|
1776|Black Bog Shale|22857|5|Briefly described|p458 App.1, Tb.A1.6|Late Silurian|Late Silurian|Of the Booroo Ponds Group. Contains rich fauna: corals, brachiopods, trilobites. Max. thickness: 147m. Geological Province: Canberra-Yass Shelf.||||||
1776|Black Bog Shale|24248|5|Briefly described|p52, p50 Fig.1|Ludfordian|Ludfordian|Geological Province: Yass Syncline. Overlying: Rosebank Shale. Underlying Unit: Silverdale Formation.||||||
1776|Black Bog Shale|30069|6|Mentioned|p5|||||||||
1776|Black Bog Shale|30252|6|Mentioned|p183|||||||||
1776|Black Bog Shale|30332|6|Mentioned|Table 1|||Refers Link(1971)||||||
1776|Black Bog Shale|31852|6|Mentioned|p711|||See also P714,719,720 & Figs. 1,2,4,5. U.Sil.||||||
1776|Black Bog Shale|32675|6|Mentioned|p8|||Refers Link (1970, 1971)||||||
1776|Black Bog Shale|32820|6|Mentioned|Table 1|||Refers Pogson & Baker (1974)||||||
1776|Black Bog Shale|33116|5|Briefly described|Fig.11|||Correlation||||||
1776|Black Bog Shale|33325|5|Briefly described|Table 2|||See also Table 3.||||||
1776|Black Bog Shale|34405|4|Described|p113|||||||||
1776|Black Bog Shale|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
1776|Black Bog Shale|35386|3|Fully described|p35|||||||||
1776|Black Bog Shale|36411|6|Mentioned|p267|||Refers Cramsie et al 1978 for definition.||||||
1776|Black Bog Shale|36413|6|Mentioned|Table 3|||||||||
1776|Black Bog Shale|37013|6|Mentioned|p24|||||||||
1776|Black Bog Shale|37727|4|Described|p38|||See also p6 and p8..||||||12-JUN-08
1776|Black Bog Shale|37752|6|Mentioned|p115|||||||||
1776|Black Bog Shale|38151|6|Mentioned|p42|||||||||
1776|Black Bog Shale|38378|6|Mentioned|p142|||||||||
1776|Black Bog Shale|38787|6|Mentioned|p127|||||||||
1776|Black Bog Shale|39331|6|Mentioned|Fig.5-5|||||||||
1776|Black Bog Shale|39975|6|Mentioned|p128|||||||||
1776|Black Bog Shale|40328|3|Fully described|p51|||||||||
1776|Black Bog Shale|42994|6|Mentioned|p72|||of Booroo Ponds Group||||||
1776|Black Bog Shale|43344|14|Not recorded|p113,119||Late Silurian|Yass||||||
1776|Black Bog Shale|43385|14|Not recorded|p172||Late Silurian|||||||
1776|Black Bog Shale|45075|5|Briefly described|p7|||||||||
1776|Black Bog Shale|47037|6|Mentioned|p107|||||||||
1776|Black Bog Shale|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Hattons Corner Group. Contains the Yarwood Siltstone Member. Overlies Hume Limestone Member (Silverdale Formation); underlies Rosebank Shale. Dark grey shale, mudstone, siltstone and graptolitic black shale.||||||20-MAR-07
1776|Black Bog Shale|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hattons Corner Group. Contains Yarwood Siltstone Member ("Lower Trilobite bed") - dk. grey shale, mudstone, siltstone and black graptolitic shale; +2 unnamed subunits of black graptolitic shale/mudst.(upper) and dk grey shale/mudst (lower).||||||09-SEP-08
1776|Black Bog Shale|67651|5|Briefly described|p422|||Of Yass Basin.|||Includes Yarwood Silstone Member.|||
1776|Black Bog Shale|67820|6|Mentioned|p136 Fig.3|Silurian|Silurian|||Hattons Corner Group.||||
1776|Black Bog Shale|68592|2|Defined|p429-30 Fig.89,p560-2,p583-9,p744,p772|Ludfordian|Ludfordian|See also p814, p908, p1880-3. Yass Basin. Formerly Black Bog Shales (Brown, 1940), part of her Hume Series; included as a Formation by Link (1970, 1971); Link and Druce (1972) in their Booroo Ponds Group; here transferred to redefined Hattons Corner Group. Type section described. 68-152m thick. Also appears as Black Bog shale in the same Fig.89. Sparsely fossiliferous; concentrated in several levels. A group of small epithermal vein Cu-Pb-Zn workings are exploited by Candish and Smith Workings Prospect No.14. Contains a Bohemograptus subsp. graptolite similar to those in abundance in Kerrawary Siltstone. Fossil fauna described, including the recently described, earliest holothurian body fossil Porosothyone picketti (Jell, 2010).||Unit in Hattons Corner Group.|Includes Yarwood Siltstone Member.|Overlies Silverdale Formation gradationally. Is overlain conformably by Rosebank Shale. Time-equivalent to Cardinal View Formation.|Grey, massive or finely laminated mudstone sequence ovelain by a thin but persistent calcareous mudstone or siltstone horizon; succeeded by an upper sequence of massive, black to dark-grey shale with minor thin-bedded sandy siltstone interbeds.|
1776|Black Bog Shale|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Shb[3 asterisks]. Includes two unnamed members: massive or finely laminated mudstone; massive-rarely laminated graptolitic shale. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hattons Corner Group|Includes Yarwood Siltstone Member and two unnamed members.|Overlies Hume Limestone Member (Silverdale Formation). Is overlain by Rainbow Hill Member (Rosebank Shale).|Massive-finely laminated mudstone, massive-rarely laminated shale with minor thin-bedded, sandy siltstone interbeds; minor calcareous mudstone or siltstone.|
1776|Black Bog Shale|70540|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed members; massive or finely laminated mudstone, massive-rarely laminated graptolitic shale.||Hattons Corner Group|Includes Yarwood Siltstone Member and two unnamed members.||Massive-finely laminated mudstone, massive-rarely laminated shale with minor thin-bedded, sandy siltstone interbeds; minor calcareous mudstone or siltstone.|
1776|Black Bog Shale|70546|5|Briefly described|Map Legend|Devonian|Silurian|||Hattons Corner Group|Includes Yarwood Siltstone Member||Massive or finely laminated mudstone, massive to rarely laminated shale with minor thin bedded, sandy siltstone interbeds; minor calcareous mudstone or siltstone.|
1776|Black Bog Shale|71069|6|Mentioned|p146|||||Hattons Corner Group||Part equivalent to the De Drack Formation.||
1776|Black Bog Shale|71656|4|Described|p12 Fig.2, p19, p24-25, p27, p31|Ludlow|Ludlow|Abundant brachiopods evident. Includes bivalves and graptolites. Earliest known holothurian body fossil.||Hattons Corner Group|Includes Yarwood Siltstone Member.|Underlies Rainbow Hill Member.|Fossiliferous shales.|
1776|Black Bog Shale|71657|6|Mentioned|p40|||Contains the brachiopod Apopentamerus clarkei.|||Yarwood Siltstone Member|||
1798|Black Jack Group|22609|5|Briefly described|Table 1||Late Permian|||||||
1798|Black Jack Group|22857|5|Briefly described|p264, p518 App.1 Tb.A1.9|Late Permian|Late Permian|Divided into Nea, Coogal and Brothers Subgroups. Max. thickness: 470m. Geological Province: Gunnedah Basin. See also p315 Fig. 22.8. ||||||
1798|Black Jack Group|22864|6|Mentioned|p264|||||||||
1798|Black Jack Group|23050|5|Briefly described|p9 Fig.2, 17|Late Permian|Late Permian|Of Gunnedah Basin.||||||
1798|Black Jack Group|23566|5|Briefly described|p116 Fig. 2|Late Permian|Late Permian|Geological Province: Gunnedah Basin||||||
1798|Black Jack Group|23740|5|Briefly described|p1221|Permian|Permian|Geological Province: Gunnedah Basin||||||
1798|Black Jack Group|24159|5|Briefly described|p150 Fig.3, p149|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Overlying Unit: unconformably with Digby Formation. Underlying Unit: Watermark Formation.||||||
1798|Black Jack Group|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
1798|Black Jack Group|42767|6|Mentioned|p5|||||||||
1798|Black Jack Group|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Replaces Black Jack Formation (q.v.). Age Lower Stage 5a to Upper Stage 5c. Formal re-definition published in an article released immediately prior, however a summary of new nomenclature is provided in Appendix 1.||||||13-NOV-13
1798|Black Jack Group|43582|6|Mentioned|Fig.5,p16||Late Permian|||||||
1798|Black Jack Group|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Includes: Nea Subgroup, Coogal Subgroup, Brothers Subgroup.||||||
1798|Black Jack Group|61313|5|Briefly described|p85, p94 Fig. G7|Late Permian|Late Permian|Coal-rich unit including Hoskissons Coal, "Western Sands" and Arkarula Sandstone. Max. thickness: 460m. Geological Province: Gunnedah Basin. See also p95 Fig. G8, p98 Fig. G10.||||||
1798|Black Jack Group|61377|5|Briefly described|p149 Fig. SU8|Late Permian|Late Permian|Includes Arkarula Sandstone, "Western Sands" and Hoskissons Coal. Geological Province: Gunnedah Basin.||||||07-FEB-11
1798|Black Jack Group|61612|6|Mentioned|p274, p277|Late Permian|Late Permian|||||||
1798|Black Jack Group|62357|5|Briefly described|p524 Fig. 7|Late Permian|Middle Permian|Geological Province: Gunnedah Basin.||||||
1798|Black Jack Group|63832|6|Mentioned|p131 fig 2, p136|Lopingian|Guadalupian|Of Gunnedah Basin. Final (P4) Paleozoic glaciation, but basal strata show no dispersed gravel or other glacial indicators, suggesting a brief interglacial interval in the mid-Permian.||||||
1798|Black Jack Group|64631|5|Briefly described|p44 Fig.2.|Lopingian|Guadalupian|Gunnedah Basin. Biostratigraphic age control for base and top.||||Underlain by Watermark Formation.||
1798|Black Jack Group|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Unit in the Gunnedah Basin. Overlies the Watermark Formation.||||||22-MAR-12
1798|Black Jack Group|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Gunnedah Basin. Overlies Watermark Formation.||||||10-NOV-09
1798|Black Jack Group|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
1798|Black Jack Group|65115|6|Mentioned|Fig 2 p403|Permian|Permian|Overlies the Watermark Formation in the Gunnedah Basin.||||||
1798|Black Jack Group|65116|5|Briefly described|p444, p447, p449, Fig 2 p436|Late Permian|Late Permian|Includes Pamboola and Arkarula Formations. Probably includes Brigalow Formation, Hoskissons Coal, Benelabri Formation, Clare Sandstone, Wallala and Trinkey Formations. Overlies the Watermark Formation in the Gunnedah Basin. Includes coal measures.||||||
1798|Black Jack Group|65118|5|Briefly described|p491, Fig 2 p479|Permian|Permian|Overlies the Watermark Formation in the Gunnedah Basin.||||||
1798|Black Jack Group|66191|5|Briefly described|p485 Fig.2, p485|Late Permian|Late Permian|Gunnedah Basin. Unconformably underlies Digby Formation, overlies Watermark Formation. Contains Arkarula Sandstone. Also referred to as Black Jack Formation in text. Coal bearing, upper is conglomeratic sandstone, abundant tuff and pyroclastic detritus.||||||11-SEP-14
1798|Black Jack Group|68003|5|Briefly described|p38 Fig.3-j, p41, p42, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Correlative of Singleton Supergroup (Hunter Coalfield) and Illawarra Coal Measures (Western Coalfield). Prograding fluvio-deltaic system, fed from the New England region.|||Includes Brothers, Coogal and Nea Subgroups.|Overlies Millie Group. Is unconformably overlain by Digby Formation.||
1798|Black Jack Group|68004|5|Briefly described|p23 Table 1, p84, p142, p172, p179.|||Gunnedah Basin. Equivalent to the Singleton and Illawarra Coal Measures, Sydney Basin. Source of the majority of gas flows in drilling holes in parts of the Gunnedah Basin. See also references to Black Jack Formation (p168, p169) and Blackjack Group (p139, pp166-167).|||Includes Brothers, Coogal and Nea Subgroups.|Overlies Millie Group. Is overlain by Digby Formation.||
1798|Black Jack Group|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.||||||
1798|Black Jack Group|70791|5|Briefly described|p275-277|Lopingian|Guadalupian|Gunnedah Basin. Appears as Blackjack Group on p275.|||Brothers, Coogal, Nea Subgroups.|Is overlain unconformably by Digby Formation.|Coal measures.|
1798|Black Jack Group|70878|5|Briefly described|p712, p716-718|Permian|Permian|NW Sydney Basin. 799.64m thick in Santos Brawboy 1 well.|||Pamboola, Arkarula, Brigalow, Wallala, Trinkey Formations; Hoskissons Coal; Clare Sandstone.|Overlies Millie Group.||
1798|Black Jack Group|71890|6|Mentioned|p29, p53|Late Permian|Late Permian|Gunnedah Basin. Fossiliferous.|||||Sedimentary rocks and tuffaceous rocks.|
1798|Black Jack Group|73304|6|Mentioned|p71|||Gunnedah Basin. [Top?] boundary marks a major extinction of peat-producing plants.||||||
1812|Black Range Group|12185|5|Briefly described|map legend|Lower Devonian|Lower Devonian|Includes Sugarloaf Creek Tuff, Kirawin Shale and Mountain Creek Volcanics.||||||15-AUG-07
1812|Black Range Group|22638|6|Mentioned|p67|||Previously contained Mountain Creek Volcanics||||||
1812|Black Range Group|22768|5|Briefly described|p176,178||Lochkovian|||||||
1812|Black Range Group|22857|5|Briefly described|p176, p458 App. Tb.A1.6|Lochkovian|Lochkovian|Geological Province: Canberra-Yass Shelf.||||||
1812|Black Range Group|23898|5|Briefly described|p270 Fig.1|Early Devonian|Early Devonian|||||||
1812|Black Range Group|24005|5|Briefly described|p292 Fig.1|Early Devonian|Early Devonian| Geological Province: Lachlan Fold Belt||||||
1812|Black Range Group|24248|6|Mentioned|p54|||Unconformably overlies the Elmside Formation.||||||
1812|Black Range Group|24250|5|Briefly described|p104 Fig.1|Early Devonian|Early Devonian|||||||
1812|Black Range Group|24317|5|Briefly described|p14, p15 Fig.1|Early Devonian|Early Devonian|||||||
1812|Black Range Group|24417|4|Described|p75|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
1812|Black Range Group|29989|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
1812|Black Range Group|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
1812|Black Range Group|29993|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
1812|Black Range Group|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
1812|Black Range Group|30069|6|Mentioned|p7|||||||||
1812|Black Range Group|30731|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
1812|Black Range Group|30734|6|Mentioned|p8|||||||||
1812|Black Range Group|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
1812|Black Range Group|31161|5|Briefly described|PA7|||||||||
1812|Black Range Group|32483|4|Described|p29|||L.Dev. Table 1||||||
1812|Black Range Group|32585|5|Briefly described|p207|||||||||
1812|Black Range Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
1812|Black Range Group|32672|6|Mentioned|p673|||||||||
1812|Black Range Group|32675|6|Mentioned|p8|||Refers Brunker & Offenburg (1970)||||||
1812|Black Range Group|33325|5|Briefly described|Table 4|||||||||
1812|Black Range Group|33326|6|Mentioned|p441|||Fauna.||||||
1812|Black Range Group|33327|6|Mentioned|Fig.2|||||||||
1812|Black Range Group|33732|5|Briefly described|p112|||||||||
1812|Black Range Group|34403|6|Mentioned|p141|||||||||
1812|Black Range Group|34692|6|Mentioned|p186|||||||||
1812|Black Range Group|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
1812|Black Range Group|35386|3|Fully described|p40|||Age discussed P47||||||
1812|Black Range Group|36411|6|Mentioned|p267|||Refers Cramsie et al 1978 for redefinition.||||||
1812|Black Range Group|40328|6|Mentioned|p48|||||||||
1812|Black Range Group|42421|5|Briefly described|Fig.1 P294|||||||||
1812|Black Range Group|42577|4|Described|p25|||||||||
1812|Black Range Group|43430|14|Not recorded|p143,map p.144,p144|||||||||
1812|Black Range Group|43461|14|Not recorded|p621||Devonian|||||||
1812|Black Range Group|43479|14|Not recorded|p124||Devonian|||||||
1812|Black Range Group|43491|14|Not recorded|pV/12|Middle Devonian|Early Devonian|||||||
1812|Black Range Group|44093|5|Briefly described|p196 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
1812|Black Range Group|44936|5|Briefly described|Map Legend||Early Devonian|||||||
1812|Black Range Group|45147|6|Mentioned|M179|||||||||
1812|Black Range Group|46973|6|Mentioned|Fig.17|||||||||
1812|Black Range Group|47038|6|Mentioned|Fig.1|||||||||
1812|Black Range Group|50191|6|Mentioned|p6, 21 Fig. 1|Early Devonian|Early Devonian|||||||
1812|Black Range Group|50230|5|Briefly described|Map legend|Pragian|Lochkovian|Underlies the Murrumbidgee Group.||||||
1812|Black Range Group|50231|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Mountain Creek Volcanics, Warrangong Volcanics.||||||
1812|Black Range Group|50628|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Warrangong Volcanics.||||||
1812|Black Range Group|60008|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Sediments and/or volcanics.||||||08-JUL-04
1812|Black Range Group|60009|5|Briefly described|Map Legend|Pragian|Lochkovian|Includes: Warrangong Volcanics.||||||23-DEC-09
1812|Black Range Group|63025|5|Briefly described|p1052 Fig. 1|Devonian|Devonian|Includes the informal "Bowning Group Volcanics". Geological Province: Eastern Lachlan Orogen.||||||23-JAN-07
1812|Black Range Group|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes Waynes Knob Rhyolite, Warrangong Volcanics, Sugarloaf Creek Formation, Pilleuil Andesite, Mountain Creek Volcanics, Kirawin Formation and Sharpeningstone Conglomerate.||||||17-JUN-08
1812|Black Range Group|66197|6|Mentioned|p631 Fig.3b|||Silicic volcanics and volcaniclastics.||||||14-MAR-12
1812|Black Range Group|67820|6|Mentioned|p136 Fig.3|Devonian|Devonian|||||||
1812|Black Range Group|68592|2|Defined|p73 Tb.5, p125-6, p443, p744, p926-979|Pragian|Lochkovian|See also p429-30 Fig.89. First published by Best et al. (1964); formerly Black Range Series of Brown (1940). Later used by Brunker and Offenberg (1970); Offenberg (1974); it overlay their Derringullen Formation. The name had been replaced by Bowning Group of Link (1970, 1971); Link and Druce (1972), but was reinstated by Pogson and Baker (1974); Cramsie et al. (1978), and the name Bowning Group was "suppressed". c.4400m thick. Geochemistry detailed. Fossils are extremely rare. Three SHRIMP U-Pb zircon ages, all c.419 Ma, are considered too old due to inherited zircons. Equivalent to Bindook and Boraig Groups. Silicic volcanic rocks host minor epithermal Au-Ag-base metal, orogenic Au, and base metal and magnetite-rich skarns. Binalong, Taemas and Yass structural zones: deformation and metamorphism described. Have a close geochemical/genetic association with the plutons of the Boggy Plain Supersuite.|||Includes Pilleuil Andesite; Sharpeningstone Conglomerate; Sugarloaf Creek and Kirawin Formations; Mountain Creek and Warrangong Volcanics; and Waynes Knob Rhyolite.|Unconformably overlies Hattons Corner Group and locally Goobarragandra Volcanics (Douro Group). Is overlain conformably by Fifeshire Shale or Cavan Bluff Limestone. Is faulted against Douro Group.|See constituent units.|13-JAN-17
1812|Black Range Group|70192|5|Briefly described|Map Legend|Pragian|Lochkovian|On Yass and Boorowa 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Sharpeningstone Conglomerate, Kirawin Formation, Mountain Creek Volcanics, Pilleuil Andesite, Sugarloaf Creek Formation, Warrangong Volcanics, Waynes Knob Rhyolite.|Unconformable base. Overlain by Fifeshire Shale and Cavan Bluff Limestone (of Murrumbidgee Group).||
1812|Black Range Group|70297|5|Briefly described|map legend|Pragian|Lochkovian||||Warrangong Volcanics|||
1812|Black Range Group|70540|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Sharpeningstone Conglomerate, Kirawin Formation, Mountain Creek Volcanics, Pilleuil Andesite, Sugarloaf Creek Formation, Waynes Knob Rhyolite.||Conglomerate, sandstone, volcaniclastic sandstone, rhyolite, mudstone, limestone.|29-AUG-16
1812|Black Range Group|70545|5|Briefly described|Map Legend |Devonian|Devonian||||Includes Mountain Creek Volcanics, Warrangong Volcanics|||
1812|Black Range Group|70546|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Sharpeningstone Conglomerate, Kirawin Formation, Mountain Creek Volcanics, Pileuil Andesite, Sugarloaf Creek Formation, Waynes Knob Rhyolite|||
1812|Black Range Group|71656|4|Described|p10 Fig.1, p12 Fig.2, p31-32|Pragian|Lochkovian||||Sugarloaf Creek Formation, Kirawin Formation, Mountain Creek Volcanics, Sharpeningstone Conglomerate.|Underlies Murrumbidgee Group.||
1812|Black Range Group|71700|5|Briefly described|p23, CD|||Occurs on the Goulburn 250k map sheet. |||Includes the Sharpeningstone Conglomerate.|Overlain by the Murrumbidgee Group.||
1812|Black Range Group|73215|5|Briefly described|p994-995, p999|Early Devonian|Early Devonian|Colquhoun and Pogson (2012). Yass Syncline.|||Mountain Creek Volcanics, Waynes Knob Rhyolite, Pilleuil Andesite, Sharpeningstone Conglomerate.|Unconformably overlies Elmside Formation (Hattons Corner Group).||24-JAN-23
1837|Black Snake Creek Granite|33476|2|Defined|p68|Triassic|Permian|Permian - Triassic. See also p53.||||||10-DEC-07
1837|Black Snake Creek Granite|33766|6|Mentioned|Map legend|Triassic|Triassic|||||||
1837|Black Snake Creek Granite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
1837|Black Snake Creek Granite|43008|5|Briefly described|map legend|||||||||
1837|Black Snake Creek Granite|71628|4|Described|p11: 10-11; p19: 18-20, 25, 175|||Thomson (1976). Named after a local watercourse. Forms a roughly 3 x 2 km, poorly outcropping intrusion 13 km WSW of Drake. Geochemistry described. The c.252 Ma age determination is preliminary (unpublished, pers. comm.).|c.252 Ma (SHRIMP: Waltenberg and Blevin, 2017).|Black Snake Creek Suite.||Intrudes Postmans Creek Granodiorite (Dundee Rhyodacite) and Bungulla Monzogranite.|Grey-pink, medium-grained, porphyritic to equigranular leucogranite; finer-grained grey-pink saccharoidal marginal variant. Has transitional I-A type characteristics.|
1837|Black Snake Creek Granite|72528|4|Described|p2, p4 Tb.1.2, p78-83, p109, p127.|Lopingian|Lopingian|Magmatic crystallisation age determined. Lies northeast of Tenterfield, forming a small irregular pluton. Shown as part of the New England Orogen.|252.0+/-1.2 Ma U238/Pb206 (Pb207-corrected)|Black Snake Creek Suite||Intrudes Dundee Rhyodacite and intrudes Bungulla Monzogranite.|Dated sample is massive, pale pink, fine-grained, moderately porphyritic, leucocratic biotite monzogranite. I-type.|
1841|Black Springs Granite|23214|4|Described|p258|Carboniferous|Carboniferous|Intrudes the Adaminaby Group and Rockley Volcanics.||||||
1841|Black Springs Granite|42712|4|Described|Table1p13; Fig3p9|Carboniferous|Early Carboniferous|Variation on Black Springs Granodiorite.||||||
1841|Black Springs Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
1841|Black Springs Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
1841|Black Springs Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
1841|Black Springs Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
1863|Blackmans Creek Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Blackman's Creek Leucogranite.||||||
1863|Blackmans Creek Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith.||||||
1863|Blackmans Creek Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Yewrangara Suite.  Pink, medium- to coarse-grained, massive, equigranular, equigranular, leucocratic biotite granite.||||||
1863|Blackmans Creek Granite|67820|5|Briefly described|p136|||Strongly fractionated. Has higher mineral potential than most granitoids on the Goulburn sheet.|||||A-type granite.|
1863|Blackmans Creek Granite|68592|2|Defined|p1275, p1280-1, p1482, p1531|Early Devonian|Early Devonian|These rocks were originally included in the Bigga Granite by Hasan (1957), and later Gibson (1973) included them in his Blackmans Creek Leucogranite, which also included a large part of the Spring Road Granite. Chappell et al. (1991) first used the name Blackmans Creek Granite but still included the southern part of Spring Road Granite; they also included it in their Blackmans Creek Suite. Blevin (2011) reassigned the unit to Yewrangara Suite. Named after Blackmans Creek. Forms large tors and whalebacks on several prominent hills. Type locality described. Geochemistry and geophysical properties described. Alluvial gold adjacent to this unit is of uncertain origin.|398 +/- 6 Ma (SHRIMP U-Pb zircon: Wilde, 2001).|Unit in Yewrangara Suite.||Intrudes Bigga, Blanket Flat and Spring Road Granites.|Cream to grey, medium- to occasionally coarse-grained, massive to mildly foliated, generally equigranular, leucocratic arfvedsonite-biotite granite. A-type.|
1863|Blackmans Creek Granite|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dub. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Yewrangara Suite|||Medium-coarse grained, massive-mildy foliated, generally equigranular, leucocratic arfvedsonite-biotite granite; moderately high magnetic susceptibility.|
1863|Blackmans Creek Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Yewrangara Suite|||Medium-coarse grained, massive-mildy foliated, generally equigranular, leucocratic arfvedsonite-biotite granite; moderately high magnetic susceptibility.|
1863|Blackmans Creek Granite|71206|6|Mentioned|p373, 384|||Lachlan Fold Belt. Geochemistry graphs.||Blackmans Creek Suite.|||Aluminous A-type granite.|
1865|Blackmans Flat Conglomerate|22578|6|Mentioned|p398|||||||||
1865|Blackmans Flat Conglomerate|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Cullen Bullen Subgroup (Illawarra Coal Measures). Quartz sandstone, pebbly, coarse-grained. Max. thickness: 5m. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
1865|Blackmans Flat Conglomerate|34040|4|Described|p385|||Permian||||||
1865|Blackmans Flat Conglomerate|37093|6|Mentioned|p233|||||||||
1865|Blackmans Flat Conglomerate|39232|4|Described|p108|||||||||
1865|Blackmans Flat Conglomerate|40256|6|Mentioned|Fig.3|||||||||
1865|Blackmans Flat Conglomerate|40330|6|Mentioned|p66|||||||||
1865|Blackmans Flat Conglomerate|40332|6|Mentioned|Fig.4|||||||||
1865|Blackmans Flat Conglomerate|40806|2|Defined|p153|Permian|Permian|Prob. Permian||||||
1865|Blackmans Flat Conglomerate|42657|4|Described|p75|||||||||
1865|Blackmans Flat Conglomerate|43146|6|Mentioned|p39|||||||||
1865|Blackmans Flat Conglomerate|43194|5|Briefly described|p113|Late Permian|Late Permian|Western Coalfield, Sydney Basin. Article states that this unit is a correlative of the 'quartz rich sandstone unit' of the Black Jack Formation, Gunnedah Basin. It is not clear which sandstone unit this is (may be the 'quartz rich sequence')||||||
1865|Blackmans Flat Conglomerate|43318|14|Not recorded|opp p6||Permian|||||||
1865|Blackmans Flat Conglomerate|43320|14|Not recorded|Table 1||Permian|Part of Illawarra Coal Measure||||||
1865|Blackmans Flat Conglomerate|45090|6|Mentioned|p188|||Refers Rayner(1954)||||||
1865|Blackmans Flat Conglomerate|61315|5|Briefly described|p180|Late Permian|Late Permian|Of the lower part of Illarawarra Coal Measures. Good reservoir potential. Geological Province: Sydney Basin||||||
1869|Blacks Flat Diorite|29648|3|Fully described|p21|||||||||
1869|Blacks Flat Diorite|37529|6|Mentioned|p4|||||||||
1869|Blacks Flat Diorite|42045|4|Described|p149|||||||||
1869|Blacks Flat Diorite|42313|2|Defined|p38|Ordovician|Ordovician|||||||
1869|Blacks Flat Diorite|42314|5|Briefly described|Map|Late Ordovician|Middle Ordovician|||||||
1869|Blacks Flat Diorite|42828|5|Briefly described|Fig.2 P128|||||||||
1869|Blacks Flat Diorite|69043|4|Described|p2, p5-6, p57-62, p118|Early Silurian|Early Silurian|10km ENE of Gundagai, Tumut Trough. This age determination is older than a previous K-Ar hornblende date of 417 +/- 6 Ma (Webb, 1980): reasons are discussed.|435.8 +/- 2.1 Ma.|||Intrudes Bullawyarra Schist.|Includes quartz monzodiorite.|
1869|Blacks Flat Diorite|71040|5|Briefly described|p8 Fig.5|||Tumut Trough.|436 +/- 2 Ma (Bodorkos et al., 2013).|||||
1876|Blackwater Group|13516|5|Briefly described|p147 fig 5, p157|Late Permian|Late Permian|From Denison Trough, Bowen Basin||||Overlain gradationally by Rewan Group in Denison Trough. Diachronous boundary.||
1876|Blackwater Group|22593|6|Mentioned|Table 1|||||||||
1876|Blackwater Group|22757|4|Described|Table4,p10|||400 m thick. Conformable on Back Creek Group. Unconformably overlain by Rewan Formation||||||
1876|Blackwater Group|22857|6|Mentioned|p315 Fig. 22.8|||Geological Province: Gunnedah and Bowen Basins.||||||
1876|Blackwater Group|22865|6|Mentioned|Fig22.8p315|||||||||
1876|Blackwater Group|22973|5|Briefly described|p11 Fig.2(e)|Early Triassic|Early Triassic|||||||
1876|Blackwater Group|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
1876|Blackwater Group|22987|6|Mentioned|p299|||||||||
1876|Blackwater Group|22988|5|Briefly described|p303|||||||||
1876|Blackwater Group|22992|6|Mentioned|p329|||||||||
1876|Blackwater Group|22995|6|Mentioned|p361|||||||||
1876|Blackwater Group|23002|5|Briefly described|p417|Permian|Permian|||||||
1876|Blackwater Group|23003|5|Briefly described|p423 Table 1|Permian|Permian|||||||
1876|Blackwater Group|23004|5|Briefly described|p431 Table 1|Permian|Permian|||||||
1876|Blackwater Group|23037|6|Mentioned|Fig 3|Triassic|Late Permian|||||||
1876|Blackwater Group|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
1876|Blackwater Group|23161|5|Briefly described|p31 table4 fig11||Late Permian|||||||
1876|Blackwater Group|23356|5|Briefly described|26 Tab.2|Late Permian|Late Permian|||||||
1876|Blackwater Group|23430|5|Briefly described|p514-515|||Bowen Basin Province.||||||
1876|Blackwater Group|23444|5|Briefly described|p183|||||||||
1876|Blackwater Group|23769|4|Described|p862|Triassic|Permian|Geological Province: Bowen Basin.||||||
1876|Blackwater Group|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
1876|Blackwater Group|24071|5|Briefly described|p317 Table 1|Late Permian|Early Permian|Geological Province: Galilee Basin.||||||
1876|Blackwater Group|24077|5|Briefly described|p410 Tb. 2|Late Permian|Late Permian|Includes the Bandanna Formation.  Geological Province: Bowen Basin.||||||
1876|Blackwater Group|24093|4|Described|p177|Late Permian|Late Permian|Max. thickness: 1550m.   Geological Province: Bowen Basin.||||||
1876|Blackwater Group|24159|5|Briefly described|p147|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
1876|Blackwater Group|29387|6|Mentioned|Table 4|||||||||
1876|Blackwater Group|29409|6|Mentioned|Table 1|||Base recognised as top of Carnangarra Sandstone Member.||||||
1876|Blackwater Group|29567|6|Mentioned|p72|||Upper Permian||||||
1876|Blackwater Group|29591|5|Briefly described|p96|||||||||
1876|Blackwater Group|29721|6|Mentioned|Table 65|||||||||
1876|Blackwater Group|29727|6|Mentioned|p867|||||||||
1876|Blackwater Group|30448|6|Mentioned|p100|||||||||
1876|Blackwater Group|30450|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|30508|6|Mentioned|p85|||Seven boreholes drilled to test coal-bearing formations||||||
1876|Blackwater Group|30547|6|Mentioned|p426|||Correlation||||||
1876|Blackwater Group|30549|6|Mentioned|p26|||Upper Permian age||||||
1876|Blackwater Group|30691|4|Described|p14|||See also P21,Table 3,6. Upper Permian age||||||
1876|Blackwater Group|30692|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|30696|4|Described|Table 3|||Upper Permian age||||||
1876|Blackwater Group|30698|6|Mentioned|Map legend|Permian|Permian|||||||
1876|Blackwater Group|30699|6|Mentioned|p53|||Stratigraphy. Upper Permian age||||||
1876|Blackwater Group|30701|6|Mentioned|Map legend|Late Permian|Late Permian|||||||11-JAN-10
1876|Blackwater Group|30851|6|Mentioned|p366|||||||||
1876|Blackwater Group|30852|6|Mentioned|p171|||||||||
1876|Blackwater Group|30854|6|Mentioned|p8|||||||||
1876|Blackwater Group|30914|6|Mentioned|Map legend|Permian|Permian|||||||
1876|Blackwater Group|30915|6|Mentioned|p98|||||||||
1876|Blackwater Group|30916|6|Mentioned|p97|||||||||
1876|Blackwater Group|31079|6|Mentioned|p5|||||||||
1876|Blackwater Group|31084|6|Mentioned|p12|||See also P13, 16, 21. U. Permian||||||
1876|Blackwater Group|31087|6|Mentioned|p109|||||||||
1876|Blackwater Group|31088|6|Mentioned|p390|||||||||
1876|Blackwater Group|31115|6|Mentioned|p32|||Permian||||||
1876|Blackwater Group|31120|6|Mentioned|p148|||||||||
1876|Blackwater Group|31261|6|Mentioned|p518|||||||||
1876|Blackwater Group|31262|6|Mentioned|p3|||||||||
1876|Blackwater Group|31369|6|Mentioned|p3|||||||||
1876|Blackwater Group|31380|6|Mentioned|p131|||Refers Rigby(1972)||||||
1876|Blackwater Group|31401|6|Mentioned|Fig.1|||P30||||||
1876|Blackwater Group|31531|6|Mentioned|Table 1|||||||||
1876|Blackwater Group|31620|6|Mentioned|p87|||U.Permian||||||
1876|Blackwater Group|31656|4|Described|Table 1|||U.Permian||||||
1876|Blackwater Group|31687|6|Mentioned|p281|||Section||||||
1876|Blackwater Group|31689|6|Mentioned|p247|||Thickness data||||||
1876|Blackwater Group|31690|6|Mentioned|p37|||||||||
1876|Blackwater Group|31691|5|Briefly described|p427|||Upper Permian||||||
1876|Blackwater Group|31979|4|Described|Table 1|||See also Table 2. ?disconformable on Back Creek Group.||||||
1876|Blackwater Group|31983|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|31984|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32193|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32276|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32493|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|32520|6|Mentioned|p103|||U.Permian||||||
1876|Blackwater Group|32553|4|Described|p40|||||||||
1876|Blackwater Group|32556|4|Described|Table 3|||U.Perm.||||||
1876|Blackwater Group|32577|4|Described|p23|||Permian. See also P27-29,41||||||
1876|Blackwater Group|32689|6|Mentioned|Fig.2|||Correlation table. Refers Malone et al. (1969)||||||
1876|Blackwater Group|32797|6|Mentioned|p10|||||||||
1876|Blackwater Group|32832|6|Mentioned|p7||Permian|||||||
1876|Blackwater Group|32834|6|Mentioned|Table 3|||||||||
1876|Blackwater Group|32835|6|Mentioned|p6|||Flora||||||
1876|Blackwater Group|32840|6|Mentioned|p10|||||||||
1876|Blackwater Group|32944|6|Mentioned|p703|||||||||
1876|Blackwater Group|33078|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33079|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33086|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33090|4|Described|Table 3|||U.Perm.||||||
1876|Blackwater Group|33091|5|Briefly described|p8|||Stratigraphy||||||
1876|Blackwater Group|33092|5|Briefly described|p6|||Strat. table||||||
1876|Blackwater Group|33094|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33096|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33132|6|Mentioned|Fig. 6|||||||||
1876|Blackwater Group|33250|6|Mentioned|p140|||||||||
1876|Blackwater Group|33251|6|Mentioned|p2|||||||||
1876|Blackwater Group|33366|6|Mentioned|Fig.3|||U.Perm.||||||
1876|Blackwater Group|33368|6|Mentioned|p10|||Correl. with Bandanna Fm.||||||
1876|Blackwater Group|33390|6|Mentioned|p3|||On Table.||||||
1876|Blackwater Group|33451|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|33639|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|33640|5|Briefly described|Table 4|||||||||
1876|Blackwater Group|33646|6|Mentioned|p10|||Correlation. Palynological stage.||||||
1876|Blackwater Group|33648|6|Mentioned|p17|||Palynological division.||||||
1876|Blackwater Group|34132|6|Mentioned|p2|||Upper Permian. See also P5.||||||
1876|Blackwater Group|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
1876|Blackwater Group|34174|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|34276|6|Mentioned|p42|||||||||
1876|Blackwater Group|34314|4|Described|Table 2|||U.Permian. See PP10,12||||||
1876|Blackwater Group|34331|6|Mentioned|p458|||U.Permian||||||
1876|Blackwater Group|34389|4|Described|Table 2|||Upper Permian||||||
1876|Blackwater Group|34390|4|Described|Table 2|||Permian||||||
1876|Blackwater Group|34392|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|34408|6|Mentioned|p185|||On Table||||||
1876|Blackwater Group|34480|6|Mentioned|p489|||Upper Permian. See also P492||||||
1876|Blackwater Group|34574|6|Mentioned|p115|||||||||
1876|Blackwater Group|34613|4|Described|Table 3|||||||||
1876|Blackwater Group|35138|6|Mentioned|p15|||||||||
1876|Blackwater Group|35266|6|Mentioned|p190|||||||||
1876|Blackwater Group|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
1876|Blackwater Group|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
1876|Blackwater Group|35822|6|Mentioned|p40|||||||||
1876|Blackwater Group|35845|6|Mentioned|p86|||||||||
1876|Blackwater Group|35873|6|Mentioned|p2|||||||||
1876|Blackwater Group|35901|6|Mentioned|p1|||||||||
1876|Blackwater Group|35913|6|Mentioned|p35|||||||||
1876|Blackwater Group|35914|6|Mentioned|p8|||||||||
1876|Blackwater Group|35937|6|Mentioned|p621|||||||||
1876|Blackwater Group|35940|6|Mentioned|Fig.2|||||||||
1876|Blackwater Group|36172|6|Mentioned|Appendix|||||||||
1876|Blackwater Group|36327|6|Mentioned|p3|||||||||
1876|Blackwater Group|36472|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
1876|Blackwater Group|36570|6|Mentioned|p77|||||||||
1876|Blackwater Group|36739|6|Mentioned|p1|||||||||
1876|Blackwater Group|37065|6|Mentioned|p32|||||||||
1876|Blackwater Group|37071|5|Briefly described|p84|||||||||
1876|Blackwater Group|37072|6|Mentioned|p91|||||||||
1876|Blackwater Group|37073|6|Mentioned|p99|||||||||
1876|Blackwater Group|37075|5|Briefly described|Table 1|||||||||
1876|Blackwater Group|37076|4|Described|p120|||||||||
1876|Blackwater Group|37077|6|Mentioned|p131|||||||||
1876|Blackwater Group|37079|4|Described|p139|||||||||
1876|Blackwater Group|37080|6|Mentioned|p149|||||||||
1876|Blackwater Group|37096|6|Mentioned|p248|||||||||
1876|Blackwater Group|37400|6|Mentioned|p313|||||||||
1876|Blackwater Group|37458|6|Mentioned|p435|||||||||
1876|Blackwater Group|37565|6|Mentioned|p7|||||||||
1876|Blackwater Group|37610|5|Briefly described|p302|||||||||
1876|Blackwater Group|37612|6|Mentioned|Fig.1|||See also Fig.3 and P284.||||||
1876|Blackwater Group|37726|6|Mentioned|Fig.2|||||||||
1876|Blackwater Group|37749|6|Mentioned|p186|||||||||
1876|Blackwater Group|37804|6|Mentioned|p63|||||||||
1876|Blackwater Group|37858|6|Mentioned|p82|||||||||
1876|Blackwater Group|37859|6|Mentioned|p67|||||||||
1876|Blackwater Group|38153|6|Mentioned|p368|||||||||
1876|Blackwater Group|38365|6|Mentioned|Fig.2|||||||||
1876|Blackwater Group|38373|6|Mentioned|p613|||||||||
1876|Blackwater Group|38518|6|Mentioned|Fig.3|||||||||
1876|Blackwater Group|39212|5|Briefly described|p12|||Coal deposits. P24 gas reservoir. See also P11 & 23||||||
1876|Blackwater Group|39219|6|Mentioned|p47|||Microflora||||||
1876|Blackwater Group|39252|5|Briefly described|p20|||See aslo P26 & Fig.13||||||
1876|Blackwater Group|39261|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|39264|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|39267|6|Mentioned|p236|||||||||
1876|Blackwater Group|39268|6|Mentioned|p269|||||||||
1876|Blackwater Group|39412|6|Mentioned|p24|||||||||
1876|Blackwater Group|39445|6|Mentioned|Table 8|||||||||
1876|Blackwater Group|39494|6|Mentioned|Fig.5|||||||||
1876|Blackwater Group|40030|6|Mentioned|Fig.5|||||||||
1876|Blackwater Group|40095|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|40245|6|Mentioned|Table 2|||||||||
1876|Blackwater Group|40249|6|Mentioned|p41|||||||||
1876|Blackwater Group|40256|6|Mentioned|Fig.4|||||||||
1876|Blackwater Group|40544|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|40571|6|Mentioned|p29|||||||||
1876|Blackwater Group|40574|6|Mentioned|p4|||||||||
1876|Blackwater Group|40623|5|Briefly described|p80|||||||||
1876|Blackwater Group|40767|6|Mentioned|p17|||||||||
1876|Blackwater Group|41034|5|Briefly described|p366|||||||||
1876|Blackwater Group|41102|5|Briefly described|Mention|||||||||
1876|Blackwater Group|41159|6|Mentioned|p340|||||||||
1876|Blackwater Group|41188|5|Briefly described|p231|||Mention Fig.3||||||
1876|Blackwater Group|41191|6|Mentioned|p283|||||||||
1876|Blackwater Group|41211|6|Mentioned|p178|||||||||
1876|Blackwater Group|41246|6|Mentioned|Map legend|Permian||||||||
1876|Blackwater Group|41247|6|Mentioned|Fig.7|||||||||
1876|Blackwater Group|41290|6|Mentioned|Fig.6|||||||||
1876|Blackwater Group|41460|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|41474|6|Mentioned|p63|||||||||
1876|Blackwater Group|41475|6|Mentioned|Fig.1|||||||||
1876|Blackwater Group|42091|6|Mentioned|p284|||||||||
1876|Blackwater Group|42120|6|Mentioned|p412|||||||||
1876|Blackwater Group|42250|6|Mentioned|p31|||||||||
1876|Blackwater Group|42255|6|Mentioned|p234|||||||||
1876|Blackwater Group|42257|5|Briefly described|Table 1 P263|||||||||
1876|Blackwater Group|42259|6|Mentioned|p15|||||||||
1876|Blackwater Group|42614|6|Mentioned|p13|||Bowen Basin||||||
1876|Blackwater Group|42634|5|Briefly described|Table 2 P10|||||||||
1876|Blackwater Group|42641|6|Mentioned|p108|||||||||
1876|Blackwater Group|42701|4|Described|p68|||||||||
1876|Blackwater Group|42932|5|Briefly described|Fig.15|||||||||
1876|Blackwater Group|43000|5|Briefly described|p108|||||||||
1876|Blackwater Group|43002|5|Briefly described|Fig.2,p135|||||||||
1876|Blackwater Group|43016|6|Mentioned|p366|||||||||
1876|Blackwater Group|43017|5|Briefly described|Fig.2,p374|||||||||
1876|Blackwater Group|43185|6|Mentioned|13||Permian|||||||
1876|Blackwater Group|43474|14|Not recorded|fig.1,opp.p6||Kazanian|||||||
1876|Blackwater Group|43714|5|Briefly described|p8||Late Permian|||||||
1876|Blackwater Group|43982|14|Not recorded|Map Legend|||||||||
1876|Blackwater Group|43988|14|Not recorded|Map Legend||Permian|||||||
1876|Blackwater Group|43989|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|43990|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|43994|14|Not recorded|Map Legend||Late Permian|Includes Gyranda Formation.||||||
1876|Blackwater Group|43998|4|Described|p12,13,18,map||Late Permian|= Upper Bowen Coal Measures.||||||
1876|Blackwater Group|44022|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|44023|4|Described|Tb.2,p7||Late Permian|||||||
1876|Blackwater Group|44172|14|Not recorded|Tb.1,p1325||Tatarian|Ref. to BMR 1964. Equivalent of Bandanna Formation.||||||
1876|Blackwater Group|44245|5|Briefly described|Map Legend||Permian|||||||
1876|Blackwater Group|44331|14|Not recorded|Map Legend||Late Permian|||||||
1876|Blackwater Group|44337|5|Briefly described|Map Legend||Late Permian|Lithology.||||||
1876|Blackwater Group|44390|14|Not recorded|p6,13||Permian|||||||
1876|Blackwater Group|44419|14|Not recorded|p272,273,275||Permian|||||||
1876|Blackwater Group|44421|14|Not recorded|p10||Permian|||||||
1876|Blackwater Group|44424|14|Not recorded|p293-301|||Overlies Blenheim Subgroup.||||||
1876|Blackwater Group|44618|14|Not recorded|p511||Permian|Ref. to Malone et al.1965. Includes: Rangal Coal Measures, Burngrove and Fairhill Formations.||||||
1876|Blackwater Group|44630|14|Not recorded|p494,496|||||||||
1876|Blackwater Group|44639|14|Not recorded|p56|||||||||
1876|Blackwater Group|44721|14|Not recorded|p28-36||Late Permian|||||||
1876|Blackwater Group|44814|14|Not recorded|p483|||Overlies Artinskian-Kazanian faunas.||||||
1876|Blackwater Group|45031|14|Not recorded|p6,9||Permian|||||||
1876|Blackwater Group|45071|3|Fully described|p63|||See also Table 12||||||
1876|Blackwater Group|45073|6|Mentioned|p58|||Geological history||||||
1876|Blackwater Group|45095|4|Described|p8|||||||||
1876|Blackwater Group|45110|3|Fully described|Table 14|||See also p24 and Fig.5.||||||18-JUN-09
1876|Blackwater Group|45151|5|Briefly described|Table 10|||See also Table 11 & P15. Contains part of former Upper Bowen C.M.||||||
1876|Blackwater Group|48898|2|Defined|p43|Late Permian|Late Permian|Previously Upper Bowen Beds. See also pp46,47 etc.||||||18-JUN-09
1876|Blackwater Group|48900|2|Defined|p40|Late Permian|Late Permian|||||||
1876|Blackwater Group|48919|5|Briefly described|p19|||U.Permian||||||
1876|Blackwater Group|48920|3|Fully described|p29|||Upper Permian age. See also palynology on p88.||||||18-JUN-09
1876|Blackwater Group|48922|4|Described|p22|||||||||
1876|Blackwater Group|48947|5|Briefly described|p8|||||||||
1876|Blackwater Group|48995|6|Mentioned|p37|||See also Fig.3.||||||
1876|Blackwater Group|49644|5|Briefly described|Table|||||||||
1876|Blackwater Group|50273|5|Briefly described|Map legend|Early Permian|Early Permian|Comprises Gyranda Subgroup and Baralaba Coal Measures.||||||18-MAY-04
1876|Blackwater Group|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Includes: Gyranda Subgroup, Barabala Coal Measures.||||||
1876|Blackwater Group|60282|5|Briefly described|p7|||Geological Province: Bowen Basin.||||||
1876|Blackwater Group|60472|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Includes: Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||||||
1876|Blackwater Group|60659|5|Briefly described|p20-21|Late Permian|Late Permian|Includes: Moranbah, Fort Cooper and Rangal Coal Measures. Terrestrial sediments including coal measures. Geological Province: Bowen Basin.||||||07-FEB-11
1876|Blackwater Group|61035|6|Mentioned|p16|||Geological Province: Bowen Basin. Consists of  feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashtone and cherty mudstone, carbonaceous mudstone and coal. Plant and wood fossils are common.||||||07-FEB-11
1876|Blackwater Group|61377|5|Briefly described|p149 Fig. SU8, p157-158|||Includes the Kianga Formation. See also Blackwater Formation (misspelling?). Shales and coals of this unit are rich in total organic carbon. Geological Province: Bowen and Surat Basins.||||||07-FEB-11
1876|Blackwater Group|62921|5|Briefly described|p878 Fig.2, p882-883|Changhsingian|Permian|Bowen Basin. |||Includes Black Alley Shale, Betts Creek Beds and Bandanna Formation.|Is overlain unconformably by Rewan Group but conformably by Rewan Formation.||
1876|Blackwater Group|64197|6|Mentioned|p630 Fig.7|Permian|Permian|||||Underlies the Rewan Group; overlies the Back Creek Group.||
1876|Blackwater Group|64856|6|Mentioned|p61|||| | ||||31-JAN-13
1876|Blackwater Group|64859|6|Mentioned|p195|Permian|Permian|||||||
1876|Blackwater Group|65119|5|Briefly described|p513, 526, Fig 2, 4-5,7-12,16-19|Late Permian|Late Permian|Bowen Basin. Interbedded carbon siltstone and shale, tuff, sandstone and coal. Marine, up to 1080m thick. Age: 248-251 Ma. Fission Track ages ~59-77 Ma. Present in the Cockatoo Creek Well. See also Black Water Group p504.||||||08-MAY-13
1876|Blackwater Group|65388|5|Briefly described|p193-202, p159, 191|Late Permian|Late Permian|Bowen Basin. The Blackwater Group (Mollan and others, 1969) is the succession of non-marine sediments recognised throughout the Bowen Basin between the marine Back Creek Group and the Rewan Formation (now Group), and earlier known as the Upper Bowen Coal Measures. Includes Moranbah Coal Measures.||||||
1876|Blackwater Group|65706|4|Described|p12, p16 Tb.1, p18 Tb.1|Late Permian|Late Permian|Bowen Basin. Lacustrine, fluvial and paludal sediments.||||Conformably overlies Back Creek Group; conformably underlies Rewan Group.|Feldspathic and lithic sandstone, quartzose sandstone, silty sandstone, calcareous sandstone, cherty mudstone, carbonaceous shale, coal, pebble and cobble conglomerate, tuff with commonly abundant plant fossils and fossil wood.|
1876|Blackwater Group|66086|5|Briefly described|Map legend|Permian|Permian|Includes Moranbah and Fort Cooper Coal Measures.||||||
1876|Blackwater Group|66615|6|Mentioned|p6|||In contact with the Moolayember Formation.||||||
1876|Blackwater Group|67133|6|Mentioned|p20-21|||||||Is overlain by Precipice Sandstone.||
1876|Blackwater Group|67402|5|Briefly described|p80, p82 fig BWN4, p84|Late Permian|Late Permian||||Includes the Moranbah Coal Measures, Fort Cooper Coal Measures and Rangal Coal Measures.||Coal deposits.|
1876|Blackwater Group|68003|6|Mentioned|p57 Fig.3-n.|||Bowen Basin.||||Overlies Back Creek Group. Is unconformably overlain by Rewan Group and Wandoan Formation.||
1876|Blackwater Group|68202|6|Mentioned|p176|Permian|Permian|Bowen Basin.|||Rangal Coal Measures.|||
1876|Blackwater Group|68279|6|Mentioned|p18|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
1876|Blackwater Group|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin||||Unconformably overlain by the Rewan Formation. Unconformably underlain by the Black Alley Shale.|Feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashstone and cherty mudstone, carbonaceous mudstone, and coal; commonly abundant plant fossils and fossil wood.|
1876|Blackwater Group|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.||||Underlain by the Black Alley Shale, Back Creek Group.|Feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashstone and cherty mudstone, carbonaceous mudstone and coal; commonly abundant plant fossils and fossil wood.|
1876|Blackwater Group|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Bowen Basin.||||Conformably overlies Back Creek Group. Is overlain conformably by Rewan Group.||
1876|Blackwater Group|68679|5|Briefly described|p312-313, p347, p353, p364|Permian|Permian|See also p373-374 Figs.5.66-68. Northern New England Orogen.|||Moranbah, Fort Cooper, Rangal, Coal Measures.|Overlies Back Creek Group.||
1876|Blackwater Group|68731|6|Mentioned|p173 Fig 3.85|||||||||
1876|Blackwater Group|68901|6|Mentioned|p2 Fig. i|Permian|Permian|||||||26-SEP-18
1876|Blackwater Group|69379|5|Briefly described|map legend|Permian|Permian||||||Feldspathic and lithic sandstone, silty sandstone, calcareous sandstone, ashstone and cherty mudstone, carbonaceous mudstone and coal; commonly abundant plant fossils and fossil wood|
1876|Blackwater Group|69681|6|Mentioned|p83 Fig.7|||Mineralogy and likely chemical changes from CO2 injection discussed.||||||
1876|Blackwater Group|69952|6|Mentioned|p85|Permian|Permian|||||||
1876|Blackwater Group|70330|6|Mentioned|p11|Late Permian|Late Permian|Bowen Basin.|||Moranbah, Fort Cooper, Rangal, Coal Measures.|||
1876|Blackwater Group|70673|6|Mentioned|p9|Permian|Permian|||||||
1876|Blackwater Group|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Bowen Basin.|||Includes Burngrove Formation.|||
1876|Blackwater Group|70857|5|Briefly described|Map Legend|Permian|Permian|||||Overlies Back Creek Group||
1876|Blackwater Group|70861|6|Mentioned|p37|Late Permian|Late Permian|Of Bowen Basin. |||Includes Rangal, Fort Cooper and Moranbah CM, Bandana, Burngrove, Fair Hill, Macmillan, German Creek and Peawaddy fms, Black Alley Shale, Kaloola Member.|||
1876|Blackwater Group|70940|5|Briefly described|p843-844|Permian|Permian|Bowen Basin. Late Permian.|||Moranbah, Fort Cooper, Rangal, Baralaba Coal Measures; Tinowon, Bandana, German Creek, MacMillan, Fair Hill, Burngrove, Flat Top, Gyranda Formations; Black Alley Shale; Kaloola Member.|||
1876|Blackwater Group|71264|6|Mentioned|p581 Fig.4|Permian|Permian|Bowen Basin.||||||
1876|Blackwater Group|71276|5|Briefly described|p285, p292|Permian|Permian|Mollan et al. (1969); previously the upper part of the Cheshire Formation of Schneeberger (1952). Type locality on the western side of Springsure Shelf, Galilee Basin. Use of this name is stated to have diminished in the Galilee Basin generally in favour of Bandanna Formation.|||Bandanna Formation,|Overlies Black Alley Shale.|Coal-bearing.|
1876|Blackwater Group|73036|5|Briefly described|Map legend|Late Permian|Late Permian||||Includes Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73037|5|Briefly described|Map legend|Late Permian|Late Permian||||Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone. Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73038|5|Briefly described|Map legend|Late Permian|Late Permian||||Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73040|5|Briefly described|Map legend|Late Permian|Late Permian||||Rangal Coal Measures, Fort Cooper Coal Measures, Moranbah Coal Measures.||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Labile sandstone, siltstone, mudstone, coal, conglomerate.|
1876|Blackwater Group|73246|6|Mentioned|p189-190|Upper Permian|Upper Permian|Bowen Basin. Contains major coal measures.|||Moranbah, Fort Cooper, and Rangal coal measures, Yarrabee Tuff, Burngrove Formation, Fair Hill Formation|Underlain by Back Creek Group including Exmoor Formation and German Creek Formation of Blenheim Subgroup. Overlain by Rewan Group.|Sandstone, siltstone, and coal seams.|
1876|Blackwater Group|73304|6|Mentioned|p72|||Bowen Basin.||||||
1876|Blackwater Group|73305|6|Mentioned|p547-548, p560|Late Permian|Late Permian|Bowen Basin. Stratigraphy varies across the basin reflecting periods of rifting and thermal subsidence that controlled sedimentation and relative sea level.|||Fort Cooper Coal Measures|||
1876|Blackwater Group|73472|6|Mentioned|p129|Permian|Permian|Bowen Basin. Includes at least three distinct tuff units.|||Platypus Tuff, Yarrabee Tuff, Black Alley Shale Tuff|||
1918|Blanchetown Clay|2967|5|Briefly described|p14, 48-53, 74, 155, 159, 166, 169, 205|Pleistocene|Pliocene|Firman (1965). Western Murray Basin. Up to 34m thick. See also p207, 280, 283, 285, 304, 318, 322, 327, 331, 333-334.||||Is separated from the underlying Parilla Sand by the Karoonda Surface. Is overlain locally by Tyrrell Beds.|Lacustrine sequence of olive-grey clay, silt and minor interbedded fine sand.|
1918|Blanchetown Clay|10010|5|Briefly described|p12 Fig. 3, p16|Pleistocene|Pleistocene|Fine-grained lacustrine deposits of Lake Bungunnia. Geological Province: Murray Basin.||||||13-AUG-07
1918|Blanchetown Clay|22773|5|Briefly described|Fig24.8p352|Early Pleistocene|Late Pliocene|||||||
1918|Blanchetown Clay|22799|2|Defined|p39|Late Pliocene|Late Pliocene|||||||
1918|Blanchetown Clay|22857|5|Briefly described|p352 Fig. 24.8|Early Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|22887|5|Briefly described|Fig.6 p13||Late Pliocene|||||||
1918|Blanchetown Clay|22893|3|Fully described|p52 table3||Pleistocene|Generally 2-5m thick, up to 20m.||||||
1918|Blanchetown Clay|22941|6|Mentioned|p289|||||||||
1918|Blanchetown Clay|23089|5|Briefly described|p649|||||||||
1918|Blanchetown Clay|23560|6|Mentioned|p165|||||||||
1918|Blanchetown Clay|23818|5|Briefly described|p210, p212 Fig.108|Middle Pleistocene|Early Pleistocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|23884|6|Mentioned|p153|||Geological Province: Murray Basin||||||
1918|Blanchetown Clay|24043|5|Briefly described|p525|||||||||
1918|Blanchetown Clay|24465|5|Briefly described|p351 Fig.1|Quaternary|Quaternary|||||||
1918|Blanchetown Clay|24566|5|Briefly described|p114|Pliocene|Pliocene|||||||
1918|Blanchetown Clay|24574|6|Mentioned|p706|||Geological Province: Murray Basin||||||
1918|Blanchetown Clay|29591|6|Mentioned|Table 20|||||||||
1918|Blanchetown Clay|29697|5|Briefly described|Table 1|||||||||
1918|Blanchetown Clay|30145|6|Mentioned|p183|||||||||
1918|Blanchetown Clay|30750|6|Mentioned|p1|||Pleistocene age||||||
1918|Blanchetown Clay|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|30753|4|Described|p15|||Lower Pleistocene age||||||
1918|Blanchetown Clay|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See also P22,23,31,41,42||||||
1918|Blanchetown Clay|30755|6|Mentioned|p169|||Tectonic map.||||||
1918|Blanchetown Clay|30758|6|Mentioned|p66|||Stratigraphy||||||
1918|Blanchetown Clay|30807|6|Mentioned|p101|||Suggested map symbol.||||||
1918|Blanchetown Clay|30935|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|30994|6|Mentioned|Fig. 1|||||||||
1918|Blanchetown Clay|30996|3|Fully described|p32|||Contains dolomite & limestone members.||||||03-FEB-09
1918|Blanchetown Clay|31240|5|Briefly described|p64|||Pleistocene||||||
1918|Blanchetown Clay|31319|5|Briefly described|p157|||Pleistocene||||||
1918|Blanchetown Clay|31345|6|Mentioned|p294|||||||||
1918|Blanchetown Clay|31554|6|Mentioned|p14|||||||||
1918|Blanchetown Clay|31741|6|Mentioned|p6|||||||||
1918|Blanchetown Clay|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|32007|4|Described|p159|||Palaeontology fully discussed||||||
1918|Blanchetown Clay|32099|6|Mentioned|p229|||||||||
1918|Blanchetown Clay|32323|6|Mentioned|p9|||Pleistocene||||||
1918|Blanchetown Clay|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
1918|Blanchetown Clay|32432|6|Mentioned|Fig.2|||See also Table 1||||||
1918|Blanchetown Clay|32433|6|Mentioned|p80|||See also Table 2||||||
1918|Blanchetown Clay|32439|6|Mentioned|p99|||||||||
1918|Blanchetown Clay|32861|5|Briefly described|Table 1|||Lithology||||||
1918|Blanchetown Clay|32862|5|Briefly described|Table 3|||Pleistocene||||||
1918|Blanchetown Clay|32864|6|Mentioned|Fig. 5|||||||||
1918|Blanchetown Clay|33048|6|Mentioned|p195|||See also P196||||||
1918|Blanchetown Clay|33051|6|Mentioned|p187|||||||||
1918|Blanchetown Clay|33725|6|Mentioned|p10|||Small sinkholes.||||||
1918|Blanchetown Clay|33826|6|Mentioned|p42|||Strat. table||||||
1918|Blanchetown Clay|34069|6|Mentioned|p1|||See also Fig.2. Pleist.||||||
1918|Blanchetown Clay|34114|4|Described|p50|||Pleistocene||||||
1918|Blanchetown Clay|34180|6|Mentioned|p212|||Lower - Middle Pleistocene.||||||
1918|Blanchetown Clay|34459|4|Described|p11|||||||||
1918|Blanchetown Clay|34460|4|Described|p164|||Lithology. Table 2||||||
1918|Blanchetown Clay|34461|5|Briefly described|p49|||Pleistocene||||||
1918|Blanchetown Clay|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|34690|6|Mentioned|p1|||||||||
1918|Blanchetown Clay|34758|6|Mentioned|p27|||||||||
1918|Blanchetown Clay|34933|6|Mentioned|p58|||||||||
1918|Blanchetown Clay|35029|6|Mentioned|p166|||||||||
1918|Blanchetown Clay|35071|6|Mentioned|Fig.4|||||||||
1918|Blanchetown Clay|35097|6|Mentioned|Fig.4|||||||||
1918|Blanchetown Clay|35131|6|Mentioned|p8|||||||||
1918|Blanchetown Clay|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1918|Blanchetown Clay|35232|5|Briefly described|Table.4|||||||||
1918|Blanchetown Clay|35272|4|Described|p283|||||||||
1918|Blanchetown Clay|35541|6|Mentioned|p13|||||||||
1918|Blanchetown Clay|37619|6|Mentioned|p2|||||||||
1918|Blanchetown Clay|37661|6|Mentioned|p8.2.1|||||||||
1918|Blanchetown Clay|37796|6|Mentioned|p161|||||||||
1918|Blanchetown Clay|37873|4|Described|p2|||||||||
1918|Blanchetown Clay|38068|6|Mentioned|p76|||||||||
1918|Blanchetown Clay|38605|6|Mentioned|p30|||||||||
1918|Blanchetown Clay|39322|6|Mentioned|p404|||||||||
1918|Blanchetown Clay|39329|6|Mentioned|Fig.1|||||||||
1918|Blanchetown Clay|40003|6|Mentioned|Table 8|||||||||
1918|Blanchetown Clay|40215|6|Mentioned|p56|||||||||
1918|Blanchetown Clay|40380|6|Mentioned|p221|||||||||
1918|Blanchetown Clay|40597|6|Mentioned|Fig.3|||||||||
1918|Blanchetown Clay|40779|6|Mentioned|Fig.2|||||||||
1918|Blanchetown Clay|40820|5|Briefly described|p141|||||||||
1918|Blanchetown Clay|41206|5|Briefly described|p370|||||||||
1918|Blanchetown Clay|41478|5|Briefly described|Table 1|||||||||
1918|Blanchetown Clay|41537|6|Mentioned|p350|||||||||
1918|Blanchetown Clay|41848|4|Described|p358|||Includes Bungunnia Limestone and Irymple Member. Age: Pleistocene.||||||20-OCT-08
1918|Blanchetown Clay|41868|6|Mentioned|p552|||||||||
1918|Blanchetown Clay|42125|5|Briefly described|p139|||||||||
1918|Blanchetown Clay|42130|6|Mentioned|Fig.3 P265|||||||||
1918|Blanchetown Clay|42131|5|Briefly described|p287|||||||||
1918|Blanchetown Clay|42132|6|Mentioned|p295|||||||||
1918|Blanchetown Clay|42134|6|Mentioned|Fig.3 P335|||||||||
1918|Blanchetown Clay|42137|6|Mentioned|Fig.2 P368|||||||||
1918|Blanchetown Clay|42389|5|Briefly described|p71|||||||||
1918|Blanchetown Clay|42443|6|Mentioned|p4|||||||||
1918|Blanchetown Clay|42499|5|Briefly described|Map legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|42509|5|Briefly described|p2|||||||||
1918|Blanchetown Clay|42510|5|Briefly described|p35|||||||||
1918|Blanchetown Clay|42512|6|Mentioned|p68|||||||||
1918|Blanchetown Clay|42513|6|Mentioned|p98|(IV) A||||||||13-MAY-13
1918|Blanchetown Clay|42514|6|Mentioned|p116|||||||||
1918|Blanchetown Clay|42515|6|Mentioned|p134|||||||||
1918|Blanchetown Clay|42516|6|Mentioned|p152|||||||||
1918|Blanchetown Clay|42518|5|Briefly described|p185|||||||||
1918|Blanchetown Clay|42519|6|Mentioned|p205|||||||||
1918|Blanchetown Clay|42592|6|Mentioned|p280|||||||||
1918|Blanchetown Clay|42717|5|Briefly described|map legend|Pleistocene||||||||
1918|Blanchetown Clay|42720|5|Briefly described|map legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|42813|5|Briefly described|p25|||||||||
1918|Blanchetown Clay|42827|4|Described|p358|||||||||
1918|Blanchetown Clay|42867|6|Mentioned|p13|||||||||
1918|Blanchetown Clay|42881|4|Described|Fig.3, P84|||||||||
1918|Blanchetown Clay|42966|1|Redefined|p205|Early Pleistocene|Late Pliocene|||||||
1918|Blanchetown Clay|43052|5|Briefly described|Table 2.1|||||||||
1918|Blanchetown Clay|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Sandy clay. Overlain by Bungunnia Limestone.||||||25-MAY-05
1918|Blanchetown Clay|43073|5|Briefly described|p17,Table 4|||||||||
1918|Blanchetown Clay|43258|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
1918|Blanchetown Clay|43298|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
1918|Blanchetown Clay|43655|5|Briefly described|p40-846|||||||||
1918|Blanchetown Clay|43669|4|Described|p8-9|||||||||
1918|Blanchetown Clay|43682|6|Mentioned|p289|||||||||
1918|Blanchetown Clay|43791|6|Mentioned|p372, Fig1|||||||||
1918|Blanchetown Clay|43804|6|Mentioned|Fig.2,p49|||||||||
1918|Blanchetown Clay|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Interfingers with Chowilla Sand. Thickness: 20m. Geological Province: Murray Basin. ||||||
1918|Blanchetown Clay|44188|5|Briefly described|Map Legend|Pleistocene|Pliocene|Geological province: Murray Basin. Lacustrine deposits - poorly cosolidated to friable, well-laminated, green-grey, red-brown clay; silty, sandy, calcareous and gypsiferous.||||||03-FEB-09
1918|Blanchetown Clay|44191|5|Briefly described|Map Legend|Late Pleistocene|Early Pleistocene|||||||
1918|Blanchetown Clay|49038|4|Described|Table 2|||Briefly described p32.||||||20-OCT-08
1918|Blanchetown Clay|49040|6|Mentioned|p12|||||||||
1918|Blanchetown Clay|60005|5|Briefly described|Map legend|Pleistocene|Pleistocene|Fluvial: clayey sand, sandstone, sand.||||||11-JAN-10
1918|Blanchetown Clay|60540|5|Briefly described|p1000 Fig.2,p1000,p1009 Fig.5,|Pleistocene|Pliocene||||||Lacustrine clay.|
1918|Blanchetown Clay|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Sandy clay. Overlain by: Bungunnia Limestone.||||||
1918|Blanchetown Clay|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Sandy clay. Underlies Bungunnia Limestone.||||||01-JUN-05
1918|Blanchetown Clay|61155|5|Briefly described|p18|Late Pliocene|Late Pliocene|Overlies Loxton-Parilla Sands in central area of basin. Variably overlain by Monoman Formation, Lowen Sand, Woorinen Formation and Shepparton Formation. Age: ~2.0Ma. Geological Province: Murray Basin.||||||03-MAR-10
1918|Blanchetown Clay|61207|5|Briefly described|p280 Fig. 2|Pleistocene|Late Pliocene|Lacustrine sediments. Overlies Loxton-Parilla Sands. Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Lacustrine clays. Geological Province: western Murray Basin.||||||
1918|Blanchetown Clay|61822|5|Briefly described|p107|Pleistocene|Pleistocene|Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|61964|5|Briefly described|p161|||Overlies the Pliocene "Karoonda surface". Geological Province: Murray Basin.||||||
1918|Blanchetown Clay|63887|5|Briefly described|p20, p21 Fig. 1|Pleistocene|Late Miocene|Deposited in fluvio-lacustrine environment, within a shallow lake.||||||
1918|Blanchetown Clay|63893|5|Briefly described|p191, p185, p184|||Fluvial. With Loxton-Parilla Sands, underlies lowest units of Shepparton Formation. With Loxton-Parilla Sands, underlies bentonite deposits. Geol Prov: Murray Basin.||||||
1918|Blanchetown Clay|64961|5|Briefly described|p259|Quaternary|Quaternary|First formally defined by Firman (1973). Overlain by Bungunnia Limestone; unconformably overlies Karrona Surface over Loxton-Parilla Sand in central/eastern part of basin. Thickness is variable: <40m; typically 1-10m. Geol.province: Murray Basin.||||||10-NOV-10
1918|Blanchetown Clay|65552|5|Briefly described|p5 Fig.3, p6, p23 App.2|Late Pliocene|Late Pliocene|Murray Basin unit. Contains minor gypsum. Overlies Loxton Sands, Parilla Sand, Loxton-Parilla Sands and Norwest Bend Formation. Underlies surface aeolian-fluvio-lacustrine deposits (e.g. Woorinen Formation, Coonambidgal Formation, Molineaux-Lowan Sands).||||||
1918|Blanchetown Clay|65901|6|Mentioned|p181|||May be correlative with possible Pooraka Formation sediments at River Glen Marina, Murray River.||||||
1918|Blanchetown Clay|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Firman 1973.||||||
1918|Blanchetown Clay|66287|5|Briefly described|p25 Fig. 2, p28, 31,33, 42, Fig 4,5,7|Late Pliocene|Late Pliocene|Palaeomag studies on clays from base of unit constrain minimum age for underlying Loxton-Parilla Sands to between 3.4 and 2.4 Ma. Part of the Lake Bungunnia sedimentary fill.||||Overlies the Loxton-Parilla Sands in places.||20-APR-12
1918|Blanchetown Clay|67179|4|Described|p581, p584|Calabrian|Gelasian|Deposited in a large freshwater lake (Lake Bungunnia) due to damming of ancient Murray River in the Late Pliocene (Brown and Stevenson 1991, Cupper et al. 2003). Late Pliocene-Quaternary.|ca 2.4 - 1.2 Ma (McLaren et al. 2009).|||Overlies the Loxton Sand in NW Murray Basin.||28-MAY-13
1918|Blanchetown Clay|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Murray Basin.||||||
1918|Blanchetown Clay|68116|5|Briefly described|Appendix, Maps 1-11, 14.|Pleistocene|Pliocene|Early Pleistocene minimum age.|||||Laminated greenish-grey and red-brown clay and silty clay, locally calcareous and gypsiferous; minor interbedded quartz sand, ostracod sand; contains calcareous, gypsiferous and siliceous nodules.|
1918|Blanchetown Clay|68189|6|Mentioned|p27 Tb.3.2|||||||Possibly overlain by the Shepparton Formation?||
1918|Blanchetown Clay|68194|6|Mentioned|p24|Pliocene|Pliocene|Murray Basin.||Unit in Wunghnu Group.||||
1918|Blanchetown Clay|68548|5|Briefly described|p13|Pleistocene|Pliocene|Late Pliocene to Early Pleistocene.||||Is overlain by Bungunnia Limestone.|Lacustrine clays.|
1918|Blanchetown Clay|68715|6|Mentioned|p31 Fig.5|Ionian|Zanclean|Murray Basin.||||||
1918|Blanchetown Clay|68716|6|Mentioned|p39 Fig.3|||||||Overlain by the Woorinen Formation. Underlain by the Loxton Sand.||
1918|Blanchetown Clay|70718|5|Briefly described|p25, p26,  p129|Quaternary|Quaternary|Fine grained lacustrine deposits in Lake Bungunnia.||||Disconformably overlies Loxton Sand.||
1918|Blanchetown Clay|71248|2|Defined|p1,2||Pleistocene|||||||
1918|Blanchetown Clay|72445|5|Briefly described|App.7 p7 Fig.4, p7.|Quaternary|Pliocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). Described, along with Loxton-Parilla Sands, Shepparton Formation, as fluvio lacustrine.||||Shown as unconformably overlying Loxton-Parilla Sands and partially equivalent to Bungunnia Limestone.||
1918|Blanchetown Clay|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Alluvial and lacustrine clay.|
1918|Blanchetown Clay|73228|4|Described|p50-53, p55-57, p59, p62|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia. Fluviolacustrine and coastal-shallow marine depositional environments. Identified in Cooltong 1, Loxton 1 and Overland Corner 1 drillholes. Capped by Bungunnia Limestone. Ooid-rich layers are commonly found in the upper portion; these sometimes define a transitional zone with the overlying unit.||||Underlain by Loxton Sand, Bookpurnong Formation, Karoonda Surface, upper Norwest Bend Formation, and Chowilla Sand.|Poorly laminated, or occasionally very finely laminated, clays and sandy clays, and minor quartz sand.|
1918|Blanchetown Clay|73229|5|Briefly described|p66-67, p70-72, p75|Pleistocene|Late Pliocene|Murray Basin. [Analysed using pXRF; see article].|||||Includes clay, greenish grey, sandy; limestone, thin; quartz sand; clay, green-grey, mottled, sandy.|
1918|Blanchetown Clay|73496|5|Briefly described|Map legend|Pleistocene|Pleistocene|||Wunghnu Group|||Lacustrine to fluvial silty or sandy clay; nonmagnetic; moderate to high K, Th, and U where not covered by other units; occupies distinct topographic lows typically less than 60 m ASL.|
1918|Blanchetown Clay|73505|4|Described|p2, p12-13, p36|Pliocene|Pliocene|Murray Basin. Deposited in Lake Bungunnia. Basal contact is partly erosional, upper contact is conformable. Low radiometric response. No detectable magnetic response.||Wunghnu Group||Overlies Parilla Sand, Calivil Formation|Lacustrine clay.|
1926|Blanket Flat Granite|42726|5|Briefly described|map legend|Silurian||||||||
1926|Blanket Flat Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Massive to foliated porphyritic biotite soda-granite, soda-granodiorite and soda-monzonite.||||||
1926|Blanket Flat Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Cream to blue-grey, medium- to coarse-grained, massive to foliated, equigranular to porphyritic and occasionally megacrystic cordierite?-muscovite-biotite granite and minor biotite-quartz monzonite.....||||||09-SEP-08
1926|Blanket Flat Granite|68592|2|Defined|p1262-4, p1268-9, p1274, p1278-81, p1284|Late Silurian|Late Silurian|See also p1255 Fig.220, p1260, p1664. Chappell et al. (1991). These rocks had previously been included by Brunker and Offenberg (1970) in their undifferentiated Wyangala Batholith. Here assigned to the Hovells Suite on geochemical grounds. Named after Blanket Flat locality and nearby Trig Station. Type locality described. Geochemistry detailed; geophysical properties described. Not isotopically dated; is intruded by the c.398 Ma Blackmans Creek Granite. Contacts with Bigga and Spring Road Granites are sharp but lack evidence of order of intrusion.||Unit in Hovells Suite.||Intrudes Adaminaby Group. Is intruded by Bishopthorpe Suite and Blackmans Creek Granite. Abuts Spring Road Granite.|Cream to blue-grey, medium- to coarse-grained, equigranular to porphyritic and sporadically megacrystic, massive to foliated, cordierite?-muscovite-biotite granite and minor biotite-quartz monzonite. Not fractionated. S-type.|
1926|Blanket Flat Granite|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Sol. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Medium-coarse grained, equigranular to porphyritic and locally megacrystic, massive-foliated cordierite?-muscovite-biotite granite and minor biotite-quartz monzonite. Medium-high  K and Th with low-high U response; low magnetic susceptibility.|
1926|Blanket Flat Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Hovells Suite|||Medium-coarse grained, equigranular to porphyritic and locally megacrystic, massive-foliated cordierite?-muscovite-biotite granite and minor biotite-quartz monzonite. Medium-high  K and Th with low-high U response; low magnetic susceptibility.|
1934|Blaxland Granite|42726|5|Briefly described|map legend|Carboniferous||23.  Of the Hartley Suite (Bathurst Supersuite).||||||07-FEB-05
1955|Blind Gabbro|22719|6|Mentioned|p488|||||||||
1955|Blind Gabbro|22779|5|Briefly described|p 173|||||||||
1955|Blind Gabbro|22815|4|Described|p49|Early Devonian|Silurian|||||||
1955|Blind Gabbro|23439|5|Briefly described|p135|||||||||
1955|Blind Gabbro|35263|6|Mentioned|Table 3|||||||||
1955|Blind Gabbro|39721|6|Mentioned|Table 1|||||||||
1955|Blind Gabbro|41905|2|Defined|p94|Silurian||||||||
1955|Blind Gabbro|41933|5|Briefly described|Map legend|Late Silurian||||||||
1955|Blind Gabbro|43233|5|Briefly described|Map Legend|Late Silurian||of Blind Suite. Age Middle - Late Silurian.||||||
1955|Blind Gabbro|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sg3||||||
1955|Blind Gabbro|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
1955|Blind Gabbro|67060|5|Briefly described|p503 Fig.2, p505 Table 1, p507.|Devonian|Silurian|Associated with the Jindabyne Suite. Contains acicular zircons with length-parallel zoning and high U concentrations.|414.6 +/- 4.1 Ma (this study).|||||15-MAR-12
1955|Blind Gabbro|72528|5|Briefly described|p12, p108.|Lochkovian|Lochkovian||414.6+/-4.1 Ma|||||
1957|Blind Suite|22815|5|Briefly described|p49|Early Devonian|Silurian|||||||
1957|Blind Suite|41905|6|Mentioned|p90|||||||||
1957|Blind Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
1957|Blind Suite|43233|5|Briefly described|Map Legend|Late Silurian||of Kosciusko Batholith. Age Middle - Late Silurian.||||||
1968|Blow Hole Latite Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
1968|Blow Hole Latite Member|22488|5|Briefly described|p841|||||||||
1968|Blow Hole 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 Fm. and Pheasants Nest Fm. (Illawarra C.M.) together form Gerringong volcanic facies. Geological Province: Sydney Basin.||||||
1968|Blow Hole Latite Member|23442|4|Described|p169|||of Broughton Formation||||||
1968|Blow Hole Latite Member|23544|4|Described|Table 1 p360.|||also see Fig 2 p358 and p364. Of the Gerringong Volcanics in the Sydney Basin.||||||
1968|Blow Hole Latite Member|23896|3|Fully described|p249, p264 App.1|Late Permian|Late Permian|Of Broughton Formation. See also p250 Table 1.  Overlies Westley Park Sandstone Member, overlain by Kiama Sandstone Member. Geological Province: Sydney Basin. Submarine basaltic lava flow.||||||
1968|Blow Hole Latite Member|29900|6|Mentioned|Table 2|||||||||
1968|Blow Hole Latite Member|29901|4|Described|Table 1|||||||||
1968|Blow Hole Latite Member|31128|6|Mentioned|Table 1|||||||||
1968|Blow Hole Latite Member|36220|4|Described|p37|||See also Table 1.||||||
1968|Blow Hole Latite Member|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
1968|Blow Hole Latite Member|38690|4|Described|p289|||||||||
1968|Blow Hole Latite Member|40270|6|Mentioned|p177|||||||||
1968|Blow Hole Latite Member|40519|6|Mentioned|Fig.3|||||||||
1968|Blow Hole Latite Member|41832|6|Mentioned|p569|||||||||
1968|Blow Hole Latite Member|67500|5|Briefly described|p12, Tb.1, p16|Late Permian|Late Permian|Flows with columnar jointing indicate cooling on land.||Of the Broughton Formation and Gerringong volcanic facies.||Overlain by the Kiama Sandstone Member.|Three pillowed, columnar, microporphyritic flows separated by breccias.|01-MAY-12
1968|Blow Hole Latite Member|71115|5|Briefly described|p180, 182-185, 187-188, 195|Permian|Permian|Southern Sydney Basin. Sub-aqueous eruptions. Columnar jointing; local pillow structures. Paleomagnetic results tabulated, discussed.||Gerringong Volcanics.||Overlies Westley Park Latite Member. Is overlain by Kiama Sandstone Member.|Mid-grey; fine-grained groundmass with plagioclase and zeolite clusters up to 2mm in length, and chlorite-coated augite phenocrysts.|
1968|Blow Hole Latite Member|71542|4|Described|p23, 25, 26, 30, 32-35|Late Permian|Late Permian|Of southern Sydney Basin. 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. Younger flow than the Coolangatta Latite Member.Occurs between 226 and 242m elevation near the top of Mount Coolangatta.Appears as the Berry Siltstone on p30.||Unit of Gerringong Volcanics.|||Fine-grained slightly porphyritic and folaited latite.|20-OCT-21
1968|Blow Hole Latite Member|73494|5|Briefly described|p542-543|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanics.||Is overlain by Kiama Sandstone.|Shoshonitic basalt. Porphyritic (usually plagioclase); locally vesicular or amygdaloidal.|
1991|Blue Knob Basalt|22582|5|Briefly described|Fig2,p70|||Overlies Nimbin Rhyolite||||||
1991|Blue Knob Basalt|22773|5|Briefly described|p345|||||||||
1991|Blue Knob Basalt|22857|5|Briefly described|p345|Cenozoic|Cenozoic|Included in the central-volcano provinces of NSW. Max. thickness: 350m. ||||||19-NOV-08
1991|Blue Knob Basalt|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
1991|Blue Knob Basalt|30604|4|Described|p71|||||||||
1991|Blue Knob Basalt|30605|6|Mentioned|p268|||Mineralogy||||||
1991|Blue Knob Basalt|30687|6|Mentioned|p65|||Tertiary age||||||
1991|Blue Knob Basalt|31130|6|Mentioned|Fig. 2|||Correlation||||||
1991|Blue Knob Basalt|34340|6|Mentioned|Table 6.1|||||||||
1991|Blue Knob Basalt|34593|6|Mentioned|p540|||||||||
1991|Blue Knob Basalt|35050|6|Mentioned|p130|||||||||
1991|Blue Knob Basalt|35296|5|Briefly described|p14|||See also P12.||||||
1991|Blue Knob Basalt|36806|6|Mentioned|p131|||||||||
1991|Blue Knob Basalt|40896|4|Described|p9|||||||||
1991|Blue Knob Basalt|43161|4|Described|14|||||||||
1991|Blue Knob Basalt|43881|2|Defined|p6-7,49,154|||Included in MacPherson Volcanics||||||
1991|Blue Knob Basalt|44818|6|Mentioned|p275|||||||||
1991|Blue Knob Basalt|48917|6|Mentioned|p38|||Stratigraphy||||||
1991|Blue Knob Basalt|69599|5|Briefly described|p640|||Tweed volcano, centred on Mount Warning.|c.24 Ma.|||Approximate equivalent of Hobwee Basalt in QLD.||
1991|Blue Knob Basalt|73581|5|Briefly described|p6|||Tweed Volcano. Overlies Springbrook Rhyolite to the north/Nimbin Rhyolite to the south.||Lamington Volcanics, top||||
2006|Blue Waterhole Formation|22857|4|Described|p466 App.1 Tb.A1.6|Pridolian|Ludlovian|Of the Cooleman Plains Group. Bedded chert, siltstone, mudstone. Max. thickness: 600m.||||||
2006|Blue Waterhole Formation|36441|5|Briefly described|map legend|Ludlovian|Pridolian|Of Cooleman Plains Group. Siltstone, cherty siltstone, limestone and hornfels. Includes calc-silicate hornfels (Sbw1). Underlies Mountain Creek Volcanics; overlies Peppercorn Formation. BMR map code: Sbw.||||||
2006|Blue Waterhole Formation|36443|5|Briefly described|map legend|Lochkovian|Ludlovian|Of Cooleman Plains Group. Bedded chert, siltstone and mudstone. Overlies Peppercorn Formation and Pocket Formation. Interfingers with Cooleman Limestone. BMR map code: Sbw.||||||
2006|Blue Waterhole Formation|45147|2|Defined|M102|Pridolian|Ludlovian|Ludlovian to Pridolian||||||
2006|Blue Waterhole Formation|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.||||||
2017|Bluff Limestone|32483|6|Mentioned|p31|||Refers Harper (1910)||||||
2017|Bluff Limestone|32585|6|Mentioned|p210|||Refers Harper (1909)||||||
2017|Bluff Limestone|33732|6|Mentioned|p112|||||||||
2017|Bluff Limestone|34403|4|Described|p141|||||||||
2017|Bluff Limestone|34692|5|Briefly described|p186|||||||||
2017|Bluff Limestone|43526|14|Not recorded|p556,558|Middle Devonian|Early Devonian|Taemas area||||||
2046|Boambolo Formation|22857|4|Described|p460 App.1 Tb.A1.6|Late Silurian|Middle Silurian|Shale, siltstone, medium to coarse quartz sandstone. Contains gastropods, brachiopods, ostracodes, crinoids, algae. Max. thickness: 40m. Geological Province: Canberra-Yass Shelf.||||||
2046|Boambolo Formation|32675|6|Mentioned|p8|||Stratigraphic nomenclature||||||
2046|Boambolo Formation|35070|6|Mentioned|p78|||||||||
2046|Boambolo Formation|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
2046|Boambolo Formation|35386|3|Fully described|p21|||||||||
2046|Boambolo Formation|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
2046|Boambolo Formation|39507|4|Described|p170|||||||||
2046|Boambolo Formation|40328|4|Described|p92|||||||||
2046|Boambolo Formation|40689|3|Fully described|p14|||||||||
2046|Boambolo Formation|45147|6|Mentioned|M122|||||||||
2046|Boambolo Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Douro Gp. Massive shale, laminated shale with interbedded sandstone, sparsely fossiliferous, planar tabular cross-stratified quartz-feldspathic sandstone, sporadic carbonate grit- to pebble-conglomerate.||||||13-NOV-13
2046|Boambolo Formation|68592|3|Fully described|p431, p433-4, p436, p441, p472-3, p493-6|Wenlock|Wenlock|See also p428, p521. Named after the Parish of Boambolo in Murray County; first published by Pogson and Baker (1974) for the uppermost part of Glen Bower Member (Brunker and Offenberg (1970), Offenberg (1974). Type section described. Thickness to 276m. Prograding fan-delta sequence. Contains fossils, but not suitable for precise biostratigraphic dating. Probably mid-Wenlock.||Unit in Douro Group.||Unconformably overlies Connell Member (Glen Bower Formation). Is overlain unconformably by Laidlaw Volcanics.|Upward-coarsening sequence of massive siltstone, laminated shale (often interbedded with medium- to coarse-grained, calcareous quartzo-feldspathic sandstone) and granule to pebble carbonate-conglomerate.|
2046|Boambolo Formation|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdb. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Douro Group||Is overlain by Laidlaw Volcanics. Appears to overlie Connell Member (of Glen Bower Formation).|Massive siltstone and laminated shale, commonly interbedded with medium-coarse grained, well sorted, calcareous quarzofeldspathic sandstone and granule-pebble carbonate cemented conglomerate; some trough and planar cross bedding.|
2046|Boambolo Formation|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|||Massive siltstone and laminated shale, commonly interbedded with medium-coarse grained, well sorted, calcareous quarzofeldspathic sandstone and granule-pebble carbonate cemented conglomerate; some trough and planar cross bedding.|
2046|Boambolo Formation|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|||Massive siltstone and laminated shale commonly interbedded with medium-coarse grained, well sorted, calcareous quartzofeldspathic sandstone and granule-pebble carbonate cemented conglomerate; some trough and planar cross bedding.|
2046|Boambolo Formation|71656|6|Mentioned|p12 Fig.2|Wenlock|Wenlock|Shown only in correlation chart (Fig.2).||Douro Group||Overlies Yass Formation and underlies Laidlaw Volcanics.||
2046|Boambolo Formation|73215|5|Briefly described|p993-994, 1002|||Yass Syncline.||Douro Group||Overlies Hawkins Volcanics. Is overlain by Laidlaw Volcanics.||
2049|Bobadah Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Majuba Volcanics (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||
2049|Bobadah Tuff Member|35287|6|Mentioned|p7|||||||||
2049|Bobadah Tuff Member|42566|3|Fully described|p76|||||||||
2049|Bobadah Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
2060|Boco Formation|22772|4|Described|p53,64-65,Table13.1|Cryogenian|Cryogenian|||||||
2060|Boco Formation|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Wendalpa Subgroup (Poolamacca Group). Dolomite, limestone, minor sandstone, contains stromatolites. Overlain by Wilangee Basalt. See also p53, p398 App. 1 Tb.A1.3.||||||
2060|Boco Formation|30261|4|Described|Table 1|||Willouran age||||||
2060|Boco Formation|30918|6|Mentioned|p80|||||||||
2060|Boco Formation|33004|6|Mentioned|p135|||||||||
2060|Boco Formation|34812|3|Fully described|p55|||||||||
2060|Boco Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
2060|Boco Formation|35692|6|Mentioned|p23|||||||||
2060|Boco Formation|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
2060|Boco Formation|36733|6|Mentioned|Table 5|||||||||
2060|Boco Formation|37461|6|Mentioned|p335|||||||||
2060|Boco Formation|37854|6|Mentioned|Table 1|||||||||
2060|Boco Formation|37931|4|Described|p532|||||||||
2060|Boco Formation|38157|6|Mentioned|Table II|||||||||
2060|Boco Formation|39214|6|Mentioned|Table 1|||||||||
2060|Boco Formation|40294|6|Mentioned|p8|||||||||
2060|Boco Formation|41403|5|Briefly described|p50|||||||||
2060|Boco Formation|42222|5|Briefly described|p11|||||||||
2060|Boco Formation|42223|6|Mentioned|Fig.2 P36|||||||||
2060|Boco Formation|43265|5|Briefly described|Map Legend||Neoproterozoic|of Wendalpa Subgroup.||||||
2060|Boco Formation|43269|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
2060|Boco Formation|62724|5|Briefly described|p17 Fig. 4|Willouran|Willouran|Of the Poolamacca Group. Geological Province: Broken Hill Domain.||||||07-FEB-11
2060|Boco Formation|70000|5|Briefly described|p34|Neoproterozoic|Neoproterozoic|Appears as Bocco Formation on p39.||Unit in Wendalpa Subgroup.||Is overlain by Wilangee Basalt.|Stromatolitic limestone.|
2060|Boco Formation|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Wendalpa Subgroup.||Overlies Christine Judith Conglomerate. Is overlain by Wilangee Basalt.|Quartz sandstone with well-rounded grains, minor chert, localised limestone and minor stromatolites.|
2060|Boco Formation|72461|6|Mentioned|p16 fig 9|||||||||
2084|Bogandyera Granite|40328|4|Described|p202|||||||||
2084|Bogandyera Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
2084|Bogandyera Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
2084|Bogandyera Granite|45087|6|Mentioned|p29|||Chemical analyses||||||
2084|Bogandyera Granite|69801|6|Mentioned|p104|||Central Lachlan Orogen. Said to comprise the three plutons of the Munderoo Granodiorite, Bogandyera Granite and the Prison Farm Granodiorite, although GSNSW clearly recognises the Munderoo Granodiorite as a separate entity.||Mannus Creek Suite||||25-NOV-19
2087|Bogey Hole Formation|22578|6|Mentioned|p401|||||||||
2087|Bogey Hole Formation|23055|6|Mentioned|p15|||||||||
2087|Bogey Hole Formation|29922|6|Mentioned|p49|||||||||
2087|Bogey Hole Formation|29926|6|Mentioned|Fig.3|||Permian||||||
2087|Bogey Hole Formation|34351|5|Briefly described|p343|||Fig.5.13||||||
2087|Bogey Hole Formation|37083|6|Mentioned|p173|||||||||
2087|Bogey Hole Formation|39292|6|Mentioned|Fig. 6.2|||||||||
2087|Bogey Hole Formation|39308|6|Mentioned|p470|||||||||
2087|Bogey Hole Formation|39609|6|Mentioned|Table 1|||||||||
2087|Bogey Hole Formation|41479|6|Mentioned|Fig.2|||||||||
2087|Bogey Hole Formation|43344|14|Not recorded|p85 Table||Permian|Table||||||
2087|Bogey Hole Formation|43447|14|Not recorded|diag.p26,p34|||Part of Lambton Sub-Group||||||
2087|Bogey Hole Formation|43448|14|Not recorded|p224||Permian|On table only. Unit of Lambton Subgroup (of Newcastle Coal Measures)||||||
2087|Bogey Hole Formation|45090|6|Mentioned|p186|||Refers McKenzie (1962)||||||
2087|Bogey Hole Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Lambton Subgroup|Included Cockle Creek Conglomerate Member.|||
2088|Boggabri Volcanics|721|5|Briefly described|Map legend|Sakmarian|Westphalian|Rhyolitic to dacitic lavas and ashflow tuffs with interbedded shale; rare trachyte and andesite. Geological Province: Gunnedah Basin.||||||29-JAN-08
2088|Boggabri Volcanics|22572|6|Mentioned|p108|||overlain by Permian Hunter Coalfield||||||
2088|Boggabri Volcanics|22579|5|Briefly described|p219 Fig.2|Early Permian||||||||
2088|Boggabri Volcanics|22857|4|Described|p244, p504 App.1 Tb.A1.8|Early Permian|Early Permian|Interstratified felsic lava flows and ignimbrites, minor mafic lavas. Max. thickness: >775m. Geological Province: Meandarra Rift. See also p256, p312 Fig. 22.6 and p315 Fig. 22.8.||||||
2088|Boggabri Volcanics|22863|6|Mentioned|p244|||||||||
2088|Boggabri Volcanics|22864|6|Mentioned|p256,267|||||||||
2088|Boggabri Volcanics|22865|6|Mentioned|Fig22.6p312|||||||||
2088|Boggabri Volcanics|23050|5|Briefly described|p9 Fig.2|Early Permian|Early Permian|||||||
2088|Boggabri Volcanics|23102|5|Briefly described|p562|||||||||
2088|Boggabri Volcanics|23566|5|Briefly described|p116 Fig. 2|Early Permian|Early Permian|Geological Province: Gunnedah Basin||||||
2088|Boggabri Volcanics|23740|5|Briefly described|p1219|Early Permian|Late Carboniferous|Geological Province: Gunnedah Basin.||||||17-SEP-08
2088|Boggabri Volcanics|24159|5|Briefly described|p150 Fig.3, p149|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Overlying Unit: Goonbri Formation.||||||
2088|Boggabri Volcanics|24241|5|Briefly described|p19 Fig.4|Permian|Carboniferous|||||||
2088|Boggabri Volcanics|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
2088|Boggabri Volcanics|24603|5|Briefly described|p866, p870|Early Permian|Early Permian|See also p869 Fig. 4c and p874 Tb. 1.||||||
2088|Boggabri Volcanics|29870|6|Mentioned|p7|||||||||
2088|Boggabri Volcanics|30135|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
2088|Boggabri Volcanics|30910|6|Mentioned|Map legend|Permian|Carboniferous|Permo - Carboniferous||||||
2088|Boggabri Volcanics|30911|6|Mentioned|Map legend|Permian|Permian|||||||
2088|Boggabri Volcanics|31882|6|Mentioned|p243|||||||||
2088|Boggabri Volcanics|32671|6|Mentioned|Map legend|Permian|Permian|||||||
2088|Boggabri Volcanics|32672|6|Mentioned|p674|||||||||
2088|Boggabri Volcanics|32944|6|Mentioned|p700|||See also pp701,702,704. Permian||||||22-AUG-18
2088|Boggabri Volcanics|33676|6|Mentioned|Map legend|Permian|Carboniferous|Permian - Carb.||||||
2088|Boggabri Volcanics|34043|5|Briefly described|p448|||Perm. Corr. with Dalwood Gp.||||||
2088|Boggabri Volcanics|34170|6|Mentioned|p45|||Lower Permian||||||
2088|Boggabri Volcanics|34292|6|Mentioned|p25|||See also Table 1. L.Permian||||||
2088|Boggabri Volcanics|34982|6|Mentioned|p48|||||||||
2088|Boggabri Volcanics|35095|6|Mentioned|p108|||||||||
2088|Boggabri Volcanics|36042|6|Mentioned|Fig.7|||||||||
2088|Boggabri Volcanics|36940|6|Mentioned|p128|||||||||
2088|Boggabri Volcanics|37082|6|Mentioned|p160|||||||||
2088|Boggabri Volcanics|37094|5|Briefly described|p239|||||||||
2088|Boggabri Volcanics|37856|6|Mentioned|p2|||||||||
2088|Boggabri Volcanics|38089|6|Mentioned|p4|||||||||
2088|Boggabri Volcanics|38614|6|Mentioned|p5|||||||||
2088|Boggabri Volcanics|38837|6|Mentioned|p232|||||||||
2088|Boggabri Volcanics|39063|6|Mentioned|Fig.3|||||||||
2088|Boggabri Volcanics|39287|6|Mentioned|Fig. 2.2|||||||||
2088|Boggabri Volcanics|39288|6|Mentioned|Fig. 3.3|||||||||
2088|Boggabri Volcanics|39572|6|Mentioned|p141|||||||||
2088|Boggabri Volcanics|39666|6|Mentioned|p101|||||||||
2088|Boggabri Volcanics|39693|6|Mentioned|p14|||||||||
2088|Boggabri Volcanics|39833|6|Mentioned|p298|||||||||
2088|Boggabri Volcanics|39913|6|Mentioned|p2|||||||||
2088|Boggabri Volcanics|40200|4|Described|p9|||||||||
2088|Boggabri Volcanics|40246|6|Mentioned|p173|||||||||
2088|Boggabri Volcanics|40331|6|Mentioned|p5|||||||||
2088|Boggabri Volcanics|40762|6|Mentioned|p292|||||||||
2088|Boggabri Volcanics|40767|6|Mentioned|p15|||Mention Fig.4||||||
2088|Boggabri Volcanics|40952|6|Mentioned|p5|||||||||
2088|Boggabri Volcanics|41264|6|Mentioned|p251|||||||||
2088|Boggabri Volcanics|41290|6|Mentioned|p228|||||||||
2088|Boggabri Volcanics|41451|5|Briefly described|p5|||||||||
2088|Boggabri Volcanics|41461|5|Briefly described|p11|||||||||
2088|Boggabri Volcanics|41689|6|Mentioned|Table 1|||||||||
2088|Boggabri Volcanics|41990|6|Mentioned|p8|||||||||
2088|Boggabri Volcanics|42182|6|Mentioned|Table 1|||||||||
2088|Boggabri Volcanics|42284|5|Briefly described|Fig.11 P104|||||||||
2088|Boggabri Volcanics|42463|6|Mentioned|Fig.6 P173|||||||||
2088|Boggabri Volcanics|42679|6|Mentioned|Fig.3 P3|||||||||
2088|Boggabri Volcanics|42773|6|Mentioned|p350|||||||||
2088|Boggabri Volcanics|42997|5|Briefly described|p45|||||||||
2088|Boggabri Volcanics|43017|5|Briefly described|Fig.2,p374|||||||||
2088|Boggabri Volcanics|43091|5|Briefly described|Map legend|||Of Gunnedah Basin.||||||17-SEP-08
2088|Boggabri Volcanics|43194|5|Briefly described|p97, 98 Tb. 8.2, p133 App. 1|Early Permian|Early Permian|See also references on p95, p99-100, p102, p128, p129 Tb. 8.3. With Werrie Basalt, forms basement to the Gunnedah Basin. Unconformably underlies Leard and Goonbri Formations. Considered to be synonymous with 'Gunnedah Volcanics'. In this article Boggabri Volcanics is preferred.||||||
2088|Boggabri Volcanics|43405|14|Not recorded|Map Legend|Permian|Carboniferous|(Provisional Edition)||||||
2088|Boggabri Volcanics|43408|14|Not recorded|Map Legend|||Equiv.of Gunnedah Volcanics||||||
2088|Boggabri Volcanics|43409|14|Not recorded|Map Legend|||||||||
2088|Boggabri Volcanics|43410|14|Not recorded|Map Legend|Permian|Carboniferous|(Provisional Edition)||||||
2088|Boggabri Volcanics|43429|14|Not recorded|Map Legend|||||||||
2088|Boggabri Volcanics|43582|6|Mentioned|Fig.5,p16||Early Permian|||||||
2088|Boggabri Volcanics|45006|14|Not recorded|Tb.1,opp.p3|||||||||
2088|Boggabri Volcanics|50613|6|Mentioned|p224|Early Permian|Early Permian|See also p227.||||||
2088|Boggabri Volcanics|50629|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Underlies: Leard Formation.  Interfingers with: Werrie Basalt.||||||05-JUL-04
2088|Boggabri Volcanics|61313|5|Briefly described|p94 Fig. G7|Permian|Permian|Geological Province: Gunnedah Basin. See also p 104 Table G1.||||||
2088|Boggabri Volcanics|61377|5|Briefly described|p142, p148 Tb. SU1|Early Permian|Late Carboniferous|Geological Province: Gunnedah Basin. See also p149 Fig. SU8, p154 Fig. SU9.||||||07-FEB-11
2088|Boggabri Volcanics|61612|6|Mentioned|p270, p270 Fig. 1|Late Carboniferous|Late Carboniferous|Geological Province: Gunnedah Basin.||||||13-MAR-09
2088|Boggabri Volcanics|61772|6|Mentioned|p127||Early Permian|In New England Orogen.||||||27-MAY-08
2088|Boggabri Volcanics|61776|5|Briefly described|p199|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Rhyolitic to dacitic lava, breccia and tuff with minor sediments.||||||17-SEP-08
2088|Boggabri Volcanics|61791|5|Briefly described|p325, p326 Fig. 2, p327, p328|Permian|Carboniferous|||||||
2088|Boggabri Volcanics|61792|4|Described|p335-338|Early Permian|Early Permian|Geological Province: Gunnedah Basin.||||||
2088|Boggabri Volcanics|61801|6|Mentioned|p403 Fig. 1|||Extrusive to intrusive mafic to silicic igneous rocks. Age by geochemical correlation with Mount Terrible Volcanic Complex (300+/-8 Ma U-Pb SHRIMP from 18 grains Zr).|300+/-8 Ma U-Pb SHRIMP|||Correlated with Mount Terrible Volcanic Complex, Werrie Basalt||24-SEP-18
2088|Boggabri Volcanics|62357|5|Briefly described|p524 Fig. 7|Early Permian|Early Permian|Geological Province: Gunnedah Basin.||||||
2088|Boggabri Volcanics|63774|6|Mentioned|p1075|||Geological Province: Lachlan Fold Belt.||||||
2088|Boggabri Volcanics|63832|5|Briefly described|p131 fig 2|Sakmarian|Sakmarian|Of Gunnedah Basin.||||Is overlain by and interfingers with Werrie Basalt.||13-DEC-17
2088|Boggabri Volcanics|64631|6|Mentioned|p44 Fig.2.|Sakmarian|Asselian|Gunnedah Basin. Some biostratigraphic age control. Top may be time transgressive?||||Overlain by Werrie Basalt.||
2088|Boggabri Volcanics|65112|6|Mentioned|Fig 4 p314|Early Permian|Early Permian|Unit in the Gunnedah Basin. Underlies the Werrie Basalt.||||||22-MAR-12
2088|Boggabri Volcanics|65113|5|Briefly described|Fig 4 p340|Early Permian|Early Permian|Gunnedah Basin. Underlies Werrie Basalt.||||||10-NOV-09
2088|Boggabri Volcanics|65114|5|Briefly described|p383 Tb.1, p385 Fig.3, p394|Guadalupian|Cisuralian|300-?269 Ma; Tectonic unit: Gunnedah Basin; felsic volcanic rocks; considered possibly to extend down into the APP1 palynological zone||||||
2088|Boggabri Volcanics|65115|6|Mentioned|Fig 2 p403|Permian|Permian|Gunnedah Basin. Underlies the Goonbri Formation.||||||
2088|Boggabri Volcanics|65116|4|Described|p436, Fig. 2, p444, p441 Fig. 6|Early Permian|Early Permian|?Underlies the Werrie Basalt, Gunnedah Basin. Range from basalt to rhyolite along the Boggabri Ridge and western basin margin. Interbedded lacustrine and fluvial deposits are considered equivalent to the Reids Dome beds of the Denison Trough, Bowen Basin.||||||
2088|Boggabri Volcanics|65118|5|Briefly described|Fig 2 p479, p484|Permian|Permian|Gunnedah Basin.||||||
2088|Boggabri Volcanics|66191|5|Briefly described|p484 Fig.1, p485|Early Permian|Late Carboniferous|Gunnedah Basin. Basaltic and rhyolitic rift volcanics.||||||
2088|Boggabri Volcanics|67028|6|Mentioned|p371 Tb. 5|Permian|Permian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996)|260-291 Ma magnetic age range|||||24-APR-12
2088|Boggabri Volcanics|68003|5|Briefly described|p38 Fig.3-j, p40, p57 Fig.3-n, p129.|Early Permian|Early Permian|Gunnedah and Surat Basins, Brigalow Belt South Bioregion.|||||Rhyolitic to dacitic lavas and ashflow tuffs with interbedded shale.|
2088|Boggabri Volcanics|68004|5|Briefly described|p23 Table 1, p117, p177.|||Gunnedah Basin. Probably hosts the Hill 398 epithermal Au-Ag prospect. Forms basement in Boomi Trough.||||||
2088|Boggabri Volcanics|68006|5|Briefly described|p103, p165.|||Constitutes the south and central Boggabri Ridge, which separates the Maules Creek and Mullaley Sub-basins. Has deposits of Fullers earth.||||||
2088|Boggabri Volcanics|68822|6|Mentioned|p338|||Beneath the Gunnedah Basin. Show some relic supra-subduction zone component in the melt.||||||
2088|Boggabri Volcanics|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Early Permian felsic volcanic rocks: rhyolite, dacite, tuff and shale.||||||
2088|Boggabri Volcanics|70791|5|Briefly described|p275-277, p279, p281, p286-287, p292-294|Cisuralian|Cisuralian|Is assigned in this article to the Dalwood Group, "consistent with Hunter and Newcastle coalfield stratigraphy based on palynological ages and conformity relationships". Gunnedah Basin. Usually mentioned in association with Werrie Basalt. Both units are the source of sediments for Leard and Goonbri Formations.||||Is overlain by Bellata Group and Porcupine Formation, and nonconformably by Goonbri and Leard Formations.|Grey to buff-white, flow banded rhyolite lavas, unwelded to densely welded ignimbrites, and green to purple altered rhyolite and welded tuff.|
2088|Boggabri Volcanics|70878|5|Briefly described|p716|Permian|Permian|Gunnedah Basin. 15.54m thick in Santos Slacksmith 1 well.||||Is overlain by Bellata Group.||
2088|Boggabri Volcanics|71115|5|Briefly described|p191-194|Permian|Permian|Gunnedah Basin, NW Tamworth Terrane. Paleomagnetic reconnaissance work, paleomagnetic poles for c.265 Ma, and paleomagnetic reliability, discussed.|299-260 Ma.||||Flow-banded lavas and lithic tuffs.|
2088|Boggabri Volcanics|73197|5|Briefly described|p470-471, p472 Tb.2|Artinskian|Artinskian|Eastern edge of the Sydney Basin, overlies Lachlan Orogen metasedimentary rocks. Limited outcrops with description from borehole data (Leitch, 1993). U-Pb zircon age from Allen et al. (1998).|286.7 +/- 3.1 Ma U-Pb zircon||||Volcanics including extensive ignimbrites and flows.|
2088|Boggabri Volcanics|73202|5|Briefly described|p626, p39 Fig.10, p640|Early Permian|Late Carboniferous|Sydney-Gunnedah Basin, part of the basal sequences. High concentrations of high field strength incompatible elements (Brownlow and Arculus, 1999).|ca 300-269 Ma, Ca 290 Ma SHRIMP||||Siliceous volcanics.|
2091|Boggy Plain Suite|22779|6|Mentioned|p 172|||||||||
2091|Boggy Plain Suite|22815|5|Briefly described|p49|Silurian|Silurian|||||||
2091|Boggy Plain Suite|23549|5|Briefly described|p523|||Of Boggy Plain Supersuite. Consists of one pluton only - concentrically zoned from marginal diorites inwards through granodiorites to hornblende monzogranites to a central aplitic core. Geological Province: Lachlan Fold Belt.||||||28-MAY-13
2091|Boggy Plain Suite|40882|6|Mentioned|p21|||||||||
2091|Boggy Plain Suite|42726|5|Briefly described|map legend||Early Devonian|Of the Boggy Plain Supersuite.  Contains 5 'granites' units and 8 'volcanics' units.||||||08-FEB-05
2091|Boggy Plain Suite|43233|5|Briefly described|Map Legend|Late Silurian||Of the Kosciusko Batholith. Age Middle - Late Silurian.||||||06-SEP-05
2091|Boggy Plain Suite|45147|6|Mentioned|M48|||See also M191||||||
2091|Boggy Plain Suite|60503|6|Mentioned|p224, p237|||Probably misspelt and should be Boggy Plain Supersuite. ||||||
2091|Boggy Plain Suite|66575|6|Mentioned|p949,|||Kosciusko Batholith. High-temperature I-Type. Shows increase in Zr toward more evolved compositions.||||||
2091|Boggy Plain Suite|72571|6|Mentioned|p89-90|||Type example granite within the Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|22580|5|Briefly described|p94||Early Devonian|||||||
2092|Boggy Plain Supersuite|22638|6|Mentioned|p67|||||||||
2092|Boggy Plain Supersuite|22768|5|Briefly described|p157,178|||||||||
2092|Boggy Plain Supersuite|22778|4|Described|p 159|||||||||
2092|Boggy Plain Supersuite|22831|6|Mentioned|p 69|||||||||
2092|Boggy Plain Supersuite|22857|6|Mentioned|p128, p157|||||||||
2092|Boggy Plain Supersuite|22968|5|Briefly described|Fig89 P164, P207|Early Devonian|Late Silurian|||||||
2092|Boggy Plain Supersuite|22971|6|Mentioned|p 68|||||||||
2092|Boggy Plain Supersuite|23021|5|Briefly described|Map legend|Lochkovian|Lochkovian|Nonconformably and angular unconformably underlies the Mount Elizabeth Caldera Complex||||||
2092|Boggy Plain Supersuite|23028|5|Briefly described|Map legend|Lochkovian|Lochkovian|Unconformably and nonconformably underlies the Mount Elizabeth Caldera Complex||||||
2092|Boggy Plain Supersuite|23029|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
2092|Boggy Plain Supersuite|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
2092|Boggy Plain Supersuite|23214|5|Briefly described|p85|||||||||
2092|Boggy Plain Supersuite|23245|6|Mentioned|p128|||||||||
2092|Boggy Plain Supersuite|23309|5|Briefly described|p21, 345, 388, 391, 398||Early Devonian|||||||
2092|Boggy Plain Supersuite|23439|5|Briefly described|p124 fig.1|||||||||
2092|Boggy Plain Supersuite|23548|4|Described|Table 1 p532|||I-Type granites. Also see p533.||||||
2092|Boggy Plain Supersuite|23549|5|Briefly described|p517 Fig 1, p523|||Consists of a belt of granite plutons and associated volcanic complexes. Includes the Boggy Plain Suite and Nallawa Suite. I-type granite. Geological Province: Lachlan Fold Belt.||||||14-DEC-05
2092|Boggy Plain Supersuite|23551|5|Briefly described|p493 & p490|||||||||
2092|Boggy Plain Supersuite|23967|5|Briefly described|p1342|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24133|4|Described|p68|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24142|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24143|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24144|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24145|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
2092|Boggy Plain Supersuite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24222|5|Briefly described|p5|||Formed from high temperature magmas. I-type. Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24266|5|Briefly described|p1485|Early Devonian|Early Devonian|Age: 400+/-10 Ma. Geological Province: Lachlan Fold Belt.||||||07-DEC-04
2092|Boggy Plain Supersuite|24270|6|Mentioned|p1604|||Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|24417|6|Mentioned|p45|||No longer includes "Illunie Rhyolite".||||||
2092|Boggy Plain Supersuite|24512|6|Mentioned|p5|||Geological Province: Lachlan Orogen.||||||
2092|Boggy Plain Supersuite|24514|5|Briefly described|p28, p29|||Granites and volcanic rocks. Includes Mountain Creek Volcanics. Geological Province: Lachlan Fold Belt.||||||25-MAY-05
2092|Boggy Plain Supersuite|24515|5|Briefly described|p35|Paleozoic|Paleozoic|I-type granite. Geological Province: Lachlan Fold Belt.||||||07-NOV-08
2092|Boggy Plain Supersuite|24516|5|Briefly described|p39, p40|||High temperature suite. Includes felsic rhyolites. Geological Province: Lachlan Fold Belt.||||||28-MAY-13
2092|Boggy Plain Supersuite|24551|6|Mentioned|p230|||||||||
2092|Boggy Plain Supersuite|40882|4|Described|p22|||||||||
2092|Boggy Plain Supersuite|41133|4|Described|p1114|||||||||
2092|Boggy Plain Supersuite|42726|5|Briefly described|map legend||Early Devonian|Includes 15 named suites.||||||08-FEB-05
2092|Boggy Plain Supersuite|42791|5|Briefly described|p219|||||||||
2092|Boggy Plain Supersuite|42827|4|Described|p432|||||||||
2092|Boggy Plain Supersuite|44093|5|Briefly described|p93, p103, p188|Early Devonian|Silurian|See also p114.  Includes Bogong, Burrinjuck and Gocup Suites. Intrusions.||||||25-JAN-06
2092|Boggy Plain Supersuite|46524|6|Mentioned|p123|||||||||
2092|Boggy Plain Supersuite|46525|6|Mentioned|p146|||||||||
2092|Boggy Plain Supersuite|50087|6|Mentioned|p176|||Age is post-Ordovician.||||||
2092|Boggy Plain Supersuite|60267|5|Briefly described|p14|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|60423|6|Mentioned|p374|||Geological Province: Lachlan Fold Belt. ||||||
2092|Boggy Plain Supersuite|60503|4|Described|p15, p154|Early Devonian|Early Devonian|Includes several intrusions: Boebuck, Banimboola, Anglers Rest, Bingo Munjie, Post Office and Charlestown intrusions. Geological Province: Lachlan Fold Belt.||||||01-SEP-05
2092|Boggy Plain Supersuite|60504|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|60505|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|60506|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|60507|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Anglers Rest Granite, Banimboola Quartz Diorite, Boebuck Quartz Diorite, Bingo Munjie Quartz Diorite.||||||
2092|Boggy Plain Supersuite|61160|4|Described|p78, 58-59 Fig. 6.8|Early Devonian|Early Devonian|Comprises Anglers Rest Granite and Banimboola Quartz Monzodiorite. Intrusive I-type granites and volcanic rocks. Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|61161|5|Briefly described|p105, p76-77 Fig 6.1|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. I-type granitic and volcanic rocks.||||||
2092|Boggy Plain Supersuite|61163|6|Mentioned|p118|||||||||
2092|Boggy Plain Supersuite|61164|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61165|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61166|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61167|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||07-FEB-11
2092|Boggy Plain Supersuite|61168|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite and Banimboola Quartz Monzodiorite.||||||
2092|Boggy Plain Supersuite|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton.||||||07-FEB-11
2092|Boggy Plain Supersuite|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Anglers Rest Granite, Phipps Granite, Dry Gully Granodiorite, Dougs pluton and Alpine Road pluton. ||||||
2092|Boggy Plain Supersuite|61783|5|Briefly described|p296|||Geological Province: Lachlan Fold Belt.||||||
2092|Boggy Plain Supersuite|63287|6|Mentioned|p332|Early Devonian|Late Silurian|||||||07-FEB-11
2092|Boggy Plain Supersuite|63290|6|Mentioned|p405|||Is a proxy for the distribution of Ordovician subduction-related igneous rocks in the crust.||||||11-DEC-07
2092|Boggy Plain Supersuite|66713|6|Mentioned|p13|||Of Wyborn et al. (1987). Contains Yeoval Complex.||||||
2092|Boggy Plain Supersuite|67847|6|Mentioned|p79|||Benambra Terrane, Lachlan Orogen. Hosts porphyry style copper-gold mineralisation. ||||||
2092|Boggy Plain Supersuite|68592|2|Defined|p73 Tb.5,p222,p932-4,p1318-20,p1397-1465|Early Devonian|Early Devonian|Wyborn et al. (1987), after their type pluton the Boggy Plain Granitic Complex (described). Fractionated and oxidised high-temperature granites. Includes many plutons and extends 500 km from NE Victoria to Dubbo. Geochemistry detailed. Has geochemical/genetic affinities with Mountain Creek Volcanics. Geochemical differences with Gunning Suite are described. Conflicts between isotopic and palaeontological ages discussed. Thought to be comagmatic with Mountain Creek and Warrawong Volcanics. Some plutons are adjacent to mineralisation at Murringo Iron Prospect, Murringo Copper Prospect, and the Black Andrew Mine. Taemas and Yass structural zones: deformation described.|c.419-c.415 Ma.||Includes Gooramma, Karoopa, Childowla and Burrinjuck Suites.|Intrudes Black Range Group and Young Suite.|Predominantly granite to granodiorite, generally massive; several bodies also have quartz monzonite, monzodiorite and tonalitic phases; quartz monzonite, quartz monzodiorite to diorite dykes; a small gabbro intrusion. I-type.|
2092|Boggy Plain Supersuite|70297|4|Described|map legend, on side 2 of map sheet|Emsian|Emsian||||Broula Granite, Crowther Monzodiorite, Eugowra Granite, Gumble Granite, Lords Granite||Potassium-rich, oxidised I-type biotite-hornblende granite, leucogranite, monzodiorite and aplite.|18-MAY-16
2092|Boggy Plain Supersuite|70684|6|Mentioned|p11|Early Devonian|Early Devonian|Wyborn et al. (1987).||||||
2092|Boggy Plain Supersuite|71206|6|Mentioned|p379, 384-385|||Lachlan Fold Belt. Petrogenesis discussed.|||Burrinjuck, Yeoval, Jackson Granites.||I-type granite.|
2097|Bogolo Formation|22751|4|Described|p 237|||||||||
2097|Bogolo Formation|22815|4|Described|p16|Early Silurian|Ordovician|||||||
2097|Bogolo Formation|22857|4|Described|p432 App. 1 Tb. A1.5.|Early Ordovician|Late Cambrian|Of the Wagonga Group. Max. thickness: ~850m.||||||
2097|Bogolo Formation|23309|6|Mentioned|p390|||||||||
2097|Bogolo Formation|23541|6|Mentioned|Fig 1 p396|||In the Lachlan Fold Belt||||||
2097|Bogolo Formation|24339|5|Briefly described|p45|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||02-OCT-15
2097|Bogolo Formation|29992|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
2097|Bogolo Formation|29994|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
2097|Bogolo Formation|30677|6|Mentioned|p467|||||||||
2097|Bogolo Formation|31161|5|Briefly described|PA6|||See also PA9||||||
2097|Bogolo Formation|32127|6|Mentioned|p247|||Refers Wilson (1968)||||||
2097|Bogolo Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
2097|Bogolo Formation|32673|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle to Late Ordovician||||||
2097|Bogolo Formation|35118|6|Mentioned|Fig.5|||||||||
2097|Bogolo Formation|35289|3|Fully described|p5|||Definition refers Wilson 1969.||||||
2097|Bogolo Formation|36534|6|Mentioned|p223|||||||||
2097|Bogolo Formation|38223|6|Mentioned|Table 1|||||||||
2097|Bogolo Formation|40136|5|Briefly described|p18|||||||||
2097|Bogolo Formation|40646|6|Mentioned|p11|||||||||
2097|Bogolo Formation|41827|6|Mentioned|p485|||||||||
2097|Bogolo Formation|43233|5|Briefly described|Map Legend|Late Ordovician||of Wagonga Group.||||||
2097|Bogolo Formation|44093|5|Briefly described|p225 App. 1|Ordovician|Cambrian|Of Wagonga Group. Geological Province: Lachlan Fold Belt.||||||
2097|Bogolo Formation|46574|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Monaro Slope and Basin. Geological Province: Lachlan Pre-Cratonic Province.  Slate, phyllite, sandstone, chert.||||||09-NOV-04
2097|Bogolo Formation|60902|3|Fully described|p860, p863-865, p866, p880 App.1|Late Ordovician|Late Ordovician|Basal unit of Wilson's (1968) Narooma Group and overlain by Wagonga Fm. Redefined Wagonga Group now includes Bogolo Fm. Conformably overlying Narooma Chert. Characterised by basal argillite, thin beds of ??. Geological Province: Narooma Terrane.||||||02-OCT-15
2097|Bogolo Formation|61731|5|Briefly described|p1035-1040|||Geological Province: Lachlan Fold Belt/Narooma Terrane.||||||
2097|Bogolo Formation|67322|4|Described|Fig.5, p26, p27, p39|Hirnantian|Katian|Narooma Terrane. Defined by Wilson (1969), modified by Glen et al. (2004). Presumed to be Bolindian in age due to its stratigraphic relationship with the underlying Narooma Chert. The Kianga Basalt (now invalid) has been reinterpreted as blocks of basalt within the Bogolo Formation (Glen et al. 2004). Occurs in the Narooma region.||Of the Wagonga Group.||Gradationally overlies the Narooma Chert.|Argillite, conglomerate with blocks of basalt, chert and sandstone beds in an argillaceous matrix.|21-FEB-18
2097|Bogolo Formation|67849|5|Briefly described|p22, p26. |Ordovician|Cambrian|Age from Wagonga Group.||Unit in Wagonga Group.|||A block-in-matrix melange.|21-FEB-18
2097|Bogolo Formation|68255|6|Mentioned|p1061 Fig.9|||||Of the Wagonga Group||||
2097|Bogolo Formation|68309|5|Briefly described|p225-226|||Stratigraphic relations deceptive due to subduction-related thrust faulting.||Wagonga Group.||Overlies Narooma Chert.|Chaotic clast-in-matrix melange (predominantly mudstone and sandstone); interbedded silt- and sandstone; one unit (crops out at Burrewarra Point) of basaltic breccia with associated limestone clasts and beds.|
2097|Bogolo Formation|68466|5|Briefly described|p65|Late Ordovician|Late Ordovician|Narooma Terrane.||Wagonga Group.||Overlies Narooma Chert.|Argillaceous.|
2097|Bogolo Formation|68822|6|Mentioned|p335|||||||||
2097|Bogolo Formation|69668|5|Briefly described|p929 Fig.2, p932|Late Ordovician|Late Ordovician|Narooma terrane.||Unit in Wagonga Group.||Overlies Narooma Chert.|Argillaceous.|
2097|Bogolo Formation|70026|4|Described|p40,49|||Geological province: Lachlan Orogen. Contains basalt clasts in the olistostromal melange, considered to be derived from a seamount having developed in the Cambrian off the eastern margin of Gondwana (Glen et al., 2004; this study) and indicate its possible southward extent (Glen et al. 2004).||Unit of Wagonga Group.||Underlain conformably by Narooma Chert.|Mudstone and conglomerate.|
2097|Bogolo Formation|70601|4|Described|p23, p26-27, p41, p43, p46, p49-55, p57 |Early Silurian|Late Ordovician|Wilson (1969) defined this as the basal unit of the Wagonga Group at Narooma. Various models of formation of this unit are discussed. Described as a melange. The clasts and blocks in the Bogolo Formation include basaltic pillow lava, chert and blocks of quartzose turbidite, and limestone. Bolindian deposition.||Wagonga Group||All boundaries are faulted. Overlies Warbisco Shale, Narooma Chert (conformably), Numeralla Chert, Adaminaby Group. Unconformably underlies Yalmy Group. Stratigraphically equivalent to Akuna Mudstone.|Khaki-coloured, weathered, homogeneous argillite with occasional chert laminae, bedded argillite with siltstone bands, rare fine sandstone; minor conglomerate (clasts of sandstone, chert and basalt in foliated argillaceous matrix) and breccias.|
2101|Bogong Granite|22768|6|Mentioned|p178|||||||||
2101|Bogong Granite|22857|6|Mentioned|p178|Early Devonian|Early Devonian|||||||
2101|Bogong Granite|24266|6|Mentioned|p1487|||Geological Province: Lachlan Fold Belt. Of the Boggy Plain Supersuite.||||||09-MAR-05
2101|Bogong Granite|29449|6|Mentioned|p370|||Lower-Middle Devonian||||||
2101|Bogong Granite|29450|6|Mentioned|p53|||||||||
2101|Bogong Granite|29451|6|Mentioned|Fig.1|||||||||
2101|Bogong Granite|29452|6|Mentioned|p215|||Analysis P217, age 385 M.Y.||||||
2101|Bogong Granite|29454|4|Described|p11|||M.Devonian||||||
2101|Bogong Granite|29648|4|Described|p20|||||||||
2101|Bogong Granite|29682|6|Mentioned|p15|||||||||
2101|Bogong Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
2101|Bogong Granite|29994|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
2101|Bogong Granite|30678|6|Mentioned|p118|||Kinked biotite phenocrysts||||||
2101|Bogong Granite|31063|6|Mentioned|p323|||||||||
2101|Bogong Granite|31448|6|Mentioned|p19|||||||||
2101|Bogong Granite|32088|6|Mentioned|p13|||||||||
2101|Bogong Granite|33004|6|Mentioned|p192|||||||||
2101|Bogong Granite|33325|6|Mentioned|p17|||?part of Burrinjuck Gr. Complex.||||||
2101|Bogong Granite|33480|6|Mentioned|p243|||Age dating||||||
2101|Bogong Granite|33959|6|Mentioned|p234|||||||||
2101|Bogong Granite|33995|6|Mentioned|p19|||M.Dev.  See also P26.||||||
2101|Bogong Granite|34289|6|Mentioned|p38|||||||||
2101|Bogong Granite|34405|6|Mentioned|p116|||||||||
2101|Bogong Granite|34406|6|Mentioned|p222|||||||||
2101|Bogong Granite|34544|6|Mentioned|p190|||See also P194||||||
2101|Bogong Granite|35070|6|Mentioned|p107|||||||||
2101|Bogong Granite|35185|6|Mentioned|p231|||||||||
2101|Bogong Granite|35257|6|Mentioned|p152|||||||||
2101|Bogong Granite|35522|6|Mentioned|p46|||||||||
2101|Bogong Granite|37270|6|Mentioned|Table 2|||||||||
2101|Bogong Granite|37491|6|Mentioned|Fig.1|||||||||
2101|Bogong Granite|37529|6|Mentioned|p5|||||||||
2101|Bogong Granite|40328|4|Described|p203|||||||||
2101|Bogong Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
2101|Bogong Granite|40498|6|Mentioned|p368|||||||||
2101|Bogong Granite|40882|6|Mentioned|p25|||||||||
2101|Bogong Granite|41798|6|Mentioned|Fig.1|||||||||
2101|Bogong Granite|42145|4|Described|Table 1 P624|||||||||
2101|Bogong Granite|42313|2|Defined|p154|Early Devonian||||||||
2101|Bogong Granite|42314|5|Briefly described|Map|Early Devonian||||||||
2101|Bogong Granite|42726|5|Briefly described|map legend|Early Devonian||441.  Of the Bogong Suite (Boggy Plain Supersuite).||||||08-FEB-05
2101|Bogong Granite|42828|5|Briefly described|Table 1 P129|Early Devonian||||||||
2101|Bogong Granite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|glp3||||||
2101|Bogong Granite|45087|5|Briefly described|p12|||Chemical analyses||||||
2101|Bogong Granite|45147|6|Mentioned|M128|||||||||
2101|Bogong Granite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
2101|Bogong Granite|73483|6|Mentioned|p407 Fig.1|||||||||
2108|Boiling Down Sandstone Member|34080|6|Mentioned|p248|||S. extension of Tulcumba Sst.||||||
2108|Boiling Down Sandstone Member|36528|6|Mentioned|p175|||||||||
2108|Boiling Down Sandstone Member|39331|6|Mentioned|Table 10-1|||||||||
2108|Boiling Down Sandstone Member|42547|5|Briefly described|p20|||of Crook. Equivalent to Tulcumba Sandstone.||||||
2108|Boiling Down Sandstone Member|43399|2|Defined|p196,200,205||Tournaisian|||||||
2108|Boiling Down Sandstone Member|43406|14|Not recorded|p42|||Member of Goonoo Goonoo Mudstone (Parry Group)||||||
2119|Bolairo Granodiorite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Foliated contaminated granodiorite. BMR map symbol: gmi.||||||15-AUG-07
2119|Bolairo Granodiorite|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
2119|Bolairo Granodiorite|31580|6|Mentioned|Table 1-4|||Analysis||||||
2119|Bolairo Granodiorite|31581|3|Fully described|Table 1|||Analysis||||||
2119|Bolairo Granodiorite|32905|6|Mentioned|p231|||||||||
2119|Bolairo Granodiorite|32906|6|Mentioned|p239|||||||||
2119|Bolairo Granodiorite|34544|5|Briefly described|p186|||||||||
2119|Bolairo Granodiorite|36413|6|Mentioned|p77|||||||||
2119|Bolairo Granodiorite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Xenolith-rich granodiorite. S-type. BMR map code: Sma.||||||
2119|Bolairo Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
2119|Bolairo Granodiorite|40328|4|Described|p203|||||||||
2119|Bolairo Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb4.||||||
2119|Bolairo Granodiorite|45003|14|Not recorded|p55|||||||||
2119|Bolairo Granodiorite|45147|3|Fully described|M193|||See also M194||||||
2119|Bolairo Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
2134|Boloko Granodiorite|22815|4|Described|p48|Silurian|Silurian|||||||
2134|Boloko Granodiorite|33782|6|Mentioned|p109|||||||||
2134|Boloko Granodiorite|40328|4|Described|p203|||||||||
2134|Boloko Granodiorite|41905|2|Defined|p86|Silurian||||||||
2134|Boloko Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
2134|Boloko Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Ingebyrah Suite.||||||
2134|Boloko Granodiorite|72528|5|Briefly described|p11.|||||Bullenbalong Supersuite|||S-type granodiorite.|
2139|Bolton Point Conglomerate Member|29922|6|Mentioned|p49|||||||||
2139|Bolton Point Conglomerate Member|29926|6|Mentioned|Fig.3|||Permian||||||
2139|Bolton Point Conglomerate Member|33867|6|Mentioned|p11|||||||||
2139|Bolton Point Conglomerate Member|33986|6|Mentioned|p30|||Table||||||
2139|Bolton Point Conglomerate Member|34270|6|Mentioned|p254|||Separates Fassifern Coal & Awaba Claystone Member.||||||
2139|Bolton Point Conglomerate Member|34351|6|Mentioned|p348|||See also Fig.5.13||||||
2139|Bolton Point Conglomerate Member|37083|6|Mentioned|p164|||||||||
2139|Bolton Point Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
2139|Bolton Point Conglomerate Member|39308|6|Mentioned|p459|||||||||
2139|Bolton Point Conglomerate Member|39666|6|Mentioned|Table 20|||||||||
2139|Bolton Point Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
2139|Bolton Point Conglomerate Member|43447|14|Not recorded|p36,diag.p26|||Part of Moon Island Beach Sub-Group||||||
2139|Bolton Point Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Eleebana Formation||||13-JAN-15
2145|Boltons beds|22815|6|Mentioned|p18|Ordovician|Ordovician|||||||
2145|Boltons beds|22857|4|Described|p420 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Of the Kiandra Group? Quartz arenite, siltstone and shale; distal trubidite. Contains graptolites. Max. thickness: 2km. ||||||
2145|Boltons beds|23217|6|Mentioned|p3|Silurian|Silurian|In the Tantagara region - not to be confused with Bolten Formation.||||||08-MAR-06
2145|Boltons beds|23710|14|Not recorded|p69|||Correlation.||||||
2145|Boltons beds|42294|6|Mentioned|p24|||||||||
2145|Boltons beds|44092|5|Briefly described|map legend|Ordovician|Ordovician|Of1||||||
2145|Boltons beds|45147|3|Fully described|M1|||||||||
2145|Boltons beds|60078|6|Mentioned|Map Legend|Late Ordovician|Middle Ordovician|||||||
2167|Bondi Granite|22815|4|Described|p71|||||||||
2167|Bondi Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
2167|Bondi Granite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Wallagaraugh Suite.||||||
2168|Bondonga beds|22443|6|Mentioned|p863|||||||||
2168|Bondonga beds|23811|5|Briefly described|Map Legend|Sakmarian|Asselian|||||||11-JAN-10
2168|Bondonga beds|23812|5|Briefly described|p15|||||||||
2168|Bondonga beds|42378|6|Mentioned|Table 1 P9|||||||||
2168|Bondonga beds|60079|5|Briefly described|Map Legend|Permian|Early Permian|Conglomerate, sandstone, siltstone.||||||
2168|Bondonga beds|63732|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.||||||
2168|Bondonga beds|63748|4|Described|p16, p17|Early Permian|Early Permian|Fault-bounded basin remnant enclosed within the Texas beds. Unconformably overlie Texas beds. Comprise massive orthoconglomerate, paraconglomerate, lithic arenite and minor siltstone. Also mentioned: p68.||||||07-FEB-11
2168|Bondonga beds|68005|5|Briefly described|p18, p22, pp35-36, p154, p170.|Early Permian|Early Permian|New England Fold Belt. Probable folding and local overturning apparent.||||Faulted against or unconformably overlies Texas beds.|Massive orthoconglomerate, paraconglomerate, lithic sandstone and minor siltstone.|
2168|Bondonga beds|68006|6|Mentioned|p26.|Permian|Permian|Marine sediments.||||||
2168|Bondonga beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Alum Rock Conglomerate, and the Pikedale, Silver Spur and Terrica beds, are all mapped under the symbol, Par.||||||
2168|Bondonga beds|68679|5|Briefly described|p449 Fig.5.113, p451-452, p455|Permian|Permian|Occupies a linear, NW-trending fault-bounded basin remnant, from Mole valley (NSW) to N of Glen Lyon (QLD). The Queensland part is called the Glenlyon beds. Shown in a tectonic discrimination diagram (plots in the "ocean-floor" field) and a REE plot. Bedding is steeply dipping to overturned. Has early Permian marine fossils.||||Enclosed within Texas beds.|Includes massive conglomerate (with pebbles and cobbles of Texas beds), lithic sandstone and minor siltstone, pebbly mudstone and poorly fossiliferous limestone; thin, vesicular basalt with lobate probable pillow structures.|
2168|Bondonga beds|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||26-SEP-18
2168|Bondonga beds|70373|4|Described|p789-794 fig 3, p795-797 Tb 1, p798- 804|Permian|Early Permian|Shallow marine brachiopod fossils. Includes rhyolite dyke: quartz, altered K feldspar and plagioclase phenocrysts in aphanitic groundmass. Dating of detrital zircons indicates provenance from Carboniferous materials, and deposition in the Early Permian. Other ages obtained from this unit: 295+/-18 Ma 302.4+/-5.1Ma. All LA-ICP-MS on zircon. 1400m thick. Minimum age constrained by overlying Gibraltar Ignimbrite (251.6+/-3.2 Ma)|280.7+/-3 Ma  (LA-ICP-MS)|||Assumed to overlie Texas beds, contact probably faulted. Unconformably underlie Mosman Formation.Correlated with  Silver Spur, Pikedale, Terrica and Alum Rock beds. Cut by rhyolitic dyke.|Fine to coarse grained, graded and cross bedded sandstones. Massive clast and matrix supported conglomerates; clast-rich to clast poor mudstone matrix diamictite; slightly porphyritic basalt intruded.|
2168|Bondonga beds|71628|5|Briefly described|p10:3; p15:25; p17:4; p19: 110, 148, 168|Permian|Permian|Called the Silver Spur Beds by Shaw (1964).||||Is intruded by Apple Tree Gully Granodiorite, Racehorse Porphyry, Webbs Consols and Mole Leucogranites. Is faulted against Clive Leucomonzogranite and Dandahra Creek Leucosyenogranite.||
2172|Bong Bong Basalt|34434|6|Mentioned|Fig.5.25|||||||||
2172|Bong Bong Basalt|36220|4|Described|p97|||See also P95||||||
2172|Bong Bong Basalt|36221|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic||||||
2172|Bong Bong Basalt|36223|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic.||||||
2172|Bong Bong Basalt|37253|6|Mentioned|Table 1|||||||||
2172|Bong Bong Basalt|40044|6|Mentioned|p382|||||||||
2172|Bong Bong Basalt|43346|2|Defined|p5 Map|||||||||
2172|Bong Bong Basalt|43349|14|Not recorded|Map|||||||||
2172|Bong Bong Basalt|45003|14|Not recorded|p189|||||||||
2172|Bong Bong Basalt|71115|6|Mentioned|p179-180|Permian|Permian|Southern Sydney Basin.||||||
2179|Bonnie Doon Member|40664|4|Described|p242|Miocene|Miocene|||||||13-JUN-13
2179|Bonnie Doon Member|42035|4|Described|p128|||||||||
2192|Boogledie Formation|22451|6|Mentioned|p24|||||||||
2192|Boogledie Formation|22529|4|Described|4 fig 2|Middle Devonian|Middle Devonian|Parent Kandos Group||||||
2192|Boogledie Formation|22590|6|Mentioned|Fig3 P754||Eifelian|Actually spelt Boogledie Fm.||||||
2192|Boogledie Formation|22857|4|Described|p474 App.1 Tb.A1.6|Emsian|Emsian|Of the Kandos Group. Feldspathic-lithic arenite, shale, pebbly arenite and conglomerate. Max. thickness: 950m. Geological Province: Capertee Rise.||||||
2192|Boogledie Formation|23043|5|Briefly described|Map Legend|Eifelian|Eifelian|of Kandos Group.||||||11-JAN-10
2192|Boogledie Formation|23170|2|Defined|p141|Eifelian|Eifelian|of Kandos Group.||||||
2192|Boogledie Formation|24580|5|Briefly described|p828|||Unconformably overlain by the Mount Frome Group. Conformably overlies the Mount Frome Limestone. Geological Province: Eastern Lachlan Fold Belt.||||||
2192|Boogledie Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
2192|Boogledie Formation|31161|5|Briefly described|PA5|||||||||
2192|Boogledie Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
2192|Boogledie Formation|32047|6|Mentioned|Fig.1|||||||||
2192|Boogledie Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|L.-M.Dev.||||||
2192|Boogledie Formation|32619|6|Mentioned|p461|||Fauna. Late Eifelian||||||
2192|Boogledie Formation|32622|6|Mentioned|p79|||||||||
2192|Boogledie Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
2192|Boogledie Formation|32672|6|Mentioned|p673|||||||||
2192|Boogledie Formation|33326|6|Mentioned|p445|||Fauna.||||||
2192|Boogledie Formation|34713|6|Mentioned|p119|||||||||
2192|Boogledie Formation|35246|6|Mentioned|p169|||On a table.||||||
2192|Boogledie Formation|39214|5|Briefly described|p25|||||||||
2192|Boogledie Formation|39664|6|Mentioned|p93|||||||||
2192|Boogledie Formation|40131|6|Mentioned|Fig.12|||||||||
2192|Boogledie Formation|43188|4|Described|p217,Table 5 p213||Early Devonian|Formerly Melrose Formation.Contains late early Emsian conodonts.||||||
2192|Boogledie Formation|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
2192|Boogledie Formation|68297|5|Briefly described|p192||Early Devonian|Includes Emsian vertebrate fossil and conodont fauna in informal Mount Knowles limestone member.|||Includes informal Mount Knowles limestone member|||
2192|Boogledie Formation|68592|6|Mentioned|p1198|Eifelian|Eifelian|||||||
2192|Boogledie Formation|73299|6|Mentioned|p1106|Eifelian|Eifelian|Deposition extended into the early Eifelian (Meakin and Morgan, 1999).||||Overlies the Mount Frome Limestone.||
2203|Bookpurnong Formation|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Late Miocene|See also Bookpurnong beds. Geological Province: Murray Basin.||||||13-AUG-07
2203|Bookpurnong Formation|22773|5|Briefly described|Fig24.8p352,354|Pliocene|Miocene|||||||
2203|Bookpurnong Formation|22857|5|Briefly described|p352-3 Figs. 24.8 and 24.9, p354|Early Pliocene|Late Miocene|Passes laterally into the Loxton and Parilla Sands. Geological Province: Murray Basin.||||||
2203|Bookpurnong Formation|23226|6|Mentioned|p901|||May overlap Pata Formation depending upon geographic location.  Of Murray Basin.||||||
2203|Bookpurnong Formation|23768|5|Briefly described|p27, p33, p47|||Geological Province: Murray Basin. Overlain by Norwest Bend Formation.  see also p28 Fig. 5.||||||11-SEP-09
2203|Bookpurnong Formation|24551|6|Mentioned|p450|||Supersedes Bookpurnong Beds||||||
2203|Bookpurnong Formation|30996|4|Described|p30|||||||||
2203|Bookpurnong Formation|41511|5|Briefly described|p18|||See also mention p20.||||||29-JUL-08
2203|Bookpurnong Formation|42127|5|Briefly described|p222|||||||||
2203|Bookpurnong Formation|42966|6|Mentioned|p152|||Synonym for Bookpurnong beds||||||
2203|Bookpurnong Formation|44133|5|Briefly described|p161, 152 Fig. 10.2|Early Pliocene|Late Miocene|Geological Province: Murray Basin. ||||||
2203|Bookpurnong Formation|60540|5|Briefly described|p999,p1000 Fig.2,p1002 Fig.4,p1020 |Pliocene|Pliocene|Brown and Stephenson (1991), Rogers et al. (1995). Previously Bookpurnong Beds. Zanclean age, based on biostratigraphy? Low-energy, shallow-marine deposits.||||Conformably overlain by the Loxton Sand. Onlaps [overlies] the Murray Supergroup.|Variable fossiliferous, shallow marine, glauconitic clays and marls.|06-FEB-18
2203|Bookpurnong Formation|60785|6|Mentioned|p184 Fig.1, p196.  |Zanclean|Zanclean|South Australia. Has yielded fossil cetacean elements.||||||
2203|Bookpurnong Formation|61185|5|Briefly described|p58|Late Miocene|Late Miocene|Name used interchangeably with Bookpurnong Beds. Marine sediments. Geological Province: Murray Basin.||||||07-FEB-11
2203|Bookpurnong Formation|63887|5|Briefly described|p20, p21, p21 Fig. 1|Pleistocene|Late Miocene|Shallow marine depositional environment. Consists of clays with occasional sandy, silty, carbonaceous and calcareous beds.||||||
2203|Bookpurnong Formation|64237|5|Briefly described|p19 Fig.2b|Late Miocene|Late Miocene|Superseded Bookpurnong Beds of Lawrence (1961) - revised by Rogers et al (1995). Overlies the Murray Group.||||||29-JUL-08
2203|Bookpurnong Formation|66286|5|Briefly described|p179, pp189-190.|Pliocene|Miocene|Refers to the mud-rich sediments underlying the Loxton-Parilla sands. Deposited during a marine transgression-regression into the Murray Basin. Lacks high carbonate, fossil and glauconite content of other occurrences. 1.5 - 3m blanket under Wimmera Plain.||||Overlies Loddon River Group. Is overlain by or interfingers with Loxton-Parilla sands.|Shallow marine clays and marls; grey to brown muds; pinnate cracks filled with kaolinite common; local goethite-rich lenticular mottles.|
2203|Bookpurnong Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||||||
2203|Bookpurnong Formation|68548|5|Briefly described|p13|Pliocene|Miocene|Late Miocene to Early Pliocene.||||Overlain by the Loxton Sand.|Succession of variably fossiliferous, shallow marine, glauconitic clays and marls.|
2203|Bookpurnong Formation|68715|6|Mentioned|p31 Fig.5|Pliocene|Miocene|Murray Basin. Late Miocene maximum age.||||||
2203|Bookpurnong Formation|68716|5|Briefly described|p39 Fig.3, p40, p43, p44 Fig.7|||Aquitard - extremely low permeability.||||Overlain by the Loxton Sand and Monoman Formation. Underlain by the Pata Formation.||
2203|Bookpurnong Formation|71593|4|Described|p52-p54|Pliocene||This unit is only a few metres thick generally.||||Overlain by the Loxton Sand.|Clay to marl with occasional shell fragments or mica flakes.|
2203|Bookpurnong Formation|72445|5|Briefly described|App.1; App.2.|Pliocene||App.2 is a .csv format file . Identified in Stavely 09,11,14. Accidently assigned to Murray Group in Stavely 11? Shown as ungrouped elsewhere. Minimum age from overlying units.||||Overlain by Calivil Formation, Loxton Sand (sharp contact). Overlies Renmark Group (gradational contact), Murray Group (sharp contact).|Includes glauconitic marl, fine sand and silt; marl with lesser sand and mud; silt with marl and limestone.|
2203|Bookpurnong Formation|73188|6|Mentioned|p320|Pliocene|Pliocene|Murray Basin.|||||Marl, clay, sand.|
2203|Bookpurnong Formation|73228|4|Described|p50, p52-58, p62|Early Pliocene|Late Miocene|Murray Basin. Shallow marine, lower shoreface depositional environments. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1 and Overland Corner 1 drillholes. Outcrops are limited to a small area; type section near Loxton, SA. Subsurface thickness of up to 50 m. Subsurface distribution is a broad arc in the deeper, central sections of the Murray Basin. Considered to have formed on the lower-shoreface (offshore) following major marine inundation of the area.||||Underlain by Murray Group. Overlain by Loxton Sand and Blanchetown Clay.|Brown or greenish grey marl, silty clay and minor fine sand, with relatively high carbonate contents. Includes glauconite, shell/mollusc fragments and bryozoa.|
2203|Bookpurnong Formation|73229|5|Briefly described|p66-67, p70-72, p74-75|Early Pliocene|Late Miocene|Murray Basin. [Analysed using pXRF; see article]. Shallow marine.|||||Marl; silty clay; minor fine-grained sand, glauconitic.|
2220|Boolaroo Subgroup|22969|5|Briefly described|p 49|||Newcastle Coal Measures||||||
2220|Boolaroo Subgroup|24121|5|Briefly described|p4, p61, 73, 132, 227, 231|||Of Newcastle Coal Measures.||||||25-AUG-22
2220|Boolaroo Subgroup|39609|6|Mentioned|Table 1|||||||||
2220|Boolaroo Subgroup|39666|6|Mentioned|Table 20|||||||||
2220|Boolaroo Subgroup|42214|6|Mentioned|Table 1 P462|||||||||
2220|Boolaroo Subgroup|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||Newcastle Coal Measures.||Overlies Adamstown Subgroup. Is overlain by Moon Island Beach Subgroup.||
2220|Boolaroo Subgroup|68711|5|Briefly described|p118, p116 Tbl 2|||Of McKenzie and Britten (1969). Replaced in part by Boolaroo Formation. See also p113.||Formerly of Newcastle Coal Measures|Included Mount Hutton Formation, Hartley Hill Coal, Warners Bay Formation, Lower Pilot Coal, Reids Mistake Formation, Upper Pilot Coal, Croudace Bay Formation.|||
2220|Boolaroo Subgroup|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Newcastle Coal Measures|||Sandstone, conglomerate, tuff, black coal.|
2253|Boonanghi beds|22736|6|Mentioned|p627|Permian|Carboniferous|||||||
2253|Boonanghi beds|22857|4|Described|p502 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Includes the "Byabbara beds". Turbiditic siltstone, lithic arenite, conglomerate and minor redeposited limestone; sparse fossils. Geological Province: Tamworth Forearc Basin.||||||
2253|Boonanghi beds|41347|4|Described|Table 5|||||||||
2253|Boonanghi beds|41348|5|Briefly described|Map legend|Carboniferous||In the Hastings Block.||||||16-DEC-04
2253|Boonanghi beds|43755|6|Mentioned|Fig.1,p548||Carboniferous|||||||
2253|Boonanghi beds|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.||||||01-MAR-05
2253|Boonanghi beds|70939|6|Mentioned|p826, p828, p837|Carboniferous|Carboniferous|Northern Hastings Block.||||||
2253|Boonanghi beds|71628|5|Briefly described|p17: 57, 61, 88|Carboniferous|Carboniferous|Hastings Block.||||Is intruded by Glen Esk and Gundle Monzogranites, and Banda Banda Monzodiorite.|Terrigenous clastic rocks.|
2268|Booragul Tuff Member|37083|6|Mentioned|p164|||||||||
2268|Booragul Tuff Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Catherine Hill Bay Formation.||||
2270|Boorah Limestone|40883|6|Mentioned|p5|||||||||
2271|Booral Formation|22736|6|Mentioned|p629||Namurian|||||||
2271|Booral Formation|22857|4|Described|p241, p510 App.1 Tb.A1.8|Late Carboniferous|Namurian|Grey, often siliceous mudstone, siltstone; medium-grained lithic arenite, feldspathic arenite. Max. thickness: 1125m. Geological Province: Kullatine-Yagon-Booral Shelf and Tamworth Forearc Basin.||||||
2271|Booral Formation|22863|6|Mentioned|p241|||||||||
2271|Booral Formation|24118|5|Briefly described|p3|||||||||
2271|Booral Formation|24121|5|Briefly described|p4, p233|||||||||25-AUG-22
2271|Booral Formation|29728|6|Mentioned|p394|||||||||
2271|Booral Formation|30074|6|Mentioned|p27|||See also P28.||||||
2271|Booral Formation|30668|6|Mentioned|p582|||Occurrence of Septatopora pustulosa (Crockford).||||||
2271|Booral Formation|30772|6|Mentioned|p5|||Fauna||||||
2271|Booral Formation|32141|6|Mentioned|p152|||||||||
2271|Booral Formation|32324|6|Mentioned|Table 8.1|||||||||
2271|Booral Formation|32379|6|Mentioned|p5|||||||||
2271|Booral Formation|32866|6|Mentioned|Fig.8|||||||||
2271|Booral Formation|32868|6|Mentioned|p208,Fig.7|||||||||
2271|Booral Formation|33992|6|Mentioned|p237|||M.Carb.||||||
2271|Booral Formation|34085|6|Mentioned|Cor.chart|||Westphalian||||||
2271|Booral Formation|34168|5|Briefly described|p254|||Carboniferous||||||
2271|Booral Formation|34238|6|Mentioned|Table 1|||||||||
2271|Booral Formation|36528|6|Mentioned|p180|||||||||
2271|Booral Formation|36599|6|Mentioned|Fig.1|||||||||
2271|Booral Formation|39302|5|Briefly described|p346|||||||||
2271|Booral Formation|40883|6|Mentioned|p2|||See also P8||||||
2271|Booral Formation|42547|4|Described|p32, 36|||||||||
2271|Booral Formation|43432|14|Not recorded|p208||Late Carboniferous|Ref.to Campbell 1961.Part of Crawford Formation||||||
2271|Booral Formation|43447|14|Not recorded|Table 1&2,p10,13||Carboniferous|||||||
2271|Booral Formation|43451|14|Not recorded|Map Legend|||||||||
2271|Booral Formation|43479|14|Not recorded|p161||Carboniferous|||||||
2271|Booral Formation|43983|14|Not recorded|p1,4,8,11-14||Westphalian|Middle Westphalian||||||
2271|Booral Formation|43992|14|Not recorded|p196||Westphalian|(M.Westphalian)||||||
2271|Booral Formation|44093|5|Briefly described|p229 App. 1|Late Carboniferous|Early Carboniferous|Geological Province: New England Fold Belt.||||||
2271|Booral Formation|44244|2|Defined|p149|Westphalian|Namurian|Conformably overlies Karuah and Faulkland Formations, and Salisbury Sandstone; conformably underlies McInnes Formation.  Max. thickness: 1125m.  Geological Province: Myall Block.||||||
2271|Booral Formation|44360|14|Not recorded|p34|||Unit compared with fauna in Poperima Formation.||||||
2271|Booral Formation|44372|6|Mentioned|p27|||||||||
2271|Booral Formation|44388|14|Not recorded|p113||Westphalian|Fauna comparable with Neerkol Formation.||||||
2271|Booral Formation|44859|14|Not recorded|p68|||Contains Peruvispira kuttungensis, Campbell.||||||
2271|Booral Formation|44994|6|Mentioned|p200|||||||||
2271|Booral Formation|45097|6|Mentioned|Fig.|||Carboniferous correlation chart. Refers McDonald (1972).||||||
2271|Booral Formation|46849|6|Mentioned|Fig. 2|||||||||
2271|Booral Formation|47056|6|Mentioned|Fig.2 P523|||||||||
2271|Booral Formation|48924|6|Mentioned|p4||Late Carboniferous|See also P5-8,11-14 etc. U.Carb.||||||
2271|Booral Formation|48971|6|Mentioned|p9,12|||||||||
2271|Booral Formation|50099|6|Mentioned|p18|Late Carboniferous|Late Carboniferous|||||||
2271|Booral Formation|50147|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Geological Province: Western Myall Block.||||||
2271|Booral Formation|50263|5|Briefly described|Map Legend|Westphalian|Namurian|Overlies: Karuah Formation. Underlies: McInnes Formation.  Geological Province: Western Myall Block.||||||
2271|Booral Formation|63832|5|Briefly described|p131 fig 2|Serpukhovian|Serpukhovian|Western Myall block, Southern New England Fold Belt.||||||13-DEC-17
2271|Booral Formation|64631|5|Briefly described|p44 Fig.2.|Serpukhovian|Serpukhovian|Southern New England Fold Belt, western Myall Block. Biostratigraphic age control at base and top and radiometric age control within unit.||||Overlain by Johnsons Creek Conglomerate.||
2271|Booral Formation|68297|5|Briefly described|p195|Early Carboniferous|Early Carboniferous|Reported to include an 'ichthyodorulite' described by Morris in Strzelecki, 1845.||||||
2271|Booral Formation|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Serpukhovian|Gresford Block, Tamworth Belt.||||||
2271|Booral Formation|71233|5|Briefly described|p105|Carboniferous|Carboniferous|Clarence-Gloucester district. Westphalian in its lower portion: Levipustula levis Assemblage Zone.||||Lateral equivalent of the Italia Road Formation.||
2271|Booral Formation|71628|5|Briefly described|p6:22; p19:156|||||Dewrang Group.||Is intruded by Stroud Mountain Microgranite.||
2271|Booral Formation|73487|6|Mentioned|p567, p571||||||||Sedimentary rock.|
2284|Boorook Group|33436|5|Briefly described|p233|||Perm. Constituent formations.||||||
2284|Boorook Group|33476|6|Mentioned|Table 1|||||||||
2284|Boorook Group|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
2284|Boorook Group|34340|6|Mentioned|Table 6.1|||Permian||||||
2284|Boorook Group|34423|6|Mentioned|p291|||Permian||||||
2284|Boorook Group|34556|6|Mentioned|p268|||Permian||||||
2284|Boorook Group|34589|6|Mentioned|p275|||Permian||||||
2284|Boorook Group|34940|6|Mentioned|p156|||||||||
2284|Boorook Group|35490|6|Mentioned|p132|||||||||
2284|Boorook Group|43344|14|Not recorded|p104||Permian|||||||
2284|Boorook Group|43385|14|Not recorded|p179,180||Early Permian|||||||
2284|Boorook Group|43881|14|Not recorded|p6-9|||New name for 'Upper Drake Series'.||||||
2284|Boorook Group|43894|14|Not recorded|p787||Permian|||||||
2284|Boorook Group|48940|6|Mentioned|Fig.14|||Refers Voisey (1936)||||||
2286|Booroomba Leucogranite|32820|6|Mentioned|p3|||Part of Murrumbidgee Batholith||||||
2286|Booroomba Leucogranite|32905|6|Mentioned|p228|||Age.||||||
2286|Booroomba Leucogranite|32906|6|Mentioned|Fig.1|||||||||
2286|Booroomba Leucogranite|36413|2|Defined|p84|Silurian|Silurian|||||||
2286|Booroomba Leucogranite|36414|5|Briefly described|map legend|Pridolian|Ludlovian|Coarse-textured leucogranite. GSNSW map code: gmb.||||||
2286|Booroomba Leucogranite|36441|5|Briefly described|map legend|Pridolian|Pridolian|Of Murrumbidgee Batholith. Intrusive. S-type. Leucogranite, aplite. BMR map code: Smb.||||||
2286|Booroomba Leucogranite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Leucogranite, aplite. S-type. BMR map code: Smb.||||||
2286|Booroomba Leucogranite|36633|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
2286|Booroomba Leucogranite|37728|4|Described|Table 3|||||||||
2286|Booroomba Leucogranite|39626|6|Mentioned|p275|||||||||
2286|Booroomba Leucogranite|40328|4|Described|p203|||||||||
2286|Booroomba Leucogranite|42497|5|Briefly described|Map legend|Pridolian|Ludlovian|||||||
2286|Booroomba Leucogranite|42727|5|Briefly described|map legend|Pridoli|Pridoli|Of Murrumbidgee Batholith. Leucogranite, S-type. BMR map symbol: Sga. Geol. Prov: Canberra Block.||||||
2286|Booroomba Leucogranite|42820|4|Described|p66|||||||||
2286|Booroomba Leucogranite|44092|5|Briefly described|map legend|Silurian|Silurian|glw1||||||
2286|Booroomba Leucogranite|45147|2|Defined|M203|Silurian|Silurian|||||||
2286|Booroomba Leucogranite|60078|6|Mentioned|Map Legend|Late Silurian|Late Silurian|||||||
2288|Booroomin Group|29698|6|Mentioned|p64|||||||||
2288|Booroomin Group|29870|6|Mentioned|Table 1|||||||||
2288|Booroomin Group|32944|6|Mentioned|p702|||U.Permian||||||
2288|Booroomin Group|34043|5|Briefly described|p453|||Perm.  Corr. with Singleton C.M.||||||
2288|Booroomin Group|34292|6|Mentioned|Table 1|||Permian||||||
2288|Booroomin Group|37094|4|Described|p244|||||||||
2294|Boothumble Formation|22508|6|Mentioned|p4|||In the Lachlan Fold Belt.||||||03-JUN-08
2294|Boothumble Formation|22768|5|Briefly described|p170|||||||||
2294|Boothumble Formation|22857|5|Briefly described|p170, p438 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Cobar Supergroup. Fluvial fan and shallow marine sequence. Overlain by Rast Group. Correlates with Square Head Formation. Max. thickness: 1700m. Geological Province: Mouramba Shelf.||||||
2294|Boothumble Formation|41394|2|Defined|p61|Early Devonian||||||||
2294|Boothumble Formation|41395|6|Mentioned|Map legend|Lochkovian||||||||
2294|Boothumble Formation|41821|6|Mentioned|p11 Fig.5|||Occurs in Kilparney sheet area||||||
2294|Boothumble Formation|42144|5|Briefly described|p605|||See also Fig.3.||||||26-MAR-08
2294|Boothumble Formation|42521|5|Briefly described|p16, Figs|||||||||
2294|Boothumble Formation|43089|5|Briefly described|Map Legend|||Of Cobar Supergroup.||||||26-MAR-08
2294|Boothumble Formation|43263|6|Mentioned|Map Legend||Lochkovian|||||||
2294|Boothumble Formation|43757|6|Mentioned|p510|||||||||
2294|Boothumble Formation|61964|5|Briefly described|p14 Fig. 4|Pridoli|Pridoli|Supersedes Boothumble beds. Includes Norholm Sandstone Member. Along with Yegi Conglomerate this is a transgressive sequence of basal synrift coarse, basement-derived alluvial fan clastics - but is not exposed on CARGELLIGO sheet. Overlain by Rast Group?||||||
2294|Boothumble Formation|62405|5|Briefly described|Map legend|Early Devonian|Silurian|?Probably overlain by the Bootheragandra Group.  Massive and cross-bedded granule to pebble conglomerate, pebbly lithic sandstone and well-sorted quartz sandstone; minor siltstone.||||||26-MAR-08
2294|Boothumble Formation|63019|5|Briefly described|p920|Pridoli|Pridoli|Unconformably overlies Wagga Group. Quartz-rich sandstone interpreted to be basement-derived, subaerial alluvial-fan facies. Age: 418.7Ma. Geological Province: Lachlan Orogen.||||||
2294|Boothumble Formation|63891|5|Briefly described|p236, p237|||Underlies Rast Group. Sequence of quartz-rich subaerial alluvial-fan deposits. Faulted contact with Clements Formation (Wagga Group).||||||
2294|Boothumble Formation|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, App A-VI 3.||||||
2294|Boothumble Formation|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
2294|Boothumble Formation|71039|6|Mentioned|p14|||Preserves abundant detrital micas.||||||
2294|Boothumble Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Mouramba Group.|||Massive and cross-bedded granule to cobble conglomerate, pebbly lithic sandstone, and well-sorted quartz sandstone with minor siltstone and shale.|
2294|Boothumble Formation|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||Mouramba Group?||||
2307|Borambil Creek Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
2307|Borambil Creek Formation|32482|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
2307|Borambil Creek Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
2307|Borambil Creek Formation|32944|6|Mentioned|p700|||See also P710. L.Perm.||||||
2307|Borambil Creek Formation|34043|5|Briefly described|p451|||M.Perm.  Corr. with Maitland Gp.||||||
2307|Borambil Creek Formation|34138|6|Mentioned|Cor.Chart|||Kungurian - Kazanian||||||
2307|Borambil Creek Formation|34447|6|Mentioned|Table 5.2|||||||||
2307|Borambil Creek Formation|37094|5|Briefly described|p240|||||||||
2307|Borambil Creek Formation|43407|14|Not recorded|Map Legend||Late Permian|(Provisional Edition) See also Lexicon||||||
2307|Borambil Creek Formation|43440|14|Not recorded|p82|||||||||
2307|Borambil Creek Formation|61201|4|Described|p 2, 5 Table 1, 6-7|Late Permian|Late Permian|Geological Province: Werrie Basin. Max. Thickness: 105m. Lithic Sandstone, conglomerate, shale. Overlies: Willow Tree Formation. Underlies: Toll Bar Formation.||||||
2307|Borambil Creek Formation|61776|5|Briefly described|p194 Fig. 3|Late Permian|Early Permian|Geological Province: Werrie Basin. Lithic sandstone and conglomerate.||||||17-SEP-08
2307|Borambil Creek Formation|68003|5|Briefly described|p38 Fig.3-j, p40, p42, p129.|Late Permian|Late Permian|Werrie Basin (North), Brigalow Belt South Bioregion. Coeval with lower part of Bickham Formation in the south of the Basin.||||Overlies Willow Tree Formation. Is overlain by Toll Bar Formation.|Lithic sandstone and conglomerate.|
2307|Borambil Creek Formation|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian marine sequences: conglomerate, quartzose sandstone, siltstone, calcareous mudstone and limestone.||||||
2307|Borambil Creek Formation|70791|5|Briefly described|p277, p293 Fig.17|Guadalupian|Guadalupian|Werrie Basin (north).||Maitland Group.||||
2330|Boree Creek Formation|13139|5|Briefly described|p7, p9 Fig. 4|Wenlock|Llandovery|Of the Waugoola Group. Contains a richly fossiliferous basal subunit called "Limestone A".   Geological Province: Western Molong Volcanic Belt.||||||12-APR-05
2330|Boree Creek Formation|13996|5|Briefly described|p129, p139, p143|Wenlock|Llandovery|Orange district, NSW. Contains Wenlock conodonts; compared with Clarita Formation [of Oklahoma]. An unnamed new species of conulariid mentioned. Hosts a rich, largely undescribed trilobite fauna.||||Is overlain by Mirrabooka Formation. Equivalent to Rosyth Limestone.||
2330|Boree Creek Formation|22857|5|Briefly described|p127, p468 App.1 Tb.A1.6|Llandovery|Llandovery|Of the Waugoola Group. Shallow-water limestone. Max. thickness: 100m. Geological Province: Molong Rise.||||||
2330|Boree Creek Formation|23214|2|Defined|p111|Wenlock|Llandovery|Of Waugoola Group. Originally named Rosyth Limestone Member of the Panuara Formation. Consists of three sub-units "Limestone A", "Tuffaceous Trilobite Bed" and "Limestone B". Max thickness 100m.||||||
2330|Boree Creek Formation|23245|6|Mentioned|p127||Llandovery|||||||
2330|Boree Creek Formation|23334|5|Briefly described|7|Silurian|Early Silurian|||||||
2330|Boree Creek Formation|24398|5|Briefly described|p259 Fig.2|Early Wenlockian|Llandovery|Geological Province: Lachlan Fold Belt.||||||
2330|Boree Creek Formation|29791|6|Mentioned|p90|||||||||
2330|Boree Creek Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
2330|Boree Creek Formation|32672|6|Mentioned|p672|||||||||
2330|Boree Creek Formation|33116|4|Described|p210|||Sil. See also PP211-212.||||||
2330|Boree Creek Formation|33121|5|Briefly described|p85|||Early Sil. Correlation table.||||||
2330|Boree Creek Formation|33285|6|Mentioned|p18|||Early Sil.||||||
2330|Boree Creek Formation|35137|6|Mentioned|p87|||||||||
2330|Boree Creek Formation|37013|6|Mentioned|p37|||||||||
2330|Boree Creek Formation|37727|4|Described|p78|||||||||
2330|Boree Creek Formation|39331|6|Mentioned|Fig.6-8|||||||||
2330|Boree Creek Formation|40328|3|Fully described|p140|||||||||
2330|Boree Creek Formation|41296|6|Mentioned|p130|||||||||
2330|Boree Creek Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
2330|Boree Creek Formation|43782|6|Mentioned|Map diagram|Wenlock|Llandovery|Of Waugoola Group.||||||14-APR-08
2330|Boree Creek Formation|61892|6|Mentioned|p199, p209, p211-212, p214-216, p218-219|Early Silurian|Early Silurian|See also p222-224. Central-western NSW. Contains Early Silurian (Llandovery-Wenlock) linguliformean brachiopods (described).||||||
2330|Boree Creek Formation|63083|6|Mentioned|p218|||In the Orange district, central NSW. Underlies Mirrabooka Formation. Laterally equivalent to Rosyth Limestone. Contains Wenlock trilobite fauna.||||||07-FEB-11
2330|Boree Creek Formation|63278|6|Mentioned|p146 Fig. 2a|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
2330|Boree Creek Formation|63287|6|Mentioned|p317 Fig. 2, p336|Wenlock|Llandovery|Of Waugoola Group. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
2330|Boree Creek Formation|63290|5|Briefly described|p392 Tb. 1|Wenlock|Wenlock|Of Waugoola Group. Consists of tuffaceous sandstone. Geological Province: Molong Volcanic Belt.||||||11-DEC-07
2330|Boree Creek Formation|63293|6|Mentioned|p468 Fig. 2||Llandovery|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
2330|Boree Creek Formation|67106|6|Mentioned|p673|||Molong Volcanic Belt.||||||
2330|Boree Creek Formation|67651|5|Briefly described|p414-415||||||Includes Rosyth Limestone.|Overlain unconformably by Mirrabooka Formation or Borenore Limestone.||
2330|Boree Creek Formation|70297|5|Briefly described|map legend|Early Silurian|Early Silurian|||Waugoola Group||||
2330|Boree Creek Formation|70684|6|Mentioned|p19, p74|Early Silurian|Early Silurian|Molong Volcanic Belt.||||||
2336|Borehole Coal|22578|6|Mentioned|Fig.9 p399|||||||||
2336|Borehole Coal|23055|6|Mentioned|Fig4p11|||||||||
2336|Borehole Coal|23438|6|Mentioned|p23|||||||||
2336|Borehole Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Lambton Formation.   Geological Province: Sydney Basin||||||
2336|Borehole Coal|39292|6|Mentioned|p108|||See also p110, Fig.6.6||||||
2336|Borehole Coal|39308|6|Mentioned|Fig.23.4|||||||||
2336|Borehole Coal|39609|6|Mentioned|Table 1|||||||||
2336|Borehole Coal|40516|6|Mentioned|p395|||||||||
2336|Borehole Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Borehole coal seam instead. See also p113.||Of Lambton Subgroup||||
2336|Borehole Coal|73304|6|Mentioned|p75|||||Lambton Formation, Newcastle Coal Measures||||
2341|Borenore Limestone|13996|5|Briefly described|p129, p139-140, p143-145|Silurian|Silurian|Midwestern NSW. Contains Wenlock conodonts; compared with Clarita Formation [of Oklahoma]. An unnamed new species of conulariid mentioned. Contains mid-Wenlock brachiopods. Contains a diverse Wenlock-aged trilobite fauna. Biogeographic implications.||||Equivalent to Mirrabooka Formation and Molong Limestone.||
2341|Borenore Limestone|22857|5|Briefly described|p468 App.1 Tb.A1.6|Silurian|Silurian|Of the Mumbil Group. Brecciated, fossiliferous limestone, tiffaceous siltstone and shale, calcareous arenite. Max. thickness: 600m.||||||
2341|Borenore Limestone|23214|3|Fully described|p127|Pridoli|Wenlock|Of Mumbil Group. Previously included as a member of the Gamboola Shale (Joplin 1952), Panuara Formation (Walker 1959). Max. thickness 900m.||||||
2341|Borenore Limestone|30073|6|Mentioned|p53|||Wenlockian age. Receptaculitids.||||||
2341|Borenore Limestone|33611|6|Mentioned|p130|||||||||
2341|Borenore Limestone|34406|6|Mentioned|p220|||||||||
2341|Borenore Limestone|37727|4|Described|p79|||||||||
2341|Borenore Limestone|39331|6|Mentioned|Fig.6-3|||Biostratigraphy||||||
2341|Borenore Limestone|40328|3|Fully described|p146|||||||||
2341|Borenore Limestone|40619|6|Mentioned|Plate 4|||||||||
2341|Borenore Limestone|40620|6|Mentioned|Fig.1|||||||||
2341|Borenore Limestone|42414|6|Mentioned|p60|||||||||
2341|Borenore Limestone|43344|14|Not recorded|p139,160||Silurian|||||||
2341|Borenore Limestone|43640|5|Briefly described|Map Legend||Silurian|||||||
2341|Borenore Limestone|43782|5|Briefly described|Map Legend|Pridoli|Wenlock|of Mumbil Group.||||||
2341|Borenore Limestone|50095|5|Briefly described|p108 Fig.1|Silurian|Silurian|||||||
2341|Borenore Limestone|61892|6|Mentioned|p215-216, p224|Wenlock|Wenlock|Contains Acrotretella brachiopods, contrasted with those around the world. Appears as Borenore Formation on p215-216.||||||
2341|Borenore Limestone|61894|6|Mentioned|p180 |||Orange district.||||||
2341|Borenore Limestone|63083|6|Mentioned|p218|||Together with Molong Limestone - forms lateral equivalent of Mirrabooka Formation.||||||07-FEB-11
2341|Borenore Limestone|63287|5|Briefly described|p317 Fig. 2|Pridoli|Wenlock|Of Mumbil Group. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
2341|Borenore Limestone|64994|5|Briefly described|p7|Wenlock|Wenlock|Of Bischoff (1986). Includes carbonate rocks with the conodont Kockelella ranuliformis.||||||07-JUN-22
2341|Borenore Limestone|67651|5|Briefly described|p413-416,426,428,430-432,442,445-446|Ludlow|Wenlock|Ranges in age from early Wenlock (Kockelella ranuliformis-K. amsdeni biozones) to Ludlow (K. variabilis to possibly P. siluricus biozones). Broadly contemporaneous to Mirrabooka Formation and Molong Limestone. See also p453,459-460,466-468,470,478,480,484.||||Overlain by Wallace Shale. Laterally grades into Mirrabooka Formation. Underlain unconformably by Boree Creek Formation.||
2341|Borenore Limestone|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Parent age: late early Silurian to earliest Devonian. ||Mumbil Group|||Thick carbonate unit.|
2344|Boro Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Hornblende-biotite granite. BMR map symbol: gho.||||||15-AUG-07
2344|Boro Granite|23048|6|Mentioned|p7||Devonian|||||||
2344|Boro Granite|24116|5|Briefly described|p43|||||||||
2344|Boro Granite|24128|5|Briefly described|p56|||Geological Province: Lachlan Fold Belt.||||||
2344|Boro Granite|24266|5|Briefly described|p1485|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||07-DEC-04
2344|Boro Granite|29989|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
2344|Boro Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
2344|Boro Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
2344|Boro Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
2344|Boro Granite|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
2344|Boro Granite|30734|6|Mentioned|p54|||||||||
2344|Boro Granite|30735|2|Defined|p38|Devonian|Devonian|||||||
2344|Boro Granite|30736|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2344|Boro Granite|31015|6|Mentioned|p119|||See also P120, 123, 278||||||
2344|Boro Granite|31019|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2344|Boro Granite|31411|6|Mentioned|p16|||||||||
2344|Boro Granite|32483|4|Described|p26|||||||||
2344|Boro Granite|32820|6|Mentioned|p3|||Part of Bega Batholith||||||
2344|Boro Granite|33325|5|Briefly described|p14|||Age p19.||||||07-SEP-15
2344|Boro Granite|34405|6|Mentioned|p105|||||||||
2344|Boro Granite|34519|6|Mentioned|p43|||||||||
2344|Boro Granite|34544|6|Mentioned|p188|||||||||
2344|Boro Granite|35044|6|Mentioned|p24|||||||||
2344|Boro Granite|35257|6|Mentioned|p106|||||||||
2344|Boro Granite|36413|2|Defined|p119|Devonian|Devonian|||||||
2344|Boro Granite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Hornblende-biotite granite. GSNSW map code: go.||||||
2344|Boro Granite|37727|6|Mentioned|p77|||||||||
2344|Boro Granite|39800|6|Mentioned|Map legend|Carboniferous|Late Devonian|Late Devonian or Carboniferous||||||
2344|Boro Granite|40276|6|Mentioned|p9|||||||||
2344|Boro Granite|40328|4|Described|p203|||||||||
2344|Boro Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
2344|Boro Granite|42820|5|Briefly described|p72|||||||||
2344|Boro Granite|45003|14|Not recorded|p45|||See also Lexicon||||||
2344|Boro Granite|46568|14|Not recorded|p.425|Carboniferous|Devonian|Superseded by Shoalhaven Granite. I55-16/Michelago. Devonian or Carboniferous.||||||11-MAY-04
2344|Boro Granite|48878|14|Not recorded|p.20||Early Devonian|390 m.yrs. (Lower Devonian). (I55-16).||||||
2344|Boro Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Of the Bega Batholith.||||||11-MAY-04
2344|Boro Granite|66087|5|Briefly described|p15|Early Devonian|Early Devonian|Associated with Terry Hie and Astrid skarns.|411.5 +/- 3.1 Ma U/Pb SHRIMP.|||||10-MAY-12
2344|Boro Granite|66300|5|Briefly described|p ix, p41, 46.||||411.5 +/- 3.1 Ma.|Unit in Glenbog Suite.||Intrudes Long Flat Volcanics.||29-OCT-13
2344|Boro Granite|68592|5|Briefly described|p1675-7, p1680-1|Early Devonian|Early Devonian|Some outcrops in several geological maps (listed) have been reassigned to Bundong Granite; reasons elaborated. SHRIMP U-Pb zircon age.|411.5 +/- 3.1 Ma (Bodorkos and Simpson, 2008).|Unit in Glenbog Suite.||||
2344|Boro Granite|69159|5|Briefly described|Map legend|Pragian|Pragian|||Unit in Glenbog Suite.|||Pink and white to grey, medium- to coarse-grained, massive, porphyritic, leucogranite to biotite +/- hornblende granodiorite.|07-SEP-15
2344|Boro Granite|69270|5|Briefly described|p1, p15|Early Devonian|Early Devonian|Dating: zircon U-Pb SHRIMP age, Bodorkos and Simpson (2008).|411.5+/-3.1 Ma|Glenbog Suite||||
2344|Boro Granite|71069|6|Mentioned|p40 fig 17, p178, p193|||Obsolete, now included as part of the Lockhart Igneous Complex.||Glenbog Suite||||
2344|Boro Granite|71699|5|Briefly described|Map legend.|Devonian|Devonian|The two facies are mapped separately.||Glenbog Suite.|||Pink and white to grey, medium- to coarse-grained, massive, porphyritic, leucogranite to biotite+/-hornblende granodiorite; high radiometric response.|
2344|Boro Granite|71700|3|Fully described|vi, ix, p7, p26, p44|Early Devonian|Early Devonian|It is assumed these rocks are named for the locality of Boro at GR 742494 6107832. Two representative sections are given at GR 742312 6106217 and 741896 6095262, no type section is nominated. Glasson and Paine (1965) referred to the granite as the"Shoalhaven Granite" however the name Boro Granite was already in use and takes precedence. Rocks in the Mayfield-Limekilns area previously identified as belonging to this unit have been remapped as Braidwood Granodiorite. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. See also p50, p67, p77, p82, p85, p86, p115, p119, CD.|411.5 +/- 3.1 Ma (Bodorkos & Simpson, 2008)|Glenbog Suite|||Hornblende-biotite granodiorite and leucocratic granite.|
2352|Botany Sands|23436|5|Briefly described|p46|Holocene|Pleistocene|Unconsolidated sands, clays and peats in the Botany Basin form the Botany Sands aquifer in the northern part of the Basin. It extends over an area of ~18 300 ha. Thickens to S and SE up to ~80m.||||||03-SEP-20
2352|Botany Sands|29591|6|Mentioned|p2|||||||||
2352|Botany Sands|43798|5|Briefly described|p193-195|Holocene|Pleistocene|Subdivided into 4 units: basal Unit of fluvial sand with minor gravel grades upwards into marine sand with estuarine shells and overlain by estuarine muds. up to 30 m deep. Second Unit contains beds of peat, has a higher clay content than the basal Unit, thickness 5 to 15 m. The third Unit consists of a widespread aeolian sand with discontinuous peat and clay beds, maximum depth of 30 m.  Top of this Unit may be marked by development of a weak soil, which has produced cementation by organic material to form a horizon known locally as the 'Waterloo Rock' horizon. A fourth Unit is represented by Holocene aeolian sands.||||Occupies erosional depression formed in the Triassic Hawkesbury Sandstone.|sands, silts, clays and peats.|03-SEP-20
2356|Botheram Granodiorite|22815|4|Described|p45|Silurian|Silurian|||||||
2356|Botheram Granodiorite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
2356|Botheram Granodiorite|35109|2|Defined|p61|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
2356|Botheram Granodiorite|36411|6|Mentioned|p268|||Refers White et al 1977 for definition.||||||
2356|Botheram Granodiorite|40328|4|Described|p203|||||||||
2356|Botheram Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
2356|Botheram Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb26.||||||
2356|Botheram Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
2357|Botobolar Granite|22545|6|Mentioned|p499,500, Fig.2||Carboniferous|||||||
2357|Botobolar Granite|23043|5|Briefly described|Map Legend|Namurian|Visean|||||||11-JAN-10
2357|Botobolar Granite|23170|2|Defined|p277|Carboniferous|Carboniferous|Age: Middle Carboniferous.||||||
2357|Botobolar Granite|24126|6|Mentioned|p292|||||||||
2357|Botobolar Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
2357|Botobolar Granite|32045|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
2357|Botobolar Granite|32485|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
2357|Botobolar Granite|35257|6|Mentioned|Fig.24|||P132||||||
2357|Botobolar Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
2357|Botobolar Granite|43476|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
2363|Botumburra Range Granodiorite|35664|6|Mentioned|p113|||Age dates.||||||
2363|Botumburra Range Granodiorite|40590|6|Mentioned|Fig.1|||||||||
2363|Botumburra Range Granodiorite|71628|4|Described|p17: 1-2, 13-19, 44-45|||Leitch et al. (1982). Preference for this version over the current Botumburra Range Monzogranite is explained. Originally Botumburra Range Adamellite (Leitch et al., 1971). Named after a local geographical feature. Forms an E-W intrusion ~7.5 x 3.5-5 km, about 22 km SSW of Ebor. Other, younger ages given. Geochemistry described; similar to Carrai Granodiorite. Is associated with two mineral prospects (named): Mo, W, [Ag] and [Ag].|232 Ma (SHRIMP: Waltenberg and Blevin, unpubl.).|Botumburra Range Suite.|Bitter Vine Leucomonzogranite Phase.|Intrudes Nambucca beds (Coffs Harbour Association).|Grey to pink to greenish, fine- to medium-grained biotite-hornblende granodiorite and monzogranite. Sedimentary and mafic igneous enclaves are scattered throughout. I-type.|
2417|Bowens Road Coal|40872|6|Mentioned|Fig.2|||||||||
2431|Bowna Gneiss|40498|6|Mentioned|p392|||||||||
2439|Bowspring Limestone Member|13996|6|Mentioned|p136|Ludlow|Ludlow|Yass area. Rugose coral species and biogeographic affinities. See also reference to Bowspring Limestone (p131).||||||
2439|Bowspring Limestone Member|22857|4|Described|p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Silverdale Formation (Hattons Corner Group). Fossiliferous nodular biomicrite, biosparite, shale. Max. thickness: 31.5m. Geological Province: Canberra-Yass Shelf.||||||10-FEB-06
2439|Bowspring Limestone Member|24248|5|Briefly described|p51, p52|Gorstian|Gorstian|Of the Silverdale Formation. Geological Province: Yass Syncline. Nodular, thinly bedded, muddy. Fossils not common.||||||12-JUN-08
2439|Bowspring Limestone Member|29989|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
2439|Bowspring Limestone Member|30069|6|Mentioned|p8|||||||||
2439|Bowspring Limestone Member|31852|6|Mentioned|p711|||See also P712, 719. Ludlovian||||||
2439|Bowspring Limestone Member|32155|6|Mentioned|Fig.1|||Refers fossil occurrences||||||
2439|Bowspring Limestone Member|32483|4|Described|p20|||Silutian. Table 1||||||12-JUN-08
2439|Bowspring Limestone Member|34692|5|Briefly described|p186|||||||||
2439|Bowspring Limestone Member|35244|6|Mentioned|p36|||||||||
2439|Bowspring Limestone Member|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
2439|Bowspring Limestone Member|35386|4|Described|p28|||Part of Silverdale Formation||||||
2439|Bowspring Limestone Member|35501|6|Mentioned|p156|||Source of Stromatoporoids||||||
2439|Bowspring Limestone Member|37727|6|Mentioned|p8|||See also P85.||||||
2439|Bowspring Limestone Member|39331|6|Mentioned|Fig.5-5|||||||||
2439|Bowspring Limestone Member|40328|4|Described|p110|||||||||
2439|Bowspring Limestone Member|45075|5|Briefly described|p6|||Fauna||||||
2439|Bowspring Limestone Member|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Silverdale Formation (Hattons Corner Group).  Overlies the Yanawe Formation; underlies Barrandella Shale Member.  Dark grey mudstone, biomicrite? with nodular to lenticular fossiliferous limestone interbeds.||||||
2439|Bowspring Limestone Member|61894|5|Briefly described|p180|Late Silurian|Late Silurian|Hattons Corner, Yass district.||Silverdale Formation.||||
2439|Bowspring Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Silverdale Formation (Hattons Corner Group). Dark-grey mudstone, biomicrite? with nodular to letnicular fossiliferous limestone interbeds.||||||
2439|Bowspring Limestone Member|68592|2|Defined|p524, p560, p562, p570-3, p1868, p1877-8|Ludlow|Ludlow|See also p429-30 Fig.89, p441, p466, p512, p520. Brunker and Offenberg (1970); Offenberg (1974); included this unit as a Member in their Derringullen Formation; after Bowspring Limestone of Shearsby (1912). Transferred to Silverdale Formation by Link (1970, 1971); Link and Druce (1972). Type section described. 7-32m thick. The first laterally persistent limestone member in the Yass Basin sequence: thus a very important marker. Contains late early Ludlow conodonts. Diverse fauna listed.||Basal unit in Silverdale Formation.||Conformably overlies Tullerah Sandstone Member (Yanawe Formation). Is overlain conformably by Barrandella Shale Member.|Persistent, well-bedded, semi-nodular, fossiliferous limestone with shale interbeds.|12-JAN-17
2439|Bowspring Limestone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Shsb. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Silverdale Formation (basal unit?)||Is overlain by Barrandella Shale Member. Overlies Tullerah Sandstone Member (Yanawe Formation).|Bedded, semi-nodular, fossiliferous biosparite, biomicrite and micritic limestone with interbeds of shale; shale with nodular limestone interbeds.|
2439|Bowspring Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Silurian|||Silverdale Formation|||Bedded, semi-nodular, fossiliferous biosparite, biomicrite and micritic limestone with interbeds of shale; shale with nodular limestone interbeds.|
2439|Bowspring Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Silurian|||Silverdale Formation|||Bedded, seminodular, fossiliferous, biosparite, biomicrite and micritic limestone with interbeds of shale; shale with nodular limestone interbeds.|
2439|Bowspring Limestone Member|71656|4|Described|p12 Fig.2, p19, p23, p52|Gorstian|Gorstian|Includes conodonts, brachiopods, large pentamerides, stromatoporoids, corals and sponges.||Of Silverdale Formation, Hattons Corner Group||Hattons Corner Group. Overlies Yanawe Formation and underlies Barrandella Shale Member.|Fossiliferous limestone.|
2439|Bowspring Limestone Member|73215|5|Briefly described|p994|||Yass Syncline.||Hattons Corner Group.||Overlies Yanawe Formation.||
2455|Boxvale Sandstone Member|12597|5|Briefly described|p492 Tb.1, p496|Toarcian|Toarcian|See also Boxvale Member (p501). N Surat Basin. Up to 90m thick.||Unit in Evergreen Formation.|||Thin sequence of sandstone, siltstone and coal.|
2455|Boxvale Sandstone Member|13516|5|Briefly described|p159 fig 8, p167, p169, p170, p172, p174|Early Jurassic|Early Jurassic|From Surat Basin||Of Evergreen Formation||||
2455|Boxvale Sandstone Member|22857|5|Briefly described|p296-7 Tb.22.1|||Of the Evergreen Formation (Bundamba Group). Geological Province: Surat Basin.||||||24-MAR-06
2455|Boxvale Sandstone Member|22865|4|Described|p314,Table22.1p296-7|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
2455|Boxvale Sandstone Member|24069|5|Briefly described|p284|Early Jurassic|Early Jurassic|Of Evergreen Formation. Geological Province: Surat Basin.||||||
2455|Boxvale Sandstone Member|24092|5|Briefly described|p8 Fig.3|||Of Evergreen Formation. Geological Province: Eromanga Basin.||||||
2455|Boxvale Sandstone Member|29393|6|Mentioned|Table 4|||Jurassic.||||||
2455|Boxvale Sandstone Member|29410|6|Mentioned|Fig.1|||||||||
2455|Boxvale Sandstone Member|29591|6|Mentioned|p69|||||||||
2455|Boxvale Sandstone Member|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
2455|Boxvale Sandstone Member|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|30699|6|Mentioned|p56|||Contains probable beach sands||||||
2455|Boxvale Sandstone Member|30702|6|Mentioned|Fig.1|||On Stratigraphic Table||||||
2455|Boxvale Sandstone Member|31116|4|Described|p21|||See also p1. L. Jurassic||||||10-MAR-19
2455|Boxvale Sandstone Member|31304|6|Mentioned|Fig. 1|||||||||
2455|Boxvale Sandstone Member|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|33381|14|Not recorded|p117||Early Jurassic|Unit of Evergreen Formation.Correlation chart.||||||
2455|Boxvale Sandstone Member|33672|6|Mentioned|p41|||||||||
2455|Boxvale Sandstone Member|33673|4|Described|p291|||||||||
2455|Boxvale Sandstone Member|33675|4|Described|p412|||Lithology.||||||
2455|Boxvale Sandstone Member|33774|6|Mentioned|p48|||Stratigraphy||||||
2455|Boxvale Sandstone Member|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
2455|Boxvale Sandstone Member|34905|6|Mentioned|p531|||||||||
2455|Boxvale Sandstone Member|35095|6|Mentioned|p116|||||||||
2455|Boxvale Sandstone Member|35157|6|Mentioned|p523|||||||||
2455|Boxvale Sandstone Member|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
2455|Boxvale Sandstone Member|36111|6|Mentioned|p34|||||||||
2455|Boxvale Sandstone Member|36233|6|Mentioned|Table 1|||||||||
2455|Boxvale Sandstone Member|36243|6|Mentioned|Table 7A|||||||||
2455|Boxvale Sandstone Member|37995|6|Mentioned|p62|||||||||
2455|Boxvale Sandstone Member|39212|4|Described|p36|||Excursion site. Petroleum reservoir. See also p24.||||||10-MAR-19
2455|Boxvale Sandstone Member|39494|6|Mentioned|p137|||||||||
2455|Boxvale Sandstone Member|39943|6|Mentioned|Table 9A|||||||||
2455|Boxvale Sandstone Member|40030|6|Mentioned|Fig.5|||||||||
2455|Boxvale Sandstone Member|40249|6|Mentioned|p38|||Mention P41||||||
2455|Boxvale Sandstone Member|40250|4|Described|p29|||||||||
2455|Boxvale Sandstone Member|40541|4|Described|p108|||||||||
2455|Boxvale Sandstone Member|40544|6|Mentioned|Fig.6|||||||||
2455|Boxvale Sandstone Member|40666|4|Described|p356|||||||||
2455|Boxvale Sandstone Member|40832|5|Briefly described|p455|||||||||
2455|Boxvale Sandstone Member|41210|6|Mentioned|p158|||||||||
2455|Boxvale Sandstone Member|41247|6|Mentioned|p127|||||||||
2455|Boxvale Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
2455|Boxvale Sandstone Member|41725|6|Mentioned|p400|||||||||
2455|Boxvale Sandstone Member|41747|4|Described|p469|||||||||
2455|Boxvale Sandstone Member|42157|6|Mentioned|p377|||||||||
2455|Boxvale Sandstone Member|42493|5|Briefly described|Fig. 1 P18|||||||||
2455|Boxvale Sandstone Member|42911|5|Briefly described|p13|||of Evergreen Formation||||||
2455|Boxvale Sandstone Member|43000|5|Briefly described|Fig.5,p112|||of Evergreen Formation||||||
2455|Boxvale Sandstone Member|43185|6|Mentioned|14||Jurassic|||||||
2455|Boxvale Sandstone Member|43851|14|Not recorded|Tb p106,111||Early Jurassic|||||||
2455|Boxvale Sandstone Member|43982|14|Not recorded|Map Legend|||||||||
2455|Boxvale Sandstone Member|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
2455|Boxvale Sandstone Member|43994|14|Not recorded|Map Legend|||||||||
2455|Boxvale Sandstone Member|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44023|4|Described|Tb.3,p10||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44032|14|Not recorded|462,464|||Part of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|44118|14|Not recorded|Map Legend||Jurassic|||||||
2455|Boxvale Sandstone Member|44169|2|Defined|Tb.1,p9,map|||||||||
2455|Boxvale Sandstone Member|44170|2|Defined|p21-23,32,map,Tb.1|||||||||
2455|Boxvale Sandstone Member|44174|14|Not recorded|p345,347||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44207|14|Not recorded|p116|||See also Lexicon.||||||
2455|Boxvale Sandstone Member|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
2455|Boxvale Sandstone Member|44381|14|Not recorded|p7|||||||||
2455|Boxvale Sandstone Member|44390|14|Not recorded|p6,9,15,16,Tb.1||Early Jurassic|||||||
2455|Boxvale Sandstone Member|44391|14|Not recorded|Map Legend||Early Jurassic|Part of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|44420|14|Not recorded|p14,15,18,21,27,29,|||Fig.14||||||
2455|Boxvale Sandstone Member|44421|14|Not recorded|p11,12,14,16,17||Jurassic|||||||
2455|Boxvale Sandstone Member|44422|14|Not recorded|p149 (Tb)||Jurassic|||||||
2455|Boxvale Sandstone Member|44426|14|Not recorded|p12||Early Jurassic|"On spore data the Precipice Sandstone and Evergreen Formation (including the Boxvale Sandstone Member) are regarded as of Lower Jurassic age.||||||
2455|Boxvale Sandstone Member|44636|14|Not recorded|p167(Tb)||Early Jurassic|Member of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|44637|14|Not recorded|Table|||||||||
2455|Boxvale Sandstone Member|44787|14|Not recorded|Tb.p123,125,129||Jurassic|Part of Evergreen Formation.||||||
2455|Boxvale Sandstone Member|45071|3|Fully described|Table 15|||||||||
2455|Boxvale Sandstone Member|45073|6|Mentioned|p58|||Geological history||||||
2455|Boxvale Sandstone Member|45110|3|Fully described|p91|||See also p41.||||||10-MAR-19
2455|Boxvale Sandstone Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
2455|Boxvale Sandstone Member|46989|5|Briefly described|Table 1|||||||||
2455|Boxvale Sandstone Member|48900|4|Described|p51|||||||||
2455|Boxvale Sandstone Member|48919|4|Described|p45|||See also p46-53. Jurassic||||||10-MAR-19
2455|Boxvale Sandstone Member|48920|3|Fully described|p43|||Lower Jurassic age. Member of Evergreen Formation||||||
2455|Boxvale Sandstone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
2455|Boxvale Sandstone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
2455|Boxvale Sandstone Member|60998|5|Briefly described|p145|||Of Mollan et al (1972). Superseded Boxvale Sandstone. ||||||
2455|Boxvale Sandstone Member|60999|5|Briefly described|p178 Fig. 10|||Of the Evergreen Formation.  Geological Province: Surat Basin.||||||
2455|Boxvale Sandstone Member|61377|5|Briefly described|p151|Early Jurassic|Early Jurassic|Of the Evergreen Formation. Excellent reservoir sandstone reaching up to 60m thickness. Geological Province: Surat Basin.||||||07-FEB-11
2455|Boxvale Sandstone Member|64856|4|Described|p79, p82-85|Toarcian||Surat Basin. Fine to coarse grained, cross bedded, quartzose sandstone with carbonaceous siltstone, shale and coal interbeds. Contained in the Evergreen Formation. Age from relationship with overlying Westgrove Ironstone Member.| | ||||28-NOV-17
2455|Boxvale Sandstone Member|64857|5|Briefly described|p130-132, p113 Fig.3|||Member of the Evergreen Formation. Surat Basin. Friable quartzose sandstone.||||||
2455|Boxvale Sandstone Member|65117|5|Briefly described|p467, Fig 4 p465|Toarcian|Toarcian|Of Evergreen Formation, Surat Basin. Potential reservoir.  fine to medium grained sandstone with symmetrical ripples, hummocky cross stratification. Massive beds. Overlain by Westgrove Ironstone Member.||||||
2455|Boxvale Sandstone Member|65388|5|Briefly described|p211|||Of Jensen & others (1964). Part of Evergreen Formation, along with "Evergreen Shales".||||||
2455|Boxvale Sandstone Member|66529|6|Mentioned|p12 Fig.5 |||||Unit in Evergreen Formation.||||
2455|Boxvale Sandstone Member|67133|5|Briefly described|p11|Jurassic|Jurassic|Deposited as part of a prograding delta system.||Evergreen Formation.|||Fine- to coarse-grained, cross-bedded, quartzose sandstone.|
2455|Boxvale Sandstone Member|68576|5|Briefly described|Q_4: p14-15, p17, p22, p24|Early Jurassic|Early Jurassic|Surat Basin. Is locally capped by 27 Ma basalt from the Buckland volcano. Differs from other sandstones in the Evergreen Formation which are lithic-feldspathic.||Evergreen Formation.|||Fine- to coarse-grained, cross-bedded quartzose sandstone with some argillaceous clay matrix.|
2455|Boxvale Sandstone Member|69594|5|Briefly described|p535|||Jensen et al. (1964). Previously the Boxvale Sandstone of Reeves (1947), which was incorporated as a Member into the redefined Evergreen Formation. Prograding lacustrine delta deposits.||Evergreen Formation.||Is overlain by the Westgrove Ironstone Member.|Dominated by quartzose sandstone with very minor carbonaceous siltstone, shale and coal interbeds.|
2455|Boxvale Sandstone Member|69633|4|Described|p1, p3-7, p10-13, p20, Appendix 6.|Early Jurassic|Early Jurassic|Reeves (1947). Assigned to the Evergreen Formation by Jensen et al. (1964). Surat Basin. Contains acritarchs. GSQ Chinchilla 4 core log detailed. Palynology detailed.||Evergreen Formation.||Is overlain by Westgrove Ironstone Member.|Laterally restricted sandstones fed by incised fluvial feeder channels.|
2455|Boxvale Sandstone Member|69682|5|Briefly described|p92-94|Early Jurassic|Early Jurassic|Surat Basin.||Unit in Evergreen Formation.|||Quartzose, fine- to coarse-grained sandstone.|
2455|Boxvale Sandstone Member|70821|5|Briefly described|p80|||Eromanga, Surat Basins. Aquifer: generally artesian.||Evergreen Formation.||||
2455|Boxvale Sandstone Member|71805|6|Mentioned|p79-p80|||Surat Basin.||Evergreen Formation, upper||||15-MAY-19
2455|Boxvale Sandstone Member|71806|4|Described|p483, p485|||Surat Basin. Interpreted to have been deposited in a deltaic environment on the basis of coarsening-upwards nature in outcrop and abrupt capping by the Westgrove Ironstone Member.||Evergreen Formation.||Overlain by the Westgrove Ironstone Member.||
2455|Boxvale Sandstone Member|72297|5|Briefly described|p745|||Surat Basin. Deltaic deposits. Important in stratigraphic traps for hydrocarbons within the parent Formation.||Evegreen Formation.||||
2455|Boxvale Sandstone Member|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (QLD,NSW), Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||Evergreen FZ.||Is overlain by Hutton Sandstone.||
2455|Boxvale Sandstone Member|72921|5|Briefly described|p17.|Early Jurassic|Early Jurassic|Shows marine influence. May be characterised by hummocky cross-stratification. Described with Westgrove Ironstone Member. (Mollan et al., 1972; Exon et al., 1976; Fielding, 1996; McKellar, 1998; Turner et al., 2009; Brearley et al., 2018).||Evergreen Formation|||Sandstone that may include acritarchs, proximal and distal deltaic deposits, tidal bundles, chamositic oolites, pelecypods, anoxic black shales and tempestites.|
2455|Boxvale Sandstone Member|73113|6|Mentioned|p36, p69, p80|||||||||
2455|Boxvale Sandstone Member|73600|6|Mentioned|191|Toarcian|Toarcian|||Evergreen Formation||Overlain by Westgrove Ironstone Member.||
2470|Brackendale Metamorphics|31694|6|Mentioned|p345|||||||||
2470|Brackendale Metamorphics|38804|5|Briefly described|p95|||||||||
2470|Brackendale Metamorphics|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|Part of the "Coffs Harbour Association".||||||16-DEC-04
2470|Brackendale Metamorphics|42803|6|Mentioned|Fig.1 P112|||||||||
2470|Brackendale Metamorphics|42872|6|Mentioned|p103|||||||||
2470|Brackendale Metamorphics|71628|5|Briefly described|p2:7; p3:86|Carboniferous|Carboniferous|||Coffs Harbour Association.|||Pelitic.|
2487|Braidwood Granodiorite|23439|5|Briefly described|p132|||||||||
2487|Braidwood Granodiorite|24116|6|Mentioned|p26|||||||||
2487|Braidwood Granodiorite|24265|5|Briefly described|p1451|Pridoli|Ludlow|Age: 412 +/- 4Ma (K-Ar). Geological Province: Lachlan Fold Belt||||||
2487|Braidwood Granodiorite|24272|5|Briefly described|p1646|Early Devonian|Late Silurian|Age: 403+/-9 Ma.||||||09-MAR-05
2487|Braidwood Granodiorite|24520|5|Briefly described|p97, p98|Early Devonian|Late Silurian|Major pluton comprising northern part of essentially I-type Bega Batholith. Pluton is a multiple intrusion. Age: 401-415+/-4Ma (K-Ar), 399+/-6Ma (Rb-Sr, Wyborn and Owen 1986) and 402+/-6Ma (preliminary SHRIMP, I. Williams; pers. comm. 2003).||||||25-MAY-05
2487|Braidwood Granodiorite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2487|Braidwood Granodiorite|40276|1|Redefined|p11|Early Devonian|Early Devonian|Supersedes Braidwood Granite.||||||
2487|Braidwood Granodiorite|42497|5|Briefly described|Map legend|Zlichovian|Pragian|||||||
2487|Braidwood Granodiorite|46967|6|Mentioned|p298|||||||||
2487|Braidwood Granodiorite|60308|6|Mentioned|p39|||Intruded by mafic dyke swarms in the Middle Devonian (385-395 Ma)||||||
2487|Braidwood Granodiorite|66087|5|Briefly described|p15|Early Devonian|Early Devonian|[Age prob. U/Pb SHRIMP]. Hosts Dargues Reef gold deposit.|Age 410.8 +/- 3.2 Ma (Bodorkos & Simpson 2008).|||||10-MAY-12
2487|Braidwood Granodiorite|66300|5|Briefly described|pp35-41, 46.|||Hosts gold mineralisation at Dargues Reef.|411.3 +/- 2.6 Ma.|||Intrudes Long Flat Volcanics.|Massive, equigranular, hornblende granodiorite.|29-OCT-13
2487|Braidwood Granodiorite|66713|5|Briefly described|p2 Fig.1, p13||Lochkovian|Hosts the Dargues Reef intrusion-related gold deposit. Two U-Pb SHRIMP zircon ages: 410.2+/-3.1 Ma and 410.8+/-3.2 Ma (Bodorkos and Simpson, 2008).||||||
2487|Braidwood Granodiorite|67806|5|Briefly described|p110|||In northern part of Bega Batholith. Has 2 main intrusive phases. Hosts gold mineralisation in alteration zones as well as in discrete quartz and quartz-calcite veins. It is high in K, Ba and Rb and is relatively oxidised.||||||
2487|Braidwood Granodiorite|67847|5|Briefly described|p59|Early Devonian|Early Devonian|Hosts the Dargues Reef deposit. ||||||
2487|Braidwood Granodiorite|68592|6|Mentioned|p1680-1|||||Unit in Braidwood Suite.||||
2487|Braidwood Granodiorite|69159|5|Briefly described|Map legend|Pragian|Pragian|||Unit in Braidwood Suite.|||Grey and white to pink, medium-grained, massive, equigranular to porphyritic, hornblende +/- pyroxene granodiorite.|07-SEP-15
2487|Braidwood Granodiorite|69564|4|Described|p1-21|Early Devonian|Early Devonian|Collins et al. (1982). Hosts the primary gold mineralisation in the Dargues Reef-Majors Creek area. Metamorphism described. Mineralisation, ore geology, Ar/Ar dating, sulfur isotope results, intrusive history: all described in detail. Several other similar ages given.|412 +/- 4 Ma (K-Ar biotite; Wyborn and Owen, 1986)|Braidwood Suite.||Intrudes Long Flat Volcanics.|I-type. Multi-phase intrusion. Predominantly a hornblende-biotite quartz monzonite or granodiorite to a hornblende-clinopyroxene-biotite microgranodiorite. Metaluminous and unfractionated.|03-APR-19
2487|Braidwood Granodiorite|71069|6|Mentioned|p35, p61|Early Devonian|Early Devonian|||||||
2487|Braidwood Granodiorite|71699|5|Briefly described|Map legend.|Devonian|Devonian|Three facies are mapped separately.||Glenbog Suite.|||Grey and white to pink, medium-grained, massive, equigranular to porphyritic, hornblende+/-pyroxene granodiorite; high magnetic susceptibility; high K radioelement response.|
2487|Braidwood Granodiorite|71700|2|Defined|vi, viii, ix, p7, p10, p16, p26-p28|Early Devonian|Early Devonian|Named for the town of Braidwood at GR754107 6074135. A type locality is nominated at GR 761455 6075259 along the Mongarlowe Road. Synonymy is discussed in detail. A representative locality occurs adjacent to the Kings Highway at GR 751240 6083026.Distribution, geomorphic expression, outcrop, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. Lithology is discussed in great detail for each informal subdivision. Equivalent to the Euradux Granite. This unit is interpreted as the intrusive equivalent of the Long Flat Volcanics; this relationship is confirmed by geochronology. SHRIMP U-Pb ages are derived from Bodorkos & Simpson 2008 and Bodorkos et al, 2010, respectively. An additional age of of 409 +/- 3 Ma is provided from Bodorkos & Simpson, 2008. Ar-Ar dating of alteration-related muscovite by Forster et al, 2014 gives an age of 410.9 +/- 2 Ma (within error of the other dates provided). This unit has contact metamorphosed allocthonous limestone blocks in the Limekilns area with metamorphic porphyroblasts developed up to 2.5km away from the contact. Skarn mineralisation is associated with this unit in calcareous horizons of the Cardinal View Formation. Estimated thickness of up to 4km. See also  p30, CD, p39, p41-p42, p44, p54, p56-p57, p62, p66, p67, p71, p79, p81-p83, p86-p87, p96, p100-p103, p105-p112, p118-p119, p124-p126.|410.8 +/- 3.2 and 411.3 +/- 2.6 Ma|Braidwood Suite||Intrudes the Cardinal View Formation, Bendoc Group, Mundoonen Sandstone, De Drack Formation, Long Flat Volcanics and the Abercrombie Formation. Unconformably overlain by the Minuma Range Group.|Hornblende-phyric, I-type granodiorite, leucogranitic granodiorite and equigranular granodiorite.|
2498|Branxton Formation|22601|2|Defined|401, 411, 412,417|Permian|Permian|Geol province Sydney Basin. Underlying unit Greta Coal Measures||||||
2498|Branxton Formation|22610|4|Described|Fig 1||Early Permian|Maximum thickness 1300m , Age 272+/- 3.2Ma||||||
2498|Branxton Formation|22663|5|Briefly described|NSW97 -1 Fig.2|Late Permian|Late Permian|||||||01-MAR-10
2498|Branxton Formation|22857|4|Described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Maitland Group. Conglomerate, sandstone, siltstone; includes "Fenestella Shale". Max. thickness: 963m. Geological Province: Sydney Basin. See also p536 App.1 Tb.A1.9.||||||
2498|Branxton Formation|22969|4|Described|Fig 2.2|Permian|Early Permian|Kungarian 272 Ma - SHRIMP. Max. thickness: 900 m.||||||
2498|Branxton Formation|22970|5|Briefly described|Plate 6|Early Permian||||||||
2498|Branxton Formation|23350|5|Briefly described|274|Early Permian|Early Permian|272+/-3.2Ma.  See also misspelt Branxton Fromation (p261 Fig. 2).||||||15-JUL-04
2498|Branxton Formation|23438|6|Mentioned|p30|||||||||
2498|Branxton Formation|23540|4|Described|p 420|||Of the Maitland Group. Also see p 421 and 424||||||20-FEB-07
2498|Branxton Formation|24079|5|Briefly described|p433 Fig.6|Permian|Permian|Of Maitland Group. Geological Province: Sydney Basin.||||||
2498|Branxton Formation|24121|5|Briefly described|p4, p108, p126, 136|||Of Maitland Group.||||||25-AUG-22
2498|Branxton Formation|29437|6|Mentioned|p136|||||||||
2498|Branxton Formation|29752|6|Mentioned|p34|||||||||
2498|Branxton Formation|29915|4|Described|p68|||Upper Permian||||||
2498|Branxton Formation|30340|6|Mentioned|p2528|||Lithology||||||
2498|Branxton Formation|30341|4|Described|p136|||Lower Permian age||||||
2498|Branxton Formation|30545|6|Mentioned|Fig.2|||Lower Permian. See also P24||||||
2498|Branxton Formation|30555|6|Mentioned|p299|||||||||
2498|Branxton Formation|31081|6|Mentioned|p65|||See also P69, Fig. 2||||||
2498|Branxton Formation|31124|6|Mentioned|p17|||See also Fig. 1, 2, Table 1. Petrology||||||
2498|Branxton Formation|31125|6|Mentioned|p16|||Geology||||||
2498|Branxton Formation|31598|6|Mentioned|p39|||||||||
2498|Branxton Formation|31883|6|Mentioned|p594|||See also Table 1||||||
2498|Branxton Formation|32266|6|Mentioned|p24|||||||||
2498|Branxton Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
2498|Branxton Formation|32840|6|Mentioned|Table 1|||||||||
2498|Branxton Formation|32944|6|Mentioned|p710|||L.Perm.||||||
2498|Branxton Formation|33701|6|Mentioned|Fig.1|||L.Perm.||||||
2498|Branxton Formation|33702|6|Mentioned|p222|||Trilobites. Artinskian||||||
2498|Branxton Formation|33867|4|Described|p6|||Mention P3.||||||
2498|Branxton Formation|34015|6|Mentioned|p325|||Permian||||||
2498|Branxton Formation|34036|6|Mentioned|p434|||||||||
2498|Branxton Formation|34043|6|Mentioned|p450|||M.Perm.||||||
2498|Branxton Formation|34059|6|Mentioned|Map legend|Permian|Permian|||||||
2498|Branxton Formation|34138|6|Mentioned|Cor.Chart|||Artinskian - Kungurian||||||
2498|Branxton Formation|34170|6|Mentioned|p47|||Lower Permian||||||
2498|Branxton Formation|34292|6|Mentioned|Table 3|||Permian||||||
2498|Branxton Formation|34345|3|Fully described|p330|||Permian. Stratigraphic column Fig.5.8.||||||
2498|Branxton Formation|34444|6|Mentioned|Map legend|Permian|Permian|||||||
2498|Branxton Formation|34445|6|Mentioned|Fig.5.3|||||||||
2498|Branxton Formation|34447|5|Briefly described|p318|||Permian. See also Fig.5.2||||||
2498|Branxton Formation|34448|5|Briefly described|p431|||Permian||||||
2498|Branxton Formation|34466|6|Mentioned|Fig.5.22|||||||||
2498|Branxton Formation|34568|6|Mentioned|p218|||Permian||||||
2498|Branxton Formation|34569|6|Mentioned|p11|||Permian||||||
2498|Branxton Formation|34845|6|Mentioned|Fig.4|||||||||
2498|Branxton Formation|35530|6|Mentioned|p1|||Location of Bivalvia fossils.||||||
2498|Branxton Formation|35873|6|Mentioned|p116|||||||||
2498|Branxton Formation|36009|6|Mentioned|Table 1|||||||||
2498|Branxton Formation|36042|6|Mentioned|Table 1|||||||||
2498|Branxton Formation|36045|6|Mentioned|p332|||||||||
2498|Branxton Formation|36220|6|Mentioned|p16|||||||||
2498|Branxton Formation|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
2498|Branxton Formation|36899|6|Mentioned|p1090|||||||||
2498|Branxton Formation|37082|6|Mentioned|p161|||||||||
2498|Branxton Formation|37086|6|Mentioned|p183|||||||||
2498|Branxton Formation|37087|6|Mentioned|p192|||||||||
2498|Branxton Formation|37773|4|Described|p22|||||||||
2498|Branxton Formation|37922|5|Briefly described|p483|||||||||
2498|Branxton Formation|38586|6|Mentioned|p25|||||||||
2498|Branxton Formation|38614|6|Mentioned|p14|||See also Fig. 6||||||
2498|Branxton Formation|38656|5|Briefly described|Fig.1.5.13|||P280||||||
2498|Branxton Formation|38917|6|Mentioned|p166|||||||||
2498|Branxton Formation|39267|6|Mentioned|p243|||||||||
2498|Branxton Formation|39268|6|Mentioned|Fig. 5|||||||||
2498|Branxton Formation|39287|6|Mentioned|p20|||See also Fig.2.5||||||
2498|Branxton Formation|39288|4|Described|p61|||||||||
2498|Branxton Formation|39289|6|Mentioned|p81|||||||||
2498|Branxton Formation|39290|5|Briefly described|p90|||||||||
2498|Branxton Formation|39304|5|Briefly described|p364|||Fauna||||||
2498|Branxton Formation|39307|6|Mentioned|p438|||Foraminifera||||||
2498|Branxton Formation|39308|5|Briefly described|p477|||||||||
2498|Branxton Formation|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
2498|Branxton Formation|39830|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
2498|Branxton Formation|40224|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
2498|Branxton Formation|40256|6|Mentioned|p306|||||||||
2498|Branxton Formation|40331|6|Mentioned|p7|||See also P15||||||
2498|Branxton Formation|40636|6|Mentioned|p43|||||||||
2498|Branxton Formation|41010|6|Mentioned|Fig.1|||||||||
2498|Branxton Formation|41054|6|Mentioned|p151|||||||||
2498|Branxton Formation|41275|6|Mentioned|p27|||||||||
2498|Branxton Formation|41475|6|Mentioned|p69|||||||||
2498|Branxton Formation|41580|5|Briefly described|p7|||||||||
2498|Branxton Formation|41604|6|Mentioned|Fig.2|||||||||
2498|Branxton Formation|41834|6|Mentioned|p590|||||||||
2498|Branxton Formation|41902|5|Briefly described|p5 Table 1|||||||||
2498|Branxton Formation|41903|6|Mentioned|Map legend|Late Permian||||||||
2498|Branxton Formation|42477|5|Briefly described|p124|||||||||
2498|Branxton Formation|42780|6|Mentioned|Table 1 P417|||||||||
2498|Branxton Formation|42916|5|Briefly described|Table 1||Middle Permian|||||||
2498|Branxton Formation|42925|5|Briefly described|Table 1||Early Permian|||||||
2498|Branxton Formation|42994|6|Mentioned|p234|||||||||
2498|Branxton Formation|43018|5|Briefly described|Table 1,p386|||||||||
2498|Branxton Formation|43050|5|Briefly described|p6|||||||||
2498|Branxton Formation|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 Porcupine Formation in the Gunnedah Basin. ||||||
2498|Branxton Formation|43257|5|Briefly described|Map Legend||Permian|Age Middle Permian. Of Maitland Group.||||||
2498|Branxton Formation|43344|14|Not recorded|p84,88||Permian|||||||
2498|Branxton Formation|43383|14|Not recorded|p20|||||||||
2498|Branxton Formation|43440|14|Not recorded|p32,35,62,65,71,72,|||p83,84,90||||||
2498|Branxton Formation|43447|2|Defined|p18,19,48||Permian|inc. Muree Sandstone Member, Cessnock Sandstone Member.||||||24-SEP-08
2498|Branxton Formation|43451|14|Not recorded|Map Legend||Permian|Unit of Maitland Group. Contains: Muree Sandstone Member||||||
2498|Branxton Formation|44093|6|Mentioned|p 64 Photo 4|||Geological Province: Sydney Basin.||||||
2498|Branxton Formation|44219|14|Not recorded|p29-31,32-34,39|Kungurian|Artinskian|||||||
2498|Branxton Formation|44244|4|Described|p233|Early Permian|Early Permian|Of the Maitland Group.  Max. thickness: 752m.  Type section in text.  Geological Province: Sydney Basin.||||||
2498|Branxton Formation|44855|14|Not recorded|p18||Permian|||||||
2498|Branxton Formation|44859|14|Not recorded|p69||Permian|||||||
2498|Branxton Formation|45031|14|Not recorded|p48-56,60,62,67,68|||Of Maitland Group.||||||
2498|Branxton Formation|45088|6|Mentioned|p59|||Permian succession||||||
2498|Branxton Formation|45090|5|Briefly described|p26|||Rock units. See also P42. Isopach map.||||||
2498|Branxton Formation|48940|6|Mentioned|p99|||||||||
2498|Branxton Formation|50268|5|Briefly described|Map Legend|Kazanian|Artinskian|Geological Province: Sydney Basin.  Overlies: Greta Coal Measures. Underlies: Muree Sandstone, Mulbring Siltstone.  Of the Maitland Group.||||||
2498|Branxton Formation|60281|4|Described|p9, p58|Late Permian|Early Permian|Of the Maitland Group.  Sandstone, siltstone, conglomerates, coals and rare tuffs. Age: 273-267 Ma. Max. thickness: 900m.||||||27-APR-05
2498|Branxton Formation|60290|5|Briefly described|p47|||Fossiliferous sediment. Geological Province: Cranky Corner Basin.||||||07-FEB-11
2498|Branxton Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Maitland Group. Geological Province: Sydney Basin||||||
2498|Branxton Formation|61529|5|Briefly described|p853, p854 Fig. 1b|Late Permian|Late Permian|Of the Maitland Group. Overlies Greta Coal Measures. Geological Province: Sydney Basin.||||||
2498|Branxton Formation|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin. NSW.||||||13-MAR-09
2498|Branxton Formation|61772|6|Mentioned|p129||Early Permian|||||||
2498|Branxton Formation|63773|6|Mentioned|p1059|||||||||
2498|Branxton Formation|63832|5|Briefly described|p131 fig 2, p136|Roadian|Kungurian|Cranky Corner/Gresford block, Southern New England Fold Belt; also NE Sydney Basin. Seventh glaciation (P3). Dominantly glaciomarine deposits.||Unit in Maitland Group.||||
2498|Branxton Formation|64631|6|Mentioned|p44 Fig.2, p49.|Guadalupian|Cisuralian|Southern New England Fold Belt, Cranky Corner/Gresford Block; and Sydney Basin. Distal glaciomarine deposits.||Unit in Maitland Group.||Appears to be disconformably overlain by Mulbring Siltstone.||
2498|Branxton Formation|67663|6|Mentioned|p518|Permian|Permian|Occurs at the base of the Maitland Group. Derived from underlying fluvio-deltaic sediments.||Of the Maitland Group.||||
2498|Branxton Formation|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||Maitland Group.||Overlies Greta Coal Measures. Is overlain by Muree Sandstone.||
2498|Branxton Formation|68003|5|Briefly described|p38 Fig.3-j, p40, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Basal unit in Maitland Group.||Overlies Rowan Formation. Is overlain by Muree Sandstone.|Conglomerate, sandstone, siltstone.|
2498|Branxton Formation|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields.||Basal unit in Maitland Group.||Overlies Rowan Formation (Greta Coal Measures). Is overlain by Muree Sandstone.||
2498|Branxton Formation|68493|4|Described|p1, p3 Fig.1, p4-6, p14, p17-19, p21|Wordian|Wordian|Northern Sydney Basin. SHRIMP zircon dating by Roberts et al. (1996), close to the Mulbring quarry site. Deposited in a steady marine transgression. Revised Wordian age due to CA-IDTIMS dating of the constituent Fenestella Shale Member. Deposited during Fielding et al.'s (2008) glacial episode P3.|ca. 272.2 +/- 3.2 Ma|Basal unit of the Maitland Group.|Includes the Fenestella Shale Member.|Overlies Greta Coal Measures. Overlain by the Muree Sandstone.|Conglomerate, sandstone, siltstone.|
2498|Branxton Formation|69297|6|Mentioned|p501, p502 fig 5.43, p503|Wordian|Kungurian|Sydney Basin. Has good oil and gas source rock potential. ||Maitland Group||Overlies and interfingers with the Greta Coal Measures. Overlain by the Muree Sandstone.||
2498|Branxton Formation|69683|6|Mentioned|p411 Fig.2|Middle Permian|Middle Permian|||Unit in Maitland Group.||||
2498|Branxton Formation|70096|5|Briefly described|p220-221|||Of northern Sydney Basin. See also supplementary files in appendix for additional stratigraphic and locality information.||||Correlable to Wandrawandian Siltstone.||
2498|Branxton Formation|70661|6|Mentioned|p165|Roadian|Kungurian|Hunter Valley (North Sydney Basin). Crystallisation age of the tuffaceous siltstone.|272 +/- 3 Ma (SHRIMP)|Maitland Group||Equivalent to Wandrawandian Formation.|Tuffaceous siltstone.|
2498|Branxton Formation|70791|5|Briefly described|p277, p283, p293 Fig.17|Guadalupian|Guadalupian|Hunter Coalfield.||Maitland Group.|Jasdec Park Sandstone Member.|||
2498|Branxton Formation|70878|5|Briefly described|p712, p715 Fig.10, p720-721|Permian|Permian|Hunter Valley. Calibration of palynological ages.||Maitland Group.||Overlies Rowan Formation.||
2498|Branxton Formation|73304|6|Mentioned|p75-76, p78|||Sydney Basin, northern. Hunter Valley. Includes evidence of the P3 glacial episode.||Maitland Group||||
2498|Branxton Formation|73421|6|Mentioned|p17|||Sydney Basin, northern. Correlated to Wandrawandian Siltstone in terms of biostratigraphy and sedimentary facies. U-Pb zircon age of 272.2+/-3.2 Ma (Roberts at el., 1996) adjusted to approx. 275 Ma (late Kungurian) due to use of the SL13 standard.|Approx. 275 Ma|||||
2538|Bridge Creek Limestone Member|23214|3|Fully described|p105|Llandovery|Llandovery|Of Bagdad Formation.  Contains abundant corals, algal remains, brachipods, bryozoans, conodonts and gastropods. Maximum thickness: 36m.||||||
2538|Bridge Creek Limestone Member|35258|4|Described|p116|||||||||
2538|Bridge Creek Limestone Member|40328|3|Fully described|p141|||||||||
2538|Bridge Creek Limestone Member|41048|6|Mentioned|p23|||||||||
2538|Bridge Creek Limestone Member|43385|14|Not recorded|p171|||Late Ordovician or Early Silurian||||||
2538|Bridge Creek Limestone Member|43470|14|Not recorded|p159|||See also Lexicon. Orange district.||||||
2538|Bridge Creek Limestone Member|48971|6|Mentioned|p39-40|||||||||
2538|Bridge Creek Limestone Member|63290|5|Briefly described|p401 Fig. 5(d)|Llandovery|Llandovery|Of Ashburnia Group. Overlain by Bagdad Formation.||||||
2538|Bridge Creek Limestone Member|70684|6|Mentioned|p50 Fig.24|||||Bagdad Formation.||||
2570|Bringelly Shale|22500|4|Described|p6, 7, 12  Fig 9||Triassic|Wianamatta Group||||||
2570|Bringelly Shale|22745|6|Mentioned|Fig14,p138|||Wianamatta Group, Sydney Basin.||||||
2570|Bringelly Shale|22857|4|Described|p530 App.1 Tb.A1.9|Middle Triassic|Middle Triassic|Of the Wianamatta Group. Shale, carbonaceous claystone, laminite, lithic sandstone, rare coal. Max. thickness: 257m. Geological Province: Sydney Basin. See also p265 (photo 2). ||||||
2570|Bringelly Shale|22864|6|Mentioned|p265|||||||||
2570|Bringelly Shale|22969|5|Briefly described|p 26|||||||||
2570|Bringelly Shale|29361|6|Mentioned|p3|||On table.||||||
2570|Bringelly Shale|30132|6|Mentioned|Table 1|||||||||
2570|Bringelly Shale|30286|6|Mentioned|p1099|||Stratigraphic table||||||
2570|Bringelly Shale|31056|5|Briefly described|p3|||||||||
2570|Bringelly Shale|31296|6|Mentioned|p29|||||||||
2570|Bringelly Shale|31725|6|Mentioned|p4|||||||||
2570|Bringelly Shale|32187|6|Mentioned|p6|||||||||
2570|Bringelly Shale|32801|6|Mentioned|Fig.10|||||||||
2570|Bringelly Shale|33671|6|Mentioned|p3|||||||||
2570|Bringelly Shale|34305|2|Defined|p421|Triassic|Triassic|See also Table 5.26||||||
2570|Bringelly Shale|34306|5|Briefly described|p443|||||||||
2570|Bringelly Shale|35095|6|Mentioned|p116|||||||||
2570|Bringelly Shale|35098|6|Mentioned|p4|||||||||
2570|Bringelly Shale|35312|6|Mentioned|p3|||||||||
2570|Bringelly Shale|35416|6|Mentioned|p7|||Stratigraphy and palynological framework on Fig.2||||||
2570|Bringelly Shale|35502|6|Mentioned|Fig.1|||Also on Table 1||||||
2570|Bringelly Shale|35690|1|Redefined|p182|Middle Triassic|Middle Triassic|||||||
2570|Bringelly Shale|36042|6|Mentioned|Fig.22|||||||||
2570|Bringelly Shale|36220|6|Mentioned|p91|||||||||
2570|Bringelly Shale|36804|6|Mentioned|p9|||||||||
2570|Bringelly Shale|37757|6|Mentioned|p29|||||||||
2570|Bringelly Shale|38206|6|Mentioned|p53|||Clay resources||||||
2570|Bringelly Shale|39287|6|Mentioned|Fig. 2.18|||||||||
2570|Bringelly Shale|39298|3|Fully described|p257|||See also PP266-272||||||
2570|Bringelly Shale|39300|6|Mentioned|p309|||||||||
2570|Bringelly Shale|39306|6|Mentioned|p390|||See also P429||||||
2570|Bringelly Shale|39626|6|Mentioned|p275|||||||||
2570|Bringelly Shale|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
2570|Bringelly Shale|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
2570|Bringelly Shale|40518|6|Mentioned|p344|||||||||
2570|Bringelly Shale|40592|5|Briefly described|p229|||||||||
2570|Bringelly Shale|40602|3|Fully described|p25|||||||||
2570|Bringelly Shale|40625|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
2570|Bringelly Shale|40629|6|Mentioned|p191|||||||||
2570|Bringelly Shale|40631|6|Mentioned|p156|||||||||
2570|Bringelly Shale|40651|6|Mentioned|Table 6|||||||||
2570|Bringelly Shale|40653|6|Mentioned|p121|||||||||
2570|Bringelly Shale|40767|6|Mentioned|p9|||||||||
2570|Bringelly Shale|42182|6|Mentioned|p300|||||||||
2570|Bringelly Shale|42664|5|Briefly described|p21|||See misspelling Bansk...||||||
2570|Bringelly Shale|42737|5|Briefly described|map legend|Triassic||||||||
2570|Bringelly Shale|42795|6|Mentioned|p25|||of Wianamatta Group||||||
2570|Bringelly Shale|42896|3|Fully described|p46, Table 2|||of Wianamatta Group||||||
2570|Bringelly Shale|42909|6|Mentioned|p3|||||||||
2570|Bringelly Shale|42925|3|Fully described|p24|||of Wianamatta Group||||||
2570|Bringelly Shale|42926|4|Described|map legend||Middle Triassic|||||||
2570|Bringelly Shale|43194|5|Briefly described|p122, p127, p131|Middle Triassic|Middle Triassic|Sydney Basin. Lagoonal and peat marsh facies. Time equivalent to the Deriah Formation and upper part of the Napperby Formation, Gunnedah Basin.||||||
2570|Bringelly Shale|43317|4|Described|Table 1 p13|||See also Lexicon||||||
2570|Bringelly Shale|43318|14|Not recorded|opp p6||Late Triassic|||||||
2570|Bringelly Shale|43319|14|Not recorded|Map Legend|||||||||
2570|Bringelly Shale|43320|14|Not recorded|Table 1 p13,14|||Part of Liverpool Sub-group||||||
2570|Bringelly Shale|43341|14|Not recorded|p229,230|||||||||
2570|Bringelly Shale|43344|14|Not recorded|p22,59,60,61|||Formation of Wianamatta Group||||||
2570|Bringelly Shale|43365|14|Not recorded|p169-210||Triassic|||||||
2570|Bringelly Shale|43383|14|Not recorded|p23|||||||||
2570|Bringelly Shale|43385|14|Not recorded|p182, Table||Triassic|Keuper||||||
2570|Bringelly Shale|43395|14|Not recorded|map|||||||||
2570|Bringelly Shale|45018|14|Not recorded|p162-8,172-6,180|||||||||
2570|Bringelly Shale|45090|6|Mentioned|p72|||Palynological zones||||||
2570|Bringelly Shale|60281|6|Mentioned|p64|Triassic|Triassic|||||||
2570|Bringelly Shale|61315|5|Briefly described|p176|Middle Triassic|Middle Triassic|Of the upper Wianamatta Group. Flood basin and meandering channels deposits. Geological Province: Sydney Basin||||||
2570|Bringelly Shale|65195|5|Briefly described|p3, p4 Fig.2|Triassic|Triassic|Of Wianamatta Group. Predominantly claystone and siltstone. Overlies Minchinbury Sandstone||||||
2570|Bringelly Shale|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Wianamatta Group.||||
2570|Bringelly Shale|67663|6|Mentioned|p521|Triassic|Triassic|||Of the Wianamatta Group||||
2570|Bringelly Shale|70661|3|Fully described|ix, p213, p216-p220|Middle Triassic|Middle Triassic|Named for the town of Bringelly. Originally a part of the undifferentiated Wianamatta Group and then the Liverpool Sub-group before the current definition was made. Distribution, geomorphology, structure, geochemistry, fossil assemblage, distinguishing features discussed. Deposited on an alluvial plain. Maximum thickness of 256.7m based on drillcore.||Wianamatta Group|Mount Hercules Sandstone Member, Razorback Sandstone Member, Potts Hill Sandstone Member, Cobbitty Claystone Bed|Conformably overlies Minchinbury Sandstone.|Shale - claystone or carbonaceous claystone. Sandstone, siltstone, coal and mudstone also present.|
2570|Bringelly Shale|71303|5|Briefly described|map legend|Middle Triassic|Middle Triassic|Of Sydney Basin.||Of Wianamatta Group.|||Light - dark grey, sideritic claystone - siltstone, dark grey carbonaceous claystone, sandstone - siltstone, quartz-lithic v fine to medium-grained sandstone. Plant fragments abundant locally. Strongly weathered; extensive soil development.|
2570|Bringelly Shale|73248|6|Mentioned|p301, p307|Middle Triassic|Middle Triassic|||Wianamatta Group||Unconformably overlain by Rickabys Creek Gravel.||
2570|Bringelly Shale|75059|6|Mentioned|p4, 9-10|Middle Triassic|Middle Triassic|Sydney Basin.||Wianamatta Group.||Overlies Minchinbury Sandstone.||
2589|Broad Gully Formation|34556|5|Briefly described|p267|||Permian||||||
2589|Broad Gully Formation|40872|6|Mentioned|Fig.1|||||||||
2589|Broad Gully Formation|43385|14|Not recorded|p179||Kungurian|||||||
2589|Broad Gully Formation|43447|14|Not recorded|p28|||||||||
2589|Broad Gully Formation|44244|6|Mentioned|p168 Tb. 2|Late Permian|Late Permian|||||||
2617|Broken Hill Group|6823|6|Mentioned|p203, 205, 210, 221, 234, 236|Palaeoproterozoic|Palaeoproterozoic||ca >1690 Ma|Willyama Supergroup|Includes the Hores Gneiss.|||26-MAR-22
2617|Broken Hill Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent WIllyama Supergroup Geol province Broken Hill - Olary Domain||||||
2617|Broken Hill Group|22500|4|Described|p 1, 3, 13, 14|||Of the Willyama Supergroup.||||||18-JAN-07
2617|Broken Hill Group|22553|5|Briefly described|fig2p77,p78|Proterozoic|Proterozoic|||||||
2617|Broken Hill Group|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
2617|Broken Hill Group|22588|6|Mentioned|p85|||||||||
2617|Broken Hill Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
2617|Broken Hill Group|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22665|6|Mentioned|P231|||||||||
2617|Broken Hill Group|22720|6|Mentioned|p 168|||||||||
2617|Broken Hill Group|22771|5|Briefly described|p40-42,48|||||||||
2617|Broken Hill Group|22789|6|Mentioned|p50|||||||||
2617|Broken Hill Group|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Supersedes the Broken Hill Suite.  Max. thickness: 2000m. Geological Province: Willyama Fold Belt.|Age: 1690+/-5 Ma|Of Willyama Supergroup||||11-MAR-10
2617|Broken Hill Group|22884|5|Briefly described|p40 Fig1, p43 Fig. 3||Paleoproterozoic|||||||26-MAR-09
2617|Broken Hill Group|22955|6|Mentioned|160||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22956|6|Mentioned|p147||Proterozoic|||||||
2617|Broken Hill Group|22959|4|Described|p95||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22960|5|Briefly described|p92||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|22962|5|Briefly described|p73||Statherian|||||||
2617|Broken Hill Group|22963|5|Briefly described|p69||Paleoproterozoic|Broad correlation with the Fullarton River Group of the Mt Isa Maronan Supergroup, and the lower sequence of the Georgetown (Qld) Etheridge Group.||||||07-NOV-08
2617|Broken Hill Group|22964|5|Briefly described|p54,55,56||Proterozoic|||||||
2617|Broken Hill Group|22965|6|Mentioned|p13,14,Fig1||Statherian|||||||
2617|Broken Hill Group|22966|5|Briefly described|p2,3,4||Proterozoic|Rift stage of development.||||||
2617|Broken Hill Group|22967|5|Briefly described|p25,6,30-2,9,41,2,5,||Statherian|||||||
2617|Broken Hill Group|23025|6|Mentioned|p76|||||||||
2617|Broken Hill Group|23039|6|Mentioned|p166||Statherian|||||||
2617|Broken Hill Group|23093|5|Briefly described|p619|||||||||
2617|Broken Hill Group|23160|5|Briefly described|p870 fig1|||||||||
2617|Broken Hill Group|23196|6|Mentioned|p830|||||||||
2617|Broken Hill Group|23223|5|Briefly described|p42|||Informally divided into upper and lower.  Of the informal Upper Willyama Supergroup.  In the Curnamona Province.||||||18-JAN-07
2617|Broken Hill Group|23248|5|Briefly described|Fig2p169, 179|||||||||
2617|Broken Hill Group|23346|6|Mentioned|48|||||||||
2617|Broken Hill Group|23347|5|Briefly described|p54|||Geological province: Broken Hill Domain. Equivalent to Olary Domain rocks of the Strathearn Group.||||||24-MAR-09
2617|Broken Hill Group|23461|5|Briefly described|p202|||||||||
2617|Broken Hill Group|23476|5|Briefly described|p50|||Underlain by the  'Bimba Formation'.||||||29-MAY-07
2617|Broken Hill Group|23565|5|Briefly described|p195|||||||||
2617|Broken Hill Group|23912|5|Briefly described|p779|||Of the Willyama Supergroup.||||||
2617|Broken Hill Group|23966|5|Briefly described|p1309|Proterozoic|Proterozoic|Age: 1690 +/- 5Ma.||||||
2617|Broken Hill Group|24197|5|Briefly described|p62, p132|||Of the Willyama Supergroup. Shallow marine unit. Includes Hores Gneiss and Silver King Formation. Geological province: Broken Hill Block.||||||07-FEB-11
2617|Broken Hill Group|24307|4|Described|p974|Proterozoic|Proterozoic|||||||
2617|Broken Hill Group|38969|4|Described|p208|||||||||
2617|Broken Hill Group|39662|2|Defined|p422|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|39674|6|Mentioned|p204|||||||||
2617|Broken Hill Group|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|39849|6|Mentioned|p87|||||||||
2617|Broken Hill Group|39883|6|Mentioned|p380|||||||||
2617|Broken Hill Group|40290|6|Mentioned|p1|||||||||
2617|Broken Hill Group|40595|6|Mentioned|p85|||||||||
2617|Broken Hill Group|40822|6|Mentioned|Fig.2|||||||||
2617|Broken Hill Group|41093|4|Described|p253|||||||||
2617|Broken Hill Group|41145|5|Briefly described|p827|||||||||
2617|Broken Hill Group|41630|5|Briefly described|p6|||See also Table 1.5.||||||
2617|Broken Hill Group|41633|6|Mentioned|p145|||||||||
2617|Broken Hill Group|41651|6|Mentioned|p189|||||||||
2617|Broken Hill Group|41652|6|Mentioned|p193|||||||||
2617|Broken Hill Group|42098|6|Mentioned|p57|||||||||
2617|Broken Hill Group|42171|6|Mentioned|p142|||||||||
2617|Broken Hill Group|42181|6|Mentioned|Fig,1 P252|||||||||
2617|Broken Hill Group|42261|6|Mentioned|p529|||See also Fig.1 P530||||||
2617|Broken Hill Group|42286|6|Mentioned|p7|||||||||
2617|Broken Hill Group|42323|4|Described|p3-4|||Depositional age 1680-1690 Ma.||||||29-MAY-07
2617|Broken Hill Group|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42537|4|Described|p12|||||||||
2617|Broken Hill Group|42595|6|Mentioned|Fig. 2 P5|||||||||
2617|Broken Hill Group|42672|5|Briefly described|p372|||||||||
2617|Broken Hill Group|42720|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
2617|Broken Hill Group|42813|6|Mentioned|p9|||||||||
2617|Broken Hill Group|42819|5|Briefly described|p316|||||||||
2617|Broken Hill Group|42897|5|Briefly described|Fig.3 P321|||||||||
2617|Broken Hill Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
2617|Broken Hill Group|43052|5|Briefly described|p82,Fig.4.22|||Of Willyama Supergroup. Deposition at about 1690+/-5 Ma.||||||18-JAN-07
2617|Broken Hill Group|43086|6|Mentioned|p3|||||||||
2617|Broken Hill Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
2617|Broken Hill Group|43264|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
2617|Broken Hill Group|43572|5|Briefly described|p5|||||||||
2617|Broken Hill Group|43583|4|Described|p2138||Proterozoic|Age: 1690+/-5 Ma.  Of Willyama Supergroup.||||||18-JAN-07
2617|Broken Hill Group|43591|6|Mentioned|p162|||||||||
2617|Broken Hill Group|43595|5|Briefly described|p355|||||||||
2617|Broken Hill Group|44195|6|Mentioned|p349|||||||||
2617|Broken Hill Group|46598|4|Described|p303|||||||||
2617|Broken Hill Group|50045|4|Described|p115 Fig. 2, p116, p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Sundown Group; underlain by Thackaringa Group. Age: 1690 Ma. Includes Purnamoota Subgroup. Package of pelitic to psammopelitic metasediments and minor calc-silicate rocks,|Age: 1690 Ma|||||10-DEC-09
2617|Broken Hill Group|50606|5|Briefly described|p1.1|||Of the Willyama Supergroup. Geological Province: Broken Hill Block.||||||27-JUL-04
2617|Broken Hill Group|50619|5|Briefly described|p174 Fig 1, p175|Paleoproterozoic|Paleoproterozoic|Conformably overlies the Thackaringa Group; conformably overlain by the Sundown Group.  Geological Province: Broken Hill Block.||Of the Willyama Supergroup||||28-FEB-13
2617|Broken Hill Group|60485|5|Briefly described|p27 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Domain.||||||07-NOV-08
2617|Broken Hill Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: Broken Hill.||||||07-NOV-08
2617|Broken Hill Group|61605|5|Briefly described|p769|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Broken Hill domain.||||||07-NOV-08
2617|Broken Hill Group|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||
2617|Broken Hill Group|61735|5|Briefly described|p634, p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Age: ca.1693-1683 Ma. Discussed from a geochronological aspect. Geological province: Broken Hill Domain. See also p636 Fig. 2.||||||04-JUN-15
2617|Broken Hill Group|61736|4|Described|p663|Paleoproterozoic|Paleoproterozoic|Comprises Allendale Metasediments, Parnell Formation, Freyers Metasediments and Hores Gneiss. Geological province: Broken Hill Domain.||||||24-FEB-10
2617|Broken Hill Group|61908|5|Briefly described|p146|||Geological Province: Broken Hill Block.||||||
2617|Broken Hill Group|61936|6|Mentioned|p203|||Geological Province: Curnamona Province. ||||||
2617|Broken Hill Group|62373|6|Mentioned|p502, p503|Paleoproterozoic|Paleoproterozoic|In Broken Hill region, NSW. Geological Province: Curamona Province/Broken Hill Domain.||||||07-NOV-08
2617|Broken Hill Group|62473|5|Briefly described|p72, p74|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||17-JUN-09
2617|Broken Hill Group|62535|5|Briefly described|p663-667, p671-674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, SE Curnamona Province. Time-equivalent to the Prize Supersequence. Hosts rich strata-bound Pb-Zn-Ag mineralization.|~1695-1685 Ma.|Willyama Supergroup.|Hores Gneiss.|||
2617|Broken Hill Group|62536|5|Briefly described|p633-636, 638, 643-644, 646-647, 655|||See also p658. Broken Hill area. The upper part of this unit hosts the Pb-Zn-Ag orebody. The package was deposited within a period of 10 m.y. Similar zircon provenance ages as Sundown Group and upper Paragon Group.|1693 +/- 4 Ma to 1685 +/- 3 Ma (dep'n).|Willyama Supergroup.|Allendale, Freyers Metasediments; Parnell Formation; Hores, Rasp Ridge Gneisses.|Is overlain by Sundown Group.||
2617|Broken Hill Group|62592|5|Briefly described|p14, p16 Fig.2.2.|||Formed during crustal extension. Hosts the 300 mt Broken Hill Pb-Zn-Ag deposit.||Unit in Willyama Supergroup.|Includes Allendale and Fryers Metasediments; Purnamoota Subgroup; Silver King Formation and Ettlewood Calc-silicate Member.|Intruded by Lady Louise Suite. Is overlain by Sundown Group.|Metasediments, mafic and felsic igneous rocks.|
2617|Broken Hill Group|62728|5|Briefly described|p25 Fig. 2|||Geological Province: Curnamona Province.||||||07-FEB-11
2617|Broken Hill Group|62993|5|Briefly described|p1, 2, 4, 8, 12, 14,  18, 19, 35, 37, 39|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.Broken Hill Group equivalents in the Olary Domain discussed p6.||Willyama Supergroup|Includes Purnamoota Subgroup, Allendale Metasediments|Correlated with parts of the Saltbush Group.||19-DEC-21
2617|Broken Hill Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
2617|Broken Hill Group|63102|5|Briefly described|p6,9-11,13-14,26-27,30,32-34,36,38|||Geological province: Broken Hill Domain, Curnamona Province. See also p44, p53, ,58-60.|||Includes Parnell Formation and Hores Gneiss.|Equivalent to Oonatra Creek Formation and Plumbago Formation.||22-OCT-19
2617|Broken Hill Group|63110|6|Mentioned|p1129 Fig. 8, p1131|||Comprises metasedimentary and metavolcanic rocks.||||||11-JUN-08
2617|Broken Hill Group|63186|5|Briefly described|p66, p67, p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1695 Ma and 1594+/-17 Ma (monazite mean). Geological Province: Broken Hill Domain, Curnamona Province. Intruded by Rasp Ridge and Hores Gneisses.||||||07-NOV-08
2617|Broken Hill Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metasediments, garnetiferous, quartzo-feldspathic gneiss, amphibolite, minor garnet and gahnite-rich rocks, BIF in Broken Hill Domain; unnamed equivalents in Olary Domain, including Bimba Formation.||||||07-NOV-08
2617|Broken Hill Group|63519|5|Briefly described|p5, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metasediments, Parnell Formation, Hores Gneiss and Silver King Formation. Overlain by Sundown Group; overlies Thackaringa Group. .  Age at top: 1686+/-3ma for topmost unit (Hores Gneiss). ||||||07-NOV-08
2617|Broken Hill Group|63866|4|Described|p34-p36, p38, p40|||Broken Hill Domain, Curnamona Province. Is greatly thinned or completely absent in the Olary Domain. Hosts the Broken Hill Deposit the worlds largest Pb-Zn-Ag deposit.||Willyama Supergroup|Includes the Purnamoota Subgroup and the Allendale Metasediments.|Intruded by the Rasp Ridge Gneiss. Equivalent to the Saltbush Group.||
2617|Broken Hill Group|64097|5|Briefly described|p302, p324|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metaseds, Parnell Fm, Freyers Metaseds+Hores Gneiss.Overlies Thackaringa Group. Age: ca1693-1685Ma. Geol.prov: Broken Hill Domain/Curnamona Province. Comprises siliciclastic metasediments with distinctive Potosi-type gneiss at 2 levels||||||07-FEB-11
2617|Broken Hill Group|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.||Unit in Willyama Supergroup.||||
2617|Broken Hill Group|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of lower Willyama Supergroup. Includes Purnamoota Subgroup and Allendale Metasediments. Overlies Thackaringa Gp. Hosts Broken Hill ore body. Geol.Prov: Broken Hill Block||||||07-FEB-11
2617|Broken Hill Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
2617|Broken Hill Group|64725|6|Mentioned|p58 Fig.2. |||||||||
2617|Broken Hill Group|64741|4|Described|p299-300, p309, p310|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metasediments and the Purnamoota Subgp. Overlies Himalaya Fm (Thackeringa Gp); overlain by Sundown Gp. Max. thickness: 2000m. Geological province: Broken Hill Domain (restricted in Olary Domain). Manganiferous.||Of Willyama Supergroup||||07-FEB-11
2617|Broken Hill Group|64742|5|Briefly described|p319, p323, p328, p330. |Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1695-1685 Ma.|Unit in Willyama Supergroup.|Includes Ettlewood Calc-Silicate Member, Allendale Metasediments, Parnell Formation, Freyers Metasediments and Hores Gneiss.|||
2617|Broken Hill Group|64743|6|Mentioned|pp339-340, p342, p344 Fig.5. |Paleoproterozoic|Paleoproterozoic|||Unit in Willyama Supergroup.||Overlies Thackaringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|64744|6|Mentioned|p353 Fig.4, p358, p363.|Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Thackaringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Allendale Metasediments. Geological province: Broken Hill Domain.||||||07-FEB-11
2617|Broken Hill Group|65220|6|Mentioned|p21 Fig.4|Statherian|Statherian|and equivalents, 1685-1680 Ma||||||10-DEC-09
2617|Broken Hill Group|65407|6|Mentioned|p239 Fig.3|||||||||
2617|Broken Hill Group|65681|6|Mentioned|p734 Fig. 1.|||Broken Hill Block.||||||
2617|Broken Hill Group|65887|6|Mentioned|p51-53|||Fe-rich amphibolites from this unit are spatially and temporally associated with felsic rocks of Hores Gneiss, which has been dated at 1685 +/- 3 Ma. Is overlain by Sundown and Paragon Groups.||||||
2617|Broken Hill Group|65925|5|Briefly described|Appendix 2.||||||||Sulfide-rich ironstone; marble; plagioclase-rich metasediment; calc-silicate; siliciclastic pelite; BIF; variably brecciated amphibolite.|
2617|Broken Hill Group|66302|5|Briefly described|p8, p35-37, p39-40|||Olary Domain, Curnamona Province.||Willyama Supergroup|Includes the Allendale Metasediments and the Purnamoota Subgroup|Equivalent to the Saltbush Group.|Quartz-rich sandstone and mudstone metasedimentary rocks.|
2617|Broken Hill Group|66800|5|Briefly described|p933.|||Hosts stratabound massive sulfide mineralisation. Age of metavolcanics is given (c.1690 Ma). High-grade metamorphism dated at 1600 +/- 8 Ma.|1690 +/- 5 Ma (Page and Laing 1992).||||Includes amphibolite-facies felsic volcanics.|
2617|Broken Hill Group|66857|5|Briefly described|p972 Fig.2, p976.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Contains quartzo-feldspathic metasedimentary rocks derived from an A-type felsic igneous source; supporting an intracratonic rift setting for the development of the Willyama Supergroup.||Unit in Willyama Supergroup.||Overlies Thackaringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||See also p33-34. Broken Hill Domain, Curnamona Province. Deposited during intra-continental extension.|~1720-1685 Ma.||Hores Gneiss, Freyers Metasediments, Parnell Gneiss, Allendale Metasediments.|Overlies Thackeringa Group. Is overlain by Sundown Group.||
2617|Broken Hill Group|67536|5|Briefly described|Map Legend|Statherian|Statherian|Curnamona Province.|ca. 1690 Ma|Of the Willyama Supergroup.|||Siliciclastic metasediments including calcsilicates, garnet- and gahnite-bearing rocks and calc-albites.|
2617|Broken Hill Group|67653|5|Briefly described|p4|||Geological province: Curnamona Province. ||Unit of Willyama Supergroup.||||
2617|Broken Hill Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||28-AUG-13
2617|Broken Hill Group|68126|4|Described|p6, p25-26, p29-31|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Thins and wedges out to the west.|~1695-1685 Ma (Stevens et al., 2008).|Willyama Supergroup.|Ettlewood Calc-silicate member.|Overlies Thackaringa Group. Is overlain by Sundown Group. Equivalent to Saltbush Group.|Siliciclastic metasediments and minor calc-silicates, garnet-rich BIF, quartz-gahnite rock and garnet-quartz rock.|
2617|Broken Hill Group|68315|6|Mentioned|p766|||Broken Hill district, Curnamona Province. Cut by the Stephens Creek Shear Zone.|||||Upper amphibolite-facies metapelites and felsic gneisses.|
2617|Broken Hill Group|69654|6|Mentioned|p3|||Curnamona Province.||||||
2617|Broken Hill Group|69999|5|Briefly described|p3,p9-10 Photos 12-13,p12-15,p17-18,p20|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Middle, rift-deepening, marine transgressive sedimentation with increased magmatic input. Represents much of the amphibolite facies for the Olarian Orogeny. Garnet-bearing rather than orthopyroxene-bearing, unlike Thackaringa Group: discussed.|||Includes Ettlewood Calc-silicate Member and Silver King Metadolerites.||Includes abundant basal calc-silicate rocks and abundant mafic igneous rocks in the upper parts.|
2617|Broken Hill Group|70000|5|Briefly described|p31, p33-34, p36-38|Statherian|Statherian|||Unit in Willyama Supergroup.|Includes Allendale Metasediments and Purnamoota Subgroup.|Conformably overlies Thackaringa Group. Is overlain by Sundown Group.|Includes siliciclastic, pelite-dominated rocks.|
2617|Broken Hill Group|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.|Includes basal Allendale Metasediments and Purnamoota Subgroup.|Overlies Thackaringa Group. Is overlain by Sundown Group.|Mostly comprises metasediments and interbedded quartzo-feldspathic and basic gneisses of the Purnamoota Subgroup. Zoned calc-silicate nodules are common in the metasediments.|
2617|Broken Hill Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Allendale Metasediments and Purnamoota Subgroup.|Overlies Thackaringa Group. Is overlain by Sundown Group.|Metasedimentary rock with two units of quartzofeldspathic to garnetiferous quartzofeldspathic gneiss. Calc-silicate and/or basic gneiss common in places.|
2617|Broken Hill Group|70405|5|Briefly described|P2, p15, p43 Table 3|Mesoproterozoic|Paleoproterozoic||1680 Ma- 1700 Ma|Wilyama Supergroup|Includes, Purnamoota Subgroup, Allendale metasediments|Intruded by Lady Louise Suite, correlated with (tentatively) Oonartra Creek Formation|Glacial and glaciomarine diamictite, sandstone, siltstone ironstone and conglomerate.|
2617|Broken Hill Group|70657|4|Described|p5, p6 Fig.1, p10, p11 Fig.5, p12|Statherian|Statherian|See also,p13 Fig.6, p15-17, p20, p30-31, p33-34, p37, p39-41, p44, p51, p58, p64-66. Curnamona Province; Broken Hill, Mulyungarie Domains. Shown as Broken Hill Group and equivalents in Figs. 1 and 5. Age inferred from Fig.4. Coeval magmatism includes both felsic and mafic components. Related in time to the ~1685 Ma Parnell Formation and the Lady Louise Suite (e.g. Woman-in-White Amphibolite).|~1700-1685 Ma|Willyama Supergroup|Purnamoota Subgroup, Allendale Metasediments.|Overlies Himalaya Formation (Thackaringa Group), Plumbago Formation. Underlies Sundown Group. Intruded by Parnell Gneiss and Silver City Suite. With Sundown Group, is equivalent to Saltbush Group.||
2617|Broken Hill Group|70658|5|Briefly described|p2, 7-8, 15-16, 47|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|c.1693-1685 Ma.|Willyama Supergroup.|Allendale Metasediments; Purnamoota Subgroup.|(Upper part is) equivalent to Raven Hill Subgroup.||
2617|Broken Hill Group|71262|6|Mentioned|p5 Fig 2|||||||||
2617|Broken Hill Group|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
2617|Broken Hill Group|72435|6|Mentioned|p715||||||Hores Gneiss|||
2617|Broken Hill Group|72454|5|Briefly described|p2 Fig.2,  p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain.||Willyama Supergroup|Includes Ettlewood Calc-silicate Member||Includes calc-silicates.|
2617|Broken Hill Group|72461|4|Described|p5-6, p13, p16|||Magmatism including volcanism and intrusion were syn-genetic with deposition of this group. Magmatism ended with emplacement of the Broken Hill ore body at the top of the group at 1685 Ma.||Willyama Supergroup|Includes the Hores Gneiss, Allendale Metasediments, Parnell Gneiss, and the Freyers Metasediments.|Overlies the Thackaringa Group. Overlain by the Sundown Group.|Fine grained sedimentarty rocks including shale and minor horizons of calcium- or magnesium-bearing rocks (limestones).|
2617|Broken Hill Group|73021|6|Mentioned|p224, 226|||||Willyama Supergroup.|Hores Gneiss; Bimbo, Plumbago Formations.|||
2617|Broken Hill Group|73243|6|Mentioned|p52-53, p58-59, p61, p64, p66-67, p72|Statherian|Statherian|Broken Hill block-Euriowie block. Amphibolite bodies are mostly concordant or near-concordant with bedding, interpreted as sills. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites. Shown on p52 Fig.1, p53 Fig.2 and p76.||Willyama Supergroup|||Contains amphibolite sills emplaced during or immediately after deposition.|
2617|Broken Hill Group|73308|4|Described|p605-607, 611-612, 618, 622|||Broken Hill Block. Hydrothermal plumes are proposed as the source of much of these magnetite deposits.|c.1693-1685 Ma.|Willyama Supergroup.|Hores Gneiss, Freyers Metasediments, Parnell Gneiss, Allendale Metasediments.|Is overlain by Sundown Group.|Metasediments including BIFs; contain small amounts of bedding-controlled magnetite.|
2617|Broken Hill Group|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province. Broken Hill Domain, Mulyungarie Domain.||Willyama Supergroup, upper|Allendale Metasediments, Purnamoota Subgroup|Underlies Sundown Group||
2617|Broken Hill Group|73482|5|Briefly described|p419, p422-423, p425-427, p430, p432-433|||Areas of stratigraphy are parallel to the andalusite-sillimanite isograd, in other areas the isograd crosses stratigraphy. Hosts pegmatitic masses. See also p424 Fig.4, p429 Fig.8.||Willyama Supergroup|Hores Gneiss, Freyers Metasediments, Parnell Gneiss, Allendale Metasediments|Overlies Thackaringa Group, underlies Sundown Group|Metasediments. Andalusite and silimanite metamorphic grades, partially melted in parts.|
2617|Broken Hill Group|73512|5|Briefly described|p2-3|Statherian|Statherian|Curnamona Province, Broken Hill Block. Fluviatile to shallow marine successions.||Willyama Supergroup||Underlain by Thackaringa Group. Overlain by Sundown Group.||
2617|Broken Hill Group|73524|5|Briefly described|p2-4|Statherian|Statherian|Rift-phase metasediments.|1693-1685 Ma|lower Willyama Supergroup|Freyers Metasediments, Hores Gneiss, Parnell Formation, Allendale Metasediments||Metasedimentary rocks.|
2617|Broken Hill Group|73575|5|Briefly described|p828 Fig.2, p835-836, p838-839, p841|Statherian|Statherian|See also p829 Fig.3, p830, p832.||Willyama Supergroup|Allendale Metasediments, Purnamoota Subgroup|Overlies Thackaringa Group, underlies Sundown Group||
2654|Brougham Coal Member|37773|6|Mentioned|p19|||||||||
2654|Brougham Coal Member|39288|6|Mentioned|p61|||||||||
2654|Brougham Coal Member|39346|6|Mentioned|Map legend|Permian|Permian|||||||
2654|Brougham Coal Member|40331|6|Mentioned|p13|||||||||
2654|Brougham Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Rowan Formation. ||||
2659|Broughton Formation|22433|4|Described|p12|Late Permian|Late Permian|~ 255Ma||||||
2659|Broughton Formation|22488|4|Described|p839||Late Permian|subdivided in part into 5 latite members and 3 sandstones||||||
2659|Broughton Formation|22578|6|Mentioned|p394|||||||||
2659|Broughton Formation|22591|5|Briefly described|p 65, Fig 2||Late Permian|||||||
2659|Broughton Formation|22857|4|Described|p532 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Shoalhaven Group. Contains 5 latite and 3 sandstone members. Basaltic to andesitic lava and shallow intrusives, shoshonotic; volcaniclastic sandstone, conglomerate, mudstone. Max. thickness: 370m. Geological Province: Sydney Basin.||||||
2659|Broughton Formation|22969|5|Briefly described|Fig 2.2||Late Permian|||||||
2659|Broughton Formation|23442|4|Described|p168|Permian|Permian|Sydney Basin||||||
2659|Broughton Formation|23544|4|Described|p357|||also see Fig 2 p358 and p359. Of the Shoalhaven Group in the Sydney Basin.||||||
2659|Broughton Formation|23896|4|Described|p249|Permian|Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||
2659|Broughton Formation|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Of the Upper Shoalhaven Group.||||||29-NOV-04
2659|Broughton Formation|24342|5|Briefly described|p51|Permian|Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||
2659|Broughton Formation|38690|3|Fully described|p289|||||||||
2659|Broughton Formation|41580|5|Briefly described|p7|||||||||
2659|Broughton Formation|41832|5|Briefly described|p569|||||||||
2659|Broughton Formation|42787|5|Briefly described|p129|||||||||
2659|Broughton Formation|42974|6|Mentioned|Fig.2,p192|||Of Shoalhaven Group.||||||12-MAR-09
2659|Broughton Formation|60281|5|Briefly described|Fig. 7 Appendix 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||
2659|Broughton Formation|60285|4|Described|p182 Fig.2||Kungurian|Of the Shoalhaven Group. Overlies Berry Siltstone. Nearshore marine and volcanic. Geological Province: Sydney Basin.||||||
2659|Broughton Formation|61609|5|Briefly described|p240 Tb. 1, p244|Permian|Permian|Of Shoalhaven Group. Geological Province: Sydney Basin. Base of unit consists of basic to intermediate volcanic detritus.||||||02-MAY-12
2659|Broughton Formation|62043|6|Mentioned|p438 Fig.2. |Late Permian|Late Permian|Southern Sydney Basin.||Unit in Shoalhaven Group.||Overlies Berry Siltstone.||
2659|Broughton Formation|63773|5|Briefly described|p1058 Fig. 2, p1069|Middle Permian|Middle Permian|Of Shoalhaven Group. Geological Province: Sydney Basin. Shoshonitic volcanism.||||||07-APR-09
2659|Broughton Formation|63832|5|Briefly described|p131 Fig.2, p136|Roadian|Roadian|Sydney Basin. Seventh (P3) glaciation. Dominantly glaciomarine deposits.||Unit in Shoalhaven Group.||||13-DEC-17
2659|Broughton Formation|64631|5|Briefly described|p48 Fig.4, p49.|Roadian|Roadian|Sydney Basin. Distal glaciomarine deposits. See also p44. Biostratigraphic  age control at base and top.||||Overlies Berry Siltstone. Is overlain by Illawarra Coal Measures.||
2659|Broughton Formation|64877|5|Briefly described|p296|Permian|Permian|Southern Sydney Basin.||Shoalhaven Group.||||
2659|Broughton Formation|65107|6|Mentioned|p278|Late Permian|Late Permian|Provides constraint on Australia's Later Permian "westward loop" pole path. Pre Mesozoic. No radiometric date||||||
2659|Broughton Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Shoalhaven Group.||Is overlain by Pheasants Nest Formation.||
2659|Broughton Formation|67500|4|Described|p11, p12, p12 Tb.1, p16, p18 Fig. 6|Late Permian|Late Permian|Sydney Basin. Described as early Tatarian age.|~258 Ma.|Of the Upper Shoalhaven Group.|Includes Jamberoo Sandstone, Blow Hole Latite, Kiama Sandstone, Cambewarra Latite, Dapto Latite, Saddleback Latite, Bumbo Latite, Westley Park Sandstone, Members.||Largely sandstone which interfingers eastwards into a local latite volcanic centre.|01-MAY-12
2659|Broughton Formation|67663|6|Mentioned|p518|Permian|Permian|Late Permian. Interbedded with 5 latite flows of the Gerringong Volcanics.||Of the Shoalhaven Group.||||
2659|Broughton Formation|68592|6|Mentioned|p1779|Permian|Permian|||Unit in Shoalhaven Group.||Overlies Berry Siltstone. Is overlain by Illawarra Coal Measures.||
2659|Broughton Formation|69297|6|Mentioned|p501|Wuchiapingian|Capitanian|Sydney Basin. ||||Overlies the Berry Siltstone and the Shoalhaven Group. Intruded by and overlain by the Gerringong Volcanics. Overlain by the Illawarra Coal Measures.||
2659|Broughton Formation|70661|3|Fully described|ix, p137, p139, p181- p187|Late Permian|Late Permian|Named for the Broughton Parish, creek and village. Uppermost unit in the Shoalhaven Group. Previously incorporated as part of the Broughton Tuff and Gerringong Volcanics and later the Budgong Sandstone. Distribution, distinguishing characteristics, geomorphology, depositional environment, structure and fossil assemblage discussed. Age derived from fossils and zircon dating (no ages given in text). 80ms thick in the map area, may be up to 270m thick in total. No type section yet defined.||Shoalhaven Group||Conformably (and in some places gradationally) overlies the Berry Siltstone, gradationally overlain by Illawarra Coal Measures|Poorly to well sorted feldspathic lithic sandstone, conglomerate, minor siltstone and intercalated volcanic rocks. Volcanic rocks range from andesitic to basaltic and have a shoshonitic affinity. Sporadic shelly fossils are present.|
2659|Broughton Formation|70837|5|Briefly described|p246|Capitanian|Capitanian|Of Southern Sydney Basin. CA-TIMS age of 263.51 Ma (Metcalfe etal., 2015).||||||
2659|Broughton Formation|71115|5|Briefly described|p180, 182, 184, 194|Permian|Permian|Southern Sydney Basin. 370m thick. This c.263 Ma age is from a tuff, at the top of the Formation, overlying the Cambewarra Latite Member. The base of the Formation is dated at 265.05 +/- 0.35 Ma.|263.51 +/- 0.05 Ma; ID-TIMS, Metcalfe et al. 2015|Shoalhaven Group.|Westley Park, Kiama, Jamberoo, Sandstone Members; Bumbo, Cambewarra, Latite Members.|Is overlain by Pheasants Nest Formation. Is interbedded with Gerringong Volcanics.||
2659|Broughton Formation|71303|5|Briefly described|map legend|Guadalupian|Guadalupian|Of Sydney Basin.||Of Shoalhaven Group.|||Buff to green-grey medium to coarse-grained feldspathic lithic quartz sandstone, with rare scattered shelly fossils and rounded pebbles. Thin horizons with abundant shelly fossils locally.|
2659|Broughton Formation|71538|6|Mentioned|p54 fig 2|Lopingian|Lopingian|Sydney Basin. ||||Overlies the Berry Formation. Overlain by the Illawarra Coal Measures.|Volcanic rocks.|
2659|Broughton Formation|71542|5|Briefly described|p23, 25-26, 35|Late Permian|Late Permian|Of southern Sydney Basin. Dominated by volcaniclastic detritus, and represents the last phases of deposition of the Shoalhaven Group. Volcanic-derived sandstones were sourced from the E resulting from increasing volcanic activity in the eastern orogen. Variably interpersed with latite flows of the Gerringong Volcanics. Age said to be Late Permian (Kungarian-Kazanian)[ note: Kungurian is at the top of the Early/Lower Permian or Cisuralian. Kazanian is equivalent to Roadian, base of Middle Permian or Guadalupian]||Unit of Shoalhaven Group.|Includes Cambewarra, Dapto, Saddleback, Bumbo, Blow Hole and Coolangatta latite members, Jamberoo, Kiama and Westley Park sandstone members, and Koo-Lee Tuff Member and Back Forest Tuff Bed.|Uppermost unit of Shoalhaven Group. Conformably underlain by Berry Formation. Gradational contact.||20-OCT-21
2659|Broughton Formation|73304|5|Briefly described|p64-65, p70, p74, p76, p78|Capitanian|Capitanian|Sydney Basin, southern. Age is for the top of the unit. Includes evidence of the P3 glacial episode.|263.51 +/- 0.31 Ma U-Pb CA-TIMS.|Shoalhaven Group|||Glaciomarine.|
2659|Broughton Formation|73421|4|Described|p1 Fig.1, p3, p5, p16-20|Capitanian|Wordian|Sydney Basin, southern. Deposited in a storm- and tidal-dominated shallow marine depositional system, containing immature volcanic debris of intermediate to mafic composition. Lower part dated by the 265.05+/-0.46 Ma Ar/Ar plagioclase age of Bumbo Latite (Belica et al., 2017). 263.51+/-0.31 Ma age of Broughton tuff in uppermost part from Metcalfe et al., (2015). 266-263 Ma (mid-Wordian to early Capitanian) age inferred for the formation.|265.05+/-0.46 Ma Ar/Ar, 263.51+/-0.31 Ma Ca-TIMS|Shoalhaven Group|Bumbo Latite, Kiama Sandstone Member, Blowhole Latite Member, Westley Park Sandstone Member|Conformably overlies Berry Siltstone, underlies Illawarra Coal Measures, Pheasant Nest Formation|Succession of intercalated volcaniclastic sandstones and latite lava flows.|
2659|Broughton Formation|73494|5|Briefly described|p542, 559|Permian|Permian|Southern Sydney Basin. Consists of intermediate to basic immature volcanic debris produced by the volcanism that generated the Gerringong Volcanics. Late Permian.||Shoalhaven Group.|Westley Park Sandstone, Kiama Sandstone, Jamberoo Sandstone, Members.|Overlies Berry Formation. Is overlain by Pheasants Nest Formation.|Poorly-sorted, massive to flat- and cross-bedded volcanic sandstones encompassing clasts (up to 1m) of latite; generally bioturbated and containing fossils of shallow-marine fauna. Intruded by three sets of dykes.|
2659|Broughton Formation|73625|6|Mentioned|p2|Permian|Permian|Southern coalfield, Sydney Basin.||||Overlies Berry Siltstone. Is overlain by Pheasants Nest Formation (Illawarra Coal Measures).||
2701|Bruinbun Granite|23214|5|Briefly described|p255|Carboniferous|Carboniferous|Intrudes the Chesleigh and Cookman Formation and undifferentiated Turondale and Waterbeach Formations.||||||
2701|Bruinbun Granite|24278|5|Briefly described|p1765|||Part of the Bathurst Suite.||||||
2701|Bruinbun Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
2701|Bruinbun Granite|33006|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
2701|Bruinbun Granite|33282|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
2701|Bruinbun Granite|34404|6|Mentioned|Fig.3.5b|||||||||
2701|Bruinbun Granite|38216|4|Described|p263|||||||||
2701|Bruinbun Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
2701|Bruinbun Granite|43127|5|Briefly described|p4,Fig.2,Fig.3|||||||||
2701|Bruinbun Granite|43515|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(Provisional Edition) (L.-M.Carb)||||||
2701|Bruinbun Granite|43516|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(L.-M.Carb)||||||
2701|Bruinbun Granite|43517|14|Not recorded|p156|||||||||
2701|Bruinbun Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
2701|Bruinbun Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Does not appear on map face.||||||
2701|Bruinbun Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
2701|Bruinbun Granite|73299|6|Mentioned|p1102 Fig.8|Carboniferous|Carboniferous|||||||
2726|Brushy Hill Limestone Member|22857|5|Briefly described|p498 App.1 Tb.A1.7|Visean|Tournaisian|Of the Dangarfield Formation. Grey thinly bedded and crossbedded oolitic limestone with minor mudstone interbeds. Max. thickness: 22m. Geological Province: Tamworth Forearc Basin.||||||
2726|Brushy Hill Limestone Member|32866|6|Mentioned|p15|||Fossil content||||||
2726|Brushy Hill Limestone Member|33728|6|Mentioned|p44|||||||||
2726|Brushy Hill Limestone Member|35245|2|Defined|p24|Early Carboniferous|Early Carboniferous|||||||
2726|Brushy Hill Limestone Member|36528|6|Mentioned|p175|||||||||
2726|Brushy Hill Limestone Member|41542|6|Mentioned|p234|||See also Section 1||||||
2726|Brushy Hill Limestone Member|44244|4|Described|p24|Visean|Tournaisian|Of the Dangarfield Formation.  Overlies Wroxley Lithic Sandstone Member.  Max. thickness: 22m.||||||16-SEP-04
2726|Brushy Hill Limestone Member|46803|6|Mentioned|p146|||Refers Roberts & Oversby (1974)||||||
2726|Brushy Hill Limestone Member|50268|5|Briefly described|Map Legend|Tournaisian|Tournaisian|Of the Dangarfield Formation.  Geological Province: Rouchel Block.||||||
2726|Brushy Hill Limestone Member|62095|5|Briefly described|p260, p266|Early Carboniferous|Early Carboniferous|Of the Dangarfield Formation. Oolitic limestone. Overlies Kingsfield Formation.||||||
2732|Bryden Formation|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Toogoolawah Group||||
2732|Bryden Formation|22845|6|Mentioned|p82|Triassic|Permian|||||||
2732|Bryden Formation|22846|6|Mentioned|p36,67|Middle Triassic|Early Triassic|||||||
2732|Bryden Formation|23440|4|Described|p140|Triassic|Triassic|Of Toogoolawah Group.||||||18-AUG-08
2732|Bryden Formation|23799|6|Mentioned|p36, p39|Middle Triassic|Early Triassic|See also p127.||||||
2732|Bryden Formation|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Of Toogoolawah Group.  Geological Province: Esk Trough. Maximum thickness: 1500m.||||||
2732|Bryden Formation|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Conglomerate, sandstone, shale, minor tuff.||||||
2732|Bryden Formation|30302|6|Mentioned|p414|||Lower to Middle Triassic||||||
2732|Bryden Formation|30473|6|Mentioned|p377|||Part of Toogoolawah Group. Refers Cranfield and Schwarzbock(1972)||||||
2732|Bryden Formation|30508|6|Mentioned|p91|||Palynology||||||
2732|Bryden Formation|31811|6|Mentioned|Fig. 1|||||||||
2732|Bryden Formation|35101|3|Fully described|p35|||||||||
2732|Bryden Formation|35161|6|Mentioned|p591|||||||||
2732|Bryden Formation|35427|6|Mentioned|p121|||||||||
2732|Bryden Formation|35428|6|Mentioned|p124|||Miospore assemblages||||||
2732|Bryden Formation|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early TriassicE - M||||||
2732|Bryden Formation|36954|6|Mentioned|p114|||||||||
2732|Bryden Formation|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
2732|Bryden Formation|37755|6|Mentioned|p79|||||||||
2732|Bryden Formation|38304|6|Mentioned|p83|||||||||
2732|Bryden Formation|39079|5|Briefly described|p8|||||||||
2732|Bryden Formation|39445|5|Briefly described|Table 9|||||||||
2732|Bryden Formation|39943|6|Mentioned|Table 12A|||||||||
2732|Bryden Formation|40051|4|Described|p8|||||||||
2732|Bryden Formation|40245|6|Mentioned|p182|||||||||
2732|Bryden Formation|40475|6|Mentioned|p7|||||||||
2732|Bryden Formation|40623|5|Briefly described|p65|||||||||
2732|Bryden Formation|41917|6|Mentioned|Fig.3 P528|||||||||
2732|Bryden Formation|42492|5|Briefly described|Table 2 P14|||||||||
2732|Bryden Formation|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.||||||15-JUL-04
2732|Bryden Formation|43008|5|Briefly described|map legend|||||||||
2732|Bryden Formation|43009|5|Briefly described|Map Legend|||||||||
2732|Bryden Formation|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||18-AUG-08
2732|Bryden Formation|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Conglomerate, sandstone, shale.||||||23-DEC-09
2732|Bryden Formation|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Of the Toogoolawah Group. Conglomerate, sandstone, shale, minor tuff||||||
2732|Bryden Formation|61782|5|Briefly described|p275, p277, p277 Fig. 3, p278|||Geological Province: Esk Trough. ||||||
2732|Bryden Formation|63821|6|Mentioned|p20|||Correlated with Gayndah Formation. Geological Province: Esk Trough.||||||07-FEB-11
2732|Bryden Formation|65668|6|Mentioned|p23|Middle Triassic|Early Triassic|Dated by palynology. Intruded by Avoca Creek Granodiorite.||||||
2732|Bryden Formation|67402|4|Described|p165 tbl LPB1, p204|Anisian|Anisian|Esk Trough. Only present in the eastern part of the Esk Trough. Deposited in a fluvial environment. Time equivalent of the Esk Formation. Contains a potential intraformational shale seal. Approximately 450m thick.  See also p205, p206 fig ESK/ABR6, p208, p209.||Toogoolawah Group||Conformably overlain by the Neara Volcanics.|Conglomerate, sandstone and shale.|
2732|Bryden Formation|68679|5|Briefly described|p326, p386, p389-391, p471|||Esk Basin, North D'Aguilar Subprovince, northern New England Orogen. Has a restricted, discontinuous outcrop on the E margin of the Esk Basin. Up to ~1500m thick locally. The type section, adjacent to Lake Somerset, has two subunits: a lower 410m dominated by shale and sandstone, and an upper 506m of mainly conglomerate. Differing stratigraphic interpretations discussed.||Toogoolawah Group.||Overlies Marumba beds. Is faulted against and unconformably overlies Northbrook beds.|Interbedded sandstone, shale and pebble to cobble conglomerate; thin tuff, coal lenses, trachyte, andesite and redbeds are also described.|
2732|Bryden Formation|72297|5|Briefly described|p712|Triassic|Triassic|Monsildale, 43km ESE of Nanango.|||||Mudstone and tuff, with quartz-calcite breccia and veins hosting cinnabar and native mercury.|
2732|Bryden Formation|73306|5|Briefly described|p565-566, 573|Middle Triassic|Middle Triassic|Esk Trough.||Toogoolawah Group.||||
2732|Bryden Formation|73450|6|Mentioned|p107|||||||||
2734|Brymedura Sandstone|22857|5|Briefly described|p492 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Black Rock Subgroup (Catombal Group). Wedge of fluvial arenite. Max. thickness: 250m. Geological Province: Hervey Basin.||||||
2734|Brymedura Sandstone|23043|5|Briefly described|Map Legend|Famennian|Frasnian|of Black Rock Subgroup, Catombal Group.||||||
2734|Brymedura Sandstone|23170|2|Defined|p250|Famennian|Famennian|of Black Rock Subgroup.||||||
2734|Brymedura Sandstone|23214|3|Fully described|p234|Late Devonian|Late Devonian|Of Black Rock Subgroup. Coarse pebbly quartz sandstone with minor finer grained sandstone near the base. Geological Province: Lambie Basin. Overlying unit: Macquarie Park Sandstone, Underlying unit: Paling Yard Formation. Maximum thickness: 270m.||||||
2734|Brymedura 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)||||||
2734|Brymedura Sandstone|31543|6|Mentioned|p117|||||||||
2734|Brymedura Sandstone|32151|6|Mentioned|p217|||Refers Conolly (1963)||||||
2734|Brymedura Sandstone|33732|4|Described|p119|||||||||
2734|Brymedura Sandstone|33871|6|Mentioned|p2531|||||||||
2734|Brymedura Sandstone|34109|4|Described|Table 3.9|||Upper Devonian. See also P159||||||
2734|Brymedura Sandstone|43508|14|Not recorded|p118,121,125-6,129||Late Devonian|Fm of Catombal Gp.'The undulatory quartz percentage..increases with degree of folding. p133||||||
2734|Brymedura Sandstone|43509|14|Not recorded|p113,Pl,II|||||||||
2734|Brymedura Sandstone|43512|2|Defined|p73,76-85,96-106||Late Devonian|Thickness 480ft.Conformably u/lain by Paling Yard Fm,conformably o/lain by the Macquarie Park Ss.||||||
2734|Brymedura Sandstone|43513|14|Not recorded|p72|||||||||
2734|Brymedura Sandstone|43640|5|Briefly described|Map Legend||Devonian|||||||
2734|Brymedura Sandstone|43782|6|Mentioned|Map diagram|Frasnian|Frasnian|of Black Rock Subgroup, of Catombal Group.||||||
2734|Brymedura Sandstone|73299|6|Mentioned|p1104 Fig.10, p1105|Late Devonian|Late Devonian|Molong High.||Catombal Group||Overlies the Paling Yard Formation, underlies the Macquarie Park Sandstone.||
2744|Buccleugh Granite|42726|5|Briefly described|map legend|Silurian||432. NOT variation on Buccleugh Group (misspelling of Buccleuch Group?).||||||
2754|Buchan Group|22628|6|Mentioned|p117,p118|||||||||
2754|Buchan Group|22768|6|Mentioned|p178|||||||||
2754|Buchan Group|22857|6|Mentioned|p178|||||||||
2754|Buchan Group|22968|4|Described|P37, P147|Devonian|Devonian|Conformably overlies the Snowy River Volcanics||||||
2754|Buchan Group|23020|5|Briefly described|Map legend|Early Devonian|Early Devonian|Overlain by Mount Leinster Igneous Complex.||||||08-MAR-07
2754|Buchan Group|23021|5|Briefly described|Map legend|Emsian|Pragian|Unconformably and nonconformably underlies the Mount Leinster Igneous Complex||||||
2754|Buchan Group|23028|5|Briefly described|Map legend|Emsian|Pragian|||||||
2754|Buchan Group|23029|5|Briefly described|Map legend|Emsian|Pragian|Angular unconformably and nonconformably underlies the Mount Leinster Igneous Complex||||||
2754|Buchan Group|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
2754|Buchan Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
2754|Buchan Group|23309|4|Described|p71, 106, 114  Table 2.41|Early Devonian|Early Devonian|||||||16-AUG-18
2754|Buchan Group|23615|3|Fully described|p137, p20 Fig.6|Middle Devonian|Early Devonian|Formerly known as Buchan Limestone, Buchan Series or series, Upper Buchan beds and Bindi Limestone. Composed of 3 formations: Buchan Caves Limestone, Taravale Marlstone and Murrindal Limestone.  Age: late Early to Middle Devonian ~395-385Ma. Underlain by Snowy River Volcanics.||||||16-AUG-18
2754|Buchan Group|23710|14|Not recorded|p72|||Faulting.||||||
2754|Buchan Group|23938|5|Briefly described|p31-32 Fig. 12|Early Devonian|Early Devonian|Includes the Spring Creek Member. Marlstone, limestone, dolomite.||||||
2754|Buchan Group|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
2754|Buchan Group|24004|5|Briefly described|p275 Fig.2|Devonian|Devonian|||||||
2754|Buchan Group|24098|5|Briefly described|p27 Fig. 2|Middle Devonian|Emsian| Geological Province: Lachlan Fold Belt.||||||
2754|Buchan Group|24164|6|Mentioned|p15 Fig.8|Devonian|Devonian|Shallow marine.||||||
2754|Buchan Group|24266|5|Briefly described|p1483|||Geological Province: Lachlan Fold Belt. Underlain by Snowy River Volcanics.||||||08-MAR-07
2754|Buchan Group|24275|6|Mentioned|p1696 Fig. 2|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
2754|Buchan Group|24551|3|Fully described|p147, p118 Fig. 5.1|Devonian|Devonian|||||||
2754|Buchan Group|24598|5|Briefly described|p514|Early Devonian|Early Devonian|Geological Province: Lachlan Orogen.||||||
2754|Buchan Group|29860|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2754|Buchan Group|30814|6|Mentioned|Table.2|||||||||
2754|Buchan Group|32585|6|Mentioned|p211|||Mid. Dev.||||||
2754|Buchan Group|33238|5|Briefly described|p644|||||||||
2754|Buchan Group|33393|6|Mentioned|p161|||||||||
2754|Buchan Group|33437|6|Mentioned|p63|||Sil.-Dev. Conodont faunas.||||||
2754|Buchan Group|33602|6|Mentioned|Table 1|||||||||
2754|Buchan Group|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
2754|Buchan Group|33606|3|Fully described|p66|||||||||
2754|Buchan Group|33608|6|Mentioned|p45|||||||||
2754|Buchan Group|33732|6|Mentioned|p111|||||||||
2754|Buchan Group|34184|6|Mentioned|p7|||Conodonts. Refers Philip(1966).||||||
2754|Buchan Group|34287|6|Mentioned|p97|||||||||
2754|Buchan Group|34405|6|Mentioned|Fig.3.9|||||||||
2754|Buchan Group|34519|6|Mentioned|p44|||||||||
2754|Buchan Group|34954|6|Mentioned|Fig.34|||||||||
2754|Buchan Group|35112|6|Mentioned|Table 1|||||||||
2754|Buchan Group|35274|6|Mentioned|p420|||||||||
2754|Buchan Group|35278|6|Mentioned|p360|||||||||
2754|Buchan Group|35283|6|Mentioned|p49|||||||||
2754|Buchan Group|36201|6|Mentioned|p2|||Mentioned throughout article.||||||
2754|Buchan Group|37330|5|Briefly described|p15|||||||||
2754|Buchan Group|37501|6|Mentioned|p414|||||||||
2754|Buchan Group|37727|6|Mentioned|p33|||||||||
2754|Buchan Group|38145|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2754|Buchan Group|38367|6|Mentioned|p11|||||||||
2754|Buchan Group|38545|6|Mentioned|p114|||||||||
2754|Buchan Group|38734|6|Mentioned|p10|||||||||
2754|Buchan Group|39447|4|Described|p13|||||||||
2754|Buchan Group|40728|6|Mentioned|p173|||||||||
2754|Buchan Group|40761|5|Briefly described|p230|||||||||
2754|Buchan Group|41570|6|Mentioned|p91|||||||||
2754|Buchan Group|41572|5|Briefly described|p21|||||||||
2754|Buchan Group|41585|5|Briefly described|p138|||||||||
2754|Buchan Group|41755|6|Mentioned|p168|||||||||
2754|Buchan Group|41868|6|Mentioned|p574|||||||||
2754|Buchan Group|42089|6|Mentioned|p10|||||||||
2754|Buchan Group|42577|6|Mentioned|p28|||||||||
2754|Buchan Group|42635|5|Briefly described|p27|||||||||
2754|Buchan Group|42791|5|Briefly described|Fig.9 P213|||||||||
2754|Buchan Group|42827|5|Briefly described|p138|||see also Table 4.1||||||
2754|Buchan Group|42967|4|Described|p76|||||||||
2754|Buchan Group|43206|5|Briefly described|map legend|Emsian|Pragian|||||||
2754|Buchan Group|43228|5|Briefly described|p10||Early Devonian|||||||
2754|Buchan Group|43312|5|Briefly described|Map Legend||Pragian|||||||
2754|Buchan Group|43313|5|Briefly described|Map Legend||Pragian|||||||
2754|Buchan Group|43431|14|Not recorded|p1262||Early Devonian|Lower Devonian. Previously regarded as Middle Devonian||||||
2754|Buchan Group|43461|14|Not recorded|p627, 628|||||||||
2754|Buchan Group|43530|14|Not recorded|p1025,1030-1,1034|Emsian|Siegenian|U.Siegenian-L.Emsian||||||
2754|Buchan Group|43547|14|Not recorded|p147,151,Tb p153-55|Eifelian|Emsian|U.Emsian-Eifelian.||||||
2754|Buchan Group|43770|6|Mentioned|p829||Early Devonian|||||||
2754|Buchan Group|44184|5|Briefly described|Map Legend||Early Devonian|||||||
2754|Buchan Group|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Includes Buchan Caves and Murrindal Limestones, and Taravale Marlstone.|||
2754|Buchan Group|48971|6|Mentioned|p9|||||||||
2754|Buchan Group|50077|5|Briefly described|p7|Early Devonian|Early Devonian|Includes the Buchan Caves Limestone and Taravale Formation.||||||
2754|Buchan Group|60503|5|Briefly described|p27|Early Devonian|Early Devonian|Marine clastics and carbonates. ||||||
2754|Buchan Group|60542|4|Described|p78, p15|Middle Devonian|Early Devonian|Comprises Buchan Caves Limestone and Taravale Marlstone in ORBOST. Overlies Snowy River Volcanics conformably, unconformably and disconformably. Largest outcrop is in Murrindal Synclinorium. See also p25.||||||
2754|Buchan Group|61180|5|Briefly described|p7|Devonian|Devonian|Limestone units overlying Snowy River Volcanics. Base metal mineralisation is concentrated into lower parts of this sequence.||||||
2754|Buchan Group|61181|5|Briefly described|p13, p127|Devonian|Devonian|In the Buchan-Murrindal area this group forms a sequence of carbonate and calcareous mudstone, in which the limestones are Buchan Caves (lower) and Murrindal Limestones (upper). ||||||
2754|Buchan Group|61186|6|Mentioned|p87|||Includes Buchan Caves Limestone and Murrindal Limestone. ||||||
2754|Buchan Group|61187|5|Briefly described|p5 Fig.3, p26 Fig.2, p29 Fig.4,  pp137ff|Early Devonian|Early Devonian|Tabberabbera Zone, Benambra Terrane. Correlative of Wentworth Group (Tabberabbera Zone, Benambra Terrane), and Lilydale Limestone and Wilson Creek Shale (Melbourne Zone, Melbourne Terrane).|||Includes Buchan Caves Limestone, Taravale Formation and Murrindal Limestone.|Overlies Snowy River Volcanics.|Nonmagnetic limestones, dolomites and calcareous silts.|
2754|Buchan Group|63594|5|Briefly described|p1032|||Includes Buchan Caves Limestone and Taravale Formation. See also Fig. 1.||||||04-OCT-07
2754|Buchan Group|66498|6|Mentioned|p43|Emsian|Emsian|Contains vertebrate macro-remains.||||||
2754|Buchan Group|68297|5|Briefly described|p184, 192|Pragian|Lochkovian|Vic. Includes possible shark scales.||||||
2754|Buchan Group|68592|6|Mentioned|p1007|Early Devonian|Early Devonian|||||Correlated with Taemas Limestone (Murrumbidgee Group).||
2754|Buchan Group|71040|5|Briefly described|p8, p12-13, p15|Emsian|Emsian|Bindi Syncline, NE Victoria. Post-rift shallow-marine carbonates. Shows 20-30% fold shortening and reactivation of faults, due to the Tabberabberan Orogeny.||||Overlies Snowy River Volcanics.||
2762|Buchargingah Granite|23721|5|Briefly described|Map Legend|Silurian|Silurian|||||||
2762|Buchargingah Granite|24119|5|Briefly described|p3|Silurian|Silurian|||||||
2762|Buchargingah Granite|42726|5|Briefly described|map legend|||547.||||||
2775|Buckaroo Conglomerate|22472|6|Mentioned|p47 Fig.6(e)|||of the Mt. Knowles Group||||||
2775|Buckaroo Conglomerate|22529|5|Briefly described|4 fig 2, 8|Late Devonian|Late Devonian|Parent Mount Knowles Group. Overlying unit Bumberra Formation||||||
2775|Buckaroo Conglomerate|22857|5|Briefly described|p492 App.1 Tb.A1.7|Late Devonian|Late Devonian|Quartz-rich purple conglomerate, quartz arenite and red mudstone interbeds. Max. thickness: 420m. Geological Province: Lambie Basin.||||||
2775|Buckaroo Conglomerate|23043|5|Briefly described|Map Legend|Frasnian|Frasnian|of Mount Knowles Group.||||||
2775|Buckaroo Conglomerate|23170|2|Defined|p240|Late Devonian|Late Devonian|of Mount Knowles Group.||||||
2775|Buckaroo Conglomerate|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
2775|Buckaroo Conglomerate|32485|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2775|Buckaroo Conglomerate|42310|4|Described|p209|||||||||
2775|Buckaroo Conglomerate|42379|4|Described|p209|||||||||
2775|Buckaroo Conglomerate|43043|4|Described|p99|||late Devonian age.||||||
2775|Buckaroo Conglomerate|43188|4|Described|p219,Table 6 p218||Late Devonian|?Frasnian. Of Lambie Group.||||||
2775|Buckaroo Conglomerate|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
2775|Buckaroo Conglomerate|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4, p1099|Late Devonian|Late Devonian|Capertree High. Basal unit of Mount Knowles Group. Locations in text include p1100 Fig.5.||Mount Knowles Group||Overlies the Carwell Creek Formation, underlies the Bumberra Formation, Lawsons Creek Shale.||
2778|Buckburraga Slate|22679|5|Briefly described|p 32||Devonian|||||||
2778|Buckburraga Slate|22857|4|Described|p472 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Crudine Group. Laminated silty slate. Max. thickness: ~300m. Geological Province: Hill End Trough and Capertee Rise.||||||
2778|Buckburraga Slate|23214|3|Fully described|p196|Lochkovian|Lochkovian|Of Crudine Group. First included in the Burraga Beds (now Burraga Group). Consists of thinly bedded, laminated, grey-green shale and black slate with minor carboneous shale lenses. Max. thickness 300m.||||||
2778|Buckburraga Slate|29903|6|Mentioned|p169|||||||||
2778|Buckburraga Slate|33285|5|Briefly described|p65|||||||||
2778|Buckburraga Slate|42712|4|Described|8; Table 1 p14.|Early Devonian|Late Silurian|Within Crudine Group. Conformable between Adderley Fm above and Campbells Fm below.||||||
2778|Buckburraga Slate|43639|5|Briefly described|Map Legend||Devonian|||||||
2778|Buckburraga Slate|43654|5|Briefly described|Map Legend|Devonian|Devonian|Of Crudine Group. Laminated silty slate.||||||17-JUL-08
2778|Buckburraga Slate|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of Crudine Group.||||||17-JUN-08
2778|Buckburraga Slate|50233|4|Described|Map Legend|Lochkovian|Lochkovian|Of the Crudine Group. Laminated silty slate. Overlies the Dunchurch Formation.||||||12-MAY-04
2778|Buckburraga Slate|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Crudine Group. Khaki to grey laminated siltstone with thin beds of fine- to medium-grained feldspathic sandstone.||||||17-JUN-08
2778|Buckburraga Slate|68592|3|Fully described|p1038, p1040-1, p1050-3|Lochkovian|Lochkovian|A sequence of sandstone, siltstone and shale in the Burraga-Isabella River area was first mapped as Burraga Group by Stanton (1956); informally divided into Dunchurch Formation and Buckburraga Slate by Dunnet (1961) and Gemuts (1961). Mapped as undifferentiated Burraga Group by Scheibner (1973). The name Buckburraga Slate was first published by Bowman (1974); formally defined during mapping of 2nd edition Bathurst 1:250 000 geological map (Stuart-Smith and Wallace, 1997; Wyborn and Henderson, 1997; Pogson and Watkins, 1998). No type section; a former type section of Wallace (in Pogson and Watkins, 1998) falls within Campbells Formation (Binghams Back Formation). A representative locality is described. Very restricted area (c. 0.1 km2) in the core of the Burraga Syncline, southern Hill End Trough. 30-200m thick. Geophysical properties described.||Unit in Crudine Group.||Conformably overlies Dunchurch Formation. Is overlain conformably by Adderley Formation. Correlated with Waterbeach Formation.|A sequence of grey to grey-green, laminated to thinly bedded siltstone, pyritic in places; interbedded with minor medium-grained feldspathic sandstone. Strong slaty cleavage is typically developed.|
2778|Buckburraga Slate|70192|5|Briefly described|Map Legend|Pragian|Lochkovian|Dcu. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot. Age min boundary on Time-Space plot is marked with ?-?-?. Related units inferred from Time-Space Plot.||At base of Crudine Group||Overlies Dunchurch Formation.|Laminated to thinly-bedded siltstone; minor thinly bedded , fine to medium-grained, feldspathic sandstone.|
2778|Buckburraga Slate|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
2778|Buckburraga Slate|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Crudine Group|||Laminated to thinly-bedded siltstone; minor thinly bedded , fine to medium-grained, feldspathic sandstone.|
2778|Buckburraga Slate|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Crudine Group|||Laminated-thinly bedded siltstone; minor thinly bedded, fine-medium grained, feldspathic sandstone.|
2778|Buckburraga Slate|71656|6|Mentioned|p13 Fig.2|Lochkovian|Lochkovian|Only shown in correlation chart (Fig.2).||Of Crudine Group||Overlies Dunchurch Formation.||
2780|Buckendoon Sand Member|22892|6|Mentioned|table9 p69|Quaternary|Quaternary|||||||
2780|Buckendoon Sand Member|40726|6|Mentioned|p227|||||||||
2811|Budderoo Lamprophyre|36042|6|Mentioned|p44|||||||||
2811|Budderoo Lamprophyre|36220|5|Briefly described|p95|||||||||
2811|Budderoo Lamprophyre|36221|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic||||||
2811|Budderoo Lamprophyre|43346|2|Defined|p3,4|||See also Lexicon.  Correlated with Good Dog Lamprophyres||||||
2811|Budderoo Lamprophyre|43349|14|Not recorded|Map|||||||||
2811|Budderoo Lamprophyre|45090|6|Mentioned|p89|||Cretaceous igneous rocks||||||
2812|Buddong Volcanics|22857|5|Briefly described|p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Boraig Group. Rhyolitic tuff, agglomerate. Max. thickness: 1060m. Geological Province: Bogan Gate Terrace.||||||
2812|Buddong Volcanics|29648|6|Mentioned|p19|||||||||
2812|Buddong Volcanics|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
2812|Buddong Volcanics|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
2812|Buddong Volcanics|33732|5|Briefly described|p111|||Boraig Gp.||||||
2812|Buddong Volcanics|34403|4|Described|p144|||||||||
2812|Buddong Volcanics|34405|6|Mentioned|Fig.3.15|||||||||
2812|Buddong Volcanics|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
2812|Buddong Volcanics|60086|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Boraig Group.||||||
2815|Budgong Sandstone|22500|5|Briefly described|p12  Fig 6, 11||Early Permian|Sydeny Basin||||||
2815|Budgong Sandstone|22578|6|Mentioned|Fig.6 p396|||of Shoalhaven Group||||||
2815|Budgong Sandstone|22969|4|Described|p 22, Fig 2.2||Late Permian|Max. thickness: 370 m.||||||
2815|Budgong Sandstone|22970|5|Briefly described|Plate 6|Permian|Permian|||||||
2815|Budgong Sandstone|29752|6|Mentioned|Map legend|Late Permian|Late Permian|Located in pocket||||||
2815|Budgong Sandstone|29900|4|Described|Fig.2|||||||||
2815|Budgong Sandstone|29901|5|Briefly described|p163|||||||||
2815|Budgong Sandstone|30006|6|Mentioned|p6|||||||||
2815|Budgong Sandstone|31128|5|Briefly described|p5|||||||||
2815|Budgong Sandstone|31887|5|Briefly described|p4|||||||||
2815|Budgong Sandstone|32938|6|Mentioned|p67|||Geology||||||
2815|Budgong Sandstone|36042|6|Mentioned|Table 1|||||||||
2815|Budgong Sandstone|36148|6|Mentioned|Fig.6|||||||||
2815|Budgong Sandstone|36220|3|Fully described|p26|||See also Table 1 & 18.||||||
2815|Budgong Sandstone|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
2815|Budgong Sandstone|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
2815|Budgong Sandstone|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
2815|Budgong Sandstone|38615|6|Mentioned|p22|||||||||
2815|Budgong Sandstone|38690|6|Mentioned|p288|||||||||
2815|Budgong Sandstone|39287|6|Mentioned|Fig. 2.5|||||||||
2815|Budgong Sandstone|39289|4|Described|p78|||||||||
2815|Budgong Sandstone|39290|6|Mentioned|p99|||||||||
2815|Budgong Sandstone|39305|6|Mentioned|p379|||||||||
2815|Budgong Sandstone|39307|6|Mentioned|Table 22.1|||||||||
2815|Budgong Sandstone|39308|6|Mentioned|p517|||||||||
2815|Budgong Sandstone|39309|4|Described|p117|||See also Table 7.1||||||
2815|Budgong Sandstone|40166|6|Mentioned|Table 1|||||||||
2815|Budgong Sandstone|40519|6|Mentioned|Fig.3|||||||||
2815|Budgong Sandstone|42737|5|Briefly described|map legend|Permian||||||||
2815|Budgong Sandstone|42896|3|Fully described|p9|||Of Shoalhaven Group; Late Permian age.||||||12-MAR-09
2815|Budgong Sandstone|42925|5|Briefly described|Table 18||Late Permian|||||||
2815|Budgong Sandstone|43194|5|Briefly described|p129 Tb. 8.3|Early Permian|Early Permian|Uppermost unit of Shoalhaven Group, western Sydney Basin.||||||
2815|Budgong Sandstone|45090|6|Mentioned|p7|||Time correlation chart||||||
2815|Budgong Sandstone|60281|4|Described|p60|Late Permian|Late Permian|Overlain by the Pheasants Nest Formation. Age: 264-263 Ma. Max. thickness: 370m. Geological Province: Sydney Basin. Fine-grained sandstone, with latite flows of the Gerrigong Volcanics interbedded towards the top of the unit.||||||27-APR-05
2815|Budgong Sandstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the ?Shoalhaven Group. Geological Province: Sydney Basin.||||||12-MAR-09
2815|Budgong Sandstone|61609|5|Briefly described|p240 Tb. 1, p244|Permian|Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||07-FEB-11
2815|Budgong Sandstone|66577|6|Mentioned|p996, p997 Fig.2.|Permian|Permian|||Unit in Shoalhaven Group.||Overlies Berry Siltstone.||
2815|Budgong Sandstone|68003|5|Briefly described|p38 Fig.3-j.|Late Permian|Late Permian|Western Coalfield, Brigalow Belt South Bioregion.||Unit in Shoalhaven Group.||Overlies Berry Siltstone.||
2815|Budgong Sandstone|69297|6|Mentioned|p501|Wuchiapingian|Capitanian|Sydney Basin. ||||Overlies the Berry Siltstone. Overlain by the Illawarra Coal Measures.||
2828|Buggary Granodiorite|22815|4|Described|p52|Early Devonian|Late Silurian|||||||
2828|Buggary Granodiorite|35263|6|Mentioned|Table 3|||||||||
2828|Buggary Granodiorite|41905|2|Defined|p90|Silurian||||||||
2828|Buggary Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
2828|Buggary Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Buggary Suite.||||||
2828|Buggary Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh19||||||
2828|Buggary Granodiorite|49705|5|Briefly described|p20|||||||||
2828|Buggary Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
2830|Buggs Creek Volcanic Member|22857|5|Briefly described|p512 App.1 Tb.A1.8|Visean|Visean|Of the Berrico Creek Formation. Basal lithic arenite and ignimbrite. Max. thickness: 45m.||||||
2830|Buggs Creek Volcanic Member|32868|6|Mentioned|p208,Fig.7|||||||||
2830|Buggs Creek Volcanic Member|35492|6|Mentioned|p141|||||||||
2830|Buggs Creek Volcanic Member|35856|6|Mentioned|p189|||||||||
2830|Buggs Creek Volcanic Member|42547|4|Described|p35|||||||||
2830|Buggs Creek Volcanic Member|44244|4|Described|p143|Visean|Visean|Of the Berrico Creek Formation.  Type section in text.  Max. thickness: 45m.  Geological Province: Myall Block.||||||
2830|Buggs Creek Volcanic Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Berrico Creek Formation.  Pink. purple to fawn rhyodacitic ignimbrite with minor andesite and volcanic breccia.||||||
2835|Bugs Ridge Granite|22679|4|Described|p 44|||||||||
2835|Bugs Ridge Granite|22798|6|Mentioned|Fig.2|||||||||
2835|Bugs Ridge Granite|23214|3|Fully described|p170|Late Silurian|Late Silurian|Originally named Bugs Ridge Adamellite. Intrudes Adaminaby Group and Coombing Formation. S-type granite. Strongly foliated biotite-muscovite granite containing minor altered cordierite.||||||
2835|Bugs Ridge Granite|42726|5|Briefly described|map legend|Silurian||Reserved as Bugs Ridge Adamellite.||||||
2835|Bugs Ridge Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Foliated biotite granite, leucogranite.||||||17-JUL-08
2835|Bugs Ridge Granite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|||||||
2835|Bugs Ridge Granite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian S-type granitoids.||||||
2845|Bulbodney Creek Intrusive Complex|22831|4|Described|p19||Eastonian|||||||
2845|Bulbodney Creek Intrusive Complex|24417|6|Mentioned|p39|||||||||
2845|Bulbodney Creek Intrusive Complex|43441|5|Briefly described|13, 21|||448+/-4Ma (Shrimp). Age: ?Late Ordovician||||||08-JAN-10
2845|Bulbodney Creek Intrusive Complex|48958|6|Mentioned|p13|||||||||
2852|Bulga Complex|29698|4|Described|p69|||||||||
2852|Bulga Complex|29699|4|Described|p135|||||||||
2852|Bulga Complex|61776|5|Briefly described|p194 Fig. 3|Jurassic|Jurassic|Geological Province: Surat Basin. Microsyenite, phonolite and phonolitic trachyte.||||||
2852|Bulga Complex|68003|5|Briefly described|p48, p51 Photo 3-p, p55 Fig.3-m, p128.|Cretaceous|Late Triassic|Gunnedah Basin. Forms prominent topographical features to the south and west of Mullaley. Silica-rich felsic differentiates extruded quiescently; marks the final stage in Garrawilla volcanic event.||Unit in Garrawilla Volcanics.|||Massive flows and lava domes of microsyenite, phonolitic trachyte and phonolite.|
2852|Bulga Complex|68004|5|Briefly described|p128.|||Of the Garrawilla Volcanic Event. Moderate rare earth elements potential with a level of certainty of B-C.||||||
2852|Bulga Complex|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.||||||
2857|Bulgas Monzonite|39331|6|Mentioned|Fig.8-2|||||||||
2863|Bulgo Sandstone|22549|6|Mentioned|p526||Triassic|||||||
2863|Bulgo Sandstone|22745|6|Mentioned|p129|||Narrabeen Group, Sydney Basin.||||||
2863|Bulgo Sandstone|22749|5|Briefly described|p185,Table1p187,196|||||||||
2863|Bulgo Sandstone|22857|5|Briefly described|p264, p530 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Fine to medium-grained quartz-lithic sandstone with lenticular shale interbeds. Max. thickness: ~100m. Geological Province: Sydney Basin.||||||
2863|Bulgo Sandstone|22864|6|Mentioned|p264|||||||||
2863|Bulgo Sandstone|22969|6|Mentioned|p 27|||||||||
2863|Bulgo Sandstone|23881|5|Briefly described|p69 Fig. 7.2|||Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
2863|Bulgo Sandstone|29633|6|Mentioned|p435|||Upper Permian/Lower Triassic||||||
2863|Bulgo Sandstone|29901|4|Described|Table 1|||||||||
2863|Bulgo Sandstone|30006|4|Described|p64|||||||||
2863|Bulgo Sandstone|30007|6|Mentioned|p61|||||||||
2863|Bulgo Sandstone|30132|6|Mentioned|Table 1|||||||||
2863|Bulgo Sandstone|30427|6|Mentioned|p39|||||||||
2863|Bulgo Sandstone|31061|6|Mentioned|Table 1|||||||||
2863|Bulgo Sandstone|31128|6|Mentioned|Table 1|||||||||
2863|Bulgo Sandstone|31276|6|Mentioned|p147|||Palynology||||||
2863|Bulgo Sandstone|31297|6|Mentioned|Fig. 3|||||||||
2863|Bulgo Sandstone|31426|6|Mentioned|Fig.1|||||||||
2863|Bulgo Sandstone|31725|6|Mentioned|p10|||On table||||||
2863|Bulgo Sandstone|31878|6|Mentioned|Table 1|||Triassic||||||
2863|Bulgo Sandstone|31884|6|Mentioned|Table 1|||Triassic||||||
2863|Bulgo Sandstone|31886|6|Mentioned|Table 1|||||||||
2863|Bulgo Sandstone|31887|5|Briefly described|p8|||||||||
2863|Bulgo Sandstone|32187|6|Mentioned|p4|||||||||
2863|Bulgo Sandstone|32799|6|Mentioned|p9|||||||||
2863|Bulgo Sandstone|32800|6|Mentioned|p384|||||||||
2863|Bulgo Sandstone|32801|6|Mentioned|Fig.10|||||||||
2863|Bulgo Sandstone|32802|6|Mentioned|p22|||||||||
2863|Bulgo Sandstone|33683|4|Described|Table 1|||||||||
2863|Bulgo Sandstone|33685|6|Mentioned|Table 2|||||||||
2863|Bulgo Sandstone|33867|6|Mentioned|Table 1|||||||||
2863|Bulgo Sandstone|34009|6|Mentioned|Table III|||L.Triassic||||||
2863|Bulgo Sandstone|34058|5|Briefly described|p395|||Triassic||||||
2863|Bulgo Sandstone|34139|6|Mentioned|Table|||PP23-24||||||
2863|Bulgo Sandstone|34205|6|Mentioned|Table 6|||Correlates with Banks Wall Sandstone Member.||||||
2863|Bulgo Sandstone|34236|6|Mentioned|p17|||||||||
2863|Bulgo Sandstone|34241|6|Mentioned|p404|||||||||
2863|Bulgo Sandstone|34336|6|Mentioned|Table 5.15|||||||||
2863|Bulgo Sandstone|34337|4|Described|p394|||||||||
2863|Bulgo Sandstone|34562|6|Mentioned|p60|||||||||
2863|Bulgo Sandstone|35062|6|Mentioned|p279|||||||||
2863|Bulgo Sandstone|35502|6|Mentioned|Table 1|||||||||
2863|Bulgo Sandstone|35690|6|Mentioned|p61|||||||||
2863|Bulgo Sandstone|36042|6|Mentioned|Fig.22|||See also Fig.24.||||||
2863|Bulgo Sandstone|36220|4|Described|p69|||See also P65 & Table 20.||||||
2863|Bulgo Sandstone|36222|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
2863|Bulgo Sandstone|36391|6|Mentioned|p156|||||||||
2863|Bulgo Sandstone|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
2863|Bulgo Sandstone|36594|6|Mentioned|Table 1|||See also Table II.||||||
2863|Bulgo Sandstone|37168|6|Mentioned|p231|||||||||
2863|Bulgo Sandstone|37722|6|Mentioned|p23|||||||||
2863|Bulgo Sandstone|37804|6|Mentioned|Table 1|||||||||
2863|Bulgo Sandstone|39293|6|Mentioned|Fig. 8.11|||||||||
2863|Bulgo Sandstone|39296|3|Fully described|p179|||See also PP180-184||||||
2863|Bulgo Sandstone|39306|6|Mentioned|p389|||See also P410,P411||||||
2863|Bulgo Sandstone|39308|6|Mentioned|p505|||||||||
2863|Bulgo Sandstone|39450|6|Mentioned|Fig.4|||||||||
2863|Bulgo Sandstone|39935|6|Mentioned|p58|||||||||
2863|Bulgo Sandstone|40516|6|Mentioned|Fig.3|||||||||
2863|Bulgo Sandstone|40602|4|Described|p9|||||||||
2863|Bulgo Sandstone|40652|6|Mentioned|p128|||||||||
2863|Bulgo Sandstone|40653|6|Mentioned|p121|||||||||
2863|Bulgo Sandstone|41123|6|Mentioned|p178|||||||||
2863|Bulgo Sandstone|41639|6|Mentioned|p9|||||||||
2863|Bulgo Sandstone|42737|5|Briefly described|map legend|Triassic||||||||
2863|Bulgo Sandstone|42896|3|Fully described|p28, Table 2|||of Clifton Subgroup||||||
2863|Bulgo Sandstone|42925|5|Briefly described|Table 18||Early Triassic|||||||
2863|Bulgo Sandstone|42926|4|Described|map legend||Early Triassic|||||||
2863|Bulgo Sandstone|43028|6|Mentioned|Fig.7,p618|||of Narrabeen Group||||||
2863|Bulgo Sandstone|43194|5|Briefly described|p130, p131|Triassic|Triassic|Sandy alluvial material deposited in the southern Sydney Basin.||||||
2863|Bulgo Sandstone|43323|14|Not recorded|p63,71|||Fossils (I56-9)||||||
2863|Bulgo Sandstone|43344|14|Not recorded|p21,68-70||Triassic|||||||
2863|Bulgo Sandstone|43383|14|Not recorded|p22|||Part of Clifton Sub-Group||||||
2863|Bulgo Sandstone|43392|14|Not recorded|p223,224|||Contains phosphatic pebbles at Thelma Head||||||
2863|Bulgo Sandstone|43395|14|Not recorded|p76|||||||||
2863|Bulgo Sandstone|45090|6|Mentioned|p71|||Relationships in Narrabeen Gp.||||||
2863|Bulgo Sandstone|60281|6|Mentioned|p64|||Different unit from Bulga Formation.  Extension of the Narrabeen Group under the Hawkesbury Sandstone - a coastal unit.||||||23-MAR-05
2863|Bulgo Sandstone|61315|5|Briefly described|Table SY2|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
2863|Bulgo Sandstone|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Narrabeen Group.||Overlies Stanwell Park Claystone. Is overlain by Bald Hill Claystone.||
2863|Bulgo Sandstone|67560|5|Briefly described|p258, p260-p271|Triassic|Triassic|Constrained by the age of the Narrabeen Group.||Of the Narrabeen Group.||Overlain by the Bald Hill Claystone. Underlain by the Stanwell Park Claystone.|Coarse sandstone overlain by alternating sandstone and grey shale, then grey siltstone, with fine-grained sandstone and some dark silty layers at top.|
2863|Bulgo Sandstone|68003|5|Briefly described|p42.|Triassic|Triassic|Southern Sydney Basin.|||||Fine-grained sandstone with interbedded shale units.|
2863|Bulgo Sandstone|73304|6|Mentioned|p73-74, p76, p78|||Sydney Basin, southern. Includes the Induan-Olenkian boundary.||Narrabeen Group||||
2869|Bulgoo Formation|22518|4|Described|Table 1, p 6, 7, 10|Middle Devonian|Early Devonian|Mulga Downs Group, Darling Basin||||||
2869|Bulgoo Formation|22857|5|Briefly described|p212, p488 App.1 Tb.A1.7|Devonian|Devonian|Of the Mulga Downs Group. Consists of all the strata above the Merrimerriwa Formation and below Bundycoola Formation. Max. thickness: ~1km.||||||
2869|Bulgoo Formation|22859|5|Briefly described|p212|||||||||
2869|Bulgoo Formation|23171|6|Mentioned|p16|||||||||
2869|Bulgoo Formation|23173|6|Mentioned|Map Legend|||||||||
2869|Bulgoo Formation|24588|6|Mentioned|p33|||Fluviatile. Cobar region.||||||29-NOV-13
2869|Bulgoo Formation|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2869|Bulgoo Formation|38292|6|Mentioned|Fig.1|||||||||
2869|Bulgoo Formation|40913|6|Mentioned|Map legend|Eifelian|Eifelian|||||||
2869|Bulgoo Formation|41126|2|Defined|p121|Eifelian|Emsian|Emsian to Eifelian. Mention p108.||||||27-OCT-08
2869|Bulgoo Formation|41138|6|Mentioned|Map legend|Devonian|Devonian|||||||
2869|Bulgoo Formation|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
2869|Bulgoo Formation|41821|3|Fully described|p59|Middle Devonian||||||||
2869|Bulgoo Formation|42467|5|Briefly described|Map Legend|||||||||
2869|Bulgoo Formation|42521|5|Briefly described|Fig.6 P20|||||||||
2869|Bulgoo Formation|42983|6|Mentioned|Fig.3,p345|||||||||
2869|Bulgoo Formation|43032|2|Defined|p174|Eifelian|Emsian|Of Mulga Downs Group.||||||27-OCT-08
2869|Bulgoo Formation|43389|14|Not recorded|Map Legend|||||||||
2869|Bulgoo Formation|43398|14|Not recorded|Map Legend||Late Devonian|Part of Mulga Downs Group.||||||08-APR-09
2869|Bulgoo Formation|61964|6|Mentioned|p120|Late Devonian|Late Devonian|Of the Mulga Downs Group - possible correlative within this group to Naradhan Sandstone of Cocoparra Group.||||||27-OCT-08
2869|Bulgoo Formation|64964|5|Briefly described|p163|||Of Mulga Downs Group. Presented as Bulgoo only in list of formations.||||||08-APR-09
2869|Bulgoo Formation|64967|5|Briefly described|p114 Fig. 2|Eifelian|Eifelian|Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). See also p115 Fig. 3.||||||
2869|Bulgoo Formation|65759|5|Briefly described|p114 Fig.2||Eifelian|Unconformably underlies the Bundycoola Formation, overlies the Merrimerriwa Formation. 2600m thick, part of the Mulga Downs Group.||||||
2869|Bulgoo Formation|67870|5|Briefly described|p62|Devonian|Devonian|Darling Basin. ||Mulga Downs Group.||Is overlain unconformably by Bundycoota Formation.||
2869|Bulgoo Formation|70751|6|Mentioned|p12|Emsian|Emsian|||Mulga Downs Group||||
2869|Bulgoo Formation|72958|6|Mentioned|p11|Emsian|Emsian|Cobar Basin. Nymagee area.||Mulga Downs Group||Underlain by Merrimerriwa Formation. Overlain by Bundycoola Formation.||
2885|Bullanamang Porphyry|22768|6|Mentioned|p178|||||||||
2885|Bullanamang Porphyry|22815|4|Described|p40-41|Late Silurian|Late Silurian|See also the misspelt Bullamanang Porphyry (p39 Fig. 16).||||||11-NOV-14
2885|Bullanamang Porphyry|22857|5|Briefly described|p178, p464 App.1 Tb.A1.6|Silurian|Silurian|Of the Bredbo Group. Coarse rhyolite porphyry. Max. thickness: 500m. Geological Province: Canberra-Yass Shelf. See also p468 App.1 Tb.A1.6.||||||
2885|Bullanamang Porphyry|32820|6|Mentioned|p6|||||||||
2885|Bullanamang Porphyry|36413|2|Defined|p86|Early Devonian|Early Devonian|||||||
2885|Bullanamang Porphyry|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Porphyry. GSNSW map code: S-Du.||||||
2885|Bullanamang Porphyry|39626|6|Mentioned|p275|||||||||
2885|Bullanamang Porphyry|40328|4|Described|p203|||||||||
2885|Bullanamang Porphyry|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bredbo Group.||||||20-MAY-08
2885|Bullanamang Porphyry|49690|5|Briefly described|Tb.7, p15  |||Between Bredbo and Cooma.||||Intrudes the Colinton Volcanics|Sill-like body. Very coarse, massive to sheared, grey rhyolitic porphyry similar to Livingstone Porphyry; local pink feldspar megacrysts.|
2889|Bullawyarra Schist|22638|6|Mentioned|p13|||Jindalee Group. Tumut 1: 100 000 map sheet.||||||
2889|Bullawyarra Schist|22768|6|Mentioned|p174,183|||||||||
2889|Bullawyarra Schist|22857|5|Briefly described|p418 App.1 Tb. A1.5, p183|Ordovician|Cambrian|Of the Jindalee Goup. Metabasalt, minor cherty argillite. See also p174.||||||
2889|Bullawyarra Schist|29450|6|Mentioned|p55|||||||||
2889|Bullawyarra Schist|29454|4|Described|p11|||Pre-M.Silurian||||||
2889|Bullawyarra Schist|29648|6|Mentioned|p18|||||||||
2889|Bullawyarra Schist|30334|6|Mentioned|p121|||||||||
2889|Bullawyarra Schist|35070|6|Mentioned|p11|||||||||
2889|Bullawyarra Schist|35185|6|Mentioned|p230|||||||||
2889|Bullawyarra Schist|35194|6|Mentioned|p68|||||||||
2889|Bullawyarra Schist|35609|6|Mentioned|p3|||Refers Ashley et al.(1972).||||||
2889|Bullawyarra Schist|36534|6|Mentioned|p225|||||||||
2889|Bullawyarra Schist|37529|6|Mentioned|p4|||||||||
2889|Bullawyarra Schist|37727|6|Mentioned|p39|||See also Fig.1||||||
2889|Bullawyarra Schist|39331|4|Described|p36|||See also p33.||||||19-JAN-17
2889|Bullawyarra Schist|40328|5|Briefly described|p37|||||||||
2889|Bullawyarra Schist|40497|6|Mentioned|Map legend|Ordovician|Cambrian|Ordovician - Cambrian||||||
2889|Bullawyarra Schist|40498|6|Mentioned|Fig.19|||||||||
2889|Bullawyarra Schist|42045|4|Described|p149|||||||||
2889|Bullawyarra Schist|42145|4|Described|Table 1 P624|||||||||
2889|Bullawyarra Schist|42313|3|Fully described|p27|Early Ordovician|Cambrian|||||||
2889|Bullawyarra Schist|42314|5|Briefly described|Map|Cambrian||||||||
2889|Bullawyarra Schist|42497|5|Briefly described|Map legend|Bolindian|Bolindian|||||||
2889|Bullawyarra Schist|42828|5|Briefly described|Table 1 P129|Early Ordovician|Cambrian|||||||
2889|Bullawyarra Schist|44093|6|Mentioned|p29|||Contains greenstone.||||||
2889|Bullawyarra Schist|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
2889|Bullawyarra Schist|69043|4|Described|p2, p57-58, p61|Early Silurian|Early Silurian|Tumut Trough: E of Gundagai. Type locality is on the property "Bullawyarra" (Basden, 1990).|||Jindalee Group.|Is intruded by Blacks Flat Diorite, which provides minimum age constraint..|Mafic.|19-JAN-17
2891|Bulldog Shale|12597|5|Briefly described|p492 Tb.1, p499-500|Albian|Aptian|SW Eromanga Basin. 200-320m thick.|||||Includes a basal organic mudstone, 25m thick, with a distinctive gamma-ray response.|
2891|Bulldog Shale|13497|5|Briefly described|p115 fig 6.33, p151-p154, p170-p171|Early Cretaceous|Early Cretaceous|Eromanga Basin. Forms a regional oil and gas seal. ||Marree Subgroup||Overlies the Cadna-owie Formation. Overlain by the Coorikiana Sandstone and the Oodnadatta Formation.||
2891|Bulldog Shale|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Marree Subgroup||||
2891|Bulldog Shale|22874|6|Mentioned|P18|||||||||
2891|Bulldog Shale|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Coorikiana Sandstone, underlying unit is Wyandra Sandstone Member||||||
2891|Bulldog Shale|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
2891|Bulldog Shale|22922|6|Mentioned|33 fig 2|||||||||
2891|Bulldog Shale|23054|4|Described|p21,24-5|||||||||
2891|Bulldog Shale|23056|6|Mentioned|12 table 2|||||||||
2891|Bulldog Shale|23123|5|Briefly described|p404||Cretaceous|||||||
2891|Bulldog Shale|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Parent - Marree Subgroup of the Neales River Group.||||||
2891|Bulldog Shale|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age Determinations discussed on p 30.||||||
2891|Bulldog Shale|23282|6|Mentioned|p85 Fig 6.2|||of Eromanga Basin.||||||
2891|Bulldog Shale|23341|6|Mentioned|18|||||||||
2891|Bulldog Shale|23375|4|Described|Fig2 p265|Albian|Barremian|Laterally equivalent to Wallumbilla Formation. Of Eromanga Basin.||||||31-JAN-08
2891|Bulldog Shale|23818|5|Briefly described|p141 Fig.65, p144 Fig.66, p156|Aptian|Aptian|Geological Province: Great Artesian Basin. Of the Neales River Group. Underlying unit: Cadna-owie Formation. Max. thickness: 1500 ft.||||||
2891|Bulldog Shale|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||
2891|Bulldog Shale|23849|5|Briefly described|p777|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|23879|5|Briefly described|p20|Early Cretaceous|Early Cretaceous|Max. thickness: 110m.||||||
2891|Bulldog Shale|23982|5|Briefly described|p57|||Of Neales River Group.  Geological Province: Great Artesian Basin.||||||
2891|Bulldog Shale|24085|5|Briefly described|p33, p38, p41|Albian|Albian|Geological Province: Eromanga Basin.||||||16-MAR-05
2891|Bulldog Shale|24092|5|Briefly described|p8 Fig.3|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24112|5|Briefly described|p254 Fig.2, p270|Early Cretaceous|Early Cretaceous|Max. Thickness: 2000m. Geological Province: Eromanga Basin||||||
2891|Bulldog Shale|24175|3|Fully described|p22, p17 Fig. 3|Albian|Aptian|Dark grey, bioturbated shaly mudstone with silty and very fine sandy layers. Locally includes Wilpoorinna Breccia Member at its base.  Geological Province: Eromanga Basin.||||||16-SEP-08
2891|Bulldog Shale|24204|5|Briefly described|p263 Fig.4, p266 Fig.7|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24321|5|Briefly described|Map legend|Maastrichtian|Maastrichtian|Parent: Neales River Group (of the Marree Subgroup).||||||
2891|Bulldog Shale|24392|5|Briefly described|p140, p142|Albian|Aptian|Overlies the Cadna-owie Formation disconformably. Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|24506|5|Briefly described|p17|Mesozoic|Mesozoic|Marine mudstone.||||||
2891|Bulldog Shale|29379|4|Described|p28|||Information on lithology. Lower Cretaceous.||||||
2891|Bulldog Shale|29651|6|Mentioned|p25|||||||||
2891|Bulldog Shale|30540|6|Mentioned|Fig.6|||||||||
2891|Bulldog Shale|30803|6|Mentioned|p1|||Cretaceous||||||
2891|Bulldog Shale|30804|6|Mentioned|p10|||See also Table 1||||||
2891|Bulldog Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
2891|Bulldog Shale|30917|6|Mentioned|p42|||See also P53||||||
2891|Bulldog Shale|30919|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|30921|6|Mentioned|Map legend|Turonian|Albian|Neocomian - Turonian||||||
2891|Bulldog Shale|30924|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|31208|6|Mentioned|p46|||See also Fig. 7||||||
2891|Bulldog Shale|31244|6|Mentioned|Table 1|||Lower Cretaceous. See also P6.||||||
2891|Bulldog Shale|31251|6|Mentioned|p75|||Microflora & Microplankton||||||
2891|Bulldog Shale|31699|4|Described|p133|||Lower Cretaceous||||||
2891|Bulldog Shale|31923|6|Mentioned|p14|||||||||
2891|Bulldog Shale|32033|6|Mentioned|p2|||||||||
2891|Bulldog Shale|32313|6|Mentioned|p165|||||||||
2891|Bulldog Shale|32314|6|Mentioned|Fig. 4|||||||||
2891|Bulldog Shale|33017|6|Mentioned|p5|||||||||
2891|Bulldog Shale|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
2891|Bulldog Shale|33224|6|Mentioned|Fig.33|||Photo.||||||
2891|Bulldog Shale|33490|6|Mentioned|p30|||Correlation. Cretaceous sediments||||||
2891|Bulldog Shale|33491|4|Described|p56|||Mention Fig.2||||||
2891|Bulldog Shale|33521|5|Briefly described|p8|||||||||
2891|Bulldog Shale|33523|6|Mentioned|p17|||||||||
2891|Bulldog Shale|33820|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
2891|Bulldog Shale|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|33822|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
2891|Bulldog Shale|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
2891|Bulldog Shale|33824|6|Mentioned|p12|||Table 2||||||
2891|Bulldog Shale|33825|5|Briefly described|p8|||Strat. table. Lithology||||||
2891|Bulldog Shale|33827|6|Mentioned|p13|||Table 2||||||
2891|Bulldog Shale|33828|6|Mentioned|p5|||Table 1||||||
2891|Bulldog Shale|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
2891|Bulldog Shale|33832|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|33933|6|Mentioned|Fig.4|||||||||
2891|Bulldog Shale|33936|6|Mentioned|Fig.3A|||Cret.||||||
2891|Bulldog Shale|33938|6|Mentioned|p38|||O'lain by Eyre Fm.||||||
2891|Bulldog Shale|33939|6|Mentioned|p385|||L.Cret.||||||
2891|Bulldog Shale|33971|5|Briefly described|p37|||See also Fig. 15.||||||
2891|Bulldog Shale|33976|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|34136|6|Mentioned|Fig.|||Lower Cretaceous.||||||
2891|Bulldog Shale|34611|6|Mentioned|Fig.66|||Cretaceous||||||
2891|Bulldog Shale|34830|6|Mentioned|p9|||||||||
2891|Bulldog Shale|34984|5|Briefly described|p322|||||||||
2891|Bulldog Shale|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||08-MAY-13
2891|Bulldog Shale|36213|6|Mentioned|p85|||||||||
2891|Bulldog Shale|36214|5|Briefly described|p58|||||||||
2891|Bulldog Shale|36494|6|Mentioned|p155|||||||||
2891|Bulldog Shale|36552|6|Mentioned|p60|||||||||
2891|Bulldog Shale|36571|6|Mentioned|p101|||See also Table 4.||||||
2891|Bulldog Shale|36733|6|Mentioned|p14|||||||||
2891|Bulldog Shale|36922|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|36966|6|Mentioned|p83|||||||||
2891|Bulldog Shale|38022|6|Mentioned|p29|||||||||
2891|Bulldog Shale|38068|4|Described|p72|||||||||
2891|Bulldog Shale|38199|6|Mentioned|p426|||||||||
2891|Bulldog Shale|38604|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|38605|4|Described|p24|||See also Table 4.||||||
2891|Bulldog Shale|38814|6|Mentioned|Table 1|||||||||
2891|Bulldog Shale|39211|6|Mentioned|p11|||Correlation Coreena Mb in Qld. See also Fig. 6,10,12, etc.||||||
2891|Bulldog Shale|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
2891|Bulldog Shale|39630|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|39914|6|Mentioned|p2|||||||||
2891|Bulldog Shale|40003|6|Mentioned|Fig.9|||||||||
2891|Bulldog Shale|40058|6|Mentioned|p4|||||||||
2891|Bulldog Shale|40199|6|Mentioned|p16|||||||||
2891|Bulldog Shale|40220|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|40670|6|Mentioned|Fig.9|||||||||
2891|Bulldog Shale|40681|6|Mentioned|p13|||||||||
2891|Bulldog Shale|40801|6|Mentioned|p84|||||||||
2891|Bulldog Shale|40910|6|Mentioned|p15|||||||||
2891|Bulldog Shale|40911|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|40912|6|Mentioned|Map legend|Aptian|Aptian|||||||
2891|Bulldog Shale|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|40926|3|Fully described|p16|||||||||
2891|Bulldog Shale|41060|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|41062|6|Mentioned|Fig.5|||||||||
2891|Bulldog Shale|41064|6|Mentioned|p62,p67|||||||||
2891|Bulldog Shale|41084|5|Briefly described|Fig.2|||||||||
2891|Bulldog Shale|41085|3|Fully described|p88|||||||||
2891|Bulldog Shale|41086|3|Fully described|p98|||||||||
2891|Bulldog Shale|41087|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41088|6|Mentioned|p143|||||||||
2891|Bulldog Shale|41098|4|Described|p176|||||||||
2891|Bulldog Shale|41117|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41165|6|Mentioned|p360|||See also Fig.15||||||
2891|Bulldog Shale|41175|6|Mentioned|Fig.1|||||||||
2891|Bulldog Shale|41177|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41182|3|Fully described|p289|||||||||
2891|Bulldog Shale|41183|6|Mentioned|Fig.3 p308|||||||||
2891|Bulldog Shale|41184|6|Mentioned|p347|||||||||
2891|Bulldog Shale|41187|6|Mentioned|Fig.2|||||||||
2891|Bulldog Shale|41216|6|Mentioned|Fig.18|||||||||
2891|Bulldog Shale|41266|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|41276|6|Mentioned|p62|||||||||
2891|Bulldog Shale|41288|6|Mentioned|Fig.7|||||||||
2891|Bulldog Shale|41361|6|Mentioned|Fig.3|||||||||
2891|Bulldog Shale|41427|6|Mentioned|p84|||||||||
2891|Bulldog Shale|41523|3|Fully described|p275|||||||||
2891|Bulldog Shale|41950|5|Briefly described|Fig.2 P3|||||||||
2891|Bulldog Shale|42071|6|Mentioned|p117|||||||||
2891|Bulldog Shale|42099|6|Mentioned|Fig.2 P63|||||||||
2891|Bulldog Shale|42293|4|Described|p17|Albian|Aptian|||||||
2891|Bulldog Shale|42346|4|Described|p78, Fig.3 p80|||Part of Maree Subgroup.||||||16-SEP-08
2891|Bulldog Shale|42375|5|Briefly described|Fig.5 P24,|Late Cretaceous|Jurassic|Eromanga Basin. See also Table 1 p11, Fig.28 p125.||||||
2891|Bulldog Shale|42395|5|Briefly described|Fig.13 P83|||||||||
2891|Bulldog Shale|42465|5|Briefly described|Map Legend|||||||||
2891|Bulldog Shale|42469|4|Described|p35|||||||||
2891|Bulldog Shale|42520|5|Briefly described|p6|||||||||
2891|Bulldog Shale|42546|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
2891|Bulldog Shale|42602|6|Mentioned|Fig.2 P20|||||||||
2891|Bulldog Shale|42723|5|Briefly described|map legend|Aptian||||||||
2891|Bulldog Shale|42736|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
2891|Bulldog Shale|42746|4|Described|p12|||See also Fig.6||||||
2891|Bulldog Shale|42804|6|Mentioned|p118|||||||||
2891|Bulldog Shale|42816|5|Briefly described|p18|||||||||
2891|Bulldog Shale|42899|5|Briefly described|p349|||||||||
2891|Bulldog Shale|42905|5|Briefly described|p20|||Of Marree Subgroup.||||||16-SEP-08
2891|Bulldog Shale|43048|4|Described|Table 3.|||In the Marree Subgroup.||||||17-JAN-08
2891|Bulldog Shale|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||25-MAY-05
2891|Bulldog Shale|43085|5|Briefly described|Fig.6|||||||||
2891|Bulldog Shale|43202|5|Briefly described|p17||Cretaceous|||||||
2891|Bulldog Shale|43258|5|Briefly described|Map Legend||Cretaceous|||||||
2891|Bulldog Shale|43298|5|Briefly described|Map Legend||Cretaceous|||||||
2891|Bulldog Shale|43591|6|Mentioned|p40,165||Early Cretaceous|||||||
2891|Bulldog Shale|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
2891|Bulldog Shale|43681|4|Described|p295||Early Cretaceous|||||||
2891|Bulldog Shale|43743|6|Mentioned|Fig.2,p33||Early Cretaceous|||||||
2891|Bulldog Shale|43840|5|Briefly described|Fig3 p12||Cretaceous|||||||12-JUL-16
2891|Bulldog Shale|44133|4|Described|p45, 117, 104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Marree Subgroup. Includes: Wilpoorinna Breccia Member. Maximum Thickness: ~340m. Conformably underlies: Coorikiana Sandstone.||||||08-MAY-13
2891|Bulldog Shale|44289|5|Briefly described|Map Legend||Albian|||||||
2891|Bulldog Shale|44658|14|Not recorded|map legend|||Neoc.-Albian (G53-15).||||||
2891|Bulldog Shale|44934|5|Briefly described|Map Legend||Cretaceous|||||||
2891|Bulldog Shale|44935|5|Briefly described|Map Legend||Aptian|||||||
2891|Bulldog Shale|45132|6|Mentioned|p14|||||||||
2891|Bulldog Shale|46791|6|Mentioned|p44|||Time equivalent of Wallumbilla Formation||||||
2891|Bulldog Shale|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
2891|Bulldog Shale|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
2891|Bulldog Shale|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
2891|Bulldog Shale|60564|5|Briefly described|p4, p5|||Overlain by the Alpha Mudstone.||||||
2891|Bulldog Shale|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Cadna-owie Formation. Overlain by Coorikiana Sandstone. Lateral to Wallumbilla Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
2891|Bulldog Shale|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||27-APR-05
2891|Bulldog Shale|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Of the Marree Subgroup.||||||13-APR-05
2891|Bulldog Shale|61014|6|Mentioned|p533, p543. |Early Cretaceous|Early Cretaceous|Eromanga Basin. Open marine conditions.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone.||21-JAN-15
2891|Bulldog Shale|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Marine mudstone.||||||
2891|Bulldog Shale|61560|5|Briefly described|p491|Early Cretaceous|Early Cretaceous|Contains the Mt Toondina impact structure.  Geological Province: Arckaringa Basin (SA). ||||||
2891|Bulldog Shale|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
2891|Bulldog Shale|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
2891|Bulldog Shale|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
2891|Bulldog Shale|61836|5|Briefly described|p211|Cretaceous|Cretaceous|Overlies Cadna-Owie Formation. Geological Province: Eromanga Basin.||||||05-OCT-06
2891|Bulldog Shale|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
2891|Bulldog Shale|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation and Namur Sandstone. Is overlain by Oodnadatta and Toolebuc Formations.||
2891|Bulldog Shale|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
2891|Bulldog Shale|63124|6|Mentioned|p62|||Geological Province: Eromanga Basin.||||||
2891|Bulldog Shale|63894|5|Briefly described|p169, p179-180|Cretaceous|Cretaceous|Overlies Cadna-owie Formation. Marine mudstone and aquitard, fractured. Penetrated by spring mounds forming hard carbonate caps on top of pedestal of the shale. Surrounding areas is eroded and forms the Bulldog Shale plain.||||||
2891|Bulldog Shale|63979|6|Mentioned|p48, Fig. 44|Albian|Barremian|SA unit that equates to lower section of Wallumbilla Formation in Qld.||||||07-FEB-11
2891|Bulldog Shale|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Cretaceous|Cretaceous|Eromanga Basin. Coeval with Wallumbilla Formation.||Unit in Marree Subgroup.||Underlies the Coorikiana Sandstone, overlies the Cadna-owie Formation.||
2891|Bulldog Shale|64696|5|Briefly described|p133 Fig.14|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|64778|6|Mentioned|p13, 16-17, 19-20|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins. Max. palaeotemperature analysis summary.||||||
2891|Bulldog Shale|65194|6|Mentioned|p46|||Of Marree Subgroup. Aquitard.||||||
2891|Bulldog Shale|65238|5|Briefly described|p5 Fig. 6, p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Marine deposits.||||||17-FEB-10
2891|Bulldog Shale|65309|5|Briefly described|p6 Table 1, p15, p19.|Cretaceous|Cretaceous|Flat-lying, widespread unit of an early Cretaceous marine incursion in Eromanga Basin.||||Overlies Algebuckina Sandstone in a few scattered exposures on summits of mesas.|Pale yellow to white, massive to laminated, very fine siltstone; locally silicified to porcellanite.|
2891|Bulldog Shale|65342|6|Mentioned|p9.|||Eromanga Basin. Max. thickness at least 237m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
2891|Bulldog Shale|65376|6|Mentioned|p140 Fig.4.22.|Cretaceous|Cretaceous|||||||
2891|Bulldog Shale|65385|4|Described|pS128 Fig.2, pS133, pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Mudstone, minor silt to fine-grained sandstone intervals. Overlies Cadna-owie Formation. Overlain by Coorikiana Sandstone.||||||08-MAR-12
2891|Bulldog Shale|65489|5|Briefly described|p55, p59, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 320m thick. Regional seal to Cadna-owie Formation.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone or Oodnadatta Formation.||
2891|Bulldog Shale|65689|5|Briefly described|pp154-155, p160|Albian|Aptian|Eromanga Basin. Fossiliferous; diverse range of microfossils, bivalve molluscs, gastropods, ammonites, belemnites; large quantities of wood; a range of plesiosaur taxa; fish. Glendonites indicate cold conditions/high latitudes.||Unit in Marree Subgroup.|||Sequence of shallowly dipping marine strata, mainly mudstones and claystones; coquinoid layers common; isolated sandy deposits. Extensive opal deposits, typically associated with severe leaching and weathering.|
2891|Bulldog Shale|65925|5|Briefly described|p9, p47, p49, Appendix 2.|Cretaceous|Cretaceous|Eromanga Basin. Contains abundant organic matter.||||Is unconformably overlain by Eyre Formation and Namba Formation.|Grey, bioturbated, fossiliferous and shaly mudstone; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|66131|6|Mentioned|p247, p248 Fig.6|||Crops out in flanks of many hills (and mound springs).||||||
2891|Bulldog Shale|66303|5|Briefly described|pp27-28.|Early Cretaceous|Early Cretaceous|Widespread unit in Eromanga Basin. Early Aptian to middle Albian. Correlated with Cyclosporites hughesii and Crybelosporites striatus spore-pollen zones, and extends into the Coptospora paradoxa spore-pollen zone.||||Overlies Cadna-owie Formation. Is overlain by Eyre Formation.|Dark grey, bioturbated and fossiliferous shaly mudstone.|
2891|Bulldog Shale|66518|5|Briefly described|p19, p23.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Acts as a seal for migrating hydrocarbons from significant resources in the north of the Basin.||Unit in Marree Subgroup.||Overlies Cadna-owie Formation and Parabarana Sandstone. Is overlain by Oodnadatta Formation and locally by Coorikiana Sandstone.|Greenish-grey to bluish-grey mudstones.|
2891|Bulldog Shale|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin. ||Unit in Neales River Group.||Overlies Toolebuc Formation. Is overlain by Mackunda or Normanton Formations.|Deeper marine shale and mudstone.|
2891|Bulldog Shale|66623|6|Mentioned|p254, p258, p260.|||Laterally equivalent to Wallumbilla Formation and Doncaster Member in NSW.||||Overlies Wyandra Sandstone Member.||
2891|Bulldog Shale|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Mudstone, grey, bioturbated, fossiliferous and shaly; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone and Oodnadatta Formation.||
2891|Bulldog Shale|67474|5|Briefly described|p56|Cretaceous|Cretaceous|Confining unit for the main Great Artesian Basin aquifer. Grey marine shaly mudstone.||||||21-DEC-11
2891|Bulldog Shale|67561|5|Briefly described|p51-54, p57 Fig.6, p58, p64, p65|Aptian|Aptian|Eromanga Basin. Australian Spore-Pollen zonation: C.hughesi. Deposited on a shallow marine shelf during a cold climate transgression.||||Underlain by the Wyandra Sandstone Member. Correlative of the Wallumbilla Formation.|Contains glendonites, petrified wood, and ice-rafted boulders of exotic lithology.|20-JAN-17
2891|Bulldog Shale|67578|6|Mentioned|p334, p336 Fig.3|Cretaceous|Cretaceous|||||Is overlain unconformably by Eyre Formation.||
2891|Bulldog Shale|67784|6|Mentioned|p26, p28 table 1|||Southern Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone.||08-FEB-18
2891|Bulldog Shale|68068|5|Briefly described|Map legend|Albian|Aptian|Eromanga Basin. Open marine, shallow to moderate depth; very cold, ?seasonal periglacial, conditions.||Unit in Marree Subgroup.||Overlies Parabarana Sandstone conformably to unconformably. Is overlain by Coorikiana Sandstone.|Laminated marine clay to silt, sandy lenses; dark grey to dark grey-brown, bioturbated, mid-unit concretions and exotic lonestones; glendonites; fossiliferous (molluscs, forams, wood, microflora, fish teeth, vertebrates).|18-NOV-14
2891|Bulldog Shale|68157|6|Mentioned|p8|Early Cretaceous|Early Cretaceous|core sample anaysed in this paper is a Bulldog Shale equivalent||||||07-NOV-14
2891|Bulldog Shale|68206|6|Mentioned|p27, 36-38|Albian|Aptian|S Eromanga Basin. Suggests that the South Pole was not ice-free during the Early Cretaceous (discussed).|||||Contains glendonites and dropstones.|
2891|Bulldog Shale|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Marree Subgroup.||||
2891|Bulldog Shale|68715|6|Mentioned|p30 Fig.5|Albian|Aptian|Eromanga Basin.||||||
2891|Bulldog Shale|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Albian|Barremian|Eromanga Basin (SW). Opal-bearing. Marine. The opal layer is typically found within cracks and joints proximal to the interface between heavily weathered shale.||Of the Rolling Downs Group.|||Kaolinite rich.|20-JAN-22
2891|Bulldog Shale|68821|5|Briefly described|p292, pp295-297, p307, p309|Albian|Aptian|Lower Cretaceous age. Equivalent to the Wallumbilla Formation and the Doncaster Member. Contains ubiquitous disseminated pyrite. Marine depositional environment.||Of the Rolling Downs Group.||Unconformably overlain by the Eyre Formation.|Comprises of sandstone and siltstone.|
2891|Bulldog Shale|69001|5|Briefly described|p11, p16, p17, p35, p63, p69, pp72-73|Early Cretaceous|Early Cretaceous|Marine sediments. Pyritic and organic-rich.||Of the Maree Subgroup.||Equivalent to the Whittabrenah Shale.|Comprises grey fossiliferous mudstone-siltstones with regressive marine sandstones.|
2891|Bulldog Shale|69004|6|Mentioned|p12, p15|Cretaceous|Jurassic|Eromanga Basin.||||||
2891|Bulldog Shale|69019|4|Described|p83 Fig.20, p85 Fig.21, p93-97, p167.|Albian|Aptian|Of Freytag (1966). SW Eromanga Basin. Formerly Marree Formation. Max. thickness 277 m. Hosts minor deposits of celestite and barite. Has lonestone casts (dropstones) abundant in lower third of the unit.||Unit in Marree Subgroup.|Includes Wilpoorinna Breccia Member.|Conformably overlies Cadna-owie Formation and Parabarana Sandstone. Is overlain conformably by Coorikiana Sandstone.|Grey to dark grey, laminated to thinly planar, bedded to poorly bedded shale; highly bioturbated in many areas; contains ellipsoidal carbonate concretions, esp. towards the base where cone-in-cone limestone pods also occur.|
2891|Bulldog Shale|69023|4|Described|p77, p87, p89 Fig.20, p93-94, p96-97|Albian|Aptian|See also p99-100, p103-104, p110, p119, p126, p151, p191-192, p204. Defined by Freytag (1966). Eromanga Basin. Up to 336.4m thick. Diverse animal, plant and microfossil remains are described. Local silcrete capping. Is a seal for the Parabarana Sandstone aquifer. Stratigraphic wells intersection data.|c.105 Ma.|Unit in Marree Subgroup.||Conformably overlies Parabarana Sandstone and Cadna-owie Formation. Passes laterally into Wallumbilla Formation. Is overlain conformably by Coorikiana Sandstone.|Grey to dark grey shale with carbonate concretions; laminated to poorly bedded, commonly highly bioturbated; contains glendonites, lonestones (?dropstones) and occasional pyrite-marcasite nodules or bands; basal silty to sandy section.|
2891|Bulldog Shale|69203|5|Briefly described|p11-12, p57|Cretaceous|Cretaceous||||||Clay and shale, mudstone and fine-grained sandstone; local extremely hard white potch layers.|
2891|Bulldog Shale|69457|5|Briefly described|p41:3-8, 10, 14-15|Early Cretaceous|Early Cretaceous|Freytag (1966). Eromanga Basin. This name has previously (and inappropriately) been used to describe the Wallumbilla Formation in the NT (eg Questa, 1990; Ambrose and Heugh, 2010). Has fair to occasionally excellent petroleum source intervals.||Marree Subgroup.||Disconformably overlies De Souza Sandstone. Is overlain by Coorikiana Sandstone.|Contains diverse fossil assemblages, as well as glendonite nodules and dropstones.|12-JUL-16
2891|Bulldog Shale|69554|6|Mentioned|p131|Cretaceous|Cretaceous|Northern Gawler Craton.||||||
2891|Bulldog Shale|69562|6|Mentioned|p662 Tb.2, p664 Tb.4, p666 Fig.3|Cretaceous|Cretaceous|See also p667 Fig.4, p668, p679-680, p682 Fig.11. Electrical conductivity value used in forward modelling: 1000 mS/m.||Unit in Marree Subgroup.|||Highly conductive pyritic black muds.|
2891|Bulldog Shale|69568|5|Briefly described|p443-444|Cretaceous|Cretaceous|Lake Frome region, Eromanga Basin. Non-marine.||||Is overlain unconformably by Eyre Formation.|Blue-grey, silty bioturbated clay mudstone with abundant organic matter.|
2891|Bulldog Shale|69673|6|Mentioned|p155 fig 127, p159|Cretaceous|Cretaceous|||||Overlies Mount Anna Sandstone Member, overlain by Coorikiana Sandstone, correlated with Wallumbilla Formation||
2891|Bulldog Shale|69742|5|Briefly described|p787, 788, p790, 793|Cretaceous|Cretaceous|Great Artesian Basin. Coober Pedy. Marine. Geochemistry discussed.|||||Kaolinite-dominated shale with quartz, smectite and illite.|
2891|Bulldog Shale|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
2891|Bulldog Shale|69946|3|Fully described|p19, p21-24, p38, p56-57, p94, p99-111|Early Cretaceous|Early Cretaceous|Freytag (1966), for the dark grey shale between Cadna-owie Formation and Coorikiana Sandstone. Type section is outcrop 8km S of Bulldog Creek. Large clasts include Adelaidean slate, quartzite, laminated siltstone and Gawler Range Volcanics. From c.200 to >340 m thick. Early Aptian to mid Albian. Fossil groups listed. Wireline log correlations.||Basal unit in Marree Subgroup.||Conformably overlies Cadna-owie Formation. Is overlain conformably by Coorikiana Sandstone. Lateral equivalent of Wallumbilla Formation.|Dark grey, bioturbated and fossiliferous mudstone, with minor interbeds of micaceous siltstone and very fine-grained sandstone; pyrite and diagenetic carbonate nodules; glendonite nodules in outcrop; local lonestones and layers with fossil wood.|
2891|Bulldog Shale|69947|5|Briefly described|p9, p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||Overlies Wyandra Sandstone Member (Cadna-owie Formation). Is overlain by Coorikiana Sandstone.|Thick, fossiliferous mudstones and siltstones.|
2891|Bulldog Shale|69948|6|Mentioned|p4; Figs.4.1, 18|||Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Oodnadatta Formation.|Marine shales.|
2891|Bulldog Shale|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Of Marree Subgroup.|||Grey, bioturbated, fossiliferous and shaly mudstone; minor silt to very fine-grained sandstone intervals.|12-JAN-16
2891|Bulldog Shale|70338|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Mudstone, grey, bioturbated, fossiliferous and shaly; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|70383|5|Briefly described|p45, p51-52|Early Cretaceous|Early Cretaceous|Marine deposits. Contains fossiliferous (fish) Devonian sandstone boulders; thought to originate from the Amphitheatre and Mulga Downs Groups, and been transported NW to South Australia during the Permian glaciation, and later reworked into the basal Bulldog Shale.||||Overlies Cadna-owie Formation.||
2891|Bulldog Shale|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin. Open marine deposits; shallow to moderate depth. Fossils include molluscs, forams, petrified wood, microflora, fish teeth and vertebrates. Maximum depositional age from detrital zircons.|< ~110 Ma (SHRIMP U-Pb).|Marree Subgroup.||Overlies Cadna-owie Formation. Is overlain gradationally by Coorikiana Sandstone.|Dark grey to dark grey-brown, laminated clay to silt, sandy lenses, bioturbated; mid-unit limestone concretions and exotic glacial dropstones and cone-in-cone limestone pods. Glendonites in lower midsection (periglacial).|
2891|Bulldog Shale|70789|5|Briefly described|p318, p320 Fig.4, p326, p328|Early Cretaceous|Early Cretaceous|Eromanga Basin. Aptian-early Albian. Thickness varies from <100m to maximum of 500m. An aquitard.|125-106 Ma.|||Overlies Cadna-owie Formation.|Pyritic, carbonaceous and glauconitic shales and mudstones.|
2891|Bulldog Shale|70821|5|Briefly described|p21 Fig.2.6, p23, p82, p117|Early Cretaceous|Early Cretaceous|Eromanga Basin. Highly conductive.||Marree Subgroup.||Overlies Cadna-owie Formation. Is overlain by Coorikiana Sandstone. Equivalent to Wallumbilla Formation.||
2891|Bulldog Shale|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 320m thick. Deposited in an open marine, transgressive environment.||||Overlies the Cadna-owie Formation. Overlain by the Coorikiana Sandstone.||
2891|Bulldog Shale|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
2891|Bulldog Shale|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.||||
2891|Bulldog Shale|71043|5|Briefly described|p106|||Gawler Craton.|||||Claystone, shale, ferruginous sandstone.|
2891|Bulldog Shale|71321|4|Described|p1,4,15,24-29,65|Albian|Early Aptian|Of Eromanga Basin. Crops out on the eastern and southern margin of TIEYON mapsheet. Depositional environment: marine shelf affected by high-latitude storms. Highstand systems tract following peak marine transgression during the Early Cretaceous. Micro-paleontological studies indicate an early Aptian to mid-Albian age (Krieg, et al., 1995). highly weathered in outcrop, mudstones bleached white to beige with shaly fissility, or have undergone iron oxidation.||||Underlain by Cadna-owie Formation or Algebuckina Formation. Overlain by the Oodnadatta Formation. Equivalent to Wallumbilla Formation and Rumbalara Shale.|Dark grey, laminated to massive, bioturbated and fossiliferous mudstone, with minor interbeds of micaceous siltstone and finely cross-laminated to irregularly interlaminated, fine-grained sandstone.|24-OCT-19
2891|Bulldog Shale|71342|4|Described|Ch1 p19, Ch4 p4, Ch4 p8, Ch5 p19-p24|Albian|Aptian|This unit was first defined by Freytag (1966) as the dark grey shale between the Cadna-owie Formation and the Coorikiana Sandstone. Freytag also defined the type section as outcropping 8km south of Bulldog Creek. Lithology is discussed in detail. This unit has a maximum thickness in excess of 340m in the Moomba area. Age assigned on the basis of palynology and fossil assemblage. Sedimentology and palaeoenvironment are discussed in detail. Spore-pollen zone is given in Ch5 p57. On the basis of spore-pollen zones, two major marine transgressions are inferred. See also  Ch5 p30, Ch5 p32-p33, Ch5 p38, Ch5 p100-p112, Ch6 p7-p8, Ch6 p10, Ch6 p14, Ch6 p19-p20, Ch7 p9, Ch7 p13, Ch8 p7, Ch8 p10, Ch8 p25-p26, Ch9 p20, Ch9 p21, Ch11 p4-p5, Ch14 p5.||Marree Subgroup||Conformably overlies the Cadna-owie Formation or the Algebuckina Sandstone. Conformably overlain by the Coorikiana Sandstone. Overlain by the Oodnadatta Formation.|Darl grey, bioturbated and fossiliferous mudstone with minor interbeds of micaceous siltstone and very fine-grained sandstone.|
2891|Bulldog Shale|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
2891|Bulldog Shale|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Neales River Group.||Overlies Cadna-owie FZ. Is overlain by Coorikiana Sandstone.||
2891|Bulldog Shale|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet. |||||Mudstone, grey, bioturbated, fossiliferous and shaly; minor silt to very fine-grained sandstone intervals.|
2891|Bulldog Shale|72461|6|Mentioned|p24|Mesozoic|Mesozoic|||||||
2891|Bulldog Shale|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
2891|Bulldog Shale|72478|4|Described|p1, p6, p9-12, p18, p24-26|Middle Cretaceous|Early Cretaceous|Eromanga Basin. Deposited in lower-energy, flood-plain, lacustrine and swamp environments. 80m was intersected in GOMA DH1 and GOMA DH3. Appears as a thin layer in GOMA DH2. Overlies an extremely hard massive quartzite interpreted as a correlative of the Pindyin Sandstone. See also p51, 69, 70, 72-75 [of the document].||||Overlies the Cadna-owie Formation. Unconformably overlies the Marla Group.|Fine-grained, sandstone, siltstone and coal.|29-MAR-21
2891|Bulldog Shale|73099|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga basin.||Marree Subgroup.||Overlies Cadna-owie Formation.|Kaolinised and porcellanitic claystone with layers of silt to very fine sand; surficial lag of quartz and quartzite pebbles to boulders.|
2891|Bulldog Shale|73153|6|Mentioned|p285|Aptian|Aptian|Holotype material[?] (SAM P17926) for Kakuru kujani (an indeterminate averostran or tetanuran) was recovered from this unit in South Australia.||||||
2891|Bulldog Shale|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
2891|Bulldog Shale|73203|6|Mentioned|p647, p649-650, p653|||Hosts opal at both Andamooka and Cobber Pedy.||||||
2891|Bulldog Shale|73249|4|Described|p316-323, p324 Fig.4, p325-338|Albian|Aptian|Eromanga Basin. Maximum age of early Aptian, minimum age of mid-Albian. Up to 340m thick in the central Eromanga Basin, ~200m thick on average. Deposited in an epicontinental marine environment, period of shallow marine transgression. Fossils include molluscs, gastropods, ammonites, belemnites and marine reptile remains (Drexel and Priess, 1955). Dominant clay mineral is montmorillonite, quartz is also widely abundant, mineralogy varies between lower and upper parts of the unit as well as laterally between drill holes. Deposited in a more arid, warmer envionment than the Cadna-owie Formation. Sediment sources interpreted to be from active volcanoes to the east, mix of felsic to mafic igneous rocks.||||Conformably overlies the Cadna-owie Formation, conformably underlies the Coorikiana Sandstone, lateral equivalent of the Wallumbilla Formation.|Marine sediments, composed of reduced dark grey bioturbated and fossiliferous mudstone with interbeds of siltstone to very fine sandstone, on average 200m thick.|
2891|Bulldog Shale|73251|4|Described|[See comments]|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Contains sandstone-hosted U deposit. Includes oil-prone organic facies. Marine depositional environment that are at least partly shallow-marginal marine. Contains Bulldog [organic] facies 1. [See article for organic petrology descriptions]. p: 36-37, 40, 42-45, 47-48, 50, 52-54, 56-58, 62.||||Underlain by Parabarana Sandstone unconformably, and Cadna-owie Formation. Overlain by Oodnadatta Formation and Coorikiana Sandstone. Equivalent to Wallumbilla Formation.|Grey siltstone with thin beds of ferruginised siltstone and subordinate fine-grained sandstone.|
2891|Bulldog Shale|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
2891|Bulldog Shale|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin. Hosts oil and gas.||||Underlain by Cadna-owie Formation. Overlain by Coorikiana Sandstone. Equivalent to Wallumbilla Formation.||
2891|Bulldog Shale|73398|5|Briefly described|p1-9, 12-15, 20-30|Early Cretaceous|Early Cretaceous|Eromanga Basin. Overlying the Prominent Hill IOCG deposit, this unit contains up to c.5000 ppm Cu; the authors conclude this resulted from downwards leaching of Cu from the upper, oxidised part of the unit or from physical transport/deposition of Cu-bearing phases. Marine deposits. Geochemical concentration/depth diagrams. Geochemistry, weathering analysed in great detail.|<125 Ma.|||Conformably overlies Cadna-owie Formation.|Reduced dark grey mudstone with minor interbeds of siltstone and fine sandstone. Top 50-70m intensely weathered. Bioturbated and fossiliferous.|
2891|Bulldog Shale|73479|5|Briefly described|p156 Fig.2, p159, p175|Cretaceous|Cretaceous|Eromanga Basin. Restricted open marine depositional environment.|ca 125-108 Ma|||Overlies Cadna-owie Formation, underlies Coorikiana Sandstone||
2895|Bullenbalong Suite|22606|6|Mentioned|P829, P830|||||||||
2895|Bullenbalong Suite|22768|6|Mentioned|p176|||||||||
2895|Bullenbalong Suite|22778|4|Described|p 162|||||||||
2895|Bullenbalong Suite|22815|4|Described|p43,55, fig19|Silurian|Silurian|Contains at least 17 seperate units.||||||
2895|Bullenbalong Suite|22857|5|Briefly described|p176|||Intrusive granite.||||||
2895|Bullenbalong Suite|22876|5|Briefly described|p27|||||||||
2895|Bullenbalong Suite|22877|5|Briefly described|map|Silurian|Silurian|||||||
2895|Bullenbalong Suite|22968|6|Mentioned|Fig49 P92|||||||||
2895|Bullenbalong Suite|23020|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
2895|Bullenbalong Suite|23021|5|Briefly described|Map legend|Wenlock|Wenlock|Nonconformable and angular unconformably overlain by the Enano Group||||||
2895|Bullenbalong Suite|23028|5|Briefly described|Map legend|Wenlock|Wenlock|||||||
2895|Bullenbalong Suite|23029|5|Briefly described|Map legend|Wenlock|Wenlock|Angular unconformably and nonconformably underlies the Enano Group||||||
2895|Bullenbalong Suite|23309|6|Mentioned|p338|||||||||
2895|Bullenbalong Suite|23439|6|Mentioned|p127|||||||||
2895|Bullenbalong Suite|23547|5|Briefly described|p553|||||||||
2895|Bullenbalong Suite|23549|5|Briefly described|p521|||Of Bullenbalong Supersuite. Includes the Jillamatong pluton. Mafic rocks crowded with biotite and cordierite-rich enclaves. Geological Province:  Lachlan Fold Belt.||||||06-FEB-08
2895|Bullenbalong Suite|23615|3|Fully described|p152|Early Devonian|Early Silurian|Composed of several large batholiths - Campbells Knob, Amboyne, Suggan Buggan, Chiplin, Nunniong and Mellick Munjie Granodiorites and Barrabilly Adamellite.  Geological Province: Lachlan Fold Belt.||||||
2895|Bullenbalong Suite|24099|5|Briefly described|p47, p48 Fig. 3|||S-type granite in the Kosciusko Basement Terrane.||||||
2895|Bullenbalong Suite|24222|5|Briefly described|p11|||Chemistry of samples reported. S-type. See also Bullenbalong Supersuite. Geological Province: Lachlan Fold Belt.||||||06-FEB-08
2895|Bullenbalong Suite|24514|6|Mentioned|p31|||S-type.||||||
2895|Bullenbalong Suite|41563|6|Mentioned|p513|||||||||
2895|Bullenbalong Suite|41898|5|Briefly described|p1184|||||||||
2895|Bullenbalong Suite|41905|4|Described|p75|||||||||
2895|Bullenbalong Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
2895|Bullenbalong Suite|42726|5|Briefly described|map legend||Silurian|Of the Bullenbalong Supersuite.  Contains 19 granitic units and one volcanics unit.||||||08-FEB-05
2895|Bullenbalong Suite|42827|5|Briefly described|p431|||||||||
2895|Bullenbalong Suite|43159|6|Mentioned|p3|||Intrusive equivalent of Hawkins Suite of volcanics.||||||
2895|Bullenbalong Suite|43206|5|Briefly described|map legend||Wenlock|||||||
2895|Bullenbalong Suite|43233|5|Briefly described|Map Legend|Late Silurian||of Berridale Batholith.||||||
2895|Bullenbalong Suite|44093|5|Briefly described|p188 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
2895|Bullenbalong Suite|62962|6|Mentioned|p2291|||Geological Province: Lachlan Fold Belt.||||||07-FEB-11
2895|Bullenbalong Suite|68592|6|Mentioned|p1225|||Named after its type pluton, the Bullenbalong Granodiorite.||Unit in Bullenbalong Supersuite.|Includes Bullenbalong Granodiorite.|||
2895|Bullenbalong Suite|69876|5|Briefly described|p316|||Lachlan Fold Belt. Discussed in relation to source rock.|||||S-type granite.|
2895|Bullenbalong Suite|72571|5|Briefly described|p90, p92, p99|||Of the Tasmanides of eastern Australia.|||Includes the Jillamatong Granodiorite.|||
2897|Bullenbalong Supersuite|22606|6|Mentioned|P828, P830|||||||||
2897|Bullenbalong Supersuite|22719|6|Mentioned|p487|||||||||
2897|Bullenbalong Supersuite|22779|5|Briefly described|p 174|||||||||
2897|Bullenbalong Supersuite|22968|6|Mentioned|Fig89 P164, P172||Early Silurian|||||||
2897|Bullenbalong Supersuite|23030|5|Briefly described|Map legend|Silurian|Silurian|||||||
2897|Bullenbalong Supersuite|23439|5|Briefly described|p124 fig.1|||||||||
2897|Bullenbalong Supersuite|23547|5|Briefly described|p553|||||||||
2897|Bullenbalong Supersuite|23549|4|Described|p521|||Consists of 42 S-type granite units, divided into six suites.  Geological Province: Lachlan Fold Belt.  See also Fig 2 p517.||||||05-APR-05
2897|Bullenbalong Supersuite|23551|5|Briefly described|p491|||||||||
2897|Bullenbalong Supersuite|23615|5|Briefly described|p41|||||||||
2897|Bullenbalong Supersuite|24222|5|Briefly described|p4|||See also Bullenbalong supersuite and Bullenbalong Suite.  Geological Province: Lachlan Fold Belt.||||||
2897|Bullenbalong Supersuite|24263|6|Mentioned|p1394|||Geological Province: Lachlan Fold Belt||||||
2897|Bullenbalong Supersuite|24270|6|Mentioned|p1612|||Geological Province: Lachlan Fold Belt.||||||
2897|Bullenbalong Supersuite|24551|5|Briefly described|p234, 728 Table 8.11|||Of the Deddick Province.||||||
2897|Bullenbalong Supersuite|41133|4|Described|p1117|||||||||
2897|Bullenbalong Supersuite|41563|6|Mentioned|p512|||||||||
2897|Bullenbalong Supersuite|42726|5|Briefly described|map legend||Silurian|Includes the Bullenbalong Suite (19 granites and one volcanic unit).||||||08-FEB-05
2897|Bullenbalong Supersuite|43158|5|Briefly described|3,9,10,11|||||||||
2897|Bullenbalong Supersuite|61964|5|Briefly described|p42|||S-type. Geological Province: eastern Lachlan Orogen. ||||||
2897|Bullenbalong Supersuite|68310|6|Mentioned|p236, 241|||An extensive (8750 km2) collection of mafic granites. Geochemical plots of schistose enclaves.|||Cowra Granodiorite.|||
2897|Bullenbalong Supersuite|68592|3|Fully described|p1225-52, p1256-8, p1356-7, p1547, p1549||Silurian|Named after its largest component Suite, whose type pluton was itself named after Bullenbalong North Hill, NE of Jindabyne. Comprises over 40 individual plutons in a 350km belt from NE Victoria to Cowra in NSW. Type Suite is Bullenbalong Suite. Geochemistry detailed. Distinct geochemical similarities with Goobarragandra Volcanics. Weathers readily to form low rounded hills or rolling countryside; mostly cleared for farming/grazing. Hosts Au-bearing quartz veins in the Young Granodiorite.|||Includes Bullenbalong, Young, Cowra, Clear Range and Ingebyrah Suites.|Intrudes Douro Group. Correlated with Hawkins, Goobarragandra and Canowindra Volcanics.|Predominantly granodiorite to tonalite; granite. Strongly peraluminous S-type.|
2897|Bullenbalong Supersuite|70297|4|Described|map legend, on side 2 of map sheet|Wenlock|Wenlock|Age: mid to late Silurian (Wenlock to Pridoli) for Wyangala Supersuite and Bullenbalong Supersuite. Note misspelt as Bullenbalong Group in Time-Space plot.|||Young Granodiorite, Cowra Granodiorite||Reduced, unfractionated, medium-grained S-type, cordierite-biotite granodiorite, tonalite and monzogranite.|06-JUL-16
2897|Bullenbalong Supersuite|72528|5|Briefly described|p11.||||||Includes Boloko Granodiorite.|||
2897|Bullenbalong Supersuite|73215|6|Mentioned|p1002||||||Young Granodiorite.|||
2899|Bullenbung Granite|42726|5|Briefly described|map legend|||Wagga Batholith. No.  594. Ungrouped.||||||06-JUL-16
2899|Bullenbung Granite|71889|5|Briefly described|p35-p37|||Trigg (2017) suggests this may be a part of the Collingullie Granite. Originally delineated by Chappell et al (1991) in the eastern part of LOCKHEART.|||||Medium-grained biotite granite.|
2904|Bulli Coal|22578|6|Mentioned|Fig.10 p400, p402|||||||||
2904|Bulli Coal|22969|4|Described|Fig 4.1b||Late Permian|Sydney Subgroup||||||
2904|Bulli Coal|23881|5|Briefly described|p69 Fig. 7.2|||Of the Illawarra Coal Measures.  Geological Province: Sydney Basin.||||||
2904|Bulli Coal|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||
2904|Bulli Coal|24471|4|Described|p29 Fig.2, p32|Late Permian|Late Permian|Overlies Lawrence and Loddon Sandstones. Top Of Illawarra Coal Measures. Stratigraphically equivalent to Vales Point Coal Member. Geological Province: Sydney Basin.||||||07-FEB-11
2904|Bulli Coal|29900|6|Mentioned|p169|||||||||
2904|Bulli Coal|29901|4|Described|Table 1|||||||||
2904|Bulli Coal|30006|5|Briefly described|p42|||Permian||||||
2904|Bulli Coal|30007|6|Mentioned|p78|||||||||
2904|Bulli Coal|30132|6|Mentioned|Table 1|||||||||
2904|Bulli Coal|31128|6|Mentioned|Table 1|||||||||
2904|Bulli Coal|31887|5|Briefly described|p7|||||||||
2904|Bulli Coal|32618|6|Mentioned|Table 1|||Perm. Strat. table||||||
2904|Bulli Coal|33334|6|Mentioned|Table 3|||||||||
2904|Bulli Coal|33869|6|Mentioned|Fig.2|||||||||
2904|Bulli Coal|36220|4|Described|p53|||See also Table 1, p38 & p50.||||||
2904|Bulli Coal|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
2904|Bulli Coal|36593|5|Briefly described|Table 2|||See also Fig.2||||||
2904|Bulli Coal|36594|6|Mentioned|Table 1|||||||||
2904|Bulli Coal|37089|6|Mentioned|p208|||||||||
2904|Bulli Coal|37090|4|Described|p221|||||||||
2904|Bulli Coal|37730|6|Mentioned|p18|||||||||
2904|Bulli Coal|38615|6|Mentioned|p18|||||||||
2904|Bulli Coal|39287|6|Mentioned|p42|||||||||
2904|Bulli Coal|39293|6|Mentioned|p145|||||||||
2904|Bulli Coal|39306|4|Described|Fig.21.7|||See also p405 & Fig.21.6||||||
2904|Bulli Coal|39308|5|Briefly described|p511|||||||||
2904|Bulli Coal|39309|6|Mentioned|p128|||||||||
2904|Bulli Coal|39661|6|Mentioned|p443|||||||||
2904|Bulli Coal|40044|6|Mentioned|p382|||||||||
2904|Bulli Coal|40275|6|Mentioned|p61|||||||||
2904|Bulli Coal|40631|6|Mentioned|p163|||||||||
2904|Bulli Coal|40744|6|Mentioned|p326|||||||||
2904|Bulli Coal|41226|6|Mentioned|Fig.6|||||||||
2904|Bulli Coal|41595|6|Mentioned|p24|||||||||
2904|Bulli Coal|42642|6|Mentioned|p171-175|||Sydney Basin||||||
2904|Bulli Coal|42737|5|Briefly described|map legend|Permian||||||||
2904|Bulli Coal|42787|5|Briefly described|p133|||||||||
2904|Bulli Coal|42896|4|Described|p24|||Of Sydney Subgroup.||||||12-MAR-09
2904|Bulli Coal|42925|5|Briefly described|Table 18||Late Permian|||||||
2904|Bulli Coal|42947|6|Mentioned|Fig.16|||||||||
2904|Bulli Coal|43028|6|Mentioned|Fig.7,p618|||of Illawarra Coal Measures||||||
2904|Bulli Coal|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
2904|Bulli Coal|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
2904|Bulli Coal|66577|6|Mentioned|pp996-1001.|Permian|Permian|Gives the most prominent high-amplitude reflection horizon in the seismic data, and is thus used in many diagrams in this article.||Topmost unit in Illawarra Coal Measures.||Overlies Eckersley Formation. Is overlain by Wombarra Claystone.||
2904|Bulli Coal|68202|5|Briefly described|p174, 176-178, 180-183|Permian|Permian|Sydney Basin. The stratigraphically highest Permian coal. Thickness between 1.5m and 3m. Stratigraphic column; C, N, S, trace and rare earth elements, isotope data plots. The authors conclude that the Permian-Triassic mass exinction event is recorded ~1m above the Bulli Coal, i.e. in the basal shales of the Narrabeen Group.||Illawarra Coal Measures.||Overlies Loddon Sandstone. Is overlain gradationally by Wombarra Claystone.||
2904|Bulli Coal|73304|5|Briefly described|p65, p71-72, p76-77|Changhsingian|Changhsingian|Sydney Basin, southern.|252.60 +/- 0.30 Ma U-Pb CA-TIMS.|Illawarra Coal Measures||||
2904|Bulli Coal|73421|6|Mentioned|p16, p19|Changhsingian|Wuchiapingian|Sydney Basin, southern. Age of 252.60+/-0.30 Ma from Metcalfe et al., (2015), same age also appears with the Bullie Tuff in the Eckersley Formation.|252.60+/-0.30 Ma|Sydney Subgroup||||
2904|Bulli Coal|73472|6|Mentioned|p129|Changhsingian|Changhsingian|Sydney Basin. Age of 252.60-252.31 Ma reported for an unnamed tuff.|252.60-252.31 Ma|||||
2904|Bulli Coal|73625|6|Mentioned|p2|Permian|Permian|Southern coalfield, Sydney Basin.||Illawarra Coal Measures.||||
2911|Bullio Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Bullio pluton Adamellite.||||||
2911|Bullio Granite|68592|5|Briefly described|p1611|||Occurs in the deeply incised Wollondilly River, exposed over several hundreds of metres of relief.||Unit in Arthursleigh Suite.|Intrudes Bindook Group.||Zoned or compositionally varied.|
2911|Bullio Granite|70661|6|Mentioned|p77, p78|||||||||
2926|Bulls Camp Volcanics|22768|6|Mentioned|p178|||||||||
2926|Bulls Camp Volcanics|22857|5|Briefly described|p178, p466 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Gregra Group. Crystal-vitric, leucocratic rhyolitic or latitic tuff. Max. thickness: 360m. Geological Province: Molong Rise.||||||
2926|Bulls Camp Volcanics|23214|3|Fully described|p184|Early Devonian|Late Silurian|Of Grega Group.  Previously named Bulls Camp Rhyolite. Age: 412+/-3 Ma (SHRIMP U-Pb).||||Conformably overlain by Cuga Burga Volcanics. Conformably overlies Wallace Shale.||07-SEP-18
2926|Bulls Camp Volcanics|24249|5|Briefly described|p93|||Underlying Unit: Wallace Shale||||||
2926|Bulls Camp Volcanics|30597|6|Mentioned|p29|||Gedinnian age||||||
2926|Bulls Camp Volcanics|31161|5|Briefly described|PA4|||||||||
2926|Bulls Camp Volcanics|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
2926|Bulls Camp Volcanics|33006|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian - Lower Devonian||||||
2926|Bulls Camp Volcanics|33116|5|Briefly described|Fig.12|||Correlation||||||
2926|Bulls Camp Volcanics|33121|5|Briefly described|p85|||Sil.-Dev. Correlation Table.||||||
2926|Bulls Camp Volcanics|33282|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian - Lower Devonian||||||
2926|Bulls Camp Volcanics|33285|6|Mentioned|p18|||||||||
2926|Bulls Camp Volcanics|33326|6|Mentioned|p443|||Fauna.||||||
2926|Bulls Camp Volcanics|33732|5|Briefly described|Table II|||See also P115||||||
2926|Bulls Camp Volcanics|34403|4|Described|p138|||||||||
2926|Bulls Camp Volcanics|34404|6|Mentioned|Fig.3.3a|||||||||
2926|Bulls Camp Volcanics|34405|6|Mentioned|Fig.3.9|||||||||
2926|Bulls Camp Volcanics|34406|6|Mentioned|p222|||||||||
2926|Bulls Camp Volcanics|35246|6|Mentioned|p169|||On a table.||||||
2926|Bulls Camp Volcanics|37727|4|Described|p41|||See also P34.||||||
2926|Bulls Camp Volcanics|39331|6|Mentioned|p64|||See also P87||||||
2926|Bulls Camp Volcanics|39663|6|Mentioned|Table 1|||||||||
2926|Bulls Camp Volcanics|40328|6|Mentioned|p144|||||||||
2926|Bulls Camp Volcanics|40882|6|Mentioned|p24|||Mention Fig.1||||||
2926|Bulls Camp Volcanics|42726|5|Briefly described|map legend|||||||||
2926|Bulls Camp Volcanics|43461|14|Not recorded|table p621||Gedinnian|||||||
2926|Bulls Camp Volcanics|43515|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Provisional Edition)||||||
2926|Bulls Camp Volcanics|43516|14|Not recorded|Map Legend||Early Devonian|||||||
2926|Bulls Camp Volcanics|43640|5|Briefly described|Map Legend||Devonian|||||||
2926|Bulls Camp Volcanics|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Gregra Group.||||||
2926|Bulls Camp Volcanics|63287|5|Briefly described|p317 Fig. 2, p321 Fig. 4|Lochkovian|Lochkovian|Geological Province: Molong Volcanic Belt. Consists of rhyolitic tuff, volcaniclastic conglomerate and greywacke.||||||18-MAY-16
2926|Bulls Camp Volcanics|64994|5|Briefly described|p10|Lochkovian|Lochkovian|Geological province: Lachlan Orogen.||||||07-FEB-11
2926|Bulls Camp Volcanics|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Grega Group||||
2926|Bulls Camp Volcanics|73299|6|Mentioned|p1104 Fig.10|Early Devonian|Early Devonian|Molong High. Underlies the Lambian unconformity in Fig.10 cross-section.||||Overlies the Wallace Shale, underlies the Paling Yard Formation.||
2937|Bumberra Formation|22472|6|Mentioned|p47 Fig.6(e)|||of the Mt. Knowles Group||||||
2937|Bumberra Formation|22529|6|Mentioned|4 fig 2|Late Devonian|Late Devonian|Parent Mount Knowles Group. Overlying unit Lawsons Creek Shale, Underlying unit Buckaroo Conglomerate||||||
2937|Bumberra Formation|22857|5|Briefly described|p492 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Mount Knowles Group. Quartz and sublithic arenite. Max. thickness: 400m. Geological Province: Lambie Shelf.||||||
2937|Bumberra Formation|23043|5|Briefly described|Map Legend|Famennian|Famennian|of Mount Knowles Group.||||||
2937|Bumberra Formation|23170|2|Defined|p241|Famennian|Late Devonian|of Mount Knowles Group.||||||
2937|Bumberra Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
2937|Bumberra Formation|32485|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2937|Bumberra Formation|39214|6|Mentioned|p29|||||||||
2937|Bumberra Formation|42310|5|Briefly described|p209|||||||||
2937|Bumberra Formation|42379|5|Briefly described|p209|||||||||
2937|Bumberra Formation|43043|4|Described|p99|||late Devonian age.||||||
2937|Bumberra Formation|43188|4|Described|p219||Late Devonian|?Famennian. Of Lambie Group.||||||
2937|Bumberra Formation|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
2937|Bumberra Formation|44093|5|Briefly described|p50|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
2937|Bumberra Formation|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4|Late Devonian|Late Devonian|Capertree High. Locations in text include p1100 Fig.5.||Mount Knowles Group||Overlies the Buckaroo Conglomerate, underlies the Lawsons Creek Shale.|Sandstone.|
2939|Bumberry Formation|22638|4|Described|p72|||Of the Nangar Subgroup.Conformably overlain by the Koorawatha Formation.||||||25-JUN-08
2939|Bumberry Formation|22857|5|Briefly described|p488 App.1 Tb.A1.7|Devonian|Devonian|Of the Hervey Group. Max. thickness: 425m. Geological Province: Hervey Basin. See also p490 App.1 Tb.A1.7.||||||
2939|Bumberry Formation|23214|3|Fully described|p231|Late Devonian|Late Devonian|Of Hervey Group. Geological Province: Hervey Basin. 770m thick at type section. Overlain by Cookamidgera Formation, underlain by Pipe Formation.||||||25-JUN-08
2939|Bumberry Formation|23217|4|Described|p1-2, p14-7|Famennian|Famennian|(Conolly, 1965a). Of the Hervey Group. Geological Province: Parkes Syncline.||||||15-JUL-08
2939|Bumberry Formation|23392|2|Defined|p34|||Superseded by Weddin Formation in part nth side of Lachlan River onto Parkes sheet. Large fish fossil Assemblage. Of the Hervey Group. Geological Province: Lachlan Fold Belt. Max Thickness: 707m||||||
2939|Bumberry Formation|24417|3|Fully described|p137|Famennian|Famennian|Of Hervey Group. Overlain by Eurow Formation; underlain by Mount Cole Formation. Max. thickness: 700m.||||||15-JUL-08
2939|Bumberry Formation|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2939|Bumberry Formation|29989|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2939|Bumberry Formation|30071|6|Mentioned|Fig.3|||||||||
2939|Bumberry Formation|30731|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2939|Bumberry Formation|32483|4|Described|p35|||U.Dev. Table 1||||||
2939|Bumberry Formation|32865|6|Mentioned|p484|||Fauna||||||
2939|Bumberry Formation|33006|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2939|Bumberry Formation|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
2939|Bumberry Formation|33833|6|Mentioned|Fig.1|||||||||
2939|Bumberry Formation|35608|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
2939|Bumberry Formation|43499|14|Not recorded|Map Legend|||(Provisional Edition) Part of Nangar Sub-Group||||||
2939|Bumberry Formation|43507|2|Defined|p128-130,146-156,165||Late Devonian|Introduces the formation of Nangar Subgroup (Hervey Group).||||||25-JUN-08
2939|Bumberry Formation|43508|14|Not recorded|p122,127-132|||Undulatory quartz||||||
2939|Bumberry Formation|43509|14|Not recorded|p113,117-8,Pl.II|||||||||
2939|Bumberry Formation|43510|2|Defined|p41-2,52,54-5,57-8,|||p60-67.||||||25-JUN-08
2939|Bumberry Formation|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
2939|Bumberry Formation|43516|14|Not recorded|Map Legend||Late Devonian|||||||
2939|Bumberry Formation|43640|5|Briefly described|Map Legend||Devonian|||||||
2939|Bumberry Formation|43642|5|Briefly described|Map Legend|Devonian|Devonian|Of Hervey Group. Consists of massive white sandstone fining up to red siltstone and shale.||||||15-JUL-08
2939|Bumberry Formation|43782|5|Briefly described|Map Legend|Famennian|Famennian|of Hervey Group.||||||
2939|Bumberry Formation|44192|5|Briefly described|Map Legend||Frasnian|||||||
2939|Bumberry Formation|44936|5|Briefly described|Map Legend||Late Devonian|Of Hervey Group.||||||
2939|Bumberry Formation|50231|5|Briefly described|Map Legend|Famennian|Famennian|Of the Nangar Subgroup (Hervey Group). Overlies: Mandagery Formation. Underlies: Koorawatha Formation.||||||15-JUL-08
2939|Bumberry Formation|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hervey Group.  Massive white sandstone fining to red siltstone and shale.||||||05-JUL-04
2939|Bumberry Formation|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Hervey Group. Underlies: Eurow Formation.  Overlies: Mount Cole Formation.||||||23-DEC-09
2939|Bumberry Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Nangar Subgroup (Hervey Group). Repeated upward-fining cycles of white, thick-bedded, massive to planar-laminated, or x-bedded, moderately sorted, med.-gr., quartzose to lithic-quartz sst intervals passing upwards to red, thinly bedded sst+siltstone.||||||09-SEP-08
2939|Bumberry Formation|68592|3|Fully described|p1698-9, p1713-7|Famennian|Famennian|Conolly (1965), after village of Bumberry. Type section and representative exposures described. 170-330m thick. Geophysical properties briefly described. No fossils in the Goulburn 250 area yet found, but there is a diverse fish and plant assemblage in the Forbes sheet area; age is early to late Famennian.||||Conformably overlies Mandagery Formation. Is overlain conformably by Koorawatha Formation. Equivalent to Hunter and Mount Cole Formations.|Repeated upward-fining cycles of thick-bedded, white, massive to planar-laminated or cross-bedded, medium-grained quartzose to quartz-lithic sandstone packets passing up to red, thinly-bedded, fine-grained sandstone and siltstone.|
2939|Bumberry Formation|70192|5|Briefly described|Map Legend|Famennian|Famennian|Dhb. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hervey Group||Overlies Mandagery Formation. Is overlain by Koorawatha Formation.|Upward fining cycles of thick bedded, massive-planar laminated or cross bedded, medium grained quartzose to lithic quartz sandstone passing up to bedded, planar and ripple cross laminated fine grained sandstone and siltstone.|
2939|Bumberry Formation|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|||Hervey Group||||
2939|Bumberry Formation|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Hervey Group|||Upward fining cycles of thick bedded, massive-planar laminated or cross bedded, medium grained quartzose to lithic quartz sandstone passing up to bedded, planar and ripple cross laminated fine grained sandstone and siltstone.|
2939|Bumberry Formation|71656|6|Mentioned|p12 Fig.2|Famennian|Famennian|Shown only in correlation chart (Fig.2).||Hervey Group||Overlies Mandagery Formation, underlies Koorawatha Formation.||
2947|Bumbolee Creek Formation|22638|6|Mentioned|p9|||||||||
2947|Bumbolee Creek Formation|22687|6|Mentioned|110|Early Silurian|Ordovician|Geol Province Lachlan Fold Belt||||||
2947|Bumbolee Creek Formation|22768|5|Briefly described|p173-74|Early Silurian|Late Ordovician|||||||
2947|Bumbolee Creek Formation|22857|4|Described|p173, p452 App.1, Tb.A1.6|Silurian||Age: 428Ma (U/Pb SHRIMP zircon). Major controversy has arisen in dating and interpretation of rocks of the Tumut Trough which include this unit and Jackalass Slate (see p173-174).||||||
2947|Bumbolee Creek Formation|24266|6|Mentioned|p1482|||Geological Province: Lachlan Fold Belt. Underlying unit: Jackalass Slate.||||||
2947|Bumbolee Creek Formation|37529|5|Briefly described|p8|||See also P7||||||
2947|Bumbolee Creek Formation|39319|6|Mentioned|p357|||||||||
2947|Bumbolee Creek Formation|42045|6|Mentioned|Fig.2 P148|||||||||
2947|Bumbolee Creek Formation|42313|4|Described|p104|Middle Silurian||||||||
2947|Bumbolee Creek Formation|42314|5|Briefly described|Map|Middle Silurian||||||||
2947|Bumbolee Creek Formation|42497|5|Briefly described|Map legend|Ludlovian|Wenlockian|||||||
2947|Bumbolee Creek Formation|44092|5|Briefly described|map legend|Early Silurian|Early Silurian|Smf1||||||
2947|Bumbolee Creek Formation|60078|6|Mentioned|Map Legend|Late Silurian|Early Silurian|||||||
2947|Bumbolee Creek Formation|60280|5|Briefly described|p1-2|Early Silurian|Early Silurian|Together with the Jackalass Slate is equivalent to the Brawlin Formation in the Tumut area.||||||12-AUG-04
2947|Bumbolee Creek Formation|63290|6|Mentioned|p403 Fig. 6(c)|Early Silurian|Middle Ordovician|Geological Province: Tumut Block.||||||
2947|Bumbolee Creek Formation|66197|5|Briefly described|p629, p631 Fig.3a|Early Silurian|Late Ordovician|Tumut Trough. Deep marine quartz and lithic turbidites. Underlies the Blowering Formation, overlies the Jackalass Slate or Gooandra Volcanics.||||||13-MAR-12
2963|Bundamba Group|12597|5|Briefly described|p491, p492 Tb.1, p493 Fig.2|Bathonian|Rhaetian|Clarence-Moreton Basin.|||Includes Marbung and Woogaroo Subgroups and Laytons Range Conglomerate.|||
2963|Bundamba Group|13516|5|Briefly described|p159 fig 8, p163, p166, p168, p164|Early Jurassic|Late Triassic|From Clarence-Moreton Basin.|||Includes Woogaroo Subgroup, Marburg Subgroup|||
2963|Bundamba Group|22857|5|Briefly described|p281, p284, p296-7 Tb.22.1|Early Jurassic|Late Triassic|Comprises two subgroups: the Woogaroo Subgroup and the Marburg Subgroup. Geological Province: Surat and Clarence-Moreton Basins. See also p548 App.1 Tb.A1.12.||||||
2963|Bundamba Group|22861|5|Briefly described|p281,284|Jurassic|Late Triassic|||||||
2963|Bundamba Group|22865|4|Described|p314,Table22.1p296-7|Middle Jurassic||Comprises of: Woogaroo and Marburg Subgroups.||||||
2963|Bundamba Group|22892|5|Briefly described|p7 fig6|Jurassic|Jurassic|||||||
2963|Bundamba Group|22991|5|Briefly described|p324|Jurassic|Triassic|||||||
2963|Bundamba Group|23720|5|Briefly described|Map Legend|Middle Jurassic|Late Triassic|Polymictic and quartz conglomerate, quartz and quartz-lithic sandstone, fossil wood, sitlstone, claystone, minor coal.||||||15-DEC-04
2963|Bundamba Group|23799|3|Fully described|p46|Late Triassic|Middle Triassic|Formerly Ipswich and Walloon Beds (lower and upper coal measures) of Cameron (1905,1907) separated by unproductive sandstone,  Bundamba Beds or Grits.  Now redefined to include the Woogaroo Subgroup/Marburg Fm.  Geol. Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
2963|Bundamba Group|23811|5|Briefly described|Map Legend|||Includes the Marburg and Woogaroo Subgroups. Geological Province: Clarence-Moreton Basin.||||||11-JAN-10
2963|Bundamba Group|23812|5|Briefly described|p35, p33 Fig.6|Early Jurassic|Late Triassic|Overlying unit: Walloon Coal Measures.  Geological  Province: Clarence-Moreton Basin.  Comprised of Marburg and Woogaroo Subgroups.||||||
2963|Bundamba Group|23843|4|Described|p455|Jurassic|Late Triassic|Geological Province: Moreton Basin.||||||
2963|Bundamba Group|23888|6|Mentioned|p262|||||||||
2963|Bundamba Group|24068|5|Briefly described|p270 Table 2|||Geological Province: Moreton Basin.||||||
2963|Bundamba Group|24081|6|Mentioned|p451|||Geological Province: Moreton Basin.||||||
2963|Bundamba Group|24127|5|Briefly described|p5|Jurassic|Triassic|||||||
2963|Bundamba Group|24129|5|Briefly described|p5|Jurassic|Triassic|||||||24-JAN-05
2963|Bundamba Group|24237|6|Mentioned|p6|||||||||
2963|Bundamba Group|24299|5|Briefly described|p3|Jurassic|Triassic|||||||
2963|Bundamba Group|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|||||||
2963|Bundamba Group|29385|6|Mentioned|p80|||Incl.Marburg Ss,Ripley Road Ss,Raceview Fm & Aberdare Cngl.See P81,82.||||||
2963|Bundamba Group|29386|6|Mentioned|p454|||||||||
2963|Bundamba Group|29420|6|Mentioned|p98|||||||||
2963|Bundamba Group|29591|6|Mentioned|p85|||||||||
2963|Bundamba Group|29720|6|Mentioned|p79|||||||||
2963|Bundamba Group|29869|6|Mentioned|p33|||||||||
2963|Bundamba Group|29995|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
2963|Bundamba Group|30058|6|Mentioned|p3|||||||||
2963|Bundamba Group|30086|5|Briefly described|p4|||Triassic||||||
2963|Bundamba Group|30087|6|Mentioned|p3|||See also P4. Consists of Raceview Formation, Aberdare Conglomerate.||||||
2963|Bundamba Group|30131|6|Mentioned|p9|||||||||
2963|Bundamba Group|30302|6|Mentioned|p416|||Upper Jurassic to Middle Jurassic age.See also P414,415||||||
2963|Bundamba Group|30303|6|Mentioned|p322|||Unconformable on Crow's Nest Granite||||||
2963|Bundamba Group|30455|6|Mentioned|p5|||See also P12,17,21||||||
2963|Bundamba Group|30457|6|Mentioned|p96|||||||||
2963|Bundamba Group|30458|6|Mentioned|p1|||See also P19||||||
2963|Bundamba Group|30459|6|Mentioned|p309|||||||||
2963|Bundamba Group|30460|6|Mentioned|p5|||Upper Triassic age. See also P12,13,14,20,22,26||||||
2963|Bundamba Group|30463|6|Mentioned|p464|||Jurassic-Triassic||||||
2963|Bundamba Group|30464|6|Mentioned|Fig.1|||Jurassic-Triassic, see also P1||||||
2963|Bundamba Group|30465|6|Mentioned|p3|||||||||
2963|Bundamba Group|30466|6|Mentioned|Fig.1|||||||||
2963|Bundamba Group|30470|6|Mentioned|p457|||||||||
2963|Bundamba Group|30471|6|Mentioned|p129|||||||||
2963|Bundamba Group|30474|6|Mentioned|p247|||Microfloras||||||
2963|Bundamba Group|30475|5|Briefly described|p162|||Palynology||||||
2963|Bundamba Group|30477|6|Mentioned|p461|||||||||
2963|Bundamba Group|30478|6|Mentioned|p272|||||||||
2963|Bundamba Group|30508|6|Mentioned|p91|||Stratigraphy.||||||
2963|Bundamba Group|30517|6|Mentioned|p436|||||||||
2963|Bundamba Group|30565|6|Mentioned|p129|||||||||
2963|Bundamba Group|30655|6|Mentioned|p20|||||||||
2963|Bundamba Group|30687|5|Briefly described|p63|||See also P64,65,76,77. Lower Jurassic age||||||
2963|Bundamba Group|30785|6|Mentioned|p397|||||||||
2963|Bundamba Group|30914|6|Mentioned|Map legend|Jurassic|Triassic|Triassic to Jurassic||||||
2963|Bundamba Group|30915|6|Mentioned|p97|||||||||
2963|Bundamba Group|30916|6|Mentioned|p97|||||||||
2963|Bundamba Group|31118|4|Described|p311|||||||||
2963|Bundamba Group|31276|6|Mentioned|p151|||Correlation. Palynology||||||
2963|Bundamba Group|31450|6|Mentioned|p47|||||||||
2963|Bundamba Group|31811|6|Mentioned|Fig. 1|||||||||
2963|Bundamba Group|32136|6|Mentioned|p1|||Refers de Jersey (1971)||||||
2963|Bundamba Group|32176|6|Mentioned|p2|||See also P3||||||
2963|Bundamba Group|32179|6|Mentioned|p3|||Trias.||||||
2963|Bundamba Group|32180|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|32491|5|Briefly described|p19|||L.Jur.-U.Trias.||||||
2963|Bundamba Group|32492|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
2963|Bundamba Group|32801|6|Mentioned|Fig.9|||||||||
2963|Bundamba Group|32803|6|Mentioned|p94|||||||||
2963|Bundamba Group|32912|6|Mentioned|p157|||U.Trias.-L.Jurassic||||||
2963|Bundamba Group|32916|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
2963|Bundamba Group|33436|6|Mentioned|p233|||Jurassic||||||
2963|Bundamba Group|33476|6|Mentioned|Fig.10|||||||||
2963|Bundamba Group|33709|6|Mentioned|p104|||||||||
2963|Bundamba Group|33769|6|Mentioned|p150|||||||||
2963|Bundamba Group|33881|6|Mentioned|p96|||||||||
2963|Bundamba Group|34010|6|Mentioned|Cor. chart|||Upper Triassic||||||
2963|Bundamba Group|34134|6|Mentioned|p482|||Lower Jurassic||||||
2963|Bundamba Group|34254|6|Mentioned|p490|||||||||
2963|Bundamba Group|34261|14|Not recorded|Table p.100|||||||||
2963|Bundamba Group|34287|6|Mentioned|p158|||See also P171. Triassic||||||
2963|Bundamba Group|34340|3|Fully described|p465|||||||||
2963|Bundamba Group|34354|6|Mentioned|p3|||Triassic. See also P12.||||||
2963|Bundamba Group|34400|5|Briefly described|p13|||||||||
2963|Bundamba Group|34452|6|Mentioned|p6|||U.Triassic||||||
2963|Bundamba Group|34505|6|Mentioned|p1|||Upper Triassic. See also P3.||||||
2963|Bundamba Group|34755|6|Mentioned|Map legend|Jurassic|Triassic|||||||
2963|Bundamba Group|35007|6|Mentioned|p75|||||||||
2963|Bundamba Group|35063|6|Mentioned|p80|||||||||
2963|Bundamba Group|35079|6|Mentioned|p424|||||||||
2963|Bundamba Group|35101|3|Fully described|p51|||||||||
2963|Bundamba Group|35126|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
2963|Bundamba Group|35156|4|Described|p6|||See also Table.2||||||
2963|Bundamba Group|35188|6|Mentioned|p465|||||||||
2963|Bundamba Group|35428|6|Mentioned|p125|||Biostratigraphy||||||
2963|Bundamba Group|35648|6|Mentioned|p14|||||||||
2963|Bundamba Group|35937|6|Mentioned|Fig.4|||||||||
2963|Bundamba Group|36243|6|Mentioned|p74|||||||||
2963|Bundamba Group|36351|6|Mentioned|p373|||||||||
2963|Bundamba Group|36354|6|Mentioned|p366|||||||||
2963|Bundamba Group|36440|6|Mentioned|Map legend|Early Jurassic|Late Triassic|||||||
2963|Bundamba Group|36745|6|Mentioned|p71|||||||||
2963|Bundamba Group|36779|4|Described|p7|||||||||
2963|Bundamba Group|36825|6|Mentioned|p12|||||||||
2963|Bundamba Group|36899|6|Mentioned|p1095|||||||||
2963|Bundamba Group|36914|6|Mentioned|Fig.5|||||||||
2963|Bundamba Group|36954|6|Mentioned|p114|||||||||
2963|Bundamba Group|36961|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|37111|5|Briefly described|p292|||||||||
2963|Bundamba Group|37112|6|Mentioned|p298|||||||||
2963|Bundamba Group|37122|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|37252|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
2963|Bundamba Group|37287|6|Mentioned|p36|||Mistakenly entered as in South Australia [CEBNov97]||||||
2963|Bundamba Group|37375|6|Mentioned|Fig.1|||||||||
2963|Bundamba Group|37616|6|Mentioned|p31|||||||||
2963|Bundamba Group|37812|6|Mentioned|p657|||||||||
2963|Bundamba Group|38064|5|Briefly described|p41|||||||||
2963|Bundamba Group|38074|5|Briefly described|Table 1|||||||||
2963|Bundamba Group|38076|6|Mentioned|Table 3|||||||||
2963|Bundamba Group|38306|6|Mentioned|p509|||||||||
2963|Bundamba Group|38307|6|Mentioned|p521|||||||||
2963|Bundamba Group|38358|6|Mentioned|p3|||||||||
2963|Bundamba Group|38441|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
2963|Bundamba Group|39079|5|Briefly described|p10|||||||||
2963|Bundamba Group|39445|6|Mentioned|Table 10|||||||||
2963|Bundamba Group|39494|6|Mentioned|Fig.5|||||||||
2963|Bundamba Group|39813|6|Mentioned|Map legend|Jurassic|Triassic|Triassic or Jurassic||||||
2963|Bundamba Group|39907|6|Mentioned|p5|||||||||
2963|Bundamba Group|40030|6|Mentioned|Fig.5|||||||||
2963|Bundamba Group|40051|6|Mentioned|p9|||||||||
2963|Bundamba Group|40245|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|40434|6|Mentioned|p25|||||||||
2963|Bundamba Group|40486|6|Mentioned|p84|||||||||
2963|Bundamba Group|40544|6|Mentioned|Fig.6|||||||||
2963|Bundamba Group|40579|6|Mentioned|Map legend|Early Jurassic|late Rhaetian|||||||
2963|Bundamba Group|40623|5|Briefly described|p36|||Mention Table 2||||||
2963|Bundamba Group|40896|6|Mentioned|p17|||||||||
2963|Bundamba Group|41099|6|Mentioned|Fig.9|||||||||
2963|Bundamba Group|41175|6|Mentioned|p195|||||||||
2963|Bundamba Group|41247|6|Mentioned|Fig.7|||||||||
2963|Bundamba Group|41535|6|Mentioned|Fig.2|||||||||
2963|Bundamba Group|41591|6|Mentioned|Fig.2|||||||||
2963|Bundamba Group|41631|5|Briefly described|p6|||||||||
2963|Bundamba Group|41906|5|Briefly described|p22|||||||||
2963|Bundamba Group|42248|5|Briefly described|p397|||See also Fig.2||||||
2963|Bundamba Group|42316|6|Mentioned|p7|||||||||
2963|Bundamba Group|42336|6|Mentioned|p4|||||||||
2963|Bundamba Group|42405|6|Mentioned|Table 3 P.7|||||||||
2963|Bundamba Group|42463|6|Mentioned|Fig.3 P170|||||||||
2963|Bundamba Group|42493|6|Mentioned|p20|||Moreton Basin||||||
2963|Bundamba Group|42525|5|Briefly described|Map legend|Middle Jurassic|Late Triassic|Includes the Woogaroo Sub-Group.||||||15-JUL-04
2963|Bundamba Group|42719|6|Mentioned|p15|||||||||
2963|Bundamba Group|42893|5|Briefly described|Fig.2 P7|||||||||
2963|Bundamba Group|42951|5|Briefly described|Fig.11|||||||||
2963|Bundamba Group|42987|6|Mentioned|p31|||||||||
2963|Bundamba Group|43001|6|Mentioned|Fig.3,p120|||||||||
2963|Bundamba Group|43072|6|Mentioned|p81|||||||||
2963|Bundamba Group|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Includes the Woogaroo and Marburg Subgroups. Geological Province: Clarence- Moreton Basin.||||||12-APR-05
2963|Bundamba Group|43161|6|Mentioned|36|||||||||
2963|Bundamba Group|43344|14|Not recorded|p13,102,104|Jurassic|Late Triassic|||||||
2963|Bundamba Group|43383|14|Not recorded|p24||Triassic|||||||
2963|Bundamba Group|43384|14|Not recorded|Map Legend|Jurassic|Late Triassic|||||||
2963|Bundamba Group|43404|14|Not recorded|p10|||||||||
2963|Bundamba Group|43453|14|Not recorded|Map Legend|Cretaceous|Triassic|(Provisional Edition)||||||
2963|Bundamba Group|43454|14|Not recorded|Map Legend|Cretaceous|Triassic|||||||
2963|Bundamba Group|43468|14|Not recorded|Map Legend|Jurassic|Triassic|Provisional Edition||||||
2963|Bundamba Group|43878|14|Not recorded|p85,86|||||||||
2963|Bundamba Group|43881|14|Not recorded|p2,6-7,29-38,170|||Incs.Mill Ck Stsn, Layton's Range Clm & Corindi Clm.Tabulam Gp is partial equiv.See also Lexicon.||||||
2963|Bundamba Group|43891|14|Not recorded|p312|||||||||
2963|Bundamba Group|43910|14|Not recorded|p1,2,7,10-1,13,17-20|||Should not be used in Great Artesian Basin. Spores and pollen grains from Bundamba Group. Fig. 2.||||||
2963|Bundamba Group|43911|14|Not recorded|p18|||||||||
2963|Bundamba Group|43918|14|Not recorded|p54,63,75|||||||||
2963|Bundamba Group|43919|14|Not recorded|p39,41|||||||||
2963|Bundamba Group|43920|14|Not recorded|p74,76|||||||||
2963|Bundamba Group|43921|14|Not recorded|p315,323|||||||||
2963|Bundamba Group|43922|14|Not recorded|p325,326|||Now dated as early Upper Triassic (from microflora)||||||
2963|Bundamba Group|43923|6|Mentioned|p1|||||||||
2963|Bundamba Group|43924|14|Not recorded|p2|||||||||
2963|Bundamba Group|43939|14|Not recorded|p106|||||||||
2963|Bundamba Group|43991|4|Described|p47,52||Triassic|Consists of Marburg Formation, Helidon Sandstone,"Swanbank Formation".||||||27-AUG-08
2963|Bundamba Group|43993|14|Not recorded|p95|||Ref. to Wilson 1958,1960.||||||
2963|Bundamba Group|43995|14|Not recorded|p8-63,Fig.3,4,5,9,13||Late Triassic|fig.15||||||
2963|Bundamba Group|43996|14|Not recorded|p88|||||||||
2963|Bundamba Group|43997|14|Not recorded|p113|||"This evidence on the age of the microfloras favours discontinuance of the term "Bundamba" to Jurassic sediments in the Surat Basin"||||||
2963|Bundamba Group|44028|14|Not recorded|Fig.2,p512||Jurassic|See Strat Table.||||||
2963|Bundamba Group|44030|14|Not recorded|p130|||||||||
2963|Bundamba Group|44031|14|Not recorded|Tb.2,p5,11||Early Jurassic|||||||
2963|Bundamba Group|44075|14|Not recorded|p251|||||||||
2963|Bundamba Group|44085|2|Defined|p4,13,16,17|||||||||
2963|Bundamba Group|44095|14|Not recorded|p283-6|||||||||
2963|Bundamba Group|44104|14|Not recorded|p280|||||||||
2963|Bundamba Group|44128|14|Not recorded|Tb.1,p426|||||||||
2963|Bundamba Group|44130|14|Not recorded|p281-283|||||||||
2963|Bundamba Group|44166|14|Not recorded|p14|||||||||
2963|Bundamba Group|44170|14|Not recorded|p20-22|||||||||
2963|Bundamba Group|44239|14|Not recorded|p279|||||||||
2963|Bundamba Group|44269|4|Described|p14-16,76,map||Triassic|||||||
2963|Bundamba Group|44346|14|Not recorded|p5|||||||||
2963|Bundamba Group|44375|14|Not recorded|Fig.45,p312|||||||||
2963|Bundamba Group|44377|14|Not recorded|p22|||||||||
2963|Bundamba Group|44450|4|Described|p28 Table 7|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|44510|2|Defined|p252-257|||Unconformably lies on Ipswich Coal Measures.||||||
2963|Bundamba Group|44542|14|Not recorded|p31|||||||||
2963|Bundamba Group|44554|14|Not recorded|p294-295|||See also Lexicon.||||||
2963|Bundamba Group|44572|14|Not recorded|p235|||||||||
2963|Bundamba Group|44581|14|Not recorded|p346|||||||||
2963|Bundamba Group|44608|14|Not recorded|p19|||||||||
2963|Bundamba Group|44610|14|Not recorded|p49,Tb.1|||||||||
2963|Bundamba Group|44633|14|Not recorded|p2|||||||||
2963|Bundamba Group|44654|14|Not recorded|Map Legend|||||||||
2963|Bundamba Group|44679|14|Not recorded|p272|||Moreton Basin; microflora gives early Upper Triassic age.||||||
2963|Bundamba Group|44680|14|Not recorded|p5|||||||||
2963|Bundamba Group|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
2963|Bundamba Group|44734|14|Not recorded|p5,11-13,19|||Pine Mountain area.||||||
2963|Bundamba Group|44752|14|Not recorded|p297|||||||||
2963|Bundamba Group|44771|14|Not recorded|p2,Fig.1||Triassic|||||||
2963|Bundamba Group|44774|4|Described|p30-32|||Covers whole of sediment interval between Ipswich and Walloon Coal Measures. Consists of basal Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone, which possibly grades up into Marburg Sandstone.||||||
2963|Bundamba Group|44775|4|Described|p7,9,map 2||Late Triassic|Includes Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone.||||||
2963|Bundamba Group|44776|14|Not recorded|p1,3||Late Triassic|||||||
2963|Bundamba Group|44783|14|Not recorded|p16,17,24,43|||||||||
2963|Bundamba Group|44784|14|Not recorded|map 3|||||||||
2963|Bundamba Group|44805|14|Not recorded|p388|||||||||
2963|Bundamba Group|44825|14|Not recorded|p53|||||||||
2963|Bundamba Group|44861|14|Not recorded|p266|||||||||
2963|Bundamba Group|44884|14|Not recorded|p2,3|||||||||
2963|Bundamba Group|44913|14|Not recorded|p53, Fig.1|||||||||
2963|Bundamba Group|45110|6|Mentioned|Table 18|||||||||
2963|Bundamba Group|46984|6|Mentioned|Table 1|||||||||
2963|Bundamba Group|48585|4|Described|p7,8,10,14,15,Pl.1|||||||||
2963|Bundamba Group|48600|14|Not recorded|p6,14|||||||||
2963|Bundamba Group|48626|14|Not recorded|Fig.1|Jurassic|Triassic|||||||
2963|Bundamba Group|48900|6|Mentioned|p50|||||||||
2963|Bundamba Group|48917|6|Mentioned|p1|||Sandstone Leeds,targets or oil wells||||||
2963|Bundamba Group|48928|6|Mentioned|p7|||See also P15||||||
2963|Bundamba Group|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Includes: Woogaroo Subgroup, Marburg Subgroup.||||||
2963|Bundamba Group|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Moreton Basin||||||
2963|Bundamba Group|50631|5|Briefly described|Map Legend|Jurassic|Triassic|Includes: Helidon Sandstone, Marburg Formation.||||||
2963|Bundamba Group|60077|5|Briefly described|Map legend|Middle Jurassic|Late Triassic|Includes: Marburg Formation and Woogaroo Sub-Group.||||||
2963|Bundamba Group|60079|5|Briefly described|Map Legend|Early Jurassic|Late Triassic|Sandstone, siltstone, claystone.||||||
2963|Bundamba Group|60281|5|Briefly described|p25, p28, Fig.18 App 1|Early Jurassic|Late Triassic|Subdivided into the Woogaroo and Marburg Subgroups.  Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|60993|5|Briefly described|p4, p6 Fig. 2|||Originally grouped with the Tabulam Group together with the Marburg Formation. The name now stands independently and is divided into the Marburg and Woogaroo Subgroups. Geol. Prov: Clarence-Moreton Basin. ||||||
2963|Bundamba Group|60995|4|Described|p52, p51 Fig. 3|Early Jurassic|Late Triassic|Now divided into the Woogaroo and Marburg Subgroups. Unconformably overlies Ipswich Coal. Mes. at Red Cliff and with Numboida Coal. Mes. at Nymboida; overlain by Walloon Coal. Mes. Geol. Prov: Clarence-Moreton Basin.||||||
2963|Bundamba Group|60996|5|Briefly described|p72, p129|Middle Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin. See also p133 Tb. 3.||||||
2963|Bundamba Group|60997|5|Briefly described|p139 Fig. 1|Callovian|Rhaetian|Comprises Marburg and Woogaroo Subgroups. See also p140 Fig. 2.||||||
2963|Bundamba Group|60999|5|Briefly described|p164|Early Jurassic|Late Triassic|Consists of the Woogaroo and Marburg Subgroups. Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|61000|5|Briefly described|p181|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|61002|5|Briefly described|p198 Fig 2|||Geological Province: Clarence-Moreton Basin.||||||
2963|Bundamba Group|61004|5|Briefly described|p232 Fig. 2|Jurassic|Triassic|Includes the lower Woogaroo and upper Marburg Subgroups. ||||||
2963|Bundamba Group|61310|4|Described|p20, p14 Fig. C5|Jurassic|Late Triassic|Mainly conglomerate and sandstone with mudstone, siltstone and minor coal, in a thick, non-marine, fluvial to lacustrine sequence. Overlies Nymboida Coal Measures and Chillingham Volcanics; overlain by Marburg Subgroup. Geol. Prov: Clarence-Moreton Basin.||||||27-AUG-08
2963|Bundamba Group|61775|6|Mentioned|p182 Fig. 1||Mesozoic|||||||
2963|Bundamba Group|63748|5|Briefly described|p21|||Comprises Marburg and Woogaroo Subgroups. Overlain by Walloon Coal Measures. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
2963|Bundamba Group|63979|6|Mentioned|p31|||Geological province: Moreton Basin.||||||07-FEB-11
2963|Bundamba Group|64289|5|Briefly described|p6 Fig. 2|Middle Jurassic|Late Triassic|Includes the Marburg and Woogaroo Subgroups. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
2963|Bundamba Group|64665|5|Briefly described|p53 Fig.2, p57, p59.|Middle Jurassic|Late Triassic|Clarence-Moreton and Southern Nambour Basins.|||Includes Woogaroo and Marburg Subgroups.|Unconformably overlies Ipswich Coal Measures. Is overlain by Walloon Coal Measures.||
2963|Bundamba Group|64769|5|Briefly described|p24|Early Jurassic|Late Triassic|Includes Helidon Sandstone. Geological Province: Ipswich Basin. QLD.||||||05-MAY-09
2963|Bundamba Group|64856|6|Mentioned|p80||Norian|Moreton Basin.| | ||||31-JAN-13
2963|Bundamba Group|65003|5|Briefly described|p7|||Of Clarence-Moreton Basin.||||Unconformably overlies the Ipswich Coal Measures. Overlain by Walloon Subgroup.|Mainly conglomerate and sandstone.|30-MAR-12
2963|Bundamba Group|67402|6|Mentioned|p187|||Clarence-Moreton Basin. |||Includes the Woogaroo Subgroup and the Marburg Subgroup|||
2963|Bundamba Group|67669|5|Briefly described|p11|Middle Jurassic|Early Jurassic|Of Bowen Basin.|||Includes Hutton Sandstone, Evergreen Fm and Precipice Sandstone.|Overlain by Injune Creek Group/Waloon Formation. Underlain by Mimosa Group.||
2963|Bundamba Group|68327|5|Briefly described|Map legend.|Jurassic|Triassic||||Includes Woogaroo Sub-Group and Marburg Formation.|||
2963|Bundamba Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Clarence-Moreton Basin. This unit, as well as the Marburg and Woogaroo Subgroups, and Landsborough Sandstone, are all mapped under the symbol, RJb.|||Includes Marburg and Woogaroo Subgroups.|||
2963|Bundamba Group|68579|6|Mentioned|p221|||||||Overlain unconformably by Redbank Plains Formation.||26-APR-13
2963|Bundamba Group|68679|5|Briefly described|p395, p398||||||Woogaroo Subgroup.|Unconformably overlies Ipswich Coal Measures.||
2963|Bundamba Group|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Upper Triassic|Clarence-Moreton Basin. In excess of 1000m thick. Gas or oil mature in the Clarence-Moreton Basin, but with low total organic content. |||Includes the Woogaroo Subgroup and the Mauburg Subgroup.|Overlies the Ipswich Coal Measures. Overlain by the Walloon Coal Measures.||
2963|Bundamba Group|69594|5|Briefly described|p519, p544, p547|Early Jurassic|Rhaetian|Northern Clarence-Moreton Basin and southern Nambour Basin.|||Woogaroo, Marburg Subgroups.|Unconformably overlies Ipswich Coal Measures. Is overlain by Walloon Coal Measures.||
2963|Bundamba Group|69639|6|Mentioned|p106, p224|Jurassic|Triassic|Clarence-Moreton Basin.|||Includes the Mill Creek Siltstone.|Overlies the Tallawudjah Leucomonzogranite.||
2963|Bundamba Group|69790|5|Briefly described|p1063 Fig.2|Middle Jurassic|Triassic|Northern Clarence-Moreton Basin area.|||Includes Woogaroo and Marburg Subgroups.|||
2963|Bundamba Group|70821|5|Briefly described|p80|||Clarence-Moreton Basin.|||Woogaroo, Marburg Subgroups.|Is overlain by Walloon Coal Measures.||
2963|Bundamba Group|71628|5|Briefly described|p17:68; p19:24|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.||||Partly overlies Tallawudjah Leucosyenogranite. Unconformably overlies Cullens Creek Granodiorite.||
2963|Bundamba Group|71805|5|Briefly described|p76|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.|||Includes the Marburg Subgroup and the Woogaroo Subgroup.|||15-MAY-19
2963|Bundamba Group|72528|5|Briefly described|p90.|Jurassic|Jurassic||||Includes Koreela Conglomerate Member.|||
2963|Bundamba Group|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.|||Marburg Subgroup, Woogaroo Subgroup.|Is overlain by Walloon Coal Measures.||
2992|Bundundah Granite|42726|5|Briefly described|map legend|Carboniferous||54.||||||11-MAY-11
2992|Bundundah Granite|66300|5|Briefly described|p52, pp58-63.|Middle Carboniferous|Middle Carboniferous|Eastern Lachlan Orogen. Magmatic crystallisation age is indistinguishable from that of Touga Granite to the west, establishing Middle Carboniferous plutonism in southern MOSS VALE area; but much younger than previously-linked Tullyangela Granite.|324.4 +/- 3.2 Ma.|||Intrudes Yalwal Volcanics. Is unconformably overlain by Snapper Point Formation.|Porphyritic pink granite.|
2992|Bundundah Granite|70661|3|Fully described|vii, viii, p3, p4, p6, p11, p13, p102|Serpukhovian|Serpukhovian|Named for Bundundah Creek. Previously named Bundundah Porphyritic Microgranite or Bundundah granite. Previously assigned to the Oberon Supersuite however later workers state that this classification system is unclear. Distribution, structure, metamorphism, geochemistry discussed. Exposed as low whalebacks or large boulders and tors. Temporally equivalent to Touga Granite, Wandandian Granite. Sulfide mineralisation occurs throughout this unit which is host to the Silver Dell mine and the Foundation Creek mine. See also p109, p115, p126 fig 10, p128-p131, p245, p247.|324.4 +/- 3.2 Ma (SHRIMP U-Pb)|Oberon Supersuite||Intrudes Adaminaby Group, Yalwal Volcanics, Bellbird Creek Formation, overlain by Shoalhaven Group|Leucocratic quartz and K-feldspar porphyritc fine grained microgranite and coarse-very coarse grained granite. Aplite dykes and miarolitic cavities occur throughout. Xenoliths of microgranite and country rock present.|
2992|Bundundah Granite|71303|5|Briefly described|map legend|Carboniferous|Carboniferous||||||Pink leucocratic, sparsely porphyritic quartz-K-feldspar-biotite granite. Microgranite phase gradational to coarse- to very coarse-grained phase. Aplite dykes common, miarolitic cavities locally, xenoliths uncommon.|
3000|Bunga beds|22815|5|Briefly described|p92-93|||Of the Boyd Volcanic Complex.  An association of slump masses, mass-flow breccias, mass-flow sandstone units and mudstones.||||||16-FEB-05
3000|Bunga beds|22857|5|Briefly described|p212, p215|Frasnian|Givetian|Base of the Boyd Volcanic Complex. Fossil plant fragments of Lepidosigillaria yalwensis are common in the Eden area. Contains fish fossils. ||||||
3000|Bunga beds|22859|5|Briefly described|p212, 215|Frasnian|Givetian|||||||
3000|Bunga beds|23327|4|Described|1009|Devonian|Devonian|||||||
3000|Bunga beds|23456|5|Briefly described|p53|||||||||
3000|Bunga beds|42448|6|Mentioned|p6|||Variation of Bunga Beds, Bunga Siltstone Member.||||||
3000|Bunga beds|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
3000|Bunga beds|63605|5|Briefly described|p992 Fig. 1, p994-997||Eifelian|Of Boyd Volcanic Complex. See also Bunga Beds. Orig. incl: in "Flyschoid facies" of Fergusson et al (1979). Age is questionable - discussed (p996). Thinly bedded dark shale+sandstone; includes detailed description of fossil lycopods, fish and shark remains||||||05-SEP-14
3000|Bunga beds|66499|5|Briefly described|p61, p62 Fig.6, p69|Eifelian|Eifelian|Sedimentary facies within lowest part of the Boyd Volcanic Complex. Includes fish and plant fossils. Misspelt as Bunga Beds p69.||Of Boyd Volcanic Complex||||
3000|Bunga beds|70351|5|Briefly described|p54-56,61|Frasnian|Givetian|Interpreted as the 'flyschoid facies' of 'dark colored shales containing abundant Lepidodendron clarkei' of the Boyd Volcanic Complex by Fergusson et al. (1979). Stratigraphic thickness of coastal exposures: 40-200m (Fergusson et al., 1979; Cas et al., 1990). Exhibits complex folding, faulting and intrusive dykes, where well exposed along the coast. Previous age constraints include Middle Devonian (fish fossils; Young 2007) and Early-Middle Devonian (plant fossils; Hall, 1959; White, 1986, 1988). Plant fossil analysis (Tetraxylopteris in the Bunga Pinch Quarry) yield a probably Middle to early late Devonian age (Givetian to Frasnian) for the Bunga beds.||Unit of Boyd Volcanic Complex.|||Finely-bedded carbonaceous dark shales, with some interbedded silts and sandstones.|
3000|Bunga beds|73181|5|Briefly described|p61-63, p65-66|Eifelian|Eifelian|[Also written as 'Bunga beds']. Interpreted to represent the basal sedimentary unit of the Boyd Volcanic Complex (Fergusson et al., 1979). Found in and around Bunga Pinch Quarry. Contains plant macrofossils. Includes recent Devonian plant discoveries. Upper portion was called ""Flyschoid facies"" by Fergusson et al. (1979). Complexly deformed at some localities; possible overlain by volcanics and are unconformably underlain by folded black shales. Deep-water (non-marine) depositional environment. Contains plant and fish fossils.||Boyd Volcanic Complex||Overlain by Boyd Volcanic Complex.|Includes dark coloured shales containing abundant Lepidodendron clarkei.|
3008|Bungil Formation|730|6|Mentioned|p24.|||Paralic.||||||11-NOV-14
3008|Bungil Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p501|Aptian|Early Cretaceous|N Surat Basin. 100-300m thick.||||Equivalent to Drildool beds.|Labile sandstone, siltsone and mudstone with subordinate sub-labile quartzose sandstone and thin coal seams.|
3008|Bungil Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||||||
3008|Bungil Formation|22757|5|Briefly described|Table6,p11||Early Cretaceous|120 m. Surat Basin.||||||
3008|Bungil Formation|22857|4|Described|p296-7 Tb.22.1, p546 App.1 Tb.A1.12|Early Cretaceous|Early Cretaceous|Of the Blythesdale Group. Fine-grained lithic arenite, siltstone and mudstone. Contains three members in Qld. Max. thickness: <200m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5.||||||
3008|Bungil Formation|22865|4|Described|p314,Table22.1p296-7|Barremian|Valanginian|||||||
3008|Bungil Formation|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|of Surat Basin.||||||
3008|Bungil Formation|23053|6|Mentioned|Fig10p17,27|Aptian|Hauterivian|||||||
3008|Bungil Formation|23056|6|Mentioned|10|||Geol Province Eromanga Basin||||||
3008|Bungil Formation|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Surat Basin.||||||
3008|Bungil Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
3008|Bungil Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 180m.||||||
3008|Bungil Formation|24070|5|Briefly described|p303|Cretaceous|Cretaceous|Geological Province: Coonamble Embayment.||||||
3008|Bungil Formation|24085|5|Briefly described|p42 Tb.2|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
3008|Bungil Formation|24243|5|Briefly described|p23 Fig.3|Cretaceous|Cretaceous|||||||
3008|Bungil Formation|29387|6|Mentioned|Table 5|||||||||
3008|Bungil Formation|29393|6|Mentioned|Table 4|||||||||
3008|Bungil Formation|29591|6|Mentioned|Table 15|||||||||
3008|Bungil Formation|29721|6|Mentioned|p246|||||||||
3008|Bungil Formation|30020|6|Mentioned|p33|||||||||
3008|Bungil Formation|30021|6|Mentioned|p87|||||||||
3008|Bungil Formation|30022|6|Mentioned|p28|||||||||
3008|Bungil Formation|30024|6|Mentioned|p332|||||||||
3008|Bungil Formation|30446|6|Mentioned|p39|||||||||
3008|Bungil Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|30695|4|Described|Table 4|||Lower Cretaceous age||||||
3008|Bungil Formation|30696|4|Described|Table 4|||Lower Cretaceous age||||||
3008|Bungil Formation|30697|6|Mentioned|p34|||Minor aquifer present||||||
3008|Bungil Formation|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|30699|6|Mentioned|p53|||Stratigraphy. Early Cretaceous age||||||
3008|Bungil Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||11-JAN-10
3008|Bungil Formation|30702|6|Mentioned|p52|||See also P48-51,Fig.1,2.||||||
3008|Bungil Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
3008|Bungil Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|31098|5|Briefly described|Table 1|||Lower Cretaceous||||||
3008|Bungil Formation|31116|4|Described|p41|||See also Table 2. Cretaceous||||||
3008|Bungil Formation|31208|6|Mentioned|Table 1|||See also Fig. 5||||||
3008|Bungil Formation|31369|6|Mentioned|Table 4|||Cretaceous||||||
3008|Bungil Formation|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|32797|4|Described|Table 4|||L.Cret.||||||
3008|Bungil Formation|33070|4|Described|Table 2|||L.Cret.||||||
3008|Bungil Formation|33075|6|Mentioned|p451|||||||||
3008|Bungil Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|33090|4|Described|Table 4|||L.Cret.||||||
3008|Bungil Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
3008|Bungil Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|33367|6|Mentioned|p17|||||||||
3008|Bungil Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3008|Bungil Formation|33672|6|Mentioned|p44|||||||||
3008|Bungil Formation|34613|4|Described|Table 4|||||||||
3008|Bungil Formation|35648|6|Mentioned|p18|||||||||
3008|Bungil Formation|35663|6|Mentioned|p130|||||||||
3008|Bungil Formation|35793|6|Mentioned|Fig.3|||||||||
3008|Bungil Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
3008|Bungil Formation|35937|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|36243|6|Mentioned|Table 7A|||||||||
3008|Bungil Formation|36357|6|Mentioned|p77|||||||||
3008|Bungil Formation|36570|4|Described|p50|||See also Fig.9, p60.||||||23-SEP-18
3008|Bungil Formation|36574|6|Mentioned|p602|||||||||
3008|Bungil Formation|36827|6|Mentioned|p83|||||||||
3008|Bungil Formation|37117|5|Briefly described|p313|||||||||
3008|Bungil Formation|37597|6|Mentioned|p77|||||||||
3008|Bungil Formation|37856|6|Mentioned|Table 3|||||||||
3008|Bungil Formation|37994|6|Mentioned|p146|||||||||
3008|Bungil Formation|37995|4|Described|p66|||||||||
3008|Bungil Formation|38373|6|Mentioned|p621|||||||||
3008|Bungil Formation|39211|5|Briefly described|p31|||||||||
3008|Bungil Formation|39212|4|Described|p39|||Excursion site. See also p17.||||||23-SEP-18
3008|Bungil Formation|39215|6|Mentioned|p51|||Spore/pollen record||||||
3008|Bungil Formation|39216|6|Mentioned|p55|||Fauna||||||
3008|Bungil Formation|39218|6|Mentioned|p48|||||||||
3008|Bungil Formation|39315|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|39445|5|Briefly described|Table 10|||||||||
3008|Bungil Formation|39494|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|39943|6|Mentioned|Table 9A|||||||||
3008|Bungil Formation|40030|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|40245|6|Mentioned|Table 2|||||||||
3008|Bungil Formation|40249|6|Mentioned|p38|||||||||
3008|Bungil Formation|40250|6|Mentioned|Fig.1|||||||||
3008|Bungil Formation|40541|3|Fully described|p111|||||||||
3008|Bungil Formation|40544|6|Mentioned|Fig.6|||||||||
3008|Bungil Formation|40666|4|Described|p358|||||||||
3008|Bungil Formation|40675|6|Mentioned|Table 9A|||||||||
3008|Bungil Formation|40767|6|Mentioned|Fig.1|||||||||
3008|Bungil Formation|41057|6|Mentioned|p61|||||||||
3008|Bungil Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
3008|Bungil Formation|41064|6|Mentioned|p60|||||||||
3008|Bungil Formation|41187|6|Mentioned|Fig.2|||||||||
3008|Bungil Formation|41188|6|Mentioned|Fig.3|||||||||
3008|Bungil Formation|41210|5|Briefly described|Fig.3|||||||||
3008|Bungil Formation|41216|6|Mentioned|Fig.18,p299|||||||||
3008|Bungil Formation|41247|6|Mentioned|Fig.7|||||||||
3008|Bungil Formation|41266|6|Mentioned|Fig.3|||||||||
3008|Bungil Formation|41290|6|Mentioned|Fig.5|||||||||
3008|Bungil Formation|41330|6|Mentioned|p24|||||||||
3008|Bungil Formation|41681|6|Mentioned|p23|||||||||
3008|Bungil Formation|41992|4|Described|Fig.2 P183|||||||||
3008|Bungil Formation|42007|5|Briefly described|Fig.2 P182|||||||||
3008|Bungil Formation|42135|6|Mentioned|Fig.6 P357|||||||||
3008|Bungil Formation|42429|5|Briefly described|Fig.3 P155|||||||||
3008|Bungil Formation|42463|6|Mentioned|Fig.5 P172|||See also Fig.6 P173||||||
3008|Bungil Formation|42494|5|Briefly described|Table 1 P24|||Just says 'Bungil' on Table.||||||
3008|Bungil Formation|42634|6|Mentioned|Table 8 P34|||||||||
3008|Bungil Formation|42673|5|Briefly described|Fig.2, P184|||||||||
3008|Bungil Formation|43000|5|Briefly described|p109|||see also Fig.5,p112||||||
3008|Bungil Formation|43002|5|Briefly described|Fig.2,p135|||||||||
3008|Bungil Formation|43564|6|Mentioned|p463|||||||||
3008|Bungil Formation|43582|6|Mentioned|Fig.5,p16||Early Cretaceous|||||||
3008|Bungil Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Blythesdale Group||||||
3008|Bungil Formation|43714|5|Briefly described|p8||Early Cretaceous|||||||
3008|Bungil Formation|45103|6|Mentioned|p5|||||||||
3008|Bungil Formation|45110|3|Fully described|p110|||See also p9 and p24.||||||23-SEP-18
3008|Bungil Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
3008|Bungil Formation|46791|6|Mentioned|p34|||||||||
3008|Bungil Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
3008|Bungil Formation|46984|6|Mentioned|Table 1|||||||||
3008|Bungil Formation|48919|6|Mentioned|p70|||See also P71||||||
3008|Bungil Formation|48920|6|Mentioned|Table 7|||Refers to Exon & Vine (1970)||||||
3008|Bungil Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
3008|Bungil Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
3008|Bungil Formation|61312|6|Mentioned|p71|||Equivalent to the Cadna-owie Formation in the Eromanga Basin. Geological Province: Surat Basin.||||||
3008|Bungil Formation|61313|5|Briefly described|p98 Fig.G10|Cretaceous|Cretaceous|Paralic deposits. Geological Province: Surat Basin.||||||
3008|Bungil Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Blythesdale Group. Labile sandstone, carbonaceous siltstone and mudstone. Overlies Pilliga Sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8, p154 Fig. SU9.||||||07-FEB-11
3008|Bungil Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
3008|Bungil Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||Is overlain by Wallumbilla Formation.||
3008|Bungil Formation|64197|6|Mentioned|p630 Fig.7|Cretaceous|Cretaceous|||||Underlies Wallumbilla Formation; overlies Mooga Sandstone.||
3008|Bungil Formation|64665|6|Mentioned|p53 Fig.2.|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Mooga Sandstone.||
3008|Bungil Formation|64856|3|Fully described|p41, p79, p95, p97-100|Aptian|Valanginian|Exon and Vine (1970); corresponds to the Transition beds of Whitehouse (1955). Included in his Blythesdale Formation by Day (1964). Surat Basin. Datum for the top of the Jurassic. Contains Kingull, Minmi, Nullawurt Sandstone, Members (all of Day, 1964) and Claravale Sandstone Member (Mollan et al., 1972). Conformably overlies Mooga Sandstone, correlates with the Cadna-owie Formation in the Eromanga Basin. Is overlain by the Doncaster Member (Wallumbilla Formation). Age from palynoflora (units APK2, 3, uppermost APK1). Max. thickness 269m. Fine grained lithic sandstone, siltstone, mudstone.| | ||||28-NOV-17
3008|Bungil Formation|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Mooga Sandstone, Surat Basin.||||||
3008|Bungil Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
3008|Bungil Formation|65112|6|Mentioned|p329; Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|135-101 Ma.|||Overlies the Mooga Sandstone, underlies the Doncaster Member of the Wallumbilla Formation.||22-MAR-12
3008|Bungil Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Underlies the Wallumbilla Formation and Doncaster Member, Overlies the Mooga Sandstone.||||||
3008|Bungil Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
3008|Bungil Formation|65116|5|Briefly described|p456, Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies both the Wallumbilla Formation and Doncaster Member, Overlies the Mooga Formation in the Surat Basin.||||||
3008|Bungil Formation|65119|5|Briefly described|Fig 2, Table 1, Fig 6-8, 14, 16-19|Early Cretaceous|Early Cretaceous|Surat Basin. Glauconitic to quartzose sandstone, siltstone and mudstone. Up to 270 m thick. Age: 135-116 Ma. Fission Track age: 108+/-6 Ma.||||||07-MAR-12
3008|Bungil Formation|65384|5|Briefly described|S116, S117, S118|||Probably Aptian. Includes Minmi Member. Of Surat Basin. Incorporates coastal plain and marine shelf depositional environments.||||||
3008|Bungil Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.|||Includes Kingull, Minmi, and Nullawurt Sandstone, Members.|Overlies Mooga Sandstone and Southlands Formation.||
3008|Bungil Formation|66623|6|Mentioned|p251.|||Packham et al. (2001). Surat Basin. Equivalent to the Cadna-owie Formation.||||||
3008|Bungil Formation|66915|5|Briefly described|p5, p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Surat Basin.||||Is overlain by Wallumbilla Formation.|Sandy.|12-JAN-17
3008|Bungil Formation|67133|5|Briefly described|p2, p5, p17, p19-21|Cretaceous|Cretaceous|Surat Basin. Samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (38-46%) and feldspars (over 50%), with plagioclase always dominant. Kaolinite reaches 20%, and the mixed-layer clays are <4% and illite-rich. Deposited by a coastal fluvial system that graded into a shallow marine system.||||Overlies Mooga Sandstone.|Fine-grained lithic sandstones interbedded with siltstones and mudstones, with minor sublabile to quartzose sandstones.|
3008|Bungil Formation|67402|4|Described|p43 tbl HPB1, p146 fig SRT3, p148, p156|Barremian|Tithonian|Surat Basin. Highly prospective for the storage of carbon dioxide. Deposited in fluvial to shallow marine environments. Approximately 195m thick. ||Blythesdale Group||Overlies the Mooga Sandstone. Overlain by the Wallumbilla Formation.|Sandstone, siltstone and mudstone.|
3008|Bungil Formation|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Wallumbilla Formation. Underlain by Mooga Silstone.||
3008|Bungil Formation|68003|5|Briefly described|p52, p56, p57 Fig.3-n.|Early Cretaceous|Early Cretaceous|Surat Basin. Equivalent to part of Keelindi beds.||Unit in Blythesdale Group.||Overlies Mooga Sandstone. Is overlain by Wallumbilla Formation (Rolling Downs Group).||
3008|Bungil Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Fluviatile to paralic, grading to shallow marine in the upper part.||||Overlies Mooga Sandstone. Is overlain by Wallumbilla Formation.|Fine-grained lithic sandstone, siltstone and mudstone with subdominant coarse-grained quartzose sandstone; minor thin coal seams.|
3008|Bungil Formation|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
3008|Bungil Formation|68139|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Mooga Sandstone.||
3008|Bungil Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat and Eromanga Basins. This unit, as well as Orallo and Southlands Formations; Gubberamunda, Hooray, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
3008|Bungil Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Mooga Sandstone. Is overlain by Doncaster Member (Wallumbilla Formation).||
3008|Bungil Formation|68593|5|Briefly described|p3-4, p45, p47|Early Cretaceous|Early Cretaceous|A marine incursion occurred during deposition of this unit. A minor aquifer in the map area.||||Overlies Mooga Sandstone. Is overlain by Rolling Downs Group.|Fine-grained lithic sandstone, siltstone and mudstone with subordinate coarse-grained quartzose sandstone. Thin coal seams in places.|
3008|Bungil Formation|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|Surat Basin. Marine transgressive. Pre-Barremian age. Mis-spelt as Bungill Formation in Fig.2.||||||16-JAN-17
3008|Bungil Formation|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Surat Basin. Lower Cretaceous age. Equivalent to the Cadna-owie Formation.|||||Feldspar-rich sandstones.|
3008|Bungil Formation|69582|6|Mentioned|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Mooga Sandstone. Overlain by the Wallumbilla Formation.||
3008|Bungil Formation|69594|4|Described|p519, p538, p573|Aptian|Valanginian|Exon and Vine (1970). Northern Surat Basin. Includes interbedded sandstones and mudstones along Bungil Creek N of Roma; these were assigned by Whitehouse (1955) to his Transition beds, and Day (1964) had placed them in his Blythesdale Formation. Up to 300m thick. Represents the initial marine transgression into the Surat Basin: fluviatile to paralic to shallow-marine sediments.|||Claravale Sandstone, Kingull, Nullawurt Sandstone, Minmi, Members.|Conformably overlies Mooga Sandstone. Is overlain conformably by the Doncaster Member (Wallumbilla Formation). Laterally equivalent to Cadna-owie Formation, and upper part of Kumbarilla beds.|Lithic sandstones, siltstones and common carbonaceous mudstones, with minor sublabile and quartzose sandstone. Upper parts of the Formation are glauconitic and sporadically fossiliferous.|
3008|Bungil Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
3008|Bungil Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Northern Surat Basin.||||||
3008|Bungil Formation|70036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Surat Basin. The lower part of the Formation is included in a mapped unit of a Late Jurassic to Early Cretaceous meandering stream sequence: quartzose sandstone and conglomerate with minor shale, mudstone and coal. The upper part is included in a mapped unit of a coastal plain sequence: lithic sandstone, siltstone, mudstone and coal.||||||
3008|Bungil Formation|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.|||Kingull, Nullawurt Sandstone, Minmi, Members.|Overlies Mooga Sandstone, Southlands Formation. Is overlain by Wallumbilla Formation (Rolling Downs Group).||
3008|Bungil Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Valanginian-Barremian.||||Overlies Mooga Sandstone. Is overlain by Wallumbilla Formation.||
3008|Bungil Formation|71601|6|Mentioned|p120, p121, p123|Aptian|Aptian|South western Queensland. Includes basal ankylosaurian dinosaur Minmi paravertebra.|||Includes Minmi Member.|||
3008|Bungil Formation|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
3008|Bungil Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW), Coonamble Embayment (NSW). Main confined aquifers, generally producing flowing artesian water bores.|||Kingull, Nullawurt Sandstone, Minmi Members.|Overlies Southlands FZ and Mooga Sandstone. Is overlain by Wallumbilla FZ (Rolling Downs Group).||
3008|Bungil Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88...|||Surat Basin. Partial aquifer. More locations: p. 116-117, 119, 146, 151-152, 160, 168-173, 177-178, 191.||||||
3008|Bungil Formation|73193|6|Mentioned|p369|Barremian|Hauterivian|Surat Basin.||||Underlain by Mooga Sandstone.||
3026|Bungunnia Limestone|10010|5|Briefly described|p12 Fig. 3|Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||13-AUG-07
3026|Bungunnia Limestone|22773|5|Briefly described|Fig24.8p352|Early Pleistocene|Late Pliocene|||||||
3026|Bungunnia Limestone|22799|5|Briefly described|p24 Fig.10|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|22857|5|Briefly described|p352 Fig. 24.8|Pleistocene|Late Pliocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|22887|5|Briefly described|Fig.6 p13||Late Pliocene|||||||
3026|Bungunnia Limestone|22893|5|Briefly described|fig9p27|||||||||
3026|Bungunnia Limestone|23560|6|Mentioned|p152|||||||||
3026|Bungunnia Limestone|23818|5|Briefly described|p212 Fig.108|Middle Pleistocene|Middle Pleistocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|23884|5|Briefly described|p155 Fig. 13.2|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|24176|6|Mentioned|p20|Pleistocene|Pleistocene|Of Firman (1965).||||||
3026|Bungunnia Limestone|24551|5|Briefly described|p338 Fig. 11.2, 340, 609.|Middle Pleistocene|Early Pleistocene|||||||
3026|Bungunnia Limestone|30056|6|Mentioned|Table 2|||||||||
3026|Bungunnia Limestone|30177|6|Mentioned|p106|||Pleistocene age.||||||
3026|Bungunnia Limestone|30750|6|Mentioned|p1|||Pleistocene age||||||
3026|Bungunnia Limestone|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|30753|4|Described|p15|||Middle Pleistocene age||||||
3026|Bungunnia Limestone|30754|2|Defined|Appendix 1|middle Pleistocene|middle Pleistocene|See also P22,31||||||
3026|Bungunnia Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
3026|Bungunnia Limestone|30918|6|Mentioned|p84|||||||||
3026|Bungunnia Limestone|30996|6|Mentioned|p38|||Refers Roberts (1968), Firman (1971)||||||
3026|Bungunnia Limestone|31741|6|Mentioned|p6|||||||||
3026|Bungunnia Limestone|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|31848|6|Mentioned|p12|||Quaternary||||||
3026|Bungunnia Limestone|32426|4|Described|p141|||See also P140||||||
3026|Bungunnia Limestone|32861|5|Briefly described|Table 1|||||||||
3026|Bungunnia Limestone|32862|5|Briefly described|Table 3|||Pleistocene||||||
3026|Bungunnia Limestone|33826|6|Mentioned|p42|||Strat. table||||||
3026|Bungunnia Limestone|34114|4|Described|p50|||Pleistocene||||||
3026|Bungunnia Limestone|34180|6|Mentioned|p212|||Middle Pleistocene.||||||
3026|Bungunnia Limestone|34459|4|Described|p11|||Pleistocene||||||
3026|Bungunnia Limestone|34461|5|Briefly described|p49|||||||||
3026|Bungunnia Limestone|34758|6|Mentioned|Table 1|||||||||
3026|Bungunnia Limestone|34954|6|Mentioned|p199|||||||||
3026|Bungunnia Limestone|35097|6|Mentioned|Fig.4|||||||||
3026|Bungunnia Limestone|35131|6|Mentioned|p8|||||||||
3026|Bungunnia Limestone|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3026|Bungunnia Limestone|35232|6|Mentioned|Table 4|||||||||
3026|Bungunnia Limestone|35272|4|Described|p284|||||||||
3026|Bungunnia Limestone|35274|6|Mentioned|p425|||||||||
3026|Bungunnia Limestone|37873|4|Described|p2|||||||||
3026|Bungunnia Limestone|38068|6|Mentioned|p76|||||||||
3026|Bungunnia Limestone|39329|6|Mentioned|Fig.1|||||||||
3026|Bungunnia Limestone|40380|6|Mentioned|p221|||||||||
3026|Bungunnia Limestone|40820|5|Briefly described|p142|||||||||
3026|Bungunnia Limestone|41848|5|Briefly described|p358|||At top of Blanchetown Clay sequence. Age Pleistocene||||||
3026|Bungunnia Limestone|41868|6|Mentioned|p579|||||||||
3026|Bungunnia Limestone|42125|6|Mentioned|p139|||||||||
3026|Bungunnia Limestone|42130|6|Mentioned|Fig.3 P265|||||||||
3026|Bungunnia Limestone|42134|6|Mentioned|Fig.3 P335|||||||||
3026|Bungunnia Limestone|42137|6|Mentioned|Fig.2 P368|||||||||
3026|Bungunnia Limestone|42592|6|Mentioned|p280|||||||||
3026|Bungunnia Limestone|42635|5|Briefly described|p94|||||||||
3026|Bungunnia Limestone|42717|6|Mentioned|map legend|Pleistocene||||||||
3026|Bungunnia Limestone|42813|6|Mentioned|p25|||||||||
3026|Bungunnia Limestone|42827|5|Briefly described|p359|||see also Table 9.1||||||
3026|Bungunnia Limestone|42881|4|Described|Fig.3, P84|||||||||
3026|Bungunnia Limestone|42966|1|Redefined|Table 34 p209|Early Pleistocene||||||||
3026|Bungunnia Limestone|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Lacustrine dolomitic limestone. Underlain by Blanchetown Clay.||||||
3026|Bungunnia Limestone|43073|5|Briefly described|Table 4|||||||||
3026|Bungunnia Limestone|43258|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
3026|Bungunnia Limestone|43298|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
3026|Bungunnia Limestone|43655|5|Briefly described|p40-846|||||||||
3026|Bungunnia Limestone|43791|6|Mentioned|p372, Fig1|||||||||
3026|Bungunnia Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
3026|Bungunnia Limestone|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Thickness: 3m. At the top of the Chowilla Sand and the Blanchtown Clay. Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|49040|6|Mentioned|Fig.6|||||||||
3026|Bungunnia Limestone|60540|5|Briefly described|p1000 Fig.2,p1000,|Pleistocene|Pleistocene|||||Incised into the underlying Loxton Sand|Dolostone.|
3026|Bungunnia Limestone|60953|5|Briefly described|Map Legend|Pleistocene|Pliocene|Overlies: Blanchetown Clay. Lacustrine dolomitic limestone.||||||
3026|Bungunnia Limestone|61108|5|Briefly described|map legend|Pleistocene|Pliocene|Lacustrine dolomitic limestone. Overlies Blanchetown Clay.||||||01-JUN-05
3026|Bungunnia Limestone|61181|5|Briefly described|p137|Pleistocene|Pleistocene|Lacustrine deposits occur between ridges of Parilla Sand. Dolomitic limestone of this formation is interbedded with clay and sand. In the Mallee region.||||||
3026|Bungunnia Limestone|61207|5|Briefly described|p280 Fig. 2|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Of the Wunghnu Group. Geological Province: Murray Basin.||||||
3026|Bungunnia Limestone|63887|5|Briefly described|p20, p21 Fig. 1|Pleistocene|Late Miocene|Variably dolomitic limestone.||||||
3026|Bungunnia Limestone|64961|5|Briefly described|p259, p269 Fig. 9|Quaternary|Quaternary|Overlies Blanchetown Clay. Geological province: Murray Basin. Thin, lacustrine carbonate unit, restricted in distribution. Indicated by 'BL' in Figure 9. ||||||
3026|Bungunnia Limestone|65552|5|Briefly described|p5 Fig. 3|Quaternary|Quaternary|Limestone of the central and western Murray Basin. Overlies Blanchetown Clay; underlies surface aeolian-fluvio-lacustrine deposits (e.g. Woorinen Formation, Coonambidgal Formation, Molineaux-Lowan Sands).||||||
3026|Bungunnia Limestone|66287|5|Briefly described|Fig 2,4,5|Late Pliocene|Late Pliocene|With the Blanchetown Clay and the Chowilla Sand, part of the Lake Bungunnia sedimentary fill.||||Underlies the Bakara Soil and overlies the Blanchetown Clay.||20-APR-12
3026|Bungunnia Limestone|68548|5|Briefly described|p13, p13 Fig.2|Pleistocene|Pleistocene|Early to Middle Pleistocene age.||||Overlies Blanchetown Clay.|Dolostones.|
3026|Bungunnia Limestone|71248|2|Defined|p1, 2|||||||||
3026|Bungunnia Limestone|72445|6|Mentioned|App.7 p7, p7 Fig.4.|Quaternary|Quaternary|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as overlying and partially equivalent to Blanchetown Clay.|Shown as limestone.|
3026|Bungunnia Limestone|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Lacustrine limestone.|
3026|Bungunnia Limestone|73228|4|Described|p50, p56-57, p59, p62|Pleistocene|Late Pliocene|Murray Basin. Thickness: 1-3 m. Caps the Blanchetown Clay.|||||Interlaminated calcite, dolomite and magnesite, including an abundance of pisolitic and ooid grainstones, as well as ostracod-rich sands.|
3026|Bungunnia Limestone|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
3037|Bunnyong Sandstone Member|22578|6|Mentioned|p398|||of Long Swamp Formation||||||
3037|Bunnyong Sandstone Member|39232|6|Mentioned|Table 2|||||||||
3037|Bunnyong Sandstone Member|40806|6|Mentioned|p154|||See also Fig.2||||||
3037|Bunnyong Sandstone Member|42657|6|Mentioned|Table 1 P74|||||||||
3053|Bunyan Formation|22815|6|Mentioned|p108|Tertiary|Tertiary|||||||
3053|Bunyan Formation|40664|3|Fully described|p233|||||||||
3053|Bunyan Formation|42035|4|Described|p128|||||||||
3053|Bunyan Formation|43126|5|Briefly described|p3||Miocene|||||||
3053|Bunyan Formation|61155|5|Briefly described|p19|Middle Miocene|Middle Miocene|Thickness: 100m. In Southeastern NSW.||||||03-MAR-10
3054|Bunyip Sand|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin.||||||
3054|Bunyip Sand|30750|6|Mentioned|p4|||||||||
3054|Bunyip Sand|30751|6|Mentioned|Map legend|Recent|Recent|||||||
3054|Bunyip Sand|30752|6|Mentioned|Table 1|||||||||
3054|Bunyip Sand|30753|4|Described|p14|||Recent age||||||
3054|Bunyip Sand|30754|2|Defined|Appendix 1|Recent|Recent|See also P22,42. Stratigraphic table||||||
3054|Bunyip Sand|30755|6|Mentioned|p169|||Tectonic map||||||
3054|Bunyip Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
3054|Bunyip Sand|30996|6|Mentioned|p42|||Refers Firman (1966). See also P 48. Time eq. Coonambidgal Fm.||||||
3054|Bunyip Sand|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
3054|Bunyip Sand|32432|6|Mentioned|Fig.2|||See also Table 1||||||
3054|Bunyip Sand|32861|5|Briefly described|Table 1|||Recent||||||
3054|Bunyip Sand|33826|6|Mentioned|p42|||Strat. table||||||
3054|Bunyip Sand|34180|6|Mentioned|p212|||See also P217. Recent.||||||
3054|Bunyip Sand|34459|5|Briefly described|p11|||Recent||||||
3054|Bunyip Sand|34758|6|Mentioned|Fig.2|||||||||
3054|Bunyip Sand|35071|6|Mentioned|Table 1|||||||||
3054|Bunyip Sand|35097|6|Mentioned|Fig.4|||||||||
3054|Bunyip Sand|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3054|Bunyip Sand|35232|6|Mentioned|p14|||||||||
3054|Bunyip Sand|38068|6|Mentioned|Fig.8|||Murray Basin||||||
3054|Bunyip Sand|40226|6|Mentioned|Fig.2|||||||||
3054|Bunyip Sand|42264|6|Mentioned|p11|||||||||
3054|Bunyip Sand|42966|2|Defined|Table 38 p273|Quaternary||||||||
3054|Bunyip Sand|44133|5|Briefly described|p220 Fig. 11.2, 253|Holocene|Middle Pleistocene|Geological Province: Murray Basin. ||||||
3054|Bunyip Sand|49038|4|Described|Table 2|||||||||
3060|Burcher Greywacke|22857|5|Briefly described|p446 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Part of Ootha Formation. Massive quartz greywackes and shales; contains crinoids. Max. thickness: ~4km. ||||||
3060|Burcher Greywacke|24417|3|Fully described|p49|Silurian|Silurian|Includes the Blow Clear Member.  Intruded by Billys Lookout Granite.  Overlies Girilambone Group.||||||
3060|Burcher Greywacke|35503|2|Defined|p206|Silurian|Silurian|New name refs Kemezys (1976)Prob. Silurian||||||
3060|Burcher Greywacke|40328|5|Briefly described|p38|||||||||
3060|Burcher Greywacke|50385|5|Briefly described|Map Legend|Silurian|Silurian|Fine to medium-grained greywacke, silty lenses||||||
3060|Burcher Greywacke|50554|5|Briefly described|Map legend|Silurian|Silurian|Fine to medium-grained greywacke, silty lenses.||||||21-JUN-04
3060|Burcher Greywacke|60008|5|Briefly described|Map Legend|Silurian|Silurian|Sediments.||||||
3060|Burcher Greywacke|60009|5|Briefly described|Map Legend|Wenlock|Llandovery|Includes: Blow Clear Member.||||||23-DEC-09
3060|Burcher Greywacke|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, App A-VI 3.||||||
3060|Burcher Greywacke|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped.|||||Fine- to medium-grained greywacke, silty lenses.|
3066|Burgoon Formation|22857|4|Described|p456 App.1 Tb.1A1.6|Late Silurian|Late Silurian|Of the Goonigal Group. Pyritic, lithic and feldspathic tuffs interbedded with cherts. Max. thickness: 630m. Geological Province: Cowra Trough. ||||||
3066|Burgoon Formation|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|of Goonigal Group.||||||
3066|Burgoon Formation|23170|2|Defined|p112|Pridoli|Pridoli|of Goonigal Group.||||||
3066|Burgoon Formation|23214|3|Fully described|p154|Pridoli|Pridoli|Of Goonigal Group. Includes the Yarran Cherts. Intruded by Gumble Granite. Max. thickness 630m.||||||
3066|Burgoon Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
3066|Burgoon Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
3066|Burgoon Formation|40328|3|Fully described|p105|||||||||
3066|Burgoon Formation|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
3066|Burgoon Formation|43494|4|Described|p22||Pridolian|Shale grading up into chert and then interbedded chert and volcaniclastic (andesitic) sst. Conformable over Jews Creek Volcanics and the Mackeys Creek Shale to the east.; conformably overlain by Wansey Formation to the west. Est. max. thickness: ~400m.||||||16-MAR-06
3066|Burgoon Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
3066|Burgoon Formation|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|of Goonigal Group.||||||
3066|Burgoon Formation|66197|5|Briefly described|p633 Fig.4c|||Cowra Trough-Molong High. Deep marine shale. Underlies the Wansey Formation, overlies the Burrawong Limestone.||||||13-MAR-12
3066|Burgoon Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Goonigal Group|Jews Creek Volcanics|||
3078|Burly Jacky Sandstone Member|22486|6|Mentioned|p 7|||Waugoola Group||||||
3078|Burly Jacky Sandstone Member|23214|4|Described|p110|Wenlock|Llandovery|Coarse, calcareous, quartz feldspathic sandstone facies of Glendalough Formation.||||||
3078|Burly Jacky Sandstone Member|35258|4|Described|p125|||||||||
3078|Burly Jacky Sandstone Member|63290|5|Briefly described|p401 Fig. 5(d)|Llandovery|Llandovery|Of Waugoola Group. Overlain by Chaucer Redbed Member, underlain by Cobblers Creek Limestone.||||||
3078|Burly Jacky Sandstone Member|70684|6|Mentioned|p50 Fig.24|Early Silurian|Early Silurian|Molong Volcanic Belt. ||Glendalough Formation.||||
3097|Burnt Hill Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
3097|Burnt Hill Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Fine grained leucocratic granite.||||||
3097|Burnt Hill Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Whick Whack Suite. Pinkish-grey, fine- to medium-grained, generally massive, equigranular, biotite granite.||||||
3097|Burnt Hill Granite|67820|5|Briefly described|p136-137|||Has higher mineral potential than most granitoids on the Goulburn sheet. Associated with disseminated molybdenite.|||||A-type granite.|
3097|Burnt Hill Granite|68592|3|Fully described|p1482, p1508-14|Early Devonian|Early Devonian|First recognised and named by Gibson (1973); first published by Chappell et al. (1991) (after Yacopetti, 1987) who assigned this unit to their Burnt Hill Suite. Blevin (2011) included it (tentatively) in his Whick Whack Suite. A very small (0.1 km2) pluton. Type locality described. Geochemistry and geophysical properties briefly described. Age from intrusive relationship and parent. No mineral deposits; traces of Mo on some fracture surfaces.||Unit in Whick Whack Suite.||Intrudes Cuddyong Formation.|Pinkish-grey, fine- to medium-grained, generally massive, equigranular biotite granite. A-type. Strongly fractionated.|
3097|Burnt Hill Granite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dwb. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Whick Whack Suite|||Fine-medium grained, generally massive, equigranular biotite granite.|
3097|Burnt Hill Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Whick Whack Suite|||Fine-medium grained, generally massive, equigranular biotite granite.|
3097|Burnt Hill Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.||Burnt Hill Suite.|||Aluminous A-type granite.|
3106|Burra Group|7931|5|Briefly described|p98|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
3106|Burra Group|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Slates, greywackes, quartzites, dolomites and dolomite arenites.||||||11-JAN-10
3106|Burra Group|22510|5|Briefly described|table1 p37|||Age: Willouran- Torrension in age.||||||
3106|Burra Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
3106|Burra Group|22589|6|Mentioned|p129||Neoproterozoic|||||||
3106|Burra Group|22631|6|Mentioned|p177, fig2 p170|Cryogenian|Cryogenian|||||||
3106|Burra Group|22643|5|Briefly described|p183, fig3p187|Cryogenian|Cryogenian|||||||
3106|Burra Group|22677|6|Mentioned|Fig.2 p735||Neoproterozoic|||||||
3106|Burra Group|22725|6|Mentioned|p241|Cambrian|Neoproterozoic|overlies Callana Group||||||
3106|Burra Group|22772|4|Described|p65,Table13.1|Cryogenian|Cryogenian|||||||
3106|Burra Group|22787|6|Mentioned|p42|||||||||
3106|Burra Group|22802|6|Mentioned|p871|||Age: <780Ma||||||
3106|Burra Group|22830|6|Mentioned|P25||Adelaidean|||||||
3106|Burra Group|22857|5|Briefly described|p65, Tb. 13.1 (insert p70-71)|Sturtian|Torrensian|Of the Warrina Supergroup. Divided into 4 subgroups: Belair, Mundallio, River Wakefield, Emeroo Subgroups.||||||
3106|Burra Group|22869|5|Briefly described|P37, Fig2||Neoproterozoic|||||||
3106|Burra Group|22884|6|Mentioned|p40 Fig1|Neoproterozoic|Neoproterozoic|||||||26-MAR-09
3106|Burra Group|22889|4|Described|p30-40|Adelaidean|Adelaidean|New stratigraphic classification and correlation of the Burra Group is proposed.||||||
3106|Burra Group|22901|6|Mentioned|76 fig 2|||Geol province Adelaide Rift Complex||||||
3106|Burra Group|22907|6|Mentioned|41|||Geol province Adelaide Rift Complex||||||
3106|Burra Group|22926|5|Briefly described|37|||Geol. province: Adelaide Geosyncline. Overlain by Umberatana Group.||||||17-JAN-07
3106|Burra Group|22947|6|Mentioned|p16|||Mentioned under - Adelaide Geosyncline Geodevelopments.||||||
3106|Burra Group|22949|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|23023|6|Mentioned|p1797|||||||||
3106|Burra Group|23054|5|Briefly described|p11,33-4|||||||||
3106|Burra Group|23205|6|Mentioned|p133|||of Warrina Supergroup.||||||
3106|Burra Group|23211|6|Mentioned|Fig.1|||||||||
3106|Burra Group|23288|6|Mentioned|p143 Fig.18|||Equivalent of Finke beds. of Adelaide Geosyncline.||||||
3106|Burra Group|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Subdivided into Upper, Middle and Lower Burra Group. Includes Skillogalee Dolomite.||||||07-FEB-07
3106|Burra Group|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|23411|6|Mentioned|Map Legend|||||||||
3106|Burra Group|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|23477|5|Briefly described|p49 Fig 3|Neoproterozoic|Neoproterozoic|Geological Province Curnamona Province.||||||
3106|Burra Group|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex.||||||
3106|Burra Group|23719|4|Described|p24|Neoproterozoic|Adelaidean|See also page 25 table 7. Overlain by Umberatana Group; underlain by Callana Group. Geological Province: Gawler Craton.||||||17-JAN-07
3106|Burra Group|23818|4|Described|p34 Fig.8|Adelaidean|Adelaidean|Underlain by Barossa Complex. Geological Province: Willyama Block. Max. thickness: 20 000 ft. Age: oldest member is ~1000 Ma.||||||17-JAN-07
3106|Burra Group|23869|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|23913|5|Briefly described|p110 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: Adelaidean Geosyncline.  Unconformably overlain by Umberatana Group.||||||05-JUL-13
3106|Burra Group|24045|5|Briefly described|p533 Fig.2|Adelaidean|Adelaidean|||||||
3106|Burra Group|24175|3|Fully described|p10|Neoproterozoic|Neoproterozoic|Underlain by Callana Group. Max. thickness: 8470m.||||||20-FEB-07
3106|Burra Group|24176|3|Fully described|p10, p25 Tb. 1|Adelaidean|Adelaidean|Age is Torrensian. Overlies upper Callanna Beds; underlies Umberatana Group. Geological Province: Mount Painter Province.||||||16-SEP-08
3106|Burra Group|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Mundallio and Emeroo Subgroups.||||||
3106|Burra Group|24362|6|Mentioned|p41|||||||||
3106|Burra Group|24364|6|Mentioned|p29 Fig.3|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|24400|5|Briefly described|p155 Tb.2, p156|Adelaidean|Adelaidean|Age: <777+/-7Ma. Includes Boucat Volcanics. Overlies Callana Group, overlain by Umberatana Group.||||||05-FEB-08
3106|Burra Group|24481|5|Briefly described|p829 Fig. 9|||Overlain by the Umberatana Group.||||||
3106|Burra Group|24484|5|Briefly described|p798 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Age: ~780-730 Ma. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
3106|Burra Group|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 2|Adelaidean|Adelaidean|Of the Warrina Supergroup. Includes Skillogalee Dolomite. Geological Province Adelaide Geosyncline.||||||05-JUL-06
3106|Burra Group|24593|5|Briefly described|p612 Fig. 1a|||Geological Province: Mount Painter Inlier.||||||
3106|Burra Group|29656|4|Described|Fig.3|||||||||
3106|Burra Group|29697|6|Mentioned|p7|||||||||
3106|Burra Group|29758|6|Mentioned|p101|||||||||
3106|Burra Group|29763|6|Mentioned|p45|||||||||
3106|Burra Group|29776|6|Mentioned|p82|||||||||
3106|Burra Group|29778|6|Mentioned|p167|||||||||
3106|Burra Group|29780|6|Mentioned|p21|||||||||
3106|Burra Group|29781|6|Mentioned|Fig.5|||||||||
3106|Burra Group|29831|5|Briefly described|p175|||||||||
3106|Burra Group|29835|6|Mentioned|p177|||||||||
3106|Burra Group|29838|6|Mentioned|p4|||||||||
3106|Burra Group|29840|6|Mentioned|Fig.3|||||||||
3106|Burra Group|30028|6|Mentioned|Fig.4|||||||||
3106|Burra Group|30051|6|Mentioned|Fig.1|||Proterozoic age.||||||
3106|Burra Group|30052|6|Mentioned|Fig.5|||See also Fig.6. Proterozoic age.||||||
3106|Burra Group|30090|6|Mentioned|p4|||||||||
3106|Burra Group|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|30177|4|Described|p64|||See also p65-66.||||||17-JAN-07
3106|Burra Group|30190|6|Mentioned|Fig.1|||||||||
3106|Burra Group|30255|5|Briefly described|p213|||Torrensian age. See also Fig.2, p217.||||||17-JAN-07
3106|Burra Group|30713|6|Mentioned|p106|||||||||
3106|Burra Group|30782|6|Mentioned|p70|||Stratigraphy||||||
3106|Burra Group|30798|6|Mentioned|p116|||||||||
3106|Burra Group|30799|6|Mentioned|p2|||Stratigraphy and terminology.||||||
3106|Burra Group|30801|6|Mentioned|p5|||Table p5-6. Torrensian age.||||||10-NOV-16
3106|Burra Group|30802|5|Briefly described|p7|||See also p8 and p13. Torrensian age.||||||17-JAN-07
3106|Burra Group|30807|6|Mentioned|p103|||Suggested map symbol||||||
3106|Burra Group|30808|6|Mentioned|Fig.2|||||||||
3106|Burra Group|30810|6|Mentioned|p2|||||||||
3106|Burra Group|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|31022|6|Mentioned|Fig. 4|||||||||
3106|Burra Group|31109|5|Briefly described|p16|||See also p18. Map. Upper Proterozoic.||||||17-JAN-07
3106|Burra Group|31292|6|Mentioned|p3|||Refers Thomson et al. (1964)||||||
3106|Burra Group|31698|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|31923|5|Briefly described|p8|||||||||
3106|Burra Group|31965|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|31967|6|Mentioned|p.4|||||||||
3106|Burra Group|31971|6|Mentioned|p9|||||||||
3106|Burra Group|32031|6|Mentioned|Fig. 2|||||||||
3106|Burra Group|32032|6|Mentioned|p7|||||||||
3106|Burra Group|32146|6|Mentioned|p349|||Refers Thomson et al. (1964)||||||
3106|Burra Group|32319|6|Mentioned|p109|||Copper mineralization||||||
3106|Burra Group|32322|6|Mentioned|p109|||||||||
3106|Burra Group|32364|6|Mentioned|p17|||See also Fig.2,3||||||
3106|Burra Group|32419|6|Mentioned|p82|||||||||
3106|Burra Group|32424|6|Mentioned|p16|||||||||
3106|Burra Group|32501|6|Mentioned|p1|||Host rocks for fluorite. Also P2||||||
3106|Burra Group|32508|6|Mentioned|p119|||||||||
3106|Burra Group|32510|6|Mentioned|p106|||||||||
3106|Burra Group|32547|4|Described|p60|||Torrensian||||||
3106|Burra Group|32635|5|Briefly described|p5|||||||||
3106|Burra Group|32720|6|Mentioned|p5|||Middle Riphean Correlation. See also P7.||||||
3106|Burra Group|32721|6|Mentioned|p96|||||||||
3106|Burra Group|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
3106|Burra Group|32723|6|Mentioned|p96|||||||||
3106|Burra Group|32724|6|Mentioned|Fig.1|||Correlation||||||
3106|Burra Group|32726|6|Mentioned|p201|||Stromatolites||||||
3106|Burra Group|32727|6|Mentioned|p30|||||||||
3106|Burra Group|32823|6|Mentioned|p361|||||||||
3106|Burra Group|33004|6|Mentioned|p136|||||||||
3106|Burra Group|33033|6|Mentioned|p69|||||||||
3106|Burra Group|33404|5|Briefly described|p108|||Proterozoic.||||||
3106|Burra Group|33405|6|Mentioned|p141|||||||||
3106|Burra Group|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
3106|Burra Group|33423|4|Described|p12|||||||||
3106|Burra Group|33468|6|Mentioned|p209|||Willouran - Torrensian||||||
3106|Burra Group|33473|6|Mentioned|p2|||Adelaidean||||||
3106|Burra Group|33474|6|Mentioned|Fig.2|||||||||
3106|Burra Group|33490|6|Mentioned|p11|||Stratigraphy||||||
3106|Burra Group|33551|6|Mentioned|Fig.1|||Proterozoic||||||
3106|Burra Group|33577|6|Mentioned|p80|||Geol. map.||||||
3106|Burra Group|33691|6|Mentioned|p131|||||||||
3106|Burra Group|33693|6|Mentioned|p153|||||||||
3106|Burra Group|33726|6|Mentioned|p11|||||||||
3106|Burra Group|33794|6|Mentioned|p7|||See also Fig.2||||||
3106|Burra Group|33956|4|Described|p1040|||||||||
3106|Burra Group|33957|5|Briefly described|p35|||||||||
3106|Burra Group|34175|5|Briefly described|p37|||||||||
3106|Burra Group|34176|6|Mentioned|p51|||||||||
3106|Burra Group|34181|6|Mentioned|p43|||||||||17-JAN-22
3106|Burra Group|34202|6|Mentioned|p1056|||See also PP1057,1058. Precambrian.||||||
3106|Burra Group|34266|6|Mentioned|p9|||Adelaidean System||||||
3106|Burra Group|34287|6|Mentioned|p39|||||||||
3106|Burra Group|34291|6|Mentioned|p11|||Adelaide System. Adelaidean||||||
3106|Burra Group|34318|6|Mentioned|p86|||||||||
3106|Burra Group|34320|6|Mentioned|Fig.|||Regional geology plan.||||||
3106|Burra Group|34483|6|Mentioned|p113|||Age: 900 - 1050my for lower sediments.||||||17-JAN-07
3106|Burra Group|34534|6|Mentioned|Fig.2.13|||||||||
3106|Burra Group|34535|3|Fully described|p54|||Adelaidean||||||
3106|Burra Group|34536|6|Mentioned|Map legend|Precambrian|Adelaidean|Torrensian - Sturtian||||||
3106|Burra Group|34537|6|Mentioned|Fig.8|||Torrensian||||||
3106|Burra Group|34586|6|Mentioned|p27|||Torrensian. Mineralization. Drill holes.||||||
3106|Burra Group|34587|6|Mentioned|p36|||Torrensian||||||
3106|Burra Group|34718|6|Mentioned|p13|||||||||
3106|Burra Group|34719|6|Mentioned|p374|||||||||
3106|Burra Group|34766|6|Mentioned|Fig.2|||||||||
3106|Burra Group|34812|6|Mentioned|p4|||||||||
3106|Burra Group|34833|6|Mentioned|p76|||||||||
3106|Burra Group|34844|6|Mentioned|Fig.2|||||||||
3106|Burra Group|34942|6|Mentioned|p105|||||||||
3106|Burra Group|34958|6|Mentioned|p87|||||||||
3106|Burra Group|34979|6|Mentioned|p33|||||||||
3106|Burra Group|34985|6|Mentioned|p309|||||||||
3106|Burra Group|35090|6|Mentioned|p29|||||||||
3106|Burra Group|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3106|Burra Group|35217|6|Mentioned|Fig.1|||||||||
3106|Burra Group|35232|6|Mentioned|p5|||See also Table.1||||||
3106|Burra Group|35255|5|Briefly described|p9|||See also p13 and Fig.3.||||||17-JAN-07
3106|Burra Group|35270|6|Mentioned|p4|||||||||
3106|Burra Group|35327|6|Mentioned|Fig.1|||||||||
3106|Burra Group|35328|6|Mentioned|p9|||Stratigraphy||||||
3106|Burra Group|35353|6|Mentioned|Fig.2|||Regional geology||||||
3106|Burra Group|35354|6|Mentioned|p46|||||||||
3106|Burra Group|35357|6|Mentioned|p21|||||||||
3106|Burra Group|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
3106|Burra Group|35565|6|Mentioned|p21|||Mapping and stratigraphy||||||
3106|Burra Group|35675|6|Mentioned|Fig.1|||Location plan & regional geology.||||||
3106|Burra Group|35893|6|Mentioned|p714|||||||||
3106|Burra Group|35904|6|Mentioned|p6|||||||||
3106|Burra Group|36003|6|Mentioned|p1030|||||||||
3106|Burra Group|36081|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36083|6|Mentioned|Table 1|||||||||
3106|Burra Group|36096|6|Mentioned|Fig.3|||||||||
3106|Burra Group|36126|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36137|5|Briefly described|p3|||||||||
3106|Burra Group|36212|5|Briefly described|p3|||||||||
3106|Burra Group|36245|6|Mentioned|p9|||||||||
3106|Burra Group|36253|6|Mentioned|Fig.3-2|||||||||
3106|Burra Group|36514|6|Mentioned|p55|||||||||
3106|Burra Group|36623|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36626|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36731|6|Mentioned|p123|||||||||
3106|Burra Group|36733|4|Described|p38|||||||||
3106|Burra Group|36833|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36835|6|Mentioned|p31|||||||||
3106|Burra Group|36837|6|Mentioned|Fig.2|||||||||
3106|Burra Group|36838|6|Mentioned|Fig.1|||||||||
3106|Burra Group|36839|6|Mentioned|p61|||||||||
3106|Burra Group|36898|6|Mentioned|p182|||||||||
3106|Burra Group|37113|6|Mentioned|Fig.1|||||||||
3106|Burra Group|37238|6|Mentioned|Table 1|||||||||
3106|Burra Group|37371|6|Mentioned|p382|||||||||
3106|Burra Group|37461|5|Briefly described|p336|||See also p332.||||||17-JAN-07
3106|Burra Group|37501|6|Mentioned|p415|||||||||
3106|Burra Group|37854|2|Defined|p13|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|37932|6|Mentioned|p539|||||||||
3106|Burra Group|38004|6|Mentioned|p82|||||||||
3106|Burra Group|38068|4|Described|p68|||See also Fig.4.||||||
3106|Burra Group|38157|6|Mentioned|Table 1|||||||||
3106|Burra Group|38243|6|Mentioned|p359|||||||||
3106|Burra Group|38581|6|Mentioned|p252|||||||||
3106|Burra Group|38703|6|Mentioned|p131|||||||||
3106|Burra Group|38704|6|Mentioned|p133|||||||||
3106|Burra Group|38926|3|Fully described|p25|||||||||
3106|Burra Group|39210|6|Mentioned|Table 3|||||||||
3106|Burra Group|39320|6|Mentioned|p375|||||||||
3106|Burra Group|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Torrensian to Sturtian||||||
3106|Burra Group|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|39349|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
3106|Burra Group|39350|6|Mentioned|Map legend|Precambrian|Adelaidean|Torrensian to Sturtian||||||
3106|Burra Group|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3106|Burra Group|39352|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Torrensian||||||
3106|Burra Group|39490|6|Mentioned|p10|||||||||
3106|Burra Group|39635|6|Mentioned|Fig.2|||||||||
3106|Burra Group|39724|6|Mentioned|Fig.6|||||||||
3106|Burra Group|39762|6|Mentioned|Table 1|||||||||
3106|Burra Group|39802|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3106|Burra Group|40003|5|Briefly described|Table 2|||||||||
3106|Burra Group|40105|6|Mentioned|p311|||||||||
3106|Burra Group|40225|3|Fully described|Map sheet|||||||||
3106|Burra Group|40228|5|Briefly described|Fig.1|||||||||
3106|Burra Group|40257|6|Mentioned|p287|||||||||
3106|Burra Group|40294|3|Fully described|p32|||||||||
3106|Burra Group|40442|4|Described|p8|||||||||
3106|Burra Group|40448|5|Briefly described|p38|||||||||
3106|Burra Group|40456|6|Mentioned|Fig.2|||||||||
3106|Burra Group|40500|6|Mentioned|p142|||||||||
3106|Burra Group|40501|6|Mentioned|p115|||||||||
3106|Burra Group|40595|6|Mentioned|Fig.8|||||||||
3106|Burra Group|40763|5|Briefly described|p204|||||||||
3106|Burra Group|40852|5|Briefly described|p26|||||||||
3106|Burra Group|40906|6|Mentioned|Fig.9|||||||||
3106|Burra Group|40910|6|Mentioned|p10|||||||||
3106|Burra Group|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|40985|6|Mentioned|p403|||||||||
3106|Burra Group|41256|6|Mentioned|p7|||||||||
3106|Burra Group|41364|6|Mentioned|p152|||||||||
3106|Burra Group|41400|6|Mentioned|p27|||||||||
3106|Burra Group|41401|6|Mentioned|p32|||||||||
3106|Burra Group|41402|6|Mentioned|p36|||||||||
3106|Burra Group|41404|3|Fully described|p73|||||||||
3106|Burra Group|41494|5|Briefly described|p31|||||||||
3106|Burra Group|41647|6|Mentioned|p834|||||||||
3106|Burra Group|41770|6|Mentioned|p249|||||||||
3106|Burra Group|42028|6|Mentioned|p137|||||||||
3106|Burra Group|42087|5|Briefly described|Fig.2 P15|||||||||
3106|Burra Group|42088|5|Briefly described|p546|||||||||
3106|Burra Group|42090|6|Mentioned|p19|||||||||
3106|Burra Group|42093|6|Mentioned|p6|||||||||
3106|Burra Group|42098|4|Described|p51|||||||||
3106|Burra Group|42109|6|Mentioned|Fig.1 P19|||||||||
3106|Burra Group|42167|6|Mentioned|p118|||||||||
3106|Burra Group|42215|5|Briefly described|p442|||See also Fig.2||||||
3106|Burra Group|42222|4|Described|p13|||||||||
3106|Burra Group|42223|4|Described|p37|||See also Fig.2||||||
3106|Burra Group|42235|4|Described|p134|||See also Fig.3||||||
3106|Burra Group|42236|6|Mentioned|Fig.2 P106|||||||||
3106|Burra Group|42237|4|Described|p85|||See also Figs. 1 and 2||||||
3106|Burra Group|42238|4|Described|p72|||||||||
3106|Burra Group|42239|6|Mentioned|Fig.2 P151|||||||||
3106|Burra Group|42243|5|Briefly described|p211|||||||||
3106|Burra Group|42271|6|Mentioned|p372|||||||||
3106|Burra Group|42272|4|Described|p398|||||||||
3106|Burra Group|42274|5|Briefly described|p450|||||||||
3106|Burra Group|42357|6|Mentioned|p8|||||||||
3106|Burra Group|42505|5|Briefly described|Map legend|Adelaidean (Sturtian)|Adelaidean (Torrensian)|||||||
3106|Burra Group|42506|5|Briefly described|Map legend|Adelaidean (Torrensian)||||||||
3106|Burra Group|42546|5|Briefly described|Map legend|Adelaidean (Torrensian)|Adelaidean (Willouran)|||||||
3106|Burra Group|42643|6|Mentioned|Fig. 4 P19|||||||||
3106|Burra Group|42720|5|Briefly described|map legend|Torrensian||||||||
3106|Burra Group|42721|5|Briefly described|map legend|Torrensian||||||||
3106|Burra Group|42723|5|Briefly described|map legend|Torrensian||||||||
3106|Burra Group|42733|6|Mentioned|map legend|Adelaidean||||||||
3106|Burra Group|42736|5|Briefly described|map legend|Neoproterozoic||||||||
3106|Burra Group|42760|6|Mentioned|p3|||||||||
3106|Burra Group|42761|5|Briefly described|Fig.2 P8|||||||||
3106|Burra Group|42762|6|Mentioned|p14|||see also Fig.1 P15||||||
3106|Burra Group|42788|5|Briefly described|p140|||||||||
3106|Burra Group|42813|4|Described|p15|||||||||
3106|Burra Group|42882|5|Briefly described|Table 1 P3|||Of the Warrina Supergroup.||||||17-JAN-07
3106|Burra Group|43048|6|Mentioned|p12|||||||||
3106|Burra Group|43052|4|Described|p177|||See also Table 6.1||||||
3106|Burra Group|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Marine shale and siltstone; deltaic sandstone; lagoonal and lacustrine stromatolitic dolomite and sedimentary magnesite.||||||26-MAY-05
3106|Burra Group|43057|6|Mentioned|Fig.2.24|||||||||
3106|Burra Group|43094|5|Briefly described|p33|||||||||
3106|Burra Group|43190|5|Briefly described|p29, Fig.2.|||||||||
3106|Burra Group|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
3106|Burra Group|43298|5|Briefly described|Map Legend||Adelaidean|||||||
3106|Burra Group|43390|14|Not recorded|p8|||||||||
3106|Burra Group|43595|5|Briefly described|p543-545||Neoproterozoic|||||||
3106|Burra Group|43742|6|Mentioned|p37||Neoproterozoic|||||||
3106|Burra Group|43845|5|Briefly described|Fig3 p43, 41||Neoproterozoic|||||||12-JUL-16
3106|Burra Group|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline||||||
3106|Burra Group|44133|5|Briefly described|p46, 51 Fig. 7.18, 52|Adelaidian|Adeladian|Siltstone, sandstone, dolomite.||||||
3106|Burra Group|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
3106|Burra Group|44659|5|Briefly described|map legend|||Torrensian-Sturtian, lithology.||||||06-DEC-04
3106|Burra Group|44660|14|Not recorded|map legend|||Torrensian, lithology.||||||
3106|Burra Group|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
3106|Burra Group|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Torrensian.||||||
3106|Burra Group|45155|6|Mentioned|Fig.7|||Adelaide geosyncline||||||
3106|Burra Group|46798|6|Mentioned|p102|||||||||
3106|Burra Group|46865|6|Mentioned|Table 2|||||||||
3106|Burra Group|47009|6|Mentioned|p330|||||||||
3106|Burra Group|47012|6|Mentioned|p332|||||||||
3106|Burra Group|49792|6|Mentioned|Fig.5|||||||||
3106|Burra Group|50327|6|Mentioned|p307|||Contains the Rhynie Sandstone.||||||07-FEB-11
3106|Burra Group|50615|5|Briefly described|p302|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt.||||||
3106|Burra Group|60718|4|Described|p48, p49 Fig. 1, p52, 55|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.|||Comprises Emeroo, Mundallio and Bungarider Subgroups.|Unconformably underlies Umberatana Group.||15-APR-11
3106|Burra Group|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Marine shale and siltstone; deltaic sandstone; lagoonal and lacustrine stromatolitic dolomite and sedimentary magnesite.||||||05-JUL-13
3106|Burra Group|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Myrtle Springs Formation, Witchelina Quartzite.||||||
3106|Burra Group|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Warrina Supergroup.||||||
3106|Burra Group|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|||||||17-JAN-07
3106|Burra Group|61153|5|Briefly described|p344-345 Fig. 1|||Unconformably overlain by the Sturt Tillites; unconformably overlies the Gairdner Dyke Swarm. Geological Province: Adelaide Geosyncline.||||||
3106|Burra Group|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Includes Saddleworth Formation.||||||
3106|Burra Group|61263|6|Mentioned|p469|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt.||||||
3106|Burra Group|61307|6|Mentioned|p5, p20|Torrensian|Torrensian|Includes: Saddleworth Fm, Stonyfell Quartzite, Woolshed Flat Shale, Skillogalee Dolomite and Aldgate Sandstone. Geological Province: Adelaide Fold Belt.||||||
3106|Burra Group|61308|5|Briefly described|p6|Adelaidean|Adelaidean|Dolomite, quartzite, siltstone.||||||
3106|Burra Group|61732|5|Briefly described|p3 Fig. 2, p4 Fig. 3|Sturtian|Torrensian|Includes the Belair Subgroup; and the 777+/-7Ma Boucaut Volcanics. Contains microfossils. Geological Province: Adelaide Rift Complex/Stuart Shelf. See also p25, p68, p131.||||||05-JUL-13
3106|Burra Group|62453|5|Briefly described|p11 Fig. 7, 12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||05-JUL-13
3106|Burra Group|62592|5|Briefly described|p20 Fig.2.4, p50 Table 5.1, pp57-58.|Sturtian|Torrensian|Colour scheme shown for interpretation of Curnamona seismic sections.||Unit in Warrina Supergroup.|Includes Emeroo, Mundallio, Bungarider and Belair Subgroups.|Unconformably overlies Callanna Group.||
3106|Burra Group|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Upper part of Warrina Supergroup.|Includes Emeroo and Belair Subgroups.|Unconformably overlies Callanna Group. Is unconformably overlain by Umberatana Group.||
3106|Burra Group|62724|4|Described|p16, p17 Fig. 4|Torrensian|Torrensian|Includes the Bungarider and Belair Subgroups. Siltstone, sandstone, dolomite, magnesite, conglomerate. Geological Province: Curnamona Province.||||||07-FEB-11
3106|Burra Group|62962|5|Briefly described|p2284 Fig. 2, p2296 Tab. 6|Adelaidean|Adelaidean|Age: 777+/-7Ma (Preiss, 2000). Thickness: 3300m, estimated. Geological Province: Mount Painter Province. Consists of sandstone, quartzite, carbonate, siltstone and shale.||||||07-FEB-11
3106|Burra Group|63020|5|Briefly described|p973, p974 Fig. 2|Neoproterozoic|Neoproterozoic|Basement rocks of the Warren Inlier. Includes Emeroo Subgroup. ||||||
3106|Burra Group|63022|5|Briefly described|p1015|Neoproterozoic|Neoproterozoic|Of the Adelaide Rift Complex. Includes Boucaut Volcanics at base. Age: between 777+/-7 (SHRIMP U-Pb) and 700Ma. ||||||
3106|Burra Group|63102|5|Briefly described|p7-8,43,45-46,53|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province. Intruded by late mafic intrusives c. 472-431 Ma.|||||Siltstone, sandstone, dolomite, magnesite and conglomerate.|22-OCT-19
3106|Burra Group|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Undifferentiated: siltstone, sandstone, minor dark grey dolomite.||||||10-SEP-07
3106|Burra Group|64319|5|Briefly described|p354, p355, p356 Fig.2, p357 Fig.3,   |Neoproterozoic|Neoproterozoic|Hosts the Billy Springs deposit of both non-sulfide zinc and sulfide Zn-Pb mineralisation.||||Overlies Callanna Group. Is overlain by Umberatana Group.|Consists predominantly of quartzites, shales and dolomites.|
3106|Burra Group|64400|6|Mentioned|p4|||In the Adelaide Rift Complex.||||||07-FEB-11
3106|Burra Group|64647|5|Briefly described|p38 Fig. 1, p40, p41, p48|Adelaidean|Adelaidean|Overlain by Umberatana, Wilpean, Normanville and Kanmantoo Groups.||||||05-JUL-13
3106|Burra Group|64724|5|Briefly described|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Adelaide Geosyncline between Centralian 1 and Centralian 2 events.||||||
3106|Burra Group|64793|6|Mentioned|p284 fig 3, p285 Fig.4, p290, p293, p295|||Adelaide Rift Complex. Age inferred from Fig.3.|c.778 - c.745 Ma.||Includes Rhynie Sandstone; River Wakefield and Emeroo Subgroups; Skillogalee Dolomite.|||
3106|Burra Group|64796|4|Described|p181, p183 fig 2, p185-193, p195-204|Neoproterozoic|Neoproterozoic|Of Adelaide Rift Complex. Base is first influx of coarse clastics after Curdimurka Subgroup. Top is unconformity under Sturt Tillite. Generalised stratigraphic column on p.191.||Warrina Supergroup|Includes Emeroo Subgroup, Kalachalpa Formation, Rhynie Sandstone and Skillogalee Dolomite.||Sedimentary rocks.|
3106|Burra Group|64797|5|Briefly described|p151, p153 Fig.2,  p158, p160 Fig.8 |||See also p163-166, p167 Tb.10, p168 Tb.11, p169 Fig.12, p172 Tb.13. Adelaide Rift Complex. S-isotope data.|770||Includes Kalachalpa Formation and Skillogalee Dolomite.|||
3106|Burra Group|64801|5|Briefly described|p110|Neoproterozoic|Neoproterozoic|||Warrina Supergroup.|Skillogalee Dolomite.|Overlies the Callanna Group. Is overlain by Umberatana Group.|Largely siliciclastic, but contains widespread beds of magnesite intraclast conglomerate.|
3106|Burra Group|64846|6|Mentioned|p197 Fig.2, p198 Fig.3 |Cryogenian|Cryogenian|||||||
3106|Burra Group|65363|6|Mentioned|p9.|||Adelaide Rift Complex. Correlated with Kanpa Formation in Western Australia on basis of tentative identification of Baicalia burra in that unit.||||||
3106|Burra Group|65365|5|Briefly described|p1, 7, p9 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Northern Adelaide Rift Complex. Includes Kalachalpa Formation and Boucaut Volcanics. Includes stromatolite assemblages.||||||16-MAR-12
3106|Burra Group|65366|5|Briefly described|p19, 21, p23 Fig. 3, p24|Cryogenian|Cryogenian|Adelaide Rift Complex. Includes Boucaut Volcanics, stromatolite assemblages.||||||
3106|Burra Group|65375|6|Mentioned|p25.||||||Includes Emeroo Subgroup.|||
3106|Burra Group|65376|6|Mentioned|p92 Fig. 2.82. |Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|65379|5|Briefly described|p643|||Includes Opaminda Formation, Skillogalee Dolomite, Woolshed Flat Shale and Stonyfell Quartzite. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
3106|Burra Group|65493|6|Mentioned|p908, 909 Fig 1,2|Cryogenian|Cryogenian|Adelaidian units of the Flinders Ranges.||||||
3106|Burra Group|65925|5|Briefly described|pp123-124, Appendix 2.||||||Includes Humanity Seat, Opaminda, Myrtle Springs Formations; Woodnamoka Phyllite; Blue Mine Conglomerate; Wortupa Quartzite and Skillogalee Dolomite.||Siltstone, laminated; shale; sandstone, heavy mineral lamination, quartzose to feldspathic, cross bedding; dolomite, blue-grey to pale pink, lenticular.|
3106|Burra Group|66464|5|Briefly described|p167, p168 Fig.2|Tonian|Tonian|Adelaide Rift Complex. Basal carbonates with evaporites and clastics; siltstone, sandstone and dolostone.||||||
3106|Burra Group|66518|5|Briefly described|p19 Fig.4, p23.|Neoproterozoic|Neoproterozoic|Coombalarnie Platform. C.700m of this unit underlies c.550m of Umberatana Group in an 11 x 14 km basin west of Kalkaroo in a potential geothermal project.||||Unconformably overlies Callanna Group. Is overlain unconformably by Umberatana Group.||
3106|Burra Group|66522|5|Briefly described|p19, 20, 21.|Neoproterozoic|Neoproterozoic|Major changes in thickness, facies and differential erosion of the Group's units across the Nackara Arc were controlled by two major faults that were active during sedimentation. Age constrained by dating of underlying Rook Tuff (see age field).|Between 802 +/- 10 Ma  and  c.660 Ma.||Includes Skillogalee Dolomite, Bungarider Subgroup..|Overlies Curdimurka Subgroup. Is overlain by a Sturtian glacial succession.||24-SEP-15
3106|Burra Group|66884|4|Described|p36-39, p41 Fig.3, p43 Fig. 4, p44|Neoproterozoic|Neoproterozoic|Eastern Willouran Ranges.||Warrina Supergroup|Bungarider Subgroup, Mundallio Subgroup, Emeroo Subgroup|Overlies Callanna Group.||14-DEC-16
3106|Burra Group|66948|5|Briefly described|p19|Cryogenian|Cryogenian||c.800-700 Ma|||Equivalent to the lower Burra Group.||
3106|Burra Group|67180|5|Briefly described|p600, p601 Fig.1, p607|Neoproterozoic|Neoproterozoic|Established by Thomson et al (1964). Poor age constraints||||Overlies the Callanna Group, underlies the Umberatana Group.||
3106|Burra Group|67454|5|Briefly described|p564.|Neoproterozoic|Neoproterozoic|Correlated with Hussar Formation, Officer Basin (WA).||||||
3106|Burra Group|67502|6|Mentioned|p46, p57.||Cryogenian|Of the Adelaide Geosyncline. Suggested to have a time correlation with the Black River Dolomite (Calver, 1998).|||Skillogalee Dolomite.|||26-MAY-14
3106|Burra Group|67536|6|Mentioned|Map Legend||||||||Marine shale and siltstone; deltaic sandstone; lagoonal and lacustrine stromatolitic dolomite and sedimentary magnesite; fluviodeltaic sandstone and conglomerate.|
3106|Burra Group|67870|5|Briefly described|p5, p9-10, p13, p17, p20-21, p23-25|Neoproterozoic|Neoproterozoic|See also p29-30, p32-34. Adelaide Rift System. Produces a series of high amplitude, continuous, subparallel seismic reflections.|||Emeroo, Mundallio, Bungarider, Belair Subgroups.|Overlies Callanna Group. Is overlain unconformably by Umberatana Group.|Sandstone, arkose, dolostone, siltstone.|
3106|Burra Group|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section as Callanna/Burra Group equivalents, including Pindyin Sandstone.||||Equivalent to Pindyin Sandstone|Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, dolomite, minor chert and quartzite.|
3106|Burra Group|67979|6|Mentioned|p528, p530 Fig.1|Cryogenian|Cryogenian|Geol. Prov: Adelaide Geosyncline (as defined by Thomson et al. 1964 and subsequent revisions)||||is overlain by Umberatana Group; overlies Callanna Group||22-SEP-14
3106|Burra Group|68030|6|Mentioned|p238|||Flinders Ranges.||Unit of Warrina Supergroup.||||
3106|Burra Group|68067|6|Mentioned|Map legend.|||Areas with higher magnetic response are mapped separately.||||||27-AUG-13
3106|Burra Group|68243|6|Mentioned|p659, p654 |Torrensian|Torrensian|Adelaide Rift Basin.|< ca. 777 Ma|||||
3106|Burra Group|68270|5|Briefly described|p683|Cryogenian|Tonian|Adelaide Rift Complex. |||Includes Skillogalee Dolomite.|Overlain by Umberatana Group. Underlain by Callanna Group.||
3106|Burra Group|68271|5|Briefly described|p694,696|||Adelaide Rift Complex.|||Includes Skillogalee Dolomite.|||
3106|Burra Group|68713|5|Briefly described|p19, p23|||Variable exposure, from near 100% to partly obscured.||||Unconformably underlain by the Callanna Group.||
3106|Burra Group|69019|5|Briefly described|p38-41, p143.|Neoproterozoic|Neoproterozoic|Torrensian age; Adelaide Geosyncline. Thickness from 2,540 m to 8,470 m.|||Includes Emeroo, Mundallio and Bungarider Subgroups.|Overlies Callanna Group.||
3106|Burra Group|69255|6|Mentioned|p771|Neoproterozoic|Neoproterozoic|Earliest succession in the Adelaide region.||||||
3106|Burra Group|69438|6|Mentioned|p23:14|||Northern Adelaide Fold Belt.||||Lower part of this unit is correlated with Johnnys Creek beds (Amadeus Basin).||12-JUL-16
3106|Burra Group|69606|6|Mentioned|p10|||Adelaide Rift Complex. ||||Correlates with the Finke beds.||
3106|Burra Group|69666|6|Mentioned|p27 Fig.3|Neoproterozoic|Neoproterozoic|||||||
3106|Burra Group|69873|5|Briefly described|p82-83|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.||||Correlated with lower Togari Group (Tas).||
3106|Burra Group|69937|6|Mentioned|p8|||Adelaide Geosyncline.||||Lower part correlated with Johnnys Creek Member (Bitter Springs Formation).||
3106|Burra Group|70000|5|Briefly described|p39||||Between 810 Ma and 700 Ma.||||Fluviatile to shallow marine sequences.|
3106|Burra Group|70021|6|Mentioned|p97|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges, Adelaide Geosyncline.||||||
3106|Burra Group|70323|6|Mentioned|p213,220|||Adelaide Geosyncline.||||Overlain by Umberatana Group.||
3106|Burra Group|70334|6|Mentioned|p19-20,38|||Geological province: Gawler Craton. Of Adelaide Geosyncline.||||||
3106|Burra Group|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline. Age shown more specifically as Torrensian [Cryogenian].||Warrina Supergroup.|Includes Emeroo, Mundallio, Bungarider Subgroups.|Unconformably overlies Callanna Group. Is overlain  unconformably by Umberatana Group (Heysen Supergroup).||18-JAN-19
3106|Burra Group|70405|5|Briefly described|p1, 14 figure 6, p50, p79, p97|Neoproterozoic|Neoproterozoic||||Includes Belair Subgroup, Mintaro Shale, Gilbert Range Quartzite, Kadlunga Slate||Siltstone, sandstone, dolomite, magnesite, conglomerate.|
3106|Burra Group|70407|5|Briefly described|p102 Fig 1, p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Torrensian - Sturtian||Of Warrina Supergroup.||||
3106|Burra Group|70416|5|Briefly described|p80|||Adelaide Rift Complex. Contains the stromatolite Tungussia wilkatanna.||||||
3106|Burra Group|70657|5|Briefly described|p8, p9 Fig.3, p50, p54|Neoproterozoic|Neoproterozoic|Curnamona Province.||||Is overlain unconformably by Umberatana Group.|Siltstone, sandstone, dolomite, magnesite, conglomerate; low-grade metamorphosed.|
3106|Burra Group|70658|5|Briefly described|p14|Neoproterozoic|Neoproterozoic|||Yudnamutana Subgroup.|||Siltstone, sandstone, dolomite, magnesite, conglomerate.|
3106|Burra Group|70660|5|Briefly described|p46|||||||Overlain by the North Maslin Sand.||
3106|Burra Group|70790|6|Mentioned|p258|Neoproterozoic|Neoproterozoic||~777-700 Ma.|||||
3106|Burra Group|70819|6|Mentioned|p11, 13|Neoproterozoic|Neoproterozoic|Clare Valley.|||Emeroo, Mundallio, Bungarider, Belair Subgroups.|||
3106|Burra Group|71129|5|Briefly described|p101-103,107|||Of Adelaide Geosycline. Deposited during the Torrensian, contemporaneous with erosion of Beda Basalt and Backy Point Formation on the Stuart Shelf.||||||
3106|Burra Group|71237|14|Not recorded|p8, 9 |||||||||
3106|Burra Group|71238|14|Not recorded|p1,2, 9|||||||||
3106|Burra Group|71239|14|Not recorded|p3, 5, 9|||||||||
3106|Burra Group|71240|14|Not recorded|p5, p6, p7, 9-10|||New name.||||||
3106|Burra Group|71322|5|Briefly described|p52 Fig.1|Neoproterozoic|Neoproterozoic||||||Laminated siltstone; shale; sandstone, heavy mineral lamination, quartzose to feldspathic, cross-bedding; blue-grey to pale pink, lenticular dolomite.|
3106|Burra Group|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
3106|Burra Group|71529|14|Not recorded|p2, 3|||||||||
3106|Burra Group|71711|6|Mentioned|p401, p402 Fig 10|||Contains abundant 1650-1500 Ma and 1200-1000 Ma detrital zircons.|||Includes Skillogalee Dolomite.|||
3106|Burra Group|72369|5|Briefly described|p43|||Of Adelaide Rift Complex. Lower part can be correlated with Johnnys Creek Formation, Bitter Springs Group (Amadeus Basin) (Grey et al 2011, Hill et al 2011).||||||
3106|Burra Group|72375|5|Briefly described|p13|||Of Adelaide Rift Complex.||||Correlable with Johnnys Creek Formation.||
3106|Burra Group|72429|5|Briefly described|p958|||||||||
3106|Burra Group|72449|5|Briefly described|p1, p2 Map Legend|Neoproterozoic|Neoproterozoic|Subsurface only in the map area. Shown as part of diapir formation diagram, p1.||||Overlies Callanna Group and underlies Pualco Tillite.|Undifferentiated siltstone, sandstone and dolomite.|
3106|Burra Group|72450|5|Briefly described|Brochure map||||c. 750 Ma||Includes the Belair Subgroup, Mitcham Quartzite, Saddleworth Formation, Stonyfell Quartzite, Woolshed Flat Shale, Montacute Dolomite and Aldgate Sandstone.|||
3106|Burra Group|72461|6|Mentioned|p19|||Deposited during a period of rifting, not Describedribed in NSW.|c. 830-770 Ma|||||
3106|Burra Group|72478|6|Mentioned|Fig. 7 p70|||||||||
3106|Burra Group|72489|6|Mentioned|p4 Fig.3|Tonian|Tonian|Adelaide Rift Complex. Only shown on p4 Fig.3. Simplified geological maps.||||Overlies the Callanna Group.||14-SEP-20
3106|Burra Group|72601|6|Mentioned|p6||||||Boucaut Volcanics|||
3106|Burra Group|72613|6|Mentioned|p2 fig 1|Neoproterozoic|Neoproterozoic|Northern Flinders Ranges.||||||
3106|Burra Group|73086|6|Mentioned|p39, p57|||Adelaide Rift Complex. Contains the first appearance of the acritarch Cerebrosphaera buickii in the Adelaide Rift Complex, which is temporally constrained by the underlying Rock Tuff (795 +/- 6 Ma, TIMS U-Pb).||||Underlain by Callanna Group. May partly correlate to Johnnys Creek Formation (Bitter Springs Group) and Wallara Formation.||
3106|Burra Group|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
3106|Burra Group|73093|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic||||||Siltstone, shale and sandstone, minor dolomite.|09-DEC-21
3106|Burra Group|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface. Appears in the Legend as CALLANNA/BURRA GROUP EQUIVALENTS and mapped as one unit. Said to include Pindyin Sandstone, but does not specify to which Group it belongs.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3106|Burra Group|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Presented as Callanna/Burra Group equivalents. Mapped as one unit. Includes Pindyin Sandstone (but which Group contains it is not mentioned). Subsurface.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3106|Burra Group|73110|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Siltstone, laminated; shale; sandstone, heavy mineral lamination, quartzose to feldspathic, cross-bedding; dolomite, blue-grey to pale pink, lenticular.|
3106|Burra Group|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface. Mapped as one unit and named in the Map Legend as CALLANNA/BURRA GROUP EQUIVALENTS. Said to include Pindyin Sandstone, but it is not spelled out which Group is the Parent.|||||Tidal, sabkha and aeolian deposits of anhydritic siltstone, sandstone, shale, dolomite, minor chert and quartzite.|
3106|Burra Group|73188|5|Briefly described|[See comments]|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. Accommodation space provided by eastward-dipping listric extensional faults. Fluvial, deltaic, lagoonal and marine shelf environments. p: 305, 315-316, 319, 321, 323-325, 327, 330, 339-341, 352, 354.|||Belair Subgroup, Bungarider Subgroup, Mundallio Subgroup, Emeroo Subgroup, and units therein|Disconformably[?] underlain by River Broughton Beds.|Mixed siliciclastic and carbonate rocks.|
3106|Burra Group|73222|5|Briefly described|p5-6, p20|Tonian|Tonian|Adelaide Rift Complex. Torrensian to Sturtian Thickness: 3,000 to 8,000 m. Represents the opening of the rift into a shallow ocean.||Warrina Supergroup|||Shale, siltstone, heavy mineral laminated sandstone and dolomite.|
3106|Burra Group|73227|6|Mentioned|p23|||||||||
3106|Burra Group|73234|6|Mentioned|p5|||||||||
3106|Burra Group|73236|6|Mentioned|p47|Tonian|Tonian|Torrensian. Deposited in fluvial, marginal marine and marine shelf settings. Represents the oldest sedimentary rocks in the Adelaide area.|c. 800-700 Ma||||Sand, silt and dolomite.|
3106|Burra Group|73251|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.||||Unconformably underlain by Callanna Group. Unconformably overlain by Umberatana Group.|Metasediments.|
3106|Burra Group|73262|5|Briefly described|p580, p582-583, p586|[Tonian?]|[Tonian?]|Adelaide Rift Complex. Shallow marine depositional environment for basal strata interbedded with the Boucaut Volcanics. Age of the Boucaut Volcanics constrains the base of the Burra Group to 788+/-6 Ma.||Warrina Supergroup|Boucaut Volcanics|Underlain by Callanna Group.|Siltstone, shale, sandstone, dolomite. Includes mudstone and some cross-bedded sandstones.|30-JAN-23
3106|Burra Group|74367|4|Described|p3, p5-6, p7 Fig.6, p13, p17-18, p20|||Proximal marine to marine formations. Age is constrained by deposition after the Mount Crawford Granite Gneiss (812+/-6 Ma).||Warrina Supergroup|Emeroo Subgroup, Mundallio Subgroup, Bungarider Subgroup, Belair Subgroup|Unconformably overlies Wooltana Volcanics, Mount Crawford Granite Gneiss. Overlies Callanna Group|Dominated by clastic and carbonate rocks.|
3106|Burra Group|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
3117|Burraga Granite|23214|3|Fully described|p257|Carboniferous|Carboniferous|Previously Burraga Granodiorite and Thompsons Creek Granite. Intrudes the Adaminaby Group, Triangle Formation and Campbells Formation.  Age: 320Ma (Rb/Sr).||||||04-AUG-04
3117|Burraga Granite|24266|5|Briefly described|p1480, 1489|Carboniferous|Carboniferous|Geological Province: Lachlan Fold Belt.||||||
3117|Burraga Granite|42712|4|Described|Table1p13; Fig3p9.|Carboniferous|Early Carboniferous|Variation on Burraga Granodiorite.||||||
3117|Burraga Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
3117|Burraga Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
3117|Burraga Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
3117|Burraga Granite|67806|6|Mentioned|p110|Carboniferous|Carboniferous|Highly fractionated I-type granite. Mn-stabilised garnet and magnetite are present.||||||
3117|Burraga Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
3124|Burragorang Claystone Member|24471|4|Described|p27, 37-39, p29 Fig.2|Late Permian|Late Permian|Tuff. Geochemical correlation with Awaba Tuff. Thickness: up to 16 m, but variable. Erosively overlain by Lawrence Sandstone Member. Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
3124|Burragorang Claystone Member|39232|6|Mentioned|Table 2|||||||||
3124|Burragorang Claystone Member|40806|6|Mentioned|p158|||||||||
3124|Burragorang Claystone Member|42182|6|Mentioned|p299|||||||||
3124|Burragorang Claystone Member|42657|6|Mentioned|Table 1 P74|||||||||
3126|Burrandana Granite|23721|5|Briefly described|Map Legend|Silurian|Silurian|||||||
3126|Burrandana Granite|24119|5|Briefly described|p3|Silurian|Silurian|||||||
3126|Burrandana Granite|42726|5|Briefly described|map legend|Silurian||No. 543.||Kyeamba Suite.||||19-JAN-17
3126|Burrandana Granite|69043|4|Described|p1, p5-6, p15, p21, p28, p34, p40|Early Devonian|Early Devonian|See also p44-49, p53, p56, p116. SE of Wagga Wagga. Associated with Sn-W greisen- and vein-hosted mineralisation. Previously thought to be part of the c.430 Ma Koetong Supersuite; only possible if the latter were emplaced over 10-15 m.y.|417.7 +/- 2.8 Ma.|Kyeamba Suite.||Age-equivalent with Walleroobie Volcanics and Gurragong Volcanics.|Medium- to coarse-grained, porphyritic, quartz-rich biotite granodiorite. Enclaves of quartzite and other metasedimentary rocks are locally prominent. S-type.|
3126|Burrandana Granite|69371|6|Mentioned|p9, p14, p18-19|Silurian|Silurian|Appears as Burrandana granite.||||||08-DEC-17
3126|Burrandana Granite|69801|6|Mentioned|p2, p136-137|Devonian|Early Devonian|Central Lachlan Orogen. Occurs 40km to the south-east of the Collingullie Granite. Features tin mineralisation.|417.7 +/- 2.8 Ma (SHRIMP)||||S-type granite.|
3126|Burrandana Granite|70777|5|Briefly described|p80|Lochkovian|Pridoli|Lachlan Orogen.|417.7 +/- 2.8 Ma (Bodorkos et al., 2013)|||||
3126|Burrandana Granite|73457|6|Mentioned|p8|Early Devonian|Early Devonian|||||||
3130|Burrawong Limestone|22857|5|Briefly described|p456 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Cudal Group. Fossiliferous detrital limestone. Max. thickness: 730m. Geological Province: Cowra Trough.||||||
3130|Burrawong Limestone|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Cudal Group.||||||
3130|Burrawong Limestone|23170|2|Defined|p104|Ludlow|Ludlow|of Cudal Group.||||||
3130|Burrawong Limestone|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
3130|Burrawong Limestone|32485|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
3130|Burrawong Limestone|37727|6|Mentioned|p70|||||||||
3130|Burrawong Limestone|40328|3|Fully described|p76|||||||||
3130|Burrawong Limestone|43476|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
3130|Burrawong Limestone|43494|3|Fully described|p19-20||Ludlovian|Of Cudal Group. Pale to mid-grey coloured forming massive boulders; limestone consists of calcareous detritus of corals, bryozoa, crinoids, molluscs, brachiopods and algae. Conformably overlies Cary Fm; overlain by Goonigal Group.Max. thick: 730m.||||||01-OCT-09
3138|Burrill Formation|22831|4|Described|p 81-82|||Cookamidgera Subgroup||||||
3138|Burrill Formation|22857|5|Briefly described|p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Hervey Group. Reddish purple mudstone, cross-bedded off-white fine-grained quartz sandstone. Max. thickness: >305m. Geological Province: Hervey Basin.||||||
3138|Burrill Formation|29986|6|Mentioned|Map legend|Devonian|Devonian|||||||
3138|Burrill Formation|32865|6|Mentioned|p484|||Fauna||||||
3138|Burrill Formation|43441|5|Briefly described|31||Late Devonian|Type section in Hervey Range||||||08-JAN-10
3138|Burrill Formation|43500|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Part of Cookamidgera Sub-Group||||||
3138|Burrill Formation|43507|2|Defined|p128,130,161||Late Devonian|Top formation of Cookamidgera Subgroup (Hervey Group)||||||
3138|Burrill Formation|43509|14|Not recorded|p113|||||||||
3138|Burrill Formation|43510|2|Defined|p41-2,47,49-51|||red-beds||||||
3138|Burrill Formation|44160|5|Briefly described|Map Legend||Famennian|||||||08-JAN-10
3138|Burrill Formation|48958|6|Mentioned|Plate 1|||||||||
3142|Burrinjuck Granite|23214|6|Mentioned|p169|||Previously included as part of the Young Granodiorite.||||||
3142|Burrinjuck Granite|23548|5|Briefly described|p533.|||||||||
3142|Burrinjuck Granite|29452|6|Mentioned|p219|||Replaced by term Young Granodiorite?||||||25-JUN-08
3142|Burrinjuck Granite|29453|6|Mentioned|p25|||Date 406 m.y.||||||
3142|Burrinjuck Granite|29454|4|Described|p11|||Lower Devonian.||||||25-JUN-08
3142|Burrinjuck Granite|29682|6|Mentioned|p14|||||||||
3142|Burrinjuck Granite|29989|6|Mentioned|Map legend|Devonian|Devonian|||||||
3142|Burrinjuck Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
3142|Burrinjuck Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
3142|Burrinjuck Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
3142|Burrinjuck Granite|31063|6|Mentioned|p322|||Silurian - Devonian.||||||25-JUN-08
3142|Burrinjuck Granite|31065|6|Mentioned|p1017|||Silurian - Devonian age||||||
3142|Burrinjuck Granite|31928|6|Mentioned|p69|||Boundary characteristics||||||
3142|Burrinjuck Granite|32088|6|Mentioned|p13|||Predates serpentinite||||||
3142|Burrinjuck Granite|32483|4|Described|p34|||Middle Devonian.? Table 1.||||||25-JUN-08
3142|Burrinjuck Granite|33325|6|Mentioned|p17|||||||||
3142|Burrinjuck Granite|33959|6|Mentioned|p234|||||||||
3142|Burrinjuck Granite|33995|6|Mentioned|p19|||Lower Devonian.  See also p20,22.||||||25-JUN-08
3142|Burrinjuck Granite|34289|6|Mentioned|p38|||||||||
3142|Burrinjuck Granite|34544|6|Mentioned|p190|||||||||
3142|Burrinjuck Granite|42726|5|Briefly described|map legend|Silurian||431.  Of the Burrinjuck Suite (Boggy Plain Supersuite).||||||25-JUN-08
3142|Burrinjuck Granite|45147|6|Mentioned|M127|||See also M233||||||
3142|Burrinjuck Granite|50230|5|Briefly described|Map legend|Emsian|Pragian|Megacrystic, medium- to coarse-grained equigranular to porphyritic granite; contains an aplite subunit.||||||
3142|Burrinjuck Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Burrinjuck Suite. Comprises pink, medium- to fine-grained, massive, equigranular, leucocratic biotite granite; Intruded by aplite.||||||25-JUN-08
3142|Burrinjuck Granite|68592|2|Defined|p1219, p1246, p1398, p1400-3, p1405-12|Early Devonian|Early Devonian|See also p931, p956, p1197. This unit appears, un-named, on early maps (Harper, 1909; Edgell, 1949). The name Burrinjuck Granite was proposed by Yates (1942) after Burrinjuck Dam. Best et al. (1964) proposed the name Burrinjuck Adamellite and included parts of the southern Young Granite (subsequently separated and placed in the Young Granodiorite by Ashley and Basden, 1973). The name Burrinjuck Granite is herein reinstated to conform with standard igneous nomenclature. A N-S elongate body cropping out very strongly. Type locality described. Geochemistry detailed; geophysical properties described. Is the only, and therefore the type, pluton in Burrinjuck Suite (Chappell et al., 1991). Is very similar mineralogically and chemically to Jackson Granite and Gurrangorambla Granophyre. Hosts W and Bi mineralisation at the Black Andrew Mine.|415 +/- 8 Ma (K/Ar biotite; Owen and Wyborn,1979)|Unit in Burrinjuck Suite.||Intrudes Mountain Creek Volcanics and Micalong Suite. Is faulted against Hatchery Creek Group.|Pink, medium- to coarse-grained, massive, equigranular, leucocratic, biotite granite; grey, fine-grained, equigranular aplite forms gradational 100-200m wide zones along the E margin. Displays two sets of very strong, planar joints. I-type.|
3142|Burrinjuck Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Djb. Includes an unnamed aplite member. On Yass 1:100 000 mapsheet portion of Time-Space Plot.||Burrinjuck Suite|Includes one unnamed member.||Pink, medium-coarse grained, massive, equigranular leucocratic, biotite granite; high magnetic susceptibility.|
3142|Burrinjuck Granite|70540|5|Briefly described|Map Legend|Devonian|Devonian|Includes an unnamed aplite member.||Burrinjuck Suite|Includes one unnamed member.||Pink, medium-coarse grained, massive, equigranular leucocratic, biotite granite; high magnetic susceptibility.|
3142|Burrinjuck Granite|71206|6|Mentioned|p384|||Zr content >300 p.p.m.||Boggy Plain Supersuite.|||I-type granite.|
3142|Burrinjuck Granite|73215|6|Mentioned|p993, 1004|||||||||
3159|Burrundulla Shale|29993|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
3159|Burrundulla Shale|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
3159|Burrundulla Shale|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
3159|Burrundulla Shale|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
3159|Burrundulla Shale|43476|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
3177|Burthong Formation|22857|4|Described|p438 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Mouramba Group. Quartz-lithic arenite. Max. thickness: 4km. Geological Province: Mouramba Shelf. See also p440 App.1, Tb.A1.6.||||||
3177|Burthong Formation|23171|6|Mentioned|p51|||||||||
3177|Burthong Formation|23173|4|Described|Map Legend|Lochkovian|Pridoli|||||||
3177|Burthong Formation|41394|2|Defined|p47|Lochkovian||Reserved as Burthong Sandstone Member||||||
3177|Burthong Formation|41395|6|Mentioned|Map legend|Lochkovian||||||||
3177|Burthong Formation|41528|2|Defined|p50|Early Devonian||||||||
3177|Burthong Formation|41529|6|Mentioned|Map legend|Lochkovian||||||||
3177|Burthong Formation|42566|6|Mentioned|p62|||of Mouramba Group, Nymagee 1:100 000 sheet.||||||
3177|Burthong Formation|43089|5|Briefly described|Map Legend|||of Mouramba Group||||||
3177|Burthong Formation|70751|5|Briefly described|p5|||||Mouramba Group|||Very fine- to medium-grained interbedded sandstones and siltstones with minor basal conglomeratic units and minor localised felsic volcanic/volcaniclastic horizons.|
3177|Burthong Formation|70950|4|Described|p1029,1039,1040, 1041|||Geological province: Central Lachlan Orogen. An outwash fan to marine shelf sequence.||Unit of Mouramba Group.|||A sequence of very fine to medium-grained interbedded sandstones and siltstones with minor basal conglomeratic units and minor localised felsic volcanic/volcaniclastic horizons.|
3177|Burthong Formation|71039|6|Mentioned|p13-14, p17, p19, p26|||||Mouramba Group|||Arkosic sandstone and conglomerate.|09-MAR-23
3177|Burthong Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Mouramba Group.|||Laminated, moderate- to well-sorted, fine- to very fine-grained quartz-lithic sandstone with lesser laminated siltstone; some massive to bedded granule to pebble polymictic conglomerate and coarse pebbly lithic sandstone.|
3177|Burthong Formation|72908|6|Mentioned|p5, p7, p17|||||Mouramba Group|||Very fine- to medium-grained interbedded sandstones and siltstones with minor basal conglomeratic units and minor localised felsic volcanic/volcaniclastic horizons.|
3177|Burthong Formation|72958|6|Mentioned|p37|Early Devonian|Early Devonian|||||||
3199|Butheroo Shale Member|30610|2|Defined|p323|Early Jurassic|Early Jurassic|Belongs to Purlawaugh Formation||||||
3199|Butheroo Shale Member|35095|6|Mentioned|Table 1|||||||||
3199|Butheroo Shale Member|35416|6|Mentioned|p8|||||||||
3214|Byabbara beds|41348|5|Briefly described|Map legend|Carboniferous||Lithic sandstone, siltstone, mudstone, tuff, limestone.||||||16-DEC-04
3223|Bymue Member|35272|6|Mentioned|p286|||||||||
3223|Bymue Member|41848|5|Briefly described|p361|||Member of Woorinen Formation. Age 29750 +- 1450 yrs||||||
3223|Bymue Member|42264|6|Mentioned|Fig.5 P12|||||||||
3223|Bymue Member|42827|5|Briefly described|Table 9.1|||of Woorinen Formation||||||
3223|Bymue Member|42966|2|Defined|Table35 p236|Late Pleistocene||of Woorinen Formation||||||
3223|Bymue Member|44133|6|Mentioned|p253|Holocene|Middle Pleistocene|Of the Woorinen Formation. Geological Province: Murray Basin.||||||
3224|Bynguano Quartzite|13995|5|Briefly described|p81, p95|||Shergold et al. (1982). Gnalta Shelf: platform deposits associated with Delamerian Orogeny. Has a trilobite fauna similar to that of the Pacoota Sandstone; assigned to the SE China Province.|||||Coarse siliciclastics.|
3224|Bynguano Quartzite|22671|5|Briefly described|Fig2p837|Ordovician|Early Ordovician|Of the Mootwingee Group. Quartzite, sandstone.||||||17-JAN-06
3224|Bynguano Quartzite|22857|5|Briefly described|p120, p408 App. 1 Tb. A1.4.|Early Ordovician|Early Ordovician|Of the Mootwingee Group. Quartzite, sandstone. Max. thickness: 320m. Geological Province: Kanmantoo Fold Belt.||||||
3224|Bynguano Quartzite|22858|6|Mentioned|Fig14.7bp90-1|||||||||
3224|Bynguano Quartzite|23245|5|Briefly described|p120,122||Early Ordovician|||||||
3224|Bynguano Quartzite|23469|5|Briefly described|p 319|||Of Mootwingee Group.||||||27-NOV-08
3224|Bynguano Quartzite|29991|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
3224|Bynguano Quartzite|30908|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|Part of Mootwingee Group||||||
3224|Bynguano Quartzite|31572|6|Mentioned|Fig.|||L.Ordovician. Correlation chart 1.||||||
3224|Bynguano Quartzite|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3224|Bynguano Quartzite|33004|6|Mentioned|Fig.8|||||||||
3224|Bynguano Quartzite|33738|6|Mentioned|p46|||||||||
3224|Bynguano Quartzite|34469|6|Mentioned|p108|||Ordovician||||||
3224|Bynguano Quartzite|35118|6|Mentioned|Fig.5|||||||||
3224|Bynguano Quartzite|39214|4|Described|p10|||||||||
3224|Bynguano Quartzite|40136|5|Briefly described|p19|||||||||
3224|Bynguano Quartzite|40810|5|Briefly described|p14|||[Originally entered for NT. CEBMar95]||||||
3224|Bynguano Quartzite|41810|6|Mentioned|Fig.3|||||||||
3224|Bynguano Quartzite|42206|6|Mentioned|Fig.1 P258|||||||||
3224|Bynguano Quartzite|43501|14|Not recorded|Map Legend||Early Ordovician|(Provisional Edition) Part of Mootwingee Group.||||||27-NOV-08
3224|Bynguano Quartzite|43502|14|Not recorded|Map Legend||Early Ordovician|(Provisional Edition) Part of Mootwingee Group.||||||27-NOV-08
3224|Bynguano Quartzite|50129|4|Described|p16, p18|Early Ordovician|Early Ordovician|Of the Mootwingee Group. Contains marine trace fossils, Rusophycus sp. and Skolithos sp. Max. Thickness: >600m east of Rexes Tank. Unconformably overlain by the Snake Cave Sandstone at Rexes Tank. Geological Province: Rexes Tank Inlier, Darling Basin.||||||
3224|Bynguano Quartzite|62793|5|Briefly described|p270|Early Ordovician|Early Ordovician|Middle unit in Mutawintji Group, overlying Nootumbulla Sandstone and underlying Rowena Formation. Coarse siliciclastic sandstone.||||||
3224|Bynguano Quartzite|62795|5|Briefly described|p347, p349 Fig.2|Early Ordovician|Late Cambrian|Middle unit of Mutawintji Group, overlying Nootumbulla Sandstone and underlying Rowena Formation. Datsonian - Warendian Stages.||||||
3224|Bynguano Quartzite|63121|5|Briefly described|p225 Fig. 2|Early Ordovician|Early Ordovician|Age is Datsonian to Bendigonian. In the Koonenberry Belt, western NSW. Contains Hyperbolus mootwingeensis fossils.||||||13-MAR-07
3224|Bynguano Quartzite|63789|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Mootwingee Group. Quartzite, buff, cross-bedded, interbedded with lesser greenish soft sandstone and mudstone. Late Cambrian to Early Ordovician fossils.||||||
3224|Bynguano Quartzite|64671|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Of the Mootwingee Group.||||||
3224|Bynguano Quartzite|64679|5|Briefly described|Map legend|Ordovician|Late Cambrian|Of the Mutwintji Group.  Buff to grey, planar- and x-bedded quartzite; interbedded with lesser greenish and yellow soft sandstone; red and green mudstone and siltstone; trilobite and brachiopod fossils and trace fossils (Rusphycus, Cruziana and Skolithos)||||||
3224|Bynguano Quartzite|64680|5|Briefly described|Map Legend|Middle Ordovician|Early Ordovician|Of Mootwingee Group.||||||
3224|Bynguano Quartzite|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Mootwingee Group.||||||
3224|Bynguano Quartzite|66623|3|Fully described|pp134-138, pp145-146. |Early Ordovician|Late Cambrian|Named and described by Warris (1967), elaborated by Pogson and Scheibner (1976), renamed the Bynguano Formation by Droser et al. (1994), renamed Bynguano Quartzite again in this study. Forms prominent exposures. 320 m thick. Shelly fossils include trilobites, helicotomid gastropods and lingulide brachiopods; trace fossils are prolific throughout the formation.||Unit in Mutawintji Group.||Overlies Nootumbulla Sandstone. Is overlain by Rowena Formation.|Predominantly quartzite, with cross-bedded quartz sandstone; some pebbly sandstone or conglomerate near the base; red and green micaceous siltstones occur higher in the unit.|
3224|Bynguano Quartzite|66918|5|Briefly described|Map legend|||||Unit in Mutawintji Group.||Overlies Nootumbulla Sandstone. Is overlain by Rowena Formation.|Folded and weakly cleaved, buff, cross-bedded quartz sandstone, interbedded with minor greenish soft sandstone and mudstone; regionally metamorphosed to prehnite-pumpellyite facies.|
3224|Bynguano Quartzite|66929|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|||Unit in Mootwingee Group.||||
3224|Bynguano Quartzite|67322|4|Described|p8-9, p12-13; Fig.5|Tremadocian|Stage 10|Warris (1967). Droser et al. (1994) renamed the unit the Bynguano Formation without justification, but on the basis of long-established priority and lithology, the original name is retained. About 330m thick. Age determined from Fig.5 (Strat. column) and from fossils. Occurs in the Mount Wright-Mutawintji region. Contains a diverse trace-fossil assemblage, shelly fossils and trilobites.||Of the Mutawintji Group.||Conformably overlies Nootumbulla Sandstone. Overlain conformably by the Rowena Formation.|Predominantly quartzite and cross-bedded sandstone.|21-FEB-18
3224|Bynguano Quartzite|67562|6|Mentioned|p104 Fig.10, p112|Early Ordovician|Early Ordovician|> 650m thick.||||Is overlain unconformably by Snake Cave Sandstone.||23-JAN-17
3224|Bynguano Quartzite|70650|5|Briefly described|Map Legend|Ordovician|Cambrian|||Mutawintji Group|||Folded and weakly cleaved, buff, cross-bedded quartz sandstone, interbedded with minor greenish soft sandstone and mudstone.|
3226|Byong Volcanics|22638|6|Mentioned|p64|||Correlates with Cowcumbala Rhyolite||||||
3226|Byong Volcanics|22768|6|Mentioned|p178|||||||||
3226|Byong Volcanics|22831|4|Described|p47|||||||||01-NOV-13
3226|Byong Volcanics|22857|5|Briefly described|p178, p448 App.1, Tb.A1.6|Pridolian|Pridolian|Of the Derriwong Group. Feldspar porphyry lava or shallow intrusion. Max. thickness: 200m. Geological Province: Bogan Gate Terrace.||||||
3226|Byong Volcanics|23522|5|Briefly described|p253|Devonian|Devonian|||||||
3226|Byong Volcanics|24417|3|Fully described|p70|Late Silurian|Late Silurian|Formerly "Milpose Volcanics".  Of Derriwong Group.  Max. thickness: ~1000m.||||||
3226|Byong Volcanics|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
3226|Byong Volcanics|31161|5|Briefly described|PA4|||||||||
3226|Byong Volcanics|31722|6|Mentioned|p136|||Stratigraphy||||||
3226|Byong Volcanics|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
3226|Byong Volcanics|33732|5|Briefly described|Table II|||See also P114.||||||
3226|Byong Volcanics|36066|6|Mentioned|p9|||||||||
3226|Byong Volcanics|37727|6|Mentioned|p34|||See also P77.||||||
3226|Byong Volcanics|39618|6|Mentioned|Fig.7|||||||||
3226|Byong Volcanics|39663|6|Mentioned|Table 1|||||||||
3226|Byong Volcanics|40328|6|Mentioned|p41|||||||||
3226|Byong Volcanics|40365|6|Mentioned|p242|||||||||
3226|Byong Volcanics|42489|5|Briefly described|Map legend|Lochkovian||||||||
3226|Byong Volcanics|43441|5|Briefly described|27|Early Devonian|Late Silurian|||||||08-JAN-10
3226|Byong Volcanics|44160|5|Briefly described|Map Legend||Pridolian|||||||08-JAN-10
3226|Byong Volcanics|46524|6|Mentioned|Appedix 1 P129|||||||||
3226|Byong Volcanics|46525|6|Mentioned|Fig.1 P143|||||||||
3226|Byong Volcanics|46528|5|Briefly described|Map legend|Early Devonian||||||||
3226|Byong Volcanics|50299|5|Briefly described|Map Legend|Devonian|Silurian|Of the Derriwong Group.||||||
3226|Byong Volcanics|50554|5|Briefly described|Map legend|Devonian|Silurian|Of the Derriwong Group.  Silicic feldspar porphyry and rhyolite.||||||
3226|Byong Volcanics|60009|5|Briefly described|Map Legend|Lochkovian|Pridoli|Of the Derriwong Group.||||||13-JUL-04
3233|Byrock Granite|23171|6|Mentioned|p13||Early Devonian|||||||
3233|Byrock Granite|34449|6|Mentioned|Table 2-1|||||||||
3233|Byrock Granite|40328|4|Described|p204|||||||||
3233|Byrock Granite|68823|5|Briefly described|p376 Fig.3, p377, p378 Fig.4|Lochkovian|Lochkovian|Overlaps in age with deposition of Cobar Supergroup.|414.7 +/- 2.4 Ma, SHRIMP U-Pb (Black 2006)|||||
3233|Byrock Granite|69002|6|Mentioned|p12|||||Of the Westella Suite.|||I-type granite.|
3233|Byrock Granite|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|Includes an un-named but separately-mapped sub-unit of 'altered granite; extensive silica replacement with sericite and iron oxides'.||Unit in Westella Suite.|||Grey to white, medium- to coarse-grained biotite granite with abundant biotite-rich enclaves; contains xenoliths of metamorphosed country-rock; foliated locally.|
3233|Byrock Granite|69541|5|Briefly described|p645 Fig.1(b)|Early Devonian|Early Devonian|Lachlan Orogen.|414.7 +/- 2.4 Ma.|||||
3233|Byrock Granite|70210|5|Briefly described|p1, p10, p38, p40-41|Early Devonian|Late Silurian|Cobar-Bourke district.|414.7 +/- 2.4 Ma.|||||
3233|Byrock Granite|70602|6|Mentioned|p66 Fig 2,p67,72|Early Devonian|Late Silurian|Aeromagnetic map data given.|414.7+/-2.4Ma|Westella Suite||||
3233|Byrock Granite|70941|3|Fully described|pviii-px, p4 ph4, p9|Early Devonian|Late Silurian|Named for the town of Byrock. The informal Byrock, Boshs Tank and Westella granites have here been formally incorporated into the Byrock Granite.Contains one informal unit.  Type granite for the Westella Suite. Emplacement ages. Distribution, geomorphology, structure, geochemistry, geophysical characteristics and distinguishing features discussed. Type locality mentioned. Thickness is unknown. Contact metamorphosed the Girilambone Group.I type. See also p54, p58 fig 23, p59,  p67-71, p106, p112, p113, p125, p129, p131, p136, p137, p140, p145, p152|414.7 +/- 2.4 Ma, 416.8 +/- 2.5 Ma (SHRIMP U/Pb)|Westella Suite||Intrudes Girilambone Group, equivalent to the Pendianna Tank and Emohruo Granites|Pale grey to white, medium grained granite consisting of K-feldspar, quartz, plagioclase and biotite. Mafic enclaves occur throughout this unit.|
3233|Byrock Granite|71345|6|Mentioned|p22,30|||Occurs west of, and is younger than Gelnariff Granite.||||||
3233|Byrock Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: area of low magnetic intensity which shows only slight contrast with host metasedimentary rocks; the boundary is also based on geological mapping. A high-amplitude, long-wavelength magnetic anomaly in the north may relate to a deeper phase of the intrusion.|416.8 +/- 2.5 Ma and 414.7 +/- 2.5 Ma.|Westella Suite.|||Medium- to coarse-grained biotite granite with minor hornblende. Mafic enclaves, metasedimentary xenoliths and foliation occur locally. I-type.|
3233|Byrock Granite|72296|6|Mentioned|p12, p25|||||||Intrudes Narrama and Lang Formations.||
3233|Byrock Granite|72951|5|Briefly described|p1013, 1017, 1022-1023|Lochkovian|Pridoli|Lachlan Orogen. Hermidale Terrane. I-type. SHRIMP U-Pb zircon isotope analyses of Byrock Granite from Black (2007) were referred to as being from the 'Westella Granite'. eHf = 1.4 +/- 1.4, and d18O = 8.01 +/- 0.48.|416.8 +/- 2.5 Ma||||Porphyritic coarse-grained granite.|
3235|Byron Range Group|22768|6|Mentioned|p178|||||||||
3235|Byron Range Group|22857|5|Briefly described|p178, p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Geological Province: Bogan Gate Terrace.||||||
3235|Byron Range Group|23309|6|Mentioned|p390|||||||||
3235|Byron Range Group|29648|6|Mentioned|p19|||||||||
3235|Byron Range Group|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
3235|Byron Range Group|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
3235|Byron Range Group|30790|5|Briefly described|p1|||Lower Devonian age||||||
3235|Byron Range Group|31161|5|Briefly described|PA7|||||||||
3235|Byron Range Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
3235|Byron Range Group|32672|6|Mentioned|p673|||||||||
3235|Byron Range Group|33325|5|Briefly described|Table 4|||||||||
3235|Byron Range Group|33326|6|Mentioned|p441|||Fauna.||||||
3235|Byron Range Group|33327|5|Briefly described|p173|||See also Fig.2. Constituent formations.||||||
3235|Byron Range Group|33732|5|Briefly described|p111|||||||||
3235|Byron Range Group|34184|4|Described|p5|||Lower Devonian||||||
3235|Byron Range Group|34403|5|Briefly described|p144|||||||||
3235|Byron Range Group|34405|6|Mentioned|Fig.3.9|||||||||
3235|Byron Range Group|34406|6|Mentioned|p223|||||||||
3235|Byron Range Group|34692|6|Mentioned|p187|||||||||
3235|Byron Range Group|37195|6|Mentioned|Fig.1|||||||||
3235|Byron Range Group|40328|6|Mentioned|p44|||||||||
3235|Byron Range Group|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
3235|Byron Range Group|40498|6|Mentioned|p364|||||||||
3235|Byron Range Group|42994|6|Mentioned|p137|||||||||
3235|Byron Range Group|43461|14|Not recorded|p621||Devonian|||||||
3235|Byron Range Group|44092|5|Briefly described|map legend|Early Devonian|Early Devonian|Dls||||||
3235|Byron Range Group|60078|6|Mentioned|Map Legend|Early Devonian|Early Devonian|||||||
3235|Byron Range Group|60086|5|Briefly described|Map legend|Late Devonian|Middle Devonian|Includes the Round Top Formation, Lick Hole Limestone and Milk Shanty Formation.||||||
3235|Byron Range Group|63290|6|Mentioned|p403 Fig. 6(c)|Early Devonian|Early Devonian|Geological Province: Tumut Block.||||||
3248|CSA Siltstone|730|5|Briefly described|p24, 23.|Devonian|Devonian|Cobar Supergroup of Cobar Sub-basin, Darling Basin. Contains minor felsic tuffs.||||||11-NOV-14
3248|CSA Siltstone|22857|5|Briefly described|p436 App. 1, Tb.A1.6|Early Devonian|Early Devonian|Of the Amphitheatre Group (Cobar Supergroup). Max. thickness: <1.3km. Geological Province: Cobar Basin.||||||
3248|CSA Siltstone|23095|6|Mentioned|p610|||||||||
3248|CSA Siltstone|23096|4|Described|p602|||Amphitheatre Group||||||
3248|CSA Siltstone|23171|5|Briefly described|p15,44,Fig15p45|||||||||
3248|CSA Siltstone|23173|4|Described|Map Legend|||||||||
3248|CSA Siltstone|23734|5|Briefly described|p12 Fig. 1|||Parent: Amphitheatre Group.||||||
3248|CSA Siltstone|24019|6|Mentioned|p353|Early Devonian|Early Devonian|||||||
3248|CSA Siltstone|29680|6|Mentioned|Fig.1|||||||||
3248|CSA Siltstone|29947|4|Described|p685|||||||||
3248|CSA Siltstone|29948|5|Briefly described|p27|||Mention Fig.12||||||
3248|CSA Siltstone|37936|6|Mentioned|Fig.2|||||||||
3248|CSA Siltstone|37974|6|Mentioned|p312|||||||||
3248|CSA Siltstone|39083|6|Mentioned|Fig.1|||||||||
3248|CSA Siltstone|41410|6|Mentioned|Fig.1|||||||||
3248|CSA Siltstone|41452|6|Mentioned|p22|||||||||
3248|CSA Siltstone|41872|6|Mentioned|p8|||||||||
3248|CSA Siltstone|42144|5|Briefly described|p605|||See also Fig.3||||||
3248|CSA Siltstone|42172|4|Described|p162|||See also Fig.4&5||||||
3248|CSA Siltstone|42208|5|Briefly described|p304|||||||||
3248|CSA Siltstone|42285|5|Briefly described|p4|||||||||
3248|CSA Siltstone|42521|5|Briefly described|p19, Figs|||||||||
3248|CSA Siltstone|42907|6|Mentioned|Fig.8, P8|||||||||
3248|CSA Siltstone|42983|6|Mentioned|Fig.3,p345|||||||||
3248|CSA Siltstone|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|of Amphitheatre Group||||||
3248|CSA Siltstone|43757|6|Mentioned|p511||Early Devonian|Age: 390-400 Ma||||||
3248|CSA Siltstone|43774|1|Redefined|p47-53||Devonian|||||||
3248|CSA Siltstone|46943|6|Mentioned|p71|||||||||
3248|CSA Siltstone|46947|6|Mentioned|p77|||Misspelling of C.S.A. Siltstone [CEBMar95]||||||
3248|CSA Siltstone|61905|5|Briefly described|p135|||Of the Cobar Supergroup. Turbiditic siltstones and sandstones.||||||24-JAN-07
3248|CSA Siltstone|61907|5|Briefly described|p143|||Of the Cobar Group.||||||
3248|CSA Siltstone|65469|5|Briefly described|p14, App A-VI 3|Lochkovian|Pridoli|Lachlan Orogen.||Amphitheatre Group||Overlain by the Biddabirra Formation. Overlies the Great Cobar Slate.||
3248|CSA Siltstone|68823|6|Mentioned|p378 Fig.4|Early Devonian|Late Silurian|Cobar Basin. Lachlan Orogen.||||Unconformably overlies Great Cobar Slate. Is overlain by Biddabirra Formation.||
3248|CSA Siltstone|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Late Silurian|Lachlan Orogen.||||||
3248|CSA Siltstone|70821|6|Mentioned|p28|||||Cobar Supergroup.||||
3248|CSA Siltstone|70941|6|Mentioned|p78 fig 32|Late Silurian|Late Silurian|||||Overlies the Great Cobar Slate. Overlain by the Amphitheatre Group.||
3248|CSA Siltstone|71039|5|Briefly described|p15|||Outcrops in the Endeavour (Elura) mine.||Amphitheatre Group.|||Carbonate spotted siltstone.|
3248|CSA Siltstone|71285|5|Briefly described|p538-540, p546-549, p552 Fig.9|Early Devonian|Late Silurian|Cobar region. Associated with several Cu-Zn-Pb-Ag deposits (described). Sulfur isotopes, fluid inclusion temperatures detailed.||Amphitheatre Group.||||
3248|CSA Siltstone|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Amphitheatre Group.||Is overlain by Biddabirra and Shume Formations.|Thin-bedded, graded, parallel-laminated carbonaceous siltstone and mudstone with some thin, fine-grained, commonly ripple cross-laminated quartz sandstone beds. Rare medium-bedded, massive to parallel-laminated, medium-grained lithic sandstone beds.|
3248|CSA Siltstone|73143|5|Briefly described|p1-4|Early Devonian|Early Devonian|Lachlan Orogen. Conformably (or disconformably) overlies Elura Limestone Member. Cobar Superbasin, northern. Transgressive sequence from shelf edge to deep water turbidites. Host to the Endeavour Zn-Pb-Ag deposit.||Amphitheatre Group||Conformably overlies Elura Limestone Member.|Siltstone with fine-grained sandstone and shale sequences. Includes mudstone and strongly deformed fine-grained lithic sandstone in lower part.|
3248|CSA Siltstone|73174|6|Mentioned|p1036-1037|Lochkovian|Lochkovian|Cobar Basin.||Amphitheatre Group, Cobar Supergroup|Lerida Limestone Member|Overlain by Biddabirra Formation.||
3251|Cabanandra Granodiorite|22876|5|Briefly described|p28|||Dalgety Supersuite||||||
3251|Cabanandra Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Dalgety Supersuite. G67. Biotite granodiorite. S-Type.||||||26-OCT-04
3251|Cabanandra Granodiorite|23309|6|Mentioned|p426 App 1|||G67.||||||
3251|Cabanandra Granodiorite|41850|6|Mentioned|p431|||||||||
3251|Cabanandra Granodiorite|42627|5|Briefly described|Map legend|Wenlock||||||||
3251|Cabanandra Granodiorite|42647|3|Fully described|p46|||||||||
3251|Cabanandra Granodiorite|42827|5|Briefly described|p431|||||||||
3251|Cabanandra Granodiorite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Biotite granodiorite: medium grained, quartz phyric; grey; S-type.|
3277|Cadia Coach Shale|13139|5|Briefly described|p7|Llandovery|Llandovery|||||||12-APR-05
3277|Cadia Coach Shale|22503|6|Mentioned|p648||Early Silurian|||||||
3277|Cadia Coach Shale|22679|4|Described|p 25||Silurian|Ashburnia Group.||||||17-JUL-08
3277|Cadia Coach Shale|22857|5|Briefly described|p426 App. 1 Tb. A1.5|Llandovery|Llandovery|Of the Ashburnia Group. Feldspathic siltstone and arenite, limestone, conglomerate. Max. thickness: 105m.||||||
3277|Cadia Coach Shale|23090|5|Briefly described|p642||Silurian|||||||
3277|Cadia Coach Shale|23214|2|Defined|p106|Llandovery|Llandovery|Of Ashburnia Group. Originally included in the Panuara Formation (subsequently Panuara Group).  105m Thick at type section.||||||
3277|Cadia Coach Shale|23334|5|Briefly described|7|Llandovery|Llandovery|||||||
3277|Cadia Coach Shale|35258|4|Described|p117|||||||||
3277|Cadia Coach Shale|43640|5|Briefly described|Map Legend||Silurian|||||||
3277|Cadia Coach Shale|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Ashburnia Group. Consists of feldspathic siltstone, mudstone, poorly sorted sandstone, limestone, conglomerate.||||||15-JUL-08
3277|Cadia Coach Shale|43653|5|Briefly described|Map Legend||Silurian|||||||
3277|Cadia Coach Shale|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Ashburnia Group. Feldspathic siltstone, mudstone, poorly sorted sandstone, limestone, conglomerate.||||||17-JUL-08
3277|Cadia Coach Shale|43782|6|Mentioned|Map diagram|Llandovery|Llandovery|of Ashburnia Group.||||||
3277|Cadia Coach Shale|60443|4|Described|p765 Fig.3||Early Silurian|Unconformably overlies Forest Reefs Volcanics. Interbedded sandstones and siltstones. Geological Province: Lachlan Fold Belt.||||||
3277|Cadia Coach Shale|63290|5|Briefly described|p401 Fig. 5(d)|Llandovery|Llandovery|Of Ashburnia Group. Underlain by Bagdad Formation.||||||
3277|Cadia Coach Shale|67821|6|Mentioned|p150|Silurian|Silurian|||||||
3277|Cadia Coach Shale|70297|5|Briefly described|map legend, on side 2 of map sheet|Early Silurian|Early Silurian|Age: early to middle Llandovery.||Ashburnia Group||||
3277|Cadia Coach Shale|70684|6|Mentioned|p50 Fig.24, p51|Early Silurian|Early Silurian|Molong Volcanic Belt. ||Ashburnia Group.||||
3284|Cadna-owie Formation|730|6|Mentioned|p24, p25.|||Paralic.||||||11-NOV-14
3284|Cadna-owie Formation|12597|4|Described|p492 Tb.1, p499|Barremian|Early Cretaceous|Eromanga Basin. Up to 110m thick. Contains marine bivalves, gastropods, dinoflagellates and arenaceous foraminifera.|||Includes Mount Anna Sandstone, and Wyandra Sandstone, Members.|Conformably overlies Hooray Sandstone, Murta Member and Algebuckina Sandstone.|Siltstone and silty mudstone with interbeds of fine-grained labile sandstone and minor glauconite grading upwards to quartzose sandstone; overlain by Wyandra Sandstone Member (q.v.).|
3284|Cadna-owie Formation|13497|5|Briefly described|p50, p66-p67, p216|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also p115, p115 fig 6.33, p138 fig 8.17, p141, p146, p149-p152, p154 .||||Overlies the Murta Formation. Overlain by the Bulldog Shale and Wallumbilla Formation.||
3284|Cadna-owie Formation|13516|5|Briefly described|p167 fig 10,  p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Mount Anna Sandstone Member, Wyandra Sandstone Member|||
3284|Cadna-owie Formation|22839|6|Mentioned|P33|||||||||
3284|Cadna-owie Formation|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Barremian|Valanginian|Known as the Gum Vale beds in Tibooburra area. Max. thickness: 130m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6, p314.||||||
3284|Cadna-owie Formation|22865|4|Described|p314,Table22.1p296-7|Neocomian|Late Jurassic|||||||
3284|Cadna-owie Formation|22874|6|Mentioned|P18|||||||||
3284|Cadna-owie Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Wallumbilla Formation, underlying unit is Murta Formation||||||
3284|Cadna-owie Formation|22912|5|Briefly described|33|||Geol. province: Eromanga Basin.||||||03-AUG-06
3284|Cadna-owie Formation|22922|6|Mentioned|33 fig 2|||||||||
3284|Cadna-owie Formation|23054|5|Briefly described|p21,23-4|Aptian|Aptian|||||||
3284|Cadna-owie Formation|23056|6|Mentioned|93 table 5|||Geol province Eromanga Basin||||||
3284|Cadna-owie Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Parent - Neales River Group.||||||
3284|Cadna-owie Formation|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age Neocomian-Aptian. Formerly named as `Transition Beds' the new name Cadna-owie Formation was first used by Wopfner et al (1970).  On STRZELECKI the unit is underlain by Murta Formation (conformity).||||||
3284|Cadna-owie Formation|23282|6|Mentioned|p85 Fig 6.2|||of Eromanga Basin.||||||
3284|Cadna-owie Formation|23375|4|Described|Fig2 p264,265,267,269,271,277|Barremian|Valanginian|Geol. Prov:  Eromanga Basin.||||||03-AUG-06
3284|Cadna-owie Formation|23425|6|Mentioned|p391.|||Variation of Cadna-Owie Formation.||||||
3284|Cadna-owie Formation|23430|4|Described|p523 + p524 Table 14.7|||Eromanga Basin Province.||||||16-SEP-08
3284|Cadna-owie Formation|23818|4|Described|p141 Fig.65, p144 Fig.66, p156|Aptian|Aptian|Geological Province: Great Artesian Basin. Of the Neales River Group. Max. thickness: 250 ft. Overlying unit: Bulldog Shale.||||||
3284|Cadna-owie Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||
3284|Cadna-owie Formation|23849|5|Briefly described|p781|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Geological Province: Great Australian Superbasin.||||||
3284|Cadna-owie Formation|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
3284|Cadna-owie Formation|24067|5|Briefly described|p249 Fig.2|Mesozoic|Mesozoic|Geological Province: Officer Basin.||||||
3284|Cadna-owie Formation|24092|6|Mentioned|p5|||Geological Province: Great Artesian Basin.||||||
3284|Cadna-owie Formation|24112|5|Briefly described|p254 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin||||||
3284|Cadna-owie Formation|24175|3|Fully described|p19, p17 Fig. 3|Aptian|Neocomian|Thin transgressive sequence of sandstone, siltstone and shale.  Lies transitionally between Bulldog Shale above and Algebuckina Sandstone below.  Max. thickness: 50m.||||||
3284|Cadna-owie Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone Member.  Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24243|5|Briefly described|p3 Fig.2|Early Cretaceous|Early Cretaceous|Of Blythesdale Group.||||||
3284|Cadna-owie Formation|24321|5|Briefly described|Map legend|Barremian|Neocomian|Of theNeales River Group.||||||03-AUG-06
3284|Cadna-owie Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24392|5|Briefly described|p139, p144 Appendix 1|Valanginian|Berriasian|Locally known as Parabarana Sandstone. See also page 140 Fig.1. Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
3284|Cadna-owie Formation|24507|6|Mentioned|p27|||Oil production has commenced from this unit. Geological Province: Cooper Basin.||||||
3284|Cadna-owie Formation|24510|6|Mentioned|p48|||Includes Livingston Tillite Member.||||||
3284|Cadna-owie Formation|29379|4|Described|p30|||Lithology. Early-Lower Cretaceous.||||||
3284|Cadna-owie Formation|29591|6|Mentioned|Fig.22|||||||||
3284|Cadna-owie Formation|29659|6|Mentioned|p8|||||||||
3284|Cadna-owie Formation|29660|6|Mentioned|p6|||||||||
3284|Cadna-owie Formation|29838|6|Mentioned|p4|||||||||
3284|Cadna-owie Formation|30024|6|Mentioned|p335|||See also Fig.3.||||||
3284|Cadna-owie Formation|30075|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|30512|6|Mentioned|p41|||||||||
3284|Cadna-owie Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|30804|6|Mentioned|p7|||See also P10 and Table 1.||||||
3284|Cadna-owie Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
3284|Cadna-owie Formation|30917|6|Mentioned|p42|||||||||
3284|Cadna-owie Formation|30919|6|Mentioned|Map legend|Neocomian|Neocomian|||||||
3284|Cadna-owie Formation|30920|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|30924|6|Mentioned|Map legend|Aptian|Aptian|||||||
3284|Cadna-owie Formation|31208|6|Mentioned|p46|||See also Fig. 7||||||
3284|Cadna-owie Formation|31244|6|Mentioned|p3|||Lower Cretaceous||||||
3284|Cadna-owie Formation|31249|6|Mentioned|p63|||||||||
3284|Cadna-owie Formation|31251|6|Mentioned|p74|||Microfloral assemblage in type section||||||
3284|Cadna-owie Formation|31697|6|Mentioned|p5|||L.Cretaceous||||||
3284|Cadna-owie Formation|31699|4|Described|p133|||L.Cretaceous||||||
3284|Cadna-owie Formation|32033|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|32204|4|Described|p8|||Details of Refraction and p8.  L.Cret.||||||03-AUG-06
3284|Cadna-owie Formation|32205|6|Mentioned|p13|||||||||
3284|Cadna-owie Formation|32275|6|Mentioned|p8|||Refers Wopfner Freytag & Heath (1970)||||||
3284|Cadna-owie Formation|32277|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|32314|6|Mentioned|Fig. 4|||||||||
3284|Cadna-owie Formation|33017|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
3284|Cadna-owie Formation|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|33490|6|Mentioned|p30|||Correlation||||||
3284|Cadna-owie Formation|33491|4|Described|p56|||Mention Fig.2||||||
3284|Cadna-owie Formation|33521|6|Mentioned|p8|||||||||
3284|Cadna-owie Formation|33523|4|Described|p27|||||||||
3284|Cadna-owie Formation|33820|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
3284|Cadna-owie Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|33822|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
3284|Cadna-owie Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
3284|Cadna-owie Formation|33824|6|Mentioned|p12|||Table 2||||||
3284|Cadna-owie Formation|33825|6|Mentioned|p8|||Lithology||||||
3284|Cadna-owie Formation|33827|5|Briefly described|p13|||Table 2||||||
3284|Cadna-owie Formation|33828|6|Mentioned|p5|||Table 1||||||
3284|Cadna-owie Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
3284|Cadna-owie Formation|33832|6|Mentioned|p6|||Stratigraphy||||||
3284|Cadna-owie Formation|33844|6|Mentioned|p35|||Refers Wopfner (1969)||||||
3284|Cadna-owie Formation|33933|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|33936|6|Mentioned|Fig.3a|||Cretaceous.||||||
3284|Cadna-owie Formation|33938|6|Mentioned|p46|||||||||
3284|Cadna-owie Formation|33939|2|Defined|p394|Early Cretaceous|Early Cretaceous|||||||
3284|Cadna-owie Formation|33964|4|Described|p6|||Cretaceous||||||
3284|Cadna-owie Formation|33971|6|Mentioned|p24|||See also P25 & Fig.15.||||||
3284|Cadna-owie Formation|33976|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|34611|3|Fully described|p156|||Fig.65. Correlation chart. Cretaceous.||||||16-SEP-08
3284|Cadna-owie Formation|35149|5|Briefly described|Table 1|||See also mention on Fig.4.||||||
3284|Cadna-owie Formation|35239|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|35548|6|Mentioned|p18|||||||||
3284|Cadna-owie Formation|35549|6|Mentioned|Fig.8|||Now called Marree Formation||||||
3284|Cadna-owie Formation|35560|6|Mentioned|p292|||||||||
3284|Cadna-owie Formation|35628|4|Described|Table 4|||||||||
3284|Cadna-owie Formation|35663|6|Mentioned|p124|||||||||
3284|Cadna-owie Formation|35793|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
3284|Cadna-owie Formation|36214|5|Briefly described|p58|||||||||
3284|Cadna-owie Formation|36243|6|Mentioned|Table 6A|||||||||
3284|Cadna-owie Formation|36251|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|36494|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|36552|6|Mentioned|p59|||||||||
3284|Cadna-owie Formation|36571|6|Mentioned|Table 4|||||||||
3284|Cadna-owie Formation|36733|6|Mentioned|p14|||See also P53.||||||
3284|Cadna-owie Formation|36895|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|36912|6|Mentioned|p75|||||||||
3284|Cadna-owie Formation|36920|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|36922|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|36966|6|Mentioned|p83|||||||||
3284|Cadna-owie Formation|37776|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|37995|6|Mentioned|p66|||||||||
3284|Cadna-owie Formation|38022|6|Mentioned|Fig.4|||||||||
3284|Cadna-owie Formation|38068|4|Described|p72|||||||||
3284|Cadna-owie Formation|38199|6|Mentioned|p428|||||||||
3284|Cadna-owie Formation|38604|6|Mentioned|Map legend|Neocomian|Neocomian|||||||
3284|Cadna-owie Formation|38605|6|Mentioned|p20|||See also Table 4.||||||
3284|Cadna-owie Formation|38814|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|39070|4|Described|p364|||||||||
3284|Cadna-owie Formation|39211|5|Briefly described|p23|||See also Figs 4,7,8,10,13-15 etc. Correlation||||||
3284|Cadna-owie Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
3284|Cadna-owie Formation|39445|5|Briefly described|Table 10|||||||||
3284|Cadna-owie Formation|39630|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|39846|6|Mentioned|p44|||||||||
3284|Cadna-owie Formation|39847|5|Briefly described|p37|||||||||
3284|Cadna-owie Formation|39914|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|39943|6|Mentioned|Table 8A|||||||||
3284|Cadna-owie Formation|39988|6|Mentioned|p291|||||||||
3284|Cadna-owie Formation|39989|4|Described|p423|||||||||
3284|Cadna-owie Formation|40003|6|Mentioned|p33|||See also Fig.8||||||
3284|Cadna-owie Formation|40030|6|Mentioned|p132|||||||||
3284|Cadna-owie Formation|40121|6|Mentioned|p446|||||||||
3284|Cadna-owie Formation|40199|4|Described|p25|||||||||
3284|Cadna-owie Formation|40220|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|40249|6|Mentioned|p41|||||||||
3284|Cadna-owie Formation|40544|6|Mentioned|p157|||||||||
3284|Cadna-owie Formation|40670|6|Mentioned|Fig.9|||||||||
3284|Cadna-owie Formation|40675|6|Mentioned|Table 8A|||||||||
3284|Cadna-owie Formation|40681|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|40687|3|Fully described|p417|||||||||
3284|Cadna-owie Formation|40832|3|Fully described|p456|||||||||
3284|Cadna-owie Formation|40833|6|Mentioned|p468|||||||||
3284|Cadna-owie Formation|40910|6|Mentioned|p16|||||||||
3284|Cadna-owie Formation|40911|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|40926|3|Fully described|p16|||||||||
3284|Cadna-owie Formation|40962|6|Mentioned|Table 1|||||||||
3284|Cadna-owie Formation|41060|6|Mentioned|p2|||||||||
3284|Cadna-owie Formation|41061|6|Mentioned|Fig.6|||Generalized stratigraphy||||||
3284|Cadna-owie Formation|41063|5|Briefly described|p40|||||||||
3284|Cadna-owie Formation|41064|6|Mentioned|p60|||||||||
3284|Cadna-owie Formation|41084|5|Briefly described|p81|||||||||
3284|Cadna-owie Formation|41085|3|Fully described|p87|||||||||
3284|Cadna-owie Formation|41086|3|Fully described|p104; Fig.3|||||||||
3284|Cadna-owie Formation|41088|6|Mentioned|p140|||||||||
3284|Cadna-owie Formation|41089|6|Mentioned|p156|||||||||
3284|Cadna-owie Formation|41097|6|Mentioned|p165|||||||||
3284|Cadna-owie Formation|41098|4|Described|p175|||||||||
3284|Cadna-owie Formation|41165|5|Briefly described|p360|||||||||
3284|Cadna-owie Formation|41175|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|41176|6|Mentioned|Table 2|||||||||
3284|Cadna-owie Formation|41177|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|41179|6|Mentioned|p262|||||||||
3284|Cadna-owie Formation|41182|6|Mentioned|p287|||||||||
3284|Cadna-owie Formation|41183|6|Mentioned|p310|||||||||
3284|Cadna-owie Formation|41184|6|Mentioned|p328|||||||||
3284|Cadna-owie Formation|41186|4|Described|p212|||||||||
3284|Cadna-owie Formation|41214|6|Mentioned|p257|||||||||
3284|Cadna-owie Formation|41216|6|Mentioned|p305|||||||||
3284|Cadna-owie Formation|41219|4|Described|p347|||Mention p351.||||||03-AUG-06
3284|Cadna-owie Formation|41247|6|Mentioned|p126|||||||||
3284|Cadna-owie Formation|41266|6|Mentioned|Fig.3|||||||||
3284|Cadna-owie Formation|41361|6|Mentioned|p4|||||||||
3284|Cadna-owie Formation|41523|5|Briefly described|p271,p275|||||||||
3284|Cadna-owie Formation|41535|6|Mentioned|p368|||||||||
3284|Cadna-owie Formation|41681|6|Mentioned|p22,p3|||||||||
3284|Cadna-owie Formation|41705|6|Mentioned|p116|||||||||
3284|Cadna-owie Formation|41707|5|Briefly described|p163|||||||||
3284|Cadna-owie Formation|41712|6|Mentioned|p282|||||||||
3284|Cadna-owie Formation|41724|5|Briefly described|p382|||||||||
3284|Cadna-owie Formation|41950|5|Briefly described|Fig.2 P3|||||||||
3284|Cadna-owie Formation|42061|4|Described|Fig,11 P159|||||||||
3284|Cadna-owie Formation|42064|6|Mentioned|Fig.4 P.170|||||||||
3284|Cadna-owie Formation|42067|4|Described|Appendix 2|||||||||
3284|Cadna-owie Formation|42090|6|Mentioned|p28|||||||||
3284|Cadna-owie Formation|42283|6|Mentioned|p89|||||||||
3284|Cadna-owie Formation|42293|5|Briefly described|Fig.3 P.19|||||||||
3284|Cadna-owie Formation|42341|6|Mentioned|Fig.7 P57|||||||||
3284|Cadna-owie Formation|42346|5|Briefly described|Fig.3 P80|Jurassic||||||||
3284|Cadna-owie Formation|42375|6|Mentioned|Fig. 28 P125, Table1|Late Cretaceous|Jurassic|Eromanga Basin||||||
3284|Cadna-owie Formation|42395|5|Briefly described|Fig.13 P83|||||||||
3284|Cadna-owie Formation|42397|6|Mentioned|Fig.2 P3|||||||||
3284|Cadna-owie Formation|42429|5|Briefly described|Fig.3 P155|||||||||
3284|Cadna-owie Formation|42446|6|Mentioned|p13|||||||||
3284|Cadna-owie Formation|42447|6|Mentioned|Fig.1|||||||||
3284|Cadna-owie Formation|42465|5|Briefly described|Map Legend|||||||||
3284|Cadna-owie Formation|42469|4|Described|p31|||||||||
3284|Cadna-owie Formation|42474|6|Mentioned|p25|||||||||
3284|Cadna-owie Formation|42520|5|Briefly described|p6|||||||||
3284|Cadna-owie Formation|42602|6|Mentioned|Fig.2 p20|||||||||
3284|Cadna-owie Formation|42746|4|Described|p10|||See also Fig.6, Fig.2||||||
3284|Cadna-owie Formation|42749|5|Briefly described|p31, Fig.9 p31|||see also Fig.2 p27||||||03-AUG-06
3284|Cadna-owie Formation|42816|6|Mentioned|p18|||||||||
3284|Cadna-owie Formation|42905|5|Briefly described|p19|||see also Fig 5.3||||||
3284|Cadna-owie Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
3284|Cadna-owie Formation|43002|5|Briefly described|Fig.2,p135|||||||||
3284|Cadna-owie Formation|43004|5|Briefly described|Table 1,p179|||||||||
3284|Cadna-owie Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone and siltstone.||||||25-MAY-05
3284|Cadna-owie Formation|43071|6|Mentioned|p20|||||||||
3284|Cadna-owie Formation|43085|5|Briefly described|Fig.6|||||||||
3284|Cadna-owie Formation|43094|5|Briefly described|p36|||||||||
3284|Cadna-owie Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
3284|Cadna-owie Formation|43114|6|Mentioned|Table 2|||||||||
3284|Cadna-owie Formation|43122|5|Briefly described|p23|||see also Fig. 2.||||||
3284|Cadna-owie Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
3284|Cadna-owie Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
3284|Cadna-owie Formation|43591|6|Mentioned|p40|||||||||
3284|Cadna-owie Formation|43602|4|Described|191|||Geological Province: Eromanga Basin.||||||16-SEP-08
3284|Cadna-owie Formation|43743|6|Mentioned|Fig.2,p33||Early Cretaceous|||||||
3284|Cadna-owie Formation|43840|5|Briefly described|Fig3 p12|||Cretaceous-Jurassic age||||||12-JUL-16
3284|Cadna-owie Formation|44133|4|Described|p112, 104 Fig. 9.11|Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin. Previously named 'Transition beds'. Thickness: up to 100m.  Overlies: Murta Formation. Onlaps Algebuckina Sandstone.||||||11-NOV-13
3284|Cadna-owie Formation|44289|5|Briefly described|Map Legend||Aptian|||||||
3284|Cadna-owie Formation|44658|14|Not recorded|map legend|||Neoc.-Albian (G53-15).||||||
3284|Cadna-owie Formation|45110|6|Mentioned|p107|||||||||
3284|Cadna-owie Formation|45149|6|Mentioned|Table 1|||Page 15.||||||
3284|Cadna-owie Formation|45168|6|Mentioned|p9|||||||||
3284|Cadna-owie Formation|46791|6|Mentioned|Fig.11|||||||||
3284|Cadna-owie Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
3284|Cadna-owie Formation|46939|6|Mentioned|Fig.2|||||||||
3284|Cadna-owie Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
3284|Cadna-owie Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
3284|Cadna-owie Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Contains Wyandra Sandstone Member. Overlies Murta Formation and part of Algebuckina Sandstone; overlain by Wallumbilla Formation and Bulldog Shale. Geological Province: Eromanga Basin.||||||31-JAN-08
3284|Cadna-owie Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|60955|5|Briefly described|Map Legend|Cretaceous|Jurassic|Coarse sands and grits, ferruginous sandstones.||||||
3284|Cadna-owie Formation|61014|5|Briefly described|pp532-533, p545, p550.|Lower Cretaceous|Lower Cretaceous|Eromanga Basin. Fluvio-lacustrine conditions characterised by internal drainage and infill of large interior cratonic lakes.|||Includes Wyandra Sandstone Member.|Overlies Hooray Sandstone. Is overlain by Bulldog Shale.||
3284|Cadna-owie Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone, siltstone, calcareous sandstone and pebbly sandstone.||||||
3284|Cadna-owie Formation|61312|4|Described|p73, p64, p67 Fig.E5|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone and Warratta Sandstone Members. The top of the unit has been called "Main Datum". Shale, minor sandstone. Overlain by Wallumbilla Fm. Geol. Prov: Eromanga Basin. Equivalent in the Surat Basin is Bungil Fm.||||||
3284|Cadna-owie Formation|61560|6|Mentioned|p492||Cretaceous|During its deposition this unit was impacted by the Tookoonooka meterorite fragment(s) a large circular structure in the Mesozoic strata of the Eromanga Basin. ||||||
3284|Cadna-owie Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Includes Wyrandra Sandstone Member. Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
3284|Cadna-owie Formation|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|Misspelling of Cadna-Owie Formation.||||||14-APR-08
3284|Cadna-owie Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Murta Formation and Namur Sandstone. Is overlain by Wallumbilla Formation and Bulldog Shale.||
3284|Cadna-owie Formation|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Includes the Wyandra Sandstone Member. Geological Province: Eromanga Basin.||||||21-APR-08
3284|Cadna-owie Formation|63450|5|Briefly described|p83|Cretaceous|Jurassic |May be equivalent to the upper part of Longsight Sandstone, which was renamed Cadna-owie Formation by Mond and Harrison (1978). Overlain by Rolling Downs Group. Geological province: Georgina Basin.||||||07-FEB-11
3284|Cadna-owie Formation|63894|5|Briefly described|p169|Early Cretaceous|Jurassic|Aquifer. Overlies Algebuckina Sandstone. Underlies Bulldog Shale.||||||
3284|Cadna-owie Formation|63979|2|Defined|p46, Fig. 44|Barremian|Valanginian|Contains Mount Anna Sandstone Mbr at top (SA), Wyandra Sandstone Mbr (Qld). Informally subdivided into upper + lower Cadna-owie Fm. Overlies Algebuckina Sst.Thick: 90m.Geol.p: Eromanga Basin. Interbedded sandstone, siltstone, silty mudstone + mudstone.||||||07-FEB-11
3284|Cadna-owie Formation|64048|6|Mentioned|p64 Tb. 2|||Geological Province: Eromanga Basin.||||||07-FEB-11
3284|Cadna-owie Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Includes the Wyandra Sandstone Member.|Overlain by Bulldog Shale and Wallumbilla Formation; overlies Hooray and Algebuckina Sandstones.||10-DEC-15
3284|Cadna-owie Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Marks the transition from fluvio-lacustrine and deltaic, to paralic and marine, environments.||||Overlies Algebuckina Sandstone, Murta Formation and Hooray Sandstone.||
3284|Cadna-owie Formation|64696|5|Briefly described|p133 Fig.14|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|64778|6|Mentioned|p13|Jurassic|Jurassic|Pedirka and Simpson Desert Basins.||||||
3284|Cadna-owie Formation|64783|6|Mentioned|p85 Figs.3 and 4|||||||||15-NOV-17
3284|Cadna-owie Formation|64856|5|Briefly described|p98|||Eromanga Basin unit, laterally equivalent to the Bungil Formation.| | ||||31-JAN-13
3284|Cadna-owie Formation|65194|6|Mentioned|p46, p48|||Main aquifer in the Great Artesian Basin. Separated from Eyre Formation by clay-rich rocks of the Marree Subgroup.||||||
3284|Cadna-owie Formation|65238|5|Briefly described|p10|Early Cretaceous|Late Jurassic|See also variations on this name: Cadna Owie Formation and Cadnaowie Formation in the figures. Eromanga basin. Fine grained sandstone, siltstone and claystone with minor limestone||||||
3284|Cadna-owie Formation|65309|6|Mentioned|pp14-15. |||||||Is overlain by Algebuckina Sandstone in much of the Eromanga Basin.||
3284|Cadna-owie Formation|65342|5|Briefly described|pp9-10.|||Eromanga Basin. Max. thickness at least 59 m.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale.|Sandstone, siltstone.|
3284|Cadna-owie Formation|65374|5|Briefly described|p30||Cretaceous|||||||
3284|Cadna-owie Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Jurassic||||||Fluvial to marginal marine sandstone.|
3284|Cadna-owie Formation|65385|5|Briefly described|pS133, pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Includes Trinity Well Sandstone Member and Wyandra Sandstone Member. Overlies Algebuckina Sandstone, Murta Formation and Hooray Sandstone. Overlain by Bulldog Shale and Wallumbilla Formation.||||||08-MAR-12
3284|Cadna-owie Formation|65489|5|Briefly described|p49, p55-58, p61, p96, p155-156, p160|Early Cretaceous|Early Cretaceous|Eromanga Basin. 80m thick. Oil and gas shows. Regional sand sheet with good to excellent reservoir quality. Intraformational siltstone  seal.||||Overlies Murta Formation. Is overlain by Bulldog Shale or Wallumbilla Formation.||
3284|Cadna-owie Formation|65925|5|Briefly described|p20, p57, Appendix 2.|Cretaceous|Cretaceous|Frome Embayment, Eromanga Basin. Equivalent to Mount Anna Sandstone and Parabarana Sandstone. Discharge area for GAB aquifer via diffuse upwards leakage and mound springs.||||Is overlain by Bulldog Shale.|Sandstone, siltstone and carbonaceous claystone; minor conglomerate.|
3284|Cadna-owie Formation|66303|5|Briefly described|pp27-28.|Early Cretaceous|Early Cretaceous|Stratigraphically equivalent to Parabarana Sandstone. A thin, fine-grained unit widely recognised in Eromanga Basin. Correlated with Foraminisporis wonthaggiensis spore-pollen zone.|||Includes Livingston Tillite Member.|Is overlain by Bulldog Shale.|Pale grey siltstone and fine-grained sandstone, with minor carbonaceous claystone intervals; local diamictites, pebbles and coarse breccia layers.|
3284|Cadna-owie Formation|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||||Is overlain by Bulldog Shale. Age-equivalent to Parabarana Sandstone in the northern Eromanga Basin.|Sands and silts.|06-FEB-14
3284|Cadna-owie Formation|66520|5|Briefly described|p11-12. |Cretaceous|Cretaceous|Gawler Craton. 18 m thick.|||||Feldspathic sandstone.|
3284|Cadna-owie Formation|66529|5|Briefly described|p10, p12 Fig.5, p16 |||Eromanga Basin. Appears on p16 as (Cadna-owie and Hooray Sandstones).|||Includes Wyandra Sandstone Member.|Overlies Hooray, Algebuckina and Murta Sandstones. Is overlain by Neales River and Rolling Downs Groups.|Marine sandstone.|
3284|Cadna-owie Formation|66623|3|Fully described|p102, pp238-245, pp250-255. |Early Cretaceous|Early Cretaceous|Preferential weathering of the dominant calcareous and fine-grained lithologies results in largely sandstone outcrops. Thickness varies to 260 m but this may include Murta Formation. Contains a wide range of fossils. Deposited in a variety of environments. Hosts glacial dropstones. Equivalent to top of Gum Vale Beds and lower Wittabrenna Beds, and to Pelican Well and Bungil Formations.||In SA, unit in Neales River Group.|Includes Wyandra Sandstone Member.|Overlies Namur Sandstone and Murta Formation; locally incised into Algebuckina Sandstone. Is disconformably overlain by Doncaster Membr (Wallumbilla Formation). Is overlain by Marree Formation in SA.|Erosion-resistant calcareous sandstone and siltstone; subordinate weathered grey shale and siltstone; minor pebbly sandstone and conglomerate.|11-NOV-13
3284|Cadna-owie Formation|66915|5|Briefly described|p4-6, p9, p11 Fig.7|Cretaceous|Cretaceous|Eromanga Basin. The "C-Horizon" is often referred to as "top Cadna-owie Formation". A readjustment of terminology is required, therefore it is better to understand the "C-Horizon" to represent "Base Wallumbilla" rather than "top Cadna-owie", or "top Bungil" or "top Gilbert River" or top whatever other unit underlies the Wallumbilla Formation in that area. See also Wallumbilla Formation.|||Wyandra Sandstone Member at top|Is overlain by Wallumbilla Formation.||12-JAN-17
3284|Cadna-owie Formation|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous rocks are mapped separately.|||Includes Wyandra Sandstone.||Marine, calcareous sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones; ferruginous calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|66922|5|Briefly described|Map legend|Cretaceous|Cretaceous|Includes three un-named but separately mapped sub-units.|||Includes Wyandra Sandstone.||Marine, calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Sandstone, fine-grained, with coarse-grained sandstone beds, and pale grey siltstone, minor conglomerate.|18-NOV-14
3284|Cadna-owie Formation|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones; local pebbly sandstone and conglomerate interbeds and ferruginous, calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.|Overlies Namur Sandstone. Is overlain by Doncaster Member of Rolling Downs Group.|Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shales and siltstones.|
3284|Cadna-owie Formation|67323|5|Briefly described|p87, p93 Fig.12.3, p95|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member.|Overlies Hooray Sandstone. Is overlain by Wallumbilla Formation.||
3284|Cadna-owie Formation|67402|4|Described|p26 tbl RRM4, p43 tbl HPB1, p106|Aptian|Valanginian|Eromanga Basin. Deposited in a paralic or shallow marine environment. Maximum thickness of 10m. See also  p108 fig ERO4, p108-p110, p111 fig ERO8, p113 fig ERO12, p114 fig ERO13, p115.|||Includes the Wyandra Sandstone Member.|Overlies the Lower Cadna-owie Formation and the Hooray Sandstone. Overlain by the Wallumbilla Formation.|Upwards coarsening sequence of interbedded sandstone, siltstone and mudstone.|
3284|Cadna-owie Formation|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale.||
3284|Cadna-owie Formation|67784|5|Briefly described|p25-26|Aptian|Neocomian|Northern Eromanga Basin.||||Is overlain by Doncaster Member (Wallumbilla Formation).|Sandstone|08-FEB-18
3284|Cadna-owie Formation|68068|6|Mentioned|Map legend|||Time equivalent to the Parabarana Sandstone to the south.||||||18-NOV-14
3284|Cadna-owie Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Jurassic|Fluvial to marginal marine deposits. Mapped with Algebuckina Sandstone as one unit.|||||Sandstone.|
3284|Cadna-owie Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.|Includes the Trinity Well Sandstone Member.|||
3284|Cadna-owie Formation|68715|6|Mentioned|p30 Fig.5|Barremian|Valanginian|Eromanga Basin.||||||
3284|Cadna-owie Formation|68734|6|Mentioned|p218 Fig.2|||Eromanga Basin (SW and NE). Fluvial to shallow marine. Pre-Barremian age.||||||16-JAN-17
3284|Cadna-owie Formation|68821|5|Briefly described|p292 Fig.1, p295, p297 Fig.3|Cretaceous|Cretaceous|Eromanga Basin. Lower Cretaceous age. Fluvial-paralic. Equivalent to the Bungil Formation. Contains diamictite deposits at its base.|||||Comprises quartz rich sandstones and conglomerates.|
3284|Cadna-owie Formation|69001|5|Briefly described|p2 Fig.1B, p11, pp16-18, pp35-37, p63|Early Cretaceous|Early Cretaceous|Terrestrial to marine transition sediments. Of the Eromanga Basin. Calcite induration is common (but not diagnostic) in parts of weathered Cadna-owie Formation. Includes locally defined units by McMinn (1981b) and/or Morton (1982) such as the Gum Vale Beds or Gum Vale Formation.||||Equivalent to the Algebuckina Sandstone and the Gum Vale Beds.|Comprises sandstones, siltstones, and some conglomerate.|
3284|Cadna-owie Formation|69019|3|Fully described|p56-57 Pl.9, p85, p87-91, p168.|Aptian|Valanginian|Eromanga Basin. Of Freytag et al. (1967) and Wopfner et al. (1970); formerly 'Transition Beds' of Whitehouse (1955). Type section in ~3 km WSW of Algebuckina Hill. Often associated with ferricrete capping. A significant regional aquifer.||Unit in Neales River Group.|Includes Mount Anna Sandstone Member, Livingston Tillite Member and Trinity Well Sandstone Member.|Overlies Murta Formation and Algebuckina Sandstone; Bunyeroo Formation unconformably. Is equivalent to Parabarana Sandstone. Is overlain by Bulldog Shale gradationally and by Wallumbilla Formation.|Grey siltstone coarsening upwards into fine- to medium-grained sandstone; sandstone interbeds commonly calcitic; near basal siltstone commonly carbonaceous; locally a basal pebbly interval; contains exotic lonestones to 1 m.|
3284|Cadna-owie Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p90, p92-95|Aptian|Valanginian|See also p99, p101, p191-192. Freytag et al. (1967) and Wopfner et al. (1970); previously the Transition Beds of Whitehouse (1955). Contrasts with Parabarana Sandstone are discussed. Thickness to c.69m. Stratigraphic wells intersection data.||||Overlies Murta Formation. Is overlain conformably by Bulldog Shale (Marree Subgroup).|Contains fossil ice-wedges.|
3284|Cadna-owie Formation|69203|6|Mentioned|p12|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|69454|5|Briefly described|p38:3, 13, 14 Fig.38.9|Cretaceous|Cretaceous|Eromanga Basin. Potential hydrocarbon trap, either by sealing Algebuckina Sandstone reservoirs or by having its own sandstone reservoirs sealed by the Wallumbilla Formation shales.||||||12-JUL-16
3284|Cadna-owie Formation|69457|3|Fully described|p41:2-3, 5-9, 16|Early Cretaceous|Early Cretaceous|Wopfner et al. (1970). Equivalent to the Transition beds of Whitehouse (1955). Eromanga Basin. Lacustrine to restricted/marginal marine, minor fluviatile and subtidal shallow marine deposits. 81m thick (>100m in Cooper Basin). Possibly equivalent to the upper part of De Souza Sandstone. Late Valanginian to early Aptian age from dinocysts and acritarchs. Hydrocarbon source potential is briefly discussed. May form a seal for underlying Algebuckina Sandstone reservoirs, and its own shoreline sandstone reservoirs in the NT may be sealed by the Wallumbilla Formation.|||Includes Mount Anna, Trinity Well, Wyandra, Sandstone Members.|Conformably overlies Algebuckina and Hooray Sandstones and Murta Formation. Is overlain conformably by Bulldog Shale and Wallumbilla Formation. Lateral equivalent of Wallumbilla Formation.|Thinly to thickly interbedded sandstone, siltstone, silty mudstone and mudstone; minor claystone. Parallel bedding and coarsening-upwards intervals typical. Local pebble layers, diamictites and coarse breccia layers.|23-JAN-19
3284|Cadna-owie Formation|69554|6|Mentioned|p131|Cretaceous|Cretaceous|Northern Gawler Craton.||||||
3284|Cadna-owie Formation|69562|6|Mentioned|p666 Fig.3, p667 Fig.4, p668|Cretaceous|Cretaceous|||||||
3284|Cadna-owie Formation|69568|6|Mentioned|p443|Cretaceous|Cretaceous|Lake Frome region, Eromanga Basin. A transitional depositional environment from terrestrial to marine.|||||Fine-grained, pale grey siltstone and sandstone with minor carbonaceous claystone intervals.|
3284|Cadna-owie Formation|69582|6|Mentioned|p65|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies the Hooray Sandstone. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|69594|4|Described|p519, p526-528, p532-533, p538, p573|Barremian|Valanginian|Wopfner et al. (1970). Eromanga Basin. Subsurface. 60-90m thick. Paralic to shallow-marine deposits. Is a minor hydrocarbon reservoir. An important, shallow aquifer.|||Wyandra Sandstone Member.|Overlies Murta Formation and Hooray Sandstone transitionally. Is overlain by Doncaster Member (Wallumbilla Formation). Lateral equivalent to Bungil Formation.|Lower part consists of silty mudstone, siltstone and lithic to quartzose and sublabile sandstone with the proportion of sandstone increasing upwards; the upper part is mainly sublabile to lithic sandstone with minor siltstone near the top.|
3284|Cadna-owie Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
3284|Cadna-owie Formation|69673|5|Briefly described|p154, p155 fig 127, p159, p161 fig 131|Cretaceous|Cretaceous|Age derived from Palynoflora. Some source potential for oil and gas.|||Includes Mount Anna Sandstone Member, Wyandra Sandstone Member, Murta Member|Overlies Murta Formation, Algebuckina Sandstone, overlain by Wallumbilla Formation|Thinly to thickly interbedded sandstone, siltstone, silty mudstone and mudstone, minor claystone typically with parallel bedding and upwards coarsening intervals.|
3284|Cadna-owie Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Eromanga Basin.||||||
3284|Cadna-owie Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.|||Includes Wyandra Sandstone Member.|||23-JAN-19
3284|Cadna-owie Formation|69946|2|Defined|p17, p19-20, p44, p56-58, p94, p96-98|Early Cretaceous|Early Cretaceous|Wopfner et al. (1970), for the mappable interval between Algebuckina Sandstone and Bulldog Shale. Previously the Transition beds of Whitehouse (1955), for a unit that records the transition from terrestrial to marine conditions. Eromanga Basin. Type section is Big Cadna-owie Spring, 5.5km SSW of Mount Dutton. Upper boundary is strongly diachronous, younging towards the Basin margin. Typically 10-20m thick, to a maximum of >115m. Includes marine and non-marine fossils. Wireline log correlations. Lateral equivalent of Village Well and Pelican Well Formations and Parabarana Sandstone.|||Includes Wyandra, Mount Anna and Trinity Well, Sandstone Members.|Overlies Murta Formation gradationally and Algebuckina Sandstone. Is overlain conformably by Bulldog Shale or Wallumbilla Formation. See Comments.|Subsurface: pale grey siltstone with very fine- to fine-grained sandstone interbeds and minor carbonaceous claystone; pebbly layers, diamictites and coarse breccia layers around the Basin margin. Outcrop: minor calcareous sandstone beds with ooids.|
3284|Cadna-owie Formation|69947|5|Briefly described|p8-9, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|See also p31 Fig.7.20. Eromanga Basin. Marks transition from terrestrial to marine deposition.|||Wyandra Sandstone Member.|Conformably overlies Murta Formation. Is overlain by Bulldog Shale and Wallumbilla Formation.|Mudstone, siltstone, sandstone.|
3284|Cadna-owie Formation|69948|6|Mentioned|p4; Figs.4.1-2, 13-20|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin). Seismic sections across the Gidgealpa, Dullingari, Poolowanna and Big Lake Fields, and other structures.||||Overlies Murta Formation or Algebuckina Sandstone. Is overlain by Bulldog Shale or Wallumbilla Formation.||
3284|Cadna-owie Formation|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Fine-grained sandstone with coarse-grained sandstone beds and pale grey siltstone; minor conglomerate.|
3284|Cadna-owie Formation|70383|5|Briefly described|p45, p52|Early Cretaceous|Berriasian|Transgressive, marginal marine deposits. Maximum age from age of Sprigg Diamictite Member.|||Includes Sprigg Diamictite Member, Livingston Tillite Member.|Overlies Algebuckina Sandstone. Equivalent to Parabarana Sandstone.||15-JAN-19
3284|Cadna-owie Formation|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin. This unit is the distal Basin-wide equivalent to the rangelands-proximal Parabarana Sandstone. Age shown more specifically as Neocomian to Aptian.||Of Neales River Group.|Includes Livingston Tillite, Sprigg Diamictite, Trinity Well Sandstone, Members.|Equivalent to Parabarana Sandstone.|Mostly subsurface: yellow-brown, fine-grained, calcitic quartz sandstone; coarse-grained buff-yellow gritstone lenses; lower zone more silty, grey, carbonaceous. Sandy beds usually ferruginous, locally gravelly or bouldery.|23-JAN-19
3284|Cadna-owie Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes un-named unit, Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shale and siltstone. Un-named unit is ferruginous, calcareous sandstone and mudstone.|
3284|Cadna-owie Formation|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.|||Includes Wyandra Sandstone Member.||Marine calcareous, sub-labile to quartzose sandstone and siltstone interbedded with grey shale and siltstone.|
3284|Cadna-owie Formation|70789|5|Briefly described|p318, p320 Fig.4, p328|Early Cretaceous|Early Cretaceous|Eromanga Basin. Transgressive, fluvial to marginal marine deposits. Consistent thickness of 50-80m. A major aquifer in the Basin.||||Is overlain by Bulldog Shale.|Sandstones and siltstones.|
3284|Cadna-owie Formation|70821|4|Described|p21-22, p32-33, p72, p80, p82, p86|Early Cretaceous|Early Cretaceous|Eromanga Basin. Poorly expressed or unrecognised in the southern Thomson region. Late Valanginian-Early Aptian acritarchs and dinoflagellates indicate fresh to brackish water, lacustrine to restricted, marginal marine environments. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Hydrostratigraphic properties.|||Includes Wyandra Sandstone Member.|Overlies Algebuckina, Namur, Hooray (unconformably), Mooga Sandstones and Crowl Creek Formation. Is overlain by Bulldog Shale and Wallumbilla Formation.|Fairly well-bedded siltstone, fine to medium lithic sandstone and intraformational conglomerate; thin coaly layers, dark mudstone and layers of kaolin-like material, possibly altered tuff are also present. Volcanogenic components increase up-section.|23-JAN-19
3284|Cadna-owie Formation|70823|5|Briefly described|p41, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also Cadnowie Formation [which is a mis-spelling of this formation]. Age is a minimum depositional age.|c. 126 Ma|||Overlies the Murta Formation. Overlain by the Wallumbilla Formation and the Bulldog Shale.||
3284|Cadna-owie Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Murta Formation and the Hooray and Namur Sandstones. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.|Mount Anna Sandstone Member.|||
3284|Cadna-owie Formation|71043|5|Briefly described|p106|||Gawler Craton.|||||Shale, minor sandstone.|
3284|Cadna-owie Formation|71251|5|Briefly described|p7-8, p11, p15, p17, p19-20, p29, p49|||Eromanga Basin. 65m total thickness in Eulo 1 borehole. Natural gamma, magnetic susceptibility data tabulated. Conductivity diagrams.|||Wyandra Sandstone Member.|Overlies Hooray Sandstone or (where that unit is absent) Nebine Metamorphics. Is overlain by Wallumbilla Formation.|Fine quartzose sandstone, and dark grey mudstone with carbonaceous flecks; basal conglomerate composed of quartz and basement lithic fragments.|
3284|Cadna-owie Formation|71321|4|Described|p1,15,24-28,65|Early Aptian|Valanginian|Of Eromanga Basin. Deposited under shallow-water, marginal marine conditions. Marks the onset of Early Cretaceous marine transgression (Alexander, et al., 2006; Krieg, et al., 1995; Wopfner, et al., 1970) i.e. westward transgression of a marine epicontinental seaway (Keireg et al., 1995). Paleontological data indicate Valanginian to early Aptian age (Krieg, et al., 1995). Traditionally difficult to differentiate Cadna-owie Formation from the underlying Algebuckina Formation in the TIEYON area, and included as part of Algebuckina Formation in the TIEYON area.||||Conformably underlain by Algebuckina Sandstone. Underlain by the Murta Formation.|Outcrop: Fine- to medium-grained, quartzose sandstones, minor mica, feldspar, heavy minerals, pyrite; glauconite, calcareous beds with ooids. Subsurface: pale grey siltstone with fine-grained sandstone interbeds and minor carbonaceous claystones.|24-OCT-19
3284|Cadna-owie Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p4, Ch4 p8-p9|Aptian|Valanginian|Eromanga Basin. This unit was first named the Transition beds by Whitehouse (1955) as it records the transition from terrestrial to marine conditions. This name was first assigned by Wopfner et al (1970) to the mappable interval between the Algebuckina Sandstone and the Bulldog Shale. This units type section is located at Big Cadna-owie Spring and was defined by Wopfner et al., 1970. Hosts a major confined aquifer. Petrography is discussed. This unit is typically 10-20m thick around the basin margin, increasing to 75-100m in the deeper parts of the basin and reaches a maximum thickness in excess of 115m in the Nappamerri Trough. Age based on palynology. This unit is interpreted to have been deposited in shoreface and beach environments and members have been interpreted to have been deposited in fluviodeltaic environments. Sedimentary characteristics are discussed. Spore-pollen zone is given in Ch5 p57. Thermal history briefly described in Ch9.. Laterally equivalent to the Pelican Well Formation and the Parabarana Sandstone.See also Ch4 p20-p27, Ch5 p12, Ch5 p19-p21, Ch5 p24, Ch5 p30, Ch5 p32, Ch5 p38, Ch5 p56-p58, Ch5 p97-p99, Ch6 p7-p8, Ch7 p8-p9, Ch7 p11, Ch7 p13, Ch8 p6, Ch8 p10, Ch8 p23-p24, Ch9 p7, Ch9 p12, Ch9 p18, Ch9 p21, Ch9 p23, Ch10 tbl 10.1, Ch10 p8, Ch10 p17-p20, Ch11 p2, Ch11 p4-p5, Ch12 p12-p14, Ch13 p2, Ch13 p4, Ch13 p8-p9, Ch14 p5.|||Includes the Wyandra Sandstone Member, Mount Anna Sandstone Member, Trinity Well Sandstone Member and the Livingston Tillite Member.|Conformably overlies the Murta Formation. Unconformably overlies the Mount Toondina Formation. Overlies the Algebuckina Sandstone. Overlain by the Bulldog Shale and the Wallumbilla Formation.|Pale grey siltstone with very fine to fine-grained sandstone interbeds and minor carbonaceous claystone. Pebbly layers, diamictites and coarse breccia also occurs.|
3284|Cadna-owie Formation|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
3284|Cadna-owie Formation|71415|5|Briefly described|p11-14|Valanginian|Valanginian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Terrestrial to marine transition sediments (Exon and Senior 1976). LA-ICPMS zircon age populations dominated by Neoproterozoic to Cambrian c. 600 to 316 Ma, and subordiante Mesoproterozoic c. 1300-250 Ma.||||Overlain by Rolling Downs Group. Underlain by Namur Sandstone.||19-AUG-19
3284|Cadna-owie Formation|71863|5|Briefly described|p5|Aptian|Valanginian|Eromanga Basin.|||Includes the Wyandra Sandstone Member.|Overlies the Murta Formation and the Hooray Sandstone. Overlain by the Wallumbilla Formation.||
3284|Cadna-owie Formation|71864|6|Mentioned|p14, p17||||||Includes the Wyandra Sandstone Member.|||
3284|Cadna-owie Formation|72297|6|Mentioned|p742|||Eromanga Basin. Petroleum reservoir.||||||
3284|Cadna-owie Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW). Upper part: main confined aquifers, generally producing flowing artesian water bores.||Neales River Group.|Wyandra Sandstone Member.|Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale or Wallumbilla FZ.||
3284|Cadna-owie Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Sandstone, fine-grained, with coarse-grained sandstone beds, and pale grey siltstone, minor conglomerate.|
3284|Cadna-owie Formation|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
3284|Cadna-owie Formation|72478|5|Briefly described|p6, p8-p10, p12, p25-26,|Early Cretaceous|Early Cretaceous|Eromanga Basin. Represents a marine transgressive phase. See also p51, Fig.7 p70, p72-74, p82-83 [of the document], where described as Cadnaowie sandstone, Cadnaowie sands, Cadnaowie Formation.|c. 130-114 Ma|||Underlies the Bulldog Shale. Unconformably overlies the Algebuckina Sandstone.|Grey sandstone, fine to very-fine sandstone with locally developed coarse sandstone interbeds and carbonaceous claystones.|29-MAR-21
3284|Cadna-owie Formation|72915|6|Mentioned|p27||||||Wyandra Sandstone Member|||
3284|Cadna-owie Formation|72921|6|Mentioned|p16.|||Interpreted as correlative with a variety of units across the Clarence-Moreton, Surat and Eromanga Basins. [All the other units named are Jurassic, and most don't correlate with each other so there is some confusion about the intended meaning here]||||||
3284|Cadna-owie Formation|73090|5|Briefly described|Appendix.|Cretaceous|Cretaceous||||||Sandstone, fine-grained, with coarse-grained sandstone beds and pale grey siltstone, minor conglomerate.|
3284|Cadna-owie Formation|73099|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga basin.||Marree Subgroup.||Overlies Algebuckina Sandstone conformably and Mount Toondina Formation unconformably.|Ferruginised or kaolinised gritty quartz sandstone; fossil wood.|
3284|Cadna-owie Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member|||
3284|Cadna-owie Formation|73203|6|Mentioned|p651-652|Early Cretaceous|Early Cretaceous|[Also misspelt as Cadna-Owie Formation]. A major aquifer host across the Great Artesian Basin. Found in the Jundah 1 well, central Queensland.||||||
3284|Cadna-owie Formation|73249|4|Described|p316-319, p320 Fig.2, p321-338|Barremian|Valanginian|Eromanga Basin. Minimum age of early Barremian. Depositional environments transition from continental (fluvio-deltaic to tidal) to shallow marine, period of marine transgression. Typically 60m thick, can be 10m thick at basin margins and up to 115m thick in the Nappamerri Trough. Dominant mineral phases are kaolinite and quartz, montmorillonite is also present. Deposited in a cold continental, humid climate. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks from the west and south. [Locations in text include p321 Tb.1 and p324 Fig.4.]|||Mount Anna Sandstone Member|Conformably underlies the Bulldog Shale.|Siltstone with interbedded sandstone and mudstone, sandstone dominated with lesser clay-rich horizons, typically 60m thick.|
3284|Cadna-owie Formation|73251|5|Briefly described|p:36-37, 40, 43, 48-50, 52-54, 56-57, 62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Potential hydrocarbon reservoir and fairway. Contains hydrocarbon accumulations to which the Murta Formation contributed. Non-marine to marginal marine depositional setting. Contains Bulldog [organic] facies 1 [see article].|||Wyandra Sandstone Member|Underlain by Murta Formation and Namur Sandstone. Overlain by Bulldog Shale and Wallumbilla Formation. Equivalent to Parabarana Sandstone.||
3284|Cadna-owie Formation|73281|6|Mentioned|Appendix (DIP)|||Cadna-owie Formation reinterpreted as Cadna-Owie Formation [to indicate capitalisation of both components is considered preferable in this work?]. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
3284|Cadna-owie Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.|||Wyandra Sandstone Member|Underlain by Namur Sandstone and Murta Member. Overlain by Bulldog Shale and Wallumbilla Formation.||
3284|Cadna-owie Formation|73398|5|Briefly described|p1-5, 7-8, 10-11, 13, 16, 19, 21-30|Early Cretaceous|Early Cretaceous|Eromanga Basin. Overlying the Prominent Hill IOCG deposit, this unit contains up to c.5000 ppm Cu; the authors conclude this was due to transport/deposition of mineralised sediments from underlying mineralised rock. Continental fluvial environment. One of the largest confined aquifers in the Great Australian Basin. Geochemistry, weathering analysed in great detail.|140-125 Ma.|||Unconformably overlies Boorthanna Formation. Is overlain conformably by Bulldog Shale.|Interbedded sandstone, siltstone and mudstone.|
3284|Cadna-owie Formation|73479|5|Briefly described|p156 Fig.2, p159, p164 Fig.7, p165-166|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-shallow marine depositional environment. See also p175.|ca 140-126 Ma||Wyandra Sandstone Member|Overlies Namur Sandstone, Murta Member, underlies Wyandra Sandstone Member, Bulldog Shale||
3296|Cadumble Formation|24126|5|Briefly described|p158|||||||||
3296|Cadumble Formation|29993|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
3296|Cadumble Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
3296|Cadumble Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
3296|Cadumble Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
3296|Cadumble Formation|39654|6|Mentioned|M85|||||||||
3296|Cadumble Formation|39663|6|Mentioned|Table 1|||See also Table 6||||||
3296|Cadumble Formation|40328|6|Mentioned|p85|||||||||
3296|Cadumble Formation|40882|5|Briefly described|p22|||Mention P27 and Fig.1||||||
3296|Cadumble Formation|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
3304|Caladenia Limestone Member|23309|6|Mentioned|p86|||||Towanga Sandstone||||31-OCT-14
3304|Caladenia Limestone Member|23710|5|Briefly described|p70|||||||||
3304|Caladenia Limestone Member|37727|6|Mentioned|p49|||||||||
3304|Caladenia Limestone Member|39447|6|Mentioned|p9|||||||||
3304|Caladenia Limestone Member|40328|6|Mentioned|p70|||||Towanga Formation||||23-DEC-14
3310|Calarie Sandstone|22831|4|Described|p44|Pridolian|Wenlockian|Derriwong Group||||||01-NOV-13
3310|Calarie Sandstone|22857|4|Described|p450 App.1, Tb.A1.6|Pridolian|Pridolian|Of the Derriwong Group. Lateral equivalent of Edols Conglomerate. Max. thickness: ~30m. Geological Province: Bogan Gate Terrace.||||||
3310|Calarie Sandstone|23522|5|Briefly described|p253|Devonian|Devonian|||||||
3310|Calarie Sandstone|24417|3|Fully described|p69|Pridoli|Ludlow|Of Derriwong Group. Originally included in the Forbes Group (Sherwin, 1973b) and the "Wallingalair Group" (Krynen et al, 1990).  Includes a mappable, but unnamed, fine sandstone bed. Overlain by Cookeys Plains Formation.  Max. thickness: 300m.||||||
3310|Calarie Sandstone|31722|6|Mentioned|p137|||See also Fig. 2||||||
3310|Calarie Sandstone|33118|5|Briefly described|p1|||M.-U. Sil. Forbes Gp.||||||
3310|Calarie Sandstone|33121|3|Fully described|p72|||Middle-Late Sil. See also Figs. 8, 11 & P52.||||||
3310|Calarie Sandstone|33124|6|Mentioned|Fig.2|||Section||||||
3310|Calarie Sandstone|37727|4|Described|p59|||||||||
3310|Calarie Sandstone|39214|5|Briefly described|p18|||||||||
3310|Calarie Sandstone|39618|6|Mentioned|Fig.7|||||||||
3310|Calarie Sandstone|40328|6|Mentioned|p39|||||||||
3310|Calarie Sandstone|40891|3|Fully described|p20|||||||||
3310|Calarie Sandstone|42489|5|Briefly described|Map legend|Pridoli||||||||
3310|Calarie Sandstone|43441|5|Briefly described|26|Early Devonian|Late Silurian|||||||08-JAN-10
3310|Calarie Sandstone|44160|5|Briefly described|Map Legend||Pridolian|||||||08-JAN-10
3310|Calarie Sandstone|46522|3|Fully described|p65|||||||||
3310|Calarie Sandstone|46525|6|Mentioned|p149|||||||||
3310|Calarie Sandstone|46528|5|Briefly described|Map legend|Early Devonian||||||||
3310|Calarie Sandstone|50299|5|Briefly described|Map Legend|Devonian|Silurian|Of the Derriwong Group.  Underlies: Cookeys Plains Formation.||||||
3310|Calarie Sandstone|60009|5|Briefly described|Map Legend|Pridoli|Pridoli|Of the Derriwong Group.||||||13-JUL-04
3310|Calarie Sandstone|67847|5|Briefly described|p24|Pridoli|Pridoli|||Derriwong Group||Unconformably overlies the Mumbidgle Formation.||
3322|Calivil Formation|2967|4|Described|p14, p15 Fig.2.2, p17-20, 22-23, 26-37|Pliocene|Miocene|Macumber (1973). Eastern Murray Basin. The type section is from 77m to 95m in the Mines Department Calivil No. 2 bore. Locally, these sediments occupy valleys incised into Renmark Group units. A main regional aquifer (semi-confined). Misprinted as Cavil Formation twice on p110. Hydrochemistry (""salinity"") detailed. See also p40-41, 43, 45-46, 77-88, 90-91, 93-97, 101-102, 105, 108-113, 117, 128, 132, 135, 137, 139-152, 155, 178, 181, 336-337.||Wunghnu Group.||Is separated from the underlying Olney Formation (Renmark Group) by the Mologa Surface. Is overlain by Shepparton Formation, Parilla Sand and Yando Clay.|Valley-fill, fluviatile coarse-grained quartz gravel, pebbles.|
3322|Calivil Formation|10010|5|Briefly described|p12 Fig. 3, p17|Early Pliocene|Late Miocene|Of Wunghnu Group. Overlies upper part of Renmark Group. Grades upwards into Shepparton and Coonambidgal Formations. Geological Province: Murray Basin. Considered to be fluvial counterpart of Loxton-Parilla Sands.||||||13-AUG-07
3322|Calivil Formation|22756|3|Fully described|P13, P31||Tertiary|||||||
3322|Calivil Formation|22773|5|Briefly described|Fig24.8p352,354|||||||||
3322|Calivil Formation|22782|6|Mentioned|p15|||||||||
3322|Calivil Formation|22857|5|Briefly described|p352-3 Figs. 24.8 and 24.9, p354|Early Pliocene|Early Pliocene|Of the Wunghnu Group. A porous fluvio-lacustrine unit that is an important basin-wide aquifer. At the margins of the basin this unit contains conglomerate as well as sands. Geological Province: Murray Basin.||||||09-OCT-08
3322|Calivil Formation|22886|5|Briefly described|p36|Early Pliocene|Late Miocene|||||||
3322|Calivil Formation|22887|2|Defined|p34, Fig.6 p13|Pliocene|Late Miocene|||||||
3322|Calivil Formation|22893|3|Fully described|p29 fig9 table3|Pliocene|Late Miocene|||||||
3322|Calivil Formation|22971|4|Described|p26, p27|||Max. thickness: <25m. Geological Province: Murray Basin.||||||19-JAN-06
3322|Calivil Formation|23089|5|Briefly described|p649|||||||||
3322|Calivil Formation|23164|4|Described|p15|Oligocene|Eocene|||||||
3322|Calivil Formation|23252|5|Briefly described|Map Legend|||||||||11-JAN-10
3322|Calivil Formation|23300|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23302|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23303|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23304|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
3322|Calivil Formation|23305|4|Described|p52|||Of Macumber (1972). Overlain by Newer Volcanics. Geological Province: Lachlan Fold Belt. Max. thickness: 4 m.||||||09-OCT-08
3322|Calivil Formation|23884|5|Briefly described|p153, p155 Fig.13.2|||Geological Province: Murray Basin. Of the Wunghnu Group.||||||28-APR-05
3322|Calivil Formation|23921|4|Described|p1109, p1114|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
3322|Calivil Formation|24043|5|Briefly described|p525|Pliocene|Pliocene|||||||
3322|Calivil Formation|24103|5|Briefly described|p139 Fig.3, p143 Fig.6|Tertiary|Tertiary|Middle Tertiary.||||||
3322|Calivil Formation|24105|5|Briefly described|p155|Miocene|Miocene|||||||
3322|Calivil Formation|24106|5|Briefly described|p185|Pliocene|Late Miocene|||||||
3322|Calivil Formation|24107|6|Mentioned|p224|||||||||
3322|Calivil Formation|24108|5|Briefly described|p242|Pliocene|Late Miocene|Geological Province: Murray Basin. Overlying Unit: Shepparton Formation.||||||
3322|Calivil Formation|24177|3|Fully described|p71|Late Miocene|Late Eocene|Interfingers with Parilla Sand. Overlies the Renmark Group. Overlain by the Newer Volcanics and Shepparton Volcanics. Interpretation of age varies. Geological Province: Murray Basin.||||||
3322|Calivil Formation|24219|5|Briefly described|p870|||||||||
3322|Calivil Formation|24232|5|Briefly described|p227, p231|Tertiary|Tertiary|||||||
3322|Calivil Formation|24328|5|Briefly described|Map legend|Neogene|Neogene|||||||
3322|Calivil Formation|24329|5|Briefly described|Map legend|Neogene|Neogene|||||||
3322|Calivil Formation|24383|4|Described|p10, 18|Pliocene|Oligocene|Age: 40 - 5Ma. Overlying Unit: Newer Volcanic Group. Underlying Unit: Castlemaine Group. Underlain by  White Hills Gravel, which provided source material for Calivil Formation. Geological Province: Lachlan Fold Belt||||||07-JUL-20
3322|Calivil Formation|24384|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24385|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24386|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate||||||
3322|Calivil Formation|24387|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate.||||||
3322|Calivil Formation|24388|5|Briefly described|Map legend|Eocene|Eocene|Quartz cobble conglomerate; nonmagnetic.||||||
3322|Calivil Formation|24439|5|Briefly described|p8, p23|||See also p9 Fig. 3. Author disputes presence of this unit in BENDIGO as defined by Macumber (1991) - see p. 37.  Fluvial deposits.||||||14-SEP-05
3322|Calivil Formation|24440|5|Briefly described|Map legend|||||||||
3322|Calivil Formation|24551|5|Briefly described|p322, 321, 421, 543|||Of the Murray Group.  Max thickness: 50m.||||||
3322|Calivil Formation|31713|6|Mentioned|p16|||||||||
3322|Calivil Formation|31746|6|Mentioned|p197|||In reference to Macumber (1972).||||||25-JUN-13
3322|Calivil Formation|31951|3|Fully described|p7|||||||||
3322|Calivil Formation|31953|6|Mentioned|p9|||||||||
3322|Calivil Formation|32232|6|Mentioned|p19|||||||||
3322|Calivil Formation|34735|6|Mentioned|p30|||||||||
3322|Calivil Formation|34757|6|Mentioned|p45|||||||||
3322|Calivil Formation|34813|5|Briefly described|p63|||Also mentioned on P62||||||
3322|Calivil Formation|35091|4|Described|p8|||Also p29.||||||07-JUL-20
3322|Calivil Formation|35172|4|Described|p127|||||||||
3322|Calivil Formation|35187|6|Mentioned|Table1|||||||||
3322|Calivil Formation|35242|6|Mentioned|p94|||||||||
3322|Calivil Formation|39329|6|Mentioned|p483|||||||||
3322|Calivil Formation|39330|6|Mentioned|p487|||||||||
3322|Calivil Formation|39446|6|Mentioned|p49|||||||||
3322|Calivil Formation|39967|6|Mentioned|p41|||||||||
3322|Calivil Formation|40520|6|Mentioned|Fig.5|||||||||
3322|Calivil Formation|40599|5|Briefly described|p19|||||||||
3322|Calivil Formation|40664|6|Mentioned|p248|||||||||
3322|Calivil Formation|40820|6|Mentioned|Fig.4|||||||||
3322|Calivil Formation|41068|5|Briefly described|p67|||||||||
3322|Calivil Formation|41765|4|Described|p36|||||||||
3322|Calivil Formation|41868|5|Briefly described|p551|||||||||
3322|Calivil Formation|42125|5|Briefly described|p137|||See also Fig.5||||||
3322|Calivil Formation|42126|6|Mentioned|p149,p151|||||||||
3322|Calivil Formation|42130|6|Mentioned|Fig.3 P265|||||||||
3322|Calivil Formation|42133|6|Mentioned|p302|||||||||
3322|Calivil Formation|42134|4|Described|p339|||||||||
3322|Calivil Formation|42137|6|Mentioned|p370|||||||||
3322|Calivil Formation|42138|6|Mentioned|p392|||||||||
3322|Calivil Formation|42454|4|Described|p11|early Pliocene|late Miocene|||||||
3322|Calivil Formation|42455|5|Briefly described|Map legend|early Pliocene|late Miocene|||||||
3322|Calivil Formation|42509|6|Mentioned|p4|||||||||
3322|Calivil Formation|42827|6|Mentioned|p271|||refers to Macumber (1972)||||||
3322|Calivil Formation|42881|4|Described|Fig.3, P84|||||||||
3322|Calivil Formation|42966|2|Defined|p179|Pliocene|Late Miocene|Of the Wunghnu Group.||||||09-OCT-08
3322|Calivil Formation|43198|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43199|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43211|4|Described|p4,Fig.5 p15,27-8|Oligocene|Eocene|||||||
3322|Calivil Formation|43260|5|Briefly described|Map Legend|Miocene|Oligocene|||||||
3322|Calivil Formation|43261|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
3322|Calivil Formation|43493|4|Described|32|Oligocene|Eocene|||||||
3322|Calivil Formation|43601|6|Mentioned|p224||Early Pliocene|||||||
3322|Calivil Formation|43655|5|Briefly described|p40-846|||||||||
3322|Calivil Formation|43780|6|Mentioned|p6|||||||||
3322|Calivil Formation|43791|6|Mentioned|p372, Fig1|||||||||
3322|Calivil Formation|43804|6|Mentioned|Fig.2,p49|||||||||
3322|Calivil Formation|43846|5|Briefly described|14||Oligocene|||||||
3322|Calivil Formation|44188|5|Briefly described|Map Legend|Pliocene|Pliocene|Geological province: Murray Basin. Fluvial deposits- poorly consolidated pale grey, poorly sorted coarse to granular quartz sand, conglomerate with white kaolinitic matrix.||||||25-JUN-13
3322|Calivil Formation|44931|5|Briefly described|Map Legend|Tertiary|Tertiary|Alluvial clay and sand, and minor gravel.||||||14-JUN-06
3322|Calivil Formation|49038|4|Described|Table 2|||Briefly described p26||||||07-JUL-20
3322|Calivil Formation|49040|6|Mentioned|p12|||||||||
3322|Calivil Formation|50154|5|Briefly described|p133|Pliocene|Late Miocene|Overlies the Renmark Group. Geological Province: Murray Group.||||||
3322|Calivil Formation|60451|4|Described|p30, 95 Fig. 61, 98, 253|Pliocene|Eocene|Age: 40-6Ma, but not directly dated.  Palynology indicates max age. Overlain by Miocene-Pliocene units. Interfingers with the Renmark, Murray and Wunghnu Groups. Underlies: Parilla Sand, Shepparton Formation, Newer Volcanics.||||||24-JUN-14
3322|Calivil Formation|60452|4|Described|p35|Cenozoic|Cenozoic|First named by Macumber (1973), then called Calivil Sand (Lawrence, 1975) but reverted to original name of Calivil Formation (Tickell & Humphreys, 1980). Overlies Castlemaine Group, diconformably overlies Renmark Group. Overlain by Shepparton Formation.||||||19-NOV-08
3322|Calivil Formation|60454|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequences.||||||07-NOV-08
3322|Calivil Formation|60456|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence; poorly sorted gravel, sand and minor kaolinitic clay.||||||07-NOV-08
3322|Calivil Formation|60457|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence also known as 'Older Gold Drift' and 'deep leads': often richly auriferous; poorly sorted gravel, sand and minor kaolinitic clay.||||||25-JUN-13
3322|Calivil Formation|60458|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic overbank, point bar and channel lag sequence also known as 'Older Gold Drift' and 'deep leads'.||||||07-NOV-08
3322|Calivil Formation|60459|5|Briefly described|Map Legend|Neogene|Paleogene|Pre-basaltic alluvium now entirely buried beneath younger units.||||||07-NOV-08
3322|Calivil Formation|60461|5|Briefly described|Map legend|Miocene|Oligocene|Of the Murray Group.  River valley deposits - Powlett Plains deep lead and colluvium: interbedded clay, silty clay, silt and subangular to subrounded fine to coarse-grained quartz sand, reef quartz and metasediment gravel, minor ligneous clay.||||||28-SEP-04
3322|Calivil Formation|60462|5|Briefly described|Map Legend|Neogene|Neogene|Poorly sorted fine to coarse grained terrestrial sand: magnetic where ferruginised with responses to 20 nT; where cropping out thorium high.||||||15-SEP-04
3322|Calivil Formation|60491|4|Described|p16, p21|||Interfingers with the Parilla Sand. Consists of fluvial and fluviolacustrine quartzose sand and gravel.||||||
3322|Calivil Formation|60492|5|Briefly described|Map Legend|Miocene|Miocene|Alluvium: gravel, sand, silt, conglomerate.||||||
3322|Calivil Formation|60529|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||
3322|Calivil Formation|60581|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60582|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||23-NOV-04
3322|Calivil Formation|60583|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60584|5|Briefly described|Map Legend|Pliocene|Eocene|Variably rounded gravels of vein quartz, minor bedrock and White Hills Gravel clasts with sand, silt, clay and plant material.||||||
3322|Calivil Formation|60585|4|Described|p28|Pliocene|Late Eocene|Disconformably overlain by the Moorabool Viaduct Sand. Consists of poorly to moderately sorted polymictic cobbles, pebbles, sand and clay that have been ferruginised or silicified.||||||
3322|Calivil Formation|60591|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60592|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||25-NOV-04
3322|Calivil Formation|60593|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60595|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60596|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and unconformably overlies the Urana Formation. Clay, silty clay, silt, and fine- to coarse-grained sand, gravel; poorly sorted, subangular to subrounded, unconsolidated.||||||
3322|Calivil Formation|60597|5|Briefly described|Map Legend|Pliocene|Miocene|Deep lead fluvial deposits: no distinctive magnetic responses.||||||
3322|Calivil Formation|60599|5|Briefly described|p15, p85|Late Eocene|Middle Miocene|Of the Wunghnu Group. Fluvial sediments. Geological Province: Murray Basin.||||||09-OCT-08
3322|Calivil Formation|61160|5|Briefly described|p150|Pliocene|Miocene|Buried auriferous gravels or deep leads within this unit are present in valleys of the upper Ovens River and Morses Creek in BUFFALO. ||||||
3322|Calivil Formation|61163|6|Mentioned|p99|||Of Wunghnu Gp. Overlies Shepparton Fm. Poorly sorted gravels with abundance of sandstone clasts now fragile due to in-situ weathering; vein quartz clasts are subangular to subrounded. Economically important due to placer gold content. Geol Prov: LFB||||||05-JUL-07
3322|Calivil Formation|61174|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||07-FEB-11
3322|Calivil Formation|61175|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61176|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61177|5|Briefly described|map legend|Quaternary |Quaternary |Of the Wunghnu Group. Gravel, sand, silt, clay: generally consolidated (in subsurface only). GSV map code: Nwc.||||||
3322|Calivil Formation|61185|2|Defined|p57-62, p15, p64|Pliocene|Late Miocene|Of Macumber (1973). Of Wunghnu Gp. Reworked White Hills Gravel and colluvial seds. Under Shepparton Fm and Newer Volcanics; disconf. over Renmark Gp; conform. over/interfingers with Parilla Sand. Subsurface in NAGAMBIE. See Calivil Sand. Auriferous.||||||07-FEB-11
3322|Calivil Formation|61701|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61702|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61703|5|Briefly described|Map Legend|Pliocene|Miocene|Goulburn Valley deep lead river deposits: interbedded clay, silty-clay, silt, and sub-angular to sub-rounded fine to coarse grained sand, gravel; poorly sorted, unconsolidated.||||||15-JUN-06
3322|Calivil Formation|61822|6|Mentioned|p107|Neogene|Neogene|||||||
3322|Calivil Formation|61964|3|Fully described|p14 Fig. 4p141-143|Pliocene|Late Miocene|Of Murray Group? Fluvial gravels, sands and fine-grained sands  pale grey, poorly sorted medium- to coarse-grained quartz sand/sandstone with a white kaolinitic clay matrix. Unconformably overlies Olney Formation (Renmark Group). Geol. Prov: Murray Basin||||||09-OCT-08
3322|Calivil Formation|62370|5|Briefly described|p447, p452 Fig.4|Early Pliocene|Late Miocene|Fluvial deep-lead infill of sand and cobble conglomerate, and includes pallid clay and ferruginous clasts, recycled pebbles and locally eroded bedrock, in some areas has a magnetic ferricrete cap. Unconformably underlies Shepparton Formation.||||||
3322|Calivil Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix;interbedded siltstone and claystone; silicified and ferruginised duricrust common.||||||13-MAY-13
3322|Calivil Formation|64314|5|Briefly described|p498 Fig. 3, p502 Fig. 7|Late Miocene|Late Eocene|Of Macumber (1973). Thickness: ~30m. Use also in the compound name Yaloak/Calivill Formation. See also p500 Fig. 5, p501.||||||
3322|Calivil Formation|64568|5|Briefly described|Map legend|Silurian|Silurian|Geol.Prov: Murray Basin. [Note: map symbol suggests Tertiary age]. Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust is common.||||||24-JUN-14
3322|Calivil Formation|64612|6|Mentioned|p28|Cainozoic|Cainozoic|||||||07-FEB-11
3322|Calivil Formation|64823|5|Briefly described|p1011|||Paleochannel deposits. Geological province: Murray Basin.||||||
3322|Calivil Formation|65552|5|Briefly described|p2, p5 Fig.3, p6-8, p13, p15, p19|Early Pliocene|Late Miocene|See also p24 App.3, p26 App.5. Of Wanghnu Group, eastern Murray Basin. Medium to coarse grained quartz sand/sandstone with locally thick kaolin lenses. Overlies Olney Formation (Renmark Group), conformably underlies Shepparton and Coonambidgal Formations.||||||
3322|Calivil Formation|65715|5|Briefly described|p11 Tb.7, p11-12, 14, 16, 26, 27|Miocene|Miocene|Included in Wunghnu Group by Lawrence (1975). Correlated with older Murray Group by Holdgate and Gallagher (2003). Overlies Werribee Formation. Underlies Newer Volcanics. Younger than White Hills Gravel. Distribution modified see p14.||||||06-FEB-15
3322|Calivil Formation|65969|5|Briefly described|p27 Tb.3.3, p30-1|Miocene|Oligocene|Murray Basin. Erosional contact with underlying Olney Formation. Of Murray Group. Typically clay and silt interbedded with sand and gravel. Fines to the north of the BENDIGO 1:250 000 sheet. Occurs in paleotopographic lows and fills paleovalleys. Up to 70 m thick. Extensively worked for gold near Bendigo. Minor areas have magnetic responses to 15 nT; no distinctive radiometric response.||||||
3322|Calivil Formation|66002|5|Briefly described|p10 Tb.7, p12|Paleogene|Paleogene|Correlative of (obsolete) Loddon River Group. Previously included in Wunghnu Group (1975), but shown to correlate with Murray Group (Holdgate & Gallagher 2003). See also Macumber 1991.||||||15-MAY-13
3322|Calivil Formation|67179|6|Mentioned|p581|Pliocene|Miocene|Fluvial valley fill east of study area.||||Interfingers with the Loxton Sand (lateral equivalent).||
3322|Calivil Formation|68116|5|Briefly described|Appendix, Maps 22-24, 30-32, 40-41, 50.|Miocene|Oligocene||||||Conglomerate, sandstone, silt, clay: brown to pale colours; poorly sorted; clasts variably rounded; predominant vein quartz clasts; cross-bedding prominent.|
3322|Calivil Formation|68140|5|Briefly described|p1699|Pliocene|Pliocene|No outcrop. In hydraulic conductivity with the underlying Renmark Formation throughout much of the Riverine Province; they commonly form a single aquifer, and are referred to in this article as Calivil-Renmark Formation (see references p1698, p1699, p1702, pp1705-1708).||||Underlain by the Renmark Formation.|Sands.|09-FEB-18
3322|Calivil Formation|68189|5|Briefly described|p4, p26-29, p33|Miocene|Oligocene|River valley depositional environment. Upstream time equivalent of the younger part of the Olney Formation. Truncated by the Mologa Surface. Hosts alluvial Au won in ST ARNAUD in the near surface and where it forms deep leads.||||Nonconformably underlain by the White Hills Gravel.|Comprises mud, subangular to subrounded sand, reef quartz gravel.|
3322|Calivil Formation|68194|5|Briefly described|p9, p17, p21, p23, p25-26, p35-36, p40|Pliocene|Pliocene|See also p44, p55. Macumber (1972). Preserved on hills and rises, overlying weathered bedrock or Parilla Sand. Regolith and remote sensing profiles described. Age given as Eocene on p55.||Unit in Murray Group.||Lateral facies equivalent of Geera Clay.|Alluvial sands in paleovalleys, and gravels overlying bedrock highs.|
3322|Calivil Formation|68203|6|Mentioned|p11|Pliocene|Miocene|Deposition coincided with the first of two uplifts (~15-20m) of the Cadell Fault.||||||
3322|Calivil Formation|69162|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69163|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69164|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Poorly consolidated to unconsolidated, cross-bedded, poorly sorted, medium- to coarse-grained quartz sand and sandstone, white clay-rich matrix; interbedded siltstone and claystone; silicified and ferruginised duricrust common.|
3322|Calivil Formation|69798|6|Mentioned|p4 Fig.2|Pliocene|Pliocene|Murray Basin.||Wunghnu Group.||||
3322|Calivil Formation|70718|5|Briefly described|p17, p25|Cenozoic|Cenozoic|Is one of the primary aquifers in the Hay map sheet area. Misspellt as the Calival Formation on p25.||||Overlain by the Loxton Sand. Overlies the Upper Renmark Beds [Olney Formation]. Transitionally overlain by the Shepparton Formation.|Relatively coarse and poorly sorted fluvial sands and muddy overbank deposits.|30-MAY-19
3322|Calivil Formation|71419|5|Briefly described|p8 Fig 2, p14, p17-18.|Miocene|Miocene|Fluvial sediments derived from the Western Uplands. Source for later marine deposits i.e. Sandringham Sandstone.||||Overlain by Sandringham Sandstone.|Contains conglomerate consisting almost exclusively of vein quartz clasts.|02-FEB-18
3322|Calivil Formation|71593|5|Briefly described|p52, p54|||||Wunghu Group||||
3322|Calivil Formation|72445|5|Briefly described|App.1; App.2; App.7 p7-8, p7 Fig.4.|Pliocene|Miocene|Characterised by the organic-poor nature of the sands that are a major component of this formation. Said to be non-marine. App.2 is a .csv format file.  Identified in Stavely 05,07,11,12. Partially equivalent to Torrumbarry Clay, Bookpurnong beds/Formation.||Wunghnu Group ? Of Murray Group (App 2)||Underlies Woorinen Formation (gradational), Loxton Sand (sharp or gradational contact), Shepparton Formation. Overlies Olney, Bookpurnong Formations (sharp contacts).|Shown as including sand, gravel, lignite, mud and conglomerate.|
3322|Calivil Formation|73118|5|Briefly described|p81|Pliocene|Miocene|Extensive blanket underlies much of the Riverine Plain and N fringes of the Murray Basin. Deposited in valley-fill, alluvial-fan, fluviolacustrine and braided-channel environments.||Wunghnu Group.|||Poorly consolidated, pale grey, poorly sorted coarse to granular quartz sand, conglomerate, with white kaolinitic matrix; thick intercalations of carbonaceous clay.|
3322|Calivil Formation|73228|6|Mentioned|p56, p62|Pliocene|Late Miocene|Fluvial counterpart of the Loxton Sand.||||Underlain by upper Renmark Group.|Coarse and poorly sorted fluvial sands and muddy overbank deposits.|
3322|Calivil Formation|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
3322|Calivil Formation|73497|5|Briefly described|Map legend|Pliocene|Miocene|||Wunghnu Group|||Fluvial deposits: no distinctive magnetic or radiometric response.|
3322|Calivil Formation|73505|4|Described|p2, p11, p13, p36|Miocene|Late Eocene|Murray Basin. Nonmarine, occurs in palaeotopographic lows. Lateral equivalents interfinger with the Geera Clay. Minor areas where channels have magnetic responses to 15 nT.||Murray Group||Overlies Olney Formation with erosional contacts, onshore equivalent to Geera Clay, underlies Parilla Sand, Blanchetown Clay|Fluvial sand and mud, gravel, coarsening to the south.|
3345|Callemondah Granodiorite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Foliated contaminated granodiorite. BMR map symbol: gmh.||||||
3345|Callemondah Granodiorite|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
3345|Callemondah Granodiorite|31580|6|Mentioned|p272|||See also Table 1-4 for analysis||||||
3345|Callemondah Granodiorite|31581|3|Fully described|Table 1|||Xenolith content Table 111||||||
3345|Callemondah Granodiorite|32820|6|Mentioned|p3|||Part of Murrumbidgee Batholith||||||
3345|Callemondah Granodiorite|32906|6|Mentioned|p239|||||||||
3345|Callemondah Granodiorite|34544|6|Mentioned|p186|||||||||
3345|Callemondah Granodiorite|36413|2|Defined|p81|Silurian|Silurian|||||||
3345|Callemondah Granodiorite|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Biotite granodiorite. GSNSW map code: gmh.||||||
3345|Callemondah Granodiorite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Xenolith-rich granodiorite. S-type. BMR map code: Smc.||||||
3345|Callemondah Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
3345|Callemondah Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb2.||||||
3345|Callemondah Granodiorite|45147|3|Fully described|M194|||||||||
3345|Callemondah Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
3359|Caloma Sandstone|22831|4|Described|p 81|Late Devonian|Devonian|Nangar Subgroup||||||
3359|Caloma Sandstone|22857|5|Briefly described|p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Hervey Group. Pinkish to white, thickly-bedded orthoquartzite; rarely reddish, coarse-grained with pebble bands. Max. thickness: 229m. Geological Province: Hervey Basin.||||||
3359|Caloma Sandstone|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
3359|Caloma Sandstone|32865|6|Mentioned|p484|||Fauna, flora||||||
3359|Caloma Sandstone|34109|4|Described|Table 3.10|||Nangar Sub-group||||||
3359|Caloma Sandstone|43441|6|Mentioned|31||Late Devonian|||||||08-JAN-10
3359|Caloma Sandstone|43500|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Part of Nangar Sub-Group||||||
3359|Caloma Sandstone|43507|2|Defined|p128-9,137,146,152-6||Late Devonian|Top formation of Nangar Subgroup (Hervey Group)||||||
3359|Caloma Sandstone|43509|14|Not recorded|p113|||||||||
3359|Caloma Sandstone|43510|2|Defined|p41-2,47,49-51||Late Devonian|U.Dev fish plates found||||||
3359|Caloma Sandstone|44160|5|Briefly described|Map Legend||Famennian|||||||08-JAN-10
3359|Caloma Sandstone|48958|6|Mentioned|Plate 1|||||||||
3359|Caloma Sandstone|62569|5|Briefly described|p607 Fig. 2|Late Devonian|Late Devonian|Of Hervey Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
3370|Cambewarra Latite Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
3370|Cambewarra Latite Member|22488|5|Briefly described|p841|||||||||
3370|Cambewarra 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.||||||
3370|Cambewarra Latite Member|23544|5|Briefly described|Fig 2 p358|||In the Gerringong Volcanics||||||
3370|Cambewarra Latite Member|29900|6|Mentioned|p175|||||||||
3370|Cambewarra Latite Member|29901|4|Described|Table 1|||||||||
3370|Cambewarra Latite Member|31128|6|Mentioned|Table 1|||||||||
3370|Cambewarra Latite Member|32938|6|Mentioned|Fig.2|||||||||
3370|Cambewarra Latite Member|36220|4|Described|p38|||See also Table 1.||||||
3370|Cambewarra Latite Member|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
3370|Cambewarra Latite Member|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
3370|Cambewarra Latite Member|38690|4|Described|p292|||See also p289||||||
3370|Cambewarra Latite Member|40270|6|Mentioned|p177|||||||||
3370|Cambewarra Latite Member|40519|6|Mentioned|Fig.3|||||||||
3370|Cambewarra Latite Member|45090|6|Mentioned|p171|||Refers Hanlon et al.(1953)||||||
3370|Cambewarra Latite Member|67500|5|Briefly described|p12 Tb.1, p16|Late Permian|Late Permian|Between 18-70m thick. (Bowman 1970).||Of the Broughton Formation and Gerringong volcanic facies|||Amygdaloidal, red-yellow, finely porphyritic, with labradorite phenocrysts, pillowed flow.|
3370|Cambewarra Latite Member|71115|5|Briefly described|p179-180, 182-185, 187-188|Permian|Permian|Southern Sydney Basin. The most felsic volcanic Member of the Formation. Paleomagnetic results tabulated, discussed.||Gerringong Volcanics (Broughton Formation).||Overlies Saddleback Latite Member. Is overlain by Five Islands Latite Member.|Comprises several andesitic latite flows interbedded with siltstone. Contains subparallel plagioclase phenocrysts in a felsic groundmass comprising iron oxide and feldspar microlites and interstitial iron oxide and chlorite.|
3370|Cambewarra Latite Member|71542|6|Mentioned|p25|Late Permian|Late Permian|Of southern Sydney Basin.||Unit of Gerringong Volcanics.||At top of Broughton Formation.||20-OCT-21
3370|Cambewarra Latite Member|73494|5|Briefly described|p542-543|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanics.|||Shoshonitic andesite; porphyritic, holocrystalline, grey weathering to greenish grey or purple; locally vesicles and amygdales constitute 20% of the rock.|
3378|Camboon Volcanics|13516|6|Mentioned|p145 fig 3|Early Permian|Early Permian|From Taroom Shelf, Bowen Basin. Age: APP22.||||Overlain by Buffel Formation.||
3378|Camboon Volcanics|22439|5|Briefly described|p15, Fig.2|Early Permian|Early Permian|Taroom Trough, Bowen Basin.||||||
3378|Camboon Volcanics|22857|6|Mentioned|p258|Early Permian|Early Permian|||||||
3378|Camboon Volcanics|22863|6|Mentioned|p242|||||||||
3378|Camboon Volcanics|22864|6|Mentioned|p256||Early Permian|||||||
3378|Camboon Volcanics|22973|6|Mentioned|p10|||||||||
3378|Camboon Volcanics|22975|5|Briefly described|p34 Fig.6|Early Permian|Early Permian|||||||
3378|Camboon Volcanics|22980|5|Briefly described|p249 Fig.2|Early Permian|Early Permian|||||||
3378|Camboon Volcanics|23037|4|Described|p10,24,30-42,48,52-9|Early Permian|Late Carboniferous|||||||
3378|Camboon Volcanics|23042|4|Described|p8|||||||||
3378|Camboon Volcanics|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||30-NOV-09
3378|Camboon Volcanics|23161|6|Mentioned|p23|||||||||
3378|Camboon Volcanics|24615|5|Briefly described|CD|Early Permian|Late Carboniferous|[CPvc].  Basaltic to andesitic lava and equivalent volcaniclastic rocks; subordinate felsic ignimbrite and other volcaniclastic rocks and minor lava; commonly deformed to schistose equivalents in the Gogango Deformed Zone.||||||
3378|Camboon Volcanics|29387|6|Mentioned|Table 4|||||||||
3378|Camboon Volcanics|34133|6|Mentioned|p29|||||||||
3378|Camboon Volcanics|38204|4|Described|p69|||||||||
3378|Camboon Volcanics|39262|6|Mentioned|p121|||||||||
3378|Camboon Volcanics|39267|6|Mentioned|p232|||||||||
3378|Camboon Volcanics|40090|6|Mentioned|p81|||||||||
3378|Camboon Volcanics|40091|4|Described|p69|||||||||
3378|Camboon Volcanics|40093|6|Mentioned|p26|||||||||
3378|Camboon Volcanics|40094|4|Described|p22|||||||||
3378|Camboon Volcanics|40096|6|Mentioned|p3|||||||||
3378|Camboon Volcanics|40623|5|Briefly described|p80|||||||||
3378|Camboon Volcanics|41246|6|Mentioned|Map legend|Permian||||||||
3378|Camboon Volcanics|41546|6|Mentioned|p157|||||||||
3378|Camboon Volcanics|41666|6|Mentioned|Fig.1|||||||||
3378|Camboon Volcanics|41725|6|Mentioned|Fig.2|||||||||
3378|Camboon Volcanics|42249|6|Mentioned|p21|||||||||
3378|Camboon Volcanics|42250|6|Mentioned|Fig.4 P31|||||||||
3378|Camboon Volcanics|42641|6|Mentioned|Fig.3 P110|||||||||
3378|Camboon Volcanics|42987|6|Mentioned|p25|||||||||
3378|Camboon Volcanics|43000|5|Briefly described|p106|||||||||
3378|Camboon Volcanics|43017|5|Briefly described|Fig.3,p375|||||||||
3378|Camboon Volcanics|43050|5|Briefly described|p30|||||||||
3378|Camboon Volcanics|43185|6|Mentioned|6,9||Early Permian|||||||
3378|Camboon Volcanics|43995|14|Not recorded|Table p9|Permian|Carboniferous|||||||
3378|Camboon Volcanics|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
3378|Camboon Volcanics|50215|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Includes the Mount Bulgi Conglomerate Member.  Overlie the Torsdale Volcanics.||||||17-MAY-04
3378|Camboon Volcanics|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Includes the Gonyelinka Ignimbrite and Mount Bulgi Conglomerate Members.||||||18-MAY-04
3378|Camboon Volcanics|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Includes: Mount Bulgi Conglomerate Member, Gonyelinka Ignimbrite Member.||||||27-MAY-04
3378|Camboon Volcanics|50317|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
3378|Camboon Volcanics|50597|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Basaltic to andesitic lava and volcaniclastic rocks.||||||
3378|Camboon Volcanics|50602|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Basaltic to andesitic lava and equivalent volcaniclastic rocks.||||||
3378|Camboon Volcanics|60115|5|Briefly described|p21 Fig. 1|Early Permian|Early Permian|Geological Province:  eastern margin Bowen Basin.||||||04-FEB-08
3378|Camboon Volcanics|60282|4|Described|p6|Early Permian|Late Carboniferous|Age: 291Ma and 293+/-3Ma (SHRIMP).||||||
3378|Camboon Volcanics|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Geological Province: Bowen Basin.||||||
3378|Camboon Volcanics|60298|5|Briefly described|p192|Early Permian|Late Carboniferous|Mafic. Geological Province: Bowen Basin.||||||17-DEC-07
3378|Camboon Volcanics|60386|6|Mentioned|p296|Artinskian|Asselian|Bowen/Sydney Basin. Non-marine.||||||
3378|Camboon Volcanics|61035|5|Briefly described|p5|Permian|Early Permian|In the Auburn Arch. Geological Province: Auburn Subprovince.||||||07-FEB-11
3378|Camboon Volcanics|61076|5|Briefly described|p188 Fig. 2|Early Permian|Early Permian|Age: <300Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
3378|Camboon Volcanics|61612|6|Mentioned|p270, p270 Fig. 1|Late Carboniferous|Late Carboniferous|Geological Province: Bowen Basin. QLD.||||||13-MAR-09
3378|Camboon Volcanics|61777|5|Briefly described|p224, p227-229, p230, p225 Tab. 1|Early Permian|Early Permian|Age: 298+/-3 and 308+/-6Ma (SHRIMP U/Pb). Geological Province: Yarrol Province. Mainly andesite, basalt and volcaniclastics. See p277-229 for detailed info.||||||07-FEB-11
3378|Camboon Volcanics|61782|5|Briefly described|p280|||Contain acid to intermediate volcanics and volcaniclastic sedimentary rocks.||||||
3378|Camboon Volcanics|61832|5|Briefly described|p187|Permian|Carboniferous|Hosts Cracow gold deposit. Geological Province: Bowen Basin.||||||28-MAY-08
3378|Camboon Volcanics|62357|5|Briefly described|p524 Fig. 7|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||
3378|Camboon Volcanics|64855|5|Briefly described|p28|Early Permian|Early Permian|||||||22-FEB-10
3378|Camboon Volcanics|64856|4|Described|p42-45, p49-50, p52-53, p102|Early Permian|Late Carboniferous|Taroom Trough, Bowen Basin. Supersedes Camboon Andesite. Max thickness 658m. Mainly andesite to basalt flows and tuffs. Essentially equivalent to Combarngo volcanics.  Age from palynoflora (unit APP12) and dates of 294 and 281 Ma from Runnegar (1979).| | ||||28-NOV-17
3378|Camboon Volcanics|64857|5|Briefly described|p114,116, p113 Fig.3, p115|Early Permian||Bowen Basin. Unconformably overlain by Buffel Formation. Text seems to imply an Early Permian age.||||||
3378|Camboon Volcanics|64858|6|Mentioned|p180 Fig.2|Early Permian|Early Permian|||||||30-NOV-09
3378|Camboon Volcanics|65112|5|Briefly described|p313; Fig 4 p314|Early Permian|Early Permian|Partly equivalent in age to Reids Dome beds in Denison Trough. Underlies the Buffel Formation in the Taroom Trough.||||||22-MAR-12
3378|Camboon Volcanics|65113|5|Briefly described|Fig 4 p340|Early Permian|Early Permian|Taroom Trough. Underlies Buffel Formation.||||||
3378|Camboon Volcanics|65114|5|Briefly described|p383 Tb.1, p385 Fig.3, pg 394, 395|Cisuralian||ca 297-278Ma; of Bowen Basin-Taroom Trough; occurs below Buffel Formation; may extend down into the APP1 palynological zone; dates include K/Ar age of 277.9 +/- 4Ma near top of unit, 296.3 +/- 4 Ma (dates all referenced), max SHRIMP age 309.1 +/- 3.3Ma||||||
3378|Camboon Volcanics|65115|5|Briefly described|p405, 409, 411, Fig 2 p403, Fig 4a p406|Early Permian|Early Permian|Andesitic and basaltic flows, welded tuff, agglomerate, volcanic breccia, conglomerate, lithic sandstone and carbonaceous mudstone, up to 3000m thick. Ar-Ar dates 294-281 Ma (Runnegar 1979).||||||
3378|Camboon Volcanics|65116|5|Briefly described|Fig 2 p436|Early Permian|Early Permian|Taroom Trough, Bowen Basin. Underlies Buffel Formation.||||||
3378|Camboon Volcanics|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Buffel Formation in the Taroom Trough in the Bowen Basin.||||||06-MAR-12
3378|Camboon Volcanics|65119|5|Briefly described|p511, Fig 2, table 1, Fig 4-5,7-10,15-19|Early Permian|Early Permian|Bowen Basin. Andesite, basalt, dacite, rhyolite, tuffs and flows. Sandstone, siltstone, volcaniclastic conglomerate breccia.Up to ~3000m thick. Age: 268-280 Ma. Fission Track age: 77-174 Ma.||||||07-MAR-12
3378|Camboon Volcanics|65388|2|Defined|p20-32, p11, 14, 16 , 35, 36, 43, 123|Early Permian|Late Carboniferous|Includes Mount Bulgi Conglomerate Member at base. Disconformably overlies Torsdale Vocanics. Overlain by Buffel Formation, Back Creek Group, Woolein Formation or Oxtrack Formation. SHRIMP dates: 308+/-5 Ma near base, 297 +/-2 Ma. Formerly Camboon Andesite.  Camboon Volcanics of Briggs and Waterhouse (1982). Type section proposed - Delusion Creek.  Sometimes difficult to distinguish from Torsdale Volcanics. Contacts may be diachronous. Lithology: andesitic and basaltic lavas and volcaniclastics, but rhyolitic to dacitic lavas and volcaniclastics, including ignimbrite, and pebble to boulder conglomerate also present. Intruded by gabbro/diorite. See also p126, 166, 180, 338, 339, 432, 437, 439, 446, 447||||||
3378|Camboon Volcanics|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
3378|Camboon Volcanics|67133|5|Briefly described|p7|Permian|Permian|Basal unit of the Taroom Trough in the Bowen Basin. The sample analysed in this study was a highly weathered andesitic to dacitic crystal tuff, with alteration products including two types of smectite-rich clays and hematite.|||||Includes andesitic and basaltic lavas and tuffs.|
3378|Camboon Volcanics|67402|6|Mentioned|p21|Artinskian|Asselian|Bowen Basin. ||||Overlain by the Buffel Formation.||
3378|Camboon Volcanics|68008|5|Briefly described|p132, p138, p155-156, p292|||Text unclear: may include Mount Bulgi Conglomerate as basal unit [if so, should be Mount Bulgi Conglomerate Member]. Subaerially-erupted volcanics with similar mineralogy and textures to Rookwood Volcanics.||||Overlies Torsdale Volcanics.||
3378|Camboon Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Auburn Subprovince.||||||
3378|Camboon Volcanics|68679|4|Described|p312-313, p338, p343-344, p351-355, p360|Permian|Late Carboniferous|See also p372 Fig.5.64, p375, p379-381, p397, p407, p416, p419, p468-469. Camboon Volcanic Arc, Northern New England Orogen. Extends almost continuously ~200km from S of Cracow to the Capricorn Highway. Subaerial eruptions and fluvial, lacustrine or mass flow deposition in a volcanic landscape. Some marine fossil-bearing rocks E of the Auburn Subprovince, thought to be of this unit (Dear et al. 1971; Parfrey 1986), are now attributed to the Buffel Formation (Withnall et al., 2009). Various ages given. RELATED UNITS (continued): May have been partly coeval with Torsdale Volcanics. Probably part-correlated with Nogo beds. May be continuous with Combarngo Volcanics. Is intruded by Harrami Igneous Complex; Nulambie, Wingfield Granites. Source of Woolein Formation sediments.|297-c.295 Ma (Fanning et al., 2009).||Mount Bulgi Conglomerate Member.|Overlies Torsdale Volcanics. Is interleaved (as thrust slices) with overlying Woolein Formation and Back Creek Group. Underlies Buffel (unconformably) and Woolein Formations. See COMMENTS for more.|Mainly andesitic to basaltic lavas and volcaniclastics, with some rhyolitic to dacitic lavas and volcaniclastics including ignimbrite and pebble to boulder conglomerate. Alteration is relatively pervasive.|
3378|Camboon Volcanics|68822|5|Briefly described|p321, p337|Permian|Carboniferous|Late Carboniferous to Early Permian age.|||||Basaltic to rhyolitic.|
3378|Camboon Volcanics|70033|6|Mentioned|p2, p29|||Unit at base of Bowen Basin.||||||
3378|Camboon Volcanics|70837|5|Briefly described|p246|Cisuralian|Cisuralian|Of  Bowen Basin. SHRIMP ages of 295.2 and 297.1 Ma (Fanning etal., 2009). Corresponding to APP2 zone (Cisuralian-Guadalupian).||||||
3378|Camboon Volcanics|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Dacite, ignimbrite.|
3378|Camboon Volcanics|71701|5|Briefly described|p170|Cisuralian|Cisuralian|Bowen Basin. Potential source of Cisuralian ash falls in the Galilee Basin. SHRIMP dates are derived from Fanning et al, 2009 and Nicoll et al, 2015.|297.1 +/- 3.3 and 295.2 +/- 6.2 (SHRIMP)|||||
3378|Camboon Volcanics|71702|6|Mentioned|179|||Arc-related rocks. Gympie Terrane.||||||
3378|Camboon Volcanics|72297|5|Briefly described|p710|||Near Cracow, hosts gold in quartz veins and zones of silicification.|||||Andesitic lavas, tuffs and coarse breccias.|
3378|Camboon Volcanics|73163|6|Mentioned|p467|||New England Orogen. Attribed to the initial, extensional stage of the Bowen Basin.||||||
3378|Camboon Volcanics|73197|6|Mentioned|p470-471, p472 Tb.2|Cisuralian|Gzhelian|New England Orogen, northern. Eastern margin of the Bowen Basin. Rift volcanic rocks. U-Pb zircon age from Withnall et al., (2009).|297.1 +/- 3.3 Ma, 295.2 +/- 6.2 Ma U-Pb zircon||||Volcanics.|
3378|Camboon Volcanics|73450|6|Mentioned|p55|||Bowen Basin.||||||
3385|Camden Head Claystone|22616|6|Mentioned|Fig.1 p670|Triassic|Triassic|||||||
3385|Camden Head Claystone|32719|4|Described|p208|||See also p207,209.||||||16-NOV-10
3385|Camden Head Claystone|32803|6|Mentioned|p96|||||||||
3385|Camden Head Claystone|35488|6|Mentioned|p74|||||||||
3385|Camden Head Claystone|35647|5|Briefly described|p50|||||||||
3385|Camden Head Claystone|41348|5|Briefly described|Map legend|Triassic||Of the Camden Haven Group.||||||16-DEC-04
3385|Camden Head Claystone|43072|5|Briefly described|p55|||||||||
3385|Camden Head Claystone|60281|5|Briefly described|p18, Fig. 8 App. 1|Triassic||Of the Camden Haven Group.  Sequence of red-brown claystone and siltstone with lesser amounts of  grey, fossil-bearing siltstone, sandstone and conglomerate; usually has a thin basal conglomerate.  Max. thickness: 75m.  Geological Province: Lorne Basin||||||17-MAR-05
3385|Camden Head Claystone|66090|1|Redefined|pp1-2, p4, pp8-9, pp11-22, p32.|Early Triassic|Early Triassic|Redefined in this study. Formally named by Pratt and Herbert (1973). Type section described. Most widespread unit in Camden Haven Group (and Lorne Basin). Identified by high frequency of reddish purple mudstone beds. Few exposures: recessive and deeply weathered (apart from Coopernook Conglomerate Member); forms rich red soil. Deposited in a fluviatile / back-swamp environment. Lithology plots for various locations are detailed. Beds have been tilted by intrusion of underlying Middle Brother laccolith. Thickness: complete section not located; 82 m and 74 m sections measured. Age based on megaflora fossils and palynology - probable upper Early Triassic.||Basal unit in Camden Haven Group.|Includes Coopernook Conglomerate Member.|Is overlain by Laurieton Conglomerate and, locally, the Coorabakh Conglomerate. No correlates.|An overall upward-fining sequence of pebble and granule conglomerate with interbedded sandstone and characteristic reddish purple mudstone; lithologies interbedded throughout, though conglomerates confined to lower part of formation.|12-OCT-15
3390|Camelford Limestone|6969|5|Briefly described|p13 Fig. 1|Early Devonian|Pridoli |Geological Province: Lachlan Fold Belt.||||||
3390|Camelford Limestone|22857|5|Briefly described|p466 App.1 Tb.A1.6|Lochkovian|Pridolian|Of the Mumbil Group. Massive to poorly bedded limestone. Max. thickness: 200m.||||||
3390|Camelford Limestone|23043|5|Briefly described|Map Legend|Lochkovian|Pridoli|of Mumbil Group.||||||
3390|Camelford Limestone|23170|2|Defined|p93|Lochkovian|Pridoli|of Mumbil Group.||||||
3390|Camelford Limestone|23214|5|Briefly described|p126|Early Devonian|Early Devonian|||||||
3390|Camelford Limestone|23225|5|Briefly described|Fig.1|Early Devonian|Pridoli|||||||
3390|Camelford Limestone|23522|5|Briefly described|p248 Fig 4|Lochkovian|Pridoli|||||||
3390|Camelford Limestone|24247|5|Briefly described|p37|Early Devonian|Early Devonian|See also p39 Fig.2, p40 Fig.3||||||
3390|Camelford Limestone|42033|6|Mentioned|p657|||||||||
3390|Camelford Limestone|43039|5|Briefly described|p4|||||||||
3390|Camelford Limestone|50095|3|Fully described|p107|Lochkavian; delta Zone (conodont)|Pridoli|Well bedded limestone to limestone conglomerate. Overlain by Cuga Burga Volcanics. Overlies Barnby Hills Shale, probably conformably. Max. thickness: at least 610 m. Contains conondonts, brachiopods and corals.||||||
3390|Camelford Limestone|50096|6|Mentioned|p78|||Occurrence of Ozarkodina martinssoni auriformis (conodont).||||||29-NOV-04
3390|Camelford Limestone|60332|5|Briefly described|p937|Early Devonian|Ludlow|Has faulted contact with Oakdale Formation. Conformably overlies Oakdale Formation. Conformably overlain by Cuga Burga Volcanics. Limestone with minor limestone conglomerate. Contains conodonts, that are used for biostratigraphy.||||||
3390|Camelford Limestone|60987|5|Briefly described|p154 Fig.1, p155, p157-158  |Early Devonian|Silurian|Wellington district. Shallow-water strata.||||Conformably overlies Barnby Hills Shale.||
3390|Camelford Limestone|61892|6|Mentioned|p206, p216, p229|Early Devonian|Late Silurian|Contains a relatively broad-based population of conodont elements. Appears as Camelford Formation on p206.||||||22-MAY-17
3390|Camelford Limestone|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Wellington and Molong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3390|Camelford Limestone|66498|6|Mentioned|p45|Lochkovian|Lochkovian|||||||
3390|Camelford Limestone|71600|6|Mentioned|p23 Fig 1|Silurian|Silurian|Geological province: Lachlan Fold Belt.||Unit of Mumbil Group.||||
3390|Camelford Limestone|73143|6|Mentioned|p6, p8-9|Lochkovian|Lochkovian|Contains conodonts including Caudicriodus woschmidti (Farrell 2004a) re-assigned by Drygant and Szaniawski (2012) to Ca. ruthmawsonae indicating a slightly younger age of middle Lochkovian. Contains Lochkovian age corals.||||||
3390|Camelford Limestone|73299|6|Mentioned|p1105|Early Devonian|Silurian|Molong High. [Map symbol suggests Silurian age]||||Overlies the Oakdale Formation, underlies the Cuga Burga Volcanics.||
3392|Camels Hump Quartzite|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline (East). Of the Farnell Group.  Age - Ediacarian in text.||||||30-SEP-08
3392|Camels Hump Quartzite|29991|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
3392|Camels Hump Quartzite|30261|6|Mentioned|Table 1|||Marinoan age.||||||
3392|Camels Hump Quartzite|30375|6|Mentioned|p205|||||||||
3392|Camels Hump Quartzite|30908|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Marinoan. Part of Torrowangee Group||||||23-DEC-09
3392|Camels Hump Quartzite|33729|4|Described|p83|||||||||
3392|Camels Hump Quartzite|33734|5|Briefly described|p493|||Correlation & trace fossils.||||||
3392|Camels Hump Quartzite|34469|6|Mentioned|p109|||Upper Proterozoic. Torrowangee Group||||||
3392|Camels Hump Quartzite|38632|6|Mentioned|p20|||||||||
3392|Camels Hump Quartzite|41429|5|Briefly described|p246|||||||||
3392|Camels Hump Quartzite|41801|6|Mentioned|Fig.4|||||||||
3392|Camels Hump Quartzite|43501|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition) Part of Torrowangee Group.||||||30-SEP-08
3392|Camels Hump Quartzite|43502|14|Not recorded|Map Legend||Proterozoic|(Provisional Edition) Marinoan.||||||23-DEC-09
3392|Camels Hump Quartzite|46889|6|Mentioned|Table1|||||||||
3392|Camels Hump Quartzite|66623|5|Briefly described|p13, p18, p428.|||Thick, extensive marker unit.||Unit in Farnell Group.||Overlies Fowlers Gap Formation. Is overlain by Lintiss Vale Formation.|Medium- to fine-grained quartzite, well sorted, silicified; massive, sporadic zones of fine lamination.|
3392|Camels Hump Quartzite|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Farnell Group.||||
3392|Camels Hump Quartzite|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.||Unit in Farnell Group.||Overlies Fowlers Gap Formation. Is overlain by Lintiss Vale Formation.|Massive to finely-laminated, medium- to fine-grained quartzite, well-sorted, silicified; sporadic finely-laminated zones.|07-SEP-15
3427|Campbells Group|23048|5|Briefly described|p9 fig14||Late Ordovician|||||||
3427|Campbells Group|23214|5|Briefly described|p144|||Reassigned formation status.  See Campbells Formation.||||||
3427|Campbells Group|24269|5|Briefly described|p1554 Fig.1B|Late Silurian|Early Silurian|Geological Province: Lachlan Fold Belt||||||
3427|Campbells Group|24317|5|Briefly described|p15 Fig.1|Early Devonian|Early Silurian|Shallow to deep marine sedimentary rocks.||||||
3427|Campbells Group|29903|6|Mentioned|p169|||||||||
3427|Campbells Group|29989|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3427|Campbells Group|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
3427|Campbells Group|30109|6|Mentioned|Fig.1|||Silurian age||||||
3427|Campbells Group|30453|6|Mentioned|p59|||Queried as Formation||||||
3427|Campbells Group|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
3427|Campbells Group|30734|6|Mentioned|p28|||||||||
3427|Campbells Group|32483|6|Mentioned|p4|||Sil. Table 1||||||
3427|Campbells Group|32671|6|Mentioned|Map legend|Silurian|Ordovician|Ordovician-Silurian||||||
3427|Campbells Group|32672|6|Mentioned|p672|||||||||
3427|Campbells Group|32999|6|Mentioned|p9|||Refers Stanton(1956) L.Sil.||||||
3427|Campbells Group|33002|6|Mentioned|p417|||Tectonic history||||||
3427|Campbells Group|33004|6|Mentioned|p176|||||||||
3427|Campbells Group|33006|6|Mentioned|Map legend|Silurian|Silurian|||||||
3427|Campbells Group|33285|5|Briefly described|p19|||Early Sil.||||||
3427|Campbells Group|33742|6|Mentioned|p116|||Strat. Table.||||||
3427|Campbells Group|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
3427|Campbells Group|34481|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
3427|Campbells Group|37727|6|Mentioned|p42|||Variation of Campbells Formation||||||
3427|Campbells Group|40328|6|Mentioned|p166|||||||||
3427|Campbells Group|42413|5|Briefly described|p50|||||||||
3427|Campbells Group|42842|5|Briefly described|p11|||||||||
3427|Campbells Group|42941|5|Briefly described|p1|||||||||
3427|Campbells Group|43479|14|Not recorded|p106,116|Late Silurian|Early Silurian|||||||
3427|Campbells Group|43515|14|Not recorded|Map Legend||Silurian|(Provisional Edition)||||||
3427|Campbells Group|43516|14|Not recorded|Map Legend||Silurian|||||||
3427|Campbells Group|50124|5|Briefly described|p125 Fig.2|Late Silurian|Silurian|Formerly the Campbells Formation. Redefined and now includes the Kangaloolah Volcanics (M. Scott pers. comm. 2002). Geological Province: eastern Lachlan Fold Belt.||||||
3427|Campbells Group|50230|5|Briefly described|Map legend|Early Silurian|Early Silurian|Siltstone, phyllite, black siltstone, quartzose and minor volcaniclastic sandstone, quartzite, quartz-muscovite schist, felsic tuff.||||||
3427|Campbells Group|50231|5|Briefly described|Map Legend|Late Silurian|Early Silurian|On BOOROWA sheet these are undifferentiated sediments.||||||13-MAY-04
3427|Campbells Group|50232|5|Briefly described|Map legend|Ludlow|Wenlock|Contains undifferentiated sediments and Wet Lagoon Volcanics.||||||
3427|Campbells Group|50233|5|Briefly described|Map Lagend|Early Devonian|Early Silurian|See also Campbells Formation.  Overlies Mumbil Group.||||||13-MAY-04
3427|Campbells Group|50234|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Wet Lagoon Volcanics and undifferentiated sediments.||||||13-MAY-04
3427|Campbells Group|63633|5|Briefly described|Map Legend|Llandovery|Bolindian|Includes Bummaroo Formation.||||||
3427|Campbells Group|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Box Ridge Volcanics, Wet Lagoon Volcanics, Wrens Nest Trachyte, Kangaloolah Volcanics, Kildrummie Formation, Fosters Creek Conglomerate, Cuddyong and Binghams Formations.||||||11-JUN-08
3427|Campbells Group|66087|6|Mentioned|p5|Devonian|Devonian|||||Underlies the Crudine Group.||10-MAY-12
3427|Campbells Group|67820|5|Briefly described|p133, p134, p136 Fig.3, p137|Pridoli|Wenlock|Underwent regional metamorphism (biotite grade) during the Middle Devonian Tabberabberan Orogeny.|||Kangaloolah, Wet Lagoon Volcanics.||Quartz-lithic sandstone and siltstone.|
3427|Campbells Group|67847|5|Briefly described|p30|||||||Overlain by the Triangle Formation.||
3427|Campbells Group|68592|1|Redefined|p607-724, p731-2, p742, p744, p750, p803|Lochkovian|Wenlock|See also xxiii, p74 Tb.5, p85-86, p129-131, p169, p230, p241, p259, p269, p272, p282, p298, p424-425, p457, p863. The original definition of Stanton (1956) is herein changed, as it included rocks of the Jeremy Formation. Included Kildrummie, Bummaroo Formations. Downgraded to Formation status (in the Mumbil Group) by Raymond et al. (1998). Reinstated to Group level in this study, including several units previously placed in Mumbil Group by Pogson and Watkins (1998). Representative section described. Up to c.5km thick. Fossils are rare. Hill End Trough. Mapped in a continuous belt from Peelwood to Collector. Quarried locally for road material. Volcanosedimentary units host VHMS mineralisation. Has a number of small, uneconomic limestone lenses. Contemporaneous with Mount Fairy Group; correlated with Chesleigh Group, Bells Creek Volcanics and (?) Cookman Formation. Middle to upper greenschist metamorphism; commonly biotite grade. Geophysical properties described. Wyangala and Peelwood structural zones: deformation and metamorphism described.|||Includes Binghams Back and Cuddyong Formations; Box Ridge, Wet Lagoon and Kangaloolah Volcanics; Wrens Nest Trachyte and Fosters Creek Conglomerate (at base).|Disconformably or unconformably overlies Rockley Volcanics and Jeremy Formation. Is intruded by Burridgee Diorite. Is overlain gradationally by Dunchurch Formation (Crudine Group).|Mostly deep-water siltstone and quartzose sandstone turbidites with felsic volcaniclastic rocks, black shale and rare limestone; sandstones contain diagnostic volcanic quartz.|
3427|Campbells Group|70192|5|Briefly described|Map Legend|Lochkovian|Wenlock|On Gunning, Crookwell and Taralga 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Binghams Back Formation, Cuddyong Formation, Fosters Creek Conglomerate, Kildrummie Formation, Kangaloolah Volcanics, Wrens Nest Trachyte, Wet Lagoon Volcanics, Box Ridge Volcanics.|Is overlain by Dunchurch Formation (of Crudine Group) and undifferentiated Crudine Group.||
3427|Campbells Group|70296|6|Mentioned|p1, p19|||Was contact metamorphosed by Parkesbourne Granite.|||Includes the Kangaloolah Volcanics.|||21-JAN-21
3427|Campbells Group|70297|4|Described|map legend, on side 2 of map sheet|Lochkovian|Wenlock|Age: late early Silurian to earliest Devonian. Erosional base. Hosts base metal-barite mineralisation, at Kempfield; classified as siliciclastic-felsic hosted (i.e. Iberian-type).|||Kangaloolah Volcanics|Underlies Chesleigh Group; adjacent to Mumbil Group (relationship?).|Fine- to coarse-grained quartzo-feldspathic sandstone, interbedded with siltstone and mudstone, sporadic conglomerate; rhyolite, dacite, volcaniclastic rocks; sporadic limestone and allochthonous limestone blocks.|
3427|Campbells Group|70541|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Cuddyong Formation, Wet Lagoon Volcanics|||
3427|Campbells Group|70542|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Cuddyong Formation, Wet Lagoon Volcanics.|||
3427|Campbells Group|70543|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Binghams Back Formation, Cuddyong Formation, Fosters Creek Conglomerate, Kildrummie Formation, Kangaloolah Volcanics|||
3427|Campbells Group|70544|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Binghams Back Formation, Cuddyong Formation, Kangaloolah Volcanics, Wrens Nest Trachyte, Box Ridge Volcanics.|||
3427|Campbells Group|71069|5|Briefly described|p23, p24, p36, p41, p42, p100|||Hill End Trough. Hosts small scale skarn-related mineral deposits and gold vein deposits. See also p106, p134, p135, p146, p154, p163.|||Includes the Wet Lagoon Volcanics, Bummaroo Formation, Box Ridge Volcanics, Cuddyong Formation,  Kangaloolah Volcanics and the Kildrummie Formation.|Equivalent to parts of the Hoskinstown and Mount Fairy Groups.|Limestone and shale overlain by predominantly quartzose deep marine turbidite sequence.|
3427|Campbells Group|71656|4|Described|p10 Fig.1,  p13 Fig.2, p27-28|Lochkovian|Wenlock||||Includes Kildrummie Formation, Kangaloolah Volcanics, Cuddyong Formation, Binghams Back Formation, Box Ridge Volcanics.|||
3427|Campbells Group|71700|6|Mentioned|CD||||||Includes the Bummaroo Formation.|||
3427|Campbells Group|72528|6|Mentioned|p25.|Ordovician|Ordovician|[Previous, or new, name for Adaminaby Group sediments in this area?]||||||
3427|Campbells Group|73582|5|Briefly described|p99, 105-107, 110, 117, 126|Late Silurian|Early Silurian|Southern Hill End Trough. Crops out W of Jenolan Caves.||||Is faulted against Jenolan Caves Limestone.|Chert, mudstone; andesite.|
3429|Camperdown Complex|23720|5|Briefly described|Map Legend|Early Permian|Early Permian|Pyroxene gabbro, pyroxene diorite, hornblende diorite, tonalite, granodiorite.||||||15-DEC-04
3429|Camperdown Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
3429|Camperdown Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
3429|Camperdown Complex|71628|5|Briefly described|p2: 17-19|||Named by Collerson (1967) but first published by Leitch et al. (1971). Named after Camperdown homestead. Comprises several small bodies ~42 km ENE of Armidale. Crops out as small rounded to blocky cornerstones. Assigned to Bakers Creek Suite by Landenberger (1996). Here assigned to Bakers Creek Supersuite.||||Intrudes Girrakool beds. Abuts (?and intrudes) Abroi Granodiorite.||
3442|Canangle Subgroup|22857|5|Briefly described|p217, p490 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Upper fluvial sequence of the Catombal Group. Contains fossil plant remains. Geological Province: Lambie Basin.||||||
3442|Canangle Subgroup|22859|6|Mentioned|p217|||||||||
3442|Canangle Subgroup|23043|5|Briefly described|Map Legend|Famennian|Famennian|Of Catombal Group.||||||04-MAR-09
3442|Canangle Subgroup|23170|6|Mentioned|p253|Late Carboniferous||Of Catombal Group.||||||04-MAR-09
3442|Canangle Subgroup|23214|3|Fully described|p236|Late Devonian|Late Devonian|Of Catombal Group.   Geological Province: Lambie Basin. Underlying unit: Black Rock Subgroup.||||||
3442|Canangle Subgroup|24126|6|Mentioned|p172|||Of the Catombal Group.||||||
3442|Canangle Subgroup|24247|5|Briefly described|p37|Late Devonian|Late Devonian|Fossil evidence suggests age is Famennian. Parent: Catombal Group.||||||04-MAR-09
3442|Canangle Subgroup|39655|6|Mentioned|Plate 1|||||||||
3442|Canangle Subgroup|43507|14|Not recorded|p125|||||||||
3442|Canangle Subgroup|43513|14|Not recorded|p71-73|||Is'essentially a red bed sequence'.||||||04-MAR-09
3442|Canangle Subgroup|43782|5|Briefly described|Map Legend|Famennian|Famennian|Of Catombal Group.||||||04-MAR-09
3442|Canangle Subgroup|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Catombal Group.  Includes: Curra Curra Conglomerate.||||||
3442|Canangle Subgroup|64826|5|Briefly described|p1040 Tb. 1|Late Devonian|Late Devonian|Of the Catombal Group.||||||04-MAR-09
3442|Canangle Subgroup|68003|5|Briefly described|pp141-142.|Devonian|Devonian|||Unit in Catombal Group.|Includes Kurrool Formation and Curra Creek Conglomerate.|||
3447|Canberra Formation|22768|5|Briefly described|p176||Llandovery|||||||
3447|Canberra Formation|22857|4|Described|p176, p462 App.1 Tb.A1.6|Silurian|Silurian|Mudstone and siltstone with minor arenite and limestone; dacitic welded tuffs. Overlain by Hawkins Suite. Includes Narrabundah Ashstone Member at top. Max. thickness: 1000m.||||||
3447|Canberra Formation|24248|6|Mentioned|p67, p69|||See also p72 Tb.3||||||
3447|Canberra Formation|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
3447|Canberra Formation|37728|4|Described|Table 2|||||||||
3447|Canberra Formation|38664|5|Briefly described|p5|||||||||
3447|Canberra Formation|39947|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
3447|Canberra Formation|41356|4|Described|p5|||||||||
3447|Canberra Formation|42497|5|Briefly described|Map legend|Wenlockian|Wenlockian|||||||
3447|Canberra Formation|42727|5|Briefly described|map legend|Wenlock|Wenlock|Incl Narrabundah Ashstone, Camp Hill Sst Mbrs. Mudst, siltst, sandst, limest, hornfels, dacitic ignimbrite, volcaniclastic seds. Over Black Mountain Sst, State Circle Shale, Pittman Fm; under Mount Ainslie Volcanics. BMRmap: Smc. GeolProv: Canberra Block.||||||22-MAY-08
3447|Canberra Formation|42820|2|Defined|p15|Ludlow|Wenlock|Age discussed as 'late Wenlock', with reasons given for questioning a previously accepted Ludlow minimum age.||||||04-DEC-15
3447|Canberra Formation|42994|6|Mentioned|p20|||||||||
3447|Canberra Formation|43158|5|Briefly described|3||Early Silurian|||||||
3447|Canberra Formation|43159|5|Briefly described|Fig.2p4,p3,p9.||Early Silurian|||||||
3447|Canberra Formation|43481|5|Briefly described|3-12|||||||||
3447|Canberra Formation|47037|6|Mentioned|p107|||||||||
3447|Canberra Formation|49043|4|Described|p7|||||||||
3447|Canberra Formation|49690|6|Mentioned|p26|Middle Silurian|Middle Silurian|Canberra-Yass Shelf.||||||
3447|Canberra Formation|66197|5|Briefly described|p631 Fig.3c||Wenlock|Canberra-Yass and Ngunawal Basins. Shallow marine mixed clastic and carbonate rocks. Overlain by Hawkins Volcanics in Tuggeranong area.||||||13-MAR-12
3447|Canberra Formation|68592|5|Briefly described|p16, p428, p443, p457|Wenlock|Llandovery|Abell (1991). Equivalent to, but not yet formally included in, the Douro Group.|||Includes Camp Hill Sandstone Member.|Unconformably overlies State Circle Shale. Is correlated with lower part of Douro Group.||
3447|Canberra Formation|71657|6|Mentioned|p33-35, p38-40, p42, p45-47|Silurian|Silurian|Contains a brachiopod fauna of seven species dominated by Atrypa duntroonensis [see article for details]. Also contains uncommon trilobites (mostly Batocara mitchelli), corals, gastropods and bryozoans. Fossils occur in repeated crowded layers which probably represent storm deposits. Notable fossil locality at Woolshed Creek. Age was reported as late Sheinwoodian to early Homerian [ca 428-426 Ma and ca 426-423 Ma, respectively, at time of publication]. Holotype materials of the brachiopods Mesoleptostrophia oepiki and Hedeina oepiki were recovered from this unit. Includes strata of the superseded Riverside Formation (of Opik, 1958).||||||
3447|Canberra Formation|73211|5|Briefly described|p907-909|early Homerian|early Homerian|Mudstone near the top of the formation contains brachiopods Atrypa duntroonensis; fossil site at Woolshed Creek is on the ACT Government Heritage List. Geochron based on age of brachiopods (Strusz, 2011). Deposited in a shallow marine, tropical environment during the earliest part of the Tabberabberan Tectonic Cycle (ca 430-380 Ma).|ca 430.5 Ma||Camp Hill Sandstone Member, Acton limestone, Narrabundah Ashstone Member||Includes mudstone, siltstone, sandstone, limestone, dacitic ignimbrite and volcaniclastic sediments.|
3447|Canberra Formation|73215|6|Mentioned|p994|||Canberra area.||||||
3452|Candelo Supersuite|22878|6|Mentioned|p82|||||||||
3452|Candelo Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
3452|Candelo Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Nungatta Granodiorite||||||01-OCT-04
3452|Candelo Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
3452|Candelo Supersuite|24551|5|Briefly described|p235|||||||||
3452|Candelo Supersuite|42726|5|Briefly described|map legend||Early Devonian|Includes the Belowra, Braidwood, Candelo, Hopping Joe, Jinden, Nungatta and Watch Box Suites.||||||09-FEB-05
3452|Candelo Supersuite|42827|5|Briefly described|p430|||||||||
3452|Candelo Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
3452|Candelo Supersuite|69564|5|Briefly described|p3, p5|||Chappell et al. (1988); Chappell et al. (1991). Lachlan Orogen. Extends from near Wangarabell (Vic) to Lower Boro (NSW).|||Braidwood Suite.|||
3452|Candelo Supersuite|69801|6|Mentioned|p129|||Eastern Lachlan Orogen.|||Includes the Yurammie Granite.|||
3452|Candelo Supersuite|71069|6|Mentioned|p43|Early Devonian|Early Devonian|||||Intrudes the Bungonia and Bindook Groups.||
3452|Candelo Supersuite|71700|2|Defined|vi, CD|Early Devonian|Early Devonian|Named for the village of Candelo after which the type pluton, the Candelo Tonalite (Lewis et al. 1994) is named. See the Braidwood Suite for geomorphic expression, outcrop, lithology, structure, metamorphism and relationships. Distribution, geochemistry, geophysical characteristics, distinguishing features, economic geology and geological hazards are discussed. Age is derived from SHRIMP U-Pb zircon dates for Braidwood Granodiorite of the constituent Braidwood Suite.|||Includes the Braidwood Suite, Belowra Suite, Candelo Suite, Hopping Joe Suite, Jinden Suite, Nungatta Suite and Watch Box Suite.|||
3456|Candoin Creek Tonalite|35248|4|Described|p239|||Mention Fig.1||||||
3473|Canobolas Volcanic Complex|22503|5|Briefly described|p641, Fig.7 p650||Miocene|See also p652||||||
3473|Canobolas Volcanic Complex|23090|5|Briefly described|p642||Miocene|||||||
3473|Canobolas Volcanic Complex|23214|5|Briefly described|p17|Late Miocene|Middle Miocene|Age: 11 -13Ma||||||
3473|Canobolas Volcanic Complex|24233|5|Briefly described|p253 Fig.1, p256|Tertiary|Tertiary|Geological Province: Lachlan Orogen.||||||
3473|Canobolas Volcanic Complex|33007|5|Briefly described|p12|||History & genesis||||||
3473|Canobolas Volcanic Complex|33116|4|Described|p230|||Refers Joplin et al.(1952). Cainozoic. See also P231||||||
3473|Canobolas Volcanic Complex|33756|4|Described|p257|||Age dating||||||
3473|Canobolas Volcanic Complex|34547|6|Mentioned|p516|||Melilite in hawaiites. See also P521||||||
3473|Canobolas Volcanic Complex|35045|6|Mentioned|p110|||||||||
3473|Canobolas Volcanic Complex|37389|6|Mentioned|p55|||||||||
3473|Canobolas Volcanic Complex|37391|6|Mentioned|p26|||||||||
3473|Canobolas Volcanic Complex|43127|4|Described|p4,Fig.2,Fig.3|||||||||
3473|Canobolas Volcanic Complex|43578|6|Mentioned|p339|||||||||
3473|Canobolas Volcanic Complex|68592|5|Briefly described|p1793|Miocene|Miocene||||||Includes basalts.|
3473|Canobolas Volcanic Complex|70297|5|Briefly described|map legend, on side 2 of map sheet|Neogene|Paleogene|Included in general description for Unnamed volcanic rocks and sediments. Age: middle to late Miocene (11-13 Ma) - age used in context of Province?|||||Mafic volcanic rocks.|18-MAY-16
3473|Canobolas Volcanic Complex|70684|5|Briefly described|p43|Miocene|Miocene|Forms the Mount Canobolas extinct shield volcano. The age range explains the obvious terracing and silicified logs between basalt flows.|12.4-11.2 Ma (K-Ar: Wellman and McDougall, 1974).||||Very widespread, olivine- and pyroxene-phyric basalt flows. The central complex comprises several domes, mostly trachyte but with minor phonolite, microsyenite and alkali rhyolite; also thick trachytic pyroclastics.|
3473|Canobolas Volcanic Complex|73299|6|Mentioned|p1094 Fig.2|Cenozoic|Cenozoic|||||||
3476|Canomodine Limestone|22857|4|Described|p424 App.1 Tb.A1.5|Ordovician|Ordovician|Of the Barrajin Group. Thick-bedded to massive, wackestone, limey mudstone, minor shale and tuff. Max. thickness: 60m. ||||||
3476|Canomodine Limestone|23213|6|Mentioned|p21|||Contains Halysites praecedens.||||||
3476|Canomodine Limestone|23214|3|Fully described|p50|Eastonian|Eastonian|Of Barrajin Group. Type Locality GR 666200 6290800 to GR 664900 628900. Max thickness 400m||||||
3476|Canomodine Limestone|24398|6|Mentioned|p264|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
3476|Canomodine Limestone|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3476|Canomodine Limestone|32156|6|Mentioned|p233|||Refers fossil content||||||
3476|Canomodine Limestone|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3476|Canomodine Limestone|32672|6|Mentioned|p672|||||||||
3476|Canomodine Limestone|33006|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle to Upper OrdovicianM - U||||||
3476|Canomodine Limestone|33116|6|Mentioned|Fig.6|||Ord. Correlation.||||||
3476|Canomodine Limestone|33125|6|Mentioned|p15|||Correlation chart||||||
3476|Canomodine Limestone|33282|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle - Upper OrdovicianM - U||||||
3476|Canomodine Limestone|33735|6|Mentioned|p206|||||||||
3476|Canomodine Limestone|33741|6|Mentioned|Fig.1|||Ord.||||||
3476|Canomodine Limestone|34404|4|Described|p80|||||||||
3476|Canomodine Limestone|34405|6|Mentioned|Fig.3.9|||||||||
3476|Canomodine Limestone|34575|6|Mentioned|p637|||Ordovician. See also PP659,643 etc.||||||
3476|Canomodine Limestone|34576|6|Mentioned|p345|||Fauna||||||
3476|Canomodine Limestone|34692|6|Mentioned|p184|||||||||
3476|Canomodine Limestone|35062|6|Mentioned|p279|||||||||
3476|Canomodine Limestone|35118|6|Mentioned|Fig.5|||||||||
3476|Canomodine Limestone|38219|6|Mentioned|Table 2|||||||||
3476|Canomodine Limestone|39331|6|Mentioned|Fig.6-1|||||||||
3476|Canomodine Limestone|39657|6|Mentioned|M30|||||||||
3476|Canomodine Limestone|39663|6|Mentioned|Table 1|||||||||
3476|Canomodine Limestone|40127|6|Mentioned|p9|||||||||
3476|Canomodine Limestone|40136|5|Briefly described|p19|||||||||
3476|Canomodine Limestone|40328|6|Mentioned|Plate 4|||||||||
3476|Canomodine Limestone|42479|5|Briefly described|Fig. 1 P108|||||||||
3476|Canomodine Limestone|43385|14|Not recorded|p169|Late Ordovician|Early Ordovician|Ref. to Stevens 1957||||||
3476|Canomodine Limestone|43479|14|Not recorded|p95f|Caradocian|Llandeilian|||||||
3476|Canomodine Limestone|43515|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(Provisional Edition) (M.-U.Ord)||||||
3476|Canomodine Limestone|43516|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(M.-U.Ord)||||||
3476|Canomodine Limestone|43569|6|Mentioned|p477||Ordovician|||||||
3476|Canomodine Limestone|43640|5|Briefly described|Map Legend||Ordovician|||||||
3476|Canomodine Limestone|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Barrajin Group. Consists of thick-bedded to massive, wackestone, limey mudstone, minor shale and tuff.||||||28-NOV-13
3476|Canomodine Limestone|43782|5|Briefly described|Map Legend|Eastonian|Eastonian|of Barrajin Group.||||||
3476|Canomodine Limestone|44086|14|Not recorded|p97,98,103,107,`|Late Ordovician|Early Ordovician|||||||
3476|Canomodine Limestone|48926|6|Mentioned|p26|||P26 et seq.||||||24-FEB-10
3476|Canomodine Limestone|63278|5|Briefly described|p154|||Beneath the Rockdale Formation. Geological Province: Lachlan Fold Belt. Contains corals and stromatoporoids with equivalent age to Quondong and Ballingoole Limestones.||||||28-NOV-13
3476|Canomodine Limestone|63286|5|Briefly described|p308 Fig. 9|Bolindian|Eastonian|Unconformably overlain by Malongulli Formation, underlain by Fairbridge Volcanics. Geological Province: Molong Volcanic Belt.||||||28-NOV-13
3476|Canomodine Limestone|63287|4|Described|p317 Fig. 2, p333|Eastonian|Eastonian|Of Barrajin Group. Overlain by Malongulli Formation.  Geological Province: Molong Volcanic Belt. Consists of limestone.||||||28-NOV-13
3476|Canomodine Limestone|64963|5|Briefly described|p182 Fig. 2|||Within the Molong Volcanic Belt.||||||22-APR-09
3476|Canomodine Limestone|67322|5|Briefly described|Fig.5; p23|Katian||Macquarie Arc. (Stevens 1950). Did not accumulate until Eastonian 2 time, extending into the late Eastonian. Synonymous with the Cargo Creek Limestone.||Of the Cabonne Group.||Overlies Cargo Volcanics. Overlain by the Rockdale Formation.||21-FEB-18
3476|Canomodine Limestone|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
3476|Canomodine 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.|c. 455-450 Ma|Cabonne Group||||
3476|Canomodine Limestone|70754|6|Mentioned|p448|||||||||
3476|Canomodine Limestone|71091|6|Mentioned|p146, p148|||Cargo district. Coral fauna listed and discussed.||||||
3476|Canomodine Limestone|73209|5|Briefly described|p880|Late Ordovician|Late Ordovician||||||Massive grey limestones.|
3476|Canomodine Limestone|73210|6|Mentioned|p892|||Canomodine, NSW.||||||
3476|Canomodine Limestone|73492|6|Mentioned|p704, p706|Katian|Katian|Cargo Creek Limestone is now synonymised into Canomodine Limestone (Percival et al., 2011, p23).||||||
3480|Caoura basalt|39356|6|Mentioned|Fig.2|||||||||
3480|Caoura basalt|73581|5|Briefly described|p22|Oligocene|Oligocene|Southern Highlands Volcanic Province. Correlates temporally and petrographically with the South Coast Volcanic Province. See also Caoura Basalt p23.|||||Low-K tholeiite to alkali basalt. High-Ti mineralogy and mantle xenoliths.|
3498|Cape Horn Coal Member|24471|5|Briefly described|p31 Fig.3|Late Permian|Late Permian|Within boundary of Eckersley Formation and Lawrence Sandstone. Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
3498|Cape Horn Coal Member|29900|6|Mentioned|p175|||||||||
3498|Cape Horn Coal Member|29901|4|Described|Table 1|||||||||
3498|Cape Horn Coal Member|30006|5|Briefly described|p37|||||||||
3498|Cape Horn Coal Member|31128|6|Mentioned|Table 1|||||||||
3498|Cape Horn Coal Member|32849|6|Mentioned|Table 1|||Permian||||||
3498|Cape Horn Coal Member|36220|6|Mentioned|p50|||See also Table 1 & P50.||||||
3498|Cape Horn Coal Member|36593|6|Mentioned|Table 2|||||||||
3498|Cape Horn Coal Member|37089|6|Mentioned|p208|||||||||
3498|Cape Horn Coal Member|39661|6|Mentioned|Fig.1|||||||||
3498|Cape Horn Coal Member|42787|6|Mentioned|Table 1 P126|||||||||
3498|Cape Horn Coal Member|42896|5|Briefly described|p23|||of Eckersley Formation||||||
3554|Cappanana Formation|22768|5|Briefly described|p176|Ludlow|Late Wenlockian|||||||
3554|Cappanana Formation|22815|2|Defined|p38, fig10,16|Late Silurian|Late Silurian|||||||
3554|Cappanana Formation|22857|4|Described|p176, p464 App. 1 Tb.A1.6|Ludlovian|Wenlockian|Of the Bredbo Group. Shallow marine deposits. Overlain by Colinton Volcanics. Max. thickness: 700m. Geological Province: Canberra-Yass Shelf and Monaro Forearc Basin. See also p468 App.1 Tb.A1.6.||||||
3554|Cappanana Formation|24128|5|Briefly described|p3|||Geological Province: Lachlan Fold Belt.||||||
3554|Cappanana Formation|32820|6|Mentioned|Table 1|||Sil.||||||
3554|Cappanana Formation|36413|2|Defined|p33|Late Silurian|Late Silurian|This is correct spelling of name.||||||
3554|Cappanana Formation|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Includes unnamed limestone unit. Siltstone, shale, sandstone and minor tuff. Underlies Colinton Volcanics. Unconformably overlies Foxlow Beds. GSNSW map code: Sp.||||||
3554|Cappanana Formation|37251|5|Briefly described|p239|||||||||
3554|Cappanana Formation|39626|6|Mentioned|p275|||||||||
3554|Cappanana Formation|40328|3|Fully described|p60|||||||||
3554|Cappanana Formation|40689|6|Mentioned|p4|||||||||
3554|Cappanana Formation|41356|5|Briefly described|p42|||||||||
3554|Cappanana Formation|42497|5|Briefly described|Map legend|Ludlovian|Ludlovian|||||||
3554|Cappanana Formation|42727|5|Briefly described|map legend|Ludlow|Ludlow|Shale, siltstone and minor quartzite and tuff. Unconformable over Pittman Formation; underlies Colinton Volcanics. BMR map symbol: Scp. Geol. Prov: Canberra Block.||||||
3554|Cappanana Formation|42820|2|Defined|p39|early Ludlow||||||||
3554|Cappanana Formation|43233|5|Briefly described|Map Legend||Late Silurian|of Bredbo Group||||||
3554|Cappanana Formation|44093|5|Briefly described|p198 App. 1|Late Silurian|Late Silurian|In the Canberra Block. Geological Province: Lachlan Fold Belt.||||||
3554|Cappanana Formation|49690|4|Described|p1, p2, p4, p5, p27, p29 |Late Silurian|Late Silurian|Of Richardson (1979). Type section is between GR 992188 and GR982188 east of Bredbo; 700m thick.||||Gradationally overlain by the Colinton Volcanics or Rothlyn Formation.|Comprises shale and calcareous shale with numerous limestone lenses, minor sandstone and tuff.|
3554|Cappanana Formation|61895|6|Mentioned|p134 Fig.1|||||||||24-SEP-14
3554|Cappanana Formation|62070|5|Briefly described|p37, p38|Ludlow|Wenlock|||Bredbo Group.|[said to include the] Quidong Limestone Member.|Underlies the Colinton Volcanics.|Interbedded quartz arenite, siltstone and shale with laterally restricted limestone bodies.|
3554|Cappanana Formation|66197|5|Briefly described|p631 Fig.3c|Ludlow||Canberra-Yass and Ngunawal Basins. Overlain by Colinton Volcanics.||||||13-MAR-12
3554|Cappanana Formation|68592|6|Mentioned|p428|||Equivalent to, but not yet formally included in, the Douro Group.||||||
3554|Cappanana Formation|69635|6|Mentioned|p19|||||||Underlies Colinton Volcanics.||15-JUL-15
3563|Captains Flat Formation|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Interbedded slate and lithic tuff, thin basalt and dacite, sandstone. Overlies Kohinoor Volcanics. BMR map symbol: Suf.||||||
3563|Captains Flat Formation|22768|6|Mentioned|p177|||||||||
3563|Captains Flat Formation|22857|4|Described|p177, p474 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Hoskinstown Group. Shale, siltstone sediments with volcaniclastic interbeds. Max. thickness: 1200m. Geological Province: Captains Flat-Goulburn Trough.||||||
3563|Captains Flat Formation|23048|5|Briefly described|p3 fig5||Late Silurian|||||||
3563|Captains Flat Formation|24128|5|Briefly described|p35|||Geological Province: Lachlan Fold Belt.||||||
3563|Captains Flat Formation|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
3563|Captains Flat Formation|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
3563|Captains Flat Formation|30433|5|Briefly described|p695|||||||||
3563|Captains Flat Formation|31017|6|Mentioned|p45|||||||||
3563|Captains Flat Formation|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
3563|Captains Flat Formation|31020|5|Briefly described|p12|||Also mention Fig. 5.||||||
3563|Captains Flat Formation|31111|6|Mentioned|p112|||See also P114, 116, 120, 124, 126, 130, 134||||||
3563|Captains Flat Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
3563|Captains Flat Formation|32820|6|Mentioned|p3|||Hoskinstown Gp.||||||
3563|Captains Flat Formation|33325|5|Briefly described|Table 2|||||||||
3563|Captains Flat Formation|36413|2|Defined|p65|Late Silurian|Late Silurian|||||||
3563|Captains Flat Formation|36414|5|Briefly described|map legend|Pridolian|Ludlovian|Of Hoskinstown Group. Includes Sinclair Conglomerate Member and Yandyguinula Member. Overlies Carwoola Formation and Kohinoor Volcanics. GSNSW map code: Sf.||||||
3563|Captains Flat Formation|37727|4|Described|p44|||||||||
3563|Captains Flat Formation|39331|6|Mentioned|p52|||||||||
3563|Captains Flat Formation|40328|4|Described|p181|||||||||
3563|Captains Flat Formation|42497|5|Briefly described|Map Legend|Pridolian|Ludlovian|||||||
3563|Captains Flat Formation|42727|5|Briefly described|map legend|Pridoli|Ludlow|Of Hoskinstown Group. Includes Sinclair Conglomerate Member. Shale, siltstone, acid and basic volcanic flows and tuff. Over Kohinoor Volcanics and Copper Creek Shale; interfingers with Carwoola Fm. BMR map symbol: Suf. Geol. Prov: Captains Flat Block.||||||
3563|Captains Flat Formation|42820|2|Defined|p50|Late Silurian|Late Silurian|of Hoskinstown Group||||||
3563|Captains Flat Formation|43472|14|Not recorded|p420, fig.1|||||||||
3563|Captains Flat Formation|48878|2|Defined|p.8-11||Late Silurian|On many pages. p.7,5,15-17,19,20,22-24,26-28,39,44,45,Pl.3,4. 2500'- over 4000', O/lies Kohinoor Volcs & Carwoola Beds. U.Silurian. Fig.3.||||||
3563|Captains Flat Formation|66197|5|Briefly described|p631 Fig.3c|||Canberra-Yass and Ngunawal Basins. Mixed mafic/silicic volcanics and clastics. In the Hoskinstown Group. Overlies the Carwoola and Kohinoor Formations.||||||13-MAR-12
3563|Captains Flat Formation|68592|5|Briefly described|p732, p744, p1160|||Richardson (1979). Occurs in the Canberra and Michelago 1:100 000 map sheet areas. Deep water conformable sequence.||Hoskinstown Group|Includes Sinclair Conglomerate Member.||Shale and siltstone-rich, also contains volcanic rocks.|
3563|Captains Flat Formation|69270|5|Briefly described|p4, p9|Late Silurian|Late Silurian|||||a klippe of Ordovician Abercrombie Formation has been structurally emplaced above Late Silurian Captains Flat Formation||
3563|Captains Flat Formation|69635|4|Described|p32-42, 46|Lochkovian|Wenlock|Eastern Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation age. Dacite and rhyolite sampled. Rhyolite in close proximity to Cu mineralisation. Ages indicate unit deposited over a time interval of at least several million years.|419.6+/-2.7 Ma; 428.1+/-2.9 Ma|Of Hoskinstown Group.||Younger dacite sample compared with dacite from Rothlyn Formation, and rhyolite from Woodlawn Volcanics.|Cream-grey, often brecciated/pseudo-brecciated dacite interbedded with feldspar-rich volcanogenic sandstone with diffuse layering, lithic clasts including cherts; White to pink-grey, fine-grained quartz and feldspar-phyric rhyolite; Grey-khaki shale|
3563|Captains Flat Formation|71069|3|Fully described|p10, p21 fig 7, p23, p25, p26, p27|Ludlow|Wenlock|Named for the township of Captains Flat. Previously known as the Captains Flat Beds. Previous type section mentioned and a new type area is proposed, other representative sections also mentioned. Includes a number of unnamed volcanic members. Estimated thickness ranges from 500m to in excess of 2 kms. Hosts the Anembo Gossan Zn, Pb, Cu, Au deposit and the Clare Zn, Pb, Cu prospect. Fossil evidence corroborates SHRIMP U-Pb age.  Distribution, fossil assemblage, geochemistry, tectonic structure, metamorphism and geophysical characteristics discussed. Lithology (including that of unnamed members) is discussed in detail. Equivalent to the De Drack Formation.  Part equivalent of the Kildrummie Formation and Kohinoor Volcanics.  Intruded by the Briars Sharrow Gabbro. Unnamed basalt in this formation is equivalent to the Currawang Basalt and the mafic phase of the Lockhart Igneous Complex. See also p29, p29 fig 11, p30, p33, p38 fig 15, p39 fig 16, p43, p45, p50 tbl 3, p99 fig 30, p100, p101 fig 31, p101, p102-104 fig 32, p105-119, p125, p146, p162, p179, p185, p197.|428.1 +/- 2.9 Ma (SHRIMP U-Pb)|Hoskinstown Group|Includes the Newtown Bed, Yandyguinula Member and the Sinclair and Rutledge Conglomerate Members.|Unconformably overlies (or is faulted against) the Abercrombie Formation. Overlies the Rutledge Conglomerate Member. Overlain by the Carwoola Formation. Interbedded with the Kohinoor Volcanics.|Mudstone, siltstone,shale,that is interbedded with fine-grained lithic sandstone. Basal conglomerates, pillow basalt lenses and thinly laminated, micritic to crystalline limestones also occur.|
3563|Captains Flat Formation|71691|5|Briefly described|Map legend.|Silurian|Silurian|Six un-named facies (trachyte, basalt, dacite, rhyolite, volcanilithic sandstone, limestone) are mapped separately.||Hoskinstown Group.|Sinclair Conglomerate Member, Rutledge Conglomerate Member.|Is overlain by Carwoola Formation. Encloses/is interbedded with Kohinoor Volcanics.|Laminated siltstone interbedded with quartzose to feldspar-lithic quartz sandstone, with minor bedded to fossiliferous limestone and calc-arenite; lesser trachyte, dacite, rhyolite lava, volcanic-derived sandstone and polymictic conglomerate.|
3563|Captains Flat Formation|71700|5|Briefly described|p15|Early Devonian|Silurian|Potentially contains early Devonian Bindook Group correlatives.|||Conformably overlies the Carwoola Formation.|||
3566|Caragabal Granite|24417|3|Fully described|p103|Early Devonian|Early Devonian|Intrudes Kirribilli Formation.||||||
3566|Caragabal Granite|29907|2|Defined|Appendix 1|Early Devonian|Early Devonian|Prob.Early Devonian||||||
3566|Caragabal Granite|29910|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
3566|Caragabal Granite|36411|6|Mentioned|p268|||Refers Bowman 1977.||||||
3566|Caragabal Granite|40328|4|Described|p204|||||||||
3566|Caragabal Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
3566|Caragabal Granite|60009|5|Briefly described|Map Legend|Lochkovian|Pridoli|||||||13-JUL-04
3566|Caragabal Granite|60548|5|Briefly described|map legend|Silurian|Silurian|Granite.||||||
3566|Caragabal Granite|71040|6|Mentioned|p16|Devonian|Devonian|Currowong Syncline.||||||
3588|Carcoar Granodiorite|22503|5|Briefly described|p651, Fig.7 p650|Early Devonian|Silurian|||||||
3588|Carcoar Granodiorite|22679|3|Fully described|p 46, 47|||||||||
3588|Carcoar Granodiorite|22798|5|Briefly described|p851 Table.1|Early Devonian|Late Silurian|Age: Rb/Sr 407 +/- 4Ma.||||||
3588|Carcoar Granodiorite|23100|5|Briefly described|p575 (Fig 1)||Silurian|||||||
3588|Carcoar Granodiorite|23202|6|Mentioned|p1059, Fig.1||Late Silurian|||||||
3588|Carcoar Granodiorite|23214|3|Fully described|p171|Late Silurian|Late Silurian|Originally named Carcoar Granite and included two sub units; Stokefield Diorite (see Stokefield Metagabbro) and Long Hill Diorite (obselete).  Intrudes the Coombing Formation and Stokefield Metagabbro.||||||
3588|Carcoar Granodiorite|24266|5|Briefly described|p1476|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
3588|Carcoar Granodiorite|42802|5|Briefly described|p104|||||||||
3588|Carcoar Granodiorite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Consists of hornblende biotite granodiorite and tonalite.||||||15-JUL-08
3588|Carcoar Granodiorite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Hornblende biotite granodiorite and tonalite.||||||17-JUL-08
3588|Carcoar Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|||||||
3588|Carcoar Granodiorite|63286|6|Mentioned|p300|Early Silurian|Early Silurian|Age: 430+/-5Ma (U-Pd SHRIM: Kovacs 2000).||||||07-FEB-11
3588|Carcoar Granodiorite|63290|6|Mentioned|p403|Early Silurian|Early Silurian|Age: ca 433Ma (U/Pb . Lennox et al. 2005).||||||
3588|Carcoar Granodiorite|66713|5|Briefly described|p13|Telychian|Aeronian|Adjacent to the large Browns Creek Au-Cu skarn. Two U-Pb SHRIMP zircon dates; 430.4 +/- 4.7 Ma (Kovacs, 2000) and 434.4 +/- 5.5 Ma (Lennox et al., 2005). Called Carcoar Granite on p13.||||||
3588|Carcoar Granodiorite|67806|5|Briefly described|p109, p110|Silurian|Silurian||430.4 +/- 4.7 Ma (SHRIMP).|Unit in Browns Creek Intrusive Complex|||Consists of strongly zoned plagioclases, primary amphibole, with late-crystallizing quartz and alkali feldspar.|
3588|Carcoar Granodiorite|69539|5|Briefly described|p608 Fig.1, p614|Silurian|Silurian|Dating by K-Ar, 40Ar/39Ar and Rb-Sr on hornblende and biotite consistently produce ages of 416-407 Ma; reflects resetting due to Bowning event.|434.4 +/- 5.5 Ma (U-Pb zircon).|||||03-MAY-16
3588|Carcoar Granodiorite|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Unassigned Silurian I-type intrusion. Associated skarn-type mineralisation (gold-copper). Age: mid Silurian.|||||I-type.|
3588|Carcoar Granodiorite|73431|5|Briefly described|p363 Fig.1, p364, p367 Tb.1|Devonian|Silurian|Original name for the Browns Creek Intrusive Complex (Pogson and Watkins, 1998). Covers most parts of the intrusive complex. Previous ages include 429.8+/-3.4 Ma zircon U/Pb SHRIMP (Kovacs, 2000), 416+/-2.2 Ar/Ar hornblende, 413+/-8 Ma and 414+/-8 Ma Ar/Ar biotite (Perkins et al., 1995b), 407+/-4 Ma Rb/Sr biotite (Lennox et al., 1998) and 426.6 +/-2.3 Ma zircon Pb-evaporation (Lennox et al., 2005). Appears as 'Carcoar Granodiorite' p364.|434.4+/-5.5 Ma SHRIMP U/Pb, 407+/-4.0 Rb/Sr|Browns Creek Intrusive Complex|||Granodiorite.|
3604|Carellan beds|31519|6|Mentioned|p910|||||||||
3610|Cargo Creek Limestone|22857|5|Briefly described|p424 App.1 Tb.A1.5|Ordovician|Ordovician|Of the Barrajin Group. Thick-bedded to massive, bioclastic limestone, limey mudstone. Max. thickness: 400m.||||||
3610|Cargo Creek Limestone|23213|6|Mentioned|p21||Eastonian|Age: Late Eastonian. Informal division to upper Cargo Creek Limestone have Quepora calamus fossil assemblage.||||||
3610|Cargo Creek Limestone|23214|3|Fully described|p50|Eastonian|Eastonian|Of Barrajin Group. Mostly composed of massive, dark grey limestone.  Max. thickness 400m||||||
3610|Cargo Creek Limestone|24398|6|Mentioned|p264|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
3610|Cargo Creek Limestone|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3610|Cargo Creek Limestone|32156|6|Mentioned|p232|||Refers fossil content||||||
3610|Cargo Creek Limestone|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3610|Cargo Creek Limestone|32672|6|Mentioned|p672|||||||||
3610|Cargo Creek Limestone|32821|6|Mentioned|p10|||||||||
3610|Cargo Creek Limestone|33006|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle and Upper OrdovicianM - U||||||
3610|Cargo Creek Limestone|33282|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle to Upper OrdovicianM - U||||||
3610|Cargo Creek Limestone|33735|6|Mentioned|p206|||||||||
3610|Cargo Creek Limestone|33740|6|Mentioned|p125|||||||||
3610|Cargo Creek Limestone|33741|6|Mentioned|Fig.1|||Ord. Fauna.||||||
3610|Cargo Creek Limestone|34404|4|Described|p81|||||||||
3610|Cargo Creek Limestone|34575|6|Mentioned|p659|||Ordovician. See also PP637,638,639 etc.||||||
3610|Cargo Creek Limestone|34576|6|Mentioned|p345|||Fauna||||||
3610|Cargo Creek Limestone|34692|6|Mentioned|p184|||||||||
3610|Cargo Creek Limestone|35118|6|Mentioned|Fig.5|||||||||
3610|Cargo Creek Limestone|38219|6|Mentioned|p304|||See also Table 2.||||||
3610|Cargo Creek Limestone|39325|6|Mentioned|p431|||||||||
3610|Cargo Creek Limestone|39657|6|Mentioned|M30|||||||||
3610|Cargo Creek Limestone|40127|6|Mentioned|p9|||||||||
3610|Cargo Creek Limestone|40136|5|Briefly described|p20|||||||||
3610|Cargo Creek Limestone|40328|6|Mentioned|p115|||||||||
3610|Cargo Creek Limestone|42479|6|Mentioned|p111|||||||||
3610|Cargo Creek Limestone|43385|14|Not recorded|p169|Late Ordovician|Early Ordovician|Ref.to Stevens 1957||||||
3610|Cargo Creek Limestone|43479|14|Not recorded|p95f|Caradocian|Llandeilian|||||||
3610|Cargo Creek Limestone|43515|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(Provisional Edition)  (M.-U.Ord)||||||
3610|Cargo Creek Limestone|43516|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(M.-U.Ord)||||||
3610|Cargo Creek Limestone|43569|6|Mentioned|p475||Late Ordovician|||||||
3610|Cargo Creek Limestone|43640|5|Briefly described|Map Legend||Ordovician|||||||
3610|Cargo Creek Limestone|43782|5|Briefly described|Map Legend|Eastonian|Eastonian|of Barrajin Group.||||||
3610|Cargo Creek Limestone|44086|14|Not recorded|p97-8,104,107,Pl.IV|Early Silurian|Late Ordovician|See also Lexicon.||||||
3610|Cargo Creek Limestone|48926|6|Mentioned|p34|||P34 et seq.||||||24-FEB-10
3610|Cargo Creek Limestone|67322|6|Mentioned|p23|Katian|Katian|Did not accumulate until Eastonian 2 time, extending into the late Eastonian. Synonymous with the Canomodine Limestone.||||||
3610|Cargo Creek Limestone|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
3610|Cargo 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 Cargo Ck Limestone.||Cabonne Group||||
3610|Cargo Creek Limestone|70754|6|Mentioned|p448|||||||||
3610|Cargo Creek Limestone|71091|6|Mentioned|p148|Ordovician|Ordovician|See also reference to Cargo Limestone (p146).||||||
3610|Cargo Creek Limestone|73209|5|Briefly described|p880|Late Ordovician|Late Ordovician||||||Massive grey limestones.|
3610|Cargo Creek Limestone|73492|6|Mentioned|p706|||Now synonymised into Canomodine Limestone (Percival et al., 2011, p23).||||||
3613|Cargo Volcanics|36534|6|Mentioned|p223|||||||||
3613|Cargo Volcanics|43357|14|Not recorded|155-161||Early Ordovician|||||||
3613|Cargo Volcanics|63277|5|Briefly described|p139|Ordovician|Ordovician|Dominat lithology is medium-K basaltic to dacitic lavas. Produced in a single edifice and has distinctively higher Zr/Nb values than most other volcanics of the Maquarie Arc. Geological Province: Lachlan Fold Belt.||||||
3613|Cargo Volcanics|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p153|Late Ordovician|Middle Ordovician|Overlain by Bowan Park Limestone Subgroup. Geological Province: Molong Volcanic Belt, LFB. Contains no fossils.||||||07-FEB-11
3613|Cargo Volcanics|63283|5|Briefly described|p191 Tb. 2, p195 Fig. 2, p209|Late Ordovician|Early Ordovician|Overlain by Bowan Park Subgroup. Age: 465-450Ma . Consist of basaltic andestie with subordinate evolved andesites and felsic lavas and pumice breccias + volcaniclastic sediments.  Geol Prov: Molong Volcanic Belt. See p198-199.||||||07-FEB-11
3613|Cargo Volcanics|63284|6|Mentioned|p249|Darriwilian|Darriwilian|Geological Province: Molong Volcanic Belt.||||||
3613|Cargo Volcanics|63286|6|Mentioned|p310, p308 Fig. 9|Late Ordovician|Middle Ordovician|Consists of medium-K calc-alkaline composition. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
3613|Cargo Volcanics|63287|4|Described|p317 Fig. 2, p320-333, p336-343|Late Ordovician|Middle Ordovician|Of the Kenilworth Group. Overlain by Bowan Park  Limestone Sub-group and Malachis Hill Formation. Thickness: 2800 m. Consists of volcaniclastic rocks, coherent basalt, andesite. See also p320-333 and p336-343 for detailed information of petrology.||||||07-FEB-11
3613|Cargo Volcanics|63290|6|Mentioned|p389, p396 Fig. 3|Gisbornian|Middle Ordovician|Geological Province: Molong Volcanic Belt.||||||
3613|Cargo Volcanics|63293|5|Briefly described|p470, p469 Fig. 2, p473|Gisbornian|Darriwilian|Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
3613|Cargo Volcanics|64295|5|Briefly described|p198 Fig. 1, p201|||Overlain by Bowan Park Limestone Subgroup. Successions of volcaniclastic-dominated rocks. On the Molong Volcanic Belt.||||||01-SEP-08
3613|Cargo Volcanics|64963|5|Briefly described|p181, p182 Fig. 2|Late Odovician|Middle Ordovician|Age: ca 466-454Ma. Comprises mainly medium-K calc-alkaline volcanic rocks. See also p183.||||||22-APR-09
3613|Cargo Volcanics|67106|6|Mentioned|p673, 675-679, 681-683|||Molong Volcanic Belt. Age range 476-455 Ma.|463.4 +/- 3.4 Ma.|||Is overlain by Ranch Member (Daylesford Limestone).||
3613|Cargo Volcanics|67107|6|Mentioned|p694-695, 701|||Hosts the Cargo porphyry-style Cu-Au deposits; mineralisation is associated with dacitic intrusions. MDA is from a zircon in a mid-Eastonian sandstone unit. Mineralisation was at 462 +/- 9 Ma.|453 Ma (MDA).||||Dominantly basaltic andesite sequence; subordinate evolved andesites and more felsic lavas and pumice breccias that grade up-sequence into volcaniclastic sediments.|
3613|Cargo Volcanics|67322|4|Described|p20 Fig.5, p22-23|Katian|Ordovician|Macquarie Arc. Although Morgan, Scott and Krynen (in Pogson and Watkins, 1998) advocated for the Cargo Andesite to be replaced by the Fairbridge Volcanics, the studies of Simpson et al. (2007) and Crawford, Meffre et al. (2007), have shown that the Cargo Volcanics are distinct geochemically from the Fairbridge Volcanics. The name Cargo Volcanics (modified after Stevens 1950) is thus reinstated. Age is determined from p20 Fig.5 (Strat. column); minimum age not well constrained. Occurs in the Bowan Park region and South of Canomodine.||Of the Cabonne Group.||Overlain unconformably by the Bowan Park Limestone Subgroup or Canomodine Limestone.|Succession of lavas and volcaniclastics.|21-FEB-18
3613|Cargo Volcanics|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
3613|Cargo 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. Hosts Cargo U-Au system. Molong Volcanic Belt.|c. 470-455 Ma|Cabonne Group||||
3613|Cargo Volcanics|70684|5|Briefly described|p3, p12-13, p33-40, p75|Late Ordovician|Middle Ordovician|Southern Molong Volcanic Belt. Preserves all the attributes of a (thrust-faulted) stratovolcano with a basal diameter of at least 25-30km. Lithologies well-described and illustrated.|c.465 Ma.|||Is overlain unconformably by Bowan Park Subgroup.|A basaltic andesite-dominated succession of massive and pillow lava, volcanic breccia, high-level porphyritic sills and dykes, and a smaller volume of volcaniclastic rocks interpreted as turbidites and debris-flow deposits.|
3613|Cargo Volcanics|70754|6|Mentioned|p450 Fig.2|Late Ordovician||||||Is overlain ?unconformably by Cliefden Caves Limestone Subgroup.||
3613|Cargo Volcanics|72495|5|Briefly described|p231, p235|Gisbornian|Darriwilian|Of the Molong Volcanic Belt, 70-100km to the southeeast of the London-Victoria Shear zone. Geochemically similar to the Parkes Volcanics in the vicinity of the London-Victoria gold mine.||||||
3613|Cargo Volcanics|73154|5|Briefly described|p75, p77 Fig.3|Gisbornian|Darriwilian|Macquarie Arc, Phase 2. Molong belt, western. Medium-K volcanics.|||||Intermediate-mafic lavas, volcaniclastic rocks including conglomerate with dacitic clasts at top of unit.|
3613|Cargo Volcanics|73210|6|Mentioned|p893 Fig.2|||||||||
3613|Cargo Volcanics|73492|5|Briefly described|p707|||Molong Volcanic Belt.||||Underlies Bowan Park Limestone Subgroup||
3651|Caroda Formation|721|5|Briefly described|Map legend|Namurian|Namurian|Contains the Barneys Spring Andesite Member.  Crossbedded sandstone,minor lenticular oolitic limestone and magnetite sandstone, succeeded by coarse fluvial litharenite, minor pebbly sandstone, shale, thin coal, conglomerate, rare andesitic tuff.||||||21-DEC-04
3651|Caroda Formation|22857|4|Described|p496 App.1 Tb.A1.7|Visean|Visean|Crossbedded arenite, minor lenticular oolitic limestone amd magnetite arenite. Max. thickness: 650m. Geological Province: Tamworth Forearc Basin.||||||
3651|Caroda Formation|23050|5|Briefly described|p9 Fig.2, p31|Early Carboniferous|Early Carboniferous|||||||
3651|Caroda Formation|23051|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of Tamworth Belt.||||||14-APR-08
3651|Caroda Formation|23185|6|Mentioned|Fig1p156|Carboniferous|Carboniferous|||||||
3651|Caroda Formation|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt.||||||14-APR-08
3651|Caroda Formation|23861|5|Briefly described|p3, p4 Fig. 2|Visean|Visean|Geological Province: New England Orogen.||||||
3651|Caroda Formation|24010|5|Briefly described|p379|Early Carboniferous|Early Carboniferous|||||||
3651|Caroda Formation|24348|5|Briefly described|p131, p133|Carboniferous|Carboniferous|||||||
3651|Caroda Formation|24366|5|Briefly described|p5, 17 Fig. 3|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt.||||||
3651|Caroda Formation|24603|5|Briefly described|p866|Visean|Visean|In the Rocky Creek Block.  Geological Province: Tamworth Belt.||||||
3651|Caroda Formation|24605|2|Defined|p931, p947 App.1|Visean|Visean|Disconformably overlain by the Spion Kop Conglomerate. Maximum Thickness: 640m. Geological Province: New England Orogen.||||||
3651|Caroda Formation|30133|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
3651|Caroda Formation|30135|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
3651|Caroda Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
3651|Caroda Formation|31586|6|Mentioned|p6|||Equiv. in part to Cannindah Lst.||||||
3651|Caroda Formation|31802|6|Mentioned|p142|||Unconformities. Refers McKelvey (1966)||||||
3651|Caroda Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
3651|Caroda Formation|32866|6|Mentioned|p22|||Fossil content||||||
3651|Caroda Formation|32867|6|Mentioned|p67|||||||||
3651|Caroda Formation|34072|6|Mentioned|Fig.4.5|||Carb. Fossils||||||
3651|Caroda Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
3651|Caroda Formation|34086|6|Mentioned|p262|||Assemblages||||||
3651|Caroda Formation|34349|4|Described|p246|||||||||
3651|Caroda Formation|36528|6|Mentioned|p178|||See also P179.||||||
3651|Caroda Formation|37919|6|Mentioned|p477|||||||||
3651|Caroda Formation|37987|2|Defined|p230|late Visean|late Visean|||||||
3651|Caroda Formation|38222|5|Briefly described|p358|||||||||
3651|Caroda Formation|39331|6|Mentioned|Table 10-1|||||||||
3651|Caroda Formation|41009|6|Mentioned|Fig.2|||||||||
3651|Caroda Formation|41990|5|Briefly described|p5|||||||||
3651|Caroda Formation|42002|6|Mentioned|p94|||||||||
3651|Caroda Formation|42547|4|Described|p18|Visean|Visean|Rocky Creek Syncline. Age: middle to late Visean.||||||14-APR-08
3651|Caroda Formation|42631|5|Briefly described|Fig.1 P265|||||||||
3651|Caroda Formation|42728|4|Described|p8|||See also Fig 1, P2||||||
3651|Caroda Formation|43091|5|Briefly described|Map legend|||||||||
3651|Caroda Formation|43383|14|Not recorded|p17|||||||||
3651|Caroda Formation|43421|4|Described|p677||Carboniferous|||||||
3651|Caroda Formation|43429|14|Not recorded|Map Legend|||Has a basal paralic facies, marine transgressive facies,and upper paralic and fluvial facies||||||
3651|Caroda Formation|43434|4|Described|Map Legend||Carboniferous|||||||
3651|Caroda Formation|43435|2|Defined|Map Legend||Carboniferous|||||||
3651|Caroda Formation|43436|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
3651|Caroda Formation|43479|14|Not recorded|p159,177|Namurian|Visean|||||||
3651|Caroda Formation|43538|14|Not recorded|p2|||Lower Carboniferous fauna||||||
3651|Caroda Formation|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||01-MAR-05
3651|Caroda Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
3651|Caroda Formation|46803|6|Mentioned|Fig. 3|||||||||
3651|Caroda Formation|47056|6|Mentioned|Fig.2 P523|||||||||
3651|Caroda Formation|50613|5|Briefly described|p206 Fig. 2|Carboniferous|Carboniferous|Includes Barneys Springs Andesite Member.  See also p208 Fig. 3 and p210 Fig. 4.||||||
3651|Caroda Formation|50629|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Includes: Barneys Spring Andesite Member.  Geological Province: New England Orogen.||||||
3651|Caroda Formation|60299|5|Briefly described|p212 Fig.2c|Carboniferous|Carboniferous|Geological Province: Rocky Creek Block.||||||
3651|Caroda Formation|61214|6|Mentioned|p170, p171 Fig. 1|Visean|Visean|Geological Province: Boomi Block. See also p172 Fig. 2. ||||||
3651|Caroda Formation|61767|4|Described|p71|Visean|Visean|Geological Province: Tamworth Belt. Max. thickness: 490m.||||||
3651|Caroda Formation|61769|6|Mentioned|p99 Fig. 4|||||||||
3651|Caroda Formation|61776|5|Briefly described|p194 Fig. 3|Early Carboniferous|Early Carboniferous|Geological Province: New England Orogen. Sandstone, conglomerate, siltstone, minor coal and limestone.||||||
3651|Caroda Formation|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Devonian|Geological Province: Tamworth Belt.||||||10-DEC-07
3651|Caroda Formation|63832|6|Mentioned|p131 fig 2|Visean|Visean|Rocky Creek Syncline, Southern New England Fold Belt.||||||
3651|Caroda Formation|64631|5|Briefly described|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt, Rocky Creek Syncline.  Some biostratigraphic and radiometric age control within unit. ||||Overlies Namoi Formation.|Includes oolitic limestone interval.|
3651|Caroda Formation|65107|6|Mentioned|P276, Fig 4 p279||Late Paleozoic|Member of the Rocky Creek Block. No age given||||||
3651|Caroda Formation|65382|5|Briefly described|p714|Visean|Visean|Includes Barney Springs Andesite [Member]. Maximum age from Barney Springs Andesite, minimum age from occurrence of 'middle to late Visean' (calibrated as 335-330 Ma) conodonts overlying the Barney Springs Andesite. Underlies Spion Kop Conglomerate.||||||07-MAR-12
3651|Caroda Formation|65902|5|Briefly described|p203|Carboniferous|Carboniferous|Includes Barneys Springs Andesite Member. Volcanics.||||||09-MAR-12
3651|Caroda Formation|66720|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous||||An un-named unit of massive, fine-grained limestone is mapped separately.||Cross-bedded fossiliferous sandstone, coarse-grained fluvial lithic sandstone; minor pebbly sandstone, shale and conglomerate.|
3651|Caroda Formation|68003|5|Briefly described|p32 Fig.3-h, p34 Photo.3-e, pp137-138.|Visean|Visean|Tamworth Belt (North), New England Fold Belt.|||Includes Barneys Springs Andesite Member.|Overlies Namoi Formation. Is overlain by Spion Kop Conglomerate.|Cross-bedded lithic arenite and conglomerate; subordinate laminated shale, siltstone, lenticular oolitic limestone, magnetite horizons; then coarse fluvial litharenite, minor pebbly sandstone, shale, thin coal, conglomerate and andesite tuff.|
3651|Caroda Formation|68004|6|Mentioned|p137.|||Titanomagnetite has been noted in sandstone in this unit, but not evaluated in any detail.||||||
3651|Caroda Formation|68005|5|Briefly described|p49 Fig.3-M, p56, pp145-146, p170.|Visean|Visean|Rocky Creek Block, Tamworth Belt. A marine to terrestrial transition sequence.|||Includes Barneys Springs Andesite Member, Garrambeel Sandstone Member, West Lynne Andesite Tuff, Yunedoo Andesite Tuff.|Overlies Namoi Formation.|Cross-bedded lithic arenite and conglomerate, subordinate laminated shale, siltstone, lenticular oolitic limestone, magnetite horizons; overlain by coarse fluvial litharenite, minor pebbly sandstone, shale, thin coal, conglomerate and andesitic tuff.|
3651|Caroda Formation|68006|6|Mentioned|p115.|||Tamworth Belt. Contains extensive but thin and impure beds of limestone.||||||
3651|Caroda Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Rocky Creek Block, Tamworth Belt.||||||
3651|Caroda Formation|70050|5|Briefly described|p329-331, p352, p354-355, p357,p365,p367|Visean|Visean|Willeroi Station. Contains Cionodendron and Australastraea coral fossils (illustrations and systematic palaeontology), including the holotype of A. columellaris. |||||Includes fossiliferous limestone beds.|
3651|Caroda Formation|70728|5|Briefly described|p265,271-273|Visean|Visean|Geological province: North Tamworth terrane, New England Orogen.||||Overlain by Clifden Formation or Spion Kop Conglomerate. Underlain by Namoi Formation.||
3651|Caroda Formation|70907|6|Mentioned|p774 Fig.2|||||||||
3671|Carrai Granodiorite|23720|5|Briefly described|Map Legend|Early Triassic|Early Triassic|hornblende-biotite granodiorite and monzogranite, minor biotite leucogranite.||||||15-DEC-04
3671|Carrai Granodiorite|35664|6|Mentioned|p113|||Age dates.||||||
3671|Carrai Granodiorite|38842|6|Mentioned|p286|||||||||
3671|Carrai Granodiorite|38916|6|Mentioned|p346|||||||||
3671|Carrai Granodiorite|40590|6|Mentioned|p333|||||||||
3671|Carrai Granodiorite|40762|6|Mentioned|p297|||||||||
3671|Carrai Granodiorite|41347|6|Mentioned|p376|||||||||
3671|Carrai Granodiorite|42659|6|Mentioned|p119|||||||||
3671|Carrai Granodiorite|44450|5|Briefly described|p35|Middle Triassic|Middle Triassic|Geological Province: New England Fold Belt.||||||
3671|Carrai Granodiorite|61772|6|Mentioned|p132|||Age: 224-226 and another age 242+/-11Ma (Honma et al, 1988).||||||
3671|Carrai Granodiorite|68111|5|Briefly described|p969 Tb.1|Carnian|Carnian||227 - 224 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Round Mountain Supersuite.||||16-OCT-14
3671|Carrai Granodiorite|69188|6|Mentioned|p32|Late Triassic|Late Triassic||~231-228 Ma (Leitch and McDougall, 1979).|||||
3671|Carrai Granodiorite|69639|5|Briefly described|p3, p6, p8,p118-p124|Triassic|Triassic|New England Orogen. Sampling locality, petrography and geochronology are discussed. Rb-Sr dating places the age range between 226-224 Ma (Shaw, 1994). See also p128, p223-p224, p238.|229.7 +/- 1.3 Ma (SHRIMP U-Pb)|Carrai Suite|||Massive, medium- to coarse-grained, inequigranular, biotite-hornblende granite.|
3671|Carrai Granodiorite|71628|4|Described|p17: 2, 13, 15, 17, 19-27, 29, 44, 48|||See also p17: 71, 90, 98; p19-140. Gilligan et al. (1992). Previously Carrai Adamellite (Pogson and Hitchins, 1973) after unpublished work by Atkinson et al. (1969). Named after the locality of Carrai. Forms a ~18 x 12 km intrusion centred on Ovens Mountain, 65 km ESE of Uralla. Crops out as low rounded whalebacks. Geochemistry similar to Botumburra Range Granodiorite. Is spatially associated with numerous Sn, Au, Mo, Sb, Ag, As, Au and W deposits (named).|229.7 +/- 1.3 Ma (SHRIMP: Chisholm et al., 2014).|Carrai Suite.||Intrudes Pee Dee, Parrabel, and ?Nambucca beds. Encloses (?is intruded by) Daisy Plains Leucosyenogranite).|Medium-grained, porphyritic and equigranular, hornblende-biotite granodiorite and mafic to leucocratic monzogranite, crosscut by porphyritic and aplitic dykes. Abundant dioritic enclaves. I-type.|
3673|Carramere Coal Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Geological Province: Sydney Basin||||||
3673|Carramere Coal Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Lucernia Coal. Geological Province: Sydney Basin||||||
3673|Carramere Coal Member|29942|3|Fully described|p11|||||||||
3673|Carramere Coal Member|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Basal unit in Lucernia Coal.||Overlies Strathmore Formation. Is overlain by Hillsdale Claystone.||
3698|Carsonville Formation|32324|6|Mentioned|Table 8.1|||||||||
3698|Carsonville Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
3698|Carsonville Formation|35492|6|Mentioned|p141|||||||||
3698|Carsonville Formation|35856|5|Briefly described|p189|||||||||
3698|Carsonville Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
3698|Carsonville Formation|36599|6|Mentioned|Fig.1|||||||||
3698|Carsonville Formation|41348|5|Briefly described|Map legend|Carboniferous||||||||16-DEC-04
3698|Carsonville Formation|42547|4|Described|p34|||||||||
3712|Carwell Creek Formation|22529|6|Mentioned|4 fig 2|Emsian|Emsian|||||||
3712|Carwell Creek Formation|22590|6|Mentioned|Fig3 P754||Emsian|||||||
3712|Carwell Creek Formation|22857|4|Described|p474 App.1 Tb.A1.6|Emsian|Pragian|Of the Kandos Group. Lithic arenite, crinoidal lithic arenite, shale, basal limestone. Contains corals, stromatoporoids, brachiopods, conodonts. Max. thickness: 1050m. Geological Province: Capertee Rise.||||||
3712|Carwell Creek Formation|23043|5|Briefly described|Map Legend|Emsian|Emsian|of Kandos Group.||||||
3712|Carwell Creek Formation|23170|2|Defined|p136|Emsian||of Kandos Group.||||||
3712|Carwell Creek Formation|23214|3|Fully described|p205|Emsian|Pragian|Of Kandos Group. Originally Carwell Creeks beds. Max. thickness 1000m.||||||
3712|Carwell Creek Formation|23522|5|Briefly described|p248 Fig 4|Emsian|Pragian|||||||
3712|Carwell Creek Formation|24394|5|Briefly described|p171|Emsian|Pragian|Geological Province: Hill End Trough.||||||
3712|Carwell Creek Formation|42379|4|Described|p208, Fig.3 p203|||Intended as a redefinition ?of Carwell Creek Beds.||||||
3712|Carwell Creek Formation|43188|4|Described|p211,Table 3 p208||Emsian|Representative section location given. Age early to middle Emsian. Of Kandos Group.||||||
3712|Carwell Creek Formation|43641|5|Briefly described|Map Legend||Devonian|||||||
3712|Carwell Creek Formation|43782|5|Briefly described|Map Legend|Emsian|Emsian|of Kandos Group.||||||
3712|Carwell Creek Formation|44093|5|Briefly described|p212 App. 1|Early Devonian|Early Devonian|Of Kandos Group. See also p64 Photo 2. Overlain by Shoalhaven Group of Sydney Basin, with angular unconformity.||||||26-NOV-10
3712|Carwell Creek Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Cudgegong. Appears in text as Carwell Ck Formation. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3712|Carwell Creek Formation|68003|5|Briefly described|p24 Fig.3-e. |Emsian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Kandos Group.||||
3712|Carwell Creek Formation|70297|4|Described|map legend|Early Devonian|Early Devonian||||Brogans Creek Limestone Member||Lithic sandstone, crinoidal lithic sandstone, shale, fossiliferous limestone. Contains corals, stromatoporoids, brachiopods, conodonts.|18-MAY-16
3712|Carwell Creek Formation|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4, p1099|Early Devonian|Early Devonian|Capertree High. Onlaps onto Silurian unit in the east. Locations in text include p1100 Fig.5, p1101 Fig.7.||||Overlies the Riversdale Volcanics, Tanabutta Group, underlies the Buckaroo Conglomerate.||
3716|Carwoola Formation|22768|6|Mentioned|p177|||||||||
3716|Carwoola Formation|22857|4|Described|p177, p474 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Hoskinstown Group. Deep water sediments. Max. thickness: 1200m. Geological Province: Captains Flat-Goulburn Trough.||||||
3716|Carwoola Formation|23048|5|Briefly described|p3 fig5||Late Silurian|||||||
3716|Carwoola Formation|24128|5|Briefly described|p35|||Geological Province: Lachlan Fold Belt.||||||
3716|Carwoola Formation|32820|6|Mentioned|p3|||Hoskinstown Gp.||||||
3716|Carwoola Formation|36413|2|Defined|p64|Late Silurian|Late Silurian|||||||
3716|Carwoola Formation|36414|5|Briefly described|on cross-section only|Pridolian|Ludlovian|Of Hoskinstown Group. Underlies Captains Flat Formation; overlies Kohinoor Volcanics. Siltstone, shale, argillaceous sandstone. GSNSW map code: Sa.||||||
3716|Carwoola Formation|39626|6|Mentioned|p275|||||||||
3716|Carwoola Formation|40328|5|Briefly described|p181|||||||||
3716|Carwoola Formation|42727|5|Briefly described|map legend|Pridoli|Ludlow|Of Hoskinstown Group. Sandstone, siltstone, shale (proximal quartz turbidites). Overlies Kohinoor Volcanics and Copper Creek Shale; interfingers with Captains Flat Formation. BMR map symbol: Sur. Geol. Prov: Captains Flat Block.||||||
3716|Carwoola Formation|42820|2|Defined|p49|Late Silurian||of Hoskinstown Group||||||
3716|Carwoola Formation|66197|6|Mentioned|p631 Fig.3c|||Canberra-Yass and Ngunawal Basins. Deep marine shale and sandstone. In the Hoskinstown Group. Underlies the Captains Flat Formation, overlies the Kohinoor Formation and Copper Creek Shale.||||||15-JUL-15
3716|Carwoola Formation|68592|5|Briefly described|p743, p822, p834|||Covan Creek, Argyle and Carwoola Formations are probable correlatives, proposed by Huleatt (1971) and Davis (1990).||Hoskinstown Group||Overlies Copper Creek Shale, and ?Kohinoor Volcanics.|Turbidites.|
3716|Carwoola Formation|69270|5|Briefly described|p1, p2, p4, p9|Late Silurian|Late Silurian|||||conformably overlies Kohinoor Volcanics|lithic arenite|
3716|Carwoola Formation|69635|5|Briefly described|p11|||||||Overlies Kohinoor Volcanics. Correlated with Covan Creek Formation.||
3716|Carwoola Formation|71069|3|Fully described|p9, p21 fig 7, p24, p27, p30, p38 fig 15|Lochkovian|Ludlow|Named for the Carwoola Trigonometric Station. Previously termed the Carwoola Beds. Contains three unnamed packages. Type are nominated at GR 722726 6077118. Maximum exposed thickness of 2km, real thickness likely exceeds this; constituents are roughly 350m thick.  Possible source of gold in placer deposits near the map sheet (Captains Flat) area.Hosts the Woodlands Mine which is a small quartz vein associated orogenic gold deposit. Age derived from stratigraphic relationships. Interpreted to have been deposited in a marine environment above storm wave base. Distribution, geomorphology, primary structures/textures,  tectonic structure, metamorphism and geophysical characteristics discussed. Lithology discussed in detail. See also p41, p42, p43, p99 fig 30, p100, p101 fig 31, p103 fig 32, p105, p106, p111, p118, p120-124, p169. ||Hoskinstown Group||Overlies the Captains Flat Formation and Sinclair Conglomerate Member (which is also its lateral equivalent). Equivalent to the Covan Creek Formation.|Medium to coarse grained,thickly bedded, moderately sorted lithic arenite or quartz arenite interlayered with laminated siltstone or fine grained sandstone rich horizons.|
3716|Carwoola Formation|71691|5|Briefly described|Map legend.|Silurian|Silurian|Three un-named facies are mapped separately.||Hoskinstown Group.||Overlies Captains Flat Formation.|Medium- to very thick-bedded, medium- to coarse-grained sedlitharenite to quartz arenite and interbedded khaki to grey siltstone and laminated siltstone to very fine-grained quartz sandstone.|
3716|Carwoola Formation|71700|5|Briefly described|p15|Silurian|Silurian|||Hoskinstown Group||Equivalent to the Covan Creek Formation. Conformably overlain by the Captains Flat Formation.||
3779|Cataract River Member|22601|6|Mentioned|416|Permian|Permian|||||||
3779|Cataract River Member|39279|4|Described|p370,368|Late Permian|Late Permian|||Oldest member of Drake Volcanics.||||13-NOV-15
3779|Cataract River Member|41413|4|Described|p327|||||||||
3779|Cataract River Member|42378|6|Mentioned|Table 1 p10|||||||||13-NOV-15
3779|Cataract River Member|43017|6|Mentioned|p377|||of Drake Volcanics||||||
3787|Cathedral Group|12100|5|Briefly described|p819|Early Devonian|Early Devonian|Upward fining succession with an upward decrease in lithic content; very rapidly deposited.||Upper Group of the Yarra Supergroup.||||08-MAY-12
3787|Cathedral Group|22768|6|Mentioned|p188|||||||||
3787|Cathedral Group|22857|5|Briefly described|p188|Devonian|Devonian|Non-marine unit. Unconformably overlain by Marysville Igneous Complex; underlain by Walhalla Group.||||||
3787|Cathedral Group|23229|5|Briefly described|p25-6, 31, 35|Middle Devonian|Zlichovian|||||||
3787|Cathedral Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
3787|Cathedral Group|23309|5|Briefly described|p147, 154  Table 2.56|Middle Devonian|Early Devonian|||||||
3787|Cathedral Group|23522|5|Briefly described|p247 Fig 3|Devonian|Early Devonian|||||||
3787|Cathedral Group|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
3787|Cathedral Group|24098|5|Briefly described|p27 Fig. 2|Middle Devonian|Middle Devonian|Of the Murrindindi Supergroup. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
3787|Cathedral Group|24177|5|Briefly described|p13, p50 Fig.22, p60|Devonian|Devonian|Overlies the Walhalla Group. Geological Province: Mount Easton Province, Melbourne Trough.||||||
3787|Cathedral Group|24588|5|Briefly described|p12, 13, 15, 30, 33|Middle Devonian|Emsian|Conformably overlies Walhalla Group. Max Thickness: >2.5 km. Geological Province: Mount Easton Province. Unconformably underlies Marysville Igneous Complex.||||||29-NOV-13
3787|Cathedral Group|33238|4|Described|p642|||||||||
3787|Cathedral Group|35283|6|Mentioned|p46|||||||||
3787|Cathedral Group|40761|5|Briefly described|p234|||Mention P226||||||
3787|Cathedral Group|41585|4|Described|p115|||Mention p103, Fig 4.1.||||||06-JUN-06
3787|Cathedral Group|42827|4|Described|p115|||see also Table 4.1||||||
3787|Cathedral Group|44187|5|Briefly described|Map Legend||Middle Devonian|||||||
3787|Cathedral Group|60599|6|Mentioned|p14|Middle Devonian||Overlies Walhalla Group. ||||||
3787|Cathedral Group|61185|5|Briefly described|p14, p47, p24-25 Fig. 7, p21 Fig. 6|||Fluvial sediments. Overlies Montys Hut Formation (Walhalla Group).||||||07-FEB-11
3787|Cathedral Group|64612|6|Mentioned|p27|Middle Devonian|Early Devonian|Fluvial sandstones.||||||07-FEB-11
3787|Cathedral Group|64616|6|Mentioned|p156 Fig.6.5|Middle Devonian|Early Devonian|Overlies Walhalla Group.||||||
3787|Cathedral Group|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Walhalla. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3787|Cathedral Group|67804|5|Briefly described|p64|Early Devonian|Early Devonian|||||Overlies Jordan and Walhalla Groups conformably.||
3787|Cathedral Group|68116|5|Briefly described|Appendix, Maps 33, 42.|Emsian|Emsian||||||Fluvial: red and green sandstone, siltstone, conglomerate.|
3787|Cathedral Group|70629|6|Mentioned|p986|Middle Devonian|Early Devonian|Melbourne Zone. Mis-spelt as Cathederal Group in Fig.1.||||||
3787|Cathedral Group|70742|5|Briefly described|p161-163|||Non-marine deposits.||Murrindindi Supergroup.||Overlies Walhalla Group. Is overlain by Marysville Igneous Complex.||
3787|Cathedral Group|71040|6|Mentioned|p26|||Youngest unit in the Melbourne Zone to be deformed by the Tabberabberan Orogeny, but it lacks fossils for dating.||||||
3791|Catherine Hill Bay Formation|23055|6|Mentioned|Fig11p23|||||||||
3791|Catherine Hill Bay Formation|29922|6|Mentioned|p49|||||||||
3791|Catherine Hill Bay Formation|29926|6|Mentioned|Fig.3|||Permian||||||
3791|Catherine Hill Bay Formation|29942|4|Described|Fig.2|||Permian||||||
3791|Catherine Hill Bay Formation|31549|6|Mentioned|p159|||Stratigraphic succession||||||
3791|Catherine Hill Bay Formation|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
3791|Catherine Hill Bay Formation|33986|6|Mentioned|p30|||Table||||||
3791|Catherine Hill Bay Formation|34270|6|Mentioned|p254|||Table 1||||||
3791|Catherine Hill Bay Formation|34351|6|Mentioned|p348|||Fig.5.13||||||
3791|Catherine Hill Bay Formation|37083|6|Mentioned|p164|||||||||
3791|Catherine Hill Bay Formation|39292|6|Mentioned|Fig. 6.2|||||||||
3791|Catherine Hill Bay Formation|39308|6|Mentioned|p459|||||||||
3791|Catherine Hill Bay Formation|39609|6|Mentioned|Table 1|||||||||
3791|Catherine Hill Bay Formation|39666|6|Mentioned|Table 20|||||||||
3791|Catherine Hill Bay Formation|41463|6|Mentioned|Fig.1|||||||||
3791|Catherine Hill Bay Formation|41479|6|Mentioned|Fig.2|||||||||
3791|Catherine Hill Bay Formation|43344|14|Not recorded|p85||Permian|On table||||||
3791|Catherine Hill Bay Formation|43447|14|Not recorded|diag.p.26|||Part of Moon Island Beach Sub-Group||||||
3791|Catherine Hill Bay Formation|43448|14|Not recorded|p224,230||Permian|Unit of Moon Island Beach Subgroup (Newcastle Coal Measures)||||||
3791|Catherine Hill Bay Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Moon Island Beach Subgroup|Included Booragul Tuff Member, Teralba Conglomerate Member, Buff Point Coal Member, Toukley Coal Member, Mannering Park Tuff Member.|||
3797|Catombal Group|22451|5|Briefly described|p23|||||||||
3797|Catombal Group|22472|6|Mentioned|p47|||||||||
3797|Catombal Group|22857|5|Briefly described|p217, p490 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Comprises basal Black Rock Subgroup, and Canangle Subgroup. Max. thickness: >2km, 1580m in the south. Geological Province: Lambie Basin.||||||
3797|Catombal Group|22859|5|Briefly described|p213,217||Late Devonian|||||||
3797|Catombal Group|23043|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
3797|Catombal Group|23170|2|Defined|p245|Early Carboniferous|Late Devonian|Of Lachlan Fold Belt.||||||04-MAR-09
3797|Catombal Group|23213|5|Briefly described|p13, Fig.6|Late Devonian|Middle Devonian|||||||
3797|Catombal Group|23214|2|Defined|p232|Late Devonian|Late Devonian|Originally Catombal Formation.  Comprised of two subgroups; Canangle and Black Rock Subgroups. Max. thickness 1650m.||||||
3797|Catombal Group|23522|5|Briefly described|p248 Fig 4|Late Devonian|Late Devonian|||||||
3797|Catombal Group|23739|5|Briefly described|p213 Fig. 1|Late Devonian|Middle Devonian|||||||
3797|Catombal Group|24007|5|Briefly described|p337|Late Devonian|Late Devonian|||||||
3797|Catombal Group|24126|6|Mentioned|p172|||||||||
3797|Catombal Group|24233|5|Briefly described|p256, p258 Fig.6|Devonian|Devonian|Geological Province: Lachlan Orogen.||||||
3797|Catombal Group|24247|3|Fully described|p37|Late Devonian|Late Devonian|Comprises two major subgroups - Canangle and Black Rock Subgroups.||||||04-MAR-09
3797|Catombal Group|24580|6|Mentioned|p828 Fig.1|||Group is Gp in text. Geological Province: Eastern Lachlan Fold Belt.||||||
3797|Catombal Group|29362|6|Mentioned|Table 1|||Upper Devonian.||||||
3797|Catombal Group|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
3797|Catombal Group|30044|6|Mentioned|Fig.7|||||||||
3797|Catombal Group|30100|6|Mentioned|p205|||||||||
3797|Catombal Group|30139|5|Briefly described|Table 1|||||||||
3797|Catombal Group|30597|6|Mentioned|p29|||Unconformably overlies Garra Formation. Upper Devonian age||||||
3797|Catombal Group|31161|5|Briefly described|PA5|||||||||
3797|Catombal Group|31543|5|Briefly described|p117|||||||||
3797|Catombal Group|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
3797|Catombal Group|32151|6|Mentioned|p196|||U.Dev. Dominantly fluviatile||||||
3797|Catombal Group|32485|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
3797|Catombal Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
3797|Catombal Group|32672|6|Mentioned|p674|||||||||
3797|Catombal Group|32708|5|Briefly described|p407|||PP407-416||||||
3797|Catombal Group|32865|5|Briefly described|p483|||||||||
3797|Catombal Group|32986|5|Briefly described|p6|||Geological Map. Frasnian||||||
3797|Catombal Group|33006|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
3797|Catombal Group|33121|6|Mentioned|p90|||Middle Dev.? Middle-Late Dev.||||||
3797|Catombal Group|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
3797|Catombal Group|33285|5|Briefly described|p18|||Late Dev.||||||
3797|Catombal Group|33732|4|Described|p119|||See also P118 & Table II||||||
3797|Catombal Group|33871|4|Described|p2531|||||||||
3797|Catombal Group|34109|3|Fully described|p158|||Upper Devonian||||||
3797|Catombal Group|34403|6|Mentioned|p138|||Upper Devonian||||||
3797|Catombal Group|34404|6|Mentioned|Fig.3.3b|||||||||
3797|Catombal Group|34405|6|Mentioned|Fig.3.9|||||||||
3797|Catombal Group|34510|6|Mentioned|p304|||Upper Devonian. Fig.1.||||||
3797|Catombal Group|34567|6|Mentioned|p160|||Fig.1||||||
3797|Catombal Group|34895|6|Mentioned|Fig. 1|||||||||
3797|Catombal Group|35128|6|Mentioned|p361|||Appears on figure||||||
3797|Catombal Group|35185|6|Mentioned|p246|||||||||
3797|Catombal Group|35246|6|Mentioned|p165|||||||||
3797|Catombal Group|35258|6|Mentioned|p109|||||||||
3797|Catombal Group|35291|6|Mentioned|Fig.7|||||||||
3797|Catombal Group|35412|6|Mentioned|Fig.9|||Shows geology||||||
3797|Catombal Group|36534|6|Mentioned|p223|||||||||
3797|Catombal Group|37818|6|Mentioned|p82|||||||||
3797|Catombal Group|39331|6|Mentioned|p64|||See also P95||||||
3797|Catombal Group|40130|6|Mentioned|p195|||||||||
3797|Catombal Group|40132|6|Mentioned|p243|||||||||
3797|Catombal Group|40328|6|Mentioned|Plate 3|||||||||
3797|Catombal Group|42032|6|Mentioned|Fig.2 P490|||||||||
3797|Catombal Group|43039|4|Described|p9|||||||||
3797|Catombal Group|43188|5|Briefly described|p219||Late Devonian|Molong High.||||||
3797|Catombal Group|43263|6|Mentioned|Map Legend|Early Carboniferous|Middle Devonian|||||||
3797|Catombal Group|43344|14|Not recorded|p139,160-162||Late Devonian|||||||
3797|Catombal Group|43383|14|Not recorded|p12,15||Late Devonian|||||||
3797|Catombal Group|43461|14|Not recorded|table p621,625||Famennian|||||||
3797|Catombal Group|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
3797|Catombal Group|43479|14|Not recorded|132m,134m,151||Late Devonian|||||||
3797|Catombal Group|43507|14|Not recorded|p124-126,129||Late Devonian|||||||
3797|Catombal Group|43508|14|Not recorded|p117,125|||Includes Brymedura Sandstone||||||
3797|Catombal Group|43509|14|Not recorded|p111,114-5,Pl.I,II|||p117-9||||||
3797|Catombal Group|43510|14|Not recorded|p37,38,46|||||||||
3797|Catombal Group|43511|14|Not recorded|p129,139||Late Devonian|||||||
3797|Catombal Group|43512|2|Defined|p73,76-8,82-3,86,88,||Late Devonian|p92-3,95-106||||||
3797|Catombal Group|43513|14|Not recorded|p70-72|||Some red beds||||||
3797|Catombal Group|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)  Includes Canangle and Black Rock Sub Groups||||||
3797|Catombal Group|43516|14|Not recorded|Map Legend||Late Devonian|||||||
3797|Catombal Group|43522|5|Briefly described|p85-90||Late Devonian|||||||
3797|Catombal Group|43523|14|Not recorded|p427||Late Devonian|||||||
3797|Catombal Group|43525|14|Not recorded|map p124,Tb p126-7||Frasnian|||||||
3797|Catombal Group|43526|14|Not recorded|p547||Late Devonian|on map only||||||
3797|Catombal Group|43527|14|Not recorded|p518,521,544|||Overlies Garra Formation||||||
3797|Catombal Group|43528|14|Not recorded|p134||Late Devonian|||||||
3797|Catombal Group|43640|5|Briefly described|Map Legend||Devonian|||||||
3797|Catombal Group|43782|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
3797|Catombal Group|44093|5|Briefly described|p201 App. 1|Early Carboniferous|Late Devonian|||||||
3797|Catombal Group|50095|5|Briefly described|p107|Late Devonian|Late Devonian|Unconformbaly overlies Garra Limestone.||||||11-FEB-08
3797|Catombal Group|50097|5|Briefly described|p41|Late Devonian|Middle Devonian|Unconformably overlies Fairbridge Volcanics. Quartz-rich clastic rocks. Geological Province: Lachlan Orogen. NSW||||||07-FEB-11
3797|Catombal Group|50590|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Canangle Subgroup, Black Rock Subgroup.||||||
3797|Catombal Group|60987|6|Mentioned|p154 Fig.1, p155|Late Devonian|Late Devonian|||||||
3797|Catombal Group|63290|6|Mentioned|p401 Fig. 5(d)|Late Devonian|Late Devonian|||||||
3797|Catombal Group|64826|5|Briefly described|p1040 Tb. 1|Late Devonian|Late Devonian|Appears as the corrupted CatoMemberal Group in Table 1. Contains the Black Shale and Canangle Subgroup.||||||04-MAR-09
3797|Catombal Group|65214|6|Mentioned|p281|Devonian|Devonian|NSW, Manildra and Wellington. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
3797|Catombal Group|67823|6|Mentioned|p365|||||||||
3797|Catombal Group|67847|5|Briefly described|p60 fig 3.3.4|||Lambie Basin. Of the authors' proposed Kanimblan cycle. ||||||
3797|Catombal Group|68003|5|Briefly described|p24 Fig.3-e, pp141-142. |Famennian|Givetian|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Black Rock and Canangle Subgroups, Kurrool Formation and Curra Creek Conglomerate.|||
3797|Catombal Group|68298|5|Briefly described|p216|||With Lambie Group forms eastern province of Connolly (1965), in which basal equivalents of Beargamil Subgroup are marine.||||||
3797|Catombal Group|68592|5|Briefly described|p1722, p1737-8|Late Devonian|Late Devonian|One of a number of sequences (also Lambie and Hervey Groups) which were previously collectively referred to as "Lambie Series" and "Lambie Stage", following Browne (1929).|||Includes Macquarie park Sandstone.|||
3797|Catombal 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.||||||
3797|Catombal Group|70297|4|Described|map legend, on side 2 of map sheet|Famennian|Frasnian|Erosional base.|||Black Rock Subgroup, Carnangle Subgroup [misspelt Canangle]|Overlies Dulladerry Volcanics.|Massive to bedded, red to brown, purple and green quartz and lithic sandstone, siltstone, shale and conglomerate.|18-MAY-16
3797|Catombal Group|70684|6|Mentioned|p27 Fig.11, p50 Fig.24|Devonian|Devonian|||||||
3797|Catombal Group|71600|5|Briefly described|p22, p23 Fig 1|Devonian|Devonian|Geological province: Lachlan Fold Belt.|||Includes Curra Creek Conglomerate, Kurrool Formation and Macquarie Park Sandstone.|||
3797|Catombal Group|73299|6|Mentioned|p1103-1104, p1106 Fig.12|Famennian|Frasnian|Molong High. Unconformably overlies Ordovician units west of Bakers Swamp.|||Paling Yard Formation, Brymedura Sandstone, Macquarie Park Sandstone, Black Rock Subgroup, Kurrool Formation, Curra Creek Conglomerate.|Low-angle discordance with underlying Garra Formation. Faulted under the Garra Formation in the Mount Arthur Syncline.||
3797|Catombal Group|73457|6|Mentioned|p2|Late Devonian|Late Devonian|||||||
3818|Cauldwell Vale 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).||||||24-SEP-19
3818|Cauldwell Vale Conglomerate Member|35287|6|Mentioned|p7|||||||||
3818|Cauldwell Vale Conglomerate Member|39618|6|Mentioned|Table 9|||||||||
3818|Cauldwell Vale Conglomerate Member|42566|3|Fully described|p64||||||||Massive unsorted, largely unstratified pebble to boulder conglomerate and coarse-grained pebbly quartz -lithic sandstone.|24-SEP-19
3818|Cauldwell Vale Conglomerate Member|42568|5|Briefly described|Map legend|Early Devonian|Late Silurian|||||||
3818|Cauldwell Vale Conglomerate Member|70751|6|Mentioned|p12|Pridoli|Pridoli|||||||
3818|Cauldwell Vale Conglomerate Member|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Equivalent to Wirrilah Conglomerate Member and Mount Susannah Conglomerate.||
3824|Cavan Bluff Limestone|12185|5|Briefly described|map legend|Middle Devonian|Middle Devonian|Limestone, some shale and quartz sandstone. BMR map symbol: Dmc.||||||
3824|Cavan Bluff Limestone|13996|6|Mentioned|p135|Emsian|Emsian|Taemas area. Contains the rugose coral Zelolasma gemmiformis.||||||
3824|Cavan Bluff Limestone|23898|4|Described|p269, p271 Fig.2|Early Devonian|Early Devonian|Of Murrumbidgee Group.  Geological Province: Lachlan Fold Belt.||||||
3824|Cavan Bluff Limestone|24250|5|Briefly described|p109 Fig.5|Early Devonian|Early Devonian|Of the Murrumbidgee Group. Overlain by Majurgong Formation.||||||18-JUN-08
3824|Cavan Bluff Limestone|29989|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
3824|Cavan Bluff Limestone|30069|5|Briefly described|p7|||||||||
3824|Cavan Bluff Limestone|30731|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
3824|Cavan Bluff Limestone|31019|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
3824|Cavan Bluff Limestone|31111|6|Mentioned|p222|||Also mention pP224.||||||18-JUN-08
3824|Cavan Bluff Limestone|31502|5|Briefly described|p94|||Devonian corals. See also p95 for age.||||||18-JUN-08
3824|Cavan Bluff Limestone|32483|4|Described|p31|||Lower Devonian. Table 1.||||||18-JUN-08
3824|Cavan Bluff Limestone|32585|6|Mentioned|p210|||Member||||||
3824|Cavan Bluff Limestone|33327|5|Briefly described|p173|||Unit of Cavan Fm?||||||18-JUN-08
3824|Cavan Bluff Limestone|33481|6|Mentioned|p11|||Base Couvinian or top Coblenzian. See also p15.||||||18-JUN-08
3824|Cavan Bluff Limestone|34405|6|Mentioned|Fig.3.12|||||||||
3824|Cavan Bluff Limestone|34692|5|Briefly described|p186|||||||||
3824|Cavan Bluff Limestone|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
3824|Cavan Bluff Limestone|35386|3|Fully described|p48|||||||||
3824|Cavan Bluff Limestone|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
3824|Cavan Bluff Limestone|42033|6|Mentioned|p654|||||||||
3824|Cavan Bluff Limestone|43344|14|Not recorded|p117|||Yass-Taemas area||||||
3824|Cavan Bluff Limestone|43527|14|Not recorded|p535|||||||||
3824|Cavan Bluff Limestone|43532|14|Not recorded|p201,220||Devonian|||||||
3824|Cavan Bluff Limestone|45078|6|Mentioned|p2|||On locality map.||||||
3824|Cavan Bluff Limestone|50230|5|Briefly described|Map legend|Pragian|Pragian|Of the Murrumbidgee Group.  Overlies the Fifeshire Shale; underlies the Majurgong Formation.  Limestone, shaly limestone, shale.||||||
3824|Cavan Bluff Limestone|63594|6|Mentioned|p1032|||Contains conodonts in the Taemas-Wee Jasper area of NSW.||||||18-JUN-08
3824|Cavan Bluff Limestone|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Murrumbidgee Group. Limestone, shaly limestone, shale.||||||
3824|Cavan Bluff Limestone|64296|6|Mentioned|p90|||||||||
3824|Cavan Bluff Limestone|64992|5|Briefly described|p60 Fig. 1, p59|Devonian|Devonian|Part of the Taemas-Wee Jasper succession. Contains Dipnorhynchus kiandrensis (lungfish) and Speonesydrion iani? Shale and bedded limestone, initiated as a series of banded carbonate algal beds (marine deposits).||||||26-MAR-09
3824|Cavan Bluff Limestone|65940|6|Mentioned|p205|||Taeman, NSW.||||||
3824|Cavan Bluff Limestone|68592|3|Fully described|p239, p982-4,p986,p994-8,p1857-8,p1894-5|Emsian|Pragian|Originally called Bluff Limestone by Harper (1909); Browne (1959) used the name in the text but called the rocks Cavan Bluff Limestone in the map. This latter name is used in preference to subsequent variations: Cavan Bluff Formation (Pedder, 1965), Cavan Limestone (Owen and Wyborn, 1979 and others), Cavan Formation (Pedder in Oswald, 1967). Type section and suggested type locality decribed. Estimated thickness of 75-152m. Potential source of industrial and agricultural lime. Rich and diverse fauna in upper parts described.||Unit in Murrumbidgee Group.||Conformably overlies Fifeshire Shale, and Sugarloaf Creek Formation of the Black Range Group. Is overlain gradationally by Majurgong Formation.|Blue-grey, massive, thin- to medium-bedded, flaggy, impure silty limestone interbedded with shale, mudcracks widely developed on bed tops; overlain by blue-grey, medium- to thick-bedded, highly fossiliferous limestone.|
3824|Cavan Bluff Limestone|70192|5|Briefly described|Map Legend|Emsian|Pragian|Dmc. 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) and Fifeshire Shale. Is overlain by Majurgong Formation.|Blue-grey, massive, thin to medium bedded, flaggy, impure, silty limestone interbedded with shale overlain by medium-thick bedded highly fossiliferous limestone.|
3824|Cavan Bluff Limestone|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|||Blue-grey, massive, thin to medium bedded, flaggy, impure, silty limestone interbedded with shale overlain by medium-thick bedded highly fossiliferous limestone.|
3824|Cavan Bluff Limestone|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|||Blue-grey, massive, thin to medium bedded, flaggy, impure, silty limestone interbedded with shale overlain by medium-thick bedded highly fossiliferous limestone.|
3824|Cavan Bluff Limestone|71656|4|Described|p12 Fig.2, p32-33, p34|Emsian|Pragian|The Cavan Bluff Limestone [known as Cavan Formation of previous authors] is well-dated on the basis of conodonts. Also includes corals, bivalves, brachiopods, fish.||Murrumbidgee Group||Murrumbidgee Group. Previously Cavan Formation. Overlies Fifeshire Shale and underlies Majurgong Formation.|Fossiliferous flaggy limestone associated with shale and quartzite; massive algal limestones.|
3824|Cavan Bluff Limestone|71700|5|Briefly described|CD|||Occurs in the Lake Burrinjuck area near Yass. This unit may be equivalent to the Bongalaby Formation.||Murrumbidgee Group||Equivalent to the Lake Bathurst Limestone Member.||
3824|Cavan Bluff Limestone|73143|6|Mentioned|p17|Pragian|Pragian|Contains ""Cystiphyllum"" rugose coral (Hill, 1941).||||||
3824|Cavan Bluff Limestone|73215|5|Briefly described|p994|||Talmo-Taemas area.||Murrumbidgee Group.||Overlies Sugarloaf Creek and Kirawin Formations. Is overlain by Majurgong Formation.||24-JAN-23
3832|Cave Creek Limestone|22857|5|Briefly described|p454 App.1, Tb.A1.6|Silurian|Silurian|Massive limestone. Max. thickness: 450m. Geological Province: Tumut Trough.||||||
3832|Cave Creek Limestone|29648|6|Mentioned|p20|||||||||
3832|Cave Creek Limestone|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
3832|Cave Creek Limestone|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
3832|Cave Creek Limestone|31161|5|Briefly described|PA6|||||||||
3832|Cave Creek Limestone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
3832|Cave Creek Limestone|34405|4|Described|p116|||||||||
3832|Cave Creek Limestone|40328|6|Mentioned|p44|||||||||
3832|Cave Creek Limestone|40497|6|Mentioned|Map legend|Silurian|Silurian|||||||
3832|Cave Creek Limestone|40498|6|Mentioned|p424|||||||||
3832|Cave Creek Limestone|43383|14|Not recorded|p12|||||||||
3832|Cave Creek Limestone|60086|5|Briefly described|Map legend|Late Silurian|Late Silurian|Massive limestone.||||||
3853|Cedar Party Limestone|22857|5|Briefly described|p512 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Manning Group. Max. thickness: 120m. Geological Province: Barnard Basin.||||||
3853|Cedar Party Limestone|30911|6|Mentioned|Map legend|Permian|Permian|||||||
3853|Cedar Party Limestone|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3853|Cedar Party Limestone|32672|6|Mentioned|p675|||||||||
3853|Cedar Party Limestone|32944|6|Mentioned|p708|||Permian||||||
3853|Cedar Party Limestone|33702|6|Mentioned|p222|||||||||
3853|Cedar Party Limestone|34138|6|Mentioned|Cor.Chart|||Sakmarian - Artinskian||||||
3853|Cedar Party Limestone|34556|4|Described|p266|||Permian||||||
3853|Cedar Party Limestone|35129|5|Briefly described|p50|||||||||
3853|Cedar Party Limestone|38685|4|Described|p27|||Geological Province: New England Fold Belt. Overlying Unit: Colraine Mudstone. Underlying Unit: Kimbriki Formation||||||
3853|Cedar Party Limestone|41347|6|Mentioned|p368|||||||||
3853|Cedar Party Limestone|41348|5|Briefly described|Map legend|Permian||Of the Manning Group.||||||16-DEC-04
3853|Cedar Party Limestone|43018|6|Mentioned|p390|||||||||
3853|Cedar Party Limestone|43385|14|Not recorded|p179,180||Sakmarian|See also Lexicon||||||
3853|Cedar Party Limestone|43755|6|Mentioned|Fig.2,p550||Permian|||||||
3853|Cedar Party Limestone|44093|5|Briefly described|p232 App. 1|Early Permian|Early Permian|Of the Manning Group. Geological Province: New England Fold Belt.||||||
3853|Cedar Party Limestone|47059|5|Briefly described|p146|||||||||
3873|Cerberean Volcanics|22451|5|Briefly described|p24|Late Devonian||||||||
3873|Cerberean Volcanics|23229|6|Mentioned|p37|||||||||
3873|Cerberean Volcanics|23309|5|Briefly described|p161 Table 2.60|Devonian|Devonian|||||||
3873|Cerberean Volcanics|29786|6|Mentioned|p85|||||||||
3873|Cerberean Volcanics|31161|5|Briefly described|PA11|||||||||
3873|Cerberean Volcanics|32074|6|Mentioned|Table 3|||See also p184||||||30-AUG-22
3873|Cerberean Volcanics|33238|6|Mentioned|p643|||||||||
3873|Cerberean Volcanics|33732|5|Briefly described|Table III|||||||||
3873|Cerberean Volcanics|35186|4|Described|p6|||||||||
3873|Cerberean Volcanics|35277|3|Fully described|p87|||||||||
3873|Cerberean Volcanics|35278|6|Mentioned|p360|||||||||
3873|Cerberean Volcanics|35283|6|Mentioned|p54|||||||||
3873|Cerberean Volcanics|35526|6|Mentioned|p97|||Discussion of ages.||||||
3873|Cerberean Volcanics|37727|6|Mentioned|p27|||||||||
3873|Cerberean Volcanics|38327|6|Mentioned|p558|||||||||
3873|Cerberean Volcanics|38367|6|Mentioned|Fig.1|||||||||
3873|Cerberean Volcanics|38787|6|Mentioned|p143|||||||||
3873|Cerberean Volcanics|39291|6|Mentioned|p210|||See also Table 1||||||
3873|Cerberean Volcanics|40995|6|Mentioned|Fig.31|||||||||
3873|Cerberean Volcanics|41385|6|Mentioned|p363|||||||||
3873|Cerberean Volcanics|41585|6|Mentioned|Fig.4.5|||||||||
3873|Cerberean Volcanics|41641|4|Described|p157|||See also p160.||||||30-AUG-22
3873|Cerberean Volcanics|41868|6|Mentioned|p485|||||||||
3873|Cerberean Volcanics|42827|4|Described|p157|||see also Fig 5.2 and p160||||||30-AUG-22
3873|Cerberean Volcanics|43461|14|Not recorded|p628|||||||||
3873|Cerberean Volcanics|43547|14|Not recorded|p150|||||||||
3873|Cerberean Volcanics|48894|6|Mentioned|p92|||See also pp93-95. 365+-90my.||||||30-AUG-22
3873|Cerberean Volcanics|64571|5|Briefly described|p827, p828|Late Devonian|Late Devonian|Age: 367+/-2Ma (K/Ar and Rb/Sr). Victoria.||||||15-DEC-08
3873|Cerberean Volcanics|68311|5|Briefly described|p273, 276, 278|Late Devonian|Late Devonian|Cerberean Cauldron, Central Victoria.|375.0 +/- 2 Ma (SIMS U-Pb; Compston, 2004).|||Overlies Snobs Creek Volcanics.|S-type.|
3873|Cerberean Volcanics|70933|14|Not recorded|p98||Late Devonian|Table of Upper Devonian cauldron sequences.||||||
3883|Chaelundi Complex|23720|5|Briefly described|Map Legend|Late Permian||Porphyritic hornblende-biotite granite, leucogranite.||||||15-DEC-04
3883|Chaelundi Complex|23811|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Coarse-grained leucocratic hornblende-biotite granite.||||||11-JAN-10
3883|Chaelundi Complex|23812|5|Briefly described|p10, p22 Tb.2|Middle Triassic|Middle Triassic|Age: 235-323[probably 233]Ma (Rb-Sr).||||||17-SEP-18
3883|Chaelundi Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
3883|Chaelundi Complex|31695|6|Mentioned|Fig. 1|||||||||
3883|Chaelundi Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
3883|Chaelundi Complex|35173|6|Mentioned|p102|||||||||
3883|Chaelundi Complex|35257|6|Mentioned|p75|||||||||
3883|Chaelundi Complex|44450|5|Briefly described|p35|||Geological Province: Coffs Harbour Block.||||||
3883|Chaelundi Complex|63599|6|Mentioned|p985|||Geological Province: New England Fold Belt.||||||10-DEC-07
3883|Chaelundi Complex|69188|5|Briefly described|p17, p22|||NW of Smokey Cape. Previously (Shaw, unpublished data, 1989) dated at 235-233 Ma.|||||I- and A-type.|
3883|Chaelundi Complex|69639|5|Briefly described|p3, p6, p8, p118|||New England Orogen. An additional date of 237.4 +/- 1.4 Ma is also derived in this study. I and A type geochemistry. Sampling locality, petrography and geochronology are discussed.  See also p123-p134, p223-p224, p238.|237.7 +/- 1.5 Ma (SHRIMP U-Pb) |||Intrudes the Moombil Beds and Brooklana Beds.|I and A type monzogranites, generally coarse-grained, leucocratic hornblende-biotite granites and granodiorites with marginal quartz porphyries.|
3883|Chaelundi Complex|71206|6|Mentioned|p380|||||||||
3883|Chaelundi Complex|71628|4|Described|p1:6; p2: 20, 46, 56-57; p3:27; p17: 5-6|||See also p17: 8, 10, 28-30, 33, 90-92; p19: 96, 102. Leitch et al. (1971). Previously Chaelundi Adamellte; also Chaelundi Granite (Babaahmadi and Rosenbaum, 2013). Named after either the parish or one of several local geographic features. Crops out ~40 km NW of Dorrigo, covering ~110 km2. Deeply weathered. The two strongly contrasting components are assigned to different Supersuites. Geochemistry summarised; see constituents for details. Has similarities with Charon Creek Quartz Diorite but they have different ages and hence not cogenetic. Part of Coastal Granite Association. Contains a single minor Mo(W) deposit.|237.4 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).||Chaelundi Mountain Monzogranite, Guy Fawkes Granodiorite.|Intrudes Moombil Siltstone and Brooklana beds.|Comprises medium-grained, I-type hornblende-biotite granodiorite to monzogranite (Guy Fawkes Granodiorite), and coarse- to medium-grained, leucocratic A-type monzogranite and rare quartz monzonite (Chaelundi Mountain Monzogranite).|
3883|Chaelundi Complex|73197|6|Mentioned|p482|Late Triassic|Late Triassic|New England Orogen, southern. Partly A-type granitoid (Landenberger and Collins, 1996).|||||Includes granitoids.|
3886|Chain Valley Coal Member|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Moon Island Beach Formation.   Geological Province: Sydney Basin||||||
3886|Chain Valley Coal Member|37083|6|Mentioned|p169|||||||||
3886|Chain Valley Coal Member|39666|6|Mentioned|Table 20|||||||||
3886|Chain Valley Coal Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Eleebana Formation.||||13-JAN-15
3911|Chapmans Creek Granite|42726|5|Briefly described|map legend|Carboniferous||51. Reserved as Chapmans Creek Granodiorite.||||||
3917|Charbon Subgroup|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
3917|Charbon Subgroup|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|||||||
3917|Charbon Subgroup|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
3917|Charbon Subgroup|39232|3|Fully described|p108|||See also P111||||||
3917|Charbon Subgroup|40806|1|Redefined|p149|Permian|Permian|Prob. Permian. Redefinition of Charbon Sub-Group?||||||
3917|Charbon Subgroup|42925|5|Briefly described|Table 18||Late Permian|||||||
3917|Charbon Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
3917|Charbon Subgroup|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Of Illawarra Coal Measures, western Sydney Basin.||||||
3917|Charbon Subgroup|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin||||||
3917|Charbon Subgroup|63832|5|Briefly described|p131 fig 2|||Of Sydney Basin. Final (P4) Paleozoic glaciation.||Unit in Illawarra Coal Measures.||||13-DEC-17
3917|Charbon Subgroup|64631|6|Mentioned|p44 Fig.2.|Wuchiapingian|Capitanian|Sydney Basin.||Unit in Illawarra Coal Measures.||||
3917|Charbon 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 Baal Bone Formation.|Overlies Cullen Bullen Subgroup. Is overlain by Wallerawang Subgroup.||
3917|Charbon Subgroup|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Unit in Illawarra Coal Measures.||Overlies Cullen Bullen Subgroup. Is overlain by Wallerawang Subgroup.||
3917|Charbon Subgroup|70661|6|Mentioned|p187|||Not present in map area (Moss Vale).||Illawarra Coal Measures||||
3921|Charlestown Conglomerate Member|23055|6|Mentioned|p26|||||||||
3921|Charlestown Conglomerate Member|29922|6|Mentioned|p49|||||||||
3921|Charlestown Conglomerate Member|29926|6|Mentioned|p2|||Permian||||||
3921|Charlestown Conglomerate Member|33867|5|Briefly described|p11|||||||||
3921|Charlestown Conglomerate Member|34351|5|Briefly described|p344|||Fig.5.13||||||
3921|Charlestown Conglomerate Member|37083|6|Mentioned|p164|||||||||
3921|Charlestown Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
3921|Charlestown Conglomerate Member|39308|5|Briefly described|p467|||||||||
3921|Charlestown Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
3921|Charlestown Conglomerate Member|43447|14|Not recorded|diag.p26,34,35|||Part of Cardiff Sub-Group||||||
3921|Charlestown Conglomerate Member|45090|6|Mentioned|p186|||Stratigraphic table||||||
3921|Charlestown Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Tickhole Formation. ||||
3925|Charlton Formation|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Apple Tree Flat Subgroup.  Includes Stafford Coal Member and Monkey Place Creek Tuff Member.   Geological Province: Sydney Basin||||||
3925|Charlton Formation|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Apple Tree Flat Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
3925|Charlton Formation|29942|3|Fully described|p11|||||||||
3925|Charlton Formation|45090|6|Mentioned|p188|||Refers Britten.(1972)||||||
3925|Charlton Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Upper unit in Apple Tree Flat Sub-group.|Includes Monkey Place Tuff Member and Stafford Coal Member.|Overlies Abbey Green Coal. Is overlain by Clifford Formation.|Sandstone, siltstone and minor shale, bounded at the top by inferior coal and at the base by a distinctive biotite rich tuffaceous claystone.|
3937|Chaucer Redbed Member|35258|6|Mentioned|Fig.3|||Variation of Red Beds?||||||
3937|Chaucer Redbed Member|63290|5|Briefly described|p401 Fig. 5(d)|Llandovery|Llandovery|Of Waugoola Group. Overlain Glendalough Formation, underlain by Burly Jacky Sandstone Member.||||||
3937|Chaucer Redbed Member|70684|5|Briefly described|p50 Fig.24|Early Silurian|Early Silurian|Molong Volcanic Belt. ||Glendalough Formation.||||
3938|Checkers Member|5250|6|Mentioned|p50||Late Ordovician|Member of Regans Creek Limestone. Includes brachiopod fauna||||||
3938|Checkers Member|23214|3|Fully described|p49|Eastonian|Eastonian|Of Regans Creek Limestone. Overlying unit: Malongulli Formation, underlying unit: Red East Member. 48m thick at type section.||||||
3938|Checkers Member|32151|3|Fully described|p204|||||||||
3938|Checkers Member|32590|6|Mentioned|p13|||||||||
3938|Checkers Member|38219|5|Briefly described|p301|||||||||
3938|Checkers Member|40136|6|Mentioned|p38|||||||||
3938|Checkers Member|42479|5|Briefly described|p109|||||||||
3938|Checkers Member|42561|6|Mentioned|p89|||of Regans Creek Limestone.||||||
3959|Chesney Formation|730|6|Mentioned|p17.|Devonian|Devonian|Contains Drysdale Conglomerate Member in its lower part.||||||11-NOV-14
3959|Chesney Formation|22857|4|Described|p436 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Nurri Group (Cobar Supergroup). Max. thickness: 1400m. Geological Province: Cobar Basin.||||||
3959|Chesney Formation|23095|5|Briefly described|p610 (table 1)|Early Devonian|Early Devonian|||||||
3959|Chesney Formation|23096|6|Mentioned|p601 (Fig 1)|||||||||
3959|Chesney Formation|23101|5|Briefly described|p567 (Fig 1)|||||||||
3959|Chesney Formation|23171|6|Mentioned|p15,40,Fig15p45|||||||||
3959|Chesney Formation|23173|4|Described|Map Legend|Lochkovian|Pridoli|||||||
3959|Chesney Formation|23734|5|Briefly described|p12 Fig. 1|||Parent: Nurri Group.  Sandstone, siltstone and conglomerate.||||||
3959|Chesney Formation|29621|4|Described|p6|||||||||
3959|Chesney Formation|33123|6|Mentioned|p8|||||||||
3959|Chesney Formation|35185|6|Mentioned|p226|||||||||
3959|Chesney Formation|35219|6|Mentioned|Fig.2|||||||||
3959|Chesney Formation|35287|6|Mentioned|p6|||||||||
3959|Chesney Formation|35383|6|Mentioned|Map legend|Early Devonian|Late Silurian|||||||
3959|Chesney Formation|35385|3|Fully described|p21|||||||||
3959|Chesney Formation|37668|6|Mentioned|Fig.1|||||||||
3959|Chesney Formation|37936|6|Mentioned|Fig.2|||||||||
3959|Chesney Formation|38292|6|Mentioned|p3|||||||||
3959|Chesney Formation|39083|6|Mentioned|p30|||||||||
3959|Chesney Formation|39214|6|Mentioned|p11|||See also Table 11||||||
3959|Chesney Formation|39618|3|Fully described|p83|||||||||
3959|Chesney Formation|39683|6|Mentioned|Fig.3|||||||||
3959|Chesney Formation|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
3959|Chesney Formation|41090|6|Mentioned|Fig.1|||||||||
3959|Chesney Formation|41138|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
3959|Chesney Formation|41410|5|Briefly described|p295|||||||||18-JAN-10
3959|Chesney Formation|41452|6|Mentioned|p22|||||||||
3959|Chesney Formation|41872|6|Mentioned|p8|||||||||
3959|Chesney Formation|42144|5|Briefly described|p607|||See also Fig.6 and 8||||||
3959|Chesney Formation|42172|4|Described|Fig.4 p166|||||||||23-SEP-19
3959|Chesney Formation|42208|6|Mentioned|Fig.1 P305|||||||||
3959|Chesney Formation|42344|5|Briefly described|p57|||||||||
3959|Chesney Formation|42521|5|Briefly described|p19, Fig.3 p16|||||||||
3959|Chesney Formation|42907|6|Mentioned|Fig.8, P8|||||||||
3959|Chesney Formation|42914|5|Briefly described|p10|||||||||
3959|Chesney Formation|42983|6|Mentioned|Fig.3,p345|||||||||
3959|Chesney Formation|43032|2|Defined|p30|Early Devonian|Late Silurian|of Nurri Group||||||
3959|Chesney Formation|43153|5|Briefly described|Map Legend||Lochkovian|of Nurri Group||||||
3959|Chesney Formation|43757|6|Mentioned|p511||Early Devonian|Age: approx. 390-400 Ma||||||
3959|Chesney Formation|43774|1|Redefined|p36-40|||||||||
3959|Chesney Formation|46900|5|Briefly described|p16|||Part of Nurri Group||||||
3959|Chesney Formation|61905|5|Briefly described|p135 Fig. 1|||Geological Province: Cobar Basin.||||||
3959|Chesney Formation|65469|5|Briefly described|p14, p15, p17, p43, p52|Pridoli|Pridoli|Lachlan Orogen. See also p55 fig 3-19, p62, p67, p133, p135, p136, p139, p333, p343, p353, App A-VI 3.||Nurri Group||Overlain by the Great Cobar Slate.||
3959|Chesney Formation|68823|6|Mentioned|p378 Fig.4|Lochkovian|Pridoli|||Unit in Nurri Group.||Is overlain by Great Cobar Slate.||
3959|Chesney Formation|69002|6|Mentioned|p11, p14, p17, Map 1b||Sheinwoodian|Maximum age provided by concordant zircons at 421 and 433 Ma.|< 433 Ma|||||
3959|Chesney Formation|69043|4|Described|p3, p5-6, p79-85, p120|Lochkovian|Pridoli|Cobar Basin. Contains earliest Devonian faunal assemblages, and detrital zircons aged c.421 Ma (Glen et al., 2010). SHRIMP age from interbedded rhyolite.|418.1 +/- 3.0 Ma.|Nurri Group.|||Sedimentary rocks interbedded with flow-banded rhyolite.|
3959|Chesney Formation|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Late Silurian|Lachlan Orogen.||||||
3959|Chesney Formation|70941|5|Briefly described|p78, p78 fig 32|Late Silurian|Late Silurian|Greater than 423 Ma based on the ages of the Peak Rhyolite and Queen Bee Porphyry. |||Includes the Bee Conglomerate Member, Drysdale Conglomerate Member.|Intruded by the Queen Bee Porphyry and Peak Rhyolite. Overlain by the Great Cobar Slate. Overlies the Bee Conglomerate Member and the Drysdale Conglomerate Member.||
3959|Chesney Formation|71039|6|Mentioned|p19-20, p27|||Rhyolitic complex dated at 418.3 +/- 3 Ma displays peperitic textures and intrusive relationships with this unit.||Nurri Group||||09-MAR-23
3959|Chesney Formation|71285|4|Described|p538-540, p542, p544-545, p547-548, p552|Late Silurian|Late Silurian|Cobar region. Spatially related to several Cu-Au deposits. Sulfur isotopes, fluid inclusion temperatures detailed.||Nurri Group.||Is overlain by, and faulted against, the Great Cobar Slate.|Medium- to thin-bedded turbidite sequence of greywackes and siltstones; very minor felsic volcaniclastic rocks.|
3959|Chesney Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Nurri Group.||Is overlain by Great Cobar Slate.|Thick-bedded, massive and graded, coarse- to fine-grained quartz-lithic sandstone interbedded with siltstone and mudstone. Pebbles and cobbles are abundant in conglomeratic units at or near the base.|
3959|Chesney Formation|73143|6|Mentioned|p2|||||Nurri Group||||
3959|Chesney Formation|73174|5|Briefly described|p1036-1039|Lochkovian|Lochkovian|Cobar Basin.||Nurri Group, Cobar Supergroup|Drysdale Conglomerate Member|Overlain by and equivalent to Great Cobar Slate.|Grades from coarse-grained clastic rocks through thinly bedded sandstone and mudstone. Sandstones are lithic-rich.|24-NOV-22
3959|Chesney Formation|73264|5|Briefly described|p1394 Fig.16, p1407|Early Devonian|Silurian|Cobar Basin.|||||Quartz-lithic sandstone.|
3959|Chesney Formation|73578|6|Mentioned|p25, p28|||||Nurri Group||||
3972|Cheyenne Complex|23720|5|Briefly described|Map Legend|Early Permian|Early Permian|Pyroxene, gabbro, diorite, monzogranite, granophyre.||||||15-DEC-04
3972|Cheyenne Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
3972|Cheyenne Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
3972|Cheyenne Complex|44450|6|Mentioned|p33|||Geological Province: New England Fold Belt.||||||
3972|Cheyenne Complex|71628|4|Described|p2: 3, 22-27|||Binns et al. (1967). Named after a local homestead, 40 km S of Uralla and ~35 km NE of Walcha. Comprises several small stocks. This 280 Ma age determination is anomalous. Assigned to the Bakers Creek Suite by Landenberger (1996) and later to the Bakers Creek Supersuite by Landenberger et al. (2010). Its affiliation is uncertain: discussed. Geochemistry discussed. Associated with minor Cu mineralisation in sulfide-bearing quartz veins; also with the Winterbourne graphite mine.|280 Ma (Rosenbaum et al., 2012).|Bakers Creek Supersuite.||Intrudes Girrakool beds and Agnes Greywacke.|Mafic igneous complex comprising (quartz) gabbro, (quartz) diorite, quartz monzodiorite and granophyre, amphibole-bearing quartz diorite - quartz monzodiorite to granodiorite - monzogranite, biotite-bearing granodiorite-monzogranite-syenogranite.|
3991|Chillingham Volcanics|22857|4|Described|p284, p542 App.1 Tb.A1.11|Late Triassic|Early Triassic|Rhyolitic lavas, ignimbrites and airfall tuffs interbedded with non-marine strata, mainly conglomerate. Max. thickness: 200m. Geological Province: Ipswich Basin (under Clarence-Moreton Basin).||||||
3991|Chillingham Volcanics|22861|5|Briefly described|p284|||||||||
3991|Chillingham Volcanics|22865|6|Mentioned|Fig22.9p317|||||||||
3991|Chillingham Volcanics|23811|5|Briefly described|Map Legend|Norian|Carnian|Alkali basalt and andesite; basalt is massive and columnar-jointed; the andesite includes massive and banded varieties overlain by hyaloclastite. Geological Province: Clarence-Moreton Basin.||||||11-JAN-10
3991|Chillingham Volcanics|23812|5|Briefly described|p31, p35 Tb.4|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin. Maximum thickness: 1500m.||||||21-SEP-05
3991|Chillingham Volcanics|23888|6|Mentioned|p262|||||||||
3991|Chillingham Volcanics|24082|6|Mentioned|p452|||||||||
3991|Chillingham Volcanics|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|24299|5|Briefly described|p3|Triassic|Triassic|||||||
3991|Chillingham Volcanics|29995|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|30131|4|Described|p8|||Lithology||||||
3991|Chillingham Volcanics|30302|6|Mentioned|p414|||See also P415||||||
3991|Chillingham Volcanics|30687|4|Described|p63|||See also P64,65,76. Triassic age||||||
3991|Chillingham Volcanics|30911|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|33004|6|Mentioned|p78|||See also P225||||||
3991|Chillingham Volcanics|33476|6|Mentioned|Fig.10|||||||||
3991|Chillingham Volcanics|33881|6|Mentioned|p96|||||||||
3991|Chillingham Volcanics|34340|3|Fully described|p542|||Triassic. See Table 6.1||||||29-SEP-05
3991|Chillingham Volcanics|34593|6|Mentioned|p539|||Triassic. Equivalent Copes Creek Tuff.||||||24-SEP-08
3991|Chillingham Volcanics|34755|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|35007|6|Mentioned|p75|||||||||
3991|Chillingham Volcanics|35126|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|35156|4|Described|p6|||See also Table.2||||||
3991|Chillingham Volcanics|37065|6|Mentioned|p36|||||||||
3991|Chillingham Volcanics|37112|5|Briefly described|p298|||||||||
3991|Chillingham Volcanics|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
3991|Chillingham Volcanics|38074|5|Briefly described|Table 1|||||||||
3991|Chillingham Volcanics|38307|6|Mentioned|p523|||||||||
3991|Chillingham Volcanics|38837|6|Mentioned|p235|||Geological Province: New England Fold Belt||||||
3991|Chillingham Volcanics|39445|6|Mentioned|Table 9|||||||||
3991|Chillingham Volcanics|40245|6|Mentioned|p185|||Mention Fig.2||||||
3991|Chillingham Volcanics|40328|6|Mentioned|p195|||||||||
3991|Chillingham Volcanics|40479|6|Mentioned|p32|||||||||
3991|Chillingham Volcanics|40517|6|Mentioned|p358|||||||||
3991|Chillingham Volcanics|40623|5|Briefly described|p40|||||||||
3991|Chillingham Volcanics|40780|4|Described|p5|||||||||
3991|Chillingham Volcanics|40784|6|Mentioned|p982|||||||||
3991|Chillingham Volcanics|41591|5|Briefly described|p18|||||||||
3991|Chillingham Volcanics|41738|6|Mentioned|p168|||||||||
3991|Chillingham Volcanics|42041|6|Mentioned|Fig.5 P227|||||||||
3991|Chillingham Volcanics|42182|5|Briefly described|p302|||||||||
3991|Chillingham Volcanics|42317|5|Briefly described|p2|||||||||
3991|Chillingham Volcanics|43001|5|Briefly described|p121|||||||||
3991|Chillingham Volcanics|43003|6|Mentioned|Fig.21,p173|||||||||
3991|Chillingham Volcanics|43092|5|Briefly described|p31|||||||||
3991|Chillingham Volcanics|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
3991|Chillingham Volcanics|43161|5|Briefly described|14, 36||Triassic|||||||
3991|Chillingham Volcanics|43383|14|Not recorded|p24||Triassic|||||||
3991|Chillingham Volcanics|43384|14|Not recorded|Map Legend||Triassic|||||||
3991|Chillingham Volcanics|43479|14|Not recorded|p224,243||Early Triassic|||||||
3991|Chillingham Volcanics|43736|6|Mentioned|p3||Middle Triassic|||||||
3991|Chillingham Volcanics|43881|14|Not recorded|p6-7,10,13,29,34,49|||p51-52,58(anal.)66,80,143,168-9||||||
3991|Chillingham Volcanics|45003|14|Not recorded|p107|||QLD and NSW||||||
3991|Chillingham Volcanics|48917|6|Mentioned|p9|||Correlation||||||
3991|Chillingham Volcanics|60281|6|Mentioned|p25|||Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|60993|6|Mentioned|p8 Tb. 2|||Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|60996|6|Mentioned|p76|||Geological Province: Clarence-Moreton Basin.||||||
3991|Chillingham Volcanics|61002|5|Briefly described|p202|Middle Triassic|Middle Triassic|Felsic to basaltic rocks. Conformably overlain by Ipswich C.M. See also p199 Fig. 3.||||||
3991|Chillingham Volcanics|61006|6|Mentioned|p277|Middle Triassic|Middle Triassic|||||||
3991|Chillingham Volcanics|61310|5|Briefly described|p14 Fig. C5, p34|||Overlain by Ipswich Coal Measures. Geological Province: Clarence-Moreton Basin. Equivalent to Nymboida Coal Measures.||||||24-SEP-08
3991|Chillingham Volcanics|61772|6|Mentioned|p128, p129 Fig. 4||Middle Triassic|In New England Orogen.||||||24-SEP-08
3991|Chillingham Volcanics|61775|6|Mentioned|p182 Fig. 1|||||||||
3991|Chillingham Volcanics|64665|6|Mentioned|p53 Fig.2.|Late Triassic|Late Triassic|Ipswich Basin.||||||
3991|Chillingham Volcanics|65452|6|Mentioned|p4 Fig.1|Late Triassic|Late Triassic|||||||
3991|Chillingham Volcanics|66855|5|Briefly described|pp955-956.|Late Triassic|Late Triassic|Andesitic rocks at Evans Head included (Scott 1982) with New England Fold Belt; basaltic rocks  were mapped as correlates of Tertiary Lismore Basalt. This study shows they are both part of a Late Triassic volcanic province extending 360 km to the north.|||||Rhyolitic pyroclastic rocks and lavas; associated volcanic rocks including basaltic andesites in southern Queensland.|
3991|Chillingham Volcanics|67203|6|Mentioned|p3|Triassic|Triassic|||||||
3991|Chillingham Volcanics|67402|5|Briefly described|p222, p223|Carnian|Ladinian|Ipswich Basin.|||||Sub-aerial tuffaceous conglomerate and sandstone.|
3991|Chillingham Volcanics|68327|5|Briefly described|Map legend.|Triassic|Triassic||||||Rhyolite flows and tuff.|
3991|Chillingham Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
3991|Chillingham Volcanics|68679|5|Briefly described|p388, p392-394, p433-435|Late Triassic|Late Triassic|Base of the Ipswich Basin: Brisbane/Beenleigh/offshore. Previously thought equivalent to Nymboida Coal Measures, but contradicted by macrofloral and radiometric dating.|||||Early pyroclastic phase: rhyolitic ignimbrites (<1m to ~200m thick) with abundant felsic volcanic lithic fragments; less common air fall and surge deposits associated with epiclastic sediments; later effusive phase of flow-banded felsic lava flows.|
3991|Chillingham Volcanics|69594|6|Mentioned|p519, p543|||Ipswich Basin.||||Is overlain by Ipswich Coal Measures and locally by Raceview Formation.||
3991|Chillingham Volcanics|72297|5|Briefly described|p755, p758|Triassic|Triassic|Source of thunder eggs at Thunderbird Park at Mount Tamborine. At Back Creek, SE of Canungra, amethyst and quartz crystals occur with chalcedony and common opal in veins in this unit.|||||Spherulitic rhyolite.|
3991|Chillingham Volcanics|73306|5|Briefly described|p564-566, 568, 572 Fig.8|Late Triassic|Late Triassic|||||Probable equivalent to the Brisbane Tuff.|A thick sequence of rhyolite and tuff.|
3991|Chillingham Volcanics|73450|5|Briefly described|p38|||Gold Coast hinterland. Divided into a lower and upper package (Roach, 1993; 1996).|||||Felsic pyroclastic deposits including ignimbrites up to ca 200 m thick with abundant felsic volcanic lithic fragments, flow-banded felsic lava flows, less common airfall and surge deposits, and epiclastic sedimentary rocks.|
4013|Chinghee Conglomerate|30604|6|Mentioned|p66|||||||||
4013|Chinghee Conglomerate|30687|4|Described|p64|||See also P65. Miocene age.||||||
4013|Chinghee Conglomerate|31130|6|Mentioned|Fig. 2|||Lower Miocene||||||
4013|Chinghee Conglomerate|32491|6|Mentioned|p25|||Early Miocene||||||
4013|Chinghee Conglomerate|32924|6|Mentioned|p112|||Refers McTaggart (1962)||||||
4013|Chinghee Conglomerate|35296|4|Described|p13|||See also P12.||||||
4013|Chinghee Conglomerate|39445|5|Briefly described|Table 14|||||||||
4013|Chinghee Conglomerate|40623|5|Briefly described|p39|||||||||
4013|Chinghee Conglomerate|40780|5|Briefly described|p9|||||||||
4013|Chinghee Conglomerate|40896|4|Described|p47|||||||||
4013|Chinghee Conglomerate|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
4013|Chinghee Conglomerate|44813|14|Not recorded|p80,81,88||Tertiary|||||||
4013|Chinghee Conglomerate|44871|2|Defined|p139|Tertiary|Tertiary|of Lamington Group.||||||
4013|Chinghee Conglomerate|48917|6|Mentioned|p33|||Refers McTaggart. Stratigraphic relationships||||||
4013|Chinghee Conglomerate|69599|5|Briefly described|p595, p640|Miocene|Miocene|Up to 30m thick. Includes cobbles and boulders sourced from the Mount Barney Granophyre. Underlies Tweed volcano lavas. Contains sporadic dicotyledonous leaves.||Lamington Volcanics.||Overlies the Mount Gillies Rhyolite.|Sandstone with siltstone lenses, and coarse-boulder polymictic conglomerate.|
4013|Chinghee Conglomerate|73450|4|Described|p96, 98|||Associated with the Focal Peak volcano. Parts appear to fill deep gorges and paleovalleys. Include boulder-sized clasts of Mount Gillies Rhyolite, granophyre from the Mount Barny Central Complex, Mesozoic and Carboniferous sedimentary rocks, basalt and fluidal riebeckite-bearing comendite.||||Underlain by Mount Gillies Rhyolite. Overlain by Beechmont Basalt.|Fluvial conglomerate and coarse, feldspathic sandstones that are variably cemented; possibly includes lahar deposits.|
4042|Chowilla Sand|23818|5|Briefly described|p212 Fig.108|Early Pleistocene|Early Pleistocene|Geological Province: Murray Basin. Of the Blanchetown Clay.||||||18-APR-05
4042|Chowilla Sand|24551|5|Briefly described|p338 Fig. 11.2, 340|Middle Pleistocene|Late Pliocene|||||||
4042|Chowilla Sand|30145|6|Mentioned|p183|||||||||
4042|Chowilla Sand|30754|2|Defined|Appendix 1|early Pleistocene|early Pleistocene|See stratigraphic table on p22.||||||31-MAR-09
4042|Chowilla Sand|30994|6|Mentioned|Fig. 1|||||||||
4042|Chowilla Sand|30996|3|Fully described|p39|||Refers Firman (1971).||||||31-MAR-09
4042|Chowilla Sand|31345|6|Mentioned|p294|||||||||
4042|Chowilla Sand|31385|6|Mentioned|Table 4|||||||||
4042|Chowilla Sand|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
4042|Chowilla Sand|32007|6|Mentioned|Fig. 2|||Pleistocene||||||
4042|Chowilla Sand|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
4042|Chowilla Sand|32861|5|Briefly described|Table 1|||||||||
4042|Chowilla Sand|33048|6|Mentioned|p197|||||||||
4042|Chowilla Sand|33826|6|Mentioned|p42|||Strat. table||||||
4042|Chowilla Sand|34180|6|Mentioned|p212|||Lower Pleistocene.||||||
4042|Chowilla Sand|34459|4|Described|p11|||Pleistocene||||||
4042|Chowilla Sand|34758|6|Mentioned|Table 1|||||||||
4042|Chowilla Sand|35232|6|Mentioned|p15|||||||||
4042|Chowilla Sand|37873|4|Described|p2|||||||||
4042|Chowilla Sand|38068|5|Briefly described|p76|||||||||
4042|Chowilla Sand|40003|6|Mentioned|Table 8|||||||||
4042|Chowilla Sand|41537|6|Mentioned|p350|||||||||
4042|Chowilla Sand|41848|6|Mentioned|p353|||Only on stratigraphic table p353, not in text||||||
4042|Chowilla Sand|42125|5|Briefly described|p138|||||||||
4042|Chowilla Sand|42443|6|Mentioned|p4|||||||||
4042|Chowilla Sand|42827|5|Briefly described|Table 9.1|||||||||
4042|Chowilla Sand|42966|1|Redefined|Table 31 p199|Pleistocene||||||||
4042|Chowilla Sand|44133|5|Briefly described|p252|Middle Pleistocene|Late Pliocene|Thickness: 10m. Geological Province: Murray Basin. Equivalent to Irymple Member. Interfingers with Blanchetown Clay.||||||20-NOV-17
4042|Chowilla Sand|64961|5|Briefly described|p260|||Name used interchangeably with Chowilla Sand Member. Of Blanchetown Clay. Well-sorted sand unit considered as, etc; sand is possibly reworked Loxton-Parilla Sand (see p260).||||||21-APR-09
4042|Chowilla Sand|66287|5|Briefly described|p28,31, Fig 4-5,10|Late Pliocene|Late Pliocene|Similar in appearance to the Loxton-Parilla Sands, but occupies a higher stratigraphic level. With the Blanchetown Clay and the Bungunnia Limestone, part of the Lake Bungunnia sedimentary fill. Included in the Blanchetown Clay by Firman (1965, 1973).||||||25-FEB-13
4042|Chowilla Sand|73228|6|Mentioned|p50, p56, p59|Pleistocene|Late Pliocene|Murray Basin, Lake Bungunnia. Fluvial.||||Unconformably underlain by Karoonda Surface. Overlain by Blanchetown Clay.|Dark-yellow to pale-yellow fine quartz-sand.|
4042|Chowilla Sand|73229|6|Mentioned|p67|Pleistocene|Late Pliocene|Murray Basin.||||||
4080|Clagger Sandstone|22831|4|Described|p78-79|Famennian|Famennian|Beargamil Subgroup||||||01-NOV-13
4080|Clagger Sandstone|22857|5|Briefly described|p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Hervey Group. Red, poorly sorted sandstones and pebbly sandstone, lesser red shales and siltstones. Max. thickness: 259m. Geological Province: Hervey Basin.||||||
4080|Clagger Sandstone|23217|5|Briefly described|p3, p6|||Of the Hervey Group. In the Hervey Range (NARROMINE sheet).||||||07-MAR-06
4080|Clagger Sandstone|23392|6|Mentioned|p7|||Broad correlation to Peaks Fm. Of the Beargamil Sub-Group||||||
4080|Clagger Sandstone|24417|6|Mentioned|p128|||Of "Beargamil Sub-Group".||||||
4080|Clagger Sandstone|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
4080|Clagger Sandstone|34109|4|Described|Table 3.10|||Beargamil Sub-Group||||||
4080|Clagger Sandstone|43441|6|Mentioned|31||Late Devonian|||||||08-JAN-10
4080|Clagger Sandstone|43500|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition) Part of Beargamil Sub-Group||||||
4080|Clagger Sandstone|43507|2|Defined|p126,128,132,140||Late Devonian|Top formation of Beargamil Subgroup (Hervey Group)||||||
4080|Clagger Sandstone|43510|2|Defined|p41,42,47,49,50|||||||||
4080|Clagger Sandstone|44160|5|Briefly described|Map Legend||Famennian|||||||08-JAN-10
4080|Clagger Sandstone|48958|6|Mentioned|Plate 1|||||||||
4080|Clagger Sandstone|62569|5|Briefly described|p606 Fig. 1E, p612|Late Devonian|Late Devonian|Of the Hervey Group. Geological Province: Lachlan Fold Belt. Contains fish remains.||||||10-AUG-07
4081|Claire Creek Limestone Member|24551|6|Mentioned|p614||Devonian|Of the Cowombat Siltstone.||||||31-JAN-06
4081|Claire Creek Limestone Member|37727|5|Briefly described|p51|||||||||
4081|Claire Creek Limestone Member|39447|6|Mentioned|p8|||||||||
4081|Claire Creek Limestone Member|40328|6|Mentioned|p70|||||||||
4081|Claire Creek Limestone Member|41585|6|Mentioned|p128|||||||||
4081|Claire Creek Limestone Member|42827|6|Mentioned|p128|||||||||
4098|Clarendon Formation|31056|5|Briefly described|p6|||||||||
4098|Clarendon Formation|33671|6|Mentioned|Fig.2|||||||||
4098|Clarendon Formation|35098|4|Described|p4|||||||||
4098|Clarendon Formation|35312|6|Mentioned|Fig.2|||||||||
4098|Clarendon Formation|41391|6|Mentioned|p49|||||||||
4098|Clarendon Formation|42925|2|Defined|p42||Pleistocene|||||||
4098|Clarendon Formation|42926|4|Described|map legend|Holocene|Pleistocene|||||||
4098|Clarendon Formation|73248|6|Mentioned|App. p3|Pleistocene|Pliocene?||||||Fluvial deposit.|
4124|Clear Creek Formation|22857|4|Described|p454 App.1, Tb.A1.6|Middle Silurian|Middle Silurian|Of Tumut Pond Group. Rhythmically bedded sandstone and slate. Max. thickness: 570m. Geological Province: Tumut Trough.||||||
4124|Clear Creek Formation|34405|4|Described|p114|||||||||
4124|Clear Creek Formation|40328|6|Mentioned|p45|||||||||
4124|Clear Creek Formation|42227|5|Briefly described|p22 Fig. 3|||Appears to be incorrectly included in the legend for Fig. 3.  The unit containing both Scotts Peak Road Member and Gelignite Creek Member is Huon River Formation.||||||
4128|Clear Range Granodiorite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Foliated contaminated granodiorite. BMR map symbol: gma.||||||
4128|Clear Range Granodiorite|22815|4|Described|p60,61|||||||||
4128|Clear Range Granodiorite|23866|5|Briefly described|p120, p121 Fig. 1|||Grades into a tonalitic variety to the south which is named Clear Range Tonalite. Geological Province: Murrumbidgee Batholith.  See also p122 Fig. 2.||||||20-MAY-08
4128|Clear Range Granodiorite|24222|5|Briefly described|p2|||Most mafic S-type granite in the Lachlan Fold Belt.  Mafic granodiorite to tonalite. Isotope data given.  Geological Province: Murrumbidgee Batholith in the Lachlan Fold Belt.||||||24-JAN-06
4128|Clear Range Granodiorite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
4128|Clear Range Granodiorite|31580|6|Mentioned|p272|||See also Table 1-4 for analysis||||||
4128|Clear Range Granodiorite|31581|3|Fully described|Table 1|||Xenolith content Table 111||||||
4128|Clear Range Granodiorite|32820|6|Mentioned|p3|||Part of Murrumbidgee Batholith||||||
4128|Clear Range Granodiorite|32905|6|Mentioned|p225|||See also P231||||||
4128|Clear Range Granodiorite|32906|6|Mentioned|p239|||||||||
4128|Clear Range Granodiorite|34544|4|Described|p185|||||||||
4128|Clear Range Granodiorite|36413|2|Defined|p78|Silurian|Silurian|Type area on top of Clear Range (ACT/NSW border). Sample 20535 (Joyce, 1973a), from GR 814533 is said to be fairly representative.||||||24-SEP-20
4128|Clear Range Granodiorite|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Biotite granodiorite. GSNSW map code: gma.||||||
4128|Clear Range Granodiorite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Xenolith-rich granodiorite. S-type. BMR map code: Smr.||||||
4128|Clear Range Granodiorite|36633|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
4128|Clear Range Granodiorite|37728|4|Described|Table 3|||||||||
4128|Clear Range Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
4128|Clear Range Granodiorite|40328|4|Described|p204|||||||||
4128|Clear Range Granodiorite|43233|5|Briefly described|Map Legend||Silurian|Possible Silurian age. Of Murrumbidgee Batholith.||||||
4128|Clear Range Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb1.||||||
4128|Clear Range Granodiorite|45003|14|Not recorded|p55|||||||||
4128|Clear Range Granodiorite|45147|3|Fully described|M194|||||||||
4128|Clear Range Granodiorite|46574|5|Briefly described|Map Legend|Silurian|Silurian|Of the Murrumbidgee Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
4128|Clear Range Granodiorite|49705|5|Briefly described|p29|||||||||
4128|Clear Range Granodiorite|60078|6|Mentioned|Map Legend|Late Silurian|Late Silurian|||||||
4128|Clear Range Granodiorite|68310|6|Mentioned|p240|||Murrumbidgee Batholith. Chemical analyses of schistose enclaves tabulated.|||||S-type granite.|
4137|Clematis Group|13516|5|Briefly described|p138, p159 fig 8, 160-162, p169|Middle Triassic|Middle Triassic|From Bowen Basin, Galilee Basin||||||
4137|Clematis Group|22857|6|Mentioned|p315 Fig. 22.8|||||||||
4137|Clematis Group|22865|6|Mentioned|Fig22.8p315|||||||||
4137|Clematis Group|22973|6|Mentioned|p12|||||||||
4137|Clematis Group|22975|5|Briefly described|p34 Fig.6|Triassic|Triassic|||||||
4137|Clematis Group|22976|5|Briefly described|p42 Fig.4|Triassic|Triassic|||||||
4137|Clematis Group|22980|5|Briefly described|p249 Fig.2|Triassic|Triassic|||||||
4137|Clematis Group|23052|5|Briefly described|Map Legend|Triassic|Triassic|||||||
4137|Clematis Group|23161|4|Described|p33 table4 fig11||Triassic|||||||
4137|Clematis Group|23430|5|Briefly described|p514-515|||Overlying Unit Moolayember Formation. Bowen Basin Province.||||||
4137|Clematis Group|24093|5|Briefly described|p176 Fig. 2|Triassic|Triassic|Age: 241-235Ma. Geological Province: Bowen Basin.||||||
4137|Clematis Group|24159|5|Briefly described|p147|Middle Triassic|Middle Triassic|Geological Province: Bowen Basin.||||||
4137|Clematis Group|24615|5|Briefly described|CD|Triassic|Triassic|[Re]. Medium- to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.||||||
4137|Clematis Group|30692|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
4137|Clematis Group|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
4137|Clematis Group|31079|6|Mentioned|Fig. 6|||||||||
4137|Clematis Group|31401|6|Mentioned|Fig.1|||P30||||||
4137|Clematis Group|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
4137|Clematis Group|35901|6|Mentioned|Fig.1|||||||||
4137|Clematis Group|36121|6|Mentioned|p25|||||||||
4137|Clematis Group|36233|6|Mentioned|Table 1|||||||||
4137|Clematis Group|36472|6|Mentioned|Map legend|Triassic|Triassic|||||||
4137|Clematis Group|37565|6|Mentioned|p7|||||||||
4137|Clematis Group|37610|6|Mentioned|Fig.3|||||||||
4137|Clematis Group|37612|6|Mentioned|Fig.1|||See also Fig.3 and P284.||||||
4137|Clematis Group|38518|6|Mentioned|Fig.3|||||||||
4137|Clematis Group|39212|6|Mentioned|p14|||||||||
4137|Clematis Group|39269|6|Mentioned|Fig.1|||||||||
4137|Clematis Group|39445|5|Briefly described|p116|||Early-mid Trias Group status in Bowen B., Fm. status in Galilee B. See also Chart 7.||||||
4137|Clematis Group|39491|4|Described|p22|||||||||
4137|Clematis Group|39943|6|Mentioned|Table 5A|||See also Table 5B||||||
4137|Clematis Group|40120|4|Described|p428|||||||||
4137|Clematis Group|40245|6|Mentioned|Table 2|||||||||
4137|Clematis Group|40250|6|Mentioned|Table 6|||||||||
4137|Clematis Group|40539|6|Mentioned|Fig.2|||||||||
4137|Clematis Group|40574|6|Mentioned|p4|||||||||
4137|Clematis Group|40675|6|Mentioned|Table 5A|||||||||
4137|Clematis Group|40767|6|Mentioned|p14|||||||||
4137|Clematis Group|40999|6|Mentioned|p303|||||||||
4137|Clematis Group|41101|6|Mentioned|p295|||||||||
4137|Clematis Group|41191|6|Mentioned|p284|||||||||
4137|Clematis Group|41246|6|Mentioned|Map legend|Triassic||||||||
4137|Clematis Group|41266|6|Mentioned|Fig.3|||||||||
4137|Clematis Group|41605|6|Mentioned|fig.2|||||||||
4137|Clematis Group|42259|6|Mentioned|p18|||||||||
4137|Clematis Group|42634|5|Briefly described|Table 2 P10|||||||||
4137|Clematis Group|42701|4|Described|p74|||||||||
4137|Clematis Group|42911|5|Briefly described|p11|||||||||
4137|Clematis Group|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
4137|Clematis Group|42999|5|Briefly described|Table 1,p90|Middle Triassic|Early Triassic|||||||
4137|Clematis Group|43000|5|Briefly described|p108|||see also Fig.5,p112||||||
4137|Clematis Group|43185|5|Briefly described|6||Triassic|||||||
4137|Clematis Group|43714|6|Mentioned|Fig.3,p5||Triassic|||||||
4137|Clematis Group|44245|5|Briefly described|Map Legend||Triassic|||||||
4137|Clematis Group|45095|6|Mentioned|p3|||||||||
4137|Clematis Group|45110|3|Fully described|Table 17|||See also Fig.5.||||||
4137|Clematis Group|45151|5|Briefly described|Table 10|||See also Table 11 & p15. Contains former Carborough Sandstone.||||||05-SEP-18
4137|Clematis Group|46989|5|Briefly described|Table 1|||||||||
4137|Clematis Group|50602|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Sandstone, siltstone, mudstone, conglomerate.||||||
4137|Clematis Group|60659|5|Briefly described|p21, p89|Middle Triassic|Triassic|Medium- to coarse-grained quartzose to sublabile micaceous sandstone, siltstone, minor mudstone and granule to pebble conglomerate. Conformably overlies the Rewan Group. Geological Province: Bowen Basin.||||||07-FEB-11
4137|Clematis Group|61076|5|Briefly described|p188 Fig. 2|Triassic|Triassic|Age: >240Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
4137|Clematis Group|61612|6|Mentioned|p275, p270 Fig. 1|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||13-MAR-09
4137|Clematis Group|61782|5|Briefly described|p281|||Geological Province: Taroom Trough. Quartzose.||||||
4137|Clematis Group|62357|5|Briefly described|p524 Fig. 7|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
4137|Clematis Group|63713|5|Briefly described|p1507 Fig.2, p1512|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Overlies Rewan Group. Is overlain by Moolayember Formation and Warang Sandstone.||
4137|Clematis Group|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Is overlain by Moolayember Formation.||
4137|Clematis Group|64856|3|Fully described|p42, p69, p71-75, p77-78, p102|Middle Triassic|Early Triassic|Originally the Clematis Sandstone of Jensen (1926). Upgraded to Group status by Jensen (1975). Bowen Basin, Galilee Basin. Mainly quartzose sandstone. Contains the Glenidal Formation and Expedition Sandstone. Conformably to disconfomably overlies the Rewan Group; the nature of the contact is uncertain. Is overlain conformably by Snake Creek Mudstone Member (Moolayember Formation). Up to 460m thick. Age from palynoflora (units APT2-3).| | ||||28-NOV-17
4137|Clematis Group|64857|5|Briefly described|p113 Fig.3|||Denison Trough, Taroom Trough of Bowen Basin. Includes Showgrounds Sandstone.||||||
4137|Clematis Group|64858|6|Mentioned|p180 Fig.2, p181 Tb.1, p182 Fig.3, p183|Middle Triassic|Middle Triassic|Bowen Basin.||||||30-NOV-09
4137|Clematis Group|65003|5|Briefly described|p6|||Of Bowen Basin.||||Overlies the Rewan Formation.|Sandstone.|30-MAR-12
4137|Clematis Group|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Early Triassic|Unit in the Bowen Basin. Includes Showgrounds Sandstone. Underlies Moolayember Formation.||||||22-MAR-12
4137|Clematis Group|65113|5|Briefly described|p347, Fig 4 p340|Middle Triassic|Early Triassic|Overlies the Rewan Group, contains more quartz rich units than overlying and underlying units. Depositional environment was a braided river system.||||||
4137|Clematis Group|65114|5|Briefly described|p385 Fig.3|Middle Triassic|Early Triassic|||||||
4137|Clematis Group|65115|5|Briefly described|p425, Fig 2 p403, p421 Fig.14|Middle Triassic|Early Triassic|Underlies the Moolayember Formation in the Denison Trough, Bowen Basin. Includes Expedition Sandstone and Glenidal Formation.||||||
4137|Clematis Group|65116|5|Briefly described|p450, Fig 2 p436|Middle Triassic|Early Triassic|Includes Showgrounds Sandstone at top. Underlies the Moolayember Formation in the Bowen Basin.||||||
4137|Clematis Group|65118|5|Briefly described|p491, Fig 2 p479|Triassic|Triassic|Underlies the Moolayember Formation in the Denison Trough, Bowen Basin. Includes Showgrounds Sandstone?||||||06-MAR-12
4137|Clematis Group|65119|5|Briefly described|Fig 2 p503, Fig 7- 8, 11-12|Middle Triassic|Early Triassic|Bowen Basin. Sandstone and conglomeratic sandstone, minor siltstone. Max thickness 3220m.||||||
4137|Clematis Group|65388|6|Mentioned|p203|||?Overlies Rewan Group, but not in the area of this report.||||||
4137|Clematis Group|65706|4|Described|p12, p18 Tb.1|Middle Triassic|Early Triassic|Bowen Basin. Fluvial.||||Conformable on Rewan Group.|Medium to coarse-grained, cross-bedded, quartzose to sublabile and micaceous sandstone; siltstone, mudstone and granule to pebble conglomerate; some fine conglomerate and grey and red mudstone.|
4137|Clematis Group|66188|6|Mentioned|441, 450, Fig 3, TB1, Fig 16-17|Middle Triassic|Late Permian|||||||
4137|Clematis Group|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p5 Fig.3, p6-8|||Denison and Southern Taroom Trough, Bowen Basin.||||||
4137|Clematis Group|67133|6|Mentioned|p20-21|||||||Overlies Rewan Group. Is overlain by Moolayember Formation.||
4137|Clematis Group|67402|4|Described|p19 fig WSD3, WSD4, p21|Anisian|Olenekian|Galilee Basin. Prospective unit for the storage of carbon dioxide, particularly the fluvial sandstone unit which has a porosity of 16.8%. Deposited in fluvial to fluvial-deltaic depositional environments. See also p45, p48 fig BWS1, p55, p57, p72, p80, p85 tbl BWN2, p124 fig GLL1, p165 tbl LPB1.||||Unconformably overlies the Rewan Group. Overlain by the Showgrounds Sandstone.|Quartzose to sublabile, micaceous sandstone, siltstone, mudstone and conglomerate.|
4137|Clematis Group|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.|||Includes Showgrounds Sandstone.|Overlies Rewan Group. Is overlain by Moolayember Formation.||
4137|Clematis Group|68279|5|Briefly described|p1-2,p4, p5 Tb.2, p7, p12-13,p15,p17-19|Anisian|Anisian|See also p16 Tb.4. Galilee Basin. A carbon geostorage target reservoir, sealed by Moolayember Formation. Deposited by a braided river system. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Overlies Rewan Group. Is overlain conformably by Moolayember Formation.|Predominantly quartzose. Includes very fine-grained, moderately sorted, angular sandstone consisting of quartz, minor feldspars and rock fragments; limited occurrence of 50cm intercalations of clayey siltstones.|
4137|Clematis Group|68411|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably overlain by the Moolayember Formation. Conformably underlain by the Rewan Formation.|Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin.||||Conformably overlies Rewan Group. Is overalin conformably by Moolayember Formation.||
4137|Clematis Group|68576|5|Briefly described|Q_4: p1, p3, p5-7, p10, p12 Fig.14|Middle Triassic|Early Triassic|See also p14 Fig.17, p16, p21, p24. Bowen Basin. Sediments sourced from the craton to the W.|||Expedition Sandstone, Glenidal Formation.|Unconformably overlies Rewan Group. Is overlain by Snake Creek Mudstone Member (Moolayember Formation).|Sub-labile to quartzose sandstone, conglomeratic sandstone.|
4137|Clematis Group|68679|5|Briefly described|p353, p364, p376-377, p381, p397|Triassic|Triassic|Connors-Auburn Province. Quartzose sediment supply was mainly from the craton (in the W).||||Overlies the Rewan Group. Is overlain by the Moolayember Formation. In Roma area, upper part is equivalent to Showgrounds Sandstone.||
4137|Clematis Group|68731|5|Briefly described|p198, p200, p201, pp201-202 Fig 3.111|Middle Triassic|Early Triassic|Swarbrick and Wallin (1976). Bowen Basin. Has a comparable distribution to the Rewan Group. Possibly equivalent to the Clematis Sandstone.||||Unconformably to disconformably underlain by the Dunda beds.||03-JUL-14
4137|Clematis Group|68901|6|Mentioned|p2 Fig. i|Triassic|Triassic|||||||26-SEP-18
4137|Clematis Group|69681|6|Mentioned|p83 Fig.7|||Mineralogy and likely chemical changes from CO2 injection discussed.||||||
4137|Clematis Group|69952|6|Mentioned|p85|Triassic|Triassic|||||||
4137|Clematis Group|71710|4|Described|p370, 380, 381, 382, 383, 384, 385, 387|Middle Triassic|Early Triassic|Geological province: Galilee Basin.  ?Also Bowen Basin?(p387) Also known as Clematis Sandstone in northern Galilee Basin?. Provenance may be from Anakie Inlier as an intrusive high during Early Triassic, and other volcaniclastic input. Sequence 9.||sequence 9 + part 10.||Overlain by Moolayember Formation. Unconformably to disconformably underlain by Rewan Group. Possible lateral equivalent to Warang Sandstone and Dunda beds in upper and lower section respectively.|Moderately sorted, fine to coarse-grained quartzose sandstone with minor red siltstone and mudstone and rare conglomerate|22-MAY-19
4137|Clematis Group|72088|5|Briefly described|p8, p15, p17, p21-p23, p91|Anisian|Anisian|Southern and Eastern Galilee Basin and Bowen Basin. Deposited by braided rivers.||||Unconformably overlies the Dunda beds and Rewan Group. Conformably overlain by the Moolayember Formation.|Sandstone with a kaolonitic matrix and lesser amounts of siltstone and mudstone.|
4137|Clematis Group|72297|5|Briefly described|p744|||Bowen Basin. A significant regional hydrocarbon reservoir.|||Showgrounds Sandstone.|||
4137|Clematis Group|73036|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73037|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73038|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73040|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Medium to coarse-grained quartzose to sublabile, micaceous sandstone, siltstone, mudstone and granule to pebble conglomerate.|
4137|Clematis Group|73113|6|Mentioned|p22-24, p36, p41, p46, p172, p191|||Bowen Basin. Regional aquifer. Written as equivalent to Showgrounds Sandstone [now a parent unit].||||||
4137|Clematis Group|73246|6|Mentioned|p190|Middle Triassic|Middle Triassic|Bowen Basin, northeast and northwest.||||Underlain by Rewan Group. Overlain by Moolyamber Formation.||
4137|Clematis Group|73304|6|Mentioned|p76|||||||||
4137|Clematis Group|73472|5|Briefly described|p115, p120, p129, p131, App.1|Anisian|Anisian|Bowen Basin. Not represented in the northeastern Galilee Basin. Previously thought to occur within Porcupine Gorge; however, these strata are younger and were formalized as the Porcupine Gorge Formation.||||Underlain by Rewan Group. Overlain by Moolayember Formation. Equivalent to Clematis Formation.||
4137|Clematis Group|73570|5|Briefly described|p914, p915 Fig.4, p916, p919 Fig.6|Middle Triassic|Middle Triassic|Bowen Basin.|||||Includes fluviatile, quartz-rich sandstones.|
4144|Clevedale Migmatite|6823|6|Mentioned|p205|Palaeoproterozoic|Palaeoproterozoic|||||Underlies the Thackaringa Group.||26-MAR-22
4144|Clevedale Migmatite|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|Part of Willyama Supergroup.||||||11-JUN-08
4144|Clevedale Migmatite|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
4144|Clevedale Migmatite|22588|6|Mentioned|p85|||||||||
4144|Clevedale Migmatite|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
4144|Clevedale Migmatite|22771|5|Briefly described|Table12.2p45,47|||||||||
4144|Clevedale Migmatite|22857|5|Briefly described|p45 Tb. 12.2, p392 App.1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: 425m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
4144|Clevedale Migmatite|22884|6|Mentioned|p41, p43 Fig. 3|||Geological province: Broken Hill Domain.  Correlates with Morialpa Migmatite in the Olary Domain.||||||26-MAR-09
4144|Clevedale Migmatite|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|22962|6|Mentioned|p74||Statherian|||||||
4144|Clevedale Migmatite|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Gandry Dam Gneiss (Mt Isa Maronan Supergroup) and lower sequence of the Georgetown (Qld) Etheridge Group.||||||07-NOV-08
4144|Clevedale Migmatite|22965|6|Mentioned|Fig 1||Statherian|||||||
4144|Clevedale Migmatite|22966|6|Mentioned|Fig1||Proterozoic|Early rift stage of devlopment.||||||
4144|Clevedale Migmatite|22967|5|Briefly described|p25,6,39,41||Statherian|||||||
4144|Clevedale Migmatite|23025|6|Mentioned|Fig1p75|||||||||
4144|Clevedale Migmatite|23160|6|Mentioned|fig1|||||||||
4144|Clevedale Migmatite|23248|5|Briefly described|Fig2p169|||||||||
4144|Clevedale Migmatite|23347|6|Mentioned|p52|||Geological province: Broken Hill Domain. Equivalent to parts of Wiperaminga Subgroup.||||||24-MAR-09
4144|Clevedale Migmatite|24307|5|Briefly described|p967 Fig. 2|Proterozoic|Proterozoic|||||||
4144|Clevedale Migmatite|38969|4|Described|p204|||||||||
4144|Clevedale Migmatite|39662|2|Defined|p411|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|39883|6|Mentioned|p380|||||||||
4144|Clevedale Migmatite|40290|6|Mentioned|Fig.2|||||||||
4144|Clevedale Migmatite|40822|6|Mentioned|Fig.2|||||||||
4144|Clevedale Migmatite|41093|4|Described|p251|||||||||
4144|Clevedale Migmatite|41145|6|Mentioned|Fig.4|||||||||
4144|Clevedale Migmatite|41630|5|Briefly described|p6|||Mention p65||||||10-OCT-06
4144|Clevedale Migmatite|42261|6|Mentioned|Fig 1 P530|||||||||
4144|Clevedale Migmatite|42537|6|Mentioned|Fig.2 P5|||||||||
4144|Clevedale Migmatite|42595|6|Mentioned|Fig. 2 P5|||||||||
4144|Clevedale Migmatite|42720|5|Briefly described|map legend|Paleoproterozoic||Variation on Clevedale Migmatite, NSW.||||||07-NOV-08
4144|Clevedale Migmatite|42897|5|Briefly described|Fig.3, P321|||||||||
4144|Clevedale Migmatite|42942|6|Mentioned|p17|||Of Willyama Supergroup.||||||11-JUN-08
4144|Clevedale Migmatite|43052|6|Mentioned|Fig.4.22|||||||||
4144|Clevedale Migmatite|43086|6|Mentioned|Fig.3|||||||||
4144|Clevedale Migmatite|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
4144|Clevedale Migmatite|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
4144|Clevedale Migmatite|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
4144|Clevedale Migmatite|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
4144|Clevedale Migmatite|43572|6|Mentioned|Fig.3.2 p6|||||||||
4144|Clevedale Migmatite|43583|5|Briefly described|Table 1, p2139|||||||||
4144|Clevedale Migmatite|46598|5|Briefly described|p303|||||||||
4144|Clevedale Migmatite|50045|5|Briefly described|p116 Fig. 3, p114 Fig. 1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Thorndale Composite Gneiss.||||||31-MAY-07
4144|Clevedale Migmatite|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.  Metasedimentary pelitic to psammitic migmatite.  Geological Province: Broken Hill Block.||||||07-NOV-08
4144|Clevedale Migmatite|60485|5|Briefly described|p28 Fig. 2|||Not of the Thackaringa Group. Geological Province: Broken Hill Domain.||||||23-JUN-08
4144|Clevedale Migmatite|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||18-MAY-06
4144|Clevedale Migmatite|61735|5|Briefly described|p635 Fig. 1, p653|Paleoproterozoic|Paleoproterozoic|Overlain by Thorndale Composite Gneiss. See also p636 Fig. 2.||||||30-JUN-09
4144|Clevedale Migmatite|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological province: Olary Domain.||||||
4144|Clevedale Migmatite|62535|6|Mentioned|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||||||
4144|Clevedale Migmatite|62536|5|Briefly described|p635-636, 653|||Broken Hill area.||||Is overlain by Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
4144|Clevedale Migmatite|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
4144|Clevedale Migmatite|63102|5|Briefly described|p13-15|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
4144|Clevedale Migmatite|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
4144|Clevedale Migmatite|63866|5|Briefly described|p36||||c. 1710 Ma (Max. deposition)|Willyama Supergroup||||
4144|Clevedale Migmatite|64097|5|Briefly described|p303, p325|Paleoproterozoic|Paleoproterozoic|Underlies Thorndale Composite Gneiss. Geological province: Broken Hill Domain/Curnamona province. Partially melted metasediments with or without albitic alteration.||||||07-FEB-11
4144|Clevedale Migmatite|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-FEB-11
4144|Clevedale Migmatite|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
4144|Clevedale Migmatite|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Underlies Thorndale Composite Migmatite. Geological province: Broken Hill Domain. Comprises partially melted clastic metasediments distinguished by thin layers or laminae of albitised metasediments; magnetite-bearing.G55||||||07-FEB-11
4144|Clevedale Migmatite|64743|6|Mentioned|p339 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
4144|Clevedale Migmatite|64744|5|Briefly described|p353 Fig.4, p354. |Statherian|Statherian|Broken Hill Domain. High-grade metasedimentary rocks.||Unit in Willyama Supergroup.||Overlies Redan Gneiss. Is overlain by Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||07-FEB-11
4144|Clevedale Migmatite|65681|6|Mentioned|p734 Fig.1.|||Broken Hill Block.||||||
4144|Clevedale Migmatite|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. |ca. 1710 (U-Pb zircon)|Thackaringa Group||Overlain by the Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Is overlain by Thorndale Composite Gneiss.||
4144|Clevedale Migmatite|70000|5|Briefly described|p34-35|Statherian|Statherian|Among the oldest outcropping units in the Broken Hill Domain. Protolith was relatively sandy shallow marine sedimentary rocks with a possible evaporitic or hypersaline component represented by albitic horizons.||Unit in Thorndale Composite Gneiss.|||Metasedimentary gneiss and migmatite +/- albitic horizons hosting ubiquitous sills and dykes of basic gneiss.|
4144|Clevedale Migmatite|70014|5|Briefly described|Map legend|||Bedding extensively disrupted and mainly thin and discontinuous.||Unit in Willyama Supergroup.||Is overlain by Thorndale Composite Gneiss.|Mainly migmatite to quartzo-feldspathic composite gneiss (commonly leucocratic). Minor basic gneiss and vey rare, thin, plagioclase-quartz rock and medium-grained biotite-rich quartzo-feldspathic gneiss.|
4144|Clevedale Migmatite|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Thorndale Composite Gneiss.|||Migmatite to migmatitic composite gneiss; minor basic gneiss, rare plagioclase-quartz rock and biotite-rich quartzofeldspathic gneiss.|
4144|Clevedale Migmatite|70657|5|Briefly described|p10 Fig.4, p12, p13 Fig.6, p15, p34|Statherian|Statherian|Curnamona Province; Mulyungarie, Broken Hill Domains. Shown as Thackaringa Group + Thorndale Composite Gneiss + Clevedale Migmatite in Fig.4.|> ~1705 Ma|Thorndale Composite Gneiss (Thackaringa Group ).||Overlies Redan Gneiss.||
4144|Clevedale Migmatite|70658|6|Mentioned|p15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
4144|Clevedale Migmatite|72461|6|Mentioned|p16 fig 9|||||||||
4144|Clevedale Migmatite|73243|6|Mentioned|p52 Fig.1, p53 Fig.2 p59|||Broken Hill block-Euriowie block. Some amphibolite bodies appear to transgress bedding, interpreted as dykes emplaced during or immediately after deposition of the Broken Hill Group. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.||Willyama Supergroup|||Contains amphibolite dykes.|
4144|Clevedale Migmatite|73308|6|Mentioned|p607 Fig.1|||||Willyama Supergroup.||||
4144|Clevedale Migmatite|73482|6|Mentioned|p422 Fig.3|||||Thorndale Composite Gneiss||||
4144|Clevedale Migmatite|73512|6|Mentioned|p7|||||Willyama Supergroup||||
4144|Clevedale Migmatite|73524|6|Mentioned|p5 Fig.3|||||Thackaringa Group||||
4144|Clevedale Migmatite|73575|6|Mentioned|p828 Fig.2, p829 Fig.3|||||Thorndale Composite Gneiss||||
4147|Clifden Formation|721|5|Briefly described|Map legend|Westphalian|Namurian|Crossbedded, feldspathic and lithic sandstone, subordinate conglomerate, shale, rhyodacitic and dacitic airfall tuffs.  Geological Province: Tamworth Belt.||||||21-DEC-04
4147|Clifden Formation|22857|5|Briefly described|p506 App.1 Tb.A1.8|Carboniferous|Carboniferous|Feldspathic and lithic sandstone, subordinate conglomerate, shale, rhyodacitic and dacitic airfall tuffs. Max. thickness: 600m.||||||
4147|Clifden Formation|23050|5|Briefly described|p9 Fig.2|Late Carboniferous|Late Carboniferous|Of Tamworth Belt.||||||
4147|Clifden Formation|23051|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|of Tamworth Belt.||||||
4147|Clifden Formation|23861|5|Briefly described|p3, p4 Fig. 2|Namurian|Namurian|Overlain by Rocky Creek Conglomerate; underlain by Ermelo Pyroclastics.  Geological Province: New England Orogen.||||||
4147|Clifden Formation|24010|5|Briefly described|p379|Namurian|Namurian|||||||
4147|Clifden Formation|24334|5|Briefly described|p49 Tb.1|Namurian|Namurian|Age: 316 - 321 Ma.||||||
4147|Clifden Formation|24348|5|Briefly described|p131|Carboniferous|Carboniferous|||||||
4147|Clifden Formation|24603|5|Briefly described|p866|Namurian|Namurian|See also p895 Fig. 16.  Geological Province: Tamworth Belt.||||||
4147|Clifden Formation|24605|2|Defined|p931, p937, p949 App.1|Namurian|Namurian|Overlain by the Rocky Creek Conglomerate. Overlies the Wanganui Andesite Member. Maximum Thickness: 650m. Geological Province: New England Orogen.||||||
4147|Clifden Formation|30133|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
4147|Clifden Formation|30135|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4147|Clifden Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4147|Clifden Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4147|Clifden Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
4147|Clifden Formation|34085|6|Mentioned|Cor.chart|||Westphalian - Stephanian||||||
4147|Clifden Formation|34349|5|Briefly described|p246|||||||||
4147|Clifden Formation|36528|6|Mentioned|p180|||||||||
4147|Clifden Formation|36961|6|Mentioned|Fig.3|||||||||
4147|Clifden Formation|37919|5|Briefly described|p477|||||||||
4147|Clifden Formation|38837|6|Mentioned|p232|||||||||
4147|Clifden Formation|39331|6|Mentioned|Table 10-1|||||||||
4147|Clifden Formation|41009|6|Mentioned|Fig.2|||||||||
4147|Clifden Formation|42547|4|Described|p19|||319my.||||||
4147|Clifden Formation|43091|5|Briefly described|Map legend|||||||||
4147|Clifden Formation|43383|14|Not recorded|p17|||||||||
4147|Clifden Formation|43421|4|Described|p677||Carboniferous|||||||
4147|Clifden Formation|43429|14|Not recorded|Map Legend|||1000-2000ft thick. Includes Peri Rhyolite Tuff (q.v.), a useful marker horizon||||||
4147|Clifden Formation|43434|4|Described|Map Legend||Carboniferous|||||||
4147|Clifden Formation|43435|2|Defined|Map Legend||Carboniferous|||||||
4147|Clifden Formation|43436|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
4147|Clifden Formation|43479|14|Not recorded|p177||Westphalian|||||||
4147|Clifden Formation|43538|14|Not recorded|p2|||Lower Carboniferous fauna||||||
4147|Clifden Formation|43582|6|Mentioned|p17|||||||||
4147|Clifden Formation|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
4147|Clifden Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
4147|Clifden Formation|47056|6|Mentioned|Fig.2 P523|||||||||
4147|Clifden Formation|50132|6|Mentioned|p246||Late Carboniferous|||||||
4147|Clifden Formation|50613|5|Briefly described|p206 Fig. 2|Namurian|Namurian|Of the Currangandi Group.  Geological Province: New England Orogen.  See also p226.||||||
4147|Clifden Formation|50629|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: New England Orogen.||||||05-JUL-04
4147|Clifden Formation|60299|5|Briefly described|p208|Carboniferous|Carboniferous|Age: c. 318 Ma. Geological Province: Rocky Creek Block.||||||
4147|Clifden Formation|61214|5|Briefly described|p170, p171 Fig. 1|Namurian|Namurian|Includes the several members. Geological Province: Boomi, Kathrose and Darthula blocks. See also p172 Fig. 2.||||||23-JAN-06
4147|Clifden Formation|61767|4|Described|p71|||Composed of terrestrial pebbly lithic sandstone, sandstone, siltstone and ash-rich siltstone and a variety of volcanic rocks including pyroclastic flow, fall and surge deposits. Max. thickness: >600m. Geological Province: Tamworth Belt.||||||
4147|Clifden Formation|62095|6|Mentioned|p267|||In Rocky Creek block/Tamworth Belt.||||||
4147|Clifden Formation|63832|5|Briefly described|p131 fig 2, p134|Bashkirian|Serpukhovian|Rocky Creek Syncline, Tamworth Belt. Marks the termination of glacial conditions at the end of Glaciation C1.||||Overlies Spion Kop Conglomerate.|Fluvial sandstones, conglomerates and commonly carbonaceous mudrocks with plant fossils. Alluvial facies and pyroclastic rocks underlie glacial deposits of C3.|13-DEC-17
4147|Clifden Formation|64631|5|Briefly described|p44 Fig.2.|Bashkirian|Serpukhovian|Southern New England Fold Belt, Rocky Creek Syncline. Some biostratigraphic and radiometric age control within unit. ||||Overlies Spion Kop Conglomerate. Underlies Rocky Creek Conglomerate.||
4147|Clifden Formation|65107|6|Mentioned|p276, 282||Late Paleozoic|Member of the Rocky Creek Block. No age given.||||||
4147|Clifden Formation|65382|5|Briefly described|p714|Bashkirian|Serpukhovian|Includes Ermelo Pyroclastics and Peri Rhyolite Member. Overlies Spion Kop Conglomerate. Age inferred from member ages.||||||
4147|Clifden Formation|65902|5|Briefly described|p203-4|Carboniferous|Carboniferous|Includes Wanganui Andesite Member and Ermelo Pyroclastics. Volcanics.||||||09-MAR-12
4147|Clifden Formation|68003|5|Briefly described|p32 Fig.3-h, p137. |Namurian|Namurian|Tamworth Belt (North), New England Fold Belt.|||Includes Peri Rhyodacite Tuff, Appleogue Dacite and Wanganui Andesite.|Overlies Ermelo Dacite Tuff. Is overlain by Rocky Creek Conglomerate and, locally, by Peri Tuff.|Cross-bedded, coarse-grained, fluvial feldspathic and lithic sandstone; subordinate orthoconglomerate, mudstone, carbonaceous shale; felsic to intermediate tuff; rhyolitic ignimbrites.|
4147|Clifden Formation|68004|5|Briefly described|p134.|||Potential for zeolite resources and levels of certainty are discussed.||||||
4147|Clifden Formation|68005|5|Briefly described|p49 Fig.3-M, p57, pp144-145, p170.|Westphalian|Namurian|Rocky Creek Block, Tamworth Belt. With Spion Kop Conglomerate, represents a period of glacial retreat.|||Includes Peri Rhyodacite Tuff, Appleogue Dacite and Wanganui Andesite.|Overlies Ermelo Dacite Tuff. Is overlain by Rocky Creek Conglomerate and, locally, by Peri Tuff.|Cross-bedded coarse-grained fluvial feldspathic and lithic sandstone, subordinate orthoconglomerate, mudstone, carbonaceous shale and felsic to intermediate tuff.|
4147|Clifden Formation|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Visean|Rocky Creek Block, Tamworth Belt.||||||
4147|Clifden Formation|70728|5|Briefly described|p265,271-273|Serphukovian|Visean|Geological province: North Tamworth terrane, New England Orogen. Contains SHRIMP zircon ages of 324.9+\-2.8 and 327+\-2.9 Ma from the top and middle of the unit respectively (Roberts et al., 2003; Roberts et al., 2006; Roberts and James, 2010).|||Includes Spion Kop Conglomerate.|Overlain by Rocky Creek Conglomerate. Underlain by Spion Kop Conglomerate or Caroda Formation.||
4152|Clifford Formation|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Horshoe Creek (spelt Horshoe Creek) Subgroup.   Geological Province: Sydney Basin||||||
4152|Clifford Formation|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Horseshoe Creek Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
4152|Clifford Formation|29942|3|Fully described|p11|||||||||
4152|Clifford Formation|45090|6|Mentioned|p187|||Refers Britten (1972)||||||
4152|Clifford Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Basal unit in Horseshoe Creek Sub-group.||Overlies Charlton Formation. Is overlain by Alcheringa Coal.|A dominantly sandstone sequence with minor tuffaceous claystone and vestigial coal beds.|
4152|Clifford Formation|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. CA-TIMS ages of 255.02 and 255.26 Ma on Nobbys Tuff (Metcalfe etal., 2015). Corresponding to APP5 zone (Lopingian).||Unit of Newcastle Coal Measures.|Includes Nobbys Tuff.|||24-DEC-21
4152|Clifford Formation|73304|6|Mentioned|p65|||||||||
4163|Clifton Subgroup|22549|5|Briefly described|p526||Late Permian|contains 5 sub-units, Wombarra, Scarborough, Lower Bulgo, Bald Hill operational units||||||12-OCT-15
4163|Clifton Subgroup|22857|5|Briefly described|p520 App.1 Tb.A1.9|Early Triassic|Late Permian|Of the Narrabeen Group. Max. thickness: 492m in Newcastle Coalfield area. Geological Province: Sydney Basin. See also pages 524 and 530 in App.1 Tb.A1.9.||||||
4163|Clifton Subgroup|22969|5|Briefly described|Fig 2.2||Early Triassic|Narrabeen Group.||||||
4163|Clifton Subgroup|24121|5|Briefly described|p231|Permian|Permian|Of Narrabeen Group.||||||
4163|Clifton Subgroup|31878|6|Mentioned|Table 1|||||||||
4163|Clifton Subgroup|40602|6|Mentioned|p9|||||||||
4163|Clifton Subgroup|42737|5|Briefly described|map legend|Triassic||||||||
4163|Clifton Subgroup|42896|4|Described|p25, Table 2|||of Narrabeen Group||||||
4163|Clifton Subgroup|42916|5|Briefly described|Table 1||Early Triassic|||||||
4163|Clifton Subgroup|42925|5|Briefly described|Table 18||Early Triassic|||||||
4163|Clifton Subgroup|42926|4|Described|map legend|Early Triassic|Late Permian|||||||
4163|Clifton Subgroup|43257|5|Briefly described|Map Legend|Early Triassic|Late Permian|Of Narrabeen Group||||||
4163|Clifton Subgroup|43317|6|Mentioned|p10|||||||||
4163|Clifton Subgroup|43318|14|Not recorded|opp p6||Late Triassic|||||||
4163|Clifton Subgroup|43320|14|Not recorded|Table 1 p10||Triassic|Part of Narrabeen Group||||||
4163|Clifton Subgroup|43448|14|Not recorded|p224||Early Triassic|On table only. Inc. Munmorah Formation. Unit of Narrabeen Group.||||||
4163|Clifton Subgroup|43449|14|Not recorded|p11;opp.12;Pl.2|||||||||
4163|Clifton Subgroup|43980|14|Not recorded|Pl.1|||||||||
4163|Clifton Subgroup|60281|5|Briefly described|Fig. 7 Appendix 1|Early Triassic|Early Triassic|Of the Narrabeen Group.  Age: <250Ma.  Geological Province: Sydney Basin.||||||
4163|Clifton Subgroup|61315|5|Briefly described|Table SY1|Eary Triassic|Early Triassic|Of the Narrabeen Group. Includes 6 named units. Geological Province: Sydney Basin||||||
4163|Clifton Subgroup|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.||||||
4163|Clifton Subgroup|69297|6|Mentioned|p501|Olenekian|Induan|Sydney Basin. ||Narrabeen Group||Unconformably overlies the Illawarra Coal Measures. Overlain by the Gosford Group.||
4163|Clifton Subgroup|70647|5|Briefly described|Map Legend|Middle Triassic|Late Permian|Sydney Basin.||Narrabeen Group|Includes Patonga Claystone, Tuggerah Formation, Munmorah Conglomerate, Dooralong Formation.|||04-OCT-16
4165|Cliftonwood Limestone Member|22857|4|Described|p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Yass Formation. Argillaceous black limestone, mudstone. Richly fossiliferous, important corals, and conodonts. Max. thickness: 65m. Geological Province: Canberra-Yass Shelf.||||||03-APR-07
4165|Cliftonwood Limestone Member|38035|6|Mentioned|p91|||||||||
4165|Cliftonwood Limestone Member|42820|5|Briefly described|p36|||Of the Yass Formation.||||||02-JUN-08
4165|Cliftonwood Limestone Member|42994|6|Mentioned|p73|||Of the Yass Formation.||||||02-JUN-08
4165|Cliftonwood Limestone Member|50230|4|Described|Map legend|Wenlock|Wenlock|Of the Yass Formation (Douro Group). Interbedded with the O'Briens Creek Sandstone Member within the Yass Formation. Grey limestone in mudstone breccia, clast-supported, pebbles of crystalline fossiliferous limestone.||||||03-APR-07
4165|Cliftonwood Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yass Formation (Douro Gp). Grey to khaki laminated to very thinly-bedded chloritic siltst./ mudstone with thin fine-gr.sst beds, schistose massive to diffusely med.-gr. poorly-sorted chloritic feldspathic sandstone, and minor qtz-rich sandstone.||||||02-JUN-08
4165|Cliftonwood Limestone Member|68592|2|Defined|p497-503, p509-13, p515, p517-8, p521|Early Silurian|Early Silurian|See also p428, p430 Fig.89, p433-5, p440, p485, p492, p1875-6. Owen and Wyborn (1979); a unit in their Yass Formation. Formerly Cliftonwood Limestone of Link (1970, 1971); Link and Druce (1972), a Formation in their Yass Group. Named after Cliftonwood property. Type section described. Over 64m thick. Supratidal to intertidal environments of deposition. Contains a rich fauna of corals, brachiopods, molluscs, trilobites, bryozoans, algae, sponges, ostracods, annelids and conodonts.||Unit in Yass Formation.||Gradationally overlies O'Briens Creek Sandstone Member. Is overlain conformably by Laidlaw Volcanics. Correlates with Connell Member (Glen Bower Formation).|Well-bedded fossiliferous limestone and calcareous mudstone, limestone breccia and conglomerate.|10-JAN-17
4165|Cliftonwood Limestone Member|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdyc. On Yass 1:100 000 mapsheet portion of Time-Space Plot.||Yass Formation|||Well bedded, stromatolitic, calcareous mudstone; poorly fossiliferous limestone, micritic nodular limestone, intraclastic limestone, interbedded mudstone and fine-medium grained sandstone; algal biomicrite and intramicrudite with abundant fossils.|
4165|Cliftonwood Limestone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yass Formation|||Well bedded, stromatolitic, calcareous mudstone; poorly fossiliferous limestone, micritic nodular limestone, intraclastic limestone, interbedded mudstone and fine-medium grained sandstone; algal biomicrite and intramicrudite with abundant fossils.|
4165|Cliftonwood Limestone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yass Formation|||Well bedded stromatolitic calcareous mudstone, poorly fossiliferous limestone, micritic nodular limestone, intraclastic limestone and interbedded mudstone and fine-medium grained sandstone; algal biomicrite and intramicrudite with shelly fossils.|
4165|Cliftonwood Limestone Member|71656|5|Briefly described|p12 Fig.2, p19, p22|Wenlock|Wenlock|Includes brachiopods, ostracods and corals. Species previously used for age determination (Wurmiella excavata) now have a more extended range and can no longer be used as a zonal indicator.||Top of Yass Formation, Douro Group||Partially underlies Laidlaw Volcanics.|Fossiliferous limestone.|
4165|Cliftonwood Limestone Member|71657|6|Mentioned|p48|Silurian|Silurian|Contains the brachiopod Spirinella caecistriata.||Yass Formation||||
4250|Cobargo Supersuite|22878|6|Mentioned|p83|||||||||
4250|Cobargo Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
4250|Cobargo Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Wangarabell Granodiorite||||||01-OCT-04
4250|Cobargo Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
4250|Cobargo Supersuite|24551|5|Briefly described|p236|||Consists of: Wangarabell Suite||||||
4250|Cobargo Supersuite|42726|5|Briefly described|map legend||Early Devonian|Includes the Brogo, Cobargo, Merricumbene and Wangrah Suites.||||||09-FEB-05
4250|Cobargo Supersuite|42827|6|Mentioned|p430|||||||||
4250|Cobargo Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
4257|Cobbitty Claystone Bed|35690|2|Defined|p183|Middle Triassic|Middle Triassic|||||||
4257|Cobbitty Claystone Bed|39298|5|Briefly described|p272|||||||||
4257|Cobbitty Claystone Bed|39626|6|Mentioned|p275|||||||||
4257|Cobbitty Claystone Bed|40602|5|Briefly described|p26|||||||||
4257|Cobbitty Claystone Bed|42896|4|Described|p48|||of Bringelly Shale||||||
4257|Cobbitty Claystone Bed|42925|3|Fully described|p24|||of Bringelly Shale||||||
4260|Cobblers Creek Limestone|22486|6|Mentioned|p 7|||Waugoola Group.||||||15-JUL-08
4260|Cobblers Creek Limestone|22857|5|Briefly described|p468 App.1 Tb.A1.6|Silurian|Silurian|Of the Waugoola Group. Max. thickness: 44m. Geological Province: Molong Rise.||||||
4260|Cobblers Creek Limestone|23214|2|Defined|p109|Llandovery|Llandovery|Basal unit of the Waugoola Group. Mainly comprises thinly bedded calcarenite to calcirudite and calcareous sandstone. Max. thickness 44m.||||||18-MAY-16
4260|Cobblers Creek Limestone|35258|4|Described|p122|||||||||
4260|Cobblers Creek Limestone|40328|6|Mentioned|p20|||||||||
4260|Cobblers Creek Limestone|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Waugoola Group. Consists of coarse, feldspathic and calcareous conglomeratic sandstone; limestone; conglomerate.||||||15-JUL-08
4260|Cobblers Creek Limestone|43653|5|Briefly described|Map Legend||Silurian|||||||
4260|Cobblers Creek Limestone|43782|6|Mentioned|Map diagram|Llandovery|Llandovery|Of Waugoola Group.||||||15-JUL-08
4260|Cobblers Creek Limestone|60989|6|Mentioned|p111, p113|||||Basal Waugoola Group.||||
4260|Cobblers Creek Limestone|63287|6|Mentioned|p317 Fig. 2, p336|Llandovery|Llandovery|Of Waugoola Group. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
4260|Cobblers Creek Limestone|63290|5|Briefly described|p392 Tb. 1, p401 Fig. 5(d), p395|Llandovery|Bolindian|Of Waugoola Group. Overlain by Burly Jacky Sandstone Member. Arc detritus material. Geological Province: Molong Volcanic Belt. ||||||
4260|Cobblers Creek Limestone|70297|5|Briefly described|map legend|Early Silurian|Early Silurian|||Waugoola Group||||
4260|Cobblers Creek Limestone|70684|6|Mentioned|p50 Fig.24|Early Silurian|Early Silurian|Molong Volcanic Belt. ||Waugoola Group.||||
4266|Cobcroft Microgranite|22857|6|Mentioned|p543 App.1 Tb.A1.11|||Pluton. Age: younger than Late Triassic.||||||
4266|Cobcroft Microgranite|42659|5|Briefly described|119|||||||||
4279|Cockburn Formation|22857|6|Mentioned|p204|||||||||
4279|Cockburn Formation|22859|6|Mentioned|p204|||||||||
4279|Cockburn Formation|38194|3|Fully described|p383|||||||||
4279|Cockburn Formation|38804|6|Mentioned|p95|||||||||
4279|Cockburn Formation|39441|6|Mentioned|p30|||||||||
4279|Cockburn Formation|40762|5|Briefly described|p290|||||||||
4279|Cockburn Formation|40960|6|Mentioned|p223|||||||||
4279|Cockburn Formation|41347|6|Mentioned|p162|||||||||
4279|Cockburn Formation|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Part of the "Sandon Association".||||||16-DEC-04
4279|Cockburn Formation|41796|6|Mentioned|p307|||||||||
4281|Cockle Creek Conglomerate Member|29922|6|Mentioned|p49|||||||||
4281|Cockle Creek Conglomerate Member|34351|6|Mentioned|Fig.5.13|||||||||
4281|Cockle Creek Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
4281|Cockle Creek Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
4281|Cockle Creek Conglomerate Member|43447|14|Not recorded|diag.p.26,34|||Part of Lambton Sub-Group||||||
4281|Cockle Creek Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Bogey Hole Formation ||||
4293|Cocoparra Group|22508|3|Fully described|p6||Late Devonian|Geological province: Lachlan Fold Belt. Some units previously in the Cocoparra Group now in the Walters Range Group.||||||09-OCT-08
4293|Cocoparra Group|22638|4|Described|p69|||||||||
4293|Cocoparra Group|22857|5|Briefly described|p211, p212, p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Includes Barrat Conglomerate (basal), Naradhan Sandstone, Womboyne Formation and Rankin Formation. Max. thickness: >5.8km. Geological Province: Barka Basin.||||||
4293|Cocoparra Group|22859|6|Mentioned|p211-12|||||||||
4293|Cocoparra Group|22887|5|Briefly described|p28, Fig.4 p11|Middle Devonian|Early Devonian|||||||
4293|Cocoparra Group|23252|5|Briefly described|Map Legend|||||||||
4293|Cocoparra Group|24005|5|Briefly described|p293|Late Devonian|Middle Devonian|||||||
4293|Cocoparra Group|24580|6|Mentioned|p828 Fig.1|||Group is Gp in text. Geological Province: Eastern Lachlan Fold Belt.||||||
4293|Cocoparra Group|29987|4|Described|p22|||||||||
4293|Cocoparra Group|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
4293|Cocoparra Group|31161|5|Briefly described|PA8|||||||||
4293|Cocoparra Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
4293|Cocoparra Group|32672|6|Mentioned|p674|||||||||
4293|Cocoparra Group|32676|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
4293|Cocoparra Group|32865|6|Mentioned|p484|||Fauna||||||
4293|Cocoparra Group|33269|6|Mentioned|p46|||Refers Conolly (1965). Kaolinite||||||
4293|Cocoparra Group|33732|4|Described|p103|||U.Dev.||||||
4293|Cocoparra Group|34109|3|Fully described|p170|||Upper Devonian||||||
4293|Cocoparra Group|34331|6|Mentioned|p459|||U.Dev.||||||
4293|Cocoparra Group|34400|6|Mentioned|p6|||Upper Devonian - ?Lower Carboniferous||||||
4293|Cocoparra Group|34404|6|Mentioned|Fig.3.8|||Upper Devonian||||||
4293|Cocoparra Group|34406|6|Mentioned|p225|||||||||
4293|Cocoparra Group|34418|6|Mentioned|p502|||||||||
4293|Cocoparra Group|34449|6|Mentioned|Table 2-1|||||||||
4293|Cocoparra Group|34469|6|Mentioned|p116|||||||||
4293|Cocoparra Group|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
4293|Cocoparra Group|35608|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
4293|Cocoparra Group|35609|4|Described|p13|||||||||
4293|Cocoparra Group|36316|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
4293|Cocoparra Group|36317|5|Briefly described|p147|||||||||
4293|Cocoparra Group|40130|6|Mentioned|p195|||||||||
4293|Cocoparra Group|40328|6|Mentioned|p206|||||||||
4293|Cocoparra Group|41126|6|Mentioned|p87|||||||||
4293|Cocoparra Group|41394|6|Mentioned|p94|||||||||
4293|Cocoparra Group|42179|6|Mentioned|Fig.2 P234|||||||||
4293|Cocoparra Group|43383|14|Not recorded|p14,15|||||||||
4293|Cocoparra Group|43389|14|Not recorded|Map Legend||Late Devonian|||||||
4293|Cocoparra Group|43507|14|Not recorded|p124-126,129||Late Devonian|||||||
4293|Cocoparra Group|43508|14|Not recorded|p117,121-123,125|||Relation between grainsize and percent of polycrystalline quartz discussed||||||
4293|Cocoparra Group|43509|14|Not recorded|p111,115,117-9|||||||||
4293|Cocoparra Group|43510|14|Not recorded|p37,38,46|||||||||
4293|Cocoparra Group|43511|3|Fully described|p129-147|||Petrology and origin.||||||25-MAR-08
4293|Cocoparra Group|44192|5|Briefly described|Map Legend|||||||||
4293|Cocoparra Group|44534|5|Briefly described|map legend||Late Devonian|SI 55-6. Upper Devonian.||||||
4293|Cocoparra Group|44936|5|Briefly described|Map Legend||Late Devonian|||||||
4293|Cocoparra Group|50191|6|Mentioned|p6, 21, Fig. 1|Late Devonian|Late Devonian|||||||
4293|Cocoparra Group|60303|5|Briefly described|p5, p6 Fig. 1|Late Devonian|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
4293|Cocoparra Group|61964|3|Fully described|p14 Fig. 4, p113-114|Late Devonian|Late Devonian|Includes: Rankin, Confreys, Barrat + Edithvale Formations, and Hazeldene Sandstone. Mainly fluvial sequence. Max.thickness: ~4064m.Geol.Prov: Lachlan Fold Belt. Possibly correlates with Mulga Downs Group.  For geophysics of this group - see p228-229.||||||09-OCT-08
4293|Cocoparra Group|62367|5|Briefly described|p4 Fig. 2|Late Devonian|Late Devonian|||||||
4293|Cocoparra Group|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Includes Swastika Siltstone, Barrat Formation, Naradhan and Hazeldene Sandstones, Edithvale and Confreys Formations, Melbergen Sandstone., Jimberoo and Rankin Formations.||||||
4293|Cocoparra Group|65469|5|Briefly described|p18, p22|Late Devonian|Early Devonian|Lachlan Orogen.||||Equivalent to the Winduck Group.||
4293|Cocoparra Group|67823|6|Mentioned|p365|||||||||
4293|Cocoparra Group|67847|5|Briefly described|p60 fig 3.3.4|||Lambie Basin. Of the authors' proposed Kanimblan cycle. ||||||
4293|Cocoparra Group|69160|5|Briefly described|Map legend|Late Devonian|Late Devonian||||Includes Barrat Formation, Hazeldene Sandstone and Edithvale Formation.||Undifferentiated quartz sandstone and pebbly sandstone.
|
4293|Cocoparra Group|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian||||Includes Barrat, Confreys, Jimberoo and Rankin Formations; Naradhan and Melbergen Sandstones.||Undifferentiated quartz sandstone and pebbly sandstone.|
4293|Cocoparra Group|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian||||Includes Barrat, Jimberoo and Rankin Formations; Naradhan and Melbergen Sandstones.||Undifferentiated quartz sandstone and pebbly sandstone.|
4293|Cocoparra Group|69164|5|Briefly described|Map legend|Late Devonian|Late Devonian||||Includes Swastika Siltstone and Barrat Formation.||Undifferentiated quartz sandstone and pebbly sandstone.|
4293|Cocoparra Group|69798|6|Mentioned|p6|||Part of the basement to Oaklands Basin.||||||
4293|Cocoparra Group|70751|5|Briefly described|p11, p29|Middle Devonian|Lower Devonian|Cargelligo 1:250k map sheet area. Potentially overlaps in time with the Winduck Group. Fossils are few and poorly preserved but indicate early to mid Devonian age. Fossils were deposited in a marine environment.||||Equivalent to the Mulga Downs Group.||
4293|Cocoparra Group|70777|6|Mentioned|p16|Late Devonian|Late Devonian|||||||
4293|Cocoparra Group|71039|6|Mentioned|p6-p7|Devonian|Silurian|||||||
4293|Cocoparra Group|71040|5|Briefly described|p15, p28, p31|Eifelian|Emsian|Griffith region. Age was previously assessed as Upper Devonian. Deformed in the Tabberabberan Orogeny. 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.|||Rankin Formation.||Conglomerate, sandstone.|
4293|Cocoparra Group|71364|5|Briefly described|p4, p7-8|||Hall (1955, 1958). ?Upper Devonian.|||Barrat Conglomerate (at base).||Conglomerate, sandstone, quartzite and shale.|15-FEB-18
4293|Cocoparra Group|71365|5|Briefly described|map legend|||Upper Devonian?|||Barrat Conglomerate.||Conglomerate, sandstone, quartzite, shale.|15-FEB-18
4293|Cocoparra Group|71693|5|Briefly described|Map legend; p2.|Devonian|Devonian||||||Quartz-rich and lesser lithic sandstone, pebbly sandstone, conglomerate, siltstone, grit; mainly fluvial sequence.|
4293|Cocoparra Group|71889|4|Described|p7-p8, p15, p17-p18|||Fossil fish fragments are recognised. Outcrops on the top of Galore Hill.Poorly exposed rocks occuring as low rises on the southern side of the Murrumbidgee River flood plain were mapped as undifferentiated Cocoparra Group by Wynn (1962a) and by Pogson (1974). Descriptions are provided for numerous locales. See also p47-p49, p53-p58, p60-p64, p67.|||Includes the Barrat Formation, Naradhan Sandstone, Confreys Formation, Bogolong Formation, Narrandera Sandstone, Melbergen Sandstone, Jimberoo Formation, Rankin Formation and Upper Cocoparra Group.|Overlies the Gillenbah Granite.|Medium-grained quartz rich sandstone,pebbly sandstone and conglomerate overlain by quartz sandstone and thin intercalated siltstone beds and lenses.|
4293|Cocoparra Group|72082|6|Mentioned|p3|Devonian|Devonian|||||||
4293|Cocoparra Group|72083|5|Briefly described|p7-9, p11, p24, p26, p32, p34 Fig.5|Early Devonian|Early Devonian|See also p35-36, p39-57. Extends N-S over c.150 km. Forms ranges in the SW of Ardlethan sheet area. Possible deformation events in the Early Devonian (e.g. Bindian Orogeny) discussed. Few fossils found.|||Barrat, Bogolong Formations; Narrandera Sandstone; Galore Hill Formation.|Overlies Gillenbah Granite and Wongajong conglomerate.||
4301|Coffs Harbour beds|38755|6|Mentioned|p63|||Geological Province: Coffs Harbour Block||||||
4301|Coffs Harbour beds|39673|6|Mentioned|p218|||||||||
4301|Coffs Harbour beds|40108|6|Mentioned|p183|||||||||
4301|Coffs Harbour beds|40514|4|Described|p6|||||||||
4301|Coffs Harbour beds|42901|5|Briefly described|Fig.11 P411|||||||||
4301|Coffs Harbour beds|43852|14|Not recorded|p197|||Ref.to Voisey 1934 (Proc.Linn.Soc.N.S.W.,59,333) Later called Fitzroy Series by Kenny 1936.||||||
4301|Coffs Harbour beds|60079|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of the "Coffs Harbour Association".  Includes: Coramba and Brooklana beds.||||||
4301|Coffs Harbour beds|71628|6|Mentioned|p3:55|||Associated with As (Au-Ag) mineralisation.||||||
4334|Colinton Volcanics|12185|5|Briefly described|map legend|Middle Silurian|Middle Silurian|Tuff, crystal tuff, dacite, shale, sandstone, limestone lenses. BMR map symbol: Smo.||||||
4334|Colinton Volcanics|22768|5|Briefly described|p176|||||||||
4334|Colinton Volcanics|22815|2|Defined|p40,41, fig10,16|Late Silurian|Late Silurian|Transitional over Cappanana Formation; conformably overlain by Rothlyn Formation.||||||16-FEB-05
4334|Colinton Volcanics|22857|4|Described|p176, p464 App. 1 Tb.A1.6|Late Silurian|Ludlovian|Of Bredbo Group. Correlates with Deakin and Laidlaw Volcanics. Includes part of former "Bransby Beds" (Richardson, 1979). Overlies Cappanana Fm. Max. thickness: 4km. Geol. Prov: Canberra-Yass Shelf and Monaro Forearc Basin. See also p468 App.1 Tb.A1.6.||||||
4334|Colinton Volcanics|23048|6|Mentioned|p2|||||||||
4334|Colinton Volcanics|24128|5|Briefly described|p3|||Geological Province: Lachlan Fold Belt.||||||
4334|Colinton Volcanics|24266|5|Briefly described|p1481|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt. Age: 418 Ma.||||||
4334|Colinton Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
4334|Colinton Volcanics|29994|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
4334|Colinton Volcanics|30332|6|Mentioned|p127|||Refers Packham(1969)||||||
4334|Colinton Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
4334|Colinton Volcanics|31111|6|Mentioned|p112|||Also mention P114, 116, 120, 124, 126, 130.||||||
4334|Colinton Volcanics|31284|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Upper Silurian M - U||||||23-APR-07
4334|Colinton Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
4334|Colinton Volcanics|32672|6|Mentioned|p672|||||||||
4334|Colinton Volcanics|32820|5|Briefly described|p5|||||||||
4334|Colinton Volcanics|33325|5|Briefly described|Table 2|||||||||
4334|Colinton Volcanics|33328|4|Described|Table 1|||p14.||||||08-FEB-18
4334|Colinton Volcanics|34405|6|Mentioned|p121|||||||||
4334|Colinton Volcanics|34406|6|Mentioned|p220|||Overlies Silurian sediments||||||
4334|Colinton Volcanics|36413|2|Defined|p38|Late Silurian|Late Silurian|||||||
4334|Colinton Volcanics|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Includes Tuggeranong Tuff Member. Rhyolitic to rhyodacitic crystal and lithic tuff, minor siltstone, sandstone, limestone. Underlies Bransby Beds; overlies Cappanana Formation; interfingers with Williamsdale Volcanics. GSNSW map code: Sv.||||||
4334|Colinton Volcanics|36633|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Late Silurian.||||||
4334|Colinton Volcanics|37251|5|Briefly described|p240|||||||||
4334|Colinton Volcanics|37727|4|Described|p47|||See also p18.||||||08-FEB-18
4334|Colinton Volcanics|37728|4|Described|Table 2|||||||||
4334|Colinton Volcanics|39331|6|Mentioned|Fig.5-11|||||||||
4334|Colinton Volcanics|40328|3|Fully described|p61|||||||||
4334|Colinton Volcanics|42497|5|Briefly described|Map legend|Pridolian|Ludlovian|||||||
4334|Colinton Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
4334|Colinton Volcanics|42727|5|Briefly described|map legend|Ludlow|Ludlow|Dark green dacitic ignimbrite and minor volcaniclastic sediments. Overlies Cappanana Formation. BMR map symbol: Svc. Geol. Prov: Canberra Block.||||||
4334|Colinton Volcanics|42820|2|Defined|Fig.16||early Ludlow|Age early Ludlow inferred.||||||
4334|Colinton Volcanics|43233|5|Briefly described|Map Legend||Late Silurian|of Bredbo Group||||||
4334|Colinton Volcanics|43472|14|Not recorded|p420-1,431-3,436|||fig.1||||||
4334|Colinton Volcanics|43473|14|Not recorded|fig.1,opp.p1080,1088||Early Silurian|p1090,1098 (M.Sil)||||||
4334|Colinton Volcanics|44093|5|Briefly described|p198 App. 1|Late Silurian|Late Silurian|Felsic volcanics. In the Canberra Block. Geological Province: Lachlan Fold Belt.||||||
4334|Colinton Volcanics|46574|5|Briefly described|Map Legend|||||||||
4334|Colinton Volcanics|49690|5|Briefly described|p1-2,p4-7, p9, p12-22, p27, p29, Tb.9-10|Late Silurian|Late Silurian|Defined by Richardson (1979) after Best et al. (1974). 16 sub-units. c.3000 m thick increasing northwards to ?8000 m. Correlates petrographically and chemically with the Deakin and Laidlaw Volcanics. K/Ar age 418+/-3, 413+/-3,. Rb/Sr age 411+/-5, 403+/-4|418+/- 3 Ma (K/Ar) max; 403 +/- 4 Ma (Rb/Sr) min.||Includes Williamsdale Dacite Member and Ingalara Ashstone Member.|Gradationally overlies Cappanana Formation. Overlain by the Rothlyn Formation.|Partly marine, partly terrestrial felsic volcanics ranging in composition from dacite (lower part) to rhyolite (upper part only) with minor interbedded sedimentary lenses in some places.|11-NOV-14
4334|Colinton Volcanics|61895|6|Mentioned|p134 Fig.1|||||||||24-SEP-14
4334|Colinton Volcanics|62070|5|Briefly described|p38|||||||Overlies the Cappanana Formation.|Felsic volcanics.|
4334|Colinton Volcanics|66197|5|Briefly described|p631 Fig.3c|||Canberra-Yass and Ngunawal Basins. Silicic volcanics. Overlies Cappanana Formation.||||||13-MAR-12
4334|Colinton Volcanics|68592|6|Mentioned|p428|||Equivalent to, but not yet formally included in, the Douro Group.||||||
4334|Colinton Volcanics|69635|4|Described|p18-24, 12, 14, 25, 43|Pridoli|Wenlock|Eastern Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation age on dacitic ignimbrite. Sample underlies Williamsdale Dacite Member.|425.1+/-3.2 Ma CV; 427.5+/-3.1 Ma WDM|Of Bredbo Group.|Includes Williamsdale Dacite Member.|Overlies Cappanana Formation. Overlain by Rothlyn Formation. Temporal equivalent to Kohinoor Volcanics, Woodlawn Volcanics.|Grey, crystal-rich dacite containing equant quartz and feldspar crystals, and rare lithic fragments up to 40 mm. Contains a fine flow-foliation and in places is sheared, giving a schistose appearance.|
4362|Colo Vale Sandstone|22857|5|Briefly described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Clifton Subgroup (Narrabeen Group). Quartz-lithic sandstone. Max. thickness: ~180m. Geological Province: Sydney Basin.||||||24-MAR-06
4362|Colo Vale Sandstone|22969|5|Briefly described|Appendix 3a p 1|||||||||
4362|Colo Vale Sandstone|31297|6|Mentioned|p6|||||||||
4362|Colo Vale Sandstone|36220|4|Described|p69|||See also P65 & Table 20.||||||
4362|Colo Vale Sandstone|36221|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
4362|Colo Vale Sandstone|42737|5|Briefly described|map legend|Triassic||||||||
4362|Colo Vale Sandstone|42896|4|Described|p27, Table 2|||of Clifton Subgroup||||||
4362|Colo Vale Sandstone|42925|6|Mentioned|p156|||||||||
4362|Colo Vale Sandstone|42948|6|Mentioned|p50|||||||||
4365|Colong Limestone|40398|6|Mentioned|p35|||||||||
4374|Colraine Mudstone|22612|6|Mentioned|423, 424 fig 2 tbl 1|Early Permian|Early Permian|Parent Manning Group. Max thickness 900 m. Also on pages 425-427, 429. Geol province New England Orogen||||||
4374|Colraine Mudstone|22857|5|Briefly described|p512 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Manning Group. Max. thickness: 495m. Geological Province: Barnard Basin. ||||||
4374|Colraine Mudstone|32944|6|Mentioned|p708|||Permian||||||
4374|Colraine Mudstone|32945|6|Mentioned|p88|||||||||
4374|Colraine Mudstone|34556|4|Described|p266|||Permian||||||
4374|Colraine Mudstone|38685|5|Briefly described|p27|||Geological Province: New England Fold Belt. Underlying Unit: Cedar Party Limestone||||||
4374|Colraine Mudstone|39262|6|Mentioned|p126|||||||||
4374|Colraine Mudstone|41347|6|Mentioned|p368|||||||||
4374|Colraine Mudstone|41348|5|Briefly described|Map legend|Permian|Permian|Of the Manning Group.||||||16-DEC-04
4374|Colraine Mudstone|43385|14|Not recorded|p179,180||Sakmarian|(Early Permian)||||||
4374|Colraine Mudstone|43755|6|Mentioned|Fig.2,p550||Permian|||||||
4375|Columba Granite|22678|6|Mentioned|p723|||||||||
4375|Columba Granite|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
4375|Columba Granite|30734|6|Mentioned|p36|||||||||
4375|Columba Granite|32999|4|Described|p38|||||||||
4375|Columba Granite|34481|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Early - Middle DevonianE - M||||||
4375|Columba Granite|40328|4|Described|p204|||||||||
4375|Columba Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
4375|Columba Granite|63633|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Bindook Porphyry Complex. Fine grained biotite granite, with gabbro outcrop.||||||
4375|Columba Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Pale pink to reddish fine- to medium-grained, equigranular to porphyritic, leucocratic granite with traces of biotite and muscovite, and micrographic quartz and K-feldspar. Locally vut by cataclasite veins.||||||
4375|Columba Granite|68592|2|Defined|p896, p901, p922, p1610-3, p1621-5|Early Devonian|Early Devonian|Mapped by Phipps (1950), but defined by Scheibner (1973) who suggested an association with Bindook Group. Placed in Oberon Supersuite by Phipps (1950) and Chappell et al.(1991); here it is assigned to the Arthursleigh Suite because of its shape, geochemistry and geophysical response. Near Wombeyan Caves. Type area described. Geochemistry detailed; geophysical properties described. Forms steep and dissected landscape; deep weathering causes poor exposure. Tenuous geochemical correlation with other Arthursleigh Suite granites is the basis for mid to late Early Devonian age.||Unit in Arthursleigh Suite.||Intrudes Wombeyan Limestone and metamorphosed it into marble; intrudes Mares Forest Volcanics.|Uniform internal composition. Pink to red, leucocratic, variable grainsize: porphyritic in the centre of the main pluton, coarse-grained equigranular granite in the eastern part, scattered microgranite throughout. Likely I-type.|
4375|Columba Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dao. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. [Note: shown erroneously as 'Dao' Corridgery Granite on Taralga 1:100 000 sheet]||Arthursleigh Suite|||Reddish, leucocratic, fine/coarse-grained, equigranular to porphyritic granite; micrographic quartz and K-feldspar intergrowths; v.minor biotite and muscovite; locally cut by cataclasite veins. High radioelement response; low magnetic susceptibility|
4375|Columba Granite|70661|6|Mentioned|p75, p76|||||||Intrudes Wombeyan Limestone, Mares Forest Volcanics.||
4387|Comboyne Basalt|29990|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4387|Comboyne Basalt|32671|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4387|Comboyne Basalt|32719|6|Mentioned|p207|||Geological map.||||||
4387|Comboyne Basalt|40876|6|Mentioned|p128|||||||||
4387|Comboyne Basalt|41348|5|Briefly described|Map legend|Tertiary||||||||16-DEC-04
4387|Comboyne Basalt|60281|5|Briefly described|Fig. 8 Appendix 1|Tertiary|Tertiary|Geological Province: Lorne Basin.||||||
4387|Comboyne Basalt|61155|5|Briefly described|p19|Middle Miocene|Middle Miocene|Of the Comboyne Province Volcanics.  In the Kempsey area.||||||03-MAR-10
4387|Comboyne Basalt|73581|5|Briefly described|p8|||Of the Comboyne volcano.|||||Wide compositional range from trachybasalt and trachyandesite to trachyte.|
4403|Compton Downs Granite|23171|6|Mentioned|p13||Early Devonian|||||||
4403|Compton Downs Granite|34449|6|Mentioned|Table 2-1|||||||||
4403|Compton Downs Granite|68823|5|Briefly described|p394|Lochkovian|Lochkovian|Within the Louth-Eumarra Shear Zone. Inferred magmatic SHRIMP zircon age.|416.4 +/- 2.53 Ma, SHRIMP zircon|||||
4403|Compton Downs Granite|69002|6|Mentioned|p12|Early Devonian|Early Devonian||~416 Ma|Of the Tarcoon plutonic complex (informal name).||||28-NOV-13
4403|Compton Downs Granite|69635|5|Briefly described|p127, 131, 134, 136|Early Devonian|Early Devonian|I-type.|416.4+/-2.5 Ma, Black, 2006|Of Tarcoon Suite. ||Similar magnetic signature, I-type geochemistry and proximal to Bobelah Granite.||
4403|Compton Downs Granite|70210|5|Briefly described|p1, p10-11, p38, p40-41|Early Devonian|Late Silurian|Cobar-Bourke district.|416.4 +/- 2.5 Ma.|||||
4403|Compton Downs Granite|70602|5|Briefly described|p65-67,72,74|Early Devonian|Late Silurian|Aeromagnetic map data given.|416.4+/-2.5Ma|Tarcoon Plutonic Complex||Intrudes Girilambone Group.|I-type granite.|
4403|Compton Downs Granite|71345|2|Defined|p4,6-7,9|Early Devonian|Early Devonian|Type location: Lat -30.4204 Long 146.5737; GR459059 6634556. Described by Brunker (1968). Named after Compton Downs railway station (GR459020 6634400). Referred to informally as Compton Downs granite by Black (2006), Hegarty (2011) and Blevin (2011). Officially defined herein after Blevin (2011). Forms prominent granite tors to 2m high, boulders and low flat outcrops along the Byrock-Tarcoon road. Generally massive nature of the granite and the presence of amphibole distinguish the granite from surrounding metasedimentary rocks. Distinct ellipsoid magnetic signature, and a radiometric high on the SE side. Approximately 6km long trending NE-SW, and 3km wide trending NW-SE, based on radiometric and magnetic data. Described by Blevin (2011) as 'weakly to moderately oxidised, unfractionated I-type with a SiO2 range of 61 to 72 wt%, and is 'high-K, calc-alkaline'. Ages: SHRIMP U-Pb age of 416.4+\-2.5 Ma (Black 2006); K-Ar date from biotite in granite of 403+\-13 Ma (Richards and McDougall, in Jones 1986). Geochemically, petrologically and in age similar to the Bobelah Granite (~10km to the NW; Blevin 2011), suggesting they are separate plutons from the same magmatic reservoir. Blevin (2011) interpreted modest Au-Bi and Au-W prospectivity associated with the granite.|416.4+\-2.5 Ma (SHIRMP U-Pb; magmatic)|Unit of Tarcoon Suite.|||Granodiorite with 'euhedral amphibole often with felted cores after pyroxene, with biotite in subequal amounts, and apatite, zircon, allanite and opaques' (Blevin 2011).|02-DEC-19
4403|Compton Downs Granite|71360|5|Briefly described|Map legend|Early Devonian|Early Devonian|Geophysical signature: lobate area of moderate magnetic intensity showing concentric banding patterns.|416.4 +/- 2.5 Ma.|Tarcoon Plutonic Complex.|||Granodiorite, with local pegmatite and alteration.|
4403|Compton Downs Granite|72522|5|Briefly described|p1, p10, p13, p16, p29, p133.|Cambrian|Cambrian|Magmatic age by Black, 2006.|416.4 +/- 2.5 Ma|Tarcoon Suite|||Includes granite.|
4414|Condadilly Formation|30135|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
4414|Condadilly Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
4414|Condadilly Formation|31882|5|Briefly described|p245|||||||||
4414|Condadilly Formation|32482|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
4414|Condadilly Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
4414|Condadilly Formation|32944|6|Mentioned|p700|||See also P702 & Fig.3. Permian||||||
4414|Condadilly Formation|34043|5|Briefly described|p449|||||||||
4414|Condadilly Formation|36940|6|Mentioned|p142|||||||||
4414|Condadilly Formation|37094|6|Mentioned|p240|||||||||
4414|Condadilly Formation|39572|6|Mentioned|p141|||||||||
4414|Condadilly Formation|41264|6|Mentioned|p251|||Recently Leard Formation||||||
4414|Condadilly Formation|43407|14|Not recorded|Map Legend||Late Permian|(Provisional Edition)||||||
4414|Condadilly Formation|43408|14|Not recorded|Map Legend|||To 120ft thick, Curlewis sheet||||||
4414|Condadilly Formation|43409|2|Defined|Map Legend|||Permian shale & thin sstn bands with Glossopteris. Overlies Gunnible Formation||||||
4417|Condamine beds|22601|6|Mentioned|405|Permian|Permian|||||||
4417|Condamine beds|39071|6|Mentioned|p353|||||||||
4417|Condamine beds|43008|5|Briefly described|map legend|||||||||
4417|Condamine beds|63731|5|Briefly described|Map legend|Late Permian|Late Permian|Dark grey to black, slightly calcareous mudstone, with beds of coarse-grained pebbly arenite and conglomerate; some epiclastic sediments and rhyolitic crystal-lithic tuff beds; locally richly fossiliferous.||||||
4417|Condamine beds|63748|4|Described|p20, p21, p50|Late Permian|Late Permian|Faulted against Silverwood Group rocks; unconformably overlain by Marburg Subgroup sediments. Divided into 4 sequences (Olgers et al 1974) of arenites and mudstones, both fossiliferous and unfossiliferous. Geological province: Wandsworth Province.||||||07-FEB-11
4417|Condamine beds|68679|5|Briefly described|p446, p453|Permian|Permian|Silver Spur Subprovince, Woolomin Province. Occurs 20km SE of Warwick as a 10 km2 outlier. Olgers et al. (1974) identified four subunits in the type area, each ~300m thick, briefly described in LITHOLOGY (DESCRIPTION). Abundant marine fauna includes the most diverse crinoid fauna in the State. Late Permian.||||Is faulted against the Silverwood Group. Is overlain unconformably by the Marburg Subgroup.|Mudstones, sandstones, conglomerate, rhyolitic crystal-lithic tuff.|
4417|Condamine beds|71628|5|Briefly described|p16:4|Permian|Permian|||||Is intruded by Cullendore Syenogranite.||
4423|Condong Gabbro|42726|5|Briefly described|map legend|||||||||
4424|Condor Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Hornblende-biotite granite. BMR map symbol: ghh.||||||
4424|Condor Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
4424|Condor Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
4424|Condor Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
4424|Condor Granite|33325|5|Briefly described|p18|||Late Sil. - early Dev.||||||
4424|Condor Granite|40328|4|Described|p204|||||||||
4424|Condor Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
4424|Condor Granite|43159|6|Mentioned|p10||Silurian|||||||
4433|Conger Formation|22857|4|Described|p512 App.1 Tb.A1.8|Visean|Visean|Grey to brown, fine- to coarse-grained lithic arenite beds up to 6m thick; interbedded lenticular boulder conglomerate, mudstone and thin andesitic to rhyodacitic ignimbrites. Overlies Wootton beds. Max. thickness: 400m. ||||||
4433|Conger Formation|24118|5|Briefly described|p4|Carboniferous|Carboniferous|||||||
4433|Conger Formation|24121|5|Briefly described|p4, p249|||||||||25-AUG-22
4433|Conger Formation|29990|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4433|Conger Formation|30074|6|Mentioned|p24|||||||||
4433|Conger Formation|32324|6|Mentioned|Table 8.1|||||||||
4433|Conger Formation|32379|6|Mentioned|p5|||||||||
4433|Conger Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4433|Conger Formation|32869|5|Briefly described|p171|||Depositional environment. Equiv. Wallaringa Fm.||||||
4433|Conger Formation|34059|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4433|Conger Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
4433|Conger Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
4433|Conger Formation|34168|5|Briefly described|p254|||Carboniferous||||||
4433|Conger Formation|34238|6|Mentioned|Table 1|||||||||
4433|Conger Formation|36057|6|Mentioned|p352|||||||||
4433|Conger Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
4433|Conger Formation|37068|5|Briefly described|p59|||||||||
4433|Conger Formation|39302|5|Briefly described|p345|||See also Fig. 17.1||||||
4433|Conger Formation|39979|6|Mentioned|p42|||||||||
4433|Conger Formation|40883|6|Mentioned|p7|||Mention Fig.2||||||
4433|Conger Formation|42547|4|Described|p34|||||||||
4433|Conger Formation|43432|14|Not recorded|p208|||Part of Myall Facies||||||
4433|Conger Formation|43447|4|Described|Table 1&2,p10,13||Carboniferous|||||||
4433|Conger Formation|43451|14|Not recorded|Map Legend||Carboniferous|||||||
4433|Conger Formation|43479|14|Not recorded|p161,177||Visean|||||||
4433|Conger Formation|44093|5|Briefly described|p230 App. 1|Late Devonian|Late Devonian|Geological Province: New England Fold Belt.||||||
4433|Conger Formation|44244|2|Defined|p131|Visean|Visean|Formerly the "Carsonville Formation" of Peou and Engel (1979).  Overlies the Wootton beds; underlies Nerong Volcanics, Berrico Creek Formation.  Max. thickness: 1070m.||||||
4433|Conger Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
4433|Conger Formation|50147|5|Briefly described|Map legend|Visean|Visean|Sandstone, conglomerate and minor mudstone, carbonaceous shale, interbedded dacite.||||||
4433|Conger Formation|50263|5|Briefly described|Map Legend|Visean|Visean|Overlies: Wootton Beds.  Underlies: Nerong Volcanics.  Geological Province: Western Myall Block.||||||17-MAY-04
4433|Conger Formation|63832|6|Mentioned|p131 fig 2|Carboniferous|Carboniferous|Western Myall block, Southern New England Fold Belt.||||||
4433|Conger Formation|64631|6|Mentioned|p44 Fig.2.|Visean|Tournaisian|Southern New England Fold Belt, western Myall Block. Some biostratigraphic and radiometric age control.||||||
4433|Conger Formation|69323|5|Briefly described|p62|||Geological province: New England Orogen.Marine to continental sedimentary rocks.||||Overlain conformably by Nerong Volcanics.||
4433|Conger Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Myall Block, Tamworth Belt.||||||
4433|Conger Formation|70028|6|Mentioned|p79|Miocene|Oligocene|Offshore Gippsland Basin.||||||
4433|Conger Formation|70076|5|Briefly described|South-Eastern: Fig.2; Regional: Fig.3|Miocene|Miocene|||Angler Subgroup.||Overlies Swordfish Formation. Is overlain by Cod Formation.||
4433|Conger Formation|73487|6|Mentioned|p566, p568 Fig.3, p574, p581|Visean|Visean|Western Myall Block. Abbreviated as Conger p566.||||||
4444|Conjola Subgroup|22591|5|Briefly described|Fig 1||Early Permian|||||||
4444|Conjola Subgroup|22969|5|Briefly described|p 6||Early Permian|||||||
4444|Conjola Subgroup|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
4444|Conjola Subgroup|23544|5|Briefly described|Fig 2 p358|||Of the Shoalhaven Group in the Sydney Basin.||||||12-MAR-09
4444|Conjola Subgroup|35145|6|Mentioned|Fig.2|||||||||
4444|Conjola Subgroup|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
4444|Conjola Subgroup|35862|6|Mentioned|p277|||||||||
4444|Conjola Subgroup|36207|6|Mentioned|Text Fig.2|||||||||
4444|Conjola Subgroup|36600|6|Mentioned|p109|||||||||
4444|Conjola Subgroup|37092|6|Mentioned|Table 2|||||||||
4444|Conjola Subgroup|39316|6|Mentioned|p328|||[Originally entered for WA. CEBMar95]||||||
4444|Conjola Subgroup|42848|5|Briefly described|Fig.2 P530|Permian|Permian|Of Shoalhaven Group. Overlies the Bellbird Creek Formation (Merrimbula Group).||||||09-MAY-05
4444|Conjola Subgroup|42850|5|Briefly described|p546|Permian|Permian|Quartz sandstone and conglomerate.||||||09-MAY-05
4444|Conjola Subgroup|42925|5|Briefly described|Table 18||Early Permian|||||||
4444|Conjola Subgroup|43194|5|Briefly described|p129 Tb. 8.3|Early Permian|Early Permian|Abbreviated to Conjola Subgp in text. Of Shoalhaven Group, southern Sydney Basin. Contains Wasp Head Formation, Clyde Coal Measures, Pebbley Beach Formation, Snapper Point Formation.||||||
4444|Conjola Subgroup|61315|5|Briefly described|Table SY2|Early Permian|Early Permian|Of the Shoalhaven Group. Includes: Wasp Head and Pebbley Beach Formations, Clyde Coal Measures, Snapper Point Formation. Geological Province: Sydney Basin.||||||12-MAR-09
4444|Conjola Subgroup|61609|5|Briefly described|p240 Tb. 1|Permian|Permian|Of Shoalhaven Group. Includes Snapper Point, Pebbley Beach and Wasp Head Formations. Geological Province: Sydney Basin.||||||07-FEB-11
4444|Conjola Subgroup|73494|5|Briefly described|p541|Permian|Permian|Southern Sydney Basin. Early Permian.||Basal Shoalhaven Group.|Pebbley Beach, Snapper Point Formations.|Overlies Talaterang Group.|Transgressive nearshore and terrestrial sediments.|
4452|Connolly Volcanics|22601|6|Mentioned|416|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
4452|Connolly Volcanics|31400|5|Briefly described|p165|||Mineralization discussed.||||||07-SEP-18
4452|Connolly Volcanics|32491|5|Briefly described|p7|||Sil.?-L.Devonian||||||
4452|Connolly Volcanics|32492|6|Mentioned|Map legend|Early Devonian|Silurian|Silurian? - Lower Devonian. Of Silverwood Group.||||||25-OCT-05
4452|Connolly Volcanics|32672|6|Mentioned|p673|||||||||
4452|Connolly Volcanics|33146|5|Briefly described|p2|||See also p3. ?Sil.-L.Dev.||||||07-SEP-18
4452|Connolly Volcanics|33326|6|Mentioned|p446|||Fauna.||||||
4452|Connolly Volcanics|33703|6|Mentioned|p207|||||||||
4452|Connolly Volcanics|35008|6|Mentioned|p175|||||||||
4452|Connolly Volcanics|35311|6|Mentioned|p207|||||||||
4452|Connolly Volcanics|35424|5|Briefly described|p8|||||||||
4452|Connolly Volcanics|35652|4|Described|p6|||||||||
4452|Connolly Volcanics|37252|6|Mentioned|Map legend|Devonian|Devonian|||||||
4452|Connolly Volcanics|39071|6|Mentioned|p345|||||||||
4452|Connolly Volcanics|39445|5|Briefly described|Table 5|||||||||
4452|Connolly Volcanics|42031|5|Briefly described|Fig.3 P759|||||||||
4452|Connolly Volcanics|48940|3|Fully described|p21|||||||||
4452|Connolly Volcanics|61392|4|Described|p163-165, p166|Emsian|Pridoli|Of Silverwood Group. Comprises lower extrusive lava flows, interbedded with sediments; upper unit deposited on a normal clastic or sand/mud-rich slope apron with sediments richer in primary volcaniclastic debris. Age: 422-389Ma. Max. thick: 2430m.||||||02-APR-13
4452|Connolly Volcanics|63731|5|Briefly described|Map legend|Devonian|Silurian|Of the Silverwood Group. Basaltic to locally dacitic volcaniclastic deposits, incl. volcanic breccia and crystal tuff, tog. with some flows; turbiditic volcaniclastic sediments; minor conglomerate lenses and limestone lenses; mod.-high magnetic response.||||||
4452|Connolly Volcanics|63748|4|Described|p6, p7 Fig. 3|Early Devonian|Middle Silurian|Of Silverwood Group. Conformable on Risdon Stud Formation; overlain by Bald Hill Formation. Max. thickness: ~2430m. In the Silverwood Province. Lower pyroclastics and lavas and upper thin bedded turbidites woth scattered coarse conglomeratic horizons||||||07-SEP-18
4452|Connolly Volcanics|68679|5|Briefly described|p445-446, p452-453|Early Devonian|Late Silurian|Olgers et al. (1974). Silverwood Province. 2430m thick. Lacks direct evidence of age. Some areas mapped as this unit were re-assigned to the Eight Mile Creek beds by Van Noord (1999).||Silverwood Group.||Overlies Risdon Stud Formation. Is overlain unconformably by Bald Hill Formation and Fitz Creek beds (or is faulted against the latter).|A lower succession of submarine volcaniclastics and lavas and associated intrusive dolerites: low-K tholeiitic basalt; overlain by mainly thin-bedded turbidites with scattered coarse conglomerate and limestone lenses, rich in volcaniclastic debris.|
4452|Connolly Volcanics|71628|5|Briefly described|p16:4|||||Silverwood Group.||Is intruded by Cullendore Syenogranite.||
4471|Coocoran Claystone Member|22857|5|Briefly described|p544 App.1 Tb.A1.12|Albian|Albian|Of the Griman Creek Formation (Rolling Downs Group). Fine-grained pale kaolinitic claystone, often silicified to porcelanite. Max. thickness: 36m. Geological Province: Surat Basin.||||||
4471|Coocoran Claystone Member|42346|5|Briefly described|p83|||||||||
4471|Coocoran Claystone Member|68069|5|Briefly described|p2.|Early Cretaceous|Early Cretaceous|||Upper unit in Griman Creek Formation.||Overlies Wallangulla Sandstone Member.|White to cream claystone, commonly silicified to porcellanite.|
4471|Coocoran Claystone Member|68593|5|Briefly described|p5|||Byrnes (1977). 0-3.6m thick.||Griman Creek Formation.||Overlies Wallangulla Sandstone Member.|Fine-grained, pale, kaolinitic claystone; often silicified to porcellanite ('shincracker'); thin sandy and clayey laminae.|
4489|Cooinbil Limestone|40328|6|Mentioned|p7|Llandovery|Llandovery|||||||08-FEB-18
4495|Cookamidgera Subgroup|22638|4|Described|p72|||Of the Hervey Group.||||||24-AUG-04
4495|Cookamidgera Subgroup|22831|6|Mentioned|Table 24|||||||||
4495|Cookamidgera Subgroup|22859|6|Mentioned|p213|||||||||
4495|Cookamidgera Subgroup|23214|6|Mentioned|p226|||Of Hervey Group. Name discontinued. Geological Province: Hervey Basin. See Cookamidgera Formation.||||||
4495|Cookamidgera Subgroup|24417|3|Fully described|p149|Late Devonian|Late Devonian|Max. thickness: 500m.||||||
4495|Cookamidgera Subgroup|30071|6|Mentioned|Fig.1|||||||||
4495|Cookamidgera Subgroup|43441|5|Briefly described|31||Late Devonian|||||||08-JAN-10
4495|Cookamidgera Subgroup|43461|14|Not recorded|Table p625|Carboniferous|Late Devonian|||||||
4495|Cookamidgera Subgroup|43507|2|Defined|p123-130,160-63,166||Late Devonian|Includes Burrill(top), Eurow, Koorawatha and Belvedere(base) Formations (Hervey Group)||||||
4495|Cookamidgera Subgroup|43510|14|Not recorded|p37,41-2,45-7,49,52,|||Constituent formations defined.  p58,60-1,63,65-6,68-71,73-4,77-9||||||
4495|Cookamidgera Subgroup|44192|5|Briefly described|Map Legend|||||||||
4495|Cookamidgera Subgroup|50231|5|Briefly described|Map Legend|Famennian|Famennian|Of the Hervey Group.  Includes Koorawatha Formation.  Overlies Nangar Subgroup.||||||25-JUN-08
4495|Cookamidgera Subgroup|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hervey Group - undifferentiated sandstone, siltstone, shale.||||||09-JUN-04
4495|Cookamidgera Subgroup|60009|5|Briefly described|Map Legend|Famennian|Famennian|Of the Hervey Group. Overlies Weddin Sandstone, Cudgelbar Sandstone Member.||||||25-JUN-08
4495|Cookamidgera Subgroup|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Hervey Group. Contains the Koorawatha Formation.||||||
4495|Cookamidgera Subgroup|68298|5|Briefly described|p216||Late Devonian|Of Connolly (1965), central and western NSW sediments.||Hervey Group||Overlies Nangar Subgroup.||
4495|Cookamidgera Subgroup|68592|6|Mentioned|p1698|||Conolly (1965). Obsolete due to problems in correlation.||Unit in Hervey Group.||||
4499|Cookman Formation|22472|4|Described|p37|Early Devonian|Early Devonian|Of the Crudine Group.||||||28-AUG-08
4499|Cookman Formation|22529|5|Briefly described|4 fig 2, 8|Lochkovian|Lochkovian|Geol province Hill End Trough. Overlying unit Turondale Formation, underlying unit Chesleigh Group.||||||28-AUG-08
4499|Cookman Formation|22590|6|Mentioned|P750|||||||||
4499|Cookman Formation|22768|6|Mentioned|p180|||||||||
4499|Cookman Formation|22857|4|Described|p180, p470 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Crudine Group. Sequence of quartz-rich greywackes with conglomerate interbeds. Max. thickness: 700m. Geological Province: Hill End Trough and Capertee Rise. See also p470 App.1 Tb.A1.6.||||||
4499|Cookman Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of Crudine Group.||||||28-AUG-08
4499|Cookman Formation|23170|2|Defined|p156|Lochkovian|Lochkovian|Of Crudine Group.||||||28-AUG-08
4499|Cookman Formation|23214|3|Fully described|p188|Lochkovian|Lochkovian|Basal unit of Crudine Group.  Interbedded cream to dark grey fine to medium grained quartz rich sandstone, siltstone, laminated shale and minor dark to black cherty tuff. Max. thickness 650m.||||||
4499|Cookman Formation|23738|4|Described|p251|Devonian|Devonian|||||||
4499|Cookman Formation|24126|6|Mentioned|p234|||||||||24-JAN-05
4499|Cookman Formation|24278|6|Mentioned|p1765 Fig. 1|||||||||
4499|Cookman Formation|24394|5|Briefly described|p170|Lochkovian|Lochkovian|||||||
4499|Cookman Formation|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
4499|Cookman Formation|30099|6|Mentioned|Fig.2|||||||||
4499|Cookman Formation|31852|6|Mentioned|Fig. 5|||Ludlovian to Pridolian||||||
4499|Cookman Formation|32045|6|Mentioned|Map legend|Silurian|Ordovician|Siluro-Ordovician||||||
4499|Cookman Formation|32046|6|Mentioned|p250|||See also p251,262||||||
4499|Cookman Formation|32047|6|Mentioned|p2|||||||||
4499|Cookman Formation|32485|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
4499|Cookman Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
4499|Cookman Formation|32672|6|Mentioned|p672|||||||||
4499|Cookman Formation|33006|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
4499|Cookman Formation|33282|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
4499|Cookman Formation|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
4499|Cookman Formation|34403|6|Mentioned|p131|||Equivalent. See also P134.||||||
4499|Cookman Formation|34404|6|Mentioned|Fig.3.5b|||Upper Silurian||||||
4499|Cookman Formation|34405|4|Described|p107|||Silurian||||||
4499|Cookman Formation|34406|6|Mentioned|p221|||||||||
4499|Cookman Formation|34572|6|Mentioned|p89|||See also PP90,98. Silurian||||||
4499|Cookman Formation|35318|5|Briefly described|p467|||||||||
4499|Cookman Formation|35877|6|Mentioned|p126|||||||||
4499|Cookman Formation|36390|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Late Silurian||||||
4499|Cookman Formation|37727|4|Described|p47|||See also P33.||||||
4499|Cookman Formation|37746|6|Mentioned|Notes|||||||||
4499|Cookman Formation|38216|5|Briefly described|p253|||||||||
4499|Cookman Formation|39331|6|Mentioned|Fig.7-1|||||||||
4499|Cookman Formation|40107|6|Mentioned|p259|||||||||
4499|Cookman Formation|40328|3|Fully described|p172|||||||||
4499|Cookman Formation|43127|4|Described|p4,Fig.2,Fig.3||Early Devonian|||||||
4499|Cookman Formation|43263|6|Mentioned|Map Legend|Late Silurian||Age Middle-Late Silurian.||||||
4499|Cookman Formation|43344|14|Not recorded|p139,149,150,152,153||Silurian|p156||||||
4499|Cookman Formation|43384|14|Not recorded|Map Legend||Silurian|||||||
4499|Cookman Formation|43461|14|Not recorded|table p621||Ludlovian|||||||
4499|Cookman Formation|43476|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
4499|Cookman Formation|43494|4|Described|p25-26|Devonian|Devonian|Lowermost unit of the Crudine Group.  Consists mainly of hard resistant quartz sandstone with minor siltstone and a few thin lenses of coarse feldspathic sandstone. Conformable over Chesleigh Fm. Max. thickness: 800m.||||||28-AUG-08
4499|Cookman Formation|43515|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
4499|Cookman Formation|43516|14|Not recorded|Map Legend||Late Silurian|||||||
4499|Cookman Formation|43517|2|Defined|p112,119-122,131-163|||O/lies Chesleigh Fm.Type section along Turon Riv.  Map Plate XII||||||
4499|Cookman Formation|43525|14|Not recorded|Table p127||Ludlovian|||||||
4499|Cookman Formation|43639|5|Briefly described|Map Legend||Devonian|||||||
4499|Cookman Formation|43641|5|Briefly described|Map Legend||Devonian|||||||
4499|Cookman Formation|43653|5|Briefly described|Map Legend||Devonian|||||||
4499|Cookman Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of Crudine Group.||||||28-AUG-08
4499|Cookman Formation|44093|5|Briefly described|p50|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||02-MAR-05
4499|Cookman Formation|64296|5|Briefly described|p84 Tb. 1|||||||||
4499|Cookman Formation|68592|6|Mentioned|p624|||||||Correlated with Campbells Group.||
4499|Cookman Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
4499|Cookman Formation|71924|6|Mentioned|p2, 3|||Hill End Trough? No significant fauna known. Unlikely to correlate with basal Mullamuddy {Formation].||||||
4499|Cookman Formation|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4|Early Devonian|Late Silurian|Hill End Trough. Locations in text include p1102 Fig.8. [Map symbol suggests Devonian age]||||Overlies the Piambong Formation, underlies the Turondale Formation.||
4506|Coolac Serpentinite|22687|5|Briefly described|110,119|||Geol province Lachlan Fold Belt||||||
4506|Coolac Serpentinite|22768|5|Briefly described|p155,184|||||||||
4506|Coolac Serpentinite|22857|5|Briefly described|p155,,p184, p450 App.1, Tb.A1.6|||Schistose and massive serpentinite. Minor chromitite. Interpreted by Stuart-Smith (1989, 1990a,b) as being most likely a high-emplaced Cambrian upper mantle complex (basement of Jindalee Gp). Age: 392+/-14-409+/-11Ma (U/Pb SHRIMP). Geol Prov: Tumut Trough||||||
4506|Coolac Serpentinite|29450|6|Mentioned|p53|||||||||
4506|Coolac Serpentinite|29453|6|Mentioned|p25|||||||||
4506|Coolac Serpentinite|29454|4|Described|p11|||L-M Devonian||||||
4506|Coolac Serpentinite|29648|6|Mentioned|p18|||||||||
4506|Coolac Serpentinite|29682|4|Described|p11|||||||||
4506|Coolac Serpentinite|29902|6|Mentioned|p4|||||||||
4506|Coolac Serpentinite|30172|6|Mentioned|p43|||||||||
4506|Coolac Serpentinite|30662|6|Mentioned|p189|||Refers to Ashley et al.(1969).||||||
4506|Coolac Serpentinite|30663|6|Mentioned|p25|||||||||
4506|Coolac Serpentinite|31279|6|Mentioned|p215|||||||||
4506|Coolac Serpentinite|31448|5|Briefly described|p19|||||||||
4506|Coolac Serpentinite|31928|6|Mentioned|p69|||Refers Ashley et al. (1971) Golding (1969)||||||
4506|Coolac Serpentinite|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
4506|Coolac Serpentinite|33004|6|Mentioned|p175|||||||||
4506|Coolac Serpentinite|33480|6|Mentioned|p243|||Age dating||||||
4506|Coolac Serpentinite|35070|2|Defined|p29|Early Silurian|Early Silurian|Prob.Early Silurian||||||
4506|Coolac Serpentinite|35185|6|Mentioned|p238|||||||||
4506|Coolac Serpentinite|35194|6|Mentioned|p67|||||||||
4506|Coolac Serpentinite|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
4506|Coolac Serpentinite|35607|6|Mentioned|p161|||See also P162,163.||||||
4506|Coolac Serpentinite|35608|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
4506|Coolac Serpentinite|35609|5|Briefly described|p15|||||||||
4506|Coolac Serpentinite|36411|6|Mentioned|p268|||Refers Basden et al 1978 for definition.||||||
4506|Coolac Serpentinite|37529|5|Briefly described|p7|||See also P5||||||
4506|Coolac Serpentinite|37727|6|Mentioned|p63|||||||||
4506|Coolac Serpentinite|39319|6|Mentioned|p357|||||||||
4506|Coolac Serpentinite|39331|6|Mentioned|Fig.4-3|||||||||
4506|Coolac Serpentinite|40328|4|Described|p38|||||||||
4506|Coolac Serpentinite|40497|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
4506|Coolac Serpentinite|40498|6|Mentioned|p378|||||||||
4506|Coolac Serpentinite|40762|6|Mentioned|p279|||||||||
4506|Coolac Serpentinite|42045|6|Mentioned|p148|||||||||
4506|Coolac Serpentinite|42145|4|Described|Table 1 P624|||||||||
4506|Coolac Serpentinite|42313|1|Redefined|p71|Late Silurian|Middle Silurian|Age: early Middle Silurian to Late Silurian||||||
4506|Coolac Serpentinite|42314|5|Briefly described|Map|Middle Silurian||||||||
4506|Coolac Serpentinite|42322|6|Mentioned|p2|||||||||
4506|Coolac Serpentinite|42497|5|Briefly described|Map Legend|Wenlockian|Bolindian|||||||
4506|Coolac Serpentinite|42828|5|Briefly described|Table 1 P129|Late Silurian|Middle Silurian|||||||
4506|Coolac Serpentinite|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sc1||||||
4506|Coolac Serpentinite|44093|6|Mentioned|p94 (photo)|||Schistose rocks. Geological Province: Tasman Fold Belt.||||||
4506|Coolac Serpentinite|44192|5|Briefly described|Map Legend||Llandoverian|||||||
4506|Coolac Serpentinite|44936|5|Briefly described|Map Legend||Silurian|||||||
4506|Coolac Serpentinite|46967|6|Mentioned|p289|||||||||
4506|Coolac Serpentinite|50191|6|Mentioned|p6, 21 Fig. 1|Silurian|Early Silurian|Intruded by the Young Granodiorite.||||||02-AUG-04
4506|Coolac Serpentinite|60078|6|Mentioned|Map Legend|Late Silurian|Early Silurian|||||||
4506|Coolac Serpentinite|60423|5|Briefly described|p371 Fig. 2|Early Devonian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||17-JAN-17
4506|Coolac Serpentinite|68822|6|Mentioned|p335|||Partial ophiolite.||||||
4506|Coolac Serpentinite|69043|6|Mentioned|p63||||||||Harzburgite and serpentinite.|
4506|Coolac Serpentinite|71708|4|Described|p335-338,340,342-344,347-352|Early Ordovician||3km wide by 60km long linear belt of ultramafic rocks. Lithological description is restricted for use to this paper only. Min. age 426.8+/-2.2 from intrusive North Mooney Complex, and  483.5+/-2.3 Ma from a granite dyke intruding the related Wambidgee Serpentinite. Convoluted history involving multi stage melt rock interactions makes  direct dating impossible. See also Coolac Serpentinite belt and Coolac Ophiolite Suite. Interpreted to have belonged to a larger ultramafic massif called the Tumut Serpentinite Province by Graham (2000).||||In fault contact with Blowering Formation, Honeysuckle beds. Intruded by North Mooney Complex. Genetically related to the Wambidgee Serpentinite.|Ultramafic rocks comprising partially to completely serpentinised hazburgite, minor dunite and podiform chromitite. Also includes intrusions of wehrlites, pyroxenites, gabbros, basalts and various granitoids.|31-MAR-20
4506|Coolac Serpentinite|73483|6|Mentioned|p406, p407, p414|||Lachlan Orogen. Also referred to as Coolac Serpentinite Belt p406-9, p413-416, inferred Cambro-Ordovician age, contains crustally derived zircons.||||||
4526|Cooleman Mountains Granodiorite|39409|6|Mentioned|Table XVII|||||||||
4528|Cooleman Plains Group|22857|5|Briefly described|p466 App.1 Tb.A1.6|Silurian|Silurian|||||||
4528|Cooleman Plains Group|23309|6|Mentioned|p390|||||||||
4528|Cooleman Plains Group|36441|5|Briefly described|map legend|Late Silurian|Late Silurian|Includes Peppercorn Formation, Blue Waterhole Formation and Micalong Creek Beds.||||||
4528|Cooleman Plains Group|36443|5|Briefly described|map legend|Early Devonian|Llandoverian|Includes Blue Waterhole Formation, Cooleman Limestone, Peppercorn Formation and Pocket Formation.||||||
4528|Cooleman Plains Group|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Ssc||||||
4528|Cooleman Plains Group|44093|5|Briefly described|p189 App. 1|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||03-MAR-05
4528|Cooleman Plains Group|45147|3|Fully described|M76|||See also M137||||||
4528|Cooleman Plains Group|60078|6|Mentioned|Map Legend|Late Silurian|Late Silurian|||||||
4528|Cooleman Plains Group|71040|5|Briefly described|p9, p11|Late Silurian|Late Silurian|Affected by the Bindian (=Bowning) Orogeny.||||Is overlain unconformably by Kellys Plains Volcanics and Mountain Creek Volcanics.||
4571|Cooma Granodiorite|22603|6|Mentioned|p100|||||||||
4571|Cooma Granodiorite|22778|6|Mentioned|p 160|||||||||
4571|Cooma Granodiorite|22779|6|Mentioned|p 179|||||||||
4571|Cooma Granodiorite|22815|4|Described|p63,64|Devonian|Early Devonian|Age range: 385-400 ma||||||
4571|Cooma Granodiorite|22857|6|Mentioned|p422 App. 1, Tb. A1.5|||See also p15 Fig. 11.9.||||||
4571|Cooma Granodiorite|22933|6|Mentioned|Fig11.9p15|||||||||
4571|Cooma Granodiorite|23321|5|Briefly described|p430 Fig. 1, p438|||||||||07-FEB-07
4571|Cooma Granodiorite|23464|6|Mentioned|p246|||||||||
4571|Cooma Granodiorite|23546|4|Described|p559|||Lachlan Fold Belt.||||||
4571|Cooma Granodiorite|23616|6|Mentioned|p79|||||||||
4571|Cooma Granodiorite|23866|5|Briefly described|p120, p121 Fig. 1|||Geological Province: Lachlan Fold Belt.||||||
4571|Cooma Granodiorite|24222|5|Briefly described|p2|||Regional aureole S-type granite.  Geological Province: Lachlan Fold Belt.||||||24-JAN-06
4571|Cooma Granodiorite|33781|6|Mentioned|Table 1|||||||||
4571|Cooma Granodiorite|35198|4|Described|p81|||||||||
4571|Cooma Granodiorite|35634|6|Mentioned|p151|||||||||
4571|Cooma Granodiorite|38216|6|Mentioned|p253|||||||||
4571|Cooma Granodiorite|38823|5|Briefly described|p208|||||||||
4571|Cooma Granodiorite|39240|5|Briefly described|p80|||||||||
4571|Cooma Granodiorite|39721|6|Mentioned|p48|||||||||
4571|Cooma Granodiorite|39822|6|Mentioned|p217|||||||||
4571|Cooma Granodiorite|41197|5|Briefly described|p257|||||||||
4571|Cooma Granodiorite|41418|4|Described|p363|||||||||
4571|Cooma Granodiorite|42110|6|Mentioned|p127|||||||||
4571|Cooma Granodiorite|43060|6|Mentioned|p109|||||||||
4571|Cooma Granodiorite|43147|5|Briefly described|p49,p51|||||||||
4571|Cooma Granodiorite|43158|4|Described|9,11|||||||||
4571|Cooma Granodiorite|43159|6|Mentioned|p3|||||||||
4571|Cooma Granodiorite|43233|5|Briefly described|Map Legend||Late Silurian|Possible Silurian age. Of Cooma Suite.||||||
4571|Cooma Granodiorite|49705|4|Described|p9|||||||||
4571|Cooma Granodiorite|61413|4|Described|pp2-7, pp48-50, pp76-83.|Silurian|Silurian|Surrounded by high-grade regional metamorphic rocks, commonly migmatite with which it is intimately related. S-type. Has a unique isotopic signature: detailed. Cooled rapidly after peak temperatures of in situ partial melting of surrounding metasediments.|c.440 Ma (Chappell et al. 1991).||||Strongly peraluminous with abundant andalusite and euhedral cordierite; many metasedimentary xenoliths and small pegmatite xenoliths; numerous undeformed plagioclase crystals; very high quartz content.|
4571|Cooma Granodiorite|63290|6|Mentioned|p403, p407|Early Silurian|Early Silurian|Age: 433Ma (Williams 2001).||||||
4571|Cooma Granodiorite|63770|5|Briefly described|p1024|||Age: 432.8 +/- 3.5 Ma (95% c.l.) SHRIMP U-Pb zircon; See Cooma Complex. Also referred to as Cooma granodiorite in figures and tables. Geol. Prov: Lachlan Fold Belt.||||||
4571|Cooma Granodiorite|65396|6|Mentioned|p162|||Lachlan Zone. Surrounded by low-pressure metamorphics.||||||
4571|Cooma Granodiorite|66183|6|Mentioned|p373|||In Cooma Complex.||||||
4571|Cooma Granodiorite|66575|6|Mentioned|p957,|||Anatectic. Of the Lachlan S-type field which are generally dissimilar to the more fractionated, felsic Tasmanian S-types.||||||
4571|Cooma Granodiorite|68310|6|Mentioned|p239|||The origin of lumps or nodules of milky quartz is controversial (discussed).||||||
4571|Cooma Granodiorite|69876|6|Mentioned|p313|||Anatectic. Comparison with the higher radiogenic Sr compositions in western Tasmanian granites.||||||
4571|Cooma Granodiorite|70125|6|Mentioned|p392|||Zircon ages discussed.||||||
4571|Cooma Granodiorite|70727|6|Mentioned|p187|||Geological province: Hill End Zone, Eastern Lachlan Orogen. Experienced a long period between emplacement and deformation, attributed to 'slow coolong' (Williams and Pulford, 2008).||||||
4571|Cooma Granodiorite|73264|5|Briefly described|p1391, p1393 Fig.15|Silurian|Silurian|Lachlan Orogen, eastern. S-type granitoid, formed from locally exposed adjacent metasedimentay rocks. Surrounded by diatextite and outwardly lower metamorphic facies. Age distribution of zircon cores matches that of adjacent migmatite melanosomes and biotite schist (Williams, 2001).|433.4+/-3.1 Ma zircon + monazite age|||||
4572|Cooma Metamorphic Complex|22721|6|Mentioned|Fig.1 p502, p504|||||||||
4572|Cooma Metamorphic Complex|22768|6|Mentioned|p155|||||||||
4572|Cooma Metamorphic Complex|22815|3|Fully described|p30, fig13||Early Silurian|||||||
4572|Cooma Metamorphic Complex|22857|4|Described|p135, p422 App. 1, Tb. A1.5|Early Ordovician|Early Ordovician|Metamorphosed Adaminaby Group. Turbiditic sequence with metamorphic zones around the anatectic Cooma Granodiorite. Intruded by Late Silurian Murrumbidgee Batholith. Geological Province: Monaro Forearc Basin. ||||||
4572|Cooma Metamorphic Complex|23245|6|Mentioned|p135|||||||||
4572|Cooma Metamorphic Complex|23309|5|Briefly described|p63, 69|||Equivalent to Kuark Metamorphic Complex in Victoria.||||||
4572|Cooma Metamorphic Complex|23866|4|Described|p120|||See also Cooma Complex.  Geological Province: Lachlan Fold Belt.||||||
4572|Cooma Metamorphic Complex|24310|5|Briefly described|p1044|||Geological Province: Lachlan Fold Belt||||||
4572|Cooma Metamorphic Complex|24517|5|Briefly described|p49|||Contains a core of heterogeneous diatexitic granite (Cooma suite). Geological Province: Lachlan Fold Belt.||||||04-MAY-05
4572|Cooma Metamorphic Complex|31386|3|Fully described|p345|||See also p346-360.||||||17-JAN-07
4572|Cooma Metamorphic Complex|40663|6|Mentioned|p219|||||||||
4572|Cooma Metamorphic Complex|42851|6|Mentioned|p555|||||||||
4572|Cooma Metamorphic Complex|43126|5|Briefly described|p3|||||||||
4572|Cooma Metamorphic Complex|43233|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
4572|Cooma Metamorphic Complex|43577|6|Mentioned|p381|||||||||
4572|Cooma Metamorphic Complex|44093|5|Briefly described|p192 App. 1|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
4572|Cooma Metamorphic Complex|60904|5|Briefly described|p784 Fig. 10|||Of the Lachlan Orogen. See also p794. ||||||
4572|Cooma Metamorphic Complex|61413|6|Mentioned|p2 Fig.1.|||||||||
4572|Cooma Metamorphic Complex|67322|6|Mentioned|p16|||||||||
4573|Cooma Suite|22815|6|Mentioned|p62|||||||||
4573|Cooma Suite|42110|6|Mentioned|p127|||||||||
4573|Cooma Suite|42726|5|Briefly described|map legend||Silurian|Of the Cooma Supersuite.  Includes the Cooma Granite (informal name).||||||09-FEB-05
4573|Cooma Suite|43233|5|Briefly described|Map Legend||Silurian|Possible Silurian age. Of Murrumbidgee Batholith.||||||
4573|Cooma Suite|44093|5|Briefly described|p192 App. 1|Silurian|Silurian|Foliated granite. Geological Province: Lachlan Fold Belt.||||||
4573|Cooma Suite|64571|6|Mentioned|p832|||||||||
4594|Coombing Formation|13139|5|Briefly described|p10|||Underlies the Weemalla Formation.||||||12-APR-05
4594|Coombing Formation|22503|6|Mentioned|p645|||||||||
4594|Coombing Formation|22679|2|Defined|p 9, 10|Ordovician|Early Ordovician|Of the Kenilworth Group, Lachlan Fold Belt. Maximum thickness: 3000m.||||||21-MAY-08
4594|Coombing Formation|22704|5|Briefly described|p59||Early Ordovician|Kenilworth Group. Overlain by Weemala Formation||||||
4594|Coombing Formation|22798|5|Briefly described|p857||Ordovician|Age: Middle Ordovician.||||||
4594|Coombing Formation|22857|4|Described|p134, p428 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Of the Kenilworth Group. Feldspathic siltstone and arenite, chert. Max. thickness: 3000m. Geological Province: Monaro Forearc Basin. ||||||
4594|Coombing Formation|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
4594|Coombing Formation|23170|6|Mentioned|p34||Darriwilian|of Kenilworth Group.||||||
4594|Coombing Formation|23202|6|Mentioned|Fig.1|||of Kenilworth Group||||||
4594|Coombing Formation|23214|2|Defined|p28|Ordovician|Ordovician|Of Kenilworth Group. Type Section: GR 700200 6273500.  Max. thickness 3000m. Underlain by Adaminaby Group. Geological Province: Lachlan Fold Belt.  Fine grained dark feldspathic mudstone. Age determined by Palaeontological evidence.||||||21-MAY-08
4594|Coombing Formation|23245|6|Mentioned|p134||Early Ordovician|||||||
4594|Coombing Formation|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
4594|Coombing Formation|24006|6|Mentioned|p318|||||||||
4594|Coombing Formation|24007|6|Mentioned|p342|||||||||
4594|Coombing Formation|24263|5|Briefly described|p1387|Late Ordovician|Late Ordovician|||||||
4594|Coombing Formation|24268|4|Described|p1535|Middle Ordovician|Early Ordovician|Overlain by Forest Reefs Volcanics. Underlain by Mount Pleasant Basalt. Geological Province: Lachlan Fold Belt||||||21-MAY-08
4594|Coombing Formation|24398|5|Briefly described|p265, p259 Fig. 2|Bendigonian|Lancefieldian|Overlain by Weemalla Formation.  Geological Province: Lachlan Fold Belt.||||||
4594|Coombing Formation|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
4594|Coombing Formation|43569|6|Mentioned|p480|||'informal'?||||||
4594|Coombing Formation|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Kenilworth Group. Consists of feldspathic siltstone and sandstone, chert.||||||15-JUL-08
4594|Coombing Formation|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Kenilworth Group. Feldspathic siltstone and sandstone, chert.||||||17-JUL-08
4594|Coombing Formation|43782|5|Briefly described|Map Legend|Darriwilian|Darriwilian|of Kenilworth Group.||||||
4594|Coombing Formation|49794|4|Described|p11|||||||||
4594|Coombing Formation|60417|5|Briefly described|p153|Gisbornian|Darriwilian|Overlain by Forest Reefs Volcanics.||||||
4594|Coombing Formation|63277|6|Mentioned|139|Early Ordovician|Early Ordovician|Overlain by part of the Forest Reefs Volcanics. Consists of volcaniclastic rocks. Contains zircons with the age of 467+/-4Ma.||||||
4594|Coombing Formation|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p156|Late Ordovician|Middle Ordovician|Overlain by Forest Reefs Volcanics, and Blaney Volvanics (in  Blaney area). Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
4594|Coombing Formation|63283|5|Briefly described|p188 Tb. 1, p195 Fig. 2, p202|Late Ordovician|Middle Ordovician|Overlain by Forest Reefs Volcanics and Blayney Volcanics. Geological Province: Molong Volcanic Belt. Consists of feldspathic turbidites.||||||07-FEB-11
4594|Coombing Formation|63285|4|Described|p275 Fig. 2, p275, p285, p288|Middle Ordovician|Middle Ordovician|Conformably overlain by Forest Reefs Volcanics. Geological Province: Molong Volcanic Belt. Consists of feldspathic sandstone, black mudstone and feldspathic turbidites.||||||10-DEC-07
4594|Coombing Formation|63286|5|Briefly described|p294 Fig. 1, p295, p298, p308 Fig. 9|Middle Ordovician|Middle Ordovician|Overlain by Blayney Volcanics, Millthorpe Volcanics, Byng Volcanics and Forest Reefs Volcanics. Intruded by Eagle Hawk Basalt. Consists of feldspathic sandstone and mudstone, minor basalt intrusions.||||||07-FEB-11
4594|Coombing Formation|63289|5|Briefly described|p367, p369, p372, p374|Gisbornian|Darriwilian|Conformably underlain by Adaminaby Group. Consists of greenschist-facies volcaniclastic sandstone, metamorphosed to chlorite-grade and contains graptolites (squire, 2001).||||||07-FEB-11
4594|Coombing Formation|63290|6|Mentioned|p396 Fig. 3|Gisbornian|Middle Ordovician|Geological Province: Molong Volcanic Belt. Consists of siltstone.||||||
4594|Coombing Formation|63293|6|Mentioned|p469 Fig. 2|Gisbornian|Darriwilian|Overlain by Forest Reefs Volcanics and Blayney Volcanics. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
4594|Coombing Formation|64963|5|Briefly described|p182 Fig. 2|||Age: 467+/-4Ma (detrital zircons, Meffre et al 2007). Relatively deep marine deposits. ||||||
4594|Coombing Formation|67106|6|Mentioned|p673, 681|||Molong Volcanic Belt.|466.7 +/- 4.4 Ma (Crawford et al., 2007).|||||
4594|Coombing Formation|67322|4|Described|Fig.5; p24-25|Late Ordovician|Middle Ordovician|Macquarie Arc. Modified by Wyborn, in Pogson and Watkins (1998), from the description of Wyborn (1992). Ages from laser ablation ICP-MS U/Pb of detrital zircons by Crawford, Meffre et al. (2007). Graptolites of Darriwilian to Gisbornian age have also been found in the unit. Occurs in the Blayney region.|467 +/- 4 Ma.|||Overlain by the Forest Reefs Volcanics. Overlain by the Lower Blayney Volcanics.|Feldspathic mudstone which is commonly silicified and grades to fine-grained volcaniclastic sandstone.|21-FEB-18
4594|Coombing Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
4594|Coombing Formation|69539|6|Mentioned|p607|||||||||
4594|Coombing 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. Molong Volcanic Belt. Shown as Coombing Fm. |c. 470-455 Ma|Cabonne Group||||
4594|Coombing Formation|70684|6|Mentioned|p3, p33, p75|||||||||
4594|Coombing Formation|70727|6|Mentioned|p172|Ordovician|Ordovician|Geological province: Hill End Zone, Eastern Lachlan Orogen.||||Passive intruded by Wyangala Granite.||
4594|Coombing Formation|73154|5|Briefly described|p77 Fig.3, p91|Gisbornian|Darriwilian|Macquarie Arc, Phase 2. Molong Volcanic Belt.|467+/-4 Ma|||Underlies Forest Reef Volcanics, lower Blayney Volcanics.|Shale, includes volcaniclastic rock.|
4594|Coombing Formation|73431|6|Mentioned|p364-365, p366 Fig.3|Ordovician|Ordovician|Lachlan Orogen.||||Intruded by Browns Creek Intrusive Complex||
4598|Coonambidgal Formation|2967|5|Briefly described|p40, 107|||Lawrence (1966, 1975). Murray Basin.|||||Brown and grey clays; a terrace with large wavelength meander scroll.|
4598|Coonambidgal Formation|10010|5|Briefly described|p16|Quaternary|Pliocene|Grades downwards into Calivil Formation  Geological Province: Murray Basin.||||||20-FEB-09
4598|Coonambidgal Formation|22531|5|Briefly described|p22|||||||||
4598|Coonambidgal Formation|22532|5|Briefly described|map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|22756|6|Mentioned|P39|||||||||
4598|Coonambidgal Formation|22782|6|Mentioned|p15|||||||||
4598|Coonambidgal Formation|22799|3|Fully described|p58|Holocene|Late Pleistocene|Age: <14 000 years BP.||||||21-MAY-08
4598|Coonambidgal Formation|22887|2|Defined|p47|Holocene|Holocene|||||||
4598|Coonambidgal Formation|22893|3|Fully described|p62,63 table3,11||Holocene|Unconsolidated. Broken up into older and younger alluvial terraces.||||||
4598|Coonambidgal Formation|23164|5|Briefly described|p16|||||||||
4598|Coonambidgal Formation|23166|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23167|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23168|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23169|5|Briefly described|Map legend||Quaternary|||||||
4598|Coonambidgal Formation|23252|5|Briefly described|Map Legend|||||||||11-JAN-10
4598|Coonambidgal Formation|23603|5|Briefly described|p12|||||||||
4598|Coonambidgal Formation|23604|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23605|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23606|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23607|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|23921|5|Briefly described|p1109 Table 2|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|24103|6|Mentioned|p139 Fig.3|||||||||
4598|Coonambidgal Formation|24107|6|Mentioned|p224|||||||||
4598|Coonambidgal Formation|24133|6|Mentioned|p51|||Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|24177|3|Fully described|p77|Recent|Recent|Defined by Lawrence (1966) from type locality in NSW. Disconformably overlies the Shepparton Formation. Geological Province: Murray Basin.||||||17-JUN-09
4598|Coonambidgal Formation|24178|6|Mentioned|p18|Devonian|Ordovician|||||||
4598|Coonambidgal Formation|24232|5|Briefly described|p226 Fig.2, p227|||||||||
4598|Coonambidgal Formation|24326|5|Briefly described|Map legend|Recent|Pleistocene|||||||
4598|Coonambidgal Formation|24439|5|Briefly described|p8, p18|Quaternary|Quaternary|Fluvial sediments of Lawrence (1966).  Diachronous with Shepperton Formation.  See also p47 Fig. 22, Appendix 2.||||||
4598|Coonambidgal Formation|24440|5|Briefly described|Map legend|||||||||
4598|Coonambidgal Formation|24551|5|Briefly described|p338 Fig. 11.2, 342|Holocene|Late Pleistocene|Of the Wunghnu Group.||||||
4598|Coonambidgal Formation|29860|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|29898|6|Mentioned|p213|||||||||
4598|Coonambidgal Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|30750|6|Mentioned|p4|||||||||
4598|Coonambidgal Formation|30751|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30753|4|Described|p14|||Recent age||||||
4598|Coonambidgal Formation|30754|2|Defined|Fig.33|Recent|Recent|||||||
4598|Coonambidgal Formation|30755|6|Mentioned|p169|||Tectonic map||||||
4598|Coonambidgal Formation|30758|6|Mentioned|p66|||Riverine||||||
4598|Coonambidgal Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
4598|Coonambidgal Formation|30906|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|30934|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30935|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30936|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|30996|3|Fully described|p48|||Age discussed.||||||21-MAY-08
4598|Coonambidgal Formation|31654|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|31713|5|Briefly described|p17|||||||||
4598|Coonambidgal Formation|31741|6|Mentioned|p6|||||||||
4598|Coonambidgal Formation|31742|5|Briefly described|p6|||Upper Cainozoic||||||
4598|Coonambidgal Formation|31745|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|31746|6|Mentioned|p197|||||||||
4598|Coonambidgal Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|32007|6|Mentioned|Fig. 2|||||||||
4598|Coonambidgal Formation|32432|6|Mentioned|Fig.2|||Table 1||||||
4598|Coonambidgal Formation|34180|6|Mentioned|p212|||Recent||||||
4598|Coonambidgal Formation|34735|4|Described|p41|||Also mention p8||||||
4598|Coonambidgal Formation|34758|6|Mentioned|p27|||||||||
4598|Coonambidgal Formation|34986|6|Mentioned|p339|||||||||
4598|Coonambidgal Formation|35091|4|Described|p18|||||||||
4598|Coonambidgal Formation|35097|6|Mentioned|Fig.4|||||||||
4598|Coonambidgal Formation|35111|6|Mentioned|p2|||||||||
4598|Coonambidgal Formation|35174|6|Mentioned|p167|||||||||
4598|Coonambidgal Formation|35187|6|Mentioned|Table1|||||||||
4598|Coonambidgal Formation|35200|6|Mentioned|Map legend|Holocene|Holocene|||||||
4598|Coonambidgal Formation|35232|5|Briefly described|Table.4|||||||||
4598|Coonambidgal Formation|35272|3|Fully described|p280|||||||||
4598|Coonambidgal Formation|37871|4|Described|p13|||||||||
4598|Coonambidgal Formation|37873|4|Described|p4|||||||||
4598|Coonambidgal Formation|37881|6|Mentioned|p16|||||||||
4598|Coonambidgal Formation|37882|4|Described|p7|||||||||
4598|Coonambidgal Formation|37883|6|Mentioned|p11|||||||||
4598|Coonambidgal Formation|37884|6|Mentioned|p14|||||||||
4598|Coonambidgal Formation|37885|5|Briefly described|p6|||||||||
4598|Coonambidgal Formation|38068|5|Briefly described|p79|||||||||
4598|Coonambidgal Formation|38879|6|Mentioned|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|39858|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
4598|Coonambidgal Formation|39860|5|Briefly described|p33|||||||||
4598|Coonambidgal Formation|40226|6|Mentioned|p51|||||||||
4598|Coonambidgal Formation|40522|6|Mentioned|Fig.2|||||||||
4598|Coonambidgal Formation|41765|4|Described|p42|||||||||
4598|Coonambidgal Formation|41848|3|Fully described|p355|||Use of name has been varied. Here basal "Monoman Formation is not distinguished.||||||
4598|Coonambidgal Formation|41849|6|Mentioned|p409|||Age Pleistocene-Recent||||||
4598|Coonambidgal Formation|41868|6|Mentioned|p552|||||||||
4598|Coonambidgal Formation|42125|6|Mentioned|p139|||||||||
4598|Coonambidgal Formation|42128|5|Briefly described|p227|||See also Fig.2||||||
4598|Coonambidgal Formation|42184|6|Mentioned|Fig.2 P348|||||||||
4598|Coonambidgal Formation|42264|4|Described|p9|||See also Fig.3||||||
4598|Coonambidgal Formation|42454|5|Briefly described|p12|||Maximum age: 25 000BP.||||||20-OCT-08
4598|Coonambidgal Formation|42455|5|Briefly described|Map legend|Recent|Recent|||||||
4598|Coonambidgal Formation|42827|3|Fully described|p356|||see also Table 9.1||||||
4598|Coonambidgal Formation|42966|1|Redefined|p276|Holocene|Late Pleistocene|Of Wunghnu Group.||||||13-AUG-07
4598|Coonambidgal Formation|43053|5|Briefly described|Map Legend|Holocene|Holocene|||||||25-MAY-05
4598|Coonambidgal Formation|43258|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43261|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43298|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|43493|5|Briefly described|32-38|Recent|Pleistocene|Radiocarbon date: 25 000 years BP.||||||20-OCT-08
4598|Coonambidgal Formation|43655|5|Briefly described|p40-846|||||||||
4598|Coonambidgal Formation|44133|5|Briefly described|p254 Fig. 11.28|Holocene|Holocene|||||||
4598|Coonambidgal Formation|44185|5|Briefly described|Map legend.|Holocene|Holocene||||||Fluvial, lacustrine: clay, sand, sandy clay.|
4598|Coonambidgal Formation|44186|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|44187|5|Briefly described|Map Legend||Holocene|||||||
4598|Coonambidgal Formation|44188|5|Briefly described|Map Legend|Holocene|Pleistocene|Geological province: Murray Basin. Fluvial/alluvial deposits.||||||20-OCT-08
4598|Coonambidgal Formation|44191|5|Briefly described|Map Legend|Holocene|Late Pleistocene|||||||
4598|Coonambidgal Formation|46909|6|Mentioned|Fig.2|||||||||
4598|Coonambidgal Formation|49038|4|Described|Table 2|||Briefly described p32.||||||20-OCT-08
4598|Coonambidgal Formation|60005|5|Briefly described|Map legend|Holocene|Holocene|Fluvial, lacustrine: clay, sand, sandy clay.||||||11-JAN-10
4598|Coonambidgal Formation|60452|4|Described|p41-42|Quaternary|Quaternary|Alluvial deposits.||||||
4598|Coonambidgal Formation|60461|5|Briefly described|Map legend|Pleistocene|Pleistocene|Alluvial flood plain and fan deposits, channel sands and clay playettes; clay, silt, fine to coarse-grained sand, gravel.||||||
4598|Coonambidgal Formation|60491|4|Described|p23|Quaternary|Quaternary|Deposited by modern day streams and consists of unconsolidated grey-brown silt, clay, gravel and sand.||||||22-NOV-04
4598|Coonambidgal Formation|60492|5|Briefly described|Map Legend|Pleistocene|Pliocene| Alluvium of modern day streams and recent ancestors: sand, silt, clay.||||||30-SEP-04
4598|Coonambidgal Formation|60529|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||14-JUN-06
4598|Coonambidgal Formation|60591|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60592|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60593|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60595|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60596|5|Briefly described|Map Legend|Recent|Pliocene|Overlies the Shepparton Formation. Clay, silt, fine-to coarse grained sand, gravel, moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|60597|5|Briefly described|Map Legend|Recent|Pliocene|Nonmagnetic with dendritic, moderately magnetic responses (10-20 nT) coinciding with present and prior streams; low K, Th, and variable U.||||||
4598|Coonambidgal Formation|60599|2|Defined|p24 Tb. 4, p95-96|Quaternary|Quaternary|Of Wunghnu Group. Includes Cobram Sand. Pale grey-brown silt +clay or fine- to coarse-g.qtz+ lithic sand, silt/clay; parts contain well-rounded qtz pebbles + ironstone fragments. Disconformable on Shepparton Formation; unconformable on Newer Volcanics. ||||||
4598|Coonambidgal Formation|60953|5|Briefly described|Map Legend|Holocene|Holocene|Stream alluvium in Murray River valley.||||||11-MAY-05
4598|Coonambidgal Formation|61108|5|Briefly described|map legend|Holocene|Holocene|Stream alluvium in Murray River valley.||||||
4598|Coonambidgal Formation|61163|5|Briefly described|p99, p109|||Term often used to include all the Quaternary alluvium in the Riverine Plains, but it is in fact a geomorphic unit and not primarily defined from its lithology.||||||
4598|Coonambidgal Formation|61185|2|Defined|p20 Fig. 5, p57, p64, p69-73|Recent|Pliocene|Of Lawrence (1966). Considered to now include Cobram Sand (Lawrence 1975). Deposits of existing streams cut into older Shepparton Formation sediments. Nonconformable on Strathbogie Granite. Actively deposited today.||||||07-FEB-11
4598|Coonambidgal Formation|61701|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61702|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61703|5|Briefly described|Map Legend|Recent|Pliocene|Alluvial flood plain, scroll deposits and source bordering dunes: clay, silt, fine to coarse grained sand, gravel: moderately sorted, unconsolidated.||||||
4598|Coonambidgal Formation|61704|6|Mentioned|Map legend|Quaternary|Quaternary|From stream deposits derived from Strathbogie Granite; high K, variable Th; sediments deposited by the Goulburn River have moderate to high K, low Th.||||||12-FEB-15
4598|Coonambidgal Formation|61964|5|Briefly described|p143, p177|Quaternary|Quaternary|Of the Wunghnu Group. Associated with the Shepparton Formation. Geological Province: Murray Basin.||||||
4598|Coonambidgal Formation|64612|6|Mentioned|p56|||Name no longer used. Lawrence (1966).||||||07-FEB-11
4598|Coonambidgal Formation|65552|5|Briefly described|p2,p5-7,p12-13,p17,p19; p24,27 App.3,6 |Quaternary|Early Pliocene|Of Wanghnu Group. Poorly consolidated, mottled, variegated clay and silty lenses of sand and gravel. Hosts silica sand and minor clay deposits. With Shepparton Formation, overlies Calivil Formation and is the uppermost sequence in the Murray Basin.||||||
4598|Coonambidgal Formation|65715|6|Mentioned|p17|||Lapsed into disuse by GSV.||||||
4598|Coonambidgal Formation|65969|5|Briefly described|p27 Tb.3.3, p30|Quaternary|Quaternary|Fluvial mud and sand. Conformably overlies other units. Underlain by Karoonda Surface. Fills current river valleys and debouchments onto the Murray Valley. No magnetic response; mostly Th-rich but variable radiometric response, depending on source rocks.||||||
4598|Coonambidgal Formation|66002|6|Mentioned|p18|||Disused name. Use extended beyond type section and lithology, to all modern-day alluvial sediments N of Great Dividing Range, so GSV has dropped name.||||||
4598|Coonambidgal Formation|66287|6|Mentioned|p30 Fig. 8|Holocene|Pleistocene|||||||
4598|Coonambidgal Formation|67179|5|Briefly described|p580 Fig.1b, p581, 582|Holocene|Pleistocene|Laid down under arid climate by 'ancestral streams' that are precursors to current rivers in the region. See VandenBerg (1997d) and Macumber (1991).||||Conformably overlies the Shepparton Formation.||
4598|Coonambidgal Formation|68194|5|Briefly described|p24, p35|Holocene|Pleistocene|Butler (1958); Lawrence (1966). Channel and floodplain sediments, including alluvial sediments currently being deposited in the south of the map area. Appears as Coonambigil on p35.||||Overlies Shepparton Formation.||
4598|Coonambidgal Formation|68716|6|Mentioned|p39 Fig.3, p40|||||||Underlain by the Monoman Formation.||
4598|Coonambidgal Formation|69089|5|Briefly described|Map legend|Holocene|Holocene||||||Fluvial, lacustrine: clay, sand, sandy clay.|
4598|Coonambidgal Formation|70718|5|Briefly described|p25|||Alluvial fan formation. See also misspelling Coonabidgal Formation p23.||||Overlies Calivil Formation gradationally.||
4598|Coonambidgal Formation|70961|14|Not recorded|p133|||Refers to Lawrence (1966).||||||
4598|Coonambidgal Formation|73188|6|Mentioned|p320|Holocene|Holocene|Murray Basin.|||||Sand, clay, gravel, loam.|
4598|Coonambidgal Formation|73228|6|Mentioned|p62|Quaternary|Pliocene|||||||
4598|Coonambidgal Formation|73496|5|Briefly described|Map legend|Holocene|Pleistocene|[misspelt in map legend as Coornambidgal]||Wunghnu Group|||Nonmagnetic; high total count, K, Th, U; occupies regional topographic lows.|
4598|Coonambidgal Formation|73505|5|Briefly described|p2, p12-13|Quaternary|Quaternary|Murray Basin. Conformably overlies other units. Fills active river valleys. Often high K, Th radiometric response. No detectable magnetic response.|||||Fluvial mud and sand.|
4616|Coonigan Formation|12066|5|Briefly described|p13|Cambrian|Cambrian|||||||
4616|Coonigan Formation|22671|5|Briefly described|Table1p833,Fig2p837||Middle Cambrian|Of the Gnalta Group. Shale, limestone, sandstone.||||||17-JAN-06
4616|Coonigan Formation|22857|5|Briefly described|p90 Fig. 14.7B|Middle Cambrian|Early Cambrian|Of the Gnalta Group. White shale; limestone, shale, sandstone. Max. thickness: 115m. Geological Province: Mount Wright Block. See also p404 App. 1 Tb. A1.4||||||
4616|Coonigan Formation|22858|6|Mentioned|Fig14.7bp90-1|||||||||
4616|Coonigan Formation|29991|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
4616|Coonigan Formation|30908|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Lower Middle Cambrian. Part of Gnalta Group.||||||23-DEC-09
4616|Coonigan Formation|31507|6|Mentioned|p181|||||||||
4616|Coonigan Formation|31705|6|Mentioned|p27|||||||||
4616|Coonigan Formation|32948|4|Described|p110|||Re. fossil locality.||||||11-SEP-07
4616|Coonigan Formation|34469|6|Mentioned|p109|||Lower & Middle Cambrian. Gnalta Group.||||||27-NOV-08
4616|Coonigan Formation|34889|6|Mentioned|Fig. 2|||Also P117||||||
4616|Coonigan Formation|38692|6|Mentioned|p139|||||||||
4616|Coonigan Formation|39214|4|Described|p10|||||||||
4616|Coonigan Formation|40136|6|Mentioned|p34|||||||||
4616|Coonigan Formation|40455|6|Mentioned|Fig.2|||||||||
4616|Coonigan Formation|40642|6|Mentioned|p169|||See also P171 and P174||||||
4616|Coonigan Formation|41109|6|Mentioned|p184|||||||||
4616|Coonigan Formation|41810|6|Mentioned|Fig.3|||||||||
4616|Coonigan Formation|42070|6|Mentioned|p4|||||||||
4616|Coonigan Formation|42206|4|Described|p257|||See also Fig.1||||||
4616|Coonigan Formation|43192|5|Briefly described|p64||Middle Cambrian|Of Gnalta Group.||||||11-SEP-07
4616|Coonigan Formation|43501|14|Not recorded|Map Legend|Middle Cambrian|Early Cambrian|(Provisional Edition) Part of Cinaltra Group.||||||27-NOV-08
4616|Coonigan Formation|43502|14|Not recorded|Map Legend||Middle Cambrian|(Provisional Edition) Part of Gnalta Group (Lower Middle Cambrian).||||||23-DEC-09
4616|Coonigan Formation|43704|6|Mentioned|p67|||||||||
4616|Coonigan Formation|44133|5|Briefly described|p28|Templetonian|Templetonian|||||||
4616|Coonigan Formation|47035|6|Mentioned|p89|||||||||
4616|Coonigan Formation|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Bancannia Shelf. NSW.  Contains fauna of Ordian age.||||||
4616|Coonigan Formation|60990|5|Briefly described|p81-82 |Middle Cambrian|Middle Cambrian|||Gnalta Group. ||Disconformably overlies the Cymbric Vale Formation.||
4616|Coonigan Formation|62787|5|Briefly described|p81, p82 Fig. 3|||Includes First Discovery Limestone Member. Unconformably underlain by Cymbric Vale Formation.||||||07-FEB-11
4616|Coonigan Formation|63489|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Shale with minor limestone.||||||
4616|Coonigan Formation|63789|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Gnalta Group. Shale and siltstone with minor limestone.||||||
4616|Coonigan Formation|63793|5|Briefly described|p23.|Middle Cambrian||At least 113 m thick. Contains trilobites and brachiopods.||Top unit in Gnalta Group. ||Overlies Cymbric Vale Formation.|Shales, siltstones and limestones.|
4616|Coonigan Formation|64671|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Gnalta Group.  Shale with minor limestone.||||||
4616|Coonigan Formation|64679|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Of the Gnalta Group. Sahel and siltstone with minor limestone; abundant trilobite, brachiopod and algal fossils.||||||27-NOV-08
4616|Coonigan Formation|64680|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Gnalta Group. Shale with minor limestone.||||||
4616|Coonigan Formation|66623|3|Fully described|pp56-58, pp61-65, p144. |Middle Cambrian|Middle Cambrian|Defined by Warris (1967). Formerly part of lower 'Gnalta Stage' of Mootwingee Series (Kenny 1934). Ordian-early Templetonian. Stratigraphic equivalent of Pincally and Wydjah Formations. Thickness >130 m. Outcrops very poorly. Contains trilobites in upper shale and siltstone, and oncolites in the lower.||Unit in Gnalta Group.|Includes First Discovery Limestone Member.|Disconformably overlies Cymbric Vale Formation. Is unconformably or disconformably overlain by Nuchea Conglomerate.|White to very light brown shale and interbedded siltstone, massive-style bedding.|
4616|Coonigan Formation|66918|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Gnalta Group.||Overlies Cymbric Vale Formation.|Shale and siltstone with minor limestone.|
4616|Coonigan Formation|66929|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian||||||Shale; minor limestone.|
4616|Coonigan Formation|67322|4|Described|p5, p8-9, p28; Fig.5|Middle Cambrian|Early Cambrian|Of Warris (1967). Age from upper Ordian trilobites. Occurs in the Mount Wright-Mutawintji region. Underlies the Delamerian unconformity.||Topmost unit of the Gnalta Group.|First Discovery Limestone Member|Disconformably overlies Cymbric Vale Formation.|Basal limestone and shale, overlain by fossiliferous limestones, and c.14 m of white micaceous shale at the top which contains a diverse trilobite fauna.|21-FEB-18
4616|Coonigan Formation|69573|6|Mentioned|p656, 657, 659, 661, 670|||Gnalta Shelf. Features Cambrian Stage 5 fossil sites.||||||
4616|Coonigan Formation|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Koonenberry Belt.||Unit in Gnalta Group.||||
4616|Coonigan Formation|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|||Gnalta Group|||Shale and siltstone with minor limestone.|20-JAN-22
4616|Coonigan Formation|70752|5|Briefly described|p127, p129, p131, p135, p139-140|||Koonenberry Belt. Linguliformean brachiopods have close affinity with those in Giles Creek Dolostone (NT).|||First Discovery Limestone Member.|||
4616|Coonigan Formation|70838|5|Briefly described|p269|Cambrian|Cambrian|Koonenberry Belt. Shown as lateral equivalent to First Discovery Limestone. Both overlie a tuff dated at 510 +/- 2.3 Ma.||Gnalta Group.|First Discovery Limestone.|Overlies Cymbric Vale Formation.||
4618|Coonongooba Formation|45090|6|Mentioned|p218|||Tatarian.||||||
4633|Coorabin Coal Measures|22773|5|Briefly described|Fig24.5p350|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|22857|5|Briefly described|p518 App.1 Tb.A1.9||Late Permian|Includes the Nowranie Creek, Loughmore and Narrow Plain Formations. Geological Province: Ovens Graben of the Tasman Epicratonic Province. See also p350 Fig.24.5..||||||
4633|Coorabin Coal Measures|22893|6|Mentioned|fig4 p9|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|23836|5|Briefly described|p93|Late Permian|Late Permian|Geological Province: Murray Basin.||||||
4633|Coorabin Coal Measures|24551|6|Mentioned|p212|Late Permian|Late Permian|||||||
4633|Coorabin Coal Measures|32315|6|Mentioned|Fig. 2|||||||||
4633|Coorabin Coal Measures|34418|5|Briefly described|p502|||||||||
4633|Coorabin Coal Measures|35498|3|Fully described|p142|||New units defined on P144||||||
4633|Coorabin Coal Measures|35767|6|Mentioned|p31|||||||||
4633|Coorabin Coal Measures|36172|6|Mentioned|Appendix|||||||||
4633|Coorabin Coal Measures|36329|6|Mentioned|p62|||||||||
4633|Coorabin Coal Measures|37065|6|Mentioned|p35|||||||||
4633|Coorabin Coal Measures|37101|4|Described|p261|||||||||
4633|Coorabin Coal Measures|38293|4|Described|p20|||||||||
4633|Coorabin Coal Measures|39929|6|Mentioned|p276|||||||||
4633|Coorabin Coal Measures|40324|6|Mentioned|p53|||||||||
4633|Coorabin Coal Measures|40520|6|Mentioned|Fig.5|||||||||
4633|Coorabin Coal Measures|41226|6|Mentioned|Table 1|||||||||
4633|Coorabin Coal Measures|42454|6|Mentioned|p19|||Oaklands Basin.||||||
4633|Coorabin Coal Measures|42547|5|Briefly described|p83|||||||||
4633|Coorabin Coal Measures|42648|5|Briefly described|p39|||||||||
4633|Coorabin Coal Measures|42966|4|Described|p64|||||||||
4633|Coorabin Coal Measures|43218|5|Briefly described|p27||Late Permian|Ovens Graben.||||||
4633|Coorabin Coal Measures|43841|4|Described|8||Late Permian|Unconformable over Urana Fm, unconformable under Jerilderie Fm. Mostly coal that totals up to 20m.||||||
4633|Coorabin Coal Measures|44340|14|Not recorded|p.3,4||Permian|I/55-14.||||||
4633|Coorabin Coal Measures|44341|14|Not recorded|map legend||Permian|Shale and mudstone with coal sandstone bands.||||||
4633|Coorabin Coal Measures|49040|6|Mentioned|p12|||||||||
4633|Coorabin Coal Measures|61314|5|Briefly described|p128|Late Permian|Late Permian|Upward-fining sequence of conglomerate, sandstone, siltstone, mudstone, carbonaceous clay and coal. Overlain by the Jerilderie Formation. Geological Province: Murray Basin.||||||
4633|Coorabin Coal Measures|69798|5|Briefly described|p4, p7, p11-18|Late Permian|Early Permian|Oaklands Basin. Seismic profiles. Late Permian. Fine-grained units in the upper part provide a seal for lower reservoirs. Fluvial-point bar depositional environment.|||Nowranie Creek, Loughmore, Narrow Plain, Formations.|Unconformably overlies the Urana Formation. Is overlain disconformably by Jerilderie Formation.||06-FEB-18
4633|Coorabin Coal Measures|70125|5|Briefly described|p396|Permian|Permian|Oaklands Basin. 80m thick.||||Overlies Urana Formation. Is overlain by Jerilderie Formation.||
4654|Cootamundra Group|22638|3|Fully described|p63|||3250 m thick.||||||
4654|Cootamundra Group|22857|5|Briefly described|p450 App.1, Tb.A1.6|Devonian|Devonian|Geological Province: Bogan Gate Terrace.||||||
4654|Cootamundra Group|23309|6|Mentioned|p390|||||||||
4654|Cootamundra Group|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
4654|Cootamundra Group|30172|6|Mentioned|p43|||||||||
4654|Cootamundra Group|35070|2|Defined|p110|Early Devonian|Early Devonian|||||||
4654|Cootamundra Group|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
4654|Cootamundra Group|35607|6|Mentioned|p101|||||||||
4654|Cootamundra Group|35609|4|Described|p11|||||||||
4654|Cootamundra Group|36411|6|Mentioned|p268|||Refs Basden et al 1978 for definition of modified name.||||||
4654|Cootamundra Group|40328|6|Mentioned|p40|||||||||
4654|Cootamundra Group|42313|5|Briefly described|p144, p178|Devonian||||||||
4654|Cootamundra Group|44093|5|Briefly described|p182 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
4654|Cootamundra Group|44192|5|Briefly described|Map Legend||Lochkovian|||||||
4654|Cootamundra Group|50191|5|Briefly described|p6, 9, 14|Early Devonian|Early Devonian|Includes: Cowcumbala Rhyolite.||||||
4654|Cootamundra Group|60280|5|Briefly described|p2, p3 Fig. 1|||||||||
4654|Cootamundra Group|73215|5|Briefly described|p994|||Tumut Trough.|416 +/- 3 Ma (Black, 2007).|||||
4667|Copeland Road Formation|22857|4|Described|p512 App.1 Tb.A1.8|Visean|Visean|Lithic arenite interbedded with minor mudstone and siltstone; cross-bedded or massive arenite; black hard siltstone; rich brachiopod fauna. Overlies the Wootton Beds. Max. thickness: 760m.||||||03-MAR-06
4667|Copeland Road Formation|30074|6|Mentioned|p8|||See also P9,10,11,12,19.||||||
4667|Copeland Road Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
4667|Copeland Road Formation|32866|6|Mentioned|p22|||Fossil content||||||
4667|Copeland Road Formation|32867|6|Mentioned|p36|||||||||
4667|Copeland Road Formation|32868|6|Mentioned|p199|||||||||
4667|Copeland Road Formation|32869|6|Mentioned|Fig.2|||See also Fig.3B||||||
4667|Copeland Road Formation|34072|6|Mentioned|Fig.4.5|||Carb. Fossils||||||
4667|Copeland Road Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
4667|Copeland Road Formation|34086|6|Mentioned|p264|||||||||
4667|Copeland Road Formation|34168|5|Briefly described|p254|||Carboniferous||||||
4667|Copeland Road Formation|36057|6|Mentioned|Fig.1|||||||||
4667|Copeland Road Formation|36528|6|Mentioned|p179|||||||||
4667|Copeland Road Formation|38801|6|Mentioned|Fig.3|||||||||
4667|Copeland Road Formation|39302|4|Described|p348|||||||||
4667|Copeland Road Formation|39308|4|Described|p484|||Faunal list p485.||||||22-MAY-08
4667|Copeland Road Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Tamworth Belt.||||||16-DEC-04
4667|Copeland Road Formation|42547|4|Described|p34, p36|||||||||
4667|Copeland Road Formation|43447|14|Not recorded|p12|||||||||
4667|Copeland Road Formation|44093|5|Briefly described|p230 App. 1|Late Devonian|Late Devonian|Geological Province: New England Fold Belt.||||||
4667|Copeland Road Formation|44244|2|Defined|p136|Visean|Visean|Overlies the Verulam Oolite Member (Wotton beds).  Max. thickness: 760m. Geological Province: Myall Block.  Type section in text.  This unit is represented by the Conger and Berrico Creek Formations in the south.||||||22-MAY-08
4667|Copeland Road Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
4667|Copeland Road Formation|46803|6|Mentioned|p146|||||||||
4667|Copeland Road Formation|47056|6|Mentioned|Fig.2 P523|||||||||
4667|Copeland Road Formation|48924|6|Mentioned|p9||Early Carboniferous|L.Carb. See also P11-15,18,19.||||||
4667|Copeland Road Formation|50147|5|Briefly described|Map legend|Visean|Visean|Massive to cross bedded lithic sandstone, mudstone and siltstone.||||||
4677|Copper Creek Shale|12185|5|Briefly described|map legend|Middle Silurian|Middle Silurian|Grouped with Rutledge Quartzite in legend. Siltstone, graphitic slate, tuff, limestone lenses, quartzite. Underlies Kohinoor Volcanics. BMR map symbol: Smc.||||||
4677|Copper Creek Shale|22768|6|Mentioned|p177|||||||||
4677|Copper Creek Shale|22857|4|Described|p177, p474 App.1 Tb.A1.6|Late Silurian|Late Silurian|Basal sediments of Hoskinstown Group. Shale and siltstone, arenite beds near base; minor limestone; contains corals. Max. thickness: 150m. Geological Province: Captains Flat-Goulburn Trough. ||||||
4677|Copper Creek Shale|23048|5|Briefly described|p2 fig5||Silurian|||||||
4677|Copper Creek Shale|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
4677|Copper Creek Shale|29994|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
4677|Copper Creek Shale|30433|5|Briefly described|p695|||||||||
4677|Copper Creek Shale|31017|6|Mentioned|p45|||||||||
4677|Copper Creek Shale|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
4677|Copper Creek Shale|31020|5|Briefly described|p12|||Also mention Fig. 5.||||||
4677|Copper Creek Shale|31161|5|Briefly described|PA7|||||||||
4677|Copper Creek Shale|31411|5|Briefly described|p17|||See also p18.||||||22-MAY-08
4677|Copper Creek Shale|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
4677|Copper Creek Shale|32820|6|Mentioned|p3|||Mb. Hoskinstown Gp.||||||
4677|Copper Creek Shale|33325|5|Briefly described|Table 2|||||||||
4677|Copper Creek Shale|36413|2|Defined|p56|Silurian|Silurian|||||||
4677|Copper Creek Shale|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Of Hoskinstown Group. Includes Rutledge Quartzite Member, and unnamed tuff (Sct) and limestone (Scl) units. Underlies Kohinoor Volcanics. Unconformably overlies Foxlow Beds. GSNSW map code: Sc.||||||
4677|Copper Creek Shale|37727|4|Described|p48|||||||||
4677|Copper Creek Shale|40328|5|Briefly described|p181|||||||||
4677|Copper Creek Shale|42497|5|Briefly described|Map Legend|Ludlovian|Ludlovian|||||||
4677|Copper Creek Shale|42727|5|Briefly described|map legend|Ludlow|Ludlow|Of Hoskinstown Group. Includes Rutledge Quartzite Mbr. Shale, siltstone and minor limestone. Under Carwoola Fm and Captains Flat Fm; over Bullongong Shale, Birkenburn beds and Pittman Formation. BMR map symb: Suo. Geol Prov: Captains Flat Block.||||||22-MAY-08
4677|Copper Creek Shale|42820|2|Defined|p46|Ludlow||Of Hoskinstown Group.||||||20-MAY-08
4677|Copper Creek Shale|48873|14|Not recorded|p.9|||(I55-16/Michelago).||||||
4677|Copper Creek Shale|48878|2|Defined|p.6-8||Wenlockian|On many pages. p.7,1,5,15-17,19,22-25,29,31,36-38,44-49,50-55,Pl.3-4. Contains Wenlockian corals. Wenlockian (I55-16).||||||
4677|Copper Creek Shale|66197|5|Briefly described|p629, p631 Fig.3c|Siluran||Ngunawal Basin. Conglomerate base with basement-derived clasts, deep marine shale. Overlain by Kohinoor and Carwoola Formations. Probably Late Silurian.||||||13-MAR-12
4677|Copper Creek Shale|68592|5|Briefly described|p743, p772|||||Hoskinstown Group||Is overlain by Kohinoor Volcanics|Shale-rich with sporadic limestone bodies.|
4677|Copper Creek Shale|71069|6|Mentioned|p71, p105, p106, p146|||Obsolete name, remapped in this field area as Bumballa Formation (including the type section and representative sections in Michelago100 and Canberra100). Type area for this unit mentioned near the disused Captains Flat railway station. ||Hoskinstown Group|Includes the Rutledge Quartzite Member.|Equivalent to the De Drack Formation.||
4690|Coppermine Creek Volcanics|34404|4|Described|p92|||||||||
4690|Coppermine Creek Volcanics|45147|6|Mentioned|M10|||||||||
4698|Coramba beds|22857|5|Briefly described|p516 App.1 Tb.A1.8|Carboniferous|Carboniferous|Included in the informal "Coffs Harbour Association". Lithofeldspathic wacke, minor siltstone, siliceous siltstone, mudstone, metabasalt, chert and jasper. Several kms thick. Geol. Prov: Texas-Coffs Harbour Slope and Basin. See also p318 Fig.22.10A.||||||
4698|Coramba beds|22865|6|Mentioned|Fig22.10bp319||Late Carboniferous|||||||
4698|Coramba beds|23720|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Part of the "Coffs Harbour Association".  Lithofeldspathic wacke, minor siltstone, siliceous siltstone, mudstone, metabasalt, chert and jasper, rare calcareous siltstone and felsic volcanics.||||||02-MAY-13
4698|Coramba beds|23811|5|Briefly described|Map Legend|Westphalian|Tournaisian|Part of the "Coffs Harbour Association".  Lithofeldspathic wacke, minor siltstone, siliceous siltstone, mudstone, metabasalt, chert and jasper, rare calcareous siltstone and felsic volcanic rocks.||||||02-MAY-13
4698|Coramba beds|23812|5|Briefly described|p10, p12 Tb.1|Late Carboniferous|Early Carboniferous|Included in the informal "Coffs Harbour Association".||||||
4698|Coramba beds|31695|6|Mentioned|p253|||||||||
4698|Coramba beds|37489|5|Briefly described|p261|||||||||
4698|Coramba beds|39468|6|Mentioned|p204|||||||||
4698|Coramba beds|40177|6|Mentioned|p47|||||||||
4698|Coramba beds|41631|6|Mentioned|p4|||[Superseded by Coramba Formation. CEBMar95]||||||
4698|Coramba beds|44450|3|Fully described|p14 Table 2|Late Carboniferous|Late Carboniferous|Geological Province: Coffs Harbour Block. Max. thickness: >1000 m.||||||
4698|Coramba beds|60079|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of the Coffs Harbour beds.||||||
4698|Coramba beds|60995|5|Briefly described|p51 Fig. 3|Late Carboniferous|Late Carboniferous|Material from this unit is found in Laytons Range Conglomerate in the form of argillite, chert and quartz clasts. Geological Province: Clarence-Moreton Basin. See also p54 Fig. 5, p56.||||||29-MAY-06
4698|Coramba beds|65380|5|Briefly described|p660, p662 Fig.3, p664, 672 Table 3|||Coffs Harbour Association/Block. Depositional age constrained by detrital zircon and Hillgrove Suite intrusions to between ~323 Ma and 305 Ma. ||||Elements of Hillgrove Suite intrude.|Volcanic-lithic sandstone.|
4698|Coramba beds|71628|5|Briefly described|p17: 4, 66, 68|Late Carboniferous|Late Carboniferous|Appears as Cooramba beds on p17-4.||Coffs Harbour Association.||Is intruded by Kellys Creek Leucomonzogranite, and Tallawudjah and Dundahra Creek Leucosyenogranites.||
4698|Coramba beds|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen, accretionary complex.|||||Includes coarse-grained hornblende-feldspathic sandstone, and hornblende-bearing quartz-poor, volcanic-lithic sandstone.|
4710|Cordeaux Crinanite|29901|4|Described|Table 1|||||||||
4710|Cordeaux Crinanite|35524|6|Mentioned|p76|||Age discussed.||||||
4710|Cordeaux Crinanite|36220|4|Described|p101|||||||||
4710|Cordeaux Crinanite|36222|6|Mentioned|Map legend|Quaternary|Late Triassic|Post Late Triassic to Quaternary.||||||
4710|Cordeaux Crinanite|42896|4|Described|p55|||Age: 26.2 +/- 3.0 Ma.||||||22-MAY-08
4710|Cordeaux Crinanite|43346|2|Defined|p4 Map||Eocene|See also Lexicon||||||
4710|Cordeaux Crinanite|43349|14|Not recorded|Map|||||||||
4710|Cordeaux Crinanite|67663|6|Mentioned|p519 Fig.1|||[Doubly mis-spelt as Courdeaux Crinnite].||||||
4714|Cordillo Silcrete|22912|6|Mentioned|34|||||||||
4714|Cordillo Silcrete|23155|6|Mentioned|p36|||From the Innamincka Dome on the eastern Innamincka map sheet.  Data from STRZELECKI suggest that this material could well be mainly late Tertiary, not Oligocene-Miocene as suggested by Wopfner (1974).||||||
4714|Cordillo Silcrete|24204|6|Mentioned|p270|Eocene|Eocene|Geological Province: Poolowanna Trough.||||||
4714|Cordillo Silcrete|38605|6|Mentioned|p35|||||||||
4714|Cordillo Silcrete|39322|6|Mentioned|p396|||||||||
4714|Cordillo Silcrete|40910|6|Mentioned|p17|||||||||
4714|Cordillo Silcrete|40911|6|Mentioned|Map legend|Oligocene|Eocene|||||||03-JUL-06
4714|Cordillo Silcrete|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
4714|Cordillo Silcrete|40926|3|Fully described|p25|||||||||
4714|Cordillo Silcrete|41098|5|Briefly described|p177|||||||||
4714|Cordillo Silcrete|42375|6|Mentioned|p21|||? Lake Eyre Basin. ? Oligocene.||||||
4714|Cordillo Silcrete|42469|5|Briefly described|p46|||used by Wopfner, 1978.||||||
4714|Cordillo Silcrete|42746|5|Briefly described|p19|||||||||
4714|Cordillo Silcrete|42905|5|Briefly described|p23, Fig 5.3|||||||||
4714|Cordillo Silcrete|44133|6|Mentioned|p202|||||||||
4714|Cordillo Silcrete|61836|5|Briefly described|p211||Eocene|||||||03-JUL-06
4714|Cordillo Silcrete|64778|6|Mentioned|p13|Tertiary|Tertiary|Pedirka and Simpson Desert Basins.||||||
4714|Cordillo Silcrete|65238|6|Mentioned|p6|Eocene|Eocene|||||||
4714|Cordillo Silcrete|65925|6|Mentioned|p139.|||||||||
4714|Cordillo Silcrete|66131|5|Briefly described|p242 Fig.2, p245, p249, p259|Oligocene|Eocene|Occurs in upper Cordillo Surface. Called Cordillo Silcrete Surface on p245. Developed over the Eyre Formation.||Of the Cordillo Surface.||Overlain by the Doonbarra Formation.||
4714|Cordillo Silcrete|66623|1|Redefined|p239, pp266-283.|Oligocene|Oligocene|Redefined and discussed in detail. Followed deep weathering of Eyre Formation and exists over much of inland Australia. Forms a resistant cap on escarpments, producing flat crests and mesas. More weakly silicified sandstones are mapped as Eyre Formation.||||Grades downwards into Eyre Formation. Locally overlain unconformably by Doonbara Formation. Forms capping over Winton Formation.|Variably siliceous, sheet-like bodies of silica-indurated sandstone and some conglomerate, now mainly comprising chalcedonic and locally opaline rocks; light grey to pale orange-brown.|05-JUN-13
4714|Cordillo Silcrete|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|19-SEP-11
4714|Cordillo Silcrete|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|20-SEP-13
4714|Cordillo Silcrete|67209|5|Briefly described|Map legend.|Paleogene|Paleogene|Two un-named sub-units with differing lithologies are mapped separately.||||Overlies Allaru Mudstone.|Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants; local light grey highly siliceous silcrete; local pale brown/grey moderately siliceous silcrete with common relict sedimentary features (bedding and pebbles).|
4714|Cordillo Silcrete|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.|||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants; local light grey highly siliceous silcrete; local pale brown/grey moderately siliceous silcrete with common relict sedimentary features (bedding and pebbles).|
4714|Cordillo Silcrete|69019|6|Mentioned|p118.|Miocene|Oligocene|Developed widely across northern and central SA.||||||
4714|Cordillo Silcrete|69023|6|Mentioned|p120|||See also Cordillo Surface (p108). Developed in the top of the Eyre Formation. Silcrete genesis and timing discussed in detail.||||||
4714|Cordillo Silcrete|69946|5|Briefly described|p29, p129|Oligocene|Oligocene|Caps Eyre Formation to produce prominent mesas. Gently folded and tilted during Early Oligocene. Reworked into the Mirackina Conglomerate.||||||
4714|Cordillo Silcrete|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Silcrete, variably silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|70648|5|Briefly described|Map Legend|Neogene|Paleogene||||||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|20-JAN-22
4714|Cordillo Silcrete|70649|5|Briefly described|Map Legend|Neogene|Paleogene|2 un-named units: Light grey highly siliceous silcrete, conglomeratic in places; commonly columnar and massive. Pale brown to grey moderately siliceous silcrete with common relict sedimentary features including bedding and pebbles.|||Includes 2 un-named units.||Silcrete, variable silicified sandstone and conglomerate; columnar and massive variants.|
4714|Cordillo Silcrete|71321|6|Mentioned|p65|Oligocene|Late Eocene|Of Eromanga Basin. Nomenclature after Wopfner (1974, 1978).||||||
4714|Cordillo Silcrete|71342|6|Mentioned|Ch5 p29, Ch5 p130|Oligocene|Eocene|Lake Eyre Basin. This unit was gently folded and tilted during the Oligocene.||||Overlies the Eyre Formation.||
4714|Cordillo Silcrete|73234|6|Mentioned|p13|Early Oligocene|Late Eocene|Correlated with the topographically high-lying silcrete surface named 'Tent Hill surface' by Twidale et al. (1970).||||||
4718|Coreen Creek Coal Member|35498|2|Defined|p145|Late Permian|Late Permian|||||||
4718|Coreen Creek Coal Member|35503|6|Mentioned|p201|||Defined in Standing Committee Coalfield Geology NSW (1978)||||||
4718|Coreen Creek Coal Member|38293|5|Briefly described|p20|||||||||
4718|Coreen Creek Coal Member|42966|4|Described|p64|||Of Loughmore Formation.||||||22-MAY-08
4718|Coreen Creek Coal Member|43841|6|Mentioned|8||Late Permian|Member of Coorabin Coal Measures.||||||22-MAY-08
4718|Coreen Creek Coal Member|69798|5|Briefly described|p4 Fig.2|Permian|Permian|Oaklands Basin. Fluvial-point bar depositional environment.||Loughmore Formation.||||06-FEB-18
4721|Coreena Member|12597|4|Described|p492 Tb.1, p493 Fig.2, p495 Fig.3|Albian|Albian|See also p498, p499. E Eromanga Basin. 50-200m thick. Fossil wood and worm burrows are common in the upper part of the sequence. Also equivalent to upper part of Bulldog Shale and lower part of Oodnadatta Formation.||Unit in Wallumbilla Formation.||Overlies Doncaster Member. Equivalent to Coorikiana Formation. Is overlain by Surat Siltstone.|Interbedded mudstone, siltstone, and fine-grained, thickly-bedded lithic sandstone which is commonly glauconitic and calcareous; belemnite coquinites and marine molluscs also recorded in this sequence.|
4721|Coreena Member|13516|5|Briefly described|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||Of Wallumbilla Formation||||
4721|Coreena Member|22757|5|Briefly described|Table6,p11||Early Cretaceous|165 m. Wallumbilla Formation, Rolling Downs Group, Surat Basin.||||||
4721|Coreena Member|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Albian|Aptian|Of Wallumbilla Formation (Rolling Downs Group); in the Tibooburra area these rocks are included in Oornoo beds. Equivalent to Surat Siltstone (Surat Basin). Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6, p544 App.1 Tb.A1.12.||||||
4721|Coreena Member|22865|5|Briefly described|Table22.1p296-7|Albian|Aptian|||||||
4721|Coreena Member|23430|4|Described|p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province. Maximum thickness <245 m.||||||
4721|Coreena Member|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group).  Geological Province: Great Australian Superbasin.||||||
4721|Coreena Member|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Wallumbilla Formation. Geological Province: Great Artesian Basin.||||||
4721|Coreena Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
4721|Coreena Member|24251|6|Mentioned|p245|||Parent: Wallumbilla Formation||||||
4721|Coreena Member|30024|6|Mentioned|p331|||||||||
4721|Coreena Member|30042|5|Briefly described|p5|||Faunas correlation.||||||
4721|Coreena Member|30691|4|Described|p17|||See also P21,Table 4,6. Lower -Upper Cretaceous||||||
4721|Coreena Member|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
4721|Coreena Member|30696|4|Described|Table 4|||Albian||||||
4721|Coreena Member|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30700|6|Mentioned|p28|||Lower Cretaceous age. Unit of Wallumbilla Formation||||||
4721|Coreena Member|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|30853|6|Mentioned|p10|||Correlate in Wallumbilla Formation||||||
4721|Coreena Member|30854|4|Described|Table 4|||Lower Cretaceous.||||||
4721|Coreena Member|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31098|5|Briefly described|Table 1|||L.Cretaceous||||||
4721|Coreena Member|31116|4|Described|p43|||See also P44||||||
4721|Coreena Member|31208|6|Mentioned|Table 1|||See also Figs. 3, 5, 6, 7.||||||
4721|Coreena Member|31209|6|Mentioned|p159|||||||||
4721|Coreena Member|31376|6|Mentioned|Table 104|||||||||
4721|Coreena Member|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31430|6|Mentioned|p10|||L.Cretaceous. See also P11||||||
4721|Coreena Member|31432|4|Described|Table 1|||L.Cretaceous||||||
4721|Coreena Member|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|32314|6|Mentioned|Fig. 4|||||||||
4721|Coreena Member|32796|6|Mentioned|p302|||||||||
4721|Coreena Member|32797|4|Described|Table 4|||Lower Cretaceous||||||
4721|Coreena Member|33016|6|Mentioned|p1|||On table||||||
4721|Coreena Member|33017|6|Mentioned|p5|||||||||
4721|Coreena Member|33070|4|Described|Table 2|||L.Cret.||||||
4721|Coreena Member|33071|6|Mentioned|p6|||L.Cret.||||||
4721|Coreena Member|33072|4|Described|Table 1|||||||||
4721|Coreena Member|33075|6|Mentioned|Table 1|||||||||
4721|Coreena Member|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33088|4|Described|Table 3|||Wallumbilla Fm.||||||
4721|Coreena Member|33090|4|Described|Table 4|||L.Cret.||||||
4721|Coreena Member|33091|5|Briefly described|p9|||Stratigraphy||||||
4721|Coreena Member|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
4721|Coreena Member|33182|6|Mentioned|p192|||||||||
4721|Coreena Member|33372|6|Mentioned|p20|||||||||
4721|Coreena Member|33414|6|Mentioned|p212,Tb.||Cretaceous|Part of Wallumbilla Formation.||||||
4721|Coreena Member|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
4721|Coreena Member|33449|4|Described|Table 1|||L.Cret.||||||
4721|Coreena Member|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|33639|5|Briefly described|Table 2|||Wallumbilla Fm. L.Cret.||||||
4721|Coreena Member|33640|4|Described|Table 2|||L.Cret.||||||
4721|Coreena Member|33642|2|Defined|p144|Early Cretaceous|Early Cretaceous|Brief formal definition by Day 1967. Now part of Wallumbilla Formation. Underlain by Doncaster Member and overlain by Allaru Mudstone. Dominantly pelecypod fauna, basal has marine fossils. Lower part is Early Albian, upper part is possibly Middle Albian.||||||08-MAY-13
4721|Coreena Member|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
4721|Coreena Member|34613|4|Described|Table 4|||||||||
4721|Coreena Member|35793|6|Mentioned|Fig.3|||||||||
4721|Coreena Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
4721|Coreena Member|36251|6|Mentioned|Fig.2|||||||||
4721|Coreena Member|36552|6|Mentioned|p61|||||||||
4721|Coreena Member|36571|6|Mentioned|p98|||See also Table 4.||||||
4721|Coreena Member|36581|6|Mentioned|p464|||||||||
4721|Coreena Member|37995|4|Described|p66|||||||||
4721|Coreena Member|38199|6|Mentioned|p426|||||||||
4721|Coreena Member|38226|6|Mentioned|Table 1|||||||||
4721|Coreena Member|38814|6|Mentioned|Table 1|||||||||
4721|Coreena Member|39070|4|Described|p365|||||||||
4721|Coreena Member|39211|5|Briefly described|Fig.3|||Correlation P11. See also Figs 7-9,11-16 etc.||||||
4721|Coreena Member|39212|4|Described|p18|||||||||
4721|Coreena Member|39215|6|Mentioned|p53|||||||||
4721|Coreena Member|39216|6|Mentioned|p56|||||||||
4721|Coreena Member|39478|6|Mentioned|Table 1|||||||||
4721|Coreena Member|39708|6|Mentioned|p478|||||||||
4721|Coreena Member|39847|5|Briefly described|p39|||||||||
4721|Coreena Member|39942|6|Mentioned|p468|||||||||
4721|Coreena Member|39989|4|Described|p424|||||||||
4721|Coreena Member|40199|6|Mentioned|Fig.2|||||||||
4721|Coreena Member|40245|6|Mentioned|Table 2|||||||||
4721|Coreena Member|40249|6|Mentioned|p38|||Mention P41||||||
4721|Coreena Member|40687|3|Fully described|p418|||||||||
4721|Coreena Member|40801|6|Mentioned|p46|||See also P85||||||
4721|Coreena Member|40832|3|Fully described|p457|||||||||
4721|Coreena Member|40833|6|Mentioned|p468|||||||||
4721|Coreena Member|40926|6|Mentioned|Table 2|||||||||
4721|Coreena Member|41012|5|Briefly described|p137|||||||||
4721|Coreena Member|41064|6|Mentioned|p62|||||||||
4721|Coreena Member|41086|3|Fully described|p104, Fig.3|||||||||
4721|Coreena Member|41087|3|Fully described|p126|||||||||
4721|Coreena Member|41088|5|Briefly described|p141|||||||||
4721|Coreena Member|41117|6|Mentioned|Fig.2|||||||||
4721|Coreena Member|41178|6|Mentioned|p242|||||||||
4721|Coreena Member|41198|6|Mentioned|Table 1|||||||||
4721|Coreena Member|41219|6|Mentioned|Fig.4|||||||||
4721|Coreena Member|41266|6|Mentioned|Fig.3|||||||||
4721|Coreena Member|42071|6|Mentioned|p117|||||||||
4721|Coreena Member|42429|5|Briefly described|p155|||||||||
4721|Coreena Member|42494|5|Briefly described|Table 1 P24|||||||||
4721|Coreena Member|42673|5|Briefly described|Fig.2, P184|||||||||
4721|Coreena Member|43008|5|Briefly described|map legend|||of Wallumbilla Formation||||||
4721|Coreena Member|43989|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
4721|Coreena Member|44082|6|Mentioned|p22,Tb.34||Albian|Part of Wallumbilla Formation. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
4721|Coreena Member|44099|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
4721|Coreena Member|44374|14|Not recorded|p10-12||Cretaceous|Contains Aptian and Albian species. Aptian species, remanie (reworked) fossils from Doncaster Member. Basal part in early Albian time. Member of Wilgunya Formation.||||||
4721|Coreena Member|44414|14|Not recorded|p110-112,114||Cretaceous|Cretaceous correlation in Northern Eromanga Basin. Correlated with Ranmoor Member.||||||
4721|Coreena Member|45110|2|Defined|p119|middle Albian|middle Albian|See also Table 18, p24 & 43. Member of Wallumbilla Formation.||||||01-MAY-19
4721|Coreena Member|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
4721|Coreena Member|45145|6|Mentioned|Table 5|||||||||
4721|Coreena Member|46791|4|Described|p44|||||||||
4721|Coreena Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
4721|Coreena Member|46939|6|Mentioned|Fig.1|||||||||
4721|Coreena Member|46984|6|Mentioned|Table 1|||||||||
4721|Coreena Member|48920|3|Fully described|p60|||Lower Cretaceous age||||||
4721|Coreena Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
4721|Coreena Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
4721|Coreena Member|60331|5|Briefly described|p34 Fig.3|Albian|Aptian|Of Wallumbilla Formation. Overlies Doncaster Member. Geological Province: Eromanga Basin.||||||
4721|Coreena Member|61312|5|Briefly described|p64, p67 Fig.E5|Albian|Albian|Of the Wallumbilla Formation. Siltstone and fine sandstone interbedded with mudstone of the Doncaster Member. Geological Province: Eromanga Basin.||||||
4721|Coreena Member|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
4721|Coreena Member|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||Unit in Wallumbilla Formation.||Overlies Doncaster Member.||
4721|Coreena Member|63979|6|Mentioned|p48, Fig. 44|||Of Wallumbilla Formation. Overlies Doncaster Member.||||||07-FEB-11
4721|Coreena Member|64048|6|Mentioned|p72|Early Cretaceous|Early Cretaceous|Of the upper Wallumbilla Formation. Geological Province: Eromanga Basin.||||||07-FEB-11
4721|Coreena Member|64856|3|Fully described|p99-101|Albian|Albian|Named by Vine (1966); defined by Vine et al. (1967) with a type area at Coreena Station near Barcaldine. Top of Wallumbilla Formation, but originally defined in Eromanga Basin. Is overlain by Surat Siltstone. Siltstone with lesser mudstone and minor coal. Associated with palynofloral unit APK4, and in Eromanga Basin APK5 contains dinoflagellate assemblages equivalent to unit ADK19.| | ||||28-NOV-17
4721|Coreena Member|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.||Wallumbilla Formation.||Overlies the Doncaster Member. Underlies the Surat Siltstone||22-MAR-12
4721|Coreena Member|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation? Underlies the Surat Siltstone, overlies the Doncaster Member.||||||
4721|Coreena Member|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||Of Wallumbilla Formation?||||||
4721|Coreena Member|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation. Underlies the Surat Siltstone, overlies the Doncaster Member, Surat Basin||||||
4721|Coreena Member|65119|6|Mentioned|Fig 14 p 521|||Present in the Flinton 1 and MacIntyre 1 wells.||||||07-MAR-12
4721|Coreena Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Wallumbilla Formation.||||
4721|Coreena Member|66623|3|Fully described|p239, p242, pp256-264.|Albian|Aptian|Formerly Tambo Formation (Rose et al. 1967), Oornoo Sandstone (Morton 1982), part of Oornoo Beds (Rose and Brunker 1969). Equivalent to Coorikiana Sandstone (SA) and Ranmoor Member (QLD). Sandy and calcareous units crop out moderately. Contains a very wide range of fossils and intense bioturbation. Matrix cement in sandstones is 40%-50% calcite. Nearshore deposition.||Unit in Wallumbilla Formation.||Gradationally overlies, and is disconformable over, Doncaster Member. Is gradationally overlain by Allaru Mudstone.|Fine- to medium-grained, calcareous and glauconitic, blue-grey (weathering to buff) sandstones; local cone-in-cone calcite and mudstone pebbles; large spherical concretions abundant; fibrous gypsum veins ubiquitous.|07-JUN-13
4721|Coreena Member|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Wallumbilla Formation||||
4721|Coreena Member|67133|5|Briefly described|p17|Early Cretaceous|Early Cretaceous|Shallow lagoon and swamp (regressive) deposits.||Wallumbilla Formation.||Overlies Doncaster Member.||
4721|Coreena Member|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Overlies Doncaster Member.|Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Overlies Doncaster Member of Wollumbilla Formation. Is overlain by Allaru Mudstone.|Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.|||Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|67784|6|Mentioned|p26, p28, p31|Albian|Albian|Age derived from Sr isotopic data. Mis-spelt as Coorena Member on p31.||Walumbilla Formation||Overlies Doncaster Member. Is overlain by Toolebuc Formation.||08-FEB-18
4721|Coreena Member|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Doncaster Member. Is overlain by Winton Formation.||
4721|Coreena Member|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shallow marine environment. Shown on cross-sections and time-space plot and basement interpretation only.||Unit in Wallumbilla Formation.||Conformably overlies Doncaster Member.|Siltstone interbedded with mudstone and minor, very fine- to fine-grained lithic sandstone and thin coal seams.|
4721|Coreena Member|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||||
4721|Coreena Member|68206|6|Mentioned|p32|Albian|Albian|NE Eromanga Basin.||||||
4721|Coreena Member|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Surat Siltstone.||
4721|Coreena Member|68593|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Surat Siltstone.|Siltstone interbedded with mudstone and minor, very fine- to fine-grained lithic sandstone. Thin coal seams in places.|
4721|Coreena Member|68734|5|Briefly described|p218 Fig.2|Albian|Aptian|Eromanga Basin (NE). Marine to coastal paralic.||Of the Wallumbilla Formation.||||
4721|Coreena Member|69457|5|Briefly described|p41:3, 10|Early Cretaceous|Early Cretaceous|Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
4721|Coreena Member|69594|5|Briefly described|p519, p526, p528, p538, p550|Albian|Aptian|Eastern Eromanga, northern Surat Basins. Deposited during regression in shallow-marine coastal mudflats, lagoons and swamps. Modest fossil fauna.||Wallumbilla Formation.||Conformably overlies Doncaster Member. Is overlain by Toolebuc Formation and (conformably) the Surat Siltstone. Laterally equivalent to Ranmoor Member. Correlated with Styx Coal Measures.|Mudstone, siltstone, sandstone, minor coquinite, interbedded calcareous units and intraformational conglomerates.|
4721|Coreena Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||Wallumbilla Formation||Overlies Doncaster Member||
4721|Coreena Member|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||Unit in Wallumbilla Formation.||||
4721|Coreena Member|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Wallumbilla Formation|Includes un-named unit.||Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions. Un-named unit is grey to pale brown cone-in-cone limestone and calcareous mudstone.|
4721|Coreena Member|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.||Wallumbilla Formation|||Fine-grained calcareous labile and sub-labile sandstone, clayey sandstone, sandy siltstone; cone-in-cone structures and spheroidal calcareous concretions.|
4721|Coreena Member|70720|6|Mentioned|p6|||Eromanga Basin.||||Overlies Doncaster Member. Is overlain by Winton Formation.||
4721|Coreena Member|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p31, p33, p72|Early Cretaceous|Early Cretaceous|See also p79-80, p82, p85-89, p115-116. Eromanga and Surat Basins. Varying thicknesses given (30-123m) from wells. Middle to Late Albian age. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Hydrochemistry mentioned, hydrostratigraphic properties.||Wallumbilla Formation.||Conformably overlies Doncaster Member. Is overlain by Toolebuc Formation or Surat Siltstone. Equivalent to upper Bulldog Shale.|Labile sandstone, siltstone and mudstone, locally calcareous; locally coquinite.|
4721|Coreena Member|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Albian.||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Surat Siltstone.||
4721|Coreena Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
4721|Coreena Member|71251|5|Briefly described|p11-12, p15, p17, p49, p51|||Eromanga Basin. Natural gamma wireline log. Conductivity diagram.||Wallumbilla Formation.||Overlies Doncaster Member. Is overlain by Winton Formation.||
4721|Coreena Member|71863|5|Briefly described|p5|Albian|Aptian|Eromanga Basin.||Wallumbilla Formation||Overlies the Doncaster Member. Overlain by the Toolebuc Formation.||
4721|Coreena Member|71864|6|Mentioned|p13-p14, p17|||Could not be distinguished in GSQ Eulo 2 borehole.||Wallumbilla Formation||||
4721|Coreena Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||Wallumbilla FZ.||Overlies Doncaster Member. Is overlain by Toolebuc FZ.||
4735|Corner Limestone Member|23214|4|Described|p39|Eastonian|Eastonian|Of Ballingoole Limestone. Typically massive limestone. Max. thickness 120m. Overlain by Clearview Limestone Member.||||||26-MAY-08
4735|Corner Limestone Member|33063|2|Defined|p83|Ordovician|Ordovician|||||||
4735|Corner Limestone Member|33740|6|Mentioned|Fig.1|||||||||
4735|Corner Limestone Member|38219|6|Mentioned|Table 2|||||||||
4735|Corner Limestone Member|40136|5|Briefly described|p16|||See also p22.||||||26-MAY-08
4735|Corner Limestone Member|41046|6|Mentioned|Fig.2|||||||||
4735|Corner Limestone Member|70684|5|Briefly described|p39 Fig.17|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Ballingoole Limestone.||||
4751|Corringle Formation|22857|5|Briefly described|p446 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Part of Ootha Formation? Fine sedimentary breccia. Max. thickness: 100m. ||||||
4751|Corringle Formation|35503|2|Defined|p206|Silurian|Silurian|New name refs Kemezys (1976)Prob. Silurian||||||
4751|Corringle Formation|40328|5|Briefly described|p38|||||||||
4755|Corryong Granite|23309|5|Briefly described|p338, 346||Silurian|G92 - S-Type.  Age: 404 Ma, 429 Ma, 421+/-3 Ma.||||||
4755|Corryong Granite|24133|3|Fully described|p59|Silurian|Silurian|Age: 421+/-3Ma.  Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
4755|Corryong Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Two-mica cordierite granite: grey, medium to very course grained; equigranular to strongly porphyritic in K-feldspar; locally contains sillimanite or andalusite.||||||09-SEP-04
4755|Corryong Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Age: 421 +/- 3 Ma (K/Ar). Biotite-muscovite-cordierite granite: S-type, nonmagnetic; high K, high Th, moderate to high U.||||||09-SEP-04
4755|Corryong Granite|24551|6|Mentioned|p445, 464|||S-Type||||||
4755|Corryong Granite|29860|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
4755|Corryong Granite|29953|4|Described|p3|||||||||
4755|Corryong Granite|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
4755|Corryong Granite|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
4755|Corryong Granite|31800|5|Briefly described|p207|||||||||
4755|Corryong Granite|33004|6|Mentioned|p167|||||||||
4755|Corryong Granite|33874|5|Briefly described|p6|||||||||
4755|Corryong Granite|34544|6|Mentioned|p183|||||||||
4755|Corryong Granite|35278|4|Described|p358|||||||||
4755|Corryong Granite|37029|6|Mentioned|p48|||||||||
4755|Corryong Granite|37529|6|Mentioned|Fig.1|||||||||
4755|Corryong Granite|38367|5|Briefly described|p153|Silurian|Silurian|Age: 430m.y. Grey granite.||||||16-DEC-08
4755|Corryong Granite|38782|6|Mentioned|p43|||||||||
4755|Corryong Granite|39291|6|Mentioned|Fig.20|||||||||
4755|Corryong Granite|39331|5|Briefly described|p27|||||||||
4755|Corryong Granite|39860|5|Briefly described|p17|||See also p22.||||||26-MAY-08
4755|Corryong Granite|40328|6|Mentioned|p204|||||||||
4755|Corryong Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
4755|Corryong Granite|40498|6|Mentioned|p364|||||||||
4755|Corryong Granite|41572|6|Mentioned|p19|||||||||
4755|Corryong Granite|41868|6|Mentioned|p569|||||||||
4755|Corryong Granite|42089|6|Mentioned|p19|||||||||
4755|Corryong Granite|42726|5|Briefly described|map legend|Silurian||||||||
4755|Corryong Granite|42827|5|Briefly described|p19|||||||||
4755|Corryong Granite|44184|5|Briefly described|Map Legend||Early Silurian|||||||
4755|Corryong Granite|45087|5|Briefly described|p27|||Chem. analyses.||||||
4755|Corryong Granite|50542|6|Mentioned|p91, p96|Silurian|Silurian|||||||07-FEB-11
4755|Corryong Granite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
4755|Corryong Granite|64571|6|Mentioned|p825|Early Silurian|Early Silurian|||||||
4755|Corryong Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Two-mica cordierite granite: grey, medium to very coarse grained; equigranular to strongly porphyritic in K-feldspar; locally contains sillimanite or andalusite; S-type.|
4755|Corryong Granite|70910|6|Mentioned|p47|||Example of gneissic granite p43.||||||
4789|Covan Creek Formation|22768|6|Mentioned|p176-77||Early Devonian|||||||
4789|Covan Creek Formation|22857|4|Described|p176, p472 App.1 Tb.A1.6|Early Devonian|Pridolian|Of the Mount Fairy Group. Max. thickness: 1200m. Geological Province: Captains Flat-Goulburn Trough.||||||
4789|Covan Creek Formation|23048|5|Briefly described|p7 fig9|||||||||
4789|Covan Creek Formation|24317|5|Briefly described|p14|Late Silurian|Late Silurian|Of Mount Fairy Group.||||||
4789|Covan Creek Formation|24318|6|Mentioned|p19|||||||||
4789|Covan Creek Formation|30730|4|Described|p8|||||||||
4789|Covan Creek Formation|30735|2|Defined|p25|Silurian|Silurian|||||||
4789|Covan Creek Formation|30736|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
4789|Covan Creek Formation|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
4789|Covan Creek Formation|35503|6|Mentioned|p201|||Defined in Felton and Huleatt (1977)||||||
4789|Covan Creek Formation|35662|6|Mentioned|p139|||Geology of the Woodlawn district.||||||
4789|Covan Creek Formation|36413|6|Mentioned|Table 3|||||||||
4789|Covan Creek Formation|39331|6|Mentioned|p56|||See p57.||||||07-SEP-15
4789|Covan Creek Formation|40276|6|Mentioned|p3|||Mention p33.||||||07-SEP-15
4789|Covan Creek Formation|40328|4|Described|p184|||||||||
4789|Covan Creek Formation|41140|6|Mentioned|p143|||||||||
4789|Covan Creek Formation|41742|5|Briefly described|p337|||||||||
4789|Covan Creek Formation|42727|5|Briefly described|map legend|Pridoli|Pridoli|Of Mount Fairy Group. Sandstone, siltstone and shale (proximal quartz turbidites). Overlies Currawang Basalt; unconformably overlies Birkenburn beds. BMR map symbol: Sua. Geol. Prov: Rocky Pic Block.||||||
4789|Covan Creek Formation|42820|3|Fully described|p55|||Of Mount Fairy Group.||||||26-MAY-08
4789|Covan Creek Formation|50232|4|Described|Map legend|Ludlow|Ludlow|Of the Mount Fairy Group.  Overlies Woodlawn Volcanics and Currawang Basalt.||||||
4789|Covan Creek Formation|50234|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Mount Fairy Group.  Overlies: Currawang Basalt, Woodlawn Volcanics, Joppa Formation, Sooley Volcanics.  Underlies: Boxers Creek Formation.||||||
4789|Covan Creek Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group.  Massive to graded, medium- to coarse-grained well-sorted lithic-quartz to quartzose sandstone with variable percentage clay-rich matrix, quarzite, thinly-bedded to laminated fine-grained sandstone, siltstone, mudstone and shale.||||||09-SEP-08
4789|Covan Creek Formation|66087|5|Briefly described|p3 Fig. 2|Early Devonian|Silurian|||Of the Mount Fairy Group.||||10-MAY-12
4789|Covan Creek Formation|67820|5|Briefly described|p133, p136 Fig.3|Late Silurian|Late Silurian|||Mount Fairy Group.|||Quartz-lithic sandstone and siltstone.|
4789|Covan Creek Formation|68592|2|Defined|p815-22, p827, p834, p843, p852 Fig.143|Lochkovian|Ludlow|See also p228, p298, p726, p728-31, p758, p761, p778, p792-7, p802, p804, p808, p813, p855-6, p873-4, p883, p888-90, p1665. Felton 1974. Revised in Felton and Huleatt (1977). Current definition of Covan Creek Formation incorporates Covan Creek Formation in the sense of Felton and Huleatt (1977), part of Towrang Beds (Felton 1974), Towrang Formation (Jones et al. 1995) and 'Wollondilly beds' (O'Reilly 1972). Geomorphic expression: ridge forming. Quarried for quartzite at Barina quarry, near Collector, and currently for structural clay/shale and kaolin E of Goulburn. Graptolitic siltstone and shale of uppermost De Drack Formation and Kerrawary Siltstone occupy same stratigraphic position directly beneath Covan Creek Formation. Type section: on Braidwood 1:100 000 - only ~800 m of stratigraphy is preserved. Representative section: occurs in several road cuttings. Max thickness: ~1500 m. Sediments sources discussed. Structure: regional-scale overturned folds (~20 km wavelength) with small parasitic folds throughout. Regional metamorphism: sub-greenschist to lower greenschist facies. No unequivocal, age-diagnostic fossils; age constraints come from fossils in underlying and overlying units. Age: possibly late Ludlow to earliest Lochkovian. Is intruded by Komungla Rhyolite Member, Forest Lodge Quartz Monzodiorite, Lockyersleigh Granite. Is faulted against Kerrawary Siltstone, Longreach Volcanics. Argyle, Covan Creek and Carwoola Formations are probable correlatives. Classification and provenance plots. Hosts massive magnetite-garnet-rich mineralisation E of Inveralochy.||Unit in Mount Fairy Group.||Overlies Kerrawary Siltstone, Joppa Siltstone Member, Woodlawn Volcanics, Currawang Basalt (conf.). Overlain by Boxers Creek, Kowmung, Rhyanna Formations (conf.), and by Gundary Volcanics (unconf.).|Thin- to very thick-bedded, lithic-quartz to quartzose sandstone often containing black shale and chert lithics, with interbedded, laminated, pale-grey to buff, commonly bioturbated siltstone and mudstone; rare rhyolitic volcanic breccia.|
4789|Covan Creek Formation|69159|5|Briefly described|Map legend|Pridoli|Ludlow|||Unit in Mount Fairy Group.|||Massive to graded, medium- to coarse-grained, well-sorted, lithic-quartz to quartzose sandstone and quartzite, interbedded with thinly-bedded to laminated fine-grained sandstone, siltstone and mudstone.|07-SEP-15
4789|Covan Creek Formation|69635|5|Briefly described|p11|||||Of Mount Fairy Group. ||Correlated with Carwoola Formation.||
4789|Covan Creek Formation|70192|5|Briefly described|Map Legend|Lochkovian|Pridoli|Sfo. Includes one unnamed unit of rhyolitic volcanic breccia with pumiceous and perlitic clasts. On Gunning, Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot. Related Units continued: Overlies Woodlawn Volcanics, Kerrawary Siltstone, Joppa Siltstone Member and De Drack Formation.||Mount Fairy Group|Includes one unnamed unit.|Is overlain by Boxers Creek Formation, Kowmung Formation and Covan Creek Formation. Interleaves with Arglye Formation.Interleaves with, and overlies, Cobra Formation and Currawang Basalt. See comments|Thin-thick bedded, very fine-very coarse grained, lithic quartz-quartzose sandstone with interbedded, laminated, siltstone and mudstone.Rare felsic volcanic rocks; sandstone typically contains fragments of dark chert and fine grained metasediments.|
4789|Covan Creek Formation|70541|4|Described|Map Legend|Devonian|Silurian|Includes one unnamed mapped member of rhyolitic breccia with pumiceous and perlitic clasts; coarsely grained quartz-andesine-phyric dacite with spherulitic quartz-K feldspar groundmass.||Mount Fairy Group|Includes an unnamed member.||Thin to thickly bedded, very fine to coarse grained lithic quartz sandstone with interbedded, laminated, siltstone and mudstone; very rare felsic volcanic rocks; sandstone typically contains fragments of chert and fine grained metasedimentary rock.|
4789|Covan Creek Formation|70542|5|Briefly described|Map Legend|Devonian|Silurian|Contains one unnamed mapped member of rhyolitic breccia with pumiceous and perlitic clasts; coarsely grained quartz-andesine-phyric dacite with spherulitic quartz-K feldspar groundmass.||Mount Fairy Group|||Thin to thickly-bedded, very fine to coarse-grained lithic quartz sandstone interbedded with laminated siltstone and mudstone; very rare felsic volcanic rocks; sandstone typically contains fragments of chert and fine grained metasedimentary rock.|
4789|Covan Creek Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|||Thin-thick bedded, very fine-very coarse grained, lithic quartz-quartzose sandstone with interbedded, laminated, siltstone and mudstone.Rare felsic volcanic rocks; sandstone typically contains fragments of dark chert and fine grained metasediments.|
4789|Covan Creek Formation|71069|3|Fully described|p9, p21 fig 7, p27, p30, p38 fig 15|Ludlow|Ludlow|Named for the Covan Creek property. Originally mapped as a combination of Towrang Beds and De Drack Formation; also mapped as Towrnag Formaton, Wollondilly beds or Birkenburn Beds. Goulburn Basin. Type section given from GR 739613 6115284 to GR 738713 6115184; representative section also mentioned. Hosts numerous skarn related deposits (the Ryans, Astrids and Terry Hie prospects). Forms prominent ridges in the map area.  Estimated to range from 70m to 1500m thick. Deposited in a deep marine setting below storm wave base.Distribution, geomorphology, geophysical characteristics, tectonic structure, primary structures/textures and metamorphism discussed.Overlain by the Boxers Creek Formation, Rhyanna Formation and Kowmung Formation. Unconformably overlain by the Gundary Volcanics. Lateral equivalent of the Sinclair Conglomerate Member. Equivalent to the Carwoola Formation. Intruded by the Komungla Rhyolite Member. See also p40 fig 17, p41, p50 tbl 3, p118, p120, p123, p133, p135, p136 fig 44, p139 fig 45, p142, p144, p145, p149, p151, p154, p156, p159, p162-p164, p168-173||Mount Fairy Group||Conformably overlies the Currawang Basalt, Kerrawary Siltstone, Woodlawn Volcanics and the De Drack Formation. Overlies the Adaminaby, Bendoc and Margules Groups. Conformably.|Massive to graded, medium to coarse grained, lithic-quartz to quartzose, planar and ripple cross laminated sandstone, siltstone and mudstone turbidite package. Rare conglomerate and felsic volcanic rocks also occur.|
4789|Covan Creek Formation|71656|6|Mentioned|p13 Fig.2, p30|Silurian|Silurian|Unfossiliferous strata.||Mount Fairy Group||Overlies De Drack Formation, partially overlying Kerrawary Siltstone. Underlies Boxers Creek Formation.|Unfossiliferous strata.|
4789|Covan Creek Formation|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Mount Fairy Group.||Overlies Currawang Basalt and De Drack Formation.|Massive to graded, medium- to coarse-grained, well-sorted, lithic-quartz to quartzose ssndstone and quartzite interbedded with thin-bedded to laminated fine-grained sandstone, siltstone and mudstone.|
4789|Covan Creek Formation|71699|5|Briefly described|Map legend.|Devonian|Silurian|||Mount Fairy Group.||Overlies Currawang Basalt and De Drack Formation. Is overlain by Boxers Creek Formation.|Massive to graded, medium- to coarse-grained, well-sorted, lithic-quartz to quartzose sandstone and quartzite, interbedded with thinly bedded to laminated fine-grained sandstone, siltstone and mudstone.|
4789|Covan Creek Formation|71700|2|Defined|vi, p7, p14-p16, p41|Pridoli|Ludlow|Named for the Covan Creek property in Goulburn100. The type section occurs in a creek from GR 739613 6115284 to GR 738713 6115184 (Felton and Huleatt 1977). A representative section occurs from GR 737200 6135920 to 738540 6136060. Previously informal and also a combination of Towrang Beds, De Drack Formation and undifferentiated rocks before being named by Felton and Huleatt 1977. Thomas and Pogson (2012) expanded the original definition to incorporate parts of the Towrang Beds, Towrang Formation, Wollondilly beds, Birkenburn Beds and parts of De Drack Formation. Contains an unnamed informal constituent. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geophysical characteristics, fossils and distinguishing features are discussed. Considered equivalent to the Argyle Formation and the Carwoola Formation. Together with the Boxers Creek Formation forms a 3km thick turbidite package. Age is derived from fossil assemblages of the overlying and underlying formations. See also p48-p51, p57-p60, p63, p76, p86, CD.||Mount Fairy Group||Conformably overlies De Drack Formation, Woodlawn Volcanics and the Currawang Basalt. Conformably overlain by the Boxers Creek Formation. Unconformably overlain by the Mulwaree Group.|Thin- to very thick-bedded lithic quartz to quartzose sandstone with interbedded laminated pale grey to buff siltstone and mudstone.|
4811|Cowra Granodiorite|13139|5|Briefly described|p9 Fig. 4, p11|Silurian|Silurian|Geological Province: Cowra Trough.||||||
4811|Cowra Granodiorite|22778|6|Mentioned|p 162|||||||||
4811|Cowra Granodiorite|23214|3|Fully described|p116|Late Silurian|Late Silurian|Originally included as part of the Young Granodiorite. Intrudes the Avoca Valley Shale and Canowindra Volcanics.||||||24-AUG-04
4811|Cowra Granodiorite|24417|5|Briefly described|p164|||Not related to "Cowra Formation".||||||
4811|Cowra Granodiorite|29452|4|Described|p218|||||||||
4811|Cowra Granodiorite|29682|6|Mentioned|p14|||||||||
4811|Cowra Granodiorite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
4811|Cowra Granodiorite|33006|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Prob.Middle Devonian||||||
4811|Cowra Granodiorite|33282|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
4811|Cowra Granodiorite|33285|6|Mentioned|p21|||||||||
4811|Cowra Granodiorite|34404|6|Mentioned|Fig.3.3b|||||||||
4811|Cowra Granodiorite|34544|4|Described|p188|||||||||
4811|Cowra Granodiorite|38823|5|Briefly described|p204|||||||||
4811|Cowra Granodiorite|39240|5|Briefly described|p80|||||||||
4811|Cowra Granodiorite|39655|6|Mentioned|Plate 1|||||||||
4811|Cowra Granodiorite|40328|4|Described|p205|||||||||
4811|Cowra Granodiorite|43158|4|Described|Fig1p2; p5,9-13|||||||||
4811|Cowra Granodiorite|43202|5|Briefly described|Table 2,p20.|||||||||
4811|Cowra Granodiorite|43515|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
4811|Cowra Granodiorite|43516|14|Not recorded|Map Legend||Middle Devonian|||||||
4811|Cowra Granodiorite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Consists of mafic granet cordierite granodiorite, abundant enclaves.||||||15-JUL-08
4811|Cowra Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|||||||
4811|Cowra Granodiorite|63288|6|Mentioned|p354 Fig. 1|||||||||
4811|Cowra Granodiorite|63290|6|Mentioned|p405, p407, p406 Fig. 7|||Intrudes Canowindra Volcanics (Ryall 1966). Comagmatic S-type.||||||
4811|Cowra Granodiorite|67847|5|Briefly described|p32-p33|Ludlow|Wenlock|Age constrained on the basis of ages for units which are intruded by this granodioirte. ||||||
4811|Cowra Granodiorite|68310|5|Briefly described|p235-240, 244|||A N-S elongate intrusion of 72 km2. Chemical analyses tabulated. Likely the intrusive (subvolcanic) equivalent of Canowindra Volcanics. Enclaves described in detail. Chemical analyses of schistose enclaves, and primary microgranular enclaves, tabulated.|428.5 Ma (U-Pb zircon; Ickert and Williams, 2011)|Bullenbalong Supersuite.|||Medium- to coarse-grained, garnet-cordierite granodiorite. S-type.|
4811|Cowra Granodiorite|68592|3|Fully described|p1229-32, p1234, p1246|Late Silurian|Late Silurian|Described by Stevens (1951, 1952). Ashley and Basden (1973), and Basden et al. (1978) included this unit in their Young Granodiorite; now regarded as a separate body (Chappell et al., 1991; Pogson and Watkins, 1998). Type pluton for Cowra Suite. Peraluminous: geochemistry detailed. Probably comagmatic with Canowindra Volcanics. Very low magnetic susceptibility.||Unit in Cowra Suite.||Intrudes Canowindra Volcanics.|Grey, medium to coarse-grained, equigranular, biotite-cordierite granodiorite; characteristically contains a wide range of enclaves and large fragments of milky quartz. Large garnets rimmed by cordierite are sparse but characteristic. S-type.|
4811|Cowra Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|||Bullenbalong Supersuite||||
4811|Cowra Granodiorite|73264|5|Briefly described|p1392, p1393 Fig.15, p1407|Silurian|Silurian|Lachlan Orogen, eastern. Mafic S-type granitoid. Zircon ages in granite and metasedimentary enclave define a 430-610 Ma population.|~425 Ma||||Granitoid, rich in microgranitoid enclaves.|
4811|Cowra Granodiorite|73431|6|Mentioned|p365-366, p372, p373 Fig.8, p374|Silurian|Silurian|Lachlan Orogen. S-type granite with abundant zircon xenocrysts.||||||
4813|Cowridge Siltstone|13996|6|Mentioned|p142|Silurian|Silurian|Yass area. Bivalve taxa distribution Table.||||||
4813|Cowridge Siltstone|22639|5|Briefly described|p267 Fig.2|Late Silurian|Late Silurian|||||||
4813|Cowridge Siltstone|22857|4|Described|p458 App.1, Tb.A1.6|Late Silurian|Late Silurian|Of the Barambogie Group. Siltstone, fine sandstone, mudstone; contains graptolites, brachiopods, trilobites. Max. thickness: >140m. Geological Province: Canberra-Yass Shelf.||||||
4813|Cowridge Siltstone|23522|5|Briefly described|p248 Fig 4|Pridoli|Ludlow|||||||
4813|Cowridge Siltstone|24248|5|Briefly described|p50 Fig.1, p52|Pridoli|Pridoli|Conformably overlies the Rosebank Shale. Overlain by the Elmside Formation.||||||
4813|Cowridge Siltstone|24249|5|Briefly described|p90 Fig.3, p91|Pridoli|Pridoli|Overlain by Elmside Formation. Underlain by Rosebank Shale.||||||12-JUN-08
4813|Cowridge Siltstone|30069|6|Mentioned|p5|||||||||
4813|Cowridge Siltstone|31852|6|Mentioned|p711|||Correlation on P712-714 & Figs. 1,2,4,5. Silurian||||||
4813|Cowridge Siltstone|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Nomenclature||||||
4813|Cowridge Siltstone|32820|6|Mentioned|p5|||||||||
4813|Cowridge Siltstone|33116|6|Mentioned|Fig.11|||||||||
4813|Cowridge Siltstone|33325|5|Briefly described|Table 2|||See also Table 3.||||||
4813|Cowridge Siltstone|33326|6|Mentioned|p441|||Fauna. Pridolian.||||||
4813|Cowridge Siltstone|35384|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
4813|Cowridge Siltstone|35386|3|Fully described|p38|||||||||
4813|Cowridge Siltstone|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
4813|Cowridge Siltstone|36413|6|Mentioned|Table 3|||||||||
4813|Cowridge Siltstone|37727|5|Briefly described|p51|||See also P6 and P51.||||||
4813|Cowridge Siltstone|38151|6|Mentioned|Table 1|||||||||
4813|Cowridge Siltstone|39331|6|Mentioned|Fig.5-3|||See Fig.5-5||||||
4813|Cowridge Siltstone|40328|3|Fully described|p48|||||||||13-JAN-17
4813|Cowridge Siltstone|42029|5|Briefly described|Fig.1 P96|||||||||
4813|Cowridge Siltstone|43575|6|Mentioned|Fig.2,p267||Late Silurian|||||||
4813|Cowridge Siltstone|45075|5|Briefly described|p8|||||||||
4813|Cowridge Siltstone|47037|6|Mentioned|p107|||||||||
4813|Cowridge Siltstone|50230|4|Described|Map legend|Pridoli|Pridoli|Of the Hattons Corner Group.  Interbedded siltstone, fine-grained sandstone, mudstone.||||||
4813|Cowridge Siltstone|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hattons Corner Group. Interbedded siltstone, fine-grained sandstone, mudstone. Also includes an upper and lower mudstone subunit.||||||12-JUN-08
4813|Cowridge Siltstone|67820|6|Mentioned|p136 Fig.3|Silurian|Silurian|||Hattons Corner Group.||||
4813|Cowridge Siltstone|68592|2|Defined|p340 Fig.89, p560-3, p598-601, p1884|Pridoli|Pridoli|Named after Cowridge property. Link (1970, 1971); Link and Druce (1972); unit in their Barambogie Group. Here included in redefined Hattons Corner Group. "Incomplete" type section described. 85-155m thick. Early to late Pridoli graptolites, and other fauna, listed.||Unit in Hattons Corner Group.||Conformably overlies Rosebank Shale. Is overlain gradationally by Elmside Formation.|Two cycles of turbidites: a siltstone-dominated sequence overlain by mudstone.|13-JAN-17
4813|Cowridge Siltstone|70192|5|Briefly described|Map Legend|Pridoli|Pridoli|Shc. Includes two unnamed members of massive to finely laminated mudstone with minor graded siltstone/fine grained sandstone interbeds. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hattons Corner Group|Includes two unnamed members.|Is overlain by Elmside Formation. Overlies Rosebank Shale.|Thin-medium bedded, graded siltstone to very fine grained sandstone interbedded with grey mudstone.|
4813|Cowridge Siltstone|70540|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed members of massive to finely laminated mudstone with minor graded siltstone/fine grained sandstone interbeds.||Hattons Corner Group|Includes two unnamed members.||Thin-medium bedded, graded siltstone to very fine grained sandstone interbedded with grey mudstone.|
4813|Cowridge Siltstone|70546|5|Briefly described|Map Legend|Devonian|Silurian|Includes two unnamed members of massive to finely laminated mudstone with minor graded siltstone or fine grained sandstone interbeds.||Hattons Corner Group|||Thin to medium bedded, graded siltstone to very fine grained sandstone interbedded with mudstone.|
4813|Cowridge Siltstone|71656|6|Mentioned|p12 Fig.2 , p19|Pridoli|Pridoli|Fauna including graptolites, brachiopods and a gastropod found. Contains Ludlovian to Pridolian graptolites.||Hattons Corner Group||Overlies Rosebank Shale and underlies Elmside Formation.||
4822|Coxs River Gabbro|42726|5|Briefly described|map legend|Carboniferous||30. Variation on Coxs River Granite.||||||
4846|Cranebrook Formation|31056|4|Described|p6|||||||||
4846|Cranebrook Formation|33671|6|Mentioned|p8|||||||||
4846|Cranebrook Formation|35098|4|Described|p5|||||||||
4846|Cranebrook Formation|35312|6|Mentioned|p8|||||||||
4846|Cranebrook Formation|39308|6|Mentioned|p496|||||||||
4846|Cranebrook Formation|41391|6|Mentioned|p49|||||||||
4846|Cranebrook Formation|41939|5|Briefly described|p24|||||||||
4846|Cranebrook Formation|42925|2|Defined|p43||Pleistocene|||||||
4846|Cranebrook Formation|42926|4|Described|map legend|Holocene|Pleistocene|||||||
4846|Cranebrook Formation|65195|6|Mentioned|p4 Fig.2, p7 & 14 Fig.4, p22 & 29 Fig.9|Quarternary|Quarternary|Overlies Agnes Banks Sands||||||
4847|Cranky Corner Sandstone|22857|5|Briefly described|p536 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Green massive fine to medium-grained sandstone. Max. thickness: 70m.||||||24-MAR-06
4847|Cranky Corner Sandstone|23350|5|Briefly described|262|||||||||
4847|Cranky Corner Sandstone|23540|5|Briefly described|p 420|||Age: 284.1+/-2.2Ma (SHRIMP). Also see p417.||||||
4847|Cranky Corner Sandstone|32094|6|Mentioned|p383|||||||||
4847|Cranky Corner Sandstone|32097|6|Mentioned|p231|||Occurrence of Martiniopsis konicki||||||
4847|Cranky Corner Sandstone|32950|6|Mentioned|Table 31.1|||||||||
4847|Cranky Corner Sandstone|35284|6|Mentioned|p37|||||||||
4847|Cranky Corner Sandstone|35862|6|Mentioned|p274|||||||||
4847|Cranky Corner Sandstone|36042|6|Mentioned|Fig.11|||||||||
4847|Cranky Corner Sandstone|39288|6|Mentioned|p57|||||||||
4847|Cranky Corner Sandstone|39304|6|Mentioned|Fig. 19.2|||||||||
4847|Cranky Corner Sandstone|46849|6|Mentioned|p195|||||||||
4847|Cranky Corner Sandstone|60289|5|Briefly described|p2 Fig. 2|Early Permian|Early Permian|Of Dalwood Group. Overlies Beckers Formation. Underlies Billy Brook Formation. Geological Province: Cranky Corner Basin.||||||
4847|Cranky Corner Sandstone|60290|3|Fully described|p15, 26, 43|Early Permian|Early Permian|Of Dalwood Gp. Thick: 51 m. Overlies Beckers Fm. Overlain by Billy Brooks Fm. Laterally equivalent to Allandale Fm. Grey-green to grey, very fine to medium grained upwards coarsening fossiliferous sst, minor siltst. G.P: Cranky Corner Basin.||||||07-FEB-11
4847|Cranky Corner Sandstone|60291|4|Described|p51, 53 Tb.1|Early Permain|Early Permain|Of Dalwood Group. Green sandstone, siltstone. Coarsens upwards. Fossiliferous. Lower to upper shoreface. Geological Province: Cranky Corner Basin. Petrology descirbed.||||||
4847|Cranky Corner Sandstone|60292|4|Described|p65|Early Permian|Early Permian|Overlies Beckers Formation. Overlain by Billy Brook Formation. Geological Province: Cranky Corner Basin. Petrography and geochemistry described.||||||
4847|Cranky Corner Sandstone|60293|5|Briefly described|p108 Fig.1|||Overlies Beckers Formation. Overlain by Billy Brook Formation. Vitrinite reflectance of organic matter described.||||||
4847|Cranky Corner Sandstone|60294|5|Briefly described|p116 FIg.1|Early Permian|Early Permian|Overlies Beckers Formation. Overlain by Billy Brook Formation. Geological Province: Cranky Corner Basin.||||||
4847|Cranky Corner Sandstone|60295|4|Described|p127, p133 Fig.9|Sakmarian|Sakmarian|Of the Dalwood Group. Overlies the Beckers Formation. Overlain by Billy Brook Formation. Near shore shallow deposition with restricted circulation indicated by plant microfossils. Age: Paly zones APP21, APP22 - Sakmarian. Geological Province: Cranky Corner Basin.||||||19-SEP-18
4847|Cranky Corner Sandstone|60296|5|Briefly described|p155, p156 Fig.1|Sakmarian|Sakmarian|Of the Dalwood Group. Correlated with Allandale Formation, lower Pebbley Beach Formation, Bundella Formation, Callytharra Formation and Golden Valley Group. Geological Province: Cranky Corner Basin.||||||18-MAY-05
4847|Cranky Corner Sandstone|60297|5|Briefly described|p167|Permian|Permian|Of the Dalwood Group. Geological Province: Cranky Corner Basin||||||
4847|Cranky Corner Sandstone|60298|5|Briefly described|p180, 189|Sakmarian|Asselian|Age: 284.1+/-2.2 Ma (SHRIMP zircon U-Pb) from tuffaceous unit. inherited zircons (from Mount Durham Tuf Member?) gave age of 308.4 +/-3.7 Ma. Fossiliferous sandstone.||||||19-SEP-18
4847|Cranky Corner Sandstone|60299|5|Briefly described|p218|||Palaeomagnetism measured||||||
4847|Cranky Corner Sandstone|60300|5|Briefly described|p242 Tb.1|Early Permian|Early Permian|Of the Dalwood Group. Overlies Beckers Formation. Overlain by Billy Brook Formation. Fossiliferous sandstone.||||||30-JUN-05
4847|Cranky Corner Sandstone|63832|5|Briefly described|p131 fig 2|Artinskian|Sakmarian|Cranky Corner/Gresford block, Southern New England Fold Belt. Sixth (P2) glaciation.||Unit in Dalwood Group.||||13-DEC-17
4847|Cranky Corner Sandstone|64631|5|Briefly described|p44 Fig.2.|Sakmarian|Sakmarian|Southern New England Fold Belt, Cranky Corner/Gresford Block. Biostratigraphic and radiometric age control near boundaries.||Unit in Dalwood Group.||Overlies Beckers Sandstone. Is overlain by Billy Brook Formation.||
4847|Cranky Corner Sandstone|68493|5|Briefly described|p10, p10 Fig.4|Sakmarian|Sakmarian|Cranky Corner Basin. Rich in Eurydesma and Keeneia fossil fauna.||||Correlative of the Allandale Formation in the Sydney Basin.||
4847|Cranky Corner Sandstone|69793|6|Mentioned|p1121 Fig.12|Sakmarian|Sakmarian|Gresford Block, Tamworth Belt.||||||
4847|Cranky Corner Sandstone|70096|5|Briefly described|p220-221;Supp1-2|Artinskian|Artinskian|Of northern Sydney Basin. SHRIMP U-Pb age of 281+\-2.2 Ma. See also supplementary files in appendix for additional stratigraphic and locality information.||||Overlain by Billy Creek Formation. Underlain by Beckers Formation.||
4869|Crawney Limestone Member|22857|5|Briefly described|p482 App.1 Tb.A1.6|Givetian|Givetian|Of the Yarrimie Formation (Tamworth Group). Coralline biohermal limestone. Max. thickness: 116m. Geological Province: Tamworth Forearc Basin. ||||||
4869|Crawney Limestone Member|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
4869|Crawney Limestone Member|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
4869|Crawney Limestone Member|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
4869|Crawney Limestone Member|34554|6|Mentioned|p234|||Fauna||||||
4869|Crawney Limestone Member|40867|6|Mentioned|Fig.1|||||||||
4869|Crawney Limestone Member|43400|2|Defined|p178,179,180,map||Givetian|Member of Yarrimie Formation (M.Devn)||||||
4869|Crawney Limestone Member|43407|14|Not recorded|Map Legend|||(Provisional Edition)Yarrimie Formation. Tamworth Group.||||||
4869|Crawney Limestone Member|43428|14|Not recorded|p140|||List of fauna||||||
4869|Crawney Limestone Member|68005|5|Briefly described|p150.|Devonian|Devonian|||Unit in Yarrimie Formation.|||Fossiliferous and recrystallised limestone and calcareous mudstone.|
4869|Crawney Limestone Member|68006|6|Mentioned|p114.|Early Devonian|Early Devonian|||Unit in Tamworth Group.||||
4879|Crescent Complex|22636|5|Briefly described|p471,2,4,5|Miocene|Eocene|||||||
4879|Crescent Complex|24127|5|Briefly described|p5|||||||||
4879|Crescent Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
4879|Crescent Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
4879|Crescent Complex|40590|6|Mentioned|Fig.1|||||||||
4879|Crescent Complex|44450|5|Briefly described|p30|Miocene|Miocene|Geological Province: Nambucca Block.||||||
4879|Crescent Complex|61773|6|Mentioned|p138|||Probably a structural term.||||||
4879|Crescent Complex|73581|5|Briefly described|p8|Miocene|Miocene|Intrusive, represents the core and main feeder zone of the Ebor-Dorrigo volcano. Exposed by erosion in 2 square kilometres.|18.2+/-2.2 Ma fission track apatite||||Mafic to felsic stock made up of coarse-grained gabbro, monzodiorite, monzonite, and monzogranite in the core, surrounded by felsic dykes.|
4910|Croajingalong Granite|23309|5|Briefly described|p346||Early Devonian|G5 - I-Type.  Supersedes Croajingalong Adamellite||||||
4910|Croajingalong Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Croajingalong Adamellite, Vic.||||||
4910|Croajingalong Granite|68116|5|Briefly described|Appendix, Maps 37, 46.|Early Devonian|Early Devonian||||||Biotite granite: pink, coarse, porphyritic; rare microgranitoid enclaves.|
4945|Croudace Bay Formation|29922|6|Mentioned|Appendix 4|||||||||
4945|Croudace Bay Formation|29926|6|Mentioned|Fig.3|||||||||
4945|Croudace Bay Formation|29942|4|Described|Fig.2|||||||||
4945|Croudace Bay Formation|34351|6|Mentioned|p346|||Fig.5.13||||||
4945|Croudace Bay Formation|35319|6|Mentioned|Table 1|||||||||
4945|Croudace Bay Formation|37083|6|Mentioned|p164|||||||||
4945|Croudace Bay Formation|37966|6|Mentioned|p4|||||||||
4945|Croudace Bay Formation|39292|6|Mentioned|Fig. 6.2|||||||||
4945|Croudace Bay Formation|39308|6|Mentioned|Fig. 23.4|||||||||
4945|Croudace Bay Formation|39609|6|Mentioned|Table 1|||||||||
4945|Croudace Bay Formation|39666|6|Mentioned|Table 20|||||||||
4945|Croudace Bay Formation|41463|6|Mentioned|Fig.1|||||||||
4945|Croudace Bay Formation|41479|6|Mentioned|Fig.2|||||||||
4945|Croudace Bay Formation|43344|14|Not recorded|p85||Permian|||||||
4945|Croudace Bay Formation|43447|14|Not recorded|diag.p26|||Part of Boolaroo Sub-Group||||||
4945|Croudace Bay Formation|43448|14|Not recorded|p244||Permian|On table only. Unit of Boolaroo Subgroup.(Newcastle Coal Measures)||||||
4945|Croudace Bay Formation|45090|6|Mentioned|p186|||Stratigraphic table||||||
4945|Croudace Bay Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Boolaroo Subgroup|Included Belmont Conglomerate Member.|||
4948|Crow Mountain Creek beds|32683|4|Described|p204|||See also PP205-207. Informal (author's note)||||||
4948|Crow Mountain Creek beds|38222|6|Mentioned|p358|||||||||
4949|Crow Valley Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Biotite granite. BMR map symbol: gbc.||||||
4949|Crow Valley Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
4949|Crow Valley Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
4949|Crow Valley Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
4949|Crow Valley Granite|33325|6|Mentioned|p19|||||||||
4949|Crow Valley Granite|40328|4|Described|p205|||||||||
4949|Crow Valley Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
4961|Crowthers Road Conglomerate|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures). Poorly sorted imbricated conglomerate interbedded with sandstone; minor siltstone. Max. thickness: 15m. Geological Province: Sydney Basin.||||||03-MAR-06
4961|Crowthers Road Conglomerate|37099|6|Mentioned|p257|||||||||
4961|Crowthers Road Conglomerate|40872|6|Mentioned|Fig.2|||||||||
4961|Crowthers Road Conglomerate|41054|6|Mentioned|Fig.3|||||||||
4961|Crowthers Road Conglomerate|44244|4|Described|p188|Permian|Permian|Max. thickness: 350m.  Geological Province: Myall Block.  Reference section in text.||||||
4961|Crowthers Road Conglomerate|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures).  Massive polymictic boulder to pebble conglomerate.  Geological Province: Western Myall Block.||||||
4970|Crudine Group|22472|5|Briefly described|p39|||||||||
4970|Crudine Group|22503|5|Briefly described|Fig. 3b, p645|Late Devonian|Early Devonian|See also p648||||||
4970|Crudine Group|22529|6|Mentioned|1|||||||||
4970|Crudine Group|22590|4|Described|P750, Fig1||Early Devonian|||||||
4970|Crudine Group|22679|3|Fully described|p 32|Devonian|Devonian|formerly part of the Burrga Group and Mulgunnia Formation||||||
4970|Crudine Group|22704|6|Mentioned|p65||Early Devonian|Also Fig7,p66||||||
4970|Crudine Group|22768|5|Briefly described|p179-80|||||||||
4970|Crudine Group|22798|6|Mentioned|p851 Fig.2||Devonian|||||||
4970|Crudine Group|22857|5|Briefly described|p179, p180, p470 App.1 Tb.A1.6|Pragian|Lochkovian|Felsic tuffs, tuffaceous breccias, banded tuffs interbedded with greywackes, siltstones and slates. Max. thickness: ~2km. Geological Province: Hill End trough and Capertee Rise. See also p478 App.1 Tb.A1.6.||||||
4970|Crudine Group|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|||||||
4970|Crudine Group|23170|2|Defined|p152|Pragian|Lochkovian|Of Lachlan Fold Belt.||||||28-AUG-08
4970|Crudine Group|23214|2|Defined|p186|Pragian|Lochkovian|Max. thickness 2700m. Geological Province: Lachlan Fold Belt.||||||28-AUG-08
4970|Crudine Group|23309|6|Mentioned|p390|||||||||
4970|Crudine Group|23522|5|Briefly described|p248 Fig 4|Early Devonian|Early Devonian|||||||
4970|Crudine Group|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
4970|Crudine Group|24278|5|Briefly described|p1765|||Well bedded metre-scale graded wacke capped by mudstone. Overlain by Merrions tuff.||||||
4970|Crudine Group|24317|5|Briefly described|p15 Fig.1|Early Devonian|Early Devonian|||||||
4970|Crudine Group|24588|5|Briefly described|p31 Fig.15|Emsian|Emsian|Geological Province: Lachlan Fold Belt.||||||
4970|Crudine Group|29909|6|Mentioned|p139|||||||||
4970|Crudine Group|29993|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
4970|Crudine Group|30099|6|Mentioned|p396|||See also Fig.2||||||
4970|Crudine Group|31161|5|Briefly described|PA4|||||||||
4970|Crudine Group|31706|6|Mentioned|p645|||Devonian correlation chart||||||
4970|Crudine Group|31852|6|Mentioned|Fig. 5|||Gedinnian||||||
4970|Crudine Group|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
4970|Crudine Group|32046|6|Mentioned|p59|||See also p260,261,263,264||||||
4970|Crudine Group|32047|6|Mentioned|p18|||Refers gold mineralization||||||
4970|Crudine Group|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
4970|Crudine Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
4970|Crudine Group|32672|6|Mentioned|p673|||||||||
4970|Crudine Group|33006|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian to Lower Devonian||||||
4970|Crudine Group|33282|6|Mentioned|Map legend|Early Devonian|Late Silurian|U.Sil.-L.Dev.||||||
4970|Crudine Group|33285|6|Mentioned|p9|||||||||
4970|Crudine Group|33732|4|Described|p116|||Table II||||||
4970|Crudine Group|34059|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
4970|Crudine Group|34403|4|Described|p131|||Early Devonian fauna. See also P134||||||
4970|Crudine Group|34404|6|Mentioned|Fig.3.4b|||||||||
4970|Crudine Group|34405|6|Mentioned|Fig.3.9|||||||||
4970|Crudine Group|34572|6|Mentioned|p89|||Upper Silurian - Lower Devonian. See also PP90,91 etc.||||||
4970|Crudine Group|35072|6|Mentioned|p363|||||||||
4970|Crudine Group|35257|6|Mentioned|p134|||||||||
4970|Crudine Group|37746|6|Mentioned|Notes|||||||||
4970|Crudine Group|38216|5|Briefly described|p253|||||||||
4970|Crudine Group|39331|6|Mentioned|Fig.7-1|||||||||
4970|Crudine Group|40328|3|Fully described|p173|||||||||
4970|Crudine Group|41207|5|Briefly described|Table 1, P94|||||||||
4970|Crudine Group|42051|6|Mentioned|p139|||||||||
4970|Crudine Group|42712|4|Described|Table1p14; p8,16|Early Devonian|Late Silurian|||||||
4970|Crudine Group|43127|4|Described|p4,Fig.2,Fig.3||Early Devonian|||||||
4970|Crudine Group|43263|6|Mentioned|Map Legend|Early Devonian|Late Silurian|||||||
4970|Crudine Group|43344|14|Not recorded|p139,140,150,153-5|Early Devonian|Late Silurian|||||||
4970|Crudine Group|43384|14|Not recorded|Map Legend||Silurian|||||||
4970|Crudine Group|43461|14|Not recorded|table p621,p622||Gedinnian|||||||
4970|Crudine Group|43476|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Provisional Edition)||||||
4970|Crudine Group|43515|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Provisional Edition)||||||
4970|Crudine Group|43516|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
4970|Crudine Group|43517|14|Not recorded|p111-2,120,122-3,|||Type section p123. p126-163, map plate XII||||||
4970|Crudine Group|43519|14|Not recorded|p118,Tb p119,120|Siegenian|Gedinnian|||||||
4970|Crudine Group|43525|14|Not recorded|map p124,Tb p126-7||Gedinnian|||||||
4970|Crudine Group|43641|5|Briefly described|Map Legend||Devonian|||||||
4970|Crudine Group|43654|5|Briefly described|Map Legend|Devonian|Devonian|Includes; Turondale Formation, Dunhurch Formation, Bushranger Volcanics, Buckburraga Slate, Waterbeach Formation.||||||
4970|Crudine Group|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|||||||
4970|Crudine Group|44093|5|Briefly described|p206, p207 App. 1|Middle Devonian|Silurian|Includes Merrions Tuff and Turondale Formation. Geological Province: Lachlan Fold Belt.||||||17-MAR-05
4970|Crudine Group|49916|5|Briefly described|p509-510|Neoproterozoic|Neoproterozoic|Geological Province: Hill End Trough.||||||
4970|Crudine Group|50233|5|Briefly described|Map Legend|Pragian|Lochkovian|Overlies the Campbells Group.  Includes Bushranger Volcanics, Buckburraga Slate and Dunchurch Formation.||||||13-MAY-04
4970|Crudine Group|60424|5|Briefly described|p351 Fig. 2|Devonian|Devonian|Includes: Bay Formation. Geological Province: Hill End Trough.||||||
4970|Crudine Group|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes Buckburraga Slate, Bushranger Volcanics and Dunchurch Formation.||||||17-JUN-08
4970|Crudine Group|64296|5|Briefly described|p84 Tb. 1|||||||||
4970|Crudine Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Limekilns. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
4970|Crudine Group|66087|6|Mentioned|p5|Devonian|Devonian|||||Overlies the Campbells Group.||10-MAY-12
4970|Crudine Group|66197|5|Briefly described|p633 Fig.4a, b|Emsian||Capertee High-Hill End Trough. Mudstone dominated deep marine turbidites. Underlies Cunningham Formation, overlies Chesleigh Group. Includes Turondale Formation and Merrions Formation at top.||||||13-MAR-12
4970|Crudine Group|67820|6|Mentioned|p136 Fig.3|Lockhovian|Lockhovian|||||||
4970|Crudine Group|68003|5|Briefly described|p24 Fig.3-e, p25, p143.|Lochkovian|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion. Thick deposits of subaerial sediments.|||Includes basal Turondale Formation, Waterbeach, Guroba and Merrions Formations.|Overlies Cuga Burga Volcanics. Is overlain by Cunningham Formation.||
4970|Crudine Group|68592|2|Defined|xxiii, p74 Tb.5, p609, p1038-59, p1078|Pragian|Lochkovian|Packham (1968). Includes units in the Burraga Group (Stanton 1955, 1956), which became redundant (Raymond et al., 1998). Additional units (added by Pogson and Watkins, 1998; Meakin and Morgan, 1999) have expanded the definition. Type sections for both the original and current component formations are described. 1300-2200m thick. Stratigraphic sequences of the two outcrops in the Goulburn250 area are detailed. Deepwater deposits. Geochemistry by Pogson and Watkins (1998) described as I-type, medium-K calc-alkaline. Peelwood structural zone: deformation described.|411 +/- 4 Ma (SHRIMP U-Pb zircon; Black,1998).||Includes Bay, Merrions, Guroba, Waterbeach, Turondale, Adderley and Dunchurch Formations; Bushranger Volcanics; Buckburraga Slate.|Conformably overlies or faulted against Campbells Group. Is overlain conformably by Cunningham Formation. Age-equivalent to Bindook Group and Mountain Creek Volcanics.|Undifferentiated: medium- to thick-bedded siltstone and volcaniclastic sandstone, interbedded with less common tuffaceous sandstone and coarse to pebbly polymict, mostly volcaniclastic, bands.|
4970|Crudine 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.||||||
4970|Crudine Group|70192|5|Briefly described|Map Legend|Pragian|Lochkovian|Dc. Undifferentiated Crudine Group. On Crookwell and Taralga 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Dunchurch Formation, Bushranger Volcanics, Buckburraga Slate.|Overlies Box Ridge Volcanics, Cuddyong Formation and Binghams Back Formation (of Campbells Group). Is overlain by Cunningham Formation.|Medium-thickly bedded, volcaniclastic sandstone and siltstone, lesser interbedded vitric tuff and coarse grained-pebbly volcaniclastic sandstone where undifferentiated.|
4970|Crudine Group|70297|4|Described|map legend, on side 2 of map sheet|Pragian|Lochkovian|Age: Early Devonian. Deposited in deep water environment.|||Adderley Formation, Bay Formation, Cookman Formation, Dunchurch Formation, Merrions Formation, Bushranger Volcanics, Turondale Formation, Buckburraga Slate, Waterbeach Formation|Is overlain by Cunningham Formation and Limekilns Formation. ?Intruded by Wologorong Supersuite. ?Overlies Chesleigh Group.|Thin- to thick-bedded and massive, quartzose, feldspathic and crystal-lithic felsic volcaniclastic sandstones; dacitic to rhyolitic and andesitic lavas and volcaniclastic rocks; slate, tuff, siltstone, conglomerate, phyllite, rare limestone.|
4970|Crudine Group|70543|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Dunchurch Formation, Buckburraga Slate.||Medium-thickly bedded, volcaniclastic sandstone and siltstone, lesser interbedded vitric tuff and coarse grained-pebbly volcaniclastic sandstone where undifferentiated.|
4970|Crudine Group|70544|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Dunchurch Formation, Bushranger Volcanics, Buckburraga Slate||Medium-thickly bedded, volcaniclastic sandstone and siltstone, lesser interbedded vitric tuff and coarse grained-pebbly volcaniclastic sandstone, where undifferentiated.|
4970|Crudine Group|71656|6|Mentioned|p13 Fig.2|Pragian|Lochkovian|Only shown in correlation chart (Fig.2).|||Bushranger Volcanics, Buckburraga Slate, Dunchurch Formation.|Overlies Campbells Group. Underlies Cunningham Formation.|Including volcanics and slate.|
4970|Crudine Group|71700|5|Briefly described|p23, CD|Early Devonian|Early Devonian|Hill End Trough; deep water succsession.|||Includes the Merrions Formation.|||
4970|Crudine Group|71924|5|Briefly described|p2|Lochkovian||Of Garratt & Wright 1988. Hill End Trough. Fauna older than lower Mullamuddy [Formation]. |||Includes Waterbeach Formation at top.|||
4970|Crudine Group|73299|6|Mentioned|p1102 Fig.8, p1105|Devonian|Devonian|Hill End Trough.||||||
4973|Cucum Granite|42726|5|Briefly described|map legend|Silurian||||||||
4973|Cucum Granite|68592|6|Mentioned|p1260|||Chappell et al. (1991). Much of this unit is now assigned to the Wyangala Granite (Hovells Suite).||Unit in Cowra Suite.||||
4974|Cudal Group|13139|5|Briefly described|p9 Fig. 4|Wenlock|Llandovery|Geological Province: Western Molong Volcanic Belt.||||||
4974|Cudal Group|22503|5|Briefly described|p648||Late Silurian|||||||
4974|Cudal Group|22768|6|Mentioned|p179|||||||||
4974|Cudal Group|22857|5|Briefly described|p127, p456 App.1, Tb.A1.6|Silurian|Silurian|Disconformably overlies the Millambri Formation. Geological Province: Cowra Trough. See also p179.||||||
4974|Cudal Group|23043|5|Briefly described|Map Legend|Lochkovian|Wenlock|||||||
4974|Cudal Group|23170|2|Defined|p99|Ludlow|Llandovery|Of Lachlan Fold Belt.||||||04-MAR-09
4974|Cudal Group|23213|6|Mentioned|p20||Silurian|Overlies Oakdale Formation near Ponto.||||||
4974|Cudal Group|23214|3|Fully described|p113|Late Silurian|Early Silurian|First referred to by map only as Cudal Shale. Comprises of a thick shaly sequence containing occasional carbonate bearing intervals and includes a major rhyolitic volcaniclastic unit. Max. thickness 2000m. Overlying unit: Goonigal Group.||||||
4974|Cudal Group|23245|6|Mentioned|p127|||||||||
4974|Cudal Group|23309|6|Mentioned|p384||Silurian|||||||
4974|Cudal Group|23334|5|Briefly described|9 Fig.4|Silurian|Early Silurian|||||||
4974|Cudal Group|24007|6|Mentioned|p336|||||||||
4974|Cudal Group|24417|6|Mentioned|p46|||||||||
4974|Cudal Group|29989|6|Mentioned|Map legend|Silurian|Silurian|||||||
4974|Cudal Group|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
4974|Cudal Group|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
4974|Cudal Group|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
4974|Cudal Group|32047|6|Mentioned|p12|||||||||
4974|Cudal Group|32483|4|Described|p16|||Sil. Table 1||||||
4974|Cudal Group|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
4974|Cudal Group|32672|6|Mentioned|p672|||||||||
4974|Cudal Group|33125|6|Mentioned|p15|||Correlation chart||||||
4974|Cudal Group|34404|6|Mentioned|Fig.3.4b|||||||||
4974|Cudal Group|34498|6|Mentioned|p150|||See also P151. Silurian||||||
4974|Cudal Group|37727|4|Described|p52|||||||||
4974|Cudal Group|40136|6|Mentioned|p31|||[Originally entered for NT. CEBMar95]||||||
4974|Cudal Group|40328|1|Redefined|p71|Silurian|Silurian|||||||
4974|Cudal Group|43263|6|Mentioned|Map Legend|Late Silurian||Age Middle-Late Silurian.||||||
4974|Cudal Group|43494|6|Mentioned|p18||Silurian|Includes: Canowindra Volcanics, Cary Formation, Burrawong Limestone and Hanover Formation.||||||16-MAR-06
4974|Cudal Group|43515|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
4974|Cudal Group|43516|14|Not recorded|Map Legend|Late Silurian|Early Silurian|||||||
4974|Cudal Group|43640|5|Briefly described|Map Legend||Silurian|||||||
4974|Cudal Group|43782|5|Briefly described|Map Legend|Ludlow|Llandovery|||||||
4974|Cudal Group|44093|5|Briefly described|p195 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
4974|Cudal Group|50590|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Hanover Formation, Cary Formation, Canowindra Volcanics.||||||
4974|Cudal Group|60987|5|Briefly described|p153, p155, |Earliest Devonian|Early Silurian |Meakin and Morgan (1999).|||Hanover Formation.|||
4974|Cudal Group|63278|6|Mentioned|p147 Fig. 2b|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
4974|Cudal Group|63283|6|Mentioned|p195 Fig. 2|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
4974|Cudal Group|63287|5|Briefly described|p317 Fig. 2, p349|Late Silurian|Early Silurian|Includes; Liscombe Pools Limestone, Gospal Oak Shale, Canowindra Volcanics, Avoca Valley Shale, Ghost Hill Formation, Belubula Shale. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
4974|Cudal Group|63290|5|Briefly described|p396 Fig. 3|Wenlock|Llandovery|Overlain by Canowindra Volcanics. Geological Province: Molong Volcanic Belt.||||||
4974|Cudal Group|63293|6|Mentioned|p469 Fig. 2||Llandovery|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
4974|Cudal Group|64826|5|Briefly described|p1040 Tb. 1|Frasnian|Wenlock|Contains Gospel Oak Shale.||||||04-MAR-09
4974|Cudal Group|67106|6|Mentioned|p673|||Molong Volcanic Belt.||||||
4974|Cudal Group|67322|6|Mentioned|p25|Silurian|Silurian||||Sourges Shale|||
4974|Cudal Group|67847|5|Briefly described|p32|||Previously included the Kabadah Formation. ||||||
4974|Cudal Group|68003|5|Briefly described|p24 Fig.3-e, p145. |Pridoli|Llandovery|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Canowindra Volcanics and Hanover Formation.|Is overlain by Cuga Burga Volcanics.|Weakly feldspar-phyric rhyolite; rhyolitic tuff, tuffaceous sandstone; siltstone; fossiliferous limestone (?allochthonous); minor calcareous sandstone, breccia.|
4974|Cudal Group|68310|6|Mentioned|p237|||Cowra-Canowindra region.||||||
4974|Cudal Group|68592|6|Mentioned|p23, p416|||Percival (1976); Pickett (1982). Comagmatic with Cowra Suite.|||Includes Liscombe Pools Limestone and Canowindra Volcanics.|||
4974|Cudal 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.||||||
4974|Cudal Group|70297|4|Described|map legend, on side 2 of map sheet|Ludlow|Llandovery|In lower part of Cowra Trough sequence. Age: middle late Llandovery to late Ludlow. Includes two major felsic to intermediate volcaniclastic and pyroclastic units (Canowindra and Nargong Volcanics).|||Shale: Avoca Valley, Belubula, Mackeys Creek, Gospel Oak, Sourges. Volcanics: Canowindra, Nargong Volcanics. Formation: Greengrove, Ghost Hill, Kurrajong Park, Tenandra.|Conformably overlain by Goonigal Group|Thick sequence of shale, mudstone and siltstone containing sporadic carbonate-bearing (limestone) intervals; a thick, felsic volcanic unit includes calc-alkaline high-K garnet-bearing rhyolitic to rhyodacitic lava facies.|
4974|Cudal Group|70684|6|Mentioned|p34, p75|Early Silurian|Early Silurian|Molong Volcanic Belt.||||||
4974|Cudal Group|71600|6|Mentioned|p23 Fig 1|Silurian|Silurian|Geological province: Lachlan Fold Belt.|||Includes Hanover Formation, Canowindra Volcanics.|||
4974|Cudal Group|73154|6|Mentioned|p77 Fig.3|Wenlock|Llandovery|||||||
4978|Cudgegong Volcanics|22529|4|Described|3|Silurian|Gisbornian|Now Sofala Volcanics||||||
4978|Cudgegong Volcanics|23181|6|Mentioned|p1|||Now equated with the Sofala Volcanics.||||||
4978|Cudgegong Volcanics|40106|4|Described|p593|||||||||
4978|Cudgegong Volcanics|43188|3|Fully described|p199,Table 1 p200||Gisbornian|Type section location given in Table 1,Capertee High.||||||
4978|Cudgegong Volcanics|43316|14|Not recorded|p12||Ordovician|||||||
4981|Cuga Burga Volcanics|22466|4|Described|P8, Fig8 P8||Early Devonian|||||||
4981|Cuga Burga Volcanics|22768|5|Briefly described|p178-79|||||||||
4981|Cuga Burga Volcanics|22857|4|Described|p178, p454 App.1, Tb.A1.6|Late Silurian|Silurian|Of the Gregra Group. Mafic submarine volcanics. Overlies the Mumbil Group. Equivalent to the Berkley Formation. Max. thickness: 1000m. See also p466 App.1 Tb.A1.6.||||||
4981|Cuga Burga Volcanics|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Gregra Group.||||||
4981|Cuga Burga Volcanics|23170|2|Defined|p194|Early Devonian|Late Silurian|Of Gregra Group.||||||19-MAY-09
4981|Cuga Burga Volcanics|23214|3|Fully described|p14|Lochkovian|Lochkovian|Of Gregra Group. Originally included in Molong Beds. Also previously mapped as part of the Malachis Hill Formation and Bulls Camp Volcanics. Max. thickness 1000m.||||||
4981|Cuga Burga Volcanics|23522|5|Briefly described|p248 Fig 4|Lochkovian|Lochkovian|||||||
4981|Cuga Burga Volcanics|23738|6|Mentioned|p252|||||||||
4981|Cuga Burga Volcanics|24126|5|Briefly described|p98|||||||||
4981|Cuga Burga Volcanics|24247|5|Briefly described|p39 Fig.2|Early Devonian|Early Devonian|||||||
4981|Cuga Burga Volcanics|24417|5|Briefly described|p41|Early Devonian|Early Devonian|||||||
4981|Cuga Burga Volcanics|29362|6|Mentioned|Table 1|||Silurian-Devonian.||||||
4981|Cuga Burga Volcanics|29993|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
4981|Cuga Burga Volcanics|30597|6|Mentioned|Fig.1|||||||||
4981|Cuga Burga Volcanics|30657|3|Fully described|p26|||Silurian age. Geology||||||
4981|Cuga Burga Volcanics|31161|5|Briefly described|PA4|||||||||
4981|Cuga Burga Volcanics|31543|5|Briefly described|p111|||||||||
4981|Cuga Burga Volcanics|31852|6|Mentioned|p719|||See also Fig.4. Gedinnian||||||
4981|Cuga Burga Volcanics|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
4981|Cuga Burga Volcanics|32046|6|Mentioned|p132|||See also P139||||||
4981|Cuga Burga Volcanics|32047|6|Mentioned|p2|||||||||
4981|Cuga Burga Volcanics|32088|6|Mentioned|p6|||Siluro-Devonian||||||
4981|Cuga Burga Volcanics|32154|6|Mentioned|Fig.|||Geological sketch map.||||||
4981|Cuga Burga Volcanics|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
4981|Cuga Burga Volcanics|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
4981|Cuga Burga Volcanics|32672|6|Mentioned|p673|||||||||
4981|Cuga Burga Volcanics|33004|6|Mentioned|p193|||||||||
4981|Cuga Burga Volcanics|33006|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian to Lower Devonian||||||
4981|Cuga Burga Volcanics|33282|6|Mentioned|Map legend|Early Devonian|Late Silurian|U.Sil.-L.Dev.||||||
4981|Cuga Burga Volcanics|33285|6|Mentioned|p22|||||||||
4981|Cuga Burga Volcanics|33611|6|Mentioned|p125|||||||||
4981|Cuga Burga Volcanics|33732|5|Briefly described|p115|||Table II||||||
4981|Cuga Burga Volcanics|34059|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
4981|Cuga Burga Volcanics|34403|3|Fully described|p140|||||||||
4981|Cuga Burga Volcanics|34404|6|Mentioned|Fig.3.4b|||||||||
4981|Cuga Burga Volcanics|34405|6|Mentioned|Fig.3.9|||||||||
4981|Cuga Burga Volcanics|34406|6|Mentioned|p221|||2000 feet||||||
4981|Cuga Burga Volcanics|34498|6|Mentioned|p148|||Upper Silurian - Lower Devonian||||||
4981|Cuga Burga Volcanics|34567|6|Mentioned|p160|||Fig.1||||||
4981|Cuga Burga Volcanics|35185|6|Mentioned|p256|||||||||
4981|Cuga Burga Volcanics|35257|6|Mentioned|p130|||||||||
4981|Cuga Burga Volcanics|35374|6|Mentioned|p68|||||||||
4981|Cuga Burga Volcanics|36534|6|Mentioned|p229|||||||||
4981|Cuga Burga Volcanics|37488|6|Mentioned|Fig.1|||||||||
4981|Cuga Burga Volcanics|37727|5|Briefly described|p53|||See also P34.||||||
4981|Cuga Burga Volcanics|39331|6|Mentioned|Fig.8-1|||||||||
4981|Cuga Burga Volcanics|39654|6|Mentioned|M92|||||||||
4981|Cuga Burga Volcanics|39663|6|Mentioned|Table 1|||||||||
4981|Cuga Burga Volcanics|40026|5|Briefly described|p245|||||||||
4981|Cuga Burga Volcanics|40328|6|Mentioned|p17|||||||||
4981|Cuga Burga Volcanics|40365|6|Mentioned|p315|||||||||
4981|Cuga Burga Volcanics|40882|5|Briefly described|p22|||||||||
4981|Cuga Burga Volcanics|42726|5|Briefly described|map legend|Early Devonian||V15.  Of the Boggy Plain Suite (Boggy Plain Supersuite).||||||08-FEB-05
4981|Cuga Burga Volcanics|43039|6|Mentioned|p6|||||||||
4981|Cuga Burga Volcanics|43461|14|Not recorded|table p621,p622||Ludlovian|||||||
4981|Cuga Burga Volcanics|43476|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
4981|Cuga Burga Volcanics|43479|14|Not recorded|p116,124,126-7,151|Early Devonian|Ludlovian|||||||
4981|Cuga Burga Volcanics|43494|6|Mentioned|p9|Devonian|Devonian|Contain keratophyre and quartz keratophyre, lavas and tuffs, sediments and limestone.||||||09-MAR-06
4981|Cuga Burga Volcanics|43515|14|Not recorded|Map Legend|Early Devonian|Late Silurian|(Provisional Edition)||||||
4981|Cuga Burga Volcanics|43516|14|Not recorded|Map Legend|Early Devonian|Late Silurian|||||||
4981|Cuga Burga Volcanics|43517|14|Not recorded|p116,124-161|||Overlies Barnby Hills Shale,equiv to Bay Fm,just above Sil.-Dev.boundary. Map Plate XII||||||
4981|Cuga Burga Volcanics|43525|14|Not recorded|map p124,Tb p126-7,|||Table p132||||||
4981|Cuga Burga Volcanics|43528|2|Defined|p132,133|Devonian|Silurian|||||||
4981|Cuga Burga Volcanics|43640|5|Briefly described|Map Legend||Devonian|||||||
4981|Cuga Burga Volcanics|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Gregra Group.||||||
4981|Cuga Burga Volcanics|50095|4|Described|p107|Lochkavian|Lochkavian|Andesitic volcanics and derived sediments. Conformably underlies Garra Limestone. Overlies Camelford Limestone.||||||11-FEB-08
4981|Cuga Burga Volcanics|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Gregra Group.  Lava and intrusives, volcaniclastic sandstone, breccia, siltstone, shale and limestone.||||||
4981|Cuga Burga Volcanics|60308|6|Mentioned|p38|||||Boggy Plains Suite||||
4981|Cuga Burga Volcanics|60332|5|Briefly described|p938|Early Devonian|Early Devonian|Conformably overlies Camelford Limestone. Conformably overlain by Garra Formation. Andesite lavas, tuffs.||||||
4981|Cuga Burga Volcanics|60987|5|Briefly described|p154 Fig.1, p155, p157-158|Early Devonian|Early Devonian|||||Overlies the Hanover Formation.|Dominantly mafic to intermediate volcanics, volcanilitharenite and volcanilithrudite and limestone blocks.|
4981|Cuga Burga Volcanics|63283|6|Mentioned|p202|Early Devonian|Early Devonian|||||||07-FEB-11
4981|Cuga Burga Volcanics|63290|6|Mentioned|p406 Fig. 7|||||||||
4981|Cuga Burga Volcanics|64994|5|Briefly described|p10|Lochkovian|Lochkovian|Geological province: Lachlan Orogen.||||||07-FEB-11
4981|Cuga Burga Volcanics|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Wellington and Molong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
4981|Cuga Burga Volcanics|66197|5|Briefly described|p634, p633 Fig.4c|Emsian|Lochkovian|Cowra Trough-Molong High. Mafic-intermediate volcanics. Overlies the Barnby Hills Shale and Hanover Formation. Age: 409 +/ - 9 Ma.||||||13-MAR-12
4981|Cuga Burga Volcanics|67127|6|Mentioned|p111|Devonian|Silurian|Cut by a pipe-like body that hosts the Toongi deposit.|||||Volcanic rocks.|
4981|Cuga Burga Volcanics|67847|5|Briefly described|p34|||In contact with the Oakdale Formation although the relationship is not given. ||||||
4981|Cuga Burga Volcanics|68003|5|Briefly described|p24 Fig.3-e, p143. |Lochkovian|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gregra Group.||Overlies Cudal and Mumbil Groups. Is overlain by Gregra and Crudine Groups.|Latitic, crystal-lithic sandstone, breccia, siltstone, tuff; latite and lesser andesite, basalt; minor allochthonous limestone, quartzose sandstone.|
4981|Cuga Burga Volcanics|68592|5|Briefly described|p845 Fig.141, p932, p934, p1170|Early Devonian|Early Devonian|In the Bathurst and Dubbo 1:250 000 map areas. Figure caption: Th/Yb vs Ta/Yb plot of Pearce (1983) for selected mafic to intermediate (<58% SiO2) units of GOULBURN250. The Early Devonian Cuga Burga Volcanics of the Wellington area are included for comparison (data from Geoscience Australia and GSNSW). Mentioned as having geochemical affinities with Boggy Plain Supersuite.||Unit in Gregra Group.|||Voluminous basaltic to andesitic volcanics.|
4981|Cuga Burga Volcanics|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Grega Group||||
4981|Cuga Burga Volcanics|73299|6|Mentioned|p1105|Early Devonian|Silurian|Hill End Trough, Molong High. [Map symbol suggests Devonian age]||||Overlies the Camelford Limestone, Barnby Hills Shale, underlies the Garra Formation, Tolga Member.||
4981|Cuga Burga Volcanics|73492|5|Briefly described|p696|Early Devonian|Early Devonian|Contains allochthonous limestones with T. blandus Biozone fauna of early Katian age.|||Overlies Barnaby Hills Shale|||
4983|Culaden Granodiorite|38915|6|Mentioned|p338|||||||||
4983|Culaden Granodiorite|69188|5|Briefly described|p1-2, p5, p72-75, p79|Early Triassic|Permian|Emmaville-Tent Hill-Ottery area. Forms small stocks and dykes. Same age as Wandsworth Volcanic Group; geochemically similar to the Uralla Supersuite. Contains cassiterite, arsenopyrite and pyrite mineralisation (presumably from the Mole Granite).|252.2 +/- 1.9 Ma (magmatic age)|||Is cut by the Mole Granite.|Grey, medium- to coarse-grained, strongly porphyritic quartz, feldspar biotite amphibole granodiorite.|16-APR-20
4983|Culaden Granodiorite|69639|5|Briefly described|p38, p220|Induan|Changhsingian|New England Orogen.|252.2 +/- 1.0 Ma (Cross and Blevin, 2010)|||Intruded by the Mole Granite.||
4983|Culaden Granodiorite|71628|4|Described|p8: 4, 82-85|||Wood (1982). Later  referred to as Taylors Adamellite (Henley et al., 2000) where it is only mentioned in the map legend. The name Taylors Monzogranite is reserved in ASUD. Named in this study as Culaden Granodiorite because of precedence. Named after a local homestead. A narrow, elongate dyke-like body; distribution described. Has low, fresh and rubbly outcrop. Limited geochemistry described. Is spatially (probably not genetically) associated with numerous small Sn, As, Bi, Ag deposits, likely sourced from Mole Leucogranite.|252.2 +/- 1.9 Ma (SHRIMP: Cross and Blevin, 2013).|Wards Mistake Suite.||Abuts Emmaville Volcanics. Is intruded (and contact metamorphosed) by Mole Leucogranite.|Strongly porphyritic, biotite-hornblende-(pyroxene) monzogranitic to granodiorite porphyrite; lesser hornblende-biotite granodiorite to quartz diorite. I-type.|
4992|Cullerin Granite|42726|5|Briefly described|map legend|Silurian||||||||
4992|Cullerin Granite|68592|6|Mentioned|p1312|||Of Chappell et al. (1991). Now included in the redefined Gunning Granite.||||||
5014|Cumberland Rhyolite|22857|5|Briefly described|p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Boraig Group. Rhyolite, rhyolitic tuff. Max. thickness: 240m. Geological Province: Bogan Gate Terrace.||||||
5014|Cumberland Rhyolite|29648|6|Mentioned|p22|||||||||
5014|Cumberland Rhyolite|29953|6|Mentioned|Fig.1|||||||||
5014|Cumberland Rhyolite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
5014|Cumberland Rhyolite|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
5014|Cumberland Rhyolite|33732|6|Mentioned|p111|||Unit of Boraig Gp.||||||
5014|Cumberland Rhyolite|34403|4|Described|p144|||||||||
5014|Cumberland Rhyolite|34405|6|Mentioned|Fig.3.15|||||||||
5014|Cumberland Rhyolite|35070|6|Mentioned|p115|||||||||
5014|Cumberland Rhyolite|37491|6|Mentioned|Fig.1|||||||||
5014|Cumberland Rhyolite|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
5014|Cumberland Rhyolite|60086|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Boraig Group. Rhyolite, some tuff.||||||
5017|Cumbijowa Granite|24417|3|Fully described|p105|Early Devonian|Early Devonian|Previously named "Cumbijowa Adamellite" (Turner, 1993).  Brunker (1972) and Bowman (1976) both included it as part of Eugowra Granite.||||||
5017|Cumbijowa Granite|42726|5|Briefly described|map legend|Early Devonian||420.||||||
5017|Cumbijowa Granite|60009|5|Briefly described|Map Legend|Emsian|Emsian|||||||13-JUL-04
5018|Cumborah Gravel|23053|6|Mentioned|p11,38,86|Early Miocene|Oligocene|(Taylor 1976, 1978a). See also Cumborah Formation p17. Used in the Walgett-Cumborah region.  Gravels shown on the Nyngan & Walgett 1:250 000 sheets asTg have been correlated with this unit.||||||
5018|Cumborah Gravel|24042|5|Briefly described|p510|Oligocene|Oligocene|||||||
5018|Cumborah Gravel|35187|6|Mentioned|p55|||||||||
5018|Cumborah Gravel|61155|5|Briefly described|p19|Early Miocene|Early Miocene|Age: 23-21Ma.  In the Walgett area.||||||03-MAR-10
5018|Cumborah Gravel|68593|5|Briefly described|p1, p10|Miocene|Miocene|Taylor (1972). Mention on p10 of Cumborah Gravels, attributed to Taylor, is in fact a mis-quote.||||Unconformably overlies Griman Creek Formation.|Quartz-rich gravel sheet.|
5030|Cunglebung Creek beds|23811|5|Briefly described|Map Legend|Westphalian|Tournaisian|Part of the "Coffs Harbour Association".  Black-grey massive and laminated metaclaystone and meta siltstone, with rare lithic wacke, breccia, chert.||||||08-DEC-04
5030|Cunglebung Creek beds|23812|5|Briefly described|p10, p12 Tb.1|Carboniferous|Carboniferous|Included in the informal "Coffs HArbour Association".||||||
5030|Cunglebung Creek beds|38755|6|Mentioned|p63|||Geological Province: Coffs Harbour Block||||||
5030|Cunglebung Creek beds|39673|6|Mentioned|p218|||||||||
5030|Cunglebung Creek beds|40108|6|Mentioned|p183|||||||||
5030|Cunglebung Creek beds|60079|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of the "Coffs Harbour Association".||||||
5030|Cunglebung Creek beds|71628|5|Briefly described|p17:4|||||Coffs Harbour Asociation.||Is intruded by Dundahra Creek Leucosyenogranite.||
5031|Cunningham Formation|22472|6|Mentioned|p40|||||||||
5031|Cunningham Formation|22503|6|Mentioned|p646|||||||||
5031|Cunningham Formation|22529|4|Described|4 fig 2, 8|Emsian|Emsian|Geological province: Hill End Trough.||||||17-JUN-08
5031|Cunningham Formation|22590|5|Briefly described|P750|||||||||
5031|Cunningham Formation|22679|6|Mentioned|p 32|||||||||
5031|Cunningham Formation|22768|5|Briefly described|p180|Middle Devonian|Early Devonian|||||||
5031|Cunningham Formation|22857|5|Briefly described|p179, p180, p472 App.1 Tb.A1.6|Middle Devonian|Early Devonian|Contains the Nubrigyn Member. Max. thickness: >1km. Geological Province: Hill End Trough.||||||
5031|Cunningham Formation|23039|5|Briefly described|p166,7|Devonian|Silurian|||||||
5031|Cunningham Formation|23043|5|Briefly described|Map Legend|Emsian|Lochkovian|||||||
5031|Cunningham Formation|23170|2|Defined|p177|Emsian|Lochkovian|||||||17-MAY-18
5031|Cunningham Formation|23214|3|Fully described|p201|Emsian|Lochkovian|Predominantly composed of thin bedded turbidites. Max. thickness 3000m.||||||17-JUN-08
5031|Cunningham Formation|23522|5|Briefly described|p248 Fig 4|Early Devonian|Early Devonian|||||||
5031|Cunningham Formation|23738|4|Described|p255|Devonian|Devonian|||||||
5031|Cunningham Formation|24007|6|Mentioned|p340|||||||||
5031|Cunningham Formation|24126|6|Mentioned|p234|||Geological Province: Hill End Trough.||||||
5031|Cunningham Formation|24278|5|Briefly described|p1765 Fig. 1, p1766|||Slate, bedded mudstone in lower section and minor thin feldspathic sandstone beds. Thickness: >3.5km.||||||
5031|Cunningham Formation|24394|5|Briefly described|p170 Fig. 1, p175|Pragian|Pragian|Overlies both Merrions and Guroba Formaitons conformably. Geological Province: Hill End Trough.  See also p171 Fig. 2.||||||
5031|Cunningham Formation|29906|6|Mentioned|p13|||||||||
5031|Cunningham Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
5031|Cunningham Formation|30099|6|Mentioned|Fig.2|||||||||
5031|Cunningham Formation|30100|6|Mentioned|p205|||Stratigraphy.||||||
5031|Cunningham Formation|30657|6|Mentioned|p26|||Devonian age. Geology||||||
5031|Cunningham Formation|31161|5|Briefly described|PA4|||||||||
5031|Cunningham Formation|31706|6|Mentioned|p645|||Devonian correlation chart||||||
5031|Cunningham Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
5031|Cunningham Formation|32046|6|Mentioned|p136|||See also P191,253,257,259,265.||||||
5031|Cunningham Formation|32047|6|Mentioned|p3|||See also P10||||||
5031|Cunningham Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
5031|Cunningham Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
5031|Cunningham Formation|32672|6|Mentioned|p673|||||||||
5031|Cunningham Formation|33006|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower and Middle Devonian||||||
5031|Cunningham Formation|33282|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
5031|Cunningham Formation|33285|6|Mentioned|p22|||||||||
5031|Cunningham Formation|33326|6|Mentioned|p444|||Fauna.||||||
5031|Cunningham Formation|33732|4|Described|p116|||Table II||||||
5031|Cunningham Formation|34059|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
5031|Cunningham Formation|34403|4|Described|p136|||||||||
5031|Cunningham Formation|34404|6|Mentioned|Fig.3.4b|||||||||
5031|Cunningham Formation|34405|6|Mentioned|Fig.3.9|||||||||
5031|Cunningham Formation|34406|6|Mentioned|p223|||||||||
5031|Cunningham Formation|34567|6|Mentioned|p160|||Fig.1||||||
5031|Cunningham Formation|34692|5|Briefly described|p184|||||||||
5031|Cunningham Formation|37488|6|Mentioned|p251|||||||||
5031|Cunningham Formation|37746|6|Mentioned|Notes|||||||||
5031|Cunningham Formation|37747|6|Mentioned|Notes|||||||||
5031|Cunningham Formation|38216|5|Briefly described|p254|||||||||
5031|Cunningham Formation|39214|5|Briefly described|p23|||||||||
5031|Cunningham Formation|39331|6|Mentioned|Fig.7-1|||||||||
5031|Cunningham Formation|40328|6|Mentioned|p154|||See also P176||||||
5031|Cunningham Formation|42577|6|Mentioned|p37|||near Mumbil, NSW||||||
5031|Cunningham Formation|42712|4|Described|8; Table 1 p13.|Middle Devonian|Middle Devonian|Conformable with the Crudine Group below and the Limekilns Group above.||||||
5031|Cunningham Formation|43127|4|Described|p4,Fig.2,Fig.3||Early Devonian|||||||
5031|Cunningham Formation|43263|6|Mentioned|Map Legend||Early Devonian|||||||
5031|Cunningham Formation|43344|14|Not recorded|p139,150,153,154|Early Devonian||||||||
5031|Cunningham Formation|43461|14|Not recorded|table p621,p622|Eifelian|Emsian|||||||
5031|Cunningham Formation|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
5031|Cunningham Formation|43479|14|Not recorded|p127,151|Middle Devonian|Early Devonian|||||||
5031|Cunningham Formation|43494|4|Described|p28||Devonian|Conformable over Merrions Tuff.  Consists mainly of slaty grey siltstone with subordinate coarse lithic and feldspathic sandstone. Thickness at Hill End: >3700m.||||||08-MAR-06
5031|Cunningham Formation|43515|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
5031|Cunningham Formation|43516|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
5031|Cunningham Formation|43517|14|Not recorded|p112,124,129-163,||Early Devonian|Type section on Turon River. Conf.on Merrions Tuff. Map plate XII||||||
5031|Cunningham Formation|43519|14|Not recorded|Table p119|||||||||
5031|Cunningham Formation|43525|14|Not recorded|map p124,Tb p126-7,|||||||||
5031|Cunningham Formation|43528|14|Not recorded|p129,133,135||Devonian|||||||
5031|Cunningham Formation|43641|5|Briefly described|Map Legend||Devonian|||||||
5031|Cunningham Formation|43653|5|Briefly described|Map Legend||Devonian|||||||
5031|Cunningham Formation|43654|5|Briefly described|Map Legend|Devonian|Devonian|Includes Copperhannia Member. Slate, laminated siltstone, lithic sandstone.||||||17-JUL-08
5031|Cunningham Formation|43782|5|Briefly described|Map Legend|Emsian|Pragian|||||||
5031|Cunningham Formation|44093|5|Briefly described|p207 App. 1|Early Devonian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
5031|Cunningham Formation|50095|6|Mentioned|p114|||||||||
5031|Cunningham Formation|50233|5|Briefly described|Map Legend|Emsian|Pragian|Slate, laminated siltstone, lithic sandstone.  Contains the Copperhannia Member.  Overlies the Bushranger Volcanics.||||||13-MAY-04
5031|Cunningham Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Contains the Copperhannia Member. Slate, laminated siltstone, lithic sandstone.||||||
5031|Cunningham Formation|64296|5|Briefly described|p83|Early Devonian|Early Devonian|Contains a fossiliferous horizon extending for hundreds of metres along strike; fossils include tetracorals and associated tabulate corals, bryozoans, stromatoproids, pelmatozoans and comminuted shelly debris. Geological province: Hill End Trough. ||||||
5031|Cunningham Formation|64994|5|Briefly described|p8|||Basal beds contain transported shelly fauna of a Pragian age.||||||07-FEB-11
5031|Cunningham Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Molong. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
5031|Cunningham Formation|66197|5|Briefly described|p632, p633 Fig.4a, b|Emsian|Lochkovian|Capertee High-Hill End Trough. Mud dominated deep marine turbidites. Overlies Merrions Formation and Bay Formation.||||||13-MAR-12
5031|Cunningham Formation|67820|6|Mentioned|p136 Fig.3|Devonian|Devonian|||||||
5031|Cunningham Formation|68003|5|Briefly described|p24 Fig.3-e, p143. |Emsian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Tolga Member.||Phyllite, slate, shale, siltstone, quartz-feldspar-lithic calcareous sandstone, tuff.|
5031|Cunningham Formation|68592|2|Defined|p74 Tb.5, p177, p179-80, p681, p1205-13|Emsian|Pragian|Ungrouped. Near Tuena. These rocks were formerly assigned to the Trunkey Series (Booker, 1939) and Kildrummie and Campbells Groups (Packham, 1968). Named after Parish of Cunningham, County Wellington. Type section along the Turon River, 105 km N of Tuena, and a representative section E of Tuena, are described. Thickness may be 2250m. Cleared and generally rounded hills. Geophysical properties described. Poorly constrained age. Hosts several gold prospects including Trunkey gold field and Tuena area; also base metal mineralisation near contact with Box Ridge Volcanics. Peelwood structural zone: deformation described.|||Includes Copperhannia Member.|Conformably overlies Bushranger Volcanics. Is faulted against Campbells Formation and Box Ridge Volcanics.|Mostly fawn-coloured rocks; dominantly siltstone, in places ranging to phyllite; minor shale, and sandstone including doubtfully volcaniclastic bodies resembling Bushranger Volcanics. All outcrops affected by pervasive cleavage.|
5031|Cunningham Formation|70192|5|Briefly described|Map Legend|Pragian|Emsian|Dxn. Ungrouped Devonian formation. Age min boundary on Time-Space plot is marked with ?-?-?. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Copperhannia Member.|Overlies Bushrangers Volcanics (of Crudine Group).|Slaty siltstone with minor shale and sandstone [and limestone?].|
5031|Cunningham 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 represents final phase of sedimentation in the Hill End Trough after the end of volcanic activity. Also shown as Cunningham Fm.|||Copperhannia Member|Overlies Crudine Group.|Phyllite, slate, shale, siltstone, quartz-feldspar-lithic calcareous sandstone and tuff. Includes deep water sandstone, siltstone and minor conglomerate.|
5031|Cunningham Formation|70544|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Copperhannia Member||Slaty siltstone with minor shale and sandstone [and limestone?].|
5031|Cunningham Formation|71656|5|Briefly described|p13 Fig.2, p41|Emsian|Pridoli|Described under 'Ungrouped Devonian strata'.|||Includes Copperhannia Member.|Overlies Bushranger Volcanics.|Includes thin-bedded calcarenite and other fossiliferous strata.|
5031|Cunningham Formation|71924|5|Briefly described|p1, 2||Pragian|Includes poorly preserved allochthonous fauna of brachiopods, tetracorals, tabulate corals, rare trilobits and abundant crinoidal debris. Also includes conodonts. Lower part correlated with upper Mullamuddy Formation.||||Correlated with upper Mullamuddy Formation, Taylors Hill Formation and possibly Ingleburn Formation, Suchers Creek Formation.||
5031|Cunningham Formation|73299|6|Mentioned|p1096 Fig.3, p1098 Fig.4, p1102 Fig.8|Early Devonian|Late Silurian|Hill End Trough. Locations in text include p1105. [Map symbol suggests Devonian age]||||Overlies the Merrions Formation, Bay Formation, Tolga Member.||
5052|Curra Creek Conglomerate|22857|5|Briefly described|p492 App.1 Tb.A1.7||Late Devonian|Of the Canangle Subgroup (Catombal Group). Massive oligomictic conglomerate. Max. thickness: 1000m. Geological Province: Hervey Basin. ||||||
5052|Curra Creek Conglomerate|23043|5|Briefly described|Map Legend|Famennian|Famennian|of Canangle Subgroup, Catombal Group.||||||
5052|Curra Creek Conglomerate|23170|2|Defined|p254|Famennian|Late Devonian|of Canangle Subgroup.||||||
5052|Curra Creek Conglomerate|24247|5|Briefly described|p37, p42|Early Carboniferous|Famennian|Age is suggested by presence of fossils. Parent: Canangle Subgroup (Catombal Group)||||||
5052|Curra Creek Conglomerate|32151|6|Mentioned|p218|||Refers Conolly (1963)||||||
5052|Curra Creek Conglomerate|32708|6|Mentioned|Fig.6|||||||||
5052|Curra Creek Conglomerate|33732|4|Described|p119|||See also P120.||||||
5052|Curra Creek Conglomerate|33871|6|Mentioned|p2531|||||||||
5052|Curra Creek Conglomerate|34109|4|Described|p159|||Upper Devonian. Canangle Sub Group. See also P160||||||
5052|Curra Creek Conglomerate|43512|2|Defined|p73,77-8,85,88-93,96||Late Devonian|Massive red cgls interbedded with red&green Slts and Ss 3200ft th,subdiv.into 3 mbrs.p98-101,104,106||||||
5052|Curra Creek Conglomerate|43513|14|Not recorded|p72|||||||||
5052|Curra Creek Conglomerate|68003|5|Briefly described|p24 Fig.3-e, p142. |Famennian|Famennian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Canangle Subgroup.||Overlies Kurrool Formation.|Red-purple conglomerate, minor interbedded red-purple sandstone and siltstone.|
5052|Curra Creek Conglomerate|71600|5|Briefly described|p23 Fig 1|Devonian|Devonian|Geological province: Lachlan Fold Belt.||Unit of Catombal Group.|||Red-purple conglomerate, minor interbedded red-purple sandstone and siltstone.|
5052|Curra Creek Conglomerate|73299|6|Mentioned|p1105|Late Devonian|Late Devonian|||Catombal Group||Overlies the Kurrool Formation.||
5055|Currabubula Formation|721|5|Briefly described|Map legend|Stephanian|Namurian|Paraconglomerate and orthoconglomerate with subordinate pebbly sandstone, sandstone, mudstone, felsic ashflow and airfall tuff.  Geological Province: Tamworth Belt.||||||21-DEC-04
5055|Currabubula Formation|22572|6|Mentioned|p108||Carboniferous|||||||
5055|Currabubula Formation|22736|6|Mentioned|p628 Fig7||Namurian|||||||
5055|Currabubula Formation|22857|5|Briefly described|p240, p506 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Polymictic boulder paraconglomerate and orthoconglomerate, diamictite, lithic arenite, siltstone, carbonaceous siltstone, varved siltstone, felsic ashflow and airfall tuffs. See also p220.||||||
5055|Currabubula Formation|22859|6|Mentioned|p220|||||||||
5055|Currabubula Formation|22863|6|Mentioned|p240|||||||||
5055|Currabubula Formation|23102|5|Briefly described|p561|Late Carboniferous|Late Carboniferous|||||||
5055|Currabubula Formation|24010|6|Mentioned|p394 Fig. 11|||||||||
5055|Currabubula Formation|24040|5|Briefly described|p473|Late Carboniferous|Late Carboniferous|Contains rhyolites.||||||21-AUG-08
5055|Currabubula Formation|24334|5|Briefly described|p49 Tb.1|Westphalian|Namurian|Age: 305 - 314 Ma||||||
5055|Currabubula Formation|24348|5|Briefly described|p133 Fig.3, p134|Carboniferous|Carboniferous|||||||
5055|Currabubula Formation|24603|4|Described|p866|Stephanian|Westphalian|See also p869 Fig. 4, p886 Fig.11, p872 Tb.1.  Geological Province: Tamworth Belt - in Kankool Basin and Werrie Basin.||||||14-APR-08
5055|Currabubula Formation|30135|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
5055|Currabubula Formation|30340|6|Mentioned|p2530|||||||||
5055|Currabubula Formation|30341|5|Briefly described|p138|||||||||
5055|Currabubula Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
5055|Currabubula Formation|31883|6|Mentioned|Table 1|||||||||
5055|Currabubula Formation|32286|5|Briefly described|p56|||||||||
5055|Currabubula Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
5055|Currabubula Formation|32672|6|Mentioned|p674|||||||||
5055|Currabubula Formation|32866|6|Mentioned|Fig.3|||||||||
5055|Currabubula Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
5055|Currabubula Formation|34081|6|Mentioned|p261|||||||||
5055|Currabubula Formation|34083|4|Described|p248|||||||||
5055|Currabubula Formation|34085|6|Mentioned|Cor.chart|||Westphalian - Stephanian||||||
5055|Currabubula Formation|34238|6|Mentioned|p8|||||||||
5055|Currabubula Formation|35803|6|Mentioned|Fig.1|||||||||
5055|Currabubula Formation|36042|6|Mentioned|Fig.7|||||||||
5055|Currabubula Formation|36045|6|Mentioned|p329|||||||||
5055|Currabubula Formation|36253|6|Mentioned|p130|||||||||
5055|Currabubula Formation|36528|6|Mentioned|p180|||||||||
5055|Currabubula Formation|36940|6|Mentioned|p125|||||||||
5055|Currabubula Formation|36961|6|Mentioned|p210|||See also Fig.3 & P221.||||||
5055|Currabubula Formation|37919|6|Mentioned|p476|||||||||
5055|Currabubula Formation|38684|6|Mentioned|p17|||Geological Province: New England Fold Belt.||||||14-APR-08
5055|Currabubula Formation|38818|5|Briefly described|p169|Late Carboniferous|Late Carboniferous|Geological Province: New England Fold Belt.||||||14-APR-08
5055|Currabubula Formation|39287|6|Mentioned|p21|||See also Fig.2.2||||||
5055|Currabubula Formation|39299|5|Briefly described|p279|||||||||
5055|Currabubula Formation|39572|5|Briefly described|p135, p141|||Ignimbrites near top yielded K-Ar ages of 293 +/- 4 Ma (hornblende) and 302 +/- 4 Ma (plagioclase).||||||15-FEB-10
5055|Currabubula Formation|40246|6|Mentioned|p173|||||||||
5055|Currabubula Formation|40960|6|Mentioned|p230|||||||||
5055|Currabubula Formation|41009|6|Mentioned|p5|||||||||
5055|Currabubula Formation|41347|4|Described|Table 3|||||||||
5055|Currabubula Formation|41348|5|Briefly described|Map legend|Carboniferous||In the Tamworth Belt.||||||16-DEC-04
5055|Currabubula Formation|41611|5|Briefly described|p139|||||||||
5055|Currabubula Formation|41800|4|Described|p487|||||||||
5055|Currabubula Formation|41990|6|Mentioned|p6|||||||||
5055|Currabubula Formation|42214|6|Mentioned|p466|||||||||
5055|Currabubula Formation|42339|4|Described|p51|||||||||
5055|Currabubula Formation|42399|5|Briefly described|PB10|||||||||
5055|Currabubula Formation|42547|4|Described|p22|||||||||
5055|Currabubula Formation|42773|5|Briefly described|p349|||||||||
5055|Currabubula Formation|42849|5|Briefly described|p541|Late Carboniferous|Late Carboniferous|||||||09-MAY-05
5055|Currabubula Formation|42913|5|Briefly described|p9|||||||||
5055|Currabubula Formation|42987|5|Briefly described|p28|||||||||
5055|Currabubula Formation|42997|6|Mentioned|p42|||||||||
5055|Currabubula Formation|43091|5|Briefly described|Map legend|||||||||
5055|Currabubula Formation|43383|14|Not recorded|p17,18|||||||||
5055|Currabubula Formation|43409|14|Not recorded|Map Legend|||||||||
5055|Currabubula Formation|43418|14|Not recorded|Map Legend|||||||||
5055|Currabubula Formation|43432|14|Not recorded|p203||Visean|||||||
5055|Currabubula Formation|43435|14|Not recorded|Map Legend|||||||||
5055|Currabubula Formation|43446|14|Not recorded|p6026,6029,6032,||Late Carboniferous|p6033,6044,6049,||||||
5055|Currabubula Formation|43479|14|Not recorded|p159,177|Stephanian|Namurian|||||||
5055|Currabubula Formation|43545|4|Described|p418|||Formerly Upper Kuttung Series. From reprint. Correct reference not given.||||||14-APR-08
5055|Currabubula Formation|43718|6|Mentioned|Table 8.2,p129||Late Carboniferous|||||||
5055|Currabubula Formation|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
5055|Currabubula Formation|44450|5|Briefly described|p16|Late Carboniferous|Late Carboniferous|Geological Province: Tamworth Belt.||||||
5055|Currabubula Formation|44835|2|Defined|p43,45-48,50,52-54,||Westphalian|Pl.2.||||||
5055|Currabubula Formation|45097|5|Briefly described|p17|||See also P24. Floral assemblage. Correlation chart.||||||14-APR-08
5055|Currabubula Formation|47056|6|Mentioned|Fig.2 P523|||||||||
5055|Currabubula Formation|50613|5|Briefly described|p207|Namurian|Namurian|Of the Currangandi Group.||||||
5055|Currabubula Formation|50629|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: New England Orogen.||||||
5055|Currabubula Formation|60299|5|Briefly described|p209|Carboniferous|Carboniferous|Geological Province: Werrie Block.||||||
5055|Currabubula Formation|61201|5|Briefly described|p3|Carboniferous|Carboniferous|Overlain by Temi Formation and Werrie Basalt.||||||
5055|Currabubula Formation|61612|6|Mentioned|p270 Fig. 1|Late Carboniferous|Late Carboniferous|Geological Province: Gunnedah Basin.||||||13-MAR-09
5055|Currabubula Formation|61769|6|Mentioned|p95, p97||Late Carboniferous|||||||
5055|Currabubula Formation|61770|6|Mentioned|p108|||||||||
5055|Currabubula Formation|61776|5|Briefly described|p194 Fig. 3|Late Carboniferous|Carboniferous|Geological Province: New England Orogen. Conglomerate, sandstone, siltstone, tuff and minor limestone.||||||
5055|Currabubula Formation|61801|5|Briefly described|p403, p404|Late Carboniferous|Late Carboniferous|Consists of calc-alkaline volcanic arc derived fluviatile sedimentary rocks and calc-alkaline volcanic rocks. Overlain by the Temi Formation.||||||
5055|Currabubula Formation|62095|1|Redefined|p272 Appdx., p250, p255, p256 and Plate|Westphalian|Namurian|Synonymous with Upper Kuttung Series, Rossmore Formation and Currabubula Fm. Of Voisey and Williams (1964). Includes 18 members, some unnamed. Disconformably overlies Merlewood Fm., disconformably overlain by Woodton or Temi Fms. or Werrie Basalt.||||||13-MAR-09
5055|Currabubula Formation|63832|5|Briefly described|p131 fig 2, p134-135|Moscovian|Bashkirian|Werrie Syncline, Tamworth Belt. Third (C3) and fourth (C4) glaciations.|||Includes Rosedale Member.||Alluvial facies (mudrocks, sandstones and conglomerates) and pyroclastic rocks underlie glacial deposits of C3. Laminated mudrocks, diamictites, siltstone clast breccias, interbedded with lesser siltstones, sandstones and conglomerates, of C4.|13-DEC-17
5055|Currabubula Formation|64631|4|Described|pp47-49, p51, p54, p44 Fig.2.|Moscovian|Serpukhovian|Southern New England Fold Belt, Werrie Syncline. Contains intervals of continental proglacial strata. Some biostratigraphic and radiometric age control within unit. |||Includes Canah Creek Tuff and Taggarts Mountain Ignimbrite.||Thick intervals of alluvial sandstones and conglomerates, prominent pyroclastic members (ignimbrites), and intervals of laminated mudrocks and rhythmites, with lesser diamictites.|
5055|Currabubula Formation|64855|5|Briefly described|p34-35|Late Carboniferous|Late Carboniferous|Tamworth Belt. K-Ar ages of 293+/-4 and 302+/-4 Ma (McPhie 1984).||||||22-FEB-10
5055|Currabubula Formation|65107|6|Mentioned|Fig 9 p283|||Late Carboniferous?||||||
5055|Currabubula Formation|65382|6|Mentioned|p717 App. 2|||Includes Piallaway Trig Ignimbrite Member.||||||
5055|Currabubula Formation|65902|4|Described|p194, 197, 201-4, Figs. 2, 5, 6, 7|Carboniferous|Carboniferous|Includes Iventure, Taggarts Mountain, Piallaway Trig, Figtree Creek Ignimbrite Members, and Cana Creek Tuff Member. Also now includes Coeypolly Conglomerate Member. Correlates with Willuri Formation. Overlies Merlewood Formation. Formerly Upper Kuttung Series.||||||09-MAR-12
5055|Currabubula Formation|66720|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||Unit in Currangandi Group.|||Paraconglomerate and orthoconglomerate with subordinate pebbly sandstone, sandstone, mudstone, felsic ash flow and airfall tuff.|
5055|Currabubula Formation|68003|5|Briefly described|p32 Fig.3-h, p33, pp133-135.|Westphalian|Namurian|Tamworth Belt (South); New England Fold Belt. Coeval with lower Seaham Formation, and Willuri Formation to the north.|||This article includes at least 15 named Members.||Conglomerate, feldspathic and lithic sandstones, siltstone, mudstone; minor limestone; felsic ashflow and airfall tuff, rhyolitic-andesitic crystal and vitric tuff; ignimbrite; rhyodacite; dark grey andesite.|
5055|Currabubula Formation|68004|5|Briefly described|p65, p134, p207.|Late Carboniferous|Late Carboniferous|Werrie Basin. Conglomerates very similar to those of Temi Formation. Potential for zeolite production is discussed. Mis-spelt as Currububula Formation on p201.||||Is overlain by Temi Formation and Werrie Basalt.|Includes conglomerates.|
5055|Currabubula Formation|68005|5|Briefly described|p49 Fig.3-M, p57, pp139-141, p170.|Stephanian|Namurian|Werrie Block, Tamworth Belt. Of Whetten (1965). Includes all Late Carboniferous sedimentary rocks above the Merlewood Formation. Includes many (named and un-named) ignimbrite and tuff members.|||Includes Inglewood Member; Willawarra Dacite; and Cana Creek, Brogans, Iventure, Piallaway Trig and Taggarts Mountain, Ignimbrite Members.||Paraconglomerate, orthoconglomerate, crossbedded feldspathic and lithic sandstone, siltstone, mudstone and minor limestone. Felsic ashflow and airfall tuff, rhyolitic-andesitic crystal and vitric tuff. Also talus at base of Mooki Thrust escarpment.|
5055|Currabubula Formation|68006|5|Briefly described|p115, p130.|||Tamworth Belt. Contains extensive but thin and impure beds of limestone. Has the highest prospectivity for zeolite deposits in this study area.||||||
5055|Currabubula Formation|68822|6|Mentioned|p321|Late Carboniferous|Late Carboniferous|Includes clasts of quartz-rich sandstone, locally containing brachiopods.||||||
5055|Currabubula Formation|69793|6|Mentioned|p1121 Fig.12, p1122|Kasimovian|Bashkirian|Werrie Block, Tamworth Belt.||||||
5055|Currabubula Formation|70728|5|Briefly described|p265,271-273|Kasimovian|Bashkarian|Geological province: North Tamworth terrane, New England Orogen. Broadly correlable to Paddys Flat and Emu Creek formations. Contains SHRIMP zircon ages of 306+\-4.2 and 311.5+\-2.9  Ma at the top of the unit, and 315.3+\-2.5 and 317.9+\-3.7 Ma at the middle and bottom of the unit respectively (Roberts et al., 2003; Roberts et al., 2006; Roberts and James, 2010).||||Overlain by Woodton Formation. Underlain by Coepolly Conglomerate or Merlewood Formation.||
5055|Currabubula Formation|70777|6|Mentioned|p8|Carboniferous|Carboniferous|Werrie Block, New England Orogen.||||||
5055|Currabubula Formation|73197|5|Briefly described|p466, p467|Carboniferous|Carboniferous|New England Orogen, southern. Tamworth Belt. Forearc basin, preserves volcanic rocks sourced from the Currabubula-Connors Arc. Glacial till described by Whetton (1965).|||||Contains voluminous glacial till, also includes volcanic rocks, predominantly ignimbrite.|
5060|Currajong Limestone Member|22857|5|Briefly described|p462 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Taemas Limestone. Massive fossiliferous limestone. Max. thickness: 83m. Geological Province: Canberra-Yass Shelf.||||||
5060|Currajong Limestone Member|23898|4|Described|p270|Early Devonian|Early Devonian|Of Taemas Limestone. Overlain by Bloomfield Limestone Member.  Maximum Thickness: 83m.  Geological Province: Lachlan Fold Belt.||||||
5060|Currajong Limestone Member|24250|5|Briefly described|p105, p109 Fig5|Early Devonian|Early Devonian|Of the Taemas Limestone (Murrumbidgee Group). Maximum Thickness: 120m. Overlain by Bloomfield Limestone Member (conformable). Underlain by Spirifer yassensis Limestone Member (conformable)||||||18-JUN-08
5060|Currajong Limestone Member|32483|6|Mentioned|p33|||Refers Harper (1910)||||||
5060|Currajong Limestone Member|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
5060|Currajong Limestone Member|35386|4|Described|p53|||||||||
5060|Currajong Limestone Member|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
5060|Currajong Limestone Member|50230|4|Described|Map legend|Emsian|Emsian|Of the Taemas Limestone (Murrumbidgee Group).  Overlies the Spirifer Yassensis Limestone Member (Taemas Limestone) and underlies the Bloomfield Limestone Member.  Massive fossiliferous limestone.||||||
5060|Currajong Limestone Member|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Taemas Limestone (Murrumbidgee Group). Massive fossiliferous limestone.||||||
5060|Currajong Limestone Member|64992|5|Briefly described|p60 Fig. 1, p61|Devonian|Devonian|Part of the Taemas-Wee Jasper succession. Of the Taemas Formation. Overlain by Bloomfield Limestone Member. Contains Dipnorhynchus kurikae (lungfish) and Cathlorhynchus trismodipterus (new genus of lungfish). Bedded limestone.||||||26-MAR-09
5060|Currajong Limestone Member|65214|6|Mentioned|p272|Devonian|Devonian|NSW, Taemas. Appears in text as Currajong Limestone Mb. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
5060|Currajong Limestone Member|68592|2|Defined|p982,p984 Fig.162, p985-7, p1012-6,p1898|Emsian|Emsian|Referred to as The Currajong limestone by Harper (1909); more rigorously defined as Currajong Limestone by Browne (1959). Became a Member of Offenberg's (1974) Taemas Formation after its elevation from Taemas Stage. Type locality described. 47-122m thick. Large fauna described; silicification common. Good marker horizon. Characteristically supports kurrajong trees.||Unit in Taemas Limestone.||Conformably overlies Spirifer yassensis Limestone Member. Is overlain conformably by Bloomfield Limestone Member.|Thin- to thick-bedded, massive or laminated, blue-grey fossiliferous limestone: bioclastic crinoidal limestone, sparsely fossiliferous bedded limestone, and richly fossiliferous silicified limestone.|
5060|Currajong Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmtc. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Taemas Limestone||Overlies Spirifer yassensis Limestone Member. Is overlain Bloomfield Limestone Member.|Blue-grey, massive-well laminated, thinly-thickly bedded, fossiliferous limestone.|
5060|Currajong Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, massive-well laminated, thinly-thickly bedded, fossiliferous limestone.|
5060|Currajong Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Blue-grey, massive-well laminated, thinly-thickly bedded, fossiliferous limestone.|
5060|Currajong Limestone Member|71656|4|Described|p12 Fig.2, p34-35|Emsian|Emsian|Contains species of conodonts identical to those in the underlying Spirifer yassensis Limestone Member.||Of Taemas Limestone, Murrumbidgee Group.||Overlies Spirifer yassensis Limestone Member and underlies Bloomfield Limestone Member.|Includes banded fossiliferous limestone in early parts of strata.|
5065|Currambene Dolerite|29750|6|Mentioned|p1|||||||||
5065|Currambene Dolerite|29752|6|Mentioned|p5|||||||||
5065|Currambene Dolerite|35524|6|Mentioned|p75|||||||||
5065|Currambene Dolerite|36042|6|Mentioned|p41|||||||||
5065|Currambene Dolerite|36954|6|Mentioned|Fig.1|||||||||
5065|Currambene Dolerite|37253|6|Mentioned|Table 1|||||||||
5065|Currambene Dolerite|39289|6|Mentioned|p79|||Age||||||
5065|Currambene Dolerite|45090|6|Mentioned|p83|||Table of Permian igneous rocks||||||
5068|Currangorambla Granophyre|39409|6|Mentioned|Table XVII|||||||||
5077|Currawinya Conglomerate|31694|6|Mentioned|p348|||||||||
5077|Currawinya Conglomerate|32086|2|Defined|p326|Late Carboniferous|Late Carboniferous|See also P325||||||
5077|Currawinya Conglomerate|36528|6|Mentioned|p171|||See also P182.||||||
5077|Currawinya Conglomerate|36936|6|Mentioned|p211|||||||||
5077|Currawinya Conglomerate|36961|6|Mentioned|p212|||||||||
5077|Currawinya Conglomerate|68679|6|Mentioned|p351|||North of Drake (NSW); similar acid igneous clasts to those in the Mount Barney beds across the QLD border near Mount Barney.||||||
5084|Currowong Granodiorite|22815|4|Described|p56|Silurian|Silurian|Rb/Sr Age: 415.3+/-3.7 Ma.||||||
5084|Currowong Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
5084|Currowong Granodiorite|40328|4|Described|p205|||||||||
5084|Currowong Granodiorite|41905|2|Defined|p57|Silurian||||||||
5084|Currowong Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
5084|Currowong Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Currowong Suite.||||||
5085|Currowong Suite|22719|6|Mentioned|p485|||||||||
5085|Currowong Suite|22815|5|Briefly described|p57|Silurian|Silurian|||||||
5085|Currowong Suite|22877|5|Briefly described|map|Silurian|Silurian|||||||
5085|Currowong Suite|23549|5|Briefly described|p518, p524|||Geological Province:  Berridale Batholith.||||||05-APR-05
5085|Currowong Suite|24551|6|Mentioned|p235, 729 Table 8.12|||Of the Kuark Province||||||
5085|Currowong Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
5085|Currowong Suite|42627|5|Briefly described|Map legend|Wenlock||||||||
5085|Currowong Suite|42726|5|Briefly described|map legend||Silurian|Of the Currowong Supersuite.  Includes the Currowong, Bimbimbie, Iona, Bonang and Brodribb Granites.||||||09-FEB-05
5085|Currowong Suite|42827|5|Briefly described|p431|||||||||
5085|Currowong Suite|43233|5|Briefly described|Map Legend|Late Silurian||of Berridale Batholith.||||||
5085|Currowong Suite|67060|5|Briefly described|p503, p505 Table 1.|||Southern Berridale Batholith. I-type. Includes the compositionally-similar Iona, Currowong and Bimbimbie plutons.|c.417 Ma.|||||15-MAR-12
5085|Currowong Suite|72571|6|Mentioned|p88, p90-91, 94, 97, 99-101,103,105-107|||Of the Tasmanides of eastern Australia. I-type. Exhibits petrographic features and preserves geochemical and isotopic compositions that do not lend themselves to a simple restite or magma mixing model.|||Includes the Bimbimbie Granodiorite.|||
5087|Currowong Supersuite|42726|5|Briefly described|map legend|||Includes the Currowong, Goongerah, and Jungke Creek Suites.||||||09-FEB-05
5087|Currowong Supersuite|42827|5|Briefly described|p431|||||||||
5090|Currumbene Siltstone Member|45090|6|Mentioned|p218|||Kazanian||||||
5094|Cusack Creek Conglomerate Member|32127|6|Mentioned|p253|||Renaming Cusack Creek Member?||||||
5094|Cusack Creek Conglomerate Member|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Lochiel Formation (Budawang Rift). Geological Province: Lambian Transitional Province.||||||
5097|Cut Hill Formation|32324|6|Mentioned|Table 8.1|||||||||
5097|Cut Hill Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
5097|Cut Hill Formation|32868|6|Mentioned|p208,Fig.7|||||||||
5097|Cut Hill Formation|35492|6|Mentioned|Fig.2|||Stratigraphic table||||||
5097|Cut Hill Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
5097|Cut Hill Formation|36599|6|Mentioned|Fig.1|||||||||
5097|Cut Hill Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Tamworth Belt.||||||16-DEC-04
5097|Cut Hill Formation|42547|6|Mentioned|p36|||||||||
5119|Daalboro Sandstone|9548|5|Briefly described|Map Legend|Zlichovian|Pragian|Of the Yarra Yarra Creek Group. Underlies: Inverleith Sandstone.  Overlies: Myamely Sandstone.||||||06-JUL-04
5119|Daalboro Sandstone|22831|3|Fully described|p 55|||||||||
5119|Daalboro Sandstone|22857|4|Described|p446 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Yarra Yarra Creek Group. Max. thickness: <75m. Geological Province: Darling Basin.||||||03-MAR-06
5119|Daalboro Sandstone|24417|5|Briefly described|p78|||Of Yarra Yarra Creek Group.||||||
5119|Daalboro Sandstone|42449|6|Mentioned|p24|||Reserved 1977, D. Pogson. Last update May 1991.||||||
5119|Daalboro Sandstone|42566|5|Briefly described|Fig.25 P103|||||||||
5119|Daalboro Sandstone|43441|6|Mentioned|29||Early Devonian|||||||08-JAN-10
5119|Daalboro Sandstone|44160|5|Briefly described|Map Legend||Pragian|||||||08-JAN-10
5119|Daalboro Sandstone|61894|6|Mentioned|p179 Fig.3|||||||||
5119|Daalboro Sandstone|70751|6|Mentioned|p12|Lochkovian|Lochkovian|||Yarra Yarra Creek Group||||
5119|Daalboro Sandstone|72958|6|Mentioned|p11|Lochkovian|Lochkovian|Cobar Basin. Nymagee area.||Yarra Yarra Creek Group, Cobar Supergroup||Underlain by Myamley Sandstone. Overlain by Inverleith Sandstone.||
5129|Dakiel Formation|30451|4|Described|p27|||||||||
5129|Dakiel Formation|31586|5|Briefly described|p6|||Fauna||||||
5129|Dakiel Formation|31587|6|Mentioned|p60|||Lithostrotion species distribution||||||
5129|Dakiel Formation|31659|6|Mentioned|p54|||Part of Caswell Ck. Gp.||||||
5129|Dakiel Formation|32866|6|Mentioned|p25|||Fossil content||||||
5129|Dakiel Formation|32867|6|Mentioned|p60|||||||||
5129|Dakiel Formation|32868|6|Mentioned|p208,Fig.7|||||||||
5129|Dakiel Formation|34155|6|Mentioned|p94||Early Carboniferous|Lower Carboniferous. Caswell Creek Group.||||||20-AUG-09
5129|Dakiel Formation|39445|5|Briefly described|Table 6|||||||||
5129|Dakiel Formation|42547|5|Briefly described|p51|||||||||
5129|Dakiel Formation|44360|2|Defined|p1-4,7,10-12,18,21,||Visean|p23-28,30-33,35,map.Unit of Caswell Creek Group.||||||
5129|Dakiel Formation|44379|14|Not recorded|p15|||Ref. to McKellar 1967.||||||
5129|Dakiel Formation|45097|6|Mentioned|Fig.|||Correlation Chart||||||
5129|Dakiel Formation|46803|6|Mentioned|Fig. 4|||||||||
5129|Dakiel Formation|50190|5|Briefly described|p39, 21, 59|Carboniferous|Carboniferous|Of the Casell Creek Group.||||||
5129|Dakiel Formation|68008|6|Mentioned|p596|||An area N of Cannindah Creek, previously mapped as this unit, has been assigned to Lorray Formation.||||||
5142|Dalgety Granodiorite|22815|4|Described|p56|Silurian|Silurian|Rb/Sr Ages: 416.4 Ma, 419.1 Ma, 413.1 Ma.||||||
5142|Dalgety Granodiorite|23551|5|Briefly described|p490|||S-type granite. Berridale Batholith.||||||
5142|Dalgety Granodiorite|33779|6|Mentioned|p168|||Map||||||
5142|Dalgety Granodiorite|33780|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
5142|Dalgety Granodiorite|33852|6|Mentioned|p502|||Date given.||||||
5142|Dalgety Granodiorite|33959|6|Mentioned|p234|||Fig.||||||
5142|Dalgety Granodiorite|35109|2|Defined|p42|Early Devonian|Late Silurian|Late Silurian to Early Devonian.||||||18-FEB-08
5142|Dalgety Granodiorite|36411|6|Mentioned|p268|||Refers White et al 1977 for definition.||||||
5142|Dalgety Granodiorite|38327|6|Mentioned|Table 4|||||||||
5142|Dalgety Granodiorite|38500|6|Mentioned|p81|||||||||
5142|Dalgety Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
5142|Dalgety Granodiorite|40328|4|Described|p205|||||||||
5142|Dalgety Granodiorite|41905|2|Defined|p46|Silurian||||||||
5142|Dalgety Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
5142|Dalgety Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Of the Dalgety Suite.||||||18-FEB-08
5142|Dalgety Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb21.||||||
5142|Dalgety Granodiorite|49705|5|Briefly described|p43|||||||||
5142|Dalgety Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
5142|Dalgety Granodiorite|72528|5|Briefly described|p12, p108.|Wenlock|Llandovery|Age is indistinguishable from porphyry dyke that intrudes the Warbisco Shale and is associated with Cu-Au mineralisation.|435.1+/-4.4 Ma||||Includes granodiorite.|01-FEB-21
5142|Dalgety Granodiorite|72571|6|Mentioned|p90, p94, p96-100|||Of the Tasmanides of eastern Australia. Petrography of sample and zircon description and analyses are discussed in detail. S-type.||||||
5143|Dalgety Suite|22815|5|Briefly described|p56|Silurian|Silurian|Consists of 7 plutons.||||||18-FEB-08
5143|Dalgety Suite|24222|5|Briefly described|p11|||Chemistry of samples reported. S-type granite, felsic.  Geological Province: Berridale Batholith, Lachlan Fold Belt.||||||
5143|Dalgety Suite|24551|6|Mentioned|p234, 728 Table 8.11|||||||||
5143|Dalgety Suite|41563|6|Mentioned|p512|||||||||
5143|Dalgety Suite|41905|6|Mentioned|p42|||||||||
5143|Dalgety Suite|41933|5|Briefly described|Map legend|||||||||
5143|Dalgety Suite|42726|5|Briefly described|map legend||Silurian|Of the Dalgety Supersuite.  Includes nine 'granite' units.||||||09-FEB-05
5143|Dalgety Suite|42827|6|Mentioned|p431|||||||||
5143|Dalgety Suite|43233|5|Briefly described|Map Legend|Late Silurian||Of Berridale Batholith.||||||18-FEB-08
5143|Dalgety Suite|44093|5|Briefly described|p190 App. 1|Early Devonian|Silurian|||||||
5143|Dalgety Suite|67060|5|Briefly described|p503, p505 Table 1.|||Includes two S-type, N-S trending plutons: the granodioritic Dalgety pluton and the granitic Numbla Vale pluton.|435 +/- 4.4 Ma.|||||15-MAR-12
5143|Dalgety Suite|68592|5|Briefly described|p1253-4, p1264|||A discontinuous string of 9 plutons stretching 100km south from Lake Eucumbene into Victoria.||Unit in Wyangala Supersuite.|||Equigranular, non-fractionated granitoids.|
5143|Dalgety Suite|72571|6|Mentioned|p90, p92, p97, p100|||Of the Tasmanides of eastern Australia.||||||
5145|Dalgety Supersuite|22876|5|Briefly described|p28|||||||||
5145|Dalgety Supersuite|22877|5|Briefly described|map|Silurian|Silurian|||||||
5145|Dalgety Supersuite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|||||||18-FEB-08
5145|Dalgety Supersuite|42726|5|Briefly described|map legend|||Includes the Dalgety Suite, containing 9 'granite' units.||||||09-FEB-05
5145|Dalgety Supersuite|42827|6|Mentioned|p431|||||||||
5150|Dalmally Basalt Member|22833|6|Mentioned|p653|||Age: 237+/-0.4 Ma. of Sydney Basin.||||||
5150|Dalmally Basalt Member|32801|6|Mentioned|Fig.5|||||||||
5150|Dalmally Basalt Member|32803|2|Defined|p79|Triassic|Triassic|||||||
5150|Dalmally Basalt Member|35161|6|Mentioned|p592|||||||||
5150|Dalmally Basalt Member|35503|6|Mentioned|p201|||Defined in Retallack, Gould and Runnegar (1977)||||||
5150|Dalmally Basalt Member|36954|6|Mentioned|Fig.1|||See also p114.||||||
5150|Dalmally Basalt Member|37757|6|Mentioned|p29|||||||||
5150|Dalmally Basalt Member|61310|5|Briefly described|Table C1 (p22-23)|Middle Triassic|Middle Triassic|Of the Bardool Conglomerate (Nymboida Coal Measures). Subalkaline vesicular basalt. Geological Province: Clarence-Moreton Basin.||||||
5150|Dalmally Basalt Member|73306|5|Briefly described|p565-566|Late Triassic|Middle Triassic||c.237 Ma (Ar/Ar; Retallack et al., 1993).|Bardool Conglomerate.||||
5170|Danberry loamy sand|39512|6|Mentioned|p2|||||||||
5187|Dapto Latite Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
5187|Dapto Latite Member|22488|4|Described|p840-3|||||||||
5187|Dapto 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 Fm. and Pheasants Nest Fm. (Illawarra C.M.) together form Gerringong volcanic facies. Geological Province: Sydney Basin.||||||
5187|Dapto Latite Member|23544|5|Briefly described|Table 1 p360.|||Of the Broughton Formation.||||||
5187|Dapto Latite Member|29900|6|Mentioned|p175|||||||||
5187|Dapto Latite Member|29901|4|Described|Table 1|||||||||
5187|Dapto Latite Member|31128|6|Mentioned|Table 1|||||||||
5187|Dapto Latite Member|32938|6|Mentioned|p67|||Geology||||||
5187|Dapto Latite Member|35189|6|Mentioned|p385|||||||||
5187|Dapto Latite Member|36220|4|Described|p38|||See also P95 & Table 1.||||||
5187|Dapto Latite Member|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
5187|Dapto Latite Member|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
5187|Dapto Latite Member|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
5187|Dapto Latite Member|38690|4|Described|p292|||||||||
5187|Dapto Latite Member|40270|6|Mentioned|Table 1|||||||||
5187|Dapto Latite Member|40519|6|Mentioned|Fig.3|||||||||
5187|Dapto Latite Member|42737|5|Briefly described|map legend|Permian||||||||
5187|Dapto Latite Member|42896|4|Described|p15|||of Shoalhaven Group; age of 251 +/- 5 Ma||||||
5187|Dapto Latite Member|67500|5|Briefly described|p12 Tb.1, p16|Late Permian|Late Permian|Up to 85m thick.||Of the Broughton Formation and Gerringong volcanic facies|||Two porphyritic flows, separated by breccia.|01-MAY-12
5187|Dapto Latite Member|71115|5|Briefly described|p178-180, 182-185, 187-188, 191-192, 195|Permian|Permian|Southern Sydney Basin. Note revised stratigraphic location of this Member and Saddleback Latite Member. Geochemically similar to Saddleback Latite Member. Paleomagnetic results tabulated, discussed. Flow direction to the NE.||Gerringong Volcanics.||Overlies Jamberoo Sandstone. Is overlain by Saddleback Latite Member.|A lower flow of green porphyritic basalt with large plagioclase laths and secondary calcite-filled amygdales, and a darker upper flow with elongate plagioclase crystals aligned layer parallel.|
5187|Dapto Latite Member|71542|6|Mentioned|p25|Late Permian|Late Permian|Of southern Sydney Basin.||Unit of Gerringong Volcanics.||Within Broughton Formation.||20-OCT-21
5187|Dapto 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.|
5221|Darkes Forest Sandstone|22578|6|Mentioned|Fig.10 p400|||||||||
5221|Darkes Forest Sandstone|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Sydney Subgroup||||||
5221|Darkes Forest Sandstone|24157|5|Briefly described|p209 Fig.19|||Parent: Illawarra Coal Measures. Geological Province: Sydney Basin||||||
5221|Darkes Forest Sandstone|24471|4|Described|p32 Fig.4, p33|Late Permian|Late Permian|Deltaic. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Waratah Sandstone. Geological Province: Sydney Basin.||||||07-FEB-11
5221|Darkes Forest Sandstone|29900|5|Briefly described|Fig.4|||||||||
5221|Darkes Forest Sandstone|29901|4|Described|Table 1|||||||||
5221|Darkes Forest Sandstone|29944|6|Mentioned|Fig.18|||||||||
5221|Darkes Forest Sandstone|30006|4|Described|p13|||||||||
5221|Darkes Forest Sandstone|31128|6|Mentioned|Table 1|||||||||
5221|Darkes Forest Sandstone|31887|5|Briefly described|p5|||||||||
5221|Darkes Forest Sandstone|33334|6|Mentioned|Table 3|||Perm.||||||
5221|Darkes Forest Sandstone|34060|6|Mentioned|p24|||Perm. Table||||||
5221|Darkes Forest Sandstone|36042|6|Mentioned|Fig.20|||||||||
5221|Darkes Forest Sandstone|36220|4|Described|p52|||See also Table 1 & P49.||||||
5221|Darkes Forest Sandstone|37087|6|Mentioned|p198|||||||||
5221|Darkes Forest Sandstone|39232|6|Mentioned|p105|||See also P110||||||
5221|Darkes Forest Sandstone|39287|6|Mentioned|Fig. 2.15|||||||||
5221|Darkes Forest Sandstone|39309|5|Briefly described|p127|||Isopach map Fig. 7.3||||||
5221|Darkes Forest Sandstone|40166|6|Mentioned|p348|||See also Table 1||||||
5221|Darkes Forest Sandstone|40321|6|Mentioned|Fig.3|||||||||
5221|Darkes Forest Sandstone|40602|6|Mentioned|p7|||||||||
5221|Darkes Forest Sandstone|40744|6|Mentioned|Table 1|||||||||
5221|Darkes Forest Sandstone|42787|5|Briefly described|p133|||||||||
5221|Darkes Forest Sandstone|42896|4|Described|p21|||Of Sydney Subgroup.||||||12-MAR-09
5221|Darkes Forest Sandstone|42925|5|Briefly described|Table 18||Late Permian|||||||
5221|Darkes Forest Sandstone|43194|5|Briefly described|p130|Late Permian|Late Permian|Sydney Basin. Deposited during a marine incursion during the Late Permian.||||||
5221|Darkes Forest Sandstone|45090|6|Mentioned|p189|||Refers Bowman (1970)||||||
5221|Darkes Forest Sandstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
5221|Darkes Forest Sandstone|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
5221|Darkes Forest Sandstone|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Bargo Claystone. Is overlain by Allans Creek Formation.||
5221|Darkes Forest Sandstone|68003|6|Mentioned|p41.|Late Permian|Late Permian|Sydney Basin. A marine incursion interrupting coal formation.||||||
5221|Darkes Forest Sandstone|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
5221|Darkes Forest Sandstone|73421|5|Briefly described|p3, p19|Wuchiapingian|Wuchiapingian|Sydney Basin, southern. Misspelt as Drakes Forest Sandstone p19.||Sydney Subgroup||Overlies Bargo Claystone, underlies Allans Creek Formation|Sandstone with cross bedding in parts.|
5274|Davies Creek Granite|22679|6|Mentioned|p 28|||||||||
5274|Davies Creek Granite|23214|3|Fully described|p174|Early Devonian|Late Silurian|Intrudes Rockley Volcanics. Comprises of a series of syntectonic S-type granophyre dykes and stocks.||||||
5274|Davies Creek Granite|33004|6|Mentioned|p181|||||||||
5274|Davies Creek Granite|33006|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Prob.Middle Devonian||||||
5274|Davies Creek Granite|33007|5|Briefly described|p12|||Genesis & history.||||||
5274|Davies Creek Granite|33282|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
5274|Davies Creek Granite|33285|6|Mentioned|p19|||||||||
5274|Davies Creek Granite|33732|6|Mentioned|p117|||||||||
5274|Davies Creek Granite|34255|6|Mentioned|p202|||Early - Mid Devonian||||||
5274|Davies Creek Granite|34400|6|Mentioned|p8|||||||||
5274|Davies Creek Granite|34406|6|Mentioned|p224|||||||||
5274|Davies Creek Granite|34544|6|Mentioned|p193|||||||||
5274|Davies Creek Granite|40328|4|Described|p205|||||||||
5274|Davies Creek Granite|42712|4|Described|8, 16; Table 1 p14.|Early Devonian|Late Silurian|||||||
5274|Davies Creek Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
5274|Davies Creek Granite|43469|4|Described|p131,132,142-143||Early Devonian|(Bowning)||||||26-FEB-14
5274|Davies Creek Granite|43515|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition) See also Lexicon||||||
5274|Davies Creek Granite|43516|14|Not recorded|Map Legend||Middle Devonian|(U.M.Dev)||||||
5274|Davies Creek Granite|43639|5|Briefly described|Map Legend||Silurian|||||||
5274|Davies Creek Granite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|||||||
5274|Davies Creek Granite|44093|5|Briefly described|p207 App. 1|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
5274|Davies Creek Granite|68592|6|Mentioned|p1542|||||Unit in Wologorong Supersuite.||||
5274|Davies Creek Granite|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Wologorong Supersuite||||
5274|Davies Creek Granite|73431|5|Briefly described|p362-367, p369-370, p372, p374-375|Silurian|Silurian|Lachlan Orogen. Includes two plutons, cut by a series of N-S striking Carboniferous dolerite dykes and some syn-tectonic granophyre dykes. Intrudes Macquarie Arc. Compositionally plots on I-, S-type transitional line of Chappell et al., (1998). The sampled Davies Creek Granite dykes of aplite has igneous age of 394.6+/-1.7 Ma, and inherited granite age of 434.7+/-1.5 Ma, eHf values of -5.1 to +4.7. Granite age is coeval with Sunset Hills Granite and Canowindra Volcanics. Aplite dyke is coeval with recrystallisation age of Browns Creek Igneous Complex granodiorite. Previous Rb-Sr biotite age of 327+/-1.6 Ma (Lennox et al., 1998). Contains rare xircon zenocrysts. Location in text includes p371 Fig.7, p373 Fig.8.|434.7+/-1.5 Ma SHRIMP zircon U-Pb, 327+/-1.6 Ma|||Intrudes Rockley Volcanics|Includes aplite dykes.|
5275|Davies Plains Limestone Member|32590|6|Mentioned|p13|||||||||
5279|Davys Plains Limestone Member|23214|3|Fully described|p37|Eastonian|Eastonian|Of Daylesford Limestone. For lithology description see Semeniuk (1973a,b). 95m thick at type section.||||||
5279|Davys Plains Limestone Member|33063|2|Defined|p81|Ordovician|Ordovician|||||||
5279|Davys Plains Limestone Member|33064|4|Described|p450|||See also PP454,455. Stratigraphy.||||||
5279|Davys Plains Limestone Member|33065|6|Mentioned|Table 1|||Lithology||||||
5279|Davys Plains Limestone Member|33737|6|Mentioned|p182|||||||||
5279|Davys Plains Limestone Member|33740|6|Mentioned|Fig.1|||||||||
5279|Davys Plains Limestone Member|35646|6|Mentioned|Fig.6|||||||||
5279|Davys Plains Limestone Member|40136|6|Mentioned|p23|||||||||
5279|Davys Plains Limestone Member|41046|6|Mentioned|Fig.2|||||||||
5279|Davys Plains Limestone Member|42479|5|Briefly described|p111|||||||||
5279|Davys Plains Limestone Member|70684|5|Briefly described|p39 Fig.17|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Daylesford Limestone.||||
5279|Davys Plains Limestone Member|73210|5|Briefly described|p893|||Semeniuk (1973, 2011). Exhibits subaerial disconformities and diagenesis/pedogenesis. See also Davys Creek Limestone Member (p903).||Daylesford Limestone.|||Pisolite- and lithoclast-dominated limestone.|
5283|Dawes Range Group|34085|6|Mentioned|Cor.chart|||Famennian||||||
5290|Days Creek Gabbro|23720|5|Briefly described|Map Legend|Early Permian|Early Permian|Olivene-hypersthene and hypersthene gabbro, agmatite, minor diorite and granite.||||||15-DEC-04
5290|Days Creek Gabbro|30787|6|Mentioned|p45|||See also p46.||||||18-FEB-08
5290|Days Creek Gabbro|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||18-FEB-08
5290|Days Creek Gabbro|30911|6|Mentioned|Map legend|Permian|Permian|||||||
5290|Days Creek Gabbro|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
5290|Days Creek Gabbro|44450|5|Briefly described|p57 Fig 8|||Geological Province: New England Fold Belt.||||||
5290|Days Creek Gabbro|71628|4|Described|p2: 3, 27-33, 61; p3: 2, 92-93, 95|||See also  p8: 92, 96. Binns et al. (1967) after Neilson (1965). Named after a watercourse of that name. Located 17 km E of Guyra. Comprises two small elevated plutons. Has a 100m -wide aureole (described). Assigned to Bakers Creek Suite by Landenberger (1996); assigned to Bakers Creek Supersuite by Landenberger et al. (2010). Separate detailed descriptions by different workers are given. Geochemistry detailed.|305.1 +/- 2.9 Ma (SHRIMP: McKibbin et al., 2017).|Bakers Creek Supersuite.||Intrudes Girrakool beds. Is intruded by Wards Mistake and Tobermory Monzogranites.|Dominantly tholeiitic: coarse-grained opx gabbro to opx leucogabbro, lesser olivine-opx gabbro to olivine-opx leucogabbro; local pegmatitic and granular variants; granoblastic to sparsely porphyritic; minor segregations of diorite and granite.|
5291|Daysdale Granite|22857|5|Briefly described|p213|Devonian|Devonian|Pink and porphyritic. Geological Province: Barka Basin.||||||24-MAR-06
5291|Daysdale Granite|22859|6|Mentioned|p213|||||||||
5291|Daysdale Granite|42726|5|Briefly described|map legend|||||||||
5292|De Drack Formation|22624|6|Mentioned|p683|Late Silurian|Late Silurian|||||||
5292|De Drack Formation|22768|6|Mentioned|p176|||||||||
5292|De Drack Formation|22857|4|Described|p176, p474 App.1 Tb.A1.6|Ludlovian|Ludlovian|Of the Mount Fairy Group. Time correlative of Woodlawn Volcanics. Chert-rich conglomerate, quartzose siltstone, fine-grained arenite; contains graptolites. Max. thickness: >300m estimated.||||||
5292|De Drack Formation|23048|5|Briefly described|p6 fig9|Late Silurian|Silurian|||||||
5292|De Drack Formation|23309|6|Mentioned|p390|||||||||
5292|De Drack Formation|30730|4|Described|p7|||Silurian||||||
5292|De Drack Formation|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
5292|De Drack Formation|30735|2|Defined|p16|Silurian|Silurian|||||||
5292|De Drack Formation|30736|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
5292|De Drack Formation|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
5292|De Drack Formation|31161|5|Briefly described|PA7|||||||||
5292|De Drack Formation|31411|5|Briefly described|p16|||||||||
5292|De Drack Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
5292|De Drack Formation|32672|6|Mentioned|p672|||||||||
5292|De Drack Formation|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
5292|De Drack Formation|34713|6|Mentioned|p118|||||||||
5292|De Drack Formation|35503|6|Mentioned|p201|||Redefined in Felton and Huleatt (1977)||||||
5292|De Drack Formation|35662|6|Mentioned|p139|||Geology of the Woodlawn district.||||||
5292|De Drack Formation|36413|6|Mentioned|Table 3|||||||||
5292|De Drack Formation|37727|4|Described|p54|||||||||
5292|De Drack Formation|39028|6|Mentioned|Map legend|Ludlovian|Ludlovian|||||||
5292|De Drack Formation|39143|6|Mentioned|p226|||||||||
5292|De Drack Formation|39331|6|Mentioned|p56|||See P57||||||
5292|De Drack Formation|40276|2|Defined|p3|Late Silurian|Late Silurian|||||||
5292|De Drack Formation|40328|4|Described|p185|||||||||
5292|De Drack Formation|42414|6|Mentioned|p60|||||||||
5292|De Drack Formation|42497|5|Briefly described|Map Legend|Ludlovian|Ludlovian|||||||
5292|De Drack Formation|42820|5|Briefly described|Fig.16|||of Mount Fairy Group||||||
5292|De Drack Formation|43659|6|Mentioned|p4|||||||||
5292|De Drack Formation|44093|5|Briefly described|p221 App. 1|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
5292|De Drack Formation|50234|5|Briefly described|Map Legend|Ludlow|Wenlock|Of Mount Fairy Group.  Interbedded with the Joppa Formation.||||||13-MAY-04
5292|De Drack Formation|62070|5|Briefly described|p37, p38|Ludlow|Ludlow|||Mount Fairy Group.||Underlies the Long Flat Volcanics.|Interbedded quartz arenite, siltstone and shale with laterally restricted limestone bodies.|
5292|De Drack Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Mount Fairy Group. Includes the Wowagin Dacite, Sooley Volcanic, Kingsdale Limestone and Joppa Siltstone Members. Siltstone and quartzose to feldspar-lithic-quartz sst+ fossiliferous limest., marble + calc-arenite; lesser rhyolite to dacite lava..||||||09-SEP-08
5292|De Drack Formation|66087|4|Described|p5-6, 11, Figs 2-3|Late Silurian|Middle Silurian|Intruded by ?Early Devonian monzodiorites and dolerites. Hosts the Collector deposit.||Of the Mount Fairy Group.||Overlain by Woodlawn Volcanics.|Is hornfelsed, with massive fossiliferous marble, shales, fine grained siltstones, quartzose sandstones, tuffaceous sandstones and tuffs.|10-MAY-12
5292|De Drack Formation|67820|6|Mentioned|p136 Fig.3|Late Silurian|Silurian|||Mount Fairy Group.||||
5292|De Drack Formation|68592|2|Defined|p726-30, p760-96, p797-8, p801-3, 806-8|Late Silurian|Early Silurian|See also p209-10, p813-5, p818, p820-1, p824, p833, p1669, p1672, p1888-9. On Goulburn 1:250 000, this unit occurs in a discontinuous north-northeasterly oriented belt. Occupies ridges and slopes with gentle gradients; actual outcrops are uncommon (except road cuttings). Type section (in Braidwood 1:100 000) is not representative; other localities are provided. Thickness: min. ~300 m; max. ~ 2.5 km, base not visible or faulted. Age: probably early Wenlock to mid-Ludlow (middle to Late Silurian), on palaeontological grounds. Graptolitic siltstone and shale of uppermost De Drack Formation and Kerrawary Siltstone occupy same stratigraphic position directly beneath Covan Creek Formation. Fossil fauna of some Members listed. Hosts a massive pyrrhotite-pyrite (with minor Zn-Cu-Pb) prospect at Collector (detailed).||Unit in Mount Fairy Group.|Wowagin Dacite, Sooley Volcanic, Joppa Siltstone, Members; Sandhills Creek, Fairy Meadow, Bendethera, Wyanbene, Marble Arch, Cheitmore and Kingsdale, Limestone Members.|Overlies Shivering Conglomerate and Woodlawn Volcanics. Overlain by Argyle Formation and Covan Creek Formation (conformably) where volcanic units are not present. Intruded by Bishopthorpe Dolerite.|Diverse; predominantly fine-grained clastic lithologies and limestone; includes quartzose sandstone.|
5292|De Drack Formation|69159|5|Briefly described|Map legend|Devonian|Silurian|Six un-named sub-units are separately mapped.||Unit in Mount Fairy Group.|Includes Sandhills Creek Limestone Member.||Undivided: siltstone and quartzose, quartzofeldspathic and feldspar-lithic-quartz sandstone and fossiliferous limestone, marble and calc-arenite. Lesser rhyolite lava, rhyolitic volcanic sandstone and polymictic conglomerate.|
5292|De Drack Formation|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sfd. Includes 4 named units and 6 unnamed units. Unnamed units include: sandstone and minor siltstone/sandstone; barite with ferruginous laminae; pyritic shale/mudstone/siltstone and limestone blocks; fossiliferous limestone and marble with minor marl; rhyolite to dacite; siltstone with subordinate sandstone. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Mount Fairy Group|Includes Wowagin Dacite Member, Sooley Volcanic Member, Kingsdale Limestone Member, Joppa Siltstone Member.|Is overlain by Kerrawary Siltstone, Covan Creek Formation and Argyle Formation. Joppa Siltstone Member (De Drack Fm) interfingers with Woodlawn Volcanics. Is overlain by Woodlawn Volcanics.|Siltstone and thinly-very thickly bedded, fine-coarse grained lithic/feldspar/quartz sandstone; biohermal limestone + calcareous facies, locally calcareous siltstone, mudstone; rhyolitic volcaniclastic sandstone, vitric tuff; rhyolite-andesite.|
5292|De Drack Formation|70542|5|Briefly described|Map Legend|Devonian|Silurian|Includes nine unnamed members composed primarily of volcanic sandstone, siltstone and mudstone.||Mount Fairy Group|Includes Joppa Siltstone Member, Kingsdale Limestone Member, Sooley Volcanic Member, Wowagin Dacite Member and nine unnamed members.||Siltstone and thinly-thickly bedded, fine-coarse grained lithic feldspar quartz sandstone, limestone and calcareous facies. Locally calcareous siltstone, mudstone, rhyolitic volcaniclastic sandstone. Minor rhyolite, rhyodacite, dacite and andesite.|
5292|De Drack Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Mount Fairy Group|Includes Wowagin Dacite Member||Siltstone and thinly-very thickly bedded, fine-coarse grained lithic/feldspar/quartz sandstone; biohermal limestone + calcareous facies, locally calcareous siltstone, mudstone; rhyolitic volcaniclastic sandstone, vitric tuff; rhyolite-andesite.|
5292|De Drack Formation|70661|6|Mentioned|p36|||||Mount Fairy Group|Kingsdale Limestone Member|||
5292|De Drack Formation|71069|2|Defined|p21 fig 7, p24-p26, p38 fig 15|Ludlow|Wenlock|Name derived from the De Drack Trigonometrical station. Previously referred to as the Mount Fairy Series, Mount Fairy Beds or alternatively incorporated into the lower Lambie Group. Misspellt as De-Drack Formation on p45. Type section given at GR 737413 6102884 to 737013 6103084.  Hosts the Collector Zn, Cu, Pb, Au, Ag  prospect. Outcrops poorly. Ranges from 300m thick at the type section to around 2500m thick elsewhere. Contains conodont fossils in the Kingsdale Limestone Member, brachiopods in the basal conglomerates and graptolites in shale seqeunces.Age derived from fossil assemblage.   Deposited in a shallow marine environment that was exposed to sea level fluctuation. Equivalent to the Captains Flat Formation, Copper Creek Shale, Cobra Formation and Cuddyong Formation. Equivalent in part to the Kerrawary Siltstone, Black Bog Shale, Barnby Hills Shale and the Kildrummie Formation. Overlies or is faulted against the Adaminaby, Bendoc and Margules Groups. Also conformably overlain by the  Kerrawary Siltstone, Currawang Basalt and the Long Flat Volcanics. Intruded by the Forest Lodge Quartz Monzodiorite and Bishopthorpe Dolerite. Also includes  Bendethera Limstone Member, Wyanbene Limestone Member, Marble Arch Limestone Member, Cheitmore Limestone Member and the Wowagin Dacite Member. Distribution, primary structures/textures, geochemistry, tectonic structure, metamorphism, fossil assemblage and geophysical characteristics discussed. Lithology discussed in detail. See also p40 fig 17, p41, p45, p50 tbl 3, p106, p125, p133-p139, p142-p154, p156, p159, p160, p162, p168, p171, p172.||Mount Fairy Group|Includes the Kingsdale Limestone Member, Sooley Volcanic Member, Sandhills Creek Limestone Member, Joppa Siltstone Member.|Interfingers with the Woodlawn Volcanics. Conformably overlain by the Covan Creek Formation, Argyle Formation. Unconformably overlain by the Lambie Group|Polymictic conglomerate, laminated to medium bedded siltstone, very fine grained sandstone,volcaniclastic sandstone, dolomitised, micritic to biomicritic limestone and bimodal volcanics including rhyolite and dacite.|
5292|De Drack Formation|71656|4|Described|p13 Fig.2,p28-29|Ludow|Llandovery|Includes brachiopods, graptolites, conodonts.||Mount Fairy Group|Includes Kingsdale Limestone Member near base, Sooley Volcanic Member, Joppa Siltstone Member.|Overlain by Covan Creek Formation.|Includes fossiliferous limestone, black shale.|
5292|De Drack Formation|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Mount Fairy Group.||Is overlain by Covan Creek Formation. Abuts/interfingers with Woodlawn Volcanics.|Siltstone and quartzofeldspathic- and feldspar-lithic quartz sandstone and fossiliferous limestone, marble, and calc-arenite; lesser rhyolite lava, rhyolitic volcanic sandstone and polymictic conglomerate.|
5292|De Drack Formation|71699|5|Briefly described|Map legend.|Devonian|Silurian|Seven facies (including the formal Member) are mapped separately.||Mount Fairy Group.|Sandhills Creek Limestone Member.|Is overlain by Covan Creek Formation.|Siltstone and quartzose to quartzofeldspathic and feldspar-lithic-quartz sandstone and fossiliferous limestone, marble and calc-arenite; lesser rhyolite lava rock, rhyolitic volcanic sandstone and polymictic conglomerate.|
5292|De Drack Formation|71700|2|Defined|vi, p7, p12, p14-p15, p21, p48|Late Silurian|Middle Silurian|Named for the De Drack Trigonometrical Station. The type section occurs at the junction of Fairy Meadow Creek and Sandhills Creek from GR 737413 6102884 to GR 737013 6103084 (Felton and Huleatt, 1977). Previously this unit has been identified as the "Mount Fairy Series" by Garretty (1936), Mount Fairy Group by Joplin et al. 1953 and "Mount Fairy Beds" by Best et al (1964). Felton and Huleatt (1977) defined a "Fairy Meadow Limestone Member" as part of this unit but due to its ambiguity is not used in this study. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical charateristics, fossils, distinguishing features, stratigraphic correlations, economic geology and geological hazards are discussed. Contains a number of unnamed limestone lenses and a basal polymictic conglomerate. This unit as a whole contains volumetrically more limestone than the rest of the Mount Fairy Group. This unit is around 1km thick west of the Woolowolar Fault but only around 200m thick to the east of the fault. Also includes the Joppa Siltstone Member,  Bendethera Limestone Member, Wyanbene Limestone Member, Marble Arch Limestone Member and the Cheitmore Limestone Member. This unit is equivalent to the lower Bungonia Group. See also p50-p51, p59-p60, p64, p75-p76, p79-p80, p84, p116, CD.||Mount Fairy Group|Includes the Sandhills Creek Limestone Member, Kingsdale Limestone Member, Sooley Volcanic Member, Wowagin Dacite Member.|Interfingered with the Woodlawn Volcanics. Conformably overlain by the Covan Creek Formation. Unconformably overlies the Bendoc Group.|Siltstone dominated package that also includes sandstone, limestone, volcaniclastic sedimentary rocks, rhyolite and pebble conglomerate.|
5335|Deep Gully Creek Conglomerate Member|22638|1|Redefined|p64||Early Devonian|Cowcumbala Rhyolite, Cootamundra Group. 50 m thick.||||||
5335|Deep Gully Creek Conglomerate Member|22857|5|Briefly described|p450 App.1, Tb.A1.6|Pragian|Pragian|Of the Cowcumbala Rhyolite (Cootamundra Group). Pebble conglomerate, tuffaceous sandstone, shale. Max. thickness: 50m. Geological Province: Bogan Gate Terrace.||||||
5335|Deep Gully Creek Conglomerate Member|35070|2|Defined|p116|Early Devonian|Early Devonian|||||||
5335|Deep Gully Creek Conglomerate Member|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5335|Deep Gully Creek Conglomerate Member|35608|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
5335|Deep Gully Creek Conglomerate Member|35609|6|Mentioned|p11|||||||||
5335|Deep Gully Creek Conglomerate Member|36411|6|Mentioned|p268|||Refers Basden et al 1978 for definition.||||||
5335|Deep Gully Creek Conglomerate Member|44192|5|Briefly described|Map Legend||Lochkovian|||||||
5352|Delegate River Mudstone|13996|6|Mentioned|p149|||||||||
5352|Delegate River Mudstone|22768|6|Mentioned|p177|Ludlow||||||||
5352|Delegate River Mudstone|22815|2|Defined|p38|Ludlow|Llandovery|||||||
5352|Delegate River Mudstone|22857|4|Described|p177, p466 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Bredbo Group. Fissile mudstone, occasional siltstone, sandstone and limestone; fossiliferous. Max. thickness: 200m. Geological Province: Quidong Basin. ||||||
5352|Delegate River Mudstone|23329|5|Briefly described|1042|Late Silurian|Silurian|||||||
5352|Delegate River Mudstone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
5352|Delegate River Mudstone|32672|6|Mentioned|p672|||||||||
5352|Delegate River Mudstone|34692|6|Mentioned|p187|||||||||
5352|Delegate River Mudstone|37727|4|Described|p55|||See also P19.||||||
5352|Delegate River Mudstone|38151|6|Mentioned|Table 1|||||||||
5352|Delegate River Mudstone|40328|3|Fully described|p87|||||||||
5352|Delegate River Mudstone|41869|6|Mentioned|p9|||||||||
5352|Delegate River Mudstone|43233|5|Briefly described|Map Legend||Ludlow|of Bredbo Group||||||
5352|Delegate River Mudstone|46574|5|Briefly described|Map Legend|Late Silurian|Silurian|Of the Yass-Canberra Rise. Geological Province: Lachlan Pre-Cratonic Province.  Mudstone, siltstone, sandstone, limestone.||||||09-NOV-04
5352|Delegate River Mudstone|60988|5|Briefly described|p143-146 |Late Silurian|Middle Silurian|Quidong Basin. Contains brachiopods which were compared with those in the Silverdale Formation.||||Conformably overlies the Quidong Limestone.||
5360|Demon Creek Granite|29988|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
5360|Demon Creek Granite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
5365|Dempsey Formation|22578|5|Briefly described|p400, Fig.9 p399|||||||||
5365|Dempsey Formation|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Tomago Coal Measures. Siltstone, sandstone, tuff; minor carbonaceous claystone; several coal seams. Max. thickness: >590m. Geological Province: Sydney Basin.||||||
5365|Dempsey Formation|22969|4|Described|p 23, Fig 2.2||Permian|Max. thickness: >590 m.||||||
5365|Dempsey Formation|23055|5|Briefly described|p9|||||||||
5365|Dempsey Formation|24157|5|Briefly described|p188 Tb.1, p209 Fig.19|Permian|Permian|Parent: Tomago Coal Measures. Geological Province: Sydney Basin||||||
5365|Dempsey Formation|24471|4|Described|p32 Fig.4, p33|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to Bargo Claystone. Overlain by Waratah Sandstone. Geological Province: Sydney Basin.||||||07-FEB-11
5365|Dempsey Formation|33334|5|Briefly described|p8|||Perm.||||||
5365|Dempsey Formation|33867|4|Described|p7|||||||||
5365|Dempsey Formation|34465|5|Briefly described|Fig.5.11|||See also P337||||||
5365|Dempsey Formation|36042|6|Mentioned|Fig.7|||||||||
5365|Dempsey Formation|37084|6|Mentioned|p177|||||||||
5365|Dempsey Formation|37087|6|Mentioned|p198|||||||||
5365|Dempsey Formation|37924|6|Mentioned|p488|||||||||
5365|Dempsey Formation|38656|5|Briefly described|Fig.1.5.13|||P280. See also Fig.1.5.14.||||||
5365|Dempsey Formation|39232|6|Mentioned|p113|||||||||
5365|Dempsey Formation|39287|6|Mentioned|p33|||See also Fig.2.2||||||
5365|Dempsey Formation|39292|6|Mentioned|Fig. 6.3|||||||||
5365|Dempsey Formation|39299|6|Mentioned|p288|||||||||
5365|Dempsey Formation|39308|6|Mentioned|Fig. 23.4|||||||||
5365|Dempsey Formation|39609|6|Mentioned|Table 1|||||||||
5365|Dempsey Formation|40166|6|Mentioned|p347|||See also Table 1 and Fig.2||||||
5365|Dempsey Formation|40256|6|Mentioned|p303|||||||||
5365|Dempsey Formation|40321|6|Mentioned|p19|||||||||
5365|Dempsey Formation|40971|6|Mentioned|p210|||||||||
5365|Dempsey Formation|41474|6|Mentioned|p63|||||||||
5365|Dempsey Formation|42182|6|Mentioned|p297|||||||||
5365|Dempsey Formation|42657|5|Briefly described|p81|||Newcastle Coalfield||||||
5365|Dempsey Formation|43017|5|Briefly described|Fig.1,p372|||||||||
5365|Dempsey Formation|43194|5|Briefly described|p112, p129 Tb. 8.3, p130|Late Permian|Late Permian|Uppermost unit of Wittingham Coal Measures, Hunter Coalfield, Sydney Basin. Correlated 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.||||||
5365|Dempsey Formation|43447|14|Not recorded|Table 1,diag.p22,23|||Tomago Coal Measures||||||
5365|Dempsey Formation|43491|14|Not recorded|not on card|||||||||
5365|Dempsey Formation|44244|5|Briefly described|p276|Late Permian|Late Permian|Of the Tomago Coal Measures.||||||26-AUG-04
5365|Dempsey Formation|45090|6|Mentioned|p26|||Relationship of rock units||||||
5365|Dempsey Formation|60281|5|Briefly described|p61|Late Permian|Late Permian|Of the Tomago Coal Measures.  Siltstone, claystone, sandstone and minor coal.  Max. thickness: >590m.  Geological Province: Sydney Basin.||||||
5365|Dempsey Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Tomago Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
5365|Dempsey Formation|61612|6|Mentioned|p274, p277, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||13-MAR-09
5365|Dempsey Formation|61770|6|Mentioned|p110|||||||||
5365|Dempsey Formation|62033|5|Briefly described|p25 (Table)|||Of the Tomago Coal Measures. Overlain by Newcastle Coal Measures. Geological Province: Sydney Basin.||||||14-MAR-07
5365|Dempsey Formation|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Late Permian.||Of the Tomago Coal Measures.||||
5365|Dempsey Formation|68003|6|Mentioned|p41.|Late Permian|Late Permian|Sydney Basin. A marine incursion interrupting coal formation.||||||
5365|Dempsey Formation|68004|5|Briefly described|p23 Table 1.|||Newcastle Coalfield.||Unit in Tomago Coal Measures.||Is overlain by Waratah Sandstone.||
5365|Dempsey Formation|68493|5|Briefly described|p5 Fig.2|Lopingian|Lopingian|||Of the Tomago Coal Measures.||Overlies Four Mile Creek Formation.|Siltstone, sandstone, coal, tuff, minor carbonaceous claystone.|
5365|Dempsey Formation|69297|6|Mentioned|p502 fig 5.43, p503|Upper Permian|Upper Permian|Sydney Basin. Has good oil and gas source rock potential.||||Unconformably overlies the Tomago Coal Measures.||
5387|Derale Sandstone|22472|6|Mentioned|p47 Fig.6(e)|||of the Mt. Knowles Group||||||
5387|Derale Sandstone|22529|6|Mentioned|4 fig 2|Late Devonian|Late Devonian|Parent Mount Knowles Group. Underlying unit Bumberra Formation||||||
5387|Derale Sandstone|22857|5|Briefly described|p492 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Mount Knowles Group. Richly fossiliferous quartz arenite and sublithic arenite, rare shale. Max. thickness: 800m. Geological Province: Lambie Shelf.||||||
5387|Derale Sandstone|23043|5|Briefly described|Map Legend|Famennian|Famennian|of Mount Knowles Group.||||||
5387|Derale Sandstone|23170|2|Defined|p245|Famennian|Late Devonian|of Mount Knowles Group.||||||
5387|Derale Sandstone|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
5387|Derale Sandstone|32485|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
5387|Derale Sandstone|39214|6|Mentioned|p29|||||||||
5387|Derale Sandstone|43043|6|Mentioned|p100|||||||||
5387|Derale Sandstone|43188|4|Described|p219,Table 6 p218||Late Devonian|Mudgee district. Of Lambie Group.||||||
5387|Derale Sandstone|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
5387|Derale Sandstone|73299|6|Mentioned|p1096 Fig.3, p1097 Fig.4, p1100 Fig.5|Late Devonian|Late Devonian|Capertree High.||Mount Knowles Group||Overlies the Lawsons Creek Shale.||
5391|Deriah Formation|22500|5|Briefly described|p 7||Late Triassic|||||||
5391|Deriah Formation|22579|5|Briefly described|p219 Fig.2|Late Triassic|Early Triassic|||||||
5391|Deriah Formation|22857|4|Described|p265, p518 App1, Tb.A1.9|Middle Triassic|Middle Triassic|Green lithic arenite rich in volcanic fragments and mud clasts. Max. thickness: 160m. Geological Province: Gunnedah Basin. See also p315 Fig.22.8.||||||
5391|Deriah Formation|22864|6|Mentioned|p265|||||||||
5391|Deriah Formation|22865|6|Mentioned|Fig22.8p315|||||||||
5391|Deriah Formation|23566|5|Briefly described|p116 Fig. 2|Triassic|Triassic|Geological Province: Gunnedah Basin.||||||17-SEP-08
5391|Deriah Formation|24159|5|Briefly described|p150, Fig.3, p151|Middle Triassic|Middle Triassic|Geological Province: Gunnedah Basin. Underlying Unit: Digby Formation. Overlying Unit: unconformably with Purlawaugh Formation.||||||
5391|Deriah Formation|41472|4|Described|p56|||||||||
5391|Deriah Formation|42463|6|Mentioned|Fig.6 P173|||||||||
5391|Deriah Formation|42809|5|Briefly described|p436|||see also Fig.2 P438||||||
5391|Deriah Formation|43194|1|Redefined|p98 Tb. 8.2, p121, p125-127, p133 App. 1|Middle Triassic|Middle Triassic|See also references on p95, p122, p129 Tb. 8.3, p131. Gunnedah Basin. Re-defined to include a section previously included in underlying Napperby Formation. Disconformably overlain by Purlawaugh Formation. Correlated with upper part of Bringelly Shale (Sydney Basin).||||||
5391|Deriah Formation|50629|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Geological Province: Gunnedah Basin. Underlies: Garrawilla Volcanics. Overlies: Napperby Formation.||||||05-JUL-04
5391|Deriah Formation|60266|5|Briefly described|p2|Middle Triassic|Middle Triassic|Overlies the Napperby Formation.  Geological Province: Gunnedah Basin.||||||
5391|Deriah Formation|61313|5|Briefly described|p104 Table G1|Middle Triassic|Early Triassic|Green-white, lithic sandstone, mudstone.||||||
5391|Deriah Formation|61377|5|Briefly described|p149 Fig. SU8|||Geological Province: Gunnedah Basin.||||||07-FEB-11
5391|Deriah Formation|61612|6|Mentioned|p270 Fig. 1|Middle Triassic|Middle Triassic|Geological Province: Gunnedah Basin.||||||13-MAR-09
5391|Deriah Formation|61776|5|Briefly described|p194 Fig. 3|Middle Triassic|Triassic|Geological Province: Gunnedah Basin. Lithic sandstone and siltstone.||||||17-SEP-08
5391|Deriah Formation|62357|5|Briefly described|p524 Fig. 7|Early Triassic|Early Triassic|Geological Province: Gunnedah Basin.||||||
5391|Deriah Formation|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Middle Triassic|Unit in the Gunnedah Basin, overlies Napperby Formation.||||||15-JAN-15
5391|Deriah Formation|65113|5|Briefly described|Fig 4 p340|Middle Triassic|Middle Triassic|Gunnedah Basin. Overlies the Napperby Formation.||||||
5391|Deriah Formation|65114|5|Briefly described|p385 Fig.3|Middle Triassic||||||||
5391|Deriah Formation|65115|6|Mentioned|Fig 2 p403|Triassic|Triassic|Overlies the Napperby Formation in the Gunnedah Basin.||||||
5391|Deriah Formation|65116|5|Briefly described|p451, Fig 2 p436, Fig6 p441|Middle Triassic|Middle Triassic|Overlies the Napperby Formation in the Gunnedah Basin. Fine to coarse-grained green-grey lithic sandstone, with minor siltstone and claystone.||||||
5391|Deriah Formation|65118|5|Briefly described|Fig 2 p479|Triassic|Triassic|Overlies the Napperby Formation, Gunnedah Basin.||||||
5391|Deriah Formation|66191|5|Briefly described|p485 Fig.2, p485|Late Triassic|Early Triassic|Gunnedah Basin. Unconformably underlies the Garrawilla Volcanics, overlies the Napperby Formation. Green sandstone.||||||
5391|Deriah Formation|68003|5|Briefly described|p38 Fig.3-j, p43, p57 Fig.3-n, p128.|Middle Triassic|Middle Triassic|Gunnedah Basin, Brigalow Belt South Bioregion. Contemporaneous with Napperby Formation. Possibly produced by volcanic activity in the New England Fold Belt.||||Overlies Napperby Formation. Is unconformably overlain by Purlawaugh Formation.|Very distinctive green sandstone: fine- to medium-grained lithic sandstone rich in volcanic fragments, with common mudstone clasts overlain by off-white lithic sandstone and dark grey mudstone.|
5391|Deriah Formation|68004|6|Mentioned|p23 Table 1. |||Gunnedah Basin.||||Overlies Napperby Formation.||
5391|Deriah Formation|70036|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Included in a mapped unit of fluvial and lacustrine sequences: conglomerate, quartzose and lithic sandstone, siltstone and mudstone.||||||
5391|Deriah Formation|70791|5|Briefly described|p277|Middle Triassic|Middle Triassic|Gunnedah Basin. Alluvial deposits.||||||
5403|Derriwong Group|22519|6|Mentioned|p3|||||||||
5403|Derriwong Group|22638|6|Mentioned|p62|||Equivalent of the Combaning Formation||||||
5403|Derriwong Group|22768|5|Briefly described|p170-71|Early Devonian|Late Silurian|||||||
5403|Derriwong Group|22797|5|Briefly described|P838||Pridolian|||||||
5403|Derriwong Group|22831|4|Described|p 42|Early Devonian|Late Silurian|||||||
5403|Derriwong Group|22857|5|Briefly described|p171, p448 App.1. Tb.A1.6|Early Devonian|Late Silurian|Unconformably overlies Ootha Formation. Geological Province: Bogan Gate Terrace. See also p446 App.1. Tb.A1.6.||||||
5403|Derriwong Group|23099|5|Briefly described|p582|Devonian|Silurian|||||||
5403|Derriwong Group|23309|6|Mentioned|p390|||||||||
5403|Derriwong Group|23522|5|Briefly described|p249 Fig 5|Lochkovian|Ludlow|||||||
5403|Derriwong Group|23736|6|Mentioned|p13 Fig. 2|||||||||
5403|Derriwong Group|24007|5|Briefly described|p327|Devonian|Silurian|||||||
5403|Derriwong Group|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
5403|Derriwong Group|24267|5|Briefly described|p1509|Silurian|Silurian|Geological Province: Parkes-Narromine Belt.||||||28-AUG-08
5403|Derriwong Group|24417|3|Fully described|p67|Early Devonian|Late Silurian|Previously included in "Ootha Formation" (now separated to form Ootha Group).  Overlain by Trundle Group.||||||
5403|Derriwong Group|36066|4|Described|p6|||||||||
5403|Derriwong Group|37258|6|Mentioned|p2|||||||||
5403|Derriwong Group|40365|6|Mentioned|p240|||||||||
5403|Derriwong Group|40891|6|Mentioned|p18|||||||||
5403|Derriwong Group|41528|6|Mentioned|p35|||||||||
5403|Derriwong Group|41869|4|Described|p5|||||||||
5403|Derriwong Group|42456|6|Mentioned|p4|||||||||
5403|Derriwong Group|42714|5|Briefly described|Fig.1 P25|||||||||
5403|Derriwong Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
5403|Derriwong Group|43441|4|Described|20,26|Early Devonian|Late Silurian|||||||08-JAN-10
5403|Derriwong Group|44093|5|Briefly described|p178 App. 1|Early Devonian|Silurian|In the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
5403|Derriwong Group|44160|5|Briefly described|Map Legend|Lochkovian|Pridolian|||||||08-JAN-10
5403|Derriwong Group|44936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
5403|Derriwong Group|46522|6|Mentioned|p65|||||||||
5403|Derriwong Group|50191|5|Briefly described|p6, 11|Early Devonian|Early Devonian|Includes: Yiddah Formation, Combaning Formation.||||||
5403|Derriwong Group|50299|5|Briefly described|Map Legend|Devonian|Silurian|||||||
5403|Derriwong Group|50385|5|Briefly described|Map Legend|Devonian|Silurian|||||||11-JUN-04
5403|Derriwong Group|50554|5|Briefly described|Map legend|Devonian|Silurian|Includes the Ootha Subgroup, Yarrabandai Formation, Byong Volcanics and the Edols Conglomerate.||||||
5403|Derriwong Group|50628|5|Briefly described|Map Legend|Devonian|Silurian|Includes undifferentiated sediments.||||||
5403|Derriwong Group|60008|5|Briefly described|Map Legend|Devonian|Silurian|Sediments and/or volcanics.||||||08-JUL-04
5403|Derriwong Group|60009|5|Briefly described|Map Legend|Lochkovian|Pridoli|||||||13-JUL-04
5403|Derriwong Group|60548|5|Briefly described|map legend|Devonian|Silurian|||||||
5403|Derriwong Group|61821|5|Briefly described|p101|Devonian|Silurian|Includes sandstone sediments. Geological Province: Lachlan Fold Belt.||||||
5403|Derriwong Group|61894|6|Mentioned|p179 Fig.3, p181||||||Cookeys Plains Formation, Meloola Volcanics.|||
5403|Derriwong Group|61964|6|Mentioned|p67|||Includes sandstones.||||||
5403|Derriwong Group|62569|5|Briefly described|p605-606|Devonian|Silurian|Unconformably underlies Hervey Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
5403|Derriwong Group|63120|5|Briefly described|p217|||Includes Cookeys Plains Formation. Age: ?Late Silurian to Early Devonian?||||||
5403|Derriwong Group|63289|6|Mentioned|p373 Fig. 7|Early Devonian|Silurian|||||||07-FEB-11
5403|Derriwong Group|63290|6|Mentioned|p391, p395|||Includes; Edols Conglomerate. Underlain by Girilambone Group.||||||
5403|Derriwong Group|64015|5|Briefly described|p58 Fig. 1|||||||||
5403|Derriwong Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
5403|Derriwong Group|66197|5|Briefly described|p634|||Murda Syncline. Also shown on p635 Fig.5a as (mis-spelt) Deriwong Group.|||||Includes silicic volcanics and volcaniclastics, shallow marine clastics; basal conglomerate.|13-MAR-12
5403|Derriwong Group|67847|5|Briefly described|p22-p24|Pridoli|Ludlow||||Includes the Calarie Sandstone.|Unconformably overlies the Kirribilli Formation.||
5403|Derriwong Group|71039|6|Mentioned|p14|||||||||
5403|Derriwong Group|71040|6|Mentioned|p12 Fig.7, p15, p18-19|Early Devonian|Late Silurian|Lachlan Orogen. Has a basal unconformity.||||||
5403|Derriwong Group|73143|6|Mentioned|p8-9|Lochkovian|Lochkovian|Bogan Gate-Mineral Hill-Trundle areas. Contains Caudicriodus woschmidti conodonts, Lochkovian corals.|||Cookeys Plains Formation|||
5403|Derriwong Group|73287|6|Mentioned|p665 Fig.2|Early Devonian|Early Devonian||||||Includes planar laminated sandstone, plagioclase phyric rhyolite lava, cherty siltstone, ripple laminated sandstone.|
5426|Deua Formation|22815|4|Described|p102|Late Devonian|Late Devonian|||||||
5426|Deua Formation|22857|5|Briefly described|p216, p494 App. 1 Tb.A1.7|Frasnian|Frasnian|Of the Minuma Range Group. Well-bedded arenite with minor shale interbeds. Max. thickness: 360m. Geological Province: Lambie Shelf.||||||
5426|Deua Formation|22859|5|Briefly described|p216|||of Minuma Range Group||||||
5426|Deua Formation|39028|6|Mentioned|Map legend|Famennian|Famennian|||||||
5426|Deua Formation|40276|2|Defined|p25|Late Devonian|Late Devonian|||||||
5426|Deua Formation|42497|5|Briefly described|Map Legend|Famennian||||||||
5426|Deua Formation|43233|5|Briefly described|Map Legend||Late Devonian|||||||
5426|Deua Formation|68298|5|Briefly described|p214-215|||Contains marine sediments and fish fauna. Includes brachiopods and bivalves.||||||
5426|Deua Formation|71700|5|Briefly described|CD|Late Devonian|Late Devonian|Ages derived from fossil assemblage.||Minuma Range Group||||
5426|Deua Formation|73181|6|Mentioned|p65-66|Frasnian|Frasnian|Contains invertebrate fossils.||Minuma Range Group||Underlain by Curmulee Conglomerate. Overlain by Khan Yunis Formation.||
5432|Devils Elbow Limestone Member|42376|5|Briefly described|p35|||Apparently intended as informal name. Reserved as Devils Elbow, E.C. Leitch 1984. Listed NLR 1991.||||||
5445|Dhruwalgha Tinguaite|36220|4|Described|p97|||||||||
5445|Dhruwalgha Tinguaite|36221|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic||||||
5445|Dhruwalgha Tinguaite|37253|6|Mentioned|Table 1|||||||||
5445|Dhruwalgha Tinguaite|43346|2|Defined|p4 Map|||||||||
5445|Dhruwalgha Tinguaite|43349|14|Not recorded|Map|||||||||
5445|Dhruwalgha Tinguaite|45003|14|Not recorded|p173|||See also Lexicon||||||
5470|Digby Formation|721|5|Briefly described|Map legend|Scythian|Scythian|Poorly sorted pebble to boulder orthoconglomerate, rare sandstone.  Geological Province: Gunnedah Basin.||||||
5470|Digby Formation|22579|5|Briefly described|p219 Fig.2|Triassic|Triassic|||||||
5470|Digby Formation|22857|5|Briefly described|p264, p518 App.1 Tb.A1.9|Early Triassic|Early Triassic|Includes the Ulinda Sandstone Member. Poorly sorted pebble to boulder orthoconglomerate; clasts of chert and jasper. Max. thickness: 204m. Geological Province: Gunnedah Basin. See also p315 Fig. 22.8.||||||
5470|Digby Formation|22864|6|Mentioned|p264|||||||||
5470|Digby Formation|22865|6|Mentioned|Fig22.8p315|||||||||
5470|Digby Formation|23050|5|Briefly described|p 82 Fig.17|Early Triassic|Early Triassic|In the Gunnedah Basin.||||||29-MAR-10
5470|Digby Formation|23214|6|Mentioned|p270|Middle Triassic|Middle Triassic|Geological Province: Gunnedah Basin.||||||
5470|Digby Formation|23566|5|Briefly described|p116 Fig. 2|Triassic|Triassic|Geological Province: Gunnedah Basin||||||
5470|Digby Formation|23740|5|Briefly described|p1221|Triassic|Triassic|Geological Province: Gunnedah Basin||||||
5470|Digby Formation|24159|5|Briefly described|p150 Fig.3, p149|Early Triassic|Early Triassic|Geological Province: Gunnedah Basin. Underlying Unit: unconformity with Black Jack Group.||||||
5470|Digby Formation|24243|5|Briefly described|p3 Fig.2|Triassic|Triassic|||||||
5470|Digby Formation|38614|4|Described|p10|||||||||
5470|Digby Formation|39063|6|Mentioned|p19|||||||||
5470|Digby Formation|39693|6|Mentioned|p17|||||||||
5470|Digby Formation|39913|5|Briefly described|p6|||||||||
5470|Digby Formation|40200|4|Described|p6|||||||||
5470|Digby Formation|40332|6|Mentioned|Fig.3|||||||||
5470|Digby Formation|40680|6|Mentioned|p23|||||||||
5470|Digby Formation|40767|4|Described|p8|||||||||
5470|Digby Formation|40952|6|Mentioned|p8|||||||||
5470|Digby Formation|41264|6|Mentioned|p252|||||||||
5470|Digby Formation|41290|4|Described|p226|||||||||
5470|Digby Formation|41330|6|Mentioned|p21|||||||||
5470|Digby Formation|41451|6|Mentioned|p14|||||||||
5470|Digby Formation|41472|4|Described|p55|||||||||
5470|Digby Formation|42284|5|Briefly described|Fig.11 P104|||||||||
5470|Digby Formation|42463|6|Mentioned|Fig.6 P173|||||||||
5470|Digby Formation|42679|5|Briefly described|Fig.3 P3|||||||||
5470|Digby Formation|42767|5|Briefly described|Fig.5|||||||||
5470|Digby Formation|42773|5|Briefly described|p354|||||||||
5470|Digby Formation|42809|5|Briefly described|p436|||see also Fig.2 P438||||||
5470|Digby Formation|42950|5|Briefly described|p40|||||||||
5470|Digby Formation|43091|5|Briefly described|Map legend|||In the Gunnedah Basin.||||||14-FEB-07
5470|Digby Formation|43194|1|Redefined|p98 Tb 8.2, p115-122, p133 App. 1|Early Triassic|Early Triassic|See also references on p95-96, p106, p129 Tb. 8.3. Supersedes Digby Conglomerate, Digby Series, Digby beds. Has been updated to include Ulinda Sandstone Member, Bomera Conglomerate Member. Unconformably overlies Black Jack, Watermark, Porcupine Formations. Disconformably underlies Napperby Formation.||||||
5470|Digby Formation|43582|6|Mentioned|Fig.5,p16||Early Triassic|||||||
5470|Digby Formation|44093|5|Briefly described|p192 App. 1|Triassic|Triassic|Clastic sediments. Geological Province: Lachlan Fold Belt.||||||07-MAR-05
5470|Digby Formation|50629|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Geological Province: Gunnedah Basin. Underlies: Napperby Formation.  Overlies: Coogal & Nea Subgroups.||||||05-JUL-04
5470|Digby Formation|60266|5|Briefly described|p2, p3 Tb. 1|Early Triassic|Early Triassic|High-energy piedmont sedimentary units of quartz-lithic sandstone, conglomerate and siltstone.  Overlies Dunedoo Formation and Rylstone Volcanics; overlain by Napperby Formation.  Geological Province: Gunnedah Basin.||||||
5470|Digby Formation|60267|5|Briefly described|p15, p28 Fig. 8|Triassic|Triassic|||||||
5470|Digby Formation|60386|6|Mentioned|p296||Early Triassic|Bowen/Sydney Basin. Non-marine.||||||
5470|Digby Formation|61201|5|Briefly described|p2|Early Triassic|Early Triassic|||||||
5470|Digby Formation|61313|5|Briefly described|p88, P94 Fig.G7, p97|Triassic|Triassic|Coarse clastics - basal massive bedded pebble conglomerate, and quartz clasts dominate higher in the sequence. Overlain disconformably (in parts) by Napperby Formation. Max. thickness: 250m (south eastern part of basin). Geol. Prov: Gunnedah Basin.||||||
5470|Digby Formation|61377|5|Briefly described|p149 Fig. SU8|Early Triassic|Early Triassic|Alluvial fan deposits; lower part of this unit is known as the 'conglomerate facies' in Gunnedah Basin. Geological Province: Gunnedah Basin. See also p154 Fig, SU9.||||||07-FEB-11
5470|Digby Formation|61612|6|Mentioned|p274, p270 Fig. 1|Early Triassic|Late Permian|Geological Province: Gunnedah Basin.||||||13-MAR-09
5470|Digby Formation|61776|5|Briefly described|p194 Fig. 3|Early Triassic|Triassic|Geological Province: Gunnedah Basin. Lithic pebble conglomerate, lithic and quartz lithic sandstone.||||||
5470|Digby Formation|62357|5|Briefly described|p524 Fig. 7|Early Triassic|Late Permian|Geological Province: Gunnedah Basin.||||||
5470|Digby Formation|65112|6|Mentioned|Fig 4 p314|Early Triassic|Early Triassic|Unit in the Gunnedah Basin, underlies the Napperby Formation.||||||14-SEP-09
5470|Digby Formation|65113|5|Briefly described|Fig 4 p340|Early Triassic|Late Permian|Gunnedah Basin.||||||29-MAR-10
5470|Digby Formation|65114|5|Briefly described|p385 Fig.3|Early Triassic|Late Permian|||||||
5470|Digby Formation|65115|6|Mentioned|Fig 2 p403|Triassic|Permian|Underlies the Napperby Formation in the Gunnedah Basin.||||||
5470|Digby Formation|65116|4|Described|p449, 450, Fig 2 p436, Fig 6 p441|Early Triassic|Early Triassic|Lithic pebble conglomerate and fluvial quartz-lithic grading up to quartzose sandstones, Gunnedah Basin. Equivalent to the Rewan Group in Qld.||||||
5470|Digby Formation|65118|5|Briefly described|p491, Fig 2 p479|Early Triassic|Early Triassic|Overlies Watermark Formation in Bellata 1. Age equivalent of the Rewan Group (Bowen Basin), sits in the Gunnedah Basin. See also Digby Conglomerate p495 Fig 13.||||||06-MAR-12
5470|Digby Formation|66191|5|Briefly described|p485 Fig.2|Early Triassic|Early Triassic|Gunnedah Basin. Underlies the Napperby Formation, unconformably overlies the Black Jack Group.||||||
5470|Digby Formation|66529|6|Mentioned|p12 Fig.5 |||Coonamble Embayment.||||Unconformably overlies Black Jack Formation. Is overlain by Napperby Formation.||
5470|Digby Formation|68003|5|Briefly described|p38 Fig.3-j, pp42-43, p57 Fig.3-n, p128.|Middle Triassic|Early Triassic|Gunnedah Basin, Brigalow Belt South Bioregion. Correlative of the Narrabeen Group in the Hunter and Western Coalfields. Deposition followed a major depositional break and a period of uplift and erosion.|||Includes Bomera Conglomerate Member and Wollar Sandstone Member.|Unconformably overlies Trinkey Formation. Is overlain by Napperby Formation.|Poorly sorted, pebble to boulder conglomerate; rare sandstone.|
5470|Digby Formation|68004|4|Described|p23 Table 1, p62, p84, p139, p172, p176.|Triassic|Triassic|Gunnedah Basin. Equivalent to the Narrabeen Group, Sydney Basin. Conventional gas-bearing. Sealed by Napperby Formation shale. Kaolin prospectivity is discussed.|||Includes Wollar Sandstone Member.|Overlies Black Jack Group, Nea Subgroup, Trinkey Formation. Is overlain by Napperby Formation.|Conglomerate at base, overlain by quartz-lithic sandstone which gradually changes into quartzose sandstone unit of cross-bedded sandstone with well-rounded quartz pebbles; a siltstone/sandstone and grey/purple claystone palaeosol is present on top.|
5470|Digby Formation|70036|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Included in a mapped unit of fluvial and lacustrine sequences: conglomerate, quartzose and lithic sandstone, siltstone and mudstone.||||||
5470|Digby Formation|70791|5|Briefly described|p276-278|Middle Triassic|Early Triassic|Gunnedah Basin. Terrestrial sediments.||||Unconformably overlies Black Jack Group.||
5470|Digby Formation|70878|5|Briefly described|p715, p726|Triassic|Triassic|Gunnedah Basin.||Narrabeen Group.||||
5470|Digby Formation|72298|5|Briefly described|p801|Paleozoic|Paleozoic|Coonamble Embayment (NSW). Confined aquifers, generally producing flowing artesian water bores.||||Unconformably overlies Black Jack FZ. Is overlain by Napperby FZ.||
5479|Dights Creek Coal|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Glen Gallic Subgroup.  Includes the Hillsdale Coal Member, Nalleeen Tuff Member and Hobden Gully Coal Member.   Geological Province: Sydney Basin||||||
5479|Dights Creek Coal|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Glen Gallic Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
5479|Dights Creek Coal|29942|3|Fully described|p11|||||||||
5479|Dights Creek Coal|39666|6|Mentioned|p79|||||||||
5479|Dights Creek Coal|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Basal unit in Glen Gallic Sub-group.|Includes Hobden Gully Member, Naleen Tuff Member and Hillsdale Coal Member.|Overlies Waterfall Gully Formation. Is overlain by Redmanvale Creek Formation.|Durain rich coals separated by tuffaceous claystone.|
5480|Digilah Formation|12597|6|Mentioned|p492 Tb.1, p497|Callovian|Callovian|S Surat Basin.||||||
5480|Digilah Formation|22857|4|Described|p546 App.1 Tb.A1.12|Middle Jurassic|Early Jurassic|Monotonous succession of thinly bedded mudstones and siltstones, lenticular beds of clay-ironstone. Lateral equivalent of Purlawaugh Formation. Max. thickness: 30m. Geological Province: Surat Basin.||||||
5480|Digilah Formation|31326|6|Mentioned|p38|||Stratigraphy||||||
5480|Digilah Formation|35065|6|Mentioned|p44|||||||||
5480|Digilah Formation|35095|4|Described|p113|||||||||
5480|Digilah Formation|43494|6|Mentioned|p14||Jurassic|Of Loughnan and Evans (1978). Formerly (?) the upper section of the Purlawaugh Formation, which overlay the Ukebung Formation, representing the lower section of Purlawaugh Formation.||||||10-MAR-19
5480|Digilah Formation|61377|5|Briefly described|p152|Middle Jurassic|Middle Jurassic|Together with Ukebung Fm + Doona Sst Mbr, is equiv. of Purlawaugh Fm in other parts of basin.Monotonous sequence of thinly bedded mudstone and siltstone; lenticular ironstone beds in weathered profiles; minor white flint clay.Geol.Prov:Surat Basin||||||07-FEB-11
5547|Djuan Tonalite|23799|3|Fully described|p90, p11 Tb. 1|Triassic|Permian|Grey to dark tonalite, common xenoliths, hornblendite.  Unconformably overlain by Tarong beds and Main Range Volcanics.  Intrudes Sugarloaf Metamorphics and Maronghi Creek Beds.  Geolological Province: Yarraman Subprovince.||||||
5547|Djuan Tonalite|23800|5|Briefly described|Map Legend|Triassic|Triassic|||||||
5547|Djuan Tonalite|24560|5|Briefly described|Map legend|Triassic|Triassic|Of Cressbrook Creek Group.   Grey to dark grey tonalite (common xenoliths); hornblendite.||||||
5547|Djuan Tonalite|30303|2|Defined|p323|Early Triassic|Early Triassic|K/Ar dating 230m.y.||||||
5547|Djuan Tonalite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
5547|Djuan Tonalite|35161|6|Mentioned|p591|||||||||
5547|Djuan Tonalite|36954|6|Mentioned|Fig.1|||||||||
5547|Djuan Tonalite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
5547|Djuan Tonalite|39445|5|Briefly described|Table 12|||||||||
5547|Djuan Tonalite|40245|6|Mentioned|p185|||||||||
5547|Djuan Tonalite|42525|5|Briefly described|Map legend|Triassic|Permian|||||||
5547|Djuan Tonalite|43008|5|Briefly described|map legend|||||||||
5547|Djuan Tonalite|61781|6|Mentioned|p271|||||||||
5547|Djuan Tonalite|68679|5|Briefly described|p323, p411-416|Triassic|Permian|West of the Esk Basin, northern New England Orogen. Just N of the Eskdale Igneous Complex. Two other, significantly older, ages given. Has lower Na2O and K2O and higher CaO. Geochemical plot.|234.8 +/- 8 Ma (K-Ar: Cranfield et al., 1976).|||Intrudes Sugarloaf Metamorphics. Is bounded to the N by Woolshed Mountain and Kenewah Granodiorites.|Xenolithic tonalite; prominent foliation.|
5553|Docker Head Claystone Member|31725|6|Mentioned|p10|||On table||||||
5553|Docker Head Claystone Member|31886|3|Fully described|p396|||||||||
5553|Docker Head Claystone Member|32800|6|Mentioned|p390|||||||||
5556|Dodger Diorite|40882|6|Mentioned|p25|||||||||
5556|Dodger Diorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh27.||||||
5556|Dodger Diorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
5593|Doncaster Member|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p495 Fig.3|Barremian|Barremian|See also p497-498, p499. Eromanga Basin. 100-200m thick.||Unit in Wallumbilla Formation.||Equivalent to lower part of Bulldog Shale.|Marine carbonaceous mudstone with minor siltstone and fine-grained labile glauconitic sandstone; rich fauna, predominantly molluscs, in the calcareous strata; fossil logs locally common.|
5593|Doncaster Member|13516|5|Briefly described|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Wallumbilla Formation||||
5593|Doncaster Member|22757|5|Briefly described|Table6,p11||Early Cretaceous|275 m. Wallumbilla Formation, Rolling Downs Group, Surat Basin.||||||
5593|Doncaster Member|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Aptian|Aptian|Of the Wallumbilla Formation (Rolling Downs Group). Siltstone and fine sandstone. Become the Wittabrenna beds in Tibooburra area. Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6.||||||
5593|Doncaster Member|22865|5|Briefly described|Table22.1p296-7|Aptian|Aptian|||||||
5593|Doncaster Member|23183|6|Mentioned|p222|||||||||
5593|Doncaster Member|23224|5|Briefly described|p3||Aptian|Of McMinn 1981. Hosts Opal Deposits in White Cliffs. Of Wallumbilla Formation. Great Australian Basin.||||||07-MAR-06
5593|Doncaster Member|23430|4|Described|p523 + p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province.||||||
5593|Doncaster Member|23499|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation, Eromanga Basin.||||||14-APR-08
5593|Doncaster Member|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group). Geological Province: Great Australian Superbasin.||||||
5593|Doncaster Member|23982|5|Briefly described|p57|||Of the Wallumbilla Formation. Geological Province: Great Artesian Basin.||||||14-APR-08
5593|Doncaster Member|24085|5|Briefly described|Not recorded|Albian|Aptian|Of Wallumbilla Formation.||||||
5593|Doncaster Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
5593|Doncaster Member|30020|6|Mentioned|p40|||||||||
5593|Doncaster Member|30021|6|Mentioned|p87|||||||||
5593|Doncaster Member|30024|6|Mentioned|p331|||||||||
5593|Doncaster Member|30042|4|Described|p4|||Description of cores DM Wanaarine DDH1 & DM Weilmoringle DDH1.||||||
5593|Doncaster Member|30443|6|Mentioned|p2|||Map legend, also on P4. Aptian age.||||||
5593|Doncaster Member|30446|6|Mentioned|p39|||||||||
5593|Doncaster Member|30691|4|Described|p17|||See also P19,21,Table 4,6,7. Lower-Upper Cretaceous||||||
5593|Doncaster Member|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
5593|Doncaster Member|30696|4|Described|Table 4|||Aptian age||||||
5593|Doncaster Member|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|30854|4|Described|Table 4|||Lower Cretaceous||||||
5593|Doncaster Member|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
5593|Doncaster Member|31116|4|Described|p43|||See also P44||||||
5593|Doncaster Member|31208|6|Mentioned|Table 1|||See also Figs.2,3,5,6,7. Aptian.||||||
5593|Doncaster Member|31209|6|Mentioned|p159|||||||||
5593|Doncaster Member|31376|6|Mentioned|Table P4|||||||||
5593|Doncaster Member|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31432|4|Described|Table 1|||L.Cretaceous||||||
5593|Doncaster Member|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|32314|6|Mentioned|Fig. 4|||||||||
5593|Doncaster Member|32797|4|Described|Table 4|||L.Cret.||||||
5593|Doncaster Member|33016|6|Mentioned|p1|||On table||||||
5593|Doncaster Member|33017|6|Mentioned|p2|||||||||
5593|Doncaster Member|33070|4|Described|Table 2|||||||||
5593|Doncaster Member|33071|6|Mentioned|p6|||L.Cret.||||||
5593|Doncaster Member|33072|4|Described|Table 1|||L.Cret.||||||
5593|Doncaster Member|33075|6|Mentioned|p445|||||||||
5593|Doncaster Member|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33088|4|Described|Table 3|||Wallumbilla Fm.||||||
5593|Doncaster Member|33090|4|Described|Table 4|||L.Cret.||||||
5593|Doncaster Member|33091|5|Briefly described|p9|||Stratigraphy||||||
5593|Doncaster Member|33092|5|Briefly described|p6|||Strat. table||||||
5593|Doncaster Member|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
5593|Doncaster Member|33368|6|Mentioned|p25|||Strat.table.||||||
5593|Doncaster Member|33372|6|Mentioned|p20|||||||||
5593|Doncaster Member|33414|6|Mentioned|p212|||Part of Wallumbilla Formation.||||||
5593|Doncaster Member|33448|4|Described|Table 1|||L.Cret.||||||
5593|Doncaster Member|33449|4|Described|Table 1|||L.Cret.||||||
5593|Doncaster Member|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33638|5|Briefly described|Table 1|||||||||
5593|Doncaster Member|33639|5|Briefly described|Table 2|||.Cret.||||||14-APR-08
5593|Doncaster Member|33640|4|Described|Table 2|||L.Cret.||||||
5593|Doncaster Member|33642|6|Mentioned|147-8,151,Tb.1,Fig.2|||Refes Vine & Day (1965).  Contains Roma fauna.||||||
5593|Doncaster Member|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33645|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33646|6|Mentioned|p16|||Geol. history.||||||
5593|Doncaster Member|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|33648|6|Mentioned|p21|||Stratigraphy.||||||
5593|Doncaster Member|33672|6|Mentioned|p44|||||||||
5593|Doncaster Member|33673|6|Mentioned|p287|||||||||
5593|Doncaster Member|34091|5|Briefly described|Table 1|||L.Cret.||||||
5593|Doncaster Member|34172|6|Mentioned|p54|||||||||
5593|Doncaster Member|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5593|Doncaster Member|34613|4|Described|Table 4|||||||||
5593|Doncaster Member|35239|6|Mentioned|p265|||||||||
5593|Doncaster Member|35560|6|Mentioned|p291|||||||||
5593|Doncaster Member|35663|6|Mentioned|p126|||||||||
5593|Doncaster Member|35793|6|Mentioned|Fig.3|||||||||
5593|Doncaster Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
5593|Doncaster Member|36251|6|Mentioned|Fig.2|||||||||
5593|Doncaster Member|36552|6|Mentioned|p59|||||||||
5593|Doncaster Member|36571|6|Mentioned|p101|||See also Table 4||||||
5593|Doncaster Member|36574|6|Mentioned|p602|||||||||
5593|Doncaster Member|37608|6|Mentioned|p324|||||||||
5593|Doncaster Member|37995|4|Described|p66|||||||||
5593|Doncaster Member|38199|6|Mentioned|p426|||||||||
5593|Doncaster Member|38226|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|38373|6|Mentioned|p619|||||||||
5593|Doncaster Member|38374|6|Mentioned|p605|||||||||
5593|Doncaster Member|38814|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|39070|4|Described|p364|||||||||
5593|Doncaster Member|39211|5|Briefly described|Fig.3|||See also Figs 7-9,11-16, etc. Correlation||||||
5593|Doncaster Member|39212|4|Described|p18|||Excursion site. See also P40||||||
5593|Doncaster Member|39215|6|Mentioned|p53|||||||||
5593|Doncaster Member|39216|6|Mentioned|p55|||Fauna||||||
5593|Doncaster Member|39478|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|39846|6|Mentioned|p44|||||||||
5593|Doncaster Member|39847|6|Mentioned|p38|||||||||
5593|Doncaster Member|39989|4|Described|p423|||||||||
5593|Doncaster Member|40199|6|Mentioned|Fig.2|||||||||
5593|Doncaster Member|40245|6|Mentioned|Table 2|||||||||
5593|Doncaster Member|40249|6|Mentioned|p38|||Mention P41||||||
5593|Doncaster Member|40541|4|Described|p111|||||||||
5593|Doncaster Member|40666|6|Mentioned|Table 2|||||||||
5593|Doncaster Member|40687|3|Fully described|p418|||||||||
5593|Doncaster Member|40801|6|Mentioned|p65|||||||||
5593|Doncaster Member|40832|3|Fully described|p457|||||||||
5593|Doncaster Member|40833|6|Mentioned|p468|||||||||
5593|Doncaster Member|40926|6|Mentioned|Table 2|||||||||
5593|Doncaster Member|40962|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|41064|6|Mentioned|p60,p62|||See also Fig.4||||||
5593|Doncaster Member|41086|3|Fully described|Fig.3|||||||||
5593|Doncaster Member|41088|6|Mentioned|p143|||||||||
5593|Doncaster Member|41196|6|Mentioned|Fig.1|||||||||
5593|Doncaster Member|41198|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|41219|6|Mentioned|Fig.4|||||||||
5593|Doncaster Member|41266|6|Mentioned|Fig.3|||||||||
5593|Doncaster Member|41523|6|Mentioned|p276|||||||||
5593|Doncaster Member|42071|6|Mentioned|p117|||||||||
5593|Doncaster Member|42429|5|Briefly described|Fig.3 P155|||||||||
5593|Doncaster Member|42446|6|Mentioned|p20|||||||||
5593|Doncaster Member|42494|5|Briefly described|Table 1 P24|||||||||
5593|Doncaster Member|42673|5|Briefly described|Fig.2, P184|||||||||
5593|Doncaster Member|43008|5|Briefly described|map legend|||of Wallumbilla Formation.||||||14-APR-08
5593|Doncaster Member|43564|6|Mentioned|p453||Aptian|(Late Aptian)||||||
5593|Doncaster Member|43989|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
5593|Doncaster Member|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
5593|Doncaster Member|44082|6|Mentioned|p6,8,10,16,22,26,34||Aptian|Part of Wallumbilla Formation. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
5593|Doncaster Member|44087|14|Not recorded|p4,opp.7|||||||||
5593|Doncaster Member|44089|14|Not recorded|not on card|||||||||
5593|Doncaster Member|44099|14|Not recorded|Map Legend||Early Cretaceous|Member of Wallumbilla Formation.||||||
5593|Doncaster Member|44346|14|Not recorded|p4|||||||||
5593|Doncaster Member|44373|14|Not recorded|p19-21|||Contains new species of ammonite Lithancylus Australia||||||
5593|Doncaster Member|44374|14|Not recorded|p10-12||Aptian|Remanie (reworked) fossils from this, in Coreena Member preferred explanation to extending time ranges of Roma or Tambo species.||||||
5593|Doncaster Member|44376|14|Not recorded|p3,4,12-14,16,20,22,|||p24. Of Wallumbilla Formation. Fossils.||||||
5593|Doncaster Member|44406|14|Not recorded|p4,opp.p6|||Basal member of Wilgunya Formation.||||||
5593|Doncaster Member|44408|14|Not recorded|p4,opp.p6|||||||||
5593|Doncaster Member|44414|14|Not recorded|p111,112,114||Cretaceous|||||||
5593|Doncaster Member|44417|2|Defined|p416-418,420|||Aptian fossils.||||||
5593|Doncaster Member|44668|14|Not recorded|p59,63|||||||||
5593|Doncaster Member|44915|14|Not recorded|p18||Early Cretaceous|Ref. to Vine and Day 1965.||||||
5593|Doncaster Member|45104|6|Mentioned|p35|||||||||
5593|Doncaster Member|45110|2|Defined|p115|Aptian|Aptian|Member of Wallumbilla Fm., formerly Wilgunya Fm. See also P10.||||||
5593|Doncaster Member|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
5593|Doncaster Member|46791|4|Described|p44|||||||||
5593|Doncaster Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
5593|Doncaster Member|46939|6|Mentioned|Fig.1|||||||||
5593|Doncaster Member|46984|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
5593|Doncaster Member|48919|4|Described|p71|||See also P72. L.Cretaceous||||||
5593|Doncaster Member|48920|3|Fully described|p58|||See also Table 8. Refers Vine & Day (1965).||||||14-APR-08
5593|Doncaster Member|48951|6|Mentioned|Table 1|||||||||
5593|Doncaster Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
5593|Doncaster Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
5593|Doncaster Member|60331|5|Briefly described|p34 Fig.3|Aptian|Aptian|Of the Wallumbilla Formation. Overlain by Jones Valley Member and Coreena Member. Geological Province: Eromanga Basin.||||||
5593|Doncaster Member|61312|5|Briefly described|p64, p67 Fig.E5|Aptian|Aptian|Of the Wallumbilla Formation. Mudstone. Interbedded with siltstone and fine sandstone of the Coreena Member. Geological Province: Eromanga Basin.||||||
5593|Doncaster Member|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
5593|Doncaster Member|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||Unit in Wallumbilla Formation.||Is overlain by Coreena Member.||
5593|Doncaster Member|63979|6|Mentioned|p48, Fig. 44|||Of Wallumbilla Formation. Underlies Coreena Member.||||||07-FEB-11
5593|Doncaster Member|64856|3|Fully described|p98-101|Aptian|Aptian|Vine and Day (1965). Lower Member of Wallumbilla Formation. Forms the lower part of Wilgunya Formation in the northern Eromanga Basin. Comprises mainly mudstone with subordinate siltstone, sandstone. Associated with palynofloral unit APK3, contains late Aptian faunas, and dinoflagellate assemblages equivalent to units ADK17 and 18.| | ||||28-NOV-17
5593|Doncaster Member|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Wallumbilla Formation. Underlies the Coreena Member; overlies the Bungil Formation.||||||22-MAR-12
5593|Doncaster Member|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation? Underlies the Coreena Member, Overlies the Bungil Formation.||||||
5593|Doncaster Member|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||Of Wallumbilla Formation?||||||
5593|Doncaster Member|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation. Underlies the Coreena Member, Overlies the Bungil Formation in the Surat Basin.||||||
5593|Doncaster Member|65119|6|Mentioned|p512 Fig 6, p521 Fig 14|||Present in the Cabawin 1, Flinton 1 and MacIntyre 1 wells.||||||07-MAR-12
5593|Doncaster Member|65384|5|Briefly described|S116, S118|||Probably Aptian. Of Wallumbilla Formation. Dominated by a marine shelf depositional environment.||||||21-DEC-10
5593|Doncaster Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Wallumbilla Formation.||||
5593|Doncaster Member|66623|3|Fully described|p239, p242, pp256-261.|Aptian|Aptian|Correlates with superseded Wittabrenna and Oornoo Beds (Rose and Brunker 1969) and informal Wittabrenna Shale (Morton 1982). Hosts the White Cliffs opal field. Very poorly exposed. Thickness from 150 m to 300 m. Contains a wide range of fossils.||Unit in Wallumbilla Formation.||Disconformably overlies Cadna-owie Formation. Is disconformably and gradationally overlain by Coreena Member.|Grey, muddy sandstone and siltstone; local large spherical calcareous concretions and cone-in-cone carbonate; black shale and minor sandstone with abundant dropstones; black pyritic and bioturbated mudstone, claystone, shale, micritic limestone.|07-JUN-13
5593|Doncaster Member|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Wallumbilla Formation||||
5593|Doncaster Member|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.|||Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67133|5|Briefly described|p17|Early Cretaceous|Early Cretaceous|Deposited during a rapid transgression episode.||Wallumbilla Formation.||Is overlain by Coreena Member.||
5593|Doncaster Member|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Is overlain by Coreena Member.|Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.||Overlies Cadna-owie Formation. Is overlain by Coreena Member of Wallumbilla Formation.|Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Wallumbilla Formation.|||Marine mudstone and subordinate siltstone.|
5593|Doncaster Member|67784|5|Briefly described|p25, p26, p28-33|Aptian|Aptian|Age derived from biostratigraphy. 120-150m thick. Northern Eromanga Basin.||Wallumbilla Formation||Overlies Cadna-owie Formation. Is overlain by Jones Valley Member/Coreena Member.|Thick mudstone unit|08-FEB-18
5593|Doncaster Member|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Bungil Formation. Is overlain by Coreena Member.||
5593|Doncaster Member|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shallow marine environment. Shown on cross-sections and time-space plot and basement interpretation only.||Unit in Wallumbilla Formation.||Is overlain conformably by Coreena Member.|Mudstone with subdominant siltstone.|
5593|Doncaster Member|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||||
5593|Doncaster Member|68206|6|Mentioned|p32-33|Aptian|Aptian|Carpentaria, NE Eromanga Basins.||Wallumbilla Formation.||||
5593|Doncaster Member|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||Wallumbilla Formation.||Overlies Bungil Formation. Is overlain by Coreena Member.||
5593|Doncaster Member|68593|5|Briefly described|p4, p46|Early Cretaceous|Early Cretaceous|||Wallumbilla Formation.||Overlies Bungil Formation. Is overlain by Coreena Member.|Mudstone with subordinate siltstone.|
5593|Doncaster Member|68734|5|Briefly described|p218 Fig.2|Aptian|Barremian|Eromanga Basin (NE) and Surat Basin. Shallow marine.||Of the Wallumbilla Formation.||||16-JAN-17
5593|Doncaster Member|68821|6|Mentioned|p295|||Surat Basin. Equivalent to the Bulldog Shale.|||||Comprises pyrite and carbonaceous-rich marine mudstones and siltstones interbedded with fine sandstones.|
5593|Doncaster Member|69001|6|Mentioned|p30|Cretaceous|Cretaceous|||Of the Rolling Downs Group.||||
5593|Doncaster Member|69379|5|Briefly described|map legend|Cretaceous|Cretaceous|||Of Wallumbilla Formation|||Carbonaceous mudstone, siltstone, minor siltstone [?]; some glauconitic and calcareous; shelly fossils|03-SEP-14
5593|Doncaster Member|69457|5|Briefly described|p41:3, 10|Early Cretaceous|Early Cretaceous|Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
5593|Doncaster Member|69594|4|Described|p519, p526, p528-529, p538|Albian|Barremian|Vine et al. (1965). Eromanga, northern Surat Basins. Previously known as the Blackdown Formation of Laing and Power (1959); Woods (1961). 50-60m thick in outcrop; may be up to 150m thick subsurface. Has an abundant and diverse fossil fauna (listed). Represents maximum flooding of the Great Australian Superbasin with shallow-marine to basinal-marine deposits with contemporary volcanic detritus.||Basal Wallumbilla Formation.||Conformably overlies Cadna-owie, Bungil, Gilbert River Formations. Is overlain conformably by Jones Valley, Coreena Members.|Mudstone, siltstone, concretionary limestone and lesser labile and glauconitic sandstone. Sporadically fossiliferous.|
5593|Doncaster Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||Wallumbilla Formation||Overlies Wyandra Sandstone Member, overlain by Coreena Member||
5593|Doncaster Member|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||Unit in Wallumbilla Formation.||||
5593|Doncaster Member|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Wallumbilla Formation|||Marine mudstone and subordinate siltstone.|20-JAN-22
5593|Doncaster Member|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Wallumbilla Formation|||Marine mudstone and lesser siltstone.|20-JAN-22
5593|Doncaster Member|70720|5|Briefly described|p6, p24-25|Aptian|Aptian|Eromanga Basin.||Wallumbilla Formation.||Nonconformably overlies Granite Springs Granite. Is overlain by Coreena Member.||
5593|Doncaster Member|70821|4|Described|p21-22 Figs.2.6-7, p28, p30-31, p33, p72|Early Cretaceous|Early Cretaceous|See also p80, p82, p86-89, p111-112, p115-116. Eromanga and Surat Basins. Varying thicknesses given (65-241m) from wells. Shallow to deep marine deposits. Contains a diverse, mostly marine, biota (molluscs, reptiles, fish). Appears as Doncaster Formation on p30. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Highly conductive. Hydrostratigraphic properties.||Wallumbilla Formation.||Overlies Wyandra Sandstone Member (Cadna-owie Formation), Hooray Sandstone or Minmi Member (Bungil Formation). Is overlain conformably by Coreena Member. Equivalent to lower Bulldog Shale.|Mudstone, dark, glauconitic; minor sandstone and siltstone; partly calcareous.|
5593|Doncaster Member|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Barremian-Aptian.||Wallumbilla Formation.||Overlies Bungil Formation. Is overlain by Coreena Member.||
5593|Doncaster Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
5593|Doncaster Member|71251|5|Briefly described|p11-13, p15, p17, p49|||Eromanga Basin. Natural gamma wireline log. Conductivity diagram.||Wallumbilla Formation.||Is overlain by Coreena Member.||
5593|Doncaster Member|71863|5|Briefly described|p5|Aptian|Aptian|Eromanga Basin.||Wallumbilla Formation||Overlies the Wyandra Sandstone Member. Overlain by the Coreena Member.||
5593|Doncaster Member|71864|6|Mentioned|p13-p14, p17|||Could not be distinguished in GSQ Eulo 2 borehole.||Wallumbilla Formation||||
5593|Doncaster Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||Wallumbilla FZ.||Overlies Cadna-owie and Bungil FZs; Kumbarilla and Ronlow beds. Is overlain by Coreena Member.||
5593|Doncaster Member|73203|6|Mentioned|p653|Early Cretaceous|Early Cretaceous|Hosts White Cliffs opal.||Wallumbilla Formation||||
5605|Donkey Gap Gabbro|42726|5|Briefly described|map legend|||Not a variation on reserved name Donkey Gap Volcanics.||||||
5620|Doona Sandstone Member|22857|5|Briefly described|p546 App.1 Tb.A1.12|Late Jurassic|Middle Jurassic|Of the Ukebung Formation. Dull grey to white, fine to medium-grained arenite. Max. thickness: 3m. Geological Province: Surat Basin.||||||
5620|Doona Sandstone Member|35095|6|Mentioned|p112|||||||||
5620|Doona Sandstone Member|61377|5|Briefly described|p152|Middle Jurassic|Middle Jurassic|Together with Digilah Fm + Ukebung Fm, is equivalent of Purlawaugh Fm in other parts of basin. Dull grey to white, fine- to med.-gr.sst with angular qtz grains + rounded fragments of flint clay in a kaolinite matrix;plant remains.Geol.Prov:Surat Basin.||||||07-FEB-11
5621|Doonbah Clay|40726|6|Mentioned|p227|||||||||
5622|Doonbara Formation|22730|4|Described|p567-70|Miocene|Oligocene|after Wopfner 1974||||||
5622|Doonbara Formation|23336|5|Briefly described|p4|Miocene|Miocene|||||||21-MAR-06
5622|Doonbara Formation|29658|6|Mentioned|p5|||||||||
5622|Doonbara Formation|29660|6|Mentioned|p7|||||||||
5622|Doonbara Formation|30055|6|Mentioned|p153|||||||||
5622|Doonbara Formation|30056|6|Mentioned|p140|||||||||
5622|Doonbara Formation|30921|6|Mentioned|Map legend|Miocene|Miocene|||||||
5622|Doonbara Formation|30924|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
5622|Doonbara Formation|33820|6|Mentioned|Map legend|Miocene|Miocene|Prob. Miocene||||||
5622|Doonbara Formation|33827|6|Mentioned|p14|||See also Table 1||||||
5622|Doonbara Formation|33828|6|Mentioned|p11|||||||||
5622|Doonbara Formation|33937|4|Described|p6|||See also p7.||||||13-MAR-19
5622|Doonbara Formation|35149|6|Mentioned|Fig.4|||||||||
5622|Doonbara Formation|35691|6|Mentioned|p5|||||||||
5622|Doonbara Formation|35793|6|Mentioned|Fig.2|||||||||
5622|Doonbara Formation|38605|6|Mentioned|p35|||||||||
5622|Doonbara Formation|39322|6|Mentioned|Fig.3|||||||||
5622|Doonbara Formation|39445|5|Briefly described|Table 14|||||||||
5622|Doonbara Formation|39908|6|Mentioned|p10|||||||||
5622|Doonbara Formation|40910|6|Mentioned|p19|||||||||
5622|Doonbara Formation|41098|6|Mentioned|p177|||||||||
5622|Doonbara Formation|42746|5|Briefly described|p17|||||||||
5622|Doonbara Formation|42905|5|Briefly described|p23, Fig 5.3|||||||||
5622|Doonbara Formation|43053|5|Briefly described|Map Legend|Pleistocene|Tertiary|Undifferentiated Early Tertiary to Plio-Pleistocene alluvial, colluvial and residual clastics, commonly silicified or ferruginised.||||||25-MAY-05
5622|Doonbara Formation|43258|5|Briefly described|Map Legend|Pliocene|Paleocene|||||||
5622|Doonbara Formation|43298|6|Mentioned|Map Legend|Pleistocene|Tertiary|||||||
5622|Doonbara Formation|44133|5|Briefly described|p194, 190 Fig. 10.30|Early Pliocene|Late Miocene|Geological Province: Lake Eyre Basin. Thickness: 40m.||||||03-MAY-13
5622|Doonbara Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
5622|Doonbara Formation|60080|5|Briefly described|Map legend|Pliocene|Miocene|Brick-red ferruginous pisolitic silty-sandstone. Interfingers with Cadelga Limestone in the Haddon Syncline.||||||03-MAY-13
5622|Doonbara Formation|60953|5|Briefly described|Map Legend|Miocene|Eocene|Alluvial, colluvial and residual clastics, commonly silicified or ferruginised.||||||27-APR-05
5622|Doonbara Formation|61108|5|Briefly described|map legend|Pleistocene|Paleocene|Undifferentiated early Tertiary to Plio-Pleistocene alluvial, colluvial and residual clastics, commonly silcreted or ferricreted. Geological Province: Lake Eyre Basin.||||||02-JUN-05
5622|Doonbara Formation|66131|4|Described|p240, p242 Fig.2, p245, p249.|Miocene|Miocene|~7-40 m thick. Pisolitic ferricrete is extensively developed in this unit in the northeastern and central parts of the Lake Eyre Basin.||||Overlies Eyre Formation or Cordillo Silcrete. Overlain by the Cadelga Limestone. equivalent to the Whitula Formation in Qld.|Pisolitic, ferruginous fine to medium sand.|25-AUG-22
5622|Doonbara Formation|66623|3|Fully described|pp270-272, pp282-284.|Miocene|Oligocene|Youngest lithified sedimentary rock in Koonenberry Belt: Late Oligocene - Early Miocene. Wopfner (1974) tentatively correlated with basal Etadunna Formation (in SA) and Namba Formation. Uplift of Cordillo Silcrete and Eyre Formation led to accelerated fluvial erosion and deposition of tens of metres of sandstone and conglomerate at the foot of fault scarps.||||Unconformably overlies Cordillo Silcrete.|Basal ferruginous silcrete conglomerate with reworked silcrete clasts; succeeded by distinctive brick-red, friable, ferruginous quartzose sandstone and granule conglomerate with maghemite pisoliths; bedding irregular, generally less than 20cm thick.|03-JUN-13
5622|Doonbara Formation|66922|5|Briefly described|Map legend|Neogene|Neogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|67119|5|Briefly described|Map legend.|Pliocene|Miocene|Fluvial facies.|||||Fine- to medium-grained, pisolitic and ferruginous sand.|
5622|Doonbara Formation|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|19-SEP-11
5622|Doonbara Formation|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|20-SEP-13
5622|Doonbara Formation|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.|||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|69001|6|Mentioned|p2 Fig.1B, p23, p23 Fig.13|Neogene|Neogene|||||||
5622|Doonbara Formation|69019|6|Mentioned|p105 Fig.25.|Miocene|Miocene|Callabonna Sub-basin.||||||
5622|Doonbara Formation|69023|6|Mentioned|p108|Miocene|Miocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
5622|Doonbara Formation|69599|5|Briefly described|p584, p601-602|Pliocene|Miocene|A thin, sporadically outcropping unit, mainly in SA and NSW but extending into QLD. Thickness generally 7-10m, but up to 40m.||||Is overlain by, and locally interdigitates with, Cadelga Limestone. Correlated with Whitula, Poodyea Formations; Horse Creek, Noranside, Austral Downs Limestones; and Mount Coley Sinter.|Silty, commonly pisolitic, ferruginous sandstone.|
5622|Doonbara Formation|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|
5622|Doonbara Formation|70336|5|Briefly described|Map legend|Pliocene|Miocene||||||Pisolitic and ferruginous, fine- to medium-grained sand. Fluvial facies.|
5622|Doonbara Formation|70648|5|Briefly described|Map Legend|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|18-JAN-22
5622|Doonbara Formation|70649|5|Briefly described|Map Legend|Neogene|Paleogene||||||Ferruginous quartzose sandstone and granule conglomerate with maghemite pisolites.|18-JAN-22
5622|Doonbara Formation|71415|6|Mentioned|p11|Neogene|Paleogene|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||||
5622|Doonbara Formation|73106|5|Briefly described|Map legend.|Pliocene|Miocene||||||Sand, pisolitic and ferruginous, fine to medium-grained. Fluvial facies.|
5628|Doonside Formation|23799|6|Mentioned|p18|||Of Curtis Island Group.||||||
5628|Doonside Formation|24420|5|Briefly described|p7|Carboniferous|Late Devonian|Of Curtis Island Group. Includes the Balnagowan Volcanic Member.||||||
5628|Doonside Formation|24488|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||
5628|Doonside Formation|24489|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||
5628|Doonside Formation|24490|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group. Chert, mudstone, minor tuff and arenite.||||||04-SEP-08
5628|Doonside Formation|24615|5|Briefly described|CD|Carboniferous|Devonian|[DCcd].  Chert, jasper, mudstone, siltstone, lithic sandstone, tuff, limestone, and altered basalt.||||||
5628|Doonside Formation|30451|6|Mentioned|p8|||Lower ? Palaeozoic age||||||
5628|Doonside Formation|30777|4|Described|p417|||Discussed.||||||18-AUG-08
5628|Doonside Formation|31657|4|Described|p91|||See also P92. Ordovician - Silurian.||||||
5628|Doonside Formation|31658|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5628|Doonside Formation|31659|2|Defined|p19|Early Paleozoic|Early Paleozoic|max. thickness: >9000ft. red, green and white chert, mudstone, limestone, acid tuff, tuffaceous arenite. See also Table 1.||||||07-NOV-08
5628|Doonside Formation|32357|4|Described|Table 1|||||||||
5628|Doonside Formation|32358|4|Described|Table 1|||||||||
5628|Doonside Formation|32361|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5628|Doonside Formation|33769|5|Briefly described|p150|||||||||
5628|Doonside Formation|33774|3|Fully described|p6|||See also P7. ?Pre Devonian.||||||18-AUG-08
5628|Doonside Formation|34408|6|Mentioned|p185|||On table.||||||
5628|Doonside Formation|34947|6|Mentioned|p360|||||||||
5628|Doonside Formation|35008|6|Mentioned|p177|||||||||
5628|Doonside Formation|35266|6|Mentioned|p203|||||||||
5628|Doonside Formation|36211|6|Mentioned|p269|||||||||
5628|Doonside Formation|36333|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous||||||
5628|Doonside Formation|36488|6|Mentioned|p3|||||||||
5628|Doonside Formation|36528|6|Mentioned|p170|||||||||
5628|Doonside Formation|37453|5|Briefly described|p313|||||||||
5628|Doonside Formation|37676|6|Mentioned|p4|||||||||
5628|Doonside Formation|38081|5|Briefly described|Table 1|||||||||
5628|Doonside Formation|38391|6|Mentioned|p6|||||||||
5628|Doonside Formation|38406|5|Briefly described|p9|||||||||
5628|Doonside Formation|38447|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous||||||
5628|Doonside Formation|39445|5|Briefly described|Table 6|||||||||
5628|Doonside Formation|39632|6|Mentioned|p208|||||||||
5628|Doonside Formation|39973|6|Mentioned|p4|||||||||
5628|Doonside Formation|39998|6|Mentioned|p189|||||||||
5628|Doonside Formation|40246|6|Mentioned|Fig.1|||||||||
5628|Doonside Formation|40475|6|Mentioned|p2|||||||||
5628|Doonside Formation|40960|6|Mentioned|p215|||||||||
5628|Doonside Formation|41576|4|Described|p16|||See also Table 1.||||||18-AUG-08
5628|Doonside Formation|41577|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|||||||
5628|Doonside Formation|41922|4|Described|Table 1, P11|||||||||
5628|Doonside Formation|41927|6|Mentioned|p61|||||||||
5628|Doonside Formation|42143|6|Mentioned|p592|||||||||
5628|Doonside Formation|42547|4|Described|p53|||Age Devonian?||||||
5628|Doonside Formation|42660|4|Described|p23 p169|||||||||
5628|Doonside Formation|42901|5|Briefly described|p404|||see also Fig.12 P412.||||||18-AUG-08
5628|Doonside Formation|45107|6|Mentioned|p6|||||||||
5628|Doonside Formation|50207|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Curtis Island Group.  Contains the Balnagowan Volcanic Member.||||||17-MAY-04
5628|Doonside Formation|50208|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
5628|Doonside Formation|50209|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
5628|Doonside Formation|50212|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||28-MAY-08
5628|Doonside Formation|60557|5|Briefly described|p19 Fig. 5b, p23|Early Carboniferous|Late Devonian|Contains the Balnagowan Volcanic Member.  Massive to ribbon-bedded chert and mudstone, with less abundant mafic volcanics, minor sandstone and rare small limestone lenses. See also p36.||||||18-AUG-08
5628|Doonside Formation|61035|5|Briefly described|p14|||Geological Province: Wandilla Province. Consists of chert-mudstone assemblage + some lithic sandstone, tuff, limestone, + altered basalt.||||||07-FEB-11
5628|Doonside Formation|64398|5|Briefly described|Map legend|Carboniferous|Late Devonian|Of the Curtis Island Group. Chert, jasper, mudstone, siltstone, lithic sandstone, limestone and altered basalt.||||||
5628|Doonside Formation|64399|5|Briefly described|Map legend|Carboniferous|Late Devonian|Of Curtis Island Group. Comprises predominantly chert, jasper, mudstone, siltstone, lithic sandstone, limestone and altered basalt; with a subordinate unit of mudstone, siltstone, lithic sandstone, limestone and altered basalt.||||||
5628|Doonside Formation|64429|5|Briefly described|p20|Carboniferous|Devonian|Juxtaposed against Chalmers Formation||||||
5628|Doonside Formation|68008|3|Fully described|p50, p110-113, p119, p270, p273, p297|Early Carboniferous|Early Devonian|See also p426, p465, p480, p616. Kirkegaard et al. (1970), who defined it as the uppermost [sic] unit in the Group. Part of the Wandilla terrane. Usually forms prominent hills and strike ridges. Deep ocean-floor association. Repetition by faulting makes thickness determination impossible; certainly less than the 2100-3600m of Kirkegaard et al. (1970). Age from conodonts. Hosts Mn mineralisation. Geophysics modelling.||Basal Curtis Island Group.|Balnagowan Volcanic Member.|Is overlain by Alton Downs Basalt. Is faulted against Channer Creek beds. Is intruded by Targinie Quatrz Monzonite and Mount Hedlow Trachyte. Time equivalent of Mount Alma Formation.|Rhythmically interbedded radiolarian chert and jasper with argillite; minor greywacke, fine-grained volcaniclastic sandstone, and limestone.|
5628|Doonside Formation|68679|4|Described|p317-318, p338, p425|Mississippian|Devonian|Coastal Subprovince, Wandilla Province, New England Orogen. Forms a discontinuous belt immediately east of the Yarrol Fault, from Mundubbera to The Pointers. Includes a belt containing lenses of manganese mineralisation (psilomelane with some pyrolusite) from Mount Miller to Mount Beecher. Formed by slow deposition on abyssal sea-floor. Estimated thickness of 2100-3600m is almost certainly a gross overestimate from fault repetition. Brief mention of possible time-equivalence with Mount Alma Formation.||Curtis Island Group.|Balnagowan Volcanic Member.|Is faulted against, and locally overlain by, Wandilla Formation.|Ribbon chert and jasper, thin-bedded with slumps to very thick-bedded and massive; argillite and minor tuff and limestone; rhythmically interbedded radiolarian chert and mudstone dominate. Sporadic spilitic volcanics.|
5642|Dorrigo Mountain Complex|22636|6|Mentioned|p473||Permian|||||||
5642|Dorrigo Mountain Complex|23720|5|Briefly described|Map Legend|Late Permian||Microdiorite, microgranite.||||||15-DEC-04
5642|Dorrigo Mountain Complex|24127|6|Mentioned|p4|||||||||
5642|Dorrigo Mountain Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
5642|Dorrigo Mountain Complex|31695|6|Mentioned|Fig. 1|||||||||
5642|Dorrigo Mountain Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
5642|Dorrigo Mountain Complex|44450|6|Mentioned|p21|||Geological Province: New England Fold Belt.||||||
5642|Dorrigo Mountain Complex|69639|6|Mentioned|p217|Sakmarian|Asselian||295.5 +/- 3.0 Ma (SHRIMP U-Pb)|Hillgrove Supersuite||||
5642|Dorrigo Mountain Complex|71628|5|Briefly described|p2: 33-36; p3: 3, 10, 27|||Leitch et al. (1971). Crops out ~13 km SE of Dorrigo as a broadly circular, c.4 x 5 km pluton. Assigned to the Bakers Creek Suite by Landenberger (1996) and to the Bakers Creek Supersuite by Landenberger et al. (2010). Has similarities with Rockisle Suite. Distinctive geochemistry described.|295.5 +/- 3 Ma (Rosenbaum et al., 2012).|||Intrudes Buffers Creek Formation and McGraths Hump Metabasalt. Is intruded by Dundurrabin Granodiorite.|Mafic igneous complex comprising fine-grained (quartz) gabbro, (quartz) diorite, monzogranite and minor microgranodiorite.|
5644|Dorroughby Tuff Member|34340|6|Mentioned|Table 6.1|||||||||
5644|Dorroughby Tuff Member|43881|14|Not recorded|p6-7,49,56-7,132||Tertiary|This name supersedes 'Dorroughby Tuff'||||||
5654|Doubtful River Gabbro|39627|6|Mentioned|p267|||||||||
5654|Doubtful River Gabbro|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Og2||||||
5654|Doubtful River Gabbro|45147|6|Mentioned|M48|||||||||
5654|Doubtful River Gabbro|60078|6|Mentioned|Map Legend|Ordovician|Ordovician|||||||
5654|Doubtful River Gabbro|63278|4|Described|p157|Eastonian|Darriwilian |Intrudes Nine Mile Volcanics and possibly Temperance Formation. Age: 445+/-10Ma (K-Ar hornblende). Geological Province: Kiandra Volcanic Belt, LFB. Consists of high-k to shoshonitic pyroxenite-gabbro-monzonite sills.||||||07-FEB-11
5654|Doubtful River Gabbro|63290|6|Mentioned|p394 Tb. 1|Late Ordovician|Late Ordovician|Age: 455+/-10Ma (K/Ar). Geological Province: Kiandra Volcanic Belt. Belived to be related to the Nine Mile Volcanics.||||||
5654|Doubtful River Gabbro|63293|5|Briefly described|p470|||Age: 455+/-10Ma (K-Ar, Owen and Wyborn 1979; Percival and Glen 2007). Geological Province: Kiandra Volcanic Belt.||||||07-FEB-11
5668|Douro Group|22638|6|Mentioned|p32|||||||||12-SEP-05
5668|Douro Group|22691|6|Mentioned|P321||Silurian|||||||
5668|Douro Group|23214|6|Mentioned|p168|||Intruded by the Young Granodiorite.||||||
5668|Douro Group|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
5668|Douro Group|24266|5|Briefly described|p1481|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
5668|Douro Group|24317|5|Briefly described|p15 Fig.1|Early Silurian|Early Silurian|Shallow marine-subaerial volcanics.||||||
5668|Douro Group|24417|4|Described|p44|Silurian|Silurian|Overlies Forbes Group.||||||
5668|Douro Group|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
5668|Douro Group|30732|6|Mentioned|p184|||||||||
5668|Douro Group|30734|4|Described|p17|||||||||
5668|Douro Group|32675|5|Briefly described|p7|||Nomenclature. Refers Link (1971); Brunker & Offenberg (9170).||||||01-SEP-08
5668|Douro Group|32820|6|Mentioned|Table 1|||Refers Pogson & Baker (1974)||||||
5668|Douro Group|32858|6|Mentioned|p32|||||||||
5668|Douro Group|33004|6|Mentioned|p175|||||||||
5668|Douro Group|35070|2|Defined|p77|Late Silurian|Middle Silurian|Middle to Late Silurian.||||||01-SEP-08
5668|Douro Group|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
5668|Douro Group|35384|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Late Silurian||||||
5668|Douro Group|35386|3|Fully described|p14|||Age discussed P40.||||||01-SEP-08
5668|Douro Group|35607|6|Mentioned|p168|||See also P169,170.||||||
5668|Douro Group|35608|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
5668|Douro Group|35609|4|Described|p7|||||||||
5668|Douro Group|36411|6|Mentioned|p268|||Refs Cramsie et al 1978 for redefinition.||||||
5668|Douro Group|36413|6|Mentioned|Table 3|||||||||
5668|Douro Group|37529|6|Mentioned|p8|||||||||
5668|Douro Group|38151|6|Mentioned|Table 1|||||||||
5668|Douro Group|39221|6|Mentioned|p263|||||||||
5668|Douro Group|40328|3|Fully described|p88|||||||||
5668|Douro Group|40497|6|Mentioned|Map legend|Silurian|Silurian|||||||
5668|Douro Group|40498|6|Mentioned|p366|||||||||
5668|Douro Group|40882|6|Mentioned|p24|||||||||
5668|Douro Group|42313|6|Mentioned|p122|||||||||
5668|Douro Group|42994|6|Mentioned|p73|||||||||
5668|Douro Group|43795|5|Briefly described|p280|||||||||
5668|Douro Group|44093|5|Briefly described|p187 App. 1|Silurian|Silurian|Volcanics. Geological Province: Lachlan Fold Belt.||||||
5668|Douro Group|45147|6|Mentioned|M128|||||||||
5668|Douro Group|50230|5|Briefly described|Map legend|Ludlow|Wenlock|||||||
5668|Douro Group|50231|5|Briefly described|Map Legend|Ludlow|Wenlock|Includes: Yass Formation, Hawkins Volcanics, Goobragandra Volcanics.||||||
5668|Douro Group|50232|5|Briefly described|Map legend|Wenlock|Wenlock|Contains the Hawkins Volcanics.||||||
5668|Douro Group|50628|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Illunie Volcanics, Glenisla Volcanics.||||||
5668|Douro Group|60008|5|Briefly described|Map Legend|Silurian|Silurian|Felsic volcanics.||||||08-JUL-04
5668|Douro Group|60009|5|Briefly described|Map Legend|Wenlock|Wenlock|Includes: Glenisla Volcanics, Illunie Volcanics.||||||13-JUL-04
5668|Douro Group|61910|5|Briefly described|p152|Silurian|Silurian|Includes Hawkins Volcanics. Geological Province: Lachlan Fold Belt.||||||
5668|Douro Group|64295|5|Briefly described|p198 Fig. 1, p199|Early Silurian|Early Silurian|||||||
5668|Douro Group|66300|6|Mentioned|p92.|Middle Silurian|Middle Silurian||||Includes Hawkins Volcanics.|||
5668|Douro Group|67820|6|Mentioned|p134, p136 Fig.3|Silurian|Silurian|Volcanics in this Group are sulphur-rich and host orogenic base metal-gold vein occurrences.||||||
5668|Douro Group|68592|3|Fully described|p282, p298, p324, p354, p356, p427-558|Ludlow|Wenlock|See also p17, p73 Tb.5, p125-6, p238-9. The complicated history of this unit's stratigraphic nomenclature, starting from the Douro Series of Brown (1940), is dealt with in detail. Over 5,000m thick. Includes major resources of lime. Unlikely to be older than earliest Wenlock; age determinations detailed. Has close geochemical affinity with Young Suite. Taemas, Yass and Frogmore structural zones: deformation and metamorphism described.|c.432 Ma max.||Includes Laidlaw, Hawkins and Goobarragandra Volcanics; Yanawe, Boambolo, Glen Bower and Yass Formations.|Unconformably overlies Kenyu Group. Is overlain conformably by Hattons Corner Group, and unconformably by Black Range and Hervey Groups. Is intruded by Bullenbalong Supersuite.|Felsic ignimbrites and volcaniclastics; terrestrial and marine deposits.|
5668|Douro Group|69635|6|Mentioned|p19|Wenlock|Wenlock|||||||15-JUL-15
5668|Douro Group|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|On Yass, Gunning and Boorowa 1:100 000 mapsheets. Related units inferred from Time-Space Plot.|||Includes Boambolo Formation, Hawkins Volcanics, Laidlaw Volcanics, Goobarragandra Volcanics, Glen Bower Formation, Yanawe Formation, Yass Formation.|Is overlain by Hattons Corner Group. Unconformably overlies Laidlaw Volcanics.||
5668|Douro Group|70540|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Boamblo Formation, Hawkins Volcanics, Laidlaw Volcanics, Goobarragandra Volcanics, Glen Bower Formation, Yanawe Formation, Yass Formation.|||
5668|Douro Group|70541|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Hawkins Volcanics.|||
5668|Douro Group|70545|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Hawkins Volcanics, Goobarragandra Volcanics, Yass Formation.|||
5668|Douro Group|70546|5|Briefly described|Map Legend|Silurian|Silurian||||Includes Boambolo Formation, Hawkins Volcanics, Laidlaw Volcanics, Glen Bower Formation, Yanawe Formation, Yass Formation|||
5668|Douro Group|71069|6|Mentioned|p23, p75, p95|Silurian|Silurian|Occurs in an imbricate thrust system along with the Warbisco Shale and the Bumballa Formation.|||Includes the Hawkins Volcanics|||
5668|Douro Group|71656|3|Fully described|p10 Fig.1, p12 Fig.2, p19-23|Ludlow|Wenlock|Includes a variety of brachiopods, conodonts, graptolites, rugose and tabulate corals, pentamerides, sponges, crinoids, nautiloids,bryazoan and bivalves.|||Laidlaw Volcanics, Yanawe Formation, Boambolo Formation, Glen Bower Formation, Yass Formation, Eurimbla Formation, Goolbarragandra Volcanics and Hawkins Volcanics.|Partially underlying Hattons Corner Group.|Includes volcanics and fossiliferous strata.|
5668|Douro Group|73215|5|Briefly described|p992, 994-995, 1001||||||Goobarragandra, Hawkins (lower), Laidlaw (upper), Volcanics; Yass, Glen Bower, Boambolo, Yanawe Formations.||Interbedded sedimentary units and massive volcanic units.|
5685|Downderry Limestone Member|13139|5|Briefly described|p4|Late Ordovician|Late Ordovician|Of the Ballingoole Limestone.||||||
5685|Downderry Limestone Member|23214|4|Described|p39|Eastonian|Eastonian|Of Ballingoole Limestone. Age determined by fossil assemblages. Max. thickness 7.5m.  Underlying unit: Clearview Limestone Member.||||||21-FEB-18
5685|Downderry Limestone Member|23334|6|Mentioned|4|||||||||
5685|Downderry Limestone Member|24398|5|Briefly described|p264|Eastonian|Eastonian|Of Bowan Park Limestone Subgroup.  Geological Province: Lachlan Fold Belt.||||||
5685|Downderry Limestone Member|33063|2|Defined|p84|Ordovician|Ordovician|||||||
5685|Downderry Limestone Member|33740|6|Mentioned|Fig.1|||||||||
5685|Downderry Limestone Member|38219|6|Mentioned|Table 2|||||||||
5685|Downderry Limestone Member|40136|5|Briefly described|p17|||See also P24||||||
5685|Downderry Limestone Member|41046|6|Mentioned|Fig.2|||||||||
5685|Downderry Limestone Member|62799|5|Briefly described|p420|Late Ordovician|Late Ordovician|Topmost Bowan Park Group. Around Malachi's Hill on the Molong High. Late Eastonian. Contains trilobites.||Unit in Ballingoole Formation.||||04-DEC-12
5685|Downderry Limestone Member|63278|5|Briefly described|p153|||Of the Ballingoole Limestone, Bowan Park Limestone Subgroup. Comprises fossiliferous calcarenite debris. Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
5685|Downderry Limestone Member|67322|5|Briefly described|Fig.5; p23|Katian|Katian|T.tumidus Zone: indicative of a late Eastonian age. Occurs in the Bowan Park region.||Of the Ballingoole Limestone.||Is overlain by Malachis Hill Formation.||21-FEB-18
5685|Downderry Limestone Member|70684|5|Briefly described|p39 Fig.17, p40-42|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Represents an abrupt deepening/drowning event in the late Eastonian.||Ballingoole Limestone.|||Grey weathering to brown calcarenite, massive to bedded, with angular quartz grains and occasional lithic fragments. Shallow-water, fossiliferous calcarenite debris infilling probable submarine channels.|
5685|Downderry Limestone Member|70754|5|Briefly described|p447, p450-451, p455, p457-464, p466-468|Katian|Katian|See also p472-473, p477-480. Contains a comparatively rich and diverse lingulate fauna: species listed. Systematic palaeontological descriptions.||Ballingoole Limestone.||Is overlain conformably by Malachis Hill Formation.|Calcarenite.|
5685|Downderry Limestone Member|71091|6|Mentioned|p143|||Contains late Eastonian conodonts.||Ballingoole Limestone.||||
5686|Doyalson Formation|31549|6|Mentioned|p159|||Stratigraphic succession||||||
5686|Doyalson Formation|31551|6|Mentioned|p93|||||||||
5686|Doyalson Formation|34270|6|Mentioned|p254|||Fassifern Coal||||||
5688|Doyles Creek Subgroup|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wollombi Coal Measures (Singleton Supergroup). Max. thickness: 60m. Geological Province: Sydney Basin.||||||
5688|Doyles Creek Subgroup|22969|4|Described|Fig 4.1a||Late Permian|Wollombi Coal Measures.||||||
5688|Doyles Creek Subgroup|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures.   Geological Province: Sydney Basin||||||
5688|Doyles Creek Subgroup|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures. Geological Province: Sydney Basin||||||
5688|Doyles Creek Subgroup|41010|6|Mentioned|Table 1|||||||||
5688|Doyles Creek Subgroup|42078|6|Mentioned|Table 1 P5|||||||||
5688|Doyles Creek Subgroup|42916|5|Briefly described|Table 1||Late Permian|||||||
5688|Doyles Creek Subgroup|43257|5|Briefly described|Map Legend||Late Permian|Of Wollombi Coal Measures||||||
5688|Doyles Creek Subgroup|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wollombi Newcastle Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
5689|Dr George Mountain Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Doctor George Granite.||||||
5689|Dr George Mountain Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.||Mumbulla Suite.|||Aluminous A-type granite.|
5750|Duckmaloi Granite|22857|6|Mentioned|p231|Carboniferous|Carboniferous|||||||
5750|Duckmaloi Granite|22863|6|Mentioned|p231|||||||||
5750|Duckmaloi Granite|23214|4|Described|p260|Carboniferous|Carboniferous|Intrudes the Mumbil Group. Mostly quartz monzodiorite.||||||
5750|Duckmaloi Granite|42712|4|Described|Table 1 p13; Fig3p9.|Carboniferous|Early Carboniferous|||||||
5750|Duckmaloi Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
5750|Duckmaloi Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
5750|Duckmaloi Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
5750|Duckmaloi Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
5752|Duddo Limestone|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 29, 42, 155-156|Miocene|Oligocene|Lawrence (1966). Western Murray Basin. Up to 130m thick. A major (water) aquifer. See also p158.||Murray Group.||Overlies Ettrick Marl conformably and diachronously. Is separated from the unconformably overlying Bookpurnong beds by the Mologa Surface. Grades laterally into Winnambool Formation.|Buff-coloured, bryozoal calcarenite, with interbedded layers of calcisiltite and calcilutite.|
5752|Duddo Limestone|10010|5|Briefly described|p12 Fig. 3||Early Miocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
5752|Duddo Limestone|22773|5|Briefly described|Fig24.8p352+24.9p353|||||||||
5752|Duddo Limestone|22799|2|Defined|p32|Middle Miocene|Late Oligocene|||||||
5752|Duddo Limestone|22857|5|Briefly described|p352 Fig.24.8, p353 Fig. 24.9|Early Miocene|Late Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
5752|Duddo Limestone|22887|5|Briefly described|Fig.6 p13||Early Miocene|||||||
5752|Duddo Limestone|22893|6|Mentioned|p27 fig9|Miocene|Miocene|||||||
5752|Duddo Limestone|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
5752|Duddo Limestone|23226|6|Mentioned|p889|||Of Murray Group.||||||
5752|Duddo Limestone|23417|6|Mentioned|p6|||||||||
5752|Duddo Limestone|23884|5|Briefly described|p155 Fig. 13.2|Early Miocene|Early Miocene|Geological Province: Murray Basin. Of the Murray Group.||||||
5752|Duddo Limestone|23909|6|Mentioned|p298|||||||||
5752|Duddo Limestone|24551|5|Briefly described|p322 Fig. 10.29, 520, p731 Table 17.1|||Of the Murray Group.  Geological Province: Murray Basin.  Max thickness: 130m.||||||
5752|Duddo Limestone|29591|6|Mentioned|Table 20|||||||||
5752|Duddo Limestone|29898|6|Mentioned|p216|||||||||
5752|Duddo Limestone|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
5752|Duddo Limestone|30754|6|Mentioned|p13|||Used in deeper parts of basin where Morgan & Mannum indistinguishable||||||
5752|Duddo Limestone|30934|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene & Miocene||||||
5752|Duddo Limestone|31625|6|Mentioned|Fig. 5.2|||Miocene||||||
5752|Duddo Limestone|31745|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
5752|Duddo Limestone|31746|3|Fully described|p195|||||||||
5752|Duddo Limestone|34360|6|Mentioned|p11|||||||||
5752|Duddo Limestone|34813|6|Mentioned|p62|||||||||
5752|Duddo Limestone|35285|5|Briefly described|p413|||||||||
5752|Duddo Limestone|37809|6|Mentioned|p7|||||||||
5752|Duddo Limestone|37873|6|Mentioned|p1|||||||||
5752|Duddo Limestone|39329|6|Mentioned|Fig.1|||||||||
5752|Duddo Limestone|39929|6|Mentioned|Fig.3|||||||||
5752|Duddo Limestone|40820|6|Mentioned|Fig.4|||||||||
5752|Duddo Limestone|41511|6|Mentioned|p20|||||||||
5752|Duddo Limestone|41537|6|Mentioned|Fig.2|||||||||
5752|Duddo Limestone|41868|5|Briefly described|p551|||||||||
5752|Duddo Limestone|42125|6|Mentioned|p136|||||||||
5752|Duddo Limestone|42134|6|Mentioned|Fig.3 P335|||||||||
5752|Duddo Limestone|42137|6|Mentioned|p369|||||||||
5752|Duddo Limestone|42827|3|Fully described|p269|||Of the Murray Group.||||||29-JUL-08
5752|Duddo Limestone|42881|4|Described|Fig.3, P84|||||||||
5752|Duddo Limestone|42966|2|Defined|Table 23, p139|Middle Miocene|Late Oligocene|Of the Murray Group.||||||29-JUL-08
5752|Duddo Limestone|43655|5|Briefly described|p40-846|||||||||
5752|Duddo Limestone|43791|6|Mentioned|p372, Fig1|||||||||
5752|Duddo Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
5752|Duddo Limestone|44191|5|Briefly described|Map Legend|Middle Miocene|Late Oligocene|||||||
5752|Duddo Limestone|46909|6|Mentioned|Fig.2|||||||||
5752|Duddo Limestone|49038|5|Briefly described|p26|||||||||
5752|Duddo Limestone|49040|6|Mentioned|p11|||||||||
5752|Duddo Limestone|50154|2|Defined|p129, p135-136|Early Miocene|Late Oligocene|Of the Murray Group. Max. thickness: 127m. Lies conformably over and interfingers with Ettrick Marl. Disconformably overlain by Parilla Sand or Bookpurnong beds. Nonconformably overlies the Glenelg River Metamorphic Complex in parts.||||||15-SEP-04
5752|Duddo Limestone|50155|5|Briefly described|Map Legend|Miocene|Oligocene|Calcarenite, bryozoal limestone||||||
5752|Duddo Limestone|50156|5|Briefly described|Map Legend|Miocene|Oligocene|Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50157|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlies Ettrick Marl and Dergholm Granite. Overlain by Parilla Sand and Whalers Bluff Formation. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||25-JUN-04
5752|Duddo Limestone|50158|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50159|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||
5752|Duddo Limestone|50160|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlain by Lowan Sand. Overlies Glenelg River Metamorphic Complex and Hypatia Formation. Marine deposit of bryozoal limestone and calcarenite||||||25-JUN-04
5752|Duddo Limestone|50161|5|Briefly described|Map Legend|Miocene|Oligocene|Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous. Of the Murray Group.||||||26-AUG-04
5752|Duddo Limestone|50162|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||22-JUN-04
5752|Duddo Limestone|50163|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Overlies Ferres Creek Tonalite, Glenelg River Metamorphic Complex, Dergholm Granite and Nangeela Formation. Overlain by Shepparton Formation, Parilla and Lowan Sands. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||25-JUN-04
5752|Duddo Limestone|50164|5|Briefly described|Map Legend|Miocene|Oligocene|Of Murray Group. Marine: calcarenite, bryozoal limestone; prodigiously fossiliferous||||||24-JUN-04
5752|Duddo Limestone|60421|5|Briefly described|p409, 413 Fig. 3, 414 Fig. 4|Middle Miocene|Late Oligocene|Underlies: Dorodong Sands. Overlies: Bacchus Marsh Formation.||||||
5752|Duddo Limestone|61314|5|Briefly described|p129|Miocene|Miocene|Of the Murray Group. Geological Province: western part of Murray Basin.||||||
5752|Duddo Limestone|63460|5|Briefly described|p838, p839 Fig. 2b|Middle Miocene|Late Oligocene|Of Lawrence and Abele (1976).Max.thickness:130m. Suggested here that this Victoria nomenclature be replaced by the South Australia mappable units of Mannum, Finniss, Glensforlan, Bryant Creek and Pata Fm, as they are recognisable in subsurface Victoria.  ||||||
5752|Duddo Limestone|64237|5|Briefly described|p17, p18, p19|Early Miocene|Early Miocene|Of Lawrence (1966). Retained as formal unit through the Lawrence (1975) and Lawrence and Abele(1988) name revisions where it overlay Netherby Marl. Appears to have been excluded from the Murray Supergp...........................reinstated in SA Murray Gp||||||15-JUL-08
5752|Duddo Limestone|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
5752|Duddo Limestone|66002|5|Briefly described|p10 Tb.7|Paleogene|Paleogene|Of Murray Group. Defined by Lawrence 1966.||||||
5752|Duddo Limestone|66286|5|Briefly described|pp178-179, pp188-189.|Miocene|Oligocene|Contains a variety of goethite-replaced marine fossils including bryozoans, echinoids and foraminifera. 1 - 2 m thick. Open marine shelf or shallow marine deposit.||Unit in Murray Group.|||Limestones of skeletal debris admixed with varying proportions of quartz sand, micrite, and calcareous clay. Well-indurated, fossiliferous, dusky-brown to yellow goethite-rich laminated duricrust with c.10% pisoliths and ooliths.|
5752|Duddo Limestone|66287|6|Mentioned|p30 Fig. 8, p31|Middle Miocene|Middle Miocene|Victorian equivalent of the Murray Group Limestones of South Australia.||||Underlies Bookpurnong Beds.||20-APR-12
5752|Duddo Limestone|67179|6|Mentioned|p579|||||||||
5752|Duddo Limestone|68116|5|Briefly described|Appendix, Maps 29, 38.|Langhian|Chattian||||||Calcarenite, bryozoal limestone.|
5752|Duddo Limestone|68189|6|Mentioned|p29|||||Of the Murray Group.||||
5752|Duddo Limestone|70961|14|Not recorded|p136|||Geological section.||||||
5752|Duddo Limestone|71593|4|Described|p52, p54|Miocene|Oligocene|Murray Basin.||Murray Group||Interfingered with the Ettrick Formation and the Winnambool Formation. Unconformably overlain by the Loxton Sand and Bookpurnong Formation.|Pale bioclastic limestone.|
5752|Duddo Limestone|72445|5|Briefly described|App.6 p2 Fig.1; App.7 p7 Fig.4.|Middle Miocene|Late Oligocene|Of Lawrence and Abele (1976). See also Duddo Limestone Member, App.7 p7 text.||Murray Group||Unconformably overlies Renmark Group and is laterally equivalent with Winnambool Formation.|Includes marl and marly limestone.|
5752|Duddo Limestone|73118|6|Mentioned|p17, 21, 24, 34|||Drill core summary logs.||||Overlies Ettrick Formation. Is overlain by Loxton-Parilla Sands, and Shepparton Formation.||
5752|Duddo Limestone|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
5755|Dudley Coal|23055|6|Mentioned|Fig4p11|||||||||
5755|Dudley Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Lambton Formation.   Geological Province: Sydney Basin||||||
5755|Dudley Coal|39292|6|Mentioned|p108|||See also Fig.6.6||||||
5755|Dudley Coal|39308|6|Mentioned|p467|||||||||
5755|Dudley Coal|39609|5|Briefly described|p3|||See also Table 1||||||
5755|Dudley Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Dudley coal seam instead. See also p113.||Of Lambton Subgroup||||
5755|Dudley Coal|73304|6|Mentioned|p75|||||Lambton Formation, Newcastle Coal Measures||||
5803|Duncans Creek Trondhjemite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
5803|Duncans Creek Trondhjemite|35257|6|Mentioned|Fig.17|||||||||
5803|Duncans Creek Trondhjemite|41347|6|Mentioned|p389|||||||||
5803|Duncans Creek Trondhjemite|41348|5|Briefly described|Map legend|Early Paleozoic||Of the Nundle Plutonic Suite.||||||07-NOV-08
5803|Duncans Creek Trondhjemite|42376|6|Mentioned|p35|Permian||||||||
5803|Duncans Creek Trondhjemite|50014|6|Mentioned|p251|||Geological Province: New England Fold Belt||||||
5803|Duncans Creek Trondhjemite|63748|6|Mentioned|p29|||In the Clarence River Supersuite.||||||07-FEB-11
5803|Duncans Creek Trondhjemite|63774|6|Mentioned|p1084|Permian|Permian|||||||
5803|Duncans Creek Trondhjemite|68005|6|Mentioned|p135.|Permian|Permian|||Unit in Nundle Suite.||||
5803|Duncans Creek Trondhjemite|68006|5|Briefly described|p135, p146.|||Hosts a Cu-Au-Mo occurrence. Mis-spelt as Duncan's Creek Trondjemite on p135.||Unit in Clarence River Supersuite.||||
5803|Duncans Creek Trondhjemite|68008|6|Mentioned|p333|||Geochemistry mentioned. Similar composition to Duncans Creek Trondhjemite.||||||
5803|Duncans Creek Trondhjemite|68111|5|Briefly described|p968 Tb.1|Olenekian|Induan||252 - 249 Ma, U-Pb SHRIMP (Cawood et al. 2011).|Of the Clarence River Supersuite.||||
5803|Duncans Creek Trondhjemite|68679|5|Briefly described|p465|||Bryant et al. (1997). Geochemistry briefly described; geochemical plots.||Clarence River Supersuite.|||A TTG Group granitoid.|
5803|Duncans Creek Trondhjemite|70125|5|Briefly described|p397 Fig.11|||Southern New England Batholith.|249.4 +/- 2.9 Ma.|||||
5803|Duncans Creek Trondhjemite|70217|5|Briefly described|p73 tbl 14.1|Olenekian|Changhsingian|New England Orogen. Another SHRIMP age of 249.4 +/- 2.9 Ma is also provided (also from Cawood et al, 2011).|252.1 +/- 3.2 Ma (SHRIMP, Cawood et al, 2011)|Clarence River Supersuite||||
5803|Duncans Creek Trondhjemite|70876|5|Briefly described|p78|Triassic|Permian|New England Orogen. Dates are derived from Cawood et al, 2011 and are SHRIMP U-Pb ages. A Rb-Sr age of c. 248-246 Ma is provided from Shaw and Flood (1993). [Either part of the Clarence River Supersuite or a correlative-not made clear in the text].|249.4 +/- 2.9 Ma to 252.1 +/- 3.2 Ma|||||
5803|Duncans Creek Trondhjemite|71628|4|Described|p9:2; p18: 1-7, 12, 18, 21-22|||Originally Duncan's Creek Trondhjemite. Named after a local watercourse. Forms a broadly ovoid, 8 x 3 km intrusion ~8 km NE of Nundle. Crops out as large tors with occasional whalebacks and rubbly angular blocks. Lithology, mineralogy and geochemistry detailed. Is associated with minor Cu (Mo) vein mineralisation.|250.9 +/- 2.2 Ma (SHRIMP: Cawood et al., 2011).|Duncans Creek Suite.||Intrudes Woolomin Association.|Grey, medium-grained, equigranular biotite-hornblende tonalite to trondhjemite with minor granodiorite; fine-grained marginal variants, minor leucomonzogranitic dykes. I-type.|
5806|Dunchurch Formation|22679|5|Briefly described|p 32|Devonian|Devonian|||||||
5806|Dunchurch Formation|22857|4|Described|p472 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Crudine Group. Feldspathic quartz arenite; minor slate, ashstone dacite. Max. thickness: 1500m. Geological Province: Hill End Trough and Capertee Rise.||||||
5806|Dunchurch Formation|23214|3|Fully described|p195|Lochkovian|Lochkovian|Of Crudine Group. First included in the Burraga Beds (now Burraga Group). Includes an unnamed metadacite unit. Age: 411 +/- 4Ma (SHRIMP U/Pb zircon). Max. thickness 1800m.||||||
5806|Dunchurch Formation|29903|5|Briefly described|p168|||||||||
5806|Dunchurch Formation|33285|5|Briefly described|p65|||||||||
5806|Dunchurch Formation|42712|4|Described|8; Table 1 p14|Early Devonian|Late Silurian|Within Crudine Group. Buckburraga Slate overlies, Campbells Fm and Vale Creek Volcanics underlie, conformably.||||||
5806|Dunchurch Formation|43639|5|Briefly described|Map Legend||Devonian|||||||
5806|Dunchurch Formation|43654|5|Briefly described|Map Legend|Devonian|Devonian|Of Crudine Group. Feldspathic quartz sandstone, minor slate, ashstone and dacite.||||||17-JUL-08
5806|Dunchurch Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Crudine Group.||||||17-JUN-08
5806|Dunchurch Formation|50233|4|Described|Map Legend|Lochkovian|Lochkovian|Of the Crudine Group. Feldspathic quartz sandstone, siltstone and ashstone, minor rhyolitic tuff. Overlies the Campbells Group. Overlain by Buckburraga Slate.||||||13-NOV-13
5806|Dunchurch Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Crudine Group. Dark grey, very thickly bedded, massive to normal graded, fine-grained to pebbly, crystal-rich, dacitic to andesitic volcaniclastic sandstone, interbedded grey siltstone and shale.||||||
5806|Dunchurch Formation|68592|2|Defined|p609,p611, p671, p1038, p1040-1, p1045-9|Pragian|Lochkovian|See also p259. First mapped as Burraga Group by Stanton (1956); informally divided into Dunchurch Formation and Buckburraga Slate by Dunnet (1961) and Gemuts (1961). Mapped as undifferentiated Burraga Group by Scheibner (1973). The name Dunchurch Formation was first published by Bowman (1974); formally defined during mapping of 2nd edition Bathurst 1:250 000 geological map (Stuart-Smith and Wallace, 1997; Wyborn and Henderson, 1997; Pogson and Watkins, 1998). Type section described. 400-1800m thick. SHRIMP U-Pb zircon age; the underlying Campbells Group is 423.7 +/- 2.5 Ma (Black, 2005). Geophysical properties described. Unfossiliferous.|411 +/- 4 Ma (Pogson and Watkins, 1998).|Unit in Crudine Group.||Gradationally overlies Binghams Back Formation (Campbells Group). Is overlain conformably by Buckburraga Slate. Is correlated with Turondale Formation.|Grey, coarse- to very coarse=grained, moderately to poorly sorted, arkosic sandstone, pebbly in places; 30-40m thick cycles with intervals of fine-grained, grey to khaki sandstone and siltstone; rare porphyritic andesitic lava.|
5806|Dunchurch Formation|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dcd. On Crookwell and Taralga 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Crudine Group||Overlies Binghams Back Formation (of Campbells Group). Is overlain by Buckburraga Slate.|Very thickly bedded, massive-graded, fine grained-pebbly, crystal rich, dacitic-andesitic, volcaniclastic sandstone; interbedded grey siltstone and mudstone; rare medium grained porphyritic andesite.|
5806|Dunchurch Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
5806|Dunchurch Formation|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Crudine Group|||Very thickly bedded, massive-graded, fine grained-pebbly, crystal rich, dacitic-andesitic, volcaniclastic sandstone; interbedded grey siltstone and mudstone; rare medium grained porphyritic andesite.|
5806|Dunchurch Formation|70544|5|Briefly described|Map Legend|Devonian|Devonian|||Crudine Group|||Very thickly bedded, massive to graded, fine grained-pebbly, crystal rich, dacitic-andesitic volcaniclastic sandstone; interbedded grey siltstone and mudstone; rare medium grained porphyritic andesite.|
5806|Dunchurch Formation|71656|6|Mentioned|p13 Fig.2|Lochkovian|Lochkovian|Only shown in correlation chart (Fig.2).||Base of Crudine Group||Overlies Binghams Back Formation, Campbells Group. Overlain by Buckburraga Slate.||
5829|Dundee Rhyodacite|22490|6|Mentioned|4|Late Permian|Late Permian|Geol. province: New England Fold Belt. Of the Wandsworth Volcanic Group.||||||31-MAY-07
5829|Dundee Rhyodacite|22678|6|Mentioned|p724||Tertiary|||||||
5829|Dundee Rhyodacite|22857|5|Briefly described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Volcanic Group, part included in the Coombadhja Volcanic Complex within the same group. Ignimbritic rhyodacite; minor porphyritic dacite lava, bedded tuff and breccia. Max. thickness: 2km. Geological Province: New England Fold Belt.||||||
5829|Dundee Rhyodacite|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Of the Wandsworth Volcanic Group.  Geological Province: New England Fold Belt.||||||31-MAY-07
5829|Dundee Rhyodacite|23811|5|Briefly described|Map Legend|Permian|Early Permian|Of Wandsworth Volcanic Group. Comprises informally named geographically separated masses including "Dundee Adamellite Porphyrite" and "Blue Granite".||||||31-MAY-07
5829|Dundee Rhyodacite|23812|4|Described|p25, 30|Early Triassic|Early Triassic|Of the Wandsworth Group.  Age:246-249Ma (Rb-Sr).  Maximum thickness: 2000m. Intruded by the Stanthorpe Monzogranite.||||||08-NOV-05
5829|Dundee Rhyodacite|23859|5|Briefly described|p930 Fig 2|Late Permian|Late Permian|Age: 248.7-245.8 Ma (Radiometric dating). Of Wandsworth Volcanic Group. Underlain by Emmaville Volcanics. Geological Province: New England Fold Belt.||||||31-MAY-07
5829|Dundee Rhyodacite|24424|5|Briefly described|p538|Early Triassic|Early Triassic|Age: ~247 Ma. Palaeomagnetic poles given.||||||
5829|Dundee Rhyodacite|32513|6|Mentioned|p318|||||||||
5829|Dundee Rhyodacite|33476|6|Mentioned|p54|||As a footnote||||||
5829|Dundee Rhyodacite|35173|6|Mentioned|Fig.3|||||||||
5829|Dundee Rhyodacite|35803|6|Mentioned|p321|||||||||
5829|Dundee Rhyodacite|36290|6|Mentioned|p164|||||||||
5829|Dundee Rhyodacite|38823|5|Briefly described|p207|||||||||
5829|Dundee Rhyodacite|38824|4|Described|p215|||||||||
5829|Dundee Rhyodacite|38825|4|Described|p221|||||||||
5829|Dundee Rhyodacite|38842|6|Mentioned|p291|||||||||
5829|Dundee Rhyodacite|38915|4|Described|p337|||||||||
5829|Dundee Rhyodacite|39238|6|Mentioned|p123|||||||||
5829|Dundee Rhyodacite|39279|6|Mentioned|p370|||||||||
5829|Dundee Rhyodacite|39445|6|Mentioned|p148|||||||||
5829|Dundee Rhyodacite|40507|6|Mentioned|p75|||||||||
5829|Dundee Rhyodacite|40509|6|Mentioned|p47|||||||||
5829|Dundee Rhyodacite|40514|6|Mentioned|p7|||||||||
5829|Dundee Rhyodacite|40773|6|Mentioned|p458|||||||||
5829|Dundee Rhyodacite|41041|3|Fully described|p266|||||||||
5829|Dundee Rhyodacite|41413|6|Mentioned|Fig.1|||||||||
5829|Dundee Rhyodacite|41998|5|Briefly described|p481|||||||||
5829|Dundee Rhyodacite|42284|6|Mentioned|p108|||||||||
5829|Dundee Rhyodacite|42378|3|Fully described|p25|||Supersedes "Dundee Ignimbrite" and "Dundee Porphyritic Adamellite"||||||
5829|Dundee Rhyodacite|42559|4|Described|p11|||Variation on Dundee Rhyodacite, NSW.||||||
5829|Dundee Rhyodacite|43008|5|Briefly described|map legend|||||||||
5829|Dundee Rhyodacite|43017|5|Briefly described|Fig.1,p372|||||||||
5829|Dundee Rhyodacite|43161|4|Described|32|||||||||
5829|Dundee Rhyodacite|43705|6|Mentioned|p19||Triassic|||||||
5829|Dundee Rhyodacite|43755|6|Mentioned|Fig.9,p556|||||||||
5829|Dundee Rhyodacite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group, Coombadjha Volcanic Complex. Formerly Dundee "Adamellite Porphyrite", an "Blue Granite".||||||20-JUL-04
5829|Dundee Rhyodacite|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|Of the Wandsworth Volcanic Group.||||||
5829|Dundee Rhyodacite|61793|5|Briefly described|p341, p344|||Geological Province: New England Fold Belt.||||||07-FEB-11
5829|Dundee Rhyodacite|62534|4|Described|p8, p11 (legend)|Early Triassic|Late Permian|Of the Wandsworth Volcanic Group. Enveloped by Tent Hill Volcanics. Strongly porphyritic rhyodacitic ignimbrite. Magnetics/radiometrics discussed.||||||07-FEB-11
5829|Dundee Rhyodacite|63732|5|Briefly described|Map legend|Late Permian|Late Permian|Dacitic to rhyolitic ignimbrites -subdivided into Timbarra Mass, Tenterfield Mass, Sunnyside Mass and Tarban Mass.||||||13-DEC-07
5829|Dundee Rhyodacite|63748|4|Described|p20|Late Permian|Late Permian|Formerly Dundee Adamellite-Porphyrite (Shaw 1969). Of Wandsworth Group. Unconformable on Wallangarra Volcanics. Age: 257.6+/-0.5Ma (U-Pb zircon).  Distinct, widespread, highly fragmented rhyolitic ignimbrite with a distinctive microgranitic groundmass.||||||07-FEB-11
5829|Dundee Rhyodacite|65668|6|Mentioned|p32,p34|Permian|Permian|Stanthorpe area; New England Orogen. Overlies the Wallangarra Volcanics.||||||
5829|Dundee Rhyodacite|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Triassic|Permian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996)|242-252 Ma magnetic age range|||||24-APR-12
5829|Dundee Rhyodacite|68111|5|Briefly described|p968 Tb.1, p970 Fig.2|Wuchiapingian|Capitanian|LA-ICP-MS U-Pb dating (Belousova et al. 2006). Also 254.34 +/- 0.34 Ma (TIMS U-Pb; Brownlow and Cross, 2010).|257.6 +/- 2.5 Ma|Of the Wandsworth Volcanic Group.||Overlies Emmaville Volcanics.||
5829|Dundee Rhyodacite|68679|4|Described|p453-456, p458|Permian|Permian|Previously the Dundee Adamellite-Porphyrite (Shaw, 1969). Very restricted extent in QLD but a distinctive (a useful regional marker) and widespread unit in NSW, where it forms several separate ignimbrite masses throughout the Tenterfield-Dundee-Coombadjha area. Another age, U-Pb (LA-ICP-MS) of 257.6 +/- 0.5 Ma by Belousova et al. (2006) contradicts stratigraphic relationships.|254.34 +/- 0.34 Ma (Brownlow and Cross, 2010).|Wandsworth Volcanic Group.||Unconformably overlies the Wallangarra Volcanics.|Very crystal-rich and contains abundant fragments of plagioclase, deformed biotite, hornblende, pyroxene and quartz phenocrysts in a groundmass of abundant, strongly welded glass shards.|
5829|Dundee Rhyodacite|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||26-SEP-18
5829|Dundee Rhyodacite|69188|5|Briefly described|p64|Permian|Permian|Age is interpreted as a magmatic crystallisation age.|254.1 +/- 2.2 Ma (Brownlow and Cross, 2010).|||Overlies Emmaville Volcanics (Wandsworth Volcanic Group).||16-APR-20
5829|Dundee Rhyodacite|69323|5|Briefly described|p1, p70|Lopingian|Lopingian|Geological province: New England Orogen.|254.1+\-2.2 Ma (Brownlow and Cross, 2010)|Unit of Wandsworth Volcanic Group.||||03-DEC-19
5829|Dundee Rhyodacite|69639|4|Described|p2, p21, p57, p62, p68, p87, p219, p222|Lopingian|Lopingian|New England Orogen. Contact with the Billyrimba Leucomonzogranite is obscured by poor outcrop.|254.1 +/- 2.2 Ma (Brownlow and Cross, 2010)|Wandsworth Volcanic Group||Intruded by the Dandahra Creek Leucogranite and (inferred) the Cottesbrook Monzogranite.||
5829|Dundee Rhyodacite|70876|5|Briefly described|p82|Late Permian|Late Permian|Additional ages are provided as follows: 254.1 +/- 2.2 Ma (SHRIMP, Brownlow et al, 2010), 254.34 +/- 0.34 Ma (TIMS U-Pb zircon, Brownlow et al, 2010), 257.6 +/- 2.5 Ma (LAICPMS, Belousova et al, 2006), c. 249-246 Ma (Rb-Sr biotite, Shaw and Flood, 1993), c. 242 Ma (K-Ar, Evernden and Richards, 1962).|250.9 +/- 1.9 Ma (Black, 2007)|Wandsworth Volcanic Group||Overlies the Emmaville Volcanics.||
5829|Dundee Rhyodacite|71628|5|Briefly described|p1:15; p8: 80, 87; p11: 8-11; p12: 5-6|||See also p13-3; p14: 7, 28; p15: 5, 9, 65, 106; p17: 4-5; p19: 18, 72, 111, 128, 130, 160. Now interpreted to include Postmans Creek Granodiorite (Blevin, pers. comm., 2013). Metamorphosed (by Mole Leucogranite) at 245 +/- 2 Ma (K-Ar biotite: Kleeman et al., 1997). RELATED UNITS (continued): Is also intruded by Black Snake Creek Granite; Sandy Flat and Bolivia Range Leucomonzogranites; Dandahra Creek and Tenterfield Creek Leucosyenogranites; Grasstree Quartz Monzodiorite. Is faulted against Surface Hill Leucomonzogranite. Is bounded by Moonta Gully Monzogranite.||Wandsworth Volcanic Group.||Conformably overlies Welcome Volcanic Member. Is intruded by Cottesbrook, Bungulla, Blacksmiths Creek, Mount Lindesay Monzogranites; Kingsgate Syenogranite; see COMMENTS for more.||
5829|Dundee Rhyodacite|71701|5|Briefly described|p170|Lopingian|Lopingian|Age is a SHRIMP date.|254.3 +/- 0.3 Ma (Brownlow and Cross, 2010)|||||
5829|Dundee Rhyodacite|72528|5|Briefly described|p2, p78, p109.|Lopingian|Lopingian||254.34+/-0.34 Ma ID-TIMS U-Pb|||Intruded by Black Snake Creek Granite.||
5838|Dunedin Park Sand Member|30996|2|Defined|p50|Holocene|Holocene|Time eq. Coonambidgal Fm. See also P48.||||||
5838|Dunedin Park Sand Member|42966|6|Mentioned|p239|||of Lake Victoria Sand||||||
5840|Dunedoo Formation|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Pebbly quartz-lithic sandstone to conglomerate, breccia, white claystone, thin coal seams. Max. thickness: 150m. Geological Province: Gunnedah Basin.||||||
5840|Dunedoo Formation|23043|5|Briefly described|Map Legend|Late Permian|Late Permian|of Gunnedah Basin.||||||
5840|Dunedoo Formation|23170|2|Defined|p300 Fig.61 p283|Late Permian|Permian|of Sydney Basin||||||
5840|Dunedoo Formation|31326|6|Mentioned|p34|||Stratigraphic nomenclature||||||
5840|Dunedoo Formation|31381|6|Mentioned|p53|||||||||
5840|Dunedoo Formation|35095|4|Described|p108|||||||||
5840|Dunedoo Formation|37794|6|Mentioned|Table 1|||||||||
5840|Dunedoo Formation|39664|6|Mentioned|p203|||||||||
5840|Dunedoo Formation|42641|6|Mentioned|p124|||||||||
5840|Dunedoo Formation|43494|4|Described|p9, p11-12|Permian|Permian|Consists of basal conglomerate overlain by whitish, coarse and fine-grained feldspathic sandstone and siltstone, shale, minor black carbonaceous shale, thin coal seams. Unconformably overlie Gollan Beds. Westerly equivalent of Illawarra C.M. Thickness 60m||||||01-OCT-09
5840|Dunedoo Formation|50590|5|Briefly described|Map Legend|Permian|Permian|Pebbly quartz-lithic sandstone to conglomerate, white claystone.||||||19-JUL-04
5840|Dunedoo Formation|60266|5|Briefly described|p2, p3 Tb.1|Late Permian|Late Permian|Terrestrial sedimentary sequence of quartzose sandstone, conglomerate, tuffaceous claystone and coal.  Unconformably overlies Rylstone Volcanics; underlies the Digby Formation.  Geological Province: Gunnedah Basin.||||||08-DEC-04
5840|Dunedoo Formation|68003|6|Mentioned|p44 Photo.3-h.|||Renamed Trinkey Formation.||||||
5845|Dungeree Volcanics|22529|4|Described|6|Silurian|Silurian|||||||
5845|Dungeree Volcanics|22545|6|Mentioned|p502||Late Silurian|||||||
5845|Dungeree Volcanics|22590|6|Mentioned|Fig3 P754|Pridoli|Ludlow|||||||
5845|Dungeree Volcanics|22857|4|Described|p476 App.1 Tb.A1.6|Pridolian|Wenlockian|Of the Tanabutta Group. Age: 419.2+/-4.8Ma, 416+/-5Ma, 415+/-7Ma (U/Pb SHRIMP). Max. thickness: 1000m. Geological Province: Capertee Rise.||||||
5845|Dungeree Volcanics|23043|5|Briefly described|Map Legend|Pridoli|Ludlow|of Tannabutta Group.||||||
5845|Dungeree Volcanics|23170|2|Defined|p62|Pridoli|Wenlock|Tannabutta Group.||||||
5845|Dungeree Volcanics|24126|6|Mentioned|p126|||||||||
5845|Dungeree Volcanics|24463|5|Briefly described|p321|Late Silurian|Late Silurian|Conformably overlies Coomber Formation.   Geological Province: Lachlan Fold Belt.||||||
5845|Dungeree Volcanics|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
5845|Dungeree Volcanics|30329|6|Mentioned|p30|||On table P30||||||
5845|Dungeree Volcanics|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
5845|Dungeree Volcanics|32485|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
5845|Dungeree Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
5845|Dungeree Volcanics|37727|4|Described|p57|||||||||
5845|Dungeree Volcanics|39331|6|Mentioned|Fig.0-3|||||||||
5845|Dungeree Volcanics|39663|6|Mentioned|Table 1|||||||||
5845|Dungeree Volcanics|40328|5|Briefly described|p137|||||||||
5845|Dungeree Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
5845|Dungeree Volcanics|43188|5|Briefly described|p202,Table 2 p201|||Capertee High. See also Fig.2 p197.||||||
5845|Dungeree Volcanics|43476|14|Not recorded|Map Legend||Ordovician|(Provisional Edition)||||||
5845|Dungeree Volcanics|43494|4|Described|p8, p15|Silurian|Silurian|Consist of greenish-grey almost aphanitic rhyolite and white altered rhyolite.; brecciation is common.||||||09-MAR-06
5845|Dungeree Volcanics|44093|5|Briefly described|p211 App. 1, 212 App. 1|Ludlovian|Wenlockian|Geological Province: Lachlan Fold Belt.||||||
5845|Dungeree Volcanics|50124|6|Mentioned|p126, p130|Late Silurian|Late Silurian|Geological Province: eastern Lachlan Fold Belt.||||||
5845|Dungeree Volcanics|66197|5|Briefly described|p632, p633 Fig.4a|Early Devonian|Late Silurian|Capertee High-Hill End Trough. Shallow marine clastics, limestone and silicic volcanics. Underlies the Kandos Group. Ages: 419 +/- 9 Ma, 415 +/- 9 Ma.||||||13-MAR-12
5845|Dungeree Volcanics|66713|6|Mentioned|p13|||Hosts the Tallawang magnetite skarn. Western contact with the Tallawang Granite.||||||
5845|Dungeree Volcanics|67847|5|Briefly described|p59|Silurian|Silurian|Intrusion of the Tallawang Granite resulted in the formation of the Tallawang magnetic skarn. Misspelt as the Dungaree Volcanics also on p59. ||||Intruded by the Tallawang Granite.||
5845|Dungeree Volcanics|68003|5|Briefly described|p24 Fig.3-e, p28 Photo.3-b, p146.|Pridoli|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Tannabutta Group.|||Rhyolite to dacite lava (autoclastic and volcaniclastic), rare latitic to trachytic lava.|
5846|Dunkeld Granite|23214|3|Fully described|p248|Carboniferous|Carboniferous|Of Bathurst Batholith.  Formerly Rankin Granite.  Intrudes the Crudine Group and consists of I-type felsic granite.||||||
5846|Dunkeld Granite|42726|5|Briefly described|map legend|Carboniferous||14. Variation on informal Dunkeld adamellite.||||||
5846|Dunkeld Granite|43127|5|Briefly described|p4,Fig.2,Fig.3|||Middle Carboniferous||||||
5846|Dunkeld Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
5846|Dunkeld Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
5846|Dunkeld Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|of Bathurst Batholith.||||||
5846|Dunkeld Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
5873|Duri Andesite Member|32286|6|Mentioned|p50|||Refers Voisey & Williams (1964)||||||
5881|Duxford Member|32482|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Of Namoi Formation.||||||
5881|Duxford Member|43407|14|Not recorded|Map Legend||Early Carboniferous|(Provisional Edition)||||||
5881|Duxford Member|43417|4|Described|Map Legend||Early Carboniferous|Part of Martindale Mudstone||||||
5881|Duxford Member|45088|4|Described|p14|||||||||
5881|Duxford Member|68005|5|Briefly described|p148.|Carboniferous|Carboniferous|||Unit in Tangaratta Formation.|||Lithic sandstone, polymictic conglomerate, siltstone.|
5883|Dyamberin beds|22857|5|Briefly described|p516 App.1 Tb.A1.8|Permian||Lithic wacke, siltstone and mudstone; minor diamictite and felsic volcanics. Several kilomteres thick. Geological Province: Barnard Basin (Nambucca Basin).||||||
5883|Dyamberin beds|23720|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Lithic wacke, siltstone and mudstone, minor diamictite, and felsic volcanics.||||||15-DEC-04
5883|Dyamberin beds|23812|5|Briefly described|p14|Early Permian|Early Permian|||||||
5883|Dyamberin beds|42834|5|Briefly described|p239|||||||||
5883|Dyamberin beds|42866|5|Briefly described|Table 2, P12|||||||||
5883|Dyamberin beds|43017|5|Briefly described|Fig.2,p374|||||||||
5883|Dyamberin beds|44093|5|Briefly described|p243 App. 1|Early Permian|Late Carboniferous|Geological Province: New England Fold Belt.||||||
5883|Dyamberin beds|44450|4|Described|p18 Table 3|Late Carboniferous|Late Carboniferous|Geological Province: Dyamberin Block.||||||
5883|Dyamberin beds|61805|6|Mentioned|p436|||Geological Province: New England Orogen.||||||17-NOV-08
5883|Dyamberin beds|66183|6|Mentioned|p360 Fig.2, p367-368|||New England Fold Belt. Written as Dyamberin Beds on Fig.2. Low metamorphic grade.||||||
5883|Dyamberin beds|71628|5|Briefly described|p2:41; p3: 5, 14, 71; p17:33; p19:74|||Dyamberin Block, E of Wongwibinda Fault.||||Intruded by Hillgrove Supersuite (Kookabookra Monzogranite; also faulted against it and Abroi Granodiorite), Round Mountain Leucomonzogranite, ?Gulf Station Leucosyenogranite and ?Mornington Complex.|Foliated and metamorphosed claystone, siltstone and lithic greywacke.|
5883|Dyamberin beds|72253|6|Mentioned|p98-99|early Permian|early Permian|[Also written as Dymberin beds on p99]. New England domain.|||||Siliciclastic.|
5888|Dyrring Formation|32380|6|Mentioned|p781|||||||||
5888|Dyrring Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
5888|Dyrring Formation|32869|6|Mentioned|p170|||Refers Pogson (1973). Flagstaff Formation unit||||||
5888|Dyrring Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
5888|Dyrring Formation|37068|6|Mentioned|p60|||||||||
5895|Eagleton Volcanics|24121|5|Briefly described|p4, p151|||Of Gilmore Volcanic Group.||||||25-AUG-22
5895|Eagleton Volcanics|32869|6|Mentioned|p171|||Refers Rattigan (1967). Gilmore Volcanics.||||||
5895|Eagleton Volcanics|39666|6|Mentioned|p103|||||||||
5895|Eagleton Volcanics|44244|5|Briefly described|p87|||Of the Gilmore Volcanic Group.  Previously assigned to the "Volcanic Stage" of the "Kuttung Series" (Osborne, 1922), and then to the "Gilmore Volcanics" (Roberts, 1961).||||||18-AUG-04
5895|Eagleton Volcanics|44254|2|Defined|p75,77,79,80||Early Carboniferous|||||||
5895|Eagleton Volcanics|50132|6|Mentioned|p246 Fig. 4|Late Carboniferous|Late Carboniferous|New England Fold Belt, Raymond Terrace area||||||
5895|Eagleton Volcanics|73487|6|Mentioned|p565, p574 Fig.8, p583-585|||||||||
5903|East Maitland Coal Measures|34287|6|Mentioned|p135|||Permian||||||
5903|East Maitland Coal Measures|43491|14|Not recorded|pVII/52||Permian|See also Lexicon||||||
5907|Eastern Branch Member|40590|6|Mentioned|p335|||Equivalent of the Yassabah Limestone. Refers Leitch 1972||||||
5907|Eastern Branch Member|44450|5|Briefly described|p112 Fig 35|||Geological Province: New England Fold Belt.||||||
5907|Eastern Branch Member|47059|5|Briefly described|p152|||of Parrabel Beds||||||
5917|Eastern Limestone|41863|6|Mentioned|p11|||||||||
5944|Eckersley Formation|22578|5|Briefly described|Fig.10 p400, p402|||Of Illawarra Coal Measures.||||||12-MAR-09
5944|Eckersley Formation|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Sydney Subgroup. Possibly misspelt - Eskersley.||||||
5944|Eckersley Formation|23881|5|Briefly described|p69 Fig. 7.2|||Of the Illawarra Coal Measures.  Geological Province: Sydney Basin.||||||
5944|Eckersley Formation|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Overlies: Wongawilli Coal||||||29-NOV-04
5944|Eckersley Formation|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||
5944|Eckersley Formation|24471|4|Described|p31 Fig.3|Late Permian|Late Permian|Overlies Wongawilli Coal. Contains Woronora, Hargrave and Cape Horn Coal Members. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Boolaroo Formation, Pilot Coals and Reids Mistake Formation. Geological Province: Sydney Basin.||||||07-FEB-11
5944|Eckersley Formation|29900|6|Mentioned|p169|||||||||
5944|Eckersley Formation|29901|4|Described|Table 1|||||||||
5944|Eckersley Formation|30006|4|Described|p25|||||||||
5944|Eckersley Formation|31128|6|Mentioned|Table 1|||||||||
5944|Eckersley Formation|31887|5|Briefly described|p5|||||||||
5944|Eckersley Formation|32618|6|Mentioned|Table 1|||Perm. Strat. table||||||
5944|Eckersley Formation|32849|6|Mentioned|Table 1|||Permian||||||
5944|Eckersley Formation|33129|5|Briefly described|p5|||||||||
5944|Eckersley Formation|34060|6|Mentioned|p24|||Perm. Table.||||||
5944|Eckersley Formation|34569|6|Mentioned|p8|||Permian. See Fig.2. Sydney Sub Group||||||
5944|Eckersley Formation|36220|4|Described|p53|||See also Table 1 & P50.||||||
5944|Eckersley Formation|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
5944|Eckersley Formation|37089|6|Mentioned|p208|||||||||
5944|Eckersley Formation|37090|6|Mentioned|p221|||||||||
5944|Eckersley Formation|39309|6|Mentioned|p128|||||||||
5944|Eckersley Formation|39661|6|Mentioned|Fig.1|||||||||
5944|Eckersley Formation|40744|6|Mentioned|Table 1|||||||||
5944|Eckersley Formation|42787|5|Briefly described|p133|||||||||
5944|Eckersley Formation|42896|4|Described|p22|||Of Sydney Subgroup.||||||12-MAR-09
5944|Eckersley Formation|42925|5|Briefly described|Table 18||Late Permian|||||||
5944|Eckersley Formation|45090|6|Mentioned|p219|||Tatarian||||||
5944|Eckersley Formation|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
5944|Eckersley Formation|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
5944|Eckersley Formation|63832|5|Briefly described|p131 fig 2|Lopingian|Lopingian|Of Sydney Basin.||Unit in Illawarra Coal Measures.||||13-DEC-17
5944|Eckersley Formation|64631|6|Mentioned|p44 Fig.2.|Changhsingian|Wuchiapingian|SE Sydney Basin. Biostratigraphic age control at base.||Unit in Illawarra Coal Measures.||||
5944|Eckersley Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Wongawilli Coal. Is overlain by Bulli Coal.||
5944|Eckersley Formation|73304|6|Mentioned|p74, p76|||Sydney Basin, southern.||||||
5944|Eckersley Formation|73421|5|Briefly described|p3, p19|Changhsingian|Changhsingian|Sydney Basin, southern. Bullie Tuff in the upper part of the Eckersley Formation dated to 252.60+/-0.30 Ma (Metcalfe et al., 2015), same age also shown with the Bulli Coal.|252.60+/-0.30 Ma|Sydney Subgroup||Underlies Narabeen Group|Includes conglomerate with cross bedding, siltstone and claystone/shale.|
5944|Eckersley Formation|73625|6|Mentioned|p2|Permian|Permian|Southern coalfield, Sydney Basin.||Illawarra Coal Measures.||Overlies Bargo Claystone. Is overlain by Narrabeen Group.||
5949|Edderton Coal Member|29942|3|Fully described|Fig.1|||||||||
5949|Edderton Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
5949|Edderton Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Foybrook Formation.||||
5970|Edgeworth Tuff Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Of the Adamstown Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||14-MAR-07
5970|Edgeworth Tuff Member|37083|6|Mentioned|p164|||||||||
5970|Edgeworth Tuff Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Glebe Formation?||||16-APR-14
6004|Egebek pegmatite|39652|6|Mentioned|p38|||||||||
6020|Ekersley Formation|29944|6|Mentioned|Fig.18|||||||||
6045|Elderslie Formation|22601|6|Mentioned|411|Permian|Permian|Geol province Sydney Basin. Lower Branxton Formation||||||
6045|Elderslie Formation|22969|5|Briefly described|p 21|||Branxton Formation||||||
6045|Elderslie Formation|23540|6|Mentioned|p 426|||||||||
6045|Elderslie Formation|30442|6|Mentioned|p24|||||||||
6045|Elderslie Formation|31081|6|Mentioned|Fig. 2|||Listed in Table.||||||
6045|Elderslie Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis brevis||||||
6045|Elderslie Formation|33711|6|Mentioned|Table 2|||||||||
6045|Elderslie Formation|34345|6|Mentioned|p329|||||||||
6045|Elderslie Formation|34533|6|Mentioned|p1285|||||||||
6045|Elderslie Formation|35160|6|Mentioned|p1|||||||||
6045|Elderslie Formation|35284|6|Mentioned|Fig.1|||||||||
6045|Elderslie Formation|38586|6|Mentioned|p38|||||||||
6045|Elderslie Formation|39267|6|Mentioned|p237|||See also P245||||||
6045|Elderslie Formation|39423|6|Mentioned|p66|||||||||
6045|Elderslie Formation|41071|6|Mentioned|p19|||||||||
6045|Elderslie Formation|42994|6|Mentioned|p264|||||||||
6045|Elderslie Formation|43017|5|Briefly described|Fig.1,p372|||||||||
6045|Elderslie Formation|43385|14|Not recorded|p179||Permian|||||||
6045|Elderslie Formation|43448|4|Described|p223,224,229||Permian|Unit of Branxton Subgroup (of Maitland Group)||||||
6045|Elderslie Formation|43477|14|Not recorded|p15,18,42||Permian|||||||
6045|Elderslie Formation|43479|14|Not recorded|p190,218||Artinskian|||||||
6045|Elderslie Formation|43882|14|Not recorded|p88-90|||||||||
6045|Elderslie Formation|45006|14|Not recorded|Tb.1,opp.p3,6,45|||||||||
6045|Elderslie Formation|49644|5|Briefly described|Table|||||||||
6045|Elderslie Formation|65380|5|Briefly described|p671|Kungurian|Artinskian|Includes ammonite with age constrained by SHRIMP date (272+/-3 Ma, but recalculated with modern standard to ~275 Ma), on zircons in tuffaceous siltstone ~80 m below the fossil horizon||Of Branxton Subgroup, Sydney Basin.||||27-MAR-12
6050|Eleebana Formation|29922|6|Mentioned|Appendix 4|||||||||
6050|Eleebana Formation|29926|6|Mentioned|Fig.3|||Permian||||||
6050|Eleebana Formation|29942|4|Described|Fig.2|||Permian||||||
6050|Eleebana Formation|31549|6|Mentioned|p159|||Stratigraphy||||||
6050|Eleebana Formation|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
6050|Eleebana Formation|33986|6|Mentioned|p30|||Table||||||
6050|Eleebana Formation|34270|6|Mentioned|p254|||||||||
6050|Eleebana Formation|34351|6|Mentioned|p348|||Fig.5.13||||||
6050|Eleebana Formation|37083|6|Mentioned|p164|||||||||
6050|Eleebana Formation|37966|6|Mentioned|p4|||||||||
6050|Eleebana Formation|39292|6|Mentioned|Fig.6.2|||||||||
6050|Eleebana Formation|39308|6|Mentioned|p459|||||||||
6050|Eleebana Formation|39609|6|Mentioned|Table 1|||||||||
6050|Eleebana Formation|39666|6|Mentioned|Table 20|||||||||
6050|Eleebana Formation|41463|6|Mentioned|Fig.1|||||||||
6050|Eleebana Formation|41479|6|Mentioned|p93|||||||||
6050|Eleebana Formation|43344|14|Not recorded|p85||Permian|||||||
6050|Eleebana Formation|43447|14|Not recorded|diag.p26|||Moon Island Beach Sub-Group||||||
6050|Eleebana Formation|43448|14|Not recorded|p224||Permian|On table only.Unit of Moon Island Beach Subgroup (Newcastle Coal Measures)||||||
6050|Eleebana Formation|45090|6|Mentioned|p186|||Refers McKenzie (1962)||||||
6050|Eleebana Formation|60726|6|Mentioned|p37.|Late Permian|Late Permian|Sydney area. Contains the insect fossil Tychticoloides (Order Hemiptera).||||||
6050|Eleebana Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Moon Island Beach Subgroup|Included Bolton Point Conglomerate Member, Chain Valley Coal Member, Awaba Tuff Member.|||
6092|Ellerslie Granodiorite|24265|5|Briefly described|p1452|Early Devonian|Early Devonian|Age: 404 +/- 6Ma (K-Ar). Geological Province: Lachlan Fold Belt||||||
6092|Ellerslie Granodiorite|37529|5|Briefly described|p5|||||||||
6092|Ellerslie Granodiorite|40678|6|Mentioned|p3|||||||||
6092|Ellerslie Granodiorite|42313|3|Fully described|p126|Late Silurian||||||||
6092|Ellerslie Granodiorite|42314|5|Briefly described|Map|Late Silurian||||||||
6092|Ellerslie Granodiorite|42497|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
6102|Elliots Shale Member|36413|6|Mentioned|p62|||||||||
6102|Elliots Shale Member|40328|6|Mentioned|p182|||||||||
6102|Elliots Shale Member|71069|6|Mentioned|p105 , p125|||Informal name for the shale horizons of the Captains Flat Formation. ||||Interbeds with the Kohinoor Volcanics.|Shale.|
6137|Emmagool Tuff|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
6137|Emmagool Tuff|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
6137|Emmagool Tuff|40328|4|Described|p126|||||||||
6137|Emmagool Tuff|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
6143|Emmaville Volcanics|22490|5|Briefly described|4|Late Permian|Late Permian|Of the Wandsworth Volcanic Group. Geol. Province: New England Fold Belt.||||||04-JUN-07
6143|Emmaville Volcanics|22857|4|Described|p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Group. Dominantly rhyolite volcanics, including crystal, lithic and vitric tuffs, agglomerate, breccia; intercalated lava flows. Thickness is several hundred metres. Geological Province: New England Fold Belt.||||||
6143|Emmaville Volcanics|23050|4|Described|p14 Table.1|Late Permian|Late Permian|Age: unconformably overlies Permian-Carboniferous sediments and is intruded by Early Triassic granites.||||||
6143|Emmaville Volcanics|23051|5|Briefly described|Map Legend|Late Permian|Early Permian|of Wandsworth Volcanic Group.||||||
6143|Emmaville Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Wandsworth Volcanic Group.  Includes the Nioka Porphyritic Dacite Member.  Undifferentiated felsic volcanic rocks: ignimbrite rhyolite and rhyodacite; rhyodacitic lava, minor dacite, andesite; minor interbedded sedimentary rock.||||||20-DEC-04
6143|Emmaville Volcanics|23812|5|Briefly described|p25, p27 Tb.3|Late Permian|Early Permian|Of Wandsworth Volcanic Group.||||||
6143|Emmaville Volcanics|23859|5|Briefly described|p930|Late Permian|Permian|Of Wandsworth Volcanic Group. Overlain by Dundee Rhyodacite;  underlain by Dummy Creek Conglomerate. Geological Province: New England Fold Belt. Max. thickness ~2500 m.||||||04-JUN-07
6143|Emmaville Volcanics|29988|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
6143|Emmaville Volcanics|30911|6|Mentioned|Map legend|Permian|Permian|||||||
6143|Emmaville Volcanics|31435|6|Mentioned|p23|||||||||
6143|Emmaville Volcanics|31694|6|Mentioned|p350|||||||||
6143|Emmaville Volcanics|32671|6|Mentioned|Map legend|Permian|Permian|||||||
6143|Emmaville Volcanics|32672|6|Mentioned|p675|||||||||
6143|Emmaville Volcanics|33476|6|Mentioned|p13|||||||||
6143|Emmaville Volcanics|35257|6|Mentioned|p49|||||||||
6143|Emmaville Volcanics|35803|6|Mentioned|p321|||||||||
6143|Emmaville Volcanics|36961|6|Mentioned|p216|||||||||
6143|Emmaville Volcanics|38824|5|Briefly described|p212|||||||||
6143|Emmaville Volcanics|38839|6|Mentioned|p245|||Geological Province: New England Fold Belt||||||
6143|Emmaville Volcanics|38915|6|Mentioned|p343|||Geological Province: New England Fold Belt||||||
6143|Emmaville Volcanics|39072|6|Mentioned|p1206|||||||||
6143|Emmaville Volcanics|39279|6|Mentioned|p370|||||||||
6143|Emmaville Volcanics|40245|6|Mentioned|Table 1|||||||||
6143|Emmaville Volcanics|40246|6|Mentioned|p173|||||||||
6143|Emmaville Volcanics|40507|6|Mentioned|p75|||||||||
6143|Emmaville Volcanics|40509|6|Mentioned|p47|||||||||
6143|Emmaville Volcanics|40514|6|Mentioned|Fig.3|||||||||
6143|Emmaville Volcanics|40530|6|Mentioned|Table 1|||||||||
6143|Emmaville Volcanics|40773|6|Mentioned|p458|||||||||
6143|Emmaville Volcanics|41390|6|Mentioned|p125|||||||||
6143|Emmaville Volcanics|41998|6|Mentioned|p481|||||||||
6143|Emmaville Volcanics|42180|5|Briefly described|p244|||||||||
6143|Emmaville Volcanics|42284|6|Mentioned|p108|||||||||
6143|Emmaville Volcanics|42300|6|Mentioned|p207|Late Permian||||||||
6143|Emmaville Volcanics|42378|4|Described|Table 1 P6|||Supersedes "Emmaville Volcanic Fmn" and "Vegetable Creek Volcanics"?  Redefined by Pogson 1972.||||||
6143|Emmaville Volcanics|42559|6|Mentioned|p10|||Correlated with Wallangarra Volcanics.||||||
6143|Emmaville Volcanics|42659|3|Fully described|p117|||||||||
6143|Emmaville Volcanics|42748|6|Mentioned|Fig.3 P9|Permian||||||||
6143|Emmaville Volcanics|43017|6|Mentioned|p377|||||||||
6143|Emmaville Volcanics|44450|5|Briefly described|p24|Permian|Permian|Of Wandsworth Volcanic Group.||||||
6143|Emmaville Volcanics|48940|6|Mentioned|p53|||||||||
6143|Emmaville Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group.||||||
6143|Emmaville Volcanics|61793|3|Fully described|p341-349, p343 Tb. 1, p342 Fig. 1(b)|Later Permian|Late Permian|Incl; Magistrate Vols, Four Mile Mdst, Dellwood Ignimbrite, Echo Volcaniclastics, Echo Ssts, Arranmor Ignimbrite, Rockdale Vols, Yarramundi Andesite. Inferred to underlie Dundee Rhyodacite Ignimbrite. Geol P: New England Fold Belt.||||||07-FEB-11
6143|Emmaville Volcanics|61804|5|Briefly described|p419, p420|||Wandsworth Volc. Gp. is locally termed Emmaville Vols. Geol Prov: NEFB. Rhyolitic and minor dacite pyroclastic rocks with subordinate amounts of volcanogenic sedimentary rocks. Volcaniclastics are slightly metamorphosed to biotite grade||||||30-OCT-08
6143|Emmaville Volcanics|62534|4|Described|p7, p11 (legend)|Early Triassic|Late Permian|Of Wandsworth Volcanic Group. Overlain by Tent Hill Volcanics. Intruded by Webbs Consols Leucogranite. Flat-lying rhyolitic to rhyodacitic ignimbritic flows and minor lavas and epiclastic rocks. Magnetics/radiometrics discussed.||||||07-FEB-11
6143|Emmaville Volcanics|63347|5|Briefly described|p5 Fig. 2|Late Permian|Late Permian|Of the Wandsworth Volcanic Group. Geological Province: New England Orogen.||||||
6143|Emmaville Volcanics|63748|6|Mentioned|p20, p69|||Correlated with Wallangarra Volcanics to the north (Godden 1982).||||||07-FEB-11
6143|Emmaville Volcanics|65668|6|Mentioned|p32|Permian|Permian|Considered to be closely related to Wallangarra Volcanics; both units placed in Wandsworth Volcanic Group by Barnes et al. (1991).||||||
6143|Emmaville Volcanics|67818|6|Mentioned|p131|||||||||
6143|Emmaville Volcanics|68005|5|Briefly described|p18, p34, p43-46, pp152-153.|Late Permian|Late Permian|New England Fold Belt. Highly magnetic; heterogeneous. High radiometric signature. Appendix 4 describes 11 un-named radiometric members.||Unit in Wandsworth Volcanic Group.|||Flat-lying rhyolitic, rhyodacitic and rare andesitic ignimbrite flows and minor lavas and epiclastic rocks; minor epiclastic sediments. Variants include ignimbrites (welded tuffs), lava flows, airfall tuffs and flow banded rhyolite.|
6143|Emmaville Volcanics|68006|5|Briefly described|p26, p128, p137, p138, p146, p155.|Late Permian|Late Permian|Kaolin clay deposits derived from weathered rhyodacite in this unit have been reported east of Inverell. May host buried epithermal Au-Ag systems.||Unit in Wandsworth Volcanic Group.||||
6143|Emmaville Volcanics|68111|5|Briefly described|p970 Fig.2, p973|Late Permian|Late Permian|Characteristic continental subduction-related geochemistry, associated with high-K calc-alkaline composition, enrichment in Al2O3 and LILE (Rb, K and LREE) and depletion in HFSE (Ti, Nb and Zr) (Stewart 2001).||Of the Wandsworth Volcanic Group||Is overlain by Dundee Rhyodacite.||
6143|Emmaville Volcanics|68679|6|Mentioned|p453|||||||Equated with the Wallangarra Volcanics.||
6143|Emmaville Volcanics|69188|5|Briefly described|p1-2, p5, p64-67, p72, p79|Early Triassic|Permian|New England region. Partially hosts the Glen Eden porphyry tin deposit.|252.3 +/- 2.0 Ma (magmatic age)|Wandsworth Volcanic Group.||Is overlain by Dundee Rhyodacite.|Includes relatively massive, uniformly grey crystal-lithic rock with minor veining and joints; well-developed grey feldspar phenocrysts to 3mm.|16-APR-20
6143|Emmaville Volcanics|69323|5|Briefly described|p1, p70|Lopingian|Lopingian|Geological province: New England Orogen.|252.3+\-2.0 Ma (Cross and Blevin, 2013)|Unit of Wandsworth Volcanic Group.||||03-DEC-19
6143|Emmaville Volcanics|70210|6|Mentioned|p2, p38|||New England district. [This unit contains the Arranmoor Ignimbrite Member, Dellwood Ignimbrite Member and Magistrate Volcanics, all of which are misspelt here as formations].||||||11-APR-18
6143|Emmaville Volcanics|70876|4|Described|p82|Late Permian|Late Permian||252.3 +/- 2.0 Ma (Cross and Blevin, 2013)|Wandsworth Volcanic Group|Includes the Magistrate Volcanic Member, Dellwood Ignimbrite Member and the Arranmor Ignimbrite Member.|Overlies the Wallangarra Volcanics. Overlain by the Dundee Rhyodacite.||
6143|Emmaville Volcanics|71628|5|Briefly described|p8: 16-17, 83, 85-87, 92-93; p10:3,9-10|||See also p14: 7, 12, 22; p15: 12, 22, 29; p19: 43, 110, 168. Hosts a lens with Zn, Pb (Ag, As) mineralisation close to Wellingrove Monzogranite. RELATED UNITS (continued): Is also intruded by Gilgai, Webbs Consols and Mole Leucogranites; Red Range, Glen Eden Microleucogranites; Deepwater Syenogranite. Bounds the Dry Creek Granodiorite, Mount Jonblee Leucomonzogranite and Kingsgate Syenogranite.||Wandsworth Volcanic Group.|Magistrate and Welcome Volcanic Members.|Is intruded by Wellingrove, Hell Hole, Wards Mistake Monzogranites; Pyes Creek Leucomonzogranite; Apple Tree Gully and ?Kings Plains Granodiorites; see COMMENTS for more.||
6143|Emmaville Volcanics|72528|5|Briefly described|p2, p71, p109.|Lopingian|Lopingian|Date from Arranmor Ignimbrite Member. Occuring 40km north of Glen Innes. Includes roof pendant in Deepwater Syenogranite.|256.4+/-1.6 Ma (Black, 2006)|Wandsworth Volcanic Group|Includes Arranmor Ignimbrite Member|||01-FEB-21
6156|Emu Creek Formation|22857|4|Described|p514 App.1 Tb.A1.8|Early Permian|Westphalian|Predominantly dark grey pink mudstone. Max. Thickness: est. 3500m. Geological Province: Yarrol Forearc Basin.||||||
6156|Emu Creek Formation|23812|6|Mentioned|p30|||||||||
6156|Emu Creek Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
6156|Emu Creek Formation|32086|6|Mentioned|p325|||Refers Olgers & Flood (in pres)||||||
6156|Emu Creek Formation|32491|5|Briefly described|p6|||U.Carboniferous||||||
6156|Emu Creek Formation|32492|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
6156|Emu Creek Formation|32494|6|Mentioned|p84|||U.Carb.||||||
6156|Emu Creek Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
6156|Emu Creek Formation|32672|6|Mentioned|p675|||||||||
6156|Emu Creek Formation|33476|6|Mentioned|p86|||||||||
6156|Emu Creek Formation|33766|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
6156|Emu Creek Formation|36528|6|Mentioned|p180|||||||||
6156|Emu Creek Formation|36936|3|Fully described|p208|||||||||
6156|Emu Creek Formation|36961|6|Mentioned|p212|||||||||
6156|Emu Creek Formation|37252|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous-Permian||||||
6156|Emu Creek Formation|40505|6|Mentioned|Fig.1|||||||||
6156|Emu Creek Formation|40514|6|Mentioned|Fig.7|||||||||
6156|Emu Creek Formation|40773|3|Fully described|p458|||||||||
6156|Emu Creek Formation|40960|6|Mentioned|p221|||||||||
6156|Emu Creek Formation|41413|6|Mentioned|p327|||||||||
6156|Emu Creek Formation|42378|6|Mentioned|Table 1 P11|||||||||
6156|Emu Creek Formation|42547|4|Described|p42|||||||||
6156|Emu Creek Formation|42963|5|Briefly described|Fig.2|||||||||
6156|Emu Creek Formation|43008|5|Briefly described|map legend|||||||||
6156|Emu Creek Formation|44093|5|Briefly described|p233 App. 1|Late Carboniferous|Late Carboniferous|Geological Province: New England Fold Belt.||||||
6156|Emu Creek Formation|45097|6|Mentioned|p24|||L. levis zone. Correlation chart||||||
6156|Emu Creek Formation|48940|3|Fully described|p36|||||||||
6156|Emu Creek Formation|69639|5|Briefly described|p170, p176|Late Carboniferous|Late Carboniferous|||||Intruded by the Koreelan Creek Granodiorite.||
6156|Emu Creek Formation|69793|4|Described|p1109, p1111, p1113-1121|Late Carboniferous|Late Carboniferous|Redefined here to include only the western part of the former Emu Creek Formation; the eastern part is renamed the Paddys Flat Formation. Type section in Oaky Creek. Originally part of the Pretty Gully Series (Andrews, 1908); later Emu Creek Series (Voisey, 1936), Emu Creek Formation (Olgers et al., 1974), Emu Creek Beds (McCarthy et al., 1974) and Emu Creek Formation again (Thomson, 1976). Shallow marine succession. Deformed by tight, asymmetric and steeply inclined folds. Maximum ICP-MS U-Pb depositional age from detrital zircons.|323.2 +/- 2.3 Ma (Hoy et al., 2014).||Includes Currawinya Conglomerate Member.|Corresponds chronologically with Lark Hill, Willuri and Currabubula Formations.|Predominantly siltstone thinly interlaminated with fine sandstone, and massive grey to black siltstones, as well as subordinate sandstone and conglomerate. Locally abundant marine macrofossils.|
6156|Emu Creek Formation|70728|5|Briefly described|p265-268,272|Bashkarian|Serpukhovian|Geological province: Emu Creek terrane, New England Orogen. Slightly deformed, immature, shallow-marine sedimentary rocks. Age constrained: Levipustula levis assemblage (Voisey, 1936; McCarthy et al., 1974; Roberts et al., 1995), indicating Bashkirian-Serpukhovian age. LA-ICP-MS detrital zircon age of c. 323 Ma (Hoy et al., 2014) as a maximum depositional age constraint. Broadly correlable to Currabubula Formation.|323-315 Ma (fossil: Levipustula levis)||Includes Currawinya Conglomerate Member.|Overlain unconformably by Paddy Flat Formation.||
6156|Emu Creek Formation|71628|6|Mentioned|p9: 5,32; p16: 26,29; p19: 24,52; p19-90|||||||Is intruded by Bruxner, Koreelah Creek and Cullens Creek Granodiorites, Rivertree Syenogranite and Jenny Lind Tonalite.||
6156|Emu Creek Formation|72528|5|Briefly described|p90.|Permian|Carboniferous|||||Intruded by Cullens Creek Granite.||
6162|Emu Flat Formation|36936|6|Mentioned|Fig.5|||||||||
6265|Esk Formation|13516|5|Briefly described|p159 fig 8, p163, 164|Middle Triassic|Middle Triassic|From Clarence-Moreton Basin.||Of Toogoolawah Group||||
6265|Esk Formation|22845|6|Mentioned|p82|Triassic|Permian|||||||
6265|Esk Formation|23440|4|Described|p140|||Of Toogoolawah Group.||||||18-AUG-08
6265|Esk Formation|23799|3|Fully described|p38, p12 Tb. 1, p37 Tb. 3|Middle Triassic|Early Triassic|Formerly "Esk Shales", "Esk Beds" and "Esk Formation".  Unconformably overlain by Tarong beds, Main Range Volcs, Oakdale Sst; unconformably overlies Maronghi Creek beds.  Intruded by phases of Tarameo Tonalite.  Max.thick: ~3000m.  Geol. Prov: Esk Trough.||||||
6265|Esk Formation|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||
6265|Esk Formation|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Of Toogoolawah Group.  Geological Province: Esk Trough. Maximum thickness: 3000m.||||||
6265|Esk Formation|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Polymictic pebble to boulder conglomerate, feldspathic sandstone, shale, minor acid tuff.||||||
6265|Esk Formation|30302|6|Mentioned|p414|||Lower to Middle Triassic||||||
6265|Esk Formation|30471|6|Mentioned|Fig.2|||See also P130. Correlation of drillhole sections||||||
6265|Esk Formation|30473|6|Mentioned|p377|||Refers Cranfield and Schwarzbock(1972). Part of Toogoolawah Group||||||
6265|Esk Formation|30475|6|Mentioned|p159|||||||||
6265|Esk Formation|30508|6|Mentioned|p88|||Triassic age. Esk Sewerage Scheme||||||
6265|Esk Formation|30565|6|Mentioned|p133|||||||||
6265|Esk Formation|31300|6|Mentioned|Pl. 9|||See also Pl. 10||||||
6265|Esk Formation|31450|6|Mentioned|p47|||||||||
6265|Esk Formation|31811|6|Mentioned|Fig. 1|||||||||
6265|Esk Formation|32022|6|Mentioned|p24|||||||||
6265|Esk Formation|32136|6|Mentioned|p6|||Miospores||||||
6265|Esk Formation|32838|6|Mentioned|p320|||||||||
6265|Esk Formation|35101|3|Fully described|p41|||||||||
6265|Esk Formation|35161|6|Mentioned|p591|||||||||
6265|Esk Formation|35427|6|Mentioned|p121|||||||||
6265|Esk Formation|35428|6|Mentioned|p124|||Miospore assemblages||||||
6265|Esk Formation|35647|6|Mentioned|p58|||||||||
6265|Esk Formation|35648|6|Mentioned|p13|||||||||
6265|Esk Formation|35901|6|Mentioned|p17|||||||||
6265|Esk Formation|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early Triassic||||||
6265|Esk Formation|36825|6|Mentioned|p12|||||||||
6265|Esk Formation|36899|6|Mentioned|p1085|||||||||
6265|Esk Formation|36954|6|Mentioned|p114|||||||||
6265|Esk Formation|37065|6|Mentioned|p36|||Formerly Esk Shales||||||
6265|Esk Formation|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
6265|Esk Formation|37376|6|Mentioned|p491|||||||||
6265|Esk Formation|37755|6|Mentioned|p79|||||||||
6265|Esk Formation|37812|6|Mentioned|p657|||||||||
6265|Esk Formation|38304|6|Mentioned|p83|||||||||
6265|Esk Formation|38306|6|Mentioned|p509|||||||||
6265|Esk Formation|38358|6|Mentioned|p14|||||||||
6265|Esk Formation|39079|5|Briefly described|p9|||||||||
6265|Esk Formation|39218|6|Mentioned|p47|||Flora||||||
6265|Esk Formation|39445|5|Briefly described|Table 9|||||||||
6265|Esk Formation|40051|6|Mentioned|p8|||||||||
6265|Esk Formation|40245|6|Mentioned|p182|||||||||
6265|Esk Formation|40475|5|Briefly described|p8|||||||||
6265|Esk Formation|40484|6|Mentioned|p63|||||||||
6265|Esk Formation|40623|5|Briefly described|p65|||||||||
6265|Esk Formation|40634|6|Mentioned|Fig.3|||||||||
6265|Esk Formation|41059|6|Mentioned|p168|||||||||
6265|Esk Formation|41738|6|Mentioned|p168|||||||||
6265|Esk Formation|41906|6|Mentioned|p14|||||||||
6265|Esk Formation|42336|6|Mentioned|p2|||||||||
6265|Esk Formation|42492|5|Briefly described|Table 2 P14|||||||||
6265|Esk Formation|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.||||||15-JUL-04
6265|Esk Formation|42893|6|Mentioned|p6|||of Toogoolawah Group||||||
6265|Esk Formation|43008|5|Briefly described|map legend|||||||||
6265|Esk Formation|43009|5|Briefly described|Map Legend|||||||||
6265|Esk Formation|43072|6|Mentioned|p80|||||||||
6265|Esk Formation|43150|6|Mentioned|Map Legend||Triassic|Name used only in context of equivalents.||||||12-APR-05
6265|Esk Formation|44115|14|Not recorded|p17|||||||||
6265|Esk Formation|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
6265|Esk Formation|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group. Geological Province: Esk Trough (Wandilla Province)||||||28-MAY-04
6265|Esk Formation|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Shale, sandstone, conglomerate, acid tuff.||||||
6265|Esk Formation|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Of the Toogoolawah Group. Polymictic pebble to boulder conglomerate, feldspathic sandstone, shale, minor acid tuff.||||||
6265|Esk Formation|60371|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group. Geological Province: Esk Trough. Polymictic pebble to cobble conglomerate, feldspathic sandstone, shale, minor acid tuff.||||||03-SEP-04
6265|Esk Formation|60726|6|Mentioned|p5.|Middle Triassic|Middle Triassic|Wivenhoe/Bellevue area. Contains some fossil insects.||||||
6265|Esk Formation|60993|6|Mentioned|p8 Tb. 2|||See also Esk beds.||||||
6265|Esk Formation|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Ipswich C.M. ||||||
6265|Esk Formation|61781|6|Mentioned|p267, p270|||Geological Province: Esk Trough.||||||
6265|Esk Formation|61782|5|Briefly described|p275, p277, p277 Fig. 3|||Geol Prov: Esk Trough.||||||
6265|Esk Formation|63821|6|Mentioned|p20|||||||||07-FEB-11
6265|Esk Formation|67402|5|Briefly described|p204, p205 tbl ESK/ABR1|Ladinian|Anisian|Esk Trough. Is only present in the western portion of this basin. Deposited in a fluvial environment. Time equivalent of the Neara Volcanics and Bryden Formation.  See also p206 fig ESK/ABR6, p208-p210.||Toogoolawah Group|||Sandstone, shale, conglomerate and tuff.|
6265|Esk Formation|68679|4|Described|p322, p324, p326,p389-391,p397,p427,p471|Middle Triassic|Middle Triassic|McDonnell (1956) and others (listed). Esk Basin, North D'Aguilar Subprovince, northern New England Orogen. Crops out along the entire W margin of the Basin. Has a basal conglomerate at the type section, west of Moore, where the Formation is ~3000m thick; it thins southward to 300m near Esk. Differing stratigraphic interpretations discussed. Rich in plant macrofossils and miospores.||Toogoolawah Group.||Is faulted against the Bjelke-Petersen and ?Maronghi Creek beds. Is intruded by Brisbane Valley Porphyrite.|Interbedded sandstone, shale, conglomerate, minor andesite and tuff.|
6265|Esk Formation|73306|5|Briefly described|p565-566, 573|Middle Triassic|Middle Triassic|Esk Trough.||Toogoolawah Group.||||
6324|Ettlewood Calc-Silicate Member|22500|4|Described|p 3, 10, 13|||Of the Broken Hill Group.||||||11-SEP-07
6324|Ettlewood Calc-Silicate Member|22553|5|Briefly described|fig2p77,p81|Proterozoic|Proterozoic|||||||
6324|Ettlewood Calc-Silicate Member|22575|6|Mentioned|p179 Fig.2|||Of the Broken Hill Group.||||||11-JUN-08
6324|Ettlewood Calc-Silicate Member|22720|6|Mentioned|p 168|||||||||
6324|Ettlewood Calc-Silicate Member|22771|6|Mentioned|Table12.2p45,45|||||||||
6324|Ettlewood Calc-Silicate Member|22884|6|Mentioned|p43 Fig. 3, p45|||Close affinity to the Meningie Well Formation.||||||26-MAR-09
6324|Ettlewood Calc-Silicate Member|22960|6|Mentioned|p90||Paleoproterozoic|||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|22965|6|Mentioned|Fig 1||Statherian|||||||
6324|Ettlewood Calc-Silicate Member|22967|6|Mentioned|p39||Statherian|||||||
6324|Ettlewood Calc-Silicate Member|38969|4|Described|p208|||||||||
6324|Ettlewood Calc-Silicate Member|39662|2|Defined|p424|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|39849|6|Mentioned|p86|||See also Table 2.||||||
6324|Ettlewood Calc-Silicate Member|40290|6|Mentioned|Fig.2|||||||||
6324|Ettlewood Calc-Silicate Member|40822|6|Mentioned|Fig.2|||||||||
6324|Ettlewood Calc-Silicate Member|41093|6|Mentioned|p252|||||||||
6324|Ettlewood Calc-Silicate Member|41630|6|Mentioned|Fig.1.3|||||||||
6324|Ettlewood Calc-Silicate Member|42181|4|Described|p251|||See also Fig.1.||||||11-SEP-07
6324|Ettlewood Calc-Silicate Member|42261|6|Mentioned|Fig 1 P530|||||||||
6324|Ettlewood Calc-Silicate Member|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42537|4|Described|p13|||||||||
6324|Ettlewood Calc-Silicate Member|42720|5|Briefly described|map legend|Paleoproterozoic||Variation on Ettlewood Calc-Silicate Member, NSW.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|42813|6|Mentioned|p9|||||||||
6324|Ettlewood Calc-Silicate Member|43086|6|Mentioned|Fig.3|||same as Ettlewood Calcsilicate Member||||||
6324|Ettlewood Calc-Silicate Member|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of the Allendale Metasediments.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of the Allendale Metasediments.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|43572|6|Mentioned|Fig.3.2 p6|||||||||
6324|Ettlewood Calc-Silicate Member|46598|4|Described|p304|||||||||
6324|Ettlewood Calc-Silicate Member|50045|4|Described|p116 Fig. 3, p115 Fig. 2|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Allendale Metasediments (Broken Hill Group, Willyama Supergroup).||||||11-SEP-07
6324|Ettlewood Calc-Silicate Member|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments (Broken Hill Group).  Geological Province: Broken Hill Block.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|60485|5|Briefly described|p26|||Of the Allendale Metasediments.  See also Ettlewood Calc-silicate Member.||||||03-MAR-05
6324|Ettlewood Calc-Silicate Member|61606|5|Briefly described|p4 Fig.2|||Of the Allendale Metasediments.||||||18-MAY-06
6324|Ettlewood Calc-Silicate Member|61735|5|Briefly described|p635 Fig. 1, p639, p658|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments (Broken Hill Group). Age: 1693+/-4Ma U/Pb SHRIMP deposition of tuffaceous sediment. Presented as Ettlewood CS only in Fig. 1.||||||04-JUN-15
6324|Ettlewood Calc-Silicate Member|61736|6|Mentioned|p665, p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments (Broken Hill Group). Age: 1693+/-4Ma. Geological province: Broken Hill Domain. Displays poly-metallic mineralization.||||||24-FEB-10
6324|Ettlewood Calc-Silicate Member|62535|5|Briefly described|p663, p665 Fig.2,|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, SE Curnamona Province. Regionally developed. Hosts polymetallic mineralization (Zn-Pb-Ag-Cu-Co-W). A metasiltstone immediately overlying this unit was dated at 1693 +/- 4 Ma, virtually identical with Bimba Formation. See also p666 Fig.3, p668, p671-674.||Allendale Metasediments.||Equivalent to the Bimba Formation.||
6324|Ettlewood Calc-Silicate Member|62536|5|Briefly described|p633, 636, 638-639, 641, 644-645, 658|||Broken Hill area. Contains significant concentrations of W and Zn as well as minor Pb and Zn.|1693 +/- 4 Ma.|Allendale Metasediments.||Is overlain by Parnell Formation.|Tuffaceous metasedimentary rocks: layered, diopside- and/or clinozoisite-rich, calc-silicate rocks. Locally, grey graphitic metasiltstone, which overlies and underlies the calc-silicate rock, is tuffaceous and zircon-datable.|
6324|Ettlewood Calc-Silicate Member|62993|6|Mentioned|p6, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Ettlewood Calcsilicate Member Equivalent discused p6.||Allendale Metasediments||Correlated with Bimba Formation||
6324|Ettlewood Calc-Silicate Member|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Within the Broken Hill Group. Pale, planar to irregularly layered epidote and clinopyroxene-rich calc-silicate in Broken Hill Domain; unnamed equivalents in Olary Domain.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|63519|5|Briefly described|p5, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Allendale Metasediments. Age: ~1695Ma. Occurs in lenses of layered cliozoisite-quartz rich rock, engulfed by pegmatitic granitoid. Mentioned in Abstract also.  See also p10 Fig. 3.||||||07-NOV-08
6324|Ettlewood Calc-Silicate Member|63866|4|Described|p36, p38, p40|||Broken Hill Domain, Curnamona Province. Appears as the Ettlewood calc-silicate member on p38. An adjacent tuffaceous metasiltstone was dated at 1693 +/- 4 Ma (Page et al., 2005a).||Allendale Metasediments||Equivalent to the Plumbago Formation.|Metamorphosed carbonate.|
6324|Ettlewood Calc-Silicate Member|64097|5|Briefly described|p302 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Allendale Metasediments (lower Broken Hill Group). Age: 1693+/-4Ma. Written as Ettlewood CS.||||||07-FEB-11
6324|Ettlewood Calc-Silicate Member|64741|4|Described|p301 Fig. 4, p309|Paleoproterozoic|Paleoproterozoic|Of Allendale Metasediments (Broken Hill Group). Geol.prov: Broken Hill Domain. Continues into the Olary Domain as the Bimba Formation. See p309 for detailed description for the "Bimba-Ettlewood" unit; correlations have also been made with Portia Fm.||||||07-FEB-11
6324|Ettlewood Calc-Silicate Member|64742|6|Mentioned|pp320-321, p323. ||||1693 Ma.|Unit in Broken Hill Group.||||
6324|Ettlewood Calc-Silicate Member|64944|5|Briefly described|p26, p28 Fig. 1, , p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Allendale Metasediments (Broken Hill Group). Equivalent to the marker unit, Bimba Formation, in the Olary Domain. Geological province: western Broken Hill Domain||||||07-FEB-11
6324|Ettlewood Calc-Silicate Member|66302|4|Described|p36 Fig.9, p37, p38-p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Also misspelt as the Ettlewood calc-silicate member on p39.  |1693 +/- 4 Ma (Page et al, 2005)|Allendale Metasediments||Equivalent to the Bimba Formation.|Metamorphosed carbonate with tuffaceous metasiltstone.|
6324|Ettlewood Calc-Silicate Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain. The rank [Member] is omitted.||Allendale Metasediments.||||
6324|Ettlewood Calc-Silicate Member|70000|6|Mentioned|p36|||Mis-spelt as Ettelwood Calc-silicate Member.||Unit in Allendale Metasediments.||||
6324|Ettlewood Calc-Silicate Member|70014|5|Briefly described|Map legend|||||Unit in Allendale Metasediments.|||Small pods and thin, elongate, tabular, conformable bodies. Thinly-bedded, fine to coarse quartz-plagioclase-clinopyroxene-amphibole-epidote rocks, pale brown or grey-green in colour, interpreted as metamorphosed impure dolomitic limestone.|
6324|Ettlewood Calc-Silicate Member|70657|4|Described|p10 Fig.4, p13 Fig.6, p14-17, p33,p37-41|Statherian|Statherian|See also p43-44, p65. Curnamona Province; Broken Hill Domain. Appears as Bimba Formation + Ettlewood Calcsilicate Member in Fig.4. Is presented also as Ettlewood Calc-silicate Member in Fig.6 and on p17 and p38. Highly anomalous in Pb, Zn, Ag, Co and locally Au. Similar to Bimba Formation.|1693 +/- 3 Ma.|Allendale Metasediments||Equivalent to Bimba Formation (Larry Macs Subgroup).||
6324|Ettlewood Calc-Silicate Member|70658|5|Briefly described|p6, 15-16, 47|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Allendale Metasediments.|||Sulphidic calc-silicate unit.|
6324|Ettlewood Calc-Silicate Member|73308|6|Mentioned|p607 Fig.1|||For reasons of space in the diagram, appears as Ettlewood CS.|1693 +/- 4 Ma.|Allendale Metasediments||||
6324|Ettlewood Calc-Silicate Member|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Broken Hill Domain. Correlated with Bimba Formation.|1693+/-4 Ma maximum depositional age|Allendale Metasediments||||
6324|Ettlewood Calc-Silicate Member|73482|5|Briefly described|p422 Fig.3, p432, p436 Fig.16|Statherian|Statherian|Abbreviated as Ettlewood CS p422 Fig.3.|1693+/-4 Ma|Allendale Metasediments||||
6324|Ettlewood Calc-Silicate Member|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|Statherian|Statherian||1693+/-4 Ma|Allendale Metasediments||||
6333|Ettrema Limestone Member|22605|5|Briefly described|p 12||Frasnian|||||||
6333|Ettrema Limestone Member|32129|6|Mentioned|p5|||||||||
6333|Ettrema Limestone Member|42848|5|Briefly described|p532|Late Devonian|Late Devonian|Of Bellbird Creek Formation. Contains a number of Late Famennian fossils. Max. thickness: 30m.||||||29-AUG-12
6333|Ettrema Limestone Member|70661|4|Described|viii, p107 fig 8, p113, p114, p116-p119|Frasnian|Frasnian|Named after Ettrena Creek. Previously known as Ettrema Limestone. Distribution, economic geology,  geomorphology, metamorphism, geochemistry, geophysical characteristics, structure and fossil assemblage discussed. Type section mentioned. Age derived from conodont identification. Deposited in a shallow marine environment. May be more than 275m thick. Host to the Ettrema mines (Zn-Cu-Pb).||Bellbird Creek Formation|||Grey fossiliferous limestone with intercalated shale and quartzite. Minor mudstone and fissile siltstone.|
6333|Ettrema Limestone Member|71303|5|Briefly described|map legend|Frasnian|Frasnian|||Of Bellbird Creek Formation|||Grey limestone and intercalated shale; conodonts and invertebrate macrofauna. Grey fine-grained quartzose sandstone and brown, micaceous siltstone.|
6337|Ettrick Formation|2967|6|Mentioned|p24|||Ludbrook (1957). Renamed Ettrick Marl (see references p14, p15 Fig.2.2, p24) and assigned to the Murray Group by Lawrence (1966).||||||
6337|Ettrick Formation|10010|5|Briefly described|p12 Fig. 3|Late Oligocene|Early Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
6337|Ettrick Formation|22587|6|Mentioned|p79 Fig.7|Late Oligocene|Early Oligocene|||||||
6337|Ettrick Formation|22626|6|Mentioned|446 fig 10|Early Miocene|Late Oligocene|Geol province Murray Basin. Overlying unit Lower Mannum Formation||||||
6337|Ettrick Formation|22773|5|Briefly described|p351,Fig24.8p352|Oligocene|Oligocene|||||||
6337|Ettrick Formation|22799|2|Defined|p30|Early Miocene|Oligocene|Murray Group.||||||13-AUG-07
6337|Ettrick Formation|22857|5|Briefly described|p351, p352 Fig.24.8|Early Miocene|Oligocene|Basal conglomerate of the Murray Group. Composed of sand and silt. Equivalent of Compton Conglomerate. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
6337|Ettrick Formation|22887|5|Briefly described|Fig.6 p13||Early Oligocene|||||||
6337|Ettrick Formation|22893|5|Briefly described|fig4 p9|||||||||
6337|Ettrick Formation|22938|5|Briefly described|fig5|Oligocene|Oligocene|Eastern Mount Lofty Ranges.||||||
6337|Ettrick Formation|23179|6|Mentioned|Fig.2|Early Miocene|Late Oligocene|Murray Supergroup||||||
6337|Ettrick Formation|23226|6|Mentioned|p889,890,891,894|||Of Murray Supergroup.||||||
6337|Ettrick Formation|23671|6|Mentioned|p3|||Disconformably overlies the Renmark Beds.||||||
6337|Ettrick Formation|23768|5|Briefly described|p28 Fig.5|Miocene|Oligocene|Geological Province: Murray Basin.||||||11-SEP-09
6337|Ettrick Formation|23818|5|Briefly described|p174 Fig.84, p180|Oligocene|Oligocene|Geological Province: Murray Basin. Overlying units: Buccleuch Group and Renmark Beds.[this seems unlikely CEBDec 2013] Contains foraminifer Massilina torquayensis.||||||03-DEC-13
6337|Ettrick Formation|23884|5|Briefly described|p153, p155 Fig.13.2|Early Oligocene|Early Oligocene|Geological Province: Murray Basin||||||
6337|Ettrick Formation|23921|5|Briefly described|p1109|Early Miocene|Early Miocene|Geological Province: Murray Basin.||||||
6337|Ettrick Formation|24563|5|Briefly described|p485|||Included in the Murray Supergroup by Lukasik and James (1998).  However, Murray Supergroup now abandoned and Murray Group reinstated - Ettrick Formation not included.  Geological Province: Murray Basin.||||||
6337|Ettrick Formation|29591|6|Mentioned|Table 20|||||||||
6337|Ettrick Formation|29697|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|29828|6|Mentioned|p25|||||||||
6337|Ettrick Formation|29898|6|Mentioned|p216|||||||||
6337|Ettrick Formation|30751|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6337|Ettrick Formation|30753|4|Described|Table 2|||Oligocene age||||||
6337|Ettrick Formation|30754|6|Mentioned|p14|||Stratigraphic table. See also P42 section||||||
6337|Ettrick Formation|30758|6|Mentioned|p66|||Oliogocene. Marine transgression||||||
6337|Ettrick Formation|30918|6|Mentioned|p85|||||||||
6337|Ettrick Formation|31241|6|Mentioned|p99|||Equivalent in age to Gambier Lst.||||||
6337|Ettrick Formation|31625|6|Mentioned|Fig. 5.2|||Oligocene||||||
6337|Ettrick Formation|31746|6|Mentioned|p194|||||||||
6337|Ettrick Formation|31848|5|Briefly described|p15|||Oligocene - Miocene||||||
6337|Ettrick Formation|31850|6|Mentioned|p36|||||||||
6337|Ettrick Formation|31851|4|Described|p12|||Lithostratigraphy.||||||
6337|Ettrick Formation|31922|6|Mentioned|p173|||||||||
6337|Ettrick Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area||||||
6337|Ettrick Formation|32432|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|32653|6|Mentioned|p285|||||||||
6337|Ettrick Formation|32859|4|Described|p69|||Oligocene||||||
6337|Ettrick Formation|32862|6|Mentioned|Fig. 3|||Section from boreholes||||||
6337|Ettrick Formation|32864|6|Mentioned|Fig. 5|||||||||
6337|Ettrick Formation|33224|6|Mentioned|Fig.35|||Photo.||||||
6337|Ettrick Formation|33490|4|Described|p10|||See also p27. Oligocene -Miocene.||||||28-JUL-08
6337|Ettrick Formation|33798|6|Mentioned|p98|||Fig.2||||||
6337|Ettrick Formation|33834|5|Briefly described|p11|||||||||
6337|Ettrick Formation|33982|6|Mentioned|p116|||||||||
6337|Ettrick Formation|34029|5|Briefly described|Table 1|||Oligo-Miocene||||||
6337|Ettrick Formation|34114|6|Mentioned|Fig.2|||||||||
6337|Ettrick Formation|34191|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
6337|Ettrick Formation|34295|5|Briefly described|p36|||Oligocene||||||
6337|Ettrick Formation|34296|4|Described|p97|||Olig.- Miocene. Lithology||||||
6337|Ettrick Formation|34308|5|Briefly described|p180|||Correlation chart. Olig.- L.Miocene||||||
6337|Ettrick Formation|34418|4|Described|p506|||Equivalent||||||
6337|Ettrick Formation|34461|5|Briefly described|p52|||Oligocene||||||
6337|Ettrick Formation|34758|6|Mentioned|Fig.2|||||||||
6337|Ettrick Formation|35071|6|Mentioned|Table 1|||||||||
6337|Ettrick Formation|35200|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6337|Ettrick Formation|35232|6|Mentioned|p11|||See also Table 3.||||||
6337|Ettrick Formation|35541|6|Mentioned|p13|||||||||
6337|Ettrick Formation|37132|5|Briefly described|p368|||||||||
6337|Ettrick Formation|38068|6|Mentioned|Fig.7|||||||||
6337|Ettrick Formation|38070|6|Mentioned|Fig.12|||Murray Basin||||||
6337|Ettrick Formation|38601|6|Mentioned|p7|||||||||
6337|Ettrick Formation|39329|6|Mentioned|Fig.1|||||||||
6337|Ettrick Formation|39929|6|Mentioned|p268|||||||||
6337|Ettrick Formation|40003|5|Briefly described|p38|||||||||
6337|Ettrick Formation|40033|6|Mentioned|p228|||||||||
6337|Ettrick Formation|41478|5|Briefly described|Table 1|||||||||
6337|Ettrick Formation|41511|5|Briefly described|p18|||||||||
6337|Ettrick Formation|41517|6|Mentioned|p139|||||||||
6337|Ettrick Formation|41520|5|Briefly described|Fig.11|||||||||
6337|Ettrick Formation|42125|5|Briefly described|p135|||See also Fig.5||||||
6337|Ettrick Formation|42126|6|Mentioned|p156|||||||||
6337|Ettrick Formation|42127|5|Briefly described|p219|||See also Fig.3||||||
6337|Ettrick Formation|42129|6|Mentioned|p254|||See also Fig.6||||||
6337|Ettrick Formation|42130|6|Mentioned|Fig.3 P265|||||||||
6337|Ettrick Formation|42132|6|Mentioned|Fig.5 P298|||||||||
6337|Ettrick Formation|42134|6|Mentioned|Fig.3 P335|||||||||
6337|Ettrick Formation|42137|4|Described|p370|||See also Table 1||||||
6337|Ettrick Formation|42138|6|Mentioned|p388|||||||||
6337|Ettrick Formation|42443|5|Briefly described|p6|||||||||
6337|Ettrick Formation|42623|6|Mentioned|p2|||aquitard||||||
6337|Ettrick Formation|42717|5|Briefly described|map legend|Miocene|Oligocene|||||||
6337|Ettrick Formation|42881|4|Described|Fig.3, P84|||||||||
6337|Ettrick Formation|42966|2|Defined|p116|Early Miocene|Oligocene|Of Murray Group.||||||13-AUG-07
6337|Ettrick Formation|43073|4|Described|Table 3|||||||||
6337|Ettrick Formation|43195|5|Briefly described|Map Legend||Oligocene|See also commentary on back of map.||||||
6337|Ettrick Formation|43383|14|Not recorded|p29||Oligocene|||||||
6337|Ettrick Formation|43466|14|Not recorded|p3,fig.2,Pl.1|||Equivalent to SA||||||
6337|Ettrick Formation|43467|14|Not recorded|p3,20,25,31,32|||||||||
6337|Ettrick Formation|43667|6|Mentioned|Fig.3,p12|Miocene|Oligocene|||||||
6337|Ettrick Formation|43686|6|Mentioned|Fig.5,p233|||||||||
6337|Ettrick Formation|43780|6|Mentioned|p5|||||||||
6337|Ettrick Formation|43791|6|Mentioned|p372, Fig1|||||||||
6337|Ettrick Formation|43804|6|Mentioned|Fig.2,p49|||||||||
6337|Ettrick Formation|44133|5|Briefly described|p158, 152 Fig. 10.2|Early Miocene|Early Oligocene|Geological Province: Murray Basin. ||||||
6337|Ettrick Formation|44191|5|Briefly described|Map Legend||Late Oligocene|||||||
6337|Ettrick Formation|46802|6|Mentioned|Table 1|||||||||
6337|Ettrick Formation|46839|6|Mentioned|p82|||||||||
6337|Ettrick Formation|49038|4|Described|Table 2|||Briefly described p26.||||||19-SEP-18
6337|Ettrick Formation|49040|6|Mentioned|p11|||||||||
6337|Ettrick Formation|60785|5|Briefly described|p184 Fig.1, p195. |Chattian|Chattian|South Australia. Has yielded several fossil cetacean heterodont teeth.|||||Glauconitic marl, calcareous clay, and mudstone, with silt and sand.|
6337|Ettrick Formation|61155|5|Briefly described|p18||Early Oligocene|Of the Murray group. Glauconitic marls; diachronous. Overlain by Gambier Limestone; interfingers with Duddo Limestone and Geera Clay in central Murray Basin. Age: 32-14.9Ma. Max. thickness: 50m. Geological Province: Murray Basin. See also p3. p4.||||||03-MAR-10
6337|Ettrick Formation|61314|5|Briefly described|p129|Oligocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
6337|Ettrick Formation|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999)  incorporates this unit,  the Geera Clay and Winnambool Formation into their new Murray Supergroup. These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
6337|Ettrick Formation|63460|5|Briefly described|p837, p839 Fig. 2b|Erly Miocene|Late Oligocene|Overlain by Mannum Fm. Passes laterally into Winnambool Formation and Geera Clay to the north and east. Max. thickness" 40m. Geological province: Murray Basin. Dark grey-greenish, glauconitic calcareous clay and marl. ||||||
6337|Ettrick Formation|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Marl.||||||
6337|Ettrick Formation|64237|4|Described|p17,p18,p18|Oligocene|Oligocene|Formerly part of the now obsolete Glenelg Group together with Compton Conglomerate; now incorporates Compton Conglomerate (obsolete) and is the basal unit of Murray Group ( in South Australia).||||||18-SEP-09
6337|Ettrick Formation|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Late Oligocene|Deposited during the final stages of an Oligocene-Miocene marine incursion. Contemporaneous with Geera Clay, Murray Group and Winnambool, Olney Formations. Locally underlies Murray Group. Overlies Buccleuch beds.||||||
6337|Ettrick Formation|67462|5|Briefly described|Map legend.|||Murray Basin.||||||
6337|Ettrick Formation|68140|6|Mentioned|p1701|Neogene|Paleogene|Middle Tertiary age.||||||
6337|Ettrick Formation|68715|6|Mentioned|p31 Fig.5|Chattian|Rupelian|Murray Basin.||Murray Group.||||07-APR-17
6337|Ettrick Formation|70718|5|Briefly described|p24|Middle Miocene|Late Oligocene|Murray Basin. Deposited as a marginal-marine muddy facies.||||||
6337|Ettrick Formation|70961|14|Not recorded|p136|||Geological section.||||||
6337|Ettrick Formation|71248|14|Not recorded|p2||Oligocene|||||||
6337|Ettrick Formation|71593|4|Described|p52-p54|Miocene|Oligocene|Murray Basin. Palynology in Stavely 14 linked ot Ettrick Fm.||Murray Group||Interfingered with the Geera Clay, Olney Formation and the Calivil Formation.|Muddy shallow marine marl.|19-SEP-18
6337|Ettrick Formation|72445|5|Briefly described|App.7 p2, p5, p7 Fig.4, p19-20; App.2.|Middle Miocene|Early Oligocene|See also App.1, App.6 p1 Tb.1, p2 Fig.1, p4. Mentioned in text as marls in the far west of the Murray Basin (see Truswell 1987, Macphail & Truswell 1989). Identified in Stavely 08,11,14,16. App.6 sample in Stavely 11 include a high diversity of marine bioclast types including abundant bryozoans. A Middle Miocene M5 zone (16.39-15.73 Ma) determined from foraminifera(p.4, but table 1 gives M6 zone 15.10-14.78 Ma). Early Oligocene spore/pollen zone identified in samples from Stavely 14 (App.7).|16.39 - 14.78 Ma min age.|Murray Group||Shown as underlying Gambier Limestone. Overlies Renmark Group (unconformity), Olney Formation (gradational or sharp contact), Compton Conglomerate. Laterally equivalent with Geera Clay.|Including glauconitic marl, sand and limestone. Includes lesser silt and mud.|
6337|Ettrick Formation|73107|5|Briefly described|Map legend.|||Murray Basin. Equivalent to an un-named Oligocene unit of silicified dolomitic calcilutite, boulders of which are washed up at Cape Hart, Point Reynolds, Cape Linois and Cape Gantheaume.||||||
6337|Ettrick Formation|73118|5|Briefly described|p17, 24, 30, 34, 45, 82|||Murray Basin. Drill core summary logs. <30m thick. Almost entirely concealed. Deposited in shallow-marine, restricted platform to lagoonal environments.||Murray Group.||Overlies Olney Formation. Is overlain by Duddo Limestone and Geera Clay.|Weakly lithified grey, green glauconitic, highly fossiliferous calcareous clay (marl), silt, sandy skeletal clay, thin micritic limestone intercalations. Contains abundant and diverse faunas.|
6337|Ettrick Formation|73188|6|Mentioned|p320|Oligocene|Oligocene|Murray Basin.||||||
6337|Ettrick Formation|73228|4|Described|p50, p52-57, p60|Middle Miocene|Late Paleocene|Murray Basin. From the lower Murray Group. Estuarine and marginal marine depositional environments. Represents a transgressive phase of shallow-marine shelf environment. Identified in Cooltong 1, Berri North 1, Nadda 1, and Loxton 1 drillholes.||Murray Group, lower||Underlain by Renmark Group including Olney Formation. Overlain by Gambier Limestone.|Grey to green glauconitic and fossiliferous marl, calcareous clay and mudstone, and silt and fine quartz sand, as well as skeletal debris.|
6337|Ettrick Formation|73229|5|Briefly described|p66-67, p70-72, p74|Early Miocene|Late Oligocene|Murray Basin. [Analysed using pXRF; see article]. From the lower Murray Group.||Murray Group, lower|||Includes clayey limestone with interbedded clay and calcareous, glauconitic shelly fragments; glauconitic, fossiliferous marl; calcareous clay and mudstone; silt; fine-grained sand.|
6348|Eucumbene Granite|40328|4|Described|p205|||||||||
6348|Eucumbene Granite|45087|5|Briefly described|p11|||Chemical analyses.||||||
6369|Eungai Mudstone|721|5|Briefly described|Map legend|Famennian|Famennian|Of the Parry Group.  Dark mudstone with with rare to minor thin tuffaceous beds.||||||
6369|Eungai Mudstone|22857|5|Briefly described|p498 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Parry Group. Dark mudstone with rare to minor tuffaceous beds. Max. thickness: >800m. Geological Province: Tamworth Forearc Basin.||||||
6369|Eungai Mudstone|23051|5|Briefly described|Map Legend|Late Devonian|Late Devonian|of Parry Group.||||||
6369|Eungai Mudstone|30133|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
6369|Eungai Mudstone|30135|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
6369|Eungai Mudstone|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
6369|Eungai Mudstone|31999|6|Mentioned|p152|||||||||
6369|Eungai Mudstone|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
6369|Eungai Mudstone|32865|6|Mentioned|p481|||Corr. with Baldwin Fm.||||||
6369|Eungai Mudstone|34555|4|Described|p240|||Correlated with Baldwin Formation||||||
6369|Eungai Mudstone|35761|5|Briefly described|p64|||Stratigraphy discussed. See also Table 1.||||||
6369|Eungai Mudstone|37987|6|Mentioned|p214|||||||||
6369|Eungai Mudstone|39331|6|Mentioned|Table 10-1|||||||||
6369|Eungai Mudstone|41009|6|Mentioned|Fig.2|||||||||
6369|Eungai Mudstone|43091|5|Briefly described|Map legend|||of Parry Group||||||
6369|Eungai Mudstone|43428|14|Not recorded|p140|||||||||
6369|Eungai Mudstone|43429|14|Not recorded|Map Legend||Late Devonian|Turbidites and pelagic mudstones||||||
6369|Eungai Mudstone|43434|4|Described|Map Legend||Late Devonian|||||||
6369|Eungai Mudstone|43435|2|Defined|Map Legend||Late Devonian|||||||
6369|Eungai Mudstone|43436|14|Not recorded|Map Legend||Devonian|(Provisional Edition)||||||
6369|Eungai Mudstone|47056|6|Mentioned|Fig.2 P523|||||||||
6369|Eungai Mudstone|68005|5|Briefly described|p49 Fig.3-M, p54, p149, p170.|Late Devonian|Late Devonian|Tamworth Belt.||Unit in Parry Group.||Overlies Lowana Formation and Noumea beds. Is overlain by Keepit Conglomerate.|Massive and laminated grey mudstone with rare wacke horizons and tuffaceous laminae and beds.|
6372|Euralie Limestone Member|22857|4|Described|p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Silverdale Formation. Fossiliferous tuffaceous sandstone, mudstone, limestone; contains mainly corals, conodonts. Max. thickness: 22.4m. Geological Province: Canberra-Yass Shelf.||||||
6372|Euralie Limestone Member|24248|5|Briefly described|p52|Wenlock|Wenlock|Of the Silverdale Formation. Basal member of Silverdale Formation.||||||02-JUN-08
6372|Euralie Limestone Member|30069|6|Mentioned|p8|||Fig. on p8.||||||02-JUN-08
6372|Euralie Limestone Member|31852|5|Briefly described|p711|||See also p718. Upper Silurian.||||||02-JUN-08
6372|Euralie Limestone Member|32155|6|Mentioned|Fig.1|||Refers fossil occurrences||||||
6372|Euralie Limestone Member|33116|6|Mentioned|Fig.11|||Correlation. Member of Laidlaw Formation.||||||02-JUN-08
6372|Euralie Limestone Member|34692|6|Mentioned|p186|||||||||
6372|Euralie Limestone Member|35244|6|Mentioned|p36|||||||||
6372|Euralie Limestone Member|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
6372|Euralie Limestone Member|35386|3|Fully described|p25|||||||||
6372|Euralie Limestone Member|36411|6|Mentioned|p268|||Refers Cramsie et al 1978 for definition||||||
6372|Euralie Limestone Member|37727|4|Described|p68|||||||||
6372|Euralie Limestone Member|38035|6|Mentioned|p91|||||||||
6372|Euralie Limestone Member|38274|6|Mentioned|p209|||||||||
6372|Euralie Limestone Member|39331|6|Mentioned|p46|||See also Fig.5-5.||||||02-JUN-08
6372|Euralie Limestone Member|40328|4|Described|p109|||||||||
6372|Euralie Limestone Member|42994|6|Mentioned|p61|||Of Silverdale Formation?||||||02-JUN-08
6372|Euralie Limestone Member|45075|5|Briefly described|p6|||Fauna||||||
6372|Euralie Limestone Member|45147|6|Mentioned|M152|||||||||
6372|Euralie Limestone Member|50230|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Yanawe Formation (Douro Group).  Fossiliferous tuffaceous sandstone, mudstone and limestone interbeds, calcareous nodules sporadically developed.||||||
6372|Euralie Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Yanawe Formation (Douro Group).  Fossiliferous tauffaceous sandstone, mudstone and limestone interbeds, calcareous nodules sporadically developed.||||||02-JUN-08
6372|Euralie Limestone Member|68592|2|Defined|p430 Fig.89, p434-6,p441,p514-5, p523-58|Wenlock|Llandovery|See also p239, p427, p1868-9, p1876. 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. 7-45m thick. Contains uneconomic limestone deposits. Diverse faunas, particularly corals and stromatoporoids; also the conodont Ozarkodina excavata. Minimum age of early Early Ludlow inferred from stratigraphic relationships, but mid-Wenlock from conodonts.||Unit in Yanawe Formation.||Overlies Laidlaw Volcanics disconformably. Is overlain gradationally by Excursion Creek Sandstone Member.|Limestone (micrite, biomicrite and nodular), interbedded tuffaceous sandstone, calcareous mudstone.|
6372|Euralie Limestone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdwe[asterisk]. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Yanawe Formation||Is overlain by Excursion Creek Limestone Member. Erosionally overlies unnamed member within Yanawe Formation.|Limestone (including micrite, biomicrite and nodular limestone), fossiliferous tuffaceous sandstone and calcareous mudstone.|
6372|Euralie Limestone Member|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Limestone (including micrite, biomicrite and nodular limestone), fossiliferous tuffaceous sandstone and calcareous mudstone.|
6372|Euralie Limestone Member|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Yanawe Formation|||Limestone (including micrite, biomicrite and nodular limestone) fossiliferous tuffaceous sandstone and calcareous mudstone.|
6372|Euralie Limestone Member|71656|6|Mentioned|p19, p21-22|Sheinwoodian|Wenlock|Contains some conodonts that constrain the age of the top of the Hawkins Volcanics.||Yanawe Formation, Douro Group|||Fossiliferous strata.|
6376|Euranbene Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Euranbene Adamellite.||||||
6382|Euriowie Subgroup|22553|6|Mentioned|p83|Proterozoic|Proterozoic|||||||
6382|Euriowie Subgroup|22772|4|Described|p66,Table13.1|Neoproterozoic III|Cryogenian|||||||
6382|Euriowie Subgroup|22857|5|Briefly described|p66, Tb. 13.1 (insert p70-71)|Marinoan|Sturtian|Of the Torrowangee Group. Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb.A1.3.||||||
6382|Euriowie Subgroup|36733|6|Mentioned|Table 5|||||||||
6382|Euriowie Subgroup|38157|6|Mentioned|p261|||||||||
6382|Euriowie Subgroup|41405|5|Briefly described|p204|||||||||
6382|Euriowie Subgroup|43268|5|Briefly described|Map Legend||Neoproterozoic|Of the Torrowangee Group.||||||11-SEP-07
6382|Euriowie Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Siltstone, minor sandstone, limestone, sandy limestone and conglomerate. South Australian equivalent is Farina Subgroup.||||||11-SEP-07
6382|Euriowie Subgroup|70000|5|Briefly described|p34, p39|Neoproterozoic|Neoproterozoic|Represents interglacial sedimentation during marine transgressions caused possibly by eustatic sea level rise from melting of ice sheets. Mined at Torrowangee quarries for flux for the Broken Hill smelter.||Unit in Torrowangee Group.|Includes Wammerra, Mitchie Well, Tanyarto, Yowahro, Floods Creek, Formations.|Overlies Yancowinna Subgroup. Is overlain unconformably by Teamsters Creek Subgroup.|Limestone, dolomite and calcareous siltstone and sandstone.|
6382|Euriowie Subgroup|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Torrowangee Group.|Includes Wammerra, Mitchie Well, Tanyarto, Yowahro and Floods Creek Formations; Corona Dolomite.|Overlies Yancowinna Subgroup. Is overlain by Teamsters Creek Subgroup.|Calcareous sedimentary rocks with interbedded sandstone and siltstone; includes dolomite, marl and conglomerate of marine origin.|
6386|Eurombah Formation|12597|5|Briefly described|p492 Tb.1, p496|Callovian|Callovian|N Surat Basin. Up to 100m thick.||Unit in Injune Creek Group.|||Interbedded lithic sandstone and minor polymictic conglomerate, siltstone and mudstone.|
6386|Eurombah Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Middle Jurassic|Middle Jurassic|In Surat Basin, Eromanga Basin.||||||
6386|Eurombah Formation|22857|5|Briefly described|p296-7 Tb.22.1, p315 Fig. 22.8|Bathonian|Bajocian|Of the Injune Creek Group. Geological Province: Surat Basin.||||||
6386|Eurombah Formation|22865|5|Briefly described|Table22.1p296-7||Bajocian|||||||
6386|Eurombah Formation|23056|6|Mentioned|10|||Geol province Eromanga Basin||||||
6386|Eurombah Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
6386|Eurombah Formation|24068|4|Described|p270 Table 2|Middle Jurassic|Middle Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 95m.||||||
6386|Eurombah Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
6386|Eurombah Formation|30699|6|Mentioned|p53|||Middle Jurassic age||||||
6386|Eurombah Formation|33367|3|Fully described|p16|||||||||
6386|Eurombah Formation|33371|2|Defined|p57|Jurassic|Jurassic|See also p58.?mid Jurassic.||||||
6386|Eurombah Formation|33672|5|Briefly described|p44|||||||||
6386|Eurombah Formation|33774|6|Mentioned|p55|||Refers Swarbrick et al. (1973)||||||
6386|Eurombah Formation|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
6386|Eurombah Formation|35937|6|Mentioned|Fig.5|||||||||
6386|Eurombah Formation|36243|6|Mentioned|Table 6A|||||||||
6386|Eurombah Formation|36570|6|Mentioned|p66|||||||||
6386|Eurombah Formation|37117|5|Briefly described|p313|||||||||
6386|Eurombah Formation|37463|6|Mentioned|p479|||||||||
6386|Eurombah Formation|37993|6|Mentioned|Fig.2|||||||||
6386|Eurombah Formation|37995|4|Described|p64|||||||||
6386|Eurombah Formation|39212|5|Briefly described|p16|||||||||
6386|Eurombah Formation|39445|5|Briefly described|Table 10|||||||||
6386|Eurombah Formation|39494|6|Mentioned|Fig.5|||||||||
6386|Eurombah Formation|39943|6|Mentioned|Table 9A|||||||||
6386|Eurombah Formation|40030|6|Mentioned|Fig.5|||||||||
6386|Eurombah Formation|40245|6|Mentioned|Table 2|||||||||
6386|Eurombah Formation|40249|6|Mentioned|p38|||Mention P41||||||
6386|Eurombah Formation|40250|6|Mentioned|Fig.7|||||||||
6386|Eurombah Formation|40541|6|Mentioned|p114|||||||||
6386|Eurombah Formation|40544|6|Mentioned|Fig.6|||||||||
6386|Eurombah Formation|41187|5|Briefly described|p225|||||||||
6386|Eurombah Formation|41247|6|Mentioned|Fig.7|||||||||
6386|Eurombah Formation|41266|6|Mentioned|Fig.3|||||||||
6386|Eurombah Formation|41992|4|Described|Fig.2 P183|||||||||
6386|Eurombah Formation|42007|5|Briefly described|Fig.2 P182|||||||||
6386|Eurombah Formation|42248|6|Mentioned|p410|||||||||
6386|Eurombah Formation|42493|5|Briefly described|Fig. 1 P18|||||||||
6386|Eurombah Formation|42911|5|Briefly described|p13, p37|||||||||
6386|Eurombah Formation|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
6386|Eurombah Formation|43002|5|Briefly described|Fig.2,p135|||||||||
6386|Eurombah Formation|45110|2|Defined|p93|Middle Jurassic|Middle Jurassic|See also p24. Formerly Eurombah Beds, Exon (1971).||||||
6386|Eurombah Formation|46937|6|Mentioned|Fig.10|||||||||
6386|Eurombah Formation|46984|6|Mentioned|Table 1|||||||||
6386|Eurombah Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
6386|Eurombah Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
6386|Eurombah Formation|60995|6|Mentioned|p66|||Geological Province: Surat Basin. ||||||
6386|Eurombah Formation|60999|5|Briefly described|p177, p178 Fig. 10|||Partly equivalent to Walloon Coal Measures.  Geological Province: Surat Basin.||||||
6386|Eurombah Formation|61000|5|Briefly described|p183|Bajocian|Bajocian|Geological Province: Surat Basin.||||||
6386|Eurombah Formation|61377|5|Briefly described|p148 Tb. SU1|Early Jurassic|Early Jurassic|Labile sandstone, polymictic conglomerate, siltstone, mudstone. Geological Province: Surat Basin.||||||07-FEB-11
6386|Eurombah Formation|63218|6|Mentioned|p211 Fig.2, p212 Fig.3. |Middle Jurassic|Middle Jurassic|Surat Basin.||Basal unit in Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Durabilla Formation.||
6386|Eurombah Formation|64197|6|Mentioned|p630 Fig.7|Middle Jurassic|Middle Jurassic|||||Underlies the Walloon Coal Measures, overlies the Hutton Sandstone.||
6386|Eurombah Formation|64665|5|Briefly described|p60.|Middle Jurassic|Middle Jurassic|Surat Basin. With the Hutton Sandstone and Walloon Subgroup, forms the second of six cyclothems.||||Overlies Hutton Sandstone. Is overlain by Walloon Subgroup.||
6386|Eurombah Formation|64856|4|Described|p86-87|Middle Jurassic|Middle Jurassic|Swarbrick et al. (1973). Formerly Eurombah beds of Exon et al. (1967). Type section set as the interval 27-120m in stratigraphic bore DRD 22. Surat Basin. Conformably overlies Hutton Sandstone. Thickly cross-bedded, fine to coarse-grained sandstones and interbedded siltstones and mudstones. Included in the Walloon Coal Measures in this article (and therefore of Middle Jurassic age).| | ||||28-NOV-17
6386|Eurombah Formation|64857|5|Briefly described|p132-133, p113 Fig.3|||Surat Basin. Sublabile to labile sandstones. Relationship with overlying unit not clear: Text states it underlies Walloon Coal Measures, however figures suggest Hutton Sandstone underlies Walloon Coal Measures.||||||
6386|Eurombah Formation|65003|6|Mentioned|p32|||||||||
6386|Eurombah Formation|65096|5|Briefly described|p368, p370 Fig.2|Middle Jurassic|Middle Jurassic|Previously Eurombah Beds of Exon (1971). Later defined as Formation (Swarbrick et al., 1973). ~100 m thick. Distinguishable from underlying Hutton Sandstone by higher gamma response, lower resistivity, flat SP response and much lower water production. Not readily distinguishable from overlying units - lithologically or on wireline logs.||Of the Walloon Coal Measures/Walloon Subgroup.||Gradationally overlies the Hutton Sandstone.|Variably a sandstone or shale and is largely devoid of coal.|
6386|Eurombah Formation|65117|5|Briefly described|p469, 470, Fig 4 p465|Bathonian|Middle Jurassic|Conformably overlies Hutton Sandstone and conformably underlies and interfingers with Walloon Coal Measures. Not laterally extensive. Lithic conglomeratic sandstone with mudstone and siltstone beds. Up to 100m thick. Seismic resolution does not allow identification of base of unit.||||||
6386|Eurombah Formation|65388|5|Briefly described|p214, 215|||Basal Injune Creek Group in SW Bungaban map sheet area. Defined by Swarbrick & others (1973), but cannot  be consistently differentiated from Walloon Coal Measures (Green & others, 1997). Poor outcrop. Overlies Hutton Sandstone.||||||
6386|Eurombah Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|68117|4|Described|p345-349|Middle Jurassic|Middle Jurassic|Swarbrick, Gray and Exon (1973) in their redefinition of the Injune Creek Group of Exon (1966). Recognised throughout the eastern Surat Basin. 80m thick, thinning to zero eastwards. Recognisable in resistivity and spontaneous potential logs.||Basal Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Durabilla Formation (Walloon Subgroup).|Porous sandstones.|
6386|Eurombah Formation|68139|5|Briefly described|p25 Fig.4|Middle Jurassic|Middle Jurassic|"Surat Basin. Appears as ""Durabilla Formation""/Eurombah Formation. Scott et al. (2004) had this Formation underlying the Durabilla Formation which was their basal unit in the Walloon Subgroup."||Basal Walloon Subgroup.||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.||
6386|Eurombah Formation|69574|6|Mentioned|p24|||"Surat Basin. Presented on p24 as ""Durabilla Formation""/Eurombah Formation."||||||
6386|Eurombah Formation|69582|5|Briefly described|p38|||Surat Basin.|||||Sandstone, mudstone and coal.|
6386|Eurombah Formation|69594|5|Briefly described|p536|||Exon et al. (1967); Swarbrick et al. (1973). Surat Basin. Has been included in basal Injune Creek Group (Exon, 1971), and Walloon Coal Measures (Green et al., 1997). Fluviatile deposits. In this study, it is regarded as a Member of the Walloon Coal Measures only in the NE Surat Basin.||||Conformably overlies the Hutton Sandstone.|Sublabile sandstone with minor interbedded conglomerate and carbonaceous mudstone. Contains a significant volcanic detrital component, unlike the underlying Hutton Sandstone.|
6386|Eurombah Formation|69790|5|Briefly described|p1066|||Early nomenclatural work restricted this unit to W side of the Mimosa Syncline. Its continued recognition is under debate: in this article it is included in Durabilla Formation.||||Overlies Hutton Sandstone. Is overlain by Walloon Subgroup.||
6386|Eurombah Formation|70374|5|Briefly described|p808, p809, figure 1,p813|Callovian|Callovian|Previously considered Bathonian - Callovian age. New dating within overlying Walloon Coal Measures, Surat Basin, suggest this unit now wholly Callovian. Amalgamated with Durabilla Formation in areas where the wireline log responses cannot be distinguished. ||Included in Walloon Subgroup by some, but not in Walloon Coal Measures by others.||Overlies Hutton Sandstone. Underlies Walloon Coal Measures conformably. Underlies Taroom Coal Measures.||28-SEP-16
6386|Eurombah Formation|70628|5|Briefly described|p952,953|Jurassic|Jurassic|Age inferred from stratigraphic description.||||Grades up into Walloon Subgroup (Taroom Coal Measures), overlies Hutton Sandstone conformably.|Heterolithic succession of isolated channel sandstones encased in overbank and flood-basin siltstones and mudstones, fines upward.|
6386|Eurombah Formation|70725|6|Mentioned|p13|Middle Jurassic|Middle Jurassic|Surat Basin. Is presented as Durabilla/Eurombah Formation.||||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.||
6386|Eurombah Formation|70821|5|Briefly described|p80|||Surat Basin.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|72297|5|Briefly described|p699 Fig.10.11|Jurassic|Jurassic|Surat Basin.||||Is overlain ?conformably by Walloon Coal Measures or Walloon Subgroup.||
6386|Eurombah Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Walloon Coal Measures.||
6386|Eurombah Formation|72921|4|Described|p13, p15 Fig.2, p16, p20, p40-42,46|Middle Jurassic|Middle Jurassic|Shown as located in the Surat Basin in Queensland.  Acts an aquitard between the Walloon Coal Measures and the Hutton Sandstone.||||Overlies and is equivalent to Hutton Sandstone and is underlying Walloon Coal Measures.||
6386|Eurombah Formation|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
6386|Eurombah Formation|73393|6|Mentioned|p20-22|Callovian|Bathonian|Surat Basin.||Injune Creek Group||Underlain by Hutton Sandstone. Overlain by Walloon Coal Measures. Equivalent to Birkhead Formation.||
6403|Evans Crown Granite|23214|3|Fully described|p254|Late Carboniferous|Late Carboniferous|Of Bathurst Batholith.  Intrudes the Lambie Group, Tarana Granite and Gibbons Creek Sandstone. Age:312Ma (Rb/Sr).||||||
6403|Evans Crown Granite|42712|4|Described|Table1p13; Fig3p9.|Carboniferous|Carboniferous|Variation on "Evans Crown Granite".||||||
6403|Evans Crown Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
6403|Evans Crown Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
6403|Evans Crown Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|of Bathurst Batholith.||||||
6403|Evans Crown Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
6416|Evergreen Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p496, p498, p501|Aalenian|Pliensbachian|N Surat and Mulgildie Basins. Thickness to 260m.|||Includes Boxvale Sandstone Member.|Conformably overlies Precipice Sandstone.|Siltstone; mudstone, locally highly carbonaceous, with well-preserved plant impressions; and labile to sub-labile sandstone; also contains an acritarch-bearing oolitic ironstone horizon.|
6416|Evergreen Formation|13516|5|Briefly described|p159, 167, 168, 169, 170-174, 139|Early Jurassic|Early Jurassic|From Eromanga and Surat Basins|||Includes Boxvale Sandstone Member, Westgrove Ironstone Member|||
6416|Evergreen Formation|22464|6|Mentioned|p9|Middle Jurassic|Early Jurassic|Eromanga Basin, overlies Precipice Formation||||||
6416|Evergreen Formation|22757|5|Briefly described|Table6,p12|Early Jurassic|Early Jurassic|250 m. Also Table5,p10. as 255 m. Ipswich-Moreton Basin.||||||
6416|Evergreen Formation|22857|4|Described|p295, p296-7 Tb 22.1, p546 Tb A1.12|Middle Jurassic|Early Jurassic|Of the Bundamba Group. Lacustrine shale, siltstone and sandstone interleaved with fluviatile Boxvale Sandstone Member (Qld.). Geological Province: Surat Basin. See also p314. ||||||
6416|Evergreen Formation|22865|4|Described|p295,Table22.1p296-7|Aalenian|Pliensbachian|||||||
6416|Evergreen Formation|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
6416|Evergreen Formation|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
6416|Evergreen Formation|23037|5|Briefly described|p34,47,114,117,8||Jurassic|||||||
6416|Evergreen Formation|23050|5|Briefly described|p82 Fig.17|Early Jurassic|Early Jurassic|of Surat Basin.||||||
6416|Evergreen Formation|23053|6|Mentioned|Fig10p17|Toarcian|Pliensbachian|||||||
6416|Evergreen Formation|23056|6|Mentioned|8 table 1B|||Geol province Eromanga Basin||||||
6416|Evergreen Formation|23799|3|Fully described|p51, p10 Tb. 1|Toarcian|Pliensbachian|Includes the former "Evergreen Shales" and Boxvale Sandstone as a member. Conformably overlies Precipice Sst; part unconformably overlies Chahpingah Meta-Igneous Complex; a subunit overlies the Tondahra Granite also. Geological Province: Surat Basin.||||||19-AUG-08
6416|Evergreen Formation|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
6416|Evergreen Formation|23841|4|Described|p448|||Geological Province: Great Artesian Basin.||||||
6416|Evergreen Formation|23883|5|Briefly described|p129 Fig. 11.2|Early Jurassic|Early Jurassic|Geological Province: Great Australian Superbasin.||||||
6416|Evergreen Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
6416|Evergreen Formation|24068|4|Described|p269|Middle Jurassic|Early Jurassic|Geological Province: Surat Basin.  Maximum thickness: 200m.||||||
6416|Evergreen Formation|24069|5|Briefly described|p284|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.||||||
6416|Evergreen Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
6416|Evergreen Formation|24159|5|Briefly described|p148 Fig.2, p151|Early Jurassic|Early Jurassic|Geological Province: Surat Basin. Overlying Unit: Hutton Sandstone. Underlying Unit: Precipice Sandstone.||||||
6416|Evergreen Formation|24241|5|Briefly described|p19 Fig.4|Jurassic|Jurassic|||||||
6416|Evergreen Formation|24488|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|24615|5|Briefly described|CD|Jurassic|Jurassic|[Je, Je/o].  Labile and sublabile, fine- to medium-grained sandstone, carbonaceous mudstone, siltstone and minor coal;  local oolitic ironstone.||||||
6416|Evergreen Formation|29385|6|Mentioned|p80|||Also P81.Jurassic||||||
6416|Evergreen Formation|29387|6|Mentioned|p30|||Also Table 5.||||||
6416|Evergreen Formation|29389|6|Mentioned|p19|||Early Jurassic.||||||
6416|Evergreen Formation|29393|6|Mentioned|Table 4|||Jurassic.||||||
6416|Evergreen Formation|29410|6|Mentioned|p274|||Geological map. Jurassic.||||||
6416|Evergreen Formation|29489|6|Mentioned|p11|||||||||
6416|Evergreen Formation|29496|6|Mentioned|p21|||||||||
6416|Evergreen Formation|29591|6|Mentioned|p69|||||||||
6416|Evergreen Formation|29721|6|Mentioned|p246|||||||||
6416|Evergreen Formation|29958|6|Mentioned|p13|||||||||
6416|Evergreen Formation|29960|5|Briefly described|p2|||||||||
6416|Evergreen Formation|29961|5|Briefly described|p14|||||||||
6416|Evergreen Formation|30022|6|Mentioned|p38|||||||||
6416|Evergreen Formation|30102|6|Mentioned|p17|||Correlation with basal Hutton Sandstone.||||||
6416|Evergreen Formation|30103|6|Mentioned|p10|||||||||
6416|Evergreen Formation|30232|6|Mentioned|p667,668,677||Early Jurassic|||||||
6416|Evergreen Formation|30451|3|Fully described|p72|||See also p73. Jurassic age.||||||07-APR-08
6416|Evergreen Formation|30455|6|Mentioned|p5|||See also P13||||||
6416|Evergreen Formation|30456|6|Mentioned|p95|||||||||
6416|Evergreen Formation|30457|6|Mentioned|p96|||||||||
6416|Evergreen Formation|30458|6|Mentioned|p3|||Jurassic age||||||
6416|Evergreen Formation|30460|6|Mentioned|p5|||Jurassic age||||||
6416|Evergreen Formation|30462|6|Mentioned|p356|||||||||
6416|Evergreen Formation|30464|6|Mentioned|Fig.1|||iniospores||||||
6416|Evergreen Formation|30465|6|Mentioned|p4|||||||||
6416|Evergreen Formation|30466|6|Mentioned|p5|||Jurassic age||||||
6416|Evergreen Formation|30472|6|Mentioned|p132|||Pollen distribution.||||||
6416|Evergreen Formation|30474|6|Mentioned|p251|||Correlation chart||||||
6416|Evergreen Formation|30494|6|Mentioned|p9|||||||||
6416|Evergreen Formation|30508|6|Mentioned|p81|||See also P90. Early Jurassic palynology||||||
6416|Evergreen Formation|30691|6|Mentioned|p15|||On Table 4||||||
6416|Evergreen Formation|30692|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30695|4|Described|Table 3|||Lower Jurassic age||||||
6416|Evergreen Formation|30696|4|Described|Table 4|||Lower Jurassic age||||||
6416|Evergreen Formation|30698|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30699|5|Briefly described|p52|||Structure map. See also stratigraphy p53.||||||18-SEP-18
6416|Evergreen Formation|30701|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|30702|6|Mentioned|Fig.1|||See Stratigraphic Table||||||
6416|Evergreen Formation|30854|4|Described|Table 4|||Lower Jurassic age||||||
6416|Evergreen Formation|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|30915|6|Mentioned|p98|||||||||
6416|Evergreen Formation|30916|6|Mentioned|p97|||||||||
6416|Evergreen Formation|31116|4|Described|p21|||L. Jurassic. See also p1.||||||18-SEP-18
6416|Evergreen Formation|31117|5|Briefly described|p379|||Jurassic. Lithology.||||||18-SEP-18
6416|Evergreen Formation|31118|6|Mentioned|p313|||Refers Casey et al. (1966)||||||
6416|Evergreen Formation|31120|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|31304|5|Briefly described|p628|||Lithology in drill hole.||||||
6416|Evergreen Formation|31369|6|Mentioned|Table 4|||Jurassic||||||
6416|Evergreen Formation|31438|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|31659|6|Mentioned|p74|||Jurassic||||||
6416|Evergreen Formation|32136|5|Briefly described|p3|||Late Toarcian age for upper section. Jur. miospores.||||||18-SEP-18
6416|Evergreen Formation|32137|6|Mentioned|p355|||Refers oolite beds||||||
6416|Evergreen Formation|32138|6|Mentioned|p396|||||||||
6416|Evergreen Formation|32182|4|Described|p3|||Jurassic||||||
6416|Evergreen Formation|32193|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|32276|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|32712|6|Mentioned|p127|||See also Table 1||||||
6416|Evergreen Formation|32715|6|Mentioned|p1186|||Re oil||||||
6416|Evergreen Formation|32797|4|Described|Table 4|||L. Jur.||||||
6416|Evergreen Formation|33059|4|Described|p113|||L.Jur.||||||
6416|Evergreen Formation|33071|4|Described|p6|||L.Jur.||||||
6416|Evergreen Formation|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33088|4|Described|Table 3|||Injune Ck.Gp.||||||
6416|Evergreen Formation|33090|4|Described|Table 4|||L.Jur.||||||
6416|Evergreen Formation|33094|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33192|6|Mentioned|p21|||||||||
6416|Evergreen Formation|33367|5|Briefly described|Table 1|||||||||
6416|Evergreen Formation|33381|5|Briefly described|p117|||Correl. chart. L. Jur. Constituent formations. See also p119.||||||18-SEP-18
6416|Evergreen Formation|33451|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|33530|5|Briefly described|Table 1|||Lower Jurassic.||||||18-SEP-18
6416|Evergreen Formation|33639|6|Mentioned|p10|||||||||
6416|Evergreen Formation|33672|4|Described|p41|||||||||
6416|Evergreen Formation|33673|4|Described|p291|||||||||
6416|Evergreen Formation|33675|4|Described|p412|||Lithology.||||||
6416|Evergreen Formation|33728|6|Mentioned|p38|||||||||
6416|Evergreen Formation|33774|3|Fully described|p48|||||||||
6416|Evergreen Formation|33971|6|Mentioned|Appendix 1|||Palynology. Doubtful about Formation assignment.||||||
6416|Evergreen Formation|34001|6|Mentioned|p18|||In Noona No.1 Well||||||
6416|Evergreen Formation|34065|6|Mentioned|p10|||L.Jur.||||||
6416|Evergreen Formation|34134|6|Mentioned|Cor.Chart|||Lower Jurassic||||||
6416|Evergreen Formation|34172|6|Mentioned|p53|||||||||
6416|Evergreen Formation|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|34212|6|Mentioned|p2|||Jurassic. See also PP8,14 etc.||||||
6416|Evergreen Formation|34213|6|Mentioned|p356|||See also P360.||||||
6416|Evergreen Formation|34452|6|Mentioned|p1|||L.Jurassic. See also PP2,3,4,5 etc||||||
6416|Evergreen Formation|34507|6|Mentioned|p87|||||||||
6416|Evergreen Formation|34613|4|Described|Table 4|||||||||
6416|Evergreen Formation|34618|6|Mentioned|p9|||||||||
6416|Evergreen Formation|34905|6|Mentioned|p531|||||||||
6416|Evergreen Formation|35079|6|Mentioned|Fig.3|||||||||
6416|Evergreen Formation|35095|6|Mentioned|p116|||||||||
6416|Evergreen Formation|35148|4|Described|p415|||See also Fig.1 and Table 1.||||||
6416|Evergreen Formation|35157|6|Mentioned|p518|||||||||
6416|Evergreen Formation|35562|6|Mentioned|p295|||Stratigraphy||||||
6416|Evergreen Formation|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
6416|Evergreen Formation|35811|5|Briefly described|Table 5|||||||||
6416|Evergreen Formation|35901|6|Mentioned|p17|||||||||
6416|Evergreen Formation|35937|6|Mentioned|Fig.5|||||||||
6416|Evergreen Formation|36111|6|Mentioned|p34|||||||||
6416|Evergreen Formation|36113|6|Mentioned|p21|||||||||
6416|Evergreen Formation|36233|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|36236|6|Mentioned|p183|||||||||
6416|Evergreen Formation|36241|6|Mentioned|p110|||||||||
6416|Evergreen Formation|36243|6|Mentioned|Table 6A|||||||||
6416|Evergreen Formation|36333|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|36570|6|Mentioned|p26,p55|||See also Table 1.||||||
6416|Evergreen Formation|36574|6|Mentioned|p599|||||||||
6416|Evergreen Formation|36613|6|Mentioned|p1876|||||||||
6416|Evergreen Formation|36643|6|Mentioned|p61|||||||||
6416|Evergreen Formation|36708|6|Mentioned|p52|||||||||
6416|Evergreen Formation|36825|6|Mentioned|p14|||||||||
6416|Evergreen Formation|36905|6|Mentioned|p20|||||||||
6416|Evergreen Formation|36914|6|Mentioned|p87|||||||||
6416|Evergreen Formation|36919|6|Mentioned|p160|||||||||
6416|Evergreen Formation|36926|6|Mentioned|p162|||||||||
6416|Evergreen Formation|37065|5|Briefly described|p38|||||||||
6416|Evergreen Formation|37117|5|Briefly described|p313|||||||||
6416|Evergreen Formation|37252|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|37288|6|Mentioned|p41|||||||||
6416|Evergreen Formation|37463|6|Mentioned|p479|||||||||
6416|Evergreen Formation|37618|6|Mentioned|p26|||||||||
6416|Evergreen Formation|37994|6|Mentioned|p144|||||||||
6416|Evergreen Formation|37995|4|Described|p62|||||||||
6416|Evergreen Formation|37996|6|Mentioned|p71|||||||||
6416|Evergreen Formation|38205|6|Mentioned|p96|||||||||
6416|Evergreen Formation|38226|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|38358|6|Mentioned|Fig.1|||||||||
6416|Evergreen Formation|38373|6|Mentioned|p617|||||||||
6416|Evergreen Formation|38447|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|39070|4|Described|p362|||||||||
6416|Evergreen Formation|39212|4|Described|p15|||p24 Petroleum reservoir. See also P36 excursion site.||||||18-SEP-18
6416|Evergreen Formation|39215|6|Mentioned|p53|||||||||
6416|Evergreen Formation|39218|6|Mentioned|p48|||Flora||||||
6416|Evergreen Formation|39315|6|Mentioned|Fig.5|||||||||
6416|Evergreen Formation|39445|5|Briefly described|p127|||Depositional environment. See also Table 10.||||||18-SEP-18
6416|Evergreen Formation|39478|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|39494|6|Mentioned|p137|||||||||
6416|Evergreen Formation|39505|6|Mentioned|p179|||||||||
6416|Evergreen Formation|39632|6|Mentioned|p209|||||||||
6416|Evergreen Formation|39757|6|Mentioned|p1601|||||||||
6416|Evergreen Formation|39815|6|Mentioned|p444|||||||||
6416|Evergreen Formation|39847|6|Mentioned|p35|||||||||
6416|Evergreen Formation|39907|6|Mentioned|F15|||||||||
6416|Evergreen Formation|39943|6|Mentioned|Table 8A|||||||||
6416|Evergreen Formation|39989|6|Mentioned|p426|||||||||
6416|Evergreen Formation|40030|6|Mentioned|p135|||||||||
6416|Evergreen Formation|40121|6|Mentioned|p446|||||||||
6416|Evergreen Formation|40245|6|Mentioned|Table 2|||||||||
6416|Evergreen Formation|40249|6|Mentioned|p38|||||||||
6416|Evergreen Formation|40250|4|Described|p29|||||||||
6416|Evergreen Formation|40540|6|Mentioned|p150|||||||||
6416|Evergreen Formation|40541|3|Fully described|p108|||||||||
6416|Evergreen Formation|40544|6|Mentioned|p161|||||||||
6416|Evergreen Formation|40623|5|Briefly described|p72|||Briefly described p109.||||||18-SEP-18
6416|Evergreen Formation|40666|4|Described|p355|||||||||
6416|Evergreen Formation|40675|6|Mentioned|Table 8A|||||||||
6416|Evergreen Formation|40687|3|Fully described|p412|||||||||
6416|Evergreen Formation|40688|6|Mentioned|p424|||||||||
6416|Evergreen Formation|40767|5|Briefly described|p14|||||||||
6416|Evergreen Formation|40832|3|Fully described|p254|||||||||
6416|Evergreen Formation|40833|6|Mentioned|p468|||||||||
6416|Evergreen Formation|40953|6|Mentioned|p19|||||||||
6416|Evergreen Formation|40962|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|41060|6|Mentioned|p2|||||||||
6416|Evergreen Formation|41061|6|Mentioned|p19|||||||||
6416|Evergreen Formation|41064|6|Mentioned|p60|||||||||
6416|Evergreen Formation|41097|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|41159|6|Mentioned|Fig.4|||||||||
6416|Evergreen Formation|41177|6|Mentioned|p223|||||||||
6416|Evergreen Formation|41187|6|Mentioned|Fig.2|||||||||
6416|Evergreen Formation|41188|6|Mentioned|p232|||||||||
6416|Evergreen Formation|41198|6|Mentioned|Table 1|||||||||
6416|Evergreen Formation|41210|3|Fully described|p158|||||||||
6416|Evergreen Formation|41211|6|Mentioned|p179|||||||||
6416|Evergreen Formation|41246|6|Mentioned|Map legend|Jurassic||||||||
6416|Evergreen Formation|41247|6|Mentioned|p127|||||||||
6416|Evergreen Formation|41266|6|Mentioned|Fig.3|||||||||
6416|Evergreen Formation|41455|6|Mentioned|p68|||||||||
6416|Evergreen Formation|41591|6|Mentioned|p17|||||||||
6416|Evergreen Formation|41725|6|Mentioned|p400|||||||||
6416|Evergreen Formation|41747|6|Mentioned|p469|||||||||
6416|Evergreen Formation|41992|4|Described|Fig.2 P183|||||||||
6416|Evergreen Formation|42007|5|Briefly described|Fig.2 P182|||||||||
6416|Evergreen Formation|42067|4|Described|Apendix 2|||See also p311.||||||18-SEP-18
6416|Evergreen Formation|42157|6|Mentioned|p377|||||||||
6416|Evergreen Formation|42248|6|Mentioned|p410|||||||||
6416|Evergreen Formation|42316|6|Mentioned|p8|||||||||
6416|Evergreen Formation|42463|6|Mentioned|Fig.5 P172|||||||||
6416|Evergreen Formation|42493|5|Briefly described|p17, Fig.1 p18|||||||||
6416|Evergreen Formation|42634|6|Mentioned|p12|||||||||
6416|Evergreen Formation|42865|6|Mentioned|p18|||||||||
6416|Evergreen Formation|42893|6|Mentioned|p12|||||||||
6416|Evergreen Formation|42911|5|Briefly described|p13|||||||||
6416|Evergreen Formation|43000|5|Briefly described|Fig.5,p112|||||||||
6416|Evergreen Formation|43002|5|Briefly described|Fig.2,p135|||||||||
6416|Evergreen Formation|43004|5|Briefly described|Table 1,p179|||||||||
6416|Evergreen Formation|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Surat Basin.||||||12-APR-05
6416|Evergreen Formation|43185|6|Mentioned|6||Jurassic|||||||
6416|Evergreen Formation|43582|6|Mentioned|Fig.5,p16,28||Early Jurassic|||||||
6416|Evergreen Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
6416|Evergreen Formation|43714|6|Mentioned|Fig.3,p5||Early Jurassic|||||||
6416|Evergreen Formation|43851|14|Not recorded|Tb p106,111,113||Early Jurassic|||||||
6416|Evergreen Formation|43923|6|Mentioned|p4||Jurassic|||||||
6416|Evergreen Formation|43982|14|Not recorded|Map Legend|||||||||
6416|Evergreen Formation|43983|14|Not recorded|p2,Fig.1|||||||||
6416|Evergreen Formation|43989|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|43994|14|Not recorded|Map Legend|||||||||
6416|Evergreen Formation|43997|14|Not recorded|p114|||||||||
6416|Evergreen Formation|43998|4|Described|p14,17,map||Early Jurassic|||||||
6416|Evergreen Formation|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|44023|4|Described|Tb.3,p10||Early Jurassic|||||||
6416|Evergreen Formation|44026|14|Not recorded|p123,124||Jurassic|||||||
6416|Evergreen Formation|44028|14|Not recorded|Fig.2,p512||Jurassic|See Strat Table.||||||
6416|Evergreen Formation|44031|14|Not recorded|p9,11||Early Jurassic|||||||
6416|Evergreen Formation|44032|14|Not recorded|p462,map,p463,464|||Surat Basin,= to Marburg Formation of Moreton Basin. Inlcudes Westgrove Ironside Member and Boxvale Sandstone Member.||||||
6416|Evergreen Formation|44084|14|Not recorded|p18,0,22,24,26,28,32||Early Jurassic|||||||
6416|Evergreen Formation|44091|14|Not recorded|p57||Jurassic|||||||
6416|Evergreen Formation|44115|14|Not recorded|p17-24|||||||||
6416|Evergreen Formation|44116|14|Not recorded|p28,33|||||||||
6416|Evergreen Formation|44118|14|Not recorded|Map Legend||Jurassic|||||||
6416|Evergreen Formation|44124|14|Not recorded|p4|||||||||
6416|Evergreen Formation|44129|14|Not recorded|p95-96||Jurassic|||||||
6416|Evergreen Formation|44169|2|Defined|Tb.1,p9,map|||||||||
6416|Evergreen Formation|44170|2|Defined|p21-23,32,25,40,map||Early Jurassic|Tb.1.||||||
6416|Evergreen Formation|44174|14|Not recorded|p345,347-349||Early Jurassic|||||||
6416|Evergreen Formation|44207|14|Not recorded|p115|||||||||
6416|Evergreen Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
6416|Evergreen Formation|44379|14|Not recorded|p21|||||||||
6416|Evergreen Formation|44381|14|Not recorded|p7|||||||||
6416|Evergreen Formation|44390|14|Not recorded|p9,13,15,16,Tb.1||Early Jurassic|||||||
6416|Evergreen Formation|44391|14|Not recorded|Map Legend||Early Jurassic|||||||
6416|Evergreen Formation|44415|14|Not recorded|Fig.2,p23|||||||||
6416|Evergreen Formation|44419|14|Not recorded|p274,278||Jurassic|||||||
6416|Evergreen Formation|44420|14|Not recorded|p1,3-5,9-11,18,20,22|||p26,Fig.14||||||
6416|Evergreen Formation|44421|14|Not recorded|p,6,10-17,19-21||Jurassic|||||||
6416|Evergreen Formation|44422|14|Not recorded|p149,153||Jurassic|||||||
6416|Evergreen Formation|44426|14|Not recorded|p12||Early Jurassic|Early Jurassic on spore data. Contains spores, bone fragments and leaves, including Pagiophyllum, Cladophlebis, Coniopteris, Otozamites and Nilssonia.||||||
6416|Evergreen Formation|44525|14|Not recorded|p520|||||||||
6416|Evergreen Formation|44573|14|Not recorded|p97||Jurassic|||||||
6416|Evergreen Formation|44636|2|Defined|p161,164,165,167||Early Jurassic|||||||
6416|Evergreen Formation|44637|14|Not recorded|Table||Jurassic|||||||
6416|Evergreen Formation|44640|14|Not recorded|p30|||||||||
6416|Evergreen Formation|44644|14|Not recorded|p18|||||||||
6416|Evergreen Formation|44668|14|Not recorded|p59,60|||||||||
6416|Evergreen Formation|44742|14|Not recorded|p91|||Lower part correlated with Razorback Beds on palynological evidence.||||||
6416|Evergreen Formation|44787|14|Not recorded|Tb.123,125,diag.p126||Jurassic|||||||
6416|Evergreen Formation|44805|14|Not recorded|p388|||||||||
6416|Evergreen Formation|45071|3|Fully described|Table 15|||||||||
6416|Evergreen Formation|45073|6|Mentioned|p58|||Geological history||||||
6416|Evergreen Formation|45110|3|Fully described|p90|||See also p13 and p24.||||||18-SEP-18
6416|Evergreen Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
6416|Evergreen Formation|46984|6|Mentioned|p154|||See also Table 1.||||||
6416|Evergreen Formation|46989|5|Briefly described|Table 1|||||||||
6416|Evergreen Formation|48900|4|Described|p51|||Lower Jurassic.||||||
6416|Evergreen Formation|48919|4|Described|p45|||See also p46-53. Jurassic.||||||18-SEP-18
6416|Evergreen Formation|48920|5|Briefly described|p44|||||||||
6416|Evergreen Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
6416|Evergreen Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
6416|Evergreen Formation|50190|5|Briefly described|p37, 85|Jurassic|Jurassic|Contains oolitic ironstone units. Geological Province: Mulgildie Basin.||||||06-APR-05
6416|Evergreen Formation|50214|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
6416|Evergreen Formation|50301|5|Briefly described|Map Legend|Jurassic|Jurassic|Ironstone, sandstone, siltstone, mudstone.||||||09-JUN-04
6416|Evergreen Formation|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Surat Basin||||||
6416|Evergreen Formation|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Mudstone, siltstone, sandstone, ironstone, minor coal.||||||
6416|Evergreen Formation|50598|5|Briefly described|Map Legend|Jurassic|Jurassic|Fine to medium grained sandstone, carbonaceous mudstone, siltstone and minor coal.||||||21-JUL-04
6416|Evergreen Formation|60281|5|Briefly described|p27|||Geological Province: Surat Basin, Cecil Plains Sub-basin.||||||
6416|Evergreen Formation|60282|5|Briefly described|p11, p39|Jurassic|Jurassic|Contains oolitic ironstone units.  Geological Province: Mulgildie Basin.||||||13-APR-05
6416|Evergreen Formation|60993|6|Mentioned|p17, p6 Fig. 2|||Correlates with Marburg Subgroup units. Geological Province: Surat Basin.||||||
6416|Evergreen Formation|60997|5|Briefly described|p140|||Includes the Boxvale Member. Geological Province: Surat Basin. ||||||
6416|Evergreen Formation|60998|5|Briefly described|p145|||Supersedes "Evergreen Shale". Comprises the original "Evergreen Shale", Boxvale Sandstone, Westgrove Ironstone Member and overlying shale sequence. Overlies Precipice Sandstone; underlies Hutton Sandstone.||||||
6416|Evergreen Formation|60999|5|Briefly described|p176, p178 Fig. 10|||Includes the basal oolitic Westgrove Ironstone Member. Lowermost part broadly correlates with Gatton Sandstone.  Geological Province: Surat Basin.||||||
6416|Evergreen Formation|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Gatton Sandstone. See also p255 Figs. 23, 24 and 25. ||||||
6416|Evergreen Formation|61087|5|Briefly described|Map Legend|Jurassic|Jurassic|mudstone, siltstone and fine-grained sublabile to labile sandstone; oolitic chamositic ironstone at the base.||||||
6416|Evergreen Formation|61310|6|Mentioned|p22|||Together with the Hutton Sandstone, correlated with Marburg Formation and "Upper Bundamba Unit".||||||
6416|Evergreen Formation|61377|5|Briefly described|p139, p148 Tb. |Early Jurassic|Early Jurassic|Major lacustrine shale/sltst/sst sequence; good hydrocarbon source rock - incl: Boxvale Sst Mbr (good reservoir sst). Conformably overlies Precipice Fm providing a good reservoir seal; conformably overlain by Hutton Sst. Geol.Prov:Surat Basin.||||||07-FEB-11
6416|Evergreen Formation|61611|6|Mentioned|p265 Fig. 3|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.||||||13-MAR-09
6416|Evergreen Formation|61832|5|Briefly described|p187|Jurassic|Jurassic|On the MUNDUBERRA sheet.  Overlain by Hutton Sandstone; overlies Precipice Sandstone. Geological Province: Surat Basin.||||||03-JUL-06
6416|Evergreen Formation|63218|6|Mentioned|p211 Fig.2. |Early Jurassic|Early Jurassic|Surat Basin.|||Includes Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|63748|6|Mentioned|p23|||Correlative of Marburg Subgroup.  Geological province: Surat Basin.||||||07-FEB-11
6416|Evergreen Formation|63979|6|Mentioned|p33, Fig. 44|Toarcian|Toarcian|Overlies Precipice Sandstone. Geological province: Surat Basin. Time-equivalent of Poolowanna Formation.||||||07-FEB-11
6416|Evergreen Formation|64197|6|Mentioned|p630 Fig.7|Early Jurassic|Early Jurassic|||||Underlies Hutton Sandstone; overlies Precipice Sandstone.||
6416|Evergreen Formation|64398|5|Briefly described|Map legend|Jurassic|Jurassic|Pale grey to greenish grey, flaggy, fine- to medium-grained, micaceous, labile to sublabile sandstone; pale green or khaki mudstone, carbonaceous mudstone; minor white siltstone and coal.||||||18-AUG-08
6416|Evergreen Formation|64399|5|Briefly described|Map legend|Jurassic|Jurassic|Overlain by Hutton Sst.  Flaggy, fine/med.-gr.micaceous, labile to sublabile sst; mudstone, carb.mudst.; minor siltst+coal. Fine lithic sst, siltst, mudst, oolitic or pelletal ironstone.Mudst., siltst.and fine-gr.sublabile sst; oolitic ironstone at base.||||||19-AUG-08
6416|Evergreen Formation|64665|5|Briefly described|p53 Fig.2, p60, p61.|Early Jurassic|Early Jurassic|Eromanga and Surat Basins. Lateral equivalent of upper part of Poolowanna Formation. Correlates with Ma Ma Creek Member (Clarence-Moreton Basin) and Brighton beds (Southern Nambour Basin). With the Precipice Sandstone, forms the first of six cyclothems in the Surat Basin.|||Includes Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.|Contains thin coals.|
6416|Evergreen Formation|64856|4|Described|p46 Fig.4, p76, p79, p81-85|Toarcian|Pleinsbachian|Surat Basin. Contains the Boxvale Sandstone, and the Westgrove Ironstone, Members. Conformably overlies the Precipice Sandstone and locally unconformably overlies Moolayember Formation of Bowen Basin /basement. Is overlain by Hutton Sandstone. Sandstone, siltstone, mudstone, shale. Age from palynoflora (units APJ21, 22, 3).| | ||||28-NOV-17
6416|Evergreen Formation|64857|4|Described|p130-132, p113 Fig.3|||Contains Boxvale Sandstone Member and Westgrove Ironstone Member. Conformably overlies Precipice Sandstone. Surat Basin.||||||
6416|Evergreen Formation|64858|5|Briefly described|p183-187, p181 Tb. 1|||Basal Surat Basin unit in the west, southwest and south of the basin.||||||30-NOV-09
6416|Evergreen Formation|64859|6|Mentioned|p195|||||||||
6416|Evergreen Formation|65003|5|Briefly described|p8||Early Jurassic|Of Surat Basin.||||Overlies the Precipice Sandstone.||
6416|Evergreen Formation|65096|6|Mentioned|p373|||Surat Basin. Along with Hutton Sandstone, compared with the  Marburg sub-group [sic] of the Clarence-Moreton Basin, east of the Toowoomba Strait.||||||
6416|Evergreen Formation|65112|5|Briefly described|p327; 328; Fig 11 p324, p329|Lower Jurassic|Lower Jurassic|Unit from Surat and Eromanga Basins, deposited in non-marine conditions.|194.5-178 Ma.|||Underlies the Hutton Sandstone and overlies the Precipice Sandstone.||22-MAR-12
6416|Evergreen Formation|65113|5|Briefly described|Fig 4 p340|Middle Jurassic|Early Jurassic|Overlies Precipice Sandstone, underlies Hutton Sandstone.||||||
6416|Evergreen Formation|65114|5|Briefly described|p385 Fig.3|Middle Jurassic|Early Jurassic|||||||
6416|Evergreen Formation|65116|5|Briefly described|p454-5, Fig 2 p437|Middle Jurassic|Early Jurassic|Underlies the Hutton Sandstone, Overlies the Precipice Sandstone, Surat Basin. Lithic sandstone, mudstone and minor coal. Upward coarsening and progradational sequence. ||||||
6416|Evergreen Formation|65117|5|Briefly described|p466, 7, 9, 470, 2, 4, Fig 4 p465|Toarcian|Pliensbachian|Surat Basin. Includes Boxvale Sandstone Member, Westgrove Ironstone Member., Overlies the Precipice Sandstone with gradational contact. Up to 300m thick. More widespread than Precipice Sandstone.||||||
6416|Evergreen Formation|65119|5|Briefly described|Fig 2, Table 1, Fig 4-5, 6-19|Early Jurassic|Early Jurassic|Surat Basin. Siltstone, mudstone, lithic to quartzose sandstone, minor oolithic ironstone, coal. Up to 260 m thick. Age: 188-198Ma. Fission Track age: 116+/-6 Ma . Present in Cockatoo Creek Well.||||||
6416|Evergreen Formation|65385|5|Briefly described|pS134 Fig.7|Early Jurassic|Early Jurassic|Of Eromanga Basin. Overlies Precipice Sandstone. Overlain by Hutton Sandstone.||||||08-MAR-12
6416|Evergreen Formation|65388|3|Fully described|p211-213, 204, 210, 17, 19, 42, 43, 46|Toarcian|Pliensbachian|Surat Basin, Mulgildie Basin.  Jensen & others (1964) defined the Evergreen Formation to include the "Evergreen Shales" as the lower unit, the overlying Boxvale Sandstone as a member and an upper mudstone, siltstone and sandstone containing an oolitic basal member (now Westgrove Ironstone Member).  Thickness 30-307m.  Conformably overlies Precipice Sandstone. Unconformably overlies Nogo beds, and Narayen beds, Torsdale Volcanics. Laterally continuous with the lower part of the Marburg Subgroup, Moreton Basin. Overlain by Hutton Sandstone. Palynofloras are largely Pliensbachian-Toarcian (Early Jurassic) and associated with units  APJ22, and APJ32. See also p208, 210, 289||||||
6416|Evergreen Formation|65489|6|Mentioned|p24|||Craton-derived sediment; potential reservoir.||||||
6416|Evergreen Formation|66529|6|Mentioned|p12 Fig.5 |||Eromanga Basin.|||Includes Boxvale Sandstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|66915|5|Briefly described|p6 Fig.3, p12|Middle Jurassic|Early Jurassic|Eromanga and Surat Basins.||||||
6416|Evergreen Formation|67133|5|Briefly described|p1-3, p5, p10-11, p19-21|Jurassic|Jurassic|Seal for Hutton Sandstone. Represents change from braided to meandering fluvial system of deposition. 29 samples of this unit were analysed by XRD and optical microscopy for this study. Quartz is the main component (25-97%) and kaolinite (2-35%) is the dominant clay mineral. Mixed-layer clays vary from smectite-rich to illite-rich.|||Boxvale Sandstone Member, Westgrove Ironstone Member.|Conformably overlies Precipice Sandstone. Is overlain by Hutton Sandstone.|Sandstones and mudstones.|
6416|Evergreen Formation|67402|4|Described|p146 fig SRT3, p147 fig SRT5|Bajocian|Pliensbachian|Surat and Mulgildie Basins. Potential conventional seal for carbon dioxide storage. Deposited in fresh-water lacustrine, meandering streams or deltal depositional environments. Generally less than 100m thick. Mistakenly referred to as the Evergreen Sandstone on p154. See also p148, p149 fig SRT7, p151, p152, p154, p155 fig SRT17, p156, p159, p160, p162, p252, p253, p306.|||Includes the Boxvale Member|Overlies the Precipice Sandstone and Boxvale Sandstone. Overlain by the Hutton Sandstone.|Sandstone, carbonaceous mudstone and siltstone, shale and coal.|
6416|Evergreen Formation|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Bundamba Group.||Overlain by Hutton Sandstone. Underlain by Precipice Sandstone.||
6416|Evergreen Formation|68003|5|Briefly described|p57 Fig.3-n, p58 Fig.3-o.|Early Jurassic|Early Jurassic|Bowen Basin. See also reference to [superseded] Evergreen Sandstone.||||Overlies Precipice Sandstone and, locally, unconformably overlies Napperby Formation. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|68004|5|Briefly described|p87, p172.|Early Jurassic|Early Jurassic|Surat Basin. Hydrocarbon reservoir in Queensland; targeted for oil/gas exploration in New South Wales from the 1960s; only minor fluorescence and low level gas shows. Excellent reservoir; exploration targetting limited to very northern part of the Basin in NSW.||||||
6416|Evergreen Formation|68008|4|Described|p233, p236-238, p240, p297|Early Jurassic|Early Jurassic|Jensen et al. (1964), for Jurassic sediments between Precipice Sandstone and Hutton Sandstone in the Surat Basin. Included Evergreen Shales (Whitehouse, 1953) and Boxvale Sandstone (Reeves, 1947). Surat and Mulgildie Basins. Fresh-water fluvial and lacustrine deposits. 105-260m thick. Age from microflora. The oolitic ironstone is a time marker linking this Formation to Landsborough Sandstone, Brighton beds and Tiaro Coal Measures. Has zones of deep weathering.||||Conformably overlies Precipice Sandstone. Is overlain conformably by Hutton Sandstone.|White and grey, fine-grained quartzose flaggy sandstone and siltstone, overlain by a ferruginous oolite horizon 3-4m thick, above which is thin-bedded, cream, friable flaggy sandstone. Local grey-black carbonaceous shale, siltstone and minor coal.|
6416|Evergreen Formation|68117|5|Briefly described|p346|Early Jurassic|Early Jurassic|Surat Basin.|||Westgrove Ironstone Member.|||
6416|Evergreen Formation|68135|5|Briefly described|p52 Fig.2b, p59, p64|Toarcian||Surat Basin (QLD). Vertebrate body parts, invertebrate and plant macrofossils throughout; including the freshwater plesiosaur Siderops.||||Overlies Precipice Sandstone. Is overlain unconformably by Hutton Sandstone|Silty sandstone with oolitic ironstone beds.|14-SEP-17
6416|Evergreen Formation|68139|6|Mentioned|p23, 32|Early Jurassic|Early Jurassic|Surat Basin. A regional seal.|||Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
6416|Evergreen Formation|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Surat and Mulgildie Basins. This unit, as well as the Hutton and Precipice Sandstones, are all mapped under the symbol, Jb.||||||
6416|Evergreen Formation|68576|4|Described|Q_4: p3, p12, p14, p17, p22|Early Jurassic|Early Jurassic|Surat Basin. Fluvio-lacustrine or prograding lacustrine delta deposits. Is locally capped by 27 Ma basalt from the Buckland volcano. Pliensbachian to Toarcian.|||Westgrove Ironstone Member, Boxvale Sandstone Member.|Conformably overlies Precipice Sandstone. Is overlain conformably by Hutton Sandstone.|Green-grey sandstone, carbonaceous mudstone and argillite, minor carbonaceous siltstone, shale and coal; then the Boxvale Sandstone Member; then dark green to black mudstone (laminated with sandstone, siltstone and shale) and fine-grained sandstone.|
6416|Evergreen Formation|68679|6|Mentioned|p312-313, p338|Jurassic|Jurassic|Northern New England Orogen.||||||
6416|Evergreen Formation|69457|5|Briefly described|p41:2-3|||NE Eromanga Basin and Surat Basin.|||Overlies Precipice Sandstone.|Lateral equivalent of (part) Poolowanna Formation.||12-JUL-16
6416|Evergreen Formation|69582|5|Briefly described|p36, p38|Lower Jurassic|Lower Jurassic|Surat Basin.||||Overlies the Precipice Sandstone. Overlain by the Hutton Sandstone.|Sandstone.|
6416|Evergreen Formation|69594|4|Described|p519, p524, p534-535, p536 Fig.7.17|Toarcian|Pliensbachian|See also p539, p544-546, p572. Whitehouse (1955), for the shales between the Precipice Sandstone and Boxvale Sandstone of Reeves (1947); redefined by Jensen et al. (1964) to include also the Boxvale Sandstone Member and the Westgrove Ironstone Member. Eromanga, northern Surat Basins. 10-40m, up to 307m, thick. Lacustrine, or meandering streams and deltas, deposits. A secondary-importance Surat Basin reservoir for oil condensate, gas and LPG.|||Boxvale Sandstone Member, Westgrove Ironstone Member.|Conformably overlies Precipice Sandstone. Is overlain by Hutton Sandstone. Laterally equivalent to the lower Marburg Subgroup and the Poolowanna Formation.|Fine sandstone, carbonaceous mudstone, lesser carbonaceous siltstone, shale and coal; overlain by the Boxvale Sandstone Member (mostly quartzose sandstone); then mudstone interlaminated with sandstone and shale and fine-grained labile sandstone.|
6416|Evergreen Formation|69633|4|Described|p1-5, p7-12, p14, p20-21|Early Jurassic|Early Jurassic|Surat Basin. Lacustrine sediments. Seal for the Precipice Sandstone hydrocarbon reservoir. GSQ Chinchilla 4 and Roma 8 core logs detailed (Appendix 4 & 5). The authors argue that at least part of the lowest c.58m of this unit, ie below the Boxvale Sandstone Member, should be assigned to the Precipice Sandstone. Palynology detailed. Data from sections from well completion reports are included in Appendix 1.|||Boxvale Sandstone, Westgrove Ironstone, Members.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|69681|5|Briefly described|p74-87|Early Jurassic|Early Jurassic|Yields oil in the Moonie field. Most of the core samples used for this study are from this unit and the Precipice Sandstone. Regarded as a seal for Precipice Sandstone CO2 geostorage.||||Overlies Precipice Sandstone.|Mainly interbedded sandstones, siltstones and shales.|
6416|Evergreen Formation|69682|4|Described|p92-110|Early Jurassic|Early Jurassic|Surat Basin. Potential intraformational seal to CO2 reservoir. Up to 307m thick. Mineralogy discussed in detail.|||Includes Boxvale Sandstone Member and Westgrove Ironstone Member.|Conformably overlies Precipice Sandstone.|Basal very fine to medium-grained sandstone, overlain by carbonaceous silt and mudstone, shale, oolitic ironstone and minor coal.|
6416|Evergreen Formation|69790|6|Mentioned|p1063 Fig.2|Early Jurassic|Early Jurassic|Eromanga Basin.|||Includes Westgrove Ironstone Member.|||
6416|Evergreen Formation|69946|6|Mentioned|p75|||||||||
6416|Evergreen Formation|69947|6|Mentioned|p23 Fig.7.12|||Surat Basin. Craton-derived sediments.||||||
6416|Evergreen Formation|70374|6|Mentioned|p809 figure 1|Bajocian|Pliensbachian|Surat Basin.|||Westgrove Ironstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||17-JAN-22
6416|Evergreen Formation|70628|6|Mentioned|p952 fig 4|Toarcian|Pliensbachian|Shown only as 'Evergreen' in fig 4. Along with Precipice Sandstone, forms part of the J-sequence (Hoffman et al 2009) of the Surat Basin.||||Overlies Precipice Sandstone. Underlies Hutton Sandstone.||
6416|Evergreen Formation|70821|5|Briefly described|p80|||Eromanga, Surat Basins.|||Boxvale Sandstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|71282|6|Mentioned|p457 Fig.1, p460|||Appears just as Evergreen in Fig.1.||||||
6416|Evergreen Formation|71342|6|Mentioned|Ch5 p74|||Surat Basin.||||||
6416|Evergreen Formation|71805|4|Described|p75-p79, p84, p86-p87|Toarcian|Toarcian|Eromanga Basin and northern Surat Basin. This unit is interpreted to have been deposited in a lacustrine or locally marine environment. In sequence stratigraphy of Hoffman et al (1997) the base of this unit is equivalent to S20 and the top S30. Placement of boundary with underlying Precipice Sandstone discussed.|||Includes Boxvale Sandstone Member and Westgrove Ironstone Member.|Conformably overlies the Precipice Sandstone. Overlain by the Hutton Sandstone.|Fine- to medium-grained, lithic, argillaceous sandstones, carbonaceous shales, siltstones and rarer thin discontinuous coal bands.|16-MAY-19
6416|Evergreen Formation|71806|4|Described|p483-p486, p500|Jurassic|Jurassic|Surat Basin. This unit is alluvial to lacustrine. Displays some evidence of marine influence including chamositic oolite layers, wavy to symmetrical ripples and brackish-tolerant acritarchs.|||Westgrove Ironstone Member and Boxvale Sandstone Member.|Overlies the Precipice Sandstone.||
6416|Evergreen Formation|72297|5|Briefly described|p712, p726, p745, p748|Early Jurassic|Early Jurassic|Surat-Mulgildie Basins. Iron deposits occur at Dawsonvale in the Mundubbera area. Is quarried for dimension stone (various applications listed) at Einsvold. Fair to good potential hydrocarbon source rock. Produced gas at the Grafton Range gasfield. Seal for Precipice Sandstone reservoirs; traps are structural-stratigraphic (briefly described),|||Boxvale Sandstone Member.||Grey to dark grey shales and mudstones; oolitic ironstone occurs in two distinct subunits in flat-lying sandstone.|
6416|Evergreen Formation|72298|5|Briefly described|p801|Jurassic|Triassic|Eromanga Basin (QLD,NSW), Surat Basin (QLD,NSW).|||Boxvale Sandstone Member.|Overlies Precipice Sandstone. Is overlain by Hutton Sandstone.||
6416|Evergreen Formation|72921|4|Described|p8, 9-10, p15-17, p20, 21 Fig.7, p23.|Early Jurassic|Early Jurassic|Of Surat Basin in Queensland. Forms a regional seal above the Precipice Sandstone reservoir, but lithology is vertically and lateraly variable. Shows evidence of marine influence. Shallow marine to lacustrine. Evergreen Formation and its correlatives are found across the Clarence-Moreton, Surat and Eromanga Basins. See also p23 Fig.9, p28, p32, p35, p42, p45, p48-p52, p54 Fig.29, p63, p66.|||Includes Westgrove Ironstone Member, Boxvale Sandstone Member|Conformably overlies Precipice Sandstone and underlies Hutton Sandstone with transitional contact.|Includes acritarchs, proximal and distal deltaic deposits, tidal bundles, chamositic oolites, pelecypods, anoxic black shales and tempestites.|
6416|Evergreen Formation|73113|5|Briefly described|p. 3, 19, 22-24, 31, 36-37, 41, 46...|||Surat Basin. Includes the Boxvale Sandstone [Boxvale Sandstone Member]. Groundwater model divides unit into upper and lower layers separated by the Boxvale Sandstone. Tight aquitard. More locations: p. 49, 60, 67, 69, 78-80, 87-88, 98, 115-116, 119, 148, 152-153, 171-172, 191.||||Underlain by Precipice Sandstone. Overlain by Hutton Sandstone.||
6416|Evergreen Formation|73147|6|Mentioned|p127|Early Jurassic|Early Jurassic||||Westgrove Ironstone Member|||
6416|Evergreen Formation|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
6416|Evergreen Formation|73393|6|Mentioned|p19-22|Toarcian|Pliensbachian|Surat and Eromanga Basins. An almost complete Jurassic tetrapod amphibian, Siderops kehli, was recovered from this unit (Kolane cattle station, SE QLD) along with two partially articulated freshwater plesiosaur specimens.|||Westgrove Ironstone Member|Underlain by Precipice Sandstone. Overlain by Hutton Sandstone.|Contains oolitic ironstone.|
6416|Evergreen Formation|73600|4|Described|p189-192, p194-203, p205|Toarcian|Pliensbachian|Surat Basin. Maximum thickness of ca 300 m. Gradational lower boundary. Palynology was previously used for biostratigraphic age constraint. Two new CA-TIMS zircon ages of 179.91 +/- 0.06 Ma and 184.61 +/- 0.33 Ma from tuffs; these corroborate palynological interpretations. A U-Pb detrital zircon age of 176.6 +/- 2.0 Ma was reported by Todd et al. (2019). Various detrital zircon maximum depositional ages are presented, which support the CA-TIMS tuff age. Complex sediment sourcing dominated by the Thomson Orogen. The presence of glauconite suggests marine influence.|179.91 +/- 0.06 Ma U-Pb CA-TIMS||Westgrove Ironstone Member, Boxvale Sandstone Member|Conformably underlain by Precipice Sandstone. Overlain by Hutton Sandstone.|Fine-grained sandstones and mudstones. Contains scattered tuffs.|
6437|Excelsior Porphyry Member|29903|5|Briefly described|p169|||||||||
6445|Exmouth Granodiorite|23720|5|Briefly described|Map Legend|Permian|Permian|Of Uralla Plutonic Suite.  Hornblende-biotite granodiorite.  Age most likely to be late Middle Permian p35.||||||15-DEC-04
6445|Exmouth Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
6445|Exmouth Granodiorite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
6445|Exmouth Granodiorite|38288|6|Mentioned|Fig.4|||||||||
6445|Exmouth Granodiorite|71628|5|Briefly described|p8: 3, 21-22, 33-34|||Neilson (1970; unpublished). Named after the locality of Exmouth, this is a small 1.5km diameter ovoid intrusion, 15km NNW of Armidale. Exposure is poor.||Mount Duval Suite.||Entirely surrounded and intruded by Mount Duval Monzogranite.|Fine- to medium-grained, equigranular to weakly porphyritic biotite-hornblende granodiorite.|
6451|Eyre Formation|13497|5|Briefly described|p115, p115 fig 6.33, p146, p151|Tertiary|Tertiary|Lake Eyre Basin.||||Unconformably overlies the Mount Howie Sandstone and the Winton Formation. Unconformably overlain by the Namba Formation.|Fluvial sandstone with a basal conglomerate.|
6451|Eyre Formation|22442|6|Mentioned|p54|Tertiary|Tertiary|||||||
6451|Eyre Formation|22495|6|Mentioned|P222|Eocene|Paleocene|||||||
6451|Eyre Formation|22587|4|Described|p71|Middle Eocene|Paleocene|||||||
6451|Eyre Formation|22671|6|Mentioned|Fig2p837|Tertiary|Tertiary|Sandstone sediments.||||||17-JAN-06
6451|Eyre Formation|22700|6|Mentioned|p775|Tertiary|Tertiary|Of Thomson Fold Belt.||||||18-SEP-06
6451|Eyre Formation|22712|5|Briefly described|p132|Tertiary|Tertiary|||||||
6451|Eyre Formation|22730|4|Described|p557,66,67|Eocene|Paleocene|After Wopfner 1974.||||||18-SEP-06
6451|Eyre Formation|22773|5|Briefly described|p355|||||||||
6451|Eyre Formation|22857|5|Briefly described|p355|Middle Eocene|Paleocene|Thickness: ~30m in SA borehole near border. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|22912|5|Briefly described|32|||Geol province Lake Eyre Basin.||||||26-NOV-08
6451|Eyre Formation|23154|5|Briefly described|Map Legend|Middle Eocene|Late Paleocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
6451|Eyre Formation|23155|4|Described|p33|Tertiary|Tertiary|Location of type section is advised p33. Unit does not crop out on STRZELECKI, but is present over all of the area. Overlying unit - Namba Formation (disconformity).  Underlain by Winton Formation (disconformity).||||||03-MAY-13
6451|Eyre Formation|23224|5|Briefly described|p3|Eocene|Paleocene|May correlate to Tertiary cover over White Cliffs Opal fields.||||||07-MAR-06
6451|Eyre Formation|23336|6|Mentioned|4|||||||||
6451|Eyre Formation|23339|5|Briefly described|4|Tertiary|Tertiary|||||||
6451|Eyre Formation|23380|5|Briefly described|p107-108|Eocene|Paleocene|||||||
6451|Eyre Formation|23477|5|Briefly described|p49 Fig 3|Tertiary|Tertiary|Geological Province: Curnamona Province.||||||
6451|Eyre Formation|23478|5|Briefly described|p28|Eocene|Paleocene|||||||
6451|Eyre Formation|23889|5|Briefly described|p18|Paleogene|Paleogene|||||||07-NOV-08
6451|Eyre Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
6451|Eyre Formation|24175|3|Fully described|p32, p32 Fig. 6|Eocene|Paleocene|Unconformably overlain by Etadunna Formation. Max. thickness: ~100 m. Geological Province: Lake Eyre Basin.||||||03-MAY-13
6451|Eyre Formation|24176|5|Briefly described|p19, p22 Tb. 1|Tertiary|Tertiary|Freshwater sands and gravels - calcareous sandstone, quartzite; agate, quartz and chert pebbles. Corresponds to the Murnpeowie Formation defined by Forbes (1966).||||||26-NOV-08
6451|Eyre Formation|24204|5|Briefly described|p263 Fig.4|Tertiary|Tertiary|Geological Province: Eyre Basin.||||||
6451|Eyre Formation|24321|5|Briefly described|Map legend|Early Eocene|Late Paleocene|Geological Province: Lake  Eyre Basin.||||||26-NOV-08
6451|Eyre Formation|24345|5|Briefly described|p82, 84-85 Fig.2|Eocene|Paleocene|||||||
6451|Eyre Formation|29658|6|Mentioned|p5|||||||||
6451|Eyre Formation|29660|6|Mentioned|p4|||||||||
6451|Eyre Formation|30054|5|Briefly described|p803|||||||||
6451|Eyre Formation|30055|6|Mentioned|p160|||||||||
6451|Eyre Formation|30056|6|Mentioned|p125|||See also p129, p134.||||||18-SEP-06
6451|Eyre Formation|30176|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
6451|Eyre Formation|30540|6|Mentioned|Fig.6|||||||||
6451|Eyre Formation|30804|4|Described|p12|||Lithology. See also Table 1||||||
6451|Eyre Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
6451|Eyre Formation|30919|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|30920|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|30921|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6451|Eyre Formation|31850|6|Mentioned|p33|||||||||
6451|Eyre Formation|32121|6|Mentioned|p422|||||||||
6451|Eyre Formation|32275|6|Mentioned|p9|||||||||
6451|Eyre Formation|33568|6|Mentioned|p48|||||||||
6451|Eyre Formation|33820|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|33821|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|33822|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
6451|Eyre Formation|33823|6|Mentioned|Map legend|Eocene|Paleocene|Paleocene - Eocene||||||
6451|Eyre Formation|33824|6|Mentioned|p7|||See also p12, Tables 1 and 2.||||||18-SEP-06
6451|Eyre Formation|33825|5|Briefly described|p8|||Strat. table. Lithology||||||
6451|Eyre Formation|33827|5|Briefly described|p14|||See also Table 1||||||
6451|Eyre Formation|33828|6|Mentioned|p11|||Table 1||||||
6451|Eyre Formation|33831|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|33832|6|Mentioned|p6|||Strat.||||||
6451|Eyre Formation|33937|6|Mentioned|p1|||||||||
6451|Eyre Formation|33938|2|Defined|p18|early Tertiary|early Tertiary|||||||
6451|Eyre Formation|33971|6|Mentioned|p37|||Strat. section Fig. 15.||||||
6451|Eyre Formation|34882|6|Mentioned|Fig. 1|||||||||
6451|Eyre Formation|35187|6|Mentioned|Table1|||||||||
6451|Eyre Formation|35793|6|Mentioned|p237|||||||||
6451|Eyre Formation|36554|6|Mentioned|p1647|||||||||
6451|Eyre Formation|36618|5|Briefly described|Table 1|||||||||
6451|Eyre Formation|36620|5|Briefly described|Fig.1|||See also p24.||||||18-SEP-06
6451|Eyre Formation|36922|6|Mentioned|Fig.3|||||||||
6451|Eyre Formation|36966|6|Mentioned|p81|||||||||
6451|Eyre Formation|37062|6|Mentioned|p182|||||||||
6451|Eyre Formation|37607|6|Mentioned|p333|||See also Fig.4.||||||
6451|Eyre Formation|37776|6|Mentioned|Fig.2|||||||||
6451|Eyre Formation|38022|6|Mentioned|p29|||||||||
6451|Eyre Formation|38226|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|38557|5|Briefly described|p291|||||||||
6451|Eyre Formation|38605|6|Mentioned|p35|||||||||
6451|Eyre Formation|38740|5|Briefly described|p306|||||||||
6451|Eyre Formation|39084|6|Mentioned|p22|||||||||
6451|Eyre Formation|39085|6|Mentioned|p13|||||||||
6451|Eyre Formation|39087|6|Mentioned|p15|||||||||
6451|Eyre Formation|39322|6|Mentioned|Fig.2|||||||||
6451|Eyre Formation|39352|6|Mentioned|Map legend|Miocene|Paleocene|Miocene to Palaeocene||||||
6451|Eyre Formation|39445|5|Briefly described|Table 14|||See also Fig.11.2||||||
6451|Eyre Formation|39478|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|39949|6|Mentioned|p274|||||||||
6451|Eyre Formation|40220|6|Mentioned|p7|||||||||
6451|Eyre Formation|40395|6|Mentioned|p313|||||||||
6451|Eyre Formation|40595|6|Mentioned|p93|||||||||
6451|Eyre Formation|40756|6|Mentioned|p1|||||||||
6451|Eyre Formation|40757|6|Mentioned|p75|||||||||
6451|Eyre Formation|40910|6|Mentioned|p17|||||||||
6451|Eyre Formation|40911|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene-Eocene||||||
6451|Eyre Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|40925|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|40926|3|Fully described|p22|||||||||
6451|Eyre Formation|40950|6|Mentioned|p250|||||||||
6451|Eyre Formation|40982|6|Mentioned|p363|||||||||
6451|Eyre Formation|41085|6|Mentioned|Fig.8|||||||||
6451|Eyre Formation|41098|4|Described|p177|||||||||
6451|Eyre Formation|41125|6|Mentioned|p34|||||||||
6451|Eyre Formation|41165|5|Briefly described|p364|||Mention  Fig.21||||||
6451|Eyre Formation|41184|6|Mentioned|p347|||||||||
6451|Eyre Formation|41198|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|41517|6|Mentioned|p140|||||||||
6451|Eyre Formation|41535|6|Mentioned|p368|||||||||
6451|Eyre Formation|41600|6|Mentioned|p816|||||||||
6451|Eyre Formation|42084|6|Mentioned|Fig.3 P356|||||||||
6451|Eyre Formation|42090|3|Fully described|p14|||See also Table 2.||||||18-SEP-06
6451|Eyre Formation|42340|5|Briefly described|p25|Eocene|Late Paleocene|||||||07-NOV-08
6451|Eyre Formation|42375|3|Fully described|p21-25, p29|early Oligocene?|Paleocene|Geological province: Birdsville Basin.||||||18-SEP-06
6451|Eyre Formation|42469|5|Briefly described|p35, p43, p44|||||||||
6451|Eyre Formation|42475|6|Mentioned|p20|||Birdsville Basin||||||
6451|Eyre Formation|42496|5|Briefly described|Fig.3 P132|||||||||
6451|Eyre Formation|42508|5|Briefly described|p66, p74|||||||||
6451|Eyre Formation|42541|6|Mentioned|p220|||||||||
6451|Eyre Formation|42543|5|Briefly described|Fig.4 P6|||||||||
6451|Eyre Formation|42592|5|Briefly described|Fig. 4 P270|||||||||
6451|Eyre Formation|42746|4|Described|p13|||See also Fig.2, Fig.9||||||
6451|Eyre Formation|42905|5|Briefly described|p23|||see also Fig.5.3||||||
6451|Eyre Formation|42957|6|Mentioned|p40|||||||||
6451|Eyre Formation|42999|6|Mentioned|p98|||||||||
6451|Eyre Formation|43035|5|Briefly described|p27|||||||||
6451|Eyre Formation|43048|5|Briefly described|p22|||||||||
6451|Eyre Formation|43052|5|Briefly described|Table 2.1|||||||||
6451|Eyre Formation|43053|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||25-MAY-05
6451|Eyre Formation|43071|5|Briefly described|p17|||||||||
6451|Eyre Formation|43094|5|Briefly described|p38|||||||||
6451|Eyre Formation|43258|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
6451|Eyre Formation|43298|5|Briefly described|Map Legend|Eocene|Paleocene|||||||
6451|Eyre Formation|44041|6|Mentioned|p242|||||||||
6451|Eyre Formation|44133|4|Described|p192, 124, 190 Fig. 10.30|Middle Eocene|Late Paleocene|Geological Province: Lake Eyre Basin. Includes the Macumba Sandstone, Murnpowie Formation. Overlain unconformably by the Etadunna and Namba Formations.||||||
6451|Eyre Formation|44934|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6451|Eyre Formation|45145|6|Mentioned|Table 7|||||||||
6451|Eyre Formation|46800|4|Described|p112|||See also p114.||||||18-SEP-06
6451|Eyre Formation|46802|6|Mentioned|Table 1|||||||||
6451|Eyre Formation|46833|6|Mentioned|p53|||||||||
6451|Eyre Formation|46854|6|Mentioned|p242|||||||||
6451|Eyre Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
6451|Eyre Formation|46911|5|Briefly described|p113|||Analyses of weathered profiles and parent rocks.||||||
6451|Eyre Formation|60648|6|Mentioned|p42|Cenozoic|Cenozoic|||||||19-NOV-08
6451|Eyre Formation|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|60955|5|Briefly described|Map Legend|Miocene|Eocene|Carbonaceous sandstones, siltstones, mudstones.||||||
6451|Eyre Formation|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial sand and conglomerate, usually silcreted. Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|61155|5|Briefly described|p2, p17|Middle Eocene|Late Paleocene|Sediments spread in thin sheets over large areas of the Birdsville Basin. Age: ~62-~42Ma. Max. thickness: 120m (in Lake Eyre Basin). Geological province: Oodnadatta area, Lake Eyre Basin and Tarkarooloo Basin.||||||03-MAR-10
6451|Eyre Formation|61823|5|Briefly described|p118|Middle Eocene|Paleocene|Overlain by Namba Formation. Age is Palaeogene.  Geological Province: Lake Eyre Basin.||||||
6451|Eyre Formation|61824|5|Briefly described|p128|Paleogene|Paleogene|Age is uncertain - it is also suggested that the rocks may be Mesozoic.||||||07-NOV-08
6451|Eyre Formation|61825|5|Briefly described|p138|Late Cretaceous|Late Cretaceous|Quartz and kaolin-rich sediments.  Overprinted by the "Cordillo Silcrete".  Geological Province:  Eromanga Basin.||||||
6451|Eyre Formation|62376|5|Briefly described|p84|Tertiary|Tertiary |Geological Province: Pedirka Basin.||||||09-FEB-10
6451|Eyre Formation|62724|5|Briefly described|p16 Fig. 2|Tertiary|Tertiary|Sandstone. Geological Province: Curnamona Province.||||||07-FEB-11
6451|Eyre Formation|63102|4|Described|p8,62,67,71,73|Late Eocene|Late Paleocene|Geological province: Curnamona Province. Of Callabonna Sub-basin. Deposited in palaeochannels incised into weathered basement rocks in the area north of the Ranges but occurs as a more widespread sheet facies further to the north. Southern channelled facies sourced from erosion of weather basement rocks in the Olary Domain and is dominated by clay (kaolinite) mineralogy.||||Overlain by Namba Formation.|Carbonaceous sand; very fine to coarse, moderately sorted, subrounded to subangular, with minor clay lenses.|
6451|Eyre Formation|63789|5|Briefly described|Map Legend|Tertiary|Tertiary|Predominatly coarse-grained quartozse sandstone, derived in part fom decayed granites with lesser fine sandstone and fine conglomeratic lenses with highly polished pebbles including fossil wood.||||||
6451|Eyre Formation|63793|5|Briefly described|p30, p49.|Eocene|Paleocene|Earliest Tertiary; apparently locally derived.|||||Soft, white, friable, flat-lying, gritty sandstones.|
6451|Eyre Formation|64047|5|Briefly described|p60, p61|Middle Eocene|Late Paleocene|Broad correlation with Marion Formation is indicated.  Upper section is probably equivalent to Glendower Formation.||||||
6451|Eyre Formation|64197|6|Mentioned|p627, p630 Fig.6|Late Eocene|Late Palaeocene|||||Unconformably overlies the Winton Formation. Is overlain unconformably by Etadunna Formation.||
6451|Eyre Formation|64679|5|Briefly described|Map legend|Tertiary|Tertiary|Quartz sandstone, siltstone, claystone and conglomerate; commonly silicified.||||||11-AUG-09
6451|Eyre Formation|64682|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone and silty or clay rich sandstone.||||||
6451|Eyre Formation|64778|6|Mentioned|p13|Tertiary|Tertiary|Pedirka and Simpson Desert Basins.||||||
6451|Eyre Formation|64964|5|Briefly described|p160|Eocene|Paleocene|Thickness: 80m. Comprises fine-grained brown sandstone and clay with some boulders of Devonian sandstone. No fossils apart from a few worm burrows.||||||08-APR-09
6451|Eyre Formation|65194|5|Briefly described|p44-50|Eocene|Eocene|Fluvial sands. Overlain by Namba Formation. Fining-upward, braided-river sequences of angular, quartz-rich, poorly sorted sands interbedded with kaolinitic clays.||||||
6451|Eyre Formation|65238|5|Briefly described|p7 Fig. 8|Tertiary|Tertiary |Geological province: Eyre Basin. Fluvial and aeolian deposits.||||||
6451|Eyre Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 191 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Winton Formation.|Carbonaceous sandstone, siltstone, mudstone.|
6451|Eyre Formation|65484|5|Briefly described|p 28, 30, Fig 2|Tertiary|Tertiary|Tectonically  tilted exposure, laterally equivalent to sediments hosting Four Mile mineralisation. Later stages include silcrete development.||||||01-MAY-15
6451|Eyre Formation|65489|6|Mentioned|p60|||||||Unconformably overlies Winton Formation.||
6451|Eyre Formation|65925|4|Described| pp16-21, p47-69,  p139, Appendix 2.|Eocene|Latest Paleocene|Callabonna Sub-basin. Organic-rich sands host uranium deposits. Basal unit of Lake Eyre Basin. Fills a network of paleochannels.|Two-stage deposition: c.55-49 Ma and c.45-37 Ma.||Includes Murnpeowie Formation.|Unconformably overlies Bulldog Shale. Is disconformably overlain by Namba Formation.|Pyritic, carbonaceous sand, grain-size ranges from silt to small cobble, with beds of lignite and clay. Clays are montmorillonite, kaolinite and illite. Has silcrete cap. Braided streams.|
6451|Eyre Formation|66131|4|Described|p240-245, p248-253, p255, p258-259|Eocene|Paleocene|Widespread throughout Lake Eyre Basin. Latest Paleocene to Middle Eocene age based on palynological dating. ~100m thick. Plant fossils widespread. Largely deposited by braided streams.||||Correlative of the Glendower and Marion Formations. Equivalent to Mount Sarah Sandstone. Overlain by the Etadunna and Doonbarra Formations. Disconformably overlain by the Namba Formation.|Sandstone, carbonaceous clays and conglomerates. Lignite and clay, sometimes with root horizons, leaf beds and cross-bedding, are common. Diagnostic basal polished gravel.|
6451|Eyre Formation|66303|6|Mentioned|pp27-28, p31 Fig.5.|Paleogene|Paleogene|Lake Eyre Basin. Early Late Paleocene (Lygistepollenites balmei Zone) to Early Oligocene (Upper Nothofagidites asperus Zone). Uplifted, eroded and redeposited from Late Paleocene to Late Eocene. ||||Overlies Bulldog Shale. Is disconformably overlain by Namba Formation.||
6451|Eyre Formation|66518|5|Briefly described|p19 Fig.4, p20.|Cenozoic|Cenozoic|Basal unit in the Callabonna Sub-basin within Lake Eyre Basin. Fluvial sediments and alluvium. ||||Unconformably underlies Namba Formation.||
6451|Eyre Formation|66573|5|Briefly described|p873, p874 Fig.5, p875 Tb.2|Eocene|Paleocene|Disconformably overlain by the Etadunna Formation. Red claystones and silcretized sandstones.||||||
6451|Eyre Formation|66623|3|Fully described|p239, p248, pp268-276.|Eocene|Late Paleocene|Formerly Eyrian Series (Woolnough and David 1926). Equivalent to Glendower and Marion Formations; partly to Mount Sarah and Willalinchina Sandstones. Contains small polished erratic pebbles from underlying Cretaceous sequence. More strongly silicified sandstones are mapped as Cordillo Silcrete. Forms regional angular unconformity over variety of Cretaceous basement rocks. Top of this formation is marked by a palaeosol (Cordillo Surface, Wopnfer 1974) with silcrete cap (Cordillo Silcrete, Wopnfer 1978). Erosion of silcrete cap and Eyre Formation formed the overlying Doonbara Formation.|||In South Australia, incorporates Murnpeowie Formation and Macumba Sandstone.|Locally unconformably overlies Namur Sandstone and Easter Monday Formation. Grades upwards into Cordillo Silcrete. Is overlain unconformably by Doonbara Formation.|Sequence of mature quartz sandstones with local beds and laminae of distinctive and diagnostic, highly glossy, well-rounded, low-sphericity discoidal quartz pebble conglomerate  with subordinate black chert, yellow agate and silicified wood.|30-MAY-13
6451|Eyre Formation|66917|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|66920|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|66921|5|Briefly described|Map legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67119|5|Briefly described|Map legend.|Eocene|Paleocene|Braided stream deposits.|||||Pyritic, carbonaceous sand, silt- to small cobble-sized grains, with beds of lignite and clay (montmorillonite, kaolinite and illite).|
6451|Eyre Formation|67207|5|Briefly described|Map legend.|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|19-SEP-11
6451|Eyre Formation|67208|5|Briefly described|Map legend.|||Shown in Paleogene - Neogene age grouping.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|20-SEP-13
6451|Eyre Formation|67209|5|Briefly described|Map legend.|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67210|5|Briefly described|Map legend.|||Age given as Paleogene-Neogene.||||Overlies Rolling Downs Group.|Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67211|5|Briefly described|Map legend.|||Age stated as Paleogene-Neogene.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|67462|5|Briefly described|Map legend.|Paleogene|Paleogene|Lake Eyre Basin.||||||
6451|Eyre Formation|67562|6|Mentioned|p105 Fig.11|Eocene|Eocene||||||Kaolinitic fine-grained sandstone.|
6451|Eyre Formation|67578|5|Briefly described|p333-334, p336-337, p341-342, p344, p347|Eocene|Paleocene|Birdsville Basin. Multi-channel or braided stream deposits. Upper part widely affected by post-depositional silicification.||||Unconformably overlies Bulldog Shale.|Yellow and yellow-orange cross-bedded sands and thin grey-brown silty-clay.|
6451|Eyre Formation|68068|5|Briefly described|Map legend|Middle Eocene|Late Paleocene|Callabonna Sub-basin, Lake Eyre Basin. Gravel clasts include quartz, chalcedony, silicified wood, silcrete; occasional leaf impressions, often lignitic in drill sections. Commonly silcreted.||||Overlies Mulligan Dam Regolith.|Basal gravel of highly-polished well-rounded clasts, consolidated but not cemented; fluvial quartz sand, rounded to angular, fine- to coarse-grained, grit beds common, occasional laminated lacustrine silt and clay.|
6451|Eyre Formation|68157|6|Mentioned|p1, p13-16|Paleogene|Paleogene|Hosts Four Mile East, Honeymoon and Goulds Dam sandstone-hosted uranium deposits. Includes detrital zircons aged ~1.58 Ga, ~900 Ma and ~485 Ma.|||||Includes coarse-grained sandstone.|
6451|Eyre Formation|68203|6|Mentioned|p9 Fig.6|||Mount Lofty Ranges.||||Is faulted against Willawortina Formation.||
6451|Eyre Formation|68713|6|Mentioned|p23||||||||Fluvial-paludal sediment dominated by fine-grained quartz sand and silt, and has been overprinted by groundwater silcrete.|
6451|Eyre Formation|68715|6|Mentioned|p29, p31, p32 Fig.6|Paleogene|Paleogene|Lake Eyre Basin. Fluvial and aeolian deposits.||||Is overlain unconformably by Namba Formation.||07-APR-17
6451|Eyre Formation|68821|3|Fully described|p296, p297 Fig.3, p307, p310|Lutetian|Danian|< 120 m thick. Fluvial and locally lacustrine sedimentary rocks. Locally abundant wood fragments, and contains large trunks of fossil trees.|62 - 42 Ma|||Locally overlain by the Etadunna Formation and Namba Formation. Unconformably underlain by the Bulldog Shale Formation, Oodnadatta Formation, and Winton Formation.|Includes conglomerate, pyritic mature quartz sandstone with interbeds of clay lenses (44% kaolinite) and shale pebbles, carbonaceous and micaceous siltstone, dolomitic siltstone and lignite.|03-OCT-13
6451|Eyre Formation|69001|5|Briefly described|p2 Fig.1B, p16, p18 Fig.8, p22 p23|Eocene|Paleocene|Late Paleocene to Middle Eocene age. Fluvial sediments. Previously incorrectly correlated with the Gum Vale Beds and Gum Vale Formation.|||||Comprises dominantly fluvial sandstone, carbonaceous clastics and quartzose conglomerates.|
6451|Eyre Formation|69019|4|Described|p83, p94, p104-110 Figs.20,24-26.|Eocene|Paleocene|Of Wopfner et al. (1974) after the term 'Eyrian Series' of Woolnough and David (1926); also previously known as Murnpeowie Formation (Forbes, 1966). Extensive sandy flood plain deposits. Thickness from <10 to >170 m. Has developed silcrete-porcellanite horizons. Of interest to explorers for biogenic coal seam gas. See also Pl.20, p119.||||Disconformably overlies Winton Formation. Is overlain unconformably by Namba and Etadunna Formations. Faulted against Marree Subgroup.|Well-washed, mature, moderately sorted quartz sand; grit beds common; comnmonly carbonaceous and pyritic, with lignite interbeds towards the base.|
6451|Eyre Formation|69023|4|Described|p79, p87, p101, p105-106, p108-120|Eocene|Paleocene|See also p122-123, p125, p143-144, p153, p162-163, p193. Defined by Wopfner et al. (1974); previously Eyrian Series of Woolnough and David (1926), and Murnpeowie Formation of Forbes (1966). Seven reference areas are described in the definition; two are mentioned here. Lake Eyre Basin. c.62m thick. Plant matter is commonly preserved. A measured section is provided. Deposited as a widespread fluvial sand sheet. Weathering has formed porcellanite and a silcrete cap. Probable source (with Namba Formation) of Yandruwantha Sand. Potential supply of construction sand and road gravel. Stratigraphic wells intersection data.||||Conformably overlies Mulligan Dam Regolith. Disconformably overlies Winton Formation or Bulldog Shale. Is overlain unconformably by Namba Formation.|Black, grey and brown coloured. Well-washed, mature, fine- to medium-grained, moderately sorted sand with subrounded grains; commonly carbonaceous and pyritic; interbeds of lignite towards the base. Local silcrete and calcite cemented zones.|
6451|Eyre Formation|69458|5|Briefly described|p42:16|Eocene|Paleocene|Lake Eyre Basin. Extensive shallow, braided stream system deposits with local swamp and lake settings.|||||Basal conglomerate with highly polished, resistant pebble clasts overlain by cross-bedded, mature pyritic and carbonaceous coarse-grained sandstone; lignite and clay units, containing plant fossils, occur.|12-JUL-16
6451|Eyre Formation|69562|5|Briefly described|p662 Tb.2, p663 Fig.2, p664 Tb.4|Eocene|Paleocene|See also p666 Fig.3, p667 Fig.4, p668-669, p674-676, p679-684. Lake Eyre Basin. Deposition in paleovalleys. Hosts more than 90% of known (U) mineralisation in Lake Frome area; highly permeable sands: 5 sq.m/day measured. Rich in organic material (plants and pyrite) for reductants. Electrical conductivity value used in forward modelling: 200-500 mS/m.|c.55 Ma.|||Overlies Marree Subgroup. Is overlain by Namba Formation.|Mature, fine- to coarse-grained, unconsolidated, carbonaceous, pyritic sands; occasional lignitic sandy lenses near the base.|06-APR-22
6451|Eyre Formation|69568|5|Briefly described|p441, 443-444|Eocene|Paleocene|Lake Frome region; basal Lake Eyre Basin. Hosts the Beverley North uranium deposits. Occurs in S-N paleochannels, commonly incised into underlying strata. Two depositional stages: ~55-49 Ma and ~45-37 Ma. Drill-core logs.||||Unconformably overlies Bulldog Shale. Is overlain disconformably by Namba Formation.|Dominantly fluvial and lacustrine deposits, characterised by pyritic carbonaceous mature sands of very fine to pebble size; includes coal seams; regionally capped by silcrete lenses.|
6451|Eyre Formation|69599|5|Briefly described|p584, p599-600|Eocene|Paleocene|Senior (1979) and Senior and Mabbutt (1979) included under this name all Eyre Formation equivalents in the SW corner of QLD; Draper (2002) excepted the Marion Formation. Capped by silcrete and laterite of the Canaway profile.||||Correlated (at least partly) with Moonie, Glendower, Edkins, Springvale and Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.||
6451|Eyre Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
6451|Eyre Formation|69946|5|Briefly described|p29, p125, p129|Eocene|Paleocene|Lake Eyre Basin. Wopfner et al. (1974). Up to 140m thick. Weathering down to 60m. Local Cordillo Silcrete caps produce prominent mesas.|||||Fluvial, fine- to medium-grained quartz sandstone with lignite interbeds and a basal conglomerate which includes reworked Late Cretaceous sediment.|
6451|Eyre Formation|69947|5|Briefly described|p13 Fig.7.2|Eocene|Paleocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
6451|Eyre Formation|69961|5|Briefly described|Map legend|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70383|5|Briefly described|p45, p62|Paleogene|Paleogene|Lake Eyre Basin. Fluvial sediments.||||Is overlain by Namba Formation.||
6451|Eyre Formation|70384|5|Briefly described|Map legend.|Eocene|Paleocene|Callabonna Sub-basin, Lake Eyre Basin. Dominantly a braided stream and floodplain deposit. Palynology age range: late Paleocene to middle Eocene. Rare leaf fossils in silt or clay layers; variably lignitic near base (+/- pyrite). Reddish horizons and silcrete mark paleosols.|||||Quartz sand, rounded to angular, fine- to coarse-grained; grit beds common, cross-bedded channel fill; occasional laminated lacustrine silt and clay; basal gravel with highly polished, well-rounded clasts. Consolidated, rarely cemented.|
6451|Eyre Formation|70649|5|Briefly described|Map Legend|Neogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70651|5|Briefly described|Map Legend|Paleogene|Paleogene||||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70652|5|Briefly described|Map Legend|Paleogene|Paleogene|Fluvial sandstone. In-situ regolith and transported sediments also described.|||||Variably silcrete-altered quartzose sandstone, minor pebbly sandstone and conglomerate; ubiquitous glossy quartz pebbles.|
6451|Eyre Formation|70657|5|Briefly described|p9 Fig.3, p68, p72, p77-80|Neogene|Paleogene|Cover sequence in Olary Domain. Deposition in palaeochannels incised into weathered basement rocks, or as widespread sheet facies. Hosts roll-front U mineralisation (described) near the Benagerie Ridge. Late Eocene to late Paleocene.||||Is overlain by Namba Formation.|Sandstone; carbonaceous sand, fine to coarse, subrounded to subangular, and minor clay (mainly kaolinite) lenses.|
6451|Eyre Formation|70658|6|Mentioned|p14|Tertiary|Tertiary||||||Sandstone.|
6451|Eyre Formation|70821|5|Briefly described|p25|Eocene|Eocene|Previously the Eyre Gravel (eg Lovering et al., 1972) [misquoted as the Eyre gravel in this study]. Lake Eyre Basin (SA). Is equivalent to the dendritic ridges formed by the Glendower Formation in Queensland and NSW.|||||Silcrete and ferricrete.|
6451|Eyre Formation|70823|5|Briefly described|p46-p47|Middle Eocene|Paleocene|Interpreted to have been deposited in a braided stream fluvial setting.|||||Carbonaceous sand, silt and gravel with some lignite and clay beds.|
6451|Eyre Formation|71342|4|Described|Ch1 p6, Ch5 p29, Ch5 p130, Ch7 p13|Eocene|Paleocene|Lake Eyre Basin. Hosts a major confined aquifer. Deposited in a fluvial environment. Up to 140m thick in the Cooper region. ||||Overlain by the Cordillo Silcrete. Unconformably overlies the Winton Formation. Unconformably overlain by the Namba Formation.|Fine to medium-grained, quartz sandstone with lignite interbeds and a basal conglomerate.|
6451|Eyre Formation|71415|5|Briefly described|p11|Neogene|Paleogene|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||||
6451|Eyre Formation|72456|5|Briefly described|Map Legend|Eocene|Paleocene|Marree 1:250k map sheet. Deposited in a braided stream environment.|||||Pyritic, carbonaceous sand, grain-size ranges from silt to small cobble, with bands of lignite and clay. Clays are montmorillite, kaolinite and illite.|
6451|Eyre Formation|72457|5|Briefly described|p91|Eocene|Palaeocene|Callabonna sub-basin.||||Is overlain by Namba Formation.|Fluvial sands and gravels.|
6451|Eyre Formation|72461|6|Mentioned|p24|Cenozoic|Cenozoic|||||||
6451|Eyre Formation|73090|6|Mentioned|p6|Eocene|Palaeocene|||||||
6451|Eyre Formation|73106|5|Briefly described|Map legend.|Eocene|Paleocene||||||Pyritic carbonaceous sand; grain size ranges from silt to small cobble, with beds of lignite and clay. Clays are montmorillonite, kaolinite and illite. Braided streams.|
6451|Eyre Formation|73188|6|Mentioned|p345|Eocene|Paleocene|Similar to North Maslin Sand.||||||
6451|Eyre Formation|73251|4|Described|p36-38, p40-48, p50-51, p53, p56-58, p62|Eocene|Eocene|Lake Eyre Basin (widespread), Callabonna Sub-basin (basal unit). Potential detrital U reductant and potential shallow hydrocarbon source rock. Sandstone hosts U mineralisation at Four Mile East, Goulds Dam, Honeymoon, Oban, and Pepegoona. Thermally sub-mature. Includes oil-prone organic facies. Depositional environments include non-marine, meandering fluvial, fluviolacustrine, peat swamp, and floodplains. Sediment recovery in drill holes was poor, especially where the sands are clean (clay-free). Thickness in drill holes ranges from ca 23 m to 45 m thickening eastwards. Contains Eyre [organic] facies 1, 2, and 3. [See article for organic petrology descriptions].||||Unconformably overlain by Namba Formation.|Amalgamated fine- to medium-grained quartz sandstone (both clean and carbonaceous), lignite and carbonaceous mudstone.|
6451|Eyre Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Welldata.xlsx.||||||
6451|Eyre Formation|73479|5|Briefly described|p156 Fig.2|Paleogene|Paleogene|Lake Eyre Basin.||||Unconformably overlies Winton Formation, underlies Etadunna Formation|Fresh water coarse sand.|
6463|Eyriebower Coal Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Geological Province: Sydney Basin||||||
6463|Eyriebower Coal Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Of Lucernia Coal. Geological Province: Sydney Basin||||||22-OCT-08
6463|Eyriebower Coal Member|29942|6|Mentioned|p11|||||||||
6463|Eyriebower Coal Member|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Lucernia Coal.||Overlies Longford Creek Siltstone. Is overlain by Pinegrove Formation.||
6481|Fairfield Creek Member|33476|6|Mentioned|p33 Table 4|||Of Carpentaria Exploration, in Offenburg & Cochrane (1972) unpub.||||||13-NOV-15
6481|Fairfield Creek Member|39279|4|Described|p370, 368|Late Permian|Late Permian|Compared with Emmaville Volcanics, Dundee Rhyodacite. May be temporal equivalents.||Of Drake Volcanics.|||Well-laminated rhyolitic crystal-lithic tuff.|13-NOV-15
6481|Fairfield Creek Member|40505|6|Mentioned|p83|||||||||
6481|Fairfield Creek Member|40773|6|Mentioned|p462|||||||||
6481|Fairfield Creek Member|42378|6|Mentioned|Table 1 p10|||||Of Drake Volcanics.||||13-NOV-15
6491|Fairford Formation|40805|2|Defined|p138|Permian|Permian|||||||
6491|Fairford Formation|41010|6|Mentioned|Fig.2|||||||||
6491|Fairford Formation|42078|6|Mentioned|Table 1 P5|||||||||
6491|Fairford Formation|42648|6|Mentioned|p37|||||||||
6491|Fairford Formation|42922|6|Mentioned|Fig.14|||||||||
6491|Fairford Formation|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Jerrys Plains Subgroup (Wittingham Coal Measures).   Overlies the Burnamwood Formation.||||||
6491|Fairford 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.||||||
6491|Fairford Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. Overlies a consistently dulling section of the Mount Arthur seam (Burnamwood Formation). About 2 m thick; occurs throughout most of the Coalfield.||Unit in Jerrys Plains Subgroup.||Overlies Burnamwood Formation. Is overlain by Mount Thorley Formation.|A distinctive off-white tuffaceous claystone to lithic (volcanigenic) sandstone.|
6491|Fairford Formation|69683|6|Mentioned|p411 Fig.2, p415-416 Fig.3|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.||||
6491|Fairford Formation|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. CA-TIMS ages of 257.04 and 257.43 Ma (Metcalfe etal., 2015). Corresponding to APP5 zone (Lopingian).||Unit of Wittingham Coal Measures.||||
6491|Fairford Formation|70878|5|Briefly described|p710, p712, p723, p725|Permian|Permian|Hunter Valley. 4.55m thick in Amoco Wybong 1 well. Calibration of palynological ages (D. parvithola Zone).|257.43 +/- 0.09 Ma.|Wittingham Coal Measures.|||Includes tuff layers.|
6491|Fairford Formation|73304|5|Briefly described|p65-67, p75|Wuchiapingian|Wuchiapingian|Dating by U-Pb CA-TIMS method.|257.43 +/- 0.31, 257.04 +/- 0.31 Ma|Jerrys Plains Subgroup, Whittingham Coal Measures, Singleton Supergroup||||
6504|Fairy Meadow Limestone Member|22857|5|Briefly described|p474 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the De Drack Formation. Contains corals.Max. thickness: >10m.||||||24-MAR-06
6504|Fairy Meadow Limestone Member|30735|2|Defined|p20|Silurian|Silurian|||||||
6504|Fairy Meadow Limestone Member|30736|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
6504|Fairy Meadow Limestone Member|35503|6|Mentioned|p202|||Redefined in Felton and Huleatt (1977)||||||
6504|Fairy Meadow Limestone Member|40328|6|Mentioned|p184|||||||||
6504|Fairy Meadow Limestone Member|68592|5|Briefly described|p760, p725 Fig.130|||Defined on Braidwood 1:100 000; Felton and Huleatt (1977).||Unit in De Drack Formation.|||Limestone.|
6526|Farley Formation|22601|6|Mentioned|410, 411|Permian|Permian|Geol Province: Sydney Basin. Overlying unit Greta Coal Measures.||||||05-AUG-08
6526|Farley Formation|22610|5|Briefly described|Fig 1|||Maximum thickness 300m.||||||05-AUG-08
6526|Farley Formation|22663|5|Briefly described|NSW97 - 1 p2||Early Permian|||||||01-MAR-10
6526|Farley Formation|22857|5|Briefly described|p522 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Silty sandstone. Max. thickness: 300m. Geological Province: Sydney Basin.||||||
6526|Farley Formation|22969|4|Described|p 18, Fig 2.2||Early Permian|||||||
6526|Farley Formation|22970|5|Briefly described|Plate 6|||||||||
6526|Farley Formation|23350|5|Briefly described|262|Early Permian|Early Permian|||||||
6526|Farley Formation|23540|4|Described|p 419|||Of the Dalwood Group. Also see Fig 2 p 419||||||20-FEB-07
6526|Farley Formation|24079|5|Briefly described|p432|Permian|Permian|Of Dalwood Group.  Geological Province: Sydney Basin. Maximum thickness: 300m.||||||05-AUG-08
6526|Farley Formation|24121|5|Briefly described|p4, p108|||Of Dalwood Group.||||||25-AUG-22
6526|Farley Formation|29437|6|Mentioned|p136|||Permian||||||
6526|Farley Formation|29441|6|Mentioned|p113|||||||||
6526|Farley Formation|29752|6|Mentioned|p34|||||||||
6526|Farley Formation|29915|6|Mentioned|p68|||||||||
6526|Farley Formation|30153|6|Mentioned|p151|||Fauna correlates with that of Cascades Group||||||
6526|Farley Formation|30340|6|Mentioned|Table 3|||||||||
6526|Farley Formation|30341|6|Mentioned|p136|||Lower Permian age||||||
6526|Farley Formation|30442|6|Mentioned|p24|||||||||
6526|Farley Formation|30450|6|Mentioned|Table 1|||Permian age. Sydney Basin.||||||05-AUG-08
6526|Farley Formation|30545|6|Mentioned|Fig.2|||Lower Permian. See also p24.||||||20-AUG-18
6526|Farley Formation|31081|6|Mentioned|p61|||See also P65, Fig. 2||||||
6526|Farley Formation|31883|6|Mentioned|Table 1|||||||||
6526|Farley Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis branxtonensis||||||
6526|Farley Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
6526|Farley Formation|32672|6|Mentioned|p675|||||||||
6526|Farley Formation|32840|6|Mentioned|Table 1|||||||||
6526|Farley Formation|32943|6|Mentioned|p87|||See also P105||||||
6526|Farley Formation|32945|6|Mentioned|p83|||See also p88 & Fig.1.||||||20-AUG-18
6526|Farley Formation|32946|6|Mentioned|p910|||Fossil||||||
6526|Farley Formation|32950|6|Mentioned|Table 31.1|||||||||
6526|Farley Formation|33334|6|Mentioned|Fig.6|||||||||
6526|Farley Formation|33701|6|Mentioned|p600|||Artinskian.See also Fig.1.||||||
6526|Farley Formation|33702|6|Mentioned|p223|||Trilobites||||||
6526|Farley Formation|33711|6|Mentioned|p382|||Table 2||||||
6526|Farley Formation|33867|5|Briefly described|p5|||||||||
6526|Farley Formation|34043|6|Mentioned|p449|||||||||
6526|Farley Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
6526|Farley Formation|34170|6|Mentioned|p47|||Lower Permian||||||
6526|Farley Formation|34292|6|Mentioned|Table 1|||Permian||||||
6526|Farley Formation|34444|6|Mentioned|Map legend|Permian|Permian|||||||
6526|Farley Formation|34445|3|Fully described|p322|||||||||
6526|Farley Formation|34447|5|Briefly described|p318|||Fossils. See also Fig.5.2||||||
6526|Farley Formation|34448|6|Mentioned|p431|||Permian||||||
6526|Farley Formation|34512|6|Mentioned|p52|||||||||
6526|Farley Formation|35284|6|Mentioned|Fig.1|||||||||
6526|Farley Formation|35862|6|Mentioned|p262|||||||||
6526|Farley Formation|36042|6|Mentioned|Table 1|||||||||
6526|Farley Formation|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
6526|Farley Formation|37065|6|Mentioned|p32|||||||||
6526|Farley Formation|37082|6|Mentioned|p161|||||||||
6526|Farley Formation|37086|6|Mentioned|p183|||||||||
6526|Farley Formation|37087|6|Mentioned|p192|||||||||
6526|Farley Formation|38204|6|Mentioned|p77|||||||||
6526|Farley Formation|38586|6|Mentioned|p29|||||||||
6526|Farley Formation|38656|5|Briefly described|Fig.1.5.13|||p280.||||||20-AUG-18
6526|Farley Formation|38820|6|Mentioned|p180|||||||||
6526|Farley Formation|38917|6|Mentioned|p169|||||||||
6526|Farley Formation|39262|6|Mentioned|p124|||||||||
6526|Farley Formation|39287|6|Mentioned|p20|||See also Fig.2.5||||||
6526|Farley Formation|39288|4|Described|p59|||||||||
6526|Farley Formation|39304|6|Mentioned|p364|||Fauna.See also Fig. 19.2||||||
6526|Farley Formation|39307|6|Mentioned|p438|||Foraminifera||||||
6526|Farley Formation|40093|6|Mentioned|p37|||||||||
6526|Farley Formation|40166|6|Mentioned|p345|||See also P343, Table 1 and Fig.2||||||
6526|Farley Formation|40636|6|Mentioned|p43|||||||||
6526|Farley Formation|40997|6|Mentioned|p413|||||||||
6526|Farley Formation|41315|6|Mentioned|p149|||||||||
6526|Farley Formation|41514|6|Mentioned|p79|||||||||
6526|Farley Formation|41580|6|Mentioned|Table 1|||||||||
6526|Farley Formation|41902|5|Briefly described|p5 Table 1|||||||||
6526|Farley Formation|42250|6|Mentioned|p26|||||||||
6526|Farley Formation|42925|5|Briefly described|Table 1||Early Permian|||||||
6526|Farley Formation|43017|5|Briefly described|Fig.1,p372|||||||||
6526|Farley Formation|43018|5|Briefly described|Table 1,p386|||||||||
6526|Farley Formation|43050|5|Briefly described|p9|||||||||
6526|Farley Formation|43194|5|Briefly described|p129 Tb. 8.3|Early Permian|Early Permian|Of Gyarran Volcanics (Hunter region) and Dalwood Group (Newcastle region), Sydney Basin.||||||
6526|Farley Formation|43257|5|Briefly described|Map Legend||Early Permian|Of Dalwood Group.||||||
6526|Farley Formation|43344|14|Not recorded|p84||Permian|||||||
6526|Farley Formation|43385|14|Not recorded|p179,180|||Newcastle SI56-2, Singleton SI56-1||||||
6526|Farley Formation|43440|14|Not recorded|p32,36,64,74,91|||||||||
6526|Farley Formation|43447|14|Not recorded|p16,17||Permian|||||||
6526|Farley Formation|43448|14|Not recorded|p224,229||Permian|Unit of Dalwood Group||||||
6526|Farley Formation|43471|14|Not recorded|p229,239-241,251|||Megadesmus, Astartila||||||
6526|Farley Formation|43474|14|Not recorded|p7,25,53,55,61,69-71||Artinskian|p102,22||||||
6526|Farley Formation|43475|14|Not recorded|p553||Permian|||||||
6526|Farley Formation|43479|14|Not recorded|p186,218||Artinskian|||||||
6526|Farley Formation|43882|14|Not recorded|p87-90,92|||Permian ammonoids.||||||
6526|Farley Formation|44040|14|Not recorded|p27|||||||||
6526|Farley Formation|44219|14|Not recorded|p29,31-33,37||Artinskian|||||||
6526|Farley Formation|44244|6|Mentioned|p230|||||||||
6526|Farley Formation|44372|6|Mentioned|p43|||||||||
6526|Farley Formation|44378|14|Not recorded|p201|Artinskian|Sakmarian|Uraloceras pokolbinense. (Late Sakmarian-Early Artinskian)||||||
6526|Farley Formation|44379|14|Not recorded|p19|||||||||
6526|Farley Formation|44855|14|Not recorded|p18|Permian|Carboniferous|||||||
6526|Farley Formation|45006|14|Not recorded|Tb.1,p6,78,114,126|||||||||
6526|Farley Formation|45016|14|Not recorded|p.72|||Tb. at back. Correlated with Callytharra Formation.||||||
6526|Farley Formation|45090|6|Mentioned|p7|||Time correlation chart. Isopach map P34.||||||
6526|Farley Formation|47041|6|Mentioned|Fig.2|||||||||
6526|Farley Formation|48926|6|Mentioned|p52|||P52 et seq.||||||24-FEB-10
6526|Farley Formation|49644|5|Briefly described|Table|||||||||
6526|Farley Formation|60281|5|Briefly described|p56|Early Permian|Early Permian|Included in the Upper Dalwood Group. Consists of pro-deltaic, fossiliferous silty sandstone becoming coarser northwards.  Age: 275-274Ma.  Thickness at type section: 300m.  Geological Province: Sydney Basin.||||||
6526|Farley Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: Sydney Basin/ Newcastle area.||||||
6526|Farley Formation|61612|6|Mentioned|p270, p276, p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||13-MAR-09
6526|Farley Formation|63172|6|Mentioned|p305|||In NSW.||||||07-FEB-11
6526|Farley Formation|63832|6|Mentioned|p131 Fig.2|Artinskian|Artinskian|NE Sydney Basin. Sixth (P2) glaciation.||||||
6526|Farley Formation|68003|5|Briefly described|p38 Fig.3-j.|Early Permian|Early Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Unit in Dalwood Group.||Overlies Rutherford Formation. Is overlain by Skeletar Formation.||
6526|Farley Formation|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields.||Unit in Dalwood Group.||Overlies Rutherford Formation. Is overlain by Skeletar Formation.||
6526|Farley Formation|68493|5|Briefly described|p3 Fig.1, p5 Fig.2, p6, p12, p21|Cisuralian|Cisuralian|Sydney Basin. Approximately 300m thick. Depositional environment below wave base. Deposited during Fielding et al.'s (2008) glacial episode P2.||Topmost unit of the Dalwood Group.|Includes Ravensfield Sandstone Member.|Overlies the Rutherford Formation.|Contains moderately abundant, mostly fragmentary, abraded and disarticulated fossils within a coarsening-upward sequence of silty sandstone.|
6526|Farley Formation|69297|6|Mentioned|p501, p502 fig 5.43|Kungurian|Artinskian|Sydney Basin. ||Dalwood Group||Overlies the Rutherford Formation. Overlain by the Greta Coal Measures.||
6526|Farley Formation|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|||Unit in Gyarran Volcanics.||||
6526|Farley Formation|70096|5|Briefly described|p221;Supp2-3|||Of northern Sydney Basin. See also supplementary files in appendix for additional stratigraphic and locality information.||Unit of Dalwood Group.||Overlain by Millfield Farm member.||
6526|Farley Formation|73304|6|Mentioned|p75|||||Gyarran Volcanics||||
6531|Farnell Group|22553|5|Briefly described|p77|||Part of the Adelaidean sequence.||||||11-SEP-07
6531|Farnell Group|22646|6|Mentioned|Fig 4 on p 102||Neoproterozoic|Adelaide Geosyncline (East).  Age - Ediacarian in text.||||||
6531|Farnell Group|22772|4|Described|p63,66,Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
6531|Farnell Group|22857|5|Briefly described|p63, p66, Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Geological Province: Adeliade Fold Belt. See also p400 App. 1 Tb.A1.3.||||||
6531|Farnell Group|22858|5|Briefly described|p92||Neoproterozoic|||||||
6531|Farnell Group|30261|4|Described|Table 1|||Marinoan||||||
6531|Farnell Group|31012|6|Mentioned|p8|||Adelaidean. Lithology.||||||
6531|Farnell Group|32671|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6531|Farnell Group|33004|6|Mentioned|p136|||||||||
6531|Farnell Group|34812|4|Described|p100|||||||||
6531|Farnell Group|34814|6|Mentioned|Fig.2|||||||||
6531|Farnell Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6531|Farnell Group|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
6531|Farnell Group|37931|6|Mentioned|p531|||||||||
6531|Farnell Group|38157|6|Mentioned|p265|||||||||
6531|Farnell Group|39214|5|Briefly described|p9|||Table 1||||||
6531|Farnell Group|39885|6|Mentioned|p427|||||||||
6531|Farnell Group|40595|6|Mentioned|p92|||||||||
6531|Farnell Group|41429|6|Mentioned|p245|||||||||
6531|Farnell Group|41801|6|Mentioned|p216|||||||||
6531|Farnell Group|42982|5|Briefly described|Table 1,p333|||||||||
6531|Farnell Group|43263|6|Mentioned|Map Legend||Neoproterozoic|||||||
6531|Farnell Group|44093|5|Briefly described|p139 App. 1|Early Paleozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt.||||||07-NOV-08
6531|Farnell Group|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Siltstone and sandstone with minor carbonates. South Australian equivalent is Wilpena Group.||||||10-SEP-07
6531|Farnell Group|66623|3|Fully described|p v, p13, p18. |||The uppermost division of the Adelaide Supergroup. West of the Grey Range Group and correlative of Kara Formation: shallow marine setting and transitional alkaline volcanic rocks. Contains stromatolites. Correlative of Wilpena Group.||Unit in Adelaide Supergroup.|Includes Mantappa Dolomite, Picnic Creek Basalt, Faraway Hills and Camels Hump Quartzites, Sturts Meadows Siltstone, Fowlers Gap and Lintiss Vale Formations.|Overlies (conformably) the Teamsters Creek Subgroup of the Torrowangee Group.||
6531|Farnell Group|67105|5|Briefly described|p654, 659, 663|Adelaidean|Adelaidean|Shares close geochemical affinities with the Mount Arrowsmith Volcanics.||||Equivalent to the Grey Range Group and Mount Arrowsmith Volcanics.|Basaltic rocks.|
6531|Farnell Group|70000|5|Briefly described|p32, p34, p40|Ediacaran|Ediacaran|Represents deposition, by marine transgression followed by regression, on a stable shelf environment.|||Includes Mantappa Dolomite; Sturts Meadows Siltstone; Faraway Hills and Camels Hump Quartzites; Fowlers Gap and Lintiss Vale Formations.||Grades from basal cap dolomite, through a thick siltstone-rich package into an upwards-coarsening sequence of quartzite and sandstone.|
6531|Farnell Group|70015|5|Briefly described|Map legend|Ediacaran|Ediacaran|Mineral deposits (if any) are shown.|||Includes Mantappa Dolomite; Sturts Meadows Siltstone; Faraway Hills and Camels Hump Quartzites; Fowlers Gap and Lintiss Vale Formations.|Overlies Torrowangee Group.||
6531|Farnell Group|73512|6|Mentioned|p2|||||||||
6531|Farnell Group|74367|6|Mentioned|p18|||Upper most division of the NSW component of the Adelaide Supergroup. Interpreted as the stratigraphic equivalent of the Grey Range Group.||||||
6536|Farquhar Limestone Member|23309|5|Briefly described|p86, 95|Early Silurian|Early Silurian|||Towanga Sandstone||||31-OCT-14
6536|Farquhar Limestone Member|23710|5|Briefly described|p70|||||||||
6536|Farquhar Limestone Member|24551|6|Mentioned|p614||Late Llandovery|Of the Towanga Formation||||||
6536|Farquhar Limestone Member|37727|5|Briefly described|p49|||See also P19.||||||
6536|Farquhar Limestone Member|39447|6|Mentioned|p9|||||||||
6536|Farquhar Limestone Member|40328|6|Mentioned|p71|||||||||
6550|Fassifern Coal|22578|6|Mentioned|Fig.9 p399, p402|||||||||
6550|Fassifern Coal|23055|6|Mentioned|p1,Fig4p11|||||||||
6550|Fassifern Coal|23438|6|Mentioned|p25|||||||||
6550|Fassifern Coal|23717|5|Briefly described|p118 Fig 2|Permian|Permian|Parent: Boolaroo Formation. Geological Province: Sydney Basin||||||
6550|Fassifern Coal|24158|5|Briefly described|p173 Fig.4|Late Permian|Late Permian|Geological Province: Sydney Basin||||||
6550|Fassifern Coal|31549|6|Mentioned|p159|||||||||
6550|Fassifern Coal|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
6550|Fassifern Coal|34270|5|Briefly described|p254|||Refers David (1907)||||||
6550|Fassifern Coal|36327|6|Mentioned|p8|||||||||
6550|Fassifern Coal|39308|6|Mentioned|Fig. 23.4|||||||||
6550|Fassifern Coal|39609|6|Mentioned|Table 1|||||||||
6550|Fassifern Coal|39666|6|Mentioned|Table 20|||||||||
6550|Fassifern Coal|40516|6|Mentioned|p395|||||||||
6550|Fassifern Coal|41226|6|Mentioned|Fig.12|||||||||
6550|Fassifern Coal|41463|6|Mentioned|Fig.1|||||||||
6550|Fassifern Coal|41477|6|Mentioned|p79|||||||||
6550|Fassifern Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Fassifern coal seam instead, and is now included in the Boolaroo Formation. See also p113.||Of Moon Island Beach Subgroup||||
6550|Fassifern Coal|73304|6|Mentioned|p75|||||Boolaroo Formation, Newcastle Coal Measures||||
6555|Faulkland Formation|22857|4|Described|p510 App.1 Tb.A1.8|Namurian|Visean|Massive red and grey lithic arenite; shell banks. Locally richly fossiliferous. Max. thickness: 750m.||||||
6555|Faulkland Formation|32324|6|Mentioned|Table 8.1|||||||||
6555|Faulkland Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
6555|Faulkland Formation|32868|6|Mentioned|p200|||||||||
6555|Faulkland Formation|35492|6|Mentioned|p141|||||||||
6555|Faulkland Formation|35856|6|Mentioned|Fig.1|||||||||
6555|Faulkland Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
6555|Faulkland Formation|36528|6|Mentioned|p179|||||||||
6555|Faulkland Formation|36599|6|Mentioned|Fig.1|||||||||
6555|Faulkland Formation|40883|6|Mentioned|p8|||||||||
6555|Faulkland Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Tamworth Belt.||||||16-DEC-04
6555|Faulkland Formation|42547|4|Described|p36|||||||||
6555|Faulkland Formation|44093|5|Briefly described|p230 App. 1|Late Devonian|Late Devonian|Geological Province: New England Fold Belt.||||||08-MAR-05
6555|Faulkland Formation|44244|2|Defined|p146|Namurian|Visean|Conformably overlies Berrico Creek Formation; conformably underlies Booral Formation.   Max. thickness: >750m.  Type section in text.  Geological Province: Myall Block.||||||
6555|Faulkland Formation|50147|5|Briefly described|Map legend|Namurian|Visean| Geological Province: Western Myall Block.||||||
6555|Faulkland Formation|63832|6|Mentioned|p131 fig 2|Visean|Visean|Western Myall block, Southern New England Fold Belt.||||||
6555|Faulkland Formation|64631|6|Mentioned|p44 Fig.2.|Serpukhovian|Visean|Southern New England Fold Belt, western Myall Block. Biostratigraphic age control at base and top.||||||
6555|Faulkland Formation|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Visean|Myall Block, Tamworth Belt.||||||
6594|Fern Valley Coal|22578|6|Mentioned|Fig.9 p399|||||||||
6594|Fern Valley Coal|23055|6|Mentioned|Fig5p12,15,18|||||||||
6594|Fern Valley Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Of Adamstown Formation.   Geological Province: Sydney Basin||||||28-OCT-08
6594|Fern Valley Coal|39308|6|Mentioned|p467|||||||||
6594|Fern Valley Coal|39609|6|Mentioned|Table 1|||||||||
6594|Fern Valley Coal|40516|6|Mentioned|p395|||||||||
6594|Fern Valley Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Fern Valley coal seam instead. See also p113.||Of Adamstown Subgroup||||
6594|Fern Valley Coal|73304|6|Mentioned|p75|||||Adamstown Formation, Newcastle Coal Measures||||
6600|Ferndale Conglomerate Member|29922|6|Mentioned|Table 49|||||||||
6600|Ferndale Conglomerate Member|29926|6|Mentioned|Fig.3|||Permian||||||
6600|Ferndale Conglomerate Member|34351|6|Mentioned|Fig.5.13|||||||||
6600|Ferndale Conglomerate Member|37083|6|Mentioned|p164|||||||||
6600|Ferndale Conglomerate Member|39287|6|Mentioned|Fig. 2.16|||||||||
6600|Ferndale Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
6600|Ferndale Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
6600|Ferndale Conglomerate Member|43447|14|Not recorded|diag.p26,34|||Part of Lambton Sub-Group||||||
6600|Ferndale Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Tighes Hill Formation||||
6647|Figtree Coal Member|29900|5|Briefly described|p168|||||||||
6647|Figtree Coal Member|29901|4|Described|Table 1|||||||||
6647|Figtree Coal Member|30006|6|Mentioned|p7|||||||||
6647|Figtree Coal Member|31128|6|Mentioned|Table 1|||||||||
6647|Figtree Coal Member|33869|6|Mentioned|Fig.2|||||||||
6647|Figtree Coal Member|36220|6|Mentioned|p38|||See also Table 10 & P38.||||||
6647|Figtree Coal Member|37089|6|Mentioned|p208|||||||||
6647|Figtree Coal Member|39661|6|Mentioned|Fig.1|||||||||
6647|Figtree Coal Member|42182|5|Briefly described|p300|||||||||
6647|Figtree Coal Member|42787|6|Mentioned|Table 1 P126|||||||||
6647|Figtree Coal Member|45090|6|Mentioned|p219|||L.Tatarian||||||
6647|Figtree Coal Member|71115|5|Briefly described|p180|Permian|Permian|Southern Sydney Basin.||Pheasants Nest Formation.||Overlies Unanderra Coal Member.||
6655|Finister Granodiorite|22815|4|Described|p54||Silurian|Rb/Sr Ages: 421.5 Ma to 415.9 Ma. 207Pb/206Pb Age: 440Ma.||||||
6655|Finister Granodiorite|33852|6|Mentioned|p502|||Date given.||||||
6655|Finister Granodiorite|38327|6|Mentioned|Table 4|||||||||
6655|Finister Granodiorite|38500|4|Described|p93|||||||||
6655|Finister Granodiorite|39721|6|Mentioned|Table 1|||||||||
6655|Finister Granodiorite|40328|4|Described|p205|||||||||
6655|Finister Granodiorite|41133|6|Mentioned|p1118|||||||||
6655|Finister Granodiorite|41905|2|Defined|p36|Late Silurian||||||||
6655|Finister Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
6655|Finister Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Berridale Batholith.||||||
6655|Finister Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh18||||||
6655|Finister Granodiorite|49705|6|Mentioned|p42|||||||||
6655|Finister Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
6655|Finister Granodiorite|73154|5|Briefly described|p77, p78 Tb.1, p79, p83-84, p89 Tb.2|Wenlock|Llandovery|Lachlan Orogen. Nominally I-type, has S-type characteristics. Comprises a small lozenge-shaped pluton in the southern part of the Berridale Batholith, oldest phase of the Berridale Batholith, separates dominantly S-type granitic intrusives to the west from younger I-type granitic rocks to the east. Location in text includes p81.|433.6+/-2.7 Ma zircon U-Pb, 436+/-5 Ma SHRIMP U-Pb||||Hornblende-bearing granitic batholith. Includes medium, even-grained dark grey rock, with blocky plagioclase laths in poikilitic orthoclase, reddish brown biotite and ragged hornblende prisms, some partially replaced by biotite aggregates.|
6656|Finister Suite|22719|6|Mentioned|p485|||||||||
6656|Finister Suite|22815|6|Mentioned|p54|Early Devonian|Silurian|||||||
6656|Finister Suite|41905|6|Mentioned|p36|||||||||
6656|Finister Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
6656|Finister Suite|42726|5|Briefly described|map legend||Silurian|||||||
6656|Finister Suite|43233|5|Briefly described|Map Legend|Late Silurian||of Berridale Batholith.||||||
6656|Finister Suite|44093|5|Briefly described|p190 App. 1|Early Devonian|Silurian|||||||
6656|Finister Suite|72571|6|Mentioned|p90, p99|||Of the Tasmanides of eastern Australia. I-type.||||||
6710|Five Islands Latite Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
6710|Five Islands Latite Member|22488|5|Briefly described|p840-2|||||||||
6710|Five Islands 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.||||||
6710|Five Islands Latite Member|23544|5|Briefly described|Fig 2 p358|||In the Gerringong Volcanics||||||
6710|Five Islands Latite Member|38690|4|Described|p293|||||||||
6710|Five Islands Latite Member|40270|6|Mentioned|Table 1|||||||||
6710|Five Islands Latite Member|67500|5|Briefly described|p12 Tb.1 |||||Of the Pheasants Nest Formation and Gerringong volcanic facies|||Fine-grained pillowed flow.|
6710|Five Islands Latite Member|71115|5|Briefly described|p180, 182, 188|Permian|Permian|Southern Sydney Basin.||Gerringong Volcanics Pheasants Nest Formation).||Overlies Cambewarra Latite Member. Is overlain by Calderwood Latite Member.|Basaltic andesite.|
6710|Five Islands 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.|
6721|Flagstaff Formation|22500|6|Mentioned|p 7|||||||||
6721|Flagstaff Formation|22857|4|Described|p241, p510 App.1 Tb.A1.8|Visean|Visean|Conformably overlain by Gilmore Volcanic Group; conformably overlies Bonnington Siltstone. Geological Province: Kullatine-Yagon-Booral Shelf and Tamworth Forearc Basin.||||||
6721|Flagstaff Formation|22863|6|Mentioned|p241|||||||||
6721|Flagstaff Formation|24121|6|Mentioned|p4, p80, p86, p129|||||||||25-AUG-22
6721|Flagstaff Formation|30074|6|Mentioned|p25|||||||||
6721|Flagstaff Formation|31519|6|Mentioned|Fig. 1|||||||||
6721|Flagstaff Formation|32324|6|Mentioned|Table 8.1|||||||||
6721|Flagstaff Formation|33728|6|Mentioned|p50|||||||||
6721|Flagstaff Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
6721|Flagstaff Formation|37068|6|Mentioned|p58|||See also P60.||||||
6721|Flagstaff Formation|39979|6|Mentioned|p62|||||||||
6721|Flagstaff Formation|40883|6|Mentioned|p7|||||||||
6721|Flagstaff Formation|42547|4|Described|p29|||||||||
6721|Flagstaff Formation|43576|6|Mentioned|p347|||||||||
6721|Flagstaff Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
6721|Flagstaff Formation|44093|5|Briefly described|p229 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
6721|Flagstaff Formation|44244|2|Defined|p63|Visean|Visean|Previously "Flagstaff Sandstone".  Includes 7 members and the Verulam Oolite Member of the Wootton beds.  Conformably overlies Bonnington Siltstone; conformably underlies Chichester Fm. and Gilmore Volcanic Gp; also underlies Nerong Volcanics, Conger Fm.||||||18-AUG-04
6721|Flagstaff Formation|46803|6|Mentioned|p148|||||||||
6721|Flagstaff Formation|47056|6|Mentioned|Fig.2 P523|||||||||
6721|Flagstaff Formation|50147|5|Briefly described|Map legend|Visean|Visean|Sandstone, mudstone and conglomerate and minor oolitic, skeletal and coralline limestone.||||||
6721|Flagstaff Formation|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Gresford Block.  Includes: Allyn River Member, Cuygallon Volcanic Member, Mount Rivers Ignimbrite Member.  Underlies: Martins Creek Ignimbrite Member, Wallaringa Formation.||||||
6721|Flagstaff Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Gresford Block, Tamworth Belt.|||Includes Allyn River Member.|||
6721|Flagstaff Formation|71628|6|Mentioned|p6:22|||||Gilmore Volcanic Group.||||
6764|Floods Creek Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
6764|Floods Creek Formation|22857|5|Briefly described|Tb 13.1 (insert p70), p400 App.1 Tb A1.3|Marinoan|Marinoan|Of the Eurowie Subgroup (Torrowangee Group). Calcareous sandstone, interbedded grey-green siltstone. Age: <700Ma. Max. thickness: 1070m. Geological Province: Adelaide Fold Belt. ||||||
6764|Floods Creek Formation|30261|4|Described|Table 1|||Marinoan age||||||
6764|Floods Creek Formation|34812|3|Fully described|p79|||||||||
6764|Floods Creek Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6764|Floods Creek Formation|36411|6|Mentioned|p268|||Refs Cooper et al. 1978 for definition.||||||
6764|Floods Creek Formation|36733|6|Mentioned|Table 5|||||||||
6764|Floods Creek Formation|37931|4|Described|p534|||||||||
6764|Floods Creek Formation|39214|5|Briefly described|p7|||||||||
6764|Floods Creek Formation|41405|5|Briefly described|p204|||||||||
6764|Floods Creek Formation|46889|6|Mentioned|p272|||||||||
6764|Floods Creek Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Euriowie Subgroup.||||
6764|Floods Creek Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Euriowie Subgroup.||Overlies Corona Dolomite and Mitchie Well Formation.|Calcareous sandstone and interbedded grey-green siltstone.|08-SEP-15
6774|Florida Volcanics|22768|6|Mentioned|p170|||||||||
6774|Florida 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: 1km. Geological Province: Kopyje Shelf (Darling Basin).||||||
6774|Florida Volcanics|23171|5|Briefly described|p15,31,Fig9p34|||||||||
6774|Florida Volcanics|23173|4|Described|Map Legend|Lochkovian|Lochkovian|||||||
6774|Florida Volcanics|35219|6|Mentioned|p16|||||||||
6774|Florida Volcanics|35287|6|Mentioned|p7|||||||||
6774|Florida Volcanics|39618|3|Fully described|p62|||||||||
6774|Florida Volcanics|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
6774|Florida Volcanics|41528|6|Mentioned|p17|||||||||
6774|Florida Volcanics|42566|6|Mentioned|p47|||||||||
6774|Florida Volcanics|42726|5|Briefly described|map legend|||||||||
6774|Florida Volcanics|46900|6|Mentioned|Fig.2|||Stratigraphic table||||||
6774|Florida Volcanics|65469|5|Briefly described|p15, p17|Early Devonian|Late Silurian|Lachlan Orogen.||Kopyje Group||||
6774|Florida Volcanics|67416|6|Mentioned|p85|||Canbelego-Mineral Hill Volcanic Belt.|||||I-type.|
6774|Florida Volcanics|69801|6|Mentioned|p1, p11, p135|Silurian|Silurian|Cobar Basin. Date provided is a U-Pb SHRIMP age.|421.7 +/- 2.3 Ma (Black, 2005)|||Interfingers with the Baledmund Formation.||
6774|Florida Volcanics|70210|6|Mentioned|p38|||Mentioned in a previous (2004/05) Report.||||||
6774|Florida Volcanics|70296|5|Briefly described|p1, p8, p10-11, p24|Ludlow|Ludlow|Cobar district. Has an inherited component ranging in age from 470 Ma-1050 Ma.|421.7 +/- 2.3 Ma (SHRIMP U-Pb)|||||21-JAN-21
6774|Florida Volcanics|70751|6|Mentioned|p11, p17, p21-p22||||421.7 +/- 2.3 Ma (SHRIMP U-Pb, Black, 2005)|Kopyje Group||Interfingers with the Baledmund Formation.||
6774|Florida Volcanics|70876|5|Briefly described|p9, p76|||Lachlan Orogen.||Kopyje Group|||Felsic, I-type volcanics.|
6774|Florida Volcanics|70941|6|Mentioned|pviii, px, p78, p78 fig 32, P152|||Eruption age. |421.7 +/- 2.3 Ma (Black, 2005)|||Interfingers and partly overlies the Baledmund Formation||
6774|Florida Volcanics|71039|5|Briefly described|p11-p12, p25|Devonian|Silurian|Consistently preserve zeolite to epizone greenschist facies rift basin metamorphic mineral assemblages. Many samples are partly recrystallised and hydrated.||Kopyje Group||||
6774|Florida Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|Lithologies are described in more detail.||Kopyje Group.|||Coherent lavas zoned from rhyolitic base to dacitic top with intercalated volcaniclastics.|
6774|Florida Volcanics|73174|4|Described|p1035-1041, p1043-1046|Lochkovian|Lochkovian|Kopyje Shelf. I-type. Less than 1 km thick. Distributed across ~50 km2. Interpreted as deposited over a short time period in a shallow marine to possible terrestrial environment. Geochron are magmatic ages from LA-ICP-MS (herein) and SHRIMP (Black, 2005).|415.6 +/- 3.6 Ma, 421.5 +/- 2.3 Ma|Kopyje Group, Cobar Supergroup||Equivalent to[?] Mount Boppy Conglomerate.|Coarse-grained rhyolitic crystal tuff, lithic-bedded crystal tuff, volcanic breccia, dacitic to rhyo-dacitic glassy lava and rhyolite lava. Includes a course-grained dacitic flow.|22-NOV-22
6774|Florida Volcanics|73175|5|Briefly described|p1062|Early Devonian|Early Devonian||ca 415 Ma|Cobar Super Group|||Dominated by rhyolitic and dacitic pyroclastic units with subtle magnetic anomalies.|
6774|Florida Volcanics|73578|6|Mentioned|p7, p14, p21, p32, p35|Pridoli|Ludfordian|Shallow-level I-type rocks. Age of 421.7 +/- 2.3 Ma reported by Black (2005).|421.7 +/- 2.3 Ma|||||
6789|Foggs Hollow Granite|42726|5|Briefly described|map legend|Silurian||||||||
6789|Foggs Hollow Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Massive to foliated porphyritic to megacrystic biotite-muscovite-soda-granite, soda-syenite.||||||
6789|Foggs Hollow Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Cream to grey, coarse-grained, massive to occasionally mildly foliated, equigranular to occasionally porphyritic(or megacrystic)biotite-muscovite granite + characteristic smoky grey qtz. High K, U and mod.to high Th radioelement response||||||12-JUN-08
6789|Foggs Hollow Granite|67820|6|Mentioned|p136|||Strongly fractionated. Has higher mineral potential than most granitoids on the Goulburn sheet.||||||
6789|Foggs Hollow Granite|68592|2|Defined|p1262-4, p1268-9, p1274, p1282-6, p1664|Early Devonian|Late Silurian|See also xxiv, p324, p1255 Fig.220. Named (after Foggs Hollow Road) and described by Yacopetti (1987); previously included in the undifferentiated Wyangala Batholith (Stevens, 1955; Brunker and Offenberg, 1970). Published by Chappell et al. (1991). Type locality described. Part of Wyangala Batholith. Here assigned to the Hovells Suite on geochemical grounds. Geochemistry detailed; geophysical properties described. Hosts two localities of W mineralisation in quartz veins and/or greisen. Not isotopically dated. Contact with Bigga Granite gives no indication of relative age.||Unit in Hovells Suite.||Intrudes Adaminaby Group. Is intruded by Bishopthorpe Suite.|Cream to grey, medium- to coarse-grained, equigranular to sporadically porphyritic (or megacrystic), massive to mildly foliated, biotite-muscovite granite. Characterised by smokey grey quartz. Highly fractionated. S-type.|
6789|Foggs Hollow Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sof. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Medium-coarse grained, massive-mildly foliated, equigranular to porphyritic or megacrystic biotite-muscovite granite with smoky grey quartz crystals; high K, medium-high Th and low-high U responses. Low magnetic susceptibility.|
6789|Foggs Hollow Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Hovells Suite|||Medium-coarse grained, massive-mildly foliated, equigranular to porphyritic or megacrystic biotite-muscovite granite with smoky grey quartz crystals; high K, medium-high Th and low-high U responses. Low magnetic susceptibility.|
6789|Foggs Hollow Granite|71069|6|Mentioned|p74|Late Silurian|Late Silurian|||||||
6801|Forbesdale Volcanic Member|42547|5|Briefly described|p36|||||||||
6819|Forest Reefs Volcanics|13139|5|Briefly described|p3 Fig. 2, p9 Fig. 4|||Conformably overlie the Weemalla Formation. Geological Province: Eastern Molong Volcanic Belt. See also p10.||||||12-APR-05
6819|Forest Reefs Volcanics|22679|4|Described|p 15, 17||Ordovician|||||||
6819|Forest Reefs Volcanics|22704|6|Mentioned|Fig6(b),p61|||||||||
6819|Forest Reefs Volcanics|22857|4|Described|p428 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Mafic volcaniclastics, volcanic conglomerate, siltstone. Overlies the Weemalla Formation. Max. thickness: 1000m. Geological Province: Molong Volcanic Arc. ||||||
6819|Forest Reefs Volcanics|23090|5|Briefly described|p642||Ordovician|||||||
6819|Forest Reefs Volcanics|23214|2|Defined|p63|Late Ordovician|Late Ordovician|Of Cabonne Group. Formerly Forest Reefs Beds||||||
6819|Forest Reefs Volcanics|23334|5|Briefly described|3 Fig.2|Late Ordovician|Late Ordovician|||||||
6819|Forest Reefs Volcanics|24007|5|Briefly described|p342|||||||||
6819|Forest Reefs Volcanics|24268|4|Described|p1536 Fig.2|Silurian|Middle Ordovician|Overlying Unit: Panuara Formation. Underlying Unit: Coombing Formation. Geological Province: Lachlan Fold Belt||||||
6819|Forest Reefs Volcanics|42759|6|Mentioned|p14|||||||||
6819|Forest Reefs Volcanics|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
6819|Forest Reefs Volcanics|43640|5|Briefly described|Map Legend||Ordovician|||||||
6819|Forest Reefs Volcanics|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Consists of mafic volcaniclastics , volcanic conglomerate, siltstone. Also clinopyroxene basalt, agglomeratic in places, basaltic subvolcanic intrusives.||||||15-JUL-08
6819|Forest Reefs Volcanics|43653|5|Briefly described|Map Legend||Ordovician|||||||
6819|Forest Reefs Volcanics|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Mafic volcaniclastics, volcanic conglomerate, siltstone.||||||17-JUL-08
6819|Forest Reefs Volcanics|43782|5|Briefly described|Map Legend|Bolindian|Bolindian|of Cabonne Group.||||||
6819|Forest Reefs Volcanics|44093|5|Briefly described|p202 App. 1|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
6819|Forest Reefs Volcanics|60417|5|Briefly described|p153|Late Ordovician|Late Ordovician|Overlies Coombing Formaiton and Weemalla Formation (conformable). Previously part of Weemalla Formaiton.||||||
6819|Forest Reefs Volcanics|60443|4|Described|p762, 765 Fig.3|Eastonian|Eastonian|Conformably overlies Weemalla Formaiton. Unconformably overlain by Cadia Coach Shale. Max. thickness: >2000m. Pyroxene-phyric volcanics, limestone, lapillistone and volcanics sandstone and conglomerate. Age: ~448 Ma. Geological Province: Lachlan Fold Belt||||||
6819|Forest Reefs Volcanics|63277|6|Mentioned|p139|||Unit divided informally into two parts; lower shosonitic basalts, upper shoshonitic trachyandesites.||||||
6819|Forest Reefs Volcanics|63278|4|Described|p145 Fig. 1, p147 Fig. 2b, p155|Late Ordovician|Late Ordovician|Conformably underlain by Weemalla Formation, and Coombing Formation (in Forest Reefs area). Geological Province: Molong Volcanic Belt, LFB. Consists of volcaniclastics and lavas. See also p155.||||||07-FEB-11
6819|Forest Reefs Volcanics|63283|5|Briefly described|p191 Tb. 2, p195 Fig. 2|Late Ordovician|Late Ordovician|Underlain by Weemalla Formation and Coombing Formation. Age: 440Ma (dioritic intrusive). Geological Province: Molong Volcanic Belt.||||||07-FEB-11
6819|Forest Reefs Volcanics|63285|2|Defined|p273, p291-292 App. 1, p276-288|Llandovery|Darriwilian|Of Cabonne Group. Includes; Mt Pleasant Basalt Member. Comformably underlain by Coombing Formation and Weemalla Formation. Thickness inferred: 2-2.5 km. Geol Prov: Molong Volcanic Belt. Hosts Cadia deposit. See p276-288.||||||21-FEB-18
6819|Forest Reefs Volcanics|63286|5|Briefly described|p294 Fig. 1, p295, p300, p308 Fig. 9|Early Silurian|Middle Ordovician|Includes; Mount Pleasant Basalt Member, Nullawonga Latite Member, Cadia Limestone, Junction Reefs Limestone.  Underlain by Coombing Formation + Weemalla Formation. Consists of breccia, conglomerate, sandstone + mudstone. Geol Prov: Molong Volcanic Belt.||||||07-FEB-11
6819|Forest Reefs Volcanics|63288|6|Mentioned|p359|Late Ordovician|Late Ordovician|Has shoshonitic composition.||||||09-AUG-07
6819|Forest Reefs Volcanics|63290|5|Briefly described|p392 Tb. 1, p395, p399 Fig. 5(a)|Bolindian|Gisbornian|Underlain by Weemalla Fm. Contains limestones, top of the unit ages inferred to be 444-443Ma. Geol Prov: Molong Volcanic Belt. Consists also of banded calcareous part, pyroxene-phyric volcanics + Pyroxene-feldspar-phyric lapilli volcaniclastics.||||||
6819|Forest Reefs Volcanics|63292|6|Mentioned|p453|||||||||
6819|Forest Reefs Volcanics|63293|4|Described|p467, p471, p469 Fig. 2|Bolindian|Gisbornian|Includes; Mount Pleasant Basalt Member. Underlain by Weemala Volcanics, Coombing Formation. Geological Province: Molong Volcanic Belt. Cadia Monzonite intrudes unit.||||||07-FEB-11
6819|Forest Reefs Volcanics|67106|6|Mentioned|p673, 679|||Molong Volcanic Belt.|||Nullawonga Latite Member.|||
6819|Forest Reefs Volcanics|67107|6|Mentioned|p689-691, 698, 702|||With Weemalla Formation, hosts the Cadia system of world-class Au-Cu deposits. Skarn mineralization is hosted by limestone. Putative source of ca.438 Ma Pb mineralisation event discussed.||||Overlies Weemalla Formation. Is intruded by Cadia Intrusive Complex.|Volcanic rocks with minor limestone.|
6819|Forest Reefs Volcanics|67322|4|Described|Fig.5; p24-25|Katian|Katian|Macquarie Arc. Defined by Wyborn, in Pogson and Watkins (1998). Conodonts from altered limestone beds in the upper part of the formation are of Eastonian age. Occurs in the Cadia and Forest Reefs-Junction Reefs region.|||Mount Pleasant Basalt Member.|Conformably overlies the Weemalla Formation. Overlies the Coombing Formation.|Andesitic volcanics and volcaniclastic strata.|21-FEB-18
6819|Forest Reefs Volcanics|67821|5|Briefly described|p150, p157, p159|Ordovician|Ordovician|Cadia area.|||||Volcaniclastics.|08-FEB-18
6819|Forest Reefs Volcanics|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
6819|Forest Reefs Volcanics|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.|c. 449-443 Ma|Cabonne Group|Burnt Yards Basalt Member, Nullawonga Latite Member|||
6819|Forest Reefs Volcanics|70684|5|Briefly described|p3, p13, p33-34, p45-47, p48 Fig.23b|Late Ordovician|Late Ordovician|See also p49, p75. Southern Molong Volcanic Belt. The two phases of magmatism were accompanied by normal faulting.|||||Lower part contains deposits from a basaltic submarine volcanic centre overlain by marine calcareous sandstone facies; followed by deposition of volcaniclastics and emplacement of shallow-level sills from submarine trachyandesite cones.|
6819|Forest Reefs Volcanics|72495|6|Mentioned|p235|||Occurs to the south of Orange.||||||
6819|Forest Reefs Volcanics|73154|5|Briefly described|p77 Fig.3|Early Silurian|Middle Ordovician|Macquarie Arc, Phase 4. Molong Volcanic Belt. Gisbornian to Bolindian age indicated p77.|||Mount Pleasant Basalt Member.|Overlies Weemala Formation, Coombing Formation. Intruded by Cadia Igneous Complex, Tallwood Monzonite, Mount Olive diorite.|Shoshonitic intermediate-mafic lava, conglomerate.|
6862|Fossil Hill Limestone|5250|5|Briefly described|p42, p44, p45, p47|Late Ordovician|Early Caradoc|Includes  Gleesons, Wyoming, Transmission and Taplow Limestone Members. ||||||
6862|Fossil Hill Limestone|13995|5|Briefly described|p70, p73|Ordovician|Ordovician|Central NSW. Early Eastonian age. Contains a rich invertebrate fauna including a diverse labechiid assemblage and bryozoans.||Cliefden Caves Limestone Group.||||
6862|Fossil Hill Limestone|22503|6|Mentioned|Fig.4 p646|||||||||
6862|Fossil Hill Limestone|23213|6|Mentioned|p19,22|||Correlates with Reedy Creek Limestone. Fossil assemblages of Belodina confluent in lower part of formation. of Cliefden Caves Subgroup.||||||
6862|Fossil Hill Limestone|23214|2|Defined|p41|Eastonian|Eastonian|Of Cliefden Caves Limestone Subgroup. 114m thick at type section. Overlying unit: Belubula Limestone.||||||
6862|Fossil Hill Limestone|23736|6|Mentioned|p19|||||||||
6862|Fossil Hill Limestone|23739|6|Mentioned|p234|||||||||
6862|Fossil Hill Limestone|24398|5|Briefly described|p264|Late Ordovician|Late Ordovician|Of the Cliefden Caves Limestone Subgroup.  Geological Province: Lachlan Fold Belt.||||||
6862|Fossil Hill Limestone|38219|2|Defined|p306|Late Ordovician|Late Ordovician|Part of Cliefden Caves Group. See also Fig.2.||||||
6862|Fossil Hill Limestone|41046|6|Mentioned|p143|||||||||
6862|Fossil Hill Limestone|41108|6|Mentioned|Fig.2|||||||||
6862|Fossil Hill Limestone|41508|6|Mentioned|Abb.1|||||||||
6862|Fossil Hill Limestone|42479|4|Described|p108|||||||||
6862|Fossil Hill Limestone|42603|5|Briefly described|p57|||||||||
6862|Fossil Hill Limestone|42612|5|Briefly described|Fig.2 P29|||||||||
6862|Fossil Hill Limestone|43569|6|Mentioned|p475||Late Ordovician|||||||
6862|Fossil Hill Limestone|43571|6|Mentioned|p821|||||||||
6862|Fossil Hill Limestone|50098|5|Briefly described|p4, p10|Ordovician|Ordovician|Of the lower Cliefden Caves Limestone Group.||||||04-MAY-05
6862|Fossil Hill Limestone|60989|6|Mentioned|p114|Late Ordovician|Late Ordovician|Cliefden Caves. Shell beds contain trimerellide brachiopods.||||||
6862|Fossil Hill Limestone|61893|5|Briefly described|p236|Eastonian|Eastonian|Conodont species mentioned.||Cliefden Caves Limestone Group.||||
6862|Fossil Hill Limestone|63278|4|Described|p153, p154|||Include; Gleesons Member, Wyoming Limestone Member. Of the Cliefden Caves Limestone Subgroup. Geological Province: Molong Volcanic Belt, LFB. Lower part consists of a high clastic content.||||||07-FEB-11
6862|Fossil Hill Limestone|63290|6|Mentioned|p400 Fig. 5(c)|||||||||
6862|Fossil Hill Limestone|64015|6|Mentioned|p79|Late Ordovician|Late Ordovician|Contains the Ballingoole Limestone.||||||28-AUG-08
6862|Fossil Hill Limestone|64295|5|Briefly described|p201|||Of the Cliefden Caves Limestone Subgroup. Disconformably overlies Walli Volcanics. Shallow water sedimentary rocks. Age is early Eastonian.||||||01-SEP-08
6862|Fossil Hill Limestone|67322|4|Described|Fig.5; p24; cover photograph.|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. Appears as a Member on p24.||Of the Cliefden Caves Limestone Subgroup.||Disconformably overlies the Walli Volcanics. Overlain by the Belubula Limestone.|Well-bedded limestone.|21-FEB-18
6862|Fossil Hill Limestone|70754|5|Briefly described|p447, p449-450, p455, p459, p462, p465|Katian|Katian|Cliefden Caves area. Systematic palaeontological descriptions.||Cliefden Caves Limestone Subgroup.|Gleesons, Kalimna, Wyoming, Dunhill Bluff, Limestone Members.|Correlated with Daylesford Limestone.||
6862|Fossil Hill Limestone|73208|5|Briefly described|p870 Fig.2, 873 Fig.5, 874|Late Ordovician|Late Ordovician|Type locality is Fossil Hill, near Cliefden Caves, central-west NSW. Represents carbonate deposits flanking a volcanic island. Has excellent preservation and relative continuity.||Cliefden Caves Limestone Subgroup.||||
6862|Fossil Hill Limestone|73209|5|Briefly described|p879-888|Late Ordovician|Late Ordovician|The type section is in the Cliefden Caves area. A detailed stratigrapic column is given. Table 1 (p883) contrasts its rich variety of fossil species with 17 Late Ordovician fossiliferous limestones throughout the world. Diagrams of polished slabs and microphotographs.||Cliefden Caves Limestone Subgroup||Overlies Walli Volcanics (Cliefden Caves Limestone Subgroup). Is overlain by Belubula Limestone.|Thinly-bedded, fossiliferous limestone. Includes shallow-water basal marls succeeded by bioturbated lime muds. Periodic exposure produced sheets/lenses of sand and subaerial disconformities (detailed).|
6862|Fossil Hill Limestone|73210|5|Briefly described|p891-893, 896-897, 899, 901, 903, 905|Late Ordovician|Late Ordovician|Cliefden Caves, NSW. Exhibits subaerial disconformities and diagenesis/pedogenesis. Microphotographs, stratigraphic column. Summary profile of a subaerial disconformity.||Cliefden Caves Limestone Subgroup.|||A variety of limestone types: skeletal wackestone, pelletal grainstones to skeletal, lithoclast and calcrete ooid grainstones. Richly fossiliferous. Local biostromes and small bioherms.|14-DEC-22
6862|Fossil Hill Limestone|73492|5|Briefly described|p696, p703, p706|Katian|Katian|T. philipi Biozone in basal part, earliest Katian age.||Cliefden Caves Limestone Subgroup|Kalimna Limestone Member|||
6881|Frampton Volcanics|22638|3|Fully described|p31|Wenlock|Llandovery|Age: 428 +/- 6 Ma||||||14-DEC-04
6881|Frampton Volcanics|22685|5|Briefly described|p728,Fig1p729|Silurian|Silurian|Rhyolite, dacite, sandstone and conglomerate.  Age is Middle Silurian.||||||17-JAN-06
6881|Frampton Volcanics|22687|6|Mentioned|110|Early Silurian|Ordovician|Geol province Lachlan Fold Belt||||||
6881|Frampton Volcanics|22768|5|Briefly described|p173-74|Early Wenlockian|Llandovery|Max Age: 428 (+/-) 6 Ma||||||
6881|Frampton Volcanics|22857|4|Described|p174, p452 App.1, Tb.A1.6|Wenlockian|Llandovery|Mapped as part of Gooandra Volcanics below Jackalass Slate and Bumbolee Creek Fm by Stuart-Smith (1990b) with an age of 425Ma - a controversial interpretation. Corrected age: 428+/-6Ma (U/Pb SHRIMP zircon; Stuart-Smith, 1992). Geol. Prov: Tumut Trough.||||||
6881|Frampton Volcanics|23309|5|Briefly described|p383.||| Age: 428+/-6 Ma.||||||
6881|Frampton Volcanics|23454|5|Briefly described|p32|Silurian|Ordovician|428+/-6Ma||||||
6881|Frampton Volcanics|24266|5|Briefly described|p1487|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||09-MAR-05
6881|Frampton Volcanics|29648|6|Mentioned|p19|||||||||
6881|Frampton Volcanics|29682|4|Described|p13|||||||||
6881|Frampton Volcanics|30172|6|Mentioned|p43|||||||||
6881|Frampton Volcanics|35070|3|Fully described|p71|||||||||
6881|Frampton Volcanics|35185|6|Mentioned|p231|||||||||
6881|Frampton Volcanics|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
6881|Frampton Volcanics|35607|6|Mentioned|p144|||See also P145,146,148.||||||
6881|Frampton Volcanics|35608|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Late Silurian||||||
6881|Frampton Volcanics|35609|4|Described|p8|||||||||
6881|Frampton Volcanics|36534|6|Mentioned|p225|||||||||
6881|Frampton Volcanics|37529|5|Briefly described|p6|||||||||
6881|Frampton Volcanics|40328|4|Described|p40|||||||||
6881|Frampton Volcanics|40497|6|Mentioned|Map legend|Silurian|Silurian|||||||
6881|Frampton Volcanics|40498|6|Mentioned|p380|||||||||
6881|Frampton Volcanics|40678|5|Briefly described|p11|||||||||
6881|Frampton Volcanics|42045|6|Mentioned|Fig.2 P148|||||||||
6881|Frampton Volcanics|42313|4|Described|p44|||Age latest Silurian||||||
6881|Frampton Volcanics|42314|5|Briefly described|Map|Early Silurian||||||||
6881|Frampton Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
6881|Frampton Volcanics|42828|5|Briefly described|Fig.2 P128|||||||||
6881|Frampton Volcanics|43834|6|Mentioned|p32|||Tumut region||||||
6881|Frampton Volcanics|44093|5|Briefly described|p183 App. 1|Late Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
6881|Frampton Volcanics|44192|5|Briefly described|Map Legend|Wenlockian|Llandoverian|||||||
6881|Frampton Volcanics|44936|5|Briefly described|Map Legend||Silurian|||||||
6881|Frampton Volcanics|50191|6|Mentioned|p6, 14|Late Silurian|Early Silurian|||||||
6881|Frampton Volcanics|60280|5|Briefly described|p2, p3 Fig. 1|||||||||
6881|Frampton Volcanics|66197|5|Briefly described|p629, p631 Fig.3a|Wenlock|Llandovery|Tumut Trough. Silicic volcanics, ?with mafic volcanics. Age: 428 +/- 6 Ma (U-Pb zircon: Stuart-Smith et al. 1992).||||||13-MAR-12
6881|Frampton Volcanics|69801|6|Mentioned|p2, p53, p138|||Eastern Lachlan Orogen. SHRIMP age is derived from Geoscience Australia, 2007: SampleID 98844516.|420.1 +/- 1.7 Ma (SHRIMP, magmatic age)|||Intruded by the Mishurley Creek Granite and the Yammatree Granite.||
6881|Frampton Volcanics|70890|6|Mentioned|p337|Wenlock|Wenlock|Of Tumut Trough. U-Pb zircon age of 428+\-6 Ma reported by Stuart-Smith et al., 1992).||||||
6881|Frampton Volcanics|73082|6|Mentioned|p16-17|||Gundagai area.|||||Contains auriferous quartz (+/- calcite, talc) veins and auriferous shear zones.|
6881|Frampton Volcanics|73215|5|Briefly described|p994|||Tumut Trough.|420 +/- 2 Ma (Black, 2007).|||||
6881|Frampton Volcanics|73483|6|Mentioned|p408||||||||Includes unfoliated rhyolite.|
6926|Frome Hill Formation|5253|5|Briefly described|p97|Devonian|Silurian|Comprises three members: Folly Point Limestone Member, Efflux Siltstone Member, and Sawtooth Ridge Limestone (in ascending order).||||||16-JAN-12
6926|Frome Hill Formation|22842|4|Described|p25,29|Early Devonian||Contains Folly Point Limestone , Efflux Limestone and Sawtooth Ridge Limestone Members.||||||
6926|Frome Hill Formation|40698|6|Mentioned|p53|||||||||
6926|Frome Hill Formation|50234|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of the Bungonia Group.  Includes: Folly Point Limestone Member.  Overlies: Cardinal View Formation.||||||
6926|Frome Hill Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Bungonia Group. Includes Folly Point Limestone Member.  Medium-grained, well-sortedm highly fossiliferous sandstone and shale  (no outcrop).||||||
6926|Frome Hill Formation|67820|6|Mentioned|p136 Fig.3|Early Devonian|Late Silurian|||Bungonia Group.||||
6926|Frome Hill Formation|68592|3|Fully described|p850, p898, p900, p914-21, p1892|Lochkovian|Pridoli|These rocks had been included in Bungonia Limestone. Name first published by James, Francis and Jennings (1979); defined by Bauer (1994). 25-565m thick. Brayton Limestone Member (Longreach Volcanics) may overlap in age with the top of the Frome Hill Formation (Bungonia Group). Fossil fauna described.||Unit in Bungonia Group.|Includes Sawtooth Ridge and Folly Point, Limestone Members and Efflux Siltstone Member.|Overlies Cardinal View Formation: faulted contact.|Basal sequence of fossiliferous limestone and interbedded calcareous sandstone; locally overlain by a siliciclastic succession of siltstone, shale and minor sandstone, or a micritic limestone with mass flow units with limestone and chert pebbles.|
6926|Frome Hill Formation|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Sbf. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Bungonia Group|Includes Folly Point Limestone Member.|Overlies Cardinal View Formation.|Fossiliferous limestone interbedded with well sorted, medium grained fossiliferous calcareous sandstone, siltstone, shale, micrite-rich limestone and minor conglomerate with pebble clasts of limestone and chert.|
6926|Frome Hill Formation|70542|5|Briefly described|Map Legend|Silurian|Silurian|||Bungonia Group|Includes Folly Point Limestone Member||Fossiliferous limestone interbedded with well sorted, medium grained fossiliferous calcareous sandstone, siltstone, shale, micrite-rich limestone and minor conglomerate with pebble clasts of limestone and chert.|
6926|Frome Hill Formation|70661|3|Fully described|p31 tbl 1, p42|Lochkovian|Pridoli|Named after Frome Hill. Previously included as part of the Bungonia Limestone. 25-565m thick. Outcrop associated with gentle slope and slight prominence associated with outcrops of Folly Point Limestone Member. Deposited in marine barrier system. Structure, metamorphism and geophysical characteristics discussed.||Bungonia Group|Sawtooth Ridge Limestone Member, Efflux Siltstone Member, Folly Point Limestone Member|Probably disconformably or unconformably overlain by Tangerang Formation, overlies Cardinal View Formation (faulted contact in Moss Vale)|Fossiliferous limestone interbedded with well sorted medium-grained fossiliferous calcareous sandstone. This is overlain by siltstone, shale and minor medium grained fossiliferous sandstone or where absent, micrite rich limestone.|
6926|Frome Hill Formation|71303|5|Briefly described|map legend|Lochkovian|Ludlow|||Of Bungonia Group.|Includes Folly Point Limestone Member, Efflux Siltstone Member, Sawtooth Ridge Limestone Member.||Fossiliferous limestone horizons, medium-grained fossiliferous calcareous sandstone, siltstone, shale.|
6926|Frome Hill Formation|71656|5|Briefly described|p13 Fig.2, p31|Pridoli|Ludlow|Fossils of brachiopods, conodonts, trilobites and ostracods have been identified in this formation. Top possibly Devonian (from brachiopod in Sawtooth Ridge limestone Member).||Bungonia Group|Includes Efflux Siltstone Member, Folley Point Limestone Member, Sawtooth Ridge Limestone Member.|Overlies Cardinal View Formation. Partially equivalent with Wombeyan Limestone.|Includes fossiliferous limestone.|
6926|Frome Hill Formation|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.||Bungonia Group|Includes the Folly Point Limestone Member.|Overlies the Cardinal View Formation. Interbedded with the Folly Point Limestone Member.|Fossiliferous limestone.|
6942|Fyshwick Gravel|12185|5|Briefly described|map legend|||Quartz pebble gravel, coarse sandstone. Age: Permian ?. BMR map symbol: Pf.||||||
6942|Fyshwick Gravel|29992|6|Mentioned|Map legend|Permian|Permian|||||||
6942|Fyshwick Gravel|29994|6|Mentioned|Map legend|Permian|Permian|||||||
6942|Fyshwick Gravel|31019|6|Mentioned|Map legend|Permian|Permian|||||||
6942|Fyshwick Gravel|31284|6|Mentioned|Map legend|Permian|Permian|Prob. Permian||||||
6942|Fyshwick Gravel|31527|6|Mentioned|p376|||Permian ?||||||
6942|Fyshwick Gravel|33328|4|Described|Table 1|||p15.||||||29-OCT-20
6942|Fyshwick Gravel|34396|6|Mentioned|p179|||||||||
6942|Fyshwick Gravel|35110|6|Mentioned|p3|||||||||
6942|Fyshwick Gravel|37348|6|Mentioned|p97|||||||||
6942|Fyshwick Gravel|42820|6|Mentioned|p61|Miocene|Paleocene|Refers to Opik (1958), Permian age refuted by.Jennings (1972) and Ollier and Brown (1975). Age uncertain but likely to be in the Paleocene- Miocene range.||||||24-SEP-20
6942|Fyshwick Gravel|43344|14|Not recorded|p110,113,114||Permian|||||||
6942|Fyshwick Gravel|44970|2|Defined|p57-9,61,64-5,68,75||Permian|Fluvioglacial. map||||||
6942|Fyshwick Gravel|48878|14|Not recorded|p.10,20||Permian|Compared to river gravels at the foot of Mt.Bollard.||||||
6947|Gabo Suite|22815|4|Described|p95|Late Devonian|Late Devonian|K/Ar Age: 356+/-12 Ma.||||||
6947|Gabo Suite|23309|5|Briefly described|p317, 348|Early Carboniferous|Late Devonian|Gabo Island and Howe Range Granites.||||||
6947|Gabo Suite|23550|5|Briefly described|p511|||||||||
6947|Gabo Suite|24222|6|Mentioned|p22|||See also Gabo suite.  Geological Province: Lachlan Fold Belt.||||||
6947|Gabo Suite|24551|6|Mentioned|p235, 236|||||||||
6947|Gabo Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
6947|Gabo Suite|42827|5|Briefly described|p428|||||||||
6947|Gabo Suite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
6947|Gabo Suite|44093|5|Briefly described|p222 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
6947|Gabo Suite|63605|5|Briefly described|p992 Fig. 1, p997|||Includes Gabo Island and Watergums Granites. Associated with the Boyd Volcanic Complex - intrusive relationship.||||||07-FEB-11
6947|Gabo Suite|67779|6|Mentioned|p66.|||Lachlan Fold Belt. A-type granites. Has remarkable chemical similarity with Tin Camp Granite, McArthur Basin.||||||
6947|Gabo Suite|67847|5|Briefly described|p60 fig 3.3.4|Middle Devonian|Middle Devonian|A-type intrusive rocks. ||||||
6947|Gabo Suite|70351|6|Mentioned|p55|||||||||
6947|Gabo Suite|70601|5|Briefly described|p31|Late Devonian|Middle Devonian|||||Intrudes Boyd Volcanic Complex.|A-type subvolcanic granites.|
6947|Gabo Suite|71206|6|Mentioned|p373, 375, 377, 379-382|||Presented as Gabo Island Suite. Geochemistry discussed.|||Watergums, Naghi, Nagha, Carlyle, Howe Range, Gabo Island, Granites.||Aluminous A-type granite.|
6947|Gabo Suite|73431|6|Mentioned|p374 Fig.8|||A-type granites.||||||
6976|Gambier Limestone|10010|5|Briefly described|p12 Fig. 3|Late Oligocene|Early Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
6976|Gambier Limestone|12781|6|Mentioned|p386|Miocene|Eocene|Otway Basin. Maximum thickness 400m.||Heytsbury Group.||Overlies Gellibrand Marl.||
6976|Gambier Limestone|22541|6|Mentioned|Fig 16|||||||||
6976|Gambier Limestone|22587|6|Mentioned|p79 Fig.7|Early Miocene|Late Eocene|||||||
6976|Gambier Limestone|22626|6|Mentioned|446 fig 10|Early Miocene|Late Oligocene|Geol province West Otway Basin. Overlying unit Heytesbury Group||||||
6976|Gambier Limestone|22773|5|Briefly described|Fig24.8p352+24.9p353|||||||||
6976|Gambier Limestone|22799|5|Briefly described|p23 Fig.7|Early Miocene|Oligocene|Glenelg Group||||||
6976|Gambier Limestone|22857|5|Briefly described|p352 Fig.24.8, p353 Fig. 24.9|Early Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
6976|Gambier Limestone|22887|5|Briefly described|Fig.6 p13||Late Oligocene|Of Murray Group, Murray Basin.||||||03-FEB-09
6976|Gambier Limestone|22893|5|Briefly described|fig4 p9|||||||||
6976|Gambier Limestone|22913|6|Mentioned|29|||||||||
6976|Gambier Limestone|22938|5|Briefly described|fig5|Oligocene|Oligocene|Eastern Mount Lofty Ranges.||||||
6976|Gambier Limestone|23249|5|Briefly described|Fig.2|||Informally divided into Upper/Middle and Lower Gambier Limestone.||||||
6976|Gambier Limestone|23322|4|Described|955, 957|Middle Miocene|Middle Eocene|Geological Province: Gambier Basin.||||||07-SEP-09
6976|Gambier Limestone|23671|6|Mentioned|p2|||Overlies the Compton Conglomerate; disconformably overlies the Burrungule Member.||||||16-AUG-04
6976|Gambier Limestone|23731|6|Mentioned|p20, p27|Miocene|Oligocene|||||||
6976|Gambier Limestone|23768|5|Briefly described|p28 Fig.5, p69|Miocene|Oligocene|Geological Province: Gambier Basin. See also p89, p154.||||||29-MAR-05
6976|Gambier Limestone|23818|5|Briefly described|p174 Fig.84, p177|Middle Miocene|Oligocene|Geological Province: Otway Basin. Max. thickness: 500 ft.||||||
6976|Gambier Limestone|23879|5|Briefly described|p19|||||||||
6976|Gambier Limestone|23884|5|Briefly described|p155 Fig. 13.2|Late Oligocene|Late Oligocene|Geological Province: Murray Basin. Of the Murray Group.||||||
6976|Gambier Limestone|24160|6|Mentioned|p18|Middle Miocene|Middle Miocene|Hosts a calcium bentonite deposit below weathered Newer Volcanics.||||Is overlain by Newer Volcanics.||
6976|Gambier Limestone|24202|5|Briefly described|p313 Fig.2|Middle Miocene|Early Oligocene|Geological Province: Gambier Sub-basin.  See also p314.||||||
6976|Gambier Limestone|24314|5|Briefly described|p61 Fig.2|Miocene|Eocene|Geological Province: Otway Basin. Max. Thickness 400m. Of the Heytesbury Group.||||||30-NOV-04
6976|Gambier Limestone|24363|5|Briefly described|p37|Early Miocene|Oligocene|max. thickness: 400 m. Age: 38-15 Ma.||||||
6976|Gambier Limestone|24410|6|Mentioned|p6|Late Oligocene|Early Miocene|||||||
6976|Gambier Limestone|24551|6|Mentioned|p296, 555, 625|||||||||
6976|Gambier Limestone|24562|5|Briefly described|p15 Fig. 4|Tertiary|Late Cretaceous|Geological Province: Otway Basin.||||||
6976|Gambier Limestone|29591|6|Mentioned|p90|||||||||
6976|Gambier Limestone|29654|6|Mentioned|p101|||||||||
6976|Gambier Limestone|29666|6|Mentioned|p22|||||||||
6976|Gambier Limestone|29697|6|Mentioned|p2|||||||||
6976|Gambier Limestone|29828|6|Mentioned|p25|||||||||
6976|Gambier Limestone|29866|6|Mentioned|p84|||||||||
6976|Gambier Limestone|29891|5|Briefly described|p77|||||||||
6976|Gambier Limestone|29892|6|Mentioned|p77|||||||||
6976|Gambier Limestone|29894|6|Mentioned|p27|||||||||
6976|Gambier Limestone|30179|6|Mentioned|p33|||Oligocene - Miocene age||||||
6976|Gambier Limestone|30184|6|Mentioned|p173|||||||||
6976|Gambier Limestone|30514|6|Mentioned|p108|||||||||
6976|Gambier Limestone|30520|6|Mentioned|p41|||Groundwater||||||
6976|Gambier Limestone|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
6976|Gambier Limestone|30751|6|Mentioned|Map legend|Oligocene|Eocene|Miocene-Eocene||||||
6976|Gambier Limestone|30753|4|Described|Table 2|||Middle Miocene to Upper Eocene age.||||||07-SEP-18
6976|Gambier Limestone|30754|5|Briefly described|p13|||Strat.tables p14,22. See also p20,24,28. Map, block diag.,section.||||||07-SEP-18
6976|Gambier Limestone|30807|6|Mentioned|p101|||Suggested map symbol||||||
6976|Gambier Limestone|30828|6|Mentioned|p113|||||||||
6976|Gambier Limestone|30917|6|Mentioned|p26|||||||||
6976|Gambier Limestone|30918|6|Mentioned|p85|||||||||
6976|Gambier Limestone|30932|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene to Miocene||||||
6976|Gambier Limestone|30996|6|Mentioned|Fig. 3|||||||||
6976|Gambier Limestone|31241|4|Described|p99|||See also P101. Equ. in age to Ettrick Fm.||||||
6976|Gambier Limestone|31245|6|Mentioned|p81|||||||||
6976|Gambier Limestone|31372|6|Mentioned|Fig. 2|||||||||
6976|Gambier Limestone|31424|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|31515|6|Mentioned|p292|||||||||
6976|Gambier Limestone|31517|6|Mentioned|p1|||Fossil sites of decapods.||||||
6976|Gambier Limestone|31624|2|Defined|p96|Tertiary|Tertiary|||||||
6976|Gambier Limestone|31625|6|Mentioned|Fig. 5.2|||Oligocene- Miocene||||||
6976|Gambier Limestone|31629|6|Mentioned|Fig.5.2|||Miocene-Oligocene||||||
6976|Gambier Limestone|31746|6|Mentioned|p195|||||||||
6976|Gambier Limestone|31848|6|Mentioned|p15|||Refers Ludbrook (1969)||||||
6976|Gambier Limestone|31851|6|Mentioned|p10|||Also P15||||||
6976|Gambier Limestone|31920|4|Described|p59|||Oligocene. Sponge spicule mb. See also Figs 3-2,4.||||||
6976|Gambier Limestone|31922|6|Mentioned|Table 3|||||||||
6976|Gambier Limestone|31923|6|Mentioned|p16|||||||||
6976|Gambier Limestone|32116|4|Described|p45|||Oligocene. See also p46-47.||||||01-NOV-22
6976|Gambier Limestone|32344|6|Mentioned|p121|||||||||
6976|Gambier Limestone|32552|6|Mentioned|p184|||Longfordian||||||
6976|Gambier Limestone|32570|6|Mentioned|p6|||||||||
6976|Gambier Limestone|32601|6|Mentioned|p682|||||||||
6976|Gambier Limestone|32653|6|Mentioned|Table 1|||||||||
6976|Gambier Limestone|32841|6|Mentioned|p6|||||||||
6976|Gambier Limestone|32859|4|Described|p69|||L.Miocene||||||
6976|Gambier Limestone|32860|5|Briefly described|p91|||Lower Pliocene.||||||07-SEP-18
6976|Gambier Limestone|32894|6|Mentioned|p287|||Olig.-Miocene||||||
6976|Gambier Limestone|32895|6|Mentioned|p328|||Tertiary||||||
6976|Gambier Limestone|32897|6|Mentioned|Fig. 7-1|||||||||
6976|Gambier Limestone|32898|6|Mentioned|p27|||See also Table 2-1||||||
6976|Gambier Limestone|33109|6|Mentioned|p84|||Main aquifer system||||||
6976|Gambier Limestone|33236|6|Mentioned|p19|||Olig. - Miocene||||||
6976|Gambier Limestone|33490|4|Described|p10|||See also p27. Oligocene - Miocene.||||||07-SEP-18
6976|Gambier Limestone|33579|6|Mentioned|p52|||||||||
6976|Gambier Limestone|33712|6|Mentioned|p9|||See also Fig.1. Oligo. - Mioc. Refers Ludbrook (1961).||||||
6976|Gambier Limestone|33713|4|Described|p27|||See also p28.||||||07-SEP-18
6976|Gambier Limestone|33716|3|Fully described|p15|||See also pp16 & 20 & Table 2.||||||07-SEP-18
6976|Gambier Limestone|33798|6|Mentioned|p98|||Fig.2||||||
6976|Gambier Limestone|33940|6|Mentioned|p414|||||||||
6976|Gambier Limestone|33943|6|Mentioned|p379|||||||||
6976|Gambier Limestone|34180|6|Mentioned|p212|||Tertiary||||||
6976|Gambier Limestone|34185|6|Mentioned|p131|||Protected from marine erosion in Pliocene.||||||
6976|Gambier Limestone|34191|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
6976|Gambier Limestone|34308|3|Fully described|p177|||Aldingian - Balcombian. Correlation chart||||||
6976|Gambier Limestone|34418|4|Described|p506|||||||||
6976|Gambier Limestone|34421|6|Mentioned|p261|||See also P262||||||
6976|Gambier Limestone|34524|5|Briefly described|p105|||||||||
6976|Gambier Limestone|34615|6|Mentioned|p3|||||||||
6976|Gambier Limestone|34658|5|Briefly described|p98|||||||||
6976|Gambier Limestone|34954|6|Mentioned|Fig.33|||Analysis.||||||
6976|Gambier Limestone|34958|6|Mentioned|p88|||||||||
6976|Gambier Limestone|34988|6|Mentioned|p294|||||||||
6976|Gambier Limestone|35018|5|Briefly described|p29|||||||||
6976|Gambier Limestone|35051|6|Mentioned|p203|||Analysis.||||||
6976|Gambier Limestone|35066|6|Mentioned|p210|||||||||
6976|Gambier Limestone|35097|6|Mentioned|Fig.4|||||||||
6976|Gambier Limestone|35147|6|Mentioned|p127|||||||||
6976|Gambier Limestone|35200|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
6976|Gambier Limestone|35232|6|Mentioned|p11|||||||||
6976|Gambier Limestone|36492|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|37500|6|Mentioned|p385|||||||||
6976|Gambier Limestone|37548|6|Mentioned|p131|||||||||
6976|Gambier Limestone|38068|6|Mentioned|Fig.7|||||||||
6976|Gambier Limestone|38070|6|Mentioned|Fig.12|||Otway Basin||||||
6976|Gambier Limestone|38663|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|38699|6|Mentioned|p8|||||||||
6976|Gambier Limestone|38826|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|38903|5|Briefly described|Table 2|||||||||
6976|Gambier Limestone|38932|5|Briefly described|p98|||See also Fig.4.||||||07-SEP-18
6976|Gambier Limestone|39077|6|Mentioned|Table 2|||||||||
6976|Gambier Limestone|39329|6|Mentioned|Fig.1|||||||||
6976|Gambier Limestone|39408|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|39923|6|Mentioned|p354|||||||||
6976|Gambier Limestone|39929|6|Mentioned|Fig.3|||||||||
6976|Gambier Limestone|40003|5|Briefly described|p44|||||||||
6976|Gambier Limestone|40032|6|Mentioned|p225|||||||||
6976|Gambier Limestone|40125|6|Mentioned|p353|||||||||
6976|Gambier Limestone|40230|6|Mentioned|p6|||||||||
6976|Gambier Limestone|40298|6|Mentioned|p432|||||||||
6976|Gambier Limestone|40429|6|Mentioned|Fig.2|||||||||
6976|Gambier Limestone|40521|6|Mentioned|p307|||||||||
6976|Gambier Limestone|40555|6|Mentioned|p51|||||||||
6976|Gambier Limestone|40556|6|Mentioned|p61|||||||||
6976|Gambier Limestone|40557|6|Mentioned|p169|||||||||
6976|Gambier Limestone|40560|6|Mentioned|p6|||||||||
6976|Gambier Limestone|40561|6|Mentioned|p8|||||||||
6976|Gambier Limestone|40829|5|Briefly described|p14|||||||||
6976|Gambier Limestone|40877|5|Briefly described|p55|||||||||
6976|Gambier Limestone|40947|6|Mentioned|p3|||||||||
6976|Gambier Limestone|40980|6|Mentioned|p335|||||||||
6976|Gambier Limestone|41076|6|Mentioned|p63|||||||||
6976|Gambier Limestone|41185|6|Mentioned|Fig.5|||||||||
6976|Gambier Limestone|41517|6|Mentioned|p138|||||||||
6976|Gambier Limestone|41518|6|Mentioned|p146|||||||||
6976|Gambier Limestone|41519|6|Mentioned|p172|||||||||
6976|Gambier Limestone|41520|5|Briefly described|Fig.12|||||||||
6976|Gambier Limestone|41578|6|Mentioned|p7|||||||||
6976|Gambier Limestone|41599|6|Mentioned|p191|||||||||
6976|Gambier Limestone|41626|6|Mentioned|p54|||||||||
6976|Gambier Limestone|42097|6|Mentioned|p40|||||||||
6976|Gambier Limestone|42125|5|Briefly described|p136|||||||||
6976|Gambier Limestone|42127|5|Briefly described|p223|||||||||
6976|Gambier Limestone|42130|6|Mentioned|Fig.3 P265|||||||||
6976|Gambier Limestone|42137|6|Mentioned|p370|||||||||
6976|Gambier Limestone|42335|5|Briefly described|p338|||||||||
6976|Gambier Limestone|42457|6|Mentioned|p170|||||||||
6976|Gambier Limestone|42594|5|Briefly described|p247|||Oligocene-Miocene||||||
6976|Gambier Limestone|42599|5|Briefly described|Fig.3 P614|||Cooper Basin.||||||07-SEP-18
6976|Gambier Limestone|42601|6|Mentioned|Fig.2 p15|||||||||
6976|Gambier Limestone|42717|6|Mentioned|map legend|Miocene|Oligocene|||||||
6976|Gambier Limestone|42827|6|Mentioned|p285|||||||||
6976|Gambier Limestone|42881|4|Described|Fig.3, p84|||||||||01-NOV-22
6976|Gambier Limestone|42966|2|Defined|Table 15, p126|Early Miocene|Late Oligocene|Of Murray Group, Murray Basin & Glenelg Group, Otway Basin.||||||03-FEB-09
6976|Gambier Limestone|43073|5|Briefly described|p11|||||||||
6976|Gambier Limestone|43171|6|Mentioned|5|||Of Heytesbury Group.||||||03-FEB-09
6976|Gambier Limestone|43195|5|Briefly described|Map Legend|Middle Miocene|Late Eocene|see also commentary on back of map. Of Heytesbury Group.||||||
6976|Gambier Limestone|43258|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6976|Gambier Limestone|43298|5|Briefly described|Map Legend|Miocene|Eocene|||||||
6976|Gambier Limestone|43383|14|Not recorded|p29||Early Miocene|||||||
6976|Gambier Limestone|43466|14|Not recorded|p3,Pl.1|||Equivalent to SA||||||
6976|Gambier Limestone|43467|14|Not recorded|p3,20,31,32|||||||||
6976|Gambier Limestone|43660|6|Mentioned|Fig.7,p16|||||||||
6976|Gambier Limestone|43667|6|Mentioned|Fig.3,p12|Early Miocene|Early Oligocene|||||||
6976|Gambier Limestone|43686|6|Mentioned|Fig.5,p233|||||||||
6976|Gambier Limestone|43733|6|Mentioned|p30||Tertiary|||||||
6976|Gambier Limestone|43744|6|Mentioned|Fig.3,p3|||||||||
6976|Gambier Limestone|43791|6|Mentioned|p372, Fig1|||||||||
6976|Gambier Limestone|43797|5|Briefly described|p201|Miocene|Oligocene|||||||
6976|Gambier Limestone|43799|5|Briefly described|p185|||||||||
6976|Gambier Limestone|43804|6|Mentioned|Fig.2,p49|||||||||
6976|Gambier Limestone|43814|6|Mentioned|Fig.3,p115|||||||||
6976|Gambier Limestone|44133|4|Described|p156, 259, 268|Miocene|Miocene|Thickness: 400m. Of the Heytesbury Group. Geological Province: Gambier Basin. Includes: Greenways Member, Camelback Member, Green Point Member, Naracoorte Limestone Member.||||||
6976|Gambier Limestone|46802|6|Mentioned|Table 1|||||||||
6976|Gambier Limestone|46839|6|Mentioned|p81|||||||||
6976|Gambier Limestone|46899|6|Mentioned|p13|||Thermal conductivity||||||
6976|Gambier Limestone|46909|6|Mentioned|p83|||||||||
6976|Gambier Limestone|48624|14|Not recorded|p4,6,Fig.2|||(J54-6/Benara).||||||
6976|Gambier Limestone|48625|14|Not recorded|p4,5|||(J54-6/Kennion). map opp.p.1.||||||
6976|Gambier Limestone|48911|6|Mentioned|Chart 1|||Heytesbury Gp.||||||
6976|Gambier Limestone|49038|5|Briefly described|p26|||||||||
6976|Gambier Limestone|49040|6|Mentioned|p11|||||||||
6976|Gambier Limestone|50133|5|Briefly described|p3, Fig.1|Mid Miocene|Late Eocene|Also called Mount Gambier Limestone (superseded term) in this article (at p6, p8 Tb 1, p11 Tb.2). Major & trace element geochemistry for 2 samples given.|||Includes Camelback Member.||Fossiliferous carbonate|27-MAR-12
6976|Gambier Limestone|60538|5|Briefly described|p471 Fig. 10, 473 Fig. 12|||Of the Nirranda Group.||||||
6976|Gambier Limestone|60785|6|Mentioned|p184 Fig.1. |Chattian|Chattian|South Australia.|||Includes the Camelback Member.|||
6976|Gambier Limestone|60953|5|Briefly described|Map Legend|Miocene|Eocene|Marine fossiliferous limestone. Geological Province: Gambier Basin.||||||
6976|Gambier Limestone|61108|5|Briefly described|map legend|Miocene|Eocene|Marine fossiliferous limestone. Geological Province: Gambier Basin.||||||
6976|Gambier Limestone|61155|5|Briefly described|p18|Middle Miocene|Early Oligocene|Murray Group. Overlies Ettrick Formation; overlain by Mannum Formation. Age: 27.5-~24Ma to ~33-15Ma. Interfingered with Naracoorte Limestone. Thickness: 100m. Geological Province: Murray and Otway Basin.||||||03-MAR-10
6976|Gambier Limestone|61547|6|Mentioned|p461 Fig.2. |Miocene|Eocene|||Unit in Heytesbury Group.||Overlies Gellibrand Marl.||
6976|Gambier Limestone|61622|5|Briefly described|p436 Fig. 2|Miocene|Eocene|Of Heytsbury Group. Geological Province: Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|61627|5|Briefly described|p500 Fig. 2|Miocene|Late Eocene|Of Heytesbury Group. Geological Province: Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|62640|6|Mentioned|p76.|||Tertiary. Restricted cave development is due to substantial intergranular porosity and permeability; hence considerable groundwater flow through the limestone matrix and less flow through karst conduits.||||||
6976|Gambier Limestone|63122|5|Briefly described|p17 Fig. 4.3|Early Miocene|Late Eocene|Of the Heytesbury Group. Max. thickness: 400m. Geological Province: Otway Basin. ||||||
6976|Gambier Limestone|63124|4|Described|p49 Fig. 5.2, p87 Fig. 5.29, p91|Miocene|Late Eocene|Of the Heytesbury Group. Supersedes "Mount Gambier Limestone". Comprises Greenways, Gellibrand, Camelback, and Green Point Members, and Naracoorte Limestone Member. Max. thickness: 400m. Geological Province: Otway Basin.||||||
6976|Gambier Limestone|63129|6|Mentioned|p139|||Geological Province: Otway Basin. Surface aquifer.||||||30-JAN-08
6976|Gambier Limestone|63222|5|Briefly described|p40, p41|||Dimension stone from the South East, S.A.||||||01-MAR-10
6976|Gambier Limestone|63431|5|Briefly described|p677 Fig. 2|Miocene|Eocene|Of the Heytesbury Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
6976|Gambier Limestone|63887|5|Briefly described|p21 Fig. 1|||||||||
6976|Gambier Limestone|64769|6|Mentioned|p28|Miocene|Miocene|Material mined is named the Gambier Stone. SA.||||||06-MAY-09
6976|Gambier Limestone|64966|5|Briefly described|p137, p144|Middle Miocene|Late Oligocene|Of the Heytesbury Group. Max. thickness: 400m. Major fossiliferous unit with strong erosional unconformity at the top. Geol.province: Gambier Basin. Equivalent to Mannum Limestone in Murray Basin. Forms bedrock platform beneath most of Lacepede Shelf.||||||07-FEB-11
6976|Gambier Limestone|65374|6|Mentioned|p35|||||||||
6976|Gambier Limestone|65552|6|Mentioned|p5 Fig. 3|Miocene|Oligocene|Of Murray Group (western Murray Basin).||||||
6976|Gambier Limestone|65891|5|Briefly described|p221 Fig.5, p229.|Paleogene|Paleogene|Western Otway Basin. Rupelian age. Pure and temporally persistent neritic carbonate unit. Same suite of planktonic foraminifera as Aldinga Member, but with higher numbers plus Globoturborotalita brevis. ||||||
6976|Gambier Limestone|68211|5|Briefly described|p28, p28 Fig.1, p29|Langhian|Bartonian|Occurs extensively in the Gambier Basin and southwestern Murray Basin. Produced as  a dimension stone and sold under the trade name: Compton Sandstone.|c. 40 - 15 Ma, (White 1996)||||Dolomitic rock.|
6976|Gambier Limestone|68811|6|Mentioned|p110, p130, p156 app 1, p192 tbl 46|Tertiary|Tertiary|Hosts an unconfined aquifer. Also referred to informally as the Gambier limestone on p156 app 1.  ||||Overlies the Dilwyn Formation.||
6976|Gambier Limestone|69297|5|Briefly described|p79|Langhian|Rupelian|Otway Basin.||Heytesbury Group|Includes the Greenways Member, Camelback Member, Green Point Member and the Narracoorle Limestone Member.|Overlies the Narrawaturk Marl. Unconformably overlain by the Bridgewater Formation or the Coomandook Formation.|Limestones.|
6976|Gambier Limestone|70029|5|Briefly described|p151-153,165|Miocene|Oligocene|Affected by localised regional uplift related to volcanism (Mount Burr volcanics), and defines a broad dome near volcanic centres, rising from sea level to 60m APSL east of mount Gambier. Subaerially exposed, karstified marine abrasion surface in which dolines and depressions are common.||||Overlain unconformably by Bridgewater Formation.||04-SEP-19
6976|Gambier Limestone|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4|Miocene|Oligocene|Otway Basin: Gambier Embayment and Voluta Trough, and Robe-Penola Trough.||Heytesbury Group.|Naracoorte Limestone, Green Point, Camelback and Greenways Members.|Overlies Narrawaturk Marl. Is overlain by Coomandook Formation.||
6976|Gambier Limestone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Miocene|Miocene|Gambier Embayment and Voluta Trough.||Heytesbury Group.|Greenways, Camelback, Green Point and Naracoorte Members.|Overlies Narrawaturk Marl. Is overlain by Coomandook Formation.||
6976|Gambier Limestone|72445|6|Mentioned|App.7 p7 Fig.4.|Oligocene|Oligocene|See also Gambier Limestone Member in text.||Murray Group||||
6976|Gambier Limestone|73118|6|Mentioned|p17|||||||||
6976|Gambier Limestone|73228|4|Described|p50, p52, p56|Middle Miocene|Late Early Oligocene|Murray Basin. Open shelf environment. Identified in Cooltong 1 drillhole.||||Underlain by Ettrick Formation. Overlain by Mannum Formation, Murray Group.|Includes grey, cream bryozoal limestone, dolomitic in part, with minor glauconite.|
6976|Gambier Limestone|73229|5|Briefly described|p66-67, p70-71, p74|Middle Miocene|Early Miocene|Murray Basin. [Analysed using pXRF; see article]. Incuded in group of early Oligocene to Middle Miocene units p67.|||||Includes limestone, bryzoal, grey-cream, dolomitic in part, minor glauconite.|01-NOV-22
6976|Gambier Limestone|73383|6|Mentioned|p82, p213|||Limestone and sub-litharenite lithologies based on geochemistry using the ChemLith classification and the Herron classification (1988).||||||
6987|Ganantagi Granite|24417|3|Fully described|p111|Late Devonian|Middle Devonian|Previously referred to as "Ganatagai Granite".||||||
6987|Ganantagi Granite|29907|6|Mentioned|p10|||||||||
6987|Ganantagi Granite|29910|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
6987|Ganantagi Granite|29985|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
6987|Ganantagi Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
6987|Ganantagi Granite|33732|6|Mentioned|p114|||||||||
6987|Ganantagi Granite|40328|4|Described|p206|||||||||
6987|Ganantagi Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
6987|Ganantagi Granite|43499|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
6987|Ganantagi Granite|43510|14|Not recorded|p66||Middle Devonian|Trundle-Bogan Gate area||||||
6987|Ganantagi Granite|60009|5|Briefly described|Map Legend|Eifelian|Eifelian|||||||13-JUL-04
6992|Gap Road Conglomerate|42214|6|Mentioned|p466|||||||||
6993|Gap Sandstone|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wallerawang Subgroup (Illawarra Coal Measures). Lithic, medium-grained sandstone. Max. thickness: 13m. Geological Province: Sydney Basin.||||||
6993|Gap Sandstone|39232|4|Described|p110|||||||||
6993|Gap Sandstone|40332|6|Mentioned|Fig.4|||||||||
6993|Gap Sandstone|42657|4|Described|p84|||||||||
6993|Gap Sandstone|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
6993|Gap Sandstone|43194|5|Briefly described|p115|Late Permian|Late Permian|Of Wallerawang Subgroup, Illawarra Coal Measures, western Sydney Basin. Loosely correlated with the 'lithic conglomeratic unit' (now Wallala Formation) of the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
6993|Gap Sandstone|44026|14|Not recorded|p123||Jurassic|Ref. to Wilson 1958,1960 unpubl.(invalid)||||||
6993|Gap Sandstone|68004|4|Described|p60 Table 6, p62.|Late Permian|Late Permian|Western Coalfield. Usually 3 to 5 m thick; 11 m in Wilpinjong area. Locally, truncates the entire State Mine Creek Formation and part or all of the underlying Watts Sandstone.||Unit in Wallerawang Subgroup.||Overlies State Mine Creek Formation. Is overlain by Middle River Coal Member.|Off-white, upward-fining, medium- to coarse-grained, high-angle cross-bedded quartz-lithic to lithic sandstone with a pebbly base.|
7014|Garie Formation|22549|6|Mentioned|p526||Triassic|||||||
7014|Garie Formation|22745|6|Mentioned|Fig2,p127|||Sydney Basin.||||||
7014|Garie Formation|22749|5|Briefly described|p187,Table1p187|||||||||
7014|Garie Formation|22833|6|Mentioned|p653|||of Sydney Basin.||||||
7014|Garie Formation|22857|5|Briefly described|p530 App.1 Tb.A1.9|Middle Triassic|Early Triassic|Of the Gosford Subgroup (Narrabeen Group). Clay pellet sandstone. Max. thickness: 3m. Geological Province: Sydney Basin.||||||
7014|Garie Formation|22969|4|Described|p 6, Fig 4.1b|Middle Triassic|Early Triassic|||||||
7014|Garie Formation|29749|6|Mentioned|p16|||||||||
7014|Garie Formation|30007|6|Mentioned|p61|||||||||
7014|Garie Formation|30707|6|Mentioned|p6|||||||||
7014|Garie Formation|31061|5|Briefly described|p1332|||Depositional environment discussed||||||
7014|Garie Formation|31128|6|Mentioned|Table 1|||||||||
7014|Garie Formation|31297|6|Mentioned|p4|||||||||
7014|Garie Formation|31725|6|Mentioned|p10|||On table||||||
7014|Garie Formation|31886|6|Mentioned|p393|||||||||
7014|Garie Formation|31887|5|Briefly described|p8|||||||||
7014|Garie Formation|32537|5|Briefly described|p3|||||||||
7014|Garie Formation|32799|6|Mentioned|p9|||||||||
7014|Garie Formation|32800|6|Mentioned|p384|||||||||
7014|Garie Formation|32801|6|Mentioned|Fig.10|||||||||
7014|Garie Formation|32802|6|Mentioned|p19|||||||||
7014|Garie Formation|33685|5|Briefly described|p397|||||||||
7014|Garie Formation|33867|6|Mentioned|Table 1|||||||||
7014|Garie Formation|35280|6|Mentioned|p148|||||||||
7014|Garie Formation|35416|6|Mentioned|Fig.2|||Stratigraphy and palynological framework shown||||||
7014|Garie Formation|35647|6|Mentioned|p64|||||||||
7014|Garie Formation|36042|6|Mentioned|Fig.25|||||||||
7014|Garie Formation|36220|4|Described|p71|||See also P65 & Table 20.||||||
7014|Garie Formation|37804|6|Mentioned|Table 1|||||||||
7014|Garie Formation|39293|6|Mentioned|p152|||||||||
7014|Garie Formation|39306|6|Mentioned|p418|||||||||
7014|Garie Formation|39308|6|Mentioned|p494|||See also P505||||||
7014|Garie Formation|40602|3|Fully described|p13|||||||||
7014|Garie Formation|40625|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Early to Middle Triassic||||||
7014|Garie Formation|40631|6|Mentioned|p159|||||||||
7014|Garie Formation|40652|6|Mentioned|p128|||||||||
7014|Garie Formation|40653|6|Mentioned|Fig.20|||||||||
7014|Garie Formation|41102|5|Briefly described|p319|||||||||
7014|Garie Formation|41718|6|Mentioned|p237|||||||||
7014|Garie Formation|42737|5|Briefly described|map legend|Triassic||||||||
7014|Garie Formation|42896|3|Fully described|p29, Table 2|||of Gosford Subgroup||||||
7014|Garie Formation|42925|5|Briefly described|Table 18||Middle Triassic|||||||
7014|Garie Formation|42926|4|Described|map legend||Middle Triassic|||||||
7014|Garie Formation|61315|5|Briefly described|Table SY2|Middle Triassic|Middle Triassic|Of the Gosford Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
7014|Garie Formation|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Narrabeen Group.||Overlies Bald Hill Claystone. Is overlain by Hawkesbury Sandstone.||
7014|Garie Formation|67560|5|Briefly described|p258, p261 Fig.3|Triassic|Triassic|Constrained by the age of the Narrabeen Group.||Of the Narrabeen Group.||Overlain by Newport Formation. Underlain gradationally by Bald Hill Claystone.|Clay pellet claystone, dark lithic fine sandstone, chocolate claystone bands.|23-MAY-17
7014|Garie Formation|70878|5|Briefly described|p726|Olenekian|Olenekian|Southern Coalfield, Sydney Basin. CA-IDTIMS age from a tuff bed.|248.33 +/- 0.13 Ma (Metcalfe et al., 2015).|||||25-SEP-18
7014|Garie Formation|73304|5|Briefly described|p64-66, p72-74, p76|Olenekian|Olenekian|Sydney Basin, southern. Dating by U-Pb CA-TIMS.|248.23 +/- 0.32 Ma, 247.87 +/- 0.31 Ma|Narrabeen Group||Possibly overlain by Newport Formation.||
7019|Garoo Conglomerate Member|34080|6|Mentioned|p248|||||||||
7019|Garoo Conglomerate Member|34555|6|Mentioned|p241|||||||||
7019|Garoo Conglomerate Member|37987|6|Mentioned|p224|||||||||
7019|Garoo Conglomerate Member|39331|6|Mentioned|Table 10-1|||||||||
7019|Garoo Conglomerate Member|43399|2|Defined|p196,198,201,205||Early Carboniferous|Early L.Carb||||||
7019|Garoo Conglomerate Member|43406|14|Not recorded|p42,44||Tournaisian|Part of Parry Group (L.Carb)||||||
7019|Garoo Conglomerate Member|43407|14|Not recorded|Map Legend|||(Provisional Edition) Part of Tangaratta Formation||||||
7019|Garoo Conglomerate Member|43418|14|Not recorded|Map Legend|||||||||
7019|Garoo Conglomerate Member|44244|5|Briefly described|p21|||Of the Goonoo Goonoo Mudstone.  Conodont-bearing deposit.||||||18-AUG-04
7025|Garra Formation|5178|6|Mentioned|p106 Fig.1, p107, p108, p109 Table 4|||At Wellington it is over 1km thick and dominated by carbonates (including fossiliferous limestones)with minor siltstones, shales and dolomitic limestones.||||||
7025|Garra Formation|5252|5|Briefly described|p66, p70|Pragian|Lochkovian|Includes late Silurian to Early Devonian brachiopod fauna.||||||
7025|Garra Formation|22768|6|Mentioned|p180|||||||||
7025|Garra Formation|22857|4|Described|p180, p454 App.1, Tb.A1.6|Emsian|Pragian|Of Gregra Group. Fossiliferous limestone, minor cherty tuffaceous arenite and siltstone, tuff; contains brachiopods, corals, conodonts. Overlies Berkley Formation? Max. thickness: 1015m. Geol. Prov.: Molong Rise/Cowra Trough. See also p466 App.1 Tb.A1.6.||||||
7025|Garra Formation|22952|6|Mentioned|Table1p179||Devonian|||||||
7025|Garra Formation|23043|5|Briefly described|Map Legend|Pragian|Lochkovian|Of Gregra Group.||||||28-AUG-08
7025|Garra Formation|23170|2|Defined|p202|Emsian|Lochkovian|Of Gregra Group.||||||28-AUG-08
7025|Garra Formation|23214|3|Fully described|p182|Pragian|Lochkovian|Of Gregra Group. Originally named Garra Beds. Fossilerous limestone with minor cherty and volcaniclastic sandstone, fissile shale and marly siltstone, with minor rare tuff. Max. thickness 1015m.||||||
7025|Garra Formation|23555|5|Briefly described|p3|Middle Devonian|Middle Devonian|||||||
7025|Garra Formation|24126|6|Mentioned|p135|||||||||
7025|Garra Formation|24248|5|Briefly described|p59|Devonian|Devonian|||||||
7025|Garra Formation|24611|6|Mentioned|p195, p198|Emsian|Pragian|||||||
7025|Garra Formation|24612|5|Briefly described|p12|Pragian|Pragian|Contains Carlinastraea fauna.||||||
7025|Garra Formation|29362|6|Mentioned|Table 1|||Lower-Middle Devonian.||||||
7025|Garra Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
7025|Garra Formation|30100|6|Mentioned|p205|||Stratigraphy.||||||
7025|Garra Formation|30597|4|Described|p29|||Lower Devonian age. Conodonts||||||
7025|Garra Formation|30814|6|Mentioned|Table.2|||||||||
7025|Garra Formation|31161|5|Briefly described|PA4|||||||||
7025|Garra Formation|31331|6|Mentioned|p182|||||||||
7025|Garra Formation|31332|6|Mentioned|p30|||||||||
7025|Garra Formation|31502|5|Briefly described|p94|||Coral fauna. See also P95 for age.||||||
7025|Garra Formation|31543|4|Described|p113|||See also P116-117||||||
7025|Garra Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
7025|Garra Formation|32150|6|Mentioned|p32|||Refers Etheridge (1903) ?Emsian||||||
7025|Garra Formation|32151|6|Mentioned|p217|||Stratigraphy||||||
7025|Garra Formation|32155|6|Mentioned|p185|||||||||
7025|Garra Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
7025|Garra Formation|32583|6|Mentioned|p384|||||||||
7025|Garra Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
7025|Garra Formation|32672|6|Mentioned|p673|||||||||
7025|Garra Formation|32708|6|Mentioned|p414|||||||||
7025|Garra Formation|32865|6|Mentioned|p483|||||||||
7025|Garra Formation|32982|6|Mentioned|p657|||Fauna||||||
7025|Garra Formation|32983|6|Mentioned|p388|||||||||
7025|Garra Formation|32986|6|Mentioned|p2|||Stratigraphy||||||
7025|Garra Formation|33006|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
7025|Garra Formation|33066|6|Mentioned|p235|||Dev. Fauna||||||
7025|Garra Formation|33116|6|Mentioned|p229|||L.Dev.||||||
7025|Garra Formation|33121|6|Mentioned|p85|||Early Dev.||||||
7025|Garra Formation|33282|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
7025|Garra Formation|33285|5|Briefly described|p21|||Early Dev.||||||
7025|Garra Formation|33329|6|Mentioned|p119|||Siegenian - Emsian. Corals.||||||
7025|Garra Formation|33392|6|Mentioned|p93|||Fauna.||||||
7025|Garra Formation|33434|6|Mentioned|p80|||||||||
7025|Garra Formation|33437|6|Mentioned|p64|||Correlation. Conodonts P66.||||||
7025|Garra Formation|33732|4|Described|p115|||||||||
7025|Garra Formation|34109|6|Mentioned|p158|||Devonian||||||
7025|Garra Formation|34250|6|Mentioned|p7|||Siegenian ? - Emsian||||||
7025|Garra Formation|34403|3|Fully described|p138|||||||||
7025|Garra Formation|34404|6|Mentioned|Fig.3.4b|||||||||
7025|Garra Formation|34405|6|Mentioned|Fig.3.9|||||||||
7025|Garra Formation|34406|6|Mentioned|p223|||||||||
7025|Garra Formation|34478|6|Mentioned|p472|||||||||
7025|Garra Formation|34509|6|Mentioned|p281|||Emsian. See also PP288,292 etc.||||||
7025|Garra Formation|34510|6|Mentioned|p304|||Emsian. See also PP305,307||||||
7025|Garra Formation|34567|6|Mentioned|p159|||See also PP160-164||||||
7025|Garra Formation|34692|6|Mentioned|p184|||||||||
7025|Garra Formation|35246|6|Mentioned|p169|||On a table.||||||
7025|Garra Formation|36118|6|Mentioned|p69|||||||||
7025|Garra Formation|38064|6|Mentioned|p39|||||||||
7025|Garra Formation|38378|6|Mentioned|p134|||||||||
7025|Garra Formation|39331|6|Mentioned|p87|||See also Fig.8-1||||||
7025|Garra Formation|39654|6|Mentioned|M85|||||||||
7025|Garra Formation|39663|6|Mentioned|Table 1|||||||||
7025|Garra Formation|40328|6|Mentioned|p160|||See also Plate 3||||||
7025|Garra Formation|40406|6|Mentioned|p3|||||||||
7025|Garra Formation|41000|6|Mentioned|p284|||||||||
7025|Garra Formation|41108|5|Briefly described|p210|||||||||
7025|Garra Formation|42032|6|Mentioned|p491|||||||||
7025|Garra Formation|42033|6|Mentioned|p653|||||||||
7025|Garra Formation|42051|6|Mentioned|p140|||||||||
7025|Garra Formation|42414|6|Mentioned|p59|||||||||
7025|Garra Formation|42421|6|Mentioned|p303|||||||||
7025|Garra Formation|42449|6|Mentioned|p26|||||||||
7025|Garra Formation|42477|5|Briefly described|p100|||||||||
7025|Garra Formation|42933|6|Mentioned|p242|||||||||
7025|Garra Formation|43039|4|Described|p6|||||||||
7025|Garra Formation|43263|6|Mentioned|Map Legend||Early Devonian|||||||
7025|Garra Formation|43344|14|Not recorded|p8|Early Devonian||||||||
7025|Garra Formation|43383|14|Not recorded|p13|Middle Devonian|Early Devonian|||||||
7025|Garra Formation|43461|14|Not recorded|table p621||Emsian|||||||
7025|Garra Formation|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
7025|Garra Formation|43479|14|Not recorded|p126,151|Middle Devonian|Early Devonian|||||||
7025|Garra Formation|43515|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
7025|Garra Formation|43516|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
7025|Garra Formation|43517|14|Not recorded|p153-55|Emsian|Siegenian|||||||
7025|Garra Formation|43521|14|Not recorded|p91|Middle Devonian|Early Devonian|See also Garra Beds||||||
7025|Garra Formation|43522|2|Defined|p85-90||Early Devonian|||||||
7025|Garra Formation|43523|14|Not recorded|p426,432,433||Early Devonian|||||||
7025|Garra Formation|43524|14|Not recorded|p11|||||||||
7025|Garra Formation|43525|14|Not recorded|p123,map p124,||Emsian|Table p126, 127-130,Table p131,132||||||
7025|Garra Formation|43526|14|Not recorded|p544-598|Middle Devonian|Early Devonian|Describes fauna||||||
7025|Garra Formation|43527|14|Not recorded|p518-22,535-65|||Probably Emsian, possibly extending to early Couvinian or Siegenian||||||
7025|Garra Formation|43530|14|Not recorded|p1026,1028,1033-34||Siegenian|||||||
7025|Garra Formation|43640|5|Briefly described|Map Legend||Devonian|||||||
7025|Garra Formation|43782|5|Briefly described|Map Legend|Emsian|Lochkovian|Of Gregra Group.||||||28-AUG-08
7025|Garra Formation|44416|14|Not recorded|p368,375,378||Early Devonian|||||||
7025|Garra Formation|45075|6|Mentioned|p28|||Devonian||||||
7025|Garra Formation|45078|6|Mentioned|p10|||||||||
7025|Garra Formation|48926|6|Mentioned|p19|||P19 et seq.||||||
7025|Garra Formation|50590|5|Briefly described|Map Legend|Devonian|Devonian|Of the Gregra Group.  Fossiliferous limestone; minor cherty, tuffaceous sandstone and siltstone.||||||
7025|Garra Formation|60332|5|Briefly described|p938|Early Devonian|Early Devonian|Conformably overlies Cuga Burga Volcanics.||||||28-AUG-08
7025|Garra Formation|61859|6|Mentioned|p5|||Originally the Garra Beds of Joplin and Culey (1938); renamed the Garra Formation by Strusz (1965, 1967). The authors of this work rename it the Garra Limestone to recognise the overwhelming dominance of that lithology.||||||
7025|Garra Formation|64296|5|Briefly described|p84||Early Devonian|On the Molong High, west of Hill End Trough. Includes limestone lithology. ||||||
7025|Garra Formation|65940|6|Mentioned|p203-204|Emsian|Emsian|Contains A. aff. clermontense (Strusz 1966); P. oculoides (Hill, 1942d).||||||
7025|Garra Formation|66197|5|Briefly described|p634, p633 Fig.4c|Emsian|Lochkovian|Cowra Trough-Molong High. Shallow marine limestone. Overlies the Berkley Formation and Cuga Burga Volcanics.||||||13-MAR-12
7025|Garra Formation|68003|5|Briefly described|p24 Fig.3-e, p143. |Pragian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gregra Group.|||Well-bedded, fossiliferous limestone; calcareous sandstone, siltstone, breccia; shale; minor tuffaceous sandstone.|
7025|Garra Formation|68298|5|Briefly described|p222|Pragian|Lochkovian|Rare placoderm remains of late Lochkovian - early Pragian age (pesavus-sulcatus Zones; Strusz, 1972; Mawson et al., 1985).||||||
7025|Garra Formation|68592|6|Mentioned|p1899|Early Devonian|Early Devonian|Wellington Caves district. Contains receptaculitid fossils.||||||
7025|Garra Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Grega Group||||
7025|Garra Formation|71040|6|Mentioned|p19|Early Devonian|Early Devonian|||||||
7025|Garra Formation|71600|5|Briefly described|p22, p23 Fig 1, p24-30, 34, 35|Emsian||Geological province: Lachlan Fold Belt. Replaces Garra Beds; see Strusz 1965a-b.  Conodont data indicate that all fossil coral specimens are from the Pragian to early Emsian upper part of the Garra Formation.||Unit of Gregra Group.|||Well bedded, fossiliferous limestone; calcareous sandstone, siltstone, breccia; shale; minor tuffaceous sandstone|
7025|Garra Formation|71656|6|Mentioned|p35|||Mentioned only in text as from the Wellington Caves district of NSW.||||||
7025|Garra Formation|73143|6|Mentioned|p9-11|Emsian|Lochkovian|Late Lochkovian to early Emsian age. Contains rugose coral, and Favosites allani tabulate coral (Hill and Jones, 1940).||||||
7025|Garra Formation|73299|6|Mentioned|p1103, p1105|Early Devonian|Early Devonian|Molong High, Cowra Trough.||||Faulted over the Catombal Group in the Mount Arthur Syncline. Overlies the Cuga Burga Volcanics, Berkley Formation, underlies the Catombal Group.||
7046|Gattamurh Granite|23309|6|Mentioned|p431 Appendix 1|||G73, I-Type. Supersedes Willis Granite.||||||22-FEB-13
7046|Gattamurh Granite|42726|5|Briefly described|map legend|||||||||
7046|Gattamurh Granite|68115|5|Briefly described|pp6-7.|||Deddick Zone. White and Chappell (1988); changed to Willis (?Granite) in Chappell et al. (1991) as the locality of Willis is within the pluton's outcrop. The name reverted to Gattamurh Granite in VandenBerg et al. (2000) as it had precedence, even though the pluton does not lie on Gattamurh Creek (presumably the source of the name).||||||
7046|Gattamurh Granite|68116|5|Briefly described|Appendix, Map 28.|Early Devonian|Wenlock||||||Granite: mafic I-type; magnetic.|
7050|Gatton Sandstone|12597|5|Briefly described|p492 Tb.1|Toarcian|Pliensbachian|Clarence-Moreton Basin. 500m thick. The coal is of no economic significance.||Unit in Marburg Subgroup.||Overlies Ripley Road Sandstone. Is overlain by Koukandowie Formation.|Medium- to very coarse-grained, quartz-feldspathic-lithic sandstone including beds of pebbly sandstone with calcareous cement; minor beds of conglomerate and siltstone-shale, and fossil wood; thin coal seams.|
7050|Gatton Sandstone|13516|5|Briefly described|p159 fig 8|Early Jurassic|Early Jurassic|From Clarence-Moreton Basin.||Of Marburg Subgroup||||
7050|Gatton Sandstone|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Quartz-lithic arenite, conglomerate, minor fossil wood. Contains the Calamia Member. Max. thickness: 600m. Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|22865|6|Mentioned|Fig.22.10ap318|||||||||
7050|Gatton Sandstone|23799|5|Briefly described|p48, p10 Tb. 1|Jurassic|Jurassic|Of Marburg Group.  Lithic labile and feldspathic labile sandstone.  Overlain by Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Marburg Subgroup.||||||
7050|Gatton Sandstone|23811|5|Briefly described|Map Legend|Toarcian|Pliensbachian|Of Marburg Subgroup.  Thin- to thick-bedded, coarse- to medium-grained, feldspathic to lithic feldspathic sandstone with clay matrix; subordinate intervals of granule, pebble and minor cobble polymictic conglomeGeological Province: Clarence-Moreton Basin.||||||20-DEC-04
7050|Gatton Sandstone|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Maximum thickness: 600m. Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Marburg Subgroup (Bundamba Group).  Lithic labile and feldspathic labile sandstone (Clarence-Moreton Basin).||||||
7050|Gatton Sandstone|29591|6|Mentioned|p83|||||||||
7050|Gatton Sandstone|31118|4|Described|Table 3|||Lithology||||||
7050|Gatton Sandstone|41631|4|Described|p17|||See also Fig.2||||||
7050|Gatton Sandstone|42248|2|Defined|App.1 p412|Early Jurassic||||||||15-MAY-19
7050|Gatton Sandstone|42463|6|Mentioned|Fig.3 P170|||||||||
7050|Gatton Sandstone|42869|5|Briefly described|Table 1, P33|||Of Marburg Group.||||||27-AUG-08
7050|Gatton Sandstone|42951|5|Briefly described|Fig.11|||Of Marburg Subgroup.||||||27-AUG-08
7050|Gatton Sandstone|43001|6|Mentioned|Fig.6,p123|||||||||
7050|Gatton Sandstone|43150|5|Briefly described|Map Legend||Jurassic|Of the Marburg Subgroup.  Geological Province: Clarence-Moreton Basin.||||||12-APR-05
7050|Gatton Sandstone|43736|5|Briefly described|Table 1,p4|||||||||
7050|Gatton Sandstone|44026|14|Not recorded|p123||Jurassic|||||||
7050|Gatton Sandstone|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Marburg Subgroup.  Overlies: Woogaroo Subgroup.  Underlies: Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
7050|Gatton Sandstone|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Formation.||||||
7050|Gatton Sandstone|60281|5|Briefly described|p24, Fig.18 App 1|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group).  Sandstone, conglomerate, minor fossil wood.  Overlain by Koukandowie Formation; overlies the Ripley Road Sandstone.  Max. thickness: 800m.  Geological Province: Clarence-Moreton Basin.||||||17-MAR-05
7050|Gatton Sandstone|60993|3|Fully described|p21, p18|||Supersedes the Gatton Sst Mbr. Includes the conglomeratic beds of the former Tenthill Conglomerate Mbr or Winwill Conglomerate Mbr. Overlies: Woogaroo Subgp. Max. thickness: >100m. Geol. Prov: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|60995|4|Described|p62, p51 Fig. 3|Early Jurassic|Early Jurassic|Of Marburg Subgp. Formerly informally known as "Peak Fm"; and partly equivalent to "Olive Gap Fm". Overlies Laytons Range Conglom.  Max. thick: ~500m. Geol. Prov: Clarence-Moreton Basin. Equivalent to Blaxland Fossil Wood Conglom. mbr.||||||
7050|Gatton Sandstone|60996|5|Briefly described|p72, p93||| Unconformably overlies the Laytons Range and Aberdare Conglomerates, or Raceview Fm; and also overlaps Ripley Road Sst onto basement at the basin edges.  Max. thickness: 1100m. Geol. Prov: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|60997|5|Briefly described|p138|Toarcian|Sinemurian|Formerly the "Blaxland Fossil Wood Conglomerate Member" (McElroy 1963). Conformably overlain by Koukandowie Formation. Geological Province: Clarence-Moreton Basin. ||||||
7050|Gatton Sandstone|60998|5|Briefly described|p146 Fig. 2|||Characterised by medium to coarse-grained quartz-lithic sandstone with mainly upward-fining cycles. Overlain by Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|60999|5|Briefly described|p164, p173|Early Jurassic|Early Jurassic|Of the Marburg Subgroup. Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6, p176. Broadly correlated in time with uppermost Precipice Sandstone and lowermost Evergreen Formation, both in the Surat Basin. ||||||
7050|Gatton Sandstone|61001|6|Mentioned|p189|||Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|61002|6|Mentioned|p202|||Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
7050|Gatton Sandstone|61005|5|Briefly described|p242|||See also p255 Figs. 23, 24 and 25. ||||||
7050|Gatton Sandstone|61006|5|Briefly described|p277|Jurassic|Jurassic|Includes the Calamia Member. Labile sandstone. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285.||||||
7050|Gatton Sandstone|63731|5|Briefly described|Map legend|Jurassic|Jurassic|Of the Marburg Subgroup. Includes the Koreelah Conglomerate Member. Thick-bedded, medium- to coarse-grained, quartz-lithic amd feldspathic sandstone.||||||12-DEC-07
7050|Gatton Sandstone|63748|5|Briefly described|p21-22|Early Jurassic|Early Jurassic|Of Marburg Subgp. Includes Koreelah Conglomerate Member at base. Unconformable on Texas beds and Silverwood Group; conformable below Koukandowie Fm. Geol.province: Clarence-Moreton Basin. Quartz-lithic and feldspathic sandstone in a calcareous cement.||||||07-FEB-11
7050|Gatton Sandstone|64289|5|Briefly described|p6 Fig. 2, p17|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Overlain by Koukandowie Formation. Max. thickness: 500m. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
7050|Gatton Sandstone|64665|5|Briefly described|p53 Fig.2, p59.|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Correlates with the middle part of Landsborough Sandstone (Southern Nambour Basin).||Basal unit in Marburg Subgroup.||Overlies Ripley Road Sandstone.Is overlain by Ma Ma Creek Member (of Koukandowie Formation).||
7050|Gatton Sandstone|67402|5|Briefly described|p165 tbl LPB1|Sinemurian|Sinemurian|Clarence-Moreton Basin. Deposited in a braided stream to floodplain environment. Sandstones are often of reservoir quality. Greater than 150m thick. See also p187, p188, p190, p192, p193, p307.||Marburg Subgroup|Includes the Calamia Member.|Overlies the Ripley Road Sandstone. Overlain by the Ma Ma Creek Member,  Koukandowie Formation.|Medium to very coarse grained, quartz-feldspathic-lithic sandstone.|
7050|Gatton Sandstone|68135|5|Briefly described|p52 fig 2b, p64|Pleinsbachian||Clarence-Moreton Basin. Includes plant macrofossils and invertebrate fossils, including the oldest Australian leech cocoons.||||Overlies Ripley Road Sandstone. Is overlain by Koukandowie Formation.|Cross-bedded sandstone.|14-SEP-17
7050|Gatton Sandstone|69297|5|Briefly described|p487 fig 5.38, p488|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 200-600m thick. Appears as Gatton Formation on p488. Potential hydrocarbon reservoir rock. ||Mauburg Subgroup|Includes the Koreelah Conglomerate and the Calamia Member.||Sandstone, conglomerate and minor fossilised wood.|
7050|Gatton Sandstone|69594|4|Described|p519, p544-547, p572|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.||Marburg Subgroup.|Calamia Member, Koreelah Conglomerate Member.|Overlies Ripley Road Sandstone. Is overlain by Ma Ma Creek Member (Koukandowie Formation). Correlated with upper Precipice Sandstone and lower Evergreen Formation.|Predominantly thick-bedded, medium- and coarse-grained, quartz-lithic and feldspathic sandstone, blue-grey (fresh) commonly with calcareous cement; large-scale trough cross-bedding, carbonised wood fragments and pebble beds generally characteristic.|
7050|Gatton Sandstone|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Marburg Subgroup.||||
7050|Gatton Sandstone|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
7050|Gatton Sandstone|70821|5|Briefly described|p80|||Clarence-Moreton Basin. Aquifer: generally artesian.||Marburg Subgroup.|Koreelah Conglomerate Member.|Overlies Ripley Road Sandstone. Is overlain by Koukandowie Formation.||
7050|Gatton Sandstone|71628|6|Mentioned|p9: 5, 32|||||||Overlies Bruxner Granodiorite and (locally) Jenny Lind Tonalite.||
7050|Gatton Sandstone|71805|5|Briefly described|p76|Pleinsbachian|Sinemurian|Clarence-Moreton Basin.||Marburg Subgroup||Overlies the Ripley Road Sandstone. Overlain by the Ma Ma Creek Member.||
7050|Gatton Sandstone|72921|5|Briefly described|p15 Fig.2.|Early Jurassic|Early Jurassic|Shown as located within the Clarence-Moreton Basin.||||Overlies Ripley Road Sandstone and underlies Koukandowie Formation|Includes fossiliferous sandstone.|
7050|Gatton Sandstone|73570|5|Briefly described|p912 Fig.2, p913-914, p915 Fig.4|Early Jurassic|Early Jurassic|Clarence-Morton Basin.|187+/-1 Ma|Marburg Subgroup||||
7086|Geehi Granite|29953|6|Mentioned|p3|||||||||
7086|Geehi Granite|40328|4|Described|p206|||||||||
7086|Geehi Granite|40498|6|Mentioned|p392|||||||||
7086|Geehi Granite|45087|5|Briefly described|p36|||Chemical analyses.||||||
7090|Geera Clay|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 29, 50, 158|Miocene|Oligocene|Lawrence (1966). Murray Basin. 170m thick. A significant aquiclude. See also p178-179, 231, 285, 300, 304, 315, 318, 320.||Murray Group.||Overlies Renmark Group. Is overlain by Winnambool Formation. Is separated from the overlying Parilla Sand by the Mologa Surface. Grades westwards into the Ettrick Marl.|Sparingly fossiliferous, dark grey to black clay.|
7090|Geera Clay|10010|5|Briefly described|p12 Fig. 3|Middle Miocene|Late Oligocene|Of the Murray Group. Overlain by Renmark beds. Geological Province: Murray Basin.||||||13-AUG-07
7090|Geera Clay|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|22773|5|Briefly described|p351,Fig24.8p352|||||||||
7090|Geera Clay|22799|2|Defined|p31|Middle Miocene|Late Oligocene|Of the Murray Group.||||||29-JUL-08
7090|Geera Clay|22857|5|Briefly described|p351, p353 Fig. 24.9|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
7090|Geera Clay|22887|5|Briefly described|Fig.6 p13|Miocene|Oligocene|||||||
7090|Geera Clay|22893|3|Fully described|p28 fig8a,9 table3|Miocene|Miocene|||||||
7090|Geera Clay|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
7090|Geera Clay|23226|6|Mentioned|p889,890,891|||Of Murray Supergroup.||||||
7090|Geera Clay|23884|5|Briefly described|p153, p155 Fig.13.2|Miocene|Oligocene|Geological Province: Murray Basin.||||||
7090|Geera Clay|23909|6|Mentioned|p298|||||||||
7090|Geera Clay|23921|5|Briefly described|p1109|Early Miocene|Early Miocene|Geological Province: Murray Basin.||||||
7090|Geera Clay|24100|6|Mentioned|p99|||Geological Province: Murray Basin.||||||19-APR-05
7090|Geera Clay|24177|5|Briefly described|p69|Middle Miocene|Late Oligocene|Renmark Group grades westward into this deposit (Lawrence, 1975). Geological Province: Murray Basin.||||||
7090|Geera Clay|24551|6|Mentioned|p322 Fig. 10.29|||Of the Murray Group.||||||
7090|Geera Clay|24563|5|Briefly described|p485|||Included in the Murray Supergroup by Lukasik and James (1998).  However, Murray Supergroup now abandoned and Murray Group reinstated - Geera Clay not included.  Geological Province: Murray Basin.||||||
7090|Geera Clay|29591|6|Mentioned|Table 20|||||||||
7090|Geera Clay|29898|6|Mentioned|Table 20|||||||||
7090|Geera Clay|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
7090|Geera Clay|30934|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
7090|Geera Clay|30935|6|Mentioned|Map legend|Tertiary|Tertiary|Subsurface||||||
7090|Geera Clay|30936|6|Mentioned|Map legend|Eocene|Eocene|||||||
7090|Geera Clay|31741|6|Mentioned|p6|||||||||
7090|Geera Clay|31746|3|Fully described|p195|||||||||
7090|Geera Clay|31747|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
7090|Geera Clay|34735|4|Described|p32|||Also mention P31.||||||
7090|Geera Clay|34813|6|Mentioned|p62|||||||||
7090|Geera Clay|37796|6|Mentioned|p164|||||||||
7090|Geera Clay|37809|6|Mentioned|p7|||||||||
7090|Geera Clay|38601|4|Described|p7|||||||||
7090|Geera Clay|39329|6|Mentioned|Fig.1|||||||||
7090|Geera Clay|39929|4|Described|p267|||||||||
7090|Geera Clay|40820|6|Mentioned|Fig.4|||||||||
7090|Geera Clay|41423|6|Mentioned|p284|||||||||
7090|Geera Clay|41511|6|Mentioned|p20|||||||||
7090|Geera Clay|41868|6|Mentioned|p551|||||||||
7090|Geera Clay|42125|5|Briefly described|p134|||See also Fig.5||||||
7090|Geera Clay|42126|6|Mentioned|p149|||||||||
7090|Geera Clay|42130|6|Mentioned|p271|||||||||
7090|Geera Clay|42132|6|Mentioned|p295|||||||||
7090|Geera Clay|42133|6|Mentioned|p301|||||||||
7090|Geera Clay|42134|4|Described|p339|||||||||
7090|Geera Clay|42137|4|Described|p372,p376|||See also Table 3||||||
7090|Geera Clay|42138|6|Mentioned|p388|||||||||
7090|Geera Clay|42375|5|Briefly described|p26|early Miocene|late Oligocene|Murray Basin||||||
7090|Geera Clay|42509|5|Briefly described|p2|||||||||
7090|Geera Clay|42510|5|Briefly described|p35|||||||||
7090|Geera Clay|42511|6|Mentioned|Fig.2 P55|||||||||
7090|Geera Clay|42512|6|Mentioned|p68|||||||||
7090|Geera Clay|42514|6|Mentioned|p116|||||||||
7090|Geera Clay|42515|6|Mentioned|p134|||||||||
7090|Geera Clay|42517|5|Briefly described|p169|||||||||
7090|Geera Clay|42518|5|Briefly described|p185|||||||||
7090|Geera Clay|42519|6|Mentioned|p205|||||||||
7090|Geera Clay|42720|5|Briefly described|map legend|Miocene|Oligocene|||||||
7090|Geera Clay|42813|5|Briefly described|p24|||||||||
7090|Geera Clay|42827|3|Fully described|p269|||Of Murray Group.||||||03-FEB-09
7090|Geera Clay|42881|4|Described|Fig.3, P84|||||||||
7090|Geera Clay|42966|2|Defined|p139|Middle Miocene|Late Oligocene|Of the Murray Group.||||||03-FEB-09
7090|Geera Clay|43655|5|Briefly described|p40-846|||||||||
7090|Geera Clay|43669|4|Described|p22|Middle Miocene|Early Miocene|||||||
7090|Geera Clay|43780|6|Mentioned|p5|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|43790|5|Briefly described|p383|||||||||
7090|Geera Clay|43791|5|Briefly described|p371|||||||||
7090|Geera Clay|43804|5|Briefly described|p47|Miocene|Oligocene|||||||
7090|Geera Clay|44133|5|Briefly described|p159|Middle Miocene|Early Miocene|Of the Muray Group. Geological Province: Murray Basin. ||||||
7090|Geera Clay|44188|5|Briefly described|Map Legend|Late Miocene|Late Oligocene|Geological province: Murray Basin. Poorly consolidated, plastic to friable, black, grey dark green clay, silt, minor sand; commonly glauconitic, fossiliferous, calcareous, carbonaceous; local sandy dolomitic intercalations.||||||15-MAY-08
7090|Geera Clay|44191|5|Briefly described|Map Legend|Middle Miocene|Late Oligocene|||||||
7090|Geera Clay|47060|6|Mentioned|p183|||||||||
7090|Geera Clay|49038|4|Described|Table 2|||||||||
7090|Geera Clay|49040|5|Briefly described|p12|||See also P11||||||
7090|Geera Clay|50154|5|Briefly described|p135|||Of the Murray Group.||||||
7090|Geera Clay|60452|5|Briefly described|p33|Middle Miocene|Late Oligocene|Marine Deposits.||||||
7090|Geera Clay|60491|4|Described|p21|||Of the Murray Group. Conformably overlies the Olney Formation. Geological Province: Murray Basin.||||||
7090|Geera Clay|60538|5|Briefly described|p480 Fig. 19|||Geological Province: Murray Basin.||||||
7090|Geera Clay|61155|5|Briefly described|p4, p18|Middle Miocene|Late Oligocene|Of the Murray group. Carbonaceous silts and minor carbonates. Interfingers with Olney Formationand ettrick Formation. Max. thickness: 150m.  Geological Province: Murray Basin.||||||03-MAR-10
7090|Geera Clay|61181|5|Briefly described|p153 Fig. 47|||Carbonaceous clay. ||||||
7090|Geera Clay|61314|5|Briefly described|p129|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||
7090|Geera Clay|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999)  incorporates this unit and the Ettrick and Winnambool Formations into their new Murray Supergroup.  These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
7090|Geera Clay|63460|5|Briefly described|p838, p839 Fig. 2b|Middle Miocene|Late Oligocene|Geological province: Murray Basin. Bioturbated, dark grey to black, slightly calcareous and poorly fossiliferous clay. Equivalent to Winnambool and Ettrick Formations. ||||||
7090|Geera Clay|63777|6|Mentioned|p1104 Fig. 1, p1105|||Geological Province: Murray Basin.||||||18-MAR-09
7090|Geera Clay|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Lagoonal and marginal marine muddy facies.||||||
7090|Geera Clay|64237|5|Briefly described|p17, p18|Late Oligocene|Late Oligocene|Included in the Murray Group stratigraphic scheme by Lawrence (1966), retained through the various revisions of the Murray Group up to Murray Supergroup; and is now included in the reinstated Murray Group in South Australia.||||||
7090|Geera Clay|64823|5|Briefly described|p1011|Late Miocene|Paleocene|Clays and marls. Geological province: Murray Basin||||||
7090|Geera Clay|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Early Oligocene|Clay/claystone with occasional dolomite. Deposited during a marine incursion. Unconformably underlies Loxton-Parilla Sands and Bookpurnong beds. Contemporaneous with Murray Group and Winnambool, Ettrick and Olney Formations.||||||
7090|Geera Clay|65719|5|Briefly described|p7|Miocene|Oligocene|In Murray Basin. Lateral equivalent of Mystic Park Formation. Marginal marine or paralic.||||||10-MAY-12
7090|Geera Clay|66573|6|Mentioned|p873|Miocene|Miocene|Murray Basin. Marine.||||||
7090|Geera Clay|67127|6|Mentioned|p73|||||||Overlies the Renmark Group. Underlies the Parilla Sand.||
7090|Geera Clay|67179|6|Mentioned|p579|||||||||
7090|Geera Clay|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||Unit in Murray Group.||||
7090|Geera Clay|68140|5|Briefly described|p1700 Fig.1, p1701, p1704 Fig.5|Neogene|Paleogene|Up to 75m thick. Acts as an effective aquitard. Middle Tertiary age.|||||Comprises massive clays with minor sand and silt layers.|09-FEB-18
7090|Geera Clay|68189|5|Briefly described|p27 Tb.3.2, p29|Miocene|Oligocene|Depositional environment: marginal marine, lagoonal, tidal flats. The Geera Clay is the only part of the Murray Group previously recorded in ST ARNAUD. It is an important barrier which separates water flows between the Parilla Sand and Renmark Groups.||Of the Murray Group.||Underlain by the Olney Formation. Overlain by the Parilla Sand.|Comprises plastic black-green mud and sand; glauconitic.|
7090|Geera Clay|68194|5|Briefly described|p23|Miocene|Oligocene|Lawrence (1966). Murray Basin. Over 50m thick.||Unit in Murray Group.||Lateral facies equivalent of Calivil Formation.|Glauconitic claystone and interbedded dolomitic siltstone.|
7090|Geera Clay|68715|6|Mentioned|p31 Fig.5|Miocene|Miocene|Murray Basin. Early to Middle Miocene age.||Murray Group.||||07-APR-17
7090|Geera Clay|70718|4|Described|p24-p25, p103|Middle Miocene|Late Oligocene|Murray Basin. Deposited as a marginal-marine muddy facies. Improperly concatenated as Geera Formation on p24. Approximately 150m thick. Silt and sand are primarily terriginous in origin.||Murray Group|||Black, olive grey, dark-grey or dark-green silty mud, silt and clay with minor dark sand.|
7090|Geera Clay|71593|6|Mentioned|p52-p54|||||||||
7090|Geera Clay|72445|5|Briefly described|.App.1, App.2; App.6 p1, p3-4, p6; App.7|Miocene|Oligocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). See also App. 7 p2, p4, p16-18. Identified in Stavely 12,16. App.6, App.7 propose Early Miocene Geera Clay at 65m in Stavely 11, but this is identified as Olney Formation, Renmark Group in well logs.||Murray Group||Underlies Port Campbell Limestone,conformity; Calivil Formation, sharp contact; Loxton Sand. Overlies Carrolls Amphibolite,sharp contact; Winnambool Formation, gradational; Renmark Group, unconformity|Includes carbonaceous fine sand and (black) clays, grey and mottled silty mud.|
7090|Geera Clay|73118|5|Briefly described|p17, 37, 45, 48, 61, 82|||Glenelg Zone, Western Victoria. Drill core summary logs. 170m thick; mainly <50m. Entirely concealed. Deposited in shallow and marginal marine, interdistributary bay, lagoonal and tidal flat environments.||Murray Group.||Overlies Ettrick, Olney Formations and Saint Arnaud Group. Is overlain by Bookpurnong Beds and Loxton-Parilla Sands.|Poorly consolidated, black to dark green silt, clay, minor sand; commonly glauconitic, fossiliferous, calcareous, carbonaceous; locally includes sandy dolomitic intercalations. Abundant low-diversity faunas.|
7090|Geera Clay|73188|6|Mentioned|p320|Miocene|Miocene|Murray Basin.|||||Clay.|
7090|Geera Clay|73228|4|Described|p50, p55-57, p60|Middle Miocene|Late Early Oligocene|Murray Basin. Muddy lagoonal and marginal marine / tidal environments [although Fabris 2003 provided a different interpretation]. Represents marine incursions within the Murray Group.||Murray Group|||Black to grey-green, carbonaceous, pyritic clay and silt with minor sand and glauconite and sparse marine fossils.|
7090|Geera Clay|73229|6|Mentioned|p67|Middle Miocene|Late Early Oligocene|Murray Basin.||Murray Group||||
7090|Geera Clay|73496|6|Mentioned|Map legend|Miocene|Oligocene|||||||
7090|Geera Clay|73505|4|Described|p2, p11, p13-14, p36|Miocene|Late Eocene|Murray Basin. Mostly deposited in a marginal marine environment, includes intertital and estuarine deposits. Interfingers with lateral equivalents of the Calivil Formation. No detectable magnetic response.||Murray Group||Overlies Norval Regolith, offshore equivalent to Calivil Formation, underlies Bookpurnong beds|Marginal marine, marine to nonmarine clay, 100 m thick.|
7118|Geneffe Shale|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
7118|Geneffe Shale|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
7118|Geneffe Shale|40328|4|Described|p106|||||||||
7118|Geneffe Shale|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
7133|Georgica Rhyolite Member|30604|6|Mentioned|p71|||||||||
7133|Georgica Rhyolite Member|36411|6|Mentioned|p268|||Refs Duggan & Masson 1978 for definition.||||||
7133|Georgica Rhyolite Member|36806|6|Mentioned|p131|||||||||
7155|Gerringong Volcanics|22601|6|Mentioned|417|||Geol province Sydney Basin||||||
7155|Gerringong Volcanics|22969|4|Described|p 6|Late Permian|Permian|258 +/-5 Ma||||||
7155|Gerringong Volcanics|23544|4|Described|p373|||also see Fig 2 p358 and p359. In the Sydney Basin.||||||
7155|Gerringong Volcanics|24240|6|Mentioned|p21|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||
7155|Gerringong Volcanics|24334|5|Briefly described|p48 Tb.1|Scythian|Kazanian|Age: 249 - 257 Ma.||||||
7155|Gerringong Volcanics|24424|6|Mentioned|p538|Late Permian|Permian|||||||
7155|Gerringong Volcanics|29437|6|Mentioned|p136|||||||||
7155|Gerringong Volcanics|29900|5|Briefly described|p174|||||||||
7155|Gerringong Volcanics|30449|6|Mentioned|p2|||Brachiopods. See also P16||||||
7155|Gerringong Volcanics|30450|6|Mentioned|Table 1|Permian|Permian|Permian age. Sydney Basin||||||19-OCT-10
7155|Gerringong Volcanics|30545|6|Mentioned|p24|||||||||
7155|Gerringong Volcanics|30549|6|Mentioned|p24|||Age 250 m.y.||||||
7155|Gerringong Volcanics|31062|6|Mentioned|p478|||Permian. On Table||||||
7155|Gerringong Volcanics|31081|6|Mentioned|p51|||||||||
7155|Gerringong Volcanics|31128|6|Mentioned|p11|||||||||
7155|Gerringong Volcanics|31725|6|Mentioned|p6|||||||||
7155|Gerringong Volcanics|31884|6|Mentioned|p61|||||||||
7155|Gerringong Volcanics|32618|6|Mentioned|Table 1|Permian|Permian|Perm. Strat. table.||||||19-OCT-10
7155|Gerringong Volcanics|32800|6|Mentioned|p395|||||||||
7155|Gerringong Volcanics|32802|6|Mentioned|p20|||Dates||||||
7155|Gerringong Volcanics|32849|6|Mentioned|p7|Permian|Permian|Permian||||||19-OCT-10
7155|Gerringong Volcanics|32945|6|Mentioned|p80|||See also P84,85 & 90||||||
7155|Gerringong Volcanics|32946|6|Mentioned|p910|||Fossil||||||
7155|Gerringong Volcanics|33345|6|Mentioned|p491|||||||||
7155|Gerringong Volcanics|33930|6|Mentioned|p15|||See also P16.||||||
7155|Gerringong Volcanics|34039|6|Mentioned|p355|||||||||
7155|Gerringong Volcanics|34059|6|Mentioned|Map legend|Permian|Permian|||||||
7155|Gerringong Volcanics|34084|6|Mentioned|p368|Permian|Permian|Perm.||||||19-OCT-10
7155|Gerringong Volcanics|34138|6|Mentioned|Cor.Chart|Kazanian|Kazanian|Kazanian||||||19-OCT-10
7155|Gerringong Volcanics|34292|6|Mentioned|p25|||Permian. Correlation with Toll Bar Group. See also PP26,27,32||||||
7155|Gerringong Volcanics|34331|6|Mentioned|p457|||||||||
7155|Gerringong Volcanics|34334|6|Mentioned|p357|||||||||
7155|Gerringong Volcanics|34339|6|Mentioned|p442|||Influence on sedimentation.||||||
7155|Gerringong Volcanics|34434|3|Fully described|p366|||See also p367-368||||||22-JUN-16
7155|Gerringong Volcanics|34533|6|Mentioned|p1285|||||||||
7155|Gerringong Volcanics|34574|6|Mentioned|p114|||Age 250my||||||
7155|Gerringong Volcanics|34605|6|Mentioned|p372|||||||||
7155|Gerringong Volcanics|35145|6|Mentioned|Fig.2|||||||||
7155|Gerringong Volcanics|35160|6|Mentioned|p1|||||||||
7155|Gerringong Volcanics|35284|6|Mentioned|Fig.1|||||||||
7155|Gerringong Volcanics|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
7155|Gerringong Volcanics|35878|6|Mentioned|p115|||||||||
7155|Gerringong Volcanics|36042|6|Mentioned|p20|||See also Fig.16.||||||
7155|Gerringong Volcanics|36147|6|Mentioned|Fig.2|||||||||
7155|Gerringong Volcanics|36148|6|Mentioned|p266|||||||||
7155|Gerringong Volcanics|36207|6|Mentioned|Text Fig.2|||||||||
7155|Gerringong Volcanics|36220|4|Described|p16|||See also Table 1.||||||
7155|Gerringong Volcanics|36594|6|Mentioned|p11|||||||||
7155|Gerringong Volcanics|36954|6|Mentioned|Fig.1|||||||||
7155|Gerringong Volcanics|37253|6|Mentioned|Table 1|||||||||
7155|Gerringong Volcanics|38656|6|Mentioned|Fig.1.5.14|||P281||||||
7155|Gerringong Volcanics|38690|6|Mentioned|p288|||||||||
7155|Gerringong Volcanics|39267|6|Mentioned|p237|||See also P243||||||
7155|Gerringong Volcanics|39287|6|Mentioned|p18|||||||||
7155|Gerringong Volcanics|39289|5|Briefly described|p78|||||||||
7155|Gerringong Volcanics|39304|6|Mentioned|Photo 19.1|||||||||
7155|Gerringong Volcanics|39305|5|Briefly described|p379|||Fossil occurrences||||||
7155|Gerringong Volcanics|39306|6|Mentioned|p399|||||||||
7155|Gerringong Volcanics|39308|6|Mentioned|p505|||||||||
7155|Gerringong Volcanics|39423|6|Mentioned|p66|||||||||
7155|Gerringong Volcanics|39450|6|Mentioned|Table 1|||||||||
7155|Gerringong Volcanics|40631|6|Mentioned|p160|||||||||
7155|Gerringong Volcanics|40653|6|Mentioned|p121|||||||||
7155|Gerringong Volcanics|41809|6|Mentioned|p74|||||||||
7155|Gerringong Volcanics|42000|6|Mentioned|p63|||||||||
7155|Gerringong Volcanics|42171|6|Mentioned|p141|||||||||
7155|Gerringong Volcanics|42767|6|Mentioned|p3|||||||||
7155|Gerringong Volcanics|42925|5|Briefly described|Table 1||Late Permian|||||||
7155|Gerringong Volcanics|43194|5|Briefly described|p129 Tb. 8.3|Permian|Permian|Southern Sydney Basin.||||||
7155|Gerringong Volcanics|43344|14|Not recorded|p20,25,69,71-73,186||Permian|||||||
7155|Gerringong Volcanics|43345|14|Not recorded|p3 Table 1||Permian|||||||
7155|Gerringong Volcanics|43346|2|Defined|p1,5 Map|||||||||
7155|Gerringong Volcanics|43349|14|Not recorded|Map|||||||||
7155|Gerringong Volcanics|43357|14|Not recorded|155-161|Early Ordovician||||||||
7155|Gerringong Volcanics|43383|14|Not recorded|p20, Fig.5||Permian|||||||
7155|Gerringong Volcanics|43384|14|Not recorded|Map Legend||Late Permian|||||||
7155|Gerringong Volcanics|43385|14|Not recorded|p179||Late Permian|||||||
7155|Gerringong Volcanics|43437|14|Not recorded|p169-175||Late Permian|||||||
7155|Gerringong Volcanics|43460|14|Not recorded|p96|||||||||
7155|Gerringong Volcanics|43471|14|Not recorded|p242,244,245,247,252|Late Permian|Late Permian|U.Permian; has Megadesmus and Astartila assoc. with it||||||19-OCT-10
7155|Gerringong Volcanics|43474|14|Not recorded|p10,38-9,44,47-52,||Late Permian|p66,86,90,92,96,98||||||
7155|Gerringong Volcanics|43475|14|Not recorded|p553||Permian|||||||
7155|Gerringong Volcanics|43477|14|Not recorded|p19,41,59||Permian|||||||
7155|Gerringong Volcanics|43479|14|Not recorded|p188m,189,218|Kazanian|Kungurian|||||||
7155|Gerringong Volcanics|43491|4|Described|pVII/50||Permian|||||||
7155|Gerringong Volcanics|43545|14|Not recorded|p415,417|||From reprint. Correct reference not given||||||
7155|Gerringong Volcanics|43893|14|Not recorded|p200,202||Permian|||||||
7155|Gerringong Volcanics|44282|14|Not recorded|p.17,18;Pl.3|||(I56-9/Kiama).||||||
7155|Gerringong Volcanics|44489|14|Not recorded|p71|||||||||
7155|Gerringong Volcanics|44814|14|Not recorded|p483||Late Permian|early Late Permian.||||||
7155|Gerringong Volcanics|44861|4|Described|p226,228,229|||||||||
7155|Gerringong Volcanics|45090|6|Mentioned|Fig.4|||||||||
7155|Gerringong Volcanics|45138|6|Mentioned|p2|||||||||
7155|Gerringong Volcanics|48926|6|Mentioned|p47|||P47 et seq.||||||
7155|Gerringong Volcanics|49644|5|Briefly described|Table|||||||||
7155|Gerringong Volcanics|60281|4|Described|p60|Late Permian|Late Permian|Collective term for 5 latite flows interbedded within the Budgong Sandstone, and 2 flows within the overlying Pheasants Nest Formation.  Age: 258+/-5Ma.  Geological Province: Sydney Basin.||||||27-APR-05
7155|Gerringong Volcanics|60299|6|Mentioned|p208|||Geological Province: Sydney Basin||||||
7155|Gerringong Volcanics|61612|6|Mentioned|p272, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin. Shoshonitic lavas.||||||13-MAR-09
7155|Gerringong Volcanics|65107|6|Mentioned|p278|Late Permian|Late Permian|Provides constraint on Australia's Later Permian "westward loop" pole path. Pre Mesozoic. No radiometric date||||||
7155|Gerringong Volcanics|66577|6|Mentioned|p995.|Permian|Permian|This unit may signify beginning of subduction related magmatism and deformation along the eastern margin of the Permian Sydney Basin.||Unit in Shoalhaven Group.||Overlies Berry Siltstone. Is overlain by Pheasants Nest Formation.||
7155|Gerringong Volcanics|67028|6|Mentioned|p371 Tb. 5|Permian|Permian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996)|251-271 Ma magnetic age range|||||24-APR-12
7155|Gerringong Volcanics|67663|5|Briefly described|p518-520, p524-529, p532-535, p540|Permian|Permian|Marks onset of a major phase of shoshonitic volcanism. 5 latite flows are interbedded with Broughton Formation, and 4 with Pheasants Nest Formation.||Of the Shoalhaven Group.||Overlain by the Illawarra Coal Measures. Overlies Shoalhaven Group.|Latites and volcaniclastic sediments.|
7155|Gerringong Volcanics|68822|5|Briefly described|p339|Capitanian|Capitanian|Southern Sydney Basin. Shoshonitic and extrusive.|ca. 264 - 263 Ma|||||27-JUL-15
7155|Gerringong Volcanics|69297|6|Mentioned|p501|Wuchiapingian|Capitanian|Sydney Basin. ||||Unconformably overlies and intrudes the Broughton Formation. Unconformably overlain by the Illawarra Coal Measures.||
7155|Gerringong Volcanics|70661|6|Mentioned|ix, p137|Late Permian|Late Permian|||||||
7155|Gerringong Volcanics|71115|5|Briefly described|p178-183, 185-190, 192-195|Permian|Permian|Southern Sydney Basin. Reversely magnetised rocks from the c.318-265 Ma Kiaman Reverse Superchron. Volcanic source was c.40 km SE of Kiama. Paleomagnetic poles for c.265 Ma tabulated and discussed.|265.05 +/- 3.5 Ma.||Blow Hole, Berkeley, Bumbo, Dapto, Saddleback, Cambewarra, Five Islands, Calderwood, Minnamurra Latites.|Is interbedded with Broughton Formation.|A series of flat-lying mafic to intermediate lava flows; comprises nine distinct basaltic to andesitic units interbedded with several volcaniclastic sandstones and tuffs.|
7155|Gerringong Volcanics|71542|5|Briefly described|p23, 26, 35|Permian|Permian|Of southern Sydney Basin. Shoshonitic latite flows variably interspersed with Broughton Formation. K-Ar minimum ages of 253-258 Ma (Facer and Carrm 1979; Carr and Facer 1980). SHRIMP zircon data from the Newcastle Coal Measures, combined with correlation based on brachiopod zones, suggested the Gerringong Volcanics is older than 253 Ma (Roberts et al., 1994).|||Includes Cambewarra, Dapto, Saddleback, Bumbo, Blow Hole and Coolangatta latite members, and Koo-Lee Tuff Member and Back Forest Tuff Bed.|||20-OCT-21
7155|Gerringong Volcanics|73197|5|Briefly described|p475 Fig.6, p477-479|Guadalupian|Guadalupian|New England Orogen, southern. Sydney Basin, southern edge. Attributed to the Currarong Arc. Originally dated to ca 258-240 Ma based on K-Ar dating (Carr, 1998), later estimated to be ca 265 Ma (Campbell et al., 2001). Age range in text of 265-263 Ma, U-Pb zircon age including additional 263.51 +/- 0.31 U-Pb zircon age from Carr et al., (2003) and Metcalfe et al., (2015). Ar/Ar (pl) age from Belica et al., (2017).|265.05 +/- 0.46 Ma Ar/Ar, 263.4 +/- 2.4 Ma U-Pb||||Potassic trachyandesites.|
7155|Gerringong Volcanics|73421|6|Mentioned|p15||||||||Includes latite lava flows.|
7155|Gerringong Volcanics|73494|4|Described|p539-540, 555-556|Permian|Permian|Southern Sydney Basin. Comprises the non-sandstone units of the Gerringong Volcanic Complex. Late Permian.||Shoalhaven Group (lower part); Illawarra Coal Measures (upper part).|Berkeley, Minnamurra, Calderwood, Five Islands, Cambewarra, Saddleback, Dapto, Bumbo, Blow Hole, Coolangatta, Latite Members; Koo-Lee Tuff Member.|Intercalated with the Shoalhaven Group.|Numerous mafic (shoshonitic) extrusions.|
7159|Gerybong Limestone Member|5250|5|Briefly described|p42, p48, p53|Mid Caradoc|Early Caradoc|Member of  Daylesford Limestone. Overlies Manooka Limestone Member. Includes brachiopod fauna||||||09-MAY-12
7159|Gerybong Limestone Member|23213|5|Briefly described|p22|||Macrofauna fossil assemblage matches Sourges Shale. Corals also present. Of Daylesford Limestone.||||||16-JAN-12
7159|Gerybong Limestone Member|23214|3|Fully described|p37|Late Ordovician|Late Ordovician|Of Daylesford Limestone. 25m thick at type section. For lithology description see Semeniuk (1973a,b).  Overlying unit: Glenrae Limestone Member, underlying unit: Manooka Limestone Member.||||||
7159|Gerybong Limestone Member|33063|2|Defined|p80|Ordovician|Ordovician|||||||
7159|Gerybong Limestone Member|33064|4|Described|p450|||See also p451-453. Strat. column.||||||16-JAN-12
7159|Gerybong Limestone Member|33065|6|Mentioned|Table 1|||Lithology||||||
7159|Gerybong Limestone Member|33737|6|Mentioned|p167|||||||||
7159|Gerybong Limestone Member|33740|6|Mentioned|Fig.1|||||||||
7159|Gerybong Limestone Member|35646|6|Mentioned|Fig.5|||||||||
7159|Gerybong Limestone Member|38219|6|Mentioned|Table 2|||||||||
7159|Gerybong Limestone Member|40136|6|Mentioned|p23|||||||||
7159|Gerybong Limestone Member|41046|6|Mentioned|p144|||See also Fig.2||||||
7159|Gerybong Limestone Member|42479|5|Briefly described|p111|||||||||
7159|Gerybong Limestone Member|70684|5|Briefly described|p39 Fig.17|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Eastonian.||Daylesford Limestone.||||
7159|Gerybong Limestone Member|73210|5|Briefly described|p900 Fig.7|||||Daylesford Limestone.||Overlies Manooka Limestone Member.||
7161|Ghost Hill Formation|22857|5|Briefly described|p458 App.1, Tb.A1.6|Silurian|Silurian|Of the Cudal Group. Lithic, feldspathic and quartz arenite, coarse quartzofeldspathic arenite, minor laminated chert. Max. thickness: 140m. Geological Province: Cowra Trough.||||||
7161|Ghost Hill Formation|23214|3|Fully described|p120|Ludlow|Ludlow|Of Cudal Group. Intrudes Woodstock and Burley Limestones. Max. thickness 140m||||||
7161|Ghost Hill Formation|31852|6|Mentioned|p718|||See also Fig.4. Ludlovian||||||
7161|Ghost Hill Formation|33006|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
7161|Ghost Hill Formation|33282|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
7161|Ghost Hill Formation|34404|6|Mentioned|Fig.3.3b|||||||||
7161|Ghost Hill Formation|34405|6|Mentioned|p122|||||||||
7161|Ghost Hill Formation|37727|5|Briefly described|p59|||||||||
7161|Ghost Hill Formation|40328|3|Fully described|p79|||||||||
7161|Ghost Hill Formation|43515|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition) (M.Sil)||||||
7161|Ghost Hill Formation|43516|14|Not recorded|Map Legend||Early Silurian|(M.Sil)||||||
7161|Ghost Hill Formation|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of lithic, feldspathic and quartz sandstone; conglomerate; limestone; tuffaceous shale.||||||15-JUL-08
7161|Ghost Hill Formation|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Cudal Group.||||||15-JUL-08
7161|Ghost Hill Formation|63287|5|Briefly described|p317 Fig. 2|Ludlow|Ludlow|Of the Cudal Group. Overlain by Belubula Shale, underlain by Avoca Vally Shale. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
7161|Ghost Hill Formation|67847|5|Briefly described|p33|||Graptolite fauna briefly discussed. ||||Overlies the Avoca Valley Shale.||
7161|Ghost Hill Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group||||
7165|Gibbons Creek Sandstone|22472|5|Briefly described|p40|||||||||
7165|Gibbons Creek Sandstone|22529|5|Briefly described|8|Late Devonian|Late Devonian|||||||
7165|Gibbons Creek Sandstone|22857|4|Described|p216, p494 App. 1 Tb.A1.7|Late Devonian|Late Devonian|Of the Lambie Group. Formerly the "Cox Subgroup" of Conolly (1962, 1969a,b). Fossiliferous quartz arenite, siltstone, mudstone. Max. thickness: 1300m. Geological Province: Lambie Shelf. ||||||
7165|Gibbons Creek Sandstone|22859|5|Briefly described|p216|||Previously known as 'Cox Subgroup'||||||
7165|Gibbons Creek Sandstone|23043|5|Briefly described|Map Legend|Famennian|Frasnian|of Lambie Group.||||||
7165|Gibbons Creek Sandstone|23170|2|Defined|p237|Late Devonian|Late Devonian|of Lambie Group.||||||
7165|Gibbons Creek Sandstone|23214|3|Fully described|p239|Late Devonian|Late Devonian|Of Lambie Group. Now includes Mount Schofield Formation and Coxs Formation. Sandstone and siltstone. Unconformably overlies Drogheda Volcanics.  Max. thickness 1300m.||||||17-JAN-06
7165|Gibbons Creek Sandstone|32708|6|Mentioned|Fig.2|||||||||
7165|Gibbons Creek Sandstone|35166|6|Mentioned|Fig.3|||||||||
7165|Gibbons Creek Sandstone|35246|6|Mentioned|p172|||||||||
7165|Gibbons Creek Sandstone|43639|5|Briefly described|Map Legend||Devonian|||||||
7165|Gibbons Creek Sandstone|43641|5|Briefly described|Map Legend||Devonian|||||||
7165|Gibbons Creek Sandstone|43782|5|Briefly described|Map Legend|Famennian|Frasnian|of Lambie Group.||||||
7165|Gibbons Creek Sandstone|68592|5|Briefly described|p34, p1737|||Occurs in the type area of the Lambie Group. Appears as Gibbons Creek Formation on p1737.||Basal unit in Lambie Group.||Is correlated with Strathaird and Bellbird Creek Formations and Macquarie Park Sandstone.||
7165|Gibbons Creek Sandstone|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|Shown as Gibbons Ck Sandstone.||Lambie Group||||
7167|Gibraltar Ignimbrite|22857|5|Briefly described|p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Group. Porphyritic rhyolitic ignimbrite. Max. thickness: >80m. Geological Province: New England Fold Belt.||||||
7167|Gibraltar Ignimbrite|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Wandsworth Volcanic Group.  Ignimbrite rhyolite.||||||20-DEC-04
7167|Gibraltar Ignimbrite|23812|5|Briefly described|p28 Tb.3|Late Permian|Early Permian|Of Wandsworth Volcanic Group.  Maximum thickness: 80m.||||||
7167|Gibraltar Ignimbrite|23859|5|Briefly described|p930|Late Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
7167|Gibraltar Ignimbrite|31694|6|Mentioned|p350|||||||||
7167|Gibraltar Ignimbrite|38914|6|Mentioned|p328|||||||||
7167|Gibraltar Ignimbrite|42378|5|Briefly described|Table 1 P8|||||||||
7167|Gibraltar Ignimbrite|43017|5|Briefly described|Fig.2,p374|||||||||
7167|Gibraltar Ignimbrite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group.||||||
7167|Gibraltar Ignimbrite|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
7167|Gibraltar Ignimbrite|68005|5|Briefly described|p152.|Permian|Permian|||Unit in Wandsworth Volcanic Group.|||Ignimbritic rhyolite.|
7167|Gibraltar Ignimbrite|70373|5|Briefly described|p792 fig 2, p793, p795, p797 Tb 1, p801|Early Triassic|Permian|20-80m thick. Previously undated and assumed to be correlative to middle to late Permian Emmavillie Creek Volcanics. [Dating likely to indicate crystallisation age] Provides minimum age constraint for underlying Bondonga beds.|251.6 +/-3.2 Ma (LA-ICP-MS on zircons)|||Overlies Mosman Formation. Correlated with Emmaville Creek Volcanics.|Porphyritic rhyolite. Large quartz, plagioclase and sanidine phenocrysts within an aphanitic groundmass of volcanic shards.|
7167|Gibraltar Ignimbrite|73472|6|Mentioned|App.2|Olenekian|Wuchiapingian|Roughly equivalent in age to the Galah Tuff. [Supersedes Gibraltar Rhyolite].|251.6 +/- 3.5 Ma|||||
7222|Gilgunnia Granite|29987|5|Briefly described|p15|||||||||
7222|Gilgunnia Granite|34449|6|Mentioned|Table 2-1|||||||||
7222|Gilgunnia Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
7222|Gilgunnia Granite|37772|6|Mentioned|p1|||||||||
7222|Gilgunnia Granite|40269|4|Described|p141|||||||||
7222|Gilgunnia Granite|40328|4|Described|p206|||||||||
7222|Gilgunnia Granite|41528|2|Defined|p105|Early Devonian||Mention p98.||||||20-SEP-19
7222|Gilgunnia Granite|41529|6|Mentioned|Map legend|Lochkovian||||||||
7222|Gilgunnia Granite|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
7222|Gilgunnia Granite|41821|2|Defined|p50|Early Devonian||||||||
7222|Gilgunnia Granite|42726|5|Briefly described|map legend|||||||||
7222|Gilgunnia Granite|43089|5|Briefly described|Map Legend|||||||||
7222|Gilgunnia Granite|43389|14|Not recorded|Map Legend||Silurian|||||||
7222|Gilgunnia Granite|69511|5|Briefly described|p1-2, p6, p10, p14, p18|Early Devonian|Late Silurian|A high-level pluton that is inferred to be co-magmatic with Mount Halfway Volcanics. Is petrographically and chemically related to the Mount Halfway Volcanics. |422.5 +/- 3.6 Ma (Armstrong, unpublished).||||Cordierite-biotite-bearing (S-type) granite.|
7222|Gilgunnia Granite|70751|5|Briefly described|p8, p10, p12, p25, p28, p38|Silurian|Silurian|More extensive than is apparent in outcrop. Related to the high strain zone developed in the Gilgunnia area that is host to structurally controlled high-sulfide gold-base metal mineralisation.|422.5 +/- 3.6 Ma (SHRIMP, this study)||||Medium-grained, S-type granite.|
7222|Gilgunnia Granite|70876|5|Briefly described|p1, p17, p76|Devonian|Silurian|Cobar Basin. An age of 422.8 +/- 4.9 Ma is also derived for an inferred equivalent of this unit. S-type geochemistry.|422.5 +/- 3.6 Ma (Downes et al., 2016)|||||
7222|Gilgunnia Granite|71039|5|Briefly described|p15, p21|||S-type. Contact metamorphosed the Northwestern Amphitheatre Group.|422.5 +/- 3.6 Ma|||Intrudes the Amphitheatre Group.||09-MAR-23
7222|Gilgunnia Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped S-type intrusion.|||||Coarse-grained equigranular cordierite-biotite granite and monzogranite, minor fine-grained sparsely porphyritic biotite granite and porphyritic microgranodiorite.|
7222|Gilgunnia Granite|72908|6|Mentioned|p5, p25|Late Silurian|Late Silurian||~427-419 Ma|||||
7222|Gilgunnia Granite|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Intrudes[?] Mount Hope Group. Equivalent to Mount Allen Granite.||
7222|Gilgunnia Granite|73578|6|Mentioned|p7, p14, p21|Lochkovian|Gorstian|Age of 422.5 +/- 3.6 Ma reported by Downes et al. (2016).|422.5 +/- 3.6 Ma|||||
7225|Gilgurry Mudstone|22601|6|Mentioned|416|Permian|Permian|||||||
7225|Gilgurry Mudstone|22857|4|Described|p536 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wandsworth Volcanic Group. Grey siltstone, feldspathic sandstone, quartzite, carbonaceous mudstone; minor tuff. Max. thickness: 573m. Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|23103|5|Briefly described|p551, Fig.1|Permian|Permian|||||||
7225|Gilgurry Mudstone|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Parent: Wandsworth Volcanic Group.  Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|23812|6|Mentioned|p30|||||||||
7225|Gilgurry Mudstone|23859|5|Briefly described|p929|Late Permian|Late Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|29441|6|Mentioned|p113|||||||||
7225|Gilgurry Mudstone|30911|6|Mentioned|Map legend|Permian|Permian|||||||
7225|Gilgurry Mudstone|32086|6|Mentioned|p325|||Marine mudstones||||||
7225|Gilgurry Mudstone|32484|6|Mentioned|Fig.1|||||||||
7225|Gilgurry Mudstone|32491|5|Briefly described|p13|||Permian||||||
7225|Gilgurry Mudstone|32492|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
7225|Gilgurry Mudstone|32671|6|Mentioned|Map legend|Permian|Permian|||||||
7225|Gilgurry Mudstone|32944|6|Mentioned|p709|||||||||
7225|Gilgurry Mudstone|32945|6|Mentioned|p90|||||||||
7225|Gilgurry Mudstone|33436|3|Fully described|Fig.1|||Upper Permian.||||||13-NOV-08
7225|Gilgurry Mudstone|33476|2|Defined|p45|Permian|Permian|||||||
7225|Gilgurry Mudstone|33766|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
7225|Gilgurry Mudstone|34340|6|Mentioned|Table 6.1|||Permian||||||
7225|Gilgurry Mudstone|34350|6|Mentioned|p17|||Permian||||||
7225|Gilgurry Mudstone|34556|5|Briefly described|p268|||||||||
7225|Gilgurry Mudstone|35257|6|Mentioned|Fig.18|||||||||
7225|Gilgurry Mudstone|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
7225|Gilgurry Mudstone|36961|6|Mentioned|Fig.5|||||||||
7225|Gilgurry Mudstone|37252|6|Mentioned|Map legend|Permian|Permian|||||||
7225|Gilgurry Mudstone|38837|6|Mentioned|p234|||||||||
7225|Gilgurry Mudstone|39279|4|Described|p367|||||||||
7225|Gilgurry Mudstone|40504|6|Mentioned|p97|||||||||
7225|Gilgurry Mudstone|40505|5|Briefly described|p81|||||||||
7225|Gilgurry Mudstone|40773|3|Fully described|p450|||Mention p458.||||||13-NOV-08
7225|Gilgurry Mudstone|41413|6|Mentioned|p327|||||||||
7225|Gilgurry Mudstone|42378|5|Briefly described|Table 1 P10, Fig.1 5|||Redefined Offenberg 1968 (P21)||||||
7225|Gilgurry Mudstone|42963|5|Briefly described|Fig.2|||||||||
7225|Gilgurry Mudstone|43008|5|Briefly described|map legend|||||||||
7225|Gilgurry Mudstone|43017|5|Briefly described|Fig.2,p374|||||||||
7225|Gilgurry Mudstone|43385|14|Not recorded|p179,180||Kungurian|||||||
7225|Gilgurry Mudstone|43745|6|Mentioned|p16||Late Permian|||||||
7225|Gilgurry Mudstone|43881|14|Not recorded|p6-7,9||Permian|Lower formation of Boorook Group.||||||
7225|Gilgurry Mudstone|43894|14|Not recorded|p787||Permian|Part of Boorook Group. Late Kungurian or Early Kazanian.||||||
7225|Gilgurry Mudstone|44093|5|Briefly described|p233 App. 1|Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
7225|Gilgurry Mudstone|48940|3|Fully described|p48|||Refers Voisey (1957).||||||14-APR-08
7225|Gilgurry Mudstone|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|Of the Wandsworth Volcanic Group.||||||
7225|Gilgurry Mudstone|60937|5|Briefly described|p426, p437|Late Permian|Late Permian|See also Gilgurry mudstones. Geological Province: texas Block. See also p434.||||||14-APR-08
7225|Gilgurry Mudstone|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
7225|Gilgurry Mudstone|67908|6|Mentioned|p285|Permian.|Permian.|Late Permian. Not affected by the deformation producing the Texas Orocline.||||||
7225|Gilgurry Mudstone|69793|6|Mentioned|p1113 Fig.3|Permian|Permian|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
7225|Gilgurry Mudstone|71628|6|Mentioned|p11: 26, 29; p15: 33, 57; p16: 2, 4|||||||Is intruded by Cullendore Supersuite, Rocky River Monzogranite, and Mount Lindesay Monzogranite (Stanthorpe Complex).||
7238|Gilmore Volcanic Group|22857|4|Described|p241, p508 App.1 Tb.A1.8|Visean|Visean|Sequence of felsic volcanics, mostly ignimbrite, and sediments. Conformably overlie Wallaringa and Flagstaff Formations. Age: ~331Ma (K/Ar). Geological Province: Kullatine-Yagon-Booral Shelf and Tamworth Forearc Basin.||||||
7238|Gilmore Volcanic Group|22863|6|Mentioned|p241|||||||||
7238|Gilmore Volcanic Group|24121|5|Briefly described|p4, p83, p151|||Shown as Gilmore Volcanics p122.||||||25-AUG-22
7238|Gilmore Volcanic Group|24603|6|Mentioned|p898|||In the eastern Gresford Block.  Geological Province: Tamworth Belt.||||||
7238|Gilmore Volcanic Group|31228|4|Described|p80|||Age. Harland et al. (1964)||||||
7238|Gilmore Volcanic Group|32379|6|Mentioned|p5|||||||||
7238|Gilmore Volcanic Group|32672|6|Mentioned|p674|||||||||
7238|Gilmore Volcanic Group|32836|6|Mentioned|Table 1|||Palaeobotany||||||
7238|Gilmore Volcanic Group|32868|6|Mentioned|p209|||||||||
7238|Gilmore Volcanic Group|32869|6|Mentioned|Fig.2|||See also Fig.3B||||||
7238|Gilmore Volcanic Group|34238|6|Mentioned|p8|||See also Fig.2||||||
7238|Gilmore Volcanic Group|35803|6|Mentioned|p321|||||||||
7238|Gilmore Volcanic Group|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
7238|Gilmore Volcanic Group|36528|6|Mentioned|p178|||||||||
7238|Gilmore Volcanic Group|38801|6|Mentioned|Fig.3|||||||||
7238|Gilmore Volcanic Group|39302|6|Mentioned|p345|||||||||
7238|Gilmore Volcanic Group|39303|6|Mentioned|p352|||Flora||||||
7238|Gilmore Volcanic Group|39306|6|Mentioned|p391|||||||||
7238|Gilmore Volcanic Group|39308|6|Mentioned|p490|||||||||
7238|Gilmore Volcanic Group|39666|6|Mentioned|p103|||||||||
7238|Gilmore Volcanic Group|42547|5|Briefly described|p30|||||||||
7238|Gilmore Volcanic Group|43417|6|Mentioned|Map Legend|||Equivalent of Isismurra Formation. Ref. to Rattigan 1967||||||
7238|Gilmore Volcanic Group|44093|5|Briefly described|p229 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
7238|Gilmore Volcanic Group|44244|2|Defined|p87|Carboniferous|Carboniferous|Includes Eagleton Volcanics, Mosmans Swamp Andesite, Newtown and Mowbray Formations.  Conformably overlies the Wallaringa Formation; disconformably underlies Mount Johnstone Formation.  Type section in text.||||||18-AUG-04
7238|Gilmore Volcanic Group|44253|14|Not recorded|p6||Carboniferous|Part of Kuttung Facies.||||||
7238|Gilmore Volcanic Group|44254|2|Defined|p76-81||Visean|Includes: Eagleton Volcanics, Mosman's Swamp Andesites.||||||
7238|Gilmore Volcanic Group|44255|14|Not recorded|p119||Carboniferous|||||||
7238|Gilmore Volcanic Group|50147|5|Briefly described|Map legend|Visean|Visean|Geological Province: Gresford Block||||||
7238|Gilmore Volcanic Group|50268|5|Briefly described|Map Legend|Visean|Visean|Includes: Mowbray Formation, Newtown Formation.  Geological Province: Rouchel and Gresford Blocks.||||||
7238|Gilmore Volcanic Group|65107|6|Mentioned|p276|Visean|Visean|Part of the Gresford Block, overlying the Martins Creek Ignimbrite. No dates.||||||
7238|Gilmore Volcanic Group|71628|6|Mentioned|p6:22||||||Flagstaff Formation, Wootton beds.|||
7238|Gilmore Volcanic Group|73487|6|Mentioned|p583|||||||||
7248|Gindoono Limestone|32087|6|Mentioned|p9|||||||||
7248|Gindoono Limestone|34449|6|Mentioned|Fig.|||Nymagee map attached to report||||||
7249|Gingara Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
7250|Gingenbullen Dolerite|30661|6|Mentioned|Table 1|||||||||
7250|Gingenbullen Dolerite|43870|14|Not recorded|p276,308,341-2||Jurassic|Based on radiometric determinations. Rests on U.Triassic sediments.||||||
7250|Gingenbullen Dolerite|70661|4|Described|ix, p4, p221-p223|Jurassic|Jurassic|Named after Gingebullen Mountain (which is formed primarily by this unit). No type section has been proposed. 100m thick. Distribution, geophysical characteristics, economic geology and structure briefly discussed.||||intrudes? Bringelly Shale.|Dense, columnar jointed tholeiitic dolerite composed of feldspar, augite, olivine and magnetite.|
7250|Gingenbullen Dolerite|71303|5|Briefly described|map legend|Jurassic|Jurassic||||||Tholeiitic dolerite; dark medium to fine-grained holocrystalline magnetite and olivine bearing rock; columnar jointing.|
7253|Gingera Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Foliated granodiorite. BMR map symbol: gfg.||||||
7253|Gingera Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
7253|Gingera Granite|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
7253|Gingera Granite|33325|6|Mentioned|p18|||Late Sil. - early Dev.||||||
7253|Gingera Granite|34544|5|Briefly described|p186|||||||||
7253|Gingera Granite|39800|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
7253|Gingera Granite|40328|4|Described|p206|||||||||
7253|Gingera Granite|41563|6|Mentioned|p512|||||||||
7253|Gingera Granite|45003|14|Not recorded|p55|||See also Lexicon||||||
7253|Gingera Granite|45087|5|Briefly described|p40|||Chemical analyses||||||
7253|Gingera Granite|45147|6|Mentioned|M211|||See also M216||||||
7253|Gingera Granite|46574|5|Briefly described|Map Legend|Silurian|Silurian|Of the Murrumbidgee Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
7262|Ginninderra Porphyry|36441|5|Briefly described|map legend|Ludlovian|Ludlovian|Intrusive. ?I-type. Red porphyry with quartz, plagioclase and mafic phenocrysts, rare K-feldspar megacrysts. BMR map code: Spg.||||||
7262|Ginninderra Porphyry|40328|6|Mentioned|Fig.12(H3)|||||||||
7262|Ginninderra Porphyry|42820|6|Mentioned|p71|||||||||
7262|Ginninderra Porphyry|45147|2|Defined|M255|Ludlovian|Ludlovian|||||||
7292|Giro beds|22857|5|Briefly described|p512 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Manning Group. Max. thickness: ?>6m. Geological Province: Barnard Basin.||||||
7292|Giro beds|41348|5|Briefly described|Map legend|Permian||Of the Manning Group.||||||16-DEC-04
7292|Giro beds|44450|5|Briefly described|p20|||Of Manning Group. Geological Province: New England Fold Belt.||||||
7292|Giro beds|65317|6|Mentioned|p632 Fig.10|Early Permian|Early Permian|||||||
7295|Girrakool beds|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
7295|Girrakool beds|24366|5|Briefly described|p8 Fig. 6|Early Carboniferous|Early Carboniferous|||||||
7295|Girrakool beds|37489|6|Mentioned|p266|||||||||
7295|Girrakool beds|42866|5|Briefly described|Table 2, P12|||||||||
7295|Girrakool beds|42915|5|Briefly described|p12|||||||||
7295|Girrakool beds|42984|5|Briefly described|p365|||||||||
7295|Girrakool beds|44450|3|Fully described|p12 Table 1|Late Carboniferous|Late Carboniferous|Geological Province: New England Fold Belt.||||||
7295|Girrakool beds|61805|6|Mentioned|p436|||Geological Province: New England Orogen.||||||17-NOV-08
7295|Girrakool beds|66183|5|Briefly described|p359, p367-368|Carboniferous|Carboniferous|New England Fold Belt. Part of a subduction-accretion complex, east of a volcanic front. Written as Girrakool Beds on Fig.2.||||||
7295|Girrakool beds|69639|6|Mentioned|p133|||Informal name.||||Intruded by the Llangothlin Monzogranite.||
7295|Girrakool beds|71628|5|Briefly described|p2: 8-9, 12, 14, 17, 27; p3: 13-14, 22|Carboniferous|Carboniferous|See also p3: 35, 39, 56, 71, 80, 92, 97; p8: 5, 13, 92; p13: 10, 24. Formerly the Lyndhurst Beds. Underwent contact metamorphism and partial melting adjacent to the Bakers Creek Complex intrusion. Deformation related to Wongwibinda Complex described in detail. Associated with Sb-Au(W) deposits in the Hillgrove-Metz area. RELATED UNITS (continued): Is also intruded by Blue Nobby, Enmore, Gara, Hillgrove, Llangothlin (?), Rockvale, Tobermory, Wards Mistake Monzogranites and Barney House Gabbro.||||Is intruded by the Bakers Creek, Billygoat Hill, and Camperdown Complexes; Abroi Granodiorite, Aberfoyle River Porphyrite; see COMMENTS for more.|Shales, silty quartzites, greywackes and cherts.|
7302|Gladefield Volcanics|12185|5|Briefly described|map legend|Middle Silurian|Middle Silurian|Acid lavas, tuff, ashstone, interbedded shale. BMR map symbol: Smg.||||||
7302|Gladefield Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
7302|Gladefield Volcanics|29994|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
7302|Gladefield Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
7302|Gladefield Volcanics|31111|6|Mentioned|p112|||See also P114, 116, 120, 124, 126, 130, 134||||||
7302|Gladefield Volcanics|31284|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Upper SilurianM - U||||||
7302|Gladefield Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
7302|Gladefield Volcanics|33325|5|Briefly described|Table 2|||See also Table 3.||||||
7302|Gladefield Volcanics|33328|4|Described|Table 1|||P13||||||
7302|Gladefield Volcanics|35110|6|Mentioned|p3|||||||||
7302|Gladefield Volcanics|36413|6|Mentioned|p38|||||||||
7302|Gladefield Volcanics|37348|6|Mentioned|p98|||||||||
7302|Gladefield Volcanics|37727|5|Briefly described|p60|||See also P18.||||||
7302|Gladefield Volcanics|37728|6|Mentioned|Table 4|||||||||
7302|Gladefield Volcanics|40328|4|Described|p99|||||||||
7302|Gladefield Volcanics|47037|6|Mentioned|p107|||||||||
7306|Gladstone Formation|29870|6|Mentioned|Table 1|||||||||
7306|Gladstone Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
7306|Gladstone Formation|31659|6|Mentioned|p11|||||||||
7306|Gladstone Formation|32482|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
7306|Gladstone Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
7306|Gladstone Formation|32944|6|Mentioned|p700|||Barra Gp. U.Perm. See also P702 & Fig.3||||||
7306|Gladstone Formation|34043|5|Briefly described|p452|||M.Perm.||||||
7306|Gladstone Formation|36961|6|Mentioned|p210|||See also Fig.3.||||||
7306|Gladstone Formation|37082|6|Mentioned|p161|||||||||
7306|Gladstone Formation|37094|6|Mentioned|p238|||||||||
7306|Gladstone Formation|39288|6|Mentioned|Fig. 3.3|||||||||
7306|Gladstone Formation|39468|6|Mentioned|Fig.2|||||||||
7306|Gladstone Formation|40166|6|Mentioned|Table 1|||||||||
7306|Gladstone Formation|43384|14|Not recorded|Map Legend||Late Permian|||||||
7306|Gladstone Formation|43385|14|Not recorded|p179||Late Permian|||||||
7306|Gladstone Formation|43407|14|Not recorded|Map Legend||Late Permian|(Provisional Edition)||||||
7306|Gladstone Formation|43408|14|Not recorded|Map Legend|||About 300 ft thick||||||
7306|Gladstone Formation|43409|14|Not recorded|Map Legend|||Shale etc, equiv. of Watermark Formation(i.e.late Permian)Marine||||||
7306|Gladstone Formation|45006|14|Not recorded|Tb.1,opp.p3|||||||||
7306|Gladstone Formation|48600|14|Not recorded|Plate 3|||||||||
7326|Glebe Formation|23055|6|Mentioned|Fig11p23|||||||||
7326|Glebe Formation|29922|6|Mentioned|Appendix 4|||||||||
7326|Glebe Formation|29926|6|Mentioned|Fig.3|||Permian||||||
7326|Glebe Formation|29942|4|Described|Fig.2|||||||||
7326|Glebe Formation|34351|6|Mentioned|Fig.5.13|||Proposed name change from Highfields Formation||||||
7326|Glebe Formation|37083|6|Mentioned|p164|||||||||
7326|Glebe Formation|39292|6|Mentioned|Fig. 6.2|||||||||
7326|Glebe Formation|39308|6|Mentioned|p467|||||||||
7326|Glebe Formation|39609|6|Mentioned|Table 1|||||||||
7326|Glebe Formation|41479|6|Mentioned|Fig.2|||||||||
7326|Glebe Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Adamstown Subgroup|Included Redhead Conglomerate Member, Edgeworth Tuff Member, Tingira Conglomerate Member.|||
7343|Glen Logan Gravel|34600|5|Briefly described|p547|||||||||
7343|Glen Logan Gravel|34813|6|Mentioned|p62|||||||||
7343|Glen Logan Gravel|41136|5|Briefly described|p217|||||||||
7343|Glen Logan Gravel|43493|6|Mentioned|32|||||||||
7343|Glen Logan Gravel|61155|5|Briefly described|p19|Middle Eocene|Middle Eocene|Geological Province: Lachlan Valley.||||||03-MAR-10
7344|Glen Munro Coal Member|29942|4|Described|Fig.1|||Permian||||||
7344|Glen Munro Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
7344|Glen Munro Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
7344|Glen Munro Coal Member|40805|6|Mentioned|Table 1|||||||||
7344|Glen Munro Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Mount Ogilvie Formation||||
7360|Glenbawn oolite|31519|6|Mentioned|p917|||||||||
7361|Glenbog Suite|22606|6|Mentioned|P831|||||||||
7361|Glenbog Suite|22719|6|Mentioned|p486|||||||||
7361|Glenbog Suite|22778|4|Described|p 163|||||||||
7361|Glenbog Suite|22815|5|Briefly described|p75, fig 25|||||||||
7361|Glenbog Suite|22876|4|Described|p25|||||||||
7361|Glenbog Suite|22878|6|Mentioned|p57 Table 7|||||||||
7361|Glenbog Suite|23309|5|Briefly described|p345|||||||||
7361|Glenbog Suite|23439|5|Briefly described|p124 fig.1|||||||||
7361|Glenbog Suite|23549|4|Described|p520-521|||Of Glenbog Supersuite. Comprises 12 putons. Mineral assemblage is: quartz, plagioclase, K-feldspar, sepia-brown biotite, hornblende and minor magnetite, ilmenite and allanite; titanite is absent. Geological Province: Bega Batholith.  See also Fig 4 p518.||||||04-DEC-15
7361|Glenbog Suite|23551|5|Briefly described|p495|||I-Type Granite. of Bega Batholith.||||||
7361|Glenbog Suite|24222|5|Briefly described|p9, p17|||Chemistry of samples reported. Comrpises 12 separate plutons. See also Glenbog Supersuite.  Geological Province: Bega Batholith, Lachlan Fold Belt.||||||
7361|Glenbog Suite|24514|5|Briefly described|p33|||I-type granites. Geological Province: Lachlan Fold Belt.||||||
7361|Glenbog Suite|24551|6|Mentioned|p235|||||||||
7361|Glenbog Suite|38822|6|Mentioned|p198|||||||||
7361|Glenbog Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
7361|Glenbog Suite|42827|6|Mentioned|p428|||||||||
7361|Glenbog Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
7361|Glenbog Suite|44093|5|Briefly described|p218 App. 1|Early Devonian|Early Devonian|Orogenic granite. Geological Province: Lachlan Fold Belt.||||||
7361|Glenbog Suite|60423|6|Mentioned|p374|||Geological Province: Lachlan Fold Belt. Of the Bega Batholith||||||
7361|Glenbog Suite|64571|6|Mentioned|p834|||||||||
7361|Glenbog Suite|66300|6|Mentioned|p41, 46.||||||Includes Boro Granite.|||29-OCT-13
7361|Glenbog Suite|68592|3|Fully described|p74 Tb.5, p1674-81|Early Devonian|Early Devonian|Glenbog Granodiorite (Chappell et al. 1987) is the type pluton: E of Nimmitabel. Named after nearby Glenbog State Forest. Called Lake Bathurst Suite by Chappell et al. (1991). Low Sr values. Goulburn structural zone: deformation described.||Unit in Glenbog Supersuite.|Includes Bundong, Ballallaba, Boro Granites; Glenbog, Yalgatta, Towamba, Frogs Hollow, Anembo Granodiorites; Nimmitabel, Towneys Creek and Cannabul Adamellites.|Intrudes Abercrombie Formation, Bendoc and Margules Groups, Covan Creek Formation and Long Flat Volcanics.|Granite, granodiorite, monzogranite.|
7361|Glenbog Suite|69159|5|Briefly described|Map legend|Pragian|Pragian||||Includes Bundong, Mullens, Boro and Ballallaba Granites.|||07-SEP-15
7361|Glenbog Suite|69270|5|Briefly described|p1, p15-16, p20, p23, p30, p34|Early Devonian|Early Devonian|Chappell et al. (1991) assigned Anembo Granodiorite to Glenbog Suite, an interpretation supported by the fact that this new magmatic crystallisation age is indistinguishable from that of the only other dated unit within the suite: ~412 Ma Boro Granite (Bodorkos and Simpson, 2008).||Glenbog Supersuite|Anembo Granodiorite, Towneys Creek Monzogranite, Glenbog Granite and Boro Granite|||
7361|Glenbog Suite|69876|5|Briefly described|p316|||Australian mainland. Discussed in relation to mafic enclaves and restite model.|||||I-type granite.|
7361|Glenbog Suite|70192|5|Briefly described|Map Legend|Pragian|Pragian|On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Bundong Granite.|||
7361|Glenbog Suite|70542|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Bundong Granite|||
7361|Glenbog Suite|71069|5|Briefly described|p9, p26 fig 9, p28, p29, p40 fig 17, p42|Early Devonian|Early Devonian||||Includes the Anembo Granodiorite, Boro Granite and the Bundong Granite|Overlain by the Hoskinstown Group.|Granites.|
7361|Glenbog Suite|71699|5|Briefly described|Map legend.|Devonian|Devonian||||Boro, Ballallaba, Mullens, Bundong Granites.|||
7361|Glenbog Suite|71700|2|Defined|viii, ix, p7, p26, p28, CD|Early Devonian|Early Devonian|Named for the Glenbog Granodiorite which is also the type pluton for this suite. Chappell et al. (1991) used the invalid name"Lake Bathurst Suite" which included a single pluton, the"Lake Bathurst Granite". This pluton is now regarded as Bundong Granite (Dgo) and is included in the Glenbog Suite (Thomas & Pogson 2012). the Glenbog Suite also includes the Glenbog Granodiorite, Yalgatta Granodiorite, Towamba Granodiorite, Frogs Hollow Granodiorite, Anembo Granodiorite, Nimmitabel Adamellite, Towneys Creek Adamellite and Cannabul Adamellite. See also p36-p38, p41, p44, p50, p57, p65-p66, p76, p80-p81, p85. Distribution, geomorphic expression, outcrop,  structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed.||Glenbog Supersuite|Includes the Ballallaba Granite, Boro Granite, Bundong Granite and the Mullens Granite.|Faulted against the Thurralilly Suite and Braidwood Suite.|Granitoids containing quartz, plagioclase, K-feldspar, biotite, hornblende and minor magnetite, ilmenite and allanite.|
7362|Glenbog Supersuite|22876|6|Mentioned|p23 Table 4|||||||||
7362|Glenbog Supersuite|22877|5|Briefly described|map|Silurian|Silurian|||||||
7362|Glenbog Supersuite|22878|4|Described|p57|||||||||
7362|Glenbog Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
7362|Glenbog Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Blue Gum Tonalite, Buldah Gap Granodiorite, Weeragua Granodiorite, Cann Mountain Granite, Whitegum Tonalite, Fiddlers Green Granite, Archie Granodiorite, Coopracambra Tonalite||||||01-OCT-04
7362|Glenbog Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
7362|Glenbog Supersuite|23549|4|Described|p520|||Occurs along the western side of the Bega Batholith. Includes the Blue Gum and Glenbog Suites.||||||05-APR-05
7362|Glenbog Supersuite|24222|6|Mentioned|p14|||See also Glenbog Suite.  Geological Province: Lachlan Fold Belt.||||||
7362|Glenbog Supersuite|24551|5|Briefly described|p235|||Includes the Blue Gum and Glenbog suites.||||||
7362|Glenbog Supersuite|42627|5|Briefly described|Map legend|Wenlock|Wenlock|Variation on Glenbog Suite?||||||
7362|Glenbog Supersuite|42726|5|Briefly described|map legend|||||||||
7362|Glenbog Supersuite|42827|5|Briefly described|p429|||||||||
7362|Glenbog Supersuite|60541|6|Mentioned|p64|||Includes Blue Gums Tonalite. Watchmaker Granodiorite may be associated with this supersuite because of its similarity to the Blue Gums Tonalite. Geological Province: Lachlan Fold Belt.||||||20-JUN-05
7362|Glenbog Supersuite|68592|5|Briefly described|p24, p1674-81|Early Devonian|Early Devonian|First mapped and described by Beams (1980), and decribed by Douglas and Ferguson (1988). Named after Glenbog Granodiorite (Chappell et al. 1987). A north-trending belt 300 x 15 km forming the westernmost part of the Bega Batholith. Unfractionated I-type.|||Includes Badja, Blue Gum, Cathcart, Glenbog and Myocum Suites (NSW); and Archie Granodiorite with Blue Gums, Coopracambra and Whitegum Tonalites (Vic).|||
7362|Glenbog Supersuite|69270|6|Mentioned|p15||||||Glenbog Suite|||
7362|Glenbog Supersuite|71700|2|Defined|vi, CD|||Named for the Glenbog Granodiorite which is also the type pluton for this supersuite. See Glenbog Suite for further information regarding distribution, geomorphic expression, outcrop, depositional environment, lithology, structure, metamorphism, geochemistry, geophysical characteristics, unit relationships, age, distinguishing features and economic geology.|||Includes the Glenbog Suite, Badja Suite, Cathcart Suite, Myocum Suite, Archie Granodiorite, Blue Gum Suite, Blue Gums Tonalite, Coopracambra Tonalite and Whitegum Tonalite.|||
7375|Glendalough Formation|13139|5|Briefly described|p7|Llandovery|Llandovery|Of the Waugoola Group. Geological Province: Lachlan Orogen.||||||15-JUL-08
7375|Glendalough Formation|22486|5|Briefly described|p 7|||Waugoola Group.||||||15-JUL-08
7375|Glendalough Formation|22857|4|Described|p468 App.1 Tb.A1.6|Wenlockian|Llandovery|Of the Waugoola Group. Shale, limestone, siltstone, calcareous and feldspathic arenite, conglomerate; contains graptolites. Max. thickness: 132m. Geological Province: Molong Rise. ||||||
7375|Glendalough Formation|23214|2|Defined|p110|Wenlock|Llandovery|Of Waugoola Group. Originally included in the Panuara Formation (subsequently Panuara Group).||||||
7375|Glendalough Formation|23334|5|Briefly described|7|||||||||
7375|Glendalough Formation|35258|4|Described|p122|||||||||
7375|Glendalough Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
7375|Glendalough Formation|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Waugoola Group. Consists of green-grey, black and red shale; calcareous, feldspathic sandstone; limestone.||||||15-JUL-08
7375|Glendalough Formation|43653|5|Briefly described|Map Legend||Silurian|||||||
7375|Glendalough Formation|43782|6|Mentioned|Map diagram|Wenlock|Llandovery|Of Waugoola Group.||||||15-JUL-08
7375|Glendalough Formation|63287|5|Briefly described|p317 Fig. 2|Wenlock|Llandovery|Of Waugoola Group. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
7375|Glendalough Formation|63290|5|Briefly described|p401 Fig. 5(d)|Llandovery|Llandovery|Of Waugoola Group. Underlain by Chaucer Redbed Member.||||||
7375|Glendalough Formation|68592|6|Mentioned|p416, p1866-7|Llandovery|Llandovery|15-20 km E of Canowindra. Contains the conodont Astropentagnathus irregularis.||Unit in Waugoola Group.||||
7375|Glendalough Formation|70297|5|Briefly described|map legend|Early Silurian|Early Silurian|||Waugoola Group||||
7375|Glendalough Formation|70684|5|Briefly described|p50 Fig.24|Early Silurian|Early Silurian|Molong Volcanic Belt. ||Waugoola Group.|Burly Jacky Sandstone Member, Chaucer Redbed Member.|||
7380|Glendon Siltstone Member|33867|5|Briefly described|p6|||||||||
7380|Glendon Siltstone Member|34043|6|Mentioned|p451|||||||||
7380|Glendon Siltstone Member|34345|4|Described|p333|||||||||
7380|Glendon Siltstone Member|39830|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
7380|Glendon Siltstone Member|45090|5|Briefly described|p165|||||||||
7380|Glendon Siltstone Member|61201|6|Mentioned|p7|||Of the Mulbring Siltstone.||||||
7410|Gleneski Formation|22857|5|Briefly described|p466 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Mumbil Group. Rhyolitic, felsic to latitic lava, intrusives and tuff. Max. thickness: 1200m. ||||||
7410|Gleneski Formation|23043|5|Briefly described|Map Legend|Lochkovian|Wenlock|Of the Mumbil Group.||||||18-FEB-08
7410|Gleneski Formation|23170|2|Defined|p94|Ludlow|Ludlow|Of the Mumbil Group. Age: 417Ma. U/Pb SHRIMP Zircon.||||||18-FEB-08
7410|Gleneski Formation|24126|6|Mentioned|p148|||||||||
7410|Gleneski Formation|30657|6|Mentioned|p26|||Silurian age||||||
7410|Gleneski Formation|31161|5|Briefly described|PA3|||||||||
7410|Gleneski Formation|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
7410|Gleneski Formation|32046|6|Mentioned|p127|||See also p128,131,135,137||||||
7410|Gleneski Formation|32047|6|Mentioned|p2|||Acid volcanism along Molong Rise||||||
7410|Gleneski Formation|32088|6|Mentioned|p10|||||||||
7410|Gleneski Formation|32485|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
7410|Gleneski Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
7410|Gleneski Formation|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
7410|Gleneski Formation|37727|4|Described|p60|||See also p31.||||||18-FEB-08
7410|Gleneski Formation|39663|6|Mentioned|Table 1|||||||||
7410|Gleneski Formation|40328|5|Briefly described|p143|||||||||
7410|Gleneski Formation|43476|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition) Middle Silurian||||||
7410|Gleneski Formation|43494|6|Mentioned|p10|Silurian|Silurian|Volcanics.||||||09-MAR-06
7410|Gleneski Formation|50124|5|Briefly described|p126|Early Devonian|Late Silurian|Of the Mumbil Group. Geological Province: eastern Lachlan Fold Belt.||||||
7410|Gleneski Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Mumbil Group.  Rhyolitic, felsic to latitic lava, intrusive and tuff and volcaniclastic sandstone.||||||
7410|Gleneski Formation|68003|5|Briefly described|p24 Fig.3-e, p145. |Pridoli|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion. Mis-spelt as Glenesgi Formation on p24.||Unit in Mumbil Group.|||Rhyolitic to latitic lava, intrusion and tuff and volcaniclastic sandstone.|
7410|Gleneski Formation|68004|5|Briefly described|p119.|Late Silurian|Middle Silurian|Hosts known Kuroko VHMS occurrences. Has high potential and a certainty level of C.||||||
7410|Gleneski Formation|73299|6|Mentioned|p1105|Early Devonian|Silurian|Hill End Trough, western. [Map symbol suggests Silurian age]||||||
7413|Glengarry Granite|42726|5|Briefly described|map legend|Silurian||235. Wyangala Batholith.||||||
7413|Glengarry Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Massive hornblende -biotite allanite granite.||||||
7413|Glengarry Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Coarse- to medium-grained, massive, equigranularallanite-hornblende?- biotite granite. High K, Th and U. redioelement response.||||||27-JUN-13
7413|Glengarry Granite|68592|2|Defined|p1379, p1382, p1393-6|Early Devonian|Late Silurian|Named after Olde Glengarry homestead and Parish of Glengarry. Originally recorded by Stevens (1955) and Brunker and Offenberg (1970) as part of undifferentiated Wyangala Batholith. Individually described and named by Yacopetti (1987). Forms a small sub-circular pluton which crops out as large rounded tors. Type locality described. Geochemistry detailed; highly felsic, may be A-type, and thus possibly part of the nearby Keverstone Supersuite. Geophysical properties briefly described. Very poor age constraints.||||Intrudes Adaminaby Group.|Massive, coarse- to medium-grained, equigranular, hornblende?-biotite granite.|
7413|Glengarry Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sxg. Ungrouped Silurian intrusion. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.|||||Coarse to medium grained, massive, equigranular, hornblende?-biotite granite.|
7413|Glengarry Granite|70544|5|Briefly described|Map Legend|Silurian|Silurian||||||Coarse to medium grained, massive, equigranular, hornblende?-biotite granite.|
7420|Gleninga Formation|9548|5|Briefly described|Map Legend|Zlichovian|Zlichovian|Of the Yarra Yarra Creek Group. Overlies: Inverleith Sandstone.||||||
7420|Gleninga Formation|22831|4|Described|p 56- 57|Emsian|Pragian|Yarra Yarra Creek Group||||||
7420|Gleninga Formation|22857|4|Described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Yarra Yarra Creek Group. Max. thickness: 350m. Geological Province: Darling Basin. ||||||
7420|Gleninga Formation|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
7420|Gleninga Formation|42449|6|Mentioned|p22|||Reserved 1978, D. Pogson. Last update May 1991.||||||
7420|Gleninga Formation|42566|5|Briefly described|Fig.25 P103|||||||||
7420|Gleninga Formation|43441|6|Mentioned|29||Early Devonian|||||||08-JAN-10
7420|Gleninga Formation|44160|5|Briefly described|Map Legend|Emsian|Pragian|||||||08-JAN-10
7420|Gleninga Formation|66498|6|Mentioned|p43|Emsian|Pragian|Contains vertebrate macro-remains closely resembling those in the Buchan Group.|||Jerula Limestone Member.|||
7420|Gleninga Formation|70751|6|Mentioned|p12|Pragian|Lochkovian|||Yarra Yarra Creek Group|Includes the Jerula Limestone Member.|||
7420|Gleninga Formation|72958|6|Mentioned|p11|Emsian|Pragian|Cobar Basin. Nymagee area.||Yarra Yarra Creek Group, Cobar Supergroup|Jerula Limestone Member|Underlain by Inverleith Sandstone.||
7422|Glenlawn Mudstone|32865|6|Mentioned|p481|||||||||
7422|Glenlawn Mudstone|32869|6|Mentioned|p166|||Refers Manser (1968)||||||
7422|Glenlawn Mudstone|37987|6|Mentioned|p223|||||||||
7422|Glenlawn Mudstone|43417|4|Described|Map Legend||Early Carboniferous|||||||
7422|Glenlawn Mudstone|45088|6|Mentioned|p11|||Refers Manser (1967,1968)||||||
7422|Glenlawn Mudstone|68005|5|Briefly described|p147.|Carboniferous|Carboniferous|||Unit in Tangaratta Formation.|||Mudstone, siltstone, sandstone, lithic sandstone.|
7423|Glenlee Rhyolite|22857|5|Briefly described|p492 App.1 Tb.A1.7|Devonian|Devonian|Of the Hyandra Creek Group. Porphyritic rhyolite, green rhyolite. Max. thickness: 200m.||||||
7423|Glenlee Rhyolite|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Hyandra Creek Group.||||||
7423|Glenlee Rhyolite|23170|2|Defined|p210||Early Devonian|of Hyandra Creek Group.||||||
7423|Glenlee Rhyolite|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
7423|Glenlee Rhyolite|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
7423|Glenlee Rhyolite|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
7423|Glenlee Rhyolite|68003|5|Briefly described|p24 Fig.3-e, p142. |Lochkovian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Hyandra Group.|||Porphyritic rhyolite, green rhyolite.|
7435|Glenmore Formation|22857|4|Described|p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Volcanic Group. Boulder conglomerate coarse arenite, epiclastics and fossiliferous limestone. Max. thickness: 100m. Geological Province: New England Fold Belt.||||||17-FEB-06
7435|Glenmore Formation|23050|4|Described|p14 Table 1|Late Permian|Early Permian|Age: Fossils indicate an Early to early Late Permian age.||||||
7435|Glenmore Formation|23051|5|Briefly described|Map Legend|Late Permian|Early Permian|of Wandsworth Volcanic Group.||||||
7435|Glenmore Formation|42748|2|Defined|p4|Late Permian|Early Permian|previously known as the Glenmore beds and Lower Glenmore Beds.||||||
7435|Glenmore Formation|44093|5|Briefly described|p238 App. 1|Late Permian|Late Permian|Age: Early-early Late Permian. Shallow marine, minor folding, unmetamorphosed. Geological Province: New England Fold Belt.||||||
7435|Glenmore Formation|68005|5|Briefly described|p22, p42, p153, p170.|Early Permian|Early Permian|Central Block, New England Fold Belt. Shallow-marine sequence. Average thickness 30 m; up to 100 m.||||Unconformably overlies Texas beds. Is unconformably overlain by Emmaville Volcanics.|Texturally and mineralogically immature clastic sediments interbedded rarely with limestone and epiclastic sediments: boulder conglomerate, coarse arenite, minor fossil-bearing calcareous horizons, claystone and coal.|
7435|Glenmore Formation|68006|5|Briefly described|p115.|||||Basal unit of Wandsworth Volcanic Group.|||Contains clastic sediments with rare interbeds of massive fine-grained limestone.|
7440|Glenrock Granodiorite|34544|5|Briefly described|p194|||||||||
7440|Glenrock Granodiorite|34566|6|Mentioned|p38|||Middle Devonian||||||
7440|Glenrock Granodiorite|35257|6|Mentioned|p128|||||||||
7440|Glenrock Granodiorite|36945|6|Mentioned|p13|||||||||
7440|Glenrock Granodiorite|39078|6|Mentioned|p115|||||||||
7440|Glenrock Granodiorite|39568|5|Briefly described|p78|||||||||
7440|Glenrock Granodiorite|40328|4|Described|p206|||||||||
7440|Glenrock Granodiorite|41899|6|Mentioned|p126|||||||||
7440|Glenrock Granodiorite|42931|5|Briefly described|p485|||||||||
7440|Glenrock Granodiorite|68592|5|Briefly described|p1610-2, p1634|||First described (but not named) by Woolnough (1910), then in more detail by Osborne (1949), Osborne and Lovering (1953) and Wesley (2005).||Unit in Arthursleigh Suite.||Intrudes and contact metamorphoses the Bindook Group.|Very homogeneous composition.|
7440|Glenrock Granodiorite|70661|3|Fully described|p3, p4, p33, p36|Early Devonian|Early Devonian|Has metamorphosed Bungonia Group to skarn and marble. Name derived either from Glenrock property or Glenrock trigonometrical station. Now includes rocks of the former Uringalla Granodiorite. Type section mentioned.  Distribution, structure, metamorphism, geochemistry and geophysical characteristics discussed. Age constrained by the age of the Bindook Group that it intrudes and the age of the overlying Tallong Conglomerate. See also  p75, p79 fig 6, p81-p83, p145.||Arthursleigh Suite||Intrudes Bungonia Group, Bindook Group, Adaminaby Group, overlain by Tallong Conglomerate|Equigranular, moderately coarse grained biotite hornblende granodiorite with minor pyroxene. A thin rim of  microgranodiorite occurs throughout. Country rock xenoliths common throughout. Minor pegmatite and aplite phases are also present.|
7440|Glenrock Granodiorite|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Arthursleigh Suite.|||Pink to grey equigranular, moderately coarse-grained biotite hornblende granodiorite with minor pyroxene. Abundant fine-grained enclaves and country rock xenoliths locally.|
7444|Glenroy Conglomerate Member|22857|5|Briefly described|p498 App.1 Tb.A1.7|Visean|Visean|Of the Ararat Formation. Geological Province: Tamworth Forearc Basin.||||||
7444|Glenroy Conglomerate Member|31228|6|Mentioned|p77|||Stratigraphy.||||||
7444|Glenroy Conglomerate Member|44244|5|Briefly described|p48|Carboniferous|Carboniferous|Of the Ararat Formation.  Previously regarded as belonging to the Bingleburra Formation.||||||
7444|Glenroy Conglomerate Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Ararat Formation.  Geological Province: Gresford Block||||||
7447|Glenwood Formation|29986|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
7447|Glenwood Formation|40328|4|Described|p127|||||||||
7447|Glenwood Formation|43500|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition) Part of Toongi Group||||||
7447|Glenwood Formation|48958|6|Mentioned|Plate 1|||||||||
7449|Glory Vale Conglomerate|22612|6|Mentioned|423, 424 fig 2 tbl 1|Early Permian|Early Permian|Parent Manning Group. Max thickness 850 m. Also on pages 425, 426, 428, 429. Geol province New England Orogen||||||
7449|Glory Vale Conglomerate|32094|6|Mentioned|p383|||||||||
7452|Gloucester Coal Measures|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Includes the Craven and Avon Subgroups. Equivalent to Wittingham Coal Measures. Geological Province: Sydney Basin.||||||
7452|Gloucester Coal Measures|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Divided into the Craven and the Avon Subgroups.   Geological Province: New England Fold Belt||||||
7452|Gloucester Coal Measures|29990|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
7452|Gloucester Coal Measures|30911|6|Mentioned|Map legend|Permian|Permian|||||||
7452|Gloucester Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
7452|Gloucester Coal Measures|36057|6|Mentioned|Fig.1|||||||||
7452|Gloucester Coal Measures|36390|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
7452|Gloucester Coal Measures|37065|6|Mentioned|p31|||||||||
7452|Gloucester Coal Measures|37099|4|Described|p255|||||||||
7452|Gloucester Coal Measures|39302|6|Mentioned|p349|||||||||
7452|Gloucester Coal Measures|39308|6|Mentioned|p482|||||||||
7452|Gloucester Coal Measures|40872|6|Mentioned|Fig.2|||||||||
7452|Gloucester Coal Measures|41054|6|Mentioned|p152|||||||||
7452|Gloucester Coal Measures|41226|6|Mentioned|Fig.9|||||||||
7452|Gloucester Coal Measures|41347|4|Described|Table 3|||||||||
7452|Gloucester Coal Measures|41348|5|Briefly described|Map legend|Permian|Permian|Lithic and feldspathic sandstone, conglomerate, carbonaceous siltstone and coal.||||||16-DEC-04
7452|Gloucester Coal Measures|42182|5|Briefly described|p301|Permian|Permian|Overlie the Dewrang Group.  Geological Province: Gloucester Basin||||||
7452|Gloucester Coal Measures|42648|5|Briefly described|p39|||||||||
7452|Gloucester Coal Measures|43447|14|Not recorded|Table 1,p40||Permian|||||||
7452|Gloucester Coal Measures|43491|14|Not recorded|pVII/54||Permian|See also Lexicon||||||
7452|Gloucester Coal Measures|44244|5|Briefly described|p174|Late Permian|Late Permian|Replaced "Avon Coal Measures" of Loughan (1955).  Includes the lower Avon Subgroup and upper Craven Subgroup separated by Speldon Formation. Geological Province: Myall Block : within the Stroud-Gloucester Syncline.  See also p167 and p168 Tb. 2.||||||18-AUG-04
7452|Gloucester Coal Measures|47056|6|Mentioned|Fig.2 P523|||||||||
7452|Gloucester Coal Measures|50099|5|Briefly described|p11-12|Permian|Permian|Overlie the Alum Mountain Volcanics. Max. thickness: 2040m in Booral-Weismantels area. Age: 275 Ma. Geological Province: Tamworth Belt/New England Orogen.||||||
7452|Gloucester Coal Measures|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Includes the Craven and Avon Subgroups.  Geological Province: Western Myall Block.||||||
7452|Gloucester Coal Measures|63832|6|Mentioned|p131 fig 2|Guadalupian|Guadalupian|Myall block, Southern New England Fold Belt. Seventh (P3) and eighth (P4) glaciations.||||||
7452|Gloucester Coal Measures|64631|5|Briefly described|p44 Fig.2.|Wordian|Wordian|Southern New England Fold Belt, Myall Block. Biostratigraphic age control for base and top.||||Overlies Dewrang Group.||
7460|Gnalta Group|12066|5|Briefly described|p13|Cambrian|Cambrian|Includes the Pincally Formaiton, Wydjah Formation and Wyarra Shale.||||||
7460|Gnalta Group|22671|5|Briefly described|p832-33,Fig2p837|Middle Cambrian|Early Cambrian|Comprises: Mount Wright Volcanics, Cymbric Vale  and Coonigan Formations. Consists of volcanics and shallow marine sediments including limestones. Geological Province: Kanmantoo Fold Belt. Geol. Prov: Kanmantoo Fold Belt.||||||16-MAY-13
7460|Gnalta Group|22857|5|Briefly described|p75, p90 Fig. 14.7B|Middle Cambrian||See also p404 App. 1 Tb. A1.4.||||||
7460|Gnalta Group|22858|6|Mentioned|p75,83|||||||||
7460|Gnalta Group|23833|5|Briefly described|p256 Table 1|Cambrian|Cambrian|||||||
7460|Gnalta Group|29991|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
7460|Gnalta Group|30683|6|Mentioned|Table 1|||||||||
7460|Gnalta Group|30908|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower - Middle Cambrian||||||
7460|Gnalta Group|31507|6|Mentioned|p181|||||||||
7460|Gnalta Group|31705|6|Mentioned|p27|||||||||
7460|Gnalta Group|32671|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7460|Gnalta Group|32672|5|Briefly described|p671|||||||||
7460|Gnalta Group|32677|4|Described|p7||Early Cambrian|||||||
7460|Gnalta Group|32948|6|Mentioned|p110|||||||||
7460|Gnalta Group|33000|6|Mentioned|p2|||||||||
7460|Gnalta Group|33004|6|Mentioned|p140|||||||||
7460|Gnalta Group|34469|6|Mentioned|p109|||Table. Lower & Middle Cambrian||||||
7460|Gnalta Group|35235|6|Mentioned|p209|||||||||
7460|Gnalta Group|35320|6|Mentioned|p463|||||||||
7460|Gnalta Group|36534|6|Mentioned|p227|||||||||
7460|Gnalta Group|39214|5|Briefly described|p9|||||||||
7460|Gnalta Group|40595|6|Mentioned|Fig.7|||||||||
7460|Gnalta Group|40642|6|Mentioned|p171|||||||||
7460|Gnalta Group|41457|6|Mentioned|p1|||||||||
7460|Gnalta Group|41810|6|Mentioned|p111|||||||||
7460|Gnalta Group|42206|5|Briefly described|p257|||See also Fig.1||||||
7460|Gnalta Group|42982|5|Briefly described|Table 1,p333|||||||||
7460|Gnalta Group|43192|4|Described|p63,Table 1 p61.|Middle Cambrian|Early Cambrian|Time equivalent to Teltawongee Beds?||||||
7460|Gnalta Group|43213|5|Briefly described|p63|||Folded into tight upright folds during Delamerian Orogeny (late Middle Cambrian).||||Correlated with Teltawongee beds.|Mafic to silicic volcanics, sandstone and carbonates.|
7460|Gnalta Group|43263|6|Mentioned|Map Legend||Early Cambrian|||||||
7460|Gnalta Group|43502|14|Not recorded|Map Legend|Middle Cambrian|Early Cambrian|(Provisional Edition) Inc. Coonigan Formation,Cymbric Vale Formation,Mount Wright Volcs(L-L.M.Camb)||||||
7460|Gnalta Group|43704|4|Described|p67|Middle Cambrian|Early Cambrian|||||||
7460|Gnalta Group|44093|5|Briefly described|p143 App. 1|Early Cambrian|Early Cambrian|Calc-alkaline volcanics, limestone and clastic sediments. Geological Province: Kanmantoo Fold Belt.||||||
7460|Gnalta Group|47026|6|Mentioned|Fig.5|||||||||
7460|Gnalta Group|50618|5|Briefly described|p248 Fig. 1|Middle Cambrian|Early Cambrian|Geological Province: Wonominta Block.||||||
7460|Gnalta Group|60567|5|Briefly described|p39|||||||||
7460|Gnalta Group|60648|5|Briefly described|p43 Fig. 3|Early Paleozoic|Early Paleozoic|Geological Province: Darling Basin.||||||07-NOV-08
7460|Gnalta Group|60990|5|Briefly described|p81, p86|Middle Cambrian|Early Cambrian||||Mount Wright Volcanics, Cymbric Vale Formation and Coonigan Formation.|Considered to be coeval with the Teltawongee beds by Mills(1992)||
7460|Gnalta Group|61311|5|Briefly described|p43 Table D1|Early Paleozoic|Precambrian|Marine carbonates, volcanics and clastics. Geological Province: Darling Basin.||||||07-NOV-08
7460|Gnalta Group|62787|4|Described|p76 Fig. 1, p80|Middle Cambrian|Early Cambrian|Includes Wyarra Shale, Wydjah, Coonigan and Pincally Formations, Mount Wright Volcanics. Unconf. Overlain by Nootumbulla Sandstone. Geological province: Koonenberry Belt.||||||16-MAY-13
7460|Gnalta Group|62795|6|Mentioned|p347, p348 Fig.1|Middle Cambrian|Middle Cambrian|Unconformably underlies Mutawintji Group.||||||
7460|Gnalta Group|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Basic, intermediate and acid volcanics, shale, carbonate.||||||
7460|Gnalta Group|63789|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Includes Coonigan Formation, Cymbric Vale Formation and Mount Wright Volcanics.||||||08-DEC-08
7460|Gnalta Group|63793|5|Briefly described|p18,20,22.|Middle Cambrian|Early Cambrian|Formerly part of Wonominta beds (Warris 1967). Contains archaeocyathans. Shallow-water, near-shore facies coeval with Teltawongee beds, slope deposits to the east.||Unit in Wonominta beds.|Includes Mount Wright Volcanics, Cymbric Vale Formation and Coonigan Formation.|Is unconformably overlain by Mootwingee Group.||19-JAN-15
7460|Gnalta Group|64168|5|Briefly described|p30, p31|Early Cambrian|Early Cambrian|Age: 525Ma. Geological Province: Koonenberry Belt. Shows calc-alkaline volcanism.||||||01-JUL-08
7460|Gnalta Group|64671|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Includes Coonigan and Cymbric Vale Formations. Unconformably overlain by Mootwingee Group; fault bounded against Ponto beds and Mount Arrowsmith Volcanics.||||||
7460|Gnalta Group|64679|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Comprises Mount wright Volcanics, Cymbric Vale and Coonigan Formations.||||||
7460|Gnalta Group|64680|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Includes Coonigan and Cymbric Vale Formations, and Mount Wright Volcanics. Unconformably overlain by Mootwingee Group, fault bounded against Ponto Group and Mount Arrowsmith Volcanics. Basic, intermediate, felsic volcanics, shale, carbonates.||||||
7460|Gnalta Group|64684|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Unconformably overlain by Mootwingee Group, fault bounded against Ponto Group and Mount Arrowsmith Volcanics. Basic, intermediate, felsic volcanics, shale carbonates.||||||16-MAY-13
7460|Gnalta Group|64686|5|Briefly described|Map Legend|Middle Cambrian|Early Cambrian|Unconformably overlain by Mootwingee Group, fault bounded against Ponto Group and Mount Arrowsmith Volcanics. Basic, intermediate, felsic volcanics, shale, carbonate.||||||08-DEC-08
7460|Gnalta Group|65381|6|Mentioned|p691, Fig 2|Middle Cambrian|Early Cambrian|||||||
7460|Gnalta Group|65892|6|Mentioned|p43. |||Western New South Wales. Contains 13 species of archaeocyatha in common with Cymbric Vale Formation in South Australia.||||||
7460|Gnalta Group|66623|1|Redefined|pp56-73, p v, p44. |Late Cambrian|Early Cambrian|Formerly the lower 'Gnalta Stage' of Mootwingee Series (Kenny 1934); redefined as Gnalta Group by Warris (1967); again redefined (this study) to include clastic and volcaniclastic rocks on southwestern flanks of Mount Arrowsmith Inlier because of age, felsic volcaniclastic content and geographic position. 500m to c.3800m thick. Low-grade metamorphosed. Coeval with Ponto Group.|||Includes Mount Wright Volcanics; Cymbric Vale, Coonigan, Pincally and Wydjah Formations; and Wyarra Shale.|Is unconformably or disconformably overlain by Nuchea Conglomerate. Fault-bound against Pimbilla Tank Group.|Calc-alkaline volcanic rocks (andesite, dacite), tuff, chert, mudstone, siltstone, limestone and dolostone with oncolites, sandstone; minor conglomerate.|
7460|Gnalta Group|66917|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Pincally and Wydjah Formations and Wyarra Shale.||Undifferentiated fossiliferous shale, carbonate and siltstone.|
7460|Gnalta Group|66918|5|Briefly described|Map legend|Cambrian|Cambrian||||Includes Mount Wright Volcanics, Cymbric Vale and Coonigan Formations.||Undifferentiated fossiliferous shale, carbonate and siltstone.|
7460|Gnalta Group|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Narrow zone of low magnetic intensity with rare moderately-magnetic lenticular trends.|||||Shale, carbonate and siltstone.|
7460|Gnalta Group|66929|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|||||Faulted against Ponto Group and Mount Arrowsmith Volcanics. Is unconformably overlain by Mootwingee Group.|Basic, intermediate, felsic volcanics; shale; carbonate.|
7460|Gnalta Group|67105|5|Briefly described|p650, 652-655, 659, 661|Cambrian|Cambrian|Wonnaminta Zone (arc and forearc), Koonenberry Belt. Delamerian Orogeny Cycle deposits. Contains Templetonian stage trilobites (~508 Ma; Percival, 2010).|||Mount Wright Volcanics, Cymbric Vale Formation.||Includes calc-alkaline volcanics, and volcaniclastic rocks.|
7460|Gnalta Group|67208|5|Briefly described|Map legend.|Cambrian|Cambrian||||Includes basal Mount Wright Volcanics, Pincally and Wydjah Formations, and Wyarra Shale.||Fossiliferous shale, carbonate and siltstone; regionally metamorphosed to prehnite-pumpellyite facies; sandstone and conglomerate; andesitic lavas|20-SEP-13
7460|Gnalta Group|67322|5|Briefly described|p3 Fig.1, p5, p8-9; Fig.5|Series 3|Series 2|Koonenberry Belt, Delamerian Orogen. Of Warris (1967); redefined by Percival, in Greenfield et al. (2010). Age from p20 Fig.5 (Strat. column). Occurs in the Mount Wright-Mutawintji area.|||Mount Wright Volcanics, Coonigan Formation, Wydjah Formation, Pincally Formation, Cymbric Vale Formation, Wyarra Shale||Mostly shallow-water lithologies.|22-FEB-18
7460|Gnalta Group|69445|5|Briefly described|p30:17|Early Cambrian|Early Cambrian|Gnalta Shelf, western NSW.|||Mount Wright Volcanics, Cymbric Vale Formation.|Correlated with Kalkarindji Suite.||12-JUL-16
7460|Gnalta Group|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Interpreted equivalent to sedimentary and volcanic rocks in the Wirryilka (geophysical basement) Zone. Thought to have accumulated in close proximity to the Mount Wright Volcanic Arc, which was active along the E margin of Gondwana at the time.|||Includes Mount Wright Volcanics, Cymbric Vale and Coonigan Formations.|||
7460|Gnalta Group|70210|5|Briefly described|p1|Middle Cambrian|Middle Cambrian|Koonenberry-Tibooburra district.|||Cymbric Vale Formation.|||
7460|Gnalta Group|70296|6|Mentioned|p2|||Koonenberry District.|||Includes the Cymbric Vale Formation.|||22-JAN-21
7460|Gnalta Group|70648|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Mount Wright Volcanics, Cymbric Vale Formation.||Fossiliferous shale, carbonate and siltstone; undifferentiated andesitic lavas, felsic ignimbrites, reworked tuffs, and associated intrusions; regionally metamorphosed to prehnite-pumpellyite facies.|20-JAN-22
7460|Gnalta Group|70650|5|Briefly described|Map Legend|Cambrian|Cambrian||||Includes Coonigan Formation, Cymbric Vale Formation, Mount Wright Volcanics.||Fossiliferous shale, carbonate and siltstone; andesitic lavas, felsic ignimbrites, reworked tuffs, and associated intrusions; regionally metamorphosed to prehnite-pumpellyite facies.|
7460|Gnalta Group|70749|6|Mentioned|p43|Cambrian|Cambrian|Southern Thomson and Koonenberry area.||||||
7460|Gnalta Group|70838|5|Briefly described|p267 Fig.1, p268-269, p271|Cambrian|Cambrian|NW Koonenberry Belt. Possible tectonic settings discussed. Maximum depositional age is poorly constrained. Deformed during the Delamerian Orogeny (c.500 Ma).|||Mount Wright Volcanics; Cymbric Vale, Coonigan Formations.|Is overlain unconformably by Mutawintji Group.|Volcanic and sedimentary sequences.|
7460|Gnalta Group|71262|5|Briefly described|p3, p5 Fig 2, p10|Middle Cambrian|Early Cambrian||||Includes Mount Wright Volcanics||Calc-alkaline volcanic and associated sedimentary rocks.|
7460|Gnalta Group|71593|5|Briefly described|p188|Early Cambrian|Early Cambrian|Koonenberry Province.|c. 511-506 Ma|||||
7460|Gnalta 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).||||||
7460|Gnalta Group|71966|6|Mentioned|p990,999|Cambrian|Cambrian|Geological province: Delamarian Orogen.||||||
7460|Gnalta Group|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Undifferentiated fossiliferous shale, carbonate and siltstone.|09-DEC-21
7460|Gnalta Group|73177|5|Briefly described|p1098, 1100, 1114, 1115 Fig.17|Middle Cambrian|Early Cambrian||||Mount Wright Volcanics, Cymbric Vale Formation.|||30-AUG-22
7460|Gnalta Group|73430|6|Mentioned|p494|Middle Cambrian|Early Cambrian|Koonenberry Belt. Deformed by the Delamerian Orogeny.|||||Sedimentary unit.|
7469|Gobondery Granite|22519|5|Briefly described|p8|Devonian|Devonian|||||||
7469|Gobondery Granite|22831|4|Described|p 50|Lochkovian|Lochkovian|Perviously "Gillenbine granite"||||||
7469|Gobondery Granite|29986|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
7469|Gobondery Granite|33480|6|Mentioned|p243|||Refers age dating||||||
7469|Gobondery Granite|33732|6|Mentioned|p114|||||||||
7469|Gobondery Granite|36066|6|Mentioned|Fig.4|||||||||
7469|Gobondery Granite|39627|6|Mentioned|Appendix|||||||||
7469|Gobondery Granite|40328|4|Described|p206|||||||||
7469|Gobondery Granite|40365|6|Mentioned|p243|||||||||
7469|Gobondery Granite|42077|5|Briefly described|p27|||||||||
7469|Gobondery Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
7469|Gobondery Granite|42906|6|Mentioned|p4|||||||||
7469|Gobondery Granite|43441|5|Briefly described|28|Early Devonian|Early Devonian|||||||08-JAN-10
7469|Gobondery Granite|43510|14|Not recorded|p69,70||Middle Devonian|Tullamore area. Significant contact metamorphism present||||||
7469|Gobondery Granite|44160|5|Briefly described|Map Legend||Lochkovian|||||||08-JAN-10
7469|Gobondery Granite|48958|6|Mentioned|Plate 1|||||||||
7469|Gobondery Granite|71206|6|Mentioned|p384|||Lachlan Fold Belt.||||||
7470|Gocup Granite|22768|6|Mentioned|p175,178|||||||||
7470|Gocup Granite|22857|6|Mentioned|p175|||||||||
7470|Gocup Granite|29648|3|Fully described|p16|||||||||
7470|Gocup Granite|35318|6|Mentioned|p469|||Structural geology||||||
7470|Gocup Granite|36534|6|Mentioned|p229|||||||||
7470|Gocup Granite|37259|6|Mentioned|p5|||||||||
7470|Gocup Granite|37270|6|Mentioned|Table 2|||||||||
7470|Gocup Granite|37529|6|Mentioned|p5|||||||||
7470|Gocup Granite|39331|6|Mentioned|p36|||||||||
7470|Gocup Granite|40328|4|Described|p206|||||||||
7470|Gocup Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
7470|Gocup Granite|40498|6|Mentioned|p368|||||||||
7470|Gocup Granite|42313|2|Defined|p151|Early Devonian|Early Devonian|||||||
7470|Gocup Granite|42314|5|Briefly described|Map|Early Devonian||||||||
7470|Gocup Granite|42497|5|Briefly described|Map Legend|Lochkovian|Pridolian|||||||
7470|Gocup Granite|42726|5|Briefly described|map legend|Silurian||||||||
7470|Gocup Granite|42828|5|Briefly described|Table 1 P129|Early Devonian||||||||
7470|Gocup Granite|44092|5|Briefly described|map legend|Silurian|Silurian|glw6||||||
7470|Gocup Granite|44093|6|Mentioned|p30 Fig 4.8B|||||||||
7470|Gocup Granite|60078|6|Mentioned|Map Legend||Silurian|||||||
7470|Gocup Granite|63290|6|Mentioned|p403 Fig. 6(c)|Silurian|Silurian|Granite.||||||
7470|Gocup Granite|64571|5|Briefly described|p822, p828|Devonian|Silurian|Age: 409+/-3Ma (K/Ar and Rb/Sr).||||||15-DEC-08
7470|Gocup Granite|66197|6|Mentioned|p631 Fig.3a|Early Devonian|Early Devonian|Granitic pluton. 411 +/- 5 Ma. ?Underlies the Minjary Volcanics. Tumut Trough.||||||14-MAR-12
7470|Gocup Granite|71040|5|Briefly described|p8 Fig.5, p9, p11, p26|||Tumut Trough. Predates (and provides a maximum age for) deformation associated with Bindian (= Bowning) Orogeny.|411 +/- 5 Ma (Stuart-Smith et al., 1992).|||||
7470|Gocup Granite|73215|5|Briefly described|p994|||Tumut Trough.|411 +/- 5 Ma (Stuart-Smith et al., 1992).|||||
7481|Gogs Top Trondhjemite|39874|6|Mentioned|p374|||||||||
7481|Gogs Top Trondhjemite|70217|5|Briefly described|p72, p73 tbl 14.1|Wuchiapingian|Wuchiapingian|New England Orogen. Ages are similar to the Mount Ephraim Granodiorite. |c. 255 Ma (Rb-Sr, Hensel et al, 1985)|Clarence River Supersuite||||
7481|Gogs Top Trondhjemite|70876|5|Briefly described|p78|Permian|Permian|New England Orogen. Date is derived from Rb-Sr whole rock dating. [Either part of the Clarence River Supersuite or a correlative-not made clear in the text].|c. 255 Ma (Hensel et al, 1985 Ma)|||||
7481|Gogs Top Trondhjemite|71628|4|Described|p18: 1-2, 7-10|||Named after unpublished work by Heugh (1971) and Hensel (1982). Named after a local range or creek. Occurs ~22 km SE of Nundle; poor outcrop. Extensively sheared. Limited (one analysis) geochemistry described. Is associated with minor copper-haematite mineralisation.|253 Ma (Rb-Sr biotite; Hensel, 1982 unpub).|Duncans Creek Suite.||Abuts Barry Igneous Complex. Is bounded by (?intrudes) Cascade Creek Beds).|Fine- and medium-grained, equigranular, hornblende-biotite trondhjemite-tonalite; locally sheared. I-type.|
7502|Golden Gully beds|35118|6|Mentioned|p436|||||||||
7540|Good Dog Lamprophyre|40044|6|Mentioned|p382|||||||||
7540|Good Dog Lamprophyre|40266|6|Mentioned|p16|||||||||
7540|Good Dog Lamprophyre|43346|2|Defined|p3,4 Map|||See also Lexicon.  Correlated with Buderoo Lamprophyre||||||
7540|Good Dog Lamprophyre|43349|14|Not recorded|Map|||||||||
7552|Goodravale Limestone|32585|6|Mentioned|p210|||Refers Etheridge (1892)||||||
7560|Goolang Siltstone Member|32801|6|Mentioned|Fig.5|||||||||
7560|Goolang Siltstone Member|32803|6|Mentioned|Fig. 1|||||||||
7560|Goolang Siltstone Member|34340|2|Defined|p461|Triassic|Triassic|||||||
7560|Goolang Siltstone Member|37112|5|Briefly described|Table 1|||||||||
7560|Goolang Siltstone Member|43881|2|Defined|p6-7,10,20-22||Triassic|Member of Bardool Conglomerate||||||
7560|Goolang Siltstone Member|61310|5|Briefly described|Table C1 (p22-23)|Middle Triassic|Middle Triassic|Of the Bardool Conglomerate (Nymboida Coal Measures). Siltstone, claystone, sandstone, minor conglomerate. Geological Province: Clarence-Moreton Basin||||||
7562|Goombargana Granite|42726|5|Briefly described|map legend|Silurian||||||||
7566|Goonda Point Shale|41463|6|Mentioned|Fig.1|||||||||
7567|Goondiwindi Conglomerate|30133|6|Mentioned|Map legend|Permian|Permian|||||||
7567|Goondiwindi Conglomerate|43436|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
7573|Goonoo Goonoo Mudstone|22639|5|Briefly described|p276|||||||||
7573|Goonoo Goonoo Mudstone|22736|6|Mentioned|p630||Tournaisian|||||||
7573|Goonoo Goonoo Mudstone|22857|5|Briefly described|p498 App.1 Tb.A1.7, p220 (photo)|Visean|Fammenian|Of the Parry Group. Max. thickness: ~3400m. Geological Province: Tamworth Forearc Basin.||||||
7573|Goonoo Goonoo Mudstone|22859|5|Briefly described|p220|||||||||
7573|Goonoo Goonoo Mudstone|23157|6|Mentioned|p126|Visean|Late Devonian|||||||
7573|Goonoo Goonoo Mudstone|23185|6|Mentioned|Fig1p156,160||Famennian|||||||
7573|Goonoo Goonoo Mudstone|30070|6|Mentioned|Fig.2|||Devonian age.||||||
7573|Goonoo Goonoo Mudstone|30911|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
7573|Goonoo Goonoo Mudstone|31802|6|Mentioned|p136|||Refers Crook (1961)||||||
7573|Goonoo Goonoo Mudstone|31999|5|Briefly described|p151|||Table 1||||||
7573|Goonoo Goonoo Mudstone|32529|5|Briefly described|p198|||Refers Crook (1961)||||||
7573|Goonoo Goonoo Mudstone|32530|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|L.Carb.-U.Dev.||||||
7573|Goonoo Goonoo Mudstone|32866|6|Mentioned|Fig.11|||||||||
7573|Goonoo Goonoo Mudstone|32869|5|Briefly described|p166|||Depositional environment. See also Fig.2||||||
7573|Goonoo Goonoo Mudstone|34072|6|Mentioned|Fig.4.5|||U.Dev.-Carb.  Fossils||||||
7573|Goonoo Goonoo Mudstone|34080|5|Briefly described|p248|||U.Dev. - Carb.||||||
7573|Goonoo Goonoo Mudstone|34081|6|Mentioned|p259|||||||||
7573|Goonoo Goonoo Mudstone|34555|4|Described|p241|||||||||
7573|Goonoo Goonoo Mudstone|36528|6|Mentioned|p175|||||||||
7573|Goonoo Goonoo Mudstone|37987|2|Defined|p223|Carboniferous|Devonian|Carboniferous - Devonian||||||
7573|Goonoo Goonoo Mudstone|38222|6|Mentioned|p358|||||||||
7573|Goonoo Goonoo Mudstone|39214|6|Mentioned|p33|||||||||
7573|Goonoo Goonoo Mudstone|39331|6|Mentioned|Table 10-1|||||||||
7573|Goonoo Goonoo Mudstone|39623|6|Mentioned|Fig.2|||||||||
7573|Goonoo Goonoo Mudstone|40883|6|Mentioned|p5|||||||||
7573|Goonoo Goonoo Mudstone|41238|4|Described|p82|||||||||
7573|Goonoo Goonoo Mudstone|41279|6|Mentioned|p129|||||||||
7573|Goonoo Goonoo Mudstone|41347|6|Mentioned|p390|||||||||
7573|Goonoo Goonoo Mudstone|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Of the Parry Group.||||||16-DEC-04
7573|Goonoo Goonoo Mudstone|42547|5|Briefly described|p20, p25|||Part equivalent to Tangaratta Formation.||||||
7573|Goonoo Goonoo Mudstone|42997|5|Briefly described|p36|||||||||
7573|Goonoo Goonoo Mudstone|43399|2|Defined|p189,195-197|Tournaisian|Late Devonian|=Lower Burindi Group and Barraba Mudstone(Late U.Devn-Late Tour)||||||
7573|Goonoo Goonoo Mudstone|43400|14|Not recorded|map opp.p.188|Early Carboniferous|Late Devonian|||||||
7573|Goonoo Goonoo Mudstone|43406|14|Not recorded|p42,45,48-50||Tournaisian|Has nine members||||||
7573|Goonoo Goonoo Mudstone|43418|14|Not recorded|Map Legend|||||||||
7573|Goonoo Goonoo Mudstone|43428|14|Not recorded|p141|||||||||
7573|Goonoo Goonoo Mudstone|43432|14|Not recorded|p204|Early Carboniferous|Late Devonian|||||||
7573|Goonoo Goonoo Mudstone|43446|14|Not recorded|p6041,6049||Tournaisian|||||||
7573|Goonoo Goonoo Mudstone|43461|14|Not recorded|p619|||||||||
7573|Goonoo Goonoo Mudstone|43479|14|Not recorded|p158,177|Visean|Tournaisian|||||||
7573|Goonoo Goonoo Mudstone|43575|6|Mentioned|p276|||||||||
7573|Goonoo Goonoo Mudstone|44093|5|Briefly described|p228 App. 1|Tournaisian|Late Devonian|Geological Province: New England Fold Belt.||||||
7573|Goonoo Goonoo Mudstone|44244|2|Defined|p18|Visean|Famennian|Overlies the Baldwin Formation; conformably underlies Waverley Formation.  Max. thickness: >2000m.  Type section in text.  Geological Province: Rouchel Block.||||||
7573|Goonoo Goonoo Mudstone|45088|3|Fully described|p10|||Refers Crook (1961). See also Plate 2||||||
7573|Goonoo Goonoo Mudstone|46803|6|Mentioned|Fig. 3|||||||||
7573|Goonoo Goonoo Mudstone|47056|6|Mentioned|Fig.2 P523|||||||||
7573|Goonoo Goonoo Mudstone|48600|14|Not recorded|Plate 3|||||||||
7573|Goonoo Goonoo Mudstone|48940|6|Mentioned|p15|||Refers Crook||||||
7573|Goonoo Goonoo Mudstone|50099|5|Briefly described|p8-9, p21|Early Carboniferous|Late Devonian|Max. thickness: 1200m. Olive-green to olive-brown mudstone with minor interbedded conglomerate, lithic sandstone and limestone. Geological Province: Tamworth Belt/New England Orogen. Conformably overlain by Waverly Formation.||||||
7573|Goonoo Goonoo Mudstone|50268|5|Briefly described|Map Legend|Tournaisian|Devonian|Underlies: Waverley Formation.  Geological Province: Rouchel Block.||||||
7573|Goonoo Goonoo Mudstone|68005|6|Mentioned|p54.|||(Crook 1961a). The lowest conglomeratic unit is now known as the Keepit Conglomerate.||||||
7573|Goonoo Goonoo Mudstone|71628|6|Mentioned|p18:20|||||Parry Group.||||
7578|Goonumbla Volcanics|5250|6|Mentioned|p42|Late Ordovician||Includes Billabong Creek Limestone Member||||||
7578|Goonumbla Volcanics|13139|6|Mentioned|p10|Ordovician|Ordovician|||||||
7578|Goonumbla Volcanics|22434|5|Briefly described|11 fig 15|Ordovician|Ordovician|See also Goonumbla Volcanic Group p12. Geol province Lachlan Fold Belt||||||
7578|Goonumbla Volcanics|22519|5|Briefly described|p6|||||||||
7578|Goonumbla Volcanics|22659|4|Described|p 280|||||||||
7578|Goonumbla Volcanics|22831|5|Briefly described|p 5|Early Silurian|Late Ordovician|||||||
7578|Goonumbla Volcanics|22857|4|Described|p127, p416 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Andesitic lavas and volcaniclastic arenites. Max. thickness: 4km.||||||
7578|Goonumbla Volcanics|23213|5|Briefly described|p8,23 Fig.10|Late Ordovician|Darriwilian|Correlated with Fairbridge Volcanics, Oakdale Formation, Sofala Volcanics and Wagonga Group. of Junee-Narromine Volcanics Belt.||||||
7578|Goonumbla Volcanics|23245|6|Mentioned|p127|||||||||
7578|Goonumbla Volcanics|23309|6|Mentioned|p390|||||||||
7578|Goonumbla Volcanics|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
7578|Goonumbla Volcanics|23538|4|Described|p 457-458|||Also see p 461 and Fig 1 p 458||||||
7578|Goonumbla Volcanics|23736|4|Described|p11|Eastonian||||||||
7578|Goonumbla Volcanics|24125|5|Briefly described|p3|Silurian|Ordovician|Geological Province: Lachlan Fold Belt.||||||
7578|Goonumbla Volcanics|24215|5|Briefly described|p805|||Geological Province:  Lachlan Fold Belt||||||
7578|Goonumbla Volcanics|24230|5|Briefly described|p171|||||||||
7578|Goonumbla Volcanics|24266|5|Briefly described|p1497|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
7578|Goonumbla Volcanics|24267|4|Described|p1506|||Overlying Unit: Wombin Volcanics. Underlying Unit: Nelungaloo Volcanics. Latitic flows and volcanic breccias. Geological Province: Parkes-Narromine Belt.||||||04-MAR-09
7578|Goonumbla Volcanics|24268|6|Mentioned|p1543 Fig.8|||Geological Province: Lachlan Fold Belt||||||
7578|Goonumbla Volcanics|24417|2|Defined|p21|Ordovician|Ordovician|Bowman et al (1983) subdivided into lower "The Secrets Andesite" and upper "Black Ridge Tuff".  No longer includes Billabong Creek Limestone Mbr and Gunningbland Shale Mbr (raised to formation status). Of Northparkes Volcanic Group.  Max.thickness: 4000m.||||||
7578|Goonumbla Volcanics|29985|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
7578|Goonumbla Volcanics|29986|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
7578|Goonumbla Volcanics|31618|6|Mentioned|p104|||||||||
7578|Goonumbla Volcanics|32156|6|Mentioned|p231|||||||||
7578|Goonumbla Volcanics|32591|6|Mentioned|p119|||||||||
7578|Goonumbla Volcanics|33121|3|Fully described|p57|||Refers Brunker (1968,72).||||||
7578|Goonumbla Volcanics|33125|6|Mentioned|p15|||Correlation chart||||||
7578|Goonumbla Volcanics|33737|6|Mentioned|p168|||||||||
7578|Goonumbla Volcanics|33740|6|Mentioned|p125|||||||||
7578|Goonumbla Volcanics|35118|6|Mentioned|Fig.5|||||||||
7578|Goonumbla Volcanics|35489|6|Mentioned|p91|||||||||
7578|Goonumbla Volcanics|36066|6|Mentioned|Fig.3|||||||||
7578|Goonumbla Volcanics|36297|6|Mentioned|p175|||||||||
7578|Goonumbla Volcanics|39214|5|Briefly described|p17|||||||||
7578|Goonumbla Volcanics|39663|6|Mentioned|Table 4|||||||||
7578|Goonumbla Volcanics|39684|6|Mentioned|Fig.1|||||||||
7578|Goonumbla Volcanics|40127|6|Mentioned|p9|||||||||
7578|Goonumbla Volcanics|40136|5|Briefly described|p26|||||||||
7578|Goonumbla Volcanics|40791|5|Briefly described|p182|||||||||
7578|Goonumbla Volcanics|40891|3|Fully described|p5|||||||||
7578|Goonumbla Volcanics|41046|6|Mentioned|p144|||||||||
7578|Goonumbla Volcanics|42171|6|Mentioned|p144|||||||||
7578|Goonumbla Volcanics|42262|4|Described|p1817|||See also Fig.2 P1810.||||||
7578|Goonumbla Volcanics|42479|6|Mentioned|p107, Fig.2 p110|||||||||
7578|Goonumbla Volcanics|42489|5|Briefly described|Map legend|Llandovery|Darriwilian|||||||
7578|Goonumbla Volcanics|42603|6|Mentioned|p56|||||||||
7578|Goonumbla Volcanics|42718|6|Mentioned|p1|||||||||
7578|Goonumbla Volcanics|43263|6|Mentioned|Map Legend||Ordovician|||||||
7578|Goonumbla Volcanics|43441|5|Briefly described|17, 21|||Age: ?Late Ordovician - Early Silurian||||||08-JAN-10
7578|Goonumbla Volcanics|43499|14|Not recorded|Map Legend||Late Ordovician|(Provisional Edition)||||||
7578|Goonumbla Volcanics|43500|14|Not recorded|Map Legend||Early Ordovician|(Provisional Edition) (M.Ord)||||||
7578|Goonumbla Volcanics|44093|5|Briefly described|p178 App. 1|Ordovician|Ordovician|Of the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||08-MAR-05
7578|Goonumbla Volcanics|44160|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||08-JAN-10
7578|Goonumbla Volcanics|46522|2|Defined|p15|Late Ordovician||||||||
7578|Goonumbla Volcanics|46524|4|Described|p99|||See alsomAppendix 1 P129||||||
7578|Goonumbla Volcanics|46525|6|Mentioned|p149|||||||||
7578|Goonumbla Volcanics|46528|5|Briefly described|Map legend|Ordovician||||||||
7578|Goonumbla Volcanics|48958|6|Mentioned|p3|||||||||
7578|Goonumbla Volcanics|50299|5|Briefly described|Map Legend|Ordovician|Ordovician|Contains the Gunningbland Shale Member.||||||09-JUN-04
7578|Goonumbla Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
7578|Goonumbla Volcanics|60009|5|Briefly described|Map Legend|Late Ordovician|Middle Ordovician|Of the Northparkes Volcanic Group. Interbedded with Billabong Creek Limestone, Gunningbland Formation.||||||13-JUL-04
7578|Goonumbla Volcanics|60443|5|Briefly described|p782|Caradoc|Caradoc|Age: 450.9+/-4.2 Ma (zircon U-Pb, Butera et al., 2001).||||||
7578|Goonumbla Volcanics|61724|3|Fully described|p864 Fig.1, p866|Late Ordovician|Middle Ordovician|Poorly exposed succession of thin basaltic andesites, prominent volcanic conglomerate and minor sandstone and siltstone. Overlies Yarrimbah Formation unconformably; overlain by Wombin Volcanics. Max. age: 466 Ma. See also p870-872.||||||
7578|Goonumbla Volcanics|61821|5|Briefly described|p101|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
7578|Goonumbla Volcanics|61893|6|Mentioned|p251||||||Gunningbland Shale Member.|||
7578|Goonumbla Volcanics|62478|4|Described|p89|Early Silurian|Ordovician|Overlies Neelungaloo Volcanics. Of the Goonumbla Volcanic Complex. Intermediate volcaniclastic rocks, epiclastic sequences, lavas and limestones. Overlain by Wombin Volcanics.||||||
7578|Goonumbla Volcanics|62799|6|Mentioned|p413||Ordovician|Included Gunningbland Shale Member (Percival 1991).||||||
7578|Goonumbla Volcanics|63278|4|Described|p145 Fig. 1, p150|Late Ordovician|Late Ordovician|Overlain by Wombin Volcanics, underlain by Gunningbland Formation. Age: 450.8+/-4.2Ma from monzodiorite (SHRIMP). Comprises volcaniclastic sandstones, conglomerates + ignimbrites. Geol Prov: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
7578|Goonumbla Volcanics|63279|5|Briefly described|p168 Fig. 1, p170 Fig. 3|Ordovician|Ordovician|Upper volcanic-rich component, lower sediment (+/- volcanic)-rich component. Geological Province: Junee-Narromine Volcanic Belt.||||||
7578|Goonumbla Volcanics|63283|4|Described|p185 Tb. 1, p194 Fig. 2, p196 Fig. 4|Darriwilian|Darriwilian|Of Northparkes Gp. Overlain by Wombin Vol, underlain by Billabong Creek Limestone.Age: 445Ma. Geol Prov: Junee-Narromine Volcanic Belt. Eruption age indicated at ca 463Ma. Volcanic-volcaniclastic succession. See p185-189.||||||07-FEB-11
7578|Goonumbla Volcanics|63284|6|Mentioned|p247|Late Ordovician|Late Ordovician|In the Narromine Igneous Complex.||||||
7578|Goonumbla Volcanics|63286|5|Briefly described|p308 Fig. 9|Early Silurian|Middle Ordovician|Includes; Billabong Creek Limestone, Gunningbland Formation. Geological Province: Junee - Narromine Volcanic Belt.  Consists of shoshonitic lavas.||||||07-FEB-11
7578|Goonumbla Volcanics|63287|6|Mentioned|p343|||Geological Province: Junee - Narromine Volcanic Belt. Late Ordovician monzodiorite intrudes.||||||07-FEB-11
7578|Goonumbla Volcanics|63288|6|Mentioned|p358|||Has shoshonitic composition.||||||
7578|Goonumbla Volcanics|63290|6|Mentioned|p393 Tb. 1, p397 Fig. 3(b)|Bolindian|Darriwilian|Geological Province: Junee - Narromine Volcanic Belt.||||||
7578|Goonumbla Volcanics|63291|4|Described|p421, p423|Late Ordovician|Middle Ordovician|Of Northparkes Gp. Includes; Billabong Ck Lst Mbr, Gunningbland Fm. Underlain by Nelungaloo Vol, low-angle unconformity. Thick: 2.5-4Km. Geol Prov: Junee - Narromine Volcanic Belt. Consists mainly of basaltic andesite to trachyandesite + volcaniclastics.||||||
7578|Goonumbla Volcanics|63293|4|Described|p467, p468 Fig. 2, p473|Late Ordovician|Middle Ordovician|Includes: Billabong Creek Limestone, Gunningbland Formation. Geological Province: Junee - Narromine Volcanic Belt.||||||07-FEB-11
7578|Goonumbla Volcanics|64015|5|Briefly described|p57, p58 Fig. 1|Late Ordovician|Late Ordovician|Overlain by ?Billabong Creek Limestone. Contains assemblages of coral and conodont fauna.||||||28-AUG-08
7578|Goonumbla Volcanics|64826|5|Briefly described|p1040 Tb. 1|Eastonian|Gisbornian|Appears as the corrupted GoonMemberla Volcanics in Table 1. Goonumbla Volcanics are part of Northparkes Group.||||||04-MAR-09
7578|Goonumbla Volcanics|67106|6|Mentioned|p673, 675|||Junee-Narromine Volcanic Belt.||||||
7578|Goonumbla Volcanics|67107|6|Mentioned|p688, 693-694, 696, 699, 701|Late Ordovician|Middle Ordovician|Goonumbla district, 20km NW of Parkes. Junee-Narromine Volcanic Belt. Eastonian to Llandovery. Intruded by a monzonite dated 450.8 +/- 4.2 Ma. Hosts the mineralised Goonumbla skarns (Peak Hill deposits).|||Mingelo Volcanics.|Is overlain by Gunningbland and Cotton Formations. Is intruded by the Goonumbla Volcanic Complex. Faulted against Nelungaloo Volcanics.||
7578|Goonumbla Volcanics|67322|4|Described|Fig.5; p22|Katian|Darriwilian|Macquarie Arc. (Sherwin 1973; Krynen et al. 1990). The concept of the Goonumbla Volcanics has been modified several times, by Percival (in Lyons et al. 2000), Simpson et al. (2005) and Percival and Glen (2007). Now included in the Northparkes Group. The age of the Goonumbla Volcanics is assumed to range from the Darriwilian to early Bolindian, based on coral and conodonts. Occurs in the Junee-Narromine region.||Of the Northparkes Group.||Correlative of the Raggatt Volcanics. Overlies the Gunningbland Formation. Overlain by the Wombin Volcanics. Unconformably overlies the Yarrimbah Formation.|Volcanic rocks and andesitic lavas.|22-FEB-18
7578|Goonumbla Volcanics|67805|5|Briefly described|p73|Ordovician|Ordovician|Host to Northparkes porphyry copper-gold deposits. Early Members are chemically and petrographically similar to Mingelo Volcanics.||||||
7578|Goonumbla Volcanics|67821|6|Mentioned|p170, p173|Early Silurian|Late Ordovician|Thought to include the volcanics at the Peak Hill Cu-Au mine. Equated with the Mingelo Volcanics.||||||08-FEB-18
7578|Goonumbla Volcanics|70278|5|Briefly described|p1609, 1611-1612, 1627, 1633|Late Ordovician|Middle Ordovician|Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW. 2.5-4 km thick. This c.451 Ma age (Butera et al., 2001) is from a monzodiorite intrusion.|450.8 +/- 4.2 Ma (minimum).|Goonumbla Volcanic Complex.||Unconformably overlies Nelungaloo Volcanics.|Mainly coherent, basaltic andesitic to trachyandesitic volcanic rocks (lavas and shallow sills with peperitic margins), less abundant volcaniclastic rocks of similar composition, and minor intercalated limestones.|
7578|Goonumbla Volcanics|70684|5|Briefly described|p3, p12-13, p55-56, p59, p61-65, p74-75|Late Ordovician|Middle Ordovician|See also p66 Fig.32. Junee-Narromine Volcanic Belt. Intruded by several monzonite and quartz monzonite bodies.||Northparkes Group.||Overlies Billabong Creek Formation. The upper part overlies Gunningbland Formation. Is overlain by Wombin Volcanics.|Basal, medium- to coarse-grained volcanic sandstone with local masses of allochthonous limestone; coarsens upwards into pebbly volcanic sandstone and thick conglomerate beds; basaltic andesite.|
7578|Goonumbla Volcanics|70754|5|Briefly described|p450 Fig.2, p475|Late Ordovician|Late Ordovician|Systematic palaeontological descriptions.||||Overlies Gunningbland Formation.||
7578|Goonumbla Volcanics|72495|5|Briefly described|p222, 225, 228, 230-231, 240|||See also Goonumbla volcanics, lower and Goonumbla volcanics, upper. This unit has densities of 2.7 -2.86 t/m^3 and magnetic susceptibilites between 0.001-0.05 SI. Geophysical response and inferred subsurface extent are provided.||Of Northparkes Group.||Faulted against the Cotton Formation.||05-APR-20
7578|Goonumbla Volcanics|73154|6|Mentioned|p75, p77 Fig.3|Late Ordovician|Darriwilian|Macquarie Arc, Phase 2. Junee-Narromine belt. High-K volcanics. Goonumbla monzodiorites (439 Ma; Butera et al., 2001) mentioned on p92.||||||
7578|Goonumbla Volcanics|73287|4|Described|p660-662, p664-666, p672, p675, p678|Late Ordovician|Middle Ordovician|Macquarie Arc. Intruded by monzodiorite. Host to ca 455-439 Ma monzonitic porphyries. Host to the Two-Thirty Cu-Au (Mo) prospect. Shallow to transitional submarine environment proximal to an emergent volcano indicated by turbidite-like sequences, imbricated clasts, peperitic breccias on some upper latite lava contacts. Intruded by the Two-Thirty intrusive complex and Two-Thirty breccia complex, LA-ICPMS U-Pb zircon dating of emplacement between 450.5 +/- 5.5 Ma and 438.8 +/- 4.4 Ma. Location in text includes p669 Fig.7.|460-444 Ma, 450.2 +/- 2.8 Ma|Goonumbla Volcanic Complex||Unconformably overlies the Nelungaloo Volcanics, conformably underlies the Wombin Volcanics. Intruded by the Two-Thirty intrusive complex, Two-Thirty breccia complex.|Comprises a basal unit of minor basaltic andesite lava, overlain by massive to autobrecciated trachyandesitic lavas and associated volcaniclastic conglomerates. 2.5-4km thick. Includes volcaniclastic breccia, sandstones, siltstones, limestone lenses.|
7578|Goonumbla Volcanics|73492|6|Mentioned|p691, p693, p695, p707|Ordovician||Temporal correlative with Mingelo Volcanics. See also upper Goonumbla Volcanics p4.||||||
7583|Goorangoola Formation|29941|6|Mentioned|p14|||||||||
7583|Goorangoola Formation|30005|6|Mentioned|p81|||||||||
7583|Goorangoola Formation|31124|5|Briefly described|p17|||See also Fig. 1, 2, Table 1. Petrology||||||
7583|Goorangoola Formation|31125|6|Mentioned|p16|||||||||
7583|Goorangoola Formation|34466|3|Fully described|p353|||||||||
7608|Gordonbrook Serpentinite|22580|6|Mentioned|p99|||||||||
7608|Gordonbrook Serpentinite|23186|6|Mentioned|p470|||||||||
7608|Gordonbrook Serpentinite|23811|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Serpentinised peridotites Mainly dunite and harzburgite) and pyroxenites.||||||20-DEC-04
7608|Gordonbrook Serpentinite|23812|5|Briefly described|p8, p13 Tb.1, p48|||Unconformably overlain by Drake Volcanics.  Intruded by Dumbudgery Creek Granodiorite.  Early Permian?||||||
7608|Gordonbrook Serpentinite|34220|6|Mentioned|p297|||||||||
7608|Gordonbrook Serpentinite|42997|6|Mentioned|p42|||||||||
7608|Gordonbrook Serpentinite|71628|5|Briefly described|p9: 10-11, 19, 23, 27, 35|||Contact with and metamorphism by Dumbudgery Creek Complex detailed.||||Is intruded and faulted against Dumbudgery Creek Complex.||
7610|Gore Series|48940|6|Mentioned|Fig.14|||Refers Wade (1941)||||||
7628|Gosford Subgroup|22969|5|Briefly described|Fig 2.2||Triassic|Narrabeen Group.||||||05-AUG-08
7628|Gosford Subgroup|36121|6|Mentioned|p25|||||||||
7628|Gosford Subgroup|36616|6|Mentioned|p4|||||||||
7628|Gosford Subgroup|40602|6|Mentioned|p9|||||||||
7628|Gosford Subgroup|40653|6|Mentioned|Fig.20|||||||||
7628|Gosford Subgroup|42287|5|Briefly described|p15|||||||||
7628|Gosford Subgroup|42737|5|Briefly described|map legend|Triassic||||||||
7628|Gosford Subgroup|42896|3|Fully described|p29, Table 2|||Of Narrabeen Group.||||||05-AUG-08
7628|Gosford Subgroup|42916|5|Briefly described|Table 1||Early Triassic|||||||
7628|Gosford Subgroup|42925|5|Briefly described|Table 18||Middle Triassic|||||||
7628|Gosford Subgroup|42926|4|Described|map legend||Middle Triassic|||||||
7628|Gosford Subgroup|60281|5|Briefly described|Fig. 7 Appendix 1|Middle Triassic|Early Triassic|Of the Narrabeen Group. Geological Province: Sydney Basin.||||||05-AUG-08
7628|Gosford Subgroup|61315|5|Briefly described|Table SY2|Middle Triassic|Middle Triassic|Of the Narrabeen Group. Geological Province: Sydney Basin||||||
7628|Gosford Subgroup|63172|6|Mentioned|p321|||||||||07-FEB-11
7628|Gosford Subgroup|69297|6|Mentioned|p501|Anisian|Olenekian|Sydney Basin. ||Narrabeen Group||Overlies the Clifton Subgroup. Overlain by the Hawkesbury Sandstone.||
7628|Gosford Subgroup|70647|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Sydney Basin.||Narrabeen Group|Includes Terrigal Formation.|||
7631|Gosforth Shale|32943|6|Mentioned|p94|||Eurydesma recorded.||||||
7631|Gosforth Shale|32945|6|Mentioned|p74|||Permian. Lochinvar Formation.||||||
7631|Gosforth Shale|45090|6|Mentioned|p145|||Eurydesma - Permian base||||||
7643|Gowrie Sandstone Member|34080|6|Mentioned|p248|||||||||
7643|Gowrie Sandstone Member|37987|6|Mentioned|p224|||||||||
7643|Gowrie Sandstone Member|39331|6|Mentioned|Table 10-1|||||||||
7643|Gowrie Sandstone Member|43399|2|Defined|p196,200,205||Tournaisian|||||||
7643|Gowrie Sandstone Member|43406|14|Not recorded|p41,42|||Unit of Goonoo Goonoo Mudstone (Parry Group)||||||
7643|Gowrie Sandstone Member|43418|14|Not recorded|Map Legend|||||||||
7661|Grafton Formation|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p494|Early Cretaceous|Tithonian|S Clarence-Moreton Basin.|||||Lithic quartz sandstones containing beds of montmorillonitic mudstone; contains plant fragments, reed impressions and traces of coal.|
7661|Grafton Formation|22857|4|Described|p318-9, p548 App. 1 Tb.A1.12|Early Cretaceous|Late Jurassic|Sandstone, clayey siltstone; minor claystone, coal. Max. thickness: 276m. Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|22865|6|Mentioned|p318,Fig22.9p317|Cretaceous|Late Jurassic|||||||
7661|Grafton Formation|22892|5|Briefly described|p7 fig6|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|23811|5|Briefly described|Map Legend|Tithonian|Oxfordian|Interbedded sandstone (lithic to quartz arenites ans wackes), clayey siltstone, claystone and local coal; bedding thin to thick; commonly with ferruginous lateritic weathering profile.  Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
7661|Grafton Formation|23812|5|Briefly described|p34 Tb.4, p31|Late Jurassic|Late Jurassic|Maximum thickness: 250m.  Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|23843|5|Briefly described|p456 Table 1|Cretaceous|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 440m.||||||
7661|Grafton Formation|23888|6|Mentioned|p262|||||||||
7661|Grafton Formation|24237|5|Briefly described|p6 Fig.2|Cretaceous|Jurassic|Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|29591|5|Briefly described|p85|||||||||
7661|Grafton Formation|29988|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7661|Grafton Formation|29995|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7661|Grafton Formation|30785|6|Mentioned|p397|||||||||
7661|Grafton Formation|30911|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|32491|5|Briefly described|p18|||U.Jurassic||||||
7661|Grafton Formation|32492|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7661|Grafton Formation|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|32916|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7661|Grafton Formation|33476|6|Mentioned|Fig.10|||||||||
7661|Grafton Formation|33709|6|Mentioned|p104|||||||||
7661|Grafton Formation|34340|3|Fully described|p472|||||||||
7661|Grafton Formation|34400|5|Briefly described|p14|||||||||
7661|Grafton Formation|35065|6|Mentioned|p45|||||||||
7661|Grafton Formation|36354|6|Mentioned|Fig.1|||||||||
7661|Grafton Formation|37122|5|Briefly described|Table 1|||||||||
7661|Grafton Formation|37252|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
7661|Grafton Formation|38064|5|Briefly described|p41|||||||||
7661|Grafton Formation|41631|4|Described|p20|||See also Fig.2||||||
7661|Grafton Formation|42463|6|Mentioned|Fig.3 P170|||||||||
7661|Grafton Formation|42869|5|Briefly described|Table 1, P33|||||||||
7661|Grafton Formation|43001|5|Briefly described|p131|||||||||
7661|Grafton Formation|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Clarence-Moreton Basin.||||||12-APR-05
7661|Grafton Formation|43344|14|Not recorded|p102|Cretaceous|Jurassic|||||||
7661|Grafton Formation|43383|14|Not recorded|p28|Cretaceous|Jurassic|||||||
7661|Grafton Formation|43384|14|Not recorded|Map Legend|Cretaceous|Jurassic|||||||
7661|Grafton Formation|43468|14|Not recorded|Map Legend||Cretaceous|Provisional Edition||||||
7661|Grafton Formation|43479|14|Not recorded|p251,262||Tithonian|||||||
7661|Grafton Formation|43736|5|Briefly described|Table 1,p4|||||||||
7661|Grafton Formation|43881|14|Not recorded|p5-7,11-14,44-8,64,|Cretaceous|Late Jurassic|Replaces Grafton Beds. p73,76,79-80,115,153,156.||||||
7661|Grafton Formation|44028|14|Not recorded|Fig.2|Cretaceous|Jurassic|See Strat Table.||||||
7661|Grafton Formation|48917|3|Fully described|p30|||See also P47. Water.||||||
7661|Grafton Formation|60079|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Interbedded sandstone, clayey siltstone, claystone and minor coal.||||||
7661|Grafton Formation|60281|5|Briefly described|p27, Fig.20 App.1|Cretaceous|Late Jurassic|Overlies the Kangaroo Creek Sandstone.  Sandstone, clayey siltstone, minor claystone, coal.  Max. thickness: 250m.  Geological Province: Clarence-Moreton Basin.||||||17-MAR-05
7661|Grafton Formation|60993|3|Fully described|p4, p36|Tithonian|Callovian|Initially termed the "Grafton Beds" and the "Grafton Stage". Sandstone, siltstone and claystone; coal. Conformably/gradationally overlies Kangaroo Creek Sst. Thickness in grafton 2 bore: 267m. Geol. Prov: Clarence-Moreton Basin. ||||||
7661|Grafton Formation|60995|4|Described|p69, p51 Fig. 3|Late Jurassic|Late Jurassic|Thin and thick-bedded, silty quartz sandstone,lithic sandstone,clayey siltstone, minor claystone, and coal. Overlies Kangaroo Creek Sandstone. Max. thickness: 250m. Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|60997|5|Briefly described|p139|Berriasian|Tithonian|Composed of lithic-labile sandstone. Conformably overlies Kangaroo Creek Sandstone. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1.||||||29-JAN-08
7661|Grafton Formation|60999|5|Briefly described|p164|||Overlies Walloon C. M. in places.||||||
7661|Grafton Formation|61000|5|Briefly described|p181, p183|Late Jurassic|Middle Jurassic|Siltstone and mudstone are common. Geological Province: Clarence-Moreton Basin. See also p186.||||||
7661|Grafton Formation|61002|5|Briefly described|p213|Late Jurassic|Late Jurassic|Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|||||||
7661|Grafton Formation|61005|6|Mentioned|p248, p252|||An eroded unit. ||||||
7661|Grafton Formation|61006|5|Briefly described|p278 Fig. 2||Jurassic|Mudstone, labile sandstone. Geological Province: Clarence-Moreton Basin.||||||
7661|Grafton Formation|61310|5|Briefly described|p14 Fig. C5|Early Cretaceous|Early Cretaceous|Comprises clayey siltstone and soft sadstone with minor claystone and coal. Overlies Kangaroo Creek Sandstone. Max. thickness: 276m. Geological Province: Clarence -Moreton Basin. See also p24.||||||
7661|Grafton Formation|61377|6|Mentioned|p159|||||||||07-FEB-11
7661|Grafton Formation|64289|5|Briefly described|p6 Fig. 2|Late Jurassic|Late Jurassic|Geological province: Clarence-Moreton Basin.||||||07-FEB-11
7661|Grafton Formation|67402|5|Briefly described|p187, p193|Berriasian|Oxfordian|Clarence-Moreton Basin. ||||Overlies the Kangaroo Creek Formation.||
7661|Grafton Formation|68135|5|Briefly described|p52 fig 2b |Early Cretaceous|Late Jurassic|Clarence-Moreton Basin.||||Overlies Kangaroo Creek Sandstone|Interbedded siltstone and sandstone.|14-SEP-17
7661|Grafton Formation|69297|5|Briefly described|p487 fig 5.38|Cretaceous|Upper Jurassic|Clarence-Moreton Basin. Between 150-250m thick. Deposited in a low-energy, mixed load meandering fluvial environment. ||||Overlies the Kangaroo Creek Sandstone.|Sandstone, clayey siltstone, minor claystone and coal.|
7661|Grafton Formation|69594|5|Briefly described|p544-545|||Clarence-Moreton Basin (NSW only). In QLD it is known as the (upper part of) Woodenbong beds. 250+ m thick. Fluvial to lacustrine sediments, derived from Texas Subprovince.||||Overlies Kangaroo Creek Sandstone.|Sublabile to labile, tough, sandstone, siltstone and shale; conglomerates up to 2.5m thick. Sandstones cross-bedded in places; plant fossils common. Abundant andesitic fragments suggest contemporaneous volcanism.|
7661|Grafton Formation|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurrasic|Shown as located within the Clarence-Moreton Basin.||||Overlies Kangaroo Creek Sandstone|May includes siltstone.|
7661|Grafton Formation|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.||||Overlies Kangaroo Creek Sandstone.||
7661|Grafton Formation|73570|6|Mentioned|p913-915, p917 Fig.5, p921, p923|Early Cretaceous|Late Jurassic|Clarence-Morton Basin.|134 Ma|||||
7665|Gragin Conglomerate|23050|4|Described|p23 Table.4|Middle Triassic|Early Triassic|In the Warialda Trough. Age: Megaflora and palynology data indicate a middle Triassic age.||||||04-JUN-07
7665|Gragin Conglomerate|23051|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|In the Warialda Trough.||||||04-JUN-07
7665|Gragin Conglomerate|29869|4|Described|p34|||||||||
7665|Gragin Conglomerate|32413|6|Mentioned|p103|||||||||
7665|Gragin Conglomerate|34134|6|Mentioned|Cor.Chart|||Lower Jurassic||||||
7665|Gragin Conglomerate|34254|6|Mentioned|p489|||L.- M. Jurassic||||||
7665|Gragin Conglomerate|36570|2|Defined|p22|Middle Triassic|Middle Triassic|See also p63, Fig.9.||||||04-JUN-07
7665|Gragin Conglomerate|37757|6|Mentioned|p29|||||||||
7665|Gragin Conglomerate|42492|5|Briefly described|Table 2 P14|||||||||
7665|Gragin Conglomerate|44093|5|Briefly described|p238 App. 1|Triassic|Triassic|Geological Province: New England Fold Belt.||||||
7665|Gragin Conglomerate|62534|5|Briefly described|p10 (legend)|Early Triassic|Early Triassic|Overlies Dunboy-Gragin Granite. Leucocratic granitoid.||||||07-FEB-11
7665|Gragin Conglomerate|63347|5|Briefly described|p5 Fig. 2|Middle Triassic|Middle Triassic|Geological Province: Warialda Trough.||||||
7665|Gragin Conglomerate|68003|5|Briefly described|p38 Fig.3-j, p43, p54, p128.|Late Triassic|Middle Triassic|Warialda Trough, Brigalow Belt South Bioregion. Deposited in a high energy valley-fill and braided stream environment. Called Gragin Formation in Fig.3-j.||||Overlies Gunnee Formation. Is paraconformably overlain by Hutton Sandstone.|Orthoconglomerate, sporadic paraconglomerate, minor lithic arenite and rare mudstone at the top of the unit.|
7665|Gragin Conglomerate|68005|6|Mentioned|p170.|Triassic|Triassic|Warialda Trough.||||Overlies Gunnee Formation.||
7665|Gragin Conglomerate|70036|5|Briefly described|Map legend|Middle Triassic|Middle Triassic|Warialda Trough. Included in a mapped unit of coal measures: conglomerate, arkosic sandstone, siltstone, carbonaceous mudstone and coal.||||||
7665|Gragin Conglomerate|71628|6|Mentioned|p19:27|||||||Unconformably overlies Dumboy-Gragin Leucosyenogranite.||
7672|Grampians Group|22531|4|Described|p19|Silurian|Ordovician|||||||
7672|Grampians Group|22532|5|Briefly described|map legend|Silurian|Ordovician|||||||
7672|Grampians Group|22628|5|Briefly described|p115, fig3p111|||||||||
7672|Grampians Group|22708|6|Mentioned|p212|||||||||
7672|Grampians Group|22768|5|Briefly described|p141,146,184|Early Devonian|Late Silurian|||||||
7672|Grampians Group|22773|5|Briefly described|Fig24.5p350|Early Devonian|Silurian|||||||
7672|Grampians Group|22857|5|Briefly described|p141, p166, p183|Early Devonian|Late Silurian|Equivalents mentioned on p350 Fig. 24.5. Geological Province: Kanmantoo Fold Belt, Grampians Basin. ||||||
7672|Grampians Group|22887|5|Briefly described|Fig.5 p12|Middle Devonian|Silurian|||||||
7672|Grampians Group|22893|6|Mentioned|fig4 p9|||Describing an equivalent to this unit.||||||
7672|Grampians Group|23061|6|Mentioned|293 fig 1|||Underlying unit Saint Arnaud Beds||||||
7672|Grampians Group|23110|5|Briefly described|p502|||||||||
7672|Grampians Group|23229|4|Described|p24-5|||||||||
7672|Grampians Group|23231|6|Mentioned|Fig5-4p51|||||||||
7672|Grampians Group|23232|5|Briefly described|p62|||||||||
7672|Grampians Group|23234|5|Briefly described|p85|Mesozoic|Late Devonian|||||||
7672|Grampians Group|23235|5|Briefly described|p68|Devonian|Silurian|||||||
7672|Grampians Group|23236|6|Mentioned|Fig10-1.2p99|||||||||
7672|Grampians Group|23247|4|Described|Fig12-1.1p182, 183-4|Early Devonian|Late Silurian|||||||
7672|Grampians Group|23306|6|Mentioned|Map legend|||||||||
7672|Grampians Group|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
7672|Grampians Group|23309|4|Described|p76-83, 203-208, 349|||||||||
7672|Grampians Group|23402|3|Fully described|p25, p7 Tb. 1|Silurian|Silurian|Previously mapped on WILLAURA as 'Willaura Sandstones' (Spencer-Jones, 1965), later modified to 'Willaura Sandstone' (Buckland, 1987).   Age: 412.6+/-3.5Ma (U-Pb zircon).   Unconformably overlies Wickliffe Rhyolite and Glenthompson Sandstone.||||||
7672|Grampians Group|23417|6|Mentioned|p6 Fig.4||Silurian|||||||
7672|Grampians Group|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|||||||
7672|Grampians Group|23857|5|Briefly described|p907|Silurian|Silurian|||||||
7672|Grampians Group|23918|6|Mentioned|p1327|||Geological Province: Lachlan Fold Belt.||||||
7672|Grampians Group|23991|5|Briefly described|p188 Fig.1|Silurian|Silurian|||||||
7672|Grampians Group|24002|5|Briefly described|p227 fig. 1|Ordovician|Ordovician|Age: 425Ma.||||||21-OCT-08
7672|Grampians Group|24100|6|Mentioned|p98 Fig. 4|||Geological Province: Stawell Zone.||||||19-APR-05
7672|Grampians Group|24311|5|Briefly described|p1061, p1059 Fig. 2|Silurian|Silurian|||||||
7672|Grampians Group|24323|5|Briefly described|p138|Silurian|Silurian|||||||
7672|Grampians Group|24383|6|Mentioned|p56 Tb.6|||||||||
7672|Grampians Group|24581|5|Briefly described|p811|Ludlovian|Late Ordovician|Geological Province: Kanmantoo Fold Belt.||||||
7672|Grampians Group|24588|5|Briefly described|p31 Fig.15|Emsian|Emsian|Geological Province: Lachlan Fold Belt.||||||
7672|Grampians Group|29889|6|Mentioned|p141|||||||||
7672|Grampians Group|30329|6|Mentioned|p30|||On table P30||||||
7672|Grampians Group|30522|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Lower Carboniferous to Upper Devonian||||||
7672|Grampians Group|30579|6|Mentioned|Map legend|Silurian|Silurian|||||||
7672|Grampians Group|30928|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
7672|Grampians Group|30934|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
7672|Grampians Group|31161|5|Briefly described|PA11|||||||||
7672|Grampians Group|32001|6|Mentioned|p77|||||||||
7672|Grampians Group|32865|6|Mentioned|p486|||||||||
7672|Grampians Group|33232|3|Fully described|p71|||||||||
7672|Grampians Group|33236|6|Mentioned|p24|||U.Dev. _ L.Carb.||||||
7672|Grampians Group|33238|5|Briefly described|p640|||||||||
7672|Grampians Group|33394|6|Mentioned|p78|||||||||
7672|Grampians Group|33602|6|Mentioned|Table 1|||||||||
7672|Grampians Group|33608|6|Mentioned|p45|||||||||
7672|Grampians Group|33940|6|Mentioned|p416|||||||||
7672|Grampians Group|34990|6|Mentioned|p435|||||||||
7672|Grampians Group|35013|6|Mentioned|p390|||||||||
7672|Grampians Group|35099|6|Mentioned|p325|||||||||
7672|Grampians Group|35112|6|Mentioned|Table.1|||||||||
7672|Grampians Group|35278|6|Mentioned|p349|||||||||
7672|Grampians Group|35281|6|Mentioned|p19|||||||||
7672|Grampians Group|36534|6|Mentioned|p221|||||||||
7672|Grampians Group|36732|6|Mentioned|p300|||||||||
7672|Grampians Group|37501|5|Briefly described|p407|||||||||
7672|Grampians Group|38070|5|Briefly described|p97|||||||||
7672|Grampians Group|38367|6|Mentioned|p158|||See also Fig.1||||||
7672|Grampians Group|38436|6|Mentioned|p420|||||||||
7672|Grampians Group|39291|6|Mentioned|p214|||||||||
7672|Grampians Group|39331|6|Mentioned|Fig.0-3|||See Fig.0-3||||||
7672|Grampians Group|39446|6|Mentioned|p11|||See also P65||||||
7672|Grampians Group|39967|4|Described|p33|||||||||
7672|Grampians Group|40172|6|Mentioned|Map legend|Silurian|Silurian|||||||
7672|Grampians Group|40761|6|Mentioned|p215|||See also p225.||||||07-SEP-18
7672|Grampians Group|40887|6|Mentioned|p25|||||||||
7672|Grampians Group|40947|6|Mentioned|p4|||||||||
7672|Grampians Group|41002|5|Briefly described|p183|||||||||
7672|Grampians Group|41563|6|Mentioned|p516|||||||||
7672|Grampians Group|41571|4|Described|p38|||||||||
7672|Grampians Group|41572|6|Mentioned|p3|||||||||
7672|Grampians Group|41585|4|Described|p141|||||||||
7672|Grampians Group|41637|6|Mentioned|p210|||||||||
7672|Grampians Group|41641|6|Mentioned|p191|||||||||
7672|Grampians Group|42119|5|Briefly described|p524|||||||||
7672|Grampians Group|42745|5|Briefly described|p3, p6|||Also P9.||||||
7672|Grampians Group|42827|6|Mentioned|p141|||see also Table 4.3||||||
7672|Grampians Group|42966|5|Briefly described|Fig. 25 p47|||||||||
7672|Grampians Group|42971|5|Briefly described|p142|||||||||
7672|Grampians Group|43027|5|Briefly described|p601|||||||||
7672|Grampians Group|43193|5|Briefly described|p71,78.|||Minimum age: Late Silurian-earliest Devonian.||||||
7672|Grampians Group|43218|4|Described|Fig.3 p22, p25|Early Devonian|Late Silurian|||||||
7672|Grampians Group|43461|14|Not recorded|table p625|Early Carboniferous|Late Devonian|||||||
7672|Grampians Group|43547|14|Not recorded|Table p153,154|Famennian|Frasnian|||||||
7672|Grampians Group|43627|5|Briefly described|p2, p6|||Age: 410 Ma.||||||21-OCT-08
7672|Grampians Group|43753|5|Briefly described|p621-624|Early Carboniferous|Late Silurian|||||||
7672|Grampians Group|43846|4|Described|9, 11|Early Devonian|Late Silurian|Intrusives into group aged around 400Ma.||||||21-OCT-08
7672|Grampians Group|44093|5|Briefly described|p47, p91|Early Devonian|Late Silurian|See also p102 Fig 10.3. Geological Province: Kanmantoo Fold Belt.||||||08-MAR-05
7672|Grampians Group|44186|5|Briefly described|Map Legend||Silurian|||||||
7672|Grampians Group|44929|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|44930|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficult and Red Man Bluff Sub-Groups.||||||13-JUN-06
7672|Grampians Group|44931|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone, minor conglomerate and mudstone. Undifferentiated for this interpretation.||||||14-JUN-06
7672|Grampians Group|44932|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|44933|5|Briefly described|Map Legend|Silurian|Ordovician|Includes Mount Difficulty and Red Man Bluff Sub-Groups.||||||14-JUN-06
7672|Grampians Group|48911|6|Mentioned|p7|||Lithology||||||
7672|Grampians Group|49038|6|Mentioned|p22|||||||||
7672|Grampians Group|49040|6|Mentioned|p6|||||||||
7672|Grampians Group|50154|2|Defined|p17, p18 Fig3.1, p110-113|Ludlow|Early Silurian|Max. thickness: 3700m. Overlies the Gringegalgona Granite and unconformably overlies the Nargoon Group. Unconformably overlain by the Rocklands Volcanic Group. Geological Province: Lachlan Fold Belt.||||||15-SEP-04
7672|Grampians Group|50155|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone||||||
7672|Grampians Group|50156|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||
7672|Grampians Group|50157|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||
7672|Grampians Group|50158|5|Briefly described|Map Legend|Silurian||Unconformably overlies Nargoon Group. Overlain by Barangaroo Ignimbrite. Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded||||||25-JUN-04
7672|Grampians Group|50159|5|Briefly described|Map Legend|Silurian||Overlies Nargoon Group. Overlain by Barangaroo Ignimbrite, Parilla Sand and Shepparton Formation. Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded.||||||21-OCT-08
7672|Grampians Group|50160|5|Briefly described|Map Legend|Silurian||||||||16-JUN-04
7672|Grampians Group|50161|5|Briefly described|Map Legend|Silurian||Sandstone: quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded.||||||21-OCT-08
7672|Grampians Group|50162|5|Briefly described|Map Legend|Silurian||Quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded sandstone.||||||21-OCT-08
7672|Grampians Group|50163|5|Briefly described|Map Legend|Silurian||Quartz-rich to micaceous or feldspathic, well sorted, medium grained, cross-bedded, thickly bedded sandstone||||||
7672|Grampians Group|50371|5|Briefly described|Map Legend|Silurian|Silurian|Includes the Willaura Sandstone.||||||21-JUN-04
7672|Grampians Group|50546|6|Mentioned|p1232 Fig.1a|||||||||
7672|Grampians Group|60412|6|Mentioned|p237||||499 +/- 2 Ma (40Ar-39Ar biotite).||||Sandstones.|
7672|Grampians Group|60421|5|Briefly described|p408 Fig. 1, 416, 418 Fig. 5|Silurian|Silurian|||||||
7672|Grampians Group|60451|4|Described|p20, 24, 75, 142-143|Silurian|Silurian|Age: ~425-415Ma Maximum Thickness: ~3700m. Includes Red Man Bluff Subgroup, Silverband Formation.||||||
7672|Grampians Group|60454|5|Briefly described|Map Legend|Silurian|Ordovician|Units do not appear on this map.||||||
7672|Grampians Group|60456|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: quartz-rich to micaceous or feldspathic; occasional scattered or lag horizons of vein quartz pebbles; with planar, cross and trough cross lamination, thin to thickly bedded.||||||
7672|Grampians Group|60457|5|Briefly described|Map Legend|Silurian|Ordovician|Units do not appear on this map.||||||24-SEP-04
7672|Grampians Group|60458|5|Briefly described|Map Legend|Silurian|Ordovician|Sandstone: quartz rich to micaceous or feldspathic; occasional scattered or lag horizons of vein quartz pebbles; with planar, trough or trough cross lamination, thin to thickly bedded.||||||
7672|Grampians Group|60459|5|Briefly described|Map Legend|Silurian|Ordovician|Includes: Mount Difficult Sub-Group, Red Man Bluff Sub-Group, Silverband Formation.||||||
7672|Grampians Group|60491|6|Mentioned|p13 Fig.5|||||||||
7672|Grampians Group|60543|5|Briefly described|Map legend|Devonian|Silurian|Terrestrial to marine sandstone with lesser conglomerate and siltstone.||||||23-DEC-09
7672|Grampians Group|61180|5|Briefly described|p5|Early Devonian|Silurian|Overlies Saint Arnaud Beds.||||||
7672|Grampians Group|61181|5|Briefly described|p153 Fig. 47|Devonian|Devonian|Sandstone and shale. ||||||
7672|Grampians Group|61183|3|Fully described|p7, p23-24, p28-33|Early Silurian|Ordovician|Incl: Red Man Bluff Subgp(lower), Silverband Fm(middle) and Difficult Subgp(upper). Fluvial/shallow marine lower quartzo-feldspathic to micaceous sst; intervening micaceous mudst. and upper quartzose sst package. Overlain by Rocklands Volcs. Thick:~3700m.||||||
7672|Grampians Group|61186|6|Mentioned|p76|||Source of the Grampians Sandstone dimension stone in Victoria quarried in the Heatherlie quarry which lies within the Serra Sandstone Formation of the Grampians Group. ||||||
7672|Grampians Group|61187|5|Briefly described|p4, p5 Fig.3, p6, p9, p69. |Silurian||Glenelg Zone, Melbourne Terrane. Marginal marine to terrestrial deposition on the Delamerian Craton. Folded during Benambran Orogeny. Early Devonian A-type volcanics were deposited over this deformed and eroded Group.|||Includes Willaura Sandstone.|||
7672|Grampians Group|61410|5|Briefly described|p7 Fig.2, p8-9|Silurian|Ordovician|Overlies the Glenelg Zone. Crops out as a series of spectacular rugged strike ranges. Hosts only scattered small amounts of gold mineralisation.||||Intruded by the Mafeking Granodiorite|Includes conglomerate hosting minor auriferous quartz veins.|
7672|Grampians Group|61726|5|Briefly described|p924 Fig.3|Silurian|Silurian|||||||
7672|Grampians Group|61749|6|Mentioned|p11, p14|Silurian|Silurian|Includes Red Man Bluff and Mount Difficulty Subgroup seperated by Silverband Formation. Fluvial to shallow marine sequence.||||||21-JAN-10
7672|Grampians Group|61752|4|Described|p10|Silurian|Ordovician|Fluvial to marginal marine sequence. Geological Province: Lachlan Fold Belt.||||||07-FEB-11
7672|Grampians Group|61841|5|Briefly described|p242, p244|Silurian|Silurian|Sediments on the Dundas Tablelands. Overlain by Rocklands Volcanic Group.||||||
7672|Grampians Group|62741|5|Briefly described|p678 Fig. 1, p682|Silurian|Silurian|Predominantly sandstone. A cover sequence overlying a Cambrian basement possibly deposited in Late Ordovician?||||||
7672|Grampians Group|62755|5|Briefly described|p876 Fig. 1|Silurian|Silurian|Sandstone, siltstone. See also p885 Fig. 8. See also misspelt Grampian Group.||||||
7672|Grampians Group|63124|5|Briefly described|p52|Early Devonian|Late Silurian|Thick sequence of quartzose sandstone, red siltstone and shale with minor conglomerate. ||||||
7672|Grampians Group|63446|5|Briefly described|Map legend|Silurian|Silurian||||||Marine, fluvial: sandstone, minor conglomerate, siltstone.|
7672|Grampians Group|63457|5|Briefly described|p123, p125.|||>3.5 km thickness of fluviatile and shallow marine sequences, sourced from Delamerian Highlands to the W (in the Adelaide Fold Belt). Forms two major strike ridges: the Serra and Victoria Ranges.|||||More than 3.5 km thick, including fluviatile and shallow-marine sedimentary sequences.|
7672|Grampians Group|63599|5|Briefly described|p976|Silurian|Silurian|||||||
7672|Grampians Group|64314|5|Briefly described|p495 Fig. 2a, p502|Silurian|Silurian|||||||
7672|Grampians Group|64541|5|Briefly described|Map Legend|Silurian|Silurian|Sandstone: quartz-rich to micaceous or feldspathic, occasional scattered or lag horizions of vein quartz pebbles; laminated, cross-laminated and trough cross-laminated; thin to thickly bedded; shallow marine trace fossils.||||||07-FEB-11
7672|Grampians Group|64597|6|Mentioned|p760 Fig.1. |||||||||
7672|Grampians Group|64610|5|Briefly described|Map legend|Silurian|Ordovician|Includes Red Man Bluff and Mount Difficult Subgroups.  Predominantly sandstones, and conglomerates.||||||12-NOV-08
7672|Grampians Group|64616|6|Mentioned|p343 Fig.23|||||||||
7672|Grampians Group|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Grampians. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
7672|Grampians Group|65313|5|Briefly described|p580, p576|Silurian|Silurian|Quartzites are poorly fossiliferous, riverine and minor intertidal facies. Silurian paleosols studied.||||||26-MAR-12
7672|Grampians Group|65665|6|Mentioned|p1144 Fig.1|Silurian|Silurian|||||||
7672|Grampians Group|66002|5|Briefly described|p5, p5 Tb.3|Silurian|Silurian|Includes Mount Difficult Subgroup, Silverband Formation and Red Man Bluff Subgroup. Defined by Spencer-Jones, 1965. Revised Cayley & Taylor, 1997. Formerly called Grampians sandstone series (Selwyn, 1862) and Grampian sandstone group (Selwyn and Ulrich, 1866)||||||
7672|Grampians Group|66769|5|Briefly described|117, 148|Silurian|Silurian|Grampians-Stavely Zone. Fluvial to shallow marine siliciclastics. Deformed in the Late Silurian-early Devonian. Restricted to Moyston Fault footwall; deposited in a shallow-marine foreland-basin depocentre.||||||
7672|Grampians Group|67104|5|Briefly described|p631 Fig.2, p635, p646, |Early Silurian|Late Ordovician|Confined to the area immediately west of the Moyston Fault. Younger than the Leap Year Group.|ca. 425 Ma|||||
7672|Grampians Group|67127|6|Mentioned|p73|Devonian|Devonian|Forms basement below the WIM 150 heavy mineral deposit.||||Underlies the Renmark Group.||
7672|Grampians Group|67847|6|Mentioned|p10 fig 2.3, p81|Silurian|Silurian|||||||
7672|Grampians Group|68116|5|Briefly described|Appendix, Maps 21, 22, 29, 30, 38.|Early Devonian|Late Ordovician||||||Sandstone, quartz-rich to micaceous or feldspathic; mudstone; minor polymict conglomerate.|05-JUN-14
7672|Grampians Group|68298|5|Briefly described|p220-222|Pragian|Pragian|Includes Early Devonian possible tetrapod trackways. Pragian age based on isotopic evidence. ||||||
7672|Grampians Group|70211|5|Briefly described|p3|Silurian|Late Ordovician|Fluvial to shallow-marine siliciclastic rocks.||||Unconformably overlies Nargoon Group.||
7672|Grampians Group|70493|6|Mentioned|p56||Late Ordovician|Grampians-Stavely Zone, Lachlan Orogen.||||Unconformably overlies Nargoon Group.||
7672|Grampians Group|70877|4|Described|p10, p12-p13, p170-p171|Silurian|Late Ordovician|Grampians-Stavely Zone. Deposited in fluvial to shallow marine environments. Thickest and most structurally complex close to the eastern edge of the Grampians-Stavely Zone.||||Overlies the Nargoon Group and the Rocklands Volcanics. Intruded by the Dwyer Granite, Mirranatwa Granite, Bullawin Porphyry, Mafeking Suite and Duchembegarra Granite.|Sandstone and siltstone.|
7672|Grampians Group|70904|14|Not recorded|p 38|||Stratigraphy.||||||
7672|Grampians Group|70967|6|Mentioned|p3-4, 10-11, 13|Silurian|Late Ordovician|Cayley and Taylor (1997). Fluvial to shallow-marine siliciclastic rocks. Structurally complex.|||||Sandstones and conglomerate.|
7672|Grampians Group|71040|5|Briefly described|p3, p6, p22|||W of the Moyston Fault, but has characteristics of the Lachlan Orogen, including Silurian to Early Devonian sedimentation and deformation. Age given as probably Silurian.||||Is overlain unconformably by Rocklands Volcanics.|Fluvial to shallow-marine deposits.|
7672|Grampians Group|71419|6|Mentioned|p16 Fig 17|Silurian|Silurian|Fluvial and paralic sediments.||||||
7672|Grampians Group|71593|4|Described|p8-p9, p12, p24, p44-p48|Silurian|Ordovician|Silurian. See also p57, p59, p62, p68-p70, p73-p75, p77-p78, p80-p85, p92, p95, p98-p100, p102, p133, p138-p139, p166, p169, p179, p195, p202-p203.|ca. 440 Ma|||Overlain by the Rocklands Volcanic Group. Unconformably overlies the Nargoon Group.|Fluvial to shallow marine red bed sandstone and mudstone.|
7672|Grampians Group|72445|5|Briefly described|p2-3, p9-10, p12, p16, App.1, App.7.|Silurian|Late Ordovician|See also App.2; App.5, App.7 p6 Fig.3. Contains significant structural complexity. Identified in STAVELY02. App.2 is a .csv format file. Also overlies the Nargoon Group.||||Overlies Mount Stavely Volcanic Complex, also in faulted or sheared contact. Intruded by Dwyer Granite, Mirranatwa Granite, Bullawin Porphyry, Mafeking Suite and Duchembegarra Granite.|Dominantly sandstone to conglomeratic sandstone with 0.7-2.3 m lenses of conglomerate. Includes fluvial to shallow marine siliciclastic rocks; sandstone and conglomerate.|15-OCT-20
7672|Grampians Group|73059|6|Mentioned|p1059|Late Ordovician|Late Ordovician|Grampians-Stavely Zone.||||||
7672|Grampians Group|73118|5|Briefly described|p6-8, 14, 19, 42, 48, 53, 64-72, 74|Silurian|Silurian|Glenelg Zone, Western Victoria. A terrestrial to marginal marine sequence. Features basal subhorizontal cataclastic zones; underwent repeated thrusting and extensional faulting.|||Wartook Sandstone.|Is overlain by Rocklands Rhyolite, Shepparton Formation or Loxton-Parilla Sands. Is intruded by Victoria Valley Granite. Is metamorphosed locally by Duchembegarra Granite.|Includes massive to banded quartz sandstones, and intraclast conglomerate.|
7672|Grampians Group|73576|6|Mentioned|p818|Devonian|Devonian|||||||
7672|Grampians Group|74367|6|Mentioned|p16|Early Cambrian|Early Cambrian|||||||
7702|Grants Head Formation|22616|6|Mentioned|Fig.1 p670|Triassic|Triassic|||||||
7702|Grants Head Formation|22736|6|Mentioned|p611 Fig2||Triassic|||||||
7702|Grants Head Formation|22857|5|Briefly described|p538 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Camden Haven Group. Conglomerate, crossbedded quartz to quartz-lithic sandstone, carbonaceous shale, laminated shale. Max. thickness: 75m. Geological Province: Lorne Basin.||||||
7702|Grants Head Formation|32719|4|Described|p208|||Section p209, map p207. see also p212.||||||
7702|Grants Head Formation|35647|5|Briefly described|p50|||||||||
7702|Grants Head Formation|36826|5|Briefly described|p89|||||||||
7702|Grants Head Formation|41348|5|Briefly described|Map legend|Triassic|Triassic|Of the Camden Haven Group.||||||16-DEC-04
7702|Grants Head Formation|44093|5|Briefly described|p67 Fig 6.6|Triassic|Triassic|Geological Province: Lorne Basin.||||||
7702|Grants Head Formation|60281|5|Briefly described|p18, Fig.8 App. 1|Tiras|Triassic|Top unit of the Camden Haven Group. Overlies the Laurieton Conglomerate, but nature of the contact is unknown. Geological Province: Lorne Basin.||||||12-OCT-15
7702|Grants Head Formation|62058|5|Briefly described|map sheet|Early Triassic|Early Triassic|||Unit in Camden Haven Group.|||Sandstone, shale.|
7702|Grants Head Formation|63763|5|Briefly described|p4-5 Fig. 1|Early Triassic|Eary Triassic|Of Camden Haven Group. Sandstone and shale.||||||03-FEB-09
7702|Grants Head Formation|66090|1|Redefined|p2, p4, pp8-9, pp26-28. |Early Triassic|Early Triassic|Redefined in this study. Northeast Lorne Basin. Well-exposed in coastal cliffs and rock platforms. Identified by absence of reddish purple mudstone beds. Capped with ferruginized matrix of mud to pebble conglomerate. Contains Dicroidium palynomorphs.||Uppermost unit in Camden Haven Group.||Overlies conformably the Laurieton Conglomerate.|An upwards-fining sequence of 60% mudstone interbedded with 40% sandstone; minor basal pebble and granule conglomerate interbedded with lithic-quartz sandstone and siltstone; a variety of sedimentary structures. Thickness over 155 m.|
7707|Granya Granite|22508|5|Briefly described|p2||Silurian|Keotong Supersuite, Lachlan Fold Belt||||||
7707|Granya Granite|23309|6|Mentioned|p432 App1|||Supersedes Granya Adamellite G103 S-Type.||||||
7707|Granya Granite|29953|5|Briefly described|p13|||||||||
7707|Granya Granite|32684|6|Mentioned|Fig.2|||||||||
7707|Granya Granite|39860|4|Described|p18|||Contains quartz, K-feldspar, plagioclase, biotite and muscovite; abundant xenoliths.||||||30-NOV-04
7707|Granya Granite|41868|6|Mentioned|p478|||||||||
7707|Granya Granite|42726|5|Briefly described|map legend|Silurian||||||||
7707|Granya Granite|44184|5|Briefly described|Map Legend||Early Silurian|Shown as Granya Unassigned.||||||
7707|Granya Granite|64571|6|Mentioned|p825|Early Silurian|Early Silurian|||||||
7707|Granya Granite|68116|5|Briefly described|Appendix, Map 20.|Wenlock|Llandovery||||||Granite: coarse grained, leucocratic; contains quartz, K-feldspar, plagioclase, biotite, muscovite and accessory apatite, zircon, tourmaline and sillimanite; abundant enclaves; S-type.|
7707|Granya Granite|68310|6|Mentioned|p241-242|||Wagga Batholith. Geochemical plots of schistose enclaves.||||||
7707|Granya Granite|69801|5|Briefly described|p2, p4-p5, p122-p127, p135-137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs on the NSW-Victoria border east of Albury. This unit is the same age as granites near Holbrook but younger than the Granya Granite sampled 10km further south. Sample locality, petrography, zircon characteristics, SHRIMP analyses and interpretation are detailed.|428.2 +/- 2.7 Ma|Koetong Suite||Intruded by the Holbrook Granite.|S-type granite.|
7707|Granya Granite|73457|5|Briefly described|p10-13|Silurian|Silurian|Boundary with the Budginigi Ignimbrite is either a fault or a nonconformity.||||Nonconformably underlies Yambla Formation, faulted against Adaminaby Group|Strongly sheared, contains a well-developed subvertical shear fabric.|
7711|Grasstrees Coal Member|37773|6|Mentioned|p19|||||||||
7711|Grasstrees Coal Member|39346|6|Mentioned|Map legend|Permian|Permian|||||||
7711|Grasstrees Coal Member|40331|6|Mentioned|p15|||||||||
7711|Grasstrees Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Rowan Formation. ||||
7731|Great Cobar Slate|22857|4|Described|p436 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Nurri Group (Cobar Supergroup). Max. thickness: >1km. Geological Province: Cobar Basin. ||||||
7731|Great Cobar Slate|23095|5|Briefly described|p610 (table 1)||Early Devonian|||||||
7731|Great Cobar Slate|23096|6|Mentioned|p601 (Fig 1)|||||||||
7731|Great Cobar Slate|23101|5|Briefly described|p567 (Fig 1)|||||||||
7731|Great Cobar Slate|23171|5|Briefly described|p15,42,Fig15p45|||||||||
7731|Great Cobar Slate|23173|4|Described|Map Legend|||||||||
7731|Great Cobar Slate|23734|5|Briefly described|p12 Fig. 1|||Parent: Nurri Group.||||||
7731|Great Cobar Slate|29621|4|Described|p9|||||||||
7731|Great Cobar Slate|29947|6|Mentioned|p685|||||||||
7731|Great Cobar Slate|29948|5|Briefly described|p27|||Mention Fig.12||||||
7731|Great Cobar Slate|29987|6|Mentioned|p13|||||||||
7731|Great Cobar Slate|31592|6|Mentioned|Fig. 1|||L.-U.Sil. Part of Cobar Gp.||||||
7731|Great Cobar Slate|33123|6|Mentioned|p8|||||||||
7731|Great Cobar Slate|33342|4|Described|p172|||?Early Sil.||||||
7731|Great Cobar Slate|34057|6|Mentioned|Map legend|Silurian|Silurian|||||||
7731|Great Cobar Slate|34449|6|Mentioned|p128|||||||||
7731|Great Cobar Slate|34469|6|Mentioned|p114|||Table p108. Ordovician?||||||23-SEP-19
7731|Great Cobar Slate|35185|6|Mentioned|p226|||||||||
7731|Great Cobar Slate|35219|6|Mentioned|Fig.2|||||||||
7731|Great Cobar Slate|35287|6|Mentioned|p6|||See also Fig.2.||||||
7731|Great Cobar Slate|35383|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
7731|Great Cobar Slate|35385|3|Fully described|p25|||||||||
7731|Great Cobar Slate|37668|6|Mentioned|Fig.1|||||||||
7731|Great Cobar Slate|37727|6|Mentioned|p47|||||||||
7731|Great Cobar Slate|37936|6|Mentioned|Fig.2|||||||||
7731|Great Cobar Slate|38064|6|Mentioned|p43|||||||||
7731|Great Cobar Slate|38292|6|Mentioned|p3|||||||||
7731|Great Cobar Slate|39083|6|Mentioned|Fig.1|||||||||
7731|Great Cobar Slate|39214|6|Mentioned|p11|||||||||
7731|Great Cobar Slate|39618|3|Fully described|p89|||See also Table 1||||||
7731|Great Cobar Slate|39683|6|Mentioned|Fig.3|||||||||
7731|Great Cobar Slate|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
7731|Great Cobar Slate|41090|6|Mentioned|p78|||||||||
7731|Great Cobar Slate|41138|6|Mentioned|Map legend|Pragian|Lochkovian|Pragian-Lochkovian||||||
7731|Great Cobar Slate|41410|5|Briefly described|p295|||||||||18-JAN-10
7731|Great Cobar Slate|41452|6|Mentioned|p22|||||||||
7731|Great Cobar Slate|41872|6|Mentioned|p8|||||||||
7731|Great Cobar Slate|42144|5|Briefly described|p607|||||||||
7731|Great Cobar Slate|42172|4|Described|p162|||See also Fig.4&5||||||
7731|Great Cobar Slate|42208|6|Mentioned|Fig.1 P305|||||||||
7731|Great Cobar Slate|42344|5|Briefly described|p57|||||||||
7731|Great Cobar Slate|42467|5|Briefly described|Map Legend|||||||||
7731|Great Cobar Slate|42521|5|Briefly described|p19, Fig.3 p16|||||||||
7731|Great Cobar Slate|42907|6|Mentioned|Fig.8, P8|||||||||
7731|Great Cobar Slate|42914|5|Briefly described|p10|||||||||
7731|Great Cobar Slate|42983|6|Mentioned|Fig.3,p345|||||||||
7731|Great Cobar Slate|43032|2|Defined|p55|Early Devonian||of Nurri Group||||||
7731|Great Cobar Slate|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|of Nurri Group||||||
7731|Great Cobar Slate|43398|14|Not recorded|Map Legend||Silurian|Part of Cobar Group||||||
7731|Great Cobar Slate|43757|6|Mentioned|p511||Early Devonian|Age: approx. 390-400 Ma||||||
7731|Great Cobar Slate|43774|3|Fully described|p42-44|Lochkovian|Pridolian|||||||
7731|Great Cobar Slate|46032|14|Not recorded|p.411-414.||Silurian|mineralised.||||||
7731|Great Cobar Slate|46900|5|Briefly described|p16|||Part of Nurri Group||||||
7731|Great Cobar Slate|61907|5|Briefly described|p143 Fig. 1|||Of the Cobar Group.||||||
7731|Great Cobar Slate|65469|5|Briefly described|p14, p15, p17, p43, p52|Lochkovian|Pridoli|Lachlan Orogen. Two pyrite-pyrrhotite anomalies have been identified in this unit. See also p55 fig 3-19, p62, p67, p133, p135, p136, p139, p334, p344, p354, App A-VI 3.||Nurri Group||Overlain by the CSA Siltstone. Overlies the Chesney Formation.||
7731|Great Cobar Slate|68823|6|Mentioned|p378 Fig.4|Lochkovian|Ludlow|||Unit in Nurri Group.||Overlies Chesney Formation.||
7731|Great Cobar Slate|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Late Silurian|Lachlan Orogen.||||||
7731|Great Cobar Slate|70821|6|Mentioned|p16|||Quartz-rich zones host localised Cu-Pb-Zn deposits (Gladestone, Dapville and Great Cobar).||||||
7731|Great Cobar Slate|70941|6|Mentioned|p78 fig 32|Early Devonian|Late Silurian|||||Overlies the Chesney Formation. Overlain by the CSA Siltstone and the Amphitheatre Group.||
7731|Great Cobar Slate|71039|6|Mentioned|p19-20|||Hosts the Cobar-type mineral deposits.||Nurri Group||||09-MAR-23
7731|Great Cobar Slate|71285|4|Described|p538-540, p544-549, p552|Late Silurian|Late Silurian|Cobar region. Spatially related to several Cu-Au deposits; at the contact with the Chesney Formation, and in association with the Great Cobar Fault; discussed in detail. Sulfur isotopes, fluid inclusion temperatures detailed.||Nurri Group.||Overlies and is faulted against the Chesney Formation.|Pelite-dominated, thin-bedded turbidites; very minor felsic volcaniclastic rocks.|
7731|Great Cobar Slate|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Nurri Group.||Overlies Chesney Formation.|Carbonaceous mudstone with thin interbeds of fine-grained siltstone, rare graded medium- to fine-grained quartzose sandstone.|
7731|Great Cobar Slate|71860|6|Mentioned|p9|||Copper-Pb-Zn deposits are localised in quartz-rich zones.||||||
7731|Great Cobar Slate|73143|6|Mentioned|p2|||||Nurri Group||||
7731|Great Cobar Slate|73174|5|Briefly described|p1036-1037|Lochkovian|Lochkovian|Cobar Basin.||Nurri Group, Cobar Supergroup||Underlain by and equivalent to Chesney Formation. Overlain by and equivalent to Lower Amphitheatre Group.|Predominantly mudstone.|
7738|Great Northern Coal|22578|6|Mentioned|Fig.9 p399|||||||||
7738|Great Northern Coal|23055|6|Mentioned|Fig4p11|||||||||
7738|Great Northern Coal|23438|5|Briefly described|p25|||Of the Newcastle Coal Measures.||||||20-NOV-08
7738|Great Northern Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Of the  Moon Island Beach Formation.||||||20-NOV-08
7738|Great Northern Coal|24158|5|Briefly described|p172 Fig.3|||Of the Newcastle Coal Measures. Geological Province: Sydney Basin||||||
7738|Great Northern Coal|31549|6|Mentioned|p159|||Stratigraphy||||||
7738|Great Northern Coal|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
7738|Great Northern Coal|34270|6|Mentioned|p254|||||||||
7738|Great Northern Coal|36327|6|Mentioned|p8|||||||||
7738|Great Northern Coal|39308|5|Briefly described|p458|||See also p473.||||||20-NOV-08
7738|Great Northern Coal|39609|6|Mentioned|Table 1|||||||||
7738|Great Northern Coal|39666|6|Mentioned|Table 20|||||||||
7738|Great Northern Coal|40516|6|Mentioned|p395|||||||||
7738|Great Northern Coal|41226|6|Mentioned|Fig.12|||||||||
7738|Great Northern Coal|41463|6|Mentioned|p38|||||||||
7738|Great Northern Coal|41477|6|Mentioned|p79|||||||||
7738|Great Northern Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Great Northern coal seam instead. See also p113.||Of Moon Island Beach Subgroup||||
7738|Great Northern Coal|73304|5|Briefly described|p75|Changhsingian|Changhsingian||252.85 +/- 0.12 Ma U-Pb CA-TIMS.|Moon Island Beach Formation, Newcastle Coal Measures||||02-DEC-22
7753|Green Hills Granodiorite|37529|5|Briefly described|p4|||See also P5||||||
7753|Green Hills Granodiorite|42313|3|Fully described|p41|Middle Silurian|Early Silurian|||||||
7753|Green Hills Granodiorite|42314|5|Briefly described|Map|Early Silurian||||||||
7753|Green Hills Granodiorite|42828|5|Briefly described|Fig.2 P128|||||||||
7753|Green Hills Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb9.||||||
7753|Green Hills Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
7753|Green Hills Granodiorite|63290|6|Mentioned|p403 Fig. 6(c)|Silurian|Silurian|Granodiorite.||||||
7753|Green Hills Granodiorite|68115|5|Briefly described|p7.|||Omeo Zone. Most of the supposed Tom Groggin Granite shown by Chappell et al. (1991) continuing well into NSW from Victoria is now shown as Green Hills Granodiorite in the NSW 1:250 000 data. A small outcrop on the SE corner of Corryong, interpreted as Tom Groggin Granite, is now considered to be Green Hills Granodiorite.||||||
7753|Green Hills Granodiorite|68116|5|Briefly described|Appendix, Map 28.|Pridoli|Llandovery||||||Biotite granodiorite and granite: grey, medium to coarse grained, commonly containing cordierite; common metasedimentary xenoliths.|
7753|Green Hills Granodiorite|69801|5|Briefly described|p2, p4-p5, p110-115, p135, p137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Occurs on the NSW-Victoria border east of Albury. This unit is the same age as granites near Holbrook but younger than the Granya Granite sampled 10km further south.|428.3 +/- 2.1 Ma (SHRIMP U-Pb)|Tom Groggin Suite||Intrudes the Wagga Group.|Medium to coarse-grained, biotite monzogranite and S-type granodiorite.|
7753|Green Hills Granodiorite|73082|6|Mentioned|p17|||Underlies, but is not the source of gold in, the Laurel Hill-Tumbarumba deep lead.||||||
7758|Greenbergers Granite|22638|3|Fully described|p75||Late Devonian|New name.||||||
7758|Greenbergers Granite|42726|5|Briefly described|map legend|Late Devonian||Misspelling? Reserved as Greenburgers Granite.||||||
7758|Greenbergers Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
7762|Greengrove Formation|22768|6|Mentioned|p179|||||||||
7762|Greengrove Formation|22857|5|Briefly described|p179, p458 App.1, Tb.A1.6|Llandovery|Llandovery|Of the Cudal Group. Grey to brown shale, minor lithic arenite; massive fossiliferous limestone horizons. Max. thickness: 8m. Geological Province: Cowra Trough.||||||
7762|Greengrove Formation|23214|3|Fully described|p121|Wenlock|Llandovery|Of Cudal Group. Defined by Savage 1969 (a). Max. thickness 430m. Overlying unit: Kurrajong Park Formation.||||||
7762|Greengrove Formation|32986|6|Mentioned|p6|||Geological map. Llandoverian.||||||
7762|Greengrove Formation|33116|6|Mentioned|Fig.12|||Correlation||||||
7762|Greengrove Formation|33121|6|Mentioned|p85|||Correlation table.||||||
7762|Greengrove Formation|37727|4|Described|p61|||See also P9.||||||
7762|Greengrove Formation|40328|3|Fully described|p80|||||||||
7762|Greengrove Formation|43494|6|Mentioned|p17|Early Silurian|Early Silurian|||||||16-MAR-06
7762|Greengrove Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
7762|Greengrove Formation|43782|5|Briefly described|Map Legend|Wenlock|Llandovery|of Cudal Group.||||||
7762|Greengrove Formation|60989|6|Mentioned|p111|mid to late Llandovery|lower mid Llandovery|Manildra district. Contains a possible Trimerella brachiopod, but probably allochthonous.||||||
7762|Greengrove Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group||||
7765|Greenland Ignimbrite Member|31918|6|Mentioned|p42|||||||||
7768|Greenridge Formation|40726|6|Mentioned|p227|||||||||
7780|Greenwood Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Biotite granite. BMR map symbol: gbd.||||||
7780|Greenwood Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
7780|Greenwood Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
7780|Greenwood Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
7780|Greenwood Granite|31284|6|Mentioned|Map legend|Devonian|Silurian|Silurian to Devonian||||||
7780|Greenwood Granite|33325|6|Mentioned|p19|||Sutton Gp.||||||
7780|Greenwood Granite|33328|5|Briefly described|p17|||||||||
7780|Greenwood Granite|36633|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
7780|Greenwood Granite|37728|4|Described|Table 3|||||||||
7780|Greenwood Granite|39800|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
7780|Greenwood Granite|40328|4|Described|p206|||||||||
7780|Greenwood Granite|44970|14|Not recorded|p22|||||||||
7789|Gregra Group|22503|6|Mentioned|Fig.6 p649||Early Devonian|||||||
7789|Gregra Group|22768|5|Briefly described|p178|Emsian|Pragian|||||||
7789|Gregra Group|22857|4|Described|p178, p454 App.1, Tb.A1.6|Early Devonian|Early Devonian|Overlies Toongi, Goonigal and Mumbil Groups. Occurs in the Cowra Trough, Molong Rise and Hill End Trough; contains invertebrate fauna. Geological Province: Cowra Trough. See also p466 App.1 Tb.A1.6.||||||
7789|Gregra Group|23043|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||
7789|Gregra Group|23170|2|Defined|p190|Emsian|Lochkovian|of Lachlan Fold Belt.||||||
7789|Gregra Group|23214|2|Defined|p179-186|Pragian|Lochkovian|Includes the Garra and Berkley Formations, Maradana Shale, Cuga Burga and Bulls Camp Volcanics. Max. thickness 1400m. Overlying unit: Catombal Group.||||||25-NOV-14
7789|Gregra Group|23309|6|Mentioned|p390|||||||||
7789|Gregra Group|24007|5|Briefly described|p336|Early Devonian|Early Devonian|||||||
7789|Gregra Group|24580|6|Mentioned|p828|||Geological Province: Eastern Lachlan Fold Belt.||||||
7789|Gregra Group|32983|6|Mentioned|p387|||Refers Savage (1968)||||||
7789|Gregra Group|32986|6|Mentioned|p2|||Refers Savage (1968).||||||
7789|Gregra Group|33121|6|Mentioned|p85|||Early Dev.||||||
7789|Gregra Group|34478|6|Mentioned|p472|||||||||
7789|Gregra Group|39331|6|Mentioned|p64|||||||||
7789|Gregra Group|40328|6|Mentioned|p103|||||||||
7789|Gregra Group|43494|6|Mentioned|p22|Devonian|Devonian|Includes the Maradana Shale.||||||16-MAR-06
7789|Gregra Group|43782|5|Briefly described|Map Legend|Emsian|Lochkovian|||||||
7789|Gregra Group|50590|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Nubingerie Formation, Garra Formation, Cuga Burga Volcanics.||||||19-JUL-04
7789|Gregra Group|68003|5|Briefly described|p24 Fig.3-e, p143. |Pragian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Garra Formation and Cuga Burga Volcanics.|Overlies Cuga Burga Volcanics.||
7789|Gregra Group|68592|6|Mentioned|p932, p1170|||Mentioned as having geochemical affinities with Boggy Plain Supersuite.|||Includes Cuga Burga Volcanics.|||
7789|Gregra 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.||||||
7789|Gregra Group|71600|6|Mentioned|p23 Fig 1|Devonian|Devonian|Geological province: Lachlan Fold Belt.|||Includes Garra Formation, Curga Burga Volcanics and Berkley Formation.|||
7790|Greigs Creek Coal|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Of the Glen Gallic Subgroup.  Geological Province: Sydney Basin||||||14-MAR-07
7790|Greigs Creek Coal|29942|3|Fully described|p11|||||||||
7790|Greigs Creek Coal|37087|6|Mentioned|p198|||||||||
7790|Greigs Creek Coal|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Topmost unit in Glen Gallic Sub-group.||Overlies Redmanvale Creek Formation. The unit is not always present. Is overlain by Narrabeen Group.|Durain rich coal.|
7790|Greigs Creek Coal|73625|6|Mentioned|p2|Permian|Permian|Hunter coalfield, Sydney Basin.||||||
7795|Grenfell Granite|24125|5|Briefly described|p87|||Geological Province: Lachlan Fold Belt.||||||
7795|Grenfell Granite|24266|5|Briefly described|p1486|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
7795|Grenfell Granite|24417|2|Defined|p112|Middle Devonian|Early Devonian|Unit subdivided into "Bogalong Granodiorite" and "Warraderry Porphyry" by Bowman (1977a).  Now retained as one unit.  Age: 384+/-3.4Ma (U-Pb SHRIMP).  Max. thickness: ~1km.||||||
7795|Grenfell Granite|29907|6|Mentioned|p9|||||||||
7795|Grenfell Granite|29908|6|Mentioned|p237|||||||||
7795|Grenfell Granite|29910|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
7795|Grenfell Granite|29985|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
7795|Grenfell Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
7795|Grenfell Granite|31993|6|Mentioned|p679|||||||||
7795|Grenfell Granite|39331|6|Mentioned|Fig.7-3|||||||||
7795|Grenfell Granite|40328|4|Described|p206|||||||||
7795|Grenfell Granite|40772|5|Briefly described|p444|||||||||
7795|Grenfell Granite|40882|5|Briefly described|p24|||||||||
7795|Grenfell Granite|42726|5|Briefly described|map legend|Early Devonian||419.  Of the Grenfell Suite (Boggy Plain Supersuite).||||||08-FEB-05
7795|Grenfell Granite|43499|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
7795|Grenfell Granite|49705|6|Mentioned|p20|||||||||
7795|Grenfell Granite|50628|5|Briefly described|Map Legend|Devonian|Devonian|Coarse pink biotite granite. Overlies: Kirribilli Formation.||||||05-JUL-04
7795|Grenfell Granite|60009|5|Briefly described|Map Legend|Eifelian|Eifelian|||||||13-JUL-04
7795|Grenfell Granite|72084|5|Briefly described|p56|Middle Devonian|Middle Devonian||384 +/- 3.4 Ma.||||A-type.|
7796|Gresford Conglomerate Member|22857|5|Briefly described|p498 App.1 Tb.A1.7|Visean|Visean|Geological Province: Tamworth Forearc Basin.||||||
7796|Gresford Conglomerate Member|31228|6|Mentioned|p77|||||||||
7796|Gresford Conglomerate Member|44244|6|Mentioned|p48|||of the Ararat Formation.  Previously regarded as belonging to the Bingleburra Formation.  Geological Province: Gresford Block.||||||
7796|Gresford Conglomerate Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Ararat Formation.  Geol. Province: Gresford Block||||||
7798|Greta Coal Measures|22601|2|Defined|401,407,409-411, 417|Permian|Permian|Geol province Sydney Basin. Overlying unit Branxton Formation, underlying unit Farley Formation.||||||24-SEP-08
7798|Greta Coal Measures|22820|6|Mentioned|p31 Fig. 11|Permian|Permian|At Cessnock in NSW.||||||
7798|Greta Coal Measures|22857|4|Described|p522 App.1 Tb.A1.9|Late Permian|Early Permian|Sandstone, conglomerate, siltstone: contains Pelton, Greta and Homeville coal seams. Includes Rowan and Skeletar Formations. Equivalent of Ashford Coal Measures. Max. thickness: 334m. Geol. Prov.: Sydney Basin. See also pages 524 and 536 App.1 Tb.A1.9.||||||
7798|Greta Coal Measures|22969|4|Described|p 18|||||||||
7798|Greta Coal Measures|22970|5|Briefly described|Plate 6||Permian|||||||
7798|Greta Coal Measures|23350|4|Described|259|Artinskian|Artinskian|||||||
7798|Greta Coal Measures|23438|4|Described|p23|||||||||
7798|Greta Coal Measures|23540|4|Described|Fig2 p 419|||In Cranky Corner Basin nd Maitland-Cessnock-Greta Coalfield.  Also see p417, 421, 424.||||||20-FEB-07
7798|Greta Coal Measures|23837|5|Briefly described|p441|||Geological Province: Tasmania Basin.||||||
7798|Greta Coal Measures|24040|6|Mentioned|p471|Early Permian|Early Permian|Age: ca. 270Ma.||||||21-AUG-08
7798|Greta Coal Measures|24079|5|Briefly described|p432|Permian|Permian|Geological Province: Sydney Basin.||||||
7798|Greta Coal Measures|24121|5|Briefly described|p4, p108|||||||||25-AUG-22
7798|Greta Coal Measures|24240|6|Mentioned|p21|||Geological Province: Sydney Basin.||||||
7798|Greta Coal Measures|24423|5|Briefly described|p230 Fig.3|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
7798|Greta Coal Measures|29437|6|Mentioned|p136|||||||||
7798|Greta Coal Measures|29635|6|Mentioned|p563|||||||||
7798|Greta Coal Measures|29752|6|Mentioned|p37|||||||||
7798|Greta Coal Measures|29922|6|Mentioned|Appendix 1|||||||||
7798|Greta Coal Measures|29944|4|Described|p236|||||||||
7798|Greta Coal Measures|30155|6|Mentioned|p461|||||||||
7798|Greta Coal Measures|30340|6|Mentioned|Table 3|||||||||
7798|Greta Coal Measures|30341|6|Mentioned|p135|||Lower Permian age||||||
7798|Greta Coal Measures|30442|6|Mentioned|p24|||||||||
7798|Greta Coal Measures|30450|6|Mentioned|Table 1|||Permian age. Sydney Basin||||||
7798|Greta Coal Measures|30545|6|Mentioned|Fig.2|||Lower Permian.||||||
7798|Greta Coal Measures|30555|6|Mentioned|Fig.21.5|||||||||
7798|Greta Coal Measures|31062|6|Mentioned|p477|||See also P486||||||
7798|Greta Coal Measures|31081|6|Mentioned|p56|||See also Fig. 2||||||
7798|Greta Coal Measures|31559|6|Mentioned|p156|||||||||
7798|Greta Coal Measures|31560|6|Mentioned|p632|||||||||
7798|Greta Coal Measures|31649|6|Mentioned|p59|||||||||
7798|Greta Coal Measures|31706|6|Mentioned|p657|||Permian correlation chart||||||
7798|Greta Coal Measures|31855|6|Mentioned|p12|||Isolated occurrences of oil shale||||||
7798|Greta Coal Measures|31880|6|Mentioned|p18|||||||||
7798|Greta Coal Measures|31881|6|Mentioned|p329|||See also Table 1. Equiv. Koogah Fm.||||||
7798|Greta Coal Measures|31882|4|Described|p243|||See also p244.||||||20-AUG-18
7798|Greta Coal Measures|31883|4|Described|p594|||See also Table 1||||||
7798|Greta Coal Measures|31885|5|Briefly described|p1438|||Table 1||||||
7798|Greta Coal Measures|31886|6|Mentioned|p393|||||||||
7798|Greta Coal Measures|31887|5|Briefly described|p7|||See also P3||||||
7798|Greta Coal Measures|32073|6|Mentioned|p21|||||||||
7798|Greta Coal Measures|32266|6|Mentioned|p24|||||||||
7798|Greta Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
7798|Greta Coal Measures|32672|6|Mentioned|p675|||||||||
7798|Greta Coal Measures|32833|6|Mentioned|p108|||||||||
7798|Greta Coal Measures|32834|6|Mentioned|Table 3|||||||||
7798|Greta Coal Measures|32836|6|Mentioned|p7|||||||||
7798|Greta Coal Measures|32840|6|Mentioned|Table 1|||||||||
7798|Greta Coal Measures|32920|6|Mentioned|p93|||||||||
7798|Greta Coal Measures|32944|6|Mentioned|p709|||||||||
7798|Greta Coal Measures|32945|6|Mentioned|p83|||Permian||||||
7798|Greta Coal Measures|33128|5|Briefly described|p51|||Permian. Geochemistry.||||||
7798|Greta Coal Measures|33129|6|Mentioned|Table 1|||Adapted from Packham (1969)||||||
7798|Greta Coal Measures|33131|6|Mentioned|Fig.9|||||||||
7798|Greta Coal Measures|33132|6|Mentioned|p1465|||||||||
7798|Greta Coal Measures|33216|6|Mentioned|p10|||Permian||||||
7798|Greta Coal Measures|33334|6|Mentioned|p4|||See also PP5-9.||||||
7798|Greta Coal Measures|33685|6|Mentioned|Table 1|||Permian.||||||
7798|Greta Coal Measures|33686|6|Mentioned|p20|||||||||
7798|Greta Coal Measures|33701|6|Mentioned|Fig.1|||Artinskian||||||
7798|Greta Coal Measures|33711|6|Mentioned|p382|||See also P383 & Table 2.||||||
7798|Greta Coal Measures|33786|6|Mentioned|p17|||||||||
7798|Greta Coal Measures|33867|4|Described|p5|||||||||
7798|Greta Coal Measures|33989|6|Mentioned|p500|||Permian||||||
7798|Greta Coal Measures|34015|4|Described|p323|||Permian||||||
7798|Greta Coal Measures|34036|6|Mentioned|p434|||?equiv to part Shoalhaven Gp.||||||
7798|Greta Coal Measures|34037|6|Mentioned|Table 5.27|||||||||
7798|Greta Coal Measures|34043|6|Mentioned|p451|||Permian||||||
7798|Greta Coal Measures|34048|6|Mentioned|p28|||||||||
7798|Greta Coal Measures|34059|6|Mentioned|Map legend|Permian|Permian|||||||
7798|Greta Coal Measures|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
7798|Greta Coal Measures|34170|6|Mentioned|p47|||Lower Permian.||||||
7798|Greta Coal Measures|34171|6|Mentioned|p16|||||||||
7798|Greta Coal Measures|34287|6|Mentioned|p131|||See also PP133, 135. Permian||||||
7798|Greta Coal Measures|34292|6|Mentioned|p24|||Permian. See also P25||||||
7798|Greta Coal Measures|34300|6|Mentioned|p13|||||||||
7798|Greta Coal Measures|34345|6|Mentioned|p329|||||||||
7798|Greta Coal Measures|34350|6|Mentioned|p16|||Permian. Correlation. See also PP17,18,19.||||||
7798|Greta Coal Measures|34399|6|Mentioned|p312|||||||||
7798|Greta Coal Measures|34400|5|Briefly described|p9|||||||||
7798|Greta Coal Measures|34444|6|Mentioned|Map legend|Permian|Permian|||||||
7798|Greta Coal Measures|34445|6|Mentioned|p319|||||||||
7798|Greta Coal Measures|34447|6|Mentioned|Table 5.2|||||||||
7798|Greta Coal Measures|34448|4|Described|p432|||Permian||||||
7798|Greta Coal Measures|34465|6|Mentioned|p334|||||||||
7798|Greta Coal Measures|34466|6|Mentioned|Fig.5.22|||||||||
7798|Greta Coal Measures|34516|6|Mentioned|p16|||||||||
7798|Greta Coal Measures|34517|6|Mentioned|p46|||||||||
7798|Greta Coal Measures|34556|6|Mentioned|p267|||Refers Osborne (1950)||||||
7798|Greta Coal Measures|34569|6|Mentioned|p11|||Permian||||||
7798|Greta Coal Measures|34614|6|Mentioned|p29|||||||||
7798|Greta Coal Measures|34839|6|Mentioned|p110|||||||||
7798|Greta Coal Measures|34845|6|Mentioned|Fig.4|||||||||
7798|Greta Coal Measures|35065|6|Mentioned|p44|||||||||
7798|Greta Coal Measures|35095|6|Mentioned|p114|||||||||
7798|Greta Coal Measures|35284|6|Mentioned|Fig.1|||||||||
7798|Greta Coal Measures|35767|6|Mentioned|p6|||||||||
7798|Greta Coal Measures|35862|6|Mentioned|p274|||||||||
7798|Greta Coal Measures|35873|6|Mentioned|p56|||||||||
7798|Greta Coal Measures|36042|6|Mentioned|Table 1|||||||||
7798|Greta Coal Measures|36045|6|Mentioned|p332|||||||||
7798|Greta Coal Measures|36069|6|Mentioned|p23|||||||||
7798|Greta Coal Measures|36172|6|Mentioned|Appendix|||||||||
7798|Greta Coal Measures|36327|6|Mentioned|p3|||||||||
7798|Greta Coal Measures|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7798|Greta Coal Measures|36549|6|Mentioned|p519|||||||||
7798|Greta Coal Measures|36604|6|Mentioned|p21|||||||||
7798|Greta Coal Measures|36899|6|Mentioned|p1090|||||||||
7798|Greta Coal Measures|36940|6|Mentioned|p125|||||||||
7798|Greta Coal Measures|37065|5|Briefly described|p29|||||||||
7798|Greta Coal Measures|37081|6|Mentioned|p156|||||||||
7798|Greta Coal Measures|37082|6|Mentioned|p161|||||||||
7798|Greta Coal Measures|37083|6|Mentioned|p165|||||||||
7798|Greta Coal Measures|37084|6|Mentioned|p176|||||||||
7798|Greta Coal Measures|37085|6|Mentioned|p180|||||||||
7798|Greta Coal Measures|37086|4|Described|p182|||||||||
7798|Greta Coal Measures|37087|4|Described|p192|||||||||
7798|Greta Coal Measures|37092|6|Mentioned|p227|||||||||
7798|Greta Coal Measures|37094|6|Mentioned|p238|||||||||
7798|Greta Coal Measures|37100|6|Mentioned|p260|||||||||
7798|Greta Coal Measures|37102|4|Described|p265|||||||||
7798|Greta Coal Measures|37561|6|Mentioned|p105|||||||||
7798|Greta Coal Measures|37773|6|Mentioned|p18|||||||||
7798|Greta Coal Measures|37922|5|Briefly described|p481|||||||||
7798|Greta Coal Measures|38064|6|Mentioned|p41|||||||||
7798|Greta Coal Measures|38614|6|Mentioned|Fig.6|||||||||
7798|Greta Coal Measures|38656|5|Briefly described|Table1.5.5|||p220.||||||20-AUG-18
7798|Greta Coal Measures|38958|5|Briefly described|p490|||||||||
7798|Greta Coal Measures|39266|5|Briefly described|Table 1|||||||||
7798|Greta Coal Measures|39287|6|Mentioned|p20|||See also Fig.2.5||||||
7798|Greta Coal Measures|39288|4|Described|p59|||||||||
7798|Greta Coal Measures|39289|6|Mentioned|p81|||||||||
7798|Greta Coal Measures|39290|6|Mentioned|p88|||||||||
7798|Greta Coal Measures|39292|6|Mentioned|Fig. 6.1|||||||||
7798|Greta Coal Measures|39304|6|Mentioned|p364|||||||||
7798|Greta Coal Measures|39306|6|Mentioned|p398|||||||||
7798|Greta Coal Measures|39307|6|Mentioned|Table 22.1|||||||||
7798|Greta Coal Measures|39308|6|Mentioned|p491|||||||||
7798|Greta Coal Measures|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
7798|Greta Coal Measures|39572|6|Mentioned|p134|||||||||15-FEB-10
7798|Greta Coal Measures|39664|6|Mentioned|Table 8|||||||||
7798|Greta Coal Measures|39754|6|Mentioned|p1690|||||||||
7798|Greta Coal Measures|39777|6|Mentioned|p151|||||||||
7798|Greta Coal Measures|40166|4|Described|p343|||||||||
7798|Greta Coal Measures|40222|6|Mentioned|Figure|||||||||
7798|Greta Coal Measures|40224|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7798|Greta Coal Measures|40321|6|Mentioned|p19|||||||||
7798|Greta Coal Measures|40330|6|Mentioned|Fig.1|||||||||
7798|Greta Coal Measures|40331|4|Described|p1|||||||||
7798|Greta Coal Measures|40396|5|Briefly described|p13|||||||||
7798|Greta Coal Measures|40631|6|Mentioned|p162|||||||||
7798|Greta Coal Measures|40635|6|Mentioned|p39|||||||||
7798|Greta Coal Measures|40652|6|Mentioned|p127|||||||||
7798|Greta Coal Measures|40807|6|Mentioned|p161|||||||||
7798|Greta Coal Measures|40883|6|Mentioned|p8|||||||||
7798|Greta Coal Measures|40963|6|Mentioned|p265|||||||||
7798|Greta Coal Measures|41054|6|Mentioned|Fig.3|||||||||
7798|Greta Coal Measures|41130|6|Mentioned|p45|||||||||
7798|Greta Coal Measures|41131|6|Mentioned|Fig.13|||||||||
7798|Greta Coal Measures|41226|6|Mentioned|p22|||||||||
7798|Greta Coal Measures|41264|6|Mentioned|p251|||||||||
7798|Greta Coal Measures|41290|6|Mentioned|Fig.8|||||||||
7798|Greta Coal Measures|41580|6|Mentioned|Table 1|||||||||
7798|Greta Coal Measures|41689|6|Mentioned|Table 1|||||||||
7798|Greta Coal Measures|41834|6|Mentioned|p590|||||||||
7798|Greta Coal Measures|41902|5|Briefly described|p5 Table 1|||||||||
7798|Greta Coal Measures|41903|6|Mentioned|Map legend|Early Permian||||||||
7798|Greta Coal Measures|41904|6|Mentioned|Map legend|||Age not stated on map||||||
7798|Greta Coal Measures|41911|6|Mentioned|p147|||||||||
7798|Greta Coal Measures|42182|4|Described|p297|Early Permian|Early Permian|See also Table 1||||||04-NOV-04
7798|Greta Coal Measures|42214|6|Mentioned|Fig.1 P461|||||||||
7798|Greta Coal Measures|42309|6|Mentioned|p264|||||||||
7798|Greta Coal Measures|42526|6|Mentioned|Map legend|||||||||
7798|Greta Coal Measures|42648|4|Described|p35, 36|||||||||
7798|Greta Coal Measures|42713|5|Briefly described|Fig. P18|||||||||
7798|Greta Coal Measures|42780|6|Mentioned|p413, p420|||||||||
7798|Greta Coal Measures|42916|5|Briefly described|Table 1|Middle Permian|Early Permian|||||||
7798|Greta Coal Measures|42925|5|Briefly described|Table 1||Early Permian|||||||
7798|Greta Coal Measures|42943|5|Briefly described|p22|||||||||
7798|Greta Coal Measures|42945|6|Mentioned|p27|||||||||
7798|Greta Coal Measures|42949|6|Mentioned|p23|||||||||
7798|Greta Coal Measures|42964|5|Briefly described|p32|||||||||
7798|Greta Coal Measures|42992|6|Mentioned|p36|||||||||
7798|Greta Coal Measures|43017|5|Briefly described|Fig.1,p372|||||||||
7798|Greta Coal Measures|43018|5|Briefly described|Table 1,p386|||||||||
7798|Greta Coal Measures|43084|5|Briefly described|p141|||||||||
7798|Greta Coal Measures|43194|5|Briefly described|p128, 129 Tb. 8.3|Early Permian|Early Permian|Sydney Basin. Contains Skeletar and Rowan Formations. Correlative of the Leard, Goonbri and Maules Creek Formations in the Gunnedah Basin. Deposited during a marine regression beginning in the late Early Permian.||||||
7798|Greta Coal Measures|43257|5|Briefly described|Map Legend||Permian|Age Early to Middle Permian.||||||
7798|Greta Coal Measures|43344|14|Not recorded|p11,18,19,78,84,170||Permian|||||||
7798|Greta Coal Measures|43382|14|Not recorded|p74|||||||||
7798|Greta Coal Measures|43383|14|Not recorded|p20,Fig.5||Permian|||||||
7798|Greta Coal Measures|43384|14|Not recorded|Map Legend|Early Permian||||||||
7798|Greta Coal Measures|43385|14|Not recorded|p179||Artinskian|||||||
7798|Greta Coal Measures|43417|14|Not recorded|Map Legend||Permian|||||||
7798|Greta Coal Measures|43424|14|Not recorded|p11|||||||||
7798|Greta Coal Measures|43437|14|Not recorded|p169-175||Permian|||||||
7798|Greta Coal Measures|43440|14|Not recorded|p36,44,62-65,82,84,|||p90||||||
7798|Greta Coal Measures|43447|14|Not recorded|p15,17,18,28,39,48-9|||||||||
7798|Greta Coal Measures|43448|4|Described|p222-224||Permian|O/lain by Maitland Group. U/Lain by Dalwood Group||||||
7798|Greta Coal Measures|43451|14|Not recorded|Map Legend|||||||||
7798|Greta Coal Measures|43471|14|Not recorded|p240|||Megadesmus, Astartila discussed||||||
7798|Greta Coal Measures|43474|14|Not recorded|p10|||||||||
7798|Greta Coal Measures|43477|2|Defined|p12-18,23,28-40,42,||Permian|p44,46,60,61,Pl.1,3,5||||||
7798|Greta Coal Measures|43479|14|Not recorded|p188,190,192,213,218||Artinskian|p219||||||
7798|Greta Coal Measures|43491|4|Described|pVII/44,46,48||Permian|||||||
7798|Greta Coal Measures|43552|14|Not recorded|p99|||||||||
7798|Greta Coal Measures|43852|14|Not recorded|Fig.3,p200|||||||||
7798|Greta Coal Measures|43881|14|Not recorded|p87-8(prox.anals),99|||||||||
7798|Greta Coal Measures|43984|14|Not recorded|p135-138|||||||||
7798|Greta Coal Measures|44040|14|Not recorded|p23|||||||||
7798|Greta Coal Measures|44063|14|Not recorded|p281|||||||||
7798|Greta Coal Measures|44135|6|Mentioned|p43|||Unit in New South Wales.||||||07-DEC-09
7798|Greta Coal Measures|44219|14|Not recorded|p31||Artinskian|||||||
7798|Greta Coal Measures|44243|14|Not recorded|p645|||||||||
7798|Greta Coal Measures|44244|4|Described|p232|Permian|Permian|Includes Skeletar and Rowan Formations.  Overlies Gyarran Volcanics, Dalwood Group; underlies the Maitland Group.  Max. thickness: >123m.  Geological Province: Sydney Basin.||||||18-AUG-04
7798|Greta Coal Measures|44266|14|Not recorded|p82|||||||||
7798|Greta Coal Measures|44450|5|Briefly described|p147 Fig 43|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
7798|Greta Coal Measures|44489|14|Not recorded|p70|||||||||
7798|Greta Coal Measures|44855|14|Not recorded|p18||Permian|||||||
7798|Greta Coal Measures|44861|14|Not recorded|p245|||||||||
7798|Greta Coal Measures|44998|14|Not recorded|p104||Artinskian|l. Artinskian.||||||
7798|Greta Coal Measures|45006|14|Not recorded|Tb.1,opp.p3|||||||||
7798|Greta Coal Measures|45088|6|Mentioned|p59|||Permian succession||||||
7798|Greta Coal Measures|45090|6|Mentioned|p26|||Relationship of rock units. Isopach map||||||
7798|Greta Coal Measures|46849|6|Mentioned|p197|||||||||
7798|Greta Coal Measures|48600|14|Not recorded|p34|||||||||
7798|Greta Coal Measures|48830|14|Not recorded|p.6|||||||||
7798|Greta Coal Measures|48926|6|Mentioned|p10|||P10 et seq.||||||
7798|Greta Coal Measures|49644|5|Briefly described|Table|||||||||
7798|Greta Coal Measures|50268|5|Briefly described|Map Legend|Artinskian|Artinskian|Geological Province: Sydney Basin.  Overlies: Dalwood Group.  Underlies: Branxton Formation.||||||
7798|Greta Coal Measures|60281|4|Described|p56, p4, p8|Early Permian|Early Permian|A wedge of coal-bearing deltaic sediments - comprising sandstones, conglomerates, coals (seams up to 8m thick), siltstones and clays.  Overlie Dalwood Group and Farley Formation. Max. thickness: 480m.  Geological Province: northern edge of Sydney Basin.||||||22-MAR-05
7798|Greta Coal Measures|60289|5|Briefly described|p1, p2 Fig. 2|Early Permian|Early Permian|Overlies Billy Brook Formation of Dalwood Group. Geological Province: Cranky Corner Basin.||||||22-FEB-05
7798|Greta Coal Measures|60290|3|Fully described|p15, 28-33, 45-47|Late Permian|Early Permian|Unconformably overlies Billy Brook Fm. Overlain by Big table Top Formation. Conglomerate + sst, with minor siltst, clayst + coal. Sandy to gravelly braidplain environments. Thick: 119 m. Age: 278-268 Ma. GeolProv: Cranky Corner Basin.||||||07-FEB-11
7798|Greta Coal Measures|60291|4|Described|p51, 53 Tb.1|Permian|Permian|Overlies Dalwood Group. Overlain by Maitland Group. Thickness: 90-400 m. Conglomerate, sandstone, minor siltstone, claystone and coal. Prograding terrestrial wedge. Geological Province: Cranky Corner Basin. Petrology descirbed.||||||
7798|Greta Coal Measures|60292|5|Briefly described|p65|Early Permian|Early Permian|Overlies Billy Brook Formation. Geological Province: Cranky Corner Basin.||||||
7798|Greta Coal Measures|60293|5|Briefly described|p108 Fig.1|||Overlies Billy Brook Formation. Vitrinite reflectance of organic matter described.||||||
7798|Greta Coal Measures|60294|5|Briefly described|p115, p116 Fig.1|Early Permian|Early Permian|Overlies Billy Brook Formation. Contains hydrocarbon source rock potential.  Geological Province: Cranky Corner Basin.||||||18-MAY-05
7798|Greta Coal Measures|60295|4|Described|p127, p133 Fig.9||Artinskian|Overlies Billy Brook Formation. Plant microfossils suggest deposition in oxygenated channel-plain swamps. Geological Province: Cranky Corner Basin, Sydney Basin.||||||
7798|Greta Coal Measures|60296|5|Briefly described|p155|||Geological Province: Cranky Corner Basin||||||
7798|Greta Coal Measures|60297|4|Described|p167, 170-171 Fig.2|Permian|Permian|Overlies Dalwood Group. Overlain by Maitland Group. Max. thickness: 480m. Conglomerates, sandstone and coals. Braid plain sediments. Sedimentary facies and depositional environments logged and described in detail. Geological Province: Cranky Corner Basin.||||||
7798|Greta Coal Measures|60298|6|Mentioned|p190|||||||||
7798|Greta Coal Measures|60299|6|Mentioned|p208, 218|||Palaeomagnetism measured||||||
7798|Greta Coal Measures|60300|5|Briefly described|p239|Early Permian|Early Permian|Overlies the Dalwood Group. Geological Province: Cranky Corner Basin.||||||
7798|Greta Coal Measures|60386|6|Mentioned|p296|||Bowen/Sydney Basin. Non-marine, coal.||||||
7798|Greta Coal Measures|61201|6|Mentioned|p3|||||||||
7798|Greta Coal Measures|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Incl: Paxton and Kitchener Fms, Kurri Kurri Conglom.and Neath Sst in Newcastle area; Skeletar and Rowan Fm in Hunter Valley area. Noted for its high exinite content relative to other coals in the basin.Geol.Prov:Sydney Basin (restricted to northern part)||||||
7798|Greta Coal Measures|61529|5|Briefly described|p853, p854 Fig. 1b|Early Permian|Early Permian|Overlies Dalwood Group; overlain by Branxton Formation (Maitland Group). Geological Province: Sydney Basin.||||||
7798|Greta Coal Measures|61612|6|Mentioned|p270, p272, p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||13-MAR-09
7798|Greta Coal Measures|61770|6|Mentioned|p112|||||||||
7798|Greta Coal Measures|61772|6|Mentioned|p129, p133||Early Permian|Contains sparse felsic tuffs in the upper parts of the unit.||||||24-SEP-08
7798|Greta Coal Measures|62043|6|Mentioned|pp437-439.||||||||Local thick, areally restricted coal bodies.|
7798|Greta Coal Measures|63172|6|Mentioned|p303, p305|Early Permian|Early Permian|The NSW equivalent of Mersey Coal Measures in Tasmania and Collinsville Coal Measures in Queensland.||||||07-FEB-11
7798|Greta Coal Measures|63832|5|Briefly described|p131 fig 2, p136|Kungurian|Artinskian|Cranky Corner/Gresford Block, Southern New England Fold Belt; also NE Sydney Basin.|||||Paralic coal-bearing deposits.|13-DEC-17
7798|Greta Coal Measures|64571|6|Mentioned|p828|||||||||
7798|Greta Coal Measures|64631|5|Briefly described|p44 Fig.2.|Kungurian|Artinskian|Southern New England Fold Belt, Cranky Corner/Gresford Block, and NE Sydney Basin.  Biostratigraphic age control for base and top, and radiometric control near top.||||Overlies Dalwood Group. Is overlain by Maitland Group.||
7798|Greta Coal Measures|65114|5|Briefly described|p396|||Above the Dalwood Group||||||
7798|Greta Coal Measures|67663|5|Briefly described|p518, p520 Tb.1, p529, p536|Permian|Permian|Early Permian.||||Overlain by the Maitland Group. Overlies Gyarran Volcanics and Dalwood Group.|Comprises thick sequence of sand and silt.|
7798|Greta Coal Measures|67786|6|Mentioned|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||||Overlies Dalwood Group. Is overlain by Maitland Group.||
7798|Greta Coal Measures|68003|5|Briefly described|p38 Fig.3-j.|Early Permian|Early Permian|Hunter Coalfield (Sydney Basin), Brigalow Belt South Bioregion. Correlative of Bellata Group in the Gunnedah Basin, and of Koogah and Willow Tree Formations in the Werrie Basin. A thick fluvio-deltaic wedge, prograding southwards from the tectonically-active New England area as far as Newcastle region.|||Includes Skeletar and Rowan Formations.|Overlies Dalwood Group. Is overlain by Maitland Group.||
7798|Greta Coal Measures|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields. Equivalent to Bellata Group of Gunnedah Basin, and partly to lower Shoalhaven Group.|||Includes Skeletar and Rowan Formations.|Overlies Gyarran Volcanics and Dalwood Group. Is overlain by Maitland Group.||
7798|Greta Coal Measures|68005|6|Mentioned|p39.|||Sydney Basin. Correlated with Ashford Coal Measures.||||||
7798|Greta Coal Measures|68493|4|Described|p3 Fig.1, p5, p5 Fig.3, p6, p19|Roadian|Roadian|Sydney Basin. CA-IDTIMS age from Metcalfe et al. (2012) from the top of this unit. Up to 63m thick in the type section; coal seams up to 11 m thick. Interpreted to have been deposited during a lowstand regression event in an alluvial fan delta environment.|ca. 271 Ma at the top.|||Overlies Dalwood Group. Overlain conformably by the Maitland Group.|Consists of upwards-coarsening conglomerates, as well as sandstones with few thin siltstone and mudstone layers; coal.|
7798|Greta Coal Measures|68592|6|Mentioned|p1782|Permian|Permian|Hunter Valley.||||Broadly equivalent to Shoalhaven Group.||
7798|Greta Coal Measures|69297|6|Mentioned|p501, p502 fig 5.43, p503|Wordian|Kungurian|Sydney Basin. High exinite content suggests that this unit has a high potential to also produce petroleum.  ||||Overlies the Farley Formation and the Dalwood Group. Overlain and interfingers with the Branxton Formation.||
7798|Greta Coal Measures|69683|5|Briefly described|p410-411 Figs.1-2, p420 Fig.5, p421 Tb.4|Middle Permian|Early Permian.||||Includes Skeletar, Rowan, Kitchener, Paxton Formations; Neath Sandstone; Kurri Kurri Conglomerate.||Coal seams, siltstone, sandstone, claystone, chert.|
7798|Greta Coal Measures|69793|6|Mentioned|p1121 Fig.12|Artinskian|Artinskian|Gresford Block, Tamworth Belt.||||||
7798|Greta Coal Measures|70096|5|Briefly described|p221;Supp4|||Of northern Sydney Basin. See also supplementary files in appendix for additional stratigraphic and locality information.|||Includes Rowan Formation.|||
7798|Greta Coal Measures|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
7798|Greta Coal Measures|70791|5|Briefly described|p275, p277, p285, p293|Cisuralian|Cisuralian|Hunter Coalfield and north Werrie Basin. Up to 180m thick (at Werris Creek Mine).|||Skeletar, Rowan Formations.|||
7798|Greta Coal Measures|70878|5|Briefly described|p712, p715 Fig.10, p720-721|Permian|Permian|Hunter Coalfield, Sydney Basin.|||Rowan Formation, Greta Seam.|Is overlain by Maitland Group.||
7798|Greta Coal Measures|71701|5|Briefly described|p169-p170|||Sydney Basin.||Rowan Formation||Overlain by the Wittingham Coal Measures.||
7798|Greta Coal Measures|73197|6|Mentioned|p478|Guadalupian|Guadalupian|Sydney Basin. Tuff layers sourced from the Currarong Orogen.|272-266 Ma||||Includes tuff layers.|
7798|Greta Coal Measures|73304|6|Mentioned|p66, p75||||||Rowan Formation, Skeletar Formation|||
7798|Greta Coal Measures|73421|6|Mentioned|p17|||Sydney Basin, northern.|||Rowan Formation|||
7798|Greta Coal Measures|73495|6|Mentioned|p506|Kungurian|Artinskian|Sydney Basin.||||||
7815|Grey Mare Granodiorite|34519|6|Mentioned|p43|||||||||
7815|Grey Mare Granodiorite|39860|5|Briefly described|p21|||||||||
7815|Grey Mare Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb30.||||||
7815|Grey Mare Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
7819|Greymare Granodiorite|32491|5|Briefly described|p16|||Upper Permian or Triassic.||||||19-NOV-07
7819|Greymare Granodiorite|32492|6|Mentioned|Map legend|Triassic|Late Permian|Upper Permian or Triassic||||||
7819|Greymare Granodiorite|32876|6|Mentioned|Map legend|Early Triassic|Late Permian|Upper Permian-Lower Triassic||||||
7819|Greymare Granodiorite|32880|4|Described|p3|||See also p11. Upper Permian or Lower Triassic.||||||19-NOV-07
7819|Greymare Granodiorite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
7819|Greymare Granodiorite|38905|6|Mentioned|p303|||||||||
7819|Greymare Granodiorite|39071|6|Mentioned|p346|||||||||
7819|Greymare Granodiorite|39445|5|Briefly described|Table 12|||||||||
7819|Greymare Granodiorite|43008|5|Briefly described|map legend|||||||||
7819|Greymare Granodiorite|48940|4|Described|p65|||||||||
7819|Greymare Granodiorite|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Grey, medium-grained, uneven-grained to slightly porphyritic, quartz-rich, biotite tonalite to granodiorite; moderate to high magnetic response.||||||
7819|Greymare Granodiorite|63748|4|Described|p16, p26, p28-30|Early Triassic|Permian|Of Greymare Suite. Age:279.6+/-2.6Ma (SHRIMP). Intrudes Texas beds. I-type; grey, fine- to med.-grained, slightly porphyritic to uneven-grained, quartz-rich tonalite to granodiorite? Possibly should be termed a 'tonalite'. Further lith.details included.||||||07-FEB-11
7819|Greymare Granodiorite|65668|6|Mentioned|p1, p16|Permian|Permian|Age: c.280 Ma. Undeformed; intrudes accretionary wedge sediments.||||||
7819|Greymare 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 Boxwell Granodiorite, are all mapped under the symbol, Pgn.||||||
7819|Greymare Granodiorite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
7819|Greymare Granodiorite|68679|4|Described|p455-457, p464-466|Permian|Permian|Northern New England Batholith (NNEB). Originally assigned to the Greymare Supersuite by Donchak et al. (2007). ~45 km2. Compositionally distinct from all other granitoids in the NNEB. Cut by a dyke swarm extending from Braeside to Greymare. Geochemistry described in some detail; geochemical plots. Has adakitic affinities; may be prospective for Cu and Cu-Au.|279.6 +/- 2.6 Ma (SHRIMP: PRISE, ANU).|Greymare Suite.||Intrudes Texas beds.|Grey, fine- to medium-grained, porphyritic to uneven-grained tonalite to granodiorite?; slightly altered; slightly to moderately deformed. Widespread ~2cm biotite phenocrysts and rare hornblende, are characteristic. Unevolved, low-medium-K, I-type.|
7819|Greymare Granodiorite|68901|5|Briefly described|p8, p6|Early Permian|Early Permian|New England Region. SHRIMP age derived from Donchak et al, 2007.|279.6 +/- 2.6 Ma (SHRIMP U-Pb)|||||26-SEP-18
7819|Greymare Granodiorite|70373|6|Mentioned|p790|Early Permian|Early Permian|Probable variation on Greymare Granite, p800.||||||
7819|Greymare Granodiorite|70876|5|Briefly described|p77|Early Permian|Early Permian|New England Orogen. SHRIMP date is derived from Donchak et al, 2013.|279.6 +/- 2.6 Ma (SHRIMP U-Pb)|Clarence River Supersuite||||
7819|Greymare Granodiorite|71628|6|Mentioned|p18: 10|||Robertson (1970). Now Greymare Tonalite.||||||
7819|Greymare Granodiorite|72297|6|Mentioned|p726|||Source of dimension stone; quarried at Warwick.||||||
7819|Greymare Granodiorite|73197|6|Mentioned|p475 Fig.6, p477-478|Cisuralian|Cisuralian|New England Orogen, southern. Depleted in K, Th and U.|279 Ma||||Granitic intrusive.|
7822|Grieg Creek Conglomerate|40276|6|Mentioned|p23|||||||||
7826|Griman Creek Formation|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p495 Fig.3, p498|Albian|Albian|N Surat Basin. Up to 48m thick.|||||Labile glauconitic and commonly calcareous sandstone, with siltstone and minor mudstone; intraformational conglomerates and thin coal lenses in upper part; molluscan coquinites in lower part.|
7826|Griman Creek Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Albian|Albian|In Surat Basin, Eromanga Basin.||||||
7826|Griman Creek Formation|22757|5|Briefly described|Table6,p11||Early Cretaceous|200 m thick. Surat Basin||||||
7826|Griman Creek Formation|22857|5|Briefly described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Cenomanian|Albian|Of the Rolling Downs Group. Lithic arenite, siltstone, minor conglomerate. Contains the Coocoran Claystone Member. Max. thickness: 30m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5..||||||
7826|Griman Creek Formation|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Albian|||||||
7826|Griman Creek Formation|23053|6|Mentioned|p86|||||||||
7826|Griman Creek Formation|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Surat Basin.||||||
7826|Griman Creek Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
7826|Griman Creek Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 345m.||||||
7826|Griman Creek Formation|24085|5|Briefly described|p42 Tb.2|Early Cretaceous|Early Cretaceous|Freshwater deposit.||||||
7826|Griman Creek Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
7826|Griman Creek Formation|29387|6|Mentioned|Table 5|||||||||
7826|Griman Creek Formation|29721|6|Mentioned|Table 246|||||||||
7826|Griman Creek Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7826|Griman Creek Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
7826|Griman Creek Formation|31116|4|Described|p45|||See also P1. L.Cretaceous||||||
7826|Griman Creek Formation|31208|6|Mentioned|Table 1|||See also Fig. 7||||||
7826|Griman Creek Formation|31376|6|Mentioned|p4|||||||||
7826|Griman Creek Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|32314|6|Mentioned|Fig. 4|||||||||
7826|Griman Creek Formation|32796|2|Defined|p30|middle Albian|early Albian|Lower to Middle Albian.||||||17-NOV-15
7826|Griman Creek Formation|33070|4|Described|Table 2|||L.Cret.||||||
7826|Griman Creek Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|33090|4|Described|Table 4|||L.Cret.||||||
7826|Griman Creek Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
7826|Griman Creek Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
7826|Griman Creek Formation|33448|6|Mentioned|p7|||||||||
7826|Griman Creek Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|33642|6|Mentioned|p144|||Refers Jenkins (1960).||||||
7826|Griman Creek Formation|34613|6|Mentioned|Table 4|||||||||
7826|Griman Creek Formation|34948|6|Mentioned|Fig. 70|||||||||
7826|Griman Creek Formation|35793|6|Mentioned|Fig.3|||||||||
7826|Griman Creek Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
7826|Griman Creek Formation|35937|6|Mentioned|Fig.5|||||||||
7826|Griman Creek Formation|36243|6|Mentioned|Table 7A|||||||||
7826|Griman Creek Formation|36356|6|Mentioned|p66|||||||||
7826|Griman Creek Formation|36581|6|Mentioned|p464|||||||||
7826|Griman Creek Formation|36749|6|Mentioned|p144|||||||||
7826|Griman Creek Formation|37117|5|Briefly described|p313|||||||||
7826|Griman Creek Formation|37995|4|Described|p66|||||||||
7826|Griman Creek Formation|38199|6|Mentioned|p431|||||||||
7826|Griman Creek Formation|39211|5|Briefly described|p33|||||||||
7826|Griman Creek Formation|39212|5|Briefly described|p18|||||||||
7826|Griman Creek Formation|39216|6|Mentioned|p56|||||||||
7826|Griman Creek Formation|39445|5|Briefly described|Table 11|||||||||
7826|Griman Creek Formation|39943|6|Mentioned|Table 9A|||||||||
7826|Griman Creek Formation|40245|6|Mentioned|Table 2|||||||||
7826|Griman Creek Formation|40249|6|Mentioned|p38|||Mention Fig.1||||||
7826|Griman Creek Formation|41060|6|Mentioned|Fig.3|||Generalized stratigraphy||||||
7826|Griman Creek Formation|41064|6|Mentioned|p62|||||||||
7826|Griman Creek Formation|41187|6|Mentioned|Fig.2|||||||||
7826|Griman Creek Formation|41216|6|Mentioned|Fig.18|||||||||
7826|Griman Creek Formation|41266|6|Mentioned|Fig.3|||||||||
7826|Griman Creek Formation|41628|6|Mentioned|p86|||||||||
7826|Griman Creek Formation|41992|4|Described|Fig.2 P183|||||||||
7826|Griman Creek Formation|42007|5|Briefly described|p182|||||||||
7826|Griman Creek Formation|42071|6|Mentioned|p117|||||||||
7826|Griman Creek Formation|42429|5|Briefly described|p156|||||||||
7826|Griman Creek Formation|42494|5|Briefly described|Table 1 P24|||||||||
7826|Griman Creek Formation|42673|5|Briefly described|Fig.2, P184|||||||||
7826|Griman Creek Formation|43000|5|Briefly described|Fig.5,p112|||Of Rolling Downs Group.||||||13-MAR-09
7826|Griman Creek Formation|43002|5|Briefly described|Fig.2,p135|||||||||
7826|Griman Creek Formation|43085|5|Briefly described|Fig.4|||0f Rolling Downs Group||||||
7826|Griman Creek Formation|43196|6|Mentioned|p418|||||||||
7826|Griman Creek Formation|43459|14|Not recorded|p316-7|||||||||
7826|Griman Creek Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Rolling Downs Group||||||
7826|Griman Creek Formation|43995|14|Not recorded|Tb.p9||Cretaceous|Equivalent to Blythesdale Group.||||||
7826|Griman Creek Formation|45110|2|Defined|p121|late Albian|late Albian|See also p24 & Table 18. Formerly Griman Ck.Gp. (Jenkins,59).||||||17-NOV-15
7826|Griman Creek Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
7826|Griman Creek Formation|46791|4|Described|p48|||||||||
7826|Griman Creek Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
7826|Griman Creek Formation|46984|6|Mentioned|Table 1|||||||||
7826|Griman Creek Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
7826|Griman Creek Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
7826|Griman Creek Formation|60524|5|Briefly described|p485, p486 Fig. 1|Aptian|Aptian|Coastal brackish/estuarine to freshwater fluviatile-lacustrine unit; contains viviparids, thiarids and other non-marine gastropod taxa.  Geological Province: Surat Basin.  See also p488.||||||21-OCT-04
7826|Griman Creek Formation|61198|5|Briefly described|p5, p6 Tb. 1, p18-20, p43|Cretaceous|Cretaceous|Where exposed, rock is weathered and silicified; unweathered rock is bluish-grey (due to finely disseminated pyrite) and greenish-grey glauconitic rocks; dominantly siltstone and very fine sst in which sedimentary structures have been preserved. p29-30.||||||25-JAN-06
7826|Griman Creek Formation|61199|5|Briefly described|p1, p4|Cretaceous|Cretaceous|Meta-sediments. Mentioned also in terms of equivalent rocks. See also pages, 7,9,11 etc. - Figures 4, 5, and 7 etc.||||||25-JAN-06
7826|Griman Creek Formation|61200|5|Briefly described|p1, p7 Tb. 2|Cretaceous|Cretaceous|Deltaic to marine deposits at base, and fluviatile deposits in upper part of unit - characterised by labile sandstone, siltstone, minor mudstone; variably kaolinised, silicified and ferruginised.||||||
7826|Griman Creek Formation|61221|4|Described|p1-2, p5, p13|Cretaceous|Cretaceous|Geological Province: Surat Basin. Weathered and mottled sandstone in outcrop. Fresher rock consists of red coloured, commonly medium grained, well sorted arkosic sandstone frequently interbedded with shale beds.||||||
7826|Griman Creek Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Labile sandstone, siltstone, minor conglomerate. Geological Province: Surat Basin.||||||07-FEB-11
7826|Griman Creek Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
7826|Griman Creek Formation|63218|6|Mentioned|p211. |Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|64061|4|Described|p66, p67|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group. Geol. prov: Surat Basin. Mostly non-marine: comprises interbedded fine-grained sandstones, mudstones + siltstones (sporadically with intraformational conglomerate, coal+glauconitic pellets reworked from underlying marine strata.||||||17-APR-08
7826|Griman Creek Formation|64197|6|Mentioned|p630 Fig.7|Cretaceous|Cretaceous|Surat Basin||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|64856|3|Fully described|p79, p100-102|Albian|Albian|Reiser (1970) after Jenkins (1960). Originally the Griman Creek Group (Jenkins, 1959), which also included a weathered upper unit which he named the Telgazli Formation. Superseded by Griman Creek Formation (Jenkins, 1960). This was expanded by Thomas and Reiser (1968) to include the Telgazli Formation, in their informal Griman Creek beds. This last was redefined by Reiser (1970) as the Griman Creek Formation, with a reference section 8-346m in GSQ Surat 3. Surat Basin. Thinly bedded fine to medium grained labile sandstone, siltstone, mudstone, with thick sandstone beds and minor muddy siltstone, intraformational conglomerate and coal. Conformably overlies Surat Siltstone. Age from palynoflora (unit APK5).| | ||||29-NOV-17
7826|Griman Creek Formation|64857|5|Briefly described|p113 Fig.3|||Overlies Surat Siltstone, Surat Basin.||||||
7826|Griman Creek Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
7826|Griman Creek Formation|65112|6|Mentioned|p329, Fig 11 p324; Fig 16 p328|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|135-101 Ma.|||Overlies Surat Siltstone.||22-MAR-12
7826|Griman Creek Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Surat Siltstone.||||||
7826|Griman Creek Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
7826|Griman Creek Formation|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Overlies the Surat Siltstone, Surat Basin||||||
7826|Griman Creek Formation|65119|5|Briefly described|Table 1 p504, fig 2,7- 8, 14, 16-19|Aptian|Aptian|Surat Basin. Lithic glauconitic, sandstone, siltstone and mudstone, up to 480 m thick. Age: ?-107Ma. Fission Track age: 103+/-9 Ma.||||||07-MAR-12
7826|Griman Creek Formation|65386|5|Briefly described| S141, S142, S146 Fig.7, S147|Cretaceous|Cretaceous|Marginal marine and freshwater sediments. Slightly deformed and extensively weathered. Western margin of Surat Basin.||||||
7826|Griman Creek Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Rolling Downs Group.||Overlies Surat Siltstone.||
7826|Griman Creek Formation|66623|6|Mentioned|p265.|||Surat Basin. Equivalent in part to Allaru Mudstone, Koonenberry Belt.||||||
7826|Griman Creek Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
7826|Griman Creek Formation|67402|4|Described|p146 fig SRT3, p148, p156|Albian|Albian|Surat Basin. Deposited in nearshore marine to deltaic environments. Approximately 346m thick.||||Overlies the Surat Siltstone.|Sandstone, minor muddy siltstone, intraformational conglomerate and coal.|
7826|Griman Creek Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Surat Siltstone.||
7826|Griman Creek Formation|68069|4|Described|Map legend, p2.|Early Cretaceous|Early Cretaceous|Surat Basin. Terrestrial (possibly estuarine) environment. Forms subdued outcrop and is only exposed on the margins of slope systems where preserved by Tertiary silcrete. Zone to 30 m is host for opal mineralisation.||Topmost unit in Rolling Downs Group.|Includes Coocoran Claystone Member and the Wallangulla Sandstone Member.|Overlies Surat Siltstone conformably.|Interbedded fine- to medium-grained sandstone with rhyolite detritus, siltstone and claystone, minor coal; grey when unweathered, surface exposures are kaolinised and locally silicified; plant fossils common; opalised plant and animal fossils.|12-JUN-14
7826|Griman Creek Formation|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
7826|Griman Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat Basin. ||Unit in Rolling Downs Group.||Conformably overlies Wallumbilla Formation.||
7826|Griman Creek Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|68593|3|Fully described|p4-8, p11, p23, p44, p47, p84-86|Albian|Albian|Said to be redefined, but most information only refers to Angledool. Defined by Reiser (1970): his type section was the interval between 25' and 1135' (7.6m and 346m) in GSQ drillhole Surat 3. Named after Griman Creek near Surat (Qld). 196.5m thick in borehole (Bourke, 1973); up to 400m thick in Surat Inlier. New type section [actually new Reference section]: eastern walls in Lunatic Hill open cut (GR 593940mE 6740354mN). Felsic volcanic origin. Relatively abundant and highly diverse fossils (listed in Appendix 6). Middle to possibly late Albian. Depositional environment changed from beach or near-shore marine at the base, to flood-plain in upper parts.||Rolling Downs Group.|Wallangulla Sandstone, Coocoran Claystone, Members.|Conformably overlies Surat Siltstone. Is overlain unconformably by Cumborah Gravel.|Grey, weathering to white, fine- to medium-grained sandstone, laminated to massive siltstone, and mudstone; kaolinised. Intraformational conglomerate and coal present in upper part.|11-DEC-15
7826|Griman Creek Formation|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Albian|Albian|Surat Basin. Fluvial floodplain to paralic.||Of the Rolling Downs Group.|Includes Coocoran Claystone, Wallangulla Sandstone, Finch Claystone, and Lower Griman Creek Formation.|||16-JAN-17
7826|Griman Creek Formation|68821|5|Briefly described|p292 Fig.1, p292, p295, pp298-301, p307|Cretaceous|Cretaceous|Lower Cretaceous age. Contains ubiquitous disseminated pyrite. Fluvial to fluvial-lacustrine depositional environment (brackish).||Of the Rolling Downs Group.||Underlain by the Surat Siltstone.|Comprises fluvial sandstone and siltstone.|
7826|Griman Creek Formation|69582|5|Briefly described|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Surat Siltstone.||
7826|Griman Creek Formation|69594|5|Briefly described|p519, p538-539, p550, p574|Albian|Albian|Jenkins (1959, 1960); Reiser (1970). The uppermost unit of the Surat Basin. Refers to most of the Cretaceous rocks S and E of Surat, including its weathered equivalent, the Telgazli Formation (Jenkins, 1959) as synonymised by Thomas and Reisler (1968). Up to 400m thick. Initially shallow-marine or shoreline deposits, followed by paralic to deltaic grading to floodplain conditions in the upper part. Diverse fossils (in NSW).||||Conformably overlies Surat Siltstone. Correlated with Styx Coal Measures.|Labile sandstones, siltstones and mudstones, with intraformational conglomerate and minor coal, mostly in the upper parts. Shelly coquinas occur low in the Formation.|
7826|Griman Creek Formation|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||||||
7826|Griman Creek Formation|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.||Rolling Downs Group.||Overlies Surat Siltstone.||
7826|Griman Creek Formation|70836|5|Briefly described|p473-475|Albian|Albian|Surat Basin; Lightning Ridge area. Contains fragmentary remains of a new, unnamed megaraptorid: systematic paleontology. Regressive beach or nearshore marine deposits, followed by paralic to deltaic and finally fluvial floodplain conditions. Diverse vertebrate fauna (listed). Limited age determinations discussed.|~107 Ma to c.99 Ma (fission-track).|Rolling Downs Group.||Overlies Surat Siltstone. Coeval with Toolebuc and Allaru Formations.|Primarily non-marine, thinly-bedded and interlaminated fine- to medium-grained sandstone and mudstone. Freshwater and brackish molluscs in lower part; coal seams and freshwater molluscs in upper part.|
7826|Griman Creek Formation|71092|6|Mentioned|p237|Early Cretaceous|Early Cretaceous|Lightning Ridge. Contains the turtle fossil Spoochelys ormondea.||||||
7826|Griman Creek Formation|71601|5|Briefly described|p120, p121-122, 123|Albian|Albian|Geological province: Surat Basin. Near Lightning Ridge, NSW. A succession of regressive beach or nearshore marine to paralic/deltaic, and finally fluvial floodplain deposits. Includes diverse dinosaurian fauna, e.g. plesiosaurs. Evidence of ankylosaurians described.||Unit of Rolling Downs Group.|Wallangulla Sandstone Member, Finch clay facies.||Includes some coal seams near top.|
7826|Griman Creek Formation|72297|6|Mentioned|p758|Cretaceous|Cretaceous|An extension of this unit in the Hebel-Dirranbandi area hosts opal.||||||
7826|Griman Creek Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||||Overlies Surat Siltstone.||
7826|Griman Creek Formation|73113|6|Mentioned|p22|Late Cretaceous|Late Cretaceous|Partial aquifer.||||||
7826|Griman Creek Formation|73153|6|Mentioned|p285|Cenomanian|Cenomanian|Holotype material[?] (NHMUK R3718) for Rapator ornitholestoides (a megaraptoran) was recovered from this unit in New South Wales, as well as a fragmentary cervical vertebra (LRF 3050.AR) classified within Noasauridae.||||||
7826|Griman Creek Formation|73203|6|Mentioned|p648|Cretaceous|Cretaceous|Hosts opal at Lightning Ridge.|||Finch Clay Facies|||
7840|Grove Porphyrite|31140|6|Mentioned|p55|||||||||
7848|Gubberamunda Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497|Tithonian|Kimmeridgian|Mis-spelt as Gubbermunda in Tb.1. The permeable sandstones form a major fresh-water subsurface aquifer. Thickness generally <100m.||||Grades laterally into Hooray Sandstone. Interfingers with upper part of Pilliga Sandstone; equivalent to Kumbarilla beds.|Quartzose sub-labile sandstone with minor siltstone and mudstone beds.|
7848|Gubberamunda Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Late Jurassic|In Surat Basin, Eromanga Basin.||||||
7848|Gubberamunda Sandstone|22757|5|Briefly described|Table6,p12|Late Jurassic|Late Jurassic|200 m. Surat Basin||||||
7848|Gubberamunda Sandstone|22857|5|Briefly described|p296-7 Tb.22.1, p314|Tithonian|Oxfordian|Of the Injune Creek Group. Merges with the Pilliga Sandstone from NSW. Geological Province: Surat Basin. See also p546 App.1 Tb.A1.12.||||||
7848|Gubberamunda Sandstone|22865|4|Described|p314,Table22.1p296-7|Early Cretaceous|Late Jurassic|||||||
7848|Gubberamunda Sandstone|23056|6|Mentioned|9|||Geol province Eromanga Basin||||||
7848|Gubberamunda Sandstone|23818|6|Mentioned|p141 Fig.65, p142|Jurassic|Jurassic|Geological Province: Great Artesian Basin. Of the Blythesdale Group.||||||
7848|Gubberamunda Sandstone|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
7848|Gubberamunda Sandstone|24068|4|Described|p270 Table 2|Late Jurassic|Late Jurassic|Geological Province: Surat Basin.  Maximum thickness: 250m.||||||
7848|Gubberamunda Sandstone|24070|5|Briefly described|p303|Late Jurassic|Middle Jurassic|Geological Province: Coonamble Embayment.||||||
7848|Gubberamunda Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
7848|Gubberamunda Sandstone|29387|6|Mentioned|Table 5|||||||||
7848|Gubberamunda Sandstone|29393|6|Mentioned|Table 4|||Jurassic.||||||
7848|Gubberamunda Sandstone|29591|6|Mentioned|p77|||||||||
7848|Gubberamunda Sandstone|29698|6|Mentioned|p65|||||||||
7848|Gubberamunda Sandstone|29721|6|Mentioned|Table 246|||||||||
7848|Gubberamunda Sandstone|30021|6|Mentioned|p89|||||||||
7848|Gubberamunda Sandstone|30024|6|Mentioned|p332|||||||||
7848|Gubberamunda Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
7848|Gubberamunda Sandstone|30694|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|30695|4|Described|Table 4|||Upper Jurassic age||||||
7848|Gubberamunda Sandstone|30696|4|Described|Table 4|||Middle to Upper Jurassic age||||||
7848|Gubberamunda Sandstone|30697|6|Mentioned|p34|||Major aquifer present||||||
7848|Gubberamunda Sandstone|30700|6|Mentioned|p22|||Map. Jurassic-Cretaceous||||||
7848|Gubberamunda Sandstone|30701|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|30702|6|Mentioned|p48|||See also P49-51, Fig.1,2,Table 1||||||
7848|Gubberamunda Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
7848|Gubberamunda Sandstone|31097|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|31098|5|Briefly described|Table 1|||||||||
7848|Gubberamunda Sandstone|31116|4|Described|p38|||See also Table 2. Jurassic||||||
7848|Gubberamunda Sandstone|31369|6|Mentioned|Table 4|||||||||
7848|Gubberamunda Sandstone|32136|6|Mentioned|p9|||Miospores||||||
7848|Gubberamunda Sandstone|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Mid.-U.JurassicM - U||||||
7848|Gubberamunda Sandstone|32276|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
7848|Gubberamunda Sandstone|32797|4|Described|Table 4|||||||||
7848|Gubberamunda Sandstone|33070|4|Described|Table 2|||U.Jur.||||||
7848|Gubberamunda Sandstone|33071|6|Mentioned|p6|||L.Cret.||||||
7848|Gubberamunda Sandstone|33075|6|Mentioned|p451|||||||||
7848|Gubberamunda Sandstone|33080|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|33090|4|Described|Table 4|||U.Jur.||||||
7848|Gubberamunda Sandstone|33091|5|Briefly described|p10|||Stratigraphy||||||
7848|Gubberamunda Sandstone|33094|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|33367|4|Described|p11|||See also Table 1.||||||
7848|Gubberamunda Sandstone|33371|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|33451|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
7848|Gubberamunda Sandstone|33672|6|Mentioned|p44|||||||||
7848|Gubberamunda Sandstone|33828|6|Mentioned|Table 3|||||||||
7848|Gubberamunda Sandstone|33939|6|Mentioned|p412|||Unit of Blythesdale Gp.||||||
7848|Gubberamunda Sandstone|33971|6|Mentioned|p36|||See also Fig.29.||||||
7848|Gubberamunda Sandstone|34212|6|Mentioned|p2|||Jurassic||||||
7848|Gubberamunda Sandstone|34254|6|Mentioned|p489|||||||||
7848|Gubberamunda Sandstone|34543|6|Mentioned|p98|||||||||
7848|Gubberamunda Sandstone|34611|6|Mentioned|Fig.65|||Correlation chart. Blythesdale Group||||||
7848|Gubberamunda Sandstone|34613|4|Described|Table 4|||||||||
7848|Gubberamunda Sandstone|35793|6|Mentioned|Fig.3|||||||||
7848|Gubberamunda Sandstone|36243|6|Mentioned|Table 7A|||||||||
7848|Gubberamunda Sandstone|36570|6|Mentioned|Table 1|||Also mention P55.||||||
7848|Gubberamunda Sandstone|37117|5|Briefly described|p313|||||||||
7848|Gubberamunda Sandstone|37993|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|37995|4|Described|p64|||||||||
7848|Gubberamunda Sandstone|38068|6|Mentioned|p71|||||||||
7848|Gubberamunda Sandstone|38199|6|Mentioned|p428|||||||||
7848|Gubberamunda Sandstone|39211|5|Briefly described|Fig.3|||||||||
7848|Gubberamunda Sandstone|39212|4|Described|p38|||Excursion site. Aquifers. See also P16 & 25||||||
7848|Gubberamunda Sandstone|39315|6|Mentioned|Fig.5|||||||||
7848|Gubberamunda Sandstone|39445|5|Briefly described|Table 10|||||||||
7848|Gubberamunda Sandstone|39494|6|Mentioned|Fig.5|||||||||
7848|Gubberamunda Sandstone|39943|6|Mentioned|Table 9A|||||||||
7848|Gubberamunda Sandstone|40030|6|Mentioned|Fig.5|||||||||
7848|Gubberamunda Sandstone|40245|6|Mentioned|Table 2|||||||||
7848|Gubberamunda Sandstone|40249|6|Mentioned|p38|||||||||
7848|Gubberamunda Sandstone|40250|6|Mentioned|Fig.7|||||||||
7848|Gubberamunda Sandstone|40540|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|40541|3|Fully described|p110|||||||||
7848|Gubberamunda Sandstone|40544|6|Mentioned|Fig.6|||||||||
7848|Gubberamunda Sandstone|40623|5|Briefly described|p108|||||||||
7848|Gubberamunda Sandstone|40666|4|Described|p357|||||||||
7848|Gubberamunda Sandstone|40675|6|Mentioned|Table 9A|||||||||
7848|Gubberamunda Sandstone|40687|6|Mentioned|p417|||||||||
7848|Gubberamunda Sandstone|40926|6|Mentioned|p13|||||||||
7848|Gubberamunda Sandstone|41060|6|Mentioned|Fig.3|||||||||
7848|Gubberamunda Sandstone|41064|6|Mentioned|p60|||||||||
7848|Gubberamunda Sandstone|41187|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|41210|5|Briefly described|Fig.3|||||||||
7848|Gubberamunda Sandstone|41216|6|Mentioned|Fig.18|||||||||
7848|Gubberamunda Sandstone|41246|6|Mentioned|Map legend|Jurassic||||||||
7848|Gubberamunda Sandstone|41247|6|Mentioned|Fig.7|||||||||
7848|Gubberamunda Sandstone|41266|6|Mentioned|Fig.3|||||||||
7848|Gubberamunda Sandstone|41681|6|Mentioned|p7|||||||||
7848|Gubberamunda Sandstone|41992|4|Described|Fig.2 P183|||||||||
7848|Gubberamunda Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
7848|Gubberamunda Sandstone|42493|5|Briefly described|p20, Fig. 1 p18|||||||||
7848|Gubberamunda Sandstone|42494|5|Briefly described|Table 1 P24|||||||||
7848|Gubberamunda Sandstone|42634|6|Mentioned|Table 8 P34|||||||||
7848|Gubberamunda Sandstone|42950|6|Mentioned|p41|||||||||
7848|Gubberamunda Sandstone|43000|5|Briefly described|Fig.5,p112|||of Blythesdale Group||||||
7848|Gubberamunda Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
7848|Gubberamunda Sandstone|43404|14|Not recorded|Table p4||Late Jurassic|||||||
7848|Gubberamunda Sandstone|43539|14|Not recorded|p398|||||||||
7848|Gubberamunda Sandstone|43602|6|Mentioned|207|||In Surat Basin||||||
7848|Gubberamunda Sandstone|43982|14|Not recorded|Map Legend||Late Jurassic|||||||
7848|Gubberamunda Sandstone|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
7848|Gubberamunda Sandstone|43991|5|Briefly described|p50|Cretaceous|Jurassic|Part of Blythesdale "Group".||||||
7848|Gubberamunda Sandstone|43994|14|Not recorded|Map Legend|||||||||
7848|Gubberamunda Sandstone|43995|14|Not recorded|p13,57,58,Fig.5|||Part of Blythesdale Group.||||||
7848|Gubberamunda Sandstone|43998|4|Described|p16,map|Cretaceous|Jurassic|||||||
7848|Gubberamunda Sandstone|44021|14|Not recorded|p232-234,236,238|||Ref. to Saltern Creek No.1 Well. At 1750-1850' =Adori Sandstone (not Gubberamunda Sandstone).||||||
7848|Gubberamunda Sandstone|44022|14|Not recorded|Map Legend||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44023|4|Described|Tb.3,p12||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44027|14|Not recorded|p110||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44028|14|Not recorded|Fig.2,p512,513||Jurassic|Equivalent of Pilliga Sandstone. See Strat Table.||||||
7848|Gubberamunda Sandstone|44031|14|Not recorded|p10,11,12||Late Jurassic|Artesian water.||||||
7848|Gubberamunda Sandstone|44088|14|Not recorded|p6|||Possibly equivalent to part of Blythesdale Group?||||||
7848|Gubberamunda Sandstone|44091|14|Not recorded|p57||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44124|14|Not recorded|p1,2,6,10,25|||||||||
7848|Gubberamunda Sandstone|44171|14|Not recorded|p194,197,198|||||||||
7848|Gubberamunda Sandstone|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
7848|Gubberamunda Sandstone|44371|14|Not recorded|Map Legend||Jurassic|||||||
7848|Gubberamunda Sandstone|44375|14|Not recorded|p310|||Aquifer.||||||
7848|Gubberamunda Sandstone|44377|14|Not recorded|p1-5,8,11,22,map||Late Jurassic|Fluviatile (probably Late Jurassic)||||||
7848|Gubberamunda Sandstone|44381|14|Not recorded|p8|||||||||
7848|Gubberamunda Sandstone|44414|14|Not recorded|p114|Cretaceous|Jurassic|||||||
7848|Gubberamunda Sandstone|44415|14|Not recorded|Fig.2,p23|||||||||
7848|Gubberamunda Sandstone|44636|14|Not recorded|p167(Tb)||Late Jurassic|||||||
7848|Gubberamunda Sandstone|44637|14|Not recorded|Table||Jurassic|||||||
7848|Gubberamunda Sandstone|45071|4|Described|Table 15|||||||||
7848|Gubberamunda Sandstone|45110|2|Defined|p99|Late Jurassic|Late Jurassic|See also p24 and Fig.5.||||||18-SEP-18
7848|Gubberamunda Sandstone|46791|6|Mentioned|Fig.2|||||||||
7848|Gubberamunda Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
7848|Gubberamunda Sandstone|46984|6|Mentioned|Table 1|||||||||
7848|Gubberamunda Sandstone|48606|14|Not recorded|p21|||(G/55-12).||||||
7848|Gubberamunda Sandstone|48919|4|Described|p67|||U.Jurassic||||||
7848|Gubberamunda Sandstone|48920|6|Mentioned|Table 7|||Refers Day (1964)||||||
7848|Gubberamunda Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
7848|Gubberamunda Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin.||||||
7848|Gubberamunda Sandstone|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
7848|Gubberamunda Sandstone|61000|5|Briefly described|p186 Fig. 4|Tithonian|Tithonian|Geological Province: Surat Basin.||||||
7848|Gubberamunda Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
7848|Gubberamunda Sandstone|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Late Jurassic|Surat Basin.||||||
7848|Gubberamunda Sandstone|63979|6|Mentioned|p40|Late Jurassic|Late Jurassic|Geological province: Surat Basin.||||||07-FEB-11
7848|Gubberamunda Sandstone|64197|6|Mentioned|p630 Fig.7|Cretaceous|Jurassic|||||Underlies Orallo Formation; overlies Westbourne Formation.||
7848|Gubberamunda Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Late Jurassic|Surat Basin.||||Overlies Westbourne Formation. Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|64856|3|Fully described|p79, p91, p92 Fig.43, p94-95|Tithonian|Tithonian|Surat Basin. Of Day (1964) after Reeves (1947). Type area near Bungil Creek, c.35km N of Roma. Conformably overlies the Westbourne Formation, locally disconformably. Transitionally overlain by Orallo Formation. Age from palynofloral units APJ62, APK1. Max thickness 298m. Virtually uncemented quartzose sandstone.| | ||||29-NOV-17
7848|Gubberamunda Sandstone|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Westbourne Formation, Surat Basin.||||||
7848|Gubberamunda Sandstone|64858|6|Mentioned|p187-188|||Referred to as Gubberamunda Formation on tables and figures.||||||30-NOV-09
7848|Gubberamunda Sandstone|65112|5|Briefly described|p323|Jurassic|Jurassic|||||Overlies Westbourne Formation; underlies Orallo Formation.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
7848|Gubberamunda Sandstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Westbourne Formation, underlies the Orallo.||||||
7848|Gubberamunda Sandstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
7848|Gubberamunda Sandstone|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies the Orallo Formation, Overlies the Westbourne Formation, Surat Basin.||||||
7848|Gubberamunda Sandstone|65117|6|Mentioned|p463|||Surat Basin. Overlies Westbourne Formation. ||||||
7848|Gubberamunda Sandstone|65119|5|Briefly described|Table 1, Fig 7-8, 13-14, 16-19|Late Jurassic|Late Jurassic|Age: 149-153 Ma. Fission Track age: 131+/-11 Ma .Quartzose to clayey lithic sandstone, some conglomerate and siltstone, up to 300m thick. See also Gubberamunda Formation p503, Gubberamunda Siltstone p512||||||07-MAR-12
7848|Gubberamunda Sandstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Injune Creek Group. Is overlain by Southlands and Orallo Formations.||
7848|Gubberamunda Sandstone|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Surat Basin.||||||
7848|Gubberamunda Sandstone|67133|5|Briefly described|p2, p5, p16, p18-21|Late Jurassic|Late Jurassic|16 samples of this unit were analysed by XRD and optical microscopy for this study. Meandering stream deposits. Quartz is the main component (30-90%); feldspars vary (8-28%) with plagioclase always dominant. Kaolinite (up to 30%) is the dominant clay mineral. The small concentrations (only a few percent) of mixed-layer clays are smectite-rich.||||Overlies Westbourne Formation. Is overlain conformably by Orallo Formation.|Medium- to coarse-grained, largely quartzose, poorly sorted sandstone with minor conglomerates and siltstones.|
7848|Gubberamunda Sandstone|67402|4|Described|p146 fig SRT3, p148|Barremian|Tithonian|Surat Basin. Deposited in a braided and meandering stream system. Maximum thickness of 200m. See also p154 fig SRT15/16, p156.||Blythesdale Group||Overlies the Westbourne Formation. Overlain by the Orallo Formation.|Quartzose sandstone with lesser conglomerate, siltstone and mudstone.|
7848|Gubberamunda Sandstone|67669|5|Briefly described|p11|Late Jurassic|Late Jurassic|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Orallo Formation. Underlain by Westbourn Formation.||
7848|Gubberamunda Sandstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||||Overlies Injune Creek Group. Is overlain by Blythesdale Group.||
7848|Gubberamunda Sandstone|68117|6|Mentioned|p346|Early Cretaceous|Late Jurassic|Surat Basin.||||||
7848|Gubberamunda Sandstone|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Tithonian|Surat Basin (QLD).||||Unconformably overlies Westbourne Formation. Is overlain by Orallo Formation|Cross-bedded sandstone.|14-SEP-17
7848|Gubberamunda Sandstone|68139|6|Mentioned|p23|Early Cretaceous|Late Jurassic|Surat Basin.||||Overlies Westbourne Formation. Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Hooray, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
7848|Gubberamunda Sandstone|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Late Jurassic|Surat Basin.||||Unconformably overlies Westbourne Formation (Injune Creek Group). Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|69574|6|Mentioned|p34|Early Cretaceous|Late Jurassic|||||||
7848|Gubberamunda Sandstone|69582|5|Briefly described|p36, p38|Early Cretaceous|Late Jurassic|Surat Basin.||||Unconformably overlies the Westbourne Formation. Overlain by the Orallo Formation.|Sandstone.|
7848|Gubberamunda Sandstone|69594|4|Described|p519, p527, p537, p573|Berriasian|Tithonian|Reeves (1947); Day (1964). Northern Surat Basin. The type section is 35km N of Roma, in Bungil Creek. Generally ~100m thick, up to 298m. Meandering and braided stream deposits.||||Overlies Westbourne Formation conformably (locally disconformably). Is overlain transitionally by Orallo Formation. Equivalent to Hooray Sandstone and parts of Kumbarilla beds.|Quartzose to sublabile sandstone, lesser conglomerate, siltstone, mudstone and claystone.|
7848|Gubberamunda Sandstone|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Late Jurassic|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
7848|Gubberamunda Sandstone|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Overlies Westbourne Formation.||
7848|Gubberamunda Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Late Jurassic|Northern Surat Basin.||||||
7848|Gubberamunda Sandstone|70628|6|Mentioned|p952 fig 4|Kimmeridgian|Kimmeridgian|Shown only as 'Gubberamunda' in fig 4. Along with Springbok Formation, Westbourne [Formation],  forms part of the L-sequence (Hoffman et al 2009) of the Surat Basin.||||Overlies Westbourne Formation.||
7848|Gubberamunda Sandstone|70821|5|Briefly described|p21 Fig.2.6, p80|Early Cretaceous|Jurassic|Surat Basin. Aquifer: generally artesian.||||Overlies Westbourne Formation. Is overlain by Orallo and Southlands Formations.||
7848|Gubberamunda Sandstone|70836|6|Mentioned|p474|Late Jurassic|Late Jurassic|Lightning Ridge area, Surat Basin.||||Is overlain by Orallo Formation.||
7848|Gubberamunda Sandstone|71282|6|Mentioned|p457 Fig.1|||The lithology is omitted in Fig.1.||||||
7848|Gubberamunda Sandstone|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
7848|Gubberamunda Sandstone|72297|6|Mentioned|p761|||Temperatures in its aquifers highlight a broad heat anomaly through the Carpentaria and Eromanga Basins; potential for geothermal energy.||||||
7848|Gubberamunda Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Westbourne FZ (Injune Creek Group). Is overlain by Orallo and Southlands FZs.||
7848|Gubberamunda Sandstone|72921|5|Briefly described|p15 Fig.2, p24.|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in Queensland. Described as a 'shallower aquifer' [presumably than Hutton Sandsotne].||||Unconformably overlies Westbourne Formation and partially underlies Orallo Formation.||
7848|Gubberamunda Sandstone|73113|5|Briefly described|p. 22-24, 31, 36-37, 41, 69, 80, 88...|||Surat Basin. Regional aquifer. More locations: p. 98, 116-117, 119, 123, 129, 146, 151-152, 158, 160, 167, 169-173, 177-178, 191.||||Underlain by Westbourne Formation.||
7848|Gubberamunda Sandstone|73193|6|Mentioned|p369|Berriasian|Tithonian|Surat Basin.||||Unconformably underlain by Westbourne Formation (Injune Creek Group). Overlain by Orallo Formation.||
7860|Gulgong Granite|22728|5|Briefly described|p599 table1||Carboniferous|||||||
7860|Gulgong Granite|23043|5|Briefly described|Map Legend|Visean|Visean|of Gulgong Plutonic Suite.||||||
7860|Gulgong Granite|23170|2|Defined|p270|Carboniferous|Carboniferous|Age: SHRIMP date 325+/- 5 Ma. of Gulgong Plutonic Suite.||||||
7860|Gulgong Granite|24126|5|Briefly described|p4|||||||||
7860|Gulgong Granite|24266|5|Briefly described|p1487|Carboniferous|Carboniferous|Age: ~320 Ma. Geological Province: Lachlan Fold Belt.||||||
7860|Gulgong Granite|29909|6|Mentioned|Table 1|||Carboniferous||||||
7860|Gulgong Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
7860|Gulgong Granite|30329|6|Mentioned|p30|||On table P30||||||
7860|Gulgong Granite|30910|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
7860|Gulgong Granite|31726|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
7860|Gulgong Granite|31993|6|Mentioned|p680|||||||||
7860|Gulgong Granite|32045|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Early to Middle CarboniferousE - M||||||
7860|Gulgong Granite|32047|5|Briefly described|p24|||Mineralization. See also P10||||||
7860|Gulgong Granite|32485|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
7860|Gulgong Granite|32708|6|Mentioned|Fig.1|||||||||
7860|Gulgong Granite|33788|6|Mentioned|p8|||Carboniferous ?||||||
7860|Gulgong Granite|34130|6|Mentioned|p178|||Carboniferous||||||
7860|Gulgong Granite|35065|6|Mentioned|p45|||||||||
7860|Gulgong Granite|35257|6|Mentioned|Fig.24|||||||||
7860|Gulgong Granite|36600|6|Mentioned|Table 1|||||||||
7860|Gulgong Granite|39331|6|Mentioned|Fig.0-3|||See also Fig.7-3||||||
7860|Gulgong Granite|39664|6|Mentioned|p85|||||||||
7860|Gulgong Granite|40328|6|Mentioned|p139|||||||||
7860|Gulgong Granite|42657|5|Briefly described|p73|||||||||
7860|Gulgong Granite|42726|5|Briefly described|map legend|Carboniferous||1.  Of the Gulgong Suite (Bathurst Supersuite).||||||07-FEB-05
7860|Gulgong Granite|43043|5|Briefly described|p103|||age of 312 Ma.||||||
7860|Gulgong Granite|43355|14|Not recorded|Map Legend||Carboniferous|Provisional Edition||||||
7860|Gulgong Granite|43356|14|Not recorded|Map Legend||Carboniferous|||||||
7860|Gulgong Granite|43405|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
7860|Gulgong Granite|43476|14|Not recorded|Map Legend|||(Provisional Edition)||||||
7860|Gulgong Granite|43494|4|Described|p8, p15|Carboniferous|Carboniferous|Consists of two phases - a core of granite (very coarse-grained -quartz, K-feldspar and lesser plagioclase; ) and rim of granodiorite (less coarse with feldspar being the dominant plagioclase and more abundant biotite).   Part is dated as Carboniferous||||||09-MAR-06
7860|Gulgong Granite|43519|14|Not recorded|p118|||||||||
7860|Gulgong Granite|43637|5|Briefly described|p16,18||Late Carboniferous|||||||
7860|Gulgong Granite|66191|6|Mentioned|p484 Fig.1|||Gunnedah Basin||||||
7860|Gulgong Granite|67663|6|Mentioned|p529 Tb.2|||||||||
7860|Gulgong Granite|68003|5|Briefly described|p24 Fig.3-e, p140. |Visean|Tournaisian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Gulgong Plutonic Suite.|||Leucocratic medium- to coarse-grained porphyritic megacrystic granite, minor aplite phases, minor quartz monzonite.|
7860|Gulgong Granite|68004|6|Mentioned|p21.|Early Carboniferous|Early Carboniferous|||||||
7860|Gulgong Granite|73299|6|Mentioned|p1098|Carboniferous|Carboniferous|Tallawang Fault reactivated after intrusion of Gulgong granite, western margin faulted against Ordovician and Devonian rocks.|325 Ma|||||
7863|Gullengumbel Formation|22857|5|Briefly described|p456 App.1 Tb.1A1.6|Devonian|Silurian|Of the Toongi Group. Sandstone, siltstone, shale. Max. thickness: 940m. Geological Province: Cowra Trough.||||||24-MAR-06
7863|Gullengumbel Formation|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Toongi Group.||||||
7863|Gullengumbel Formation|23170|2|Defined|p115|Late Silurian|Late Silurian|of Toongi Group.||||||
7863|Gullengumbel Formation|29986|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
7863|Gullengumbel Formation|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
7863|Gullengumbel Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
7863|Gullengumbel Formation|40328|3|Fully described|p128|||||||||
7863|Gullengumbel Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
7863|Gullengumbel Formation|43500|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition) Part of Toongi Group||||||
7863|Gullengumbel Formation|48958|6|Mentioned|Plate 1|||||||||
7863|Gullengumbel Formation|68003|5|Briefly described|p24 Fig.3-e, p145. |Wenlock|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion. Mis-spelt as Gullemgumble Formation in p24 Fig.3-e. [That and the formal name are both variations of the location Gullengambel Creek].||Unit in Toongi Group.||Is overlain by Gilgal Formation.|Sandstone, siltstone, shale, phyllite, hornfels.|
7872|Gumble Granite|23214|3|Fully described|p207|Middle Devonian|Early Devonian|Of Boggy Plains Supersuite. Intrudes the Kabadah Formation, Cudal, Goonigal and Gregra Groups.  I-Type granite.||||||
7872|Gumble Granite|24007|5|Briefly described|p336|||||||||
7872|Gumble Granite|24233|5|Briefly described|p258 Fig.6|Devonian|Devonian|Geological Province: Lachlan Orogen.||||||
7872|Gumble Granite|24417|5|Briefly described|p94|||Not on FORBES 1:250 000 sheet - probably part of Eugowra Suite.||||||
7872|Gumble Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
7872|Gumble Granite|32986|6|Mentioned|p3|||Metaliferous deposits||||||
7872|Gumble Granite|33006|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Prob.Middle Devonian||||||
7872|Gumble Granite|33282|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
7872|Gumble Granite|33285|6|Mentioned|p21|||||||||
7872|Gumble Granite|35257|6|Mentioned|p145|||||||||
7872|Gumble Granite|39331|6|Mentioned|p64|||See also Fig.7-3||||||
7872|Gumble Granite|39529|6|Mentioned|p27|||||||||
7872|Gumble Granite|40328|4|Described|p207|||||||||
7872|Gumble Granite|40882|6|Mentioned|p27|||Mention Fig.1||||||
7872|Gumble Granite|42384|6|Mentioned|p10|||||||||
7872|Gumble Granite|42726|5|Briefly described|map legend|Early Devonian||413.  Of the Gumble Suite (Boggy Plain Supersuite).||||||08-FEB-05
7872|Gumble Granite|43515|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
7872|Gumble Granite|43516|14|Not recorded|Map Legend||Middle Devonian|||||||
7872|Gumble Granite|43640|5|Briefly described|Map Legend||Devonian|||||||
7872|Gumble Granite|43782|5|Briefly described|Map Legend|Emsian|Emsian|||||||
7872|Gumble Granite|70297|5|Briefly described|map legend, on side 2 of map sheet|Early Devonian|Early Devonian|Minor skarn-type mineralisation adjacent to Gumble Granite. Cowra Trough.||Boggy Plain Supersuite||||
7886|Gundahl Complex|22857|5|Briefly described|p219, p319 Fig.22.10B|Carboniferous|Early Carboniferous|In the Coffs Harbour Block.||||||
7886|Gundahl Complex|22859|5|Briefly described|p220|||||||||
7886|Gundahl Complex|22865|6|Mentioned|Fig22.10bp319||Early Carboniferous|||||||
7886|Gundahl Complex|23811|5|Briefly described|Map Legend|Visean|Tournaisian|Tectonic melange: blocks of metasediment, chert, greenstone, and massive lithic wacke in a sheared argiccaceous matrix; with subordinate gossan, ferruginous chert, breccia, jasper, limestone, and calcareous shales.||||||20-DEC-04
7886|Gundahl Complex|23812|5|Briefly described|p10, p12 Tb.1, p59|Tournaisian|Tournaisian|Faulted to the north against the Silverwood Group, to the south against Cunglebung Creek beds.  Intruded by Dandahra Creek Leucogranite.||||||
7886|Gundahl Complex|39648|4|Described|p258|||||||||
7886|Gundahl Complex|39673|6|Mentioned|p217|||||||||
7886|Gundahl Complex|40108|4|Described|p185|||||||||
7886|Gundahl Complex|40435|6|Mentioned|p47|||||||||
7886|Gundahl Complex|40514|4|Described|p6|||||||||
7886|Gundahl Complex|40787|6|Mentioned|p346|||||||||
7886|Gundahl Complex|40960|6|Mentioned|p219|||||||||
7886|Gundahl Complex|41612|6|Mentioned|p141|||||||||
7886|Gundahl Complex|41822|6|Mentioned|p240|||||||||
7886|Gundahl Complex|42218|5|Briefly described|p397|||||||||
7886|Gundahl Complex|42629|6|Mentioned|p361|||||||||
7886|Gundahl Complex|42719|4|Described|p7|||||||||
7886|Gundahl Complex|42866|5|Briefly described|Table 2, P12|||||||||
7886|Gundahl Complex|42901|5|Briefly described|p412|||see also Fig.11 P411||||||
7886|Gundahl Complex|43745|6|Mentioned|Fig.4,p13|||||||||
7886|Gundahl Complex|60079|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
7886|Gundahl Complex|60937|6|Mentioned|p422|||Represents a classic tectonic melange, typically found in subduction-realted accretionary wedges.||||||
7886|Gundahl Complex|60995|5|Briefly described|p51 Fig. 3|Early Carboniferous|Early Carboniferous|Geological Province: Clarence-Moreton Basin. See also p56 Fig. 7. ||||||
7886|Gundahl Complex|69639|5|Briefly described|p57, p219|||New England Orogen.||||Intruded by the Moonta Gully Monzogranite.||
7886|Gundahl Complex|71628|5|Briefly described|p17: 4, 11; p19: 128, 147|||||Coffs Harbour Asociation.||Is intruded by Dundahra Creek Leucosyenogranite, Moonta Gully and Purgatory Monzogranites and Mann River Leucogranite.|Mudstone, greywacke, greenstones and slate.|
7886|Gundahl Complex|72528|5|Briefly described|p96.|Carboniferous|Devonian|Situated in what is now called the Nymboida National Park.||||Intruded by Mann River Leucogranite.||
7892|Gundangaroo Formation|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Cullen Bullen Subgroup (Illawarra Coal Measures). Thin coal seams, carbonaceous shale, fossil wood horizons, grey shale. Max. thickness: 23.5m. Geological Province: Sydney Basin. ||||||
7892|Gundangaroo Formation|29751|5|Briefly described|p5|||||||||
7892|Gundangaroo Formation|34204|6|Mentioned|Table|||||||||
7892|Gundangaroo Formation|34205|2|Defined|p10|Permian|Permian|Nile Sub-Group||||||
7892|Gundangaroo Formation|34569|6|Mentioned|p10|||Permian. Nile Sub-Group||||||
7892|Gundangaroo Formation|39232|6|Mentioned|Table 1|||||||||
7892|Gundangaroo Formation|39293|6|Mentioned|Fig. 8.2|||||||||
7892|Gundangaroo Formation|40256|6|Mentioned|p305|||Mention Fig.3||||||
7892|Gundangaroo Formation|40806|2|Defined|p151|Permian|Permian|Prob. Permian||||||
7892|Gundangaroo Formation|42657|6|Mentioned|Table 1 P74|||||||||
7892|Gundangaroo Formation|43360|14|Not recorded|Map Legend||Permian|(Provisional first edition)Part of Nile Sub-Group of Illawarra Coal Measures||||||
7892|Gundangaroo Formation|43362|14|Not recorded|Map Legend||Permian|(Provisional first edition)Part of Nile Sub-Group of Illawarra Coal Measures||||||
7892|Gundangaroo Formation|43363|14|Not recorded|Map Legend||Permian|(Provisional first edition)||||||
7892|Gundangaroo Formation|45090|6|Mentioned|p27|||Relationship of rock units||||||
7892|Gundangaroo Formation|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Unit in Nile Subgroup.||Overlies Coorongooba Creek Sandstone. Is overlain by Marrangaroo Formation.||
7899|Gundurimba Clay|22892|6|Mentioned|table9 p69|Quaternary|Quaternary|Age: 120000yrs Bp.||||||
7899|Gundurimba Clay|40726|5|Briefly described|p227|||||||||
7908|Gungoandra Siltstone|22815|2|Defined|p26,27,124, fig10|Llandovery|Llandovery|||||||
7908|Gungoandra Siltstone|22857|4|Described|p420 App.1 Tb. A1.5|Llandovery|Llandovery|Of the Bendoc Group. Distinctive khaki mudrock with faint planar lamination; interbeds of thin siltstone and fine-grained arenite. Max. thickness: 100m.||||||14-NOV-13
7908|Gungoandra Siltstone|42294|5|Briefly described|p24|||Variation on Gungoandra Siltstone Member.||||||
7908|Gungoandra Siltstone|42820|6|Mentioned|p12|||||||||
7908|Gungoandra Siltstone|43233|5|Briefly described|Map Legend||Llandovery|of Bendoc Group.||||||
7908|Gungoandra Siltstone|61413|6|Mentioned|p82 Fig.103.|Early Silurian|Early Silurian|||||Is overlain by Ryrie Formation.||
7908|Gungoandra Siltstone|63290|5|Briefly described|p403, p396 Fig. 3|Llandovery|Llandovery|Of Bendoc Group. Underlain by Warbisco Shale. Consists of poorly graptolitic Llandovery buff-coloured shale, northeast of Cooma.||||||
7908|Gungoandra Siltstone|67322|5|Briefly described|p16|Silurian|Late Ordovician|Modified after Richardson 1975: Gungoandra Siltstone Member; raised to Formation status (Gungoandra Siltstone) by Glen et al. (1990), and defined by Glen (1994). Occurs in the Cooma region. Occurrence of late Llandovery monograptid graptolites in this unit suggests further investigation is necessary.||||Gradationally overlies the Warbisco Shale. Correlative of the Akuna Mudstone.|A distinctive khaki mudrock.|22-FEB-18
7908|Gungoandra Siltstone|71069|5|Briefly described|p72, p74, p75, p77|Llandovery|Llandovery|Estimated to be up to 100m thick. Age derived from graptolite fossils, although Lewis et al. (1994) propose that this may require reassessment.||Bendoc Group||Is equivalent to the Akuna Mudstone, members of the Margules Group and may correlate with the State Circle Shale. Conformably overlain by the Ryrie Formation.|Dominantly khaki mudstone with faint planar laminations and conchoidal fracturing. Minor interbeds of fine grained sandstone that is planar laminated or ripple cross laminated.|
7908|Gungoandra Siltstone|73140|5|Briefly described|p495|Bolindian|Bolindian|Proposed to be reassigned from the Bendoc Group to Margules Group.||Margules Group||Overlies Warbisco Shale||
7913|Gunnee Formation|23050|4|Described|p23 Table 4|Middle Triassic|Early Triassic|In the Warialda Trough. Age: Mega flora indicate a Middle Triassic age.||||||04-JUN-07
7913|Gunnee Formation|23051|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|of Warialda Trough.||||||
7913|Gunnee Formation|23790|5|Briefly described|p10 Fig. 2|Middle Triassic|Middle Triassic|Geological Province: Warialda Trough||||||
7913|Gunnee Formation|36570|2|Defined|p15|Middle Triassic|Middle Triassic|See also p63, Fig.9.Probably Middle Triassic.||||||04-JUN-07
7913|Gunnee Formation|44093|5|Briefly described|p238 App. 1|Triassic|Triassic|Geological Province: New England Fold Belt.||||||
7913|Gunnee Formation|62534|5|Briefly described|p24|Middle Triassic|Early Triassic|Geological province: Warialda Trough.||||||07-FEB-11
7913|Gunnee Formation|63347|5|Briefly described|p5 Fig. 2|Middle Triassic|Middle Triassic|Geological Province: Warialda Trough.||||||
7913|Gunnee Formation|68003|5|Briefly described|p38 Fig.3-j, p43, p54, p128.|Middle Triassic|Middle Triassic|Warialda Trough, Brigalow Belt South Bioregion. Mis-spelt as Gunee Formation in Fig.3-j. Deposited in a high energy valley-fill and braided stream environment.||||Is overlain by Gragin Formation and, unconformably, by Hutton Sandstone.|Interbedded conglomerate and very coarse lithic arenite; very coarse feldspatholithic gravel at the base; grades upwards into labile sandstone, siltstone and carbonaceous mudstone and minor coal.|
7913|Gunnee Formation|68005|6|Mentioned|p170.|Triassic|Triassic|Warialda Trough.||||Is overlain by Gragin Conglomerate.||
7913|Gunnee Formation|68006|6|Mentioned|p91.|||Warialda Trough. Minor coal is reported from this unit.||||||
7913|Gunnee Formation|70036|5|Briefly described|Map legend|Middle Triassic|Middle Triassic|Warialda Trough. Included in a mapped unit of coal measures: conglomerate, arkosic sandstone, siltstone, carbonaceous mudstone and coal.||||||
7913|Gunnee Formation|71628|5|Briefly described|p19:27|Early Triassic|Early Triassic|Stroud (1989, unpublished). Warialda Trough.||||Unconformably overlies Dumboy-Gragin Leucosyenogranite.|Arkosic arenite, with finer-grained interbeds of arenite and argillite.|
7914|Gunnible Formation|29870|6|Mentioned|Table 1|||||||||
7914|Gunnible Formation|30135|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7914|Gunnible Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
7914|Gunnible Formation|31882|5|Briefly described|p245|||||||||
7914|Gunnible Formation|32482|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7914|Gunnible Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
7914|Gunnible Formation|32944|6|Mentioned|p700|||See also P702 & Fig.3||||||
7914|Gunnible Formation|34043|5|Briefly described|p449|||||||||
7914|Gunnible Formation|36940|6|Mentioned|p142|||||||||
7914|Gunnible Formation|39572|6|Mentioned|p141|||||||||15-FEB-10
7914|Gunnible Formation|43407|14|Not recorded|Map Legend||Early Permian|(Provisional Edition)||||||
7914|Gunnible Formation|43408|14|Not recorded|Map Legend|||Limited extent on this sheet||||||
7914|Gunnible Formation|43409|2|Defined|Map Legend||Permian|||||||
7915|Gunning Granite|34544|5|Briefly described|p188|||||||||
7915|Gunning Granite|42726|5|Briefly described|map legend|Silurian||||||||
7915|Gunning Granite|43344|14|Not recorded|p122-124|||Probably Upper Silurian||||||
7915|Gunning Granite|44861|14|Not recorded|p220|||Yass.||||||
7915|Gunning Granite|50232|5|Briefly described|Map legend|Ludlow|Ludlow|Part of the Wyangala Batholith.  Porphyritic hornblende granodiorite with biotite, magnetite, allanite,apatite, zircon, and relict calcic cores in plagioclase; aplite.||||||
7915|Gunning Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Gunning Suite. Grey to cream, med- to coarse-gr., equigran. to porphyritic hornblende-biotite granite, grading to granodiorite in central part, lesser tonalite in E. Dk. grey ovoid micrdioritic enclaves+clots occur throughout. Strongly schistose...||||||12-JUN-08
7915|Gunning Granite|66300|5|Briefly described|p92.|||I-type.|428.6 +/- 2.4 Ma.|Unit in Gunning Suite.||||
7915|Gunning Granite|68592|2|Defined|p279, p291, p294, p1312-21, p1323-30|Early Silurian|Early Silurian|See also p83-4, p98-9, p231, p257-9, p269-70, p277. Vallance (in Packham, 1969). after the town of Gunning. Now includes the Cullerin Granite of Chappell et al. (1991) with which it is continuous. Remains the type pluton for the redefined Gunning Suite. Type section detailed. Geochemistry and geophysical properties detailed. SHRIMP U-Pb zircon age. Crops out as large boulders and tors in undulating countryside with scattered low rounded hills. Lithologies detailed. Hosts only minor mineral occurrences. Two quarries used to extract dimension stone. There is potential for renewed quarrying.|428.6 +/- 2.4 Ma (Bodorkos and Simpson, 2008).|Unit in Gunning Suite.||Intrudes Abercrombie Formation and ?Mulgowrie Granodiorite. Is overlain nonconformably by Crookwell Basalt.|Medium- to coarse-grained, equigranular to porphyritic, massive to foliated granite, aplitic granite, granodiorite and tonalite. Ovoid microgranitic enclaves and irregular more mafic clots are abundant throughout.|
7915|Gunning Granite|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sgu. Includes two unnamed units of: subaplitic granite and aplite; leucocratic, biotite granite with miarolitic cavities. On Crookwell and Gunning 1:100 000 mapsheet portions of Time-Space Plot.||Gunning Suite|Includes two unnamed units.||Medium-coarse grained, equigranular to porphyritic, hornblende-biotite granite, granodiorite and lesser tonalite; dark grey ovoid microdioritic enclaves and clots; granite is strongly schistose along the eastern margin.|
7915|Gunning Granite|70541|4|Described|Map Legend|Devonian|Silurian|Includes two unnamed mapped members: fine to medium grained equigranular to porphyritic subaplitic granite and aplite; medium grained, equigranular to porphyritic, leucocratic biotite granite with miarolitic cavities. High Th and K, medium to high U response.||Gunning Suite|Includes two unnamed subunits.||Grey to cream, medium to coarse grained equigranular to porphyritic, hornblende biotite granite, granodiorite and lesser tonalite; dark grey ovoid microdioritic enclaves and clots; granite is strongly schistose along the eastern margin.|
7915|Gunning Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Gunning Suite|||Medium-coarse grained, equigranular to porphyritic, hornblende-biotite granite, granodiorite and lesser tonalite; dark grey ovoid microdioritic enclaves and clots; granite is strongly schistose along the eastern margin.|
7925|Gurnang Porphyry|32999|3|Fully described|p48|||Structural relationships||||||
7927|Gurrangorambla Granophyre|23548|5|Briefly described|p533.|||||||||
7927|Gurrangorambla Granophyre|29456|6|Mentioned|p424|||||||||
7927|Gurrangorambla Granophyre|36050|6|Mentioned|p399|||||||||
7927|Gurrangorambla Granophyre|36443|5|Briefly described|map legend|Lochkovian|Lochkovian|Of Boggy Plain I-type Suite. Intrusive. Granophyre. BMR map code: Dlg.||||||
7927|Gurrangorambla Granophyre|40328|4|Described|p207|||||||||
7927|Gurrangorambla Granophyre|40882|6|Mentioned|Fig.1|||||||||
7927|Gurrangorambla Granophyre|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|glp5||||||
7927|Gurrangorambla Granophyre|45147|2|Defined|M265|Early Devonian|Early Devonian|Refers Stevens(1958)||||||
7927|Gurrangorambla Granophyre|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
7927|Gurrangorambla Granophyre|68592|6|Mentioned|p1411|||Is very similar mineralogically and chemically to Burrinjuck Granite.||Unit in Boggy Plain Supersuite.||||
7980|Hallett Coal Member|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
7980|Hallett Coal Member|40331|6|Mentioned|p14|||||||||
7980|Hallett Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Rowan Formation. ||||
7986|Halls Creek Arenite|42631|5|Briefly described|Fig.1 P265|Permian||Invalid name. Halls Creek Group etc., WA and NT has precedence.||||||25-SEP-06
7997|Hambledon Hill Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Pinegrove Formation. Geological Province: Sydney Basin||||||
7997|Hambledon Hill Member|29942|4|Described|Fig.2|||Permian||||||
8022|Hampden Member|33476|6|Mentioned|Table 4|||||||||
8022|Hampden Member|39279|4|Described|p370|||||||||
8022|Hampden Member|40505|6|Mentioned|p83|||||||||
8022|Hampden Member|40773|3|Fully described|p451|||||||||
8022|Hampden Member|42378|6|Mentioned|Table 1 P10|||||||||
8032|Hampton Granite|42726|5|Briefly described|map legend|Carboniferous||28.||||||
8050|Hanover Formation|22857|4|Described|p456 App.1 Tb.A1.6|Ludlovian|Ludlovian|Of the Cudal Group. Massive greenish-buff and purple siltstone, interbedded cherts and slates; one horizon interfingers with Canowindra Volcanics. Max. thickness: >300m. Geological Province: Cowra Trough. ||||||
8050|Hanover Formation|23043|5|Briefly described|Map Legend|Lochkovian|Wenlock|of Cudal Group.||||||
8050|Hanover Formation|23170|2|Defined|p105|Pridoli|Wenlock|of Cudal Group.||||||
8050|Hanover Formation|23213|6|Mentioned|p22|||Sourges Shale faulted against it south east of Brookvale homestead.||||||
8050|Hanover Formation|24126|5|Briefly described|p158|||||||||
8050|Hanover Formation|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
8050|Hanover Formation|32046|6|Mentioned|p181|||||||||
8050|Hanover Formation|32485|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
8050|Hanover Formation|40328|3|Fully described|p81|||||||||
8050|Hanover Formation|43476|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition) Middle Silurian||||||
8050|Hanover Formation|43494|3|Fully described|p20-21||Ludlovian|Of the Cudal Group. Consists of greenish buff almost massive siltstone with some purple siltstone and chert near base. Conformably overlies Canowindra Volcanics. Intruded by Yeoval Batholith.  Thickness: 230m+ (est.)||||||01-OCT-09
8050|Hanover Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Cudal Group.  Massive siltstone, shale and minor chert. Rhyolite.||||||
8050|Hanover Formation|60987|4|Described|p153,p155,p157-158,p160,p162,p164-165|Late Silurian|Late Silurian|Term introduced by Maggs (1963) and first published by Offenberg et al. (1971). Included in the Cudal Group by Bradley (in Pickett, 1982). Cumnock area, Cowra Trough, Lachlan Fold Belt. Crops out in meridional fold and fault repetitions. Thickness estimated at 300m. Documents the first Silurian graptolites from this unit. Graptolites described in detail.||Cudal Group.||Conformably overlies the Canowindra Volcanics. Overlain either by the Cuga Burga Volcanics or their lateral equivalent, the Berkley Formation.|Dominantly shale and siltstone; subordinate interbedded fine- to coarse-grained volcaniclastic sandstone, radiolarian chert, marly siltstone and detrital calcareous horizons.|
8050|Hanover Formation|66197|5|Briefly described|p633 Fig.4c|Pridoli|Wenlock|Cowra Trough-Molong High, deep marine shale, overlies the Canowindra Volcanics||||||
8050|Hanover Formation|68003|5|Briefly described|p24 Fig.3-e, p145. |Pridoli|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Cudal Group.|||Massive to laminated, buff to grey to green to purple, quartzose micaceous shale, siltstone, fine-grained sandstone; rhyolitic tuff, tuffaceous sandstone; minor latitic sandstone and breccia.|
8050|Hanover Formation|71600|6|Mentioned|p23 Fig 1|Silurian|Silurian|Geological province: Lachlan Fold Belt.||Unit of Cudal Group.||||
8050|Hanover Formation|73299|6|Mentioned|p1105|||Cowra Trough. [Map symbol suggests Silurian age]||||||
8051|Hanrahan Agglomerate Member|29903|5|Briefly described|p169|||||||||
8074|Harden basalt|35070|6|Mentioned|p136|||Reference Curran 1891||||||
8089|Hargrave Coal Member|24471|5|Briefly described|p31 Fig.3|Late Permian|Late Permian|Within Eckersley Formation.Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
8089|Hargrave Coal Member|29900|6|Mentioned|Table 2|||||||||
8089|Hargrave Coal Member|29901|4|Described|Table 1|||||||||
8089|Hargrave Coal Member|30006|6|Mentioned|p5|||||||||
8089|Hargrave Coal Member|31128|6|Mentioned|Table 1|||||||||
8089|Hargrave Coal Member|32849|6|Mentioned|Table 1|||Permian||||||
8089|Hargrave Coal Member|36220|6|Mentioned|p50|||See also Table 1 & P50.||||||
8089|Hargrave Coal Member|36593|6|Mentioned|Table 2|||||||||
8089|Hargrave Coal Member|37089|6|Mentioned|p208|||||||||
8089|Hargrave Coal Member|39661|6|Mentioned|Fig.1|||||||||
8089|Hargrave Coal Member|42787|6|Mentioned|Table 1 P126|||||||||
8089|Hargrave Coal Member|42896|5|Briefly described|p23|||of Eckersley Formation||||||
8112|Hartley Hill Coal|22578|6|Mentioned|Fig.9 p399, p402|||||||||
8112|Hartley Hill Coal|23055|6|Mentioned|p22|||||||||
8112|Hartley Hill Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Boolaroo Formation. Geological Province: Sydney Basin||||||
8112|Hartley Hill Coal|39308|6|Mentioned|Fig.23.4|||||||||
8112|Hartley Hill Coal|39609|6|Mentioned|Table 1|||||||||
8112|Hartley Hill Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Hartley Hill coal seam instead. See also p113.||Of Boolaroo Subgroup||||
8112|Hartley Hill Coal|73304|6|Mentioned|p75|||||Boolaroo Formation, Newcastle Coal Measures||||
8114|Hartley Hill coal seam|22857|6|Mentioned|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Informal reference to a seam within the Boolaroo Formation (Newcastle Coal Measures). ||||||
8114|Hartley Hill coal seam|23055|6|Mentioned|Fig11p23|||||||||
8114|Hartley Hill coal seam|29687|6|Mentioned|p18|||||||||
8114|Hartley Hill coal seam|68711|4|Described|p117, p118, p116 Tbl 2|||Informal unit. Variously defined over the years and sometimes correlated with the Australasian Coal seam. The definition of Bewley and Crapp (1972), after Jones (1929) is used here, where the seam overlies and is separated from the Australasian seam by a characteristic tuffaceous bed (Warners Bay Tuff).||Within Boolaroo Formation||||
8116|Hartley Vale Claystone Member|22745|6|Mentioned|p127|||Sydney Basin.||||||
8116|Hartley Vale Claystone Member|31373|6|Mentioned|Table 1|||||||||
8116|Hartley Vale Claystone Member|33683|6|Mentioned|Table 1|||Narrabeen Gp.||||||
8116|Hartley Vale Claystone Member|33685|6|Mentioned|Table 2|||||||||
8116|Hartley Vale Claystone Member|34205|2|Defined|p23|Triassic|Triassic|||||||
8116|Hartley Vale Claystone Member|34209|6|Mentioned|Table 1|||See also P141. Triassic.||||||
8116|Hartley Vale Claystone Member|39293|5|Briefly described|p144|||See also Fig.8.2||||||
8116|Hartley Vale Claystone Member|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
8116|Hartley Vale Claystone Member|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)Part of Caley Formation of Narrabeen Group||||||
8116|Hartley Vale Claystone Member|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
8145|Hattons Corner Group|22768|5|Briefly described|p176|Lochkovian|Ludlow|||||||
8145|Hattons Corner Group|22857|5|Briefly described|p176, p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Strongly fossiliferous unit. Geological Province: Canberra-Yass Shelf.||||||
8145|Hattons Corner Group|30069|5|Briefly described|p5|||||||||
8145|Hattons Corner Group|30332|6|Mentioned|Table 1|||Refers to Link(1971)||||||
8145|Hattons Corner Group|31852|5|Briefly described|p711|||See also P715,718,719,720. Ludlovian||||||
8145|Hattons Corner Group|31918|6|Mentioned|Table 5|||||||||
8145|Hattons Corner Group|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
8145|Hattons Corner Group|32672|6|Mentioned|p672|||||||||
8145|Hattons Corner Group|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Strat. Nomenclature||||||
8145|Hattons Corner Group|32820|6|Mentioned|Table 1|||Refers Pogson & Baker (1974)||||||
8145|Hattons Corner Group|33325|5|Briefly described|Table 2|||See also Table 3.||||||
8145|Hattons Corner Group|33606|6|Mentioned|p64|||||||||
8145|Hattons Corner Group|33611|6|Mentioned|p131|||||||||
8145|Hattons Corner Group|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
8145|Hattons Corner Group|35386|3|Fully described|p25|||Age discussed p40||||||12-JAN-17
8145|Hattons Corner Group|36411|6|Mentioned|p269|||Refs Cramsie et al 1978 for redefinition.||||||
8145|Hattons Corner Group|36413|6|Mentioned|Table 3|||||||||
8145|Hattons Corner Group|37727|6|Mentioned|p62|||||||||
8145|Hattons Corner Group|38151|6|Mentioned|Table 1|||||||||
8145|Hattons Corner Group|39331|6|Mentioned|Fig.5-5|||||||||
8145|Hattons Corner Group|40328|4|Described|p108|||||||||
8145|Hattons Corner Group|45075|4|Described|p6|||Fauna||||||
8145|Hattons Corner Group|45147|6|Mentioned|M150|||See also M152||||||
8145|Hattons Corner Group|50230|5|Briefly described|Map legend|Late Silurian|Late Silurian|||||||
8145|Hattons Corner Group|64238|5|Briefly described|Map legend|Silurian|Silurian|Includes Silverdale Formation, Rosebank Shale, Elmside Formation, Cowridge Siltstone and Black Bog Shale.||||||
8145|Hattons Corner Group|66197|5|Briefly described|p632, p631 Fig.3b|Lochkovian|Ludlow|Canberra-Yass Basin. Deep marine shale from the upper Ludlow upwards (shallow marine limestone below). Overlies the Silverdale Formation.||||||13-MAR-12
8145|Hattons Corner Group|67820|5|Briefly described|p133, p136 Fig.3|Lochkovian|Ludlow||||Elmside, Silverdale Formations; Cowridge Siltstone; Rosebank, Black Bog Shales.||Includes shale.|
8145|Hattons Corner Group|68592|1|Redefined|p456, p514, p524, p559-606, p744, p772|Lochkovian|Ludlow|See also p73 Tb.5, p111-2, p427, p429-30 Fig.89, p442. Redefined. Link (1970, 1971); Link and Druce (1972); numerous changes since. The development of the complicated stratigraphy of this unit is displayed in Fig.89, but note that the top and bottom boundaries of the Group are wrongly shown in this figure. Representative section described. c.500m thick. Yass structural zone: deformation described.|||Includes Silverdale and Elmside Formations; Black Bog and Rosebank Shales; Cowridge Siltstone.|Overlies Yanawe Formation (Douro Group) conformably. Is overlain unconformably by Black Range Group.|Hemipelagic, calcareous and non-calcareous mudstone, siltstone, shale, limestone; minor sandstone.|12-JAN-17
8145|Hattons Corner Group|70192|5|Briefly described|Map Legend|Lochkovian|Ludlow|On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.|||Includes Black Bog Shale, Cowridge Siltstone, Elmside Formation, Rosebank Shale, Silverdale Formation.|Overlies Douro Group.||
8145|Hattons Corner Group|70540|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Black Bog Shale, Cowridge Siltstone, Elmside Formation, Rosebank Shale, Silverdale Formation.|||
8145|Hattons Corner Group|70546|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Black Bog Shale, Cowridge Siltstone, Elmside Formation, Rosebank Shale, Silverdale Formation|||
8145|Hattons Corner Group|71069|6|Mentioned|p146||||||Includes the Black Bog Shale|||
8145|Hattons Corner Group|71656|4|Described|p10 Fig.1 , p12 Fig.2, p23-27|Lochkovian|Ludlow|Includes richly fosiliferous strata that with examples of brachiopods, conodonts, graptolites, rugose and tabulate corals, pentamerides, sponges, crinoids, nautiloids, bryazoan and bivalves.|||Elmside Formation,  Cowridge Siltstone, Rosebank Shale, Black Bog Shale, Silverdale Formation.|Overlies Douro Group.|Fossiliferous limestone, shale and siltstone.|
8145|Hattons Corner Group|71700|5|Briefly described|p24|Early Devonian|Late Silurian|Yass Basin, Goulburn 250k map sheet. This unit is analagous to the Bungonia Group.||||||
8145|Hattons Corner Group|73215|5|Briefly described|p994-995|||Yass Syncline.|||Elmside Formation, Bowspring Limestone Member.|Overlies Yanawe Formation. Is overlain by Pilleuil Andesite and, unconformably, by Black Range Group.||
8145|Hattons Corner Group|73582|5|Briefly described|p112|||Yass district. Mentioned as age-equivalent to Jenolan Caves Limestone.|||Silverdale Formation|||
8157|Havilah Granite|22529|5|Briefly described|1|||||||||
8157|Havilah Granite|22545|6|Mentioned|p499,504, Fig.2||Carboniferous|||||||
8157|Havilah Granite|23043|5|Briefly described|Map Legend|Namurian|Visean|||||||
8157|Havilah Granite|23170|2|Defined|p278|Carboniferous|Carboniferous|Age: Middle Carboniferous.||||||
8157|Havilah Granite|24126|6|Mentioned|p292|||||||||
8157|Havilah Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
8157|Havilah Granite|32045|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
8157|Havilah Granite|32046|6|Mentioned|p169|||||||||
8157|Havilah Granite|32485|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
8157|Havilah Granite|42726|5|Briefly described|map legend|Carboniferous||3.  Of the Gulgong Suite (Bathurst Supersuite).||||||07-FEB-05
8157|Havilah Granite|43188|5|Briefly described|Fig.2 p197||Carboniferous|Accidental formalization of Havilah granite?||||||
8157|Havilah Granite|43476|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
8165|Hawkesbury Sandstone|22447|4|Described|p624, Fig.1 p624||Middle Triassic|Fluvial quartzose||||||
8165|Hawkesbury Sandstone|22549|6|Mentioned|p526||Middle Triassic|||||||
8165|Hawkesbury Sandstone|22594|6|Mentioned|p148||Triassic|||||||
8165|Hawkesbury Sandstone|22607|6|Mentioned|p 57|||||||||
8165|Hawkesbury Sandstone|22608|4|Described|p 65, 66||Middle Triassic|Maximum thickness 250m||||||
8165|Hawkesbury Sandstone|22663|6|Mentioned|NSW97 - 1 p2|||||||||
8165|Hawkesbury Sandstone|22731|6|Mentioned|p536|||||||||
8165|Hawkesbury Sandstone|22745|5|Briefly described|p125|Anisian|Anisian|Sydney Basin. 250 m.||||||
8165|Hawkesbury Sandstone|22749|5|Briefly described|p185,Table1p187|||||||||
8165|Hawkesbury Sandstone|22833|6|Mentioned|p653|||of Sydney Basin.||||||
8165|Hawkesbury Sandstone|22857|4|Described|p265, p520 App.1 Tb.A1.9|Middle Triassic|Middle Triassic|Fluvial deposits - massive-bedded, crossbedded and horizontally bedded quartz sandstone; minor siltstone and shale. Max. thickness: 278m. Geological Province: Sydney Basin. See also pages 524 and 530 of App.1 Tb.A1.9.||||||
8165|Hawkesbury Sandstone|22864|5|Briefly described|p265|||||||||
8165|Hawkesbury Sandstone|22892|5|Briefly described|p7 fig6||Triassic|||||||
8165|Hawkesbury Sandstone|22934|6|Mentioned|p374|||||||||
8165|Hawkesbury Sandstone|22938|6|Mentioned|p234,237-239|||Numerous mentions.||||||
8165|Hawkesbury Sandstone|22943|6|Mentioned|p509-10,517||Triassic|||||||
8165|Hawkesbury Sandstone|22969|4|Described|p 6, 26||Early Triassic|||||||
8165|Hawkesbury Sandstone|22970|5|Briefly described|Plate 6||Triassic|||||||
8165|Hawkesbury Sandstone|23013|6|Mentioned|p326|||||||||
8165|Hawkesbury Sandstone|23015|6|Mentioned|p319|||||||||
8165|Hawkesbury Sandstone|23218|5|Briefly described|Diagram p4, Map. p17, 28|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|23256|6|Mentioned|p50|||Geographically and stratigraphically close to Narrabeen Sandstone.||||||
8165|Hawkesbury Sandstone|23275|6|Mentioned|p466, 468, 472||Triassic|||||||
8165|Hawkesbury Sandstone|23349|5|Briefly described|247|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|23436|5|Briefly described|p46|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|23450|6|Mentioned|p527 Fig.1|||||||||
8165|Hawkesbury Sandstone|23540|5|Briefly described|Fig 1 p 418|||||||||
8165|Hawkesbury Sandstone|23881|5|Briefly described|p69 Fig. 7.2|||Geological Province: Sydney Basin.||||||
8165|Hawkesbury Sandstone|24079|5|Briefly described|p433|Triassic|Triassic|Geological Province: Sydney Basin. Maximum thickness: 240m.||||||
8165|Hawkesbury Sandstone|24117|5|Briefly described|p3|||Geological Basin: Sydney Basin.||||||
8165|Hawkesbury Sandstone|24123|5|Briefly described|p3|||Geological Province: Sydney Basin.||||||
8165|Hawkesbury Sandstone|24129|5|Briefly described|p4|||||||||
8165|Hawkesbury Sandstone|24342|5|Briefly described|p51|||Underlying unit: Narrabeen Group. Geological Province: Sydney Basin.||||||
8165|Hawkesbury Sandstone|24343|6|Mentioned|p63, p65 Fig. 2|||||||||
8165|Hawkesbury Sandstone|24471|5|Briefly described|p29 Fig.2|Triassic|Triassic|Overlies Narrabeen Group. Geological Province: Sydney Basin.||||||07-FEB-11
8165|Hawkesbury Sandstone|24478|5|Briefly described|p14-15|Triassic|Triassic|Overlain by Wianamatta Group.||||||
8165|Hawkesbury Sandstone|27476|14|Not recorded|?|||||||||
8165|Hawkesbury Sandstone|27526|14|Not recorded|?|||||||||
8165|Hawkesbury Sandstone|29360|6|Mentioned|p42|||Foundations.||||||
8165|Hawkesbury Sandstone|29361|5|Briefly described|p4|||||||||
8165|Hawkesbury Sandstone|29376|6|Mentioned|p435|||||||||
8165|Hawkesbury Sandstone|29448|6|Mentioned|p117|||||||||
8165|Hawkesbury Sandstone|29591|5|Briefly described|p97|||||||||
8165|Hawkesbury Sandstone|29745|6|Mentioned|p7|||||||||
8165|Hawkesbury Sandstone|29752|6|Mentioned|p30|||||||||
8165|Hawkesbury Sandstone|29869|6|Mentioned|p37|||||||||
8165|Hawkesbury Sandstone|29901|4|Described|Table 1|||||||||
8165|Hawkesbury Sandstone|29918|6|Mentioned|p17|||||||||
8165|Hawkesbury Sandstone|29920|6|Mentioned|p14|||||||||
8165|Hawkesbury Sandstone|29924|6|Mentioned|p13|||||||||
8165|Hawkesbury Sandstone|30006|4|Described|p65|||||||||
8165|Hawkesbury Sandstone|30007|6|Mentioned|p61|||||||||
8165|Hawkesbury Sandstone|30109|6|Mentioned|Fig.1|||Triassic age.||||||
8165|Hawkesbury Sandstone|30132|4|Described|p3|||||||||
8165|Hawkesbury Sandstone|30223|4|Described|p275|||Refers depositional model||||||
8165|Hawkesbury Sandstone|30228|6|Mentioned|p17|||Lithology. Triassic age.||||||
8165|Hawkesbury Sandstone|30229|4|Described|p2020|||||||||
8165|Hawkesbury Sandstone|30285|6|Mentioned|p546|||Fossil horizons described||||||
8165|Hawkesbury Sandstone|30286|6|Mentioned|p1099|||Stratigraphy||||||
8165|Hawkesbury Sandstone|30455|6|Mentioned|p12|||Triassic age||||||
8165|Hawkesbury Sandstone|30460|6|Mentioned|p12|||||||||
8165|Hawkesbury Sandstone|30465|6|Mentioned|p5|||||||||
8165|Hawkesbury Sandstone|30466|6|Mentioned|p5|||Triassic age||||||
8165|Hawkesbury Sandstone|30547|6|Mentioned|p427|||Correlation||||||
8165|Hawkesbury Sandstone|30555|6|Mentioned|p296|||||||||
8165|Hawkesbury Sandstone|30565|6|Mentioned|p135|||||||||
8165|Hawkesbury Sandstone|30610|6|Mentioned|p326|||Refers Helby (1966)||||||
8165|Hawkesbury Sandstone|30707|6|Mentioned|p5|||See also Table 1 & Fig.2||||||
8165|Hawkesbury Sandstone|30716|6|Mentioned|p930|||||||||
8165|Hawkesbury Sandstone|31057|6|Mentioned|p2|||See also P8 re potential use.||||||
8165|Hawkesbury Sandstone|31061|6|Mentioned|Table 1|||||||||
8165|Hawkesbury Sandstone|31062|6|Mentioned|p478|||Triassic. On Table||||||
8165|Hawkesbury Sandstone|31126|6|Mentioned|p19|||||||||
8165|Hawkesbury Sandstone|31128|5|Briefly described|p7|||See also P3.||||||
8165|Hawkesbury Sandstone|31156|6|Mentioned|p9|||Refers residual sand.||||||
8165|Hawkesbury Sandstone|31276|6|Mentioned|p141|||Microflora||||||
8165|Hawkesbury Sandstone|31296|6|Mentioned|p29|||Overlain by Wianamatta Gp.||||||
8165|Hawkesbury Sandstone|31297|6|Mentioned|p6|||||||||
8165|Hawkesbury Sandstone|31426|4|Described|p65|||Triassic||||||
8165|Hawkesbury Sandstone|31544|6|Mentioned|p405|||||||||
8165|Hawkesbury Sandstone|31552|5|Briefly described|p105|||Lithology||||||
8165|Hawkesbury Sandstone|31613|6|Mentioned|Fig. 19|||||||||
8165|Hawkesbury Sandstone|31725|4|Described|p11|||See also P6||||||
8165|Hawkesbury Sandstone|31740|6|Mentioned|p11|||||||||
8165|Hawkesbury Sandstone|31855|6|Mentioned|p14|||Stratigraphic table||||||
8165|Hawkesbury Sandstone|31878|6|Mentioned|Table 1|||||||||
8165|Hawkesbury Sandstone|31879|5|Briefly described|p294|||Triassic||||||
8165|Hawkesbury Sandstone|31884|6|Mentioned|Table 1|||Triassic||||||
8165|Hawkesbury Sandstone|31885|6|Mentioned|Table 1|||||||||
8165|Hawkesbury Sandstone|31886|6|Mentioned|p394|||||||||
8165|Hawkesbury Sandstone|31887|5|Briefly described|p8|||||||||
8165|Hawkesbury Sandstone|31890|6|Mentioned|p77|||Stratigraphy||||||
8165|Hawkesbury Sandstone|31947|6|Mentioned|p28|||||||||
8165|Hawkesbury Sandstone|32101|6|Mentioned|p107|||Depositional environment||||||
8165|Hawkesbury Sandstone|32135|6|Mentioned|p1056|||||||||
8165|Hawkesbury Sandstone|32136|6|Mentioned|p7|||Miospores||||||
8165|Hawkesbury Sandstone|32168|6|Mentioned|p49|||||||||
8165|Hawkesbury Sandstone|32187|5|Briefly described|p4|||||||||
8165|Hawkesbury Sandstone|32266|6|Mentioned|p24|||||||||
8165|Hawkesbury Sandstone|32315|6|Mentioned|p5|||||||||
8165|Hawkesbury Sandstone|32537|4|Described|p7|||Description of sediments||||||
8165|Hawkesbury Sandstone|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|32672|6|Mentioned|p675|||||||||
8165|Hawkesbury Sandstone|32719|6|Mentioned|p209|||Equivalent. Section||||||
8165|Hawkesbury Sandstone|32799|6|Mentioned|p9|||||||||
8165|Hawkesbury Sandstone|32800|6|Mentioned|p384|||||||||
8165|Hawkesbury Sandstone|32801|6|Mentioned|p256|||||||||
8165|Hawkesbury Sandstone|32802|6|Mentioned|p19|||See also P32||||||
8165|Hawkesbury Sandstone|32803|6|Mentioned|p83|||||||||
8165|Hawkesbury Sandstone|32938|6|Mentioned|p67|||Geology||||||
8165|Hawkesbury Sandstone|33129|6|Mentioned|Table 1|||Refers Packham (1969)||||||
8165|Hawkesbury Sandstone|33131|6|Mentioned|Fig.9|||||||||
8165|Hawkesbury Sandstone|33334|6|Mentioned|p6|||Triassic||||||
8165|Hawkesbury Sandstone|33583|6|Mentioned|p3|||||||||
8165|Hawkesbury Sandstone|33671|6|Mentioned|p3|||||||||
8165|Hawkesbury Sandstone|33683|6|Mentioned|p77|||Triassic||||||
8165|Hawkesbury Sandstone|33684|4|Described|p27|||||||||
8165|Hawkesbury Sandstone|33685|6|Mentioned|Table 1|||Triassic.||||||
8165|Hawkesbury Sandstone|33709|6|Mentioned|p103|||||||||
8165|Hawkesbury Sandstone|33867|4|Described|p12|||Mention Fig.1||||||
8165|Hawkesbury Sandstone|33872|6|Mentioned|Fig.1|||||||||
8165|Hawkesbury Sandstone|33930|6|Mentioned|p15|||||||||
8165|Hawkesbury Sandstone|33985|6|Mentioned|p100|||||||||
8165|Hawkesbury Sandstone|33988|6|Mentioned|p47|||||||||
8165|Hawkesbury Sandstone|34010|6|Mentioned|Cor. chart|||L - M Triassic||||||
8165|Hawkesbury Sandstone|34032|6|Mentioned|p37|||||||||
8165|Hawkesbury Sandstone|34034|6|Mentioned|p555|||||||||
8165|Hawkesbury Sandstone|34037|6|Mentioned|Table 5.27|||||||||
8165|Hawkesbury Sandstone|34039|6|Mentioned|p355|||||||||
8165|Hawkesbury Sandstone|34041|4|Described|p415|||||||||
8165|Hawkesbury Sandstone|34045|6|Mentioned|p444|||||||||
8165|Hawkesbury Sandstone|34059|6|Mentioned|Map legend|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|34106|6|Mentioned|p401|||||||||
8165|Hawkesbury Sandstone|34107|3|Fully described|p218|||Triassic||||||
8165|Hawkesbury Sandstone|34139|6|Mentioned|p23|||Table||||||
8165|Hawkesbury Sandstone|34140|6|Mentioned|p45|||||||||
8165|Hawkesbury Sandstone|34141|6|Mentioned|p8|||Triassic||||||
8165|Hawkesbury Sandstone|34158|6|Mentioned|p400|||||||||
8165|Hawkesbury Sandstone|34167|6|Mentioned|p64|||Triassic||||||
8165|Hawkesbury Sandstone|34172|6|Mentioned|p53|||||||||
8165|Hawkesbury Sandstone|34205|4|Described|p33|||||||||
8165|Hawkesbury Sandstone|34209|5|Briefly described|p137|||Triassic. See also PP144,148.||||||
8165|Hawkesbury Sandstone|34224|6|Mentioned|p21|||Refers Culey (1933, 1939)||||||
8165|Hawkesbury Sandstone|34228|6|Mentioned|p170|||||||||
8165|Hawkesbury Sandstone|34236|6|Mentioned|p17|||||||||
8165|Hawkesbury Sandstone|34240|6|Mentioned|p395|||Triassic. See also P396||||||
8165|Hawkesbury Sandstone|34241|6|Mentioned|p404|||||||||
8165|Hawkesbury Sandstone|34242|6|Mentioned|p417|||Microfossils||||||
8165|Hawkesbury Sandstone|34254|6|Mentioned|p488|||||||||
8165|Hawkesbury Sandstone|34283|6|Mentioned|p577|||Geomorphology||||||
8165|Hawkesbury Sandstone|34287|6|Mentioned|p154|||See also PP155, 161. Triassic||||||
8165|Hawkesbury Sandstone|34301|6|Mentioned|p403|||||||||
8165|Hawkesbury Sandstone|34305|6|Mentioned|Table 5.26|||||||||
8165|Hawkesbury Sandstone|34306|4|Described|p443|||Lithology||||||
8165|Hawkesbury Sandstone|34328|6|Mentioned|p68|||||||||
8165|Hawkesbury Sandstone|34331|6|Mentioned|p457|||||||||
8165|Hawkesbury Sandstone|34336|6|Mentioned|Fig.5.33|||Comparitive sections.||||||
8165|Hawkesbury Sandstone|34337|6|Mentioned|Table 5.18|||||||||
8165|Hawkesbury Sandstone|34338|6|Mentioned|p400|||||||||
8165|Hawkesbury Sandstone|34339|6|Mentioned|p439|||Appears to overlap Narrabeen Group.||||||
8165|Hawkesbury Sandstone|34340|6|Mentioned|p471|||||||||
8165|Hawkesbury Sandstone|34399|6|Mentioned|p312|||||||||
8165|Hawkesbury Sandstone|34400|5|Briefly described|p13|||||||||
8165|Hawkesbury Sandstone|34425|6|Mentioned|p40|||||||||
8165|Hawkesbury Sandstone|34429|6|Mentioned|p63|||||||||
8165|Hawkesbury Sandstone|34434|6|Mentioned|Fig.5.25|||||||||
8165|Hawkesbury Sandstone|34444|6|Mentioned|Map legend|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|34490|4|Described|p69|||||||||
8165|Hawkesbury Sandstone|34506|3|Fully described|p407|||See also PP408-415||||||
8165|Hawkesbury Sandstone|34547|6|Mentioned|p518|||Dykes weathered to clay in Hawkesbury Sst. areas.||||||20-APR-09
8165|Hawkesbury Sandstone|34560|6|Mentioned|p30|||Triassic||||||
8165|Hawkesbury Sandstone|34561|6|Mentioned|p41|||||||||
8165|Hawkesbury Sandstone|34605|6|Mentioned|p377|||||||||
8165|Hawkesbury Sandstone|34845|6|Mentioned|Fig.4|||||||||
8165|Hawkesbury Sandstone|34944|6|Mentioned|p361|||||||||
8165|Hawkesbury Sandstone|35065|5|Briefly described|p44|||||||||
8165|Hawkesbury Sandstone|35095|6|Mentioned|p114|||||||||
8165|Hawkesbury Sandstone|35098|6|Mentioned|p4|||||||||
8165|Hawkesbury Sandstone|35280|6|Mentioned|p148|||||||||
8165|Hawkesbury Sandstone|35312|6|Mentioned|p3|||||||||
8165|Hawkesbury Sandstone|35416|6|Mentioned|p4|||Stratigraphy and palynological framework on Fig.2||||||
8165|Hawkesbury Sandstone|35472|6|Mentioned|p8|||||||||
8165|Hawkesbury Sandstone|35502|6|Mentioned|Fig.1|||Also on Table 1||||||
8165|Hawkesbury Sandstone|35524|6|Mentioned|Fig.2|||Stratigraphic sequence in southeastern part of Sydney Basin.||||||
8165|Hawkesbury Sandstone|35587|6|Mentioned|p46|||||||||
8165|Hawkesbury Sandstone|35690|6|Mentioned|Fig.1.1|||||||||
8165|Hawkesbury Sandstone|35833|6|Mentioned|p35|||||||||
8165|Hawkesbury Sandstone|35874|5|Briefly described|p1|||||||||
8165|Hawkesbury Sandstone|35878|6|Mentioned|p115|||||||||
8165|Hawkesbury Sandstone|35901|6|Mentioned|p4|||||||||
8165|Hawkesbury Sandstone|36042|6|Mentioned|Table 1|||||||||
8165|Hawkesbury Sandstone|36121|6|Mentioned|p25|||||||||
8165|Hawkesbury Sandstone|36147|6|Mentioned|Fig.2|||||||||
8165|Hawkesbury Sandstone|36148|6|Mentioned|p266|||||||||
8165|Hawkesbury Sandstone|36220|4|Described|p85|||||||||
8165|Hawkesbury Sandstone|36221|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
8165|Hawkesbury Sandstone|36223|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic.||||||
8165|Hawkesbury Sandstone|36376|6|Mentioned|p157|||||||||
8165|Hawkesbury Sandstone|36390|6|Mentioned|Map legend|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|36567|6|Mentioned|p11|||||||||
8165|Hawkesbury Sandstone|36570|6|Mentioned|p22|||||||||
8165|Hawkesbury Sandstone|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
8165|Hawkesbury Sandstone|36594|6|Mentioned|Table 1|||See also Table II.||||||
8165|Hawkesbury Sandstone|36601|6|Mentioned|p73|||||||||
8165|Hawkesbury Sandstone|36616|6|Mentioned|p4|||||||||
8165|Hawkesbury Sandstone|36777|6|Mentioned|Fig.1|||||||||
8165|Hawkesbury Sandstone|36804|6|Mentioned|p9|||||||||
8165|Hawkesbury Sandstone|36899|6|Mentioned|p1085|||||||||
8165|Hawkesbury Sandstone|36961|6|Mentioned|Table 1|||||||||
8165|Hawkesbury Sandstone|37082|6|Mentioned|p161|||||||||
8165|Hawkesbury Sandstone|37083|6|Mentioned|p164|||||||||
8165|Hawkesbury Sandstone|37089|5|Briefly described|p208|||||||||
8165|Hawkesbury Sandstone|37091|5|Briefly described|p226|||||||||
8165|Hawkesbury Sandstone|37093|5|Briefly described|p231|||||||||
8165|Hawkesbury Sandstone|37168|6|Mentioned|Fig.2|||||||||
8165|Hawkesbury Sandstone|37319|6|Mentioned|p606|||||||||
8165|Hawkesbury Sandstone|37346|6|Mentioned|p44|||||||||
8165|Hawkesbury Sandstone|37505|6|Mentioned|Fig.2|||||||||
8165|Hawkesbury Sandstone|37561|6|Mentioned|p101|||||||||
8165|Hawkesbury Sandstone|37623|6|Mentioned|p36|||||||||
8165|Hawkesbury Sandstone|37707|6|Mentioned|p22|||||||||
8165|Hawkesbury Sandstone|37722|6|Mentioned|p23|||||||||
8165|Hawkesbury Sandstone|37757|6|Mentioned|p19|||||||||
8165|Hawkesbury Sandstone|37775|6|Mentioned|p7|||||||||
8165|Hawkesbury Sandstone|37804|6|Mentioned|p55|||||||||
8165|Hawkesbury Sandstone|37812|6|Mentioned|p657|||||||||
8165|Hawkesbury Sandstone|37857|5|Briefly described|p1|||||||||
8165|Hawkesbury Sandstone|38017|6|Mentioned|p100|||||||||
8165|Hawkesbury Sandstone|38063|6|Mentioned|p32|||Building stone and brick making material.||||||
8165|Hawkesbury Sandstone|38206|6|Mentioned|p53|||Clay resources||||||
8165|Hawkesbury Sandstone|38220|5|Briefly described|p319|||Structure||||||
8165|Hawkesbury Sandstone|38304|6|Mentioned|p83|||||||||
8165|Hawkesbury Sandstone|38358|6|Mentioned|p10|||||||||
8165|Hawkesbury Sandstone|38375|6|Mentioned|p547|||||||||
8165|Hawkesbury Sandstone|38575|6|Mentioned|p107|||||||||
8165|Hawkesbury Sandstone|38615|6|Mentioned|p18|||||||||
8165|Hawkesbury Sandstone|38656|6|Mentioned|Fig.1.5.12|||P279||||||
8165|Hawkesbury Sandstone|38664|5|Briefly described|p13|||||||||
8165|Hawkesbury Sandstone|38754|6|Mentioned|p228|||||||||
8165|Hawkesbury Sandstone|38784|4|Described|p75|||||||||
8165|Hawkesbury Sandstone|38813|6|Mentioned|p254|||||||||
8165|Hawkesbury Sandstone|38820|6|Mentioned|p182|||||||||
8165|Hawkesbury Sandstone|39087|6|Mentioned|p10|||||||||
8165|Hawkesbury Sandstone|39287|5|Briefly described|p48|||||||||
8165|Hawkesbury Sandstone|39293|4|Described|p156|||||||||
8165|Hawkesbury Sandstone|39295|6|Mentioned|Fig. 10.1|||||||||
8165|Hawkesbury Sandstone|39296|6|Mentioned|Fig. 11.1|||||||||
8165|Hawkesbury Sandstone|39297|3|Fully described|p189|||See also PP 190-253||||||
8165|Hawkesbury Sandstone|39298|6|Mentioned|p257|||See also P259||||||
8165|Hawkesbury Sandstone|39300|6|Mentioned|p298|||Diatremes||||||
8165|Hawkesbury Sandstone|39306|6|Mentioned|p389|||See also P423,P426||||||
8165|Hawkesbury Sandstone|39308|5|Briefly described|p453|||||||||
8165|Hawkesbury Sandstone|39356|6|Mentioned|p226|||||||||
8165|Hawkesbury Sandstone|39450|6|Mentioned|Table 1|||||||||
8165|Hawkesbury Sandstone|39467|5|Briefly described|p1249|||||||||
8165|Hawkesbury Sandstone|39664|6|Mentioned|Table 8|||||||||
8165|Hawkesbury Sandstone|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|40044|6|Mentioned|p382|||||||||
8165|Hawkesbury Sandstone|40076|6|Mentioned|Fig.20|||||||||
8165|Hawkesbury Sandstone|40516|6|Mentioned|p382|||||||||
8165|Hawkesbury Sandstone|40526|6|Mentioned|p148|||||||||
8165|Hawkesbury Sandstone|40591|6|Mentioned|p323|||||||||
8165|Hawkesbury Sandstone|40592|5|Briefly described|p229|||||||||
8165|Hawkesbury Sandstone|40601|6|Mentioned|p98|||||||||
8165|Hawkesbury Sandstone|40602|3|Fully described|p18|||||||||
8165|Hawkesbury Sandstone|40603|6|Mentioned|p1|||||||||
8165|Hawkesbury Sandstone|40625|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
8165|Hawkesbury Sandstone|40629|6|Mentioned|p184|||||||||
8165|Hawkesbury Sandstone|40630|6|Mentioned|p174|||||||||
8165|Hawkesbury Sandstone|40631|6|Mentioned|p153|||||||||
8165|Hawkesbury Sandstone|40633|6|Mentioned|Fig.1-D|||||||||
8165|Hawkesbury Sandstone|40650|6|Mentioned|Table 7|||||||||
8165|Hawkesbury Sandstone|40651|6|Mentioned|p137|||||||||
8165|Hawkesbury Sandstone|40653|6|Mentioned|p121|||||||||
8165|Hawkesbury Sandstone|40654|6|Mentioned|p116|||||||||
8165|Hawkesbury Sandstone|40655|6|Mentioned|p41|||||||||
8165|Hawkesbury Sandstone|40656|6|Mentioned|p35|||||||||
8165|Hawkesbury Sandstone|40742|6|Mentioned|p297|||||||||
8165|Hawkesbury Sandstone|40744|4|Described|p325|||||||||
8165|Hawkesbury Sandstone|40767|6|Mentioned|p14|||||||||
8165|Hawkesbury Sandstone|40870|6|Mentioned|p7|||||||||
8165|Hawkesbury Sandstone|40886|6|Mentioned|Fig.1|||||||||
8165|Hawkesbury Sandstone|41195|6|Mentioned|p325|||||||||
8165|Hawkesbury Sandstone|41290|6|Mentioned|Fig.8|||||||||
8165|Hawkesbury Sandstone|41299|6|Mentioned|p118|||||||||
8165|Hawkesbury Sandstone|41476|6|Mentioned|p76|||||||||
8165|Hawkesbury Sandstone|41617|4|Described|p302|||||||||
8165|Hawkesbury Sandstone|41658|6|Mentioned|p545|||||||||
8165|Hawkesbury Sandstone|41703|6|Mentioned|p246|||||||||
8165|Hawkesbury Sandstone|41939|5|Briefly described|p23|||||||||
8165|Hawkesbury Sandstone|42122|3|Fully described|p123|||||||||
8165|Hawkesbury Sandstone|42190|6|Mentioned|p267|||||||||
8165|Hawkesbury Sandstone|42287|5|Briefly described|p15|||||||||
8165|Hawkesbury Sandstone|42377|6|Mentioned|p16|||||||||
8165|Hawkesbury Sandstone|42477|6|Mentioned|p44|||||||||
8165|Hawkesbury Sandstone|42630|4|Described|p5-|||Engineering properties||||||
8165|Hawkesbury Sandstone|42656|6|Mentioned|p63|||||||||
8165|Hawkesbury Sandstone|42663|4|Described|Table 2, P11|||||||||
8165|Hawkesbury Sandstone|42668|5|Briefly described|p222|||||||||
8165|Hawkesbury Sandstone|42737|5|Briefly described|map legend|Triassic||||||||
8165|Hawkesbury Sandstone|42795|5|Briefly described|Fig.2 P23|||||||||
8165|Hawkesbury Sandstone|42821|5|Briefly described|p25, p125|||||||||
8165|Hawkesbury Sandstone|42896|3|Fully described|p32, Table 2|||Middle Triassic age||||||
8165|Hawkesbury Sandstone|42900|6|Mentioned|p388|||||||||
8165|Hawkesbury Sandstone|42916|5|Briefly described|Table 1||Middle Triassic|||||||
8165|Hawkesbury Sandstone|42925|3|Fully described|p14|||see also Table 1||||||
8165|Hawkesbury Sandstone|42926|4|Described|map legend||Middle Triassic|||||||
8165|Hawkesbury Sandstone|43028|6|Mentioned|p614|||||||||
8165|Hawkesbury Sandstone|43044|5|Briefly described|p123|||||||||
8165|Hawkesbury Sandstone|43072|6|Mentioned|p78|||||||||
8165|Hawkesbury Sandstone|43080|6|Mentioned|p120|||||||||
8165|Hawkesbury Sandstone|43194|5|Briefly described|p122, p131|Middle Triassic|Middle Triassic|Sydney Basin. Coarse quartzose sand. Time equivalent to the middle part of the Napperby Formation, Gunnedah Basin.||||||
8165|Hawkesbury Sandstone|43257|5|Briefly described|Map Legend||Triassic|||||||
8165|Hawkesbury Sandstone|43263|6|Mentioned|Map Legend||Triassic|||||||
8165|Hawkesbury Sandstone|43317|4|Described|Table 1 p13|||||||||
8165|Hawkesbury Sandstone|43319|14|Not recorded|Map Legend|||||||||
8165|Hawkesbury Sandstone|43320|4|Described|Table 1|Middle Triassic|Middle Triassic|p13,15,16,20,25-31||||||
8165|Hawkesbury Sandstone|43321|14|Not recorded|p7,15|||||||||
8165|Hawkesbury Sandstone|43323|14|Not recorded|p68,71|||Fossil, Aratrisporites||||||
8165|Hawkesbury Sandstone|43324|14|Not recorded|p18,19||Triassic|||||||
8165|Hawkesbury Sandstone|43325|14|Not recorded|Map Legend||Triassic|||||||
8165|Hawkesbury Sandstone|43339|14|Not recorded|p6-7||Triassic|||||||
8165|Hawkesbury Sandstone|43340|14|Not recorded|p129|||||||||
8165|Hawkesbury Sandstone|43342|14|Not recorded|Table 1 p107|||||||||
8165|Hawkesbury Sandstone|43343|14|Not recorded|p119|||||||||
8165|Hawkesbury Sandstone|43344|14|Not recorded|p13,18,19,21-2,24,26||Triassic|28-30,33-43,46-49,51-58,60-69,71-73,76-7,102,163,170,173,182,186||||||
8165|Hawkesbury Sandstone|43345|14|Not recorded|p2,3,6,9||Triassic|||||||
8165|Hawkesbury Sandstone|43346|3|Fully described|p1,2,4 Map|||||||||
8165|Hawkesbury Sandstone|43349|14|Not recorded|Map|||||||||
8165|Hawkesbury Sandstone|43351|14|Not recorded|p 85|||||||||
8165|Hawkesbury Sandstone|43352|3|Fully described|p 209-223||Triassic|||||||
8165|Hawkesbury Sandstone|43353|14|Not recorded|p 228|||Reference not on card||||||
8165|Hawkesbury Sandstone|43358|14|Not recorded|p47,48,51,58,60|||||||||
8165|Hawkesbury Sandstone|43359|14|Not recorded|Map Legend||Mesozoic|Provisional first edition||||||
8165|Hawkesbury Sandstone|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
8165|Hawkesbury Sandstone|43361|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
8165|Hawkesbury Sandstone|43363|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
8165|Hawkesbury Sandstone|43365|14|Not recorded|p169-210||Triassic|||||||
8165|Hawkesbury Sandstone|43372|14|Not recorded|p85|||||||||
8165|Hawkesbury Sandstone|43373|14|Not recorded|p163|||||||||
8165|Hawkesbury Sandstone|43376|14|Not recorded|p149|||||||||
8165|Hawkesbury Sandstone|43378|14|Not recorded|p141|||||||||
8165|Hawkesbury Sandstone|43383|14|Not recorded|Fig.5,p22,23,Fig.3||Triassic|Conformable on Narrabeen Group||||||
8165|Hawkesbury Sandstone|43384|14|Not recorded|Map Legend||Triassic|||||||
8165|Hawkesbury Sandstone|43385|14|Not recorded|p181,182||Triassic|U.Bunter||||||
8165|Hawkesbury Sandstone|43395|14|Not recorded|p70,71|||||||||
8165|Hawkesbury Sandstone|43412|14|Not recorded|p15|||||||||
8165|Hawkesbury Sandstone|43414|14|Not recorded|p15,16||Triassic|||||||
8165|Hawkesbury Sandstone|43416|14|Not recorded|p2|||||||||
8165|Hawkesbury Sandstone|43420|14|Not recorded|p282||Triassic|||||||
8165|Hawkesbury Sandstone|43440|14|Not recorded|p34,fig.4-3|||||||||
8165|Hawkesbury Sandstone|43445|14|Not recorded|p22,23|||||||||
8165|Hawkesbury Sandstone|43449|14|Not recorded|p11;opp 12;Pl 2|||||||||
8165|Hawkesbury Sandstone|43479|14|Not recorded|p227,243|Late Triassic|Middle Triassic|||||||
8165|Hawkesbury Sandstone|43491|14|Not recorded|pVIII/8,8a,11,11a,12||Triassic|pVIII/13,15a,16||||||
8165|Hawkesbury Sandstone|43505|14|Not recorded|p113-115|||'The areal extent and thickness suggests was deposited in the fluvial regime of a large delta||||||
8165|Hawkesbury Sandstone|43506|14|Not recorded|p766-768|||Large-scale cross-stratification: S headlands of Long Bay and Coogee Beach||||||
8165|Hawkesbury Sandstone|43508|14|Not recorded|p126|||'stylolitic contacts between adjacent quartz grains are common'||||||
8165|Hawkesbury Sandstone|43549|14|Not recorded|p131|||||||||
8165|Hawkesbury Sandstone|43550|14|Not recorded|p171|||||||||
8165|Hawkesbury Sandstone|43551|14|Not recorded|p47|||||||||
8165|Hawkesbury Sandstone|43560|6|Mentioned|p234||Triassic|Age: 600 Ma||||||
8165|Hawkesbury Sandstone|43676|6|Mentioned|p326|||||||||
8165|Hawkesbury Sandstone|43677|6|Mentioned|p319||Triassic|||||||
8165|Hawkesbury Sandstone|43686|6|Mentioned|p234,237-239|||||||||
8165|Hawkesbury Sandstone|43705|6|Mentioned|p10||Triassic|||||||
8165|Hawkesbury Sandstone|43798|6|Mentioned|p195||Triassic|||||||
8165|Hawkesbury Sandstone|43873|14|Not recorded|p53|||||||||
8165|Hawkesbury Sandstone|43880|14|Not recorded|p57|||||||||
8165|Hawkesbury Sandstone|43881|14|Not recorded|p12,44,76,78-9,151|||Compared with Kangaroo Creek Sandstone. p159.||||||
8165|Hawkesbury Sandstone|43885|14|Not recorded|p418-9,424-5|||"Widespread distribution of authigenic dickite explains high matrix content in quartzose sandstone"||||||
8165|Hawkesbury Sandstone|43890|14|Not recorded|p562|||||||||
8165|Hawkesbury Sandstone|43895|14|Not recorded|p116|||||||||
8165|Hawkesbury Sandstone|43965|14|Not recorded|p24|||Bauxite in weathered shale lens at Somersby.||||||
8165|Hawkesbury Sandstone|43980|14|Not recorded|p3,opp.1,Pl.1|||||||||
8165|Hawkesbury Sandstone|44004|4|Described|p18|||||||||
8165|Hawkesbury Sandstone|44005|14|Not recorded|p26,opp.23,Pl.4|||||||||
8165|Hawkesbury Sandstone|44244|5|Briefly described|p290 Tb. 5|Triassic|Triassic|Age: >240Ma.  Geological Province: northern Sydney Basin.||||||18-AUG-04
8165|Hawkesbury Sandstone|44247|14|Not recorded|p8|||Anaspidites antiquus (syncarid crustacean) found.||||||
8165|Hawkesbury Sandstone|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
8165|Hawkesbury Sandstone|44450|5|Briefly described|p147 Fig 43|Middle Triassic|Middle Triassic|Geological Province: Sydney Basin.||||||
8165|Hawkesbury Sandstone|44507|14|Not recorded|p103,106|||||||||
8165|Hawkesbury Sandstone|44610|14|Not recorded|p49|||||||||
8165|Hawkesbury Sandstone|44668|14|Not recorded|p60|||||||||
8165|Hawkesbury Sandstone|44855|14|Not recorded|p18|Late Triassic|Middle Triassic|||||||
8165|Hawkesbury Sandstone|44861|14|Not recorded|p27,28,32,77-9,137,|||p232,241,300||||||
8165|Hawkesbury Sandstone|44998|14|Not recorded|p104|||Correlated with Erskine Sandstone & Blina Shale in W.A.||||||
8165|Hawkesbury Sandstone|45018|14|Not recorded|p17-23,25|||||||||
8165|Hawkesbury Sandstone|45090|6|Mentioned|p7|||Time correlation chart||||||
8165|Hawkesbury Sandstone|45095|6|Mentioned|p137|||Refers McElroy (1969)||||||
8165|Hawkesbury Sandstone|45138|6|Mentioned|p3|||||||||
8165|Hawkesbury Sandstone|45168|6|Mentioned|p8|||||||||
8165|Hawkesbury Sandstone|48735|6|Mentioned|p88|||||||||
8165|Hawkesbury Sandstone|48744|6|Mentioned|p.88.|||||||||
8165|Hawkesbury Sandstone|48926|6|Mentioned|p15|||P15 et seq.||||||
8165|Hawkesbury Sandstone|60281|4|Described|p9, p63|Middle Triassic|Middle Triassic|Overlies the Narrabeen Group.  Max. thickness: up to 290m. Geological Province: Sydney Basin.||||||16-JAN-08
8165|Hawkesbury Sandstone|60297|6|Mentioned|p168 Fig.1|Permian|Permian|||||||
8165|Hawkesbury Sandstone|60299|6|Mentioned|p223|||||||||
8165|Hawkesbury Sandstone|60726|5|Briefly described|p1, p3, throughout text.|Middle Triassic|Middle Triassic|||||Is overlain by the Mittagong Formation.||
8165|Hawkesbury Sandstone|61044|6|Mentioned|p32 Fig. 3.3, p34|||Produces soils with low clay content.||||||
8165|Hawkesbury Sandstone|61186|6|Mentioned|p8, p75|||Dimension stone from the Sydney Basin. Also informally referred to as Sydney sandstone. SEE also p30 Plate 15||||||
8165|Hawkesbury Sandstone|61209|5|Briefly described|p225 Fig. 7b|Mesozoic|Mesozoic|Geological Province: Sydney Basin.||||||
8165|Hawkesbury Sandstone|61310|6|Mentioned|p21|||Geological Province: Sydney Basin.||||||
8165|Hawkesbury Sandstone|61315|5|Briefly described|Table SY1|MiddleTriassic|Middle Triassic|Primary hydrocarbon reservoir in the offshore part of the basin. Geological Province: Sydney Basin||||||
8165|Hawkesbury Sandstone|61610|6|Mentioned|p252 Fig. 2|Early Triassic|Early Triassic|Geological Province: Sydney Basin.||||||07-FEB-11
8165|Hawkesbury Sandstone|61612|6|Mentioned|p275, p270 Fig. 1|Early Triassic|Early Triassic|Geological Province: Sydney Basin.||||||17-MAR-09
8165|Hawkesbury Sandstone|62349|6|Mentioned|p73|||Geological Province: Sydney Basin.||||||
8165|Hawkesbury Sandstone|64769|6|Mentioned|p23|Triassic|Triassic|||||||
8165|Hawkesbury Sandstone|65195|6|Mentioned|p3-5, p7-15, p17, p21-30, p33|Triassic|Triassic|Overlain by Rickaby's Creek Gravels in the Lapstone Structural Complex. One of the most exposed units in the Lapstone Structural Complex||||||
8165|Hawkesbury Sandstone|65490|5|Briefly described|p 874, Fig. 1 p875|Middle Triassic|Early Triassic|Sedimentary unit of the Sydney Basin Cut by faults dating between ~163 and 120 Ma, and reactivated post 51 Ma. See p882-883 for age discussion.||||||
8165|Hawkesbury Sandstone|65492|6|Mentioned|p894, 889, p890 Fig. 1,p896, 901|Triassic|Triassic|Overlies the Narrabeen Group.||||||06-MAY-11
8165|Hawkesbury Sandstone|65664|6|Mentioned|p1099|Triassic|Triassic|Of the Sydney Basin.||||||09-MAY-12
8165|Hawkesbury Sandstone|66577|6|Mentioned|pp995-997, p1001 Fig.6.|Triassic|Triassic|Quartz-rich sediments sourced from Lachlan Fold Belt.|||Includes Mittagong Formation.|Overlies Narrabeen Group. Is overlain by Wianamatta Group.||
8165|Hawkesbury Sandstone|67560|5|Briefly described|p258, p260-p272|Triassic|Triassic|~ 262m thick in Eveleigh No.1 DDH. Maximum age constrained by the underlying Narrabeen Group. Freshwater braided stream depositional environment, sourced from the SW.||||Underlain by Newport Formation (Narrabeen Group). Overlain by Ashfield Shale.|Fluvial succession derived from a quartz-rich sand source.|23-MAY-17
8165|Hawkesbury Sandstone|67663|5|Briefly described|p519 Fig.1, p520 Tb.1, p521-522|Triassic|Triassic|~ 250m thick.||||Unconformably overlies Narrabeen Group, Terrigal and Newport Formations. Overlain by the Wianamatta Group.|Dominantly coarse quartz sandstone.|
8165|Hawkesbury Sandstone|67786|6|Mentioned|p96|Triassic|Triassic|Newcastle Coalfield, Sydney Basin.||||Overlies Narrabeen Group.||
8165|Hawkesbury Sandstone|67850|5|Briefly described|p51 Table 1, pp52-53, pp55-57. |Triassic|Triassic|Contains large-scale cross-beds and lenticular geometry, complicating dip measurements.||||||
8165|Hawkesbury Sandstone|68003|5|Briefly described|p43.|Triassic|Triassic|Sydney Basin. Sediment source was Late Devonian quartzites in the Lachlan Fold Belt.|||||Coarse-grained quartzose sandstone.|
8165|Hawkesbury Sandstone|68004|5|Briefly described|p23 Table 1. |||Sydney Basin.||||Overlies Narrabeen Group. Is overlain by Wianamatta Group and Napperby Formation.||
8165|Hawkesbury Sandstone|68204|6|Mentioned|p46-47, 55|Triassic|Triassic|Mittagong-Bowral area, Sydney Basin.||||||
8165|Hawkesbury Sandstone|68576|6|Mentioned|QLD_D1: p10|||Sydney. Used in St. John's Cathedral, Brisbane.||||||
8165|Hawkesbury Sandstone|68811|5|Briefly described|p57, p165 tbl 27|Triassic|Triassic|Hosts a deep, confined, fractured and porous aquifer beneath the Botany Sand Beds. ||||Overlain by the Botany Sand Beds.||
8165|Hawkesbury Sandstone|69297|6|Mentioned|p403, p418, p434, p499, p501, p504|Triassic|Triassic|Sydney Basin. Deposited in a braided fluvial to tidal environment. Sandstones are good potential hydrocarbon reservoirs. ||||Overlies the Narrabeen Group, Burralow Formation and the Gosford Subgroup. Overlain by the Wianamatta Group.||
8165|Hawkesbury Sandstone|69683|5|Briefly described|p410 Fig.1, p411 Fig.2, p412, p420 Fig.5|Triassic|Triassic|Maximum thickness of 250m used in modelling in this study.|||||Bedded quartz sandstone, minor siltstone.|
8165|Hawkesbury Sandstone|70125|5|Briefly described|p385-p386 Fig.1, p387-393, p395-405|Triassic|Triassic|Sydney Basin. Fluvial braided-channel quartzose (light) deposits. Origins and ages of sediment from SSW detailed. Detrital zircons are dominated by 700-500 Ma ages of the Pacific-Gondwana Igneous Component; their properties are compared in detail with those of the Lachlan Orogen.|242 Ma.|||Coeval with Jerilderie Formation (same palynozone).||14-MAY-20
8165|Hawkesbury Sandstone|70587|5|Briefly described|Map Legend|Triassic|Triassic ||||||Cross bedded to massive quartz sandstone with mudstone lenses.|
8165|Hawkesbury Sandstone|70647|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Sydney Basin.|||||Medium- to very coarse-grained quartz sandsdone, minor laminated mudstone and siltstone lenses.|
8165|Hawkesbury Sandstone|70661|3|Fully described|vii, ix, p140, p189, p193|Anisian|Anisian|Named for the Hawkesbury River. Previously termed the Hawkesbury Rocks, Hawkesbury beds, Hawkesbury Formation or the Hawkesbury Series before the final name was adopted. Distribution, distinguishing characteristics, geomorphology, structure, geophysical characteristics and fossil assemblage described. Lithology discussed in further detail.  40-100m thick in the map area. Deposited in a fluvial environment. Age based on palynology. Quarried for dimension stone and gravel in places. See also p196-p203, p213, p240.||||Disconformably overlies Berry Siltstone, Illawarra Coal Measures, Narrabeen Group,Conformably overlain by Mittagong Formation,  overlain by Ashfield Shale|Quartzose, medium to very coarse grained sandstone  that is often intercalated with recessive sequences of shale, interbedded fine grained sandstone and sitlstone.  Rare clast supported conglomerate is also present.|
8165|Hawkesbury Sandstone|70744|6|Mentioned|p948|Triassic|Triassic|The Pacific-Gondwana detrital zircon signature (650-500 Ma) is prominent in this unit.||||||
8165|Hawkesbury Sandstone|71303|5|Briefly described|map legend|Middle Triassic|Middle Triassic|Of Sydney Basin.|||||Buff to yellow, very quartzose; fine to very coarse-grained sandstone, pebbly sandstone, rare conglomerate; lenses of grey laminated shale and interbedded fine-grained sandstone and siltstone. Characteristically cross-bedded.|
8165|Hawkesbury Sandstone|71538|6|Mentioned|p54 fig 2|Triassic|Triassic|Sydney Basin.  Fluvial depositional environment.||||Overlies the Illawarra Coal Measures.||
8165|Hawkesbury Sandstone|73059|5|Briefly described|p1062|Triassic|Triassic|Sydney Basin. Detrital zircons are dominantly 700-500 Ma and widely considered to be derived from East Antarctica.|||||Quartz-rich sandstones.|
8165|Hawkesbury Sandstone|73146|6|Mentioned|p15|||Sydney Basin. Has magnetic overprinting with a uniformly normal polarity and steep inclination.|||||Sandstones.|
8165|Hawkesbury Sandstone|73147|5|Briefly described|p130|||Braided fluvial system deposits.|||||Cross-bedded and cross-stratified sandstones.|
8165|Hawkesbury Sandstone|73181|6|Mentioned|p61|||||||||
8165|Hawkesbury Sandstone|73248|5|Briefly described|p301, p305-310, App. p1-3|Middle Triassic|Middle Triassic|Vitrinite reflectance values from coals and authigenic overgrowths on detrital quartz fragments may be a result of heat flow and near-surface diagenetic processes rather than deep burial (Branagan, 1983). Has experienced major tilting along the Lapstone Monocline. Predates upwarping related to the development of the Hornsby Plateau. The major movement of this unit along the Lapstone Structural Complex appears to have taken place after around 90 Ma.||||Overlain by Wianamatta Group and Mittagong Formation. Unconformably overlain by Rickabys Creek Gravel and Robertson Basalt.||
8165|Hawkesbury Sandstone|73264|6|Mentioned|p1402 Fig.23, p1404|Triassic|Triassic|Sydney Basin. Derived from Ordovician turbidites or Antarctic source.||||||
8165|Hawkesbury Sandstone|73304|6|Mentioned|p74-75|Anisian|Anisian|Sydney Basin, southern.||||||
8165|Hawkesbury Sandstone|75059|6|Mentioned|p4, 9-10|Middle Triassic|Middle Triassic|Sydney Basin.||||Is overlain by Mittagong Formation or Wianamatta Group.||
8179|Hawkins Suite|22768|4|Described|p176|||||||||
8179|Hawkins Suite|22857|5|Briefly described|p176|||In the Canberra area - composed of dacitic lava, ignimbrite and interbedded sediments at base (Mount Ainslie, Paddys River and Walker Volcanics) overlain by Wenlock strata followed by a large dacitic ignimbrite. Overlies Canberra Fm; underlies Yass Fm.||||||
8179|Hawkins Suite|23439|6|Mentioned|p130|||||||||
8179|Hawkins Suite|23547|5|Briefly described|p553|||||||||
8179|Hawkins Suite|23549|5|Briefly described|p522|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||05-APR-05
8179|Hawkins Suite|24128|5|Briefly described|p3|||Geological Province: Lachlan Fold Belt.||||||
8179|Hawkins Suite|41563|6|Mentioned|p512|||||||||
8179|Hawkins Suite|43158|4|Described|Fig1p2; p3,4,5,7,13||Early Silurian|||||||
8179|Hawkins Suite|43159|4|Described|Fig.2p4,p1,p3,p9.|Late Silurian|Early Silurian|Volcanics.Intrusive rocks of the suite known as Bullenballong Suite. Extend from Dubbo to Kiandra.||||||
8179|Hawkins Suite|50606|6|Mentioned|p4.3|||Geological Province: Lachlan Fold Belt.||||||
8184|Hawkins Volcanics|22691|6|Mentioned|Fig2 P316||Silurian|||||||
8184|Hawkins Volcanics|22768|5|Briefly described|p176|||||||||
8184|Hawkins Volcanics|22857|4|Described|p176, p460 App.1 Tb.A1.6|Middle Silurian|Middle Silurian|Dacitic crystal tuff and ignimbrite, fine tuff, andesitic and dacite lava with interbedded limestone, sandstone, shale. Contains graptolites, brachiopods, nautiloids. Max. thickness: ~1770m(Est.). Geological Province: Canberra-Yass Shelf.||||||
8184|Hawkins Volcanics|23549|5|Briefly described|p522.|||Of the Hawkins Suite.  Closely related to the Bullenbalong Supersuite rocks.||||||05-APR-05
8184|Hawkins Volcanics|24248|5|Briefly described|p50 Fig.1|Wenlock|Wenlock|Geological Province: Yass Syncline.||||||
8184|Hawkins Volcanics|24317|5|Briefly described|p14, p15 Fig.1|Silurian|Silurian|Volcanics and volcaniclastics with minor sedimentary rocks and limestone, subaerial to shallow marine deposits.||||||
8184|Hawkins Volcanics|24417|6|Mentioned|p45|Silurian|Silurian|||||||
8184|Hawkins Volcanics|30069|5|Briefly described|p5|||||||||
8184|Hawkins Volcanics|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
8184|Hawkins Volcanics|32675|6|Mentioned|p7|||Strat. Nomenclature||||||
8184|Hawkins Volcanics|32820|6|Mentioned|Table 1|||Refers Pogson & Baker (1974)||||||
8184|Hawkins Volcanics|32858|4|Described|p32|||Lithology||||||
8184|Hawkins Volcanics|33325|5|Briefly described|Table 2|||See also Table 3.||||||
8184|Hawkins Volcanics|35070|6|Mentioned|p78|||||||||
8184|Hawkins Volcanics|35384|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
8184|Hawkins Volcanics|35386|3|Fully described|p14|||||||||
8184|Hawkins Volcanics|36411|6|Mentioned|p269|||Refs Cramsie et al 1978 for redefinition.||||||
8184|Hawkins Volcanics|36413|6|Mentioned|Table 3|||||||||
8184|Hawkins Volcanics|36441|5|Briefly described|map legend|Wenlockian|Wenlockian|Extrusive. Grey green dacite ignimbrite. Underlies Glen Bower Formation. BMR map code: Svh.||||||
8184|Hawkins Volcanics|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
8184|Hawkins Volcanics|37728|4|Described|Table 2|||||||||
8184|Hawkins Volcanics|37752|6|Mentioned|p105|||||||||
8184|Hawkins Volcanics|38035|6|Mentioned|p91|||||||||
8184|Hawkins Volcanics|38151|6|Mentioned|Table 1|||||||||
8184|Hawkins Volcanics|38202|5|Briefly described|p52|||Base metal sulfide mineralization.||||||
8184|Hawkins Volcanics|40328|3|Fully described|p95|||||||||
8184|Hawkins Volcanics|40689|6|Mentioned|p4|||||||||
8184|Hawkins Volcanics|40738|5|Briefly described|p622|||||||||
8184|Hawkins Volcanics|41133|6|Mentioned|p1118|||||||||
8184|Hawkins Volcanics|42497|5|Briefly described|Map legend|Wenlockian|Wenlockian|||||||
8184|Hawkins Volcanics|42726|5|Briefly described|map legend|Silurian||V40.  Of the Bullenbalong Suite (Bullenbalong Supersuite).  Formal name not intended.||||||08-FEB-05
8184|Hawkins Volcanics|43147|5|Briefly described|p53|||Of Bullenbalong Supersuite.||||||20-NOV-08
8184|Hawkins Volcanics|43158|4|Described|3,13|||||||||
8184|Hawkins Volcanics|43834|6|Mentioned|p32|||||||||
8184|Hawkins Volcanics|44093|5|Briefly described|p196 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||10-MAR-05
8184|Hawkins Volcanics|45147|3|Fully described|M150|||See also M128.||||||02-JUN-08
8184|Hawkins Volcanics|49705|6|Mentioned|p29|||||||||
8184|Hawkins Volcanics|50230|5|Briefly described|Map legend|Wenlock|Wenlock|Of the Douro Group.  Ignimbrite; occasional quartz and dioritic xenoliths. Contains the Ledgeworth Facies and Vale View Facies. Overlain by the Yass Formation.||||||03-OCT-07
8184|Hawkins Volcanics|50231|5|Briefly described|Map Legend|Ludlow|Wenlock|Of the Douro Group.||||||
8184|Hawkins Volcanics|61910|5|Briefly described|p152|Silurian|Silurian|Of the Douro Group. Geological Province: Lachlan Fold Belt.||||||
8184|Hawkins Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Douro Gp. Blue-grey massive, med.- to coarse-gr., often welded porphyritic crystal vitric biotite-cordierite-garnet rhyolitic to dacitic ignimbrite. Occasional quartz and dioritic xenoliths. Flow-banded, vesicular rhyodacitic to dacitic lava, volc.sst.||||||
8184|Hawkins Volcanics|64994|5|Briefly described|p7|Wenlock|Wenlock|Of Sherwin and Strusz (2002). Includes shales containing graptolites. Ewuivalent of the Canowindra Volcanics.||||||07-FEB-11
8184|Hawkins Volcanics|66197|5|Briefly described|p630, p631 Fig.3b, p632|Wenlock|Llandovery|Canberra-Yass Basin.| Shown as 428 +/- 5 Ma.||Includes Bango Limestone Member.|Underlies the Yass Formation and Yarralumla Formation. Overlies the Canberra Formation in places.|Massive S-type ignimbrites; locally contains late Wenlock shallow marine sedimentary rocks.|14-MAR-12
8184|Hawkins Volcanics|66300|5|Briefly described|p92.||||433.7 +/- 3.0 Ma.|Unit in Douro Group.||Intruded by Rye Park Granite.||
8184|Hawkins Volcanics|66713|5|Briefly described|p1, p3 Fig.2, p4 Fig.3, p6, p10|Wenlock|Llandovery|Early Silurian. Felsic volcanics, quartz-lithic sandstone and tuffaceous shale; characteristic abundant feldspar and quartz crystal fragments. Hosts the Western vein in the Phoenix W deposit. Is intruded by Rye Park Granite.||||||
8184|Hawkins Volcanics|68310|6|Mentioned|p237|||Wyborn et al. (1981). Crops out within and N of Canberra.||||||
8184|Hawkins Volcanics|68592|2|Defined|p437-45, p451-2, p456-71, p498, p517|Wenlock|Wenlock|See also p126-7, p187-91, p204-6, p226, p231, p236, p239, p265, p269, p349-50, p354, p356-7, p376, p384-5, p409, p412, p415-6, p427-8, p430 Fig.89, p431, p433-4, p519-21, p777, p1873-4. Pogson and Baker (1974); Cramsie et al. (1978); after Hawkins Series (Brown, 1940). Original type locality and new type section decribed. Thickness up to 5,000m. Metamorphism described; geophysical properties detailed. Early to Middle Wenlock age from conodonts discussed: minimum age from intrusive Young Granodiorite: 428.8 +/- 1.9 Ma (SHRIMP U-Pb zircon; Black, in Lyons et al., 2000). Is intruded by Young Granodiorite and by Licking Gully, Rye Park and Hume Park Granites. Hosts numerous, mostly minor, Cu +/- Pb +/- Zn +/- Au veins, eg Frogmore and Kangiara, and the Red Hill Cu deposit (all detailed). Prospective for aggregate. Felsic volcanic rocks in the Yass-Bookham area have been used for dimension stone. Isolated lenses of limestone have been quarried for lime. S-type. Stratigraphically equivalent to Canowindra and Glenisla Volcanics. Fossil fauna described.|433 +/- 3.0 Ma; SHRIMP U-Pb zircon; Black, (2006)|Unit in Douro Group.|Includes Bango Limestone Member.|Overlies Mundoonen Sandstone and Kenyu Formation unconformably. Is overlain conformably by Yass Formation, and unconformably by Hervey Group and Mountain Creek Volcanics.|Blue-grey/green, 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; local limestone lenses.|
8184|Hawkins Volcanics|70192|4|Described|Map Legend|Wenlock|Wenlock|Sdh. Includes three unnamed members: diatremes of volcanic breccia with clasts of felsic volcanic quartz sandstone and siltstone; massive-locally bedded limestone; volcanic mudstone and siltstone interbedded with volcaniclastic sandstone and rhyolitic ignimbrite. On Yass, Boorowa and Gunning 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Douro Group|Includes Bango Limestone Member and three unnamed units.|Is overlain by O'Briens Creek Sandstone Member (of Yass Formation) and Wyelba Member (of Glen Bower Formation). Is erosional at base, on Yass 1:100 000.|Medium-coarse, massive, welded porphyritic dacitic-rhyolitic ignimbrite; subordinate medium-coarse, massive volcaniclastic sandstone, siltstone,mudstone and conglomerate; minor coherent dacite and rhyolite, very minor limestone and volcanic breccia.|
8184|Hawkins Volcanics|70210|5|Briefly described|p39|||The younger age determination (from a 2004/05 Report) is within error of the new age (431.7 +/- 3.1 Ma: this Report) for the correlative Canowindra Volcanics.|438.0 +/- 3.0 Ma and 433.7 +/- 3.0 Ma.|||Correlated with Canowindra Volcanics.||
8184|Hawkins Volcanics|70296|5|Briefly described|p1, p14-15, p19, p24|Llandovery|Llandovery|Goulburn-Yass district. Two samples dated.|433.7 +/- 3.0 Ma, 438.0+/-3 Ma (SHRIMP U-Pb)|||||22-JAN-21
8184|Hawkins Volcanics|70540|5|Briefly described|Map Legend|Silurian|Silurian|Includes two unnamed members: massive to locally bedded, fossiliferous limestone; massive, thinly bedded or laminated volcanic mudstone and siltstone.|||Includes Bango Limestone Member.||Medium-coarse grained, massive, welded porphyritic dacitic-rhyolitic ignimbrite. subordinate medium-coarse grained, massive volcaniclastic sandstone, siltstone, mudstone and conglomerate; minor coherent dacite and rhyolite.|
8184|Hawkins Volcanics|70541|4|Described|Map Legend|Devonian|Silurian|Includes three unnamed members: diatremes of volcanic breccia with clasts of felsic volcanic quartz sandstone and siltstone; massive-locally bedded limestone; volcanic mudstone and siltstone interbedded with volcaniclastic sandstone and rhyolitic ignimbrite.||Douro Group|Includes three unnamed members.||Medium-coarse, massive, welded porphyritic dacitic-rhyolitic ignimbrite; subordinate medium-coarse, massive volcaniclastic sandstone, siltstone, mudstone and conglomerate; minor coherent dacite and rhyolite, very minor limestone and volcanic breccia.|
8184|Hawkins Volcanics|70545|5|Briefly described|Map Legend|Silurian|Silurian|Includes two unnamed subunits; one of massive to locally bedded, fossiliferous, recrystallised limestone and a massive, thinly bedded or laminated volcanic mudstone and siltstone interbedded with volcaniclastic sandstone.||Douro Group|||Medium-coarse grained, massive, commonly welded, porphyritic, crystal-vitric dacitic-rhyolitic ignimbrite. Subordinate medium-coarse grained, massive volcaniclastic sandstone, siltstone, mudstone and conglomerate. Minor coherent dacite and rhyolite.|20-SEP-17
8184|Hawkins Volcanics|70546|5|Briefly described|Map Legend|Silurian|Silurian|Includes one unnamed member of massive, thinly bedded or laminated volcanic mudstone and siltstone. Also includes minor dacite and rhyolite; very minor limestone and volcanic breccia.||Douro Group|||Medium-coarse grained, massive, commonly welded, porphyritic, crystal vitric, dacitic to rhyolitic ignimbrite. Subordinate medium-coarse grained, massive volcaniclastic sandstone, siltstone, mudstone and conglomerate.|
8184|Hawkins Volcanics|71069|6|Mentioned|p89, p93|Wenlock|Wenlock|Age is only probable. ||Douro Group|Includes the Bango Limestone Member|Is faulted against the Margules Group. Overlies the Mundoonen Sandstone.||
8184|Hawkins Volcanics|71656|4|Described|p12 Fig.2, p19, p20 Fig.3, p21, 52-55|Wenlock|Wenlock|Includes graptolites in mudstone, conodonts, corals, brachiopods in limestone, gastropods in sandstone. The age of the top of the Hawkins Volcanics is constrained by conodonts from the Euralie Limestone Member (of the overlying Yanawe Formation) that are most likely to be no younger than latest Sheinwoodian, or mid-Wenlockian.||Douro Group|Includes Bango Limestone Member.|Underlies Boambolo Formation, Yass Formation.|Volcanics containing fossiliferous limestone blocks. Mudstone, sandstone.|
8184|Hawkins Volcanics|71700|6|Mentioned|CD||||||Includes the Bango Limestone Member.|Overlies the Mundoonen Sandstone.||
8184|Hawkins Volcanics|73215|4|Described|p992-994, 1002-1004|Middle Silurian|Middle Silurian|Yass Syncline. Compositionally grouped with Bullenbalong Supersuite. These two age determinations, by Black (2005) and Kemp et al. (2008), are from lower and higher points in the Formation respectively.|438 +/- 3 Ma to 430 +/- 4 Ma.|Douro Group||Is overlain by Yass, Glen Bower, Boambolo Formations. Lower part is lateral equivalent to Goobarragandra Volcanics. Is intruded by Young Granodiorite.|Local columnar jointing. Also contains limestone and shallow marine units interbedded with the volcanics.|
8189|Hawksview Granite|23309|6|Mentioned|p448 App1|||This publication lists it as an obsolete granite name, but later GSV publications have used the name.||||||06-SEP-07
8189|Hawksview Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
8189|Hawksview Granite|32684|6|Mentioned|p250|||See also Fig.2. Petrology P252||||||
8189|Hawksview Granite|37029|6|Mentioned|p48|||||||||
8189|Hawksview Granite|39331|6|Mentioned|p27|||||||||
8189|Hawksview Granite|40328|4|Described|p207|||||||||
8189|Hawksview Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8189|Hawksview Granite|40498|6|Mentioned|p392|||||||||
8189|Hawksview Granite|42726|5|Briefly described|map legend|Silurian||||||||
8189|Hawksview Granite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
8189|Hawksview Granite|70777|5|Briefly described|p2, p63, p81|Pridoli|Pridoli|Lachlan Orogen.|422.0 +/- 3.0 Ma (Keay et al., 1999)|||||
8214|Heatherdale Shale|22531|6|Mentioned|p15|||||||||
8214|Heatherdale Shale|22581|6|Mentioned|Fig.2,p37|||Of the Normanville Group.  In the Kanmantoo Basin. Overlies Fork Tree Limestone. Overlain by Truro Volcanics.||||||12-FEB-07
8214|Heatherdale Shale|22643|5|Briefly described|p186, fig3,6|Early Cambrian|Early Cambrian|||||||
8214|Heatherdale Shale|22671|6|Mentioned|p848||Early Cambrian|Underlies the Kanmantoo Group. Max Age: 526 (+/-) 4 Ma.||||||18-JAN-06
8214|Heatherdale Shale|22755|6|Mentioned|p556|||||||||
8214|Heatherdale Shale|22766|4|Described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|Age of unit 526+/-4 Ma.||||||15-JAN-08
8214|Heatherdale Shale|22830|6|Mentioned|P25|||||||||
8214|Heatherdale Shale|22857|5|Briefly described|p94|Early Cambrian|Early Cambrian|Age: 526+/-6Ma (SHRIMP zircon). ||||||
8214|Heatherdale Shale|22858|6|Mentioned|p94||Early Cambrian|Max Age: 526 (+/-) 6 Ma.||||||
8214|Heatherdale Shale|23309|5|Briefly described|p27,45|||||||||
8214|Heatherdale Shale|23539|5|Briefly described|p 467|||||||||
8214|Heatherdale Shale|23818|5|Briefly described|p87 Fig.33|Cambrian|Cambrian|||||||
8214|Heatherdale Shale|23827|5|Briefly described|p260|Cambrian|Cambrian|||||||
8214|Heatherdale Shale|23854|5|Briefly described|p864|||Of Normanville Group.||||||
8214|Heatherdale Shale|23981|4|Described|p8-9 Fig. 4, p10 Fig. 5, p26|Early Cambrian|Early Cambrian|Supersedes Heatherdale Shales. Of Normanville Gp. Pyritic, calcareous shale and siltstone. Ages: 526+/4Ma, and 526+/-1.6Ma. Lower part is 300m thick. Geol.Prov: Stansbury Basin. Over Fork Tree Lst; interfingers with Truro Volca; overlain by Carrickalinga.||||||04-FEB-08
8214|Heatherdale Shale|24465|6|Mentioned|p358|Early Cambrian|Early Cambrian|Of Normanville Group.  Geological Province: Stansbury Basin.||||||19-JAN-05
8214|Heatherdale Shale|30051|6|Mentioned|Fig.1|||||||||
8214|Heatherdale Shale|30052|6|Mentioned|Fig.3|||Cambrian age.||||||
8214|Heatherdale Shale|30377|5|Briefly described|p202|||Lower Cambrian age||||||
8214|Heatherdale Shale|30378|6|Mentioned|p432|||||||||
8214|Heatherdale Shale|30381|6|Mentioned|Fig.4|||||||||
8214|Heatherdale Shale|30801|6|Mentioned|p5|||Lower Cambrian. Table p5-6.||||||12-FEB-07
8214|Heatherdale Shale|30805|6|Mentioned|p1|||||||||
8214|Heatherdale Shale|30807|6|Mentioned|p102|||Suggested map symbol||||||
8214|Heatherdale Shale|32547|6|Mentioned|p60|||L.Camb. Equiv. Unit of Hawker Gp.||||||12-FEB-07
8214|Heatherdale Shale|32551|5|Briefly described|p100|||Cambrian lithology.||||||15-JAN-08
8214|Heatherdale Shale|33224|6|Mentioned|Fig.37|||Photo.||||||
8214|Heatherdale Shale|33332|4|Described|p10|||See also pp 12 and 15. Lower Cambrian.||||||15-JAN-08
8214|Heatherdale Shale|33471|5|Briefly described|p555|||||||||
8214|Heatherdale Shale|33953|6|Mentioned|Fig.4|||Cambrian||||||
8214|Heatherdale Shale|34014|5|Briefly described|p23|||Cambrian||||||
8214|Heatherdale Shale|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Equiv.||||||
8214|Heatherdale Shale|34612|6|Mentioned|Fig.33|||Correlation chart. Cambrian||||||
8214|Heatherdale Shale|35255|6|Mentioned|Fig.8|||||||||
8214|Heatherdale Shale|36731|6|Mentioned|p125|||||||||
8214|Heatherdale Shale|38873|6|Mentioned|Table 2|||||||||
8214|Heatherdale Shale|39489|6|Mentioned|p8|||||||||
8214|Heatherdale Shale|39806|5|Briefly described|p207|||||||||
8214|Heatherdale Shale|40442|5|Briefly described|p16|||Also mention on Table 1.||||||
8214|Heatherdale Shale|40454|6|Mentioned|Table 1|||||||||
8214|Heatherdale Shale|40455|5|Briefly described|p69|||||||||
8214|Heatherdale Shale|40763|5|Briefly described|p206|||||||||
8214|Heatherdale Shale|40852|6|Mentioned|p33|||||||||
8214|Heatherdale Shale|40856|5|Briefly described|p312|||||||||
8214|Heatherdale Shale|41103|6|Mentioned|p261|||||||||
8214|Heatherdale Shale|41526|6|Mentioned|p39|||See also p61||||||12-FEB-07
8214|Heatherdale Shale|41853|6|Mentioned|p195|||See also p199.||||||12-FEB-07
8214|Heatherdale Shale|42192|6|Mentioned|p7|||||||||
8214|Heatherdale Shale|42222|6|Mentioned|p21|||||||||
8214|Heatherdale Shale|42225|6|Mentioned|Fig.4 P224|||||||||
8214|Heatherdale Shale|42232|6|Mentioned|p283|||||||||
8214|Heatherdale Shale|42266|5|Briefly described|p291|||||||||
8214|Heatherdale Shale|42268|6|Mentioned|p330|||||||||
8214|Heatherdale Shale|42270|5|Briefly described|p353|||See also Fig.3||||||
8214|Heatherdale Shale|42272|5|Briefly described|p404|||||||||
8214|Heatherdale Shale|42488|4|Described| 185, Fig.2 P187|||||||||
8214|Heatherdale Shale|43190|5|Briefly described|Fig.2p29,p34.|||U-Pb zircon age in tuff bed at Sellicks Hill: 526 +/-4 Ma. Of Normanville Group.||||||15-JAN-08
8214|Heatherdale Shale|43192|6|Mentioned|p63|||Of the Normanville Group.||||||12-FEB-07
8214|Heatherdale Shale|43560|6|Mentioned|Table 1,p231||Botoman|Age: 526+/-4 Ma (Early Cambrian).||||||12-FEB-07
8214|Heatherdale Shale|43703|6|Mentioned|p75||Botoman|||||||
8214|Heatherdale Shale|43759|4|Described|p446||Early Cambrian|||||||
8214|Heatherdale Shale|43781|6|Mentioned|p3|||||||||
8214|Heatherdale Shale|44133|5|Briefly described|p4 Fig. 7.2, 6, 14|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Normanville Group.||||||
8214|Heatherdale Shale|50154|5|Briefly described|p58|Early Cambrian|Early Cambrian|Age: 524 +/- 6 Ma (U/Pb). Of the Normanville Group.||||||
8214|Heatherdale Shale|60567|5|Briefly described|p41|||Of the upper part of the Normanville Group.||||||
8214|Heatherdale Shale|60712|5|Briefly described|p28 Fig. 1|Early Cambrian|Early Cambrian|Of the Normanville Group.||||||
8214|Heatherdale Shale|61307|5|Briefly described|p6 Fig. 3, p23|Cambrian|Cambrian|Of the Normanville Group. Geological Province: Adelaide Fold Belt.||||||15-JAN-08
8214|Heatherdale Shale|63848|4|Described|p531, p532, p533 Fig.2, p534 Fig.4.|Early Cambrian|Early Cambrian|Dated by a tuff in its upper part by Cooper et al. (1992) at 526 +/- 4 Ma; recalculated by Jenkins et al.|522.0 +/- 2.1 Ma (Jenkins et al. 2002).|Unit in Normanville Group.||Overlies Fork Tree Limestone. Is overlain by Carrickalinga Head Formation.|Mainly pale- to dark-grey laminated phyllite with interbedded lava (including pillow lava), tuffs, and volcaniclastic sediments.|
8214|Heatherdale Shale|64571|6|Mentioned|p828|Early Cambrian|Early Cambrian|Age: 526+/-4Ma (SHRIMP). SA.||||||15-DEC-08
8214|Heatherdale Shale|65375|5|Briefly described|p33, p55.|Early Cambrian|Early Cambrian|Stansbury Basin, Yorke Peninsula. Possible hydrocarbon source rock (TOC max. = 2.43%, mean = 0.64%).||Unit in Normanville Group.||Overlies Fork Tree Limestone.||
8214|Heatherdale Shale|65379|5|Briefly described|p643, p644, p646|Cambrian|Cambrian|Of Normanville Group, Moralana Supergroup. Shales; limestone with rare trilobites, hyoliths, sponge spicules, gastropods and worm tracks. N.B. Asbestos deposit host, contains Dutton 2 asbestos prospect.||||||07-MAR-12
8214|Heatherdale Shale|65664|5|Briefly described|p1096, p1103|Early Cambrian|Early Cambrian||Tuff dated at 522 +/ - 2 Ma.|Of Normanville Group.||||09-MAY-12
8214|Heatherdale Shale|65686|5|Briefly described|p420||Cambrian|Stansbury Basin.|522 +/- 2 Ma from tuff horizon.|||Overlain unconformably by Kanmantoo Group.||07-MAY-12
8214|Heatherdale Shale|65892|4|Described|p9 Fig.4, p15, p17, p19. |Early Cambrian|Early Cambrian|Fleurieu Peninsula. Age from a tuff bed; recalculated from 526 +/- 4 Ma (Cooper et al., 1992). Rare fossils include hyoliths, helcionellids, lingulate brachiopods and arthropods. Trace fossils locally abundant.|522 +/- 2 Ma (Pb-U SHRIMP; Jenkins et al., 2002).|Unit in Normanville Group.||Conformably overlies Fork Tree Limestone. Is disconformably overlain by Carrickalinga Head Formation.|Lower calcareous member and an upper black shale and siltstone unit; nodules and stringers of black phosphate common locally.|
8214|Heatherdale Shale|66623|5|Briefly described|p430.|||||||Is overlain by Carrickalinga Head Formation.|Well-bedded and laminated muddy limestones and calcareous siltstones and mudstones.|
8214|Heatherdale Shale|66761|5|Briefly described|p254|Cambrian|Cambrian|Deepwater shale. Fleurieu Peninsula. Younger than Fork Tree Limestone, older than Kanmantoo Group.||||||14-MAR-12
8214|Heatherdale Shale|67344|5|Briefly described|p264|Cambrian|Cambrian|~335m thick. Deposited in a more distal, outer ramp setting. Age defined by the partly contemporaneous Emu Bay Shale.|||||Succession of dark grey calcareous shale and siltstone, variously pyritic and rich in nodular phosphate.|
8214|Heatherdale Shale|68735|5|Briefly described|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Of the Normanville Group.||||
8214|Heatherdale Shale|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Fleurieu Peninsula.||Of the Normanville Group.||||
8214|Heatherdale Shale|70125|6|Mentioned|p400 Tb.5||||526 Ma (tuff: Haines and Flottmann, 1998).|||||
8214|Heatherdale Shale|70660|5|Briefly described|p35, p37-p40, p46|Early Cambrian|Early Cambrian|This unit is in unconformable contact with the Port Willunga Formation [however the author doesn't state what their relationship is].||||Overlies the Christies Beach Formation. Unconformably overlain by the Port Willunga Formation.||
8214|Heatherdale Shale|70744|6|Mentioned|p941|||Delamerian Orogen. Contains abundant "Grenville-age" detrital zircons (1.3 - 1 Ga).||||||
8214|Heatherdale Shale|70833|5|Briefly described|p200,202|Cambrian|Cambrian|Of Eastern Stansbury Basin. Deepwater facies, recording relatively slow continuous basinal depositional cycles. Includes D. odyssei and M. etheridgei zones in the upper and lower parts of the section respectively. Equivalent to Parara Limestone, and Mernmerna Formation and Ajax Limestone (D. odessei zone), and to Wilkawillina (Hideaway Well and Winnitinny Creek members) and Wirrapowie limestones (M. etheridgei zone).||||Overlain unconformably by Kanmantoo Group. Underlain by Fork Tree Limestone.||
8214|Heatherdale Shale|71102|6|Mentioned|p254|||Of Stansbury Basin.||||||
8214|Heatherdale Shale|71593|5|Briefly described|p22|||||||Overlain by the Kanmantoo Group.||
8214|Heatherdale Shale|72450|5|Briefly described|Brochure map||||c. 520 Ma|Normanville Group|||Dark grey, slaty siltstone with black phosphate nodules.|
8214|Heatherdale Shale|73059|6|Mentioned|p1061|||||Normanville Group.||||
8214|Heatherdale Shale|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Pyritic, calcareous shale and siltstone; thin tuff bed.|09-DEC-21
8214|Heatherdale Shale|73188|5|Briefly described|p315-316, p336-338, p353, p356, p358|Early Cambrian|Early Cambrian|Mount Lofty Ranges. Extensional tectonism commenced during deposition.||Normanville Group||Disconformably overlain by Kanmantoo Group.|Carbonaceous siltstone.|
8214|Heatherdale Shale|73247|6|Mentioned|p205|Cambrian (Stage 4)|Cambrian (Stage 3)|Fleurieu Peninsula.||||Underlain by Fork Tree Limestone. Unconformably overlain by Kanmantoo Group.||
8214|Heatherdale Shale|73264|6|Mentioned|p1387 Fig.10|||||Normanville Group||||
8214|Heatherdale Shale|73430|5|Briefly described|p492||||514.98+/-0.22 Ma (Betts et al., 2018)|Normanville Group|||Thin-bedded turbidites.|
8214|Heatherdale Shale|74367|5|Briefly described|p19|Early Cambrian|Early Cambrian|Age revised from 526+/-4 Ma (COOPER et al., 1992), which was revised to 522+/-2 Ma (Jenkins et al., 2002) and later revised by Betts et al., (2018).|514.98+/-0.22 Ma U-Pb SHRIMP zircon|Normanville Group, top||Stratigraphically equivalent to Mernmerna Formation.||
8235|Hebden Gully Coal Member|29942|4|Described|Fig.2|||Permian||||||
8248|Heifer Creek Sandstone Member|13516|5|Briefly described|p159 fig 8|Middle Jurassic|Middle Jurassic|From Clarence-Moreton Basin.||of Koukandowie Formation||||
8248|Heifer Creek Sandstone Member|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup, Bundamba Group). Coarse quartz arenite, granule conglomerate. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|22865|6|Mentioned|Fig.22.10ap318|||||||||
8248|Heifer Creek Sandstone Member|23799|5|Briefly described|p47|Middle Jurassic|Middle Jurassic|See also Heifer Creek Sandstone. Of the Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.  See also p34 Fig. 3.||||||
8248|Heifer Creek Sandstone Member|23812|5|Briefly described|p34 Tb.4|Middle Jurassic|Early Jurassic|Of Koukandowie Formation.  Geological Province:Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Early Jurassic|Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|30058|6|Mentioned|p4|||Refers to McTaggart(1963)||||||
8248|Heifer Creek Sandstone Member|31118|6|Mentioned|p320|||||||||
8248|Heifer Creek Sandstone Member|33381|4|Described|p117|||See also P118. L.-M. Jur. Marburg Fm.||||||
8248|Heifer Creek Sandstone Member|33476|6|Mentioned|Table 6 P100|||Refers Swindon 1971||||||
8248|Heifer Creek Sandstone Member|37375|6|Mentioned|p472|||||||||
8248|Heifer Creek Sandstone Member|37436|6|Mentioned|p540|||||||||
8248|Heifer Creek Sandstone Member|37463|6|Mentioned|p483|||||||||
8248|Heifer Creek Sandstone Member|38205|6|Mentioned|p84|||Member of Marburg Formation.||||||
8248|Heifer Creek Sandstone Member|38441|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8248|Heifer Creek Sandstone Member|39907|5|Briefly described|p9|||||||||
8248|Heifer Creek Sandstone Member|40623|5|Briefly described|p107|||||||||
8248|Heifer Creek Sandstone Member|41631|4|Described|p19|||See also Fig.2||||||
8248|Heifer Creek Sandstone Member|41906|3|Fully described|Table 2 P15|||See also P32||||||
8248|Heifer Creek Sandstone Member|42248|1|Redefined|App.1 P411|Early Jurassic||||||||
8248|Heifer Creek Sandstone Member|42463|6|Mentioned|Fig.3 P170|||||||||
8248|Heifer Creek Sandstone Member|42869|5|Briefly described|Table 1, P33|||of Koukandowie formation||||||
8248|Heifer Creek Sandstone Member|42951|5|Briefly described|Fig.11|||of Koukandowie Formation||||||
8248|Heifer Creek Sandstone Member|43993|2|Defined|p93,97,100||Triassic|Unit of Marburg Formation.||||||
8248|Heifer Creek Sandstone Member|44026|14|Not recorded|p123||Jurassic|Ref. to McTaggart 1963||||||
8248|Heifer Creek Sandstone Member|44028|14|Not recorded|Fig.2,p509||Jurassic|Of Marburg Formation. See Strat Table.||||||
8248|Heifer Creek Sandstone Member|44032|14|Not recorded|p462,464,465|||Part of Marburg Formation.||||||
8248|Heifer Creek Sandstone Member|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||20-JUL-04
8248|Heifer Creek Sandstone Member|60281|5|Briefly described|p30, Fig.18 App 1|Early Jurassic|Early Jurassic|Of the Koukandowie Formation. Coarse quartz sandstone, granite conglomerate.  Max. thickness: 50m.  Geological Province: Clarence-Moreton Basin.  See also the misspelt Heffer Creek Sandstone Member.||||||20-JAN-05
8248|Heifer Creek Sandstone Member|60993|4|Described|p6 Fig. 2, p27|||First named by Gray (1975 as part of Marburg Fm), and retained in current use as member of Koukandowie Fm (Marburg Subgrp). Tough, quartzose sst, cross-bedded. Geol. Prov: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|60995|4|Described|p66, p51 Fig. 3|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup). Coarse quartz sandstone, granite conglomerate. Overlies Ma Ma Creek Member. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin. ||||||
8248|Heifer Creek Sandstone Member|60996|5|Briefly described|p72|||Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|60997|5|Briefly described|p140 Fig. 2|||Superseded by Heifer Creek Member. Formerly part of McTaggart's Marburg Formation (1963).||||||
8248|Heifer Creek Sandstone Member|60998|5|Briefly described|p146 Fig. 2|||Consists of fluvial stacked channel sand. Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|60999|6|Mentioned|p174|||Probably should be Heifer Creek Member - names used interchangeably.||||||
8248|Heifer Creek Sandstone Member|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
8248|Heifer Creek Sandstone Member|61006|5|Briefly described|p278|||Of the Koukandowie Formation. Quartzose sandstone unit (sheet-like braided-stream deposits) with potential as reservoir rocks. See also Heifer Creek Member - names used interchangeably. See also p279 Tb. 1, p285.||||||
8248|Heifer Creek Sandstone Member|64665|5|Briefly described|p53 Fig.2.|Middle Jurassic|Middle Jurassic|Clarence-Moreton Basin. Correlates with Hutton Sandstone (Eromanga and Surat basins).||Upper unit in Koukandowie Formation.||Overlies Ma Ma Creek Member. Is overlain by Walloon Coal Measures.||
8248|Heifer Creek Sandstone Member|67402|4|Described|p187, p190 fig CLM6, p193|Aalenian|Pliensbachian|Clarence-Moreton Basin. Represents a change in depositional environment from floodplain back to braided stream deposition. ||Koukandowie Formation||Overlies the Ma Ma Creek Member. Overlain by the Walloon Subgroup.|Thick to very thickly bedded, coarse to very coarse-grained, white to grey, quartzose and minor quartz lithic sandstone and granule conglomerate.|
8248|Heifer Creek Sandstone Member|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. 10-50m thick. Deposited as channel fill deposits in a meandering fluvial system. Good reservoir potential in coarse sandstone and granule conglomerates. ||Koukandowie Formation||Overlies the Ma Ma Creek Member.|Coarse quartz sandstone and granite conglomerate.|
8248|Heifer Creek Sandstone Member|69594|5|Briefly described|p519, p544, p573|Middle Jurassic|Middle Jurassic|Clarence-Moreton Basin. Diachronous. Forms prominent topographic features. Appears as Heifer Creek Sandstone on p544.||Koukandowie Formation.||Overlies Ma Ma Creek Member. Is overlain by Walloon Coal Measures.|Coarse-grained, cross-bedded, quartzose sandstone.|
8248|Heifer Creek Sandstone Member|69790|5|Briefly described|p1063 Fig.2|Middle Jurassic|Middle Jurassic|Northern Clarence-Moreton Basin area.||Unit in Koukandowie Formation.||||
8248|Heifer Creek Sandstone Member|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
8248|Heifer Creek Sandstone Member|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Koukandowie Formation.||Overlies Ma Ma Creek Member.||
8248|Heifer Creek Sandstone Member|71805|5|Briefly described|p76|Bajocian|Aalenian|Clarence-Moreton Basin.||Koukandowie Formation||Overlies the Ma Ma Creek Sandstone Mmeber.||
8248|Heifer Creek Sandstone Member|72297|5|Briefly described|p746|||Clarence-Moreton Basin. Hydrocarbon reservoir potential.||Marburg Subgroup.||||
8271|Helms moraine|34367|6|Mentioned|p571|||||||||
8273|Henry River Granite|22490|5|Briefly described|4|Early Permian|Early Permian|Geol. Province: New England Fold Belt.||||||15-JAN-08
8273|Henry River Granite|23811|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Hillgrove Plutonic Suite.  Foliated, fine-grained, biotite granite (monzogranite?); characterised by an irregular texture and blue quartz; with common metasedimentary enclaves.||||||20-DEC-04
8273|Henry River Granite|23812|5|Briefly described|p22 Tb.2, p14|Early Permian|Early Permian|Of Hilgrove Plutonic Suite.||||||
8273|Henry River Granite|29988|6|Mentioned|Map legend|Permian|Permian|||||||
8273|Henry River Granite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
8273|Henry River Granite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
8273|Henry River Granite|35257|6|Mentioned|Fig.12|||||||||
8273|Henry River Granite|40679|6|Mentioned|Fig.1 REF|||||||||
8273|Henry River Granite|60079|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Hillgrove Suite.||||||21-JUL-04
8273|Henry River Granite|69639|6|Mentioned|p217|Sakmarian|Sakmarian||293.1 +/- 5.1 Ma (SHRIMP U-PB)|Hillgrove Supersuite||||
8273|Henry River Granite|71628|6|Mentioned|p3:51|||Pogson and Hitchins (1973). Renamed here.||||||
8277|Hensleigh Siltstone|13139|5|Briefly described|p8|Bendigonian|Bendigonian|Overlain by the Fairbridge Volcanics.||||||
8277|Hensleigh Siltstone|13995|5|Briefly described|p89, p99|||Northern Molong High. Contains a recently-recognised, early Bendigonian conodont fauna (species listed).||||||
8277|Hensleigh Siltstone|22857|4|Described|p426 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Laminated graptolitic siltstone; minor volcaniclastic sandstone, allochthonous limestone. Max. thickness: 310m. ||||||
8277|Hensleigh Siltstone|23043|5|Briefly described|Map Legend|Bendigonian|Bendigonian|||||||
8277|Hensleigh Siltstone|23170|2|Defined|p26 Fig.3|Bendigonian|Bendigonian|Age: Early Bendigonian. represents a cessation of volcanic activity.||||||
8277|Hensleigh Siltstone|23213|3|Fully described|p10, Fig.10|Bendigonian|Bendigonian|see also Fig.2&6. Conodont asemblage resembles that in Emmanuel Formation, Canning Basin. of Northern Molong Volcanic Belt. Age: Early to Middle Bendigonian.||||||
8277|Hensleigh Siltstone|23214|5|Briefly described|p24|Early Ordovician|Early Ordovician|||||||
8277|Hensleigh Siltstone|23334|6|Mentioned|8|||||||||
8277|Hensleigh Siltstone|23739|4|Described|p212|Early Ordovician|Early Ordovician|Geological Province: Lachlan Fold Belt.||||||
8277|Hensleigh Siltstone|24398|4|Described|p261|Early Ordovician|Early Ordovician|Deepwater deposit of laminated siltstone and shale with interbedded volcaniclastic sandstone at base.  Overlies the Mitchell Formation.  Geological Province: Lachlan Fold Belt.||||||
8277|Hensleigh Siltstone|35118|6|Mentioned|Fig.5|||||||||
8277|Hensleigh Siltstone|35415|6|Mentioned|Fig.2|||Stratigraphic correlations.||||||
8277|Hensleigh Siltstone|40136|5|Briefly described|p27|||See also P17 and P24||||||
8277|Hensleigh Siltstone|40746|5|Briefly described|p359|||||||||
8277|Hensleigh Siltstone|50097|3|Fully described|p39, 41|Bendigonian|Bendigonian|Lamninated calcareous siltstones+ limestones, with minor volcaniclastic sandstone. Thickness: 310 m-2 km. Conformably overlies Mitchell Formation, unconformably overlain by Fairbridge Volcanics. Geol Prov: Lachlan Orogen.||||||07-FEB-11
8277|Hensleigh Siltstone|63121|5|Briefly described|p225 Fig. 2, p226|Bendigonian|Bendigonian|In Bakers Swamp area, south of Wellington, NSW.||||||13-MAR-07
8277|Hensleigh Siltstone|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a|Middle Ordovician|Early Ordovician|Overlain unconformably by Fairbridge Volcanics, underlain conformably + transitionally by Mitchell Formation. Geol Prov: Molong Volcanic Belt, LBF. Has conodont zone faunas in carbonates in lower part of unit + graptolite fauna in upper beds.||||||07-FEB-11
8277|Hensleigh Siltstone|63283|5|Briefly described|p199, p194 Fig. 2, p208|Early Ordovician|Early Ordovician|Overlain by Wahringa Limestone Member. Geological Province: Molong Volcanic Belt. Carbonates in this unit conatin conodonts.||||||07-FEB-11
8277|Hensleigh Siltstone|63286|6|Mentioned|p308 Fig. 9|Early Odrovician|Early Ordovician|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
8277|Hensleigh Siltstone|63287|6|Mentioned|p317 Fig. 2|Early Ordovician|Early Ordovician|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
8277|Hensleigh Siltstone|63293|6|Mentioned|p468 Fig. 2|Early Ordovician|Early Ordovician|Underlain by Mitchell Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
8277|Hensleigh Siltstone|67106|6|Mentioned|p672-675, 681|Early Ordovician|Early Ordovician|Molong Volcanic Belt, Lachlan Orogen.|481.5 to 476.7 Ma.|||Transitionally overlies Mitchell Formation.||
8277|Hensleigh Siltstone|67322|5|Briefly described|Fig.5, p23|Floian|Floian|Macquarie Arc. Defined by Wolf et al. (1968). Conodont fauna in the lower part of this unit are Bendigonian in age. Bakers Swamp area.||||Conformably overlies Mitchell Formation.||22-FEB-18
8277|Hensleigh Siltstone|68592|5|Briefly described|p370|Early Ordovician|Early Ordovician|South of Wellington. Is not included in the much younger Cabonne Group.||||Conformably overlies Mitchell Formation. Is overlain unconformably by Cabonne Group.||
8277|Hensleigh Siltstone|70684|5|Briefly described|p3, p12, p18-26, p58, p74|Early Ordovician|Early Ordovician|Northern Molong Volcanic Belt. c.310m thick. Lithologically very similar to Yarrimbah Formation, and only slightly younger. Fossils (listed) indicate a late Bendigonian age.||||Conformably overlies Mitchell Formation.|Thinly bedded sandstone, siltstone and shale and granule conglomerate; carbonates at the base, with graptolitic siltstone higher up. Contains clasts of trachyandesite, vesicular basalt and monzonite.|
8277|Hensleigh Siltstone|72263|6|Mentioned|p515|||Geological province: Lachlan Orogen. See Hensleigh Formation.||||||
8329|Higgins Creek Conglomerate|34040|6|Mentioned|p384|||||||||
8329|Higgins Creek Conglomerate|34585|4|Described|p380|||Permian||||||
8329|Higgins Creek Conglomerate|34605|6|Mentioned|Fig.5.28|||||||||
8329|Higgins Creek Conglomerate|37804|6|Mentioned|Table 1|||||||||
8329|Higgins Creek Conglomerate|39232|6|Mentioned|p108|||||||||
8329|Higgins Creek Conglomerate|40806|6|Mentioned|p152|||||||||
8329|Higgins Creek Conglomerate|45090|5|Briefly described|p183|||||||||
8336|Highfields Formation|22578|6|Mentioned|p401|||||||||
8336|Highfields Formation|34351|5|Briefly described|p344|||Fig.5.13 - proposed name change to Glebe Formation.||||||
8336|Highfields Formation|43344|14|Not recorded|p85||Permian|||||||
8336|Highfields Formation|43447|14|Not recorded|diag.p26|||Part of Cardiff Sub-Group||||||
8336|Highfields Formation|43448|14|Not recorded|p224||Permian|On table only. Unit of Cardiff Subgroup. (Newcastle Coal Measures)||||||
8337|Highlands Complex|23720|5|Briefly described|Map Legend|Late Permian||Hypersthene-augite-amphibole-biotite monzonite, amphibole-biotite monzogranite, syenite.||||||15-DEC-04
8337|Highlands Complex|42866|5|Briefly described|Table 2, P12|||Variation of Highlands Monzonite?||||||25-MAY-06
8337|Highlands Complex|44450|6|Mentioned|p26.|||||||||
8337|Highlands Complex|62757|6|Mentioned|p13 Fig. 5, p16 Fig.6|||Granitoid of the Moonbi Supersuite.||||||07-FEB-11
8337|Highlands Complex|69188|4|Described|p1-2, p5, p60-63, p79|Early Triassic|Early Triassic|Same age as the main magmatic stages of the Moonbi and Uralla Supersuites. Geochemically unique; described as "a poor fit in the Moonbi Supersuite, to which it is sometimes ascribed".|251.5 +/- 1.9 Ma(magmatic age)|Moonbi Supersuite.||Intrudes Sandon beds and Dummy Creek Conglomerate.|Includes pink medium-grained alkali feldspar-rich biotite-amphibole monzogranite.|16-APR-20
8337|Highlands Complex|71628|4|Described|p1:6; p13: 1-23, 25, 27|||Binns et al. (1967). History of its complex nomenclature explained. Occurs 17-20 km NNE of Armidale. Metamorphic aureole described. Other age determinations given. Petrology detailed; geochemistry described. I-type. Asociated with minor Sb (Ag) mineralisation. Numerous small bodies (""masses"") are described.",,|251.5 +/- 1.9 Ma (SHRIMP: Cross and Blevin, 2013).|Highlands Suite.||Intrudes Sandon Association, Sandon beds, Girrakool beds, Dummy Creek Conglomerate.|Cpx-opx-biotite-(+/- olivine, +/- amphibole)-bearing high-K granite complex dominated by quartz monzonite and quartz-poor monzonite, with minor marginal quartz syenite to syenite, rare (quartz)-alkali feldspar syenite, and alkali feldspar granite.|
8344|Hill 60 Member|31586|6|Mentioned|p6|||Equiv. upper part Cannindah Lst.||||||
8344|Hill 60 Member|31587|6|Mentioned|p67|||Rugose corals||||||
8344|Hill 60 Member|32286|6|Mentioned|p50|||||||||
8344|Hill 60 Member|32866|6|Mentioned|p13|||Fossil content||||||
8344|Hill 60 Member|34081|6|Mentioned|p260|||||||||
8344|Hill 60 Member|34083|6|Mentioned|p248|||||||||
8344|Hill 60 Member|37987|6|Mentioned|p229|||||||||
8344|Hill 60 Member|43418|14|Not recorded|Map Legend|||||||||
8344|Hill 60 Member|43432|14|Not recorded|p203||Visean|||||||
8344|Hill 60 Member|45097|6|Mentioned|p24|||Late Visean corals.||||||
8346|Hill End conglomerate|37433|6|Mentioned|p244|||||||||
8354|Hillsborough Tuff Member|29926|6|Mentioned|Fig.3|||||||||
8354|Hillsborough Tuff Member|33867|6|Mentioned|Fig.3|||||||||
8354|Hillsborough Tuff Member|34351|6|Mentioned|Fig.5.13|||Proposed name change from Wave Hill Tuff Member.||||||
8354|Hillsborough Tuff Member|37083|6|Mentioned|p164|||||||||
8354|Hillsborough Tuff Member|39292|6|Mentioned|Fig. 6.2|||||||||
8354|Hillsborough Tuff Member|41479|6|Mentioned|Fig.2|||||||||
8354|Hillsborough Tuff Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Kahibah Formation.||||
8357|Hillsdale Coal Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Dights Creek Coal.  Equivalent to the Wallarah and Great Northern seams (Newcastle Coal Measures)   Geological Province: Sydney Basin||||||
8357|Hillsdale Coal Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Dights Creek Coal. Geological Province: Sydney Basin||||||
8357|Hillsdale Coal Member|29942|4|Described|Fig.2|||Permian||||||
8357|Hillsdale Coal Member|68004|5|Briefly described|p51 Table 5, p53.|Late Permian|Late Permian|Upper Hunter Coalfield.||Top unit in Dights Creek Coal.||Overlies Naleen Tuff Member. Is overlain by Redmanvale Creek Formation.||
8363|Hilltop Coal Member|37773|6|Mentioned|p19|||||||||
8363|Hilltop Coal Member|39346|6|Mentioned|Map legend|Permian|Permian|||||||
8363|Hilltop Coal Member|40331|6|Mentioned|p13|||||||||
8363|Hilltop Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Rowan Formation. ||||
8373|Himalaya Formation|6823|5|Briefly described|p205, 207-208|Palaeoproterozoic|Palaeoproterozoic|U-Pb SHRIMP maximum depositional ages of Love (1992).|1762 +/- 17 Ma; 1793 +/- 22 Ma (Max dep, U-Pb)|Thackaringa Group||||26-MAR-22
8373|Himalaya Formation|22553|5|Briefly described|p75,fig2p77|Statherian|Statherian|Part of Willyama Supergroup.||||||11-JUN-08
8373|Himalaya Formation|22575|6|Mentioned|p179 Fig.2|||Of the Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|22641|5|Briefly described|Fig. 2 p689, p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|22720|6|Mentioned|p 168|||Of the Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|22771|6|Mentioned|Table12.2p45,45|||||||||
8373|Himalaya Formation|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Lateral equivalent of Rasp Ridge Gneiss. Max. thickness: 1000m. Geological Province: Willyama Fold Belt. ||||||07-NOV-08
8373|Himalaya Formation|22884|6|Mentioned|p43 Fig. 3|||Of the Thackaringa Group. Geological province: Broken Hill Domain.||||||30-APR-13
8373|Himalaya Formation|22965|6|Mentioned|p13, Fig1||Statherian|Part of the Thackaringa Group.||||||
8373|Himalaya Formation|22966|6|Mentioned|Fig 1||Proterozoic|Rift stage of geological development.||||||
8373|Himalaya Formation|22967|6|Mentioned|p39||Statherian|||||||
8373|Himalaya Formation|23025|6|Mentioned|Fig1p75|||||||||
8373|Himalaya Formation|23160|6|Mentioned|fig1|||||||||
8373|Himalaya Formation|23223|5|Briefly described|p39|||Described in article as 'upper albite - Himalaya Formation (UA-HF)'. Within the Willyama Supergroup.||||||16-JAN-07
8373|Himalaya Formation|23248|5|Briefly described|Fig2p169|||||||||
8373|Himalaya Formation|23461|5|Briefly described|p204 Fig. 3|||Of Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|24307|5|Briefly described|p973|Proterozoic|Proterozoic|Of the Thackaringa Group.   Geological Province: Broken Hill Block||||||16-JAN-07
8373|Himalaya Formation|38969|4|Described|p206|||||||||
8373|Himalaya Formation|39662|2|Defined|p420|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|39674|6|Mentioned|p204|||||||||
8373|Himalaya Formation|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8373|Himalaya Formation|39849|6|Mentioned|Table 2|||||||||
8373|Himalaya Formation|40290|6|Mentioned|p1|||||||||
8373|Himalaya Formation|40822|6|Mentioned|Fig.2|||||||||
8373|Himalaya Formation|41093|6|Mentioned|p252|||||||||
8373|Himalaya Formation|41145|6|Mentioned|Fig.4|||||||||
8373|Himalaya Formation|41630|6|Mentioned|p45|||||||||
8373|Himalaya Formation|41633|6|Mentioned|p141|||||||||
8373|Himalaya Formation|42261|6|Mentioned|Fig 1 P530|||||||||
8373|Himalaya Formation|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8373|Himalaya Formation|42537|4|Described|p11|||||||||
8373|Himalaya Formation|42595|6|Mentioned|Fig. 2 P5|||||||||
8373|Himalaya Formation|42813|6|Mentioned|p10|||Of Thackaringa Group.||||||16-JAN-07
8373|Himalaya Formation|42897|5|Briefly described|p323|||see also Fig.3, p321.||||||16-JAN-07
8373|Himalaya Formation|43052|6|Mentioned|Fig.4.22|||||||||
8373|Himalaya Formation|43086|6|Mentioned|Fig.3|||||||||
8373|Himalaya Formation|43264|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
8373|Himalaya Formation|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43267|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43268|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|43572|6|Mentioned|Fig.3.2 p6|||||||||
8373|Himalaya Formation|46598|5|Briefly described|p303|||||||||
8373|Himalaya 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 Broken Hill Group (Allendale Metasediments); underlain by Cues Formation.||||||31-MAY-07
8373|Himalaya Formation|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Himalaya Suite. Geological Province: Broken Hill Block. Age: 1750-1860Ma (U-Pb). Intruded by Potosi Supersuite.||||||07-NOV-08
8373|Himalaya Formation|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
8373|Himalaya Formation|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group.  Geological Province: Broken Hill Domain.||||||03-MAR-05
8373|Himalaya Formation|61258|5|Briefly described|p399|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Age: <1710+/-5Ma and >1704+/-3Ma (Page et al 2000a,b). Geological Province: Broken Hill-Olary region.||||||07-NOV-08
8373|Himalaya Formation|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group.||||||07-NOV-08
8373|Himalaya Formation|61735|5|Briefly described|p635 Fig. 1, p636 Fig.2,  639|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Ages: </-1710-1700Ma and >1690+/-11Ma. Max depositional age ~1730 Ma, metamorphic age from rutile 1595+/-6 Ma U/Pb SHRIMP.||||||04-JUN-15
8373|Himalaya Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological province: Olary Domain.||||||
8373|Himalaya Formation|62373|6|Mentioned|p508|||||||||
8373|Himalaya Formation|62473|5|Briefly described|p72|Paleoproterozoic|Paleoproterozoic|Age: ca.1710Ma. Thin bedded quartz-albite rocks.||||||17-JUN-09
8373|Himalaya Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1730-c.1720 Ma.|Thackaringa Group.||||
8373|Himalaya Formation|62536|5|Briefly described|p636, 639-642, 655|||Broken Hill area. Metamorphosed at 1595 +/- 6 Ma. Appears only as Himalaya on p636.|~1730 Ma (MDA).|Thackaringa Group.|||Extensive quartz-albite metasedimentary rocks; some with climbing ripples indicate sandstone progenitors.|
8373|Himalaya Formation|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
8373|Himalaya Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Thackaringa Group||||15-DEC-21
8373|Himalaya Formation|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
8373|Himalaya Formation|63110|6|Mentioned|p1132|||Albite-rich rocks.||||||11-JUN-08
8373|Himalaya Formation|63519|5|Briefly described|p5, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Age: 1710-1700Ma. Mentioned in Abstract also. See also p9, p10 Fig. 3.. ||||||07-NOV-08
8373|Himalaya Formation|63866|5|Briefly described|p36|||Broken Hill Domain, Curnamona Province.|<1704 Ma|Thackaringa Group||||
8373|Himalaya Formation|64097|5|Briefly described|p303, p317|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Ages: ca1798+/-15Ma, 1762+/-17Ma, ca1720Ma (all zircon). Max. age considered to be close to +1730Ma.||||||07-FEB-11
8373|Himalaya Formation|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group (Willyama Supergroup). Geological Province: Broken Hill Block.||||||07-FEB-11
8373|Himalaya Formation|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological province: Broken Hill Domain.||||||30-APR-13
8373|Himalaya Formation|64742|6|Mentioned|p321 Fig.3. ||||<1710-1700 Ma.|Unit in Thackaringa Group.||||
8373|Himalaya Formation|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Thackaringa Group. Geological province: Broken Hill Domain.||||||30-APR-13
8373|Himalaya Formation|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. ||Thackaringa Group||Overlies the Cues Formation. Overlain by the Allendale Metasediments.||
8373|Himalaya Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.||Thackaringa Group.||||
8373|Himalaya Formation|68126|5|Briefly described|p31|Paleoproterozoic|Paleoproterozoic||||||Medium-grained saccharoidal leucocratic psammitic and albitic metasediment. Variably-interbedded albite-quartz rich rocks, composite gneiss, basic gneiss, horizons of thinly-beded quartz-magnetite rock. Pyrite-rich rocks towards bottom.|
8373|Himalaya Formation|70000|5|Briefly described|p34-36|Statherian|Statherian|Hosts cobalt-rich pyritic horizons at Pyrite Hill and Big Hill. Protolith probably sandy marine shelf sediments with variable evaporitic or hypersaline component.||Unit in Thackaringa Group.||Overlies Cues Formation.||
8373|Himalaya Formation|70014|5|Briefly described|Map legend|||Plagioclase-quartz rocks are well-bedded (beds 20 - 30mm thick), with rare scour-and-fill and crossbed structures. Thin to thick (0.5 - 10m) horizons of thinly-bedded quartz-magnetite rock also occur with the plagioclase-quartz rocks. In some areas the Formation consists of thin interbeds of plagioclase-quartz rocks within metasediments or metasedimentary composite gneiss.||Unit in Thackaringa Group.||Overlies Cues Formation. Is overlain by Allendale Metasediments (Broken Hill Group).|Extensive bodies of medium-grained, saccharoidal leucocratic sodic plagioclase-quartz(-K-feldspar)(-biotite) rocks, with variably developed interbedded metasedimentary composite gneiss, and basic gneiss; pyrite-rich rocks occur towards the base.|
8373|Himalaya Formation|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Thackaringa Group.||Overlies Cues FZ.|Albite-quartz +/- K feldspar +/- biotite rock, with variably interbedded metasedimentary composite gneiss and basic gneiss; horizons of quartz-magnetite rock; locally pyritic.|
8373|Himalaya Formation|70405|6|Mentioned|p9 table 1, p40|Paleoproterozoic|Paleoproterozoic||1700 Ma|Thackaringa Group||||
8373|Himalaya Formation|70657|5|Briefly described|p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|~1700 Ma.|Thackaringa Group||Overlies Cues Formation. Underlies Allendale Metasediments (Broken Hill Group). Is intruded by Georges Bore Granite Gneiss and Rasp Ridge Granite Gneiss of Silver City Suite.||
8373|Himalaya Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Thackaringa Group.||||
8373|Himalaya Formation|72004|6|Mentioned|p85|||Broken Hill region.||Unit of Thackaringa Group.||Uppermost unit of the Thackaginga Group.||
8373|Himalaya Formation|72461|6|Mentioned|p13, p16-17|||||Thackaringa Group||Overlies the Cues Formation. Overlain by the Allendale Metasediments.||
8373|Himalaya Formation|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Thackaringa Group||Overlies Cues Formation||
8373|Himalaya Formation|73482|6|Mentioned|p422 Fig.3|||||Thackaringa Group||||
8373|Himalaya Formation|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p831 Fig.5|Statherian|Statherian||<1710-1700 Ma, >1690+/-11 Ma|Thackaringa Group||Overlies Cues Formation, underlies Allendale Metasediments||
8391|Hobden Gully Coal Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Dights Creek Coal. Geological Province: Sydney Basin||||||
8391|Hobden Gully Coal Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Dights Creek Coal. Geological Province: Sydney Basin||||||
8391|Hobden Gully Coal Member|29942|4|Described|Fig.1|||||||||
8395|Hobwee Basalt|22773|5|Briefly described|p345|||||||||
8395|Hobwee Basalt|22857|5|Briefly described|p345|Cenozoic|Cenozoic|Included in the central-volcano provinces of NSW. Max. thickness: 600m. ||||||19-NOV-08
8395|Hobwee Basalt|30604|6|Mentioned|p66|||||||||
8395|Hobwee Basalt|30687|4|Described|p65|||See also P67,68,76. Tertiary age||||||
8395|Hobwee Basalt|30689|5|Briefly described|p76|||Also mention P73||||||
8395|Hobwee Basalt|31130|6|Mentioned|Fig. 2|||L. Miocene||||||
8395|Hobwee Basalt|32924|4|Described|p112|||Tholeiitic. Thickest N. of Mt. Warning||||||
8395|Hobwee Basalt|33290|4|Described|p38|||Anal. P39||||||
8395|Hobwee Basalt|35296|5|Briefly described|p14|||See also P12.||||||
8395|Hobwee Basalt|36806|6|Mentioned|p131|||||||||
8395|Hobwee Basalt|39445|5|Briefly described|Table 14|||||||||
8395|Hobwee Basalt|40623|5|Briefly described|p39|||||||||
8395|Hobwee Basalt|40896|4|Described|p9|||||||||
8395|Hobwee Basalt|43161|4|Described|13, 14|||Dated: 20.5 to 23.5 Ma||||||
8395|Hobwee Basalt|44784|14|Not recorded|p12||Tertiary|Lamington Group.||||||
8395|Hobwee Basalt|44813|14|Not recorded|p80||Tertiary|||||||
8395|Hobwee Basalt|44818|6|Mentioned|p275|||||||||
8395|Hobwee Basalt|44871|2|Defined|p141,map|||||||||
8395|Hobwee Basalt|48917|6|Mentioned|p38|||One map symbol for all units of Lamington Volcanics||||||
8395|Hobwee Basalt|69599|5|Briefly described|p640|||Northern side of the Tweed volcano, centred on Mount Warning.|23.6 +/- 0.4 Ma (Knesel et al., 2008)..|||Approximate equivalent of Blue Knob Basalt in NSW.||
8395|Hobwee Basalt|73450|6|Mentioned|p99-100|||Associated with the Tweed Volcano. Up to 600 m thick.|||||Basaltic lavas.|
8395|Hobwee Basalt|73581|5|Briefly described|p6|||Tweed Volcano. Overlies Springbrook Rhyolite to the north/Nimbin Rhyolite to the south.||Lamington Volcanics, top|||Olivine-bearing basalt.|
8422|Holbrook Granite|42726|5|Briefly described|map legend|Early Devonian||548.||||||
8422|Holbrook Granite|69801|5|Briefly described|p2, p4-p5, p71-76, p137|Devonian|Devonian|Central Lachlan Orogen. Occurs immediately east of Holbrook. Sample locality, sample description, petrography, SHRIMP analyses and interpretation are detailed. In hand specimen resembles the Thologolong Granite.|415.1 +/- 2.0 Ma (SHRIMP)|||Intrudes the Woomargama Granite and the Granya Granite of the Koetong Supersuite.|I-type, coarse-grained, alkali feldspar granitic rocks.|
8422|Holbrook Granite|70777|5|Briefly described|p2, p81|Lochkovian|Lochkovian|Lachlan Orogen. I-type geochemistry.|415.1 +/- 2 Ma (Bodorkos et al., 2015)|||||
8440|Homeleigh Agglomerate Member|30604|2|Defined|p68|Cenozoic|Cenozoic|||||||19-NOV-08
8440|Homeleigh Agglomerate Member|36411|6|Mentioned|p269|||Refs Duggan & Masson 1978 for definition.||||||
8446|Homeville Coal Member|22610|5|Briefly described|p 125, Fig 1|||||||||
8446|Homeville Coal Member|23540|5|Briefly described|p 421|||also see p 419. Divided into upper and lower.||||||
8446|Homeville Coal Member|37086|6|Mentioned|p185|||||||||
8446|Homeville Coal Member|40166|6|Mentioned|p345|||||||||
8446|Homeville Coal Member|45090|5|Briefly described|p151|||||||||
8451|Honeybugle Complex|23053|5|Briefly described|p20,65,75||Late Ordovician|Max Age: 445 (+/-) 6 Ma.||||||
8451|Honeybugle Complex|23171|5|Briefly described|p12,28||Late Ordovician|Max Age: 445 Ma.||||||
8451|Honeybugle Complex|23173|4|Described|Map Legend|Late Ordovician|Late Ordovician|||||||
8451|Honeybugle Complex|41594|6|Mentioned|p29|||||||||
8451|Honeybugle Complex|63290|6|Mentioned|p391|Llandovery|Bolindian|Age: 445+/-6Ma (SHRIMP).||||||
8451|Honeybugle Complex|69635|4|Described|p69-74 |||North-western Lachlan Orogen and southern Thomson Orogen.  U-Pb SHRIMP zircon magmatic crystallisation age. Previous SHRIMP zircon age 445.6+/-6 Ma (Barron et al. 2004).|442.1+/-2.1 Ma|Of Fifield Suite.||Intrudes Girilambone Group.|Massive, medium-grained hornblende diorite sampled. Ultramafic complex.|
8451|Honeybugle Complex|72296|5|Briefly described|p32, p38, p59|Early Silurian|Late Ordovician|The largest body and representative of the dioritic phase of the Fifield suite of mafic to ultramafic intrusions.|442.1 +/- 2.1 Ma (SHRIMP: Fraser et al., 2014).|||||
8451|Honeybugle Complex|72951|5|Briefly described|p1013, 1018, 1022, 1024, 1027, 1030|Llandovery|Late Ordovician|Lachlan Orogen. Hermidale Terrane. I-type. SHRIMP U-Pb zircon isotope analyses from Fraser et al. (2014). eHf = 8.0 +/- 0.5, and d18O = 6.02 +/- 0.17. May be related to Macquarie Arc.|442.1 +/- 2.1 Ma||||Includes Hornblende-quartz-pyroxene diorite.|
8451|Honeybugle Complex|73154|6|Mentioned|p84|Llandovery|Late Ordovician||442+/-2 Ma zircon Pb/U|Fifield complexes||||
8476|Hooray Sandstone|730|6|Mentioned|p24, p25.|||Fluviatile.||||||11-NOV-14
8476|Hooray Sandstone|8187|5|Briefly described|Map legend|Mesozoic|Mesozoic|Sandstone, siltstone, shale, conglomerate.||||||21-JUN-04
8476|Hooray Sandstone|8217|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Sandstone, siltstone, shale, conglomerate.||||||
8476|Hooray Sandstone|9694|5|Briefly described|Map Legend|Cretaceous|Jurassic|Deeply weathered sandstone, feldspathic sandstone, siltstone, basal conglomerate.||||||
8476|Hooray Sandstone|12597|5|Briefly described|p492 Tb.1, p497, p499, p501|Early Cretaceous|Kimmeridgian|Eromanga Basin. 100-200m thick. Coal reported (John, 1985) at top of the Formation in GSQ Wyandra No. 1.||||Equivalent to Murta Member and upper Namur Sandstone Member, and Algebuckina Sandstone.|Interbedded quartzose to sub-labile sandstone and siltstone.|
8476|Hooray Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Late Jurassic|In Eromanga Basin.||||||
8476|Hooray Sandstone|22464|5|Briefly described|p9|Early Cretaceous|Late Jurassic|Eromanga Basin, overlain by Cadna-Owie Formation.||||||16-SEP-08
8476|Hooray Sandstone|22826|6|Mentioned|p576|Early Cretaceous|Late Jurassic|Geological Province - Eromanga Basin.||||||
8476|Hooray Sandstone|22857|5|Briefly described|p295, p296-7 Tb.22.1, p314|Valanginian|Tithonian|Pale medium to coarse-grained quartzose sandstone. Equivalent of Mooga Sandstone (Surat Basin). Max. thickness: 200m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
8476|Hooray Sandstone|22865|4|Described|p295,Table22.1p296-7|Neocomian|Tithonian|||||||
8476|Hooray Sandstone|22954|6|Mentioned|Fig3p9||Cretaceous|||||||
8476|Hooray Sandstone|23056|4|Described|23|||Geol province Eromanga Basin.||||||16-SEP-08
8476|Hooray Sandstone|23375|4|Described|Fig2 p265, 291|Valanginian|Tithonian|Laterally equivalent to Namur Sandstone and Murta Formation. In the Eromanga Basin.||||||11-MAY-17
8476|Hooray Sandstone|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
8476|Hooray Sandstone|23430|4|Described|p523 + p524 Table 14.7|||Underlain by Westbourne Formation - unconformable. Eromanga Basin Province.||||||26-SEP-06
8476|Hooray Sandstone|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Jurassic|Geological Province: Great Australian Superbasin.||||||
8476|Hooray Sandstone|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
8476|Hooray Sandstone|24047|6|Mentioned|p109 Appendix 2|||Geological Province: Eromanga Basin.||||||
8476|Hooray Sandstone|24092|6|Mentioned|p5|||Geological Province: Great Artesian Basin.||||||
8476|Hooray Sandstone|24204|5|Briefly described|p266||Jurassic|Geological Province: Eromanga Basin.||||||
8476|Hooray Sandstone|29591|6|Mentioned|p69|||||||||
8476|Hooray Sandstone|30020|6|Mentioned|p33|||||||||
8476|Hooray Sandstone|30021|6|Mentioned|p89|||||||||
8476|Hooray Sandstone|30022|6|Mentioned|p28|||||||||
8476|Hooray Sandstone|30024|6|Mentioned|p331|||||||||
8476|Hooray Sandstone|30102|4|Described|p25|||See also p26,28,29. Upper Jurassic - Lower Cretaceous age.||||||26-SEP-06
8476|Hooray Sandstone|30103|6|Mentioned|p8|||||||||
8476|Hooray Sandstone|30104|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
8476|Hooray Sandstone|30510|6|Mentioned|p103|||||||||
8476|Hooray Sandstone|30691|4|Described|p6|||See also p15-17,20,21,Table 4,6. Jurassic - Cretaceous age||||||26-SEP-06
8476|Hooray Sandstone|30692|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Lower Cretaceous to Upper Jurassic||||||
8476|Hooray Sandstone|30694|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|30695|4|Described|Table 4|||Upper Jurassic to Lower Cretaceous age.||||||16-SEP-08
8476|Hooray Sandstone|30699|6|Mentioned|p56|||Map||||||
8476|Hooray Sandstone|30702|6|Mentioned|p48|||See also Fig.1. Stratigraphic table||||||
8476|Hooray Sandstone|30853|5|Briefly described|Table 3|||Upper Jurassic to Cretaceous||||||
8476|Hooray Sandstone|30854|4|Described|Table 4|||Upper Jurassic-Lower Cretaceous age.||||||
8476|Hooray Sandstone|30855|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|30856|4|Described|Table 3|||Upper Jurassic-Lower Cretaceous age.||||||
8476|Hooray Sandstone|30857|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic-Lower Cretaceous||||||
8476|Hooray Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
8476|Hooray Sandstone|31097|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|31098|5|Briefly described|Table 1|||U. Jurassic -  L. Cretaceous||||||
8476|Hooray Sandstone|31116|6|Mentioned|p43|||||||||
8476|Hooray Sandstone|31145|5|Briefly described|Table 1|||U. Jurassic - L. Cretaceous||||||
8476|Hooray Sandstone|31244|6|Mentioned|p8|||||||||
8476|Hooray Sandstone|31425|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic to L.Cretaceous||||||
8476|Hooray Sandstone|31430|5|Briefly described|Table 1|||U.Jurassic-L.Cretaceous.||||||
8476|Hooray Sandstone|31431|5|Briefly described|Table 3|||U.Jurassic - L.Cretaceous||||||
8476|Hooray Sandstone|31432|4|Described|Table 1|||U.Jurassic - L.Cretaceous.||||||16-SEP-08
8476|Hooray Sandstone|31436|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
8476|Hooray Sandstone|31438|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Lower Cretaceous to Upper Jurassic||||||
8476|Hooray Sandstone|31441|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
8476|Hooray Sandstone|31443|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic-L.Cretaceous||||||
8476|Hooray Sandstone|31553|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|32138|6|Mentioned|p398|||||||||
8476|Hooray Sandstone|32275|6|Mentioned|p8|||Refers Galloway & Senior (1971)||||||
8476|Hooray Sandstone|32314|6|Mentioned|Fig. 4|||||||||
8476|Hooray Sandstone|32490|6|Mentioned|Table 1|||Equivalent Ronlow Beds?||||||
8476|Hooray Sandstone|33017|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|33067|4|Described|Table 1|Early Cretaceous|Late Jurassic|Sublabile sandstone, quartz sandstone, conglomerate.||||||07-JUL-04
8476|Hooray Sandstone|33069|4|Described|p7|||U.Jur. and L.Cret.||||||26-SEP-06
8476|Hooray Sandstone|33071|4|Described|p2|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33072|4|Described|Table 1|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33075|5|Briefly described|p445|||||||||
8476|Hooray Sandstone|33078|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jurassic - L.Cretaceous||||||
8476|Hooray Sandstone|33079|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33080|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33082|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33083|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33086|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
8476|Hooray Sandstone|33087|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.- L.Cret.||||||
8476|Hooray Sandstone|33088|4|Described|Table 3|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33089|4|Described|Table 2|||U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33095|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33169|6|Mentioned|p322|||||||||
8476|Hooray Sandstone|33176|6|Mentioned|p177|||||||||
8476|Hooray Sandstone|33182|6|Mentioned|Table 1|||L.Cret.- U.Jur.||||||
8476|Hooray Sandstone|33183|6|Mentioned|p233|||||||||
8476|Hooray Sandstone|33448|4|Described|Table 1|||U.Jur.-L.Cret.||||||11-JAN-10
8476|Hooray Sandstone|33449|4|Described|Table 1|||J.Jur.-L.Cret.||||||
8476|Hooray Sandstone|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
8476|Hooray Sandstone|33523|6|Mentioned|p27|||||||||
8476|Hooray Sandstone|33638|5|Briefly described|Table 1|||||||||
8476|Hooray Sandstone|33639|5|Briefly described|Table 2|||U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33640|4|Described|Table 3|||L.Jur.||||||
8476|Hooray Sandstone|33643|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|33644|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33646|6|Mentioned|p12|||||||||
8476|Hooray Sandstone|33647|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|33648|6|Mentioned|p19|||Stratigraphy.||||||
8476|Hooray Sandstone|33672|5|Briefly described|p44|||Lithology.||||||
8476|Hooray Sandstone|33673|6|Mentioned|p287|||||||||
8476|Hooray Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
8476|Hooray Sandstone|33964|6|Mentioned|p6|||Equivalent Transition Beds & Cadna-owie Formation.||||||
8476|Hooray Sandstone|34065|4|Described|p6|||U.Jur. - L.Cret.||||||
8476|Hooray Sandstone|34091|5|Briefly described|Table 1|||Jur. - L.Cret.  See also P9||||||
8476|Hooray Sandstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
8476|Hooray Sandstone|34174|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|34218|4|Described|Table 1|||See also Table 2. Upper Jurassic - Lower Cretaceous.||||||
8476|Hooray Sandstone|34254|6|Mentioned|p491|||||||||
8476|Hooray Sandstone|34485|4|Described|Table 1|||Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|34486|4|Described|Table 1|||Lower Cretaceous||||||
8476|Hooray Sandstone|34487|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
8476|Hooray Sandstone|34847|6|Mentioned|Table 1|||Stratigraphy & hydrocarbon prospects||||||
8476|Hooray Sandstone|35139|6|Mentioned|p17|||||||||
8476|Hooray Sandstone|35239|6|Mentioned|Fig.4|||||||||
8476|Hooray Sandstone|35457|6|Mentioned|p623|||||||||
8476|Hooray Sandstone|35560|4|Described|p290|||||||||
8476|Hooray Sandstone|35663|5|Briefly described|p126|||||||||
8476|Hooray Sandstone|35793|6|Mentioned|Fig.3|||||||||
8476|Hooray Sandstone|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
8476|Hooray Sandstone|35811|5|Briefly described|Table 3|||||||||
8476|Hooray Sandstone|35936|6|Mentioned|p615|||||||||
8476|Hooray Sandstone|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
8476|Hooray Sandstone|36243|6|Mentioned|Table 6A|||||||||
8476|Hooray Sandstone|36251|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|36473|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8476|Hooray Sandstone|36580|6|Mentioned|p469|||||||||
8476|Hooray Sandstone|37116|6|Mentioned|p310|||||||||
8476|Hooray Sandstone|37451|6|Mentioned|Table 2|||||||||
8476|Hooray Sandstone|37603|6|Mentioned|p444|||||||||
8476|Hooray Sandstone|37608|3|Fully described|Table 1|||||||||
8476|Hooray Sandstone|37995|6|Mentioned|p65|||||||||
8476|Hooray Sandstone|38199|5|Briefly described|p423|||Palynology||||||
8476|Hooray Sandstone|38226|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|38532|4|Described|Fig.4|||||||||
8476|Hooray Sandstone|38814|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|39070|4|Described|p364|||||||||
8476|Hooray Sandstone|39211|5|Briefly described|p23|||See also Figs 4,6-8,14,15 etc. Correlation||||||
8476|Hooray Sandstone|39212|6|Mentioned|p25|||Aquifer||||||
8476|Hooray Sandstone|39445|5|Briefly described|Table 10|||||||||
8476|Hooray Sandstone|39478|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|39846|6|Mentioned|p45|||||||||
8476|Hooray Sandstone|39847|5|Briefly described|p37|||||||||
8476|Hooray Sandstone|39898|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Medium to coarse quartz sandstone with kaolinitic cement. Upper part altered to ironstone.||||||14-FEB-06
8476|Hooray Sandstone|39943|6|Mentioned|Table 8A|||||||||
8476|Hooray Sandstone|39988|6|Mentioned|p289|||||||||
8476|Hooray Sandstone|39989|4|Described|p422|||||||||
8476|Hooray Sandstone|40121|6|Mentioned|p446|||||||||
8476|Hooray Sandstone|40199|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|40249|6|Mentioned|p41|||||||||
8476|Hooray Sandstone|40250|6|Mentioned|Fig.7|||||||||
8476|Hooray Sandstone|40538|5|Briefly described|Map legend|Cretaceous|Jurassic|Quartz arenite to quartz wacke, kaolinitic, poorly bedded, white.||||||15-NOV-05
8476|Hooray Sandstone|40670|6|Mentioned|Fig.9|||||||||
8476|Hooray Sandstone|40675|6|Mentioned|Table 8A|||||||||
8476|Hooray Sandstone|40687|3|Fully described|p416|||||||||
8476|Hooray Sandstone|40801|6|Mentioned|p29|||||||||
8476|Hooray Sandstone|40832|3|Fully described|p456|||||||||
8476|Hooray Sandstone|40833|6|Mentioned|p468|||||||||
8476|Hooray Sandstone|40906|4|Described|p30|||||||||
8476|Hooray Sandstone|40962|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|41060|6|Mentioned|Fig.3|||||||||
8476|Hooray Sandstone|41061|6|Mentioned|p21|||||||||
8476|Hooray Sandstone|41062|6|Mentioned|Fig.5|||||||||
8476|Hooray Sandstone|41064|6|Mentioned|p60,p65|||||||||
8476|Hooray Sandstone|41097|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|41177|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|41182|5|Briefly described|Fig.2|||||||||
8476|Hooray Sandstone|41186|4|Described|p209|||||||||
8476|Hooray Sandstone|41187|6|Mentioned|Fig.2|||||||||
8476|Hooray Sandstone|41198|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|41216|6|Mentioned|Fig.18|||||||||
8476|Hooray Sandstone|41246|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|41247|6|Mentioned|p126|||See also Fig.4||||||
8476|Hooray Sandstone|41266|6|Mentioned|Fig.3|||||||||
8476|Hooray Sandstone|41361|6|Mentioned|p5|||||||||
8476|Hooray Sandstone|41523|6|Mentioned|p271|||||||||
8476|Hooray Sandstone|41681|4|Described|p2|||See also pp16,22.||||||26-SEP-06
8476|Hooray Sandstone|41686|6|Mentioned|p64|||||||||
8476|Hooray Sandstone|41707|5|Briefly described|p163|||||||||
8476|Hooray Sandstone|42067|4|Described|p309|||||||||
8476|Hooray Sandstone|42071|6|Mentioned|Fig.2A P116|||||||||
8476|Hooray Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
8476|Hooray Sandstone|42412|6|Mentioned|p228|||||||||
8476|Hooray Sandstone|42446|4|Described|p13|||||||||
8476|Hooray Sandstone|42447|5|Briefly described|p5 + Fig. 1|||||||||
8476|Hooray Sandstone|42474|5|Briefly described|p25|||||||||
8476|Hooray Sandstone|42493|6|Mentioned|p20|||Eromanga Basin.||||||
8476|Hooray Sandstone|42496|5|Briefly described|p136, Fig.3 p132|||||||||
8476|Hooray Sandstone|42504|5|Briefly described|p83|||or De Sousa Sandstone||||||
8476|Hooray Sandstone|42746|6|Mentioned|p9|||||||||
8476|Hooray Sandstone|42749|4|Described|p31, Fig.7 p30|||see also Fig.2 p27.||||||26-SEP-06
8476|Hooray Sandstone|42940|5|Briefly described|Plate 2|Mesozoic|Mesozoic|Sandstone, pebbly sandstone, siltstone.  Geological province: Amadeus Basin.||||||23-JAN-08
8476|Hooray Sandstone|42999|5|Briefly described|Table 2,p90|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
8476|Hooray Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
8476|Hooray Sandstone|43035|6|Mentioned|p27|||||||||
8476|Hooray Sandstone|43105|5|Briefly described|Fig.9,p15.|||||||||
8476|Hooray Sandstone|43114|5|Briefly described|p13|||||||||
8476|Hooray Sandstone|43122|5|Briefly described|p20|||see also Fig. 2.||||||
8476|Hooray Sandstone|43565|6|Mentioned|p422|Late Jurassic|Early Jurassic|||||||
8476|Hooray Sandstone|43602|4|Described|191|||In Eromanga Basin.||||||16-SEP-08
8476|Hooray Sandstone|43748|6|Mentioned|p7|Late Jurassic|Early Jurassic|Eromanga Basin.||||||19-DEC-11
8476|Hooray Sandstone|44019|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|44020|14|Not recorded|p13,15,Tb.1,2,3|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|44022|14|Not recorded|Map Legend|Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|44023|4|Described|Tb.3,p12|Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|44028|14|Not recorded|Fig.2,p514|Cretaceous|Jurassic|See Strat Table.||||||
8476|Hooray Sandstone|44042|14|Not recorded|Map Legend|Early Cretaceous|Jurassic|||||||
8476|Hooray Sandstone|44082|14|Not recorded|Table p34|||||||||
8476|Hooray Sandstone|44084|14|Not recorded|p32|Late Jurassic|Middle Jurassic|||||||
8476|Hooray Sandstone|44099|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|44133|6|Mentioned|p110|Cretaceous|Cretaceous|Superseded by Namur Sandstone.||||||
8476|Hooray Sandstone|44337|5|Briefly described|Map Legend|Cretaceous|Jurassic|Lithology.||||||
8476|Hooray Sandstone|44362|6|Mentioned|p12|||||||||
8476|Hooray Sandstone|44375|14|Not recorded|p311,312|||||||||
8476|Hooray Sandstone|44415|14|Not recorded|p22,Fig.1,p23|Early Cretaceous|Late Jurassic|||||||
8476|Hooray Sandstone|45071|3|Fully described|Table 15|||||||||
8476|Hooray Sandstone|45103|6|Mentioned|p5|||||||||
8476|Hooray Sandstone|45110|2|Defined|p106|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous. See also Fig.5.||||||
8476|Hooray Sandstone|45168|6|Mentioned|p6|||||||||
8476|Hooray Sandstone|46791|5|Briefly described|p42|||||||||
8476|Hooray Sandstone|46881|6|Mentioned|Table 2|||||||||
8476|Hooray Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
8476|Hooray Sandstone|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
8476|Hooray Sandstone|46959|6|Mentioned|Table 1|||||||||
8476|Hooray Sandstone|48919|4|Described|p65|||U.Jur. - L.Cert.||||||
8476|Hooray Sandstone|48920|3|Fully described|p55|||Middle Jurassic-Lower Cretaceous age.||||||16-SEP-08
8476|Hooray Sandstone|48992|6|Mentioned|p38|||||||||
8476|Hooray Sandstone|48997|6|Mentioned|p6|||||||||
8476|Hooray Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
8476|Hooray Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
8476|Hooray Sandstone|49027|4|Described|p21|||||||||
8476|Hooray Sandstone|50372|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Eromanga Basin. Medium grained, poorly sorted kaolinitic quartz sandstone.||||||22-JUN-04
8476|Hooray Sandstone|60122|5|Briefly described|p33, p35|Jurassic|Jurassic|Subsumed both the Tarlton Fm and Longsight Sst. (Mond and Harrison, in Senior et al 1978) - although prominent outcrops previously mapped as Tarlton Formation are now assigned to Kelly Creek Formation.  Unconformably overlies Ethabuka Sandstone.||||||17-MAY-05
8476|Hooray Sandstone|60551|5|Briefly described|Map Legend|Cretaceous|Jurassic|Geological Province: Eromanga Basin. Sandstone, feldspathic sandstone, siltstone, basal boulder conglomerate.||||||17-NOV-04
8476|Hooray Sandstone|61014|6|Mentioned|p533 Fig.2.|Early Cretaceous|Early Cretaceous|Eromanga Basin.|||Includes Namur and  Murta Members.|Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|61312|5|Briefly described|p71, p64, p67 Fig.E5|Early Cretaceous|Late Jurassic|Name now restricted to the "Lower Hooray Sandstone" - fluvial sst. sequence. The original "Upper Hooray Sandstone" has been replaced by Cadna-owie Fm. Upper section considered to be equivalent to Mooga Fm. Geol Prov: Eromanga Basin||||||16-JUN-06
8476|Hooray Sandstone|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||13-MAR-09
8476|Hooray Sandstone|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
8476|Hooray Sandstone|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
8476|Hooray Sandstone|61823|5|Briefly described|p118|Cretaceous|Jurassic|Geological Province:  Eromanga Basin.||||||
8476|Hooray Sandstone|62028|5|Briefly described|p10 Fig. 1|||Includes the Namur Sandstone Member.||||||26-FEB-08
8476|Hooray Sandstone|62029|6|Mentioned|p15|||||||||
8476|Hooray Sandstone|62376|5|Briefly described|p53|Tertiary|Mesozoic|Geological Province: Georgina Basin||||||09-FEB-10
8476|Hooray Sandstone|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
8476|Hooray Sandstone|63450|5|Briefly described|p83|Cretaceous|Jurassic |May contain Cadna-owie Formation (in upper section) as the unit previously mapped as Longsight Sandstone was renamed Hooray Sandstone. Overlain by Rolling Downs Group.||||||07-FEB-11
8476|Hooray Sandstone|63789|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Of Rolling Downs Group. Thickness: 30m. Medium-grained cross-bedded white sandstone with some white vein quartz and quartzite pebble conglomerate at the base.Surface exposures often as ferruginised sandstone and conglom.||||||26-NOV-08
8476|Hooray Sandstone|63790|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Of Rolling Downs Group. Medium-grained cross-bedded white quartz sandstone with some white vein quartz and quartzite pebble conglomerate at base. Thickness: 30 m.||||||
8476|Hooray Sandstone|63979|2|Defined|p41, Fig. 44|Valanginian|Tithonian|Lower+upper sections originally informally designated as ""Namur Sst Mbr" and "Murta Mbr" respectively (both now upgraded). Thick: 165m. Mainly sandstone+lesser siltstone and mudstone, minor coal. Overlain by Cadna-owie Fm;underlain by Westbourne Fm.||||||07-FEB-11
8476|Hooray Sandstone|64048|6|Mentioned|p64 Tb. 2, p70|||Geological Province: Eromanga Basin.||||||07-FEB-11
8476|Hooray Sandstone|64068|6|Mentioned|p78|||Georgina Basin.||||Unconformably overlies Ethabuka Sandstone.||05-APR-12
8476|Hooray Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Early Cretaceous|Late Jurassic|Eromanga Basin.|||Includes Namur Sandstone Member and Murta Member.|Overlies Birkhead and Westbourne Formations. Is overlain by Cadna-owie Formation.||10-DEC-15
8476|Hooray Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Late Jurassic|Eromanga Basin.||||Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|64683|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Rolling Downs Group. Medium-grained cross-bedded white quartz sandstone with some white vein quartz and quartzite pebble conglomerate at the base. Thickness: 30m.||||||
8476|Hooray Sandstone|64856|6|Mentioned|p94-97|||Eromanga Basin. Correlated with Gubberamunda Sandstone of Surat Basin. Upper part grades into Mooga Sandstone.| | ||||29-NOV-17
8476|Hooray Sandstone|65238|5|Briefly described|p10|||Contains Murta Member. Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||
8476|Hooray Sandstone|65309|6|Mentioned|p14.|Jurassic|Jurassic|Known in South Australia as Algebuckina Sandstone, and in Northern Territory as De Souza Sandstone.||||||
8476|Hooray Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Westbourne Formation. Overlain by Cadna-owie Formation.||||||08-MAR-12
8476|Hooray Sandstone|65489|6|Mentioned|p49, p96|Cretaceous|Jurassic|Eromanga Basin. Source and reservoir rocks.||||||
8476|Hooray Sandstone|66529|5|Briefly described|p10, p12 Fig.5, p16  |||Eromanga Basin. |||||Sandstone.|
8476|Hooray Sandstone|66623|6|Mentioned|p240.|||Lithologically and stratigraphically identical with Namur Sandstone in NSW and SA.||||||
8476|Hooray Sandstone|66915|5|Briefly described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Late Jurassic|Eromanga Basin.||||||12-JAN-17
8476|Hooray Sandstone|67323|5|Briefly described|p87-88, p93 Fig.12.3, p95 Fig.12.5, p96|Early Cretaceous|Late Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin; also probable reservoir (the unit is one of the main continuous aquifers in the region).||||Overlies Westbourne Formation. Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|67402|4|Described|p26 tbl RRM4, p43 tbl HPB1|Early Cretaceous|Early Jurassic|Eromanga Basin. Deposited in fluvial to fluvio-lacustrine environments during a series of regressive-transgressive cycles. Maximum thickness of 165m. Prospective unit for the storage of carbon dioxide. See also p106, p109, p111 fig ERO8, p113 fig ERO12, p114 fig ERO13, p115, p120, p304.||||Overlies the Westbourne Formation. Overlain by the Lower Cadna-owie Formation. Equivalent to the Namur Sandstone and Murta Formation.|Sandstones interbedded with siltstone, mudstone and minor coal.|
8476|Hooray Sandstone|67561|6|Mentioned|p53 Fig.3, p67|||Correlative of the Livingston Tillite Member.||||||
8476|Hooray Sandstone|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Jurassic|Surat Basin.||||Is overlain by Bungil Formation.||
8476|Hooray Sandstone|68004|5|Briefly described|p174.|||Major aquifer for water production; excellent quality reservoir. Sealed by Wallumbilla Formation shales. A major hydrocarbon exploration target.||||||
8476|Hooray Sandstone|68135|5|Briefly described|p52 Fig.2b|Early Cretaceous|Tithonian|Eromanga Basin.||||Unconformably overlies Westbourne Formation.|Predominantly sandstone.|
8476|Hooray Sandstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
8476|Hooray Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
8476|Hooray Sandstone|68731|6|Mentioned|pp209-211|||||||||
8476|Hooray Sandstone|68734|6|Mentioned|p218 Fig.2|||Eromanga Basin (NE). Fluvial.||||||
8476|Hooray Sandstone|69443|6|Mentioned|p28:30|||Eromanga Basin.||||Unconformably overlies Ethabuka Sandstone.||12-JUL-16
8476|Hooray Sandstone|69457|5|Briefly described|p41:3-4, 6-7|Early Cretaceous|Early Cretaceous|NE Eromanga Basin. This name was used in the ILLOGWA CREEK map area (Shaw and Freeman, 1985) and TOBERMOREY and HAY RIVER map areas (Mond and Harrison in Senior et al., 1978). It appears that it is to be superseded by the Algebuckina Sandstone.||||Is overlain conformably by Cadna-owie Formation.|Mesa-forming planar to cross-bedded, medium-coarse sandstone and minor mudstone, siltstone and conglomerate.|12-JUL-16
8476|Hooray Sandstone|69582|5|Briefly described|p29, p65-p66|||Eromanga Basin. Intersected in GSQ Julia Creek 1 and in GSQ Longreach 2 drillholes.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.|Sandstone, mudstone.|
8476|Hooray Sandstone|69594|4|Described|p519, p526-528, p532-533, p537-538, p573|Hauterivian|Tithonian|Woolley (1941); Hill and Denmead (1960). Eromanga Basin. Reference section in GSQ Tambo 2 (Wallin, 1974). Cannot be divided in E and N parts of the Basin; in SW QLD, it had been divided into a lower Namur Sandstone Member and an overlying Murta Member (both superseded). Petroleum companies include basal Cadna-owie Formation in their idea of the Murta Member. 90-165m thick. Braided fluvial deposits. A significant hydrocarbon reservoir. An important, shallow aquifer. RELATED UNITS (continued); Equivalent to Gubberamunda Sandstone, Orallo Formation and Mooga Sandstone (grades into the last).||||Overlies Westbourne Formation conformably to unconformably. Is overlain transitionally by Cadna-owie Formation. Lower part interfingers with lower Southlands Formation. See COMMENTS for more.|Sublabile to quartzose sandstone, with subordinate siltstone and mudstone and sporadic minor coal seams.|
8476|Hooray Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Late Jurassic|Eromanga Basin.||||||
8476|Hooray Sandstone|69946|6|Mentioned|p16|||||||||
8476|Hooray Sandstone|69947|5|Briefly described|p29 Fig.7.18|||||||Is overlain by McKinlay Member (Murta Formation). ?Correlates with Namur Sandstone.||07-FEB-18
8476|Hooray Sandstone|70821|4|Described|p21-22,p28,p30-31,p33,p72,p79-83,p85-86|Early Cretaceous|Jurassic|Woolley (1941), Exon (1966). Eromanga Basin. Formerly part of Rolling Downs Group. A major aquifer in the Great Artesian Basin: one of the two main groundwater resources in the area. Borehole wireline electrical and natural gamma logging and AEM inversion soundings. Hydrochemistry mentioned, hydrostratigraphic properties.||||Overlies Birkhead and Westbourne Formations (Injune Creek Group). Is overlain by Cadna-owie Formation or Doncaster Member (Wallumbilla Formation). Lateral equivalent to Algebuckina Sandstone.|Sub-labile, quartz sandstone with minor conglomerate.|
8476|Hooray Sandstone|70823|6|Mentioned|p78|Cretaceous|Jurassic|Eromanga Basin.||||||
8476|Hooray Sandstone|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
8476|Hooray Sandstone|70860|6|Mentioned|p280-281|||Great Artesian Basin. Part of the uppermost aquifer in the Basin. Is presented also as Cadna-owie - Hooray Sandstone aquifer. Fluvial, paralic and littoral sediments.|||||Quartzose and lithic sandstone.|
8476|Hooray Sandstone|71251|5|Briefly described|p13, p15, p17, p20, p49, p51|||Natural gamma wireline log. Conductivity diagram. An artesian aquifer with very high water pressures.||||Is overlain by Cadna-owie Formation.||
8476|Hooray Sandstone|71342|5|Briefly described|Ch5 p16-p17|||The lower part of this unit is equivalent to the Namur Sandstone and the upper part is equivalent to the Murta Formation. ||||||
8476|Hooray Sandstone|71382|5|Briefly described|p4, p12, p16-p17, p19, p25|Cretaceous|Late Jurassic|Eromanga Basin. Intersected in GSQ Julia 1 from 310.49m-320.05m for a total of 9.56m thickness. An aquifer occurs within this unit where it was intersected. Temp log and stratlog are provided. See also p27-p28, App 3, 4.||||Overlies the Millungera Basin - quartzite 81261. Overlain by the Wallumbilla Formation.|Yellowish-brown, medium to coarse-grained, well-sorted and subnrounded quartzose sandstone, medium grey mudstone laminae also occur.|
8476|Hooray Sandstone|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
8476|Hooray Sandstone|71863|5|Briefly described|p5|Valanginian|Tithonian|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
8476|Hooray Sandstone|71864|6|Mentioned|p14, p17|||Waterbores intersect this unit which has a very high artesian groundwater flow.||||||
8476|Hooray Sandstone|72297|6|Mentioned|p742, p761|||Eromanga Basin. Petroleum reservoir. A major aquifer with excellent prospects for HSA (hot sedimentary aquifer) geothermal energy.||||||
8476|Hooray Sandstone|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA,QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Westbourne FZ (Injune Creek Group). Is overlain by Cadna-owie FZ.||
8476|Hooray Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurassic|Shown with Namur Sandstone as located in the Eromanga Basin.||||Unconformably overlies Westbourne Formation.||
8476|Hooray Sandstone|73113|6|Mentioned|p207|||Great Artesian Basin.||||||
8476|Hooray Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains oil.||||||
8476|Hooray Sandstone|73203|6|Mentioned|p652|Jurassic|Jurassic|||||||
8476|Hooray Sandstone|73343|6|Mentioned|p337|Cretaceous|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Westbourne Formation. Overlain by Murta Member. Equivalent to Namur Sandstone.||
8476|Hooray Sandstone|73479|5|Briefly described|p156 Fig.2|Cretaceous|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.||||Overlies Westbourne Formation, underlies Murta Member||
8489|Hores Gneiss|6823|5|Briefly described|p203, 205-208, 210-211, 216-217,|Palaeoproterozoic|Palaeoproterozoic|Incorporated the Purnamoota gneiss of Browne (1922), but unit gives different ages at different locations e.g. Purnamoota Road and Yanco Glen. Contains the Broken Hill orebody (conformable within this unit), which is interpreted to have formed contemporanesouly with this unit. Additional SHRIMP magmatic ages of 1680 +/- 12 Ma and 1665 +/-12 and metamorphic ages 1599+/-9, 1600+/-8 Ma are also derived from Page and Laing (1992). Further ages of 1643 +/- 14 Ma (crystallisation) and 1590 +/- 27 Ma (metamorphic) are derived from this study. See also p220, 222, 226-227, 229-230, 233-234, 236.|1689 +/- 5 Ma (SHRIMP magmatic age)|Broken Hill Group|||Quartzo-feldspathic, highly deformed gneiss, sometimes containing garnet porphyroblasts.|26-MAR-22
8489|Hores Gneiss|22500|6|Mentioned|Fig 12|||||||||
8489|Hores Gneiss|22553|5|Briefly described|p75,fig2p77|Statherian|Statherian|Part of Willyama Supergroup.||||||11-SEP-07
8489|Hores Gneiss|22575|6|Mentioned|p179 Fig.2|||of the Pumamoota Subgroup, Broken Hill Group, Broken Hill Block||||||
8489|Hores Gneiss|22641|5|Briefly described|p687, Fig.2 p689|Paleoproterozoic|Paleoproterozoic|Age of unit 1690 Ma. See also p692||||||07-NOV-08
8489|Hores Gneiss|22771|5|Briefly described|p36,44,47-48|||||||||
8489|Hores Gneiss|22857|4|Described|p36, p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Supersedes the Parnell Gneiss of Cordwell and Williams (1922). Age: 1690+/-5Ma (U/Pb, Page and Lang, 1990). Of Purnamoota Subgroup. Contains the Broken Hill orebody in stratabound interpretations. Max. thickness: 200m. Geol. Prov: Willyama Fold Belt. ||||||07-NOV-08
8489|Hores Gneiss|22884|6|Mentioned|p47||Statherian|Unit at top of Broken Hill Group. Age of unit is 1680-1690 Ma. Geological province: Broken Hill Domain.||||||26-MAR-09
8489|Hores Gneiss|22962|6|Mentioned|p73||Statherian|||||||
8489|Hores Gneiss|22964|4|Described|p55,57,58||Statherian|||||||
8489|Hores Gneiss|22965|5|Briefly described|p11,14,Fig1||Statherian|||||||
8489|Hores Gneiss|22966|4|Described|p3,4 Fig1||Statherian|Rift stage of development.||||||
8489|Hores Gneiss|22967|6|Mentioned|p31,3,9,42,5,9||Statherian|||||||
8489|Hores Gneiss|23025|6|Mentioned|p76|||||||||
8489|Hores Gneiss|23093|5|Briefly described|p619|||||||||
8489|Hores Gneiss|23094|6|Mentioned|p616|||||||||
8489|Hores Gneiss|23160|5|Briefly described|p870 fig1,2|||||||||
8489|Hores Gneiss|23248|5|Briefly described|p168, Fig2p169, 180||Statherian|Max Age: 1690 (+/-) 5 Ma.||||||
8489|Hores Gneiss|23347|5|Briefly described|p55|Statherian|Statherian|Of Lady Louise Suite. Age: 1686+/-3Ma (Page et al 2000).  Formation-type amphibolites and felsic intrusives.||||||24-MAR-09
8489|Hores Gneiss|23461|5|Briefly described|p204 Fig.3|||||||||
8489|Hores Gneiss|23565|5|Briefly described|p195|||Of Broken Hill Group.||||||
8489|Hores Gneiss|23912|6|Mentioned|p780|||||||||
8489|Hores Gneiss|24197|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of the Potosi Supersuite. Age: 1690+/-5Ma. Geological province: Broken Hill Inlier.||||||07-FEB-11
8489|Hores Gneiss|24307|5|Briefly described|p975|Proterozoic|Proterozoic|Parent: Broken Hill Group.   Previously included in the Purnamoota Subgroup, which has been abandoned by this study.||||||
8489|Hores Gneiss|38969|4|Described|p209|||||||||
8489|Hores Gneiss|39662|2|Defined|p429|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8489|Hores Gneiss|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8489|Hores Gneiss|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8489|Hores Gneiss|39849|6|Mentioned|Table 2|||||||||
8489|Hores Gneiss|39883|6|Mentioned|p381|||||||||
8489|Hores Gneiss|40290|6|Mentioned|Fig.2|||||||||
8489|Hores Gneiss|40822|6|Mentioned|Fig.2|||||||||
8489|Hores Gneiss|41093|6|Mentioned|p252|||||||||
8489|Hores Gneiss|41145|6|Mentioned|Fig.4|||||||||
8489|Hores Gneiss|41630|6|Mentioned|p27|||||||||
8489|Hores Gneiss|41633|6|Mentioned|p139|||||||||
8489|Hores Gneiss|41651|6|Mentioned|p188|||||||||
8489|Hores Gneiss|41791|6|Mentioned|p270|||||||||
8489|Hores Gneiss|41870|6|Mentioned|p125|||||||||
8489|Hores Gneiss|42181|4|Described|p251|||See also Fig.1||||||
8489|Hores Gneiss|42261|5|Briefly described|p529|||See also Fig.1 P530||||||
8489|Hores Gneiss|42286|6|Mentioned|p7|||||||||
8489|Hores Gneiss|42323|5|Briefly described|p4|||||||||
8489|Hores Gneiss|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8489|Hores Gneiss|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8489|Hores Gneiss|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
8489|Hores Gneiss|42537|6|Mentioned|Fig.2 P5|||||||||
8489|Hores Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
8489|Hores Gneiss|42819|5|Briefly described|p316|||||||||
8489|Hores Gneiss|42897|5|Briefly described|p320|||||||||
8489|Hores Gneiss|43052|5|Briefly described|p98|||||||||
8489|Hores Gneiss|43086|6|Mentioned|Fig.3|||||||||
8489|Hores Gneiss|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of the Purnamoota Subgroup||||||07-NOV-08
8489|Hores Gneiss|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of the Purnamoota Subgroup.||||||07-NOV-08
8489|Hores Gneiss|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Purnamoota Subgroup.||||||07-NOV-08
8489|Hores Gneiss|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of the Purnamoota Sub-Group.||||||07-NOV-08
8489|Hores Gneiss|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Purnamoota Subgroup.||||||07-NOV-08
8489|Hores Gneiss|43572|6|Mentioned|p5||Paleoproterozoic|Dated: 1690+/-5 Ma 1670||||||07-NOV-08
8489|Hores Gneiss|43583|4|Described|Table 1, p2139,2140|||||||||
8489|Hores Gneiss|46598|5|Briefly described|p304|||||||||
8489|Hores Gneiss|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Broken Hill Group (Willyama Supergroup). Overlain by Sundown Group. Underlain by Freyers Metasediments.||||||31-MAY-07
8489|Hores Gneiss|50606|5|Briefly described|p1.1, 1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Potosi Supersuite. Geological Province: Broken Hill Block. Age: 1689-1668 +/- 14Ma (U-Pb).||||||07-NOV-08
8489|Hores Gneiss|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Purnamoota Subgroup (Broken Hill Group).  Geological Province: Broken Hill Block.||||||07-NOV-08
8489|Hores Gneiss|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Extrusive rocks.  Age: 1685+/-3Ma.  Geological Province: Broken Hill Domain.||||||
8489|Hores Gneiss|61318|4|Described|pp581-600.|Proterozoic|Proterozoic|Relict volcanic textures preserved at low metamorphic grades. Has a diatexitic outcrop 300 - 600 m wide with 3 types : metatexite, schlieren diatexite and massive diatexite. Each zone's petrology and geochemistry are described in detail. The elevated melt contents produced during upper-amphibolite facies metamorphism reflect an influx of hydrous fluids from surrounding metapelites.|||||Metamorphosed volcaniclastic to volcanigenic unit with minor intercalated pelitic to psammitic metasedimentary rocks.|
8489|Hores Gneiss|61606|5|Briefly described|p4 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group.||||||07-NOV-08
8489|Hores Gneiss|61735|5|Briefly described|p634, p636, p643|Paleoproterozoic|Paleoproterozoic|Magmatic and stratigraphic age: 1685+/-3Ma U/Pb SHRIMP. Felsic gneiss unit of the Broken Hill Domain. See also p636 Fig. 2.||||||04-JUN-15
8489|Hores Gneiss|61736|5|Briefly described|p665, p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Age: 1685+/-3Ma. Geological province: Olary Domain. Volcaniclastic unit.||||||
8489|Hores Gneiss|62473|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Age: 1686+/-3Ma.||||||17-JUN-09
8489|Hores Gneiss|62535|5|Briefly described|p665, p666 Fig.3, p671-673|Paleoproterozoic|Paleoproterozoic|Hosts the giant Broken Hill Pb-Zn-Ag orebody.|1685 +/- 3 Ma.|Broken Hill Group.|||Volcaniclastic metasediments.|
8489|Hores Gneiss|62536|5|Briefly described|p633-634, 636, 638-641, 643-647|||See also p654-655, 658-659. Broken Hill area. Spatially and stratigraphically associated with the orebody. Magmatism of this unit was coeval with that of Rasp Ridge Gneiss. Zircons with 1690 Ma cores have 1600 Ma high U, low Th/U overgrowths.|1685 +/- 3 Ma (protolith).|Broken Hill Group.|||Regionally extensive, metamorphosed felsic volcaniclastic unit.|
8489|Hores Gneiss|62592|5|Briefly described|p16 Fig.2.2. |Statherian|Statherian|Broken Hill Domain, Curnamona Province.|1685 +/- 3 Ma.|||||
8489|Hores Gneiss|62728|6|Mentioned|p26|||Host to the Broken Hill Ag-Pb-Zn mine. Geological Province: Broken Hill Domain/Curnamona Province.||||||07-FEB-11
8489|Hores Gneiss|62993|5|Briefly described|p7, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Hosts Broken Hill Pb-Zn-Ag lodes.|1685+/-3 Ma (SHRIMP)|Purnamoota Subgroup|||Volcaniclastic sedimentary rocks.|16-DEC-21
8489|Hores Gneiss|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: 1686+/-5Ma. Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
8489|Hores Gneiss|63102|5|Briefly described|p10,13-14,33,38,40,53-54|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province. S-type felsic magmatism hosting Broken Hill Pb-Zn-Ag lodes. Chronostratigraphic equivalent of Lady Louise Suite. Separates the Broken Hill and Sundown groups.|1685+\-3 Ma|Unit of the Broken Hill Group.||Intrudes Broken Hill Group.||22-OCT-19
8489|Hores Gneiss|63110|6|Mentioned|p1130|Statherian|Statherian|Age: 1686+/-3Ma. Rocks are mainly volcanic in origin.||||||11-JUN-08
8489|Hores Gneiss|63186|5|Briefly described|p68, p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1685 Ma. Geological Province: Curnamona Province.||||||07-NOV-08
8489|Hores Gneiss|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Quartz-feldspar-biotite-garnet gneiss, interpreted as metadacite. Age: 1690+/-5Ma (U-Pb zircon). Minor metasediments included. Geological Province: Broken Hill Domain; with unnamed equivalents in Olary Domain.||||||07-NOV-08
8489|Hores Gneiss|63519|4|Described|p5, p6 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Age: 1660-1640Ma (zircon) and 1686+/-3Ma. Quartzo-feldspathic gneiss; metavolcanic. Surficial deposit, not an intrusion. Hosts the Broken Hill orebody.  See also p10 Fig. 3 and throughout publication.||||||07-NOV-08
8489|Hores Gneiss|63866|4|Described|p36, p38-p39, p41|||Broken Hill Domain, Curnamona Province.  Hosts the Broken Hill Pb-Zn-Ag lode. Protoliths are interpreted to have been mass-flow felsic volcanics. |1685 +/- 3 Ma (Page et al., 2005a)|Purnamoota Subgroup||Overlain by the Sundown Group.|Quartz-feldspar-garnet-biotite gneiss and quartzofeldspathic gneiss with intercalated metasedimentary rocks.|
8489|Hores Gneiss|64097|5|Briefly described|p302 Tb. 1, p303|Paleoproterozoic|Paleoproterozoic|At top of Purnamoota Subgroup (Broken Hill Group). Age: 1685+/-3Ma. Hosts the Broken Hill orebody. Lithology includes Potosi-type gneiss.||||||07-FEB-11
8489|Hores Gneiss|64316|5|Briefly described|p531, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Purnamoota Subgroup (Broken Hill Group, Willyama Supergroup). Ages: 1689+/-5Ma and 1685+/-3Ma (SHRIMP U-Pb). Geological Province: Broken Hill Block. Includes the Potosi-type gneiss, and metasedimentary xenoltihs. .||||||07-FEB-11
8489|Hores Gneiss|64741|4|Described|p301 Fig. 4, p309, p310|Paleoproterozoic|Paleoproterozoic|Of Purnamoota Subgp (Broken Hill Gp). Age: 1685+/-3Ma. Geol.prov: Broken Hill Domain.Uppermost "Potosi-type" gneiss unit overlying Freyers Metasediments. Extensive/thick sheet-like complex of felsic extrusives, volcaniclastic + clastic metasediments||||||07-FEB-11
8489|Hores Gneiss|64742|6|Mentioned|p321 Fig.3.|||||Unit in Broken Hill Group.||||
8489|Hores Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Purnamoota Subgroup (Broken Hill Group). Geological province: Broken Hill Domain.||||||07-FEB-11
8489|Hores Gneiss|65887|5|Briefly described|p51|Statherian|Statherian|Felsic rocks from this unit, spatially and temporally associated with Fe-rich amphibolites in Broken Hill Group, are aged 1685+/-3 Ma (Page et al., 2005).||||||
8489|Hores Gneiss|66302|5|Briefly described|p36 Fig.9, p38-40|Statherian|Statherian|Broken Hill Domain, Curnamona Province. Time equivalent of the Rasp Ridge granite gneiss.||Purnamoota Subgroup||Overlies the Freyers Metasediments.||
8489|Hores Gneiss|66857|5|Briefly described|p971.|Paleoproterozoic|Paleoproterozoic|Yanco Glen. Contains convincing porphyritic and volcaniclastic textures indicating its provenance.||Unit in Willyama Supergroup.|||Quartzo-feldspathic gneiss.|
8489|Hores Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1685 +/- 3 Ma.|Broken Hill Group.||||
8489|Hores Gneiss|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
8489|Hores Gneiss|68126|5|Briefly described|p6, p25-26, p29-30|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Apparently related to a c.1690 Ma thermal event.|1684 +/- 6 Ma (Stevens et al., 2008).|||||
8489|Hores Gneiss|69999|6|Mentioned|p5|||||||||
8489|Hores Gneiss|70000|5|Briefly described|p34, p36|Statherian|Statherian|Granulite facies metasediments. Hosts the massive Pb-Zn-Ag sulfide mineralisation of the giant Broken Hill Line of Lode.||Unit in Purnamoota Subgroup.|||Garnet-bearing quartzofeldspathic Potosi-type gneiss.|
8489|Hores Gneiss|70014|5|Briefly described|Map legend|||Lithologies listed in some detail. Interpreted as a rhyodacitic-dacitic metavolcanic, probably an ashflow tuff or submarine lava flow.||Unit in Purnamoota Subgroup.||Overlies Freyers Metasediments. Is overlain by Sundown Group.|Mainly garnet-bearing quartzo-feldspathic gneiss. Medium- to fine-grained quartz-plagioclase-K feldspar-biotite-garnet gneiss ("Potosi" or "Parnell" gneiss). Minor migmatitic units. Various proportions of intercalated metasediments.|
8489|Hores Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Purnamoota Subgroup.|||Massive quartzofeldspathic +/- garnet gneiss; quartz-plagioclase-K feldspar-biotite garnet gneiss ("Potosi"-type gneiss); minor metasedimentary rocks.|
8489|Hores Gneiss|70405|5|Briefly described|p41|Paleoproterozoic|Paleoproterozoic||1685 Ma|Purnamoota Subgroup|||Volcaniclastic metasediments.|
8489|Hores Gneiss|70657|4|Described|p10 Fig.4, p12, p13 Fig.6, p15-16, p31|Statherian|Statherian|See also p40, p45-46, p58. Curnamona Province; Broken Hill, Mulyungarie Domains. Is interpreted to host the Broken Hill Pb-Zn-Ag lodes. Similar age to Silver City Suite (Stevens and Barron 2002) and approximates the age of Lady Louise Suite.|1685 +/- 3 Ma (Page et al., 2003).|Willyama Supergroup.||Overlies Freyers Metasediments (Broken Hill Group). Underlies Sundown Group.|Volcaniclastic gneiss of extrusive igneous origin.|
8489|Hores Gneiss|70658|6|Mentioned|p15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|1685 +/- 3 Ma.|Purnamoota Subgroup.||||
8489|Hores Gneiss|72435|6|Mentioned|p715|Statherian|Statherian||1685 +/- 3 Ma|Broken Hill Group||||
8489|Hores Gneiss|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain. Shown only on p2 Fig.2 and p8 Fig.6.|||||Includes gneiss.|
8489|Hores Gneiss|72461|4|Described|p6, p11, p13, p16-19|||Interpreted to have comprised felsic extrusive material, volcaniclastic and clastic metasediment. Uppermost Potosi-type gneiss of the Broken Hill Group. Hosts the Broken Hill Pb-Zn-Ag lodes and Hores-type Tungsten (stratabound scheelite and wolframite). Petrographic Descriptions of both the highly metamorphosed and less metamorphosed examples of this unit are provided.|1685 Ma|Broken Hill Group||Overlies the Freyers Metasediments. Overlain by the Sundown Group.|Medium- to coarse-grained, porphyritic, garnet-bearing quartzo-feldspathic gneiss.|
8489|Hores Gneiss|73021|6|Mentioned|p224|||Hosts the Broken Hill Zn-Pb-Ag deposit.||Broken Hill Group.||||
8489|Hores Gneiss|73243|6|Mentioned|p52 Fig.1|Statherian|Statherian|Broken Hill block-Euriowie block.|1685 +/- 3 Ma|Broken Hill Group||||
8489|Hores Gneiss|73308|5|Briefly described|p606-607, 612-613, 615, 617-618|||Formed on or at shallow depths below the sea-floor. Hydrothermal plumes are proposed as the source of much of these magnetite deposits.|1685 +/- 3 Ma (SHRIMP: Page et al., 2005).|Broken Hill Group.||Is overlain by Sundown Group.|Hosts the Pb-Zn-Ag orebody in the Broken Hill Group.|
8489|Hores Gneiss|73482|5|Briefly described|p422 Fig.3, p423, p428 Fig.7|Statherian|Statherian|See also p432 Fig.11.|1685+/-3 Ma (Page and Stevens et al., 2005)|Broken Hill Group|||Includes an extensive volcanic component.|
8489|Hores Gneiss|73512|6|Mentioned|p2|||||||||
8489|Hores Gneiss|73524|6|Mentioned|p5 Fig.3|Statherian|Statherian||1685+/-3 Ma|Broken Hill Group||||
8489|Hores Gneiss|73575|5|Briefly described|p828, p829 Fig.3, p830, p831 Fig.5, p838|Statherian|Statherian|Host to the Line of Lode mineral deposit.|1685+/-3 Ma|Purnamoota Subgroup||Overlies Freyers Metasediments, underlies Sundown Group|Locally consists of acid metavolcanics ('Potosi-type gneiss') and variously altered metasedimentary rocks. Includes amphibolite units.|
8506|Horseshoe Creek Subgroup|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Wollombi Coal Measures (Singleton Supergroup). Max. thickness: 110m. Geological Province: Sydney Basin.||||||
8506|Horseshoe Creek Subgroup|22969|4|Described|Fig 4.1a||Late Permian|Wollombi Coal Measures.||||||
8506|Horseshoe Creek Subgroup|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Wollombi Coal Measures. Geological Province: Sydney Basin||||||
8506|Horseshoe Creek Subgroup|41010|6|Mentioned|Table 1|||||||||
8506|Horseshoe Creek Subgroup|42078|6|Mentioned|Table 1 P5|||||||||
8506|Horseshoe Creek Subgroup|42916|5|Briefly described|Table 1||Late Permian|||||||
8506|Horseshoe Creek Subgroup|43257|5|Briefly described|Map Legend||Late Permian|Of Wollombi Coal Measures||||||
8506|Horseshoe Creek Subgroup|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Wollombi Newcastle Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
8512|Hoskinstown Group|22768|5|Briefly described|p177|Ludlow|Wenlock|||||||
8512|Hoskinstown Group|22857|5|Briefly described|p177, p474 App.1 Tb.A1.6|Ludlovian|Wenlockian|Geological Province: Captains Flat-Goulburn Trough.||||||
8512|Hoskinstown Group|23048|6|Mentioned|p2||Late Silurian|||||||
8512|Hoskinstown Group|32820|6|Mentioned|p3|||Formation members.||||||20-MAY-08
8512|Hoskinstown Group|36413|2|Defined|p55|Silurian|Silurian|||||||
8512|Hoskinstown Group|36414|5|Briefly described|map legend|Pridolian|Ludlovian|Includes Captains Flat Formation, Carwoola Formation, Kohinoor Volcanics and Copper Creek Shale.||||||
8512|Hoskinstown Group|37727|6|Mentioned|p63|||||||||
8512|Hoskinstown Group|40328|4|Described|p180|||||||||
8512|Hoskinstown Group|42727|5|Briefly described|map legend|Pridoli|Ludlow|Includes Captains Flat and Carwoola Formations, Kohinoor Volcanics and Copper Creek Shale. Geol. Prov: Captains Flat Block.||||||
8512|Hoskinstown Group|42820|2|Defined|p45|Pridoli|Ludlow|||||||
8512|Hoskinstown Group|44093|5|Briefly described|p209 App. 1|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
8512|Hoskinstown Group|48878|14|Not recorded|Fig.3,p.7||Silurian|(I55-16). Defn. on Tech.File I/55-16.||||||
8512|Hoskinstown Group|66197|5|Briefly described|p631 Fig.3c|Late Silurian|Late Silurian|Includes Captains Flat, Carwoola and Kohinoor Formations and the Copper Creek Shale.||||||13-MAR-12
8512|Hoskinstown Group|68592|5|Briefly described|p743-4|||The Hoskinstown Group on the Canberra and Michelago 1:100 000 map sheets is similar to the Mount Fairy Group in that it has a shale-rich base with sporadic limestone bodies (Copper Creek Shale), an overlying felsic volcanic pile (Kohinoor Volcanics), Carwoola Formation turbidites (Abell 1991) and the overlying to laterally equivalent shale and siltstone-rich Captains Flat Formation which also contains some volcanic rocks.|||Copper Creek Shale, Kohinoor Volcanics, Carwoola Formation, Captains Flat Formation.|||
8512|Hoskinstown Group|69270|5|Briefly described|p20|Late Silurian|Late Silurian||||Kohinoor Volcanics||Mineralised basal volcanosedimentary sequences.|15-JUL-15
8512|Hoskinstown Group|69635|5|Briefly described|p11, 32, 38, 1|||See also Hoskintown Group p12, 14, 19, 25|||Includes Kohinoor Volcanics, Captains Flat Formation.|||
8512|Hoskinstown Group|71069|3|Fully described|p9, p10, p21 fig 7, p24, p26 fig 9|Pridoli|Wenlock|Named after the Village of Hoskinstown. Originally rocks of this group were mapped as Mount Fairy Group. Estimated to be around 3.9km thick. Hosts the Captains Flat mine VAMS mineralisation, gold vein deposits and small scale skarn-related deposits (Jerangle and Bold Slate Range prospects). Age constrained by SHRIMP dates of constituent units. Intruded by the Briars Sharrow Gabbro. Equivalent to the Mount Fairy Group and parts of the Campbells Group and Kangaloolah Volcanics. Distribution, geochemistry, tectonic structure, metamorphism and geological hazards discussed. See also p28, p29, p31, p35, p36, p38 fig 15, p41, p42, p50 tbl 3, p71, p85, p99-105, p109, p114-p118, p124, p125, p133, p134, p146, p154, p175, p185.|||Includes the Kohinoor Volcanics, Carwoola Formation, Copper Creek Shale and the Captains Flat Formation.|Overlies the Glenbog Suite. Unconformably overlies the Adaminaby, Bendoc and Margules Groups. Is faulted against the Warbisco Shale and the Bumballa Formation.|Volcanic and sedimentary rocks including: felsic to intermediate coherent volcanics, volcaniclastic basalt, conglomerate and quartz sandstones.|
8512|Hoskinstown Group|71691|5|Briefly described|Map legend.|Silurian|Silurian||||Carwoola Formation, Captains Flat Formation, Kohinoor Volcanics.|Overlies Margules Group.||
8512|Hoskinstown Group|71700|5|Briefly described|p14-p15|Early Devonian|Silurian|Potentially contains an early Devonian deep-water sequence.|||Includes the Kohinoor Volcanics and the Carwoola Formation.|||
8515|Hoskissons Coal|22857|4|Described|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Coogal Subgroup (Black Jack Group). Coal with subordinate sandstone, carbonaceous siltstone, claystone and tuff. Max. thickness: 18m. Geological Province: Gunnedah Basin.||||||17-FEB-06
8515|Hoskissons Coal|23050|5|Briefly described|p82 Fig.17|Late Permian|Late Permian|of Black Jack Group, Gunnedah Basin||||||
8515|Hoskissons Coal|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
8515|Hoskissons Coal|41290|6|Mentioned|p226|||||||||
8515|Hoskissons Coal|42767|5|Briefly described|Fig.5|||||||||
8515|Hoskissons Coal|43194|5|Briefly described|p133 App. 1|Late Permian|Late Permian|Replaces Hoskissons Coal 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.||||||
8515|Hoskissons Coal|43582|6|Mentioned|Fig.5,p16||Late Permian|May be incomplete name from figure caption||||||
8515|Hoskissons Coal|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Coogal Subgroup.||||||05-JUL-04
8515|Hoskissons Coal|61313|5|Briefly described|p96 Fig.G9, p97, p98 Fig.G10|Permian|Permian|Of Black Jack Group. An Important marker bed in Gunnedah area; part of the upper Black Jack Group which acts as seal for the basal Black Jack Group 'western bed load' reservoir sandstones. Overlain by Clare Sandstone Member. Geol. Prov: Gunnedah Basin.||||||16-JUN-06
8515|Hoskissons Coal|61377|5|Briefly described|p154 Fig. SU9|Late Permian|Late permian|Of the Black Jack Group. Geological Province: Gunnedah Basin.||||||07-FEB-11
8515|Hoskissons Coal|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Coogal Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Coal with minoe tuff, claystone, siltstone and sandstone.||||||
8515|Hoskissons Coal|65116|5|Briefly described|p447, 448, 449, Fig 6 p441|Late Permian|Late Permian|?Of Black Jack Group. Regionally extensive coal seam. Low energy fluvial deposits including coal. Sequence D2||||||
8515|Hoskissons Coal|68003|5|Briefly described|p38 Fig.3-j, p41, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Mis-spelt as Hosskissons Coal on p41.||Unit in Coogal Subgroup.||Overlies Brigalow and Arkarula Formations. Is overlain by Clare Sandstone and Benelabri Formation.||
8515|Hoskissons Coal|68004|4|Described|p23 Table 1, p142, pp146-153, p166.|||Gunnedah Basin. In one paragraph on p85, this unit is written as Hoskissons Coal Member and Huskisson Coal, and is stated to overlie a sodium bicarbonate-bearing aquifer. Has economic potential for coal in both the northern and southern sections of the Mullaley Sub-basin. Average thickness 6 m. Described in detail. See also references to Hoskissons Seam (pp169-170).||Basal unit in Coogal Subgroup.||Overlies Brigalow and Arkarula Formations.|Predominantly low to medium ash, high volatile thermal coal: thick coal plies with minor sandstone, siltstone, claystone and tuff bands.|
8515|Hoskissons Coal|70791|5|Briefly described|p277|Lopingian|Lopingian|Gunnedah Basin.||Coogal Subgroup.||||
8515|Hoskissons Coal|70878|4|Described|p715-718, p723|Permian|Permian|Gunnedah Basin. Lithostratigraphy reinterpreted; discussed. Calibration of palynological ages.|258.05 +/- 0.08 Ma.|Black Jack Group.||Overlies Pamboola Formation. Is overlain by Clare Sandstone or Benelabri Formation.|Includes tuff layers.|
8538|Howqua Chert|22628|6|Mentioned|fig1p108|||||||||
8538|Howqua Chert|22832|5|Briefly described|p635|Ordovician|Cambrian|||||||
8538|Howqua Chert|23229|5|Briefly described|Table3-1p16, 19||Cambrian|||||||
8538|Howqua Chert|23307|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
8538|Howqua Chert|23309|5|Briefly described|p43|||||||||
8538|Howqua Chert|23860|5|Briefly described|p944|Ordovician|Cambrian|Overlying unit Pinnak Sandstone.||||||
8538|Howqua Chert|24002|5|Briefly described|p228 Fig.2|Cambrian|Cambrian|||||||
8538|Howqua Chert|24003|5|Briefly described|p258|||||||||
8538|Howqua Chert|24004|5|Briefly described|p275 Fig.2|Ordovician|Ordovician|||||||
8538|Howqua Chert|24037|6|Mentioned|p425 Fig.2|Early Ordovician|Cambrian|Geological Province: Lachlan Fold Belt.||||||
8538|Howqua Chert|24098|5|Briefly described|p27 Fig. 2|Late Cambrian|Late Cambrian|Geological Province: Lachlan Fold Belt.||||||
8538|Howqua Chert|24551|4|Described|p90|Early Ordovician|Early Ordovician|||||||
8538|Howqua Chert|24576|6|Mentioned|p737|||Geological Province: Lachlan Fold Belt||||||
8538|Howqua Chert|29709|5|Briefly described|p33|||||||||
8538|Howqua Chert|30329|6|Mentioned|p30|||On table P30||||||
8538|Howqua Chert|31161|5|Briefly described|PA9|||||||||
8538|Howqua Chert|32074|6|Mentioned|p18|||||||||
8538|Howqua Chert|33602|6|Mentioned|p18|||||||||
8538|Howqua Chert|33607|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8538|Howqua Chert|35073|4|Described|p4|||||||||
8538|Howqua Chert|35112|6|Mentioned|p276|||||||||
8538|Howqua Chert|35281|6|Mentioned|p23|||||||||
8538|Howqua Chert|36534|6|Mentioned|p222|||||||||
8538|Howqua Chert|39331|6|Mentioned|Fig.0-3|||||||||
8538|Howqua Chert|41571|6|Mentioned|Table 2.6|||||||||
8538|Howqua Chert|42827|5|Briefly described|Fig 2.6|||||||||
8538|Howqua Chert|61160|5|Briefly described|p46|||Conformably overlain by Pinnak Sandstone. ||||||
8538|Howqua Chert|61161|5|Briefly described|p78, p14|||Underlies Pinnak Sandstone.||||||
8538|Howqua Chert|62742|5|Briefly described|p699 Fig. 2|Late Cambrian|Late Cambrian|Siliceous siltstone (chert). In the Mount Wellington Greenstone Belt.||||||
8538|Howqua Chert|62744|5|Briefly described|p708|Late Cambrian|Late Cambrian|Geological Province: Mount Wellington Greenstone Belt.||||||
8538|Howqua Chert|66196|4|Described|p616, p617, p622, 623|Early Ordovician|Early Cambrian|Conformably overlies Lickhole Volcanics, underlies Adaminaby Group. To 480m thick. Dated from conodonts and graptolites. Deep-sea environment. Lower chert is blue/dark-grey and vitreous; middle and upper is pale-grey to white with thin shale interbeds.||||||
8538|Howqua Chert|67322|6|Mentioned|p15|Datsonian|Datsonian|Late Cambrian age based on the presence of Cordylodus conodonts (Stewart and Fergusson 1988, Kakuwa and Webb 2010).||||||
8538|Howqua Chert|68116|5|Briefly described|Appendix, Maps 26, 34, 52.|Floian|Late Cambrian|Minimum age written as Lancefieldian in text.|||||Black chert, siliceous shale, mafic sandstone, pebbly sandstone and chert conglomerate.|
8538|Howqua Chert|68314|5|Briefly described|p750, p754, p756|Late Cambrian|Late Cambrian|Mount Wellington Greenstone Belt. Contains Datsonian conodonts.|||||Fine-grained siliceous siltstones; abundantly fossiliferous.|
8538|Howqua Chert|68466|6|Mentioned|p70|Ordovician|Cambrian|Lachlan Orogen. Very low degree of bioturbation implying low oxygen in Early Ordovician deep ocean waters.||||||
8538|Howqua Chert|68592|5|Briefly described|p279, p287|Early Ordovician|Early Ordovician|||||Overlies Lickhole Volcanics. Is overlain conformably by Pinnak Sandstone.||
8538|Howqua Chert|68822|6|Mentioned|p346|||||||Underlain by the Mount Read Volcanics.||
8538|Howqua Chert|70493|6|Mentioned|p56|Late Cambrian|Middle Cambrian|Tabberabbera Zone, Lachlan Orogen.||||Overlies Lickhole Volcanics. Is overlain by Adaminaby Group.||
8538|Howqua Chert|70601|4|Described|p43-48, p52|Lancefieldian|Middle Cambrian|Howqua East area. Jamieson Volcanics could be source of felsic tuff bands in chert. Estimated thickness 480m. Contains 480 Ma graptolites in carbonaceous shale at top. Howqua Chert fragments and blocks found in melange within Cobannah Group. |c.485 Ma: zone fossil conodont Cordylodus proavus.|||Underlies Pinnak Sandstone (Adaminaby Group). Conformably overlies Eagles Peak Basalt and Dookie Igneous Complex. Equivalent to "Melville Chert".|Carbonaceous shale, graptolites and conodont Cordylodus proavus in upper horizon of chert. At Dookie, the chert contains felsic tuff bands, minor sandstone and conglomerate with gabbroic detritus.|
8538|Howqua Chert|70661|6|Mentioned|p14|Lancefieldian|Lancefieldian|||||Conformably overlain by Adaminaby Group, overlies Lickhole Volcanics.||
8538|Howqua Chert|71069|6|Mentioned|p52|Lancefieldian|Lancefieldian|||||Overlies the Lickhole Volcanics. Overlain by the Pinnak Sandstone.||
8538|Howqua Chert|71700|6|Mentioned|CD|Lancefieldian|Lancefieldian|||||||
8538|Howqua Chert|73059|6|Mentioned|p1053 Fig.2, 1059|Ordovician|Cambrian|||||Overlies Lickhole Volcanics. Is overlain by Adaminaby Group.||
8569|Hume Limestone Member|6969|5|Briefly described|p14, p15|Middle Ludlow|Middle Ludlow|Contains conodont fauna, Oulodus elegans, in Yass area.  Geological Province: Lachlan Fold Belt.||||||
8569|Hume Limestone Member|13996|6|Mentioned|p134-135|Silurian|Silurian|Yass area. Rugose corals described; affinities with China, Kazakhstan. See also references to Hume Limestone (p131, p136).||||||
8569|Hume Limestone Member|22857|4|Described|p460 App.1 Tb.A1.6|Ludlovian|Ludlovian|Of the Silverdale Formation. Coral and crinoidal biomicrites and biosparites, shaly mudstone. Max. thickness: 26.5m. Geological Province: Canberra-Yass Shelf. ||||||
8569|Hume Limestone Member|24248|5|Briefly described|p52, p54|Ludfordian|Gorstian|Parent: Silverdale Formation. Overlying Unit: Black Bog Shale (tr.). Biostromal limestone.||||||
8569|Hume Limestone Member|29791|6|Mentioned|p89|||||||||
8569|Hume Limestone Member|29989|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
8569|Hume Limestone Member|30069|6|Mentioned|p9|||Table on P9.||||||
8569|Hume Limestone Member|31852|5|Briefly described|p711|||See also P712,714,715. Ludlovian||||||
8569|Hume Limestone Member|32155|6|Mentioned|Fig.1|||Fossil occurrences||||||
8569|Hume Limestone Member|32413|6|Mentioned|p101|||||||||
8569|Hume Limestone Member|32483|4|Described|p20|||Sil. Strat. table 1||||||
8569|Hume Limestone Member|34692|5|Briefly described|p186|||||||||
8569|Hume Limestone Member|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
8569|Hume Limestone Member|35386|3|Fully described|p31|||Part of Silverdale Formation||||||
8569|Hume Limestone Member|35501|6|Mentioned|p156|||||||||
8569|Hume Limestone Member|37727|6|Mentioned|p8|||See also P64.||||||
8569|Hume Limestone Member|39331|6|Mentioned|Fig.5-5|||||||||
8569|Hume Limestone Member|40328|4|Described|p111|||||||||
8569|Hume Limestone Member|42477|5|Briefly described|p85|||||||||
8569|Hume Limestone Member|45075|5|Briefly described|p7|||Fauna||||||
8569|Hume Limestone Member|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Silverdale Formation (Hattons Corner Group).  Overlies Barrandella Shale Member; partly underlies Black Bog Shale.||||||
8569|Hume Limestone Member|61894|5|Briefly described|p180|Late Silurian|Late Silurian|Hattons Corner, Yass district.||Silverdale Formation.||||
8569|Hume Limestone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Silverdale Formation (Hattons Corner Group). Coralline limestone, biomicrite.||||||
8569|Hume Limestone Member|68592|2|Defined|p429-30 Fig.89, p560, p562, p579-82|Ludfordian|Gorstian|See also p1879-80. Brunker and Offenberg (1970); Offenberg (1974); included this unit as a Member in their Derringullen Formation. Formerly Hume Limestone (Brown, 1940). Transferred to Silverdale Formation by Link (1970, 1971). Type section described. 7-26m thick. Richly fossiliferous: fauna listed.||Unit in Silverdale Formation.||Gradationally overlies Barrandella Shale Member. Is overlain conformably by Black Bog Shale.|Generally thin but persistent limestone, consisting of coralline and crinoidal biomicrite interbedded with shaly mudstone.|
8569|Hume Limestone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Shsh. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Silverdale Formation (upper unit)||Overlies Barrandella Shale Member. Is overlain by Black Bog Shale.|Coralline and crinoidal biomicrite and biosparite interbedded with shaly mudstone.|
8569|Hume Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Silurian|||Silverdale Formation|||Coralline and crinoidal biomicrite and biosparite interbedded with shaly mudstone.|
8569|Hume Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Silurian|||Silverdale Formation|||Coralline and crinoidal biomicrite and biosparite interbedded with shaly mudstone.|
8569|Hume Limestone Member|71656|4|Described|p12 Fig.2, p19, p23-24, p52|Late Silurian|Late Silurian|The fauna of the Hume Limestone Member is dominated by framework-building organisms such as corals, stromatoporoids and sponges.||Of Silverwood Formation, Hattons Corner Group||Overlies Barrandella Shale Member.|Fossiliferous limestone.|
8572|Hume Park Granite|29989|6|Mentioned|Map legend|Devonian|Late Silurian|Siluro-Devonian||||||
8572|Hume Park Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
8572|Hume Park Granite|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
8572|Hume Park Granite|30734|6|Mentioned|p18|||||||||
8572|Hume Park Granite|32483|4|Described|p27|||Sil.-Dev. Strat. table 1||||||
8572|Hume Park Granite|33732|6|Mentioned|p112|||||||||
8572|Hume Park Granite|34405|6|Mentioned|Fig.3.12|||||||||
8572|Hume Park Granite|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
8572|Hume Park Granite|35386|4|Described|p61|||Early? Devonian.||||||
8572|Hume Park Granite|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
8572|Hume Park Granite|40328|4|Described|p207|||||||||
8572|Hume Park Granite|42726|5|Briefly described|map legend|Silurian||||||||
8572|Hume Park Granite|50230|5|Briefly described|Map legend|Ludlow|Ludlow|Part of the Wyangala Batholith.  Biotite granite.||||||
8572|Hume Park Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Part of the Young Suite. Grey, medium- to coarse-grained, equigranular to porphyritic, cordierite?-biotite granite and granodiorite with occasional biotite-rich dioritic enclaves.||||||
8572|Hume Park Granite|68592|2|Defined|p443, p467, p957, p1225, p1227, p1239-45|Wenlock|Wenlock|Originally mapped by Browne (1959); remapped by Cramsie et al. (1975, 1978). Chappell et al. assigned the granite to their Hume Park Suite; reassigned by Blevin (2011) to the Young Suite of the Bullenbalong Supersuite. Named after Hume Park locality on the edge of Lake Burrinjuck. Type locality and representative outcrops are described. A small pluton (2.9 km2) 11km SW of Yass. Undeformed. Geochemistry, geophysical properties described. No known mineralisation. Comagmatic with Douro Group volcanics. Not isotopically dated; age from affinity with Young Granodiorite.||Unit in Young Suite.||Intrudes Hawkins Volcanics. Is faulted against Mountain Creek Volcanics.|Grey, medium- to coarse-grained, equigranular to porphyritic, cordierite?-biotite granite and granodiorite; the granite contains sporadic, small, biotite-rich dioritic enclaves and rare schistose, quartzitic metasandstone xenoliths. S-type.|
8572|Hume Park Granite|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Syh. Shown on Time-Space Plot as in Yass 1:100 000 map sheet area.||Young Suite|||Medium-coarse grained, equigranular to porphyritic, cordierite?-biotite granite and granodiorite with sparse biotite rich dioritic enclaves and rare metasandstone xenoliths.|
8572|Hume Park Granite|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Young Suite|||Medium-coarse grained, equigranular to porphyritic, cordierite?-biotite granite and granodiorite with sparse biotite rich dioritic enclaves and rare metasandstone xenoliths.|
8572|Hume Park Granite|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Young Suite|||Medium-coarse grained, equigranular to porphyritic, cordierite?-biotite granite and granodiorite with sparse biotite rich dioritic enclaves and rare metasandstone xenoliths.|
8589|Hungerford Granite|34469|6|Mentioned|p108|||Devonian||||||
8589|Hungerford Granite|42467|5|Briefly described|Map Legend|||||||||
8589|Hungerford Granite|43386|14|Not recorded|Map Legend||Devonian|||||||
8589|Hungerford Granite|43411|14|Not recorded|Map Legend||Late Devonian|361 million years||||||
8589|Hungerford Granite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
8589|Hungerford Granite|68731|5|Briefly described|p166 Fig 3.78, p167 Tb 3.2|Early Devonian|Silurian|Includes sparse inclusions of biotite schist (to ~10 cm). See also Eulo Ridge Granite.|419.1 +/- 2.5 Ma||||Pale grey, medium-grained, moderately porphyritic; muscovite-biotite monzogranite; scattered phenocrysts of white K-feldspar (to ~ 5 cm); gneiss (to ~30 cm); reduced; cut by sparse, thin quartz veins; deformed; very poorly exposed.|
8589|Hungerford Granite|68823|5|Briefly described|p378 Fig.4, p393|Lochkovian|Ludlow|Geochronology by Bultitude and Cross (2012).|419.1 +/- 2.5 Ma, SHRIMP-IIe|||||
8589|Hungerford Granite|68901|5|Briefly described|p7 Fig. ii|Late Silurian|Late Silurian|Eulo Ridge, Thomson Region.
|||||Grey, porphyritic muscovite-biotite monzogranite.|26-SEP-18
8589|Hungerford Granite|69002|5|Briefly described|p10, p13, Map 1b|Famennian|Givetian|Exposed in scattered outcrops between Hungerford on the NSW-QLD border and  Eulo 100km north in QLD. K-Ar dating by Evernden and Richards (1962) and SHRIMP-IIe dating by Geoscience Australia.|c.361 Ma, K-Ar; 385 Ma, SHRIMP-IIe|||||
8589|Hungerford Granite|69042|5|Briefly described|map, map legends|Devonian|Silurian|Thomson Orogen. ?Low-magnetic intensity||||||
8589|Hungerford Granite|69043|6|Mentioned|p11|||Thomson Orogen.||||||
8589|Hungerford Granite|69541|6|Mentioned|p644 Fig.1(a)|Early Devonian|Late Silurian|Thomson Orogen.||||||
8589|Hungerford Granite|69952|5|Briefly described|p1, p2 Tb.i, p16, p30-33, p123|Late Silurian|Late Silurian|Southern part of the Eulo Ridge, Thomson Orogen. Deeply weathered; poor exposures of sparse low boulders and bouldery rubble. SHRIMP U-Pb zircon age of emplacement.|419.1 +/- 2.5 Ma (Cross et al., 2015).||||Grey, porphyritic muscovite-biotite monzogranite.|
8589|Hungerford Granite|70033|6|Mentioned|p1, p18|Silurian|Silurian|Age: late Silurian.|419.1 +/- 2.5 Ma, Cross et al. 1995|||||16-JUL-15
8589|Hungerford Granite|70720|6|Mentioned|p2|||Eulo Ridge, southern Thomson Orogen.||||||
8589|Hungerford Granite|70744|5|Briefly described|p939|||Thomson Orogen (NW NSW). Age by Bultitude and Cross (2013).|c.419 Ma (estimated from Fig.7).|||||
8589|Hungerford Granite|70749|5|Briefly described|p43|Devonian|Devonian|Southern Thomson and Koonenberry area.|419.1 +/- 2.5 Ma.|||||
8589|Hungerford Granite|70821|5|Briefly described|p9-10, p12, p13 Tb.2.1, p89|Early Devonian|Late Silurian||419.1 +/- 2.5 Ma (Bultitude and Cross, 2013).||||Includes monzogranite.|01-DEC-16
8589|Hungerford Granite|71592|5|Briefly described|Appendix A.|||Thomson Orogen.|419+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
8589|Hungerford Granite|71860|5|Briefly described|p7|||Age is a SHRIMP U-Pb date.|419.1 +/- 2.5 Ma (Bultitude et al. 2012)||||Monzogranite.|
8589|Hungerford Granite|71965|5|Briefly described|p897,901-904,906,910,913|Lochkovian|Pridoli|Geological province: Thomson Orogen. Outcropping S-type granite in the southern Thomson Orogen. Dated at 419.5+\-2.5 Ma (Cross et al., 2015).|419.5+\-2.5 Ma||||Deeply weathered, medium-grained, moderately porphyritic muscovite-biotite monzogranite with metasedimentary inclusions.|
8589|Hungerford Granite|71966|5|Briefly described|p988-993,995,1000-1002,1004-1005|Early Devonian|Late Silurian|Geological province: Thomson Orogen. S-type granitic intrusion associated with c. 430-395 Ma magmatism in the southern Thomson Orogen. Crops out along the Eulo Ridge basement high; part of a batholithic scale belt of intrusions termed the Ella belt (Purdy et al., 2018). Outcrop sample collected and analysed for SHRIMP U-Pb geochronology, and Lu and Hf isotopic analysis. Sample 2122055 yielded an age of 419.1+\-2.5 Ma, which is interpreted as the crystallisation age of this rock. Age equivalent to Tibooburra Suite. Hf and O isotopic analysis confirms S-type affinity, with less evolved Hf isotopic signatures than the Ordovician granites, indicating different source components between Silurian and Ordovician granites.|419.1+\-2.5 Ma (crystallisation)|||||25-OCT-19
8589|Hungerford Granite|72522|5|Briefly described|p49|Lochkovian|Pridoli|Along Eulo Ridge, south of Granite Springs Granite.|419.1+/-2.5 Ma|||||
8589|Hungerford Granite|72914|6|Mentioned|p16|Lochkovian|Silurian|S-type affinity. Similar U-Pb age, geochemistry and petrological characteristics as Brewarrina Granite. These two units potentially represent intrusions with a close spatial affinity but were separated by extension related to the Paka Tank Trough (~400 Ma).|419.1 +/- 2.5 Ma|Tibooburra Suite?||||
8589|Hungerford Granite|72915|6|Mentioned|p5, p17|||May be intrinsically related to the metamorphic basement rock from the Congararra 1 borehole [tentatively interpreted as the Twin Tanks Metamorphics]. Map symbol suggests Silurian age.||||||
8589|Hungerford Granite|72951|6|Mentioned|p1026, 1028|Lochkovian|Pridoli|Thomson Orogen, southern.|419.1 +/- 2.5 Ma|||||
8589|Hungerford Granite|73179|6|Mentioned|p1133, p1134 Fig.1, p1153-1154|late Silurian|late Silurian|||||||20-SEP-22
8593|Hunter Valley Volcanics|33220|6|Mentioned|Fig.4c|||||||||
8610|Hutton Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p496, p498-499|Callovian|Aalenian|Eromanga and Mulgildie Basins. An important aquifer. Up to 250m thick.||||Conformably overlies Poolowanna Formation. Equivalent to Algebuckina Sandstone.|Well-sorted, cross-bedded, quartzose to sub-labile fluvial sandstone, with minor thin conglomerate bands and thin beds of siltstone and mudstone.|
8610|Hutton Sandstone|13497|4|Described|ix, p26, p89, p104, p112|Jurassic|Jurassic|Eromanga Basin. Deposited in a low sinuosity fluvial environment. Disconformably overlies the Arrabury Formation.  Overlain by the Birkhead Formation and Algebuckina Sandstone. Disconformably overlain by the Cuddapan Formation. See also p114-p115, p136, p138 fig 8.17, p139 fig 8.18, p141, p144 fig 9.2, p146, p148-p154, p171-p172, p184, p216.||||Overlies the Patchawarra Formation and the Poolowanna Formation. Unconformably overlies the Tinchoo Formation.||
8610|Hutton Sandstone|13516|6|Mentioned|p159, 167, 169, 170, 171,172,173, 139|Middle Jurassic|Middle Jurassic|Eromanga and Surat Basins||||||
8610|Hutton Sandstone|22464|6|Mentioned|p9||Middle Jurassic|Eromanga Basin, overlain by Birkhead Formation.||||||18-SEP-18
8610|Hutton Sandstone|22757|5|Briefly described|Table6,p12|Late Jurassic|Middle Jurassic|Thickness: 290 m. Also Table5, p10. as 260 m. Ipswich-Moreton Basin.||||||17-JAN-08
8610|Hutton Sandstone|22839|6|Mentioned|P33|||||||||
8610|Hutton Sandstone|22857|5|Briefly described|p295, p296-7 Tb 22.1, p546 Tb.A1.12|Bajocian|Aalenian|Of the Bundamba Group. Sequence of stacked quartzose braided stream sands. Max. thickness: 200m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314.||||||
8610|Hutton Sandstone|22865|4|Described|p295,Table22.1p296-7|Bajocian|Aalenian|||||||
8610|Hutton Sandstone|22883|5|Briefly described|P28, Fig2|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|22924|6|Mentioned|49|||||||||
8610|Hutton Sandstone|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|23050|4|Described|p23 Table 4|Middle Jurassic|Early Jurassic|In the Surat Basin. Age: Palynology data indicates an Early to Middle Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|23051|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|In the Surat Basin.||||||17-JAN-08
8610|Hutton Sandstone|23053|6|Mentioned|Fig10p17|Toarcian|Toarcian|||||||
8610|Hutton Sandstone|23054|6|Mentioned|Fig5p22|||||||||
8610|Hutton Sandstone|23056|4|Described|12|||Geol province Eromanga Basin||||||
8610|Hutton Sandstone|23154|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province - Eromanga Basin.||||||
8610|Hutton Sandstone|23155|4|Described|p26 & Fig 14 on p27|Middle Jurassic|Early Jurassic|On southern STRZELECKI the Hutton Sandstone passes into Algebuckina Sandstone.||||||
8610|Hutton Sandstone|23375|4|Described|Fig2 p265|Callovian|Aalenian|In the Eromanga Basin.||||||17-JAN-08
8610|Hutton Sandstone|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
8610|Hutton Sandstone|23430|4|Described|p523-524 Table 14.7|Middle Jurassic|Early Jurassic|Eromanga Basin Province.  Maximum thickness <120 m.||||||
8610|Hutton Sandstone|23790|5|Briefly described|p10 Fig. 2|Jurassic|Jurassic|Geological Province: Surat Basin||||||
8610|Hutton Sandstone|23799|5|Briefly described|p52|Middle Jurassic|Middle Jurassic|Correlative of Heifer Creek Sandstone (Clarence-Moreton Basin).  Geological Province:Surat Basin.||||||
8610|Hutton Sandstone|23818|5|Briefly described|p140, p144 Fig.66|Jurassic|Jurassic|Geological Province: Great Artesian Basin. Dated upon palynological evidence.||||||
8610|Hutton Sandstone|23830|5|Briefly described|Fig. 3a|Jurassic|Jurassic|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||12-SEP-05
8610|Hutton Sandstone|23883|5|Briefly described|p129 Fig. 11.2|Jurassic|Early Jurassic|Geological Province: Great Australian Superbasin.||||||
8610|Hutton Sandstone|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
8610|Hutton Sandstone|24068|4|Described|p269|Middle Jurassic|Middle Jurassic|Geological Province: Surat Basin.  Maximum thickness: 245m.||||||
8610|Hutton Sandstone|24092|5|Briefly described|p7|||Geological Province: Great Artesian Basin.||||||
8610|Hutton Sandstone|24159|5|Briefly described|p148, Fig. 2, p152|Middle Jurassic|Early Jurassic|Geological Province: Surat Basin. Overlying Unit: Walloon Coal Measures. Underlying Unit: Evergreen Formation.||||||
8610|Hutton Sandstone|24175|5|Briefly described|p17 Fig. 3|Callovian|Aalenian|Geological Province: Eromanga Basin.||||||
8610|Hutton Sandstone|24204|5|Briefly described|p266|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
8610|Hutton Sandstone|24210|5|Briefly described|p133 Fig. 2||Middle Jurassic|Unconformable over Poolowanna Formation.  Geological Province: Eromanga Basin.  See also p132.||||||
8610|Hutton Sandstone|24241|5|Briefly described|p19 Fig.4|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|24243|5|Briefly described|p3 Fig.2|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|24282|6|Mentioned|p11|||Cooper-Eromanga Basin.||||||
8610|Hutton Sandstone|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
8610|Hutton Sandstone|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
8610|Hutton Sandstone|24488|5|Briefly described|Map Legend|Jurassic|Jurassic|Fine to medium-grained sublabile to quartzose sandstone, siltstone, mudstone, minor conglomerate and coal.||||||
8610|Hutton Sandstone|24615|5|Briefly described|CD|Jurassic|Jurassic|[Jh].  Fine- to medium-grained, sublabile to quartzose sandstone, siltstone, mudstone, minor conglomerate and coal.||||||
8610|Hutton Sandstone|29385|6|Mentioned|p80|||Also p82. Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|29387|6|Mentioned|p30|||Also Table 5. Jurassic.||||||
8610|Hutton Sandstone|29393|6|Mentioned|Table 4|||Jurassic.||||||
8610|Hutton Sandstone|29410|6|Mentioned|p274|||Geological map. Jurassic.||||||
8610|Hutton Sandstone|29591|5|Briefly described|p79|||||||||
8610|Hutton Sandstone|29721|6|Mentioned|Table 246|||||||||
8610|Hutton Sandstone|29869|6|Mentioned|p34|||See also Fig.1||||||
8610|Hutton Sandstone|29870|6|Mentioned|p15|||||||||
8610|Hutton Sandstone|29961|4|Described|p14|||||||||
8610|Hutton Sandstone|30024|6|Mentioned|p332|||||||||
8610|Hutton Sandstone|30102|4|Described|p17|||See also p18-21. Lower Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|30103|6|Mentioned|p8|||||||||
8610|Hutton Sandstone|30133|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|30451|4|Described|p74|||See also p75. Late Lower and Early Middle Jurassic.||||||17-JAN-08
8610|Hutton Sandstone|30455|6|Mentioned|p13|||Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30456|6|Mentioned|p95|||||||||
8610|Hutton Sandstone|30457|6|Mentioned|p96|||||||||
8610|Hutton Sandstone|30458|6|Mentioned|p3|||Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30460|6|Mentioned|p6|||See also p15,21, Table 4. Lower Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30461|6|Mentioned|p100|||||||||
8610|Hutton Sandstone|30464|6|Mentioned|p4|||miospores.||||||18-SEP-18
8610|Hutton Sandstone|30465|6|Mentioned|p4|||||||||
8610|Hutton Sandstone|30466|6|Mentioned|p5|||Jurassic age.||||||18-SEP-18
8610|Hutton Sandstone|30472|6|Mentioned|p132|||Pollen distribution.||||||18-SEP-18
8610|Hutton Sandstone|30474|6|Mentioned|p132|||Pollen distribution.||||||18-SEP-18
8610|Hutton Sandstone|30508|6|Mentioned|p81|||See also p90.||||||18-SEP-18
8610|Hutton Sandstone|30540|6|Mentioned|Fig.6|||||||||
8610|Hutton Sandstone|30691|4|Described|p6|||See also p15,21,Table 4. Lower Jurassic age||||||17-JAN-08
8610|Hutton Sandstone|30692|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30695|4|Described|Table 3|||Lower Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|30696|4|Described|Table 4|||Lower Jurassic age.||||||17-JAN-08
8610|Hutton Sandstone|30698|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30699|6|Mentioned|p53|||Early Jurassic. Stratigraphy||||||
8610|Hutton Sandstone|30700|6|Mentioned|p22|||Lower Jurassic. Map||||||
8610|Hutton Sandstone|30701|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30702|6|Mentioned|p48|||See also Fig.1. Stratagraphic table||||||
8610|Hutton Sandstone|30804|6|Mentioned|p10|||On Table 1.||||||18-SEP-18
8610|Hutton Sandstone|30853|5|Briefly described|Table 3|||Lower to Middle Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|30854|4|Described|Table 4|||Lower Jurassic age||||||
8610|Hutton Sandstone|30855|6|Mentioned|Map legend|Middle Jurassic|Early Jurassic|Lower - Middle Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|30856|4|Described|Table 3|||Lower Jurassic||||||
8610|Hutton Sandstone|30857|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|30915|6|Mentioned|p98|||||||||
8610|Hutton Sandstone|30921|6|Mentioned|Map legend|Late Jurassic|Early Jurassic|Early - Late Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|31098|6|Mentioned|p5|||L.Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|31116|4|Described|p24|||See also p10. Jurassic||||||17-JAN-08
8610|Hutton Sandstone|31117|5|Briefly described|p379|||Lithology. Jurassic||||||
8610|Hutton Sandstone|31118|6|Mentioned|p311|||||||||
8610|Hutton Sandstone|31120|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|31121|6|Mentioned|p390|||||||||
8610|Hutton Sandstone|31122|6|Mentioned|p344|||||||||
8610|Hutton Sandstone|31145|5|Briefly described|Table 1|||L. - Mid. Jurassic||||||
8610|Hutton Sandstone|31304|6|Mentioned|Fig. 1|||||||||
8610|Hutton Sandstone|31369|4|Described|p26|||Triassic. See also p27.||||||17-JAN-08
8610|Hutton Sandstone|31431|5|Briefly described|Table 2|||L.-M.Jurassic||||||
8610|Hutton Sandstone|31432|4|Described|Table 1|||L.Jurassic||||||
8610|Hutton Sandstone|31436|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|31438|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|31553|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|32040|6|Mentioned|p885|||Stratigraphic sequence.||||||18-SEP-18
8610|Hutton Sandstone|32136|6|Mentioned|p3|||Aalenian (Late Liassic) miospores.||||||18-SEP-18
8610|Hutton Sandstone|32138|6|Mentioned|p396|||||||||
8610|Hutton Sandstone|32182|4|Described|p4|||Jurassic. See also p5.||||||17-JAN-08
8610|Hutton Sandstone|32193|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
8610|Hutton Sandstone|32490|6|Mentioned|Table 1|||Equivalent Ronlow Beds?||||||
8610|Hutton Sandstone|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|32696|6|Mentioned|Fig.4|||See also Figs 6 & 7.||||||18-SEP-18
8610|Hutton Sandstone|32797|4|Described|Table 4|||L. Jur.||||||
8610|Hutton Sandstone|33059|4|Described|Table 1|||See also Fig.4. L-M.Jur.||||||
8610|Hutton Sandstone|33067|4|Described|Table 1|Early Jurassic|Early Jurassic|Quartz sandstone, minor siltstone, shale.||||||07-JUL-04
8610|Hutton Sandstone|33069|4|Described|p7|||L.Jur.||||||
8610|Hutton Sandstone|33070|4|Described|Table 2|||Lower Jurassic.||||||17-JAN-08
8610|Hutton Sandstone|33071|4|Described|p6|||L.Jur.||||||
8610|Hutton Sandstone|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33080|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
8610|Hutton Sandstone|33082|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33086|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33087|6|Mentioned|Map legend||Early Jurassic|||||||
8610|Hutton Sandstone|33088|4|Described|Table 3|||Injune Ck.Gp.||||||
8610|Hutton Sandstone|33089|5|Briefly described|Table 2|||L.Jur.||||||
8610|Hutton Sandstone|33090|4|Described|Table 4|||L.Jur.||||||
8610|Hutton Sandstone|33091|5|Briefly described|p10|||Stratigraphy||||||
8610|Hutton Sandstone|33092|5|Briefly described|p6|||Strat. Table||||||
8610|Hutton Sandstone|33094|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33096|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33367|5|Briefly described|Table 1|||See also p3.||||||18-SEP-18
8610|Hutton Sandstone|33371|6|Mentioned|Fig.2|||||||||
8610|Hutton Sandstone|33381|6|Mentioned|Table 1|||L.-M. Jur.||||||
8610|Hutton Sandstone|33451|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33530|5|Briefly described|Table 1|||Lower - Middle Jurassic||||||
8610|Hutton Sandstone|33638|5|Briefly described|Table 1|||||||||
8610|Hutton Sandstone|33639|5|Briefly described|Table 2|||L. Jur.||||||
8610|Hutton Sandstone|33640|4|Described|Table 3|||L.Jur.||||||
8610|Hutton Sandstone|33643|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33644|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33646|6|Mentioned|p12|||||||||
8610|Hutton Sandstone|33647|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33648|6|Mentioned|p19|||Stratigraphy.||||||
8610|Hutton Sandstone|33672|5|Briefly described|p44|||Lithology.||||||
8610|Hutton Sandstone|33673|6|Mentioned|p291|||Good reservoir potential.||||||
8610|Hutton Sandstone|33674|6|Mentioned|Fig.1|||||||||
8610|Hutton Sandstone|33762|6|Mentioned|p369|||Late Jurassic||||||
8610|Hutton Sandstone|33774|6|Mentioned|p40|||L.Jurassic. Faulting||||||
8610|Hutton Sandstone|33820|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|33821|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
8610|Hutton Sandstone|33822|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|33824|6|Mentioned|p7|||See also Table 2.||||||18-SEP-18
8610|Hutton Sandstone|33825|6|Mentioned|p9|||Lithology.||||||18-SEP-18
8610|Hutton Sandstone|33827|6|Mentioned|p7|||See also Table 2.||||||18-SEP-18
8610|Hutton Sandstone|33828|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|33832|5|Briefly described|p11|||Strat. and correlation.||||||17-JAN-08
8610|Hutton Sandstone|33936|6|Mentioned|Fig.3A|||Jurassic.||||||
8610|Hutton Sandstone|33971|6|Mentioned|Fig.29|||Strat. table.||||||
8610|Hutton Sandstone|33977|6|Mentioned|p9|||Lithology Equiv.||||||
8610|Hutton Sandstone|33998|6|Mentioned|p31|||||||||
8610|Hutton Sandstone|34065|4|Described|p7|||L.-M. Jur.||||||
8610|Hutton Sandstone|34091|5|Briefly described|Table 1|||L.Jur   See also P4||||||
8610|Hutton Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic.||||||
8610|Hutton Sandstone|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|34212|6|Mentioned|p2|||Jurassic||||||
8610|Hutton Sandstone|34218|4|Described|Table 1|||Lower - Middle Jurassic. See also Table 2.||||||
8610|Hutton Sandstone|34254|6|Mentioned|p481|||||||||
8610|Hutton Sandstone|34282|6|Mentioned|p95|||||||||
8610|Hutton Sandstone|34287|6|Mentioned|p70|||Jurassic||||||
8610|Hutton Sandstone|34386|6|Mentioned|p98,100-103,106-107|||Assemblages in. See also Figs.3,4,5,6,7.||||||
8610|Hutton Sandstone|34412|6|Mentioned|p108|||See also p109. Jurassic.||||||18-SEP-18
8610|Hutton Sandstone|34452|6|Mentioned|p1|||L.Jurassic. See also pp2,3,4,5 etc||||||18-SEP-18
8610|Hutton Sandstone|34486|4|Described|Table 1|||Lower Jurassic. See also Table 2, p10||||||17-JAN-08
8610|Hutton Sandstone|34487|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|34507|6|Mentioned|p87|||||||||
8610|Hutton Sandstone|34611|6|Mentioned|p140|||Jurassic. See also Fig.65, Fig.66.||||||18-SEP-18
8610|Hutton Sandstone|34613|4|Described|Table 4|||||||||
8610|Hutton Sandstone|34743|6|Mentioned|p27|||||||||
8610|Hutton Sandstone|34905|6|Mentioned|p531|||||||||
8610|Hutton Sandstone|35030|6|Mentioned|p335|||||||||
8610|Hutton Sandstone|35067|6|Mentioned|Fig.4|||||||||
8610|Hutton Sandstone|35148|6|Mentioned|Fig.1|||||||||
8610|Hutton Sandstone|35157|6|Mentioned|p524|||||||||
8610|Hutton Sandstone|35239|6|Mentioned|p258|||||||||
8610|Hutton Sandstone|35457|6|Mentioned|p633|||||||||
8610|Hutton Sandstone|35560|4|Described|p288|||||||||
8610|Hutton Sandstone|35562|6|Mentioned|p295|||Stratigraphy.||||||18-SEP-18
8610|Hutton Sandstone|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
8610|Hutton Sandstone|35663|6|Mentioned|Fig.1|||Revised outcrop geology.||||||
8610|Hutton Sandstone|35811|5|Briefly described|Table 3|||See also Table 5.||||||
8610|Hutton Sandstone|35901|6|Mentioned|p17|||||||||
8610|Hutton Sandstone|35937|6|Mentioned|Fig.5|||||||||
8610|Hutton Sandstone|36233|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|36243|6|Mentioned|p74|||See also Table 6A.||||||
8610|Hutton Sandstone|36331|6|Mentioned|Fig.5|||||||||
8610|Hutton Sandstone|36333|6|Mentioned|Map legend|Middle Jurassic|Early Jurassic|||||||15-JUL-04
8610|Hutton Sandstone|36570|2|Defined|p26|Jurassic|Jurassic|See also p20, Fig.9, p55, Table 1, p34.||||||17-JAN-08
8610|Hutton Sandstone|36574|6|Mentioned|p599|||||||||
8610|Hutton Sandstone|36708|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|36825|6|Mentioned|p21|||||||||
8610|Hutton Sandstone|36910|6|Mentioned|p60|||||||||
8610|Hutton Sandstone|36914|6|Mentioned|p87|||||||||
8610|Hutton Sandstone|37116|6|Mentioned|p310|||||||||
8610|Hutton Sandstone|37117|5|Briefly described|p313|||||||||
8610|Hutton Sandstone|37119|5|Briefly described|p318|||||||||
8610|Hutton Sandstone|37252|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|37287|6|Mentioned|p33|||||||||
8610|Hutton Sandstone|37288|6|Mentioned|p41|||||||||
8610|Hutton Sandstone|37451|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|37463|6|Mentioned|p479|||||||||
8610|Hutton Sandstone|37608|3|Fully described|Table 1|||||||||
8610|Hutton Sandstone|37703|6|Mentioned|p2240|||||||||
8610|Hutton Sandstone|37856|6|Mentioned|Table 3|||||||||
8610|Hutton Sandstone|37993|6|Mentioned|Fig.2|||||||||
8610|Hutton Sandstone|37994|6|Mentioned|p144|||||||||
8610|Hutton Sandstone|37995|4|Described|p64|||||||||
8610|Hutton Sandstone|38064|6|Mentioned|42|||||||||
8610|Hutton Sandstone|38068|6|Mentioned|p71|||||||||
8610|Hutton Sandstone|38205|6|Mentioned|p96|||||||||
8610|Hutton Sandstone|38358|6|Mentioned|Fig.1|||||||||
8610|Hutton Sandstone|38447|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|38730|6|Mentioned|p29|||||||||
8610|Hutton Sandstone|38779|6|Mentioned|p7|||||||||
8610|Hutton Sandstone|39070|4|Described|p363|||||||||
8610|Hutton Sandstone|39212|4|Described|p37|||Excursion site. p24 petroleum reservoir. p25 aquifer. See also p16.||||||17-JAN-08
8610|Hutton Sandstone|39276|6|Mentioned|Fig. 2|||||||||
8610|Hutton Sandstone|39315|6|Mentioned|Fig.5|||||||||
8610|Hutton Sandstone|39445|5|Briefly described|Table 10|||||||||
8610|Hutton Sandstone|39478|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|39482|6|Mentioned|Fig.7|||||||||
8610|Hutton Sandstone|39494|6|Mentioned|p129|||See also Fig.3.||||||18-SEP-18
8610|Hutton Sandstone|39632|6|Mentioned|p209|||||||||
8610|Hutton Sandstone|39815|6|Mentioned|p444|||||||||
8610|Hutton Sandstone|39846|6|Mentioned|p44|||||||||
8610|Hutton Sandstone|39847|5|Briefly described|p35|||||||||
8610|Hutton Sandstone|39907|6|Mentioned|Fig.3|||||||||
8610|Hutton Sandstone|39943|6|Mentioned|Table 8A|||||||||
8610|Hutton Sandstone|39988|6|Mentioned|p288|||||||||
8610|Hutton Sandstone|39989|4|Described|p421|||||||||
8610|Hutton Sandstone|40003|5|Briefly described|p33|||||||||
8610|Hutton Sandstone|40030|6|Mentioned|p132|||||||||
8610|Hutton Sandstone|40121|6|Mentioned|p446|||||||||
8610|Hutton Sandstone|40245|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|40249|6|Mentioned|p38|||Mention p41.||||||18-SEP-18
8610|Hutton Sandstone|40250|4|Described|p30|||||||||
8610|Hutton Sandstone|40540|6|Mentioned|p151|||||||||
8610|Hutton Sandstone|40541|3|Fully described|p109|||||||||
8610|Hutton Sandstone|40544|6|Mentioned|p156|||||||||
8610|Hutton Sandstone|40623|5|Briefly described|p72|||See also p109.||||||18-SEP-18
8610|Hutton Sandstone|40642|6|Mentioned|p172|||||||||
8610|Hutton Sandstone|40666|4|Described|p356|||||||||
8610|Hutton Sandstone|40675|6|Mentioned|p306|||Mention Table 8A.||||||18-SEP-18
8610|Hutton Sandstone|40687|3|Fully described|p413|||||||||
8610|Hutton Sandstone|40767|6|Mentioned|p14|||||||||
8610|Hutton Sandstone|40832|3|Fully described|p455|||||||||
8610|Hutton Sandstone|40833|6|Mentioned|p468|||||||||
8610|Hutton Sandstone|40910|6|Mentioned|Table 3|||||||||
8610|Hutton Sandstone|40926|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|40953|4|Described|p19|||||||||
8610|Hutton Sandstone|40962|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|41060|5|Briefly described|p2|||Generalized stratigraphy||||||
8610|Hutton Sandstone|41061|6|Mentioned|p19|||||||||
8610|Hutton Sandstone|41062|6|Mentioned|p28,p34|||See also Fig.5.||||||18-SEP-18
8610|Hutton Sandstone|41063|6|Mentioned|p46|||||||||
8610|Hutton Sandstone|41064|6|Mentioned|p60|||||||||
8610|Hutton Sandstone|41084|5|Briefly described|Fig.2|||||||||
8610|Hutton Sandstone|41097|6|Mentioned|p166|||||||||
8610|Hutton Sandstone|41099|6|Mentioned|p185|||||||||
8610|Hutton Sandstone|41123|6|Mentioned|p177|||||||||
8610|Hutton Sandstone|41164|6|Mentioned|p422|||||||||
8610|Hutton Sandstone|41165|6|Mentioned|p373|||See also Fig.18, Fig.20.||||||18-SEP-18
8610|Hutton Sandstone|41175|6|Mentioned|p195|||||||||
8610|Hutton Sandstone|41176|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|41177|6|Mentioned|p222|||||||||
8610|Hutton Sandstone|41182|5|Briefly described|Fig.2|||||||||
8610|Hutton Sandstone|41183|6|Mentioned|p307|||||||||
8610|Hutton Sandstone|41186|4|Described|p204|||||||||
8610|Hutton Sandstone|41187|5|Briefly described|p216|||||||||
8610|Hutton Sandstone|41188|6|Mentioned|p235|||||||||
8610|Hutton Sandstone|41189|6|Mentioned|p249|||||||||
8610|Hutton Sandstone|41198|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|41210|5|Briefly described|p158|||||||||
8610|Hutton Sandstone|41212|6|Mentioned|p203|||||||||
8610|Hutton Sandstone|41214|6|Mentioned|p254|||||||||
8610|Hutton Sandstone|41216|6|Mentioned|Fig.18,p299|||||||||
8610|Hutton Sandstone|41219|4|Described|p345|||||||||
8610|Hutton Sandstone|41246|6|Mentioned|Map legend|Jurassic||||||||
8610|Hutton Sandstone|41247|6|Mentioned|p119|||||||||
8610|Hutton Sandstone|41266|6|Mentioned|Fig.3|||||||||
8610|Hutton Sandstone|41281|6|Mentioned|p7|||||||||
8610|Hutton Sandstone|41286|6|Mentioned|p114|||||||||
8610|Hutton Sandstone|41536|6|Mentioned|Fig.3|||||||||
8610|Hutton Sandstone|41681|6|Mentioned|p16|||||||||
8610|Hutton Sandstone|41707|5|Briefly described|p161|||||||||
8610|Hutton Sandstone|41712|6|Mentioned|p272|||See also p289.||||||18-SEP-18
8610|Hutton Sandstone|41724|5|Briefly described|p381|||||||||
8610|Hutton Sandstone|41725|6|Mentioned|p407|||||||||
8610|Hutton Sandstone|41992|4|Described|Fig.2 P183|||||||||
8610|Hutton Sandstone|42006|6|Mentioned|Fig.3 P23|||See also Fig.4 p24, 25.||||||18-SEP-18
8610|Hutton Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
8610|Hutton Sandstone|42067|4|Described|Appendix 2|||||||||
8610|Hutton Sandstone|42071|6|Mentioned|p116|||||||||
8610|Hutton Sandstone|42084|6|Mentioned|Fig.3 P356|||||||||
8610|Hutton Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
8610|Hutton Sandstone|42248|6|Mentioned|p410|||||||||
8610|Hutton Sandstone|42263|6|Mentioned|p14|Jurassic|Jurassic|||||||13-AUG-08
8610|Hutton Sandstone|42357|6|Mentioned|p11|||||||||
8610|Hutton Sandstone|42395|6|Mentioned|p80|||||||||
8610|Hutton Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
8610|Hutton Sandstone|42446|4|Described|p11|||||||||
8610|Hutton Sandstone|42447|5|Briefly described|p5 + Fig. 1|||||||||
8610|Hutton Sandstone|42463|6|Mentioned|Fig.5 P172|||||||||
8610|Hutton Sandstone|42474|5|Briefly described|p25|||||||||
8610|Hutton Sandstone|42493|5|Briefly described|Fig. 1 P18|||||||||
8610|Hutton Sandstone|42496|4|Described|p140|||||||||
8610|Hutton Sandstone|42520|5|Briefly described|p6|||||||||
8610|Hutton Sandstone|42634|6|Mentioned|Table 8 P34|||||||||
8610|Hutton Sandstone|42746|4|Described|p10|||See also Fig.6||||||
8610|Hutton Sandstone|42749|4|Described|p29, Fig.3 p28|||see also Fig.2 p27.||||||17-JAN-08
8610|Hutton Sandstone|42911|5|Briefly described|p13|||||||||
8610|Hutton Sandstone|42999|5|Briefly described|Table 2,p90||Jurassic|||||||
8610|Hutton Sandstone|43000|5|Briefly described|Fig.5,p112|||||||||
8610|Hutton Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
8610|Hutton Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
8610|Hutton Sandstone|43105|5|Briefly described|p15|||||||||
8610|Hutton Sandstone|43114|5|Briefly described|p10|||||||||
8610|Hutton Sandstone|43122|5|Briefly described|p7|||see also Fig. 2.||||||
8610|Hutton Sandstone|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Surat Basin.||||||12-APR-05
8610|Hutton Sandstone|43185|6|Mentioned|6||Jurassic|||||||
8610|Hutton Sandstone|43436|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
8610|Hutton Sandstone|43539|14|Not recorded|p396|||||||||
8610|Hutton Sandstone|43582|6|Mentioned|Fig.5,p16,28||Middle Jurassic|||||||
8610|Hutton Sandstone|43591|6|Mentioned|p40|||||||||
8610|Hutton Sandstone|43602|6|Mentioned|191|||||||||
8610|Hutton Sandstone|43628|6|Mentioned|Fig.3|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|43630|6|Mentioned|Fig.4,p7||Jurassic|||||||
8610|Hutton Sandstone|43711|6|Mentioned|p18|||||||||
8610|Hutton Sandstone|43851|14|Not recorded|Tb p106,111||Middle Jurassic|||||||
8610|Hutton Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
8610|Hutton Sandstone|43910|14|Not recorded|p19,20|||Correlated with Marburg Sandstone||||||
8610|Hutton Sandstone|43912|14|Not recorded|p2,4|||(Moonie No.1)||||||
8610|Hutton Sandstone|43923|6|Mentioned|p14||Jurassic|||||||
8610|Hutton Sandstone|43924|14|Not recorded|p1,2,15|||Liassic-Bajocian boundary in age.||||||
8610|Hutton Sandstone|43925|14|Not recorded|p31,40-2,49-50,|||Figs.3,4||||||
8610|Hutton Sandstone|43982|14|Not recorded|Map Legend|||||||||
8610|Hutton Sandstone|43989|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|43993|14|Not recorded|p101||Triassic|Ref. to Reeves.||||||
8610|Hutton Sandstone|43994|14|Not recorded|Map Legend|||||||||
8610|Hutton Sandstone|43996|14|Not recorded|p89|||||||||
8610|Hutton Sandstone|43998|4|Described|p14,17,map||Early Jurassic|||||||
8610|Hutton Sandstone|44016|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44019|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44020|14|Not recorded|p15,Tb.1,2,3||Early Jurassic|||||||
8610|Hutton Sandstone|44021|14|Not recorded|p232-234|||||||||
8610|Hutton Sandstone|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44023|4|Described|Tb.3,p11||Early Jurassic|||||||
8610|Hutton Sandstone|44026|14|Not recorded|p123,123|||||||||
8610|Hutton Sandstone|44028|14|Not recorded|Fig.2,p509,512-514||Jurassic|See Strat Table.||||||
8610|Hutton Sandstone|44031|14|Not recorded|p6,8,9-11||Late Jurassic|Artesian water.||||||
8610|Hutton Sandstone|44032|14|Not recorded|p46,map,p463,464|||= to Marburg Formation. Of Moreton Basin.||||||
8610|Hutton Sandstone|44042|14|Not recorded|Map Legend||Early Jurassic|||||||
8610|Hutton Sandstone|44084|14|Not recorded|p20,22,32|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44116|14|Not recorded|p28|||||||||
8610|Hutton Sandstone|44124|14|Not recorded|p2,5,10,17-19|||||||||
8610|Hutton Sandstone|44129|14|Not recorded|p95-96||Jurassic|||||||
8610|Hutton Sandstone|44133|5|Briefly described|p109, 105 Fig. 9.12|Late Jurassic|Middle Jurassic|Intertounges with Poolowanna Formation. Intertounges and is overlain by the Birkhead Formation.||||||
8610|Hutton Sandstone|44163|4|Described|p10-14||Jurassic|||||||
8610|Hutton Sandstone|44170|14|Not recorded|p20||Early Jurassic|||||||
8610|Hutton Sandstone|44171|14|Not recorded|p194,195,197,198|||||||||
8610|Hutton Sandstone|44174|14|Not recorded|p345,347||Early Jurassic|||||||
8610|Hutton Sandstone|44207|14|Not recorded|p116|||||||||
8610|Hutton Sandstone|44208|14|Not recorded|p94||Jurassic|||||||
8610|Hutton Sandstone|44304|14|Not recorded|p1|||||||||
8610|Hutton Sandstone|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
8610|Hutton Sandstone|44379|14|Not recorded|p21|||||||||
8610|Hutton Sandstone|44381|14|Not recorded|p7-8|||||||||
8610|Hutton Sandstone|44390|14|Not recorded|p6,9,10,13,15,Tb.1|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44391|14|Not recorded|Map Legend|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44414|14|Not recorded|p113-115||Jurassic|||||||
8610|Hutton Sandstone|44415|14|Not recorded|Figs.1,2,p23,24||Early Jurassic|||||||
8610|Hutton Sandstone|44419|14|Not recorded|p278||Jurassic|||||||
8610|Hutton Sandstone|44420|14|Not recorded|p1,3-5,9,10,22,27,29||Early Jurassic|Fig.14.||||||
8610|Hutton Sandstone|44421|14|Not recorded|p1,6,10,11,13,14,19,||Jurassic|p20-21||||||
8610|Hutton Sandstone|44422|14|Not recorded|p149,153|Middle Jurassic|Early Jurassic|||||||
8610|Hutton Sandstone|44426|14|Not recorded|p12|||Pelecypods, indeterminate plant fragments; 'may extend into the Middle Jurassic'.||||||
8610|Hutton Sandstone|44525|14|Not recorded|p520|||||||||
8610|Hutton Sandstone|44566|14|Not recorded|p15,16,Pl.2|||||||||
8610|Hutton Sandstone|44567|14|Not recorded|p11,13,14,Pls.1,2|||||||||
8610|Hutton Sandstone|44568|14|Not recorded|p3,4,Pl.1|||||||||
8610|Hutton Sandstone|44573|14|Not recorded|p97||Jurassic|||||||
8610|Hutton Sandstone|44585|14|Not recorded|p45-Fig.2|||||||||
8610|Hutton Sandstone|44610|14|Not recorded|p49,Tb.1|||||||||
8610|Hutton Sandstone|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
8610|Hutton Sandstone|44627|14|Not recorded|p139,141-144||Jurassic|||||||
8610|Hutton Sandstone|44636|14|Not recorded|p165,166|Bajocian|Lias|(Late Liassic-Bajocian)||||||
8610|Hutton Sandstone|44637|14|Not recorded|Table||Jurassic|||||||
8610|Hutton Sandstone|44640|14|Not recorded|p30|||||||||
8610|Hutton Sandstone|44727|14|Not recorded|p304|||Marburg equivalent North of Roma.||||||
8610|Hutton Sandstone|44787|14|Not recorded|p122,Tb.p123,125,126||Early Jurassic|||||||
8610|Hutton Sandstone|44819|14|Not recorded|p89||Jurassic|Marine, sparse microfauna indicating brackish marine conditions.||||||29-JUN-16
8610|Hutton Sandstone|44852|14|Not recorded|p78||Jurassic|||||||
8610|Hutton Sandstone|45071|6|Mentioned|p136|||||||||
8610|Hutton Sandstone|45073|6|Mentioned|p58|||Geol. history||||||
8610|Hutton Sandstone|45110|2|Defined|p92|Early Jurassic|Early Jurassic|See also p9,24 and Fig.5.||||||17-JAN-08
8610|Hutton Sandstone|45145|6|Mentioned|p21|||||||||
8610|Hutton Sandstone|45168|6|Mentioned|p6|||||||||
8610|Hutton Sandstone|46791|6|Mentioned|Fig.6|||||||||
8610|Hutton Sandstone|46881|6|Mentioned|Table 2|||||||||
8610|Hutton Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
8610|Hutton Sandstone|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
8610|Hutton Sandstone|46984|6|Mentioned|Table 1|||||||||
8610|Hutton Sandstone|46989|5|Briefly described|Table 1|||||||||
8610|Hutton Sandstone|48606|14|Not recorded|p5,6,11,13,14,19,21|||(H/55-8 ; G/55-12). Pl.1, Sh.1: Pl.2.||||||
8610|Hutton Sandstone|48634|14|Not recorded|p6,21||Jurassic|See also Figs. 2,6, Pl.1,2 p5,19. Lower-Middle Jurassic. (G54-14).||||||
8610|Hutton Sandstone|48900|4|Described|p52|||Lower - Middle Jurassic.||||||
8610|Hutton Sandstone|48919|2|Defined|p53|Middle Jurassic|Early Jurassic|See also p54-55. Lower to Middle Jurassic.||||||17-JAN-08
8610|Hutton Sandstone|48920|3|Fully described|p44|||Jurassic age.||||||19-AUG-08
8610|Hutton Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin.||||||18-SEP-18
8610|Hutton Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin.||||||18-SEP-18
8610|Hutton Sandstone|50190|5|Briefly described|p85|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
8610|Hutton Sandstone|50214|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Sandstone, carbonaceous siltstone, mudstone and rare conglomerate.||||||
8610|Hutton Sandstone|60114|6|Mentioned|p16|||Oil-bearing deposits.  Geological Province:  Cooper - Eromanga Basins.||||||21-JUL-04
8610|Hutton Sandstone|60281|5|Briefly described|p27|||Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|60282|5|Briefly described|p11|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
8610|Hutton Sandstone|60386|6|Mentioned|p299|Middle Jurassic|Early Jurassic|Cooper/Eromanga Basin. Non-marine.||||||
8610|Hutton Sandstone|60717|5|Briefly described|p40 Fig. 2, p42|Middle Jurassic|Early Jurassic|Overlies Poolowanna Formation; underlies and partially interfingers with Birkhead Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
8610|Hutton Sandstone|60993|6|Mentioned|p17, p6 Fig. 2|||Correlates with Marburg Subgroup units. Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|60998|5|Briefly described|p144|||Overlies Evergreen Formation. ||||||
8610|Hutton Sandstone|60999|5|Briefly described|p177, p178 Fig. 10|||Partly equivalent to Walloon Coal Measures.  Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|61000|5|Briefly described|p183|Bajocian|Aalenian|Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Koukandowie Formation. See also p255 Figs. 23, 24 and 25. ||||||
8610|Hutton Sandstone|61015|6|Mentioned|p44|||||||||
8610|Hutton Sandstone|61087|5|Briefly described|Map Legend|Jurassic|Jurassic|Fine to medium-grained, sublabile to quartzose sandstone, siltstone, mudstone, minor conglomerate and coal.||||||
8610|Hutton Sandstone|61310|6|Mentioned|p22|||Together with the Evergreen Formation, correlated with Marburg Formation and "Upper Bundamba Unit".||||||
8610|Hutton Sandstone|61312|6|Mentioned|p71, p78|Middle Jurassic|Early Jurassic|Sandstone, minor shale. Productive reservoir unit. See also p72 Fig. E9.||||||
8610|Hutton Sandstone|61377|5|Briefly described|p151, p153, p142, p148|Middle Jurassic|Early Jurassic|Thick sequence of stacked quartzose braided stream sands. Ssts are good quality reservoirs sealed by Walloon C.M.above (conformable). Conformable on Evergreen Fm. Geol.Prov: Surat Basin||||||07-FEB-11
8610|Hutton Sandstone|61611|6|Mentioned|p265 Fig. 3|Middle Jurassic|Early Jurassic|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
8610|Hutton Sandstone|61613|6|Mentioned|p282-284, p287, p288, p282 Fig. 2|Middle Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
8610|Hutton Sandstone|61614|6|Mentioned|p289, p293, p297, p290 Fig. 2|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
8610|Hutton Sandstone|61615|5|Briefly described|p302, p302 Fig. 2, p306, p307|Late Jurassic|Jurassic|Geological Province: Eromanga Basin. Comprises thick succession of stacked fluvial channel sandstones.||||||07-FEB-11
8610|Hutton Sandstone|61832|5|Briefly described|p187|Jurassic|Jurassic|On the MUNDUBERRA sheet.  Overlain by Injune Creek Group; overlies Evergreen Formation. Geological Province: Surat Basin.||||||03-JUL-06
8610|Hutton Sandstone|62028|5|Briefly described|p10 Fig. 1|||||||||
8610|Hutton Sandstone|62537|6|Mentioned|p191 Fig.2. |Middle Jurassic|Early Jurassic|Eromanga Basin.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|62730|5|Briefly described|p352 Fig. 1|Middle Jurassic|Middle Jurassic|Geological Province: Eromanga Basin.||||||21-APR-08
8610|Hutton Sandstone|63218|6|Mentioned|p211 Fig.2. |Middle Jurassic|Early Jurassic|Surat Basin.||||Overlies Evergreen Formation. Is overlain by Eurombah Formation.||
8610|Hutton Sandstone|63347|5|Briefly described|p5 Fig. 2|Early Cretaceous|Middle Jurassic|Geological Province: Surat Basin.||||||
8610|Hutton Sandstone|63748|6|Mentioned|p23|||Correlative of Marburg Subgroup.  Geological province: Surat Basin.||||||07-FEB-11
8610|Hutton Sandstone|63979|2|Defined|p34, Fig. 44|Callovian|Toarcian|Informally subdivided into "lower and upper Hutton Sandstone".Conformable on Poolowanna Fm; conformably overlain by Birkhead Fm. Max thickness: 244m.Dominantly sandstone, +rare interbedded siltstone+mudstone (more so in lower section). In Eromanga Basin.||||||07-FEB-11
8610|Hutton Sandstone|64048|6|Mentioned|p64 Tb. 2, p70|||Geological Province: Eromanga Basin.||||||07-FEB-11
8610|Hutton Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Middle Jurassic|Early Jurassic|Eromanga, Surat/Bowen Basins.||||Eromanga/Cooper Basins: underlies Birkhead Formation; overlies Poolowanna Formation. Surat/Bowen Basins: overlies Evergreen Formation; underlies Eurombah Formation.||10-DEC-15
8610|Hutton Sandstone|64399|5|Briefly described|Map legend|Jurassic|Jurassic|Over Evergreen Fm;under Mulgildie C.M. Poorly sorted, medium-grained, feldspathic sublabile sandstone (at base) and fine-grained , well-sorted quartzose sandstone (at top); minor dark grey carbomaceous siltstone, mudstone and rare pebbl;e conglomerate.||||||19-AUG-08
8610|Hutton Sandstone|64665|5|Briefly described|p53 Fig.2, p60, p61.|Middle Jurassic|Early Jurassic|Eromanga and Surat Basins. Correlates with Heifer Creek Sandstone Member (Clarence-Moreton Basin). Equivalent to Algebuckina Sandstone (Eromanga Basin). With the Eurombah Formation and Walloon Subgroup, forms the second of six cyclothems in the Surat Basin.||||Overlies Poolowanna and Evergreen Formations. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|64856|3|Fully described|p79, p82, p83 Fig.29, p85-88|Bathonian|Aalenian|Reeves (1947) regarded this as the top member of the Bundamba Series. Redesignated as a Formation by Mollan et al. (1965) with a type section near Hutton Creek, 19km ENE of Injune. Surat Basin. Mainly sandstone with interbedded siltstone and shale, minor mudstone and coal, continuous with the top part of the Marburg Subgroup in the Moreton Basin. Up to 266m thick. Age from palynoflora (units APJ33, 41, 42). Overlies Evergreen Formation. Underlies Walloon Coal Measures or Eurombah Formation.| | ||||29-NOV-17
8610|Hutton Sandstone|64857|5|Briefly described|p132-133, p113 Fig.3|||Conformably overlies Evergreen Formation. Consists mainly of sandstone and interbedded siltstone, shale with minor mudstone and coal. Surat Basin.||||||
8610|Hutton Sandstone|64858|6|Mentioned|p181 Tb.1, 187|||Surat Basin.||||||30-NOV-09
8610|Hutton Sandstone|65003|5|Briefly described|p8||Jurassic|Of Surat Basin. ||||||
8610|Hutton Sandstone|65096|5|Briefly described|p368, p370 Fig.2, p372, p373|||Of the Surat Basin. Formation top sometimes difficult to distinguish on wireline log.  Along with Evergreen Formation, compared with the  Marburg sub-group [sic] of the Clarence-Moreton Basin, east of the Toowoomba Strait.||||Gradationally overlain by the Eurombah Formation of the Walloon Subgroup||
8610|Hutton Sandstone|65112|5|Briefly described|p323; p328; Fig11 p324; Fig16 p328|Early Cretaceous|Jurassic||178-166 Ma.|||Underlies the Walloon Coal Measures, overlies the Evergreen Formation.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
8610|Hutton Sandstone|65113|5|Briefly described|Fig 4 p340|Middle Jurassic|Middle Jurassic|Overlies the Evergreen Formation and underlies the Walloon CM.||||||
8610|Hutton Sandstone|65114|5|Briefly described|p385 Fig.3, p389|Middle Jurassic||Part of the Surat Basin, base of unit commonly cut by reactivation of major extensional marginal faults ||||||
8610|Hutton Sandstone|65116|5|Briefly described|p455, Fig 2 p437|Middle Jurassic|Middle Jurassic|Medium- fine grained quartzose-sublithic sandstone. Underlies the Walloon CM; overlies the Evergreen Formation, Surat Basin.||||||06-MAR-12
8610|Hutton Sandstone|65117|5|Briefly described|p461, 469,470, Fig 4 p465, Tbl 1 p466|Middle Jurassic|Aalenian|Surat Basin, Potential reservoir unit. Up to 266m thick in study area. Overlies Evergreen Formation. Fine to medium grained quartzose lithic sandstone. Is both thick bedded and cross-bedded. Deposited by meandering streams.||||||
8610|Hutton Sandstone|65119|5|Briefly described|p513, fig 2, Table 1, Fig 6-19|Middle Jurassic|Middle Jurassic|Surat Basin. Quartzose to sublabile sandstone, some siltstone, mudstone, minor conglomerate.  Age:168-188Ma. Fission Track ages:105-166Ma.||||||07-MAR-12
8610|Hutton Sandstone|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||
8610|Hutton Sandstone|65385|5|Briefly described|pS134 Fig.7|Late Jurassic|Early Jurassic|Of Eromanga Basin. Overlies Poolowanna Formation.||||||08-MAR-12
8610|Hutton Sandstone|65388|3|Fully described|p213-214, p210 Fig 74|Middle Jurassic|Middle Jurassic|Surat, Mulgildie, Moreton and Eromanga Basins. First used by Reeves (1947) for sandstones as the top member of the "Bundamba Series" north-west of Injune. Mollan & others (1965) raised it to formation status.  It is the most widespread Jurassic unit in the Great Artesian Basin.  72-266m thick. Overlies Evergreen Formation in Mulgildie Basin. Is continuous into, and forms the upper part of the Marburg Subgroup in the Moreton Basin to the east. Is overlain by  Mulgildie Coal Measures or Eurombah Formation. Palynofloral assemblages range from units APJ33 to APJ42 (Aalenian to Bathonian) (Green & others, 1997; Price, 1997). Fine to medium-grained, cream or brown, well sorted argillaceous, micaceous quartzose sandstone interbedded with mudstone.||||||
8610|Hutton Sandstone|65489|5|Briefly described|p10-13, p15, p26, p47, p49, p61, p96|Middle Jurassic|Early Jurassic|See also p154-155, p157-160. Eromanga Basin. 230m thick. Good to excellent reservoir quality. Predominantly anticlinal traps. Gas and oil reservoir accounting for 61% and 57% respectively of the Basin's production. Appears as Hutton Formation on p96, and as Hutton sandstone on p157.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.|Braided fluvial sandstone.|
8610|Hutton Sandstone|65925|5|Briefly described|Appendix 2.||||||||White, fine- to coarse-grained sandstone; with minor dark grey lenticular carbonaceous siltstone and shale interbeds.|
8610|Hutton Sandstone|66188|6|Mentioned|441|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|66529|5|Briefly described|p10, p12 Fig.5 |||Eromanga Basin. ||||Overlies Poolowanna and Evergreen Formations; overlies Moolayember Formation unconformably. Is overlain by Injune Creek Group.|Medium grained sandstone, non-marine.|
8610|Hutton Sandstone|66915|5|Briefly described|p6 Fig.3, p12|Middle Jurassic|Early Jurassic|Eromanga and Surat Basins.||||||
8610|Hutton Sandstone|67133|5|Briefly described|p1-3, p5, p11-13, p19-21|||A carbon geostorage target reservoir, sealed by Walloon Subgroup. Braided stream deposits. 73 samples of this unit were analysed by XRD and optical microscopy for this study. Quartz is the main component (25-94%) and kaolinite (2-37%) is the dominant clay mineral. Mixed-layer clays are smectite-rich.||||Overlies Evergreen Formation. Is overlain conformably by Walloon Subgroup.|White to light grey, fine- to medium-grained, sublabile to quartzose sandstone, with dark grey micaceous or carbonaceous siltstone interbeds.|
8610|Hutton Sandstone|67323|5|Briefly described|p87-88, p93 Fig.12.3, p95 Fig.12.5, p96|Middle Jurassic|Early Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin; also probable reservoir (the unit is one of the main continuous aquifers in the region).||||Overlies Poolowanna and Moolayember Formations. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|67402|4|Described|p26, p26 tbl RRM4, p36|Bathonian|Toarcian|Eromanga, Mulgildie and Surat Basins. Forms an extensive aquifer in the Surat Basin. Primary porosity has been partially occluded by quartz overgrowths, kaolinite, chlorite and calcite cement.  Fluvial to fluvio-lacustrine depositional environment.  Maximum thickness of 275m. Major hydrocarbon reservoir with a potential to store up to 5.8 megatonnes of carbon dioxide in the Eromanga Basin and 1198 megatonnes in the Surat Basin.  See also p36 fig VEM6, VEM7,p37, p43 tbl HPB1, p104, p108-p110, p111 fig ERO8, p113 , p114 fig ERO13, p115, p117, p118, p146 fig SRT3, p148, p151, p154, p155 fig SRT17, p156, p161, p162, p239, p252, p253, p306.|f|||Overlies the Upper Poolowanna Formation and the Evergreen Formation. Overlain by the Birkhead Formation or Walloon Subgroup.|Thick sandstone unit that is interbedded with siltstone, shale and minor mudstone and coal.|
8610|Hutton Sandstone|67561|6|Mentioned|p53 Fig.3|||||||||
8610|Hutton Sandstone|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Bundamba Group.||Overlain by Wallon CM. Underlain by Evergreen Formation.||
8610|Hutton Sandstone|68003|5|Briefly described|p55 Fig.3-m, p57 Fig.3-n, p61-63, p127.|Middle Jurassic|Early Jurassic|Surat Basin. Stratigraphic equivalent of upper part of Purlawaugh Formation. Toarcian to Aalenian. Maximum known thickness 275 m. Forms hill tops and small cliffs.||||Overlies Evergreen Formation. Unconformably overlies Deriah Formation; paraconformably overlies Gragin Conglomerate. Is overlain conformably by Walloon Coal Measures.|Well-sorted, medium- to coarse-grained quartzose sandstone, with some siltstone and mudstone, fragments of coal and silicified wood; local conglomerate beds.|
8610|Hutton Sandstone|68004|5|Briefly described|pp173-174.|||Excellent hydrocarbon reservoir potential and a major exploration target in NSW. Sealed by Walloon Coal Measures. A major hydrocarbon-producing reservoir in the Eromanga Basin in SW Queensland.||||||
8610|Hutton Sandstone|68008|4|Described|p186, p236, p238-240, p297|Middle Jurassic|Early Jurassic|Appears to have been defined by Gray (1972); 275m thick in GSQ Monto 1-2R. The type section is in the Eddystone 250k sheet area. Surat and Mulgildie Basins. Forms a N-S trending belt 27 x 5 km. Has zones of deep weathering.||||Conformably and gradationally overlies Evergreen Formation. Faulted against and/or unconformably overlies Cynthia beds. Is overlain conformably and gradationally by Mulgildie Coal Measures.|Pale grey to white, well-bedded, quartzose sandstone, minor granule conglomerate, and thin sandy siltstone beds.|
8610|Hutton Sandstone|68068|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|Eromanga Basin. Subsurface only. Mainly fluvial, with possible aeolian and lacustrine deposition. Palynological age. Is replaced by Algebuckina Sandstone as it pinches out at Eromanga Basin margin.||||Overlies Algebuckina Sandstone. Is overlain by Birkhead Formation.|White, fine- to very coarse-grained and conglomeratic quartzose sandstone, flat to cross-bedded; common reworked clasts and minor interbeds of mudstone; carbonaceous partings.|
8610|Hutton Sandstone|68117|5|Briefly described|p346, p348-349|Middle Jurassic|Middle Jurassic|Surat Basin.||||Overlies Evergreen Formation. Is overlain by Eurombah Formation or, where absent, Durabilla Formation.||
8610|Hutton Sandstone|68135|5|Briefly described|p52 fig 2b, p57 fig 4, p62, p64|Callovian|Toarcian|Surat Basin (QLD) and Eromanga Basin. Age derived from fossils of Osmundacaulis. Vertebrate body parts present, eg the sauropod Rhoetosaurus brownei.||||Overlies Evergreen and Poolawanna Formations. Is overlain by Walloon Coal Measures (Surat Basin) or Birkhead Formation (Eromanga Basin).|Fossiliferous and cross-bedded, iron-rich sandstone.|14-SEP-17
8610|Hutton Sandstone|68139|6|Mentioned|p23-25, 32|Middle Jurassic|Early Jurassic|Surat Basin. A major aquifer. Hydrocarbons present are thought to be connected with fault leakage.||||Overlies Evergreen Formation. Is overlain by Walloon Subgroup (Injune Creek Group).||
8610|Hutton Sandstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
8610|Hutton Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Surat and Mulgildie Basins. This unit, as well as the Evergreen Formation and Precipice Sandstone, are all mapped under the symbol, Jb.||||||
8610|Hutton Sandstone|68576|5|Briefly described|Q_4: p3, p12 Fig.14, p17, p22, p24|Middle Jurassic|Early Jurassic|Surat Basin. A widely-used aquifer in the Great Artesian Basin. Extends E into the Clarence-Moreton Basin and W into the Eromanga Basin. Sediments deposited by meandering streams on a broad floodplain.||||Conformably overlies Evergreen Formation. Is overlain by Walloon Coal Measures.|White to light grey, sub-labile to quartzose sandstone with interbedded siltstone, shale, minor mudstone and coal: partly arkosic, and with a higher proportion of siltstone and shale to the S.|
8610|Hutton Sandstone|68679|6|Mentioned|p312-313, p338|Jurassic|Jurassic|Northern New England Orogen.||||||
8610|Hutton Sandstone|68731|6|Mentioned|pp207-211|||||||Unconformably underlain by the Nappamerri Group and the Tinchoo Formation.||
8610|Hutton Sandstone|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
8610|Hutton Sandstone|69019|5|Briefly described|p85 Fig.21.|Middle Jurassic|Early Jurassic|Southern Eromanga Basin.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.||
8610|Hutton Sandstone|69023|5|Briefly described|p79, p89 Fig.20, p90-91, p191-192|Middle Jurassic|Middle Jurassic|Defined by Reeves (1947) from outcrops in Roma (Qld); applied by Kapel (1966) to subsurface Early-Middle Jurassic sandstones in Eromanga Basin. Up to 260m thick. Equivalent to part of Algebuckina Sandstone. Stratigraphic wells intersection data.||||Overlies Patchawarra Formation unconformably, and overlies and intertongues with Poolowanna Formation. Is overlain conformably by Birkhead Formation.|White fine- to very coarse-grained quartzose sandstone, flat to planar cross-bedded; minor channel lag conglomerate and brown laminated and carbonaceous mudstone/siltstone interbeds. Local in situ duricrusts of calcrete and silcrete.|
8610|Hutton Sandstone|69457|5|Briefly described|p41:2-5|||Eromanga Basin. Lateral equivalent of lower Algebuckina Sandstone. ||||Conformably overlies, and locally intertongues with, Poolowanna Formation. Is overlain conformably by Cadna-owie Formation or disconformably by Bulldog Shale.||12-JUL-16
8610|Hutton Sandstone|69574|6|Mentioned|p23-24|Middle Jurassic|Early Jurassic|Surat Basin. A major regional aquifer.||||Is overlain by Walloon Subgroup.||
8610|Hutton Sandstone|69582|5|Briefly described|p36, p38, p65-p66|Middle Jurassic|Middle Jurassic|Surat Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Evergreen Formation and the Poolowanna Formation. Overlain by the Walloon Coal Measures and the Birkhead Formation.|Sandstone.|
8610|Hutton Sandstone|69594|4|Described|p519, p524-526, p531, p533-536,p545,p573|Bathonian|Aalenian|Reeves (1947). Eromanga, northern Surat Basins; originally defined in the latter. Kapel (1966) included Early and Middle Jurassic sandstones in the Cooper Basin region (probably included the Poolowanna Formation). Braided fluvial deposits. Mostly 90-210m thick; up to 266m. The most widespread Jurassic unit in the Great Australian Superbasin; constitutes the upper Marburg Subgroup in the Clarence-Moreton Basin. Late Toarcian to Callovian. The most important hydrocarbon reservoir in the Eromanga Basin, but minor in the Surat Basin. The most heavily used groundwater aquifer, and the main hot aquifer (geothermal energy) target, in the Basin.||||Conformably overlies Poolowanna (and intertongues with it) and Evergreen Formations. Is overlain conformably by Birkhead and Eurombah Formations and Walloon Coal Measures.|Quartzose to sublabile sandstones with interbedded siltstone and shale and minor coal and mudstone.|
8610|Hutton Sandstone|69633|5|Briefly described|p3-4, p7, p10, p14, p21, Appendix 6.|Middle Jurassic|Early Jurassic|Surat Basin. Fluviatile braided-stream sediments.||||Overlies Evergreen Formation. Is overlain by Walloon Coal Measures.||
8610|Hutton Sandstone|69673|6|Mentioned|p154, p155 fig 127|Jurassic|Jurassic|||||Overlies Poolowanna Formation, overlain by Birkhead Formation||
8610|Hutton Sandstone|69681|5|Briefly described|p74-87|Middle Jurassic|Early Jurassic|Generally high permeability, although permeability decreases by an order of magnitude below ~1500m. Potential for CO2 geostorage, sealed by Walloon Subgroup, discussed. Mineralogy and likely chemical changes from CO2 injection discussed.||||||
8610|Hutton Sandstone|69682|4|Described|p91-110|Middle Jurassic|Middle Jurassic|Laterally extensive: Surat Basin, extending into Moreton and Eromanga Basins. Average thickness 120-180m, to maximum of 266m. Mineralogy discussed in detail. Potential CO2 reservoir, but its immature mineralogy indicates potential geochemical reactivity during CO2 sequestration. ||||Overlies Evergreen Formation. Is overlain by Walloon Subgroup (Injune Creek Group).|Mica-rich, sublithic to quartzose, well-sorted, fine- to medium-grained sandstone, with interbedded siltstone and mudstone, rip-up clasts and pebble lags; minor coal and mudstone.|
8610|Hutton Sandstone|69790|6|Mentioned|p1062, p1064 Fig.3, p1066-1069, p1073|Middle Jurassic|Early Jurassic|See also p1077-1078. Surat Basin.||||Conformably overlies Evergreen Formation. Is overlain by Durabilla Formation.||
8610|Hutton Sandstone|69797|5|Briefly described|p17 Fig.2|||Age: Middle Jurassic - Early Cretaceous (approximated from figure). Geol. Prov: Eromanga Basin.||||||
8610|Hutton Sandstone|69946|3|Fully described|p10-15, p51, p57-58, p60-61, p68-78|Middle Jurassic|Middle Jurassic|Reeves (1947) used the name for a Member of the 'Bundamba series' in the Roma area (Qld). The name was applied to sandstone of 'Lower-Middle Jurassic age' in the Cooper region by Kapel (1966). Type section is an outcrop on Westgrove Station, N of Injune (Qld). Thickness from 40m to >360m, thickening northwards. Wireline log correlations.||||Intertongues with and overlies Poolowanna Formation. Intertongues with or is gradational into overlying Birkhead Formation. Passes laterally into Algebuckina Sandstone.|Mineralogically mature, fine- to coarse-grained quartzose sandstone with minor siltstone interbeds. Thin calcite and silica-cemented horizons occur in upper parts.|
8610|Hutton Sandstone|69947|5|Briefly described|p3, p5-7, p13 Fig.7.2, p16-17 Figs.7.5-6|Late Jurassic|Middle Jurassic|See also p21-27 Figs.7.10-16. Eromanga Basin. Sand-rich lowstand deposits form the principal hydrocarbon reservoirs throughout the Basin. Paleogeography maps. Generalised stratigraphic section.||||Overlies Poolowanna Formation. Is overlain by Birkhead Formation.|Thick, laterally extensive, amalgamated sandstones.|
8610|Hutton Sandstone|69948|6|Mentioned|p3|||Cooper region, Eromanga Basin.||||||
8610|Hutton Sandstone|70036|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|Surat Basin. Included in a mapped unit of fluvial and lacustrine sequences: lithic to quartzose sandstone, siltstone, mudstone, claystone and coal.||||||
8610|Hutton Sandstone|70374|5|Briefly described|p808, p809, figure 1,|Callovian|Aalenian|Previously considered Aalenian - Bathonian age. Radiometric dating of tuffs in overlying Walloon Coal Measures suggests Hutton Sandstone may extend into the Callovian.||||Overlies Evergreen Formation. Underlies Walloon Subgroup conformably. Underlies Eurombah, Durabilla, Birkhead Formations.||28-SEP-16
8610|Hutton Sandstone|70628|6|Mentioned|p951, 953, p952 Fig 4|Aalenian|Aalenian|Erosive base forms a sequence boundary for the K-sequence (Hoffman et al 2009) of the Surat Basin.||||Unconformably overlies Evergreen Formation. Comformably (gradationally?) underlies Durabilla Formation, Eurombah Formation, Walloon Subgroup.|Sandstone, erosive base, fluvial sediments fine upwards.|
8610|Hutton Sandstone|70725|6|Mentioned|p13|Middle Jurassic|Middle Jurassic|Surat Basin.||||Is overlain by Durabilla and Eurombah Formations (Walloon Subgroup).||
8610|Hutton Sandstone|70821|5|Briefly described|p21 Fig.2.6, p79-80|Jurassic|Jurassic|A high-quality aquifer in the Great Artesian Basin. Appears as Hutton Sandstone Formation in Fig.2.6. Hydrochemistry mentioned.||||Overlies Evergreen Formation. Is overlain by Birkhead Formation or Walloon Coal Measures (Injune Creek Group).||
8610|Hutton Sandstone|70823|5|Briefly described|p6, p43-p44, p78|Early Cretaceous|Early Jurassic|Eromanga Basin. See also Hutton Formation. Up to 230m thick. Deposited in a braided fluvial environment with some aeolian influence.||||Intertongues with the Namur Sandstone. Overlies the Poolowanna Formation. Overlain by and interfingers with the Birkhead Formation.||
8610|Hutton Sandstone|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Poolowanna Formation. Overlain by the Birkhead Formation.||
8610|Hutton Sandstone|71282|6|Mentioned|p456, p457 Fig.1, p460|||Amalgamated braided channels passing up into occasional meandering channels. Appears as Durabilla & Hutton Formation on p460.||||Is overlain by Durabilla Formation.||
8610|Hutton Sandstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
8610|Hutton Sandstone|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch3  p17-p18|Callovian|Aalenian|Eromanga Basin. First used by Reeves (1947) for a member of the 'Bundamba series'. It was subsequently redefined by Kapel (1966b) as sandstone of 'Lower-Middle Jurassic age' in the Cooper region. A type section outcropping on Westgrove station was designated by Reeves (1947). Age derived from palynology. Sedimentary features and palaeoenvironment are discussed in some detail. Spore-pollen zone is given in Ch5 p57. This unit was the source of the first discovery of commercial quantities of oil in the Eromanga Basin. A complete sedimentary facies log is given in Ch5 p68. Sequence stratigraphy detailed in Ch7 as is source rock potential and hydrocarbon geochemistry (Ch8). Seal and reservoir characteristics discussed in Ch11. This unit is one of the primary sources of petroleum production in the Eromanga Basin. See also Ch5 p12-p15, Ch5 p31, Ch5 p51, Ch5 p57-p58, Ch5 p67-p74, Ch5 p76, Ch6 p5-p6, Ch7 p3, Ch7 p5-p7, Ch7 p10, Ch7 p13, Ch7 p16, Ch7, Ch8 p p21, Ch7 p27, Ch8 p4, Ch8 p10, Ch8 p13-p14, Ch9 p5, Ch9 p11, Ch10 p3, Ch10 tbl 10.1, Ch10 p6-p8, Ch10 p14, Ch10 p17-p20, Ch11 p2-p5, Ch11 p7-p8, Ch11 p14, Ch12 p2, Ch12 p5, Ch12 p12, Ch12 p14, Ch13 p2-p4, Ch13 p6-p10, Ch13 p19, Ch13 p21, Ch13 p23-p24, Ch13 p37-p38, Ch14 p3, Ch14 p5-p7.||||Overlies the Poolowanna Formation. Conformably overlain by the Birkhead Formation. Equivalent to the Algebuckina Sandstone.|Fine to coarse-grained, planar to cross-bedded, quartzose sandstone with minor siltstone interbeds. Thin calcite and silica cemented horizons occur in the Hutton Sandstone.|
8610|Hutton Sandstone|71805|5|Briefly described|p76-p77, p86|Bajocian|Toarcian|Eromanga Basin and Northern Surat Basin.||||Overlies the Poolowanna Formation and the Evergreen Formation.||
8610|Hutton Sandstone|71806|6|Mentioned|p484-p485|Jurassic|Jurassic|Surat Basin.||||||
8610|Hutton Sandstone|72297|5|Briefly described|p739, p742-743, p745, p748, p751, p761|||The most important reservoir rock in the Eromanga Basin; sealed by Birkhead Formation. Gas produced from 31 fields. Minor oil reserves in fault-related traps. A major aquifer with excellent prospects for HSA (hot sedimentary aquifer) geothermal energy.||||||
8610|Hutton Sandstone|72298|5|Briefly described|p796, p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW). A source of groundwater in the Monto area. Main confined aquifers and confining beds, generally producing flowing artesian water bores.||||Overlies Poolowanna FZ and Boxvale Sandstone Member (Evergreen FZ) conformably and Moolayember FZ unconformably. Underlies Birkhead or Eurombah FZs (Injune Creek Group) and Walloon Coal Measures.||
8610|Hutton Sandstone|72921|4|Described|p8-14, p15 Fig.2, p16-25, p27-32.|Middle Jurassic|Middle Jurassic|First significant regional aquifer above proposed Precipice Sandstone CO2 storage reservoir in Surat Basin, but extends across the Clarence-Moreton and Eromanga Basins as well. Braided and meandering fluvial to deltaic depositional system interpreted. Mineralogy discussed. Sedimentology & facies discussed. See also p36-41, p42-54, p56, p59, p61-67, p69-72, p77-78, p80, p81 Fig.43, p83 Fig.44-45.||||Partially overlies and is laterally equivalent to Evergreen Fm, Poolawanna Fm, Marburg Fm, and partially underlies and is laterally equivalent to Durabilla Fm, Eurombah Fm and Birkhead Fm.|Includes fragments of volcanic rocks within the fine to medium-grained thick-bedded quartzose to sublabile sandstone and tuffaceous layers. Also includes siltstone, shale, minor coal and fossils.|
8610|Hutton Sandstone|73113|5|Briefly described|p. 19, 22-24, 26-27, 31, 36-37, 41...|||Surat Basin. Groundwater model divides unit into upper and lower layers. Lower layer = tight aquifer. Upper layer = partial aquifer. More locations: p. 49, 61, 67, 69, 76, 79-80, 93, 98, 116-117, 119, 123, 126-130, 147-149, 152-153, 158-160, 162, 164-173, 177, 179, 191-193, 200.||||Underlain by Evergreen Formation. Overlain by Durabilla Formation.|Upper portion is typically characterised by thick, indurated sandstones; lower portion comprises more thinly interbedded sandstone/siltstones.|
8610|Hutton Sandstone|73147|6|Mentioned|p128|Jurassic|Jurassic|Eromanga Basin.||||||
8610|Hutton Sandstone|73167|6|Mentioned|p664 Fig. 2|Jurassic|Jurassic|Eromanga Basin. Contains oil, hydrocarbon source.||||||
8610|Hutton Sandstone|73193|6|Mentioned|p369|Callovian|Aalenian|Surat Basin.||||Overlain by Walloon Subgroup (Injune Creek Group).||
8610|Hutton Sandstone|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
8610|Hutton Sandstone|73203|6|Mentioned|p652|||Found in the Jundah 1 well, central Queensland.||||||
8610|Hutton Sandstone|73251|6|Mentioned|p49, p62|Middle Jurassic|Middle Jurassic|Eromanga Basin. Deposited in a braided fluvial setting with aeolian influence. Contains[?] oil.||||Underlain by Poolowanna Formation. Overlain by [and equivalent to?] Birkhead Formation. Equivalent to Algebuckina Sandstone.||
8610|Hutton Sandstone|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Source rock that hosts oil.||||Underlain by Poolowanna Formation. Overlain by Birkhead Formation.||
8610|Hutton Sandstone|73393|6|Mentioned|p20-23|Bajocian|Aalenian|Surat and Eromanga Basins. Previously reported (in error) to have hosted the sauropod Rhoetosaurus brownei.||||Underlain by Evergreen Formation. Overlain by Birkhead Formation and Eurombah Formation (Injune Creek Group).||
8610|Hutton Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p164, p179|Jurassic|Jurassic|Eromanga Basin. Braided fluvial depositional environment.|ca 178-160 Ma|||Overlies Poolowanna Formation, underlies Birkhead Formation||
8610|Hutton Sandstone|73600|6|Mentioned|p190-191|Aalenian|Toarcian|Somewhat uniform thickness.||||Underlain by Evergreen Formation.||
8619|Hyandra Creek Group|22768|5|Briefly described|p180||Early Devonian|||||||
8619|Hyandra Creek Group|22857|5|Briefly described|p180, p492 App.1 Tb.A1.7|Early Devonian|Early Devonian|Rhyolite, dacite, spillite. Geological Province: Dulladerry Rift.||||||
8619|Hyandra Creek Group|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|||||||
8619|Hyandra Creek Group|23170|4|Described|p206|||of Lachlan Fold Belt.||||||
8619|Hyandra Creek Group|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
8619|Hyandra Creek Group|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
8619|Hyandra Creek Group|42726|5|Briefly described|map legend|Early Devonian||V10.  Of the Boggy Plain Suite (Boggy Plain Supersuite).||||||08-FEB-05
8619|Hyandra Creek Group|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
8619|Hyandra Creek Group|50590|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Cumboogle Formation, Ellersley Formation, Peachvale Formation, Mudgingar Creek Formation.||||||
8619|Hyandra Creek Group|68003|5|Briefly described|p24 Fig.3-e, pp142-143. |Lochkovian|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Peachvale and Glenlee Rhyolites, Dunoon Dacite and Ellersley Formation.|Overlies Toongi Group.||
8619|Hyandra Creek 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.||||||
8621|Hyde Greywacke Member|34555|4|Described|p241|||||||||
8621|Hyde Greywacke Member|43399|2|Defined|p195,196,203-205|Early Carboniferous|Late Devonian|||||||
8621|Hyde Greywacke Member|43400|14|Not recorded|map opp.p.188|Early Carboniferous|Late Devonian|||||||
8621|Hyde Greywacke Member|43406|14|Not recorded|p42|||Member of Goonoo Goonoo Mudstone (Parry Group)||||||
8621|Hyde Greywacke Member|68005|5|Briefly described|p148.|Devonian|Devonian|||Unit in Parry Group.|||Labile lithic wacke.|
8630|Hylea Intrusive Complex|730|6|Mentioned|p22 Fig.5.|||||||||11-NOV-14
8630|Hylea Intrusive Complex|22519|6|Mentioned|p6|||||||||
8630|Hylea Intrusive Complex|22831|4|Described|p 19-20|Devonian||K-Ar age: 405Ma (Pogson and Hilyard, 1981) - possible metamorphic age.  SHRIMP age: 448+/-4Ma (Elliott and Martin, 1991).  See also "Hylea Intrusive Complex".||||||21-JUL-04
8630|Hylea Intrusive Complex|40365|2|Defined|p325|Early Devonian|Early Devonian|||||||
8630|Hylea Intrusive Complex|40682|4|Described|p5|||||||||
8630|Hylea Intrusive Complex|42077|6|Mentioned|p21|||||||||
8630|Hylea Intrusive Complex|42912|6|Mentioned|Fig.1|||||||||
8630|Hylea Intrusive Complex|43441|5|Briefly described|13|||397 +/- 12 Ma (K-Ar) but Age: ?Late Ordovician||||||08-JAN-10
8630|Hylea Intrusive Complex|44160|5|Briefly described|Map Legend||Eastonian|||||||08-JAN-10
8630|Hylea Intrusive Complex|73154|5|Briefly described|p78 Tb.1|Llandovery|Late Ordovician|Junee-Narromine structural belt. 442.8+/-2.4 Ma zircon U-Pb age from Hylea monzonite sample p89 Tb.2, shown as from Hylea Intrusive Complex in p78 Tb.1, and called Hylea Intrusion p79.|442.8+/-2.4 Ma zircon U-Pb|Of Fifield Complex?|||Pipe-like intrusion comprises medium to coarse grained hornblende-dominant cumulate gabbro and diorite with zones, vein dykes and segregations of pegmatite and pink to grey medium grained monzonite differentiates.|
8637|Icely Granite|23214|3|Fully described|p248|Carboniferous|Carboniferous|Poorly exposed circular felsic pluton.  Geological Province: Bathurst Batholith||||||
8637|Icely Granite|42726|5|Briefly described|map legend|Carboniferous|Carboniferous|13.  Of the Bathurst Suite (Bathurst Supersuite). Variation on Icely Road Quartz Monzonite.||||||07-FEB-05
8637|Icely Granite|43127|5|Briefly described|p4,Fig.2,Fig.3|||Middle Carboniferous||||||
8637|Icely Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
8637|Icely Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|of Bathurst Batholith. Does not appear on map face.||||||
8637|Icely Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
8688|Ingebyrah Granodiorite|22815|4|Described|p47,48|Silurian|Silurian|||||||
8688|Ingebyrah Granodiorite|33782|6|Mentioned|Fig.2|||||||||
8688|Ingebyrah Granodiorite|35263|6|Mentioned|Table 3|||||||||
8688|Ingebyrah Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
8688|Ingebyrah Granodiorite|40328|4|Described|p207|||||||||
8688|Ingebyrah Granodiorite|41898|6|Mentioned|p1184|||||||||
8688|Ingebyrah Granodiorite|41905|2|Defined|p82|Silurian||||||||
8688|Ingebyrah Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
8688|Ingebyrah Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Ingebyrah Suite.||||||
8688|Ingebyrah Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb12.||||||
8688|Ingebyrah Granodiorite|49705|6|Mentioned|p19|||This reference does not constitute 'publication'. BMR Records became publications in July 1991.||||||
8688|Ingebyrah Granodiorite|68115|5|Briefly described|p7.|||In New South Wales. Deddick Zone. Non-magnetic. Continues to the Victorian border, across which it is called Suggan Buggan Granodiorite. Probably the same pluton.|||||Biotite-cordierite granodiorite.|15-FEB-13
8689|Ingebyrah Suite|22815|5|Briefly described|p45|Silurian|Silurian|Composed of 5 plutons.||||||
8689|Ingebyrah Suite|23549|4|Described|p521-522|||Named from Ingebyrah pluton but consists of two plutons (Ingebyrah and Pot Hole). The I. pluton rocks are grey cordierite ; rocks of P.H.pluton have some mineral assemblage and contain large quartz aggregates. granites||||||05-APR-05
8689|Ingebyrah Suite|41898|6|Mentioned|p1184|||||||||
8689|Ingebyrah Suite|41905|6|Mentioned|p74|||||||||
8689|Ingebyrah Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
8689|Ingebyrah Suite|42726|5|Briefly described|map legend||Silurian|||||||
8689|Ingebyrah Suite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Kosciusko Batholith.||||||
8689|Ingebyrah Suite|44093|5|Briefly described|p188 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
8689|Ingebyrah Suite|68592|6|Mentioned|p1225|||||Unit in Bullenbalong Supersuite.||||
8689|Ingebyrah Suite|72571|6|Mentioned|p90, p99|||Of the Tasmanides of eastern Australia.||||||
8696|Ingleburn Formation|22529|4|Described|4 fig 2, 7|Emsian|Emsian|Parent Queens Pinch Group. Overlying unit Sutchers Creek Formation, underlying unit Warratra Mudstone||||||
8696|Ingleburn Formation|22590|6|Mentioned|Fig3 P754||Emsian|Actually spelt Ingleburn Fm.||||||
8696|Ingleburn Formation|22857|4|Described|p476 App.1 Tb.A1.6|Emsian|Emsian|Of the Queens Pinch Group. Dacite and andesite lava, fossiliferous mudstone, polymictic conglomerate, quartz arenite. Max. thickness: 600m. Geological Province: Capertee Rise.||||||
8696|Ingleburn Formation|23043|5|Briefly described|Map Legend|Emsian|Emsian|of Queens Pinch Group.||||||
8696|Ingleburn Formation|23170|2|Defined|p151|Emsian|Pragian|of Queens Pinch Group.||||||
8696|Ingleburn Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
8696|Ingleburn Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
8696|Ingleburn Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
8696|Ingleburn Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
8696|Ingleburn Formation|33326|6|Mentioned|p434|||Fauna.||||||
8696|Ingleburn Formation|42033|5|Briefly described|p656|||||||||
8696|Ingleburn Formation|43188|4|Described|p216,Table 4 p212|Emsian|Pragian|Age late Pragian to early Emsian.||||||
8696|Ingleburn Formation|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
8696|Ingleburn Formation|71924|5|Briefly described|p3|||Fossiliferous.||||Correlated with Cunningham [Formation], Suchers Creek [Formation].||
8696|Ingleburn Formation|73299|6|Mentioned|p1096 Fig.3, p1097 Fig.4|Early Devonian|Early Devonian|||Queens Pinch Group||||
8710|Injune Creek Group|12597|5|Briefly described|p492 Tb.1, p496, p497, p499|Kimmeridgian|Callovian|Of Swarbrick (1973). Eromanga Basin.|||Includes Westbourne, Birkhead and Eurombah Formations; Adori and Springbok Sandstones; and Walloon Subgroup.|Conformably overlies Hutton Sandstone.||
8710|Injune Creek Group|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Jurassic|Middle Jurassic|In Surat Basin, Eromanga Basin.||||||
8710|Injune Creek Group|22857|5|Briefly described|p296-7 Tb.22.1, p314|Tithonian|Bajocian|Includes the Eurombah Formation, Walloon Coal Measures, Springbok, Pilliga and Gubberamunda Sandstones. Geological Province: Surat Basin.||||||
8710|Injune Creek Group|22865|4|Described|p314,Table22.1p296-7|Tithonian|Bajocian|||||||
8710|Injune Creek Group|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
8710|Injune Creek Group|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
8710|Injune Creek Group|23425|5|Briefly described|Plate 10.2|||||||||
8710|Injune Creek Group|23430|4|Described|p525|||Also see p524 Table 14.7. Eromanga Basin Province.||||||
8710|Injune Creek Group|23799|5|Briefly described|p48 Fig. 3|Callovian|Bathonian|Includes the Walloon Coal Measures and the Birkhead Formation.  Geological Province: Surat Basin.||||||
8710|Injune Creek Group|23883|5|Briefly described|p129 Fig. 11.2|Late Jurassic|Late Jurassic|Includes the Westbourne Fm., Adori Sandstone and Birkhead Formation.  Geological Province: Sydney Basin.||||||
8710|Injune Creek Group|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
8710|Injune Creek Group|24068|4|Described|p271|Late Jurassic|Middle Jurassic|Geological Province: Surat Basin.  Maximum thickness: 775m.||||||
8710|Injune Creek Group|24069|5|Briefly described|p284|Late Jurassic|Middle Jurassic|Geological Province: Surat Basin.||||||
8710|Injune Creek Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
8710|Injune Creek Group|24243|5|Briefly described|p3 Fig.2|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|29385|6|Mentioned|p80|||Also P81&82.Jurassic.||||||
8710|Injune Creek Group|29387|6|Mentioned|p30|||Table 5 also.||||||
8710|Injune Creek Group|29389|6|Mentioned|p19|||Middle Jurassic.||||||
8710|Injune Creek Group|29393|6|Mentioned|Table 4|||Jurassic.||||||
8710|Injune Creek Group|29591|5|Briefly described|p69|||||||||
8710|Injune Creek Group|29721|6|Mentioned|p246|||||||||
8710|Injune Creek Group|30021|6|Mentioned|p90|||||||||
8710|Injune Creek Group|30024|6|Mentioned|p331|||||||||
8710|Injune Creek Group|30102|4|Described|p21|||See also p22-25. Middle to Upper Jurassic age.||||||22-AUG-18
8710|Injune Creek Group|30103|5|Briefly described|p9|||Table 3 on p9. Middle to Upper Jurassic age.||||||22-AUG-18
8710|Injune Creek Group|30104|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|Middle to Upper Jurassic age.||||||
8710|Injune Creek Group|30457|6|Mentioned|p96|||||||||
8710|Injune Creek Group|30461|6|Mentioned|p100|||||||||
8710|Injune Creek Group|30508|6|Mentioned|p81|||See also p90. Early Jurassic palynology||||||22-AUG-18
8710|Injune Creek Group|30691|4|Described|p15|||See also Table 4||||||
8710|Injune Creek Group|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|30694|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|30695|4|Described|Table 4|||Middle to Upper Jurassic age||||||
8710|Injune Creek Group|30696|4|Described|Table 4|||Middle-Upper Jurassic age||||||
8710|Injune Creek Group|30698|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle-Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|30700|6|Mentioned|p22|||Middle-Upper Jurassic. Map||||||
8710|Injune Creek Group|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
8710|Injune Creek Group|30853|5|Briefly described|Table 3|||Middle to Upper Jurassic age||||||
8710|Injune Creek Group|30854|4|Described|Table 4|||Middle-Upper Jurassic||||||
8710|Injune Creek Group|30855|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|30856|4|Described|p10|||Lower to Upper Jurassic age. On Table 3||||||
8710|Injune Creek Group|30857|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
8710|Injune Creek Group|30915|6|Mentioned|p98|||||||||
8710|Injune Creek Group|31098|6|Mentioned|p5|||M. - U. Jurassic||||||
8710|Injune Creek Group|31116|4|Described|p27|||See also Table 2. Jurassic||||||
8710|Injune Creek Group|31117|6|Mentioned|p378|||Jurassic||||||
8710|Injune Creek Group|31121|6|Mentioned|p385|||||||||
8710|Injune Creek Group|31369|6|Mentioned|Table 4|||Jurassic||||||
8710|Injune Creek Group|31425|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|31430|5|Briefly described|Table 1|||M.-U.Jurassic||||||
8710|Injune Creek Group|31431|4|Described|Table 3|||M.-U.Jurassic||||||
8710|Injune Creek Group|31432|4|Described|Table 1|||Middle-Upper Jurassic||||||
8710|Injune Creek Group|31436|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|31438|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|31553|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|32040|6|Mentioned|p886|||Geological map||||||
8710|Injune Creek Group|32136|6|Mentioned|p3|||Basal section early Bajocian||||||
8710|Injune Creek Group|32138|6|Mentioned|p396|||||||||
8710|Injune Creek Group|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Mid.-U.Jurassic||||||22-AUG-18
8710|Injune Creek Group|32797|4|Described|Table 4|||M.-U. Jur.||||||
8710|Injune Creek Group|33067|4|Described|Table 1|||Includes the Westbourne and Birkhead Formations and the Adori Sandstone.||||||07-JUL-04
8710|Injune Creek Group|33069|4|Described|p7|||M.-U.Jur.||||||
8710|Injune Creek Group|33070|4|Described|Table 2|||M.-U.Jur.||||||
8710|Injune Creek Group|33071|4|Described|p6|||M.-U.Jur.||||||
8710|Injune Creek Group|33078|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33079|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Mid.- U.Jur.||||||22-AUG-18
8710|Injune Creek Group|33080|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33082|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33087|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||22-AUG-18
8710|Injune Creek Group|33088|4|Described|Table 3|||Jurassic||||||
8710|Injune Creek Group|33089|5|Briefly described|Table 2|||M.-U.Jur.||||||
8710|Injune Creek Group|33090|4|Described|Table 4|||Mid.-U.Jur.||||||
8710|Injune Creek Group|33092|5|Briefly described|p6|||Strat. table||||||
8710|Injune Creek Group|33094|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33096|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33176|6|Mentioned|p175|||||||||
8710|Injune Creek Group|33367|4|Described|Table 1|||See also p3. suggested type sect. p15.||||||22-AUG-18
8710|Injune Creek Group|33371|3|Fully described|p57|||||||||
8710|Injune Creek Group|33449|4|Described|Table 1|||Mid.-U.Jur.||||||
8710|Injune Creek Group|33451|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|M.-U.Jur.||||||22-AUG-18
8710|Injune Creek Group|33638|5|Briefly described|Table 1|||||||||
8710|Injune Creek Group|33639|5|Briefly described|Table 2|||M.-U.Jur.||||||
8710|Injune Creek Group|33640|4|Described|Table 3|||M.-U.Jur.||||||
8710|Injune Creek Group|33643|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33647|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|33648|6|Mentioned|p14|||Equiv. Strat. Table.||||||
8710|Injune Creek Group|33672|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|33774|5|Briefly described|Table 1|||||||||
8710|Injune Creek Group|33825|6|Mentioned|Table 4|||||||||
8710|Injune Creek Group|33832|5|Briefly described|p11|||Strat. & correlation||||||
8710|Injune Creek Group|34061|6|Mentioned|p54|||||||||
8710|Injune Creek Group|34091|5|Briefly described|Table 1|||Jur.||||||
8710|Injune Creek Group|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
8710|Injune Creek Group|34174|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.||||||22-AUG-18
8710|Injune Creek Group|34212|6|Mentioned|p2|||Jurassic||||||
8710|Injune Creek Group|34254|6|Mentioned|p481|||||||||
8710|Injune Creek Group|34487|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic||||||
8710|Injune Creek Group|34543|6|Mentioned|p98|||||||||
8710|Injune Creek Group|34613|4|Described|Table 4|||||||||
8710|Injune Creek Group|34905|6|Mentioned|p531|||||||||
8710|Injune Creek Group|35148|6|Mentioned|Fig.1|||||||||
8710|Injune Creek Group|35239|6|Mentioned|Fig.4|||||||||
8710|Injune Creek Group|35457|6|Mentioned|Fig.5|||Stratigraphic correlation||||||
8710|Injune Creek Group|35560|4|Described|p289|||||||||
8710|Injune Creek Group|35562|6|Mentioned|p295|||Stratigraphy||||||
8710|Injune Creek Group|35663|6|Mentioned|p124|||||||||
8710|Injune Creek Group|35811|5|Briefly described|Table 3|||||||||
8710|Injune Creek Group|35937|6|Mentioned|Fig.5|||||||||
8710|Injune Creek Group|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
8710|Injune Creek Group|36233|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|36243|6|Mentioned|p74|||See also Table 6A.||||||
8710|Injune Creek Group|36333|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|36570|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|36914|6|Mentioned|Fig.5|||||||||
8710|Injune Creek Group|36939|6|Mentioned|p214|||||||||
8710|Injune Creek Group|37065|6|Mentioned|p39|||||||||
8710|Injune Creek Group|37116|6|Mentioned|p310|||||||||
8710|Injune Creek Group|37451|6|Mentioned|Table 2|||||||||
8710|Injune Creek Group|37608|3|Fully described|Table 1|||||||||
8710|Injune Creek Group|37993|6|Mentioned|p153|||||||||
8710|Injune Creek Group|37995|4|Described|p64|||||||||
8710|Injune Creek Group|38064|6|Mentioned|42|||||||||
8710|Injune Creek Group|38199|5|Briefly described|p421|||Palynology||||||
8710|Injune Creek Group|38205|6|Mentioned|p96|||||||||
8710|Injune Creek Group|38226|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|39212|6|Mentioned|p16|||P24-petroleum reservoir. P25-aquifer||||||
8710|Injune Creek Group|39315|6|Mentioned|Fig.5|||||||||
8710|Injune Creek Group|39445|6|Mentioned|Table 10|||||||||
8710|Injune Creek Group|39478|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|39494|6|Mentioned|Fig.3|||See also Fig.5||||||
8710|Injune Creek Group|39847|6|Mentioned|p40|||||||||
8710|Injune Creek Group|39943|6|Mentioned|Table 8A|||||||||
8710|Injune Creek Group|40030|6|Mentioned|Fig.3|||||||||
8710|Injune Creek Group|40199|6|Mentioned|Fig.2|||||||||
8710|Injune Creek Group|40249|6|Mentioned|p38|||||||||
8710|Injune Creek Group|40250|6|Mentioned|p35|||||||||
8710|Injune Creek Group|40541|6|Mentioned|p114|||||||||
8710|Injune Creek Group|40544|6|Mentioned|Fig.4|||See also Fig.6||||||
8710|Injune Creek Group|40623|5|Briefly described|p73|||||||||
8710|Injune Creek Group|40801|6|Mentioned|p29|||||||||
8710|Injune Creek Group|40832|6|Mentioned|p459|||||||||
8710|Injune Creek Group|41061|6|Mentioned|p19|||||||||
8710|Injune Creek Group|41064|6|Mentioned|p60|||||||||
8710|Injune Creek Group|41097|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|41175|6|Mentioned|p195|||||||||
8710|Injune Creek Group|41177|6|Mentioned|Fig.2|||||||||
8710|Injune Creek Group|41198|6|Mentioned|Table 1|||||||||
8710|Injune Creek Group|41246|6|Mentioned|Map legend|Jurassic||||||||
8710|Injune Creek Group|41247|6|Mentioned|Fig.4|||See also Fig.7||||||
8710|Injune Creek Group|41266|6|Mentioned|Fig.3|||||||||
8710|Injune Creek Group|41681|6|Mentioned|p2|||||||||
8710|Injune Creek Group|41725|6|Mentioned|Fig.2|||||||||
8710|Injune Creek Group|41992|4|Described|Fig.2 P183|||||||||
8710|Injune Creek Group|42007|6|Mentioned|Fig.2 P182|||||||||
8710|Injune Creek Group|42061|4|Described|Fig,11 P159|||||||||
8710|Injune Creek Group|42493|5|Briefly described|Fig. 1 P18|||||||||
8710|Injune Creek Group|42634|6|Mentioned|Table 8 P34|||||||||
8710|Injune Creek Group|42911|6|Mentioned|p38|||||||||
8710|Injune Creek Group|43000|5|Briefly described|p109|||see also Fig.5,p112||||||
8710|Injune Creek Group|43122|5|Briefly described|Fig.2.|||||||||
8710|Injune Creek Group|43185|6|Mentioned|6||Jurassic|||||||
8710|Injune Creek Group|43539|14|Not recorded|p396,398|||gas||||||
8710|Injune Creek Group|43602|6|Mentioned|191|Late Jurassic|Middle Jurassic|In Eromanga Basin||||||
8710|Injune Creek Group|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44020|14|Not recorded|Tb.1|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44021|2|Defined|p232-234|Late Jurassic|Middle Jurassic|="Injune Creek Beds". Contains Birkhead Formation (Includes Springbok Sandstone Lens) and Westbourne Formation, Adori Sandstone (in Eromanga Basin). Is the sequence between Hutton and Gubberamunda Sandstones.||||||
8710|Injune Creek Group|44022|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44023|6|Mentioned|p11|||||||||
8710|Injune Creek Group|44028|14|Not recorded|p514||Jurassic|Lithological equivalent of the Injune Creek Beds. See Strat Table.||||||
8710|Injune Creek Group|44031|14|Not recorded|p6,8,9,11|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44042|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44099|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
8710|Injune Creek Group|44129|14|Not recorded|p95-96||Jurassic|||||||
8710|Injune Creek Group|44171|14|Not recorded|p194,197|||||||||
8710|Injune Creek Group|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
8710|Injune Creek Group|44414|14|Not recorded|p114,|Cretaceous|Jurassic|||||||
8710|Injune Creek Group|44415|14|Not recorded|Fig.2,p23|||||||||
8710|Injune Creek Group|44637|14|Not recorded|p287-291||Jurassic|||||||
8710|Injune Creek Group|45071|6|Mentioned|p134|||On Table 15||||||
8710|Injune Creek Group|45110|3|Fully described|p93|||See also P6.||||||
8710|Injune Creek Group|46881|6|Mentioned|Table 2|||||||||
8710|Injune Creek Group|46937|6|Mentioned|Fig.10|||||||||
8710|Injune Creek Group|46939|6|Mentioned|p50|||See also Table 1.||||||
8710|Injune Creek Group|46984|6|Mentioned|p157|||See also Table 1.||||||
8710|Injune Creek Group|46989|5|Briefly described|Table 1|||||||||
8710|Injune Creek Group|48900|6|Mentioned|p53|||||||||
8710|Injune Creek Group|48919|4|Described|p55|||See also p56. Jurassic||||||22-AUG-18
8710|Injune Creek Group|48920|5|Briefly described|p47|||Jurassic||||||
8710|Injune Creek Group|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
8710|Injune Creek Group|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
8710|Injune Creek Group|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Sandstone, siltstone, mudstone, coal, conglomerate.||||||
8710|Injune Creek Group|61312|5|Briefly described|p71, p79 Table E2|||In Queensland this unit occupies the interval between the Hutton and Hooray Sandstones; including, from base to top: Birkhead Formation, Adori Sandstone and Westbourne Formation. Geological Province: Eromanga Basin.||||||
8710|Injune Creek Group|61377|5|Briefly described|p148 Tb. SU1|Late Jurassic|Middle Jurassic|Includes the Westbourne Formation and Springbok Sandstone. Grey-brown siltstone and shale, coal, minor sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
8710|Injune Creek Group|61832|5|Briefly described|p187|Middle Jurassic|Jurassic|On the MUNDUBERRA sheet. Overlies Hutton Sandstone. Geological Province: Surat Basin.||||||03-JUL-06
8710|Injune Creek Group|62028|5|Briefly described|p10 Fig. 1|||||||||
8710|Injune Creek Group|63218|4|Described|p209, p211, p221.|Late Jurassic|Middle Jurassic|Surat Basin. Originally the informally-named Injune Creek Beds (Jensen 1921); subsequently renamed and formally defined as Injune Creek Group by Exon (1966); its stratigraphy was amended by Swarbrick et al. (1973). Includes a number of fluvial and lacustrine units.|||Includes basal Eurombah Formation; Walloon Subgroup; Birkhead Formation; Springbok Sandstone; and Westbourne Formation at the top.|||
8710|Injune Creek Group|64665|5|Briefly described|p53 Fig.2.|Late Jurassic|Middle Jurassic|Surat Basin.|||Includes Walloon Coal Measures, Springbok Sandstone and Westbourne Formation.|Overlies Hutton Sandstone. Is overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|64856|6|Mentioned|p87|||Andesitic detritus common.| | ||||29-NOV-17
8710|Injune Creek Group|65003|5|Briefly described|p1, p6, p13, p16, p25||Jurassic|Of Surat Basin. Fluvatile and paludal sediments derived largely from volcanism. Contains discontinuous coal beds.||||?Underlies the Orallo Formation.||
8710|Injune Creek Group|65096|6|Mentioned|p368|||||||The lower beds of the Injune Creek Group are equivalent to the Walloon Coal Measures.||
8710|Injune Creek Group|65119|5|Briefly described|p526, Fig 2, table 1, Fig 7-12, 16-19|Late Jurassic|Middle Jurassic|Surat Basin. Includes the Walloon Coal Measures. Sandstone, siltstone, mudstone, coal and lithic sandstone. Alluvial deposition up to 1200m thick.  Age: 153-168 Ma. Fission Track age: 132-145 Ma.||||||07-MAR-12
8710|Injune Creek Group|65388|3|Fully described|p215-216; p 204 Fig72, p214||Middle Jurassic|Rocks conformably overlying the Hutton Sandstone in the south-west corner of the study area. Thickness 62m to at least 150m. Includes Eurombah Formation in SW Bungaban map sheet area, and Walloon Coal Measures. Age of lower part of Group is same as Walloon Coal Measures: late Middle Jurassic (Bathonian to Callovian), based on palynofloras attributed to units APJ42, APJ43 and APJ5 (Price, 1997).||||||
8710|Injune Creek Group|65489|6|Mentioned|p96|||Eromanga Basin.||||||
8710|Injune Creek Group|66529|5|Briefly described|p12 Fig.5|||Eromanga Basin. Is called Injune Group on p10.|||Includes Birkhead and Westbourne Formations and Adori Sandstone.|Overlies Hutton Sandstone. Is overlain by Namur, Hooray and Gubberamunda Sandstones.|Fine grained lacustrine sandstone, siltstone and shale.|
8710|Injune Creek Group|66623|6|Mentioned|p449.|Middle Jurassic|Middle Jurassic|Formerly Injune Creek beds. Surat Basin. Petrified tree-fern, Osmundacaulis hoskingii, found also in Tibooburra area, was first described from this unit by Gould (1973).||||||
8710|Injune Creek Group|66915|5|Briefly described|p6 Fig.3|Late Jurassic|Middle Jurassic|Surat Basin.|||Westbourne Formation, Springbok Sandstone, Walloon Coal Measures|||
8710|Injune Creek Group|67669|5|Briefly described|p11|Late Jurassic|Middle Jurassic|Of Bowen Basin.|||Includes Westbourn Fm, Springbok Sandstone and Wallon CM.|Overlain by Blythesdale Group. Underlain by Bundamba Group.||
8710|Injune Creek Group|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.|||Includes Eurombah Formation, Walloon Coal Measures, Springbok Sandstone and Westbourne Formation.|Overlies Hutton Sandstone. Is overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|68117|5|Briefly described|p345-346, p348|Late Jurassic|Middle Jurassic|Formally defined by Exon (1966); previously the (informal) Injune Creek Beds of Jensen (1921). Redefined by Swarbrick, Gray and Exon (1973) who defined the basal Eurombah Formation, and included the Norwood Mudstone Member in the Westbourne Formation at the top. Drilling by Queensland Gas Company Limited has led to further redefinition of this unit in this study.|||Eurombah, Durabilla, Birkhead, Westbourne Formations; Springbok Sandstone.|||
8710|Injune Creek Group|68135|6|Mentioned|p55 fig 3, p59|Callovian|Bathonian|Northern Surat Basin.||||||14-SEP-17
8710|Injune Creek Group|68139|5|Briefly described|p23|Late Jurassic|Middle Jurassic|Surat Basin.|||Walloon Subgroup, Springbok Sandstone, Westbourne Formation.|Overlies Hutton Sandstone. Is overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Clarence-Moreton and Surat Basins. This unit, as well as the Mulgildie and the Walloon Coal Measures, are all mapped under the symbol, Ji.||||||
8710|Injune Creek Group|68576|5|Briefly described|Q_4: p3|Late Jurassic|Late Jurassic|Surat Basin.|||Includes Walloon Coal Measures, Springbok Sandstone, Westbourne Formation.|Overlies Hutton Sandstone.  Is overlain unconformably by Gubberamunda Sandstone.||22-OCT-19
8710|Injune Creek Group|68679|6|Mentioned|p312-313|Jurassic|Jurassic|Northern New England Orogen.||||||
8710|Injune Creek Group|69594|5|Briefly described|p519|||Northern Surat Basin.|||Westbourne Formation, Springbok Sandstone, Walloon Coal Measures.|Overlies Hutton Sandstone. Is overlain unconformably by Gubberamunda Sandstone.||
8710|Injune Creek Group|69681|6|Mentioned|p74 Fig.3|Late Jurassic|Middle Jurassic||||Includes Walloon Coal Measures, Springbok Sandstone and Westbourne Formation.|||
8710|Injune Creek Group|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Middle Jurassic|Surat Basin.|||Includes Walloon Subgroup; Springbok and Gubberamunda Sandstones; Westbourne Formation.|Overlies Hutton Sandstone.||
8710|Injune Creek Group|69790|6|Mentioned|p1063 Fig.2|Late Jurassic|Middle Jurassic|Northern Surat Basin.|||Includes Walloon Subgroup, Springbok Sandstone and Westbourne Formation.|||
8710|Injune Creek Group|70374|5|Briefly described|p808, p809 figure 1,|Jurassic|Jurassic||||Includes Birkhead, Eurombah, Westbourne Formations, Springbok Sandstone, Walloon Coal Measures.|||28-SEP-16
8710|Injune Creek Group|70821|5|Briefly described|p80|||Eromanga, Surat Basins.|||Birkhead, Westbourne, Eurombah Formations; Adori, Springbok, Pilliga Sandstones; Walloon Coal Measures.|Overlies Hutton Sandstone. Is overlain by Hooray Sandstone.||
8710|Injune Creek Group|71282|6|Mentioned|p456||||||Durabilla Formation [of Walloon Subgroup].|||22-AUG-18
8710|Injune Creek Group|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
8710|Injune Creek Group|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).|||Birkhead, Westbourne, Eurombah FZs; Adori, Springbok Sandstones; Walloon Coal Measures.|Overlies Hutton Sandstone. Is overlain by Namur, Hooray or Gubberamunda Sandstones.||
8710|Injune Creek Group|73193|6|Mentioned|p369|Tithonian|Callovian|Surat Basin.|||Westbourne Formation, Springbok Sandstone, Walloon Subgroup|Underlain by Hutton Sandstone. Unconformably overlain by Gubberamunda Sandstone.||
8710|Injune Creek Group|73393|6|Mentioned|p19-21|Tithonian|Bathonian|Surat and Eromanga Basins. Supersedes Injune Creek Beds.|||Walloon Coal MeasuresWestbourne Formation, Adori Sandstone, Springbok Sandstone, Walloon Coal Measures, Birkhead Formation, Eurombah Formation|Underlain by Hutton Sandstone.||
8735|Inner Barrier formation|31011|6|Mentioned|p570|||200+/-1150 years||||||
8748|Inverleith Sandstone|9548|5|Briefly described|Map Legend|Zlichovian|Zlichovian|Of the Yarra Yarra Creek Group. Underlies: Gleninga Formation. Overlies: Daalboro Sandstone.||||||06-JUL-04
8748|Inverleith Sandstone|22831|3|Fully described|p55-56||Lochkovian|Yarra Yarra Creek Group||||||01-NOV-13
8748|Inverleith Sandstone|22857|4|Described|p446 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Yarra Yarra Creek Group. Max. thickness: 350m. Geological Province: Darling Basin. ||||||
8748|Inverleith Sandstone|42449|6|Mentioned|p24|||Reserved 1977, D. Pogson. Last update May 1991.||||||
8748|Inverleith Sandstone|42566|5|Briefly described|Fig.25 P103|||||||||
8748|Inverleith Sandstone|43441|6|Mentioned|29||Early Devonian|||||||08-JAN-10
8748|Inverleith Sandstone|44160|5|Briefly described|Map Legend||Pragian|||||||08-JAN-10
8748|Inverleith Sandstone|61894|6|Mentioned|p179 Fig.3|||||||||
8748|Inverleith Sandstone|70751|6|Mentioned|p12|Lochkovian|Lochkovian|||Yarra Yarra Creek Group||||
8748|Inverleith Sandstone|72958|6|Mentioned|p11|Pragian|Lochkovian|Cobar Basin. Nymagee area.||Yarra Yarra Creek Group, Cobar Supergroup||Underlain by Daalboro Sandstone. Overlain by Gleninga Formation.||
8753|Iona Tonalite|22815|4|Described|p56|Silurian|Silurian|Formerly known as Iona Granodiorite.||||||
8753|Iona Tonalite|22876|4|Described|p24|||Currawong Suite||||||
8753|Iona Tonalite|22877|5|Briefly described|map|Silurian|Silurian|Currowong Suite. G54. Tonalite. I-Type.||||||26-OCT-04
8753|Iona Tonalite|23309|5|Briefly described|p68, 338, 344, 350|Silurian|Silurian|G54 - I-Type. Age: 422 +/- 3 Ma.||||||
8753|Iona Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
8753|Iona Tonalite|41572|6|Mentioned|Fig.1.10|||||||||
8753|Iona Tonalite|41905|2|Defined|p61|Silurian||||||||
8753|Iona Tonalite|41933|5|Briefly described|Map legend|Late Silurian||||||||
8753|Iona Tonalite|42627|5|Briefly described|Map legend|Wenlock||||||||
8753|Iona Tonalite|42647|4|Described|p39|||Currowong Suite||||||
8753|Iona Tonalite|42827|6|Mentioned|Fig 1.10|||||||||
8753|Iona Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||of Currowong Suite.||||||
8753|Iona Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh23||||||
8753|Iona Tonalite|60078|6|Mentioned|Map Legend|Devonian|Late Silurian|||||||
8753|Iona Tonalite|68116|5|Briefly described|Appendix, Map 36.|Wenlock|Llandovery||||||Tonalite: medium to fine grained, pale green to pink; moderately foliated.|
8762|Ipswich Coal Measures|12597|6|Mentioned|p493 Fig.2, p494|||||||||
8762|Ipswich Coal Measures|13516|5|Briefly described|p159 fig 8, p163, p164|Late Triassic|Late Triassic|From Clarence-Moreton Basin.|||Includes Kholo and Brassal Subgroups|||
8762|Ipswich Coal Measures|22857|5|Briefly described|p277, p318-9 Figs. 22.10A,B|Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|22860|6|Mentioned|p277||Late Triassic|||||||
8762|Ipswich Coal Measures|22861|6|Mentioned|p284|||||||||
8762|Ipswich Coal Measures|22865|5|Briefly described|p295,Fig22.9p317||Late Triassic|||||||
8762|Ipswich Coal Measures|23056|6|Mentioned|6|||Geol province Eromanga Basin||||||
8762|Ipswich Coal Measures|23440|6|Mentioned|p146|||||||||
8762|Ipswich Coal Measures|23799|5|Briefly described|p46|Norian|Carnian|Supersedes the Ipswich Beds.  Lower coal measures of the Bundamba Group.  Geological Province: Ipswich Basin.||||||
8762|Ipswich Coal Measures|23811|6|Mentioned|Map Legend|||Mentioned as equivalent to Red Cliff Measures.||||||20-DEC-04
8762|Ipswich Coal Measures|23812|5|Briefly described|p31, p33 Fig.6|||Geological Province: Ipswich Basin.||||||
8762|Ipswich Coal Measures|23843|5|Briefly described|p456 Table 1|Triassic|Triassic|Geological Province: Ipswich Basin.  Maximum thickness: 1220m.||||||
8762|Ipswich Coal Measures|24081|6|Mentioned|p451|||||||||
8762|Ipswich Coal Measures|24082|5|Briefly described|p453|Late Triassic|Late Triassic|Geological Province: Ipswich Basin.||||||
8762|Ipswich Coal Measures|24237|5|Briefly described|p5 Fig.1|||Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|24551|6|Mentioned|p241|||||||||
8762|Ipswich Coal Measures|29385|6|Mentioned|p81|||Also P82. Triassic.||||||
8762|Ipswich Coal Measures|29591|6|Mentioned|p83|||||||||
8762|Ipswich Coal Measures|29720|6|Mentioned|Fig.1|||||||||
8762|Ipswich Coal Measures|29869|6|Mentioned|p37|||See also P33||||||
8762|Ipswich Coal Measures|29995|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|30086|5|Briefly described|p4|||Triassic||||||
8762|Ipswich Coal Measures|30087|4|Described|p3|||Consists of Blackstone, Cooneana and Tivoli Formations.||||||
8762|Ipswich Coal Measures|30131|5|Briefly described|p9|||See also P8||||||
8762|Ipswich Coal Measures|30302|5|Briefly described|p414|||Upper Triassic age||||||
8762|Ipswich Coal Measures|30455|6|Mentioned|p5|||See also P12,18. Triassic age||||||
8762|Ipswich Coal Measures|30458|6|Mentioned|p1|||||||||
8762|Ipswich Coal Measures|30459|6|Mentioned|p309|||||||||
8762|Ipswich Coal Measures|30460|6|Mentioned|p5|||See also P12-14,16,22,26. Triassic age||||||
8762|Ipswich Coal Measures|30463|6|Mentioned|p464|||Triassic age||||||
8762|Ipswich Coal Measures|30464|6|Mentioned|Fig.1|||Triassic||||||
8762|Ipswich Coal Measures|30465|5|Briefly described|p1|||See also P2-22. Late Triassic age||||||
8762|Ipswich Coal Measures|30466|6|Mentioned|p1|||Triassic age||||||
8762|Ipswich Coal Measures|30467|6|Mentioned|p412|||Triassic age||||||
8762|Ipswich Coal Measures|30470|6|Mentioned|p457|||||||||
8762|Ipswich Coal Measures|30471|6|Mentioned|p132|||||||||
8762|Ipswich Coal Measures|30472|6|Mentioned|p134|||Pollen distribution.||||||
8762|Ipswich Coal Measures|30474|6|Mentioned|p249|||Microflora||||||
8762|Ipswich Coal Measures|30475|5|Briefly described|p164|||Refer palynology||||||
8762|Ipswich Coal Measures|30477|6|Mentioned|p461|||||||||
8762|Ipswich Coal Measures|30478|6|Mentioned|p272|||||||||
8762|Ipswich Coal Measures|30517|6|Mentioned|p436|||||||||
8762|Ipswich Coal Measures|30565|6|Mentioned|p132|||||||||
8762|Ipswich Coal Measures|30654|6|Mentioned|p48|||||||||
8762|Ipswich Coal Measures|30687|6|Mentioned|p65|||Triassic age||||||
8762|Ipswich Coal Measures|30784|6|Mentioned|p70|||Correlated with Red Cliff & Nymboiden Coal Measures (McElroy,1963,1969)||||||
8762|Ipswich Coal Measures|30785|6|Mentioned|p397|||Correlated with Red Cliff Coal Measures||||||
8762|Ipswich Coal Measures|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|30915|6|Mentioned|p98|||||||||
8762|Ipswich Coal Measures|31086|6|Mentioned|p33|||Triassic. Refers Jones & de Jersey (1947)||||||
8762|Ipswich Coal Measures|31118|6|Mentioned|p311|||||||||
8762|Ipswich Coal Measures|31272|6|Mentioned|p47|||||||||
8762|Ipswich Coal Measures|31276|6|Mentioned|p151|||Palynology||||||
8762|Ipswich Coal Measures|31300|6|Mentioned|p79|||Triassic plants.||||||
8762|Ipswich Coal Measures|31450|6|Mentioned|p47|||||||||
8762|Ipswich Coal Measures|31649|6|Mentioned|p63|||||||||
8762|Ipswich Coal Measures|31739|6|Mentioned|p85|||Stratigraphy||||||
8762|Ipswich Coal Measures|32136|6|Mentioned|p5|||Miospores||||||
8762|Ipswich Coal Measures|32176|6|Mentioned|p2|||Triassic||||||
8762|Ipswich Coal Measures|32178|6|Mentioned|p2|||||||||
8762|Ipswich Coal Measures|32179|6|Mentioned|p3|||Trias.||||||
8762|Ipswich Coal Measures|32180|6|Mentioned|Table 1|||||||||
8762|Ipswich Coal Measures|32491|5|Briefly described|p20|||M.-U. Triassic||||||
8762|Ipswich Coal Measures|32492|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Mid.-U.TriassicM - U||||||
8762|Ipswich Coal Measures|32801|6|Mentioned|Fig.9|||||||||
8762|Ipswich Coal Measures|32803|6|Mentioned|p83|||||||||
8762|Ipswich Coal Measures|32838|6|Mentioned|p320|||||||||
8762|Ipswich Coal Measures|32920|6|Mentioned|p89|||||||||
8762|Ipswich Coal Measures|33128|5|Briefly described|p50|||Geochemistry. See also Fig. 5.||||||
8762|Ipswich Coal Measures|33381|4|Described|p109|||Triassic. See also PP110-116,122.||||||
8762|Ipswich Coal Measures|33769|6|Mentioned|p149|||U.Triassic||||||
8762|Ipswich Coal Measures|33881|5|Briefly described|p96|||||||||
8762|Ipswich Coal Measures|34010|6|Mentioned|Cor. chart|||||||||
8762|Ipswich Coal Measures|34070|6|Mentioned|p2|||Triassic.  See also P3||||||
8762|Ipswich Coal Measures|34148|6|Mentioned|p18|||See also PP20,21. Upper Triassic.||||||
8762|Ipswich Coal Measures|34172|5|Briefly described|p50|||Palynological subdivision and correlations.||||||
8762|Ipswich Coal Measures|34340|6|Mentioned|p457|||Coal measures in Kyogle No.1 Well||||||
8762|Ipswich Coal Measures|34354|6|Mentioned|p3|||Triassic. See also P12.||||||
8762|Ipswich Coal Measures|34457|6|Mentioned|p484|||||||||
8762|Ipswich Coal Measures|34505|6|Mentioned|p1|||Middle Triassic. See also P3.||||||
8762|Ipswich Coal Measures|34755|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|35007|6|Mentioned|p75|||||||||
8762|Ipswich Coal Measures|35095|6|Mentioned|p115|||||||||
8762|Ipswich Coal Measures|35126|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|35156|4|Described|p6|||See also Table.2||||||
8762|Ipswich Coal Measures|35161|6|Mentioned|p591|||||||||
8762|Ipswich Coal Measures|35280|6|Mentioned|p143|||||||||
8762|Ipswich Coal Measures|35428|6|Mentioned|p125|||Biostratigraphy||||||
8762|Ipswich Coal Measures|35435|6|Mentioned|p44|||||||||
8762|Ipswich Coal Measures|35648|6|Mentioned|p13|||||||||
8762|Ipswich Coal Measures|35812|6|Mentioned|p568|||||||||
8762|Ipswich Coal Measures|35866|6|Mentioned|p403|||||||||
8762|Ipswich Coal Measures|35901|6|Mentioned|p5|||||||||
8762|Ipswich Coal Measures|35937|6|Mentioned|Fig.4|||||||||
8762|Ipswich Coal Measures|36045|6|Mentioned|p335|||||||||
8762|Ipswich Coal Measures|36237|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
8762|Ipswich Coal Measures|36243|6|Mentioned|p74|||||||||
8762|Ipswich Coal Measures|36351|6|Mentioned|p373|||||||||
8762|Ipswich Coal Measures|36354|6|Mentioned|p366|||||||||
8762|Ipswich Coal Measures|36440|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
8762|Ipswich Coal Measures|36779|4|Described|p6|||||||||
8762|Ipswich Coal Measures|36825|6|Mentioned|p4|||||||||
8762|Ipswich Coal Measures|36899|6|Mentioned|p1085|||||||||
8762|Ipswich Coal Measures|36941|6|Mentioned|p162|||||||||
8762|Ipswich Coal Measures|36954|6|Mentioned|p114|||||||||
8762|Ipswich Coal Measures|36961|6|Mentioned|Table 1|||||||||
8762|Ipswich Coal Measures|37065|6|Mentioned|p36|||||||||
8762|Ipswich Coal Measures|37109|6|Mentioned|p283|||||||||
8762|Ipswich Coal Measures|37111|5|Briefly described|p291|||||||||
8762|Ipswich Coal Measures|37112|6|Mentioned|p298|||||||||
8762|Ipswich Coal Measures|37122|5|Briefly described|Table 1|||||||||
8762|Ipswich Coal Measures|37135|6|Mentioned|p300|||||||||
8762|Ipswich Coal Measures|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|37375|6|Mentioned|Fig.1|||||||||
8762|Ipswich Coal Measures|37405|6|Mentioned|p30|||||||||
8762|Ipswich Coal Measures|37755|6|Mentioned|p79|||||||||
8762|Ipswich Coal Measures|37757|6|Mentioned|p17|||||||||
8762|Ipswich Coal Measures|37812|6|Mentioned|p657|||||||||
8762|Ipswich Coal Measures|38074|5|Briefly described|Table 1|||||||||
8762|Ipswich Coal Measures|38076|6|Mentioned|Table 3|||||||||
8762|Ipswich Coal Measures|38077|5|Briefly described|p30|||||||||
8762|Ipswich Coal Measures|38079|6|Mentioned|p46|||||||||
8762|Ipswich Coal Measures|38306|6|Mentioned|p509|||||||||
8762|Ipswich Coal Measures|38307|6|Mentioned|p519|||||||||
8762|Ipswich Coal Measures|38358|6|Mentioned|p3|||||||||
8762|Ipswich Coal Measures|38391|6|Mentioned|p10|||||||||
8762|Ipswich Coal Measures|38441|6|Mentioned|Map legend|Triassic|Triassic|||||||
8762|Ipswich Coal Measures|39079|5|Briefly described|p10|||||||||
8762|Ipswich Coal Measures|39218|6|Mentioned|p47|||Flora||||||
8762|Ipswich Coal Measures|39306|6|Mentioned|p425|||||||||
8762|Ipswich Coal Measures|39445|6|Mentioned|Table 9|||||||||
8762|Ipswich Coal Measures|39907|4|Described|p10|||Sedimentology||||||
8762|Ipswich Coal Measures|40245|6|Mentioned|p185|||||||||
8762|Ipswich Coal Measures|40434|6|Mentioned|p25|||||||||
8762|Ipswich Coal Measures|40479|6|Mentioned|p32|||||||||
8762|Ipswich Coal Measures|40579|6|Mentioned|Map legend|late Carnian|late Carnian|||||||
8762|Ipswich Coal Measures|40623|5|Briefly described|p7|||||||||
8762|Ipswich Coal Measures|40634|6|Mentioned|p33|||||||||
8762|Ipswich Coal Measures|40780|5|Briefly described|p6|||||||||
8762|Ipswich Coal Measures|41058|6|Mentioned|p51|||||||||
8762|Ipswich Coal Measures|41059|6|Mentioned|p168|||||||||
8762|Ipswich Coal Measures|41063|6|Mentioned|p45|||||||||
8762|Ipswich Coal Measures|41475|6|Mentioned|p72|||||||||
8762|Ipswich Coal Measures|41550|6|Mentioned|p491|||||||||
8762|Ipswich Coal Measures|41591|6|Mentioned|p15|||||||||
8762|Ipswich Coal Measures|41631|6|Mentioned|p4|||||||||
8762|Ipswich Coal Measures|41738|6|Mentioned|p168|||||||||
8762|Ipswich Coal Measures|41906|6|Mentioned|p44|||||||||
8762|Ipswich Coal Measures|42187|6|Mentioned|p319|||||||||
8762|Ipswich Coal Measures|42248|5|Briefly described|p397|||||||||
8762|Ipswich Coal Measures|42256|6|Mentioned|Fig.2 P243|||||||||
8762|Ipswich Coal Measures|42316|6|Mentioned|p5|||||||||
8762|Ipswich Coal Measures|42336|4|Described|p4|||||||||
8762|Ipswich Coal Measures|42370|6|Mentioned|p329|||||||||
8762|Ipswich Coal Measures|42405|6|Mentioned|Table 3 P.7|||||||||
8762|Ipswich Coal Measures|42463|6|Mentioned|Fig.3 P170|||||||||
8762|Ipswich Coal Measures|42474|6|Mentioned|p30|||Bundamba||||||
8762|Ipswich Coal Measures|42492|5|Briefly described|Table 2 P14|||||||||
8762|Ipswich Coal Measures|42525|5|Briefly described|Map legend|Late Triassic|Late Triassic|Includes the Kholo and Brassall Sub-Groups.||||||15-JUL-04
8762|Ipswich Coal Measures|42539|6|Mentioned|p183|||||||||
8762|Ipswich Coal Measures|42541|6|Mentioned|p203|||||||||
8762|Ipswich Coal Measures|42648|5|Briefly described|Fig.7 P43|||||||||
8762|Ipswich Coal Measures|42725|6|Mentioned|p24|||||||||
8762|Ipswich Coal Measures|42869|5|Briefly described|p33|||see also Fig.2 P32||||||
8762|Ipswich Coal Measures|42893|5|Briefly described|Fig.2 P7|||||||||
8762|Ipswich Coal Measures|43001|5|Briefly described|p121|||||||||
8762|Ipswich Coal Measures|43009|5|Briefly described|Map Legend|||||||||
8762|Ipswich Coal Measures|43072|6|Mentioned|p80|||||||||
8762|Ipswich Coal Measures|43076|5|Briefly described|p8|||||||||
8762|Ipswich Coal Measures|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
8762|Ipswich Coal Measures|43736|6|Mentioned|p9||Triassic|||||||
8762|Ipswich Coal Measures|43881|14|Not recorded|p13,25,28,74,79,80,|||p85(prox.anal.),99-102,134,146. Comparison with equivalent Nymboida Coal Measures in NSW.||||||
8762|Ipswich Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||||||||
8762|Ipswich Coal Measures|43895|4|Described|p114,115|||Important source for ceramics.||||||
8762|Ipswich Coal Measures|43905|14|Not recorded|p87||Triassic|Flora||||||
8762|Ipswich Coal Measures|43908|14|Not recorded|p6|||||||||
8762|Ipswich Coal Measures|43910|14|Not recorded|p2,4-5,7-8,10-13,|||p18-19, Fig.2||||||
8762|Ipswich Coal Measures|43911|14|Not recorded|p17,18|||||||||
8762|Ipswich Coal Measures|43914|14|Not recorded|p14|||||||||
8762|Ipswich Coal Measures|43918|14|Not recorded|p54,63,64|||||||||
8762|Ipswich Coal Measures|43919|14|Not recorded|p39|||||||||
8762|Ipswich Coal Measures|43920|14|Not recorded|p74|||||||||
8762|Ipswich Coal Measures|43921|14|Not recorded|p315,323|||Now "the entire Triassic sequence in the Brisbane area is correlated with the Ipswich Coal Measures."||||||
8762|Ipswich Coal Measures|43922|14|Not recorded|p324,325|||Middle or late Upper Triassic.||||||
8762|Ipswich Coal Measures|43923|6|Mentioned|p1|||||||||
8762|Ipswich Coal Measures|43924|14|Not recorded|p3|||||||||
8762|Ipswich Coal Measures|43984|14|Not recorded|p129,139|||||||||
8762|Ipswich Coal Measures|43993|14|Not recorded|p93-95,97,102|||||||||
8762|Ipswich Coal Measures|43995|14|Not recorded|p8,Tb.p10,26,28,29,||Middle Triassic|p38,42,43,54,57,60,Fig.16.||||||
8762|Ipswich Coal Measures|43997|14|Not recorded|p113|||||||||
8762|Ipswich Coal Measures|44026|14|Not recorded|p122,123||Triassic|||||||
8762|Ipswich Coal Measures|44029|14|Not recorded|p157,167|||||||||
8762|Ipswich Coal Measures|44030|14|Not recorded|p117,122,125,130|Late Triassic|Middle Triassic|||||||
8762|Ipswich Coal Measures|44075|14|Not recorded|p251|||||||||
8762|Ipswich Coal Measures|44076|14|Not recorded|p269,271|||||||||
8762|Ipswich Coal Measures|44091|14|Not recorded|p51,52||Triassic|||||||
8762|Ipswich Coal Measures|44093|5|Briefly described|p72|Late Triassic|Late Triassic|Geological Province: Ipswich Basin.||||||11-MAR-05
8762|Ipswich Coal Measures|44128|14|Not recorded|Tb.1,p426,430|||||||||
8762|Ipswich Coal Measures|44164|14|Not recorded|p26|||||||||
8762|Ipswich Coal Measures|44239|14|Not recorded|p278|||||||||
8762|Ipswich Coal Measures|44247|14|Not recorded|p3|||Chonchostracan (crustacean) found.||||||
8762|Ipswich Coal Measures|44250|14|Not recorded|p90|||See also Lexicon.||||||
8762|Ipswich Coal Measures|44382|14|Not recorded|p113|||||||||
8762|Ipswich Coal Measures|44384|14|Not recorded|p119|||||||||
8762|Ipswich Coal Measures|44387|14|Not recorded|p17|||||||||
8762|Ipswich Coal Measures|44428|14|Not recorded|p277|||||||||
8762|Ipswich Coal Measures|44430|14|Not recorded|p263,266-268|||Unconformably overlies Brisbane Metamorphics.||||||
8762|Ipswich Coal Measures|44510|2|Defined|p252-256,260-262,|||Figs.35,36. Overlain unconformably by Bundamba Group and Aberdare Conglomerate.||||||
8762|Ipswich Coal Measures|44542|2|Defined|p32||Middle Triassic|||||||
8762|Ipswich Coal Measures|44543|14|Not recorded|p27|||||||||
8762|Ipswich Coal Measures|44554|14|Not recorded|p295|||||||||
8762|Ipswich Coal Measures|44570|14|Not recorded|p677|||||||||
8762|Ipswich Coal Measures|44581|14|Not recorded|p346|||||||||
8762|Ipswich Coal Measures|44607|14|Not recorded|p36|||||||||
8762|Ipswich Coal Measures|44633|14|Not recorded|p2|||Includes Blackstone and Cooneana Formations.||||||
8762|Ipswich Coal Measures|44668|14|Not recorded|p60|||||||||
8762|Ipswich Coal Measures|44678|14|Not recorded|Fig.1|||||||||
8762|Ipswich Coal Measures|44687|5|Briefly described|p221|Triassic|Triassic|Described by Bryan & Jones (1960) as sandstone, shale and conglomerate with minor coal seams, unconformably overlying the Neranleigh-Fernvale "Group".||||||21-MAR-13
8762|Ipswich Coal Measures|44703|14|Not recorded|Map|||||||||
8762|Ipswich Coal Measures|44705|14|Not recorded|p1,15|||||||||
8762|Ipswich Coal Measures|44706|14|Not recorded|p413-415|||||||||
8762|Ipswich Coal Measures|44707|14|Not recorded|p1,3,5|||||||||
8762|Ipswich Coal Measures|44708|14|Not recorded|p19,Sheet 2,section||Middle Triassic|||||||
8762|Ipswich Coal Measures|44716|14|Not recorded|p74,75,105|||||||||
8762|Ipswich Coal Measures|44734|14|Not recorded|p7-11|||||||||
8762|Ipswich Coal Measures|44771|14|Not recorded|p1,3|||||||||
8762|Ipswich Coal Measures|44772|14|Not recorded|p3|||||||||
8762|Ipswich Coal Measures|44774|6|Mentioned|p30||Middle Triassic|||||||
8762|Ipswich Coal Measures|44775|4|Described|p7,9,map 2||Triassic|||||||
8762|Ipswich Coal Measures|44776|14|Not recorded|p1,3||Middle Triassic|||||||
8762|Ipswich Coal Measures|44777|14|Not recorded|p55|||||||||
8762|Ipswich Coal Measures|44783|14|Not recorded|p2-6,9-12,16-20|||Brisbane District.||||||
8762|Ipswich Coal Measures|44786|14|Not recorded|p193-202||Permian|||||||
8762|Ipswich Coal Measures|44789|14|Not recorded|p18,19||Triassic|Unconformably overlies Bunya Phyllites||||||
8762|Ipswich Coal Measures|44801|14|Not recorded|p25|||||||||
8762|Ipswich Coal Measures|44814|14|Not recorded|p485||Middle Triassic|De Jersey: Middle-Late Triassic.||||||
8762|Ipswich Coal Measures|44828|14|Not recorded|p14|||||||||
8762|Ipswich Coal Measures|44884|14|Not recorded|p2|||||||||
8762|Ipswich Coal Measures|44913|14|Not recorded|p57,Fig.3,68|||||||||
8762|Ipswich Coal Measures|45110|6|Mentioned|p80|||||||||
8762|Ipswich Coal Measures|48917|4|Described|p9|||See also correlation P7||||||
8762|Ipswich Coal Measures|48920|6|Mentioned|p90|||||||||
8762|Ipswich Coal Measures|48928|6|Mentioned|p2|||See also P10||||||
8762|Ipswich Coal Measures|60079|5|Briefly described|Map Legend|||Equivalent to Evans Head and Red Cliff Coal Measures.||||||
8762|Ipswich Coal Measures|60281|5|Briefly described|p28, Fig.18 App1|Late Triassic|Early Triassic|Overlie the Nymboida Coal Measures; underlie the Raceview Formation.  Geological Province: Ipswich Basin.||||||20-JAN-05
8762|Ipswich Coal Measures|60726|5|Briefly described|p1-4, throughout text.|Late Triassic|Late Triassic||||Mount Crosby, Blackstone Formations.|||
8762|Ipswich Coal Measures|60991|6|Mentioned|p46|||||||||
8762|Ipswich Coal Measures|60993|5|Briefly described|p5, p6 Fig. 2|Carnian (Late Triassic)|Carnian (Late Triassic)|Unconformably overlain by the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin. Equivalent to Evans Head Coal Measures. ||||||
8762|Ipswich Coal Measures|60995|5|Briefly described|p52 Tb. 1|Late Triassic|Late Triassic|Includes Redcliff and Evans head Coal Measures. Geological Province: Clarence-Moreton Basin. Coal Measures is written as C.M. in text.  See also p51 Fig. 3 (equivalents mentioned). ||||||
8762|Ipswich Coal Measures|60996|5|Briefly described|p73|||Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|60997|5|Briefly described|p140 Fig. 2|||Overlain by the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|61002|5|Briefly described|p198, p202|Late Triassic|Late Triassic|Conformably overlie Chillingham Volcanics. Age is Carnian. Geological Province: Ipswich Basin.See also p199 Fig. 3. ||||||
8762|Ipswich Coal Measures|61004|5|Briefly described|p230, p232 Fig. 2|Triassic|Triassic|Contains minor component inertinite.   Geological Province: Clarence-Moreton Basin.||||||
8762|Ipswich Coal Measures|61005|5|Briefly described|p239, p242|Late Triassic|Late triassic|Geological Province: Ipswich Basin.  See also p248.||||||
8762|Ipswich Coal Measures|61006|5|Briefly described|p278 Fig. 2|Triassic|Triassic|Contain coal and carbonaceous shale. Underlie the Clarence-Moreton Basin. ||||||
8762|Ipswich Coal Measures|61310|4|Described|p16, p11 Fig. C2|Late Triassic|Late Triassic|Considered to have both hydrocarbon source and reservoir potential. Overlie Nymboida Coal Measures and Chillingham Volcanics. Geological Province: Clarence-Moreton Basin. Equivalents are Red Cliff and Evans Head Coal Measures.||||||
8762|Ipswich Coal Measures|61772|6|Mentioned|p129, p130 Fig. 5||Late Triassic|Contains tuffs.||||||24-SEP-08
8762|Ipswich Coal Measures|63117|6|Mentioned|p158, p162|||Contains Ginkgoites fossils.||||||
8762|Ipswich Coal Measures|63979|6|Mentioned|p31|||In south eastern Queensland.||||||07-FEB-11
8762|Ipswich Coal Measures|64298|6|Mentioned|p122|||||||||
8762|Ipswich Coal Measures|64665|5|Briefly described|p53 Fig.2, p57.|Late Triassic|Late Triassic|Ipswich Basin. First coal mined in Queensland. Up to 1200 m thick. Dominantly bright coal with some interbanded bright and dull coal; ash content generally high; rank is high volatile bituminous; predominantly thermal, some local coking coal in the north.|||Includes Kholo and Brassall Subgroups.|Is unconformably overlain by Bundamba Group.||
8762|Ipswich Coal Measures|65003|5|Briefly described|p7|||Of Clarence-Moreton Basin.||||Unconformably overlain by the Bundamba Group.|Shale, conglomerate, sandstone, coal, siltstone, basalt and tuff.|30-MAR-12
8762|Ipswich Coal Measures|67402|4|Described|p186, p205, p209, p222-p225|Late Triassic|Late Triassic|Clarence-Moreton Basin. Maximum thickness of 1200m.  |||Includes the Kholo and Brassall Subgroups.|Overlies the Neara Volcanics.|Conglomerates, sandstones, shales, coals and minor volcanics.|
8762|Ipswich Coal Measures|68008|6|Mentioned|p220, p261|Late Triassic|Late Triassic|||||Correlated with Callide Coal Measures.||
8762|Ipswich Coal Measures|68327|5|Briefly described|Map legend.|Triassic|Triassic||||||Conglomerate, sandstone, shale, tuff, coal seams.|
8762|Ipswich Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Ipswich Basin.||||||
8762|Ipswich Coal Measures|68579|6|Mentioned|p221, 222|||||||Overlain unconformably by Redbank Plains Formation.||26-APR-13
8762|Ipswich Coal Measures|68679|5|Briefly described|p321, p388, p391-395, p398-399, p435|Late Triassic|Late Triassic|Ipswich Basin, northern New England Orogen. Appears as Ipswich Basin Coal Measures on p321. Represents a thermal relaxation phase. ~1200m thick. Previously considered equivalent to Nymboida Coal Measures, but contradicted by macrofloral and radiometric dating. Carnian-Norian age.|||Kholo and Brassall Subgroups.|Unconformably overlies Neranleigh-Fernvale beds. Is overlain unconformably by the Woogaroo Subgroup (Bundamba Group). Equivalent to the Evans Head and Red Cliff, Coal Measures.||
8762|Ipswich Coal Measures|69297|6|Mentioned|p370, p386, p487 fig 5.38, p488|Lower Jurassic|Middle Triassic|Clarence-Moreton Basin. Gas prone source rocks are present. |||||Coal and mudstones.|
8762|Ipswich Coal Measures|69594|5|Briefly described|p519, p543, p545-546|Late Triassic|Late Triassic|Ipswich Basin.||||Overlies Chillingham Volcanics and Brisbane Tuff. Is overlain unconformably by Bundamba Group.||
8762|Ipswich Coal Measures|69599|5|Briefly described|p610|||Offshore Ipswich Basin. A 277m succession of carbonaceous sediments with several igneous intervals, intersected in APS Matjara 1 drilled 15km off Moreton Island, is interpreted as this unit. The igneous rocks compared with the Brisbane Tuff.||||||
8762|Ipswich Coal Measures|72297|5|Briefly described|p698, p700|Triassic|Triassic|Ipswich Basin. Mining ceased in 2003 after 160 years of continuous mining.|||Tivoli Formation.||High-volatile, low-sulfur bituminous coals.|
8762|Ipswich Coal Measures|73294|6|Mentioned|p1014, p1006|late Triassic|late Triassic|Late Triassic Craterisporites rotundus spore-pollen zone age. Correlated with the Brisbane Tuff. Misspelt as Ipswich Coal measures p1006.||||||
8762|Ipswich Coal Measures|73570|6|Mentioned|p912 Fig.2|||||||Underlies Laytons Range Conglomerate||
8777|Ironbark Creek Arenite|721|5|Briefly described|Map legend|Early Permian|Early Permian|Massive fossiliferous quartzose and lithic sandstone.||||||
8777|Ironbark Creek Arenite|22857|4|Described|p506 App.1 Tb.A1.8|Early Permian|Early Permian|Massive fossiliferous quartzose and lithic sandstone. Max. thickness: 30m. Geological Province: Tamworth Forearc Basin.||||||
8777|Ironbark Creek Arenite|32683|2|Defined|p204|Permian|Permian|See also p207.||||||27-SEP-06
8777|Ironbark Creek Arenite|39331|6|Mentioned|Table 10-1|||||||||
8777|Ironbark Creek Arenite|41009|6|Mentioned|p5|||See also Fig.2||||||
8777|Ironbark Creek Arenite|43091|5|Briefly described|Map legend|||||||||
8777|Ironbark Creek Arenite|44093|5|Briefly described|p226 App. 1|Early Permian|Early Permian|Clastic sediments. Geological Province: New England Fold Belt.||||||
8777|Ironbark Creek Arenite|47056|6|Mentioned|Fig.2 P523|||||||||
8777|Ironbark Creek Arenite|68005|5|Briefly described|p49 Fig.3-M, p57, p137, p170.|Sakmarian|Sakmarian|Tamworth Belt. One of a number of units that occur in narrow fault slivers immediately west of the Peel Fault.|||||Massive fossiliferous quartzose and lithic sandstone.|
8777|Ironbark Creek Arenite|68822|6|Mentioned|p342|||||||||
8780|Irondale Coal|22578|6|Mentioned|p398|||||||||
8780|Irondale Coal|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Charbon Subgroup (Illawarra Coal Measures). Max. thickness: 3m. Geological Province: Sydney Basin.||||||
8780|Irondale Coal|38603|6|Mentioned|p79|||||||||
8780|Irondale Coal|39232|4|Described|p109|||||||||
8780|Irondale Coal|40256|6|Mentioned|p305|||||||||
8780|Irondale Coal|40806|2|Defined|p154|Permian|Permian|Prob. Permian||||||
8780|Irondale Coal|41226|6|Mentioned|Fig.6|||||||||
8780|Irondale Coal|42657|5|Briefly described|p78|||||||||
8780|Irondale Coal|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
8780|Irondale Coal|68004|5|Briefly described|p60 Table 6, p61, p157.|Late Permian|Late Permian|Western Coalfield. A thin, persistent unit. Correlated with Coolah seam.||Unit in Charbon Subgroup.||Is overlain by Newnes Formation.|Bright coal, generally brighter and thicker towards the top; two or three stone layers.|
8785|Irondoon Granodiorite|22876|5|Briefly described|p18 Table 3|Late Silurian|Late Silurian|||||||
8785|Irondoon Granodiorite|22877|5|Briefly described|map|Silurian|Silurian|Kuark Metamorphic Complex Supersuite. G32. Biotite granodiorite.||||||26-OCT-04
8785|Irondoon Granodiorite|22878|4|Described|p87|||||||||
8785|Irondoon Granodiorite|22879|5|Briefly described|map|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite granodiorite: dark grey, medium grained, strongly foliated; dyke like bodies; abundant elongate mafic inclusions.||||||01-OCT-04
8785|Irondoon Granodiorite|22880|5|Briefly described|Map Legend|Silurian|Silurian|Of the Kuark Metamorphic Complex. Biotite granodiorite: dark grey, medium grained, strongly foliated; dyke like bodies; abundant elongate mafic inclusions.||||||01-OCT-04
8785|Irondoon Granodiorite|22881|5|Briefly described|Map legend|Silurian|Silurian|Of the Kuark Metamorphic Complex Supersuite. Biotite granodiorite: Moderately magnetic (40-60 nT). High K, Th and U.||||||06-OCT-04
8785|Irondoon Granodiorite|23309|6|Mentioned|p433 App 1|||G32 I-Type.||||||
8785|Irondoon Granodiorite|30574|6|Mentioned|p9|||||||||
8785|Irondoon Granodiorite|30938|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
8785|Irondoon Granodiorite|40328|4|Described|p207|||||||||
8785|Irondoon Granodiorite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Berridale Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
8787|Irwin Creek Breccia|36220|5|Briefly described|p95|||||||||
8795|Isaacs Formation|29728|6|Mentioned|p398|||||||||
8795|Isaacs Formation|30074|6|Mentioned|p28|||||||||
8795|Isaacs Formation|30772|6|Mentioned|p4|||Fauna||||||
8795|Isaacs Formation|32094|6|Mentioned|p385|||||||||
8795|Isaacs Formation|32379|6|Mentioned|p5|||||||||
8795|Isaacs Formation|32868|6|Mentioned|p209|||||||||
8795|Isaacs Formation|34072|6|Mentioned|Fig.4.5|||Carb. Fossils||||||
8795|Isaacs Formation|34085|6|Mentioned|Cor.chart|||Stephanian||||||
8795|Isaacs Formation|34086|6|Mentioned|p264|||||||||
8795|Isaacs Formation|34168|5|Briefly described|p254|||Carboniferous||||||
8795|Isaacs Formation|34238|6|Mentioned|p5|||||||||
8795|Isaacs Formation|34239|6|Mentioned|p264|||Non marine portion contains microflora||||||
8795|Isaacs Formation|42547|6|Mentioned|p122|||||||||
8795|Isaacs Formation|43432|14|Not recorded|p208||Carboniferous|Part of Crawford Formation. Ref. to Campbell 1961||||||
8795|Isaacs Formation|43447|14|Not recorded|Table 1&2,p10,13,14||Carboniferous|||||||
8795|Isaacs Formation|43451|14|Not recorded|Map Legend||Carboniferous|Included in Crawford Formation||||||
8795|Isaacs Formation|43479|14|Not recorded|p161||Carboniferous|||||||
8795|Isaacs Formation|44360|14|Not recorded|p34|||Upper Kuttung Series.||||||
8795|Isaacs Formation|44372|6|Mentioned|p48|||||||||
8795|Isaacs Formation|44859|14|Not recorded|p68|||Peruvispira kuttungensis, Campbell.||||||
8795|Isaacs Formation|45097|5|Briefly described|p18|||See P24. Correlation chart||||||
8795|Isaacs Formation|46849|6|Mentioned|Fig. 2|||||||||
8795|Isaacs Formation|48924|6|Mentioned|p5||Late Carboniferous|U.Carb. See also P6-9,11,15,18.||||||
8801|Isismurra Formation|22736|6|Mentioned|p629|Visean|Visean|||||||
8801|Isismurra Formation|22857|4|Described|p508 App.1 Tb.A1.8|Visean|Tournaisian|Lithic and lithofeldspathic arenite with 3 thin ignimbrite units. Disconformably overlies Waverley and Dangarfield Formations. Max. thickness: 2250m. Geological Province: Tamworth Forearc Basin.||||||
8801|Isismurra Formation|24348|5|Briefly described|p133|Carboniferous|Carboniferous|||||||
8801|Isismurra Formation|24603|6|Mentioned|p898|||Geological Province: Tamworth Belt.||||||
8801|Isismurra Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
8801|Isismurra Formation|31918|4|Described|p42|||Palaeomagnetic results Table 4 & Fig.6.||||||
8801|Isismurra Formation|32482|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
8801|Isismurra Formation|32529|4|Described|p198|||Refers Manser (1968)||||||
8801|Isismurra Formation|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
8801|Isismurra Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
8801|Isismurra Formation|32866|6|Mentioned|Fig.4|||||||||
8801|Isismurra Formation|32869|4|Described|p167|||Depositional environment. See also P168 & Figs. 2, 3B||||||
8801|Isismurra Formation|35245|6|Mentioned|p21|||||||||
8801|Isismurra Formation|35803|6|Mentioned|p321|||||||||
8801|Isismurra Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
8801|Isismurra Formation|36528|6|Mentioned|p177|||||||||
8801|Isismurra Formation|39214|5|Briefly described|p29|||||||||
8801|Isismurra Formation|40883|6|Mentioned|p5|||||||||
8801|Isismurra Formation|41279|6|Mentioned|Fig.2|||||||||
8801|Isismurra Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In Barrington Tops district.||||||16-DEC-04
8801|Isismurra Formation|41542|6|Mentioned|p234|||||||||
8801|Isismurra Formation|42547|4|Described|p28|Visean||||||||
8801|Isismurra Formation|43407|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition) Middle Carboniferous||||||
8801|Isismurra Formation|43417|4|Described|Map Legend||Late Carboniferous|||||||
8801|Isismurra Formation|43576|6|Mentioned|Fig.1,p348|||||||||
8801|Isismurra Formation|43792|5|Briefly described|p363||Carboniferous|||||||
8801|Isismurra Formation|44093|5|Briefly described|p228 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
8801|Isismurra Formation|44244|2|Defined|p32-34|Visean|Visean|Includes Ayr Conglomerate, Native Dog, Martins Creek, Lambs Valley Ignimbrite, Curra Keith Tongue and Oakfields Tongue Members.  Disconformably overlies Waverley and Dangarfield Fms; disconformably underlies Mount Johnstone Fm. Max. thickness: 2200m.||||||19-AUG-04
8801|Isismurra Formation|45088|3|Fully described|p42|||See also Plate 2 & P9||||||
8801|Isismurra Formation|45097|5|Briefly described|p15|||See also P18, 25 & correlation chart.||||||
8801|Isismurra Formation|46803|6|Mentioned|Fig. 3|||||||||
8801|Isismurra Formation|50099|5|Briefly described|p9-10|Early Carboniferous|Early Carboniferous|Dominantly volcanogenic zeolitic lithic sandstone, conglomerate, minor siltstone and mudstone. Overlain by Mount Johnstone Formation. Max. thickness: >2200m. Geological Province: Tamworth Belt/New England Orogen.||||||
8801|Isismurra Formation|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Rouchel Block.  Includes: Ayr Conglomerate Member, Native Dog Member, Curra Keith Tongue, Oakfields Tongue.  Overlies: Wolooma Formation.||||||
8801|Isismurra Formation|60299|5|Briefly described|p209|Early Carboniferous|Early Carboniferous|Geological Province: Rouchel and Gresford Blocks||||||
8801|Isismurra Formation|61768|6|Mentioned|p86|||||||||
8801|Isismurra Formation|62095|1|Redefined|p280 Appdx.|Early Carboniferous|Early Carboniferous|Parts are now mapped as Merlewood Formation. Overlain by Currabubula Formation. Thickness in type section: 620m; max. thickness: 670m. Age is Visean. Geological  Province: Rouchel block/Tamworth Belt See also Plate 1, p250, p251, p264.||||||31-JAN-08
8801|Isismurra Formation|63025|5|Briefly described|p1052 Fig. 1|Visean|Visean|Geological Province: Gresford and Rouchel Blocks, New England Orogen.||||||
8801|Isismurra Formation|63832|5|Briefly described|p131 fig 2|Visean|Visean|Rouchel block, Southern New England Fold Belt.|||||Thick succession of glacial diamictite and poorly sorted conglomerate with striated and faceted clasts.|13-DEC-17
8801|Isismurra Formation|64631|6|Mentioned|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt, Rouchel Block. Some radiometric age control within unit. ||||||
8801|Isismurra Formation|65107|5|Briefly described|p275, 276 Fig 4 p279, 282|Visean|Visean|Author uses example of the Curra Keith Tongue (it is not clear is this is a unit or a place), Age: 342.1-3.2 Ma from SHRIMP U-Pb zircons. This formation also helps to constrain the older "eastward" loop of the New England Orogen (NEO) paleopole path.||||||
8801|Isismurra Formation|68003|5|Briefly described|p32 Fig.3-h, p136. |Visean|Visean|Tamworth Belt (South); New England Fold Belt. Coeval with Merlewood Formation.|||Includes Native Dog Member and Ayr Conglomerate [Member].|Overlies Waverly and Dangarfield Formations.|Coarse lithic sandstone and conglomerate; welded and nonwelded tuffs; red, purple or beige ignimbrites, welded or unwelded.|
8801|Isismurra Formation|68005|5|Briefly described|p49 Fig.3-M, p56, p170.|Visean|Visean|Rouchel Block, Tamworth Belt. A marine to terrestrial transition sequence.||||Overlies Waverly Formation.|Limestone, andesite, dacite, conglomerate, sandstone and siltstone with rare coal.|
8801|Isismurra Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Rouchel Block, Tamworth Belt.||||||
8801|Isismurra Formation|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.|||Includes the Martins Creek Ignimbrite Member, Native Dog Member, Curra Keith Tongue and the Oakfields Tongue.|||
8801|Isismurra Formation|71628|6|Mentioned|p6: 18, 22|||||||Is intruded by Barrington River Granodiorite.||
8801|Isismurra 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.|
8801|Isismurra Formation|73487|6|Mentioned|p583|||||||||
8807|Ivanhoe Sandstone Member|39232|6|Mentioned|Table 2|||||||||
8807|Ivanhoe Sandstone Member|40806|6|Mentioned|p154|||||||||
8807|Ivanhoe Sandstone Member|42657|6|Mentioned|Table 1 P74|||||||||
8810|Iventure Ignimbrite Member|24603|5|Briefly described|p868|||Of the Currabubula Formation.  Relatively coarse-grained, crystal-rich, lithic, variably welded ignimbrite.  Geological Province: Tamworth Belt.||||||
8810|Iventure Ignimbrite Member|41800|4|Described|p495|||Reserved as Iventure Ignimbrite||||||
8810|Iventure Ignimbrite Member|43718|6|Mentioned|Table 8.2,p129|||||||||
8810|Iventure Ignimbrite Member|50613|5|Briefly described|p213, p220 App. 1|Namurian|Namurian|Of the Currabubula Formation (Werrie Syncline).  Synonymous with Yarralumba Ignimbrite Member -see p230 Appendix 1.||||||22-FEB-05
8810|Iventure Ignimbrite Member|62095|5|Briefly described|p251|Carboniferous|Carboniferous|Of the Currabubula Formation. Geological Province: Werrie block/Tamworth Belt.  See also Plate 1.||||||
8810|Iventure Ignimbrite Member|65902|5|Briefly described|p195 Fig.2, p198, p202-4, p203 Fig.7|Late Carboniferous|Late Carboniferous|Of Currabubula Formation. Also occurs within Willuri Formation, and is thus useful for correlation between Werrie Syncline and Clifton-Carroll Block. Andesitic flow.||||||09-MAR-12
8810|Iventure Ignimbrite Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Ignimbrite.|
8810|Iventure Ignimbrite Member|68005|6|Mentioned|p57, p140.|Late Carboniferous|Late Carboniferous|||Unit in Currabubula Formation.||||
8829|Jackson Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Pink Granite. BMR map symbol: gij.||||||
8829|Jackson Granite|23548|5|Briefly described|p533.|||||||||
8829|Jackson Granite|24266|6|Mentioned|p1486|||Geological Province: Lachlan Fold Belt. Of the Boggy Plain Supersuite.||||||
8829|Jackson Granite|29456|6|Mentioned|p424|||||||||
8829|Jackson Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
8829|Jackson Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
8829|Jackson Granite|31013|6|Mentioned|p3|||Lower Devonian||||||
8829|Jackson Granite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
8829|Jackson Granite|33325|6|Mentioned|p18|||?early M.Dev.||||||
8829|Jackson Granite|33959|6|Mentioned|p233|||||||||
8829|Jackson Granite|36050|6|Mentioned|p399|||||||||
8829|Jackson Granite|36441|5|Briefly described|map legend|Pragian|Lochkovian|Intrusive. Boggy Plain I-type Suite. Granite, aplite, adamellite. BMR map code: Dgj.||||||
8829|Jackson Granite|36443|5|Briefly described|map legend|Pragian|Pragian|Of Boggy Plain I-type Suite. Intrusive. Granite, aplite, adamellite. BMR map code: Dgj.||||||
8829|Jackson Granite|39409|6|Mentioned|Table XVII|||||||||
8829|Jackson Granite|39800|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Late Middle Devonian.||||||
8829|Jackson Granite|40328|4|Described|p207|||||||||
8829|Jackson Granite|40882|6|Mentioned|p26|||||||||
8829|Jackson Granite|42726|5|Briefly described|map legend|Silurian||292.  Of the Jackson Suite (Boggy Plain Supersuite).  Formal name not intended.||||||08-FEB-05
8829|Jackson Granite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|glp4||||||
8829|Jackson Granite|45003|14|Not recorded|p15|||See also Lexicon||||||
8829|Jackson Granite|45147|2|Defined|M279|Early Devonian|Early Devonian|||||||
8829|Jackson Granite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
8829|Jackson Granite|68592|6|Mentioned|p1411|||Is very similar mineralogically and chemically to Burrinjuck Granite.||Unit in Boggy Plain Supersuite.||||
8829|Jackson Granite|71206|6|Mentioned|p384|||Lachlan Fold Belt.||Boggy Plain Supersuite.|||I-type granite.|
8837|Jagungal Volcanics|36512|6|Mentioned|p26|||||||||
8837|Jagungal Volcanics|44092|5|Briefly described|map legend|Early Ordovician|Early Ordovician|Ovj1||||||
8837|Jagungal Volcanics|60078|6|Mentioned|Map Legend|Middle Ordovician|Middle Ordovician|||||||15-JUL-04
8837|Jagungal Volcanics|63289|6|Mentioned|p367|||||||||07-FEB-11
8837|Jagungal Volcanics|68822|6|Mentioned|p335|||||||||
8843|Jamberoo Sandstone Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
8843|Jamberoo Sandstone Member|22488|5|Briefly described|p841|||||||||
8843|Jamberoo Sandstone Member|22578|6|Mentioned|p394|||Of Broughton Formation.||||||04-DEC-08
8843|Jamberoo Sandstone Member|22857|5|Briefly described|p532 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Broughton Formation (Shoalhaven Group). Geological Province: Sydney Basin.||||||
8843|Jamberoo Sandstone Member|23544|5|Briefly described|Table 1 p360.|||Of the Broughton Formation.||||||04-DEC-08
8843|Jamberoo Sandstone Member|29900|6|Mentioned|Table 2|||||||||
8843|Jamberoo Sandstone Member|29901|4|Described|Table 1|||||||||
8843|Jamberoo Sandstone Member|31128|6|Mentioned|Table 1|||||||||
8843|Jamberoo Sandstone Member|36220|6|Mentioned|p37|||See also Table 1.||||||
8843|Jamberoo Sandstone Member|38690|5|Briefly described|p291|||Formerly Jamberoo Tuffs, and Jamberoo Sandstone.||||||04-DEC-08
8843|Jamberoo Sandstone Member|39308|6|Mentioned|p518|||||||||
8843|Jamberoo Sandstone Member|39309|5|Briefly described|Table 7.1|||||||||
8843|Jamberoo Sandstone Member|40519|6|Mentioned|Fig.2|||||||||
8843|Jamberoo Sandstone Member|45090|6|Mentioned|p171|||Refers Hanlon et al. (1953)||||||
8843|Jamberoo Sandstone Member|67500|4|Described|p12 Tb.1, p16|Late Permian|Late Permian|Between 55-155m thick. Stated to occur stratigraphically between the Dapto and Cambewarra Latite Members [of Gerringong Volcanics]. Includes marine fossils and burrows, and palaeosols.||Of the Broughton Formation and Gerringong volcanic facies.|||Red and green, volcaniclastic sandstones, with interbedded conglomerates, common marine fossils, Harvey paleosols in the upper part.|05-APR-13
8843|Jamberoo Sandstone Member|71115|5|Briefly described|p180, 182, 188|Permian|Permian|Southern Sydney Basin.||Broughton Formation.||Overlies Bumbo Latite Member. Is overlain by Dapto Latite Member.||
8843|Jamberoo Sandstone Member|71542|6|Mentioned|p25|Late Permian|Late Permian|Of southern Sydney Basin.||Of Broughton Formation.||||20-OCT-21
8843|Jamberoo Sandstone Member|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.||Broughton Formation.||Overlies Bumbo Latite Member.||
8889|Jaunter Tuff|40622|6|Mentioned|p29|||||||||
8889|Jaunter Tuff|73582|5|Briefly described|p104|||Informal name by Shiels (1959). Appears in text as 'Jaunter Tuff'. Exposed in lower car park and behind Caves House.|||||An andesitic volcanic unit.|
8912|Jenolan Caves Limestone|22857|4|Described|p478 App.1 Tb.A1.6|Pridoli|Pridolian|Of the Mumbil Group. Limestone, shales. Max. thickness: 168m. Geological Province: Murruin Basin. ||||||
8912|Jenolan Caves Limestone|30109|4|Described|p55|||Upper Silurian age.||||||
8912|Jenolan Caves Limestone|32672|6|Mentioned|p672|||||||||
8912|Jenolan Caves Limestone|37727|4|Described|p64|||Also called Caves Limestone||||||
8912|Jenolan Caves Limestone|40328|3|Fully described|p183|||||||||
8912|Jenolan Caves Limestone|40622|6|Mentioned|p29|||||||||
8912|Jenolan Caves Limestone|41863|4|Described|p7|||||||||
8912|Jenolan Caves Limestone|42414|4|Described|p60|||||||||
8912|Jenolan Caves Limestone|42939|6|Mentioned|p591|||||||||
8912|Jenolan Caves Limestone|61894|6|Mentioned|p180 |||||||||
8912|Jenolan Caves Limestone|62368|5|Briefly described|p377, p388 Fig.7, p403|Late Silurian|Late Silurian|Overlain by the "Jenolan beds". Max. thickness: 265m. See also p391 Fig.10||||||
8912|Jenolan Caves Limestone|73582|5|Briefly described|p99, 101, 103-108, 110-114, 118-121|Early Silurian|Early Silurian|See also p123-124, 126. Chalker (1971). Goulburn Basin. Initially 'Jenolan Cave Limestone' of Etheridge (1894). Assigned a Ludlovian age by Pickett (1981, 1982); here given a mid-Wenlockian age on basis of conodonts. Crops out along an 11 km N-S linear belt. Steeply dipping. Up to 350m thick. Paleozoic and subsequent episodes of cave development discussed in detail.||||Is overlain conformably by Inspiration Point Limestone and locally by Shoalhaven Group unconformably. Is faulted against Campbells Group.|Light to dark grey bioclastic limestone, massive to bedded; occasional mudstone lenses and minor dolomite. Locally abundantly fossiliferous (pentamerid brachiopods).|05-FEB-23
8926|Jerilderie Formation|22773|5|Briefly described|Fig24.5p350|Middle Triassic|Middle Triassic|||||||
8926|Jerilderie Formation|22857|5|Briefly described|p277, p540 App.1 Tb.A1.10|Middle Triassic|Middle Triassic|Conglomerate, sandstone, mudstone. Max. thickness: 220m. Geological Province: Oaklands Basin, Tasman Epicratonic Province. See also p350 Fig. 24.5. ||||||
8926|Jerilderie Formation|22860|5|Briefly described|p277||Middle Triassic|||||||
8926|Jerilderie Formation|22887|5|Briefly described|Fig.5 p12|Middle Triassic|Middle Triassic|||||||
8926|Jerilderie Formation|22893|6|Mentioned|fig4 p9|||||||||
8926|Jerilderie Formation|35498|2|Defined|p145|Triassic|Triassic|||||||
8926|Jerilderie Formation|35503|6|Mentioned|p202|||Defined in Standing Committee Coalfield Geology NSW (1978)||||||
8926|Jerilderie Formation|38293|4|Described|p22|||||||||
8926|Jerilderie Formation|40520|6|Mentioned|Fig.5|||||||||
8926|Jerilderie Formation|42966|3|Fully described|p64|||||||||
8926|Jerilderie Formation|43841|4|Described|8||Triassic|Unconformably overlies Coorabin Coal Measures||||||
8926|Jerilderie Formation|44093|5|Briefly described|p245 App. 1|Middle Triassic|Middle Triassic|||||||
8926|Jerilderie Formation|49038|6|Mentioned|p23|||||||||
8926|Jerilderie Formation|49040|6|Mentioned|p8|||||||||
8926|Jerilderie Formation|61314|5|Briefly described|p129|Middle Triassic|Early Triassic|Fluvial sandstone, conglomerate and mudstone. Overlies the Coorabin Coal Measures. Geological Province: Oaklands Basin, Murray Basin.||||||
8926|Jerilderie Formation|69798|5|Briefly described|p4, p9, p11, p13-16|Triassic|Triassic|Oaklands Basin. Seismic profiles. Very low-amplitude high-frequency reflections.||||Disconformably overlies Coorabin Coal Measures.||
8926|Jerilderie Formation|70125|5|Briefly described|p391, p396-397|Middle Triassic|Middle Triassic|Oaklands Basin. 220m of dominantly fluvial sand deposits.|242 Ma.|||Overlies Coorabin Coal Measures. Coeval with Hawkesbury Sandstone (same palynozone).||
8937|Jerrawa beds|23245|5|Briefly described|p134||Early Silurian|||||||
8937|Jerrawa beds|42560|6|Mentioned|p55|||Variation on Jerrawa Beds. Ordovician.||||||
8938|Jerricho Limestone|34692|5|Briefly described|p185|||Refers Binns(1958)||||||
8950|Jews Creek Volcanics|22857|4|Described|p456 App.1 Tb.1A1.6|Pridolian|Pridolian|Of the Goonigal Group. Pyroxene andesites, green and grey cherts, vitric tuff. Max. thickness: 215m. Geological Province: Cowra Trough.||||||
8950|Jews Creek Volcanics|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|of Goonigal Group.||||||
8950|Jews Creek Volcanics|23170|2|Defined|p111||Ludlow|of Goonigal Group.||||||
8950|Jews Creek Volcanics|23214|3|Fully described|p153|Ludlow|Ludlow|Of Goonigal Group. Intruded by Gumble Granite. Max. thickness 215m.  Overlying unit: Burgoon Formation, underlying unit: Mackeys Creek Shale.||||||
8950|Jews Creek Volcanics|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
8950|Jews Creek Volcanics|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
8950|Jews Creek Volcanics|40328|3|Fully described|p106|||||||||
8950|Jews Creek Volcanics|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
8950|Jews Creek Volcanics|43494|5|Briefly described|p21-22||Silurian|Lowermost unit of the Goonigal Group. Conformably overlie Mackeys Creek Shale; conformably overlain by Burgoon Formation.||||||16-MAR-06
8950|Jews Creek Volcanics|43640|5|Briefly described|Map Legend||Silurian|||||||
8950|Jews Creek Volcanics|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|of Goonigal Group.||||||
8950|Jews Creek Volcanics|70297|5|Briefly described|map legend|Silurian|Silurian|||Burgoon Formation||||
8971|Jindabyne Suite|22719|6|Mentioned|p485|||||||||
8971|Jindabyne Suite|22779|5|Briefly described|p 172|||||||||
8971|Jindabyne Suite|22815|4|Described|p49|Early Devonian|Silurian|||||||
8971|Jindabyne Suite|23439|5|Briefly described|p124 fig.1|||||||||
8971|Jindabyne Suite|23548|5|Briefly described|p533.|||||||||
8971|Jindabyne Suite|23549|4|Described|p517 Fig 2, p524|||Of the Kosciuszko Batholith. Comprises 8 plutons. Includes the Jindabyne Tonalite. I-Type granite. Geological Province: Lachlan Fold Belt.  See also p516 and p522||||||05-APR-05
8971|Jindabyne Suite|24222|5|Briefly described|p11, p17-18|||Chemistry of samples reported. Comprises 9 plutons of tonailte with minor granodiorite and quartz diorite.  Geological Province: Kosciusko Batholith, Lachlan Fold Belt.||||||
8971|Jindabyne Suite|41133|6|Mentioned|p1134|||||||||
8971|Jindabyne Suite|41563|6|Mentioned|p506|||||||||
8971|Jindabyne Suite|41898|6|Mentioned|p1184|||||||||
8971|Jindabyne Suite|41905|4|Described|p92|||||||||
8971|Jindabyne Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
8971|Jindabyne Suite|42726|5|Briefly described|map legend||Silurian|||||||
8971|Jindabyne Suite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Kosciusko Batholith.||||||
8971|Jindabyne Suite|44093|5|Briefly described|p189 App. 1|Early Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||14-MAR-05
8971|Jindabyne Suite|45147|6|Mentioned|M254|||||||||
8971|Jindabyne Suite|67060|5|Briefly described|p503, p513.|Devonian|Silurian|Includes the probably cogenetic Jindabyne and Round Flat plutons. The former is dated at 424.1 +/- 4.2 Ma (this study) and the latter at 416 +/- 4 Ma (Kemp et al. 2005).|424 - 416 Ma.||||Minor gabbro and diorite.|15-MAR-12
8971|Jindabyne Suite|72571|6|Mentioned|p90, p101|||Of the Tasmanides of eastern Australia.||||||
8971|Jindabyne Suite|73264|6|Mentioned|p1393, p1405|Early Devonian|Early Devonian|Lachlan Orogen, eastern. I-type.|415 Ma|||||
8971|Jindabyne Suite|73514|6|Mentioned|p8|||Lachlan Fold Belt.|||||I-type.|
8972|Jindabyne Tonalite|22778|5|Briefly described|p 162|||||||||
8972|Jindabyne Tonalite|22815|4|Described|p49|Early Devonian|Silurian|Formerly named Jindabyne Granite.||||||
8972|Jindabyne Tonalite|23439|5|Briefly described|p135|||||||||
8972|Jindabyne Tonalite|23549|5|Briefly described|p516|||Of the Jindabyne Suite.  Geological province: Lachlan Fold Belt.||||||05-APR-05
8972|Jindabyne Tonalite|23551|5|Briefly described|p495|||I-type granite.||||||
8972|Jindabyne Tonalite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
8972|Jindabyne Tonalite|35109|2|Defined|p71|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
8972|Jindabyne Tonalite|35263|6|Mentioned|Table 3|||||||||
8972|Jindabyne Tonalite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
8972|Jindabyne Tonalite|40328|4|Described|p207|||||||||
8972|Jindabyne Tonalite|41563|6|Mentioned|p506|||||||||
8972|Jindabyne Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Jindabyne Suite.||||||
8972|Jindabyne Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh14||||||
8972|Jindabyne Tonalite|49705|5|Briefly described|p39|||See also P40||||||
8972|Jindabyne Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
8972|Jindabyne Tonalite|72571|5|Briefly described|p90-91, p95-99|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail. I-type.|||||Hornblende Tonalite with magnetite, ilmenite, allanite and no titanite.|
8980|Jindera Granite|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
8980|Jindera Granite|30909|6|Mentioned|Map legend|Early Devonian|Early Devonian|Prob.Lower Devonian||||||
8980|Jindera Granite|33553|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8980|Jindera Granite|37029|6|Mentioned|p48|||||||||
8980|Jindera Granite|40328|4|Described|p207|||||||||
8980|Jindera Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8980|Jindera Granite|40498|6|Mentioned|p376|||||||||
8980|Jindera Granite|42726|5|Briefly described|map legend|Silurian||||||||
8980|Jindera Granite|43344|14|Not recorded|p132|||||||||
8980|Jindera Granite|44340|14|Not recorded|p.9,Table.1,p.5|||||||||
8980|Jindera Granite|44341|14|Not recorded|map legend||Devonian|||||||
8980|Jindera Granite|69801|5|Briefly described|p2, p4-p5, p116-120, p137|Devonian|Devonian|Central Lachlan Orogen. Occurs north of Albury. Sole occupant of the Jindera Suite. Classified by Chappell et al (1991) as an I-type felsic fractionated pluton of Silurian age and the sole member of the Jindera Suite. Chappell et al (1999) noted that this unit features significant geochemical variation and is likely mapped as a composite body. Sample locality, sample description, petrography, SHRIMP analyses and interpretation are detailed.|403.4 +/- 2.5 Ma (SHRIMP)|Jindera Suite|||Medium- to coarse-grained, seriate-textured biotite granite.|
8980|Jindera Granite|70777|5|Briefly described|p2, p64, p81|Emsian|Emsian|Lachlan Orogen.|403.4 +/- 2.5 Ma (Bodorkos et al., 2015)|||||
8980|Jindera Granite|71206|6|Mentioned|p384|||Lachlan Fold Belt.||||||
8980|Jindera Granite|72528|5|Briefly described|p1, p49, p109.|Emsian|Emsian|Name assigned in company reports to granite dated herein as Mount Royal Granite from Hickory Hill. Date given for Jindera Granite is from Bodorkos et al (2015), from 40km to S. Geochemical variation in the Jindera Granite as described by Chappell (1999) indicate the Jindera Granite is most likely a composite of multiple intrusions, which has been supported by recent mapping.|403+/-2.5 Ma U-Pb SHRIMP||||A composite I-type biotite granite.|
8987|Jingera Rock Syenite Complex|22815|2|Defined|p103, fig34|Middle Jurassic|Middle Jurassic|K/Ar Age: 168.2+/-2.5 Ma.||||||
8987|Jingera Rock Syenite Complex|35525|5|Briefly described|p81|||||||||
8987|Jingera Rock Syenite Complex|43233|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|||||||
8987|Jingera Rock Syenite Complex|61819|5|Briefly described|p90|Middle Jurassic|Middle Jurassic|Intrusive complex.||||||
8987|Jingera Rock Syenite Complex|72528|5|Briefly described|p18.|Jurassic|Jurassic|||||Intrudes into Whipstick Monzogranite.|Includes syenite.|
9012|Johnsons Creek Conglomerate|22736|6|Mentioned|p629||Namurian|||||||
9012|Johnsons Creek Conglomerate|22857|4|Described|p510 App.1 Tb.A1.8|Westphalian|Westphalian|Coarse, massive, pebble to cobble conglomerate. Max. thickness: 830m. Geological Province: Tamworth Forearc Basin.||||||
9012|Johnsons Creek Conglomerate|32324|6|Mentioned|Table 8.1|||||||||
9012|Johnsons Creek Conglomerate|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
9012|Johnsons Creek Conglomerate|32868|6|Mentioned|p210|||||||||
9012|Johnsons Creek Conglomerate|36057|6|Mentioned|Fig.1|||||||||
9012|Johnsons Creek Conglomerate|36528|6|Mentioned|p182|||||||||
9012|Johnsons Creek Conglomerate|38801|6|Mentioned|Fig.3|||||||||
9012|Johnsons Creek Conglomerate|39302|6|Mentioned|p347|||||||||
9012|Johnsons Creek Conglomerate|39308|4|Described|p488|||||||||
9012|Johnsons Creek Conglomerate|40872|6|Mentioned|Fig.1|||||||||
9012|Johnsons Creek Conglomerate|40883|6|Mentioned|p8|||||||||
9012|Johnsons Creek Conglomerate|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Tamworth Belt.||||||16-DEC-04
9012|Johnsons Creek Conglomerate|42547|4|Described|p36|||||||||
9012|Johnsons Creek Conglomerate|43017|5|Briefly described|Fig.1,p372|||||||||
9012|Johnsons Creek Conglomerate|44093|5|Briefly described|p230 App. 1|Early Permian|Late Carboniferous|Geological Province: New England Fold Belt.||||||
9012|Johnsons Creek Conglomerate|44244|2|Defined|p160|Westphalian|Westphalian|Together with McInnes Formation replaces "Isaacs Formation" (Rattigan, 1967a).  Conformably overlies McInnes Formation; disconformably underlies Alum Mountain Volcanics.  Max. thickness: 830m.  Type section in text.  Geological Province: Myall Block.||||||
9012|Johnsons Creek Conglomerate|50099|5|Briefly described|p13|||Unconformably overlain by "Bucketts rhyolites".||||||
9012|Johnsons Creek Conglomerate|50147|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Massive pebble to cobble conglomerate with clasts dominantly of acid volcanics, interbedded yellow to grey lithic sandstone, and pale-brown diamictite at top of formation.  Geological Province: Western Myall Block.||||||
9012|Johnsons Creek Conglomerate|60281|6|Mentioned|p54|Namurian|Namurian|Age: 320Ma.  Geological Province: New England Fold Belt.||||||
9012|Johnsons Creek Conglomerate|63832|4|Described|p131 Fig.2, p134|Serpukhovian|Serpukhovian|Roberts et al. (1991). Of western Myall block. Second Paleozoic glaciation (C2). Proximal proglacial facies. Appears as Johnson's Creek Conglomerate on p134.|||||A suite of proximal proglacial facies, including diamictites and rhythmically laminated mudrocks interbedded with other facies such as thick fluvial conglomerates.|13-DEC-17
9012|Johnsons Creek Conglomerate|65382|5|Briefly described|p714|Serpukhovian|Serpukhovian|Ages of 321.9 +/- 4.0 and 323.2 +/- 3.2 Ma from tuffs, (Roberts et al. 1995). Eastern Australia.||||||
9012|Johnsons Creek Conglomerate|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Serpukhovian|Myall Block, Tamworth Belt.||||||
9018|Jones Creek Diorite|22638|6|Mentioned|p13|||Jindalee Group. Tumut 1: 100 000 map sheet.||||||
9018|Jones Creek Diorite|42313|3|Fully described|p25|Early Ordovician|Cambrian|Mentioned informally as "Jones Creek Diorite Porphyrite" in 79/19459 P11 and herein.||||||
9018|Jones Creek Diorite|42314|5|Briefly described|Map legend|Cambrian||||||||
9026|Jooriland Group|34039|6|Mentioned|p355|||Permian||||||
9026|Jooriland Group|43477|14|Not recorded|p27,60,Pl.1|||Formerly Upper Marine Series.Correlated with Capertee,Shoalhaven Groups & Branxton Sub-group||||||
9034|Jounama Creek Limestone|40498|6|Mentioned|p425|||||||||
9077|Junction Reefs Monzodiorite|13139|5|Briefly described|p3 Fig. 2|||Geological Province: Lachlan Orogen.||||||
9077|Junction Reefs Monzodiorite|22679|5|Briefly described|p 37|Ordovician|Ordovician|||||||
9077|Junction Reefs Monzodiorite|23214|3|Fully described|p93|Late Ordovician|Late Ordovician|Intrudes the Weemalla Formation. Consists of a small circular stock 300m in diameter.||||||19-MAY-16
9077|Junction Reefs Monzodiorite|23334|5|Briefly described|3 Fig.2|||||||||
9077|Junction Reefs Monzodiorite|24265|5|Briefly described|p1445|Wenlock|Caradoc|Age: 449 +/- 10Ma (K-Ar), 428.6 +/- 7.6Ma (U-Pb). Geological Province: Lachlan Fold Belt||||||
9077|Junction Reefs Monzodiorite|24266|5|Briefly described|p1471|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt. Age: 430 Ma (U-Pb zircon).||||||
9077|Junction Reefs Monzodiorite|24268|4|Described|p1533, p1537 Fig.3|Early Silurian|Late Ordovician|Parent: Coombing Formation. Geological Province: Lachlan Fold Belt||||||
9077|Junction Reefs Monzodiorite|24398|5|Briefly described|p259 Fig. 2|Llandovery|Llandovery|Geological Province: Lachlan Fold Belt.||||||
9077|Junction Reefs Monzodiorite|42802|5|Briefly described|p101|||||||||
9077|Junction Reefs Monzodiorite|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Monzodiorite.||||||15-JUL-08
9077|Junction Reefs Monzodiorite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
9077|Junction Reefs Monzodiorite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
9091|Jurambula sand|39512|6|Mentioned|p2|||||||||
9184|Kameruka Granodiorite|22815|4|Described|p69|||||||||
9184|Kameruka Granodiorite|23456|5|Briefly described|p51|Middle Devonian|Middle Devonian|||||||
9184|Kameruka Granodiorite|35526|6|Mentioned|p95|||||||||
9184|Kameruka Granodiorite|37501|6|Mentioned|p414|||||||||
9184|Kameruka Granodiorite|40646|5|Briefly described|p39|||Mention P23||||||
9184|Kameruka Granodiorite|43147|5|Briefly described|p49|||||||||
9184|Kameruka Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Kameruka Suite.||||||
9184|Kameruka Granodiorite|66197|6|Mentioned|p639|||Shows 24 km of dextral displacement along Burragate Fault.||||||14-MAR-12
9184|Kameruka Granodiorite|68298|5|Briefly described|p233|||Of Bega Batholith. Age ~420 Ma [SHRIMP?] zircon is too old to help constrain overlying Boyd Volcanic Complex fish fauna ages.|381+/-7 Ma Rb/Sr (Fergusson et. al, 1979)|||Nonconformably overlain by Boyd Volcanic Complex||
9184|Kameruka Granodiorite|73181|6|Mentioned|p63-64|||||||||
9185|Kameruka Suite|22778|5|Briefly described|p 161|||||||||
9185|Kameruka Suite|22815|6|Mentioned|p69|||||||||
9185|Kameruka Suite|24517|6|Mentioned|p48|||Informal name. Of the Bega Batholith. Name used interchangeably with Kameruka pluton.||||||25-MAY-05
9185|Kameruka Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
9185|Kameruka Suite|42827|5|Briefly described|p430|||of Kameruka Supersuite||||||
9185|Kameruka Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
9187|Kameruka Supersuite|22878|5|Briefly described|p83|||||||||
9187|Kameruka Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
9187|Kameruka Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Yambula Granodiorite||||||01-OCT-04
9187|Kameruka Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
9187|Kameruka Supersuite|23309|5|Briefly described|p339|||G5, G7, G8, G9, G10, G31, G521||||||
9187|Kameruka Supersuite|24551|5|Briefly described|p235|||Consists of: Wallagaraugh Suite, Betka Suite.||||||
9187|Kameruka Supersuite|42726|5|Briefly described|map legend||Early Devonian|||||||
9187|Kameruka Supersuite|42827|5|Briefly described|p430|||||||||
9187|Kameruka Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
9187|Kameruka Supersuite|69801|5|Briefly described|p3, p129, p138|Devonian|Devonian|Eastern Lachlan Orogen.|||Includes the Wallagaraugh Suite, Pericoe Monzogranite and the Yambulla Granodiorite.|||
9187|Kameruka Supersuite|72528|5|Briefly described|p108.|Emsian|Emsian|Age from dating of Mount Poole Monzogranite.|||Includes Mount Poole Monzogranite.|||
9203|Kanangra Granite|23214|4|Described|p261|Carboniferous|Carboniferous|Intrudes the Adaminaby Group.||||||
9203|Kanangra Granite|30731|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
9203|Kanangra Granite|30734|6|Mentioned|p54|||||||||
9203|Kanangra Granite|32999|3|Fully described|p44|||||||||
9203|Kanangra Granite|34481|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
9203|Kanangra Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
9203|Kanangra Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
9203|Kanangra Granite|45087|5|Briefly described|p17|||Chemical analyses||||||
9203|Kanangra Granite|63633|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Grainte, coarse porphyritic granite.||||||27-JAN-09
9203|Kanangra Granite|64238|5|Briefly described|Map legend|Carboniferous|Carboniferous|Of the Tuglow Suite. Pale pink, massive, medium- to coarse-grained leucocratic biotite granite.||||||
9203|Kanangra Granite|68592|2|Defined|p1754-9, p1768-70, p1774-7|Carboniferous|Early Carboniferous|First used informally by Shiels (1959), and formally defined by Scheibner (1973). Named after Kanangra Walls. Synonymous with Tuglow Adamellite and Tuglow Granite, both of which are superseded. Type pluton of Tuglow Suite. Type area defined here. Geochemistry detailed; geophysical properties described. Undeformed: post-dates the Kanimblan deformation. Has roof pendants.||Unit in Tuglow Suite.||Intrudes Abercrombie and Kowmung Formations and the Lambie Group. Correlative of Abercorn Granite.|Pale pink, coarse-grained, leucocratic and potassic granite; porphyritic to megacrystic; massive and non-foliated but locally strongly jointed; local equigranular granite and occurrences of aplite and pegmatite. I-type.|
9203|Kanangra Granite|70192|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Ctk. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Tuglow Suite|||Leucocratic, coarse grained, massive, biotite granite with orthoclase megacrysts.|
9203|Kanangra Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
9203|Kanangra Granite|70543|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||Tuglow Suite|||Leucocratic, coarse grained, massive, biotite granite with orthoclase megacrysts.|
9205|Kandie Tank Limestone|22857|5|Briefly described|p122, p410 App. 1 Tb. A1.4.|Early Ordovician|Late Cambrian|Limestone and shale. Geological Province: Gnalta Shelf. ||||||
9205|Kandie Tank Limestone|23245|6|Mentioned|p122||Early Ordovician|||||||
9205|Kandie Tank Limestone|23380|5|Briefly described|p107 Fig.2, p106 Fig.1||Late Cambrian|In the Wonaminta Block.||||||26-NOV-08
9205|Kandie Tank Limestone|23469|5|Briefly described|Fig 13 p 327|||||||||
9205|Kandie Tank Limestone|32671|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
9205|Kandie Tank Limestone|32677|5|Briefly described|p4|||||||||
9205|Kandie Tank Limestone|33004|6|Mentioned|p141|||||||||
9205|Kandie Tank Limestone|35320|6|Mentioned|p464|||||||||
9205|Kandie Tank Limestone|36534|6|Mentioned|p227|||||||||
9205|Kandie Tank Limestone|38692|6|Mentioned|p138|||||||||
9205|Kandie Tank Limestone|41810|6|Mentioned|p111|||||||||
9205|Kandie Tank Limestone|44093|5|Briefly described|p109|Early Ordovician|Late Cambrian|Overlies Copper Mine Range beds. See also p148 Appendix 1. Geological Province: Tasman Fold Belt.||||||
9205|Kandie Tank Limestone|62793|5|Briefly described|p270|Early Ordovician|Late Cambrian|Occurs as a small outcrop immediately east of Coturaundee Range. Contains conodonts including species of Cordylodus. Approximately contemporaneous with Watties Bore Formation.||||||21-MAR-12
9205|Kandie Tank Limestone|63489|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Shallow-marine shale, carbonate and quartzite.||||||
9205|Kandie Tank Limestone|63793|6|Mentioned|p46.|||||||||
9205|Kandie Tank Limestone|64671|5|Briefly described|Map legend|Ordovician|Late Cambrian|Unconformably overlies Copper Mine Range beds. Contains conodonts.||||||26-NOV-08
9205|Kandie Tank Limestone|64683|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Massive microcrystalline grey limestone with conodonts.||||||
9205|Kandie Tank Limestone|64684|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Unconformably overlies Copper Mine Range beds. Contains conodonts.||||||
9205|Kandie Tank Limestone|66623|1|Redefined|p33, p44, pp130-131. |Early Ordovician|Late Cambrian|Mapped by Rose and Brunker (1967); defined by Pogson and Scheibner (1971); redefined in this study. Possible correlation with Nootumbulla Sandstone. Single outcrop of massive to brecciated limestone capping low rises. Tightly folded by Benambran Orogeny, including the unconformable basal contact. 5-50 m thick. ||Unit in Kayrunnera Group.||Unconformably overlies Copper Mine Range Formation. No overlying younger units.|Pale-grey, massive to brecciated recrystallised fine-grained limestone; biostromal with massive algal biomicrite grading into crinoidal biosparite; contains brachiopods and conodonts in fine-grained organic detritus.|
9205|Kandie Tank Limestone|66929|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|Contains conodonts.||||Unconformably overlies Copper Mine Range beds.||
9205|Kandie Tank Limestone|67322|5|Briefly described|p11-12; Fig.5|Tremadocian|Stage 10|Described by Pogson and Scheiber (1971) with minor redefinition by Greenfield (in Greenfield et al., 2010). The unit is up to 50m thick. Age determination is based on species of Cordylodus indicating an age close to the Cambro-Ordovician boundary. Occurs E of northern end of Coturaundee Range in the Kayrunnera-Koonenberry region.||Of the Kayrunnera Group.|||An isolated limestone pod.|22-FEB-18
9205|Kandie Tank Limestone|71284|5|Briefly described|p487-488, p490-494|Early Ordovician|Early Ordovician|Pogson and Scheibner (1971); redefined by Greenfield (Greenfield et al., 2010). Northern end of the Coturaundee Range. Thickness unknown; possibly up to 50m. Contains the first documented occurrence in Australia of the conodont species Iapetognathus fluctivagus which is the international primary marker defining the base of the Ordovician. Other species described. International correlations.||Kayrunnera Group.||||
9206|Kangaloolah Volcanics|22679|4|Described|p 26, 27|Silurian|Silurian|||||||
9206|Kangaloolah Volcanics|22857|4|Described|p468 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the Mumbil Group. Max. thickness: 1.2km. Geological Province: Molong Rise and Hill End Trough. See also p472 App.1 Tb.A1.6.||||||
9206|Kangaloolah Volcanics|23048|5|Briefly described|p9 fig14|Late Silurian|Silurian|||||||
9206|Kangaloolah Volcanics|23214|3|Fully described|p142|Late Silurian|Late Silurian|Of Mumbil Group. Parts of this unit have previously been mapped as Thompsons Volcanics. Can be divided into three unnamed subunits. Max. thickness 2000m.||||||
9206|Kangaloolah Volcanics|23335|5|Briefly described|p14, p15 Tb. 1|Late Silurian|Late Silurian|||||||27-OCT-04
9206|Kangaloolah Volcanics|24317|5|Briefly described|p14|Late Silurian|Late Silurian|||||||
9206|Kangaloolah Volcanics|29989|6|Mentioned|Map legend|Silurian|Silurian|||||||
9206|Kangaloolah Volcanics|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
9206|Kangaloolah Volcanics|30329|6|Mentioned|p30|||On table P30||||||
9206|Kangaloolah Volcanics|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
9206|Kangaloolah Volcanics|30734|6|Mentioned|p28|||||||||
9206|Kangaloolah Volcanics|32088|6|Mentioned|p10|||||||||
9206|Kangaloolah Volcanics|32483|6|Mentioned|p4|||Sil. Strat. table 1||||||
9206|Kangaloolah Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
9206|Kangaloolah Volcanics|32672|6|Mentioned|p672|||||||||
9206|Kangaloolah Volcanics|32999|3|Fully described|p29|||||||||
9206|Kangaloolah Volcanics|33004|6|Mentioned|p181|||||||||
9206|Kangaloolah Volcanics|33007|6|Mentioned|p11|||Distribution||||||
9206|Kangaloolah Volcanics|34481|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
9206|Kangaloolah Volcanics|35773|5|Briefly described|p286|||||||||
9206|Kangaloolah Volcanics|37727|4|Described|p66|||||||||
9206|Kangaloolah Volcanics|39331|6|Mentioned|Fig.0-3|||||||||
9206|Kangaloolah Volcanics|40328|5|Briefly described|p176|||||||||
9206|Kangaloolah Volcanics|42726|5|Briefly described|map legend|||||||||
9206|Kangaloolah Volcanics|43639|5|Briefly described|Map Legend||Silurian|||||||
9206|Kangaloolah Volcanics|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group (east). Rhyolite; minor siltstone.||||||17-JUL-08
9206|Kangaloolah Volcanics|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Mumbil Group.||||||27-JAN-09
9206|Kangaloolah Volcanics|44093|5|Briefly described|p207 App. 1|Early Devonian|Early Devonian|Of the Mumbil Group. Geological Province: Lachlan Fold Belt.||||||
9206|Kangaloolah Volcanics|50124|5|Briefly described|p126, p130|Late Silurian|Late Silurian|Of the Campbells Group. Geological Province: eastern Lachlan Fold Belt.||||||
9206|Kangaloolah Volcanics|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Campbells Group. Rhyolitic crystal vitric volcanic and volcaniclastic sandstone, quartz-feldspar-muscovite schist, minor siltstone.||||||
9206|Kangaloolah Volcanics|63633|5|Briefly described|Map Legend|Early Devonian|Llandoverian|Quartz - feldspar porphyry, acid tuff - schistose, "porphyroids", tuffaceous sandstone.||||||
9206|Kangaloolah Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Grey to cream and pink rhyolitic crystal-vitric volcanic and volcaniclastic sandstone, quartz-feldspar-muscovite schist, minor siltstone.||||||11-JUN-08
9206|Kangaloolah Volcanics|67820|6|Mentioned|p136 Fig.3|Late Silurian|Late Silurian|||Campbells Group.||||
9206|Kangaloolah Volcanics|67847|5|Briefly described|p30, p59|Silurian|Silurian|Hosts mineralisation at the contact between fine-grained sediments and felsic tuffs in the Peelwood district. ||||Overlies the Triangle Formation. Equivalent to the Mullions Range Volcanics.|Felsic volcanic rocks and limestones.|
9206|Kangaloolah Volcanics|68592|2|Defined|p259, p607-14, p616-8, p622, p652-9,p803|Ludlow|Wenlock|See also p151-63. Markham (1961) after Mutton (1960). Named after Kangaloolah Creek, an obsolete name for Peelwood Creek. In the Goulburn 1:250 000 sheet, this unit has been mapped as gneiss of the Wologorong Granite N of Laggan, and as Rockley Volcanics at Thalaba. Outcrops of Rockley Volcanics in the Phils River area are reassigned to this unit. A type section and representative sections are described. From 280m to c. 2000m thick. Bouldery, locally tombstone-like, outcrops; forms steep slopes or hilly ground. Representative section in Abercrombie River. Trace elements, geochemistry detailed; geophysical properties described. SHRIMP U-Pb zircon ages by Wilde (2001) and Black (2005) respectively. Syn-eruptive resedimented pyroclastics deposited in a deep subaqueous environment by mass flows. Regionally metamorphosed to middle greenschist facies; deformed at 386 +/- 2 Ma (Tabberabberan Orogeny) and 352 +/- 2 Ma (Kanimblan Orogeny). Correlated with Cuddyong Formation and Bells Creek Volcanics. Hosts deformed base metals and gold VHMS (Cordillera and John Fardy deposits detailed).|429 +/- 5 Ma and (at the top) 423.7 +/- 2.5 Ma.|Unit in Campbells Group.||Conformably overlies Fosters Creek Conglomerate and Cuddyong Formation. Is overlain conformably by Binghams Back Formation. Equivalent to part of Woodlawn Volcanics.|Includes biotite-grade metamorphosed, quartzo-feldspathic and feldspathic crystal-rich volcaniclastic rocks, commonly massive and very thickly bedded; minor laminated, fine-grained, volcaniclastic rock, siltstone, breccia, conglomerate and limestone.|
9206|Kangaloolah Volcanics|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sck. Includes one unnamed unit of allochtnonous limestone. On Crookwell and Taralga 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Campbells Group|Includes one unnamed unit.|Is overlain by, and interfingers with, Binghams Back Formation. Overlies, and interfingers with, Cuddyong Formation.|Rhyolitic-dacitic, crystal rich, quartzo-feldspathic and feldspathic volcaniclastic sandstone. Minor laminated fine-grained volcaniclastic sandstone, siltstone, breccia, conglomerate and limestone.|
9206|Kangaloolah Volcanics|70210|6|Mentioned|p1|Late Silurian|Late Silurian||c.422 Ma.|||||
9206|Kangaloolah Volcanics|70296|5|Briefly described|p1, p15, p18-19, p24|Pridoli|Ludlow|Goulburn-Yass district. Temporally equated with the Woodlawn Volcanics. Must be only marginally older than Parkesbourne Granite, which caused contact metamorphism in Campbells Group units.|423.7 +/- 2.5 Ma (SHRIMP U-Pb)|Campbells Group||||22-JAN-21
9206|Kangaloolah Volcanics|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Parent age: mid-Silurian to Early Devonian.||Campbells Group|||Rhyolitic and dacitic volcanic rocks.|19-MAY-16
9206|Kangaloolah Volcanics|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Campbells Group|||Rhyolitic-dacitic, crystal rich, quartzo-feldspathic and feldspathic volcaniclastic sandstone. Minor laminated fine-grained volcaniclastic sandstone, siltstone, breccia, conglomerate and limestone.|
9206|Kangaloolah Volcanics|70544|5|Briefly described|Map Legend|Devonian|Silurian|Includes one unnamed member; allochthonous limestone with locally contained crinoid ossicles.||Campbells Group|Includes one unnamed member||Rhyolitic-dacitic, crystal rich, quartzofeldspathic and feldspathic volcaniclastic sandstone; minor laminated fine grained volcaniclastic sandstone, siltstone, breccia, conglomerate and limestone.|
9206|Kangaloolah Volcanics|71069|6|Mentioned|p100, p125, p134, p154|||Misspellt on p100 and p134 as the Kangaloola Volcanics. ||Campbells Group||Equivalent to the Woodlawn Volcanics, parts of the Hoskinstown and Mount Fairy Groups.||
9206|Kangaloolah Volcanics|71656|5|Briefly described|p13 Fig.3, p27-28||Ludlow|||Campbells Group||Overlain by Binghams Back Formation. Appears to interfinger in part with Cuddyong Formation||
9207|Kangaloon Sandstone|29901|4|Described|Table 1|||||||||
9207|Kangaloon Sandstone|36220|6|Mentioned|p65|||See also Table 20.||||||
9207|Kangaloon Sandstone|36221|6|Mentioned|Map legend|Middle Triassic|Late Permian|Late Permian to Middle Triassic||||||
9207|Kangaloon Sandstone|36223|6|Mentioned|Map legend|Middle Triassic|Late Permian|Late Permian to Middle Triassic.||||||
9207|Kangaloon Sandstone|42896|6|Mentioned|Table 6|||||||||
9207|Kangaloon Sandstone|70661|6|Mentioned|p193, p195|||||Narrabeen Group||||
9211|Kangaroo Creek Sandstone|12597|5|Briefly described|p491, p492 Tb.1, p493 Fig.2|Tithonian|Oxfordian|S Clarence-Moreton Basin. Forms characteristic escarpments up to 90m high.||||Is overlain by Grafton Formation.|Coarse-grained, cross-bedded quartz sandstone.|
9211|Kangaroo Creek Sandstone|22857|4|Described|p318-9, p548 App. 1 Tb.A1.12|Early Cretaceous|Late Jurassic|Quartzose crossbedded sandstone. Unconformably overlies Walloon Coal Measures. Max. thickness: ~500m. Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|22865|6|Mentioned|p318,Fig22.9p317|Cretaceous|Late Jurassic|||||||
9211|Kangaroo Creek Sandstone|22892|5|Briefly described|p7 fig6|Jurassic|Jurassic|||||||
9211|Kangaroo Creek Sandstone|23720|5|Briefly described|Map Legend|||Quartz arenite, quartz and lithic conglomerate.||||||15-DEC-04
9211|Kangaroo Creek Sandstone|23811|5|Briefly described|Map Legend|Oxfordian|Callovian|Quartz arenite, minor quartz and lithic conglomerate; thick to very thin-bedded, high-angle crossbedding.  Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
9211|Kangaroo Creek Sandstone|23812|4|Described|p31, p34 Tb.4|Middle Jurassic|Middle Jurassic|Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|23843|5|Briefly described|p456 Table 1|Cretaceous|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 290m.||||||
9211|Kangaroo Creek Sandstone|23888|6|Mentioned|p262|||||||||
9211|Kangaroo Creek Sandstone|24127|5|Briefly described|p5|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|24129|5|Briefly described|p4|||Geological Province: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|24299|5|Briefly described|p4|Cretaceous|Jurassic|||||||
9211|Kangaroo Creek Sandstone|29591|6|Mentioned|p85|||||||||
9211|Kangaroo Creek Sandstone|29698|6|Mentioned|p65|||||||||
9211|Kangaroo Creek Sandstone|29988|6|Mentioned|Map legend|Cretaceous|Jurassic|Cretaceous-Jurassic||||||
9211|Kangaroo Creek Sandstone|29995|6|Mentioned|Map legend|Jurassic|Jurassic|Cretaeous||||||
9211|Kangaroo Creek Sandstone|30785|6|Mentioned|p397|||||||||
9211|Kangaroo Creek Sandstone|30911|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
9211|Kangaroo Creek Sandstone|31806|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
9211|Kangaroo Creek Sandstone|32491|5|Briefly described|p18|||U.Jurassic||||||
9211|Kangaroo Creek Sandstone|32492|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
9211|Kangaroo Creek Sandstone|32671|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
9211|Kangaroo Creek Sandstone|32916|6|Mentioned|Map legend|Cretaceous|Jurassic|Cretaceous-Jurassic||||||
9211|Kangaroo Creek Sandstone|33476|6|Mentioned|Fig.10|||||||||
9211|Kangaroo Creek Sandstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
9211|Kangaroo Creek Sandstone|34254|6|Mentioned|p490|||||||||
9211|Kangaroo Creek Sandstone|34340|3|Fully described|p471|||||||||
9211|Kangaroo Creek Sandstone|34400|5|Briefly described|p13|||||||||
9211|Kangaroo Creek Sandstone|34755|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
9211|Kangaroo Creek Sandstone|36354|6|Mentioned|Fig.1|||||||||
9211|Kangaroo Creek Sandstone|37122|5|Briefly described|Table 1|||||||||
9211|Kangaroo Creek Sandstone|37252|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic-Cretaceous||||||
9211|Kangaroo Creek Sandstone|38064|5|Briefly described|p41|||||||||
9211|Kangaroo Creek Sandstone|39907|6|Mentioned|Fig.6|||||||||
9211|Kangaroo Creek Sandstone|39969|6|Mentioned|p11|||||||||
9211|Kangaroo Creek Sandstone|41631|4|Described|p20|||See also Fig.2, Fig.5 and P 19||||||
9211|Kangaroo Creek Sandstone|42248|6|Mentioned|Fig.8 P403|||||||||
9211|Kangaroo Creek Sandstone|42463|6|Mentioned|Fig.3 P170|||||||||
9211|Kangaroo Creek Sandstone|42869|5|Briefly described|Table 1, p33|||||||||12-SEP-21
9211|Kangaroo Creek Sandstone|43008|5|Briefly described|map legend|||||||||
9211|Kangaroo Creek Sandstone|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Clarence-Moreton Basin.||||||12-APR-05
9211|Kangaroo Creek Sandstone|43344|14|Not recorded|p14,102|||||||||
9211|Kangaroo Creek Sandstone|43383|14|Not recorded|p25,28|Cretaceous|Jurassic|Above Walloon Coal Measures?||||||
9211|Kangaroo Creek Sandstone|43384|14|Not recorded|Map Legend|Cretaceous|Jurassic|||||||
9211|Kangaroo Creek Sandstone|43468|14|Not recorded|Map Legend|Cretaceous|Jurassic|Provisional Edition||||||
9211|Kangaroo Creek Sandstone|43479|14|Not recorded|p251,252||Early Cretaceous|||||||
9211|Kangaroo Creek Sandstone|44028|14|Not recorded|p509,512,Fig.2||Late Jurassic|||||||
9211|Kangaroo Creek Sandstone|44450|4|Described|p28 Table 7|Late Jurassic|Middle Jurassic|Geological Province: Clarence-Moreton Basin||||||
9211|Kangaroo Creek Sandstone|48917|3|Fully described|p30|||||||||
9211|Kangaroo Creek Sandstone|60079|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|Quartz arenite, conglomerate.||||||
9211|Kangaroo Creek Sandstone|60281|5|Briefly described|p27, p31|Cretaceous|Late Jurassic|Interconnected quartzose cross-bedded sandstone deposited by braided streams. Overlain by Grafton Formation; overlies the Walloon Coal Measures.  Max. thickness: ?500m.||||||27-APR-05
9211|Kangaroo Creek Sandstone|60993|3|Fully described|p35, p19 Fig. 16|Late Jurassic|Middle Jurassic|First termed Kangaroo Creek "Series" and Kangaroo Creek "Stage". Overlies Walloon Coal Measures; grades into the Woodenbong beds. Conformably underlies Grafton Fm.  Max. thickness: >870m. Geol. Prov: Clarence-Moreton Basin.||||||04-DEC-08
9211|Kangaroo Creek Sandstone|60995|4|Described|p69, p51 Fig. 3|Late Jurassic|Late Jurassic|Massive, coarse-grained, cross-bedded, white saccharoidal, quartz sandstone.Overlies Walloon C.M.  Max. thickness: ~500m. Geological Province: Clarence-Moreton Basin. See also p52.||||||
9211|Kangaroo Creek Sandstone|60997|5|Briefly described|p139|Tithonian|Kimmeridgian|Highly quartzose sandstone.  Overlies the Walloon Coal Measures; conformably overlain by Grafton Formation. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1.||||||
9211|Kangaroo Creek Sandstone|60999|5|Briefly described|p164|||Overlies Walloon C. M. in places.||||||
9211|Kangaroo Creek Sandstone|61000|5|Briefly described|p181, p183|Middle Jurassic|Middle Jurassic|Clean and cross-bedded sandstones are common. Overlies Walloon C.M. Probably Bajocian in age. Geological Province: Clarence-Moreton Basin. See also p186.||||||
9211|Kangaroo Creek Sandstone|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|||||||
9211|Kangaroo Creek Sandstone|61006|5|Briefly described|p278 Fig. 2|Jurassic|Jurassic|Quartzose sandstone. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285, p289.||||||
9211|Kangaroo Creek Sandstone|61310|4|Described|p14 Fig. C5|Early Cretaceous|Late Jurassic|Distinctive medium- to coarse-grained, white to cream, saccharoidal sst., with minor siltstone, shale and quartz pebble sst. Unconformably overlies Walloon Coal Measures; overlain by Grafton Fm. Max. thickness: ?500m. Geol. Prov: Clarence-Moreton Basin.||||||
9211|Kangaroo Creek Sandstone|64289|5|Briefly described|p6 Fig. 2|Late Jurassic|Middle Jurassic|Geological province: Clarence-Moreton Basin.||||||07-FEB-11
9211|Kangaroo Creek Sandstone|67402|4|Described|p187, p192, p193|Oxfordian|Bathonian|Clarence-Moreton Basin. Deposited in a fluvial environment. Sandstones are often of reservoir quality.  ||||Overlain by the Grafton Formation. Overlies the Walloon Coal Measures.|Fine feldspathic, sub-labile to coarse-grained quartzose sandstone.|
9211|Kangaroo Creek Sandstone|68135|5|Briefly described|p52 fig 2b|Oxfordian|Oxfordian|Clarence-Moreton Basin.||||Unconformably overlies Walloon Coal Measures. Overlain by Grafton Formation|Sandstone.|14-SEP-17
9211|Kangaroo Creek Sandstone|69297|5|Briefly described|p487 fig 5.38, p488, p490|Upper Jurassic|Upper Jurassic|Clarence-Moreton Basin. Between 200-500m thick. Deposited in a braided fluvial environment. Potential reservoir rock.||||Overlies the Maclean Sandstone Member and Walloon Coal Measures. Overlain by the Grafton Formation.|Cross-bedded, quartzose sandstone.|
9211|Kangaroo Creek Sandstone|69594|5|Briefly described|p544-545|||Clarence-Moreton Basin (NSW only). In QLD it is known as the (lower part of) Woodenbong beds. Cliff-forming unit. Sediment derived from the Texas Subprovince.||||Overlies Walloon Coal Measures conformably or disconformably (in part unconformably). Is overlain by Grafton Formation.|White quartzose sandstone.|
9211|Kangaroo Creek Sandstone|72921|5|Briefly described|p15 Fig.2.|Late Jurassic|Late Jurassic|Shown as located within the Clarence-Moreton Basin.||||Shown as unconformably overlying Walloon Coal Measures and underlies Grafton Formation.||
9211|Kangaroo Creek Sandstone|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.||||Overlies Walloon Coal Measures. Is overlain by Grafton Formation.||
9211|Kangaroo Creek Sandstone|73570|6|Mentioned|p911, p912 Fig.2, p914, p915 Fig.4, p920|Late Jurassic|Late Jurassic|Clarence-Morton Basin. Paleocurrent directions predominantly to the east and southeast. Grades laterally into Woodenbong beds. Misspelt as Kangaroo Formation p913.|||||Quartz-rich sandstones.|
9253|Kantappa Quartzite Member|22857|5|Briefly described|p398 App. 1 Tb.A1.3.|Neoproterozoic|Neoproterozoic|Of the Mulcatcha Formation? Orthoquartzite horizon. Geological Province: Adelaide Fold Belt.||||||
9253|Kantappa Quartzite Member|30261|6|Mentioned|p2|||||||||
9253|Kantappa Quartzite Member|34812|6|Mentioned|p69|||||||||
9253|Kantappa Quartzite Member|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
9253|Kantappa Quartzite Member|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
9253|Kantappa Quartzite Member|41405|6|Mentioned|p204|||||||||
9253|Kantappa Quartzite Member|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in [Mulcatcha Formation] Yancowinna Subgroup.||||
9253|Kantappa Quartzite Member|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Mulcatcha Formation.|||Thin-bedded pebble- and cobble-bearing orthoquartzite.|
9302|Karrakurra Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
9302|Karrakurra Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
9305|Karuah Formation|22857|4|Described|p510 App.1 Tb.A1.8|Visean|Visean|Polymictic conglomerate and lithic arenite; boulder conglomerate, pebbly sandstone and mudstone; schlieren of heavy minerals. Disconformably overlies Nerong Volcanics. Max. thickness: 600m.||||||17-FEB-06
9305|Karuah Formation|24118|5|Briefly described|p4|||||||||
9305|Karuah Formation|24121|5|Briefly described|p4, p255|||||||||25-AUG-22
9305|Karuah Formation|30074|6|Mentioned|p27|||||||||
9305|Karuah Formation|32324|6|Mentioned|Table 8.1|||||||||
9305|Karuah Formation|32379|6|Mentioned|p5|||||||||
9305|Karuah Formation|32868|6|Mentioned|p208,Fig.7|||||||||
9305|Karuah Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
9305|Karuah Formation|34085|6|Mentioned|Cor.chart|||Namurian||||||
9305|Karuah Formation|34168|5|Briefly described|p254|||Carboniferous||||||
9305|Karuah Formation|34238|6|Mentioned|Table 1|||||||||
9305|Karuah Formation|39302|5|Briefly described|p346|||||||||
9305|Karuah Formation|40883|6|Mentioned|p8|||||||||
9305|Karuah Formation|42547|4|Described|p37, 32|||||||||
9305|Karuah Formation|43432|14|Not recorded|p208||Carboniferous|Ref. to Campbell 1961||||||
9305|Karuah Formation|43447|14|Not recorded|Table 1&2,p10,13||Carboniferous|||||||
9305|Karuah Formation|43451|14|Not recorded|Map Legend||Carboniferous|Included in Crawford Formation||||||
9305|Karuah Formation|43479|14|Not recorded|p161||Carboniferous|||||||
9305|Karuah Formation|44093|5|Briefly described|p230 App. 1|Late Devonian|Late Devonian|Geological Province: New England Fold Belt.||||||14-MAR-05
9305|Karuah Formation|44244|2|Defined|p144-145|Westphalian|Visean|Disconformably overlies Nerong Volcanics; conformably underlies Booral Formation.  Max. thickness: 600m.  Geological Province: Myall Block.  Type section in text.||||||
9305|Karuah Formation|44360|14|Not recorded|p34|||Ref. to Campbell 1961.||||||
9305|Karuah Formation|50147|5|Briefly described|Map legend|Namurian|Visean|Geological Province: Western Myall Block.||||||
9305|Karuah Formation|50263|5|Briefly described|Map Legend|Namurian|Visean|Underlies: Booral Formation. Geological Province: Western Myall Block.||||||
9305|Karuah Formation|63832|6|Mentioned|p131 fig 2|Visean|Visean|Western Myall block, Southern New England Fold Belt.||||||
9305|Karuah Formation|64631|6|Mentioned|p44 Fig.2.|Serpukhovian|Visean|Southern New England Fold Belt, western Myall Block. Biostratigraphic age control at base and top.||||||
9305|Karuah Formation|69323|5|Briefly described|p62|||Geological province: New England Orogen.||||Underlain disconformably by Nerong Volcanics.||
9305|Karuah Formation|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Visean|Myall Block, Tamworth Belt.||||||
9306|Katandra Member|29898|5|Briefly described|p213|||||||||
9306|Katandra Member|34735|5|Briefly described|p40|||||||||
9306|Katandra Member|35272|5|Briefly described|p279|||||||||
9306|Katandra Member|41848|5|Briefly described|p355|||Part of Shepparton Formation.||||||27-OCT-08
9306|Katandra Member|42827|5|Briefly described|p355|||see also Table 9.1, of Shepparton Formation.||||||27-OCT-08
9306|Katandra Member|42966|2|Defined|Table 30 p196|Pleistocene||Of Shepparton Formation.||||||27-OCT-08
9306|Katandra Member|60599|5|Briefly described|p92|Quaternary|Quaternary|Of Shepparton Formation.||||||
9306|Katandra Member|70961|4|Described|p133|||Refers to Lawrence (1966). Alluvial.||||||
9333|Katoomba Coal Member|39232|6|Mentioned|Table 2|||||||||
9333|Katoomba Coal Member|40806|6|Mentioned|p158|||||||||
9333|Katoomba Coal Member|42657|6|Mentioned|Table 1 P74|||||||||
9333|Katoomba Coal Member|73625|6|Mentioned|p2|Permian|Permian|Western coalfield, Sydney Basin.||Illawarra Coal Measures.||Is overlain by Narrabeen Group.||
9352|Kayrunnera Group|22671|5|Briefly described|p832|Ordovician|Late Cambrian|Coarse terrestrial and shallow marine sediments.||||||17-JAN-06
9352|Kayrunnera Group|22857|5|Briefly described|p91 Fig. 14.7B, p122|Early Ordovician|Late Cambrian|Includes Watties Bore Formation, Boshy Formation and Morden Formation. Geol. Prov: Gnalta Shelf. See also p410 App. 1 Tb. A1.4.||||||
9352|Kayrunnera Group|22858|6|Mentioned|Fig14.7bp90-1|||||||||
9352|Kayrunnera Group|23245|5|Briefly described|p122|Early Ordovician|Late Cambrian|||||||
9352|Kayrunnera Group|23309|5|Briefly described|p366||Cambrian|||||||
9352|Kayrunnera Group|23889|6|Mentioned|p35 Fig. 30|||||||||
9352|Kayrunnera Group|41587|3|Fully described|p908|||||||||
9352|Kayrunnera Group|41810|6|Mentioned|p107|||||||||
9352|Kayrunnera Group|42982|6|Mentioned|Table 1,p333|||||||||
9352|Kayrunnera Group|43192|4|Described|p64,Table1,p61.|Early Ordovician|Mindyallan|Defined by Wang Qizheng et al (1989).||||||
9352|Kayrunnera Group|43213|6|Mentioned|p63|Ordovician|Late Cambrian|Fluvial to shallow marine.||||||
9352|Kayrunnera Group|44093|5|Briefly described|p148 App. 1|Late Cambrian|Late Cambrian|Clastic sediments. Geological Province: Kanmantoo Fold Belt.||||||
9352|Kayrunnera Group|44133|5|Briefly described|p31, 46|Early Ordovician|Late Cambrian|||||||
9352|Kayrunnera Group|50618|5|Briefly described|p248 Fig. 1|Ordovician|Late Cambrian|Geological Province: Wonominta Block.||||||
9352|Kayrunnera Group|62793|5|Briefly described|p269, p270|Early Ordovician|Late Cambrian| Overlies deformed Late Proterozoic to Middle Cambrian Teltawongee beds in Northern Koonenberry Belt. Trilobites indicate age.|||Includes Morden Formation, Boshy Formation and Watties Bore Formation.||Marine sedimentary rocks, some fossiliferous limestones.|21-MAR-12
9352|Kayrunnera Group|63489|5|Briefly described|Map legend|Ordovician|Late Cambrian|Shallow-marine shale, carbonate and quartzite.||||||10-SEP-07
9352|Kayrunnera Group|63790|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Includes Watties Bore Formation., Boshy Formation and Morden Formation. Well-laminated quartzose sandstone and quartzites, mostly white, some red and maroon. Festoon cross-bedding in some units. Minor limestone, siltstone and conglomerate interbeds.||||||
9352|Kayrunnera Group|63793|6|Mentioned|p19 Table 1, p24, 38.|||Time-equivalent with Mootwingee Group.||||||19-JAN-15
9352|Kayrunnera Group|64671|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Contains Watties Bore , Boshy and Morden Formations. Unconformably overlies Copper Mine Range beds and Teltawongee beds east of Koonenberry Fault. Shallow marine shale, carbonate, sandstone, conglomerate.||||||26-NOV-08
9352|Kayrunnera Group|64683|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Includes Cupala Creek Formation.||||||
9352|Kayrunnera Group|64684|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Unconformable overlie Copper Mine Range beds and Teltawongee beds east of Kooenberry Fault. Shallow marine shale, carbonate, sandstone and conglomerate.||||||01-DEC-08
9352|Kayrunnera Group|64687|5|Briefly described|Map Legend|Ordovician|Late Cambrian|||||||
9352|Kayrunnera Group|65381|6|Mentioned|p689|Cambrian|Cambrian|||||||
9352|Kayrunnera Group|66623|1|Redefined|p49, p96, pp110-133. |Early Ordovician|Late Cambrian|Formerly part of Torrowangee Series (Mawson 1912); Warris (1967) split off the Wonominta beds and in these Brunker et al. (1971) named the Kayrunnera Beds; defined by Webby et al. (1988), Mills and Hicks (2000), and redefined in this study. Mainly shallow marine, with some limestone. Trilobites, conodonts and other fossils indicate Iverian to Floian age. Moderately tight folding in late Ordovician/early Silurian. Up to 5 km thick.|||Includes Williams Creek Conglomerate; Morden, Hummock, Boshy, Cupala Creek, Watties Bore and Wheeney Creek Formations; and Funeral Creek and Kandie Tank Limestones.|Unconformably overlies Bunker Creek Formation and Bittles Tank Volcanics. Is unconformably overlain by Ravendale Formation.|General fining-up sequence of basal polymictic conglomerate, sandstones, siltstones and mudstones, limestone and shale, variably deformed; regionally metamorphosed to greenschist facies.|
9352|Kayrunnera Group|66929|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Equivalent to Cupala Creek Formation.||||Unconformably overlies Copper Mine Range beds and Teltawongee beds.|Shallow marine shale, carbonate, sandstone, conglomerate.|
9352|Kayrunnera Group|66933|6|Mentioned|Map legend|Ordovician|Late Cambrian||||Includes Watties Bore, Boshy and Morden Formations.|Unconformably overlies Copper Mine Range beds and Teltawongee beds.||
9352|Kayrunnera Group|67105|5|Briefly described|p653-654, 659, 662-663|Early Ordovician|Late Cambrian|Kayrunnera Zone, Koonenberry Belt. Post-Delamerian Orogeny, Lachlan Orogenic Cycle deposits.|~500 - 476 Ma.||||Dominantly shallow-marine sedimentary rocks, deposited in restricted, fining-upward basins.|
9352|Kayrunnera Group|67208|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian||||||Moderately to weakly deformed slate and slaty siltstone; originally shallow marine carbonate, siltstone, sandstone and conglomerate; fossiliferous; regionally metamorphosed to greenschist facies.|
9352|Kayrunnera Group|67322|4|Described|p3 Fig.1, p11, p39; Fig.5|Floian|Drumian|Koonenberry Belt. Delamerian Orogen. Greenfield, Mills and Percival, in Greenfield et al.,(2010). SE of Koonenberry Mountain, the Group was divided into three Formations defined by Webby et al. (1988). These rocks occupy several small basins E of the Koonenberry Fault. Occurs in the Kayrunnera-Koonenberry region.|||Williams Creek Conglomerate, Hummock Formation, Morden Formation, Cupala Creek Formation, Boshy and Watties Bore Formations, Funeral Creek Limestone, Kandie Tank Limestone, Wheeney Creek Formation.|Correlates with lower and middle Mutawintji Group.|Basal conglomerates or quartzites pass upwards into sandstones and siltstones; carbonate beds and lenses are rare until higher in the succession.|22-FEB-18
9352|Kayrunnera Group|69573|6|Mentioned|p657, 659, 661, 667||||||Boshy Formation.|||
9352|Kayrunnera Group|69961|5|Briefly described|Map legend|Ordovician|Cambrian||||Includes Funeral Creek and Wheeney Creek Formations.|||
9352|Kayrunnera Group|70648|5|Briefly described|Map Legend|Ordovician|Cambrian||||Includes Wheeney Creek Formation, Watties Bore Formation, Boshy Formation, Morden Formation.||Moderately to weakly deformed slate and slaty siltstone; originally shallow marine carbonate, siltstone, sandstone and conglomerate, with Late Cambrian to Early Ordovician fossils; regionally metamorphosed to greenschist facies.|20-JAN-22
9352|Kayrunnera Group|70749|6|Mentioned|p43|Ordovician|Cambrian|Southern Thomson and Koonenberry area.||||||
9352|Kayrunnera Group|70838|4|Described|p268-272, p274, p277-278, p280-281|Ordovician|Cambrian|Kayrunnera Basin, SE Koonenberry Belt. Possible tectonic settings discussed. Deposition in small post-orogenic pull-apart basins. Detrital zircon analyses.|||Williams Creek Conglomerate; Cupala Creek, Morden, Boshy Formations.|Unconformably overlies Teltawongee Group.|Generally consists of overall fining-upward sequences of conglomerate, turbiditic sandstone, mudstone and fossiliferous limestone.|
9352|Kayrunnera Group|71262|6|Mentioned|p9 Fig 7|Ordovician|Cambrian|||||||
9352|Kayrunnera Group|71284|5|Briefly described|p487-488|Early Ordovician|Late Cambrian|Central Koonenberry Belt, far western NSW. Open-marine, shallow shelf deposits.|||Funeral Creek, Kandie Tank Limestones.|||
9352|Kayrunnera Group|71593|4|Described|p188|Mindyallan |Mindyallan |Koonenberry Province. Age derived from trilobite fossil assemblage. Potential time correlative of the Nargoon Group.|c. 502-499 Ma (Greenfield et al, 2010)|||||
9352|Kayrunnera Group|71966|6|Mentioned|p990|Ordovician|Cambrian|Geological province: southern Thomson Orogen.||||||
9352|Kayrunnera Group|73177|5|Briefly described|p1112-1113, 1114-1115 Figs.16-17|Early Ordovician|Late Cambrian||||Boshy Formation.||Fluvial to shallow marine.|
9352|Kayrunnera Group|73430|6|Mentioned|p494, p518|Early Ordovician|Late Cambrian|Koonenberry Belt. Latest Cambrian or earliest Ordovician age. Overlies the Delamerian Unconformity which has a maximum age of 496.3+/-3.1 Ma. Includes post-tectonic mafic magmatism.|||||Sediments.|
9357|Kearsley Lens|23540|5|Briefly described|Fig 2 p 419|||Of Kitchener Formation.||||||20-FEB-07
9357|Kearsley Lens|34015|5|Briefly described|p325|||||||||
9357|Kearsley Lens|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Lochinvar area.||Unit in Kitchener Formation.||||
9358|Keatings Shale Member|36413|6|Mentioned|p62|||||||||
9358|Keatings Shale Member|37727|6|Mentioned|p67|||||||||
9358|Keatings Shale Member|40328|6|Mentioned|p182|||||||||
9358|Keatings Shale Member|48878|2|Defined|p.8||Wenlockian|On many pages. p.1,5,7,15,16,17,22,25,26,37-40,52,Pl.3,4. (I55-16). Wenlockian. Contains major orebodies. Defn. on Tech.File I/55-16.||||||
9358|Keatings Shale Member|71069|5|Briefly described|p26, p105, p126|||Obsolete name, incorporated into the Captains Flat Formation. Up to 60m thick.||||Overlies the Kohinoor Volcanics.|Siltstone and shale.|
9360|Kedumba Granite|42726|5|Briefly described|map legend|Carboniferous||33. Not variation on reserved name Kedumba Complex, Qld.||||||
9364|Keelindi beds|12597|5|Briefly described|p492 Tb.1, p497|Early Cretaceous|Tithonian|S Surat Basin. Up to 150m thick.|||||Well-sorted and cross-stratified quartzose labile sandstone and interbedded shale and mudstone.|
9364|Keelindi beds|23053|4|Described|p8,11,26-7|Neocomian|Late Jurassic|||||||
9364|Keelindi beds|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
9364|Keelindi beds|24092|5|Briefly described|p8 Fig.3|||||||||
9364|Keelindi beds|42596|5|Briefly described|Fig.1 P24|||||||||
9364|Keelindi beds|43276|5|Briefly described|Map Legend|Early Cretaceous|Late Silurian|||||||
9364|Keelindi beds|43277|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Of the Great Australian Basin.||||||04-JUN-07
9364|Keelindi beds|60266|5|Briefly described|p2, p3 Tb.1|Cretaceous|Cretaceous|Quartz-lithic sandstone, siltstone, mudstone.  Conformably overlies the Pilliga Sandstone.  Geological Province: Surat Basin.||||||08-DEC-04
9364|Keelindi beds|60267|5|Briefly described|p14, p28 Fig. 8|Early Cretaceous|Early Cretaceous|Conformably overlie the Pilliga Sandstone.  Geological Province: Surat Basin.  See also p29.||||||
9364|Keelindi beds|63347|5|Briefly described|p5 Fig. 2|Early Cretaceous|Middle Jurassic|Geological Province: Surat Basin.||||||
9364|Keelindi beds|68003|4|Described|p52, p55 Fig.3-m, p56, pp67-69, p127.|Early Cretaceous|Late Jurassic|Surat Basin. Name proposed by Hawke and Cramsie (1984) for the numerous sands of Late Jurassic to Early Cretaceous age above the Pilliga Sandstone, given the difficulty of distinguishing the Orallo Formation and Mooga Sandstone. Deposited in a floodplain, meandering fluvial environment; uppermost parts are marginal marine. Equivalent to Orallo Formation, Mooga Sandstone and lowermost Bungil Formation. Distinguished by enhanced K band in airborne radiometry.||||Conformably overlies Pilliga Sandstone. Is overlain by Drildool beds.|Off-white, coarse-grained, cross-bedded, well-sorted, porous, labile to sub-labile quartz lithic sandstone and conglomerate, interbedded with minor shale, siltstone and coal; rare silicified wood.|
9364|Keelindi beds|68004|5|Briefly described|p132, p137, p209.|Early Cretaceous|Late Jurassic|Opal potential tracts and levels of certainty are discussed. Believed to be the source of heavy mineral sands concentrations in the Brigalow Belt South Bioregion. The article states that the Bungil Formation occurs within this unit.||||||
9364|Keelindi beds|68005|5|Briefly described|p131.|Jurassic|Jurassic|Surat Basin.|||||Off-white, fine- to coarse-grained, poorly to well-sorted, quartzose sandstone, pebbly sandstone and conglomerate interbedded with minor shale, siltstone and coal; cross-bedded, kaolinitic and iron-stained; rare silicified wood, ?worm burrows.|
9364|Keelindi beds|70821|5|Briefly described|p80|||Coonamble Embayment. Shown as leaky aquitard and partial aquifer.||||Overlies Pilliga Sandstone. Is overlain by Drildool beds.||04-JAN-17
9364|Keelindi beds|71890|4|Described|p5-p7, p17-p18, p26, p31, p52|Valanginian|Tithonian|Surat Basin. Informal unit. Inferred to represent a transition to lower energy fluvial systems including meandering stream and floodplain deposition. Mapped across the northwestern and western portion of the project area. Topography is typically subdued except where this unit is inferred to cap Pilliga Sandstone exposures.|152.1 to 133.9 Ma|||Conformably overlies the Pilliga Sandstone. Conformably overlain by the Drildool beds.|Fine to coarse-grained, poorly to well sorted, quartzose to quartz-lithic sandstone, pebbly sandstone and conglomerate interbedded with minor shale, siltstone and coal.|
9364|Keelindi beds|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Coonamble Embayment (NSW).||||Overlies Pilliga Sandstone. Is overlain by Drildool beds.||
9364|Keelindi beds|72700|5|Briefly described|Mapsheet 1|Mesozoic|Paleozoic||||||Buff, fine- to coarse-grained, cross-bedded quartz sandstone and conglomerate, minor shale, siltstone and coal.|02-NOV-20
9376|Keepit Conglomerate|721|5|Briefly described|Map legend|Famennian|Famennian|Of the Parry Group. Pebble to boulder orthoconglomerate and paraconglomerate, pebbly sandstone, sandstone, minor mudstone; rare local andesite and dacite olistoliths.||||||25-FEB-08
9376|Keepit Conglomerate|22571|6|Mentioned|p13||Devonian|New England Orogen.||||||
9376|Keepit Conglomerate|22736|6|Mentioned|p628 Fig7||Famennian|||||||
9376|Keepit Conglomerate|22857|5|Briefly described|p219, p496 App.1 Tb.A1.7|Famennian|Fammenian|Of the Parry Group. Disconformably overlies the Mostyn Vale Formation. Max. thickness: 510m. Geological Province: Tamworth Forearc Basin.||||||
9376|Keepit Conglomerate|22859|6|Mentioned|p219|||||||||
9376|Keepit Conglomerate|23051|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of Parry Group.||||||25-FEB-08
9376|Keepit Conglomerate|23157|6|Mentioned|p126|||||||||
9376|Keepit Conglomerate|23185|6|Mentioned|Fig1p156,Fig5p161||Famennian|||||||
9376|Keepit Conglomerate|23522|5|Briefly described|p249 Fig 5|Famennian|Famennian|||||||
9376|Keepit Conglomerate|24366|5|Briefly described|p5, 17 Fig. 3|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||
9376|Keepit Conglomerate|30133|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
9376|Keepit Conglomerate|30135|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
9376|Keepit Conglomerate|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
9376|Keepit Conglomerate|31802|4|Described|p134|||||||||
9376|Keepit Conglomerate|31999|5|Briefly described|p151|||See also Table 1||||||
9376|Keepit Conglomerate|32286|6|Mentioned|Fig. 1|||||||||
9376|Keepit Conglomerate|32482|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
9376|Keepit Conglomerate|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
9376|Keepit Conglomerate|32672|6|Mentioned|p674|||||||||
9376|Keepit Conglomerate|32865|4|Described|p480|||See also P481||||||
9376|Keepit Conglomerate|34555|3|Fully described|p240|||||||||
9376|Keepit Conglomerate|35761|5|Briefly described|p64|||Stratigraphy discussed. See also Table 1.||||||
9376|Keepit Conglomerate|35783|6|Mentioned|Fig.1|||Mineral deposits and geology of Nundle gold field.||||||
9376|Keepit Conglomerate|36286|4|Described|p35|||||||||
9376|Keepit Conglomerate|36287|4|Described|p277|||||||||
9376|Keepit Conglomerate|36961|6|Mentioned|p208|||See also Fig.3 & Table 1.||||||
9376|Keepit Conglomerate|37803|5|Briefly described|p84|||||||||
9376|Keepit Conglomerate|37987|6|Mentioned|p214|||||||||
9376|Keepit Conglomerate|38222|6|Mentioned|Fig.2|||||||||
9376|Keepit Conglomerate|39214|6|Mentioned|p33|||||||||
9376|Keepit Conglomerate|39331|6|Mentioned|Table 10-1|||||||||
9376|Keepit Conglomerate|39468|6|Mentioned|Fig.2|||||||||
9376|Keepit Conglomerate|40245|6|Mentioned|p199|||Mention Table 2||||||
9376|Keepit Conglomerate|40246|6|Mentioned|p168|||||||||
9376|Keepit Conglomerate|41009|6|Mentioned|p3|||Mention Fig.2||||||
9376|Keepit Conglomerate|41347|6|Mentioned|p357|||||||||
9376|Keepit Conglomerate|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Of the Parry Group.||||||16-DEC-04
9376|Keepit Conglomerate|42547|6|Mentioned|p21|||Devonian Late.||||||
9376|Keepit Conglomerate|42728|6|Mentioned|p5|||||||||
9376|Keepit Conglomerate|42849|4|Described|p540|Late Devonian|Late Devonian|Consists of massive normal and inverse-graded pebble to boulder sized conglom., pebble conglomerate and pebbly and graded sandstone together with mudstone and thinly bedded sandstone. Overlies Mostyn Vale Fm; underlies the Kiah Lmst.Mbr.. See also Fig.1||||||09-MAY-05
9376|Keepit Conglomerate|43091|5|Briefly described|Map legend|||Of Parry Group.||||||25-FEB-08
9376|Keepit Conglomerate|43407|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
9376|Keepit Conglomerate|43409|14|Not recorded|Map Legend||Late Devonian|||||||
9376|Keepit Conglomerate|43417|14|Not recorded|Map Legend|||||||||
9376|Keepit Conglomerate|43418|14|Not recorded|Map Legend|||||||||
9376|Keepit Conglomerate|43428|14|Not recorded|p140|||||||||
9376|Keepit Conglomerate|43429|14|Not recorded|Map Legend|||||||||
9376|Keepit Conglomerate|43434|14|Not recorded|Map Legend||Late Devonian|||||||
9376|Keepit Conglomerate|43435|14|Not recorded|Map Legend|||||||||
9376|Keepit Conglomerate|43436|14|Not recorded|Map Legend||Devonian|(Provisional Edition)||||||
9376|Keepit Conglomerate|43455|14|Not recorded|p458,460||Late Devonian|||||||
9376|Keepit Conglomerate|43461|14|Not recorded|p619||Famennian|(U.Famennian)||||||
9376|Keepit Conglomerate|44093|5|Briefly described|p122|Late Devonian|Late Devonian|||||||
9376|Keepit Conglomerate|47056|6|Mentioned|Fig.2 P523|||||||||
9376|Keepit Conglomerate|50132|6|Mentioned|p247 Fig. 5, p248 Fig.6|Devonian|Devonian|||||Overlies Mostyn Vale Formation. Is overlain by Mandowa Mudstone.||27-MAR-12
9376|Keepit Conglomerate|61392|6|Mentioned|p177 Fig. 4|||||||||07-FEB-11
9376|Keepit Conglomerate|61762|6|Mentioned|p13|Late Devonian|Late Devonian|Geological Province: Tamworth Belt.||||||25-FEB-08
9376|Keepit Conglomerate|61765|6|Mentioned|p58 Fig. 1|||Geological Province: Tamworth Belt.||||||07-FEB-11
9376|Keepit Conglomerate|61769|6|Mentioned|p95, p99 Fig. 4||Late Devonian|||||||
9376|Keepit Conglomerate|65214|6|Mentioned|p280|Devonian|Devonian|NSW, Tamworth and Keepit. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
9376|Keepit Conglomerate|65902|5|Briefly described|p195 Fig.2, p199, p203 Fig.7|Devonian|Devonian|Disconformably overlies Mostyn Vale Formation. Overlain by Mandowa Mudstone.||||||09-MAR-12
9376|Keepit Conglomerate|66720|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Parry Group.|Includes two un-named but separately mapped members: andesitic olistoliths; thinly bedded mudstone and siltstone with minor interbedded lithic sandstone.||Polymictic, pebble to cobble conglomerate; labile lithic and feldspatholithic sandstone; subordinate massive and laminated mudstone; rare local andesite and dacite olistoliths.|
9376|Keepit Conglomerate|68003|5|Briefly described|p32 Fig.3-h, p139. |Famennian|Famennian|Tamworth Belt (North), New England Fold Belt. Repeatedly mis-spelt as Kepit Conglomerate on p139.||Unit in Parry Group.||Overlies Mostyn Vale and Lowanna Formations and Noumea beds. Is overlain by Mandowa Mudstone.|Polymictic pebble to boulder conglomerate, labile lithic and feldspatholithic arenite, subordinate massive and laminated mudstone; tuff; rare local andesite and dacite olistoliths.|
9376|Keepit Conglomerate|68005|5|Briefly described|p49 Fig.3-M, p54, p59, pp148-149, p170.|Late Devonian|Late Devonian|Tamworth Belt. A regional scale marker unit. Formerly the lowermost conglomeratic unit of the Goonoo Goonoo Mudstone (Crook 1961a). Moderate to strong magnetic response.||Unit in Parry Group.||Overlies Mostyn Vale Formation and Eungai Mudstone. Is conformably overlain by Mandowa Mudstone.|Boulder to pebble conglomerate, mudstone and thinly bedded sandstone; andesite.|
9376|Keepit Conglomerate|68731|6|Mentioned|p221|Devonian|Devonian|||||||
9376|Keepit Conglomerate|68822|6|Mentioned|p347|Devonian|Devonian|Upper Devonian timing supported by Korsch et al. (2010) from detrital zircon populations.||||||
9376|Keepit Conglomerate|70907|6|Mentioned|p774 Fig.2|||||||||
9376|Keepit Conglomerate|71628|6|Mentioned|p18:20|||||Parry Group.||||
9376|Keepit Conglomerate|73197|6|Mentioned|p463, p468|Famennian|Famennian|New England Orogen, southern, Tamworth Belt. Possibly contains clasts of Lachlan Orogen quartz arenite, constrains timing of Calliope-Gamilaroi Oceanic Arc accretion. Abrupt increase in zircon abundance compared to older units, age peak at ca 366 Ma (Korsch et al., 2010).|ca 366 Ma U-Pb zircon age peak||||Conglomerate with clasts of quartz arenite.|
9376|Keepit Conglomerate|73264|6|Mentioned|p1396|Famennian|Famennian|Forearc basin. Unimodal 366 Ma zircon peak consistent with Famennian biostratigraphic age.|366 Ma|||||
9376|Keepit Conglomerate|73440|6|Mentioned|p128|Late Devonian|Late Devonian|[Also written as Keepit conglomerate, p128]. Underlain by a regional unconformity. Marks the first input of Gondwanan Lachlan-derived detritus following accretion of the Gamilaroi Siluro-Devonian island arc assemblage.|ca 360 Ma||||Includes quartzite.|
9380|Keginni Conglomerate Member|22857|5|Briefly described|p212, p488 App.1 Tb.A1.7|Devonian|Devonian|Of the Bundycoola Formation. Massive to thickly bedded pebble to cobble polymictic conglomerate. Max. thickness: 200m.||||||
9380|Keginni Conglomerate Member|22859|5|Briefly described|p212|||||||||
9380|Keginni Conglomerate Member|40913|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Early Carboniferous-Late Devonian||||||
9380|Keginni Conglomerate Member|41126|2|Defined|p131|Givetian|Givetian|Mention P22||||||
9380|Keginni Conglomerate Member|43032|6|Mentioned|p190|||Of Bundycoola Formation.||||||08-APR-09
9380|Keginni Conglomerate Member|61213|5|Briefly described|p322|||Of the Bundycoola Formation. Geological Province: Darling Basin.||||||
9380|Keginni Conglomerate Member|64964|4|Described|p159, p163, p169-70|Givetian|Givetian|Marker unit within Bundycoola Formation. Age is mid-Givetian. Displays four paleotrends within its rocks. See also p172.||||||08-APR-09
9380|Keginni Conglomerate Member|67562|6|Mentioned|p96-97, p96, p111|Givetian|Givetian|NE Darling Basin. Mid Givetian age. ~ 100m thick. Represents the NW-most part of a braidplain that is best known S of Cobar.||||||23-JAN-17
9380|Keginni Conglomerate Member|71040|5|Briefly described|p28 Fig.15|Devonian|Devonian|Diagram of major faults and contractional deformation related to Tabberabberan Orogeny.||Bundycoola Formation.||||
9380|Keginni Conglomerate Member|73264|6|Mentioned|p1395 Fig.17, p1402 Fig.23|Late Devonian|Middle Devonian|Lachlan Orogen.||Mulga Downs Group||||
9380|Keginni Conglomerate Member|73457|5|Briefly described|p7|||||Mulga Downs Group|||Polymictic conglomerate.|
9392|Kelle Volcanic Breccia Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Majuba Volcanics (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||
9392|Kelle Volcanic Breccia Member|42566|3|Fully described|p75|||Variation of Kelle Agglomerate Member.||||||
9392|Kelle Volcanic Breccia Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
9408|Kellys Plain Volcanics|22691|6|Mentioned|Fig2 P316||Silurian|||||||
9408|Kellys Plain Volcanics|22857|4|Described|p464 App.1 Tb.A1.6|Early Devonian|Late Silurian|Dacitic and rhyodacite ignimbrites, rhyolite tuffs, agglomerates. Max. thickness: 300m. ||||||
9408|Kellys Plain Volcanics|23309|6|Mentioned|p390|||||||||
9408|Kellys Plain Volcanics|29456|6|Mentioned|p424|||||||||
9408|Kellys Plain Volcanics|33959|6|Mentioned|Fig.234|||Fig.||||||
9408|Kellys Plain Volcanics|36443|5|Briefly described|map legend|Lochkovian|Lochkovian|S-type. Extrusive. Dacite ignimbrite, rhyodacite ignimbrite, tuff, agglomerate, rhyolite. Disconformably underlying Rolling Grounds Latite. BMR map code: Dlk.||||||
9408|Kellys Plain Volcanics|39409|6|Mentioned|Table XVII|||||||||
9408|Kellys Plain Volcanics|40328|3|Fully described|p112|||||||||
9408|Kellys Plain Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
9408|Kellys Plain Volcanics|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|Sdv1||||||
9408|Kellys Plain Volcanics|44093|5|Briefly described|p189 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
9408|Kellys Plain Volcanics|45147|2|Defined|M165|Early Devonian|Late Silurian|Early Devonian, possibly Latest Silurian||||||
9408|Kellys Plain Volcanics|60078|6|Mentioned|Map Legend|Early Devonian|Late Silurian|||||||
9408|Kellys Plain Volcanics|63290|6|Mentioned|p402 Fig. 6(b)|Ordovician|Ordovician|Geological Province: Kiandra Volcanic Belt.||||||
9417|Kembla Sandstone|22578|5|Briefly described|Fig.10 p400, p402|||Of Illawarra Coal Measures.||||||12-MAR-09
9417|Kembla Sandstone|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Sydney Subgroup||||||
9417|Kembla Sandstone|23881|5|Briefly described|p69 Fig. 7.2|||Of the Illawarra Coal Measures.  Geological Province: Sydney Basin.||||||
9417|Kembla Sandstone|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Overlies: Allans Creek Formation. Underlies: Wongawilli Coal.||||||
9417|Kembla Sandstone|24471|4|Described|p31 Fig.3|Late Permian|Late Permian|Overlies Allans Creek Formation. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to Mount Hutton Formation. Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
9417|Kembla Sandstone|29900|6|Mentioned|Table 2|||||||||
9417|Kembla Sandstone|29901|4|Described|Table 1|||||||||
9417|Kembla Sandstone|29944|6|Mentioned|Fig.18|||||||||
9417|Kembla Sandstone|30006|4|Described|p25|||||||||
9417|Kembla Sandstone|31128|6|Mentioned|Table 1|||||||||
9417|Kembla Sandstone|31887|5|Briefly described|p5|||||||||
9417|Kembla Sandstone|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
9417|Kembla Sandstone|32849|6|Mentioned|Table 1|||Permian||||||
9417|Kembla Sandstone|34569|6|Mentioned|p8|||See also Fig.2. Sydney Sub-Group||||||
9417|Kembla Sandstone|36042|6|Mentioned|p28|||||||||
9417|Kembla Sandstone|36220|4|Described|p52|||See also Table 1 & P50||||||
9417|Kembla Sandstone|37089|6|Mentioned|p208|||||||||
9417|Kembla Sandstone|37090|6|Mentioned|Fig.2|||||||||
9417|Kembla Sandstone|39287|6|Mentioned|p40|||||||||
9417|Kembla Sandstone|39309|5|Briefly described|p128|||Isopach map Fig. 7.4||||||
9417|Kembla Sandstone|39661|6|Mentioned|p445|||Replaces Colemans Creek Sandstone||||||
9417|Kembla Sandstone|40631|6|Mentioned|p162|||||||||
9417|Kembla Sandstone|40744|6|Mentioned|Table 1|||||||||
9417|Kembla Sandstone|42787|5|Briefly described|p133|||||||||
9417|Kembla Sandstone|42896|4|Described|p22|||Of Sydney Subgroup.||||||12-MAR-09
9417|Kembla Sandstone|42925|5|Briefly described|Table 18||Late Permian|||||||
9417|Kembla Sandstone|45090|6|Mentioned|p189|||Refers Hanlon (1956)||||||
9417|Kembla Sandstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
9417|Kembla Sandstone|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
9417|Kembla Sandstone|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Allans Creek Formation. Is overlain by Wongawilli Coal.||
9417|Kembla Sandstone|73304|6|Mentioned|p61, p70, p74, p78|Changhsingian|Wuchiapingian|Sydney Basin, southern. Equates approximately with the Wuchiapingian-Changhsingian boundary.||Illawarra Coal Measures||||
9417|Kembla Sandstone|73421|6|Mentioned|p3, p19|Wuchiapingian|Wuchiapingian|Sydney Basin, southern.||Sydney Subgroup||||
9426|Kempsey beds|22736|6|Mentioned|p611 Fig2||Permian|||||||
9426|Kempsey beds|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Lithic sandstone, mudstone, pebbly mudstone; minor conglomerate. Max. Thickness: 2000m.||||||
9426|Kempsey beds|23720|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Lithic sandstone, mudstone, pebbly sandstone, minor conglomerate.||||||15-DEC-04
9426|Kempsey beds|38803|6|Mentioned|p107|||||||||
9426|Kempsey beds|41347|4|Described|Table 7|||||||||
9426|Kempsey beds|41348|5|Briefly described|Map legend|Permian|Carboniferous|Lithic sandstone, mudstone, pebbly sandstone, minor conglomerate.||||||16-DEC-04
9426|Kempsey beds|43755|6|Mentioned|Fig.1,p548||Permian|||||||
9426|Kempsey beds|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|See also p232 and p243 Appendix 1. Geological Province: New England Fold Belt.||||||
9426|Kempsey beds|44450|3|Fully described|p22 Table 4|Early Permian|Late Carboniferous|Geological Province: Nambucca Block. Max. thickness: 2000 m||||||
9426|Kempsey beds|61771|6|Mentioned|p116, p118|Permian|Permian|See also Kempsey Beds.||||||
9426|Kempsey beds|69188|5|Briefly described|p17|Permian|Carboniferous|||||Is intruded by Smokey Cape Adamellite.||
9426|Kempsey beds|70939|6|Mentioned|p824, p826, p830|Permian|Permian|Appears as Kempsey Beds on p830.||||||
9426|Kempsey beds|71628|5|Briefly described|p17: 43, 99, 102|Permian|Carboniferous|||||Is intruded by Yarrahapinni Monzogranite and Smoky Cape Syenogranite.|Includes metamorphosed black pebbly mudstone (hornfels).|
9426|Kempsey beds|72253|6|Mentioned|p98-99|early Permian|early Permian|New England domain.|||||Siliciclastic.|
9449|Kenyu Formation|22679|6|Mentioned|p 13|||||||||
9449|Kenyu Formation|22857|5|Briefly described|p424 App.1 Tb.A1.5|Early Ordovician|Early Ordovician|Of the Kenilworth Group. Porphyritic feldspar andesite, tuff, volcanic arenite.||||||
9449|Kenyu Formation|23214|3|Fully described|p28|Ordovician|Ordovician|Of Kenilworth Group. No type section Geological Province: Lachlan Fold Belt.||||||01-SEP-08
9449|Kenyu Formation|24266|5|Briefly described|p1481|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
9449|Kenyu Formation|24317|5|Briefly described|p14|Late Ordovician|Late Ordovician|||||||
9449|Kenyu Formation|29989|6|Mentioned|Map legend|Silurian|Ordovician|Ordovician-Silurian||||||
9449|Kenyu Formation|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
9449|Kenyu Formation|30731|6|Mentioned|Map legend|Silurian|Ordovician|Ordovician-Silurian||||||
9449|Kenyu Formation|30734|6|Mentioned|p3|||||||||
9449|Kenyu Formation|32088|6|Mentioned|p5|||Refers Packham (1969)||||||
9449|Kenyu Formation|32483|6|Mentioned|p4|||Strat. table 1. Ord.-Sil.||||||
9449|Kenyu Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
9449|Kenyu Formation|33006|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
9449|Kenyu Formation|33282|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
9449|Kenyu Formation|33285|6|Mentioned|p17|||||||||
9449|Kenyu Formation|33875|6|Mentioned|p29|||Uranium prospects.||||||
9449|Kenyu Formation|34404|4|Described|p83|||||||||
9449|Kenyu Formation|39655|6|Mentioned|Plate 1|||||||||
9449|Kenyu Formation|40136|5|Briefly described|p29|||||||||
9449|Kenyu Formation|40328|6|Mentioned|p212|||||||||
9449|Kenyu Formation|41414|6|Mentioned|p340|||||||||
9449|Kenyu Formation|43515|14|Not recorded|Map Legend||Ordovician|(Provisional Edition) See also Lexicon||||||
9449|Kenyu Formation|43516|14|Not recorded|Map Legend||Ordovician|||||||
9449|Kenyu Formation|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Kenilworth Group. Consists of porphyritic feldspar andesite, tuff, volcanic sandstone.||||||15-JUL-08
9449|Kenyu Formation|43782|5|Briefly described|Map Legend|Darriwilian|Yapeenian|Of Kenilworth Group.||||||15-JUL-08
9449|Kenyu Formation|44093|5|Briefly described|p196 App. 1|Early Ordovician|Early Ordovician|Mafic volcanics. Geological Province: Lachlan Fold Belt.||||||
9449|Kenyu Formation|45147|6|Mentioned|M35|||||||||
9449|Kenyu Formation|46524|6|Mentioned|p123|||||||||
9449|Kenyu Formation|50231|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Of the Cabonne Group.||||||
9449|Kenyu Formation|61910|5|Briefly described|p152|Late Ordovician|Late Ordovician|Volcaniclastics and sediments. Geological Province: Lachlan Fold Belt.||||||
9449|Kenyu Formation|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p154|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt, LFB. Age is Gisbornian, and is based on conodonts.||||||07-FEB-11
9449|Kenyu Formation|63283|6|Mentioned|p195 Fig. 2|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
9449|Kenyu Formation|63286|5|Briefly described|p295, p308 Fig. 9|Late Ordovician|Middle Ordovician|Overlain by Walli Volcanics and Cargo Volcanics. Consists of feldspathic turbidites. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
9449|Kenyu Formation|63290|6|Mentioned|p396 Fig. 3|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt.||||||
9449|Kenyu Formation|63293|6|Mentioned|p469 Fig. 2|Gisbornian|Darriwilian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
9449|Kenyu Formation|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Cabonne Group. Includes volcanic mudst+siltst. interbedded with fine-gr.volcaniclastic sst., limest., matrix-supported volcanic conglom., clast supported chert pebble conglom., volcanilithic sst; massive basalt and andesite, + undiff. rocks.||||||
9449|Kenyu Formation|64295|5|Briefly described|p197-204|Late Ordovician|Late Ordovician|Abuts Early-Middle Adaminaby Group, Late Ordovician Bendoc Group and Early Silurian Douro Gp. Faulted against Wyangala Batholith.Intruded by Licking Gully Granite. Volcaniclastic and sedimentary deposits, including allochthonous limestone. ||||||
9449|Kenyu Formation|66185|4|Described|p397, p398 Fig.2, p399|Late Ordovician|Middle Ordovician|Arc-related volcanism. In the Cabonne Group. Contains basaltic pillow lavas, feldspar-phyric andesite, tuffs and volcaniclastic sandstone.||||||
9449|Kenyu Formation|66713|5|Briefly described|p3 Fig.2, p5, p10|Ordovician|Ordovician|Mafic volcaniclastic and sedimentary rocks. In the Molong Volcanic Belt.||||||
9449|Kenyu Formation|67322|5|Briefly described|Fig.5; p24|Sandbian|Sandbian|Stevens (1955). Latest Gisbornian age based on conodonts in the limestone block in its upper part. Occurs in the Cliefden Caves region. ||Of the Cabonne Group.||Correlative of the Walli Volcanics.|Volcanic and volcaniclastic unit.|22-FEB-18
9449|Kenyu Formation|67820|6|Mentioned|p135|Ordovician|Ordovician|Mafic. Fault slivers of this unit in the Frogmore Fault Zone may have been a source of Au and Cu (briefly discussed).||||||
9449|Kenyu Formation|68592|3|Fully described|p370-89, p400, p404, p409, p412-3, p416|Late Ordovician|Late Ordovician|See also p73 Tb.5, p200-1, p263, p437, p442-3, p464, p1866. Stevens (1955); revised by Bartolo (1994) and O'Sullivan (1993); included in Kenilworth Group by Pogson and Watkins (1998). Pogson et al. (2012) here recommend discontinuation of Kenilworth Group, and place Kenyu Formation in Cabonne Group. Thickness over 2000m. Representative section details. Geochemistry in comparison with Mount Darling Basalt is detailed. Geophysical properties detailed. Fossils, esp. conodonts, from allochthonous limestone listed. Quartz veins host minor Cu and Au mineralisation; hosts the Nasdaq Au-Cu skarn deposit (detailed). Lithology described in detail. Yass structural zone: deformation described.||Unit in Cabonne Group.||Is overlain unconformably by Eurimbla Formation and Hawkins Volcanics. Is intruded by Licking Gully and Wyangala Granites.|Greenish-grey, very thinly-bedded, cherty, mafic volcaniclastic siltstone/mudstone; interbedded with volcaniclastic sandstone and massive volcaniclastic conglomerate; subordinate basalt/andesite, mafic ignimbrite; very minor allochthonous limestone.|22-SEP-16
9449|Kenyu Formation|70192|5|Briefly described|Map Legend|Bolindian|Darriwilian|[Theta]cu. Includes four unnamed subunits consisting of: porphyritic, massive to pillowed andesite and basalt. Matrix-clast supported volcaniclastic conglomerate and sandstone. Recrystallised limestone and laminated volcanic mudstone and siltstone. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Cabonne Group|Includes four unnamed units.||Thinly bedded, cherty, mafic volcanic siltstone and mudstone, interbedded with thin-medium bedded, fine grained, basaltic-andesitic sandstone & massive volcaniclastic conglomerate. Massive-pillowed basalt/andesite with intermediate-mafic ignimbrite.|
9449|Kenyu 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. Molong Volcanic Belt.|c. 470-455 Ma|Cabonne Group||||
9449|Kenyu Formation|70545|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes four unnamed subunits consisting of: porphyritic, massive to pillowed andesite and basalt. Matrix-clast supported volcaniclastic conglomerate and sandstone. Recrystallised limestone and laminated volcanic mudstone and siltstone.||Cabonne Group|||Thinly bedded, cherty, mafic volcanic siltstone and mudstone, interbedded with thin-medium bedded, fine grained, basaltic-andesitic sandstone & massive volcaniclastic conglomerate. Massive-pillowed basalt/andesite with intermediate-mafic ignimbrite.|20-SEP-17
9449|Kenyu Formation|70684|6|Mentioned|p3, p34, p75|Late Ordovician|Middle Ordovician|Molong Volcanic Belt.||||||
9449|Kenyu Formation|71656|5|Briefly described|p12 Fig.2, p16|Bolindian|Darriwilian|An allochthonous limestone lens towards the top of the Kenyu Formation hosts numerous documented conodonts. Includes also brachiopods, flat-spired gastropods and hyolithids.||Cabonne Group|||Includes fossiliferous limestone.|
9458|Kerang Sand Member|2967|4|Described|p35, 46|||One line after the first appearance in the text, it appears as Kerang Sand; this [presumed] abbreviation continues in the text; see references (p35, p36 Fig.2.19, p46-47, 80-81, 148).||Parilla Sand.||Locally overlies, and partly intertongues with, the Calivil Formation.||
9458|Kerang Sand Member|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Late Miocene|Of Loxton-Parilla Sand. Geological Province: Murray Basin.||||||13-AUG-07
9458|Kerang Sand Member|22773|5|Briefly described|Fig24.8p352||Late Miocene|||||||
9458|Kerang Sand Member|22782|6|Mentioned|p15|||||||||
9458|Kerang Sand Member|22799|5|Briefly described|p24 Fig.10|Early Pliocene|Late Miocene|||||||
9458|Kerang Sand Member|22857|5|Briefly described|p352 Fig.24.8|Early Pliocene|Late Miocene|Of the Loxton-Parilla Sand? (relationship not clear in figure). Geological Province: Murray Basin.||||||
9458|Kerang Sand Member|22887|5|Briefly described|Fig.6 p13||Late Miocene|||||||
9458|Kerang Sand Member|22893|5|Briefly described|fig4 p9|||||||||
9458|Kerang Sand Member|23884|5|Briefly described|p155 Fig.13.2|Early Pliocene|Late Miocene|Geological Province: Murray Basin.||||||
9458|Kerang Sand Member|34757|6|Mentioned|p50|||||||||
9458|Kerang Sand Member|39329|6|Mentioned|p483|||||||||
9458|Kerang Sand Member|40820|6|Mentioned|Fig.4|||||||||
9458|Kerang Sand Member|42130|6|Mentioned|Fig.3 P265|||||||||
9458|Kerang Sand Member|42134|6|Mentioned|Fig.3 P335|||||||||
9458|Kerang Sand Member|42966|2|Defined|Table 27, p172|Early Pliocene|Late Miocene|of Loxton-Parilla Sands||||||
9458|Kerang Sand Member|43791|6|Mentioned|p372, Fig1|||||||||
9458|Kerang Sand Member|43804|6|Mentioned|Fig.2,p49|||||||||
9458|Kerang Sand Member|49040|6|Mentioned|Fig.6|||||||||
9458|Kerang Sand Member|60452|5|Briefly described|p37|Cenozoic|Cenozoic|Basal unit of the Parilla Sand. Medium to coarse-grained marine quartz sand. Overlain by the Tragowel Member. Maximum Thickness: 30m.||||||19-NOV-08
9458|Kerang Sand Member|65552|5|Briefly described|p5 Fig. 3|Early Pliocene|Late Miocene|Of Loxton-Parilla Sands. Unconformably overlies Geera Clay and Olney Formation. Underlies Tragowel and Wandella Sandstone Members.||||||
9458|Kerang Sand Member|66286|6|Mentioned|p179, 188|||Southern Murray Basin. Transgressive beach facies.||Unit in Loxton-Parilla sands.||Is overlain by Tragowel Member.||
9458|Kerang Sand Member|67179|4|Described|p581|Pliocene|Miocene|Transgressive. Also described as Kerang Sand.||Of Loxton Sand||Underlies by the Tragowel Member.|Coarse-grained quartz sand, swash zone.|
9458|Kerang Sand Member|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Miocene|Shown only on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as underlying and partially equivalent to  Tragowel Member and Bookpurnong beds.|Includes sand.|
9466|Kergunyah Leucitite|34449|4|Described|Table 2-1|||||||||
9490|Khatoun Tonalite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Massive, equigranular tonalite and pyroxene tonalite.||||||21-DEC-04
9490|Khatoun Tonalite|24366|6|Mentioned|p13|||||||||
9490|Khatoun Tonalite|30135|6|Mentioned|Map legend|Permian|Permian|Misspelling of Khartoun Tonalite? Comment added 1993.||||||
9490|Khatoun Tonalite|42866|5|Briefly described|Table 2, P12|||||||||
9490|Khatoun Tonalite|43091|5|Briefly described|Map legend|||||||||
9490|Khatoun Tonalite|62757|6|Mentioned|p13 Fig. 5, p16 Fig.6|||Granitoid pluton of the Uralla Supersuite.||||||07-FEB-11
9490|Khatoun Tonalite|69323|4|Described|p1-3,6,13,41-46,48,70-71, 76|Lopingian|Lopingian|Geological province: New England Orogen. Nomenclature of Chestnut et al., 1973. SHRIMP U-Pb zircon geochronology of GA 2129544 (tonalite) yielded an interpreted (weighted mean 206Pb/238U) magmatic crystallisation age of 253.3+\-1.4 Ma. Sample details, SHRIMP analyses, zircon characteristics and geochronology results are discussed.|253.3+\-1.4 Ma (SHRIMP U-Pb; this study)|Unit of Uralla Suite.||Intrudes into 'Uralla volcanics' and Sandon beds. Intruded by Uralla Granodiorite, Manuka Farm Porphyritic Microtonalite.||03-DEC-19
9490|Khatoun Tonalite|69639|5|Briefly described|p8, p32, 68, p95, p133, p219|Changhsingian|Wuchiapingian|New England Orogen.|253.3 +/- 1.4 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
9490|Khatoun Tonalite|71628|4|Described|p8: 3, 55-62, 72, 75-76, 79|||Binns et al. (1967). Named after a local property. Also appears in the literature as Khartoun (issue of precedence discussed). Forms a small, elongate (~5 x 1.5km) body 7km W of Uralla. Crops out as small boulders or large rounded tors in a narrow depression. Contains numerous metasedimentary pendants. Geochemistry described. Associated with substantial Au-Sb-Ag-base metal mineralisation and minor Au alluvial deposits.|253.3 +/- 1.4 Ma (SHRIMP: Chisholm et al., 2014).|Uralla Suite.||Intrudes Sandon beds and Wandsworth Volcanic Group. Abuts Uralla Granodiorite (possibly gradationally) and Manuka Farm Porphyritic Microgranodiorite (and probably intrudes the latter).|Medium-grained, equigranular hornblende-biotite-(pyroxene) granodiorite to tonalite, with minor pyroxene tonalite; fine-grained, porphyritic chilled margin. Contains abundant sedimentary xenoliths. I-type.|
9503|Kiah Limestone Member|721|5|Briefly described|Map legend|Famennian|Famennian|Of the Mandowa Formation (Parry Group).  Fine-grained, grey, thinly bedded and laminated micritic limestone.||||||
9503|Kiah Limestone Member|22857|5|Briefly described|p496 App.1 Tb.A1.7|Famennian|Fammenian|Of the Mandowa Mudstone (Parry Group). Fine-grained, grey, thinly bedded and laminated micritic limestone. Geological Province: Tamworth Forearc Basin.||||||
9503|Kiah Limestone Member|23185|5|Briefly described|p160|||Equivalent of Borah Limestone (Mory 1981).||||||
9503|Kiah Limestone Member|31999|6|Mentioned|Table 1|||||||||
9503|Kiah Limestone Member|32602|6|Mentioned|p67|||Fauna. Mandowa Mudst. unit||||||
9503|Kiah Limestone Member|32865|6|Mentioned|p481|||||||||
9503|Kiah Limestone Member|34262|6|Mentioned|p243|||||||||
9503|Kiah Limestone Member|34555|3|Fully described|p240|||||||||
9503|Kiah Limestone Member|37987|6|Mentioned|p214|||||||||
9503|Kiah Limestone Member|39331|6|Mentioned|Table 10-1|||||||||
9503|Kiah Limestone Member|41009|6|Mentioned|Fig.2|||||||||
9503|Kiah Limestone Member|41238|6|Mentioned|p83|||||||||
9503|Kiah Limestone Member|42849|6|Mentioned|p541|||Of Mandowa Mudstone. Overlies Keepit Conglomerate.||||||09-MAY-05
9503|Kiah Limestone Member|43091|5|Briefly described|Map legend|||of Parry Group||||||
9503|Kiah Limestone Member|43406|14|Not recorded|p42,45|||Lens within Goonoo Goonoo Mstn (Parry Group)Same unit as Borah Lstn Mbr;Latter name has priority||||||
9503|Kiah Limestone Member|43409|14|Not recorded|Map Legend|||Absent from Gunnedah area||||||
9503|Kiah Limestone Member|43417|14|Not recorded|Map Legend||Late Devonian|Part of Lincount Mudstone||||||
9503|Kiah Limestone Member|43418|14|Not recorded|Map Legend|||||||||
9503|Kiah Limestone Member|43428|14|Not recorded|p141|||||||||
9503|Kiah Limestone Member|45097|6|Mentioned|Fig.|||Late Famennian (Roberts et al., 1972) Correlation chart||||||
9503|Kiah Limestone Member|61765|5|Briefly described|p58 Fig. 1|Middle Devonian|Emsian|Of Mandowa Mudstone. Member is MBR in text. Geological Province: Tamworth Belt.||||||07-FEB-11
9508|Kiama Sandstone Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
9508|Kiama Sandstone Member|22488|5|Briefly described|p841|||||||||
9508|Kiama Sandstone Member|22857|5|Briefly described|p532 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Broughton Formation (Shoalhaven Group). Geological Province: Sydney Basin.||||||
9508|Kiama Sandstone Member|23442|5|Briefly described|p169|||of Broughton Formation||||||
9508|Kiama Sandstone Member|23544|4|Described|Table 1 p360.|||also see p358-59 + Fig 2 p358. Of the Broughton Formation.||||||
9508|Kiama Sandstone Member|23896|3|Fully described|p249, p264 App.1|Late Permian|Late Permian|See also p250 Table 1.  Overlies Blow Hole Latite Member. Geological Province: Sydney Basin.||||||
9508|Kiama Sandstone Member|29900|6|Mentioned|Table 2|||||||||
9508|Kiama Sandstone Member|29901|4|Described|Table 1|||||||||
9508|Kiama Sandstone Member|31128|6|Mentioned|Table 1|||||||||
9508|Kiama Sandstone Member|36220|6|Mentioned|p37|||See also Table 1.||||||
9508|Kiama Sandstone Member|38690|5|Briefly described|p291|||Formerly Kiama Tuff,Kiama Tuff Member & Kiama Sandstone.||||||
9508|Kiama Sandstone Member|39308|5|Briefly described|p517|||||||||
9508|Kiama Sandstone Member|40519|6|Mentioned|Fig.2|||||||||
9508|Kiama Sandstone Member|41580|6|Mentioned|p9|||||||||
9508|Kiama Sandstone Member|41832|6|Mentioned|p569|||||||||
9508|Kiama Sandstone Member|45090|6|Mentioned|p171|||Refers Hanlon et al. (1953)||||||
9508|Kiama Sandstone Member|67500|5|Briefly described|p12, p12 Tb.1, p16|Late Permian|Late Permian|Includes marine bivalves and the Loveleigh palaeosol near base.||Of the Broughton Formation and Gerringong volcanic facies.||Underlain by the Blow Hole Latite Member.|Purple-brown volcaniclastic sandstone with rare marine fossils; Loveleigh palaeosol near base.|01-MAY-12
9508|Kiama Sandstone Member|71115|5|Briefly described|p180, 182, 188|Permian|Permian|Southern Sydney Basin.||Broughton Formation.||Overlies Blow Hole Latite Member. Is overlain by Bumbo Latite Member.||
9508|Kiama Sandstone Member|71542|5|Briefly described|p25,29-30,34|Late Permian|Late Permian|Of southern Sydney Basin. Observed thickness: at least 55m toward the summit of Mount Coolangatta. Shallow marine origin, confirmed by presence of brachiopods. Contains a permafrost paleosol near the base of the unit and provides evidence for a humid frigid climate. Deposited during subsidence and marine transgression onto the Blow Hole Latite Member.||Unit of Broughton Formation.||Overlies Blow Hole Latite Member.|Pinkish brown to red (hematitic) , medium grained, poorly-bedded, silty marine sandstone, bioturbated.|20-OCT-21
9508|Kiama Sandstone Member|73421|6|Mentioned|p18|||||Broughton Formation||Underlies Bumbo Latite, overlies Blowhole Latite Member||
9508|Kiama Sandstone Member|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.||Broughton Formation.||Overlies Blow Hole Latite Member. Is overlain by Bumbo Latite Member.||
9537|Kikoira Granite|22508|5|Briefly described|p2||Ludlow|In the Lachlan Fold Belt. Age: 417 Ma. Keotong Supersuite.||||||26-MAR-08
9537|Kikoira Granite|22638|3|Fully described|p55|Early Devonian|Llandovery|Part of the Kikoira Granite superseded by "Bland Granite". K-Ar date of 417 +/- 13 Ma.||||||
9537|Kikoira Granite|29987|5|Briefly described|p14|||||||||
9537|Kikoira Granite|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
9537|Kikoira Granite|30076|4|Described|p1051|||||||||
9537|Kikoira Granite|32579|6|Mentioned|p37|||||||||
9537|Kikoira Granite|32676|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
9537|Kikoira Granite|34449|6|Mentioned|Table 2-1|||||||||
9537|Kikoira Granite|34544|6|Mentioned|p187|||||||||
9537|Kikoira Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
9537|Kikoira Granite|35608|6|Mentioned|Map legend|Early Devonian|Middle Silurian|Middle Silurian to Early Devonian||||||
9537|Kikoira Granite|35609|6|Mentioned|p19|||||||||
9537|Kikoira Granite|36316|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
9537|Kikoira Granite|39083|6|Mentioned|p30|||||||||
9537|Kikoira Granite|40328|4|Described|p208|||||||||
9537|Kikoira Granite|40678|6|Mentioned|p5|||||||||
9537|Kikoira Granite|42726|5|Briefly described|map legend|Silurian||||||||
9537|Kikoira Granite|43389|14|Not recorded|Map Legend||Silurian|||||||
9537|Kikoira Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
9537|Kikoira Granite|44534|5|Briefly described|map legend|Devonian|Silurian|SI 55-6. Siluri-Dev.||||||
9537|Kikoira Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
9537|Kikoira Granite|50191|5|Briefly described|p6, 32|Early Silurian|Early Silurian|S Type.||||||25-MAY-04
9537|Kikoira Granite|60303|5|Briefly described|p6 Fig. 1, p7|Early Devonian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
9537|Kikoira Granite|61964|3|Fully described|p14 Fig. 4, p37-38, p41 Tb. 2, p43|Early Silurian|Early Silurian|Granite unit formerly within "Kikoira  Suite" (Chappell et al 1991).Now of Koetong Suite.Fractionated, relatively leucocratic: coarse- to medium-grained porphyritic biotite granite, sporadically megacrystic. Age: ~428.2Ma, 417+/-13Ma (K-Ar Jones 1986)  ||||||
9537|Kikoira Granite|62034|5|Briefly described|p26|Silurian|Silurian|Geological Province: Lachlan Orogen.||||||10-APR-06
9537|Kikoira Granite|62367|5|Briefly described|p4 Fig. 2|Early Devonian|Silurian|||||||02-JUN-06
9537|Kikoira Granite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Coarse- to medium-grained porphyritic biotite granite, sporadically megacrystic, feldspar megacrysts to 10cm; abundant schist and quartz  xenoltihs and biotite-rich microgranular enclaves.||||||26-MAR-08
9537|Kikoira Granite|64568|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Coarse- to medium-grained porphyritic granite, sporadically megacrystic, feldspar megacrysts to 9cm;  abundant schistose to quartzitic xenoliths and melancocratic enclaves.||||||23-SEP-08
9537|Kikoira Granite|65469|5|Briefly described|p18|Early Silurian|Early Silurian|Lachlan Orogen.||Koetong Suite||||
9537|Kikoira Granite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian|||Unit in Koetong Suite.|||Coarse-to medium-grained porphyritic granite, sporadically megacrystic, feldspar megacrysts to 9 cm; abundant schistose to quartzitic xenoliths and melanocratic enclaves.|
9537|Kikoira Granite|69161|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Koetong Suite.|||Coarse- to medium-grained porphyritic granite, sporadically megacrystic, feldspar megacrysts to 9 cm; abundant schistose to quartzitic xenoliths and melanocratic enclaves.|
9537|Kikoira Granite|70296|5|Briefly described|p1, p5-6, p10, p24|Llandovery|Llandovery|Cargelligo district. Includes inherited zircon components.|430.2 +/- 3.4 Ma (SHRIMP U-Pb)|Koetong Supersuite|||S-type granite.|21-JAN-21
9537|Kikoira Granite|70777|5|Briefly described|p1, p39, p80|Wenlock|Wenlock|Lachlan Orogen. Age also derived from Colquhoun et al., 2005. |430.2 +/- 3.1 Ma (Black, 2005)|||||
9537|Kikoira Granite|71213|5|Briefly described|p94|Silurian|Silurian|Of Griffin (1957). Intrudes both Ordovician and Silurian rocks. Probably intruded in Bowning Orogeny. Regarded as co-magmatic with Ardlethan Granite, Ungarie Granite. Pre-dates Devonian sediments. Restdown Mining field, Weethalle district, Kikoira-Buddigower district.|||||Medium to coarse-grained  muscovite granite; medium to coarse-grained  biotite-muscovite granite.|25-JUN-17
9537|Kikoira Granite|71364|5|Briefly described|p5, p10|Silurian|Silurian|Wynn (1958, 1960); Griffin (1960).|||||Feldspar-phyric biotite-muscovite granite.|15-FEB-18
9537|Kikoira Granite|71365|5|Briefly described|map legend|||Silurian?|||||Porphyritic biotite granite.|15-FEB-18
9537|Kikoira Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Coarse- to medium-grained porphyritic biotite granite, sporadically megacrystic, feldspar megacrysts to 10cm; abundant schist and quartzite xenoliths and biotite-rich microgranular enclaves.|
9537|Kikoira 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]. At the contact with Ordovician metasediments, a deep, 3km-long alluvial tin lead system was worked, followed by underground mining of deep leads and later open-cut mining.||||||
9545|Kildrummie Formation|13996|6|Mentioned|p129|Silurian|Silurian|Likely of Wenlock age. Knowledge of conodont fauna is currently inadequate. Contains Kockelella ranuliformis (Walliser), as Spathognathodus crispus (Walliser), up to the Ludlow, after its extinction elsewhere around the world.||||||
9545|Kildrummie Formation|22486|6|Mentioned|p 6|||||||||
9545|Kildrummie Formation|22679|6|Mentioned|p 30|||||||||
9545|Kildrummie Formation|23214|5|Briefly described|p14|||Reassigned member status - see Kildrummie Limestone Member of Campbells Formation.||||||
9545|Kildrummie Formation|30453|2|Defined|p59|Late Silurian|Late Silurian|||||||
9545|Kildrummie Formation|35244|6|Mentioned|p36|||||||||
9545|Kildrummie Formation|36390|6|Mentioned|Map legend|Late Silurian|Middle Silurian|Middle to Late Silurian||||||
9545|Kildrummie Formation|37727|4|Described|p66|||See also p8.||||||11-JUN-08
9545|Kildrummie Formation|40328|5|Briefly described|p177|||||||||
9545|Kildrummie Formation|41746|5|Briefly described|p451|||||||||
9545|Kildrummie Formation|41869|6|Mentioned|p9|||||||||
9545|Kildrummie Formation|42413|5|Briefly described|p51|||||||||
9545|Kildrummie Formation|42712|4|Described|8; Table1p14;  p16|Early Devonian|Late Silurian|Within Campbells/Kildrummie Group. Intertongues with Campbells Formation.||||||
9545|Kildrummie Formation|42842|4|Described|p11|||Supersedes Kildrummie Group of De Deckker (1976).||||||
9545|Kildrummie Formation|43263|6|Mentioned|Map Legend|Late Silurian||Age Middle-Late Silurian.||||||
9545|Kildrummie Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Campbells Group. Grey, massive medium-bedded calcareous siltstone and mudstone interbedded in places with well sorted mica-feldspar-quartz sandstone. Grey thickly bedded recrystallised calc-arenite commonly present near base.||||||
9545|Kildrummie Formation|68592|3|Fully described|p142, p425, p611, p614, p632-6, p1886|Ludlow|Wenlock|Originally the Kildrummie Group of Stanton (1956), for a succession of limestone, dolomitic limestone, marl and shale. On the Taralga geological sheet (first edition), Scheibner (1973) incorporated a calcareous unit and overlying non-calcareous sedimentary sequences including Binghams Back Formation, and part of the Cuddyong Formation immediately below Kangaloolah Volcanics. Redefined as Kildrummie Formation by De Decker (1976) who described a type section (location given). Downgraded to Member status (of Campbells Formation) by Pogson and Watkins (1998); here restored to Formation status within a redefined Campbells Group. Named after Kildrummie property, 11km S of Rockley. 200-300m thick. Geophysical properties described. Age from fossils; conodonts described.||Unit in Campbells Group.||Unconformably overlies Jeremy Formation. Is overlain conformably by Cuddyong Formation. Correlated with Cobra and De Drack Formations.|Grey calcareous siltstone and mudstone, massive to well-bedded; locally interbedded with fine to medium-grained, well-sorted mica-feldspar-quartz sandstone; local basal conglomerate; intervals of thickly bedded calc-arenite; small limestone lenses.|
9545|Kildrummie Formation|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sci. On Crookwell and Taralga 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||At base of Campbells Group||Basal unit in Campbells Group. Is overlain by, and interfingers with, Cuddyong Formation.|Massive to thin-medium bedded calcareous siltstone and mudstone interbedded with well sorted, mica-feldspar-quartz sandstone; thickly bedded recrystallised calc-arenite limestone.|
9545|Kildrummie Formation|70297|5|Briefly described|map legend|Silurian|Silurian|Presented as Kildrummie Fm.||||||
9545|Kildrummie Formation|70543|5|Briefly described|Map Legend|Devonian|Silurian|||Campbells Group|||Massive to thin-medium bedded calcareous siltstone and mudstone interbedded with well sorted, mica-feldspar-quartz sandstone; thickly bedded recrystallised calc-arenite limestone.|
9545|Kildrummie Formation|71069|6|Mentioned|p106, p146|||||Campbells Group||Equivalent in part to the Captains Flat Formation and De Drack Formation.||
9545|Kildrummie Formation|71656|5|Briefly described|p13 Fig.2, p27-p28|Wenlock|Wenlock|Conodonts restrict minimum age to mid-Wenlock to Ludlow.||Base of Campbells Group.||Campbells Group. Underlying and partially equivalent to Cuddyong Formation.|Fossiliferous strata.|
9545|Kildrummie Formation|73582|6|Mentioned|p104, 110-112|||Proposed ages discussed.||Campbells Group||||
9552|Kilgower Member|23229|6|Mentioned|p35||Early Devonian|||||||
9552|Kilgower Member|23309|5|Briefly described|p104, 133. Tb 2.38||Early Devonian|||||||
9552|Kilgower Member|23710|14|Not recorded|p84|||Excursion.||||||
9552|Kilgower Member|24551|5|Briefly described|p138, 620||Late Pragian|Of the Tabberabbera Formation.||||||
9552|Kilgower Member|30790|6|Mentioned|p3|||Member Tabberabbera Formation. Early Emsian? age||||||
9552|Kilgower Member|32399|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
9552|Kilgower Member|32583|6|Mentioned|p374|||||||||
9552|Kilgower Member|33326|6|Mentioned|p433|||Fauna.||||||
9552|Kilgower Member|33393|6|Mentioned|p163|||||||||
9552|Kilgower Member|33408|6|Mentioned|p234|||||||||
9552|Kilgower Member|33481|6|Mentioned|p16|||||||||
9552|Kilgower Member|33606|6|Mentioned|p68|||||||||
9552|Kilgower Member|33732|5|Briefly described|Table III|||||||||
9552|Kilgower Member|34250|6|Mentioned|p19|||L.Dev.||||||
9552|Kilgower Member|34251|6|Mentioned|p540|||L.Dev. See also PP545, 547||||||
9552|Kilgower Member|34403|6|Mentioned|p149|||||||||
9552|Kilgower Member|34954|6|Mentioned|Fig.34|||||||||
9552|Kilgower Member|35193|6|Mentioned|p21|||||||||
9552|Kilgower Member|36587|6|Mentioned|p8|||||||||
9552|Kilgower Member|37330|5|Briefly described|p17|||||||||
9552|Kilgower Member|41000|6|Mentioned|p279|||||||||
9552|Kilgower Member|41585|6|Mentioned|Fig.4.9|||||||||
9552|Kilgower Member|42015|6|Mentioned|p316|||||||||
9552|Kilgower Member|42033|6|Mentioned|p653|||||||||
9552|Kilgower Member|42577|5|Briefly described|Fig.3, P28|||||||||
9552|Kilgower Member|43461|14|Not recorded|p628|||Part of Tabberabbera Formation||||||
9552|Kilgower Member|43530|14|Not recorded|p1030|||Part of Wentworth Group||||||
9552|Kilgower Member|43541|14|Not recorded|p263|||||||||
9552|Kilgower Member|43547|14|Not recorded|p150,154||Emsian|Part of Tabberabbera Formation||||||
9552|Kilgower Member|43871|14|Not recorded|p12-55||Early Devonian|||||||
9552|Kilgower Member|47037|6|Mentioned|p114|||||||||
9552|Kilgower Member|48971|6|Mentioned|p10|||See also P40, P24.||||||
9552|Kilgower Member|61161|5|Briefly described|p118|||Of Tabberabbera Formation. Overlies Dead Bull Member. Underlies Roaring Mag Member. Interbedded mudstone and sandstone.||||||
9552|Kilgower Member|70742|6|Mentioned|p173|||Tabberabbera area. Age approximately early Emsian. Contains possible Taungurungetes taggertyensis brachiopods.||||||
9567|Kiloran Conglomerate|45088|6|Mentioned|p12|||Refers Manser (1967,1968)||||||
9576|Kimbriki Formation|22736|6|Mentioned|p611 Fig2||Permian|||||||
9576|Kimbriki Formation|22857|5|Briefly described|p512 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Manning Group. Thickness is some hundred metres. Geological Province: Barnard Basin.||||||
9576|Kimbriki Formation|32944|6|Mentioned|p708|||Permian||||||
9576|Kimbriki Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
9576|Kimbriki Formation|34556|4|Described|p266|||Permian. Manning Group||||||
9576|Kimbriki Formation|35129|5|Briefly described|p49|||||||||
9576|Kimbriki Formation|38685|5|Briefly described|p27|||Geological Province: New England Fold Belt. Overlying Unit: Cedar Party Limestone||||||
9576|Kimbriki Formation|41348|5|Briefly described|Map legend|Permian|Permian|Of the Manning Group.||||||16-DEC-04
9576|Kimbriki Formation|43018|6|Mentioned|p390|||||||||
9576|Kimbriki Formation|43385|14|Not recorded|p179,180||Sakmarian|||||||
9576|Kimbriki Formation|43755|6|Mentioned|Fig.2,p550||Permian|||||||
9617|Kingsfield Formation|22736|6|Mentioned|p629||Tournaisian|||||||
9617|Kingsfield Formation|22857|4|Described|p498 App.1 Tb.A1.7|Tournaisian|Tournaisian|Brown to purple lithic arenite, dark arenite with heavy minerals, dacitic tuff, devitrified ignimbrite, conglomerate and purple shale. Max. thickness: 700m. Geological Province: Tamworth Forearc Basin.||||||
9617|Kingsfield Formation|35245|2|Defined|p19|Early Carboniferous|Early Carboniferous|||||||
9617|Kingsfield Formation|36528|6|Mentioned|p175|||||||||
9617|Kingsfield Formation|38215|6|Mentioned|p276|||||||||
9617|Kingsfield Formation|40883|6|Mentioned|p5|||See also P13||||||
9617|Kingsfield Formation|42547|4|Described|p23|Tournaisian early||||||||
9617|Kingsfield Formation|44244|2|Defined|p21-22|Tournaisian|Tournaisian|Underlies Macqueen Member (Dangarfield Formation).  Max. thickness: c.700m.  Geological Province: Rouchel Block.  Type section in text.||||||11-SEP-12
9617|Kingsfield Formation|50268|5|Briefly described|Map Legend|Tournaisian|Devonian|Underlies: Dangarfield Formation.  Geological Province: Rouchel Block.||||||
9617|Kingsfield Formation|62095|5|Briefly described|p250|Early Carboniferous|Late Devonian|Volcanolithic sandstone, conglomerate, tuffs, minor pyroclastics and siltstone. Geological Province: Rouchel Block/Tamworth Belt.  See also Plate 1.||||||
9617|Kingsfield Formation|63832|6|Mentioned|p131 fig 2|Tournaisian|Tournaisian|Rouchel block, Southern New England Fold Belt. Appears only as the abbreviated Kingsfield & Goonoo Goonoo Formations.||||||
9617|Kingsfield Formation|64571|6|Mentioned|p828|||NSW.||||||15-DEC-08
9617|Kingsfield Formation|64631|6|Mentioned|p44 Fig.2.|Tournaisian|Tournaisian|Southern New England Fold Bel,: Rouchel Block.||||||
9617|Kingsfield Formation|70777|5|Briefly described|p2, p8, p74, p82|Early Carboniferous|Early Carboniferous|New England Orogen.|355.8 +/- 5.6 (SHRIMP, Claoue-Long et al., 1992)|||Overlain by the Waverley Formation.|Volcaniclastic rocks.|
9634|Kirawin Formation|22768|6|Mentioned|p178||Pragian|||||||
9634|Kirawin Formation|22857|4|Described|p178, p462 App.1 Tb.A1.6|Pragian|Pragian|Black shale, siltstone, tuffaceous beds, mudstone. Max. thickness: 1000m. ||||||
9634|Kirawin Formation|24005|5|Briefly described|p292 Fig.1|Early Devonian|Early Devonian|Of Black Range Group. Geological Province: Lachlan Fold Belt||||||
9634|Kirawin Formation|36441|5|Briefly described|map legend|Lochkovian|Lochkovian|Black shale and mudstone. Underlies Sugarloaf Creek Formation; overlies Mountain Creek Volcanics. BMR map code: Dlw.||||||
9634|Kirawin Formation|42497|5|Briefly described|Map Legend|Lochkovian|Lochkovian|||||||
9634|Kirawin Formation|45147|2|Defined|M303|late Lochkovian|late Lochkovian|||||||
9634|Kirawin Formation|50230|4|Described|Map legend|Pragian|Pragian|Of the Black Range Group.  Overlies Mountain Creek Volcanics; underlies Sugarloaf Creek Formation.  Black shale, siltstone, and thin-bedded tuffaceous sandstone.||||||10-MAY-04
9634|Kirawin Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Black Range Group. Contains two unnamed subunits - volcaniclastic conglomerate and a rhyolitic intrusive. Main lithology: black shale, siltstone and thin bedded tuffaceous sandstone.||||||17-JUN-08
9634|Kirawin Formation|66197|5|Briefly described|p631 Fig.3b|||Canberra-Yass Basin. Shallow marine/subaerial clastics. Underlies the Murrumbidgee Group, overlies the Mountain Creek Volcanics.||||||13-MAR-12
9634|Kirawin Formation|67823|6|Mentioned|p363 Fig.7|Pragian|Pragian|Ages from Fig.7(a).|412-c.410 Ma.|||Overlies Mountain Creek Volcanics. Is overlain by Murrumbidgee Group.||
9634|Kirawin Formation|68592|2|Defined|p196, p236, p926-30, p969-74|Pragian|Pragian|Originally Kirawin Shale (Best et al., 1964); changed to Kirawin Formation by Pedder et al. (1970) and used since, as it includes other lithologies. Named after Kirawin property. Type section and a more inclusive representative section are described. 220-1000m thick. Geophysical properties described. Extremely sparse fossils: none age-diagnostic; age from surrounding units. Associated with the Harpers Find Au-Ag occurrence and hosts the Woolgarlo lead-fluorite-Cu deposit.||Unit in Black Range Group.||Conformably and gradationally overlies Mountain Creek Volcanics. Is overlain conformably and gradationally by Sugarloaf Creek Formation. Is intruded by Gooramma Suite sills.|Black or dark green, massive to well-laminated mudstone or shale with thin volcaniclastic interbeds of fine-grained silty sandstone and minor lenses of pebble- to granule-conglomerate and pebbly sandstone; rare silty limestone lenses; rhyolite sill.|
9634|Kirawin Formation|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dbk. Includes two unnamed members; massive, volcaniclastic pebble to granule conglomerate and sandstone, massive, fine grained rhyolite intrusion. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Black Range Group|Includes two unnamed members.|Is overlain by Sugarloaf Creek Formation. Overlies Mountain Creek Volcanics.|Massive-well laminated mudstone or shale, thin interbeds of fine grained, silty, volcaniclastic sandstone, minor lenses of volcaniclastic, pebble to granule conglomerate and pebbly sandstone, rare lenses of silty limestone.|
9634|Kirawin Formation|70540|5|Briefly described|Map Legend|Devonian|Devonian|Includes two unnamed members; massive,volcaniclastic pebble to granule conglomerate and sandstone, massive, fine grained rhyolitie intrusion.||Black Range Group|Includes two unnamed members.||Massive-well laminated mudstone or shale, thin interbeds of fine grained, silty, volcaniclastic sandstone, minor lenses of volcaniclastic, pebble to granule conglomerate and pebbly sandstone, rare lenses of silty limestone.|
9634|Kirawin Formation|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Massive to well laminated mudstone or shale, thin interbeds of fine grained, silty, volcaniclastic sandstone, minor lenses of volcaniclastic, pebble to granule conglomerate and pebbly sandstone. Rare lenses of silty limestone.|
9634|Kirawin Formation|71656|5|Briefly described|p12 Fig.2, p31|Pragian|Pragian|Formation probably identified by a terrestrial myriapod arthropod 'Maldybulakia angusi'.||Black Range Group||Overlies Mountain Creek Volcanics, underlies Sugarloaf Creek Formation.|Fossiliferous strata.|
9634|Kirawin Formation|73215|5|Briefly described|p994|||Talmo-Taemas area.||||Overlies Mountain Creek Volcanics. Is overlain by Cavan Bluff Limestone.||
9701|Koetong Granite|22508|5|Briefly described|p2||Silurian|Keotong Supersuite, Lachlan Fold Belt||||||
9701|Koetong Granite|22968|6|Mentioned|P19|||||||||
9701|Koetong Granite|23309|5|Briefly described|p296, 298, 343, 346, 350.||Late Silurian|G101 S-Type. Age: 421 Ma, 418+/-4 Ma, 419+/- 6 Ma. Supersedes Koetong Granodiorite.||||||
9701|Koetong Granite|23547|5|Briefly described|p554|||||||||
9701|Koetong Granite|24133|3|Fully described|p62|Silurian|Silurian|Age: 419+/-6Ma (U-Pb); 418+/-4Ma (Rb-Sr).   Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
9701|Koetong Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Two mica cordierite granite: bluish grey, coarse grained biotite muscovite granite; mostly equigranular but centre is porphyritic & parts of margins are fine grained; locally abundant enclaves; S-type; nonmagnetic||||||09-SEP-04
9701|Koetong Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Age: 419 +/- 6 Ma (U/Pb), 418 +/- 4 Ma (Rb/Sr). Biotite-muscovite-cordierite-granite: S-type; nonmagnetic; variable K, moderate-low Th, variable U||||||09-SEP-04
9701|Koetong Granite|24438|6|Mentioned|p14|||Radiometric response false anomaly is probably due to pine tree plantations.||||||10-JUN-14
9701|Koetong Granite|24551|6|Mentioned|p232 Fig. 8.17|||||||||
9701|Koetong Granite|29953|4|Described|p3|||||||||
9701|Koetong Granite|31800|6|Mentioned|p203|||||||||
9701|Koetong Granite|32684|6|Mentioned|p250|||See also Fig.2||||||
9701|Koetong Granite|35257|6|Mentioned|p11|||See also P154.||||||
9701|Koetong Granite|35278|4|Described|p358|||||||||
9701|Koetong Granite|37871|4|Described|p8|||||||||
9701|Koetong Granite|38335|6|Mentioned|p1728|||||||||
9701|Koetong Granite|39858|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
9701|Koetong Granite|39860|6|Mentioned|p17|||See also P42||||||
9701|Koetong Granite|40328|6|Mentioned|p204|||||||||
9701|Koetong Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
9701|Koetong Granite|40498|6|Mentioned|p392|||||||||
9701|Koetong Granite|40761|6|Mentioned|p242|||||||||
9701|Koetong Granite|41433|6|Mentioned|Fig.3|||||||||
9701|Koetong Granite|41572|6|Mentioned|p19|||||||||
9701|Koetong Granite|41868|6|Mentioned|p586|||||||||
9701|Koetong Granite|42089|6|Mentioned|p16|||||||||
9701|Koetong Granite|42726|5|Briefly described|map legend|Silurian||||||||
9701|Koetong Granite|42827|5|Briefly described|p586|||||||||
9701|Koetong Granite|64571|6|Mentioned|p825|Early Silurian|Early Silurian|||||||
9701|Koetong Granite|68116|5|Briefly described|Appendix, Map 20.|Lochkovian|Ludlow||||||Two-mica cordierite granite: bluish grey, coarse grained biotite muscovite granite; mostly equigranular but centre is porphyritic and parts of margins are fine grained; locally abundant metasedimentary enclaves; S-type; nonmagnetic.|
9701|Koetong Granite|68310|6|Mentioned|p241-242|||Wagga Batholith. Geochemical plots of schistose enclaves.|||||S-type granite.|
9701|Koetong Granite|70910|14|Not recorded|p43|||Gneissic granite.||||||
9701|Koetong Granite|73264|6|Mentioned|p1392|||S-type granite.||||||
9703|Koetong Suite|22778|5|Briefly described|p 159|||||||||
9703|Koetong Suite|23439|5|Briefly described|p124 fig.1|||||||||
9703|Koetong Suite|23549|5|Briefly described|p523.|||The major component of the Koetong Supersuite. S-type granite. Geological Province:  Wagga Batholith in the Lachlan Fold Belt.||||||05-APR-05
9703|Koetong Suite|23550|5|Briefly described|p502|||S-type granite. Lachlan Fold Belt.||||||
9703|Koetong Suite|23551|6|Mentioned|p491|||||||||
9703|Koetong Suite|24514|5|Briefly described|p29|||Felsic S-type granites.||||||
9703|Koetong Suite|24551|6|Mentioned|p233|||||||||
9703|Koetong Suite|41898|6|Mentioned|p1182|||||||||
9703|Koetong Suite|42726|5|Briefly described|map legend||Silurian|||||||
9703|Koetong Suite|42827|6|Mentioned|p432|||||||||
9703|Koetong Suite|44093|5|Briefly described|p170 App. 1|Late Silurian|Silurian|Max age: Middle Silurian. In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||
9703|Koetong Suite|61964|3|Fully described|p14 Fig. 4, p37|Middle Silurian|Early Silurian|Of Koetong Supersuite.Incorporates former "Ungarie Suite (mafic) + felsic "Kikoira Suite" (Chappell et al 1991). Now includes; Erigolia, Eura Bonny, Weethalle, Kikoira, Yalgongrin + Ungarie Granites + Cookaburragong Granodiorite. Lith.details included||||||
9703|Koetong Suite|62405|5|Briefly described|Map legend|Silurian|Silurian|Includes: Ugalong Dacite, Cookaburragong Granodiorite, Erigolia, Eura Bonny, Weethalle, Yalgogrin, Ungarie (and its Derrida Phase) and Kikoira Granites.||||||26-MAR-08
9703|Koetong Suite|63290|6|Mentioned|p399|Early Silurian|Early Silurian|Age: ca 432Ma (Colquhoun et al. 2005). Granites.||||||
9703|Koetong Suite|64568|5|Briefly described|Map legend|Silurian|Silurian|Includes Ungarie Granite, Cookaburragong Granodiorite, Kinoira Granite and Ugalong Dacite.||||||
9703|Koetong Suite|65469|5|Briefly described|p15, p18|Middle Silurian|Early Silurian|Lachlan Orogen.|432 Ma (Colquhoun et al., 2005)||Includes the Thule Granite, Ungarie Granite, Ugalong Dacite, Cookaburragong Granodiorite and Kikoira Granite.|Intrudes the Wagga Group.||
9703|Koetong Suite|67060|5|Briefly described|p503, p505 Table 1.|||Of the Wagga Batholith. S-type.  Includes Wantabagdery/Wantabadgery,  Mount Flakney, Granya plutons.|435.8 +/- 4.4 to 432.3 +/- 4.3 Ma.||||Ranges from granodiorite rich in mafic minerals to highly-fractionated Sn-mineralised leucogranites.|13-JUN-13
9703|Koetong Suite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian||||Includes Ugalong, Eura Bonny, Weethalle, Yalgogrin, Ungarie and Kikoira Granites.|||
9703|Koetong Suite|69161|5|Briefly described|Map legend|Silurian|Silurian||||Includes Erigolia and Kikoira Granites.|||
9703|Koetong Suite|69801|6|Mentioned|p32, p85, p91, p122, p135|||Central Lachlan Orogen. Incorporates the Grong Grong Granite of the former Grong Grong Suite.||Koetong Supersuite|Includes the Woomargama Granite, the Grong Grong Granite and the Granya Granite.|||
9703|Koetong Suite|70777|6|Mentioned|p39, p52-p53, p79|||||Koetong Supersuite||||
9703|Koetong Suite|71039|6|Mentioned|p6|Silurian|Silurian|||||||
9703|Koetong Suite|71069|6|Mentioned|p75|||||||||
9704|Koetong Supersuite|22508|5|Briefly described|p2||Silurian|Lachlan Fold Belt||||||
9704|Koetong Supersuite|22606|6|Mentioned|P830|||||||||
9704|Koetong Supersuite|23309|5|Briefly described|p346|||Comprises of Corryong Granite (G92) and Mount Willis Granite (G111).||||||
9704|Koetong Supersuite|23547|5|Briefly described|p554|||||||||
9704|Koetong Supersuite|23549|4|Described|Fig 2 p517, p523|||S-Type granites within the Wagga Batholith. The major component is the Koetong Suite.  Geological Province: Lachlan Fold Belt.||||||05-APR-05
9704|Koetong Supersuite|24133|6|Mentioned|p57|||Geological Province: Lachlan Fold Belt.||||||
9704|Koetong Supersuite|24222|5|Briefly described|p4|||S-type.  See also Koetong supersuite.   Geological Province: Lachlan Fold Belt.||||||24-JAN-06
9704|Koetong Supersuite|24263|6|Mentioned|p1394|||Geological Province: Wagga Belt||||||
9704|Koetong Supersuite|24270|6|Mentioned|p1608|||Geological Province: Wagga tin belt.||||||
9704|Koetong Supersuite|24271|6|Mentioned|p1621|||Geological Province: Lachlan Fold Belt.||||||
9704|Koetong Supersuite|24512|6|Mentioned|p5|||Geological Province: Lachlan Orogen.||||||
9704|Koetong Supersuite|41563|6|Mentioned|p514|||||||||
9704|Koetong Supersuite|42726|5|Briefly described|map legend|||||||||
9704|Koetong Supersuite|61964|4|Described|p14 Fig. 4, p37|Middle Silurian|Early Silurian| Well-defined group of high-K, peraluminous, S-type granites extending from northern Victoria to Cargelligo area.  Age: c.432Ma.  For geophysics of suite - see p222||||||
9704|Koetong Supersuite|62367|5|Briefly described|p10|Early Silurian|Early Silurian|Includes the Ungarie Granite. Fractionated S-type granites.||||||31-MAY-06
9704|Koetong Supersuite|65469|6|Mentioned|p16, p17|||Lachlan Orogen.||||||
9704|Koetong Supersuite|69043|5|Briefly described|p1, p24, p28, p30, p34, p44|Silurian|Silurian|Indistinguishable age from that of the Mine Granite (this study) of 428.1 +/- 2.8 Ma.|c.433-c.427 Ma (Black,2005; Colquhoun et al.,2005)||Kyeamba Suite; Mine Granite.||S-type.|
9704|Koetong Supersuite|69511|6|Mentioned|p1-2|Silurian|Silurian||c.427 Ma.|||||
9704|Koetong Supersuite|69798|6|Mentioned|p6|||||||||
9704|Koetong Supersuite|69801|6|Mentioned|p1-p2, p18, p39, p85, p91, p135-137|||Central Lachlan Orogen.|||Includes the Koetong Suite and the Tom Groggin Suite.|Intruded by the Holbrook Granite.||
9704|Koetong Supersuite|70296|6|Mentioned|p1, p10|Llandovery|Llandovery||||Includes the Kikoira Granite, Yalgogrin Granite and the Erigolia Granite.|||
9704|Koetong Supersuite|70777|5|Briefly described|p1, p39, p52, p79-p80|||Lachlan Orogen.|||Includes the Koetong Suite, Yalgogrin Granite, Wargin Granite, Ungarie Granite and the Buddigower Granite.|||
9704|Koetong Supersuite|71039|6|Mentioned|p6|Silurian|Silurian|||||||
9704|Koetong Supersuite|71345|6|Mentioned|p26|||Occurs to the south of the Wilgaroon Granite.|||||S-type granitic rocks.|
9704|Koetong Supersuite|71693|5|Briefly described|Map legend.|Silurian|Silurian||||Ungarie, Currah, Yalgogrin, Weethalle, Eura Bonny, Nyora, Erigolia, Kikoira Granites; Ugalong Dacite.||Coarse- to medium-grained equigranular to porphyritic biotite +/- cordierite and muscovite granite and granodiorite with locally abundant metasedimentary xenoliths. Felsic fractionated members usually tourmaline-bearing.|
9801|Koorainghat beds|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|||||||16-DEC-04
9803|Koorawatha Formation|22638|4|Described|p72|||Of the Cookamidgera Subgroup. Thickness: 300 m.||||||25-JUN-08
9803|Koorawatha Formation|22857|5|Briefly described|p490 App.1 Tb.A1.7|Devonian|Devonian|Of the Hervey Group. Red siltstone and shale, minor medium-grained red sandstone. Max. thickness: 300m. Geological Province: Hervey Basin.||||||
9803|Koorawatha Formation|29989|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
9803|Koorawatha Formation|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
9803|Koorawatha Formation|32483|4|Described|p38|||Upper Devonian. Strat. table 1||||||25-JUN-08
9803|Koorawatha Formation|35608|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
9803|Koorawatha Formation|43507|2|Defined|p128,130,161,162||Late Devonian|Formation of Cookamidgera Subgroup (Hervey Group).||||||25-JUN-08
9803|Koorawatha Formation|43510|2|Defined|p41-2,63-5,67|||||||||
9803|Koorawatha Formation|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
9803|Koorawatha Formation|44936|5|Briefly described|Map Legend||Late Devonian|Of the Hervey Group.||||||25-JUN-08
9803|Koorawatha Formation|50231|5|Briefly described|Map Legend|Famennian|Famennian|Of the Cookamidgera Subgroup (Hervey Group).  Overlies Bumberry Formation.||||||25-JUN-08
9803|Koorawatha Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Cookamidgera Subgroup (Hervey Group). Red to fawn, thin to medium bedded, well-sorted, planar-laminated and ripple x-laminated, interbedded. fine-grained lithic-quartz sst + red siltstone, with minor interbeds of white, thin-bedded, fine-gr. qtz sst.||||||
9803|Koorawatha Formation|68592|2|Defined|p35, p1698, p1701, p1718-21, p1753|Late Devonian|Late Devonian|Conolly (1965), after the town of Koorawatha. Poor outcrop: type area (not section) and representative exposures described. Up to 650m thick. Geophysical properties briefly described. No fossils known. Late Famennian age inferred from surrounding units.||Topmost unit in Hervey Group.||Conformably overlies Bumberry and Mandagery Formations. Equivalent to Eurow and Tarlo Formations.|Monotonous, interbedded sequence of red, thin- to medium-bedded, planar-laminated and ripple cross-laminated siltstone, and red to fawn, fine-grained lithic-quartz sandstone with rare interbeds of white, thin-bedded, fine-grained quartzose sandstone.|
9803|Koorawatha Formation|70192|5|Briefly described|Map Legend|Famennian|Famennian|Dhk. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hervey Group||Overlies Bumberry Formation.|Thin to medium bedded, well sorted, planar and ripple cross laminated, interbedded fine-grained, lithic quartz sandstone and siltstone with minor interbeds of thinly bedded, fine grained quartzose sandstone.|
9803|Koorawatha Formation|70545|5|Briefly described|Map Legend|Devonian|Devonian|||Hervey Group|||Thin to medium bedded, well sorted, planar and ripple cross laminated, interbedded fine-grained, lithic quartz sandstone and siltstone with minor interbeds of thinly bedded, fine grained quartzose sandstone.|
9803|Koorawatha Formation|71656|6|Mentioned|p12 Fig.2|Famennian|Famennian|Shown only in correlation chart (Fig.2).||Top of Hervey Group||Overlies Bumberry Formation.||
9831|Kosciusko Granite|29860|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
9831|Kosciusko Granite|29953|6|Mentioned|p3|||||||||
9831|Kosciusko Granite|31800|6|Mentioned|p203|||||||||
9831|Kosciusko Granite|33606|5|Briefly described|p70|||||||||
9831|Kosciusko Granite|34367|6|Mentioned|p570|||Pebbles in moraine||||||
9831|Kosciusko Granite|34400|6|Mentioned|p7|||Associated with Bowning Orogeny.||||||
9831|Kosciusko Granite|36602|6|Mentioned|p115|||||||||
9831|Kosciusko Granite|38064|6|Mentioned|p39|||||||||
9831|Kosciusko Granite|43344|14|Not recorded|p8|||Associated with Bowning Orogeny||||||
9831|Kosciusko Granite|45087|6|Mentioned|p31|||Chemical analyses||||||
9831|Kosciusko Granite|60007|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Included in undifferentiated granites of the Kosciusko Batholith.||||||
9831|Kosciusko Granite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
9831|Kosciusko Granite|70910|14|Not recorded|p44|||Stratigraphic confirmation of K-Ar ages.||||||
9839|Koukandowie Formation|12597|5|Briefly described|p491, p492 Tb.1|Bathonian|Toarcian|Clarence-Moreton Basin. 250m thick. Generally fluviatile. Basal claystones include (shallow lacustrine?) chamositic oolite beds containing acritarch-bearing horizons.||Unit in Marburg Subgroup.|||Predominantly arenaceous: fine- to coarse-grained quartzose to quartz-lithic sandstone, with a variable sandstone/siltstone/shale sequence at the base.|
9839|Koukandowie Formation|13516|5|Briefly described|p159 fig 8|Jurassic|Jurassic|From Clarence-Moreton Basin.||Of Marburg Subgroup|Includes Ma Ma Creek Member, Heifer Creek Sandstone Member|||
9839|Koukandowie Formation|22857|5|Briefly described|p318-9 Figs. 22.10 A, B; p548 Tb A1.12|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Interbedded sandstone, siltstone, claystone, coal. Contains the Heifer Creek Sandstone, Ma Ma Creek and Towallum Members. Max. thickness: 400m. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|22865|6|Mentioned|Fig.22.10ap318|||||||||
9839|Koukandowie Formation|23799|4|Described|p48, p10 Tb. 1|Middle Jurassic|Early Jurassic|Upper unit of Marburg Subgroup (Bundamba Group).  Includes Ma Ma Creek and Heifer Creek Sandstone Members.  Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Marburg Subgroup.||||||
9839|Koukandowie Formation|23811|5|Briefly described|Map Legend|Bajocian|Aalenian|Of Marburg Subgroup.  Fine- to coarse-grained, quartz to quartz-lithic sandstone in fining-up sequences.  Crossbedded and rippled; thin pebble conglomerates at base of sand channels; shale and siltstone.  Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
9839|Koukandowie Formation|23812|5|Briefly described|p34 Tb.4|Middle Jurassic|Early Jurassic|Of Bundamba Group.  Maximum thickness: 400m. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Early Jurassic|Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Marburg Subgroup (Bundamba Group).||||||
9839|Koukandowie Formation|41631|4|Described|p18|||See also Fig.2||||||
9839|Koukandowie Formation|42248|2|Defined|App.1 p410|Bajocian|Toarcian|Age: late Toarcian to early Bajocian.||||||21-NOV-21
9839|Koukandowie Formation|42463|6|Mentioned|Fig.3 P170|||||||||
9839|Koukandowie Formation|42869|5|Briefly described|Table 1, P33|||of Marburg Subgroup||||||
9839|Koukandowie Formation|42893|6|Mentioned|p11|||||||||
9839|Koukandowie Formation|42951|5|Briefly described|Fig.11|||Of Marburg Subgroup.||||||27-AUG-08
9839|Koukandowie Formation|43150|5|Briefly described|Map Legend||Jurassic|Of the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||12-APR-05
9839|Koukandowie Formation|43736|5|Briefly described|Table 1,p4|||||||||
9839|Koukandowie Formation|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Marburg Subgroup.  Overlies: Gatton Sandstone.  Underlies: Walloon Coal Measures, Main Range Volcanics.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
9839|Koukandowie Formation|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
9839|Koukandowie Formation|60281|5|Briefly described|p22, Fig.18 App.1|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group).  Contains the Heifer Creek Sandstone and Ma Ma Creek Members, and Towallum Basalt. Overlies the Gatton Sandstone; underlies the Walloon C.M.  Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60993|3|Fully described|p6 Fig. 2, p27|||Supersedes Koukandowie Sst Mbr. Mixed sandstone, siltstone and shale unit. Conformably overlain by Walloon Coal Measures; conformably overlies Gatton Sst. Max. thickness: ~345m. Geol. Prov: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60995|4|Described|p65-66, p51 Fig. 3|Early Jurassic|Early Jurassic|Of Marburg Subgroup. Originally called "Marburg Formation" in NSW.  Interbedded sandstone, siltstone, claystone, coal; detailed lithology presented (p66).  Max. thickness: 400m. Geological Province: Clarence-Moreton Basin. ||||||
9839|Koukandowie Formation|60996|5|Briefly described|p72, p113|||Of the Marburg Subgroup (Bundamba Group). Contains the Ma Ma Creek Member and heifer Creek Sandstone Member. Conformably overlies Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60997|5|Briefly described|p138|Callovian|Toarcian|Conformably overlies Gatton Sandstone; conformably overlain by Walloon C.M. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1, p140 Fig. 2.||||||
9839|Koukandowie Formation|60998|5|Briefly described|p146 Fig. 2|||Of the Marburg Subgroup. Overlies the Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|60999|5|Briefly described|p164, p174|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6, p176-177.||||||
9839|Koukandowie Formation|61001|6|Mentioned|p189|||Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|61002|6|Mentioned|p202|||Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|61004|5|Briefly described|p230, p232 Fig. 2|Jurassic|Jurassic|Of the Marburg Subgroup (Bundamba Group). Oil mature unit in the western and central parts of NSW.  Geological Province: Clarence-Moreton Basin.||||||
9839|Koukandowie Formation|61005|5|Briefly described|p242|||See also p255 Figs. 23, 24 and 25. ||||||
9839|Koukandowie Formation|61006|5|Briefly described|p277, p289|Jurassic|Jurassic|Includes the Ma Ma Creek and Heifer Creek Members. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285.||||||
9839|Koukandowie Formation|63748|5|Briefly described|p21|||Top part of Marburg Subgroup (Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
9839|Koukandowie Formation|64289|5|Briefly described|p6 Fig. 2|Middle Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Includes the Ma Ma Creek and Heifer Creek Members. Overlies Gatton Sandstone. Max. thickness: 250m. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
9839|Koukandowie Formation|64665|5|Briefly described|p53 Fig.2, p59.|Middle Jurassic|Early Jurassic|Clarence-Moreton Basin.||Upper unit in Marburg Subgroup.|Includes Ma Ma Creek Member and Heifer Creek Sandstone Member.|Overlies Gatton Sandstone. Is overlain by Walloon Coal Measures.||
9839|Koukandowie Formation|67402|5|Briefly described|p165 tbl LPB1|Aalenian|Sinemurian|Clarence-Moreton Basin. Deposited in fresh water lakes or lagoon environments. In excess of 150m thick. See also p188, p190, p190 fig CLM6, p193.||Marburg Subgroup|Includes the Ma Ma Creek Member and the Heifer Creek Sandstone Member.|Overlies the Gatton Sandstone. Overlain by the Walloon Subgroup.|Sandstone, siltstone and shale.|
9839|Koukandowie Formation|68135|5|Briefly described|p52 fig 2b|Bajocian|Pleinsbachian|Clarence-Moreton Basin. Includes plant macrofossils and invertebrate fossils. ||||Overlies Gatton Sandstone, overlain by Walloon Coal Measures|Silty sandstone with oolitic ironstone beds.|14-SEP-17
9839|Koukandowie Formation|69297|5|Briefly described|p487 fig 5.38, p488, p489, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 50-400m thick. Deposited as overbank or flood plain deposits as part of a meandering fluvial system. Good potential as a hydrocarbon source rock.  ||Mauburg Subgroup|Includes the Heifer Creek Sandstone Member, Ma Ma Creek Member and the Towallum Basalt.|||
9839|Koukandowie Formation|69594|4|Described|p519, p536 Fig.7.17, p544-547, p572|Toarcian|Toarcian|Clarence-Moreton Basin. Weakly sinuous river deposits with linguoid bars. Appears as Koukandouie Formation in Fig.7.17.||Marburg Subgroup.|Heifer Creek Sandstone Member, Ma Ma Creek Member.|Overlies Gatton Sandstone. Is overlain by Walloon Coal Measures.|Mixed sandstone, siltstone and shale; near the base in the head of the Lockyer Valley is a 25m unnamed member of stacked quartz-lithic channel-sandstones with planar and trough cross-bed sets interpreted as dunes, transverse bars and sand waves.|
9839|Koukandowie Formation|69790|5|Briefly described|p1063 Fig.2|Middle Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Marburg Subgroup.|Includes Ma Ma Creek, and Heifer Creek Sandstone, Members.|||
9839|Koukandowie Formation|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
9839|Koukandowie Formation|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Marburg Subgroup.|Ma Ma Creek Member, Heifer Creek Sandstone Member.|Overlies Gatton Sandstone. Is overlain by Walloon Coal Measures.||
9839|Koukandowie Formation|71805|5|Briefly described|p76|Bajocian|Pleinsbachian|Clarence-Moreton Basin.||Marburg Subgroup|Includes the Ma Ma Creek Member and the Heifer Creek Sandstone Member.|||
9839|Koukandowie Formation|72921|5|Briefly described|p15 Fig.2.|Middle Jurassic|Early Jurassic|Shown as located within the Clarence-Moreton Basin. Along with Evergreen Formaiton, shown as including the Westgrove Ironstone Member in Fig.2.||||Overlies Gatton Sandstone and underlies Walloon Coal Measures||10-JUN-22
9839|Koukandowie Formation|73570|6|Mentioned|p912 Fig.2, p913-914, p915 Fig.4|Middle Jurassic|Middle Jurassic|Clarence-Morton Basin.||||||
9844|Kow Sand|2967|5|Briefly described|p67-68|||Thorne and Macumber (1969). Kow Swamp, northern Victoria,|||||Wind-blown sand forming a low dune on the SE shoreline of Kow Swamp.|
9844|Kow Sand|31385|6|Mentioned|Table 5|||||||||
9844|Kow Sand|31954|4|Described|p10|||||||||
9844|Kow Sand|31957|4|Described|p312|||Mention P309||||||
9844|Kow Sand|32232|6|Mentioned|p19|||||||||
9844|Kow Sand|33486|6|Mentioned|p316|||||||||
9844|Kow Sand|42966|5|Briefly described|p407|||||||||
9854|Kuark Metamorphic Complex|22708|6|Mentioned|p210|||||||||
9854|Kuark Metamorphic Complex|22721|6|Mentioned|Fig.1 p502|||||||||
9854|Kuark Metamorphic Complex|22794|5|Briefly described|p65|||||||||
9854|Kuark Metamorphic Complex|22876|5|Briefly described|p14|||||||||
9854|Kuark Metamorphic Complex|22878|6|Mentioned|p8|||||||||
9854|Kuark Metamorphic Complex|22879|5|Briefly described|map|Silurian|Silurian|||||||
9854|Kuark Metamorphic Complex|22880|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Ino Creek Granodiorite, Kanuka Granodiorite, Irondoon Granodiorite||||||01-OCT-04
9854|Kuark Metamorphic Complex|23309|5|Briefly described|p67-69, 312-313|||||||||
9854|Kuark Metamorphic Complex|23938|5|Briefly described|p31-32 Fig. 12|Middle Ordovician|Early Ordovician|See also p139 Tb. 1 Appendix.||||||09-DEC-08
9854|Kuark Metamorphic Complex|24004|6|Mentioned|p285 Fig.6|||||||||
9854|Kuark Metamorphic Complex|24310|5|Briefly described|p1044|||Geological Province: Lachlan Fold Belt||||||
9854|Kuark Metamorphic Complex|24551|6|Mentioned|p47 Fig. 2.58|Lower Silurian|Lower Silurian|||||||
9854|Kuark Metamorphic Complex|42627|5|Briefly described|Map legend|Silurian|Silurian|Variation on Kuark Metamorphics.||||||
9854|Kuark Metamorphic Complex|42647|3|Fully described|p50|||Supersedes Kuark Metamorphics. Derived from Pinnak Sandstone.||||||
9854|Kuark Metamorphic Complex|43314|5|Briefly described|Map Legend|||||||||
9854|Kuark Metamorphic Complex|43315|5|Briefly described|Map Legend|||See also Rock Relationship Diagram and Main Structural Features map.||||||03-MAY-05
9854|Kuark Metamorphic Complex|60541|4|Described|p31, p85, p10|||Comprises an elliptical-shaped region of regionally metamorphosed Pinnak Sst and possibly some Bendoc Gp sediments. The Kuark Met. Belt is in middle of MURRUNGOWAR. Considered to be continuous with Cambalong Met. Complex near Bombala. See also Kuark Mets.||||||20-JUN-05
9854|Kuark Metamorphic Complex|60542|6|Mentioned|p13|||||||||
9854|Kuark Metamorphic Complex|60904|5|Briefly described|p784 Fig. 10|||Of the Lachlan Orogen.||||||
9854|Kuark Metamorphic Complex|61187|5|Briefly described|p6, p5 Fig.3.|Early Silurian|Early Silurian|Kuark Zone. Generated during Benambran Orogeny. Name shortened to Kuark Metamorphics on p.5.||||||
9854|Kuark Metamorphic Complex|61413|6|Mentioned|p2 Fig.1.|||||||||
9854|Kuark Metamorphic Complex|67847|6|Mentioned|p78|||Kuark Zone, Lachlan Orogen. ||||||
9854|Kuark Metamorphic Complex|68116|5|Briefly described|Appendix, Maps 36-37, 45.|Wenlock|Llandovery|Informally subdivided into K-feldspar-silimanite and cordierite-andalusite zones. Most cordierite is replaced by fine aggregates of muscovite, biotite and chlorite.|||||Cordierite-andalusite schist and phyllite with porphyroblasts of andalusite and/or cordierite in a mica/quartz matrix. K-feldspar-sillimanite schist, gneiss and minor migmatite with biotite, sillimanite, K-feldspar, quartz, cordierite, plagioclase.|
9879|Kullatine Formation|22736|6|Mentioned|p625,8|Namurian|Visean|||||||
9879|Kullatine Formation|22857|4|Described|p514 App.1 Tb.A1.8|Namurian|Namurian|Pebbly mudstone, conglomerate, lithic arenite, mudstone, red diamictite. Max. thickness: 1370m.||||||
9879|Kullatine Formation|23720|5|Briefly described|Map Legend|||Siltstone, lithic sandstone, diamictite and conglomerate.||||||15-DEC-04
9879|Kullatine Formation|24124|5|Briefly described|p3|||||||||
9879|Kullatine Formation|24603|5|Briefly described|p897 Fig. 17|Namurian|Namurian|Geological Province: Tamworth Belt.  In the Northern Hastings Block.||||||
9879|Kullatine Formation|29990|6|Mentioned|Map legend|Early Permian|Early Permian|Upper Carboniferous||||||
9879|Kullatine Formation|30340|6|Mentioned|p2530|||Lithology||||||
9879|Kullatine Formation|30341|4|Described|p139|||||||||
9879|Kullatine Formation|30668|6|Mentioned|p582|||Occurrence of Septatopora pustulosa (Crockford).||||||
9879|Kullatine Formation|30772|6|Mentioned|p6|||Fauna||||||
9879|Kullatine Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
9879|Kullatine Formation|31802|6|Mentioned|p143|||U.Carboniferous. Unconformity||||||
9879|Kullatine Formation|31806|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
9879|Kullatine Formation|32094|6|Mentioned|p383|||||||||
9879|Kullatine Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
9879|Kullatine Formation|32672|6|Mentioned|p676|||||||||
9879|Kullatine Formation|32867|6|Mentioned|p21|||||||||
9879|Kullatine Formation|33002|6|Mentioned|p420|||Tectonic history||||||
9879|Kullatine Formation|33992|6|Mentioned|p238|||M.Carb.  See also P239||||||
9879|Kullatine Formation|34085|6|Mentioned|Cor.chart|||Nam. - Steph.||||||
9879|Kullatine Formation|34293|1|Redefined|p45|Carboniferous|Carboniferous|||||||
9879|Kullatine Formation|35129|6|Mentioned|p49|||||||||
9879|Kullatine Formation|35862|6|Mentioned|p277|||||||||
9879|Kullatine Formation|36253|6|Mentioned|p130|||||||||
9879|Kullatine Formation|36528|6|Mentioned|p180|||||||||
9879|Kullatine Formation|36961|6|Mentioned|Fig.5|||||||||
9879|Kullatine Formation|37919|6|Mentioned|p476|||||||||
9879|Kullatine Formation|38685|6|Mentioned|p27|||||||||
9879|Kullatine Formation|38803|5|Briefly described|p107|||||||||
9879|Kullatine Formation|38916|6|Mentioned|p347|||||||||
9879|Kullatine Formation|39299|6|Mentioned|p277|||Diamictites||||||
9879|Kullatine Formation|40883|6|Mentioned|p2|||||||||
9879|Kullatine Formation|41347|4|Described|Table 5|||||||||
9879|Kullatine Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|||||||16-DEC-04
9879|Kullatine Formation|42547|4|Described|p39|||||||||
9879|Kullatine Formation|43755|6|Mentioned|Fig.1,p548||Carboniferous|||||||
9879|Kullatine 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.||||||
9879|Kullatine Formation|44450|4|Described|p24 Table 5|Late Carboniferous|Late Carboniferous|[Of Youdale Formation]. Indexing error: KF is overlain by Youdale Formation, and overlies Majors Creek Formation. Geological Province: Hastings Block.||||||29-JAN-14
9879|Kullatine Formation|45097|6|Mentioned|p27|||Brachiopods & correlation. Correlation chart.||||||
9879|Kullatine Formation|47056|6|Mentioned|Fig.2 P523|||||||||
9879|Kullatine Formation|47059|5|Briefly described|p145|||||||||
9879|Kullatine Formation|63832|5|Briefly described|p131 fig 2, p134|Serpukhovian|Serpukhovian|Voisey (1939); Lindsay (1966); Bourke (1971). Northern Hastings Block, Southern New England Fold Belt. Second Paleozoic glaciation (C2).|||||Dominated by thick intervals of probable marine diamictites with striated and faceted clasts, with local interbedded sandstones and conglomerates. Includes continental coal-bearing successions deposited between P1 and P2 glaciations.|13-DEC-17
9879|Kullatine Formation|64631|5|Briefly described|p44 Fig.2, p47.|Serpukhovian|Serpukhovian|Southern New England Fold Belt: northern Hastings Block. Biostratigraphic age control for base and top.||||Overlies Majors Creek Formation. Is overlain by Youdale Formation.|Thick intervals of probable marine diamictites.|
9879|Kullatine Formation|65107|5|Briefly described|p288, 289, Fig 11 p286-7|Namurian|Namurian|Hastings Block. Namurian age. Shows the rotation of 130-150 degrees (from paleomag) compared with the northwestern Tamworth Belt, or alternatively c.f. Australian craton.||||||
9879|Kullatine Formation|65382|5|Briefly described|p714|Serpukhovian|Serpukhovian|Shown as Youdale C/Kullatine Formation [presumably some combination of Youdale Formation and Kullatine Formation]. Radiometric age of ~323 Ma given (from personal communication with J. Roberts and J. C. Claoue-Long, 2008), and late Arnsbergian (320 Ma) fossils (after Roberts et al., 1993). See also Youdale Formation p717 App. 2. ||||||
9879|Kullatine Formation|70939|5|Briefly described|p823, p826, p828-829|Carboniferous|Carboniferous|Youngest Carboniferous sequence in the Hastings Block.|c.320 Ma.|||||
9879|Kullatine Formation|73487|6|Mentioned|p574 Fig.8, p585|Namurian|Namurian|||||||
9886|Kulnura Marine Tongue|22578|4|Described|Fig.7p397, p396|||of Illawarra Coal Measures||||||
9886|Kulnura Marine Tongue|22857|5|Briefly described|p264, p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Tomago Coal Measures. Bioturbated and burrowed siltstone and sandstone. Age: 256Ma. Max. thickness: 160m. Geological Province: Sydney and Gunnedah Basins.||||||
9886|Kulnura Marine Tongue|22969|5|Briefly described|p 24|||||||||
9886|Kulnura Marine Tongue|29900|4|Described|p173|||||||||
9886|Kulnura Marine Tongue|29901|4|Described|Table 1|||||||||
9886|Kulnura Marine Tongue|30006|4|Described|p8|||||||||
9886|Kulnura Marine Tongue|31128|6|Mentioned|Table 1|||||||||
9886|Kulnura Marine Tongue|36009|6|Mentioned|Table 1|||||||||
9886|Kulnura Marine Tongue|36042|6|Mentioned|Fig.7|||||||||
9886|Kulnura Marine Tongue|36220|6|Mentioned|p38|||See also Table 10.||||||
9886|Kulnura Marine Tongue|38615|6|Mentioned|p25|||||||||
9886|Kulnura Marine Tongue|39268|6|Mentioned|Fig. 5|||||||||
9886|Kulnura Marine Tongue|39287|6|Mentioned|p33|||||||||
9886|Kulnura Marine Tongue|39299|6|Mentioned|p288|||||||||
9886|Kulnura Marine Tongue|39308|6|Mentioned|p494|||See also Fig.23.12. Cored ddh||||||
9886|Kulnura Marine Tongue|39309|6|Mentioned|p125|||||||||
9886|Kulnura Marine Tongue|40256|6|Mentioned|p303|||||||||
9886|Kulnura Marine Tongue|40602|6|Mentioned|p7|||||||||
9886|Kulnura Marine Tongue|40631|6|Mentioned|p161|||||||||
9886|Kulnura Marine Tongue|42284|6|Mentioned|p106|||||||||
9886|Kulnura Marine Tongue|42787|6|Mentioned|Table 1 P126|||||||||
9886|Kulnura Marine Tongue|43194|5|Briefly described|p110, p129 Tb. 8.3|Late Permian|Late Permian|A lithofacies correlative of the Arkarula Sandstone Member (now Arkarula Formation) of the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
9886|Kulnura Marine Tongue|44244|6|Mentioned|p276|||Geological Province: Sydney Basin.||||||
9886|Kulnura Marine Tongue|45090|6|Mentioned|p27|||Relationship of rock units||||||
9886|Kulnura Marine Tongue|60281|4|Described|p9, p61|Late Permian|Late Permian|At top of Wallis Creek Formation.  Marine transgression associated with the Tomago and Newcastle Coal Measures.  Consists of dark grey to black bioturbated, fossiliferous marine siltstone and sandstone.   Max. thickness: ~160m.  Geol.Prov: Sydney Basin.||||||
9886|Kulnura Marine Tongue|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Marine incursion into Late Permian coal measures - offers good hydrocarbon source potential. Appears in both the Tomago Coal Measures and Wittingham Coal Measures (within the Vane Subgroup). Geological Province: Sydney Basin.||||||
9886|Kulnura Marine Tongue|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Late Permian.||Of the Tomago Coal Measures.||||
9886|Kulnura Marine Tongue|68003|5|Briefly described|p41.|Late Permian|Late Permian|Sydney Basin. Has lateral equivalents in the Bulga and Archerfield Formations (northern Sydney Basin), the Erins Vale Formation (southern Sydney Basin), and the Arkarula Formation (Mullaley Sub-basin, Gunnedah Basin).||||||
9886|Kulnura Marine Tongue|68004|6|Mentioned|p23 Table 1. |||Newcastle Coalfield.||Unit in Tomago Coal Measures.||||
9886|Kulnura Marine Tongue|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Wallis Creek Subgroup|||Siltstone, mudstone and claystone; sporadic fossil, dropstones and glendonites.|
9886|Kulnura Marine Tongue|73421|6|Mentioned|p16, p18|Capitanian|Capitanian|Sydney Basin, southern. Misspelt as Kulinura p16.||Erins Vale Formation|||Contains glendonites.|
9906|Kunderang Brook Limestone|29990|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
9924|Kurool Formation|34109|4|Described|p159|||See also P160||||||
9925|Kurrajong Park Formation|13996|6|Mentioned|p139|||Manildra, western Cowra Trough. Contains a small fauna of late Wenlock brachiopods.||||||
9925|Kurrajong Park Formation|22857|5|Briefly described|p458 App.1, Tb.A1.6|Silurian|Silurian|Of the Cudal Group. Coarse lithic arenite, siltstone, shale and chert. Max. thickness: 392m. Geological Province: Cowra Trough. ||||||
9925|Kurrajong Park Formation|23214|3|Fully described|p122|Wenlock|Wenlock|Of Cudal Group. Originally defined by Savage 1969 (a). 362m thick at type section. Interbedded grey to brown and black siltstone and fine to coarse grained lithic sandstone with minor shale and siliceous sandstone.||||||
9925|Kurrajong Park Formation|31852|6|Mentioned|p718|||Fig.||||||
9925|Kurrajong Park Formation|32986|6|Mentioned|p4|||Brachiopods & graphtolites||||||
9925|Kurrajong Park Formation|33116|6|Mentioned|Fig.12|||Correlation||||||
9925|Kurrajong Park Formation|33121|6|Mentioned|p85|||Late Sil. Correlation table.||||||
9925|Kurrajong Park Formation|37727|4|Described|p67|||||||||
9925|Kurrajong Park Formation|40328|3|Fully described|p82|||Also mentioned on p81.||||||23-SEP-18
9925|Kurrajong Park Formation|43494|6|Mentioned|p19|Silurian|Silurian|||||||16-MAR-06
9925|Kurrajong Park Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
9925|Kurrajong Park Formation|43782|5|Briefly described|Map Legend|Wenlock|Wenlock|of Cudal Group.||||||
9925|Kurrajong Park Formation|63290|5|Briefly described|p393 Tb. 1, p397 Fig. 3(b)|Wenlock|Wenlock|Age: 425-423Ma. Geological Province: Molong Volcanic Belt. Contains arc detritus.||||||
9925|Kurrajong Park Formation|70297|5|Briefly described|map legend|Silurian|Silurian|Shown as Kurrajong Park Fm.||Cudal Group||||
9934|Kurri Kurri Conglomerate|22601|6|Mentioned|410|Permian|Permian|Parent Greta Coal Measures. Geol province Sydney Basin||||||
9934|Kurri Kurri Conglomerate|22610|5|Briefly described|Fig 1|||Maximum thickness 43m||||||
9934|Kurri Kurri Conglomerate|22969|4|Described|Fig 4.1a||Early Permian|||||||
9934|Kurri Kurri Conglomerate|23540|5|Briefly described|p 419|||Of the Greta Coal Measures.||||||20-FEB-07
9934|Kurri Kurri Conglomerate|33867|6|Mentioned|p5|||||||||
9934|Kurri Kurri Conglomerate|34015|4|Described|p325|||Permian||||||
9934|Kurri Kurri Conglomerate|37086|6|Mentioned|p185|||||||||
9934|Kurri Kurri Conglomerate|42648|6|Mentioned|p35|||||||||
9934|Kurri Kurri Conglomerate|45090|5|Briefly described|p151|||||||||
9934|Kurri Kurri Conglomerate|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
9934|Kurri Kurri Conglomerate|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Lochinvar area.||Unit in Greta Coal Measures.|Includes Abernethy Lens.|||
9935|Kurrool Formation|22857|5|Briefly described|p492 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Canangle Subgroup (Catombal Group). Fine-grained arenite and red mudstone. Geological Province: Hervey Basin.||||||
9935|Kurrool Formation|23043|5|Briefly described|Map Legend|Famennian|Famennian|of Canangle Subgroup, Catombal Group.||||||
9935|Kurrool Formation|23170|2|Defined|p253|Late Carboniferous||of Canangle Subgroup.||||||
9935|Kurrool Formation|24247|5|Briefly described|p37|Late Devonian|Late Devonian|Parent: Canangle Subgroup (Catombal Group)||||||
9935|Kurrool Formation|32151|6|Mentioned|p218|||Refers Conolly (1963)||||||
9935|Kurrool Formation|32708|6|Mentioned|Fig.6|||||||||
9935|Kurrool Formation|33732|4|Described|p120|||See also P119.||||||
9935|Kurrool Formation|33871|6|Mentioned|p2531|||||||||
9935|Kurrool Formation|43509|14|Not recorded|p113,Pl.I||Late Devonian|Unit of Catombal Group||||||
9935|Kurrool Formation|43512|2|Defined|p73,77-8,85,88-91,96||Late Devonian|Conformably o/lies Macquarie Park Ss,conformably u/lies Curra Creek Conglomerate.p98-101,104,106||||||
9935|Kurrool Formation|43513|14|Not recorded|p72|||||||||
9935|Kurrool Formation|68003|5|Briefly described|p24 Fig.3-e, p141. |Frasnian|Frasnian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Canangle Subgroup.||Overlies Black Rock Subgroup. Is overlain by Curra Creek Conglomerate.|Red siltstone, minor sandstone and conglomerate.|
9935|Kurrool Formation|71600|5|Briefly described|p23 Fig 1|Devonian|Devonian|Geological province: Lachlan Fold Belt.||Unit of Catombal Group.|||Red siltstone, minor sandstone and conglomerate|
9935|Kurrool Formation|73299|6|Mentioned|p1105|Late Devonian|Late Devonian|||Catombal Group||Overlies the Black Rock Subgroup, underlies the Curra Creek Conglomerate.||
9951|Kuttung Formation|22757|4|Described|Table4,p10|Carboniferous|Late Devonian|Conformable on Texas Beds. Unconformably underlies Back Creek Group.||||||
9951|Kuttung Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
9951|Kuttung Formation|29721|6|Mentioned|p267|||||||||
9951|Kuttung Formation|30692|6|Mentioned|Map legend|Late Carboniferous|Early Carboniferous|Lower to Upper Carboniferous||||||
9951|Kuttung Formation|30699|6|Mentioned|p55|||||||||
9951|Kuttung Formation|30701|6|Mentioned|Map legend|Carboniferous|Late Devonian|Upper Devonian to Upper Carboniferous||||||
9951|Kuttung Formation|31118|6|Mentioned|Fig. 4|||||||||
9951|Kuttung Formation|32276|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|Upper Devonian? to Upper? Carboniferous. Prob.Upper Carboniferous||||||
9951|Kuttung Formation|33091|5|Briefly described|p6|||Stratigraphy||||||
9951|Kuttung Formation|33451|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
9951|Kuttung Formation|34613|6|Mentioned|Table 3|||||||||
9951|Kuttung Formation|39907|6|Mentioned|Fig.3|||||||||
9951|Kuttung Formation|42634|5|Briefly described|p8|||||||||
9951|Kuttung Formation|43000|5|Briefly described|p106|||||||||
9951|Kuttung Formation|43003|5|Briefly described|p168|||||||||
9951|Kuttung Formation|43008|5|Briefly described|map legend|||||||||
9951|Kuttung Formation|43925|14|Not recorded|p30,32,Fig.3|||||||||
9951|Kuttung Formation|44163|14|Not recorded|p11|||||||||
9951|Kuttung Formation|44166|14|Not recorded|p1,10,15,Pl.1||Carboniferous|K-Ar: 300+/- 10 Ma.||||||
9951|Kuttung Formation|44567|14|Not recorded|p10-17|||Not shown on white card.||||||
9951|Kuttung Formation|44585|14|Not recorded|p45-Fig.2|||||||||
9951|Kuttung Formation|44627|14|Not recorded|p139-143|Early Permian|Devonian|Unit of Horton Gruop.||||||
9951|Kuttung Formation|48600|14|Not recorded|p3-7,24|Early Permian|Carboniferous|Formation of Horton Group.||||||
9951|Kuttung Formation|61377|5|Briefly described|p150|Early Permian|Late Carboniferous|Sequence of marine to non-marine andesitic volcanics and volcaniclastics. Limited reservoir potential. Unconformably overlain by the Back Creek Group. Geological Province: Surat, Gunnedah and Bowen Basins.||||||07-FEB-11
9951|Kuttung Formation|67669|5|Briefly described|p11-12,22-23|Late Carboniferous|Late Carboniferous|Of Bowen Basin. Part of the basement assemblage to the Bowen Basin. Also known as Cracow Formation. Intersected in inglestone-1 borehole at 3.8 km depth, as modelled on Line 270.||||Overlain by, and laterally grades into Timbury Hills Formation. Also overlain by Camboon and Connors volcanics.||
9966|Kyambra Granodiorite|40328|4|Described|p208|||||||||
9966|Kyambra Granodiorite|45003|14|Not recorded|p37|||||||||
9979|Kyndalyn Mudstone Member|32286|3|Fully described|p50|||||||||
9979|Kyndalyn Mudstone Member|37987|2|Defined|p229|late Visean|late Visean|||||||
9979|Kyndalyn Mudstone Member|38222|6|Mentioned|Fig.2|||||||||
9979|Kyndalyn Mudstone Member|42547|4|Described|p21|||of Merlewood Formation.||||||
9979|Kyndalyn Mudstone Member|66720|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|||Unit in Merlewood Formation.|||Well-bedded mudstone with subordinate siltstone.|
9979|Kyndalyn Mudstone Member|68003|5|Briefly described|p135.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Merlewood Formation.|||Contains ignimbrite and limestone lenses.|
9979|Kyndalyn Mudstone Member|68005|5|Briefly described|p141.|Visean|Visean|||Unit in Merlewood Formation.|||Ignimbrite.|
9979|Kyndalyn Mudstone Member|70050|5|Briefly described|p334, p347-348, p355, p358, p364-365|Visean|Visean|Babbinboon area. Contains Cionodendron voiseyi and Australastraea coral fossils (illustrations and systematic palaeontology). ||Merlewood Formation.||Correlated biostratigraphically with Lion Creek Limestone and upper part of Cannindah Limestone.||
